{"meta":{"query_hash":"96c101101a1b","filters":{"venue":"Canadian Journal of Earth Sciences"},"cohort_total":2460,"direct_labels_cover":2,"predictions_cover":2460,"exported":2460,"export_cap":100000,"truncated":false,"label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12"},"permalink":"https://metacan.xera.ac/q/96c101101a1b","api":"https://metacan.xera.ac/api/v1/cohort?venue=Canadian+Journal+of+Earth+Sciences"},"results":[{"id":"W11542012","doi":"10.1139/e85-209","title":"Disaster Resistant Communities Initiative: Assessment Of The Pilot Phase - Year 3","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evaluation and Performance Assessment","field":"Decision Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Federal Emergency Management Agency","keywords":"General partnership; Program evaluation; Impact assessment; Public relations; Political science; Environmental planning; Environmental resource management; Engineering; Geography; Public administration","score_opus":0.4214026578139658,"score_gpt":0.4794232770345788,"score_spread":0.05802061922061302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W11542012","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9417146,0.00019001648,0.00012420594,0.0036853817,0.00066285237,0.0000872536,0.00003755504,0.0000013198774,0.053496804],"genre_scores_gemma":[0.9979767,0.000019411344,0.00071622804,0.000529826,0.00005121962,7.885349e-7,2.2911587e-7,0.0000025026504,0.0007030517],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971052,0.00042809683,0.00066284847,0.0000880292,0.0014981941,0.0002176623],"domain_scores_gemma":[0.9978341,0.00048058853,0.0006118566,0.00028615497,0.00054700667,0.00024030288],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0049115825,0.000078682,0.00019407136,0.00038590745,0.00055963936,0.00029565903,0.0012084948,0.000019157049,0.00726345],"category_scores_gemma":[0.00043702833,0.000042391322,0.00009203504,0.00088408805,0.00095831254,0.0006351805,0.000033333057,0.00019000676,0.000024233685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004042052,0.0003225907,0.9087098,0.00001487271,0.00006709902,0.000022830136,0.024143126,0.0031227246,0.0008735666,0.026119174,0.019380301,0.017183486],"study_design_scores_gemma":[0.0019306008,0.0032571785,0.81728023,0.00023610765,0.00003179115,0.0000473069,0.045976836,0.0129610235,0.00040271177,0.0059363027,0.11167917,0.00026073493],"about_ca_topic_score_codex":0.00055870775,"about_ca_topic_score_gemma":0.05220498,"teacher_disagreement_score":0.092298865,"about_ca_system_score_codex":0.000014068719,"about_ca_system_score_gemma":0.0016158826,"threshold_uncertainty_score":0.99364406},"labels":[],"label_agreement":null},{"id":"W1239552352","doi":"10.1139/e2012-049","title":"Discussion of the reply by R.L. Romer and U. Kroner on “Geochemical signature of Ordovician Mn-rich sedimentary rocks on the Avalonian shelf” <sup>1</sup>Appears in Canadian Journal of Earth Sciences, <b>49</b>(6): 775–780, 10.1139/e2012-006.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University; Nova Scotia Department of Energy; Technical University of Nova Scotia; University of Alberta","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Zircon; Ordovician; Sedimentary depositional environment; Provenance; Sedimentary rock; Paleontology; Laurentia; Geochronology; Geochemistry; Detritus; Structural basin","score_opus":0.008532535409212342,"score_gpt":0.19349626503244435,"score_spread":0.18496372962323201,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1239552352","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98842275,0.0019619593,5.3633795e-7,0.006185838,0.00023366189,0.00011389829,0.00020607795,0.0000011497527,0.0028741548],"genre_scores_gemma":[0.99853164,0.000032485554,0.00007183269,0.00080419425,0.00014165553,2.9893877e-7,0.000009317113,0.0000041136577,0.00040446554],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9969829,0.00024235134,0.0007423357,0.00025379975,0.00092141225,0.00085722696],"domain_scores_gemma":[0.99769926,0.00019390842,0.0006246215,0.0002216058,0.00013115875,0.0011294656],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0028276287,0.00023431369,0.00039610334,0.0004995833,0.0007705042,0.00012071021,0.0010405409,0.00011719521,0.0027357626],"category_scores_gemma":[0.0002841751,0.00011560225,0.0001725968,0.0013455766,0.001552764,0.00054184784,0.000020195044,0.0006302398,0.000009888081],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003013347,0.000033260963,0.98763096,0.00001476355,0.00003984129,0.00001614739,0.0013963461,0.0054180454,0.00065319036,0.00002053792,0.0035232136,0.0012235476],"study_design_scores_gemma":[0.00091874495,0.0018527963,0.90252054,0.0009537335,0.00017696418,0.0003515775,0.010755861,0.0017405098,0.021781309,0.0005100765,0.057807907,0.0006299931],"about_ca_topic_score_codex":0.13138916,"about_ca_topic_score_gemma":0.5278473,"teacher_disagreement_score":0.39645815,"about_ca_system_score_codex":0.000013935776,"about_ca_system_score_gemma":0.001952251,"threshold_uncertainty_score":0.99817586},"labels":[],"label_agreement":null},{"id":"W1241273620","doi":"10.1139/e2012-017","title":"U–Pb zircon age of an Ordovician tuff in southeast Yukon: implications for the age of the Cambrian–Ordovician boundary<sup>1</sup>Yukon Geological Survey Contribution 013.<sup>2</sup>Geological Survey of Canada Earth Science Sector (ESS) Contribution 20110362.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geoscience BC; Yukon University; Geological Survey of Canada","funders":"","keywords":"Geology; Ordovician; Conodont; Zircon; Rhyolite; Paleontology; Volcanic rock; Unconformity; Sedimentary depositional environment; Geochemistry; Volcano; Biostratigraphy; Sedimentary rock","score_opus":0.02944808935964342,"score_gpt":0.22887035376010328,"score_spread":0.19942226440045988,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1241273620","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99467444,0.00094460713,0.00027011914,0.0012671951,0.00022752986,0.0004561211,0.0019125468,0.000004413861,0.00024300584],"genre_scores_gemma":[0.99916136,0.000023378576,0.00021961509,0.00026218715,0.00010512896,0.0000032355363,0.00019501391,0.000003231607,0.000026827696],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.995321,0.0009900301,0.0011810482,0.00042688975,0.00081242924,0.0012686471],"domain_scores_gemma":[0.99506843,0.0016231297,0.0007981541,0.0004021804,0.0012485941,0.00085951],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0092028,0.00028318382,0.0007863667,0.00032063207,0.00113855,0.00012290932,0.0016784874,0.00018526528,0.000734953],"category_scores_gemma":[0.0050707026,0.00015804847,0.0002211115,0.0026260717,0.0043307603,0.00054403767,0.000051885898,0.00045383922,0.000003211913],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007186156,0.000049281614,0.98497236,0.000007888637,0.00002598107,0.000005428834,0.00017080661,0.013155543,0.00053123944,0.00061002205,0.000019479812,0.00038008436],"study_design_scores_gemma":[0.00040088475,0.0004284614,0.98932165,0.00003763279,0.00004608793,0.000034756693,0.00051006844,0.007211344,0.0003950303,0.00091797404,0.00049269915,0.00020339299],"about_ca_topic_score_codex":0.7987978,"about_ca_topic_score_gemma":0.99358356,"teacher_disagreement_score":0.19478576,"about_ca_system_score_codex":0.000026870986,"about_ca_system_score_gemma":0.0034479273,"threshold_uncertainty_score":0.9983789},"labels":[],"label_agreement":null},{"id":"W1481175427","doi":"10.1139/e10-032","title":"Lifetime of an ocean island volcano feeder zone: constraints from U–Pb dating on coexisting zircon and baddeleyite, and <sup>40</sup>Ar/<sup>39</sup>Ar age determinations, Fuerteventura, Canary IslandsThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Baddeleyite; Zircon; Geology; Amphibole; Geochemistry; Magma; Mafic; Plagioclase; Mineralogy; Volcano; Quartz; Paleontology","score_opus":0.017775040350818432,"score_gpt":0.19162307937313966,"score_spread":0.17384803902232124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1481175427","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931413,0.00025223166,0.000001112866,0.0004986483,0.000030084651,0.000099939236,0.0002944604,0.0000011608905,0.0056810537],"genre_scores_gemma":[0.99883497,0.000047205842,0.0008650335,0.00013906874,0.00006702671,2.4000755e-7,0.000011196722,0.0000019776633,0.000033287433],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981707,0.00019683292,0.0007595939,0.0002449966,0.00032172553,0.00030618804],"domain_scores_gemma":[0.9984847,0.00045187646,0.00055503123,0.00013622823,0.00014104575,0.00023112819],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010733966,0.00014942282,0.00052201207,0.00035756352,0.000120292214,0.000032761527,0.00036283513,0.00009198132,0.012774932],"category_scores_gemma":[0.00057496433,0.0001005874,0.00006716554,0.00056406984,0.0017132864,0.0003611794,0.000019585039,0.00023769471,9.3620275e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016144724,0.00007990106,0.9750255,0.000040027935,0.00006306456,0.00005501402,0.010105104,0.0010066672,0.0018452351,0.00008261683,0.000112219124,0.011423226],"study_design_scores_gemma":[0.0009824086,0.0020600408,0.9515248,0.0005130278,0.00007351597,0.000049435996,0.01547649,0.007869861,0.018156795,0.0028718535,0.00015653348,0.00026523473],"about_ca_topic_score_codex":0.08290988,"about_ca_topic_score_gemma":0.29086673,"teacher_disagreement_score":0.20795685,"about_ca_system_score_codex":0.0000035829662,"about_ca_system_score_gemma":0.0003194714,"threshold_uncertainty_score":0.9881275},"labels":[],"label_agreement":null},{"id":"W1547289598","doi":"10.1139/e09-076","title":"How the crust meets the mantle: Lithoprobe perspectives on the Mohorovičić discontinuity and crust–mantle transitionThis article is one of a series of papers published in this Special Issue on the theme <i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Geological Survey of Canada; University of British Columbia; Memorial University of Newfoundland","funders":"","keywords":"Crust; Geology; Mantle (geology); Discontinuity (linguistics); Lithosphere; Tectonics; Oceanic crust; Geophysics; Seismology; Transect; Continental crust; Subduction","score_opus":0.009757262496140943,"score_gpt":0.18099052039585128,"score_spread":0.17123325789971033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1547289598","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93524694,0.00085491076,0.0000020993762,0.060794085,0.00021768094,0.00039337703,0.00012608996,0.0000013430838,0.0023634504],"genre_scores_gemma":[0.9992243,0.00014133462,0.0000674429,0.00022878083,0.00022558888,0.0000027848378,4.7604928e-7,0.0000024846236,0.00010681879],"study_design_codex":"qualitative","study_design_gemma":"observational","domain_scores_codex":[0.9985318,0.00029304053,0.0003262187,0.00017829797,0.00042199806,0.00024862957],"domain_scores_gemma":[0.9984366,0.0006456275,0.00041165247,0.00022312572,0.00018875429,0.000094212846],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0026701214,0.00012881863,0.0002747394,0.00008062793,0.00049835484,0.00036327183,0.00053700316,0.000044501463,0.0013053188],"category_scores_gemma":[0.00055524224,0.00004733608,0.00006699905,0.0004180107,0.0030968678,0.00043281747,0.000012577878,0.00025653667,7.5933485e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0034100926,0.00047942818,0.17844902,0.0005360833,0.00076824677,0.000041339976,0.49316615,0.0010033385,0.044192176,0.25162184,0.011056493,0.015275804],"study_design_scores_gemma":[0.0020494268,0.0018358115,0.7517113,0.00064241653,0.00026394526,0.00009998571,0.14414416,0.00069193833,0.053672444,0.022853162,0.02152559,0.0005098411],"about_ca_topic_score_codex":0.018003175,"about_ca_topic_score_gemma":0.20843652,"teacher_disagreement_score":0.5732623,"about_ca_system_score_codex":0.0000021969527,"about_ca_system_score_gemma":0.00043164266,"threshold_uncertainty_score":0.99961615},"labels":[],"label_agreement":null},{"id":"W1568063242","doi":"10.1139/e10-034","title":"Neoproterozoic extension in the Greater Dharwar Craton: a reevaluation of the “Betsimisaraka suture” in MadagascarThis article is one of a series of papers published in this Special Issue on the theme of<i>Geochronology</i>in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Gneiss; Archean; Geochemistry; Dharwar Craton; Metamorphism; Craton; Anatexis; Precambrian; Schist; Felsic; Mafic; Orogeny; Igneous rock; Petrology; Crust; Metamorphic rock; Paleontology; Partial melting; Tectonics","score_opus":0.03727593691791558,"score_gpt":0.19775385869800835,"score_spread":0.16047792178009276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1568063242","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912784,0.00028520884,1.831502e-7,0.005004341,0.00007345241,0.00015749394,0.000018150335,3.9852833e-7,0.0031823642],"genre_scores_gemma":[0.99952376,0.000031618514,0.00012589555,0.00025020025,0.000044577348,6.6295814e-7,7.1414917e-7,9.128961e-7,0.000021650132],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980551,0.00038691238,0.0006996854,0.00016026077,0.0004408646,0.00025718796],"domain_scores_gemma":[0.99895054,0.00018355034,0.0004638002,0.00019499761,0.00013675021,0.00007037863],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0025506,0.000099629135,0.00036382797,0.00031315367,0.000055565182,0.0000142548115,0.00064045185,0.0000740513,0.013506855],"category_scores_gemma":[0.0005071314,0.000046690388,0.0001149624,0.0013263999,0.0009817542,0.00022532229,0.00001495792,0.00025452144,0.0000021287904],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011511827,0.00004913706,0.9869622,0.000014588723,0.00001165275,0.000011521223,0.007724855,0.0008430621,0.0016973072,0.000117027,0.000062057836,0.0023914943],"study_design_scores_gemma":[0.0002329533,0.00043844216,0.9656462,0.0001409001,0.000013356557,0.000008780745,0.0026685495,0.00032835064,0.025730934,0.0046647373,0.00007400088,0.00005279834],"about_ca_topic_score_codex":0.048588783,"about_ca_topic_score_gemma":0.4987566,"teacher_disagreement_score":0.4501678,"about_ca_system_score_codex":0.000003418368,"about_ca_system_score_gemma":0.00032334847,"threshold_uncertainty_score":0.9873949},"labels":[],"label_agreement":null},{"id":"W1611367146","doi":"10.1139/e2012-038","title":"The northernmost occurrence of <i>Prognathodon</i> (Squamata: Mosasauridae) from the Western Interior Seaway of North America","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Squamata; Cretaceous; Range (aeronautics); Genus; Paleontology; Geology; Geography; Zoology; Biology","score_opus":0.024281111052130804,"score_gpt":0.22467649391525601,"score_spread":0.20039538286312522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1611367146","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98633933,0.010455139,0.000046817935,0.0009562234,0.001032078,0.00006396882,0.00048033413,0.0000016571425,0.0006244283],"genre_scores_gemma":[0.99913484,0.00018151086,0.00022213577,0.00027913545,0.00014759772,2.3275247e-7,0.00001039178,8.4919463e-7,0.00002333537],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985824,0.00024261326,0.0004128204,0.00010836136,0.00022480813,0.0004289907],"domain_scores_gemma":[0.9981741,0.0007580902,0.00049030635,0.00015511981,0.00011613687,0.00030628365],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009651563,0.00010125839,0.00021551535,0.0000656873,0.00057791924,0.000027921844,0.0009309164,0.000041275667,0.00022779327],"category_scores_gemma":[0.00021263424,0.000051225546,0.00008272084,0.0003543906,0.0024935636,0.00034803717,0.0000103613775,0.00019686486,0.000027710399],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015906617,0.00000336299,0.98496455,0.0000019328645,0.00001749209,0.0000037443058,0.00072891347,0.00013061099,0.000008502153,0.00000948604,0.000273197,0.013842328],"study_design_scores_gemma":[0.00006877839,0.00020503008,0.9718249,0.000022736918,0.000014910037,0.000053909516,0.0005409591,0.00007847427,0.00003499055,0.000038872262,0.027053727,0.00006273679],"about_ca_topic_score_codex":0.023639418,"about_ca_topic_score_gemma":0.7044734,"teacher_disagreement_score":0.680834,"about_ca_system_score_codex":0.0000014231966,"about_ca_system_score_gemma":0.00078746054,"threshold_uncertainty_score":0.98286223},"labels":[],"label_agreement":null},{"id":"W1616071577","doi":"10.1139/cjes-2014-0028","title":"New information on the rare horned dinosaur<i>Arrhinoceratops brachyops</i>(Ornithischia: Ceratopsidae) from the Upper Cretaceous of Alberta, Canada","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; University of Calgary; University of Alberta; Canadian Museum of Nature","funders":"","keywords":"Geology; Paleontology; Cretaceous; Holotype; Skull; Canyon; Quadrate bone; Biology; Taxonomy (biology); Zoology; Geomorphology","score_opus":0.008556516926163098,"score_gpt":0.17204599327482017,"score_spread":0.16348947634865707,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1616071577","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9688768,0.00096492685,0.000049807208,0.014797864,0.0011125607,0.000082763654,0.00008472171,0.000001946327,0.014028643],"genre_scores_gemma":[0.99522907,0.000016451084,0.0001674028,0.004221039,0.00022673866,1.6625494e-7,0.000014646666,9.899652e-7,0.00012347854],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99864066,0.00025976764,0.00036271027,0.00011285266,0.0002865686,0.00033745362],"domain_scores_gemma":[0.9978653,0.0011970733,0.00031670916,0.00016039345,0.000105790845,0.00035473297],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000713217,0.00012178188,0.00018893223,0.0000883913,0.0007473982,0.000081860584,0.00072381564,0.000079493344,0.002391646],"category_scores_gemma":[0.000568747,0.00006241638,0.0000636696,0.00028786017,0.0004770347,0.00043732818,0.0000049069545,0.00030650233,0.000045548702],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020215384,0.0000010080494,0.98408496,0.0000012172997,0.00002008198,0.000004473914,0.0006181731,0.0015068772,0.0000025502113,0.00064579427,0.008913343,0.004181278],"study_design_scores_gemma":[0.00012758456,0.00017932257,0.90000165,0.000020517675,0.000012705266,0.00008308686,0.0004819292,0.00077323127,0.000051845454,0.0008319198,0.097352244,0.00008399911],"about_ca_topic_score_codex":0.9165889,"about_ca_topic_score_gemma":0.9986922,"teacher_disagreement_score":0.0884389,"about_ca_system_score_codex":0.000004042628,"about_ca_system_score_gemma":0.0041689225,"threshold_uncertainty_score":0.9985203},"labels":[],"label_agreement":null},{"id":"W1619153954","doi":"10.1139/e09-031","title":"Volcanic reconstruction of Paleoproterozoic arc volcanoes: the Hidden and Louis formations, Flin Flon, Manitoba, CanadaThis is a companion paper to DeWolfe, Y.M., Gibson, H.L., and Piercey, S.J. 2009. Petrogenesis of the 1.9 Ga mafic hanging wall sequence to the Flin Flon, Callinan, and Triple 7 massive sulphide deposits, Flin Flon, Manitoba, Canada. Canadian Journal of Earth Sciences, <b>46</b>: this issue.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Mount Royal University; Laurentian University; Geoscience BC; Manitoba Hydro","funders":"","keywords":"Geology; Lava; Mafic; Volcano; Petrogenesis; Sill; Geochemistry; Pyroclastic rock; Volcanism; Petrology; Basalt; Volcanic rock; Seismology; Tectonics","score_opus":0.016740980092795055,"score_gpt":0.19017558594014924,"score_spread":0.17343460584735418,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1619153954","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97487086,0.0055070687,0.000031776173,0.018454585,0.00038102598,0.00036774608,0.00027846836,0.0000023375922,0.00010616037],"genre_scores_gemma":[0.9959186,0.0002993025,0.0012807224,0.0022684857,0.0001438846,0.0000014219612,0.0000042644015,0.00000431586,0.00007901771],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9966168,0.00028110904,0.0010688839,0.00037906424,0.00085162476,0.00080253935],"domain_scores_gemma":[0.99685884,0.00021907831,0.00073558645,0.0002635485,0.0006535165,0.0012694617],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0019105164,0.00030327993,0.00055597804,0.0005610549,0.0017012204,0.00034175644,0.0011063655,0.000091225804,0.00048364815],"category_scores_gemma":[0.0004934708,0.00017122425,0.0001300658,0.0017315412,0.0011186856,0.000501114,0.000032172007,0.00039539725,0.0000029594453],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041875683,0.000010722857,0.9604791,0.000047056514,0.00009025791,0.000094298775,0.002257127,0.0033479282,0.00077224727,0.00006690417,0.003030906,0.029761571],"study_design_scores_gemma":[0.00035193955,0.0007019097,0.9765459,0.00039295998,0.00018319534,0.0015406213,0.0061111692,0.0038742742,0.0020248499,0.0009313558,0.0069608316,0.00038101283],"about_ca_topic_score_codex":0.9469684,"about_ca_topic_score_gemma":0.99965435,"teacher_disagreement_score":0.052686017,"about_ca_system_score_codex":0.000035870962,"about_ca_system_score_gemma":0.0045570554,"threshold_uncertainty_score":0.99959844},"labels":[],"label_agreement":null},{"id":"W1624418154","doi":"10.1139/e08-054","title":"Late Quaternary paleoceanography and paleo-sea ice conditions in the Mackenzie Trough and Canyon, Beaufort SeaThis article is one of a series of papers published in this Special Issue on the theme <i>Polar Climate Stability Network</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Dalhousie University; Université du Québec à Rimouski; Natural Resources Canada","funders":"Japan Agency for Marine-Earth Science and Technology","keywords":"Geology; Oceanography; Foraminifera; Paleoceanography; Trough (economics); Arctic; Benthic zone; Sea ice; Canyon; Paleontology; Geomorphology","score_opus":0.02717987215841379,"score_gpt":0.22330237373053252,"score_spread":0.19612250157211875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1624418154","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9867912,0.0010030008,7.515629e-8,0.006414178,0.00012247308,0.00015287857,0.00013313629,0.00000113358,0.005381943],"genre_scores_gemma":[0.9985314,0.0007916493,0.000052940173,0.0004991996,0.000104168765,7.1765396e-7,0.0000043179534,0.000001225307,0.000014354014],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982242,0.00042417477,0.00041052638,0.00017293428,0.00029816086,0.000470021],"domain_scores_gemma":[0.99882746,0.00057627726,0.00018783919,0.00014205021,0.00007848523,0.00018791089],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0026935118,0.00010378983,0.0002658459,0.00023834311,0.0004897056,0.000049242717,0.00037183697,0.000069815826,0.00405755],"category_scores_gemma":[0.00016357092,0.000057811656,0.000051164,0.00077745947,0.0026471806,0.00039990887,0.000009749246,0.00034959018,0.0000024269063],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000059273065,0.000012714706,0.99526924,0.000013928193,0.000012515602,0.0000658811,0.0040606675,0.00011815328,0.0000047357003,0.00013454202,0.00019431727,0.000054045366],"study_design_scores_gemma":[0.00022666705,0.00038754195,0.99517953,0.00004493126,0.0000088251545,0.00014793922,0.001605755,0.00017072585,0.00009547281,0.0013905368,0.0006764709,0.00006560396],"about_ca_topic_score_codex":0.010505618,"about_ca_topic_score_gemma":0.6388769,"teacher_disagreement_score":0.6283713,"about_ca_system_score_codex":6.42685e-7,"about_ca_system_score_gemma":0.00039324514,"threshold_uncertainty_score":0.9968529},"labels":[],"label_agreement":null},{"id":"W1641070731","doi":"10.1139/e07-061","title":"Statistical analysis of mixed-motive shell borings in Ordovician, Silurian, and Devonian brachiopods from northern and eastern CanadaThis article is one of a selection of papers published in this Special Issue on the theme<i>The dynamic reef and shelly communities of the Paleozoic. This Special is in honour of our colleague and friend Paul Copper</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Marine Biology and Environmental Chemistry","field":"Engineering","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Ordovician; Paleozoic; Devonian; Trilobite; Paleontology; Geology; Paleoecology; Predation","score_opus":0.008303845277210476,"score_gpt":0.19025738513007032,"score_spread":0.18195353985285984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1641070731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99814314,0.00018681739,6.890275e-7,0.00046437242,0.000044511246,0.00007238077,0.0001806196,4.2872043e-7,0.0009070167],"genre_scores_gemma":[0.99966055,0.00016977388,0.000061403,0.000035103192,0.000040705065,6.1559444e-7,0.000001286954,0.000003574502,0.000026962176],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99905324,0.000110246554,0.0004092695,0.00010073666,0.00017415585,0.00015237887],"domain_scores_gemma":[0.9993853,0.0002100395,0.00019243032,0.00009722979,0.000033813147,0.000081162114],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049478834,0.00009635844,0.00032200033,0.00019898485,0.00009774983,0.000012814242,0.0001827554,0.00006245894,0.00046668213],"category_scores_gemma":[0.00009408696,0.00006617879,0.00002867317,0.00047371918,0.0008983616,0.000092125825,0.000029604576,0.00024590897,5.0188607e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003484396,0.00001737661,0.9885147,0.00001840655,0.00006112961,0.0000039913075,0.009356311,0.00020098497,0.0012512606,0.000008676687,0.000027288475,0.0005050258],"study_design_scores_gemma":[0.00027332877,0.00011544268,0.98717564,0.000079308105,0.000038504895,0.000008830614,0.008165917,0.001748062,0.0022060084,0.000054294695,0.000073714895,0.00006092755],"about_ca_topic_score_codex":0.06761678,"about_ca_topic_score_gemma":0.9363462,"teacher_disagreement_score":0.8687294,"about_ca_system_score_codex":0.000022393559,"about_ca_system_score_gemma":0.00016633363,"threshold_uncertainty_score":0.938592},"labels":[],"label_agreement":null},{"id":"W1653226853","doi":"10.1139/e08-031","title":"Impact of melting of the Laurentide Ice Sheet on sediments from the upper continental slope off southeastern Canada: evidence from Sm–Nd isotopesThis article is one of a series of papers published in this Special Issue on the theme<i>Polar Climate Stability Network</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Proterozoic; Glacial period; Ice sheet; Last Glacial Maximum; Paleontology; Younger Dryas; Geochemistry; Oceanography","score_opus":0.03067128427804457,"score_gpt":0.22698863435691782,"score_spread":0.19631735007887324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1653226853","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99266404,0.0009796368,8.816903e-8,0.0036167894,0.0003694821,0.00018917359,0.00043411396,7.4507324e-7,0.0017459326],"genre_scores_gemma":[0.999414,0.00008554038,0.000043388864,0.00026059267,0.00016755909,3.546033e-7,0.0000031681834,0.0000021153712,0.000023280898],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973073,0.00064935547,0.0006596886,0.00020370366,0.00069611595,0.00048383622],"domain_scores_gemma":[0.99725556,0.0014604019,0.0006188197,0.00029829625,0.00018093968,0.00018598631],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0022237976,0.00013945931,0.0004069041,0.000083408464,0.0004000399,0.00003188293,0.0010152466,0.00006872098,0.016955085],"category_scores_gemma":[0.0008012315,0.000069533315,0.00014244304,0.00056743796,0.0018965373,0.00032483376,0.00002905883,0.00039764808,0.00000419356],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019366432,0.000017279954,0.99449015,0.0000054724287,0.000050862902,0.000009239689,0.0034534622,0.0010543355,0.00010651704,0.000007529392,0.000491346,0.00012013921],"study_design_scores_gemma":[0.00022903354,0.0003377949,0.9947235,0.00024907902,0.00001811045,0.000011011808,0.0018399386,0.00027647268,0.0020041056,0.000080574566,0.00016514947,0.000065219894],"about_ca_topic_score_codex":0.7041458,"about_ca_topic_score_gemma":0.98140466,"teacher_disagreement_score":0.2772588,"about_ca_system_score_codex":0.0000040739196,"about_ca_system_score_gemma":0.0022004698,"threshold_uncertainty_score":0.9839435},"labels":[],"label_agreement":null},{"id":"W1654299927","doi":"10.1139/e08-065","title":"Variabilité décennale à millénaire des océans arctiques et sub-arctiques et des terres adjacentes : une contribution du Réseau d’étude de la stabilité du climat polaire du Canada à l’Année polaire internationaleCet article présente une sélection d’articles publiés dans le numéro spécial de la thematique <i>Réseau d’étude de la stabilité du climat polaire du Canada</i>. À la mémoire du Dr. Roy M. (« Fritz ») Koerner (1932–2008). [Traduit par la Rédaction]","year":2008,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Humanities; Forestry; Geology; Physical geography; Geography; Art","score_opus":0.015131926040587418,"score_gpt":0.2487948830394407,"score_spread":0.23366295699885328,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1654299927","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9286456,0.0032861687,0.00045273697,0.06244592,0.0007995406,0.0004418178,0.000483943,0.0000628074,0.003381482],"genre_scores_gemma":[0.9932995,0.00412412,0.0007806197,0.00093275576,0.000640247,0.000022352167,0.0000697468,0.000040405408,0.00009025487],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9857643,0.008778725,0.0013209777,0.0008414683,0.0011004217,0.002194101],"domain_scores_gemma":[0.9892228,0.0067191585,0.00066719734,0.00036400842,0.001047957,0.0019788458],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":["sts"],"category_scores_codex":[0.01026119,0.0007183937,0.0008785884,0.00054000993,0.003991546,0.000793502,0.0011875234,0.0006604628,0.00047279574],"category_scores_gemma":[0.0059948126,0.00065248,0.00033330964,0.0014102916,0.008954161,0.0023160945,0.00009061595,0.0017525944,0.0000059115655],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026491095,0.000366138,0.96273905,0.00016839709,0.00021960857,0.0019440595,0.01901094,0.0040744105,0.0004839729,0.005756784,0.0046426496,0.000329067],"study_design_scores_gemma":[0.0011902864,0.00042171657,0.9449134,0.00039624778,0.000095039875,0.015985921,0.009161285,0.005680654,0.0016490937,0.007437459,0.01244779,0.00062110147],"about_ca_topic_score_codex":0.97032374,"about_ca_topic_score_gemma":0.9993396,"teacher_disagreement_score":0.06465391,"about_ca_system_score_codex":0.00062078424,"about_ca_system_score_gemma":0.035074797,"threshold_uncertainty_score":0.99959266},"labels":[],"label_agreement":null},{"id":"W1654924868","doi":"10.1139/e08-024","title":"Altering Avalonia: oxygen isotopes and terrane distinction in the Appalachian peri-Gondwanan realmLaboratory for Stable Isotope Science (LSIS), The University of Western Ontario, Contribution 236.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University; Western University","funders":"Infrastructure Canada; Natural Sciences and Engineering Research Council of Canada; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Terrane; Felsic; Geology; Igneous rock; Paleozoic; Geochemistry; Magmatism; Gondwana; Petrology; Paleontology; Mafic; Structural basin; Tectonics","score_opus":0.01727220916042179,"score_gpt":0.183417912384604,"score_spread":0.1661457032241822,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1654924868","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973807,0.00045753442,0.000090169975,0.0014995626,0.00007264838,0.00010864679,0.000026151403,0.000001261807,0.00036336563],"genre_scores_gemma":[0.99957776,0.00003575574,0.00018761458,0.000117441254,0.000027414873,1.3798734e-7,0.0000029400535,4.789889e-7,0.000050467734],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99904096,0.0000689415,0.00019073654,0.00015585234,0.0002504748,0.00029302426],"domain_scores_gemma":[0.9993171,0.00010120203,0.00015077357,0.00008122626,0.00015329212,0.00019637668],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014588863,0.00007288639,0.00015996465,0.00014014676,0.0011536314,0.00006919671,0.00047998579,0.000026888574,0.0003095304],"category_scores_gemma":[0.00012530466,0.00004009716,0.000047578847,0.0006370556,0.0015390622,0.0003644435,0.000008648245,0.00013467328,0.0000017897738],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013423303,0.0000039011666,0.99723905,0.0000030929673,0.000004351154,0.000013090306,0.0013186691,0.00068188534,0.00012564179,0.000034475168,0.00001743032,0.00054496696],"study_design_scores_gemma":[0.00014806716,0.00020801816,0.99320483,0.000016112972,0.000015277963,0.000063053834,0.0015068768,0.00074926345,0.00007784307,0.00034268008,0.0036085313,0.00005942382],"about_ca_topic_score_codex":0.2498189,"about_ca_topic_score_gemma":0.95152533,"teacher_disagreement_score":0.7017064,"about_ca_system_score_codex":0.0000065596973,"about_ca_system_score_gemma":0.00087190093,"threshold_uncertainty_score":0.8872916},"labels":[],"label_agreement":null},{"id":"W1663855975","doi":"10.1139/e08-002","title":"Correlation of mid-Cretaceous granites with source terranes in the northern Canadian CordilleraLithoprobe Publication 1475.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Terrane; Geology; Subduction; Cretaceous; Geochemistry; Paleontology; Continental margin; Tectonics","score_opus":0.01777509962939291,"score_gpt":0.1776534604931491,"score_spread":0.15987836086375617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1663855975","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911251,0.00073379173,0.000027727081,0.0033021544,0.000056262852,0.000068812325,0.000014627584,0.0000017392412,0.00466977],"genre_scores_gemma":[0.9991945,0.000019526962,0.00022213356,0.00041338077,0.00003842366,2.1986921e-7,0.000013042239,9.905913e-7,0.00009775143],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988235,0.00009637313,0.00030495875,0.00013014498,0.00032227274,0.00032272126],"domain_scores_gemma":[0.9989586,0.00013097681,0.00021082525,0.000091255184,0.00021901866,0.00038936376],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00064461736,0.000090602145,0.0001738939,0.00039263628,0.00034433135,0.0000626211,0.00044598302,0.000043132983,0.0015653038],"category_scores_gemma":[0.00018962761,0.000048222988,0.000061942876,0.0011010622,0.00066774554,0.00025717355,0.0000016201493,0.00016327637,0.000019664698],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000058199985,0.0000033719582,0.9854723,0.0000019653141,0.0000057816155,0.000038644448,0.00077373424,0.01189921,0.0000044803164,0.000011464423,0.000041848245,0.0017413613],"study_design_scores_gemma":[0.000115751325,0.00023326332,0.9919221,0.000017392053,0.00001187912,0.00035242212,0.0006872313,0.0023628843,0.000019189027,0.00046996065,0.003722447,0.000085484775],"about_ca_topic_score_codex":0.69314706,"about_ca_topic_score_gemma":0.9951661,"teacher_disagreement_score":0.3020191,"about_ca_system_score_codex":0.0000026577625,"about_ca_system_score_gemma":0.0009831083,"threshold_uncertainty_score":0.9993474},"labels":[],"label_agreement":null},{"id":"W1667101375","doi":"10.1139/e07-043","title":"Onshore migration of a deep-water brachiopod fauna from the Lower Ordovician Tonggao Formation, Jiangnan Slope, southeastern Guizhou Province, South ChinaThis article is one of a series of papers published in this Special Issue on the theme <i>The dynamic reef and shelly communities of the Paleozoic. This Special is in honour of our colleague and friend Paul Copper</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"Ministry of Science and Technology of the People's Republic of China; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Fauna; Geology; Biozone; Ordovician; Paleontology; Facies; Species richness; Benthic zone; Biostratigraphy; Ecology; Biology; Oceanography; Structural basin","score_opus":0.013160353331229668,"score_gpt":0.18762477567948463,"score_spread":0.17446442234825496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1667101375","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9849086,0.00085352943,7.359238e-7,0.0055752634,0.00014631027,0.00025176126,0.0002983916,7.9475876e-7,0.007964623],"genre_scores_gemma":[0.9995134,0.0000920064,0.00007682431,0.00018041456,0.00009392721,6.5253676e-7,0.0000017928738,0.0000014389151,0.000039571343],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99817103,0.0003820285,0.00067586295,0.0001211559,0.00040206796,0.00024788242],"domain_scores_gemma":[0.99875855,0.00023342106,0.0005622113,0.00022334752,0.00013515839,0.00008729596],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012615677,0.00013470664,0.00035179008,0.00020324567,0.00048216846,0.000054243992,0.00061841524,0.00007867204,0.0007088817],"category_scores_gemma":[0.00013135435,0.0000646892,0.000087545995,0.00046855744,0.002018588,0.0004803102,0.000009928737,0.00030533495,4.5738952e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013218811,0.000027371192,0.8999332,0.000015229394,0.000026022955,0.0000046484442,0.09754882,0.00004181099,0.00010477225,0.00007692237,0.00014286136,0.0019461535],"study_design_scores_gemma":[0.00032206374,0.00043860846,0.9546299,0.00017853662,0.000018173858,0.000026614118,0.042273607,0.00037594137,0.0009431979,0.00047956072,0.00023719041,0.00007662557],"about_ca_topic_score_codex":0.019868264,"about_ca_topic_score_gemma":0.90670025,"teacher_disagreement_score":0.88683194,"about_ca_system_score_codex":0.000002291199,"about_ca_system_score_gemma":0.00045991846,"threshold_uncertainty_score":0.9866585},"labels":[],"label_agreement":null},{"id":"W1673467074","doi":"10.1139/e08-037","title":"Geochemical reconstruction of Pacific decadal variability from the eastern North Pacific during the HoloceneThis article is one of a series of papers published in this Special Issue on the theme<i>Polar Climate Stability Network</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; University of British Columbia","funders":"","keywords":"Holocene; Geology; Oceanography; Pacific decadal oscillation; Inlet; Holocene climatic optimum; Physical geography; Climatology; Pacific ocean; Geography","score_opus":0.02334842026501558,"score_gpt":0.1989176068450477,"score_spread":0.17556918658003212,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1673467074","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99060076,0.0002684489,3.0778259e-7,0.003304576,0.00035848,0.0001491088,0.00011700151,0.0000014849655,0.005199803],"genre_scores_gemma":[0.99942017,0.00014270066,0.00009503716,0.000059491867,0.000262621,5.095086e-7,0.000002501543,0.0000014608264,0.000015496924],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99751925,0.0007523967,0.00061734224,0.00021624776,0.00042397794,0.00047078554],"domain_scores_gemma":[0.9976849,0.0012648974,0.0004011371,0.0003030942,0.00017963417,0.00016631313],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0035378153,0.000114509494,0.00031638547,0.00008999841,0.0005883773,0.000036612324,0.0006886588,0.000098476325,0.011439592],"category_scores_gemma":[0.00068888895,0.000059491784,0.00010211495,0.0007190023,0.0045634843,0.0002955358,0.000018128783,0.0005275315,0.0000074710124],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014706007,0.0000132136265,0.9964356,0.000009652176,0.00002029787,0.0000071524473,0.002699682,0.0002926112,0.00004259943,0.000026479853,0.000063884974,0.00024176482],"study_design_scores_gemma":[0.00015750964,0.00016891945,0.99423766,0.000038848193,0.000010135273,0.00007745552,0.0023725217,0.00023958931,0.0016948088,0.000729193,0.00021310704,0.00006023919],"about_ca_topic_score_codex":0.008178028,"about_ca_topic_score_gemma":0.25507358,"teacher_disagreement_score":0.24689555,"about_ca_system_score_codex":0.0000021954436,"about_ca_system_score_gemma":0.00071636017,"threshold_uncertainty_score":0.9984266},"labels":[],"label_agreement":null},{"id":"W1702267567","doi":"10.1139/cjes-2013-0003","title":"Paleomagnetism of ∼1.09 Ga Lake Shore Traps (Keweenaw Peninsula, Michigan): new results and implications","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Paleomagnetism; Lava; Shore; Peninsula; Paleontology; Declination; Geomorphology; Seismology; Oceanography; Archaeology; Volcano; Geography","score_opus":0.014284755789107862,"score_gpt":0.222981531440715,"score_spread":0.20869677565160713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1702267567","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9829424,0.008637562,0.000028659124,0.0035914762,0.0001597733,0.00012940656,0.00007329788,0.0000016610529,0.0044357763],"genre_scores_gemma":[0.9959197,0.0005972615,0.0019740288,0.00014100118,0.0001655881,0.0000020128339,0.000008068915,0.0000056004824,0.0011867062],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99889886,0.0000379758,0.00038234008,0.00021773242,0.0001376715,0.00032539477],"domain_scores_gemma":[0.9988649,0.000028058756,0.00021070811,0.0001741229,0.00018462555,0.0005375837],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002596241,0.00012852256,0.00019119876,0.00015912684,0.0002070385,0.00007487199,0.00032390148,0.000079334575,0.000115732975],"category_scores_gemma":[0.00015278648,0.000108201406,0.00007072202,0.0002105254,0.0006364037,0.000023648508,0.000026459162,0.00008886032,0.0000052677683],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005683375,0.000049513448,0.7201388,0.000052223026,0.00012668423,0.00003469189,0.003818476,0.00011863717,0.18720968,0.00063833286,0.035647724,0.05210841],"study_design_scores_gemma":[0.00050413545,0.0012473016,0.948077,0.000033055363,0.000020672798,0.00015981462,0.00047655168,0.0000061999417,0.0020713801,0.00053569075,0.046714976,0.00015320737],"about_ca_topic_score_codex":0.0026436355,"about_ca_topic_score_gemma":0.18060762,"teacher_disagreement_score":0.22793822,"about_ca_system_score_codex":5.625265e-7,"about_ca_system_score_gemma":0.00076581084,"threshold_uncertainty_score":0.83434415},"labels":[],"label_agreement":null},{"id":"W1716191719","doi":"10.1139/cjes-2013-0143","title":"Distribution of Paleogene and Cretaceous rocks around the Nazko River belt of central British Columbia from 3-D long-offset first-arrival seismic tomography","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Cretaceous; Sedimentary rock; Volcanic rock; Basement; Igneous rock; Paleontology; Paleogene; Sedimentary basin; Bouguer anomaly; Seismology; Volcano; Gravity anomaly","score_opus":0.007351207522123456,"score_gpt":0.17388504591306173,"score_spread":0.16653383839093827,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1716191719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99541694,0.0023393962,0.00076271757,0.00043412184,0.00033633874,0.00006491785,0.00042529884,0.0000044180665,0.00021586353],"genre_scores_gemma":[0.99908465,0.00016965935,0.0003156711,0.0002841714,0.00008863791,9.656577e-8,0.000028249977,0.0000015291846,0.000027355647],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883866,0.000092664966,0.0003133499,0.00014820116,0.0003049054,0.0003022252],"domain_scores_gemma":[0.9990109,0.00014889287,0.0002912361,0.00010297262,0.000120354474,0.0003256041],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000617413,0.00007597508,0.0002029516,0.00008587841,0.00048018812,0.00021678816,0.0003858664,0.00005032902,0.00037200804],"category_scores_gemma":[0.000117177646,0.00007053224,0.000089328554,0.00031010946,0.001409002,0.00027034263,0.0000071201475,0.00013685712,0.0000011097085],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000047790054,0.0000027007839,0.9741224,0.0000060516386,0.000012955177,0.000012401353,0.00018234694,0.00060623593,0.0000039123124,0.0000011439193,0.0027528908,0.022292167],"study_design_scores_gemma":[0.00016094526,0.00028400458,0.9769834,0.00011603189,0.000025844676,0.00014076765,0.0002540499,0.009131849,0.00024045134,0.0011071512,0.011459564,0.000095913034],"about_ca_topic_score_codex":0.4540843,"about_ca_topic_score_gemma":0.53124285,"teacher_disagreement_score":0.07715857,"about_ca_system_score_codex":0.0000020956036,"about_ca_system_score_gemma":0.00030609895,"threshold_uncertainty_score":0.549551},"labels":[],"label_agreement":null},{"id":"W1720950091","doi":"10.1139/e11-056","title":"Ecological controls on Devonian stromatoporoid-dominated and coral-dominated reef growth in the Mackenzie Basin, Northwest Territories, Canada","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Aurora Research Institute","keywords":"Reef; Geology; Coral reef; Oceanography; Devonian; Coral; Structural basin; Paleozoic; Paleontology","score_opus":0.01898128081576274,"score_gpt":0.1999135359264697,"score_spread":0.18093225511070699,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1720950091","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9877546,0.0009128549,8.059224e-7,0.00108941,0.000451362,0.000118000484,0.00017937894,0.000002403524,0.00949119],"genre_scores_gemma":[0.9991842,0.000019202796,0.00019021009,0.00054554053,0.00004908162,4.901469e-7,0.000005175788,6.760481e-7,0.0000054100224],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983888,0.00025529723,0.00037232827,0.00019520413,0.00028592834,0.0005024127],"domain_scores_gemma":[0.99880177,0.0003194339,0.0002119653,0.00008744011,0.00009061951,0.0004887872],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010699494,0.00015183956,0.00027255787,0.00023455777,0.000513695,0.00008325569,0.00058176747,0.00008519376,0.00022557325],"category_scores_gemma":[0.0002360086,0.00009315568,0.000045101253,0.00043123454,0.0009767032,0.0002825222,0.000001038522,0.00031737558,0.000001068411],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041777315,0.000008471344,0.99663126,0.000002201981,0.0000095223695,0.00089894613,0.00038410374,0.0000058171654,0.0000013962294,0.0003434102,0.00013156632,0.0015415078],"study_design_scores_gemma":[0.00043126222,0.00076828303,0.9960907,0.000025853877,0.00000960371,0.00036313524,0.0009494423,0.00006939718,0.00003783959,0.00062262913,0.00051086105,0.00012100871],"about_ca_topic_score_codex":0.9260283,"about_ca_topic_score_gemma":0.99971884,"teacher_disagreement_score":0.07369053,"about_ca_system_score_codex":0.0000042868455,"about_ca_system_score_gemma":0.002265111,"threshold_uncertainty_score":0.40182096},"labels":[],"label_agreement":null},{"id":"W1722919204","doi":"10.1139/cjes-2012-0122","title":"The southern Coast Mountains, British Columbia: New interpretations from geological, seismic reflection, and gravity data","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of British Columbia","funders":"","keywords":"Geology; Terrane; Cretaceous; Pluton; Structural basin; Sedimentary rock; Paleontology; Volcanic rock; Metamorphic rock; Fault (geology); Clastic rock; Thrust fault; Seismology; Volcano; Tectonics","score_opus":0.024432411238028917,"score_gpt":0.220337662269901,"score_spread":0.1959052510318721,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1722919204","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99410886,0.0024697897,0.00013350132,0.0022105803,0.0002803649,0.000054732067,0.0003301904,0.0000033669498,0.00040861696],"genre_scores_gemma":[0.997172,0.00020665929,0.0004432396,0.00064698484,0.0001554397,1.0013603e-7,0.00002498862,0.0000012680584,0.0013493225],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989967,0.000090108326,0.00025242614,0.00019121867,0.00019694277,0.0002726169],"domain_scores_gemma":[0.998851,0.00021892422,0.00016292495,0.0001521236,0.000080863996,0.0005341538],"candidate_categories":["scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000593768,0.000062303676,0.00014061916,0.000055574383,0.0011989366,0.0021236353,0.0006639009,0.000037722322,0.0019981123],"category_scores_gemma":[0.00022811467,0.000049993516,0.000039050832,0.00028185578,0.0006141555,0.00054823083,0.000014750996,0.0001616617,0.00004472399],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000010182265,0.0000010606373,0.95642924,5.4709477e-7,0.00002405648,0.000012642421,0.00014137114,0.0005602782,0.000002799929,0.0000017733041,0.009775354,0.033049837],"study_design_scores_gemma":[0.00012985877,0.00017171222,0.93095994,0.000028069504,0.000039020048,0.00013544757,0.00341264,0.027215581,5.720734e-7,0.007797355,0.029992405,0.00011740358],"about_ca_topic_score_codex":0.9481961,"about_ca_topic_score_gemma":0.99522406,"teacher_disagreement_score":0.047027946,"about_ca_system_score_codex":0.0000014738014,"about_ca_system_score_gemma":0.00065417576,"threshold_uncertainty_score":0.9989142},"labels":[],"label_agreement":null},{"id":"W1726448194","doi":"10.1139/e11-047","title":"Upper Ordovician conodont biostratigraphy and the age of the Collingwood Member, southern Ontario, Canada<sup>1</sup>Earth Science Sector (ESS) Contribution 20100302.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; University of Calgary; Government of Nunavut; Nunavut Research Institute","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Conodont; Ordovician; Geology; Paleontology; Biostratigraphy; Fauna; Facies; Chemostratigraphy; Ecology","score_opus":0.018917040618163888,"score_gpt":0.18746031910526456,"score_spread":0.16854327848710068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1726448194","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9809591,0.0029959844,0.000007229358,0.0004963763,0.0005269099,0.00019695573,0.00013067422,0.0000023655684,0.014684398],"genre_scores_gemma":[0.99936527,0.00001796038,0.00026496936,0.00024792232,0.0000438974,4.085415e-7,8.6395056e-7,9.001398e-7,0.000057819496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980213,0.0001880465,0.000460128,0.0002322335,0.0005251888,0.0005730983],"domain_scores_gemma":[0.99848914,0.0001778732,0.00039257068,0.00019613105,0.00025801323,0.00048625216],"candidate_categories":["sts"],"consensus_categories":["sts"],"category_scores_codex":[0.002042473,0.0001677763,0.00031381735,0.00025340862,0.0015096444,0.00015369573,0.00096768595,0.00007376558,0.00063233054],"category_scores_gemma":[0.00019258639,0.00009018862,0.00012705167,0.0007906013,0.006650204,0.0003967459,0.0000038811677,0.00034456718,0.0000013328588],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037001435,0.000003954498,0.99406457,0.000002775835,0.000028695875,0.00002624426,0.004047355,0.00012808271,0.000025777967,0.00095175445,0.000036916274,0.00064687256],"study_design_scores_gemma":[0.0004772898,0.00017621063,0.9946635,0.000043124244,0.000034611774,0.00011859542,0.0019936666,0.000280942,0.00028459218,0.0007963161,0.0010055259,0.00012566811],"about_ca_topic_score_codex":0.9731829,"about_ca_topic_score_gemma":0.9998546,"teacher_disagreement_score":0.026671715,"about_ca_system_score_codex":0.000004969792,"about_ca_system_score_gemma":0.009687558,"threshold_uncertainty_score":0.99979025},"labels":[],"label_agreement":null},{"id":"W1727379991","doi":"10.1139/cjes-2013-0111","title":"How feasible was subduction in the Archean?","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Asthenosphere; Geology; Subduction; Mantle (geology); Archean; Lithosphere; Mantle convection; Partial melting; Crust; Oceanic crust; Eclogitization; Geophysics; Petrology; Mantle wedge; Hotspot (geology); Crustal recycling; Geochemistry; Continental crust; Seismology; Tectonics","score_opus":0.0269510506331437,"score_gpt":0.20288968541686606,"score_spread":0.17593863478372235,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1727379991","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99053806,0.00035145204,0.0000067398764,0.005487719,0.000748525,0.00008934061,0.000007997772,0.0000013776926,0.0027688162],"genre_scores_gemma":[0.9990253,0.000014891254,0.0002827464,0.00022163911,0.00025605844,3.08069e-7,0.0000014524859,8.3772613e-7,0.00019680607],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990817,0.00010047814,0.00014844022,0.00009119891,0.00023935895,0.00033885436],"domain_scores_gemma":[0.99945074,0.00006314126,0.00010142153,0.00007756863,0.000061894134,0.0002452354],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001024461,0.000063141306,0.000108361484,0.00018111328,0.00024425582,0.0006641393,0.000433352,0.000024426201,0.0010982748],"category_scores_gemma":[0.00007494421,0.000035916197,0.000035462486,0.00034570022,0.0002455056,0.00072114926,0.0000018394427,0.00010265197,0.00006688616],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000085132515,0.000015643252,0.9600146,0.000021661152,0.000017848522,0.00013412932,0.004576244,0.0043790983,0.0011393995,0.0022778823,0.008176008,0.019239008],"study_design_scores_gemma":[0.00009845983,0.00018866209,0.96881616,0.00001991604,0.00000440745,0.00008830002,0.0017464845,0.00023155335,0.00020208443,0.005959284,0.022556705,0.00008799465],"about_ca_topic_score_codex":0.05710592,"about_ca_topic_score_gemma":0.36818936,"teacher_disagreement_score":0.31108344,"about_ca_system_score_codex":7.897445e-7,"about_ca_system_score_gemma":0.0005299184,"threshold_uncertainty_score":0.99981487},"labels":[],"label_agreement":null},{"id":"W1731876635","doi":"10.1139/e10-098","title":"Near-surface and crustal-scale images of the Nechako basin, British Columbia, Canada, from magnetotelluric investigations<sup>1</sup>This article is one of a series of papers published in this Special Issue on the theme of <i>New insights in Cordilleran Intermontane geoscience: reducing exploration risk in the mountain pine beetle-affected area, British Columbia</i>.<sup>2</sup>Geological Survey of Canada, GSC Contribution No.: 20100129.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Magnetotellurics; Terrane; Crust; Imbrication; Sedimentary rock; Electrical resistivity and conductivity; Sedimentary basin; Volcano; Basement; Cretaceous; Basalt; Structural basin; Seismology; Paleontology; Petrology; Tectonics","score_opus":0.016046006782454682,"score_gpt":0.18020474228695116,"score_spread":0.16415873550449647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1731876635","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997489,0.00041296412,0.000003322496,0.0006672042,0.00011094481,0.00035422388,0.00056496385,0.0000011067126,0.00039627712],"genre_scores_gemma":[0.99908984,0.00008980506,0.00040853128,0.0001834799,0.0000466362,0.0000011171447,0.000010039739,0.0000026002479,0.00016796398],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9965944,0.001142273,0.0008890125,0.00027323686,0.00070783595,0.00039324095],"domain_scores_gemma":[0.99760073,0.00087121106,0.0006385351,0.00018869457,0.00045360564,0.00024723227],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0023606662,0.00011896698,0.00054288737,0.000069120615,0.00028051104,0.00019565523,0.0006214044,0.00008939937,0.0037371952],"category_scores_gemma":[0.003197806,0.00010417628,0.000056764427,0.0019990297,0.0015711412,0.0004895124,0.000022928176,0.00040752554,2.4814568e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000069812835,0.00006641294,0.9813854,0.000016440132,0.00001463562,0.000025363574,0.0035841991,0.0037398313,0.0002359204,0.0000029448756,0.0026281725,0.008230852],"study_design_scores_gemma":[0.0003894067,0.00076348265,0.9895917,0.00023624537,0.000014944986,0.0000150092765,0.0016589224,0.0055103586,0.00068148033,0.0009166306,0.00010949416,0.00011228118],"about_ca_topic_score_codex":0.99975336,"about_ca_topic_score_gemma":0.999954,"teacher_disagreement_score":0.008206329,"about_ca_system_score_codex":0.000023890503,"about_ca_system_score_gemma":0.0033920996,"threshold_uncertainty_score":0.99717355},"labels":[],"label_agreement":null},{"id":"W1744557775","doi":"10.1139/cjes-2015-0062","title":"Sedimentology of the lower Serpukhovian (upper Mississippian) Mabou Group in the Cumberland Basin of eastern Canada: tectonic, halokinetic, and climatic implications","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Gondwana; Geology; Fluvial; Paleontology; Structural basin; Glacial period; Sea level; Paleosol; Red beds; Diachronous; Loess; Oceanography","score_opus":0.027955148275569122,"score_gpt":0.23723502004341643,"score_spread":0.2092798717678473,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1744557775","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98385143,0.0016388994,0.0000020022942,0.0103952885,0.00025243775,0.00010631898,0.00002483452,4.56757e-7,0.00372833],"genre_scores_gemma":[0.9994023,0.000017588025,0.0001038116,0.0004009581,0.000017329363,3.9013761e-7,0.0000012769306,9.518469e-7,0.00005539507],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99863106,0.00031509128,0.0003391692,0.000114965944,0.0002577999,0.00034191663],"domain_scores_gemma":[0.9989419,0.0003043061,0.00020761453,0.00015375788,0.00010370693,0.00028869053],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014297928,0.00007890331,0.00021082723,0.00017588444,0.00018549387,0.000025471636,0.0006232482,0.000058789723,0.00023133217],"category_scores_gemma":[0.00021565238,0.00004306645,0.0000358873,0.00046098174,0.0012100771,0.00011067525,0.0000092439495,0.00021664963,0.0000024648352],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000082910165,0.0000060653383,0.99884397,0.000009091465,0.000007372388,0.000017918295,0.00047120586,0.00012567065,0.0000021553265,0.00014499128,0.0001738305,0.000189422],"study_design_scores_gemma":[0.00021456645,0.00021656722,0.9955513,0.00003366437,0.000011128175,0.00046906513,0.0009896084,0.00028483896,0.000010828427,0.0005938783,0.0015780968,0.000046456928],"about_ca_topic_score_codex":0.41633552,"about_ca_topic_score_gemma":0.99501127,"teacher_disagreement_score":0.57867575,"about_ca_system_score_codex":0.0000012551176,"about_ca_system_score_gemma":0.0027558408,"threshold_uncertainty_score":0.5875511},"labels":[],"label_agreement":null},{"id":"W1750025403","doi":"10.1139/cjes-2013-0054","title":"Stratigraphy and infill history of the glacially eroded Matane River Valley, eastern Quebec, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Rimouski","funders":"Natural Sciences and Engineering Research Council of Canada; Université du Québec à Rimouski","keywords":"Geology; Deglaciation; Outwash plain; Fluvial; Holocene; Radiocarbon dating; Moraine; Sedimentary depositional environment; Glacial period; Delta; Paleontology; Last Glacial Maximum; River terraces; Glacier; Geomorphology; Structural basin","score_opus":0.01377020011396293,"score_gpt":0.161522103762292,"score_spread":0.14775190364832907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1750025403","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9876513,0.0024496766,0.0000043603964,0.0011233349,0.00047244463,0.00005833068,0.000015772466,9.94091e-7,0.008223806],"genre_scores_gemma":[0.99867725,0.00002558069,0.00023158923,0.00040765738,0.00002476621,9.706175e-8,7.431745e-7,5.254941e-7,0.0006317829],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99920297,0.000043779713,0.00023603463,0.000071980416,0.000245573,0.00019967671],"domain_scores_gemma":[0.9992257,0.00005950854,0.00019648673,0.00006331666,0.00014850186,0.0003064878],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022605757,0.000067451416,0.00011532156,0.00009662677,0.00016876937,0.000060423823,0.00034879072,0.000026502348,0.0024093222],"category_scores_gemma":[0.00007023031,0.00003793724,0.000032371237,0.00020698771,0.0007229466,0.00045536645,0.000004098153,0.0000953695,0.0000050625854],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000014941519,0.0000011996996,0.9928167,0.000010032302,0.0000062759177,0.0000044472395,0.00035830482,0.0005892108,0.0000054298903,0.00014328993,0.0024176321,0.0036459921],"study_design_scores_gemma":[0.000056974714,0.00006331213,0.9802744,0.000021354203,0.00000489444,0.000028643752,0.0003428003,0.00037446225,0.000008938303,0.0008643124,0.017901737,0.00005817987],"about_ca_topic_score_codex":0.9758336,"about_ca_topic_score_gemma":0.99958867,"teacher_disagreement_score":0.023755036,"about_ca_system_score_codex":0.0000035463624,"about_ca_system_score_gemma":0.004617924,"threshold_uncertainty_score":0.9985026},"labels":[],"label_agreement":null},{"id":"W1750884694","doi":"10.1139/e2012-023","title":"Cryostratigraphic record of permafrost degradation and recovery following historic (1898–1992) surface disturbances in the Klondike region, central Yukon Territory<sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of <i>Fundamental and applied research on permafrost in Canada</i>.<sup>2</sup>Yukon Geological Survey Contribution 008.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; University of Waterloo","keywords":"Permafrost; Geology; Disturbance (geology); Aggradation; Vegetation (pathology); Thermokarst; Physical geography; Active layer; Ecological succession; Table (database); Geomorphology; Hydrology (agriculture); Earth science; Geography; Oceanography; Ecology","score_opus":0.056391681400614346,"score_gpt":0.23927348593751596,"score_spread":0.18288180453690162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1750884694","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946801,0.0013181907,8.801978e-8,0.0014850356,0.00020182364,0.00028413063,0.001233459,7.561565e-7,0.0007964064],"genre_scores_gemma":[0.9992072,0.00040354507,0.000011572794,0.00012919948,0.00014079204,0.0000012271373,0.00008647785,0.0000029003204,0.000017099912],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99709255,0.0006901111,0.0006938173,0.0002292681,0.0007244838,0.00056976284],"domain_scores_gemma":[0.9981517,0.0010352742,0.00035492735,0.00014744296,0.00009623324,0.00021439619],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.003846451,0.00016082436,0.00042801187,0.0003825252,0.0002482177,0.00008229807,0.00036513305,0.00008599525,0.0010623607],"category_scores_gemma":[0.00036266254,0.0001046472,0.000059520688,0.0010014516,0.00090649596,0.0006176705,0.000012679301,0.00037192155,4.3038938e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026052177,0.000038446316,0.990994,0.000022511776,0.000010112471,0.000009042269,0.006653739,0.0005624482,0.00030897997,0.00005334561,0.0007670154,0.0003198327],"study_design_scores_gemma":[0.0003927791,0.0005735015,0.9850622,0.00017363534,0.000008786044,0.000012540653,0.012267349,0.0003432969,0.00041082528,0.000066732675,0.000578359,0.00010999633],"about_ca_topic_score_codex":0.765587,"about_ca_topic_score_gemma":0.9871829,"teacher_disagreement_score":0.22159596,"about_ca_system_score_codex":0.000049916536,"about_ca_system_score_gemma":0.0008270888,"threshold_uncertainty_score":0.9998508},"labels":[],"label_agreement":null},{"id":"W1758940491","doi":"10.1139/e08-061","title":"Reorganization of the upper ocean circulation in the mid-Holocene in the northeastern AtlanticThis article is one of a series of papers published in this Special Issue on the theme <i>Polar Climate Stability Network</i>.GEOTOP Publication 2009-0002.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Agence Nationale de la Recherche","keywords":"Holocene; Dinocyst; Geology; Oceanography; Paleoceanography; Meltwater; Ocean current; Westerlies; Radiocarbon dating; Climatology; Ridge; Glacial period; Paleontology; Palynology","score_opus":0.02502805575073503,"score_gpt":0.20791095068230805,"score_spread":0.18288289493157303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1758940491","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9789355,0.00018059954,2.3510016e-7,0.016199037,0.00012493477,0.00024744388,0.000022122827,7.893179e-7,0.00428938],"genre_scores_gemma":[0.99928373,0.00007240949,0.000015648444,0.0005066988,0.000102928454,5.7190874e-7,0.000004209509,0.0000013635241,0.000012460306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99761665,0.00088215654,0.0005452588,0.00014198033,0.0004694097,0.00034453088],"domain_scores_gemma":[0.9986947,0.00044569344,0.0003547461,0.00024990307,0.00019471455,0.00006023909],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.004993176,0.00008273376,0.00019581588,0.00020173773,0.00032101772,0.00004702837,0.0008074228,0.0000728539,0.0035393806],"category_scores_gemma":[0.0006785017,0.00003983378,0.000052121166,0.0018031703,0.0012377719,0.00036081846,0.0000098906075,0.00032607792,0.0000048412376],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003424058,0.000022880344,0.99036545,0.000008255543,0.000004113569,0.0000039682836,0.0073115923,0.0018709629,0.0000103201955,0.00017182696,0.00011244067,0.00008396694],"study_design_scores_gemma":[0.00015378481,0.00012367088,0.9961513,0.000038343675,0.0000049013356,0.000049552946,0.0017907363,0.000711922,0.00023666475,0.00043173923,0.00026609562,0.000041235136],"about_ca_topic_score_codex":0.007202144,"about_ca_topic_score_gemma":0.3142592,"teacher_disagreement_score":0.30705705,"about_ca_system_score_codex":0.0000020204227,"about_ca_system_score_gemma":0.00053239975,"threshold_uncertainty_score":0.99940896},"labels":[],"label_agreement":null},{"id":"W1761655294","doi":"10.1139/cjes-2012-0137","title":"Geothermal exploration of Paleozoic formations in Central Alberta","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta","funders":"","keywords":"Geology; Devonian; Paleozoic; Geothermal gradient; Structural basin; Carboniferous; Geochemistry; Petrology; Geomorphology; Paleontology","score_opus":0.025738420189407155,"score_gpt":0.2207527665366848,"score_spread":0.19501434634727766,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1761655294","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99388087,0.00009949008,0.0007632787,0.0004055465,0.0002092665,0.000036132977,0.0000012947285,5.068468e-7,0.0046036453],"genre_scores_gemma":[0.9993356,0.0000052821583,0.0002358144,0.00006135826,0.000028761093,7.672775e-7,2.6708096e-7,0.00000114993,0.0003310388],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993259,0.00002713033,0.0002057385,0.000038802238,0.00015601038,0.00024645182],"domain_scores_gemma":[0.9996453,0.000025133764,0.00010667663,0.000034597608,0.00001266041,0.00017564335],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003679837,0.000040135095,0.00007233725,0.0001136626,0.000113547096,0.000021296422,0.00013093623,0.000014176855,0.00056015875],"category_scores_gemma":[0.00003843288,0.00003157956,0.000025317133,0.0002519267,0.00022868057,0.0016782107,0.000008183623,0.000041166702,0.000024573677],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[8.153407e-7,0.000007766902,0.9895734,0.0000011316836,0.0000017207834,7.681495e-7,0.0057479613,0.0007804994,0.00013678242,0.0003201563,0.00006022997,0.0033687702],"study_design_scores_gemma":[0.00009718695,0.000043299126,0.9890624,0.000011083418,0.000002825377,0.000008579671,0.0014353619,0.00012762418,0.00038319154,0.00007360191,0.008711542,0.00004328446],"about_ca_topic_score_codex":0.0096473945,"about_ca_topic_score_gemma":0.35757124,"teacher_disagreement_score":0.34792387,"about_ca_system_score_codex":0.000012181937,"about_ca_system_score_gemma":0.00007762378,"threshold_uncertainty_score":0.99694747},"labels":[],"label_agreement":null},{"id":"W1764111153","doi":"10.1139/e11-005","title":"Quartz arenites of the Cambro-Ordovician Kamouraska Formation, Quebec Appalachians, Canada: I. Deep-water depositional processes in a continental-slope environment","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Arenite; Turbidity current; Sedimentary depositional environment; Conglomerate; Submarine canyon; Canyon; Siliciclastic; Turbidite; Clastic rock; Sedimentary rock; Ordovician; Geomorphology; Paleocurrent; Geochemistry; Paleontology; Structural basin","score_opus":0.01314257752953849,"score_gpt":0.1607373171297038,"score_spread":0.1475947396001653,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1764111153","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961128,0.001119393,0.00003337219,0.00088958716,0.00016671923,0.00009706338,0.000064016705,0.0000013613643,0.0015156728],"genre_scores_gemma":[0.999238,0.0000343814,0.00038527203,0.00025075366,0.000024567003,8.6776544e-7,0.0000072927887,0.0000010857208,0.000057763307],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99876696,0.000060237588,0.0004488383,0.00009385283,0.00031499178,0.00031514035],"domain_scores_gemma":[0.99931777,0.000053247626,0.00022685558,0.000064052394,0.00011079973,0.00022729812],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034563016,0.00009950595,0.000152716,0.00017442732,0.0003478706,0.00005700237,0.0004293259,0.00003502221,0.0023478668],"category_scores_gemma":[0.000056789082,0.000053702788,0.00003956763,0.0003546016,0.00037310622,0.0005915015,0.0000062473678,0.000121499885,0.000007702796],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005751148,0.000007576545,0.9941031,0.000026524933,0.0000052855034,0.000009776158,0.0020057003,0.0025985197,0.000011276298,0.00006585921,0.00003200495,0.0011286654],"study_design_scores_gemma":[0.00011358315,0.000089416404,0.994207,0.00006749983,0.00000894662,0.00007167344,0.0020227323,0.00031953352,0.00092473306,0.00046416323,0.0016139876,0.00009667898],"about_ca_topic_score_codex":0.8770547,"about_ca_topic_score_gemma":0.9997553,"teacher_disagreement_score":0.12270065,"about_ca_system_score_codex":0.000007534892,"about_ca_system_score_gemma":0.0024910616,"threshold_uncertainty_score":0.9985641},"labels":[],"label_agreement":null},{"id":"W1765423974","doi":"10.1139/e2012-029","title":"Low-pressure regional amphibolite-facies to granulite-facies metamorphism of the Paleoproterozoic Thompson Nickel Belt, Manitoba","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Geochemistry; Metamorphic facies; Metamorphism; Sillimanite; Staurolite; Mafic; Hornblende; Granulite; Metamorphic rock; Craton; Pelite; Andalusite; Migmatite; Kyanite; Petrology; Facies; Geomorphology; Gneiss; Biotite; Paleontology","score_opus":0.026497914461425735,"score_gpt":0.20169458077766517,"score_spread":0.17519666631623942,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1765423974","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9877871,0.005840113,0.000010154907,0.0039087753,0.00042786784,0.00010384686,0.00008316219,0.0000038679755,0.0018350704],"genre_scores_gemma":[0.99784195,0.000034517856,0.0007293038,0.0008711968,0.0001846665,5.2253665e-7,0.0000041547028,0.0000015690297,0.00033211824],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99792445,0.00014078068,0.00044756389,0.00018900135,0.0006373084,0.0006609107],"domain_scores_gemma":[0.9982488,0.00014678502,0.00028846788,0.00018789685,0.00019542722,0.0009325864],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009755246,0.00017166077,0.00033880706,0.00026662552,0.00050021434,0.0001063675,0.0009728904,0.00007070645,0.0036875631],"category_scores_gemma":[0.00029779848,0.000092896924,0.00027344955,0.0010631816,0.0010598169,0.0004606501,0.000022660932,0.00022745861,0.000054933396],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008494804,0.00000970696,0.9959386,0.000011315647,0.000035026675,0.000004604612,0.00038427528,0.0013693142,0.00030542107,0.0002462489,0.00037558435,0.0013113848],"study_design_scores_gemma":[0.00008810387,0.00012324507,0.979792,0.000058987884,0.00006378331,0.000067847766,0.0007270858,0.00007026326,0.0015935305,0.0026959828,0.014567616,0.00015153857],"about_ca_topic_score_codex":0.022875063,"about_ca_topic_score_gemma":0.3139149,"teacher_disagreement_score":0.29103982,"about_ca_system_score_codex":0.0000016986617,"about_ca_system_score_gemma":0.0002863665,"threshold_uncertainty_score":0.9972232},"labels":[],"label_agreement":null},{"id":"W1767309897","doi":"10.1139/cjes-2014-0073","title":"“<i>Saurornitholestes</i>”<i>robustus</i>is a troodontid (Dinosauria: Theropoda)","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Holotype; Theropoda; Geology; Paleontology; Anatomy; Biology; Zoology; Taxonomy (biology); Cretaceous","score_opus":0.018054538131287903,"score_gpt":0.2038988054843067,"score_spread":0.1858442673530188,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1767309897","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94984895,0.0029255105,0.0002682457,0.0029897143,0.00161108,0.00006316617,0.000041264313,0.000009160567,0.042242907],"genre_scores_gemma":[0.99571913,0.000038290847,0.0018458584,0.0018070926,0.00032762304,1.2930609e-7,0.0000031302463,0.0000017141424,0.0002570522],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998459,0.00021248951,0.00032918347,0.00020793284,0.00022454264,0.000566867],"domain_scores_gemma":[0.99873316,0.00018722547,0.00022099164,0.00012488762,0.000109948865,0.00062376074],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012823708,0.00013625465,0.00024990778,0.0003261935,0.000623429,0.00007367551,0.00060841267,0.00011120746,0.0023402784],"category_scores_gemma":[0.00020348073,0.000099211975,0.00010464717,0.000392361,0.0011136541,0.000382443,0.0000037912696,0.00025508399,0.00020522579],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009665897,0.000003198269,0.99413216,0.0000024854958,0.000012742552,0.00003069185,0.0001644991,0.0004443643,0.000023624165,0.00030173233,0.0010632668,0.0038115508],"study_design_scores_gemma":[0.00021317137,0.0005383717,0.92229265,0.000020376981,0.000014643679,0.00051413296,0.00016881606,0.0009276967,0.00003582611,0.001959968,0.07317837,0.00013599716],"about_ca_topic_score_codex":0.004114717,"about_ca_topic_score_gemma":0.4188832,"teacher_disagreement_score":0.4147685,"about_ca_system_score_codex":0.0000013744581,"about_ca_system_score_gemma":0.000901385,"threshold_uncertainty_score":0.9985717},"labels":[],"label_agreement":null},{"id":"W1768029082","doi":"10.1139/e11-076","title":"Mineralogic evidences of a mid-Paleozoic tectono-thermal event in the Zonguldak terrane, northwest Turkey: implications for the dynamics of some Gondwana-derived terranes during the closure of the Rheic Ocean","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Sivas Cumhuriyet Üniversitesi","keywords":"Terrane; Geology; Devonian; Unconformity; Paleontology; Gondwana; Paleozoic; Basement; Ordovician; Siliciclastic; Sedimentary rock; Tectonics; Facies","score_opus":0.020864872669052893,"score_gpt":0.2196418857317857,"score_spread":0.1987770130627328,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1768029082","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98477346,0.004136468,0.0000051138,0.010507253,0.0001614584,0.00021252973,0.00011595665,0.0000010849235,0.00008668369],"genre_scores_gemma":[0.9995697,0.000058360536,0.000060620758,0.00018594126,0.00009613521,0.0000015252793,0.000003764177,0.0000013079438,0.000022647444],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984483,0.00017661043,0.00055068923,0.00012474798,0.0003081705,0.00039147687],"domain_scores_gemma":[0.99827534,0.00070262945,0.00052465143,0.00022742519,0.00012952794,0.0001404517],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001382342,0.00012578526,0.00026123368,0.0001266109,0.0004668639,0.000038851336,0.0014226167,0.00004791339,0.00023384037],"category_scores_gemma":[0.0002837813,0.000045745062,0.00027635196,0.00073497865,0.0014506498,0.00022909185,0.000014675712,0.00019166095,6.9698143e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009607783,0.000013313176,0.9893004,0.000018144867,0.000025472738,5.447182e-7,0.0007688014,0.008687455,0.0005651332,0.00008932389,0.000010302664,0.0005115385],"study_design_scores_gemma":[0.000109033695,0.00012677313,0.99515784,0.000045832454,0.000060866747,0.000038180282,0.0015048754,0.0010430765,0.0004301591,0.001321165,0.00009490928,0.00006726159],"about_ca_topic_score_codex":0.031620774,"about_ca_topic_score_gemma":0.53573996,"teacher_disagreement_score":0.5041192,"about_ca_system_score_codex":0.0000029409784,"about_ca_system_score_gemma":0.00029875428,"threshold_uncertainty_score":0.97482777},"labels":[],"label_agreement":null},{"id":"W1768479834","doi":"10.1139/e07-065","title":"Kimberlite-sourced bentonite, its paleoenvironment and implications for the Late Cretaceous K14 kimberlite cluster, northern AlbertaThis article is one of a selection of papers published in this Special Issue on the theme<i>Geology of northeastern British Columbia and northwestern Alberta: diamonds, shallow gas, gravel, and glaciers</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Alberta Energy; University of Alberta; Geological Survey of Canada","funders":"Natural Resources Canada; University of Alberta","keywords":"Kimberlite; Geology; Geochemistry; Zircon; Cenomanian; Craton; Xenolith; Paleontology; Cretaceous; Basalt; Mantle (geology)","score_opus":0.010641689200381813,"score_gpt":0.17654651957906706,"score_spread":0.16590483037868525,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1768479834","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946693,0.0012193554,0.000001621297,0.0031580273,0.000037595855,0.00021253427,0.00005952212,8.289465e-7,0.0006412228],"genre_scores_gemma":[0.9986112,0.00046541833,0.000056654473,0.00031520883,0.00006056889,0.0000019924662,0.000004448606,0.0000021359792,0.00048236447],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987398,0.00008279341,0.00046076986,0.00021401558,0.00020880139,0.0002938627],"domain_scores_gemma":[0.99854684,0.00065279164,0.00033453747,0.00010095194,0.000115400646,0.0002494875],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004697277,0.000104090264,0.0003079756,0.00008446847,0.00044524728,0.00012292432,0.00023371,0.000059579528,0.0029651204],"category_scores_gemma":[0.00017631406,0.00007612244,0.000078066914,0.00039820693,0.0010666647,0.0001528365,0.000012485997,0.00013617799,9.863855e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024896171,0.000019582527,0.99245113,0.000010833919,0.000036923215,0.0000017260238,0.0018389244,0.000411183,0.00012708234,0.0000029900593,0.000033454733,0.005041266],"study_design_scores_gemma":[0.0003254918,0.00042911267,0.994811,0.000031642034,0.00004647463,0.0000712533,0.0004065317,0.0020926613,0.00010999872,0.00039246483,0.0011977773,0.00008559747],"about_ca_topic_score_codex":0.27057555,"about_ca_topic_score_gemma":0.98595095,"teacher_disagreement_score":0.7153754,"about_ca_system_score_codex":0.0000022804584,"about_ca_system_score_gemma":0.000101153266,"threshold_uncertainty_score":0.9979463},"labels":[],"label_agreement":null},{"id":"W1772601770","doi":"10.1139/e07-052","title":"Failed predation in Late Ordovician gastropods (Mollusca) from Manitoulin Island, Ontario, CanadaThis article is one of a selection of papers published in this Special Issue on the theme<i>The dynamic reef and shelly communities of the Paleozoic. This Special is in honour of our colleague and friend Paul Copper</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Ordovician; Paleontology; Geology; Predation; Bay; Mollusca; Reef; Range (aeronautics); Oceanography; Ecology; Biology","score_opus":0.014095782286732106,"score_gpt":0.1936012891231544,"score_spread":0.1795055068364223,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1772601770","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98935366,0.00034361816,2.7084766e-7,0.0020367822,0.0001909194,0.00017259459,0.00018313271,5.118081e-7,0.0077185347],"genre_scores_gemma":[0.99954385,0.0001183231,0.000092495655,0.00009087208,0.00009396572,4.608283e-7,0.000001617381,0.0000010133732,0.000057393245],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99836737,0.0003599998,0.0005567927,0.00013023359,0.00034096575,0.00024465576],"domain_scores_gemma":[0.99899316,0.0002584151,0.00043788983,0.00013128498,0.00008265455,0.00009660175],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001141025,0.00011113466,0.00031829384,0.00031877885,0.0003196495,0.00003673699,0.00040626837,0.00007929383,0.0026991095],"category_scores_gemma":[0.000113149035,0.000069526635,0.000051728137,0.0006728683,0.0009559241,0.00028908072,0.0000048751967,0.00039036042,2.650392e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010306395,0.00001659218,0.975602,0.000005548424,0.000016994823,0.000007756815,0.021923257,0.00015857165,0.00010172552,0.000011239546,0.000293172,0.001760093],"study_design_scores_gemma":[0.00044378417,0.0003483976,0.98795867,0.00013337542,0.00001133376,0.000014138642,0.00927812,0.00087330566,0.00041918104,0.00028873174,0.00016518614,0.00006575593],"about_ca_topic_score_codex":0.6467064,"about_ca_topic_score_gemma":0.99933267,"teacher_disagreement_score":0.35262623,"about_ca_system_score_codex":0.000010423793,"about_ca_system_score_gemma":0.0011785778,"threshold_uncertainty_score":0.9982126},"labels":[],"label_agreement":null},{"id":"W1777568429","doi":"10.1139/cjes-2013-0160","title":"The geometry of the North Anatolian transform fault in the Sea of Marmara and its temporal evolution: implications for the development of intracontinental transform faults","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":125,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"North Anatolian Fault; Geology; Transform fault; Seismology; Fault (geology); Strike-slip tectonics; Structural basin; Echelon formation; Shear (geology); Context (archaeology); Bathymetry; Paleontology; Oceanography","score_opus":0.019524196766460424,"score_gpt":0.22855609707538482,"score_spread":0.2090319003089244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1777568429","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9904365,0.0027911228,0.00008548514,0.0054960204,0.00013866813,0.00027354603,0.0000899471,6.817913e-7,0.0006880283],"genre_scores_gemma":[0.9996813,0.00009837828,0.00012795473,0.00005004795,0.000026004089,0.0000015402599,0.0000012923085,0.0000010880428,0.000012412588],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988741,0.000058200305,0.00046121894,0.00008686464,0.00025167596,0.00026789322],"domain_scores_gemma":[0.9989011,0.00054693443,0.000242836,0.000097432145,0.00012648675,0.00008515416],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018199318,0.00008172096,0.00015862446,0.0001132464,0.0007628961,0.000026576809,0.0006216037,0.000025544095,0.000016259872],"category_scores_gemma":[0.000119823046,0.000033680797,0.00008267927,0.0006074888,0.0006919427,0.0001468035,0.00000386274,0.00013094091,2.710143e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010631994,0.000003646439,0.9550965,0.000014108465,0.000021503645,1.5088803e-7,0.0017723033,0.00022034916,0.0000040608925,0.00050522765,0.000021149657,0.042330384],"study_design_scores_gemma":[0.00020049882,0.00012888636,0.99328357,0.00003024323,0.000015480093,0.000019701138,0.0026566898,0.0005499555,0.0001527203,0.0004992852,0.0024170126,0.000045984274],"about_ca_topic_score_codex":0.0042536864,"about_ca_topic_score_gemma":0.769472,"teacher_disagreement_score":0.7652183,"about_ca_system_score_codex":0.0000025128622,"about_ca_system_score_gemma":0.000827044,"threshold_uncertainty_score":0.64303297},"labels":[],"label_agreement":null},{"id":"W1778966713","doi":"10.1139/e10-068","title":"Upper Cretaceous palynostratigraphy of the Dry Island areaThis article is one of a series of papers published in this Special Issue on the theme<i>Albertosaurus</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; University of Alberta","funders":"","keywords":"Geology; Canyon; Paleontology; Palynology; Unconformity; Group (periodic table); Cretaceous; Pollen; Structural basin; Geomorphology","score_opus":0.014132899117276174,"score_gpt":0.18034375210562253,"score_spread":0.16621085298834637,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1778966713","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9563256,0.00022451511,2.2174031e-7,0.009885015,0.00046059894,0.00009230901,0.000039079794,6.647915e-7,0.032972],"genre_scores_gemma":[0.9991754,0.00006528603,0.00009499615,0.000332076,0.0002177393,2.4823308e-7,5.6052653e-7,8.9698034e-7,0.00011276791],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988136,0.000077699435,0.00038313185,0.00011239878,0.0003782527,0.00023490348],"domain_scores_gemma":[0.9990848,0.00021995185,0.00031601675,0.00013518242,0.00011769485,0.00012637433],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008054764,0.00008551153,0.0002152208,0.00012187964,0.00023609973,0.000058854657,0.00044945115,0.00005167861,0.022662627],"category_scores_gemma":[0.00047806912,0.000040694304,0.00010715776,0.00066051044,0.0011276412,0.0002708776,0.00000726209,0.0002260338,0.000004601177],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029795276,0.000013846299,0.99204856,0.0000056024837,0.000016088163,0.00000310199,0.0033373309,0.00023464444,0.00047463994,0.00032903982,0.0013859024,0.002121453],"study_design_scores_gemma":[0.00014935853,0.0005764212,0.9718553,0.00005104058,0.000012423704,0.0000076122165,0.0027832026,0.0001000666,0.006181774,0.0020874233,0.01612097,0.000074436866],"about_ca_topic_score_codex":0.016431758,"about_ca_topic_score_gemma":0.6999647,"teacher_disagreement_score":0.68353295,"about_ca_system_score_codex":6.9923294e-7,"about_ca_system_score_gemma":0.00029094424,"threshold_uncertainty_score":0.9901179},"labels":[],"label_agreement":null},{"id":"W1780554789","doi":"10.1139/e11-035","title":"The Jackass Mountain Group of south-central British Columbia: depositional setting and evolution of an Early Cretaceous deltaic complex<sup>1</sup>This article is one of a series of papers published in this Special Issue on the theme of <i>New insights in Cordilleran Intermontane geoscience: reducing exploration risk in the mountain pine beetle-affected area, British Columbia</i>.<sup>2</sup>Earth Science Sector (ESS) Contribution 20100280.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Simon Fraser University","funders":"","keywords":"Geology; Facies; Sedimentology; Cretaceous; Group (periodic table); Paleontology; Sedimentary depositional environment; Petrography; Lithology; Stratigraphy; Geochemistry; Tectonics; Structural basin","score_opus":0.01450166571079257,"score_gpt":0.18379399543839553,"score_spread":0.16929232972760297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1780554789","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99845177,0.0004170132,0.000022034357,0.0001602505,0.00006951558,0.00038350731,0.00028844466,0.000002305735,0.00020517754],"genre_scores_gemma":[0.99939436,0.000092386945,0.00038084964,0.00004257135,0.000059498692,0.0000022083957,0.000012888507,0.000002313638,0.000012904901],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972136,0.00043010435,0.0009223175,0.00025143274,0.0007401614,0.000442408],"domain_scores_gemma":[0.9980986,0.00030628158,0.0007682739,0.0001486339,0.0004886574,0.00018954185],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0031725268,0.00010698221,0.00035479225,0.00024119731,0.00064353406,0.00046185203,0.00064365997,0.000078539895,0.0017378561],"category_scores_gemma":[0.000999761,0.00009519325,0.00005815769,0.0017226288,0.0024810699,0.0017617461,0.00002039538,0.00030593976,3.8245915e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000119342534,0.00008300057,0.9689873,0.000030188561,0.000014010811,0.000017611876,0.019378025,0.005565916,0.000689691,0.00006155392,0.00008091662,0.0049724537],"study_design_scores_gemma":[0.00054437993,0.0014059822,0.9660165,0.0003082947,0.000013999864,0.000081040605,0.012448868,0.01726629,0.00031104783,0.0014763377,0.00002184577,0.00010544511],"about_ca_topic_score_codex":0.6234683,"about_ca_topic_score_gemma":0.94282126,"teacher_disagreement_score":0.319353,"about_ca_system_score_codex":0.00002074758,"about_ca_system_score_gemma":0.00090248755,"threshold_uncertainty_score":0.9991747},"labels":[],"label_agreement":null},{"id":"W1781190018","doi":"10.1139/e2012-031","title":"Modelling and mapping permafrost at high spatial resolution in Wapusk National Park, Hudson Bay Lowlands<sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of<i>Fundamental and applied research on permafrost in Canada</i>.<sup>2</sup>Earth Science Sector Contribution 20110058.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; University of Alberta; Parks Canada; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada; University of Manitoba","keywords":"Permafrost; Land cover; Geology; Physical geography; Longitude; Peat; Elevation (ballistics); Latitude; Terrain; Active layer; Spatial distribution; Bay; Remote sensing; Land use; Cartography; Geography; Oceanography; Geodesy; Archaeology; Layer (electronics); Ecology","score_opus":0.05749576678632493,"score_gpt":0.2395883188661604,"score_spread":0.18209255207983546,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1781190018","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940001,0.000414352,6.899366e-7,0.0012122694,0.00013665909,0.00024529343,0.0018322787,9.152516e-7,0.0021574395],"genre_scores_gemma":[0.9992592,0.00015361182,0.00005018696,0.00014757978,0.00030380927,0.0000014978981,0.000052484156,0.0000034016987,0.000028266464],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970588,0.00019730823,0.0005910034,0.00027492273,0.0011755166,0.00070242235],"domain_scores_gemma":[0.9986272,0.00044975206,0.00024466295,0.0001129868,0.00021788002,0.00034754793],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0040771747,0.00015262143,0.00033994197,0.00086675305,0.00043693357,0.0001242288,0.00031632342,0.000069527094,0.005999227],"category_scores_gemma":[0.00023582652,0.00011559074,0.000032896445,0.0011159326,0.001319099,0.0007837528,0.000029696435,0.00034688704,0.0000037935763],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021792133,0.000025653382,0.96259767,0.000022989194,0.000006052257,0.0000055350956,0.009690023,0.025399812,0.0013767945,0.00024269694,0.00020998337,0.00020486889],"study_design_scores_gemma":[0.00083723187,0.00036497437,0.9233431,0.00031063103,0.0000055847313,0.00002521293,0.009225921,0.060531132,0.0038525553,0.00013751474,0.001179554,0.00018656113],"about_ca_topic_score_codex":0.59620184,"about_ca_topic_score_gemma":0.9491289,"teacher_disagreement_score":0.35292706,"about_ca_system_score_codex":0.00008834748,"about_ca_system_score_gemma":0.0018587267,"threshold_uncertainty_score":0.9949094},"labels":[],"label_agreement":null},{"id":"W1788302416","doi":"10.1139/e10-090","title":"Basaltic to andesitic volcaniclastic rocks in the Blake River Group, Abitibi Greenstone Belt: 1. Mode of emplacement in three areas<sup>1</sup>This article is a companion paper to Ross et al. 2011. Basaltic to andesitic volcaniclastic rocks in the Blake River Group, Abitibi Greenstone Belt: 2. Origin, geochemistry, and geochronology. Canadian Journal of Earth Sciences, 48: this issue.<sup>2</sup>MRNF Contribution BEGQ 8439-2010/2011-1. Natural Resources Canada, Earth Science Sector Contribution 20100253.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Ministère des Ressources naturelles et des Forêts (Québec); Institut National de la Recherche Scientifique","funders":"","keywords":"Pyroclastic rock; Geology; Mafic; Lava; Geochemistry; Volcanic rock; Breccia; Basalt; Felsic; Igneous rock; Rhyolite; Explosive eruption; Outcrop; Greenstone belt; Petrology; Volcano; Archean","score_opus":0.012620713896225143,"score_gpt":0.21231895030228884,"score_spread":0.19969823640606368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1788302416","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99028647,0.0013862102,0.0002194202,0.006738695,0.0002553116,0.00065243203,0.00030729186,0.000005649699,0.00014852258],"genre_scores_gemma":[0.99461794,0.0000323721,0.0003965735,0.004761711,0.0001037477,0.0000059487174,0.000024279105,0.000007744318,0.00004970881],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9938337,0.0005033668,0.0013439502,0.00083812367,0.0015930084,0.0018878042],"domain_scores_gemma":[0.9957702,0.00067095243,0.00052657694,0.00038541155,0.0008456708,0.0018011979],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0047268807,0.0005081569,0.0008990394,0.0012518233,0.0011172969,0.00031891602,0.0016882061,0.00018081215,0.0026846086],"category_scores_gemma":[0.0011496878,0.00034506118,0.00015613936,0.0024388756,0.002757958,0.0009582971,0.00006538456,0.000964965,0.000038229104],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018867732,0.00008899611,0.961262,0.000023413066,0.00004650334,0.00030911394,0.007596233,0.027355142,0.000977193,0.000094957075,0.001375326,0.00068247854],"study_design_scores_gemma":[0.0011778105,0.0012652826,0.95665574,0.0002862484,0.00009667933,0.00040162235,0.0015763892,0.036493946,0.00023592424,0.0006609614,0.0006798584,0.00046953373],"about_ca_topic_score_codex":0.9467426,"about_ca_topic_score_gemma":0.99848443,"teacher_disagreement_score":0.051741894,"about_ca_system_score_codex":0.00012490421,"about_ca_system_score_gemma":0.0035736149,"threshold_uncertainty_score":0.99995595},"labels":[],"label_agreement":null},{"id":"W1792063757","doi":"10.1139/cjes-2015-0063","title":"GIS analyses of ice-sheet erosional impacts on the exposed shield of Baffin Island, eastern Canadian Arctic","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Natural Resources Canada; University of Colorado Boulder","keywords":"Geology; Fjord; Ice sheet; Bedrock; Greenland ice sheet; Erosion; Arctic; Glacial period; Geomorphology; Physical geography; Oceanography; Ice stream; Cryosphere; Sea ice","score_opus":0.11017289758995706,"score_gpt":0.29131965739999677,"score_spread":0.1811467598100397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1792063757","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98846775,0.0010096608,0.00000261206,0.0029907718,0.000349379,0.00007004457,0.000068279754,9.157715e-7,0.0070406008],"genre_scores_gemma":[0.9993437,0.000019318753,0.00009751503,0.00037546753,0.00005405394,1.456838e-7,0.0000044589656,0.0000014446726,0.000103902996],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99820656,0.00027493935,0.0003791899,0.00014103363,0.0004612121,0.000537081],"domain_scores_gemma":[0.99744546,0.00067566504,0.0002629735,0.00015370158,0.00028256088,0.0011796225],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0020316767,0.00011228185,0.00027506045,0.0006772447,0.00028589103,0.000051076786,0.0007298062,0.00009070597,0.002476932],"category_scores_gemma":[0.001149426,0.000066829416,0.00009342452,0.000637132,0.001225023,0.00020695764,0.000005471003,0.0002910004,0.00006143766],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026842865,0.0000041757867,0.99555016,0.0000062375234,0.000022729106,0.000061597384,0.00050577964,0.0032837328,0.000014120743,0.00010120503,0.00028174126,0.0001416852],"study_design_scores_gemma":[0.00025425554,0.0009934277,0.9944787,0.00009462606,0.000019291669,0.0001502523,0.0013806763,0.001084142,0.0003813561,0.0007017143,0.0003652483,0.00009630251],"about_ca_topic_score_codex":0.4341667,"about_ca_topic_score_gemma":0.9951248,"teacher_disagreement_score":0.56095815,"about_ca_system_score_codex":0.0000018780792,"about_ca_system_score_gemma":0.005795625,"threshold_uncertainty_score":0.9998406},"labels":[],"label_agreement":null},{"id":"W1794351417","doi":"10.1139/cjes-2013-0075","title":"Late Holocene glacial history of Scimitar Glacier, Mt. Waddington area, British Columbia Coast Mountains, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Moraine; Geology; Glacier; Glacial period; Holocene; Physical geography; Glacier mass balance; Tidewater glacier cycle; Glacier morphology; Radiocarbon dating; Period (music); Geomorphology; Archaeology; Paleontology; Oceanography; Ice stream; Geography; Cryosphere; Sea ice","score_opus":0.01726088947686275,"score_gpt":0.1892091778329089,"score_spread":0.17194828835604614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1794351417","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9885551,0.0031719145,0.0000017214783,0.00049527443,0.0014141138,0.00010578548,0.00006474781,0.0000031912066,0.00618817],"genre_scores_gemma":[0.9966502,0.00008007769,0.00020766431,0.00041492766,0.00007684135,4.129039e-7,0.00000937943,0.0000023972295,0.0025580695],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979647,0.00014989702,0.00044642636,0.00021971611,0.00047116395,0.00074810156],"domain_scores_gemma":[0.99817604,0.00018309584,0.0002830598,0.00011893311,0.00034666932,0.00089219905],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009770547,0.00010727652,0.0003322001,0.00020875024,0.00047853639,0.00016013617,0.00070241914,0.00010958062,0.011635857],"category_scores_gemma":[0.00028603908,0.00012333176,0.000072825926,0.00036780868,0.0017764388,0.00048500716,0.000009496011,0.0003473748,0.000028560511],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000041008702,0.0000036275499,0.98184997,0.000008849544,0.000012993818,0.00022882276,0.00011360314,0.00033442202,0.0000045360553,0.0000033390347,0.016376397,0.001059346],"study_design_scores_gemma":[0.00022255688,0.00023897168,0.9860759,0.000046441673,0.000009776347,0.0005188001,0.00030904685,0.00070235686,0.000006140223,0.00023462762,0.011496761,0.00013862949],"about_ca_topic_score_codex":0.9915376,"about_ca_topic_score_gemma":0.9999402,"teacher_disagreement_score":0.013044253,"about_ca_system_score_codex":0.000009918423,"about_ca_system_score_gemma":0.013054172,"threshold_uncertainty_score":0.9925409},"labels":[],"label_agreement":null},{"id":"W1797827191","doi":"10.1139/cjes-2014-0176","title":"An edentulous frog (Lissamphibia; Anura) from the Upper Cretaceous (Campanian) Dinosaur Park Formation of southeastern Alberta, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Amphibian and Reptile Biology","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Cretaceous; Paleontology; Geology; Mesozoic; Laurasia; Sauropoda; Vertebrate; Biology; Structural basin","score_opus":0.01795789881650406,"score_gpt":0.21200703058207343,"score_spread":0.19404913176556937,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1797827191","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99522734,0.00024574748,0.000065301356,0.0012933105,0.0006707988,0.00008352225,0.000042751508,0.0000017405829,0.0023694707],"genre_scores_gemma":[0.99886394,0.0000065149598,0.00025834385,0.0005029903,0.00015145152,5.146741e-7,0.0000039063852,0.0000048285724,0.00020753994],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851966,0.00013826291,0.00036388892,0.00016514819,0.0004474001,0.0003656296],"domain_scores_gemma":[0.99854136,0.00008485567,0.0003324544,0.00019273597,0.00004593413,0.0008026577],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053921517,0.00011787081,0.00018632972,0.00005170469,0.0002590563,0.00007772679,0.00074270484,0.00005773505,0.0007704242],"category_scores_gemma":[0.000115163624,0.00007247322,0.000057547008,0.0002164023,0.0007708374,0.00045814415,0.00002502286,0.00012413911,0.000038664002],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013655556,0.000010296932,0.98904455,0.0000011656324,0.0000089796995,0.000029936684,0.0035673757,0.0019554442,0.00034651684,0.000023219025,0.0028699806,0.002128856],"study_design_scores_gemma":[0.00071372004,0.0008122856,0.88821304,0.000081057144,0.00004692464,0.000495844,0.015841382,0.0036098468,0.0012821933,0.00064245635,0.08783616,0.00042507268],"about_ca_topic_score_codex":0.9043998,"about_ca_topic_score_gemma":0.99781185,"teacher_disagreement_score":0.10083152,"about_ca_system_score_codex":0.00003228382,"about_ca_system_score_gemma":0.0013370917,"threshold_uncertainty_score":0.8435605},"labels":[],"label_agreement":null},{"id":"W1798463790","doi":"10.1139/e2012-042","title":"Stratigraphy of the upper Hazelton Group and the Jurassic evolution of the Stikine terrane, British Columbia<sup>1</sup>ESS Contribution 20120051.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Dalhousie University; University of Alberta","funders":"","keywords":"Geology; Terrane; Rift; Unconformity; Paleontology; Group (periodic table); Diachronous; Facies; Stratigraphy; Sedimentary rock; Structural basin; Geochemistry; Tectonics","score_opus":0.006741679491690722,"score_gpt":0.16571035355653577,"score_spread":0.15896867406484505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1798463790","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99270415,0.0050599845,0.000013162477,0.0010972888,0.00018957036,0.00010433918,0.00009876005,0.0000010971493,0.0007316385],"genre_scores_gemma":[0.9996351,0.000043552984,0.000047774403,0.0001248707,0.00008098825,2.7429235e-7,0.00000201467,6.3293464e-7,0.00006476275],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998634,0.00021986493,0.00034393524,0.00010098974,0.00037217714,0.00032906793],"domain_scores_gemma":[0.9990276,0.00016580963,0.00032118478,0.00010646847,0.00012991735,0.00024901432],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013265271,0.00007045447,0.00021484983,0.00004978144,0.0005232897,0.00012047651,0.00044934606,0.000054781634,0.001148362],"category_scores_gemma":[0.00027264876,0.00003716761,0.00017744307,0.0006773423,0.002296729,0.00029649187,0.0000112504795,0.00019188573,0.0000013700192],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006099346,0.0000064606697,0.99735445,0.000003855094,0.000014651776,5.179059e-7,0.00008991862,0.0005016591,0.000035907946,0.00022032944,0.00018447445,0.0015816719],"study_design_scores_gemma":[0.00025553975,0.00008344014,0.99231917,0.000048413458,0.000052187697,0.000061989405,0.000292931,0.0013893227,0.000041400297,0.004673782,0.00072611397,0.00005569037],"about_ca_topic_score_codex":0.26513764,"about_ca_topic_score_gemma":0.8501806,"teacher_disagreement_score":0.585043,"about_ca_system_score_codex":0.0000019876545,"about_ca_system_score_gemma":0.00021696796,"threshold_uncertainty_score":0.99976474},"labels":[],"label_agreement":null},{"id":"W1802744687","doi":"10.1139/e09-033","title":"Petrogenesis of the 1.9 Ga mafic hanging wall sequence to the Flin Flon, Callinan, and Triple 7 massive sulphide deposits, Flin Flon, Manitoba, CanadaThis is a companion paper to DeWolfe, Y.M., Gibson, H.L., Lafrance , B., and Bailes, A.H. 2009. Volcanic reconstruction of Paleoproterozoic arc volcanoes: the Hidden and Louis formations, Flin Flon, Manitoba, Canada. Canadian Journal of Earth Sciences, <b>46</b>: this issue.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Mafic; Basaltic andesite; Basalt; Geochemistry; Andesite; Petrogenesis; Volcanic rock; Volcano","score_opus":0.01558218690456718,"score_gpt":0.18659414114057582,"score_spread":0.17101195423600865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1802744687","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9736974,0.007728879,0.00003210971,0.017309252,0.00038768296,0.00036287773,0.00039236344,0.0000023719817,0.00008703111],"genre_scores_gemma":[0.99595994,0.0003563364,0.0012455826,0.0022077034,0.0001451218,0.0000015762132,0.0000043784894,0.000004316047,0.00007503261],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99667686,0.0002738001,0.0010466983,0.00038273403,0.0008320198,0.0007878889],"domain_scores_gemma":[0.9969557,0.00021374355,0.00074480445,0.0002654556,0.00064264436,0.0011776738],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.001787655,0.0003010552,0.0005539662,0.00050007127,0.0016239523,0.0003193834,0.001107506,0.000088816145,0.00044626242],"category_scores_gemma":[0.00045356664,0.0001717406,0.00012415138,0.0017267435,0.0010901453,0.0005049138,0.000029554212,0.00039138083,0.0000025715715],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003746703,0.000008758642,0.96785057,0.00004637633,0.00007304302,0.0000837379,0.0017401439,0.0032227214,0.00063875876,0.00006545187,0.0029342496,0.023298722],"study_design_scores_gemma":[0.00036911154,0.00062542135,0.97460186,0.00045481618,0.00016039769,0.0013269153,0.005140992,0.0037853897,0.0023412327,0.00084005686,0.009962455,0.00039137056],"about_ca_topic_score_codex":0.9367716,"about_ca_topic_score_gemma":0.9996254,"teacher_disagreement_score":0.06285383,"about_ca_system_score_codex":0.000032752625,"about_ca_system_score_gemma":0.004245,"threshold_uncertainty_score":0.9996758},"labels":[],"label_agreement":null},{"id":"W1805219736","doi":"10.1139/cjes-2014-0200","title":"Origins of dinosaur bonebeds in the Cretaceous of Alberta, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Geology; Cretaceous; Paleontology; Taphonomy; Canyon; Paleoecology; Geomorphology","score_opus":0.024375039282752833,"score_gpt":0.21440880194266487,"score_spread":0.19003376265991204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1805219736","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9847393,0.0028056032,0.0000023541836,0.0014353596,0.00053064397,0.000034285105,0.000024752422,2.909289e-7,0.010427426],"genre_scores_gemma":[0.9995764,0.000016017855,0.00011742189,0.0002159849,0.000040246567,5.664733e-8,0.0000018167095,3.8649188e-7,0.000031658295],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989995,0.00014053017,0.0002984526,0.000076111566,0.00022463658,0.000260785],"domain_scores_gemma":[0.9991108,0.00026276318,0.00020171577,0.00007368782,0.000090212336,0.00026083062],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010084216,0.00005973352,0.00017618839,0.00017502002,0.0000873743,0.000008066276,0.00049823715,0.000042753214,0.00019757947],"category_scores_gemma":[0.0002680345,0.000036410616,0.000032160497,0.00039828836,0.0007042843,0.00014305254,0.0000017638271,0.00012369487,0.000002852536],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008483167,0.000002268081,0.99624056,0.0000020518087,0.00000474885,0.000052249143,0.0004389407,0.0019091343,0.0000021013886,0.000443514,0.00049630186,0.00039967016],"study_design_scores_gemma":[0.00012703393,0.0002931518,0.9709351,0.000013150031,0.0000053468,0.00027355904,0.001098482,0.00029789924,0.00001474408,0.0005900144,0.026304575,0.000046944457],"about_ca_topic_score_codex":0.97798395,"about_ca_topic_score_gemma":0.99989444,"teacher_disagreement_score":0.025808273,"about_ca_system_score_codex":0.000006297602,"about_ca_system_score_gemma":0.0070737517,"threshold_uncertainty_score":0.99855524},"labels":[],"label_agreement":null},{"id":"W1805487525","doi":"10.1139/e2012-057","title":"A Sault-outlet-referenced mid- to late-Holocene paleohydrograph for Lake Superior constructed from strandplains of beach ridges","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"College of Family Physicians of Canada","funders":"U.S. Forest Service; U.S. Geological Survey; Michigan Department of Natural Resources","keywords":"Geology; Water level; Physical geography; Hydrology (agriculture); Geography; Cartography","score_opus":0.0354905891508588,"score_gpt":0.25562370819105046,"score_spread":0.22013311904019167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1805487525","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99528646,0.0016218203,0.00003371415,0.0006109051,0.0006815512,0.00018155246,0.00066127453,0.000004472188,0.0009182424],"genre_scores_gemma":[0.9966535,0.000019197018,0.0030088853,0.0001312139,0.00010311349,8.743257e-7,0.0000466761,0.000002251689,0.000034312416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99819547,0.00013539805,0.00041477138,0.00018476113,0.00026734234,0.0008022583],"domain_scores_gemma":[0.9979535,0.00046648388,0.00016898965,0.00012013029,0.0002078265,0.0010831136],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011032858,0.00014008043,0.000365209,0.0005531855,0.00040235664,0.000056350138,0.0005551069,0.00013564121,0.00198406],"category_scores_gemma":[0.0002978892,0.00010707721,0.00011376677,0.00059480564,0.0011846664,0.0003133653,0.0000051805523,0.00021530675,0.000023975932],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000049695744,0.0000069723455,0.9981254,0.000008156432,0.00003278356,0.0000133931,0.00059625827,0.0002250476,0.00008088689,0.00003423991,0.00006824335,0.00075895205],"study_design_scores_gemma":[0.00043380578,0.00046651473,0.99534816,0.000040315805,0.000024073537,0.00007953858,0.00067078666,0.00007632597,0.000943847,0.00024553077,0.0015395118,0.00013159952],"about_ca_topic_score_codex":0.004871195,"about_ca_topic_score_gemma":0.5327664,"teacher_disagreement_score":0.5278952,"about_ca_system_score_codex":4.0822374e-7,"about_ca_system_score_gemma":0.0009613263,"threshold_uncertainty_score":0.99892825},"labels":[],"label_agreement":null},{"id":"W1806885152","doi":"10.1139/cjes-2013-0108","title":"Post-convergent structures in lower parts of the 1090–1050 Ma (early-Ottawan) thrust-sheet stack, Grenville Province of Ontario, southern Canadian Shield","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Iron Ore Company (Canada); Emissions Reduction Alberta; Memorial University of Newfoundland; University of Toronto","funders":"","keywords":"Geology; Lineation; Gneiss; Pluton; Flattening; Seismology; Petrology; Metamorphic rock; Tectonics","score_opus":0.008851473142223029,"score_gpt":0.16842595708243094,"score_spread":0.1595744839402079,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1806885152","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.992405,0.00027608007,0.0000016280859,0.0011268572,0.00033966932,0.00008544215,0.00011156985,0.0000010032272,0.0056527355],"genre_scores_gemma":[0.99909735,0.0000035886333,0.00015613968,0.00036987773,0.000047569636,1.4660277e-7,0.000002626143,0.000001568485,0.00032112014],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998226,0.00011219157,0.00050575513,0.00020523129,0.00042735488,0.0005234636],"domain_scores_gemma":[0.9985406,0.00009389441,0.00032649303,0.00017986429,0.0001355275,0.00072363525],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007710316,0.00014378873,0.00032354656,0.0002797022,0.00020514311,0.000054142503,0.000797782,0.00008445659,0.0145194605],"category_scores_gemma":[0.0002474884,0.00008254287,0.00017139188,0.00048937043,0.00075383106,0.0001385405,0.00001189642,0.0002729558,0.00001322161],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010301914,0.000004740398,0.99196184,0.0000058098476,0.00001293947,0.000017808617,0.00068353146,0.0057554063,0.000028683851,0.0001079409,0.000042391814,0.001368638],"study_design_scores_gemma":[0.00014786975,0.00036777093,0.992,0.00004135727,0.000019585961,0.000014812961,0.0004246774,0.00036213975,0.00032631232,0.003161279,0.003001224,0.00013297668],"about_ca_topic_score_codex":0.9777059,"about_ca_topic_score_gemma":0.99981254,"teacher_disagreement_score":0.022106659,"about_ca_system_score_codex":0.000010685,"about_ca_system_score_gemma":0.0035253314,"threshold_uncertainty_score":0.9863814},"labels":[],"label_agreement":null},{"id":"W1807458611","doi":"10.1139/cjes-2014-0189","title":"Marine turtles from the Late Cretaceous of Alberta, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; Royal Tyrrell Museum","funders":"","keywords":"Geology; Postcrania; Carapace; Cretaceous; Paleontology; Turtle (robot); Taxon; Biology; Ecology","score_opus":0.01942817841984346,"score_gpt":0.19168317627305215,"score_spread":0.1722549978532087,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1807458611","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97829247,0.003460103,0.0000033349052,0.0032790394,0.00100705,0.000026493482,0.000056051776,7.3466015e-7,0.013874751],"genre_scores_gemma":[0.9987676,0.000023468305,0.0002664775,0.0005044958,0.00011360613,3.834256e-8,0.0000071563877,5.6711383e-7,0.00031660422],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99915296,0.000106488995,0.00022283154,0.00007813564,0.00018109026,0.00025850398],"domain_scores_gemma":[0.99885947,0.0003652873,0.00016956466,0.000079087964,0.000099162215,0.00042741044],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005171694,0.00006678447,0.00014749104,0.000060197235,0.0001990299,0.000018316412,0.0004862622,0.00004159796,0.001438465],"category_scores_gemma":[0.00030033567,0.000038885548,0.00003313122,0.0001926635,0.00071828504,0.00013577976,0.000004459406,0.00012352255,0.0000152553075],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009962004,7.2758803e-7,0.99436426,4.4060033e-7,0.00001228118,0.0000342987,0.0002016111,0.002276075,0.0000012266773,0.000036638456,0.0017326762,0.0013297725],"study_design_scores_gemma":[0.0000986248,0.00013082291,0.9601661,0.0000072848666,0.000008762835,0.00010996294,0.00044960104,0.0006040707,0.000011339095,0.0011906244,0.037170533,0.00005228803],"about_ca_topic_score_codex":0.9917399,"about_ca_topic_score_gemma":0.9999573,"teacher_disagreement_score":0.035437856,"about_ca_system_score_codex":0.0000023160703,"about_ca_system_score_gemma":0.0057797614,"threshold_uncertainty_score":0.99985653},"labels":[],"label_agreement":null},{"id":"W1808183113","doi":"10.1139/cjes-2015-0091","title":"Silurian conodont biostratigraphy and carbon (δ<sup>13</sup>C<sub>carb</sub>) isotope stratigraphy of the Victor Mine (V-03-270-AH) core in the Moose River Basin","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Conodont; Geology; Chemostratigraphy; Biostratigraphy; Paleontology; Carbonate; Isotopes of carbon; Structural basin; Stratigraphy; Dolostone; Total organic carbon; Carbonate rock; Sedimentary rock","score_opus":0.025954277731820026,"score_gpt":0.20894839266903395,"score_spread":0.18299411493721393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1808183113","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97188735,0.00887053,0.0000010274979,0.0012283145,0.00030898253,0.00022915643,0.000093583774,0.0000030937458,0.017377988],"genre_scores_gemma":[0.9994114,0.00007613464,0.00017530895,0.00024049035,0.00008655258,6.6900935e-7,0.0000013279068,0.0000013280134,0.0000067657165],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99783623,0.00028586327,0.00056320144,0.00026357785,0.00052405766,0.00052703876],"domain_scores_gemma":[0.998393,0.00024446475,0.00037816484,0.00023240746,0.00014243327,0.00060952647],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0017907775,0.00022532183,0.00036542557,0.0005369649,0.00035628068,0.00014132123,0.00091987883,0.00013291686,0.000033951612],"category_scores_gemma":[0.0001613266,0.00013006381,0.00016983523,0.0011896733,0.002880346,0.0004176518,0.0000028315783,0.00039921506,0.0000011042334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024677805,0.000010918947,0.9927542,0.0000075367443,0.000021766191,0.00006964895,0.002988998,0.00037810716,0.000105755054,0.00027766282,0.0002057013,0.003154977],"study_design_scores_gemma":[0.00045263348,0.0006131571,0.9918254,0.000074600284,0.00002939905,0.00018398179,0.0027091478,0.00096702814,0.00028708114,0.0023156023,0.0003790503,0.00016290614],"about_ca_topic_score_codex":0.04015871,"about_ca_topic_score_gemma":0.7656656,"teacher_disagreement_score":0.7255069,"about_ca_system_score_codex":0.0000017245087,"about_ca_system_score_gemma":0.0015113433,"threshold_uncertainty_score":0.9998332},"labels":[],"label_agreement":null},{"id":"W1811163103","doi":"10.1139/e07-045","title":"Environmental control on temporal and spatial differentiation of Early Silurian pentameride brachiopod communities, Anticosti Island, eastern CanadaThis article is one of a selection of papers published in this Special Issue on the theme<i>The dynamic reef and shelly communities of the Paleozoic. This Special is in honour of our colleague and friend Paul Copper</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Substrate (aquarium); Ecological succession; Range (aeronautics); Fauna; Geology; Ecology; Carbonate; Paleontology; Geography; Oceanography; Physical geography; Biology; Chemistry","score_opus":0.012149429809389588,"score_gpt":0.1858427651548053,"score_spread":0.1736933353454157,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1811163103","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962557,0.0004275711,5.660789e-7,0.0011267561,0.00013108054,0.00018531654,0.00038489234,3.9385282e-7,0.0014877327],"genre_scores_gemma":[0.99964523,0.00017393126,0.00001567131,0.000083034865,0.00006499013,3.2921787e-7,0.0000018182366,0.0000011949663,0.000013769279],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984456,0.00043076588,0.0004914343,0.00009189813,0.00034935394,0.00019096366],"domain_scores_gemma":[0.99890614,0.0003060242,0.0005354276,0.00012379144,0.000036411995,0.000092188384],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00074846094,0.000113431975,0.00033554214,0.0002341171,0.00036172775,0.000030826057,0.00031165127,0.000059872073,0.00081727456],"category_scores_gemma":[0.0000501025,0.000071461945,0.000051325544,0.00023403433,0.0016481621,0.00020821001,0.000005524499,0.00029961098,1.1261202e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020320855,0.00003149593,0.9836421,0.0000104284345,0.000027495305,0.000002781099,0.0133802695,0.000024292825,0.00020306538,0.00000991096,0.000058473404,0.0024064807],"study_design_scores_gemma":[0.00070980215,0.00095013104,0.9856684,0.0001226118,0.000019265168,0.00002876409,0.01090213,0.0009110664,0.00052754954,0.000057492565,0.000036789428,0.00006596194],"about_ca_topic_score_codex":0.24142097,"about_ca_topic_score_gemma":0.9505596,"teacher_disagreement_score":0.7091387,"about_ca_system_score_codex":0.000004147419,"about_ca_system_score_gemma":0.00033673015,"threshold_uncertainty_score":0.89485836},"labels":[],"label_agreement":null},{"id":"W1815808211","doi":"10.1139/cjes-2013-0175","title":"John Tuzo Wilson: a man who moved mountains","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia; Earthgen; University of Toronto","funders":"","keywords":"Plate tectonics; Tribute; Geology; Tectonics; Earth science; History; Environmental ethics; Archaeology; Paleontology; Philosophy","score_opus":0.013459797676333275,"score_gpt":0.18634913162532069,"score_spread":0.17288933394898742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1815808211","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.961797,0.0006063902,0.000089865185,0.0029714524,0.00021624194,0.000029969031,0.000012370056,0.000004923709,0.03427181],"genre_scores_gemma":[0.99700797,0.0000207434,0.00090412603,0.0015373593,0.0002119257,7.969314e-8,0.000002731066,9.839939e-7,0.00031411133],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99859273,0.00008253569,0.00030028768,0.00018699565,0.0003382491,0.0004992067],"domain_scores_gemma":[0.9985292,0.00012195774,0.0001631891,0.00009943462,0.00011102955,0.000975207],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00088320643,0.00011697944,0.0002501754,0.00024665118,0.00039980334,0.00018648022,0.0005702764,0.000052834697,0.009242458],"category_scores_gemma":[0.00028891565,0.00007466254,0.00013696899,0.00063889945,0.0005692194,0.00029202682,0.000005452956,0.00018561936,0.00015732327],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045883894,0.0000033819042,0.9883493,0.0000029427806,0.0000126771765,0.000037659975,0.000081854705,0.002398668,0.000033429093,0.00053101813,0.00039618585,0.008148253],"study_design_scores_gemma":[0.00015604109,0.00042137387,0.9220206,0.000027009213,0.000021581807,0.0000954214,0.00018207775,0.010221945,0.00014553223,0.018624486,0.047896296,0.00018762138],"about_ca_topic_score_codex":0.032158237,"about_ca_topic_score_gemma":0.5075652,"teacher_disagreement_score":0.475407,"about_ca_system_score_codex":0.0000013246449,"about_ca_system_score_gemma":0.00034892082,"threshold_uncertainty_score":0.9916632},"labels":[],"label_agreement":null},{"id":"W1816943236","doi":"10.1139/e10-092","title":"Geochemical signature of Ordovician Mn-rich sedimentary rocks on the Avalonian shelf","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Deutscher Akademischer Austauschdienst","keywords":"Geology; Clastic rock; Ordovician; Sedimentary rock; Siliciclastic; Geochemistry; Volcanic rock; Facies; Petrology; Paleontology; Volcano","score_opus":0.018534867583277992,"score_gpt":0.18780901192377386,"score_spread":0.16927414434049587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1816943236","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97138566,0.00050390733,0.0000023848238,0.001189612,0.0002112294,0.00004228713,0.000072148316,0.000002054232,0.026590696],"genre_scores_gemma":[0.9987369,0.000010453815,0.00022051192,0.0007620301,0.00009989479,1.1668341e-7,0.000007713136,0.000001282058,0.00016105267],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987587,0.0000541321,0.00030337984,0.00014946042,0.00037578863,0.00035857942],"domain_scores_gemma":[0.99905306,0.00008810162,0.00021254222,0.00012356714,0.000082971594,0.00043977745],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006919716,0.000114423274,0.00017071064,0.0001631004,0.00038224005,0.000045596895,0.00067514804,0.000057501376,0.010896988],"category_scores_gemma":[0.00007029733,0.000068397734,0.000112556176,0.0005540363,0.0004805487,0.00018201399,0.000006030517,0.0002637699,0.000037923106],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021597416,0.000017527116,0.9942869,0.000007697568,0.000059477847,0.00007500266,0.0010705433,0.0006463272,0.00037696134,0.00007703814,0.0015298895,0.0018310567],"study_design_scores_gemma":[0.0003932806,0.0015260521,0.89547837,0.00019102532,0.00015605062,0.00023896237,0.0073802713,0.00078993256,0.07377754,0.0041816705,0.015389333,0.00049754453],"about_ca_topic_score_codex":0.022013014,"about_ca_topic_score_gemma":0.15839475,"teacher_disagreement_score":0.13638175,"about_ca_system_score_codex":0.0000020783355,"about_ca_system_score_gemma":0.00049580197,"threshold_uncertainty_score":0.99000716},"labels":[],"label_agreement":null},{"id":"W1818614918","doi":"10.1139/e09-008","title":"Sedimentology of perennial ice-covered, meromictic Lake A, Ellesmere Island, at the northern extreme of CanadaPolar Continental Shelf Program Contribution 00109.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université Laval; Queen's University","funders":"","keywords":"Geology; Sedimentology; Sedimentary rock; Sedimentary structures; Oceanography; Chemocline; Varve; Algal mat; Meltwater; Sedimentary depositional environment; Facies; Sediment; Paleontology; Geochemistry; Water column; Glacial period; Ecology; Structural basin","score_opus":0.011198228699244363,"score_gpt":0.213415018387738,"score_spread":0.20221678968849363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1818614918","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943067,0.00068323256,0.000006946515,0.0018447858,0.0003022275,0.00019140742,0.000068092086,0.0000018973184,0.0025947427],"genre_scores_gemma":[0.99933845,0.000030429632,0.000086609005,0.00017491028,0.000044563243,7.353521e-7,0.0000053987465,0.0000034924958,0.0003154121],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984625,0.00010676927,0.00046780036,0.00015989011,0.00039313472,0.0004099009],"domain_scores_gemma":[0.9989258,0.000055580953,0.0005040941,0.00012462866,0.00005833522,0.0003315814],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000742555,0.0001236734,0.0002671813,0.0000914059,0.00031278643,0.000027753493,0.00041995329,0.000072293384,0.0026777538],"category_scores_gemma":[0.000062651096,0.00007814741,0.000105602165,0.0003549087,0.0010103973,0.00016290994,0.00001814817,0.00018352797,0.000011950137],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001320439,0.000127839,0.9625129,0.000008021602,0.000110559675,0.000086678316,0.002220478,0.0062351786,0.01636905,0.00029469034,0.0017838589,0.01011872],"study_design_scores_gemma":[0.0036035196,0.004915346,0.83637345,0.0001791904,0.00026739397,0.00082592893,0.0019852635,0.0026545525,0.012280699,0.00078251935,0.1354914,0.00064071675],"about_ca_topic_score_codex":0.031087087,"about_ca_topic_score_gemma":0.8849364,"teacher_disagreement_score":0.85384935,"about_ca_system_score_codex":0.000039923296,"about_ca_system_score_gemma":0.00041768985,"threshold_uncertainty_score":0.9982339},"labels":[],"label_agreement":null},{"id":"W1821706316","doi":"10.1139/cjes-2014-0144","title":"A new tribotherian (Mammalia, Boreosphenida) from the late Santonian to early Campanian upper Milk River Formation, Alberta","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Dirección General de Asuntos del Personal Académico, Universidad Nacional Autónoma de México","keywords":"Geology; Molar; Paleontology; Mammal","score_opus":0.027341617494102716,"score_gpt":0.21889109663686795,"score_spread":0.19154947914276524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1821706316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9701131,0.0024956171,0.00020106649,0.016341126,0.0011151959,0.00011440705,0.000054338456,0.000004953355,0.009560215],"genre_scores_gemma":[0.99332273,0.000021387566,0.0025215263,0.0023066776,0.0003460745,2.3588451e-7,0.000003518762,0.0000023531818,0.0014754776],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985681,0.00013309017,0.00034159076,0.00014084944,0.00035196266,0.000464368],"domain_scores_gemma":[0.99794036,0.00025497182,0.00018755198,0.00013528578,0.0001495613,0.0013322836],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007421014,0.0001336491,0.0002210696,0.00015413949,0.00059385254,0.00021767487,0.0006052206,0.00005621117,0.0013978078],"category_scores_gemma":[0.00035728456,0.000083023624,0.000085970234,0.0005338618,0.00041580334,0.0005959543,0.0000057754846,0.00014911292,0.00037886953],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015391393,0.0000010142248,0.9702213,5.4846385e-7,0.000018538283,0.000013077378,0.012678131,0.0003487396,0.0000012560861,0.00006021365,0.01359588,0.0030459207],"study_design_scores_gemma":[0.00018962276,0.00017049623,0.8817881,0.000028544033,0.000015041687,0.000037695558,0.0019719219,0.00012719918,0.000008739291,0.0007154767,0.11483143,0.000115729206],"about_ca_topic_score_codex":0.4878691,"about_ca_topic_score_gemma":0.99095845,"teacher_disagreement_score":0.5030893,"about_ca_system_score_codex":0.0000045910515,"about_ca_system_score_gemma":0.0018223501,"threshold_uncertainty_score":0.99951506},"labels":[],"label_agreement":null},{"id":"W1824687917","doi":"10.1139/cjes-2012-0098","title":"<i>Scolosaurus cutleri</i> (Ornithischia: Ankylosauria) from the Upper Cretaceous Dinosaur Park Formation of Alberta, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Cretaceous; Holotype; Taxon; Paleontology; Fauna; Taxonomy (biology); Biology; Zoology; Ecology","score_opus":0.01138611034951449,"score_gpt":0.18126628664455144,"score_spread":0.16988017629503696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1824687917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98092055,0.0035461967,0.000013163151,0.0067298603,0.0010584105,0.00011434313,0.00012061057,0.0000016773341,0.0074951686],"genre_scores_gemma":[0.99803823,0.000049861912,0.0002975536,0.0013409337,0.00016013496,5.6839605e-7,0.00001814833,0.0000011626908,0.00009338339],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99856544,0.00017644143,0.0004107035,0.00013542653,0.00025064903,0.0004613574],"domain_scores_gemma":[0.9984556,0.00056492543,0.00032540524,0.00012429382,0.00015126502,0.00037853557],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004404905,0.00011571138,0.00021707609,0.00009702655,0.00061769964,0.00005187523,0.00061090157,0.00008291094,0.003405395],"category_scores_gemma":[0.00024873504,0.00007098812,0.00006586266,0.0002674049,0.00073918275,0.0005933044,0.0000054394577,0.00021590348,0.0000597508],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000733108,0.0000019931567,0.99165046,0.0000022034387,0.000015730004,0.000014378374,0.00028429856,0.00060313113,0.000021114603,0.000049087343,0.006127722,0.0012225533],"study_design_scores_gemma":[0.00012099191,0.0001534433,0.96643454,0.000020725975,0.00001529082,0.00015967527,0.0007218065,0.0010082785,0.00006600487,0.0007272083,0.030475276,0.00009677115],"about_ca_topic_score_codex":0.9686452,"about_ca_topic_score_gemma":0.9995427,"teacher_disagreement_score":0.030897481,"about_ca_system_score_codex":0.0000047107856,"about_ca_system_score_gemma":0.0030996879,"threshold_uncertainty_score":0.9975056},"labels":[],"label_agreement":null},{"id":"W1826023556","doi":"10.1139/cjes-2011-0115","title":"The Drift des Demoiselles on the Magdalen Islands (Québec, Canada): sedimentological and micromorphological evidence of a Late Wisconsinan glacial diamict","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Rimouski","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Deglaciation; Glacial period; Archipelago; Oceanography; Paleontology; Geomorphology; Glacier","score_opus":0.0460226954133222,"score_gpt":0.24325180190018617,"score_spread":0.19722910648686398,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1826023556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9748384,0.013489531,0.0000015865412,0.0095989425,0.0002713355,0.00007271147,0.000008870888,0.0000012131911,0.0017174289],"genre_scores_gemma":[0.99891984,0.00036398787,0.000079264726,0.00048768058,0.000056799832,2.945844e-7,3.75097e-7,8.566392e-7,0.00009089385],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99836844,0.00039654618,0.00025598262,0.000116586496,0.00026945324,0.0005929829],"domain_scores_gemma":[0.9969096,0.002332309,0.00015414787,0.00009471754,0.00007998614,0.00042923796],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.002380589,0.00010096167,0.00018199094,0.00008102309,0.0012511689,0.00006894507,0.00052521995,0.00006837709,0.0005850985],"category_scores_gemma":[0.0008463016,0.00004561549,0.00004302396,0.00022075606,0.0042853593,0.00018801892,0.000011768655,0.0003131393,0.0000093581675],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032795546,0.000002798005,0.9985117,0.0000029729113,0.000011496662,0.00004810297,0.0002676274,0.000026709324,0.000011751898,0.00019425683,0.00040656092,0.0004832771],"study_design_scores_gemma":[0.00007561623,0.00037499302,0.9952679,0.000040081242,0.000010746179,0.0004781341,0.00047154786,0.00009458209,0.000099017765,0.0003503092,0.002673956,0.00006309391],"about_ca_topic_score_codex":0.31972447,"about_ca_topic_score_gemma":0.99549466,"teacher_disagreement_score":0.67577016,"about_ca_system_score_codex":0.0000014220653,"about_ca_system_score_gemma":0.0023750146,"threshold_uncertainty_score":0.9984244},"labels":[],"label_agreement":null},{"id":"W1826884892","doi":"10.1139/e2012-024","title":"Albanerpetontid amphibians from the Late Cretaceous (Santonian) of Iharkút, Hungary, with remarks on regional differences in Late Cretaceous Laurasian amphibian assemblages","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Amphibian and Reptile Biology","field":"Environmental Science","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Royal Tyrrell Museum","funders":"Muséum National d'Histoire Naturelle","keywords":"Cretaceous; Paleontology; Geology; Laurasia; Salamander; Paleoecology; Gondwana; Genus; Tetrapod (structure); Mesozoic; Taphonomy; Faunal assemblage; Taxon; Ecology; Structural basin; Biology","score_opus":0.01480606532514329,"score_gpt":0.20634801825503452,"score_spread":0.19154195292989123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1826884892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9850428,0.00054539467,0.00001232502,0.00580726,0.00023304905,0.00023931147,0.000015804828,0.000006177908,0.008097859],"genre_scores_gemma":[0.99753535,0.00012888183,0.00048544444,0.00083194074,0.00009178068,0.000003392134,0.0000024100777,0.000013232716,0.0009075539],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99748796,0.0002739638,0.0005781846,0.00037788,0.00059041934,0.000691573],"domain_scores_gemma":[0.99820065,0.0003139401,0.000541653,0.00030459286,0.00004943031,0.0005897038],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00070766883,0.00027074738,0.00045242326,0.00022446425,0.00037665234,0.00015846595,0.0010954641,0.00014180987,0.0023245416],"category_scores_gemma":[0.000106228086,0.00015322624,0.00012779249,0.0005963147,0.0027729734,0.0004159755,0.000044729863,0.00040802784,0.000093990595],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024960345,0.00003304478,0.9901756,0.0000033908627,0.000032813805,0.00017459513,0.0016726746,0.0012055002,0.0025098268,0.00005176505,0.0015731476,0.0025426848],"study_design_scores_gemma":[0.00035774408,0.0007701195,0.9924299,0.00022802177,0.000017702801,0.00010923639,0.0009588351,0.0004160196,0.00041578247,0.0004568777,0.003587215,0.00025250783],"about_ca_topic_score_codex":0.027583685,"about_ca_topic_score_gemma":0.48971945,"teacher_disagreement_score":0.4621358,"about_ca_system_score_codex":0.00004081054,"about_ca_system_score_gemma":0.00049975264,"threshold_uncertainty_score":0.99994093},"labels":[],"label_agreement":null},{"id":"W1828625419","doi":"10.1139/e2012-060","title":"The Paint Pots, Kootenay National Park, Canada — a natural acid spring analogue for Mars","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Alberta Innovates - Technology Futures; Parks Canada","keywords":"Weathering; Geology; Acid mine drainage; Pyrite; Geochemistry; Spring (device); Jarosite; Sulfur; Outcrop; Goethite; Environmental chemistry; Mineralogy; Chemistry; Adsorption","score_opus":0.015998808413085548,"score_gpt":0.19912249860447773,"score_spread":0.18312369019139219,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1828625419","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9662219,0.0143058775,0.00004922679,0.0065773716,0.0019753268,0.00019877881,0.000072464194,0.0000033934218,0.010595623],"genre_scores_gemma":[0.9984953,0.000021148264,0.0009331448,0.00035376262,0.00014424452,8.603077e-7,0.0000012851362,5.194574e-7,0.000049751092],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99866,0.00006881735,0.0002772846,0.00012851319,0.00036109317,0.0005042643],"domain_scores_gemma":[0.99865466,0.00038263184,0.00018045159,0.000060172184,0.00024570877,0.0004763573],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001125944,0.00009727182,0.00012968767,0.00013706624,0.0012452016,0.00024719475,0.0005354544,0.00003825311,0.00014238247],"category_scores_gemma":[0.00035959776,0.000058706384,0.00008441863,0.00025065592,0.00054558844,0.0003868212,7.8256636e-7,0.00018306925,0.000003542804],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010052986,0.0000012820401,0.93877375,0.0000043794244,0.000043948654,0.000034594468,0.00008474817,0.00068456854,0.000028909377,0.0010517791,0.0046405126,0.054641448],"study_design_scores_gemma":[0.00009908039,0.00008545818,0.9857048,0.000013027818,0.0000045283878,0.00007704504,0.0003042101,0.0023935542,0.000029762738,0.0017027031,0.009494831,0.00009101117],"about_ca_topic_score_codex":0.7715787,"about_ca_topic_score_gemma":0.9990567,"teacher_disagreement_score":0.22747794,"about_ca_system_score_codex":0.0000054064844,"about_ca_system_score_gemma":0.0060875844,"threshold_uncertainty_score":0.999547},"labels":[],"label_agreement":null},{"id":"W1828650523","doi":"10.1139/cjes-2014-0056","title":"Enhancing bonebed mapping with GIS technology using the Danek Bonebed (Upper Cretaceous Horseshoe Canyon Formation, Edmonton, Alberta, Canada) as a case study","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Species Distribution and Climate Change","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"University of Alberta","keywords":"Canyon; Geology; Cretaceous; Horseshoe (symbol); Paleontology; Geomorphology; Computer science","score_opus":0.017714678239104956,"score_gpt":0.22317528700263106,"score_spread":0.20546060876352612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1828650523","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99378103,0.000118730386,0.00027036274,0.0021947355,0.00018623628,0.00020101795,0.0000060586385,0.000005121783,0.0032367136],"genre_scores_gemma":[0.9991208,0.0000033909205,0.0001785374,0.00049861375,0.000034219647,0.0000031815853,7.0772325e-7,0.0000069058124,0.00015365495],"study_design_codex":"observational","study_design_gemma":"qualitative","domain_scores_codex":[0.99824697,0.0000900007,0.00037132282,0.00020686799,0.00053073047,0.0005541206],"domain_scores_gemma":[0.99886876,0.00007236807,0.00032504223,0.00020005062,0.000082538296,0.0004512077],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008160613,0.00015598125,0.00020687969,0.00018663415,0.0012980062,0.00018720071,0.00043867136,0.000046539197,0.0030074732],"category_scores_gemma":[0.00022188331,0.000103432874,0.000037045327,0.00096431485,0.00064400653,0.00060369034,0.00003751098,0.00020380461,0.000015401234],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038072794,0.0001075964,0.94843984,0.000026154912,0.00011220975,0.0064871656,0.025825413,0.0052050673,0.0063711596,0.0008229781,0.00284908,0.0037152646],"study_design_scores_gemma":[0.0019272397,0.0022468437,0.15286997,0.00023722534,0.0001884081,0.06550007,0.618177,0.005783609,0.0047519715,0.00023981361,0.14680856,0.0012693006],"about_ca_topic_score_codex":0.90413374,"about_ca_topic_score_gemma":0.9995542,"teacher_disagreement_score":0.7955699,"about_ca_system_score_codex":0.0002637582,"about_ca_system_score_gemma":0.001143082,"threshold_uncertainty_score":0.9983345},"labels":[],"label_agreement":null},{"id":"W1829440091","doi":"10.1139/e10-011","title":"Great earthquakes on Canada’s west coast: a review This article is one of a series of papers published in this Special Issue on the theme<i>Lithoprobe — parameters, processes, and the evolution of a continent</i>. Geological Survey of Canada Contribution 20090196.","year":2010,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"University of Victoria","keywords":"Geology; Subduction; Seismology; Thrust fault; Slip (aerodynamics); Limiting; Continental margin; Fault (geology); Episodic tremor and slip; Tectonics","score_opus":0.02772243639399464,"score_gpt":0.2225424397122526,"score_spread":0.19482000331825797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1829440091","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.036081776,0.95514095,1.5237283e-7,0.0033004354,0.00038043302,0.00075472577,0.0010039727,0.0000011336464,0.0033364417],"genre_scores_gemma":[0.3538497,0.6455579,0.000024137027,0.0002990762,0.00011122969,0.0000029927746,0.000012975894,0.0000039216934,0.00013806355],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9965631,0.00068326335,0.0012311912,0.0002569163,0.00083840144,0.00042714152],"domain_scores_gemma":[0.995288,0.0019645332,0.0016382481,0.00023994005,0.0006547855,0.00021446311],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0042755646,0.00025972124,0.001590691,0.0001904416,0.00023836178,0.000042162505,0.00060927746,0.00011063429,0.003816432],"category_scores_gemma":[0.0052509126,0.00012901655,0.00014026513,0.0011473147,0.0017801332,0.00016109727,0.00001505117,0.00048676442,7.385019e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009379094,0.00016307666,0.58149517,0.015375955,0.0009995255,0.00013295254,0.0023605137,0.00016612129,0.0000025991721,0.002329568,0.04477609,0.35126054],"study_design_scores_gemma":[0.0010026543,0.0016028513,0.53070897,0.023194445,0.0004397076,0.00015416277,0.0007046683,0.000018135788,0.00007835439,0.00019077571,0.44144022,0.0004650336],"about_ca_topic_score_codex":0.98780835,"about_ca_topic_score_gemma":0.9998813,"teacher_disagreement_score":0.39666414,"about_ca_system_score_codex":0.000019285484,"about_ca_system_score_gemma":0.016428372,"threshold_uncertainty_score":0.9970942},"labels":[],"label_agreement":null},{"id":"W1830422697","doi":"10.1139/cjes-2014-0047","title":"Stratigraphic and chronologic analysis of the Warren Beach, northwest Ohio, USA","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Aeolian processes; Sedimentary depositional environment; Radiocarbon dating; Facies; Ground-penetrating radar; Paleontology; Geomorphology; Overwash; Thermoluminescence dating; Sedimentary rock; Marine transgression; Structural basin; Barrier island; Oceanography; Radar; Shore","score_opus":0.021528933964681068,"score_gpt":0.22517847975182972,"score_spread":0.20364954578714867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1830422697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99398196,0.0013474923,0.000007228264,0.00075924885,0.00016961347,0.000036256355,0.000017012344,9.254316e-7,0.0036802844],"genre_scores_gemma":[0.999643,0.000034565728,0.0001373613,0.00010879366,0.000023966082,7.313447e-8,0.0000026118005,4.4416353e-7,0.00004912707],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988967,0.00021445604,0.00024291273,0.00013145445,0.00019724543,0.0003172174],"domain_scores_gemma":[0.9990569,0.00025158442,0.00019097148,0.00011836089,0.00008205651,0.00030017062],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012590621,0.00007357581,0.00023409826,0.0005810826,0.00045921683,0.00004498352,0.00051729823,0.00006759591,0.0009493807],"category_scores_gemma":[0.00019410446,0.000042445306,0.00009765864,0.0012439365,0.0020849514,0.00015086254,0.0000052373293,0.00020950745,0.000005749748],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000019641707,0.0000014342231,0.9967017,0.000002659376,0.000053688003,0.0000050632107,0.000102940416,0.002234711,0.0000016645585,0.00023038923,0.000009715602,0.0006540615],"study_design_scores_gemma":[0.00006775565,0.00020952395,0.99638987,0.000008005539,0.00007785292,0.00006284403,0.00010204617,0.0021246267,0.000015153838,0.0004072367,0.0004853393,0.000049775503],"about_ca_topic_score_codex":0.01155559,"about_ca_topic_score_gemma":0.95104486,"teacher_disagreement_score":0.93948925,"about_ca_system_score_codex":1.6591883e-7,"about_ca_system_score_gemma":0.000595563,"threshold_uncertainty_score":0.9999639},"labels":[],"label_agreement":null},{"id":"W1831713658","doi":"10.1139/cjes-2015-0026","title":"Chronostratigraphy of the Hottah terrane and Great Bear magmatic zone of Wopmay Orogen, Canada, and exploration of a terrane translation model","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Government of Northwest Territories","funders":"","keywords":"Terrane; Geology; Zircon; Craton; Geochemistry; Subduction; Geochronology; Archean; Paleontology; Tectonics","score_opus":0.0464982567862914,"score_gpt":0.19570611287412987,"score_spread":0.14920785608783846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1831713658","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99671555,0.0020421792,0.00008333208,0.000699842,0.00003446224,0.000053284566,0.00003952813,4.2648725e-7,0.0003313865],"genre_scores_gemma":[0.9987559,0.000036710313,0.0011460871,0.00003719089,0.000009746404,8.3909555e-8,0.0000020559921,5.0238094e-7,0.000011779926],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99916005,0.000038709215,0.00031368056,0.00008325345,0.0002743154,0.00012999962],"domain_scores_gemma":[0.99927515,0.000040517458,0.00021744153,0.000056328285,0.00011364565,0.0002969365],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034270805,0.00006445534,0.00020574522,0.0001141204,0.00006659499,0.0000145222675,0.00012868475,0.000027922444,0.00011839723],"category_scores_gemma":[0.00005017188,0.00003728103,0.000046591023,0.00035626415,0.0005717952,0.00023515508,0.0000022531206,0.00005948185,1.0509717e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015384207,0.0000044589783,0.98186135,0.00003381347,0.000020173458,0.0000032273042,0.00072872656,0.0123924455,0.00071164203,0.000017210235,0.000015865924,0.0041956976],"study_design_scores_gemma":[0.0003103442,0.00044644086,0.955573,0.00009081799,0.00007630254,0.000046328154,0.00076572405,0.035645314,0.0034897493,0.0034262072,0.00003901729,0.00009070445],"about_ca_topic_score_codex":0.4242363,"about_ca_topic_score_gemma":0.97149163,"teacher_disagreement_score":0.54725534,"about_ca_system_score_codex":9.2875445e-7,"about_ca_system_score_gemma":0.00096423697,"threshold_uncertainty_score":0.5795978},"labels":[],"label_agreement":null},{"id":"W1831870448","doi":"10.1139/cjes-2015-0004","title":"Vesicle distribution in basalt lava flow units in the Mesozoic rift basins of northeast China and its application in gas reservoir prediction","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Basalt; Lava; Geology; Rift; Outcrop; Petrology; Rift zone; Lava field; Geochemistry; Volcano; Geomorphology; Structural basin","score_opus":0.022317512530792158,"score_gpt":0.2203183957188971,"score_spread":0.19800088318810494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1831870448","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979122,0.0005008548,0.00027136842,0.00088195025,0.000055822376,0.000076154414,0.00002405791,0.0000023559962,0.00027518003],"genre_scores_gemma":[0.9998574,0.00006585912,0.000024053888,0.000011427175,0.000026752985,0.000002172603,0.0000068123945,0.0000024472342,0.0000030545498],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99921286,0.00008844944,0.0002783463,0.00006925833,0.00020220711,0.0001488573],"domain_scores_gemma":[0.99962723,0.000021047621,0.00005794801,0.00006284744,0.000072289964,0.0001586119],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012584075,0.00005354162,0.00010934634,0.0003786608,0.00004373624,0.000031617634,0.00016517844,0.000034110355,0.0000034203272],"category_scores_gemma":[0.00015109866,0.00004016697,0.000014613597,0.0015938273,0.000069722926,0.0003418793,0.0000038079447,0.00014459621,8.519151e-7],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000060196344,0.000011694556,0.32900012,0.00001255029,0.0000041009366,0.000012101902,0.0036210245,0.66620743,0.00016770382,0.00016006833,0.00006347139,0.00073369907],"study_design_scores_gemma":[0.0002538201,0.000058031168,0.38821554,0.00005143912,0.0000036565702,0.000010065186,0.0012692127,0.60916406,0.00016430287,0.00018432812,0.00058086135,0.000044694058],"about_ca_topic_score_codex":0.0030215315,"about_ca_topic_score_gemma":0.4685488,"teacher_disagreement_score":0.46552727,"about_ca_system_score_codex":0.000022861532,"about_ca_system_score_gemma":0.0003567586,"threshold_uncertainty_score":0.5411488},"labels":[],"label_agreement":null},{"id":"W1833722030","doi":"10.1139/e2012-027","title":"Southampton, Canada’s third pallasite","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University; Lakehead University","funders":"Monash University; Lakehead University","keywords":"Troilite; Kamacite; Geology; Iron meteorite; Mineralogy; Olivine; Meteorite; Neutron activation analysis; Metal; Analytical Chemistry (journal); Geochemistry; Chemistry; Materials science; Chondrite; Radiochemistry; Metallurgy; Environmental chemistry; Physics","score_opus":0.009143366480062051,"score_gpt":0.18042740089387765,"score_spread":0.1712840344138156,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1833722030","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96610045,0.00010484422,0.00022377438,0.001031186,0.00053873006,0.0000464351,0.000024897261,0.0000012126343,0.031928446],"genre_scores_gemma":[0.9982058,3.5241834e-7,0.00056608114,0.00022982711,0.00018871353,2.6562077e-7,0.0000013172739,0.0000016017516,0.0008060734],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991072,0.000020986525,0.00018637953,0.00009584272,0.00023385922,0.00035576453],"domain_scores_gemma":[0.99899596,0.000035823152,0.00013226543,0.00006898628,0.0001008252,0.00066613546],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023905872,0.00007442577,0.00010710991,0.000094514995,0.00030686278,0.00015656314,0.0004038428,0.00001119458,0.0035522021],"category_scores_gemma":[0.000010387603,0.00005567342,0.000037546724,0.0002000576,0.00020011245,0.0003577416,0.0000054420275,0.00011945528,0.00005909376],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[2.5645718e-7,0.0000011573742,0.98945093,4.7871254e-7,0.000005787039,0.000007626644,0.00015428047,0.00054681645,0.000049136874,0.00043730406,0.0072964914,0.0020497185],"study_design_scores_gemma":[0.00009903347,0.00008109824,0.952176,0.0000207703,0.000005298551,0.00002141445,0.0014740168,0.0004985332,0.00012786529,0.0006282934,0.04472473,0.00014298694],"about_ca_topic_score_codex":0.95186096,"about_ca_topic_score_gemma":0.9759652,"teacher_disagreement_score":0.037428237,"about_ca_system_score_codex":0.000003651599,"about_ca_system_score_gemma":0.0061692614,"threshold_uncertainty_score":0.9994648},"labels":[],"label_agreement":null},{"id":"W1839737813","doi":"10.1139/cjes-2014-0087","title":"A new chernetid pseudoscorpion from the Miocene Chiapas – Amber Lagerstätte, Mexico","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Subterranean biodiversity and taxonomy","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Lagerstätte; Neogene; Paleontology; Genus; Taxon; Geology; Zoology; Biology; Structural basin","score_opus":0.03536792923571092,"score_gpt":0.1807474589003292,"score_spread":0.14537952966461828,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1839737813","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97469854,0.0009977113,0.00040415867,0.0039627803,0.0012912845,0.000067162764,0.000046038258,0.00000582606,0.01852652],"genre_scores_gemma":[0.9943522,0.000018854536,0.0029496737,0.0019126493,0.0005122578,3.2210245e-8,0.000004980736,0.0000013207176,0.00024803574],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886,0.000110953304,0.00020248297,0.0001661236,0.0003038252,0.00035661113],"domain_scores_gemma":[0.9986973,0.0002462954,0.00018271926,0.00012740241,0.0000442551,0.0007020496],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00071764644,0.000111071575,0.00015388064,0.00011991253,0.00056369667,0.00026736048,0.0007059919,0.00005176056,0.008795128],"category_scores_gemma":[0.00013021017,0.00007058288,0.000092454015,0.00033708086,0.00039340145,0.00041587997,0.000005890011,0.0001868604,0.00027668063],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000812165,0.0000012969143,0.98265773,6.6946194e-7,0.0000117283125,0.000016473088,0.00032028297,0.00048014201,0.000005441011,0.000048875172,0.005897598,0.010551634],"study_design_scores_gemma":[0.00023684584,0.00017512271,0.8763247,0.000027829832,0.00001748728,0.00005016852,0.00030039408,0.00052885886,0.000093687304,0.0008581377,0.1212711,0.00011566849],"about_ca_topic_score_codex":0.13649824,"about_ca_topic_score_gemma":0.54940206,"teacher_disagreement_score":0.41290385,"about_ca_system_score_codex":0.0000018443105,"about_ca_system_score_gemma":0.00086626626,"threshold_uncertainty_score":0.99211097},"labels":[],"label_agreement":null},{"id":"W1843710198","doi":"10.1139/cjes-2013-0057","title":"Early Devonian graptolites and graptolite biostratigraphy, Arctic Islands, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Biozone; Devonian; Geology; Paleontology; Biostratigraphy; Fauna; Arctic; Ecology; Oceanography; Biology","score_opus":0.010868442431176135,"score_gpt":0.18605538957194107,"score_spread":0.17518694714076494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1843710198","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97349375,0.010500513,0.000004719802,0.0013690123,0.0004392484,0.00008896989,0.00004205927,0.0000035824085,0.014058153],"genre_scores_gemma":[0.9989456,0.000055427674,0.00068327645,0.00022898043,0.00006226032,3.2083716e-7,9.902991e-7,7.441002e-7,0.000022410637],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985071,0.00007905042,0.00034481715,0.00019369106,0.00028959112,0.0005857725],"domain_scores_gemma":[0.9983481,0.00015053088,0.00018657705,0.000094162875,0.00014096132,0.0010796618],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037779,0.00015644557,0.0002291258,0.00042278506,0.0006801629,0.0003123696,0.00038655667,0.00006601213,0.00067029404],"category_scores_gemma":[0.00007641486,0.000116775474,0.00007108813,0.000531536,0.0009966686,0.0007048095,7.7027613e-7,0.00022153025,0.0000043990294],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021698033,0.0000012186205,0.99022,0.0000054776265,0.000018501669,0.000055320575,0.00018671245,0.00000605657,0.000008640306,0.00035253994,0.00018498753,0.008958338],"study_design_scores_gemma":[0.00013520522,0.00026321964,0.9944277,0.000031391904,0.000009886984,0.0002955111,0.0003575762,0.000077595156,0.000023897313,0.0033585376,0.00086673524,0.0001527408],"about_ca_topic_score_codex":0.928936,"about_ca_topic_score_gemma":0.99777967,"teacher_disagreement_score":0.06884367,"about_ca_system_score_codex":0.0000010796516,"about_ca_system_score_gemma":0.0024389012,"threshold_uncertainty_score":0.733925},"labels":[],"label_agreement":null},{"id":"W1845430774","doi":"10.1139/cjes-2014-0054","title":"New geoscientific constraints on the hydrocarbon potential of the Nechako–Chilcotin plateau of central British Columbia","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geoscience BC","funders":"","keywords":"Geology; Plateau (mathematics); Earth science; Tectonics; Prospectivity mapping; Volcano; Hydrocarbon exploration; Geological survey; Paleontology; Geomorphology","score_opus":0.01000915916002755,"score_gpt":0.1661312688279091,"score_spread":0.15612210966788154,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1845430774","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912993,0.00016444227,0.00008160977,0.0007992467,0.00083067146,0.000072031005,0.00006232534,0.0000014809104,0.006688904],"genre_scores_gemma":[0.9992994,0.000009398275,0.00023445362,0.00017709866,0.00006044337,4.2417536e-8,0.0000014115296,7.762195e-7,0.0002169899],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988007,0.000095184136,0.00032986657,0.000101666694,0.00036644287,0.0003061159],"domain_scores_gemma":[0.9990718,0.00012859196,0.0003181178,0.00009830874,0.000088482484,0.0002947464],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00093323033,0.000057399007,0.0001415927,0.000065227134,0.00050747953,0.0002684357,0.0006655545,0.000039077808,0.0047071073],"category_scores_gemma":[0.00030993007,0.00003863004,0.00008905128,0.00046710126,0.0011741576,0.00016512527,0.0000059991016,0.00015004317,0.0000065612926],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000075209673,0.000009960317,0.90694726,0.000017165195,0.000017358792,0.000009372001,0.00038170704,0.017221445,0.000071324124,0.0007427575,0.0032420298,0.0713321],"study_design_scores_gemma":[0.000115147704,0.00026360934,0.9908886,0.00008934586,0.000009648018,0.000112731424,0.0002630829,0.0017391229,0.00015904714,0.0040006195,0.0022962475,0.000062825806],"about_ca_topic_score_codex":0.14801122,"about_ca_topic_score_gemma":0.7560045,"teacher_disagreement_score":0.6079933,"about_ca_system_score_codex":8.707392e-7,"about_ca_system_score_gemma":0.0009794041,"threshold_uncertainty_score":0.9962027},"labels":[],"label_agreement":null},{"id":"W1850729550","doi":"10.1139/e11-010","title":"Cambrian acritarchs from the Bourinot belt, Cape Breton Island, Nova Scotia: age and stratigraphic implications<sup>1</sup>This article is one of a series of papers published in<i>CJES Special Issue: In honour of Ward Neale</i>on the theme of Appalachian and Grenvillian geology.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University; Mount Saint Vincent University","funders":"Natural Sciences and Engineering Research Council of Canada; Ministerio de Ciencia e Innovación; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Acritarch; Geology; Paleontology; Unconformity; Nova scotia; Biostratigraphy; Oceanography; Sedimentary rock","score_opus":0.016665883551963957,"score_gpt":0.19278360067454148,"score_spread":0.1761177171225775,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1850729550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9890412,0.0013340933,3.868446e-7,0.007887265,0.000043352324,0.00009543133,0.00013775412,6.26794e-7,0.001459892],"genre_scores_gemma":[0.9993555,0.00014894722,0.00014890522,0.00021290737,0.00011537044,2.551011e-7,0.0000046603036,0.0000010985605,0.000012353685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985956,0.0001559437,0.00051458896,0.00015641363,0.0002441747,0.0003333028],"domain_scores_gemma":[0.9989303,0.00030971481,0.00029900597,0.00014229598,0.00007568298,0.0002430466],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010285965,0.00011122412,0.00035345613,0.00020017898,0.000121639176,0.000037339116,0.00038931676,0.00006359631,0.0045806384],"category_scores_gemma":[0.00023090577,0.000061438404,0.0000730375,0.0007242925,0.0018968104,0.00029652735,0.000015320751,0.00023153659,0.0000012334544],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028088967,0.000020324704,0.99466467,0.000010035044,0.000021610073,0.0000031107375,0.0028426023,0.00014630552,0.0003786969,0.00025096463,0.00005447311,0.0015791001],"study_design_scores_gemma":[0.00018541409,0.0002502352,0.99316216,0.0000513359,0.00002260688,0.000013316329,0.002713232,0.00014242457,0.0005506109,0.0026528668,0.00018769696,0.00006809835],"about_ca_topic_score_codex":0.15991104,"about_ca_topic_score_gemma":0.8322686,"teacher_disagreement_score":0.67235756,"about_ca_system_score_codex":0.0000013018688,"about_ca_system_score_gemma":0.00018095635,"threshold_uncertainty_score":0.9963293},"labels":[],"label_agreement":null},{"id":"W1852399985","doi":"10.1139/cjes-2013-0078","title":"Late Wisconsinan helmeted muskoxen (<i>Bootherium bombifrons</i>) from southwestern Alberta, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Calgary Laboratory Services; University of Calgary","funders":"Hope Funds for Cancer Research","keywords":"Radiocarbon dating; Fauna; Geology; Aeolian processes; Grassland; Antler; Archaeology; Steppe; Paleontology; Physical geography; Ecology; Geography; Biology","score_opus":0.015320509289193585,"score_gpt":0.196790695885306,"score_spread":0.18147018659611241,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1852399985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98587,0.0009337095,0.000005099646,0.0035572706,0.000937582,0.00010038933,0.000051464252,0.000002996862,0.008541463],"genre_scores_gemma":[0.9972862,0.0000117017125,0.00041775117,0.0010949923,0.0001026897,3.913671e-7,0.000009892401,0.0000027499884,0.0010736382],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99814194,0.00020550117,0.00035476233,0.0002260877,0.00031476727,0.00075695966],"domain_scores_gemma":[0.9980331,0.00047074983,0.00019171945,0.0001553079,0.00014743197,0.001001699],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004844115,0.00015088372,0.00027769685,0.0002418142,0.00052148337,0.0001779336,0.0006844607,0.00010666581,0.012841076],"category_scores_gemma":[0.00018766966,0.000114519666,0.00006165338,0.000344694,0.00089963793,0.00045344082,0.00000711805,0.00034977595,0.00044404558],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004084869,0.0000016113852,0.9981807,0.0000018563891,0.000021300422,0.00013638232,0.00023707864,0.00034400067,0.000009340637,0.000008879055,0.00063470803,0.0004200663],"study_design_scores_gemma":[0.0001941061,0.00014007167,0.99228156,0.00002378401,0.000010597482,0.00017291709,0.0004983683,0.0006747109,0.000054346965,0.0007654588,0.0050355704,0.00014852383],"about_ca_topic_score_codex":0.99020565,"about_ca_topic_score_gemma":0.99991167,"teacher_disagreement_score":0.012397029,"about_ca_system_score_codex":0.0000012101174,"about_ca_system_score_gemma":0.0053387955,"threshold_uncertainty_score":0.9880613},"labels":[],"label_agreement":null},{"id":"W1853999391","doi":"10.1139/cjes-2014-0035","title":"Fault reconstructions using aeromagnetic data in the Great Bear magmatic zone, Northwest Territories, Canada","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Terrane; Orogeny; Seismology; Fault (geology); Tectonics; Fold (higher-order function); Echelon formation; Geochemistry","score_opus":0.024931791408227395,"score_gpt":0.1993974689366548,"score_spread":0.1744656775284274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1853999391","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963271,0.0004873326,0.000015226153,0.0014726621,0.00032733634,0.000039052917,0.00010436851,0.0000011317413,0.0012257764],"genre_scores_gemma":[0.99755114,0.000009697475,0.0018221359,0.00042012622,0.00014876461,6.63299e-8,0.000025969448,6.66203e-7,0.000021412265],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99877274,0.000104166254,0.000298504,0.00016424025,0.00032022543,0.00034012372],"domain_scores_gemma":[0.9990746,0.00016789306,0.00011813035,0.00020052196,0.000059352755,0.0003795326],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000716533,0.00008697596,0.0001754445,0.00013909627,0.000361892,0.00014556103,0.0008147828,0.00002954025,0.0015938332],"category_scores_gemma":[0.00027033407,0.00005045776,0.000036849637,0.0007079985,0.00044011365,0.00025910873,0.000007961936,0.00018255819,0.0000051990673],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000010054333,0.0000016286536,0.9943963,0.0000031185348,0.0000045323527,0.00005171031,0.000026594791,0.0022855492,0.0000022354748,0.000013936417,0.000041352618,0.0031720258],"study_design_scores_gemma":[0.00007689099,0.00010518515,0.97512555,0.00002666639,0.00002848622,0.00056606357,0.0004187815,0.015469495,0.0000039586394,0.00067344063,0.0074174805,0.00008799392],"about_ca_topic_score_codex":0.9819515,"about_ca_topic_score_gemma":0.99986345,"teacher_disagreement_score":0.019270753,"about_ca_system_score_codex":0.0000032146565,"about_ca_system_score_gemma":0.0017074037,"threshold_uncertainty_score":0.99931884},"labels":[],"label_agreement":null},{"id":"W1854794405","doi":"10.1139/cjes-2014-0071","title":"The first appearance of <i>Troodon</i> in the Upper Cretaceous site of Danek Bonebed, and a reevaluation of troodontid quantitative tooth morphotypes","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia; University of Alberta","funders":"Ministerio de Economía y Competitividad","keywords":"Canyon; Geology; Paleontology; Horseshoe (symbol); Cretaceous; Taxon; Geomorphology","score_opus":0.018712983550221194,"score_gpt":0.22446865429265536,"score_spread":0.20575567074243417,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1854794405","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98547995,0.010773175,0.000038520207,0.0016096457,0.00014122669,0.000070731934,0.000022190285,4.6885086e-7,0.0018640921],"genre_scores_gemma":[0.99918574,0.00019145249,0.0004939487,0.00009737784,0.000018105537,1.8114959e-7,0.000001036274,5.652594e-7,0.000011573481],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989136,0.00026727834,0.0003429511,0.00009307028,0.00019067463,0.00019246656],"domain_scores_gemma":[0.99882364,0.0005648,0.00035346724,0.00008483504,0.00010282924,0.0000704041],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002553042,0.00006225361,0.00019247123,0.00014190648,0.00022386582,0.000013380701,0.00029187617,0.00004079888,0.000032880725],"category_scores_gemma":[0.000396261,0.00003389929,0.000042372147,0.0002965754,0.0015875244,0.00019266424,0.0000026974494,0.0001048177,0.0000016684501],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005741129,0.000003464352,0.99514925,0.000009171611,0.000008138695,0.0000027540668,0.0011924385,0.001345284,0.000081459424,0.0010733018,0.000035910893,0.0010414083],"study_design_scores_gemma":[0.00018099388,0.0007344633,0.9911586,0.00005161607,0.00001076975,0.000069995396,0.0008354782,0.0035715047,0.0000419719,0.0011088102,0.002195937,0.000039882787],"about_ca_topic_score_codex":0.008735369,"about_ca_topic_score_gemma":0.6510103,"teacher_disagreement_score":0.6422749,"about_ca_system_score_codex":7.6310175e-7,"about_ca_system_score_gemma":0.00032676896,"threshold_uncertainty_score":0.99786556},"labels":[],"label_agreement":null},{"id":"W1855646878","doi":"10.1139/e2012-030","title":"Non-trionychid turtles from the Paleocene of Alberta, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"H2020 European Research Council; University of Alberta; University of Calgary","keywords":"Geology; Turtle (robot); Cretaceous; Paleontology; Carapace; Taxon; Juvenile; Ecology; Biology; Crustacean","score_opus":0.01001463151652406,"score_gpt":0.17545433099275412,"score_spread":0.16543969947623005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1855646878","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9848359,0.0027895053,0.000005256761,0.004061655,0.00092493824,0.00005247867,0.00005021168,6.021411e-7,0.007279432],"genre_scores_gemma":[0.9988018,0.000034456585,0.00023661084,0.000662512,0.00014367167,1.3981335e-7,0.000005846898,6.0339664e-7,0.000114321694],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99908465,0.000069679125,0.00026769235,0.00010470746,0.000168034,0.00030526464],"domain_scores_gemma":[0.99881065,0.00047758495,0.00019611111,0.000090561065,0.000098198645,0.00032692117],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00030395013,0.00007716206,0.0001611784,0.000072027964,0.00034080783,0.000027565886,0.0005567568,0.000049197064,0.0049305335],"category_scores_gemma":[0.00014861154,0.000043966247,0.00004592039,0.00022110176,0.00077482715,0.0002172071,0.00000275324,0.00013699097,0.000041215873],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026620376,9.615109e-7,0.9943001,7.1671934e-7,0.000012218682,0.000008941363,0.00011953165,0.0005209129,0.000008163466,0.000024743893,0.0033285683,0.0016724311],"study_design_scores_gemma":[0.00007665873,0.00009328534,0.9890604,0.000014032062,0.0000069724515,0.000057846224,0.00036843368,0.0005350043,0.000030980806,0.0006792791,0.009018457,0.00005866775],"about_ca_topic_score_codex":0.9937846,"about_ca_topic_score_gemma":0.9998949,"teacher_disagreement_score":0.013965917,"about_ca_system_score_codex":0.0000014923644,"about_ca_system_score_gemma":0.0035735092,"threshold_uncertainty_score":0.9959791},"labels":[],"label_agreement":null},{"id":"W1857582244","doi":"10.1139/e10-094","title":"Nearshore articulate crinoid from the Albian of Alberta, Canada (Early Cretaceous, Echinodermata)","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Crinoid; Cretaceous; Paleontology; Marine transgression; Facies; Mesozoic; Shore; Oceanography; Structural basin","score_opus":0.023603884858878137,"score_gpt":0.1889480867662384,"score_spread":0.16534420190736027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1857582244","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96245897,0.0046366137,0.000006929693,0.0006020899,0.0005585621,0.000053830725,0.00007114572,0.000001497838,0.031610344],"genre_scores_gemma":[0.9991471,0.00001710728,0.00050958927,0.00023581179,0.00006156599,7.677655e-8,0.000001076747,7.4364857e-7,0.000026919928],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861896,0.000119164644,0.0003749128,0.00014676053,0.00031452096,0.00042565272],"domain_scores_gemma":[0.9987023,0.00023467258,0.00027362947,0.00016064494,0.00008513525,0.0005436391],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042197292,0.00011997289,0.00022200038,0.00010158114,0.00046673257,0.0000684105,0.00076808396,0.000054477827,0.0011087703],"category_scores_gemma":[0.00010530648,0.00007557513,0.00009191705,0.00029030163,0.00089655444,0.0003572219,0.0000013773606,0.00022196106,0.000006040157],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008961824,0.0000018947638,0.99422044,0.0000015750992,0.000027563476,0.00009845396,0.0016116874,0.00006788773,0.0000068649147,0.00010664294,0.00028289945,0.0035651077],"study_design_scores_gemma":[0.00008796431,0.00014203212,0.99674594,0.000029037588,0.000022877735,0.00009305715,0.0005307046,0.00018599605,0.00028720155,0.00088802556,0.0008884163,0.000098714336],"about_ca_topic_score_codex":0.9874284,"about_ca_topic_score_gemma":0.9998102,"teacher_disagreement_score":0.036688123,"about_ca_system_score_codex":0.0000011915891,"about_ca_system_score_gemma":0.0031030006,"threshold_uncertainty_score":0.9998044},"labels":[],"label_agreement":null},{"id":"W1861593326","doi":"10.1139/e10-041","title":"A new articulated freshwater fish (Clupeomorpha, Ellimmichthyiformes) from the Horseshoe Canyon Formation, Maastrichtian, of Alberta, CanadaThis article is one of a series of papers published in this Special Issue on the theme<i>Albertosaurus</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; University of Alberta","funders":"","keywords":"Geology; Canyon; Horseshoe (symbol); Paleontology; Cretaceous; Genus; Anatomy; Archaeology; Geography; Geomorphology; Medicine; Biology; Zoology","score_opus":0.010665499318353677,"score_gpt":0.18084087511505792,"score_spread":0.17017537579670425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1861593326","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9720043,0.00017483387,0.000001513938,0.018387038,0.000673009,0.00012267471,0.00028006104,9.732765e-7,0.008355613],"genre_scores_gemma":[0.99822074,0.00002696481,0.00023055931,0.00091979234,0.00031053615,3.3808755e-7,0.00001422993,0.0000016513919,0.0002751768],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99840903,0.0001383444,0.0006187733,0.00014384073,0.00031957406,0.00037046152],"domain_scores_gemma":[0.9984991,0.00044934388,0.00045538662,0.00019562716,0.00014829877,0.00025226586],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000817112,0.000121394725,0.0002840993,0.00019540921,0.00022546225,0.00003839483,0.00065528817,0.00010871901,0.053000778],"category_scores_gemma":[0.000476711,0.000067842935,0.00007936642,0.0006252188,0.0009868732,0.0005498536,0.000007541437,0.00031062242,0.000014862523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013415873,0.000017447246,0.9621886,0.000005793496,0.000056836547,0.000012482185,0.005324105,0.0004113904,0.0017080222,0.00033168672,0.02826223,0.0015472467],"study_design_scores_gemma":[0.00038105316,0.0004533319,0.9179475,0.000064121785,0.000035972484,0.00007050013,0.0014740297,0.0006056888,0.0115582105,0.0011452987,0.06613398,0.0001303239],"about_ca_topic_score_codex":0.5487736,"about_ca_topic_score_gemma":0.99703765,"teacher_disagreement_score":0.4482641,"about_ca_system_score_codex":0.0000036535139,"about_ca_system_score_gemma":0.0014992256,"threshold_uncertainty_score":0.9478649},"labels":[],"label_agreement":null},{"id":"W1864817717","doi":"10.1139/cjes-2015-0046","title":"The tectonic significance of the Early Cretaceous forearc-metamorphic assemblage in south-central Alaska based on detrital zircon U–Pb dating of sedimentary protoliths","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"University of Texas at El Paso; University of Arizona; National Science Foundation","keywords":"Geology; Terrane; Forearc; Zircon; Metamorphic rock; Protolith; Cretaceous; Geochemistry; Accretionary wedge; Basement; Metamorphic facies; Detritus; Paleontology; Plutonism; Pluton; Subduction; Tectonics; Facies; Structural basin; Archaeology","score_opus":0.023452688088694006,"score_gpt":0.20429735323729345,"score_spread":0.18084466514859945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1864817717","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969429,0.0007878311,0.00002147328,0.0007336374,0.00015286326,0.00020415081,0.000033604734,0.0000014584041,0.0011221259],"genre_scores_gemma":[0.999369,0.0000032336784,0.00044261047,0.00012047588,0.00004039417,8.070053e-7,0.0000013985058,0.0000012553119,0.000020824438],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981083,0.00019457849,0.0004674343,0.00016378805,0.00059652625,0.00046931987],"domain_scores_gemma":[0.9985597,0.00034618576,0.00039555164,0.00014897005,0.0001305407,0.00041903017],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001558399,0.000110790985,0.00024126735,0.00017289515,0.00021336898,0.000068258276,0.0007573401,0.00004373817,0.00034001705],"category_scores_gemma":[0.00064071757,0.00005450616,0.0001425812,0.00096703804,0.00087391865,0.00019182013,0.0000101321475,0.0002642025,0.0000041208555],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026690308,0.000008871833,0.9823186,0.000005431288,0.000010044684,0.00001745198,0.00020996481,0.015889531,0.00036329665,0.000011752442,0.000012956542,0.0011254232],"study_design_scores_gemma":[0.0003914945,0.0009045974,0.97700566,0.00009933917,0.000026213067,0.000015172129,0.001006148,0.009273334,0.009454952,0.0014701256,0.00022967494,0.00012329765],"about_ca_topic_score_codex":0.016784908,"about_ca_topic_score_gemma":0.14177527,"teacher_disagreement_score":0.12499036,"about_ca_system_score_codex":0.0000048996176,"about_ca_system_score_gemma":0.0012331671,"threshold_uncertainty_score":0.9897624},"labels":[],"label_agreement":null},{"id":"W1865572750","doi":"10.1139/cjes-2012-0119","title":"An unusual mid-Cambrian faunule from St. John's Island, Fortune Bay, Newfoundland","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"St. John’s Health Sciences Centre","funders":"","keywords":"Cove; Geology; Laurentia; Bay; Paleontology; Sequence (biology); Ordovician; Oceanography; Geomorphology","score_opus":0.019123056377128397,"score_gpt":0.2219249543489269,"score_spread":0.20280189797179848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1865572750","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9610223,0.0032986058,0.000077049786,0.0006372697,0.0010174257,0.00009363035,0.00018005937,0.00000659544,0.033667058],"genre_scores_gemma":[0.9980521,0.000029055416,0.0012435905,0.00023663079,0.00034114876,3.0266858e-7,0.000010942684,0.0000011426237,0.00008508922],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99829334,0.00012908739,0.00038009713,0.00025126315,0.00033054527,0.00061564514],"domain_scores_gemma":[0.9979849,0.00014095944,0.00023006716,0.00015589462,0.000113703114,0.0013744936],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005823724,0.00016551603,0.00027152893,0.00039056133,0.0007007557,0.000489805,0.00072427443,0.000111921814,0.004788517],"category_scores_gemma":[0.000064913926,0.00012380925,0.00010622391,0.00038920974,0.00082676765,0.0015464034,9.079606e-7,0.0002505139,0.00007222824],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000068294617,0.0000046605956,0.9729098,0.0000013400153,0.000019314468,0.000083972656,0.00023822855,0.00009337691,0.000038093734,0.00005920858,0.00039334482,0.026151842],"study_design_scores_gemma":[0.0002737777,0.00057127763,0.99190533,0.000021992275,0.00001475889,0.000116975854,0.00047653166,0.0010724493,0.000029300905,0.0024432854,0.0028976267,0.00017669701],"about_ca_topic_score_codex":0.27110508,"about_ca_topic_score_gemma":0.9823556,"teacher_disagreement_score":0.7112505,"about_ca_system_score_codex":0.0000017000943,"about_ca_system_score_gemma":0.0013056392,"threshold_uncertainty_score":0.9961212},"labels":[],"label_agreement":null},{"id":"W1870959666","doi":"10.1139/cjes-2012-0085","title":"Ceratopsia increase: history and trends","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"University of Alberta","keywords":"China; Geography; Archaeology; Physical geography; Paleontology; Geology","score_opus":0.023740706073596612,"score_gpt":0.20045969737254082,"score_spread":0.17671899129894422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1870959666","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8621065,0.02053038,0.0000032996593,0.0017901107,0.00064938253,0.000023674947,0.0000060555712,0.0000035147125,0.11488705],"genre_scores_gemma":[0.99729115,0.000075211006,0.00053005293,0.0005805161,0.00008089561,1.0482007e-7,6.114373e-7,5.911107e-7,0.0014408818],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99932337,0.00005298527,0.00016204487,0.00009285435,0.0001241704,0.00024459235],"domain_scores_gemma":[0.99920326,0.0000654762,0.00009436961,0.000042260788,0.000072433984,0.00052220805],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034190348,0.000065624365,0.000121193036,0.00032095175,0.00028113622,0.000055587676,0.00016019926,0.00003184041,0.008769948],"category_scores_gemma":[0.000069653666,0.00004755252,0.000029993435,0.00017965926,0.0008284449,0.00038700766,0.0000018033822,0.00009826284,0.000065046435],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.0173125e-7,7.0121945e-7,0.9781596,0.0000012556302,0.000005890926,0.000016322927,0.00022920557,0.0000164037,0.0000024505923,0.00015807302,0.008789679,0.0126194935],"study_design_scores_gemma":[0.000073762465,0.00011038755,0.9191662,0.0000072265548,0.0000047801764,0.00016585099,0.00025888474,0.00022778907,0.0000012029956,0.00020320964,0.07972179,0.000058907066],"about_ca_topic_score_codex":0.059100356,"about_ca_topic_score_gemma":0.8290216,"teacher_disagreement_score":0.7699212,"about_ca_system_score_codex":0.000002005236,"about_ca_system_score_gemma":0.00048511045,"threshold_uncertainty_score":0.9921362},"labels":[],"label_agreement":null},{"id":"W1871400194","doi":"10.1139/e11-062","title":"<i>Huehuecanauhtlus tiquichensis</i>, a new hadrosauroid dinosaur (Ornithischia: Ornithopoda) from the Santonian (Late Cretaceous) of Michoacán, Mexico","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology; Gondwana; Cretaceous; Cladistics; Theropoda; Tectonics; Phylogenetic tree; Biology","score_opus":0.021388123602697286,"score_gpt":0.21550028628854484,"score_spread":0.19411216268584755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1871400194","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96263736,0.025477307,0.00007194116,0.0042867805,0.0017203161,0.00008755888,0.000180284,0.0000058141986,0.005532608],"genre_scores_gemma":[0.9963819,0.00015969544,0.0014274975,0.0013079022,0.0005220058,1.4619941e-7,0.00001226228,0.0000027933847,0.00018581508],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99790984,0.0002884697,0.0005015135,0.00019626427,0.00031880577,0.00078512804],"domain_scores_gemma":[0.99773043,0.0004910304,0.00043617867,0.0001957639,0.00011076552,0.0010358026],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013303307,0.00018496143,0.0003461632,0.00021209038,0.00064758345,0.000053833548,0.0008474269,0.00015311872,0.002632801],"category_scores_gemma":[0.00033052833,0.00011679112,0.00014189609,0.0004758211,0.0014700433,0.00058692595,0.000010228435,0.00040959206,0.00012755067],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002387915,0.0000050510303,0.99390024,0.0000016830744,0.000042014242,0.000025070209,0.00071667385,0.00038385764,0.000113656984,0.00006503749,0.002505307,0.0022175082],"study_design_scores_gemma":[0.00020261917,0.00021479778,0.9534588,0.000032191136,0.00004661979,0.00036171454,0.0004245059,0.00019501078,0.0001573642,0.0007663179,0.043991596,0.00014849522],"about_ca_topic_score_codex":0.04454106,"about_ca_topic_score_gemma":0.6818474,"teacher_disagreement_score":0.63730633,"about_ca_system_score_codex":0.000003324952,"about_ca_system_score_gemma":0.0023043538,"threshold_uncertainty_score":0.9982789},"labels":[],"label_agreement":null},{"id":"W1872930339","doi":"10.1139/cjes-2013-0101","title":"Grenvillia and Laurentia — a Precambrian Wilson cycle?","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Geochronology; Terrane; Laurentia; Craton; Paleomagnetism; Hornblende; Radiometric dating; Proterozoic; Metamorphism; Precambrian; Plate tectonics; Orogeny; Accretion (finance); Isochron dating; Paleontology; Geochemistry; Continental crust; Subduction; Zircon; Tectonics; Biotite; Isochron","score_opus":0.010048911060853349,"score_gpt":0.17248058816859704,"score_spread":0.1624316771077437,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1872930339","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887707,0.0017541269,0.0000083207215,0.0020399168,0.00015338446,0.000039757328,0.000007711812,0.0000028116187,0.0072232177],"genre_scores_gemma":[0.99850565,0.000036911933,0.0009017818,0.00032080663,0.000081864,1.2279496e-7,0.0000017966138,6.2828394e-7,0.0001504557],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990804,0.00003896247,0.000210706,0.00014090551,0.00019012888,0.00033886245],"domain_scores_gemma":[0.9988884,0.0000612388,0.000108095635,0.00005416057,0.00007696276,0.0008111733],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031067102,0.00008385849,0.0001560325,0.00016182456,0.00025494347,0.00021675714,0.00026482323,0.000038547078,0.018109072],"category_scores_gemma":[0.00011080335,0.00005211651,0.000062354775,0.00035169694,0.00051375304,0.00039637653,0.0000044594804,0.00012001326,0.00015699734],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000010108433,0.0000016869358,0.9847979,0.0000020724485,0.000008719466,0.000012851802,0.000050162682,0.0002606831,0.000037609883,0.00006267443,0.00024303324,0.014521627],"study_design_scores_gemma":[0.00006925834,0.00015621135,0.98436725,0.000014120931,0.0000127484445,0.00007228349,0.0001200306,0.002027996,0.00005393858,0.009974786,0.003044003,0.00008735575],"about_ca_topic_score_codex":0.07530778,"about_ca_topic_score_gemma":0.52460986,"teacher_disagreement_score":0.44930205,"about_ca_system_score_codex":4.3572572e-7,"about_ca_system_score_gemma":0.00017932031,"threshold_uncertainty_score":0.9827885},"labels":[],"label_agreement":null},{"id":"W1874571700","doi":"10.1139/e11-036","title":"Source rock potential of Lower to Middle Jurassic black clastic sequences of the Intermontane belt<sup>1</sup>This article is one of a series of papers published in this Special Issue on the theme of <i>New insights in Cordilleran Intermontane geoscience: reducing exploration risk in the mountain pine beetle-affected area, British Columbia</i>.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ministry of Environment","funders":"","keywords":"Clastic rock; Geology; Source rock; Terrane; Lithology; Geochemistry; Paleontology; Volcanic rock; Basement; Total organic carbon; Lithic fragment; Paleozoic; Maturity (psychological); Structural basin; Volcano; Tectonics; Archaeology","score_opus":0.018821620165984418,"score_gpt":0.1881023815838859,"score_spread":0.1692807614179015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1874571700","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99817353,0.0001143964,0.00006441875,0.0005269404,0.00014244491,0.00022830881,0.00001718218,0.000002207127,0.0007305539],"genre_scores_gemma":[0.99962574,0.00006899697,0.0000820841,0.00005234037,0.00006552121,0.0000029992889,7.749336e-7,0.000006964529,0.00009455618],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9978485,0.00022895046,0.00092353125,0.00017205269,0.0005735894,0.00025333758],"domain_scores_gemma":[0.9988889,0.00009451251,0.00045969797,0.00022484132,0.00020116118,0.00013086078],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010188316,0.00011819853,0.00042057483,0.00044935834,0.00009294148,0.00009346612,0.0007693044,0.000063913954,0.0012424808],"category_scores_gemma":[0.0005032726,0.00008648948,0.00012344052,0.0020980441,0.00064765976,0.0005861997,0.000029332312,0.0002786701,6.6340306e-7],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002764557,0.0003683938,0.039432682,0.000141372,0.00015742549,0.00008292353,0.22976613,0.6549419,0.06990212,0.00005451701,0.0014074855,0.0034685794],"study_design_scores_gemma":[0.0032546932,0.0055884733,0.4275452,0.0068110456,0.00026998026,0.0001398531,0.15225318,0.29669344,0.10413833,0.0019329134,0.00043167878,0.00094123365],"about_ca_topic_score_codex":0.10313703,"about_ca_topic_score_gemma":0.6927797,"teacher_disagreement_score":0.58964264,"about_ca_system_score_codex":0.000036276502,"about_ca_system_score_gemma":0.00043983603,"threshold_uncertainty_score":0.9996705},"labels":[],"label_agreement":null},{"id":"W1876905666","doi":"10.1139/cjes-2015-0015","title":"Comparing global and local calibration schemes from a differential split-sample test perspective","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Hydro-Québec; Université Laval","funders":"","keywords":"Equifinality; Environmental science; Calibration; Robustness (evolution); Climate change; Context (archaeology); Mathematics; Computer science; Statistics; Geology","score_opus":0.02906504455672332,"score_gpt":0.23536339985288057,"score_spread":0.20629835529615725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1876905666","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912096,0.00017999939,0.0037231203,0.0012655573,0.00018108782,0.000037423233,0.000010193363,0.000003085751,0.003389887],"genre_scores_gemma":[0.9987032,0.000004273613,0.0010783353,0.0001389696,0.00005163522,3.5190013e-7,6.078389e-7,0.0000012519905,0.00002138316],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993442,0.000028485241,0.00012165046,0.00013531966,0.00016845802,0.00020187709],"domain_scores_gemma":[0.9994867,0.000044629927,0.00006928103,0.000041738353,0.000015987802,0.00034165228],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020841975,0.000067397144,0.000112633265,0.00003962855,0.00026519044,0.000081615624,0.00016253708,0.000023501945,0.00019171168],"category_scores_gemma":[0.00015784056,0.000052481635,0.000019713496,0.00014403352,0.0010677058,0.0003617023,0.000050670427,0.0000644071,0.0000126976975],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000047709473,0.0000059403046,0.996674,4.1497614e-7,0.000009179219,0.0000134147,0.0006781744,0.0009817611,0.000011666254,0.0010964068,0.0003125753,0.0002116885],"study_design_scores_gemma":[0.00042192012,0.00026888328,0.961804,0.000014728954,0.000026716798,0.000018522687,0.003928579,0.013503508,0.000084900676,0.017493332,0.0023026217,0.00013232733],"about_ca_topic_score_codex":0.0557689,"about_ca_topic_score_gemma":0.25715363,"teacher_disagreement_score":0.20138474,"about_ca_system_score_codex":0.00003504107,"about_ca_system_score_gemma":0.00010174857,"threshold_uncertainty_score":0.9505188},"labels":[],"label_agreement":null},{"id":"W1877729059","doi":"10.1139/e11-012","title":"Tectonic significance of Late Ordovician silicic magmatism, Avalon terrane, northern Antigonish Highlands, Nova Scotia <sup>1</sup> This article is one of a series of papers published in <i>CJES Special Issue: In honour of Ward Neale</i> on the theme of Appalachian and Grenvillian geology.<sup>2</sup> Contribution to International Geological Correlation Programme (IGCP) Project 497.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; St. Francis Xavier University","funders":"","keywords":"Geology; Felsic; Zircon; Ordovician; Geochemistry; Volcanic rock; Silicic; Magmatism; Rhyolite; Baltica; Terrane; Provenance; Paleontology; Basalt; Mafic; Tectonics; Volcano","score_opus":0.015293383499823095,"score_gpt":0.20187167329731145,"score_spread":0.18657828979748836,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1877729059","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99524516,0.00025427365,0.000004885691,0.0031866548,0.00008062402,0.00029413938,0.00009196341,0.000002071163,0.0008402426],"genre_scores_gemma":[0.9993934,0.00004010715,0.0003126211,0.00012332956,0.00009031115,0.0000010033534,0.000014674359,0.0000018841747,0.000022688182],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978286,0.00024157981,0.00084299245,0.0002125694,0.00042842544,0.00044582688],"domain_scores_gemma":[0.9985537,0.00028171737,0.0005921772,0.0001188432,0.00023971488,0.00021388335],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017544363,0.00015079846,0.0005187723,0.0004092113,0.00007544286,0.000029616387,0.00042624827,0.00010676206,0.0033972184],"category_scores_gemma":[0.0007406324,0.000095146046,0.0001035457,0.0010902712,0.0010791392,0.00034954757,0.000019997995,0.00024962536,0.0000041923076],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016614726,0.00007495203,0.9827082,0.000025708123,0.00003365634,0.0000036038093,0.0023026401,0.011855738,0.0004145345,0.00009796645,0.000018540044,0.0022982846],"study_design_scores_gemma":[0.0004195319,0.00078144105,0.989248,0.00015088008,0.000026299427,0.00001399604,0.0011082666,0.005430005,0.001884088,0.0006235472,0.00020534942,0.00010864222],"about_ca_topic_score_codex":0.04940576,"about_ca_topic_score_gemma":0.31906447,"teacher_disagreement_score":0.2696587,"about_ca_system_score_codex":0.0000071200684,"about_ca_system_score_gemma":0.0002719301,"threshold_uncertainty_score":0.99751383},"labels":[],"label_agreement":null},{"id":"W1878008342","doi":"10.1139/cjes-2015-0009","title":"Macro- and microstructural analysis of the North Tea Lake Mylonite Zone: an extensional shear zone in the Central Gneiss Belt, Grenville Province, Ontario","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Vedecká Grantová Agentúra MŠVVaŠ SR a SAV","keywords":"Mylonite; Geology; Shear zone; Gneiss; Protolith; Geochemistry; Shear (geology); Petrology; Geomorphology; Seismology; Metamorphic rock; Tectonics","score_opus":0.015460556797872421,"score_gpt":0.1874568092214462,"score_spread":0.17199625242357378,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1878008342","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99800575,0.00049530837,0.0000030289575,0.0009541248,0.00011703664,0.000062725616,0.0000782509,9.109344e-7,0.0002828676],"genre_scores_gemma":[0.99913615,0.000006336642,0.00032460803,0.00036327448,0.00004217917,1.0384116e-7,0.000016886816,7.311831e-7,0.00010971714],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984371,0.00014580383,0.00034919896,0.00019536517,0.0004500154,0.00042251134],"domain_scores_gemma":[0.99891615,0.00007816386,0.00019796488,0.00013314316,0.00011632444,0.00055824575],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00073377974,0.00011736882,0.000281701,0.00027788515,0.00029430052,0.0001171689,0.000634291,0.00004182908,0.0011704287],"category_scores_gemma":[0.00007587123,0.00005491635,0.0001340889,0.0014610017,0.00096972904,0.00021946664,0.000013909791,0.0002521813,0.000002048971],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013241935,0.000006263939,0.9893631,0.0000012148952,0.00003078888,0.000033526496,0.00066794764,0.008749571,0.000013304962,0.000016534826,0.000026462214,0.0010780559],"study_design_scores_gemma":[0.00013163633,0.00024005769,0.99494916,0.0000071247937,0.00010755627,0.00008721993,0.0005129469,0.0019690567,0.00000999247,0.00033514932,0.0015640679,0.000086017964],"about_ca_topic_score_codex":0.4356223,"about_ca_topic_score_gemma":0.99882853,"teacher_disagreement_score":0.5632062,"about_ca_system_score_codex":0.0000040342074,"about_ca_system_score_gemma":0.001104619,"threshold_uncertainty_score":0.9997426},"labels":[],"label_agreement":null},{"id":"W1882002156","doi":"10.1139/e09-040","title":"Teleseismic studies of the Canadian landmass: Lithoprobe and its legacyThis article is one of a series of papers published in this Special Issue on the theme<i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.ESS Contribution 20090305.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; University of British Columbia; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lithosphere; Geology; Subduction; Craton; Seismology; Plate tectonics; Earth science; Tectonics; Paleontology","score_opus":0.012318321302582227,"score_gpt":0.20117687588025251,"score_spread":0.18885855457767028,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1882002156","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9898946,0.0016135387,2.6716486e-7,0.006664582,0.00036162103,0.00029071755,0.00020090875,7.141805e-7,0.00097300584],"genre_scores_gemma":[0.99952275,0.00013983021,0.000043177875,0.00011167791,0.0001244981,0.0000011101731,7.928307e-7,0.0000015704633,0.000054583354],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986769,0.00016356003,0.0004521349,0.00012795851,0.0003289474,0.00025052103],"domain_scores_gemma":[0.99845105,0.00031504207,0.00052775594,0.00012677575,0.0004349582,0.00014443217],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002196795,0.00009991932,0.00035604078,0.00015089223,0.00027929185,0.00010694106,0.00034881217,0.000053052165,0.0005333313],"category_scores_gemma":[0.0012694488,0.00004832964,0.000044307104,0.0005220001,0.001581633,0.00041500528,0.0000107423975,0.00016293286,4.9291054e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00081699603,0.000089974594,0.9036831,0.0006337788,0.0004019958,0.000016461117,0.039699696,0.00086085114,0.016965829,0.030406862,0.002343907,0.0040805526],"study_design_scores_gemma":[0.0023113906,0.0010545821,0.87874067,0.0008754854,0.00017968593,0.00006061474,0.009212716,0.0004802065,0.08081295,0.012579177,0.013362109,0.0003304333],"about_ca_topic_score_codex":0.28393692,"about_ca_topic_score_gemma":0.92356044,"teacher_disagreement_score":0.6396235,"about_ca_system_score_codex":0.000004218098,"about_ca_system_score_gemma":0.0014007137,"threshold_uncertainty_score":0.7208314},"labels":[],"label_agreement":null},{"id":"W1884322885","doi":"10.1139/e11-075","title":"Climate and ground temperature relations at sites across the continuous and discontinuous permafrost zones, northern Canada<sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of <i>Fundamental and applied research on permafrost in Canada</i>.<sup>2</sup>Earth Science Sector (ESS) Contribution 20110128.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Ottawa","funders":"Office of Polar Programs; Natural Sciences and Engineering Research Council of Canada; Ministère de la Défense Nationale; Government of Canada","keywords":"Permafrost; Bedrock; Tundra; Arctic; Snow; Geology; Active layer; Vegetation (pathology); Elevation (ballistics); Physical geography; Solifluction; Atmospheric sciences; Geomorphology; Oceanography; Glacial period; Geography","score_opus":0.026832635168925225,"score_gpt":0.2366226810763521,"score_spread":0.20979004590742686,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1884322885","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9877527,0.0012593823,1.1207922e-8,0.0027428686,0.000119840646,0.0003292052,0.006678818,0.0000010667222,0.0011161454],"genre_scores_gemma":[0.9991375,0.00020720834,0.0000073845554,0.00029215842,0.00020666498,0.000001875559,0.000056042416,0.0000049658724,0.00008616622],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972007,0.00019846566,0.00055502367,0.00028751642,0.00090058066,0.0008576648],"domain_scores_gemma":[0.998182,0.00066603627,0.00029509325,0.00019022012,0.00023658537,0.00043008899],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00281022,0.00019306572,0.00040645554,0.00026570828,0.001109829,0.00027810744,0.00039750116,0.000068795765,0.003312045],"category_scores_gemma":[0.00027433626,0.00012090894,0.000033694625,0.0009425524,0.0027132968,0.0007349288,0.000050593233,0.0004283005,0.0000019947315],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012390553,0.000017598013,0.98179877,0.000019878842,0.000010687211,0.000009488819,0.015126142,0.0002854144,0.0017840052,0.0001213533,0.0004656912,0.00023709478],"study_design_scores_gemma":[0.0004457035,0.0002662017,0.9614458,0.00013970169,0.000010968823,0.00005577169,0.033965148,0.0003752087,0.0015425035,0.000023584691,0.0015827692,0.00014664776],"about_ca_topic_score_codex":0.9162033,"about_ca_topic_score_gemma":0.99954337,"teacher_disagreement_score":0.08334003,"about_ca_system_score_codex":0.000059781825,"about_ca_system_score_gemma":0.002095394,"threshold_uncertainty_score":0.9997255},"labels":[],"label_agreement":null},{"id":"W1889994824","doi":"10.1139/e2012-052","title":"Patterns and mechanisms of fluvial sediment flux and accumulation in two subarctic fjords: Nachvak and Saglek Fjords, Nunatsiavut, Canada","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland","funders":"Canada Research Chairs","keywords":"Fjord; Geology; Sediment; Sedimentary rock; Fluvial; Glacier; Subarctic climate; Sedimentary depositional environment; Oceanography; Sedimentation; Structural basin; Sediment transport; Geomorphology; Geochemistry","score_opus":0.024837193540621846,"score_gpt":0.23684015983164228,"score_spread":0.21200296629102044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1889994824","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99731797,0.0015822876,0.00007347723,0.00040420605,0.00020704787,0.000055480185,0.00002859671,8.8836913e-7,0.0003300586],"genre_scores_gemma":[0.9991768,0.000051414776,0.00055670005,0.00016476505,0.000035370216,1.4213708e-7,0.0000033141237,8.06345e-7,0.000010689295],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991554,0.00004684022,0.00024105563,0.000085252876,0.00019942525,0.00027200344],"domain_scores_gemma":[0.99924916,0.00010799599,0.0001253491,0.00003293406,0.000047784706,0.00043680193],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000681032,0.000075338794,0.00014255577,0.00017761561,0.00019184087,0.000065056636,0.00009585486,0.000023234965,0.00042136363],"category_scores_gemma":[0.000077345,0.000054873144,0.000010566965,0.00019578158,0.00015337399,0.0005816321,0.000005698563,0.00008928715,6.115027e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000034889424,0.0000018915001,0.99563044,0.000018140174,0.0000028367906,0.0000047769654,0.00029660555,0.00032924567,0.000009525178,0.00036033968,0.000011662066,0.0033310507],"study_design_scores_gemma":[0.00018559482,0.00013941164,0.99457294,0.00003851606,0.000006960585,0.00009952242,0.0009852452,0.001423561,0.00013529896,0.0019838712,0.0003539432,0.00007513603],"about_ca_topic_score_codex":0.69008726,"about_ca_topic_score_gemma":0.98675823,"teacher_disagreement_score":0.296671,"about_ca_system_score_codex":0.0000026460173,"about_ca_system_score_gemma":0.00058888015,"threshold_uncertainty_score":0.46136364},"labels":[],"label_agreement":null},{"id":"W1891288283","doi":"10.1139/e2012-033","title":"Enigmatic teeth of small theropod dinosaurs from the Upper Cretaceous (Cenomanian–Turonian) of Uzbekistan","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Cenomanian; Cretaceous; Paleontology; Geology; Theropoda; Taxon","score_opus":0.017635778696634772,"score_gpt":0.19385746912112528,"score_spread":0.1762216904244905,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1891288283","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98350817,0.008613515,0.00003069796,0.0017464377,0.00045858868,0.00009180177,0.00007887084,0.0000019343972,0.0054699657],"genre_scores_gemma":[0.9981887,0.000073255316,0.0013272967,0.00024938426,0.00008403373,1.8556027e-7,0.0000037799236,0.0000013005164,0.00007206063],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873006,0.00019764244,0.00041186716,0.00013294017,0.00017731125,0.0003502027],"domain_scores_gemma":[0.99865246,0.0004312017,0.00036673495,0.00014350773,0.0001236861,0.00028241074],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00058867235,0.00010457199,0.00025064743,0.00013791326,0.00028233064,0.000032447668,0.00075626734,0.00007990289,0.0040427796],"category_scores_gemma":[0.00016865623,0.000060260256,0.00009326799,0.00025021646,0.0017309893,0.0002230731,0.0000050490617,0.00017919125,0.000053104108],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000070323035,0.0000034054983,0.9953848,0.000003299467,0.000024945884,0.000010091316,0.0005507215,0.00036985698,0.00007172431,0.00015569091,0.00017626057,0.003242179],"study_design_scores_gemma":[0.00011231766,0.0003196078,0.9932649,0.000035302346,0.000017500734,0.00008154046,0.0010154619,0.0006148385,0.000048399626,0.0024618877,0.0019541094,0.00007414725],"about_ca_topic_score_codex":0.0680488,"about_ca_topic_score_gemma":0.5774964,"teacher_disagreement_score":0.50944763,"about_ca_system_score_codex":0.000001965902,"about_ca_system_score_gemma":0.0009850914,"threshold_uncertainty_score":0.99686766},"labels":[],"label_agreement":null},{"id":"W1893160325","doi":"10.1139/cjes-2013-0159","title":"The Rock Physical Property Database of British Columbia, and the distinct petrophysical signature of the Chilcotin basalts<sup>,</sup>","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Lithology; Geology; Basalt; Petrophysics; Magnetic susceptibility; Rock magnetism; Magnetic survey; Magnetic mineralogy; Remanence; Mineralogy; Magnetite; Geochemistry; Magnetic anomaly; Geophysics; Magnetization; Porosity; Paleontology; Magnetic field; Chemistry","score_opus":0.008132775907864544,"score_gpt":0.19066662625500963,"score_spread":0.1825338503471451,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1893160325","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99624455,0.0006098491,0.000045589106,0.0017547096,0.00017197365,0.00014306011,0.00009212468,0.0000017367173,0.0009363908],"genre_scores_gemma":[0.9989131,0.000018359671,0.00019210506,0.00018375732,0.00027754458,3.7568392e-7,0.0000010405818,0.0000020577631,0.0004116723],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99803406,0.00057345233,0.00031659516,0.00017996739,0.00051770965,0.00037822386],"domain_scores_gemma":[0.9977958,0.0012493286,0.00027982015,0.00018940549,0.00014486033,0.00034077634],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014187769,0.00009465976,0.0003090232,0.000029039658,0.00076143723,0.00023101366,0.0008887299,0.000034350487,0.00008106781],"category_scores_gemma":[0.0012163172,0.000043833967,0.00016115828,0.0006556973,0.0019957763,0.0001765483,0.000023950055,0.0004182183,0.0000032874423],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001779363,0.0001203091,0.41853726,0.00010418669,0.00011518517,0.000028156577,0.0012913814,0.010796298,0.00021652857,0.001607837,0.005215271,0.56178963],"study_design_scores_gemma":[0.00043118364,0.000572402,0.9368177,0.00009637978,0.00004011349,0.0000617389,0.00020133806,0.05068127,0.000066713066,0.005636424,0.0052782814,0.00011643936],"about_ca_topic_score_codex":0.113392055,"about_ca_topic_score_gemma":0.35468268,"teacher_disagreement_score":0.5616732,"about_ca_system_score_codex":0.0000010450877,"about_ca_system_score_gemma":0.00047578258,"threshold_uncertainty_score":0.89251196},"labels":[],"label_agreement":null},{"id":"W1893436742","doi":"10.1139/e11-009","title":"Thermal and hydrocarbon-charge history and the relationship between diagenesis and reservoir connectivity: Venture field, offshore Nova Scotia, eastern Canada<sup>1</sup>Geological Survey of Canada Contribution 20100418.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada; Saint Mary's University","funders":"Dalhousie University; University of Bern","keywords":"Diagenesis; Geology; Cementation (geology); Carbonate; Fluid inclusions; Geochemistry; Quartz; Petrography; Calcite; Mineralogy; Cement; Paleontology; Chemistry","score_opus":0.04407386875628436,"score_gpt":0.21104149283672102,"score_spread":0.16696762408043667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1893436742","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934782,0.0051476206,0.000045846853,0.0006721533,0.00013659941,0.000071483344,0.000028490884,0.0000023104794,0.0004173275],"genre_scores_gemma":[0.999789,0.000036074744,0.000013933353,0.00008048004,0.00003662058,5.8697066e-7,0.000002679482,0.0000044724957,0.000036160003],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989065,0.00020907552,0.00029461333,0.0001180382,0.00023845574,0.00023333738],"domain_scores_gemma":[0.9987113,0.0005924713,0.00012061039,0.00009190171,0.0001147785,0.00036897475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010181739,0.000108529384,0.0002807388,0.00012965203,0.00016650307,0.000025629013,0.00016436723,0.000070099835,0.00007493888],"category_scores_gemma":[0.000767084,0.00007502105,0.000027313636,0.00021064104,0.0004175607,0.0001615396,0.000014880876,0.00021435256,1.7392031e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001178562,0.0000012427078,0.99716496,0.000009706686,0.00004027715,0.000019749215,0.0005364866,0.0017029329,0.0000031675052,0.00010769319,0.00033623012,0.000065756125],"study_design_scores_gemma":[0.0003237407,0.000050868435,0.98328364,0.000030346904,0.00003776335,0.000017329177,0.00021264046,0.015557609,0.000050883868,0.0000588309,0.00027516994,0.00010116646],"about_ca_topic_score_codex":0.9775317,"about_ca_topic_score_gemma":0.9992636,"teacher_disagreement_score":0.021731915,"about_ca_system_score_codex":0.00004213993,"about_ca_system_score_gemma":0.0017433875,"threshold_uncertainty_score":0.3092695},"labels":[],"label_agreement":null},{"id":"W1893669072","doi":"10.1139/cjes-2014-0113","title":"Second known occurrence of the early Paleocene plesiadapiform <i>Pandemonium</i> (Mammalia: Primates), with description of a new species","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Royal Tyrrell Museum; University of Calgary; University of Alberta","funders":"Core Research for Evolutional Science and Technology; Directorate for Biological Sciences; Government of Alberta","keywords":"Holotype; Paleontology; Geology; Genus; Zoology; Biology","score_opus":0.031250875672979045,"score_gpt":0.1989347478989038,"score_spread":0.16768387222592476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1893669072","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97669625,0.0019980287,0.00008628969,0.0004296552,0.0004485018,0.00006886025,0.000042918637,0.000002248045,0.020227231],"genre_scores_gemma":[0.9984684,0.000056001805,0.00066781265,0.00010027974,0.00006759753,7.7117924e-8,8.673562e-7,8.863173e-7,0.0006380995],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99881667,0.00007676129,0.00035918964,0.000122761,0.000323525,0.00030110078],"domain_scores_gemma":[0.9988396,0.00011030149,0.0004710214,0.00011325827,0.00017591691,0.00028991033],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006808035,0.00010803386,0.00025568984,0.00017025774,0.000317912,0.000048215865,0.0004637488,0.00004513584,0.0006166987],"category_scores_gemma":[0.00011720745,0.000060790317,0.00007417564,0.00048575766,0.0012853906,0.00034638596,0.0000050693297,0.00014774347,0.00000541271],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013803192,0.000002465196,0.99738616,0.000015593583,0.000013115425,0.0000017762442,0.0005807675,0.00025339652,0.000032215627,0.00018017364,0.00062868523,0.0008918492],"study_design_scores_gemma":[0.00022797684,0.00047241093,0.9910887,0.00009827732,0.000020220268,0.000059226022,0.0003898935,0.00010351743,0.00031613963,0.00024585356,0.006898146,0.000079633974],"about_ca_topic_score_codex":0.0078108073,"about_ca_topic_score_gemma":0.8484572,"teacher_disagreement_score":0.8406464,"about_ca_system_score_codex":0.0000017585978,"about_ca_system_score_gemma":0.0012297145,"threshold_uncertainty_score":0.9987963},"labels":[],"label_agreement":null},{"id":"W1895040822","doi":"10.1139/e10-016","title":"The consequences of Canadian Cordillera thermal regime in recent tectonics and elevation: a reviewThis article is one of a series of papers published in this Special Issue on the theme <i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.Geological Survey of Canada Contribution 20090195.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Craton; Geology; Lithosphere; Crust; Tectonics; Plate tectonics; Mantle (geology); Geothermal gradient; Mountain formation; Oceanic crust; Geophysics; Seismology; Earth science; Subduction","score_opus":0.015018014665127298,"score_gpt":0.18266258762597104,"score_spread":0.16764457296084373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1895040822","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97797686,0.0025286272,1.725806e-7,0.017839856,0.00006407261,0.00018880233,0.000094014234,3.284131e-7,0.0013072601],"genre_scores_gemma":[0.99899197,0.00076432066,0.000054500666,0.00015046801,0.000020330604,8.191595e-7,0.0000021788546,6.0441874e-7,0.000014806652],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99828726,0.00032303212,0.0006568921,0.0001294722,0.00034728425,0.00025603414],"domain_scores_gemma":[0.99751556,0.0010086087,0.000621097,0.000109944165,0.00058407255,0.00016072067],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0036395516,0.00008828647,0.000392929,0.00015950156,0.00014942898,0.000028532439,0.00032959584,0.000055911543,0.0025155675],"category_scores_gemma":[0.0049989894,0.00004029099,0.000037048238,0.0014463058,0.002877619,0.00012709669,0.000008142364,0.00021992381,1.1006713e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019534068,0.0000135665005,0.9962121,0.000026277554,0.000027767283,0.0000028956983,0.00041727792,0.00015080422,0.0005960932,0.0010616925,0.00014800558,0.0011481382],"study_design_scores_gemma":[0.00036486046,0.00032528702,0.9905844,0.00012142966,0.000022170223,0.000012123859,0.0008575688,0.00031160325,0.003706817,0.002365179,0.0012584777,0.00007010162],"about_ca_topic_score_codex":0.95314837,"about_ca_topic_score_gemma":0.99896026,"teacher_disagreement_score":0.045811936,"about_ca_system_score_codex":0.0000063388106,"about_ca_system_score_gemma":0.002654326,"threshold_uncertainty_score":0.99983597},"labels":[],"label_agreement":null},{"id":"W1895131872","doi":"10.1139/e09-057","title":"Melting of the continental crust during orogenesis: the thermal, rheological, and compositional consequences of melt transport from lower to upper continental crustThis article is one of a selection of papers published in this Special Issue on the the theme<i>Lithoprobe—parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":163,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Continental crust; Anatexis; Crust; Partial melting; Metamorphism; Petrology; Geochemistry; Mineralogy","score_opus":0.008385485404939753,"score_gpt":0.17799265072181575,"score_spread":0.169607165316876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1895131872","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9878745,0.00048128725,0.0000011008971,0.010613788,0.00009077583,0.00022287577,0.000080745,9.459342e-7,0.0006339715],"genre_scores_gemma":[0.99952537,0.000028323046,0.00012274976,0.00023341655,0.00007311208,0.0000013989813,9.827577e-7,0.0000011787919,0.000013458107],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984161,0.000191658,0.0005894465,0.00016205315,0.00043933312,0.00020140635],"domain_scores_gemma":[0.99829376,0.00069599994,0.00056516856,0.00010997476,0.0002405582,0.00009455697],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013374127,0.00011089815,0.00033526673,0.0000833017,0.00028160025,0.000037388905,0.00048898236,0.00005316937,0.0049357545],"category_scores_gemma":[0.00046137202,0.00004130433,0.0001238467,0.000673066,0.003866319,0.0001390046,0.000016620332,0.00023372285,3.582395e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025693135,0.00003599651,0.9466696,0.000014058517,0.000059195074,9.470579e-7,0.0014599849,0.000303537,0.05062922,0.00034425894,0.000020284624,0.00020602877],"study_design_scores_gemma":[0.000429639,0.00020961276,0.90268165,0.00010196233,0.00007173436,0.000017388491,0.0025733905,0.00033875176,0.09267809,0.0007791272,0.00005647615,0.00006215461],"about_ca_topic_score_codex":0.047822822,"about_ca_topic_score_gemma":0.12583989,"teacher_disagreement_score":0.07801706,"about_ca_system_score_codex":0.0000022152117,"about_ca_system_score_gemma":0.0002637344,"threshold_uncertainty_score":0.99884456},"labels":[],"label_agreement":null},{"id":"W1897211107","doi":"10.1139/e10-026","title":"Application of modern 2-D and 3-D seismic-reflection techniques for uranium exploration in the Athabasca BasinThis article is one of a series of papers published in this Special Issue on the theme<i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; Cameco (Canada); Geological Survey of Canada","funders":"","keywords":"Geology; Unconformity; Structural basin; Borehole; Basement; Geochemistry; Drilling; Seismology; Geomorphology; Mining engineering; Paleontology","score_opus":0.01756182333700454,"score_gpt":0.21626273028116366,"score_spread":0.19870090694415912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1897211107","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916532,0.000574328,0.00012976635,0.0059093023,0.000060888102,0.00042943083,0.000027493563,0.000001135806,0.001214442],"genre_scores_gemma":[0.9992884,0.000102840386,0.0004587215,0.00007357347,0.00006170305,0.000005067494,7.0788866e-7,0.0000011079944,0.000007910437],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991373,0.000089274305,0.0003406368,0.000100882295,0.00021272576,0.00011918017],"domain_scores_gemma":[0.99896353,0.0003918579,0.0003612305,0.000088614834,0.00016252836,0.000032239597],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019977884,0.00006482912,0.00018808962,0.0001606935,0.00012784453,0.000038923838,0.00017854657,0.00003587471,0.00008284948],"category_scores_gemma":[0.0003856938,0.00003253292,0.00003254835,0.00048234945,0.00088594033,0.00038610687,0.0000038629555,0.00011872772,8.595548e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009620517,0.00007302049,0.8566192,0.00025183844,0.000058462585,0.0000010236438,0.043557115,0.00039247426,0.0045916704,0.004712376,0.0003171975,0.088463575],"study_design_scores_gemma":[0.0018452875,0.0030696935,0.8200033,0.000398918,0.000093480114,0.00004825402,0.018182455,0.010326651,0.10681796,0.0350944,0.0038786647,0.00024094793],"about_ca_topic_score_codex":0.019445216,"about_ca_topic_score_gemma":0.35918787,"teacher_disagreement_score":0.33974266,"about_ca_system_score_codex":0.0000018132373,"about_ca_system_score_gemma":0.00025582322,"threshold_uncertainty_score":0.9870844},"labels":[],"label_agreement":null},{"id":"W1905061550","doi":"10.1139/e08-051","title":"Lower Silurian subduction-related volcanic rocks in the Chaleurs Group, northern New Brunswick, CanadaGeological Survey of Canada, Contribution No. 2008-0166.Contribution to Natural Resources Canada’s Targeted Geoscience Initiative 3 (2005–2010).","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Geological Survey of Canada","funders":"","keywords":"Geology; Felsic; Mafic; Geochemistry; Volcanic rock; Subduction; Volcanic arc; Zircon; Conglomerate; Continental crust; Sedimentary rock; Crust; Paleontology; Volcano; Tectonics","score_opus":0.014997062968555578,"score_gpt":0.18118573998346385,"score_spread":0.16618867701490828,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1905061550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9900158,0.0016957254,0.000020788508,0.0066790897,0.0010233868,0.00017067997,0.00019446672,0.00000324174,0.00019680196],"genre_scores_gemma":[0.99844337,0.000025367232,0.00003766446,0.0010324252,0.000101861966,3.459667e-7,0.00006989152,0.0000018559524,0.0002872271],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99634725,0.0004610238,0.0007639717,0.00036758443,0.0010188525,0.0010413085],"domain_scores_gemma":[0.996916,0.0004841074,0.0004560867,0.00015645589,0.00083789905,0.0011494309],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019319118,0.00023226952,0.00046201365,0.00028167068,0.0008215047,0.000057453606,0.0009531496,0.00010185846,0.00144295],"category_scores_gemma":[0.0033021115,0.00014646954,0.00008968833,0.0019536822,0.0006738275,0.00029046863,0.000013399128,0.0005113605,0.000008858329],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004608801,0.000009711758,0.9889949,0.0000012574894,0.000018807454,0.00024251213,0.00017014687,0.0075144363,0.000019034958,0.000014579185,0.0028603,0.00010820567],"study_design_scores_gemma":[0.00025943262,0.0002887837,0.99278563,0.000021304779,0.000013142971,0.00014441027,0.00022567832,0.001377204,0.000037526417,0.0001560494,0.004485143,0.00020570453],"about_ca_topic_score_codex":0.9998195,"about_ca_topic_score_gemma":0.99999964,"teacher_disagreement_score":0.022994844,"about_ca_system_score_codex":0.00006485192,"about_ca_system_score_gemma":0.023059696,"threshold_uncertainty_score":0.9994699},"labels":[],"label_agreement":null},{"id":"W1906830522","doi":"10.1139/cjes-2013-0009","title":"Ordovician conodont biostratigraphy and redefinition of the age of lithostratigraphic units on northeastern Melville Peninsula, Nunavut","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Nunavut; Nunavut Research Institute","funders":"","keywords":"Conodont; Ordovician; Geology; Paleontology; Peninsula; Biostratigraphy; Paleozoic; Bay; Trilobite; Macrofossil; Outcrop; Oceanography; Archaeology; Geography","score_opus":0.03548779827284864,"score_gpt":0.19099070622074124,"score_spread":0.1555029079478926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1906830522","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99121255,0.00079783483,0.000002587067,0.0011138857,0.00017744128,0.00010218105,0.000028655622,0.0000011166943,0.0065637482],"genre_scores_gemma":[0.99959314,0.000083408624,0.00012502231,0.0001615199,0.000023392764,2.3597883e-7,0.0000023372647,6.8644414e-7,0.000010247155],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99912703,0.00007338315,0.00030165742,0.000095740405,0.00021624894,0.00018592835],"domain_scores_gemma":[0.99925786,0.00008560717,0.0002618208,0.00007087628,0.00014572342,0.00017812534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003222959,0.00007817495,0.00016218165,0.00015529525,0.00029975342,0.00006147588,0.00021152884,0.00003601295,0.00027704044],"category_scores_gemma":[0.00010172919,0.000043459917,0.00005127874,0.00057806313,0.0007947986,0.00016821551,0.0000034584348,0.0000963395,0.0000038760713],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004326961,0.0000032303171,0.9968753,0.000005325251,0.000007799963,0.000003364951,0.00028895139,0.0004554779,0.00005102202,0.00040459054,0.000020455276,0.0018801544],"study_design_scores_gemma":[0.000093898794,0.0007687448,0.99573934,0.00006108018,0.0000071350887,0.00001179252,0.001205514,0.00019000967,0.000111976835,0.0012538478,0.00050302467,0.000053618125],"about_ca_topic_score_codex":0.036784727,"about_ca_topic_score_gemma":0.6289662,"teacher_disagreement_score":0.59218144,"about_ca_system_score_codex":4.144945e-7,"about_ca_system_score_gemma":0.00022500267,"threshold_uncertainty_score":0.9696294},"labels":[],"label_agreement":null},{"id":"W1911857431","doi":"10.1139/cjes-2012-0164","title":"Introduction to Special Issue of<i>Canadian Journal of Earth Sciences</i>: Canadian contributions to planetary geoscience","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; University of British Columbia; Geological Survey of Canada","funders":"","keywords":"Enthusiasm; Library science; Attendance; Earth science; Planetary science; Publication; Session (web analytics); Geology; Astrobiology; Political science; Computer science; Physics","score_opus":0.012737556063248053,"score_gpt":0.21471354683457244,"score_spread":0.2019759907713244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1911857431","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9581978,0.00010946902,0.0005694846,0.03012303,0.004115012,0.00032071685,0.00041569505,0.000002013687,0.0061468338],"genre_scores_gemma":[0.99146754,0.000004009469,0.0023429608,0.0006740027,0.0052241366,0.0000011742651,0.000013143155,0.000003832931,0.00026921212],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99767727,0.000073805604,0.00061936054,0.00024782962,0.0005222069,0.0008595045],"domain_scores_gemma":[0.99547887,0.00004858424,0.0003518722,0.00014556495,0.0007303831,0.0032447537],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016441508,0.00015437603,0.00029943156,0.002914221,0.0010979756,0.00048593516,0.0009709044,0.000044468903,0.003110034],"category_scores_gemma":[0.00022350083,0.00013183648,0.000088830115,0.002962668,0.00079941977,0.0018456592,0.0000100986945,0.00023954321,0.00038141123],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019097475,0.00004215269,0.59630185,0.000010369203,0.000071121256,0.000104848266,0.0063086925,0.07556318,0.0044338824,0.011933123,0.2897706,0.015441062],"study_design_scores_gemma":[0.00026972714,0.0013474657,0.28003493,0.00009709379,0.000029099896,0.00017301078,0.00334326,0.0004909629,0.0016271106,0.0018297863,0.71037334,0.00038419457],"about_ca_topic_score_codex":0.73168486,"about_ca_topic_score_gemma":0.9587805,"teacher_disagreement_score":0.42060274,"about_ca_system_score_codex":0.000024048151,"about_ca_system_score_gemma":0.014443288,"threshold_uncertainty_score":0.99780124},"labels":[],"label_agreement":null},{"id":"W1912087970","doi":"10.1139/cjes-2014-0097","title":"Palaeobiogeographic relationships and palaeoenvironmental implications of an earliest Oligocene Tethyan ichthyofauna from Egypt","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Ichthyology and Marine Biology","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Fauna; Cenozoic; Paleontology; Brackish water; Shore; Oceanography; Ecology; Structural basin; Salinity; Biology","score_opus":0.013728546677670235,"score_gpt":0.20781203887202074,"score_spread":0.1940834921943505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1912087970","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953808,0.00012508054,0.00006198215,0.000702942,0.00013220843,0.000051348747,0.000021078995,0.0000027061512,0.0035218266],"genre_scores_gemma":[0.997409,0.000026457106,0.0022888167,0.00018702107,0.000047840553,9.4064393e-7,0.000005148426,0.0000037009274,0.00003108299],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990069,0.0001644559,0.00027787272,0.00018769526,0.00011387998,0.00024919107],"domain_scores_gemma":[0.9991005,0.00012647256,0.00018412195,0.00014773732,0.000011728844,0.00042941616],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00079612876,0.00009130617,0.00015352025,0.00014813399,0.00041767198,0.000023051574,0.00033222025,0.000083877734,0.0008018663],"category_scores_gemma":[0.00012834842,0.0000766239,0.000040329618,0.00023807897,0.0020521707,0.00029740672,0.00003972308,0.00016679273,0.000028865006],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002904097,0.000010737188,0.9953058,5.7253294e-7,0.000005961031,0.0000016684996,0.00017184422,0.00014198115,0.0013191784,0.0006796143,0.000032132815,0.0023276552],"study_design_scores_gemma":[0.00014874201,0.0003076315,0.9908162,0.000006040822,0.000016491542,0.00005455652,0.00018020527,0.000071920294,0.0003141409,0.0053119967,0.0026876822,0.000084398926],"about_ca_topic_score_codex":0.010870807,"about_ca_topic_score_gemma":0.15670209,"teacher_disagreement_score":0.14583129,"about_ca_system_score_codex":0.0000069393404,"about_ca_system_score_gemma":0.000078358644,"threshold_uncertainty_score":0.9957159},"labels":[],"label_agreement":null},{"id":"W1917589268","doi":"10.1139/cjes-2013-0046","title":"U–Pb zircon ages and field relationships of Archean basement and Proterozoic intrusions, south-central Wopmay Orogen, NWT: implications for tectonic assignments","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of British Columbia; Memorial University of Newfoundland; Government of Northwest Territories","funders":"","keywords":"Geology; Zircon; Metamorphism; Geochemistry; Terrane; Archean; Basement; Craton; Plutonism; Proterozoic; Pluton; Petrology; Paleontology; Tectonics; Archaeology","score_opus":0.03607198036993034,"score_gpt":0.2176303517284608,"score_spread":0.18155837135853045,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1917589268","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99353266,0.0008132705,0.00044050458,0.0047369204,0.00004048561,0.0001885605,0.00003331166,0.0000016860618,0.00021259091],"genre_scores_gemma":[0.9954912,0.000034926717,0.0042368965,0.00017065299,0.0000295082,0.000002179194,0.0000048322077,7.209951e-7,0.0000290971],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991506,0.000052127758,0.0002701722,0.00013941558,0.000112047324,0.00027567075],"domain_scores_gemma":[0.9989649,0.00024456257,0.00015754049,0.000060160866,0.00008123081,0.00049161416],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00044050385,0.00007315716,0.00014455951,0.00014141221,0.00037084188,0.00007992552,0.00015853313,0.000040302468,0.001074533],"category_scores_gemma":[0.00033650533,0.000048224614,0.000046076933,0.0002028188,0.00031727002,0.00018544457,0.0000070338488,0.000115205316,0.000003318699],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000024200942,0.0000034931395,0.9925917,0.0000071299432,0.000011302697,5.4251257e-7,0.00014381637,0.00008762477,0.0007682897,0.00013974328,0.00005253613,0.00619141],"study_design_scores_gemma":[0.00012487789,0.00028011415,0.985232,0.000024120474,0.000021182817,0.000013571733,0.0002921284,0.0005794836,0.0010632399,0.012044723,0.000255515,0.00006905336],"about_ca_topic_score_codex":0.007180165,"about_ca_topic_score_gemma":0.059041098,"teacher_disagreement_score":0.051860936,"about_ca_system_score_codex":0.0000013393978,"about_ca_system_score_gemma":0.00019077788,"threshold_uncertainty_score":0.9998386},"labels":[],"label_agreement":null},{"id":"W1918164806","doi":"10.1139/cjes-2015-0041","title":"Early Wisconsinan (MIS 4) glaciation on Haida Gwaii, British Columbia, and implications for biological refugia","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of the Fraser Valley; Simon Fraser University","funders":"Hakai Institute; Natural Sciences and Engineering Research Council of Canada; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Geology; Pleistocene; Radiocarbon dating; Glacial period; Peat; Silt; Marine isotope stage; Palynology; Interglacial; Paleontology; Archaeology; Pollen; Oceanography; Ecology; Geography","score_opus":0.059810908769301944,"score_gpt":0.2649001392501636,"score_spread":0.20508923048086164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1918164806","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930695,0.0009933406,0.000020087013,0.0020959422,0.00026510312,0.00011454681,0.000058712947,0.0000034118384,0.0033793466],"genre_scores_gemma":[0.9984332,0.000025259116,0.00091542065,0.00027386547,0.00006657871,7.430994e-7,0.000007348828,9.4009664e-7,0.00027664614],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990799,0.000096700525,0.00019621776,0.00016471524,0.00010715064,0.00035535338],"domain_scores_gemma":[0.99874806,0.00025001296,0.00011112241,0.00006349419,0.0001821743,0.0006451131],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011752992,0.000052389903,0.00014621182,0.00012627622,0.00060318003,0.0003142524,0.00023098224,0.00009116852,0.00025620463],"category_scores_gemma":[0.0005144721,0.000054388776,0.000034856694,0.0002346429,0.0008784422,0.00023063045,0.0000025398558,0.0001434054,0.00001814368],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000069530142,0.0000024598492,0.9957452,0.0000013411208,0.0000047938165,0.000014487308,0.00006841759,0.000038128666,9.873389e-7,0.000119483026,0.00055645325,0.003441294],"study_design_scores_gemma":[0.00022396591,0.0009792129,0.988888,0.000015259095,0.000004426131,0.0004167853,0.0001349391,0.00008572385,0.0000017617272,0.0044372533,0.0047444534,0.00006818562],"about_ca_topic_score_codex":0.040144637,"about_ca_topic_score_gemma":0.91298074,"teacher_disagreement_score":0.8728361,"about_ca_system_score_codex":7.455782e-7,"about_ca_system_score_gemma":0.0009954864,"threshold_uncertainty_score":0.96624714},"labels":[],"label_agreement":null},{"id":"W1919454924","doi":"10.1139/cjes-2013-0171","title":"Conodonts recovered from the carbonate xenoliths in the kimberlites confirm the Paleozoic cover on the Hall Peninsula, Nunavut","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Peregrine Diamonds (Canada); Government of Nunavut; Nunavut Research Institute","funders":"","keywords":"Geology; Kimberlite; Paleozoic; Paleontology; Ordovician; Conodont; Xenolith; Sedimentary rock; Geochemistry; Biostratigraphy; Mantle (geology)","score_opus":0.02161798564507902,"score_gpt":0.18901091797809827,"score_spread":0.16739293233301925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1919454924","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9335652,0.0012125681,0.0000016722385,0.032173667,0.00025356843,0.00010539559,0.000071118564,0.0000019228016,0.032614917],"genre_scores_gemma":[0.9910514,0.000039631064,0.000018148088,0.008536402,0.00020127214,6.961346e-7,0.000006217668,0.0000011910976,0.00014505877],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979861,0.00055250933,0.00033474693,0.0002004135,0.0004760516,0.00045020203],"domain_scores_gemma":[0.9959941,0.0032288213,0.00022114444,0.00025418028,0.000076838005,0.00022493291],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002622694,0.00014367425,0.00020462065,0.00006160941,0.0007362978,0.00038592858,0.001628387,0.000051073275,0.004950607],"category_scores_gemma":[0.0009422945,0.000046220222,0.000145862,0.00054111116,0.0011393679,0.00012838696,0.000009672883,0.00044435507,0.00015489839],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014457966,0.0000053855347,0.9922495,7.7215384e-7,0.000019664232,0.000019195706,0.00082166994,0.0034148844,0.000011667692,0.0009602563,0.0009170319,0.0015655257],"study_design_scores_gemma":[0.0001501038,0.0001867794,0.9257485,0.000025422298,0.000026259988,0.00002485531,0.0011031239,0.005796866,0.000033371092,0.029437676,0.037358146,0.00010888593],"about_ca_topic_score_codex":0.1262928,"about_ca_topic_score_gemma":0.7380671,"teacher_disagreement_score":0.61177427,"about_ca_system_score_codex":0.0000020356429,"about_ca_system_score_gemma":0.0003014406,"threshold_uncertainty_score":0.995959},"labels":[],"label_agreement":null},{"id":"W1919854441","doi":"10.1139/e2012-047","title":"Metallogeny of the Marco zone, Corvet Est, disseminated gold deposit, James Bay, Quebec, Canada","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Université Laval","funders":"University of Ottawa","keywords":"Geology; Arsenopyrite; Geochemistry; Metamorphism; Andesite; Dacite; Metamorphic rock; Basaltic andesite; Basalt; Volcanic rock; Petrology; Chalcopyrite; Volcano","score_opus":0.010324664815224349,"score_gpt":0.17901691333627828,"score_spread":0.16869224852105394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1919854441","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896389,0.0046663587,0.000005741519,0.0016009038,0.00043455497,0.0000428877,0.000041826457,0.000001620194,0.003567182],"genre_scores_gemma":[0.9986055,0.000021587779,0.00021853256,0.00041481727,0.000078503246,1.12928504e-7,0.0000034789066,0.0000010853981,0.000656393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99842334,0.00010488119,0.00036620273,0.0001224175,0.0004468122,0.00053632754],"domain_scores_gemma":[0.99848914,0.0001786508,0.0002694621,0.00012230221,0.00011995789,0.0008204924],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005805585,0.00012187606,0.0002576241,0.00010840121,0.00024620624,0.000055348133,0.0007475091,0.000045729616,0.003805658],"category_scores_gemma":[0.00025756808,0.0000644028,0.0001454815,0.00081057654,0.0006316573,0.0002588833,0.000012404928,0.00018125695,0.000008271929],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003304006,0.0000046768805,0.9963091,0.00000418563,0.00002473516,0.000015421547,0.000061713996,0.00056799187,0.0001264435,0.000052280127,0.000889149,0.0019409704],"study_design_scores_gemma":[0.000056109853,0.000046274028,0.9902994,0.000021747881,0.000046023524,0.0000708645,0.00034495545,0.0002670399,0.0013689146,0.00019781844,0.0071762325,0.00010462687],"about_ca_topic_score_codex":0.9814035,"about_ca_topic_score_gemma":0.9997356,"teacher_disagreement_score":0.018332075,"about_ca_system_score_codex":0.0000042821066,"about_ca_system_score_gemma":0.001274656,"threshold_uncertainty_score":0.997105},"labels":[],"label_agreement":null},{"id":"W1920874772","doi":"10.1139/e2012-039","title":"Taxonomic diversity, stratigraphic range, and exceptional preservation of Juro-Cretaceous salamanders from northern China","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Amphibian and Reptile Biology","field":"Environmental Science","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Chinese Academy of Geological Sciences; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Cretaceous; Salamander; Paleontology; Aptian; Geology; Range (aeronautics); Mesozoic; China; Taxon; Ecology; Geography; Biology; Archaeology; Structural basin","score_opus":0.015479499439950915,"score_gpt":0.18599342990339668,"score_spread":0.17051393046344576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1920874772","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99722815,0.00017955799,0.000045628585,0.00049304246,0.000112898866,0.000071962815,0.00000820236,0.0000013249569,0.0018592398],"genre_scores_gemma":[0.99933004,0.00003022384,0.00045261008,0.00006250959,0.00003680061,3.4341633e-7,8.2999935e-7,0.0000015544069,0.00008505658],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993657,0.000037691065,0.00016517028,0.000117122974,0.00015855319,0.00015576725],"domain_scores_gemma":[0.99947643,0.00002738207,0.00017187801,0.000054744807,0.000017396604,0.00025216755],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019878993,0.00006124917,0.00010518069,0.000088005705,0.00025028986,0.000035891055,0.00024683026,0.000040303188,0.0021932072],"category_scores_gemma":[0.000024362405,0.00004683801,0.000039423165,0.00012524285,0.0010611893,0.00044123302,0.000042841682,0.00007032533,0.00001987955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000022144472,0.0000033821439,0.99712265,8.509608e-7,0.000006104737,0.0000026113432,0.0003141684,0.0003437915,0.0007566562,0.000017088461,0.00022632629,0.0012041517],"study_design_scores_gemma":[0.00013698661,0.00012379553,0.997752,0.0000084814155,0.000005686535,0.000012348403,0.0002276053,0.00021953434,0.000034174085,0.0010722498,0.0003516985,0.00005542543],"about_ca_topic_score_codex":0.030351777,"about_ca_topic_score_gemma":0.3337233,"teacher_disagreement_score":0.30337152,"about_ca_system_score_codex":0.000007748471,"about_ca_system_score_gemma":0.00012739548,"threshold_uncertainty_score":0.9987189},"labels":[],"label_agreement":null},{"id":"W1923076431","doi":"10.1139/cjes-2013-0186","title":"A previously undescribed caenagnathid mandible from the late Campanian of Alberta, and insights into the diet of<i>Chirostenotes pergracilis</i>(Dinosauria: Oviraptorosauria)","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Omnivore; Mandible (arthropod mouthpart); Herbivore; Mandibular symphysis; Biology; Symphysis; Shearing (physics); Anatomy; Geology; Predation; Zoology; Paleontology; Genus","score_opus":0.011691276432326364,"score_gpt":0.19071112508671492,"score_spread":0.17901984865438855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1923076431","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9837219,0.012143755,0.000011696616,0.0021952493,0.0004935367,0.000087612076,0.000025287864,0.0000015611926,0.0013194083],"genre_scores_gemma":[0.9989616,0.0003201154,0.00021271102,0.00034308337,0.00009387955,2.657943e-7,0.0000052570595,0.0000013256708,0.000061712126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986469,0.00033608737,0.00036786223,0.00015321051,0.00019222747,0.00030370362],"domain_scores_gemma":[0.99806356,0.0011207177,0.00031811197,0.00015905421,0.00008815623,0.0002503983],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009653169,0.0001190236,0.00026998934,0.000119219396,0.0006241633,0.000041711617,0.00059515005,0.000089170644,0.00021696447],"category_scores_gemma":[0.0004005635,0.000059514954,0.000076512515,0.00027256057,0.0021658945,0.0002516833,0.000010533082,0.00020047405,0.000006543337],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003784936,0.0000038259773,0.9875319,0.0000066895177,0.000035925794,0.000004486072,0.009783818,0.0004696862,0.00012864028,0.00063861825,0.000097340104,0.0012611912],"study_design_scores_gemma":[0.00019971219,0.0006847346,0.98469245,0.000055270466,0.00003757243,0.000038391998,0.001248773,0.00076352817,0.00006722156,0.006410903,0.005712238,0.00008919845],"about_ca_topic_score_codex":0.15597309,"about_ca_topic_score_gemma":0.93253183,"teacher_disagreement_score":0.77655876,"about_ca_system_score_codex":0.0000014930307,"about_ca_system_score_gemma":0.00057521753,"threshold_uncertainty_score":0.84964734},"labels":[],"label_agreement":null},{"id":"W1923754883","doi":"10.1139/cjes-2015-0067","title":"Geology of the orogenic Cheminis gold deposit along the Larder Lake – Cadillac deformation zone, Ontario","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Archean; Volcanic rock; Greenstone belt; Basalt; Shear zone; Lineation; Cleavage (geology); Cataclastic rock; Crenulation; Petrology; Volcano; Tectonics; Paleontology","score_opus":0.018397057786426335,"score_gpt":0.18218005640480103,"score_spread":0.1637829986183747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1923754883","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98960334,0.00094223017,0.000009414797,0.0022281702,0.00022042402,0.00004467832,0.000010525148,0.0000014632457,0.006939758],"genre_scores_gemma":[0.9988644,0.000007801997,0.00020042379,0.000464812,0.00005530823,1.3652344e-7,0.0000031056884,6.076273e-7,0.00040341163],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988615,0.000069736205,0.00032534834,0.00010162361,0.00033457566,0.00030723406],"domain_scores_gemma":[0.9989899,0.00008590804,0.0002417501,0.00011508748,0.00017415264,0.0003931954],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008683391,0.00008403457,0.00016911948,0.00007863461,0.0002349498,0.000057115813,0.0006646154,0.000054830845,0.0026090033],"category_scores_gemma":[0.00018765316,0.000037436726,0.00012944244,0.0005094928,0.0007139407,0.0001813949,0.000012394833,0.00019872586,0.000036463625],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000037064221,0.0000021258193,0.99463,0.0000014069734,0.000014841682,0.0000065535837,0.0005062457,0.0037697514,0.0000078276935,0.000035703226,0.00024403207,0.00077779655],"study_design_scores_gemma":[0.00011270366,0.000111550806,0.98357964,0.000011106129,0.00003303018,0.0002221059,0.0005526475,0.000639355,0.0004295975,0.0014022772,0.012834178,0.000071811555],"about_ca_topic_score_codex":0.3440446,"about_ca_topic_score_gemma":0.9962389,"teacher_disagreement_score":0.65219426,"about_ca_system_score_codex":0.0000033165225,"about_ca_system_score_gemma":0.001138766,"threshold_uncertainty_score":0.99830276},"labels":[],"label_agreement":null},{"id":"W1924849930","doi":"10.1139/cjes-2015-0064","title":"The black rock coatings in Rouyn-Noranda, Québec: fingerprints of historical smelter emissions and the local ore","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University; Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Jarosite; Geology; Mineralogy; Smelting; Geochemistry; Hematite; Chromite; Metallurgy; Materials science","score_opus":0.020896731850533857,"score_gpt":0.19786744348089869,"score_spread":0.17697071163036482,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1924849930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9823288,0.0030686557,0.000056643217,0.012220243,0.00011985259,0.00003910553,0.0000037763732,0.0000010375777,0.0021618956],"genre_scores_gemma":[0.99935126,0.00003863713,0.00008610594,0.00021674926,0.00004057724,1.1587262e-7,3.4557573e-7,5.3056846e-7,0.00026568474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989307,0.000107284795,0.0003240079,0.00010609078,0.0002785107,0.00025341724],"domain_scores_gemma":[0.99869543,0.00045173138,0.00016329755,0.000068926645,0.00011707954,0.00050352834],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014180443,0.00007102449,0.0001981208,0.000082877974,0.00026933543,0.000064616375,0.0004001966,0.00003500233,0.00043511295],"category_scores_gemma":[0.0008898008,0.000029807386,0.000061412655,0.0004413846,0.0011379103,0.00010596151,0.0000107772275,0.00019557173,0.0000095501355],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034468674,0.0000030392794,0.9882862,0.0000017884684,0.0000054853676,0.000014325361,0.0007112242,0.0054559293,0.000003733334,0.00007952402,0.0007050725,0.0046992116],"study_design_scores_gemma":[0.0012032439,0.00046826748,0.8999691,0.00007662603,0.000044558892,0.00011013217,0.003881011,0.03205099,0.000097454,0.019185958,0.04269478,0.00021785621],"about_ca_topic_score_codex":0.3127175,"about_ca_topic_score_gemma":0.87585855,"teacher_disagreement_score":0.56314105,"about_ca_system_score_codex":0.0000057493635,"about_ca_system_score_gemma":0.00095025153,"threshold_uncertainty_score":0.6918592},"labels":[],"label_agreement":null},{"id":"W1930767292","doi":"10.1139/cjes-2013-0115","title":"Plume–plate interaction","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Plume; Geology; Plate tectonics; Mantle plume; Panache; Hotspot (geology); Geophysics; Meteorology; Paleontology; Geography; Lithosphere; Tectonics","score_opus":0.015486874880743242,"score_gpt":0.2080923402778804,"score_spread":0.19260546539713716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1930767292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98023087,0.00013109847,0.00010478667,0.000386113,0.002415798,0.000029337574,0.00002211294,0.0000033799452,0.016676534],"genre_scores_gemma":[0.99874586,0.0000078880885,0.00052117556,0.00019213904,0.00037313186,3.988363e-8,0.0000019552353,0.0000011135783,0.00015670455],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999196,0.00006189488,0.00020589009,0.00009597515,0.00018025361,0.00025999523],"domain_scores_gemma":[0.9992389,0.00006600398,0.00016322204,0.00006381284,0.00006741683,0.00040061702],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008324875,0.000066545355,0.00013193098,0.00017794505,0.0002674469,0.00023992741,0.0002804082,0.000027257847,0.0027047738],"category_scores_gemma":[0.000087951485,0.000048493108,0.000044197917,0.00018072309,0.00017166874,0.00048041748,0.000002101993,0.00008123159,0.00013841817],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052482952,0.000016033382,0.8267945,0.00004302849,0.00007894182,0.00017489861,0.0023786742,0.05449405,0.0023101743,0.006877519,0.0063789207,0.10040079],"study_design_scores_gemma":[0.00023193556,0.00063242484,0.6255617,0.000073342846,0.000019704725,0.0001636988,0.00023539412,0.003666687,0.0011284754,0.004688795,0.36336648,0.0002313434],"about_ca_topic_score_codex":0.018373815,"about_ca_topic_score_gemma":0.18874167,"teacher_disagreement_score":0.35698757,"about_ca_system_score_codex":5.656228e-7,"about_ca_system_score_gemma":0.000374007,"threshold_uncertainty_score":0.9982069},"labels":[],"label_agreement":null},{"id":"W1930878863","doi":"10.1139/cjes-2015-0025","title":"Early Devonian graptolites from the Qinzhou–Yulin region, southeast Guangxi, China","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Biozone; Geology; Devonian; Paleontology; Biostratigraphy","score_opus":0.034467571050614466,"score_gpt":0.21588364295107157,"score_spread":0.1814160719004571,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1930878863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9492357,0.014835895,0.000048521335,0.00346755,0.00088665856,0.00006356745,0.000064497086,0.0000064684195,0.031391148],"genre_scores_gemma":[0.99872655,0.000020974305,0.00067959604,0.00020000721,0.00032666986,1.4227601e-7,0.000001625872,8.771221e-7,0.000043575918],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99844325,0.00018646244,0.00032941537,0.00018621761,0.00036700492,0.00048765782],"domain_scores_gemma":[0.9982745,0.00017156724,0.00024368984,0.00015966337,0.000121324294,0.0010292735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010780259,0.00013918312,0.00020506297,0.00020409352,0.0007225688,0.00028724252,0.00090140855,0.00007994412,0.00027015852],"category_scores_gemma":[0.00025311092,0.00008330747,0.0001181197,0.00052964484,0.0013381295,0.0005296058,0.0000012914469,0.0002885259,0.00003995695],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011559264,0.000001939524,0.98658067,5.2376316e-7,0.000016123202,0.00010501921,0.0023396965,0.00008937669,9.46247e-7,0.00026393286,0.0007368926,0.009853324],"study_design_scores_gemma":[0.00018521078,0.0002646546,0.9870815,0.000031184187,0.000013387584,0.0002006353,0.0018784215,0.00012412622,0.000007722771,0.0064931046,0.0036023436,0.00011769208],"about_ca_topic_score_codex":0.10647996,"about_ca_topic_score_gemma":0.6765446,"teacher_disagreement_score":0.57006466,"about_ca_system_score_codex":0.0000010877582,"about_ca_system_score_gemma":0.0018249359,"threshold_uncertainty_score":0.8994701},"labels":[],"label_agreement":null},{"id":"W1931619923","doi":"10.1139/cjes-2014-0011","title":"The Cambrian Basal Sandstone Unit in central Alberta — an investigation of temperature distribution, petrography, and hydraulic and geomechanical properties of a deep saline aquifer","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geothermal Energy Systems and Applications","field":"Energy","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Alberta Energy; University of Alberta","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ","keywords":"Geology; Petrography; Geothermal gradient; Permeability (electromagnetism); Sedimentary rock; Aquifer; Porosity; Geochemistry; Karst; Petrology; Geomorphology; Geotechnical engineering; Groundwater","score_opus":0.011088300542865887,"score_gpt":0.19738084634089054,"score_spread":0.18629254579802465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1931619923","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99830735,0.00051721884,0.000015409405,0.0010080216,0.000052031228,0.0000433767,0.000005012587,9.2288866e-7,0.000050674153],"genre_scores_gemma":[0.9997972,0.000019059602,0.00004914712,0.00005161851,0.00004980815,0.0000015423315,0.0000026376301,0.0000030878919,0.00002589536],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99920696,0.00009765169,0.00029548057,0.000092036054,0.00012387865,0.00018399737],"domain_scores_gemma":[0.99933964,0.000038859034,0.00015708889,0.00008045948,0.000101939266,0.000282018],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00050845294,0.00006584167,0.00013902679,0.00008346114,0.00018915096,0.000057556612,0.00014345143,0.000043084205,0.000005907328],"category_scores_gemma":[0.00008916969,0.00004126162,0.000023418836,0.00032467407,0.00062040094,0.00015225557,0.000006649959,0.00008281216,9.35213e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031629246,0.00002405026,0.85887253,0.000039056355,0.00003127811,0.0000023539087,0.0019481032,0.0055960515,0.029625848,0.10166292,0.000017385724,0.0021487956],"study_design_scores_gemma":[0.00038927887,0.00031671027,0.9844591,0.00012751196,0.000013675605,0.000045559063,0.0010612569,0.006355659,0.0037637823,0.0011683054,0.0021911382,0.00010801668],"about_ca_topic_score_codex":0.11835473,"about_ca_topic_score_gemma":0.78424966,"teacher_disagreement_score":0.6658949,"about_ca_system_score_codex":0.000002528042,"about_ca_system_score_gemma":0.00022873696,"threshold_uncertainty_score":0.8875162},"labels":[],"label_agreement":null},{"id":"W1931809205","doi":"10.1139/cjes-2012-0145","title":"Geochemical and isotopic (Nd–Sr–Hf–Pb) evidence for a lithospheric mantle source in the formation of the alkaline Monteregian Province (Quebec)","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Geochemistry; Mantle (geology); Mantle plume; Basalt; Fractional crystallization (geology); Lithosphere; Igneous rock; Olivine; Archean; Incompatible element; Carbonatite; Partial melting; Paleontology; Tectonics","score_opus":0.02498120799697498,"score_gpt":0.2076224933287321,"score_spread":0.1826412853317571,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1931809205","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99096507,0.0016087433,0.00014458927,0.006840624,0.00004794092,0.00017715481,0.000005367892,0.0000010221282,0.00020951191],"genre_scores_gemma":[0.99864876,0.000028214901,0.0006503888,0.00047415853,0.000041719053,0.0000012260326,0.0000011086004,5.575093e-7,0.00015389017],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990921,0.00006873104,0.0002828336,0.00010968459,0.00020057964,0.00024604256],"domain_scores_gemma":[0.99920195,0.00027994387,0.00018818742,0.00008866523,0.00008514648,0.00015612965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005575615,0.00007273578,0.00014139876,0.00005463048,0.00017532245,0.0001033261,0.00051190756,0.000035775392,0.00050290435],"category_scores_gemma":[0.00037868271,0.00003368338,0.00007588098,0.00036955194,0.00047286725,0.00041511434,0.000008084047,0.00011978313,0.000005950832],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012120696,0.000009897416,0.97898585,0.000039694864,0.000007189707,0.0000044309936,0.0008681587,0.0010686605,0.0006480612,0.00008485049,0.0006099911,0.017661087],"study_design_scores_gemma":[0.0001679719,0.00024914066,0.97146016,0.0001395241,0.000021058431,0.000064120875,0.0012747082,0.016461497,0.0009989179,0.0059060855,0.0031499302,0.00010690579],"about_ca_topic_score_codex":0.08757237,"about_ca_topic_score_gemma":0.6853067,"teacher_disagreement_score":0.5977344,"about_ca_system_score_codex":0.0000017969058,"about_ca_system_score_gemma":0.00021440958,"threshold_uncertainty_score":0.9185036},"labels":[],"label_agreement":null},{"id":"W1933340339","doi":"10.1139/e2012-043","title":"Physical and temporal factors controlling the development of near-surface ground ice at Illisarvik, western Arctic coast, Canada","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Permafrost; Tundra; Geology; Hydrology (agriculture); Aggradation; Thermokarst; Arctic; Soil water; Physical geography; Geomorphology; Structural basin; Oceanography; Soil science; Geography","score_opus":0.05251806904385937,"score_gpt":0.23296060265930035,"score_spread":0.180442533615441,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1933340339","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972971,0.0015089841,0.0000024237474,0.00032317155,0.00048784926,0.000057079378,0.00017191585,8.955975e-7,0.00015054792],"genre_scores_gemma":[0.99954253,0.000010346497,0.00009410969,0.00016409428,0.00012664465,5.7418283e-8,0.0000121195235,0.0000018798434,0.000048190264],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99878585,0.000056918525,0.0002656498,0.00009316174,0.00036988818,0.00042854296],"domain_scores_gemma":[0.99878436,0.000278165,0.00021502213,0.000062535975,0.000067451,0.0005924741],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000695185,0.0001090742,0.00020082544,0.000032387987,0.00070944545,0.00012440879,0.0002690632,0.00002323271,0.00038246013],"category_scores_gemma":[0.000040772367,0.00006453959,0.00003493896,0.00018389012,0.0004461001,0.00034902678,0.000009200789,0.00011708535,0.000004813318],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000050663366,0.0000021783926,0.9940828,0.0000078354415,0.000009646853,0.00000413829,0.0052032648,0.00034847148,0.000043976263,0.0000018231041,0.00003614532,0.0002546445],"study_design_scores_gemma":[0.00011894645,0.0000576254,0.9874329,0.000030695966,0.0000118174175,0.000046993486,0.0028562234,0.00046622206,0.00013045808,0.0000071078252,0.008747081,0.000093904855],"about_ca_topic_score_codex":0.8103258,"about_ca_topic_score_gemma":0.9990943,"teacher_disagreement_score":0.18876849,"about_ca_system_score_codex":0.000008325051,"about_ca_system_score_gemma":0.0017127112,"threshold_uncertainty_score":0.54565525},"labels":[],"label_agreement":null},{"id":"W1938190950","doi":"10.1139/cjes-2013-0124","title":"Constraints on the relationships between Paleoproterozoic intrusions and dyke swarms, East Arm of Great Slave Lake, N.W.T., Canada","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Avalon Rare Metals","keywords":"Geology; Geochemistry; Paleontology; Mining engineering","score_opus":0.03396136217836985,"score_gpt":0.18635964656562934,"score_spread":0.1523982843872595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1938190950","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98643464,0.00013673761,0.000019723595,0.0051793978,0.00009391672,0.000049787985,0.00009169996,0.000001301787,0.007992804],"genre_scores_gemma":[0.99938,0.000007473615,0.0001934172,0.00029004182,0.000077772296,1.2612928e-7,0.000004585198,6.712626e-7,0.000045946465],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885327,0.00015411497,0.00029051935,0.00013268976,0.00030179686,0.0002676328],"domain_scores_gemma":[0.99846745,0.00060197356,0.00019545449,0.00008683632,0.00008953812,0.0005587572],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009748376,0.0000920955,0.00019780644,0.000119901786,0.0005067612,0.00005429642,0.00031610942,0.000040517127,0.0046197097],"category_scores_gemma":[0.0007610537,0.00004920019,0.000050209317,0.00037942413,0.0010800044,0.00008239172,0.000005754896,0.0002621809,0.000008891354],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000019064449,0.0000013399605,0.9926249,0.0000021516562,0.000011764659,0.0000065418385,0.00006784211,0.00044771648,0.0000031409188,0.00040182873,0.00009645891,0.006334413],"study_design_scores_gemma":[0.000074783005,0.00019650564,0.9901023,0.000036039066,0.00002119472,0.000024965255,0.00032226718,0.00043077327,0.0000633327,0.006156202,0.0024951221,0.0000765258],"about_ca_topic_score_codex":0.32668245,"about_ca_topic_score_gemma":0.9952614,"teacher_disagreement_score":0.6685789,"about_ca_system_score_codex":0.0000012191554,"about_ca_system_score_gemma":0.0006566986,"threshold_uncertainty_score":0.9962902},"labels":[],"label_agreement":null},{"id":"W1939313350","doi":"10.1139/cjes-2014-0192","title":"Implementation of a rigorous least-squares modification of Stokes’ formula to compute a gravimetric geoid model over Saudi Arabia (SAGEO13)","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Plan for Science, Technology and Innovation; King Abdulaziz City for Science and Technology","keywords":"Geoid; Undulation of the geoid; Geodesy; Geopotential; Levelling; Elevation (ballistics); Least-squares function approximation; Geology; Global Positioning System; Gravimetric analysis; Mathematics; Geophysics; Geometry; Computer science; Statistics","score_opus":0.07251172866970294,"score_gpt":0.28092752698513307,"score_spread":0.2084157983154301,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1939313350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964253,0.00034016342,0.0021807845,0.00015761974,0.00023904201,0.00014789555,0.00011678253,0.0000016712937,0.00039078252],"genre_scores_gemma":[0.9970222,0.0000053813324,0.002818696,0.00007513675,0.00003963083,2.4493852e-7,0.000007329689,0.0000018602457,0.000029491282],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983295,0.000054904292,0.00045118685,0.000145199,0.00070913846,0.0003100546],"domain_scores_gemma":[0.9983581,0.000031958363,0.0004318186,0.00011363118,0.00044551305,0.00061902317],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012097788,0.00010150071,0.00022532548,0.000651321,0.0001405976,0.00006867958,0.00038659712,0.000029410108,0.00009405139],"category_scores_gemma":[0.0000648235,0.000084386906,0.00007518462,0.00094420684,0.00014468348,0.00043548323,0.000005781941,0.000080783764,0.000009103323],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019128758,0.0000147659575,0.74856144,0.000015789807,0.000020460662,0.0000043123073,0.0014049589,0.22163995,0.0002636888,0.00022681609,0.00032011484,0.027508587],"study_design_scores_gemma":[0.00043396695,0.0007880504,0.9559446,0.000039109353,0.000022729533,0.0000110130695,0.00069324597,0.03764677,0.00068814866,0.0033059986,0.00030026748,0.0001261],"about_ca_topic_score_codex":0.08138537,"about_ca_topic_score_gemma":0.23011516,"teacher_disagreement_score":0.20738316,"about_ca_system_score_codex":0.0000056893373,"about_ca_system_score_gemma":0.0014472305,"threshold_uncertainty_score":0.9247318},"labels":[],"label_agreement":null},{"id":"W1941835490","doi":"10.1139/e11-051","title":"The Late Cretaceous paleomagnetic field in North America: a South American perspective","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Paleomagnetism; Cretaceous; Geology; Paleontology; North American Plate; Seismology; Plate tectonics; Tectonics","score_opus":0.0133515410703627,"score_gpt":0.2152763334354735,"score_spread":0.2019247923651108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1941835490","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9847812,0.006659706,0.000020126294,0.00059640635,0.00020160849,0.00007068979,0.000007888235,0.0000013313975,0.007661052],"genre_scores_gemma":[0.9982253,0.0004958813,0.00043772144,0.00031983727,0.00008080372,0.000002444211,4.370595e-7,0.0000045681336,0.00043304634],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989903,0.00007211283,0.0002398783,0.00015731773,0.00013118685,0.00040917788],"domain_scores_gemma":[0.99925715,0.00003428969,0.00019377514,0.0001412383,0.00012643615,0.00024710517],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002434382,0.000112997186,0.00014719443,0.00012706498,0.00032038198,0.000053000353,0.0004308293,0.000029105184,0.000046533078],"category_scores_gemma":[0.00027227247,0.0000783937,0.000073054565,0.00040575519,0.0010956007,0.000008523807,0.000025039015,0.00013169501,0.000007193823],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005315334,0.000013160847,0.98044556,0.0000026793089,0.00003436395,0.00013787636,0.00943989,0.00009279243,0.0003254687,0.00007041582,0.00035307807,0.009031545],"study_design_scores_gemma":[0.00023272651,0.0038259875,0.9657927,0.000011960375,0.000015404243,0.00006747267,0.014280514,0.000015377786,0.00033196656,0.00016122122,0.015077866,0.00018681424],"about_ca_topic_score_codex":0.0071243085,"about_ca_topic_score_gemma":0.5600087,"teacher_disagreement_score":0.5528844,"about_ca_system_score_codex":0.0000025995691,"about_ca_system_score_gemma":0.00056382414,"threshold_uncertainty_score":0.99948734},"labels":[],"label_agreement":null},{"id":"W1943041151","doi":"10.1139/cjes-2013-0142","title":"Deep seismic reflection constraints on Paleogene crustal extension in the south-central Intermontane belt, British Columbia","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Terrane; Crust; Seismology; Subduction; Oceanic crust; Paleontology; Mantle (geology); Lithosphere; Metamorphic core complex; Geochemistry; Extensional definition; Tectonics","score_opus":0.014833066126084102,"score_gpt":0.19192635536663954,"score_spread":0.17709328924055545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1943041151","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99395096,0.00027352877,0.000057613855,0.0006153641,0.00026056616,0.000051592346,0.000009632316,0.000002588774,0.0047781346],"genre_scores_gemma":[0.99863243,0.000013942797,0.0001336011,0.0010565663,0.000121551864,1.5674102e-7,0.00000541823,8.0951827e-7,0.00003554376],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998607,0.00017855229,0.00028344808,0.0001883708,0.00030345778,0.00043917712],"domain_scores_gemma":[0.99921525,0.0001366884,0.00013401755,0.00007404947,0.000060194863,0.00037983223],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010135977,0.000076954944,0.00018225229,0.00010717376,0.00036970957,0.00037920295,0.0003736467,0.000051745348,0.005282044],"category_scores_gemma":[0.00031776546,0.000059518978,0.00009655296,0.0004701277,0.00066681835,0.00013625028,0.0000033093331,0.00025106626,0.000021607544],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000100907555,0.0000064080946,0.93349767,0.0000019163117,0.000005475012,0.0001876186,0.00017928047,0.006203011,0.000023312334,0.0000041073276,0.00010261769,0.059778504],"study_design_scores_gemma":[0.00017223501,0.0006530777,0.98604727,0.000040413168,0.00001196108,0.0004761435,0.00039131512,0.010278745,0.000016258504,0.0012392317,0.0005808244,0.00009254856],"about_ca_topic_score_codex":0.11744718,"about_ca_topic_score_gemma":0.9717905,"teacher_disagreement_score":0.8543433,"about_ca_system_score_codex":0.0000023644454,"about_ca_system_score_gemma":0.00016388862,"threshold_uncertainty_score":0.9956273},"labels":[],"label_agreement":null},{"id":"W1944709855","doi":"10.1139/e09-070","title":"The Grenville Orogen explained? Applications and limitations of integrating numerical models with geological and geophysical dataThis article is one of a series of papers published in this Special Issue on the theme <i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Convergence (economics); Series (stratigraphy); Crust; Tectonics; Shear zone; Scale (ratio); Geophysics; Consistency (knowledge bases); Plate tectonics; Seismology; Paleontology; Geometry; Geography","score_opus":0.017638753709008567,"score_gpt":0.18071948081211628,"score_spread":0.16308072710310773,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1944709855","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99093413,0.0004977718,0.00003457402,0.007030589,0.00001161778,0.00013019105,0.000030173867,5.992342e-7,0.0013303414],"genre_scores_gemma":[0.99841875,0.00011854551,0.0013529018,0.00006308695,0.00003329609,0.0000021464941,0.0000011108638,6.1359555e-7,0.000009567818],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991304,0.000077436765,0.00031606742,0.0001211821,0.00021361523,0.00014126263],"domain_scores_gemma":[0.99823445,0.0011289071,0.0002777916,0.00008977166,0.0001622071,0.00010686756],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00075207476,0.00006798353,0.00021798864,0.000057095705,0.00019870354,0.000043585333,0.00022767627,0.000029213268,0.00029347502],"category_scores_gemma":[0.0007419054,0.000026924385,0.00003052021,0.00055146427,0.0028466424,0.00017878068,0.000013194949,0.00016529656,1.7428505e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005232107,0.00011995227,0.9079567,0.00006192166,0.00012764781,0.0000033701283,0.0072183423,0.001594473,0.0019615758,0.06348523,0.00009197522,0.01685561],"study_design_scores_gemma":[0.0017226489,0.0028694437,0.7390819,0.00021942414,0.00025079792,0.000115675815,0.030518508,0.037330475,0.0066312873,0.17839995,0.002490921,0.00036897097],"about_ca_topic_score_codex":0.011160974,"about_ca_topic_score_gemma":0.154186,"teacher_disagreement_score":0.1688748,"about_ca_system_score_codex":6.851142e-7,"about_ca_system_score_gemma":0.00018541307,"threshold_uncertainty_score":0.999867},"labels":[],"label_agreement":null},{"id":"W1946695498","doi":"10.1139/e08-033","title":"Early Devonian putative gyracanthid acanthodians from eastern CanadaInternational Geoscience Programme (IGCP) Contribution 491, Middle Palaeozoic Vertebrate Biogeography, Palaeogeography, and Climate.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Devonian; Paleontology; Paleozoic; Geology; Laurentia; Genus; Carboniferous; Biogeography; Palaeogeography; Tectonics; Biology; Zoology; Structural basin","score_opus":0.024782378183075965,"score_gpt":0.21053779075293833,"score_spread":0.18575541256986236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1946695498","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99206424,0.004071736,0.00014787943,0.0009760837,0.0009420635,0.00014295075,0.0008919759,0.000012285712,0.0007508011],"genre_scores_gemma":[0.9977479,0.00035810456,0.0013353059,0.00033036305,0.00014068218,0.0000011653406,0.00006456082,0.0000025468871,0.000019391624],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99745363,0.0002333103,0.00047641323,0.0004062339,0.0004073375,0.0010230483],"domain_scores_gemma":[0.9978851,0.00026369395,0.00035882444,0.00010288847,0.00027902774,0.0011104392],"candidate_categories":["sts"],"consensus_categories":["sts"],"category_scores_codex":[0.0009273058,0.0002209462,0.00031978966,0.00068158,0.0015141927,0.00012904745,0.000566313,0.00014589798,0.00052704476],"category_scores_gemma":[0.00020781538,0.00017976473,0.00011871223,0.0007947483,0.0037535536,0.00076570286,0.000011767334,0.00030058803,0.00003533681],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028402837,0.000008026206,0.9967268,0.0000021916262,0.000034772504,0.00027785826,0.00043306846,0.00007050724,0.000013888585,0.00018674943,0.000021893344,0.0021958507],"study_design_scores_gemma":[0.0003998553,0.00053393794,0.9927325,0.00004247886,0.000018931876,0.0005923963,0.00038140026,0.0025441383,0.000019755096,0.000939819,0.0015760633,0.00021870223],"about_ca_topic_score_codex":0.21718493,"about_ca_topic_score_gemma":0.8460474,"teacher_disagreement_score":0.6288625,"about_ca_system_score_codex":0.000006713463,"about_ca_system_score_gemma":0.0018418333,"threshold_uncertainty_score":0.9997857},"labels":[],"label_agreement":null},{"id":"W1950147882","doi":"10.1139/cjes-2015-0055","title":"Oil–source rock correlation for tight oil in tuffaceous reservoirs in the Permian Tiaohu Formation, Santanghu Basin, northwest China","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Source rock; Kerogen; Sterane; Phytane; Organic matter; Hopanoids; Geochemistry; Total organic carbon; Sedimentary rock; Maceral; Mineralogy; Petrography; Environmental chemistry; Structural basin; Paleontology; Chemistry","score_opus":0.020765533384016883,"score_gpt":0.22450547240699228,"score_spread":0.2037399390229754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1950147882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987276,0.00088883156,0.002399451,0.0030572393,0.0003607597,0.000047406713,0.0000101668775,0.000009706037,0.0059504393],"genre_scores_gemma":[0.99923265,0.00006140337,0.0002069876,0.000112756505,0.00008887522,0.0000038749263,0.0000069493763,0.0000067996707,0.00027967946],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988506,0.00007487269,0.0003973987,0.00008705246,0.00030403925,0.0002860811],"domain_scores_gemma":[0.9993508,0.000053980642,0.000096449665,0.000102494654,0.00010601721,0.00029029683],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012049538,0.00009591197,0.00016414859,0.0006545817,0.00016490053,0.00015684594,0.00037330182,0.00005391657,0.000025829095],"category_scores_gemma":[0.00021020115,0.000068293324,0.00006376505,0.001012256,0.00006330937,0.0007105502,0.0000042399047,0.00019773454,0.0000099449035],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000043241976,0.0000051163383,0.02402267,0.000012129702,0.0000051239576,0.000021834489,0.0077221566,0.96603185,0.0000087950075,0.000039656374,0.00078030105,0.0013460398],"study_design_scores_gemma":[0.00065268687,0.00013050612,0.02648294,0.000116031835,0.000015826998,0.00011959675,0.008107474,0.9036004,0.000051891067,0.00015261851,0.060366955,0.00020309795],"about_ca_topic_score_codex":0.003644162,"about_ca_topic_score_gemma":0.59866524,"teacher_disagreement_score":0.59502107,"about_ca_system_score_codex":0.00004443443,"about_ca_system_score_gemma":0.00050475146,"threshold_uncertainty_score":0.55089074},"labels":[],"label_agreement":null},{"id":"W1952619490","doi":"10.1139/e10-036","title":"The Lithoprobe trans-continental lithospheric cross sections: imaging the internal structure of the North American continentThis article is one of a series of papers published in this Special Issue on the theme<i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.Lithoprobe Publication 1487.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Shell (Canada); University of Calgary; University of British Columbia","funders":"","keywords":"Geology; Subduction; Craton; Rift; Basement; Tectonics; Lithosphere; Continental margin; Paleontology; Foreland basin; Seismology; Earth science; Geography; Archaeology","score_opus":0.004872977587805065,"score_gpt":0.1812059062401928,"score_spread":0.17633292865238775,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1952619490","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97785294,0.00061936333,0.0000073363726,0.019922094,0.00020780727,0.00028398313,0.00008407349,0.0000019835663,0.0010204243],"genre_scores_gemma":[0.99923587,0.00006566078,0.0002008551,0.00027201345,0.00014139534,0.000002154099,0.0000016879134,0.0000022267577,0.00007812083],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99791443,0.00024819162,0.0007675594,0.00021094084,0.00053917064,0.00031970523],"domain_scores_gemma":[0.99741334,0.0005787194,0.0010625594,0.00026276844,0.00055698014,0.00012560775],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016680607,0.00015049576,0.00034686772,0.000090966525,0.00046892048,0.00022015387,0.0009852975,0.000038211365,0.0016556289],"category_scores_gemma":[0.0016096691,0.000056469675,0.00017224105,0.001797439,0.0055830237,0.00038568454,0.000025291274,0.00046208422,4.183628e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015384569,0.00002170265,0.9931116,0.000019267847,0.00004454247,5.133792e-7,0.0021997185,0.00020227843,0.00077952817,0.00047502067,0.00007764149,0.0029143314],"study_design_scores_gemma":[0.00040025797,0.0001880586,0.9837383,0.00006089916,0.00005682039,0.000033488166,0.0031935635,0.00090518396,0.0066320333,0.0029466508,0.0017544812,0.00009025141],"about_ca_topic_score_codex":0.058391605,"about_ca_topic_score_gemma":0.52010125,"teacher_disagreement_score":0.46170965,"about_ca_system_score_codex":0.00000437593,"about_ca_system_score_gemma":0.00043135826,"threshold_uncertainty_score":0.99925697},"labels":[],"label_agreement":null},{"id":"W1953797851","doi":"10.1139/cjes-2015-0033","title":"Ice-proximal Labrador Sea Heinrich layers: a sedimentological approach","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Terrigenous sediment; Oceanography; Ice sheet; Sedimentary depositional environment; Sea ice; Foraminifera; Debris; Iceberg; Paleontology; Geomorphology; Geochemistry; Sediment","score_opus":0.06865843975314936,"score_gpt":0.26129766328541315,"score_spread":0.1926392235322638,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1953797851","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9516803,0.0028746258,0.000048459195,0.0018525092,0.0005765344,0.00008910608,0.000014303406,0.000007112398,0.042857043],"genre_scores_gemma":[0.99520946,0.000013309878,0.0039348206,0.0004218619,0.00015202505,3.413144e-7,0.0000059150434,0.0000014210442,0.00026083057],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980222,0.00028069434,0.00029402215,0.00022560376,0.0004408181,0.0007366509],"domain_scores_gemma":[0.99794483,0.00015866573,0.00013973574,0.00010945116,0.00019757444,0.0014497198],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0024671417,0.00012538423,0.00025947735,0.00039202243,0.00040703287,0.00013413795,0.00071652746,0.00013610354,0.0012879531],"category_scores_gemma":[0.00038452077,0.00008645943,0.000072065806,0.0006634234,0.001298252,0.00042770556,0.000008870288,0.00040616692,0.00024325395],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021051965,0.000007739753,0.99708444,0.0000039894217,0.000013519315,0.0002581038,0.0003215216,0.0010349415,6.227011e-7,0.00023725045,0.00065885985,0.00035797968],"study_design_scores_gemma":[0.0005346433,0.0011076162,0.979713,0.000013985198,0.000015497655,0.0023732663,0.0019968534,0.004142556,0.000023956994,0.0014348271,0.008450661,0.0001931356],"about_ca_topic_score_codex":0.0058842036,"about_ca_topic_score_gemma":0.18664618,"teacher_disagreement_score":0.18076198,"about_ca_system_score_codex":8.5016086e-7,"about_ca_system_score_gemma":0.002765453,"threshold_uncertainty_score":0.999625},"labels":[],"label_agreement":null},{"id":"W1955727102","doi":"10.1139/cjes-2014-0165","title":"Fishes from the Lower Triassic portion of the Sulphur Mountain Formation in Alberta, Canada: geological context and taxonomic composition","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Geology; Fauna; Paleontology; Context (archaeology); Shore; Craton; Oceanography; Ecology; Tectonics","score_opus":0.02728560486395432,"score_gpt":0.1918314827881794,"score_spread":0.1645458779242251,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1955727102","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918644,0.0010628757,0.000008623397,0.0058698854,0.0004709068,0.000061662264,0.000034062454,3.9383426e-7,0.00062718487],"genre_scores_gemma":[0.99941534,0.000011754077,0.000036045592,0.00047375957,0.000043873206,1.6479429e-7,0.0000061639416,2.7486152e-7,0.000012639184],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992334,0.00018969076,0.0002461973,0.0000692979,0.0001055945,0.0001558159],"domain_scores_gemma":[0.99929786,0.00026709447,0.00020565474,0.00004670407,0.000046442332,0.00013623569],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006349299,0.000049897786,0.0001139034,0.00004786101,0.00018140831,0.000017257002,0.00021656955,0.00004577484,0.00011993864],"category_scores_gemma":[0.00016959962,0.000026075373,0.000021126405,0.00013019006,0.000579832,0.0002483258,0.0000033603042,0.000111380534,0.0000019698882],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027012731,0.0000018150498,0.99693716,4.299723e-7,0.000003023067,0.000006881104,0.00015738294,0.0012903201,0.0000037640607,0.000105994804,0.00056575617,0.0009004849],"study_design_scores_gemma":[0.00019967093,0.00012002701,0.9943345,0.0000141735445,0.0000049077034,0.00010391571,0.00075915374,0.0020384402,0.0000149539765,0.0007299514,0.0016450529,0.000035245885],"about_ca_topic_score_codex":0.9336865,"about_ca_topic_score_gemma":0.99970853,"teacher_disagreement_score":0.06602204,"about_ca_system_score_codex":0.00000734348,"about_ca_system_score_gemma":0.0013476558,"threshold_uncertainty_score":0.23906834},"labels":[],"label_agreement":null},{"id":"W1960192646","doi":"10.1139/cjes-2014-0173","title":"The significance of the theropod collections of the Royal Tyrrell Museum of Palaeontology to our understanding of Late Cretaceous theropod diversity","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"University of Cambridge","keywords":"Cretaceous; Paleontology; Taxon; Theropoda; Geology; Archaeology; Geography","score_opus":0.053624773787742754,"score_gpt":0.22328691781774085,"score_spread":0.1696621440299981,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1960192646","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98793745,0.0013544557,0.00007052594,0.0035428377,0.0012728533,0.00013731365,0.000079172474,0.0000010906433,0.0056043155],"genre_scores_gemma":[0.9995553,0.000021851281,0.00008153126,0.000054999833,0.000025988027,1.1762896e-7,1.8884799e-7,8.257671e-7,0.00025923114],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99869657,0.00035801445,0.00033122054,0.000103427534,0.00025020845,0.0002605443],"domain_scores_gemma":[0.9987079,0.00025574333,0.00050415564,0.00015937316,0.00019071314,0.00018213369],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011723493,0.00007636475,0.00021694471,0.00011772303,0.000853934,0.000009296022,0.0009199552,0.00006800186,0.000066165405],"category_scores_gemma":[0.00032017182,0.00003714867,0.00010810276,0.00066050875,0.0018922613,0.00006738417,0.000027050552,0.00015658606,0.0000012702843],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048622234,0.0000063458783,0.98289233,0.0000036509123,0.00003540026,0.000002026177,0.0012924635,0.014689595,0.000047019294,0.00036595826,0.0004951256,0.00012146444],"study_design_scores_gemma":[0.00020134417,0.0005737933,0.98655576,0.00003442806,0.0000325344,0.000035997415,0.0075140316,0.0007963728,0.0002468011,0.0028250623,0.001122429,0.00006144377],"about_ca_topic_score_codex":0.021036882,"about_ca_topic_score_gemma":0.6951352,"teacher_disagreement_score":0.6740983,"about_ca_system_score_codex":0.000007825219,"about_ca_system_score_gemma":0.0015830164,"threshold_uncertainty_score":0.9854821},"labels":[],"label_agreement":null},{"id":"W1963974910","doi":"10.1139/e99-080","title":"Crustal models of the eastern Superior Province, Quebec, derived from new gravity data","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Bouguer anomaly; Mafic; Gravity anomaly; Crust; Greenstone belt; Geochemistry; Seismology; Geophysics; Archean; Paleontology","score_opus":0.03458785359232985,"score_gpt":0.19818788544971216,"score_spread":0.1636000318573823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1963974910","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943962,0.0010732135,0.000025158633,0.0014566735,0.00012500833,0.00004595552,0.00024820032,0.000001908501,0.0026276635],"genre_scores_gemma":[0.9976911,0.000022515504,0.0006660678,0.0002645937,0.00010185805,2.5418702e-8,0.000011580955,7.8425757e-7,0.001241469],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875104,0.00007109978,0.00031132097,0.00020513101,0.0003578103,0.0003036199],"domain_scores_gemma":[0.99890816,0.00007576448,0.00014064177,0.00024320505,0.000055326695,0.00057690137],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031306024,0.000097265875,0.0002154404,0.00006984142,0.00022629782,0.000112056616,0.0014878818,0.00004394051,0.016995473],"category_scores_gemma":[0.00008145178,0.000052308456,0.00010329419,0.00037096118,0.0006959129,0.00057554385,0.000018635576,0.00015720307,0.00004581005],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013415111,0.0000055828755,0.97300535,0.0000018257873,0.000019629464,0.000019577745,0.00013850928,0.008823348,0.00010010787,0.000012736289,0.00022865027,0.017631268],"study_design_scores_gemma":[0.00017919704,0.000098516466,0.9520099,0.000036961286,0.000045978053,0.000022217628,0.0002000004,0.03240097,0.00036459844,0.01112043,0.0033791326,0.00014206405],"about_ca_topic_score_codex":0.7437816,"about_ca_topic_score_gemma":0.9816161,"teacher_disagreement_score":0.23783445,"about_ca_system_score_codex":0.0000010414261,"about_ca_system_score_gemma":0.0018153375,"threshold_uncertainty_score":0.9839031},"labels":[],"label_agreement":null},{"id":"W1964143800","doi":"10.1139/e03-078","title":"Hot spring and geyser sinters: the integrated product of precipitation, replacement, and deposition","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Mineralogy and Gemology Studies","field":"Earth and Planetary Sciences","cited_by":118,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Hot spring; Calcite; Deposition (geology); Cementation (geology); Geochemistry; Detritus; Precipitation; Spring (device); Mineralogy; Cement; Geomorphology; Paleontology; Materials science; Metallurgy; Structural basin","score_opus":0.019698834692604028,"score_gpt":0.21531188440886742,"score_spread":0.1956130497162634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964143800","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99381316,0.003611291,0.000044706645,0.0007675802,0.00020985605,0.000048859194,0.000003287673,7.825477e-7,0.0015004806],"genre_scores_gemma":[0.99876153,0.00007571657,0.00094358064,0.00012425256,0.000017408269,9.6552775e-8,3.4946646e-7,4.789132e-7,0.00007655968],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994566,0.000095435,0.00015672749,0.000089395595,0.00007155681,0.00013031503],"domain_scores_gemma":[0.9995742,0.00009494165,0.00011428526,0.000039983137,0.000078176556,0.00009842979],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008460945,0.000049309798,0.00008644342,0.000108930755,0.0003048325,0.000039996663,0.00007709725,0.000015596885,0.000122009624],"category_scores_gemma":[0.00027313587,0.000028750252,0.000013051934,0.00015828607,0.0007145157,0.00019715024,0.0000016695964,0.00007550442,0.000001036799],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000085743795,0.0000010496506,0.9973634,0.0000036288418,0.000013960712,0.0000044101075,0.0007560497,0.0001270188,0.0000633925,0.00019476253,0.00009958156,0.0013641908],"study_design_scores_gemma":[0.00009778522,0.00026634804,0.99581844,0.000028981958,0.0000128125575,0.00016480658,0.0011278639,0.000120072,0.0004191266,0.00036964886,0.0015318055,0.000042297455],"about_ca_topic_score_codex":0.0066689057,"about_ca_topic_score_gemma":0.2600278,"teacher_disagreement_score":0.2533589,"about_ca_system_score_codex":5.350123e-7,"about_ca_system_score_gemma":0.00022568554,"threshold_uncertainty_score":0.99994576},"labels":[],"label_agreement":null},{"id":"W1964161522","doi":"10.1139/e01-042","title":"New information on<i>Shanshanosaurus huoyanshanensis</i>, a juvenile tyrannosaurid (Theropoda, Dinosauria) from the Late Cretaceous of China","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Northwestern University","keywords":"Theropoda; Paleontology; Cretaceous; Geology; Juvenile; Subfamily; China; Geography; Biology; Archaeology; Ecology","score_opus":0.014251224407420247,"score_gpt":0.20082382678661514,"score_spread":0.1865726023791949,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964161522","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.982416,0.0029153195,0.000107576874,0.0040864605,0.0010936426,0.00008764853,0.00017065513,0.0000056137405,0.009117104],"genre_scores_gemma":[0.99810684,0.00014454193,0.00042280307,0.0008954578,0.00024517823,1.4548424e-7,0.00002449209,0.0000013100525,0.00015925938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985898,0.0001483183,0.00045222536,0.0001166503,0.0002837865,0.0004092006],"domain_scores_gemma":[0.99871176,0.0002676454,0.0003790464,0.0001493733,0.000085584245,0.0004066151],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00062366144,0.00013480222,0.00025079094,0.00023109702,0.00047544087,0.000063736006,0.0006759721,0.00010439094,0.0033780222],"category_scores_gemma":[0.00019998531,0.00008539087,0.000107073065,0.00047810946,0.0005937944,0.00061005494,0.000004685863,0.0002541266,0.00015513586],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000098065546,0.000005126333,0.96383727,0.0000023348982,0.00003924532,0.00006442276,0.0012837896,0.006744527,0.000038994564,0.00016255578,0.0022176798,0.025505964],"study_design_scores_gemma":[0.0002623133,0.0005024407,0.9605262,0.000038609094,0.000019680207,0.00019662893,0.00030284032,0.0005902294,0.000051466457,0.0014407198,0.035958983,0.00010987051],"about_ca_topic_score_codex":0.045392964,"about_ca_topic_score_gemma":0.45747483,"teacher_disagreement_score":0.41208184,"about_ca_system_score_codex":0.000002600409,"about_ca_system_score_gemma":0.0012002215,"threshold_uncertainty_score":0.997533},"labels":[],"label_agreement":null},{"id":"W1964426952","doi":"10.1139/e00-055","title":"Conodonts and corals in kimberlite xenoliths confirm a Devonian seaway in central Ontario and Quebec","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Conodont; Geology; Devonian; Paleontology; Ordovician; Outcrop; Late Devonian extinction; Paleozoic; Ladinian; Biozone; Sedimentary rock; Pennsylvanian; Biostratigraphy; Structural basin; Carboniferous","score_opus":0.01625832075561134,"score_gpt":0.20546827413421853,"score_spread":0.1892099533786072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964426952","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9543021,0.0062621515,3.1331328e-7,0.00047244085,0.0001135202,0.000064291,0.000013288066,0.0000011990562,0.03877075],"genre_scores_gemma":[0.9993088,0.00011773038,0.00020679215,0.0001467166,0.000019258712,1.0389964e-7,5.4638326e-7,3.7888873e-7,0.00019964398],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988443,0.00008203484,0.00029353457,0.00016738889,0.00012445514,0.00048824798],"domain_scores_gemma":[0.9991725,0.00007989666,0.000076894896,0.000046188994,0.00002111873,0.00060341804],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00058022357,0.00010038706,0.00022078634,0.00031941684,0.00017475957,0.00014893232,0.00016632529,0.00006948537,0.0016338422],"category_scores_gemma":[0.000026734599,0.000082747276,0.000023382005,0.0002653892,0.0008559222,0.0004908102,4.823888e-7,0.00022473061,0.000002549218],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015396146,0.0000023256944,0.9375036,0.0000019994284,0.0000033671836,0.00022695579,0.0017081356,0.00005650738,0.0000011196944,0.000068663554,0.000009251789,0.060402684],"study_design_scores_gemma":[0.00036372137,0.00016282237,0.994375,0.000052175455,0.0000029293847,0.00025527977,0.00028529603,0.00014561386,0.00000391437,0.0005272091,0.0037253578,0.00010069878],"about_ca_topic_score_codex":0.85118467,"about_ca_topic_score_gemma":0.99986583,"teacher_disagreement_score":0.14868116,"about_ca_system_score_codex":0.0000038932803,"about_ca_system_score_gemma":0.0020059142,"threshold_uncertainty_score":0.9992788},"labels":[],"label_agreement":null},{"id":"W1964607901","doi":"10.1139/e2012-005","title":"Contemporaneous eruption of Nb-enriched basalts – K-adakites – Na-adakites from the 2.7 Ga Penakacherla terrane: implications for subduction zone processes and crustal growth in the eastern Dharwar craton, India","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Adakite; Basalt; Geology; Geochemistry; Mantle (geology); Andesites; Partial melting; Mantle wedge; Primitive mantle; Subduction; Craton; Oceanic crust; Andesite; Volcanic rock; Tectonics","score_opus":0.03194402144037632,"score_gpt":0.2241470880825198,"score_spread":0.19220306664214348,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964607901","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9906476,0.004791015,0.00010895276,0.0038289193,0.00008868341,0.00015592766,0.000099041594,0.0000022026497,0.00027763817],"genre_scores_gemma":[0.99907047,0.0000627571,0.00035081175,0.00032532887,0.00014874726,0.0000019282074,0.000023369039,0.0000013576571,0.000015211087],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988577,0.00011519285,0.00035103312,0.0001463386,0.00020940979,0.00032035858],"domain_scores_gemma":[0.99839807,0.0007819573,0.00029248314,0.00007961672,0.00020096419,0.00024693456],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010506617,0.00010945665,0.00020016437,0.00012657928,0.0003331762,0.0001190042,0.00039532813,0.00005242935,0.00034350215],"category_scores_gemma":[0.00058694114,0.000055501634,0.000065192355,0.00062010216,0.00055193907,0.00045235464,0.0000051585644,0.00014083114,0.0000037103216],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015828735,0.0000129210575,0.9970036,0.000011545439,0.000012193787,0.0000016066418,0.0012115362,0.000052730375,0.00020060729,0.00007150307,0.000047492642,0.0013584176],"study_design_scores_gemma":[0.00016251969,0.00017085194,0.9924499,0.00002240221,0.000037459748,0.00005719571,0.0024664365,0.0002431861,0.00018022196,0.003735068,0.0003879657,0.00008682511],"about_ca_topic_score_codex":0.036913224,"about_ca_topic_score_gemma":0.3084514,"teacher_disagreement_score":0.2715382,"about_ca_system_score_codex":0.0000016388726,"about_ca_system_score_gemma":0.00030115317,"threshold_uncertainty_score":0.96950006},"labels":[],"label_agreement":null},{"id":"W1964791102","doi":"10.1139/e07-050","title":"Rb–Sr and U–Pb geochronology and setting of the Buffalo Head Hills kimberlite field, northern AlbertaThis article is one of a selection of papers published in this Special Issue on the theme<i>Geology of northeastern British Columbia and northwestern Alberta: diamonds, shallow gas, gravel, and glaciers</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Stornoway Diamond (Canada); Alberta Energy; University of Alberta","funders":"","keywords":"Kimberlite; Geology; Phlogopite; Geochemistry; Isochron; Geochronology; Ultramafic rock; Magmatism; Diamond; Silicic; Chromite; Paleontology; Mantle (geology); Volcano","score_opus":0.007401996214850722,"score_gpt":0.16917126902115195,"score_spread":0.16176927280630124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964791102","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954377,0.00088397536,3.1989833e-7,0.0025155486,0.000054560187,0.000088853565,0.000024547478,5.84518e-7,0.0009939492],"genre_scores_gemma":[0.9992674,0.00024706539,0.000060683986,0.00025961123,0.000056574903,2.9184628e-7,0.0000013479364,0.0000013374387,0.00010567617],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875766,0.00012169664,0.00044575406,0.00020575243,0.00020801932,0.0002610994],"domain_scores_gemma":[0.9987643,0.00049574947,0.00035314294,0.00008361719,0.00012059869,0.00018264003],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00045983592,0.00009173812,0.00036444288,0.00008855357,0.00025874973,0.0000634255,0.00019389541,0.00007624604,0.0029808313],"category_scores_gemma":[0.0002979364,0.00006684787,0.000057233112,0.00042823024,0.0014616768,0.00015446257,0.000017810204,0.00017393369,3.726015e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017479102,0.000012948097,0.9909855,0.00001575177,0.000024958945,0.0000046938308,0.0017279685,0.000038455026,0.00018568759,0.0000041027224,0.000037480368,0.006944936],"study_design_scores_gemma":[0.00026237074,0.0005079036,0.9965076,0.00006694482,0.000024641808,0.00015010202,0.0005544357,0.00043813273,0.0005148589,0.0006126752,0.00028845522,0.00007187462],"about_ca_topic_score_codex":0.70309013,"about_ca_topic_score_gemma":0.9965852,"teacher_disagreement_score":0.29349503,"about_ca_system_score_codex":0.00000141181,"about_ca_system_score_gemma":0.00016176737,"threshold_uncertainty_score":0.9979306},"labels":[],"label_agreement":null},{"id":"W1965041490","doi":"10.1139/e05-043","title":"Accretion-related metamorphism of the Metchosin Igneous Complex, southern Vancouver Island, British Columbia","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Geology; Metamorphism; Geochemistry; Greenschist; Actinolite; Metamorphic facies; Metamorphic rock; Igneous rock; Epidote; Paleontology; Chlorite; Facies","score_opus":0.01237789379951182,"score_gpt":0.1739222252112303,"score_spread":0.16154433141171848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965041490","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9910405,0.00108812,0.0000067395267,0.00091091474,0.00027896484,0.000052008763,0.000120998695,0.000002833978,0.006498869],"genre_scores_gemma":[0.9970873,0.000014860223,0.00053292146,0.00040083076,0.000076897515,8.938386e-8,0.000002861396,0.0000011786553,0.0018830724],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986148,0.00009529493,0.00042670767,0.00015059322,0.00038125712,0.00033136675],"domain_scores_gemma":[0.99896526,0.00009909254,0.00030520465,0.000099053395,0.00014987655,0.00038148757],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00060444325,0.00007778078,0.0002527583,0.00007562551,0.0004307549,0.0001939595,0.00063934183,0.000056725206,0.04481288],"category_scores_gemma":[0.00017805176,0.00005922411,0.00021254308,0.00070345326,0.00085482345,0.00017588542,0.0000083517925,0.00018558864,0.000053172073],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000024686065,0.0000082973975,0.97677666,0.0000025254908,0.00004134514,0.000025808087,0.00016756808,0.0072692195,0.00007718997,0.000007386178,0.0056421976,0.009979322],"study_design_scores_gemma":[0.0002607536,0.0001703834,0.9624975,0.000045995945,0.000081516475,0.00020148301,0.0004530951,0.0034611982,0.00006575161,0.0068174354,0.025771001,0.00017393002],"about_ca_topic_score_codex":0.41875353,"about_ca_topic_score_gemma":0.9966017,"teacher_disagreement_score":0.57784814,"about_ca_system_score_codex":0.0000018216758,"about_ca_system_score_gemma":0.00038456396,"threshold_uncertainty_score":0.9560603},"labels":[],"label_agreement":null},{"id":"W1965241082","doi":"10.1139/e01-023","title":"Hidden Cretaceous basins in Nova Scotia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Cretaceous; Paleontology; Unconformity; Facies; Mesozoic; Graben; Cenomanian; Fluvial; Geochemistry; Structural basin; Geomorphology","score_opus":0.030910866443550556,"score_gpt":0.22407374531017982,"score_spread":0.19316287886662925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965241082","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9601377,0.001869101,0.000022099031,0.0013988275,0.00039878226,0.000034912493,0.000015408314,0.0000024432686,0.036120687],"genre_scores_gemma":[0.9983288,0.00005472631,0.0010595991,0.00034755556,0.00006964361,2.1076689e-8,0.0000015748597,6.619587e-7,0.00013742305],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990602,0.000036390982,0.00026504754,0.00009224249,0.00019496598,0.00035113585],"domain_scores_gemma":[0.9992912,0.00007568462,0.00010528423,0.000051565545,0.00007812108,0.0003981449],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006567376,0.00007006054,0.00012600535,0.0003918596,0.00017922334,0.0001575995,0.00036536867,0.000039181756,0.010330973],"category_scores_gemma":[0.00017001329,0.000048567552,0.000037432426,0.0008609335,0.00029250767,0.0005860587,0.0000021996075,0.0001394609,0.00023303654],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000028736704,0.0000019314539,0.98724264,0.0000019078018,0.0000014187669,0.00012095465,0.00012976803,0.002274849,9.039085e-7,0.0000643035,0.00010505942,0.010053401],"study_design_scores_gemma":[0.000097111995,0.00021191593,0.9689565,0.00002687968,0.0000024365518,0.00045226727,0.00034579722,0.00066016096,0.00001063347,0.0014352791,0.027721502,0.000079530735],"about_ca_topic_score_codex":0.029257324,"about_ca_topic_score_gemma":0.9399811,"teacher_disagreement_score":0.9107238,"about_ca_system_score_codex":0.0000011495164,"about_ca_system_score_gemma":0.0008803443,"threshold_uncertainty_score":0.9905737},"labels":[],"label_agreement":null},{"id":"W1965529574","doi":"10.1139/e10-021","title":"Paleomagnetic evidence for multiple late Cenozoic glaciations in the Tintina Trench, west-central Yukon, CanadaThis article is a companion paper to Duk-Rodkin et al., also in this issue.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Lethbridge","funders":"","keywords":"Geology; Paleontology; Pleistocene; Cenozoic; Interglacial; Magnetostratigraphy; Glacial period; Stadial; Early Pleistocene; Quaternary; Paleomagnetism; Structural basin","score_opus":0.03892723054495574,"score_gpt":0.28427672180589963,"score_spread":0.2453494912609439,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965529574","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9389611,0.00063563825,0.0000036607219,0.05869409,0.00045780436,0.0002613308,0.000030721243,0.0000022271006,0.00095344806],"genre_scores_gemma":[0.9917897,0.0000529999,0.00067769527,0.007278467,0.000047384085,0.0000028357672,0.000003568925,0.0000017847638,0.0001455852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99798805,0.00028636708,0.00038600797,0.00024097726,0.00030645708,0.00079213106],"domain_scores_gemma":[0.9980253,0.0011102736,0.00011770118,0.00016036785,0.00010660046,0.00047976154],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0029036282,0.000116380616,0.00020107083,0.0004214314,0.00042160525,0.00014313408,0.00068922585,0.0000737734,0.0038932962],"category_scores_gemma":[0.0013336365,0.00008265481,0.00005529561,0.0008560006,0.0004383801,0.00047149102,0.000006870621,0.0004982172,0.00008512736],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014712485,0.0000089620125,0.9933241,0.000004094049,0.0000027262572,0.000054913344,0.0026950527,0.0009251376,0.000094140196,0.00004143948,0.0022307541,0.0006039484],"study_design_scores_gemma":[0.00027480462,0.0002578383,0.9729542,0.00004929485,0.000005365861,0.000104072315,0.00041775036,0.0052574393,0.000032345335,0.00020521057,0.020337518,0.00010416307],"about_ca_topic_score_codex":0.116140485,"about_ca_topic_score_gemma":0.99336123,"teacher_disagreement_score":0.87722075,"about_ca_system_score_codex":0.0000018021851,"about_ca_system_score_gemma":0.0014540211,"threshold_uncertainty_score":0.99701726},"labels":[],"label_agreement":null},{"id":"W1965657251","doi":"10.1139/e06-015","title":"Paleomagnetism of the Wintering Lake pluton and the Early Proterozoic tectonic motion of the Superior Boundary Zone, Manitoba","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Parks Canada; University of Windsor","funders":"University of Windsor; U.S. Department of Energy","keywords":"Geology; Paleomagnetism; Craton; Apparent polar wander; Proterozoic; Pluton; Archean; Paleontology; Fold (higher-order function); Polar wander; Remanence; Geochemistry; Overprinting; Orogeny; Tectonics","score_opus":0.007028543920957537,"score_gpt":0.1562023332470095,"score_spread":0.14917378932605196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965657251","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956839,0.0013826231,0.0000068360428,0.0016824408,0.00017133876,0.000104184386,0.000017964538,0.0000010643581,0.000949659],"genre_scores_gemma":[0.9997098,0.000011962049,0.00007330934,0.00007607917,0.000052406194,2.6133984e-7,3.579372e-7,6.8972486e-7,0.00007515522],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989828,0.00011270256,0.0003074742,0.00010143406,0.00028277296,0.00021282768],"domain_scores_gemma":[0.9994154,0.000078962825,0.00023325137,0.00010617305,0.00006864356,0.00009759622],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006164039,0.000076336095,0.00017362082,0.00006624829,0.00038905654,0.00008758584,0.00052468147,0.00003155871,0.00064123195],"category_scores_gemma":[0.000084177685,0.000029968434,0.00013532523,0.00043946222,0.0021557293,0.00013827575,0.000015462645,0.00015743695,0.0000017746072],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007708099,0.0000023813393,0.9966731,0.000006954502,0.000006847226,0.000002350577,0.00011131725,0.0006716279,0.00032150763,0.00007366916,0.0000061593955,0.002116381],"study_design_scores_gemma":[0.00015795117,0.00010705043,0.9943468,0.000047162863,0.00002148338,0.000049098813,0.00014270593,0.0004620422,0.000708627,0.0033755943,0.0005385629,0.000042936],"about_ca_topic_score_codex":0.07841748,"about_ca_topic_score_gemma":0.85465705,"teacher_disagreement_score":0.7762396,"about_ca_system_score_codex":9.0880576e-7,"about_ca_system_score_gemma":0.0002068166,"threshold_uncertainty_score":0.9277194},"labels":[],"label_agreement":null},{"id":"W1965795483","doi":"10.1139/e10-018","title":"Giant short-faced bear (<i>Arctodus simus</i>) from late Wisconsinan deposits at Cowichan Head, Vancouver Island, British Columbia","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Pleistocene-Era Hominins and Archaeology","field":"Social Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature; Royal British Columbia Museum","funders":"","keywords":"Geology; Radiocarbon dating; Context (archaeology); Head (geology); Quaternary; Mainland; Archaeology; Paleontology; Geography","score_opus":0.015996598426114932,"score_gpt":0.24437317411995513,"score_spread":0.2283765756938402,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965795483","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99005675,0.00036175415,0.000026113597,0.0011971106,0.0032965634,0.00015099363,0.00012814312,0.0000105650315,0.0047719753],"genre_scores_gemma":[0.99406785,0.00006252102,0.0012788685,0.00059752155,0.0005088983,0.0000014674181,0.0000024337114,0.0000112870775,0.0034691603],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976236,0.00017651635,0.0004392902,0.0003332637,0.0005246105,0.0009026799],"domain_scores_gemma":[0.99774,0.000187625,0.00022887153,0.0001639124,0.00023332321,0.0014463018],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001143099,0.00013230347,0.00035390322,0.00015852817,0.0023785795,0.00060997106,0.0007983636,0.00017173313,0.0021861396],"category_scores_gemma":[0.0003719174,0.00016222498,0.00012936624,0.0004633336,0.0022828633,0.0005162224,0.000049824317,0.00044436005,0.000024561627],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008397576,0.000016175423,0.9788872,0.0000022409001,0.000025981697,0.00080924336,0.0036121295,0.000080644815,0.0021268039,0.00008779937,0.010756234,0.0035871733],"study_design_scores_gemma":[0.00058382907,0.00032806612,0.81126356,0.000114827,0.00003562153,0.00017470961,0.001607269,0.00016407087,0.00041607395,0.001835846,0.18302763,0.00044846462],"about_ca_topic_score_codex":0.33565918,"about_ca_topic_score_gemma":0.9999612,"teacher_disagreement_score":0.664302,"about_ca_system_score_codex":0.000032051474,"about_ca_system_score_gemma":0.0034740013,"threshold_uncertainty_score":0.9989202},"labels":[],"label_agreement":null},{"id":"W1966025348","doi":"10.1139/e03-051","title":"Deposition and diagenesis of Mammoth Hot Springs travertine, Yellowstone National Park, Wyoming, U.S.A.","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Isotope Analysis in Ecology","field":"Environmental Science","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Geological Society of America","keywords":"Geology; Diagenesis; Calcite; Sedimentary depositional environment; Carbonate; Tufa; Pyroclastic rock; Sedimentary rock; Geochemistry; Deposition (geology); Lithology; Aragonite; Dolomite; Carbonate rock; Chalcedony; Mineralogy; Paleontology; Volcano; Sediment","score_opus":0.011304471671413406,"score_gpt":0.2130085829673718,"score_spread":0.2017041112959584,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966025348","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98684263,0.00016538608,0.00021245034,0.000146255,0.00010528974,0.000036425237,0.0000019700724,9.080625e-7,0.012488691],"genre_scores_gemma":[0.9952789,0.000027930519,0.0042712945,0.00017935187,0.000016682367,5.4723483e-7,1.6291527e-7,0.000002854309,0.00022229664],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990123,0.00006645077,0.00027075832,0.00012882575,0.0003028889,0.00021876468],"domain_scores_gemma":[0.9993958,0.000056868965,0.00021080507,0.000051710576,0.00003774677,0.00024708392],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010013593,0.000066524604,0.00013772049,0.00018542609,0.00018865454,0.000028781324,0.00018975289,0.00003454253,0.0012433532],"category_scores_gemma":[0.00025616545,0.00005832602,0.000048113117,0.0003602155,0.0010049132,0.00026533028,0.000009943737,0.000065572334,0.000014434816],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000439532,0.000018754969,0.98581743,0.0000038870426,0.000019555908,0.000034836605,0.000547947,0.0026827636,0.007991448,0.0010909106,0.00039286772,0.0013952208],"study_design_scores_gemma":[0.00022572979,0.00020688194,0.97515666,0.000017959044,0.00003023063,0.00021968014,0.000337981,0.0004943703,0.016588716,0.0008666445,0.0057189963,0.00013613355],"about_ca_topic_score_codex":0.0032676612,"about_ca_topic_score_gemma":0.099313244,"teacher_disagreement_score":0.09604558,"about_ca_system_score_codex":0.000022194698,"about_ca_system_score_gemma":0.00029265895,"threshold_uncertainty_score":0.9996697},"labels":[],"label_agreement":null},{"id":"W1966171119","doi":"10.1139/e02-073","title":"The Frasnian-Famennian (mid-Late Devonian) boundary in the type section of the Long Rapids Formation, James Bay Lowlands, northern Ontario, Canada","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Conodont; Geology; Extinction event; Devonian; Late Devonian extinction; Paleontology; Marine transgression; Carbonate; Tournaisian; Extinction (optical mineralogy); Global Boundary Stratotype Section and Point; Chemostratigraphy; Biostratigraphy; Isotopes of carbon; Carboniferous; Total organic carbon; Structural basin","score_opus":0.013096727844208664,"score_gpt":0.18317462716098762,"score_spread":0.17007789931677897,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966171119","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9754622,0.007783792,0.0000031282566,0.0025277273,0.0011657858,0.00008915108,0.000011040423,0.0000011001907,0.012956048],"genre_scores_gemma":[0.9995042,0.000060517,0.000024308953,0.00021820999,0.00006818364,2.0893465e-7,5.70505e-7,5.600767e-7,0.00012322376],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861455,0.00018306913,0.00035992102,0.000096021395,0.00038349433,0.0003629637],"domain_scores_gemma":[0.99912846,0.0001885823,0.0002727182,0.00013920506,0.000101999656,0.00016904915],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0010688922,0.00009957442,0.0001316324,0.00011778268,0.0013437894,0.00017115733,0.00075632404,0.000052212323,0.00037720706],"category_scores_gemma":[0.00008776068,0.000047636157,0.000065399814,0.00063142466,0.00071538816,0.00041130724,0.0000012018463,0.00034372465,0.0000020853238],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000061135597,0.0000019269494,0.98850375,0.0000023422288,0.000009541243,0.000021468628,0.0025901224,0.00073442346,8.1291785e-7,0.000008248613,0.0005796598,0.0075415755],"study_design_scores_gemma":[0.00011411806,0.0001273099,0.9844136,0.000030995034,0.0000073034207,0.00013996982,0.0011061562,0.00042521761,0.000010758434,0.0001647718,0.0133930575,0.00006669956],"about_ca_topic_score_codex":0.90080875,"about_ca_topic_score_gemma":0.99998564,"teacher_disagreement_score":0.0991769,"about_ca_system_score_codex":0.00000964906,"about_ca_system_score_gemma":0.0030331837,"threshold_uncertainty_score":0.9999563},"labels":[],"label_agreement":null},{"id":"W1966242579","doi":"10.1139/e06-113","title":"Protaspides of uppermost Cambrian trilobite<i>Missisquoia</i>, with implications for suprafamilial level classification of the genus","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Trilobite; Geology; Paleontology; Genus; Ordovician; Zoology; Biology","score_opus":0.06062805990201171,"score_gpt":0.25910524856814515,"score_spread":0.19847718866613345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966242579","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9903106,0.001124869,0.00055576407,0.0010174904,0.00022399519,0.0002635509,0.00024155012,0.0000014800647,0.006260674],"genre_scores_gemma":[0.99741524,0.00000633708,0.0024576404,0.00003841137,0.000057294405,5.905058e-7,0.0000014495295,6.6627615e-7,0.000022394599],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989402,0.00004690211,0.0004198566,0.000121530036,0.00018387969,0.0002876153],"domain_scores_gemma":[0.99865115,0.00022021894,0.00048388712,0.00012973568,0.00024814147,0.00026689694],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012619742,0.0000819215,0.00017981771,0.00022563389,0.0004299131,0.000026667429,0.00047913656,0.00005704573,0.000028021186],"category_scores_gemma":[0.00017986426,0.000049155195,0.00010161657,0.0005586882,0.0011746146,0.00021862106,6.1525606e-7,0.00010144764,3.0012333e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003515833,0.000005260448,0.9713848,0.000009027097,0.000014263343,0.0000010953634,0.00017083136,0.000060759852,0.0006888478,0.0009299261,0.000041738134,0.026658265],"study_design_scores_gemma":[0.00021307233,0.00042794505,0.9966098,0.00003915672,0.000021638725,0.00007402699,0.00036299412,0.00007256613,0.0011809039,0.00035994593,0.00057448936,0.00006345211],"about_ca_topic_score_codex":0.005224856,"about_ca_topic_score_gemma":0.52140003,"teacher_disagreement_score":0.5161752,"about_ca_system_score_codex":0.0000013360152,"about_ca_system_score_gemma":0.0018613947,"threshold_uncertainty_score":0.78984547},"labels":[],"label_agreement":null},{"id":"W1966258949","doi":"10.1139/e10-044","title":"High-precision U–Pb geochronology of the Butedale pluton, British ColumbiaThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Ann and Gordon Getty Foundation; Getty Foundation","keywords":"Pluton; Geology; Zircon; Geochronology; Geochemistry; Batholith; Paleomagnetism; Geophysics; Paleontology","score_opus":0.015284993710580846,"score_gpt":0.17040670611945682,"score_spread":0.15512171240887598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966258949","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99145055,0.00049280864,5.806949e-7,0.0017812642,0.0001912028,0.0000997707,0.000112320944,8.740745e-7,0.005870628],"genre_scores_gemma":[0.99918234,0.000100928606,0.00042244923,0.00014125477,0.00006529109,3.437325e-7,0.0000012731265,0.0000012459395,0.00008489477],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99805284,0.00020566673,0.0008492156,0.00018747323,0.00037403926,0.00033077737],"domain_scores_gemma":[0.9984577,0.0002690577,0.0007148253,0.00019686403,0.00022467122,0.0001369383],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012762357,0.00009958986,0.0005284636,0.00024478402,0.0000865008,0.000017710938,0.000881906,0.000109924935,0.050220665],"category_scores_gemma":[0.0007506766,0.00006467845,0.0001536112,0.0011962716,0.002199713,0.00023259713,0.000030353063,0.00025573873,0.0000038075138],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010217428,0.00010162948,0.9855677,0.000023423489,0.00004279086,0.00001633777,0.0021234148,0.0008175222,0.0030671677,0.00029693655,0.00046864204,0.007372288],"study_design_scores_gemma":[0.00030546507,0.00082695304,0.9400711,0.00015774592,0.000022269553,0.000020012847,0.0011829663,0.000107726526,0.048961353,0.007821531,0.0004434863,0.000079399055],"about_ca_topic_score_codex":0.25652805,"about_ca_topic_score_gemma":0.77897894,"teacher_disagreement_score":0.5224509,"about_ca_system_score_codex":0.0000038759463,"about_ca_system_score_gemma":0.000552165,"threshold_uncertainty_score":0.95064753},"labels":[],"label_agreement":null},{"id":"W1966345744","doi":"10.1139/e06-008","title":"A test of detailed Nd isotope mapping in the Grenville Province: delineating a duplex thrust sheet in the KipawaMattawa region","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Archean; Geology; Allochthon; Nappe; Terrane; Shear zone; Proterozoic; Crust; Geochemistry; Diachronous; Petrology; Tectonics; Paleontology","score_opus":0.022081770108768557,"score_gpt":0.19696634471712732,"score_spread":0.17488457460835877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966345744","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9889986,0.0009904995,0.000016541397,0.0041795955,0.000037207756,0.00010284288,0.000007346128,0.0000010097884,0.0056663593],"genre_scores_gemma":[0.9989887,0.00001233256,0.00039664723,0.0004905752,0.00008195484,5.0429566e-7,0.0000027004785,6.852981e-7,0.000025905147],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984739,0.00016115991,0.00049996073,0.00014651997,0.00034817206,0.0003702873],"domain_scores_gemma":[0.99899524,0.00048211848,0.00025168218,0.00010149073,0.00006458905,0.00010489097],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018608797,0.00009728434,0.0002040462,0.0002613634,0.00023886861,0.00011370745,0.00074548606,0.000041551135,0.00068209873],"category_scores_gemma":[0.0004330518,0.000045701112,0.00008536583,0.001301546,0.00046189374,0.00016492681,0.000005274214,0.00023760222,0.000006611673],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000019263098,0.000010246776,0.98940295,0.000004751923,0.0000016092279,0.00009707168,0.00029469893,0.00850961,0.000040271996,0.000047475838,0.00010381506,0.0014855937],"study_design_scores_gemma":[0.00013247402,0.00013071104,0.98419696,0.000054831053,0.000006855219,0.000108345856,0.0023754959,0.010400951,0.000022879229,0.001648544,0.00084683526,0.00007510769],"about_ca_topic_score_codex":0.091091655,"about_ca_topic_score_gemma":0.84430975,"teacher_disagreement_score":0.7532181,"about_ca_system_score_codex":0.0000018836593,"about_ca_system_score_gemma":0.00038597497,"threshold_uncertainty_score":0.91496086},"labels":[],"label_agreement":null},{"id":"W1966437433","doi":"10.1139/cjes-2012-0048","title":"The middle Eocene to early Miocene integrated sedimentary record in the Qaidam Basin and its implications for paleoclimate and early Tibetan Plateau uplift","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":106,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China; National Science Foundation","keywords":"Geology; Aridification; Sedimentary rock; Structural basin; Paleoclimatology; Plateau (mathematics); Weathering; Paleontology; Geochemistry; Climate change; Arid; Oceanography","score_opus":0.043500221611316524,"score_gpt":0.25085480794508613,"score_spread":0.2073545863337696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966437433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9770909,0.0021886756,0.0000042451466,0.019596571,0.00017134234,0.00037241273,0.000036578946,0.0000021148576,0.00053713715],"genre_scores_gemma":[0.99860436,0.0001628952,0.00042970356,0.0006822898,0.000035879253,0.0000054369757,0.0000029318362,0.0000017173384,0.00007476952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99869084,0.00016445591,0.00028816392,0.00018468992,0.00012155672,0.00055030826],"domain_scores_gemma":[0.9984404,0.0007897019,0.000100321,0.000100493555,0.00012877949,0.00044031846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017003079,0.00010486089,0.00016663087,0.0002491601,0.0009945057,0.00029329103,0.00048183126,0.00006266187,0.0001291175],"category_scores_gemma":[0.00019326246,0.000057746714,0.00003143112,0.00045718893,0.0005357124,0.0003552843,0.000007817914,0.00023500956,0.000027393107],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013038345,0.0000022603226,0.99652183,0.0000036205142,0.000007824983,0.0000060982716,0.0006119024,0.000017841208,0.000006777432,0.00014587556,0.00014160729,0.0025213135],"study_design_scores_gemma":[0.00016507292,0.00048404868,0.99453944,0.000026158534,0.0000070005285,0.00014250974,0.0008229771,0.0002589366,0.000014569297,0.001775317,0.0016886005,0.000075384305],"about_ca_topic_score_codex":0.015516334,"about_ca_topic_score_gemma":0.45175117,"teacher_disagreement_score":0.43623483,"about_ca_system_score_codex":6.9052004e-7,"about_ca_system_score_gemma":0.00037523187,"threshold_uncertainty_score":0.99103945},"labels":[],"label_agreement":null},{"id":"W1966450145","doi":"10.1139/e00-013","title":"Cryostratigraphy of the Klondike \"muck\" deposits, west-central Yukon Territory","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Geology; Holocene; Loess; Muck; Glacial period; Quaternary; Deglaciation; Geomorphology; Geochemistry; Paleontology","score_opus":0.02225638449498518,"score_gpt":0.20392228701503778,"score_spread":0.1816659025200526,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966450145","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9852122,0.0025041073,6.230392e-7,0.0007314278,0.00084267114,0.000060123202,0.00025217258,0.0000019820295,0.010394671],"genre_scores_gemma":[0.9990013,0.00014249851,0.0000763678,0.0003962055,0.00022545802,6.907463e-8,0.0000066465514,0.0000015707523,0.00014983704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987455,0.00007137108,0.00030606228,0.000117474825,0.00033087662,0.0004287294],"domain_scores_gemma":[0.99914,0.0000584071,0.00015786351,0.00011539395,0.000047049183,0.00048123696],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034753836,0.000100030404,0.00015323942,0.00017044762,0.00041961393,0.00012077425,0.0006017397,0.000047455305,0.012155727],"category_scores_gemma":[0.00001982358,0.00006241792,0.00013452975,0.0004491589,0.00064640644,0.0003502918,0.0000021703943,0.00015963252,0.00002474128],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000053965864,0.0000034601103,0.9925103,0.0000051799507,0.0000060961925,0.000023252735,0.0005137215,0.0005697852,0.0000832767,0.000014654277,0.0005120784,0.0057527553],"study_design_scores_gemma":[0.00010413032,0.00018383499,0.98574984,0.00006316587,0.000011515298,0.00014824033,0.00027898178,0.00015276065,0.00031514105,0.00010077013,0.012806912,0.00008470263],"about_ca_topic_score_codex":0.05079751,"about_ca_topic_score_gemma":0.8817621,"teacher_disagreement_score":0.8309646,"about_ca_system_score_codex":0.0000012883118,"about_ca_system_score_gemma":0.0009031613,"threshold_uncertainty_score":0.9887473},"labels":[],"label_agreement":null},{"id":"W1966504742","doi":"10.1139/e06-128","title":"Radiogenic isotope characteristics of the Mesoproterozoic intrusive rocks of the Nipigon Embayment, northwestern Ontario","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geoscience BC; University of Alberta; Lakehead University","funders":"Northern Ontario Heritage Fund Corporation; Lakehead University","keywords":"Sill; Geology; Radiogenic nuclide; Archean; Geochemistry; Proterozoic; Igneous rock; Precambrian; Rift; Sedimentary rock; Basalt; Petrogenesis; Mantle (geology); Geochronology; Tectonics; Paleontology","score_opus":0.012363187388874756,"score_gpt":0.1836517740964435,"score_spread":0.17128858670756875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966504742","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967839,0.00035853486,0.000023254815,0.00061060593,0.0004104655,0.00008573405,0.000029654673,7.930209e-7,0.0016970474],"genre_scores_gemma":[0.99918246,0.000009284455,0.0001359609,0.00039413534,0.00006956522,7.4288415e-8,0.0000012734724,8.370433e-7,0.00020641951],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985445,0.000065967775,0.0005162028,0.0001256599,0.00041764465,0.00032999396],"domain_scores_gemma":[0.9986744,0.00011168714,0.0005635562,0.00015624893,0.00019899497,0.00029510376],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008468104,0.000102336635,0.00024444197,0.000115226714,0.0002633888,0.000035387486,0.0009096706,0.000050073115,0.002039294],"category_scores_gemma":[0.00013791717,0.00004789541,0.00022339882,0.0006382667,0.0007914307,0.00013383891,0.000019262663,0.00022096853,0.000005409277],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009306432,0.0000053505796,0.9963784,0.0000031838101,0.000021514274,0.000007818907,0.00052596896,0.00028828013,0.00011696792,0.000016262271,0.000012063553,0.002614854],"study_design_scores_gemma":[0.000087342196,0.00015881806,0.9939959,0.00003794771,0.000040466668,0.000053737207,0.0002727268,0.000044234523,0.002344601,0.00072837103,0.0021705294,0.00006530138],"about_ca_topic_score_codex":0.3561278,"about_ca_topic_score_gemma":0.97491115,"teacher_disagreement_score":0.61878335,"about_ca_system_score_codex":0.0000046494542,"about_ca_system_score_gemma":0.00084943004,"threshold_uncertainty_score":0.998873},"labels":[],"label_agreement":null},{"id":"W1966640135","doi":"10.1139/e01-029","title":"The interplay of regional structure and emplacement mechanisms at the contact of the South Mountain Batholith, Nova Scotia: floor-down or wall-up?","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Batholith; Lineation; Bedding; Pluton; Devonian; Bed; Shear (geology); Shear zone; Fold (higher-order function); Geochemistry; Nova scotia; Geomorphology; Petrology; Seismology; Tectonics; Anisotropy","score_opus":0.016690326560861227,"score_gpt":0.21475089160697217,"score_spread":0.19806056504611094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966640135","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937561,0.0008803904,0.000014414935,0.0046690586,0.00023610935,0.00007449477,0.000056035573,7.8816765e-7,0.00031261164],"genre_scores_gemma":[0.9988555,0.000037473907,0.00010077028,0.0005859707,0.00003667589,7.1155995e-8,0.0000016415804,8.4853053e-7,0.0003810575],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986489,0.00011697987,0.00035335717,0.00014068218,0.00043073675,0.00030938003],"domain_scores_gemma":[0.99892676,0.00023423386,0.00033220224,0.00013665935,0.00012549295,0.00024462916],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00085587776,0.0001086973,0.00019961693,0.00006909275,0.00052718725,0.00007694335,0.00067378127,0.000038974016,0.004913505],"category_scores_gemma":[0.00019134815,0.00003738458,0.00010443635,0.000451733,0.001159342,0.00010053668,0.000024302895,0.00017971804,0.000005021268],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010138012,0.0000035186401,0.99454147,0.0000056896015,0.000055679186,0.000015731805,0.00096111343,0.0015240307,0.00045823742,0.00050139916,0.00023805306,0.0015936991],"study_design_scores_gemma":[0.00030354664,0.0005219478,0.9797843,0.00006559892,0.000064069885,0.0004488981,0.0033730096,0.00096591417,0.0017333026,0.009678123,0.002931676,0.00012961474],"about_ca_topic_score_codex":0.024427528,"about_ca_topic_score_gemma":0.751152,"teacher_disagreement_score":0.72672445,"about_ca_system_score_codex":0.0000030773701,"about_ca_system_score_gemma":0.0004144672,"threshold_uncertainty_score":0.9959961},"labels":[],"label_agreement":null},{"id":"W1966656923","doi":"10.1139/e03-094","title":"Biostratigraphic significance of lower Paleozoic microfaunas from eastern Canada","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Institut National de la Recherche Scientifique; Centre de Géomatique du Québec; Geological Survey of Canada","funders":"","keywords":"Geology; Paleontology; Devonian; Ordovician; Peninsula; Gondwana; Conodont; Paleozoic; Biostratigraphy; Palynology; Facies; Archaeology; Geography; Tectonics; Pollen","score_opus":0.01607872705919222,"score_gpt":0.19692661007326456,"score_spread":0.18084788301407234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966656923","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97970533,0.009284166,0.000027224165,0.00068980386,0.0009968056,0.00005970689,0.00014679319,0.000002037576,0.009088128],"genre_scores_gemma":[0.99870414,0.000032672164,0.0010348363,0.00013239087,0.00008208392,9.5313844e-8,0.0000015018629,6.118851e-7,0.000011688727],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998588,0.000056587152,0.00042084232,0.00018247467,0.0003402717,0.00041178986],"domain_scores_gemma":[0.99873245,0.0001073169,0.00032670415,0.000116973315,0.00010576066,0.00061080983],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003383047,0.00013285763,0.00025511565,0.00025146484,0.00028085103,0.00006114822,0.000578242,0.00006738299,0.000451013],"category_scores_gemma":[0.000058929712,0.0001055752,0.00009875514,0.0005122075,0.0009827896,0.0003071936,5.4628487e-7,0.00018978267,0.0000037244738],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001474068,0.000004222371,0.9937685,0.0000038744183,0.000024308623,0.00024620772,0.000142567,0.00059083087,0.00017461156,0.00010864449,0.00005106573,0.004870436],"study_design_scores_gemma":[0.00023267063,0.00033696851,0.99561137,0.00006567836,0.000012785459,0.00005524147,0.00031255247,0.000027871214,0.0009473026,0.0017657678,0.00050380826,0.00012799725],"about_ca_topic_score_codex":0.9450706,"about_ca_topic_score_gemma":0.9995989,"teacher_disagreement_score":0.0545283,"about_ca_system_score_codex":0.0000017958387,"about_ca_system_score_gemma":0.00792788,"threshold_uncertainty_score":0.9976962},"labels":[],"label_agreement":null},{"id":"W1966666139","doi":"10.1139/e02-058","title":"Hydrogeology of the Oak Ridges Moraine aquifer system: implications for protection and management from the Duffins Creek watershed","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"The Scarborough Hospital","funders":"Natural Sciences and Engineering Research Council of Canada; Ministry of Natural Resources","keywords":"Moraine; Aquifer; Geology; Hydrogeology; Groundwater; Groundwater flow; Watershed; Hydrology (agriculture); Terminal moraine; Geomorphology; Glacial period","score_opus":0.029737613805182545,"score_gpt":0.2029820216126647,"score_spread":0.17324440780748215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966666139","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9847789,0.00019818693,0.0010306834,0.01272571,0.00014283166,0.0002759322,0.000019577119,0.0000018270637,0.0008263618],"genre_scores_gemma":[0.99888915,0.000014217183,0.00020184478,0.00018195907,0.000025259047,0.000013033269,2.61712e-7,0.0000015898436,0.00067268393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994647,0.00004043034,0.00016193656,0.00009344272,0.000103002254,0.00013649826],"domain_scores_gemma":[0.99966776,0.000037302794,0.000119290475,0.00008706156,0.000022473501,0.000066131215],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031358615,0.00004610877,0.000077134035,0.000031940628,0.0005687483,0.00005087463,0.00025618347,0.000014539971,0.00007314103],"category_scores_gemma":[0.000021627477,0.000025174279,0.00003496284,0.00016423012,0.0005609692,0.0001186356,0.000029239156,0.00003701573,0.0000038885987],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006362648,0.000024691059,0.95230335,0.000026335443,0.00009219665,0.0000039963584,0.003653219,0.00081616984,0.001933757,0.0029645553,0.004197837,0.033977535],"study_design_scores_gemma":[0.0001671415,0.00008298905,0.97091454,0.00002092562,0.000027740016,0.000024579893,0.0010830346,0.0005604429,0.00022017036,0.00036337695,0.026489766,0.000045313547],"about_ca_topic_score_codex":0.0068142028,"about_ca_topic_score_gemma":0.09322467,"teacher_disagreement_score":0.08641046,"about_ca_system_score_codex":0.00001179578,"about_ca_system_score_gemma":0.000014219852,"threshold_uncertainty_score":0.9997995},"labels":[],"label_agreement":null},{"id":"W1967201289","doi":"10.1139/e07-018","title":"Diversity dynamics of Early Jurassic ostracods of the Cordillera Ibérica (Spain) and the re-evaluation of the Pliensbachian–Toarcian mass extinction","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Ostracod; Extinction event; Geology; Paleontology; Extinction (optical mineralogy); Marine invertebrates; Mesozoic; Oceanography; Ecology; Biological dispersal; Structural basin; Biology","score_opus":0.025367569621865493,"score_gpt":0.22675277590192353,"score_spread":0.20138520628005804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967201289","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98229754,0.0011488283,0.000051150084,0.0009652061,0.0004584271,0.00013199606,0.00002904532,6.846629e-7,0.014917149],"genre_scores_gemma":[0.9997679,0.000015997419,0.00014775869,0.00003167378,0.000025579835,5.4389943e-8,1.7147752e-7,3.6210704e-7,0.000010500687],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983904,0.00030814458,0.00033873547,0.00009570589,0.0006608109,0.00020623348],"domain_scores_gemma":[0.99862105,0.00029318058,0.0006218501,0.0001315717,0.00019882263,0.00013355339],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0045653265,0.00007337961,0.00017293158,0.000111214424,0.0010412008,0.000021107888,0.0005522045,0.00005811471,0.000102802725],"category_scores_gemma":[0.00025600055,0.000035946243,0.00011686287,0.0005120957,0.0028311408,0.00020251259,0.000006186544,0.00019331605,1.2869184e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000036779165,0.0000029009832,0.9610847,0.0000043629434,0.00001768623,9.979935e-7,0.0011616483,0.000382171,0.000023072475,0.00019138063,0.0000044837034,0.037089817],"study_design_scores_gemma":[0.00029934174,0.0001566657,0.9934185,0.00003597377,0.00005962835,0.000016334243,0.0014800314,0.002965057,0.00011656242,0.0013986047,0.000012035119,0.0000412273],"about_ca_topic_score_codex":0.0068004164,"about_ca_topic_score_gemma":0.51607233,"teacher_disagreement_score":0.5092719,"about_ca_system_score_codex":0.0000028369273,"about_ca_system_score_gemma":0.00067781174,"threshold_uncertainty_score":0.9998826},"labels":[],"label_agreement":null},{"id":"W1967250324","doi":"10.1139/e06-058","title":"Glacial and rocky-shore dynamics of the Karlebotn monadnocks: late Neoproterozoic of northern Norway","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Brock University","keywords":"Geology; Unconformity; Glacial period; Shore; Fjord; Glacier; Paleontology; Geomorphology; Bedrock; Geochemistry; Oceanography; Sedimentary rock","score_opus":0.010398510437862848,"score_gpt":0.20070058431998938,"score_spread":0.19030207388212653,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967250324","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935885,0.0010904883,0.000008317042,0.001107858,0.00025817732,0.0000749742,0.00003592698,8.3733823e-7,0.0038349254],"genre_scores_gemma":[0.9995629,0.000015433257,0.00014133859,0.00003842576,0.000044902856,9.891225e-8,0.0000019097772,0.0000011608109,0.00019381764],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886215,0.000114790426,0.00032336463,0.0001153882,0.000252499,0.00033182936],"domain_scores_gemma":[0.99918306,0.0001207379,0.0002599518,0.000096909636,0.0001433427,0.00019600791],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006833188,0.00008391499,0.00020722667,0.00021014891,0.00031674703,0.000027967866,0.00047518875,0.00007930242,0.00045227222],"category_scores_gemma":[0.00008318635,0.00005290866,0.000067125424,0.0003907426,0.001645741,0.00015389782,0.000009150439,0.00020990655,0.000007908984],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000971607,0.0000025976458,0.9962573,0.000009363413,0.0000072783523,0.000017406583,0.00017044775,0.0027665254,0.000009190087,0.000091696566,0.00001046863,0.00064802537],"study_design_scores_gemma":[0.00012985461,0.00018388956,0.9945924,0.000027985718,0.000009487849,0.00014734922,0.00019213997,0.0019552333,0.00008785775,0.0024965538,0.00012107818,0.000056146637],"about_ca_topic_score_codex":0.022680635,"about_ca_topic_score_gemma":0.9537997,"teacher_disagreement_score":0.9311191,"about_ca_system_score_codex":5.7949285e-7,"about_ca_system_score_gemma":0.0009485807,"threshold_uncertainty_score":0.9838274},"labels":[],"label_agreement":null},{"id":"W1967333903","doi":"10.1139/e10-088","title":"Tholeiitic to calc-alkaline cyclic volcanism in the Roy Group, Chibougamau area, Abitibi Greenstone Belt — revised stratigraphy and implications for VHMS explorationGeological Survey of Canada Contribution 20100254. Ministère des Ressources naturelles et de la Faune Contribution 8439-2010-2011-17.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; Ministère des Ressources naturelles et des Forêts (Québec); Institut National de la Recherche Scientifique; Geological Survey of Canada","funders":"","keywords":"Greenstone belt; Mafic; Geology; Geochemistry; Archean; Felsic; Zircon; Volcanic rock; Basalt; Craton; Volcano; Paleontology","score_opus":0.034060668048975055,"score_gpt":0.24293876801619976,"score_spread":0.2088780999672247,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967333903","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940372,0.0016824027,0.00035568216,0.0027457485,0.00006330776,0.00021683838,0.0005320252,0.0000026245057,0.0003641846],"genre_scores_gemma":[0.99843377,0.00010723095,0.00068057206,0.0006174478,0.000028968403,0.0000038706153,0.00011310972,0.0000012325063,0.0000137725],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99825287,0.000428491,0.0004595006,0.00021258704,0.00022221897,0.00042433353],"domain_scores_gemma":[0.9978578,0.0009587262,0.000262095,0.000104420025,0.00038234887,0.00043460343],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0029773267,0.00013807567,0.00030661927,0.00019520616,0.0005143602,0.00008284292,0.0003764001,0.0001006723,0.00023543772],"category_scores_gemma":[0.0013828165,0.00008512087,0.000075076,0.00061720965,0.001015847,0.00019261056,0.0000059954655,0.00021439695,5.3917637e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003401345,0.000020708741,0.9972078,0.000005059297,0.000013406282,0.0000099363915,0.00054047495,0.0003022492,0.00021143946,0.0010490512,0.0002747789,0.0003310412],"study_design_scores_gemma":[0.00023643125,0.00038699264,0.9874598,0.000035274752,0.00002800276,0.000048956084,0.00032443766,0.00026494637,0.0000929066,0.010576845,0.0004326088,0.000112833084],"about_ca_topic_score_codex":0.824475,"about_ca_topic_score_gemma":0.9976411,"teacher_disagreement_score":0.1731661,"about_ca_system_score_codex":0.000005623064,"about_ca_system_score_gemma":0.000567495,"threshold_uncertainty_score":0.3956095},"labels":[],"label_agreement":null},{"id":"W1967350649","doi":"10.1139/e09-026","title":"Paleomagnetism and U–Pb geochronology of the Lac de Gras diabase dyke swarm, Slave Province, Canada: implications for relative drift of Slave and Superior provinces in the PaleoproterozoicGeological Survey of Canada Contribution 20080350.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Craton; Paleomagnetism; Geochronology; Baddeleyite; Large igneous province; Archean; Apparent polar wander; Paleontology; Rodinia; Laurentia; Sinistral and dextral; Latitude; Seismology; Zircon; Structural basin; Paleozoic; Tectonics; Geodesy","score_opus":0.011657468668284168,"score_gpt":0.19409731117124612,"score_spread":0.18243984250296197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967350649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9903913,0.0017881201,0.00002192561,0.0069999862,0.00003687403,0.00024881435,0.00039649292,4.872955e-7,0.00011599999],"genre_scores_gemma":[0.99950945,0.00004254187,0.0002042241,0.00021171193,0.000011725742,0.0000011427069,0.000008161616,4.8508184e-7,0.000010572675],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986645,0.00023811459,0.00042136697,0.00015440526,0.00018826358,0.0003333768],"domain_scores_gemma":[0.99845606,0.0006796846,0.00034119523,0.00008846167,0.00023315268,0.00020141917],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00097351806,0.00009717786,0.0002989833,0.00007591386,0.00021969755,0.00001587161,0.00034125656,0.000056887253,0.00005485136],"category_scores_gemma":[0.0010613449,0.00005056387,0.00004256088,0.00040929907,0.001013969,0.00009714512,0.000007244626,0.00014544383,2.6587157e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015319647,0.0000061828027,0.9979209,0.000006366636,0.000008705532,0.000004771113,0.000081956496,0.00028707608,0.000104893676,0.000352734,0.00004194033,0.0011691547],"study_design_scores_gemma":[0.0001807581,0.00048787563,0.99359465,0.000020824995,0.000020390447,0.00003329606,0.00017935147,0.00036789782,0.0004354396,0.0045105517,0.00010652206,0.0000624389],"about_ca_topic_score_codex":0.98230374,"about_ca_topic_score_gemma":0.99993473,"teacher_disagreement_score":0.017630948,"about_ca_system_score_codex":0.0000064576916,"about_ca_system_score_gemma":0.004417454,"threshold_uncertainty_score":0.78363734},"labels":[],"label_agreement":null},{"id":"W1967489728","doi":"10.1139/e03-022","title":"The distribution of igneous rocks beneath Mont Mégantic (the easternmost Monteregian) as revealed by gravity","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Dominion Astrophysical Observatory; Université Laval","funders":"","keywords":"Geology; Gabbro; Bouguer anomaly; Geochemistry; Precambrian; Leucogranite; Basement; Intrusion; Petrology; Igneous rock; Geomorphology; Paleontology; Gravity anomaly; Gneiss; Metamorphic rock","score_opus":0.009662315129354827,"score_gpt":0.18300127968464935,"score_spread":0.17333896455529452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967489728","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99195415,0.0034348487,0.00006510925,0.0020127094,0.00016952392,0.000056483736,0.00005560057,0.0000015857706,0.002249991],"genre_scores_gemma":[0.99939024,0.000077340235,0.000037516395,0.0001410846,0.000029591667,1.5796884e-7,0.0000061348537,7.094956e-7,0.00031724054],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986337,0.00015122448,0.00033995885,0.0001373998,0.00035841845,0.0003793444],"domain_scores_gemma":[0.9988205,0.00022896986,0.00026080344,0.00012214514,0.00014264807,0.00042496072],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010082345,0.00010069908,0.00018516257,0.00004031816,0.0007683326,0.00012761,0.000561837,0.00003968605,0.0008159662],"category_scores_gemma":[0.000535719,0.000046590114,0.00013239251,0.0004829461,0.00076345686,0.00012442541,0.0000045981556,0.00016910279,0.000026011972],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011515893,0.000007759151,0.99191034,0.0000029031196,0.000025184869,0.000029806151,0.0000928886,0.0017494588,0.00005905987,0.00029633442,0.0005771104,0.0052376245],"study_design_scores_gemma":[0.00033776803,0.0010424585,0.91964495,0.000072017276,0.00010972408,0.00047838915,0.001833008,0.0018086906,0.001519853,0.029928386,0.042909317,0.00031541442],"about_ca_topic_score_codex":0.037843842,"about_ca_topic_score_gemma":0.29978055,"teacher_disagreement_score":0.26193672,"about_ca_system_score_codex":0.000001968216,"about_ca_system_score_gemma":0.0003426535,"threshold_uncertainty_score":0.96856326},"labels":[],"label_agreement":null},{"id":"W1967557881","doi":"10.1139/e02-019","title":"Extensional exhumation of a high-pressure granulite terrane in Payer Land, Greenland Caledonides: structural, petrologic, and geochronologic evidence from metapelites","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Nationale Geologiske Undersøgelser for Danmark og Grønland","keywords":"Geology; Granulite; Kyanite; Geochemistry; Metamorphism; Gneiss; Mafic; Petrology; Metamorphic rock; Metamorphic facies; Eclogite; Zircon; Sillimanite; Facies; Geomorphology; Quartz; Biotite; Subduction; Tectonics; Paleontology","score_opus":0.029570050003668483,"score_gpt":0.20259370530382328,"score_spread":0.1730236553001548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967557881","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9740813,0.02434906,0.000007611143,0.0012305379,0.000085788095,0.000043415137,0.00006474202,0.0000022975958,0.00013527313],"genre_scores_gemma":[0.99793893,0.00042328786,0.001408791,0.0001489108,0.000050178343,1.7418728e-7,0.00000717163,6.8880246e-7,0.000021865357],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99866086,0.00012321697,0.0004045877,0.00022740726,0.0002855569,0.00029839377],"domain_scores_gemma":[0.998845,0.00043592078,0.00023478907,0.000083506966,0.00010259719,0.0002982104],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004918169,0.000121394434,0.00034830047,0.00025836413,0.00015137575,0.00006725962,0.00031081025,0.00007094513,0.019954052],"category_scores_gemma":[0.00045592478,0.00007082821,0.000071329305,0.00039913473,0.00064001576,0.00040822537,0.000009438426,0.00017839982,0.000012772734],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012269419,0.0000028498353,0.9903314,0.000006460063,0.000015321966,0.000045215154,0.00013373407,0.0035648735,0.00012687853,0.000008795205,0.000016765844,0.005735428],"study_design_scores_gemma":[0.00018853498,0.0002549596,0.97983414,0.00006729738,0.000036907455,0.00004847157,0.000072592105,0.011444918,0.000063505395,0.007807428,0.00008504331,0.0000962184],"about_ca_topic_score_codex":0.11277307,"about_ca_topic_score_gemma":0.39618796,"teacher_disagreement_score":0.2834149,"about_ca_system_score_codex":0.0000010545722,"about_ca_system_score_gemma":0.000066977016,"threshold_uncertainty_score":0.98094183},"labels":[],"label_agreement":null},{"id":"W1967624713","doi":"10.1139/e08-004","title":"Internal structure and conditions of permafrost mounds at Umiujaq in Nunavik, Canada, inferred from field investigation and electrical resistivity tomography","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval; Center for Northern Studies; University of Alberta; Defence Research and Development Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Permafrost; Electrical resistivity tomography; Electrical resistivity and conductivity; Geology; Soil science; Geophysics; Geomorphology; Mineralogy","score_opus":0.023814742304208422,"score_gpt":0.21648272731297197,"score_spread":0.19266798500876353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967624713","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954261,0.0013582703,6.318195e-7,0.0003976501,0.00015775813,0.000036707846,0.0023843194,7.7879184e-7,0.00023777141],"genre_scores_gemma":[0.999369,0.00011246384,0.000051519804,0.00031216312,0.00005314083,7.644419e-8,0.00008385419,0.0000010426378,0.000016718903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991822,0.00004994101,0.00023216037,0.00012505331,0.00020191334,0.00020868183],"domain_scores_gemma":[0.9991414,0.0002263071,0.00013035971,0.000046771216,0.000052078492,0.00040308636],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015099443,0.00007991917,0.00016280134,0.0002695327,0.00027353255,0.00004296877,0.00012670248,0.000049090868,0.0010358811],"category_scores_gemma":[0.0001011522,0.00006668667,0.000021950254,0.0003382841,0.0005057121,0.00025530445,0.000005546031,0.00015519476,3.1868555e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010107293,9.311586e-7,0.99831116,0.0000030995764,0.0000042545526,0.00006469732,0.00056389516,0.000057467772,0.00047734202,0.000006494785,0.0002994769,0.00020106685],"study_design_scores_gemma":[0.00015826606,0.00013743133,0.997563,0.000040072602,0.000005812814,0.00018584392,0.00012908928,0.00061379833,0.00049160497,0.00036329275,0.00023590236,0.00007587456],"about_ca_topic_score_codex":0.951113,"about_ca_topic_score_gemma":0.99945784,"teacher_disagreement_score":0.048344873,"about_ca_system_score_codex":0.0000060926363,"about_ca_system_score_gemma":0.0010911785,"threshold_uncertainty_score":0.99987733},"labels":[],"label_agreement":null},{"id":"W1967730717","doi":"10.1139/e03-030","title":"Basin architecture and density structure beneath the Strait of Georgia, British Columbia","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada","funders":"British Geological Survey","keywords":"Geology; Structural basin; Basement; Tectonics; Submarine pipeline; Seismology; Paleontology; Oceanography; Archaeology","score_opus":0.00767839979509548,"score_gpt":0.17326388539590032,"score_spread":0.16558548560080483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967730717","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960972,0.0011434896,0.00006789574,0.00044957362,0.00022034528,0.000049072238,0.00007264873,0.0000030174658,0.0018967614],"genre_scores_gemma":[0.99604124,0.000028674698,0.0029306673,0.0007931141,0.000031949225,2.0541075e-8,9.907369e-7,0.0000011639956,0.00017218845],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991578,0.000094473784,0.00018314953,0.00011239972,0.00021814182,0.0002340767],"domain_scores_gemma":[0.9993493,0.00007722658,0.00014308753,0.000073557494,0.00008372094,0.00027312117],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00068696524,0.000057546564,0.00013906017,0.00008465816,0.00046837228,0.00032267006,0.00027171467,0.000038852566,0.0015343179],"category_scores_gemma":[0.00016063954,0.000049403003,0.0000433797,0.000253652,0.00087988324,0.00016945053,0.0000025710435,0.00019078793,7.186685e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000012089423,0.0000011931091,0.9671788,0.0000054251473,0.0000072491594,0.000034655073,0.00028299668,0.00023748007,0.00002876409,0.00005223273,0.0023087175,0.029861238],"study_design_scores_gemma":[0.00011727046,0.00021845299,0.9603727,0.000064945576,0.000013770524,0.0014581914,0.00062233786,0.00023287315,0.0005813612,0.0075930394,0.028616412,0.00010864432],"about_ca_topic_score_codex":0.34917352,"about_ca_topic_score_gemma":0.7721035,"teacher_disagreement_score":0.42292997,"about_ca_system_score_codex":0.0000011902043,"about_ca_system_score_gemma":0.0009793403,"threshold_uncertainty_score":0.99937844},"labels":[],"label_agreement":null},{"id":"W1967798302","doi":"10.1139/e00-036","title":"SHRIMP U-Pb geochronology of volcanic rocks, Belt Supergroup, western Montana: evidence for rapid deposition of sedimentary strata","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":156,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; Northwestern University","keywords":"Geology; Geochronology; Rhyolite; Zircon; Geochemistry; Volcanic rock; Sedimentary rock; Felsic; Paleontology; Volcano","score_opus":0.031070075450974673,"score_gpt":0.22939153493310568,"score_spread":0.198321459482131,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967798302","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924462,0.0055470583,0.00008903124,0.0012029422,0.000115305964,0.00006786971,0.00009445875,0.0000021067751,0.00043506522],"genre_scores_gemma":[0.9983681,0.00023835801,0.0010265002,0.00021668631,0.00007963148,3.4950116e-7,0.0000155476,0.0000011437446,0.000053688425],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99857086,0.000056852812,0.0005230508,0.00019853683,0.00026929984,0.0003813924],"domain_scores_gemma":[0.9988663,0.00025142898,0.00023506451,0.00010724472,0.0001371545,0.00040281736],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005250591,0.00011471057,0.0003270254,0.00019613715,0.00020211928,0.000031148535,0.0005244183,0.00006644524,0.009794504],"category_scores_gemma":[0.00009171631,0.00008275729,0.00016384397,0.0004176042,0.0005762726,0.00043967742,0.0000049159707,0.00011220372,0.000009913599],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006584757,0.000016008076,0.96687764,0.000029824845,0.00004980244,0.000025416613,0.0001292493,0.0081399735,0.0007650046,0.000014093072,0.00010974423,0.023777412],"study_design_scores_gemma":[0.00041488872,0.0028546173,0.98255867,0.00019397757,0.00013050802,0.00016064488,0.00033535203,0.0037200956,0.0061477004,0.001993055,0.0012727737,0.00021769982],"about_ca_topic_score_codex":0.10811228,"about_ca_topic_score_gemma":0.7633798,"teacher_disagreement_score":0.65526754,"about_ca_system_score_codex":0.0000028107133,"about_ca_system_score_gemma":0.0005211172,"threshold_uncertainty_score":0.9911107},"labels":[],"label_agreement":null},{"id":"W1967986246","doi":"10.1139/e04-070","title":"The Archean deep-marine environment: turbidite architecture of the Burwash Formation, Slave Province, Northwest Territories","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Archean; Sedimentary rock; Clastic rock; Sedimentary depositional environment; Geochemistry; Basement; SLATES; Paleontology; Turbidite; Conglomerate; Structural basin; Archaeology","score_opus":0.008371339490953096,"score_gpt":0.1729873022916543,"score_spread":0.1646159628007012,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967986246","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9846198,0.0017180591,0.000135183,0.007342271,0.00042556948,0.00014891395,0.00007709944,0.0000033770912,0.0055297436],"genre_scores_gemma":[0.99846387,0.00009764029,0.00095155335,0.00016311364,0.00017670775,2.5128014e-7,0.000005702838,8.939261e-7,0.00014027038],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989251,0.0000623564,0.00033398657,0.00007522705,0.00031828225,0.00028508084],"domain_scores_gemma":[0.9991721,0.00015212744,0.00027694504,0.00011175069,0.000069321766,0.0002177524],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006149027,0.00008504266,0.00010320632,0.00009326406,0.0009737925,0.00015122954,0.00065600587,0.00003129102,0.00051011844],"category_scores_gemma":[0.00013098815,0.000038584036,0.00006631343,0.00026645552,0.0009231134,0.0004718882,0.000012259581,0.0001805383,0.000012028175],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000067667506,0.0000043018845,0.8684373,0.000011459689,0.000008632128,0.0000028014829,0.0010016483,0.042009566,0.000003584052,0.00036127743,0.00008917915,0.088063516],"study_design_scores_gemma":[0.000079845966,0.00017532951,0.7900224,0.000019565914,0.000008326983,0.000108466644,0.00041328036,0.0013107483,0.00023663575,0.0029686505,0.20457965,0.000077149314],"about_ca_topic_score_codex":0.010421478,"about_ca_topic_score_gemma":0.8362364,"teacher_disagreement_score":0.82581496,"about_ca_system_score_codex":0.0000022325587,"about_ca_system_score_gemma":0.0005496927,"threshold_uncertainty_score":0.9961682},"labels":[],"label_agreement":null},{"id":"W1968245628","doi":"10.1139/e00-020","title":"Potential-field signatures of buried Precambrian basement in the Western Canada Sedimentary Basin","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Precambrian; Basement; Rock magnetism; Sedimentary rock; Igneous rock; Lithology; Magnetic susceptibility; Magnetic anomaly; Geochemistry; Geophysics; Magnetization; Remanence; Magnetic field","score_opus":0.009376028927491148,"score_gpt":0.20710602462662744,"score_spread":0.1977299956991363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968245628","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98890597,0.00068523,0.000010234213,0.006767098,0.00027877273,0.00008177016,0.000024014553,8.307429e-7,0.003246079],"genre_scores_gemma":[0.99554175,0.000013653766,0.0003869618,0.0037582412,0.00013174524,1.5191146e-7,0.0000017428176,8.748496e-7,0.00016489657],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985084,0.00024024385,0.0003066251,0.00012109956,0.00046517578,0.00035848148],"domain_scores_gemma":[0.99917597,0.0002871373,0.00010563637,0.00008409616,0.000038488368,0.0003086483],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00096082326,0.000088962595,0.00017590541,0.00013006978,0.00016362706,0.00006002597,0.0005349053,0.000032363576,0.0027631575],"category_scores_gemma":[0.00006973013,0.0000532347,0.000057202906,0.0005932119,0.0001465483,0.00016473641,0.0000019184363,0.0002175086,0.000004666577],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007520509,0.00003325443,0.639554,0.000017863544,0.000025905347,0.00049284456,0.0005856282,0.02333904,0.000060430946,0.000045362933,0.0067134066,0.32905707],"study_design_scores_gemma":[0.00013481877,0.00048557878,0.9784193,0.000028241833,0.000009783773,0.000027410764,0.00015874884,0.00046199118,0.0003540362,0.00038106827,0.019459605,0.000079391626],"about_ca_topic_score_codex":0.9554415,"about_ca_topic_score_gemma":0.9895647,"teacher_disagreement_score":0.33886534,"about_ca_system_score_codex":0.000002329992,"about_ca_system_score_gemma":0.0016667332,"threshold_uncertainty_score":0.99814844},"labels":[],"label_agreement":null},{"id":"W1968474907","doi":"10.1139/e04-069","title":"Lithospheric structure in northwestern Canada from Lithoprobe seismic refraction and related studies: a synthesis","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Terrane; Lithosphere; Crust; Craton; Tectonics; Seismology; Seismic refraction; Paleontology","score_opus":0.010696862725369766,"score_gpt":0.18861441499108977,"score_spread":0.17791755226572,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968474907","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9897492,0.006903743,0.0000013651266,0.0027387813,0.00017001077,0.000029859293,0.000046090117,0.0000019877416,0.00035894127],"genre_scores_gemma":[0.9985471,0.00016587025,0.0007348807,0.00041433898,0.000068310386,1.15970316e-7,0.0000028217607,9.1489716e-7,0.000065672364],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988831,0.00006738577,0.00033772195,0.00019102165,0.00022410827,0.00029666288],"domain_scores_gemma":[0.999033,0.00024637,0.0001731312,0.00006088723,0.00007105656,0.00041558],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002908347,0.00010571601,0.00024523222,0.00011083632,0.00018534674,0.00006377242,0.00020454725,0.000050441482,0.0027936217],"category_scores_gemma":[0.00023647417,0.000069789116,0.00003685085,0.0005640682,0.00025076253,0.000296739,0.0000046499877,0.0002061423,0.000005691254],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000044324574,0.0000015585098,0.9668543,0.0000025023849,0.000022368671,0.00008434624,0.00024023646,0.013830544,0.000011980022,0.0000019663955,0.000033684963,0.01891212],"study_design_scores_gemma":[0.000093635696,0.00006193902,0.98700285,0.000050429928,0.000025411962,0.00008138967,0.0011405622,0.0060822708,0.000086970256,0.0021666377,0.0030842891,0.00012364096],"about_ca_topic_score_codex":0.94646025,"about_ca_topic_score_gemma":0.99967355,"teacher_disagreement_score":0.05321334,"about_ca_system_score_codex":0.000007986845,"about_ca_system_score_gemma":0.00081882696,"threshold_uncertainty_score":0.998118},"labels":[],"label_agreement":null},{"id":"W1968724912","doi":"10.1139/e99-118","title":"Major end moraines of Younger Dryas age on Wollaston Peninsula, Victoria Island, Canadian Arctic: implications for paleoclimate and for formation of hummocky moraine","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":97,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University; Geological Survey of Canada","funders":"","keywords":"Moraine; Younger Dryas; Geology; Deglaciation; Glacier; Arctic; Ice sheet; Radiocarbon dating; Meltwater; Ice core; Paleoclimatology; Physical geography; Glacial period; Paleontology; Oceanography; Climate change; Geography","score_opus":0.029614544822120413,"score_gpt":0.2630895233208913,"score_spread":0.23347497849877089,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968724912","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926864,0.0005842818,0.000036004985,0.002754814,0.00020294939,0.0003245938,0.0007363588,0.0000015166161,0.0026731025],"genre_scores_gemma":[0.9984514,0.00006574394,0.0010684851,0.00013978437,0.000066474815,0.0000029796859,0.000055123164,0.0000023701148,0.00014762254],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987932,0.00005000175,0.00039567892,0.00015503472,0.00013598157,0.0004701374],"domain_scores_gemma":[0.99852985,0.00039743743,0.00021138575,0.00010361243,0.00027148952,0.00048622765],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00093622616,0.000108037515,0.0002718994,0.00053488836,0.00050993665,0.000046446145,0.00028509993,0.0000879683,0.0009800803],"category_scores_gemma":[0.00022789412,0.00008632302,0.0000756736,0.00030965227,0.000691244,0.0003269562,0.0000018701342,0.00010281461,0.000004615357],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008369214,0.000004739136,0.99658847,0.000046048626,0.000015844389,0.0000058660817,0.00041215227,0.0006014324,0.00003057749,0.0010411978,0.000106774714,0.0010631989],"study_design_scores_gemma":[0.0006817086,0.0012202379,0.98594993,0.00005774953,0.00003250862,0.00016548607,0.00023179289,0.0013060622,0.00013722455,0.0040501393,0.006040196,0.00012693513],"about_ca_topic_score_codex":0.038796578,"about_ca_topic_score_gemma":0.96605164,"teacher_disagreement_score":0.92725503,"about_ca_system_score_codex":0.0000016318168,"about_ca_system_score_gemma":0.0009812174,"threshold_uncertainty_score":0.9999332},"labels":[],"label_agreement":null},{"id":"W1968812716","doi":"10.1139/e02-006","title":"\"Sudbury Breccia\" at Whitefish Falls, Ontario: evidence for an impact origin","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Waterloo","funders":"","keywords":"Breccia; Geology; Cataclastic rock; Clastic rock; Geochemistry; Impact structure; Conglomerate; Metamorphic rock; Igneous rock; Sedimentary rock; Petrology; Impact crater; Paleontology","score_opus":0.15717924623362922,"score_gpt":0.32029914062296966,"score_spread":0.16311989438934044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968812716","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98875666,0.0038199872,0.000010493339,0.00072231016,0.0006520687,0.00013071661,0.000030500858,0.0000045312504,0.0058727274],"genre_scores_gemma":[0.9962553,0.00007092067,0.00077548873,0.000310152,0.00013022742,4.804584e-7,0.0000040120276,0.000002072357,0.002451353],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99815065,0.00014944875,0.00032014912,0.00025317734,0.00030140634,0.0008251929],"domain_scores_gemma":[0.99782723,0.0004897092,0.00017676043,0.00015196954,0.0001797146,0.0011745928],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016576023,0.00014095905,0.0002559704,0.00040566528,0.00092597835,0.00016806427,0.00076278555,0.00011908871,0.023092989],"category_scores_gemma":[0.0003475248,0.00010379252,0.00013430456,0.0004007322,0.0008060283,0.0009901631,0.000005603242,0.00029926738,0.00025861117],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002573248,0.0000044918297,0.99524975,0.000004387355,0.000013460433,0.00007334757,0.0005886319,0.0010092919,0.0000031418394,0.000014381828,0.0020154733,0.0009979228],"study_design_scores_gemma":[0.00020779463,0.0014163913,0.9850032,0.000041536943,0.000013125012,0.000908763,0.00014334607,0.0015469546,0.000011427264,0.00024424103,0.010318394,0.0001448811],"about_ca_topic_score_codex":0.15419266,"about_ca_topic_score_gemma":0.99576414,"teacher_disagreement_score":0.8415715,"about_ca_system_score_codex":0.0000045860556,"about_ca_system_score_gemma":0.0018467448,"threshold_uncertainty_score":0.9778},"labels":[],"label_agreement":null},{"id":"W1968994832","doi":"10.1139/e04-059","title":"<i>Lusitanisuchus</i>, a new generic name for <i>Lisboasaurus mitracostatus</i> (Crocodylomorpha: Mesoeucrocodylia), with a description of new remains from the Upper Jurassic (Kimmeridgian) and Lower Cretaceous (Berriasian) of Portugal","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Freie Universität Berlin","keywords":"Cretaceous; Paleontology; Geology; Taxon; Skull; Structural basin; Portuguese; Philosophy","score_opus":0.02189126211771568,"score_gpt":0.20721764442063295,"score_spread":0.18532638230291726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968994832","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9803004,0.013452544,0.0013365985,0.0031684067,0.0005391177,0.00024241058,0.00028505013,0.0000038747044,0.00067158457],"genre_scores_gemma":[0.9872984,0.00024943845,0.011363978,0.00070054195,0.00023252884,5.06562e-7,0.000019042347,0.0000037671202,0.00013179306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984073,0.000076160606,0.0004979467,0.00026522842,0.0002617514,0.00049160747],"domain_scores_gemma":[0.9983394,0.00019166464,0.0005228658,0.00014398457,0.0001472543,0.0006548378],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004968394,0.00018699098,0.00039003158,0.00017016157,0.00038037938,0.00005190858,0.00043766585,0.0001228638,0.0003154093],"category_scores_gemma":[0.00011410371,0.00011858694,0.0001195701,0.00039683303,0.0012614258,0.00049208064,0.0000055629243,0.0001938217,0.0000041721264],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036154978,0.000015739239,0.9880703,0.000012030747,0.00009730199,0.000096536256,0.001358992,0.00221529,0.00066757336,0.00017237158,0.0019931893,0.004939101],"study_design_scores_gemma":[0.0011551135,0.0016877513,0.98075867,0.00011917934,0.00009909314,0.00078007334,0.0008866122,0.00012868132,0.00018564663,0.0024262355,0.01158885,0.00018412138],"about_ca_topic_score_codex":0.0418821,"about_ca_topic_score_gemma":0.6439301,"teacher_disagreement_score":0.602048,"about_ca_system_score_codex":0.000006238233,"about_ca_system_score_gemma":0.0045119296,"threshold_uncertainty_score":0.9644981},"labels":[],"label_agreement":null},{"id":"W1969023414","doi":"10.1139/e08-040","title":"Mineralogy, geochemistry, and Sr–Nd isotopes of the Cretaceous leucogranite from Karamadazı (Kayseri), central Turkey: implications for their sources and geological setting","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Leucogranite; Geology; Geochemistry; Mafic; Diorite; Biotite; Zircon; Metamorphic rock; Gneiss; Quartz; Paleontology","score_opus":0.019223388851992405,"score_gpt":0.1903813860492388,"score_spread":0.1711579971972464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969023414","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98910314,0.0061075976,0.000019403395,0.0041046212,0.00005380803,0.00006984634,0.00022548264,0.0000024144551,0.0003136881],"genre_scores_gemma":[0.99841267,0.00014327708,0.0010422228,0.0002674366,0.00008996125,4.1151233e-7,0.000009545975,9.197063e-7,0.00003352946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99903643,0.000046095996,0.0002732052,0.00019030427,0.00010894278,0.00034504943],"domain_scores_gemma":[0.9988968,0.0003416856,0.00020004253,0.0000816915,0.00009209091,0.00038773846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002464106,0.00010956671,0.00022550015,0.00005787566,0.0006015221,0.000058313923,0.00034237868,0.00006310892,0.00031993916],"category_scores_gemma":[0.00026193066,0.000058604877,0.0001020415,0.00023222664,0.001599549,0.00010605577,0.000014019545,0.00012950867,5.003163e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057500306,0.000003126009,0.996692,0.0000035874655,0.000016111184,0.0000032006344,0.00021066688,0.00046461305,0.000716599,0.000012292873,0.000082005194,0.0017900359],"study_design_scores_gemma":[0.00012634537,0.00010721587,0.98749954,0.000014790925,0.00002606964,0.0001614773,0.00024476042,0.001266403,0.0006995522,0.007139598,0.002626249,0.000088019624],"about_ca_topic_score_codex":0.01262332,"about_ca_topic_score_gemma":0.07686536,"teacher_disagreement_score":0.06424204,"about_ca_system_score_codex":7.8441894e-7,"about_ca_system_score_gemma":0.00021806646,"threshold_uncertainty_score":0.9939517},"labels":[],"label_agreement":null},{"id":"W1969190272","doi":"10.1139/e01-064","title":"Deep Probe: imaging the roots of western North America","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":154,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Archean; Geology; Lithosphere; Proterozoic; Terrane; Crust; Craton; Continental crust; Subduction; Paleontology; Baltic Shield; Sedimentary rock; Seismology; Tectonics","score_opus":0.015253635222557427,"score_gpt":0.17973001014486686,"score_spread":0.16447637492230943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969190272","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.988355,0.0033570016,0.00009746875,0.003198273,0.0001195984,0.00003648247,0.000009511215,0.00000220868,0.0048244908],"genre_scores_gemma":[0.99881774,0.000043310418,0.0004350068,0.00053657405,0.0000707156,7.664884e-8,0.0000011466808,6.1815734e-7,0.00009479416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895597,0.000051782208,0.00027642815,0.00011428632,0.00027920355,0.0003223052],"domain_scores_gemma":[0.999112,0.00010491542,0.00021606211,0.00008412832,0.000100902245,0.0003819988],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002630193,0.00007857464,0.00016841099,0.00013403104,0.00027445785,0.000077677985,0.00056227384,0.000015029284,0.007877839],"category_scores_gemma":[0.00012747466,0.000040340434,0.00009687276,0.0007198191,0.00085261784,0.00020432172,0.000005350507,0.00013617973,0.000075735785],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.181355e-7,0.000002799328,0.9776957,0.0000016251106,0.0000064974065,0.000022721073,0.0001369316,0.0045796926,0.000007123369,0.0000044936996,0.000054223663,0.01748725],"study_design_scores_gemma":[0.000050197308,0.00010971988,0.9816762,0.000010267576,0.000016276002,0.000060347564,0.00022769651,0.011191577,0.00002467155,0.0007746015,0.0057876953,0.00007070605],"about_ca_topic_score_codex":0.014328564,"about_ca_topic_score_gemma":0.4673146,"teacher_disagreement_score":0.45298606,"about_ca_system_score_codex":5.893989e-7,"about_ca_system_score_gemma":0.000108939836,"threshold_uncertainty_score":0.9930291},"labels":[],"label_agreement":null},{"id":"W1969526003","doi":"10.1139/e05-022","title":"105 Million years of igneous activity, Wrangell, Alaska, to Prince Rupert, British Columbia","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Batholith; Terrane; Igneous rock; Subduction; Pluton; Geochemistry; Continental arc; Mantle (geology); Island arc; Basalt; Paleontology; Tectonics","score_opus":0.011294617608950524,"score_gpt":0.18498728223025485,"score_spread":0.1736926646213043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969526003","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99431497,0.0007302815,0.000008180024,0.0009220316,0.00013016287,0.00005187907,0.00004521976,0.000002686257,0.0037946135],"genre_scores_gemma":[0.9974694,0.00004452935,0.0015079299,0.00035842616,0.00012484561,1.1822728e-7,0.000001964695,0.00000108456,0.0004917052],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99874985,0.000047183694,0.0002737365,0.00018290675,0.00035846836,0.00038787496],"domain_scores_gemma":[0.9987689,0.00009550116,0.00014161387,0.00008166811,0.00011201055,0.0008002606],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048697626,0.00006750621,0.00023522167,0.0001404738,0.00019342729,0.00021863396,0.0004760729,0.000049525486,0.01295246],"category_scores_gemma":[0.00019926911,0.00007245537,0.00011553226,0.000533392,0.00038495703,0.00025609243,0.000009113561,0.00013076459,0.0000719779],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005201233,0.000011422239,0.8930456,0.000003728586,0.000011967171,0.00009655495,0.0000803554,0.0044893953,0.00024454377,0.0000021262906,0.0009607944,0.10104828],"study_design_scores_gemma":[0.00009074969,0.00032935353,0.97978616,0.000041148414,0.000013332793,0.00015294836,0.000057038334,0.00036436404,0.00028041832,0.00039543232,0.018372929,0.00011612081],"about_ca_topic_score_codex":0.29885936,"about_ca_topic_score_gemma":0.9782155,"teacher_disagreement_score":0.67935616,"about_ca_system_score_codex":0.0000022164868,"about_ca_system_score_gemma":0.00038053675,"threshold_uncertainty_score":0.98794985},"labels":[],"label_agreement":null},{"id":"W1969679638","doi":"10.1139/e06-090","title":"Isotopic constraints on the thermal history of the Wind River Range, Wyoming: implications for Archean metamorphism","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"University of Michigan; Geological Society of America","keywords":"Geology; Hornblende; Geochemistry; Batholith; Terrane; Metamorphism; Monazite; Metamorphic rock; Archean; Gneiss; Geochronology; Biotite; Paleontology; Tectonics; Zircon","score_opus":0.036514146744098565,"score_gpt":0.19660676456209858,"score_spread":0.16009261781800002,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969679638","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97494334,0.00074818655,0.000016161079,0.009807182,0.00020360996,0.000093919814,0.000040525676,0.0000011560036,0.014145903],"genre_scores_gemma":[0.99862003,0.000002698017,0.00023832927,0.0006288409,0.0000887315,3.021487e-7,0.0000012410821,6.383674e-7,0.00041917816],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99922746,0.00006341238,0.00022403391,0.000101758684,0.00015524545,0.00022811473],"domain_scores_gemma":[0.9991475,0.00032012668,0.00019242718,0.00010294826,0.00009005349,0.00014698977],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00057700684,0.00006785581,0.00013044308,0.00008079519,0.00026732136,0.000021456231,0.0005223422,0.000028066075,0.0027788791],"category_scores_gemma":[0.00015194218,0.000030490184,0.00016866847,0.000212361,0.0019865711,0.00006588783,0.0000036541835,0.00011407087,0.000006517762],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000050246817,0.000008015383,0.9884178,0.0000024541366,0.00001809744,0.0000016224958,0.00016546481,0.0018829491,0.0003761039,0.004267943,0.0013517953,0.0035027398],"study_design_scores_gemma":[0.00008210428,0.00007533286,0.97185916,0.000008942353,0.000024265919,0.000010506904,0.00004665816,0.00019265323,0.00015937803,0.01868254,0.0088102445,0.00004824337],"about_ca_topic_score_codex":0.009833055,"about_ca_topic_score_gemma":0.08580721,"teacher_disagreement_score":0.07597415,"about_ca_system_score_codex":0.0000034921413,"about_ca_system_score_gemma":0.0006075948,"threshold_uncertainty_score":0.9981327},"labels":[],"label_agreement":null},{"id":"W1969919611","doi":"10.1139/e01-025","title":"Holocene eruptive history of Mount Baker, Washington","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Science Foundation","keywords":"Stratovolcano; Geology; Lahar; Mount; Volcano; Holocene; Scoria; Andesite; Volcanic ash; Volcanic hazards; Archaeology; Volcanic belt; Geochemistry; Radiocarbon dating; Geomorphology; Pyroclastic rock; Paleontology; Volcanic rock; Geography","score_opus":0.038775209381640974,"score_gpt":0.23814232363156357,"score_spread":0.1993671142499226,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969919611","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95588744,0.0068128807,0.000009930415,0.00064025423,0.0009031959,0.000040797433,0.000007389662,0.0000022945676,0.03569581],"genre_scores_gemma":[0.99820113,0.00017079202,0.00045709545,0.00019334821,0.000065869186,7.5586485e-8,0.0000017703821,0.0000011336897,0.00090877863],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99869514,0.00013505985,0.00029776592,0.00013896725,0.00027179025,0.00046126745],"domain_scores_gemma":[0.9988332,0.00019168018,0.0002106781,0.00009260732,0.00017126426,0.00050060736],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001380722,0.000086094995,0.00021929518,0.00046486125,0.00018909067,0.00002045952,0.0005179607,0.00008427597,0.004870929],"category_scores_gemma":[0.00023177425,0.0000662432,0.000071720206,0.0003471186,0.0016192511,0.00033362015,0.000004116491,0.00026319304,0.00008593922],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015636851,0.0000033571646,0.99764013,0.0000037013997,0.000009784282,0.0002366668,0.00041994164,0.0006233966,0.0000051546376,0.00018422051,0.00027476117,0.0005832598],"study_design_scores_gemma":[0.00016546097,0.00043014358,0.9825993,0.000026279722,0.000008198442,0.0009311378,0.0003660406,0.00039669528,0.00004018478,0.0005248134,0.014427471,0.00008425243],"about_ca_topic_score_codex":0.011659305,"about_ca_topic_score_gemma":0.23316747,"teacher_disagreement_score":0.22150816,"about_ca_system_score_codex":0.0000028091786,"about_ca_system_score_gemma":0.0028719143,"threshold_uncertainty_score":0.99603873},"labels":[],"label_agreement":null},{"id":"W1970081398","doi":"10.1139/cjes-2013-0138","title":"Gondwanan Eoarchean–Neoproterozoic ancient crustal material in Iran and Turkey: zircon U–Pb–Hf isotopic evidence","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Zircon; Geology; Protolith; Terrane; Archean; Geochemistry; Gondwana; Massif; Crust; Basement; Hadean; Paleontology; Tectonics","score_opus":0.029601798078206006,"score_gpt":0.2061062229855184,"score_spread":0.17650442490731238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970081398","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952031,0.0013955554,0.000014180211,0.0021316179,0.00025964985,0.00011450274,0.000012408761,0.00000308728,0.0008659261],"genre_scores_gemma":[0.99829465,0.000043522134,0.0010174023,0.000454736,0.0001094962,6.8646375e-7,0.0000018408554,0.0000010277048,0.00007665693],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984627,0.00009118469,0.00037231913,0.00024138314,0.00028848596,0.0005439324],"domain_scores_gemma":[0.99884766,0.00010168723,0.00013607138,0.000084806816,0.000069851165,0.0007599488],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00069877144,0.000127312,0.00024731408,0.00030760275,0.00022640238,0.00029742438,0.00040055468,0.000059225844,0.010467243],"category_scores_gemma":[0.00024196749,0.00008376653,0.000066349676,0.0005312514,0.00073005055,0.00078174553,0.000012023528,0.00019372998,0.00006699659],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007785928,0.000004901687,0.989238,0.000011051234,0.0000054536554,0.000066393106,0.0002359375,0.0005203505,0.0022271532,0.00003464771,0.00007579453,0.007572523],"study_design_scores_gemma":[0.00013100918,0.00036762643,0.9909935,0.00008059282,0.000008164514,0.000082105274,0.00035460727,0.0014030508,0.00093023607,0.004773253,0.00073130976,0.00014455199],"about_ca_topic_score_codex":0.14668156,"about_ca_topic_score_gemma":0.43503958,"teacher_disagreement_score":0.28835803,"about_ca_system_score_codex":0.0000029861033,"about_ca_system_score_gemma":0.00031041662,"threshold_uncertainty_score":0.9904373},"labels":[],"label_agreement":null},{"id":"W1970084100","doi":"10.1139/e00-071","title":"Reefs during the multiple crises towards the Ordovician-Silurian boundary: Anticosti Island, eastern Canada, and worldwide","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Ordovician; Reef; Geology; Paleontology; Gondwana; Extinction event; Carbonate platform; Bay; Interglacial; Oceanography; Facies; Population; Structural basin; Glacial period","score_opus":0.021905275230159005,"score_gpt":0.21084465393902202,"score_spread":0.18893937870886301,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970084100","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97146446,0.011074114,0.000008473501,0.0058695558,0.0007264402,0.00008051011,0.000044589022,0.0000027010692,0.0107291825],"genre_scores_gemma":[0.9989759,0.00013340698,0.00008163972,0.0004336398,0.00018275053,2.0004737e-7,4.7622277e-7,8.5434874e-7,0.00019114505],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985924,0.00012299561,0.00027856548,0.00016145942,0.0003311246,0.000513499],"domain_scores_gemma":[0.9989407,0.0002222362,0.00017487186,0.00013399411,0.000069280606,0.00045888318],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00075336866,0.00013049187,0.000172261,0.00014845743,0.0020372784,0.00036511855,0.00063146447,0.000039181163,0.00026889154],"category_scores_gemma":[0.00020130097,0.00006848796,0.000056631914,0.0004308437,0.001207414,0.00035089193,0.0000022832094,0.00027557556,0.0000027005958],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012687746,0.0000010672848,0.9815679,0.0000024347862,0.00001455802,0.0001939553,0.0003220904,0.00011351678,0.0000028995241,0.000012169484,0.00015837511,0.017598312],"study_design_scores_gemma":[0.00016286354,0.000084255626,0.97817975,0.000029659079,0.000013332394,0.0006877515,0.00084811926,0.0004258251,0.000009290373,0.00017972624,0.019278571,0.00010084274],"about_ca_topic_score_codex":0.882129,"about_ca_topic_score_gemma":0.9999023,"teacher_disagreement_score":0.1177733,"about_ca_system_score_codex":0.000002317309,"about_ca_system_score_gemma":0.0027063333,"threshold_uncertainty_score":0.9992619},"labels":[],"label_agreement":null},{"id":"W1970334388","doi":"10.1139/e05-078","title":"Buckle folding and deep-crustal shearing of high-grade gneisses at the junction of two major high-strain zones, Central Gneiss Belt, Grenville Province, Ontario","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Shear zone; Hinge; Gneiss; Fold (higher-order function); Shear (geology); Shearing (physics); Layering; Petrology; Geometry; Seismology; Metamorphic rock; Tectonics; Geotechnical engineering","score_opus":0.011252579390936567,"score_gpt":0.18275586453429632,"score_spread":0.17150328514335975,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970334388","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99643546,0.0017623948,0.000025219846,0.001247963,0.00016997578,0.00006644386,0.00002703804,0.0000034013165,0.00026208637],"genre_scores_gemma":[0.9980498,0.000032313303,0.0015388685,0.00007934677,0.0001042659,1.5192914e-7,0.0000064178985,0.0000020353104,0.00018678262],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985803,0.00005752416,0.00040919977,0.00018920361,0.0003261094,0.00043768022],"domain_scores_gemma":[0.9990077,0.00011829682,0.00029140798,0.00008575243,0.00006937559,0.00042745852],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00053438,0.00012270444,0.00027706788,0.00018177675,0.00030196758,0.000061731385,0.00030010132,0.000045041423,0.002176084],"category_scores_gemma":[0.00006973876,0.000073108284,0.00010005027,0.00039169178,0.0008067347,0.00025561737,0.000015567059,0.00017571532,0.000002751555],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015559672,0.000010857043,0.97430336,0.00001018275,0.00002920148,0.000014040118,0.00025316823,0.014603065,0.0007056289,0.0002452561,0.000030968364,0.009778733],"study_design_scores_gemma":[0.00026194722,0.00027256177,0.9934149,0.00003288431,0.000054783875,0.00008655849,0.00025248676,0.001015731,0.0014848524,0.0017236493,0.0012887679,0.00011089633],"about_ca_topic_score_codex":0.5550972,"about_ca_topic_score_gemma":0.9911917,"teacher_disagreement_score":0.4360944,"about_ca_system_score_codex":0.000009592602,"about_ca_system_score_gemma":0.0005515907,"threshold_uncertainty_score":0.9987361},"labels":[],"label_agreement":null},{"id":"W1970350244","doi":"10.1139/e05-042","title":"Geoelectric structure of the Proterozoic Wopmay Orogen and adjacent terranes, Northwest Territories, Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Manitoba","funders":"","keywords":"Terrane; Geology; Craton; Crust; Lithosphere; Subduction; Mantle (geology); Proterozoic; Seismology; Magnetotellurics; Paleontology; Geochemistry; Tectonics; Electrical resistivity and conductivity","score_opus":0.008940769209623988,"score_gpt":0.18886199356826924,"score_spread":0.17992122435864524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970350244","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955316,0.0019182601,0.0000037241193,0.0017407928,0.0004443296,0.00010335555,0.000100340214,0.0000012887906,0.00015627693],"genre_scores_gemma":[0.998557,0.000013246866,0.0007830094,0.0003297062,0.00025688426,9.6480136e-8,0.0000019060026,0.000001433513,0.000056744808],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986543,0.0001060712,0.00029231576,0.00014335556,0.00040115506,0.00040282265],"domain_scores_gemma":[0.99899554,0.00009801794,0.00020903331,0.00009624488,0.000095792704,0.00050537393],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025695693,0.000114277165,0.00020101681,0.00011140293,0.00034661297,0.000067859975,0.00047783018,0.00004075173,0.00035150576],"category_scores_gemma":[0.00014221392,0.000063916435,0.000048281814,0.00076938805,0.00033814894,0.00019213093,0.0000058746555,0.00022604743,7.483083e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000068997933,0.0000033802335,0.8785303,0.000010063029,0.000011663114,0.000010937888,0.00012809658,0.0012334763,0.00011231641,0.000034847944,0.0001222316,0.119795784],"study_design_scores_gemma":[0.00010562089,0.00024280368,0.9732267,0.000020523355,0.0000120121695,0.00011296459,0.000041197905,0.0004007544,0.0014547338,0.0003817164,0.023905737,0.00009521714],"about_ca_topic_score_codex":0.90783834,"about_ca_topic_score_gemma":0.9989616,"teacher_disagreement_score":0.119700566,"about_ca_system_score_codex":0.000005477638,"about_ca_system_score_gemma":0.003298634,"threshold_uncertainty_score":0.58516353},"labels":[],"label_agreement":null},{"id":"W1970649673","doi":"10.1139/e08-009","title":"An ornithischian dinosaur from the Sustut Basin, north-central British Columbia, Canada","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Dalhousie University","funders":"Dalhousie University","keywords":"Geology; Paleontology; Outcrop; Siltstone; Cretaceous; Phalanx; Postcrania; Archaeology; Structural basin; Anatomy; Geography; Taxon","score_opus":0.012943920923918528,"score_gpt":0.1723294892464214,"score_spread":0.1593855683225029,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970649673","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932522,0.0020612834,0.0000063711045,0.0012146236,0.0014822358,0.00005233984,0.00040166767,0.0000034719806,0.0015257642],"genre_scores_gemma":[0.9974423,0.00007881612,0.00023529938,0.0016683744,0.00038963833,1.1539518e-7,0.000031035972,0.0000012416082,0.00015319648],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984541,0.00020149015,0.0002786942,0.00019168951,0.00026118426,0.0006128258],"domain_scores_gemma":[0.998602,0.00018763679,0.00015354027,0.00011706533,0.00010032089,0.0008394381],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003287145,0.00008294592,0.0001808363,0.000042663363,0.0018904884,0.00015888042,0.0007802635,0.000063318505,0.003695737],"category_scores_gemma":[0.0001418507,0.00007702554,0.00005164441,0.0003061846,0.0014056588,0.00042319053,0.0000028424413,0.000271605,0.000013396751],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003228291,0.0000022352606,0.9884032,4.0562676e-7,0.000011059225,0.00063423114,0.0001266102,0.0004452904,4.782077e-7,0.0000021845465,0.008695978,0.0016750743],"study_design_scores_gemma":[0.00011840126,0.0001610276,0.9615447,0.000009325686,0.000008115612,0.0013784005,0.00030977544,0.00015579283,5.233456e-7,0.00009394293,0.03611213,0.00010786305],"about_ca_topic_score_codex":0.99835336,"about_ca_topic_score_gemma":0.9999985,"teacher_disagreement_score":0.02741615,"about_ca_system_score_codex":0.0000053029644,"about_ca_system_score_gemma":0.009443179,"threshold_uncertainty_score":0.9994089},"labels":[],"label_agreement":null},{"id":"W1970657823","doi":"10.1139/e07-030","title":"Sulfide saturation mechanisms in gabbroic intrusions in the Nipigon Embayment","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geoscience BC; Lakehead University","funders":"Lakehead University; University of Calgary","keywords":"Geology; Platinum group; Geochemistry; Sulfur; Sulfide; Mafic; Layered intrusion; Saturation (graph theory); Ultramafic rock; Platinum; Chemistry","score_opus":0.016878652717342516,"score_gpt":0.20775466786651625,"score_spread":0.19087601514917374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970657823","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928128,0.0004671967,0.0001014313,0.0027940792,0.00015921185,0.000049329763,0.0000030918716,0.0000010739902,0.0036117435],"genre_scores_gemma":[0.9984011,0.000016352342,0.00074913044,0.0007604858,0.000050500945,9.377477e-8,0.0000025170964,3.8195404e-7,0.00001941878],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988314,0.0000756113,0.00032607623,0.00011362342,0.00029021455,0.0003630961],"domain_scores_gemma":[0.9993552,0.00019517928,0.0001006831,0.000057438472,0.000037439517,0.00025406573],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002442109,0.000068121684,0.00012171475,0.00037757424,0.00017447027,0.00008104651,0.00039150633,0.00003902231,0.0018947911],"category_scores_gemma":[0.00021083388,0.00003680685,0.000052497493,0.0010733826,0.00018575267,0.00019061394,0.000003203889,0.00020908579,0.000023186769],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008946022,0.0000088579145,0.9863258,0.0000014303881,0.0000030056156,0.00018442378,0.00050158816,0.003963424,0.00030716494,0.0013022381,0.000038448074,0.0073546637],"study_design_scores_gemma":[0.000089876725,0.00014160381,0.968841,0.000016345872,0.0000044252324,0.000047920832,0.0010521831,0.0007290642,0.0003314054,0.028062593,0.0006219086,0.00006167614],"about_ca_topic_score_codex":0.043529965,"about_ca_topic_score_gemma":0.92566717,"teacher_disagreement_score":0.8821372,"about_ca_system_score_codex":0.0000025731572,"about_ca_system_score_gemma":0.0002440668,"threshold_uncertainty_score":0.9990176},"labels":[],"label_agreement":null},{"id":"W1970722600","doi":"10.1139/e09-061","title":"Subduction zone recycling processes and the rock record of crustal suture zonesThis article is one of a series of papers published in this Special Issue on the theme <i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Országos Meteorológiai Szolgálat","keywords":"Geology; Subduction; Forearc; Terrane; Fibrous joint; Underplating; Oceanic crust; Seismology; Tectonics; Basement","score_opus":0.00935247648707703,"score_gpt":0.17617727943521974,"score_spread":0.16682480294814273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970722600","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9854733,0.0011288901,0.0000040780847,0.012121668,0.000100155536,0.00013987687,0.00001862119,9.1802565e-7,0.0010125007],"genre_scores_gemma":[0.9992187,0.00019680081,0.00030168472,0.00009696439,0.0001219818,7.0496696e-7,6.9684734e-7,9.2676436e-7,0.000061560044],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987523,0.000118976284,0.00048167122,0.00014211381,0.00032112116,0.0001838384],"domain_scores_gemma":[0.9982563,0.00055715576,0.000649808,0.000098163626,0.00033420222,0.00010435797],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001686624,0.00009011458,0.00033285804,0.00012576059,0.00016763038,0.00005683028,0.00029255814,0.000054422107,0.0023546482],"category_scores_gemma":[0.0020805348,0.00003867711,0.000061917905,0.0009885991,0.0020578222,0.0003093873,0.000009821228,0.00023841579,3.9788435e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011054816,0.000053288284,0.98368335,0.00020536016,0.00007369747,0.0000032845394,0.0063925404,0.0005160495,0.0017513424,0.0012877468,0.00019529818,0.00473257],"study_design_scores_gemma":[0.0043298006,0.002541166,0.82755536,0.00086525467,0.00039865167,0.00021655214,0.033276338,0.003410027,0.055911105,0.066152126,0.004818484,0.00052513287],"about_ca_topic_score_codex":0.041346673,"about_ca_topic_score_gemma":0.3937082,"teacher_disagreement_score":0.3523615,"about_ca_system_score_codex":0.0000011946258,"about_ca_system_score_gemma":0.00040734542,"threshold_uncertainty_score":0.9985573},"labels":[],"label_agreement":null},{"id":"W1970930119","doi":"10.1139/e08-048","title":"Ordovician and Silurian nautiloid cephalopods from Anticosti Island: traject across the Ordovician–Silurian (O–S) mass extinction boundary","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Ordovician; Paleontology; Geology; Fauna; Extinction event; Baltica; Gondwana; Ecology; Tectonics; Population","score_opus":0.019789134934642832,"score_gpt":0.22879610598828945,"score_spread":0.20900697105364663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970930119","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9707625,0.014474168,0.000083827705,0.0020456158,0.0012978263,0.00011361906,0.00019500477,0.000009647431,0.011017774],"genre_scores_gemma":[0.9980068,0.00027497753,0.0009111328,0.00038338802,0.00036789008,3.0059118e-7,0.000005021868,0.0000018342721,0.000048627662],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979084,0.00020679689,0.00046021945,0.00030695542,0.00038939837,0.0007282364],"domain_scores_gemma":[0.9984543,0.00027184733,0.00029672153,0.00017175433,0.00009113103,0.0007142829],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0010750606,0.00021504295,0.00031984315,0.00024495792,0.0032149283,0.00034998864,0.00061829755,0.00013644148,0.00062756747],"category_scores_gemma":[0.0001426116,0.00014325742,0.00012607747,0.0006032553,0.0025372338,0.0007771514,0.0000020843186,0.00044144207,0.000015413507],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025983034,0.0000046881646,0.9653744,0.0000025877714,0.000030770112,0.00028036672,0.0019361868,0.00007503714,0.000048731803,0.000016420428,0.00010610657,0.03209873],"study_design_scores_gemma":[0.00032844688,0.00038286397,0.9810908,0.000032119475,0.000021747233,0.00071742147,0.0014022702,0.0004463024,0.000034774377,0.0012679767,0.014085912,0.0001894012],"about_ca_topic_score_codex":0.03553582,"about_ca_topic_score_gemma":0.9202926,"teacher_disagreement_score":0.8847568,"about_ca_system_score_codex":0.0000024538126,"about_ca_system_score_gemma":0.0014502933,"threshold_uncertainty_score":0.99808276},"labels":[],"label_agreement":null},{"id":"W1971148296","doi":"10.1139/e01-089","title":"Evidence for reversal of basin polarity during carbonate ramp development in the Mesoproterozoic Borden Basin, Baffin Island","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"","keywords":"Geology; Unconformity; Paleontology; Foreland basin; Structural basin; Facies; Carbonate platform; Craton; Carbonate; Reef; Geomorphology; Tectonics; Oceanography","score_opus":0.058530637271825066,"score_gpt":0.24327503248093427,"score_spread":0.1847443952091092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971148296","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98461616,0.010377335,0.000016705879,0.0012455067,0.00022271728,0.00016357205,0.00002213576,0.0000013838556,0.0033344738],"genre_scores_gemma":[0.99803853,0.000063921754,0.00172936,0.000093754374,0.000048968785,6.0888834e-7,3.4080753e-7,5.2624847e-7,0.000024007844],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99860173,0.00015821985,0.0003954329,0.00015471694,0.00029501462,0.00039486197],"domain_scores_gemma":[0.9990674,0.00033066867,0.00022321274,0.00009306084,0.00007433254,0.00021128284],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020022106,0.00010268274,0.000212206,0.0003189306,0.00041428403,0.00008547978,0.00060978445,0.000060718732,0.00025404047],"category_scores_gemma":[0.00035518207,0.000069170695,0.00007756528,0.00043355094,0.00046711284,0.00044236536,0.0000010766611,0.0001935312,0.0000016639636],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018812987,0.000004558845,0.9883275,0.000016170383,0.000009538914,0.00004799739,0.0017434156,0.00010840215,0.000023175526,0.000021575981,0.000057447425,0.00962141],"study_design_scores_gemma":[0.00023863511,0.00018422655,0.99766237,0.00014411501,0.000007657245,0.00010415184,0.0002996508,0.0003369102,0.00019866902,0.0001670718,0.00056803704,0.0000885245],"about_ca_topic_score_codex":0.015579212,"about_ca_topic_score_gemma":0.7613033,"teacher_disagreement_score":0.7457241,"about_ca_system_score_codex":0.0000023138539,"about_ca_system_score_gemma":0.0007061734,"threshold_uncertainty_score":0.99097615},"labels":[],"label_agreement":null},{"id":"W1971196657","doi":"10.1139/cjes-2013-0010","title":"New Early Triassic coelacanth in the family Laugiidae (Sarcopterygii: Actinistia) from the Sulphur Mountain Formation near Wapiti Lake, British Columbia, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta; City University of New York","keywords":"Paleontology; Geology; Supercontinent; Pangaea; Biostratigraphy; Permian","score_opus":0.016979332311053943,"score_gpt":0.18598655620183635,"score_spread":0.1690072238907824,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971196657","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98911864,0.0026636182,0.000020946994,0.004474782,0.00076028024,0.00017102594,0.00020023446,0.000002509599,0.0025879927],"genre_scores_gemma":[0.99708515,0.00005972994,0.0002743722,0.0021711336,0.0002093585,8.570487e-7,0.00002406994,0.0000013031363,0.0001740321],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982649,0.00036117854,0.0003826694,0.00015702657,0.00032055305,0.00051369186],"domain_scores_gemma":[0.998609,0.000610472,0.00022524335,0.000117553674,0.000078875666,0.00035887133],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010032735,0.00009137477,0.00019112429,0.000053082225,0.0009916076,0.00074297265,0.00086546317,0.00008072433,0.003288494],"category_scores_gemma":[0.00019867849,0.000071314484,0.000050077262,0.00041517292,0.00062210317,0.00077318295,0.0000045460115,0.00035240297,0.000049297512],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000062892013,0.0000018196563,0.95869356,9.1520513e-7,0.00000732922,0.00008313135,0.00042540702,0.00016903918,0.0000012120992,0.000008138195,0.022086423,0.018516762],"study_design_scores_gemma":[0.00024660406,0.00018889972,0.95363843,0.000027392995,0.000007430094,0.00023263978,0.0016891042,0.0004671398,3.939672e-7,0.0006942735,0.042713113,0.00009459789],"about_ca_topic_score_codex":0.9984621,"about_ca_topic_score_gemma":0.9999928,"teacher_disagreement_score":0.02062669,"about_ca_system_score_codex":0.0000073112583,"about_ca_system_score_gemma":0.0053545428,"threshold_uncertainty_score":0.9976226},"labels":[],"label_agreement":null},{"id":"W1971311087","doi":"10.1139/e10-063","title":"The heterodonty of<i>Albertosaurus sarcophagus</i>and<i>Tyrannosaurus rex</i>: biomechanical implications inferred through 3-D modelsThis article is one of a series of papers published in this Special Issue on the theme<i>Albertosaurus</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Anatomy; Crown (dentistry); Biomechanics; Biology; Geology; Orthodontics; Medicine","score_opus":0.02193680576325857,"score_gpt":0.2238215522960946,"score_spread":0.20188474653283603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971311087","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9578324,0.0009829844,0.0000041769604,0.023759857,0.0007434726,0.00016896597,0.0001532628,0.000002366842,0.016352538],"genre_scores_gemma":[0.9984779,0.00020847854,0.00042835445,0.0005418996,0.00025500695,0.0000012096056,0.0000028314905,0.0000022074648,0.00008215252],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981532,0.00021103527,0.0006954043,0.00022387951,0.00028690504,0.0004295748],"domain_scores_gemma":[0.99800247,0.00085193955,0.00046870517,0.00029037558,0.00016982082,0.0002166917],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001449236,0.00014313923,0.00034946736,0.00019744282,0.0004791914,0.00004882144,0.00079672196,0.00014935347,0.0038679333],"category_scores_gemma":[0.00068459555,0.00008252525,0.000110368455,0.00072976673,0.0029551145,0.00051087997,0.000016268097,0.0004207598,0.000007073542],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005150209,0.000115299634,0.92130715,0.00002951339,0.00014442293,0.000019075176,0.006752201,0.00043487144,0.018725375,0.035179053,0.004195352,0.012582674],"study_design_scores_gemma":[0.00061422744,0.0012916876,0.9209073,0.00007915699,0.00003952776,0.0002659599,0.0008667072,0.00073264865,0.010580261,0.0315481,0.03282796,0.00024647324],"about_ca_topic_score_codex":0.018825099,"about_ca_topic_score_gemma":0.5475898,"teacher_disagreement_score":0.52876467,"about_ca_system_score_codex":0.0000023480436,"about_ca_system_score_gemma":0.0007876692,"threshold_uncertainty_score":0.99975824},"labels":[],"label_agreement":null},{"id":"W1971363449","doi":"10.1139/e09-073","title":"Paleoproterozoic subduction in northwestern Canada from near-vertical and wide-angle seismic reflection data","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Subduction; Terrane; Seismology; Slab; Lithosphere; Crust; Oceanic crust; Reflection (computer programming); Magnetic dip; Geophysics; Tectonics","score_opus":0.022942997620218977,"score_gpt":0.20569330625319407,"score_spread":0.1827503086329751,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971363449","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99708223,0.00028287017,0.000011250589,0.0017706206,0.0004614059,0.000034041866,0.000056349105,0.000001787228,0.0002994242],"genre_scores_gemma":[0.999158,0.000009521491,0.00038071812,0.00031794852,0.00008791322,8.393441e-8,0.000024654912,7.444098e-7,0.000020410718],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989484,0.000049371614,0.00024898152,0.00022593429,0.00024112672,0.00028621667],"domain_scores_gemma":[0.99912226,0.0001320291,0.00006840316,0.0001298769,0.00004379259,0.0005036394],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047285712,0.00008426463,0.00016312343,0.00010231542,0.00022777705,0.00014736921,0.00038621496,0.00005167846,0.0019271172],"category_scores_gemma":[0.0002357409,0.00005811177,0.000022139891,0.00035232853,0.00038042365,0.0003924447,0.0000104253995,0.00031080403,0.00000832434],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005939865,0.0000015853716,0.99554163,0.0000011058584,0.000004423541,0.000047963294,0.000033209788,0.00043002955,0.000101622965,0.0000012280688,0.000042916232,0.0037883527],"study_design_scores_gemma":[0.00010261092,0.00010055776,0.9842967,0.000008336328,0.000012188485,0.00005885911,0.00007281066,0.011117239,0.00014865828,0.00092321954,0.003075971,0.000082873965],"about_ca_topic_score_codex":0.9814145,"about_ca_topic_score_gemma":0.9999435,"teacher_disagreement_score":0.018529033,"about_ca_system_score_codex":0.0000018126597,"about_ca_system_score_gemma":0.0009855275,"threshold_uncertainty_score":0.99898523},"labels":[],"label_agreement":null},{"id":"W1971429812","doi":"10.1139/e02-042","title":"Development of a folded thrust stack: Humber Arm Allochthon, Bay of Islands, Newfoundland Appalachians","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University; University of Alberta","funders":"Memorial University of Newfoundland","keywords":"Geology; Allochthon; Foreland basin; Nappe; Paleontology; Fold (higher-order function); Clastic rock; Sedimentary rock; Thrust fault; Imbrication; Lineation; Outcrop; Continental margin; Geomorphology; Tectonics","score_opus":0.026409962372619396,"score_gpt":0.2197080546276261,"score_spread":0.19329809225500671,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971429812","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95476276,0.00097098,0.00028860607,0.000092681265,0.00025438736,0.00005842168,0.000023553592,0.0000017750991,0.043546844],"genre_scores_gemma":[0.98758763,0.000029405808,0.012175645,0.00006350173,0.000020220661,1.1778364e-7,0.0000033526937,0.0000010290024,0.00011912228],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987341,0.00005122846,0.00050130795,0.00010172951,0.00030924412,0.00030235655],"domain_scores_gemma":[0.9989867,0.00008732789,0.00032303244,0.000070884314,0.00018605456,0.00034598843],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010342378,0.0000940124,0.0002198786,0.00024536077,0.000291317,0.00005968184,0.00030708525,0.000045823046,0.0049259583],"category_scores_gemma":[0.00016585407,0.00006282699,0.000056284778,0.00051914505,0.00035464996,0.00030862805,0.000002645254,0.000100220095,0.000014897945],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000055162573,0.0000106043635,0.9936329,0.00002165642,0.000015472604,0.0000067892684,0.0014230162,0.0014366244,0.000014835896,0.0006019922,0.00006353855,0.0027670264],"study_design_scores_gemma":[0.00034560644,0.0004928273,0.9436203,0.00008946963,0.000017394232,0.00012516063,0.002268175,0.00019843513,0.00055397366,0.0018864832,0.05021594,0.00018618611],"about_ca_topic_score_codex":0.00244774,"about_ca_topic_score_gemma":0.43239307,"teacher_disagreement_score":0.42994535,"about_ca_system_score_codex":0.0000014572284,"about_ca_system_score_gemma":0.002206225,"threshold_uncertainty_score":0.99598366},"labels":[],"label_agreement":null},{"id":"W1971581262","doi":"10.1139/e04-101","title":"Structural controls on hypozonal orogenic gold mineralization in the La Ronge Domain, Trans-Hudson Orogen, Saskatchewan","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Laurentian University","funders":"National Science Council","keywords":"Geology; Lineation; Craton; Geochemistry; Archean; Subduction; Shear zone; Lithosphere; Greenstone belt; Seismology; Tectonics","score_opus":0.014044474288620178,"score_gpt":0.1953617663384201,"score_spread":0.1813172920497999,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971581262","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920935,0.0008142952,0.000019175992,0.0040395986,0.000104294726,0.00006875609,0.00002514819,0.0000023708849,0.0028328635],"genre_scores_gemma":[0.99827635,0.0000111249765,0.0004453762,0.0011330137,0.0001001094,2.7622727e-7,0.000008040421,0.0000010132928,0.000024674337],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985623,0.00015200839,0.00031905936,0.00016796672,0.00040622376,0.00039247962],"domain_scores_gemma":[0.9992362,0.0001637994,0.000123219,0.000076166936,0.000058395617,0.00034221582],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00089021726,0.0001224912,0.00019890345,0.00019448089,0.0002124658,0.00015463696,0.00052466383,0.000060465496,0.0015188567],"category_scores_gemma":[0.0000913801,0.00006534104,0.00013087991,0.00071753305,0.0004599371,0.00022204177,0.0000017266177,0.00024365359,0.000017907274],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004659469,0.00001681125,0.90847576,0.000005554207,0.00003109256,0.0003316623,0.002412209,0.08020632,0.00034777797,0.0025923573,0.00006586421,0.005468019],"study_design_scores_gemma":[0.00069455255,0.00053634105,0.9549175,0.0000308311,0.000022713415,0.00024018207,0.0021620314,0.0004074757,0.00014397569,0.03874648,0.0019270169,0.00017089922],"about_ca_topic_score_codex":0.034880586,"about_ca_topic_score_gemma":0.88323796,"teacher_disagreement_score":0.8483574,"about_ca_system_score_codex":0.000003334867,"about_ca_system_score_gemma":0.0006597036,"threshold_uncertainty_score":0.9993939},"labels":[],"label_agreement":null},{"id":"W1971877512","doi":"10.1139/e04-075","title":"Early and Middle Proterozoic evolution of Yukon, Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":91,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of British Columbia; Yukon University; University of Alberta; Simon Fraser University","funders":"","keywords":"Geology; Proterozoic; Breccia; Orogeny; Geochemistry; Zircon; Volcanic rock; Laurentia; Paleontology; Paleozoic; Volcano; Tectonics","score_opus":0.013279771847119702,"score_gpt":0.16254544538643825,"score_spread":0.14926567353931855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971877512","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943433,0.002184671,0.000010953162,0.0012606457,0.00007615494,0.0000313578,0.000016630016,9.3349354e-7,0.0020753916],"genre_scores_gemma":[0.9989579,0.00000884481,0.00076505577,0.00012337911,0.00007045048,5.690801e-8,6.628588e-7,4.1276235e-7,0.00007326216],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991442,0.000029953879,0.00024302909,0.00010002592,0.00023692902,0.00024584396],"domain_scores_gemma":[0.99919826,0.00004651693,0.00014618333,0.00004407308,0.00009937021,0.0004656095],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003291414,0.00006221282,0.0001447211,0.00012635015,0.0001564772,0.000035538644,0.0002111023,0.000025603262,0.0017552503],"category_scores_gemma":[0.00010523947,0.000041308012,0.000037301863,0.00034982755,0.00035499764,0.00020374384,0.000003021816,0.00008938005,0.0000055475994],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000030950255,0.0000016686012,0.9951696,0.0000040457535,0.00000637763,0.000009046186,0.000045785582,0.0015312355,0.000048411184,0.00008747697,0.000044588814,0.0030486926],"study_design_scores_gemma":[0.00007356576,0.00016228201,0.99401915,0.000021736672,0.0000095834885,0.000036732363,0.00010136642,0.0011973409,0.00022209554,0.0017035017,0.0023893875,0.0000632392],"about_ca_topic_score_codex":0.92169774,"about_ca_topic_score_gemma":0.9981774,"teacher_disagreement_score":0.07647963,"about_ca_system_score_codex":0.0000027657486,"about_ca_system_score_gemma":0.0012666112,"threshold_uncertainty_score":0.9991573},"labels":[],"label_agreement":null},{"id":"W1971912724","doi":"10.1139/e09-054","title":"Magmatic affinity of modern and ancient subalkaline volcanic rocks determined from trace-element discriminant diagrams","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":423,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique; Geological Survey of Canada","funders":"","keywords":"Trace element; Geology; Volcano; Diagram; Volcanic rock; Geochemistry; Mineralogy; Mathematics; Statistics","score_opus":0.019854427561764504,"score_gpt":0.20507089847340212,"score_spread":0.18521647091163762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971912724","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935863,0.0044746837,0.00016549954,0.0011356882,0.000092783295,0.00005086343,0.000055676166,0.0000021975568,0.0004363049],"genre_scores_gemma":[0.998685,0.000058234997,0.000944747,0.00023094412,0.000051276307,8.792371e-8,0.0000049736923,6.42625e-7,0.000024106375],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986506,0.000053351912,0.00042658858,0.00018448943,0.0003193764,0.00036557327],"domain_scores_gemma":[0.99879295,0.0001114311,0.00024601075,0.000089850124,0.0000842769,0.0006754847],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005060951,0.00011812343,0.00030004926,0.00015396296,0.00018912516,0.00007524577,0.00033093736,0.000038639322,0.0018154506],"category_scores_gemma":[0.00016819232,0.000073440795,0.00010144104,0.0003430326,0.00034285444,0.00019748235,0.0000052895634,0.000116813004,0.000005428387],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017873253,0.000027302978,0.91430426,0.0000069995954,0.000018197685,0.00006844669,0.0005051531,0.0041752257,0.0009779611,0.000025455014,0.000044330056,0.07982879],"study_design_scores_gemma":[0.00017554521,0.0005881402,0.9661598,0.00003598034,0.00004665014,0.000023971219,0.0002599089,0.017637456,0.00069770153,0.014065306,0.00019337767,0.000116145464],"about_ca_topic_score_codex":0.021875298,"about_ca_topic_score_gemma":0.6348894,"teacher_disagreement_score":0.6130141,"about_ca_system_score_codex":0.0000016165035,"about_ca_system_score_gemma":0.00026578593,"threshold_uncertainty_score":0.99909705},"labels":[],"label_agreement":null},{"id":"W1971985935","doi":"10.1139/e03-100","title":"Paleogeography of the Matapédia basin in the Gaspé Appalachians: initiation of the Gaspé Belt successor basin","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"GDG Environnement; Institut National de la Recherche Scientifique","funders":"","keywords":"Siliciclastic; Geology; Ordovician; Facies; Basement; Paleontology; Geochemistry; Structural basin; Group (periodic table); Carbonate platform","score_opus":0.016308818092817937,"score_gpt":0.20794514037354447,"score_spread":0.19163632228072652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971985935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96800125,0.00044379183,0.00048834895,0.02446282,0.0004419069,0.0001428636,0.0000088699535,0.0000023363764,0.0060078204],"genre_scores_gemma":[0.9982954,0.000015441181,0.0007390934,0.000892607,0.00004052998,0.0000011704698,1.9761912e-7,9.66916e-7,0.000014584096],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99844164,0.00020614699,0.00041907863,0.0001522877,0.0004725722,0.00030825945],"domain_scores_gemma":[0.9987248,0.00013576848,0.0004949592,0.00035833844,0.00017435504,0.00011174866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020390865,0.000098196346,0.00016168786,0.00019431813,0.00035576703,0.000113594455,0.0026489282,0.000047687987,0.000027137858],"category_scores_gemma":[0.00040563336,0.00004951162,0.00014949293,0.0018459958,0.00080337253,0.00036960875,0.00005360216,0.00024673768,7.090603e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000024644512,0.00003324324,0.9739991,0.00002621608,0.000009841511,0.00002010086,0.0040130108,0.007170942,0.0004870401,0.0132852625,0.00016208403,0.00079071027],"study_design_scores_gemma":[0.00023139287,0.000078495235,0.97952884,0.00023316417,0.000005788013,0.00011916045,0.0009766727,0.00023034132,0.0041057216,0.011722667,0.0026836009,0.00008415259],"about_ca_topic_score_codex":0.0042245984,"about_ca_topic_score_gemma":0.045851428,"teacher_disagreement_score":0.04162683,"about_ca_system_score_codex":0.0000069359107,"about_ca_system_score_gemma":0.0013922134,"threshold_uncertainty_score":0.9715593},"labels":[],"label_agreement":null},{"id":"W1972040449","doi":"10.1139/e05-054","title":"Lower Ordovician trilobites from the Baumann Fiord Formation, Ellesmere Island, Arctic Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Trilobite; Macrofossil; Geology; Paleontology; Arctic; Peninsula; Ordovician; Fauna; Range (aeronautics); Fjord; Oceanography; Geography; Ecology; Archaeology; Biology; Holocene","score_opus":0.013975162693181479,"score_gpt":0.19452831622942274,"score_spread":0.18055315353624127,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972040449","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9590402,0.009335275,0.00002111959,0.010650371,0.0008472434,0.00007154714,0.00019124946,0.0000028622533,0.019840097],"genre_scores_gemma":[0.99756426,0.00004401942,0.0003188226,0.0016796811,0.00032885757,1.3203791e-7,0.0000041501253,5.6366633e-7,0.000059500693],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987229,0.00009396974,0.00033971845,0.00012455814,0.00031126698,0.00040758334],"domain_scores_gemma":[0.9988191,0.00030560835,0.00021300919,0.00011184216,0.00010057421,0.00044984845],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000522668,0.00011371939,0.00016131443,0.00011626705,0.0009450968,0.00016622533,0.0006212503,0.00004938727,0.0020694686],"category_scores_gemma":[0.00013301415,0.00006994667,0.000073965595,0.00034432203,0.00046422225,0.0006221627,7.8628943e-7,0.00023415394,0.000015594607],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009764202,0.0000021831731,0.95665884,0.0000012487967,0.000018204199,0.000049074682,0.00038320824,0.00074148754,0.0000014212656,0.00005580655,0.0056435373,0.03643522],"study_design_scores_gemma":[0.00014618141,0.00010564332,0.93408006,0.000028832439,0.000012782818,0.00007998851,0.0005639472,0.00058519555,0.000014434976,0.00027768564,0.06400584,0.000099437006],"about_ca_topic_score_codex":0.838188,"about_ca_topic_score_gemma":0.9999473,"teacher_disagreement_score":0.1617593,"about_ca_system_score_codex":0.0000034817012,"about_ca_system_score_gemma":0.0030083153,"threshold_uncertainty_score":0.9988428},"labels":[],"label_agreement":null},{"id":"W1972259187","doi":"10.1139/e09-012","title":"Evaluating debris slide occurrence using digital data: paraglacial activity in Chilliwack Valley, British Columbia","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; University of Calgary","funders":"","keywords":"Geology; Debris; Landslide; Bedrock; Digital elevation model; Geomorphology; Structural basin; Erosion; Elevation (ballistics); Sediment; Remote sensing; Oceanography","score_opus":0.05316314443830283,"score_gpt":0.29419838414842625,"score_spread":0.24103523971012342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972259187","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99751043,0.00017966924,0.00004720006,0.00014936489,0.0003081702,0.000077710116,0.00006951353,0.000003051019,0.0016548692],"genre_scores_gemma":[0.9988456,0.000023442022,0.0008849261,0.00010433859,0.00007527583,1.1974944e-7,0.0000020772318,0.000002641033,0.00006160815],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983815,0.000056517565,0.00031168875,0.00028589927,0.000481176,0.00048320764],"domain_scores_gemma":[0.99910843,0.00003945818,0.00021551707,0.00015424743,0.000021663476,0.00046068814],"candidate_categories":["scholarly_communication"],"consensus_categories":[],"category_scores_codex":[0.0011974659,0.000085043735,0.00018763104,0.00006954231,0.0004734372,0.0010650731,0.00073566916,0.000062252926,0.0006938309],"category_scores_gemma":[0.00030163833,0.00009434404,0.000049933595,0.00060370535,0.000424428,0.0017681448,0.000055364635,0.00027091068,0.000011964482],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000048280276,0.000023945504,0.8883565,0.0000014481225,0.0000048005127,0.00025991796,0.00015401188,0.011099246,0.00018279943,8.143248e-7,0.0007016239,0.09921008],"study_design_scores_gemma":[0.0003544728,0.00029503956,0.9783672,0.00013209136,0.0000127993,0.00060157187,0.0000975658,0.01752147,0.000017866458,0.00036696944,0.0020164708,0.00021645261],"about_ca_topic_score_codex":0.08739993,"about_ca_topic_score_gemma":0.69359976,"teacher_disagreement_score":0.60619986,"about_ca_system_score_codex":0.000044271324,"about_ca_system_score_gemma":0.0007807637,"threshold_uncertainty_score":0.9999719},"labels":[],"label_agreement":null},{"id":"W1972376274","doi":"10.1139/e10-002","title":"Models of large, hot orogens containing a collage of reworked and accreted terranesThis article is one of a series of papers published in this Special Issue on the theme<i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Orogeny; Terrane; Crust; Diachronous; Tectonics; Paleontology; Earth science","score_opus":0.012954205343682697,"score_gpt":0.1948832386383253,"score_spread":0.1819290332946426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972376274","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997003,0.00037449057,0.0000023486618,0.0009345986,0.00012118899,0.00019758241,0.00013610875,6.969689e-7,0.0012299771],"genre_scores_gemma":[0.9994935,0.000053429023,0.00032728395,0.000048814687,0.000053882133,5.7989826e-7,8.3629806e-7,0.0000016866851,0.000020021764],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987413,0.00012261646,0.00051718147,0.00011663009,0.00030555783,0.00019669336],"domain_scores_gemma":[0.99855214,0.00030084624,0.00066171447,0.000120616394,0.00025730536,0.00010739749],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019747938,0.00008593878,0.00039779235,0.00015208939,0.00010197357,0.000049814666,0.00027389266,0.00004971864,0.0009923683],"category_scores_gemma":[0.00041246938,0.00004841449,0.00004224464,0.00049730507,0.001253391,0.00034789363,0.0000099441695,0.000105206105,1.2489548e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0053709554,0.00021086741,0.7280664,0.0010577462,0.00044999612,0.00003187434,0.114004485,0.0029588868,0.116939224,0.02704749,0.0007576755,0.003104432],"study_design_scores_gemma":[0.007274815,0.0052958676,0.7023924,0.0020925612,0.00035856644,0.00011837373,0.035353135,0.006819015,0.21309339,0.023142265,0.0033895036,0.00067012705],"about_ca_topic_score_codex":0.02315932,"about_ca_topic_score_gemma":0.14510821,"teacher_disagreement_score":0.12194888,"about_ca_system_score_codex":9.919135e-7,"about_ca_system_score_gemma":0.0006749351,"threshold_uncertainty_score":0.99992085},"labels":[],"label_agreement":null},{"id":"W1972752914","doi":"10.1139/cjes-2013-0032","title":"Use of surficial geochemical methods to locate areas of buried uranium mineralization in the Jacque’s Lake area of the Central Mineral Belt, Labrador, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Nalcor Energy (Canada); College of the North Atlantic; Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Bedrock; Geochemistry; Mineralization (soil science); Eluvium; Humus; Uranium; Biogeochemical cycle; Bog; Peat; Soil water; Environmental chemistry; Weathering; Soil science; Geomorphology; Chemistry; Ecology","score_opus":0.0355574037819834,"score_gpt":0.23452695402622004,"score_spread":0.19896955024423663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972752914","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9872539,0.00006286046,0.0014917463,0.01036707,0.0003098444,0.00012195926,0.000011874903,9.969187e-7,0.00037974576],"genre_scores_gemma":[0.9942722,0.0000012487786,0.0051455316,0.00044078502,0.000039284365,9.5241296e-7,8.7773367e-7,0.0000010056998,0.000098143086],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99847966,0.00019724821,0.00047992155,0.00013833558,0.00036944504,0.00033540247],"domain_scores_gemma":[0.998602,0.00020131953,0.00034919695,0.0002256317,0.00040456085,0.00021728841],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00087608385,0.00009519812,0.0002183833,0.000114936105,0.00008844495,0.00006184282,0.0012265064,0.000043005966,0.00005567923],"category_scores_gemma":[0.0007749191,0.000057275778,0.00006501491,0.0010154183,0.00031386074,0.00026376088,0.000043712942,0.00012220288,9.396712e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021915386,0.00008295958,0.823446,0.00009751428,0.000049706367,0.000054850323,0.008032056,0.06930528,0.07038415,0.00746863,0.016647259,0.004409726],"study_design_scores_gemma":[0.00025997713,0.00014193411,0.92391384,0.00019337567,0.000014822027,0.00011057896,0.0006911118,0.011095651,0.052084073,0.0012611016,0.010027284,0.000206263],"about_ca_topic_score_codex":0.63701874,"about_ca_topic_score_gemma":0.9572544,"teacher_disagreement_score":0.32023567,"about_ca_system_score_codex":0.00001108918,"about_ca_system_score_gemma":0.0024456393,"threshold_uncertainty_score":0.4338459},"labels":[],"label_agreement":null},{"id":"W1972818400","doi":"10.1139/e00-115","title":"A new genus of ichthyosaur from the Late Triassic Pardonet Formation of British Columbia: bridging the Triassic Jurassic gap","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Nomen dubium; Paleontology; Genus; Type species; Geology; Type (biology); Skull; Ridge; Taxon; Biology; Zoology","score_opus":0.028604888131361084,"score_gpt":0.2081454410298865,"score_spread":0.1795405528985254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972818400","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9879563,0.0072503337,0.00020914893,0.0021738245,0.000763199,0.00009939606,0.0001438338,0.000002418336,0.001401589],"genre_scores_gemma":[0.99870366,0.00026139428,0.00022232036,0.00024028304,0.00025375848,2.0775863e-7,0.000008454921,0.0000010950857,0.0003088263],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99853456,0.00027202972,0.0005030567,0.00010855505,0.00024223365,0.0003395694],"domain_scores_gemma":[0.99854654,0.0004561069,0.00054731447,0.000117175885,0.00009180652,0.00024106032],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013537528,0.0000712102,0.00025056244,0.00008158107,0.00045785328,0.0000938247,0.00062196516,0.0000734743,0.0011403626],"category_scores_gemma":[0.00019112985,0.000054447046,0.000109832254,0.0005114559,0.0008317104,0.00042504416,0.0000050060767,0.00019577074,0.000011553064],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026487103,0.0000030589792,0.93631196,0.0000021486437,0.000025131492,0.00003592703,0.00033287253,0.0010046449,0.000019481527,0.0000096778995,0.0067391,0.055489536],"study_design_scores_gemma":[0.000381095,0.00021975962,0.98849434,0.00005487371,0.000032923508,0.00041799556,0.00049939577,0.0016230352,0.0000063098173,0.0013509057,0.0068520103,0.000067346366],"about_ca_topic_score_codex":0.36725283,"about_ca_topic_score_gemma":0.97668576,"teacher_disagreement_score":0.60943294,"about_ca_system_score_codex":0.0000025660595,"about_ca_system_score_gemma":0.0013772137,"threshold_uncertainty_score":0.9997727},"labels":[],"label_agreement":null},{"id":"W1973041579","doi":"10.1139/e04-062","title":"Eocene paleo-physiography and drainage directions, southern Interior Plateau, British Columbia","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"BGC Engineering (Canada)","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Simon Fraser University; Canadian Natural Resources Limited","keywords":"Geology; Plateau (mathematics); Cenozoic; Fluvial; Unconformity; Landform; Paleontology; Bedrock; Geomorphology; Quaternary; Colorado plateau; Structural basin; Geochemistry","score_opus":0.011882104258052192,"score_gpt":0.20936558945898207,"score_spread":0.19748348520092987,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973041579","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9850385,0.005576463,0.0000039454217,0.00077464984,0.00029299353,0.000055653327,0.000043599677,0.0000054970296,0.008208671],"genre_scores_gemma":[0.9979625,0.0001642465,0.00065422326,0.0002277459,0.00011602192,2.1856707e-7,0.0000021655658,0.0000015435782,0.00087136886],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886245,0.000108840315,0.00023129582,0.0001744744,0.00016809352,0.00045487704],"domain_scores_gemma":[0.9990632,0.00011238099,0.000107988424,0.00006634098,0.000079367404,0.00057072856],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00077428186,0.00007084335,0.00017995128,0.00026329802,0.000869957,0.0004542524,0.00029628063,0.000073992436,0.0039073746],"category_scores_gemma":[0.00008974685,0.00007942364,0.000066346074,0.0004481653,0.0012825351,0.00034573753,0.0000053449444,0.00024779685,0.0000719599],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000032047342,0.0000017987085,0.98791766,0.000003809877,0.000012082179,0.000102446764,0.00022748798,0.00004179899,0.0000020863997,0.0000064589894,0.00022033366,0.011460835],"study_design_scores_gemma":[0.00015650781,0.00019552658,0.9886908,0.00003945256,0.00000803325,0.0012321008,0.00057659677,0.00017287284,0.0000042491793,0.0010083858,0.007817558,0.000097906406],"about_ca_topic_score_codex":0.09745953,"about_ca_topic_score_gemma":0.9912453,"teacher_disagreement_score":0.8937858,"about_ca_system_score_codex":3.097652e-7,"about_ca_system_score_gemma":0.00043180975,"threshold_uncertainty_score":0.9970032},"labels":[],"label_agreement":null},{"id":"W1973232785","doi":"10.1139/e05-059","title":"Late Cenozoic architecture of the St. Pierre Slope","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Bedford Institute of Oceanography","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Cenozoic; Paleontology; Stratigraphy; Pleistocene; Radiocarbon dating; Quaternary; Ridge; Horizon; Palynology; Fault scarp; Continental shelf; Mass wasting; Geomorphology; Fault (geology); Sediment; Tectonics; Oceanography","score_opus":0.01866510446925361,"score_gpt":0.22583875822840974,"score_spread":0.20717365375915614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973232785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97685283,0.0025183554,0.0000057581906,0.0054604104,0.00043204415,0.000054205862,0.00002293201,0.0000015164559,0.014651919],"genre_scores_gemma":[0.99845606,0.00003210384,0.00054960034,0.000347242,0.0001050201,5.3637745e-8,8.908429e-7,9.124743e-7,0.0005081029],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988121,0.00015757498,0.00024386792,0.00010881525,0.00025926257,0.00041842894],"domain_scores_gemma":[0.99912995,0.00014889178,0.00016606788,0.0001172194,0.000088031964,0.0003498475],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00097361766,0.000076301265,0.00015815889,0.00023492743,0.00045154098,0.00003626822,0.00078263937,0.000067361856,0.003658387],"category_scores_gemma":[0.00016928861,0.000043344273,0.00008253727,0.00049513846,0.0013553926,0.00016494795,0.0000068163736,0.00035048972,0.000051405706],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000048709944,0.0000016582532,0.98751986,0.0000032787564,0.0000076063197,0.000016831083,0.0002466166,0.008731711,0.0000044561493,0.000060025457,0.00015065148,0.0032524068],"study_design_scores_gemma":[0.000107569904,0.0001355813,0.98032504,0.00002575678,0.0000066404864,0.00031504134,0.00009590978,0.00033739902,0.00010275871,0.00077913766,0.017712321,0.000056870496],"about_ca_topic_score_codex":0.0015544428,"about_ca_topic_score_gemma":0.64154005,"teacher_disagreement_score":0.6399856,"about_ca_system_score_codex":2.9948293e-7,"about_ca_system_score_gemma":0.0014119371,"threshold_uncertainty_score":0.9972524},"labels":[],"label_agreement":null},{"id":"W1973250535","doi":"10.1139/e00-094","title":"Magmatic evolution of the southern Great Bear continental arc, northwestern Canadian Shield: geochronological constraints","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Nexen (Canada); University of British Columbia","funders":"Harvard University; Massachusetts Institute of Technology","keywords":"Geology; Terrane; Zircon; Batholith; Geochemistry; Craton; Back-arc basin; Archean; Continental arc; Plutonism; Pluton; Island arc; Volcanic arc; Subduction; Geochronology; Felsic; Volcanic rock; Paleontology; Mafic; Volcano; Tectonics","score_opus":0.01398707764340988,"score_gpt":0.1820414990648221,"score_spread":0.16805442142141222,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973250535","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9899046,0.00055025285,0.000016311998,0.0014640893,0.00021173613,0.000063955915,0.000091034526,0.0000024797564,0.0076955296],"genre_scores_gemma":[0.9993188,0.00000891425,0.00016158291,0.0002770405,0.000071792754,1.1834681e-7,0.0000036046126,9.526043e-7,0.00015719894],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985827,0.00007782083,0.00037135324,0.00016055908,0.00030692306,0.00050060934],"domain_scores_gemma":[0.99869984,0.000081818376,0.00021883719,0.00010992032,0.00010721022,0.00078237144],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046388336,0.00011744937,0.00023331508,0.00022642109,0.00036871803,0.00007053704,0.0006226388,0.000075833224,0.01443681],"category_scores_gemma":[0.00014378001,0.00006517497,0.00017122897,0.0006207987,0.0017155964,0.00014639912,0.0000073177116,0.00020789474,0.00009206214],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000033792478,0.0000030503625,0.9957092,0.0000021948404,0.000012510038,0.00005322024,0.00012445381,0.00046446433,0.000029748611,0.00007102937,0.000017913868,0.0035088747],"study_design_scores_gemma":[0.00013330596,0.0001483474,0.9936535,0.000035589434,0.000026873411,0.0002943298,0.0013419734,0.00069895625,0.00003010037,0.002450135,0.0010843846,0.00010255265],"about_ca_topic_score_codex":0.6562653,"about_ca_topic_score_gemma":0.99508774,"teacher_disagreement_score":0.3388224,"about_ca_system_score_codex":0.000006760291,"about_ca_system_score_gemma":0.0012016456,"threshold_uncertainty_score":0.98646414},"labels":[],"label_agreement":null},{"id":"W1973505154","doi":"10.1139/e01-099","title":"Anatomy and orogenic history of a Paleoproterozoic accretionary belt: the Makkovik Province, Labrador, Canada","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University; Dalhousie University; Memorial University of Newfoundland","funders":"","keywords":"Geology; Metamorphism; Plutonism; Archean; Terrane; Geochemistry; Foreland basin; Accretion (finance); Continental crust; Passive margin; Accretionary wedge; Laurentia; Orogeny; Back-arc basin; Paleontology; Crust; Subduction; Rift; Ordovician; Magmatism; Tectonics","score_opus":0.013564876172113004,"score_gpt":0.16276002847349824,"score_spread":0.14919515230138525,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973505154","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97636706,0.0159747,0.0000013618727,0.0030940785,0.00018586338,0.000054946468,0.000025527544,0.0000014433167,0.004295015],"genre_scores_gemma":[0.99849427,0.00009402818,0.00016257192,0.00062364864,0.000049342187,1.7584281e-7,0.0000016246071,7.4340346e-7,0.0005736009],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99890363,0.0000651733,0.00027593263,0.00013852482,0.00033136894,0.0002853417],"domain_scores_gemma":[0.99908096,0.0001213593,0.00019380133,0.000085007276,0.00008646313,0.0004324093],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038828288,0.000089440706,0.00017696369,0.00011981472,0.00019678476,0.000028083956,0.00040973432,0.000032466956,0.008308247],"category_scores_gemma":[0.000115957184,0.00005037951,0.00006244979,0.00033141876,0.00086588453,0.00016050746,0.000006825518,0.00015666455,0.000005441127],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004461961,0.000004760434,0.9844136,0.000010735219,0.000024869345,0.00010417891,0.00019540712,0.00034239498,0.00002468381,0.00010151172,0.0027304743,0.012042891],"study_design_scores_gemma":[0.00014420075,0.00023762151,0.9284445,0.000025439826,0.00003299207,0.00022324616,0.0003341003,0.0030789508,0.000046094916,0.0013082961,0.06597963,0.00014494672],"about_ca_topic_score_codex":0.789625,"about_ca_topic_score_gemma":0.9965278,"teacher_disagreement_score":0.2069028,"about_ca_system_score_codex":0.0000065386344,"about_ca_system_score_gemma":0.0017827941,"threshold_uncertainty_score":0.9925983},"labels":[],"label_agreement":null},{"id":"W1973520589","doi":"10.1139/e08-042","title":"Postglacial evolution of a Pacific coastal fjord in British Columbia, Canada: interactions of sea-level change, crustal response, and environmental fluctuations — results from MONA core MD02-2494This article is one of a series of papers published in this Special Issue on the theme <i>Polar Climate Stability Network</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; Université Laval; Center for Northern Studies; Royal Roads University; Geological Survey of Canada; Fisheries and Oceans Canada","funders":"Past Global Changes; Natural Resources Canada; Royal Roads University","keywords":"Geology; Deglaciation; Oceanography; Radiocarbon dating; Post-glacial rebound; Sea level; Pleistocene; Younger Dryas; Last Glacial Maximum; Holocene; Glacial period; Sedimentary rock; Paleontology; Physical geography; Geography","score_opus":0.0378473238638785,"score_gpt":0.20556520057267408,"score_spread":0.16771787670879557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973520589","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938761,0.00029575356,1.7533375e-7,0.0010164037,0.00019695266,0.0001691285,0.003738086,6.027327e-7,0.00070679473],"genre_scores_gemma":[0.99960643,0.00011178661,0.000101964324,0.00003723405,0.000080529004,7.1328276e-7,0.00002631773,0.0000014474281,0.00003356775],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99820656,0.00034822212,0.00060169364,0.00017208791,0.00034377835,0.0003276837],"domain_scores_gemma":[0.99857277,0.00069287757,0.00035764568,0.000116228664,0.00009522421,0.00016526505],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014982283,0.0000719658,0.00029157154,0.00016758946,0.0002862224,0.000025041636,0.00023092175,0.00006638372,0.004266613],"category_scores_gemma":[0.0006137391,0.0000745692,0.000043581746,0.0005247722,0.0019866524,0.00032662466,0.000015067439,0.00026720247,6.56084e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044389637,0.000027836986,0.99616176,0.000006057815,0.000012786849,0.000035623,0.0026265478,0.00010521898,0.00012699158,0.000004319907,0.00023630772,0.00021266767],"study_design_scores_gemma":[0.0003779192,0.00038046177,0.9921623,0.00007646425,0.000006975347,0.00007547977,0.005930563,0.0004238503,0.00018286087,0.00014097686,0.00018218272,0.000059973703],"about_ca_topic_score_codex":0.93342686,"about_ca_topic_score_gemma":0.99977267,"teacher_disagreement_score":0.06634582,"about_ca_system_score_codex":0.000007688232,"about_ca_system_score_gemma":0.0016926529,"threshold_uncertainty_score":0.9966436},"labels":[],"label_agreement":null},{"id":"W1973657319","doi":"10.1139/e01-016","title":"An ontogenetic perspective on locomotion in the Late Cretaceous dinosaur<i>Maiasaura peeblesorum</i>(Ornithischia: Hadrosauridae)","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"College of Family Physicians of Canada","funders":"","keywords":"Allometry; Manus; Anatomy; Forelimb; Humerus; Hindlimb; Biology; Biomechanics; Isometric exercise; Sauropoda; Postcrania; Femur; Geology; Cretaceous; Paleontology","score_opus":0.019624998177463555,"score_gpt":0.2349957510507871,"score_spread":0.21537075287332355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973657319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9758333,0.0024532885,0.00002289187,0.005075403,0.000521664,0.00010391825,0.000018561997,0.0000043384784,0.015966639],"genre_scores_gemma":[0.9983191,0.00012241383,0.00016299673,0.0011324005,0.00017458954,3.8021588e-7,0.0000048424613,0.0000014860289,0.00008182769],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99825466,0.00044175144,0.00028617593,0.00020766068,0.00026655587,0.0005432206],"domain_scores_gemma":[0.9990644,0.00018131078,0.00016321673,0.00014421568,0.000096679985,0.00035018017],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014371846,0.00013750429,0.00018616988,0.00041968975,0.0006464041,0.000098708566,0.0007193501,0.00010285815,0.00088180136],"category_scores_gemma":[0.00012421845,0.00008791326,0.00006757255,0.0005861526,0.000852627,0.00039718722,0.0000020014115,0.00038482982,0.000087607135],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000320887,0.000015009623,0.9849691,8.7024915e-7,0.0000063843063,0.00033747964,0.001009442,0.011521967,0.00001545276,0.0004679252,0.000089918416,0.0015343591],"study_design_scores_gemma":[0.00020582567,0.0012289257,0.98744696,0.000021192553,0.000008775552,0.001068143,0.0024161614,0.0013091548,0.0000059828008,0.0029801559,0.003190451,0.00011824143],"about_ca_topic_score_codex":0.016864145,"about_ca_topic_score_gemma":0.8320789,"teacher_disagreement_score":0.81521475,"about_ca_system_score_codex":0.000007966867,"about_ca_system_score_gemma":0.0008761802,"threshold_uncertainty_score":0.9896826},"labels":[],"label_agreement":null},{"id":"W1973709020","doi":"10.1139/e03-048","title":"Paleoenvironmental analysis of the late Neoproterozoic Mistaken Point and Trepassey formations, southeastern Newfoundland","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":159,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada; Eli Lilly and Company","keywords":"Geology; Turbidity current; Paleocurrent; Slumping; Turbidite; Paleontology; Debris flow; Siltstone; Debris; Structural basin; Geologic record; Fluvial; Sedimentary depositional environment; Oceanography; Facies","score_opus":0.015441322430464553,"score_gpt":0.1888005165495503,"score_spread":0.17335919411908574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973709020","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99519587,0.0006653685,0.000055403143,0.00030106495,0.00008720844,0.00004717108,0.000040490173,8.396408e-7,0.0036065849],"genre_scores_gemma":[0.9994138,0.000023214137,0.00032906167,0.000107947526,0.000007152647,9.54016e-8,0.0000019876911,4.5477006e-7,0.00011629574],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992745,0.00006255244,0.000257773,0.000060126913,0.00017449164,0.00017058625],"domain_scores_gemma":[0.99943495,0.00005132976,0.00020867122,0.0000667748,0.000031347423,0.00020695473],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00052132615,0.00006019285,0.0001323114,0.00021340403,0.000350596,0.00009989804,0.00018944508,0.000023686945,0.0015053292],"category_scores_gemma":[0.00007188908,0.000033314973,0.00007034039,0.0005833925,0.00036424698,0.00033504088,0.0000024171213,0.00006767608,0.000006094354],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000012681578,0.0000014949538,0.99422544,0.0000030182791,0.000023940187,0.0000010522976,0.0004651549,0.0044882796,0.0000024982833,0.000072835064,0.0000037551242,0.00071128545],"study_design_scores_gemma":[0.00007581822,0.00009024629,0.9945505,0.0000099416675,0.000061716295,0.000037766968,0.000994334,0.0016582421,0.000017231501,0.00065148907,0.0018050305,0.000047660425],"about_ca_topic_score_codex":0.0055383737,"about_ca_topic_score_gemma":0.3641292,"teacher_disagreement_score":0.3585908,"about_ca_system_score_codex":7.542269e-7,"about_ca_system_score_gemma":0.00020206586,"threshold_uncertainty_score":0.9994074},"labels":[],"label_agreement":null},{"id":"W1973835690","doi":"10.1139/e03-011","title":"Anatomy of the primitive bird <i>Sapeornis chaoyangensis </i>from the Early Cretaceous of Liaoning, China","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":178,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Shanghai Ocean University; National Natural Science Foundation of China","keywords":"Pectoral girdle; Anatomy; Forelimb; Humerus; Biology; Coracoid; Cretaceous; Skull; Theropoda; Tetrapod (structure); Paleontology","score_opus":0.013019272773409018,"score_gpt":0.2054386570996764,"score_spread":0.19241938432626737,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973835690","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98336005,0.007800321,0.000008408805,0.0011042936,0.00069380086,0.00006709515,0.000078773366,0.0000019187303,0.006885315],"genre_scores_gemma":[0.9992939,0.00008018519,0.00029313582,0.00022918274,0.00005205654,1.0679683e-7,6.902942e-7,0.0000013453723,0.00004936055],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99872494,0.00031163715,0.00030954386,0.0001286981,0.00021713926,0.00030803256],"domain_scores_gemma":[0.9988566,0.00029483397,0.00039643425,0.00014008519,0.00011393566,0.00019810478],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008539281,0.00009308328,0.00020612324,0.00010723252,0.00045440672,0.000019321365,0.0006328537,0.000072177216,0.00074976287],"category_scores_gemma":[0.00037957416,0.00004853068,0.0001174494,0.0004818365,0.0020951526,0.00016322326,0.00000456814,0.00020472027,0.000010529883],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006778095,0.0000026043776,0.9976749,0.000001267298,0.000024860214,0.000009936717,0.0006798773,0.0003034091,0.00004371812,0.0003357966,0.00010864794,0.00080824335],"study_design_scores_gemma":[0.0001008501,0.00022631286,0.99141634,0.00003008703,0.000021907672,0.00010989702,0.00034917134,0.000055309694,0.00038266584,0.0010353797,0.0062118177,0.000060267623],"about_ca_topic_score_codex":0.037999053,"about_ca_topic_score_gemma":0.56655353,"teacher_disagreement_score":0.5285545,"about_ca_system_score_codex":0.0000014956355,"about_ca_system_score_gemma":0.0013141709,"threshold_uncertainty_score":0.968407},"labels":[],"label_agreement":null},{"id":"W1973895784","doi":"10.1139/e11-064","title":"Vertebrate fossils (Dinosauria) from the Bonnet Plume Formation, Yukon Territory, Canada","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon Department of Tourism and Culture; McGill University; University of Toronto; Royal Tyrrell Museum; Royal Ontario Museum","funders":"","keywords":"Vertebrate; Paleontology; Cretaceous; Geology; Vertebrate paleontology; Mesozoic; Fauna; Postcrania; Taxon; Biology; Ecology; Structural basin","score_opus":0.019794484862225747,"score_gpt":0.19281999701078703,"score_spread":0.1730255121485613,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973895784","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9791252,0.009118125,0.000019495577,0.0038268832,0.0032339985,0.000050334238,0.00015188241,0.0000027186595,0.0044713523],"genre_scores_gemma":[0.9978752,0.000024476118,0.00015010404,0.001238476,0.0006460098,1.5415573e-7,0.000014167837,7.499183e-7,0.000050661845],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99876076,0.00015633368,0.00026154405,0.00008944845,0.00020501507,0.000526871],"domain_scores_gemma":[0.99890405,0.00022310452,0.00017546002,0.000089705354,0.000052206007,0.0005555002],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00075036194,0.00009072284,0.0001343835,0.000077138284,0.000764546,0.00005569906,0.0005059515,0.00005959528,0.0015807439],"category_scores_gemma":[0.00012066664,0.000055970824,0.000040422623,0.0001751932,0.00048193475,0.00078645546,0.0000029176915,0.0001756783,0.00004429073],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000044114868,0.000001169059,0.98606956,7.028165e-7,0.000009029226,0.000013662925,0.00025787568,0.00024812756,0.000004367632,0.000071978066,0.011795489,0.001523635],"study_design_scores_gemma":[0.000087386186,0.00006270303,0.927992,0.000010622337,0.0000087896215,0.00017085284,0.00053091877,0.0007843073,0.000020417843,0.00034920973,0.06990398,0.0000788397],"about_ca_topic_score_codex":0.85536045,"about_ca_topic_score_gemma":0.9992618,"teacher_disagreement_score":0.14390133,"about_ca_system_score_codex":0.000005708955,"about_ca_system_score_gemma":0.0022412583,"threshold_uncertainty_score":0.99933195},"labels":[],"label_agreement":null},{"id":"W1973921547","doi":"10.1139/e04-009","title":"A bimodal volcanicplutonic system: the Zarembo Island extrusive suite and the Burnett Inlet intrusive complex","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Felsic; Mafic; Geochemistry; Rhyolite; Pluton; Gabbro; Volcanic rock; Magma chamber; Diorite; Igneous rock; Basalt; Magma; Silicic; Dacite; Petrology; Volcano; Zircon; Paleontology; Tectonics","score_opus":0.014750410363451715,"score_gpt":0.1893311005899918,"score_spread":0.1745806902265401,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973921547","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9799188,0.0033365737,0.000050749597,0.012084126,0.0002088728,0.00012063215,0.00003882932,0.0000039404376,0.0042374805],"genre_scores_gemma":[0.9984547,0.00006435182,0.00016716831,0.0011004325,0.0001693963,3.7071206e-7,0.0000026392215,0.0000010752069,0.000039859708],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99855626,0.00014039353,0.0003352837,0.00018191901,0.0003480389,0.000438133],"domain_scores_gemma":[0.9987327,0.00031374145,0.0002414302,0.000118379416,0.00013691442,0.00045684146],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011564355,0.00013353597,0.0002793128,0.00013413843,0.0009166876,0.00029577964,0.0006760911,0.000044227945,0.0016922501],"category_scores_gemma":[0.00021745851,0.000055452394,0.00012087528,0.0006500245,0.0023695985,0.00019098903,0.00001581767,0.00026251847,0.000038922957],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013584396,0.000010338683,0.9221551,0.000034637844,0.00021105492,0.00044879422,0.0045989486,0.04019534,0.00006995391,0.024622643,0.00065843563,0.0068589374],"study_design_scores_gemma":[0.0015783282,0.00048915914,0.9246279,0.00009702711,0.00014165712,0.0015355997,0.005738906,0.009030261,0.000055838806,0.046816815,0.0095803095,0.00030817243],"about_ca_topic_score_codex":0.070490666,"about_ca_topic_score_gemma":0.7149634,"teacher_disagreement_score":0.6444727,"about_ca_system_score_codex":0.000003863086,"about_ca_system_score_gemma":0.00067385845,"threshold_uncertainty_score":0.9992203},"labels":[],"label_agreement":null},{"id":"W1973989232","doi":"10.1139/e00-042","title":"The July 29, 1998, debris flow and landslide dam at Capricorn Creek, Mount Meager Volcanic Complex, southern Coast Mountains, British Columbia","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Spinal Cord Injury BC; University of British Columbia","funders":"","keywords":"Geology; Landslide; Colluvium; Debris flow; Aggradation; Debris; Geomorphology; Volcano; Fluvial; Bedrock; Denudation; Hyperconcentrated flow; Mudflow; Mass wasting; Hydrology (agriculture); Alluvium; Geochemistry; Tectonics; Paleontology; Sediment; Sediment transport; Oceanography; Structural basin; Geotechnical engineering","score_opus":0.008620745600180856,"score_gpt":0.1856905886152264,"score_spread":0.17706984301504552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973989232","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934582,0.0011746563,0.000005654418,0.00038599898,0.00019905856,0.00010115705,0.000088541594,0.0000060969855,0.004580595],"genre_scores_gemma":[0.9891112,0.00043645874,0.00030531597,0.00050702377,0.00010794838,0.000001285144,0.0000026991345,0.000011675841,0.009516408],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981935,0.00007881645,0.00036553753,0.00025376602,0.00049476523,0.0006135857],"domain_scores_gemma":[0.9988238,0.000070440816,0.00016141763,0.00015088989,0.00002434255,0.0007690727],"candidate_categories":["sts","scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009034039,0.00011719337,0.00020751847,0.000032127453,0.0021615506,0.0012902963,0.0005430072,0.00007826258,0.0051674093],"category_scores_gemma":[0.00004176402,0.00010163098,0.000086731874,0.00032307836,0.0012302691,0.000266124,0.000047604397,0.00026527577,0.0002310065],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013412448,0.000014402849,0.9055274,0.0000038451135,0.000037285834,0.00031622616,0.0010923459,0.002752923,0.0001268288,0.000001747212,0.037992477,0.052121095],"study_design_scores_gemma":[0.00037579416,0.00017206835,0.4484025,0.00004532368,0.000025776562,0.0009656347,0.00048167692,0.0019984874,0.0000038332732,0.00015583339,0.54717547,0.00019765094],"about_ca_topic_score_codex":0.4486055,"about_ca_topic_score_gemma":0.9928401,"teacher_disagreement_score":0.5442346,"about_ca_system_score_codex":0.00008201,"about_ca_system_score_gemma":0.0002829546,"threshold_uncertainty_score":0.99974644},"labels":[],"label_agreement":null},{"id":"W1974088811","doi":"10.1139/e01-039","title":"New species of Silurian acanthodians from the Mackenzie Mountains, Canada","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Paleontology; Geology; Genus; Ridge; SPINE (molecular biology); Biology; Zoology","score_opus":0.0218790639067093,"score_gpt":0.2028658239083842,"score_spread":0.1809867600016749,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974088811","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96974,0.0062261554,0.00006056246,0.008412765,0.0013386321,0.000046093453,0.0002309365,0.0000017900164,0.01394307],"genre_scores_gemma":[0.9975554,0.00014641049,0.0006757395,0.00076907646,0.00035126784,3.481981e-8,0.000010185457,8.0295274e-7,0.0004910955],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988893,0.00011165658,0.000284452,0.00011944005,0.00021759629,0.000377525],"domain_scores_gemma":[0.99881905,0.00033469047,0.00019876364,0.0001019908,0.000066180495,0.00047934172],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00045842156,0.00008897981,0.00017737062,0.00009550765,0.00042034074,0.000031900716,0.00068285654,0.000054852557,0.006286487],"category_scores_gemma":[0.00016769546,0.000055451874,0.000051404782,0.00034556328,0.000741847,0.00019600062,0.0000031738748,0.0001648698,0.000014946626],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011329699,7.7258693e-7,0.9892085,4.8885806e-7,0.000013165846,0.00009336506,0.00013624942,0.0007590122,0.000008527926,0.0001963071,0.0067670355,0.0028052423],"study_design_scores_gemma":[0.000093062816,0.000096564974,0.86351764,0.000012194759,0.000008696843,0.000137632,0.0007162464,0.000105092346,0.000018913155,0.0008407974,0.13439058,0.00006260099],"about_ca_topic_score_codex":0.98207724,"about_ca_topic_score_gemma":0.9998957,"teacher_disagreement_score":0.12762354,"about_ca_system_score_codex":0.0000040768705,"about_ca_system_score_gemma":0.008099441,"threshold_uncertainty_score":0.9975237},"labels":[],"label_agreement":null},{"id":"W1974144355","doi":"10.1139/e05-034","title":"Geology and thermotectonic evolution of the western margin of the Trans-Hudson Orogen: evidence from the eastern sub-Athabasca basement, Saskatchewan","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":109,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saskatoon City Hospital; Saskatchewan Research Council (Canada)","funders":"","keywords":"Geology; Imbrication; Geochemistry; Metamorphism; Batholith; Underplating; Tectonics; Mafic; Continental crust; Nappe; Shear zone; Anatexis; Crust; Petrology; Partial melting; Paleontology; Subduction","score_opus":0.01634285730711371,"score_gpt":0.1884816513787389,"score_spread":0.1721387940716252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974144355","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9847386,0.0056683924,0.00004009953,0.009200648,0.000112231995,0.000076314966,0.000034140852,0.0000010413007,0.00012853349],"genre_scores_gemma":[0.99940085,0.00005878649,0.0000889103,0.00032434904,0.00007106766,1.5490907e-7,4.680496e-7,8.6096287e-7,0.000054532513],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986762,0.00023204471,0.00033388854,0.00015159458,0.0003383147,0.00026799977],"domain_scores_gemma":[0.9989629,0.00030243312,0.00030648598,0.00016903048,0.00008234276,0.00017682972],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00081448926,0.00009858179,0.00019085086,0.000050427505,0.00028535284,0.000035374145,0.0008687656,0.000048005746,0.0011099599],"category_scores_gemma":[0.00013809619,0.000040377377,0.00015258054,0.0004528956,0.0012628494,0.00018366292,0.000017290376,0.00018745076,0.000004586914],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000068215604,0.0000032417793,0.99459463,0.0000027441001,0.000015966883,8.9998275e-7,0.00044905822,0.001160598,0.0006448577,0.0000063483362,0.000014223341,0.0031005866],"study_design_scores_gemma":[0.00009180911,0.00010510239,0.9934265,0.00008051836,0.000043030883,0.00002164317,0.0006229074,0.0020146198,0.0024664449,0.0007226174,0.00034872955,0.0000560462],"about_ca_topic_score_codex":0.16305943,"about_ca_topic_score_gemma":0.8967799,"teacher_disagreement_score":0.7337204,"about_ca_system_score_codex":0.0000029447885,"about_ca_system_score_gemma":0.0005952824,"threshold_uncertainty_score":0.9998032},"labels":[],"label_agreement":null},{"id":"W1974188877","doi":"10.1139/cjes-2012-0139","title":"Bokan Mountain peralkaline granitic complex, Alexander terrane (southeastern Alaska): evidence for Early Jurassic rifting prior to accretion with North America","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey","keywords":"Peralkaline rock; Geology; Terrane; Geochemistry; Dike; Zircon; Rift; Geochronology; Igneous rock; Paleontology; Volcano; Tectonics","score_opus":0.04573426037083493,"score_gpt":0.2345713370270847,"score_spread":0.18883707665624977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974188877","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99327034,0.00023555817,0.0008802737,0.004992234,0.000075414755,0.00023345207,0.000036734957,0.0000063776347,0.00026962237],"genre_scores_gemma":[0.99333435,0.000006593686,0.005166776,0.0011921672,0.00014523475,0.0000022369668,0.0000123689715,0.0000024956007,0.00013775354],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983392,0.00005794555,0.0003659592,0.0002695815,0.0003735495,0.00059379643],"domain_scores_gemma":[0.99816906,0.00024306067,0.00021134721,0.00010214255,0.00029758745,0.0009768177],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037439226,0.00016174762,0.00028982616,0.00025359637,0.00052671996,0.0003373053,0.00048848055,0.00003392844,0.0053700237],"category_scores_gemma":[0.00026182344,0.00009863706,0.00010189818,0.0007438019,0.00047395728,0.00057949964,0.0000066457533,0.00014803116,0.00012055569],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023848843,0.0000041060853,0.9885251,0.000007797804,0.00001534589,0.000011340897,0.00039626754,0.0028317485,0.00009091388,0.0000026535436,0.00006326914,0.008027623],"study_design_scores_gemma":[0.00017861757,0.0010417787,0.9921233,0.000082421204,0.000034726178,0.000042015723,0.0006020273,0.004617295,0.000021821072,0.00029204073,0.0007873382,0.00017660279],"about_ca_topic_score_codex":0.048861645,"about_ca_topic_score_gemma":0.42040128,"teacher_disagreement_score":0.37153962,"about_ca_system_score_codex":0.0000024962403,"about_ca_system_score_gemma":0.00033784428,"threshold_uncertainty_score":0.9955392},"labels":[],"label_agreement":null},{"id":"W1974190852","doi":"10.1139/e00-086","title":"Geology and tectonic setting of Paleoproterozoic granitoid suites in the Island Harbour Bay area, Makkovik Province, Labrador","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Dalhousie University; Nova Scotia Department of Energy; Acadia University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Mafic; Porphyritic; Archean; Pluton; Igneous rock; Batholith; Migmatite; Gneiss; Hornblende; Biotite; Petrology; Tectonics; Metamorphic rock; Paleontology","score_opus":0.011069604950873207,"score_gpt":0.18481926583904365,"score_spread":0.17374966088817045,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974190852","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942717,0.0022760176,0.0000065781956,0.001808953,0.000054149285,0.000072373135,0.0000125390925,0.0000014012653,0.0014962858],"genre_scores_gemma":[0.99931824,0.00007294478,0.00020150981,0.00030160288,0.000050880604,2.6106252e-7,0.0000018391783,6.7249425e-7,0.000052050695],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988053,0.00011528289,0.00031754668,0.00015616015,0.00022128611,0.00038441797],"domain_scores_gemma":[0.99913615,0.000321423,0.00018744306,0.00007514408,0.000058329268,0.00022150087],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010714383,0.000096581316,0.00022493867,0.00026295584,0.00020730989,0.000078090416,0.0004236695,0.000047413927,0.0019504869],"category_scores_gemma":[0.00030651668,0.00005221362,0.000059665974,0.0006766292,0.0006188058,0.00017520147,0.0000063595253,0.00020630019,0.000005707603],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000060035077,0.0000039669867,0.9962481,0.0000050909825,0.00000532181,0.00008542353,0.00016412981,0.0003423093,0.000041828367,0.000020436397,0.00001710346,0.0030602824],"study_design_scores_gemma":[0.00013579713,0.00026562862,0.99425536,0.000024804414,0.00001009482,0.00027258188,0.00050207786,0.0008661122,0.000034033925,0.002737681,0.00082063593,0.00007516292],"about_ca_topic_score_codex":0.042194188,"about_ca_topic_score_gemma":0.91671306,"teacher_disagreement_score":0.8745189,"about_ca_system_score_codex":7.730986e-7,"about_ca_system_score_gemma":0.00031424573,"threshold_uncertainty_score":0.99896187},"labels":[],"label_agreement":null},{"id":"W1974265952","doi":"10.1139/e11-018","title":"Geological and depositional setting of the Sirius Passet Lagerstätte (Early Cambrian), North Greenland","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology; Sedimentary depositional environment; Lagerstätte; Carbonate platform; Onlap; Taphonomy; Structural basin","score_opus":0.02570768988442184,"score_gpt":0.1911887640340882,"score_spread":0.16548107414966634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974265952","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98666847,0.0014793354,0.00001113108,0.0002504228,0.00022380652,0.000040458366,0.000041751533,0.0000013791005,0.011283238],"genre_scores_gemma":[0.99899787,0.000010712912,0.0008555222,0.00008328007,0.0000418645,6.496751e-8,4.2292098e-7,2.935848e-7,0.000009992836],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991022,0.00010529724,0.00023268232,0.00010842491,0.00018980252,0.0002616235],"domain_scores_gemma":[0.9992568,0.00010455432,0.00020909094,0.000059943326,0.000060880106,0.0003087501],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005091225,0.000074860625,0.00013973421,0.000121880534,0.00045180516,0.000039291,0.00032450355,0.000050494353,0.00017648702],"category_scores_gemma":[0.00007309774,0.000044410594,0.0000644889,0.00022585399,0.0010817872,0.00025756218,0.0000015620602,0.0001634082,0.0000013971733],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007187654,0.0000017021395,0.99664724,0.0000022912566,0.000010085715,0.00004438443,0.0004211742,0.000020086074,0.000004901137,0.000128275,0.000017970156,0.0026947204],"study_design_scores_gemma":[0.00009496959,0.0002378382,0.9981995,0.000018965675,0.000012058913,0.00035113425,0.000104320774,0.00008115796,0.00002757028,0.00078347296,0.000029349672,0.000059628408],"about_ca_topic_score_codex":0.01890858,"about_ca_topic_score_gemma":0.70086616,"teacher_disagreement_score":0.68195754,"about_ca_system_score_codex":3.560168e-7,"about_ca_system_score_gemma":0.00045458056,"threshold_uncertainty_score":0.9876246},"labels":[],"label_agreement":null},{"id":"W1974368699","doi":"10.1139/e06-069","title":"Brachiopod diversification during the Early–Mid Ordovician: an example from the Dawan Formation, Yichang area, central China","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Biozone; Ordovician; Geology; Paleontology; Facies; Siliciclastic; Range (aeronautics); Biostratigraphy; Structural basin","score_opus":0.02960299687392814,"score_gpt":0.206611500604723,"score_spread":0.17700850373079485,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974368699","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891328,0.0017626055,0.00019436415,0.0007839809,0.0004531663,0.00008395748,0.000036323472,0.000004666064,0.007548131],"genre_scores_gemma":[0.9994249,0.000019212575,0.0001986175,0.00012253544,0.00021696895,8.895348e-8,0.0000047676635,5.3626553e-7,0.0000123771315],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99871725,0.00010499892,0.0002821215,0.00013596602,0.00028498043,0.00047467512],"domain_scores_gemma":[0.998954,0.00017025648,0.00024849304,0.00014772196,0.00005488786,0.0004246248],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0013017602,0.00009488029,0.00010673824,0.00013738126,0.0021694934,0.00025829053,0.00074654334,0.00004874476,0.00035187512],"category_scores_gemma":[0.00004518738,0.00005305424,0.00006506816,0.00039137885,0.00061513594,0.0011197865,0.0000013321138,0.00023095116,0.0000048409443],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001256155,0.0000022384668,0.98412114,6.9420446e-7,0.000009017413,0.00001862911,0.0051512485,0.00017732666,0.000026642352,0.00012189582,0.000016673646,0.010341946],"study_design_scores_gemma":[0.00013056942,0.00010617316,0.9947231,0.000014029994,0.000011098133,0.00006435812,0.0034573663,0.0002588537,0.00009876009,0.0004862955,0.0005717896,0.00007763163],"about_ca_topic_score_codex":0.16461211,"about_ca_topic_score_gemma":0.94906354,"teacher_disagreement_score":0.7844514,"about_ca_system_score_codex":0.0000023864238,"about_ca_system_score_gemma":0.0003521891,"threshold_uncertainty_score":0.99912953},"labels":[],"label_agreement":null},{"id":"W1975050485","doi":"10.1139/e05-091","title":"An ornithurine bird from the Late Cretaceous of Alberta, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"University of Washington; University of Calgary; National Science Foundation","keywords":"Geology; Cretaceous; Paleontology; Ridge; Synapomorphy; Margin (machine learning); Anatomy; Process (computing); Medicine; Biology","score_opus":0.009630529869385946,"score_gpt":0.18283226528734897,"score_spread":0.17320173541796302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975050485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9908118,0.0029320163,0.0000058931255,0.0016383865,0.0006102157,0.000029121467,0.00007827507,0.0000016585357,0.0038926115],"genre_scores_gemma":[0.99911875,0.000014640894,0.00018900706,0.00034364022,0.00017236108,4.6319396e-8,0.000008108901,0.0000010003429,0.00015242635],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990546,0.00012055138,0.000263725,0.000097217395,0.00016338588,0.00030049274],"domain_scores_gemma":[0.99905914,0.00031808577,0.00019149354,0.00009813937,0.00007301076,0.00026012078],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038867086,0.00007586839,0.00015008826,0.00007854664,0.00036176108,0.000024452054,0.00052946096,0.000045735105,0.0016501558],"category_scores_gemma":[0.00006855122,0.00004560887,0.000035488843,0.00023517692,0.0007546326,0.00018917935,0.0000017029445,0.0001256799,0.000013594662],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007648428,0.0000017267762,0.9928396,5.303168e-7,0.0000073108868,0.000040116716,0.0000601329,0.00569616,0.000013417324,0.0000523101,0.00055771804,0.0007233514],"study_design_scores_gemma":[0.0000834297,0.00016446257,0.98370093,0.00000779721,0.000008861346,0.000100598874,0.00015905502,0.0007802342,0.000027809818,0.00078461337,0.014120146,0.00006206369],"about_ca_topic_score_codex":0.9956293,"about_ca_topic_score_gemma":0.9999818,"teacher_disagreement_score":0.013562428,"about_ca_system_score_codex":0.0000018408442,"about_ca_system_score_gemma":0.0032939285,"threshold_uncertainty_score":0.99926245},"labels":[],"label_agreement":null},{"id":"W1975288679","doi":"10.1139/e11-043","title":"Analysis of coastal dune dynamics, shoreline position, and large woody debris at Wickaninnish Bay, Pacific Rim National Park, British Columbia","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Coastal wetland ecosystem dynamics","field":"Environmental Science","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Parks Canada","keywords":"Geology; Bay; Shore; Oceanography; Debris; National park; Barrier island; Headland; Archaeology; Geography","score_opus":0.008641096030999497,"score_gpt":0.1861438654568209,"score_spread":0.1775027694258214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975288679","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915222,0.00009184634,0.00023354427,0.00009109787,0.0001508059,0.00007240103,0.0007356426,0.000003196941,0.00709929],"genre_scores_gemma":[0.99843794,0.000027937425,0.0007617804,0.00005542461,0.000021519592,7.619886e-7,0.000033729964,0.000006111318,0.000654768],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99833053,0.00005714452,0.0004834871,0.00023932195,0.0005150917,0.00037443504],"domain_scores_gemma":[0.9988718,0.000041674506,0.00033190273,0.00009416562,0.00011433601,0.0005461356],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010600355,0.00009386177,0.00028677832,0.00021681764,0.0004521931,0.00018982697,0.0003050134,0.00005802364,0.0048102783],"category_scores_gemma":[0.0000906084,0.00011649851,0.0001144438,0.001018196,0.00068377843,0.00040517052,0.00007889491,0.000103921106,0.000010264517],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000044849808,0.000022613116,0.99800396,0.0000032010937,0.00006557864,0.00005232437,0.00027784027,0.00025189423,0.00002652152,0.00003008367,0.0008133175,0.00044818912],"study_design_scores_gemma":[0.00019664239,0.00016902256,0.97130287,0.000030908453,0.000102454665,0.0002872297,0.0005517034,0.026244897,0.000004807532,0.00021056354,0.0007575592,0.00014135527],"about_ca_topic_score_codex":0.18337151,"about_ca_topic_score_gemma":0.99735045,"teacher_disagreement_score":0.81397897,"about_ca_system_score_codex":0.00006638325,"about_ca_system_score_gemma":0.0002584492,"threshold_uncertainty_score":0.9960995},"labels":[],"label_agreement":null},{"id":"W1975964301","doi":"10.1139/e04-103","title":"<sup>87</sup>Sr/<sup>86</sup>Sr of brines from the Fennoscandian Shield: a synthesis of groundwater isotopic data from the Baltic Sea region","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Forskningsrådet om Hälsa, Arbetsliv och Välfärd; European Commission","keywords":"Groundwater; Geology; Strontium; Isotopes of strontium; Seawater; Geochemistry; Shield; Salinity; Surface water; Baltic sea; Baltic Shield; Isotopic signature; Oceanography; Precipitation; Aquifer; Isotope; Crust; Paleontology; Environmental science; Chemistry; Geography","score_opus":0.03235128231846201,"score_gpt":0.2128826306428262,"score_spread":0.18053134832436418,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975964301","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99006295,0.002811802,0.000038097798,0.0048386515,0.00020307532,0.00014537078,0.0005922883,0.0000050966523,0.0013026723],"genre_scores_gemma":[0.9978723,0.00019063218,0.00042547658,0.00055573415,0.0007073817,6.915721e-7,0.00005994932,0.000005536737,0.00018228519],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99746794,0.00022857686,0.00069598295,0.00039298928,0.0006184845,0.0005960373],"domain_scores_gemma":[0.99734104,0.000928481,0.0003923567,0.0007379277,0.00012515893,0.0004750684],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011107228,0.0002379718,0.0004219999,0.00014036776,0.0005419225,0.0003258607,0.0027236831,0.00010740576,0.0026015767],"category_scores_gemma":[0.00031019037,0.00013295675,0.0001505561,0.00047702427,0.0011016633,0.0009096056,0.000051440325,0.00032338448,0.000045110606],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024105313,0.000013453897,0.9775343,0.000012684221,0.000067395835,0.0000402336,0.0021346079,0.0020586567,0.000020379211,0.000008554226,0.0024699576,0.015615695],"study_design_scores_gemma":[0.00045801318,0.00024889287,0.94112265,0.00041898832,0.00017100826,0.00031708955,0.0059754695,0.01850407,0.001376085,0.00074269786,0.03027067,0.0003943641],"about_ca_topic_score_codex":0.2514609,"about_ca_topic_score_gemma":0.5152447,"teacher_disagreement_score":0.26378378,"about_ca_system_score_codex":0.0000062909126,"about_ca_system_score_gemma":0.0010333284,"threshold_uncertainty_score":0.9983102},"labels":[],"label_agreement":null},{"id":"W1976215322","doi":"10.1139/e00-040","title":"Evidence for initial calcite-aragonite composition of Lower Algal Chert Member ooids and stromatolites, Paleoproterozoic Gunflint Formation, Ontario, Canada","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Ministry of Natural Resources","keywords":"Calcite; Geology; Aragonite; Stromatolite; Carbonate; Quartz; Carbonate minerals; Diagenesis; Mineral; Geochemistry; Mineralogy; Biogenic silica; Microbial mat; Paleontology; Chemistry; Sediment","score_opus":0.0444290620674989,"score_gpt":0.2528055319616676,"score_spread":0.2083764698941687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976215322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915943,0.004080527,0.000055820896,0.00033331985,0.00029241233,0.00014018793,0.000093438306,0.0000017756216,0.0034081794],"genre_scores_gemma":[0.9983416,0.000030362964,0.001405316,0.00012373997,0.00005694038,6.2103504e-7,0.0000042735537,6.1554005e-7,0.000036496152],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987638,0.00006199675,0.00043012612,0.00013780693,0.0002642008,0.0003420702],"domain_scores_gemma":[0.99895376,0.00018142172,0.00021164263,0.00007109156,0.00014087594,0.00044122402],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005390858,0.00011336777,0.00022103285,0.00015700377,0.0004061031,0.00008958577,0.0002451203,0.00006124228,0.0013808813],"category_scores_gemma":[0.00004507994,0.00009236193,0.00006404838,0.00018685588,0.00048569817,0.00080016727,5.8991554e-7,0.0001415643,8.708457e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001601118,0.0000064597243,0.9487525,0.000034215092,0.0000299959,0.000092087044,0.00082332944,0.0007429153,0.000058148835,0.000050928997,0.00032290153,0.048926365],"study_design_scores_gemma":[0.00025652,0.0005421346,0.99593884,0.00015457143,0.000018678185,0.0003623558,0.00008880718,0.0008932514,0.00020737057,0.00023023091,0.0011931144,0.00011413314],"about_ca_topic_score_codex":0.9019191,"about_ca_topic_score_gemma":0.9993087,"teacher_disagreement_score":0.09738958,"about_ca_system_score_codex":0.0000054496027,"about_ca_system_score_gemma":0.003211041,"threshold_uncertainty_score":0.999532},"labels":[],"label_agreement":null},{"id":"W1976299707","doi":"10.1139/e02-062","title":"Late Quaternary glaciation in the Northern Ogilvie Mountains: revised correlations and implications for the stratigraphic record","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"","keywords":"Moraine; Geology; Glacial period; Terminal moraine; Fluvial; Radiocarbon dating; Quaternary; Holocene; Geomorphology; Glacier; Paleontology; Structural basin","score_opus":0.05364047937093123,"score_gpt":0.2592316697448672,"score_spread":0.205591190373936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976299707","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9689581,0.0043658484,0.000048370093,0.025291381,0.00013848266,0.00019621137,0.000016518512,0.0000013423535,0.0009837645],"genre_scores_gemma":[0.99895555,0.00047224376,0.00012881806,0.00033538905,0.000042721374,0.0000019076879,0.0000025436548,6.642412e-7,0.000060148177],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992217,0.00014318887,0.00020895342,0.00009349062,0.00009313203,0.00023956895],"domain_scores_gemma":[0.9988072,0.0008059206,0.000119101125,0.00008531362,0.00007214961,0.000110304354],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013027835,0.000054155964,0.000087161905,0.00018299063,0.00086198736,0.00010228374,0.00034887448,0.00004125208,0.00018574815],"category_scores_gemma":[0.00020512949,0.000029480289,0.00003529589,0.00041805214,0.0005040244,0.00022134138,0.0000014580747,0.00018040609,0.00001134232],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000027709336,0.000001805993,0.9953421,0.000001922833,0.000004506932,0.0000035495414,0.0004580291,0.0008242387,3.3359325e-7,0.00037434069,0.000042696603,0.0029437547],"study_design_scores_gemma":[0.00010483765,0.00015832372,0.9850299,0.000010547097,0.000008362529,0.000093559735,0.0003756434,0.008506623,1.6887799e-7,0.0043105297,0.0013635588,0.00003794912],"about_ca_topic_score_codex":0.003350229,"about_ca_topic_score_gemma":0.846801,"teacher_disagreement_score":0.8434508,"about_ca_system_score_codex":3.753297e-7,"about_ca_system_score_gemma":0.00020395058,"threshold_uncertainty_score":0.66297966},"labels":[],"label_agreement":null},{"id":"W1976393269","doi":"10.1139/e03-003","title":"Lithospheric roots beneath western Laurentia: the geochemical signal in mantle garnets","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of New Brunswick; University of Victoria","funders":"","keywords":"Kimberlite; Geology; Laurentia; Archean; Lithosphere; Mantle (geology); Proterozoic; Craton; Geochemistry; Paleontology; Tectonics; Paleozoic","score_opus":0.01426437716535047,"score_gpt":0.19200901994826097,"score_spread":0.1777446427829105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976393269","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98653865,0.0030899148,0.000017736556,0.00107984,0.00015292941,0.000039422346,0.0000068974223,0.000002210902,0.009072406],"genre_scores_gemma":[0.9989427,0.000029877354,0.00040773515,0.00038197933,0.00006206081,1.7727925e-7,0.0000020875325,9.683757e-7,0.00017246047],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986002,0.00011159276,0.00031123104,0.00017913063,0.00030961705,0.0004882668],"domain_scores_gemma":[0.99909794,0.00014486551,0.00012525903,0.00008526793,0.00006130688,0.00048536042],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00085362734,0.00011217581,0.00019955379,0.000106450585,0.00023355302,0.00013382251,0.0004988673,0.000055895216,0.0114407735],"category_scores_gemma":[0.00015837658,0.00006136582,0.00010595496,0.0007539816,0.00047603817,0.00018109877,0.00000475671,0.00026465542,0.00006908822],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000025944287,0.000005395062,0.9957721,0.0000014637859,0.000006757323,0.000072949566,0.000060304727,0.0026671868,0.000030406445,0.000096935735,0.000080632584,0.0012032688],"study_design_scores_gemma":[0.00014632982,0.00015516806,0.9795884,0.000023234903,0.000016643442,0.00016387667,0.00024768163,0.0008576935,0.00040480972,0.00936401,0.008895876,0.00013626835],"about_ca_topic_score_codex":0.014558178,"about_ca_topic_score_gemma":0.56875855,"teacher_disagreement_score":0.5542004,"about_ca_system_score_codex":0.0000016371222,"about_ca_system_score_gemma":0.00043422612,"threshold_uncertainty_score":0.992004},"labels":[],"label_agreement":null},{"id":"W1976423556","doi":"10.1139/e01-012","title":"Holocene and latest Pleistocene fluctuations of Stutfield Glacier, Canadian Rockies","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Parks Canada","keywords":"Geology; Moraine; Tephra; Paleosol; Glacier; Younger Dryas; Paleontology; Radiocarbon dating; Glacial period; Geomorphology; Tephrochronology; Deglaciation; Pleistocene; Holocene; Physical geography; Tidewater glacier cycle; Loess; Volcano; Geography","score_opus":0.029565916434443413,"score_gpt":0.24231823666604457,"score_spread":0.21275232023160115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976423556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9829547,0.0035918406,0.0000062778727,0.0025474979,0.00026253433,0.000055326218,0.000025322597,0.0000018080041,0.010554728],"genre_scores_gemma":[0.9988807,0.00026398106,0.0003574737,0.00022122328,0.000043871314,1.2283357e-7,0.0000035251962,0.00000108064,0.00022802022],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988944,0.00007256746,0.00025614863,0.0001293324,0.00017134595,0.0004761943],"domain_scores_gemma":[0.9985871,0.0001968253,0.000113371454,0.00008154323,0.00015804022,0.0008631396],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00078444876,0.000083310064,0.0001885545,0.0006126362,0.0005798332,0.000055198958,0.00033170742,0.000085165426,0.0019893495],"category_scores_gemma":[0.00029131086,0.00006707787,0.00003616375,0.00051732076,0.0011103273,0.0002693681,0.0000036773702,0.00020130869,0.000023456952],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000056131435,0.0000015383866,0.9980909,0.0000033546285,0.000008728062,0.000113144204,0.00017723064,0.00048015933,0.0000014002958,0.0001797199,0.00009107826,0.0008471096],"study_design_scores_gemma":[0.00012879021,0.0003004687,0.9940253,0.000017719489,0.000008378631,0.00075248256,0.00031526457,0.00041925485,0.00002200347,0.00090230687,0.0030346254,0.00007338793],"about_ca_topic_score_codex":0.30683306,"about_ca_topic_score_gemma":0.98968273,"teacher_disagreement_score":0.68284965,"about_ca_system_score_codex":6.463527e-7,"about_ca_system_score_gemma":0.0025561198,"threshold_uncertainty_score":0.99892294},"labels":[],"label_agreement":null},{"id":"W1976563856","doi":"10.1139/e07-025","title":"Deciphering superimposed Ellesmerian and Eurekan deformation, Piper Pass area, northern Ellesmere Island (Nunavut)","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Sverdrup; Orogeny; Paleontology; Structural basin; Fold (higher-order function); Arctic; Paleozoic; Thrust fault; Cretaceous; Tectonics; Outcrop; Geomorphology; Oceanography","score_opus":0.02073201560382389,"score_gpt":0.1966441846629801,"score_spread":0.1759121690591562,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976563856","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99238974,0.0010015824,0.00021494357,0.0010189625,0.00028550345,0.00005647769,0.000011190842,0.0000040919726,0.0050174934],"genre_scores_gemma":[0.9989559,0.00010115204,0.0004251978,0.00037161633,0.000107653694,8.3611e-8,0.000004138055,0.0000014870235,0.000032754415],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886316,0.00003035311,0.00032349577,0.00013150087,0.00022818294,0.0004232771],"domain_scores_gemma":[0.999075,0.00008404605,0.00014007474,0.000054277312,0.000110269066,0.0005363559],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009657865,0.00010897841,0.00015870879,0.00014042042,0.00076560804,0.00017143115,0.00019686922,0.000050362512,0.00083033554],"category_scores_gemma":[0.000099995574,0.00007339128,0.00004279296,0.00031380804,0.00036442737,0.00048424478,0.000005263457,0.00012491796,0.000021373095],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008859429,0.0000016494553,0.98948693,0.0000019678926,0.000007168396,0.000041212177,0.000754812,0.0019484613,0.00001613383,0.000019597102,0.000066934066,0.0076462775],"study_design_scores_gemma":[0.00016008486,0.0002624533,0.9836997,0.000018332632,0.000006391125,0.0001325013,0.003175744,0.0006628886,0.000030420617,0.00024066879,0.011495224,0.000115582945],"about_ca_topic_score_codex":0.00681355,"about_ca_topic_score_gemma":0.9411289,"teacher_disagreement_score":0.9343153,"about_ca_system_score_codex":0.0000024543722,"about_ca_system_score_gemma":0.0002597452,"threshold_uncertainty_score":0.99980015},"labels":[],"label_agreement":null},{"id":"W1976597666","doi":"10.1139/e09-050","title":"An unusual hadrosaurid braincase from the Dinosaur Park Formation and the biostratigraphy of <i>Parasaurolophus</i> (Ornithischia: Lambeosaurinae) from southern Alberta","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Amgen (Canada); Royal Ontario Museum","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto Mississauga","keywords":"Holotype; Geology; Paleontology; Biostratigraphy; Context (archaeology); Cretaceous; Genus; Skull; Biology; Zoology","score_opus":0.010469513562868545,"score_gpt":0.19759644674027324,"score_spread":0.1871269331774047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976597666","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98637694,0.0041602775,0.00003146613,0.0071255188,0.000267682,0.0000893289,0.00033285926,0.0000026233922,0.0016132832],"genre_scores_gemma":[0.99786854,0.00006776857,0.00025184642,0.0015965644,0.00017523354,1.7597199e-7,0.000028972965,8.546631e-7,0.000010033002],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985827,0.00039157138,0.00037084933,0.0001641121,0.00018830062,0.00030244462],"domain_scores_gemma":[0.9984291,0.0007494417,0.00032766588,0.00015146272,0.0000587174,0.0002835738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009194183,0.00012472461,0.000219703,0.00010808699,0.00070349046,0.000085224325,0.00056939136,0.00008959337,0.00024053849],"category_scores_gemma":[0.00014242744,0.00006398395,0.000077689954,0.00026708303,0.0020054257,0.0005217271,0.0000028264642,0.00023586533,0.000011379551],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014612539,0.0000070095184,0.9933427,8.457688e-7,0.000022167837,0.000022756634,0.0022924575,0.0003030403,0.00006472244,0.00052130944,0.00019149481,0.0030853709],"study_design_scores_gemma":[0.00045257038,0.00046505334,0.9876686,0.000016276475,0.000029752293,0.00013540497,0.0013136406,0.0013998469,0.000055634082,0.007215115,0.0011577719,0.00009036861],"about_ca_topic_score_codex":0.12063982,"about_ca_topic_score_gemma":0.84888804,"teacher_disagreement_score":0.72824824,"about_ca_system_score_codex":6.680033e-7,"about_ca_system_score_gemma":0.0004203875,"threshold_uncertainty_score":0.88521594},"labels":[],"label_agreement":null},{"id":"W1977000408","doi":"10.1139/e02-046","title":"Structural analysis of supracrustal faults in the Charlevoix area, Quebec: relation to impact cratering and the St-Laurent fault system","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Centre de Géomatique du Québec; Institut National de la Recherche Scientifique","funders":"National Science Council","keywords":"Geology; Breccia; Devonian; Paleozoic; Impact crater; Fault (geology); Rift; Transform fault; Fault scarp; Impact structure; Extensional fault; Cataclastic rock; Seismology; Proterozoic; Sedimentary rock; Paleontology; Dike; Tectonics","score_opus":0.022511946292001345,"score_gpt":0.25373873681218556,"score_spread":0.23122679052018422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977000408","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99728703,0.00072621094,0.000009876054,0.0007333137,0.00013392376,0.0001072815,0.000029482931,8.237604e-7,0.00097206334],"genre_scores_gemma":[0.99983984,0.000007656899,0.000050288967,0.00005532014,0.000012247041,2.8056704e-7,0.0000040063687,5.6257744e-7,0.000029770887],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99852973,0.00048933376,0.0002955286,0.00011646616,0.00025364102,0.0003152935],"domain_scores_gemma":[0.9990737,0.0003841378,0.00015553265,0.000092841045,0.00008105776,0.00021277102],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027413163,0.0000791618,0.0002388366,0.0005725566,0.00036114798,0.00008913428,0.00032481726,0.00004825083,0.00047308838],"category_scores_gemma":[0.00027599378,0.00003741631,0.0000758846,0.0011277222,0.00062985346,0.00023425148,0.0000030769495,0.00020312866,0.0000033719707],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022445798,6.1486503e-7,0.96788484,0.0000034402692,0.00003970912,0.000029136369,0.0018429481,0.02973799,0.000001450369,0.00034388818,0.0000076132196,0.000085931744],"study_design_scores_gemma":[0.00018691823,0.00011104543,0.98658574,0.000018485418,0.000042271702,0.00020398315,0.003913463,0.008773261,0.000004699824,0.000068491434,0.00004633523,0.00004528786],"about_ca_topic_score_codex":0.05467158,"about_ca_topic_score_gemma":0.9164613,"teacher_disagreement_score":0.8617897,"about_ca_system_score_codex":0.0000015240912,"about_ca_system_score_gemma":0.00053388416,"threshold_uncertainty_score":0.95162344},"labels":[],"label_agreement":null},{"id":"W1977146972","doi":"10.1139/e03-072","title":"Felsenmeer persistence under non-erosive ice in the Torngat and Kaumajet mountains, Quebec and Labrador, as determined by soil weathering and cosmogenic nuclide exposure dating","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":131,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University; Université de Montréal; HEC Montréal","funders":"","keywords":"Geology; Cosmogenic nuclide; Glacial period; Weathering; Bedrock; Moraine; Glacier; Ice sheet; Geochemistry; Physical geography; Geomorphology; Cosmic ray","score_opus":0.01907635104045499,"score_gpt":0.2220486758652251,"score_spread":0.2029723248247701,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977146972","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927246,0.0045073116,0.0000043766377,0.0020948483,0.0000746387,0.00008177717,0.000010050293,0.0000013468705,0.000501061],"genre_scores_gemma":[0.99890643,0.0001905048,0.00020098269,0.0006026664,0.000023334922,3.2951738e-7,0.0000016475773,0.0000014616711,0.00007264563],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998922,0.00012343032,0.0001903499,0.00019352615,0.00017992832,0.00039079515],"domain_scores_gemma":[0.9992142,0.00026918616,0.0000926538,0.000069741734,0.00003854815,0.00031572033],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010909324,0.000104820865,0.00016134261,0.00015263203,0.00060618646,0.00020631736,0.00027236197,0.0000712538,0.0000813182],"category_scores_gemma":[0.00012334358,0.000071829236,0.000020408808,0.00022241953,0.0011538825,0.0004190278,0.000009796946,0.0002654514,0.000004359933],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007727753,0.0000018616222,0.9962607,0.0000069576618,0.000006075859,0.00011111299,0.0025354223,0.00034174146,0.00006267395,0.000038842165,0.000009030748,0.0006178369],"study_design_scores_gemma":[0.00040564986,0.00033082615,0.98466897,0.00006073275,0.000009715723,0.0014411515,0.011911384,0.00027554296,0.000057847505,0.0006033355,0.00012706053,0.000107782966],"about_ca_topic_score_codex":0.06064733,"about_ca_topic_score_gemma":0.9057241,"teacher_disagreement_score":0.84507674,"about_ca_system_score_codex":0.0000016464764,"about_ca_system_score_gemma":0.00061660085,"threshold_uncertainty_score":0.9456079},"labels":[],"label_agreement":null},{"id":"W1977428245","doi":"10.1139/e01-001","title":"The geochemical nature of the igneous rocks of the Sharbot Lake domain, Central Metasedimentary Belt, Ontario","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University; University of Windsor","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Silicic; Igneous rock; Geology; Geochemistry; Mafic; Basalt; Volcanic rock; Pyroclastic rock; Rhyolite; Continental crust; Petrology; Crust; Volcano","score_opus":0.007306111246031783,"score_gpt":0.17217398571609144,"score_spread":0.16486787447005966,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977428245","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893246,0.0020953696,0.0000013325272,0.004896026,0.00047007625,0.00006480671,0.000059445792,0.0000010730147,0.0030872487],"genre_scores_gemma":[0.99885833,0.000027916902,0.00010900556,0.0006737725,0.000088176566,1.2076904e-7,0.0000033471993,8.327077e-7,0.00023849777],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99831754,0.00010216948,0.00040040468,0.00014591815,0.00056558434,0.00046836337],"domain_scores_gemma":[0.99879354,0.00020837244,0.000330101,0.00018855382,0.000120430144,0.00035902445],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00061933306,0.00011575407,0.00021801393,0.000053718613,0.0006046458,0.000054363343,0.0013515952,0.00008051395,0.0044170166],"category_scores_gemma":[0.00018221725,0.000044739383,0.00030508652,0.000667181,0.001325215,0.00010456311,0.000025194047,0.0005050318,0.000002880007],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012189673,0.000007833567,0.9973924,0.0000016626217,0.00003509526,0.000014317013,0.00014065338,0.0013181797,0.00011560394,0.000051476527,0.00041522016,0.00049537007],"study_design_scores_gemma":[0.00011720341,0.00010856047,0.96629727,0.000031032298,0.000057081077,0.00013750356,0.0002644775,0.0001220811,0.0013907619,0.0075509124,0.023841217,0.000081883816],"about_ca_topic_score_codex":0.19804746,"about_ca_topic_score_gemma":0.9866199,"teacher_disagreement_score":0.78857243,"about_ca_system_score_codex":0.0000039589827,"about_ca_system_score_gemma":0.00094549713,"threshold_uncertainty_score":0.9964931},"labels":[],"label_agreement":null},{"id":"W1977474209","doi":"10.1139/e10-060","title":"An extensive late Cenozoic terrestrial record of multiple glaciations preserved in the Tintina Trench of west-central Yukon: stratigraphy, paleomagnetism, paleosols, and pollenThis is a companion paper to Barendregt et al., also in this issue.Geological Survey of Canada Contribution 20100035.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Lethbridge","funders":"","keywords":"Geology; Paleontology; Paleosol; Interglacial; Glacial period; Pleistocene; Unconformity; Loess; Early Pleistocene; Outwash plain; Sedimentary rock","score_opus":0.02506521356719242,"score_gpt":0.2549300833309231,"score_spread":0.22986486976373066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977474209","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99341166,0.00047413283,0.0000010741952,0.0049316552,0.00034046388,0.00022614014,0.00025972194,8.248163e-7,0.0003543153],"genre_scores_gemma":[0.9992831,0.00009246242,0.00019429739,0.00037186846,0.000018472168,7.1586527e-7,0.000025646952,9.948382e-7,0.000012478001],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99748063,0.000928709,0.00058116583,0.000201404,0.00033472845,0.00047335544],"domain_scores_gemma":[0.9981144,0.00085801526,0.0003023554,0.00014534369,0.00023340022,0.0003464565],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0026350918,0.0001144405,0.00036476288,0.00033596688,0.00015701864,0.00003105356,0.0004731913,0.000107251675,0.0017356328],"category_scores_gemma":[0.0010047494,0.00008009754,0.000042158317,0.00068267295,0.00074525276,0.00024725625,0.000007231701,0.00041013557,0.0000010278001],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007599162,0.000021266864,0.9980187,0.0000045046695,0.000007737794,0.000028242086,0.0006315488,0.00029390116,0.00010571549,0.000014612543,0.00055634545,0.00024142553],"study_design_scores_gemma":[0.0005488869,0.00074521516,0.9963784,0.00003523553,0.0000058908013,0.00003385875,0.0003412985,0.001148617,0.000064609805,0.000068427216,0.00054911996,0.00008040829],"about_ca_topic_score_codex":0.84113604,"about_ca_topic_score_gemma":0.9996565,"teacher_disagreement_score":0.15852048,"about_ca_system_score_codex":8.7319603e-7,"about_ca_system_score_gemma":0.0017567707,"threshold_uncertainty_score":0.9991769},"labels":[],"label_agreement":null},{"id":"W1977551390","doi":"10.1139/e07-010","title":"Integrated analyses constraining the provenance of sandstones, mudstones, and conglomerates, a case study: the Laojunshan conglomerate, Qilian orogen, northwest China","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Geology; Provenance; Terrane; Geochemistry; Conglomerate; Clastic rock; Mafic; Devonian; Subduction; Felsic; Petrology; Sedimentary rock; Paleontology; Tectonics","score_opus":0.04197970470606939,"score_gpt":0.2660938325711233,"score_spread":0.2241141278650539,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977551390","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939805,0.0041802237,0.000011265969,0.00069454993,0.00012862215,0.00015598132,0.000058225265,0.0000035761325,0.00078705384],"genre_scores_gemma":[0.99953574,0.00004090325,0.00013776775,0.00019667226,0.000055180724,3.5225597e-7,0.0000045441893,0.0000015368598,0.000027276672],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982746,0.00015823478,0.00057506136,0.00022069168,0.00031678347,0.0004545959],"domain_scores_gemma":[0.9983196,0.00041471317,0.00039417672,0.00013766007,0.00025856652,0.00047525717],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022816125,0.00017141017,0.00035499202,0.00020846304,0.00086850993,0.00017510289,0.0004648737,0.00004678044,0.000650499],"category_scores_gemma":[0.00030210245,0.000076177756,0.00009773551,0.0015013821,0.0024416214,0.00021533608,0.000010781039,0.00030789545,0.0000026657008],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001339495,0.000013290332,0.99026585,0.000003330706,0.00007318052,0.0010535609,0.0012730003,0.0005632174,0.00008901445,0.000042123967,0.000013890607,0.0065961387],"study_design_scores_gemma":[0.00029409127,0.0006550931,0.9670167,0.000029939889,0.00011637498,0.003950326,0.025371933,0.00094243867,0.00041920628,0.00030640516,0.00073542754,0.00016206327],"about_ca_topic_score_codex":0.30820954,"about_ca_topic_score_gemma":0.9280492,"teacher_disagreement_score":0.61983967,"about_ca_system_score_codex":0.000001787161,"about_ca_system_score_gemma":0.0007178409,"threshold_uncertainty_score":0.8996256},"labels":[],"label_agreement":null},{"id":"W1977770206","doi":"10.1139/e11-003","title":"The Krogh revolution: advances in the measurement of timeThis article is the Introduction to a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto; University of Alberta; Western University","funders":"","keywords":"Geochronology; Honour; Geology; Earth science; Earth history; Crust; Series (stratigraphy); Paleontology; Classics; Archaeology; History","score_opus":0.020247846821438993,"score_gpt":0.1904693371188506,"score_spread":0.17022149029741163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977770206","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95699817,0.0018504488,7.1535317e-7,0.0304045,0.00020158628,0.00014243039,0.0000112414555,5.927514e-7,0.010390305],"genre_scores_gemma":[0.9991722,0.00019622552,0.00013534573,0.00027875302,0.00018828988,9.4514496e-7,2.917531e-7,6.368081e-7,0.000027295411],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982447,0.00030497325,0.00056264247,0.00014115882,0.00048546775,0.0002610489],"domain_scores_gemma":[0.9989189,0.00028979484,0.0003484073,0.0001792858,0.00018690909,0.00007669498],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.004483951,0.00008444507,0.00023807198,0.00017995582,0.00014876845,0.0000221074,0.00078209216,0.000038175844,0.0062533626],"category_scores_gemma":[0.0010441164,0.000033684813,0.00008674254,0.0013830147,0.0012026791,0.00025081562,0.000011331526,0.00023300976,0.000004506691],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040106603,0.00010231632,0.9356783,0.000024524292,0.00004964607,0.000010972741,0.018843884,0.005540762,0.0011340244,0.0028895433,0.002890783,0.032434184],"study_design_scores_gemma":[0.00022228865,0.00112658,0.92816186,0.00010199737,0.000024167352,0.00001602319,0.013990105,0.00020612091,0.014828011,0.016275825,0.024939064,0.00010795024],"about_ca_topic_score_codex":0.022672921,"about_ca_topic_score_gemma":0.5378288,"teacher_disagreement_score":0.51515585,"about_ca_system_score_codex":0.0000049567757,"about_ca_system_score_gemma":0.0002890603,"threshold_uncertainty_score":0.9946551},"labels":[],"label_agreement":null},{"id":"W1977846188","doi":"10.1139/e05-081","title":"Cretaceous fossil birds from Hornby Island (British Columbia)","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Cretaceous; Mesozoic; Paleontology; Geology; Oceanography; Fossil Record; Structural basin","score_opus":0.014015588366953543,"score_gpt":0.1964363428820468,"score_spread":0.18242075451509326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977846188","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96704423,0.016722852,0.000033120097,0.00094087573,0.0009262677,0.00003945378,0.00021777485,0.000006034435,0.014069409],"genre_scores_gemma":[0.99671924,0.00013146053,0.0014532848,0.00042978028,0.00050880987,1.1244938e-7,0.0000074668287,0.0000012305213,0.0007486222],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99877733,0.00009827642,0.00028480144,0.000187566,0.00018330796,0.00046871713],"domain_scores_gemma":[0.99895936,0.00013428112,0.00015514053,0.000078668825,0.000078315024,0.00059420685],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005326517,0.00007364392,0.00019635048,0.00011615617,0.0006883209,0.00027710194,0.00045876828,0.00010714707,0.013053855],"category_scores_gemma":[0.00013370944,0.00008382562,0.00007175714,0.00025807138,0.0009506919,0.0004610571,0.0000028959237,0.00020101681,0.00015884762],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000038988615,0.0000025739985,0.96390873,6.388212e-7,0.000011885222,0.00015062444,0.000069206675,0.00060146744,0.000004299972,0.0000034622976,0.0040355073,0.031207724],"study_design_scores_gemma":[0.00016328224,0.00022134643,0.88059103,0.000018116823,0.000009406238,0.0007492369,0.00010474707,0.0009092862,0.000002705064,0.0009373782,0.11618749,0.000105970714],"about_ca_topic_score_codex":0.3381546,"about_ca_topic_score_gemma":0.99879295,"teacher_disagreement_score":0.6606383,"about_ca_system_score_codex":0.000002285075,"about_ca_system_score_gemma":0.0013033292,"threshold_uncertainty_score":0.98784834},"labels":[],"label_agreement":null},{"id":"W1977867465","doi":"10.1139/e04-044","title":"A probable late Neoproterozoic age for the Kennedy Channel and Ella Bay formations, northeastern Ellesmere Island and its implications for passive margin history of the Canadian Arctic","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Geology; Paleontology; Unconformity; Laurentia; Bay; Paleozoic; Arctic; Passive margin; Gondwana; Sedimentary rock; Structural basin; Stratigraphic section; Rift; Oceanography","score_opus":0.03414287270169061,"score_gpt":0.19680458246840393,"score_spread":0.16266170976671332,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977867465","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9440893,0.007062858,0.00039511698,0.04582268,0.000562635,0.0012367544,0.00027310994,0.000002149493,0.0005553957],"genre_scores_gemma":[0.9989854,0.00012354187,0.00019196852,0.0004547162,0.000043442567,0.0000066996263,0.0000036135143,0.0000011385996,0.00018944341],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99937594,0.000018421653,0.00017965041,0.000093150076,0.000080012476,0.0002528286],"domain_scores_gemma":[0.999299,0.000094952695,0.00016227955,0.00005480131,0.00014911304,0.0002398626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003615778,0.000067408975,0.00010367531,0.00007739973,0.000995239,0.00007851727,0.00019270163,0.000030830943,0.000025800058],"category_scores_gemma":[0.000115114475,0.000035691715,0.00003892388,0.0001266683,0.00031551428,0.00021360074,0.000004483847,0.000066682915,9.077483e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000071417875,0.000019778043,0.82995,0.00021276028,0.00014932071,0.000009340052,0.015607393,0.11698994,0.000031647945,0.007950723,0.0020892483,0.02691848],"study_design_scores_gemma":[0.00041330446,0.00041785339,0.9499765,0.00006569686,0.0000342718,0.00005008007,0.00085075287,0.0049531497,0.000006273993,0.010925004,0.032196652,0.00011044591],"about_ca_topic_score_codex":0.13232592,"about_ca_topic_score_gemma":0.9958248,"teacher_disagreement_score":0.8634989,"about_ca_system_score_codex":0.000013248011,"about_ca_system_score_gemma":0.0010840954,"threshold_uncertainty_score":0.873452},"labels":[],"label_agreement":null},{"id":"W1977977622","doi":"10.1139/e10-012","title":"Late Quaternary paleoenvironments and growth of intrusive ice in eastern Beringia (Eagle River valley, northern Yukon, Canada)","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Space Agency; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Beringia; Glacial period; Radiocarbon dating; Pleistocene; Fluvial; Quaternary; Holocene; Macrofossil; Permafrost; Geomorphology; Paleontology; Oceanography","score_opus":0.01670935633772403,"score_gpt":0.192557345562074,"score_spread":0.17584798922434997,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977977622","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976737,0.00039168887,9.730954e-7,0.00039994044,0.0005001458,0.00005211109,0.00017556608,7.3878886e-7,0.0008051495],"genre_scores_gemma":[0.99952453,0.00007765603,0.000079174584,0.0001700905,0.0000827684,9.791059e-8,0.000007619119,0.0000021927221,0.000055879987],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99893486,0.00003402888,0.0002790152,0.00014242901,0.0002868191,0.0003228478],"domain_scores_gemma":[0.9991556,0.00006846145,0.00019018915,0.00007233123,0.00004991867,0.00046350315],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003742433,0.00010283075,0.00017765822,0.00019942307,0.00013798522,0.000050595816,0.00030914522,0.00004390018,0.0013233663],"category_scores_gemma":[0.00004376568,0.000083335726,0.000027271959,0.00018976883,0.0004666859,0.00029399805,0.000009098333,0.00020045595,0.000010309573],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009393626,0.0000024153028,0.9974882,0.000007749193,0.000005282397,0.00013466558,0.0009277219,0.00016455086,0.0001221941,0.0000036100853,0.000014206623,0.0011200205],"study_design_scores_gemma":[0.00022968167,0.00011535004,0.9975709,0.000038358165,0.000005672445,0.000073938456,0.00028538966,0.00083830196,0.00007859407,0.00016085239,0.0005023439,0.00010062972],"about_ca_topic_score_codex":0.9192924,"about_ca_topic_score_gemma":0.99964815,"teacher_disagreement_score":0.08035572,"about_ca_system_score_codex":0.0000026739035,"about_ca_system_score_gemma":0.00077320274,"threshold_uncertainty_score":0.99958956},"labels":[],"label_agreement":null},{"id":"W1978042482","doi":"10.1139/e07-027","title":"Lithostratigraphy and chemostratigraphy of the Mesoproterozoic Sibley Group, northwestern Ontario, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Lakehead University; Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada; Lakehead University","keywords":"Geology; Siliciclastic; Evaporite; Unconformity; Geochemistry; Paleontology; Sabkha; Sedimentary rock; Marine transgression; Detritus; Subaerial; Proterozoic; Arenite; Lithostratigraphy; Stromatolite; Facies; Clastic rock; Structural basin; Carbonate","score_opus":0.01319220855542697,"score_gpt":0.1837316478940082,"score_spread":0.17053943933858123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978042482","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99366575,0.0011014797,0.000018094497,0.00029393434,0.0002637367,0.0000652264,0.00002024511,9.769091e-7,0.004570574],"genre_scores_gemma":[0.99904364,0.000010654484,0.0006435487,0.00024538903,0.000024661771,6.010985e-8,0.0000011187054,5.4546416e-7,0.000030401405],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989898,0.000023532128,0.0003277642,0.000090427005,0.00029019124,0.00027824534],"domain_scores_gemma":[0.9991356,0.00008382628,0.00023177029,0.000071530034,0.00010995543,0.0003673279],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007002112,0.00008361683,0.00012987174,0.0001496934,0.0003694807,0.000085717395,0.0003482335,0.00003426992,0.00052064477],"category_scores_gemma":[0.00002974393,0.000047628855,0.000051045005,0.0005972142,0.0005049154,0.000322238,0.000003053439,0.00015223323,4.3524176e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000029505977,0.000001288564,0.9971867,0.0000067018154,0.000005312234,0.000008772072,0.0003258374,0.00009377655,0.000004625872,0.000080069076,0.000029810304,0.0022541622],"study_design_scores_gemma":[0.00006799456,0.00018587608,0.9945668,0.000029720013,0.00000642726,0.000089648136,0.0005527896,0.000016496571,0.00019106062,0.0006067113,0.003622975,0.00006352311],"about_ca_topic_score_codex":0.9873599,"about_ca_topic_score_gemma":0.9999847,"teacher_disagreement_score":0.012624746,"about_ca_system_score_codex":0.0000014004088,"about_ca_system_score_gemma":0.002458086,"threshold_uncertainty_score":0.5700695},"labels":[],"label_agreement":null},{"id":"W1978492882","doi":"10.1139/e99-121","title":"Modelling 3D architecture of western Grenville from surface geology, xenoliths, styles of magma emplacement, and Lithoprobe reflectors","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Centre de Géomatique du Québec; Institut National de la Recherche Scientifique; Geological Survey of Canada","funders":"","keywords":"Geology; Felsic; Mafic; Crust; Underplating; Ultramafic rock; Petrology; Pluton; Xenolith; Gneiss; Geochemistry; Magma; Mylonite; Tectonics; Seismology; Metamorphic rock; Basalt; Lithosphere; Shear zone; Volcano","score_opus":0.01999691682316052,"score_gpt":0.20571396852055954,"score_spread":0.18571705169739902,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978492882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99402934,0.0033124527,0.0000838938,0.00044996635,0.000041490694,0.000037807487,0.000082345425,0.0000016834465,0.0019610303],"genre_scores_gemma":[0.9939264,0.0001749721,0.0056549986,0.000078016354,0.000037047175,3.939341e-8,0.00000518616,0.0000010999104,0.00012222774],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987738,0.000082071245,0.00039852838,0.0001914258,0.00023741306,0.0003167568],"domain_scores_gemma":[0.9990658,0.00014623403,0.00021898073,0.0000894873,0.00007376472,0.00040573443],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00040494715,0.000115078925,0.0003251351,0.00014337302,0.00014280008,0.000033185323,0.00032102474,0.000062697385,0.0076491367],"category_scores_gemma":[0.000035403413,0.000075723074,0.00007764256,0.00035463256,0.00087781687,0.00010905745,0.000006509988,0.00015894063,0.000007402074],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020568908,0.0000043279074,0.79382205,0.0000057440607,0.000020898287,0.00000998103,0.00020673362,0.2021066,0.00008450126,0.000008260001,0.0000049325095,0.0037054194],"study_design_scores_gemma":[0.0004740731,0.0013122148,0.94872755,0.00014090723,0.00009731292,0.00010427169,0.00067074574,0.0300693,0.0012572743,0.012646219,0.004146824,0.0003533116],"about_ca_topic_score_codex":0.13124146,"about_ca_topic_score_gemma":0.34623972,"teacher_disagreement_score":0.21499826,"about_ca_system_score_codex":7.9887053e-7,"about_ca_system_score_gemma":0.00020566052,"threshold_uncertainty_score":0.993258},"labels":[],"label_agreement":null},{"id":"W1978709100","doi":"10.1139/cjes-2014-0204","title":"Crustal magnetic anomaly and Curie surface beneath Tarim Basin, China, and its adjacent area","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Geology; Magnetic anomaly; Structural basin; Tectonics; Heat flow; Curie temperature; Curie; Anomaly (physics); Geophysics; Geomorphology; Earth's magnetic field; Tarim basin; Petrology; Seismology; Magnetic field; Geochemistry; Thermal; Condensed matter physics","score_opus":0.01953102982784411,"score_gpt":0.21848639440960985,"score_spread":0.19895536458176574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978709100","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9405952,0.05589134,0.000008978651,0.00085093454,0.00023617441,0.00006898537,0.000030336118,0.000001327666,0.002316696],"genre_scores_gemma":[0.99744385,0.00087870023,0.00074924796,0.00014430564,0.00009847385,4.5690146e-7,0.0000021597514,0.0000051001384,0.0006777036],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990648,0.00004407794,0.00018724518,0.00021007626,0.00016342102,0.0003303507],"domain_scores_gemma":[0.9989418,0.00000993179,0.000095904456,0.00008163799,0.00013710938,0.0007336307],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040055998,0.00013293319,0.00016343925,0.00008368007,0.00023131688,0.00010567288,0.00017108345,0.000061122235,0.0000433112],"category_scores_gemma":[0.00013368175,0.00011059171,0.000032345477,0.00012029104,0.00043267137,0.000021884298,0.000041999403,0.00008185275,0.0000018727768],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005677392,0.000028950915,0.97560966,0.00003682503,0.00004606643,0.00025191595,0.0017861775,0.0005452431,0.011281134,0.0003097496,0.005595187,0.0044523096],"study_design_scores_gemma":[0.0009979812,0.004702628,0.9238795,0.000059032835,0.000046427333,0.0010807904,0.00111425,0.00021331589,0.0023103813,0.00022557452,0.06499415,0.0003759634],"about_ca_topic_score_codex":0.001614775,"about_ca_topic_score_gemma":0.03601397,"teacher_disagreement_score":0.059398964,"about_ca_system_score_codex":0.0000020261534,"about_ca_system_score_gemma":0.0007744531,"threshold_uncertainty_score":0.98157626},"labels":[],"label_agreement":null},{"id":"W1978775989","doi":"10.1139/e00-067","title":"Nd and Pb isotopes from the Lake of the Woods greenstone belt, northwestern Ontario: implications for mantle evolution and the formation of crust in the southern Superior Province","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Mantle (geology); Zircon; Greenstone belt; Pluton; Crustal recycling; Felsic; Mantle wedge; Ultramafic rock; Detritus; Crust; Partial melting; Continental crust; Archean; Subduction; Petrology; Mafic; Paleontology","score_opus":0.012759013332397406,"score_gpt":0.1829921991704555,"score_spread":0.1702331858380581,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978775989","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928981,0.000852494,0.00002062188,0.005638846,0.00001881324,0.00015908177,0.00015749196,4.174092e-7,0.0002541108],"genre_scores_gemma":[0.9995727,0.000020328938,0.00009620666,0.00022697014,0.0000203665,8.8154565e-7,0.000003932395,3.9827196e-7,0.000058233236],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993668,0.0000774511,0.00022670912,0.000074728996,0.00012406,0.00013021723],"domain_scores_gemma":[0.9994008,0.00026972627,0.00013649512,0.000086788095,0.000048134694,0.000058067246],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00062874984,0.000052277843,0.00011307867,0.000029860534,0.0003521992,0.000051983578,0.00035142002,0.000021908088,0.00031789532],"category_scores_gemma":[0.000041125535,0.000018875737,0.00005322592,0.00021341756,0.0009643524,0.00014704057,0.0000049015143,0.00008941012,7.981985e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013347617,0.0000026044079,0.9920688,0.0000020652963,0.0000047041676,2.0602775e-7,0.002271022,0.00039271303,0.000017302631,0.00006993307,0.000010636509,0.0051466324],"study_design_scores_gemma":[0.00016599626,0.00006040032,0.992043,0.000016486905,0.000024284596,0.00001586206,0.001425535,0.0006947089,0.000012977457,0.004973627,0.00053784257,0.000029277111],"about_ca_topic_score_codex":0.562887,"about_ca_topic_score_gemma":0.9982516,"teacher_disagreement_score":0.4353646,"about_ca_system_score_codex":0.0000012051265,"about_ca_system_score_gemma":0.00022085028,"threshold_uncertainty_score":0.44002378},"labels":[],"label_agreement":null},{"id":"W1979098181","doi":"10.1139/e04-068","title":"Timing and duration of melting in the mid orogenic crust: Constraints from UPb (SHRIMP) data, Muskoka and Shawanaga domains, Grenville Province, Ontario","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Dalhousie University","funders":"Norges Geologiske Undersøkelse; Natural Sciences and Engineering Research Council of Canada; Norges Forskningsråd; Killam Trusts; Dalhousie University","keywords":"Geology; Metamorphism; Pegmatite; Geochemistry; Zircon; Gneiss; Protolith; Orogeny; Anatexis; Crust; Partial melting; Batholith; Precambrian; Migmatite; Petrology; Metamorphic rock; Tectonics; Seismology","score_opus":0.029063410840986206,"score_gpt":0.20370486112326228,"score_spread":0.17464145028227607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979098181","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966,0.001172418,0.000013562504,0.0010531568,0.000047863945,0.000052774194,0.000051569652,7.648649e-7,0.0010079056],"genre_scores_gemma":[0.9978652,0.000031679345,0.0018721729,0.00018070203,0.000032004264,6.567769e-8,0.00001213325,5.0957635e-7,0.0000055314704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989966,0.000051398943,0.00032075256,0.00018309824,0.0002198366,0.00022828227],"domain_scores_gemma":[0.9993195,0.00014059326,0.0001855189,0.00009148712,0.00003320941,0.00022967233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008797393,0.0000794177,0.00017330039,0.00012964864,0.00023172518,0.00010666283,0.00037966145,0.000036779744,0.00086026307],"category_scores_gemma":[0.00016758524,0.000046852994,0.00002810122,0.00026178794,0.00083801936,0.00029690578,0.000013020189,0.00015601711,0.0000022271677],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000043634504,0.0000038067058,0.99152935,0.0000031380237,0.000010110696,0.00005847717,0.000765881,0.00091215654,0.0000866813,0.000060172304,0.0000042201277,0.0065616593],"study_design_scores_gemma":[0.0002617303,0.00012557475,0.99193686,0.0000479315,0.000026116048,0.000096008356,0.0015233272,0.00065105804,0.00012905973,0.004781775,0.0003360566,0.000084490464],"about_ca_topic_score_codex":0.49973464,"about_ca_topic_score_gemma":0.99080545,"teacher_disagreement_score":0.49107078,"about_ca_system_score_codex":0.0000025853133,"about_ca_system_score_gemma":0.00079399697,"threshold_uncertainty_score":0.94192773},"labels":[],"label_agreement":null},{"id":"W1979141747","doi":"10.1139/e06-054","title":"Rocky shoreline deposits in the Lower Silurian (upper Llandovery, Telychian) Chicotte Formation, Anticosti Island, Quebec","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Geology; Unconformity; Paleontology; Sea level; Sedimentary depositional environment; Subaerial; Facies; Geomorphology; Tectonics; Oceanography; Structural basin","score_opus":0.00980013308199836,"score_gpt":0.19712535465569914,"score_spread":0.18732522157370077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979141747","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96496975,0.006098366,0.00008644694,0.002647949,0.00065914483,0.00009580899,0.000029119117,0.0000029246028,0.025410507],"genre_scores_gemma":[0.9990194,0.00003071449,0.0003086866,0.00034485545,0.00023361584,1.8820943e-7,0.0000045944385,6.426816e-7,0.000057303183],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99853593,0.00012555065,0.00042485294,0.00013641664,0.00032030387,0.00045697106],"domain_scores_gemma":[0.9992948,0.00013166,0.00018658848,0.000099681136,0.00006472126,0.00022250997],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00091636635,0.00012581679,0.00018274262,0.0003877319,0.0005588869,0.00028313696,0.00055395195,0.000074068514,0.00028538928],"category_scores_gemma":[0.00006395337,0.00007643917,0.00009439325,0.000551662,0.00040103737,0.000739303,7.0443e-7,0.00025389728,0.000014690906],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014392203,0.000009694596,0.9902993,0.0000028715551,0.0000045905686,0.00014430261,0.00034261856,0.0008917078,0.000005163533,0.00017340541,0.00095611025,0.0071558654],"study_design_scores_gemma":[0.00026344354,0.0002333549,0.99331886,0.000038433787,0.000009158925,0.0004825579,0.00027966127,0.000639534,0.000019686944,0.00094275805,0.0036606358,0.000111927584],"about_ca_topic_score_codex":0.11975138,"about_ca_topic_score_gemma":0.99568075,"teacher_disagreement_score":0.87592936,"about_ca_system_score_codex":0.0000014965019,"about_ca_system_score_gemma":0.00063433766,"threshold_uncertainty_score":0.88611025},"labels":[],"label_agreement":null},{"id":"W1979273505","doi":"10.1139/e06-116","title":"A diverse late-glacial (Mackinaw Phase) biota from Leamington, Ontario","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia, Okanagan Campus; University of Toronto; Stornoway Diamond (Canada); University of Waterloo","funders":"University of Guelph","keywords":"Biota; Glacial period; Geology; Tundra; Range (aeronautics); Boreal; Taxon; Ice age; Stadial; Ecology; Chironomidae; Paleontology; Oceanography; Arctic; Biology","score_opus":0.03856992152712291,"score_gpt":0.26406046924257076,"score_spread":0.22549054771544785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979273505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98236156,0.0006436625,0.000033823402,0.00040012773,0.0011745084,0.00005513945,0.000028798693,0.000003864722,0.015298547],"genre_scores_gemma":[0.99832016,0.000012021532,0.00068567414,0.00027663802,0.0001821432,3.570529e-8,0.0000094947345,0.0000012907987,0.00051255757],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983279,0.00008225473,0.00033212107,0.00020345539,0.00031816014,0.00073612493],"domain_scores_gemma":[0.99846256,0.00027026425,0.00016841483,0.000100537036,0.00011698255,0.0008812494],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017980564,0.000117719115,0.00022182772,0.00048267102,0.0007307083,0.000108486805,0.00060301565,0.00012547804,0.012495278],"category_scores_gemma":[0.00014497983,0.000092982205,0.000083620915,0.00043040796,0.001258509,0.00037063853,0.0000070942497,0.00043027272,0.0003021302],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041104897,0.000006309938,0.9949084,0.0000010882162,0.000016262498,0.00068647595,0.00091192266,0.000114078124,0.000010303948,0.000036340185,0.00010846354,0.0031592464],"study_design_scores_gemma":[0.00040548318,0.00046702605,0.98476213,0.000017652374,0.000013145072,0.00016501572,0.00058169634,0.000099528734,0.00014573951,0.0006658995,0.012556847,0.00011984568],"about_ca_topic_score_codex":0.35376185,"about_ca_topic_score_gemma":0.99791837,"teacher_disagreement_score":0.6441565,"about_ca_system_score_codex":0.0000017655606,"about_ca_system_score_gemma":0.002567916,"threshold_uncertainty_score":0.98840743},"labels":[],"label_agreement":null},{"id":"W1979378635","doi":"10.1139/e00-039","title":"Petrology, palynology, coal facies, and depositional environments of an Upper Carboniferous coal seam, Minto Coalfield, New Brunswick, Canada","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Petro-Canada","funders":"","keywords":"Maceral; Liptinite; Inertinite; Geology; Petrography; Vitrinite; Sedimentary depositional environment; Mire; Facies; Geochemistry; Palynology; Coal measures; Paleontology; Peat; Sedimentary rock; Pollen; Archaeology; Ecology","score_opus":0.012133308380604828,"score_gpt":0.20530081368955538,"score_spread":0.19316750530895055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979378635","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931241,0.0023108704,0.000006401028,0.0013807509,0.00024972815,0.000061276485,0.000045392313,0.0000015884216,0.0028198767],"genre_scores_gemma":[0.99835235,0.00009929759,0.00041509757,0.0004956068,0.00006490007,8.81328e-8,0.000016026674,0.0000016875682,0.0005549593],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983655,0.00018746857,0.0003352502,0.00022390208,0.0003146781,0.0005731789],"domain_scores_gemma":[0.9986006,0.00019242849,0.00012420415,0.000107751366,0.00003112747,0.0009438694],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004995437,0.00013237222,0.00027906193,0.00020700536,0.00041806858,0.000040908984,0.00044021851,0.00014233409,0.0048927413],"category_scores_gemma":[0.000047967253,0.000110564746,0.000041452844,0.00013925497,0.001735352,0.000209228,0.000006168912,0.00031590593,0.000016096013],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037284135,0.0000042532165,0.99693364,0.0000030643246,0.000022601633,0.00024704472,0.00012451819,0.0016340243,0.0000034226202,0.00006362495,0.00011595902,0.00081058434],"study_design_scores_gemma":[0.00034069744,0.0006652623,0.99121493,0.000009976699,0.000015937076,0.0020218296,0.00027149185,0.0005615808,0.00005163034,0.00021325014,0.0045214226,0.000112009904],"about_ca_topic_score_codex":0.87565076,"about_ca_topic_score_gemma":0.9990025,"teacher_disagreement_score":0.123351745,"about_ca_system_score_codex":0.0000016808649,"about_ca_system_score_gemma":0.008555813,"threshold_uncertainty_score":0.99706477},"labels":[],"label_agreement":null},{"id":"W1979412245","doi":"10.1139/e01-033","title":"Conodonts from the Kechika Formation and Road River Group (Lower to Upper Ordovician) of the Cassiar Terrane, northern British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Geological Society of America","keywords":"Conodont; Terrane; Geology; Paleontology; Ordovician; Paleozoic; Biostratigraphy; Group (periodic table); Facies; Stratigraphy; Laurentia; Tectonics; Structural basin","score_opus":0.013096107914320192,"score_gpt":0.18748247894260903,"score_spread":0.17438637102828883,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979412245","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98990923,0.0027669335,0.00001384554,0.00086991687,0.00046082455,0.00009784806,0.000071348106,0.000001531396,0.005808502],"genre_scores_gemma":[0.99920744,0.00004665215,0.00020161134,0.0004282227,0.00006340255,1.6598645e-7,7.7158603e-7,5.202786e-7,0.000051193474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990812,0.0000975253,0.00025038238,0.00011011594,0.00021006528,0.0002507285],"domain_scores_gemma":[0.99930394,0.00009101547,0.00017293537,0.00009352883,0.000064006934,0.00027457418],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047116054,0.00006255733,0.00013741384,0.000050729508,0.00074683427,0.00025518425,0.00044491558,0.000049778737,0.00039214522],"category_scores_gemma":[0.00007777032,0.000046119512,0.000067254034,0.00028822877,0.00079714064,0.00044144987,0.000001852783,0.00013822755,0.0000032177843],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000044608896,0.0000019362253,0.9260514,7.2879135e-7,0.000008073372,0.000024845021,0.00067812914,0.000028848433,0.000005431243,0.000003439537,0.00015593972,0.07303679],"study_design_scores_gemma":[0.00012855632,0.00014467344,0.9949154,0.00005445027,0.00001138052,0.00023309761,0.00047428027,0.00013769201,0.0000021074566,0.0004055659,0.0034277607,0.00006499982],"about_ca_topic_score_codex":0.5372696,"about_ca_topic_score_gemma":0.99884045,"teacher_disagreement_score":0.46157083,"about_ca_system_score_codex":0.0000011098532,"about_ca_system_score_gemma":0.0002876379,"threshold_uncertainty_score":0.5744121},"labels":[],"label_agreement":null},{"id":"W1979429290","doi":"10.1139/e06-076","title":"The morphology of the terminal phalanges in Permo-Carboniferous synapsids: an evolutionary perspective","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Amgen (Canada)","funders":"","keywords":"Amniote; Biology; Tetrapod (structure); Claw; Paleontology; Manus; Anatomy; Vertebrate; Ecology","score_opus":0.016795241463290193,"score_gpt":0.2375843066952702,"score_spread":0.22078906523198,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979429290","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98535216,0.0061019906,0.000006320749,0.001578824,0.0008218268,0.000058100934,0.000017648297,0.0000014211117,0.0060616955],"genre_scores_gemma":[0.9994857,0.000041095205,0.00017135906,0.00013260123,0.00011581736,9.8958836e-8,8.1111347e-7,7.6323505e-7,0.00005179093],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987556,0.0002235126,0.00028812865,0.00013642943,0.00016554122,0.00043084277],"domain_scores_gemma":[0.9990369,0.00033021191,0.0001963192,0.000109618755,0.0001157542,0.0002111911],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017325437,0.00007919722,0.00014067742,0.00021782154,0.00051752786,0.000015320084,0.00067044457,0.00008257789,0.00018224619],"category_scores_gemma":[0.00025375572,0.000042607626,0.000058584104,0.00039465047,0.0027098588,0.00020519321,0.0000053437825,0.00025043302,0.0000056455133],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030532407,0.0000050284093,0.99644977,7.618352e-7,0.0000067666497,0.00014077802,0.0004539175,0.0003872978,0.000029682553,0.0012249197,0.000032667867,0.0012379071],"study_design_scores_gemma":[0.00010658339,0.00037713852,0.9894234,0.000011597098,0.0000057560815,0.0019778255,0.004137326,0.00026640546,0.000016758177,0.003163139,0.0004589834,0.00005507238],"about_ca_topic_score_codex":0.028284915,"about_ca_topic_score_gemma":0.83576477,"teacher_disagreement_score":0.80747986,"about_ca_system_score_codex":0.0000073388373,"about_ca_system_score_gemma":0.0014025857,"threshold_uncertainty_score":0.9984588},"labels":[],"label_agreement":null},{"id":"W1979468191","doi":"10.1139/e02-052","title":"Sensitive high resolution ion microprobe (SHRIMP) detrital zircon geochronology provides new evidence for a hidden Neoproterozoic foreland basin to the Grenville Orogen in the eastern Midwest, U.S.A.","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Conselho Nacional de Desenvolvimento Científico e Tecnológico","keywords":"Zircon; Geochronology; Geology; Foreland basin; Geochemistry; Rodinia; Paleocurrent; Craton; Paleontology; Sedimentary rock; Rift; Structural basin; Clastic rock; Tectonics","score_opus":0.045738236621372316,"score_gpt":0.2208575553259846,"score_spread":0.17511931870461228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979468191","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96902657,0.0031278161,0.0003662248,0.02675473,0.0001781971,0.00034980057,0.000025886962,0.000002305866,0.0001684473],"genre_scores_gemma":[0.9959757,0.00004212392,0.00231549,0.0012723379,0.0002766527,0.0000019541262,0.0000031719187,0.0000014096534,0.000111193396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99838454,0.00021894433,0.00033895203,0.00025524068,0.00027068856,0.0005316286],"domain_scores_gemma":[0.99877137,0.00048396588,0.00017140288,0.00012701868,0.00008716885,0.00035907817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013008957,0.00013331923,0.00021472241,0.00022942822,0.00044205048,0.00018515998,0.00064869656,0.000069661786,0.00066621735],"category_scores_gemma":[0.000690659,0.00006726239,0.00010730117,0.00067249953,0.0003830587,0.00023526722,0.000011617704,0.00020714628,0.00007280985],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010412912,0.000021722233,0.9283929,0.000017723245,0.000041598287,0.00017693246,0.0025993397,0.0060839313,0.0009611937,0.00014318521,0.0027987882,0.05865854],"study_design_scores_gemma":[0.00062447926,0.0025556746,0.9643898,0.00022320409,0.00007826541,0.0006345465,0.0014974796,0.009630921,0.001820333,0.007277795,0.010916259,0.00035121894],"about_ca_topic_score_codex":0.114845075,"about_ca_topic_score_gemma":0.74694854,"teacher_disagreement_score":0.63210344,"about_ca_system_score_codex":0.0000059044005,"about_ca_system_score_gemma":0.00026800565,"threshold_uncertainty_score":0.89104927},"labels":[],"label_agreement":null},{"id":"W1979482254","doi":"10.1139/e00-049","title":"Evolution and extinction of the North American <i>Hiscobeccus</i> brachiopod Fauna during the Late Ordovician","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Paleontology; Siliciclastic; Ordovician; Geology; Fauna; Glacial period; Gondwana; Paleozoic; Carbonate; Extinction (optical mineralogy); Laurentia; Structural basin; Ecology; Sedimentary depositional environment; Biology","score_opus":0.009656085306815911,"score_gpt":0.19284456571228573,"score_spread":0.1831884804054698,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979482254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98966163,0.0022859564,0.000010100644,0.0007763512,0.0002664759,0.000052997402,0.000012873213,0.000001914542,0.0069316775],"genre_scores_gemma":[0.999702,0.00006690284,0.000059373328,0.00007601288,0.000059033202,8.182505e-8,1.602117e-7,4.1002755e-7,0.000036073485],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991155,0.00011230604,0.00022220013,0.00009087156,0.0001979989,0.0002611182],"domain_scores_gemma":[0.99929255,0.000067892,0.0002982254,0.000089614965,0.000048128422,0.00020356843],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045072424,0.000074314354,0.00012268953,0.00014463344,0.0009478356,0.000059333335,0.00034416857,0.000021240545,0.000054081487],"category_scores_gemma":[0.000058087702,0.000039647995,0.000062017476,0.00072439795,0.001626873,0.0003004363,0.0000013321923,0.00017778114,0.0000011224279],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000071679096,0.0000013833034,0.98906094,0.0000016973291,0.0000061571423,0.0000069859066,0.00019884178,0.00061209715,0.000019469218,0.000027715576,0.000004042868,0.010053523],"study_design_scores_gemma":[0.0000763366,0.00012965304,0.99816835,0.000013969671,0.00001065294,0.0002083744,0.00045685805,0.00022881074,0.000012439132,0.00015080729,0.0004914793,0.000052285886],"about_ca_topic_score_codex":0.025099663,"about_ca_topic_score_gemma":0.9395308,"teacher_disagreement_score":0.91443115,"about_ca_system_score_codex":0.0000012894882,"about_ca_system_score_gemma":0.00042956008,"threshold_uncertainty_score":0.98139226},"labels":[],"label_agreement":null},{"id":"W1979697710","doi":"10.1139/e06-023","title":"Structure of the Archean English River subprovince: implications for the tectonic evolution of the western Superior Province, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Orogeny; Geology; Metamorphism; Archean; Subduction; Geochemistry; Foreland basin; Tectonics; Magmatism; Syncline; Terrane; Seismology","score_opus":0.006942889789207313,"score_gpt":0.16963475109952905,"score_spread":0.16269186131032173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979697710","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99466777,0.0008542168,0.0000155088,0.0035721627,0.0002345333,0.00014969177,0.00026618256,8.0667917e-7,0.00023913156],"genre_scores_gemma":[0.99959284,0.000002669608,0.000081339436,0.000115660725,0.0000953411,2.6646282e-7,0.0000016339588,7.586113e-7,0.00010950647],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99904436,0.000053260774,0.00028400726,0.00010863577,0.00025653958,0.00025321502],"domain_scores_gemma":[0.9990023,0.00020751783,0.00026859352,0.00015797596,0.0002477899,0.000115827446],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026586605,0.00007461042,0.00013655497,0.000046192887,0.00051619124,0.000037964754,0.0008934606,0.000031740372,0.00019410603],"category_scores_gemma":[0.0002206281,0.000029734128,0.00012771202,0.0005360331,0.0011282901,0.000111197085,0.000010895141,0.00013900145,1.8891802e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000025436573,0.0000017941386,0.9922079,0.0000050487643,0.0000075565945,1.9589699e-7,0.000047220263,0.0065609575,0.0002761537,0.00020307163,0.00017392398,0.0005136397],"study_design_scores_gemma":[0.00006566902,0.00004462635,0.9919519,0.00001278532,0.0000304942,0.000009584973,0.00015576044,0.00036130613,0.0010473323,0.00392071,0.0023545306,0.000045343535],"about_ca_topic_score_codex":0.843522,"about_ca_topic_score_gemma":0.99837476,"teacher_disagreement_score":0.15485273,"about_ca_system_score_codex":0.000007834488,"about_ca_system_score_gemma":0.0037973386,"threshold_uncertainty_score":0.67363155},"labels":[],"label_agreement":null},{"id":"W1979734496","doi":"10.1139/e01-061","title":"Potential-field modeling of a Proterozoic half-graben near Blackwater Lake, Northwest Territories, Canada, and its implications for the Fort Simpson Magnetic Anomaly","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Graben; Terrane; Proterozoic; Unconformity; Paleontology; Precambrian; Geomorphology; Structural basin; Tectonics","score_opus":0.02804197012370752,"score_gpt":0.19124208832107886,"score_spread":0.16320011819737135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979734496","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98709434,0.0033726322,0.00023924808,0.008517317,0.000272534,0.00023416575,0.00012029402,0.0000016340397,0.00014784619],"genre_scores_gemma":[0.99922395,0.00011152477,0.00031914617,0.0002078651,0.00009135089,0.0000017257665,0.0000049338805,0.0000011333211,0.000038390033],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99920875,0.000018077071,0.00024737965,0.00011204394,0.00014131171,0.00027242018],"domain_scores_gemma":[0.9993829,0.000081980426,0.00011124994,0.000059637434,0.0001440636,0.00022018436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025257416,0.00007480521,0.00012287582,0.00004630815,0.00072724675,0.0001171072,0.00022686546,0.00002932647,0.0002660451],"category_scores_gemma":[0.00008612207,0.00004443159,0.000036058358,0.00017316834,0.00014610808,0.00020507992,0.000004835343,0.00007183855,8.836541e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007937846,0.0000037156492,0.9362041,0.000011983645,0.000014152756,0.000005454241,0.0003010141,0.05378387,0.0000059039053,0.000050227427,0.00025842845,0.009353243],"study_design_scores_gemma":[0.00014743677,0.00077010825,0.757874,0.000019102528,0.000028548588,0.00004373538,0.0003198766,0.2309455,0.00001396205,0.0004286646,0.00930259,0.00010648647],"about_ca_topic_score_codex":0.8264121,"about_ca_topic_score_gemma":0.9993481,"teacher_disagreement_score":0.17833008,"about_ca_system_score_codex":0.0000015723003,"about_ca_system_score_gemma":0.00033113273,"threshold_uncertainty_score":0.55934674},"labels":[],"label_agreement":null},{"id":"W1979816822","doi":"10.1139/e06-110","title":"Yukon–Tanana terrane in the southern Campbell Range, Finlayson Lake belt, southeastern Yukon: the geological setting of retrogressed eclogite of the Klatsa metamorphic complex","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon Department of Environment; Yukon University; Carleton University","funders":"","keywords":"Geology; Terrane; Metamorphic rock; Thrust fault; Geochemistry; Subduction; Devonian; Schist; Metamorphism; Paleontology; Geomorphology; Fault (geology); Tectonics","score_opus":0.03340345807455469,"score_gpt":0.21410753973684937,"score_spread":0.18070408166229468,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979816822","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99045664,0.0013516379,0.000022753153,0.005629639,0.0001235824,0.00013401378,0.00008077844,0.000002092636,0.002198848],"genre_scores_gemma":[0.99899334,0.000010913841,0.00021013683,0.000634103,0.0000946184,2.2131027e-7,0.000004053204,0.000001501705,0.0000511286],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99742347,0.00038646013,0.00072374253,0.00020584179,0.00067967,0.0005808037],"domain_scores_gemma":[0.9980579,0.00070824625,0.0006180278,0.00023788503,0.00013817259,0.0002397927],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.004645583,0.00016446736,0.00040020375,0.00018643972,0.00041887446,0.00006509837,0.0015456208,0.00008665185,0.0023669505],"category_scores_gemma":[0.0004517193,0.00006422663,0.00028523052,0.0013935576,0.0017213059,0.00010149684,0.000023216813,0.00043574607,0.000011713381],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002043217,0.000009839644,0.99389076,0.0000064190876,0.0000202864,0.000030301471,0.0011460752,0.003228327,0.00006922725,0.000038078342,0.000021252848,0.0015190132],"study_design_scores_gemma":[0.00019343292,0.00019706633,0.9909145,0.000042278807,0.00004939616,0.000079601035,0.0033996096,0.0020588553,0.00006546574,0.0023679668,0.00053523754,0.000096595155],"about_ca_topic_score_codex":0.026572825,"about_ca_topic_score_gemma":0.84366244,"teacher_disagreement_score":0.8170896,"about_ca_system_score_codex":0.0000012814216,"about_ca_system_score_gemma":0.000228098,"threshold_uncertainty_score":0.99854505},"labels":[],"label_agreement":null},{"id":"W1980119374","doi":"10.1139/e03-047","title":"New 42 Ma cratonic North American paleomagnetic pole from the Yukon underscores another Cordilleran paleomagnetism-geology conundrum","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"McGill University","keywords":"Geology; Paleomagnetism; Pluton; Terrane; Paleontology; Batholith; Devonian; Apparent polar wander; Paleozoic; Craton; Geochemistry; Geomorphology; Tectonics","score_opus":0.014203229957513405,"score_gpt":0.18417586368500327,"score_spread":0.16997263372748986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980119374","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9827473,0.00406204,0.000078084995,0.004622969,0.00034967778,0.000069774214,0.000030873853,0.000006004297,0.008033239],"genre_scores_gemma":[0.9954613,0.00010667046,0.0013799985,0.0024965748,0.0001489983,1.9714854e-7,0.000006501764,0.00000236617,0.00039741324],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998017,0.00025616217,0.00039486832,0.0002939255,0.00035031614,0.00068769755],"domain_scores_gemma":[0.9982218,0.00041334506,0.00028457594,0.00018317433,0.00008542366,0.00081166154],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00039912935,0.00019109626,0.00034433705,0.00015216497,0.0005152643,0.00018298472,0.0007458511,0.0000476093,0.028780088],"category_scores_gemma":[0.00024588945,0.000110548586,0.00016308932,0.0010620825,0.0018547368,0.00016128489,0.000006649709,0.00027413815,0.00016261706],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007652386,0.0000035525381,0.99082,7.3909916e-7,0.000023074814,0.00005339409,0.000098254735,0.0016809322,0.000012178532,0.00009452806,0.0006911351,0.0065145497],"study_design_scores_gemma":[0.00020210473,0.00064214924,0.97969383,0.000008294103,0.00003491423,0.00007097616,0.00047425306,0.00034557693,0.00004527065,0.005245867,0.013061114,0.0001756395],"about_ca_topic_score_codex":0.19358414,"about_ca_topic_score_gemma":0.9519736,"teacher_disagreement_score":0.7583895,"about_ca_system_score_codex":0.0000019240063,"about_ca_system_score_gemma":0.0010414834,"threshold_uncertainty_score":0.97210777},"labels":[],"label_agreement":null},{"id":"W1980372107","doi":"10.1139/e01-069","title":"U-Pb zircon age constraint for late Neoproterozoic rifting and initiation of the lower Paleozoic passive margin of western Laurentia","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":190,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia; Government of British Columbia; Geological Survey of Canada; Yukon University","funders":"","keywords":"Laurentia; Geology; Rodinia; Zircon; Rift; Passive margin; Paleontology; Paleozoic; Supercontinent; Craton; Breakup; Continental margin; Tectonics","score_opus":0.023606006010691898,"score_gpt":0.19407019444524612,"score_spread":0.17046418843455421,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980372107","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99725455,0.0005818649,0.00008262638,0.0008827528,0.00013396243,0.00007769542,0.000044329914,8.850315e-7,0.00094135763],"genre_scores_gemma":[0.9990177,0.000018930088,0.0007340123,0.00013290277,0.000034748005,1.840199e-7,0.0000014939008,6.1762137e-7,0.000059402955],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99917597,0.00004540559,0.00030197544,0.00010235952,0.00016933176,0.00020495748],"domain_scores_gemma":[0.99919564,0.0001319093,0.00032875905,0.0000542755,0.00010061395,0.0001887846],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032287702,0.00006853262,0.00017921877,0.00010323047,0.00015532442,0.000041880503,0.00022144064,0.00003722229,0.0017479089],"category_scores_gemma":[0.00017718379,0.000039517017,0.00009575443,0.00026722424,0.0007050696,0.00013612151,0.000004964293,0.0000903237,0.0000023891455],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000050949857,0.0000067042356,0.9914919,0.000017994098,0.000018902554,0.000012266392,0.00029017281,0.00084250764,0.00096703303,0.000044393124,0.00002498355,0.006278044],"study_design_scores_gemma":[0.00029740325,0.00048024044,0.9877377,0.00011729579,0.000051057217,0.000036583755,0.00025633004,0.0025241075,0.0029404687,0.004869146,0.0005790527,0.00011062686],"about_ca_topic_score_codex":0.0027336087,"about_ca_topic_score_gemma":0.16222383,"teacher_disagreement_score":0.15949021,"about_ca_system_score_codex":5.613043e-7,"about_ca_system_score_gemma":0.00008537642,"threshold_uncertainty_score":0.99916464},"labels":[],"label_agreement":null},{"id":"W1980619025","doi":"10.1139/e11-011","title":"New zircon shock phenomena and their use for dating and reconstruction of large impact structures revealed by electron nanobeam (EBSD, CL, EDS) and isotopic U–Pb and (U–Th)/He analysis of the Vredefort domeThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":173,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Zircon; Geology; Electron backscatter diffraction; Recrystallization (geology); Impact structure; Impact crater; Geochemistry; Petrology; Microstructure; Materials science; Composite material","score_opus":0.014788049123596098,"score_gpt":0.19840242201368957,"score_spread":0.18361437289009347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980619025","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99822146,0.00092800043,0.000002801171,0.00033427245,0.000024762168,0.000108000175,0.00015042133,3.5729553e-7,0.00022992132],"genre_scores_gemma":[0.999112,0.00023740006,0.0005764475,0.000036223995,0.00002173237,2.0495354e-7,0.0000017611158,8.544752e-7,0.0000133924395],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99890924,0.00010400811,0.0005058455,0.0001479685,0.00013700985,0.00019594382],"domain_scores_gemma":[0.99888784,0.0002593442,0.0005618681,0.00009496889,0.0000877852,0.0001081836],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008918437,0.00009352664,0.00047256934,0.0003023219,0.00007241115,0.000018345492,0.00017897808,0.000057472924,0.0020221132],"category_scores_gemma":[0.0003112466,0.00004836311,0.000080982536,0.00080938695,0.0007948788,0.00026231367,0.000014287716,0.00011604671,1.4423888e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010300153,0.00001214926,0.9756417,0.0000242573,0.0001306677,1.7345403e-7,0.001975666,0.00005482898,0.015072049,0.00007733281,0.000020791476,0.006887326],"study_design_scores_gemma":[0.00033749433,0.00085417717,0.9299299,0.000057916815,0.00010840139,0.0000073308256,0.002047281,0.00031285576,0.06225315,0.003980638,0.00004709935,0.00006371947],"about_ca_topic_score_codex":0.032404985,"about_ca_topic_score_gemma":0.1935527,"teacher_disagreement_score":0.16114771,"about_ca_system_score_codex":0.0000022140869,"about_ca_system_score_gemma":0.00016723378,"threshold_uncertainty_score":0.99889016},"labels":[],"label_agreement":null},{"id":"W1980690516","doi":"10.1139/e07-029","title":"Granulite-facies regional and contact metamorphism of the Tasiuyak paragneiss, northern Labrador: textural evolution and interpretation","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Metamorphism; Geology; Geochemistry; Granulite; Sillimanite; Metamorphic rock; Pluton; Metamorphic facies; Cordierite; Partial melting; Plagioclase; Petrology; Biotite; Facies; Geomorphology; Crust; Quartz; Paleontology; Chemistry","score_opus":0.012107909617701688,"score_gpt":0.18917987243760087,"score_spread":0.17707196281989918,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980690516","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947993,0.0033608547,0.000055308974,0.0012407843,0.00009503797,0.000035299472,0.000013004752,0.0000012357708,0.0003991481],"genre_scores_gemma":[0.9995677,0.000024041037,0.00018836021,0.00015797853,0.000030595485,3.7671303e-8,0.0000015495456,4.5835512e-7,0.000029286337],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99919134,0.00004837831,0.00024546316,0.000105656945,0.00021124026,0.00019790436],"domain_scores_gemma":[0.99926025,0.00014462812,0.00018826887,0.00004544342,0.000098294,0.0002631158],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006800065,0.0000712439,0.00014542807,0.0001298363,0.00023827385,0.00004751188,0.00018078813,0.00003253102,0.00035891004],"category_scores_gemma":[0.00015039097,0.00003786142,0.000065211694,0.00034036604,0.00078783854,0.00022194511,0.0000050698486,0.00010766431,0.0000026604357],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010931549,0.0000015464983,0.9926097,0.0000030131996,0.000011606944,0.0000051148563,0.0002149648,0.0001348936,0.00020653624,0.00026134064,0.000011098753,0.0065292884],"study_design_scores_gemma":[0.000082606966,0.00013531045,0.9914583,0.000018943309,0.000025040625,0.00010282819,0.0004258834,0.00095751125,0.00010475271,0.0060968213,0.00053761574,0.00005439266],"about_ca_topic_score_codex":0.028126834,"about_ca_topic_score_gemma":0.66926146,"teacher_disagreement_score":0.6411346,"about_ca_system_score_codex":0.0000014636071,"about_ca_system_score_gemma":0.00015618054,"threshold_uncertainty_score":0.978345},"labels":[],"label_agreement":null},{"id":"W1981074158","doi":"10.1139/e02-085","title":"The Nastapoka drift belt, eastern Hudson Bay: implications of a stillstand of the QuebecLabrador ice margin in the Tyrrell Sea at 8 ka BP","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval; Center for Northern Studies","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Bay; Ice sheet; Moraine; Geomorphology; Deglaciation; Ice stream; Oceanography; Ice shelf; Glacial period; Cryosphere; Sea ice","score_opus":0.024248498728807157,"score_gpt":0.24033643270225516,"score_spread":0.216087933973448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981074158","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9810387,0.003126424,0.0000047513377,0.0067557395,0.00024853344,0.00014848742,0.000041558917,7.036532e-7,0.008635103],"genre_scores_gemma":[0.99913955,0.00008979015,0.00007270992,0.00028639112,0.000017108187,5.345571e-7,0.0000011728583,0.0000011902684,0.0003915549],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981318,0.0006111734,0.00035960035,0.00013084455,0.00032341343,0.00044314397],"domain_scores_gemma":[0.99830633,0.000868865,0.00027278418,0.00023246715,0.00012640674,0.00019314939],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0028374572,0.000088128516,0.00016772679,0.00016261544,0.0007865997,0.0000521259,0.0010547239,0.00006375894,0.00043946787],"category_scores_gemma":[0.00034878022,0.000041684645,0.000078063786,0.00080775697,0.0019311848,0.00014154131,0.000009657521,0.00030451769,0.000012878813],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000911296,0.0000044005405,0.9973594,0.000005256657,0.0000075879134,0.000007974702,0.0006849013,0.00044504137,0.0000075762227,0.00094622397,0.00020797187,0.00031458566],"study_design_scores_gemma":[0.00014648632,0.00012429655,0.98811036,0.000028784743,0.000008416147,0.00023884649,0.0014709769,0.00018019255,0.000099584955,0.0010904369,0.008451813,0.000049804134],"about_ca_topic_score_codex":0.010062112,"about_ca_topic_score_gemma":0.91947156,"teacher_disagreement_score":0.9094094,"about_ca_system_score_codex":0.0000012946164,"about_ca_system_score_gemma":0.0015713905,"threshold_uncertainty_score":0.99653},"labels":[],"label_agreement":null},{"id":"W1981112840","doi":"10.1139/e07-009","title":"<i>Bartonaspis</i> new genus, a trilobite species complex from the base of the Upper Cambrian Sunwaptan Stage in North America","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Holotype; Trilobite; Paleontology; Geology; Genus; Biology; Zoology; Ordovician","score_opus":0.0334269981876724,"score_gpt":0.21789784515865793,"score_spread":0.18447084697098554,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981112840","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9810786,0.004096386,0.000040215535,0.0016118141,0.0004735477,0.000100194295,0.00023826257,0.0000018269984,0.012359138],"genre_scores_gemma":[0.9984333,0.000038314993,0.00061464205,0.000610395,0.00015757619,4.924626e-8,0.0000024149374,7.419455e-7,0.00014258533],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99838066,0.00014475662,0.0004635292,0.00015961402,0.00037116447,0.00048029056],"domain_scores_gemma":[0.99855614,0.00039127035,0.00033642264,0.00018012166,0.000055405613,0.00048062092],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00093055016,0.0001249986,0.0002395972,0.00020612522,0.000470345,0.00008667882,0.0009309107,0.00004624461,0.0010511486],"category_scores_gemma":[0.00013727606,0.00006915752,0.00014286427,0.0009136262,0.0015441319,0.00026776775,0.0000023563928,0.00028153008,0.0000057984294],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017312641,0.0000031100792,0.9881301,0.0000010931064,0.000010478775,0.0000536897,0.0010286809,0.0002479995,0.000036665584,0.00008158483,0.00033113177,0.010058164],"study_design_scores_gemma":[0.00020678494,0.00013185818,0.97881466,0.000021627735,0.000009130707,0.00002451566,0.0015599043,0.00009230885,0.000052481017,0.00013706191,0.018861653,0.000087998334],"about_ca_topic_score_codex":0.145661,"about_ca_topic_score_gemma":0.98458433,"teacher_disagreement_score":0.83892334,"about_ca_system_score_codex":0.0000021283352,"about_ca_system_score_gemma":0.001682806,"threshold_uncertainty_score":0.999862},"labels":[],"label_agreement":null},{"id":"W1981130870","doi":"10.1139/e11-046","title":"First evidence of percids (Teleostei: Perciformes) in the Miocene of North America","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fish Ecology and Management Studies","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Perciformes; Teleostei; Fauna; Geology; Arctic; Pleistocene; Fish <Actinopterygii>; The arctic; Paleontology; Oceanography; Geography; Fishery; Ecology; Biology","score_opus":0.036011784381296666,"score_gpt":0.21948869510767516,"score_spread":0.1834769107263785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981130870","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893122,0.00019353414,0.000015550497,0.0009082181,0.00009570937,0.000074784824,0.0000019207928,6.3001283e-7,0.009397507],"genre_scores_gemma":[0.9985488,0.0002108838,0.0008169712,0.00037087334,0.000008874728,0.0000010932246,5.3492133e-8,0.0000013889788,0.000041077674],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991086,0.000049662183,0.00028109387,0.000099123696,0.00022524565,0.00023624337],"domain_scores_gemma":[0.9994679,0.00009820197,0.00021567797,0.0001020635,0.000021116395,0.00009503189],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000743944,0.000065420376,0.00015610352,0.00013350377,0.0001962935,0.000008216046,0.000676555,0.00001719948,0.0010828287],"category_scores_gemma":[0.00018824426,0.000041976444,0.00004818328,0.0005695331,0.0016190588,0.00036577418,0.000038058595,0.00008992649,0.000015475971],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005811985,0.000014374217,0.9939796,0.000007801467,0.000004583709,0.000018438079,0.004316213,0.00030169543,0.0000040527148,0.000029655845,0.00073567586,0.0005821384],"study_design_scores_gemma":[0.000058282734,0.00045021684,0.9959607,0.000047989048,0.00000961408,0.000012132723,0.0019159684,0.00003184397,0.000035400517,0.000099405945,0.0013320817,0.000046347133],"about_ca_topic_score_codex":0.011744533,"about_ca_topic_score_gemma":0.70611554,"teacher_disagreement_score":0.694371,"about_ca_system_score_codex":0.000008812046,"about_ca_system_score_gemma":0.00011975592,"threshold_uncertainty_score":0.9998303},"labels":[],"label_agreement":null},{"id":"W1981132037","doi":"10.1139/e07-026","title":"Proterozoic and Archean geology of the Nipigon Embayment: implications for emplacement of the Mesoproterozoic Nipigon diabase sills and mafic to ultramafic intrusions","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Northern Ontario Heritage Fund Corporation","keywords":"Geology; Ultramafic rock; Sill; Mafic; Geochemistry; Felsic; Archean; Outcrop; Proterozoic; Rift; Petrology; Tectonics; Paleontology","score_opus":0.019641663069031284,"score_gpt":0.22886002724544027,"score_spread":0.209218364176409,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981132037","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98987,0.00042758917,0.00013055491,0.008881242,0.00009948773,0.0003577699,0.00006031416,9.67043e-7,0.0001720793],"genre_scores_gemma":[0.99869055,0.000012881863,0.0007755493,0.00044293498,0.000031336433,0.0000015249026,0.0000013344829,9.4115575e-7,0.00004293169],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989278,0.000060991533,0.00036885033,0.00016043447,0.00016288603,0.00031905936],"domain_scores_gemma":[0.99890226,0.00023226342,0.00024255626,0.00012902608,0.0001121804,0.00038173908],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010018462,0.00008883045,0.0001926688,0.00015470039,0.00040455928,0.000028469194,0.0003953013,0.000039605882,0.00022069938],"category_scores_gemma":[0.00030354102,0.000044021974,0.00008564075,0.00051822787,0.000896433,0.0000684529,0.000022457747,0.000112446054,7.3470295e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013339458,0.000008581069,0.9906044,0.000012611382,0.000013232546,4.886417e-7,0.0002540298,0.00043926228,0.002316659,0.00026019293,0.000033701483,0.0060434737],"study_design_scores_gemma":[0.00013334949,0.00034791764,0.98836577,0.000035057867,0.000026622904,0.000027997688,0.00023609339,0.000118477496,0.0038584652,0.0059779463,0.00081142207,0.000060857266],"about_ca_topic_score_codex":0.006061852,"about_ca_topic_score_gemma":0.1845194,"teacher_disagreement_score":0.17845754,"about_ca_system_score_codex":0.000001915599,"about_ca_system_score_gemma":0.00022452141,"threshold_uncertainty_score":0.91637474},"labels":[],"label_agreement":null},{"id":"W1981375780","doi":"10.1139/e06-081","title":"Possible refugia in the Alexander Archipelago of southeastern Alaska during the late Wisconsin glaciation","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":123,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Forest Service; U.S. Geological Survey","keywords":"Archipelago; Geology; Deglaciation; Continental shelf; Oceanography; Glacial period; Land bridge; Biological dispersal; Archaeology; Geography; Holocene; Paleontology; Population","score_opus":0.023652853794219327,"score_gpt":0.24437683465470858,"score_spread":0.22072398086048925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981375780","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920527,0.000740857,0.000007740431,0.001384232,0.00018819125,0.00006955939,0.000005006342,9.147744e-7,0.0055508097],"genre_scores_gemma":[0.9995425,0.0000123606505,0.00006348298,0.00014395424,0.000044725868,7.240771e-8,8.0225135e-7,7.579841e-7,0.00019136765],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986758,0.00023456998,0.0003029963,0.00008461928,0.0002738163,0.0004282008],"domain_scores_gemma":[0.99910176,0.00041236755,0.00016911609,0.00010085755,0.00005778667,0.00015809966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004275471,0.0000649428,0.00012292717,0.0003413,0.0004018334,0.00005072392,0.0005492462,0.00005114051,0.00048074653],"category_scores_gemma":[0.00012923431,0.000033769422,0.000045849865,0.0005298132,0.0009929746,0.00018611035,0.0000041124254,0.00031021825,0.000024380943],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000172256,0.000002090652,0.99620616,0.0000039792258,0.000004810013,0.00006218141,0.0024672176,0.00096844224,0.000008541225,0.00005628725,0.0000027151036,0.0002003611],"study_design_scores_gemma":[0.00014153951,0.00010032554,0.99568564,0.000023883169,0.0000038123376,0.00032183333,0.002801187,0.00014567334,0.00006920123,0.0005637009,0.00010263889,0.000040560666],"about_ca_topic_score_codex":0.0034800672,"about_ca_topic_score_gemma":0.8034292,"teacher_disagreement_score":0.7999491,"about_ca_system_score_codex":2.6298494e-7,"about_ca_system_score_gemma":0.00058668107,"threshold_uncertainty_score":0.52638376},"labels":[],"label_agreement":null},{"id":"W1981661000","doi":"10.1139/e03-026","title":"Emmons Lake Volcanic Center, Alaska Peninsula: source of the Late Wisconsin Dawson tephra, Yukon Territory, Canada","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Tephra; Caldera; Pyroclastic rock; Volcano; Rhyolite; Quaternary; Pumice; Peninsula; Loess; Silicic; Geochemistry; Lava; Glacial period; Geomorphology; Paleontology; Volcanic rock; Archaeology","score_opus":0.016487055669550086,"score_gpt":0.20492459787560505,"score_spread":0.18843754220605496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981661000","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9870596,0.0013874742,0.0000033358542,0.0016326373,0.0012781199,0.00008112744,0.000050942806,0.0000017100399,0.008505056],"genre_scores_gemma":[0.99840444,0.000021702894,0.00007692846,0.00031500592,0.000040924697,1.3280419e-7,0.0000023621546,0.0000019647794,0.0011365605],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99810773,0.00036085426,0.00035746134,0.00015370852,0.0003996437,0.00062061],"domain_scores_gemma":[0.99870527,0.0002130254,0.00025750275,0.0001727261,0.00011090451,0.0005405827],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010272897,0.00012488702,0.00024019962,0.00019702356,0.0006675953,0.000053795986,0.0007336831,0.000079171965,0.0014391941],"category_scores_gemma":[0.0003152177,0.0000819917,0.000086133354,0.00044307127,0.0012999619,0.00018316938,0.0000073858396,0.00037867192,0.00001407374],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004598738,0.0000035448197,0.99733126,0.00000413615,0.000013930153,0.00005167385,0.00015767508,0.00140812,0.0000045992674,0.00003927248,0.0008886339,0.000092543516],"study_design_scores_gemma":[0.00023762108,0.00013602336,0.95232695,0.000036802823,0.0000112227035,0.00057892833,0.00048444862,0.00022699994,0.00013634183,0.00013984971,0.04558328,0.000101557045],"about_ca_topic_score_codex":0.42482007,"about_ca_topic_score_gemma":0.9995961,"teacher_disagreement_score":0.57477605,"about_ca_system_score_codex":0.0000015997518,"about_ca_system_score_gemma":0.007548309,"threshold_uncertainty_score":0.99947363},"labels":[],"label_agreement":null},{"id":"W1981694413","doi":"10.1139/e10-052","title":"Evidence for post-1200 Ma — pre-Grenvillian supracrustal rocks in the Pinware terrane, eastern Grenville Province at Battle Harbour, LabradorThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Government of Newfoundland and Labrador; University of Toronto; University of Alberta","funders":"University of Toronto","keywords":"Geology; Zircon; Pegmatite; Geochemistry; Terrane; Metamorphism; Mafic; Laurentia; Metamorphic facies; Paleontology; Tectonics; Facies; Ordovician","score_opus":0.0392540843491137,"score_gpt":0.20851806091939562,"score_spread":0.16926397657028192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981694413","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918883,0.0006655999,8.4667425e-7,0.004172349,0.0000872626,0.0002052614,0.00012096795,7.346433e-7,0.0028586767],"genre_scores_gemma":[0.999294,0.00006265791,0.00022210157,0.00023939517,0.00006564521,0.0000013315325,0.000002244582,0.0000015400504,0.00011109754],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99815416,0.00018114329,0.0006947149,0.0002119647,0.0003781699,0.000379833],"domain_scores_gemma":[0.99854386,0.00050182425,0.00049221894,0.00018076003,0.00014042009,0.00014091679],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014181526,0.0001278777,0.00039479844,0.0002772862,0.000093647745,0.000024369052,0.0008340513,0.00007587021,0.023142288],"category_scores_gemma":[0.0009391697,0.00007101188,0.00012895794,0.0007545125,0.0010559289,0.00037115064,0.000022183516,0.00022080378,0.0000042094503],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028201455,0.000060846618,0.98940367,0.000036466245,0.000015945958,0.000016365986,0.005735241,0.00048328022,0.0004998496,0.00003794298,0.00010662248,0.0033217422],"study_design_scores_gemma":[0.00034309167,0.001453029,0.98162484,0.0002901267,0.000019834566,0.000018766896,0.0039995518,0.0004281571,0.010330328,0.00083112356,0.0005493096,0.000111862166],"about_ca_topic_score_codex":0.0869772,"about_ca_topic_score_gemma":0.7745627,"teacher_disagreement_score":0.68758553,"about_ca_system_score_codex":0.0000052253754,"about_ca_system_score_gemma":0.00049586943,"threshold_uncertainty_score":0.9777507},"labels":[],"label_agreement":null},{"id":"W1981811062","doi":"10.1139/e00-035","title":"Kanairiktok shear zone: the boundary between the Paleoproterozoic Makkovik Province and the Archean Nain Province, Labrador, Canada.","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Greenschist; Geology; Mylonite; Geochemistry; Shear zone; Archean; Craton; Metamorphic facies; Overprinting; Metamorphism; Facies; Metamorphic rock; Geomorphology; Paleontology; Tectonics","score_opus":0.008980191765330412,"score_gpt":0.17437365234666835,"score_spread":0.16539346058133794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981811062","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9482389,0.003712453,0.000006360187,0.043475397,0.00010201004,0.00022998698,0.000053405776,0.0000036103766,0.0041778963],"genre_scores_gemma":[0.99590784,0.00007328275,0.00010722711,0.0027110677,0.00023737803,7.676497e-7,0.0000029579612,0.0000016547388,0.0009578311],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978716,0.00033757015,0.0003877609,0.00023045758,0.00057616533,0.0005964616],"domain_scores_gemma":[0.9984338,0.00058739854,0.00017401115,0.00019969876,0.000066683344,0.0005384002],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["sts"],"category_scores_codex":[0.0021300127,0.0001625652,0.00026440187,0.00006616601,0.0018260605,0.0004098747,0.0011458056,0.000043690186,0.0031509888],"category_scores_gemma":[0.00017881373,0.000061307815,0.00010041536,0.00056173326,0.0036687898,0.00020657686,0.000013814421,0.0004818503,0.000021143553],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044811863,0.0000040537634,0.8659636,0.000010893679,0.00006250305,0.00010857163,0.00041048767,0.0013831011,0.0000017942018,0.00022084455,0.00216606,0.12962332],"study_design_scores_gemma":[0.0002486467,0.0001433862,0.8945427,0.000023249302,0.00004794554,0.00012520798,0.00043102627,0.0011240395,0.000015075936,0.004509497,0.09864839,0.00014087035],"about_ca_topic_score_codex":0.8649661,"about_ca_topic_score_gemma":0.99723005,"teacher_disagreement_score":0.13226394,"about_ca_system_score_codex":0.0000042035817,"about_ca_system_score_gemma":0.0038808263,"threshold_uncertainty_score":0.99947345},"labels":[],"label_agreement":null},{"id":"W1981931682","doi":"10.1139/e06-047","title":"Dynamics of rocky shores: Cretaceous, Pliocene, Pleistocene, and Recent, Baja California peninsula, Mexico","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Shore; Peninsula; Cretaceous; Sedimentary rock; Rocky shore; Paleontology; Clastic rock; Oceanography; Context (archaeology)","score_opus":0.009174500539948099,"score_gpt":0.19103777115792708,"score_spread":0.181863270617979,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981931682","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9812804,0.002309859,0.0001887637,0.0009881702,0.00034853912,0.00008606843,0.00042868094,0.0000050286326,0.014364476],"genre_scores_gemma":[0.9979916,0.00024007024,0.0012171805,0.0000910607,0.00008668572,9.76936e-8,0.000034731085,0.000003281862,0.00033524242],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985527,0.000041269028,0.00044810306,0.00018875385,0.0003390422,0.00043014903],"domain_scores_gemma":[0.9988325,0.0000843756,0.00028103276,0.00010000763,0.00017556812,0.0005264931],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005258988,0.00014677754,0.00026468362,0.00039177213,0.00031647674,0.00013185346,0.00037678485,0.00006091443,0.000751105],"category_scores_gemma":[0.000097899494,0.00011552173,0.000069464775,0.0005703383,0.00062151474,0.0002994872,0.000013559214,0.00016316096,0.000008232411],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017732333,0.0000056738377,0.9746442,0.000011446688,0.000007772961,0.00005174562,0.000039968883,0.005585847,0.0000059971303,0.0004934556,0.00021278963,0.018923357],"study_design_scores_gemma":[0.0002627631,0.00047353382,0.9306656,0.000047669157,0.000024068831,0.0003588067,0.0002684341,0.046404045,0.000041459436,0.00425426,0.016983185,0.00021618782],"about_ca_topic_score_codex":0.0815259,"about_ca_topic_score_gemma":0.9220286,"teacher_disagreement_score":0.8405027,"about_ca_system_score_codex":0.000005062704,"about_ca_system_score_gemma":0.0011799566,"threshold_uncertainty_score":0.9245903},"labels":[],"label_agreement":null},{"id":"W1981991569","doi":"10.1139/e03-090","title":"A structural reappraisal of the BeardmoreGeraldton Belt at the southern boundary of the Wabigoon subprovince, Ontario, and implications for gold mineralization","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Greenstone belt; Sinistral and dextral; Overprinting; Geochemistry; Archean; Clockwise; Shear zone; Mineralization (soil science); Transpression; Fold (higher-order function); Orogeny; Shear (geology); Cleavage (geology); Geomorphology; Seismology; Paleontology; Metamorphic rock; Tectonics","score_opus":0.015159924217326273,"score_gpt":0.20100155930007946,"score_spread":0.1858416350827532,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981991569","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99160737,0.00056186004,0.0000081235785,0.0069682207,0.0001128288,0.00010279545,0.000115265844,7.354756e-7,0.00052281003],"genre_scores_gemma":[0.99930876,0.000005521519,0.00016300673,0.00021438718,0.000032599874,3.1876243e-7,0.000004171908,7.466218e-7,0.00027048963],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999255,0.00003775433,0.00024564893,0.000103056176,0.00017742181,0.00018111595],"domain_scores_gemma":[0.9992428,0.00010497835,0.0002749718,0.00011562797,0.00013674915,0.0001248826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032672222,0.00006807296,0.00012555385,0.000042721305,0.0005063261,0.00004441831,0.0004370065,0.000031102005,0.00033403983],"category_scores_gemma":[0.00015829352,0.000026929636,0.0001110007,0.00038332955,0.0012374009,0.000093805334,0.0000135329965,0.00008979774,5.4111797e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007328174,0.0000017030295,0.9849642,0.0000036764523,0.000010269484,1.8602218e-7,0.00049385254,0.0126284575,0.00036556888,0.00039905714,0.00003975533,0.0010859806],"study_design_scores_gemma":[0.000111549634,0.00009307002,0.98693913,0.000015502623,0.000030123445,0.00002683181,0.00015567246,0.00023103537,0.00036144204,0.010152904,0.0018384551,0.000044252054],"about_ca_topic_score_codex":0.27472672,"about_ca_topic_score_gemma":0.9802126,"teacher_disagreement_score":0.70548594,"about_ca_system_score_codex":0.0000031121783,"about_ca_system_score_gemma":0.00079563446,"threshold_uncertainty_score":0.73010296},"labels":[],"label_agreement":null},{"id":"W1982321369","doi":"10.1139/e03-025","title":"Development of late Paleozoic volcanic arcs in the Canadian Cordillera: an example from the Klinkit Group, northern British Columbia and southern Yukon","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon University; Geological Survey of Canada; Saint Mary's University; Dalhousie University","funders":"Nature","keywords":"Geology; Terrane; Pyroclastic rock; Volcanic arc; Craton; Paleozoic; Basement; Paleontology; Volcanic rock; Sedimentary rock; Clastic rock; Island arc; Rift; Basalt; Geochemistry; Volcano; Subduction; Structural basin; Tectonics; Archaeology","score_opus":0.025052163791956465,"score_gpt":0.17425923731115173,"score_spread":0.14920707351919527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982321369","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970622,0.0011330909,0.000002130113,0.00028247276,0.00007044367,0.00007079753,0.000044527795,0.0000011186427,0.0013332398],"genre_scores_gemma":[0.9988943,0.000019614987,0.000501478,0.00049998524,0.00003411195,3.3571717e-7,0.000010716004,0.0000012246904,0.000038246482],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985557,0.00017603161,0.00035903955,0.0001891536,0.000312186,0.00040786364],"domain_scores_gemma":[0.9989521,0.00016914595,0.00015303082,0.000105072206,0.00008070007,0.0005399614],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013783304,0.0000839266,0.00019872776,0.00007210799,0.0007547981,0.00040357592,0.0005389485,0.00005218521,0.0038616986],"category_scores_gemma":[0.00010410992,0.000058082518,0.000049056125,0.000522382,0.0005480042,0.0001328067,0.0000036939773,0.00021360473,0.000008978255],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011845561,0.000004471188,0.9910925,0.0000010492055,0.000010932929,0.000037126687,0.0019664604,0.00022510347,0.0000063598213,0.0000063531256,0.000013980834,0.0066344836],"study_design_scores_gemma":[0.0001294209,0.000084105246,0.99005514,0.000025120531,0.000013460582,0.000034939992,0.0031715182,0.00031266827,0.0000032998378,0.0025625918,0.003509765,0.0000979843],"about_ca_topic_score_codex":0.9915423,"about_ca_topic_score_gemma":0.9999968,"teacher_disagreement_score":0.008454492,"about_ca_system_score_codex":0.0000036435683,"about_ca_system_score_gemma":0.001249407,"threshold_uncertainty_score":0.9970489},"labels":[],"label_agreement":null},{"id":"W1982322261","doi":"10.1139/e05-117","title":"Introduction to the Grenville Province: a geological and mineral resources perspective derived from government and academic research initiatives","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec); Geological Survey of Canada","funders":"","keywords":"Mineral exploration; Geology; Frontier; Government (linguistics); Earth science; Mineral resource classification; Geochemistry; Mining engineering; Geography; Archaeology","score_opus":0.03724380619356366,"score_gpt":0.27530497076004423,"score_spread":0.23806116456648058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982322261","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8410522,0.001105456,0.0003454854,0.15560412,0.00007142004,0.0000674988,0.0000025816903,0.0000020768205,0.0017491595],"genre_scores_gemma":[0.99487406,0.000042335123,0.003779391,0.00037858836,0.0006960775,0.0000015217104,5.3280825e-8,5.909696e-7,0.0002273924],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987941,0.00015263741,0.00015101489,0.00025665754,0.00035911694,0.00028651638],"domain_scores_gemma":[0.9991664,0.00017754186,0.00008381711,0.00009767415,0.0001564382,0.00031808644],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015337542,0.00006727878,0.00009568703,0.00008242842,0.00058521697,0.00019726252,0.00053366664,0.000042530395,0.000041842137],"category_scores_gemma":[0.0009795551,0.00004155923,0.000015553838,0.00029605473,0.0007570405,0.0003376937,0.000109193104,0.00034309772,0.0000028195661],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014395294,0.00008076493,0.61156756,0.000027178581,0.0001434772,0.0003344841,0.17712937,0.015078785,0.03873649,0.09039012,0.018965585,0.047402214],"study_design_scores_gemma":[0.00025648094,0.0006637804,0.8110709,0.000056163182,0.0000061317396,0.0002953315,0.015559543,0.004869294,0.0024722961,0.0070181107,0.15753548,0.000196457],"about_ca_topic_score_codex":0.0011649946,"about_ca_topic_score_gemma":0.017308261,"teacher_disagreement_score":0.19950336,"about_ca_system_score_codex":0.000022559,"about_ca_system_score_gemma":0.00034438976,"threshold_uncertainty_score":0.9658416},"labels":[],"label_agreement":null},{"id":"W1982375020","doi":"10.1139/e07-056","title":"Paleomagnetic and mineral magnetic constraints on Zn–Pb ore genesis in the Pend Oreille Mine, Metaline district, Washington, USA","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Galena; Sphalerite; Batholith; Pyrrhotite; Paleomagnetism; Geochemistry; Breccia; Remanence; Mineralization (soil science); Cretaceous; Ordovician; Mineralogy; Pyrite; Paleontology; Magnetization","score_opus":0.014831336780987312,"score_gpt":0.23274775949424026,"score_spread":0.21791642271325296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982375020","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9787165,0.009739479,0.000024678127,0.00069657806,0.00022944527,0.00012353159,0.000028728597,0.0000010179754,0.0104400525],"genre_scores_gemma":[0.9976934,0.00033421704,0.0008874841,0.0004510521,0.00019757709,0.0000017696325,0.000005095418,0.0000060698935,0.0004233071],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984751,0.000090450754,0.00038649113,0.00026082672,0.0002730602,0.00051408174],"domain_scores_gemma":[0.9991912,0.00008981256,0.00014099861,0.00016111774,0.00009120848,0.00032565388],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011727308,0.00018547867,0.0002073381,0.00026044098,0.00027199998,0.000105558356,0.00042723338,0.00007945446,0.00018170159],"category_scores_gemma":[0.00024464674,0.00012619053,0.000073888405,0.0003701255,0.0011839597,0.000014135833,0.00002403862,0.00014152797,0.0000043370565],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008406242,0.00008358263,0.92402476,0.000041575604,0.000045738787,0.0010302542,0.0015883959,0.00020703513,0.030370079,0.0006412107,0.0036041874,0.038279124],"study_design_scores_gemma":[0.0005910697,0.0024306858,0.98044944,0.000032805245,0.00003149866,0.0006048321,0.0012781325,0.000014210575,0.00088171934,0.00006692302,0.0134068765,0.00021183057],"about_ca_topic_score_codex":0.0016537652,"about_ca_topic_score_gemma":0.21502106,"teacher_disagreement_score":0.2133673,"about_ca_system_score_codex":0.000002555445,"about_ca_system_score_gemma":0.00033518198,"threshold_uncertainty_score":0.79930276},"labels":[],"label_agreement":null},{"id":"W1982391444","doi":"10.1139/e01-040","title":"Geology of the Chatham Sound region, southeast Alaska and coastal British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Terrane; Geology; Cretaceous; Volcanic rock; Paleozoic; Paleontology; North American Plate; Metamorphism; Accretion (finance); Geochemistry; Volcano; Subduction; Tectonics","score_opus":0.013790172723411468,"score_gpt":0.172173712101502,"score_spread":0.15838353937809055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982391444","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944954,0.0009627077,0.000008333098,0.0011600824,0.00014300982,0.000031335017,0.000019414825,0.0000013903422,0.0031783117],"genre_scores_gemma":[0.9990436,0.00005640315,0.00008220502,0.00023004058,0.00006528623,5.6082943e-8,0.0000010130127,6.133364e-7,0.00052079814],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990696,0.00006073941,0.0002448861,0.00013051555,0.00019668619,0.00029757933],"domain_scores_gemma":[0.999194,0.00006115081,0.00018134952,0.00006726922,0.000108018045,0.0003881666],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003727117,0.000055133252,0.00017903978,0.000055893997,0.00039151162,0.00016190617,0.0003512358,0.000044210938,0.0035481213],"category_scores_gemma":[0.00017057614,0.000043170407,0.00008526817,0.00044891957,0.0016040716,0.00013258331,0.000010048184,0.00012729678,0.000005749299],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000015082799,0.0000026521195,0.9973915,0.0000016044957,0.0000071297286,0.000053246047,0.000046294943,0.00017864445,0.0000034917166,0.000012906226,0.00015443026,0.0021465486],"study_design_scores_gemma":[0.000090346075,0.00013324851,0.9849562,0.000017322127,0.000012384235,0.0012889575,0.00044259615,0.00018339891,0.0000035825026,0.01112638,0.001685938,0.0000596574],"about_ca_topic_score_codex":0.32826287,"about_ca_topic_score_gemma":0.9868919,"teacher_disagreement_score":0.65862906,"about_ca_system_score_codex":3.8195947e-7,"about_ca_system_score_gemma":0.00028497443,"threshold_uncertainty_score":0.9973628},"labels":[],"label_agreement":null},{"id":"W1982823497","doi":"10.1139/e01-055","title":"Cranial anatomy of a new crocodyliform (Archosauria: Crocodylomorpha) from the Lower Cretaceous of Song-Liao Plain, northeastern China","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Core Research for Evolutional Science and Technology; Chinese Academy of Geological Sciences; Chinese Academy of Sciences","keywords":"Cretaceous; Paleontology; Genus; Anatomy; Biology; Taxon; Fauna; Geology; Zoology; Ecology","score_opus":0.01530584578992517,"score_gpt":0.22650940137330527,"score_spread":0.2112035555833801,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982823497","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9866483,0.0063296175,0.00009292941,0.0021463204,0.0008358533,0.00010241922,0.00018189932,0.0000028126185,0.0036598267],"genre_scores_gemma":[0.9986762,0.00015290522,0.00049966155,0.00022494393,0.00031739275,1.4102054e-7,0.000008031179,0.0000018204723,0.000118893564],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99836457,0.00012314979,0.0005217367,0.00018832635,0.00031930863,0.00048292452],"domain_scores_gemma":[0.9984948,0.00025767312,0.00044845618,0.00015471772,0.00012244037,0.00052188215],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00076332974,0.00014419295,0.00034001863,0.00021141447,0.0004076362,0.000035503985,0.00087650254,0.000113546244,0.0034192181],"category_scores_gemma":[0.00015333496,0.00009132339,0.0001420283,0.00047356164,0.0015828738,0.00034306894,0.000007840743,0.00026098898,0.000029833247],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001504429,0.000009984558,0.99190944,0.0000023898692,0.0000380179,0.00013802446,0.00056998566,0.0010679128,0.000019862855,0.00004432569,0.00034966198,0.0056999326],"study_design_scores_gemma":[0.00040222603,0.0008303269,0.9742035,0.000046115645,0.000025763884,0.00046309052,0.00030663412,0.0008363284,0.000019886578,0.0014952292,0.021264615,0.00010623198],"about_ca_topic_score_codex":0.09210757,"about_ca_topic_score_gemma":0.8267092,"teacher_disagreement_score":0.7346016,"about_ca_system_score_codex":0.0000022454929,"about_ca_system_score_gemma":0.0021616123,"threshold_uncertainty_score":0.9974918},"labels":[],"label_agreement":null},{"id":"W1983020091","doi":"10.1139/e08-028","title":"A paleomagnetic test for northward tectonic transport of the eastern Selwyn Basin, northern Canadian Cordillera: data from the mid-Cretaceous Ragged Pluton","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor; Yukon Department of Environment","funders":"","keywords":"Pluton; Geology; Paleomagnetism; Cretaceous; Apparent polar wander; Geochemistry; Tectonics; Geomorphology; Paleontology","score_opus":0.031462040326096195,"score_gpt":0.19095584974326435,"score_spread":0.15949380941716815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983020091","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99031305,0.002534348,0.0000080362715,0.0044015995,0.0002644569,0.00017876875,0.0013227682,0.0000029949558,0.0009739885],"genre_scores_gemma":[0.9986588,0.00005643006,0.00028694983,0.0006785035,0.0001447355,4.9868606e-7,0.00005073522,0.0000026284752,0.00012074233],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981009,0.00008271397,0.00048205853,0.00030362688,0.00044917496,0.0005815695],"domain_scores_gemma":[0.997772,0.0005387362,0.00028786663,0.00040182835,0.00022262499,0.00077699183],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005904054,0.00017129818,0.0003400123,0.00012329669,0.0009309378,0.00005487802,0.002095463,0.000060786653,0.0028645075],"category_scores_gemma":[0.00051573396,0.0000858794,0.00020845278,0.0007589153,0.0012980702,0.00018575675,0.000012007543,0.00025097548,0.000022738923],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008695534,0.000005999867,0.9972337,0.0000032603405,0.00003092428,0.00004357058,0.00022760806,0.0011493403,0.000024869443,5.8251453e-7,0.00012654086,0.0011449311],"study_design_scores_gemma":[0.00021961244,0.00022260284,0.98615587,0.000038249982,0.000087256594,0.00009897347,0.00024346607,0.0040275725,0.000089670146,0.00023298459,0.008445083,0.00013866878],"about_ca_topic_score_codex":0.7570587,"about_ca_topic_score_gemma":0.9986394,"teacher_disagreement_score":0.24158077,"about_ca_system_score_codex":0.000003925282,"about_ca_system_score_gemma":0.003167817,"threshold_uncertainty_score":0.998047},"labels":[],"label_agreement":null},{"id":"W1983252230","doi":"10.1139/e00-029","title":"Tectonic setting of the Taltson magmatic zone at 1.92.0 Ga: a granitoid-based perspective","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Subduction; Magmatism; Crust; Continental crust; Tectonics; Back-arc basin; Continental margin; Phanerozoic; Mantle (geology); Laurentia; Paleontology; Plate tectonics; Geochemistry; Cenozoic; Structural basin","score_opus":0.009091304155470825,"score_gpt":0.18392769405298062,"score_spread":0.1748363898975098,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983252230","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9881982,0.0012016451,0.000005085786,0.0031843071,0.00009807218,0.00005343007,0.0000240276,0.0000024816543,0.0072327508],"genre_scores_gemma":[0.9989743,0.000010613963,0.00039819413,0.0003200366,0.000048905265,1.2108181e-7,9.884067e-7,9.286445e-7,0.00024589908],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987287,0.00010070551,0.0002984536,0.00015067414,0.0003639952,0.00035748887],"domain_scores_gemma":[0.99905986,0.00015430391,0.0002049081,0.00010397553,0.00012283787,0.00035410305],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00058692734,0.000098238976,0.00021228672,0.00013760336,0.0004805783,0.000050980732,0.00051692466,0.000037333884,0.021350872],"category_scores_gemma":[0.00019409345,0.000053338557,0.00018648159,0.0009423759,0.00072262064,0.00012464268,0.0000046535715,0.00016885866,0.00006037072],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015330408,0.000007654658,0.9731908,0.000008128983,0.000017293829,0.000020986077,0.000297727,0.021493047,0.00018553434,0.00003411987,0.00007178398,0.004657604],"study_design_scores_gemma":[0.00019052294,0.00028836838,0.98593503,0.000067095316,0.000039474366,0.000084230334,0.00058854173,0.0072594746,0.0009828671,0.0034502966,0.0009920024,0.00012208102],"about_ca_topic_score_codex":0.050413568,"about_ca_topic_score_gemma":0.6263705,"teacher_disagreement_score":0.5759569,"about_ca_system_score_codex":0.0000051741517,"about_ca_system_score_gemma":0.00057910406,"threshold_uncertainty_score":0.97954375},"labels":[],"label_agreement":null},{"id":"W1983483840","doi":"10.1139/e09-038","title":"The enigmatic diapsid Acerosodontosaurus piveteaui (Reptilia: Neodiapsida) from the Upper Permian of Madagascar and the paraphyly of “younginiform” reptiles","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Muséum National d'Histoire Naturelle; Deutsche Forschungsgemeinschaft","keywords":"Paraphyly; Monophyly; Taxon; Clade; Phylogenetic tree; Biology; Paleontology; Permian; Evolutionary biology","score_opus":0.011275508700327123,"score_gpt":0.20043978463330453,"score_spread":0.1891642759329774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983483840","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9675134,0.021522146,0.000006948686,0.0058360365,0.00043824303,0.00010985265,0.00007496012,0.000002370826,0.004496054],"genre_scores_gemma":[0.9986894,0.00058408704,0.00026707363,0.00031621213,0.00010374922,2.6423126e-7,0.000002386863,9.246567e-7,0.000035890844],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984611,0.0003176049,0.00045765616,0.00014438495,0.00025560558,0.00036363822],"domain_scores_gemma":[0.9978895,0.0011883439,0.00041349253,0.00020077672,0.000095533935,0.00021234152],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0017543228,0.00011918904,0.000276916,0.00008914511,0.00095405296,0.000056238194,0.00077641505,0.000077214514,0.00015618841],"category_scores_gemma":[0.00029953464,0.000050995204,0.00013432436,0.00026942277,0.0041763936,0.00022801073,0.000006005539,0.00023199244,0.000004738539],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000093308074,0.0000030278247,0.986877,0.0000027287297,0.000042321124,0.000014292529,0.0017683544,0.00044763988,0.000029013388,0.001979283,0.00032875116,0.008414243],"study_design_scores_gemma":[0.0002851256,0.00030081137,0.98970836,0.000035342884,0.000031825668,0.00016955397,0.0029710063,0.0010244425,0.000023745022,0.0036900106,0.0016952783,0.00006451107],"about_ca_topic_score_codex":0.015686737,"about_ca_topic_score_gemma":0.36379305,"teacher_disagreement_score":0.3481063,"about_ca_system_score_codex":0.0000016334677,"about_ca_system_score_gemma":0.0006708242,"threshold_uncertainty_score":0.99853367},"labels":[],"label_agreement":null},{"id":"W1983605173","doi":"10.1139/e07-057","title":"The Holdfast of <i>Gilbertsocrinus tuberosus</i> (Mississippian, Crinoidea)This article is one of a selection of papers published in this Special Issue on the theme <i>The dynamic reef and shelly communities of the Paleozoic. This Special is in honour of our colleague and friend Paul Copper</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Holdfast; Crinoid; Paleontology; Geology; Devonian; Viséan; Carboniferous; Biology; Botany","score_opus":0.016951168058287534,"score_gpt":0.2062852985322005,"score_spread":0.18933413047391298,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983605173","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96769017,0.0018396056,1.16116944e-7,0.0052480656,0.0002734652,0.00018502168,0.000107223066,7.9127426e-7,0.024655513],"genre_scores_gemma":[0.99888265,0.00062591897,0.00004504489,0.00013840254,0.00012941132,5.467661e-7,3.171057e-7,0.0000014984712,0.00017622435],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978353,0.0004532437,0.00074025645,0.00014671749,0.00048940105,0.00033513203],"domain_scores_gemma":[0.99816424,0.00065718614,0.00064501475,0.00021694941,0.0001722437,0.00014434756],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001806837,0.00014591958,0.00040775313,0.0002526921,0.0006827254,0.000055051052,0.0007063531,0.00008734794,0.0014237353],"category_scores_gemma":[0.00028323103,0.00007814053,0.00011289765,0.00092121377,0.002987028,0.00029220225,0.000008906421,0.00042535376,3.7376927e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014197096,0.000032741656,0.97558016,0.000022335076,0.00004126057,0.000008069212,0.016011639,0.000051283663,0.000437051,0.00009944774,0.0023959468,0.0051781232],"study_design_scores_gemma":[0.00039588762,0.0005269064,0.9813145,0.00016408555,0.000019795216,0.00009325767,0.012037973,0.00023680835,0.0037949267,0.0003140453,0.0010148451,0.00008699269],"about_ca_topic_score_codex":0.026079223,"about_ca_topic_score_gemma":0.66395944,"teacher_disagreement_score":0.6378802,"about_ca_system_score_codex":0.000004001239,"about_ca_system_score_gemma":0.0007913848,"threshold_uncertainty_score":0.9997263},"labels":[],"label_agreement":null},{"id":"W1983765469","doi":"10.1139/e01-084","title":"Integrated teleseismic studies of the southern Alberta upper mantle","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Lithosphere; Seismometer; Subduction; Seismology; Mantle (geology); Receiver function; Magnetotellurics; Tectonics; Crust; Seismic array; Geophysics; Petrology; Electrical resistivity and conductivity","score_opus":0.028906027961729,"score_gpt":0.20761807597400125,"score_spread":0.17871204801227225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983765469","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9919244,0.001935203,0.0000015198162,0.000940095,0.0010009683,0.00004943372,0.000064505155,0.0000011630739,0.004082717],"genre_scores_gemma":[0.9977766,0.000046740086,0.00014102441,0.00015342637,0.00009644148,7.448308e-8,4.6115935e-7,0.0000014647443,0.0017837153],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909055,0.00007520663,0.00026151445,0.00009394498,0.00022312434,0.00025564668],"domain_scores_gemma":[0.99927825,0.00010305724,0.00020981742,0.00010312514,0.000120017554,0.0001857472],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042279653,0.00008295016,0.00019225568,0.00011234511,0.00028575805,0.000073930474,0.00050581846,0.000027348484,0.002962986],"category_scores_gemma":[0.00015310681,0.000043197204,0.00007509246,0.00033836588,0.0006083577,0.00016959151,0.000005968847,0.00008516093,0.00009786094],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016588272,0.000020859274,0.9505741,0.00004975698,0.00019328156,0.000054382246,0.016143486,0.0086691165,0.001195905,0.0007495219,0.008842656,0.013490344],"study_design_scores_gemma":[0.000867592,0.0011527041,0.727137,0.0007663369,0.00017551727,0.00033264284,0.021212284,0.00674612,0.0054673576,0.0073852967,0.22794034,0.0008168015],"about_ca_topic_score_codex":0.073977955,"about_ca_topic_score_gemma":0.41331145,"teacher_disagreement_score":0.33933347,"about_ca_system_score_codex":8.392041e-7,"about_ca_system_score_gemma":0.0002734047,"threshold_uncertainty_score":0.99794847},"labels":[],"label_agreement":null},{"id":"W1983825785","doi":"10.1139/e08-070","title":"Diversity and variation of theropod dinosaur teeth from the uppermost Santonian Milk River Formation (Upper Cretaceous), Alberta: a quantitative method supporting identification of the oldest dinosaur tooth assemblage in Canada","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Cretaceous; Taxon; Geology; Paleontology; Range (aeronautics); Geography; Zoology; Biology","score_opus":0.025780009736453394,"score_gpt":0.2304634249128959,"score_spread":0.2046834151764425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983825785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973971,0.000634168,0.00021042774,0.0011114822,0.00025767682,0.000095766125,0.00009856134,5.6092534e-7,0.00019423323],"genre_scores_gemma":[0.9992711,0.000059098922,0.0005178754,0.00011748382,0.000017180006,1.3795615e-7,0.00000451796,7.1119626e-7,0.00001189033],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986609,0.00036902446,0.0004115559,0.00012317735,0.00022440356,0.00021094458],"domain_scores_gemma":[0.9984325,0.0006796715,0.00060032477,0.00008721163,0.000099657525,0.000100609825],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009943699,0.000077385,0.00017421006,0.00010173855,0.0011868078,0.000010056897,0.00037009848,0.000049044094,0.00009894352],"category_scores_gemma":[0.0003967162,0.000046208057,0.000041352396,0.00033122054,0.0006249029,0.0004770146,0.000021051696,0.00013909595,7.196799e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010691174,0.0000025446016,0.9905273,0.0000029668054,0.000011730821,0.000006198178,0.0078829,0.00092145434,0.00021268496,0.00008660656,0.000019776704,0.00031519923],"study_design_scores_gemma":[0.00013019991,0.00006266139,0.9914696,0.000024667032,0.000016162345,0.00006431709,0.0020466957,0.005556945,0.00016142262,0.0003524154,0.000060080947,0.00005482316],"about_ca_topic_score_codex":0.9593889,"about_ca_topic_score_gemma":0.99887645,"teacher_disagreement_score":0.03948755,"about_ca_system_score_codex":0.000011465736,"about_ca_system_score_gemma":0.0015991864,"threshold_uncertainty_score":0.91280854},"labels":[],"label_agreement":null},{"id":"W1983914751","doi":"10.1139/e07-007","title":"Neomorphism of the Middle Devonian Ratner limestone related to dehydration of gypsum in south-central Saskatchewan","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Regina","funders":"Natural Sciences and Engineering Research Council of Canada; University of Saskatchewan","keywords":"Anhydrite; Geology; Devonian; Gypsum; Calcite; Carbonate; Geochemistry; Mineralogy; Dolomite; Aragonite; Paleontology; Chemistry","score_opus":0.02050292901310472,"score_gpt":0.21207469107678534,"score_spread":0.19157176206368062,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983914751","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921824,0.0019016683,0.00002619202,0.00040507273,0.0005302068,0.00008717737,0.000015963758,0.0000011480062,0.004850203],"genre_scores_gemma":[0.9991046,0.0000023447176,0.0007633496,0.00006266111,0.000023824015,4.7613003e-8,4.0154572e-7,5.272786e-7,0.000042212803],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986352,0.000083659754,0.0005113053,0.000112811074,0.00025849693,0.0003985683],"domain_scores_gemma":[0.99905527,0.0000881834,0.00031105016,0.00009445746,0.00007884156,0.0003721825],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013321069,0.00008317278,0.0001942712,0.0004012874,0.0001839541,0.000022204893,0.00041858724,0.000077660436,0.00015109983],"category_scores_gemma":[0.00011600843,0.00005681564,0.00008540568,0.00093703053,0.0007332207,0.00021390726,0.0000010850665,0.00018521791,0.0000019921458],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016149954,0.000004442053,0.9877924,0.0000031256775,0.000007853911,0.00002629981,0.0064290795,0.0012743119,0.0003179839,0.00007209088,0.000009398665,0.0040469174],"study_design_scores_gemma":[0.00016901024,0.00023172073,0.99495685,0.00007000794,0.000007825827,0.00004102421,0.0022308645,0.0001101145,0.001710042,0.00034188238,0.000064109896,0.00006656936],"about_ca_topic_score_codex":0.014760355,"about_ca_topic_score_gemma":0.86296636,"teacher_disagreement_score":0.848206,"about_ca_system_score_codex":0.0000017512225,"about_ca_system_score_gemma":0.001623829,"threshold_uncertainty_score":0.9918004},"labels":[],"label_agreement":null},{"id":"W1984024090","doi":"10.1139/e02-047","title":"An Early Devonian (Emsian) acanthodian from the Bear Rock Formation, Anderson River, Northwest Territories, Canada","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature","funders":"","keywords":"Devonian; Geology; Paleontology; Genus; Outcrop; Taxon; Zoology; Biology","score_opus":0.018413557903956358,"score_gpt":0.18889639775958442,"score_spread":0.17048283985562807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984024090","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98844755,0.0044236076,0.000045943656,0.0035780927,0.0014762521,0.00006182536,0.00055838726,0.0000045471616,0.0014038001],"genre_scores_gemma":[0.9982565,0.000060181326,0.0003482871,0.0008391792,0.00040773462,1.80484e-7,0.00004077668,0.0000013919157,0.00004578356],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986035,0.0001833574,0.00029149218,0.0001686417,0.0002560821,0.0004969276],"domain_scores_gemma":[0.99869704,0.00016798389,0.00019467366,0.00013627452,0.000096284595,0.00070771377],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037060393,0.00012297281,0.00016190394,0.000113069844,0.001286447,0.00011386672,0.0007408916,0.00008400849,0.0021354423],"category_scores_gemma":[0.000085788015,0.000082724626,0.000041402032,0.00032653293,0.00057615794,0.00095232,0.0000024927017,0.00024155038,0.00003174865],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004406436,0.000002069719,0.99411607,6.893144e-7,0.000009135683,0.00007329485,0.0009201301,0.00047599693,0.0000010593438,0.000022472761,0.0012524716,0.0031222159],"study_design_scores_gemma":[0.00012507162,0.00023523724,0.95656526,0.000012121019,0.000008783826,0.00015310365,0.00085167825,0.0024458303,0.0000054809307,0.000176256,0.039305955,0.0001152257],"about_ca_topic_score_codex":0.9848563,"about_ca_topic_score_gemma":0.9999463,"teacher_disagreement_score":0.038053483,"about_ca_system_score_codex":0.0000084867315,"about_ca_system_score_gemma":0.0017151585,"threshold_uncertainty_score":0.99877673},"labels":[],"label_agreement":null},{"id":"W1984276289","doi":"10.1139/e2012-058","title":"The contact aureole of the South Mountain Batholith in Halifax, Nova Scotia: geology, mineral assemblages, and isograds","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Dalhousie University","keywords":"Geology; Andalusite; Metamorphism; Geochemistry; Metamorphic rock; Hornfels; Biotite; Greenschist; Batholith; Isograd; Cordierite; Dalradian; Sillimanite; Muscovite; Metamorphic facies; Facies; Geomorphology; Paleontology; Quartz","score_opus":0.017465365396575373,"score_gpt":0.20603510402958916,"score_spread":0.1885697386330138,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984276289","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913178,0.004332593,0.000003817946,0.0026175,0.00025281022,0.00004489755,0.000020307303,9.1327666e-7,0.0014093682],"genre_scores_gemma":[0.99937683,0.000019904302,0.00011870309,0.00032387685,0.00007778574,6.224405e-8,9.90998e-7,6.830753e-7,0.000081143786],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987515,0.00014170648,0.00029941607,0.00010391445,0.00022780875,0.00047561305],"domain_scores_gemma":[0.99905545,0.00021657697,0.00019768073,0.00009098996,0.00006596772,0.00037333652],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014838806,0.00009174779,0.00019264115,0.00012066326,0.0002546907,0.000059487902,0.00044952947,0.000044848028,0.0005649805],"category_scores_gemma":[0.00030489167,0.000041026004,0.0000830081,0.0005534731,0.0010536034,0.00021532043,0.000012874991,0.00021200482,0.000007700867],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004246154,0.0000032068613,0.99851745,0.0000017501809,0.0000072932235,0.00000468354,0.0002742031,0.00024358415,0.000046382458,0.00029204026,0.000054309803,0.00055084337],"study_design_scores_gemma":[0.000103032544,0.00009655558,0.99564475,0.000014214637,0.000012683766,0.000062625,0.0009712141,0.00031247945,0.00008379345,0.0012823248,0.0013542623,0.00006206901],"about_ca_topic_score_codex":0.10990013,"about_ca_topic_score_gemma":0.82040614,"teacher_disagreement_score":0.71050596,"about_ca_system_score_codex":0.0000014563063,"about_ca_system_score_gemma":0.00027972227,"threshold_uncertainty_score":0.89602715},"labels":[],"label_agreement":null},{"id":"W1984552613","doi":"10.1139/e05-009","title":"Crustal structure and lithology of the northern Canadian Cordillera: alternative interpretations of SNORCLE seismic reflection lines 2a and 2b","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Terrane; Crust; Batholith; Lithology; Continental crust; Allochthon; Paleontology; Sedimentary rock; Accretion (finance); Basement; Fault (geology); Tectonics; Seismology; Nappe","score_opus":0.011580318261512653,"score_gpt":0.21154665587778348,"score_spread":0.19996633761627083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984552613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959098,0.0007863663,0.000005837226,0.0021198634,0.00010343913,0.000034306817,0.00006765913,6.426571e-7,0.000972083],"genre_scores_gemma":[0.9994257,0.00002369745,0.00025626292,0.00020476019,0.00005166998,4.7927667e-8,0.0000014806595,5.935607e-7,0.000035764708],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99933195,0.00005872091,0.00021713522,0.00010109337,0.0001191958,0.00017191545],"domain_scores_gemma":[0.99927205,0.00007481969,0.00017435722,0.000046089346,0.00013518882,0.00029751455],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018162648,0.000064927284,0.0001588275,0.00018295427,0.00020620527,0.000027184884,0.00018076676,0.000038699753,0.0007383162],"category_scores_gemma":[0.00015390314,0.000036813224,0.00004304794,0.00032417345,0.000767936,0.0001423391,0.000005356206,0.00012254334,8.12578e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004492023,0.0000011498088,0.98382187,0.0000031849866,0.000015306157,0.0000028901768,0.0004726503,0.0071045817,0.00013923249,0.000018374156,0.000007541995,0.0084087085],"study_design_scores_gemma":[0.0000994581,0.00027491502,0.9859663,0.000025072039,0.000029409239,0.00010770265,0.0003677817,0.00924921,0.0011446906,0.0021969585,0.00047582304,0.00006267337],"about_ca_topic_score_codex":0.35250446,"about_ca_topic_score_gemma":0.98997027,"teacher_disagreement_score":0.6374658,"about_ca_system_score_codex":0.000002060659,"about_ca_system_score_gemma":0.000397395,"threshold_uncertainty_score":0.8084045},"labels":[],"label_agreement":null},{"id":"W1984570076","doi":"10.1139/e02-009","title":"Les erratiques de dolomie à Rivière-Blanche, côte sud de l'estuaire maritime du Saint-Laurent : un indicateur de transport glaciaire et glaciel","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval","funders":"","keywords":"Dolostone; Geology; Proterozoic; Lithology; Sedimentary rock; Geomorphology; Gneiss; Paleontology; Carbonate rock; Metamorphic rock","score_opus":0.0227990840666259,"score_gpt":0.22218837866962915,"score_spread":0.19938929460300325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984570076","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9685963,0.008148677,0.00039192036,0.0039280825,0.00020878915,0.00007840236,0.00003845217,0.000015937632,0.018593455],"genre_scores_gemma":[0.9951732,0.00037483274,0.0036257498,0.0006265358,0.00013796112,6.293409e-7,0.000002361433,0.0000018968469,0.000056841123],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99791896,0.000294896,0.00040529974,0.00023428822,0.00029568403,0.00085084426],"domain_scores_gemma":[0.9983206,0.00015523698,0.00024193253,0.00011242264,0.00006608514,0.0011037573],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018952263,0.00019874828,0.00029080152,0.00036645666,0.000784115,0.0001497472,0.0006740716,0.00017930478,0.0013520918],"category_scores_gemma":[0.00014098325,0.000164513,0.00016437926,0.00040580262,0.0010032315,0.0005207523,0.0000011895504,0.0004614042,0.000009074623],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010783154,0.000012214445,0.9680703,0.0000078585845,0.000026798445,0.0005186662,0.0020370008,0.0003772173,0.000015829555,0.00039915147,0.00036381237,0.028160354],"study_design_scores_gemma":[0.00023449044,0.00033850354,0.9920956,0.00006364433,0.000027958295,0.0010010481,0.00037995935,0.0012679327,0.000088742905,0.0014592232,0.0028438042,0.00019912558],"about_ca_topic_score_codex":0.05564946,"about_ca_topic_score_gemma":0.8076789,"teacher_disagreement_score":0.7520294,"about_ca_system_score_codex":0.000010405996,"about_ca_system_score_gemma":0.0017311529,"threshold_uncertainty_score":0.99956083},"labels":[],"label_agreement":null},{"id":"W1984589303","doi":"10.1139/e04-056","title":"A comparative SEM study on the micromorphology of glacial and nonglacial clasts with varying age and lithology","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Vedecká Grantová Agentúra MŠVVaŠ SR a SAV; American Alpine Club","keywords":"Clastic rock; Glacial period; Geology; Lithology; Sedimentary depositional environment; Basalt; Geochemistry; Quartz; Sedimentary rock; Paleontology","score_opus":0.05016927267639913,"score_gpt":0.26887944305850797,"score_spread":0.21871017038210883,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984589303","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996241,0.00034443353,0.000004676076,0.0011606938,0.00011492307,0.00012561785,0.000007363666,0.0000010355875,0.0020002807],"genre_scores_gemma":[0.99958414,0.000008259339,0.00020486103,0.0001622179,0.000029313856,2.4394888e-7,5.308227e-7,7.4691974e-7,0.000009678887],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990013,0.00023839949,0.00018047227,0.00014795782,0.00013669541,0.00029515885],"domain_scores_gemma":[0.99919677,0.0003270714,0.00012726642,0.000058951242,0.00006588753,0.00022406946],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0009022337,0.00008521148,0.00024984844,0.00023452018,0.0004711348,0.000039294075,0.00021653387,0.000051814408,0.00013180317],"category_scores_gemma":[0.000065003325,0.000047946804,0.000016944341,0.0002513791,0.003019878,0.00010388084,0.000006359116,0.0002677322,0.0000061429255],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007299353,0.000009555678,0.99496776,0.000001967493,0.000019231351,0.0006588815,0.0037664867,0.0002571407,0.000018466035,0.00017075393,0.0000035383648,0.000053219985],"study_design_scores_gemma":[0.00053215335,0.0030017984,0.99196494,0.000018357166,0.0000116216415,0.0015791313,0.0021762082,0.000016625967,0.00007328403,0.0005348486,0.000036069116,0.00005493664],"about_ca_topic_score_codex":0.002464356,"about_ca_topic_score_gemma":0.47934055,"teacher_disagreement_score":0.4768762,"about_ca_system_score_codex":3.5092143e-7,"about_ca_system_score_gemma":0.00065144256,"threshold_uncertainty_score":0.99969333},"labels":[],"label_agreement":null},{"id":"W1984626430","doi":"10.1139/e06-009","title":"Paleoproterozoic submarine intrabasinal rifting, Baffin Island, Nunavut, Canada: volcanic structure and geochemistry of the Bravo Lake Formation","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Rift; Pillow lava; Mafic; Mantle plume; Volcanic rock; Basalt; Metamorphism; Continental crust; Breccia; Crust; Paleontology; Volcano; Tectonics","score_opus":0.0052305639754083606,"score_gpt":0.15427031884906658,"score_spread":0.14903975487365823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984626430","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967293,0.0006346375,0.000005655399,0.0010410151,0.00011366327,0.000038791895,0.00014391556,0.0000010976997,0.0012918852],"genre_scores_gemma":[0.99955493,0.0000068781374,0.00012362513,0.00013469992,0.000097424934,5.4036846e-8,0.000009837709,6.710624e-7,0.00007188486],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989446,0.00003704595,0.00031557144,0.000115651346,0.00030446285,0.0002826869],"domain_scores_gemma":[0.9992664,0.00005122102,0.00027443533,0.00007305004,0.000104385654,0.00023051472],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025227884,0.00009657259,0.00016862465,0.000064576205,0.00027300528,0.00006250709,0.00033083852,0.000043794113,0.0032187868],"category_scores_gemma":[0.000112287096,0.000054747376,0.000054183198,0.0003934854,0.0004013641,0.00015790504,0.000008075609,0.00018034871,6.949297e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002976876,0.0000014101604,0.9969964,0.000010535873,0.000005069903,0.000011997873,0.00001919943,0.0013295528,0.0001832002,0.000015672196,0.00023359177,0.0011903697],"study_design_scores_gemma":[0.00010175935,0.000051038074,0.99224526,0.000024343344,0.000016631757,0.00017085472,0.00006672134,0.0014894431,0.0023660278,0.0021819337,0.0012069484,0.00007905302],"about_ca_topic_score_codex":0.7276463,"about_ca_topic_score_gemma":0.9998857,"teacher_disagreement_score":0.2722394,"about_ca_system_score_codex":0.0000022141967,"about_ca_system_score_gemma":0.000910484,"threshold_uncertainty_score":0.9976924},"labels":[],"label_agreement":null},{"id":"W1984752709","doi":"10.1139/e11-068","title":"The variation of angles between anterior and posterior carinae of tyrannosaurid teeth","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Discriminant function analysis; Principal component analysis; Variation (astronomy); Dentition; Taxon; Data set; Paleontology; Multivariate statistics; Posterior teeth; Statistics; Geology; Biology; Evolutionary biology; Mathematics; Orthodontics","score_opus":0.01943672324200467,"score_gpt":0.21919315401747413,"score_spread":0.19975643077546945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984752709","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887557,0.009529024,0.000010129526,0.00040936325,0.00037256692,0.000032639768,0.000050606104,7.0285455e-7,0.0008392457],"genre_scores_gemma":[0.99941725,0.000089549925,0.00035172873,0.00002620776,0.00010139506,4.4304787e-8,0.0000011515405,4.4742012e-7,0.000012256689],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992502,0.000101185666,0.00025682416,0.000055771252,0.00009802036,0.00023802552],"domain_scores_gemma":[0.99920547,0.0002198147,0.00025132773,0.000049069335,0.0000679254,0.0002063704],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010820779,0.000050501934,0.00014714159,0.0001284802,0.00026769115,0.000013717843,0.00020231714,0.00004580499,0.000091081936],"category_scores_gemma":[0.00012427724,0.00003064855,0.000031977594,0.0001545094,0.0010224159,0.00027663875,0.0000033255656,0.00007019245,0.0000020250966],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008292984,0.0000010788574,0.993472,0.0000035683365,0.000010192004,0.0000014355668,0.00034719406,0.000011304039,0.00009412738,0.00007701504,0.0000074027394,0.005966406],"study_design_scores_gemma":[0.00006847373,0.00028653574,0.99798465,0.00001846217,0.000012195651,0.000110054076,0.0002194259,0.00002938902,0.00006913749,0.00020896996,0.0009569257,0.000035778325],"about_ca_topic_score_codex":0.010485222,"about_ca_topic_score_gemma":0.17102607,"teacher_disagreement_score":0.16054085,"about_ca_system_score_codex":6.5929913e-7,"about_ca_system_score_gemma":0.0003726762,"threshold_uncertainty_score":0.99610406},"labels":[],"label_agreement":null},{"id":"W1984823209","doi":"10.1139/e05-100","title":"Mechanisms of slope failure on Pyramid Mountain, a subglacial volcano in Wells Gray Provincial Park, British Columbia","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Geomorphology; Rock mass classification; Landslide; Volcano; Lithification; Breccia; Geotechnical engineering; Seismology; Sediment","score_opus":0.00409620540924968,"score_gpt":0.17390491062656646,"score_spread":0.16980870521731678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984823209","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99193513,0.00005588369,0.00002645894,0.00034793114,0.00033442015,0.00013068608,0.00002382135,0.0000027092442,0.007142977],"genre_scores_gemma":[0.9984485,0.000008305316,0.00047977455,0.00016178234,0.00007464675,9.679313e-7,0.0000010271093,0.0000064733754,0.00081852986],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99834543,0.000054799526,0.00042067928,0.00020429974,0.00051656476,0.00045824086],"domain_scores_gemma":[0.9992985,0.000023205745,0.00024544448,0.00008248642,0.000032080447,0.00031827905],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00080191775,0.00009277778,0.00022183398,0.0001244635,0.00027010372,0.00026824142,0.00042688646,0.00010500104,0.0020033137],"category_scores_gemma":[0.00005315728,0.000095517,0.000083086765,0.00059855403,0.00067189196,0.0002943508,0.000020801952,0.0002344353,0.00002416843],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018285045,0.000061688566,0.9790968,0.000007736185,0.000008272363,0.00059895276,0.00022262528,0.0070415833,0.0021240923,0.0005370362,0.0073767263,0.002906253],"study_design_scores_gemma":[0.0007351104,0.0008220511,0.96662885,0.0001740318,0.000015163396,0.00024525862,0.00029594795,0.00022494458,0.00093203044,0.008004584,0.021640612,0.00028140194],"about_ca_topic_score_codex":0.460798,"about_ca_topic_score_gemma":0.9907308,"teacher_disagreement_score":0.52993286,"about_ca_system_score_codex":0.000055755703,"about_ca_system_score_gemma":0.000694837,"threshold_uncertainty_score":0.998909},"labels":[],"label_agreement":null},{"id":"W1985017621","doi":"10.1139/e03-050","title":"Relict tufa at Miette Hot Springs, Jasper National Park, Alberta, Canada","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Parks Canada","keywords":"Tufa; Geology; Calcite; Facies; Precipitation; Algal mat; Paleontology; Geomorphology; Ecology; Algae; Biology; Geography; Carbonate; Chemistry","score_opus":0.022936356713621413,"score_gpt":0.21933265928755102,"score_spread":0.19639630257392962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985017621","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9101452,0.0013269566,0.0000011944669,0.0023041535,0.0007992715,0.000047974176,0.000011020129,0.000001335118,0.08536288],"genre_scores_gemma":[0.99589175,0.000029477189,0.00028804294,0.001224214,0.000065651686,1.8124891e-7,0.0000035944697,0.000001588876,0.0024955026],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99815375,0.00017718946,0.0002899977,0.00019471384,0.0005282475,0.0006560895],"domain_scores_gemma":[0.99835956,0.00040922724,0.00014160645,0.000085085536,0.00018854317,0.0008159664],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013110661,0.00011449728,0.00018492299,0.0002578311,0.0007945804,0.000064727836,0.00044929227,0.00007718057,0.010375074],"category_scores_gemma":[0.0006727411,0.00009027947,0.000058582154,0.00040147986,0.00068396976,0.00023414007,0.0000041921853,0.0002807526,0.00020381919],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006477893,0.0000014140561,0.9953263,0.0000024724188,0.000012416912,0.00014084928,0.00006332748,0.0009478174,0.000002119453,0.00043160302,0.0030227199,0.000042493593],"study_design_scores_gemma":[0.00015428216,0.00009684666,0.8665624,0.000012334919,0.0000051767393,0.0010607897,0.00009140479,0.00014620388,0.000113010436,0.0004436237,0.13119371,0.00012017084],"about_ca_topic_score_codex":0.80448747,"about_ca_topic_score_gemma":0.99972117,"teacher_disagreement_score":0.19523367,"about_ca_system_score_codex":0.0000037519517,"about_ca_system_score_gemma":0.008919221,"threshold_uncertainty_score":0.9966993},"labels":[],"label_agreement":null},{"id":"W1985039445","doi":"10.1139/e10-105","title":"A tale of both sides of Iapetus – upper Darriwilian (Ordovician) graptolite faunal dynamics on the edges of two continents","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Biozone; Ordovician; Paleontology; Geology; Laurentia; Fauna; Baltica; Group (periodic table); Biostratigraphy; Ecology","score_opus":0.027966471464503668,"score_gpt":0.2230473507801115,"score_spread":0.19508087931560783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985039445","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95792174,0.0021696445,0.00002259043,0.00021315795,0.00033186653,0.00007049027,0.00014236577,0.0000013689114,0.03912678],"genre_scores_gemma":[0.9993297,0.000032844855,0.00052889006,0.000056717916,0.000026833177,1.2357505e-7,9.1516637e-7,7.8422374e-7,0.000023201284],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985792,0.00012272308,0.0005087157,0.00013072313,0.0003203739,0.00033824603],"domain_scores_gemma":[0.9986187,0.00021032174,0.0005831019,0.00014292962,0.00014420075,0.00030070177],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00091316923,0.000119746546,0.0003140152,0.0003924617,0.0002560711,0.000021286796,0.00066243164,0.000053850366,0.00050593325],"category_scores_gemma":[0.00013433848,0.00007527118,0.00016932964,0.00043228964,0.0021711024,0.00025619657,0.0000015150827,0.00016890682,0.0000016915237],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002503005,0.000011351171,0.985453,0.000008819027,0.000033495926,0.000015375856,0.00086099905,0.000054552893,0.000041492152,0.0026357472,0.000017247196,0.010842853],"study_design_scores_gemma":[0.0001778195,0.0006721323,0.99364346,0.00010900588,0.000021240223,0.00004315048,0.0010173881,0.00027482604,0.0010628956,0.0028411176,0.00005774397,0.00007922164],"about_ca_topic_score_codex":0.033317145,"about_ca_topic_score_gemma":0.5384128,"teacher_disagreement_score":0.50509566,"about_ca_system_score_codex":8.8869143e-7,"about_ca_system_score_gemma":0.00066598965,"threshold_uncertainty_score":0.9731201},"labels":[],"label_agreement":null},{"id":"W1985174844","doi":"10.1139/e01-024","title":"Paleoproterozoic carbonatitic ultrabasic volcanic rocks (meimechites?) of Cape Smith Belt, Quebec","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Geochemistry; Lapilli; Ultramafic rock; Phlogopite; Chromite; Carbonatite; Greenschist; Zircon; Olivine; Metasomatism; Metamorphism; Pyroclastic rock; Volcano; Mantle (geology)","score_opus":0.01349337432757977,"score_gpt":0.18644745102540886,"score_spread":0.17295407669782908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985174844","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9874643,0.002789301,0.000038192942,0.000885882,0.00020366094,0.000058866837,0.000024218243,0.0000042705447,0.008531283],"genre_scores_gemma":[0.99882853,0.00006469956,0.00032771274,0.000244215,0.00011135959,1.9047647e-7,0.000004265252,0.0000014546561,0.0004175746],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99830025,0.0000727624,0.0004677725,0.0002090425,0.0004273847,0.0005227816],"domain_scores_gemma":[0.9984977,0.0001488772,0.00029044948,0.00011756559,0.00017047708,0.0007749313],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00055390835,0.00014628693,0.0003291461,0.00036070356,0.0002503346,0.000077602184,0.00059170014,0.0000644699,0.008641697],"category_scores_gemma":[0.00024817386,0.00009825747,0.00017496975,0.0010141315,0.0006531707,0.00025893206,0.0000049719442,0.00022465421,0.000035643618],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000064216533,0.000006951969,0.9913992,0.000006743996,0.000021309586,0.00009053307,0.00008578331,0.0029070775,0.00010233117,0.000025647074,0.000041269035,0.005306706],"study_design_scores_gemma":[0.00016518138,0.00039993526,0.9906974,0.000057996614,0.0000439158,0.00019522573,0.00025189618,0.0014079971,0.0005169726,0.0042263186,0.0018647356,0.00017243037],"about_ca_topic_score_codex":0.32247496,"about_ca_topic_score_gemma":0.9684716,"teacher_disagreement_score":0.64599663,"about_ca_system_score_codex":0.000002523617,"about_ca_system_score_gemma":0.0011411988,"threshold_uncertainty_score":0.99226457},"labels":[],"label_agreement":null},{"id":"W1985286786","doi":"10.1139/e03-010","title":"Le terrane de Slide Mountain (Cordillères canadiennes) : une lithosphère océanique marquée par des points chauds","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Terrane; Geochemistry; Basalt; Ultramafic rock; Mantle plume; Volcanic rock; Island arc; Mantle (geology); Mafic; Permian; Subduction; Volcano; Paleontology; Structural basin; Tectonics; Lithosphere","score_opus":0.013766432384748582,"score_gpt":0.18707951876590925,"score_spread":0.17331308638116066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985286786","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97655797,0.0016065215,0.000076918834,0.0022688876,0.00014701212,0.000051473882,0.000027745155,0.000006294653,0.019257165],"genre_scores_gemma":[0.9952608,0.000053600004,0.0036547545,0.0007517565,0.00006891029,3.4323435e-7,0.0000035876603,0.000002319351,0.00020396753],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99809045,0.0001794701,0.00037457806,0.0002444552,0.0002542365,0.0008567999],"domain_scores_gemma":[0.99796647,0.00013920433,0.00017387727,0.00011644832,0.00014135662,0.0014626629],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013864209,0.00016750667,0.00029405946,0.0002507925,0.0007359849,0.00015641654,0.00052198727,0.00007829473,0.0049200943],"category_scores_gemma":[0.0005864669,0.000120483804,0.0001477048,0.0009882937,0.0009889626,0.00035099857,0.0000049009,0.00023525875,0.00003820058],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000063668836,0.000006670412,0.9941018,0.0000063433695,0.000019762569,0.00021494739,0.0003182785,0.0017471435,0.0000711021,0.0013700529,0.00012575167,0.0020117466],"study_design_scores_gemma":[0.00020750267,0.00036103514,0.923742,0.000046438483,0.000027775879,0.0005052368,0.0009851889,0.00060859794,0.0011818035,0.053938225,0.018124335,0.00027185032],"about_ca_topic_score_codex":0.5589581,"about_ca_topic_score_gemma":0.9783178,"teacher_disagreement_score":0.41935968,"about_ca_system_score_codex":0.00000625512,"about_ca_system_score_gemma":0.002102659,"threshold_uncertainty_score":0.99598956},"labels":[],"label_agreement":null},{"id":"W1985402649","doi":"10.1139/e00-110","title":"A paleoecological analysis of a southern permafrost peatland, Charlevoix, Quebec","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Peat; Macrofossil; Permafrost; Subarctic climate; Geology; Boreal; Bog; Physical geography; Deforestation (computer science); Tundra; Taiga; Holocene; Paleontology; Geography; Forestry; Arctic; Archaeology; Oceanography","score_opus":0.028585775314361257,"score_gpt":0.2436338067976612,"score_spread":0.21504803148329993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985402649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921445,0.0012240814,0.000014179898,0.0008909723,0.00016228965,0.000046123452,0.00012315734,0.000002346198,0.005392322],"genre_scores_gemma":[0.9990612,0.00005828651,0.00012884548,0.00015053911,0.00004941128,1.4460235e-7,0.00001772705,8.4064294e-7,0.00053297885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984932,0.00019385677,0.00035866015,0.00016608588,0.0002807787,0.00050742406],"domain_scores_gemma":[0.9986952,0.00028020886,0.00021265192,0.00010462237,0.00015585306,0.0005514895],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012943675,0.00009827211,0.0003673648,0.000986202,0.0003538955,0.0000585104,0.00053400866,0.000103313345,0.014984522],"category_scores_gemma":[0.0002107482,0.000066872795,0.00018209244,0.0015013935,0.0013065854,0.00016249377,0.0000047667445,0.00023263846,0.00013481961],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018479886,0.000005231728,0.99706984,0.0000022018116,0.000100172416,0.00025825785,0.00048341227,0.0016175313,0.0000033404035,0.000032423744,0.000024771027,0.00038436102],"study_design_scores_gemma":[0.00013652974,0.0002475217,0.9952346,0.00000844202,0.00009908065,0.0002454333,0.0010255818,0.001275051,0.000003930572,0.00010659426,0.00153867,0.00007857755],"about_ca_topic_score_codex":0.03914336,"about_ca_topic_score_gemma":0.9827059,"teacher_disagreement_score":0.94356257,"about_ca_system_score_codex":4.7682875e-7,"about_ca_system_score_gemma":0.0011297681,"threshold_uncertainty_score":0.9859159},"labels":[],"label_agreement":null},{"id":"W1985540719","doi":"10.1139/e02-015","title":"U–Pb geochronologic constraints on the crustal evolution of the Long Range Inlier, Newfoundland","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":101,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; University of Alberta","funders":"","keywords":"Geology; Gneiss; Proterozoic; Geochemistry; Metamorphic rock; Metamorphism; Charnockite; Precambrian; Basement; Terrane; Pluton; Igneous rock; Granulite; Geomorphology; Paleontology; Structural basin; Tectonics; Facies; Archaeology","score_opus":0.024869174678563723,"score_gpt":0.18471864850365602,"score_spread":0.1598494738250923,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985540719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9805054,0.001535562,0.000017306405,0.0039599137,0.0002341858,0.00005311546,0.000020303116,0.0000017155896,0.013672512],"genre_scores_gemma":[0.9993698,0.00002379415,0.000055256827,0.00036623585,0.000072196235,9.460059e-8,4.1287353e-7,4.9081996e-7,0.000111715715],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989137,0.000106622174,0.00024414842,0.00011687925,0.00031435245,0.0003042648],"domain_scores_gemma":[0.9991544,0.00021454666,0.00020602321,0.00010509791,0.00008417711,0.00023575276],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005634971,0.00008454851,0.0001490716,0.00011020305,0.0004499361,0.000063902444,0.0005837816,0.0000458707,0.021166958],"category_scores_gemma":[0.00037560894,0.000035923775,0.00013311737,0.00059609144,0.002004061,0.000120393466,0.0000066301013,0.0002097933,0.000064638276],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002779122,0.0000053330978,0.99394625,0.0000015558824,0.000011064993,0.000013427362,0.000081055885,0.0020169113,0.000018960633,0.00039274414,0.00016950857,0.0033403754],"study_design_scores_gemma":[0.00009656998,0.00020298912,0.99328065,0.000024896166,0.00001552921,0.00006873153,0.00029793778,0.0016743519,0.00005985003,0.0037513354,0.00046440816,0.00006277061],"about_ca_topic_score_codex":0.021165978,"about_ca_topic_score_gemma":0.46130088,"teacher_disagreement_score":0.44013488,"about_ca_system_score_codex":0.000003630194,"about_ca_system_score_gemma":0.00023260571,"threshold_uncertainty_score":0.98535216},"labels":[],"label_agreement":null},{"id":"W1985662140","doi":"10.1139/e05-119","title":"Small shelly fossils from the basal Emigrant Formation (Cambrian, uppermost Dyeran Stage) of Split Mountain, Nevada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Fauna; Trilobite; Paleontology; Geology; Genus; Stage (stratigraphy); Structural basin; Taxon; Assemblage (archaeology); Ecology; Biology; Ordovician","score_opus":0.024878986527373703,"score_gpt":0.20449461696453577,"score_spread":0.17961563043716208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985662140","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97369075,0.0074112606,0.0001571071,0.0010478683,0.0004516575,0.00010504909,0.0002987115,0.000003485454,0.016834136],"genre_scores_gemma":[0.9981668,0.000031657364,0.0013306206,0.00018671724,0.00018049969,1.8788116e-7,0.000007296597,8.132872e-7,0.000095424126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983274,0.00014821062,0.00056234037,0.0001597433,0.00035173868,0.00045056638],"domain_scores_gemma":[0.99868,0.0002979062,0.00042526197,0.00014233634,0.00013486542,0.00031960887],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011181106,0.00014190137,0.00024329034,0.00020561829,0.0006660002,0.00019478046,0.00067912054,0.000081668535,0.00057008717],"category_scores_gemma":[0.00007728282,0.00009093109,0.0001373648,0.00042978727,0.0009062539,0.000642902,0.0000011447125,0.00022269558,0.000007556161],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020545933,0.0000039949796,0.98617077,0.0000053363306,0.000013459643,0.00004417901,0.0003374231,0.0005764018,0.00010185074,0.00055759976,0.00029915303,0.011869282],"study_design_scores_gemma":[0.00022999724,0.00021142862,0.9936615,0.00004754261,0.00001619904,0.00004897912,0.00092781807,0.0012264577,0.00028853124,0.0013568059,0.0018691743,0.00011552694],"about_ca_topic_score_codex":0.23926364,"about_ca_topic_score_gemma":0.9391931,"teacher_disagreement_score":0.6999295,"about_ca_system_score_codex":0.0000020611985,"about_ca_system_score_gemma":0.0011385013,"threshold_uncertainty_score":0.76580215},"labels":[],"label_agreement":null},{"id":"W1985668786","doi":"10.1139/e06-134","title":"The Lower Cretaceous Chaswood Formation in southern New Brunswick: provenance and tectonics","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Northwestern University","keywords":"Geology; Provenance; Paleocurrent; Zircon; Conglomerate; Geochemistry; Cretaceous; Geochronology; Monazite; Clastic rock; Heavy mineral; Felsic; Outcrop; Syncline; Paleontology; Mafic; Tectonics; Sedimentary rock","score_opus":0.01120618281711138,"score_gpt":0.18762756646991785,"score_spread":0.17642138365280646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985668786","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9903903,0.0044436166,0.000090094974,0.0020055135,0.0001163833,0.000040650673,0.0000021044712,0.0000016440177,0.0029097185],"genre_scores_gemma":[0.99903,0.000066463515,0.00043655373,0.00018876299,0.00005998043,1.7784055e-8,4.5484327e-7,5.107682e-7,0.00021728796],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910283,0.000021324538,0.00024952498,0.00009078334,0.00018435536,0.00035118216],"domain_scores_gemma":[0.9992478,0.00013043615,0.00012862087,0.000048487476,0.000045904166,0.00039877562],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010288206,0.000063838306,0.00010248043,0.00011548018,0.00029326804,0.00012491095,0.00024422235,0.000033498345,0.00035579214],"category_scores_gemma":[0.00018776384,0.00003392546,0.000040207025,0.0004446324,0.00032473815,0.00021414262,0.0000034232294,0.0001461086,0.000019249428],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022520753,0.0000045884676,0.9176182,0.000002951357,0.0000064355286,0.000103400824,0.0007553632,0.0013806731,0.0000446671,0.00023730329,0.000044502947,0.079779394],"study_design_scores_gemma":[0.00029507323,0.00057222834,0.95950216,0.000046387635,0.000012404596,0.00031094768,0.0021809898,0.005551443,0.0002876909,0.016709635,0.014346305,0.00018475555],"about_ca_topic_score_codex":0.042661235,"about_ca_topic_score_gemma":0.94974226,"teacher_disagreement_score":0.907081,"about_ca_system_score_codex":0.0000012928499,"about_ca_system_score_gemma":0.0005362915,"threshold_uncertainty_score":0.96371377},"labels":[],"label_agreement":null},{"id":"W1986086997","doi":"10.1139/e05-027","title":"Contrasting seismic characteristics of three major faults in northwestern Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Terrane; Seismology; Crust; Strike-slip tectonics; Fault (geology); Shear zone; Tectonics; Geophysics","score_opus":0.01334034053072247,"score_gpt":0.17857309609187624,"score_spread":0.16523275556115377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986086997","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971292,0.0004293392,0.000017534121,0.0011522098,0.00013413363,0.000029113931,0.00006128562,9.872537e-7,0.0010461973],"genre_scores_gemma":[0.9991105,0.0000068243025,0.00036661295,0.00038993164,0.000095155025,5.0516938e-8,0.000004068262,6.859153e-7,0.000026161335],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987678,0.000028273786,0.00045300781,0.000118616976,0.0002713857,0.00036092428],"domain_scores_gemma":[0.999032,0.00013033561,0.0002505263,0.00005428195,0.00010094019,0.00043192002],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042540347,0.00008632678,0.00025104528,0.00016821783,0.0001089755,0.000028498303,0.00034981276,0.00003172311,0.0017060969],"category_scores_gemma":[0.00014782947,0.00006047314,0.000053661333,0.00043580757,0.0002489489,0.0001722292,0.0000037324717,0.00015171019,0.000007674954],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000039540687,0.0000024455073,0.9843873,0.0000031459003,0.0000058221462,0.00005470103,0.000042428677,0.0041723787,0.000016572676,0.000005897718,0.000010972485,0.011294373],"study_design_scores_gemma":[0.00012471163,0.000074864496,0.9890387,0.000031596523,0.000009293428,0.000037378602,0.00010063604,0.009084832,0.000092073074,0.00028606938,0.0010397593,0.00008010483],"about_ca_topic_score_codex":0.93141943,"about_ca_topic_score_gemma":0.9998179,"teacher_disagreement_score":0.06839847,"about_ca_system_score_codex":0.0000032939188,"about_ca_system_score_gemma":0.0015170643,"threshold_uncertainty_score":0.9992065},"labels":[],"label_agreement":null},{"id":"W1986092739","doi":"10.1139/e04-036","title":"Arenigian (Early Ordovician) sea-level history and the response of conodont communities, western Newfoundland","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research","keywords":"Conodont; Marine transgression; Geology; Ordovician; Paleontology; Trilobite; Facies; Sea level; Macrofossil; Biostratigraphy; Oceanography; Structural basin; Holocene","score_opus":0.04355715662628615,"score_gpt":0.2171982994333197,"score_spread":0.17364114280703355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986092739","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97895664,0.013195013,0.000027037551,0.0012037054,0.00036443924,0.000062029605,0.000050809012,0.0000019690233,0.0061383513],"genre_scores_gemma":[0.99928343,0.00006615153,0.00032726742,0.00023707554,0.00003489264,1.1748022e-7,6.10782e-7,5.889929e-7,0.00004987928],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885327,0.00028657741,0.00030406387,0.000080441074,0.00020082334,0.00027482014],"domain_scores_gemma":[0.9987684,0.00042042462,0.00025019067,0.00011647994,0.00008403387,0.0003604639],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0018412342,0.00009642572,0.00023638541,0.00026769363,0.00045273956,0.00007530822,0.00047993404,0.000055409717,0.00013041338],"category_scores_gemma":[0.0000979167,0.00006172704,0.000069833644,0.0001623722,0.0037840279,0.00035635338,0.0000013797832,0.00022150358,0.0000024476165],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017825248,0.0000022094305,0.9928351,0.000003042274,0.000017022565,0.000033815842,0.0043479055,0.00011089038,0.000004672625,0.00035086676,0.000012579774,0.0021036572],"study_design_scores_gemma":[0.00075651583,0.00042866447,0.99513793,0.00005120719,0.000014054518,0.00021467282,0.0011223528,0.000021989847,0.000007427546,0.0008952505,0.0012714938,0.000078456505],"about_ca_topic_score_codex":0.28044456,"about_ca_topic_score_gemma":0.97822535,"teacher_disagreement_score":0.6977808,"about_ca_system_score_codex":0.0000045231163,"about_ca_system_score_gemma":0.002502786,"threshold_uncertainty_score":0.9989271},"labels":[],"label_agreement":null},{"id":"W1986133221","doi":"10.1139/e06-028","title":"Paleocene–Eocene high-grade metamorphism, anatexis, and deformation in the Thor–Odin dome, Monashee complex, southeastern British Columbia","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick; Geological Survey of Canada; Natural Resources Canada; Carleton University","funders":"University of Ottawa","keywords":"Anatexis; Geology; Metamorphism; Zircon; Geochemistry; Gneiss; Metamorphic rock; Pegmatite; Partial melting; Dalradian; Basement; Migmatite; Crust","score_opus":0.01760770579289412,"score_gpt":0.18450739135633112,"score_spread":0.166899685563437,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986133221","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99483633,0.0016057844,0.000009552161,0.0015947574,0.00008208709,0.000063609055,0.00006375552,0.0000029035327,0.0017412022],"genre_scores_gemma":[0.99879616,0.000044981858,0.0005182496,0.0004709739,0.00008582286,2.7163853e-7,0.00001982925,9.226633e-7,0.00006276843],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99857855,0.00012608242,0.0003829646,0.0001636232,0.00035060747,0.00039814512],"domain_scores_gemma":[0.9993131,0.00011054372,0.00017297272,0.00006865473,0.00006268622,0.0002720426],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010219873,0.00008779837,0.00022454788,0.00014419739,0.00041708068,0.0006539946,0.00041403496,0.000047699545,0.00223943],"category_scores_gemma":[0.00005703889,0.00006788133,0.00007078235,0.00071637507,0.0005627826,0.00034623113,0.000005547322,0.00017254658,0.000014917447],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000015782985,0.000006084079,0.9954421,0.0000030753786,0.0000044709477,0.00007063847,0.00005774257,0.0012768052,0.000010380699,0.000036989226,0.00022542602,0.0028647154],"study_design_scores_gemma":[0.00016634692,0.00009541632,0.97733444,0.000017061167,0.000015947688,0.00018638094,0.00033780784,0.0016686021,0.0000065750246,0.019049207,0.0010208499,0.00010134328],"about_ca_topic_score_codex":0.6435291,"about_ca_topic_score_gemma":0.9903502,"teacher_disagreement_score":0.34682104,"about_ca_system_score_codex":0.0000011550727,"about_ca_system_score_gemma":0.00014077396,"threshold_uncertainty_score":0.99867266},"labels":[],"label_agreement":null},{"id":"W1986410609","doi":"10.1139/e08-008","title":"Olenid-dominated trilobite fauna from the Shallow Bay Formation (Cow Head Group), Cambrian–Ordovician boundary interval, western Newfoundland","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Trilobite; Ordovician; Geology; Paleontology; Fauna; Laurentia; Bay; Group (periodic table); Benthic zone; Gondwana; Ecology; Oceanography; Biology; Tectonics","score_opus":0.03158027486391337,"score_gpt":0.23108425604335114,"score_spread":0.19950398117943777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986410609","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97903335,0.009453834,0.00015702957,0.001643176,0.0009784112,0.000118362026,0.0001089747,0.000008264704,0.008498622],"genre_scores_gemma":[0.99856,0.00013623193,0.0003637968,0.00061575155,0.00025242445,3.3774347e-7,0.000011949609,0.0000013099592,0.000058206795],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981368,0.00023298053,0.0005049387,0.00021107073,0.00037489945,0.00053929136],"domain_scores_gemma":[0.9985305,0.00028082592,0.00034258963,0.00015678976,0.0000976193,0.0005916743],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0009089661,0.00018100243,0.0002954971,0.00028248856,0.0016652724,0.00033634627,0.0007977951,0.000102301834,0.00038329282],"category_scores_gemma":[0.00010320078,0.00011854283,0.0001621588,0.00049781636,0.0013686498,0.0014172574,0.0000020802095,0.00035163236,0.000034364966],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031314685,0.000004310703,0.9879039,0.0000022693782,0.000022423974,0.00017300107,0.0011286412,0.00004509483,0.000012943252,0.000021046857,0.000040507097,0.010614537],"study_design_scores_gemma":[0.00042633366,0.00042839424,0.99033254,0.00007467955,0.000019047733,0.00061988796,0.00046072947,0.0006474837,0.0000028553648,0.00027738867,0.0065549784,0.00015567573],"about_ca_topic_score_codex":0.090546034,"about_ca_topic_score_gemma":0.99687076,"teacher_disagreement_score":0.90632474,"about_ca_system_score_codex":0.0000035891699,"about_ca_system_score_gemma":0.001041404,"threshold_uncertainty_score":0.99963444},"labels":[],"label_agreement":null},{"id":"W1986576603","doi":"10.1139/cjes-2014-0205","title":"Climat hivernal, aménagement du territoire et dynamique des avalanches au Québec méridional : une analyse à partir des accidents connus depuis 1825","year":2015,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université de Moncton; Université du Québec à Rimouski","funders":"","keywords":"Geology","score_opus":0.02688836241445514,"score_gpt":0.24695151944182386,"score_spread":0.22006315702736873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986576603","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9740544,0.007893643,0.0002543945,0.011164077,0.0016110301,0.000120287674,0.00005363502,0.000007272466,0.004841255],"genre_scores_gemma":[0.99445355,0.0010811666,0.0018758847,0.00043509484,0.00027436088,0.0000019085317,0.0000031368015,0.000015541511,0.0018593409],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9967341,0.00030476545,0.0007052823,0.00037202236,0.0008407299,0.0010431241],"domain_scores_gemma":[0.9966305,0.00010902697,0.0004955295,0.000192006,0.00014951933,0.00242343],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0023862235,0.0003052147,0.0004041094,0.00028828732,0.0012294521,0.0005241715,0.0009307731,0.00015006115,0.001414206],"category_scores_gemma":[0.00033343543,0.0002333834,0.00023723429,0.0008562277,0.0047915634,0.0015066473,0.00011728898,0.00041019105,0.00023527963],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023006529,0.000053673702,0.9593015,0.000021058253,0.000098623896,0.0008391005,0.0063876035,0.02014071,0.000063861145,0.00015684802,0.0024910339,0.010422996],"study_design_scores_gemma":[0.000736571,0.00073033845,0.9450875,0.000585617,0.00016794915,0.0012191145,0.0048592067,0.0039732084,0.00020646698,0.0020251044,0.040009473,0.0003994427],"about_ca_topic_score_codex":0.7262379,"about_ca_topic_score_gemma":0.9877234,"teacher_disagreement_score":0.26148552,"about_ca_system_score_codex":0.0007941117,"about_ca_system_score_gemma":0.0061963303,"threshold_uncertainty_score":0.99949867},"labels":[],"label_agreement":null},{"id":"W1986633771","doi":"10.1139/e02-083","title":"Allometric growth in tyrannosaurids (Dinosauria: Theropoda) from the Upper Cretaceous of North America and Asia","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":158,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University; North Carolina State University","keywords":"Allometry; Theropoda; Biology; Cretaceous; Skull; Paleontology; Zoology; Geology","score_opus":0.013598868802336067,"score_gpt":0.19740417214784078,"score_spread":0.1838053033455047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986633771","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9789501,0.015905995,0.000013408601,0.0009664191,0.00033620404,0.000047873502,0.000055172462,0.0000012064824,0.0037236582],"genre_scores_gemma":[0.9987471,0.00036322765,0.0005451126,0.0002774344,0.000045505585,1.0937579e-7,0.0000031589748,8.600386e-7,0.000017463633],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988684,0.00023996943,0.00027294256,0.00014307712,0.0001575148,0.00031810915],"domain_scores_gemma":[0.9990392,0.00042136366,0.00016944297,0.00006973031,0.000062091676,0.00023821664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049921294,0.00008913293,0.00020337186,0.0003422544,0.00024170015,0.000024832529,0.00035115978,0.000053909967,0.000697561],"category_scores_gemma":[0.00041800865,0.00005430432,0.000044561926,0.0009184037,0.0012670154,0.00020320308,0.0000026892305,0.0001971258,0.000011379103],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007890512,0.0000029888502,0.9971854,0.0000010153954,0.000011148695,0.000035367757,0.0001971942,0.00021663118,0.000003235667,0.00009167164,0.00008208837,0.0021653844],"study_design_scores_gemma":[0.00013550607,0.0002536726,0.9932802,0.000010051358,0.000008636024,0.000116796065,0.00033964668,0.00011092489,0.000009468631,0.000882117,0.0047857068,0.00006729856],"about_ca_topic_score_codex":0.017457437,"about_ca_topic_score_gemma":0.56121397,"teacher_disagreement_score":0.5437565,"about_ca_system_score_codex":0.0000013697831,"about_ca_system_score_gemma":0.0007303547,"threshold_uncertainty_score":0.9890854},"labels":[],"label_agreement":null},{"id":"W1986813925","doi":"10.1139/e02-005","title":"Geophysical characteristics of the continental crust along the Lithoprobe Eastern Canadian Shield Onshore–Offshore Transect (ECSOOT): a review","year":2002,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University; Memorial University of Newfoundland","funders":"","keywords":"Geology; Archean; Crust; Proterozoic; Continental crust; Accretion (finance); Metamorphic core complex; Craton; Seismology; Geochemistry; Tectonics; Extensional definition","score_opus":0.038433826793099125,"score_gpt":0.2289888925610046,"score_spread":0.19055506576790548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986813925","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00731096,0.98570055,6.8039446e-7,0.0025653786,0.0004921297,0.0003501127,0.0004556282,0.0000023913444,0.0031221588],"genre_scores_gemma":[0.14989117,0.848601,0.000030762065,0.0009168565,0.00032704615,0.0000015045346,0.00002640138,0.000004921879,0.00020035669],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.996793,0.0003756828,0.0011434394,0.00032852514,0.0006101931,0.00074918685],"domain_scores_gemma":[0.9972149,0.0003586736,0.00082921545,0.00031510353,0.0001599748,0.0011221026],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011492698,0.0003672865,0.0014709929,0.00024716477,0.00056650135,0.00016204097,0.0020465497,0.00017242397,0.0066462234],"category_scores_gemma":[0.00042889424,0.00016208817,0.0011247554,0.0014641553,0.0014700008,0.00014134988,0.000015704902,0.00088625005,0.00007887291],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000031543552,0.000018914976,0.21612765,0.0027294096,0.00020561644,0.00022773346,0.00016736815,0.000012310701,1.1977221e-7,0.00011366782,0.0011734758,0.7792206],"study_design_scores_gemma":[0.00006797717,0.00021648317,0.07897101,0.0133893285,0.0009623426,0.0005222325,0.00007045595,0.00011175032,5.8779386e-7,0.0001297448,0.9051763,0.0003818125],"about_ca_topic_score_codex":0.36714268,"about_ca_topic_score_gemma":0.9522721,"teacher_disagreement_score":0.9040028,"about_ca_system_score_codex":0.0000066703155,"about_ca_system_score_gemma":0.0028145136,"threshold_uncertainty_score":0.99426186},"labels":[],"label_agreement":null},{"id":"W1987125639","doi":"10.1139/e00-012","title":"Neoproterozoic slope deposits, Mackenzie Mountains, northwestern Canada: implications for passive-margin development and Ediacaran faunal ecology","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"","keywords":"Geology; Facies; Paleontology; Siliciclastic; Unconformity; Marine transgression; Sedimentary rock; Sedimentary depositional environment; Structural basin","score_opus":0.016365262497462407,"score_gpt":0.20717982302965948,"score_spread":0.1908145605321971,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987125639","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99545586,0.000887896,0.00007273632,0.0021976547,0.0001787225,0.00014726061,0.0001200889,0.0000027468357,0.0009370049],"genre_scores_gemma":[0.9966434,0.00005545629,0.0024144668,0.0006782906,0.00007006917,0.0000023260802,0.000027580425,0.000001327928,0.00010705893],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898076,0.000026175298,0.0003223899,0.00014336342,0.00012983907,0.00039747762],"domain_scores_gemma":[0.99904907,0.00011528438,0.00012550729,0.00005136594,0.00012472371,0.00053402525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026130647,0.00010228994,0.00015559973,0.00013097328,0.0009178856,0.00014760818,0.00029660945,0.000044694076,0.0008888332],"category_scores_gemma":[0.000037561924,0.00007536423,0.000026847554,0.00024542297,0.00021609508,0.00031414427,0.0000027599306,0.00009440296,0.000007854783],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005940969,0.0000021808578,0.8977306,0.000008903091,0.000008959074,0.000008697314,0.00015017143,0.0016312099,7.9111675e-7,0.000086142245,0.00017670216,0.10018974],"study_design_scores_gemma":[0.00012942292,0.00016161651,0.9406562,0.000012356948,0.000007570434,0.0001649598,0.00015042849,0.00017524727,0.00003089458,0.00040638613,0.05800074,0.000104214036],"about_ca_topic_score_codex":0.35743973,"about_ca_topic_score_gemma":0.99805015,"teacher_disagreement_score":0.6406104,"about_ca_system_score_codex":0.0000055982455,"about_ca_system_score_gemma":0.0034689212,"threshold_uncertainty_score":0.97321004},"labels":[],"label_agreement":null},{"id":"W1987175354","doi":"10.1139/e00-017","title":"The thermal regime of a retrogressive thaw slump near Mayo, Yukon Territory","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Slump; Slumping; Geology; Permafrost; Transect; Hydrology (agriculture); Geotechnical engineering; Geomorphology; Oceanography","score_opus":0.025798772677988614,"score_gpt":0.221477821379781,"score_spread":0.1956790487017924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987175354","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9668813,0.004544474,1.8583843e-7,0.0013169476,0.000569564,0.000056596622,0.00024790148,0.0000022782158,0.02638079],"genre_scores_gemma":[0.9984824,0.0002698279,0.0000769297,0.00026030172,0.00031098715,1.2812185e-7,0.000008594428,0.0000023129028,0.0005885118],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99868333,0.00009199243,0.00030549502,0.00012294763,0.00035387912,0.0004423818],"domain_scores_gemma":[0.9989735,0.00016290873,0.0002097183,0.00013554923,0.00007865805,0.0004396523],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008426916,0.00010123478,0.00016511437,0.00010627357,0.0007933195,0.00024286906,0.00061520335,0.000049765855,0.0153482165],"category_scores_gemma":[0.000043229382,0.000060191524,0.000099619974,0.0002988313,0.0013611862,0.00035696372,0.0000031030313,0.0001772671,0.000080571444],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002758432,0.0000030251522,0.96912974,0.0000046223563,0.000012925441,0.00010837522,0.0011849147,0.0006128574,0.000043187025,0.000027111491,0.0016534894,0.027192183],"study_design_scores_gemma":[0.00015318234,0.000439561,0.9275974,0.000077160126,0.000011757425,0.00018684639,0.0009545605,0.00074323086,0.00011016154,0.00016179697,0.06944957,0.00011476487],"about_ca_topic_score_codex":0.03935138,"about_ca_topic_score_gemma":0.5772571,"teacher_disagreement_score":0.5379057,"about_ca_system_score_codex":0.0000014181354,"about_ca_system_score_gemma":0.00092223374,"threshold_uncertainty_score":0.9855519},"labels":[],"label_agreement":null},{"id":"W1987206455","doi":"10.1139/e10-103","title":"A fission track transect across Nares Strait (Canada–Greenland): further evidence that the Wegener Fault is a myth","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Paleontology; Paleozoic; Precambrian; Fission track dating; Sedimentary rock; North American Plate; Sedimentary basin; Plate tectonics; Seismology; Tectonics","score_opus":0.10759579039649986,"score_gpt":0.23836972712484822,"score_spread":0.13077393672834836,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987206455","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98593545,0.004803686,0.00007040127,0.007110937,0.0005072259,0.00009406084,0.00007848766,0.0000032083256,0.001396528],"genre_scores_gemma":[0.99771255,0.00024049904,0.00021792541,0.0015837776,0.00010871468,3.4747995e-7,0.0000011551119,0.0000015304734,0.00013351673],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984883,0.00009544949,0.00025646156,0.00018283576,0.00046598192,0.00051094603],"domain_scores_gemma":[0.999001,0.0001337933,0.00021136865,0.000098016346,0.00009706711,0.000458701],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00089235336,0.00012899903,0.00016973983,0.000051937717,0.0009357653,0.00014586558,0.00057649775,0.000048483256,0.0048433263],"category_scores_gemma":[0.00011624153,0.00006481376,0.000085780885,0.0003424025,0.00049985,0.00046695067,0.000004707708,0.00018126014,0.000022353419],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035834855,0.000004189719,0.9490616,0.000006094402,0.000022679282,0.00010275046,0.009758647,0.0010044698,0.000010008632,0.000014019844,0.0039189807,0.03606076],"study_design_scores_gemma":[0.00009488762,0.00036156323,0.9746205,0.000061165876,0.0000108167205,0.00007256811,0.006315014,0.00039112166,0.00015329372,0.00043919403,0.017350055,0.00012981705],"about_ca_topic_score_codex":0.7532172,"about_ca_topic_score_gemma":0.9961164,"teacher_disagreement_score":0.24289922,"about_ca_system_score_codex":0.0000028686347,"about_ca_system_score_gemma":0.0009379913,"threshold_uncertainty_score":0.9960664},"labels":[],"label_agreement":null},{"id":"W1987223720","doi":"10.1139/e01-057","title":"A new bird from the Upper Cretaceous Two Medicine Formation of Montana","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Cretaceous; Paleontology; Humerus; Geology; Extant taxon; Waterfowl; Biology; Ecology; Evolutionary biology; Habitat","score_opus":0.02911312512993609,"score_gpt":0.21508418682860092,"score_spread":0.18597106169866484,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987223720","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9440495,0.030669315,0.00028197857,0.011765125,0.0009710788,0.000059752685,0.000030832547,0.0000044494636,0.0121679725],"genre_scores_gemma":[0.9982435,0.00017535526,0.00073762465,0.00048400392,0.00024847724,3.531362e-8,0.0000018415394,6.7925225e-7,0.000108459564],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991548,0.00009241192,0.0002755896,0.000080395264,0.00016738469,0.0002293974],"domain_scores_gemma":[0.99912995,0.00023626449,0.0002045254,0.00007499136,0.000056392364,0.00029785416],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004698214,0.000064587264,0.00014796157,0.0001390286,0.00028768508,0.000014941858,0.00039441447,0.0000411254,0.006776294],"category_scores_gemma":[0.00015293647,0.000035433466,0.000043709068,0.00028140418,0.0007047714,0.0003309279,0.0000017493617,0.000121040095,0.000068783054],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000065739273,9.4173356e-7,0.98128784,7.310565e-7,0.000008601065,0.000021600601,0.00084987096,0.0006270385,0.000014738196,0.00010854138,0.003925513,0.0131480275],"study_design_scores_gemma":[0.0002280506,0.00033323868,0.9751366,0.000030468986,0.000015436142,0.00028191204,0.00051774003,0.0047701197,0.00001290278,0.0021572087,0.01646172,0.000054592863],"about_ca_topic_score_codex":0.1012306,"about_ca_topic_score_gemma":0.85223097,"teacher_disagreement_score":0.75100034,"about_ca_system_score_codex":0.0000012054409,"about_ca_system_score_gemma":0.00029934183,"threshold_uncertainty_score":0.9941316},"labels":[],"label_agreement":null},{"id":"W1987334436","doi":"10.1139/e05-006","title":"A database of physical properties of rocks from the Trans-Hudson Orogen, Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"The Arctic Eider Society; University of Saskatchewan; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; National Research Council Canada; Rheinische Friedrich-Wilhelms-Universität Bonn; University of Saskatchewan","keywords":"Electrical resistivity and conductivity; Geology; Mineralogy; Archean; Porosity; Saturation (graph theory); Crust; Graphite; Geophysics; Geochemistry; Geotechnical engineering; Metallurgy; Materials science","score_opus":0.027889352212748107,"score_gpt":0.21281527387853044,"score_spread":0.18492592166578234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987334436","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950078,0.0022511426,0.000052062223,0.0018616888,0.00013703793,0.00005510819,0.00015065754,9.763139e-7,0.0004835074],"genre_scores_gemma":[0.99866676,0.0000136132,0.0008191977,0.00023490736,0.00023342061,1.0329023e-7,0.0000017434419,0.0000011340433,0.000029128285],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9987234,0.00012259572,0.0002958717,0.000117464624,0.00044297244,0.00029770168],"domain_scores_gemma":[0.9989394,0.00027744728,0.0001844801,0.00010524238,0.00011515386,0.00037828734],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041873107,0.000090916816,0.00023980367,0.0000627688,0.00017709269,0.000028740731,0.00056101993,0.000020904148,0.00040532395],"category_scores_gemma":[0.00020213134,0.000047849582,0.00008498217,0.0004911638,0.0004370708,0.00022651428,0.000003446835,0.00016646032,0.000003094553],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012602883,0.00008997422,0.45031917,0.00006137505,0.0001461479,0.000055980832,0.004299087,0.038984273,0.009824853,0.0003399604,0.0017503187,0.49400282],"study_design_scores_gemma":[0.00054600637,0.0013226507,0.8477914,0.00030547613,0.000104074075,0.000045203426,0.0014409864,0.018406423,0.09595018,0.001135336,0.032571077,0.0003812403],"about_ca_topic_score_codex":0.91118246,"about_ca_topic_score_gemma":0.99233,"teacher_disagreement_score":0.4936216,"about_ca_system_score_codex":0.0000018824234,"about_ca_system_score_gemma":0.0028764866,"threshold_uncertainty_score":0.5102764},"labels":[],"label_agreement":null},{"id":"W1987382998","doi":"10.1139/e03-092","title":"A new species of the ptilodontid multituberculate <i>Prochetodon</i> (Mammalia, Allotheria) from the Paleocene Paskapoo Formation of Alberta, Canada","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Genus; Paleontology; Geology; Taxon; Range (aeronautics); Paleogene; Cretaceous; Zoology; Biology","score_opus":0.018471464898406002,"score_gpt":0.18801818419762384,"score_spread":0.16954671929921783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987382998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98499554,0.0026281665,0.000072243936,0.005719657,0.00081422034,0.000095244875,0.000052744876,0.0000011234342,0.005621037],"genre_scores_gemma":[0.998496,0.00006479482,0.00049817224,0.00050934206,0.000095888754,9.2209845e-8,0.0000017409279,0.00000120543,0.00033276633],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988139,0.000076372155,0.00039391537,0.00009793644,0.000357362,0.0002604592],"domain_scores_gemma":[0.9989218,0.00020433239,0.0004096286,0.00012976238,0.00011850443,0.00021597548],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036985872,0.000101048776,0.00020726302,0.00005771531,0.0003682629,0.000032901447,0.0005796639,0.00003775259,0.00046173783],"category_scores_gemma":[0.00018497692,0.000054519725,0.00009150303,0.0003483091,0.00061125524,0.00024510775,0.000005860627,0.00012274444,0.0000039299193],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007901132,0.0000018529802,0.98951644,0.000003979831,0.00002525927,0.0000041266767,0.0022231396,0.0064242105,0.000059442104,0.0001148577,0.001023417,0.0005954055],"study_design_scores_gemma":[0.00025587645,0.00006547556,0.9866721,0.00007261072,0.000022127822,0.000025913874,0.0014866298,0.00009825138,0.00077976723,0.00032969294,0.010121478,0.000070100505],"about_ca_topic_score_codex":0.9748202,"about_ca_topic_score_gemma":0.9999367,"teacher_disagreement_score":0.025116507,"about_ca_system_score_codex":0.0000052129776,"about_ca_system_score_gemma":0.0032636104,"threshold_uncertainty_score":0.57895046},"labels":[],"label_agreement":null},{"id":"W1987764331","doi":"10.1139/e05-105","title":"Ovummuridae (calcareous microfossils) from a Late Devonian ramp: their distribution, preservation potential, and paleoecological significance","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Siliciclastic; Devonian; Paleozoic; Geology; Paleontology; Carbonate; Crinoid; Carboniferous; Permian; Ordovician; Calcareous; Carbonate rock; Rugosa; Sedimentary rock; Sedimentary depositional environment","score_opus":0.01424175049185911,"score_gpt":0.1967392778421103,"score_spread":0.18249752735025118,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987764331","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9824293,0.013207058,0.00032144005,0.00071989564,0.00034168037,0.00008525343,0.00033727827,0.000006918439,0.0025511484],"genre_scores_gemma":[0.9989822,0.00007572734,0.0006701959,0.00006995375,0.00015466733,3.2565706e-7,0.000020254834,5.869657e-7,0.000026110783],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986758,0.00013142447,0.00035193856,0.00022337858,0.00018956173,0.00042784668],"domain_scores_gemma":[0.9990104,0.00015981778,0.00023466493,0.00008363709,0.00010936838,0.00040211028],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055660424,0.00013399868,0.00021323987,0.00012327013,0.00075281394,0.0002629998,0.0003513681,0.00011105771,0.00032431333],"category_scores_gemma":[0.0000806366,0.00009690787,0.000076507364,0.0003004001,0.0010784379,0.000534478,0.0000013301834,0.00020063543,0.000004419164],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013613814,0.0000050153963,0.98836404,0.0000022608494,0.000011524941,0.000106652005,0.000097784905,0.00053840026,0.00018596505,0.00008364401,0.0001765691,0.010414519],"study_design_scores_gemma":[0.00017933903,0.00019716847,0.9916338,0.000020446709,0.000011355349,0.00007660297,0.00014201424,0.00083695934,0.00020362169,0.00484039,0.0017313239,0.00012700893],"about_ca_topic_score_codex":0.032602377,"about_ca_topic_score_gemma":0.4977452,"teacher_disagreement_score":0.46514282,"about_ca_system_score_codex":0.0000016865637,"about_ca_system_score_gemma":0.00066558557,"threshold_uncertainty_score":0.9738396},"labels":[],"label_agreement":null},{"id":"W1987778622","doi":"10.1139/e04-065","title":"Geology and UPb geochronology of the Neoarchean Snare River terrane: tracking evolving tectonic regimes and crustal growth mechanisms","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Government of Northwest Territories; Memorial University of Newfoundland","funders":"","keywords":"Geology; Zircon; Geochemistry; Terrane; Plutonism; Geochronology; Metamorphism; Granulite; Petrology; Mafic; Pluton; Tectonics; Facies; Geomorphology; Paleontology","score_opus":0.013525975925718246,"score_gpt":0.18898609938890734,"score_spread":0.1754601234631891,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987778622","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9907237,0.0036106866,0.000037215872,0.0043342197,0.00008167835,0.000039282968,0.000009017913,0.000002174795,0.0011619941],"genre_scores_gemma":[0.99763244,0.00006751668,0.0019019995,0.00029278657,0.00005531577,7.936238e-8,6.8235073e-7,9.033582e-7,0.000048276812],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989551,0.000084947416,0.0002557728,0.00017536046,0.0001685861,0.00036027574],"domain_scores_gemma":[0.9991926,0.0001403433,0.00018570245,0.00006838594,0.000097162774,0.0003158281],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004909796,0.0000987646,0.00022091686,0.00017506974,0.00036455016,0.000049764858,0.00033525447,0.00006805858,0.0021500173],"category_scores_gemma":[0.00024271169,0.000056833247,0.000070335234,0.00029867707,0.0018534155,0.00024783897,0.000018458828,0.00020466825,0.0000031787285],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000066259663,0.0000037596087,0.9829432,0.000009430141,0.00002145599,0.00002207864,0.00047448956,0.000543499,0.00045934366,0.0006244419,0.000030485031,0.014861186],"study_design_scores_gemma":[0.00015332806,0.00026267825,0.97358584,0.000027297134,0.000027006152,0.00040806492,0.00047784875,0.0027838626,0.00071113196,0.02113143,0.0003335812,0.00009792148],"about_ca_topic_score_codex":0.0185194,"about_ca_topic_score_gemma":0.26094294,"teacher_disagreement_score":0.24242353,"about_ca_system_score_codex":0.0000015673272,"about_ca_system_score_gemma":0.0002921591,"threshold_uncertainty_score":0.99876213},"labels":[],"label_agreement":null},{"id":"W1987923876","doi":"10.1139/e03-049","title":"Lower Paleozoic stratigraphic and biostratigraphic correlations in the Canadian Cordillera: implications for the tectonic evolution of the Laurentian margin","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Canadian Institute for Advanced Research; Geological Society of America","keywords":"Geology; Paleontology; Conodont; Ordovician; Devonian; Paleozoic; Unconformity; Facies; Biostratigraphy; Late Devonian extinction; Gondwana; Trough (economics); Tectonics; Structural basin; Carboniferous","score_opus":0.020952296517488384,"score_gpt":0.2216332212860286,"score_spread":0.20068092476854021,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987923876","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9591098,0.018975224,0.00007343564,0.007907815,0.00064803584,0.0005261406,0.00016114471,0.0000018174704,0.012596622],"genre_scores_gemma":[0.9996844,0.00005556935,0.00013749045,0.00009036148,0.000022257127,0.0000022012107,0.0000010006016,5.683193e-7,0.0000061834794],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988625,0.00018450677,0.00030711797,0.00013002369,0.00016514231,0.00035071568],"domain_scores_gemma":[0.99888456,0.0004180833,0.00020373901,0.00017033164,0.0000988847,0.00022440846],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0011145372,0.00009801022,0.0001251853,0.00038182636,0.0016886103,0.00012346845,0.0005445185,0.000074645664,0.000117736],"category_scores_gemma":[0.00019932067,0.00005003897,0.00010926108,0.0012049589,0.0014860233,0.00020536606,4.1103914e-7,0.00025877703,4.970937e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000020349185,0.0000034321506,0.98725414,0.0000025059876,0.000013315263,0.0000012959191,0.00024312778,0.00024401787,0.00000601385,0.01090538,0.00009307129,0.0012316762],"study_design_scores_gemma":[0.00013490477,0.00014080222,0.99260974,0.000025476662,0.000028069597,0.00009080889,0.0008500612,0.0002604537,0.000004063292,0.0050773104,0.0007139773,0.00006432219],"about_ca_topic_score_codex":0.14152603,"about_ca_topic_score_gemma":0.9986209,"teacher_disagreement_score":0.8570949,"about_ca_system_score_codex":0.000002374333,"about_ca_system_score_gemma":0.0030297348,"threshold_uncertainty_score":0.9996111},"labels":[],"label_agreement":null},{"id":"W1988166563","doi":"10.1139/e06-048","title":"Tectonic implications of <sup>40</sup>Ar/<sup>39</sup>Ar muscovite dates from the Mt. Haley stock and Lussier River stock, near Fort Steele, British Columbia","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University; Geological Survey of Canada","funders":"","keywords":"Geology; Muscovite; Thrust fault; Doming; Geochemistry; Pluton; Quartz monzonite; Pennsylvanian; Skarn; Metamorphic rock; Fault (geology); Seismology; Tectonics; Geomorphology; Paleontology; Hydrothermal circulation","score_opus":0.011319530108329447,"score_gpt":0.18350806960213786,"score_spread":0.1721885394938084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988166563","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99234295,0.0031873654,0.000024769699,0.0018293684,0.00005253921,0.00015982937,0.0006804275,0.000007308459,0.0017154554],"genre_scores_gemma":[0.9976079,0.000080742255,0.0011204258,0.0004441454,0.00015970603,0.0000012182712,0.000050688246,0.000003340527,0.0005318347],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99783844,0.00012278647,0.0005771457,0.00038898905,0.0004431084,0.0006295043],"domain_scores_gemma":[0.99820065,0.00039717488,0.00031407448,0.00023366575,0.00021663343,0.00063781714],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006808379,0.00016704928,0.00040074845,0.000107147804,0.001106008,0.00071818626,0.0008372205,0.00010315221,0.006460943],"category_scores_gemma":[0.00019799682,0.00013438839,0.00018839442,0.0009255638,0.0020438614,0.0004940034,0.000028214308,0.00031290503,0.000025915877],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005155192,0.000011265495,0.98050666,0.000004173632,0.000034831497,0.000023619366,0.00013962126,0.010554375,0.000018433866,0.000013516546,0.002334381,0.0063539706],"study_design_scores_gemma":[0.00021842532,0.00019512023,0.97043467,0.000048884158,0.00007340312,0.00010781539,0.0002657121,0.011076649,0.000012891513,0.0064001754,0.010977634,0.00018864869],"about_ca_topic_score_codex":0.66764057,"about_ca_topic_score_gemma":0.9236019,"teacher_disagreement_score":0.25596136,"about_ca_system_score_codex":0.0000046323375,"about_ca_system_score_gemma":0.0007117543,"threshold_uncertainty_score":0.9944473},"labels":[],"label_agreement":null},{"id":"W1988347136","doi":"10.1139/e07-023","title":"Petrology, age, and tectonic setting of the Seal Island Pluton, offshore southwestern Nova Scotia","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Mount Saint Vincent University; Acadia University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Pluton; Biotite; Geochemistry; Zircon; Terrane; Outcrop; Petrology; Tectonics; Paleontology; Quartz","score_opus":0.013709466518337893,"score_gpt":0.2046165475474438,"score_spread":0.1909070810291059,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988347136","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951227,0.0009295707,0.000014222758,0.0011207226,0.00019479179,0.000032106847,0.000019515819,0.0000014538277,0.0025649357],"genre_scores_gemma":[0.999329,0.000005967117,0.0002903677,0.00025826896,0.000074841504,9.954855e-9,0.0000011476469,7.3158816e-7,0.0000397191],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998873,0.000047257086,0.00031218055,0.00013831769,0.00024053808,0.0003887371],"domain_scores_gemma":[0.9991041,0.00015378642,0.00021520589,0.0000752966,0.00007852886,0.00037311425],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011948881,0.0000875578,0.00019689088,0.00016894816,0.00021887646,0.0000581047,0.00039751336,0.000052105457,0.0014696806],"category_scores_gemma":[0.00017224198,0.000046823992,0.00009047521,0.00056851876,0.0010031579,0.00011530996,0.000011449515,0.00020544346,0.000009024495],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000044109956,0.0000016288644,0.9979763,0.0000035375351,0.000010015787,0.00003559453,0.00016555924,0.0005360982,0.000081431346,0.000022864386,0.00001680026,0.0011457585],"study_design_scores_gemma":[0.00009718879,0.0001413218,0.99743944,0.000021039668,0.00002034804,0.00014176226,0.00032088076,0.00024557352,0.00015577539,0.0009881658,0.0003647536,0.00006373286],"about_ca_topic_score_codex":0.037777305,"about_ca_topic_score_gemma":0.96613526,"teacher_disagreement_score":0.92835796,"about_ca_system_score_codex":8.910456e-7,"about_ca_system_score_gemma":0.00030445258,"threshold_uncertainty_score":0.9994431},"labels":[],"label_agreement":null},{"id":"W1988626700","doi":"10.1139/e03-015","title":"Cave infill and associated biotic remains as indicators of Holocene environment in Gatineau Park (Quebec, Canada)","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature; Royal Ontario Museum; University of Ottawa","funders":"Université de Sherbrooke; University of Ottawa","keywords":"Holocene; Geology; Cave; Ecology; Geography; Physical geography; Archaeology; Oceanography; Biology","score_opus":0.012056638686565643,"score_gpt":0.20333480330030565,"score_spread":0.19127816461374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988626700","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99253243,0.0013527211,6.186493e-7,0.0007593043,0.00013725575,0.000058580663,0.000013591811,6.864318e-7,0.0051448],"genre_scores_gemma":[0.999493,0.000111245165,0.000108706095,0.00017123183,0.0000074392337,9.5788074e-8,0.0000023423893,0.0000010673444,0.00010484073],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985284,0.00026225185,0.00032026635,0.00014190943,0.00029604282,0.0004511249],"domain_scores_gemma":[0.99891806,0.0002568754,0.00021341721,0.00006907464,0.000030183366,0.000512395],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013467929,0.00008844303,0.00022803202,0.00045923563,0.00020809249,0.00002257628,0.00022416614,0.000087059634,0.0011278021],"category_scores_gemma":[0.00063713716,0.000071464776,0.000024224275,0.0004917898,0.0009966032,0.00011712893,0.000003408772,0.0002475011,0.000006472583],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003311665,0.0000033774206,0.998801,0.0000037098234,0.0000094277275,0.00016807343,0.00017310832,0.0005575005,0.000001438399,0.00008852,0.000037066544,0.00015349539],"study_design_scores_gemma":[0.00019612012,0.00015398,0.99793416,0.00002609295,0.0000054528255,0.00011295438,0.00047395972,0.000055051893,0.00013464011,0.00029515807,0.00053673104,0.00007572583],"about_ca_topic_score_codex":0.6458662,"about_ca_topic_score_gemma":0.9987404,"teacher_disagreement_score":0.35287416,"about_ca_system_score_codex":0.000003219807,"about_ca_system_score_gemma":0.0040549785,"threshold_uncertainty_score":0.9997853},"labels":[],"label_agreement":null},{"id":"W1988656906","doi":"10.1139/e06-037","title":"A petrological and geochemical study of the volcanic rocks of the Crowsnest Formation, southwestern Alberta, and of the Howell Creek suite, British Columbia","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta","keywords":"Geology; Geochemistry; Lithophile; Mantle (geology); Igneous rock; Trace element; Volcanic rock; Rare-earth element; Isotope geochemistry; Incompatible element; Isotope; Volcano; Mineralogy; Partial melting; Rare earth","score_opus":0.006979381095881234,"score_gpt":0.1565493938567015,"score_spread":0.14957001276082027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988656906","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984708,0.00041346045,0.0000011003914,0.00043123556,0.00006400764,0.00010331441,0.000043622622,5.6310034e-7,0.00047190092],"genre_scores_gemma":[0.9996578,0.0000062380627,0.000014191553,0.00008904355,0.000024356395,1.9348023e-7,6.160973e-7,6.49961e-7,0.00020692481],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987894,0.00011645254,0.00040833608,0.00012725056,0.00034152868,0.00021699921],"domain_scores_gemma":[0.99903685,0.00019038528,0.0003804795,0.00011387884,0.00012966755,0.00014871563],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041289322,0.00006666887,0.0002263096,0.000030036292,0.00035353232,0.00012669788,0.00055058935,0.000047088,0.00057779223],"category_scores_gemma":[0.00023603906,0.000037843103,0.00010425211,0.00047083158,0.0013024298,0.00012453075,0.000034025696,0.00015551966,3.5271597e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000024488534,0.000016219552,0.9991636,0.0000058524583,0.0000076004403,0.0000018431026,0.00014276996,0.00028963006,0.00007378601,0.0000016792127,0.00009743227,0.00019711608],"study_design_scores_gemma":[0.00018188737,0.00021070156,0.9968595,0.000029376162,0.00004019443,0.00010081916,0.000655339,0.0003127503,0.00010319457,0.0013330985,0.0001228834,0.000050293733],"about_ca_topic_score_codex":0.7335118,"about_ca_topic_score_gemma":0.9966272,"teacher_disagreement_score":0.2631154,"about_ca_system_score_codex":9.4712425e-7,"about_ca_system_score_gemma":0.00017400677,"threshold_uncertainty_score":0.632642},"labels":[],"label_agreement":null},{"id":"W1988689710","doi":"10.1139/e01-028","title":"The skull and tooth system of <i>Orlovichthys limnatis</i>, a Late Devonian dipnoan from Russia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Amgen (Canada)","funders":"","keywords":"Devonian; Skull; Dentition; Geology; Paleontology; Late Devonian extinction; Anatomy; Cusp (singularity); Biology; Geometry; Carboniferous; Mathematics; Structural basin","score_opus":0.012372237440101663,"score_gpt":0.19196958009165374,"score_spread":0.17959734265155208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988689710","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97597325,0.011147094,0.0000184305,0.0012278977,0.00065718085,0.000044744065,0.000059869344,0.0000030517547,0.010868478],"genre_scores_gemma":[0.9990146,0.00025866795,0.00039806232,0.00011347229,0.00010626277,1.0712897e-7,0.0000021933988,8.806545e-7,0.000105748964],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989283,0.00013903991,0.00030192093,0.00013087908,0.00015202216,0.0003478386],"domain_scores_gemma":[0.9989383,0.00029420736,0.00023636188,0.00008586778,0.000061308885,0.00038395787],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00078663573,0.00008625522,0.0001801523,0.00013752704,0.0006797998,0.000060009927,0.0003968077,0.000065642926,0.00025425485],"category_scores_gemma":[0.00008438375,0.000051603904,0.000043618827,0.00027022645,0.0012038839,0.00023652361,0.00000409148,0.00013701078,0.000017910432],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017027814,0.0000011660976,0.99427927,0.0000021824806,0.00001630679,0.000077467055,0.00017103,0.00020026884,0.000012693452,0.00051021477,0.00006272478,0.0046496494],"study_design_scores_gemma":[0.00012792496,0.00021896086,0.9797502,0.000036716945,0.000010641808,0.00037942437,0.0004554296,0.0011227529,0.000009544994,0.00069856155,0.01712275,0.00006710193],"about_ca_topic_score_codex":0.03081241,"about_ca_topic_score_gemma":0.7437389,"teacher_disagreement_score":0.7129265,"about_ca_system_score_codex":0.000001706614,"about_ca_system_score_gemma":0.000701002,"threshold_uncertainty_score":0.9756415},"labels":[],"label_agreement":null},{"id":"W1988698844","doi":"10.1139/e07-059","title":"Late Holocene glacial activity of Bridge Glacier, British Columbia Coast Mountains","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences; University of Victoria","keywords":"Moraine; Geology; Glacier; Subfossil; Holocene; Radiocarbon dating; Physical geography; Cirque glacier; Glacier morphology; Glacial period; Paleontology; Holocene climatic optimum; Archaeology; Oceanography; Ice stream; Geography; Cryosphere; Sea ice","score_opus":0.02565042070986739,"score_gpt":0.2485314826697793,"score_spread":0.22288106195991192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988698844","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946204,0.0006023133,0.000041989613,0.00019657478,0.00061067473,0.00007076219,0.00006562331,0.0000035158428,0.0037881879],"genre_scores_gemma":[0.9991592,0.000049223334,0.0002339761,0.00012330283,0.000107477266,5.9063016e-8,0.0000031883005,0.0000016703374,0.00032189258],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982601,0.00012846377,0.00034763405,0.000182022,0.00035607963,0.0007257228],"domain_scores_gemma":[0.9984784,0.0002342711,0.00025161565,0.00009521999,0.00021030623,0.0007301559],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002868569,0.00008137181,0.00028043304,0.00024996785,0.00063038495,0.00017928018,0.0005256629,0.0001231447,0.0018887917],"category_scores_gemma":[0.0002695725,0.000096281234,0.000090830115,0.0006489474,0.001882328,0.00039740955,0.000007828465,0.0003468265,0.000025612626],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019116489,0.000007337434,0.9947895,0.0000070433016,0.00001105368,0.00047120175,0.00011167906,0.00018177662,0.000009972296,0.0000053358913,0.00016252729,0.004223476],"study_design_scores_gemma":[0.0002499021,0.00037920556,0.99693674,0.000027986944,0.000008481746,0.0009821553,0.00009508559,0.00014749312,0.000075122436,0.0002836106,0.000714402,0.000099802804],"about_ca_topic_score_codex":0.2839212,"about_ca_topic_score_gemma":0.9945508,"teacher_disagreement_score":0.71062964,"about_ca_system_score_codex":9.659773e-7,"about_ca_system_score_gemma":0.0017591155,"threshold_uncertainty_score":0.9990236},"labels":[],"label_agreement":null},{"id":"W1988699146","doi":"10.1139/e99-109","title":"Mineral aerosols: a comparison of the last glacial maximum and preindustrial Holocene","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Last Glacial Maximum; Mineral dust; Holocene; Atmospheric sciences; Climatology; Ice core; Geology; Plume; Aerosol; Environmental science; Oceanography; Meteorology; Geography","score_opus":0.02662674884607939,"score_gpt":0.22608408496067084,"score_spread":0.19945733611459146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988699146","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931143,0.00056225166,0.0000021304697,0.00039072745,0.0003206547,0.000049154558,0.00002386999,0.0000014792092,0.0055354135],"genre_scores_gemma":[0.9990715,0.000010091725,0.0003202814,0.00007691053,0.00025356107,5.4702085e-8,7.857733e-7,0.0000010293669,0.00026582478],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990291,0.00004597065,0.0002968788,0.000112620735,0.0002482986,0.00026713137],"domain_scores_gemma":[0.9993062,0.000056089113,0.00018001166,0.000074673844,0.00003901487,0.00034398396],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034082404,0.000085932894,0.00018438818,0.000013502603,0.00033254575,0.00009280191,0.00037523243,0.000056985704,0.0030033574],"category_scores_gemma":[0.00007539293,0.00005387346,0.000060660335,0.00033221775,0.0008615332,0.0002108486,0.0000037160696,0.00017839848,0.000005762503],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017924664,0.000004301279,0.9811132,0.0000033792248,0.0000062838876,0.000008042154,0.0003020723,0.0031603253,0.00008875458,0.000004642088,0.00036602543,0.014925076],"study_design_scores_gemma":[0.000488606,0.00037559046,0.98754954,0.00007899349,0.000019259729,0.00016645841,0.00056604395,0.00084104727,0.0017317814,0.00017505573,0.007863505,0.00014409015],"about_ca_topic_score_codex":0.0040354044,"about_ca_topic_score_gemma":0.054734036,"teacher_disagreement_score":0.050698634,"about_ca_system_score_codex":9.873074e-7,"about_ca_system_score_gemma":0.00078721956,"threshold_uncertainty_score":0.99790806},"labels":[],"label_agreement":null},{"id":"W1988731536","doi":"10.1139/e99-116","title":"Granite petrogenesis in the Gander Zone, NE Newfoundland: mixing of melts from multiple sources and the role of lithospheric delamination","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"University of Oxford; Oxford Brookes University","keywords":"Geology; Magmatism; Mantle (geology); Geochemistry; Lithosphere; Subduction; Petrogenesis; Partial melting; Devonian; Igneous differentiation; Igneous rock; Petrology; Continental margin; Crust; Rift; Paleontology; Tectonics","score_opus":0.007376976343661318,"score_gpt":0.16750666217124174,"score_spread":0.16012968582758041,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988731536","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99169564,0.0067869346,0.000008086588,0.0005191481,0.000028048218,0.000037878584,0.000012480557,6.2940757e-7,0.0009111263],"genre_scores_gemma":[0.9994328,0.00015206577,0.00025623242,0.00010079655,0.00003096712,1.4496871e-7,0.0000022910738,5.1437576e-7,0.00002421499],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999085,0.00013473941,0.00027429947,0.0000939169,0.00024148719,0.0001705564],"domain_scores_gemma":[0.9991239,0.0004957425,0.00015727335,0.00005913313,0.000051267427,0.00011273581],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00081880303,0.00006435456,0.00018541906,0.0000763269,0.00016746212,0.000053310003,0.00032001536,0.000026985028,0.0015760437],"category_scores_gemma":[0.00011520334,0.00002972174,0.00007065883,0.00053163327,0.0006821069,0.00013789245,0.0000026185273,0.000085020045,0.0000024834599],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002076275,0.0000037365373,0.97578156,0.0000013601887,0.00000929909,0.0000035816543,0.00096845,0.0029312202,0.000033529323,0.000026045589,0.000001235516,0.020219231],"study_design_scores_gemma":[0.000267908,0.00008045507,0.9827181,0.000014881048,0.000025284508,0.000014284811,0.001639543,0.008475766,0.00014769676,0.0059933397,0.00057743356,0.000045326164],"about_ca_topic_score_codex":0.24163587,"about_ca_topic_score_gemma":0.74762434,"teacher_disagreement_score":0.5059885,"about_ca_system_score_codex":6.0426515e-7,"about_ca_system_score_gemma":0.000095381874,"threshold_uncertainty_score":0.99933666},"labels":[],"label_agreement":null},{"id":"W1988749992","doi":"10.1139/e05-039","title":"The edge of northwestern North America at ∼1.8 Ga","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Lithosphere; Proterozoic; Craton; Rift; Archean; Paleontology; Gravity anomaly; Structural basin; Crust; Seismology; Tectonics","score_opus":0.013968159783364785,"score_gpt":0.18336783297148007,"score_spread":0.16939967318811527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988749992","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9901844,0.0021750461,0.0000053706476,0.0022187629,0.00013322853,0.000025184425,0.000026255602,0.0000017107046,0.0052300394],"genre_scores_gemma":[0.9987338,0.00010280551,0.00035230216,0.00035750394,0.00013014411,6.629116e-8,0.0000030972756,6.2661815e-7,0.0003196092],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998843,0.00004551777,0.00033327597,0.000115574876,0.00029646166,0.00036612898],"domain_scores_gemma":[0.9988227,0.00019028575,0.00024825128,0.00009467584,0.00011891261,0.00052519655],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035084356,0.00008202519,0.00017137057,0.00010735403,0.000507671,0.000063503736,0.0005811164,0.00002360542,0.0039348383],"category_scores_gemma":[0.0001014457,0.00004211228,0.00012525017,0.0005597269,0.0010371482,0.00017006122,0.0000081789785,0.00011362612,0.00013192154],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000047702233,0.0000023465295,0.96960104,0.0000010263223,0.000009835003,0.000009674828,0.00010757672,0.0049207616,0.000010065507,0.000009442711,0.00016976999,0.02515368],"study_design_scores_gemma":[0.00006275516,0.00019599448,0.90512735,0.000006572158,0.000013987587,0.00003795234,0.00015464268,0.0009662862,0.0001421438,0.00035087476,0.09286616,0.00007530472],"about_ca_topic_score_codex":0.022716768,"about_ca_topic_score_gemma":0.9368409,"teacher_disagreement_score":0.91412413,"about_ca_system_score_codex":0.0000014855298,"about_ca_system_score_gemma":0.00034139337,"threshold_uncertainty_score":0.9969757},"labels":[],"label_agreement":null},{"id":"W1989109638","doi":"10.1139/e05-116","title":"Structural geology of the Penobsquis salt structure: late Bashkirian inversion tectonics in the Moncton Basin, New Brunswick, eastern Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Geology; Salt tectonics; Anticline; Tectonics; Structural basin; Diapir; Thrust fault; Paleontology; Geochemistry; Inversion (geology); Seismology; Petrology; Geomorphology","score_opus":0.012487436810704518,"score_gpt":0.18479582316352056,"score_spread":0.17230838635281603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989109638","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9914122,0.0019701505,0.0000012284139,0.0033968778,0.00092663587,0.00010028655,0.000022794953,0.0000014405099,0.0021683453],"genre_scores_gemma":[0.9988668,0.000015678293,0.00009804779,0.0007293965,0.00014269186,2.9884863e-8,0.0000020850755,0.0000019800418,0.00014327766],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99826884,0.00017074503,0.00040521598,0.00016455613,0.0005074486,0.00048322036],"domain_scores_gemma":[0.99903995,0.00019352867,0.00031803627,0.00016831809,0.000082098064,0.00019806658],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004866689,0.0001455223,0.0002412339,0.0001781182,0.00047063292,0.00007791762,0.00090699736,0.000056455145,0.0007655255],"category_scores_gemma":[0.000117053896,0.00007690481,0.00008001764,0.0007547238,0.00059855846,0.00020532425,0.000012338802,0.0003065701,0.0000024413214],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057343113,7.2805244e-7,0.9893187,0.000003659152,0.000007059073,0.00003570489,0.0003202597,0.0075298115,0.0000064250335,0.00013282163,0.00052220665,0.0021168396],"study_design_scores_gemma":[0.00023501576,0.00011788533,0.99189866,0.000028027225,0.000011696696,0.00010089326,0.0004678576,0.001126673,0.000097994314,0.0011166221,0.0047011566,0.00009754761],"about_ca_topic_score_codex":0.9873305,"about_ca_topic_score_gemma":0.9998831,"teacher_disagreement_score":0.012552575,"about_ca_system_score_codex":0.000007615375,"about_ca_system_score_gemma":0.008339084,"threshold_uncertainty_score":0.9972827},"labels":[],"label_agreement":null},{"id":"W1989130500","doi":"10.1139/e08-064","title":"A middle Cenomanian euselachian assemblage from the Dunvegan Formation of northwestern Alberta","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Ichthyology and Marine Biology","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Assemblage (archaeology); Geology; Cenomanian; Taxon; Paleontology; Range (aeronautics); Latitude; Oceanography; Geography; Structural basin","score_opus":0.0214054906254462,"score_gpt":0.19428013707720052,"score_spread":0.17287464645175432,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989130500","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896938,0.000084138155,0.000036859743,0.0009009774,0.00022042943,0.000048936046,0.0000053158774,0.000001131425,0.009008393],"genre_scores_gemma":[0.998875,0.000013844463,0.00029649553,0.00045222038,0.000056685927,3.6773096e-7,0.000001547189,0.0000022431561,0.00030155736],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99920046,0.0000825734,0.00024767796,0.00009505184,0.0001390804,0.00023513859],"domain_scores_gemma":[0.9993723,0.00010379534,0.00019659413,0.0001089476,0.000016450596,0.00020190592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036043458,0.00006929392,0.00011731836,0.00004704219,0.00040031373,0.000015620406,0.0005154472,0.00004676713,0.0007738859],"category_scores_gemma":[0.000071947776,0.00004420146,0.00005203684,0.000199508,0.0009868655,0.000360863,0.00002980262,0.00011166902,0.00008917004],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004688545,0.0000067998644,0.99576455,6.907119e-7,0.0000049439914,0.000025051451,0.0027370218,0.00016050259,0.0005139848,0.00010233327,0.0003258687,0.00035358628],"study_design_scores_gemma":[0.00013282074,0.00020589652,0.98292434,0.000010240959,0.000008310903,0.0002549534,0.0003713627,0.00010247304,0.0006366602,0.00021737147,0.015069592,0.00006596428],"about_ca_topic_score_codex":0.12468479,"about_ca_topic_score_gemma":0.90723515,"teacher_disagreement_score":0.7825504,"about_ca_system_score_codex":0.000008918467,"about_ca_system_score_gemma":0.00023173049,"threshold_uncertainty_score":0.881144},"labels":[],"label_agreement":null},{"id":"W1989189038","doi":"10.1139/e04-064","title":"Origin of the Archean Sask craton and its extent within the Trans-Hudson orogen: evidence from Pb and Nd isotopic compositions of basement rocks and post-orogenic intrusions","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Regina","funders":"Natural Sciences and Engineering Research Council of Canada; Geological Society of America; Syracuse University; National Science Foundation","keywords":"Craton; Geology; Geochemistry; Archean; Zircon; Pegmatite; Metallogeny; Basement; Crust; Geochronology; Yilgarn Craton; Partial melting; Terrane; Petrology; Paleontology; Tectonics; Sphalerite","score_opus":0.024323581269615237,"score_gpt":0.2162817947325329,"score_spread":0.19195821346291767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989189038","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98297,0.009553232,0.000014942124,0.007206492,0.000044718436,0.000078120516,0.00006920003,8.04876e-7,0.00006246617],"genre_scores_gemma":[0.99888176,0.00024054386,0.0005269786,0.00030121015,0.000032417593,2.0894778e-7,0.0000012374404,5.7727203e-7,0.000015073027],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990698,0.000101892954,0.00029367194,0.00013517725,0.00023163739,0.00016783513],"domain_scores_gemma":[0.9991209,0.00024054662,0.00016501079,0.0000733062,0.00008950087,0.0003107633],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048720642,0.00008080572,0.00016696252,0.00007239162,0.00036523983,0.000047114896,0.00025893273,0.000028970726,0.00081929605],"category_scores_gemma":[0.00010048896,0.000039248032,0.000056946625,0.0002601338,0.00067902403,0.00016769058,0.00001203537,0.00013564994,0.0000010012012],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012933744,0.00001034799,0.9844245,0.000010408294,0.000034825312,0.000003876823,0.0014580617,0.0020932148,0.007659405,0.00014267753,0.000016371834,0.0041334312],"study_design_scores_gemma":[0.00014089905,0.0002586211,0.98087364,0.00013110077,0.000087386754,0.00006682144,0.0010310566,0.0059252526,0.009128232,0.0020652376,0.0002058983,0.00008583729],"about_ca_topic_score_codex":0.028251603,"about_ca_topic_score_gemma":0.50198334,"teacher_disagreement_score":0.47373176,"about_ca_system_score_codex":0.0000012828225,"about_ca_system_score_gemma":0.00026764997,"threshold_uncertainty_score":0.97821933},"labels":[],"label_agreement":null},{"id":"W1989501968","doi":"10.1139/e02-084","title":"Late Middle Ordovician olistostrome formation and magmatism along the Red Indian Line, the Laurentian arc Gondwanan arc boundary, at Sops Head, Newfoundland","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Government of Newfoundland and Labrador","funders":"","keywords":"Geology; Ordovician; Conodont; Magmatism; Paleontology; Provenance; Terrane; Volcanic arc; Geochemistry; Biostratigraphy; Subduction; Tectonics","score_opus":0.02409522582841883,"score_gpt":0.19312591862369283,"score_spread":0.169030692795274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989501968","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9740855,0.003927196,0.00000929978,0.018167568,0.0002110817,0.000084874955,0.00003935653,0.0000044781796,0.003470662],"genre_scores_gemma":[0.99796563,0.00016931439,0.00017671833,0.0010195661,0.00016631726,3.4079196e-7,0.00001284077,0.0000016162484,0.00048764213],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99846125,0.000121545396,0.00038049754,0.00017306097,0.00036086203,0.0005027825],"domain_scores_gemma":[0.99881124,0.00014473716,0.00025112205,0.00013863796,0.00007600451,0.0005782751],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007507237,0.00014057873,0.00020044911,0.00018202432,0.0016795258,0.00044446267,0.00055214093,0.000054804812,0.006447793],"category_scores_gemma":[0.00012383703,0.000069221605,0.000102889564,0.0006142285,0.001094022,0.00054173043,0.000015077956,0.00026773702,0.00007338154],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007528457,0.000005329837,0.97779906,0.00000989477,0.000026486536,0.00007170424,0.0014922296,0.0010128729,0.00002355843,0.00007609868,0.00057090167,0.018904308],"study_design_scores_gemma":[0.00019048901,0.00021232494,0.95605314,0.000041437204,0.0000354525,0.000379262,0.00040417787,0.0053590215,0.000013613601,0.005822516,0.031348303,0.00014024331],"about_ca_topic_score_codex":0.063483536,"about_ca_topic_score_gemma":0.9783897,"teacher_disagreement_score":0.91490614,"about_ca_system_score_codex":0.0000048673346,"about_ca_system_score_gemma":0.00012448576,"threshold_uncertainty_score":0.99962014},"labels":[],"label_agreement":null},{"id":"W1989544004","doi":"10.1139/e09-074","title":"Initiation, development, and benefits of Lithoprobe — shaping the direction of Earth science research in Canada and beyondThis article is one of a series of papers published in this Special Issue on the theme <i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.Lithoprobe Contribution 1480.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geography; Engineering","score_opus":0.024747062645303332,"score_gpt":0.2201690240189951,"score_spread":0.19542196137369178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989544004","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99687266,0.0006639637,0.0000011825836,0.0014700389,0.00015404749,0.00027755537,0.000060220875,5.1358643e-7,0.0004997877],"genre_scores_gemma":[0.9995586,0.00010702469,0.00023854732,0.000033538985,0.00004983094,0.0000015786839,8.5033423e-7,0.0000013779407,0.000008608759],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982258,0.00018719885,0.0005675562,0.00016265776,0.00059675233,0.00026002416],"domain_scores_gemma":[0.9981451,0.00047443804,0.0005247044,0.00011195934,0.0006388075,0.00010497434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005867134,0.00008259051,0.00028189653,0.00027903894,0.0002839094,0.00008887767,0.00029300535,0.00003538153,0.00018082687],"category_scores_gemma":[0.0011767105,0.000045835222,0.000016366204,0.0012252299,0.0022330545,0.00052496715,0.000021226464,0.00017740065,7.817042e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037392369,0.000039704442,0.9458896,0.0002561676,0.000037964834,0.0000024116803,0.017728902,0.0005121438,0.01995091,0.008740957,0.000045744953,0.006421594],"study_design_scores_gemma":[0.00050933636,0.00022887797,0.90737206,0.00032101446,0.0000123637865,0.000011345345,0.0025097057,0.00022967768,0.08630106,0.002010636,0.0004185526,0.00007534801],"about_ca_topic_score_codex":0.59989464,"about_ca_topic_score_gemma":0.9666732,"teacher_disagreement_score":0.36677858,"about_ca_system_score_codex":0.000006637829,"about_ca_system_score_gemma":0.0034469983,"threshold_uncertainty_score":0.82277817},"labels":[],"label_agreement":null},{"id":"W1989839350","doi":"10.1139/e05-013","title":"Wes Wehr dedication","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Botany, Ecology, and Taxonomy Studies","field":"Agricultural and Biological Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta; Brandon University","funders":"","keywords":"Archaeology; Geology; Friendship; Natural (archaeology); Art history; Paleontology; History; Sociology","score_opus":0.03788747391474443,"score_gpt":0.21754910270151945,"score_spread":0.17966162878677502,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989839350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.976584,0.0015449609,0.00000429221,0.01435558,0.00031742486,0.000041055846,0.0000054270117,0.000004417554,0.007142832],"genre_scores_gemma":[0.9977577,0.0000709714,0.0007204944,0.00057856616,0.0006101146,7.5943666e-7,1.2294166e-7,1.934617e-7,0.00026111494],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992975,0.000029997775,0.0001921385,0.00009817924,0.00012318202,0.0002590163],"domain_scores_gemma":[0.9993618,0.00008382375,0.00014144926,0.000018367606,0.00009514936,0.00029941328],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004929899,0.000060238344,0.000107432206,0.000035687928,0.000524577,0.00007428048,0.0002897751,0.000036689697,0.00062322535],"category_scores_gemma":[0.000111503396,0.000022501781,0.000053965723,0.00027657277,0.00036852786,0.00026273643,0.0000057763527,0.00008122082,0.000042836866],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045121296,0.000019783372,0.9466683,0.0000018179064,0.000023312468,0.000017375638,0.00007052048,0.000074628806,0.0041335896,0.00039913226,0.0045008976,0.044086106],"study_design_scores_gemma":[0.00003926666,0.00021023014,0.71306294,0.000007989636,0.000004610108,0.000026181842,0.00041538835,0.000020530724,0.0002610177,0.0003092069,0.28558323,0.000059381717],"about_ca_topic_score_codex":0.00024259166,"about_ca_topic_score_gemma":0.4287092,"teacher_disagreement_score":0.42846662,"about_ca_system_score_codex":0.0000060691737,"about_ca_system_score_gemma":0.00016260745,"threshold_uncertainty_score":0.682388},"labels":[],"label_agreement":null},{"id":"W1989983775","doi":"10.1139/e00-078","title":"Geological and geochemical evidence for variable magmatism and tectonics in the southern Canadian Cordillera: Paleozoic to Jurassic suites, Greenwood, southern British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of British Columbia; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada; Universidad del Atlántico","keywords":"Geology; Terrane; Paleozoic; Permian; Paleontology; Zircon; Volcanic rock; Sedimentary rock; Island arc; Craton; Siliciclastic; Oceanic crust; Basalt; Unconformity; Crust; Geochemistry; Subduction; Tectonics; Sedimentary depositional environment; Volcano; Structural basin","score_opus":0.02538936644290254,"score_gpt":0.20802145284396492,"score_spread":0.18263208640106238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989983775","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99247515,0.003492709,0.000014174603,0.0029802308,0.000056286975,0.00017738879,0.0001333803,0.0000029294617,0.0006677244],"genre_scores_gemma":[0.9969521,0.00010604328,0.001217459,0.0014561098,0.00007816058,0.0000015667015,0.0000053318304,0.0000017040757,0.00018149668],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99832517,0.000095714655,0.0003361614,0.0002985849,0.00026296373,0.0006814011],"domain_scores_gemma":[0.9979595,0.00068439863,0.00009969113,0.000094024785,0.00011273745,0.0010496792],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013140353,0.00011564176,0.00027675758,0.00014263183,0.0005666995,0.00065808225,0.0005076564,0.00009732887,0.003657272],"category_scores_gemma":[0.0010086951,0.00009198227,0.000057651036,0.0007311065,0.0005953496,0.00017358857,0.000010934659,0.00024232881,0.000015840486],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000056764557,0.0000036342535,0.99243677,0.0000053662525,0.000007198919,0.00010537025,0.00020863616,0.00018326548,0.000013489549,0.000009890239,0.00019565338,0.0068250373],"study_design_scores_gemma":[0.00018309707,0.0003215862,0.9865153,0.00009706943,0.000027992453,0.0005898713,0.0010903088,0.0016108573,0.0000011573144,0.0058935657,0.003490466,0.0001787573],"about_ca_topic_score_codex":0.9182633,"about_ca_topic_score_gemma":0.99940616,"teacher_disagreement_score":0.08114284,"about_ca_system_score_codex":0.0000040697196,"about_ca_system_score_gemma":0.0006344651,"threshold_uncertainty_score":0.99725354},"labels":[],"label_agreement":null},{"id":"W1990058169","doi":"10.1139/e02-095","title":"Conodont biostratigraphy of the Lower to Middle Devonian Deserters Formation (new), Road River Group, northeastern British Columbia","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"","keywords":"Conodont; Devonian; Geology; Biostratigraphy; Facies; Paleontology; Group (periodic table); Carboniferous; Tournaisian; Structural basin; Paleozoic; Stratigraphic unit","score_opus":0.014870355689823924,"score_gpt":0.1846655330093632,"score_spread":0.16979517731953928,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990058169","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961213,0.0002684843,0.0011098979,0.00015207642,0.00036371106,0.00006805078,0.000005473611,0.0000038229437,0.0019072203],"genre_scores_gemma":[0.9992107,0.000012637286,0.00048029196,0.000107599444,0.000020823223,5.315034e-7,3.1403854e-7,0.000004106419,0.00016298154],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992108,0.000035899782,0.00027850523,0.00006512273,0.00021024351,0.00019946985],"domain_scores_gemma":[0.999329,0.000008088248,0.000081383456,0.0000857579,0.00007862664,0.00041715088],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002610493,0.000055496082,0.00012328873,0.00013877441,0.00025761698,0.00038296572,0.00025977712,0.000030165962,0.00012108539],"category_scores_gemma":[0.00004087563,0.000054290063,0.00010851015,0.0006586926,0.00015217758,0.0003599807,0.0000029597938,0.00007792804,0.0000040099035],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007669621,0.00005616538,0.7413976,0.000072372,0.00026999577,0.000100831436,0.009431381,0.22388983,0.0028572478,0.00017538079,0.0071557323,0.0145857595],"study_design_scores_gemma":[0.0014098097,0.0009985822,0.8758653,0.0009026099,0.00012413152,0.0004621249,0.005666523,0.044230223,0.0034210098,0.0009784616,0.065016985,0.0009242539],"about_ca_topic_score_codex":0.03354443,"about_ca_topic_score_gemma":0.9472466,"teacher_disagreement_score":0.9137022,"about_ca_system_score_codex":0.000008763473,"about_ca_system_score_gemma":0.00030687102,"threshold_uncertainty_score":0.9728913},"labels":[],"label_agreement":null},{"id":"W1990203356","doi":"10.1139/e04-100","title":"Fossil biotas from the Okanagan Highlands, southern British Columbia and northeastern Washington State: climates and ecosystems across an Eocene landscape","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":209,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; Brandon University","funders":"University of Alberta","keywords":"Ecology; Taxon; Deciduous; Paleobotany; Geography; Fagaceae; Biology","score_opus":0.014496926442007493,"score_gpt":0.18235118484858617,"score_spread":0.1678542584065787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990203356","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99604654,0.0017718828,2.561119e-7,0.0009973053,0.00012116126,0.000045731213,0.0009641473,0.000005268846,0.000047702986],"genre_scores_gemma":[0.9993467,0.00014102475,0.000032188582,0.00012495946,0.00025242378,1.5690351e-7,0.000012526152,4.650146e-7,0.000089595786],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991651,0.000060151222,0.00016013405,0.00015558791,0.00016076771,0.00029824194],"domain_scores_gemma":[0.9993396,0.00008583912,0.00012600413,0.000025041107,0.000052337266,0.0003711961],"candidate_categories":["scholarly_communication"],"consensus_categories":[],"category_scores_codex":[0.0005584301,0.00006345948,0.00012475468,0.000009707987,0.0011601192,0.0014159584,0.0002679721,0.000044106207,0.00016972859],"category_scores_gemma":[0.000025102647,0.000032305743,0.00002697705,0.00014029254,0.00025507598,0.00046564624,0.000020712085,0.00009382425,0.000006320767],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004279022,0.000004988947,0.97675306,0.0000013039552,0.000006112607,0.000016443953,0.0009003303,0.000013045603,0.00041670105,8.2092515e-7,0.000326824,0.021556074],"study_design_scores_gemma":[0.00014090024,0.00017738328,0.98017365,0.00005957478,0.0000082793285,0.00015793975,0.005817315,0.00041020196,0.000020070698,0.000080375234,0.012849683,0.00010462265],"about_ca_topic_score_codex":0.3125621,"about_ca_topic_score_gemma":0.99562216,"teacher_disagreement_score":0.6830601,"about_ca_system_score_codex":0.000003565156,"about_ca_system_score_gemma":0.00005443378,"threshold_uncertainty_score":0.9996207},"labels":[],"label_agreement":null},{"id":"W1990318832","doi":"10.1139/e02-900","title":"ERRATUM: A rewiew of <i>Leidyosuchus canadiensis</i> Lambe, 1907 (Archosauria: Crocodylia) and an assessment of cranial variation based upon new material: Erratum","year":2002,"lang":"en","type":"erratum","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Royal Tyrrell Museum; University of Calgary","funders":"","keywords":"Taxon; Paleontology; Geology; Fibrous joint; Foramen; Cretaceous; Apex (geometry); Anatomy; Variation (astronomy); Biology","score_opus":0.021820876316022524,"score_gpt":0.2539009077508563,"score_spread":0.23208003143483374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990318832","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.64294565,0.03265643,0.00053608377,0.008209683,0.13844827,0.0017032599,0.007024143,0.000050699407,0.1684258],"genre_scores_gemma":[0.9865782,0.00071972754,0.0060077105,0.0005958743,0.00193982,0.000001021027,0.00037506732,0.000012551179,0.003770001],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.996842,0.00047857332,0.0009827635,0.00045355325,0.00050932314,0.0007337702],"domain_scores_gemma":[0.9968545,0.00014438064,0.001278671,0.00025184653,0.0003273171,0.0011432851],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001582397,0.00033214618,0.0008770401,0.0009270365,0.0004376846,0.00009544554,0.00075241853,0.0005694387,0.0018204978],"category_scores_gemma":[0.0001885157,0.00028334215,0.00014035321,0.0006067252,0.001194413,0.0005493778,0.0000068001527,0.00068222184,0.0000028477937],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024778466,0.0000774635,0.49959055,0.0003939971,0.00028236996,0.000667117,0.0011510932,0.0029306295,0.00043748136,0.0008002619,0.48730135,0.006119909],"study_design_scores_gemma":[0.00047622397,0.0020696525,0.9480477,0.00032349012,0.00013419436,0.0002768649,0.000085650936,0.0036319497,0.000009833629,0.0017838966,0.0428043,0.00035622274],"about_ca_topic_score_codex":0.18954143,"about_ca_topic_score_gemma":0.9309206,"teacher_disagreement_score":0.7413792,"about_ca_system_score_codex":0.000012459393,"about_ca_system_score_gemma":0.011175619,"threshold_uncertainty_score":0.99996185},"labels":[],"label_agreement":null},{"id":"W1990340499","doi":"10.1139/e03-056","title":"The impact of climate change on an emerging coastline affected by discontinuous permafrost: Manitounuk Strait, northern Quebec","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Permafrost; Geology; Thermokarst; Shore; Post-glacial rebound; Climate change; Sea level; Glacial period; Arctic; Geomorphology; Physical geography; Oceanography; Global warming; Tectonic uplift; Outcrop; Earth science; Structural basin","score_opus":0.03708695114783231,"score_gpt":0.2672768921089601,"score_spread":0.2301899409611278,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990340499","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99234337,0.001700557,0.0000013106572,0.0002878835,0.00048199884,0.0001293456,0.0031240284,0.0000035439275,0.0019279446],"genre_scores_gemma":[0.999188,0.00033043098,0.000013482127,0.000094392424,0.00019342122,4.14045e-7,0.00010212076,0.000004875197,0.00007284685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99825066,0.00018150383,0.00036648448,0.00017896849,0.00034344697,0.000678919],"domain_scores_gemma":[0.9985961,0.00013670957,0.00033967683,0.00015223165,0.000130125,0.0006451571],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010618167,0.000180535,0.00024474112,0.00021452765,0.00079344504,0.00029979894,0.00046662663,0.000049943985,0.0017016244],"category_scores_gemma":[0.00008983213,0.00010503434,0.00014006764,0.0004383551,0.0005037696,0.00057015126,0.0000034454513,0.00019752671,0.000028433833],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021251748,0.000016006985,0.98699045,0.0000053216613,0.000016164284,0.000048968803,0.0013954561,0.0005256797,0.0003131669,0.00003905833,0.00022654691,0.010401924],"study_design_scores_gemma":[0.00026040553,0.0013047094,0.9917938,0.00007581691,0.000014091234,0.0001141684,0.0028031312,0.0006479444,0.00009715638,0.000055198976,0.0026473626,0.00018618532],"about_ca_topic_score_codex":0.23774818,"about_ca_topic_score_gemma":0.9875405,"teacher_disagreement_score":0.74979234,"about_ca_system_score_codex":0.0000069602866,"about_ca_system_score_gemma":0.00061483646,"threshold_uncertainty_score":0.99921095},"labels":[],"label_agreement":null},{"id":"W1990375628","doi":"10.1139/e03-028","title":"Geology, geochronology, and geochemistry of Archean rocks in the Eqe Bay area, north-central Baffin Island, Canada: constraints on the depositional and tectonic history of the Mary River Group of northeastern Rae Province","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"ARC Resources (Canada); University of Regina","funders":"","keywords":"Geology; Archean; Plutonism; Geochemistry; Metamorphism; Zircon; Geochronology; Felsic; Greenstone belt; Gneiss; Volcanic rock; Precambrian; Proterozoic; Terrane; Mafic; Metamorphic rock; Tectonics; Magmatism; Paleontology; Volcano","score_opus":0.009721496994432994,"score_gpt":0.1535612400339805,"score_spread":0.1438397430395475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990375628","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99449027,0.0017789529,0.0000040604054,0.0010150657,0.000057986854,0.00007436323,0.00005542307,3.4474888e-7,0.0025235452],"genre_scores_gemma":[0.9996544,0.000021140524,0.000031707314,0.0002539063,0.000010644005,2.6413272e-7,0.0000030105482,5.9440015e-7,0.000024348648],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886805,0.00015077437,0.00030955626,0.00013961282,0.00025324427,0.0002787506],"domain_scores_gemma":[0.9990984,0.00033804658,0.00025958163,0.00009789587,0.00005635036,0.00014973136],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0005270826,0.000096132906,0.00020405825,0.00006432176,0.00012073249,0.000008035315,0.0003827389,0.00004617836,0.000868393],"category_scores_gemma":[0.00013803956,0.000045743654,0.000057494926,0.00017789866,0.0033973947,0.00005000083,0.000008783622,0.00024875253,1.7283118e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013836377,0.000009313481,0.9980443,0.000009920752,0.000014637196,0.000016963464,0.00015699914,0.00054101634,0.000046903548,0.00009468028,0.000045355588,0.0010060398],"study_design_scores_gemma":[0.00018351771,0.00013014214,0.9978083,0.000032293836,0.000017086706,0.00016098598,0.0003828794,0.00028444058,0.00016714823,0.0005314579,0.00024438102,0.000057375983],"about_ca_topic_score_codex":0.38962004,"about_ca_topic_score_gemma":0.9952224,"teacher_disagreement_score":0.6056024,"about_ca_system_score_codex":0.000008377082,"about_ca_system_score_gemma":0.0021003257,"threshold_uncertainty_score":0.9993148},"labels":[],"label_agreement":null},{"id":"W1990484740","doi":"10.1139/e03-065","title":"Subaqueous silicification of the contents of small ponds in an Early Devonian hot-spring complex, Rhynie, Scotland","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Devonian; Microbial mat; Biota; Subaerial; Hot spring; Algal mat; Sedimentary depositional environment; Paleontology; Geochemistry; Algae; Ecology; Biology","score_opus":0.051743866494970224,"score_gpt":0.22932934235048863,"score_spread":0.1775854758555184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990484740","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9908554,0.0012823094,0.000010402609,0.00007064548,0.00020148199,0.00006828498,0.000016121825,9.438695e-7,0.007494422],"genre_scores_gemma":[0.9994795,0.0000095338555,0.00046544228,0.000024821307,0.000011034693,8.38749e-8,2.6683998e-7,5.002722e-7,0.000008856885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886143,0.00018028748,0.0003842538,0.00011412827,0.00019309518,0.00026680392],"domain_scores_gemma":[0.999123,0.00008215926,0.00032161773,0.00011442833,0.00010392057,0.00025487106],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00080661767,0.00007791549,0.00019280861,0.00029663235,0.0001979953,0.000039509483,0.00046798665,0.000053848114,0.00009656119],"category_scores_gemma":[0.00012081065,0.000053833315,0.00006533621,0.0004892395,0.0007663487,0.0002727971,5.793243e-7,0.00014484588,6.8008626e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008422278,0.0000055580495,0.99652964,0.000004218419,0.000004774303,0.000010627276,0.0004100819,0.00032870503,0.0005164164,0.0003167778,0.0000010071597,0.0018637795],"study_design_scores_gemma":[0.00017538862,0.00027108128,0.9976955,0.00004351734,0.000005167592,0.000042094813,0.00030318447,0.0002553248,0.0008515856,0.00026389057,0.000032656422,0.00006057912],"about_ca_topic_score_codex":0.025150293,"about_ca_topic_score_gemma":0.8379889,"teacher_disagreement_score":0.8128386,"about_ca_system_score_codex":0.0000011690114,"about_ca_system_score_gemma":0.00068971753,"threshold_uncertainty_score":0.9813413},"labels":[],"label_agreement":null},{"id":"W1991000915","doi":"10.1139/e01-081","title":"Proterozoic tectonic accretion and growth of western Laurentia: results from Lithoprobe studies in northern Alberta","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University; Geological Survey of Canada","funders":"","keywords":"Geology; Terrane; Laurentia; Shear zone; Archean; Imbrication; Continental crust; Magmatism; Accretion (finance); Geochemistry; Paleontology; Subduction; Fibrous joint; Craton; Mafic; Continental arc; Continental collision; Continental margin; Basement; Proterozoic; Tectonics; Crust","score_opus":0.03276947930702665,"score_gpt":0.2136910807444515,"score_spread":0.18092160143742486,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991000915","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923671,0.0052532763,0.0000015366519,0.0014745607,0.00007992615,0.000050655817,0.000025508109,0.0000011822686,0.00074628653],"genre_scores_gemma":[0.99939686,0.00019093767,0.00022741381,0.00006567793,0.00004357998,1.7246052e-7,0.000003324616,6.813745e-7,0.00007132241],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989304,0.00006537671,0.00038400976,0.00017761832,0.00019968812,0.00024291429],"domain_scores_gemma":[0.9991619,0.00020379548,0.00021761356,0.00006101693,0.00010662935,0.00024902172],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041902182,0.000088616456,0.00024375296,0.00021188745,0.00010647809,0.00004413255,0.00023787201,0.000041885316,0.00069012446],"category_scores_gemma":[0.0004737671,0.000056111367,0.000051212366,0.0004880324,0.00058143126,0.00023397322,0.0000071695076,0.00013256606,0.000014466816],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007983702,0.000004432789,0.99757355,0.0000054073353,0.000015633388,0.000021093954,0.0005909609,0.00020659869,0.000023264625,0.0000041526196,0.0000099551635,0.0015369628],"study_design_scores_gemma":[0.00026459602,0.00026056397,0.9937977,0.00009440663,0.000018824878,0.00002325434,0.0003006569,0.00079715863,0.00017660909,0.0040731085,0.0001029426,0.00009014608],"about_ca_topic_score_codex":0.13432485,"about_ca_topic_score_gemma":0.9644196,"teacher_disagreement_score":0.83009475,"about_ca_system_score_codex":0.000001372875,"about_ca_system_score_gemma":0.00007665955,"threshold_uncertainty_score":0.87143975},"labels":[],"label_agreement":null},{"id":"W1991024294","doi":"10.1139/e07-013","title":"A synopsis of mineral deposits in the Archean and Proterozoic rocks of the Lake Nipigon Region, Thunder Bay District, Ontario","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geoscience BC; Ministry of Energy, Northern Development and Mines","funders":"","keywords":"Geology; Geochemistry; Archean; Proterozoic; Ultramafic rock; Mafic; Craton; Rift; Geomorphology; Paleontology","score_opus":0.019247053215331832,"score_gpt":0.18871658822737358,"score_spread":0.16946953501204176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991024294","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99613285,0.00045584686,0.000021415688,0.0013678065,0.000055225424,0.00006868854,0.0000047019653,4.473189e-7,0.0018930376],"genre_scores_gemma":[0.99956614,0.0000061207998,0.0001254388,0.00018471749,0.000025971256,1.0128413e-7,7.4051997e-7,4.2312902e-7,0.00009036431],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99894494,0.00007511685,0.0003297175,0.00010591852,0.00028111707,0.00026321455],"domain_scores_gemma":[0.9993086,0.0001384052,0.00020697863,0.00008183746,0.00006609635,0.00019807708],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009273591,0.000072432245,0.0001647106,0.00013806649,0.00015725858,0.000034761655,0.00045024016,0.00003577426,0.0002018747],"category_scores_gemma":[0.00013316263,0.000032659045,0.000080907885,0.00066262844,0.0006316934,0.00010286898,0.0000071432164,0.00018597236,5.2691496e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009728411,0.000005526703,0.99740106,0.0000044619655,0.0000059428758,0.000018785018,0.0005514754,0.0002933073,0.000023776287,0.000015618598,0.000025886187,0.0016444407],"study_design_scores_gemma":[0.000083652674,0.00018930656,0.996938,0.000038589245,0.000014424275,0.000099632285,0.0003860486,0.000067461944,0.00020044779,0.0014992941,0.000437387,0.000045771652],"about_ca_topic_score_codex":0.2174718,"about_ca_topic_score_gemma":0.99652374,"teacher_disagreement_score":0.7790519,"about_ca_system_score_codex":0.0000016760177,"about_ca_system_score_gemma":0.00034537676,"threshold_uncertainty_score":0.7877391},"labels":[],"label_agreement":null},{"id":"W1991157510","doi":"10.1139/e06-050","title":"Multiple deformation episodes at Myra Falls volcanic-hosted massive sulfide camp, central Vancouver Island, British Columbia, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Fold (higher-order function); Cretaceous; Lineation; Seismology; Thrust fault; Shear zone; Basin and range topography; Outcrop; Paleontology; Geomorphology; Geochemistry; Fault (geology); Tectonics","score_opus":0.005339194809614937,"score_gpt":0.14908908666951828,"score_spread":0.14374989185990333,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991157510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995223,0.0006321854,0.000020521995,0.00031115446,0.0005853333,0.00007266589,0.0003268313,0.0000044110825,0.002823931],"genre_scores_gemma":[0.99782246,0.000017133121,0.00026662683,0.00040364906,0.00015362281,2.5461128e-7,0.000043679185,0.0000016446401,0.0012909248],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99801826,0.000066039785,0.0004764992,0.00020944272,0.0004941298,0.0007356188],"domain_scores_gemma":[0.9985228,0.00015528343,0.0002959617,0.000078983154,0.00017925914,0.0007676821],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00030094464,0.00011543216,0.00026499847,0.000086440254,0.0007092215,0.00037135952,0.00040296136,0.00006363775,0.011486304],"category_scores_gemma":[0.0002026517,0.00011158905,0.00011547197,0.00052292075,0.0003634741,0.00040855483,0.000008914243,0.00016587015,0.000022907245],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000038676453,0.0000035192315,0.9759154,0.000003528004,0.000010809307,0.00015789169,0.000028963652,0.010846159,0.000018936518,0.000001571007,0.011851041,0.0011583286],"study_design_scores_gemma":[0.00026026368,0.00009493983,0.9777635,0.000027615097,0.000020726458,0.000106520216,0.0003285107,0.004294156,0.00009259129,0.0010534074,0.01576373,0.00019404161],"about_ca_topic_score_codex":0.9981811,"about_ca_topic_score_gemma":0.99999934,"teacher_disagreement_score":0.011463396,"about_ca_system_score_codex":0.00002190692,"about_ca_system_score_gemma":0.0016376558,"threshold_uncertainty_score":0.9894173},"labels":[],"label_agreement":null},{"id":"W1991179718","doi":"10.1139/e00-064","title":"A new carnosaur (Dinosauria: Theropoda) from the Lower Cretaceous of Japan","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":125,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Theropoda; Geology; Paleontology; Cretaceous; Claw; Biology; Ecology","score_opus":0.01520590012699883,"score_gpt":0.20208111662800565,"score_spread":0.18687521650100683,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991179718","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.972751,0.009940987,0.000012870722,0.002533198,0.0007736132,0.000044736924,0.00006309387,0.0000025056788,0.013877947],"genre_scores_gemma":[0.9980045,0.00012110962,0.0006118122,0.0005002003,0.0003116083,4.4964448e-8,0.0000033187496,9.546167e-7,0.00044647735],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99889433,0.00015014363,0.00027876222,0.00013780915,0.00019349265,0.00034545065],"domain_scores_gemma":[0.9989906,0.0002916341,0.00014952601,0.0001202923,0.000050243372,0.00039771356],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005322462,0.000093910225,0.00019058122,0.000089873865,0.00037293066,0.00003415408,0.0006660162,0.0000832859,0.022870522],"category_scores_gemma":[0.00008852273,0.00005495387,0.00009106214,0.00029109858,0.0009148513,0.00021933738,0.00000205017,0.00019443466,0.00011801701],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027974142,0.0000028012014,0.9752416,4.93173e-7,0.000021725806,0.000028908371,0.00035535716,0.0010116193,0.000011866664,0.000052047457,0.0016955679,0.02155005],"study_design_scores_gemma":[0.00013638302,0.0004348305,0.9597688,0.000018179944,0.000015895654,0.00016476447,0.00024099788,0.0001759581,0.000015374808,0.0015678657,0.037388153,0.000072836],"about_ca_topic_score_codex":0.07503981,"about_ca_topic_score_gemma":0.7556957,"teacher_disagreement_score":0.6806559,"about_ca_system_score_codex":0.0000010719544,"about_ca_system_score_gemma":0.001630005,"threshold_uncertainty_score":0.9780227},"labels":[],"label_agreement":null},{"id":"W1991266475","doi":"10.1139/e05-021","title":"SHRIMP UPb geochronology of detrital zircons from the Treasure Lake Group new evidence for Paleoproterozoic collisional tectonics in the southern Hottah terrane, northwestern Canadian Shield","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Terrane; Geology; Zircon; Provenance; Geochemistry; Geochronology; Craton; Continental arc; Back-arc basin; Detritus; Basement; Laurentia; Metamorphism; Paleontology; Subduction; Tectonics; Ordovician; Archaeology","score_opus":0.04404226955892899,"score_gpt":0.22736134198043903,"score_spread":0.18331907242151005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991266475","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9842885,0.0039628,0.000037339123,0.010726938,0.00013467237,0.00017780269,0.00041959537,0.0000017233273,0.0002506407],"genre_scores_gemma":[0.9975611,0.00003031189,0.0008752849,0.0012120827,0.00026420451,0.0000010826512,0.000017946977,0.0000015087685,0.00003647409],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99829096,0.00012920021,0.00045038297,0.0002289654,0.00034986777,0.0005506077],"domain_scores_gemma":[0.99785525,0.0011097369,0.00021894992,0.00016198166,0.000088870234,0.00056523574],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011126307,0.00014512654,0.00026821578,0.00022023119,0.00037717575,0.00012920437,0.0011644905,0.00010112219,0.0032939953],"category_scores_gemma":[0.0004699939,0.00007451411,0.00016730641,0.00067981146,0.0006451878,0.00025334538,0.000006470499,0.00029659623,0.000024503106],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016796808,0.0000057435022,0.98682624,0.0000020005748,0.000016555807,0.000022283199,0.00091904105,0.0019500784,0.000022606815,0.00001414799,0.00011648162,0.010088018],"study_design_scores_gemma":[0.00027887203,0.00039499332,0.98832715,0.00007256935,0.000039591316,0.00006856135,0.0013738584,0.00078069844,0.000034000746,0.0019369344,0.0065601976,0.0001326005],"about_ca_topic_score_codex":0.8044438,"about_ca_topic_score_gemma":0.9998497,"teacher_disagreement_score":0.19540589,"about_ca_system_score_codex":0.0000047188446,"about_ca_system_score_gemma":0.0019960813,"threshold_uncertainty_score":0.9976171},"labels":[],"label_agreement":null},{"id":"W1991374367","doi":"10.1139/e03-095","title":"Postglacial emergence of Amund and Ellef Ringnes islands, Nunavut: implications for the northwest sector of the Innuitian Ice Sheet","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"University of Cambridge; University of Alberta","keywords":"Geology; Ice sheet; Oceanography; Bay; Holocene; Paleontology; Arctic ice pack; Arctic; Marine transgression; Geomorphology; Physical geography; Geography","score_opus":0.027591184794612384,"score_gpt":0.25028528068330946,"score_spread":0.22269409588869707,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991374367","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927698,0.0022583534,0.000023238674,0.003617749,0.00032772473,0.00013263928,0.00013590117,8.375054e-7,0.00073377136],"genre_scores_gemma":[0.9995367,0.00010189275,0.00018414218,0.00010120132,0.000051654137,5.0375377e-7,0.0000016916943,9.341524e-7,0.000021300082],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99918646,0.00005478938,0.0002548437,0.0001022854,0.00013152779,0.00027010086],"domain_scores_gemma":[0.99902254,0.00032363407,0.00019906482,0.000114850074,0.00017136989,0.00016851728],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007215644,0.000065620785,0.00013949336,0.00013032657,0.00069890067,0.000026230495,0.00058095244,0.000047043213,0.00026704452],"category_scores_gemma":[0.00020872714,0.000035927304,0.00006129852,0.00041309057,0.0016423394,0.00013950976,0.000007908432,0.00013465753,0.0000017561072],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007802541,0.0000027078804,0.9971203,0.000009300208,0.00001043691,0.0000013046438,0.00062280387,0.0014415077,0.000017379096,0.00057962973,0.000020074463,0.00016671889],"study_design_scores_gemma":[0.00014869767,0.00018615005,0.9962451,0.000021996742,0.000014793306,0.00014594702,0.0006172824,0.00010796654,0.00010513459,0.0020784996,0.0002856903,0.000042729032],"about_ca_topic_score_codex":0.010952901,"about_ca_topic_score_gemma":0.86557025,"teacher_disagreement_score":0.85461736,"about_ca_system_score_codex":2.905541e-7,"about_ca_system_score_gemma":0.0012709277,"threshold_uncertainty_score":0.99563324},"labels":[],"label_agreement":null},{"id":"W1991421827","doi":"10.1139/e04-076","title":"Depositional and tectonic setting of the Miocene Wood Mountain Formation, southern Saskatchewan","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Brandon University; Geological Survey of Canada; Nexen (Canada)","funders":"","keywords":"Geology; Aggradation; Tectonic uplift; Sedimentary depositional environment; Geomorphology; Tectonics; Erosion; Geochemistry; Subaerial; Deposition (geology); Sinuosity; Paleontology; Fluvial; Sediment; Structural basin","score_opus":0.009806973223368775,"score_gpt":0.18486696504479372,"score_spread":0.17505999182142495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991421827","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99636465,0.0008889608,0.00013010888,0.0017230676,0.00008165073,0.000038387534,0.000034694862,0.0000014143437,0.00073704525],"genre_scores_gemma":[0.99828327,0.000007854649,0.001486535,0.00017983731,0.000026507436,7.321182e-8,0.0000015367564,5.075304e-7,0.000013888094],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999342,0.000027175227,0.00022157429,0.00005326584,0.0001846746,0.00017130325],"domain_scores_gemma":[0.9994747,0.000045930927,0.00018071155,0.0000384937,0.00009665369,0.00016349867],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046849804,0.000051418534,0.00008014109,0.00010124822,0.00047421164,0.00007962558,0.00021703586,0.000025838184,0.00027122715],"category_scores_gemma":[0.00007506817,0.000029169754,0.000033449553,0.0003484514,0.0003044035,0.00038034303,0.0000034828806,0.00008541895,0.0000060159696],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000033562876,0.0000033359538,0.96622425,0.000018449282,0.0000067100377,0.0000034122625,0.0031192317,0.025812967,0.000042647112,0.00029556768,0.000010412851,0.0044596586],"study_design_scores_gemma":[0.00018434836,0.00017897105,0.9801037,0.000078530175,0.000009230033,0.00039757445,0.006221007,0.0005165063,0.0005734884,0.011401327,0.00025904574,0.000076323005],"about_ca_topic_score_codex":0.011962828,"about_ca_topic_score_gemma":0.46125516,"teacher_disagreement_score":0.44929233,"about_ca_system_score_codex":0.0000014446546,"about_ca_system_score_gemma":0.0009407516,"threshold_uncertainty_score":0.99461657},"labels":[],"label_agreement":null},{"id":"W1991472340","doi":"10.1139/e02-022","title":"Review of crustal architecture and evolution in the Ungava Peninsula — Baffin Island area: connection to the Lithoprobe ECSOOT transect","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Nunavut Research Institute; Government of Nunavut; Geological Survey of Canada","funders":"","keywords":"Geology; Terrane; Archean; Transect; Basement; Bay; Paleontology; Peninsula; Metamorphic rock; Submarine pipeline; Tectonics; Oceanography; Archaeology; Geography","score_opus":0.01895412521584988,"score_gpt":0.19236218491385085,"score_spread":0.17340805969800097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991472340","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.944183,0.03744366,0.00005769576,0.01606337,0.000069470705,0.000115541116,0.000024366753,0.0000010058573,0.0020419233],"genre_scores_gemma":[0.99775404,0.00090627326,0.00010732035,0.0011663391,0.00004691099,2.8314983e-7,0.0000012799934,4.269598e-7,0.000017143102],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99906224,0.00015232427,0.0002462419,0.00011449737,0.00021494912,0.00020976957],"domain_scores_gemma":[0.99942255,0.00017103135,0.00009848598,0.000066606946,0.00005888562,0.00018246927],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011169093,0.000072325376,0.00016297647,0.00013864771,0.00019752912,0.00004735204,0.00030321666,0.000026149497,0.0019628187],"category_scores_gemma":[0.0003060682,0.00003194764,0.000068687055,0.0008584215,0.0002823214,0.000088147564,0.0000025526126,0.000179912,0.000005926957],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018877909,0.000020558498,0.9542784,0.00015711981,0.000021432954,0.00004994229,0.0018408357,0.012002111,0.00006994163,0.00019298095,0.001505934,0.029841842],"study_design_scores_gemma":[0.00015159589,0.0004648653,0.9842325,0.0005195893,0.000036101515,0.0003384264,0.00054765056,0.0027922546,0.000023017767,0.0023723114,0.00841367,0.000108036744],"about_ca_topic_score_codex":0.016926598,"about_ca_topic_score_gemma":0.685653,"teacher_disagreement_score":0.6687264,"about_ca_system_score_codex":0.0000010948061,"about_ca_system_score_gemma":0.000089742316,"threshold_uncertainty_score":0.9989495},"labels":[],"label_agreement":null},{"id":"W1991657621","doi":"10.1139/e09-032","title":"High-resolution isotope stratigraphy of the Lower Ordovician St. George Group of western Newfoundland, Canada: implications for global correlation","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Memorial University of Newfoundland","funders":"","keywords":"Unconformity; Geology; Ordovician; Outcrop; Paleontology; Stratigraphy; Group (periodic table); Sedimentary depositional environment; Sedimentary rock; Tectonics; Structural basin","score_opus":0.015165129851842417,"score_gpt":0.22015507696551223,"score_spread":0.2049899471136698,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991657621","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98857903,0.002080711,0.00070069614,0.002113353,0.00081114494,0.00019006053,0.00057766464,0.000001770242,0.004945568],"genre_scores_gemma":[0.999128,0.000009539148,0.0006715994,0.00012283624,0.0000512967,2.1160787e-7,0.0000044184867,3.206012e-7,0.000011765053],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895304,0.00005767629,0.00039709033,0.00011625955,0.00020493097,0.00027098125],"domain_scores_gemma":[0.9989705,0.00008597429,0.0004395522,0.000113023,0.00015650131,0.00023441682],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039707017,0.0000885721,0.0001853108,0.000111764166,0.00040509723,0.00003389667,0.00043145602,0.00005940985,0.000044574525],"category_scores_gemma":[0.000061110855,0.00006124405,0.000106032254,0.00052300986,0.0004270157,0.0002809602,5.424605e-7,0.0000923019,1.3748691e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000135558685,0.0000070557776,0.9843218,0.0000027816259,0.00001094483,0.0000011404597,0.00002730686,0.0013382416,0.00001519984,0.005483528,0.0000920989,0.008686343],"study_design_scores_gemma":[0.000173093,0.00054488424,0.9924351,0.000029628667,0.000020962047,0.000025763138,0.000059494665,0.00022131168,0.0000059665767,0.005937957,0.0004799837,0.000065880515],"about_ca_topic_score_codex":0.5701872,"about_ca_topic_score_gemma":0.9994462,"teacher_disagreement_score":0.42925897,"about_ca_system_score_codex":0.0000041813755,"about_ca_system_score_gemma":0.0023759934,"threshold_uncertainty_score":0.43267494},"labels":[],"label_agreement":null},{"id":"W1991835812","doi":"10.1139/e00-063","title":"A synthesis of electromagnetic studies in the Lithoprobe Alberta Basement Transect: constraints on Paleoproterozoic indentation tectonics","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Geological Survey of Canada","funders":"","keywords":"Geology; Foreland basin; Laurentia; Crust; Proterozoic; Tectonics; Lithosphere; Paleontology; Geophysics","score_opus":0.030775592855664672,"score_gpt":0.25940661118616365,"score_spread":0.22863101833049898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991835812","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99265885,0.0007507727,0.0000053383706,0.0009358668,0.00008217036,0.00013370675,0.0000074374534,8.8078394e-7,0.005424964],"genre_scores_gemma":[0.9988889,0.000087144035,0.0006593166,0.00029216023,0.000036043293,0.0000011856115,3.7632338e-7,9.301124e-7,0.000033958764],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9985395,0.00031065292,0.00033238574,0.00013431477,0.00035114493,0.00033199036],"domain_scores_gemma":[0.9986583,0.00093811844,0.00011351929,0.0000739258,0.00005011401,0.00016600562],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012429669,0.00009653408,0.0002111157,0.00022451059,0.000158681,0.000046254132,0.00034930976,0.00003077738,0.002053692],"category_scores_gemma":[0.0003409215,0.00005572596,0.00007238306,0.0008399611,0.0006240572,0.00011980238,6.798409e-7,0.00018570769,0.000015971591],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005686177,0.00004212239,0.06594906,0.000032036165,0.00003154362,0.00007979459,0.0024111054,0.0027177944,0.00009490655,0.00024986704,0.000025894064,0.928309],"study_design_scores_gemma":[0.00022872267,0.0026014785,0.9908372,0.0001523277,0.000026422991,0.000094250514,0.00081721134,0.0005846621,0.001293973,0.0029180073,0.00032102453,0.00012469031],"about_ca_topic_score_codex":0.015263133,"about_ca_topic_score_gemma":0.28426048,"teacher_disagreement_score":0.92818433,"about_ca_system_score_codex":0.0000021601659,"about_ca_system_score_gemma":0.00041329814,"threshold_uncertainty_score":0.9988586},"labels":[],"label_agreement":null},{"id":"W1991951719","doi":"10.1139/e06-005","title":"ArAr and UPb ages of marble-hosted ruby deposits from central and southeast Asia","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Institut national des sciences de l'Univers; Centre National de la Recherche Scientifique","keywords":"Geology; Zircon; Metamorphism; Metamorphic rock; Geochemistry; Radiometric dating; Shear zone; Paleontology; Tectonics","score_opus":0.00843207880714506,"score_gpt":0.16090976042232882,"score_spread":0.15247768161518377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991951719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912878,0.0043941927,0.000009363272,0.0006728098,0.000072467585,0.000024966954,0.00006441566,0.0000017708762,0.0034721775],"genre_scores_gemma":[0.99899226,0.00004300387,0.00079783093,0.000053548625,0.0000723558,2.9339581e-8,0.000006179646,6.25286e-7,0.000034162706],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990795,0.000043241063,0.00025140832,0.0001423959,0.00018638284,0.00029701993],"domain_scores_gemma":[0.99918944,0.00009815976,0.0001435028,0.0000433684,0.000050619525,0.00047492285],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021223466,0.000084964966,0.00019829784,0.00012868243,0.00017779678,0.00009196582,0.0001748555,0.000045192537,0.0010510387],"category_scores_gemma":[0.000055205437,0.000055471213,0.000048318565,0.00027050028,0.00061317213,0.00016843923,0.0000050608674,0.00010020177,0.0000033815152],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000054191805,0.0000025784227,0.9968517,0.0000024122173,0.000008832135,0.00003563503,0.00003848472,0.0004894788,0.00016922604,0.000087350316,0.000024194798,0.0022847333],"study_design_scores_gemma":[0.000114570794,0.00011578104,0.99282336,0.000023459366,0.000019736157,0.000047153222,0.00022498508,0.0008497916,0.00045503693,0.0050052567,0.00024539043,0.00007550284],"about_ca_topic_score_codex":0.09784918,"about_ca_topic_score_gemma":0.50876904,"teacher_disagreement_score":0.41091985,"about_ca_system_score_codex":4.5488113e-7,"about_ca_system_score_gemma":0.00014031556,"threshold_uncertainty_score":0.99986213},"labels":[],"label_agreement":null},{"id":"W1992082284","doi":"10.1139/e04-008","title":"Conodont zonation across the PermianTriassic boundary at the Xiakou section, Yichang city, Hubei Province and its correlation with the Global Stratotype Section and Point of the PTB","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"China University of Geosciences","keywords":"Global Boundary Stratotype Section and Point; Conodont; Stratotype; Geology; Paleontology; Permian; Section (typography); Biostratigraphy; Stage (stratigraphy)","score_opus":0.013932957530864399,"score_gpt":0.21604974769383214,"score_spread":0.20211679016296774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992082284","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9839163,0.0062237745,0.000049134014,0.0073765893,0.0005340459,0.00018602732,0.000039063958,0.0000019900253,0.0016731148],"genre_scores_gemma":[0.9996638,0.000044995737,0.000016721655,0.00013914256,0.00009789107,3.2789163e-7,4.912456e-7,4.6185022e-7,0.00003619131],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910325,0.00013530873,0.0001765149,0.000120866964,0.00025349285,0.00021055553],"domain_scores_gemma":[0.99931127,0.00011503929,0.00027224646,0.000077473116,0.0001082219,0.00011574215],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0011573195,0.00008423651,0.00009354966,0.00003439353,0.0023682937,0.00020285042,0.00024399116,0.000052148564,0.000027486187],"category_scores_gemma":[0.0000637956,0.000033746277,0.00003678147,0.00035645385,0.0016023144,0.0004152618,0.0000031353404,0.00020424652,4.514233e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037399048,0.0000023583982,0.98874825,0.0000044890444,0.000020294456,0.0000054598218,0.00187394,0.0025737074,0.000016122478,0.00046682326,0.00003959684,0.0062115695],"study_design_scores_gemma":[0.00020476567,0.00027970172,0.995582,0.000029609011,0.000018895404,0.00062208436,0.0013901703,0.000519377,0.000047910933,0.00080155063,0.0004536049,0.000050362723],"about_ca_topic_score_codex":0.009092663,"about_ca_topic_score_gemma":0.91480166,"teacher_disagreement_score":0.90570897,"about_ca_system_score_codex":0.0000066615976,"about_ca_system_score_gemma":0.0010952024,"threshold_uncertainty_score":0.9989305},"labels":[],"label_agreement":null},{"id":"W1992163728","doi":"10.1139/e05-085","title":"The brachymetopid trilobite <i>Radnoria</i> in the Silurian (Wenlock) of New York State and Arctic Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor","funders":"","keywords":"Trilobite; Geology; Paleontology; Genus; Arctic; Devonian; Cape; Archaeology; Oceanography; Geography; Ordovician; Zoology; Biology","score_opus":0.018427799427903825,"score_gpt":0.20109900596134858,"score_spread":0.18267120653344476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992163728","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95739955,0.027198602,0.0000026801006,0.007138175,0.0004922077,0.00007385967,0.000019259112,6.172917e-7,0.007675082],"genre_scores_gemma":[0.9991485,0.00011796519,0.0002101884,0.00030033378,0.00013392957,7.722735e-8,2.0340634e-7,3.5459757e-7,0.000088449386],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987501,0.0001458231,0.0003429457,0.000105055864,0.00028823403,0.00036786712],"domain_scores_gemma":[0.99885166,0.00043880794,0.00021581232,0.000095669304,0.000036003592,0.0003620243],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013865555,0.000086935215,0.00015483168,0.00012870682,0.0004987896,0.00011975008,0.000556332,0.000028072094,0.00007575729],"category_scores_gemma":[0.00013330017,0.000046359146,0.000041695588,0.00044379683,0.0006382331,0.0002351158,6.9082614e-7,0.00021223574,9.1930417e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012988348,0.0000015289393,0.8899433,0.000003145094,0.000009232662,0.000025310293,0.00092425616,0.00052761263,0.000001992164,0.00015449541,0.0009177965,0.10747836],"study_design_scores_gemma":[0.00017180956,0.00015234626,0.97709244,0.000023293054,0.0000065026284,0.00014700575,0.00084340875,0.0001392513,0.000016067195,0.0007600956,0.02058562,0.00006214013],"about_ca_topic_score_codex":0.831194,"about_ca_topic_score_gemma":0.99966836,"teacher_disagreement_score":0.16847433,"about_ca_system_score_codex":0.00000181968,"about_ca_system_score_gemma":0.0038284853,"threshold_uncertainty_score":0.67915684},"labels":[],"label_agreement":null},{"id":"W1992216010","doi":"10.1139/e10-096","title":"Description of fossil muskoxen and relative abundance of Pleistocene megafauna in central Alberta","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Manitoba; Royal Alberta Museum","funders":"","keywords":"Megafauna; Pleistocene; Fauna; Mammoth; Equus; Geology; Glacial period; Ecology; Beringia; Paleontology; Quaternary; Last Glacial Maximum; Relative species abundance; Paleoecology; Abundance (ecology); Stadial; Geography; Archaeology; Biology","score_opus":0.0482031694867689,"score_gpt":0.2265611367711934,"score_spread":0.17835796728442452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992216010","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98716235,0.0020920977,0.000010807236,0.00014200038,0.00017290698,0.000052074443,0.000008070327,4.4802596e-7,0.010359263],"genre_scores_gemma":[0.9989171,0.00005903745,0.00090697524,0.000017590359,0.000010323155,8.100207e-8,6.184554e-7,6.655301e-7,0.00008761016],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898577,0.00013135966,0.0003103027,0.000108305045,0.00013806671,0.00032621354],"domain_scores_gemma":[0.99919236,0.00018000824,0.0002119378,0.000056875597,0.00008068456,0.0002781421],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008453223,0.00006272049,0.00020237773,0.00035754443,0.00011217571,0.000010321334,0.00024756545,0.00007076463,0.0007677855],"category_scores_gemma":[0.00024597824,0.000049217062,0.00003274424,0.00035191345,0.001472713,0.0004197005,0.000003611177,0.00018292546,0.0000038505254],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031792442,0.0000041302083,0.9967679,0.000009073569,0.00000687185,0.000026319529,0.002190738,0.000089880385,0.000007645209,0.00046272334,0.000005326692,0.00039760015],"study_design_scores_gemma":[0.00017879854,0.00041913113,0.9958222,0.000052069718,0.0000053822196,0.00010989657,0.00043873332,0.0003173407,0.00015476886,0.0023946853,0.00005919216,0.00004782384],"about_ca_topic_score_codex":0.08242341,"about_ca_topic_score_gemma":0.90827525,"teacher_disagreement_score":0.8258518,"about_ca_system_score_codex":5.1535136e-7,"about_ca_system_score_gemma":0.0007364672,"threshold_uncertainty_score":0.9236868},"labels":[],"label_agreement":null},{"id":"W1992453184","doi":"10.1139/e03-062","title":"Petrography and genesis of spicular and columnar geyserite from the Whakarewarewa and Orakeikorako geothermal areas, North Island, New Zealand","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Mineralogy and Gemology Studies","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Sponge spicule; Spicule; Petrography; Geology; Shrub; Diagenesis; Microbial mat; Paleontology; Geochemistry; Mineralogy; Botany; Biology","score_opus":0.011746321620525727,"score_gpt":0.17973958633453013,"score_spread":0.16799326471400441,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992453184","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9724851,0.02610793,0.000005744012,0.0008454608,0.00016317477,0.000054737873,0.00007581464,0.0000012356669,0.00026075303],"genre_scores_gemma":[0.9980289,0.0008872397,0.000549172,0.0003463856,0.000065234075,1.0459253e-7,0.0000023254684,0.0000014775933,0.00011918573],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99913365,0.00010457837,0.0002063362,0.00016228134,0.00013314553,0.00026000632],"domain_scores_gemma":[0.9991974,0.00016247491,0.00014358916,0.000070902985,0.000050736675,0.00037485565],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043761058,0.00010856227,0.00021947904,0.00012660476,0.00044659185,0.000087807086,0.00014882906,0.000045229066,0.00029843042],"category_scores_gemma":[0.000087410575,0.00006835351,0.00003420604,0.00024325303,0.0012321338,0.00020073791,0.000005158942,0.00010662335,0.0000011464226],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008178479,0.0000010977669,0.9962672,0.000002355306,0.00003491298,0.000033598713,0.0008805355,0.000064959226,0.0000036595147,0.000016891476,0.0006683185,0.00201829],"study_design_scores_gemma":[0.00024837162,0.00023260094,0.9871163,0.000019330102,0.000034784127,0.0001961682,0.0008684479,0.000028112468,0.000007611003,0.0006069341,0.010556779,0.00008457396],"about_ca_topic_score_codex":0.08024683,"about_ca_topic_score_gemma":0.840796,"teacher_disagreement_score":0.7605492,"about_ca_system_score_codex":3.6112547e-7,"about_ca_system_score_gemma":0.00030658118,"threshold_uncertainty_score":0.92587787},"labels":[],"label_agreement":null},{"id":"W1992719424","doi":"10.1139/e10-087","title":"Late Holocene glacial activity in Manatee Valley, southern Coast Mountains, British Columbia, Canada","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Glacier; Moraine; Geology; Tidewater glacier cycle; Ice field; Holocene; Glacial period; Physical geography; Terminal moraine; Glacier morphology; Rock glacier; Cirque glacier; Oceanography; Geomorphology; Geography; Ice stream; Cryosphere; Ice calving; Sea ice","score_opus":0.023880855209271856,"score_gpt":0.2050839349399766,"score_spread":0.18120307973070474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992719424","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921481,0.000491179,0.0000014586001,0.00024304472,0.00051122735,0.00007001154,0.000073415365,0.0000026110667,0.0064589605],"genre_scores_gemma":[0.9990305,0.00003528711,0.00011880473,0.00021607053,0.00004972956,2.2202371e-7,0.0000026042587,0.0000019579122,0.0005448524],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99830997,0.00020230276,0.0002659262,0.00020235436,0.00029815896,0.0007212636],"domain_scores_gemma":[0.9989588,0.00008881551,0.0001463643,0.00008651082,0.00009783467,0.0006216524],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011767906,0.00008678691,0.00023963556,0.000182406,0.0005136378,0.0001561178,0.0005799959,0.000098340686,0.0043075564],"category_scores_gemma":[0.000118687276,0.00010301679,0.000045360935,0.0004487756,0.0007927526,0.00028833598,0.000008038167,0.00039833828,0.00003223648],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011626527,0.0000048850893,0.996391,0.0000041776048,0.000007880023,0.0016029378,0.00027639067,0.00014037678,4.1772478e-7,0.0000024558003,0.00016843992,0.0013894093],"study_design_scores_gemma":[0.00023461865,0.00015631136,0.99738103,0.00002479965,0.000004565564,0.0004905896,0.0006030813,0.00019305311,0.0000051652673,0.0003984227,0.00039020917,0.00011815386],"about_ca_topic_score_codex":0.9975059,"about_ca_topic_score_gemma":0.99999785,"teacher_disagreement_score":0.0068823793,"about_ca_system_score_codex":0.0000024764656,"about_ca_system_score_gemma":0.0055144615,"threshold_uncertainty_score":0.99660265},"labels":[],"label_agreement":null},{"id":"W1992755854","doi":"10.1139/e02-068","title":"The first 20 years (1978-1979 to 1998-1999) of active-layer development, Illisarvik experimental drained lake site, western Arctic coast, Canada<sup>1</sup>","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University; University of British Columbia","funders":"Natural Resources Canada","keywords":"Permafrost; Active layer; Geology; Aggradation; Tundra; Vegetation (pathology); Snow; Frost heaving; Hydrology (agriculture); Geomorphology; Arctic; Snowmelt; Oceanography; Structural basin; Geotechnical engineering; Layer (electronics)","score_opus":0.04375401778461924,"score_gpt":0.2269750107857235,"score_spread":0.18322099300110425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992755854","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99429137,0.001253794,9.4566457e-7,0.0016833859,0.000483056,0.00012294443,0.0007067834,0.0000027401131,0.0014549949],"genre_scores_gemma":[0.99800783,0.000040427538,0.000098204466,0.0011341093,0.00017745423,7.5174984e-7,0.000027940208,0.00000419477,0.0005090947],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981303,0.000043717373,0.000422456,0.00020820586,0.00056101236,0.0006343165],"domain_scores_gemma":[0.9985373,0.00018646162,0.00020842293,0.00014254428,0.00008886428,0.0008363914],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00043696686,0.00016824044,0.00023682216,0.0002269514,0.0007858933,0.00020410429,0.0006419774,0.000045403052,0.0033797896],"category_scores_gemma":[0.000057725403,0.00012295117,0.00006549687,0.0005259773,0.0003723607,0.00035285024,0.00001570143,0.00016735149,0.00009205213],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021619167,0.000010516117,0.97720397,0.000008989194,0.000030070209,0.00014331653,0.0097534275,0.0021753204,0.000058753933,0.0000031757243,0.007222603,0.0033682615],"study_design_scores_gemma":[0.00022605479,0.00021437557,0.5164437,0.00006810039,0.000008222601,0.00011276053,0.0029947553,0.0005541242,0.0002940784,0.0000039345987,0.47888914,0.00019075195],"about_ca_topic_score_codex":0.5931392,"about_ca_topic_score_gemma":0.99957854,"teacher_disagreement_score":0.47166654,"about_ca_system_score_codex":0.0000162231,"about_ca_system_score_gemma":0.0013332017,"threshold_uncertainty_score":0.99753124},"labels":[],"label_agreement":null},{"id":"W1992776306","doi":"10.1139/e00-001","title":"Skeletal remains of a small theropod dinosaur with associated soft structures from the Lower Cretaceous Santana Formation of northeastern Brazil","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Royal Ontario Museum","funders":"","keywords":"Cretaceous; Pelvic girdle; Geology; Paleontology; Lithification; Anatomy; Sacrum; Sedimentary rock; Medicine","score_opus":0.012149954717405223,"score_gpt":0.1963905663440715,"score_spread":0.18424061162666627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992776306","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947006,0.0020547302,0.000045536224,0.00045492308,0.00016895482,0.00005823403,0.00018517331,0.000002049727,0.0023297842],"genre_scores_gemma":[0.99948454,0.000031266078,0.00021993788,0.00015955066,0.000056327328,6.426121e-8,0.0000132113255,0.0000010843524,0.000034018663],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989494,0.00015852593,0.00031605267,0.00010470719,0.00020012859,0.00027114814],"domain_scores_gemma":[0.99909794,0.00021013863,0.0003357715,0.00008986191,0.000098686396,0.00016760673],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042347616,0.000093148585,0.00020567428,0.000093783354,0.00028642153,0.000021675625,0.0004157505,0.00007180595,0.0018828213],"category_scores_gemma":[0.000073358235,0.00005098769,0.00006640292,0.0002579484,0.0010611286,0.00025121993,0.0000015486785,0.00014886081,0.000007058391],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005238802,0.000006140299,0.98960286,0.0000020298512,0.00003294819,0.000031593878,0.00055153243,0.003773971,0.000019207526,0.000016542408,0.000036590984,0.00587422],"study_design_scores_gemma":[0.0002010315,0.0007357231,0.9955664,0.000040129078,0.00002316114,0.00018044752,0.00036852466,0.0016373664,0.000024874718,0.0005708065,0.0005825604,0.00006892483],"about_ca_topic_score_codex":0.01866607,"about_ca_topic_score_gemma":0.9030823,"teacher_disagreement_score":0.8844163,"about_ca_system_score_codex":0.0000018471044,"about_ca_system_score_gemma":0.00066328933,"threshold_uncertainty_score":0.9990296},"labels":[],"label_agreement":null},{"id":"W1992903217","doi":"10.1139/e07-042","title":"A Late Triassic flora from east-central Axel Heiberg Island, Nunavut, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature; McGill University","funders":"","keywords":"Flora (microbiology); Dominance (genetics); Geology; Paleontology; Ecology; Biology","score_opus":0.022113677347406747,"score_gpt":0.17528757893721467,"score_spread":0.15317390158980793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992903217","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955452,0.00042230962,0.000008163472,0.0017189208,0.0009615375,0.00003665265,0.00021296511,0.0000031543796,0.001091099],"genre_scores_gemma":[0.99879795,0.000016645146,0.000075216514,0.0004076392,0.0004560536,6.0117216e-8,0.000010567792,2.8072162e-7,0.00023556802],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99876183,0.000036273523,0.00021992548,0.00013411896,0.000319216,0.0005286393],"domain_scores_gemma":[0.9989018,0.00010809038,0.00014818925,0.000023051884,0.00007364095,0.00074522826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005356341,0.00008784557,0.00014300624,0.000041247946,0.0005173832,0.0001046416,0.00039322439,0.00005279479,0.0006972678],"category_scores_gemma":[0.00006344447,0.000037943802,0.000066519475,0.00039573686,0.0001522629,0.00028867277,0.000010508961,0.00014183618,0.000011573549],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011327871,0.000027254639,0.95048845,0.000002919499,0.000050410727,0.0013310498,0.0006968205,0.0005264322,0.008567158,0.00018994717,0.018042793,0.019963477],"study_design_scores_gemma":[0.0001849997,0.00014127525,0.9464431,0.00003376552,0.000011701294,0.000059401365,0.0009532957,0.00012050064,0.00022095622,0.000283145,0.051411815,0.00013605827],"about_ca_topic_score_codex":0.7981343,"about_ca_topic_score_gemma":0.99966997,"teacher_disagreement_score":0.20153569,"about_ca_system_score_codex":0.00003073676,"about_ca_system_score_gemma":0.00094682444,"threshold_uncertainty_score":0.7634594},"labels":[],"label_agreement":null},{"id":"W1993159287","doi":"10.1139/e06-041","title":"Stratigraphy, structure, and geochronology of the 3.02.7 Ga Wallace Lake greenstone belt, western Superior Province, southeast Manitoba, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; McGill University","funders":"Goldcorp","keywords":"Geology; Terrane; Mafic; Rift; Paleontology; Geochemistry; Volcano; Tectonics","score_opus":0.007346216478484237,"score_gpt":0.1563912707726696,"score_spread":0.14904505429418535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993159287","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956459,0.0012519258,0.0000018171398,0.0015036921,0.00017613465,0.00005978179,0.00023781232,0.0000015293293,0.0011214142],"genre_scores_gemma":[0.9994963,0.0000067431165,0.00014915572,0.00015775168,0.00008262785,6.6306704e-8,0.0000054508237,9.651108e-7,0.00010096043],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99874145,0.00006439379,0.00033105092,0.00017171113,0.00031254083,0.00037886246],"domain_scores_gemma":[0.9992122,0.000064634965,0.00020949138,0.00010002616,0.000099387595,0.00031424983],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019774791,0.00012256533,0.00024764333,0.00011658292,0.00031300934,0.00006283061,0.00045819927,0.000051401596,0.0013275964],"category_scores_gemma":[0.000038801187,0.00006865409,0.00007181965,0.0004040228,0.00092782336,0.0001301338,0.000009648721,0.00017457905,0.0000012082936],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000035372257,0.0000019336971,0.997636,0.0000055004207,0.000010205687,0.000026667105,0.000014337243,0.0009585947,0.00007051088,0.000062520594,0.00007019161,0.0011399607],"study_design_scores_gemma":[0.00010207283,0.00011708235,0.99570394,0.000016128703,0.000022367125,0.00014093096,0.00019791,0.00015091742,0.0002143436,0.0021606812,0.0010796451,0.000094011775],"about_ca_topic_score_codex":0.9678535,"about_ca_topic_score_gemma":0.9999878,"teacher_disagreement_score":0.03213432,"about_ca_system_score_codex":0.0000023099385,"about_ca_system_score_gemma":0.0017914388,"threshold_uncertainty_score":0.99958533},"labels":[],"label_agreement":null},{"id":"W1993288433","doi":"10.1139/e08-018","title":"Évolution morphostructurale du plateau volcano-sédimentaire de Gergovie au Miocène inférieur : implications géodynamiques sur la phase tardi-tectonique du rift de Limagne (Massif central, France)","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Maar; Rift; Volcanic plateau; Massif; Volcano; Lava; Paleontology; Foreland basin; Geomorphology; Cinder cone; Lava field; Tectonics","score_opus":0.011153999092532094,"score_gpt":0.20433864256422332,"score_spread":0.19318464347169123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993288433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927148,0.0015243411,0.00019952205,0.003450179,0.00016675066,0.00007427913,0.000101893325,0.000013693645,0.0017545384],"genre_scores_gemma":[0.9973031,0.00034823065,0.0014541207,0.0005034976,0.00027600286,9.2885386e-7,0.000024105208,0.000002611513,0.0000873864],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99814296,0.00015164462,0.00039010812,0.00022275324,0.00024452127,0.00084803114],"domain_scores_gemma":[0.9980024,0.0001954342,0.00023877977,0.00011319603,0.00015217338,0.0012980226],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000618829,0.00017551737,0.00027156444,0.00020954502,0.00087025616,0.00009455417,0.00046309474,0.00009663036,0.002810682],"category_scores_gemma":[0.0003321905,0.00013038823,0.00017852511,0.0006379009,0.0011173082,0.00058100227,0.000008979693,0.00026858045,0.000018534785],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010786411,0.000019670204,0.9928671,0.000004676029,0.000020709209,0.00010738731,0.00034563392,0.003210356,0.0008713326,0.00005085118,0.0004994902,0.0019920096],"study_design_scores_gemma":[0.00028672998,0.00023253105,0.9844356,0.000020535526,0.000033326753,0.0010566885,0.000080177975,0.0035733338,0.0010311,0.0010204369,0.008047321,0.00018222151],"about_ca_topic_score_codex":0.15695925,"about_ca_topic_score_gemma":0.31180483,"teacher_disagreement_score":0.1548456,"about_ca_system_score_codex":0.000021805658,"about_ca_system_score_gemma":0.002288374,"threshold_uncertainty_score":0.9981009},"labels":[],"label_agreement":null},{"id":"W1993307104","doi":"10.1139/e06-083","title":"Tectonic histories of the Paleo- to Mesoarchean Sacawee block and Neoarchean Oregon Trail structural belt of the south-central Wyoming Province","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Washington State University; U.S. Geological Survey; Geological Society of America; National Science Foundation","keywords":"Geology; Shear zone; Zircon; Crust; Basement; Geochemistry; Archean; Tectonics; Craton; Shear (geology); Felsic; Greenschist; Seismology; Metamorphic rock; Petrology; Archaeology","score_opus":0.010267078084051664,"score_gpt":0.17222789445096928,"score_spread":0.16196081636691761,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993307104","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953183,0.0008453979,0.00000198096,0.0029938996,0.0001723504,0.000078240344,0.000035851586,0.0000013553185,0.00055265793],"genre_scores_gemma":[0.99938214,0.000001751842,0.00035460264,0.000093099035,0.00006520357,8.0668705e-8,5.1402554e-7,9.4123163e-7,0.000101688136],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986653,0.000084471314,0.0003479485,0.00014973599,0.0003609547,0.00039159603],"domain_scores_gemma":[0.99914396,0.00009008454,0.00025816262,0.00011161172,0.000087880115,0.00030832345],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041174292,0.000103122424,0.00021604747,0.00009799073,0.00037903598,0.00004303157,0.0006247099,0.000037771093,0.0003896618],"category_scores_gemma":[0.00018905856,0.00004887017,0.00013288771,0.00057155185,0.001552129,0.00010333373,0.000017514936,0.00018320545,6.314614e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007253613,0.0000018283101,0.9935527,0.000008340488,0.00000690235,0.0000032244827,0.0005943479,0.00400919,0.0004914604,0.00016195925,0.000031006486,0.0011318205],"study_design_scores_gemma":[0.00009410238,0.00014120144,0.9938467,0.0000290429,0.000025962187,0.000041557578,0.00044297968,0.00047346513,0.002077982,0.00203203,0.0007154772,0.00007949408],"about_ca_topic_score_codex":0.025225537,"about_ca_topic_score_gemma":0.6837057,"teacher_disagreement_score":0.6584801,"about_ca_system_score_codex":0.0000036141282,"about_ca_system_score_gemma":0.0007963772,"threshold_uncertainty_score":0.98126554},"labels":[],"label_agreement":null},{"id":"W1993370498","doi":"10.1139/e00-122","title":"New UPb age constraints on latest Cretaceous magmatism and associated mineralization in the Fawnie Range, Nechako Plateau, central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of British Columbia; Ministry of Energy, Northern Development and Mines; University of British Columbia","funders":"","keywords":"Geology; Magmatism; Cretaceous; Geochemistry; Igneous rock; Rhyolite; Pluton; Diorite; Felsic; Mineralization (soil science); Volcanic rock; Continental arc; Paleontology; Mafic; Zircon; Volcano; Tectonics","score_opus":0.013555131634511046,"score_gpt":0.18380529305272378,"score_spread":0.17025016141821273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993370498","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930594,0.0006955749,0.00001118906,0.0016337949,0.00011499767,0.0000633038,0.000029527515,0.000002968258,0.0043892204],"genre_scores_gemma":[0.9985335,0.00012361034,0.00015320092,0.00078755734,0.000054306453,8.797548e-8,0.0000126058385,8.5552085e-7,0.00033428505],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988208,0.00010270095,0.0002583907,0.00014582262,0.0002666315,0.00040568988],"domain_scores_gemma":[0.9991847,0.00014915745,0.00012646883,0.00004448576,0.000040562998,0.0004546045],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005601105,0.00007393768,0.00017882408,0.00008995366,0.00027640018,0.0006114618,0.00027224014,0.000059818707,0.007665642],"category_scores_gemma":[0.00029748163,0.00006111541,0.000050992232,0.00061244704,0.00040632903,0.00018141455,0.0000026692246,0.00017903323,0.000010307026],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001912371,0.0000042971055,0.9776466,0.0000010125364,0.00000646053,0.0007016791,0.00014631054,0.0011664161,0.0000040234736,0.000012020181,0.0011501975,0.019159092],"study_design_scores_gemma":[0.00023982958,0.0001747638,0.9923801,0.000045278975,0.000011561787,0.0003177522,0.00016890564,0.0011663246,9.104188e-7,0.0039548236,0.0014523172,0.00008746791],"about_ca_topic_score_codex":0.42594984,"about_ca_topic_score_gemma":0.9923691,"teacher_disagreement_score":0.56641924,"about_ca_system_score_codex":0.0000021511125,"about_ca_system_score_gemma":0.00024328846,"threshold_uncertainty_score":0.9932415},"labels":[],"label_agreement":null},{"id":"W1993725989","doi":"10.1139/e01-043","title":"The structure of the northeastern Gulf of St. Lawrence, Canada: new insight from geophysical data analysis","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography","funders":"","keywords":"Geology; Ordovician; Basement; Laurentia; Paleontology; Crust; Orogeny; Foreland basin; Magnetic anomaly; Sedimentary rock; Gravity anomaly; Geophysics; Seismology; Structural basin","score_opus":0.022856325241275156,"score_gpt":0.2007653040808801,"score_spread":0.17790897883960496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993725989","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99538463,0.0013932922,0.00004497446,0.0013496241,0.0002989025,0.000033993183,0.0006284031,5.9555384e-7,0.00086558465],"genre_scores_gemma":[0.99944776,0.0000485403,0.0002049998,0.00011698285,0.00007810493,9.036237e-9,0.000017982116,5.2310924e-7,0.00008507463],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99882895,0.000060605496,0.00034070128,0.00011179195,0.00043859502,0.00021935046],"domain_scores_gemma":[0.99875265,0.00022216982,0.00034030632,0.00026680337,0.00013684519,0.00028121372],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024616867,0.00007352063,0.00018730135,0.00009135197,0.00040912122,0.00007949316,0.0015501158,0.000027611175,0.001275123],"category_scores_gemma":[0.00016180589,0.000033057477,0.0000587676,0.0013341282,0.000499458,0.00031957772,0.000018047405,0.00013004839,0.0000011582878],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000041760977,0.0000012187938,0.98256105,0.0000012952148,0.00004506997,0.0000036951833,0.00011208823,0.01110488,0.0000035023936,0.00006954704,0.00022901602,0.0058644745],"study_design_scores_gemma":[0.0000494942,0.000052762825,0.97212386,0.000012281472,0.000060209368,0.000010624567,0.00028012358,0.0030175473,0.00003656173,0.0016365398,0.022670526,0.00004947408],"about_ca_topic_score_codex":0.9296394,"about_ca_topic_score_gemma":0.9995704,"teacher_disagreement_score":0.06993101,"about_ca_system_score_codex":0.0000011713021,"about_ca_system_score_gemma":0.003896302,"threshold_uncertainty_score":0.99963784},"labels":[],"label_agreement":null},{"id":"W1993820215","doi":"10.1139/e05-118","title":"The late Quaternary stratigraphic record northwest of Montréal: regional ice-sheet dynamics, ice-stream activity, and early deglacial events","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Institut National de la Recherche Scientifique","funders":"Université du Québec à Montréal","keywords":"Geology; Deglaciation; Ice stream; Outwash plain; Glacial landform; Glacial period; Ice sheet; Quaternary; Meltwater; Geomorphology; Seabed gouging by ice; Paleontology; Landform; Oceanography; Cryosphere; Sea ice; Moraine","score_opus":0.017284505545729644,"score_gpt":0.2206481223499917,"score_spread":0.20336361680426207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993820215","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99409944,0.0021222224,0.0000037920133,0.0020029165,0.00033645498,0.000075651325,0.000036213638,0.000002479823,0.0013208173],"genre_scores_gemma":[0.9992841,0.00027563376,0.00011199663,0.000027065234,0.00007091016,2.4284512e-7,0.000004271783,0.0000016310896,0.00022417499],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99854124,0.00019188927,0.00032959707,0.00015235007,0.00031241347,0.0004725253],"domain_scores_gemma":[0.9988242,0.0003247146,0.00029491616,0.00010229969,0.00011994319,0.0003339549],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009721663,0.000116208095,0.00021628085,0.00029356507,0.0008018209,0.000085892294,0.00045185757,0.000091832364,0.00009662494],"category_scores_gemma":[0.00005114673,0.00007842339,0.00007502384,0.00035336034,0.0015130677,0.0003625958,0.0000071862673,0.00028936405,0.000007531166],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004781063,0.0000056894846,0.99743706,0.0000044606663,0.000016113829,0.00006641121,0.000063811305,0.00035362152,0.0000030825302,0.00019781957,0.00003207708,0.0017720195],"study_design_scores_gemma":[0.000175767,0.0005056921,0.9941124,0.000025337802,0.000010577789,0.00021205477,0.00013012115,0.0011924945,0.000008206134,0.003231386,0.0003122044,0.0000837893],"about_ca_topic_score_codex":0.26197985,"about_ca_topic_score_gemma":0.9914573,"teacher_disagreement_score":0.7294774,"about_ca_system_score_codex":7.740979e-7,"about_ca_system_score_gemma":0.0007896834,"threshold_uncertainty_score":0.7429347},"labels":[],"label_agreement":null},{"id":"W1993825782","doi":"10.1139/e03-081","title":"FeAs<sub>2</sub> biomineralization on encrusted bacteria in hot springs: an ecological role of symbiotic bacteria","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Arsenic contamination and mitigation","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Kanazawa University","keywords":"Biomineralization; Bacteria; Bioremediation; Microbial mat; Mineralization (soil science); Paxillus involutus; Calcite; Environmental chemistry; Microorganism; Chemistry; Iron bacteria; Metal; Mineralogy; Cyanobacteria; Geology; Paleontology; Organic chemistry","score_opus":0.0124612503163278,"score_gpt":0.2089423059808754,"score_spread":0.1964810556645476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993825782","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997843,0.000010316458,0.000022458406,0.00008001439,0.00018854365,0.00007992817,0.0000025765423,0.0000021988783,0.0017709361],"genre_scores_gemma":[0.9994191,0.0000069169005,0.00041290658,0.000118401294,0.000013559528,5.031369e-7,0.0000013742405,0.000002945408,0.000024289606],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9990131,0.00012998402,0.00029972813,0.00014525281,0.0001975074,0.00021438996],"domain_scores_gemma":[0.99937654,0.000029333827,0.00020842387,0.00007234288,0.00002665488,0.00028671106],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00071409193,0.00007765412,0.00012428692,0.00021842624,0.00010895612,0.000049955666,0.00018212924,0.000054082655,0.0010389199],"category_scores_gemma":[0.0002208292,0.00006651525,0.00003240193,0.00043494717,0.0002961944,0.00041618128,0.000006957717,0.00007576634,0.000017966766],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001188792,0.000071720715,0.17608483,0.0000025529432,0.000002902024,0.000017190878,0.000908264,0.0010711205,0.8160671,0.001663751,0.000025403911,0.004073273],"study_design_scores_gemma":[0.0002219827,0.00035541836,0.91678625,0.000028325718,0.00000356294,0.000022375078,0.00046612805,0.00047194658,0.08081641,0.0002280929,0.000513533,0.00008596109],"about_ca_topic_score_codex":0.00068969553,"about_ca_topic_score_gemma":0.05644175,"teacher_disagreement_score":0.74070144,"about_ca_system_score_codex":0.000041949774,"about_ca_system_score_gemma":0.00025967456,"threshold_uncertainty_score":0.9998743},"labels":[],"label_agreement":null},{"id":"W1993943416","doi":"10.1139/e10-076","title":"U–Pb zircon geochronology of eclogites from the Scandian Orogen, northern Western Gneiss Region, Norway: 14–20 million years between eclogite crystallization and return to amphibolite-facies conditionsThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Eclogite; Geology; Geochemistry; Gneiss; Zircon; Metamorphic facies; Coesite; Hornblende; Petrology; Pegmatite; Geochronology; Metamorphic rock; Subduction; Facies; Tectonics; Seismology; Geomorphology; Paleontology","score_opus":0.023447494606880375,"score_gpt":0.18734091819160506,"score_spread":0.1638934235847247,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993943416","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99517745,0.00057470606,0.000004840855,0.0029752157,0.000047735695,0.00012347597,0.00022885241,0.000001097378,0.0008666393],"genre_scores_gemma":[0.99936336,0.00011605581,0.0002600793,0.00017027686,0.00005872714,5.277684e-7,0.000010785537,0.0000015766393,0.000018611252],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99843657,0.00020122161,0.00067922415,0.00018748164,0.00024206834,0.0002534435],"domain_scores_gemma":[0.9985421,0.00036760126,0.00057772093,0.00015745728,0.00021160686,0.00014355379],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00071872206,0.00011325355,0.00045303788,0.0003262517,0.000081609025,0.000020559937,0.00044422122,0.00009740828,0.006405247],"category_scores_gemma":[0.00043193632,0.000068540576,0.000085917054,0.000892368,0.0017702747,0.00023651347,0.000020190346,0.00015719282,0.0000027896149],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057387293,0.000017691938,0.992202,0.000009145893,0.000034968416,0.000005737484,0.0042190086,0.00028179164,0.001960723,0.00006857723,0.000043243814,0.0010997611],"study_design_scores_gemma":[0.00022866655,0.0006171847,0.9658294,0.00012659184,0.000030219126,0.000006466679,0.0024709252,0.000022039852,0.024638847,0.0056589423,0.0002915857,0.000079130274],"about_ca_topic_score_codex":0.053089555,"about_ca_topic_score_gemma":0.6175195,"teacher_disagreement_score":0.56442994,"about_ca_system_score_codex":0.000003978546,"about_ca_system_score_gemma":0.0002557415,"threshold_uncertainty_score":0.994503},"labels":[],"label_agreement":null},{"id":"W1994288656","doi":"10.1139/cjes-2014-0224","title":"Magnetic models of the Moyie anticline, Purcell anticlinorium, southeastern Canadian Cordillera","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Anticline; Geology; Sill; Syncline; Stratigraphy; Sedimentary rock; Detachment fault; Fault (geology); Magnetic dip; Fold (higher-order function); Paleontology; Seismology; Geomorphology; Petrology; Geophysics; Structural basin; Extensional definition; Tectonics","score_opus":0.04404914010095507,"score_gpt":0.19830843950280316,"score_spread":0.1542592994018481,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994288656","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9730887,0.0018332228,0.000008265614,0.0024130354,0.0007100152,0.00008275355,0.00004996832,0.0000021132212,0.021811942],"genre_scores_gemma":[0.9987866,0.000016212864,0.00020931113,0.00040781815,0.00013112737,8.200354e-8,6.503008e-7,0.0000013627551,0.0004467812],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984993,0.00008330471,0.0003411914,0.00014747065,0.00041454766,0.0005142086],"domain_scores_gemma":[0.99816114,0.00008009415,0.0001758367,0.00012014267,0.00026632973,0.001196435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005524835,0.00011717149,0.00024955595,0.00015113532,0.00039936753,0.0000830968,0.0006900928,0.000047196907,0.00065292063],"category_scores_gemma":[0.00019745539,0.000063564745,0.00010741954,0.00057569606,0.0009552749,0.00021053538,0.000011023132,0.00017140813,0.000101860984],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005476431,0.000005844215,0.98316365,0.000004226588,0.000008655944,0.000030040434,0.00044695733,0.0123991985,0.0000033545289,0.00014601745,0.000121232406,0.003665339],"study_design_scores_gemma":[0.00023640638,0.0006651788,0.9757096,0.000042202937,0.00002335302,0.000048725546,0.0011590805,0.012071799,0.000036118836,0.00696943,0.0028916935,0.00014637831],"about_ca_topic_score_codex":0.52710295,"about_ca_topic_score_gemma":0.9435663,"teacher_disagreement_score":0.41646338,"about_ca_system_score_codex":0.0000016678547,"about_ca_system_score_gemma":0.0017898796,"threshold_uncertainty_score":0.7149023},"labels":[],"label_agreement":null},{"id":"W1994872963","doi":"10.1139/e01-074","title":"Petrology, age, and tectonic setting of the White Rock Formation, Meguma terrane, Nova Scotia: evidence for Silurian continental rifting","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; Acadia University","funders":"Memorial University of Newfoundland; Acadia University","keywords":"Felsic; Geology; Mafic; Terrane; Geochemistry; Pluton; Zircon; Volcanic rock; Shear zone; Continental crust; Petrology; Paleontology; Volcano; Crust; Tectonics","score_opus":0.0358516752037751,"score_gpt":0.22051446275183642,"score_spread":0.1846627875480613,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994872963","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9906995,0.0020785355,0.00005958671,0.0058589363,0.00016282112,0.00007992772,0.00001740681,0.0000019737527,0.0010413082],"genre_scores_gemma":[0.99856997,0.000014819215,0.001016824,0.0002663262,0.00006541925,1.12920624e-7,0.0000010087956,7.92355e-7,0.00006471872],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99891675,0.000059467722,0.0003668219,0.00013232816,0.00019892292,0.00032569838],"domain_scores_gemma":[0.99901795,0.0002337425,0.0003154829,0.00006706251,0.00011578058,0.0002499714],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00073785556,0.000087105866,0.00019864932,0.0001334224,0.00037724862,0.000086063694,0.00038193306,0.000041102823,0.0021858956],"category_scores_gemma":[0.00073631847,0.00005005794,0.00010997001,0.00042568916,0.00038257192,0.0003239796,0.000009476463,0.00013680439,0.00000774987],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000039649926,0.0000021227247,0.99584574,0.00001261693,0.000009282273,0.0000056210547,0.0002942994,0.0019253711,0.00013812764,0.000014543068,0.00015053115,0.0015977839],"study_design_scores_gemma":[0.00019760821,0.00025232995,0.9776317,0.00011220897,0.000037160557,0.00017986506,0.0004541997,0.019468697,0.0002077645,0.0009005917,0.00046177593,0.000096115335],"about_ca_topic_score_codex":0.0081741605,"about_ca_topic_score_gemma":0.5699499,"teacher_disagreement_score":0.56177574,"about_ca_system_score_codex":0.0000012500873,"about_ca_system_score_gemma":0.000089693924,"threshold_uncertainty_score":0.99872625},"labels":[],"label_agreement":null},{"id":"W1994925477","doi":"10.1139/e08-023","title":"The White River Ash: largest Holocene Plinian tephra","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Tephra; Pumice; Lapilli; Isopach map; Lobe; Pyroclastic rock; Holocene; Geomorphology; Paleontology; Volcano; Structural basin","score_opus":0.0338964468055236,"score_gpt":0.23610899485179038,"score_spread":0.20221254804626676,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994925477","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9791761,0.0029150888,0.0000051404527,0.004560003,0.00072161865,0.00005070493,0.000011752898,0.0000035605897,0.012556029],"genre_scores_gemma":[0.99786305,0.00025785662,0.00041666228,0.00036978722,0.00012870698,1.3242301e-7,0.000001657999,0.000001275304,0.0009608549],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984398,0.0001679531,0.00026621533,0.00014742713,0.00030358654,0.00067499967],"domain_scores_gemma":[0.9986402,0.00028642427,0.00014113891,0.00012721846,0.00014273997,0.0006622762],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["sts"],"category_scores_codex":[0.0015430194,0.00009553129,0.00016070493,0.00023953039,0.0023364588,0.00008314218,0.00077786244,0.00008316627,0.0015165581],"category_scores_gemma":[0.00027942084,0.000056962715,0.00007346458,0.0004837044,0.003482153,0.00029173208,0.0000059331155,0.00037665595,0.00039356915],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007676132,0.0000014136849,0.99790657,9.946326e-7,0.00000886648,0.00036621955,0.00033266254,0.0003554875,2.7162898e-7,0.000055195145,0.00058770605,0.00037696786],"study_design_scores_gemma":[0.00013177714,0.00020979917,0.9845725,0.000008690795,0.0000041783455,0.0018108157,0.0001753291,0.00015089833,0.000010971751,0.00039546925,0.0124533,0.00007623178],"about_ca_topic_score_codex":0.0022689705,"about_ca_topic_score_gemma":0.35266918,"teacher_disagreement_score":0.3504002,"about_ca_system_score_codex":3.537551e-7,"about_ca_system_score_gemma":0.00189896,"threshold_uncertainty_score":0.9993962},"labels":[],"label_agreement":null},{"id":"W1995155093","doi":"10.1139/e00-073","title":"Newly identified Carboniferous units (the Pointe Sawyer and Chemin-des-Pêcheurs formations) in the Gaspé Peninsula, Quebec; implications regarding the evolution of the northwestern sector of the Maritimes Basin","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Carboniferous; Facies; Clastic rock; Paleontology; Bay; Lithostratigraphy; Peninsula; Geomorphology; Structural basin; Geochemistry; Archaeology; Geography","score_opus":0.02491414105407125,"score_gpt":0.20494511375665247,"score_spread":0.18003097270258123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1995155093","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9904087,0.0009223891,0.000029157332,0.005869528,0.00013422915,0.00016170197,0.000029652658,0.0000012029916,0.0024434088],"genre_scores_gemma":[0.9995183,0.000052888063,0.000031297048,0.00025182936,0.000028833832,8.960601e-7,0.0000014302994,9.655905e-7,0.0001135635],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989056,0.00017062854,0.00035641267,0.00007825022,0.00026724502,0.00022188357],"domain_scores_gemma":[0.9988561,0.0003387869,0.00031920694,0.00018729923,0.00022717196,0.00007141266],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00132137,0.000078183446,0.00010886729,0.00010220188,0.0009944516,0.00017125263,0.0008668552,0.000030772502,0.00010500143],"category_scores_gemma":[0.0003294151,0.000029383016,0.00006155232,0.0013689029,0.0010612735,0.0004534744,0.000014633727,0.00018982754,0.000001546514],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003414315,0.00000254743,0.99375224,0.000006556665,0.000004812927,6.307468e-7,0.0022858053,0.0022166271,0.000017504775,0.0004337856,0.000079207086,0.0011968763],"study_design_scores_gemma":[0.00008503077,0.00003542636,0.9891246,0.000053924385,0.000014594988,0.0002152959,0.0063811205,0.00070125726,0.000044962886,0.0023375582,0.0009641947,0.00004206027],"about_ca_topic_score_codex":0.16560206,"about_ca_topic_score_gemma":0.85744053,"teacher_disagreement_score":0.6918385,"about_ca_system_score_codex":0.0000064756077,"about_ca_system_score_gemma":0.0009249961,"threshold_uncertainty_score":0.83995426},"labels":[],"label_agreement":null},{"id":"W1995360465","doi":"10.1139/e02-023","title":"<i>Paucicanthus vanelsti</i>gen. et sp. nov., an Early Devonian (Lochkovian) acanthodian that lacks paired fin-spines","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Anatomy; Devonian; Fish fin; SPINE (molecular biology); Fin; Biology; Geology; Paleontology; Fish <Actinopterygii>","score_opus":0.056060885974989066,"score_gpt":0.23642812671961808,"score_spread":0.180367240744629,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1995360465","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9742468,0.0050194724,0.000058088615,0.0038157038,0.0014461329,0.000094362505,0.00013592927,0.000016362004,0.015167149],"genre_scores_gemma":[0.9957622,0.00015903552,0.0019211047,0.0014600432,0.00026578724,3.9125868e-7,0.000011357234,0.0000037212865,0.00041635125],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997718,0.0003000372,0.00041259883,0.00035917034,0.00031830982,0.0008919116],"domain_scores_gemma":[0.9978937,0.00018399076,0.00028416762,0.00019986615,0.00012063286,0.0013176227],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011559548,0.00022753711,0.00034040379,0.00048211488,0.0008882218,0.00016387217,0.00088677614,0.00018587067,0.005629197],"category_scores_gemma":[0.00017812046,0.00017961497,0.00011627515,0.00055473065,0.0016639696,0.0010469258,0.000006295289,0.0003806407,0.0002434173],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013788052,0.000009786382,0.99006987,0.000004056652,0.000016595182,0.00033185576,0.00059394015,0.0005420991,0.000018954821,0.00016043482,0.0006581409,0.0075805094],"study_design_scores_gemma":[0.0002321914,0.00073896756,0.97094655,0.00003635551,0.00001440492,0.0007432823,0.0002961893,0.0013727109,0.000028215081,0.00042917955,0.024907824,0.00025415368],"about_ca_topic_score_codex":0.028473362,"about_ca_topic_score_gemma":0.8061971,"teacher_disagreement_score":0.7777237,"about_ca_system_score_codex":0.000004311816,"about_ca_system_score_gemma":0.0010144347,"threshold_uncertainty_score":0.9952798},"labels":[],"label_agreement":null},{"id":"W1996174702","doi":"10.1139/e04-105","title":"Middle Eocene sedimentary and volcanic infilling of an evolving supradetachment basin: White Lake Basin, south-central British Columbia","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Smithsonian Astrophysical Observatory; Evolving Earth Foundation; Washington State University","keywords":"Geology; Facies; Alluvial fan; Sedimentary rock; Structural basin; Geomorphology; Geochemistry; Clastic rock; Alluvium; Paleontology; Fluvial; Volcano; Fault (geology)","score_opus":0.016137734622929514,"score_gpt":0.19017229657156873,"score_spread":0.1740345619486392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996174702","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958591,0.0022198542,0.000022611186,0.00047965924,0.00023335616,0.00006420305,0.00014558106,0.0000040204054,0.00097161846],"genre_scores_gemma":[0.9948005,0.000069713526,0.0044312356,0.00046854164,0.000133521,1.1309207e-7,0.0000129431555,0.0000015507494,0.000081863625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986735,0.00004902572,0.00039710445,0.00015193004,0.00029070323,0.00043775895],"domain_scores_gemma":[0.9988392,0.000046710564,0.00021794518,0.00006367593,0.00013667057,0.00069578504],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00070019567,0.00008268071,0.00020142479,0.00012821879,0.00051410875,0.0005790747,0.00027980682,0.00004675375,0.0077741803],"category_scores_gemma":[0.00006805481,0.00008679459,0.00004826594,0.00035061096,0.00040376352,0.0013006672,0.000005750105,0.00013817707,0.0000052956866],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021495343,0.00000521826,0.9877376,0.000012008396,0.000006801444,0.000012988564,0.0004965718,0.0037381193,0.000001310177,0.000001974183,0.00018287059,0.0078023975],"study_design_scores_gemma":[0.00019541541,0.00038309617,0.9870253,0.00008871752,0.000014606973,0.00025387295,0.0011076528,0.0040460364,0.000015607167,0.0001818629,0.0065697576,0.00011802603],"about_ca_topic_score_codex":0.0835435,"about_ca_topic_score_gemma":0.9546483,"teacher_disagreement_score":0.87110484,"about_ca_system_score_codex":0.0000023656862,"about_ca_system_score_gemma":0.0006498591,"threshold_uncertainty_score":0.9931328},"labels":[],"label_agreement":null},{"id":"W1996515703","doi":"10.1139/e05-061","title":"A long-term field study (1951-2003) of ventifacts formed by katabatic winds at Paulatuk, western Arctic coast, Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University; University of British Columbia","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Katabatic wind; Geology; Abrasion (mechanical); Holocene; Arctic; Aeolian processes; Glacial period; Solifluction; Radiocarbon dating; Geomorphology; Physical geography; Oceanography; Paleontology; Climatology; Geography","score_opus":0.02242713886710037,"score_gpt":0.24802635499132866,"score_spread":0.22559921612422829,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996515703","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961332,0.0015231483,0.000003347195,0.0009856174,0.00052220956,0.00014839559,0.000039950966,0.000001720862,0.0006423785],"genre_scores_gemma":[0.99873567,0.000014574038,0.00005326542,0.00033376325,0.00005692729,3.566101e-7,0.00000928849,0.0000018918382,0.0007942451],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981221,0.00013540912,0.00043689588,0.00019203384,0.00047324153,0.00064031134],"domain_scores_gemma":[0.9984193,0.00027610775,0.00025963146,0.00014681144,0.000195044,0.00070309313],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00086565653,0.00013128326,0.00030353238,0.00025236935,0.0004547433,0.000051048617,0.0005877397,0.00006942156,0.0022638254],"category_scores_gemma":[0.00028011316,0.00010321773,0.000045479963,0.0005212732,0.00045075573,0.00038352655,0.000009879822,0.00028136853,0.00003082396],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021703867,0.000013984199,0.9977248,0.000015751202,0.000029592808,0.00022437063,0.00035776893,0.00024820934,0.0000029354792,0.0000011854889,0.0005875254,0.000772188],"study_design_scores_gemma":[0.00036846087,0.00074620335,0.9969812,0.000046182748,0.000021337723,0.00040802048,0.0003322109,0.00009052399,0.00010714036,0.000012268364,0.0007774134,0.00010903822],"about_ca_topic_score_codex":0.42008314,"about_ca_topic_score_gemma":0.99960536,"teacher_disagreement_score":0.5795222,"about_ca_system_score_codex":0.0000037217803,"about_ca_system_score_gemma":0.0038708828,"threshold_uncertainty_score":0.9986482},"labels":[],"label_agreement":null},{"id":"W1996611509","doi":"10.1139/e09-066","title":"Geochemistry of the northern Cache Creek terrane and implications for accretionary processes in the Canadian Cordillera","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of British Columbia; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Victoria University; University of Victoria; Geological Society of America","keywords":"Geology; Terrane; Subduction; Seamount; Ophiolite; Geochemistry; Volcanic rock; Volcanic arc; Basement; Island arc; Basalt; North American Plate; Paleontology; Earth science; Volcano; Tectonics","score_opus":0.020099427132386806,"score_gpt":0.2115836677000011,"score_spread":0.1914842405676143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996611509","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98460484,0.00044520356,0.000001047,0.011918149,0.000057667774,0.00007776275,0.00009847754,6.0159635e-7,0.0027962725],"genre_scores_gemma":[0.9993096,0.000009390096,0.00019162036,0.000404438,0.000052346462,8.652506e-7,0.0000057921225,5.7629666e-7,0.00002537045],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993114,0.000023405599,0.0001947498,0.00010492311,0.00013139012,0.00023411821],"domain_scores_gemma":[0.9991136,0.00021699388,0.00011756492,0.00009102737,0.00017936746,0.00028143608],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00050154305,0.000058870173,0.00010742339,0.000078260055,0.0005056511,0.00008783752,0.0005574008,0.000046303765,0.00081247976],"category_scores_gemma":[0.0005406782,0.000030581585,0.000050438797,0.00051172095,0.0007314029,0.00009428093,0.0000034838708,0.0001902158,9.179474e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000012668479,0.000002653854,0.9982492,0.0000067749843,0.0000038990534,0.0000014561324,0.00014970043,0.0001141387,0.00015560226,0.00002144179,0.000050935014,0.0012429744],"study_design_scores_gemma":[0.000055445693,0.00004614659,0.9920537,0.0000111723075,0.000011747845,0.00006997051,0.0002797138,0.00015915459,0.00011169922,0.005135449,0.002016953,0.000048873117],"about_ca_topic_score_codex":0.5024719,"about_ca_topic_score_gemma":0.99927574,"teacher_disagreement_score":0.49680388,"about_ca_system_score_codex":0.000001065897,"about_ca_system_score_gemma":0.0017920393,"threshold_uncertainty_score":0.8896084},"labels":[],"label_agreement":null},{"id":"W1996850987","doi":"10.1139/e02-020","title":"Chemostratigraphy of the Neoproterozoic Alona Bay lavas, Ontario","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Bay; Geology; Flood basalt; Chemostratigraphy; Partial melting; Basalt; Geochemistry; Lava; Rift; Paleontology; Oceanography; Volcano; Tectonics; Volcanism; Chemistry","score_opus":0.02073429816889277,"score_gpt":0.16688729512416212,"score_spread":0.14615299695526934,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996850987","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9806797,0.0010729533,0.0000022135748,0.0017180756,0.00018722203,0.000038332622,0.000010243931,0.0000012724606,0.016289983],"genre_scores_gemma":[0.99880296,0.0000115960565,0.00040928816,0.00035445899,0.00004610345,6.440083e-8,5.3955324e-7,4.6821268e-7,0.00037452168],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989503,0.000042016087,0.00028597302,0.00011697926,0.00031398865,0.00029071866],"domain_scores_gemma":[0.9991838,0.00005516119,0.00019852078,0.00010074575,0.00008249614,0.0003792748],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003428657,0.000083797175,0.00017422883,0.00012066751,0.00025807382,0.00005808376,0.00060257857,0.000038995182,0.025563769],"category_scores_gemma":[0.000085120446,0.000043534194,0.00018289659,0.0006792137,0.0007180504,0.00016404898,0.0000043278974,0.00018960134,0.000029568107],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000010831279,0.0000035552412,0.99754715,0.0000016777252,0.000009852423,0.000009195971,0.00016820277,0.0004365866,0.0000378189,0.000031254993,0.00016295756,0.001590683],"study_design_scores_gemma":[0.00006921284,0.00014997352,0.990082,0.00001868544,0.000015079699,0.0000486797,0.000057358142,0.00033697946,0.0005899815,0.003009069,0.0055543017,0.0000686814],"about_ca_topic_score_codex":0.3068912,"about_ca_topic_score_gemma":0.98365164,"teacher_disagreement_score":0.67676044,"about_ca_system_score_codex":0.0000010307419,"about_ca_system_score_gemma":0.00033566987,"threshold_uncertainty_score":0.975327},"labels":[],"label_agreement":null},{"id":"W1997049501","doi":"10.1139/e99-108","title":"Instabilities in the Labrador Sea water mass structure during the last climatic cycle","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Globigerina bulloides; Oceanography; Geology; Water mass; Benthic zone; Thermocline; North Atlantic Deep Water; Water column; Thermohaline circulation; Foraminifera","score_opus":0.01180323948151538,"score_gpt":0.20752410897550103,"score_spread":0.19572086949398565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997049501","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9910065,0.00051901303,1.853556e-7,0.0041500716,0.00016526334,0.00008110034,0.000018740106,0.0000016173545,0.004057516],"genre_scores_gemma":[0.99934745,0.000027096608,0.00006412757,0.00037502608,0.00006440122,2.541489e-7,0.0000019564118,9.555096e-7,0.00011871332],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99849576,0.00034612446,0.00023303599,0.00011234128,0.00025425482,0.0005584667],"domain_scores_gemma":[0.9993861,0.0002486578,0.000042979136,0.00012139934,0.00003261845,0.00016826807],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013907722,0.00008314264,0.0001308478,0.00017598465,0.0007646439,0.00015190513,0.00077073136,0.000054732118,0.010716307],"category_scores_gemma":[0.000060874037,0.000035058918,0.00004351852,0.00033852833,0.0012164352,0.00030091897,0.0000028687632,0.00040076106,0.000109027234],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006430852,0.0000011439605,0.99075615,0.0000072287253,0.0000036196914,0.00009034107,0.0029300945,0.005814892,0.000003104567,0.000015264986,0.000009445511,0.0003622931],"study_design_scores_gemma":[0.00011873211,0.00008413791,0.99293804,0.000013729115,0.0000032390205,0.0005512968,0.0030202896,0.00047254824,0.0000405917,0.0015798652,0.0011211634,0.00005637098],"about_ca_topic_score_codex":0.004882205,"about_ca_topic_score_gemma":0.779018,"teacher_disagreement_score":0.77413577,"about_ca_system_score_codex":5.540385e-7,"about_ca_system_score_gemma":0.00037489468,"threshold_uncertainty_score":0.99018806},"labels":[],"label_agreement":null},{"id":"W1997163908","doi":"10.1139/e06-072","title":"Petrogenesis of the Leo Lake and Lyndhurst plutons, Frontenac terrane, Central Metasedimentary Belt, southeastern Ontario, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Pluton; Geology; Geochemistry; Gabbro; Terrane; Quartz monzonite; Hornblende; Zircon; Magma; Petrogenesis; Magma chamber; Mafic; Petrology; Mantle (geology); Biotite; Igneous rock; Paleontology; Tectonics; Volcano","score_opus":0.011829501376248688,"score_gpt":0.16597274139321277,"score_spread":0.15414324001696408,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997163908","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955379,0.0014793356,0.0000050628896,0.0011620857,0.0003480622,0.000041441846,0.00016902083,0.000001011744,0.00125611],"genre_scores_gemma":[0.9989963,0.00000637314,0.00020650255,0.0005600788,0.00005746032,4.0196664e-8,0.0000063100347,8.8559943e-7,0.00016600892],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985322,0.00004446681,0.0003581695,0.00015074994,0.0004142087,0.00050025125],"domain_scores_gemma":[0.9988199,0.0000926117,0.00020511694,0.0000894333,0.00006608981,0.00072686136],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006020524,0.0001129528,0.00023025519,0.000109185065,0.00032095582,0.000041354422,0.0004406741,0.00003294907,0.005215676],"category_scores_gemma":[0.000057274334,0.000062360195,0.00011019347,0.00032316727,0.00057986216,0.00012659348,0.000009611897,0.00015773017,0.0000011075706],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008385305,0.000002853283,0.9981713,0.0000025771326,0.000028375394,0.000039869377,0.00015405963,0.00030688537,0.000023312337,0.000005949671,0.00009856344,0.0011578187],"study_design_scores_gemma":[0.000116312876,0.00008572795,0.9933019,0.000017785767,0.000050659513,0.000084805404,0.00069458154,0.00007818758,0.00036334366,0.0002056055,0.0049150637,0.00008597634],"about_ca_topic_score_codex":0.9935791,"about_ca_topic_score_gemma":0.9999898,"teacher_disagreement_score":0.0064107324,"about_ca_system_score_codex":0.0000044905187,"about_ca_system_score_gemma":0.0019638508,"threshold_uncertainty_score":0.9956937},"labels":[],"label_agreement":null},{"id":"W1997554897","doi":"10.1139/e05-030","title":"The anatomy of<i>Askeptosaurus italicus</i>from the Middle Triassic of Monte San Giorgio and the interrelationships of thalattosaurs (Reptilia, Diapsida)","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"General Electric (Canada)","funders":"","keywords":"Monophyly; Paleontology; Sister group; Geology; Taxon; Clade; Anatomy; Biology; Phylogenetic tree","score_opus":0.030129875751584826,"score_gpt":0.22546775492437496,"score_spread":0.19533787917279014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997554897","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9695024,0.02244829,0.000007628706,0.0053213798,0.00035389082,0.00009243721,0.00007950704,0.000001187721,0.0021933182],"genre_scores_gemma":[0.9993442,0.0002467254,0.00014519892,0.00012378907,0.000088072346,2.6803917e-7,0.0000022697218,9.863861e-7,0.000048438895],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985797,0.00036716548,0.00049015065,0.00011261894,0.00020438997,0.0002460014],"domain_scores_gemma":[0.99749076,0.0015941757,0.00051422056,0.00015342208,0.00009299617,0.00015440752],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0017668351,0.00009021723,0.00023906818,0.000105409155,0.0005670073,0.000026158106,0.00067033735,0.00006469949,0.00024700002],"category_scores_gemma":[0.00037904698,0.000040487605,0.00011432052,0.00033061075,0.004751521,0.00023086589,0.000008520603,0.00021212922,0.000002955039],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006458615,0.0000035212463,0.989312,0.0000018614596,0.000044051118,0.0000024214141,0.0015323678,0.0007191128,0.000012097341,0.0009862432,0.00029224905,0.007029523],"study_design_scores_gemma":[0.00037243185,0.00015829036,0.98899245,0.000037921964,0.00003311148,0.0000676333,0.0026024312,0.0017129069,0.00005338977,0.0018920593,0.0040256176,0.00005177778],"about_ca_topic_score_codex":0.014852518,"about_ca_topic_score_gemma":0.61704135,"teacher_disagreement_score":0.6021888,"about_ca_system_score_codex":0.0000014351828,"about_ca_system_score_gemma":0.00053407124,"threshold_uncertainty_score":0.997957},"labels":[],"label_agreement":null},{"id":"W1998484039","doi":"10.1139/e09-044","title":"Prediction of decadal slope changes in Canada by glacial isostatic adjustment modellingThis article is one of a series of papers published in this Special Issue on the theme <i>GEODESY</i>.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Post-glacial rebound; Geology; Shore; Geodesy; Glacial period; Series (stratigraphy); Mantle (geology); Physical geography; Geomorphology; Geophysics; Oceanography; Paleontology; Geography","score_opus":0.02485892099751892,"score_gpt":0.20518418353890194,"score_spread":0.18032526254138304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998484039","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9828131,0.0005719015,5.71702e-7,0.007437051,0.00025224904,0.00011444679,0.000095545984,5.4425107e-7,0.008714599],"genre_scores_gemma":[0.99916345,0.00019255553,0.0000774229,0.00041453654,0.00008784496,3.0166095e-7,0.0000026986954,8.786636e-7,0.00006029135],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99849015,0.00016096931,0.0004301442,0.00012957955,0.00043106818,0.0003580649],"domain_scores_gemma":[0.9991838,0.00020849453,0.00024283276,0.00009106882,0.00009492226,0.00017892571],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011009473,0.00008490641,0.00026769392,0.00029388932,0.00010200223,0.000016212154,0.00036744308,0.00005459522,0.009958045],"category_scores_gemma":[0.00018156358,0.00005900323,0.0000314088,0.00062535313,0.0005458578,0.00022369684,0.0000033548324,0.00022436258,0.0000018505095],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008445668,0.000015176312,0.9928482,0.0000092790115,0.000009117411,0.00001301798,0.0016469641,0.0027627803,0.000071172195,0.00007811164,0.00077507563,0.0016866479],"study_design_scores_gemma":[0.00034154122,0.0011027259,0.98750067,0.00011058012,0.000008797537,0.000020733012,0.0021181642,0.0024561102,0.0044428525,0.00076233794,0.0010599603,0.00007550897],"about_ca_topic_score_codex":0.53001195,"about_ca_topic_score_gemma":0.99616396,"teacher_disagreement_score":0.46615198,"about_ca_system_score_codex":0.000004514335,"about_ca_system_score_gemma":0.0025220183,"threshold_uncertainty_score":0.990947},"labels":[],"label_agreement":null},{"id":"W1998843582","doi":"10.1139/e08-062","title":"Basin architecture and syndepositional fault activity during deposition of the Neoproterozoic Mackenzie Mountains supergroup, Northwest Territories, CanadaNorthwest Territories Geoscience Office Contribution 0040.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Isopach map; Basement; Subsidence; Paleozoic; Paleontology; Structural basin; Supergroup; Proterozoic; Sedimentary depositional environment; Rift; Craton; Fault (geology); Growth fault; Fault block; Carbonate platform; Onlap; Facies; Sedimentary rock; Tectonics","score_opus":0.007225527298562443,"score_gpt":0.1739796876643896,"score_spread":0.16675416036582716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998843582","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99746823,0.00032731215,0.000054114895,0.0011845218,0.0003196608,0.000087953915,0.00050032436,0.0000039580846,0.00005389367],"genre_scores_gemma":[0.9993613,0.000022045093,0.00028940788,0.000115698014,0.0001625424,6.486019e-7,0.000031433723,0.0000013313628,0.000015641845],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983332,0.000115124494,0.00032449613,0.00023473478,0.0005712084,0.00042121895],"domain_scores_gemma":[0.9988252,0.00011057804,0.0002512707,0.000110902685,0.00021912776,0.00048291395],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00031253745,0.00015262398,0.00024868827,0.00016015592,0.0013264512,0.000094681636,0.00042195883,0.00007003149,0.00017957164],"category_scores_gemma":[0.00018751419,0.00009563404,0.00010754971,0.0006863894,0.0016631751,0.00043716075,0.000015581569,0.00026386397,8.034238e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023806484,0.000008299145,0.997021,0.000009402187,0.000011749849,0.000059362974,0.00011956103,0.0015597946,0.0008087112,0.000035088924,0.000002188071,0.00034100728],"study_design_scores_gemma":[0.00015479163,0.00017788979,0.9941575,0.000048514237,0.000020944035,0.00096351973,0.00007500035,0.00046349436,0.003365967,0.00026627045,0.00018287927,0.0001232447],"about_ca_topic_score_codex":0.75942236,"about_ca_topic_score_gemma":0.98382837,"teacher_disagreement_score":0.22440603,"about_ca_system_score_codex":0.000010691181,"about_ca_system_score_gemma":0.00093290524,"threshold_uncertainty_score":0.9999737},"labels":[],"label_agreement":null},{"id":"W1999010085","doi":"10.1139/e03-073","title":"Provenance of Jurassic sedimentary rocks of south-central Quesnellia, British Columbia: implications for paleogeography","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of Saskatchewan","keywords":"Geology; Provenance; Terrane; Sedimentary rock; Zircon; Geochemistry; Geochronology; Paleontology; Petrography; Back-arc basin; Source rock; Structural basin; Subduction","score_opus":0.011062875205359826,"score_gpt":0.186780077972513,"score_spread":0.1757172027671532,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999010085","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961447,0.0018202388,0.00019795427,0.00073838694,0.00012082129,0.00010589219,0.00036748018,0.000002027933,0.00050250813],"genre_scores_gemma":[0.99749196,0.000044137876,0.0022209994,0.00014940283,0.000053621483,5.864412e-7,0.000010887332,8.954527e-7,0.000027541591],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99888563,0.000018343635,0.0004093741,0.00015372368,0.00017076365,0.00036218602],"domain_scores_gemma":[0.99890584,0.00006422217,0.0003324283,0.00007380611,0.00019561821,0.0004281173],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028969278,0.000063909916,0.00024023338,0.00010345338,0.00022458674,0.000075875105,0.00037512966,0.00004193815,0.0008806439],"category_scores_gemma":[0.00008888616,0.000063026215,0.00020365718,0.00060494675,0.00067486416,0.00017430956,0.000003497442,0.00008549619,0.0000013669818],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000028543595,0.000011531985,0.99361837,0.000011005689,0.000019849977,0.000003352388,0.000060723185,0.003166236,0.00006184591,0.000025937154,0.00008184114,0.0029364827],"study_design_scores_gemma":[0.00021427819,0.0003722923,0.9752659,0.00005776568,0.000033952492,0.000026136695,0.0001506469,0.000056588768,0.0002718746,0.022973731,0.0004960802,0.00008075938],"about_ca_topic_score_codex":0.29754055,"about_ca_topic_score_gemma":0.9013326,"teacher_disagreement_score":0.6037921,"about_ca_system_score_codex":0.0000013977977,"about_ca_system_score_gemma":0.0006623547,"threshold_uncertainty_score":0.9642433},"labels":[],"label_agreement":null},{"id":"W1999285007","doi":"10.1139/e06-122","title":"Sea-level forcing of carbon isotope excursions in epeiric seas: implications for chemostratigraphy","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Sea level; Galena; Ordovician; Isotopes of carbon; Oceanography; Carbon cycle; Chemostratigraphy; Total organic carbon; Paleontology; Geochemistry; Pyrite; Ecosystem","score_opus":0.06290210789414595,"score_gpt":0.2894197264621758,"score_spread":0.22651761856802982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999285007","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99055314,0.0012031033,0.000105896266,0.0015872832,0.00022717047,0.00014270165,0.00004606155,0.0000014793787,0.006133179],"genre_scores_gemma":[0.9978713,0.0000228824,0.0019375898,0.00008691736,0.00003582552,4.5997513e-7,0.000004801716,0.0000010552955,0.000039177434],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998832,0.000045997796,0.00035307548,0.00013155965,0.00012744906,0.0005099157],"domain_scores_gemma":[0.998727,0.00045768885,0.00016281448,0.00008741391,0.00016087048,0.00040418963],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020236443,0.000073287614,0.00018241497,0.000727462,0.00027118323,0.00002187187,0.00038789262,0.00007968672,0.00013108479],"category_scores_gemma":[0.00024923243,0.000059968494,0.00007126803,0.000890397,0.0006515651,0.0001663873,0.0000025465963,0.00017852444,0.000002018282],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010131011,0.0000039100155,0.99821925,0.000008319459,0.0000054977236,0.000009667207,0.00017094753,0.00032601622,0.000024673622,0.0003118124,0.000027957589,0.000881838],"study_design_scores_gemma":[0.00017874797,0.00022483153,0.9957717,0.000030451256,0.0000056876265,0.0001054533,0.00041164926,0.0003084792,0.00020680766,0.0024466845,0.00024537253,0.00006414864],"about_ca_topic_score_codex":0.0076940595,"about_ca_topic_score_gemma":0.81516856,"teacher_disagreement_score":0.8074745,"about_ca_system_score_codex":5.971297e-7,"about_ca_system_score_gemma":0.0013902487,"threshold_uncertainty_score":0.99891376},"labels":[],"label_agreement":null},{"id":"W1999360018","doi":"10.1139/e04-007","title":"Biostratigraphical and ecostratigraphical significance of Tremadoc (Ordovician) graptolite faunas from the Misty Creek Embayment and Selwyn Basin in Yukon and Northwest Territories","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Newcastle University","keywords":"Biozone; Geology; Ordovician; Paleontology; Fauna; Biotope; Structural basin; Acritarch; Ecology","score_opus":0.01749932417689751,"score_gpt":0.19737692626638279,"score_spread":0.17987760208948528,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999360018","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.990423,0.0041245148,0.0000083504565,0.0050461926,0.000105954394,0.00008950624,0.00010274754,0.0000014549439,0.000098266995],"genre_scores_gemma":[0.9984885,0.0007094821,0.0005415653,0.00019797932,0.000055477423,3.743834e-7,0.0000048521624,7.5650985e-7,0.0000010006919],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989921,0.000069591784,0.00031397011,0.0001822785,0.0001964674,0.00024562914],"domain_scores_gemma":[0.9992672,0.00018564565,0.00013041052,0.00005278865,0.000044553333,0.00031936198],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046601106,0.00010115449,0.00020503018,0.00009655441,0.0004006258,0.00017676275,0.00014053384,0.000051720282,0.000038694285],"category_scores_gemma":[0.000083151164,0.00006369327,0.000030725663,0.00035880724,0.0014335933,0.0002655943,0.000004661591,0.00015681905,2.2720735e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009782426,0.0000047738426,0.99609923,0.0000035803796,0.0000063815573,0.000023646611,0.00056331855,0.00012466304,0.000011452171,0.00029600697,0.0000034825987,0.0028536895],"study_design_scores_gemma":[0.00022335985,0.00048729527,0.99018455,0.0000495077,0.000008587151,0.0000298699,0.0016657015,0.00008602802,0.000017651231,0.0066026216,0.00056584046,0.000078990684],"about_ca_topic_score_codex":0.34616467,"about_ca_topic_score_gemma":0.9889423,"teacher_disagreement_score":0.6427777,"about_ca_system_score_codex":0.0000011128303,"about_ca_system_score_gemma":0.00021535216,"threshold_uncertainty_score":0.6581893},"labels":[],"label_agreement":null},{"id":"W1999495305","doi":"10.1139/e00-114","title":"Palaeoenvironmental reconstruction of the Port Moody Interstade, a nonglacial interval in southwestern British Columbia at about 18 000 <sup>14</sup>C years BP","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University; Simon Fraser University","funders":"","keywords":"Palynology; Geology; Storm; Anticyclone; Temperate climate; Tephra; Winter storm; Holocene; Climatology; Oceanography; Physical geography; Paleontology; Geography; Volcano; Ecology","score_opus":0.015844716233683883,"score_gpt":0.20663651121221574,"score_spread":0.19079179497853185,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999495305","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995871,0.0003378539,0.000001045069,0.00016476093,0.00051689526,0.000096434065,0.000049983697,0.0000016887797,0.0029603406],"genre_scores_gemma":[0.9990151,0.00005995976,0.000061021616,0.000113498674,0.000061130835,2.9535317e-7,0.0000033166086,0.0000018994333,0.00068376935],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984564,0.00019026316,0.00041575596,0.00018927555,0.00028412882,0.0004641347],"domain_scores_gemma":[0.99927384,0.00007183532,0.00021045262,0.000101682235,0.000036002257,0.00030616138],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008968266,0.00007820306,0.00022042352,0.00019106721,0.0003197309,0.00012767893,0.00053280377,0.00010379607,0.0099263685],"category_scores_gemma":[0.00007738948,0.00008002131,0.00010018148,0.00038850267,0.0019601898,0.00030460846,0.000019547442,0.00033550896,0.000038385217],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017680086,0.0000054676857,0.99535567,0.0000031995098,0.000009682032,0.0002659679,0.0005037748,0.0006834218,0.0000018065177,6.230018e-7,0.00010575233,0.0030469506],"study_design_scores_gemma":[0.00032340828,0.00020322656,0.99281573,0.000091361966,0.000007025527,0.004126568,0.0010772257,0.00047215683,0.0000036739928,0.000104149876,0.00069491484,0.00008054244],"about_ca_topic_score_codex":0.084108636,"about_ca_topic_score_gemma":0.9820644,"teacher_disagreement_score":0.89795583,"about_ca_system_score_codex":0.0000037497923,"about_ca_system_score_gemma":0.0004905966,"threshold_uncertainty_score":0.9909787},"labels":[],"label_agreement":null},{"id":"W1999525847","doi":"10.1139/e02-102","title":"Dunes and associated sand transport in a tidally influenced sand-bed channel: Fraser River, British Columbia","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Institute for Advanced Research; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Sediment transport; Sand dune stabilization; Bathymetry; Hydrology (agriculture); Geomorphology; Population; Erosion; Channel (broadcasting); Sediment; Oceanography; Geotechnical engineering","score_opus":0.007188857490281264,"score_gpt":0.19007271756122732,"score_spread":0.18288386007094606,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999525847","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962481,0.00048398433,0.000007910084,0.00013202315,0.0001296348,0.00007996345,0.000010697792,0.0000038576454,0.0029038177],"genre_scores_gemma":[0.9991888,0.0000930874,0.00012141597,0.00040818122,0.000009173296,0.0000013921656,9.669911e-7,0.0000042257216,0.00017280507],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987718,0.000057674384,0.00030961153,0.00020553627,0.00024867457,0.00040669163],"domain_scores_gemma":[0.9993433,0.000037101487,0.00012441144,0.000047406156,0.000022358314,0.00042546375],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009094707,0.00008448403,0.00020365887,0.00008767194,0.00034553895,0.00010767359,0.00022028603,0.00009036454,0.0021444832],"category_scores_gemma":[0.00010846925,0.00010234701,0.0000375482,0.0005261448,0.0010992807,0.00055953744,0.0000033198594,0.00017675161,0.0000058107303],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000029876346,0.00001594846,0.99801445,0.0000028504048,0.0000063608964,0.00027604037,0.0005310808,0.00072241534,0.0001114988,0.0000029694625,0.00009214292,0.00022125972],"study_design_scores_gemma":[0.00061029335,0.00017713741,0.9951439,0.00006347889,0.000012043097,0.000070394846,0.000106609456,0.000029130131,0.00020208918,0.0009936112,0.0024530885,0.00013824295],"about_ca_topic_score_codex":0.08055663,"about_ca_topic_score_gemma":0.9428544,"teacher_disagreement_score":0.8622978,"about_ca_system_score_codex":0.00000931209,"about_ca_system_score_gemma":0.00040547314,"threshold_uncertainty_score":0.9987677},"labels":[],"label_agreement":null},{"id":"W1999595627","doi":"10.1139/e06-032","title":"The West Indian Road pit, central Nova Scotia: key to the Early Cretaceous Chaswood Formation","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Saint Mary's University; Dalhousie University","funders":"","keywords":"Geology; Batholith; Outcrop; Syncline; Geochemistry; Sedimentary rock; Cretaceous; Detritus; Basement; Paleocurrent; Sedimentology; Arenite; Lithology; Paleontology; Clastic rock; Tectonics","score_opus":0.014061663258839587,"score_gpt":0.1945317837912998,"score_spread":0.1804701205324602,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999595627","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97923315,0.0017784175,0.0000975059,0.009782768,0.00077221345,0.00012239834,0.000026940797,0.0000042827296,0.008182319],"genre_scores_gemma":[0.9988996,0.000026247892,0.00025170392,0.00043396943,0.00023572712,1.7429701e-7,0.0000041369776,0.0000010632564,0.0001474151],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986169,0.000062460036,0.0003342256,0.000093402865,0.00034250648,0.0005505457],"domain_scores_gemma":[0.99906856,0.00010193768,0.00018654275,0.000095748546,0.00013590023,0.00041129236],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00092895364,0.00009570333,0.00010211508,0.00016088133,0.0013948488,0.00072134176,0.0006946924,0.000039309416,0.0007720721],"category_scores_gemma":[0.00013846753,0.0000458616,0.000056779118,0.0007094175,0.00035610833,0.0007548585,0.000005192774,0.00017726263,0.0002960071],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011656843,0.000005189865,0.9384407,0.0000064644687,0.0000089755695,0.00003989373,0.002427962,0.024164012,0.0000030142726,0.00063997763,0.0026026226,0.031649522],"study_design_scores_gemma":[0.00006437114,0.00027894677,0.9545684,0.000016788932,0.000005025702,0.0001855565,0.00071481284,0.00052145123,0.000032015847,0.00074470876,0.042786185,0.00008172562],"about_ca_topic_score_codex":0.08230204,"about_ca_topic_score_gemma":0.9213788,"teacher_disagreement_score":0.83907676,"about_ca_system_score_codex":0.0000025427817,"about_ca_system_score_gemma":0.00064037234,"threshold_uncertainty_score":0.9999052},"labels":[],"label_agreement":null},{"id":"W1999933416","doi":"10.1139/e05-095","title":"<sup>40</sup>Ar/<sup>39</sup>Ar dates on hornblende, muscovite, and biotite from the Mica Creek area, British Columbia: regional metamorphic and tectonic implications","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Metamorphic rock; Hornblende; Muscovite; Biotite; Precambrian; Metamorphic facies; Gneiss; Geochemistry; Tectonics; Sillimanite; Staurolite; Tectonic phase; Mica; Seismology; Schist; Geomorphology; Paleontology; Facies; Quartz","score_opus":0.01761805375973572,"score_gpt":0.17856411250922416,"score_spread":0.16094605874948845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999933416","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9851832,0.0060116164,0.000007256771,0.0071486556,0.00003861087,0.00010218726,0.0005077429,0.000008165962,0.0009925828],"genre_scores_gemma":[0.99723446,0.00036032757,0.0006186988,0.0012152488,0.00019346506,9.346753e-7,0.00006477144,0.000002808683,0.0003092708],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980669,0.00012141106,0.0004264467,0.00045524948,0.00037387686,0.0005560941],"domain_scores_gemma":[0.9981813,0.000608501,0.00021201096,0.00018701806,0.0001365802,0.0006745824],"candidate_categories":["scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005403754,0.00016288638,0.0003364623,0.00013888712,0.0012005925,0.0011771634,0.0005949905,0.00009612244,0.004115012],"category_scores_gemma":[0.00020967284,0.00013444072,0.00013275743,0.00080591376,0.0015939962,0.0003685822,0.000019996469,0.00033737955,0.00002230351],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005247291,0.000012018643,0.9881425,0.0000028061377,0.000039527196,0.00004614488,0.00004064082,0.0035924767,0.00004687805,0.000027974696,0.0038969852,0.004146826],"study_design_scores_gemma":[0.00019358902,0.0002129541,0.9694008,0.000053202006,0.00007555344,0.00025545884,0.0002450313,0.003218706,0.000008741319,0.01307892,0.013061437,0.00019557384],"about_ca_topic_score_codex":0.5910287,"about_ca_topic_score_gemma":0.94872856,"teacher_disagreement_score":0.35769984,"about_ca_system_score_codex":0.0000034129514,"about_ca_system_score_gemma":0.00040639116,"threshold_uncertainty_score":0.9998597},"labels":[],"label_agreement":null},{"id":"W1999950860","doi":"10.1139/e05-103","title":"Le magmatisme de la région de Kwyjibo, Province du Grenville (Canada) : intérêt pour les minéralisations de type fer-oxydes associées","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Geochemistry; Pluton; Biotite; Monazite; Mineralization (soil science); Leucogranite; Pegmatite; Amphibole; Allanite; Rare-earth element; Uranium; Mineralogy; Quartz; Zircon; Gneiss; Rare earth; Metamorphic rock","score_opus":0.011402818423979446,"score_gpt":0.1906961002445232,"score_spread":0.17929328182054374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999950860","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9747566,0.0007257575,0.0000966546,0.01565215,0.000059381233,0.000028663893,0.000021405687,0.0000042390475,0.008655154],"genre_scores_gemma":[0.9930403,0.000043506156,0.0056858123,0.0007489968,0.00019369426,1.8136657e-7,0.0000034112622,0.0000014525174,0.00028261196],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987403,0.00017073083,0.00023245558,0.00013295762,0.00025111018,0.00047241672],"domain_scores_gemma":[0.9987776,0.00026850347,0.00014769197,0.000060620732,0.00009847088,0.00064710726],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009666533,0.0000975627,0.00015898899,0.00012731447,0.000542777,0.00014804068,0.0004039834,0.000066907334,0.0027679878],"category_scores_gemma":[0.0005850179,0.00007420811,0.00007065741,0.00034518348,0.0004436508,0.0001985866,0.0000063199573,0.00019268497,0.0000141805685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000032669059,0.0000068969102,0.9794416,0.0000029548296,0.000012045441,0.000049207287,0.00010798119,0.012135776,0.00015313485,0.000485578,0.0016201726,0.005981396],"study_design_scores_gemma":[0.000101630794,0.00008755926,0.9581925,0.0000214502,0.000020144727,0.00018703067,0.00046665122,0.007904448,0.00043155818,0.0068464526,0.025610408,0.00013012462],"about_ca_topic_score_codex":0.6796013,"about_ca_topic_score_gemma":0.9933042,"teacher_disagreement_score":0.31370288,"about_ca_system_score_codex":0.00001616668,"about_ca_system_score_gemma":0.007003056,"threshold_uncertainty_score":0.9986263},"labels":[],"label_agreement":null},{"id":"W2000019012","doi":"10.1139/e02-072","title":"Extending the ancient margin outboard in the Canadian Cordillera: record of Proterozoic crust and Paleocene regional metamorphism in the Nicola horst, southern British Columbia","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Vernon Jubilee Hospital; Geological Survey of Canada; Simon Fraser University; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta","keywords":"Geology; Terrane; Felsic; Metamorphism; Geochemistry; Proterozoic; Plutonism; Zircon; Allochthon; Batholith; Continental crust; Horst; Island arc; Anatexis; Petrology; Crust; Nappe; Mafic; Paleontology; Subduction; Pluton; Partial melting; Tectonics","score_opus":0.03424937449596764,"score_gpt":0.1882261612858705,"score_spread":0.15397678678990284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000019012","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9856869,0.0035593167,6.028713e-7,0.008339567,0.0000836893,0.00018116043,0.000041695755,8.493391e-7,0.0021062156],"genre_scores_gemma":[0.99775434,0.00012493147,0.000121186866,0.0018270055,0.00006118352,0.0000016887132,0.0000017572922,0.000001091098,0.0001068099],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99815667,0.00030337885,0.0003902599,0.00019396102,0.0004577193,0.00049803604],"domain_scores_gemma":[0.99903256,0.00024746463,0.0001922445,0.0001228478,0.00007543249,0.0003294738],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0022710175,0.0000927743,0.00022902228,0.00017890282,0.0006498002,0.00049786817,0.00083920144,0.000053015323,0.0042130337],"category_scores_gemma":[0.00024241973,0.0000546843,0.000090795176,0.0010568795,0.0009989884,0.00014876001,0.000006254374,0.00036218204,0.000007647284],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000017979555,0.0000075498783,0.9909099,0.0000029192267,0.000006992919,0.00013178092,0.0008096572,0.00023810382,0.000002795707,0.00000835203,0.00089116266,0.006989011],"study_design_scores_gemma":[0.00012546795,0.00013940452,0.9885036,0.00004892664,0.000015086564,0.0002241813,0.0022133426,0.0015731599,7.357864e-7,0.0010871111,0.0059807836,0.000088249435],"about_ca_topic_score_codex":0.92973226,"about_ca_topic_score_gemma":0.9997248,"teacher_disagreement_score":0.06999257,"about_ca_system_score_codex":0.000004769141,"about_ca_system_score_gemma":0.0003354949,"threshold_uncertainty_score":0.99669725},"labels":[],"label_agreement":null},{"id":"W2000055411","doi":"10.1139/e02-007","title":"Correlation chart of the eastern Grenville Province and its northern foreland","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Government of Newfoundland and Labrador; Royal Ontario Museum","funders":"","keywords":"Geology; Foreland basin; Chart; Seismology; Geochemistry; Tectonics; Statistics; Mathematics","score_opus":0.020475693862280757,"score_gpt":0.1813023454388603,"score_spread":0.16082665157657955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000055411","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9825869,0.0010930772,0.0009939541,0.005530236,0.00033805543,0.000061937615,0.0000014312154,0.000001941095,0.009392423],"genre_scores_gemma":[0.99864185,0.0000064949013,0.00021266317,0.00006610268,0.000027864604,1.6422145e-7,2.2380819e-8,4.5148258e-7,0.0010444053],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99942636,0.000024086234,0.00015282586,0.000090858186,0.0001554979,0.00015038325],"domain_scores_gemma":[0.99943614,0.000027641527,0.00019445474,0.00008738516,0.000109379645,0.0001450202],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030951278,0.000047007747,0.000073339084,0.00005662125,0.00021574114,0.000058916754,0.0004975548,0.000024242701,0.000035983565],"category_scores_gemma":[0.00012727923,0.00002963553,0.000028393337,0.0002166136,0.00017094557,0.00022032703,0.000026693942,0.00008158226,0.0000036324077],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[7.4555027e-7,0.0000064049973,0.98715746,0.000014395994,0.00000617672,0.00001863644,0.0014475947,0.0026551362,0.00017644091,0.0035794529,0.00014742339,0.0047901315],"study_design_scores_gemma":[0.0005572426,0.00046255966,0.41449213,0.00032982772,0.000014847237,0.00095881196,0.0004235734,0.5402809,0.0021481914,0.004519827,0.035504915,0.00030720726],"about_ca_topic_score_codex":0.00021487048,"about_ca_topic_score_gemma":0.016684573,"teacher_disagreement_score":0.57266533,"about_ca_system_score_codex":0.000002188346,"about_ca_system_score_gemma":0.000244418,"threshold_uncertainty_score":0.9310383},"labels":[],"label_agreement":null},{"id":"W2000102304","doi":"10.1139/e04-042","title":"Applications of earth science techniques to archaeological problems Introduction","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Image Processing and 3D Reconstruction","field":"Computer Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Okanagan University College","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Basalt; Geology; Earth science; Mineralogy; Electron microprobe; Geochemistry; Thematic map; Archaeology; Geography","score_opus":0.013973503070922877,"score_gpt":0.2431264385207114,"score_spread":0.22915293544978851,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000102304","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1145415,0.0002733451,0.87464213,0.008409207,0.0005801928,0.00020068673,0.0000014165839,0.000027762775,0.0013237589],"genre_scores_gemma":[0.72488153,0.000006525043,0.27482426,0.00009336745,0.00015940618,0.0000031062052,5.673342e-8,0.0000013648322,0.000030363672],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9987902,0.00002033401,0.000294474,0.00023915572,0.00035388285,0.00030193213],"domain_scores_gemma":[0.9987015,0.000013944696,0.0002148467,0.00016475037,0.00051107723,0.00039387264],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013404028,0.00007041593,0.00012510459,0.0009242203,0.0005001044,0.00020101125,0.0010693284,0.00002906167,0.000009183581],"category_scores_gemma":[0.00015788605,0.000054899716,0.000037622318,0.002251735,0.00183282,0.0010204136,0.00004153722,0.0001362163,0.0000056274794],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000060507255,0.00007643485,0.013994569,0.00005372678,0.000012451157,0.000021577296,0.0046856743,0.009100408,0.05666173,0.18489015,0.00013138697,0.7303659],"study_design_scores_gemma":[0.00050108286,0.0029156634,0.028709732,0.00045099724,0.000018475459,0.0042593456,0.00082366506,0.0012759718,0.73414105,0.14539646,0.08078994,0.0007175882],"about_ca_topic_score_codex":0.00059748575,"about_ca_topic_score_gemma":0.0036870677,"teacher_disagreement_score":0.72964823,"about_ca_system_score_codex":0.000011336093,"about_ca_system_score_gemma":0.004128919,"threshold_uncertainty_score":0.7324525},"labels":[],"label_agreement":null},{"id":"W2000210226","doi":"10.1139/e05-075","title":"Geochemical and isotopic evidence for a genetic link between Canadian Shield brines, dolomitization in the Western Canada Sedimentary Basin, and Devonian calcium-chloridic seawater","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Light Source (Canada); University of Saskatchewan; Carleton University; Canadian Nuclear Safety Commission","funders":"Canadian Nuclear Safety Commission","keywords":"Dolomitization; Geology; Geochemistry; Devonian; Paleozoic; Seawater; Sedimentary rock; Diagenesis; Fluid inclusions; Anhydrite; Mineralogy; Hydrothermal circulation; Structural basin; Paleontology; Facies; Oceanography; Gypsum","score_opus":0.03306118949198419,"score_gpt":0.23467921365727373,"score_spread":0.20161802416528954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000210226","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98216236,0.002002247,0.000017443643,0.015380031,0.00012705168,0.00014518813,0.00005133873,0.0000010844611,0.00011326264],"genre_scores_gemma":[0.9965216,0.000045315606,0.00043846545,0.002437676,0.0004927874,8.810647e-7,0.000011176465,0.0000019659285,0.000050151855],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988274,0.00004871924,0.0002716837,0.0001899202,0.00020519119,0.00045711658],"domain_scores_gemma":[0.9989776,0.00019665321,0.00006934747,0.00007897248,0.000047786616,0.00062960916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006079907,0.00011413133,0.00015536425,0.00014614461,0.00030754818,0.00022000198,0.00031668536,0.00005553024,0.00010949991],"category_scores_gemma":[0.00007251173,0.000080882695,0.000022577184,0.00018315141,0.00023431564,0.00033371957,0.000004755493,0.00015954072,0.0000012441054],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000030167075,4.1666345e-7,0.99304956,0.000011749549,0.000004129317,0.000029004055,0.00032925518,0.00008326063,0.000008115443,8.9998144e-7,0.0002816768,0.0061988854],"study_design_scores_gemma":[0.00017369846,0.00008736761,0.97022367,0.00006605383,0.000014058805,0.00019857788,0.00020018689,0.00032184515,0.0002982913,0.000060414906,0.02823981,0.00011603222],"about_ca_topic_score_codex":0.9847793,"about_ca_topic_score_gemma":0.9995005,"teacher_disagreement_score":0.027958134,"about_ca_system_score_codex":0.000014095386,"about_ca_system_score_gemma":0.0026547522,"threshold_uncertainty_score":0.47094163},"labels":[],"label_agreement":null},{"id":"W2000228659","doi":"10.1139/e06-003","title":"Coupled landscape-lake evolution in High Arctic Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Rimouski; Université Laval; Center for Northern Studies","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Networks of Centres of Excellence of Canada; Parks Canada","keywords":"Oceanography; Shelf ice; Geology; Fjord; Limnology; Arctic; Meltwater; Halocline; Sea ice; Water column; Hydrology (agriculture); Ice shelf; Cryosphere; Snow; Geomorphology; Salinity","score_opus":0.01657045033970921,"score_gpt":0.1913113968993153,"score_spread":0.1747409465596061,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000228659","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994191,0.0013849509,0.000003867995,0.00088847394,0.0008171961,0.000042277472,0.00031181544,0.0000013882412,0.002359055],"genre_scores_gemma":[0.9992991,0.000015162824,0.00004808985,0.00021241598,0.00024491586,9.228134e-8,0.000064559215,0.0000013126004,0.00011436013],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988754,0.00003569543,0.0002710872,0.00011450829,0.0002901181,0.00041322966],"domain_scores_gemma":[0.9993487,0.00008126848,0.00012406983,0.000058098518,0.00007283414,0.00031503584],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004815348,0.00008336131,0.00014667181,0.0002942134,0.00021751951,0.00010274628,0.00024673584,0.000033449043,0.0071347174],"category_scores_gemma":[0.000045489964,0.00006634413,0.000029577266,0.0005392869,0.00014999388,0.0002710758,0.0000017252403,0.00012624888,0.000017439645],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003305964,0.0000015267045,0.9928544,0.0000036466236,0.0000012452182,0.00014040282,0.000031205756,0.006144115,0.0000072130924,0.000060998278,0.0006639932,0.00008795564],"study_design_scores_gemma":[0.00019082808,0.000072841314,0.9915383,0.000034918638,0.0000036564527,0.00010308456,0.00022860829,0.0022942845,0.000003770405,0.00047610057,0.0049616187,0.000091983165],"about_ca_topic_score_codex":0.99495506,"about_ca_topic_score_gemma":0.99999565,"teacher_disagreement_score":0.007117278,"about_ca_system_score_codex":0.000007865268,"about_ca_system_score_gemma":0.003154884,"threshold_uncertainty_score":0.9937729},"labels":[],"label_agreement":null},{"id":"W2000505601","doi":"10.1139/e04-092","title":"Origin of Recent alkaline lavas by lithospheric thinning beneath the northern Canadian Cordillera","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Basalt; Radiogenic nuclide; Mantle (geology); Lithosphere; Partial melting; Peridotite; Olivine; Amphibole; Tectonics; Paleontology","score_opus":0.019791390679577216,"score_gpt":0.20572416689545892,"score_spread":0.1859327762158817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000505601","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97386867,0.0036824713,0.0000073544043,0.010218848,0.00016299928,0.000049400376,0.00006105278,0.0000027446972,0.0119464835],"genre_scores_gemma":[0.9973248,0.00019980378,0.00084446964,0.0012453846,0.00014780283,1.2744955e-7,0.000008679091,0.000001445396,0.00022745367],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99851376,0.000068868314,0.0003883666,0.00016201266,0.00035811582,0.0005088867],"domain_scores_gemma":[0.9983552,0.00011345392,0.0002283247,0.00011340606,0.00021735243,0.00097224355],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007920765,0.00012099239,0.00023693294,0.0001287804,0.00046535875,0.00009687159,0.00067553786,0.000051066636,0.023524983],"category_scores_gemma":[0.00018515319,0.00006659794,0.00010490578,0.00090990914,0.00053977995,0.00020496242,0.0000046258806,0.00022212013,0.000063331565],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000042552706,0.000005701606,0.9611531,0.0000018829475,0.000028137672,0.000019452471,0.00025240067,0.009764501,0.00005074617,0.000036144385,0.0010169705,0.027666742],"study_design_scores_gemma":[0.0002453267,0.0004996626,0.44955245,0.00004553373,0.00006809439,0.00010273624,0.00096422347,0.0077948645,0.00066517835,0.0014060618,0.53833145,0.0003244436],"about_ca_topic_score_codex":0.693593,"about_ca_topic_score_gemma":0.99378854,"teacher_disagreement_score":0.5373145,"about_ca_system_score_codex":0.000005483809,"about_ca_system_score_gemma":0.0014531097,"threshold_uncertainty_score":0.97736764},"labels":[],"label_agreement":null},{"id":"W2000578827","doi":"10.1139/e09-058","title":"Paleomagnetic and geochemical evidence for a pre-Triassic age for the Lower Amaranth Member of the Williston Basin of Manitoba (Canada)","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor; Western University","funders":"American Academy of Sleep Medicine","keywords":"Geology; Dolomite; Dolomitization; Carboniferous; Red beds; Diagenesis; Paleontology; Pennsylvanian; Permian; Paleomagnetism; Geochemistry; Devonian; Sedimentary rock; Structural basin","score_opus":0.03720917698690113,"score_gpt":0.24631346847676394,"score_spread":0.20910429148986281,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000578827","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9821973,0.013522346,0.000038052443,0.0025515265,0.0004065213,0.0002470691,0.000063849155,6.802008e-7,0.00097264664],"genre_scores_gemma":[0.99911433,0.000057980535,0.0005866911,0.00016024285,0.00005961723,4.6235488e-7,2.1322822e-7,3.877744e-7,0.00002007377],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990014,0.00005309047,0.00030123646,0.00012079018,0.0002598168,0.00026368618],"domain_scores_gemma":[0.99842274,0.00090646296,0.00027038576,0.000109499575,0.00010424763,0.00018665471],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00084604404,0.00008477574,0.00019604899,0.00006986204,0.00035998455,0.000042171596,0.00050326565,0.000046551428,0.000042315245],"category_scores_gemma":[0.00047794264,0.000045208963,0.00010903561,0.00021848183,0.0010678488,0.00018228362,8.532831e-7,0.00010061836,3.8489972e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001670152,0.000009700795,0.94709724,0.000037349102,0.000029023038,0.000014229548,0.00028070767,0.0002034241,0.000335154,0.00021210861,0.0011219996,0.050492067],"study_design_scores_gemma":[0.00019425913,0.0006607066,0.9961421,0.00011596207,0.000039000388,0.00004486064,0.00011911166,0.00054951804,0.0004211198,0.0008572177,0.00079620304,0.000059940256],"about_ca_topic_score_codex":0.10202007,"about_ca_topic_score_gemma":0.9783714,"teacher_disagreement_score":0.8763513,"about_ca_system_score_codex":0.0000012357441,"about_ca_system_score_gemma":0.0015169103,"threshold_uncertainty_score":0.90395963},"labels":[],"label_agreement":null},{"id":"W2000616987","doi":"10.1139/e05-017","title":"Electrical-resistivity imaging of the central Trans-Hudson orogen","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Manitoba","funders":"","keywords":"Magnetotellurics; Geology; Archean; Crust; Terrane; Craton; Seismology; Electrical resistivity and conductivity; Petrology; Tectonics; Lithosphere; Geophysics; Geochemistry","score_opus":0.014923985218208128,"score_gpt":0.22158159879420197,"score_spread":0.20665761357599385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000616987","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98998183,0.0021314835,0.00027309672,0.003928625,0.0003469967,0.0000672704,0.000018443498,0.0000028453496,0.0032494059],"genre_scores_gemma":[0.9970999,0.000014659538,0.0022887422,0.00031489582,0.0001982677,5.1846204e-8,2.5090202e-7,0.0000011273432,0.00008214572],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985467,0.00016751044,0.00027895314,0.00012672214,0.00035801358,0.00052208686],"domain_scores_gemma":[0.99894804,0.00019904999,0.00016718208,0.00008480098,0.00007912777,0.0005217845],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007178166,0.000088980254,0.00018286642,0.00013481082,0.00032009315,0.0000625359,0.0005607569,0.000027650218,0.00075097167],"category_scores_gemma":[0.00026901552,0.00005128133,0.00015257238,0.0009647113,0.0004379218,0.00025975227,0.0000026691007,0.00020353582,0.000009699875],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007976797,0.000008903228,0.63196814,0.000003068733,0.0000073085334,0.000008357843,0.0001224219,0.0021378843,0.00020048807,0.00021439367,0.00014651999,0.36517456],"study_design_scores_gemma":[0.00009409088,0.00012216828,0.9829728,0.000015430958,0.000013576203,0.000038209684,0.000022033202,0.0030462046,0.0021169786,0.001366606,0.010115801,0.00007611096],"about_ca_topic_score_codex":0.011896084,"about_ca_topic_score_gemma":0.1202892,"teacher_disagreement_score":0.36509845,"about_ca_system_score_codex":0.0000024729977,"about_ca_system_score_gemma":0.0010147556,"threshold_uncertainty_score":0.9946838},"labels":[],"label_agreement":null},{"id":"W2000744341","doi":"10.1139/e06-059","title":"Neoarchean trans-subprovince sediment transport in southwestern Superior Province: sedimentological, geochemical, and geochronological evidence","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Lakehead University","funders":"","keywords":"Geology; Sedimentary rock; Geochemistry; Sedimentology; Zircon; Subduction; Island arc; Outcrop; Structural basin; Back-arc basin; Volcanic arc; Paleontology; Tectonics","score_opus":0.021528919707424522,"score_gpt":0.20894109912915093,"score_spread":0.18741217942172642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000744341","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9919255,0.003975246,0.000027800661,0.0029588216,0.00008399272,0.00012837825,0.000026845544,0.0000086145565,0.00086480635],"genre_scores_gemma":[0.9983518,0.00006705021,0.0011218553,0.00029778876,0.00009730454,7.4470137e-7,0.0000073454116,0.0000015995689,0.00005449346],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99772835,0.000088297274,0.0006171214,0.0004149944,0.0004202639,0.0007309535],"domain_scores_gemma":[0.9987946,0.00022455568,0.00015525847,0.00010281746,0.000072401446,0.0006503294],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009684833,0.00020964036,0.00040612937,0.00025760534,0.00025737376,0.00012052798,0.00051711174,0.00012959087,0.0034833304],"category_scores_gemma":[0.00010919945,0.00013624266,0.00012661057,0.000524496,0.0015983763,0.00042512975,0.00000817733,0.00035823963,0.000016276816],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024236002,0.000019217909,0.99550384,0.000011795033,0.0000055218893,0.00028984467,0.00006886743,0.0010807213,0.0007931973,0.000046102512,0.000016192467,0.0021404473],"study_design_scores_gemma":[0.00028074358,0.00058595714,0.99242675,0.000082384875,0.000025004892,0.0001493693,0.00018786354,0.000758424,0.0006988577,0.0035696956,0.0010143364,0.00022062437],"about_ca_topic_score_codex":0.07730677,"about_ca_topic_score_gemma":0.6492126,"teacher_disagreement_score":0.5719058,"about_ca_system_score_codex":0.0000057995935,"about_ca_system_score_gemma":0.0007916402,"threshold_uncertainty_score":0.99742764},"labels":[],"label_agreement":null},{"id":"W2000964276","doi":"10.1139/e10-019","title":"Significance of “gneissic” rocks in the Liscomb Complex, Nova Scotia","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University","keywords":"Geology; Geochemistry; Pluton; Gneiss; Amphibole; Sillimanite; Metamorphic rock; Greenschist; Igneous rock; Zircon; Xenolith; Metamorphic facies; Felsic; Petrology; Mafic; Basalt; Biotite; Facies; Quartz; Geomorphology; Paleontology","score_opus":0.029723572989948488,"score_gpt":0.217973654454371,"score_spread":0.18825008146442251,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000964276","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9876001,0.000262439,0.0000102878075,0.0024118216,0.00023187813,0.000043687152,0.000015287616,9.964774e-7,0.009423504],"genre_scores_gemma":[0.99887776,0.000003966889,0.00059052045,0.000418383,0.00008110945,4.3722665e-8,0.0000020313576,5.0338014e-7,0.000025691897],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988706,0.000066684755,0.00032830614,0.00012316827,0.00029645706,0.00031479096],"domain_scores_gemma":[0.9991216,0.0002167737,0.0001841064,0.00010177663,0.00008218485,0.00029353137],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010775046,0.00008010501,0.00019511308,0.00020370835,0.0001331745,0.00007577292,0.0008264962,0.00004066312,0.010467986],"category_scores_gemma":[0.00023655595,0.000042658252,0.00008871044,0.00087766524,0.00086505804,0.0001716742,0.000003875746,0.00031576853,0.000037467482],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002825268,0.0000060048874,0.99559736,0.0000025382449,0.0000035241155,0.000023987233,0.0001458471,0.0015879392,0.0005804873,0.00012252586,0.00013358101,0.0017933678],"study_design_scores_gemma":[0.00007760805,0.00015089281,0.991295,0.000010987867,0.000007752955,0.00004871108,0.0003301322,0.0008056583,0.0002641263,0.004880052,0.0020596,0.000069501104],"about_ca_topic_score_codex":0.13019162,"about_ca_topic_score_gemma":0.94008726,"teacher_disagreement_score":0.8098956,"about_ca_system_score_codex":3.8467033e-7,"about_ca_system_score_gemma":0.0004415038,"threshold_uncertainty_score":0.99043655},"labels":[],"label_agreement":null},{"id":"W2001218580","doi":"10.1139/e99-039","title":"Crustal formation in the Grenville Province: Nd-isotope evidence","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":122,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada; McMaster University","keywords":"Geology; Precambrian; Geochemistry; Shield; Isotope; Archean; Paleontology","score_opus":0.024893321774866733,"score_gpt":0.20466131887767816,"score_spread":0.17976799710281144,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001218580","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9835647,0.0017927295,0.0000044914977,0.003531699,0.00005617488,0.000056493118,0.0000055620108,0.0000012834141,0.010986862],"genre_scores_gemma":[0.99880064,0.000080449274,0.0002046787,0.0007170909,0.00006529337,1.716005e-7,0.0000012336483,3.502593e-7,0.00013012112],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99890804,0.00009796695,0.00026630395,0.00010429616,0.0003131929,0.00031022023],"domain_scores_gemma":[0.99941844,0.00014666357,0.00008672109,0.0000678974,0.000041642,0.00023861662],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00096828426,0.000068804766,0.000115417475,0.00014048669,0.0002747314,0.00015214541,0.00055586314,0.000030007863,0.017502978],"category_scores_gemma":[0.00016922233,0.000035602818,0.000066328575,0.0006535533,0.0003403205,0.0005554379,0.0000018498592,0.00016499018,0.00013399449],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014100906,0.00000720973,0.9340187,0.0000058761593,0.000003842943,0.0001892722,0.0005738328,0.009145791,0.000030081668,0.00010552434,0.00040188598,0.055503923],"study_design_scores_gemma":[0.000097495074,0.0003376299,0.97850233,0.000060688984,0.000009914649,0.00026877402,0.0006670872,0.003873873,0.000097223485,0.0048910268,0.011080395,0.00011354742],"about_ca_topic_score_codex":0.031459127,"about_ca_topic_score_gemma":0.6660568,"teacher_disagreement_score":0.6345977,"about_ca_system_score_codex":0.000001303638,"about_ca_system_score_gemma":0.0003307754,"threshold_uncertainty_score":0.98339516},"labels":[],"label_agreement":null},{"id":"W2001273809","doi":"10.1139/e03-006","title":"Constraints on early Archean crustal extraction and tholeiitic-komatiitic volcanism in greenstone belts of the Northern Superior Province","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"McGill University; Ministère des Ressources naturelles et des Forêts (Québec)","funders":"McGill University","keywords":"Archean; Greenstone belt; Geology; Geochemistry; Basalt; Mantle (geology); Trace element; Incompatible element; Rare-earth element; Partial melting; Mineralogy; Rare earth","score_opus":0.015136435235943354,"score_gpt":0.19781402806581982,"score_spread":0.18267759282987647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001273809","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949244,0.00020913279,0.000005240956,0.00058837596,0.00009583439,0.0000606992,0.00001674123,0.0000010385262,0.0040985183],"genre_scores_gemma":[0.99957985,0.000006170342,0.00024410438,0.00011298505,0.000015866459,9.739494e-8,3.9969754e-7,7.4561467e-7,0.000039789287],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989661,0.00010921363,0.000268813,0.0001299642,0.00025414772,0.00027178318],"domain_scores_gemma":[0.9993166,0.00012921706,0.00013591709,0.00006393851,0.00006280057,0.0002915282],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00057028554,0.00008168699,0.0001632434,0.00015077979,0.00019029176,0.000049577513,0.00019824109,0.00003707468,0.00092528993],"category_scores_gemma":[0.00032166185,0.000047460024,0.000059009697,0.0003404196,0.0013608391,0.000164236,0.0000028442812,0.00018967877,0.0000060275424],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000039339975,0.000006113958,0.9900096,0.0000040742657,0.00000417288,0.000034288772,0.0001562088,0.0005643986,0.00018169837,0.00026592874,0.0000014619942,0.008768129],"study_design_scores_gemma":[0.000120164295,0.00023148788,0.995267,0.00004548274,0.000008174382,0.00011031447,0.0004650143,0.00020930843,0.0005458232,0.002870863,0.000061932406,0.0000644705],"about_ca_topic_score_codex":0.03245283,"about_ca_topic_score_gemma":0.85280097,"teacher_disagreement_score":0.82034814,"about_ca_system_score_codex":0.00000215976,"about_ca_system_score_gemma":0.00064814015,"threshold_uncertainty_score":0.999988},"labels":[],"label_agreement":null},{"id":"W2001321376","doi":"10.1139/e05-003","title":"Reappraisal of the Cambrian glauconite-bearing Anse Maranda Formation, Quebec Appalachians: from deep-sea turbidites to clastic shelf deposits","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Chicoutimi","funders":"Agence Nationale de Sécurité Sanitaire de l’Alimentation, de l’Environnement et du Travail","keywords":"Geology; Glauconite; Clastic rock; Bioturbation; Turbidite; Arenite; Sedimentary depositional environment; Sedimentary rock; Paleontology; Diagenesis; Geochemistry; Sedimentary structures; Geomorphology; Sediment; Structural basin","score_opus":0.014031468673336768,"score_gpt":0.20610224172851901,"score_spread":0.19207077305518225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001321376","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939123,0.0010562785,0.0007913914,0.0016089984,0.00038386806,0.0000938836,0.00008399603,0.000004243373,0.0020650877],"genre_scores_gemma":[0.9961458,0.000018330726,0.0032016805,0.0004119464,0.00015373908,2.929514e-7,0.000006974319,0.0000014169625,0.000059822723],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986989,0.00007348094,0.00042763262,0.00011730104,0.0003218722,0.00036082068],"domain_scores_gemma":[0.99874115,0.00031871212,0.00022959875,0.00010625141,0.00016157884,0.00044268044],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005272619,0.00010720801,0.0001687107,0.00022365437,0.0005206574,0.00021980253,0.00059785997,0.00005049716,0.0007346048],"category_scores_gemma":[0.0004771558,0.00006507142,0.00007297413,0.0006507376,0.00029299821,0.0009217763,0.000008373164,0.00016338799,0.000042385233],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010870711,0.000003350279,0.97053397,0.000008383395,0.0000077715695,0.0000030486144,0.0009788111,0.014399438,0.000019962483,0.00016001552,0.000067670284,0.013806711],"study_design_scores_gemma":[0.00013363577,0.00013419936,0.9874301,0.00007775712,0.0000152225875,0.000051175237,0.0006796704,0.004169706,0.00028348056,0.00029506197,0.0066239,0.00010610296],"about_ca_topic_score_codex":0.14702517,"about_ca_topic_score_gemma":0.9692201,"teacher_disagreement_score":0.82219493,"about_ca_system_score_codex":0.000002759583,"about_ca_system_score_gemma":0.0008651047,"threshold_uncertainty_score":0.85865486},"labels":[],"label_agreement":null},{"id":"W2001357926","doi":"10.1139/e10-079","title":"Timing of Paleoproterozoic granitoid magmatism along the northwestern Superior Province margin: implications for the tectonic evolution of the Thompson Nickel BeltThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto; Manitoba Hydro; Université du Québec à Montréal; University of Alberta","funders":"","keywords":"Geology; Magmatism; Craton; Geochemistry; Pegmatite; Metamorphism; Felsic; Geochronology; Partial melting; Pluton; Tectonics; Paleontology; Mafic; Crust","score_opus":0.02252372179543578,"score_gpt":0.19107712778850494,"score_spread":0.16855340599306917,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001357926","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931136,0.0007098177,0.000005701662,0.0048998254,0.00007130654,0.00032430692,0.0001079608,6.403389e-7,0.00076686154],"genre_scores_gemma":[0.9995728,0.0000586599,0.00024182822,0.000056950375,0.000040868577,0.0000028157795,8.733398e-7,0.0000013125803,0.00002387847],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985343,0.00014525412,0.0006822563,0.00013607765,0.00025842257,0.00024363823],"domain_scores_gemma":[0.99841464,0.0003999971,0.00069598184,0.00023765702,0.00018938299,0.000062343286],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001249694,0.000095678384,0.00032002138,0.00015240055,0.00015823392,0.000013414272,0.0008684848,0.000052903066,0.0029709856],"category_scores_gemma":[0.0003272982,0.00004282594,0.00015639517,0.00083859614,0.0017011559,0.0002214842,0.000021120417,0.00017720948,7.0495423e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005516296,0.00003731207,0.9882147,0.000039899736,0.00003006719,4.7205504e-7,0.0028825055,0.0003914318,0.0037856188,0.0003510667,0.000018476258,0.004193325],"study_design_scores_gemma":[0.00016053038,0.00037171747,0.97305334,0.00012975647,0.000034126548,0.000006633278,0.0020827781,0.00030730347,0.021223217,0.0025118692,0.00007044954,0.00004827252],"about_ca_topic_score_codex":0.07703898,"about_ca_topic_score_gemma":0.75038224,"teacher_disagreement_score":0.6733433,"about_ca_system_score_codex":0.000004548579,"about_ca_system_score_gemma":0.00053357414,"threshold_uncertainty_score":0.9979404},"labels":[],"label_agreement":null},{"id":"W2001435359","doi":"10.1139/e06-017","title":"Structural analysis of the Miniss River and related faults, western Superior Province: post-collisional displacement initiated at terrane boundaries","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Queen's University; University of Regina","funders":"","keywords":"Terrane; Geology; Sinistral and dextral; Strike-slip tectonics; Fault (geology); Seismology; Transpression; Geochronology; Transform fault; Tectonics; Paleontology; Geomorphology","score_opus":0.011370499119626213,"score_gpt":0.1996924041201343,"score_spread":0.1883219050005081,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001435359","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99675953,0.000814133,7.8505565e-7,0.0014989921,0.00015410555,0.000058458932,0.00021401778,0.0000017908897,0.0004981702],"genre_scores_gemma":[0.99939454,0.0000065951226,0.00010812114,0.00015070873,0.00002061675,9.272417e-8,0.0000300312,7.934128e-7,0.00028851043],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986123,0.000080051526,0.00042801476,0.00017763239,0.0004088194,0.00029317694],"domain_scores_gemma":[0.99914044,0.00009841463,0.00025741584,0.00008408829,0.0001473429,0.00027226843],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00033332952,0.00011557433,0.00028812978,0.00026414506,0.0007090714,0.00012709001,0.0003397621,0.000052476855,0.0036988154],"category_scores_gemma":[0.00008805424,0.00006013728,0.00016737505,0.0010056142,0.002315126,0.00022178233,0.000017888826,0.00011743607,0.000004167575],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017368931,0.00000284529,0.9950946,0.0000030000558,0.00008556871,0.000023218392,0.00020424869,0.0041724946,0.000116721916,0.000041566476,0.000016453734,0.00022191122],"study_design_scores_gemma":[0.00014889066,0.00015694201,0.9948877,0.00001370568,0.00021738073,0.000057056182,0.00014898708,0.002762839,0.0001689503,0.00075581146,0.000590081,0.00009163684],"about_ca_topic_score_codex":0.059837,"about_ca_topic_score_gemma":0.75585216,"teacher_disagreement_score":0.6960152,"about_ca_system_score_codex":0.0000032845785,"about_ca_system_score_gemma":0.0005631501,"threshold_uncertainty_score":0.99721193},"labels":[],"label_agreement":null},{"id":"W2001521872","doi":"10.1139/e04-093","title":"Crustal structure across the northern Cordillera, Yukon Territory, from seismic wide-angle studies: Omineca Belt to Intermontane Belt","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia","keywords":"Terrane; Geology; Crust; Seismology; North American Plate; Lithosphere; Craton; Basement; Fault (geology); Seismic refraction; Tectonics; Plate tectonics; Geophysics","score_opus":0.01650447810550626,"score_gpt":0.22651842752168827,"score_spread":0.210013949416182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001521872","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9831848,0.0029382317,0.000010893228,0.012465445,0.0004745137,0.000080121215,0.00029608235,0.000005422414,0.0005444552],"genre_scores_gemma":[0.9956318,0.00002483177,0.00047391633,0.0031124507,0.00054549996,2.882901e-7,0.000014362307,0.0000021664396,0.000194667],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981606,0.00007913341,0.00042931142,0.00028243382,0.0004348975,0.00061359943],"domain_scores_gemma":[0.99836975,0.00027683837,0.00020488072,0.00016169286,0.00019868593,0.0007881628],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004198536,0.00018877765,0.00034759234,0.000118681724,0.00076905783,0.00021929912,0.0009307487,0.000065012566,0.0042066565],"category_scores_gemma":[0.00033838936,0.00010082116,0.0001571295,0.0004929462,0.0007434989,0.00030549002,0.000026048383,0.0003095181,0.00007777283],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029206962,0.00000968072,0.9318348,0.0000033839365,0.0001312749,0.00013807311,0.0031618527,0.027790228,0.00022565728,0.0000034716056,0.0015868766,0.03508545],"study_design_scores_gemma":[0.00027562588,0.0006508781,0.9507129,0.00007533619,0.000067886765,0.00011569436,0.0068620667,0.0035259016,0.0006007099,0.0023981188,0.034359887,0.00035499316],"about_ca_topic_score_codex":0.07422876,"about_ca_topic_score_gemma":0.9728493,"teacher_disagreement_score":0.89862055,"about_ca_system_score_codex":0.000008182271,"about_ca_system_score_gemma":0.00035804664,"threshold_uncertainty_score":0.9967036},"labels":[],"label_agreement":null},{"id":"W2001786754","doi":"10.1139/e05-014","title":"Evolution of the early Paleozoic Cordilleran margin of Laurentia: tectonic and eustatic events interpreted from sequence stratigraphy and conodont community patterns","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"","keywords":"Conodont; Laurentia; Geology; Paleontology; Paleozoic; Diachronous; Tectonics; Sea level; Passive margin; Structural basin; Stratigraphy; Biostratigraphy; Oceanography; Rift","score_opus":0.019497798812809743,"score_gpt":0.21718988643279183,"score_spread":0.19769208761998208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001786754","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9922878,0.006423693,0.00004109021,0.00014221981,0.00014707992,0.00007628742,0.00018748043,0.0000013125725,0.00069301785],"genre_scores_gemma":[0.9995914,0.000049966093,0.00032046312,0.000020631856,0.00001427037,1.11019325e-7,8.4385897e-7,4.489223e-7,0.0000018284608],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99888825,0.00028985585,0.00033356127,0.00009581671,0.00018004602,0.00021248293],"domain_scores_gemma":[0.9990668,0.00019379459,0.00033385566,0.00010733163,0.00006680181,0.00023140556],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00063600787,0.000091498725,0.00020336502,0.00019379596,0.0003375833,0.000033804812,0.00036715454,0.000051601863,0.00011411273],"category_scores_gemma":[0.00006183682,0.00006245193,0.000062997846,0.00023988237,0.0012804399,0.0003331644,0.000002350416,0.00026490184,2.1227109e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010185369,0.0000037638263,0.9911336,0.000009247775,0.000021803968,0.0000020852935,0.00093661126,0.000049090533,0.00016558345,0.000038684444,0.0000022344086,0.007627153],"study_design_scores_gemma":[0.00020714782,0.00036736394,0.99635667,0.00016358416,0.00002325985,0.000032192223,0.00093682896,0.0006823445,0.00010982751,0.0010502419,0.000006542983,0.0000640119],"about_ca_topic_score_codex":0.07707028,"about_ca_topic_score_gemma":0.84361845,"teacher_disagreement_score":0.76654816,"about_ca_system_score_codex":0.0000014722538,"about_ca_system_score_gemma":0.00047352872,"threshold_uncertainty_score":0.9290756},"labels":[],"label_agreement":null},{"id":"W2001863929","doi":"10.1139/e02-094","title":"Neodymium isotope geochemistry of felsic volcanic and intrusive rocks from the YukonTanana Terrane in the Finlayson Lake Region, Yukon, Canada","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; University of British Columbia","funders":"","keywords":"Felsic; Geology; Geochemistry; Mafic; Volcanic rock; Terrane; Continental arc; Petrology; Volcano; Paleontology; Tectonics","score_opus":0.011868869340362045,"score_gpt":0.16839808755561747,"score_spread":0.15652921821525542,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001863929","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9867343,0.003226287,0.0000045040565,0.0066889743,0.00011647577,0.000051903902,0.00005691387,6.3286046e-7,0.0031200137],"genre_scores_gemma":[0.9976271,0.000070324815,0.000043507353,0.0021427958,0.000058058624,2.0332851e-7,0.0000043971045,7.894125e-7,0.000052831998],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99869186,0.00012133082,0.0003408298,0.00017627318,0.00033213117,0.00033755397],"domain_scores_gemma":[0.9989226,0.0003497575,0.00021552261,0.00013625837,0.000092639086,0.0002832428],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00058106234,0.00011461466,0.0002200891,0.000058380472,0.00026984434,0.000073439835,0.0006017102,0.000041504976,0.0027690905],"category_scores_gemma":[0.000372678,0.000057055902,0.00006151804,0.0005940813,0.0005042881,0.0001107432,0.0000055224755,0.0002516086,0.000001994452],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000458583,0.000002871734,0.9962515,0.0000028863801,0.000012689717,0.000104911545,0.0004343862,0.00050662964,0.000015159404,0.000023882072,0.0016661384,0.0009743341],"study_design_scores_gemma":[0.00018756039,0.00011341012,0.9707608,0.000046311947,0.000033475888,0.0002058417,0.0033119824,0.0005754909,0.0003791033,0.0068239877,0.017420238,0.0001417973],"about_ca_topic_score_codex":0.8987566,"about_ca_topic_score_gemma":0.99935377,"teacher_disagreement_score":0.10059716,"about_ca_system_score_codex":0.0000027597825,"about_ca_system_score_gemma":0.0014832865,"threshold_uncertainty_score":0.99814254},"labels":[],"label_agreement":null},{"id":"W2002299927","doi":"10.1139/e06-042","title":"Terrane-specific rock magnetic characteristics preserved in glacimarine sediment from southern coastal Alaska","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Office of Polar Programs","keywords":"Geology; Terrane; Glacial period; Glacier; Geochemistry; Sediment; Oceanography; Geomorphology; Paleontology; Tectonics","score_opus":0.02062688932360128,"score_gpt":0.20328749585895928,"score_spread":0.18266060653535798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002299927","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915845,0.0017484924,0.0000081772905,0.0007937138,0.0005281369,0.00008027885,0.00012734105,0.0000033057956,0.005126074],"genre_scores_gemma":[0.9986695,0.000034898538,0.00028858884,0.000096746524,0.00021876932,2.8418137e-7,0.00003788195,0.0000020354998,0.0006512621],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983181,0.00015773799,0.00042555327,0.00020704701,0.00029819872,0.00059337716],"domain_scores_gemma":[0.9990964,0.00018576065,0.000151738,0.0001121949,0.00007615404,0.0003777469],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007159603,0.00012536703,0.00024947413,0.0003794292,0.00026275462,0.00011716599,0.00051602395,0.00009047575,0.00954724],"category_scores_gemma":[0.00005296972,0.00010069103,0.000055601064,0.00034882652,0.00046713685,0.00020921511,0.00000948249,0.00031938896,0.000363211],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024750192,0.000007901565,0.9979756,0.0000030565154,0.0000037808088,0.00034124314,0.00017028983,0.0008804778,0.0000119853485,0.000007863541,0.0001377437,0.00043529226],"study_design_scores_gemma":[0.00034109087,0.00025551426,0.99257755,0.000025698328,0.0000046655364,0.00010632684,0.00031852938,0.0010947103,0.000022626511,0.00050412246,0.00463913,0.00011000441],"about_ca_topic_score_codex":0.045287058,"about_ca_topic_score_gemma":0.8566564,"teacher_disagreement_score":0.8113693,"about_ca_system_score_codex":7.9078336e-7,"about_ca_system_score_gemma":0.0006914824,"threshold_uncertainty_score":0.99135816},"labels":[],"label_agreement":null},{"id":"W2002392262","doi":"10.1139/e04-054","title":"Age constraints on the Paleoproterozoic tectonometamorphic history of the Committee Bay region, western Churchill Province, Canada: evidence from zircon and in situ monazite SHRIMP geochronology","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Nunavut Research Institute; Government of Nunavut; Geological Survey of Canada","funders":"","keywords":"Monazite; Zircon; Geology; Geochemistry; Metamorphic rock; Metamorphism; Geochronology; Bay; Metamorphic facies; Migmatite; Protolith; Gneiss; Facies; Paleontology; Oceanography","score_opus":0.026360773663917918,"score_gpt":0.1758620912995734,"score_spread":0.14950131763565547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002392262","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9869557,0.0031261635,0.000006725195,0.0086196875,0.00019816624,0.000108805776,0.000018447396,0.0000012053048,0.0009650797],"genre_scores_gemma":[0.9987402,0.00004622277,0.000062339226,0.0010612094,0.000035687382,4.02089e-7,0.0000010485268,8.990491e-7,0.000052011852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987066,0.00014941202,0.00034745786,0.00020468418,0.00027038145,0.0003214744],"domain_scores_gemma":[0.99889755,0.00034926482,0.00027795596,0.00015735276,0.000051666255,0.00026618165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005180662,0.00011985495,0.0002563048,0.00013464922,0.00016467318,0.000032089793,0.0006658387,0.000049446033,0.0007084021],"category_scores_gemma":[0.0003239154,0.000060564103,0.00006528263,0.00030492758,0.002321801,0.00014157247,0.000014012858,0.00031979126,0.0000034303364],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008976329,0.00000420506,0.9959984,0.0000039406887,0.000011688342,0.00013044293,0.00019010746,0.001782388,0.00027357123,0.000034057783,0.000052838135,0.00150942],"study_design_scores_gemma":[0.00012718522,0.0001333313,0.9959441,0.00013460428,0.000012906626,0.000051770312,0.00012550253,0.00003947192,0.00029870373,0.0023399151,0.00070880743,0.00008371372],"about_ca_topic_score_codex":0.78039044,"about_ca_topic_score_gemma":0.9988598,"teacher_disagreement_score":0.21846941,"about_ca_system_score_codex":0.000022831533,"about_ca_system_score_gemma":0.003354109,"threshold_uncertainty_score":0.8554773},"labels":[],"label_agreement":null},{"id":"W2002801238","doi":"10.1139/e04-018","title":"Taconian and Acadian transpression between the internal Humber Zone and the Gaspé Belt in the Gaspé Peninsula: tectonic history of the Shickshock Sud fault zone","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université de Montréal; GDG Environnement; Institut National de la Recherche Scientifique","funders":"","keywords":"Geology; Transpression; Sinistral and dextral; Mylonite; Orogeny; Seismology; Shear zone; Dalradian; Devonian; Fault (geology); Shear (geology); Metamorphism; Paleontology; Tectonics","score_opus":0.015469591355776056,"score_gpt":0.19399626721892188,"score_spread":0.17852667586314583,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002801238","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9757165,0.007120242,0.000014288262,0.015600108,0.0001317788,0.000111983456,0.000016954464,0.0000012410464,0.0012869036],"genre_scores_gemma":[0.9987646,0.00019610219,0.000053234064,0.00079431385,0.00008835541,4.5409843e-7,0.000001086969,0.0000012346114,0.00010062912],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99841505,0.00026433522,0.00037550397,0.00017703156,0.00040710252,0.00036095132],"domain_scores_gemma":[0.99890405,0.0004071263,0.00022184607,0.00014432828,0.000052454066,0.0002702204],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0017956689,0.00012936916,0.0002542366,0.00010986622,0.0004602434,0.00009134606,0.0009611937,0.00006463317,0.0005470893],"category_scores_gemma":[0.00016047081,0.00004613324,0.00012364569,0.0004568474,0.003114692,0.0001872558,0.000015792893,0.0005278507,0.0000031128964],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001796809,0.000004715867,0.99215335,0.0000044694766,0.000020637819,0.000019598097,0.0031201493,0.0012555378,0.00005083126,0.00015745936,0.000050267594,0.003145043],"study_design_scores_gemma":[0.0005368678,0.00013813544,0.9896454,0.000074108604,0.00004280617,0.00013391905,0.00113075,0.00039170563,0.000075657736,0.0037011397,0.0040401462,0.00008934632],"about_ca_topic_score_codex":0.12537436,"about_ca_topic_score_gemma":0.65641063,"teacher_disagreement_score":0.53103626,"about_ca_system_score_codex":0.0000070632323,"about_ca_system_score_gemma":0.00054138224,"threshold_uncertainty_score":0.99959826},"labels":[],"label_agreement":null},{"id":"W2002981715","doi":"10.1139/e00-070","title":"Tertiary extension in the central British Columbia Intermontane Belt: magnetic and paleomagnetic evidence from the Endako region","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Sinistral and dextral; Lineament; Paleomagnetism; Seismology; Batholith; Fault (geology); Fault scarp; Mafic; Geophysics; Tectonics; Paleontology","score_opus":0.02207721428739396,"score_gpt":0.210120922847477,"score_spread":0.18804370856008304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002981715","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9825,0.012403995,0.000019376615,0.004507159,0.00025360734,0.00009813205,0.0000058731785,0.0000017579594,0.00021011003],"genre_scores_gemma":[0.9974858,0.0006500796,0.00041313234,0.0011851164,0.0001633824,2.67601e-7,8.93233e-7,0.0000010731638,0.000100241494],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984812,0.00036005644,0.0002517807,0.00018782295,0.00028437117,0.0004347579],"domain_scores_gemma":[0.99858004,0.0008438358,0.00009400117,0.00010518228,0.00004416072,0.00033279837],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008317042,0.000073543364,0.00014053694,0.000049384675,0.00041407967,0.0006575132,0.00054821797,0.000036597652,0.00062339124],"category_scores_gemma":[0.00048437828,0.000050454488,0.000049083646,0.0005656501,0.00057911227,0.00030566787,0.000006373064,0.00025953224,0.000005275436],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004358161,0.000002485147,0.7551583,0.0000010312641,0.0000010661543,0.0005091834,0.00026889463,0.00002890583,0.000012096683,9.661666e-7,0.00030033544,0.24371235],"study_design_scores_gemma":[0.00009475007,0.0005260065,0.99291563,0.00015111346,0.00001084951,0.0011565995,0.00028749346,0.0008453502,0.0000015716129,0.0026705726,0.001264019,0.00007605685],"about_ca_topic_score_codex":0.5648761,"about_ca_topic_score_gemma":0.9744899,"teacher_disagreement_score":0.40961385,"about_ca_system_score_codex":0.0000014659648,"about_ca_system_score_gemma":0.00025249776,"threshold_uncertainty_score":0.6825697},"labels":[],"label_agreement":null},{"id":"W2003077398","doi":"10.1139/e10-106","title":"Revision of the tephrostratigraphy of the lower Sixtymile River area, Yukon Territory, Canada","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Tephra; Rhyolite; Geology; Terrace (agriculture); Pleistocene; Deposition (geology); Tephrochronology; Volcano; Archaeology; Geochemistry; Paleontology; Geomorphology; Geography; Volcanic rock; Sediment","score_opus":0.026561247790222262,"score_gpt":0.2005027607442413,"score_spread":0.17394151295401905,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003077398","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98881686,0.00093160075,8.382729e-7,0.0005349754,0.0009851137,0.000071366296,0.000035508438,4.845415e-7,0.008623239],"genre_scores_gemma":[0.99958056,0.000017021106,0.00011497799,0.00016237453,0.000024806051,3.9956753e-8,3.3781714e-7,6.9759574e-7,0.00009918003],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99879605,0.00017378887,0.00028775455,0.000099060206,0.0003504509,0.00029288844],"domain_scores_gemma":[0.9990785,0.00011973485,0.0002790408,0.00017496072,0.00012771266,0.00022002339],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00070397183,0.00007400805,0.00016159257,0.000116406656,0.00037880402,0.000011258179,0.000923948,0.000055196346,0.0016062489],"category_scores_gemma":[0.00013413858,0.000036719786,0.00010064359,0.00043109746,0.0021683604,0.00013276878,0.000008770197,0.00022774766,0.0000021709104],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000682176,0.0000033437755,0.99870753,0.000005275189,0.000008158957,0.000013744936,0.00026258975,0.00008913496,0.0000052200417,0.000037789563,0.000639705,0.00022068217],"study_design_scores_gemma":[0.0000695394,0.00018026972,0.9955483,0.00006809231,0.000009039303,0.00007849618,0.00023748216,0.00004913474,0.0005063576,0.00026204652,0.002946656,0.00004457354],"about_ca_topic_score_codex":0.6055641,"about_ca_topic_score_gemma":0.9952533,"teacher_disagreement_score":0.3896892,"about_ca_system_score_codex":5.312223e-7,"about_ca_system_score_gemma":0.003507953,"threshold_uncertainty_score":0.99930644},"labels":[],"label_agreement":null},{"id":"W2003158547","doi":"10.1139/e09-049","title":"Mantle plume – volcanic arc interaction: consequences for magmatism, metallogeny, and cratonization in the Abitibi and Wawa subprovinces, CanadaThis article is one of a series of papers published in this Special Issue on the theme <i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Geology; Geochemistry; Craton; Archean; Metallogeny; Mantle plume; Terrane; Basalt; Crust; Continental arc; Andesite; Subduction; Adakite; Mantle (geology); Volcanic rock; Earth science; Petrology; Oceanic crust; Volcano; Tectonics; Paleontology","score_opus":0.010753759117760045,"score_gpt":0.18578660368518196,"score_spread":0.1750328445674219,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003158547","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9827852,0.0011776366,0.0000027919123,0.014971993,0.00006139979,0.00018199552,0.000043785494,4.8885613e-7,0.0007746637],"genre_scores_gemma":[0.99933416,0.00016909467,0.00022347095,0.00021017567,0.000040473817,0.0000013917168,0.0000012619216,6.5515457e-7,0.00001932368],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99906164,0.000108494794,0.00034197987,0.000125582,0.0002103996,0.00015187109],"domain_scores_gemma":[0.99890643,0.00052886206,0.0002890815,0.00006866696,0.00013039813,0.000076553355],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014966157,0.00007111581,0.00021577539,0.000111760055,0.00012393926,0.00007731107,0.00022014412,0.000032698303,0.0012499044],"category_scores_gemma":[0.0007384581,0.000032469474,0.00002828376,0.00044115382,0.0018456762,0.00029236407,0.0000064382275,0.0001345435,1.4400243e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024773952,0.00003347507,0.9790501,0.00013731235,0.000055731834,0.000007744331,0.0059675253,0.0002117164,0.002567051,0.0069231098,0.00019516236,0.0046033585],"study_design_scores_gemma":[0.0011246891,0.0010007881,0.91427016,0.00022823742,0.000118681775,0.00016197965,0.017001094,0.0041284496,0.0061413324,0.05297098,0.002636858,0.00021677764],"about_ca_topic_score_codex":0.15122314,"about_ca_topic_score_gemma":0.92705745,"teacher_disagreement_score":0.7758343,"about_ca_system_score_codex":0.0000018823489,"about_ca_system_score_gemma":0.00040071647,"threshold_uncertainty_score":0.9996631},"labels":[],"label_agreement":null},{"id":"W2003346563","doi":"10.1139/e00-052","title":"Records of geomagnetic secular variation since 1200 AD and the potential for chronological control of lake sediments in northern Alberta","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Resources Canada; McMaster University","keywords":"Geology; Chronology; Declination; Earth's magnetic field; Sediment; Interglacial; Geomagnetic secular variation; Paleomagnetism; Quaternary; Oceanography; Hydrology (agriculture); Paleontology; Geomagnetic storm","score_opus":0.004962693820662423,"score_gpt":0.19506192741361764,"score_spread":0.19009923359295522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003346563","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99432194,0.004124899,0.00012532681,0.00082745793,0.00009532026,0.00015460323,0.000028584689,2.5286846e-7,0.00032159532],"genre_scores_gemma":[0.99913204,0.0002555045,0.00032042264,0.00008689511,0.000044825825,0.0000027315607,0.00000232354,0.0000023164769,0.0001529321],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99925363,0.000067887704,0.00027946974,0.00011736253,0.00009980689,0.00018183555],"domain_scores_gemma":[0.99956185,0.00004475496,0.00015104775,0.00007340943,0.00008791817,0.00008104636],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004489971,0.00007237752,0.00017385774,0.00006095948,0.000091623835,0.000014514302,0.00017422455,0.000056067016,0.000078227386],"category_scores_gemma":[0.00011851908,0.000049357703,0.000059024387,0.000092858405,0.0006240258,0.000008545963,0.000007362753,0.000045024182,4.0427938e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022811927,0.00019242351,0.8600021,0.00014096446,0.0003709408,0.00006020342,0.0034452556,0.014782518,0.05216978,0.00064689084,0.00041211178,0.06549565],"study_design_scores_gemma":[0.0042385147,0.0030134318,0.98383695,0.00004481257,0.00006336085,0.000087316985,0.00017511488,0.00085340656,0.000709291,0.00046754922,0.006367514,0.00014272399],"about_ca_topic_score_codex":0.0024483707,"about_ca_topic_score_gemma":0.40457568,"teacher_disagreement_score":0.40212733,"about_ca_system_score_codex":0.0000011143676,"about_ca_system_score_gemma":0.00029556316,"threshold_uncertainty_score":0.60628927},"labels":[],"label_agreement":null},{"id":"W2003368355","doi":"10.1139/e00-077","title":"The \"Great Extinction\" that never happened: the demise of the dinosaurs considered","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Royal Tyrrell Museum; University of Saskatchewan","funders":"","keywords":"Demise; Extinction (optical mineralogy); Extinction event; Paleontology; Geology; Globe; Natural (archaeology); Cretaceous; Extraterrestrial life; Astrobiology; Biology; Demography; Law; Biological dispersal","score_opus":0.03280553964639211,"score_gpt":0.21495268928662242,"score_spread":0.18214714964023032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003368355","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95796347,0.007060726,0.000010186933,0.021296017,0.0016269296,0.00008335136,0.000015595226,0.0000020591262,0.0119416695],"genre_scores_gemma":[0.9981563,0.0002131449,0.000041663512,0.0009825084,0.000103450926,1.8383861e-7,5.3481386e-7,6.8862056e-7,0.0005015227],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886614,0.00022255201,0.00023541534,0.000105308485,0.00021016903,0.00036043426],"domain_scores_gemma":[0.99874693,0.0005540104,0.0002557606,0.00015114971,0.00008878737,0.00020336619],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["sts"],"category_scores_codex":[0.001170378,0.00008100764,0.00011895848,0.00006748258,0.0017106269,0.00005829185,0.0007889001,0.00005975024,0.0011070174],"category_scores_gemma":[0.00028776148,0.00003266448,0.00009384891,0.00034317872,0.0029675644,0.0003018805,0.00000641782,0.00020435845,0.000019997797],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013018311,9.664618e-7,0.9946659,4.8958003e-7,0.000011950873,0.000013176019,0.00012346637,0.0007160112,0.0000054005213,0.00023026398,0.0009769014,0.003242433],"study_design_scores_gemma":[0.00008450671,0.00007253616,0.8811363,0.000010678387,0.000011242971,0.0007579377,0.00053346285,0.0002745075,0.000021340418,0.0014941228,0.11555963,0.00004370829],"about_ca_topic_score_codex":0.008077188,"about_ca_topic_score_gemma":0.6533917,"teacher_disagreement_score":0.6453146,"about_ca_system_score_codex":0.0000017458495,"about_ca_system_score_gemma":0.0011015072,"threshold_uncertainty_score":0.9998061},"labels":[],"label_agreement":null},{"id":"W2003535557","doi":"10.1139/e07-017","title":"Brachiopods from Bird Fiord Formation (Devonian) of Arctic Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Brandon University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Devonian; Fjord; Fauna; Siliciclastic; Paleontology; Geology; Arctic; Biota; Paleozoic; Carboniferous; Ecological succession; Ecology; Oceanography; Structural basin; Sedimentary depositional environment; Biology","score_opus":0.01639854585104398,"score_gpt":0.2097648153328049,"score_spread":0.19336626948176092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003535557","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.978467,0.0039300886,0.00017468505,0.00029865248,0.00073306484,0.000037449798,0.00005153639,0.0000024234682,0.016305087],"genre_scores_gemma":[0.99847776,0.000013662056,0.0012927072,0.000121039564,0.00008360898,2.1626022e-8,0.0000012462538,5.1070816e-7,0.0000094430925],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987636,0.00004828092,0.00041210133,0.00009643617,0.0003172291,0.0003623055],"domain_scores_gemma":[0.9987585,0.00022196052,0.00031554356,0.00006509732,0.00010494639,0.0005339702],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00091122737,0.00008370436,0.00017478158,0.0002824845,0.00030023482,0.000043679855,0.0003423883,0.000052062966,0.0005518246],"category_scores_gemma":[0.00012731516,0.000066131186,0.00005938468,0.00039390926,0.0004328693,0.0005145506,4.809196e-7,0.00015849902,0.0000030168262],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009041176,0.0000013664909,0.96829605,0.000003998126,0.0000091420125,0.000071631635,0.00021354556,0.0001085791,0.000019806605,0.000039855095,0.00003938509,0.031187585],"study_design_scores_gemma":[0.00011278803,0.00016398914,0.9970662,0.00003706685,0.000008187229,0.0000858451,0.0005640797,0.00023042815,0.00019473606,0.00066335814,0.0007951841,0.0000781632],"about_ca_topic_score_codex":0.94121087,"about_ca_topic_score_gemma":0.9999102,"teacher_disagreement_score":0.05869935,"about_ca_system_score_codex":0.000002699207,"about_ca_system_score_gemma":0.0028999185,"threshold_uncertainty_score":0.6042092},"labels":[],"label_agreement":null},{"id":"W2003692918","doi":"10.1139/e00-004","title":"Docking of the Central Metasedimentary Belt to Laurentia in geon 12: evidence from the 1.17-1.16 Ga Chevreuil intrusive suite and host gneisses, Quebec","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Metamorphism; Geochemistry; Orogeny; Gneiss; Gabbro; Diorite; Laurentia; Pluton; Terrane; Plutonism; Petrology; Metamorphic rock; Igneous rock; Zircon; Tectonics; Seismology; Paleozoic","score_opus":0.015491479356988436,"score_gpt":0.19630518650061884,"score_spread":0.1808137071436304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003692918","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98687553,0.0049318466,0.0000013809233,0.007581169,0.00013727004,0.00008102765,0.00006173514,0.0000011655181,0.0003288599],"genre_scores_gemma":[0.99830127,0.00012082048,0.00012999077,0.0012608536,0.00008407849,1.9341839e-7,0.0000036047254,7.910773e-7,0.00009842051],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986081,0.00013438052,0.0003309137,0.00019277612,0.00032906322,0.00040474703],"domain_scores_gemma":[0.998911,0.00035542157,0.00013936889,0.000118637334,0.000046322482,0.00042919908],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00060185976,0.00010964459,0.00021151696,0.000097161035,0.00028278554,0.00011889733,0.00068811147,0.000034939352,0.012000046],"category_scores_gemma":[0.00021934009,0.000053729775,0.000092354996,0.0006848958,0.0005894967,0.00030134042,0.000015040671,0.00019684718,0.000008924621],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012507966,0.0000032906871,0.9903946,0.0000016220554,0.000014893791,0.0000135380815,0.0005012225,0.002306471,0.000110723224,0.000004903691,0.00025984863,0.0063763745],"study_design_scores_gemma":[0.00008155843,0.00008874315,0.99551415,0.00012054147,0.000035915742,0.000014364114,0.00044203087,0.00026721263,0.00052918977,0.0006333599,0.0021920395,0.00008091907],"about_ca_topic_score_codex":0.7519211,"about_ca_topic_score_gemma":0.9896699,"teacher_disagreement_score":0.23774883,"about_ca_system_score_codex":0.000004886775,"about_ca_system_score_gemma":0.00045462768,"threshold_uncertainty_score":0.9889031},"labels":[],"label_agreement":null},{"id":"W2003956655","doi":"10.1139/e99-063","title":"A summary of electromagnetic studies on the Abitibi-Grenville transect","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Crust; Archean; Magnetotellurics; Transect; Metamorphic rock; Petrology; Mantle (geology); Tectonics; Lithosphere; Foreland basin; Geophysics; Geochemistry; Seismology; Electrical resistivity and conductivity","score_opus":0.028696653117258494,"score_gpt":0.23552866997854602,"score_spread":0.20683201686128752,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003956655","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98102254,0.0034887267,0.0000016213231,0.0019697153,0.00017577027,0.00005873096,0.000011113333,0.0000016169747,0.01327018],"genre_scores_gemma":[0.9983344,0.00015889444,0.00043909237,0.000514238,0.00009566433,1.5215454e-7,2.7376774e-7,0.0000011312758,0.00045615082],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9987088,0.00020099181,0.0002926511,0.00012263321,0.000309617,0.00036534393],"domain_scores_gemma":[0.99878305,0.00065716164,0.00010659457,0.00008339486,0.00006831565,0.00030149848],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009875632,0.00009636024,0.00022156544,0.0001491272,0.00031439777,0.000041500916,0.0004074393,0.000027104872,0.0036322114],"category_scores_gemma":[0.00022241507,0.000050338836,0.000111236244,0.0007706311,0.0006900673,0.0000896567,9.573703e-7,0.00019350815,0.000046143792],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019025453,0.000066459914,0.07661688,0.000048113372,0.0001860034,0.00023740741,0.0029588183,0.016596302,0.001173836,0.0031091874,0.0027782053,0.89603853],"study_design_scores_gemma":[0.000294048,0.0076263575,0.954523,0.00015510031,0.000045368768,0.00012622304,0.00056334445,0.001143224,0.0025509673,0.021570088,0.011134911,0.0002673282],"about_ca_topic_score_codex":0.0061593684,"about_ca_topic_score_gemma":0.0796082,"teacher_disagreement_score":0.8957712,"about_ca_system_score_codex":9.910399e-7,"about_ca_system_score_gemma":0.000493929,"threshold_uncertainty_score":0.99727863},"labels":[],"label_agreement":null},{"id":"W2004071857","doi":"10.1139/e05-092","title":"New winter crane flies (Insecta: Diptera: Trichoceridae) from the Jurassic Daohugou Formation (Inner Mongolia, China) and their associated biota","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fossil Insects in Amber","field":"Agricultural and Biological Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology; Cretaceous; Biota; Inner mongolia; China; Sedimentary rock; Invertebrate; Volcano; Yixian Formation; Range (aeronautics); Mesozoic; Ecology; Structural basin; Biology; Geography; Archaeology","score_opus":0.013596996879201781,"score_gpt":0.18538397992525724,"score_spread":0.17178698304605544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2004071857","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9874437,0.0014870759,0.000009505906,0.009035559,0.00044278437,0.00008246987,0.00005950913,0.000008231808,0.001431158],"genre_scores_gemma":[0.9984302,0.000036549634,0.00008670008,0.0002956338,0.0005753531,6.2619347e-7,0.000006687695,0.0000010016462,0.00056722783],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988173,0.00010162903,0.00031433316,0.00016629742,0.00024177984,0.00035862604],"domain_scores_gemma":[0.9990742,0.00023531119,0.00027940256,0.000049187653,0.00008988807,0.00027196854],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00050546345,0.00015000835,0.0001922254,0.000048532005,0.00067727675,0.00056367746,0.0004743479,0.0000760126,0.00035478838],"category_scores_gemma":[0.00014700442,0.000047129222,0.000089428046,0.0005651788,0.0003813193,0.00064515823,0.000020929188,0.00019088986,0.000008318603],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005975514,0.00006818695,0.66352993,0.0000066576745,0.00011184644,0.000081724276,0.0044754962,0.0002892213,0.089638375,0.0005914706,0.07750503,0.16364229],"study_design_scores_gemma":[0.00014913254,0.00019534738,0.97146416,0.000051729974,0.00001000545,0.00004067696,0.00033393942,0.00019635547,0.0010138678,0.00128654,0.025126005,0.00013226576],"about_ca_topic_score_codex":0.06985691,"about_ca_topic_score_gemma":0.5959385,"teacher_disagreement_score":0.52608156,"about_ca_system_score_codex":0.000016850048,"about_ca_system_score_gemma":0.00016691901,"threshold_uncertainty_score":0.936337},"labels":[],"label_agreement":null},{"id":"W2004195896","doi":"10.1139/e04-046","title":"Magnetic and gravity models across terrane boundaries in southern New Brunswick, Canada","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University","funders":"","keywords":"Terrane; Geology; Paleontology; Basement; Tectonics; Archaeology; Geography","score_opus":0.019428781085170016,"score_gpt":0.22238230459221087,"score_spread":0.20295352350704085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2004195896","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99448806,0.0023917453,0.00012331942,0.0020738852,0.00028191923,0.000045822497,0.000020126274,0.0000017069275,0.00057340367],"genre_scores_gemma":[0.9967418,0.000011063344,0.0025025103,0.0003981127,0.000080772,2.6172744e-8,6.2478483e-7,0.0000012853405,0.00026383597],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873567,0.00005324397,0.00024012281,0.00015816995,0.00028205544,0.000530771],"domain_scores_gemma":[0.998857,0.000075306154,0.0000819353,0.000058489295,0.000041946692,0.0008853146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000500275,0.000103901235,0.00019944539,0.000105378975,0.0004175317,0.00031198573,0.0002790759,0.000036966478,0.00018229036],"category_scores_gemma":[0.00011264376,0.000076291944,0.000032423763,0.00054813013,0.00061422214,0.00029118385,0.0000042287857,0.00020855831,0.0000059888707],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003259368,0.000010118465,0.6851669,0.000014594447,0.00000952719,0.00041755065,0.0048966804,0.04935304,0.000014455687,0.0011811187,0.0000845255,0.2588189],"study_design_scores_gemma":[0.00038359262,0.00042165993,0.9432514,0.00003492239,0.000004925039,0.00012354448,0.00086253486,0.0011636049,0.000028151595,0.051092554,0.0024686835,0.00016444732],"about_ca_topic_score_codex":0.9959679,"about_ca_topic_score_gemma":0.9999283,"teacher_disagreement_score":0.25865445,"about_ca_system_score_codex":0.0000046438527,"about_ca_system_score_gemma":0.015836546,"threshold_uncertainty_score":0.98974276},"labels":[],"label_agreement":null},{"id":"W2004298744","doi":"10.1139/e06-016","title":"Anomalous early 20th century sedimentation in proglacial Green Lake, British Columbia, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Northern British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Varve; Geology; Glacier; Sedimentation; Northern Hemisphere; Period (music); Physical geography; Sediment; Climatology; Climate change; Hydrology (agriculture); Oceanography; Geomorphology; Geography","score_opus":0.009419120763096974,"score_gpt":0.194966547609903,"score_spread":0.18554742684680603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2004298744","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913565,0.0010666106,6.7699034e-7,0.0004816588,0.00056711334,0.00009690472,0.00005807638,0.0000020817379,0.0063703624],"genre_scores_gemma":[0.9989717,0.000012922985,0.0001304863,0.00017355806,0.00012392213,2.9665495e-7,0.000014849908,0.0000012770722,0.00057097053],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985193,0.0001274213,0.00030524877,0.00016005863,0.00031918488,0.0005687579],"domain_scores_gemma":[0.9992998,0.00008087652,0.00012671099,0.00005091336,0.000091879934,0.0003497796],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00067410077,0.00006429142,0.00016357117,0.00017293604,0.00042347205,0.00024416833,0.00032869994,0.00006850306,0.0024060914],"category_scores_gemma":[0.00004643303,0.000079288366,0.000030987987,0.0005048181,0.00049833424,0.0003313569,0.000003079785,0.00023588722,0.000015631744],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000039375,0.0000031786751,0.9974055,0.00000323182,0.0000031795023,0.00088104303,0.000047683585,0.00017247094,4.2810586e-7,0.0000059084487,0.00043428506,0.0010391182],"study_design_scores_gemma":[0.0002393361,0.00015851068,0.99416137,0.00002022984,0.0000032991748,0.00048013235,0.00012401483,0.00008499909,0.000002010889,0.00030000668,0.004337298,0.00008879906],"about_ca_topic_score_codex":0.99749595,"about_ca_topic_score_gemma":0.9999991,"teacher_disagreement_score":0.007615201,"about_ca_system_score_codex":0.0000018923589,"about_ca_system_score_gemma":0.0046910867,"threshold_uncertainty_score":0.99850583},"labels":[],"label_agreement":null},{"id":"W2004490360","doi":"10.1139/e05-086","title":"Pinwarian (1.50 Ga) volcanism and hydrothermal activity at the eastern margin of the Wakeham Group, Grenville Province, Quebec","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Institut National de la Recherche Scientifique; Geological Survey of Canada","funders":"","keywords":"Geology; Geochemistry; Lapilli; Felsic; Mafic; Pyroclastic rock; Gneiss; Petrology; Metamorphic rock; Volcano","score_opus":0.011177316412774906,"score_gpt":0.17290659935772856,"score_spread":0.16172928294495365,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2004490360","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9876878,0.0009898938,0.00000568748,0.007884203,0.00011619293,0.000075973825,0.00002792272,0.0000014706075,0.0032108228],"genre_scores_gemma":[0.9983064,0.000012780449,0.000114928145,0.00047391714,0.0000979685,1.7981854e-7,7.279577e-7,8.900113e-7,0.0009922138],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988208,0.000114806455,0.00022895228,0.00016241129,0.00033049533,0.00034253285],"domain_scores_gemma":[0.9991357,0.00010358019,0.00023156904,0.00012371548,0.00004057007,0.00036486983],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006317405,0.00010834416,0.00018220546,0.000079467565,0.0005351529,0.00008631621,0.00053606293,0.000044980847,0.003272338],"category_scores_gemma":[0.00006441045,0.000049296206,0.00011465208,0.00030517968,0.0013575826,0.00020705645,0.00002200169,0.00018043323,0.000025460067],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010111614,0.0000057971556,0.97875404,0.0000034176414,0.0000131197585,0.000005947836,0.00010599891,0.0012197552,0.00024716082,0.00006568673,0.000098493314,0.01947047],"study_design_scores_gemma":[0.00011591294,0.00011953915,0.9775957,0.000017017861,0.000020801584,0.000061575134,0.000090464084,0.0032850113,0.00052550103,0.0004380638,0.017641313,0.000089119094],"about_ca_topic_score_codex":0.19442256,"about_ca_topic_score_gemma":0.9797049,"teacher_disagreement_score":0.7852824,"about_ca_system_score_codex":0.000003489432,"about_ca_system_score_gemma":0.00041999863,"threshold_uncertainty_score":0.9976388},"labels":[],"label_agreement":null},{"id":"W2004638555","doi":"10.1139/e03-033","title":"Thermochronology of the Needle Falls Shear Zone: a post-collisional high-strain zone of the Trans-Hudson Orogen","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Regina; University of Saskatchewan; Ministry of Energy, Northern Development and Mines","funders":"University of Saskatchewan; Northwestern University","keywords":"Geology; Batholith; Shear zone; Hornblende; Mylonite; Geochemistry; Biotite; Metamorphism; Closure temperature; Amphibole; Craton; Terrane; Pluton; Zircon; Petrology; Quartz; Seismology; Paleontology; Tectonics","score_opus":0.010883841145978236,"score_gpt":0.17942656217324615,"score_spread":0.16854272102726792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2004638555","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99368984,0.0008907975,0.000027361548,0.003135865,0.00026739595,0.00007223505,0.00012940369,0.0000011052748,0.001785987],"genre_scores_gemma":[0.9988788,0.000015746667,0.00057090574,0.00037486697,0.000032050182,1.2918221e-7,0.0000014103765,0.0000010584085,0.00012503519],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99848044,0.00020874589,0.00040334061,0.00014492523,0.00041324098,0.00034930016],"domain_scores_gemma":[0.99895716,0.00016755602,0.0002809378,0.00014615113,0.00016671454,0.00028145392],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00078442943,0.00010635603,0.00026357808,0.0001139382,0.00028351357,0.000026217076,0.00083111564,0.00007331355,0.008389321],"category_scores_gemma":[0.0002661656,0.000048606056,0.00024303382,0.0008838971,0.0014287478,0.000113010494,0.000006922793,0.0002056036,0.000007856553],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020227086,0.00003212521,0.96805805,0.000012462213,0.00007539746,0.000013918712,0.00072829163,0.016386442,0.0075380174,0.0024210366,0.00008462433,0.0046294206],"study_design_scores_gemma":[0.00021590899,0.0003555905,0.9861253,0.00003697776,0.000042917636,0.00009812787,0.00078061724,0.00020963745,0.0066479207,0.0034231266,0.0019627253,0.00010118807],"about_ca_topic_score_codex":0.026147889,"about_ca_topic_score_gemma":0.25604123,"teacher_disagreement_score":0.22989333,"about_ca_system_score_codex":0.0000017729107,"about_ca_system_score_gemma":0.0011130868,"threshold_uncertainty_score":0.9925172},"labels":[],"label_agreement":null},{"id":"W2004680413","doi":"10.1139/e06-034","title":"A new erinaceid (Mammalia, Insectivora) from the Late Paleocene of western Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Insectivora; Taxon; Genus; Paleontology; Geology; Latitude; Zoology; Biology","score_opus":0.01709206231170409,"score_gpt":0.19245798440190118,"score_spread":0.17536592209019708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2004680413","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98172164,0.0074651386,0.000028878498,0.0033662922,0.0007899038,0.000039767277,0.00006890388,0.0000018415052,0.006517646],"genre_scores_gemma":[0.998329,0.000031953874,0.00029727243,0.0004386487,0.00020444806,4.660126e-8,0.0000020877021,9.65254e-7,0.00069557683],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989549,0.00008091782,0.00029116025,0.000096610565,0.0002795411,0.00029686117],"domain_scores_gemma":[0.99910074,0.00021235661,0.00023787816,0.00008520932,0.00008687433,0.00027696235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035816184,0.00009050889,0.0001839741,0.00008172169,0.00035962468,0.000049540085,0.00042056135,0.000032585693,0.0006870548],"category_scores_gemma":[0.000062130195,0.000057387893,0.000047950678,0.00032836993,0.00041832795,0.0001599076,0.0000033580825,0.00012881478,0.0000068889394],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000047357007,8.08601e-7,0.993973,0.000001133161,0.0000120223895,0.000030383162,0.00013915217,0.0013881514,0.0000050732533,0.000026084359,0.0034434542,0.0009760029],"study_design_scores_gemma":[0.00013088468,0.00008587719,0.9712554,0.000023732471,0.000010705598,0.000034250115,0.00033872336,0.000064401276,0.000030317555,0.00035772662,0.027598105,0.000069861606],"about_ca_topic_score_codex":0.99026376,"about_ca_topic_score_gemma":0.9999832,"teacher_disagreement_score":0.02415465,"about_ca_system_score_codex":0.0000025962117,"about_ca_system_score_gemma":0.0039167195,"threshold_uncertainty_score":0.75227684},"labels":[],"label_agreement":null},{"id":"W2004762930","doi":"10.1139/e02-079","title":"The Dorothy bentonite: an extraordinary case of secondary thickening in a late Campanian volcanic ash fall in central Alberta","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Pumice; Volcanic ash; Lapilli; Rhyolite; Volcanic glass; Outcrop; Silicic; Geochemistry; Biotite; Mineralogy; Calcite; Tephra; Plagioclase; Volcano; Quartz; Pyroclastic rock; Volcanic rock; Paleontology","score_opus":0.017619039560050478,"score_gpt":0.19990027997663382,"score_spread":0.18228124041658333,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2004762930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924665,0.0023973691,7.0524646e-7,0.0011456364,0.00013227096,0.000052793457,0.000015691689,0.0000011958249,0.0037878484],"genre_scores_gemma":[0.9994303,0.00008513454,0.00013104733,0.0001638821,0.00004174659,1.7004736e-7,0.0000018845739,0.0000011639316,0.00014465878],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99835986,0.00015282341,0.00047776417,0.00018541083,0.00020800263,0.00061616296],"domain_scores_gemma":[0.9987741,0.00027116365,0.00018709728,0.00010567858,0.00005338934,0.00060856703],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00089167,0.000113485185,0.0002320021,0.00029771385,0.0002956419,0.00011076835,0.0004981087,0.000060098017,0.0045473785],"category_scores_gemma":[0.00017927508,0.00006948174,0.000089837515,0.0009248505,0.0005597885,0.00040970897,0.0000076003817,0.0003603228,0.000012035706],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007101986,0.000009704314,0.9814325,0.0000032368448,0.0000064211954,0.0010570413,0.0013164299,0.006288849,0.000021378813,0.000034919336,0.000017951563,0.0098044565],"study_design_scores_gemma":[0.00026056907,0.00042864078,0.9695373,0.000049537866,0.000011850818,0.00064518617,0.0017886532,0.02288976,0.000037712398,0.0031021817,0.0010881311,0.00016045304],"about_ca_topic_score_codex":0.36745334,"about_ca_topic_score_gemma":0.99426615,"teacher_disagreement_score":0.6268128,"about_ca_system_score_codex":0.0000035992778,"about_ca_system_score_gemma":0.00032581252,"threshold_uncertainty_score":0.9963626},"labels":[],"label_agreement":null},{"id":"W2005016969","doi":"10.1139/e04-032","title":"Optical dating of pottery, burnt stones, and sediments from selected Quebec archaeological sites","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Archaeology and ancient environmental studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Pottery; Radiocarbon dating; Thermoluminescence dating; Geology; Archaeology; Optical dating; Woodland; Chronology; Sediment; Geoarchaeology; Holocene; Mineralogy; Paleontology; Geography","score_opus":0.01723460390249563,"score_gpt":0.20135244791609735,"score_spread":0.18411784401360173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2005016969","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965,0.002093801,0.000082748884,0.0007223642,0.00012111784,0.000038698417,0.00002868395,0.0000020970217,0.00041049486],"genre_scores_gemma":[0.9949302,0.000059533086,0.0047508553,0.00017283385,0.00005091309,7.309305e-8,0.0000060704906,8.8087467e-7,0.000028608827],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990634,0.000041405125,0.00024003297,0.00014886356,0.00021081706,0.0002954909],"domain_scores_gemma":[0.99933505,0.00012316645,0.00013508277,0.000042125608,0.000027813267,0.000336768],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032868437,0.00008712845,0.00018165924,0.00011304658,0.00034708437,0.00001780115,0.00021137048,0.000041573054,0.0006260065],"category_scores_gemma":[0.00011478156,0.000061260944,0.0000296684,0.00019920358,0.002446,0.00021481032,0.00001872364,0.00013915711,0.000008912401],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000068424233,0.000004443336,0.995952,0.0000016587853,0.000012749191,0.0000605859,0.0006082419,0.0010827577,0.00027790255,0.00011471529,0.0000067731294,0.0018713463],"study_design_scores_gemma":[0.00020312828,0.00032977582,0.9960022,0.00003057194,0.000009774846,0.00008203496,0.00056156464,0.00007886678,0.0006410766,0.001811001,0.00017710851,0.00007289501],"about_ca_topic_score_codex":0.06118806,"about_ca_topic_score_gemma":0.48777163,"teacher_disagreement_score":0.42658356,"about_ca_system_score_codex":0.000002771054,"about_ca_system_score_gemma":0.00032385765,"threshold_uncertainty_score":0.9450636},"labels":[],"label_agreement":null},{"id":"W2005263992","doi":"10.1139/e02-106","title":"Late Wisconsinan glaciation of Amund and Ellef Ringnes islands, Nunavut: evidence for the configuration, dynamics, and deglacial chronology of the northwest sector of the Innuitian Ice Sheet","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Geology; Ice sheet; Deglaciation; Oceanography; Ice stream; Ice shelf; Antarctic sea ice; Wisconsin glaciation; Arctic ice pack; Glacier morphology; Antarctic ice sheet; Paleontology; Sea ice; Physical geography; Holocene; Cryosphere; Geography","score_opus":0.028124481807317667,"score_gpt":0.2423862590488161,"score_spread":0.21426177724149845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2005263992","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945412,0.0031188864,0.000024297833,0.0014465351,0.00033257192,0.00016085505,0.00004231733,4.697842e-7,0.00033284829],"genre_scores_gemma":[0.9996703,0.00014102743,0.00006837592,0.00005725775,0.000019749808,3.174208e-7,8.6402105e-7,8.6443583e-7,0.00004123416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990474,0.00021871716,0.00028696735,0.00010173316,0.00014029471,0.00020487829],"domain_scores_gemma":[0.9984885,0.00077581586,0.00035527349,0.00010428166,0.00019407038,0.00008208314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011883547,0.000066719214,0.00016741813,0.000101551086,0.0005065884,0.000025641239,0.00032581095,0.00006265307,0.0001142352],"category_scores_gemma":[0.00075244857,0.0000341841,0.000041673677,0.0002789939,0.0026051132,0.00017031662,0.0000067266224,0.0001338193,3.349918e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013888064,0.000001659891,0.997628,0.000019570987,0.00001234671,8.1514713e-7,0.00067087985,0.00051146105,0.000020798396,0.0008790877,0.0000057257157,0.00023581627],"study_design_scores_gemma":[0.0001678434,0.00018531755,0.99559134,0.000058683163,0.000022741537,0.00009996011,0.0006197322,0.0020002874,0.00036459567,0.0007750217,0.000076259166,0.000038237242],"about_ca_topic_score_codex":0.005689597,"about_ca_topic_score_gemma":0.8865466,"teacher_disagreement_score":0.880857,"about_ca_system_score_codex":8.203623e-7,"about_ca_system_score_gemma":0.0011868426,"threshold_uncertainty_score":0.9598648},"labels":[],"label_agreement":null},{"id":"W2005381099","doi":"10.1139/e06-095","title":"Laurentide and montane glaciation along the Rocky Mountain Foothills of northeastern British Columbia","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Core Research for Evolutional Science and Technology","keywords":"Geology; Foothills; Ice sheet; Wisconsin glaciation; Glacial period; Paleontology; Geomorphology; Ice stream; Physical geography; Oceanography; Sea ice; Cryosphere; Geography","score_opus":0.012663941369763206,"score_gpt":0.21480476618515915,"score_spread":0.20214082481539594,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2005381099","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945032,0.002600808,0.000021135911,0.00036884184,0.0002190755,0.00006741393,0.000014215755,0.0000013238935,0.0022039951],"genre_scores_gemma":[0.9993671,0.000045540226,0.0001459545,0.00012314758,0.000048225807,6.1794026e-8,0.000002328799,8.795182e-7,0.0002667199],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99890524,0.00009284536,0.00028942872,0.00010644845,0.00024056867,0.00036547708],"domain_scores_gemma":[0.99904203,0.00028112181,0.00018136155,0.00006145161,0.00012875625,0.00030527028],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023615249,0.00004822824,0.00014328121,0.00010689079,0.00083689456,0.00027549526,0.00029658258,0.00005807627,0.0005546698],"category_scores_gemma":[0.00017733026,0.000044049626,0.000036399913,0.00030141333,0.0008977179,0.00022732258,0.0000035868852,0.00018431533,0.000005945891],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000048824736,0.0000016418817,0.99694216,0.0000044597996,0.000008574639,0.00011277549,0.00017184413,0.00013551346,0.0000016833109,0.0000087195285,0.000054938442,0.0025528143],"study_design_scores_gemma":[0.00012012169,0.00017899115,0.99657935,0.000030289437,0.000007490122,0.0011019284,0.0007003664,0.00021224249,0.0000100160205,0.00036376005,0.00064678246,0.000048682996],"about_ca_topic_score_codex":0.4113198,"about_ca_topic_score_gemma":0.9994136,"teacher_disagreement_score":0.5880938,"about_ca_system_score_codex":3.9090085e-7,"about_ca_system_score_gemma":0.00049475057,"threshold_uncertainty_score":0.6436801},"labels":[],"label_agreement":null},{"id":"W2005472189","doi":"10.1139/e98-099","title":"Crustal architecture and tectonic assembly of the Central Gneiss Belt, southwestern Grenville Province, Canada: a new interpretation","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University","keywords":"Geology; Allochthon; Gneiss; Mafic; Batholith; Geochemistry; Massif; Shear zone; Craton; Lithology; Crust; Metamorphic rock; Tectonics; Paleontology; Nappe","score_opus":0.005833805933433456,"score_gpt":0.1622144238023486,"score_spread":0.15638061786891513,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2005472189","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952571,0.0009106314,0.000010347445,0.0016864183,0.000101745456,0.00004680641,0.000029139108,0.0000010195474,0.001956815],"genre_scores_gemma":[0.9992449,0.000010554308,0.0001599359,0.00025798814,0.00005072511,3.9287077e-8,0.0000014366203,7.1652784e-7,0.00027366972],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99900633,0.000050650964,0.0002358332,0.00012597542,0.00026428502,0.0003168968],"domain_scores_gemma":[0.9992116,0.00005883825,0.00013419287,0.00006375683,0.000035737958,0.0004958799],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016692237,0.00008622879,0.000158387,0.000075375836,0.00020248815,0.000059062222,0.00034674667,0.00003068538,0.002938087],"category_scores_gemma":[0.000070643604,0.000046633835,0.000069872374,0.0003547536,0.00037869258,0.00009575145,0.0000049545497,0.00015195069,0.0000019695915],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013039033,0.000002261089,0.9432935,0.0000053852395,0.000015042098,0.000018448085,0.00024920725,0.010480008,0.000056089448,0.000011706895,0.0000763391,0.045778938],"study_design_scores_gemma":[0.00009467473,0.00013273752,0.99542594,0.000034776414,0.000020019312,0.000086329426,0.00013778747,0.0013152624,0.00014234633,0.000787292,0.0017481039,0.00007471268],"about_ca_topic_score_codex":0.87880504,"about_ca_topic_score_gemma":0.9987057,"teacher_disagreement_score":0.11990063,"about_ca_system_score_codex":0.0000025692098,"about_ca_system_score_gemma":0.0028248923,"threshold_uncertainty_score":0.9979734},"labels":[],"label_agreement":null},{"id":"W2005629790","doi":"10.1139/e06-040","title":"From Proterozoic strata to a synthesized seismic reflection trace: implications for regional seismic reflection patterns in northwestern Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Proterozoic; Outcrop; Lithology; Crust; Paleontology; Sedimentary rock; Seismology; Seismic refraction; Reflection (computer programming); Tectonics","score_opus":0.03181671523257804,"score_gpt":0.2505586941316822,"score_spread":0.21874197889910416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2005629790","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916345,0.0001957079,0.0010328842,0.0059506837,0.0003291744,0.00024449133,0.00045241704,0.0000041619237,0.00015600366],"genre_scores_gemma":[0.99834824,0.000007456425,0.00046664258,0.00059848285,0.00037097605,0.0000034311215,0.00005501674,0.0000037941406,0.00014596297],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984709,0.00008591988,0.0004660685,0.00029038786,0.000252481,0.00043421873],"domain_scores_gemma":[0.99897236,0.00017241317,0.00024359707,0.00012554722,0.0000938876,0.0003921773],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053541607,0.00014552713,0.00025198047,0.00046470377,0.0003963214,0.00019232735,0.00035283217,0.000055486707,0.00014363356],"category_scores_gemma":[0.00004397398,0.00011860093,0.0000895785,0.00072728976,0.00007515305,0.00034471395,0.0000023178322,0.00014449094,0.0000039921756],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038542243,0.0000050759395,0.91840863,0.000007000942,0.00001608869,0.000018255929,0.00010473746,0.07306695,0.00015112042,0.0000067121414,0.0007468892,0.007429993],"study_design_scores_gemma":[0.0003282255,0.00040011285,0.9736663,0.000079554484,0.000032286825,0.00006524727,0.0003231525,0.011439926,0.0001498081,0.0010475203,0.0122755775,0.00019229334],"about_ca_topic_score_codex":0.98084056,"about_ca_topic_score_gemma":0.99936014,"teacher_disagreement_score":0.061627023,"about_ca_system_score_codex":0.000027899032,"about_ca_system_score_gemma":0.0022366995,"threshold_uncertainty_score":0.48364055},"labels":[],"label_agreement":null},{"id":"W2005656054","doi":"10.1139/e01-092","title":"Evolution of 3.1 and 3.0 Ga volcanic belts and a new thermotectonic model for the Hopedale Block, North Atlantic craton (Canada)","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; Government of Newfoundland and Labrador","funders":"Memorial University of Newfoundland","keywords":"Felsic; Geology; Metamorphism; Geochemistry; Greenschist; Metamorphic facies; Mafic; Volcanic rock; Plutonism; Gneiss; Ultramafic rock; Petrology; Metamorphic rock; Pluton; Facies; Geomorphology; Volcano; Paleontology; Tectonics","score_opus":0.026730766074711212,"score_gpt":0.1779060040920408,"score_spread":0.15117523801732957,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2005656054","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9900184,0.007286324,0.00013366551,0.002219817,0.000045353096,0.000061431805,0.000021724949,0.0000010257398,0.0002122508],"genre_scores_gemma":[0.9992709,0.0001680126,0.00022281586,0.00017504711,0.00004523398,1.126425e-7,5.901882e-7,7.6217424e-7,0.000116497635],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991908,0.000020202448,0.00020175628,0.0001250134,0.00020372513,0.0002585205],"domain_scores_gemma":[0.9991673,0.00015990726,0.00013368802,0.000059038895,0.00007106994,0.00040899718],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025018858,0.000077921926,0.0001570294,0.00008037345,0.0003187673,0.000046873596,0.00021895042,0.000026610052,0.00044855187],"category_scores_gemma":[0.00012616691,0.000043329343,0.000046706908,0.00030229677,0.00036491617,0.00011048914,0.000004872168,0.000092126786,8.260316e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000073698134,0.0000027255674,0.9612309,0.000008361402,0.00002070188,0.000005324491,0.0001234916,0.029980114,0.000032251635,0.000066711444,0.00041492897,0.008107149],"study_design_scores_gemma":[0.000118463475,0.00014554714,0.54791844,0.000011213243,0.000033185534,0.000038134527,0.0000743614,0.44968513,0.000010282876,0.0014135563,0.00049051567,0.0000611459],"about_ca_topic_score_codex":0.58506227,"about_ca_topic_score_gemma":0.99755985,"teacher_disagreement_score":0.41970503,"about_ca_system_score_codex":0.0000020445364,"about_ca_system_score_gemma":0.0007277485,"threshold_uncertainty_score":0.49113286},"labels":[],"label_agreement":null},{"id":"W2005849264","doi":"10.1139/e02-078","title":"Stratigraphic framework for the CambrianOrdovician rift and passive margin successions from southern Quebec to western Newfoundland","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Centre de Géomatique du Québec; Geological Survey of Canada","funders":"","keywords":"Geology; Paleontology; Ordovician; Conglomerate; Passive margin; Group (periodic table); Rift; Ecological succession; Continental margin; Sedimentary depositional environment; Marine transgression; Tectonics; Sedimentary rock; Structural basin","score_opus":0.017000623557522607,"score_gpt":0.2172791404786366,"score_spread":0.200278516921114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2005849264","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.991167,0.0013791244,0.001070062,0.005416459,0.00023505202,0.00010273315,0.00013238903,0.0000023142184,0.0004948556],"genre_scores_gemma":[0.9957719,0.000017790708,0.0027805818,0.0011179867,0.00012140435,6.5515013e-7,0.0000028427505,0.0000011842604,0.00018569283],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989513,0.00006899478,0.00023341631,0.00018617783,0.00019699337,0.00036310867],"domain_scores_gemma":[0.99831414,0.0006309495,0.00012930318,0.00009321631,0.00008276081,0.0007496337],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003444629,0.00010982252,0.00018534725,0.00013371828,0.0006816409,0.0003101599,0.00036262008,0.000058809732,0.002036472],"category_scores_gemma":[0.00044353819,0.000058004436,0.00008833038,0.00047933898,0.0004095875,0.00014232467,0.000003476318,0.00016851135,0.000021107247],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004956538,0.0000020221728,0.9953365,0.0000011067643,0.000019001938,0.000009534315,0.0002859321,0.0006539057,0.000007843866,0.00068282045,0.000028128263,0.0029682594],"study_design_scores_gemma":[0.00009415841,0.00014658383,0.9614814,0.000032709824,0.00003760167,0.000012279764,0.0016555435,0.00025798543,0.000013143447,0.027729096,0.008424887,0.00011460556],"about_ca_topic_score_codex":0.42010307,"about_ca_topic_score_gemma":0.9950956,"teacher_disagreement_score":0.57499254,"about_ca_system_score_codex":0.0000010359188,"about_ca_system_score_gemma":0.0004878249,"threshold_uncertainty_score":0.9988758},"labels":[],"label_agreement":null},{"id":"W2005937040","doi":"10.1139/e08-020","title":"Dolomitization of the Lower Ordovician Aguathuna Formation carbonates, Port au Port Peninsula, western Newfoundland, Canada: implications for a hydrocarbon reservoir","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Regina; Geological Survey of Canada; Government of Newfoundland and Labrador; Memorial University of Newfoundland","funders":"","keywords":"Dolomitization; Geology; Diagenesis; Ordovician; Geochemistry; Evaporite; Petrography; Dolomite; Sabkha; Unconformity; Subaerial; Meteoric water; Fluid inclusions; Carbonate; Paleontology; Facies; Hydrothermal circulation; Sedimentary rock","score_opus":0.02790524492040757,"score_gpt":0.22474059331779067,"score_spread":0.1968353483973831,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2005937040","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9858936,0.001161121,0.000070583585,0.0020620322,0.0005880998,0.00017506856,0.000111352,0.0000022844652,0.009935853],"genre_scores_gemma":[0.9994735,0.000021132912,0.00019777165,0.00015944323,0.000086670014,8.624493e-7,0.000007675775,9.591668e-7,0.000051956566],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987542,0.000056528836,0.0004421542,0.00013071066,0.0002627753,0.00035362097],"domain_scores_gemma":[0.99879664,0.000110867,0.0004438721,0.00014020113,0.00019277606,0.0003156423],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053919916,0.00010320965,0.00019159699,0.00019299772,0.00089792826,0.000032094118,0.00048980775,0.00006299309,0.00002345681],"category_scores_gemma":[0.0001341961,0.00007213771,0.00009690983,0.00044333056,0.0005232846,0.00043720816,0.0000013192563,0.0001219264,3.572887e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009286688,0.0000041901403,0.9978482,0.000004649285,0.000009666015,0.000009016352,0.00025242643,0.00072392815,0.00001194148,0.000097478114,0.00010002826,0.0009291544],"study_design_scores_gemma":[0.00019717243,0.00019704532,0.99676454,0.000027831513,0.000016060842,0.00023768695,0.00011437099,0.0006834981,0.000027658945,0.0005880539,0.0010581606,0.000087900364],"about_ca_topic_score_codex":0.7503397,"about_ca_topic_score_gemma":0.9994989,"teacher_disagreement_score":0.24915923,"about_ca_system_score_codex":0.000010865727,"about_ca_system_score_gemma":0.008242189,"threshold_uncertainty_score":0.99738014},"labels":[],"label_agreement":null},{"id":"W2006903831","doi":"10.1139/e11-048","title":"Olenelloid trilobites from Cambrian Series 2 of Devon Island, Nunavut, Arctic Canada","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Arctic; Geology; Paleontology; Series (stratigraphy); Taxon; Trilobite; Assemblage (archaeology); Stage (stratigraphy); Oceanography; Ordovician","score_opus":0.021722938180339636,"score_gpt":0.18363396743670904,"score_spread":0.1619110292563694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006903831","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96586317,0.007287178,0.000008444678,0.00014870545,0.0008245417,0.00004358851,0.00029440018,0.0000016518251,0.025528297],"genre_scores_gemma":[0.9986179,0.00004863517,0.0011160406,0.00007893376,0.00008121526,8.443465e-8,0.0000033352976,6.693652e-7,0.000053227162],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987136,0.00008556511,0.00039108135,0.00015260627,0.0002696995,0.00038742792],"domain_scores_gemma":[0.9987838,0.00011925254,0.0003061451,0.00010390797,0.000116015064,0.0005708531],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042424255,0.000121918805,0.00026468537,0.00022575518,0.00030529907,0.0000419506,0.0005027521,0.000060283717,0.0026592868],"category_scores_gemma":[0.00011588242,0.000093801566,0.000078602636,0.00034288707,0.00079631474,0.0004652825,8.290655e-7,0.00015879834,0.000003247698],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002287492,0.0000024380588,0.99619246,0.0000044325066,0.00002538645,0.00014696107,0.00047985086,0.000026145413,0.000021038773,0.000102444144,0.000118380754,0.0028575852],"study_design_scores_gemma":[0.00014658575,0.00032962038,0.9956036,0.000049538667,0.000018993458,0.0001423262,0.00083322596,0.00003360607,0.00064022606,0.0013319044,0.00075462944,0.00011575064],"about_ca_topic_score_codex":0.9718304,"about_ca_topic_score_gemma":0.99992824,"teacher_disagreement_score":0.032754667,"about_ca_system_score_codex":0.0000019202625,"about_ca_system_score_gemma":0.0044938945,"threshold_uncertainty_score":0.9982524},"labels":[],"label_agreement":null},{"id":"W2007088125","doi":"10.1139/e99-065","title":"The climate of North America and adjacent ocean waters ca. 6 ka","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université de Montréal; University of Alberta; University of Victoria; Geological Survey of Canada; Dalhousie University; University of Ottawa","funders":"","keywords":"Boreal; Peat; Climate change; Climate model; Taiga; Geology; Sphagnum; Biosphere; Vegetation (pathology); Bog; Climatology; Physical geography; Oceanic climate; Oceanography; Environmental science; Geography; Ecology; Forestry; Paleontology; Archaeology","score_opus":0.014260582879364783,"score_gpt":0.21349970383755257,"score_spread":0.1992391209581878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007088125","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912395,0.0023794028,4.3497096e-7,0.0015169375,0.00016222756,0.000042945805,0.000024920646,0.000001192084,0.004632477],"genre_scores_gemma":[0.99785995,0.0016950837,0.0001184528,0.00015798994,0.000025648764,4.1948557e-8,0.0000023750436,7.503769e-7,0.00013972085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886894,0.000121329125,0.00023569794,0.00010557096,0.00018356311,0.00048488812],"domain_scores_gemma":[0.9991375,0.0001959564,0.00010351521,0.00007751228,0.000060534676,0.0004249867],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00063545245,0.00006939536,0.00014605619,0.00013008,0.0007620997,0.000060391743,0.00037757462,0.000028675451,0.001451397],"category_scores_gemma":[0.000053506494,0.000039700266,0.000038697952,0.00031154306,0.0021488555,0.00015883401,0.0000035993037,0.00016700648,0.00006580589],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014812286,0.0000011561092,0.98845965,0.000003239532,0.000007503525,0.000040504783,0.00020154049,0.0010748409,1.7854492e-7,0.000010080039,0.00010223145,0.010084274],"study_design_scores_gemma":[0.00008500027,0.00027166298,0.9818062,0.000010972519,0.000005824964,0.00020945373,0.00025830432,0.000407377,0.0000068624317,0.0000859503,0.016802398,0.00004997508],"about_ca_topic_score_codex":0.0032964747,"about_ca_topic_score_gemma":0.33980256,"teacher_disagreement_score":0.3365061,"about_ca_system_score_codex":2.1069059e-7,"about_ca_system_score_gemma":0.0004939381,"threshold_uncertainty_score":0.9994614},"labels":[],"label_agreement":null},{"id":"W2007415608","doi":"10.1139/e04-012","title":"Orthopyroxene, augite, and plagioclase compositions in dacite: application to bedrock sourcing of lithic artefacts in southern British Columbia","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Okanagan University College","funders":"","keywords":"Dacite; Geology; Augite; Plagioclase; Geochemistry; Andesite; Mineral; Basalt; Mafic; Breccia; Pigeonite; Lineation; Volcanic rock; Volcano; Seismology; Paleontology; Quartz; Tectonics","score_opus":0.008247515340517264,"score_gpt":0.18183022524924425,"score_spread":0.17358270990872698,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007415608","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99833417,0.00038515843,0.00007350888,0.0006187054,0.000024191862,0.0000694998,0.00005290337,0.0000015850065,0.0004403048],"genre_scores_gemma":[0.99888325,0.000011152389,0.00083305524,0.00021991889,0.000018939701,3.544944e-7,0.000005320782,7.9706814e-7,0.000027226795],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999029,0.000033974826,0.00033457324,0.00016000753,0.000177573,0.00026487504],"domain_scores_gemma":[0.9992537,0.00006185343,0.000114161485,0.00005054744,0.000062331426,0.00045738678],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043895113,0.00005638492,0.00019050017,0.0002378673,0.00014802384,0.00015032245,0.00018797687,0.00004419406,0.0004507986],"category_scores_gemma":[0.000108466236,0.000060366838,0.000038313497,0.0009221301,0.00025960407,0.00016707831,0.0000052997784,0.00014523865,0.00001000283],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000019716322,0.000008182697,0.9627748,0.0000041698295,0.00000226423,0.000039486433,0.00032719475,0.03361663,0.00012698471,0.0000061049336,0.0000046806094,0.0030875378],"study_design_scores_gemma":[0.00019613342,0.00014163966,0.99321055,0.000098399876,0.0000055863184,0.00007604257,0.0006218284,0.00084761274,0.000040386574,0.004591432,0.00008753351,0.00008286371],"about_ca_topic_score_codex":0.6200018,"about_ca_topic_score_gemma":0.9960549,"teacher_disagreement_score":0.37605307,"about_ca_system_score_codex":0.0000027547203,"about_ca_system_score_gemma":0.0003072522,"threshold_uncertainty_score":0.49359286},"labels":[],"label_agreement":null},{"id":"W2007435328","doi":"10.1139/e09-077","title":"The late Neoproterozoic Frog Lake hornblende gabbro pluton, Avalon Terrane of Nova Scotia: evidence for the origins of appinites","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Bedford Institute of Oceanography; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University","keywords":"Geology; Hornblende; Geochemistry; Gabbro; Mafic; Pluton; Terrane; Zircon; Magma; Petrology; Igneous rock; Volcano; Biotite; Quartz; Tectonics; Paleontology","score_opus":0.040889359808193464,"score_gpt":0.24207320642333485,"score_spread":0.20118384661514138,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007435328","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927669,0.0023805099,0.00005550766,0.0036668403,0.00057637406,0.00013644264,0.0000622454,0.000001936976,0.00035323272],"genre_scores_gemma":[0.9987593,0.00009113079,0.0007753376,0.00013682997,0.00013646868,3.3950414e-7,0.000001871527,0.0000011780297,0.00009751899],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99857116,0.000052388463,0.00046866547,0.00014162203,0.00036619112,0.0003999769],"domain_scores_gemma":[0.9974525,0.0013738082,0.00040964255,0.00017492412,0.00027275103,0.00031635122],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017290869,0.00011306644,0.00024843938,0.00012764009,0.00042203077,0.00010001997,0.0010239218,0.000055793167,0.0029555694],"category_scores_gemma":[0.0010687971,0.000050663388,0.00018967738,0.0005887101,0.0016662198,0.00023304173,0.00000921915,0.00027054158,0.00001707417],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003859857,0.000006783749,0.98509485,0.000018780616,0.000051967763,0.000005736225,0.00022505272,0.0027952301,0.0020988008,0.00025386078,0.00015153717,0.009258816],"study_design_scores_gemma":[0.00021855373,0.0006489067,0.96405005,0.00011080353,0.000091013084,0.000050459807,0.0003321672,0.003987451,0.004442351,0.006217739,0.019692786,0.00015771015],"about_ca_topic_score_codex":0.055930633,"about_ca_topic_score_gemma":0.9072937,"teacher_disagreement_score":0.851363,"about_ca_system_score_codex":9.899411e-7,"about_ca_system_score_gemma":0.0006546116,"threshold_uncertainty_score":0.99795586},"labels":[],"label_agreement":null},{"id":"W2007702645","doi":"10.1139/e99-043","title":"The 1830 Ma Trans-Hudson hairpin from paleomagnetism of the Wapisu gneiss dome, Kisseynew Domain, Manitoba","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University; University of Windsor","funders":"","keywords":"Geology; Craton; Archean; Apparent polar wander; Gneiss; Terrane; Yilgarn Craton; Metamorphism; Geochemistry; Metamorphic facies; Greenstone belt; Orogeny; Sill; Geomorphology; Seismology; Metamorphic rock; Tectonics; Paleozoic; Facies","score_opus":0.008540588351215012,"score_gpt":0.20186631280412543,"score_spread":0.1933257244529104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007702645","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96481866,0.026335323,0.000013780347,0.0027018243,0.00061135314,0.00014025647,0.000059920665,0.0000018241147,0.0053170375],"genre_scores_gemma":[0.9957339,0.0017992881,0.0004219346,0.00026342648,0.00029659708,0.000002780992,0.0000026258108,0.000008657411,0.0014707742],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983944,0.00012978801,0.00043701683,0.00023294285,0.00032545958,0.00048033992],"domain_scores_gemma":[0.99899805,0.000052180843,0.000210914,0.00032028084,0.00011782899,0.00030072956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051764684,0.00017936327,0.00021284468,0.000065583234,0.00083038403,0.0001108651,0.0010279677,0.00009754434,0.0004124172],"category_scores_gemma":[0.00005728179,0.000106409374,0.00019767311,0.00028841835,0.0013731469,0.000016921696,0.000018661623,0.00016093599,0.000009479464],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031729453,0.00012914692,0.61885786,0.00006995682,0.00042280246,0.0002557953,0.0043965564,0.0008961955,0.15067755,0.0009800813,0.030954052,0.19204271],"study_design_scores_gemma":[0.0005904351,0.0011249249,0.7212829,0.00008413237,0.000040437637,0.00013236706,0.001182468,0.0000071829577,0.006701351,0.0014252114,0.26720047,0.00022810178],"about_ca_topic_score_codex":0.007589537,"about_ca_topic_score_gemma":0.3865128,"teacher_disagreement_score":0.37892324,"about_ca_system_score_codex":0.000002817228,"about_ca_system_score_gemma":0.000681856,"threshold_uncertainty_score":0.999019},"labels":[],"label_agreement":null},{"id":"W2007705444","doi":"10.1139/e04-097","title":"Geophysical evidence for a pre-impact Sudbury dome, southern Superior Province, Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Doming; Dome (geology); Magmatism; Tectonics; Igneous rock; Gneiss; Impact structure; Magma; Rift; Geochemistry; Seismology; Paleontology; Metamorphic rock; Volcano; Impact crater","score_opus":0.03286632137765457,"score_gpt":0.2816248313204135,"score_spread":0.24875850994275892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007705444","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99358433,0.0025445053,0.00001762268,0.0024873791,0.00032222312,0.00017609807,0.000096193355,0.0000031004638,0.00076852157],"genre_scores_gemma":[0.9980109,0.000016379021,0.00069732143,0.00034348664,0.00029779391,7.2918016e-7,0.000003308386,0.0000021561298,0.00062793377],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99821115,0.000113716895,0.0003163522,0.00021164668,0.00035241974,0.00079472695],"domain_scores_gemma":[0.99799144,0.0006733569,0.00014262904,0.000117841824,0.0001747026,0.0009000431],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011387118,0.00013337917,0.00025744934,0.0002304611,0.00061934633,0.00011807085,0.00067819405,0.000075067124,0.0017321493],"category_scores_gemma":[0.0005280137,0.00009327231,0.000111481735,0.00033104746,0.00079571677,0.0005200711,0.000005004339,0.00026857867,0.000055847162],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000049803537,0.0000029387825,0.99478704,0.000008490691,0.00001453199,0.000065165215,0.00020577082,0.0028131376,0.0000041151575,0.000018959765,0.00047472163,0.0015553006],"study_design_scores_gemma":[0.00023368523,0.0005922621,0.98703766,0.000052887048,0.000013667336,0.00037266253,0.00024272222,0.0027375165,0.000035231962,0.0001401589,0.008395866,0.00014566573],"about_ca_topic_score_codex":0.7310164,"about_ca_topic_score_gemma":0.9992451,"teacher_disagreement_score":0.26822868,"about_ca_system_score_codex":0.0000032104379,"about_ca_system_score_gemma":0.01675157,"threshold_uncertainty_score":0.9991804},"labels":[],"label_agreement":null},{"id":"W2007893635","doi":"10.1139/e01-073","title":"The paleoenvironment of<i>Tyrannosaurus rex</i>from southwestern Saskatchewan, Canada","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Fauna; Geology; Deciduous; Vegetation (pathology); Paleontology; Paleobotany; Macrofossil; Frost (temperature); Latitude; Ecology; Biology; Holocene","score_opus":0.014657940026566162,"score_gpt":0.16718813934920856,"score_spread":0.1525301993226424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007893635","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98089725,0.012509816,0.000008187539,0.0018707269,0.0010456976,0.000038722494,0.00013171467,0.0000012592488,0.0034966203],"genre_scores_gemma":[0.99898845,0.00012195839,0.00017660293,0.0003163074,0.000113888214,9.847134e-8,0.000002759111,8.122043e-7,0.0002791082],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988028,0.00011308151,0.0003254991,0.00012637589,0.00024375814,0.00038852746],"domain_scores_gemma":[0.9989459,0.00029452817,0.0002328113,0.0001141283,0.00003646085,0.00037615866],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00043403436,0.00008921845,0.00015775928,0.000066501016,0.0005809912,0.000028282177,0.00053741847,0.000050402654,0.001621919],"category_scores_gemma":[0.00005879036,0.000055712877,0.00005250961,0.00016741344,0.0011042352,0.00013487833,0.0000032019157,0.0001533682,0.000025399224],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000050792178,0.0000015580797,0.9914056,7.408773e-7,0.000014726082,0.00006665863,0.00026081965,0.00072382216,0.0000068755207,0.000010105785,0.0008142502,0.0066897455],"study_design_scores_gemma":[0.00009925336,0.0001444345,0.9659691,0.0000108592185,0.000009237826,0.000112873655,0.0013507288,0.00039726804,0.000018395407,0.00023948085,0.031575024,0.00007336935],"about_ca_topic_score_codex":0.8041806,"about_ca_topic_score_gemma":0.9996984,"teacher_disagreement_score":0.19551778,"about_ca_system_score_codex":0.0000030278397,"about_ca_system_score_gemma":0.0011004038,"threshold_uncertainty_score":0.9992907},"labels":[],"label_agreement":null},{"id":"W2008080256","doi":"10.1139/e09-027","title":"The Late Cambrian (Steptoean; Furongian) trilobite <i>Pseudokingstonia</i> Palmer, 1965 in North America","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; National Science Foundation","keywords":"Trilobite; Geology; Genus; Paleontology; Structural basin; Archaeology; Ordovician; Geography; Zoology; Biology","score_opus":0.011870415649125063,"score_gpt":0.20402764681200802,"score_spread":0.19215723116288297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008080256","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9458909,0.010013048,0.0000073608844,0.0019030855,0.0006115716,0.00008361277,0.000022033253,0.000004716127,0.04146366],"genre_scores_gemma":[0.998722,0.00023043493,0.00027658333,0.0005323306,0.00009535133,1.2222506e-7,9.953565e-7,6.323327e-7,0.00014150796],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99822205,0.00014804212,0.00044169283,0.0001704339,0.000305347,0.00071244495],"domain_scores_gemma":[0.99871075,0.00019199154,0.0002850305,0.00013313965,0.00006224226,0.00061685883],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009243154,0.0001484205,0.00023905846,0.00036242258,0.000920529,0.00024691588,0.00075536774,0.00005929762,0.00011546601],"category_scores_gemma":[0.00011245361,0.00009676526,0.00011865201,0.0011078009,0.00097073533,0.00047217577,7.331097e-7,0.00035053282,0.000018624307],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016610924,0.000003069429,0.8584356,8.2220885e-7,0.0000067041155,0.00016477295,0.00034295497,0.0005338612,0.000005758982,0.00006988809,0.00011460271,0.14030536],"study_design_scores_gemma":[0.00020578766,0.00047726472,0.9847755,0.00002045649,0.000006957069,0.00012032343,0.00030711188,0.00030980757,0.0000075280136,0.00030808413,0.013330433,0.00013078039],"about_ca_topic_score_codex":0.010171942,"about_ca_topic_score_gemma":0.85984427,"teacher_disagreement_score":0.8496723,"about_ca_system_score_codex":0.0000016707318,"about_ca_system_score_gemma":0.0012067654,"threshold_uncertainty_score":0.9964194},"labels":[],"label_agreement":null},{"id":"W2008126188","doi":"10.1139/e00-027","title":"Hinge modifications and musculature of strophomenoid brachiopods: examples across the Ordovician-Silurian boundary, Anticosti Island, Quebec","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Ordovician; Geology; Devonian; Paleontology; Anatomy; Hinge; Foramen; Biology","score_opus":0.022907550314977248,"score_gpt":0.24121644735253073,"score_spread":0.2183088970375535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008126188","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97635734,0.015552827,0.00007099826,0.0012913275,0.0003420088,0.00007873875,0.000119134114,0.0000027804153,0.0061848676],"genre_scores_gemma":[0.9989838,0.00020743225,0.00056228583,0.00009269862,0.00009428915,1.603933e-7,0.000001945129,7.6096495e-7,0.000056650933],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875927,0.0001045117,0.00032579343,0.00016150903,0.0002387088,0.00041020874],"domain_scores_gemma":[0.99896175,0.0001769463,0.00026138852,0.00014058335,0.00009359256,0.00036576614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008464491,0.00011556313,0.00020647775,0.00018123705,0.0012716908,0.000267154,0.00049791264,0.00007302378,0.00019428846],"category_scores_gemma":[0.000117306045,0.000072652365,0.00007794325,0.00048160783,0.0019244825,0.00047164454,0.0000016351984,0.0002475301,0.000002062604],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010124285,0.000004616136,0.96657854,0.0000047062476,0.000019957102,0.000036385176,0.0019097496,0.00023680422,0.000040456966,0.00033634368,0.000032652842,0.030789645],"study_design_scores_gemma":[0.00014946946,0.00017148427,0.99016386,0.00002924707,0.000014729582,0.00025526475,0.0020224177,0.00026556957,0.000008733718,0.00070561084,0.0061238976,0.00008970205],"about_ca_topic_score_codex":0.10946832,"about_ca_topic_score_gemma":0.98676527,"teacher_disagreement_score":0.8772969,"about_ca_system_score_codex":0.0000011470363,"about_ca_system_score_gemma":0.0009829815,"threshold_uncertainty_score":0.97809464},"labels":[],"label_agreement":null},{"id":"W2008137924","doi":"10.1139/e04-060","title":"The Early Cretaceous San Juan Plutonic Suite, Ecuador: a magma chamber in an oceanic plateau?","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Ultramafic rock; Mafic; Basalt; Fractional crystallization (geology); Pluton; Mantle (geology); Magma chamber; Peridotite; Magma; Tectonics; Paleontology","score_opus":0.014753095804178162,"score_gpt":0.2022922519657854,"score_spread":0.18753915616160724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008137924","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927478,0.002132664,0.0000022587226,0.0014348215,0.00020504874,0.00006048344,0.000012699763,0.0000048841634,0.0033993728],"genre_scores_gemma":[0.999139,0.00006082705,0.00024648372,0.0003515642,0.00009828202,1.67861e-7,0.0000025422846,0.0000016274873,0.00009947032],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981812,0.000085933454,0.00040366524,0.00022987272,0.00038054568,0.0007187341],"domain_scores_gemma":[0.99859047,0.00012994237,0.00017049629,0.00014022671,0.000089876135,0.0008789868],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010134728,0.00014219322,0.00022686287,0.00024761548,0.0005963592,0.000333477,0.0006481878,0.00006782581,0.0024199593],"category_scores_gemma":[0.00015824642,0.000080342186,0.00011986512,0.00092813256,0.0007726965,0.00048392644,0.0000075781777,0.00033566853,0.0001049729],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000140395105,0.000008186435,0.98734933,0.0000016913174,0.000010558657,0.00043310362,0.00028644575,0.007976755,0.00002851992,0.00015827024,0.000018616915,0.0037144907],"study_design_scores_gemma":[0.00022216208,0.0005210804,0.9832938,0.000021802405,0.000010869893,0.00018111167,0.00036344986,0.0006661231,0.00008847249,0.01311956,0.0013654018,0.0001461943],"about_ca_topic_score_codex":0.04473161,"about_ca_topic_score_gemma":0.89789194,"teacher_disagreement_score":0.8531603,"about_ca_system_score_codex":0.0000051203183,"about_ca_system_score_gemma":0.0009208455,"threshold_uncertainty_score":0.99849194},"labels":[],"label_agreement":null},{"id":"W2008296116","doi":"10.1139/e06-105","title":"Detrital zircon geochronology and provenance of the southeastern Yukon–Tanana terrane","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Terrane; Provenance; Conglomerate; Zircon; Felsic; Paleozoic; Precambrian; Devonian; Geochronology; Paleontology; Geochemistry; Proterozoic; Rift; Craton; Mafic; Sedimentary rock; Structural basin","score_opus":0.013350403275064652,"score_gpt":0.18502558383520937,"score_spread":0.17167518056014472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008296116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930229,0.001976609,0.000064805514,0.0011569133,0.00018711072,0.000037739548,0.000014426456,0.0000011884904,0.003538311],"genre_scores_gemma":[0.9991189,0.000012208765,0.00056767586,0.00017322644,0.00005780554,2.6517908e-8,4.275874e-7,5.527863e-7,0.0000691381],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990297,0.00003411199,0.00028484518,0.000122128,0.0001965635,0.0003326709],"domain_scores_gemma":[0.99921703,0.000104159946,0.0002041574,0.000073298215,0.00007422266,0.00032714466],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00073992764,0.00007358192,0.00017162689,0.00014200843,0.00019896858,0.00003210246,0.00037047412,0.00004505484,0.00090203277],"category_scores_gemma":[0.00017903949,0.000039040046,0.000077287856,0.00044612147,0.0010995371,0.00012772373,0.000007889942,0.00013676283,0.0000069548923],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000055112596,0.0000024801022,0.9919701,0.0000038590697,0.000007631589,0.000018632607,0.00011126507,0.00015416135,0.00045675476,0.000096273805,0.000007396072,0.007165941],"study_design_scores_gemma":[0.000108326894,0.00022512859,0.9917119,0.0000248534,0.000014096416,0.00013299924,0.00038333086,0.00019899581,0.0019901018,0.0043404326,0.00080327067,0.00006652652],"about_ca_topic_score_codex":0.017640965,"about_ca_topic_score_gemma":0.5699867,"teacher_disagreement_score":0.55234575,"about_ca_system_score_codex":6.2223324e-7,"about_ca_system_score_gemma":0.0002705029,"threshold_uncertainty_score":0.98890066},"labels":[],"label_agreement":null},{"id":"W2008371452","doi":"10.1139/e09-078","title":"Evolution of a beach–dune system following a catastrophic storm overwash event: Greenwich Dunes, Prince Edward Island, 1936–2005","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Guelph; Mount Allison University","funders":"","keywords":"Overwash; Foredune; Geology; Landform; Shore; Barrier island; Storm; Geomorphology; Oceanography","score_opus":0.006098752677017081,"score_gpt":0.1950027999447851,"score_spread":0.188904047267768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008371452","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936534,0.0027211634,0.00032327097,0.00020965989,0.0018924178,0.00012295858,0.0000798156,0.0000071686363,0.000990107],"genre_scores_gemma":[0.99874645,0.000007883874,0.0007671163,0.000030147921,0.00033231956,3.4249837e-7,0.0000066602142,0.0000037734262,0.000105272666],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980474,0.0000653026,0.00046750574,0.00022701248,0.00057147257,0.0006212659],"domain_scores_gemma":[0.9983887,0.000082736035,0.0004409857,0.00016235262,0.00013299876,0.0007922161],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014127805,0.00016374244,0.0003198549,0.00040352592,0.00048229285,0.000117531745,0.00063283875,0.00009135487,0.00027218033],"category_scores_gemma":[0.00016044753,0.00012687889,0.0001619242,0.00062275934,0.0003697769,0.0007203307,0.000008147449,0.00035060235,0.000029846375],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016279902,0.0000064068736,0.99042034,0.00007800562,0.000023759047,0.00013564418,0.00029930906,0.0062302914,0.00018874761,0.00032582466,0.00018803726,0.0020873463],"study_design_scores_gemma":[0.00048069278,0.0006455374,0.96912223,0.00034000902,0.000060553415,0.00072939,0.0010000835,0.016079672,0.000116054456,0.00021075425,0.010925266,0.00028976126],"about_ca_topic_score_codex":0.039993275,"about_ca_topic_score_gemma":0.8247669,"teacher_disagreement_score":0.7847736,"about_ca_system_score_codex":0.000008060233,"about_ca_system_score_gemma":0.0025160154,"threshold_uncertainty_score":0.9663995},"labels":[],"label_agreement":null},{"id":"W2008387935","doi":"10.1139/e08-060","title":"A re-evaluation of <i>Parasaurus geinitzi</i>, the first named pareiasaur (Amniota, Parareptilia)","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Postcrania; Paleontology; Taxon; Geology; Clade; Permian; Turtle (robot); Skull; Phylogenetics; Phylogenetic tree; Evolutionary biology; Biology; Ecology","score_opus":0.06514199701213219,"score_gpt":0.2496833353482833,"score_spread":0.1845413383361511,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008387935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97601473,0.0065709474,0.000009316152,0.002365492,0.00080109976,0.00010396739,0.000030989762,0.0000027906226,0.014100673],"genre_scores_gemma":[0.99904424,0.0001284364,0.00021002333,0.00042998517,0.00012814377,5.313131e-7,0.000003894952,9.746708e-7,0.00005379884],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998353,0.00025648563,0.00039194862,0.00015618504,0.00046479283,0.00037755404],"domain_scores_gemma":[0.99865335,0.000299145,0.00033669398,0.00014105428,0.00028122423,0.0002885048],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0024925747,0.00010052126,0.00020608433,0.00021387749,0.0009121547,0.000018910236,0.00057255605,0.00008371955,0.002001631],"category_scores_gemma":[0.00045901304,0.0000634713,0.0000909301,0.0004570188,0.0020377925,0.00029577274,0.000003425313,0.00018642611,0.000050077433],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015319913,0.0000038558996,0.9908963,0.000002002001,0.000015609454,0.000038646394,0.0005974938,0.00574217,0.0000023556843,0.000039065522,0.0011329842,0.0015141915],"study_design_scores_gemma":[0.00021396815,0.00030336273,0.9843113,0.000018818124,0.000024217798,0.0004742632,0.0005348645,0.0029715905,0.000022753597,0.00071605673,0.010328324,0.00008048457],"about_ca_topic_score_codex":0.010498901,"about_ca_topic_score_gemma":0.7025853,"teacher_disagreement_score":0.6920864,"about_ca_system_score_codex":0.0000030738845,"about_ca_system_score_gemma":0.0027290864,"threshold_uncertainty_score":0.99891067},"labels":[],"label_agreement":null},{"id":"W2008940412","doi":"10.1139/e07-001","title":"Description et analyse du glissement de terrain meurtrier du 25 octobre 1870 dans le rang des Lahaie, Sainte-Geneviève-de-Batiscan, Québec","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ministère des Transports; Ministère des Ressources naturelles et des Forêts (Québec)","funders":"","keywords":"Geology; Landslide; Aftershock; Geomorphology; Seismology; Archaeology; Geography","score_opus":0.010504781671699421,"score_gpt":0.21683119351727242,"score_spread":0.20632641184557302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008940412","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98569834,0.00045890769,0.006207734,0.0017253866,0.00022658602,0.000069158086,0.000005923166,0.000006731204,0.0056012357],"genre_scores_gemma":[0.9960444,0.00008321172,0.0026413738,0.0006717526,0.00010593452,6.987561e-7,9.582255e-7,0.0000085052625,0.00044314412],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983721,0.00011779433,0.0003666595,0.00018677875,0.00035180303,0.0006048586],"domain_scores_gemma":[0.99874115,0.000049876573,0.00019432283,0.0001086566,0.000043212127,0.000862794],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003544684,0.00013378033,0.0001667179,0.00020677781,0.0007258222,0.00019958119,0.00044327235,0.00007380184,0.0007572911],"category_scores_gemma":[0.0002110216,0.000098744735,0.000115688585,0.00051390706,0.0008939598,0.00056303124,0.000029139661,0.00020309801,0.00001986551],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011222862,0.000016601398,0.9811332,0.0000026424104,0.000021213682,0.00024009295,0.003947334,0.005263388,0.0041962615,0.0001220754,0.0011539849,0.0038919374],"study_design_scores_gemma":[0.0004117835,0.00025742035,0.96661633,0.00007121979,0.00004017182,0.0005247208,0.00498026,0.0012307173,0.0021500718,0.00047135536,0.023042733,0.0002032173],"about_ca_topic_score_codex":0.42957062,"about_ca_topic_score_gemma":0.9597226,"teacher_disagreement_score":0.53015196,"about_ca_system_score_codex":0.0002711395,"about_ca_system_score_gemma":0.001550377,"threshold_uncertainty_score":0.82918066},"labels":[],"label_agreement":null},{"id":"W2008969199","doi":"10.1139/e01-019","title":"Introduction to the special issue of Canadian Journal of Earth Sciences: The Nechako NATMAP Project of the central Canadian Cordillera","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Terrane; Geochronology; Subduction; Earth science; Magmatism; Paleontology; Mesozoic; Radiometric dating; Volcanic arc; Volcanic rock; Paleomagnetism; Geochemistry; Volcano; Tectonics; Structural basin","score_opus":0.023370065049947118,"score_gpt":0.2201261192628867,"score_spread":0.19675605421293957,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008969199","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.644454,0.0008032344,0.0003592646,0.3035649,0.009862089,0.0006025504,0.000037374473,0.000004357016,0.04031222],"genre_scores_gemma":[0.9942491,0.000027955222,0.0009592156,0.0008230511,0.0031344087,7.5735267e-7,1.7760735e-7,0.000002418481,0.00080290687],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9973375,0.00021413864,0.0006527589,0.00024094139,0.00069635396,0.0008582841],"domain_scores_gemma":[0.9971235,0.00010276307,0.000681388,0.00038862388,0.00079832866,0.0009054329],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.003075421,0.00015902493,0.00028012274,0.00090347504,0.0014813095,0.00034029907,0.003638913,0.00006975885,0.0005412407],"category_scores_gemma":[0.0011541212,0.00008384181,0.0001663827,0.0040796576,0.0015769695,0.00048792173,0.000047675814,0.00040976377,0.0000042651636],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006609603,0.00010804179,0.3894372,0.00010268474,0.00032322537,0.0007065252,0.07160033,0.10417097,0.0029127817,0.0480422,0.34044367,0.04208628],"study_design_scores_gemma":[0.00017449698,0.00046644695,0.068993166,0.00012963612,0.00001976729,0.0012629355,0.0035790934,0.0008276813,0.0024931873,0.0007137911,0.92116666,0.00017313931],"about_ca_topic_score_codex":0.55050784,"about_ca_topic_score_gemma":0.98048985,"teacher_disagreement_score":0.580723,"about_ca_system_score_codex":0.000036647896,"about_ca_system_score_gemma":0.02189017,"threshold_uncertainty_score":0.9998186},"labels":[],"label_agreement":null},{"id":"W2009288560","doi":"10.1139/e10-004","title":"The Advocate ophiolite mantle, Baie Verte, Newfoundland: regional correlations and evidence for metasomatismGeological Survey of Canada, Earth Sciences Sector, Contribution 20090211.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Ophiolite; Geology; Metasomatism; Geochemistry; Mantle (geology); Peridotite; Obduction; Partial melting; Olivine; Subduction; Amphibole; Oceanic crust; Tectonics; Paleontology","score_opus":0.05157537436299228,"score_gpt":0.24300803715314212,"score_spread":0.19143266279014984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009288560","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9914133,0.00408344,0.000103391256,0.0033213804,0.00047435283,0.00011499106,0.000112586735,0.0000022062336,0.00037434432],"genre_scores_gemma":[0.9987771,0.00012854167,0.00066050433,0.000236397,0.00007227995,6.31406e-7,0.000010964914,8.288906e-7,0.00011274631],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99822754,0.0001553832,0.00044407725,0.00022547955,0.0004467101,0.000500786],"domain_scores_gemma":[0.99581206,0.0027097461,0.00034931453,0.00009587502,0.00047453883,0.0005584725],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.003169716,0.00012299784,0.0002701344,0.00012565753,0.0013726652,0.00016183697,0.00054318085,0.00006515155,0.0008524038],"category_scores_gemma":[0.0032102638,0.0000674508,0.000080284895,0.00068377086,0.0019942087,0.00033588771,0.000010166456,0.00022679952,0.0000025498955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021636275,0.000002751821,0.99681944,0.0000028665368,0.000017191813,0.0000047816693,0.000016595874,0.0011829595,0.00006593655,0.0009704287,0.00033334756,0.0005620501],"study_design_scores_gemma":[0.00013500276,0.00026437733,0.9826906,0.000027054875,0.000024571438,0.00006115998,0.000041708074,0.008162237,0.00004223972,0.00642815,0.0020220613,0.00010086314],"about_ca_topic_score_codex":0.7490229,"about_ca_topic_score_gemma":0.9983274,"teacher_disagreement_score":0.24930447,"about_ca_system_score_codex":0.0000019493013,"about_ca_system_score_gemma":0.0028445898,"threshold_uncertainty_score":0.9999274},"labels":[],"label_agreement":null},{"id":"W2009520377","doi":"10.1139/e00-007","title":"Trace element geochemistry of the Meen-Dempster greenstone belt, Uchi subprovince, Superior Province, Canada: back-arc development on the margins of an Archean protocontinent","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Saskatchewan","funders":"","keywords":"Geology; Geochemistry; Felsic; Archean; Mafic; Basalt; Pyroclastic rock; Volcanic rock; Greenstone belt; Andesite; Island arc; Subduction; Petrology; Volcano; Paleontology; Tectonics","score_opus":0.013286155941968528,"score_gpt":0.18078568185705401,"score_spread":0.1674995259150855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009520377","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912998,0.00015776945,9.888723e-7,0.0033534353,0.000054368604,0.0004246335,0.00006663142,0.0000012133864,0.0046411795],"genre_scores_gemma":[0.9985435,0.0000057092375,0.0004335762,0.00035651037,0.00004868639,0.000002675037,0.0000045080983,0.0000016545112,0.00060316577],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978688,0.00012014495,0.0006039046,0.0002236415,0.0007135043,0.00047003964],"domain_scores_gemma":[0.9987807,0.00010218768,0.00030090823,0.00020903943,0.00013213801,0.00047498083],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009330307,0.00016309314,0.00029312196,0.00007404734,0.00037275668,0.000043587002,0.0009962522,0.00004299239,0.011094936],"category_scores_gemma":[0.00007545803,0.000077934674,0.000118259515,0.00043713063,0.0008266992,0.00012204222,0.0000115155335,0.00024058901,0.000006445822],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056629167,0.000047286147,0.97347564,0.000035241294,0.000049884376,0.000030527703,0.0003116146,0.002321974,0.00050021877,0.000044021996,0.00032337967,0.022803558],"study_design_scores_gemma":[0.00018914042,0.0002917676,0.9737038,0.00008598903,0.00001914941,0.000032157248,0.00033708123,0.0006200162,0.011623225,0.00021205156,0.012736943,0.0001486565],"about_ca_topic_score_codex":0.6015962,"about_ca_topic_score_gemma":0.993395,"teacher_disagreement_score":0.39179882,"about_ca_system_score_codex":0.000009010177,"about_ca_system_score_gemma":0.0044163046,"threshold_uncertainty_score":0.98980904},"labels":[],"label_agreement":null},{"id":"W2009650281","doi":"10.1139/e08-011","title":"Petrology and textural classification of the Jericho kimberlite, northern Slave Province, Nunavut, Canada","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Kimberlite; Geology; Pyroclastic rock; Geochemistry; Diatreme; Xenolith; Magma; Phlogopite; Country rock; Breccia; Igneous rock; Petrology; Volcano; Basalt; Mantle (geology)","score_opus":0.013855041010551721,"score_gpt":0.170565249819808,"score_spread":0.1567102088092563,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009650281","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99315685,0.0008294599,0.0000029463167,0.0023472407,0.0001501066,0.000035383928,0.000020878077,9.5071755e-7,0.0034561928],"genre_scores_gemma":[0.99934286,0.000019304543,0.000116684714,0.00027323808,0.000045765722,7.538733e-8,0.0000015224571,5.569384e-7,0.00020000231],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99904895,0.00006239502,0.00025491277,0.00012321673,0.00025975634,0.000250751],"domain_scores_gemma":[0.9991458,0.000099271936,0.00022662833,0.00007630714,0.00012770639,0.000324274],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023184056,0.000074569965,0.00016310895,0.00007574656,0.00035701512,0.000020207579,0.00034933354,0.000032062784,0.000722185],"category_scores_gemma":[0.00017182315,0.000039278217,0.00005583247,0.0004142589,0.0009787186,0.00011700555,0.000005586403,0.00013663882,0.0000026842943],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003070808,0.0000014895903,0.9977346,0.0000018622492,0.0000065538015,0.000017789396,0.00005052759,0.00064285024,0.00004506408,0.000029986124,0.000097026044,0.0013691494],"study_design_scores_gemma":[0.00006198444,0.00009336035,0.99515766,0.000005924427,0.000009844061,0.00017482386,0.0001390448,0.0011578173,0.000052224885,0.00054786244,0.0025446715,0.00005479489],"about_ca_topic_score_codex":0.7740061,"about_ca_topic_score_gemma":0.9992277,"teacher_disagreement_score":0.22522157,"about_ca_system_score_codex":0.0000025656834,"about_ca_system_score_gemma":0.0024026767,"threshold_uncertainty_score":0.790742},"labels":[],"label_agreement":null},{"id":"W2009672870","doi":"10.1139/e08-043","title":"Palynological evidence of Holocene climate change in the eastern Arctic: a possible shift in the Arctic oscillation at the millennial time scaleThis article is one of a series of papers published in this Special Issue on the theme <i>Polar Climate Stability Network</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Rimouski; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; ArcticNet; Université du Québec à Rimouski","keywords":"Terrigenous sediment; Geology; Arctic; Dinocyst; Oceanography; Deglaciation; Holocene; Arctic dipole anomaly; Palynology; Climatology; Sea level; North Atlantic oscillation; Physical geography; Sedimentary rock; Arctic ice pack; Paleontology; Geography; Ecology","score_opus":0.06668241572692662,"score_gpt":0.2540956402649667,"score_spread":0.1874132245380401,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009672870","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9733206,0.0014313093,6.594249e-8,0.023174802,0.00013214292,0.00032612693,0.000026580556,9.990559e-7,0.0015873926],"genre_scores_gemma":[0.9983769,0.0006221266,0.000027320595,0.00079085556,0.0001707511,0.0000023312045,0.0000013317391,0.0000014438675,0.000006912416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9963063,0.0015926947,0.00062993396,0.00021448174,0.00061645615,0.00064013456],"domain_scores_gemma":[0.9970792,0.0020639978,0.0003656859,0.00028135642,0.00011005679,0.000099736106],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.009228294,0.00012605656,0.0003379493,0.00020244597,0.00053103204,0.000058848796,0.0010148905,0.00010820758,0.006830553],"category_scores_gemma":[0.00092039135,0.000056540124,0.00009163318,0.0012601104,0.003801567,0.00042178304,0.00003019876,0.0005394368,0.000022529719],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024588386,0.000025891066,0.986225,0.000023201064,0.000005739406,0.000033598455,0.012847849,0.00032687202,0.0000085278825,0.00007234508,0.000031239313,0.00015383681],"study_design_scores_gemma":[0.0002060162,0.0006656471,0.9959182,0.0001784965,0.000008353671,0.00009941463,0.0015110665,0.0005707228,0.00006075415,0.0006343943,0.000085170774,0.00006172319],"about_ca_topic_score_codex":0.013622507,"about_ca_topic_score_gemma":0.50520027,"teacher_disagreement_score":0.49157774,"about_ca_system_score_codex":0.0000038644275,"about_ca_system_score_gemma":0.00038356465,"threshold_uncertainty_score":0.99890953},"labels":[],"label_agreement":null},{"id":"W2009696726","doi":"10.1139/e10-033","title":"Estimating past and future dinosaur skeletal abundances in Dinosaur Provincial Park, Alberta, Canada","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"Natural Resources Canada; University of Bristol","keywords":"Geology; Paleontology; Archaeology; Physical geography; Geography","score_opus":0.008680679606738932,"score_gpt":0.2038241829529868,"score_spread":0.19514350334624786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009696726","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98438185,0.0010903835,0.0000024883018,0.003924436,0.002834368,0.00006214444,0.000025097115,0.0000019232941,0.0076773223],"genre_scores_gemma":[0.99746865,0.000017315964,0.0011973386,0.00033163562,0.000903722,2.391301e-7,0.0000016241208,0.0000012761218,0.00007818741],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987298,0.000055314387,0.00031229426,0.00018245653,0.00025765848,0.00046244968],"domain_scores_gemma":[0.9989905,0.000189311,0.00018774103,0.000060729642,0.00006620207,0.00050553447],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000536057,0.00012792634,0.00021652116,0.00020098052,0.0005983856,0.00011493321,0.00029422378,0.00006401145,0.0004296339],"category_scores_gemma":[0.00018777656,0.00009589693,0.00003210693,0.000310455,0.00070543145,0.00038265454,0.0000045413485,0.00038320952,0.000004086975],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000022521933,0.0000014428429,0.99131817,0.0000055523715,0.000004982851,0.000063198786,0.00030201804,0.00017132203,0.0000032632834,0.00010449528,0.00033280806,0.0076904874],"study_design_scores_gemma":[0.00014345453,0.000092322996,0.97228634,0.000019235033,0.00000523168,0.0001997153,0.00067982834,0.0012600572,0.000002813285,0.00014666001,0.025040565,0.00012374588],"about_ca_topic_score_codex":0.92600435,"about_ca_topic_score_gemma":0.99999017,"teacher_disagreement_score":0.0739858,"about_ca_system_score_codex":0.0000026248752,"about_ca_system_score_gemma":0.0028058058,"threshold_uncertainty_score":0.49773788},"labels":[],"label_agreement":null},{"id":"W2009936115","doi":"10.1139/e01-010","title":"Early Eocene rodents (Mammalia) from the Eureka Sound Group of Ellesmere Island, Canada","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Geographic Society","keywords":"Holarctic; Taxon; Fauna; Sound (geography); Cenozoic; Arctic; Biological dispersal; Genus; Paleontology; Geology; Group (periodic table); Biogeography; Paleogene; Ecology; Oceanography; Cretaceous; Biology; Structural basin; Population","score_opus":0.024676705628089695,"score_gpt":0.20871525703980742,"score_spread":0.18403855141171774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009936115","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9842511,0.004822575,0.00002058641,0.0024052511,0.0010425214,0.00004724403,0.00016666742,0.0000015459572,0.0072425324],"genre_scores_gemma":[0.9985178,0.00014141247,0.00009031339,0.0008045887,0.00018342095,8.079714e-8,0.0000040342547,0.0000012271416,0.0002571102],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986651,0.00011165343,0.0003177461,0.00013621282,0.00039797788,0.00037129983],"domain_scores_gemma":[0.9989158,0.00025916027,0.0002512294,0.00010574912,0.00011159113,0.0003564841],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005275326,0.0001044096,0.00020159742,0.00009365148,0.00060813694,0.0000668659,0.0005866566,0.00004091425,0.0014244458],"category_scores_gemma":[0.000121342586,0.0000656444,0.00006114792,0.00036697043,0.00067689794,0.00021023722,0.0000046299247,0.00017371489,0.000012287658],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008907481,0.0000015978676,0.99600554,8.0412707e-7,0.00002526937,0.000064681626,0.00028253775,0.0003194539,0.0000014474348,0.000035969922,0.0023581968,0.00089559954],"study_design_scores_gemma":[0.00016989915,0.000117773496,0.97869277,0.000022286942,0.00001591182,0.00006585755,0.00095570454,0.00010978289,0.000003857364,0.0003461444,0.01941883,0.00008117724],"about_ca_topic_score_codex":0.95221275,"about_ca_topic_score_gemma":0.9999597,"teacher_disagreement_score":0.047746915,"about_ca_system_score_codex":0.000002849232,"about_ca_system_score_gemma":0.0014895668,"threshold_uncertainty_score":0.9994884},"labels":[],"label_agreement":null},{"id":"W2010033623","doi":"10.1139/e07-054","title":"Benthic island community on the back of a snail: Silurian, Anticosti Island, CanadaThis article is one of a series of papers published in this Special Issue on the theme<i>The dynamic reef and shelly communities of the Paleozoic. This Special is in honour of our colleague and friend Paul Copper</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Marine Biology and Ecology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Swedish Foundation for International Cooperation in Research and Higher Education","keywords":"Benthic zone; Ecology; Trophic level; Paleoecology; Bioerosion; Chemosynthesis; Ecosystem; Paleontology; Conch; Geology; Biology; Coral reef; Hydrothermal vent","score_opus":0.029706262320536535,"score_gpt":0.21961252357650896,"score_spread":0.18990626125597243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010033623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9753604,0.00025865622,2.3584294e-8,0.012114843,0.00019155619,0.00023051257,0.0002878096,3.8318075e-7,0.011555817],"genre_scores_gemma":[0.9986491,0.00048445113,0.000011590186,0.00039311926,0.00009033737,5.423316e-7,0.0000020748066,0.0000021677872,0.00036658617],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975098,0.0010863831,0.0005760637,0.00011214489,0.000392252,0.0003233501],"domain_scores_gemma":[0.997645,0.0013206626,0.00045325662,0.00030983982,0.00015622936,0.000114975766],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0035550203,0.00012932355,0.0004171807,0.00024440713,0.00069719844,0.00003326447,0.00094962015,0.000098765755,0.0077430024],"category_scores_gemma":[0.00063358975,0.00006540432,0.00006514348,0.0006596617,0.0036529368,0.00017858723,0.000051863375,0.0006531198,0.0000014800664],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022517091,0.000037249632,0.9781272,0.000028048711,0.000034786746,0.0000068096747,0.016396873,0.0000572596,0.000050014656,0.00007179561,0.004597034,0.00036779183],"study_design_scores_gemma":[0.00044880903,0.0009721192,0.9734725,0.0001609064,0.000012125379,0.000051639778,0.021774268,0.00024318007,0.0006957148,0.00033045936,0.0017621978,0.00007607664],"about_ca_topic_score_codex":0.123891085,"about_ca_topic_score_gemma":0.96944886,"teacher_disagreement_score":0.8455578,"about_ca_system_score_codex":0.0000056158506,"about_ca_system_score_gemma":0.0010505451,"threshold_uncertainty_score":0.99905854},"labels":[],"label_agreement":null},{"id":"W2010172948","doi":"10.1139/e02-057","title":"Determination of nearshore geologic structure off western Cape Breton Island, Nova Scotia, using high-resolution marine magnetics","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography","funders":"","keywords":"Geology; Magnetic anomaly; Lineation; Carboniferous; Submarine pipeline; Outcrop; Basement; Structural basin; Seismology; Cape; Paleontology; Oceanography; Tectonics; Archaeology","score_opus":0.032471437717411025,"score_gpt":0.23625361425855348,"score_spread":0.20378217654114245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010172948","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960352,0.0013969025,0.000058728696,0.00042705916,0.0005809183,0.00007105578,0.0000370836,0.0000020788107,0.0013909695],"genre_scores_gemma":[0.9970763,0.000046997793,0.0025851817,0.00008370866,0.000084086736,2.2077092e-8,0.0000071356026,0.000001601582,0.000114987444],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99852747,0.00015366833,0.00034402788,0.00016332627,0.00035127267,0.0004602102],"domain_scores_gemma":[0.99903667,0.000103099854,0.00026394732,0.00010335224,0.00019533631,0.00029760075],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00056825596,0.000112569454,0.0002336362,0.00046108567,0.00026659385,0.000056838086,0.00040524517,0.00014276018,0.008810779],"category_scores_gemma":[0.0001429829,0.0000884689,0.00005064088,0.00045682376,0.0011001616,0.000299586,0.000010359212,0.0002778244,0.0000324988],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000073462033,0.0000030603308,0.99173194,0.000010516561,0.0000050544536,0.00009027678,0.00014003339,0.005154372,0.000028352533,0.000012470664,0.000014368006,0.0028021852],"study_design_scores_gemma":[0.00020307106,0.0005468922,0.96734256,0.000026942032,0.000018048346,0.0009760681,0.0000782221,0.030040553,0.00008666335,0.00042072337,0.00016051004,0.00009977182],"about_ca_topic_score_codex":0.0126117375,"about_ca_topic_score_gemma":0.87764794,"teacher_disagreement_score":0.8650362,"about_ca_system_score_codex":0.0000011234466,"about_ca_system_score_gemma":0.0004170881,"threshold_uncertainty_score":0.99396336},"labels":[],"label_agreement":null},{"id":"W2010426945","doi":"10.1139/cjes-2014-0215","title":"A geochronological framework for sedimentation and Mesoproterozoic tectono-magmatic activity in lower Belt–Purcell rocks exposed west of Kimberley, British Columbia","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Zircon; Monazite; Geochemistry; Titanite; Overprinting; Metamorphism; Provenance; Metamorphic rock; Supercontinent; Thermochronology; Craton; Paleontology; Tectonics","score_opus":0.023872733866291018,"score_gpt":0.21734536537614205,"score_spread":0.19347263150985103,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010426945","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980588,0.00067245576,0.00020001721,0.00044214595,0.00014046322,0.00014233383,0.00003064719,0.0000025073468,0.0003106289],"genre_scores_gemma":[0.9953486,0.0000126176,0.004436486,0.00010994904,0.00004876351,0.0000010117627,0.0000037591549,0.0000010205968,0.00003784915],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99887264,0.00006425809,0.00031794683,0.0001879936,0.00023287906,0.0003242808],"domain_scores_gemma":[0.99884844,0.00023142638,0.00022940645,0.000058918005,0.00011825841,0.0005135355],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00078267214,0.0000781411,0.00028286697,0.0001154944,0.0001474289,0.00019359261,0.00023084573,0.00009008009,0.0019512218],"category_scores_gemma":[0.00059581595,0.00007365085,0.000070588896,0.00042681838,0.0005128543,0.00025849533,0.0000073968567,0.0001744594,0.000004014976],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001818934,0.000019149134,0.9892642,0.000013519883,0.000009713497,0.000032788743,0.0001324189,0.0008556888,0.00012398131,0.0000047751814,0.00006080263,0.009464791],"study_design_scores_gemma":[0.0004102816,0.001110884,0.9704687,0.00009129683,0.000020829188,0.000064604115,0.00039960913,0.0018487233,0.00030870913,0.024973987,0.0001728996,0.00012945433],"about_ca_topic_score_codex":0.2400676,"about_ca_topic_score_gemma":0.93584,"teacher_disagreement_score":0.69577247,"about_ca_system_score_codex":0.0000039435695,"about_ca_system_score_gemma":0.0004272614,"threshold_uncertainty_score":0.99896115},"labels":[],"label_agreement":null},{"id":"W2010474982","doi":"10.1139/e03-023","title":"New information on<i>Lethiscus stocki</i>(Tetrapoda: Lepospondyli: Aistopoda) from high-resolution computed tomography and a phylogenetic analysis of Aistopoda","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Premaxilla; Anatomy; Geology; Paleontology; Maxilla; Sister group; Biology; Phylogenetic tree","score_opus":0.011383903820226762,"score_gpt":0.19186533400097378,"score_spread":0.18048143018074703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010474982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918542,0.00375058,0.001201359,0.0005309355,0.0006336278,0.00006610169,0.00015599621,0.0000040368222,0.0018031789],"genre_scores_gemma":[0.9954446,0.00003241816,0.0041498104,0.00028608803,0.000039271603,1.12708e-7,0.00003410466,7.9777436e-7,0.000012828673],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998664,0.00019435989,0.00042666015,0.00016036491,0.00024166927,0.00031291062],"domain_scores_gemma":[0.9987363,0.00021244118,0.000346088,0.00010722574,0.00012727642,0.0004706302],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056055706,0.00012428744,0.00031944757,0.0012328842,0.0003473071,0.00004324739,0.0002595295,0.00011721306,0.0005955772],"category_scores_gemma":[0.00014074042,0.00009932418,0.00011246197,0.0014162475,0.0012314396,0.00038034888,0.0000023956115,0.00017718627,0.000009898062],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026317417,0.000004216028,0.9764736,0.0000022714808,0.00012851915,0.000010347376,0.00026409733,0.018297,0.000019296616,0.0013716958,0.00011029476,0.0032923413],"study_design_scores_gemma":[0.0002644602,0.00051234104,0.9928657,0.00001539851,0.00013129441,0.00003376209,0.00024214022,0.001957119,0.00004183068,0.0013641821,0.0024587447,0.00011306673],"about_ca_topic_score_codex":0.058115814,"about_ca_topic_score_gemma":0.6332366,"teacher_disagreement_score":0.57512075,"about_ca_system_score_codex":0.0000035525795,"about_ca_system_score_gemma":0.0010248005,"threshold_uncertainty_score":0.9481563},"labels":[],"label_agreement":null},{"id":"W2010714617","doi":"10.1139/e02-064","title":"A diminutive temnospondyl amphibian from the Pennsylvanian of Illinois","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Amphibian and Reptile Biology","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Pennsylvanian; Paleontology; Anatomy; Geology; Taxon; Crinoid; Amphibian; Devonian; Biology; Structural basin","score_opus":0.01772911971338462,"score_gpt":0.21191288510075917,"score_spread":0.19418376538737456,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010714617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9821626,0.00041896474,0.000026118636,0.0007310696,0.0003989231,0.00006974219,0.000020445152,0.0000014570487,0.016170703],"genre_scores_gemma":[0.9984503,0.000018667564,0.000733708,0.00039366697,0.000055239165,3.2667856e-7,3.5000033e-7,0.000003464296,0.00034429133],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988629,0.00013873902,0.00028825793,0.0001582531,0.00023835163,0.00031348088],"domain_scores_gemma":[0.99904865,0.00013918968,0.00025988775,0.00014031293,0.0000255177,0.00038644785],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00074990815,0.0000929112,0.00016413572,0.00006523307,0.00030310862,0.000035669967,0.0005519155,0.0000538544,0.0042692632],"category_scores_gemma":[0.0002617018,0.00005383635,0.00009277148,0.00038364987,0.0021101183,0.0001708562,0.000017017474,0.00013229625,0.00007650322],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005191818,0.000010777046,0.99102694,7.3439895e-7,0.0000130896215,0.00003825556,0.0017491727,0.0002213833,0.0027028904,0.0007544402,0.001815565,0.0016615514],"study_design_scores_gemma":[0.00022005104,0.00032186997,0.872962,0.000034282843,0.000016733647,0.00010595987,0.0021258413,0.00002436964,0.0026143487,0.0014446412,0.11998283,0.00014709446],"about_ca_topic_score_codex":0.00943784,"about_ca_topic_score_gemma":0.24290158,"teacher_disagreement_score":0.23346373,"about_ca_system_score_codex":0.000015376143,"about_ca_system_score_gemma":0.0004946385,"threshold_uncertainty_score":0.9971584},"labels":[],"label_agreement":null},{"id":"W2010730984","doi":"10.1139/e07-014","title":"Cretaceous reduced granitoids in the Goodpaster Mining District, east central Alaska","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Teck (Canada); University of British Columbia","funders":"","keywords":"Diorite; Geology; Geochemistry; Pegmatite; Monazite; Hornblende; Zircon; Biotite; Lithophile; Petrology; Quartz; Partial melting; Crust; Paleontology","score_opus":0.020614386243479336,"score_gpt":0.2002751628688499,"score_spread":0.17966077662537056,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010730984","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98765105,0.00089450425,0.000024276957,0.0015828395,0.00026118348,0.0000373176,0.000010104471,0.0000018110051,0.00953694],"genre_scores_gemma":[0.9988747,0.000008798304,0.0003861745,0.0004916691,0.00018276577,5.436008e-8,0.0000030431884,7.026538e-7,0.00005208807],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99843407,0.000075199554,0.0003468272,0.00014558111,0.00035196773,0.0006463421],"domain_scores_gemma":[0.99902016,0.00019138599,0.00013219749,0.000074653624,0.000051320927,0.0005302897],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014077028,0.000098836885,0.00016401181,0.00023460637,0.00028190424,0.00015334362,0.0005991751,0.00004280351,0.0018739338],"category_scores_gemma":[0.00021436816,0.000053661326,0.00010304031,0.0010142275,0.0004540585,0.00019895207,0.0000036268325,0.00021592421,0.000023078372],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000068037516,0.0000043028986,0.99202985,0.0000011913489,0.0000046698838,0.00023263738,0.00052168884,0.0009626768,0.00002211676,0.000014483591,0.00008052297,0.006119035],"study_design_scores_gemma":[0.00009909306,0.00016551134,0.9931288,0.000014956976,0.000010611485,0.00019183815,0.0023202389,0.00045137247,0.000054192526,0.0006437829,0.002832244,0.00008740805],"about_ca_topic_score_codex":0.0098343445,"about_ca_topic_score_gemma":0.6291993,"teacher_disagreement_score":0.619365,"about_ca_system_score_codex":0.0000017461039,"about_ca_system_score_gemma":0.00029028748,"threshold_uncertainty_score":0.9990385},"labels":[],"label_agreement":null},{"id":"W2010753291","doi":"10.1139/e01-047","title":"New material of <i>Dracochelys</i> (Eucryptodira: Sinemydidae) from the Junggar Basin, Xinjiang, People's Republic of China","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Spider Taxonomy and Behavior Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Postcrania; Geology; Paleontology; Carapace; Taxon; Structural basin; Anatomy; Sulcus; Biology; Zoology","score_opus":0.01576624961904227,"score_gpt":0.23040291946112465,"score_spread":0.21463666984208238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010753291","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994017,0.0027038578,0.00010834847,0.0014929449,0.0005375864,0.000059386894,0.000041662548,9.773983e-7,0.0010382208],"genre_scores_gemma":[0.99796754,0.00020639026,0.0010614683,0.00015091531,0.00041698117,4.427618e-7,0.0000039138176,0.0000044758885,0.00018784798],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990301,0.000050543636,0.00035761957,0.00014966096,0.00017581465,0.00023625598],"domain_scores_gemma":[0.9990921,0.000020255578,0.00034646064,0.00017750917,0.00014840832,0.00021528408],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039703376,0.00010648478,0.00022238815,0.00007875965,0.00015786327,0.000050344064,0.0004781418,0.00006071602,0.00029695194],"category_scores_gemma":[0.00018427905,0.00007176734,0.0001220708,0.00026885318,0.00037096167,0.000019362733,0.00003381084,0.0000729387,0.0000014292426],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000690605,0.00002839096,0.8906621,0.000008363744,0.0000909848,0.000022424714,0.00055416557,0.000042085372,0.088233724,0.00008914709,0.0138699915,0.0063295984],"study_design_scores_gemma":[0.00034745954,0.00046435898,0.8020333,0.00005825702,0.00005594191,0.00008427973,0.0005733243,0.0000015223734,0.09682141,0.00007749362,0.09935045,0.00013216495],"about_ca_topic_score_codex":0.014753165,"about_ca_topic_score_gemma":0.072264865,"teacher_disagreement_score":0.08862874,"about_ca_system_score_codex":0.0000027300318,"about_ca_system_score_gemma":0.0013982758,"threshold_uncertainty_score":0.9918077},"labels":[],"label_agreement":null},{"id":"W2010880846","doi":"10.1139/e04-077","title":"Geochemistry and geodynamic implications of the Mesoproterozoic English Bay granite–rhyolite complex, northwestern Ontario","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada; University of Saskatchewan","keywords":"Geology; Geochemistry; Felsic; Rhyolite; Igneous rock; Outcrop; Large igneous province; Bay; Rift; Magmatism; Structural basin; Volcanic rock; Geomorphology; Mafic; Paleontology; Tectonics; Volcano","score_opus":0.014553330713985714,"score_gpt":0.18408323699051501,"score_spread":0.1695299062765293,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010880846","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99547595,0.00034509393,0.000010351688,0.0010268949,0.00009228028,0.000050660503,0.000055298726,0.0000020294885,0.0029414373],"genre_scores_gemma":[0.9992553,0.000008913558,0.00038739853,0.00023697206,0.000047019203,1.8592944e-7,0.0000064415613,7.4160056e-7,0.000057039328],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990544,0.00002485082,0.00029207824,0.0001490395,0.00019993533,0.00027975047],"domain_scores_gemma":[0.9990672,0.000050220006,0.00020630645,0.00012016204,0.00016096541,0.00039517085],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00027493096,0.0000947868,0.00017894256,0.00008907909,0.00033799413,0.000074925374,0.0004728694,0.000041374828,0.0017032246],"category_scores_gemma":[0.000060854753,0.000055495704,0.00010606077,0.0004142749,0.0008454925,0.00015256288,0.000011114318,0.00018125038,0.000003941433],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000016527757,0.0000036372314,0.9974624,0.000003925918,0.000009752884,0.0000038763346,0.0004332497,0.0014268708,0.00013799596,0.00006220871,0.0000045816155,0.0004498657],"study_design_scores_gemma":[0.00012303967,0.00007051044,0.9871536,0.000023269477,0.00002168939,0.00006691948,0.00017308939,0.00006310954,0.00016348572,0.011267354,0.00080078846,0.00007316869],"about_ca_topic_score_codex":0.35362726,"about_ca_topic_score_gemma":0.9884072,"teacher_disagreement_score":0.63477993,"about_ca_system_score_codex":0.0000038309963,"about_ca_system_score_gemma":0.00074777636,"threshold_uncertainty_score":0.99920934},"labels":[],"label_agreement":null},{"id":"W2010882148","doi":"10.1139/e99-086","title":"Data-model comparison of the Younger Dryas event","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; University of Victoria; University of Alberta","funders":"","keywords":"Younger Dryas; Geology; Climatology; Proxy (statistics); Paleoclimatology; Radiocarbon dating; Chronology; Climate model; Climate change; Global cooling; Physical geography; Oceanography; Paleontology; Geography","score_opus":0.08378467467873678,"score_gpt":0.30620938827649846,"score_spread":0.22242471359776167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010882148","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.983126,0.0019080702,0.00000780471,0.0018320553,0.00031486244,0.00004986022,0.00006809486,0.0000011249773,0.012692147],"genre_scores_gemma":[0.9988091,0.000029130255,0.00036091884,0.00019743173,0.0000378758,4.277608e-8,0.000004000043,7.199067e-7,0.0005607741],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987639,0.00013595716,0.00031133537,0.00013201525,0.00030421294,0.00035254424],"domain_scores_gemma":[0.99913806,0.00011805578,0.00014388651,0.00023456324,0.000068714115,0.00029673442],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012787805,0.0000664501,0.00018020283,0.00012923863,0.00045184154,0.000036880792,0.0014066068,0.000056403493,0.0057382747],"category_scores_gemma":[0.00010325531,0.00003924454,0.000053174434,0.00035647338,0.0012770918,0.00035157145,0.000008694582,0.00025544327,0.00008405606],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000062783038,0.0000035556914,0.9742411,0.0000023886957,0.000007358134,0.0000074071568,0.00018525108,0.02374904,0.0000013953356,0.00005076396,0.0004567641,0.0012887414],"study_design_scores_gemma":[0.00009859021,0.00011696065,0.95508367,0.000021681302,0.000011586054,0.00013102048,0.00017345508,0.03689325,0.00003366126,0.0005900004,0.006788256,0.000057866317],"about_ca_topic_score_codex":0.0034353256,"about_ca_topic_score_gemma":0.54968286,"teacher_disagreement_score":0.5462475,"about_ca_system_score_codex":2.3157101e-7,"about_ca_system_score_gemma":0.0017147062,"threshold_uncertainty_score":0.9951706},"labels":[],"label_agreement":null},{"id":"W2010906646","doi":"10.1139/e04-025","title":"Integration and spatial analysis of high-resolution geophysical and geological data, eastern Gaspé Peninsula","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Formations and Processes Exploration","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Institut National de la Recherche Scientifique","funders":"Centre Eau Terre Environnement, Institut National de la Recherche Scientifique","keywords":"Geology; Devonian; Paleontology; Outcrop; Lithology; Sedimentary rock; Ordovician; Sequence (biology); Conglomerate; Magnetic anomaly; Unconformity","score_opus":0.034393731946510776,"score_gpt":0.22638427694732338,"score_spread":0.1919905450008126,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010906646","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.991725,0.00045349897,0.0068657324,0.0005997377,0.000081991304,0.00003663716,0.000053593154,0.0000017710449,0.00018201332],"genre_scores_gemma":[0.9976597,0.00006335992,0.0020976497,0.00007549382,0.00004227203,7.221484e-8,0.00005706125,4.138857e-7,0.0000039911974],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992409,0.000040317365,0.0002524942,0.00013277394,0.00018387249,0.00014966281],"domain_scores_gemma":[0.9993685,0.0000558544,0.0001746523,0.0000709865,0.000100903235,0.00022913713],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048090258,0.00006397345,0.00017245956,0.00031583468,0.0002149634,0.00010187522,0.00019371869,0.000041169682,0.00020976608],"category_scores_gemma":[0.00014014587,0.00004257671,0.000023973858,0.0005502499,0.00046662486,0.0007410654,0.000008867138,0.00008664329,0.0000041247167],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002160404,0.000008913574,0.92379934,0.0000057755383,0.000042467615,0.000011210325,0.0004738156,0.047210302,0.000022224347,0.0017220493,0.000006426363,0.026675876],"study_design_scores_gemma":[0.00012711546,0.0003759007,0.9041757,0.000011375843,0.000057437253,0.00002361092,0.00020750384,0.09118109,0.000016876626,0.0036694377,0.00010167349,0.000052262494],"about_ca_topic_score_codex":0.07397558,"about_ca_topic_score_gemma":0.4480301,"teacher_disagreement_score":0.37405452,"about_ca_system_score_codex":9.609727e-7,"about_ca_system_score_gemma":0.00025313246,"threshold_uncertainty_score":0.9321909},"labels":[],"label_agreement":null},{"id":"W2011162932","doi":"10.1139/e09-053","title":"Depositional setting, fossil flora, and paleoenvironment of the Early Eocene Falkland site, Okanagan Highlands, British Columbia","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Brandon University; University of Saskatchewan","funders":"","keywords":"Geology; Sedimentary depositional environment; Flora (microbiology); Context (archaeology); Subtropics; Paleoclimatology; Period (music); Paleontology; Physical geography; Geography; Climate change; Ecology; Oceanography; Structural basin","score_opus":0.007596612660813977,"score_gpt":0.18422732918979015,"score_spread":0.17663071652897616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011162932","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943897,0.002568126,0.0000026878881,0.0009437715,0.00019092325,0.00006660685,0.00004981191,0.0000014218531,0.0017869266],"genre_scores_gemma":[0.9991457,0.00006977009,0.00029502518,0.00022222559,0.000053124426,8.749047e-8,0.0000026474934,7.647169e-7,0.00021066368],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998842,0.00012111404,0.000247269,0.00014428861,0.00028596426,0.00035938562],"domain_scores_gemma":[0.99924076,0.00010153921,0.00015968262,0.000080417136,0.000050438455,0.00036716482],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066278526,0.00006366775,0.00016048072,0.000084935484,0.0007060343,0.00020848085,0.0003262309,0.0000671681,0.00084131217],"category_scores_gemma":[0.00007150514,0.000057307647,0.000052246345,0.00023131886,0.0010348586,0.00019751544,0.0000055335395,0.00020318318,0.000006863953],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000036588297,0.0000036025638,0.99764496,0.0000031301265,0.0000069129505,0.000081487706,0.00010503672,0.00011758565,0.000005635384,0.000005754193,0.00023912427,0.00178314],"study_design_scores_gemma":[0.0001946015,0.00033399664,0.9970418,0.000044867495,0.000010090782,0.0009594295,0.00005947662,0.00012288598,0.000013331635,0.0007390486,0.00041278618,0.00006766236],"about_ca_topic_score_codex":0.03584665,"about_ca_topic_score_gemma":0.8792909,"teacher_disagreement_score":0.8434442,"about_ca_system_score_codex":4.268972e-7,"about_ca_system_score_gemma":0.00035075858,"threshold_uncertainty_score":0.9705737},"labels":[],"label_agreement":null},{"id":"W2011483688","doi":"10.1139/e07-051","title":"The extent of ice on the continental shelf off Hudson Strait during Heinrich events 1-3","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada","funders":"","keywords":"Geology; Continental shelf; Ice sheet; Ice shelf; Paleontology; Iceberg; Ice stream; Glacier; Debris flow; Glacial period; Geomorphology; Oceanography; Debris; Sea ice; Cryosphere","score_opus":0.021900500971805126,"score_gpt":0.2426906471753235,"score_spread":0.22079014620351836,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011483688","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98736954,0.0018095992,0.000002897475,0.0026260137,0.00051868625,0.00008249616,0.000008871547,0.0000013924272,0.007580487],"genre_scores_gemma":[0.999386,0.00008218014,0.000042158885,0.00012639916,0.000072212184,1.0646678e-7,6.608691e-7,0.0000010173542,0.000289282],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99845135,0.00015652638,0.00032627047,0.00011701322,0.00039136258,0.000557505],"domain_scores_gemma":[0.9982897,0.00095125457,0.00020815842,0.00011289873,0.00010592927,0.0003320642],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00354927,0.00008372742,0.00013605824,0.00018088766,0.0010921705,0.000049199003,0.0007280679,0.000052249983,0.000840022],"category_scores_gemma":[0.00037314446,0.000042239237,0.000075727636,0.00036392186,0.001112452,0.00013452394,0.00000618092,0.00032179966,0.000044786248],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031031886,0.0000036515562,0.9980828,0.0000024682843,0.000013340017,0.000058566522,0.00016592212,0.0003073212,0.000016431726,0.00040343273,0.0000345733,0.00088044576],"study_design_scores_gemma":[0.00013545742,0.00028089836,0.9962369,0.00002913339,0.0000049524465,0.00019722171,0.0011280118,0.000087575376,0.00032896159,0.00033964528,0.0011807702,0.000050480703],"about_ca_topic_score_codex":0.0018779783,"about_ca_topic_score_gemma":0.42983627,"teacher_disagreement_score":0.42795828,"about_ca_system_score_codex":6.496202e-7,"about_ca_system_score_gemma":0.0005345789,"threshold_uncertainty_score":0.91976523},"labels":[],"label_agreement":null},{"id":"W2011606026","doi":"10.1139/e04-061","title":"A late Pleistocene Steller sea lion (<i>Eumetopias jubatus</i>) from Courtenay, British Columbia: its death, associated biota, and paleoenvironment","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Marine animal studies overview","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Simon Fraser University; North Island College; Canadian Museum of Nature","funders":"","keywords":"Radiocarbon dating; Macrofossil; Geology; Pleistocene; Archaeology; Subfossil; Paleontology; Geography; Holocene","score_opus":0.01734289697872756,"score_gpt":0.19711917201550563,"score_spread":0.17977627503677807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011606026","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994443,0.0024376065,0.00000934183,0.0004989447,0.00021395771,0.000148918,0.00006111676,0.0000057541333,0.00218136],"genre_scores_gemma":[0.99719435,0.0011466218,0.00045975746,0.00062551914,0.00005794683,0.0000016367703,0.0000018366463,0.000009145388,0.0005031837],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982106,0.000061966646,0.00036585212,0.00031991562,0.0005130172,0.00052863796],"domain_scores_gemma":[0.99883133,0.000046755362,0.00027030602,0.00009859444,0.000025112162,0.00072790246],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005747953,0.00013487325,0.0002900408,0.000048559228,0.00066820247,0.0003945811,0.00037163895,0.00007438948,0.002604291],"category_scores_gemma":[0.0001375093,0.00015936569,0.000077908866,0.00035191543,0.00055462396,0.00037991887,0.00010675513,0.00020658884,0.0000650679],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000233901,0.000024113078,0.9938066,0.000002807149,0.000027319307,0.00019153788,0.00013413547,0.00049088674,0.000072369556,0.000003250908,0.0006878391,0.004556829],"study_design_scores_gemma":[0.00046916478,0.00035984456,0.988039,0.0000966119,0.000032002637,0.00007015715,0.00006588464,0.00008104413,0.00003281297,0.0002917615,0.010272781,0.00018891807],"about_ca_topic_score_codex":0.6152305,"about_ca_topic_score_gemma":0.9783752,"teacher_disagreement_score":0.3631447,"about_ca_system_score_codex":0.00011137947,"about_ca_system_score_gemma":0.0001809529,"threshold_uncertainty_score":0.99830747},"labels":[],"label_agreement":null},{"id":"W2011631431","doi":"10.1139/e2012-009","title":"Emplacement ages and exhumation rates for intrusion-hosted Cu–Mo–Sb–Au mineral systems at Freegold Mountain (Yukon, Canada): assessment from U–Pb, Ar–Ar, and (U–Th)/He geochronometers","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Zircon; Geology; Geochemistry; Geochronology; Biotite; Thermochronology; Hornblende; Batholith; Hydrothermal circulation; Igneous rock; Paleontology","score_opus":0.019052108054251338,"score_gpt":0.2251509163765379,"score_spread":0.20609880832228655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011631431","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99324805,0.0040926244,0.00007558088,0.0015326785,0.0004151226,0.00014595642,0.00021419411,0.0000025892225,0.00027321043],"genre_scores_gemma":[0.9982291,0.000053952674,0.0010942633,0.0002606338,0.00020223232,0.0000014889752,0.000059573853,0.0000016304657,0.00009711825],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984266,0.00009054236,0.00038671045,0.00021858724,0.00033439018,0.00054315734],"domain_scores_gemma":[0.99829775,0.00032060785,0.00025772367,0.00006968277,0.00009865623,0.0009555679],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00085082714,0.00015918855,0.00029506176,0.00017294123,0.0006175625,0.00020178498,0.00020671249,0.000054169348,0.0012670232],"category_scores_gemma":[0.00012228444,0.00010743521,0.000049758964,0.00022921442,0.0003436749,0.00039563185,0.000016827466,0.000106419335,0.000002624119],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010621814,0.000004473738,0.9956484,0.000012815928,0.000038400703,0.000005626262,0.00015862058,0.001101771,0.00017336554,0.000047591464,0.00063299766,0.0021653369],"study_design_scores_gemma":[0.0002563325,0.00021503105,0.98577064,0.00003816587,0.00005426926,0.000029497327,0.00089443376,0.008830405,0.00008548838,0.00038016125,0.003271248,0.00017433541],"about_ca_topic_score_codex":0.8608797,"about_ca_topic_score_gemma":0.9852051,"teacher_disagreement_score":0.12432539,"about_ca_system_score_codex":0.000026878797,"about_ca_system_score_gemma":0.0005855269,"threshold_uncertainty_score":0.99964595},"labels":[],"label_agreement":null},{"id":"W2011881077","doi":"10.1139/e05-087","title":"Snow avalanche activity after fire and logging disturbances, northern Gaspé Peninsula, Quebec, Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Rimouski; Université Laval; Center for Northern Studies","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Snow; Geology; Logging; Physical geography; Peninsula; Vegetation (pathology); Disturbance (geology); Snow cover; Hydrology (agriculture); Geomorphology; Forestry; Geography; Archaeology","score_opus":0.0054406470374237965,"score_gpt":0.18029237443987892,"score_spread":0.1748517274024551,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011881077","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934022,0.0012193006,0.000009209659,0.002855715,0.00024624835,0.000040502262,0.0000073896153,0.0000021272958,0.002217298],"genre_scores_gemma":[0.99828094,0.00005995312,0.00016055533,0.00033184813,0.00011584028,5.6413495e-7,2.5355513e-7,0.0000043687232,0.0010456715],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989381,0.00003135767,0.00016770184,0.00016790914,0.0003157151,0.00037922888],"domain_scores_gemma":[0.99915904,0.000034933284,0.00012791294,0.0000819069,0.000014661574,0.00058152515],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00030612707,0.00010643114,0.00014036843,0.000040754298,0.00034146506,0.00011741163,0.00023795433,0.000042524396,0.001138093],"category_scores_gemma":[0.000038401125,0.00007310489,0.00003767873,0.00017653908,0.00046648507,0.00044377588,0.000023415712,0.00019532406,0.000014240276],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007542869,0.0000043238424,0.9763192,0.0000021475873,0.0000073927076,0.00013125004,0.00033539982,0.0017340507,0.000038164762,0.0000025295215,0.0014808092,0.019937197],"study_design_scores_gemma":[0.00015181905,0.000040630133,0.8961438,0.000042052892,0.000008766788,0.00012303363,0.00011872621,0.0010553068,0.000114229195,0.000024279076,0.10203247,0.00014491513],"about_ca_topic_score_codex":0.89472175,"about_ca_topic_score_gemma":0.99968725,"teacher_disagreement_score":0.10496552,"about_ca_system_score_codex":0.00008524817,"about_ca_system_score_gemma":0.0011369607,"threshold_uncertainty_score":0.999775},"labels":[],"label_agreement":null},{"id":"W2011939042","doi":"10.1139/e04-073","title":"New Dinopanorpidae (Insecta: Mecoptera) from the Eocene Okanagan Highlands (British Columbia, Canada and Washington State, USA)","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fossil Insects in Amber","field":"Agricultural and Biological Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Rostrum; Genus; Paleontology; Paleogene; Geology; Biology; Geography; Zoology; Structural basin","score_opus":0.012427341170420632,"score_gpt":0.17989423366181312,"score_spread":0.1674668924913925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011939042","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932281,0.0014931217,9.651936e-7,0.0032909706,0.00058976177,0.00006720135,0.0001032685,0.000004358068,0.0012222572],"genre_scores_gemma":[0.9965001,0.00007085762,0.00031931428,0.0012620623,0.0007117216,4.7606642e-7,0.000002103979,0.0000010791334,0.0011323282],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984023,0.000074905234,0.00031400064,0.00022759529,0.0005032084,0.00047800838],"domain_scores_gemma":[0.9985667,0.00024325206,0.00019831223,0.000054178272,0.00013079087,0.00080675905],"candidate_categories":["scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005411513,0.00010817004,0.00019423226,0.00001596394,0.00086667616,0.0013580569,0.0006446197,0.00004755862,0.0020803832],"category_scores_gemma":[0.00018064749,0.000055526667,0.00004969478,0.00040266407,0.00031202336,0.00044283303,0.000026441527,0.00021613762,0.000004287606],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000329908,0.0000050785584,0.8302772,0.0000011858724,0.000016945809,0.00010066991,0.00017124895,0.000044495457,0.0010831375,0.000009393263,0.035302453,0.13298489],"study_design_scores_gemma":[0.00010954104,0.00014818273,0.90256023,0.000055649707,0.000007921648,0.00013250248,0.00012383357,0.000026419113,0.00015140191,0.00024833938,0.0962937,0.00014227773],"about_ca_topic_score_codex":0.9981329,"about_ca_topic_score_gemma":0.9999969,"teacher_disagreement_score":0.13284262,"about_ca_system_score_codex":0.000037526792,"about_ca_system_score_gemma":0.0016205146,"threshold_uncertainty_score":0.9996786},"labels":[],"label_agreement":null},{"id":"W2012079833","doi":"10.1139/e02-054","title":"Baltica-Laurentia link during the Mesoproterozoic: 1.27 Ga development of continental basins in the Sveconorwegian Orogen, southern Norway","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Norges Geologiske Undersøkelse","keywords":"Geology; Laurentia; Baltica; Zircon; Craton; Orogeny; Rift; Geochemistry; Rodinia; Continental margin; Proterozoic; Continental crust; Continental arc; Felsic; Archean; Metamorphism; Paleontology; Mafic; Subduction; Tectonics; Paleozoic; Ordovician; Crust","score_opus":0.01834296951180779,"score_gpt":0.18103226696824262,"score_spread":0.16268929745643484,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012079833","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99202603,0.00096671947,0.000005561686,0.003667486,0.000121782934,0.00007571153,0.000030392785,0.0000013498112,0.0031049375],"genre_scores_gemma":[0.9990475,0.000015337162,0.00041102778,0.0002700797,0.00008275306,3.0784267e-7,0.0000015021045,0.0000010360013,0.00017040975],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985136,0.00012778038,0.00046791282,0.0001507023,0.00033629846,0.0004037471],"domain_scores_gemma":[0.99920017,0.00013596492,0.000220437,0.000107388674,0.00006317742,0.00027286465],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011297526,0.00011252431,0.00020000583,0.00016177056,0.0004064016,0.00011157607,0.0008008041,0.000041049905,0.014208975],"category_scores_gemma":[0.00012602967,0.00005301211,0.00011313966,0.00056438276,0.0005871537,0.00013799578,0.000008488472,0.00022379338,0.00014103488],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000049752903,0.000009435978,0.99276435,0.000005501271,0.00001871976,0.000036112968,0.0023546587,0.0005080708,0.00009643021,0.000017532906,0.00003847539,0.0041457615],"study_design_scores_gemma":[0.00018725773,0.000089016234,0.9895614,0.000032364358,0.000016305281,0.000084419844,0.0022299062,0.0009733441,0.0005310604,0.00042902835,0.0057490487,0.000116894415],"about_ca_topic_score_codex":0.0045732646,"about_ca_topic_score_gemma":0.6542687,"teacher_disagreement_score":0.6496954,"about_ca_system_score_codex":0.0000019934455,"about_ca_system_score_gemma":0.0001892591,"threshold_uncertainty_score":0.9866922},"labels":[],"label_agreement":null},{"id":"W2012152882","doi":"10.1139/e02-096","title":"New biostratigraphic data from the Lower Jurassic Fernie Formation in the subsurface of west-central Alberta and their stratigraphic implications","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Intertek (Canada); University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Outcrop; Lithology; Stratigraphy; Paleontology; Ammonite; Oil shale; Foothills; Geochemistry; Cretaceous","score_opus":0.03467643315397799,"score_gpt":0.2283999383243925,"score_spread":0.19372350517041453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012152882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99239236,0.0022042075,0.0012343875,0.0031003268,0.000099427096,0.000073205185,0.000029081677,0.0000019421466,0.00086507556],"genre_scores_gemma":[0.9995063,0.00024810203,0.00014818739,0.00006485576,0.000020539706,4.3235497e-7,0.0000047207764,0.0000022887332,0.000004550976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992859,0.000076842436,0.0002679116,0.00007728918,0.00012258312,0.0001694796],"domain_scores_gemma":[0.99934417,0.00014905553,0.00008529561,0.00022911796,0.000029202816,0.0001631834],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044194804,0.0000732382,0.000103447936,0.00015240979,0.00014495653,0.00013826492,0.0005555941,0.000028581113,0.000054910706],"category_scores_gemma":[0.000079694386,0.00003851712,0.000037656268,0.0008085841,0.00016342496,0.00052585226,0.0000034444263,0.00013313009,8.6447756e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011007735,0.00008192004,0.7927586,0.0000399652,0.00036417678,0.000022334758,0.032927375,0.13498744,0.009438488,0.015138453,0.0075163185,0.0067139505],"study_design_scores_gemma":[0.00046089027,0.00014882932,0.92757213,0.00011481712,0.000069040085,0.00007788793,0.010145077,0.047890007,0.0012896622,0.0043249237,0.0076326113,0.00027414187],"about_ca_topic_score_codex":0.0072359242,"about_ca_topic_score_gemma":0.7651158,"teacher_disagreement_score":0.7578799,"about_ca_system_score_codex":0.0000023238883,"about_ca_system_score_gemma":0.00037619087,"threshold_uncertainty_score":0.999375},"labels":[],"label_agreement":null},{"id":"W2012237223","doi":"10.1139/e05-106","title":"Acadian deformation in the shallow crust: an example from the Siluro-Devonian Arisaig Group, Avalon terrane, mainland Nova Scotia","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada; St. Francis Xavier University","keywords":"Geology; Terrane; Orogeny; Seismology; Devonian; Shear zone; Sinistral and dextral; Crust; Fold (higher-order function); Thrust fault; Paleontology; Subduction; Shear (geology); Fault (geology); Tectonics","score_opus":0.029858301719873664,"score_gpt":0.1985730477073941,"score_spread":0.16871474598752043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012237223","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99134225,0.00064746995,0.00003293473,0.0030755505,0.00017085792,0.00008074325,0.00003177396,0.000002888317,0.004615529],"genre_scores_gemma":[0.9979656,0.000007965637,0.00043567223,0.001249134,0.00027722106,1.607396e-7,0.00004287793,0.0000011561743,0.000020262425],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99832076,0.00020049696,0.0004019817,0.00019492368,0.00040661258,0.00047520193],"domain_scores_gemma":[0.9990334,0.00026497804,0.0001825441,0.00014859035,0.00004990447,0.00032057462],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015548615,0.00012948873,0.0001836737,0.0001690397,0.00045310313,0.00037859735,0.00095369807,0.0000693579,0.0046310187],"category_scores_gemma":[0.00006498083,0.000061490755,0.000092654176,0.0007680515,0.00051475613,0.000572195,0.0000050602016,0.00032041632,0.00008539289],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005732821,0.0000068452305,0.99358475,8.802716e-7,0.000004345375,0.00003560588,0.0005772649,0.003656154,0.000017686514,0.00010011824,0.00016822902,0.0018423912],"study_design_scores_gemma":[0.0001530974,0.00014442598,0.9824768,0.000015256075,0.000014062636,0.000055029977,0.0011755535,0.0031148235,0.000012453991,0.009327724,0.0034056236,0.00010515239],"about_ca_topic_score_codex":0.82276595,"about_ca_topic_score_gemma":0.9947716,"teacher_disagreement_score":0.17200567,"about_ca_system_score_codex":0.0000027220606,"about_ca_system_score_gemma":0.00024737706,"threshold_uncertainty_score":0.9962789},"labels":[],"label_agreement":null},{"id":"W2012589759","doi":"10.1139/e02-031","title":"Relay Mountain Group, TyaughtonMethow basin, southwest British Columbia: a major Middle Jurassic to Early Cretaceous terrane overlap assemblage","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"British Geological Survey; National Science Foundation","keywords":"Geology; Terrane; Clastic rock; Paleontology; Unconformity; Cretaceous; Group (periodic table); Facies; Basement; Structural basin; Tectonics","score_opus":0.021544678814219235,"score_gpt":0.18621821660620427,"score_spread":0.16467353779198504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012589759","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99057156,0.0018884449,0.00003848894,0.0018259798,0.00032292775,0.000109603,0.000119455544,0.00001111809,0.00511242],"genre_scores_gemma":[0.9934274,0.000035284225,0.0026479608,0.0012121208,0.00019669563,6.612304e-7,0.000006388351,0.0000037007796,0.0024697718],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974657,0.00015627159,0.0005159614,0.000400209,0.000606277,0.0008555521],"domain_scores_gemma":[0.9975487,0.00019481106,0.00023065024,0.0001615027,0.00014350023,0.0017208118],"candidate_categories":["scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009554954,0.00016816599,0.00043099365,0.00024194707,0.0007465544,0.0012071999,0.0007713313,0.0001164521,0.029008217],"category_scores_gemma":[0.0004218479,0.00016620391,0.00023259543,0.0012867856,0.00052824663,0.000496907,0.000013709049,0.00035253452,0.0003988055],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004280594,0.000013919441,0.9910133,0.000005315777,0.000023861423,0.0005840625,0.0001960748,0.00048213353,0.0000743921,0.000004320215,0.0015442993,0.006054076],"study_design_scores_gemma":[0.00022580496,0.00071929273,0.9829445,0.00007249445,0.000047176673,0.00049059704,0.00043652655,0.0007321108,0.00002385142,0.00094998966,0.013062774,0.0002948791],"about_ca_topic_score_codex":0.45751795,"about_ca_topic_score_gemma":0.97782826,"teacher_disagreement_score":0.52031034,"about_ca_system_score_codex":0.0000057398083,"about_ca_system_score_gemma":0.00018090884,"threshold_uncertainty_score":0.99982965},"labels":[],"label_agreement":null},{"id":"W2012645324","doi":"10.1139/e09-017","title":"A Hirnantian (latest Ordovician) reefal bryozoan fauna from Anticosti Island, eastern Canada: taxonomy and chemostratigraphy","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ordovician; Geology; Outcrop; Reef; Fauna; Paleontology; Chemostratigraphy; Trilobite; Bay; Devonian; Baltica; Bryozoa; Taxonomy (biology); Rugosa; Ecology; Isotopes of carbon; Oceanography; Biology","score_opus":0.02010524942791346,"score_gpt":0.19323758257799417,"score_spread":0.1731323331500807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012645324","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9657509,0.01002244,0.000023845294,0.002153109,0.00053948985,0.000093181705,0.00013987007,0.0000041340995,0.021273036],"genre_scores_gemma":[0.99811685,0.00005070294,0.0011313704,0.00049683085,0.00018073538,1.0940471e-7,0.000003724216,6.6632e-7,0.000018991053],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998455,0.00006305541,0.00038542374,0.00025233952,0.00029533575,0.0005488509],"domain_scores_gemma":[0.99850297,0.00010217168,0.00025465066,0.0001135521,0.00007628865,0.0009503713],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036925887,0.00018246162,0.00030020755,0.00027688223,0.0006049011,0.00023894162,0.00044345277,0.00008440687,0.00029412273],"category_scores_gemma":[0.000067161454,0.0001448744,0.000073345465,0.00042557425,0.000578491,0.0005216984,7.666355e-7,0.00026884896,0.000002916198],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009584241,0.0000028640347,0.94104356,0.0000014594987,0.000016619166,0.0002588772,0.00010671708,0.000019716801,0.000012453713,0.000035704044,0.00028058534,0.058211863],"study_design_scores_gemma":[0.00024263233,0.00035634305,0.99146444,0.000053406246,0.000019837202,0.0002050823,0.0002964119,0.00042744892,0.00003529992,0.00047064447,0.006242983,0.00018550313],"about_ca_topic_score_codex":0.80660653,"about_ca_topic_score_gemma":0.9993083,"teacher_disagreement_score":0.19270179,"about_ca_system_score_codex":0.000001573469,"about_ca_system_score_gemma":0.0030783499,"threshold_uncertainty_score":0.5907807},"labels":[],"label_agreement":null},{"id":"W2012707211","doi":"10.1139/e01-004","title":"Data-model comparison of the Younger Dryas event: Discussion","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Younger Dryas; Rutter; Geology; Climatology; Climate change; Proxy (statistics); Pleistocene; Oceanography; Paleontology; Geography; Cartography","score_opus":0.08871648158774281,"score_gpt":0.31531308892170873,"score_spread":0.22659660733396592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012707211","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98720443,0.0015162874,0.00005299397,0.0048526074,0.0005716482,0.000057938007,0.000049776307,0.0000013609907,0.0056929504],"genre_scores_gemma":[0.999033,0.00003066442,0.00029964876,0.00013457146,0.00004505469,4.469926e-8,0.000005288421,8.175547e-7,0.00045090888],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987,0.00014768264,0.00031577577,0.0001402834,0.00032997227,0.00036626647],"domain_scores_gemma":[0.9990407,0.000103403465,0.00021570119,0.00023916716,0.000081708335,0.00031929588],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013629511,0.00007090619,0.0001839704,0.00017820696,0.00054184964,0.0000396134,0.0013693504,0.000061708306,0.0011827998],"category_scores_gemma":[0.00019887809,0.000033116714,0.000055333763,0.00045475535,0.0011664738,0.00044918052,0.000019277555,0.00026754237,0.000034782344],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007672808,0.0000041997882,0.98871297,0.0000025180007,0.0000061251685,0.000013074714,0.00020910469,0.009944351,0.0000036153406,0.00006684351,0.00034337342,0.000686166],"study_design_scores_gemma":[0.00010488778,0.00010714895,0.95639914,0.000032041145,0.000011319273,0.000195717,0.00039676568,0.036293443,0.0000246036,0.0008277413,0.0055496297,0.000057581525],"about_ca_topic_score_codex":0.0021868737,"about_ca_topic_score_gemma":0.5873866,"teacher_disagreement_score":0.5851997,"about_ca_system_score_codex":2.8503175e-7,"about_ca_system_score_gemma":0.0014068694,"threshold_uncertainty_score":0.9997302},"labels":[],"label_agreement":null},{"id":"W2012763912","doi":"10.1139/e06-137","title":"Centrum growth patterns provide evidence for two small taxa of Hiodontidae in the Cretaceous Dinosaur Park Formation","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fish Ecology and Management Studies","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"University of Kansas; University of Minnesota","keywords":"Cretaceous; Sexual dimorphism; Extant taxon; Taxon; Geology; Paleontology; Sedimentary depositional environment; Biology; Zoology; Evolutionary biology","score_opus":0.037662082829395274,"score_gpt":0.2521352149074558,"score_spread":0.2144731320780605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012763912","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916927,0.00013944959,0.0022802746,0.0035078863,0.0002097018,0.00028252037,0.0000038267854,0.0000014574285,0.0018821881],"genre_scores_gemma":[0.9984254,0.000036355872,0.0006274667,0.00082543626,0.000032842734,0.0000031776576,2.7582647e-7,0.0000017812985,0.000047210855],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989436,0.00005268446,0.0003239757,0.00010892361,0.00020055508,0.00037022546],"domain_scores_gemma":[0.9992332,0.0002749819,0.0002857849,0.000071027775,0.00002646909,0.000108539214],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026549147,0.000071566385,0.0001193527,0.0001412864,0.00028519297,0.000040003557,0.00049831846,0.000022780105,0.00008526788],"category_scores_gemma":[0.00044375067,0.000048382393,0.000049370654,0.00029587114,0.00040000986,0.0006688914,0.000026287353,0.00008791656,0.000004299012],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010151627,0.000008613936,0.99635965,0.000015134925,0.000004083326,0.000020748215,0.0011150932,0.00025592107,0.000036954443,0.00020261845,0.0010586755,0.00091233745],"study_design_scores_gemma":[0.00019899887,0.00025875273,0.9938895,0.00006526467,0.000012513107,0.000020951014,0.0013441483,0.00012883691,0.00035376265,0.000638381,0.0030238281,0.00006502733],"about_ca_topic_score_codex":0.0035681697,"about_ca_topic_score_gemma":0.7888328,"teacher_disagreement_score":0.7852646,"about_ca_system_score_codex":0.000023099734,"about_ca_system_score_gemma":0.00008367939,"threshold_uncertainty_score":0.5394029},"labels":[],"label_agreement":null},{"id":"W2012788178","doi":"10.1139/e01-006","title":"Redefinition of the Wild Bight Group, Newfoundland: implications for models of island-arc evolution in the Exploits Subzone","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Newfoundland and Labrador; Memorial University of Newfoundland","funders":"","keywords":"Geology; Group (periodic table); Bay; Paleontology; Cove; Volcanic rock; Terrane; Period (music); Oceanography; Volcano; Tectonics; Geomorphology","score_opus":0.04318143037289691,"score_gpt":0.21621640843923334,"score_spread":0.17303497806633644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012788178","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99039906,0.0006801165,0.000690718,0.0049545174,0.00007566925,0.00009085118,0.000056729135,8.109391e-7,0.0030515194],"genre_scores_gemma":[0.9994663,0.00005611393,0.00026283792,0.00014837425,0.000042440144,7.2670196e-7,0.0000059217145,5.0233916e-7,0.000016773964],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991346,0.000068110974,0.00030922232,0.000093532944,0.00018833102,0.00020622791],"domain_scores_gemma":[0.99927497,0.00019722938,0.00022265305,0.00009411286,0.00010296459,0.00010809077],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007602043,0.000057106823,0.00013873991,0.00015422588,0.00023459358,0.000026984275,0.00045705566,0.000032959793,0.00023466788],"category_scores_gemma":[0.00013162255,0.000027568334,0.00010839527,0.00087759865,0.00038583766,0.00018566032,0.0000033286003,0.00008630416,0.0000011648787],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009965821,0.000009850225,0.9844844,0.0000033831259,0.000005314508,8.09603e-7,0.00016502432,0.00925163,0.00010861687,0.004942166,0.000047401,0.0009714624],"study_design_scores_gemma":[0.00011381598,0.00014963021,0.8301982,0.000019868361,0.000014908,0.000030013269,0.00022851297,0.003002387,0.000017209803,0.16583827,0.00034799523,0.000039147504],"about_ca_topic_score_codex":0.03873619,"about_ca_topic_score_gemma":0.7871777,"teacher_disagreement_score":0.74844146,"about_ca_system_score_codex":0.0000020481232,"about_ca_system_score_gemma":0.00022466671,"threshold_uncertainty_score":0.96766496},"labels":[],"label_agreement":null},{"id":"W2012863092","doi":"10.1139/e06-065","title":"The sequence and correlation of Early Ordovician (Arenig) graptolite faunas in the Richardson Trough and Misty Creek Embayment, Yukon Territory and District of Mackenzie, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Geology; Ordovician; Biozone; Paleontology; Trilobite; Interglacial; Biostratigraphy; Pleistocene","score_opus":0.013864865732696059,"score_gpt":0.20486189410349195,"score_spread":0.1909970283707959,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012863092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98617816,0.011269269,0.000008046533,0.00043137046,0.0001235132,0.000064999265,0.0001026163,5.039876e-7,0.0018215467],"genre_scores_gemma":[0.9997327,0.000131342,0.000072926436,0.000029174518,0.000021596228,1.5359926e-7,0.0000014884183,3.4461544e-7,0.000010324649],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990407,0.00012000222,0.0002956763,0.00010596045,0.00022081031,0.00021683783],"domain_scores_gemma":[0.99925774,0.000257668,0.00024395554,0.0000595621,0.00004226715,0.000138815],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006886164,0.00007416031,0.0001420848,0.00010517698,0.00043941665,0.000087950095,0.00020349468,0.000035364727,0.0000061670826],"category_scores_gemma":[0.00004498425,0.00004278658,0.000022081209,0.00025925247,0.0010908366,0.00022344402,9.2005774e-7,0.00013159832,2.2987429e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008423481,0.0000014207508,0.9885943,0.0000052072246,0.0000040760424,0.00002036592,0.00028714378,0.000027658825,0.000015222572,0.0001633485,0.00003282698,0.010840034],"study_design_scores_gemma":[0.00012794604,0.00019657039,0.9971293,0.000030477855,0.000009194362,0.00008235111,0.00068401714,0.00035127933,0.000009865082,0.0008738603,0.00045279096,0.00005230121],"about_ca_topic_score_codex":0.9041212,"about_ca_topic_score_gemma":0.9988869,"teacher_disagreement_score":0.094765685,"about_ca_system_score_codex":0.0000016261502,"about_ca_system_score_gemma":0.00071593496,"threshold_uncertainty_score":0.4019233},"labels":[],"label_agreement":null},{"id":"W2012865441","doi":"10.1139/e09-001","title":"A new parareptile with temporal fenestration from the Middle Permian of South Africa","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Amgen (Canada); Cape Breton University","funders":"","keywords":"Laurasia; Gondwana; Paleontology; Permian; Synapomorphy; Sister group; Geology; Autapomorphy; Pectoral girdle; Biology; Phylogenetic tree; Anatomy; Structural basin; Clade","score_opus":0.03881047214038995,"score_gpt":0.19945564890531262,"score_spread":0.16064517676492268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012865441","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9898511,0.00268629,0.00010877653,0.0016215794,0.0001821255,0.000041956497,0.000038166032,0.0000020574446,0.0054679248],"genre_scores_gemma":[0.9974659,0.000004872522,0.0021347664,0.0001672868,0.00013106734,3.2294302e-8,0.000005353262,3.9918154e-7,0.00009029946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992726,0.0000690792,0.00018915902,0.000101987986,0.00014231472,0.00022485707],"domain_scores_gemma":[0.9993296,0.00008115928,0.00018594787,0.00007249087,0.000049821887,0.00028097423],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000303821,0.00006605366,0.00012346484,0.00008342631,0.0002855376,0.00003285602,0.00032386725,0.00004583267,0.00083181297],"category_scores_gemma":[0.000043883632,0.000036010388,0.000037838698,0.00025925582,0.0004484738,0.00023543964,7.5035894e-7,0.000105325504,0.000012731582],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022470527,0.0000015296339,0.99495876,3.468578e-7,0.0000060187726,0.000023209186,0.0014147804,0.00083309825,0.0000079353495,0.00007508592,0.00020536271,0.0024513758],"study_design_scores_gemma":[0.0001202328,0.0006796169,0.9944152,0.000021305832,0.000009363622,0.000075775606,0.0009969854,0.00021807392,0.0000123464815,0.0014332391,0.0019646313,0.000053194104],"about_ca_topic_score_codex":0.018595854,"about_ca_topic_score_gemma":0.5757867,"teacher_disagreement_score":0.5571909,"about_ca_system_score_codex":7.6461106e-7,"about_ca_system_score_gemma":0.0018595292,"threshold_uncertainty_score":0.9879394},"labels":[],"label_agreement":null},{"id":"W2012880656","doi":"10.1139/e05-012","title":"The Okanagan Highlands: Eocene biota, environments, and geological setting, southern British Columbia, Canada and northeastern Washington, USA","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Ecology and Vegetation Dynamics Studies","field":"Environmental Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Brandon University","funders":"","keywords":"Climate change; Geography; Temperate climate; Ecology; Biota; Global warming; Archaeology; Biology","score_opus":0.005005426286889099,"score_gpt":0.1717778114005345,"score_spread":0.1667723851136454,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012880656","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99603176,0.0008062451,0.0000070730202,0.0022787007,0.000106643856,0.00004743021,0.000012368862,0.0000010665698,0.00070873956],"genre_scores_gemma":[0.9968381,0.0001675454,0.00023477428,0.000587067,0.000041841406,7.041625e-7,3.2005886e-7,0.0000025577456,0.0021270995],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990735,0.00005152288,0.0002066725,0.00015750345,0.00018977432,0.00032105067],"domain_scores_gemma":[0.9993729,0.00010068635,0.00014257627,0.000052846117,0.000008006409,0.00032301276],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0005775691,0.00006516512,0.00010588515,0.000017194974,0.0013754821,0.00025080345,0.00021811828,0.000035060773,0.0003430496],"category_scores_gemma":[0.000078937264,0.000058786278,0.00001634164,0.000081341306,0.001430141,0.00016216497,0.000045369194,0.00012826161,0.000008713539],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[6.4679165e-7,0.0000023833006,0.99378586,6.137657e-7,0.0000068664513,0.000024769592,0.00021777354,0.00031072093,0.000004815344,0.0000069262546,0.00030551196,0.005333143],"study_design_scores_gemma":[0.00011907652,0.00006464752,0.9741801,0.00000847588,0.0000073322144,0.00017186574,0.0005453706,0.00054099964,0.0000015444285,0.00013639114,0.024144722,0.00007945458],"about_ca_topic_score_codex":0.8767792,"about_ca_topic_score_gemma":0.99995947,"teacher_disagreement_score":0.12318026,"about_ca_system_score_codex":0.000022637687,"about_ca_system_score_gemma":0.00021153982,"threshold_uncertainty_score":0.9999246},"labels":[],"label_agreement":null},{"id":"W2012954239","doi":"10.1139/e10-023","title":"Extending the Krogh legacy: development of the CA–TIMS method for zircon U–Pb geochronologyThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Aeronautics and Space Administration","keywords":"Zircon; Honor; Geology; Hadean; Leaching (pedology); Theme (computing); Geochemistry; Computer science; Soil science","score_opus":0.0333229188153754,"score_gpt":0.2170995057571147,"score_spread":0.18377658694173932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012954239","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9903185,0.000469134,0.000021207956,0.0036921185,0.00016008958,0.00016357555,0.000038758535,7.774544e-7,0.005135883],"genre_scores_gemma":[0.99336106,0.000028864863,0.0063219205,0.00017177375,0.000058903228,0.0000011394538,9.4496716e-7,0.0000013645283,0.00005403266],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980853,0.00022364315,0.000847838,0.00017639388,0.00031365015,0.00035318252],"domain_scores_gemma":[0.99828714,0.0005020924,0.00074154354,0.0001825305,0.00017929934,0.0001073931],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0026870337,0.00011929376,0.00046397504,0.00025022804,0.00015372227,0.000017109172,0.000891992,0.00008109543,0.016024752],"category_scores_gemma":[0.00070239196,0.000056960682,0.0001636131,0.00092629564,0.0015280677,0.000270678,0.000026916558,0.0002269686,0.000002027178],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000358458,0.00018857443,0.896184,0.00010002198,0.00024132321,0.000011186283,0.025503896,0.0021816962,0.02143904,0.0032541219,0.00042881875,0.05010885],"study_design_scores_gemma":[0.0003894746,0.0006991952,0.6587348,0.00016787433,0.00004805593,0.000016340404,0.006608737,0.0004518487,0.3205128,0.010172592,0.0020703455,0.00012792996],"about_ca_topic_score_codex":0.028900366,"about_ca_topic_score_gemma":0.3446174,"teacher_disagreement_score":0.31571704,"about_ca_system_score_codex":0.0000051388406,"about_ca_system_score_gemma":0.00079778454,"threshold_uncertainty_score":0.9848747},"labels":[],"label_agreement":null},{"id":"W2012973352","doi":"10.1139/e06-056","title":"Extreme sediment delivery events recorded in the contemporary sediment record of a montane lake, southern Coast Mountains, British Columbia","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Northern British Columbia; University of British Columbia; Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Varve; Sediment; Geology; Sedimentary budget; Hydrology (agriculture); Snowmelt; Glacier; Sedimentary depositional environment; Watershed; Drainage basin; Physical geography; Oceanography; Snow; Geomorphology; Structural basin; Sediment transport; Geography","score_opus":0.015286152883167807,"score_gpt":0.1883919766355577,"score_spread":0.1731058237523899,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012973352","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944696,0.00059863325,0.0000052309256,0.00038596254,0.000298346,0.00016732048,0.00005420617,0.0000021806716,0.004018508],"genre_scores_gemma":[0.9983771,0.000046673238,0.00027518236,0.00023860294,0.000056598892,0.0000018826936,0.0000030116953,0.0000056395497,0.0009953363],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99830747,0.00011758804,0.00052456267,0.00017629641,0.00052716176,0.00034692828],"domain_scores_gemma":[0.9992706,0.000043558473,0.00032685784,0.00011063376,0.000032549764,0.00021576113],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012748936,0.00009048957,0.00020378295,0.00007542635,0.00025628903,0.00014931454,0.0004958938,0.0000621029,0.0014120748],"category_scores_gemma":[0.000021163025,0.00007835016,0.000089675064,0.00044089617,0.00038849542,0.00025164333,0.000025651414,0.00019433534,0.000014516523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009890979,0.00004276244,0.98733014,0.0000030213168,0.000008932626,0.0002918656,0.00045084287,0.0008338229,0.00010070829,0.0000019330882,0.008546247,0.0023798475],"study_design_scores_gemma":[0.0009923007,0.0005615515,0.9517906,0.0002587758,0.000019984322,0.00037089907,0.003101136,0.00035912255,0.000027569064,0.0007992769,0.041495603,0.00022323437],"about_ca_topic_score_codex":0.6655866,"about_ca_topic_score_gemma":0.98918104,"teacher_disagreement_score":0.32359445,"about_ca_system_score_codex":0.000038672573,"about_ca_system_score_gemma":0.00046124472,"threshold_uncertainty_score":0.99950075},"labels":[],"label_agreement":null},{"id":"W2012976262","doi":"10.1139/e05-090","title":"SantonianCampanian planktonic foraminifera in the New Jersey coastal plain and their distribution related to the relative sea-level changes","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Geology; Foraminifera; Plankton; Paleontology; Cretaceous; Coastal plain; Oceanography; Benthic zone","score_opus":0.027031823135574496,"score_gpt":0.2348068940586462,"score_spread":0.20777507092307168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012976262","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96974593,0.0015071228,0.000052054667,0.025999522,0.0002110943,0.000159677,0.00022698577,0.000002116907,0.002095481],"genre_scores_gemma":[0.99926984,0.000025754187,0.000087113745,0.0003558151,0.00006260109,3.8304705e-7,0.000028720055,0.0000010500041,0.00016871296],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986832,0.0002899776,0.00021441157,0.00015020565,0.00018985811,0.0004723296],"domain_scores_gemma":[0.99897134,0.0005189043,0.00010253721,0.00008825926,0.000045812198,0.00027311427],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020236024,0.00010423238,0.00015002424,0.00018949213,0.0007047908,0.0001298085,0.00046521187,0.000081788974,0.00020526692],"category_scores_gemma":[0.00018152509,0.000052402345,0.00003180237,0.0006645751,0.0007180884,0.00021397327,0.000006693506,0.0003906589,0.00003068661],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012161448,0.00000190271,0.99555784,0.0000012884532,0.0000048035267,0.00007270745,0.0015132133,0.00055629364,8.0310735e-7,0.0009890458,0.00059811096,0.0006918346],"study_design_scores_gemma":[0.00017119538,0.00031197592,0.98590267,0.000025267462,0.00000433463,0.00076148775,0.0019164598,0.00049484463,0.000011034171,0.0036772024,0.0066511454,0.000072408184],"about_ca_topic_score_codex":0.018168556,"about_ca_topic_score_gemma":0.96546096,"teacher_disagreement_score":0.9472924,"about_ca_system_score_codex":0.0000010124389,"about_ca_system_score_gemma":0.0009331074,"threshold_uncertainty_score":0.9883695},"labels":[],"label_agreement":null},{"id":"W2013608438","doi":"10.1139/e99-076","title":"Lithoprobe line 55: integration of out-of-plane seismic results with surface structure, metamorphism, and geochronology, and the tectonic evolution of the eastern Grenville Province","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec); Memorial University of Newfoundland; McGill University","funders":"","keywords":"Geology; Metamorphism; Orogeny; Laurentia; Basement; Geochemistry; Geochronology; Imbrication; Metamorphic rock; Proterozoic; Alpine orogeny; Tectonics; Petrology; Crust; Diachronous; Geomorphology; Paleontology; Paleozoic","score_opus":0.009742847738139241,"score_gpt":0.17756494310365903,"score_spread":0.16782209536551979,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013608438","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953351,0.0028300616,0.000022828712,0.0012966468,0.00004524007,0.000080170204,0.00008453033,7.3499854e-7,0.00030467528],"genre_scores_gemma":[0.9993152,0.00005827883,0.00047982167,0.000030657804,0.000015753147,4.6104358e-8,0.0000025642585,5.7243665e-7,0.000097122196],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909556,0.00011061293,0.0003195914,0.00012432238,0.00019388115,0.00015605136],"domain_scores_gemma":[0.99924564,0.00012347817,0.00032972716,0.000091072805,0.00009606792,0.00011402949],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005828706,0.000080057536,0.00023047488,0.000067132765,0.00013762522,0.000020375985,0.00024955408,0.000039885945,0.00031145883],"category_scores_gemma":[0.00009126134,0.00003268437,0.00004277045,0.00031969024,0.002136397,0.000104610524,0.0000061045703,0.00013804049,9.539841e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000362693,0.000009630273,0.9304087,0.000027188655,0.00006909416,0.0000065129325,0.0006921681,0.046921577,0.0008545173,0.00018826578,0.00001482606,0.020444797],"study_design_scores_gemma":[0.0009126336,0.0007909003,0.95533454,0.00012043252,0.00011960574,0.0001947785,0.0004903193,0.03347812,0.0027468016,0.0053774742,0.00031509492,0.00011930216],"about_ca_topic_score_codex":0.04830993,"about_ca_topic_score_gemma":0.5087157,"teacher_disagreement_score":0.46040577,"about_ca_system_score_codex":0.0000013359312,"about_ca_system_score_gemma":0.0003469684,"threshold_uncertainty_score":0.9580275},"labels":[],"label_agreement":null},{"id":"W2013669710","doi":"10.1139/e02-104","title":"Seismotectonic characteristics of the Lower St. Lawrence Seismic Zone, Quebec: insights from geology, magnetics, gravity, and seismics","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Montreal Police Service; Geological Survey of Canada","funders":"Polytechnique Montréal","keywords":"Precambrian; Geology; Basement; Seismology; Lineament; Fault (geology); Nappe; Shield; Sedimentary rock; Geomorphology; Geophysics; Tectonics; Paleontology","score_opus":0.011944179379351312,"score_gpt":0.18889653261877132,"score_spread":0.17695235323942002,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013669710","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99160403,0.004839242,0.000062956635,0.0006607882,0.0011935027,0.000078349185,0.000095204814,0.0000030116598,0.0014629227],"genre_scores_gemma":[0.9984364,0.000272865,0.00042409106,0.00056077156,0.000065319895,1.0578105e-7,0.0000020490822,0.0000025295165,0.00023587042],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985695,0.00015550622,0.00040003026,0.00020450314,0.00029663346,0.00037386778],"domain_scores_gemma":[0.998784,0.00022964505,0.00034344813,0.00017373385,0.00014415992,0.00032503193],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042347578,0.00015466852,0.00030344975,0.0001685718,0.00048477363,0.00010714437,0.00046120404,0.00008104894,0.0005552967],"category_scores_gemma":[0.00024052276,0.00010074841,0.00008285699,0.00041313702,0.0017349125,0.00022570699,0.000014073662,0.0002831257,0.000010078674],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000056938547,0.000008653175,0.98858786,0.0000074178474,0.000028286384,0.00004819636,0.00052568084,0.0004927504,0.000014098462,0.00061101204,0.00011919371,0.009551161],"study_design_scores_gemma":[0.00018113083,0.00030322347,0.9735037,0.00005645627,0.000027272932,0.00009041698,0.00035316532,0.0005492346,0.00012746268,0.0028390347,0.021829553,0.0001393218],"about_ca_topic_score_codex":0.13268219,"about_ca_topic_score_gemma":0.7442793,"teacher_disagreement_score":0.6115971,"about_ca_system_score_codex":0.0000025854495,"about_ca_system_score_gemma":0.0014816851,"threshold_uncertainty_score":0.87309337},"labels":[],"label_agreement":null},{"id":"W2013673315","doi":"10.1139/e08-025","title":"Normal polarity magnetosubchrons in 24r and the age of the Paleocene–Eocene boundary","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Magnetostratigraphy; Overbank; Paleontology; Radiometric dating; Zircon; Cyclostratigraphy; Isotopes of carbon; Sequence (biology); Fluvial; Geochemistry; Isotope; Paleomagnetism; Sedimentary rock; Structural basin","score_opus":0.022679683618494522,"score_gpt":0.21650184195689554,"score_spread":0.19382215833840102,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013673315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9846647,0.005200282,0.0000012592715,0.0029156248,0.00028839157,0.0000713745,0.000012012,7.7805055e-7,0.006845581],"genre_scores_gemma":[0.99926126,0.00018491133,0.00011087944,0.0002940791,0.0000345744,1.093206e-7,8.24734e-7,6.6207105e-7,0.00011267558],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987078,0.00031401997,0.00025939682,0.000103388134,0.0002337133,0.000381715],"domain_scores_gemma":[0.9992114,0.00031262875,0.000120089644,0.000105723106,0.000053651354,0.00019655828],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0017040572,0.0000719432,0.00019094929,0.00018890336,0.0008266902,0.000036867867,0.0005652098,0.000062761195,0.0005124206],"category_scores_gemma":[0.00024389845,0.00003724998,0.000059030976,0.00048475864,0.006775237,0.00020416858,0.000011444944,0.00037499366,0.0000065224053],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019968755,0.0000021733806,0.99883455,0.0000039056417,0.0000041969847,0.00013967339,0.0005398391,0.00015775603,0.0000019062629,0.00012380582,0.000026082678,0.00014615105],"study_design_scores_gemma":[0.0004000497,0.00010482437,0.9961966,0.000015955706,0.0000047060794,0.0012589126,0.00017799439,0.00016515609,0.000019281122,0.0007353105,0.0008761066,0.000045094745],"about_ca_topic_score_codex":0.017369237,"about_ca_topic_score_gemma":0.8087799,"teacher_disagreement_score":0.7914107,"about_ca_system_score_codex":3.5279226e-7,"about_ca_system_score_gemma":0.0017395082,"threshold_uncertainty_score":0.99592775},"labels":[],"label_agreement":null},{"id":"W2013751498","doi":"10.1139/e04-030","title":"Geochemical evolution of a 10 m-thick intrusive body: the South Brenterch diabase dyke, Western Armorican Massif, France","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Massif; Geochemistry; Phenocryst; Magmatism; Igneous differentiation; Intrusion; Magma; Magma chamber; Pluton; Petrology; Basalt; Tectonics; Volcanic rock; Volcano; Paleontology","score_opus":0.01276331060769914,"score_gpt":0.193904321167131,"score_spread":0.18114101055943185,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013751498","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935996,0.0012910134,0.00017002226,0.003533132,0.00018276773,0.00005549927,0.000052079293,0.0000033865513,0.0011124824],"genre_scores_gemma":[0.99906015,0.000014069283,0.00040133897,0.00028049134,0.00015138742,2.7993582e-7,0.0000038579587,0.0000012037103,0.000087230044],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99839705,0.00007535207,0.00041148637,0.0002075949,0.00045340025,0.00045514028],"domain_scores_gemma":[0.9986391,0.00013156848,0.00031863686,0.0001308867,0.00020548012,0.0005743344],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00066676753,0.00013213318,0.00026849614,0.00019736495,0.00027389865,0.000077260665,0.0006832065,0.00006466718,0.0026221517],"category_scores_gemma":[0.00034746443,0.00007462568,0.00016977043,0.0008751929,0.0012894592,0.00021197788,0.000012352546,0.00029650723,0.00006524487],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013178667,0.000011352116,0.9958276,0.000006226551,0.000020052528,0.00003581371,0.0003201595,0.0026438013,0.00024956928,0.00012780643,0.000033737804,0.00071070023],"study_design_scores_gemma":[0.00038612087,0.00042231995,0.98135865,0.00007941073,0.000049702998,0.00010518426,0.0007349783,0.00066991965,0.0015482667,0.012927421,0.0015372095,0.00018079737],"about_ca_topic_score_codex":0.034893222,"about_ca_topic_score_gemma":0.15663403,"teacher_disagreement_score":0.12174082,"about_ca_system_score_codex":0.000005736149,"about_ca_system_score_gemma":0.0009297681,"threshold_uncertainty_score":0.9982896},"labels":[],"label_agreement":null},{"id":"W2014419642","doi":"10.1139/e08-045","title":"Paleomagnetism of fluorite veins in the Devonian St. Lawrence granite, Newfoundland, Canada","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor","funders":"","keywords":"Geology; Paleomagnetism; Devonian; Apparent polar wander; Orogeny; Zircon; Clockwise; Geochemistry; Carboniferous; Vein; Paleozoic; Paleontology; Late Devonian extinction; Fluorite; Fold (higher-order function); Tectonics; Structural basin","score_opus":0.016978782741242402,"score_gpt":0.17942837235206688,"score_spread":0.16244958961082448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014419642","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911292,0.0016130396,0.00000305849,0.0016225586,0.0001573497,0.00003513677,0.00004699477,8.478685e-7,0.005391771],"genre_scores_gemma":[0.9990402,0.00007125514,0.00026687988,0.0005044334,0.000058235728,9.976963e-8,0.0000037329687,5.4280554e-7,0.00005464124],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99864465,0.00009012723,0.00033233594,0.00012480722,0.00044342113,0.00036463546],"domain_scores_gemma":[0.99911356,0.0001991133,0.00015270489,0.000089225985,0.0000921094,0.00035327006],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000550639,0.000089664056,0.00019931317,0.00016413702,0.00030309169,0.00003634893,0.0006800253,0.00003158373,0.0026297113],"category_scores_gemma":[0.00016397824,0.000050999643,0.00006569781,0.00097175816,0.0006677961,0.00016604601,0.000003397649,0.00018835966,0.0000062506806],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002665098,0.000004476117,0.99706817,0.0000020678349,0.0000036448548,0.00024859316,0.00019145384,0.0012739769,0.00000865983,0.000043125157,0.00016572284,0.0009874451],"study_design_scores_gemma":[0.00010193036,0.00023982607,0.9903709,0.000015013271,0.0000060078264,0.0002180848,0.000276051,0.00033813412,0.000014644214,0.0011472522,0.0071959123,0.00007622324],"about_ca_topic_score_codex":0.9639124,"about_ca_topic_score_gemma":0.9998047,"teacher_disagreement_score":0.035892256,"about_ca_system_score_codex":0.0000021108865,"about_ca_system_score_gemma":0.001851965,"threshold_uncertainty_score":0.998282},"labels":[],"label_agreement":null},{"id":"W2014587165","doi":"10.1139/e01-003","title":"Time-frequency analysis of deep crustal reflection seismic data using Wigner-Ville distributions","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Centre National de la Recherche Scientifique","keywords":"Skeletonization; Instantaneous phase; Geology; Reflection (computer programming); Hilbert–Huang transform; Seismology; Energy (signal processing); Geophysics; Computer science; Radar; Artificial intelligence; Statistics","score_opus":0.0455515330707062,"score_gpt":0.26918355532039845,"score_spread":0.22363202224969225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014587165","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9856843,0.0010429234,0.0079651605,0.00053986197,0.00030301587,0.000048754206,0.00029013015,0.000015707463,0.0041101915],"genre_scores_gemma":[0.9949391,0.00005156573,0.0046196794,0.0002132469,0.000062076055,2.9771916e-8,0.000058479356,0.0000017873347,0.00005403244],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99877304,0.00007924506,0.0003571059,0.0001861157,0.00029351428,0.0003109625],"domain_scores_gemma":[0.99891883,0.00006138471,0.00029184372,0.00022643217,0.00016401343,0.00033746782],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010089214,0.00008928514,0.00022350425,0.0009699242,0.00047087308,0.00009375419,0.00067822536,0.0000442017,0.0016844446],"category_scores_gemma":[0.00017350177,0.000073257,0.00009475379,0.0023249877,0.0006113541,0.00084765884,0.000009223189,0.00013110042,0.000013296821],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001363327,0.000016702692,0.90134746,0.000006498907,0.00024238008,0.00011212365,0.00037398748,0.06707064,0.0004936396,0.000059581394,0.002264136,0.027999187],"study_design_scores_gemma":[0.00009624935,0.00019942042,0.06866224,0.00003475294,0.0002797052,0.00023127643,0.00056271994,0.91887206,0.0002600559,0.00046212904,0.010179568,0.00015980694],"about_ca_topic_score_codex":0.086283654,"about_ca_topic_score_gemma":0.07428113,"teacher_disagreement_score":0.85180146,"about_ca_system_score_codex":0.0000064793608,"about_ca_system_score_gemma":0.0009097222,"threshold_uncertainty_score":0.9992282},"labels":[],"label_agreement":null},{"id":"W2014664195","doi":"10.1139/e10-056","title":"Detrital zircon geochronology and provenance of Devono-Mississippian strata in the northern Canadian Cordilleran miogeoclineThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.Northwest Territories Geoscience Office Contribution 0047. Geological Survey of Canada Contribution 20100432.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Northwest Territories; University of Alberta","funders":"","keywords":"Zircon; Geology; Laurentia; Devonian; Provenance; Paleozoic; Baltica; Paleontology; Conodont; Geochronology; Carboniferous; Dalradian; Baltic Shield; Late Devonian extinction; Archean; Orogeny; Precambrian; Ordovician; Biostratigraphy; Metamorphism; Tectonics; Structural basin","score_opus":0.01738444595036832,"score_gpt":0.18417364909185072,"score_spread":0.1667892031414824,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014664195","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995904,0.0006410346,0.0000012583813,0.0017285527,0.00011167604,0.00018912126,0.00085743674,5.7971897e-7,0.00056629075],"genre_scores_gemma":[0.99970037,0.000060453465,0.00009765572,0.00007979196,0.00003213436,7.9428906e-7,0.000022384671,0.0000010983935,0.0000053294416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974393,0.000413584,0.0010371043,0.00023830088,0.00038618565,0.00048552],"domain_scores_gemma":[0.9976079,0.0006432496,0.0008325214,0.00017600141,0.0005169006,0.00022343897],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002797222,0.00014869228,0.00064429047,0.00034226573,0.00011038232,0.0000148856525,0.0007008602,0.00013528443,0.002556874],"category_scores_gemma":[0.002252348,0.00009046965,0.00006969568,0.0013332486,0.0026257895,0.00025845921,0.000016238651,0.0003011839,2.742306e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015739426,0.0000520651,0.99716544,0.000014924522,0.000017720327,0.000015988335,0.0007718243,0.00024404174,0.0005413363,0.00025271237,0.000015152734,0.00075137004],"study_design_scores_gemma":[0.00037722453,0.0008900457,0.9854837,0.00008629942,0.000014136948,0.000014182491,0.0011687281,0.00013968622,0.010835161,0.000765283,0.0001352022,0.00009036526],"about_ca_topic_score_codex":0.9921774,"about_ca_topic_score_gemma":0.9998856,"teacher_disagreement_score":0.011681786,"about_ca_system_score_codex":0.000016183554,"about_ca_system_score_gemma":0.0029702086,"threshold_uncertainty_score":0.9983549},"labels":[],"label_agreement":null},{"id":"W2014698113","doi":"10.1139/e07-060","title":"Sediment supply versus storm winnowing in the development of muddy and shelly interbeds from the Upper Ordovician of the Cincinnati region, USAThis article is one of a series of papers published in this Special Issue on the theme<i>The dynamic reef and shelly communities of the Paleozoic. This Special is in honour of our colleague and friend Paul Copper</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Winnowing; Geology; Taphonomy; Sedimentary rock; Paleontology; Overprinting; Storm; Sedimentary depositional environment; Clastic rock; Ordovician; Ooid; Sedimentary structures; Geologic record; Oceanography; Archaeology","score_opus":0.025553924657582525,"score_gpt":0.2109209787329818,"score_spread":0.18536705407539927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014698113","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98575646,0.001762254,1.5128315e-7,0.007906929,0.0002488658,0.00024719755,0.00010233053,4.344534e-7,0.0039753737],"genre_scores_gemma":[0.9993192,0.00028884973,0.00009825695,0.00020808559,0.00006666584,8.0996085e-7,5.414866e-7,0.0000013392025,0.000016272928],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978429,0.0005274147,0.0007464005,0.0001340841,0.00050733064,0.00024183684],"domain_scores_gemma":[0.99819505,0.0007870989,0.0005829978,0.00025051163,0.00011752669,0.00006679149],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002204213,0.00013997918,0.00036708548,0.00018530375,0.00047445484,0.000037140122,0.0008953759,0.00007105908,0.0003239691],"category_scores_gemma":[0.00022889367,0.000063619525,0.00007290761,0.0007202408,0.002663487,0.0002644787,0.000019558758,0.00036790574,9.849674e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016773347,0.000022905748,0.8663475,0.000012204307,0.000037835733,0.0000038046667,0.13049395,0.000026277174,0.000111565205,0.000079065474,0.00034416092,0.0023529897],"study_design_scores_gemma":[0.00049718865,0.00033210308,0.9119336,0.00025515686,0.000016625212,0.000018398192,0.08511723,0.000081575345,0.0010911772,0.00020730005,0.00038492124,0.00006469918],"about_ca_topic_score_codex":0.022721382,"about_ca_topic_score_gemma":0.811032,"teacher_disagreement_score":0.78831065,"about_ca_system_score_codex":0.0000062513113,"about_ca_system_score_gemma":0.00091040414,"threshold_uncertainty_score":0.9837864},"labels":[],"label_agreement":null},{"id":"W2014746811","doi":"10.1139/e05-101","title":"A reappraisal of the tectonic significance of early Tertiary low-angle shear zones exposed in the Vernon map area (82 L), Shuswap metamorphic complex, southeastern Canadian Cordillera","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta","funders":"","keywords":"Geology; Shear zone; Metamorphic rock; Cretaceous; Shear (geology); Metamorphic core complex; Tectonics; Anticline; Sedimentary rock; Crust; Seismology; Petrology; Paleontology; Geomorphology","score_opus":0.024367810137169314,"score_gpt":0.19475587494172045,"score_spread":0.17038806480455113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014746811","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99323404,0.0008122925,0.0000053699455,0.0026828037,0.00014513374,0.0001315512,0.00010997201,0.0000017633703,0.0028770785],"genre_scores_gemma":[0.9993991,0.0000044949165,0.00018770547,0.00029168732,0.00006528079,5.924692e-7,0.000005268886,0.0000018605468,0.000043979653],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99795264,0.0001997088,0.00057330035,0.00020662945,0.0005374146,0.0005303334],"domain_scores_gemma":[0.9987345,0.00024014468,0.0003441305,0.00020614004,0.00012805262,0.00034702945],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009407291,0.0001532718,0.00035275178,0.00031465117,0.00027454304,0.00007873815,0.0011158716,0.00006467866,0.0023526875],"category_scores_gemma":[0.00011312154,0.000079281024,0.00020609883,0.0010634913,0.0011569584,0.00017264829,0.000008922213,0.0002617171,0.00001367406],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001042157,0.000017814265,0.9935386,0.000011619392,0.000016401827,0.00004203445,0.00046485997,0.0048746243,0.00059571496,0.00006023729,0.00005192012,0.0003157559],"study_design_scores_gemma":[0.00015717419,0.00021575468,0.9949052,0.00006944184,0.000030299783,0.000031028256,0.00086096604,0.00185512,0.00034706993,0.00095661834,0.00045794153,0.00011339488],"about_ca_topic_score_codex":0.7861376,"about_ca_topic_score_gemma":0.9772836,"teacher_disagreement_score":0.191146,"about_ca_system_score_codex":0.0000026224704,"about_ca_system_score_gemma":0.0011423246,"threshold_uncertainty_score":0.9985593},"labels":[],"label_agreement":null},{"id":"W2014931048","doi":"10.1139/e99-117","title":"Dawson tephra: a prominent stratigraphic marker of Late Wisconsinan age in west-central Yukon, Canada","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; The Scarborough Hospital","funders":"","keywords":"Tephra; Geology; Rhyolite; Geochemistry; Zircon; Plagioclase; Loess; Quaternary; Volcano; Geomorphology; Paleontology; Volcanic rock; Quartz","score_opus":0.010443323441439051,"score_gpt":0.17030538853021965,"score_spread":0.1598620650887806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014931048","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918779,0.0011224577,6.608755e-7,0.001173507,0.00010119971,0.00005409075,0.00003342316,0.0000011874214,0.0056355507],"genre_scores_gemma":[0.99900883,0.000052643947,0.00049194036,0.00024167243,0.00003323825,1.11900086e-7,0.000004374299,7.651228e-7,0.00016640284],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99848014,0.0000716562,0.00043869845,0.00016471905,0.000334845,0.0005099215],"domain_scores_gemma":[0.9990266,0.000066034205,0.0001436025,0.00007628528,0.000054469903,0.0006330151],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004373284,0.00011237653,0.00026632234,0.00020144138,0.00012055096,0.000053521922,0.00036250416,0.0000409173,0.011704087],"category_scores_gemma":[0.00007454827,0.00007534695,0.000074448195,0.0008997183,0.00049507373,0.00018604007,0.0000021480323,0.00017729534,0.0000052455],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012635009,0.0000052846076,0.98944914,0.000004226875,0.000009668027,0.0002447112,0.0000670908,0.004546674,0.00005169358,0.000019834342,0.00011445391,0.00547461],"study_design_scores_gemma":[0.0001543542,0.0001675938,0.9939172,0.000039255807,0.000011375385,0.00003778264,0.00011294612,0.0012273941,0.000066116125,0.001290527,0.0028703166,0.00010513252],"about_ca_topic_score_codex":0.91481036,"about_ca_topic_score_gemma":0.99946344,"teacher_disagreement_score":0.084653065,"about_ca_system_score_codex":0.0000028129828,"about_ca_system_score_gemma":0.0022479824,"threshold_uncertainty_score":0.98919934},"labels":[],"label_agreement":null},{"id":"W2015102195","doi":"10.1139/e00-032","title":"Temporal evolution of a deeply eroded orogen: the Nagssugtoqidian Orogen, West Greenland","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Danmarks Grundforskningsfond; National Science Foundation","keywords":"Geology; Craton; Zircon; Laurentia; Geochemistry; Pegmatite; Geochronology; Subduction; Lithosphere; Continental collision; Sinistral and dextral; Paleontology; Thermochronology; Supercontinent; Orogeny; Tectonics","score_opus":0.014043889844996939,"score_gpt":0.184167419467084,"score_spread":0.17012352962208707,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015102195","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9883416,0.002931273,0.000009092936,0.0020929626,0.00011345533,0.000051913907,0.000035346875,0.000002904904,0.0064213984],"genre_scores_gemma":[0.99900323,0.000040317853,0.00041278353,0.0002476114,0.00011142551,1.3293919e-7,0.0000039314673,9.988468e-7,0.00017953839],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985767,0.00010690183,0.0003895323,0.00016203137,0.0003638382,0.00040098414],"domain_scores_gemma":[0.9989039,0.00010789051,0.00019229534,0.00011768364,0.00012730969,0.0005509318],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008830628,0.000110723,0.00022644165,0.00016376913,0.00041507004,0.00007883737,0.00061392476,0.000052209187,0.025725486],"category_scores_gemma":[0.00011646841,0.000059450333,0.000154557,0.00091383944,0.00089953066,0.00023856203,0.0000037288346,0.0001642843,0.00013047727],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010968094,0.0000046779505,0.98871726,0.0000025693842,0.000017808994,0.000027191187,0.00010644976,0.0026233685,0.000026775571,0.00007656412,0.00010552705,0.008280853],"study_design_scores_gemma":[0.00015143001,0.0003549561,0.9823005,0.000021180454,0.000036656165,0.00015464558,0.00035775203,0.0015291355,0.00019449445,0.0069744578,0.007801382,0.00012341788],"about_ca_topic_score_codex":0.12034315,"about_ca_topic_score_gemma":0.7482322,"teacher_disagreement_score":0.62788904,"about_ca_system_score_codex":0.0000021569476,"about_ca_system_score_gemma":0.0007345736,"threshold_uncertainty_score":0.9751651},"labels":[],"label_agreement":null},{"id":"W2015233306","doi":"10.1139/e99-106","title":"Oxygen isotope evolution of volcanic rocks at the Sturgeon Lake volcanic complex, Ontario","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum","funders":"","keywords":"Phenocryst; Geology; Geochemistry; Zircon; Volcanic rock; Quartz; Isotopes of oxygen; Igneous rock; Andesite; Volcano; Rhyolite; Magma; Paleontology","score_opus":0.01820601806448417,"score_gpt":0.18713894937276523,"score_spread":0.16893293130828108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015233306","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9818993,0.0013097029,0.000007792833,0.0015776438,0.00014072387,0.00006105764,0.00004640287,0.0000025561178,0.014954786],"genre_scores_gemma":[0.9964741,0.000025749332,0.00007388738,0.00035667332,0.00006553552,1.4790551e-7,0.000009025391,9.622587e-7,0.0029939152],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99847937,0.000082745835,0.0004065393,0.00018207192,0.0004110359,0.0004382141],"domain_scores_gemma":[0.9989453,0.00010233717,0.00020965474,0.00013027915,0.00012008947,0.0004923453],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006899589,0.00011960698,0.00025259153,0.00013517127,0.00054023595,0.00006411809,0.0006386375,0.000051822277,0.15919328],"category_scores_gemma":[0.0000669016,0.00006658675,0.00017257869,0.0006356278,0.0006877779,0.000193893,0.000008296447,0.00020161874,0.0001821868],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014066625,0.0000050589415,0.98511297,0.0000018361243,0.000020142827,0.000013451894,0.00017526576,0.010500408,0.00004636788,0.000019447056,0.0008163107,0.0032746983],"study_design_scores_gemma":[0.000103389255,0.00025410202,0.9210853,0.000013909271,0.000027464392,0.00006706196,0.00013882865,0.0009685731,0.000039857267,0.0021014223,0.07510387,0.00009619757],"about_ca_topic_score_codex":0.5772846,"about_ca_topic_score_gemma":0.9992817,"teacher_disagreement_score":0.42199713,"about_ca_system_score_codex":0.000010394154,"about_ca_system_score_gemma":0.0010526014,"threshold_uncertainty_score":0.8415753},"labels":[],"label_agreement":null},{"id":"W2015357485","doi":"10.1139/e06-002","title":"Structural variation along the Devil's Mountain fault zone, northwestern Washington","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"U.S. Geological Survey","keywords":"Geology; Seismology; Fault (geology); Transform fault; Quaternary; Fault scarp; Subduction; Strike-slip tectonics; Paleontology; Tectonics","score_opus":0.015448176634433368,"score_gpt":0.2059066781550438,"score_spread":0.19045850152061042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015357485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9917827,0.0022956063,0.000057110017,0.0009229981,0.00071479595,0.00007208026,0.000022296988,0.000005767323,0.004126591],"genre_scores_gemma":[0.9988312,0.000019288917,0.0003695311,0.00024754682,0.00036726502,1.4623738e-7,0.0000044043663,0.000001930416,0.00015868607],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985848,0.000083750485,0.00034641003,0.00015069332,0.00039757165,0.0004367813],"domain_scores_gemma":[0.99913216,0.00018847203,0.0002467173,0.00010065243,0.00012285021,0.00020915376],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00088147214,0.00012197261,0.00015909373,0.00019400998,0.0010548068,0.00035719847,0.00046863887,0.00004088218,0.0007492513],"category_scores_gemma":[0.00006589711,0.00007153984,0.000077368284,0.00047142056,0.0004381395,0.00055235316,0.0000048507745,0.00019154196,0.000037684847],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026066143,8.1270235e-7,0.98338234,0.0000020657335,0.0000098938945,0.00003569699,0.0004244814,0.009087102,0.0000039245474,0.0003062858,0.000100440295,0.006644353],"study_design_scores_gemma":[0.0001226388,0.00012518311,0.99224204,0.000020191685,0.000013613332,0.00015092162,0.00047620985,0.0015710318,0.000022906463,0.0007057842,0.004444849,0.0001046485],"about_ca_topic_score_codex":0.3120662,"about_ca_topic_score_gemma":0.97005916,"teacher_disagreement_score":0.6579929,"about_ca_system_score_codex":0.0000030281449,"about_ca_system_score_gemma":0.00079605554,"threshold_uncertainty_score":0.82037765},"labels":[],"label_agreement":null},{"id":"W2015503164","doi":"10.1139/e06-049","title":"Variable unroofing in the western Superior Province - metamorphic evidence and possible origin","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Sinistral and dextral; Metamorphic rock; Seismology; Fault (geology); Crust; Mafic; Deformation (meteorology); Compression (physics); Geochemistry","score_opus":0.029031777361440622,"score_gpt":0.21153624565990997,"score_spread":0.18250446829846934,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015503164","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905508,0.0047388496,0.00002029596,0.0025781512,0.00007145562,0.000049310944,0.000005709956,0.0000017458351,0.0019836428],"genre_scores_gemma":[0.99804574,0.000025140194,0.0012539914,0.00043729658,0.000079187936,1.7231716e-7,8.684739e-7,5.601137e-7,0.00015706511],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988592,0.00010118845,0.00026562042,0.00015671269,0.00026487093,0.00035239419],"domain_scores_gemma":[0.9992977,0.00027891365,0.00009848697,0.00006920772,0.0000481271,0.00020756038],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014582349,0.00008525436,0.00016679883,0.00017995588,0.0002800913,0.00028861416,0.00045470503,0.00003161098,0.0008924598],"category_scores_gemma":[0.00017612474,0.000045217894,0.000040787643,0.0007664039,0.0004598184,0.00051324745,0.0000048132,0.00016769496,0.000013922953],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021586684,0.000002718871,0.9965225,0.0000037038767,0.0000020879752,0.00007080359,0.00004546897,0.0024948283,0.0000420485,0.0002827536,0.000029117593,0.0005018223],"study_design_scores_gemma":[0.000064140324,0.00013583382,0.9874455,0.000051981624,0.000014315977,0.00015705082,0.00011635126,0.0010834621,0.00005394078,0.008396637,0.0023987293,0.000082069004],"about_ca_topic_score_codex":0.1726734,"about_ca_topic_score_gemma":0.7706281,"teacher_disagreement_score":0.5979547,"about_ca_system_score_codex":0.00000119099,"about_ca_system_score_gemma":0.00062800647,"threshold_uncertainty_score":0.9771809},"labels":[],"label_agreement":null},{"id":"W2016194959","doi":"10.1139/e10-045","title":"Stratigraphy, sedimentology, and taphonomy of the <i>Albertosaurus</i> bonebed (upper Horseshoe Canyon Formation; Maastrichtian), southern Alberta, CanadaThis article is one of a series of papers published in this Special Issue on the theme <i>Albertosaurus</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; University of Alberta","funders":"","keywords":"Geology; Paleontology; Taphonomy; Palaeochannel; Overbank; Trace fossil; Canyon; Macrofossil; Geomorphology; Sedimentary depositional environment; Fluvial","score_opus":0.007970705402229888,"score_gpt":0.17496534649553735,"score_spread":0.16699464109330747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016194959","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9569105,0.0003290538,3.5225906e-7,0.011342189,0.0006007923,0.0001548564,0.00018531842,8.5899234e-7,0.03047606],"genre_scores_gemma":[0.9987982,0.000022036926,0.00013742015,0.0005898189,0.00015586962,7.341833e-7,0.0000032691173,0.0000016703754,0.00029098935],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99842286,0.00018198926,0.0005739852,0.00016850836,0.00027681992,0.00037585903],"domain_scores_gemma":[0.99861,0.0003483474,0.00051306846,0.00019492807,0.00011303945,0.00022061587],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008706228,0.00013757027,0.00030913926,0.00028422652,0.0002794722,0.00003152818,0.00057981926,0.00012657224,0.011040067],"category_scores_gemma":[0.00029154727,0.00008062227,0.00009179302,0.00065397436,0.0022787016,0.00051377376,0.000010168079,0.00035213694,0.000004182471],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007981881,0.000020341853,0.9895524,0.000011994507,0.000039244962,0.0000041709313,0.004511588,0.00006426333,0.0013222394,0.0013702576,0.002052115,0.00097158924],"study_design_scores_gemma":[0.00040574715,0.0004903401,0.9682078,0.00006315184,0.000034589895,0.0001432659,0.0036419192,0.00017667918,0.004614358,0.0014258488,0.020642176,0.00015413541],"about_ca_topic_score_codex":0.33266753,"about_ca_topic_score_gemma":0.9878093,"teacher_disagreement_score":0.6551418,"about_ca_system_score_codex":0.0000025976701,"about_ca_system_score_gemma":0.0011740185,"threshold_uncertainty_score":0.989864},"labels":[],"label_agreement":null},{"id":"W2016202804","doi":"10.1139/e00-058","title":"Minette bodies and cognate mica-clinopyroxenite xenoliths from the Milk River area, southern Alberta: records of a complex history of the northernmost part of the Archean Wyoming craton","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Archean; Craton; Proterozoic; Geochemistry; Igneous rock; Xenolith; Large igneous province; Phlogopite; Mantle (geology); Tectonics; Paleontology; Magmatism","score_opus":0.027511829873088686,"score_gpt":0.17635983379639442,"score_spread":0.14884800392330572,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016202804","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912685,0.0029403064,4.1077317e-7,0.0023242284,0.00015001238,0.000061398845,0.00020075036,7.3148476e-7,0.0030536216],"genre_scores_gemma":[0.9978137,0.00006490071,0.000112566464,0.00048051812,0.000051080613,1.3380301e-7,0.00000260782,0.0000013105007,0.001473158],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998626,0.0001695111,0.0004570469,0.0001545109,0.00033215815,0.00026075405],"domain_scores_gemma":[0.9986225,0.00047367715,0.00043804347,0.00017485402,0.00011492651,0.0001760063],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042419528,0.00011523571,0.00029018792,0.000052656636,0.00026503598,0.000018455876,0.0007302895,0.000042611173,0.005506132],"category_scores_gemma":[0.00019146808,0.000050517843,0.00018468607,0.0002318207,0.003041516,0.0000794776,0.000015722628,0.00018104695,0.0000047424633],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021871168,0.000005988352,0.99034446,0.000004449961,0.000038355305,0.0000019304268,0.0036361353,0.00046709063,0.00029149317,0.000002647299,0.00040499508,0.0047805775],"study_design_scores_gemma":[0.00015814565,0.00010154534,0.9803058,0.000111127054,0.00008149747,0.00001289603,0.0011628906,0.00127196,0.00037016755,0.001734895,0.014594952,0.000094108495],"about_ca_topic_score_codex":0.3025674,"about_ca_topic_score_gemma":0.8569553,"teacher_disagreement_score":0.5543879,"about_ca_system_score_codex":0.0000030145666,"about_ca_system_score_gemma":0.0003744076,"threshold_uncertainty_score":0.99967164},"labels":[],"label_agreement":null},{"id":"W2016302018","doi":"10.1139/e03-077","title":"ReOs and UPb geochronology of the Clear Creek, Dublin Gulch, and Mactung deposits, Tombstone Gold Belt, Yukon, Canada: absolute timing relationships between plutonism and mineralization","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon University; University of Alberta","funders":"University of Alberta","keywords":"Zircon; Geology; Molybdenite; Geochemistry; Skarn; Pluton; Geochronology; Mineralization (soil science); Baddeleyite; Dike; Hydrothermal circulation; Fluid inclusions; Paleontology; Tectonics","score_opus":0.028227968974462298,"score_gpt":0.1893874558997834,"score_spread":0.1611594869253211,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016302018","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99453926,0.0028982854,0.000017010798,0.0016840126,0.00007315416,0.00004688471,0.00001943213,0.0000012634227,0.0007206848],"genre_scores_gemma":[0.998878,0.000077987046,0.0007621345,0.00013364549,0.000028116185,8.145016e-8,0.0000032252403,0.0000010365297,0.000115767594],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998972,0.00013350732,0.00029946523,0.00015575523,0.00018334763,0.00025592677],"domain_scores_gemma":[0.99907935,0.00019129885,0.00020248508,0.00006470587,0.0000779507,0.000384213],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005926477,0.00008400922,0.00019580702,0.00010809069,0.00045236637,0.000077343175,0.00015317148,0.00006277437,0.00021842222],"category_scores_gemma":[0.00037836324,0.000056743083,0.000027181564,0.0003617623,0.00059069885,0.00017496229,0.000009051135,0.00018389913,4.3408622e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000016616248,9.0347794e-7,0.99796396,0.0000056494036,0.000012953091,0.000007010562,0.00008708589,0.0005592091,0.00003693374,0.00024026386,0.00006818677,0.001016185],"study_design_scores_gemma":[0.00010922539,0.000085184045,0.99558806,0.000023268778,0.000039644838,0.000103737526,0.00019652702,0.0010184584,0.000091896756,0.0017713308,0.00089500454,0.0000776333],"about_ca_topic_score_codex":0.6736118,"about_ca_topic_score_gemma":0.99407846,"teacher_disagreement_score":0.32046664,"about_ca_system_score_codex":0.0000028878658,"about_ca_system_score_gemma":0.0005861888,"threshold_uncertainty_score":0.34792823},"labels":[],"label_agreement":null},{"id":"W2016901825","doi":"10.1139/e02-050","title":"Litho- and chronostratigraphic relationships of the SantonianCampanian Milk River Formation in southern Alberta and Eagle Formation in Montana utilising stratigraphy, UPb geochronology, and palynology","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; Royal Tyrrell Museum; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochronology; Outcrop; Sedimentary depositional environment; Cretaceous; Marine transgression; Paleontology; Facies; Lithology; Palynology; Stratigraphy; Conglomerate; Geochemistry; Sedimentary rock; Structural basin","score_opus":0.024164340983286955,"score_gpt":0.1829584004173953,"score_spread":0.15879405943410835,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016901825","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939353,0.003988333,0.0000064601218,0.0012458122,0.000024211677,0.00006359632,0.000011532077,7.816318e-7,0.0007240049],"genre_scores_gemma":[0.9995259,0.0001526654,0.00025784303,0.000045274683,0.000008173726,1.689203e-7,0.000001289952,4.736623e-7,0.000008233041],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991129,0.00013303233,0.00033326366,0.00011219649,0.00009829792,0.00021033366],"domain_scores_gemma":[0.9994426,0.0001472708,0.0001789674,0.000051712206,0.000029970259,0.0001495136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039141785,0.00007624074,0.00015906514,0.00031939967,0.00020991142,0.000046177083,0.00012186962,0.00007015102,0.00025209624],"category_scores_gemma":[0.00013587074,0.00004885695,0.000029177598,0.00053200236,0.00085412397,0.00047388836,0.0000049859163,0.00019480943,0.0000013159198],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000030939655,0.0000027761064,0.9939107,0.0000071341346,0.0000031593381,0.000004862164,0.0023771601,0.0002585132,0.00006803423,0.000085475884,0.000002390241,0.0032767584],"study_design_scores_gemma":[0.0001698773,0.000107493746,0.97643095,0.00004589635,0.000009174363,0.000113988826,0.0023705987,0.014554006,0.00007152211,0.0060416004,0.000025725185,0.00005915427],"about_ca_topic_score_codex":0.071749024,"about_ca_topic_score_gemma":0.9546734,"teacher_disagreement_score":0.8829244,"about_ca_system_score_codex":0.0000013441879,"about_ca_system_score_gemma":0.000039905568,"threshold_uncertainty_score":0.93443227},"labels":[],"label_agreement":null},{"id":"W2017107898","doi":"10.1139/e02-038","title":"Stratigraphy and structure of Pleistocene collapse in the Regina Low, Saskatchewan, Canada","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Evaporite; Devonian; Pleistocene; Paleontology; Cretaceous; Early Pleistocene; Interglacial; Geochemistry; Sedimentary rock","score_opus":0.006679728563406947,"score_gpt":0.17310404090267714,"score_spread":0.1664243123392702,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017107898","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99530905,0.0006351295,8.396483e-7,0.001467815,0.00014097868,0.000049598788,0.000013065172,3.5375848e-7,0.0023831646],"genre_scores_gemma":[0.9994695,0.00002616573,0.00013908683,0.00024217578,0.00002082371,9.838681e-8,1.1043856e-7,0.000001494353,0.00010053721],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99920714,0.000037297,0.00016362075,0.00008751606,0.00029767904,0.00020676697],"domain_scores_gemma":[0.9995447,0.00003344835,0.00012553202,0.000071778704,0.000012038321,0.00021250983],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024910877,0.0000631416,0.000106801286,0.00007265978,0.00015683877,0.000043124965,0.00032170012,0.000033423326,0.0005816993],"category_scores_gemma":[0.00002196209,0.00003588764,0.000022534794,0.00051269267,0.00053175376,0.00013456885,0.0000068193917,0.00014226974,4.353709e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008511796,0.00001308394,0.96499133,0.000012704647,0.0000149128955,0.0003412394,0.004961199,0.0061942595,0.0006669209,0.00020286004,0.017238095,0.005354902],"study_design_scores_gemma":[0.00036854643,0.00032275298,0.97272205,0.000069148075,0.000012778926,0.00036306685,0.0055278684,0.00057998556,0.0003787511,0.000576844,0.018925987,0.00015220347],"about_ca_topic_score_codex":0.6227184,"about_ca_topic_score_gemma":0.9989894,"teacher_disagreement_score":0.37627098,"about_ca_system_score_codex":0.000012903882,"about_ca_system_score_gemma":0.00050988054,"threshold_uncertainty_score":0.6369199},"labels":[],"label_agreement":null},{"id":"W2017238368","doi":"10.1139/e08-052","title":"The Churchill kimberlite field, Nunavut, Canada: petrography, mineral chemistry, and geochronology","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Kimberlite; Geology; Geochemistry; Phlogopite; Geochronology; Chromite; Xenolith; Olivine; Magmatism; Mantle (geology); Paleontology","score_opus":0.008615248932187675,"score_gpt":0.16830572249234985,"score_spread":0.15969047356016217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017238368","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9822959,0.0046900283,0.0000025054778,0.005799719,0.00016612545,0.000020523208,0.000012473847,0.0000018375238,0.007010898],"genre_scores_gemma":[0.9986615,0.00021696997,0.00018598311,0.00054780097,0.00011892939,1.0942819e-7,0.0000021411001,6.017011e-7,0.00026597411],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989345,0.000035489855,0.00023178736,0.00014417268,0.00022046019,0.00043360374],"domain_scores_gemma":[0.9988957,0.00023992977,0.0001128567,0.00007626394,0.00008113912,0.00059411203],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000281027,0.00009460409,0.00015842909,0.000044117285,0.0008436149,0.00006374032,0.00038289218,0.000039472347,0.0021721853],"category_scores_gemma":[0.00021286376,0.000052672352,0.00007089056,0.00033593187,0.001009718,0.000091429545,0.0000067835904,0.00018975913,0.000004012509],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000042890033,0.0000011953334,0.9951744,0.0000015437402,0.00001392557,0.00011273984,0.000030714615,0.00018621764,0.000022039716,0.000023351531,0.0009981976,0.0034313516],"study_design_scores_gemma":[0.00008823738,0.00013726146,0.96016747,0.000005551526,0.000009842984,0.00063691154,0.00012420914,0.0005152503,0.00012128623,0.0011388091,0.036959704,0.00009547677],"about_ca_topic_score_codex":0.812449,"about_ca_topic_score_gemma":0.99700654,"teacher_disagreement_score":0.18455757,"about_ca_system_score_codex":0.0000014841048,"about_ca_system_score_gemma":0.0013295155,"threshold_uncertainty_score":0.99873996},"labels":[],"label_agreement":null},{"id":"W2017468743","doi":"10.1139/e00-100","title":"Search for a deep-mantle component in mafic lavas using a NbYZr plot","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Mafic; Geology; Mantle plume; Basalt; Geochemistry; Flood basalt; Mantle (geology); Partial melting; Tectonics; Lithosphere; Volcanism; Paleontology","score_opus":0.05876120720331392,"score_gpt":0.2421809341491345,"score_spread":0.1834197269458206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017468743","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996002,0.0015079586,0.00023493572,0.00089394406,0.00012540758,0.00006649503,0.000011605455,0.0000019638208,0.0011556939],"genre_scores_gemma":[0.99716485,0.00004382603,0.002453782,0.00021099744,0.00008569629,1.484688e-7,0.000002862116,9.705451e-7,0.00003684629],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99876606,0.000052993728,0.00028222712,0.00015773233,0.00024265714,0.0004983239],"domain_scores_gemma":[0.99910605,0.00014514034,0.00008096126,0.00005658875,0.000088541135,0.00052272336],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008706509,0.00008371042,0.00020210852,0.0003549647,0.000255766,0.000099064506,0.0003496792,0.00003830801,0.0030191245],"category_scores_gemma":[0.000067652996,0.00005754331,0.00010042393,0.00074152084,0.00033645405,0.00018904495,0.000004545204,0.0001344001,0.000026455475],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014390294,0.0000066090133,0.9695572,0.000003001337,0.000006011172,0.00009493987,0.000096398035,0.027491845,0.00016299581,0.000057207304,0.000017056827,0.0024923084],"study_design_scores_gemma":[0.00043944537,0.00043428325,0.908896,0.00005381504,0.000016318225,0.00028555677,0.00062111433,0.076812916,0.00039910988,0.004529468,0.00730364,0.00020833114],"about_ca_topic_score_codex":0.049292788,"about_ca_topic_score_gemma":0.5537127,"teacher_disagreement_score":0.50442,"about_ca_system_score_codex":0.0000026389812,"about_ca_system_score_gemma":0.000374236,"threshold_uncertainty_score":0.99789226},"labels":[],"label_agreement":null},{"id":"W2017486262","doi":"10.1139/e2012-035","title":"A revised stratigraphy and depositional history for the Horseshoe Canyon Formation (Upper Cretaceous), southern Alberta plains","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Geology; Foreland basin; Paleontology; Progradation; Aggradation; Sedimentary depositional environment; Onlap; Diachronous; Canyon; Molasse; Geomorphology; Structural basin; Fluvial","score_opus":0.026517488065085665,"score_gpt":0.20189640489795005,"score_spread":0.17537891683286438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017486262","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96733934,0.023053974,0.0005461904,0.0018661689,0.00050004007,0.00018353171,0.000082693805,0.0000030116148,0.0064250627],"genre_scores_gemma":[0.9983449,0.00007588664,0.0008868527,0.00043954057,0.0001228813,7.767646e-7,0.0000070087203,8.553785e-7,0.00012128431],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992743,0.00003399543,0.00020265637,0.000058280075,0.00015549643,0.00027525215],"domain_scores_gemma":[0.99911386,0.0002736435,0.00014825529,0.000042140928,0.00008565469,0.00033643865],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00065329927,0.000069927446,0.000088163964,0.00013558014,0.0005818327,0.00009991432,0.00017637378,0.000034067558,0.0010625458],"category_scores_gemma":[0.00012564937,0.000039575323,0.000053581884,0.00014282849,0.00031878555,0.0007957283,0.0000015157705,0.0000816903,0.000010508437],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027254166,0.0000069014177,0.97828317,0.000039262937,0.00002467243,0.0000020764264,0.0047999476,0.0013317693,0.0000107933,0.002346049,0.00196619,0.011161941],"study_design_scores_gemma":[0.00023868484,0.0004305337,0.81601334,0.00005508568,0.000048148177,0.00037498318,0.004029203,0.0053105056,0.00002527484,0.0013635454,0.17191489,0.00019580619],"about_ca_topic_score_codex":0.0133656375,"about_ca_topic_score_gemma":0.43264034,"teacher_disagreement_score":0.4192747,"about_ca_system_score_codex":0.000002269383,"about_ca_system_score_gemma":0.00042868647,"threshold_uncertainty_score":0.99985063},"labels":[],"label_agreement":null},{"id":"W2017699297","doi":"10.1139/e04-033","title":"The Late Ordovician Middle Devonian Gaspé Belt in eastern Canada recent advances","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; GDG Environnement; Institut National de la Recherche Scientifique; Geological Survey of Canada","funders":"","keywords":"Devonian; Laurentia; Ordovician; Geology; Paleontology; Margin (machine learning); Architecture; Earth science; Archaeology; Geography","score_opus":0.017333320771698874,"score_gpt":0.1883806945258437,"score_spread":0.1710473737541448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017699297","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97581583,0.009667885,0.0000036326974,0.009527841,0.00038326666,0.00004062362,0.000013153188,0.00000170915,0.004546056],"genre_scores_gemma":[0.9982268,0.00060622627,0.00018112233,0.00082328945,0.000066811386,1.5599552e-7,0.000002244907,7.7904036e-7,0.00009254741],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985012,0.00005354297,0.0003557411,0.0001399168,0.00036682907,0.00058279856],"domain_scores_gemma":[0.998898,0.000110894405,0.00016048332,0.00008416076,0.000101172525,0.0006452384],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00060035073,0.000108001885,0.00017417746,0.00012664494,0.00056147046,0.00013328958,0.00061224727,0.000031143416,0.0012244009],"category_scores_gemma":[0.00021340282,0.000060283226,0.000055169727,0.00086608046,0.00044669618,0.00024396692,0.000005722648,0.00021160429,0.000022052243],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004068662,0.00000249761,0.95715904,0.0000014475348,0.0000055114174,0.000105257146,0.00008029038,0.025936592,0.0000023928617,0.000058874815,0.000012039253,0.016631976],"study_design_scores_gemma":[0.00020638252,0.00017857392,0.8844274,0.000050867275,0.000006469383,0.000053099542,0.0011734659,0.0005051455,0.00006347152,0.011799711,0.10137313,0.00016224604],"about_ca_topic_score_codex":0.91962224,"about_ca_topic_score_gemma":0.99995244,"teacher_disagreement_score":0.10136109,"about_ca_system_score_codex":0.000008872211,"about_ca_system_score_gemma":0.0029267974,"threshold_uncertainty_score":0.9996886},"labels":[],"label_agreement":null},{"id":"W2018127628","doi":"10.1139/e00-046","title":"Modes of extinction, pseudo-extinction and distribution in Middle Jurassic ammonites: terminology","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Marine Biology and Ecology Research","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Extinction event; Extinction (optical mineralogy); Taxon; Paleontology; Range (aeronautics); Lineage (genetic); Diachronous; Origination; Geology; Clade; Phylogenetic tree; Geography; Biology; Population; Biological dispersal; Structural basin","score_opus":0.03927692167113664,"score_gpt":0.24149880416717076,"score_spread":0.20222188249603412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018127628","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99685925,0.00057847885,0.000018812363,0.00047112358,0.0002161851,0.000045238932,0.000009888851,0.0000016119101,0.0017994118],"genre_scores_gemma":[0.99955326,0.0001580396,0.000087076136,0.000035301542,0.00005179352,2.141064e-7,0.0000073504525,6.3006604e-7,0.000106340776],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909335,0.00010641561,0.00026633855,0.00012453606,0.00009670199,0.00031266554],"domain_scores_gemma":[0.9993823,0.00013163194,0.00013940467,0.00004958288,0.000079103615,0.00021797576],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00093533215,0.000063100924,0.0001508686,0.00033321773,0.00022538895,0.000028198563,0.00017125637,0.000082639235,0.0010580844],"category_scores_gemma":[0.00020618983,0.00004901366,0.00002578517,0.00039117163,0.0008175728,0.000291523,0.0000048542497,0.00016330414,0.000009190118],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021802272,0.0000041492913,0.98737454,0.0000037789277,0.0000036252216,0.00003465273,0.000053149863,0.00036922534,0.000026824246,0.000037018523,0.000022237477,0.012048975],"study_design_scores_gemma":[0.00015438622,0.00040199494,0.99371946,0.000014359233,0.0000036075985,0.00038875366,0.00031635474,0.0023622578,0.00005269911,0.0007722993,0.0017633623,0.000050465766],"about_ca_topic_score_codex":0.008563619,"about_ca_topic_score_gemma":0.52402383,"teacher_disagreement_score":0.51546025,"about_ca_system_score_codex":0.0000026753203,"about_ca_system_score_gemma":0.0005125624,"threshold_uncertainty_score":0.9998551},"labels":[],"label_agreement":null},{"id":"W2018348481","doi":"10.1139/e00-066","title":"Lift-off moraines: markers of last ice-flow directions on the Scotian Shelf","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"","keywords":"Geology; Moraine; Ice stream; Structural basin; Ice shelf; Geomorphology; Emerald; Ice sheet; Paleontology; Oceanography; Glacier; Sea ice; Cryosphere","score_opus":0.02090051055805405,"score_gpt":0.2258667226259383,"score_spread":0.20496621206788423,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018348481","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93257326,0.0012023883,0.0000010374536,0.0046025873,0.00046698216,0.00006925537,0.000027053566,0.0000028190561,0.06105463],"genre_scores_gemma":[0.99818206,0.00018349674,0.00018893256,0.00042640345,0.00007914298,2.2236374e-7,0.0000017826434,0.0000013169042,0.0009366629],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986313,0.00023790712,0.0002662144,0.00014118156,0.0002807559,0.00044263125],"domain_scores_gemma":[0.99872464,0.0005217209,0.0001105468,0.00012974808,0.00008986897,0.00042347508],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014380037,0.00009389208,0.00017484665,0.00032612565,0.0007326368,0.00006594648,0.00057555194,0.00006614192,0.019293802],"category_scores_gemma":[0.0002480931,0.00005709253,0.00008670026,0.0006896484,0.0016733721,0.00019843361,0.0000023441942,0.0003047854,0.00025617602],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019520425,0.000004235796,0.9896353,0.000002711774,0.000015361818,0.000042662337,0.00020562713,0.004702566,5.9291335e-7,0.000081537575,0.00060242147,0.0046874946],"study_design_scores_gemma":[0.000114633454,0.00053684245,0.97574526,0.000051566647,0.00000926913,0.00026608704,0.0005441535,0.001647115,0.000018587974,0.00047417867,0.020511214,0.00008110783],"about_ca_topic_score_codex":0.003661084,"about_ca_topic_score_gemma":0.56206703,"teacher_disagreement_score":0.55840594,"about_ca_system_score_codex":4.5090408e-7,"about_ca_system_score_gemma":0.0010533904,"threshold_uncertainty_score":0.98160267},"labels":[],"label_agreement":null},{"id":"W2018642377","doi":"10.1139/e05-068","title":"Crustal development at the pre-Grenvillian Laurentian margin: a record from contrasting geochemistry of mafic and ultramafic orthogneisses in the Chochocouane River area, Quebec","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Medicago (Canada); Geological Survey of Canada; Natural Resources Canada; Institut National de la Recherche Scientifique","funders":"","keywords":"Geology; Geochemistry; Archean; Mafic; Proterozoic; Metamorphism; Ultramafic rock; Granulite; Felsic; Petrology; Continental crust; Crust; Paleontology; Facies; Tectonics","score_opus":0.013268284773236876,"score_gpt":0.18498488895908033,"score_spread":0.17171660418584345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018642377","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938709,0.0029052768,0.000006936662,0.0021749055,0.000057777987,0.000065943954,0.000041057425,0.0000015237503,0.0008756738],"genre_scores_gemma":[0.9987112,0.00004717571,0.0006952254,0.0002746318,0.000074086136,4.4101816e-7,0.000015558202,9.1819896e-7,0.00018071516],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986535,0.00007576558,0.000404896,0.00019203352,0.00031138305,0.00036242072],"domain_scores_gemma":[0.99899143,0.00033454038,0.00023631776,0.000094655436,0.00006106714,0.00028200174],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007111972,0.00012444693,0.00021195205,0.000095743926,0.00035570643,0.000108880806,0.00047589475,0.000051003422,0.007224585],"category_scores_gemma":[0.00017178056,0.00006278521,0.000069758484,0.00039643375,0.0009065679,0.00016604346,0.000009826149,0.00021378789,0.00000869529],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012209075,0.000006990159,0.97460264,0.000004483715,0.000016922853,0.00002680768,0.0010044817,0.00096559146,0.00012593636,0.0000024990352,0.0001160143,0.023115447],"study_design_scores_gemma":[0.00015227779,0.000049091388,0.98847157,0.00005674468,0.000021233373,0.00005470242,0.0011747694,0.00074869965,0.00049847923,0.00028191393,0.008387398,0.00010312478],"about_ca_topic_score_codex":0.1120488,"about_ca_topic_score_gemma":0.9632533,"teacher_disagreement_score":0.8512045,"about_ca_system_score_codex":0.0000043056752,"about_ca_system_score_gemma":0.00045040232,"threshold_uncertainty_score":0.9936829},"labels":[],"label_agreement":null},{"id":"W2018726985","doi":"10.1139/e06-004","title":"New, biostratigraphically significant ammonites from the Jurassic Fernie Formation, southern Canadian Rocky Mountains","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Paleontology; Ammonite; Outcrop; Terrane; Fauna; Cretaceous; Ecology; Tectonics","score_opus":0.014603341822159967,"score_gpt":0.1920343613819597,"score_spread":0.17743101955979973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018726985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9654591,0.005982304,0.00018778697,0.005947826,0.00046251097,0.00011377323,0.00046160806,0.000007961538,0.021377135],"genre_scores_gemma":[0.99823767,0.000018420653,0.0010368151,0.00030603426,0.00032454566,2.0125174e-7,0.000011990387,0.0000010990083,0.00006322166],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982461,0.00012113409,0.00045399918,0.00018463674,0.00035460666,0.0006395756],"domain_scores_gemma":[0.998178,0.00025019527,0.0002632186,0.00014069534,0.00011856947,0.0010492956],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0006455551,0.00016699625,0.00019508749,0.00038884158,0.0013302739,0.0004664415,0.0008388749,0.00010652979,0.00084989896],"category_scores_gemma":[0.000079241654,0.00010600255,0.00012973062,0.00066830567,0.0007164263,0.0005871399,6.801892e-7,0.00029593083,0.00004157149],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004900128,0.0000016068674,0.98785365,8.386446e-7,0.0000139492095,0.00006826146,0.00033731543,0.00035025913,0.000029227826,0.0003644038,0.0015521364,0.009423428],"study_design_scores_gemma":[0.00013183353,0.00013678604,0.9871586,0.00002388702,0.00001901064,0.00006136105,0.0010229411,0.0002970471,0.000055673143,0.0065797414,0.0043628775,0.00015025727],"about_ca_topic_score_codex":0.92323554,"about_ca_topic_score_gemma":0.9993734,"teacher_disagreement_score":0.076137826,"about_ca_system_score_codex":0.0000032678147,"about_ca_system_score_gemma":0.0046290364,"threshold_uncertainty_score":0.99996984},"labels":[],"label_agreement":null},{"id":"W2018799841","doi":"10.1139/e06-107","title":"Tectonic evolution of the Yaoundé segment of the Neoproterozoic Central African Orogenic Belt in southern Cameroon","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":128,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Nappe; Metamorphism; Overprinting; Tectonic phase; Geochemistry; Fold (higher-order function); Granulite; Tectonics; Doming; Outcrop; Orogeny; Metamorphic rock; Paleontology; Seismology; Facies; Structural basin","score_opus":0.009810882240218977,"score_gpt":0.1762153567007281,"score_spread":0.16640447446050913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018799841","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99726,0.0009802554,0.000014085496,0.00069821946,0.000180707,0.00007624891,0.000019382409,7.6875665e-7,0.000770373],"genre_scores_gemma":[0.99976194,0.0000042861616,0.00008347448,0.00006546533,0.000034006767,7.465886e-8,3.655861e-7,6.527348e-7,0.00004970629],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861574,0.00008372375,0.00039602866,0.000111765934,0.0003866487,0.00040610103],"domain_scores_gemma":[0.99918646,0.00006983094,0.00032219721,0.0001139747,0.00007549036,0.00023205871],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00096720125,0.00007774512,0.00017041939,0.00014515356,0.0001789918,0.000019068264,0.0006492849,0.00003978598,0.0009591187],"category_scores_gemma":[0.0001454507,0.00003668259,0.00016553012,0.0012019386,0.00081551145,0.000078043035,0.00001137062,0.00018006342,0.0000037488437],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000065449894,0.00000567038,0.99367493,0.000003161508,0.000007878224,0.0000028974814,0.00039649996,0.0036189135,0.00058399857,0.000029903913,0.0000027065144,0.0016669033],"study_design_scores_gemma":[0.00009247223,0.00010846902,0.9939128,0.000036519097,0.000015621326,0.000019425861,0.0017624068,0.0003413454,0.0016454477,0.0019126195,0.00010175172,0.000051077648],"about_ca_topic_score_codex":0.14304394,"about_ca_topic_score_gemma":0.8881746,"teacher_disagreement_score":0.74513066,"about_ca_system_score_codex":0.000008389553,"about_ca_system_score_gemma":0.0007151803,"threshold_uncertainty_score":0.99995416},"labels":[],"label_agreement":null},{"id":"W2018807865","doi":"10.1139/e06-121","title":"Climate warming and active layer thaw in the boreal and tundra environments of the Mackenzie Valley","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; McMaster University","funders":"","keywords":"Permafrost; Tundra; Active layer; Taiga; Environmental science; Boreal; Climate change; Soil water; Peat; Atmospheric sciences; Hydrology (agriculture); Geology; Soil science; Climatology; Arctic; Ecology; Oceanography; Geotechnical engineering; Layer (electronics)","score_opus":0.039162239370908125,"score_gpt":0.23985655946405843,"score_spread":0.2006943200931503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018807865","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99460936,0.0009569255,8.9459394e-7,0.0006108128,0.00014792861,0.000058396377,0.0002072752,3.042866e-7,0.0034081228],"genre_scores_gemma":[0.99922967,0.00033966373,0.000036593603,0.00033411762,0.00004759534,4.74636e-8,0.0000034766442,8.974119e-7,0.000007915198],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99921554,0.00004521009,0.00017828481,0.00008581542,0.00018688601,0.0002882653],"domain_scores_gemma":[0.999481,0.00016037264,0.00011894816,0.00005895005,0.000010571067,0.0001701113],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001259431,0.00006402877,0.00009773051,0.00011320527,0.00028167723,0.0000660455,0.0002453592,0.000027279684,0.00025250713],"category_scores_gemma":[0.000027476972,0.00003354174,0.000025263567,0.00019610883,0.0006012955,0.00019244621,0.0000078839275,0.00012582574,0.0000012356711],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007766148,0.000001438016,0.993481,0.0000032766482,0.0000022370207,0.000021228157,0.0026807848,0.000018604504,0.000063171734,0.000034549175,0.000017668006,0.003668266],"study_design_scores_gemma":[0.00010805574,0.00009062137,0.99257106,0.000034049765,0.000006036413,0.00012882547,0.005147999,0.00011055296,0.00018167641,0.00016415042,0.0014121203,0.000044863275],"about_ca_topic_score_codex":0.029728068,"about_ca_topic_score_gemma":0.81755966,"teacher_disagreement_score":0.7878316,"about_ca_system_score_codex":0.0000010595913,"about_ca_system_score_gemma":0.00010916872,"threshold_uncertainty_score":0.976733},"labels":[],"label_agreement":null},{"id":"W2019065408","doi":"10.1139/e06-080","title":"Thermobarometry and geochronology of the Uvauk complex, a polymetamorphic Neoarchean and Paleoproterozoic segment of the Snowbird tectonic zone, Nunavut, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Institute for Circumpolar Health Research","funders":"","keywords":"Geology; Metamorphism; Granulite; Geochemistry; Gabbro; Geothermobarometry; Zircon; Anorthosite; Geochronology; Metamorphic facies; Petrology; Orogeny; Shear zone; Hornblende; Facies; Tectonics; Plagioclase; Igneous rock; Geomorphology; Paleontology; Quartz; Structural basin","score_opus":0.01466533639203107,"score_gpt":0.1860313286434673,"score_spread":0.17136599225143623,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019065408","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99402714,0.0029259273,0.00000879059,0.002203697,0.00012789066,0.00007384945,0.00002950572,7.680431e-7,0.00060240517],"genre_scores_gemma":[0.99939877,0.000024887615,0.00017256255,0.0003423175,0.00002647217,7.918455e-8,4.496984e-7,8.416534e-7,0.000033637174],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987202,0.000095944124,0.00035795814,0.00014183248,0.00032675767,0.0003572983],"domain_scores_gemma":[0.9989899,0.00018585281,0.00029870725,0.00012549684,0.000070734415,0.00032932239],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008527648,0.000100200996,0.00024728486,0.0001283015,0.0002951704,0.000023047522,0.0005098663,0.000042556665,0.0010745345],"category_scores_gemma":[0.00012939691,0.00004749592,0.00007770928,0.0007005355,0.0018400697,0.000059395625,0.000024633435,0.00019336242,4.5780442e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005704961,0.0000029347345,0.9926884,0.000008847994,0.000020819392,0.000008410674,0.00007174334,0.00014479892,0.00088564894,0.00003620802,0.000010996185,0.0061154533],"study_design_scores_gemma":[0.00011759766,0.00014380008,0.9959373,0.000026721536,0.00002526996,0.000126843,0.00034133543,0.0002517613,0.0017251896,0.0009823665,0.0002596102,0.000062197156],"about_ca_topic_score_codex":0.7255008,"about_ca_topic_score_gemma":0.996187,"teacher_disagreement_score":0.27068615,"about_ca_system_score_codex":0.0000030827832,"about_ca_system_score_gemma":0.0010334259,"threshold_uncertainty_score":0.9998386},"labels":[],"label_agreement":null},{"id":"W2019206381","doi":"10.1139/e06-043","title":"New material of<i>Procolophon</i>(Parareptilia: Procolophonoidea) from the Lower Triassic of Brazil, with remarks on the ages of the Sanga do Cabral and Buena Vista formations of South America","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Cape Breton University","funders":"Conselho Nacional de Desenvolvimento Científico e Tecnológico","keywords":"Postcrania; Permian; Geology; Paleontology; Tetrapod (structure); Genus; Skull; Early Triassic; Structural basin; Biology; Zoology; Taxon","score_opus":0.008177265430818516,"score_gpt":0.18741199447991314,"score_spread":0.17923472904909463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019206381","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957747,0.0006783238,0.000015299598,0.0013532569,0.00025695466,0.00020288995,0.00032803408,9.600582e-7,0.0013895648],"genre_scores_gemma":[0.9992961,0.0000126227815,0.0004705455,0.000115822906,0.00006140251,5.774669e-7,0.000004201282,0.0000010072085,0.000037698148],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989142,0.00017280213,0.00040104298,0.00010512982,0.000207627,0.00019923487],"domain_scores_gemma":[0.99862254,0.00037529194,0.0006768542,0.00013726842,0.00009461864,0.00009340796],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005002462,0.00009052484,0.00023981988,0.00008724881,0.00029268232,0.000021906846,0.00047907795,0.00005473046,0.00044446855],"category_scores_gemma":[0.000115087525,0.000038839997,0.00006432305,0.00039651504,0.0020344395,0.00015063639,0.000007235015,0.00012690385,0.0000011443984],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002597701,0.000010807554,0.99454576,0.00000817356,0.000033818746,0.0000038249614,0.0009870088,0.0011079,0.00043193286,0.00018597337,0.0013937309,0.0010313164],"study_design_scores_gemma":[0.00023500074,0.00069998216,0.99589753,0.00006745946,0.00002582437,0.000028866509,0.00081560767,0.00006734195,0.00070178387,0.00059927674,0.0008110837,0.000050245915],"about_ca_topic_score_codex":0.028546656,"about_ca_topic_score_gemma":0.23618771,"teacher_disagreement_score":0.20764105,"about_ca_system_score_codex":0.0000015641591,"about_ca_system_score_gemma":0.0011892425,"threshold_uncertainty_score":0.9779223},"labels":[],"label_agreement":null},{"id":"W2019239202","doi":"10.1139/e05-097","title":"Late Permian (Changhsingian) conodont biozonation and the basal boundary, Ganxi section, western Hubei Province, south China","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Conodont; Geology; Permian; Paleontology; Section (typography); China; Stage (stratigraphy); Global Boundary Stratotype Section and Point; Biostratigraphy; Geography; Archaeology; Structural basin","score_opus":0.009941622512467375,"score_gpt":0.19078671440364894,"score_spread":0.18084509189118156,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019239202","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9756963,0.0049366583,0.0000680567,0.0023855995,0.0007280207,0.00010270141,0.000030243133,0.0000053256313,0.016047064],"genre_scores_gemma":[0.9991586,0.000020085354,0.00018000134,0.00014460932,0.0002954436,1.7220218e-7,0.0000016571382,7.737478e-7,0.00019860722],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99888116,0.00012664276,0.0002769784,0.00016017821,0.0002184035,0.0003366595],"domain_scores_gemma":[0.9993014,0.000069860136,0.00023423792,0.00006866119,0.000063603606,0.00026226757],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011273692,0.0001117129,0.00017244228,0.00027823416,0.0011663714,0.0004078955,0.0002624475,0.00006473511,0.000111959285],"category_scores_gemma":[0.000043529326,0.000069842856,0.00006776422,0.00026633652,0.0019415246,0.0005214741,9.842618e-7,0.00019838219,0.0000040809346],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019076715,0.0000018765993,0.9932661,0.0000033498054,0.00000900248,0.00003146769,0.000753747,0.00021837365,0.0000044556473,0.00023050388,0.00007061888,0.005391404],"study_design_scores_gemma":[0.0003932054,0.00018464072,0.99440086,0.000021697739,0.000013955711,0.00018533814,0.00021708827,0.00080374355,0.000014356319,0.0019879772,0.0016796048,0.00009754286],"about_ca_topic_score_codex":0.038410746,"about_ca_topic_score_gemma":0.8434848,"teacher_disagreement_score":0.8050741,"about_ca_system_score_codex":0.0000014670602,"about_ca_system_score_gemma":0.001046588,"threshold_uncertainty_score":0.96799254},"labels":[],"label_agreement":null},{"id":"W2019247266","doi":"10.1139/e02-093","title":"Tectonometamorphic evolution of the Acatlan Complex eclogites (southern Mexico)","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Epidote; Geochemistry; Eclogite; Greenschist; Amphibole; Metamorphic facies; Metamorphism; Plagioclase; Pyroxene; Mafic; Petrology; Facies; Quartz; Olivine; Chlorite; Geomorphology; Paleontology; Subduction","score_opus":0.027579287299273253,"score_gpt":0.18736631649170207,"score_spread":0.15978702919242882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019247266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893847,0.0011156735,0.000030273504,0.00091042416,0.000147022,0.00003599885,0.000027724527,0.0000017399876,0.008346439],"genre_scores_gemma":[0.9992311,0.000005143145,0.0005073155,0.00014509946,0.000029701458,5.7276115e-8,9.824089e-7,6.0893314e-7,0.00008001793],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99892,0.00012397584,0.00029251343,0.00011585292,0.0002628045,0.00028480645],"domain_scores_gemma":[0.9991398,0.00010387107,0.0002429441,0.00009697755,0.00010755628,0.00030885614],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007606591,0.000080826256,0.0001835724,0.00016165106,0.0003021062,0.000044903343,0.0005140154,0.0000374693,0.011136087],"category_scores_gemma":[0.00045359752,0.00004117585,0.00015632872,0.00089860166,0.0008559649,0.00010917161,0.0000040118475,0.00013641921,0.000040054132],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000013555081,0.0000028050845,0.9958755,0.0000015921136,0.000009804627,0.0000019625984,0.00004999378,0.0030017619,0.0002385311,0.00042530394,0.000029950503,0.0003614637],"study_design_scores_gemma":[0.00007507197,0.000111293215,0.9768739,0.000012097342,0.000020711019,0.000036378515,0.0004814739,0.00047455105,0.0006744247,0.018488565,0.0026775787,0.000073983756],"about_ca_topic_score_codex":0.02170164,"about_ca_topic_score_gemma":0.30277854,"teacher_disagreement_score":0.2810769,"about_ca_system_score_codex":0.0000018214022,"about_ca_system_score_gemma":0.00056365377,"threshold_uncertainty_score":0.98976785},"labels":[],"label_agreement":null},{"id":"W2019389498","doi":"10.1139/e00-006","title":"Isotopic evidence for the sources of Cretaceous and Tertiary granitic rocks, east-central Alaska: implications for the tectonic evolution of the Yukon-Tanana Terrane","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Flysch; Terrane; Geochemistry; Pluton; Mafic; Paleozoic; Cretaceous; Radiogenic nuclide; Crust; Sedimentary rock; Petrology; Mantle (geology); Tectonics; Paleontology","score_opus":0.02674723419589537,"score_gpt":0.21475895015063562,"score_spread":0.18801171595474025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019389498","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97107434,0.017589377,0.00029702505,0.010578434,0.000086887834,0.00023355153,0.00006037842,0.0000012829798,0.00007869263],"genre_scores_gemma":[0.9993992,0.0001843331,0.00010592038,0.0001678531,0.00006298512,0.00000185318,5.984707e-7,8.282556e-7,0.00007647293],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910986,0.000045939247,0.00028441544,0.000118660144,0.00015492161,0.00028622136],"domain_scores_gemma":[0.9986027,0.00082928373,0.00018381546,0.00012427298,0.000106631895,0.00015333605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005011463,0.00007622278,0.00014587653,0.00005462133,0.0006800443,0.000048182377,0.000596419,0.00002930536,0.00057281886],"category_scores_gemma":[0.00031145406,0.000031758398,0.00015726978,0.0003539714,0.0009941562,0.00013228976,0.0000049507094,0.000087525856,8.0127256e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001446145,0.0000039784604,0.9730285,0.000012920999,0.000030120644,3.1585697e-7,0.00021095319,0.008493498,0.00007649106,0.000052482614,0.000049713748,0.018026607],"study_design_scores_gemma":[0.00009735682,0.00016206442,0.98683465,0.00004624286,0.00010702165,0.000043009317,0.00030580384,0.0066259825,0.00011588924,0.004724697,0.00088848284,0.000048828584],"about_ca_topic_score_codex":0.01142216,"about_ca_topic_score_gemma":0.1777941,"teacher_disagreement_score":0.16637194,"about_ca_system_score_codex":0.0000021877763,"about_ca_system_score_gemma":0.00038333473,"threshold_uncertainty_score":0.9951609},"labels":[],"label_agreement":null},{"id":"W2019431122","doi":"10.1139/e04-001","title":"Regional unconformities and the sedimentary architecture of the Oak Ridges Moraine area, southern Ontario","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Unconformity; Meltwater; Geomorphology; Moraine; Sedimentary depositional environment; Bedrock; Sedimentary rock; Quaternary; Paleontology; Facies; Stratigraphy; Onlap; Glacial period; Structural basin; Tectonics","score_opus":0.020209835957443245,"score_gpt":0.1979927177318217,"score_spread":0.17778288177437845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019431122","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9797876,0.0016948509,0.0000026499356,0.015318996,0.00022133734,0.000076045384,0.000025481262,9.279079e-7,0.0028721427],"genre_scores_gemma":[0.9983821,0.000019500669,0.00015734856,0.0010039709,0.000041628595,1.5209451e-7,0.0000017737051,7.0049526e-7,0.00039280474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99907076,0.00009990352,0.0002030799,0.00008983805,0.00025539193,0.00028102082],"domain_scores_gemma":[0.9992723,0.00022602984,0.00015083584,0.00009057783,0.000063635445,0.00019661404],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0010180277,0.000078783145,0.00016077887,0.00013124006,0.00059357897,0.00004166551,0.00048553682,0.000046147135,0.0006700649],"category_scores_gemma":[0.00007093923,0.000035839224,0.000071665614,0.00019579554,0.0044153146,0.00011047396,0.000008453627,0.00032659876,0.0000060265897],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000275952,0.0000012321352,0.99195564,0.000002815369,0.000017131684,0.000015244129,0.0036039134,0.0038267667,6.8637394e-7,0.00035967183,0.000046367903,0.00014292519],"study_design_scores_gemma":[0.0005930969,0.0001597336,0.98010546,0.000044375185,0.000014834344,0.000955571,0.0028818126,0.000034434062,0.000028959987,0.012954509,0.0021683509,0.000058856825],"about_ca_topic_score_codex":0.26109362,"about_ca_topic_score_gemma":0.9849148,"teacher_disagreement_score":0.72382116,"about_ca_system_score_codex":8.270456e-7,"about_ca_system_score_gemma":0.0023002294,"threshold_uncertainty_score":0.9982941},"labels":[],"label_agreement":null},{"id":"W2019755917","doi":"10.1139/e05-008","title":"A new description of the skull of<i>Dyrosaurus phosphaticus</i>(Thomas, 1893) (Mesoeucrocodylia: Dyrosauridae) from the Lower Eocene of North Africa","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Stony Brook University; Koninklijk Belgisch Instituut voor Natuurwetenschappen; Fondation des Treilles; American Museum of Natural History","keywords":"Skull; Foramen; Taxonomy (biology); Anatomy; Biology; Phylogenetic tree; Dorsum; Coronoid process; Genus; Paleontology; Zoology; Evolutionary biology","score_opus":0.02025629123047585,"score_gpt":0.1888556594581983,"score_spread":0.16859936822772245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019755917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9832651,0.011222466,0.000079523576,0.00213227,0.00081748836,0.00009598456,0.00018849928,0.0000017936345,0.0021968798],"genre_scores_gemma":[0.9972509,0.00010741795,0.002062064,0.00022767855,0.00018807716,1.3004502e-7,0.0000037754153,0.000001373669,0.00015856992],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99847746,0.000163646,0.00054724567,0.00015014237,0.00031320323,0.0003483118],"domain_scores_gemma":[0.9985203,0.0002669144,0.000612476,0.00018392508,0.00014355769,0.00027279698],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006411908,0.00011852929,0.00028200413,0.00011350835,0.00030764917,0.000019935938,0.00088794826,0.00007806761,0.00087656174],"category_scores_gemma":[0.00018941044,0.00006500133,0.00014985922,0.00059551356,0.0013896266,0.00033516952,0.0000095084315,0.00019349832,0.000010737009],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003637883,0.000010545035,0.9890221,0.0000029749253,0.000025112075,0.000005854687,0.0005690939,0.0020960092,0.00010703857,0.00008334747,0.002568034,0.0054735495],"study_design_scores_gemma":[0.00020045048,0.0003151225,0.9795613,0.000047390426,0.000033265598,0.00004750819,0.00013777125,0.00029049665,0.00038850753,0.0005484553,0.018356536,0.00007318959],"about_ca_topic_score_codex":0.031441867,"about_ca_topic_score_gemma":0.6990325,"teacher_disagreement_score":0.6675906,"about_ca_system_score_codex":0.0000032210264,"about_ca_system_score_gemma":0.0018891873,"threshold_uncertainty_score":0.97500783},"labels":[],"label_agreement":null},{"id":"W2019785835","doi":"10.1139/e01-035","title":"Holocene paleoclimate and paleoecology determined from fossil Coleoptera at Brampton, Ontario, Canada","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Waterloo","funders":"","keywords":"Younger Dryas; Boreal; Paleoclimatology; Holocene; Geology; Paleoecology; Taiga; Fossil wood; Temperate climate; Paleontology; Ecological succession; Palynology; Glacial period; Ecology; Physical geography; Climate change; Oceanography; Geography; Pollen; Biology","score_opus":0.018895165968469553,"score_gpt":0.21426116640926557,"score_spread":0.19536600044079602,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019785835","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98859966,0.0030728276,0.0000015587387,0.0012884921,0.0007672458,0.00007347524,0.000035318106,0.0000031350512,0.006158308],"genre_scores_gemma":[0.99826205,0.00013832239,0.00031541006,0.00063609844,0.000070998634,3.2213717e-7,0.000007935254,0.0000016273578,0.00056723226],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998171,0.00015118012,0.00036274915,0.0002710445,0.00026181067,0.0007822331],"domain_scores_gemma":[0.99814075,0.00044236265,0.00019541988,0.00012449274,0.00010669782,0.000990301],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00064822845,0.00015386994,0.00032249154,0.00023283766,0.0008481504,0.00009429592,0.00042699263,0.00012170139,0.009966102],"category_scores_gemma":[0.00013269809,0.00012404245,0.000044972017,0.00025228635,0.0010725257,0.00024516587,0.000013147709,0.0003092377,0.00003998671],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034034994,0.0000016960047,0.9970414,0.0000022459963,0.000016990529,0.0013420774,0.00020331194,0.00013939364,0.0000013812321,0.000005307604,0.00022713131,0.0009850414],"study_design_scores_gemma":[0.00036858974,0.00026865638,0.9892707,0.000018266219,0.000013704492,0.0016432407,0.00012038871,0.00016203847,0.000017527715,0.00025624217,0.007718949,0.00014170149],"about_ca_topic_score_codex":0.9691158,"about_ca_topic_score_gemma":0.99999446,"teacher_disagreement_score":0.03087864,"about_ca_system_score_codex":0.0000040009477,"about_ca_system_score_gemma":0.0050413418,"threshold_uncertainty_score":0.9909389},"labels":[],"label_agreement":null},{"id":"W2020028185","doi":"10.1139/e08-041","title":"Proterozoic anorthosite–granite Nain batholith: structure and intrusion processes in an active lithosphere-scale fault zone, northern Labrador","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"BP (Canada)","funders":"","keywords":"Batholith; Geology; Anorthosite; Massif; Pluton; Geochemistry; Transtension; Quartz monzonite; Magmatism; Fibrous joint; Proterozoic; Mafic; Shear zone; Lithosphere; Fault (geology); Petrology; Sinistral and dextral; Paleontology; Tectonics; Plagioclase","score_opus":0.011173641292109437,"score_gpt":0.19112481064158426,"score_spread":0.17995116934947483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020028185","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980731,0.0011144169,0.000013645854,0.00035932122,0.0000664915,0.00010146564,0.00006759907,0.0000046112555,0.00019937017],"genre_scores_gemma":[0.9978549,0.00005836556,0.0017655493,0.00018773894,0.00008079387,3.5317257e-7,0.000009799538,0.0000018041551,0.000040690105],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985983,0.00009585266,0.00030918044,0.0002753846,0.00030046492,0.0004208445],"domain_scores_gemma":[0.9987801,0.000071607676,0.00017719284,0.00008187003,0.00020176124,0.00068746717],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00027333028,0.00015349459,0.00026852445,0.00023041577,0.00044613375,0.00010905379,0.00034045576,0.00008067022,0.0013355601],"category_scores_gemma":[0.00015929225,0.00009985785,0.000045430443,0.001047271,0.00070545095,0.00068459316,0.000008115597,0.0002738438,0.000006587023],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002070703,0.000007979387,0.9857261,0.0000107022115,0.000004349853,0.00013668225,0.0016345929,0.0012537974,0.00013463332,0.0000012769494,0.0000020099708,0.011067122],"study_design_scores_gemma":[0.00017243781,0.0004129409,0.9957208,0.000041153053,0.000009248457,0.0002597961,0.0006278022,0.00081350055,0.00059611443,0.0008722683,0.00031863002,0.00015531652],"about_ca_topic_score_codex":0.04268885,"about_ca_topic_score_gemma":0.9504308,"teacher_disagreement_score":0.9077419,"about_ca_system_score_codex":0.0000024440465,"about_ca_system_score_gemma":0.0006477884,"threshold_uncertainty_score":0.99957734},"labels":[],"label_agreement":null},{"id":"W2020266489","doi":"10.1139/e10-110","title":"A catalogue of late Cenozoic tephra beds in the Klondike goldfields and adjacent areas, Yukon Territory<sup>1</sup>Yukon Geological Survey Contribution 010.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey","keywords":"Tephra; Geology; Rhyolite; Volcano; Cenozoic; Geochemistry; Tephrochronology; Trace element; Volcanic arc; Paleontology; Volcanic rock; Structural basin; Subduction; Tectonics","score_opus":0.0296089007964152,"score_gpt":0.19488161472881038,"score_spread":0.16527271393239518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020266489","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966451,0.0014553784,0.000009130583,0.0006084202,0.000086827444,0.000080065125,0.00011017474,0.0000021935077,0.0010027128],"genre_scores_gemma":[0.9993661,0.000086052096,0.0001147673,0.0003328275,0.000046973964,3.401798e-7,0.000035105437,7.810927e-7,0.000017073195],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99827635,0.00032321122,0.0004328002,0.00020502903,0.00030588315,0.0004567416],"domain_scores_gemma":[0.9988502,0.00029472317,0.0002075629,0.00010666324,0.000121341356,0.00041948314],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0021648337,0.00013182031,0.00030633455,0.00022216694,0.00020623901,0.00006076417,0.00052513694,0.00011173386,0.0013734921],"category_scores_gemma":[0.00046029844,0.00007206694,0.000086877604,0.00057609857,0.00090033107,0.0002178686,0.0000116728725,0.00030109892,0.000012332749],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002320761,0.000014997666,0.99764395,0.0000033596134,0.000010140437,0.00006177725,0.0004714267,0.0007590393,0.000005502257,0.00005878382,0.000059119622,0.0008887119],"study_design_scores_gemma":[0.00018197508,0.00047441517,0.99364674,0.00002482848,0.000018820034,0.000068959744,0.00032978677,0.0017988995,0.00005800364,0.0027780023,0.0005160838,0.00010350212],"about_ca_topic_score_codex":0.18226948,"about_ca_topic_score_gemma":0.6750918,"teacher_disagreement_score":0.4928223,"about_ca_system_score_codex":0.0000022624665,"about_ca_system_score_gemma":0.00025641223,"threshold_uncertainty_score":0.9995394},"labels":[],"label_agreement":null},{"id":"W2020333229","doi":"10.1139/e09-036","title":"A new tomistomine (Crocodylia) from the Miocene of Taiwan","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Canadian Museum of Nature","funders":"","keywords":"Paleontology; Geology; Skull; Taxon; Anatomy; Vertebrate; Biology","score_opus":0.019416703054291586,"score_gpt":0.2118779692466588,"score_spread":0.19246126619236723,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020333229","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9744951,0.008212977,0.00009600683,0.008379095,0.0005509112,0.000047012603,0.000052339685,0.000002146486,0.008164396],"genre_scores_gemma":[0.9968328,0.000028403416,0.0020451297,0.00073180196,0.0002315917,1.8855326e-8,0.0000035101325,3.9666668e-7,0.00012635603],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991666,0.00007189889,0.00025123262,0.00010423324,0.00013632186,0.00026969664],"domain_scores_gemma":[0.99915993,0.00013514012,0.00018840795,0.00008502056,0.00005741561,0.00037408227],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046712527,0.00007030517,0.00016002225,0.00010471629,0.00026965086,0.0000235309,0.00053641776,0.0000550014,0.0020414565],"category_scores_gemma":[0.00013447246,0.00004228946,0.00006319814,0.0002803823,0.0005379662,0.00018212717,0.0000014464247,0.00012684961,0.000024736832],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022565964,0.0000020669827,0.9718722,3.973075e-7,0.000009805911,0.000028230761,0.00022254125,0.00041223838,0.00007121109,0.00020263658,0.0019775638,0.025178554],"study_design_scores_gemma":[0.00014904255,0.00038783636,0.98282325,0.000015345699,0.000009226524,0.000105072824,0.00015167003,0.00016327873,0.000057675687,0.0050716726,0.011012032,0.000053904336],"about_ca_topic_score_codex":0.0331391,"about_ca_topic_score_gemma":0.606268,"teacher_disagreement_score":0.5731289,"about_ca_system_score_codex":9.96736e-7,"about_ca_system_score_gemma":0.0016711104,"threshold_uncertainty_score":0.9988708},"labels":[],"label_agreement":null},{"id":"W2020396527","doi":"10.1139/e02-049","title":"Functional morphology of the temporal region in the Rhynchocephalia","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Canadian Museum of Nature","funders":"","keywords":"Quadrate bone; Anatomy; Condyle; Pterygoid Muscles; Mandible (arthropod mouthpart); Biology; Lateral pterygoid muscle; Flange; Skull; Cusp (singularity); Geology; Orthodontics; Mathematics; Geometry; Medicine; Zoology; Materials science; Masticatory force","score_opus":0.03480531836269341,"score_gpt":0.2094389947921006,"score_spread":0.1746336764294072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020396527","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9865825,0.0016002966,0.000020543781,0.0022995917,0.0010129425,0.000041974065,0.000005873356,5.494184e-7,0.008435683],"genre_scores_gemma":[0.99924165,0.000012421503,0.00010858445,0.0005065934,0.000047798716,1.0587682e-7,8.6225185e-7,3.418728e-7,0.000081639555],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998972,0.0003626804,0.00021836652,0.00008352077,0.00013478175,0.0002286343],"domain_scores_gemma":[0.99947864,0.00014564913,0.0001609175,0.00007773384,0.000044677236,0.00009235636],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00121459,0.00005270114,0.00010076146,0.00014556288,0.00027628106,0.000011069793,0.0003903523,0.000056966375,0.0007407759],"category_scores_gemma":[0.00021497296,0.000026260646,0.00005464366,0.00044003484,0.0012280354,0.00013583814,0.0000012641739,0.00017642028,0.0000108008],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000050432477,0.0000024112646,0.9965662,7.174133e-7,0.0000025682152,0.00003114464,0.00012072264,0.00090330886,0.0000052099626,0.0014958875,0.00068626506,0.00018054179],"study_design_scores_gemma":[0.000101517464,0.00012487256,0.9875258,0.000007057452,0.0000033099864,0.00136891,0.0003898731,0.000044732828,0.000011176899,0.003234088,0.00715577,0.000032853342],"about_ca_topic_score_codex":0.0072295098,"about_ca_topic_score_gemma":0.48461145,"teacher_disagreement_score":0.47738194,"about_ca_system_score_codex":0.0000011361977,"about_ca_system_score_gemma":0.0010876667,"threshold_uncertainty_score":0.9993814},"labels":[],"label_agreement":null},{"id":"W2020523783","doi":"10.1139/e00-108","title":"Illinoian to Late Wisconsinan stratigraphy at Woodbridge, Ontario","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; University of Waterloo","funders":"","keywords":"Geology; Paleontology; Stadial; Quaternary; Bedrock; Interglacial; Geomorphology; Holocene","score_opus":0.0337720555112826,"score_gpt":0.23462932388985014,"score_spread":0.20085726837856754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020523783","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9444945,0.0006105053,0.000007020198,0.002192647,0.00055627554,0.00007539407,0.000011469673,0.0000033212457,0.052048884],"genre_scores_gemma":[0.9952518,0.00002474937,0.0007822774,0.00066264166,0.00006515045,1.4033417e-7,0.0000026558214,0.0000012378165,0.0032093646],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984331,0.000099388846,0.00028683923,0.00020171043,0.00026844948,0.00071052316],"domain_scores_gemma":[0.9983099,0.00010891785,0.00010864551,0.00011806351,0.00011162677,0.0012428118],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009323359,0.000116233874,0.00020892643,0.0006059069,0.00076409534,0.00011028115,0.00052241946,0.00008043758,0.008494082],"category_scores_gemma":[0.000078192905,0.00009019806,0.000082126084,0.0006809846,0.0008134395,0.00029684755,0.0000059175673,0.00028616135,0.00043139243],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016702435,0.000002267189,0.996846,0.0000013877905,0.000010322654,0.00051109144,0.00040856455,0.0013412054,0.0000034185753,0.00007301121,0.00030582544,0.0004802052],"study_design_scores_gemma":[0.00012291607,0.0004699445,0.9566454,0.000018309318,0.0000055718156,0.0010028047,0.00011600362,0.000063929714,0.000030050945,0.00060072757,0.04081215,0.00011214591],"about_ca_topic_score_codex":0.12196379,"about_ca_topic_score_gemma":0.9985265,"teacher_disagreement_score":0.8765628,"about_ca_system_score_codex":0.0000013185485,"about_ca_system_score_gemma":0.002305718,"threshold_uncertainty_score":0.99241227},"labels":[],"label_agreement":null},{"id":"W2020528987","doi":"10.1139/e00-103","title":"Lithostratigraphy and limiting optical ages of the Pleistocene fill in Fraser River valley near Clinton, south-central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Glacial period; Geology; Pleistocene; Lithostratigraphy; Glacier; Aggradation; Paleontology; Sequence (biology); Bedrock; Geomorphology; Geochemistry; Fluvial; Sedimentary rock; Structural basin","score_opus":0.019251193645793568,"score_gpt":0.21565309868410915,"score_spread":0.1964019050383156,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020528987","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99558157,0.0016225517,0.000001905377,0.0004599854,0.00021442607,0.000075864926,0.000019210085,0.0000013294367,0.0020231442],"genre_scores_gemma":[0.9989177,0.00011305624,0.0007190206,0.0001448107,0.00003736909,1.317463e-7,0.0000010449328,0.0000010443027,0.00006581425],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99863034,0.00016286982,0.0003246708,0.00015291126,0.00021810945,0.0005111103],"domain_scores_gemma":[0.99907714,0.00022334902,0.00013573385,0.00007340038,0.0000804274,0.00040993767],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009837106,0.00006334233,0.00019197214,0.000104235376,0.00049086043,0.00020726927,0.0003715843,0.000088921726,0.00091872487],"category_scores_gemma":[0.0003291747,0.000058648202,0.00006519307,0.00047947295,0.0027354634,0.00020791151,0.000007649865,0.00033367117,0.0000035153787],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007060133,0.0000032739763,0.9977442,0.0000049030136,0.0000062902795,0.00020837976,0.0003639127,0.00037952495,4.4771656e-7,0.000008992834,0.00005504871,0.0012179478],"study_design_scores_gemma":[0.00022070385,0.00020014947,0.9973424,0.00007037801,0.000006230745,0.00042687092,0.0003303766,0.0004885581,0.00000355856,0.0004213793,0.0004227661,0.00006662626],"about_ca_topic_score_codex":0.09683864,"about_ca_topic_score_gemma":0.9837946,"teacher_disagreement_score":0.886956,"about_ca_system_score_codex":3.977326e-7,"about_ca_system_score_gemma":0.00082549936,"threshold_uncertainty_score":0.9999946},"labels":[],"label_agreement":null},{"id":"W2020697553","doi":"10.1139/e04-099","title":"Diatomaceous origin of siliceous shale in Eocene lake beds of central British Columbia","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Oil shale; Diagenesis; Diatom; Paleogene; Paleontology; Biogenic silica; Geochemistry; Neogene; Cretaceous; Oceanography; Structural basin","score_opus":0.013683801415216086,"score_gpt":0.21042217920496856,"score_spread":0.19673837778975248,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020697553","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9806287,0.00721452,0.0000029285009,0.00012814789,0.00027500628,0.000057704816,0.0001347654,0.0000019065043,0.011556312],"genre_scores_gemma":[0.9988322,0.00009667253,0.0008994797,0.000037033537,0.00007289927,8.4565436e-8,0.0000011995502,5.91851e-7,0.00005983481],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985691,0.000071965136,0.00048777994,0.00013741238,0.00026388225,0.00046988874],"domain_scores_gemma":[0.99899834,0.000101496065,0.00028501273,0.00007369984,0.00007843499,0.00046300422],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006187146,0.000072361145,0.0002885333,0.00023146023,0.00015394531,0.000091231035,0.0004274109,0.0000746471,0.0014234311],"category_scores_gemma":[0.00009197359,0.000085291285,0.00009490613,0.00053743884,0.000872869,0.0003688909,8.1590844e-7,0.00016775496,0.0000018524997],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045526726,0.0000081130975,0.94367915,0.000007043733,0.000007843599,0.00013298636,0.00021926043,0.0006849205,0.0000109103885,0.000008670774,0.00012013439,0.05511641],"study_design_scores_gemma":[0.0002401635,0.00028846462,0.99702805,0.0000695235,0.000007719351,0.0003289086,0.00015774004,0.0003304545,0.000054448057,0.00020930707,0.0011966093,0.00008863783],"about_ca_topic_score_codex":0.1993336,"about_ca_topic_score_gemma":0.998266,"teacher_disagreement_score":0.79893243,"about_ca_system_score_codex":0.0000013908933,"about_ca_system_score_gemma":0.0014216715,"threshold_uncertainty_score":0.9994894},"labels":[],"label_agreement":null},{"id":"W2020705769","doi":"10.1139/e06-010","title":"Age constraints for Paleoproterozoic glaciation in the Lake Superior Region: detrital zircon and hydrothermal xenotime ages for the Chocolay Group, Marquette Range Supergroup","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Australian Research Council; University of Minnesota Duluth","keywords":"Zircon; Geology; Sedimentary depositional environment; Supergroup; Geochemistry; Paleontology; Unconformity; Sedimentary rock; Population; Geochronology; Structural basin","score_opus":0.01590359326072622,"score_gpt":0.19130591802649008,"score_spread":0.17540232476576387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020705769","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918183,0.0013590546,0.00032072706,0.005405989,0.00010820308,0.00038919534,0.000103429324,0.0000024077435,0.0004926656],"genre_scores_gemma":[0.9985447,0.000018450595,0.00054887385,0.0006208142,0.00019278443,0.000006394697,0.000017221108,0.0000010348706,0.000049761107],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989438,0.00007439506,0.00027374094,0.00016034306,0.00018544125,0.00036230363],"domain_scores_gemma":[0.9991248,0.0005167028,0.00010607446,0.0000644452,0.000048556194,0.00013939623],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011697788,0.000103376944,0.0001723518,0.00012611592,0.00047535216,0.00023239084,0.00034988514,0.000051821127,0.00043856734],"category_scores_gemma":[0.0001527416,0.00005193152,0.00011174042,0.00032426268,0.00080687006,0.00024144992,0.0000027624942,0.00011891623,0.000002143709],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026176467,0.000007760706,0.9909963,0.000010087497,0.000011466713,0.00005541347,0.0001801348,0.00039748152,0.00012320076,0.0002729652,0.00016181389,0.007757188],"study_design_scores_gemma":[0.0004773816,0.0003600418,0.98715013,0.000018755994,0.00002782052,0.000113839254,0.000330874,0.0011787625,0.000052357816,0.0030178186,0.0071601663,0.00011203767],"about_ca_topic_score_codex":0.0074923784,"about_ca_topic_score_gemma":0.74370867,"teacher_disagreement_score":0.7362163,"about_ca_system_score_codex":0.0000013286631,"about_ca_system_score_gemma":0.000094392344,"threshold_uncertainty_score":0.99911684},"labels":[],"label_agreement":null},{"id":"W2020740664","doi":"10.1139/e10-009","title":"Mantle heterogeneities and their significance: results from Lithoprobe seismic reflection and refraction – wide-angle reflection studiesThis article is one of a series of papers published in this Special Issue on the theme<i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.Lithoprobe Contribution 1486.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; University of British Columbia; Geological Survey of Canada","funders":"","keywords":"Geology; Lithosphere; Craton; Mantle (geology); Subduction; Archean; Seismology; Tectonics; Geophysics; Paleontology","score_opus":0.013375847078095526,"score_gpt":0.20810172393337018,"score_spread":0.19472587685527465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020740664","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950344,0.000776744,0.000010595473,0.0027021896,0.0004082217,0.00030521266,0.00021359428,0.000002595364,0.0005464645],"genre_scores_gemma":[0.99921656,0.0002995788,0.00015806351,0.00006829264,0.00020164014,0.0000024973485,0.000004815687,0.000002456441,0.000046119192],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99858296,0.00022780348,0.0005204606,0.00021473631,0.00025071527,0.00020335107],"domain_scores_gemma":[0.998378,0.00046420106,0.0006633362,0.00012684343,0.00027271375,0.000094947805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022426713,0.00012552463,0.00034571072,0.00015515334,0.00030485343,0.0001410638,0.00014126055,0.000071362076,0.00020536732],"category_scores_gemma":[0.0007879058,0.00006986446,0.000036173627,0.00041789107,0.0011136981,0.0005612724,0.000010305796,0.00018146314,4.5858948e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.013348309,0.00026167635,0.61063194,0.00068199093,0.0007071192,0.000021377658,0.082190216,0.0019308976,0.2569667,0.0035707275,0.0022862768,0.027402794],"study_design_scores_gemma":[0.0049305325,0.0043933485,0.58258784,0.0008265034,0.00022697775,0.00010447123,0.014397615,0.001632968,0.34793127,0.027243916,0.015194002,0.0005305732],"about_ca_topic_score_codex":0.050164487,"about_ca_topic_score_gemma":0.18026793,"teacher_disagreement_score":0.13010344,"about_ca_system_score_codex":0.0000054552597,"about_ca_system_score_gemma":0.00029786793,"threshold_uncertainty_score":0.95616055},"labels":[],"label_agreement":null},{"id":"W2020784494","doi":"10.1139/e01-076","title":"Coeval migmatites and granulites, Muskoka domain, southwestern Grenville Province, Ontario","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University; Deutscher Akademischer Austauschdienst","keywords":"Granulite; Metamorphism; Geochemistry; Migmatite; Geology; Zircon; Gneiss; Mafic; Felsic; Metamorphic facies; Petrology; Facies; Metamorphic rock; Geomorphology","score_opus":0.015848860914594105,"score_gpt":0.16590142635821917,"score_spread":0.15005256544362505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020784494","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9841336,0.0030466453,0.0000066568173,0.0011733617,0.00013627073,0.000044158744,0.000021465446,0.0000031236175,0.011434735],"genre_scores_gemma":[0.9973361,0.000032754022,0.0015105485,0.00041850586,0.000075989505,9.229848e-8,0.0000024541625,9.302947e-7,0.00062261557],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99876267,0.000047672616,0.0002964272,0.0001914587,0.00029028187,0.00041151483],"domain_scores_gemma":[0.9988154,0.000096847936,0.00015214388,0.00007310071,0.00007186398,0.000790636],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004182012,0.000121476165,0.0002228235,0.00020811764,0.0003918962,0.000201252,0.0003191235,0.00004826318,0.019377442],"category_scores_gemma":[0.00007856169,0.00007807585,0.00008744749,0.0003294247,0.0007382041,0.00024419444,0.000006531226,0.00018055202,0.000107308355],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021870044,0.000004007871,0.9965254,0.00000336981,0.000009607758,0.00007131004,0.00041227954,0.00015044534,0.000012444386,0.00005282717,0.00014905787,0.002607032],"study_design_scores_gemma":[0.00018338533,0.00031617837,0.9634206,0.000026047433,0.000021254711,0.00019953637,0.00027573825,0.00061134173,0.000019202233,0.0060838712,0.028680777,0.00016206168],"about_ca_topic_score_codex":0.2304966,"about_ca_topic_score_gemma":0.9842913,"teacher_disagreement_score":0.7537947,"about_ca_system_score_codex":0.000002002362,"about_ca_system_score_gemma":0.00029149308,"threshold_uncertainty_score":0.981519},"labels":[],"label_agreement":null},{"id":"W2021314539","doi":"10.1139/e06-061","title":"Assessment of the relationship between emplacement of the Algoman plutons and regional deformation in the Rainy Lake region, Ontario","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Pluton; Geology; Geochemistry; Seismology; Deformation (meteorology); Crust; Transpression; Petrology; Shear zone; Tectonics","score_opus":0.041759200392118105,"score_gpt":0.22321349001093027,"score_spread":0.18145428961881216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2021314539","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99153703,0.00010323475,0.000011389195,0.00554006,0.00004383093,0.00006323227,0.000009285,3.577665e-7,0.0026915905],"genre_scores_gemma":[0.9996071,0.0000015626148,0.00013475992,0.00015380296,0.000025488027,1.6073376e-7,0.0000030728309,2.7644862e-7,0.000073817166],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998999,0.00013455482,0.00032069028,0.00006826667,0.00033252372,0.00014494154],"domain_scores_gemma":[0.99922436,0.0002846935,0.00028356627,0.000084053485,0.00005392535,0.00006941735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00095385016,0.000052437466,0.00010870622,0.000087498855,0.00030452135,0.000033111897,0.00038447516,0.000027670305,0.0001937392],"category_scores_gemma":[0.00008884873,0.00002154581,0.00007324845,0.00051280373,0.00057618006,0.00012335478,0.000006675985,0.00016501294,4.236857e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[7.368531e-7,0.0000025353868,0.99669886,0.000001846014,0.0000028324666,7.352022e-7,0.00022810219,0.002105824,0.0000013408315,0.0008035854,0.00007712127,0.000076483375],"study_design_scores_gemma":[0.000074404394,0.000050100207,0.9845144,0.000026680502,0.000014821592,0.000020175397,0.00026493293,0.00014960048,0.0000068871077,0.013906098,0.0009419114,0.000029986673],"about_ca_topic_score_codex":0.16390963,"about_ca_topic_score_gemma":0.9791512,"teacher_disagreement_score":0.8152416,"about_ca_system_score_codex":0.0000033027923,"about_ca_system_score_gemma":0.00059291313,"threshold_uncertainty_score":0.84165794},"labels":[],"label_agreement":null},{"id":"W2021423314","doi":"10.1139/e03-057","title":"The Burgess Shale and associated Cambrian formations west of the Fossil Gully Fault Zone on Mount Stephen, British Columbia","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum","funders":"","keywords":"Geology; Trilobite; Paleontology; Conglomerate; Oil shale; Facies; Onlap; Cliff; Escarpment; Fault (geology); Structural basin; Ordovician","score_opus":0.013089450676483297,"score_gpt":0.195136889313533,"score_spread":0.18204743863704972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2021423314","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9752437,0.004148833,0.0000043331047,0.0004472702,0.0005091714,0.00008616314,0.00009994067,0.0000017654874,0.019458847],"genre_scores_gemma":[0.9995009,0.00006841691,0.00006558409,0.00007742802,0.00002040148,2.5132374e-7,4.27049e-7,4.950874e-7,0.00026612144],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99878573,0.00017582931,0.00031200022,0.00010114587,0.00028916085,0.0003361196],"domain_scores_gemma":[0.9989095,0.00027123047,0.00030378872,0.000093911,0.00012557367,0.0002960014],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0012086335,0.000065971835,0.00014699387,0.00006053952,0.0018875157,0.00048130154,0.00039125542,0.00005895896,0.00018061152],"category_scores_gemma":[0.00046800944,0.000050172275,0.000073070296,0.00039693277,0.0012036932,0.00029971404,8.8981733e-7,0.00019252441,0.0000012669998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001610439,0.0000036640708,0.9865497,0.0000018172329,0.0000149187745,0.000011347781,0.00018213213,0.00005042674,0.0000029311768,0.00021317492,0.0003511867,0.012617104],"study_design_scores_gemma":[0.00015771444,0.00018154741,0.9959547,0.00005740916,0.000011266618,0.0001595344,0.00069762475,0.00013401444,0.0000074453656,0.00052392186,0.002048678,0.00006614706],"about_ca_topic_score_codex":0.13164636,"about_ca_topic_score_gemma":0.9881296,"teacher_disagreement_score":0.8564833,"about_ca_system_score_codex":0.0000023283228,"about_ca_system_score_gemma":0.0010235612,"threshold_uncertainty_score":0.9994119},"labels":[],"label_agreement":null},{"id":"W2021536086","doi":"10.1139/e01-060","title":"Crustal structure beneath the Western Canada Sedimentary Basin: constraints from gravity and magnetic modelling","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Gravity anomaly; Magnetic anomaly; Sill; Tectonics; Crust; Basement; Fault (geology); Seismology; Structural basin; Sedimentary rock; Bouguer anomaly; Detachment fault; Pluton; Sedimentary basin; Geophysics; Paleontology; Petrology; Extensional definition","score_opus":0.015537789305006702,"score_gpt":0.15980086591192424,"score_spread":0.14426307660691753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2021536086","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916614,0.003319631,0.000019642594,0.00387978,0.00018523335,0.00003222952,0.00025508078,0.0000012874053,0.0006456864],"genre_scores_gemma":[0.99756515,0.000040129646,0.00047261736,0.0017699915,0.00009696859,3.172256e-8,0.0000054507586,6.982511e-7,0.00004896477],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989673,0.000055719098,0.0002071884,0.00015711991,0.0002973499,0.00031531215],"domain_scores_gemma":[0.9990893,0.00013739917,0.00009508716,0.00006631564,0.00004831908,0.0005635865],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018097549,0.000102200516,0.00016297484,0.00005691519,0.00042104875,0.0001324093,0.0003171554,0.00003282268,0.012295865],"category_scores_gemma":[0.000028760795,0.00005695137,0.000042250496,0.00021921423,0.00067805545,0.00014491759,0.0000058182823,0.0001958887,0.000004210545],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000016345958,0.0000012265502,0.9759318,0.0000011209996,0.000011343553,0.00007906396,0.00010916479,0.0185816,0.0000053623708,0.0000067121805,0.0002618214,0.00500912],"study_design_scores_gemma":[0.00020700568,0.00020687496,0.93410194,0.000026452168,0.00006319087,0.00021685967,0.0006541789,0.05190587,0.00007358151,0.005706018,0.0066113556,0.00022668196],"about_ca_topic_score_codex":0.9409895,"about_ca_topic_score_gemma":0.9947543,"teacher_disagreement_score":0.05376483,"about_ca_system_score_codex":0.0000018853079,"about_ca_system_score_gemma":0.00035934933,"threshold_uncertainty_score":0.98860705},"labels":[],"label_agreement":null},{"id":"W2021599944","doi":"10.1139/e09-056","title":"Groundwater recharge trends in CanadaGeological Survey of Canada Contribution 20090009.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval; Université du Québec à Montréal; Institut National de la Recherche Scientifique; Environment and Climate Change Canada; Geological Survey of Canada","funders":"","keywords":"Baseflow; Groundwater recharge; Groundwater; Series (stratigraphy); Hydrology (agriculture); Climate change; Environmental science; Physical geography; Geology; Aquifer; Geography; Drainage basin; Streamflow; Oceanography","score_opus":0.02099345247028552,"score_gpt":0.2239475213156348,"score_spread":0.20295406884534928,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2021599944","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98994845,0.000108472595,0.000015833608,0.0034702348,0.0002067726,0.00003366717,0.000009338136,9.635135e-7,0.0062062466],"genre_scores_gemma":[0.9988542,0.0000081040325,0.00005349738,0.00063167,0.000010458061,2.2322857e-7,0.0000018983104,9.633201e-7,0.0004389601],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987964,0.00012391059,0.00029364022,0.0001268736,0.00023527164,0.00042392052],"domain_scores_gemma":[0.99950093,0.0000411088,0.00013546136,0.000060735176,0.000026118225,0.00023565092],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015954991,0.000078286575,0.00019006981,0.0001825812,0.00019621571,0.000014370168,0.00028660725,0.00003840231,0.0012411649],"category_scores_gemma":[0.00014810292,0.000058066424,0.000023994173,0.00059482735,0.00038934493,0.00018813244,0.00001336555,0.000116351424,0.0000029823316],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010349242,0.000010204647,0.9909539,4.0210367e-7,0.0000047847916,0.00010847244,0.00008177997,0.0019354029,0.00003347247,0.00012384,0.005703649,0.0010337376],"study_design_scores_gemma":[0.00014959252,0.00022647475,0.9952143,0.0000064574897,0.000003218915,0.000011885212,0.000030434048,0.000092494636,0.00010814815,0.00030959654,0.0037802996,0.00006711185],"about_ca_topic_score_codex":0.95389354,"about_ca_topic_score_gemma":0.99959844,"teacher_disagreement_score":0.045704916,"about_ca_system_score_codex":0.000056196994,"about_ca_system_score_gemma":0.0004003328,"threshold_uncertainty_score":0.9996718},"labels":[],"label_agreement":null},{"id":"W2021908084","doi":"10.1139/e04-045","title":"Tectonic implications of new SHRIMP and TIMS UPb geochronology of rocks from the Sask Craton, Peter Lake Domain, and Hearne margin, Trans-Hudson Orogen, Saskatchewan","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"National Science Foundation","keywords":"Craton; Zircon; Geology; Geochronology; Geochemistry; Gneiss; Crust; Archean; Tectonics; Paleontology; Metamorphic rock","score_opus":0.011846395689173308,"score_gpt":0.19585381083157063,"score_spread":0.18400741514239732,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2021908084","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98174757,0.0067106336,0.000100603225,0.010656888,0.00003517276,0.000055353947,0.000108140244,0.0000019358258,0.0005837286],"genre_scores_gemma":[0.9971636,0.0001486957,0.0019984613,0.0005496711,0.00008327813,1.5752305e-7,0.0000067003803,0.0000011127732,0.000048327718],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99892217,0.000059868133,0.00037077302,0.00018507725,0.00016165368,0.00030044088],"domain_scores_gemma":[0.9989263,0.00019749334,0.00020080066,0.0001124296,0.000086372245,0.00047660634],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000392366,0.00010677545,0.0002743579,0.0001111127,0.00021243573,0.000044351782,0.000335338,0.000064950065,0.0045745503],"category_scores_gemma":[0.00005562643,0.000062569874,0.00008276886,0.00035981994,0.0009338076,0.00015868896,0.000008228113,0.00015881611,0.0000050309454],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011691987,0.0000064229635,0.96968627,0.000004005344,0.000038326503,0.0000037898135,0.00095991953,0.00074987346,0.0007656323,0.000030534447,0.0002680542,0.027475467],"study_design_scores_gemma":[0.00022092448,0.0002605963,0.97778106,0.00002009217,0.000046363977,0.00007741412,0.0007913588,0.0001879126,0.0007320589,0.0081055695,0.011682019,0.000094661445],"about_ca_topic_score_codex":0.049398936,"about_ca_topic_score_gemma":0.9133022,"teacher_disagreement_score":0.8639033,"about_ca_system_score_codex":0.0000011543157,"about_ca_system_score_gemma":0.00063470565,"threshold_uncertainty_score":0.9963354},"labels":[],"label_agreement":null},{"id":"W2022143763","doi":"10.1139/cjes-2013-0040","title":"Geochemistry, U–Pb geochronology, and genesis of granitoid clasts in transported volcanogenic massive sulfide ore deposits, Buchans, Newfoundland","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Felsic; Geology; Geochemistry; Anatexis; Fractional crystallization (geology); Zircon; Rhyolite; Volcanogenic massive sulfide ore deposit; Conglomerate; Clastic rock; Breccia; Volcanic rock; Geochronology; Mafic; Petrology; Partial melting; Volcano; Basalt; Sedimentary rock","score_opus":0.010760585431925793,"score_gpt":0.18154466872876454,"score_spread":0.17078408329683875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022143763","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941594,0.0040872027,0.000015550171,0.0010082568,0.00008433036,0.00007085281,0.000032090735,0.0000023708717,0.0005399506],"genre_scores_gemma":[0.998905,0.00019496809,0.0006921503,0.00011558141,0.000049672548,4.4211043e-7,0.000010177831,0.0000013518224,0.0000306581],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985985,0.000053275468,0.00044842955,0.00022350674,0.000219983,0.00045626686],"domain_scores_gemma":[0.9988448,0.00010591286,0.00022040059,0.00008465432,0.00014831313,0.0005959274],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00030688487,0.00014072463,0.00033594287,0.00028678763,0.00015369346,0.00006290395,0.00035941618,0.00010078892,0.0039084842],"category_scores_gemma":[0.00009670797,0.00009996371,0.00009544634,0.0006171054,0.00082808465,0.00023791677,0.00000535716,0.00017609366,0.000014093437],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007276171,0.000005482714,0.99215007,0.000011229372,0.00002014106,0.000055171375,0.00012925093,0.00068626425,0.0029367362,0.000006632728,0.000025888909,0.003965831],"study_design_scores_gemma":[0.0002442278,0.00019655284,0.99322945,0.000035793306,0.000028723816,0.000103166436,0.000470587,0.00090951665,0.0019524624,0.002569561,0.00012928258,0.00013069471],"about_ca_topic_score_codex":0.27675483,"about_ca_topic_score_gemma":0.88940185,"teacher_disagreement_score":0.61264706,"about_ca_system_score_codex":0.0000028307213,"about_ca_system_score_gemma":0.00047818915,"threshold_uncertainty_score":0.99700207},"labels":[],"label_agreement":null},{"id":"W2022153838","doi":"10.1139/e06-070","title":"<i>Hikorocodium</i> Endo is not an alga but an inozoid sponge","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft","keywords":"Sponge; Permian; Algae; Genus; Taxon; Type species; Paleontology; Geology; Botany; Biology","score_opus":0.03376890421813191,"score_gpt":0.24348295299300388,"score_spread":0.20971404877487196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022153838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9507748,0.0027561325,0.00006189616,0.00038653202,0.00080964784,0.00006501406,0.00006926622,0.000007959205,0.04506875],"genre_scores_gemma":[0.99634206,0.00002692696,0.0021170455,0.0011506344,0.00030310388,7.2076205e-8,0.0000020054028,0.0000010271312,0.00005712953],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99799484,0.0001103714,0.0004374952,0.00026584696,0.0004203646,0.00077105616],"domain_scores_gemma":[0.99754524,0.00013031917,0.00023912924,0.00016738386,0.0001245931,0.0017933451],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002445356,0.00016277708,0.00024027062,0.00055161596,0.00080675667,0.00022383854,0.000828208,0.00012027538,0.001221437],"category_scores_gemma":[0.00007349264,0.00012964167,0.000103235456,0.0004970075,0.0010225913,0.0015447735,8.346283e-7,0.00030821373,0.000024566421],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003494308,0.000008565232,0.9010964,0.0000025580327,0.000011051077,0.000448608,0.00094789395,0.000040494953,0.00019620448,0.00018717622,0.000093483366,0.09693264],"study_design_scores_gemma":[0.00019864793,0.00095691823,0.9901341,0.000014732927,0.000011299659,0.0006148144,0.00087196263,0.00016300572,0.0016993751,0.0005179216,0.0046333587,0.00018384571],"about_ca_topic_score_codex":0.026605885,"about_ca_topic_score_gemma":0.8151989,"teacher_disagreement_score":0.78859305,"about_ca_system_score_codex":0.0000014299802,"about_ca_system_score_gemma":0.0013927582,"threshold_uncertainty_score":0.9996916},"labels":[],"label_agreement":null},{"id":"W2022382325","doi":"10.1139/e01-037","title":"Low-temperature cooling history of the Shuswap metamorphic core complex, British Columbia: constraints from apatite and zircon fission-track ages","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Eidgenössische Technische Hochschule Zürich; National Science Foundation","keywords":"Zircon; Fission track dating; Geology; Geochemistry; Metamorphic rock; Metamorphic core complex; Apatite; Paleontology; Extensional definition; Tectonics","score_opus":0.02499564420226454,"score_gpt":0.1844771834209236,"score_spread":0.15948153921865904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022382325","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99391896,0.0039614,0.0000016839508,0.00055676117,0.00034891538,0.000049307007,0.0001276998,0.0000024921555,0.0010327968],"genre_scores_gemma":[0.99832916,0.000118750075,0.00038889036,0.0005838876,0.000080762264,8.4647326e-8,0.000010279245,0.000001060184,0.00048711244],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99880946,0.000075337404,0.00033945555,0.00018806146,0.00030444944,0.0002832638],"domain_scores_gemma":[0.998846,0.00017399236,0.0002589665,0.00008701106,0.0001386857,0.0004953604],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004209325,0.000086313696,0.00028251295,0.00006559314,0.00031443025,0.00017381141,0.00041060935,0.00007184157,0.01703504],"category_scores_gemma":[0.00025742518,0.00006757687,0.000115093084,0.000349554,0.0020085324,0.00019077801,0.00000930815,0.00024610033,0.000005185569],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003337971,0.00000515081,0.99252933,0.000004992062,0.00002017427,0.000097062184,0.00010555939,0.0003180167,0.001972837,0.0000032039063,0.001699865,0.003240453],"study_design_scores_gemma":[0.00013404585,0.00007986372,0.9924843,0.000110062625,0.000034327517,0.00019594686,0.00020629594,0.0004123125,0.00008834838,0.0014540659,0.004698189,0.00010228205],"about_ca_topic_score_codex":0.2385063,"about_ca_topic_score_gemma":0.93019575,"teacher_disagreement_score":0.69168943,"about_ca_system_score_codex":0.0000035453645,"about_ca_system_score_gemma":0.00058796996,"threshold_uncertainty_score":0.98386353},"labels":[],"label_agreement":null},{"id":"W2022622568","doi":"10.1139/e00-072","title":"Age and composition of the Ruisseau Isabelle Mélange along the Shickshock Sud fault zone: constraints on the timing of mélanges formation in the Gaspé Appalachians","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Université du Québec à Chicoutimi; Centre de Géomatique du Québec; Institut National de la Recherche Scientifique","funders":"","keywords":"Geology; Ordovician; Outcrop; Fault (geology); Metamorphic rock; Paleontology; Geochemistry; Basement; Devonian; Siltstone; Nappe; Sedimentary rock; Tectonics; Facies; Structural basin; Archaeology","score_opus":0.030243631147101106,"score_gpt":0.21220422697738575,"score_spread":0.18196059583028465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022622568","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98483914,0.00046920325,0.000012774549,0.00958787,0.000047633126,0.00008774119,0.000016091995,7.2777516e-7,0.0049388045],"genre_scores_gemma":[0.9992507,0.000054046406,0.000039653558,0.0006094027,0.00002847719,2.3476422e-7,0.0000021251801,4.7251945e-7,0.0000148752],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99900955,0.00018938363,0.00024487302,0.00007362321,0.00028771162,0.00019486886],"domain_scores_gemma":[0.9991461,0.0004402303,0.00019552324,0.00008955954,0.000046270663,0.00008232574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010672716,0.000067489775,0.00012006104,0.00007496032,0.00038651234,0.000060407958,0.00047512224,0.000028347637,0.00062443083],"category_scores_gemma":[0.000108855624,0.000024350209,0.00006432432,0.00045733148,0.0011369989,0.000115787036,0.000006477324,0.00017890353,0.0000026658854],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014202691,0.000013925638,0.9829807,0.000010231835,0.000015079472,0.000039947307,0.0035460806,0.0043775607,0.0003423659,0.0007280703,0.00018783727,0.007743943],"study_design_scores_gemma":[0.00009847526,0.00014082967,0.98833483,0.00007218135,0.000017579561,0.0001539225,0.0050016427,0.0036675914,0.00041679328,0.0016089248,0.00043341963,0.000053821015],"about_ca_topic_score_codex":0.014821691,"about_ca_topic_score_gemma":0.37666902,"teacher_disagreement_score":0.36184734,"about_ca_system_score_codex":0.0000012972658,"about_ca_system_score_gemma":0.00007867824,"threshold_uncertainty_score":0.9917387},"labels":[],"label_agreement":null},{"id":"W2023104497","doi":"10.1139/e07-015","title":"Luminescence dating of mid- to Late Wisconsinan aeolian sand as a constraint on the last advance of the Laurentide Ice Sheet across the Tuktoyaktuk Coastlands, western Arctic Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Glacial period; Thermoluminescence dating; Ice sheet; Arctic; Deglaciation; Wisconsin glaciation; Paleontology; Radiocarbon dating; Last Glacial Maximum; Oceanography; Physical geography; Geomorphology; Sea ice; Ice stream; Cryosphere","score_opus":0.018925622138316958,"score_gpt":0.2538049797642477,"score_spread":0.23487935762593076,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023104497","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9899275,0.00032715287,0.0000066258476,0.006869779,0.0004955678,0.00014212693,0.00005879699,8.935045e-7,0.0021716063],"genre_scores_gemma":[0.9984685,0.000009014938,0.0000705185,0.001265478,0.000039332,2.1126824e-7,9.898113e-7,0.0000015230032,0.00014439599],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99816763,0.00020853488,0.00040931514,0.00016006215,0.0004500112,0.0006044386],"domain_scores_gemma":[0.9976981,0.0011356483,0.00034466895,0.0002175434,0.00019497176,0.0004090132],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027298045,0.00011502733,0.00021240879,0.00009013248,0.0007932106,0.000053605178,0.0010493752,0.000042592703,0.00030405688],"category_scores_gemma":[0.0011915731,0.000055720022,0.00005639613,0.0006214858,0.0025900663,0.0001192687,0.000020560643,0.00036508587,0.0000068456743],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000194729,0.000002441656,0.9964591,0.000009447401,0.000011363339,0.000053464446,0.0007501356,0.0020710542,0.000029599867,0.00006307135,0.000112809,0.000418032],"study_design_scores_gemma":[0.000130702,0.00019201258,0.9935143,0.0001960924,0.000007949662,0.00038914572,0.0028781467,0.00007611911,0.0010262381,0.00013407192,0.0013814418,0.00007379452],"about_ca_topic_score_codex":0.3870682,"about_ca_topic_score_gemma":0.9982213,"teacher_disagreement_score":0.61115307,"about_ca_system_score_codex":0.0000018559593,"about_ca_system_score_gemma":0.0032474427,"threshold_uncertainty_score":0.9543207},"labels":[],"label_agreement":null},{"id":"W2023148567","doi":"10.1139/e10-055","title":"Trace element geochemistry of Nova Scotia (Canada) maple syrup","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant-Derived Bioactive Compounds","field":"Chemistry","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor; University of British Columbia, Okanagan Campus; Okanagan College","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Chemistry; Trace element; Alkali metal; Sugar; Nova scotia; Mineralogy; Analytical Chemistry (journal); Environmental chemistry; Geology; Food science","score_opus":0.01612078744460847,"score_gpt":0.22265994875806133,"score_spread":0.20653916131345287,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023148567","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9797602,0.00022586179,0.0000071774266,0.00060797227,0.0005416413,0.000019458632,0.00011016521,0.0000024064964,0.018725067],"genre_scores_gemma":[0.9986515,0.000003375844,0.0008282436,0.000067580404,0.00018911672,1.5567448e-7,0.0000022212764,0.000005454136,0.0002523202],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9985414,0.000009302019,0.00037164707,0.00016595317,0.00049278187,0.00041892155],"domain_scores_gemma":[0.99848294,0.000076571814,0.0003772146,0.00017401132,0.00023842335,0.0006508111],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00039601442,0.00012825127,0.00021229578,0.00011170099,0.00014829401,0.00006881203,0.00073982717,0.00007249718,0.0047787083],"category_scores_gemma":[0.00021035447,0.00011436745,0.000070830574,0.00021412128,0.0005432742,0.00016112809,0.00001712667,0.00040240117,0.000003760892],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000074715454,0.000011723841,0.12297062,0.000034438825,0.000031676776,0.00012527336,0.000090334564,0.000028846736,0.873052,0.00009299209,0.0030067484,0.00054786674],"study_design_scores_gemma":[0.0002982693,0.000056777768,0.02947636,0.00010336408,0.000020719373,0.00050240156,0.0008232694,0.00009389863,0.9242083,0.00010345463,0.044088792,0.00022438754],"about_ca_topic_score_codex":0.32802054,"about_ca_topic_score_gemma":0.9868554,"teacher_disagreement_score":0.6588348,"about_ca_system_score_codex":0.000024452225,"about_ca_system_score_gemma":0.0076239463,"threshold_uncertainty_score":0.99800193},"labels":[],"label_agreement":null},{"id":"W2023260550","doi":"10.1139/e08-063","title":"Weathering regime and geochemical conditions in a polar desert environment, Haughton impact structure region, Devon Island, Canada","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University; Canadian Space Agency","funders":"Canadian Space Agency","keywords":"Weathering; Geology; Silt; Frost weathering; Permafrost; Impact crater; Geomorphology; Geochemistry; Clastic rock; Bay; Mineralogy; Sedimentary rock; Soil water; Soil science; Oceanography","score_opus":0.010079519279742096,"score_gpt":0.19690277631835926,"score_spread":0.18682325703861716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023260550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981978,0.0006157648,0.000009647043,0.00045603784,0.00007263806,0.000052804146,0.000052051528,7.240151e-7,0.000542539],"genre_scores_gemma":[0.9993553,0.0000912207,0.00022286463,0.00012041458,0.000027575927,3.1287396e-7,0.0000050912704,0.0000044202056,0.00017279385],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99901646,0.000042015283,0.00021124253,0.0001589965,0.00022414967,0.00034715122],"domain_scores_gemma":[0.99922407,0.000029998611,0.00011873887,0.00008164278,0.000005954568,0.00053960946],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017439545,0.00010560273,0.00014558296,0.00009992989,0.00030437985,0.000027579545,0.00020408662,0.000053232518,0.0033736606],"category_scores_gemma":[0.00003325826,0.00007740018,0.000030538093,0.0002542476,0.0005611893,0.00023717688,0.000017373737,0.00022260673,0.0000036269917],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005687973,0.0000052107684,0.9853606,0.0000019037169,0.00001052789,0.00046504193,0.00082354015,0.008025618,0.003321031,0.000017716005,0.0018702311,0.00009286345],"study_design_scores_gemma":[0.00092795247,0.00037973016,0.9404692,0.00011783621,0.00002450472,0.0061109713,0.00073038123,0.0015929716,0.0019779934,0.002244349,0.04487923,0.0005448744],"about_ca_topic_score_codex":0.7913847,"about_ca_topic_score_gemma":0.9768978,"teacher_disagreement_score":0.1855131,"about_ca_system_score_codex":0.00008263085,"about_ca_system_score_gemma":0.00065804296,"threshold_uncertainty_score":0.9975374},"labels":[],"label_agreement":null},{"id":"W2023419747","doi":"10.1139/e06-038","title":"Partial melting of metapelites in the Gagnon terrane below the high-pressure belt in the Manicouagan area (Grenville Province): pressure–temperature (<i>P</i>–<i>T</i>) and U–Pb age constraints and implications","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Metamorphism; Geochemistry; Monazite; Kyanite; Zircon; Terrane; Sillimanite; Partial melting; Metamorphic rock; Gneiss; Biotite; Quartz; Crust; Tectonics; Paleontology","score_opus":0.01158901581699298,"score_gpt":0.18855079391593996,"score_spread":0.17696177809894698,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023419747","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98274696,0.0065798922,0.0000019647355,0.009371227,0.00003336931,0.0001465026,0.00006892061,0.0000010446447,0.0010501059],"genre_scores_gemma":[0.999169,0.00006161076,0.00014588573,0.00053584547,0.000057789286,9.919086e-7,0.000006662589,7.912797e-7,0.000021418842],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986868,0.0002299256,0.000341243,0.0001748188,0.00026669877,0.00030053605],"domain_scores_gemma":[0.99905604,0.00049375946,0.00017622321,0.00012127047,0.000044787022,0.000107894484],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015428045,0.00010943072,0.00020737892,0.00010666601,0.0003819235,0.00019191475,0.00054952485,0.000051369894,0.00027649594],"category_scores_gemma":[0.00015648565,0.000046236863,0.000050284016,0.00051312,0.0013097036,0.00015021836,0.0000096319445,0.00028352617,5.445578e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000075383887,0.000016640563,0.9911918,0.000013481442,0.000020379232,0.000051887368,0.00097039505,0.002934337,0.0009549821,0.00093913573,0.00015485044,0.0027445725],"study_design_scores_gemma":[0.00014712427,0.0000978655,0.99041075,0.000028968605,0.000058541842,0.0001092897,0.0012261901,0.00047789284,0.00016621916,0.0053564347,0.0018438746,0.000076857665],"about_ca_topic_score_codex":0.036177345,"about_ca_topic_score_gemma":0.62916106,"teacher_disagreement_score":0.59298366,"about_ca_system_score_codex":4.910307e-7,"about_ca_system_score_gemma":0.00016967686,"threshold_uncertainty_score":0.97024083},"labels":[],"label_agreement":null},{"id":"W2023424842","doi":"10.1139/e06-093","title":"Geology and geochemistry of the Dengjiashan Zn–Pb SEDEX deposit, Qinling Belt, China","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"Chang'an University","keywords":"Geology; Geochemistry; Sphalerite; Galena; Volcanogenic massive sulfide ore deposit; Pyrite; Sedimentary rock; Ore genesis; Ankerite; Fluid inclusions; Hydrothermal circulation; Siderite; Paleontology","score_opus":0.007780156218311264,"score_gpt":0.1901481991490143,"score_spread":0.18236804293070302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023424842","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99230605,0.0014106175,0.000031868967,0.0003341001,0.00015126626,0.000024531131,0.000012954922,0.0000012608624,0.0057273437],"genre_scores_gemma":[0.9991496,0.000016708042,0.000493112,0.00013457755,0.00009114036,2.4540256e-8,0.000002112984,8.374899e-7,0.00011185732],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989468,0.000026621796,0.0003098978,0.00012890942,0.00023279613,0.0003549814],"domain_scores_gemma":[0.9991491,0.00006698642,0.00023258704,0.000089870686,0.000057157613,0.000404297],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010066545,0.000087958906,0.00015482909,0.000106297106,0.00047331792,0.000051795098,0.00041502516,0.00005159524,0.00072564866],"category_scores_gemma":[0.000100861645,0.00005774269,0.00008049586,0.00040795835,0.0006691517,0.00014697688,0.000010013529,0.00016504782,0.0000020076172],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003823735,0.0000021560281,0.9956046,0.000009998682,0.000014709697,0.000026106245,0.00015037869,0.00057320256,0.0012554962,0.0000077936975,0.000028661025,0.0023230694],"study_design_scores_gemma":[0.00009856618,0.00007241817,0.9783649,0.000036437697,0.000024528492,0.00038274386,0.00071398425,0.0005282939,0.018873608,0.00032659448,0.00049592665,0.00008200503],"about_ca_topic_score_codex":0.029730653,"about_ca_topic_score_gemma":0.375031,"teacher_disagreement_score":0.34530035,"about_ca_system_score_codex":0.0000016135593,"about_ca_system_score_gemma":0.00035253444,"threshold_uncertainty_score":0.97673047},"labels":[],"label_agreement":null},{"id":"W2023491773","doi":"10.1139/e11-004","title":"North Atlantic spreading axes terminate in the continental cul-de-sacs of Baffin Bay and the Laptev Sea","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Bay; North American Plate; Plate tectonics; Continental shelf; Paleontology; Transform fault; Arctic; Oceanography; Paleogene; Precambrian; Ridge; Tectonics; Seismology; Cretaceous","score_opus":0.031399444114585416,"score_gpt":0.19356668205292774,"score_spread":0.1621672379383423,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023491773","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99586856,0.0007253677,0.0000054982797,0.0007968972,0.00010744343,0.00006178193,0.0000071693603,6.5699487e-7,0.002426607],"genre_scores_gemma":[0.99948424,0.00014542002,0.00013228181,0.00019021885,0.000035002955,1.75676e-7,8.8618145e-7,4.4593446e-7,0.000011331182],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992642,0.00010681968,0.00019474044,0.00007052308,0.00014149447,0.00022223253],"domain_scores_gemma":[0.9995298,0.00015755882,0.00012788286,0.000040956853,0.000032653898,0.00011116276],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012220888,0.000056692326,0.00012813581,0.000072827206,0.00028051308,0.00006127309,0.0002884722,0.000017789049,0.0001652801],"category_scores_gemma":[0.00013303837,0.000025127652,0.000034300017,0.00023494236,0.00079056155,0.00018978494,0.000004697815,0.000100280486,0.0000036548756],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010689432,0.000001758717,0.9947022,0.0000021354585,0.0000031223574,0.000024853614,0.0033087216,0.00016303181,5.8346524e-7,0.00012419056,0.000025131589,0.0016335888],"study_design_scores_gemma":[0.00017881682,0.00015081605,0.99406385,0.000018548355,0.0000069239322,0.00006606857,0.0035443895,0.0010219457,0.000008011349,0.00049106445,0.00041141835,0.00003813962],"about_ca_topic_score_codex":0.06937588,"about_ca_topic_score_gemma":0.8310027,"teacher_disagreement_score":0.7616268,"about_ca_system_score_codex":6.6206235e-7,"about_ca_system_score_gemma":0.0001149211,"threshold_uncertainty_score":0.9368212},"labels":[],"label_agreement":null},{"id":"W2023498075","doi":"10.1139/e04-106","title":"An 1800 km cross section of the lithosphere through the northwestern North American plate: lessons from 4.0 billion years of Earth's history","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Calgary","funders":"","keywords":"Lithosphere; Geology; Crust; Mantle (geology); Archean; Subduction; Geophysics; Proterozoic; Seismology; Earth science; Tectonics; Paleontology","score_opus":0.021661305420938328,"score_gpt":0.21921542883726802,"score_spread":0.1975541234163297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023498075","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99703795,0.0009590395,0.0000130444405,0.00095259724,0.00030566443,0.000044614982,0.0001073089,0.0000026822504,0.00057708187],"genre_scores_gemma":[0.99884003,0.000055197677,0.00052004895,0.00030147613,0.00019045784,1.10971285e-7,0.000006311865,0.0000014861156,0.0000849042],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986344,0.00012218453,0.00038394335,0.00018079138,0.0003941425,0.0002845653],"domain_scores_gemma":[0.9987801,0.00013477076,0.0004958018,0.00019129168,0.000135925,0.0002621501],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035109624,0.000101510275,0.00023575367,0.00006483352,0.0002336881,0.00005155515,0.00074238284,0.000039139613,0.001981736],"category_scores_gemma":[0.00006525251,0.000053744323,0.00015882179,0.0007108115,0.0018350064,0.00037810704,0.000008930332,0.00022918379,0.000011197463],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009165598,0.000008558603,0.9645754,0.0000014481053,0.000015623837,0.0000043291125,0.00077139086,0.023937624,0.000052361298,0.000009343489,0.000037737886,0.010577005],"study_design_scores_gemma":[0.00007377282,0.00021250169,0.98524076,0.000013903812,0.000024261564,0.000012494455,0.00041944967,0.0008549339,0.00024874276,0.00025890747,0.012562196,0.000078080215],"about_ca_topic_score_codex":0.31873876,"about_ca_topic_score_gemma":0.9545103,"teacher_disagreement_score":0.6357715,"about_ca_system_score_codex":0.000003826084,"about_ca_system_score_gemma":0.000552141,"threshold_uncertainty_score":0.9989306},"labels":[],"label_agreement":null},{"id":"W2023545886","doi":"10.1139/e02-091","title":"A new dicynodont therapsid from the lowermost Beaufort Group, Upper Permian of South Africa","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Paleontology; Geology; Permian; Group (periodic table); Sister group; Biology; Structural basin","score_opus":0.02807354815496745,"score_gpt":0.19311298133015956,"score_spread":0.1650394331751921,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023545886","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95963436,0.020775337,0.000076712546,0.0027597155,0.00097160315,0.00006959932,0.00012719806,0.0000036371364,0.015581863],"genre_scores_gemma":[0.998227,0.000071586604,0.0008041503,0.00040901089,0.00024891624,8.070457e-8,0.0000035156645,0.0000012094885,0.0002345408],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988319,0.00011114881,0.00029573293,0.00015176692,0.00021467006,0.00039472416],"domain_scores_gemma":[0.9989498,0.00020633289,0.0002110308,0.00012278122,0.000049723065,0.00046032568],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005076487,0.000103822,0.00019331285,0.00013810485,0.00045655796,0.00004018911,0.000668765,0.00007925396,0.007948008],"category_scores_gemma":[0.000097211974,0.000059943945,0.000105730105,0.0003280327,0.0009522537,0.00024475867,0.0000037857415,0.00019571699,0.000080818645],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009795745,0.000002751644,0.9903659,5.832422e-7,0.00002010914,0.000028344193,0.0023960401,0.00013830255,0.000011415722,0.00009318537,0.0012791761,0.0056543923],"study_design_scores_gemma":[0.0001609235,0.00033185756,0.9736546,0.00001959768,0.000014302749,0.0000960048,0.00096995215,0.0004648767,0.000004826511,0.0007099226,0.023489682,0.00008342501],"about_ca_topic_score_codex":0.02619728,"about_ca_topic_score_gemma":0.46071187,"teacher_disagreement_score":0.43451458,"about_ca_system_score_codex":0.0000014996783,"about_ca_system_score_gemma":0.00053110806,"threshold_uncertainty_score":0.99295884},"labels":[],"label_agreement":null},{"id":"W2023689016","doi":"10.1139/e06-068","title":"Geological evolution of the northwestern Superior Province: Clues from geology, kinematics, and geochronology in the Gods Lake Narrows area, Oxford–Stull terrane, Manitoba","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Toronto; University of Waterloo","funders":"","keywords":"Geology; Terrane; Geochronology; Zircon; Conglomerate; Volcanic rock; Lithology; Geochemistry; Tectonics; Shear zone; Sinistral and dextral; Thrust fault; Paleontology; Pebble; Pluton; Geomorphology; Volcano; Sedimentary rock","score_opus":0.012147617619479452,"score_gpt":0.1794534415077465,"score_spread":0.16730582388826706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023689016","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993711,0.0022304908,0.00001361106,0.0027370863,0.0001437528,0.00009770061,0.000052202227,0.0000021822466,0.001011998],"genre_scores_gemma":[0.99927723,0.000021918715,0.0003210587,0.00024823076,0.00009525435,4.5466766e-7,0.000008941554,7.59795e-7,0.000026133517],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99853617,0.00019040161,0.00045439045,0.0001927723,0.00025021442,0.00037607635],"domain_scores_gemma":[0.99917674,0.00025239176,0.00023693552,0.00012611662,0.000071283386,0.00013651612],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00064517616,0.00012505057,0.0002792731,0.00014299463,0.00027600955,0.000061060855,0.0006852824,0.00009768326,0.001409254],"category_scores_gemma":[0.00013625504,0.00005820561,0.000094945666,0.00039094896,0.0020224312,0.00015821353,0.000018449931,0.0002515354,0.000004243983],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000064426886,0.000009482478,0.99731475,0.0000036401595,0.0000061911187,0.000032816664,0.000120625504,0.0018011642,0.000024236977,0.0000931428,0.000029982124,0.00055753853],"study_design_scores_gemma":[0.00014094278,0.00021573415,0.9820688,0.000020722411,0.000021142976,0.00011401473,0.0009897646,0.0015835072,0.00002423757,0.013980268,0.00076058536,0.00008031392],"about_ca_topic_score_codex":0.27148423,"about_ca_topic_score_gemma":0.9919224,"teacher_disagreement_score":0.7204382,"about_ca_system_score_codex":0.0000028157879,"about_ca_system_score_gemma":0.0003517601,"threshold_uncertainty_score":0.9995036},"labels":[],"label_agreement":null},{"id":"W2024122802","doi":"10.1139/cjes-2014-0195","title":"Additions to the Eocene Perissodactyla of the Margaret Formation, Eureka Sound Group, Ellesmere Island, Arctic Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"National Science Foundation","keywords":"Arctic; Geology; Paleontology; Bay; Range (aeronautics); Sound (geography); Biological dispersal; Group (periodic table); Oceanography; Latitude; Fjord; Physical geography; Geography; Population","score_opus":0.02934414417292222,"score_gpt":0.20913148551451724,"score_spread":0.17978734134159502,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024122802","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93697494,0.003491251,0.00009538764,0.040290788,0.0023528233,0.00020420559,0.0005631637,0.0000029107453,0.016024498],"genre_scores_gemma":[0.99807525,0.000016960677,0.00008821025,0.0015831657,0.00010683268,3.1888743e-7,0.000003016415,8.947548e-7,0.00012532478],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988081,0.0001282438,0.0002615129,0.00008104097,0.0004465794,0.00027452072],"domain_scores_gemma":[0.99883723,0.000111153655,0.00019527046,0.000109986744,0.00033117196,0.00041516943],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00083942025,0.00007830155,0.00012889075,0.000097387434,0.0007954987,0.000058256293,0.0005248913,0.000024504328,0.00058700814],"category_scores_gemma":[0.00048695866,0.00004083644,0.00004907146,0.0004985888,0.00046021977,0.00021096163,0.0000063565412,0.00014253255,0.000011245752],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000054897237,0.0000017657319,0.9313047,0.0000033918436,0.000014533084,0.000007245897,0.0012277408,0.0028655233,3.6313875e-7,0.00014814174,0.06400707,0.0004140544],"study_design_scores_gemma":[0.00010494922,0.000106898005,0.873765,0.000028415589,0.000012244922,0.00014004442,0.0040705586,0.00023474958,0.000003253498,0.00032778436,0.121144414,0.000061675855],"about_ca_topic_score_codex":0.5875633,"about_ca_topic_score_gemma":0.9999265,"teacher_disagreement_score":0.41236323,"about_ca_system_score_codex":0.000008566159,"about_ca_system_score_gemma":0.0028612122,"threshold_uncertainty_score":0.64273274},"labels":[],"label_agreement":null},{"id":"W2024422779","doi":"10.1139/e09-028","title":"Geoelectric structure of the northeastern Williston basin and underlying Precambrian lithosphereEarth Science Sector (ESS) Contribution 20080509.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Manitoba; Geological Survey of Canada","funders":"","keywords":"Geology; Craton; Precambrian; Magnetotellurics; Terrane; Paleozoic; Lithosphere; Structural basin; Paleontology; Archean; Proterozoic; Petrology; Tectonics; Electrical resistivity and conductivity","score_opus":0.015863609760956285,"score_gpt":0.2274574040266506,"score_spread":0.2115937942656943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024422779","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968751,0.0012727099,0.000120989236,0.0007448064,0.00035939785,0.00011245871,0.000027813401,0.000002948316,0.00048377356],"genre_scores_gemma":[0.9988189,0.000014314242,0.0007819077,0.00024939675,0.00008509288,3.3677754e-8,6.1075207e-7,0.0000012135209,0.000048554462],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982437,0.00014375584,0.00031477236,0.00021968503,0.00053629116,0.00054180133],"domain_scores_gemma":[0.99863064,0.00014233003,0.00029254897,0.00012271715,0.00024295025,0.0005688242],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00084337144,0.00012807547,0.00024400419,0.00022313268,0.0007414588,0.00018770072,0.000580657,0.00005277767,0.0001876752],"category_scores_gemma":[0.00048518364,0.00007602761,0.00007463441,0.0020347275,0.0010344245,0.0005161544,0.000005976768,0.0002661609,0.00000192158],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021389968,0.0000097772545,0.7363855,0.000008530431,0.000008693382,0.000010090127,0.0002605524,0.0019487712,0.002299047,0.0008111717,0.000012302176,0.25822413],"study_design_scores_gemma":[0.0001470461,0.0005671079,0.9895403,0.000040978954,0.000013205658,0.00008739655,0.00004430792,0.0024622653,0.0017350226,0.004833076,0.0004261341,0.000103173494],"about_ca_topic_score_codex":0.009784428,"about_ca_topic_score_gemma":0.09591441,"teacher_disagreement_score":0.25812095,"about_ca_system_score_codex":0.0000043455625,"about_ca_system_score_gemma":0.0015072171,"threshold_uncertainty_score":0.9968095},"labels":[],"label_agreement":null},{"id":"W2024425463","doi":"10.1139/e06-051","title":"Archean geochronological framework of the Bighorn Mountains, Wyoming","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Northwestern University","keywords":"Geology; Batholith; Gneiss; Archean; Zircon; Geochemistry; Plutonism; Crust; Basement; Diorite; Geochronology; Precambrian; Sill; Metamorphic rock; Paleontology; Pluton; Tectonics; Archaeology","score_opus":0.015143081820758506,"score_gpt":0.1959567286868272,"score_spread":0.1808136468660687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024425463","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9906359,0.0011870426,0.00005843513,0.0021571722,0.00021928786,0.00003031187,0.000015191781,0.0000023579873,0.005694336],"genre_scores_gemma":[0.99760246,0.000009684726,0.0019127346,0.00024433606,0.0001612768,5.709306e-8,0.0000012129542,6.242424e-7,0.000067622226],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987735,0.00006625499,0.00034091627,0.00013492459,0.00030940815,0.0003749572],"domain_scores_gemma":[0.99912256,0.00020077037,0.00022039536,0.000100166464,0.0000883566,0.0002677366],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005998452,0.00008852509,0.0001971108,0.00013765134,0.00034637784,0.000062509054,0.0006505134,0.00006855419,0.003955468],"category_scores_gemma":[0.0003147535,0.000044497152,0.00016683675,0.0007217061,0.0011694052,0.00011609819,0.000009597454,0.00025597637,0.000019669586],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000028382735,0.0000045238426,0.9920925,0.0000022444835,0.000006235508,0.000013569864,0.000027372787,0.0047969623,0.00011075796,0.0010490584,0.00006988885,0.0018240747],"study_design_scores_gemma":[0.000046775815,0.00011809487,0.9298891,0.000027330927,0.000013500698,0.000042311545,0.00012614511,0.00056577433,0.00067718193,0.06625578,0.0021666393,0.000071401955],"about_ca_topic_score_codex":0.05759562,"about_ca_topic_score_gemma":0.40929052,"teacher_disagreement_score":0.3516949,"about_ca_system_score_codex":0.0000015271157,"about_ca_system_score_gemma":0.0004448514,"threshold_uncertainty_score":0.99695504},"labels":[],"label_agreement":null},{"id":"W2024670219","doi":"10.1139/e00-043","title":"Geology and U-Pb geochronology of the Island Lake greenstone belt, northwestern Superior Province, Manitoba","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Innovation, Science and Economic Development Canada","funders":"","keywords":"Zircon; Geology; Greenstone belt; Geochronology; Geochemistry; Archean; Detritus; Population; Provenance; Sedimentary depositional environment; Sedimentary rock; Paleontology; Structural basin","score_opus":0.008792695177993456,"score_gpt":0.17004707669985344,"score_spread":0.16125438152186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024670219","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994459,0.0013347766,0.0000026794157,0.0010801877,0.000113117756,0.00005061351,0.00004730596,0.0000017306003,0.0029105989],"genre_scores_gemma":[0.9990319,0.000064226515,0.00016197664,0.0003366608,0.000068930596,1.0011816e-7,0.0000031733384,7.939277e-7,0.00033222645],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989227,0.00007579848,0.00030040788,0.00016391084,0.0001800916,0.00035705828],"domain_scores_gemma":[0.9993026,0.00008250656,0.00013569606,0.0000978485,0.00006717721,0.00031417536],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00030329564,0.0000995832,0.0002417785,0.00012143011,0.00028578634,0.000038403436,0.00044069267,0.000063294,0.011457688],"category_scores_gemma":[0.00004302192,0.000054634944,0.00008415743,0.00033291016,0.0017872609,0.0001539693,0.000009200257,0.00016553166,0.000023975856],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006751178,0.000003239772,0.98786765,0.000003490151,0.000011389902,0.000033418604,0.000057363693,0.00058638124,0.00002197792,0.00001677394,0.00002729154,0.011364278],"study_design_scores_gemma":[0.00013000317,0.00028247587,0.9927651,0.000012094098,0.000020260512,0.00032546313,0.00010902522,0.0002926609,0.000053840555,0.0011715149,0.0047608707,0.00007665213],"about_ca_topic_score_codex":0.13922079,"about_ca_topic_score_gemma":0.9953014,"teacher_disagreement_score":0.8560806,"about_ca_system_score_codex":7.1288105e-7,"about_ca_system_score_gemma":0.00045755124,"threshold_uncertainty_score":0.989446},"labels":[],"label_agreement":null},{"id":"W2024876120","doi":"10.1139/e00-024","title":"Cretaceous-Tertiary palynofloral perturbations and extinctions within the <i>Aquilapollenites</i> Phytogeographic Province","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; Geological Survey of Canada","funders":"","keywords":"Geology; Paleontology; Extinction event; Diachronous; Sedimentary depositional environment; Cretaceous; Vegetation (pathology); Earth science; Physical geography; Ejecta; Biological dispersal; Structural basin; Geography","score_opus":0.018036459049695697,"score_gpt":0.21019141254921309,"score_spread":0.1921549534995174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024876120","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95357543,0.014317784,0.000056806206,0.0033451107,0.00057220896,0.00009483017,0.00002408959,0.0000066186544,0.028007133],"genre_scores_gemma":[0.9988862,0.00015282177,0.0003842439,0.00036275908,0.00012421209,3.583275e-7,8.389742e-7,6.5473876e-7,0.00008787156],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998892,0.00011723117,0.00028115706,0.00015696368,0.0002116652,0.000340995],"domain_scores_gemma":[0.9989893,0.00018796413,0.0001933919,0.00010307962,0.00007340079,0.00045287362],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0007910634,0.00011162742,0.00013559309,0.0003144666,0.0014944361,0.00022389517,0.00037403876,0.000055615827,0.00039688498],"category_scores_gemma":[0.00010279891,0.000068354464,0.00008264286,0.0005943041,0.0015972592,0.0005543358,0.0000011265029,0.00025462947,0.0000048152215],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005721958,0.0000026115872,0.9899143,0.00000135053,0.000015408452,0.00006525166,0.0003403233,0.00018089029,0.000008778307,0.00016845723,0.00010491948,0.0091920085],"study_design_scores_gemma":[0.000109598746,0.00020132298,0.9915018,0.000014812723,0.00002273576,0.0009651835,0.0006372142,0.0009732337,0.000009946183,0.0013404612,0.004125688,0.000097978744],"about_ca_topic_score_codex":0.004153125,"about_ca_topic_score_gemma":0.6726226,"teacher_disagreement_score":0.6684695,"about_ca_system_score_codex":5.5044563e-7,"about_ca_system_score_gemma":0.0010234476,"threshold_uncertainty_score":0.9998055},"labels":[],"label_agreement":null},{"id":"W2025050632","doi":"10.1139/e00-010","title":"The paleomagnetic significance of new U-Pb age data from the Molson dyke swarm, Cauchon Lake area, Manitoba","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; College of Family Physicians of Canada","funders":"University of Alberta","keywords":"Geology; Zircon; Paleomagnetism; Baddeleyite; Apparent polar wander; Rift; Precambrian; Craton; Geochemistry; Geochronology; Large igneous province; Gondwana; Paleontology; Terrane; Tectonics; Magmatism","score_opus":0.04401424282892481,"score_gpt":0.20468286282040588,"score_spread":0.16066861999148108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025050632","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9851979,0.005096842,0.000009647851,0.0042207455,0.00019628424,0.000070312846,0.00023163231,0.0000025581837,0.004974068],"genre_scores_gemma":[0.9979516,0.00032641427,0.0003576618,0.00042883924,0.00022445265,1.18470616e-7,0.000026307067,9.970256e-7,0.00068359415],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984935,0.000101269114,0.00036863415,0.00022280625,0.00041512042,0.00039870723],"domain_scores_gemma":[0.9983514,0.0005490219,0.00018802166,0.000331531,0.000057583693,0.00052243663],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00076447806,0.00011780662,0.00020714078,0.00004621455,0.0005472626,0.000211881,0.0019290037,0.000041115545,0.01233846],"category_scores_gemma":[0.00024351124,0.000052730866,0.0000898103,0.0005413516,0.00095715246,0.00021835705,0.0000119105225,0.00021282517,0.00006756524],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002560118,0.000006628455,0.91845083,0.0000020765476,0.0000374529,0.00011142912,0.00022771137,0.004597858,0.00006743144,0.000014725072,0.0053904196,0.07106781],"study_design_scores_gemma":[0.00012126915,0.00019334808,0.90447474,0.00002691275,0.00004527264,0.000022737495,0.0004972199,0.0016664381,0.00010883775,0.006616073,0.08611504,0.00011214467],"about_ca_topic_score_codex":0.21747187,"about_ca_topic_score_gemma":0.9828282,"teacher_disagreement_score":0.7653563,"about_ca_system_score_codex":8.0696594e-7,"about_ca_system_score_gemma":0.0005868937,"threshold_uncertainty_score":0.9885644},"labels":[],"label_agreement":null},{"id":"W2025087653","doi":"10.1139/e05-057","title":"Neoarchean decoupling of upper- and mid-crustal tectonothermal domains in the southeast Slave Province: evidence from the Walmsley Lake area","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Government of Saskatchewan; Geological Survey of Canada; Government of Northwest Territories","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Greenschist; Metamorphic facies; Outcrop; Crust; Metamorphic rock; Geochemistry; Facies; Tectonics; Petrology; Geomorphology; Paleontology","score_opus":0.02418216787652172,"score_gpt":0.20955718681460753,"score_spread":0.1853750189380858,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025087653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891505,0.0029420487,0.000019031515,0.0069071776,0.000046312245,0.000069186266,0.00005113259,0.0000013679963,0.0008132105],"genre_scores_gemma":[0.9987013,0.000052309617,0.0007092503,0.0003944748,0.00012532691,1.961443e-7,0.0000018096177,8.45762e-7,0.0000144853075],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987315,0.00010563508,0.00032293325,0.00016384768,0.00033018805,0.00034592854],"domain_scores_gemma":[0.9987347,0.00068517716,0.00016925037,0.00010518006,0.000054126223,0.00025155843],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013859583,0.000101137004,0.0001814898,0.00010396739,0.00031023557,0.0001245575,0.0006749545,0.00003986981,0.0019187002],"category_scores_gemma":[0.0003399383,0.000046137404,0.00008371418,0.00041376636,0.0010247992,0.00026476878,0.000012334524,0.00024751129,0.000008762379],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011327626,0.000003888036,0.98332566,0.000001732448,0.000006876035,0.00001694294,0.001059206,0.0040425174,0.00007059835,0.000016363389,0.000013266274,0.011431602],"study_design_scores_gemma":[0.0001277095,0.00014641671,0.9869154,0.000083662766,0.000020026064,0.000053978492,0.0028777171,0.006916202,0.00020562505,0.0017090449,0.00085437123,0.00008982316],"about_ca_topic_score_codex":0.04183921,"about_ca_topic_score_gemma":0.9026775,"teacher_disagreement_score":0.8608383,"about_ca_system_score_codex":0.0000013882945,"about_ca_system_score_gemma":0.0005181954,"threshold_uncertainty_score":0.9989937},"labels":[],"label_agreement":null},{"id":"W2025196985","doi":"10.1139/e04-038","title":"Geochemistry of North Shore Hypabyssal dikes and sills in the Midcontinent Rift of Minnesota: an example the 47th Avenue sill","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Sill; Geology; Dike; Geochemistry; Shore; Basalt; Rift; Volcano; Igneous rock; Petrology; Geomorphology; Tectonics; Paleontology; Oceanography","score_opus":0.024719476417191154,"score_gpt":0.2097722252193432,"score_spread":0.18505274880215203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025196985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944177,0.0005349258,0.00013994535,0.0041499226,0.000082380786,0.000050369483,0.000005406257,0.0000012311286,0.00061811914],"genre_scores_gemma":[0.998957,0.00001447426,0.0008216469,0.00014342238,0.000047942962,6.507673e-7,4.4855102e-7,7.7453296e-7,0.000013640762],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99897593,0.000049857448,0.00030608114,0.00015735143,0.00025425918,0.00025649113],"domain_scores_gemma":[0.9990816,0.00012531677,0.00026368324,0.00023421201,0.00013885286,0.00015630045],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010847279,0.000086243745,0.00016096186,0.000081398146,0.00016263901,0.00007483521,0.0012024812,0.000028244298,0.000008160903],"category_scores_gemma":[0.00022059401,0.000049825907,0.00004572715,0.0004590063,0.0006917085,0.0002712283,0.000027806951,0.0001588199,1.8775613e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009812452,0.000101623824,0.93408626,0.000090297064,0.000027310452,0.00024962213,0.033106696,0.015531542,0.005298152,0.00461126,0.00016935171,0.006718084],"study_design_scores_gemma":[0.00045137474,0.00039749342,0.97021836,0.0001826601,0.000013224817,0.0004461375,0.0040270765,0.0009708984,0.011988974,0.0053036795,0.00580212,0.00019799575],"about_ca_topic_score_codex":0.0055916193,"about_ca_topic_score_gemma":0.06137296,"teacher_disagreement_score":0.055781346,"about_ca_system_score_codex":0.0000033950173,"about_ca_system_score_gemma":0.0006782908,"threshold_uncertainty_score":0.9557545},"labels":[],"label_agreement":null},{"id":"W2025262434","doi":"10.1139/e04-052","title":"Coupled fluid flow, heat and mass transport, and erosion in the Alberta basin: implications for the origin of the Athabasca oil sands","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Calgary","funders":"","keywords":"Geology; Aquifer; Oil sands; Structural basin; Permeability (electromagnetism); Hydrology (agriculture); Geomorphology; Deposition (geology); Petrology; Geochemistry; Groundwater; Geotechnical engineering","score_opus":0.01703769202136805,"score_gpt":0.22515938217566983,"score_spread":0.2081216901543018,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025262434","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9848993,0.0013886507,0.0015200226,0.011738285,0.00009443651,0.0000695776,0.000011391824,0.000001305911,0.00027703095],"genre_scores_gemma":[0.99934334,0.00032644064,0.0001502073,0.00012701974,0.000025195044,0.0000029790592,4.887181e-7,0.0000026588348,0.000021702286],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9995295,0.000015511216,0.0001757847,0.000056748115,0.00009994947,0.00012255248],"domain_scores_gemma":[0.99965435,0.00009676192,0.000028447945,0.000090297974,0.00003483385,0.00009528664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045415256,0.00005246967,0.00009247139,0.00009220656,0.00024751996,0.000050245413,0.00022641326,0.000021387013,0.000009434785],"category_scores_gemma":[0.000035159137,0.00002441152,0.000050568455,0.00039032282,0.00020999706,0.00013059158,0.0000018374224,0.00007406881,1.11886834e-7],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011704861,0.000014928446,0.23462851,0.00005443489,0.00007288228,0.000004243783,0.010282715,0.7438041,0.007308874,0.0021782946,0.0002219899,0.0014173152],"study_design_scores_gemma":[0.0014773491,0.00020110144,0.55687165,0.0002436772,0.00015469821,0.000114736366,0.0034730393,0.4200326,0.0015566841,0.0017556626,0.013851854,0.00026693873],"about_ca_topic_score_codex":0.005982285,"about_ca_topic_score_gemma":0.40193784,"teacher_disagreement_score":0.39595556,"about_ca_system_score_codex":0.0000057182897,"about_ca_system_score_gemma":0.00023644463,"threshold_uncertainty_score":0.9043465},"labels":[],"label_agreement":null},{"id":"W2025440381","doi":"10.1139/e07-049","title":"Desquamatia and related atrypid brachiopods from the Frasnian (Upper Devonian) of Bergisches Land, GermanyThis article is one of a selection of papers published in this Special Issue on the theme <i>The dynamic reef and shelly communities of the Paleozoic</i>. <i>This Special is in honour of our colleague and friend Paul Copper</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Devonian; Geology; Massif; Paleontology; Whorl (mollusc); Fauna; Biology; Botany","score_opus":0.012789694997804194,"score_gpt":0.1993597214121516,"score_spread":0.18657002641434742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025440381","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98617214,0.0023824414,1.8646372e-7,0.0040329457,0.00015956211,0.00016206747,0.00017058074,7.4869826e-7,0.0069193356],"genre_scores_gemma":[0.99918246,0.00046982203,0.00009456377,0.0001367789,0.00008746405,3.7316127e-7,7.598173e-7,0.0000014113134,0.000026364787],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982017,0.0004800498,0.00062015915,0.00013093062,0.00033744978,0.00022965405],"domain_scores_gemma":[0.9984044,0.00067220593,0.0005694003,0.00015514514,0.00009542069,0.00010344634],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014143306,0.00012656901,0.00036841678,0.00020193991,0.00046170084,0.000036755166,0.0004439964,0.00010526169,0.0014333451],"category_scores_gemma":[0.00018216197,0.00006784339,0.00007681955,0.00067697477,0.0023575267,0.00027453847,0.000007880667,0.00041564737,3.0444053e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007875856,0.000016651513,0.97218245,0.000011377453,0.000038578946,0.0000035992207,0.02495894,0.000031443873,0.00023276317,0.00002884476,0.00025163294,0.0021649655],"study_design_scores_gemma":[0.0004091515,0.00032795747,0.98820907,0.00016804805,0.000023466504,0.000055783217,0.008734277,0.00050414784,0.00087096076,0.00045186607,0.0001724568,0.000072841256],"about_ca_topic_score_codex":0.03565545,"about_ca_topic_score_gemma":0.75360614,"teacher_disagreement_score":0.7179507,"about_ca_system_score_codex":0.0000024145124,"about_ca_system_score_gemma":0.00047953462,"threshold_uncertainty_score":0.9994795},"labels":[],"label_agreement":null},{"id":"W2025755882","doi":"10.1139/e00-028","title":"Late Paleozoic to Cenozoic history of the offshore Sydney Basin, Atlantic Canada","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Dalhousie University","funders":"Killam Trusts; Dalhousie University; Natural Sciences and Engineering Research Council of Canada; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Geology; Carboniferous; Terrane; Permian; Onlap; Paleontology; Paleozoic; Unconformity; Inversion (geology); Outcrop; Devonian; Basement; Structural basin; Thermal subsidence; Cretaceous; Sedimentary basin; Subsidence; Tectonics","score_opus":0.015053241378287908,"score_gpt":0.16739499330127286,"score_spread":0.15234175192298496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025755882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9772521,0.001480193,2.989742e-7,0.003351218,0.000772354,0.000056677185,0.000021928312,0.0000014415367,0.01706374],"genre_scores_gemma":[0.9944472,0.000033516415,0.000052600983,0.001610896,0.00009354767,9.089466e-8,5.835711e-7,8.57711e-7,0.003760741],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987759,0.000066668275,0.00026104157,0.00013055802,0.00037476624,0.00039109154],"domain_scores_gemma":[0.9990605,0.000095609634,0.000108562526,0.00009449134,0.00008118926,0.00055962015],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00028251164,0.00009698807,0.00021272841,0.000052383446,0.00025928774,0.000022569384,0.00058026536,0.000025487332,0.0066258055],"category_scores_gemma":[0.00011906698,0.00005249633,0.00008014707,0.00041314363,0.0005394746,0.000093816714,0.0000055289634,0.00013783334,0.000066108514],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006228882,0.0000027877388,0.9816738,0.000004879116,0.000009129249,0.000032843764,0.0002001937,0.00339758,0.0000023600246,0.000024087823,0.0050643785,0.009581761],"study_design_scores_gemma":[0.00004415669,0.00013741315,0.8002552,0.000028460043,0.0000072583694,0.000015036196,0.00005769413,0.000078069716,0.00000654022,0.00019311845,0.19911088,0.00006621999],"about_ca_topic_score_codex":0.88801825,"about_ca_topic_score_gemma":0.9968357,"teacher_disagreement_score":0.1940465,"about_ca_system_score_codex":0.00000864731,"about_ca_system_score_gemma":0.0028931457,"threshold_uncertainty_score":0.99428225},"labels":[],"label_agreement":null},{"id":"W2025756787","doi":"10.1139/e03-002","title":"The Touquoy Zone deposit: an example of \"unusual\" orogenic gold mineralisation in the Meguma Terrane, Nova Scotia, Canada","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Arsenopyrite; Mylonite; Metamorphic rock; Pyrite; Lode; Mesothermal; Shear zone; Terrane; Carbonate; Hypogene; Mineralogy; Quartz; Fluid inclusions; Sphalerite; Chalcopyrite; Paleontology; Tectonics","score_opus":0.03498247456694747,"score_gpt":0.2012382583109707,"score_spread":0.16625578374402322,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025756787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938153,0.0015215768,0.0000069894845,0.0015810648,0.00019414144,0.00005251475,0.0000110630735,7.453834e-7,0.0028165902],"genre_scores_gemma":[0.9990371,0.000014345486,0.0002879967,0.0005567473,0.00004175276,1.05237355e-7,0.000004221995,7.612636e-7,0.00005696865],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99843633,0.0002309019,0.00038384603,0.00014333913,0.00043164892,0.00037393952],"domain_scores_gemma":[0.9989959,0.00028152467,0.00018300506,0.00013328082,0.000095327116,0.00031097746],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014677987,0.000092748385,0.00016568735,0.000106852145,0.00025172715,0.00010762331,0.00064459426,0.000032246455,0.001159015],"category_scores_gemma":[0.00020806909,0.000045162607,0.00006387377,0.0008366211,0.00042536083,0.00020776657,0.0000024630206,0.00016450556,0.0000040874197],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000053918984,0.0000067283117,0.9921742,0.0000027903432,0.000011503292,0.000041718667,0.00040271715,0.0032388787,0.00010835508,0.00050587405,0.00029391513,0.0032079425],"study_design_scores_gemma":[0.00014419331,0.00025151472,0.98875177,0.000013705998,0.000019523139,0.00014007882,0.001895412,0.00067014666,0.000543259,0.0019015322,0.005559111,0.00010973637],"about_ca_topic_score_codex":0.9891391,"about_ca_topic_score_gemma":0.99993783,"teacher_disagreement_score":0.0107987635,"about_ca_system_score_codex":0.0000033529416,"about_ca_system_score_gemma":0.0012555064,"threshold_uncertainty_score":0.9997541},"labels":[],"label_agreement":null},{"id":"W2025839133","doi":"10.1139/e04-037","title":"Late Pleistocene stratigraphy and chronology of lower Chehalis River valley, southwestern British Columbia: evidence for a restricted Coquitlam Stade","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of British Columbia; Ministry of Environment; Simon Fraser University","funders":"","keywords":"Geology; Glacial period; Pleistocene; Glacier; Deglaciation; Radiocarbon dating; Fluvial; Chronology; Holocene; Glacial lake; River terraces; Paleontology; Quaternary; Moraine; Physical geography; Geomorphology; Geography","score_opus":0.03957606013586632,"score_gpt":0.25188802280020633,"score_spread":0.21231196266434002,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025839133","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944653,0.0041928543,0.00003392577,0.00052471535,0.00026551337,0.0001670599,0.000095644355,0.0000030918472,0.00025190393],"genre_scores_gemma":[0.9982384,0.00025651185,0.0012914144,0.000091550035,0.00004286128,6.511166e-7,0.0000036555723,0.000001688906,0.000073275136],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99864936,0.00009043262,0.00034603008,0.0002178664,0.00019579902,0.0005005334],"domain_scores_gemma":[0.99870557,0.00031996745,0.0002306577,0.00009073336,0.00020658955,0.00044650587],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007025918,0.00008286396,0.00027300004,0.00023188934,0.0004212829,0.00015211134,0.00039492,0.00012846758,0.00047217152],"category_scores_gemma":[0.00031736176,0.000092536684,0.0000746278,0.0004036796,0.0025357383,0.00037273276,0.0000064162145,0.00020128871,0.000004371758],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032493546,0.000005506424,0.9983923,0.00001975049,0.000021926931,0.00017177053,0.00021218676,0.00056779914,0.000011935016,0.000025063877,0.00004547337,0.0004937827],"study_design_scores_gemma":[0.0005292948,0.0016990829,0.9937773,0.00013096498,0.00002019459,0.000657683,0.00014398649,0.00006468787,0.000014368748,0.0027040148,0.00016154768,0.000096890166],"about_ca_topic_score_codex":0.19363035,"about_ca_topic_score_gemma":0.9875144,"teacher_disagreement_score":0.79388404,"about_ca_system_score_codex":9.1122064e-7,"about_ca_system_score_gemma":0.0019997524,"threshold_uncertainty_score":0.93430334},"labels":[],"label_agreement":null},{"id":"W2025912731","doi":"10.1139/cjes-2013-0184","title":"Geochronology and structural setting of Latest Devonian – Early Carboniferous magmatic rocks, Cape Kiber, northeast Russia","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Carboniferous; Devonian; Late Devonian extinction; Geochemistry; Zircon; Paleontology; Geochronology; Metamorphism; Chemostratigraphy; Conglomerate; Paleozoic; Cretaceous; Sedimentary rock","score_opus":0.012960423539032602,"score_gpt":0.19136507588630491,"score_spread":0.17840465234727232,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025912731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99453974,0.0014787653,0.0000045445886,0.0014008929,0.00016856949,0.000036763286,0.000020351497,0.0000030294964,0.002347363],"genre_scores_gemma":[0.9987446,0.00000852515,0.0010493287,0.00010493953,0.000067043686,7.133577e-8,0.0000032370353,0.0000011517468,0.000021066475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99871725,0.000071228686,0.00036833878,0.00016645147,0.00025704553,0.00041967555],"domain_scores_gemma":[0.99854565,0.00009008634,0.0002512578,0.00007563664,0.0001469807,0.0008904079],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00050867675,0.00011833662,0.00029463743,0.00021878816,0.00020210548,0.00008310698,0.00032533612,0.000060049868,0.0010757302],"category_scores_gemma":[0.00021176523,0.00007760107,0.000061277,0.00044519937,0.0006406217,0.00023594983,0.000009915934,0.0001719341,0.000014548472],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004546976,0.0000012506139,0.99539846,0.000005223318,0.000012787439,0.000036733818,0.00036856587,0.0019122754,0.000011160063,0.000023004997,0.000009686623,0.0022163133],"study_design_scores_gemma":[0.00015317337,0.0003577941,0.98974925,0.000018391662,0.000023884113,0.00029070541,0.00035037313,0.0039374894,0.000045224104,0.0048517813,0.00011475214,0.000107179265],"about_ca_topic_score_codex":0.11813293,"about_ca_topic_score_gemma":0.67684734,"teacher_disagreement_score":0.5587144,"about_ca_system_score_codex":0.000001954771,"about_ca_system_score_gemma":0.0006764703,"threshold_uncertainty_score":0.9998374},"labels":[],"label_agreement":null},{"id":"W2025916598","doi":"10.1139/e06-044","title":"New high-precision U–Pb ages for the Island Lake greenstone belt, northwestern Superior Province: implications for regional stratigraphy and the extent of the North Caribou terrane","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Toronto; University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Terrane; Geology; Greenstone belt; Archean; Paleontology; Craton; Sedimentary rock; Geochemistry; Shear zone; Lithology; Pluton; Stratigraphy; Tectonics","score_opus":0.015530867668054135,"score_gpt":0.2009626094032628,"score_spread":0.18543174173520865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025916598","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9821432,0.0026503173,0.0006472175,0.013602266,0.000112903625,0.00032620158,0.00044670864,0.0000013892669,0.00006974847],"genre_scores_gemma":[0.9986146,0.000051718933,0.0007756971,0.0002485771,0.00015123734,0.0000020218974,0.000022113758,9.869448e-7,0.00013304214],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990406,0.000041592943,0.00031520994,0.00015022853,0.00020745554,0.0002448844],"domain_scores_gemma":[0.9987532,0.0005814739,0.00022166592,0.00012916404,0.00013990178,0.00017460337],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046802495,0.00009559945,0.00018462467,0.00006909425,0.00077002076,0.00010943903,0.0005291839,0.000030926083,0.00012705586],"category_scores_gemma":[0.00006726614,0.00003682153,0.00018278156,0.00034002788,0.001109772,0.00012144779,0.0000073655433,0.00009260609,2.9888503e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000292129,0.0000035627654,0.9894275,0.0000044801463,0.000019140289,5.552863e-7,0.00007691655,0.0023085626,0.000022904638,0.0005472451,0.00055109523,0.0070088278],"study_design_scores_gemma":[0.00034716274,0.00015522038,0.9830831,0.000013394029,0.00006253805,0.000028102922,0.000081979284,0.00048354408,0.000020506712,0.012757885,0.002907593,0.000058958125],"about_ca_topic_score_codex":0.16360797,"about_ca_topic_score_gemma":0.99326795,"teacher_disagreement_score":0.82966,"about_ca_system_score_codex":6.950719e-7,"about_ca_system_score_gemma":0.00044585,"threshold_uncertainty_score":0.8419616},"labels":[],"label_agreement":null},{"id":"W2026129298","doi":"10.1139/e06-127","title":"Geochemistry of the Mesoproterozoic intrusive rocks of the Nipigon Embayment, northwestern Ontario: evaluating the earliest phases of rift development","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Lakehead University; Geological Survey of Canada","funders":"Northern Ontario Heritage Fund Corporation; Lakehead University","keywords":"Geology; Sill; Mafic; Ultramafic rock; Geochemistry; Rift; Petrology; Peridotite; Gabbro; Continental crust; Crust; Igneous rock; Basalt; Paleontology; Tectonics","score_opus":0.026700726898833328,"score_gpt":0.23177637652848052,"score_spread":0.2050756496296472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026129298","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966435,0.0005406739,0.000014145736,0.00045606884,0.00016948297,0.00009206703,0.000015438585,6.917252e-7,0.0020679687],"genre_scores_gemma":[0.99924886,0.0000036965434,0.0003776868,0.00017385882,0.000036654495,1.9508393e-7,0.0000012744205,7.8359665e-7,0.0001570139],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982218,0.00007487115,0.0006128578,0.00013221502,0.00064978865,0.00030844897],"domain_scores_gemma":[0.9983483,0.00025744032,0.0007399734,0.00016500501,0.00029864456,0.00019062636],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016193577,0.0001093566,0.00022572806,0.000070662085,0.00037991226,0.000028470091,0.0009823067,0.000044483608,0.0017283134],"category_scores_gemma":[0.00029970778,0.0000460366,0.00016463295,0.0005736715,0.0010436225,0.0001026546,0.0000304503,0.00022025107,0.0000014550204],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000132910645,0.000009648045,0.99136007,0.0000073484252,0.00003254976,0.0000025971622,0.0015743042,0.0021313012,0.000869083,0.000004463315,0.0000105401405,0.0039848294],"study_design_scores_gemma":[0.00013537086,0.00019565108,0.9517387,0.000101985046,0.00004722676,0.000032698197,0.0014156967,0.000113120695,0.044897944,0.00067026465,0.00057807815,0.000073223426],"about_ca_topic_score_codex":0.27196896,"about_ca_topic_score_gemma":0.9472673,"teacher_disagreement_score":0.67529833,"about_ca_system_score_codex":0.000005028837,"about_ca_system_score_gemma":0.0015509564,"threshold_uncertainty_score":0.99918425},"labels":[],"label_agreement":null},{"id":"W2026301559","doi":"10.1139/e00-009","title":"<sup>40</sup>Ar/<sup>39</sup>Ar and Pb-Pb study of individual hornblende and feldspar grains from southeastern Baffin Island glacial sediments: implications for the provenance of the Heinrich layers","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Princeton University; National Science Foundation","keywords":"Geology; Provenance; Archean; Geochemistry; Hornblende; Glacial period; Feldspar; Detritus; Continental crust; Crust; Paleontology; Quartz; Biotite","score_opus":0.027270412471803094,"score_gpt":0.24525255875983334,"score_spread":0.21798214628803025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026301559","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944746,0.0015276249,0.000011600712,0.0025619222,0.000079097794,0.00043905142,0.00045378064,0.0000018186755,0.00045050847],"genre_scores_gemma":[0.9994203,0.000086484244,0.0001529931,0.00015189016,0.000072966905,0.0000028964726,0.0000050381886,0.000002492976,0.00010497035],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983871,0.00023532915,0.00038297044,0.00024772304,0.00030402184,0.00044285174],"domain_scores_gemma":[0.9986341,0.0005690114,0.00022074256,0.00018973346,0.00010829845,0.00027811763],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012193925,0.00013617854,0.00027498062,0.00016308035,0.00089483534,0.00009128626,0.000758094,0.00008527465,0.00033301735],"category_scores_gemma":[0.00013187151,0.000079284895,0.0000593542,0.00039348233,0.001410268,0.0002350992,0.00001882286,0.00026347855,0.0000037016425],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046649096,0.000019168012,0.9876826,0.0000068371696,0.00006431685,0.0000032404128,0.0051545613,0.004239396,0.0000035796459,0.000029918452,0.0000771649,0.0026725747],"study_design_scores_gemma":[0.0006973856,0.0006649937,0.9891221,0.000029725888,0.00006057174,0.00006963119,0.005703551,0.0019251067,0.000014428339,0.00082287163,0.0007988439,0.00009079065],"about_ca_topic_score_codex":0.005988054,"about_ca_topic_score_gemma":0.37228766,"teacher_disagreement_score":0.3662996,"about_ca_system_score_codex":6.320303e-7,"about_ca_system_score_gemma":0.0007418132,"threshold_uncertainty_score":0.90521866},"labels":[],"label_agreement":null},{"id":"W2026361809","doi":"10.1139/e09-030","title":"Comparative anatomy of selected basal ceratopsian dentitions","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Canadian Museum of Nature","funders":"","keywords":"Basal (medicine); Ridge; Enamel paint; Dentistry; Anatomy; Dental anatomy; Geology; Orthodontics; Biology; Medicine; Paleontology","score_opus":0.022138721963117603,"score_gpt":0.25528457628336987,"score_spread":0.23314585432025225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026361809","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9786775,0.0016640179,0.000053466374,0.0010756598,0.00033072382,0.00003684341,0.000041797273,0.0000025332226,0.01811745],"genre_scores_gemma":[0.99858445,0.000014436945,0.0010843897,0.00020659858,0.000059308746,3.2833515e-8,0.000005748954,2.7800772e-7,0.00004477976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99917775,0.00009599365,0.00024069932,0.00009422614,0.0001202398,0.00027106697],"domain_scores_gemma":[0.9992297,0.000067581524,0.00015931555,0.000046705598,0.00017587144,0.00032080596],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00033159187,0.00006503632,0.00018382425,0.00032114613,0.00032985758,0.000022541626,0.00027281907,0.000051918832,0.0014551483],"category_scores_gemma":[0.000058912206,0.00005098562,0.000045020108,0.0006566889,0.0006930667,0.00029894093,7.753394e-7,0.00012682864,0.000024524192],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008876952,0.0000054131797,0.9969159,9.21902e-7,0.000011603127,0.000036184643,0.0002178373,0.0007935825,0.000061079925,0.00084025046,0.00057991175,0.00052846153],"study_design_scores_gemma":[0.000105475905,0.0004917554,0.9943791,0.000012228736,0.0000072941302,0.000179872,0.0002070188,0.0005301594,0.00011701669,0.0023298329,0.001580489,0.000059753973],"about_ca_topic_score_codex":0.0033227585,"about_ca_topic_score_gemma":0.47601455,"teacher_disagreement_score":0.47269177,"about_ca_system_score_codex":0.0000011460519,"about_ca_system_score_gemma":0.0014033217,"threshold_uncertainty_score":0.99945766},"labels":[],"label_agreement":null},{"id":"W2026502981","doi":"10.1139/e03-021","title":"Silurian deformation and metamorphism of Ordovician arc rocks of the Casco Bay Group, south-central Maine","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Ordovician; Metamorphism; Devonian; Carboniferous; Paleontology; Volcanic rock; Transpression; Dalradian; Greenschist; Terrane; Allochthon; Geochemistry; Sinistral and dextral; Volcano; Fault (geology); Tectonics; Nappe; Structural basin","score_opus":0.011013488433567154,"score_gpt":0.1670344028306972,"score_spread":0.15602091439713006,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026502981","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996224,0.00087916065,0.0000534468,0.00054141745,0.00014402854,0.000040784787,0.000024325365,8.276186e-7,0.0020920397],"genre_scores_gemma":[0.9992544,0.000015859674,0.0005187276,0.00015640301,0.000024939107,4.96618e-8,0.0000013227155,5.7313736e-7,0.000027712555],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989007,0.000095797055,0.0003511485,0.00009569092,0.00026508546,0.00029155193],"domain_scores_gemma":[0.9991074,0.00006346979,0.0002962231,0.00007408682,0.00008419808,0.00037460995],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006534877,0.00007881774,0.00020330602,0.0001483304,0.00021559802,0.000033005217,0.00027648103,0.000037239548,0.0017380153],"category_scores_gemma":[0.00023623499,0.000041897434,0.000106606065,0.0005608367,0.0006089645,0.00019330083,0.0000044930653,0.00011586761,0.000002748465],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026940975,0.000003085898,0.99693114,0.0000053122826,0.000014438746,0.00000432349,0.00025344512,0.0017027264,0.000071571114,0.00032972643,0.000006379513,0.0006751318],"study_design_scores_gemma":[0.00012998695,0.00015974733,0.9911155,0.000023185934,0.000042840253,0.000073271396,0.00057592586,0.00085566955,0.00058246515,0.0054358267,0.0009353679,0.000070184884],"about_ca_topic_score_codex":0.013932926,"about_ca_topic_score_gemma":0.45951307,"teacher_disagreement_score":0.44558012,"about_ca_system_score_codex":0.0000010479542,"about_ca_system_score_gemma":0.0002808904,"threshold_uncertainty_score":0.99917454},"labels":[],"label_agreement":null},{"id":"W2027171190","doi":"10.1139/cjes-2013-0004","title":"Geochemistry, petrography, and zircon U–Pb geochronology of Paleozoic metaigneous rocks in the Mount Veta area of east-central Alaska: implications for the evolution of the westernmost part of the Yukon–Tanana terrane","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Mafic; Zircon; Terrane; Gneiss; Greenschist; Petrography; Metamorphic rock; Petrology; Paleontology; Tectonics","score_opus":0.01657586159015664,"score_gpt":0.18929002231724965,"score_spread":0.172714160727093,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027171190","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99100035,0.0028783132,0.0000555676,0.005392578,0.0000929823,0.00018601531,0.00010393585,5.500695e-7,0.00028967895],"genre_scores_gemma":[0.9997734,0.000048167643,0.00006474912,0.00006674794,0.000026151214,0.0000015730664,0.0000020257223,7.422812e-7,0.00001643953],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99878716,0.000097562384,0.00046241717,0.00013169141,0.00022629905,0.00029487663],"domain_scores_gemma":[0.99869156,0.00031038857,0.00048621077,0.00021836266,0.00017918329,0.00011429097],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005451125,0.00009462063,0.00024579145,0.00008402642,0.00022741852,0.000023663248,0.0008677917,0.000049793965,0.00034865676],"category_scores_gemma":[0.00022005608,0.00003826619,0.00020059937,0.00062857947,0.0016604627,0.00009947967,0.000015981972,0.00013513712,3.0763718e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005588514,0.000012632985,0.99445,0.000014192354,0.000035148016,2.8483421e-7,0.00022554382,0.0018575735,0.0018509635,0.00008012775,0.000044859233,0.0014230891],"study_design_scores_gemma":[0.00012411595,0.00016058728,0.9916659,0.000034205128,0.00008091081,0.00004228457,0.00143291,0.0010364905,0.001340614,0.0038312473,0.00020290849,0.000047820486],"about_ca_topic_score_codex":0.043692116,"about_ca_topic_score_gemma":0.34470922,"teacher_disagreement_score":0.3010171,"about_ca_system_score_codex":0.0000033376002,"about_ca_system_score_gemma":0.00036146323,"threshold_uncertainty_score":0.96267605},"labels":[],"label_agreement":null},{"id":"W2027173354","doi":"10.1139/e00-060","title":"The last glaciation of east-central Ellesmere Island, Nunavut: ice dynamics, deglacial chronology, and sea level change","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Glasgow; University of Alberta","keywords":"Geology; Glacier; Oceanography; Fjord; Glacier morphology; Sea ice; Deglaciation; Ice sheet; Ice stream; Glacial period; Arctic; Arctic ice pack; Cryosphere; Ice shelf; Physical geography; Holocene; Paleontology; Geography","score_opus":0.03268461522829956,"score_gpt":0.23041770180883148,"score_spread":0.1977330865805319,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027173354","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909983,0.0021343885,0.000005624632,0.0032357785,0.00035750246,0.00007945866,0.00010488912,0.0000016459013,0.0030824079],"genre_scores_gemma":[0.9990533,0.00042109142,0.0000776829,0.00015203988,0.00012233261,2.530667e-7,0.000008902271,0.0000011583757,0.00016326118],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987462,0.0001592702,0.0002479666,0.00013354668,0.00018435153,0.00052865053],"domain_scores_gemma":[0.99918354,0.00017616,0.00014033685,0.000074886986,0.000084148596,0.00034093982],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000869106,0.00008740177,0.0001654743,0.00016465192,0.0007641819,0.00006217325,0.0003716836,0.000095378164,0.0014643045],"category_scores_gemma":[0.0000953457,0.00005872663,0.000042997675,0.00027804982,0.0017889146,0.0002693296,0.000004348851,0.00024085329,0.000033503384],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021584152,0.000002279619,0.9879082,0.0000034537563,0.000011720726,0.000030223366,0.00042492323,0.00015356267,3.1080444e-7,0.00013299391,0.000054525706,0.011256234],"study_design_scores_gemma":[0.0002050228,0.00024935964,0.99291354,0.000016400283,0.000008274485,0.00039261134,0.00047846072,0.0033674126,0.000005411703,0.00024734144,0.0020510405,0.00006511336],"about_ca_topic_score_codex":0.0074556833,"about_ca_topic_score_gemma":0.97648126,"teacher_disagreement_score":0.9690256,"about_ca_system_score_codex":0.0000011071193,"about_ca_system_score_gemma":0.0008514654,"threshold_uncertainty_score":0.9994485},"labels":[],"label_agreement":null},{"id":"W2027230808","doi":"10.1139/e03-076","title":"Tectonic setting of outer trench slope volcanism: pillow basalt and limestone in the Taconian orogen of eastern New York","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada; New York State Department of Health","keywords":"Geology; Basalt; Imbrication; Ordovician; Geochemistry; Mafic; Volcanic rock; Subduction; Paleontology; Pillow lava; Petrology; Tectonics; Volcano","score_opus":0.021445360847641873,"score_gpt":0.1980887481392871,"score_spread":0.17664338729164522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027230808","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926376,0.0027952027,0.000006793878,0.0011815357,0.00006994303,0.000041903226,0.0000091206475,7.5898623e-7,0.0032571552],"genre_scores_gemma":[0.99861157,0.00002337278,0.0010113763,0.00023554321,0.000027325803,6.6982636e-8,8.6325053e-7,7.2125005e-7,0.000089146306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988167,0.00011768762,0.00037177154,0.00013446661,0.0002572657,0.0003020547],"domain_scores_gemma":[0.99917096,0.0001524705,0.00022537922,0.00008062418,0.000052898096,0.00031768627],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010612976,0.000090256246,0.00024592664,0.00020511293,0.000110621324,0.00004926675,0.00036611836,0.00003991451,0.0016257595],"category_scores_gemma":[0.00019525,0.000050435294,0.000074021424,0.0007603207,0.00040544383,0.00013176777,0.000003718272,0.00014377672,0.0000055274536],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026712194,0.0000039922456,0.99395996,0.000004624596,0.000008897447,0.00001852335,0.000643134,0.00059175404,0.00008979227,0.00005435784,0.000030047762,0.0045922655],"study_design_scores_gemma":[0.00022063522,0.00041785452,0.9918705,0.000054117085,0.000027889342,0.00013253716,0.0013513503,0.00063102227,0.00066253537,0.003302278,0.0012204886,0.00010877582],"about_ca_topic_score_codex":0.0513303,"about_ca_topic_score_gemma":0.5168209,"teacher_disagreement_score":0.46549064,"about_ca_system_score_codex":8.6645304e-7,"about_ca_system_score_gemma":0.00065757113,"threshold_uncertainty_score":0.9992869},"labels":[],"label_agreement":null},{"id":"W2027266634","doi":"10.1139/e04-003","title":"Stratigraphy, palynology, and provenance of the Colorado Creek basin, Alaska, USA: Oligocene transpressional tectonics along the central Denali fault system","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Science Foundation","keywords":"Geology; Paleontology; Thrust fault; Conglomerate; Provenance; Fault (geology); Paleocurrent; Terrane; Sedimentary rock; Basin and range topography; Structural basin; Tectonics; Clastic rock","score_opus":0.011003419715397556,"score_gpt":0.18175445134022403,"score_spread":0.17075103162482647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027266634","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932847,0.0025650945,0.000021632866,0.0028984877,0.00019712505,0.0000849037,0.000064903325,0.0000019722947,0.00088119385],"genre_scores_gemma":[0.99927413,0.000057813006,0.00038223955,0.00021777076,0.00004791303,2.2480786e-7,9.906862e-7,8.1681895e-7,0.00001809953],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986081,0.00009521853,0.00036091663,0.00016601519,0.00035362557,0.00041611708],"domain_scores_gemma":[0.9990452,0.00012717297,0.00024987274,0.00010131657,0.000107303975,0.0003691469],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005166819,0.00010783546,0.00022433931,0.00007465688,0.0005230649,0.00009472942,0.00061861397,0.0000657788,0.0004190863],"category_scores_gemma":[0.00009636796,0.000050714236,0.00014578487,0.0006250048,0.0017489825,0.0001651103,0.0000066086714,0.00024243057,0.0000024424817],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006631048,0.0000051696297,0.9900756,0.000011633545,0.00002233942,0.00002211461,0.00010866203,0.008448121,0.00008267199,0.0005443584,0.000021893247,0.0006508281],"study_design_scores_gemma":[0.00017546357,0.000182123,0.9946273,0.000107510845,0.000036706995,0.0001859185,0.0004652547,0.00036139172,0.0008080391,0.002628326,0.0003444309,0.00007751799],"about_ca_topic_score_codex":0.085642315,"about_ca_topic_score_gemma":0.8010506,"teacher_disagreement_score":0.71540827,"about_ca_system_score_codex":0.000002213861,"about_ca_system_score_gemma":0.0008833436,"threshold_uncertainty_score":0.92044646},"labels":[],"label_agreement":null},{"id":"W2027389321","doi":"10.1139/e08-003","title":"A new Jurassic pliosaur from Melville Island, Canadian Arctic Archipelago","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature","funders":"","keywords":"Geology; Archipelago; Paleontology; Arctic; Holotype; Skull; Genus; Cretaceous; Taxon; Oceanography; Biology; Zoology","score_opus":0.021673127293334645,"score_gpt":0.1986621036116442,"score_spread":0.17698897631830954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027389321","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9737194,0.0056226454,0.00006454722,0.003054389,0.0014983598,0.00005728413,0.00017273572,0.0000043902055,0.015806202],"genre_scores_gemma":[0.9965732,0.00009078259,0.0018077667,0.00075818534,0.0003975652,9.701601e-8,0.000019250578,0.0000016190043,0.0003515315],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984757,0.00011206186,0.00029946832,0.0002143891,0.00020403635,0.0006943605],"domain_scores_gemma":[0.9975568,0.00017879618,0.00014413465,0.00011455839,0.00007794413,0.0019277842],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037352627,0.00013325765,0.00023262059,0.00055707345,0.0009428649,0.000043238953,0.00059990113,0.00011074672,0.009647346],"category_scores_gemma":[0.00019794739,0.00010398649,0.000088511246,0.00044687866,0.00085907825,0.00035972762,0.000002763518,0.00028811177,0.0003333839],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009215476,0.0000012156012,0.99188316,8.3475294e-7,0.000016939419,0.00045531977,0.00045801522,0.00049930107,0.0000045028173,0.00010967955,0.0025753952,0.0039864224],"study_design_scores_gemma":[0.0001926741,0.00021854008,0.96326435,0.000019646795,0.000010185725,0.0011542636,0.00019072222,0.00030172945,0.000006049373,0.003193929,0.03131074,0.00013715899],"about_ca_topic_score_codex":0.9286885,"about_ca_topic_score_gemma":0.99968034,"teacher_disagreement_score":0.07099183,"about_ca_system_score_codex":0.0000065751665,"about_ca_system_score_gemma":0.010059708,"threshold_uncertainty_score":0.99555236},"labels":[],"label_agreement":null},{"id":"W2027396851","doi":"10.1139/e07-034","title":"Geochemistry of adakites and rhyolites from the Neoarchaean Gadwal greenstone belt, eastern Dharwar craton, India: implications for sources and geodynamic setting","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Adakite; Geochemistry; Geology; Dharwar Craton; Felsic; Mafic; Greenstone belt; Basalt; Archean; Partial melting; Continental crust; Petrology; Oceanic crust; Craton; Crust; Subduction; Tectonics","score_opus":0.01140256643313391,"score_gpt":0.20701354045560344,"score_spread":0.19561097402246952,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027396851","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918948,0.004887644,0.00008020078,0.0025322319,0.000034939145,0.000057488316,0.00022010464,0.000002104045,0.0002904754],"genre_scores_gemma":[0.99798787,0.00004280576,0.0015950826,0.00022602815,0.00010945654,2.0366394e-7,0.000018798059,0.0000010879639,0.00001869998],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990006,0.000025538904,0.00032049968,0.00017474916,0.00014154933,0.00033707754],"domain_scores_gemma":[0.998342,0.0007956662,0.00024061602,0.00007697421,0.000119622826,0.00042515362],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00083933293,0.00009888186,0.00018529686,0.000096543605,0.00045033515,0.00007946277,0.000298878,0.0000491825,0.0002793594],"category_scores_gemma":[0.0002852703,0.000059701542,0.00006453821,0.00027420936,0.001195189,0.00013781415,0.000013196456,0.00012987723,9.473953e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000053821577,0.0000019869458,0.9859097,0.0000055496666,0.000016125432,0.0000030809224,0.00023574554,0.00005533224,0.00047953002,0.000042831245,0.000015378819,0.013229385],"study_design_scores_gemma":[0.00010251396,0.00012283353,0.9871225,0.000027999195,0.000031792224,0.0000481789,0.0009899024,0.0009834806,0.00037349772,0.009903039,0.00021372933,0.00008057802],"about_ca_topic_score_codex":0.043241892,"about_ca_topic_score_gemma":0.4609066,"teacher_disagreement_score":0.4176647,"about_ca_system_score_codex":8.402431e-7,"about_ca_system_score_gemma":0.00018336641,"threshold_uncertainty_score":0.9631292},"labels":[],"label_agreement":null},{"id":"W2027497428","doi":"10.1139/e06-101","title":"Geology of the western margin of the Grand Forks complex, southern British Columbia: high-grade Cretaceous metamorphism followed by early Tertiary extension on the Granby fault","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Metamorphism; Geochemistry; Granulite; Metamorphic facies; Felsic; Greenschist; Sillimanite; Mafic; Petrology; Biotite; Facies; Geomorphology; Paleontology; Quartz","score_opus":0.014417849085551021,"score_gpt":0.18311599220648278,"score_spread":0.16869814312093176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027497428","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938704,0.0010318708,0.00001385555,0.004248772,0.00025136888,0.00013321494,0.00011007987,0.000002099783,0.00033837496],"genre_scores_gemma":[0.9980234,0.000016323107,0.000058330006,0.0012416409,0.0000423839,2.0966756e-7,0.0000028446495,0.0000019408924,0.0006129373],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99808407,0.00021586672,0.00050341565,0.0001990787,0.0005437499,0.00045381073],"domain_scores_gemma":[0.9985173,0.0003959538,0.00045854496,0.0002080259,0.00013831416,0.0002819047],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013251491,0.00011504141,0.0003313263,0.000065807064,0.0006182077,0.000120452416,0.0010949513,0.00008967406,0.001513767],"category_scores_gemma":[0.00022965817,0.00006142104,0.00029372887,0.0006271783,0.0019279375,0.00009158867,0.000022362537,0.0003251199,0.000006272712],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009659922,0.000011077966,0.9965749,0.0000027292863,0.000029452112,0.000021438023,0.00010494725,0.00029322502,0.0005064635,0.0000051498114,0.0014114034,0.001029568],"study_design_scores_gemma":[0.00021492915,0.0001975471,0.9943542,0.000044690543,0.000053035423,0.00009662059,0.00018355365,0.00016456425,0.00038167075,0.0026449335,0.0015743634,0.000089875364],"about_ca_topic_score_codex":0.31511077,"about_ca_topic_score_gemma":0.9171284,"teacher_disagreement_score":0.6020176,"about_ca_system_score_codex":0.0000017545624,"about_ca_system_score_gemma":0.00016575052,"threshold_uncertainty_score":0.999399},"labels":[],"label_agreement":null},{"id":"W2027706493","doi":"10.1139/e03-027","title":"Utilisation de la scanographie pour l'étude des sédiments : influence des paramètres physiques, chimiques et biologiques sur la mesure des intensités tomographiques","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université Laval; Institut National de la Recherche Scientifique; Université du Québec à Rimouski","funders":"","keywords":"Benthic zone; Sedimentary rock; Geology; Sediment; Bioturbation; Granulometry; Water column; Bay; Mineralogy; Geochemistry; Geomorphology; Oceanography","score_opus":0.027435912047011124,"score_gpt":0.2568173834664995,"score_spread":0.2293814714194884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027706493","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98735887,0.006047969,0.00018050162,0.00012575569,0.000050119226,0.00006868772,0.000020441676,0.000023365505,0.0061242743],"genre_scores_gemma":[0.983625,0.002790397,0.013163371,0.0003733531,0.00002157259,9.98692e-7,0.0000042967317,0.0000027622664,0.000018277098],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979033,0.0008655113,0.0003485864,0.00018113179,0.00020363403,0.00049783813],"domain_scores_gemma":[0.9981746,0.00061029644,0.00022121143,0.00008422475,0.00043196624,0.0004776762],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0031133639,0.00018159348,0.00021849899,0.00049799203,0.00071352726,0.0004618001,0.00039187106,0.00011948496,0.000311951],"category_scores_gemma":[0.0015059067,0.00012569295,0.00010543173,0.00085735664,0.0033009332,0.0015253547,0.0000058521705,0.00024966357,0.0000046887744],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000073902784,0.000011663795,0.9896187,0.000021425667,0.000018571676,0.0000227544,0.001094437,0.0018813346,0.00005203248,0.00077352807,0.00006452394,0.00643359],"study_design_scores_gemma":[0.000093864786,0.00035546877,0.9269186,0.000161644,0.000013351645,0.00024754534,0.00075021014,0.00010235224,0.0014816996,0.06798965,0.0017290846,0.00015649702],"about_ca_topic_score_codex":0.02599864,"about_ca_topic_score_gemma":0.25458318,"teacher_disagreement_score":0.22858454,"about_ca_system_score_codex":0.0000048337965,"about_ca_system_score_gemma":0.0011064397,"threshold_uncertainty_score":0.9994115},"labels":[],"label_agreement":null},{"id":"W2027872785","doi":"10.1139/e07-064","title":"AMS-dated late Pleistocene taiga vole (Rodentia: Microtus xanthognathus) from northeast British Columbia, Canada: a cautionary lesson in chronologyThis article is one of a selection of papers published in this Special Issue on the theme<i>Geology of northeastern British Columbia and northwestern Alberta: diamonds, shallow gas, gravel, and glaciers</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Alberta Museum; University of Victoria; Positive Living North; Royal British Columbia Museum","funders":"","keywords":"Pleistocene; Geology; Colluvium; Paleontology; Vole; Microtus; Taiga; Boreal; Sedimentary rock; Sequence (biology); Archaeology; Physical geography; Geography; Ecology; Biology; Population","score_opus":0.009670531851560396,"score_gpt":0.1702747612099173,"score_spread":0.16060422935835691,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027872785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952657,0.0021198809,2.9520407e-7,0.0009792435,0.00030587456,0.0001674211,0.00030199645,0.0000014784279,0.0008581006],"genre_scores_gemma":[0.9988968,0.0003621713,0.0000444149,0.00020038459,0.000085720065,0.0000010849782,0.000011996951,0.0000029073913,0.00039453493],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982334,0.00018525953,0.00061512203,0.0002877858,0.00028539935,0.00039303926],"domain_scores_gemma":[0.998847,0.00024736632,0.00041792975,0.00008952741,0.00017813352,0.00022003466],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00044418164,0.000103585444,0.0004630517,0.00013104528,0.00048791195,0.00012630115,0.0002522273,0.00010473921,0.0050465],"category_scores_gemma":[0.00015247635,0.00013144291,0.000046041587,0.00050249184,0.0018004549,0.00024845998,0.000012062124,0.00025859303,9.598447e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026878275,0.000025961028,0.9952574,0.000011071641,0.000040608866,0.0000923448,0.0013972471,0.0000651049,0.000037099588,5.999654e-7,0.0010824628,0.0019632252],"study_design_scores_gemma":[0.0006033787,0.00029915688,0.9962857,0.0001284363,0.00001938409,0.00028024946,0.0008513077,0.00043998778,0.000022542461,0.000052692656,0.0009006331,0.000116578856],"about_ca_topic_score_codex":0.9986905,"about_ca_topic_score_gemma":0.99999917,"teacher_disagreement_score":0.0050455397,"about_ca_system_score_codex":0.000013357673,"about_ca_system_score_gemma":0.001400631,"threshold_uncertainty_score":0.995863},"labels":[],"label_agreement":null},{"id":"W2028233865","doi":"10.1139/e03-061","title":"SmNd fluorite dating of Proterozoic low-sulfidation epithermal AuAg deposits and UPb zircon dating of host rocks at Mallery Lake, Nunavut, Canada","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Zircon; Geochemistry; Fluorite; Outcrop; Proterozoic; Metallogeny; Chalcedony; Geochronology; Hydrothermal circulation; Fluid inclusions; Sphalerite; Calcite; Paleontology; Tectonics","score_opus":0.011265934722796009,"score_gpt":0.17571941069755634,"score_spread":0.16445347597476034,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028233865","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969807,0.00077048485,0.0000362512,0.00016064815,0.00011926713,0.000069615184,0.000057173893,0.000001321829,0.0018045218],"genre_scores_gemma":[0.9983102,0.000016891716,0.0014652325,0.000094386254,0.000036786925,1.7703178e-7,0.0000098651535,0.000001340591,0.00006508356],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99848634,0.00010027755,0.00050841284,0.00018848639,0.00036244723,0.00035400773],"domain_scores_gemma":[0.99867785,0.00015673635,0.0004586277,0.00008576006,0.00015528803,0.0004657471],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00067215954,0.00011772899,0.00028548687,0.00014759302,0.00031028697,0.000051757277,0.00027136994,0.00004754789,0.0027556317],"category_scores_gemma":[0.00039780454,0.000085774656,0.00005467437,0.0004681277,0.00032007738,0.0002911047,0.000010086217,0.0001371377,0.0000019253516],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006821496,0.0000035598282,0.9917804,0.000024425031,0.00001695098,0.000020951225,0.000081379156,0.0027964208,0.0028358602,0.000010648211,0.000025300396,0.0023972972],"study_design_scores_gemma":[0.00020806116,0.00020750762,0.9782985,0.000121116755,0.000027035758,0.00009341378,0.00033041713,0.0015355602,0.018337656,0.00018884972,0.00050091604,0.00015095992],"about_ca_topic_score_codex":0.40765405,"about_ca_topic_score_gemma":0.9936211,"teacher_disagreement_score":0.5859671,"about_ca_system_score_codex":0.0000035512828,"about_ca_system_score_gemma":0.0009133367,"threshold_uncertainty_score":0.998156},"labels":[],"label_agreement":null},{"id":"W2028609532","doi":"10.1139/e07-075","title":"<b>Late Quaternary sedimentation on the southwestern Scotian Slope, eastern Canada: relationship to glaciation</b>Geological Survey of Canada Contribution 20070176.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Dalhousie University","funders":"","keywords":"Geology; Glacial period; Continental shelf; Last Glacial Maximum; Sediment; Sedimentation; Quaternary; Sedimentary rock; Oceanography; Holocene; Iceberg; Geomorphology; Ice sheet; Paleontology","score_opus":0.05662796983828438,"score_gpt":0.2430912125452307,"score_spread":0.1864632427069463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028609532","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936812,0.00017969051,0.00002102855,0.004426145,0.0006285149,0.00012773144,0.00010455547,0.0000014450619,0.000829672],"genre_scores_gemma":[0.9988268,0.0000047303406,0.000033915454,0.0008123107,0.000037785732,3.5232372e-7,0.000023556899,0.0000012434543,0.00025932898],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979308,0.0005288548,0.00039727357,0.00015428143,0.00052795775,0.0004608153],"domain_scores_gemma":[0.99779564,0.0009743633,0.00025715213,0.000103875595,0.00036133942,0.00050762406],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018849511,0.00010264637,0.00019606904,0.00018595935,0.00084077835,0.000028894918,0.00043412636,0.000062104475,0.00068119867],"category_scores_gemma":[0.0011367383,0.00006814854,0.000027253267,0.0005545365,0.00043785325,0.00015086406,0.000005465759,0.00025655178,0.000027377379],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000319541,0.0000021591247,0.9898238,0.0000014334529,0.000010027245,0.00010242352,0.00014803984,0.009318284,8.6913536e-7,0.000058871614,0.0004823597,0.000019769159],"study_design_scores_gemma":[0.00013653647,0.00022261273,0.9982271,0.000019857645,0.0000038112664,0.00011426487,0.00014540053,0.00072856765,0.00004612693,0.00007457489,0.0002050019,0.00007611552],"about_ca_topic_score_codex":0.99297225,"about_ca_topic_score_gemma":0.9999784,"teacher_disagreement_score":0.010901717,"about_ca_system_score_codex":0.000006428665,"about_ca_system_score_gemma":0.010908145,"threshold_uncertainty_score":0.99469906},"labels":[],"label_agreement":null},{"id":"W2029007278","doi":"10.1139/e02-053","title":"Three-dimensional velocity images beneath the KangDian Tethyan tectonic zone of China","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Chinese Academy of Sciences","keywords":"Geology; Crust; Tectonics; Seismology; Transition zone; Depth of focus (tectonics); Upper crust; Low-velocity zone; Mantle (geology); Oceanic crust; Paleontology; Lithosphere; Subduction; Geophysics","score_opus":0.01911696651476547,"score_gpt":0.20054826711603801,"score_spread":0.18143130060127255,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029007278","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9795953,0.0054122177,0.00018612806,0.006473474,0.0006027142,0.00009350819,0.00007089992,0.0000111679155,0.00755459],"genre_scores_gemma":[0.9962515,0.000046703964,0.0027231243,0.00072591245,0.00009239178,9.567733e-8,0.0000013456837,0.0000019565518,0.00015691658],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987441,0.000058248974,0.00029356117,0.00014132769,0.0004028559,0.00035993746],"domain_scores_gemma":[0.99906284,0.00011278485,0.00023493727,0.00013942663,0.00010445405,0.00034554917],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010656245,0.000108182176,0.00017887457,0.0003036619,0.00058017095,0.00009452821,0.0006383546,0.000040912873,0.003801374],"category_scores_gemma":[0.00012710369,0.00006524893,0.00010166087,0.00052719424,0.0011478679,0.00035300295,0.00000665916,0.00024135824,0.000035124987],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011761474,0.000021790687,0.7349436,0.00001583454,0.000045836972,0.0001310296,0.0010969664,0.003384345,0.000150151,0.0001692438,0.04214602,0.21788341],"study_design_scores_gemma":[0.00026335212,0.00071356905,0.9281715,0.00013124663,0.000027934462,0.0004880652,0.00032926595,0.036027838,0.0034706998,0.0020701145,0.028043449,0.00026296562],"about_ca_topic_score_codex":0.08326496,"about_ca_topic_score_gemma":0.08079239,"teacher_disagreement_score":0.21762045,"about_ca_system_score_codex":0.0000026052983,"about_ca_system_score_gemma":0.0004962507,"threshold_uncertainty_score":0.9971093},"labels":[],"label_agreement":null},{"id":"W2029024091","doi":"10.1139/e06-020","title":"Gold prospectivity maps of the Red Lake greenstone belt: application of GIS technology","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Natural Resources Canada; Geological Survey of Canada","funders":"Goldcorp","keywords":"Prospectivity mapping; Lode; Geology; Geochemistry; Greenstone belt; Archean; Geomorphology","score_opus":0.008297248804186053,"score_gpt":0.19299128361708692,"score_spread":0.18469403481290086,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029024091","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9442982,0.00038155285,0.009390425,0.027856646,0.00035198333,0.00019619279,0.00001598414,0.000012772637,0.017496238],"genre_scores_gemma":[0.9963668,0.0000012044288,0.0032939063,0.000020230764,0.00002935691,8.591152e-7,2.0777468e-7,5.5554193e-7,0.00028689692],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99919343,0.000024221321,0.00026298995,0.00013178025,0.00019784363,0.00018974773],"domain_scores_gemma":[0.99897605,0.000026505548,0.0004303574,0.00024035388,0.00025354148,0.00007320688],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054423057,0.000056786736,0.00013576017,0.00016945106,0.00013538203,0.00002159695,0.0010613694,0.00005286064,0.000008357564],"category_scores_gemma":[0.00013778344,0.000039581264,0.000052625994,0.0011477028,0.00071645295,0.00015695221,0.00004276909,0.00012079695,5.642708e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001963526,0.000031676827,0.89646274,0.000026777423,0.000009202209,0.00001574619,0.00017920356,0.0019944315,0.021148697,0.07150844,0.0007484713,0.007872683],"study_design_scores_gemma":[0.0002346942,0.00020534871,0.80961955,0.000093739975,0.000009086768,0.0003806542,0.00009556614,0.002118066,0.061028685,0.10483977,0.02122274,0.00015209224],"about_ca_topic_score_codex":0.0030020953,"about_ca_topic_score_gemma":0.14217368,"teacher_disagreement_score":0.13917159,"about_ca_system_score_codex":0.000005073344,"about_ca_system_score_gemma":0.0005730552,"threshold_uncertainty_score":0.8734794},"labels":[],"label_agreement":null},{"id":"W2029080427","doi":"10.1139/e07-058","title":"A new species of lobster (Astacidea, Erymidae) from the Smithers Formation (Middle Jurassic) of British Columbia, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Crustacean biology and ecology","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Biological dispersal; Geology; Carapace; Paleontology; Oceanography; Geography; Fishery; Crustacean; Population; Biology","score_opus":0.015004832881219033,"score_gpt":0.17923917430866879,"score_spread":0.16423434142744975,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029080427","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938442,0.00020092906,0.00018200642,0.0004269059,0.0003679227,0.000053500695,0.000037729846,6.909826e-7,0.0048861215],"genre_scores_gemma":[0.9975339,0.000008629351,0.00057711004,0.0003391245,0.000048641712,9.42891e-8,7.058657e-7,0.0000018804826,0.0014899009],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990236,0.00003158659,0.000356045,0.00008879431,0.00021914631,0.00028078415],"domain_scores_gemma":[0.99916124,0.0001665148,0.00030789975,0.00008145384,0.00002789991,0.00025497196],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007080334,0.000047144647,0.0001443888,0.00002976249,0.00018195642,0.000043470736,0.00039460568,0.000042813263,0.0050520496],"category_scores_gemma":[0.00010316902,0.0000462392,0.00004484983,0.0002504515,0.00080172863,0.00025831236,0.000019407285,0.000102199425,0.0000062531735],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004688078,0.000003038829,0.9721641,0.000001338194,0.000008050004,0.000027332355,0.0005046338,0.00021797269,0.00029212498,0.000011128684,0.022025218,0.004740356],"study_design_scores_gemma":[0.00012993398,0.00009667297,0.9689748,0.000026186954,0.0000074395484,0.000042876018,0.0026261562,0.00001595863,0.00034608974,0.00022700694,0.027453007,0.000053839278],"about_ca_topic_score_codex":0.9795801,"about_ca_topic_score_gemma":0.99993753,"teacher_disagreement_score":0.02035741,"about_ca_system_score_codex":0.000042686894,"about_ca_system_score_gemma":0.0010272709,"threshold_uncertainty_score":0.9958575},"labels":[],"label_agreement":null},{"id":"W2029217614","doi":"10.1139/e07-063","title":"Mapping Quaternary paleovalleys and drift thickness using petrophysical logs, northeast British Columbia, Fontas map sheet, NTS 94IThis article is one of a selection of papers published in this Special Issue on the theme <i>Geology of northeastern British Columbia and northwestern Alberta: diamonds, shallow gas, gravel, and glaciers</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"Ministry of Environment","keywords":"Geology; Outcrop; Bedrock; Tributary; Geomorphology","score_opus":0.011864439070848725,"score_gpt":0.18385427458786915,"score_spread":0.17198983551702043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029217614","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987461,0.00036041913,0.000015200802,0.00026743958,0.00012980125,0.00011266543,0.000016232758,0.0000028073396,0.00034933066],"genre_scores_gemma":[0.9992907,0.000233722,0.000117294076,0.000060761857,0.00014333251,0.0000014056571,0.0000014338109,0.000010279404,0.00014105726],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99850863,0.00010239125,0.00054501527,0.00021208895,0.00033728217,0.00029460643],"domain_scores_gemma":[0.9991914,0.000083422565,0.00023007183,0.00009528117,0.00013965444,0.00026014535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039025556,0.00010131087,0.00043474618,0.0001664527,0.00031159894,0.00036427585,0.00018914418,0.00007863888,0.00063631946],"category_scores_gemma":[0.000058909653,0.00012883716,0.00007135456,0.0005620704,0.0008473724,0.0003748564,0.000018983448,0.00022390853,3.5087865e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000673632,0.000027929053,0.99381936,0.000046289046,0.000065659224,0.000055564393,0.0032563643,0.00096735026,0.00066314253,8.7577104e-7,0.000106731284,0.0009839995],"study_design_scores_gemma":[0.00070237863,0.00030472217,0.9672295,0.00039695468,0.000040666666,0.0004970009,0.0023946983,0.027746912,0.00011969245,0.00008213759,0.00027633872,0.00020898602],"about_ca_topic_score_codex":0.61781067,"about_ca_topic_score_gemma":0.99291116,"teacher_disagreement_score":0.37510052,"about_ca_system_score_codex":0.000012233934,"about_ca_system_score_gemma":0.00022360477,"threshold_uncertainty_score":0.6967252},"labels":[],"label_agreement":null},{"id":"W2029226922","doi":"10.1139/e05-029","title":"A new centrosaurine ceratopsid from the Oldman Formation of Alberta and its implications for centrosaurine taxonomy and systematics","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Systematics; Parietal bone; Locus (genetics); Anatomy; Taxonomy (biology); Posterior parietal cortex; Biology; Geology; Zoology; Neuroscience; Skull; Genetics","score_opus":0.028025820152289712,"score_gpt":0.21293771859597835,"score_spread":0.18491189844368863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029226922","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9777431,0.008349998,0.00071855506,0.011966527,0.0001761475,0.00026124227,0.00017320305,0.0000014480044,0.0006098143],"genre_scores_gemma":[0.99629956,0.0000972435,0.003191782,0.00017735169,0.00015836785,6.6605537e-7,0.000010826019,5.915043e-7,0.00006359759],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99933803,0.00004332943,0.000269146,0.0000839961,0.00005214224,0.00021337114],"domain_scores_gemma":[0.9990584,0.00032320665,0.00022025919,0.00005431655,0.000062395935,0.0002814243],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033858287,0.00006079098,0.00013772321,0.00007167787,0.00032710785,0.000034759745,0.0001774655,0.000035975903,0.00011674553],"category_scores_gemma":[0.00012949544,0.000038615366,0.000026219226,0.00010056002,0.00019581047,0.0003341282,0.0000031484062,0.00005421718,0.0000025043723],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010594849,0.0000021290055,0.99043286,0.000014564466,0.000013723964,4.899962e-7,0.00032556316,0.00037487954,0.000039840983,0.00323928,0.00056743395,0.0049786447],"study_design_scores_gemma":[0.0002471519,0.00012550583,0.9780475,0.00003047379,0.000018242768,0.00014722427,0.00014221627,0.0054371892,0.000042712734,0.0010394686,0.014669533,0.000052775],"about_ca_topic_score_codex":0.00621471,"about_ca_topic_score_gemma":0.5935814,"teacher_disagreement_score":0.58736664,"about_ca_system_score_codex":0.0000016259819,"about_ca_system_score_gemma":0.00039816342,"threshold_uncertainty_score":0.9394824},"labels":[],"label_agreement":null},{"id":"W2029284369","doi":"10.1139/cjes-2013-0085","title":"Ar–Ar dating and Sr–Nd–Pb isotopic character of Paleogene basalts from the Xialiaohe Depression, northern Bohai Bay Basin: implications for transformation of the subcontinental lithospheric mantle under the eastern North China Craton","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"","keywords":"Basalt; Geology; Geochemistry; Mantle (geology); Craton; Radiogenic nuclide; Lithosphere; Paleogene; Structural basin; Paleontology; Tectonics","score_opus":0.012957972921011916,"score_gpt":0.19009905894827847,"score_spread":0.17714108602726655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029284369","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923978,0.0007005587,0.00046567572,0.0058323215,0.00011114265,0.00012262155,0.00011370432,0.0000011877593,0.00025502816],"genre_scores_gemma":[0.9993046,0.000028776787,0.00019094947,0.00035229535,0.0000884281,8.645777e-7,0.000012821179,0.0000011578867,0.00002013893],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99906856,0.00010111169,0.00034324676,0.000120821984,0.00017237246,0.00019388091],"domain_scores_gemma":[0.9990643,0.00024172712,0.0003217471,0.00013511318,0.00009636628,0.00014071757],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046222212,0.00008546923,0.000162439,0.000026497504,0.0004825458,0.000061654544,0.00047378032,0.000030677213,0.00039260383],"category_scores_gemma":[0.00009424857,0.000035900608,0.00010640704,0.00028883567,0.00039784698,0.00017691754,0.00000805537,0.000103179154,0.0000016484782],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005009864,0.0000035709697,0.9894756,0.000004148264,0.000012132354,7.909965e-8,0.00029941552,0.00047395265,0.00011418998,0.000020868682,0.000011203196,0.009579816],"study_design_scores_gemma":[0.00011382999,0.000060521026,0.99395746,0.000026881902,0.00003568759,0.000005313037,0.00029156046,0.0027829437,0.00047946337,0.0014127357,0.00078167894,0.00005190871],"about_ca_topic_score_codex":0.012011669,"about_ca_topic_score_gemma":0.498253,"teacher_disagreement_score":0.4862413,"about_ca_system_score_codex":8.641169e-7,"about_ca_system_score_gemma":0.00010030136,"threshold_uncertainty_score":0.99456745},"labels":[],"label_agreement":null},{"id":"W2029430417","doi":"10.1139/e06-087","title":"Atypical diagenetic effects on strontium-isotope composition of Early Jurassic belemnites, Queen Charlotte Islands, British Columbia, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Diagenesis; Geology; Ammonite; Strontium; Isotopes of strontium; Isotopes of oxygen; Seawater; Paleontology; Biozone; Geochemistry; Mineralogy; Oceanography; Biostratigraphy; Cretaceous; Chemistry","score_opus":0.007265597254556917,"score_gpt":0.18823551219461893,"score_spread":0.180969914940062,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029430417","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98970664,0.0026552288,0.000037725706,0.00014425055,0.00072514924,0.00011400516,0.00007183101,0.0000028795948,0.0065422654],"genre_scores_gemma":[0.99934304,0.000022459102,0.00032603327,0.00011346352,0.00013286766,1.7036284e-7,0.000003656426,0.0000010557882,0.00005727688],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99834585,0.00010801382,0.0004043932,0.00018035993,0.00042586305,0.00053550984],"domain_scores_gemma":[0.9985548,0.00029937393,0.00026468973,0.00008859775,0.00010253349,0.0006899967],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007311816,0.000102252205,0.0002837392,0.0001718183,0.0004752174,0.00018928008,0.00039543645,0.000079833124,0.00026355375],"category_scores_gemma":[0.00006831612,0.000115620336,0.00008166011,0.0003691672,0.00047612857,0.00022559521,9.3621367e-7,0.0002465309,0.000002276875],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019692114,0.0000048039824,0.96916014,0.000009038868,0.000017677683,0.00033816736,0.000053000233,0.000043496762,0.000016122758,0.00001259869,0.0005304547,0.029794801],"study_design_scores_gemma":[0.0002769938,0.0009992566,0.9975538,0.00013437534,0.000016416863,0.00012217586,0.00006330945,0.000045896453,0.000112862464,0.0000981331,0.00044900185,0.00012773805],"about_ca_topic_score_codex":0.95481414,"about_ca_topic_score_gemma":0.999676,"teacher_disagreement_score":0.044861857,"about_ca_system_score_codex":0.0000044182307,"about_ca_system_score_gemma":0.002038696,"threshold_uncertainty_score":0.47148603},"labels":[],"label_agreement":null},{"id":"W2029751832","doi":"10.1139/e09-079","title":"Diagenesis to metamorphism transition in an episutural basin: the late Paleozoic St. Mary’s Basin, Nova Scotia, Canada","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"Geology; Metamorphism; Illite; Diagenesis; Chlorite; Geochemistry; Greenschist; Metamorphic rock; Mineralogy; Clay minerals; Paleontology; Quartz","score_opus":0.015147998084698935,"score_gpt":0.19083443746794146,"score_spread":0.17568643938324252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029751832","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97991437,0.00023561378,0.000008185212,0.018423587,0.00066417165,0.00007270741,0.00007404231,0.000002241887,0.00060508156],"genre_scores_gemma":[0.9957451,0.000005310548,0.00047051805,0.0035538974,0.00015924386,1.7194807e-7,0.000009409906,0.0000014188621,0.000054915152],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99836457,0.00013189575,0.0003547889,0.00020349702,0.00041420673,0.0005310255],"domain_scores_gemma":[0.9984816,0.00016123017,0.000110076224,0.00013491369,0.000119266995,0.0009929668],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010976732,0.00013874286,0.0002528861,0.00024613325,0.00031073135,0.0001646428,0.00068320136,0.00005306186,0.012158211],"category_scores_gemma":[0.00017782372,0.00007981343,0.00009533671,0.0010550998,0.00037354702,0.0003723381,0.0000044805197,0.00033500846,0.000032962605],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008402388,0.000004777407,0.98663765,0.0000018443299,0.00000916711,0.00012914622,0.00018187815,0.0072553484,0.0002117569,0.000018301527,0.00030766637,0.005234074],"study_design_scores_gemma":[0.00008519111,0.00013795504,0.9944447,0.0000105528625,0.000019995434,0.00005558604,0.00027277102,0.0010956697,0.00021163074,0.0006949763,0.0028313943,0.00013954254],"about_ca_topic_score_codex":0.9607278,"about_ca_topic_score_gemma":0.9999209,"teacher_disagreement_score":0.0391931,"about_ca_system_score_codex":0.0000032398889,"about_ca_system_score_gemma":0.0013456375,"threshold_uncertainty_score":0.9887448},"labels":[],"label_agreement":null},{"id":"W2030012866","doi":"10.1139/e10-007","title":"Wall-rock structure at the present contact surfaces between repeatedly deformed thrust sheets, Grenville Orogen of central Ontario, Canada","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Gneiss; Thrust fault; Intraplate earthquake; Petrology; Geomorphology; Tectonics; Metamorphic rock","score_opus":0.010859851982003519,"score_gpt":0.1762345407310684,"score_spread":0.16537468874906489,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030012866","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939961,0.000648845,4.2428437e-7,0.0019767894,0.00035849737,0.00007169731,0.0001862657,0.0000015210313,0.0027598713],"genre_scores_gemma":[0.9993832,0.000010231123,0.00008846257,0.00017631533,0.00010761728,7.453024e-8,0.00001951837,0.0000012683529,0.00021328789],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981339,0.000059117854,0.0004349531,0.00020134551,0.0005676582,0.00060304115],"domain_scores_gemma":[0.9983406,0.00020064667,0.00030243574,0.00015429783,0.00014339387,0.00085862435],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000404062,0.00015015356,0.0003115919,0.000079799254,0.000532171,0.000078677,0.00077472714,0.00007627307,0.05296229],"category_scores_gemma":[0.00013823346,0.00007622094,0.0001227134,0.00036597316,0.0003979937,0.00014893399,0.000015671463,0.0003969094,0.0000060617726],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000070262076,0.0000015254402,0.9937629,0.0000028135805,0.00003971724,0.000025902275,0.00013204997,0.0044034943,0.00017653804,0.000007966903,0.00051348156,0.0009265573],"study_design_scores_gemma":[0.00010831135,0.0001283244,0.9836524,0.000009699249,0.000040824936,0.00005681081,0.00016452493,0.00025970646,0.0017980533,0.00034115076,0.013325103,0.0001150806],"about_ca_topic_score_codex":0.99277014,"about_ca_topic_score_gemma":0.9999663,"teacher_disagreement_score":0.052956227,"about_ca_system_score_codex":0.000011184942,"about_ca_system_score_gemma":0.0034684937,"threshold_uncertainty_score":0.94790345},"labels":[],"label_agreement":null},{"id":"W2030141898","doi":"10.1139/e07-070","title":"Identification of coherent links between interannual sedimentary structures and daily meteorological observations in Arctic proglacial lacustrine varves: potentials and limitations","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"Networks of Centres of Excellence of Canada; Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; ArcticNet; Canadian Natural Resources Limited","keywords":"Varve; Geology; Sediment; Arctic; Sedimentary depositional environment; Deposition (geology); Sedimentary rock; Geomorphology; Physical geography; Climatology; Hydrology (agriculture); Paleontology; Oceanography; Geotechnical engineering","score_opus":0.08415916471956118,"score_gpt":0.2698074295149512,"score_spread":0.18564826479538998,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030141898","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99766225,0.0007739844,0.000014993259,0.0012134498,0.00011629422,0.000099796714,0.000039869912,0.0000017038215,0.00007763743],"genre_scores_gemma":[0.9990379,0.000083233805,0.0007320816,0.00007845031,0.00003935216,4.0668132e-7,0.0000105559475,7.010537e-7,0.00001727959],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989362,0.00018243249,0.00039307587,0.0001307649,0.00014121427,0.00021631482],"domain_scores_gemma":[0.9990194,0.00042506956,0.00016991576,0.00004503304,0.000110058405,0.0002305475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00082787476,0.000067138055,0.00018533134,0.0003583184,0.0002975606,0.000033947435,0.00017148128,0.00009346897,0.00011699304],"category_scores_gemma":[0.00038996516,0.00005143511,0.00002427262,0.00029844782,0.0012836749,0.000309081,0.0000065774975,0.00027143548,0.0000016709702],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009723324,0.000003579216,0.99850094,0.0000072107578,0.000013357715,0.00002334556,0.0005790461,0.00027333837,0.000020764724,0.00009799424,0.000009617152,0.0004610868],"study_design_scores_gemma":[0.00020124715,0.00029362107,0.9966051,0.000013842989,0.000013863464,0.0001761513,0.00042126596,0.00027341966,0.00005833404,0.0018333633,0.00006176171,0.00004800237],"about_ca_topic_score_codex":0.0037966217,"about_ca_topic_score_gemma":0.2297528,"teacher_disagreement_score":0.22595617,"about_ca_system_score_codex":5.525022e-7,"about_ca_system_score_gemma":0.00041627773,"threshold_uncertainty_score":0.78430223},"labels":[],"label_agreement":null},{"id":"W2030144418","doi":"10.1139/e02-041","title":"Post-Taconian shortening, inversion and strike slip in the Stephenville area, western Newfoundland Appalachians","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; University of Alberta; Dalhousie University","funders":"","keywords":"Geology; Allochthon; Sinistral and dextral; Thrust fault; Paleontology; Seismology; Strike-slip tectonics; Foreland basin; Massif; Orogeny; Graben; Fault (geology); Nappe; Tectonics","score_opus":0.02124746483252223,"score_gpt":0.18367093033986906,"score_spread":0.16242346550734682,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030144418","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98966026,0.0012829846,0.0000045374204,0.0037249385,0.00008732511,0.000044214303,0.000015272444,0.000001696178,0.005178781],"genre_scores_gemma":[0.9984569,0.000059070055,0.00013418675,0.0011501365,0.000059286027,8.929033e-8,0.0000023900768,6.5767136e-7,0.0001373094],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989273,0.00008035345,0.00022974811,0.00015429998,0.0002647046,0.00034358396],"domain_scores_gemma":[0.9992403,0.00012979606,0.00010019808,0.000070992355,0.000044144326,0.00041456614],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00055470725,0.00009604933,0.0001636246,0.00021993602,0.00031807023,0.00019180148,0.00040191162,0.00004393009,0.003973737],"category_scores_gemma":[0.00007879423,0.000052321564,0.000059008096,0.00046075264,0.00045174095,0.00026105513,0.000005325191,0.00020516664,0.000027839307],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021742974,0.0000036570007,0.99490327,0.0000014642866,0.000004388121,0.00007252468,0.00046596004,0.0005521355,0.0000067906617,0.000010027245,0.000052442232,0.0039251745],"study_design_scores_gemma":[0.00013708274,0.0002861429,0.9885377,0.000017372095,0.00001332652,0.00011580854,0.0012043257,0.0056630457,0.000002520734,0.0005093992,0.0034215988,0.00009162679],"about_ca_topic_score_codex":0.053173617,"about_ca_topic_score_gemma":0.9027893,"teacher_disagreement_score":0.84961563,"about_ca_system_score_codex":0.0000012804683,"about_ca_system_score_gemma":0.00009023216,"threshold_uncertainty_score":0.99693674},"labels":[],"label_agreement":null},{"id":"W2030194729","doi":"10.1139/e03-041","title":"A study of the tectonically active Marmara region, Turkey, using a global positioning system (GPS)","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; North Anatolian Fault; Seismology; Sinistral and dextral; Global Positioning System; Geodesy; Active fault; Tectonics; Fault (geology); Eurasian Plate; Vertical displacement; Magnitude (astronomy); Displacement (psychology); Deformation (meteorology); Geomorphology; Subduction; Oceanography","score_opus":0.03493603550334034,"score_gpt":0.23747719157606476,"score_spread":0.2025411560727244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030194729","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9875432,0.0009462913,0.000021864911,0.00010008891,0.00061988394,0.00015787139,0.000013883381,0.0000035517603,0.010593362],"genre_scores_gemma":[0.99949586,0.000005256918,0.00038342824,0.000056240213,0.000042378753,1.6848021e-7,1.12874936e-7,0.0000014313215,0.000015118751],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99839324,0.00027321014,0.00038411815,0.00016419521,0.00042418993,0.0003610483],"domain_scores_gemma":[0.9989026,0.00010958877,0.00038416512,0.00013523002,0.00019867872,0.0002697188],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00075687654,0.00011663467,0.00024280677,0.00013671997,0.00089378515,0.00009705971,0.00043446786,0.000037539026,0.00011753322],"category_scores_gemma":[0.00021893544,0.0000722574,0.00010470676,0.0010020104,0.00045292528,0.00026143878,0.0000069159605,0.00016374241,0.00000364957],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008985128,0.000009813716,0.9914925,0.0000058239348,0.000045487,0.00009938665,0.00071211264,0.0064914934,0.000003797169,0.0003294564,0.000019564375,0.0007815655],"study_design_scores_gemma":[0.0003384759,0.0005237787,0.9857311,0.00014447852,0.00004829942,0.0011648976,0.011196029,0.0003504871,0.00005395171,0.00015586532,0.0001886389,0.0001039586],"about_ca_topic_score_codex":0.028936652,"about_ca_topic_score_gemma":0.2668961,"teacher_disagreement_score":0.23795946,"about_ca_system_score_codex":0.000010447654,"about_ca_system_score_gemma":0.0019294422,"threshold_uncertainty_score":0.97752976},"labels":[],"label_agreement":null},{"id":"W2030356981","doi":"10.1139/e02-035","title":"Tundra lakes and permafrost, Richards Island, western Arctic coast, Canada","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":195,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Permafrost; Geology; Tundra; Shore; Active layer; Thermokarst; Geomorphology; Littoral zone; Terrace (agriculture); Hydrology (agriculture); Arctic; Snow; Physical geography; Oceanography","score_opus":0.037034652252235636,"score_gpt":0.2092649599731727,"score_spread":0.17223030772093706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030356981","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9862811,0.0057550934,0.0000021179005,0.002207741,0.0008023932,0.00004941111,0.0018400188,0.0000022595066,0.0030598394],"genre_scores_gemma":[0.9975933,0.00031026735,0.00002316547,0.0011209022,0.00025939074,1.0573386e-7,0.000022504028,0.0000024412689,0.00066796376],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987174,0.000046875324,0.0002547328,0.00016011471,0.00034388126,0.0004769692],"domain_scores_gemma":[0.99875677,0.00011655362,0.00013499548,0.00008215297,0.00009051628,0.00081900385],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035146976,0.00012797046,0.00019982552,0.00019508209,0.00050125003,0.00026926343,0.00029886627,0.000037563022,0.010003403],"category_scores_gemma":[0.00006185849,0.00009762157,0.000038481576,0.00029341283,0.00038276816,0.00041671123,0.000005043462,0.00016269003,0.000032058186],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000019916306,0.000001411877,0.99446017,0.00000934877,0.0000059208105,0.000182623,0.00068154745,0.00013358211,0.00000977895,0.000003383918,0.0033196963,0.001190557],"study_design_scores_gemma":[0.00022143396,0.00022362838,0.9269288,0.00006451891,0.000014744783,0.00094565825,0.0011308303,0.0017916184,0.000010016818,0.00004231175,0.068433836,0.00019255848],"about_ca_topic_score_codex":0.86179286,"about_ca_topic_score_gemma":0.99990326,"teacher_disagreement_score":0.1381104,"about_ca_system_score_codex":0.000003965406,"about_ca_system_score_gemma":0.0008314573,"threshold_uncertainty_score":0.9909016},"labels":[],"label_agreement":null},{"id":"W2030438008","doi":"10.1139/e05-033","title":"Revised ages of blueschist metamorphism and the youngest pre-thrusting rocks in the San Juan Islands, Washington","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Blueschist; Geology; Metamorphism; Aptian; Geochemistry; Cretaceous; Paleontology; Facies; Subduction; Tectonics; Eclogite","score_opus":0.01833910541275537,"score_gpt":0.22157226025405552,"score_spread":0.20323315484130014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030438008","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.938846,0.036361314,0.000005145311,0.002713979,0.00019117232,0.00010023805,0.000012118495,0.0000015647677,0.021768505],"genre_scores_gemma":[0.9990281,0.0002529137,0.0003658697,0.00019420004,0.00013815057,2.0497066e-7,4.934374e-7,4.448961e-7,0.000019644556],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998689,0.00027417715,0.00036491797,0.0001221975,0.00025728092,0.00029243692],"domain_scores_gemma":[0.99897975,0.00042750651,0.00028320885,0.000099543184,0.000039842478,0.00017012586],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0031321116,0.000097329255,0.00022990437,0.00021817988,0.00053736096,0.0001429065,0.0005854842,0.000046151505,0.00011738099],"category_scores_gemma":[0.0002523831,0.000048402697,0.000074965,0.00036672357,0.0014516778,0.0004018949,0.0000011528375,0.00027779324,9.1224865e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023823533,0.0000032868866,0.9713245,0.000006747115,0.000014458825,0.000023899554,0.004475921,0.0004492366,0.000008938982,0.00030590847,0.00014209414,0.023221172],"study_design_scores_gemma":[0.00034253215,0.00013477092,0.99584633,0.00006243771,0.000026396017,0.0001743533,0.0011075,0.000703005,0.000018918396,0.00050078786,0.001016345,0.00006662872],"about_ca_topic_score_codex":0.016098883,"about_ca_topic_score_gemma":0.7109752,"teacher_disagreement_score":0.6948763,"about_ca_system_score_codex":6.198219e-7,"about_ca_system_score_gemma":0.00036592493,"threshold_uncertainty_score":0.990453},"labels":[],"label_agreement":null},{"id":"W2030582057","doi":"10.1139/e03-020","title":"Geochemistry of the Coastal Sonora batholith, Northwestern Mexico","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Consejo Nacional de Ciencia y Tecnología","keywords":"Batholith; Geology; Geochemistry; Magmatism; Radiogenic nuclide; Crust; Mantle (geology); Pluton; Trace element; Paleontology; Tectonics","score_opus":0.013687567796337436,"score_gpt":0.18347469679416972,"score_spread":0.1697871289978323,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030582057","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9827971,0.0005763521,0.00000994721,0.00047342674,0.000204586,0.000023288649,0.000041705167,0.0000012587321,0.015872348],"genre_scores_gemma":[0.9992248,0.000008697273,0.0003621658,0.00020493411,0.000035727768,4.8097686e-8,0.0000014310328,6.303972e-7,0.00016157009],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988949,0.0000666063,0.00029377686,0.00012507348,0.00030039018,0.00031927822],"domain_scores_gemma":[0.9990345,0.00007955174,0.00022229766,0.000108323766,0.0001220857,0.00043321543],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005562789,0.000088170025,0.00017864679,0.000076218756,0.0002493219,0.000057600577,0.00049969053,0.000042590138,0.00533732],"category_scores_gemma":[0.00023353193,0.000047611164,0.00015949759,0.00054341817,0.00080927566,0.00013687648,0.0000053815397,0.000158587,0.00001551532],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000013655791,0.000003222259,0.9981207,0.0000029112628,0.0000074524105,0.000012541905,0.000063970045,0.0011802571,0.00013520438,0.00007383633,0.00003077899,0.00036775263],"study_design_scores_gemma":[0.00010861512,0.00010374795,0.9812334,0.000024950063,0.000022764036,0.00017298685,0.00046002926,0.00022384117,0.007125162,0.005903489,0.0045141815,0.00010684105],"about_ca_topic_score_codex":0.018855037,"about_ca_topic_score_gemma":0.5756967,"teacher_disagreement_score":0.5568416,"about_ca_system_score_codex":5.0571066e-7,"about_ca_system_score_gemma":0.0007782666,"threshold_uncertainty_score":0.9955719},"labels":[],"label_agreement":null},{"id":"W2030597497","doi":"10.1139/e02-099","title":"Late Ordovician platform foundering, its paleoceanography and burial, as preserved in separate (eastern Michigan Basin, Ottawa Embayment) basins, southern Ontario","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Centre de Géomatique du Québec; Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Ordovician; Facies; Paleontology; Sedimentary depositional environment; Unconformity; Geochemistry; Structural basin","score_opus":0.019492449783792776,"score_gpt":0.203924779582149,"score_spread":0.18443232979835622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030597497","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9859444,0.0008823606,0.0000014547403,0.00026140845,0.00023289783,0.00007787677,0.000036031743,0.000003068036,0.012560492],"genre_scores_gemma":[0.997513,0.000029822506,0.00019953334,0.00028044273,0.000054101038,2.2041658e-7,0.0000072209486,0.000002514328,0.0019131677],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983485,0.00007024343,0.00044064224,0.00025225244,0.00031758676,0.000570794],"domain_scores_gemma":[0.998837,0.00004141053,0.00023234141,0.00010098058,0.00006116914,0.0007270835],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009954511,0.00017928162,0.00025901705,0.00038373913,0.0004413656,0.00034228634,0.00034181678,0.00006298142,0.0044899285],"category_scores_gemma":[0.000059766186,0.00014698297,0.00009936967,0.00058926584,0.00025746613,0.00058692205,0.000005663776,0.00021969536,0.000061854655],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010003739,0.000006405943,0.9968654,0.0000092376085,0.000027349519,0.00008450503,0.0014632439,0.0012066844,0.00002676126,0.000012545337,0.000022713966,0.00026514253],"study_design_scores_gemma":[0.00073913677,0.00043248877,0.9543159,0.00012989527,0.00004818798,0.00016393843,0.00449185,0.00088886096,0.0004987958,0.0012660341,0.03664142,0.00038346558],"about_ca_topic_score_codex":0.21527536,"about_ca_topic_score_gemma":0.99600255,"teacher_disagreement_score":0.78072715,"about_ca_system_score_codex":0.0000047840526,"about_ca_system_score_gemma":0.0010929798,"threshold_uncertainty_score":0.9964201},"labels":[],"label_agreement":null},{"id":"W2030795504","doi":"10.1139/e99-122","title":"The complexity of the crust and Moho under the southeastern Superior and Grenville provinces of the Canadian Shield from seismic refraction - wide-angle reflection data","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Coda; Geology; Seismology; Reflection (computer programming); Classification of discontinuities; Refraction; Crust; Seismic refraction; Amplitude; Geophysics; Optics","score_opus":0.05499567837697261,"score_gpt":0.23732864807479825,"score_spread":0.18233296969782564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030795504","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9778752,0.0013581201,0.0000063412226,0.018110745,0.00032653887,0.00010892946,0.00017626317,0.0000019355905,0.002035975],"genre_scores_gemma":[0.99839675,0.00012866908,0.000079279016,0.0011230058,0.00004474775,1.2188923e-7,0.0000016778106,0.0000014892433,0.00022427809],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99899226,0.00017322325,0.00022623925,0.00013633023,0.0002677955,0.00020415343],"domain_scores_gemma":[0.99916446,0.00016008077,0.00019355839,0.0002674071,0.000048750615,0.00016576923],"candidate_categories":["sts"],"consensus_categories":["sts"],"category_scores_codex":[0.00082994025,0.0000758108,0.0001072642,0.0000685289,0.0015685995,0.0001896938,0.000799206,0.000038269496,0.00025631892],"category_scores_gemma":[0.00008502823,0.00003230865,0.000033945278,0.00024750724,0.0027606958,0.0003004235,0.000016063477,0.00020927285,0.000001518108],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026488184,0.0000041005696,0.9260555,0.000007752964,0.000032879,0.0000023468697,0.0020035938,0.00081648614,0.00005820593,0.00010415931,0.0023122157,0.0685763],"study_design_scores_gemma":[0.00012297962,0.00013338563,0.91273546,0.000107570304,0.00003536423,0.00008983559,0.005949424,0.017419556,0.0004854619,0.0038583106,0.058960043,0.00010258193],"about_ca_topic_score_codex":0.88615674,"about_ca_topic_score_gemma":0.97952354,"teacher_disagreement_score":0.093366764,"about_ca_system_score_codex":0.000004350949,"about_ca_system_score_gemma":0.001198133,"threshold_uncertainty_score":0.9999532},"labels":[],"label_agreement":null},{"id":"W2030917166","doi":"10.1139/e00-089","title":"Geochronological and kinematic constraints on crustal shortening and escape in a two-sided oblique-slip collisional and magmatic orogen, Paleoproterozoic Taltson magmatic zone, northeastern Alberta","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Geological Survey of Canada","funders":"","keywords":"Geology; Shear zone; Mylonite; Geochemistry; Transpression; Zircon; Craton; Subduction; Terrane; Gneiss; Continental crust; Archean; Petrology; Crust; Seismology; Metamorphic rock; Tectonics","score_opus":0.012433709008201642,"score_gpt":0.2091522462210469,"score_spread":0.19671853721284524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030917166","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960987,0.00091210555,0.0000068972636,0.0010283776,0.000032919415,0.00013708885,0.0000150165115,0.0000027256094,0.0017661835],"genre_scores_gemma":[0.99808276,0.000060742423,0.0014087039,0.00035272687,0.000030337795,7.773431e-7,0.000004050263,0.0000015086722,0.000058396865],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983857,0.00010666548,0.00047417986,0.00029485815,0.00028593797,0.00045265572],"domain_scores_gemma":[0.99861294,0.00043236438,0.00013741193,0.00007118727,0.000040690185,0.0007054258],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00061143865,0.00017950674,0.0003851366,0.00028307823,0.000253541,0.00020657496,0.00019206131,0.000059489066,0.008856077],"category_scores_gemma":[0.000229149,0.000116645446,0.0000469401,0.00038819894,0.0012399559,0.00025019638,0.000009421967,0.00024012741,0.000021831052],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026940495,0.000012807151,0.9350754,0.00002766446,0.000015998896,0.00020509296,0.0002534294,0.0018147103,0.000036355003,0.000054500983,0.0000036923532,0.06247343],"study_design_scores_gemma":[0.00047716792,0.00050691114,0.96351206,0.00024422893,0.00002621846,0.00079386035,0.0004021863,0.030844744,0.000015671438,0.0029590118,0.00003065814,0.00018725335],"about_ca_topic_score_codex":0.020150837,"about_ca_topic_score_gemma":0.6297689,"teacher_disagreement_score":0.60961807,"about_ca_system_score_codex":0.0000022522845,"about_ca_system_score_gemma":0.00021708697,"threshold_uncertainty_score":0.99205},"labels":[],"label_agreement":null},{"id":"W2031091393","doi":"10.1139/e06-112","title":"Ediacaran U–Pb zircon dates for the Lac Matapédia and Mt. St.-Anselme basalts of the Quebec Appalachians: support for a long-lived mantle plume during the rifting phase of Iapetus opening","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Flood basalt; Basalt; Zircon; Geochemistry; Laurentia; Mantle plume; Rift; Mantle (geology); Apparent polar wander; Magmatism; Paleontology; Volcanism; Paleozoic; Lithosphere; Tectonics","score_opus":0.023368013325165696,"score_gpt":0.23942017860165898,"score_spread":0.2160521652764933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031091393","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956062,0.0011376351,0.0005282548,0.0018985188,0.0001879461,0.0002545509,0.00015882312,0.0000017182784,0.00022638084],"genre_scores_gemma":[0.99867487,0.000028066153,0.0008177959,0.00017744018,0.00012518506,8.7194667e-7,0.0000057713964,0.000001864993,0.00016813297],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998599,0.000053027987,0.00047311402,0.00016772862,0.00026509922,0.0004420446],"domain_scores_gemma":[0.99811226,0.0009558449,0.0004092406,0.00012860191,0.00013811205,0.00025592788],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023713072,0.00011411169,0.00025490118,0.00010606978,0.0007297599,0.00009816903,0.00068951293,0.00004236933,0.0005594647],"category_scores_gemma":[0.0004117436,0.000050929477,0.00017049973,0.00038207966,0.000961476,0.00020819428,0.000015796104,0.00014708284,9.76873e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010335837,0.00001260956,0.98734504,0.00006302762,0.00007829102,0.000009864948,0.000949157,0.0014238433,0.0024827076,0.00009956913,0.00008642478,0.0073461067],"study_design_scores_gemma":[0.00084060925,0.00041917697,0.97714156,0.00009763007,0.00014675275,0.00006967241,0.0031206668,0.004494334,0.009284027,0.0010753253,0.003148783,0.00016145667],"about_ca_topic_score_codex":0.03218734,"about_ca_topic_score_gemma":0.6282819,"teacher_disagreement_score":0.59609455,"about_ca_system_score_codex":0.0000017275751,"about_ca_system_score_gemma":0.00035456844,"threshold_uncertainty_score":0.9742574},"labels":[],"label_agreement":null},{"id":"W2031162338","doi":"10.1139/e10-057","title":"A history of <i>Albertosaurus</i> discoveries in Alberta, CanadaThis article is one of a series of papers published in this Special Issue on the theme <i>Albertosaurus</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; University of Alberta","funders":"","keywords":"Confusion; Canyon; Horseshoe (symbol); Archaeology; Taxon; Geology; Genus; Paleontology; Geography; Range (aeronautics); Theme (computing); Zoology; Cartography; Biology; Epistemology; Computer science; Engineering","score_opus":0.011443653265513078,"score_gpt":0.18028786800162352,"score_spread":0.16884421473611044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031162338","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90133655,0.00054526405,1.0738935e-7,0.008316524,0.0012168492,0.00009066793,0.00007744344,6.6842347e-7,0.088415906],"genre_scores_gemma":[0.9978502,0.000049582173,0.000119760814,0.0005958152,0.0002131317,5.1295e-7,0.000002952303,0.0000017942035,0.0011662574],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983173,0.00015849138,0.00063284993,0.00018594095,0.0003051411,0.00040025412],"domain_scores_gemma":[0.9985095,0.00055880327,0.00044016016,0.00018883133,0.00008701892,0.0002156649],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011008958,0.00012871405,0.00038803005,0.00040138175,0.000098892044,0.000014960381,0.0006398481,0.00011694314,0.032751855],"category_scores_gemma":[0.0007549779,0.000087305765,0.00008493292,0.0005393569,0.0026844798,0.0005649899,0.000008107499,0.00037622606,0.0000071043864],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013047001,0.00002900364,0.9859578,0.000013107356,0.000018441144,0.00001919516,0.004395926,0.00010981544,0.0010776204,0.0019333275,0.0055150357,0.0008002454],"study_design_scores_gemma":[0.00030312725,0.0005712497,0.87425953,0.000079636615,0.000011814098,0.000061034025,0.0009202708,0.00009137702,0.001831919,0.0012736405,0.12045665,0.00013973686],"about_ca_topic_score_codex":0.4850406,"about_ca_topic_score_gemma":0.99475604,"teacher_disagreement_score":0.50971544,"about_ca_system_score_codex":0.000009647848,"about_ca_system_score_gemma":0.0031793748,"threshold_uncertainty_score":0.9891077},"labels":[],"label_agreement":null},{"id":"W2031282523","doi":"10.1139/e01-063","title":"Late Pliocene fossils of Ecuador and their role in the development of the Panamic bioprovince after the rising of Central American Isthmus","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cephalopods and Marine Biology","field":"Agricultural and Biological Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Academy of Natural Sciences of Drexel University; Instituto de Investigaciones Marinas y Costeras","keywords":"Taxon; Boreal; Fauna; Geology; Biota; Paleontology; Neogene; Plio-Pleistocene; Land bridge; Ecology; Oceanography; Geography; Pleistocene; Structural basin; Biological dispersal; Biology","score_opus":0.012820503256704259,"score_gpt":0.1848078165340438,"score_spread":0.17198731327733954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031282523","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975503,0.0008334845,4.5622804e-7,0.0013075504,0.000050475446,0.000064356056,0.000011368732,3.7793552e-7,0.00018165108],"genre_scores_gemma":[0.99974996,0.000039082603,0.00007439587,0.0000946005,0.000026156971,5.151877e-7,1.14370664e-7,2.5516806e-7,0.000014941655],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992442,0.00008198174,0.00027206956,0.00007952285,0.00011112612,0.00021106612],"domain_scores_gemma":[0.9994641,0.000100759156,0.00028154068,0.00003938181,0.000043605,0.00007060869],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005153029,0.000062953404,0.00014139188,0.00002671104,0.00015456152,0.00002223978,0.00042412698,0.00001862292,0.00004455157],"category_scores_gemma":[0.00003915507,0.000015182898,0.000051049727,0.0004195949,0.0009578133,0.00005154191,0.000024558874,0.00007716294,1.3513771e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012743575,0.00002299154,0.7139604,0.000004544259,0.000010381087,0.0000034292382,0.0039952816,0.0000163213,0.014616434,0.00003925884,0.0000089313235,0.26730925],"study_design_scores_gemma":[0.000039453626,0.00014791373,0.9942059,0.000026000607,0.0000028363934,0.00001625074,0.0024111632,0.00005252707,0.0018260344,0.000117113836,0.001118725,0.000036074227],"about_ca_topic_score_codex":0.0082953805,"about_ca_topic_score_gemma":0.28696012,"teacher_disagreement_score":0.28024548,"about_ca_system_score_codex":0.000004446884,"about_ca_system_score_gemma":0.00011188086,"threshold_uncertainty_score":0.9983085},"labels":[],"label_agreement":null},{"id":"W2031292588","doi":"10.1139/e09-045","title":"A new ankylosaur (Dinosauria: Ankylosauria) from the Lower Cretaceous Cloverly Formation of central Montana","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Anatomy; Occiput; Theropoda; Foramen magnum; Paleontology; Occipital bone; Skull; Cretaceous; Biology","score_opus":0.01538622721348714,"score_gpt":0.20220601219496237,"score_spread":0.18681978498147522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031292588","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9801824,0.009081062,0.00030046972,0.0047208546,0.0011560144,0.000080363425,0.00013990847,0.000003816464,0.004335082],"genre_scores_gemma":[0.99762934,0.00008030228,0.0011835571,0.0006954027,0.0003505985,3.173695e-8,0.0000125418965,6.933232e-7,0.00004753001],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99865884,0.00012757174,0.00038697966,0.000135819,0.000237626,0.00045318823],"domain_scores_gemma":[0.998868,0.00018204114,0.00029219143,0.00011692878,0.0000783628,0.00046249075],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00049548905,0.00010799409,0.00020841333,0.00013445357,0.00033034335,0.00005212314,0.0005693541,0.000096079886,0.0014349235],"category_scores_gemma":[0.00014136868,0.00006906767,0.00010394032,0.00032889185,0.00040006687,0.0006337879,0.0000020790997,0.00019769678,0.000022083505],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000096540745,0.000009926688,0.9693418,0.0000016933893,0.00002396225,0.00012306214,0.00097067666,0.0019864272,0.0000894589,0.00051550975,0.004767115,0.022073835],"study_design_scores_gemma":[0.00021285376,0.0007993513,0.9824895,0.000024377985,0.00001947872,0.00020865416,0.0002552713,0.00093312253,0.000044124296,0.005070126,0.00985587,0.000087240485],"about_ca_topic_score_codex":0.021971194,"about_ca_topic_score_gemma":0.5741205,"teacher_disagreement_score":0.55214936,"about_ca_system_score_codex":0.0000032511903,"about_ca_system_score_gemma":0.0013388868,"threshold_uncertainty_score":0.9994779},"labels":[],"label_agreement":null},{"id":"W2031669613","doi":"10.1139/e03-024","title":"A new late-glacial sea-level record for St. George's Bay, Newfoundland","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada; Government of Newfoundland and Labrador; Memorial University of Newfoundland","funders":"","keywords":"Bay; Geology; Sea level; Outwash plain; Radiocarbon dating; Oceanography; Glacial period; Meltwater; Paleontology","score_opus":0.051019881518640224,"score_gpt":0.26042365472390133,"score_spread":0.2094037732052611,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031669613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9725827,0.0013359213,0.0005006782,0.0018645283,0.002651919,0.00016744513,0.00008722347,0.0000047295825,0.020804886],"genre_scores_gemma":[0.98845136,0.000044368924,0.007692357,0.00034506014,0.00030468183,3.3080698e-7,0.000008250379,0.0000024974408,0.0031510731],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983452,0.00015275931,0.00031474704,0.00020170567,0.00023716516,0.0007483991],"domain_scores_gemma":[0.99815536,0.00036515304,0.0001548533,0.00009531666,0.00015174711,0.0010775895],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017282646,0.00012098277,0.00023961371,0.00038869353,0.00072269683,0.00012440585,0.00047249213,0.00012118629,0.0065189414],"category_scores_gemma":[0.00058789115,0.00009420245,0.000097074575,0.0004403388,0.0005143319,0.00036576693,0.000002706803,0.00028701933,0.0001118504],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021029302,0.0000015335778,0.9956546,0.0000042826405,0.0000126160385,0.00006100508,0.00010367683,0.000273953,9.620876e-7,0.0005710757,0.0015320125,0.00176326],"study_design_scores_gemma":[0.00045641483,0.00055412296,0.88526565,0.00001902813,0.000013004918,0.0003941167,0.000117037955,0.00021316425,0.00001623154,0.006756486,0.10605235,0.00014242834],"about_ca_topic_score_codex":0.016094232,"about_ca_topic_score_gemma":0.9438884,"teacher_disagreement_score":0.9277942,"about_ca_system_score_codex":8.8451947e-7,"about_ca_system_score_gemma":0.004995365,"threshold_uncertainty_score":0.99438924},"labels":[],"label_agreement":null},{"id":"W2032063478","doi":"10.1139/e02-021","title":"Regional hydrogeochemistry of the carbonate rock aquifer, southern Manitoba","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Manitoba; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Aquifer; Groundwater recharge; Geochemistry; Glacial period; Carbonate; Structural basin; Pleistocene; Ordovician; Groundwater; Devonian; Carbonate rock; Geomorphology; Paleontology; Sedimentary rock","score_opus":0.022402403810262164,"score_gpt":0.1728445638874125,"score_spread":0.15044216007715033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032063478","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9800116,0.001665335,0.000001483025,0.00064474816,0.00031931602,0.000033094137,0.000040160106,0.0000021154995,0.017282173],"genre_scores_gemma":[0.9987994,0.00001863461,0.00006537476,0.00018660705,0.00014926789,7.638337e-8,0.0000013555272,0.000001612792,0.00077770726],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99884355,0.000034288132,0.00028009867,0.00012862356,0.00038165748,0.000331795],"domain_scores_gemma":[0.99916327,0.00003834845,0.00021397686,0.00014065298,0.000091356116,0.00035238534],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031959297,0.000100332865,0.00014309697,0.000077158715,0.00029797104,0.00007756866,0.000736884,0.000051899184,0.0026608747],"category_scores_gemma":[0.000052777683,0.000063154126,0.00011898244,0.00031231108,0.0004033302,0.00015769407,0.0000065654945,0.0001779572,0.00004386078],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000030556455,0.0000051018656,0.99539214,0.000012094752,0.000014417048,0.00002986757,0.0005052511,0.0016372161,0.00045094197,0.000009352936,0.00083396694,0.0011065864],"study_design_scores_gemma":[0.0011986656,0.00052776805,0.8638779,0.00047589088,0.00010135362,0.003155084,0.009376763,0.01745872,0.02524374,0.0040258174,0.07360402,0.00095426885],"about_ca_topic_score_codex":0.016176399,"about_ca_topic_score_gemma":0.14573048,"teacher_disagreement_score":0.13151424,"about_ca_system_score_codex":0.0000019918155,"about_ca_system_score_gemma":0.00041635745,"threshold_uncertainty_score":0.99825084},"labels":[],"label_agreement":null},{"id":"W2032185087","doi":"10.1139/e10-089","title":"Late Ordovician conodont biostratigraphy and redefinition of the age of oil shale intervals on Southampton IslandEarth Science Sector Contribution 20100054.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Government of Nunavut; Nunavut Research Institute","funders":"Dalhousie University; University of Oxford","keywords":"Conodont; Geology; Ordovician; Paleontology; Oil shale; Biostratigraphy; Stage (stratigraphy); Paleozoic; Group (periodic table); Sedimentary rock; Onlap; Structural basin; Facies","score_opus":0.047311886473021945,"score_gpt":0.20228549908560417,"score_spread":0.15497361261258222,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032185087","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99114895,0.00035133024,0.0000088779225,0.00027818093,0.00032832258,0.000047474477,0.000055262273,0.0000015408976,0.0077800537],"genre_scores_gemma":[0.9996346,0.00006938622,0.00013393351,0.00011700348,0.000025154988,1.3168975e-7,0.0000018379534,6.290365e-7,0.000017279075],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990081,0.000060823422,0.00030371078,0.00012633916,0.00026200985,0.00023897194],"domain_scores_gemma":[0.9992324,0.000054728607,0.00031550444,0.00007499981,0.00015071406,0.00017165516],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009868179,0.00007663654,0.00017071604,0.00019486634,0.00040710648,0.00004973419,0.00027868885,0.00003535641,0.00037163083],"category_scores_gemma":[0.0001841955,0.000043791773,0.000061095605,0.00049653166,0.0017713223,0.00020695756,0.000007187217,0.000098563134,0.0000033978297],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002696875,0.0000078174335,0.9939684,0.0000067830088,0.00000912933,0.0000059634563,0.0013726002,0.00016197312,0.00048202177,0.00078333524,0.00001595254,0.0031590157],"study_design_scores_gemma":[0.00014517423,0.0008167927,0.9946465,0.000080418635,0.000008586971,0.000010701421,0.0005616324,0.00014574696,0.0017960952,0.0014335777,0.0002953331,0.00005946394],"about_ca_topic_score_codex":0.015885904,"about_ca_topic_score_gemma":0.2899967,"teacher_disagreement_score":0.2741108,"about_ca_system_score_codex":0.0000013842478,"about_ca_system_score_gemma":0.00030283423,"threshold_uncertainty_score":0.9906674},"labels":[],"label_agreement":null},{"id":"W2032322665","doi":"10.1139/e03-029","title":"Le bassin de Tizi n'Test (Haut Atlas, Maroc) : exemple d'évolution d'un segment oblique au rift de l'Atlantique central au Trias","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies Worldwide","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Graben; Rift; Half-graben; Structural basin; Extensional definition; Seismology; Paleontology; Tectonics","score_opus":0.012399715058700276,"score_gpt":0.19254345494184288,"score_spread":0.1801437398831426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032322665","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9794064,0.00056210597,0.0004616268,0.0038239395,0.00046463896,0.00010674505,0.0000351349,0.000008200934,0.015131177],"genre_scores_gemma":[0.9961248,0.000054315627,0.0025268456,0.00057092536,0.00025483186,6.018211e-7,0.0000041215144,0.0000021671376,0.00046137627],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99765325,0.000253947,0.00036054433,0.00023156045,0.00029501165,0.0012057184],"domain_scores_gemma":[0.99803984,0.00033510526,0.00019486646,0.000089521905,0.00007710476,0.0012635624],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014117329,0.00016720787,0.0002695921,0.00015088909,0.0010795251,0.00014348538,0.000403254,0.00007835277,0.0010543378],"category_scores_gemma":[0.00071208924,0.00012209144,0.00012454749,0.0005644882,0.0005936217,0.00028188998,0.000007437238,0.00027441754,0.00005446148],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009277427,0.000019647614,0.9909902,0.0000051300162,0.000012696244,0.00009795228,0.00029890466,0.0033324533,0.000043197968,0.0012366154,0.0005733533,0.003380528],"study_design_scores_gemma":[0.00028760667,0.00046399995,0.954381,0.000032324733,0.000012940692,0.00015045506,0.00027751582,0.00044178407,0.00044076404,0.006422485,0.036916606,0.00017250536],"about_ca_topic_score_codex":0.21447176,"about_ca_topic_score_gemma":0.7959165,"teacher_disagreement_score":0.58144474,"about_ca_system_score_codex":0.000028716811,"about_ca_system_score_gemma":0.006251463,"threshold_uncertainty_score":0.99985886},"labels":[],"label_agreement":null},{"id":"W2032545016","doi":"10.1139/e04-094","title":"Flin Flon Belt seismic anisotropy: elastic symmetry, heterogeneity, and shear-wave splitting","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Shear wave splitting; Shear (geology); Seismic anisotropy; Anisotropy; Greenschist; Metamorphic rock; Overburden pressure; Metamorphic facies; Shear zone; Longitudinal wave; Mafic; Petrology; Mineralogy; Geophysics; Seismology; Wave propagation; Geotechnical engineering; Facies; Structural basin; Geomorphology; Mantle (geology); Physics","score_opus":0.02362060511449448,"score_gpt":0.22507825623392658,"score_spread":0.2014576511194321,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032545016","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99142814,0.0023087934,0.00059851754,0.0029557927,0.00043673645,0.00005755757,0.00001860153,0.000015684513,0.0021802012],"genre_scores_gemma":[0.9856456,0.00009285537,0.01176215,0.0021310134,0.00026850423,7.496638e-8,0.0000022238826,0.0000029683986,0.00009464117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986193,0.000073802636,0.00032485244,0.0002094877,0.00029931866,0.0004731992],"domain_scores_gemma":[0.99887675,0.0001068451,0.00017361226,0.00009436039,0.000080035774,0.00066839095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010396264,0.00013127334,0.00019424182,0.0004540609,0.00055458467,0.00026187662,0.00028933652,0.000055535646,0.00040678112],"category_scores_gemma":[0.00014034125,0.000105380226,0.00006573375,0.00035861123,0.0005267128,0.0005826261,0.000009135057,0.00022193402,0.000040883428],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018088253,0.000009744919,0.74535483,0.000023097105,0.000030075082,0.00018142855,0.000628621,0.0046019675,0.00014942407,0.00018740924,0.004847069,0.24396823],"study_design_scores_gemma":[0.0007072546,0.0015428541,0.5306714,0.0003606132,0.00006639084,0.003346744,0.0013199984,0.31739497,0.0068784873,0.0029944472,0.13395327,0.0007635152],"about_ca_topic_score_codex":0.020314708,"about_ca_topic_score_gemma":0.033087455,"teacher_disagreement_score":0.31279302,"about_ca_system_score_codex":0.0000047059752,"about_ca_system_score_gemma":0.00062837295,"threshold_uncertainty_score":0.9862091},"labels":[],"label_agreement":null},{"id":"W2032550651","doi":"10.1139/e06-086","title":"Redescription of <i>Aigialosaurus dalmaticus</i> Kramberger, 1892, a Cenomanian mosasauroid lizard from Hvar Island, Croatia","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Cenomanian; Geology; Paleontology; Lizard; Anatomy; Biology; Cretaceous","score_opus":0.013976121610824887,"score_gpt":0.19109893728976562,"score_spread":0.17712281567894073,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032550651","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.976263,0.004993802,0.00013924953,0.0005158004,0.0011833415,0.00006823859,0.00032156942,0.000005343323,0.016509661],"genre_scores_gemma":[0.99736947,0.00005095597,0.0018846109,0.00016193434,0.00030096268,1.5583879e-7,0.000045372533,0.0000018130762,0.00018470793],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99842656,0.00015583192,0.0005378287,0.00019938541,0.00024128771,0.00043908448],"domain_scores_gemma":[0.99889284,0.00013771087,0.00039935042,0.00012322588,0.00011641961,0.00033046803],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00059907965,0.00013533994,0.0002914785,0.0003066327,0.00037861406,0.000051407427,0.000451583,0.00012238535,0.0021375068],"category_scores_gemma":[0.000092481445,0.00010709804,0.00009886676,0.0003844983,0.0007957189,0.00043114784,0.00000389798,0.00017614874,0.00006392625],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002471146,0.000009022368,0.99440765,0.0000036898211,0.000018494931,0.00007805439,0.0001489628,0.0014128439,0.00033289756,0.00032670217,0.00248229,0.00075465575],"study_design_scores_gemma":[0.00026421936,0.00033865494,0.9807766,0.00003882013,0.000027394544,0.00019587469,0.00015244742,0.0010259748,0.00013503646,0.004455952,0.012451093,0.00013794396],"about_ca_topic_score_codex":0.13856168,"about_ca_topic_score_gemma":0.85601175,"teacher_disagreement_score":0.7174501,"about_ca_system_score_codex":0.000003194569,"about_ca_system_score_gemma":0.0010279076,"threshold_uncertainty_score":0.99877465},"labels":[],"label_agreement":null},{"id":"W2032598234","doi":"10.1139/e04-048","title":"Les écoulements et le transport glaciaires dans la partie septentrionale du Nunavik (Québec)","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université de Montréal; Université du Québec à Montréal","funders":"","keywords":"Geology; Ice stream; Glacial period; Glacier; Peninsula; Oceanography; Geomorphology; Physical geography; Cryosphere; Sea ice; Geography; Archaeology","score_opus":0.025081828604286444,"score_gpt":0.24202606813556793,"score_spread":0.21694423953128147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032598234","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9664517,0.0011089117,0.000050313534,0.005956153,0.00022232941,0.000056031913,0.000029212688,0.000004921197,0.026120447],"genre_scores_gemma":[0.99910086,0.0000587204,0.0003444421,0.00029046077,0.00004620237,3.2543443e-7,0.0000072202374,0.0000017453855,0.0001500058],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986476,0.0001369832,0.00028143148,0.0001630046,0.0002939089,0.00047708236],"domain_scores_gemma":[0.9990187,0.00015311742,0.00011833098,0.000075907315,0.00008837668,0.000545545],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013445023,0.00010612254,0.00017938834,0.00024626125,0.00073079043,0.00006181238,0.00047403484,0.00007956944,0.001855827],"category_scores_gemma":[0.00009799903,0.00008227384,0.00009176284,0.00028352241,0.0013374479,0.00037780026,0.000003109721,0.0002672284,0.00006621836],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009503279,0.0000097929515,0.98847955,0.000003821098,0.00001627763,0.0004295436,0.00073429395,0.008643564,0.0000026713158,0.0013507274,0.000035932877,0.0002842955],"study_design_scores_gemma":[0.00037468938,0.0002121212,0.98810285,0.000027618744,0.000009798278,0.0007277596,0.00071441306,0.00007019363,0.0000490757,0.0014281427,0.008187806,0.0000955388],"about_ca_topic_score_codex":0.2455297,"about_ca_topic_score_gemma":0.9805381,"teacher_disagreement_score":0.73500836,"about_ca_system_score_codex":0.0000015588292,"about_ca_system_score_gemma":0.0065665655,"threshold_uncertainty_score":0.9990653},"labels":[],"label_agreement":null},{"id":"W2032699259","doi":"10.1139/e00-011","title":"Characterization, identity, distribution, and source of late Cenozoic tephra beds in the Klondike district of the Yukon, Canada","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Barrick Gold (Canada); The Scarborough Hospital","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto; University of Calgary","keywords":"Tephra; Geology; Rhyolite; Cenozoic; Basaltic andesite; Volcano; Andesite; Silicic; Tephrochronology; Paleontology; Geochemistry; Volcanic rock; Geomorphology; Structural basin","score_opus":0.006921231007941234,"score_gpt":0.16687035652843518,"score_spread":0.15994912552049395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032699259","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996945,0.0003436041,0.0000095415135,0.0020429816,0.00005806874,0.000037906375,0.00013315973,4.3773971e-7,0.00042926313],"genre_scores_gemma":[0.9995753,0.000051724535,0.00000956082,0.00024360135,0.000023114972,6.932546e-8,0.000012580842,3.9368163e-7,0.0000836385],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989683,0.00008955495,0.00032063748,0.0000867725,0.0003331585,0.00020154602],"domain_scores_gemma":[0.9994102,0.0000882561,0.00018825162,0.00007686993,0.00007803913,0.00015835285],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000535614,0.00006328915,0.00014864828,0.000053496336,0.00021570426,0.00004956473,0.0005087527,0.00002407933,0.0014254872],"category_scores_gemma":[0.00012751743,0.00003140441,0.0000485232,0.0009863947,0.00053659757,0.00018878924,0.000005229392,0.000112597525,0.0000013643247],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002288926,0.0000032158396,0.99591607,0.000003861965,0.000004735827,0.000004605748,0.00011710864,0.0012692937,0.000036775895,0.000033770124,0.000049209135,0.0025590558],"study_design_scores_gemma":[0.00005712076,0.00004057974,0.99375325,0.00001730494,0.000012805131,0.000020339543,0.000109033055,0.000371494,0.000102464095,0.00084958476,0.0046237083,0.000042297663],"about_ca_topic_score_codex":0.70313734,"about_ca_topic_score_gemma":0.98556215,"teacher_disagreement_score":0.28242478,"about_ca_system_score_codex":0.0000017504307,"about_ca_system_score_gemma":0.0006104797,"threshold_uncertainty_score":0.99948734},"labels":[],"label_agreement":null},{"id":"W2032801116","doi":"10.1139/e06-084","title":"Early history of the Midcontinent Rift inferred from geochemistry and sedimentology of the Mesoproterozoic Osler Group, northwestern Ontario","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University; Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Rift; Geochemistry; Conglomerate; Sedimentology; Sedimentary rock; Detritus; Basalt; Proterozoic; Paleontology; Alluvial fan; Structural basin; Tectonics","score_opus":0.012936611894700096,"score_gpt":0.16892896584671382,"score_spread":0.15599235395201372,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032801116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957982,0.0015966195,0.000004419134,0.00061333826,0.0003979961,0.00004626516,0.000014527754,7.966688e-7,0.0015278668],"genre_scores_gemma":[0.9992356,0.000004358257,0.0001432633,0.00019559279,0.00004204102,7.2815524e-8,0.0000012919238,6.3273677e-7,0.00037719178],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988815,0.000046438992,0.0003894315,0.00013653655,0.0002876338,0.00025841853],"domain_scores_gemma":[0.9990215,0.000109377994,0.00038982517,0.0001271358,0.00008482323,0.00026738297],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005388714,0.00009074255,0.0002186789,0.000070716065,0.000113924514,0.000016708635,0.0005263627,0.000060841412,0.002002387],"category_scores_gemma":[0.00005918324,0.000045293957,0.00013505269,0.00020487909,0.0009665664,0.00009884028,0.000017655188,0.00020357688,0.0000013978395],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007648255,0.0000048041634,0.9980295,0.0000028165305,0.000018822648,0.000005723192,0.00063522387,0.000044368364,0.0006239253,0.0000045698416,0.000043578086,0.00057902007],"study_design_scores_gemma":[0.00012500459,0.00008532423,0.99482363,0.00002772864,0.000031214517,0.000016983468,0.00012206862,0.000031289022,0.0010394567,0.00091836194,0.002722471,0.00005648644],"about_ca_topic_score_codex":0.7528618,"about_ca_topic_score_gemma":0.9859376,"teacher_disagreement_score":0.23307578,"about_ca_system_score_codex":0.00000953508,"about_ca_system_score_gemma":0.000587585,"threshold_uncertainty_score":0.9989099},"labels":[],"label_agreement":null},{"id":"W2033092816","doi":"10.1139/e09-067","title":"A new basal hadrosauriform dinosaur (Ornithischia: Iguanodontia) from the Early Cretaceous of northwestern China","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Cretaceous; Paleontology; Geology; Sister group; Skull; Clade; Phylogenetic tree; Biology","score_opus":0.013754726533761303,"score_gpt":0.20031246001937777,"score_spread":0.18655773348561647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033092816","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9848371,0.005540068,0.00011724826,0.0037715654,0.00080055126,0.00005997036,0.00011229335,0.0000038606586,0.004757334],"genre_scores_gemma":[0.99781924,0.000046583795,0.0010811797,0.00062304054,0.00030191563,3.9640835e-8,0.000008171881,0.0000010376243,0.000118812124],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99866295,0.00010955396,0.00037413184,0.00016886806,0.00025107033,0.00043342196],"domain_scores_gemma":[0.9988219,0.00016514266,0.00030217998,0.00013643106,0.00006351209,0.00051084434],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00055669027,0.00012731322,0.0002475873,0.00016209228,0.00046554388,0.00006516473,0.0007872358,0.0001011018,0.0012539062],"category_scores_gemma":[0.000088307424,0.000078288365,0.000113669594,0.00033898395,0.00066678727,0.00043555282,0.000003557609,0.0002853198,0.00004916713],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023125023,0.0000028656073,0.99159265,5.805624e-7,0.000015757403,0.00006002032,0.0005448369,0.00037045247,0.000019803396,0.000066671295,0.0006297516,0.006673462],"study_design_scores_gemma":[0.00018652584,0.00072026515,0.9919135,0.000025836898,0.000019501602,0.00016838439,0.00012452443,0.00015197805,0.000028971157,0.0031022646,0.0034603425,0.000097906894],"about_ca_topic_score_codex":0.11108818,"about_ca_topic_score_gemma":0.85754627,"teacher_disagreement_score":0.7464581,"about_ca_system_score_codex":0.0000014892205,"about_ca_system_score_gemma":0.0016908585,"threshold_uncertainty_score":0.99965906},"labels":[],"label_agreement":null},{"id":"W2033254104","doi":"10.1139/e03-063","title":"Crustal recycling during subduction at the Eocene Cordilleran margin of North America: a petrogenetic study from the southwestern Yukon","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Geochemistry; Lile; Andesite; Subduction; Andesites; Basalt; Pyroclastic rock; Partial melting; Continental crust; Crust; Rhyolite; Continental margin; Lava; Basaltic andesite; Volcanic rock; Lithophile; Volcano; Paleontology; Tectonics","score_opus":0.018041983334447266,"score_gpt":0.18837033966886718,"score_spread":0.17032835633441992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033254104","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974298,0.0014481553,0.0000065573035,0.00046281566,0.0002152158,0.0000779793,0.000032721447,0.0000018353022,0.00032491295],"genre_scores_gemma":[0.9996592,0.000034907363,0.00008712076,0.00009020451,0.00008324818,2.3313424e-7,0.0000026545276,0.0000011719374,0.00004125494],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998476,0.0002144206,0.0003477937,0.00018093061,0.0004374709,0.0003433458],"domain_scores_gemma":[0.99900246,0.00017802189,0.00027821478,0.00013343168,0.00011156312,0.0002963062],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000670686,0.00010672402,0.00020456493,0.00008695313,0.00067801785,0.0000770918,0.00042581893,0.000020147621,0.0030472332],"category_scores_gemma":[0.0002727487,0.000051219242,0.00012232698,0.0006777649,0.0006706743,0.00010772234,0.00000893307,0.00017029187,0.000024746329],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010328811,0.000007303063,0.9889113,9.719307e-7,0.000025126266,0.000019135849,0.00041984758,0.009030696,0.00004777058,6.1936487e-7,0.000006554319,0.0015204004],"study_design_scores_gemma":[0.00013990904,0.00021744374,0.9959507,0.000010376331,0.000042488453,0.000036664624,0.002595009,0.00020472507,0.00020311913,0.00017817855,0.00034717843,0.00007419143],"about_ca_topic_score_codex":0.06583779,"about_ca_topic_score_gemma":0.808438,"teacher_disagreement_score":0.7426002,"about_ca_system_score_codex":0.0000033829442,"about_ca_system_score_gemma":0.0002667318,"threshold_uncertainty_score":0.9978641},"labels":[],"label_agreement":null},{"id":"W2033875249","doi":"10.1139/e03-080","title":"Early juvenile pterosaurs (Pterodactyloidea:<i>Pterodaustro guinazui</i>) from the Lower Cretaceous of central Argentina","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Consejo Nacional de Investigaciones Científicas y Técnicas; Universidad Nacional de San Luis; National Geographic Society","keywords":"Postcrania; Allometry; Skull; Cretaceous; Geology; Juvenile; Paleontology; Sauropoda; Anatomy; Forelimb; Biology; Taxon","score_opus":0.016832733786100892,"score_gpt":0.2020876244284726,"score_spread":0.18525489064237172,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033875249","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99040705,0.0037426383,0.000060859893,0.0018699447,0.0019112926,0.00006681903,0.00017933466,0.0000036316599,0.0017584449],"genre_scores_gemma":[0.99848354,0.00004646415,0.000752273,0.00041139792,0.00024132991,1.3759545e-7,0.00000826603,0.0000015902946,0.000055016953],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998391,0.000118464035,0.00043473445,0.00019521704,0.00024933528,0.0006112832],"domain_scores_gemma":[0.9987855,0.00015846376,0.00033377775,0.00015447031,0.000101001475,0.00046678944],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000624686,0.00013517015,0.0002549418,0.00013308956,0.0004604284,0.000062372404,0.00078222225,0.00009603217,0.0016403976],"category_scores_gemma":[0.00014964915,0.00008684667,0.00013126613,0.00028944545,0.0014614478,0.0003562589,0.00000621086,0.00025424265,0.0000642101],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031252664,0.000008410934,0.9960679,0.0000012230369,0.000023481662,0.00009685379,0.00039646358,0.0019877695,0.00007642755,0.00008240696,0.00019338285,0.0010344438],"study_design_scores_gemma":[0.00029298518,0.0006611889,0.990468,0.000034410907,0.000020376914,0.00016499366,0.0002021785,0.0000290885,0.00012984152,0.0016236899,0.006272357,0.00010087141],"about_ca_topic_score_codex":0.04856448,"about_ca_topic_score_gemma":0.51990825,"teacher_disagreement_score":0.4713438,"about_ca_system_score_codex":0.0000037850846,"about_ca_system_score_gemma":0.0012173454,"threshold_uncertainty_score":0.9992722},"labels":[],"label_agreement":null},{"id":"W2034031356","doi":"10.1139/e06-052","title":"Proterozoic evolution of the western margin of the Wyoming craton: implications for the tectonic and magmatic evolution of the northern Rocky Mountains","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":186,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Craton; Terrane; Zircon; Archean; Geochemistry; Batholith; Proterozoic; Basement; Mafic; Laurentia; Magmatism; Paleontology; Tectonics; Paleozoic","score_opus":0.010448223744693643,"score_gpt":0.187668348017145,"score_spread":0.17722012427245135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034031356","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926258,0.0015979334,0.00016795589,0.0050595864,0.00008635625,0.00024119334,0.00005092481,7.8783665e-7,0.00016946331],"genre_scores_gemma":[0.99976975,0.000004558018,0.00007164162,0.000042578664,0.00003501269,0.0000012943134,3.9272618e-7,8.2493455e-7,0.000073947136],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99906677,0.00008284088,0.0003401321,0.00009689887,0.00021909257,0.00019424921],"domain_scores_gemma":[0.9989647,0.00017699061,0.00046057018,0.0001674105,0.00016505107,0.00006527089],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005574844,0.000071030736,0.00014042151,0.00006064347,0.0005446452,0.000029652174,0.0006528821,0.00003217703,0.00005808147],"category_scores_gemma":[0.00016663375,0.00002683135,0.00014033665,0.00067631755,0.00093291386,0.00010230948,0.000016425109,0.00010615692,5.2767456e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026296375,0.0000039196066,0.992417,0.00001106946,0.000008519306,4.2875943e-8,0.000057559824,0.005986592,0.0006517663,0.00022472521,0.000010601222,0.00062558457],"study_design_scores_gemma":[0.000074786825,0.000055286062,0.98536205,0.000047880505,0.000046600122,0.000016132228,0.00022136176,0.0025555715,0.0005678589,0.010872362,0.00014353462,0.000036575108],"about_ca_topic_score_codex":0.04657213,"about_ca_topic_score_gemma":0.7176787,"teacher_disagreement_score":0.6711066,"about_ca_system_score_codex":0.000007166699,"about_ca_system_score_gemma":0.00055497413,"threshold_uncertainty_score":0.9597768},"labels":[],"label_agreement":null},{"id":"W2034125579","doi":"10.1139/e05-093","title":"Spectral and dynamical hints on the time scale of preparation of the 5 April 2003 explosion at Stromboli volcano","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Earthquake Detection and Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Strombolian eruption; Volcano; Seismology; Geology; Event (particle physics); Scale (ratio); Lava; Impact crater; Geophysics; Astrobiology; Physics; Geography; Cartography","score_opus":0.00950374545983816,"score_gpt":0.19482465404652452,"score_spread":0.18532090858668637,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034125579","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957165,0.00020035915,0.0000060618845,0.00063390395,0.00014804273,0.00005291259,0.000029255092,0.0000011168239,0.003211852],"genre_scores_gemma":[0.999277,0.000009698721,0.000087402506,0.000066840286,0.000048426326,5.788191e-8,0.0000012641467,9.0546945e-7,0.0005083793],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99904966,0.00010682468,0.00025745403,0.00009826442,0.00032381518,0.00016400489],"domain_scores_gemma":[0.99937487,0.00006806776,0.00023851267,0.000089783214,0.000092391354,0.00013638749],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00054773927,0.000064225664,0.00013309259,0.00013642976,0.00032409816,0.000045009736,0.00021855137,0.000028858482,0.0011933049],"category_scores_gemma":[0.000076506694,0.0000333708,0.00006802118,0.00051722507,0.00057220407,0.00014253214,0.00000396729,0.00008903878,0.000012473932],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023850742,0.000009742944,0.98392475,0.0000040478863,0.000014687119,0.0000030742956,0.00023305645,0.010800486,0.0021628302,0.00019109453,0.0007044509,0.0019279133],"study_design_scores_gemma":[0.00008474358,0.00026426505,0.98285127,0.00003318253,0.000018073706,0.000028147047,0.00013261907,0.010646658,0.0048998594,0.0003223825,0.0006666518,0.00005216483],"about_ca_topic_score_codex":0.0075959708,"about_ca_topic_score_gemma":0.31008688,"teacher_disagreement_score":0.3024909,"about_ca_system_score_codex":0.0000023905009,"about_ca_system_score_gemma":0.00030679497,"threshold_uncertainty_score":0.99971974},"labels":[],"label_agreement":null},{"id":"W2034181668","doi":"10.1139/cjes-2014-0153","title":"Petrology and geochronology of Paleoproterozoic intrusive rocks, Kiggavik uranium camp, Nunavut","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Carleton University","funders":"","keywords":"Geology; Zircon; Geochemistry; Geochronology; Porphyritic; Igneous rock; Titanite; Outcrop; Conglomerate; Rhyolite; Petrology; Volcanic rock; Sedimentary rock; Paleontology","score_opus":0.017774907109535852,"score_gpt":0.19797744076454832,"score_spread":0.18020253365501246,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034181668","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99250835,0.003200972,0.000040979794,0.0015537206,0.0002455637,0.000040243365,0.000020165862,0.0000022673528,0.0023877223],"genre_scores_gemma":[0.99886423,0.000041324853,0.0006753135,0.00027890722,0.0000961747,1.3740001e-7,0.0000028734732,7.813275e-7,0.000040254865],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987867,0.00009089644,0.00033838872,0.00017949827,0.00021294123,0.00039156165],"domain_scores_gemma":[0.99852943,0.000108372806,0.0002433106,0.00007835841,0.00020486626,0.0008356427],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00063187775,0.000105429746,0.00031595008,0.00027872098,0.00013755471,0.00003870007,0.00035712784,0.00007884881,0.0029154464],"category_scores_gemma":[0.00037550312,0.00006944331,0.00006911456,0.00039048557,0.0010981591,0.00018691906,0.00001065606,0.00018181342,0.00003441721],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001417551,0.0000033127171,0.99508035,0.0000038475696,0.000016500142,0.00005491742,0.00021549189,0.0012910365,0.00004742837,0.000053994456,0.00007713333,0.0031418358],"study_design_scores_gemma":[0.00030645283,0.0011680735,0.97910106,0.000015498048,0.00003297482,0.00040403087,0.0007806119,0.0009801654,0.00031781849,0.014797261,0.0019651826,0.00013088612],"about_ca_topic_score_codex":0.037548434,"about_ca_topic_score_gemma":0.6197229,"teacher_disagreement_score":0.5821745,"about_ca_system_score_codex":0.0000014280156,"about_ca_system_score_gemma":0.00073102384,"threshold_uncertainty_score":0.99799603},"labels":[],"label_agreement":null},{"id":"W2034607156","doi":"10.1139/e09-006","title":"New insights on faults in the Peace River Arch region, northwest Alberta, based on existing well-log data and refined trend surface analysis","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"University of Calgary","keywords":"Geology; Graben; Paleozoic; Permian; Mesozoic; Cretaceous; Paleontology; Feature (linguistics); Tectonics; Structural basin","score_opus":0.03992818086706101,"score_gpt":0.25482693503330733,"score_spread":0.21489875416624632,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034607156","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9853234,0.00043195015,0.0006455384,0.004554802,0.00008345857,0.00005171461,0.0000061111527,0.0000059511226,0.008897066],"genre_scores_gemma":[0.998985,0.000050684015,0.0003331247,0.00040811073,0.000051528546,1.0391506e-7,0.000010364453,0.0000032882074,0.00015779701],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99891067,0.000079735066,0.00027394912,0.00018889888,0.0003156453,0.00023110285],"domain_scores_gemma":[0.99909484,0.00017269609,0.00008513355,0.0002832707,0.000028530472,0.000335542],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005093995,0.000112902904,0.0001995224,0.0008017167,0.00020184045,0.00012079296,0.0005728823,0.000037133046,0.000024635],"category_scores_gemma":[0.000108553235,0.000073389856,0.000057045752,0.0019648322,0.00010838786,0.00025653216,0.0000048901284,0.00020698497,0.0000030625097],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000071273907,0.000008052868,0.032064028,0.0000021007686,0.0000359796,0.00011214945,0.0019882037,0.96356106,0.000014412391,0.00006924585,0.0008015751,0.0013360899],"study_design_scores_gemma":[0.00040375337,0.000254226,0.18335949,0.000080974314,0.00011125942,0.00001624922,0.0007424386,0.79909915,0.00003774748,0.0000765624,0.015607093,0.00021104622],"about_ca_topic_score_codex":0.016190354,"about_ca_topic_score_gemma":0.82153684,"teacher_disagreement_score":0.8053465,"about_ca_system_score_codex":0.000011470696,"about_ca_system_score_gemma":0.00027768794,"threshold_uncertainty_score":0.9903609},"labels":[],"label_agreement":null},{"id":"W2034693675","doi":"10.1139/e99-113","title":"Glaciological reconstruction of the Laurentide Ice Sheet: physical processes and modelling challenges","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":209,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto; University of British Columbia","funders":"","keywords":"Ice sheet; Geology; Ice-sheet model; Ice stream; Glacial period; Antarctic sea ice; Glacier morphology; Ice shelf; Pleistocene; Glacier; Paleoclimatology; Geomorphology; Paleontology; Cryosphere; Geophysics; Oceanography; Sea ice; Climate change","score_opus":0.04774082897130159,"score_gpt":0.23580270792902017,"score_spread":0.1880618789577186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034693675","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98759353,0.00517575,0.0000042562606,0.0011618088,0.00012628609,0.000036492802,0.000004774383,0.0000013634824,0.0058957166],"genre_scores_gemma":[0.9989744,0.0006515895,0.00023070426,0.000035889327,0.00005677626,8.73993e-8,2.677286e-7,5.119206e-7,0.000049793853],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99923754,0.00012135735,0.00015303952,0.000113011505,0.00013979031,0.00023525042],"domain_scores_gemma":[0.99940854,0.0001944033,0.000085988075,0.00005292003,0.00007705582,0.00018110964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005391271,0.00005845089,0.0001411309,0.00008921854,0.00033320338,0.00002478421,0.00026880656,0.000051584055,0.00075668126],"category_scores_gemma":[0.00009615178,0.000033086555,0.0000349759,0.00022667026,0.0015129915,0.00020447813,0.0000025350876,0.00018825427,0.000008932627],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000840836,0.000002408496,0.9866339,0.000012278451,0.000005392566,0.000006291219,0.00036993416,0.007056439,0.000001218318,0.0001100595,0.0000028322463,0.005790834],"study_design_scores_gemma":[0.00013614977,0.0003294629,0.98174185,0.0000779181,0.000013345462,0.001035842,0.0006736049,0.008322802,0.00008737515,0.0069048945,0.0005901136,0.0000866502],"about_ca_topic_score_codex":0.0007643622,"about_ca_topic_score_gemma":0.13242073,"teacher_disagreement_score":0.13165636,"about_ca_system_score_codex":1.4385589e-7,"about_ca_system_score_gemma":0.00054927036,"threshold_uncertainty_score":0.88341033},"labels":[],"label_agreement":null},{"id":"W2034918341","doi":"10.1139/e01-044","title":"Petrogenesis of the Early Proterozoic Matachewan dyke swarm, Canada, and implications for magma emplacement and subsequent deformation","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"College of Family Physicians of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Magma; Crust; Fractional crystallization (geology); Phenocryst; Geochemistry; Plagioclase; Plume; Petrology; Basalt; Volcano; Volcanic rock; Paleontology; Quartz","score_opus":0.01880111961239185,"score_gpt":0.19943019406392573,"score_spread":0.18062907445153387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034918341","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99549985,0.00058822567,0.000040128878,0.0034956057,0.000049194292,0.0001073461,0.00008932711,7.0723195e-7,0.00012963242],"genre_scores_gemma":[0.99941087,0.000025385378,0.00033598556,0.00016929614,0.00001942555,8.1503623e-7,0.000002603933,5.178719e-7,0.000035092093],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99932104,0.00002586378,0.00022442659,0.000090250345,0.00013849622,0.00019990865],"domain_scores_gemma":[0.9993507,0.000052720847,0.000160177,0.000058063626,0.000094869756,0.00028342594],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032687793,0.00005966392,0.0001105183,0.00007159872,0.00031255514,0.00005520237,0.0001897247,0.000019024208,0.0001769101],"category_scores_gemma":[0.00006158767,0.000033676624,0.000038199192,0.00025517892,0.0002639377,0.00013613133,0.000005228417,0.00004592871,3.4241918e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000035364367,0.0000012511216,0.9972581,0.0000051595503,0.000006995849,7.565849e-7,0.00005140681,0.00026375309,0.00005363115,0.000054248274,0.000021959828,0.0022791582],"study_design_scores_gemma":[0.00007669455,0.00010825997,0.99625754,0.0000099839735,0.000018555042,0.000063346924,0.00011602304,0.00031178896,0.0003348745,0.0019226853,0.0007331807,0.00004703976],"about_ca_topic_score_codex":0.6873415,"about_ca_topic_score_gemma":0.99208456,"teacher_disagreement_score":0.30474305,"about_ca_system_score_codex":0.0000025784718,"about_ca_system_score_gemma":0.00056510954,"threshold_uncertainty_score":0.3147405},"labels":[],"label_agreement":null},{"id":"W2035458323","doi":"10.1139/e09-064","title":"Évolution géodynamique externe et implication sur le devenir de l’or en contexte sub-sahélien","year":2010,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies Worldwide","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Humanities; Geology; Philosophy","score_opus":0.020415954739429445,"score_gpt":0.21922435271158697,"score_spread":0.19880839797215752,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2035458323","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96296585,0.002979076,0.000393231,0.025342816,0.0018855784,0.00013133184,0.00006641139,0.0000066311004,0.0062290826],"genre_scores_gemma":[0.9932678,0.000341461,0.0017246574,0.0009304727,0.0005034941,9.526543e-7,0.0000049097484,0.0000031928985,0.0032230874],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979016,0.00028620075,0.000435952,0.00027143877,0.00028072533,0.0008240751],"domain_scores_gemma":[0.99758315,0.00068697566,0.00029542478,0.000120361394,0.00023083754,0.001083274],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002226166,0.00018803915,0.00029933066,0.0001632071,0.00073535426,0.0002416185,0.00062405743,0.0001524171,0.0013954302],"category_scores_gemma":[0.0011040345,0.00013465527,0.00013680832,0.00063211663,0.001692526,0.00071744237,0.000017122411,0.00063325855,0.00016578664],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007857734,0.00009810088,0.77108866,0.000047562608,0.00006653732,0.00034383038,0.0012952426,0.0049499753,0.0036654382,0.02265718,0.00274339,0.19296548],"study_design_scores_gemma":[0.00023676039,0.00055522734,0.88548553,0.00006673431,0.000017750332,0.00036167647,0.00012295072,0.002416414,0.0002971086,0.009599169,0.100646146,0.00019455414],"about_ca_topic_score_codex":0.19063592,"about_ca_topic_score_gemma":0.934788,"teacher_disagreement_score":0.744152,"about_ca_system_score_codex":0.000009398111,"about_ca_system_score_gemma":0.0040744017,"threshold_uncertainty_score":0.99951744},"labels":[],"label_agreement":null},{"id":"W2035506442","doi":"10.1139/e08-014","title":"The Middle Cambrian Mount Roosevelt Formation (new) of northeastern British Columbia: evidence for rifting and development of the Kechika Graben System","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"","keywords":"Geology; Conglomerate; Graben; Dolostone; Siltstone; Marine transgression; Paleontology; Rift; Alluvial fan; Sedimentary rock; Geomorphology; Geochemistry; Carbonate rock; Facies; Structural basin","score_opus":0.06723016233602266,"score_gpt":0.20839883774243856,"score_spread":0.1411686754064159,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2035506442","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964773,0.0025199975,0.00022421798,0.0001464649,0.00020719068,0.00013282808,0.000018569874,0.0000013941286,0.00027203248],"genre_scores_gemma":[0.9976499,0.000045335717,0.002105034,0.000021511682,0.000027013557,3.894677e-7,8.4017387e-7,7.063317e-7,0.00014928376],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990254,0.00003812858,0.0004285644,0.000067098124,0.0002404096,0.0002003988],"domain_scores_gemma":[0.9989825,0.00019197691,0.00039126648,0.0000544985,0.00020626144,0.00017351194],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0009355018,0.000046395722,0.00012087839,0.000037401944,0.0019735084,0.00025142863,0.0003475434,0.000026183487,0.000025928326],"category_scores_gemma":[0.00026524434,0.000031835916,0.000037418886,0.0002154196,0.00034807448,0.0004349022,0.000005333983,0.000060963735,9.4499643e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000042868774,0.0000013166673,0.9800776,0.0000648787,0.0000064578535,0.0000016594242,0.0011431291,0.00061101146,0.000004293967,0.000025144069,0.00006226121,0.017997935],"study_design_scores_gemma":[0.00010229776,0.0001082719,0.992456,0.00034100414,0.000005973934,0.0003475771,0.0021063269,0.0014412964,0.0000504859,0.00010805311,0.0028791178,0.0000535943],"about_ca_topic_score_codex":0.084440604,"about_ca_topic_score_gemma":0.946458,"teacher_disagreement_score":0.8620174,"about_ca_system_score_codex":0.0000029888586,"about_ca_system_score_gemma":0.0014558877,"threshold_uncertainty_score":0.9993258},"labels":[],"label_agreement":null},{"id":"W2035872927","doi":"10.1139/e01-021","title":"Paleomagnetism of the Quottoon plutonic complex in the Coast Mountains of British Columbia and southeastern Alaska: evidence for tilting during uplift","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Transect; Sill; Paleomagnetism; Pluton; Inlet; Hornblende; Clockwise; Geomorphology; Seismology; Oceanography; Paleontology; Geochemistry; Fold (higher-order function); Tectonics","score_opus":0.03086465589165695,"score_gpt":0.24691033202790003,"score_spread":0.21604567613624306,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2035872927","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932253,0.005969594,0.000008355057,0.00033106274,0.0000985004,0.00016749937,0.00005139741,4.461599e-7,0.00014787409],"genre_scores_gemma":[0.9990743,0.0003684,0.00018218366,0.00006441999,0.000062815045,0.0000028893844,6.619528e-7,0.0000037898794,0.00024054665],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990488,0.00007178647,0.00029861473,0.0001448572,0.00016784709,0.00026807757],"domain_scores_gemma":[0.9993675,0.000065654844,0.00024693576,0.00012488566,0.00010842402,0.00008665074],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006235843,0.000069497415,0.00016259454,0.00004663159,0.00025377044,0.00007715301,0.0004250728,0.000042020576,0.000015003081],"category_scores_gemma":[0.00018870323,0.00006220063,0.00007249808,0.00019247747,0.00070810947,0.000016309346,0.000038022525,0.00007398169,1.0728731e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009432665,0.0000080886275,0.990098,0.000034654473,0.000007914491,0.00000979436,0.00058429013,0.00008196562,0.007894113,0.000004070024,0.00012797308,0.0011397043],"study_design_scores_gemma":[0.00036546355,0.00047785765,0.9952893,0.00021815307,0.00001438778,0.0003113452,0.0021091735,0.000040286355,0.00016147514,0.00004417643,0.0008969901,0.000071359784],"about_ca_topic_score_codex":0.023208529,"about_ca_topic_score_gemma":0.86641,"teacher_disagreement_score":0.8432015,"about_ca_system_score_codex":0.0000013406192,"about_ca_system_score_gemma":0.00032691096,"threshold_uncertainty_score":0.98329604},"labels":[],"label_agreement":null},{"id":"W2036257061","doi":"10.1139/e06-024","title":"Simulated weathering of dinosaur tracks and the implications for their characterization","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"University of Calgary","keywords":"Geology; Weathering; Erosion; Paleontology; Landform; Quadrupedalism","score_opus":0.017675764548812374,"score_gpt":0.2090817348188167,"score_spread":0.19140597027000433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036257061","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951933,0.001314039,0.00040618255,0.0020368467,0.00014383276,0.00007579779,0.000086501874,0.0000013267819,0.0007421724],"genre_scores_gemma":[0.99964243,0.000034506054,0.00015333851,0.000068468944,0.00006452925,1.6280258e-7,0.000010259146,4.522358e-7,0.000025835356],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99954814,0.00004253777,0.00017739872,0.000061477505,0.00003038267,0.00014008104],"domain_scores_gemma":[0.99947244,0.0002132536,0.0001458451,0.00003664625,0.000061916915,0.000069897535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004748696,0.00004118434,0.00010032102,0.0000855274,0.0003200224,0.000018848395,0.00014624007,0.000033115248,0.000057131118],"category_scores_gemma":[0.00005181794,0.000023305478,0.000033253324,0.00013507993,0.0007776328,0.00014200062,9.122782e-7,0.000042869462,6.032914e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014345104,0.0000012948182,0.99273264,0.0000018303241,0.0000052669893,3.6565183e-7,0.00009845469,0.0016973898,0.0003450114,0.0014294882,0.000007667648,0.0036662456],"study_design_scores_gemma":[0.00019755053,0.00007641991,0.99019825,0.0000062188506,0.0000059789218,0.000049900038,0.000049213006,0.003367782,0.00003692351,0.004196841,0.0017852971,0.000029649846],"about_ca_topic_score_codex":0.0033107514,"about_ca_topic_score_gemma":0.14117852,"teacher_disagreement_score":0.13786778,"about_ca_system_score_codex":3.6804383e-7,"about_ca_system_score_gemma":0.00022040847,"threshold_uncertainty_score":0.8744927},"labels":[],"label_agreement":null},{"id":"W2036325863","doi":"10.1139/e10-053","title":"Early Devonian stylonurine eurypterids from Arctic Canada","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Insect and Arachnid Ecology and Behavior","field":"Biochemistry, Genetics and Molecular Biology","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"British Geological Survey; University of Bristol; Palaeontographical Society","keywords":"Devonian; Paleontology; Geology; Fluvial; Arctic; Sedimentary depositional environment; Terrane; Carapace; Taxon; Oceanography; Structural basin; Ecology; Biology; Tectonics; Crustacean","score_opus":0.007824274782271217,"score_gpt":0.21087592278067413,"score_spread":0.20305164799840292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036325863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99778235,0.00012914267,0.0000062855806,0.00035051684,0.0012487682,0.000025244864,0.000020968866,6.7049086e-7,0.00043607675],"genre_scores_gemma":[0.998514,0.000003963311,0.0004204264,0.00039332127,0.00037925885,4.6256565e-7,0.0000039693036,0.0000035397636,0.0002810595],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99937654,0.000018631212,0.00015023733,0.00011184393,0.00009194701,0.00025081483],"domain_scores_gemma":[0.99938357,0.000008325679,0.00008538149,0.000089532514,0.00009061931,0.00034258206],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018377723,0.000071609844,0.00008683706,0.00005910461,0.00024909945,0.000045113586,0.0002814939,0.00006535837,0.00046900776],"category_scores_gemma":[0.00006505535,0.000059246442,0.000039900886,0.000077182325,0.0002558475,0.000009697783,0.0000098289765,0.00017389691,0.000004121715],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009253232,0.000007240064,0.7982818,0.0000013003772,0.000012326157,0.00012001254,0.000048300735,0.000008491756,0.20025045,0.00005738959,0.00052992086,0.00067353575],"study_design_scores_gemma":[0.0001959742,0.00034125248,0.9138613,0.00000791139,0.000011381998,0.0001414153,0.000055133634,0.000003684295,0.053165637,0.00007318707,0.032013584,0.00012953814],"about_ca_topic_score_codex":0.45520416,"about_ca_topic_score_gemma":0.9949944,"teacher_disagreement_score":0.5397903,"about_ca_system_score_codex":0.0000025763777,"about_ca_system_score_gemma":0.0030701763,"threshold_uncertainty_score":0.54842365},"labels":[],"label_agreement":null},{"id":"W2036396833","doi":"10.1139/e02-002","title":"Detrital zircon geochronology of the Taku terrane, southeast Alaska","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Terrane; Zircon; Geology; Geochronology; Geochemistry; Carboniferous; Tectonics; Paleontology","score_opus":0.021347105496923872,"score_gpt":0.17475970933447788,"score_spread":0.153412603837554,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036396833","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9809835,0.0017631131,0.000012695048,0.0025883182,0.00030438526,0.00003186567,0.000028680326,0.0000018298158,0.0142855905],"genre_scores_gemma":[0.9991629,0.000016991047,0.00037239466,0.00020568738,0.000082104314,5.1335086e-8,6.752359e-7,6.42749e-7,0.00015852158],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99889565,0.00006706652,0.0003038759,0.00012680139,0.00025424166,0.00035238027],"domain_scores_gemma":[0.99914545,0.00009399948,0.00021004061,0.000099789744,0.00008553568,0.00036516483],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003464261,0.00008514001,0.00019641324,0.00016844276,0.00026720398,0.00004255527,0.0006323559,0.000052980322,0.025579266],"category_scores_gemma":[0.00021513696,0.00004528027,0.00015941207,0.00064056454,0.001134672,0.00014771223,0.0000071949944,0.00017294883,0.00008200573],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000019271588,0.0000054578436,0.9952716,0.0000026123807,0.000012467533,0.00001763974,0.0001308247,0.0011478551,0.00023279684,0.000050971263,0.00022660375,0.0028992256],"study_design_scores_gemma":[0.00018097543,0.00035451012,0.9887602,0.000028368206,0.000030948,0.00023832514,0.0007452011,0.0012582479,0.001654415,0.003481313,0.003137557,0.00012995904],"about_ca_topic_score_codex":0.010828098,"about_ca_topic_score_gemma":0.25044945,"teacher_disagreement_score":0.23962134,"about_ca_system_score_codex":8.328859e-7,"about_ca_system_score_gemma":0.0001848764,"threshold_uncertainty_score":0.9957589},"labels":[],"label_agreement":null},{"id":"W2036596166","doi":"10.1139/e09-062","title":"Mesoproterozoic carbonate systems in the Borden Basin, Nunavut","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"","keywords":"Dolostone; Geology; Paleontology; Lithology; Facies; Graben; Carbonate; Shoal; Carbonate platform; Arctic; Bay; Sedimentary rock; Structural basin; Geochemistry; Geomorphology; Carbonate rock; Oceanography","score_opus":0.027034801645016437,"score_gpt":0.20856597974793645,"score_spread":0.18153117810292002,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036596166","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96981966,0.0051377104,0.000008162216,0.008221634,0.0005186237,0.00011598972,0.000005483863,0.0000022387296,0.01617049],"genre_scores_gemma":[0.9987895,0.00006523443,0.00007979916,0.00090366206,0.00013134336,1.7712243e-7,9.185482e-7,3.7189568e-7,0.00002900515],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989776,0.00010666624,0.00023327586,0.00009663172,0.000270088,0.00031572432],"domain_scores_gemma":[0.9995309,0.000063873194,0.00010919651,0.00005798147,0.000052392024,0.00018565293],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001310484,0.00006904878,0.00013130068,0.00013522337,0.00033634782,0.00021589732,0.00040734536,0.000029987059,0.0001831857],"category_scores_gemma":[0.000102800186,0.000036279984,0.000037736423,0.00046564284,0.00017977228,0.00026484826,0.0000012622214,0.00013683568,0.00002349105],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000067889123,0.000004606418,0.965467,0.0000026252317,0.0000042603133,0.00018358552,0.0011761304,0.022112915,0.0000027115216,0.00059781875,0.0006034068,0.009838175],"study_design_scores_gemma":[0.000078817655,0.00043288808,0.9804403,0.000020952353,0.0000029656635,0.0000777024,0.0015211051,0.001632085,0.0000013902408,0.0015423734,0.014189625,0.000059775834],"about_ca_topic_score_codex":0.045355786,"about_ca_topic_score_gemma":0.4518973,"teacher_disagreement_score":0.40654153,"about_ca_system_score_codex":0.0000014789798,"about_ca_system_score_gemma":0.00026231367,"threshold_uncertainty_score":0.9610013},"labels":[],"label_agreement":null},{"id":"W2036672823","doi":"10.1139/e02-071","title":"Origin of the Odd-twins anomaly: magnetic effect of a unique stratigraphic marker in the Appalachian foreland basin, Gulf of St. Lawrence","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada; Saint Mary's University; University of Alberta","funders":"","keywords":"Foreland basin; Geology; Orogeny; Ordovician; Devonian; Outcrop; Paleontology; Magnetic anomaly; Paleozoic; Anomaly (physics); Structural basin; Laurentia; Stratigraphy; Tectonics","score_opus":0.012525380576483483,"score_gpt":0.1835186689872129,"score_spread":0.17099328841072942,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036672823","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930139,0.001402331,0.0000034868367,0.00081700645,0.00006283787,0.000093564515,0.000042901775,6.3173803e-7,0.0045633023],"genre_scores_gemma":[0.9996628,0.000049406368,0.00013943372,0.000091885784,0.00001684124,2.3389376e-7,8.731076e-7,6.3730613e-7,0.00003787673],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99852985,0.0002697572,0.00042989507,0.00012455223,0.0003758611,0.00027007732],"domain_scores_gemma":[0.99890476,0.00040016888,0.00029765512,0.00014635597,0.000073227486,0.00017784724],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014081469,0.00010312769,0.00029390896,0.00022438928,0.00011265881,0.000026326194,0.00079321215,0.000049035738,0.003080473],"category_scores_gemma":[0.00022583803,0.00004604632,0.00017117315,0.0014080704,0.0011617435,0.000113671886,0.0000056066438,0.00019747038,0.0000018044893],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007849498,0.000007670405,0.9967863,0.000014662645,0.000007815052,0.000009415914,0.00015298884,0.0009467688,0.000039890234,0.000105784566,0.00004265258,0.0018782286],"study_design_scores_gemma":[0.00016380471,0.0008127819,0.99386674,0.000067223475,0.000030809646,0.00003236986,0.00014830232,0.0022562544,0.0003010551,0.0019615074,0.00029805762,0.00006111237],"about_ca_topic_score_codex":0.029613573,"about_ca_topic_score_gemma":0.5341332,"teacher_disagreement_score":0.5045196,"about_ca_system_score_codex":7.245421e-7,"about_ca_system_score_gemma":0.00018395077,"threshold_uncertainty_score":0.99783087},"labels":[],"label_agreement":null},{"id":"W2036785257","doi":"10.1139/e99-071","title":"Contrasting Si-saturation in troctolite-anorthosite intrusions along the Manicouagan corridor of the Abitibi-Grenville transect","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Barrick Gold (Canada); University of Calgary; McGill University","funders":"","keywords":"Anorthosite; Geology; Plagioclase; Geochemistry; Layered intrusion; Olivine; Gabbro; Petrology; Magma chamber; Magma; Intrusion; Igneous rock; Volcano; Quartz","score_opus":0.011978848489317857,"score_gpt":0.18020407486638365,"score_spread":0.1682252263770658,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036785257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99325967,0.0008168527,0.000005504917,0.00230621,0.00012413022,0.00006785319,0.000024202558,0.0000012483871,0.0033943455],"genre_scores_gemma":[0.99931353,0.00003318442,0.00008968084,0.00042297403,0.000057734713,1.408162e-7,0.0000019777963,7.4016157e-7,0.000080021615],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987599,0.00012910397,0.0003996113,0.00012497195,0.00027363037,0.00031277462],"domain_scores_gemma":[0.99922967,0.00023993006,0.00016070105,0.00008874359,0.000059653205,0.00022129311],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006908574,0.000087035536,0.00018173121,0.000106996275,0.0004268567,0.00007028274,0.00049318874,0.000038688675,0.008511138],"category_scores_gemma":[0.0001736453,0.000040640894,0.00013444229,0.00083118386,0.000583317,0.00014937445,0.0000029657417,0.00022765232,0.000011642679],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008248985,0.0000039532106,0.9794676,0.0000020797418,0.0000064417095,0.0000133786025,0.0003198309,0.009690414,0.00022033571,0.000040273473,0.000015225409,0.0102122445],"study_design_scores_gemma":[0.000114453986,0.00009154269,0.99319077,0.000041569532,0.000018008428,0.000060476214,0.00027685994,0.004369793,0.00020638609,0.0008956448,0.0006712377,0.000063266256],"about_ca_topic_score_codex":0.06801797,"about_ca_topic_score_gemma":0.8809749,"teacher_disagreement_score":0.81295687,"about_ca_system_score_codex":0.000001530693,"about_ca_system_score_gemma":0.00032427037,"threshold_uncertainty_score":0.9923952},"labels":[],"label_agreement":null},{"id":"W2037034018","doi":"10.1139/e09-002","title":"The first integrated use of in situ U–Pb geochronology and geochemical analyses to determine long-distance transport of glacial erratics from mainland Canada into the western Arctic Archipelago","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Center for Northern Studies; University of Alberta","funders":"","keywords":"Geology; Zircon; Provenance; Geochemistry; Archean; Geochronology; Arctic; Diorite; Paleontology; Oceanography","score_opus":0.023534161909505004,"score_gpt":0.21859232166663126,"score_spread":0.19505815975712626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037034018","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952622,0.00092191057,0.00006709759,0.003551217,0.000062639934,0.00005299738,0.000042612945,6.9026e-7,0.00003860729],"genre_scores_gemma":[0.99905074,0.00004497276,0.00045376905,0.00040320904,0.000029244104,1.292e-7,0.0000063460902,6.582059e-7,0.000010937377],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987348,0.00006347008,0.0004804016,0.00015667625,0.00025678394,0.00030787505],"domain_scores_gemma":[0.9987668,0.0004998449,0.00019536157,0.00011108745,0.000109559485,0.00031737777],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034019604,0.00011168656,0.0003062615,0.000115882925,0.00018788516,0.000044285334,0.00045134712,0.00004196622,0.000120487566],"category_scores_gemma":[0.00032703383,0.00005647283,0.000059831433,0.0005738335,0.00081258686,0.00010576832,0.000005396658,0.00018989471,4.8662196e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038671824,0.000004532781,0.992556,0.0000032160176,0.000015503929,0.000049382295,0.00044287846,0.002814897,0.00028636892,0.0000060637863,0.000015068916,0.0037674583],"study_design_scores_gemma":[0.0001036817,0.00020937478,0.9955165,0.00004559979,0.000028335726,0.000016801143,0.00028150817,0.000926382,0.00077864266,0.0014379926,0.0005797203,0.00007550925],"about_ca_topic_score_codex":0.8695696,"about_ca_topic_score_gemma":0.99976975,"teacher_disagreement_score":0.13020016,"about_ca_system_score_codex":0.0000045472448,"about_ca_system_score_gemma":0.00081277615,"threshold_uncertainty_score":0.29940102},"labels":[],"label_agreement":null},{"id":"W2037095255","doi":"10.1139/e00-031","title":"Predicted groundwater circulation in fractured and unfractured anisotropic porous media driven by nuclear fuel waste heatgeneration","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Australian Research Council","keywords":"Buoyancy; Groundwater; Fluid dynamics; Natural convection; Porous medium; Groundwater flow; Geology; Radioactive waste; Flow (mathematics); Heat transfer; Hydrogeology; Porosity; Petroleum engineering; Environmental science; Mechanics; Geotechnical engineering; Waste management; Aquifer; Engineering","score_opus":0.0076409536104129535,"score_gpt":0.18788919397626302,"score_spread":0.18024824036585008,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037095255","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998093,0.0002757569,0.00010915802,0.00080012187,0.00013373952,0.00007086592,0.0000054366556,0.0000037128968,0.00050818303],"genre_scores_gemma":[0.9991117,0.00003881109,0.00023621833,0.00034494232,0.000054359476,8.3712956e-7,0.0000040894283,0.000004575953,0.0002044695],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99901295,0.000059185408,0.0002528101,0.00016442536,0.00027283694,0.00023776898],"domain_scores_gemma":[0.9995968,0.000019199017,0.000084900996,0.00005745087,0.000018448398,0.0002232238],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002239275,0.00009455459,0.00013213382,0.0001170603,0.00025139886,0.0001476624,0.00014803327,0.000050750547,0.0016470678],"category_scores_gemma":[0.00002081871,0.00007505196,0.000022439866,0.00024333183,0.00031487393,0.00067813904,0.000009147334,0.0001023631,0.000016835185],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021094209,0.00003641176,0.9224465,0.00000555501,0.000018297567,0.00007257687,0.013293844,0.008422879,0.0070372326,0.00003193546,0.0012523478,0.04736133],"study_design_scores_gemma":[0.00038458064,0.00013345631,0.98319465,0.00001571959,0.0000085847405,0.000040334973,0.0003744612,0.001802205,0.00014518268,0.00014515097,0.013640373,0.00011532485],"about_ca_topic_score_codex":0.0048754606,"about_ca_topic_score_gemma":0.09153877,"teacher_disagreement_score":0.086663306,"about_ca_system_score_codex":0.000031823536,"about_ca_system_score_gemma":0.0000621923,"threshold_uncertainty_score":0.99926555},"labels":[],"label_agreement":null},{"id":"W2037131626","doi":"10.1139/e05-060","title":"A<i>Fluvioviridavis</i>-like bird from the Middle Eocene of Messel, Germany","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Taxon; Cladistics; Affinities; Phylogenetic tree; Paleontology; Beak; Zoology; Biology","score_opus":0.028496375267706202,"score_gpt":0.20790270096664623,"score_spread":0.17940632569894002,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037131626","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97894216,0.0127888,0.000020121985,0.0034463608,0.00083123904,0.000040935392,0.000084066814,0.0000044008953,0.0038419124],"genre_scores_gemma":[0.99756587,0.00012929468,0.00087662,0.0010078062,0.00032490096,8.670771e-8,0.0000031766194,0.0000012939379,0.000090983995],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99884945,0.0001283564,0.00033152677,0.00013565981,0.00019428846,0.00036070347],"domain_scores_gemma":[0.9989377,0.00029853088,0.00023693351,0.00011490223,0.000089239475,0.00032267667],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007831092,0.00009204285,0.00018612943,0.0001412473,0.00041329677,0.000031391104,0.00067165645,0.00007176292,0.002381],"category_scores_gemma":[0.00009458243,0.00005614801,0.000071859235,0.00035053035,0.0012803742,0.0003572243,0.0000040583673,0.00017547194,0.00011608483],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011349312,0.0000037343607,0.9923783,0.0000011330924,0.00001710044,0.000020228546,0.00034508316,0.0013904028,0.00005432604,0.000089523506,0.0014627229,0.0042261193],"study_design_scores_gemma":[0.0001222489,0.00014905747,0.9382501,0.000020609841,0.000013441719,0.00013254659,0.00023904968,0.00067840784,0.000056932964,0.00046945352,0.05979433,0.00007378414],"about_ca_topic_score_codex":0.035950672,"about_ca_topic_score_gemma":0.78697497,"teacher_disagreement_score":0.7510243,"about_ca_system_score_codex":0.000001479482,"about_ca_system_score_gemma":0.001207204,"threshold_uncertainty_score":0.998531},"labels":[],"label_agreement":null},{"id":"W2037303406","doi":"10.1139/e99-089","title":"The 3-D crustal structure in the Manicouagan region: new seismic and gravity constraints","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University; Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Bouguer anomaly; Geology; Seismology; Terrane; Reflection (computer programming); Tectonics; Gravity anomaly; Plateau (mathematics); Basement; Reflector (photography); Geophysics; Geodesy; Paleontology","score_opus":0.013551561292652621,"score_gpt":0.18514404548558108,"score_spread":0.17159248419292847,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037303406","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98490804,0.0015865748,0.0000023714078,0.009544204,0.00006918685,0.00003491375,0.000008160785,9.713661e-7,0.003845588],"genre_scores_gemma":[0.99858475,0.00008716457,0.00006887767,0.0009823473,0.000084168336,2.5258805e-8,8.877078e-7,3.5351147e-7,0.00019142717],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991171,0.0000834406,0.0001845629,0.0001105079,0.00020975029,0.0002946842],"domain_scores_gemma":[0.99933934,0.00016321386,0.00006642848,0.00006823269,0.000024278397,0.00033852033],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00051061076,0.00007192566,0.00010999769,0.00005852826,0.0004923909,0.00021994788,0.00044976803,0.00003349968,0.004052332],"category_scores_gemma":[0.00007248675,0.000031195796,0.000046401186,0.0004046475,0.0011843909,0.00013904828,0.0000021385133,0.00021762894,0.000010238607],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009587247,0.0000018201952,0.86004794,0.0000012873819,0.000007920129,0.00018680036,0.00044032274,0.001900458,0.000004301723,0.0002764791,0.00068154495,0.13644156],"study_design_scores_gemma":[0.00010663922,0.00011294695,0.9406803,0.000010031395,0.000009103054,0.0006908265,0.00077533064,0.0008932989,0.0000074699233,0.036623653,0.020018322,0.00007204293],"about_ca_topic_score_codex":0.02509126,"about_ca_topic_score_gemma":0.68895805,"teacher_disagreement_score":0.66386676,"about_ca_system_score_codex":6.263869e-7,"about_ca_system_score_gemma":0.0003788781,"threshold_uncertainty_score":0.9968581},"labels":[],"label_agreement":null},{"id":"W2037526071","doi":"10.1139/e01-093","title":"U–Pb geochronology of detrital zircons in metasedimentary rocks from southern Baffin Island: implications for the Paleoproterozoic tectonic evolution of Northeastern Laurentia","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Government of Nunavut; Nunavut Research Institute","funders":"Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Geology; Provenance; Archean; Detritus; Zircon; Laurentia; Craton; Geochronology; Geochemistry; Siliciclastic; Terrane; Paleontology; Tectonics; Paleozoic; Sedimentary depositional environment","score_opus":0.018637779217327746,"score_gpt":0.19443211097644936,"score_spread":0.17579433175912162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037526071","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99010104,0.007010851,0.00063729926,0.0013232062,0.000090526926,0.00010708832,0.00056598516,0.0000012230564,0.00016280537],"genre_scores_gemma":[0.9993445,0.000019622034,0.0005184126,0.000044314125,0.000043373795,9.490483e-7,0.000011939834,8.180646e-7,0.00001605396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99902624,0.00005158165,0.0003900713,0.00013859732,0.00013127837,0.00026222804],"domain_scores_gemma":[0.9990888,0.00030286028,0.00026070353,0.00010377556,0.00008655286,0.00015728928],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032592035,0.000080097576,0.00021989166,0.00023182514,0.00015037131,0.000019225145,0.00042509197,0.000045874855,0.00448476],"category_scores_gemma":[0.00010462448,0.000048052323,0.00013468787,0.0004788451,0.0004652533,0.00010839012,0.0000048460206,0.000113033144,0.000010971435],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005981809,0.0000114032755,0.9907275,0.0000029209805,0.000033602562,0.0000014174619,0.00015812276,0.004131504,0.00037071217,0.000011476663,0.00001889498,0.0045264843],"study_design_scores_gemma":[0.00028177936,0.0002902436,0.9879994,0.000021448543,0.00007233668,0.000014824726,0.00072970724,0.005092889,0.0004432068,0.0047845724,0.00019107157,0.00007853596],"about_ca_topic_score_codex":0.13962232,"about_ca_topic_score_gemma":0.9367993,"teacher_disagreement_score":0.797177,"about_ca_system_score_codex":0.0000023866094,"about_ca_system_score_gemma":0.00018086248,"threshold_uncertainty_score":0.9964253},"labels":[],"label_agreement":null},{"id":"W2037568805","doi":"10.1139/e02-028","title":"The age of the Gunflint Formation, Ontario, Canada: single zircon UPb age determinations from reworked volcanic ash","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":147,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; Lakehead University","funders":"","keywords":"Geology; Zircon; Paleontology; Precambrian; Sedimentary rock; Geochemistry; Volcano; Foreland basin; Structural basin","score_opus":0.024141450670898772,"score_gpt":0.16773818041609007,"score_spread":0.1435967297451913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037568805","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9885215,0.00082688115,0.00001762664,0.0034942483,0.00038222485,0.000048861286,0.000035737725,0.0000013822589,0.0066715386],"genre_scores_gemma":[0.9984566,0.000015102509,0.00022806892,0.00043741066,0.000056838886,1.5195003e-7,0.0000045664574,6.6954607e-7,0.00080061273],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987263,0.000078515106,0.00039016682,0.00010612179,0.00039086462,0.00030803835],"domain_scores_gemma":[0.9989287,0.0002586561,0.00027382918,0.00013370188,0.00012604483,0.00027902206],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038484676,0.00008433869,0.00015510399,0.00006194738,0.00074904715,0.0001296098,0.0007298463,0.000035955734,0.00551166],"category_scores_gemma":[0.00031749925,0.00004160033,0.00010788908,0.00047080326,0.0005546395,0.00019405264,0.000008987637,0.00019448216,0.000009445216],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000047177514,0.00001209371,0.9789264,0.0000033889633,0.00003800501,0.00011672166,0.0012103188,0.0044915867,0.0005028241,0.00008600921,0.00485796,0.009749926],"study_design_scores_gemma":[0.00009164841,0.00010229528,0.93677086,0.000033064396,0.000031822598,0.000028329428,0.00039106904,0.0015191431,0.000649237,0.004652003,0.055627003,0.000103505074],"about_ca_topic_score_codex":0.9711477,"about_ca_topic_score_gemma":0.9999778,"teacher_disagreement_score":0.050769042,"about_ca_system_score_codex":0.000011942266,"about_ca_system_score_gemma":0.00079529354,"threshold_uncertainty_score":0.99539745},"labels":[],"label_agreement":null},{"id":"W2037611554","doi":"10.1139/e04-081","title":"The tephra stratigraphy of two lakes in south-central British Columbia, Canada and its implications for mid-late Holocene volcanic activity at Glacier Peak and Mount St. Helens, Washington, USA","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Tephra; Geology; Holocene; Glacier; Volcano; Physical geography; Geochemistry; Geomorphology; Oceanography; Geography","score_opus":0.01690293713414871,"score_gpt":0.22642117488479788,"score_spread":0.20951823775064918,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037611554","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949151,0.0032224273,0.0000022281756,0.0011891273,0.00013585661,0.00015115681,0.0003145507,9.004252e-7,0.000068601155],"genre_scores_gemma":[0.99956906,0.00019889897,0.00007746137,0.00007537411,0.000019621179,8.5222416e-7,0.0000035028045,0.0000012215845,0.000053985535],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99881536,0.000079454236,0.00023551477,0.00017535403,0.00015025871,0.00054407737],"domain_scores_gemma":[0.9989799,0.00024937114,0.00015592296,0.0000691035,0.000109057306,0.00043661043],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007580832,0.00007130801,0.0001783637,0.00008896219,0.00090621633,0.00018137043,0.00027323104,0.000050001847,0.00006577574],"category_scores_gemma":[0.00014253627,0.00006777683,0.00003194875,0.00029435873,0.0008959652,0.00023052933,0.0000066708467,0.0001782856,3.24334e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000077882,0.0000021736462,0.9988449,0.000008427284,0.000009953553,0.00001719368,0.00015167207,0.0005015585,0.000029148516,0.000043863725,0.000022948885,0.00036032483],"study_design_scores_gemma":[0.00037845148,0.00014878636,0.9974619,0.000026537384,0.000007689209,0.00022645979,0.00015803265,0.00015606676,0.000030782125,0.0011455355,0.00018450624,0.00007525805],"about_ca_topic_score_codex":0.86794734,"about_ca_topic_score_gemma":0.99997985,"teacher_disagreement_score":0.13203251,"about_ca_system_score_codex":0.000003863091,"about_ca_system_score_gemma":0.0029610943,"threshold_uncertainty_score":0.69699746},"labels":[],"label_agreement":null},{"id":"W2037704177","doi":"10.1139/e05-032","title":"Lithospheric structure of the Trans-Hudson Orogen from seismic refraction - wide-angle reflection studies","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; University of British Columbia; PotashCorp (Canada)","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; National Science Foundation","keywords":"Geology; Lithosphere; Craton; Seismology; Fibrous joint; Gneiss; Mantle (geology); Archean; Fold (higher-order function); Crust; Clockwise; Tectonics; Seismic anisotropy; Metamorphic rock; Crustal recycling; Collision zone; Petrology; Geophysics; Geochemistry","score_opus":0.020524818843044773,"score_gpt":0.23426551346496496,"score_spread":0.2137406946219202,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037704177","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945139,0.0023717757,0.00002924465,0.0010828564,0.0014827797,0.000062950734,0.000101485144,0.000002696314,0.0003522833],"genre_scores_gemma":[0.9983046,0.00008955387,0.00097225135,0.00019865885,0.00034153377,6.7873714e-8,0.0000022261174,0.0000018239126,0.00008925291],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989984,0.000097077,0.00029076205,0.00012422603,0.00027256433,0.00021693978],"domain_scores_gemma":[0.99923015,0.00007891288,0.00030552596,0.00010025058,0.00011936836,0.00016579521],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032535236,0.000090901274,0.00019589353,0.00006803657,0.00036083424,0.00008083308,0.00031492457,0.000045789104,0.0009421994],"category_scores_gemma":[0.00007359641,0.00005461897,0.000069966016,0.00036706362,0.00027003651,0.0004689009,0.000003035144,0.00011161521,0.0000073170772],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000087657296,0.000023085631,0.6644153,0.000055331875,0.00033803363,0.000024661615,0.012100018,0.22511168,0.03662351,0.00017836198,0.003916442,0.057125892],"study_design_scores_gemma":[0.000317466,0.0004402152,0.85302114,0.00015179861,0.00010845542,0.000053046973,0.0016727602,0.0010488135,0.036325507,0.004918657,0.10169465,0.00024747924],"about_ca_topic_score_codex":0.030742612,"about_ca_topic_score_gemma":0.4138014,"teacher_disagreement_score":0.3830588,"about_ca_system_score_codex":0.0000034710083,"about_ca_system_score_gemma":0.00056381646,"threshold_uncertainty_score":0.9999711},"labels":[],"label_agreement":null},{"id":"W2038372824","doi":"10.1139/e02-086","title":"Early Turonian (Late Cretaceous) age of the Tuskoola sandstone Pine River area, northeastern British Columbia","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; University of Alberta","funders":"","keywords":"Geology; Cretaceous; Paleontology; Facies; Stratigraphy; Horizon; Stage (stratigraphy); Structural basin; Tectonics","score_opus":0.017282123018238837,"score_gpt":0.18166055577626508,"score_spread":0.16437843275802624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038372824","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9635934,0.008732691,0.0000056323124,0.00025062726,0.0005423286,0.00007514299,0.0000671809,0.0000030918573,0.02672989],"genre_scores_gemma":[0.99862415,0.00006666785,0.00019372627,0.00009727139,0.00006469707,1.0208783e-7,5.3673e-7,9.0673024e-7,0.0009519606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99855506,0.000107120024,0.00036853878,0.00016876184,0.0003543,0.00044619947],"domain_scores_gemma":[0.99891037,0.0000665164,0.00029068426,0.00013833561,0.000090369096,0.0005037366],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046496638,0.00009644605,0.00025295798,0.00010531821,0.0010515989,0.0005337335,0.00069615204,0.00007428545,0.002008718],"category_scores_gemma":[0.00007201211,0.000087549095,0.00015842136,0.0004816295,0.0019621835,0.0003912424,0.0000018302494,0.00025757906,0.0000090078465],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000022310942,0.000004402897,0.9739231,0.0000034661111,0.000013976312,0.00022620031,0.0004944585,0.00013186777,0.000010929853,0.000001529812,0.0002018053,0.02498606],"study_design_scores_gemma":[0.00020883369,0.00028354235,0.9964845,0.000078487115,0.000018549543,0.00040861723,0.00007459256,0.00035303817,0.000005843205,0.00024464674,0.0017298205,0.000109498964],"about_ca_topic_score_codex":0.27694,"about_ca_topic_score_gemma":0.98894745,"teacher_disagreement_score":0.71200746,"about_ca_system_score_codex":0.0000011489358,"about_ca_system_score_gemma":0.00038621607,"threshold_uncertainty_score":0.9989036},"labels":[],"label_agreement":null},{"id":"W2038760918","doi":"10.1139/e01-007","title":"Geochemical evolution of groundwater on Saturna Island, British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Nunavut Research Institute; Simon Fraser University","funders":"","keywords":"Geology; Bedrock; Aquifer; Groundwater; Saltwater intrusion; Geochemistry; Sedimentary rock; Pleistocene; Hydrology (agriculture); Geomorphology; Paleontology","score_opus":0.009620460417408789,"score_gpt":0.17996144058896105,"score_spread":0.17034098017155225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038760918","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9858167,0.00064352166,0.000023911736,0.00013510256,0.00044541815,0.00004154391,0.00003501724,0.0000026838818,0.012856094],"genre_scores_gemma":[0.9985312,0.000029772511,0.00015536933,0.000106732376,0.0001898086,9.140125e-8,0.000006233927,0.0000016637294,0.0009791134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875146,0.000036257756,0.0003176423,0.0001557767,0.00034191448,0.0003969276],"domain_scores_gemma":[0.9991384,0.00004379328,0.00015588859,0.000090196976,0.000120555436,0.0004511633],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005037837,0.000075619624,0.00018178261,0.00011020529,0.00027246683,0.00038117453,0.00038756544,0.00006778808,0.005803388],"category_scores_gemma":[0.00007384343,0.00007979278,0.00008758076,0.00033777408,0.0004556903,0.00033885174,0.0000035506987,0.00018129697,0.000030682455],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007406637,0.000007150188,0.9950225,0.000005263091,0.0000069598746,0.00011099211,0.000055907094,0.00018424285,0.00019171026,0.0000044430503,0.0015851163,0.0028183337],"study_design_scores_gemma":[0.0002582101,0.00049550046,0.9808014,0.00010408532,0.0000102577405,0.0012724557,0.00023969174,0.00017319033,0.0005010124,0.0013349334,0.014665008,0.00014425062],"about_ca_topic_score_codex":0.38185313,"about_ca_topic_score_gemma":0.9482559,"teacher_disagreement_score":0.5664028,"about_ca_system_score_codex":0.000005003902,"about_ca_system_score_gemma":0.0006829777,"threshold_uncertainty_score":0.99510545},"labels":[],"label_agreement":null},{"id":"W2039301513","doi":"10.1139/e10-017","title":"Description of a new specimen of Ianthasaurus hardestiorum (Eupelycosauria: Edaphosauridae) and a re-evaluation of edaphosaurid phylogeny","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Amgen (Canada); University of Toronto","funders":"National Geographic Society","keywords":"Pennsylvanian; Taxon; Phylogenetic tree; Sister group; Paleontology; Genus; Biology; Phylogenetics; Clade; Geology; Evolutionary biology; Zoology; Structural basin","score_opus":0.04556513927272235,"score_gpt":0.24269778732580977,"score_spread":0.19713264805308742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039301513","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99131966,0.0037583844,0.000023919847,0.0005041718,0.0009849913,0.00010746499,0.000064827465,0.0000015357543,0.0032350547],"genre_scores_gemma":[0.99735,0.00007677919,0.002358704,0.000037985577,0.00013267405,1.4957324e-7,0.00000484964,0.0000013034227,0.000037585993],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99848384,0.00014791709,0.00052843697,0.00016679132,0.00038206173,0.00029094683],"domain_scores_gemma":[0.9984025,0.00011835959,0.0005875128,0.000120553705,0.00033168265,0.0004394337],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0023642012,0.00010792884,0.00031130036,0.0004799523,0.00015504214,0.000015573833,0.00032504808,0.00012926628,0.0019246729],"category_scores_gemma":[0.000566703,0.00008735233,0.00007898627,0.00038587523,0.0014692975,0.00035035546,0.0000052669134,0.00020471653,0.000003950688],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005030877,0.0000095878895,0.98297846,0.000011307573,0.000027241658,0.000008166883,0.00039832506,0.00045894113,0.008522808,0.0002543803,0.00032310336,0.006957366],"study_design_scores_gemma":[0.0004025134,0.0005640646,0.99165714,0.000045938606,0.00005606824,0.00016925843,0.0003361094,0.00094735395,0.0017821554,0.0031039463,0.0008499022,0.00008553908],"about_ca_topic_score_codex":0.016713876,"about_ca_topic_score_gemma":0.5023784,"teacher_disagreement_score":0.48566455,"about_ca_system_score_codex":0.0000018412071,"about_ca_system_score_gemma":0.0032342733,"threshold_uncertainty_score":0.9989877},"labels":[],"label_agreement":null},{"id":"W2039388243","doi":"10.1139/e02-013","title":"New insights into the structure of the Sudbury Igneous Complex from downhole seismic studies","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Norite; Igneous rock; Seismology; Pluton; Drill; Petrology; Geochemistry; Tectonics; Gabbro","score_opus":0.03217445897608454,"score_gpt":0.2204521620952001,"score_spread":0.18827770311911557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039388243","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99533665,0.0015794523,0.00008515424,0.0021356514,0.00041697058,0.00004105172,0.000015369269,7.297528e-7,0.00038894176],"genre_scores_gemma":[0.9991428,0.000011925929,0.00024683168,0.00024884526,0.00022726857,5.196262e-8,0.0000019290721,0.0000011879406,0.000119143784],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993577,0.000040609542,0.00017409903,0.00007894014,0.00020534162,0.00014331825],"domain_scores_gemma":[0.99946564,0.000053083626,0.00017479196,0.00010127808,0.00006451329,0.00014069235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009024332,0.00006379588,0.00011051566,0.00006216719,0.00047328972,0.00007626086,0.0005013491,0.000011850903,0.00039797925],"category_scores_gemma":[0.000011716241,0.000030585423,0.00004185903,0.0002765339,0.00040626296,0.00030949127,0.000011615572,0.000107158034,0.0000136387425],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012464863,0.000030893432,0.4809097,0.000011003103,0.00037183834,0.00004000147,0.18094851,0.14826636,0.026261736,0.0063380753,0.08358524,0.07322419],"study_design_scores_gemma":[0.0011345155,0.0008793739,0.48258168,0.0003579249,0.0001839313,0.000060109007,0.07434497,0.0328664,0.013903924,0.19408494,0.19879134,0.0008108923],"about_ca_topic_score_codex":0.017450282,"about_ca_topic_score_gemma":0.06948569,"teacher_disagreement_score":0.18774687,"about_ca_system_score_codex":0.0000031555642,"about_ca_system_score_gemma":0.00038309296,"threshold_uncertainty_score":0.9890926},"labels":[],"label_agreement":null},{"id":"W2039400407","doi":"10.1139/e02-082","title":"The postcranial skeleton, phylogenetic position, and probable lifestyle of the Early Triassic reptile <i>Procolophon trigoniceps</i>","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Amphibian and Reptile Biology","field":"Environmental Science","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Toronto Zoo","funders":"","keywords":"Postcrania; Permian; Clade; Sister group; Taxon; Paleontology; Lineage (genetic); Geology; Phylogenetic tree; Biology; Structural basin","score_opus":0.007146053847782911,"score_gpt":0.19460096778894326,"score_spread":0.18745491394116034,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039400407","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.992719,0.00059730315,0.0000059415243,0.00095608976,0.00038509356,0.00018705778,0.0000029771118,0.0000012884599,0.005145263],"genre_scores_gemma":[0.9987154,0.00004313409,0.0002550599,0.00023335754,0.000043100805,0.0000016139892,5.7934166e-8,0.0000034001569,0.0007048624],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988479,0.00018233428,0.00029852078,0.0001465883,0.00021356769,0.00031106133],"domain_scores_gemma":[0.9992169,0.000082345665,0.0002818127,0.0001340108,0.00003274455,0.00025217523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010302885,0.0000827037,0.00012799774,0.00004134214,0.0007378083,0.00006661842,0.00040388567,0.000053260872,0.00019114131],"category_scores_gemma":[0.00018987051,0.00004219465,0.000067985755,0.00039787847,0.0018861652,0.00011420835,0.000020849422,0.000121004094,0.000010598988],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004153303,0.000036028585,0.95057607,0.000007331555,0.000025965706,0.000024154304,0.0013218719,0.0005681795,0.03905837,0.0014264024,0.0029600684,0.003954058],"study_design_scores_gemma":[0.0007274057,0.0011776751,0.9085108,0.000048980353,0.000029641196,0.00060108723,0.0004414811,0.000030210134,0.010401574,0.0022413894,0.07559969,0.0001900726],"about_ca_topic_score_codex":0.0011032136,"about_ca_topic_score_gemma":0.032426048,"teacher_disagreement_score":0.07263962,"about_ca_system_score_codex":0.000014709371,"about_ca_system_score_gemma":0.0006432476,"threshold_uncertainty_score":0.9852297},"labels":[],"label_agreement":null},{"id":"W2039733112","doi":"10.1139/e03-042","title":"Topography of the crustmantle interface under the Western Superior craton from gravity data","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Crust; Craton; Mantle (geology); Gravity anomaly; Seismology; Density contrast; Magmatism; Crustal recycling; Tectonics; Geophysics; Subduction; Bouguer anomaly; Paleontology","score_opus":0.03460683464811855,"score_gpt":0.22225637553033928,"score_spread":0.18764954088222074,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039733112","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99308616,0.0020589877,0.000037828955,0.0028605799,0.00030248234,0.000034084387,0.00012266336,0.0000010668624,0.0014961543],"genre_scores_gemma":[0.9990876,0.000022113798,0.00018187882,0.0005815788,0.000035706096,3.810319e-8,0.0000022517017,5.960218e-7,0.000088247456],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99893576,0.00014475625,0.00024556607,0.0001543499,0.0002798283,0.00023974592],"domain_scores_gemma":[0.9990949,0.00017528138,0.00015235115,0.00027020523,0.0000660861,0.00024114993],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00070976146,0.00007880057,0.000156986,0.000066788736,0.00032408524,0.00010014265,0.001344508,0.000033348228,0.003242893],"category_scores_gemma":[0.00016752857,0.00003389909,0.00010289813,0.0005617316,0.0010068783,0.0002132678,0.000018453507,0.00018007173,0.00001537669],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000018911431,0.0000031274635,0.997941,8.375726e-7,0.000016448716,0.0000027011506,0.00007186584,0.0011844086,0.00009033256,0.000051637864,0.00014294586,0.00049277046],"study_design_scores_gemma":[0.00006664073,0.00006649419,0.9823702,0.000016955031,0.00003382451,0.000019315159,0.0006372532,0.00030577162,0.0013106389,0.0064586513,0.008643753,0.00007052098],"about_ca_topic_score_codex":0.062323134,"about_ca_topic_score_gemma":0.70598006,"teacher_disagreement_score":0.6436569,"about_ca_system_score_codex":5.4477584e-7,"about_ca_system_score_gemma":0.00037075114,"threshold_uncertainty_score":0.99766827},"labels":[],"label_agreement":null},{"id":"W2040034412","doi":"10.1139/e00-084","title":"Modes of extinction in two Devonian ostracode faunas of western Canada","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; University of Calgary","keywords":"Paleontology; Devonian; Geology; Milankovitch cycles; Extinction (optical mineralogy); Sequence (biology); Transgressive; Sedimentary rock; Extinction event; Fauna; Late Devonian extinction; Ecology; Sedimentary depositional environment; Biology; Carboniferous; Biological dispersal","score_opus":0.028983545886273204,"score_gpt":0.24494742962287688,"score_spread":0.2159638837366037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040034412","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9846128,0.0019189314,0.000018026047,0.00048920553,0.00030782702,0.000033725253,0.000023232664,8.36464e-7,0.012595401],"genre_scores_gemma":[0.9994617,0.000070803275,0.000253709,0.00009322779,0.000035544093,5.5706273e-8,8.005672e-7,6.955525e-7,0.000083482715],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989611,0.00006886226,0.00037842724,0.000092311435,0.0002342583,0.00026504396],"domain_scores_gemma":[0.99925137,0.00009612515,0.00025441498,0.00005481207,0.00010884812,0.0002344129],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005497725,0.00007081968,0.0002037071,0.00028847906,0.00012948932,0.0000136611325,0.00023686311,0.000023463082,0.00046040927],"category_scores_gemma":[0.00008499596,0.000056839137,0.000033926863,0.00042468647,0.00044600305,0.00021884302,0.0000019353274,0.00010435551,0.0000018304257],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007910929,0.000002157783,0.98871267,0.000003985271,0.0000059838712,0.000039837632,0.00018672671,0.009188666,0.000017668528,0.000023821365,0.00003514752,0.0017754512],"study_design_scores_gemma":[0.00017699129,0.00011327563,0.99530643,0.000040745763,0.000004682897,0.000100565376,0.0010552898,0.00083059166,0.000077905686,0.0001198846,0.0021149095,0.000058710422],"about_ca_topic_score_codex":0.91062003,"about_ca_topic_score_gemma":0.9999643,"teacher_disagreement_score":0.08934425,"about_ca_system_score_codex":0.0000036266056,"about_ca_system_score_gemma":0.0022807007,"threshold_uncertainty_score":0.5041159},"labels":[],"label_agreement":null},{"id":"W2040034587","doi":"10.1139/e11-027","title":"Corrigendum: An istiodactylid pterosaur from the Upper Cretaceous Nanaimo Group, Hornby Island, British Columbia, Canada<sup>1</sup>Original paper CJES, 2011, <b>48</b>(1): 63–69.","year":2011,"lang":"en","type":"erratum","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Cretaceous; Group (periodic table); Paleontology; Holotype; Genus","score_opus":0.015791165399295697,"score_gpt":0.1877621537099726,"score_spread":0.1719709883106769,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040034587","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.54239404,0.17695606,0.000032079068,0.0044736103,0.12466633,0.0009227665,0.021230465,0.000052422398,0.12927221],"genre_scores_gemma":[0.8226088,0.0048607513,0.0008762842,0.01036065,0.0107848765,0.0000044130497,0.003027198,0.00004639504,0.14743061],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99530613,0.0006524051,0.00090876786,0.0008036271,0.0007982274,0.001530832],"domain_scores_gemma":[0.99655557,0.00023122436,0.00076283066,0.00047463938,0.00029095792,0.0016848033],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012693817,0.00045697737,0.00084872957,0.0002015059,0.0025404803,0.0007772723,0.0025818245,0.0007218557,0.058056362],"category_scores_gemma":[0.00018996047,0.0004238933,0.00025338127,0.00036187845,0.0025429053,0.0009436187,0.000020432104,0.0018181974,0.0002716967],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015561202,0.0000062305853,0.4544906,0.000004406138,0.000060701946,0.00072761934,0.00013649308,0.00005375642,1.5678401e-7,0.000006286278,0.5430151,0.0014830682],"study_design_scores_gemma":[0.0001582167,0.00030906044,0.47100526,0.000077064644,0.00006445738,0.0011516272,0.0003212715,0.00023530259,6.350236e-8,0.00034573628,0.52599585,0.000336098],"about_ca_topic_score_codex":0.99695826,"about_ca_topic_score_gemma":0.99999034,"teacher_disagreement_score":0.28021476,"about_ca_system_score_codex":0.00003150082,"about_ca_system_score_gemma":0.016275741,"threshold_uncertainty_score":0.9998213},"labels":[],"label_agreement":null},{"id":"W2040191111","doi":"10.1139/e04-015","title":"Landscape evolution and human occupation during the Archaic period on the northern Plains","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Holocene; Geology; Period (music); Prehistory; Archaeology; Excavation; Arid; Geoarchaeology; Quaternary; Archaic period; Pleistocene; Sedimentary rock; Last Glacial Maximum; Loess; Paleontology; Physical geography; Geography","score_opus":0.01916257747838452,"score_gpt":0.22695098542129744,"score_spread":0.20778840794291292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040191111","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99274874,0.00047049156,0.000004101107,0.004423423,0.00013205489,0.00006367662,0.000005526346,0.000001895938,0.0021501065],"genre_scores_gemma":[0.99974144,0.000008845467,0.00001665662,0.000114986666,0.000068760084,2.2639192e-7,0.0000010382194,7.332863e-7,0.00004729738],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991634,0.000112959686,0.00012986244,0.000096840835,0.00018556653,0.00031140374],"domain_scores_gemma":[0.99948597,0.00011560398,0.00008033029,0.0000749412,0.000049215654,0.00019394516],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0009923119,0.0000607079,0.00007532716,0.00016871339,0.0018608894,0.00009038067,0.0002973783,0.00003751934,0.00035017924],"category_scores_gemma":[0.000112315356,0.000030072199,0.000028774757,0.00023225458,0.00097000605,0.00013376142,0.0000035596015,0.00025002865,0.000037273167],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000062702084,0.000001224224,0.99549294,0.0000016995144,0.000004422877,0.0000322104,0.00048375316,0.0029780783,0.0000037007646,0.0009474341,0.0000036607391,0.000044610144],"study_design_scores_gemma":[0.00012757564,0.0002155275,0.9962865,0.000016830036,0.0000031041038,0.00043268528,0.0009376492,0.000093243994,0.000012358892,0.0017283963,0.00010583598,0.000040283863],"about_ca_topic_score_codex":0.004140735,"about_ca_topic_score_gemma":0.8375703,"teacher_disagreement_score":0.8334296,"about_ca_system_score_codex":9.4363816e-7,"about_ca_system_score_gemma":0.00059662544,"threshold_uncertainty_score":0.9994385},"labels":[],"label_agreement":null},{"id":"W2040293953","doi":"10.1139/e08-001","title":"Effects of sand supply on the morphodynamics and stratigraphy of active parabolic dunes, Bigstick Sand Hills, southwestern SaskatchewanGeological Survey of Canada Contribution 20060654.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; University of Calgary; University of Lethbridge","funders":"Core Research for Evolutional Science and Technology","keywords":"Geology; Sand dune stabilization; Beach morphodynamics; Deposition (geology); Stratigraphy; Geomorphology; Vegetation (pathology); Aeolian processes; Facies; Sediment; Sediment transport; Paleontology; Tectonics","score_opus":0.011772328504168796,"score_gpt":0.18419945490155964,"score_spread":0.17242712639739086,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040293953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964315,0.0024383191,0.000017667386,0.00012476399,0.00016283058,0.00012799741,0.000548979,8.1461e-7,0.00014710121],"genre_scores_gemma":[0.99970806,0.00014019995,0.000041997566,0.000068977446,0.000021954464,1.9516439e-7,0.000009710038,0.0000013709883,0.0000075589314],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986539,0.00019299329,0.00034060664,0.00013325809,0.00036589373,0.000313367],"domain_scores_gemma":[0.9978688,0.00102492,0.00044829908,0.000074116,0.00024863417,0.0003352391],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00069488527,0.00012395409,0.0003399352,0.00014383449,0.00023722688,0.000018859153,0.00026546704,0.000059083162,0.00007692341],"category_scores_gemma":[0.00048054248,0.00007481435,0.00004789074,0.0004918334,0.0011046578,0.00013685288,0.000003949845,0.00014603249,2.8752785e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005960521,0.000007688055,0.996772,0.000029754165,0.000024865934,0.00004510514,0.00033036413,0.0018550943,0.00009032352,0.000032274173,0.00007856304,0.0006743558],"study_design_scores_gemma":[0.00026017972,0.0006775283,0.9945015,0.00009347601,0.00001659437,0.00006694794,0.000203645,0.0009193744,0.002988436,0.00016988511,0.000021314476,0.00008116539],"about_ca_topic_score_codex":0.8124523,"about_ca_topic_score_gemma":0.9854503,"teacher_disagreement_score":0.17299801,"about_ca_system_score_codex":0.0000020311368,"about_ca_system_score_gemma":0.0029301494,"threshold_uncertainty_score":0.5197959},"labels":[],"label_agreement":null},{"id":"W2040561541","doi":"10.1139/e00-083","title":"Ammonoid faunas from the Cardium Formation (Turonian-Coniacian, Upper Cretaceous) and contiguous units, Alberta, Canada: I. Scaphitidae","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Alberta Bone and Joint Health Institute","funders":"National Research Council Canada; AGE-WELL","keywords":"Outcrop; Paleontology; Cretaceous; Geology; Sedimentary depositional environment; Siliciclastic; Structural basin; Sedimentary rock; Fauna; Sedimentary basin; Marine transgression; Sequence (biology); Ecology","score_opus":0.01566889196983627,"score_gpt":0.18741156705938591,"score_spread":0.17174267508954966,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040561541","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95046973,0.019712334,0.000019959869,0.0033285317,0.0006415774,0.00008449618,0.00009121591,0.000002542881,0.02564962],"genre_scores_gemma":[0.99886036,0.00019851139,0.00011404944,0.00060283515,0.00014554281,2.0675887e-7,0.0000037633536,8.2985804e-7,0.000073910436],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986441,0.00013157529,0.00031275442,0.00015969248,0.00028591455,0.0004659322],"domain_scores_gemma":[0.9986825,0.00030287122,0.00020146288,0.000112144146,0.00012331731,0.0005776777],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004954049,0.00013926477,0.00021755618,0.0001355891,0.0009773923,0.00022436975,0.00043354832,0.00006926973,0.0003198556],"category_scores_gemma":[0.00015263683,0.00009166175,0.00005266298,0.00040730648,0.0007396506,0.0006197836,0.0000012496978,0.00023872092,0.0000049223627],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009593277,7.93113e-7,0.9752947,0.0000013403167,0.000022984037,0.00012461326,0.0005085821,0.00015232756,0.0000031468048,0.00009360052,0.0010084925,0.0227798],"study_design_scores_gemma":[0.00016397149,0.0001064349,0.9608214,0.000026179045,0.000021763652,0.0005167547,0.0011677984,0.00039798656,0.000027299575,0.00029966127,0.036325797,0.00012493662],"about_ca_topic_score_codex":0.94108975,"about_ca_topic_score_gemma":0.99981123,"teacher_disagreement_score":0.058721457,"about_ca_system_score_codex":0.0000035252033,"about_ca_system_score_gemma":0.003015616,"threshold_uncertainty_score":0.75174105},"labels":[],"label_agreement":null},{"id":"W2040642493","doi":"10.1139/e02-069","title":"<sup>40</sup>Ar/<sup>39</sup>Ar evidence for ca. 1800 Ma tectonothermal activity along the Great Falls tectonic zone, central Montana","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"University of Michigan","keywords":"Geology; Tectonics; Supercontinent; Archean; Laurentia; Geochemistry; Craton; Radiometric dating; Hornblende; Biotite; Paleontology","score_opus":0.03589389161282474,"score_gpt":0.21481517209453768,"score_spread":0.17892128048171294,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040642493","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98846895,0.0040197936,0.00011449071,0.0051354696,0.00015690195,0.0002462804,0.00011875576,0.000012560999,0.0017267901],"genre_scores_gemma":[0.9974945,0.0001817181,0.00054652826,0.0007009286,0.00036282142,0.0000020734815,0.000003941825,0.0000047091658,0.00070278574],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9966995,0.00020340736,0.0005452622,0.0004958536,0.0006803398,0.0013756094],"domain_scores_gemma":[0.99714524,0.000803579,0.0003146084,0.000275332,0.00018916719,0.0012720871],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011896595,0.00031971035,0.00048623089,0.0002859776,0.0012149662,0.0004160769,0.0013497722,0.0001368674,0.019363398],"category_scores_gemma":[0.0006559217,0.00018895688,0.00042127844,0.0010914569,0.0011921355,0.0008958003,0.000020093024,0.0004920337,0.00016602394],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007476286,0.000024663015,0.8552532,0.000021447278,0.00009884816,0.00019057909,0.000757301,0.10968606,0.00010243204,0.00003955135,0.0010551645,0.032695964],"study_design_scores_gemma":[0.0005004171,0.0008967111,0.77929354,0.00015188067,0.00015618307,0.00039987706,0.00075776485,0.20273402,0.00042443982,0.0008552676,0.013275841,0.0005540659],"about_ca_topic_score_codex":0.08524633,"about_ca_topic_score_gemma":0.46668568,"teacher_disagreement_score":0.38143936,"about_ca_system_score_codex":0.000015198598,"about_ca_system_score_gemma":0.0005988292,"threshold_uncertainty_score":0.98153305},"labels":[],"label_agreement":null},{"id":"W2040711124","doi":"10.1139/e00-021","title":"Petrology and oxygen-isotope geochemistry of the Yamba Lake kimberlite rocks, N.W.T.","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Kimberlite; Geology; Geochemistry; Xenolith; Metasomatism; Olivine; Phlogopite; Peridotite; Eclogite; Partial melting; Mantle (geology); Petrology; Subduction; Paleontology","score_opus":0.008120341030994672,"score_gpt":0.1717424261213606,"score_spread":0.1636220850903659,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040711124","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97999156,0.0019152295,0.0000011961499,0.0019654199,0.00008351496,0.000023808852,0.000034183136,0.0000014117612,0.015983686],"genre_scores_gemma":[0.99863404,0.00007273754,0.00015306698,0.0004301277,0.000064637716,6.4319885e-8,0.000001842356,5.827547e-7,0.0006428733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990272,0.000050540566,0.0002670422,0.00013965985,0.00021139589,0.00030416631],"domain_scores_gemma":[0.9992218,0.00008039742,0.00013512938,0.000091937465,0.000068366484,0.00040235565],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038924342,0.00008488014,0.00019019327,0.00006849047,0.00025128986,0.00004586568,0.00044889122,0.000052699976,0.028979182],"category_scores_gemma":[0.00011405037,0.000046518115,0.00009972669,0.00040705138,0.0008930025,0.00011425594,0.000006168036,0.00016332514,0.000019022253],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005547077,0.0000027467706,0.9914862,0.0000037809787,0.000012069694,0.000013547816,0.000051386174,0.0011991924,0.00008810183,0.000013876063,0.00011739963,0.007006154],"study_design_scores_gemma":[0.000094256204,0.00011690366,0.9742589,0.000015485477,0.000021835784,0.00015960398,0.00006680902,0.0005773468,0.0003878076,0.0032276786,0.020998945,0.00007444932],"about_ca_topic_score_codex":0.01339911,"about_ca_topic_score_gemma":0.48678058,"teacher_disagreement_score":0.47338146,"about_ca_system_score_codex":4.3201874e-7,"about_ca_system_score_gemma":0.00030905564,"threshold_uncertainty_score":0.99317074},"labels":[],"label_agreement":null},{"id":"W2040776738","doi":"10.1139/e00-068","title":"Seismic imaging of the upper mantle beneath the Rocky Mountain foreland, southwestern Alberta","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Geological Survey of Canada; Western University","funders":"","keywords":"Geology; Seismology; Foreland basin; Crust; Mantle (geology); Tectonics; Geochemistry","score_opus":0.0074339561446724305,"score_gpt":0.1837045797332695,"score_spread":0.17627062358859708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040776738","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99293363,0.00044097923,0.0000054316424,0.001501741,0.0005187813,0.000070083835,0.000065635126,0.0000010454035,0.0044626733],"genre_scores_gemma":[0.99842936,0.000017861244,0.000041489486,0.0003635888,0.00015259538,1.313968e-7,0.0000014460676,0.0000019827162,0.0009915305],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99897647,0.000074816344,0.0002548443,0.0001081201,0.0002637311,0.00032204652],"domain_scores_gemma":[0.9993503,0.0000903569,0.00016588312,0.00014679262,0.000051561918,0.00019508287],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000558598,0.000090673784,0.00014486801,0.00006889386,0.0004951765,0.0001791429,0.00072124053,0.000022328366,0.0029419295],"category_scores_gemma":[0.000026302303,0.00004382044,0.000086600834,0.00022794314,0.0003834772,0.0002622929,0.000005951248,0.00009783228,0.000057891313],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057608627,0.0000020345733,0.97843164,0.000003901241,0.000011092808,0.000006520732,0.0010607564,0.01665285,0.000035261466,0.00010104736,0.00026346353,0.0034256927],"study_design_scores_gemma":[0.0001443776,0.00007171689,0.95914805,0.000055861587,0.000025654046,0.00011096415,0.00041686668,0.0032537975,0.00027519523,0.0014137004,0.034976445,0.000107354186],"about_ca_topic_score_codex":0.1288067,"about_ca_topic_score_gemma":0.40722236,"teacher_disagreement_score":0.27841565,"about_ca_system_score_codex":0.0000010275992,"about_ca_system_score_gemma":0.00058706285,"threshold_uncertainty_score":0.9979695},"labels":[],"label_agreement":null},{"id":"W2040958897","doi":"10.1139/e06-012","title":"A new study of<i>Marrella splendens</i>(Arthropoda, Marrellomorpha) from the Middle Cambrian Burgess Shale, British Columbia, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum","funders":"","keywords":"Seta; Appendage; Fauna; Paleontology; Geology; Arthropod; Oil shale; Range (aeronautics); Anatomy; Archaeology; Biology; Geography; Genus; Ecology","score_opus":0.017425509387323963,"score_gpt":0.18522236091406308,"score_spread":0.16779685152673912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040958897","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97054935,0.012984873,0.000007261375,0.00028828165,0.0013651149,0.00016264227,0.0002907101,0.00000312256,0.014348678],"genre_scores_gemma":[0.9987424,0.00003320923,0.00027379984,0.00010390543,0.0003180431,2.1192452e-7,0.0000043293367,0.0000013994828,0.0005226804],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99783325,0.00018752854,0.0005702011,0.00025934144,0.000609368,0.00054029893],"domain_scores_gemma":[0.9983541,0.00030178874,0.0004022927,0.00017941091,0.00012939831,0.0006330465],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00063185376,0.00013323405,0.00034964996,0.00008294492,0.00092628703,0.00043770755,0.0008550499,0.000068938905,0.0024446016],"category_scores_gemma":[0.00005655921,0.00013061515,0.00010121611,0.00051959575,0.0006795428,0.0002728533,0.000002228058,0.00027470972,0.0000029439393],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000052617825,0.000010343185,0.97055525,0.0000019017073,0.000030726285,0.0004928519,0.00019952304,0.000112219925,0.0000021622275,0.000005037476,0.008771568,0.019813187],"study_design_scores_gemma":[0.00039794442,0.00033300635,0.9911112,0.000058040237,0.00003609395,0.00023539815,0.0023939903,0.00005127368,0.000004235526,0.00033406442,0.0048880633,0.00015664265],"about_ca_topic_score_codex":0.9996765,"about_ca_topic_score_gemma":0.9999974,"teacher_disagreement_score":0.028193105,"about_ca_system_score_codex":0.0000032151977,"about_ca_system_score_gemma":0.006461174,"threshold_uncertainty_score":0.99917126},"labels":[],"label_agreement":null},{"id":"W2041420860","doi":"10.1139/e04-057","title":"Revised chronostratigraphy of the Kenai Group from <sup>40</sup>Ar/<sup>39</sup>Ar dating of low-potassium bearing minerals, Cook Inlet Basin, Alaska","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Geological Society of America","keywords":"Geology; Chronostratigraphy; Outcrop; Paleontology; Structural basin; Facies; Unconformity; Geochemistry; Geomorphology","score_opus":0.012859833092496564,"score_gpt":0.18357343244764793,"score_spread":0.17071359935515137,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041420860","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99436665,0.0018233916,0.000030088111,0.0016428073,0.00011247563,0.00011227955,0.00017983998,0.000004815931,0.0017276689],"genre_scores_gemma":[0.99729884,0.00006256627,0.0019474851,0.00043402787,0.00018018488,3.4240233e-7,0.000019564588,0.0000029071828,0.000054064705],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997334,0.00016567833,0.0008748396,0.00034776397,0.0006668667,0.00061081926],"domain_scores_gemma":[0.9979568,0.00026033932,0.00063066266,0.00026160246,0.0001995636,0.00069101737],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008767858,0.00023868644,0.0005556393,0.0003024308,0.0004352935,0.00013583232,0.0011183975,0.000109913344,0.0041230586],"category_scores_gemma":[0.0004437657,0.00014718951,0.00036014014,0.0013728926,0.0013549619,0.00047358734,0.00002486041,0.00038493096,0.000018171002],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013463096,0.00002021909,0.91385007,0.000029020244,0.00005802088,0.00002842308,0.00047689123,0.083343185,0.0005773728,0.000041503918,0.00023968994,0.0013221637],"study_design_scores_gemma":[0.0006454867,0.0005188644,0.9790506,0.0005212709,0.00011085217,0.000046414923,0.0011359125,0.010839696,0.0023865516,0.0028654733,0.0015320863,0.00034680188],"about_ca_topic_score_codex":0.049704805,"about_ca_topic_score_gemma":0.06420272,"teacher_disagreement_score":0.07250349,"about_ca_system_score_codex":0.000004960607,"about_ca_system_score_gemma":0.0006126025,"threshold_uncertainty_score":0.9967873},"labels":[],"label_agreement":null},{"id":"W2041913386","doi":"10.1139/e04-049","title":"Eggs of titanosaurid sauropods from the Upper Cretaceous of Auca Mahuevo (Argentina)","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Fundación Antorchas; National Geographic Society; University of Southern California","keywords":"Eggshell; Sauropoda; Cretaceous; Geology; Paleontology; Shell (structure); Apex (geometry); Extant taxon; Calcite; Biology; Anatomy; Materials science; Composite material","score_opus":0.017308409116841405,"score_gpt":0.22246156687594137,"score_spread":0.20515315775909998,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041913386","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98276836,0.008697498,0.000033403223,0.002393583,0.0008383839,0.00004377124,0.00013938932,0.0000016179395,0.0050840033],"genre_scores_gemma":[0.99806035,0.000107465195,0.0014341191,0.00022307562,0.00011515803,5.7802584e-8,0.000005195359,9.305433e-7,0.00005363815],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989243,0.000102897946,0.0003321818,0.00012380864,0.00020661773,0.0003101973],"domain_scores_gemma":[0.9990541,0.00018476725,0.0002912912,0.00011376102,0.00010752831,0.00024859922],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006175835,0.000085095395,0.00020757469,0.0001525393,0.000282103,0.00001607493,0.0005971109,0.00007135576,0.0021949923],"category_scores_gemma":[0.00017855442,0.00005267703,0.00009960327,0.00032763797,0.0016485513,0.00019876708,0.0000043833165,0.00015520006,0.00003239657],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014253872,0.000004358467,0.99635565,0.0000018216921,0.000019981284,0.000031982832,0.00024893266,0.0017706375,0.000103351325,0.00042558706,0.00020647296,0.00081694167],"study_design_scores_gemma":[0.00016323061,0.00034052067,0.9872389,0.00003211107,0.000016918464,0.00015241088,0.00034312092,0.0000674651,0.00025616627,0.0032081006,0.008116717,0.00006436607],"about_ca_topic_score_codex":0.026518263,"about_ca_topic_score_gemma":0.4620478,"teacher_disagreement_score":0.43552953,"about_ca_system_score_codex":0.0000017836909,"about_ca_system_score_gemma":0.0016681763,"threshold_uncertainty_score":0.9987171},"labels":[],"label_agreement":null},{"id":"W2041919422","doi":"10.1139/e00-121","title":"The Cheslatta Lake suite: Miocene mafic, alkaline magmatism in central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; University of British Columbia; Geological Survey of Canada","funders":"Division of Ocean Sciences; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Phenocryst; Basalt; Geochemistry; Olivine; Xenolith; Basaltic andesite; Mafic; Alkali basalt; Augite; Volcanic rock; Pyroxene; Plagioclase; Andesite; Petrology; Volcano; Paleontology","score_opus":0.011851324243854783,"score_gpt":0.18384521315361257,"score_spread":0.17199388890975778,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041919422","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98970497,0.0024672016,0.0000052826626,0.0027000061,0.0002795437,0.000048580834,0.00003951057,0.0000029781936,0.004751936],"genre_scores_gemma":[0.99780923,0.000351856,0.0002987899,0.00042665703,0.00012637151,1.4559589e-7,0.0000071761206,9.953475e-7,0.0009787712],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983772,0.00007519937,0.00038480893,0.00016500983,0.00030856903,0.00068921363],"domain_scores_gemma":[0.9988664,0.00016518896,0.00014155377,0.00008075495,0.00007770696,0.00066838774],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009025253,0.000076273944,0.00019329149,0.00008295384,0.00054626237,0.0007165445,0.0005803358,0.000050090614,0.02052595],"category_scores_gemma":[0.00026904122,0.00006232372,0.00009820542,0.0008599278,0.0006491798,0.00024315302,0.0000060903894,0.0002155781,0.000049260736],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000023804275,0.0000032439036,0.9783181,0.0000011260391,0.0000056732424,0.00028720393,0.000026105456,0.00091812457,0.0000031212542,0.0000076075507,0.000875272,0.019552052],"study_design_scores_gemma":[0.00012994997,0.00008764744,0.9462943,0.00002381434,0.0000071910436,0.0003228022,0.0001227638,0.0011814168,0.000003236852,0.0074683307,0.044265807,0.00009270154],"about_ca_topic_score_codex":0.44339654,"about_ca_topic_score_gemma":0.9993359,"teacher_disagreement_score":0.5559394,"about_ca_system_score_codex":0.0000017220566,"about_ca_system_score_gemma":0.00040704585,"threshold_uncertainty_score":0.98036945},"labels":[],"label_agreement":null},{"id":"W2042018162","doi":"10.1139/e02-051","title":"Communities and paleoecology of Eifelian (mid-Devonian) brachiopods from the Bird Fiord Formation of Arctic Canada","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Benthic zone; Geology; Arctic; Siliciclastic; Paleoecology; Fjord; Biota; Fauna; Paleontology; Oceanography; Peninsula; Ecology; Geography; Sedimentary depositional environment; Archaeology; Structural basin; Biology","score_opus":0.02583572447814514,"score_gpt":0.19711995235299581,"score_spread":0.17128422787485068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042018162","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9842369,0.010082936,0.0000066495872,0.001210261,0.00030562928,0.000042327265,0.000074488664,0.0000012218211,0.004039617],"genre_scores_gemma":[0.9993907,0.00016232872,0.0002563835,0.00015012907,0.00003264448,8.1304165e-8,9.343368e-7,4.6123242e-7,0.000006289814],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990271,0.00016571663,0.00033921018,0.000057521047,0.00018682407,0.00022365914],"domain_scores_gemma":[0.9987625,0.0005217951,0.0003232755,0.00009235645,0.000083993626,0.00021609223],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046130002,0.00007520916,0.00019237361,0.00014515068,0.00041064862,0.00003477515,0.00040396227,0.000044991353,0.000537622],"category_scores_gemma":[0.000086641194,0.0000498228,0.000040400806,0.0002311481,0.0012465834,0.00031820178,0.0000012243015,0.00016347495,7.732031e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003629565,0.0000017671949,0.9863889,0.0000065267736,0.000011208083,0.00000902553,0.001528281,0.00008172908,0.0000057998514,0.00003149199,0.00006522619,0.011866382],"study_design_scores_gemma":[0.00012114819,0.00023407253,0.9948747,0.000042617885,0.000012505607,0.00007747367,0.0031467613,0.0004935327,0.00004319778,0.00046441442,0.0004341939,0.00005537476],"about_ca_topic_score_codex":0.8752645,"about_ca_topic_score_gemma":0.99987775,"teacher_disagreement_score":0.12461322,"about_ca_system_score_codex":0.0000012109535,"about_ca_system_score_gemma":0.00070588366,"threshold_uncertainty_score":0.58865845},"labels":[],"label_agreement":null},{"id":"W2042226423","doi":"10.1139/e01-090","title":"A U–Pb geochronological review of the Proterozoic history of the eastern Grenville Province","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":245,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Royal Ontario Museum","funders":"","keywords":"Geology; Mafic; Subduction; Magmatism; Craton; Geochemistry; Archean; Proterozoic; Felsic; Continental margin; Continental arc; Paleontology; Tectonics","score_opus":0.029471596071611678,"score_gpt":0.1742278859944763,"score_spread":0.14475628992286463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042226423","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9240612,0.057114713,0.0000024728524,0.005962794,0.00037504113,0.00016357188,0.000015821955,0.0000013078933,0.012303078],"genre_scores_gemma":[0.9976282,0.00040391635,0.00013649205,0.0008630983,0.000037694208,2.3193091e-7,2.0416647e-7,5.543569e-7,0.00092958467],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987419,0.0001229945,0.00038984872,0.00012372008,0.00037652114,0.00024497547],"domain_scores_gemma":[0.9990188,0.00006205057,0.00044461587,0.00016165263,0.00010654222,0.00020636701],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00054576196,0.00008367476,0.0002413604,0.00005816191,0.00012682566,0.000010908498,0.00094756746,0.000037312286,0.010902424],"category_scores_gemma":[0.00039693978,0.000034519104,0.00022095759,0.0004174858,0.001494936,0.0000852494,0.000017127972,0.00018182876,0.000019245002],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000023454893,0.000012739304,0.99114823,0.0001508817,0.0000143626585,0.000008937703,0.00009000047,0.00021749068,0.00012376798,0.000046113902,0.0014785106,0.0067066345],"study_design_scores_gemma":[0.0001494959,0.0004450964,0.9271193,0.0015941337,0.00006794947,0.00012619603,0.000071370654,0.0016956432,0.0004160476,0.0013675134,0.066785,0.0001622285],"about_ca_topic_score_codex":0.009390961,"about_ca_topic_score_gemma":0.13267127,"teacher_disagreement_score":0.1232803,"about_ca_system_score_codex":0.0000043836585,"about_ca_system_score_gemma":0.00060931215,"threshold_uncertainty_score":0.9972056},"labels":[],"label_agreement":null},{"id":"W2042661888","doi":"10.1139/e99-112","title":"The subglacial geomorphology of southeast Alberta: evidence for subglacial meltwater erosion","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Geological Society of America","keywords":"Geology; Meltwater; Landform; Drumlin; Geomorphology; Fluvial; Bedrock; Erosion; Glacial landform; Glacial period; Paleontology; Ice stream; Moraine; Cryosphere; Oceanography; Structural basin","score_opus":0.04791955357236928,"score_gpt":0.27066948515309025,"score_spread":0.22274993158072098,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042661888","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99313796,0.0016146298,0.00001240866,0.0027222922,0.00063277275,0.00013117219,0.000023635905,0.0000012262411,0.0017239337],"genre_scores_gemma":[0.99874103,0.00009800742,0.0001713981,0.00011557508,0.00014880282,6.035812e-7,0.0000038891767,0.0000015007198,0.0007192017],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983836,0.00021118298,0.0003832682,0.00016674059,0.0002347961,0.00062043534],"domain_scores_gemma":[0.99790746,0.0012813101,0.00016469308,0.00011380054,0.00016924055,0.00036346802],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0021744408,0.00009865047,0.00022279233,0.00017264335,0.0010502734,0.00007059985,0.00070672896,0.000103901126,0.004940042],"category_scores_gemma":[0.00051132066,0.00005903067,0.00011036882,0.00028426104,0.0022502637,0.0002727307,0.000003965636,0.00020248885,0.0001192099],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001455154,0.0000022359693,0.9969517,0.000004614718,0.000008706162,0.000017114726,0.0003071517,0.0003583418,0.000014141118,0.0001337074,0.00013101111,0.0019257605],"study_design_scores_gemma":[0.00032717155,0.00079383835,0.9846786,0.00004518342,0.000019040603,0.0004619838,0.0002968298,0.00034548936,0.00023895722,0.0013706604,0.01131365,0.00010857768],"about_ca_topic_score_codex":0.014277335,"about_ca_topic_score_gemma":0.8718476,"teacher_disagreement_score":0.8575703,"about_ca_system_score_codex":4.3919394e-7,"about_ca_system_score_gemma":0.0012934513,"threshold_uncertainty_score":0.9959696},"labels":[],"label_agreement":null},{"id":"W2042789747","doi":"10.1139/e00-111","title":"Late Quaternary glacial and interglacial environments of the Nechako River - Cheslatta Lake area, central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"British Geological Survey","keywords":"Geology; Glacial period; Quaternary; Tributary; Interglacial; Glacial lake; Glacier; Geomorphology; Paleontology; Geography","score_opus":0.016431312922586684,"score_gpt":0.2000006823215917,"score_spread":0.18356936939900503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042789747","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996471,0.00052603637,0.000004185034,0.00045162425,0.0005616503,0.000061021103,0.000031280328,0.0000010367578,0.0018921855],"genre_scores_gemma":[0.9988175,0.00012548965,0.00006680181,0.00014514229,0.00006771571,8.880919e-8,0.0000019245317,0.0000010943726,0.0007742581],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883294,0.00012126956,0.00023633952,0.0001364307,0.00022838695,0.00044460714],"domain_scores_gemma":[0.9993222,0.000064948086,0.00014763675,0.000072232084,0.000024326364,0.00036866215],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005157279,0.000063576495,0.00016423999,0.000075750126,0.00048472267,0.00012267655,0.00044391054,0.00007488262,0.0033586493],"category_scores_gemma":[0.00007476526,0.00005880059,0.00005932171,0.00019951878,0.0021246371,0.00020468475,0.000013945832,0.00022081318,0.000011035077],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009000636,0.0000024695835,0.9979319,0.0000021771702,0.000011045472,0.00017804294,0.00025058334,0.00015010092,0.0000034412187,0.0000032288308,0.00009130985,0.0013666914],"study_design_scores_gemma":[0.00019772073,0.0001523784,0.9940781,0.000033736742,0.000008570633,0.00085750397,0.0000832308,0.00024951206,0.000007351007,0.00079502474,0.0034731023,0.000063782354],"about_ca_topic_score_codex":0.043483313,"about_ca_topic_score_gemma":0.9870388,"teacher_disagreement_score":0.9435555,"about_ca_system_score_codex":4.9878025e-7,"about_ca_system_score_gemma":0.00042815282,"threshold_uncertainty_score":0.9975524},"labels":[],"label_agreement":null},{"id":"W2042824847","doi":"10.1139/e00-025","title":"Emplacement of the Nain anorthosite: diapiric versus conduit ascent","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Anorthosite; Diapir; Geochemistry; Shear zone; Layered intrusion; Electrical conduit; Petrology; Mafic; Crust; Archean; Magma; Magma chamber; Pluton; Lineation; Batholith; Tectonics; Plagioclase; Seismology; Volcano; Paleontology","score_opus":0.024921691154309786,"score_gpt":0.20972043797388612,"score_spread":0.18479874681957634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042824847","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9852805,0.0011081286,0.0000013742444,0.0011735405,0.0002794404,0.000039858125,0.000018256615,0.0000013412891,0.012097543],"genre_scores_gemma":[0.99913347,0.000040924984,0.00014201614,0.00030402784,0.000052479438,7.177046e-8,0.0000013930545,5.3377045e-7,0.0003251087],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988514,0.00007456298,0.00028974956,0.00012127837,0.000352626,0.00031036738],"domain_scores_gemma":[0.999175,0.000106935884,0.00014506877,0.00009737792,0.00007234049,0.00040324387],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005035439,0.00008099872,0.00016472158,0.000094925745,0.00028011148,0.000050619197,0.00052893796,0.000032008455,0.03579873],"category_scores_gemma":[0.00008361865,0.00004292934,0.00014376735,0.0006913599,0.0006108255,0.00012325835,0.000004428605,0.0001260033,0.000059788585],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019663477,0.000005879765,0.9819636,0.0000023966309,0.000018480594,0.000012571615,0.000107262786,0.0059040934,0.000032268064,0.000050074348,0.00021499056,0.0116687445],"study_design_scores_gemma":[0.00022515311,0.00033295716,0.9778084,0.000019430921,0.00002744693,0.000020018857,0.00013852575,0.00048822854,0.00034272383,0.00079128315,0.019720852,0.00008493659],"about_ca_topic_score_codex":0.035181254,"about_ca_topic_score_gemma":0.42907923,"teacher_disagreement_score":0.39389798,"about_ca_system_score_codex":0.0000014334174,"about_ca_system_score_gemma":0.00045211153,"threshold_uncertainty_score":0.97124356},"labels":[],"label_agreement":null},{"id":"W2042825329","doi":"10.1139/e00-075","title":"Tectonic deformation and magmatism along the southern flank of the Maritimes Basin: the northeastern Cobequid Highlands, Nova Scotia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Bedford Institute of Oceanography","funders":"","keywords":"Geology; Terrane; Carboniferous; Tournaisian; Paleozoic; Devonian; Thrust fault; Pluton; Sill; Geochemistry; Allochthon; Paleontology; Mylonite; Fault (geology); Tectonics; Nappe; Structural basin; Shear zone","score_opus":0.011654810500704655,"score_gpt":0.17734008731372589,"score_spread":0.16568527681302123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042825329","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9872767,0.0016072374,0.000014159349,0.008717875,0.00015856388,0.00006254305,0.000024800178,0.0000015462364,0.00213658],"genre_scores_gemma":[0.9992627,0.000038271875,0.0000513511,0.00048699888,0.0000697715,6.919591e-8,0.0000016528937,7.737727e-7,0.00008840828],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989415,0.00010741705,0.0002897313,0.00009304296,0.00030237396,0.00026597205],"domain_scores_gemma":[0.99922955,0.0001726307,0.00022227288,0.00011436875,0.00008463645,0.00017652642],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00089646905,0.000085944484,0.00014209804,0.000070816146,0.00047072084,0.00013024149,0.0005756133,0.0000317864,0.0028848017],"category_scores_gemma":[0.000110866924,0.000031383563,0.000089874855,0.00050548307,0.00095449644,0.0002131794,0.00001286229,0.00016409713,0.000035152192],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000039332435,0.0000014989434,0.9931543,0.0000028349577,0.0000112639655,0.0000045950837,0.000291329,0.0009892205,0.000010749886,0.000047435784,0.000030358744,0.005452492],"study_design_scores_gemma":[0.00008487542,0.000079302925,0.9926492,0.00003410879,0.000028443685,0.0002569126,0.0008977875,0.0025096831,0.000044878954,0.0020956346,0.0012600212,0.00005917218],"about_ca_topic_score_codex":0.11763996,"about_ca_topic_score_gemma":0.87276626,"teacher_disagreement_score":0.7551263,"about_ca_system_score_codex":8.888164e-7,"about_ca_system_score_gemma":0.0002376993,"threshold_uncertainty_score":0.99802667},"labels":[],"label_agreement":null},{"id":"W2043095369","doi":"10.1139/e06-036","title":"Pickle Lake revisited: New structural, geochronological and geochemical constraints on greenstone belt assembly, western Superior Province, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Queen's University","funders":"","keywords":"Geology; Basalt; Geochemistry; Zircon; Island arc; Pyroclastic rock; Felsic; Continental arc; Volcanic belt; Greenstone belt; Volcanic rock; Subduction; Volcano; Paleontology; Tectonics; Archean","score_opus":0.011130849284670709,"score_gpt":0.19079431630825563,"score_spread":0.17966346702358493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043095369","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.992697,0.0011967669,0.000004669378,0.0027103315,0.0001348964,0.00006941988,0.00010524734,0.0000055449946,0.0030761105],"genre_scores_gemma":[0.998238,0.000018133442,0.00053114066,0.00073988974,0.0002346433,9.175415e-8,0.000027134285,0.0000014432574,0.00020950468],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982154,0.00004897059,0.0004082066,0.0003118963,0.0004260415,0.00058953435],"domain_scores_gemma":[0.9985155,0.00015563115,0.00017293758,0.000098078664,0.0000898902,0.0009679567],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002828349,0.00018916972,0.00035435965,0.00014760811,0.00036213626,0.00017287962,0.00039673597,0.00009011962,0.006503425],"category_scores_gemma":[0.00016119161,0.0001222251,0.00007830536,0.00035170148,0.0010640178,0.00020226782,0.000011462269,0.00029517236,0.000014910404],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009462435,0.0000029943646,0.9884091,0.000004655866,0.000010848305,0.0002723568,0.0000076439455,0.00040498027,0.000114578805,0.0000944429,0.001141023,0.0095279375],"study_design_scores_gemma":[0.0002125313,0.00030082345,0.9905071,0.0000347669,0.00002128037,0.00036649202,0.000045041263,0.0002597428,0.00022702683,0.0013063782,0.0065223523,0.00019643344],"about_ca_topic_score_codex":0.85030454,"about_ca_topic_score_gemma":0.9991268,"teacher_disagreement_score":0.14882225,"about_ca_system_score_codex":0.0000052263176,"about_ca_system_score_gemma":0.002385655,"threshold_uncertainty_score":0.9944048},"labels":[],"label_agreement":null},{"id":"W2043210491","doi":"10.1139/e03-900","title":"Erratum: A replacement name for <i>Lanthanocephalus</i> Modesto, Rubidge, and Welman 2002, not <i>Lanthanocephalus</i> Williams and Starmer 2000","year":2003,"lang":"en","type":"erratum","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Art history; Art","score_opus":0.02562779507191827,"score_gpt":0.23627870625005945,"score_spread":0.2106509111781412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043210491","genre_codex":"review","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.05482358,0.4731595,0.00036268856,0.011714283,0.072615646,0.0021583228,0.004945376,0.000056227625,0.38016438],"genre_scores_gemma":[0.23332812,0.0540205,0.012902984,0.020180233,0.0050447085,0.000024160992,0.00042072713,0.000101409576,0.67397714],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9966327,0.00019258856,0.0007844203,0.0006811582,0.0005923109,0.0011168214],"domain_scores_gemma":[0.99728113,0.00021931891,0.00070421223,0.00022020203,0.00029455597,0.0012805663],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017161032,0.0005136944,0.0008751544,0.0006519934,0.0013877855,0.0003428479,0.000524061,0.00039222257,0.0011150435],"category_scores_gemma":[0.00025034978,0.00041265227,0.00016403057,0.0003877209,0.0020121562,0.00049730483,0.000014286951,0.00073661143,0.000020987594],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007086131,0.000009539444,0.13029143,0.000102310776,0.00012298183,0.00008387939,0.00054824835,0.000074893986,0.0000025668487,0.00012959917,0.8672992,0.001264478],"study_design_scores_gemma":[0.00077548024,0.0012897744,0.051676903,0.00030585556,0.00015868332,0.0007871975,0.0007216857,0.000994005,0.000007316228,0.00041636272,0.94226444,0.0006023068],"about_ca_topic_score_codex":0.008191878,"about_ca_topic_score_gemma":0.61783665,"teacher_disagreement_score":0.6096448,"about_ca_system_score_codex":0.00001065896,"about_ca_system_score_gemma":0.0037887958,"threshold_uncertainty_score":0.99991226},"labels":[],"label_agreement":null},{"id":"W2043249308","doi":"10.1139/e05-098","title":"Chemical imprint of highly metamorphosed volcanic-hosted hydrothermal alterations in the La Romaine Supracrustal Belt, eastern Grenville Province, Quebec","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Institut National de la Recherche Scientifique","funders":"","keywords":"Geology; Geochemistry; Felsic; Volcanic rock; Gneiss; Mafic; Pyroclastic rock; Silicic; Metamorphism; Petrology; Metamorphic rock; Volcano","score_opus":0.010882229035551466,"score_gpt":0.19313760883439604,"score_spread":0.18225537979884457,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043249308","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99178267,0.000504643,0.000015910611,0.0036912104,0.000045331486,0.0000796971,0.000031434272,0.0000019804288,0.0038471306],"genre_scores_gemma":[0.99873054,0.0000063373436,0.0006772109,0.0003298166,0.00010346408,4.063009e-7,0.0000072564,0.0000012022392,0.00014375689],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984856,0.00015147081,0.00046261252,0.00016669062,0.0003676333,0.00036594423],"domain_scores_gemma":[0.9990752,0.00020294255,0.0002105059,0.000108701905,0.000074658594,0.00032803795],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009850123,0.00011792008,0.00024301579,0.00021596554,0.00015172597,0.00010629617,0.0006204799,0.000055669192,0.0024442368],"category_scores_gemma":[0.00015061938,0.00006700855,0.00012888799,0.0006073419,0.00065669545,0.00026533953,0.0000090345175,0.00024104556,0.000021281288],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004803234,0.00008159989,0.958019,0.000011682664,0.00005529208,0.00020198655,0.0010900175,0.016558148,0.005316867,0.0012826845,0.00015584697,0.017178835],"study_design_scores_gemma":[0.00067349133,0.00040939418,0.95814425,0.000055572433,0.00006344049,0.000284289,0.000990341,0.02173512,0.0057686483,0.0010816762,0.010479716,0.00031408868],"about_ca_topic_score_codex":0.17395243,"about_ca_topic_score_gemma":0.9419546,"teacher_disagreement_score":0.76800215,"about_ca_system_score_codex":0.0000034050277,"about_ca_system_score_gemma":0.00079189934,"threshold_uncertainty_score":0.9984677},"labels":[],"label_agreement":null},{"id":"W2043671455","doi":"10.1139/e04-013","title":"Whole-rock trace-element analyses applied to the regional sourcing of ancient basalt vessels from Egypt and Jordan","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Okanagan University College","funders":"","keywords":"Basalt; Provenance; Bedrock; Geology; Geochemistry; Archaeology; Trace element; Paleontology; Geography","score_opus":0.044837349968488885,"score_gpt":0.2558249064957317,"score_spread":0.21098755652724283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043671455","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9438272,0.0011376172,0.030043857,0.023542225,0.00021252688,0.000091924456,0.0000061433348,0.0000041746857,0.0011342929],"genre_scores_gemma":[0.9906801,0.0000052741257,0.008258761,0.0009206933,0.00008464441,0.0000010093348,2.862147e-7,9.458318e-7,0.000048312526],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9987771,0.000028908773,0.000309762,0.00021803362,0.00035254747,0.00031367215],"domain_scores_gemma":[0.9989265,0.00007324144,0.00023816901,0.00018243816,0.00014394177,0.00043569683],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00080945855,0.00009498832,0.00017000677,0.00017307214,0.00040137215,0.00017523447,0.0009037082,0.000026824482,0.000022913062],"category_scores_gemma":[0.00010267635,0.000063556814,0.000051485342,0.00060288963,0.00018760357,0.00019264981,0.000048993752,0.00012174575,0.0000031778707],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023680444,0.000085745436,0.020827692,0.000048201262,0.00014243233,0.00017960953,0.027488343,0.82372177,0.08112301,0.028307715,0.0051759914,0.012875816],"study_design_scores_gemma":[0.0020540475,0.0013547598,0.483822,0.0008396733,0.00009340515,0.0005235809,0.014938809,0.010574302,0.10543871,0.049015302,0.33024386,0.0011015752],"about_ca_topic_score_codex":0.0016988459,"about_ca_topic_score_gemma":0.0083606625,"teacher_disagreement_score":0.8131475,"about_ca_system_score_codex":0.00001010335,"about_ca_system_score_gemma":0.0012099871,"threshold_uncertainty_score":0.4665446},"labels":[],"label_agreement":null},{"id":"W2043956459","doi":"10.1139/e06-119","title":"Karst-related outliers of the Cretaceous Chaswood Formation of Maritime Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University; University of Windsor; Bedford Institute of Oceanography; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Cretaceous; Paleontology; Carboniferous; Karst; Fluvial; Petrography; Outcrop; Facies; Palynology; Geochemistry; Structural basin","score_opus":0.014201128118110267,"score_gpt":0.20938052841763657,"score_spread":0.1951794002995263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043956459","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98689246,0.0012964167,0.000010959354,0.0008640785,0.00055354065,0.00006398455,0.000022030468,7.8502666e-7,0.01029576],"genre_scores_gemma":[0.9996362,0.000013355757,0.000110706496,0.00009462953,0.0000149973175,2.6422065e-8,0.0000016143557,7.31694e-7,0.00012777816],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998693,0.0000965201,0.0004148206,0.00007303454,0.00034491043,0.00037772008],"domain_scores_gemma":[0.9989065,0.00022073266,0.0003245643,0.000089921,0.0001647824,0.00029350547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017419243,0.00006375241,0.00017110482,0.00023222702,0.00029370812,0.000012841528,0.0005079892,0.00006858136,0.00072415866],"category_scores_gemma":[0.00023979304,0.000041514115,0.000058209287,0.00054089463,0.0009947655,0.00018895834,0.0000046335126,0.00021757615,0.000004692563],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007783575,0.00000140021,0.99808526,0.000007498443,0.000008009242,0.000039024584,0.00024006772,0.0010509868,0.0000072603466,0.00006844171,0.000075695236,0.00040854336],"study_design_scores_gemma":[0.00015000894,0.00015484034,0.99592346,0.000031074687,0.000009338244,0.00049412844,0.0006604278,0.00058090047,0.00063745514,0.0003811244,0.00092649966,0.000050767227],"about_ca_topic_score_codex":0.305866,"about_ca_topic_score_gemma":0.99713296,"teacher_disagreement_score":0.69126695,"about_ca_system_score_codex":0.0000011449043,"about_ca_system_score_gemma":0.0032473071,"threshold_uncertainty_score":0.79290295},"labels":[],"label_agreement":null},{"id":"W2044215981","doi":"10.1139/e01-041","title":"The Silurian(?) Passamaquoddy Bay mafic dyke swarm, New Brunswick: petrogenesis and tectonic implications","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University","funders":"","keywords":"Mafic; Geology; Geochemistry; Felsic; Petrogenesis; Basalt; Volcanic rock; Andesite; Mantle (geology); Petrology; Volcano","score_opus":0.017447435578217863,"score_gpt":0.2019982622836587,"score_spread":0.18455082670544082,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044215981","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9739227,0.0070884395,0.00006199539,0.015874363,0.00015370961,0.000046820493,0.00000711945,0.0000050211024,0.0028398104],"genre_scores_gemma":[0.99774265,0.0005097573,0.00040693834,0.00039468083,0.00015847197,1.1970604e-7,0.000001848625,0.0000011796942,0.00078436144],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987222,0.00005940667,0.00030139598,0.0001923115,0.00022929498,0.0004953825],"domain_scores_gemma":[0.9983362,0.00027901714,0.00015436434,0.00012524278,0.00009404999,0.0010111191],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00063662353,0.00011241723,0.00016868912,0.00016142258,0.0010444574,0.00029616954,0.00054883177,0.00004488228,0.0026112539],"category_scores_gemma":[0.00024085963,0.000062137,0.00010687164,0.0008463349,0.00065870985,0.00020648405,0.000007983865,0.00015738801,0.00006752548],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003387061,0.0000018579581,0.9842162,7.03035e-7,0.0000138754685,0.00001661237,0.000035901547,0.0005768439,0.000016790405,0.00030259322,0.00020056944,0.014614631],"study_design_scores_gemma":[0.00008944522,0.00012279309,0.96212333,0.000007068094,0.000025406278,0.000285135,0.0001660196,0.0008811016,0.000037034704,0.0077473684,0.028415093,0.00010022752],"about_ca_topic_score_codex":0.05752927,"about_ca_topic_score_gemma":0.89435965,"teacher_disagreement_score":0.8368304,"about_ca_system_score_codex":0.0000017116278,"about_ca_system_score_gemma":0.001548326,"threshold_uncertainty_score":0.9983005},"labels":[],"label_agreement":null},{"id":"W2044294303","doi":"10.1139/e06-060","title":"Sedimentary and structural evidence for 2.7 Ga continental arc–oceanic-arc collision in the Savant–Sturgeon greenstone belt, western Superior Province, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Terrane; Geology; Continental crust; Continental margin; Subduction; Paleontology; Volcanic arc; Continental shelf; Geochemistry; Accretionary wedge; Oceanic crust; Island arc; Flysch; Crust; Sedimentary rock; Tectonics; Oceanography","score_opus":0.016827551589464536,"score_gpt":0.21013316816167496,"score_spread":0.19330561657221043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044294303","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930308,0.0023729736,0.0000032318665,0.0040270695,0.00018682393,0.00015778899,0.00008537124,0.0000014118547,0.00013451902],"genre_scores_gemma":[0.99873173,0.000019164047,0.00023136773,0.00082288473,0.000121946345,3.9588488e-7,0.0000142243625,0.0000010176092,0.000057258057],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99854255,0.00007117454,0.00035735272,0.00020735712,0.0003851105,0.0004364637],"domain_scores_gemma":[0.99904454,0.00037683715,0.00014634462,0.000068232686,0.00006925481,0.0002947681],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00069107895,0.00012515429,0.00022266114,0.00012268541,0.00040767863,0.00014123195,0.00041328417,0.00003344145,0.0003434376],"category_scores_gemma":[0.00012002384,0.00007033081,0.000061499035,0.0003404906,0.0004553032,0.00034048167,0.000007901439,0.00015018361,0.0000010650217],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021006437,0.0000021944352,0.99802077,0.0000060931147,0.0000041711833,0.00007148577,0.0000423583,0.0007336866,0.00004932173,0.000019422228,0.00026566102,0.0007638131],"study_design_scores_gemma":[0.00022926471,0.00025230867,0.9949313,0.000049017715,0.000018215867,0.00014379308,0.0003874819,0.0018149375,0.00007026914,0.00096467545,0.001027556,0.000111186695],"about_ca_topic_score_codex":0.9495681,"about_ca_topic_score_gemma":0.99938947,"teacher_disagreement_score":0.04982135,"about_ca_system_score_codex":0.000005920469,"about_ca_system_score_gemma":0.0011111475,"threshold_uncertainty_score":0.37604007},"labels":[],"label_agreement":null},{"id":"W2045009497","doi":"10.1139/e00-038","title":"Walker Creek fault zone, central Rocky Mountains, British Columbia-southern continuation of the Northern Rocky Mountain Trench fault zone","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Thrust fault; Shear zone; Cretaceous; Seismology; Fault (geology); Trench; Strike-slip tectonics; Fibrous joint; Paleontology; Lineation; Fold (higher-order function); Outcrop; Echelon formation; Tectonics","score_opus":0.007456352808537474,"score_gpt":0.17201830479417307,"score_spread":0.16456195198563559,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045009497","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950515,0.0010147591,0.00002115208,0.0006852542,0.0001616854,0.00010582226,0.00024041702,0.0000055596415,0.0027138365],"genre_scores_gemma":[0.9929537,0.000052974065,0.00017213807,0.00037064997,0.00013965263,3.7155183e-7,0.000017860231,0.0000025885295,0.0062900707],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99763304,0.00014809679,0.0006017603,0.00027683674,0.000660621,0.00067962153],"domain_scores_gemma":[0.9984981,0.00010219559,0.00033929627,0.0001505218,0.0002541048,0.00065578014],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005964865,0.00013653236,0.00034859148,0.000080649894,0.0006761742,0.0005009868,0.00079615554,0.00009941698,0.034825403],"category_scores_gemma":[0.00015801279,0.00011616899,0.0002445952,0.0009123287,0.0007345146,0.00030853593,0.000008512611,0.00028039922,0.000078389174],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006555896,0.000013735187,0.9311489,0.0000037381953,0.000023280987,0.000032509106,0.00023944944,0.012448314,0.000028869546,0.0000011549746,0.00024679565,0.05580671],"study_design_scores_gemma":[0.00030638074,0.00022554224,0.9828011,0.000061919054,0.000050493618,0.00013096913,0.0010057671,0.0042941943,0.000042753483,0.00095901394,0.009918949,0.00020293538],"about_ca_topic_score_codex":0.8231187,"about_ca_topic_score_gemma":0.99780303,"teacher_disagreement_score":0.17468439,"about_ca_system_score_codex":0.000006663784,"about_ca_system_score_gemma":0.0006654254,"threshold_uncertainty_score":0.9660569},"labels":[],"label_agreement":null},{"id":"W2045064400","doi":"10.1139/e09-059","title":"Thermal regime of the lithosphere in the Canadian ShieldThis article is one of a series of papers published in this Special Issue on the theme<i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Lithosphere; Mantle (geology); Geothermal gradient; Geology; Crust; Heat flow; Geophysics; Earth's internal heat budget; Shield; Basin and Range Province; Heat generation; Seismic refraction; Petrology; Thermal; Tectonics; Seismology; Mantle wedge; Thermodynamics","score_opus":0.00875305441685488,"score_gpt":0.17718491727916563,"score_spread":0.16843186286231077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045064400","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97953707,0.00033235594,1.1730847e-7,0.011248052,0.00029657612,0.00024236024,0.00007065891,4.5382058e-7,0.008272362],"genre_scores_gemma":[0.99946994,0.000021728703,0.00007326574,0.00022675787,0.00013443023,9.300249e-7,3.7427537e-7,0.0000016311083,0.000070917886],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985629,0.00023258121,0.00043846882,0.00011481767,0.00039550636,0.0002557605],"domain_scores_gemma":[0.9987362,0.0003236175,0.000460902,0.00021222417,0.00015644607,0.00011061561],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0026624575,0.00009190008,0.00026249807,0.00010436148,0.00020173534,0.00010578263,0.0007560265,0.000056283294,0.0023486293],"category_scores_gemma":[0.00051327277,0.000039167993,0.00005818279,0.0007194431,0.001699786,0.00028353735,0.000009154011,0.00023005501,7.8592916e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043818814,0.00007347265,0.905803,0.00017763514,0.0000930722,0.00001518661,0.060473047,0.001196103,0.0046812603,0.022004563,0.0017103789,0.0033340843],"study_design_scores_gemma":[0.0006499572,0.0004128286,0.9681002,0.00026894233,0.000040515904,0.000017418957,0.0069679637,0.00013001534,0.011770516,0.0047507705,0.006759452,0.0001314355],"about_ca_topic_score_codex":0.6187836,"about_ca_topic_score_gemma":0.9760853,"teacher_disagreement_score":0.35730174,"about_ca_system_score_codex":0.0000026818427,"about_ca_system_score_gemma":0.0017852847,"threshold_uncertainty_score":0.99856335},"labels":[],"label_agreement":null},{"id":"W2045080436","doi":"10.1139/e03-001","title":"Bryozoan-rich layers in surficial Labrador Slope sediments, eastern Canadian Arctic","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography","funders":"","keywords":"Geology; Benthic zone; Oceanography; Waves and shallow water; Sediment; Foraminifera; Quaternary; Debris; Fjord; Arctic; Geomorphology; Geochemistry; Paleontology","score_opus":0.015641142143395452,"score_gpt":0.213595123720489,"score_spread":0.19795398157709354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045080436","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9693524,0.0005285577,0.0000055169553,0.00065800344,0.00082580745,0.00009572178,0.000004800548,0.0000017510295,0.028527405],"genre_scores_gemma":[0.9979555,0.000026052621,0.0005523767,0.0005742237,0.00004298379,6.6812254e-7,4.7622032e-7,0.0000076056217,0.0008401063],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981538,0.0001490769,0.0003651001,0.00021906657,0.00036366217,0.0007492654],"domain_scores_gemma":[0.9982963,0.000040150633,0.00015009867,0.00011125782,0.000026795484,0.0013753823],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013968277,0.00013725302,0.00018902644,0.0004113317,0.000320375,0.00012110184,0.00044178878,0.00007507421,0.0057208417],"category_scores_gemma":[0.00015744365,0.00011239619,0.00005122499,0.0011051329,0.00041952686,0.00037280188,0.0000105601775,0.0002941187,0.0002587712],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002730906,0.000011871914,0.9870285,0.000003030577,0.000010157749,0.0002910882,0.0010368162,0.008965676,0.00008935567,0.00045117713,0.00023760568,0.001872009],"study_design_scores_gemma":[0.0012014915,0.0006370454,0.8546705,0.00017640143,0.000036250218,0.00047297822,0.0031858438,0.0011053052,0.0005110701,0.0031171052,0.13410646,0.0007795514],"about_ca_topic_score_codex":0.6293149,"about_ca_topic_score_gemma":0.9815546,"teacher_disagreement_score":0.35223973,"about_ca_system_score_codex":0.00012286923,"about_ca_system_score_gemma":0.0017858762,"threshold_uncertainty_score":0.99518806},"labels":[],"label_agreement":null},{"id":"W2045448204","doi":"10.1139/e02-100","title":"Cross-strike potential-field anomalies in the Canadian Cordillera","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Foreland basin; Dike; Precambrian; Crust; Volcanic rock; Seismology; Mesozoic; Paleontology; Fault (geology); Craton; Tectonics; Volcano; Structural basin","score_opus":0.017406195037675848,"score_gpt":0.20863813860713257,"score_spread":0.19123194356945672,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045448204","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9394348,0.001033428,0.0000040759583,0.0030167722,0.0002467917,0.000042164138,0.000015218333,0.0000012761658,0.056205425],"genre_scores_gemma":[0.9974761,0.000017983208,0.00029069217,0.0020241968,0.0000577143,1.4050832e-7,0.0000021504086,6.6051695e-7,0.00013037218],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99856263,0.00012907574,0.00029151418,0.00014852833,0.0003196986,0.0005485594],"domain_scores_gemma":[0.99887484,0.00015226379,0.00010017831,0.00009358598,0.00009844807,0.00068067026],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012293208,0.00009758398,0.0001650795,0.00034281498,0.0006577904,0.0003943658,0.0006107245,0.000065354696,0.019793741],"category_scores_gemma":[0.00054441195,0.000055384957,0.00009923435,0.0008994012,0.00049810874,0.00023477047,0.0000018079476,0.000261541,0.00006203383],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001683844,0.0000024750445,0.99562144,0.0000010392845,0.0000051606817,0.00020366708,0.00009006486,0.0025810048,0.0000041776298,0.00032094138,0.000122029836,0.0010462959],"study_design_scores_gemma":[0.00009765565,0.00019289299,0.9800426,0.000009759133,0.0000091031025,0.00018747564,0.00043755965,0.00035894098,0.000094107854,0.0051816916,0.013279563,0.00010866686],"about_ca_topic_score_codex":0.70811343,"about_ca_topic_score_gemma":0.9970674,"teacher_disagreement_score":0.28895396,"about_ca_system_score_codex":0.0000024933777,"about_ca_system_score_gemma":0.0016268381,"threshold_uncertainty_score":0.9811023},"labels":[],"label_agreement":null},{"id":"W2045573767","doi":"10.1139/e08-032","title":"Sources of placer platinum in Yukon: provenance study from detrital minerals","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon University; Geological Survey of Canada","funders":"","keywords":"Geology; Chromite; Ultramafic rock; Geochemistry; Mafic; Placer mining; Provenance; Placer deposit; Platinum group; Heavy mineral; Platinum","score_opus":0.024235802855829824,"score_gpt":0.1958295543773699,"score_spread":0.17159375152154008,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045573767","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955554,0.0014122787,0.0000019429272,0.00025389463,0.00010738959,0.00006404888,0.00003381406,0.0000015839087,0.0025696207],"genre_scores_gemma":[0.9991057,0.000014222748,0.00062638015,0.00007330287,0.00007379008,1.5093838e-7,0.0000018840693,7.2080144e-7,0.00010387299],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986787,0.000069857175,0.00042917815,0.00017067819,0.0003418611,0.00030974974],"domain_scores_gemma":[0.9990849,0.00018906557,0.00022580207,0.000071762704,0.00007939305,0.0003491009],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004562286,0.00009593802,0.00029576308,0.00027284553,0.00015510972,0.00003131856,0.00040171845,0.000038123,0.0029440378],"category_scores_gemma":[0.00026103784,0.00006220013,0.000080988924,0.00079131976,0.0005157339,0.00024701277,0.0000056137646,0.00015157385,0.000016455386],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009737802,0.000018318462,0.9951619,0.0000011607888,0.000009455731,0.00019209449,0.00053654687,0.0035033193,0.00007257795,0.000003609079,0.000037336045,0.00045396865],"study_design_scores_gemma":[0.00025577768,0.00047608715,0.99593586,0.000020559519,0.0000084280055,0.000042215976,0.0008840651,0.0005188778,0.000381608,0.001160077,0.00022639858,0.000090070906],"about_ca_topic_score_codex":0.13617314,"about_ca_topic_score_gemma":0.69505143,"teacher_disagreement_score":0.5588783,"about_ca_system_score_codex":0.0000011027547,"about_ca_system_score_gemma":0.00042308067,"threshold_uncertainty_score":0.9979674},"labels":[],"label_agreement":null},{"id":"W2045686699","doi":"10.1139/e10-095","title":"Geochronology and geochemistry of Precambrian gneisses, metabasites, and pegmatite from the Tobacco Root Mountains, northwestern Wyoming craton, MontanaThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.T.E. Krogh deceased April 2008.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Northern Illinois University","keywords":"Gneiss; Geology; Geochemistry; Archean; Zircon; Terrane; Craton; Orogeny; Metamorphism; Pegmatite; Precambrian; Geochronology; Metamorphic rock; Leucogranite; Petrology; Paleontology; Tectonics","score_opus":0.014307144280035837,"score_gpt":0.17732729432229094,"score_spread":0.1630201500422551,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045686699","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99377424,0.0031736365,7.14384e-7,0.0011517713,0.000043974713,0.000098191675,0.00016719179,9.918888e-7,0.0015893052],"genre_scores_gemma":[0.9992249,0.00016589681,0.00042710808,0.00010266796,0.00005771473,5.1211595e-7,0.000004914823,0.0000016441194,0.00001463032],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983024,0.00015626774,0.0007534189,0.00022169706,0.0002660753,0.00030012656],"domain_scores_gemma":[0.99841493,0.00040984288,0.00065983407,0.00018744354,0.00015727039,0.00017068424],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009347499,0.0001449046,0.00054862094,0.0001982757,0.00008700142,0.000023398388,0.00049645425,0.00008806119,0.0091865165],"category_scores_gemma":[0.00041741383,0.0000863504,0.00009013445,0.0006270732,0.0016005986,0.000278425,0.000027948738,0.00022480509,8.6832074e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008689212,0.000036538422,0.99161905,0.000020454314,0.00004945315,0.0000115279245,0.0019760502,0.00008047812,0.0033192285,0.000055064887,0.000034602323,0.002710651],"study_design_scores_gemma":[0.000314553,0.00035525556,0.96059734,0.00013360084,0.000047310095,0.000017732273,0.0025223098,0.00018005761,0.034259386,0.0013340198,0.0001481864,0.00009023404],"about_ca_topic_score_codex":0.19211064,"about_ca_topic_score_gemma":0.84426904,"teacher_disagreement_score":0.6521584,"about_ca_system_score_codex":0.000003504281,"about_ca_system_score_gemma":0.00039857105,"threshold_uncertainty_score":0.99171925},"labels":[],"label_agreement":null},{"id":"W2045975369","doi":"10.1139/e08-022","title":"Geology of northeast British Columbia and northwest Alberta: diamonds, shallow gas, gravel, and glaciersThis article introduces a selection of papers published in this Special Issue on the theme <i>Geology of northeastern British Columbia and northwestern Alberta: diamonds, shallow gas, gravel, and glaciers</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of British Columbia","funders":"","keywords":"Geology; Kimberlite; Stratigraphy; Glacial period; Archaeology; Earth science; Geochemistry; Paleontology; Tectonics; Geography","score_opus":0.008870709331836776,"score_gpt":0.1842022089389678,"score_spread":0.17533149960713101,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045975369","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947542,0.0020344658,2.6062511e-7,0.001063154,0.0002831081,0.0002855292,0.00006716144,0.0000025133206,0.0015096162],"genre_scores_gemma":[0.99765563,0.0012843057,0.000066733184,0.00017468467,0.00017464584,0.0000023222885,0.000013893849,0.000006437665,0.0006213315],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971038,0.00040519802,0.0007950327,0.0005465802,0.0003851837,0.0007642115],"domain_scores_gemma":[0.99768716,0.00079940015,0.0004980238,0.00017062588,0.00026340442,0.00058137183],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012571773,0.0001954422,0.0007510639,0.00026762977,0.0009617693,0.00040554645,0.0004210524,0.00022806709,0.003128849],"category_scores_gemma":[0.0005007029,0.00022147596,0.0000750103,0.00072720373,0.005995313,0.000520915,0.000036135298,0.0004960336,0.0000023179748],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058014888,0.000033251046,0.9951352,0.00004304794,0.000052241227,0.00014092817,0.0016644321,0.00002560876,0.000015819962,0.000007124359,0.00026361,0.0025607424],"study_design_scores_gemma":[0.0007772125,0.0011533806,0.99151236,0.000089712405,0.000031959215,0.0036341108,0.001045884,0.0003374979,0.0000108372005,0.00025183248,0.0009605779,0.00019461314],"about_ca_topic_score_codex":0.89030963,"about_ca_topic_score_gemma":0.99981654,"teacher_disagreement_score":0.10950687,"about_ca_system_score_codex":0.000002505616,"about_ca_system_score_gemma":0.0006901592,"threshold_uncertainty_score":0.9977824},"labels":[],"label_agreement":null},{"id":"W2045982060","doi":"10.1139/e04-071","title":"The Holland Paleosol: an informal pedostratigraphic unit in the coastal dunes of southeastern Lake Michigan","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Paleosol; Geology; Podzol; Entisol; Radiocarbon dating; Shore; Period (music); Physical geography; Soil water; Geomorphology; Loess; Paleontology; Soil science; Oceanography; Geography","score_opus":0.027758981053699748,"score_gpt":0.23857518467716668,"score_spread":0.21081620362346692,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045982060","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99508625,0.00065571966,0.0000024304006,0.0014701504,0.00018922283,0.00007180141,0.000029226565,0.0000011161328,0.002494057],"genre_scores_gemma":[0.99972576,0.00004340106,0.00004898159,0.00011273132,0.000042640706,1.7561649e-7,0.0000038773933,7.153473e-7,0.000021698854],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99868196,0.0001964441,0.0003068879,0.00008776307,0.0002867099,0.00044023184],"domain_scores_gemma":[0.99915993,0.00023378634,0.00015434809,0.00011497558,0.00008076444,0.00025621988],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020316388,0.000082359664,0.00013593107,0.00026165438,0.0006408754,0.00012326287,0.0008026193,0.000057924095,0.00013145563],"category_scores_gemma":[0.00009526334,0.000041762956,0.00005005907,0.0005558324,0.0019486799,0.0003187131,0.000003510086,0.000312341,0.000011272052],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015963129,0.0000034258624,0.99610025,0.0000028504348,0.000004860695,0.000066075474,0.0020866792,0.0014523036,9.23027e-7,0.0002481216,6.9396286e-8,0.00001848061],"study_design_scores_gemma":[0.000241421,0.0005102272,0.99179095,0.00001925255,0.0000040846685,0.00050201383,0.0054148217,0.000089363544,0.00000939336,0.0009312467,0.00043494094,0.000052292242],"about_ca_topic_score_codex":0.005386598,"about_ca_topic_score_gemma":0.999593,"teacher_disagreement_score":0.9942064,"about_ca_system_score_codex":7.692582e-10,"about_ca_system_score_gemma":0.001284541,"threshold_uncertainty_score":0.81429607},"labels":[{"model":"gemma","categories":[],"domain":null,"study_design":"observational","genre":"empirical","about_ca_system":false,"about_ca_topic":true,"confidence":"low"},{"model":"gpt","categories":[],"domain":null,"study_design":"observational","genre":"empirical","about_ca_system":false,"about_ca_topic":false,"confidence":"low"}],"label_agreement":"agree"},{"id":"W2046042749","doi":"10.1139/e03-035","title":"Continental tholeiitic mafic rocks of the Paleoproterozoic Hurwitz Group, Central Hearne sub-domain, Nunavut: insight into the evolution of the Hearne sub-continental lithosphere","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Lockheed Martin (Canada); Carleton University; Government of Nunavut; Nunavut Research Institute","funders":"","keywords":"Geology; Geochemistry; Mafic; Continental crust; Basalt; Primitive mantle; Volcanic rock; Lithophile; Continental margin; Mantle (geology); Metamorphism; Partial melting; Petrology; Paleontology; Volcano; Tectonics","score_opus":0.006567753355979,"score_gpt":0.169205421219731,"score_spread":0.162637667863752,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046042749","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9910977,0.004751489,0.000029157249,0.0020498277,0.00049179787,0.00017825203,0.000025258569,0.000002491722,0.0013740173],"genre_scores_gemma":[0.9994795,0.00003502059,0.000113060974,0.00020768434,0.0000749489,5.698237e-7,0.0000021447524,0.0000020961056,0.000084986896],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99766475,0.000372553,0.0005760416,0.00022228937,0.00060933485,0.0005550414],"domain_scores_gemma":[0.99861753,0.00013474071,0.00047366644,0.00022178784,0.00018112911,0.00037114395],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009564841,0.0001748765,0.00032097957,0.00008472848,0.0006954727,0.000086019114,0.0008886996,0.000076125616,0.0011279244],"category_scores_gemma":[0.00037857526,0.0000769639,0.00030337158,0.0013946648,0.0018615614,0.0002212276,0.000021362448,0.00037409554,0.000007402862],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011962451,0.000014304764,0.99631476,0.000008955076,0.000021866468,0.000006120482,0.0006417306,0.0008953797,0.0013374964,0.00025700784,0.000043730513,0.00044667505],"study_design_scores_gemma":[0.00024938153,0.00020690939,0.98685557,0.00008322602,0.00004124113,0.00009938636,0.0019173428,0.0002785604,0.00455128,0.00447045,0.0011304421,0.000116233176],"about_ca_topic_score_codex":0.046585158,"about_ca_topic_score_gemma":0.6077411,"teacher_disagreement_score":0.561156,"about_ca_system_score_codex":0.000009926297,"about_ca_system_score_gemma":0.0007054408,"threshold_uncertainty_score":0.9997852},"labels":[],"label_agreement":null},{"id":"W2046150982","doi":"10.1139/cjes-2013-0144","title":"East-derived strata in the Methow basin record rapid mid-Cretaceous uplift of the southern Coast Mountains batholith","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Washington State University; National Science Foundation","keywords":"Geology; Cretaceous; Provenance; Batholith; Terrane; Paleontology; Pluton; Structural basin; Craton; Zircon; Geochemistry; Tectonics","score_opus":0.0237892399150953,"score_gpt":0.20200365599664669,"score_spread":0.1782144160815514,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046150982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99260914,0.00052426074,0.000035843485,0.004277267,0.0001683608,0.00006356017,0.000051987157,0.000001548352,0.0022680503],"genre_scores_gemma":[0.99861676,0.000014883799,0.0005612075,0.0006716051,0.00008152293,1.753868e-7,0.0000016536399,0.0000010814788,0.000051096646],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981841,0.00045075876,0.0003862259,0.00017097636,0.00040632102,0.00040164293],"domain_scores_gemma":[0.9988183,0.0003168744,0.00028491678,0.00018154454,0.000095542004,0.00030281747],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0023844265,0.00011995284,0.0002668716,0.00015050425,0.00030508445,0.00011389669,0.0011209177,0.00005136893,0.0021482809],"category_scores_gemma":[0.0005475329,0.00005416219,0.00016625471,0.00083536655,0.0008639023,0.00014052351,0.0000102626855,0.00027854886,0.000017383185],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009151135,0.000006676117,0.9861255,0.0000042512524,0.000010452606,0.000013565412,0.00094961404,0.0019260524,0.00017732274,0.000042661315,0.00004969163,0.0106850555],"study_design_scores_gemma":[0.00020244437,0.00033954546,0.97869873,0.00004379094,0.000035410416,0.000089708454,0.0054817316,0.0027448838,0.00042509584,0.00636761,0.00542657,0.0001444656],"about_ca_topic_score_codex":0.053923875,"about_ca_topic_score_gemma":0.7654448,"teacher_disagreement_score":0.7115209,"about_ca_system_score_codex":0.0000013460698,"about_ca_system_score_gemma":0.0004418538,"threshold_uncertainty_score":0.9987639},"labels":[],"label_agreement":null},{"id":"W2046349430","doi":"10.1139/e02-027","title":"The Nagssugtoqidian Orogen of West Greenland: tectonic evolution and regional correlations from a West Greenland perspective","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":164,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Craton; Supercontinent; Metamorphism; Foreland basin; Continental collision; Laurentia; Continental crust; Sinistral and dextral; Continental margin; Paleontology; Tectonics; Lithosphere; Geomorphology","score_opus":0.019962646324114902,"score_gpt":0.19053583886828052,"score_spread":0.1705731925441656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046349430","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9786825,0.012360654,0.000021762935,0.0047680116,0.00012243383,0.00004763136,0.000068241585,0.0000024435342,0.0039263],"genre_scores_gemma":[0.99923545,0.0002065504,0.00025529705,0.000083573046,0.000103722225,1.5880006e-7,0.000003313032,8.502928e-7,0.00011105885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99893534,0.00007658494,0.00026552638,0.00016301377,0.00027741562,0.00028211792],"domain_scores_gemma":[0.99873495,0.00036226667,0.00020874232,0.00008184969,0.00017538606,0.00043678077],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038631484,0.00009251377,0.0001713456,0.00015637424,0.0006598366,0.00008555693,0.0003086278,0.0000497929,0.004177686],"category_scores_gemma":[0.0002402978,0.00005300178,0.00008856381,0.0005347502,0.0010878352,0.00020854607,0.000005857591,0.00017263214,0.00004274631],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005733558,0.000003933367,0.9965595,8.270112e-7,0.000025892317,0.000012582409,0.00029079185,0.0005767946,0.000013533212,0.00054860784,0.00011345367,0.0018483418],"study_design_scores_gemma":[0.00013676935,0.00020291192,0.97335416,0.000019232815,0.00003392251,0.00007606824,0.00111032,0.005235905,0.000009449298,0.018399838,0.0013380802,0.00008332877],"about_ca_topic_score_codex":0.16447805,"about_ca_topic_score_gemma":0.79890835,"teacher_disagreement_score":0.63443035,"about_ca_system_score_codex":0.000003787266,"about_ca_system_score_gemma":0.00023710856,"threshold_uncertainty_score":0.99673265},"labels":[],"label_agreement":null},{"id":"W2046462679","doi":"10.1139/e02-034","title":"Products of 2.652.58 Ga orogenesis in the Slave Province correlated with Slave Northern Cordillera Lithospheric Evolution (SNORCLE) seismic reflection patterns","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Lithosphere; Crust; Seismology; Tectonics; Proterozoic; Fibrous joint; Subduction; Paleontology","score_opus":0.016149745083495724,"score_gpt":0.1775533096026521,"score_spread":0.16140356451915636,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046462679","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957005,0.0012981448,0.00004750942,0.0013271307,0.00010923791,0.00012959568,0.000013034159,0.0000037200641,0.0013711349],"genre_scores_gemma":[0.9994485,0.000039817307,0.00018109831,0.0001387641,0.00005901023,5.0025807e-7,0.0000035417506,0.0000016514846,0.00012713413],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984191,0.00016723816,0.00037057415,0.0002326988,0.00042807285,0.00038231484],"domain_scores_gemma":[0.9990224,0.00009958926,0.00031968206,0.0001272274,0.00020836116,0.00022273342],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006140975,0.0001348902,0.0002469866,0.00017695333,0.0002533534,0.00006834214,0.00041584502,0.000056204364,0.001816123],"category_scores_gemma":[0.00014858998,0.00007127439,0.00006968652,0.001546588,0.0004016012,0.00026453682,0.0000038620537,0.00022324418,0.000024343304],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018427372,0.000014209025,0.9806822,0.000009030019,0.000015347261,0.000058413196,0.00033950416,0.014265394,0.000050108407,0.0000036584652,0.000021578464,0.00452215],"study_design_scores_gemma":[0.00021539138,0.001251731,0.9802555,0.00006957309,0.000046365545,0.00019777151,0.00063398725,0.016324513,0.00037590676,0.00021815694,0.00026708917,0.00014400524],"about_ca_topic_score_codex":0.06091715,"about_ca_topic_score_gemma":0.66868573,"teacher_disagreement_score":0.6077686,"about_ca_system_score_codex":0.000006978583,"about_ca_system_score_gemma":0.00037906214,"threshold_uncertainty_score":0.99909633},"labels":[],"label_agreement":null},{"id":"W2046690731","doi":"10.1139/e05-044","title":"Reexamination of a primitive ornithomimosaur, <i>Garudimimus brevipes</i> Barsbold, 1981 (Dinosauria: Theropoda), from the Late Cretaceous of Mongolia","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Southern Methodist University","keywords":"Holotype; Theropoda; Geology; Anatomy; Paleontology; Cretaceous; Phalanx; Biology; Genus; Zoology","score_opus":0.016798494036387945,"score_gpt":0.2070427126784977,"score_spread":0.19024421864210975,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046690731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9815674,0.010070678,0.00003336751,0.0020331438,0.00040849112,0.00009253989,0.00020452615,0.0000025987442,0.005587292],"genre_scores_gemma":[0.9983407,0.00024154145,0.0007886099,0.00034050585,0.00017606354,1.9507175e-7,0.0000093534345,0.0000014866961,0.00010152594],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99852705,0.00028294255,0.0004718238,0.0001462703,0.00024496744,0.0003269682],"domain_scores_gemma":[0.99841344,0.0005188385,0.0005123216,0.00013143044,0.0001905511,0.00023342772],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010833319,0.00011759295,0.0002854673,0.00016787667,0.00029697912,0.000021246788,0.00060328,0.000105702304,0.0009627587],"category_scores_gemma":[0.00027737094,0.00007406803,0.00009942735,0.00037188426,0.0014517908,0.00033579842,0.0000059310605,0.00021181503,0.000023422024],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004117061,0.000008795998,0.9818126,0.000003809087,0.000043476037,0.00002004334,0.0008545367,0.0034599386,0.00027990196,0.0001587155,0.00041300233,0.012904],"study_design_scores_gemma":[0.00022511628,0.00033865482,0.9892849,0.000049587943,0.000033622404,0.0000959147,0.00044732876,0.0010020614,0.00036654418,0.0005003165,0.00756743,0.000088562985],"about_ca_topic_score_codex":0.010638064,"about_ca_topic_score_gemma":0.5025234,"teacher_disagreement_score":0.4918854,"about_ca_system_score_codex":0.0000031050517,"about_ca_system_score_gemma":0.0010290161,"threshold_uncertainty_score":0.99995047},"labels":[],"label_agreement":null},{"id":"W2046868420","doi":"10.1139/e05-114","title":"Morphological and systematic reinterpretation of two enigmatic edrioasteroids (Echinodermata) from Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Reinterpretation; Ordovician; Paleontology; Geology; Taxon; Trilobite; Philosophy","score_opus":0.011338420411317515,"score_gpt":0.19918616373186926,"score_spread":0.18784774332055174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046868420","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98293257,0.010512846,0.00010287437,0.00016382542,0.00029886805,0.000065996894,0.000054209537,0.0000015847389,0.005867201],"genre_scores_gemma":[0.9986295,0.0000066357125,0.0012621131,0.000057114634,0.00003580208,1.1087024e-7,0.0000016799258,3.5623543e-7,0.0000066807906],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988283,0.00013869481,0.0004618364,0.00011045545,0.00024497815,0.00021572241],"domain_scores_gemma":[0.9989847,0.00032545347,0.0003266517,0.00006883427,0.000054845892,0.00023951051],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043494292,0.00008757827,0.0002917812,0.00016030393,0.00019169957,0.00006673334,0.00025530058,0.000036772613,0.00013430818],"category_scores_gemma":[0.000110502304,0.00006152944,0.000042510812,0.00016935068,0.00046961693,0.00025846672,7.064197e-7,0.00010599607,9.0683466e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000042504466,0.0000018002303,0.9979649,0.000099470875,0.000013969676,0.0001419654,0.00018323233,0.00054688135,0.000063707645,0.00017703205,0.000049949977,0.0007527968],"study_design_scores_gemma":[0.00014486068,0.00011511013,0.993516,0.00036922412,0.000023976101,0.00027307286,0.00030456154,0.0024494273,0.000105827705,0.0026197059,0.0000051404163,0.00007307109],"about_ca_topic_score_codex":0.8839634,"about_ca_topic_score_gemma":0.9972731,"teacher_disagreement_score":0.11330965,"about_ca_system_score_codex":0.0000012462444,"about_ca_system_score_gemma":0.0010529264,"threshold_uncertainty_score":0.25090978},"labels":[],"label_agreement":null},{"id":"W2047186653","doi":"10.1139/cjes-2013-0130","title":"Fonctionnement hydrogéologique du bassin de la Bahira (Maroc central) : apport de l’analyse des données géologiques et gravimétriques","year":2014,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies Worldwide","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geomorphology; Humanities","score_opus":0.025880883319732637,"score_gpt":0.2169145466738416,"score_spread":0.19103366335410898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047186653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95050085,0.008490188,0.0028618027,0.019642612,0.0008498454,0.00011839785,0.000036794314,0.00001962454,0.017479882],"genre_scores_gemma":[0.98119986,0.0031617228,0.01164964,0.002482345,0.00061609404,0.0000014036434,0.000004041085,0.000004389103,0.0008805103],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99510133,0.0021281869,0.000604948,0.00035688185,0.00036547618,0.001443148],"domain_scores_gemma":[0.9963001,0.0013054843,0.00039583028,0.00012863062,0.00019690144,0.0016730765],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.006524914,0.000306562,0.00050827715,0.00028285058,0.0011840601,0.00046601667,0.0007390025,0.00022530255,0.0017991004],"category_scores_gemma":[0.0017647803,0.00021995082,0.00029073976,0.00074257836,0.0044040987,0.00053816824,0.000029806593,0.0006355151,0.000045837947],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015929365,0.00004842824,0.9452599,0.000029968847,0.000059201488,0.00023719936,0.00084252,0.0073106764,0.000019879883,0.0030012196,0.0017842,0.041390833],"study_design_scores_gemma":[0.00020309024,0.0013786342,0.8207597,0.00014900193,0.00007532536,0.0003511551,0.0010029401,0.0022528893,0.00015853415,0.04648279,0.12692346,0.00026247744],"about_ca_topic_score_codex":0.11937466,"about_ca_topic_score_gemma":0.66386575,"teacher_disagreement_score":0.5444911,"about_ca_system_score_codex":0.000035461486,"about_ca_system_score_gemma":0.0025961744,"threshold_uncertainty_score":0.9991134},"labels":[],"label_agreement":null},{"id":"W2047392153","doi":"10.1139/e99-093","title":"Geochronology and radiogenic isotope geochemistry of plutonic rocks from the central Abitibi subprovince: significance to the internal subdivision and plutono-tectonic evolution of the Abitibi belt","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; Ministère des Ressources naturelles et des Forêts (Québec); Geological Survey of Canada","funders":"","keywords":"Pluton; Geology; Geochemistry; Crust; Volcanic rock; Tectonics; Volcano; Seismology","score_opus":0.0055990648218884765,"score_gpt":0.17068463514071416,"score_spread":0.16508557031882568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047392153","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893206,0.007051872,0.000025880543,0.0028889847,0.00011768376,0.00009959068,0.000105707804,0.0000016263024,0.0003880575],"genre_scores_gemma":[0.9993565,0.00017688701,0.00007016415,0.00023142624,0.00009303861,2.9955365e-7,0.000002471891,0.0000011462928,0.0000680477],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985986,0.0001183759,0.00038065587,0.00022591415,0.00028583565,0.00039061345],"domain_scores_gemma":[0.99895185,0.00026181704,0.00022976827,0.00017034788,0.00008121439,0.00030498637],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005412792,0.00012180705,0.00023641082,0.00005418345,0.0003990943,0.00006106775,0.00075881084,0.000064152766,0.0027534196],"category_scores_gemma":[0.00017156833,0.000056343586,0.00011093307,0.0004250352,0.0014090282,0.00012329331,0.000023650033,0.00024811924,0.0000040392565],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026786454,0.0000052007235,0.9824099,0.00000518063,0.000026228003,0.0000045215106,0.00030591752,0.0028846362,0.0013358464,0.000024266747,0.00008869319,0.012882822],"study_design_scores_gemma":[0.00013523675,0.00019302197,0.99210125,0.000054170214,0.00003748202,0.00006184484,0.0002780386,0.0027604797,0.0017110158,0.0017628043,0.0008241293,0.0000805375],"about_ca_topic_score_codex":0.19429913,"about_ca_topic_score_gemma":0.5162115,"teacher_disagreement_score":0.32191235,"about_ca_system_score_codex":0.0000071180602,"about_ca_system_score_gemma":0.0006548421,"threshold_uncertainty_score":0.9981582},"labels":[],"label_agreement":null},{"id":"W2047693254","doi":"10.1139/e06-079","title":"A reappraisal of the allochthonous nature of the Rosenberg slice and Stanbridge Group of southern Quebec and northwestern Vermont","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Anticline; Nappe; Foreland basin; Paleontology; Group (periodic table); Conformable matrix; Paleozoic; Ordovician; Sequence (biology); Thrust fault; Geomorphology; Tectonics","score_opus":0.008920587833865576,"score_gpt":0.2071993937155665,"score_spread":0.19827880588170094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047693254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98838955,0.008187602,0.00000568154,0.00021369282,0.00027016347,0.000061482235,0.00009970953,6.863858e-7,0.0027714039],"genre_scores_gemma":[0.9997349,0.000024543415,0.00014977138,0.000042859658,0.000028371072,2.7433037e-8,1.9403447e-7,5.235808e-7,0.000018808334],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990004,0.00008251398,0.00032267132,0.00010627308,0.00026695026,0.00022119825],"domain_scores_gemma":[0.9990068,0.00018907084,0.00041168366,0.000110064495,0.00007808189,0.00020427081],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010383996,0.00008289191,0.00018960983,0.00011559595,0.000226594,0.000023812689,0.00039734956,0.00008644887,0.000016518537],"category_scores_gemma":[0.00007795798,0.000044235825,0.00007661163,0.00030717478,0.0018415048,0.00014780433,0.0000029638124,0.00022799966,1.0049888e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018219373,0.000003163131,0.9895848,0.000010137738,0.000014776017,0.000008425981,0.0016606235,0.000022724866,0.00020466578,0.00016683854,0.00000604495,0.008299586],"study_design_scores_gemma":[0.00013641248,0.00016585572,0.99729997,0.000061349514,0.000016992675,0.00012359592,0.0014877594,0.00003063168,0.00028757972,0.000104043036,0.00023485643,0.000050974122],"about_ca_topic_score_codex":0.13381036,"about_ca_topic_score_gemma":0.9799778,"teacher_disagreement_score":0.84616745,"about_ca_system_score_codex":4.6812875e-7,"about_ca_system_score_gemma":0.0005817525,"threshold_uncertainty_score":0.87195766},"labels":[],"label_agreement":null},{"id":"W2047750474","doi":"10.1139/e03-045","title":"Post-Paleocene cooling in the southern Canadian Atlantic region: evidence from apatite fission track models","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Fission track dating; Cretaceous; Paleontology; Carboniferous; Thermochronology; Nova scotia; Passive margin; Basement; Structural basin; Zircon; Rift; Oceanography","score_opus":0.04004909500012224,"score_gpt":0.22330182907378068,"score_spread":0.18325273407365844,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047750474","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99442863,0.0020721375,0.0006723768,0.0015369412,0.00020607712,0.000053789125,0.0000062657778,0.000004668208,0.0010191121],"genre_scores_gemma":[0.9992883,0.00012356302,0.00020648347,0.00027483073,0.000060657774,7.246108e-7,0.0000011167963,0.0000057662837,0.00003856106],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989142,0.00010885899,0.00028682002,0.00010662911,0.0002574399,0.00032606005],"domain_scores_gemma":[0.99910843,0.00008710815,0.00006314264,0.00012558585,0.00008750292,0.0005281991],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00071645115,0.000095738316,0.00014722836,0.00049098657,0.00022488559,0.00018378746,0.00039826022,0.000052369123,0.00010725781],"category_scores_gemma":[0.00019738273,0.00006516035,0.00006877066,0.00072203623,0.000103621096,0.00046884522,0.0000015813148,0.00021375495,0.00001480194],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000023029056,0.0000029389423,0.08093216,0.000006881511,0.000017874767,0.00025300463,0.010176145,0.9078685,0.00012282132,0.000094983065,0.0002319452,0.000290422],"study_design_scores_gemma":[0.0005957325,0.00021802582,0.048180666,0.0013837902,0.00009615142,0.00030736468,0.025202477,0.9108113,0.0005809002,0.0027536603,0.0090515185,0.00081838045],"about_ca_topic_score_codex":0.2631698,"about_ca_topic_score_gemma":0.9743054,"teacher_disagreement_score":0.7111356,"about_ca_system_score_codex":0.00002103819,"about_ca_system_score_gemma":0.0011928442,"threshold_uncertainty_score":0.7417368},"labels":[],"label_agreement":null},{"id":"W2048062726","doi":"10.1139/e08-034","title":"Shock brecciation around the Kidd Creek deposit, Abitibi belt, Canada","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Breccia; Geology; Geochemistry; Felsic; Volcanic rock; Basalt; Clastic rock; Mafic; Petrology; Volcano; Sedimentary rock","score_opus":0.016425018402298854,"score_gpt":0.17201018187169453,"score_spread":0.1555851634693957,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048062726","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98845357,0.0012934087,0.000015177516,0.0029544742,0.00030301718,0.00003535886,0.0000215082,0.0000023135133,0.0069211866],"genre_scores_gemma":[0.99780494,0.000041209783,0.00020056617,0.0014553862,0.00019979305,9.420835e-8,0.000005360264,7.904365e-7,0.0002918334],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986412,0.00006795928,0.00028982878,0.00014295967,0.00045085177,0.00040721433],"domain_scores_gemma":[0.99882483,0.00018120391,0.00016571225,0.000085078354,0.00012743898,0.00061572227],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041252654,0.000091282585,0.0001636106,0.00008323989,0.0010768065,0.0001234521,0.0005256007,0.000033800345,0.0028393562],"category_scores_gemma":[0.00020147297,0.000054126667,0.000086133005,0.00059878716,0.0005026877,0.00022848016,0.0000043552855,0.0001885778,0.000018967703],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000019442184,0.0000016458079,0.9937178,9.740335e-7,0.000010524797,0.00012248942,0.00005344438,0.0031975966,0.00000869945,0.0000115666,0.0013851867,0.001488141],"study_design_scores_gemma":[0.00006318506,0.00010596076,0.9906439,0.000008123033,0.000014221319,0.00040479,0.00019944619,0.0014806109,0.000054769047,0.0011067695,0.0058243633,0.00009381777],"about_ca_topic_score_codex":0.98677063,"about_ca_topic_score_gemma":0.9998281,"teacher_disagreement_score":0.013057472,"about_ca_system_score_codex":0.0000042029783,"about_ca_system_score_gemma":0.0021689709,"threshold_uncertainty_score":0.9980722},"labels":[],"label_agreement":null},{"id":"W2048097867","doi":"10.1139/cjes-2013-0022","title":"Evolution of the Late Ordovician plaesiomyid brachiopod lineage in Laurentia","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Ordovician; Paleontology; Laurentia; Geology; Lineage (genetic); Biology","score_opus":0.011951067985460731,"score_gpt":0.19757755285776857,"score_spread":0.18562648487230785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048097867","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9747267,0.0035689285,0.000008058895,0.00046469882,0.0003934637,0.00007273155,0.000012642684,0.0000012764962,0.020751493],"genre_scores_gemma":[0.99960226,0.000009091854,0.00026877143,0.00004074371,0.000035550398,1.0964488e-7,2.5250682e-7,3.2876525e-7,0.00004289368],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990237,0.000107587126,0.00031073528,0.000083147905,0.00018471768,0.00029014054],"domain_scores_gemma":[0.9993274,0.00006915477,0.00022357982,0.00008443478,0.00006232986,0.00023308651],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00057717576,0.00007176782,0.00014271222,0.0003181426,0.00026486794,0.000055513774,0.00049915625,0.000057484685,0.0006582261],"category_scores_gemma":[0.00008778357,0.000043903034,0.000078587545,0.00063207326,0.00067272387,0.0004531477,9.3164545e-7,0.0001958345,0.00001013464],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000018304169,0.00000288679,0.99509597,0.0000021587048,0.000003606638,0.0000060355046,0.00016417222,0.0009433361,0.000044807668,0.00015008033,0.00003783014,0.0035472852],"study_design_scores_gemma":[0.00010558165,0.00010995826,0.99700856,0.000044307115,0.0000038434687,0.00002999715,0.00030373276,0.0010400815,0.00007545152,0.0010944863,0.00012985972,0.000054110948],"about_ca_topic_score_codex":0.08408075,"about_ca_topic_score_gemma":0.8929717,"teacher_disagreement_score":0.80889094,"about_ca_system_score_codex":0.0000011798373,"about_ca_system_score_gemma":0.0009970352,"threshold_uncertainty_score":0.9220184},"labels":[],"label_agreement":null},{"id":"W2048201145","doi":"10.1139/e01-002","title":"Historical rates of salt marsh accretion on the outer Bay of Fundy","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Coastal wetland ecosystem dynamics","field":"Environmental Science","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Louisiana State University","keywords":"Marsh; Salt marsh; Bay; Geology; Accretion (finance); Oceanography; Sea level; Sediment; Physical geography; Hydrology (agriculture); Geomorphology; Wetland; Geography; Ecology","score_opus":0.02229673736574416,"score_gpt":0.2168160528175271,"score_spread":0.19451931545178294,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048201145","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99136543,0.00006678796,0.00008981163,0.0014048768,0.00034886575,0.00005275566,0.000004069529,8.994533e-7,0.006666488],"genre_scores_gemma":[0.99920154,0.000016055956,0.0001482396,0.00007860584,0.000036803034,3.0929178e-7,1.4576426e-7,0.00000263698,0.0005156383],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999006,0.000055855016,0.00030677152,0.00009306923,0.00033200046,0.00020635987],"domain_scores_gemma":[0.99928844,0.00009883149,0.00026804267,0.000105222854,0.000025453957,0.0002139969],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00090664806,0.00006403466,0.00014125399,0.00011024491,0.00013256162,0.000026249994,0.0003931943,0.000028575101,0.0012245482],"category_scores_gemma":[0.00011904506,0.000039454233,0.000067307046,0.00037100248,0.0002947708,0.00017797852,0.000020745047,0.00009194259,0.000020707159],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010087907,0.0000109758375,0.99508667,0.0000034266768,0.0000042076313,0.000019090132,0.00023901193,0.0016971632,0.00050144724,0.00023139497,0.00089586014,0.0013006573],"study_design_scores_gemma":[0.00017475942,0.0007030612,0.9615238,0.000095395786,0.0000118077705,0.00015149523,0.00036831034,0.0019204059,0.0005191224,0.00083166454,0.03357185,0.00012835386],"about_ca_topic_score_codex":0.0064530578,"about_ca_topic_score_gemma":0.1951005,"teacher_disagreement_score":0.18864743,"about_ca_system_score_codex":0.00006178363,"about_ca_system_score_gemma":0.00015980662,"threshold_uncertainty_score":0.99968845},"labels":[],"label_agreement":null},{"id":"W2048226928","doi":"10.1139/e98-106","title":"Heat flow and deep thermal structure near the southeastern edge of the Canadian Shield","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":91,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Archean; Geology; Crust; Craton; Shield; Heat flow; Tectonics; High heat; Flow (mathematics); Terrane; Petrology; Geochemistry; Seismology; Thermal; Geography; Geometry; Meteorology","score_opus":0.009198975578967242,"score_gpt":0.16455175101499664,"score_spread":0.1553527754360294,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048226928","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9888545,0.0013658962,4.684602e-7,0.0049759224,0.0001469273,0.000042161337,0.000053031996,8.880463e-7,0.0045601935],"genre_scores_gemma":[0.9987948,0.000009358375,0.00012399258,0.0008803771,0.000083417326,4.1712134e-8,0.0000010374068,7.964153e-7,0.000106203275],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990047,0.00007928422,0.00020236913,0.00011573229,0.00024485105,0.0003530512],"domain_scores_gemma":[0.99913716,0.00007236233,0.00004661569,0.000107223204,0.000051127183,0.0005855203],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035326576,0.00008960631,0.00014518356,0.000064084525,0.0010134832,0.00021298704,0.0005866557,0.00005332097,0.018001197],"category_scores_gemma":[0.000059886992,0.00003850578,0.00008830431,0.00041954557,0.0015202293,0.00011847216,0.000004446544,0.00021998666,0.000015184885],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003687109,8.301308e-7,0.9726606,0.0000017243345,0.000011314544,0.000009213916,0.000677042,0.011596891,0.000016455673,0.000014232041,0.000019941303,0.014988095],"study_design_scores_gemma":[0.00007073298,0.000091266054,0.97996855,0.000015209652,0.000022899845,0.000085504886,0.00031578005,0.012565738,0.000081678845,0.0016652087,0.005036299,0.00008112127],"about_ca_topic_score_codex":0.58500963,"about_ca_topic_score_gemma":0.9954325,"teacher_disagreement_score":0.4104229,"about_ca_system_score_codex":9.449586e-7,"about_ca_system_score_gemma":0.00091060123,"threshold_uncertainty_score":0.9828965},"labels":[],"label_agreement":null},{"id":"W2048246159","doi":"10.1139/e05-002","title":"Geophysical transect across a Paleoproterozoic continentcontinent collision zone: The Trans-Hudson Orogen","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; Geological Survey of Canada","funders":"","keywords":"Geology; Lithosphere; Bouguer anomaly; Craton; Mantle (geology); Collision zone; Geophysics; Seismology; Archean; Gravity anomaly; Crust; Magnetotellurics; Tectonics; Geochemistry; Paleontology; Electrical resistivity and conductivity","score_opus":0.01403909613216625,"score_gpt":0.22253763056999462,"score_spread":0.20849853443782837,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048246159","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99393815,0.0008395295,0.00014947087,0.0034049626,0.0007789496,0.00019278213,0.00014318604,0.0000058844666,0.0005470817],"genre_scores_gemma":[0.9982902,0.000043522923,0.00040963563,0.00034431988,0.00071895606,7.7496145e-7,0.0000044338026,0.0000033297626,0.00018482223],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981505,0.00012789159,0.00042859875,0.00020524574,0.00045350916,0.00063425436],"domain_scores_gemma":[0.99886644,0.00011063436,0.00021208418,0.00014341829,0.0001430091,0.0005244047],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012576025,0.00016274762,0.0002896996,0.00008565269,0.0007639426,0.00043389565,0.00070335163,0.000057014313,0.0010253732],"category_scores_gemma":[0.00004376419,0.000095920084,0.00014404867,0.00043634092,0.0005157243,0.00048330228,0.0000038008689,0.00017945333,0.000077459335],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003609559,0.00017242429,0.68451977,0.000121799094,0.00039469518,0.0005571171,0.03627098,0.066545375,0.017224755,0.0018363588,0.005826407,0.18616936],"study_design_scores_gemma":[0.00080720324,0.00061696634,0.75819343,0.000095188094,0.000050121547,0.00016224253,0.0006811273,0.0015180457,0.005287683,0.00022883821,0.23201732,0.00034183727],"about_ca_topic_score_codex":0.021362582,"about_ca_topic_score_gemma":0.42430478,"teacher_disagreement_score":0.4029422,"about_ca_system_score_codex":0.0000016081704,"about_ca_system_score_gemma":0.00065852865,"threshold_uncertainty_score":0.9998878},"labels":[],"label_agreement":null},{"id":"W2048262603","doi":"10.1139/e06-035","title":"UPb ages constraining structural development of an Archean terrane boundary in the Lake of the Woods area, western Superior Province, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Toronto","funders":"","keywords":"Terrane; Geology; Archean; Geochemistry; Zircon; Gneiss; Geochronology; Greenstone belt; Basement; Continental crust; Crust; Paleontology; Tectonics; Metamorphic rock; Archaeology","score_opus":0.017482798933122674,"score_gpt":0.19284352715398018,"score_spread":0.1753607282208575,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048262603","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99760145,0.0002617137,0.0000012572629,0.00075054594,0.00009411659,0.000052379088,0.000049388567,6.4210496e-7,0.0011885023],"genre_scores_gemma":[0.99916697,8.239063e-7,0.000596824,0.00016288685,0.0000317903,1.0677135e-7,0.0000066268544,5.768065e-7,0.000033396536],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99865997,0.00009485836,0.00042327426,0.000112543654,0.00040868044,0.00030067813],"domain_scores_gemma":[0.999386,0.000099130484,0.00020501121,0.00008226225,0.00005884517,0.00016871744],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000689785,0.000088659595,0.00019692107,0.00009909491,0.00028574516,0.000060949904,0.000661598,0.00002607742,0.0007064185],"category_scores_gemma":[0.000057986297,0.00004202159,0.00005293798,0.0004080837,0.0010040059,0.0001452075,0.0000064630003,0.00016189073,2.7412014e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000032028086,0.0000025996005,0.99342483,0.0000048728475,0.0000047812277,0.0000259474,0.00042678977,0.0016750314,0.000052078783,0.000008114362,0.000010479588,0.004361251],"study_design_scores_gemma":[0.000085118496,0.00007455649,0.9962054,0.000033188608,0.000006905878,0.00006720775,0.0010685669,0.00029532053,0.00038952366,0.00051090424,0.0011977013,0.00006559579],"about_ca_topic_score_codex":0.658616,"about_ca_topic_score_gemma":0.9997216,"teacher_disagreement_score":0.3411056,"about_ca_system_score_codex":0.0000025112572,"about_ca_system_score_gemma":0.0038311908,"threshold_uncertainty_score":0.7734787},"labels":[],"label_agreement":null},{"id":"W2048355295","doi":"10.1139/e04-023","title":"Slow post-orogenic cooling in a deeply eroded orogen: Reindeer Zone, Trans-Hudson Orogen, Saskatchewan","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Dalhousie University","funders":"","keywords":"Geology; Hornblende; Metamorphism; Transect; Closure temperature; Shear zone; Muscovite; Titanite; Thermochronology; Archean; Geochemistry; Migmatite; Geomorphology; Tectonics; Paleontology; Gneiss; Metamorphic rock; Zircon; Biotite; Oceanography","score_opus":0.013092775336311775,"score_gpt":0.19069010413665025,"score_spread":0.17759732880033846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048355295","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935357,0.0027885549,0.000121627476,0.0024088956,0.00020811537,0.000084115905,0.000033407363,0.0000073883166,0.0008122257],"genre_scores_gemma":[0.99608654,0.000039139977,0.0026823755,0.0010103153,0.00010621861,3.2956694e-7,0.000009295962,0.000002707385,0.00006308426],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976879,0.00008929026,0.000589271,0.0003297364,0.00048525172,0.0008185659],"domain_scores_gemma":[0.9982917,0.00009600733,0.00019509206,0.00013040996,0.00018938583,0.0010974115],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010621995,0.00020141527,0.00038681936,0.00047192973,0.00034459855,0.00015605215,0.00067576417,0.00011435188,0.0042154687],"category_scores_gemma":[0.00018556965,0.00014458214,0.00023764055,0.0014092745,0.00054160866,0.00042715485,0.0000057030443,0.0003654048,0.000090499816],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006111542,0.000028237997,0.92303073,0.00001200695,0.000052669373,0.0007612262,0.0019354656,0.064772636,0.0014285895,0.00010078255,0.000017824366,0.007798701],"study_design_scores_gemma":[0.0013098025,0.0011212054,0.97218865,0.00014243899,0.000087999484,0.00073216954,0.0053257016,0.0014810734,0.005256932,0.0096258065,0.0020840135,0.0006441806],"about_ca_topic_score_codex":0.120232426,"about_ca_topic_score_gemma":0.94395113,"teacher_disagreement_score":0.8237187,"about_ca_system_score_codex":0.000007509831,"about_ca_system_score_gemma":0.002127686,"threshold_uncertainty_score":0.9966948},"labels":[],"label_agreement":null},{"id":"W2048472769","doi":"10.1139/e03-066","title":"Microstructure of high-temperature (&gt;73 °C) siliceous sinter deposited around hot springs and geysers, Yellowstone National Park: the role of biological and abiological processes in sedimentation","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Subaerial; Geology; Splash; Dissolved silica; Mineralogy; Deposition (geology); Porosity; Geochemistry; Geomorphology; Sediment; Chemical engineering; Dissolution; Geotechnical engineering","score_opus":0.01406090776919221,"score_gpt":0.22603113817671794,"score_spread":0.21197023040752572,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048472769","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942269,0.0050804904,4.3788546e-7,0.0003151145,0.0000625231,0.00006884463,0.00001822566,6.079974e-7,0.00022686896],"genre_scores_gemma":[0.9994377,0.00012170739,0.0003170083,0.00009790327,0.000013724716,1.8812209e-7,0.000004048437,5.492643e-7,0.000007187319],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991283,0.00016350565,0.00023031892,0.00013111476,0.0001388795,0.00020788664],"domain_scores_gemma":[0.9992726,0.00028898116,0.00013722849,0.00003198316,0.00013899448,0.00013023811],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00074945576,0.0000733957,0.00016737662,0.00017607985,0.00017753048,0.000029843999,0.00015654406,0.00010722626,0.00017121958],"category_scores_gemma":[0.00033896093,0.000041426283,0.00001853651,0.00032927628,0.0019708592,0.00012653622,0.0000041774215,0.0001920675,7.633584e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028988106,0.0000038171065,0.99742955,0.000007796164,0.000007940422,0.000014532191,0.00034653491,0.00022790405,0.0017033623,0.00015660217,0.0000028414624,0.00007013412],"study_design_scores_gemma":[0.00017314432,0.0002971388,0.9931797,0.000021376674,0.000004391732,0.00055356824,0.0009307357,0.00005796256,0.0029485521,0.0016865307,0.00009710471,0.000049801896],"about_ca_topic_score_codex":0.0011054405,"about_ca_topic_score_gemma":0.098403424,"teacher_disagreement_score":0.09729798,"about_ca_system_score_codex":5.5757715e-7,"about_ca_system_score_gemma":0.00046824315,"threshold_uncertainty_score":0.9180484},"labels":[],"label_agreement":null},{"id":"W2048946274","doi":"10.1139/e08-067","title":"A hybrid method applied to a 2.5D scalar wave equation","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Finite difference; Scalar (mathematics); Computation; Wave equation; Seismogram; Cartesian coordinate system; Finite difference method; Seismic wave; Computational complexity theory; Acoustic wave equation; Computer science; Amplitude; Applied mathematics; Algorithm; Mathematics; Mathematical analysis; Geology; Acoustic wave; Geometry; Geophysics; Acoustics; Physics; Seismology","score_opus":0.05408956540121077,"score_gpt":0.23512457975051204,"score_spread":0.18103501434930128,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048946274","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9268175,0.00041043566,0.033673167,0.003489972,0.00084470544,0.00018494522,0.000030181523,0.000028835779,0.034520295],"genre_scores_gemma":[0.9365696,0.000014530493,0.059729967,0.003401001,0.000112902,1.9436062e-7,0.0000019176225,0.0000016913327,0.00016822715],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9988466,0.000059543865,0.00024778693,0.00015785405,0.00034260983,0.0003455953],"domain_scores_gemma":[0.99891555,0.00008805907,0.00012542296,0.000087783956,0.00009867699,0.000684506],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001218889,0.000088609006,0.00015712788,0.00054141367,0.00051802036,0.00008782608,0.00031902475,0.000025274365,0.0011352943],"category_scores_gemma":[0.0001514139,0.000069299684,0.00005807397,0.00044187673,0.00026174716,0.000302042,0.0000036150889,0.00013448433,0.00012843336],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000071284536,0.000022575383,0.38965312,0.000020111302,0.000051329636,0.0011886432,0.0052120164,0.017862363,0.0007556654,0.001453672,0.08979974,0.49390948],"study_design_scores_gemma":[0.0007776582,0.0018760675,0.4817501,0.0001847295,0.000042505042,0.005474768,0.0015735833,0.08801567,0.028464813,0.011570422,0.37929025,0.0009794501],"about_ca_topic_score_codex":0.0198738,"about_ca_topic_score_gemma":0.0050884546,"teacher_disagreement_score":0.49293002,"about_ca_system_score_codex":0.0000029567811,"about_ca_system_score_gemma":0.0011211665,"threshold_uncertainty_score":0.9997778},"labels":[],"label_agreement":null},{"id":"W2048990277","doi":"10.1139/e00-015","title":"Nd isotopic characteristics of terranes within the Avalon Zone, southern New Brunswick","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Mount Saint Vincent University; Acadia University","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Terrane; Geology; Geochemistry; Igneous rock; Sedimentary rock; Paleontology; Tectonics","score_opus":0.015316506049208763,"score_gpt":0.18350376001764304,"score_spread":0.16818725396843429,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048990277","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99402386,0.00086221244,0.000012060356,0.0017877648,0.00015153378,0.000034900964,0.000016632697,0.0000020867114,0.0031089578],"genre_scores_gemma":[0.997145,0.000025138275,0.00042538528,0.00040636395,0.00016358885,2.4042054e-8,0.0000023833059,8.466057e-7,0.001831282],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99890786,0.000057895275,0.00037565487,0.000118468364,0.00027165192,0.00026847265],"domain_scores_gemma":[0.99907625,0.000090016445,0.00021658762,0.00009462591,0.000062659026,0.00045985618],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005142966,0.00009193927,0.00021241409,0.00009648734,0.00024531677,0.00008289643,0.00053710956,0.00004093568,0.02448526],"category_scores_gemma":[0.00009082472,0.00004758906,0.00010792003,0.00042372107,0.0006093767,0.00012703732,0.0000025227625,0.00015733358,0.00014100887],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008666294,0.0000032376931,0.976204,0.0000031899287,0.000013527859,0.00002016635,0.00055824465,0.001138311,0.000023444962,0.000042847143,0.00009450631,0.0218899],"study_design_scores_gemma":[0.000107632055,0.0002453099,0.98948544,0.000030081106,0.000030893825,0.00009963919,0.00041237375,0.0011309604,0.00013065782,0.00311822,0.005102788,0.00010602747],"about_ca_topic_score_codex":0.17797801,"about_ca_topic_score_gemma":0.67334515,"teacher_disagreement_score":0.49536717,"about_ca_system_score_codex":5.612071e-7,"about_ca_system_score_gemma":0.0010326839,"threshold_uncertainty_score":0.9764065},"labels":[],"label_agreement":null},{"id":"W2049131643","doi":"10.1139/e05-074","title":"A Late Cretaceous (TuronianConiacian) high-latitude turtle assemblage from the Canadian Arctic","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Cretaceous; Assemblage (archaeology); Turtle (robot); Paleontology; Latitude; Geology; Arctic; Mesozoic; Faunal assemblage; Oceanography; Fauna; Structural basin; Ecology; Biology","score_opus":0.016287702421019554,"score_gpt":0.20670566582434685,"score_spread":0.19041796340332728,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049131643","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9688602,0.0076567386,0.000016067432,0.01602534,0.0011918918,0.000074489064,0.00012416879,0.0000048797874,0.0060462374],"genre_scores_gemma":[0.9952683,0.000050018698,0.0015447902,0.0024015447,0.0005368874,2.0021739e-7,0.000009827765,0.0000016901438,0.00018675657],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851286,0.00016408913,0.00028237683,0.00019234548,0.0002025287,0.0006458004],"domain_scores_gemma":[0.9984539,0.00026279184,0.00016576747,0.00013762928,0.00010283804,0.0008770781],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007878437,0.00012816676,0.00018872479,0.00020562221,0.0012535537,0.00015101617,0.0007322186,0.00012019197,0.0041997368],"category_scores_gemma":[0.00022346055,0.000083190425,0.00007192911,0.00031993343,0.0009497118,0.0004214688,0.0000034209363,0.00035043698,0.00043315586],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005824624,0.00000169401,0.9802437,7.759654e-7,0.000023526582,0.00013107619,0.00032275333,0.0137591455,0.000005559358,0.00020329996,0.00052606105,0.004776595],"study_design_scores_gemma":[0.00012186584,0.000121235375,0.9261445,0.000018051316,0.000015112159,0.00018561208,0.000078603516,0.0016238004,0.0000068997347,0.0013550778,0.070217624,0.00011166542],"about_ca_topic_score_codex":0.8077812,"about_ca_topic_score_gemma":0.99983364,"teacher_disagreement_score":0.1920524,"about_ca_system_score_codex":0.00001393708,"about_ca_system_score_gemma":0.004246822,"threshold_uncertainty_score":0.99671054},"labels":[],"label_agreement":null},{"id":"W2049376568","doi":"10.1139/e07-022","title":"Rifting of a Mississippian continental arc system: Little Salmon formation, Yukon–Tanana terrane, northern Canadian Cordillera","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon University; Saint Mary's University; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Terrane; Rift; Geochemistry; Continental crust; Basalt; Continental arc; Continental shelf; Island arc; Paleontology; Magmatism; Crust; Subduction; Structural basin; Oceanography; Tectonics","score_opus":0.014977889485412567,"score_gpt":0.19068672950802443,"score_spread":0.17570884002261186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049376568","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9681127,0.00096998486,0.00004255512,0.0008547998,0.00023952164,0.000069591275,0.00005687907,0.000004969106,0.029648967],"genre_scores_gemma":[0.9989948,0.000006497103,0.0006087242,0.00018345121,0.00012256185,8.2425984e-8,0.000012456439,0.0000018126515,0.0000695904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980053,0.000054956836,0.000681429,0.00017336414,0.0004120512,0.00067293335],"domain_scores_gemma":[0.9975033,0.00011759357,0.00039719674,0.000103008984,0.0002859915,0.0015929491],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012838047,0.0001425939,0.00032949395,0.00058649643,0.0005328534,0.00009978537,0.00050429074,0.000074945936,0.0029942174],"category_scores_gemma":[0.00023420385,0.0001003513,0.00015689287,0.00088256714,0.00043491286,0.00034205063,0.000004374471,0.00018572429,0.000040034418],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009289956,0.000004465095,0.9917985,0.000021981372,0.000023449637,0.00014438143,0.00033574275,0.0007044834,0.0001056815,0.000051737203,0.00006994495,0.0067303046],"study_design_scores_gemma":[0.0002454615,0.00031012847,0.986051,0.00017551675,0.000048394715,0.00032366192,0.003667051,0.004283427,0.0008096784,0.00032163342,0.0035287347,0.0002353146],"about_ca_topic_score_codex":0.6784218,"about_ca_topic_score_gemma":0.99429655,"teacher_disagreement_score":0.3158747,"about_ca_system_score_codex":0.000010086328,"about_ca_system_score_gemma":0.001014758,"threshold_uncertainty_score":0.9979172},"labels":[],"label_agreement":null},{"id":"W2049478820","doi":"10.1139/e10-035","title":"A taxonomic assessment of the type series of <i>Albertosaurus sarcophagus</i> and the identity of Tyrannosauridae (Dinosauria, Coelurosauria) in the <i>Albertosaurus</i> bonebed from the Horseshoe Canyon Formation (Campanian–Maastrichtian, Late Cretaceous)This article is one of a series of papers published in this Special Issue on the theme <i>Albertosaurus</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Type (biology); Geology; Paleontology; Series (stratigraphy); Type specimen; Character (mathematics); Canyon; Taxon; Mathematics; Biology; Genus; Zoology; Geomorphology; Geometry","score_opus":0.013214456792743133,"score_gpt":0.20873142525618368,"score_spread":0.19551696846344055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049478820","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9769301,0.0010989505,0.0000015077575,0.015116986,0.0008030235,0.00049648475,0.00035521298,0.0000015154084,0.005196237],"genre_scores_gemma":[0.9985167,0.00027567285,0.00014676011,0.0007532808,0.00021895209,0.0000030130846,0.000007974206,0.0000037734037,0.00007392122],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99662954,0.0009158771,0.0011586508,0.00024363185,0.00061759225,0.0004347402],"domain_scores_gemma":[0.9961955,0.0016531984,0.0013441164,0.00046507618,0.00022386474,0.00011823264],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0034016918,0.00022562196,0.0006224542,0.00022488894,0.00039704336,0.00007887141,0.0014947398,0.00016468228,0.0027080784],"category_scores_gemma":[0.0009291464,0.00010619155,0.00017797302,0.0012259326,0.0042336145,0.0010435373,0.000042710417,0.00066326576,0.000002716966],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008482655,0.000088533314,0.97181964,0.000048959784,0.00012423588,0.000009451691,0.011132277,0.00064900966,0.008288048,0.0035736754,0.0026950922,0.00072281016],"study_design_scores_gemma":[0.0009769972,0.0005292174,0.9829964,0.00013353398,0.00008461465,0.000074021926,0.0025260274,0.0005138368,0.004366531,0.002339981,0.005314392,0.00014447035],"about_ca_topic_score_codex":0.06469215,"about_ca_topic_score_gemma":0.78351265,"teacher_disagreement_score":0.7188205,"about_ca_system_score_codex":0.0000077584955,"about_ca_system_score_gemma":0.0012026795,"threshold_uncertainty_score":0.99847627},"labels":[],"label_agreement":null},{"id":"W2049702019","doi":"10.1139/e04-091","title":"Eocene shoshonitic mafic dykes intruding the Monashee Complex, British Columbia: a petrogenetic relationship with the Kamloops Group volcanic sequence?","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University; Queen's University; University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Mafic; Geochemistry; Amphibole; Volcanic rock; Partial melting; Diorite; Mantle (geology); Phlogopite; Basalt; Petrology; Zircon; Volcano; Quartz; Paleontology","score_opus":0.03252793404404148,"score_gpt":0.19726471880008306,"score_spread":0.1647367847560416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049702019","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9873069,0.002301186,0.000032476535,0.008491533,0.00008043767,0.00008840688,0.00003,0.000005851379,0.0016632357],"genre_scores_gemma":[0.99780697,0.00003305457,0.000722591,0.0010136667,0.00019907617,7.9371796e-7,0.00000588217,0.000002005776,0.00021595789],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99832386,0.00015226347,0.00031971053,0.00021453653,0.0004530315,0.0005366155],"domain_scores_gemma":[0.99863744,0.0004273131,0.00019927943,0.00013060505,0.00013280095,0.00047259263],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009846612,0.00011012897,0.00020061996,0.000084228515,0.0016005777,0.0009059642,0.0008136982,0.00004363727,0.008003941],"category_scores_gemma":[0.00021036669,0.0000687775,0.00010919412,0.0010285019,0.00155342,0.00029453746,0.000009263657,0.0003466214,0.000047734567],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000022373472,0.000003848777,0.98932886,0.000002132412,0.000017619544,0.000044206943,0.00007352384,0.0057595484,0.000011047599,0.00012822298,0.000308405,0.0043203346],"study_design_scores_gemma":[0.00011482352,0.00021459242,0.98424226,0.000031731146,0.00004993647,0.0006869516,0.00065104925,0.0039353385,0.000003942155,0.0066808336,0.003259256,0.00012927226],"about_ca_topic_score_codex":0.15815337,"about_ca_topic_score_gemma":0.98966324,"teacher_disagreement_score":0.8315099,"about_ca_system_score_codex":0.00000674784,"about_ca_system_score_gemma":0.00048675752,"threshold_uncertainty_score":0.9996992},"labels":[],"label_agreement":null},{"id":"W2049725585","doi":"10.1139/cjes-2013-0035","title":"Monazite ages and pressure–temperature–time paths from anatectites in the southern Ruby Range, Montana, USA: evidence for delamination, ultramafic magmatism, and rapid uplift at ca. 1780 Ma","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Metamorphism; Anatexis; Ultramafic rock; Monazite; Sillimanite; Migmatite; Gneiss; Proterozoic; Igneous rock; Zircon; Kyanite; Partial melting; Metamorphic rock; Biotite; Quartz; Crust; Paleontology; Tectonics","score_opus":0.01411114377670893,"score_gpt":0.19413255867051907,"score_spread":0.18002141489381013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049725585","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97816455,0.018081458,0.0000044596986,0.0032441542,0.00005404211,0.00017433234,0.00013907382,0.0000020439104,0.00013588181],"genre_scores_gemma":[0.99841946,0.0002696813,0.00053541124,0.00045096598,0.00006160162,0.0000021585306,0.000010325202,0.0000013835779,0.00024903822],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875826,0.00012311147,0.00028737597,0.00024056999,0.00025770257,0.00033299642],"domain_scores_gemma":[0.99848014,0.00082684436,0.00014950975,0.000087099645,0.0001250295,0.00033139242],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00083514623,0.00013288442,0.00022487027,0.00016048462,0.00040904817,0.0003518353,0.0003534244,0.0000693492,0.004133799],"category_scores_gemma":[0.00043875584,0.000074215954,0.000059157093,0.00035835328,0.0004832215,0.00047944734,0.0000076024903,0.00014975174,0.00004222018],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009380798,0.0000033356703,0.9916061,0.000007976879,0.000017372331,0.000017313187,0.0007438436,0.0005942839,0.00040069036,0.000007711634,0.00037773643,0.00621422],"study_design_scores_gemma":[0.00015692509,0.00016623814,0.9878171,0.00004884767,0.000035861696,0.000040080376,0.0004858719,0.006735824,0.000074845426,0.0036598938,0.0006588045,0.00011969481],"about_ca_topic_score_codex":0.11068693,"about_ca_topic_score_gemma":0.5558957,"teacher_disagreement_score":0.44520876,"about_ca_system_score_codex":0.0000015568686,"about_ca_system_score_gemma":0.000093347095,"threshold_uncertainty_score":0.9967766},"labels":[],"label_agreement":null},{"id":"W2049738862","doi":"10.1139/e09-029","title":"Gold Run tephra: a Middle Pleistocene stratigraphic and paleoenvironmental marker across west-central Yukon Territory, Canada","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Toronto; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Tephra; Geology; Rhyolite; Pleistocene; Loess; Radiocarbon dating; Volcano; Paleontology; Geochemistry; Geomorphology; Volcanic rock","score_opus":0.016670037501634188,"score_gpt":0.20923072314936242,"score_spread":0.19256068564772824,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049738862","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99176097,0.0032622188,0.0000011045531,0.002129744,0.0004402696,0.00007925674,0.00006264935,0.0000023312427,0.002261438],"genre_scores_gemma":[0.99882776,0.000087406894,0.00017916546,0.0006667411,0.00009199496,1.3806294e-7,0.000005424845,0.0000012083119,0.000140189],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981622,0.00011391936,0.00028815237,0.00021854838,0.00033205055,0.0008851121],"domain_scores_gemma":[0.998622,0.00009746745,0.00012871354,0.000094140596,0.000027128805,0.0010305396],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00063906756,0.00014165313,0.00021597905,0.00014998211,0.000614346,0.00012126337,0.0003981916,0.00008719799,0.0009391413],"category_scores_gemma":[0.000049318165,0.00011351197,0.000048276874,0.00022462137,0.001123815,0.00040049895,0.0000040643217,0.0003280869,0.000008284756],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017551329,0.000004117208,0.9976817,0.000003801372,0.000009278518,0.00034583622,0.00014423663,0.00018115566,0.0000045388915,0.00002523395,0.00018522283,0.001397341],"study_design_scores_gemma":[0.00024094593,0.00046821169,0.99513656,0.000025335397,0.0000067631827,0.0008392164,0.0006070701,0.00028269814,0.000013577157,0.00014850247,0.0021017198,0.0001293924],"about_ca_topic_score_codex":0.42437705,"about_ca_topic_score_gemma":0.99842584,"teacher_disagreement_score":0.5740488,"about_ca_system_score_codex":0.0000018491698,"about_ca_system_score_gemma":0.0019189579,"threshold_uncertainty_score":0.99997413},"labels":[],"label_agreement":null},{"id":"W2049768016","doi":"10.1139/cjes-2013-0193","title":"Hydrocarbon resources potential mapping using evidential belief functions and frequency ratio approaches, southeastern Saskatchewan, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Petroleum; Geology; Structural basin; Petroleum system; Petroleum exploration; Scale (ratio); Petroleum engineering; Cartography; Source rock; Geomorphology","score_opus":0.05098812593553208,"score_gpt":0.2016528544286344,"score_spread":0.1506647284931023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049768016","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95599264,0.0016153001,0.033524062,0.0030392976,0.0011853601,0.000080843936,0.0000057435286,0.000010330408,0.0045464477],"genre_scores_gemma":[0.9935347,7.8623543e-7,0.005593069,0.00012006186,0.0002564864,4.7885385e-7,6.8932724e-7,0.0000018564132,0.0004918627],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99846405,0.00008765875,0.00033762047,0.00025921947,0.00043527028,0.00041617462],"domain_scores_gemma":[0.998542,0.000028310915,0.0002637782,0.00016137563,0.00019313279,0.00081141293],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009849146,0.00012903991,0.00017536242,0.00020465541,0.00054440735,0.00043838358,0.0006731788,0.000054048724,0.000011091277],"category_scores_gemma":[0.00012748834,0.00011400917,0.0000432626,0.0004746736,0.00028357812,0.0006065762,0.00005825114,0.00019470058,0.0000013022492],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038075206,0.00009715478,0.64735645,0.00024538962,0.0003430812,0.003397801,0.058282454,0.24650115,0.018828351,0.00420185,0.0033566311,0.017351609],"study_design_scores_gemma":[0.0038773427,0.0015309154,0.099625774,0.0014928533,0.00024650226,0.02016937,0.17392652,0.6092872,0.0029365085,0.023893515,0.05951967,0.0034938322],"about_ca_topic_score_codex":0.4526002,"about_ca_topic_score_gemma":0.9488713,"teacher_disagreement_score":0.5477307,"about_ca_system_score_codex":0.000023720006,"about_ca_system_score_gemma":0.0073648975,"threshold_uncertainty_score":0.9982624},"labels":[],"label_agreement":null},{"id":"W2049771509","doi":"10.1139/e06-114","title":"In suspect terrane? Provenance of the late Archean Phantom Lake metamorphic suite, Sierra Madre, Wyoming","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Terrane; Geochemistry; Gneiss; Provenance; Metamorphic rock; Detritus; Continental crust; Archean; Radiogenic nuclide; Crust; Anatexis; Igneous rock; Paleontology; Partial melting; Mantle (geology); Tectonics","score_opus":0.016144304604930132,"score_gpt":0.19244700505602136,"score_spread":0.17630270045109123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049771509","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99017715,0.0010696714,0.000003246869,0.0021745428,0.00018913105,0.000060621314,0.000027183618,0.0000016233947,0.006296821],"genre_scores_gemma":[0.99893814,0.000011996403,0.00027181857,0.00020235905,0.00008373052,1.4141615e-7,0.0000017114851,0.0000010077832,0.00048906886],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985505,0.00009380805,0.00042615546,0.0001474857,0.00033617954,0.00044591885],"domain_scores_gemma":[0.999208,0.00012122334,0.00026478452,0.000101309546,0.00007262543,0.00023205658],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00094050117,0.000105766456,0.00025844522,0.00024313666,0.00018974651,0.000062737585,0.0006149757,0.000041245603,0.0031319498],"category_scores_gemma":[0.00016679695,0.00005832618,0.00014871018,0.001117573,0.0007387689,0.0002681931,0.000008225385,0.00017906257,0.000010417026],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000059969107,0.000006474956,0.99270576,0.0000055274504,0.000006271684,0.00004464903,0.000077170764,0.0059477864,0.00041327783,0.00013249795,0.000054833134,0.0005997702],"study_design_scores_gemma":[0.0001372649,0.0001086088,0.9793924,0.000042695967,0.000014766479,0.000051767922,0.000086322834,0.0010670422,0.0014091552,0.015624298,0.001969457,0.00009622361],"about_ca_topic_score_codex":0.05711188,"about_ca_topic_score_gemma":0.89600176,"teacher_disagreement_score":0.83888984,"about_ca_system_score_codex":0.00000160066,"about_ca_system_score_gemma":0.000450533,"threshold_uncertainty_score":0.9977793},"labels":[],"label_agreement":null},{"id":"W2049815644","doi":"10.1139/e00-019","title":"Age and origin of advanced argillic alteration zones and related exotic limonite deposits in the Limonite Creek area, central British Columbia","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Mine drainage and remediation techniques","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"University of British Columbia","keywords":"Limonite; Alunite; Geology; Geochemistry; Weathering; Pyrite; Mineralogy; Paleontology; Hydrothermal circulation","score_opus":0.010672603100552666,"score_gpt":0.20193213225137452,"score_spread":0.19125952915082184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049815644","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977495,0.00058397726,0.000010011,0.00015802404,0.00004050039,0.00010946453,0.0000037961474,0.0000022679878,0.0013424255],"genre_scores_gemma":[0.9982853,0.00046307824,0.0007245153,0.00010310108,0.000012273057,0.0000010399932,9.078707e-7,0.0000023420732,0.00040742004],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99918514,0.00006305988,0.00024860422,0.000114629314,0.00018278856,0.0002057465],"domain_scores_gemma":[0.9996093,0.000041264873,0.00011241293,0.000051240906,0.000011953722,0.00017382098],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040778014,0.00004867599,0.00010623583,0.00005809711,0.00022547733,0.00028433863,0.00015515277,0.000032089105,0.00048271954],"category_scores_gemma":[0.00003723869,0.000048528593,0.000020552872,0.0003546519,0.00047981122,0.00042361833,0.000006185342,0.00009998734,0.0000011053977],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007123878,0.00003277523,0.88376355,0.000014921946,0.000008518577,0.0012134425,0.0047208024,0.0019465828,0.0029472325,0.00002659536,0.0004046997,0.10491378],"study_design_scores_gemma":[0.00017583248,0.00023295687,0.9962052,0.00008976088,0.000006652896,0.00043536356,0.00035085468,0.00035709728,0.00011686281,0.0007383743,0.0012146282,0.000076422424],"about_ca_topic_score_codex":0.046970762,"about_ca_topic_score_gemma":0.8170163,"teacher_disagreement_score":0.7700455,"about_ca_system_score_codex":0.000008533359,"about_ca_system_score_gemma":0.00006514954,"threshold_uncertainty_score":0.95937556},"labels":[],"label_agreement":null},{"id":"W2050010041","doi":"10.1139/e07-011","title":"A new ceratopsid dinosaur (Ornithischia) from the uppermost Horseshoe Canyon Formation (upper Maastrichtian), Alberta, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; Canadian Museum of Nature","funders":"","keywords":"Paleontology; Geology; Canyon; Tetrapod (structure); Premaxilla; Trace fossil; Postcrania; Cretaceous; Anatomy; Biology; Geomorphology","score_opus":0.012294125026446362,"score_gpt":0.19274676630184276,"score_spread":0.1804526412753964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050010041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9762901,0.0031214291,0.0002589397,0.006010694,0.0020249737,0.00008033479,0.00012751379,0.0000028110476,0.012083182],"genre_scores_gemma":[0.99673116,0.00002443929,0.0006364566,0.0018079492,0.0004460016,7.686641e-8,0.00002531545,0.0000013846737,0.00032719813],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984716,0.000102027014,0.0003782854,0.00016027875,0.0002881611,0.0005996099],"domain_scores_gemma":[0.9983052,0.0004955704,0.00022934485,0.00011104926,0.00008461073,0.00077421323],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007566837,0.00013017787,0.00017094765,0.00015836289,0.00086285453,0.00007788106,0.0005992997,0.000090278256,0.0029878372],"category_scores_gemma":[0.00021575046,0.000083261475,0.00005872096,0.00044860938,0.00036104326,0.0005002443,0.0000042774404,0.00028860717,0.00005268481],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014443079,9.3904316e-7,0.9853536,7.168426e-7,0.000012349512,0.0000696094,0.00025318578,0.00033598676,0.000006880951,0.000097999524,0.0076312455,0.0062230485],"study_design_scores_gemma":[0.00013678013,0.000108543354,0.9189265,0.000014776543,0.000011791263,0.00039378466,0.00065619656,0.000263881,0.00003334897,0.00028325006,0.07906231,0.00010887705],"about_ca_topic_score_codex":0.9836058,"about_ca_topic_score_gemma":0.9999602,"teacher_disagreement_score":0.07143107,"about_ca_system_score_codex":0.000010397856,"about_ca_system_score_gemma":0.0067758868,"threshold_uncertainty_score":0.99885476},"labels":[],"label_agreement":null},{"id":"W2050051347","doi":"10.1139/e01-046","title":"Late Neoproterozoic cap carbonates: Mackenzie Mountains, northwestern Canada: precipitation and global glacial meltdown","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":274,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"","keywords":"Geology; Dolostone; Aragonite; Snowball Earth; Terrigenous sediment; Grainstone; Subaerial; Wackestone; Geochemistry; Carbonate; Calcite; Facies; Paleontology; Sedimentary depositional environment; Sedimentary rock; Carbonate rock; Glacial period","score_opus":0.014381295437574527,"score_gpt":0.21383298317569777,"score_spread":0.19945168773812325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050051347","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9830218,0.006882683,0.000010092999,0.0006782102,0.0006644187,0.00008175219,0.000106865074,0.0000035636006,0.0085506365],"genre_scores_gemma":[0.9993319,0.00006723103,0.00024777665,0.00019763982,0.00012228293,2.096142e-7,0.0000037611587,5.723123e-7,0.000028610946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986555,0.00007787418,0.00030361148,0.00018643447,0.00031025746,0.00046632523],"domain_scores_gemma":[0.998884,0.000057679616,0.00019182201,0.000068552356,0.00009533432,0.00070257473],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004374339,0.00013411856,0.00019460771,0.00014761435,0.0005164747,0.00015810874,0.00030485253,0.00006645558,0.00019227523],"category_scores_gemma":[0.00004900304,0.000108699096,0.000044225086,0.00038497217,0.00053147064,0.00048687786,0.0000010142767,0.00014840199,0.0000022474003],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014027334,0.0000012811295,0.97683376,0.0000031110358,0.000013602633,0.00024772953,0.00021134758,0.0003097452,0.000002149457,0.00004182369,0.00005120273,0.022270234],"study_design_scores_gemma":[0.00019588476,0.00022094414,0.99597853,0.000023864213,0.0000136086,0.00042661134,0.00029040332,0.00050021807,0.0000062742397,0.00075028994,0.0014646027,0.00012874344],"about_ca_topic_score_codex":0.9389812,"about_ca_topic_score_gemma":0.99988544,"teacher_disagreement_score":0.06090424,"about_ca_system_score_codex":0.0000059669596,"about_ca_system_score_gemma":0.0036382785,"threshold_uncertainty_score":0.645415},"labels":[],"label_agreement":null},{"id":"W2050064570","doi":"10.1139/e04-090","title":"Accretion history of the Trans-Hudson Orogen in Manitoba and Saskatchewan from paleomagnetism","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor","funders":"","keywords":"Terrane; Geology; Craton; Paleomagnetism; Apparent polar wander; Batholith; Archean; Paleontology; Accretion (finance); Continental margin; Subduction; Tectonics; Devonian; Geochemistry; Earth science","score_opus":0.014400428797460611,"score_gpt":0.1646887688716861,"score_spread":0.15028834007422548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050064570","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9895295,0.0064663743,0.0000029703351,0.001717049,0.00014002489,0.000028872691,0.000015991032,8.8692804e-7,0.0020983408],"genre_scores_gemma":[0.99899876,0.00006070877,0.0005506014,0.00024586127,0.0000639664,5.8104558e-8,0.0000013269114,4.6554158e-7,0.00007825895],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992188,0.000060441547,0.00023730025,0.000107307555,0.00018900991,0.00018709776],"domain_scores_gemma":[0.99949527,0.000067053814,0.00011764382,0.00005503431,0.000029824923,0.00023515045],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034438178,0.00006244475,0.00014075295,0.0001084994,0.00006735827,0.000019213263,0.00028664983,0.00004016661,0.0037159862],"category_scores_gemma":[0.000046439418,0.000036698017,0.00006241679,0.0002324638,0.000519506,0.00015029206,0.000002959135,0.00012251602,0.000004755233],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000029613468,0.0000025360569,0.98546743,0.0000013774061,0.0000035567366,0.0000048442357,0.0005541761,0.0006043562,0.0002784179,0.000007968831,0.00005485515,0.013017533],"study_design_scores_gemma":[0.00010054093,0.000077798824,0.9898433,0.000020525056,0.000012060791,0.000012476693,0.00068130525,0.00067728537,0.00025192313,0.0012309317,0.0070370156,0.00005485062],"about_ca_topic_score_codex":0.16963124,"about_ca_topic_score_gemma":0.9759982,"teacher_disagreement_score":0.806367,"about_ca_system_score_codex":0.0000038027065,"about_ca_system_score_gemma":0.00049328175,"threshold_uncertainty_score":0.99719477},"labels":[],"label_agreement":null},{"id":"W2050407573","doi":"10.1139/e05-088","title":"Generation of a heavy-mineral glacial indicator dispersal train from a diabase sill, Nipigon region, northwestern Ontario","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"University of Minnesota","keywords":"Geology; Bedrock; Pigeonite; Glacial period; Geochemistry; Geomorphology; Heavy mineral; Earth science; Paleontology; Augite; Plagioclase","score_opus":0.04500387749151476,"score_gpt":0.23955552133834482,"score_spread":0.19455164384683005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050407573","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964488,0.0007139433,0.00003331856,0.001419161,0.00042741915,0.00007367042,0.00004132799,0.0000023747964,0.0008399699],"genre_scores_gemma":[0.99844456,0.000013644348,0.00069542124,0.0002808274,0.00040981415,2.6809533e-7,0.000024664154,0.0000015901009,0.00012923955],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99850804,0.00015481755,0.00039445658,0.00019756216,0.0002998454,0.00044530284],"domain_scores_gemma":[0.99884117,0.00011850003,0.00023632795,0.00010060404,0.000085232656,0.0006181655],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000654401,0.00011454844,0.0002473458,0.0003854411,0.0003573398,0.000064524196,0.00039532725,0.00010524101,0.0023624129],"category_scores_gemma":[0.0000618641,0.00009005368,0.000088808905,0.00026299816,0.0009364468,0.00046353223,0.0000042418933,0.00029057736,0.00004889564],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030191575,0.0000081503995,0.99503946,0.0000017104181,0.000015165918,0.00010134085,0.0025068817,0.00094337587,0.000024328914,0.000027497092,0.00013213097,0.0011697591],"study_design_scores_gemma":[0.0003272899,0.00037711102,0.9944486,0.000017987379,0.000014758871,0.0001947338,0.00027579506,0.0016417007,0.00017013171,0.000067226516,0.0023559749,0.00010871411],"about_ca_topic_score_codex":0.29357213,"about_ca_topic_score_gemma":0.9984593,"teacher_disagreement_score":0.70488715,"about_ca_system_score_codex":0.0000024431808,"about_ca_system_score_gemma":0.0029575434,"threshold_uncertainty_score":0.9985496},"labels":[],"label_agreement":null},{"id":"W2050515251","doi":"10.1139/e05-028","title":"Constraints on the composition of the crust and uppermost mantle in northwestern Canada: <i>Vp</i>/<i>Vs</i> variations along Lithoprobe's SNorCLE transect","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Terrane; Craton; Crust; Foreland basin; Mantle (geology); Mafic; Continental crust; Crustal recycling; Seismic refraction; Seismology; Geochemistry; Tectonics","score_opus":0.01069680597234208,"score_gpt":0.18039242210153628,"score_spread":0.1696956161291942,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050515251","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99438703,0.00012635424,0.00000766528,0.0036790024,0.0003320984,0.00010075337,0.00020918708,7.828273e-7,0.0011571313],"genre_scores_gemma":[0.99916756,0.000011394792,0.00008418938,0.0006427612,0.00007456596,2.1926235e-7,0.000002082897,0.0000012138988,0.000016025411],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909186,0.00010144214,0.0002589763,0.0000956464,0.00023562624,0.00021646106],"domain_scores_gemma":[0.99941885,0.00013829391,0.00015290703,0.00008187034,0.000048722093,0.00015935673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055719056,0.000073458155,0.00013402976,0.00006899229,0.000340885,0.000092872135,0.00028569222,0.000023195607,0.00039612528],"category_scores_gemma":[0.000019577017,0.00004189666,0.000030412368,0.00023018915,0.00041303883,0.0001729137,0.0000031167194,0.000104652,0.0000022012014],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026954194,0.000019206776,0.9598451,0.000019587522,0.000029938044,0.000046751655,0.0027740202,0.023460593,0.0015072477,0.0021672742,0.00040195428,0.0097013265],"study_design_scores_gemma":[0.00013565578,0.000077987395,0.9965588,0.000067120774,0.000009353458,0.00004742206,0.00018149763,0.00041305117,0.00081450585,0.000113766655,0.001516979,0.00006389916],"about_ca_topic_score_codex":0.6796844,"about_ca_topic_score_gemma":0.9956383,"teacher_disagreement_score":0.3159539,"about_ca_system_score_codex":0.0000029465784,"about_ca_system_score_gemma":0.0014723603,"threshold_uncertainty_score":0.4337294},"labels":[],"label_agreement":null},{"id":"W2050520180","doi":"10.1139/e05-079","title":"UPb age constraints on arenaceous and volcanic rocks of the Wakeham Group, eastern Grenville Province","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Zircon; Metamorphism; Geochemistry; Plutonism; Terrane; Volcanic rock; Provenance; Laurentia; Precambrian; Titanite; Protolith; Basement; Geochronology; Ordovician; Paleontology; Pluton; Volcano; Archaeology","score_opus":0.013942575366024019,"score_gpt":0.17821529719948576,"score_spread":0.16427272183346173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050520180","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98816967,0.0007883566,0.000008433106,0.0015936429,0.0001147155,0.000048149777,0.000024647788,0.0000014035875,0.009250998],"genre_scores_gemma":[0.9990844,0.000015726819,0.00019548339,0.00043841515,0.000074579104,6.385263e-8,7.916931e-7,7.019022e-7,0.00018984902],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989688,0.0000529727,0.00025695108,0.00014823908,0.00028004762,0.0002930159],"domain_scores_gemma":[0.9991739,0.00008746581,0.00018955726,0.00008348714,0.000046472407,0.00041911984],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00036864384,0.000093009054,0.00017892219,0.0001067081,0.00024643805,0.00006175446,0.00040574413,0.00003866207,0.0028697047],"category_scores_gemma":[0.00012232883,0.000049026177,0.00008691392,0.0002781036,0.0012156215,0.00010532008,0.00000848847,0.00016384984,0.000019873703],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000067108904,0.000007752624,0.95345575,0.0000043675227,0.00001182093,0.00003984693,0.000106210035,0.002922745,0.00006697478,0.00007353812,0.0000639581,0.04324032],"study_design_scores_gemma":[0.00018274171,0.0004609072,0.9892829,0.00006606323,0.000022233855,0.00013997722,0.00029932635,0.0022028245,0.0003291971,0.0012593131,0.0056246375,0.0001298712],"about_ca_topic_score_codex":0.009463565,"about_ca_topic_score_gemma":0.7174436,"teacher_disagreement_score":0.70798004,"about_ca_system_score_codex":0.0000014124604,"about_ca_system_score_gemma":0.0003041248,"threshold_uncertainty_score":0.9980418},"labels":[],"label_agreement":null},{"id":"W2050528402","doi":"10.1139/e00-050","title":"Mesoproterozoic graphite deposits, New Jersey Highlands: geologic and stable isotopic evidence for possible algal origins","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Pegmatite; Gneiss; Biotite; Granulite; Metamorphism; Petrogenesis; Proterozoic; Feldspar; Partial melting; Sedimentary rock; Quartz; Metamorphic rock; Facies; Geomorphology; Crust; Basalt; Paleontology; Structural basin","score_opus":0.03120320804948532,"score_gpt":0.23132523925099766,"score_spread":0.20012203120151234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050528402","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99234194,0.0053713582,0.000047421665,0.0011442796,0.00013374838,0.000097574186,0.00002486666,0.000003998228,0.0008348149],"genre_scores_gemma":[0.99623644,0.0002439017,0.0018295902,0.00026535237,0.0001550907,4.0172532e-7,0.000005250345,0.0000012109156,0.0012627532],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988373,0.000030087938,0.00026485632,0.0002080023,0.0002105358,0.0004492023],"domain_scores_gemma":[0.9989422,0.00008344927,0.00011714944,0.000083038816,0.00005179219,0.0007223557],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00050100527,0.00011669482,0.00018726762,0.00017553239,0.0005744374,0.00022631379,0.00034654554,0.000045402976,0.005713761],"category_scores_gemma":[0.000056764573,0.000085120475,0.00008258854,0.00046047755,0.0002670933,0.00061736477,0.0000028971026,0.00010033173,0.000018304558],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019761748,0.0000024150218,0.98000115,0.000012869458,0.000020613443,0.000029640107,0.00012092022,0.0014924577,0.00008374652,0.00002288766,0.0003012846,0.017892245],"study_design_scores_gemma":[0.00046846963,0.00089172425,0.9661482,0.00015284939,0.00008338547,0.00030001873,0.00030767277,0.002510903,0.0011812815,0.002554233,0.025123103,0.00027814624],"about_ca_topic_score_codex":0.057809856,"about_ca_topic_score_gemma":0.3420507,"teacher_disagreement_score":0.28424084,"about_ca_system_score_codex":0.0000025639001,"about_ca_system_score_gemma":0.0007232415,"threshold_uncertainty_score":0.99519515},"labels":[],"label_agreement":null},{"id":"W2050551919","doi":"10.1139/e04-028","title":"Superimposed Quesnel (late PaleozoicJurassic) and YukonTanana (DevonianMississippian) arc assemblages, Cassiar Mountains, northern British Columbia: field, UPb, and igneous petrochemical evidence","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Pacific Institute for the Mathematical Sciences; Geological Survey of Canada","funders":"University of British Columbia","keywords":"Geology; Terrane; Batholith; Devonian; Paleozoic; Paleontology; Permian; Pluton; Island arc; Igneous rock; Late Devonian extinction; Geochemistry; Carboniferous; Subduction; Tectonics; Structural basin","score_opus":0.01376703322358437,"score_gpt":0.1961473323318881,"score_spread":0.18238029910830375,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050551919","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9867869,0.009637008,0.000016751617,0.0026633756,0.00010601276,0.000069494556,0.000020684236,0.0000081812495,0.00069161196],"genre_scores_gemma":[0.99782395,0.0005724976,0.00076711376,0.0005875928,0.00010019332,3.229909e-7,0.000003404367,0.0000025919912,0.00014229999],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981235,0.000070327405,0.00042639792,0.00038251423,0.0003916739,0.00060555805],"domain_scores_gemma":[0.99796325,0.0002448209,0.0001748838,0.000108893306,0.00014708439,0.0013610937],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005645125,0.00016142524,0.00037013873,0.000117066666,0.0006427464,0.0008965287,0.00040177803,0.00012523863,0.001584188],"category_scores_gemma":[0.0005980774,0.00015543075,0.00010387405,0.0004391148,0.0007904027,0.00049981533,0.000016418164,0.00033497668,0.000010060615],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000757692,0.0000065136987,0.9902849,0.000012312773,0.000020429961,0.0009010349,0.00012770237,0.0002772791,0.00034221058,0.0000045848024,0.00004166143,0.007973767],"study_design_scores_gemma":[0.00029404173,0.00056482933,0.9898151,0.00021624332,0.000049531922,0.001551998,0.00034859593,0.00039443202,0.00017681018,0.005842723,0.000470593,0.00027505626],"about_ca_topic_score_codex":0.48692277,"about_ca_topic_score_gemma":0.98712116,"teacher_disagreement_score":0.50019836,"about_ca_system_score_codex":0.000006926988,"about_ca_system_score_gemma":0.00081499474,"threshold_uncertainty_score":0.9993285},"labels":[],"label_agreement":null},{"id":"W2050599985","doi":"10.1139/e11-033","title":"High-temperature brine in chalcopyrite-rich quartz vein 40 km southwest of Sudbury, Ontario","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Gabbro; Geochemistry; Fluid inclusions; Quartz; Felsic; Igneous rock; Vein; Pyrrhotite; Mineralogy; Mafic; Pyrite","score_opus":0.020622908356039672,"score_gpt":0.18021654424132563,"score_spread":0.15959363588528597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050599985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945264,0.0007013567,8.284214e-7,0.00037948773,0.00024851382,0.000040611212,0.000030488489,0.0000022706386,0.004070075],"genre_scores_gemma":[0.9986286,0.000014424851,0.0009014244,0.00014737918,0.00006735275,1.1454138e-7,0.000007740017,0.0000010890958,0.00023184158],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985061,0.00006144604,0.000468016,0.00020122725,0.00030874964,0.00045442552],"domain_scores_gemma":[0.99889493,0.00006378498,0.00021800339,0.00010432972,0.00013492105,0.00058402336],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00071997655,0.00013157251,0.00034282872,0.00041013877,0.00013971978,0.000053339263,0.0005396799,0.00008443207,0.017417997],"category_scores_gemma":[0.000103884115,0.00008841825,0.00011041653,0.0009020745,0.0005139039,0.00027686506,0.0000067379065,0.000311366,0.000047263962],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016373748,0.000012406437,0.99779904,0.0000038813873,0.000009002836,0.00011742637,0.0008598719,0.00052120636,0.000103778395,0.0000919681,0.000044568318,0.00042050364],"study_design_scores_gemma":[0.00017098861,0.00043034367,0.99374616,0.00003437869,0.00001401669,0.00004503662,0.00045865882,0.000038501214,0.0013061363,0.0031686896,0.0004651204,0.00012197191],"about_ca_topic_score_codex":0.8428709,"about_ca_topic_score_gemma":0.9960272,"teacher_disagreement_score":0.15315628,"about_ca_system_score_codex":0.0000033295141,"about_ca_system_score_gemma":0.0009140168,"threshold_uncertainty_score":0.9834802},"labels":[],"label_agreement":null},{"id":"W2050663080","doi":"10.1139/e00-056","title":"Modélisation d'un système karstique complexe (bassin de S<sup>t</sup>-Chaptes, Gard, France) : un outil de synthèse des données géologiques et hydrogéologiques","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Karst Systems and Hydrogeology","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Aquifer; Geology; Karst; Hydrogeology; Structural basin; Geomorphology; Groundwater; Petrology; Geotechnical engineering; Paleontology","score_opus":0.028272057783101656,"score_gpt":0.2186186747384869,"score_spread":0.19034661695538524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050663080","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9858693,0.00789304,0.0009795758,0.001177884,0.00015824236,0.00014630193,0.00006989432,0.000032987828,0.003672804],"genre_scores_gemma":[0.9886641,0.0006773193,0.009292311,0.0010313565,0.0002077639,0.0000013234878,0.000008435537,0.000006641395,0.000110767505],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9969268,0.0008090571,0.0006312914,0.00033031314,0.0003323403,0.0009702143],"domain_scores_gemma":[0.99809724,0.00037902597,0.0003070489,0.00017437505,0.00014438506,0.00089792965],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0036646158,0.00025921955,0.0004664602,0.0004052321,0.0008523638,0.0003254292,0.0007300903,0.00022921832,0.004249318],"category_scores_gemma":[0.00032609954,0.00020469085,0.00014995971,0.00039719522,0.0015032811,0.0006857307,0.000007041864,0.0004035669,0.000073249976],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020976882,0.000012748184,0.8500012,0.000023073731,0.000036886824,0.00029885545,0.002758493,0.12485113,0.000022901342,0.0014793118,0.00008692607,0.020407487],"study_design_scores_gemma":[0.00037999742,0.001119361,0.8689696,0.00035205635,0.000041129606,0.0024016995,0.000947568,0.06635551,0.00051338156,0.052656755,0.0057995208,0.000463369],"about_ca_topic_score_codex":0.0742579,"about_ca_topic_score_gemma":0.30296177,"teacher_disagreement_score":0.22870387,"about_ca_system_score_codex":0.000019743155,"about_ca_system_score_gemma":0.0021117313,"threshold_uncertainty_score":0.99666095},"labels":[],"label_agreement":null},{"id":"W2050678322","doi":"10.1139/cjes-2013-0157","title":"Karst geology and hydrogeology of Cape Breton Island, Nova Scotia: an overview","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Karst Systems and Hydrogeology","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Evaporite; Karst; Diapir; Geomorphology; Bedrock; Breccia; Geochemistry; Aquifer; Salt tectonics; Sinkhole; Paleontology; Structural basin; Groundwater","score_opus":0.02789253357868438,"score_gpt":0.23118694945647839,"score_spread":0.203294415877794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050678322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9882734,0.005934262,0.000025892592,0.0006004354,0.0008432535,0.00005922474,0.000017769755,0.0000025094596,0.0042432467],"genre_scores_gemma":[0.9989284,0.000092054295,0.00033936618,0.00040788524,0.00017320775,4.4838632e-8,0.0000035995567,0.0000022055776,0.00005319805],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99841386,0.00022704987,0.0004694779,0.00021978265,0.00019420472,0.00047560874],"domain_scores_gemma":[0.99861795,0.00015298699,0.00035784027,0.00013844218,0.00011023774,0.0006225538],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015300781,0.00012977833,0.00042629108,0.00041716284,0.00019870138,0.000046578454,0.000424477,0.000116811556,0.002836696],"category_scores_gemma":[0.00012264315,0.00009846241,0.000059867394,0.0003064883,0.001362072,0.0003537537,0.00000763399,0.00016669734,0.00004607002],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000577785,0.000003143886,0.9945425,0.000015345076,0.000010650275,0.000029296898,0.0002443101,0.000827726,0.00002510682,0.0017292708,0.00007090456,0.0024959594],"study_design_scores_gemma":[0.00037210895,0.001819589,0.97353137,0.000055351815,0.000022060949,0.0019182051,0.00020202823,0.004385894,0.00006750547,0.0029318652,0.014514537,0.00017950784],"about_ca_topic_score_codex":0.14638577,"about_ca_topic_score_gemma":0.94234514,"teacher_disagreement_score":0.7959594,"about_ca_system_score_codex":0.0000010021729,"about_ca_system_score_gemma":0.00067003624,"threshold_uncertainty_score":0.9980748},"labels":[],"label_agreement":null},{"id":"W2050738007","doi":"10.1139/e06-071","title":"Shallow faults, Upper Cretaceous clinoforms, and the Colonsay Collapse, Saskatchewan","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Geology; Cretaceous; Evaporite; Devonian; Glacial period; Subsidence; Paleontology; Fault (geology); Coal measures; Diapir; Graben; Tectonics; Geomorphology; Sedimentary rock; Structural basin","score_opus":0.011209609537522204,"score_gpt":0.19779090720823578,"score_spread":0.18658129767071358,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050738007","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9725495,0.00586524,0.000025342599,0.003266181,0.00028417792,0.00008846857,0.00003224149,0.000003857147,0.017885016],"genre_scores_gemma":[0.99776787,0.0000802691,0.0008719341,0.0005193804,0.00010406747,2.261283e-7,0.0000034789289,8.68545e-7,0.0006519018],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989647,0.00006326935,0.0003063343,0.00010298913,0.00022909368,0.00033361168],"domain_scores_gemma":[0.9991187,0.00024166217,0.0001701699,0.000061324936,0.00011793301,0.0002902531],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011776184,0.00008953364,0.0001675475,0.00014287695,0.0008545165,0.0002506759,0.000341607,0.000048559392,0.0012801831],"category_scores_gemma":[0.00012464423,0.000045041077,0.000055535344,0.00041139498,0.0012559522,0.00039359168,0.000004160968,0.00014145115,0.000032791162],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018700548,0.0000022856582,0.9921406,0.0000051879565,0.000005905209,0.000023313938,0.0003543628,0.0024230338,7.2365197e-7,0.0007591776,0.00052930985,0.0037374161],"study_design_scores_gemma":[0.0004275056,0.00025313703,0.92211914,0.000019364243,0.000014508558,0.00038458378,0.0018482041,0.0016601273,0.0000131352335,0.0085753035,0.06457048,0.00011449408],"about_ca_topic_score_codex":0.03191711,"about_ca_topic_score_gemma":0.7357461,"teacher_disagreement_score":0.70382893,"about_ca_system_score_codex":8.8716314e-7,"about_ca_system_score_gemma":0.0009649556,"threshold_uncertainty_score":0.9996328},"labels":[],"label_agreement":null},{"id":"W2050785728","doi":"10.1139/e10-020","title":"Ecosystem development in the Girdwood area, south-central Alaska, following late Wisconsin glaciation","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Tsuga; Tundra; Glacial period; Vegetation (pathology); Geology; Western Hemlock; Peat; Radiocarbon dating; Physical geography; Forestry; Geography; Ecology; Arctic; Paleontology; Archaeology; Oceanography","score_opus":0.022464433974717972,"score_gpt":0.22013139639002802,"score_spread":0.19766696241531004,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050785728","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936153,0.00026054226,0.0000038848184,0.000946259,0.0009506762,0.000086303495,0.000004787616,0.0000020557277,0.004130182],"genre_scores_gemma":[0.9991983,0.0000020136108,0.00049652794,0.00014769513,0.000064124986,3.0605966e-7,0.0000029765374,9.158635e-7,0.00008710694],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985105,0.00017756571,0.0003089812,0.00013523619,0.00028686767,0.00058089325],"domain_scores_gemma":[0.99918264,0.0002375227,0.0001359917,0.00008361811,0.000046563313,0.00031368903],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0027502945,0.00008672893,0.00015351753,0.00033904423,0.0005544601,0.00014377468,0.00053987256,0.000083356426,0.0012271365],"category_scores_gemma":[0.0002370955,0.000055383713,0.00005779617,0.00041750658,0.00025675722,0.00029417544,0.0000032678204,0.00045133368,0.000134418],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002959763,0.0000020738896,0.9969928,0.0000019466677,0.0000068462023,0.00016435096,0.0018209778,0.0005524485,0.0000028687673,0.000026376647,0.000020691816,0.0004056543],"study_design_scores_gemma":[0.0001633388,0.000060411952,0.9944816,0.00002156701,0.0000046170885,0.00023221018,0.00063878315,0.00046625035,0.000028152972,0.00014158062,0.0036878518,0.00007360336],"about_ca_topic_score_codex":0.0010664313,"about_ca_topic_score_gemma":0.86875355,"teacher_disagreement_score":0.8676871,"about_ca_system_score_codex":6.442573e-7,"about_ca_system_score_gemma":0.002127012,"threshold_uncertainty_score":0.9996859},"labels":[],"label_agreement":null},{"id":"W2050845223","doi":"10.1139/e10-049","title":"Detrital zircon analysis of Mesoproterozoic and Neoproterozoic metasedimentary rocks of north-central Idaho: implications for development of the Belt–Purcell basin","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Geological Survey; Washington State University; National Science Foundation","keywords":"Zircon; Geology; Supergroup; Metamorphic rock; Geochemistry; Protolith; Metamorphism; Sedimentary depositional environment; Facies; Metamorphic facies; Paleontology; Structural basin","score_opus":0.016485077615853414,"score_gpt":0.20653068492592,"score_spread":0.1900456073100666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050845223","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983747,0.0003139898,0.00027392627,0.00053946895,0.000088497174,0.0001317402,0.00020964438,8.00617e-7,0.00006720694],"genre_scores_gemma":[0.9923624,0.000005183237,0.0075180517,0.00006691848,0.000020164392,7.010828e-7,0.000016472413,8.316196e-7,0.0000092748705],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875665,0.00003689955,0.0005555903,0.00015399483,0.00022600057,0.00027088934],"domain_scores_gemma":[0.9987481,0.00014570085,0.0004655484,0.00012042264,0.0001828248,0.00033737556],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053958857,0.00009614832,0.00034797948,0.00036118474,0.00023763817,0.0000220163,0.0004667547,0.000039458384,0.0005649571],"category_scores_gemma":[0.00014167484,0.000057053006,0.00022341823,0.0011897021,0.0006514682,0.00012754506,0.000011975853,0.0001273036,3.5057857e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000064016353,0.000011215,0.9906864,0.000010262395,0.00013028695,3.955022e-7,0.00013957416,0.0007418653,0.0036905615,0.000014947817,0.0000070545507,0.0045610345],"study_design_scores_gemma":[0.000113607886,0.000124278,0.97948295,0.00000973774,0.00028612855,0.000005795497,0.00006338619,0.00039081424,0.018688839,0.000494721,0.0002739226,0.000065846914],"about_ca_topic_score_codex":0.016122198,"about_ca_topic_score_gemma":0.6433123,"teacher_disagreement_score":0.6271901,"about_ca_system_score_codex":0.0000012490315,"about_ca_system_score_gemma":0.0005108455,"threshold_uncertainty_score":0.9904295},"labels":[],"label_agreement":null},{"id":"W2050931508","doi":"10.1139/e00-109","title":"Analyses of crustal structure from bandpass and directionally filtered potential-field data: an example from western Canada","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Sinistral and dextral; Lithosphere; Seismology; Shield; Precambrian; Crust; Trench; Tectonics; Fault (geology); Indian Shield; Craton; Geophysics; Paleontology","score_opus":0.06131910493904576,"score_gpt":0.2546140007084307,"score_spread":0.19329489576938497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050931508","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99676746,0.00097002444,0.00030610207,0.00060313166,0.0004396772,0.000027242488,0.00061987527,0.0000040054942,0.0002625044],"genre_scores_gemma":[0.9964701,0.00007310868,0.0021019594,0.0010682442,0.00016194549,2.0553461e-8,0.000088772664,0.0000015284379,0.00003432186],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99891514,0.00006674506,0.00026289257,0.0002199788,0.00032397994,0.00021125578],"domain_scores_gemma":[0.99898535,0.000129451,0.00019970897,0.00018179747,0.00008600006,0.00041767905],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025374474,0.00009368863,0.0001917649,0.00018825497,0.00023606858,0.0001453931,0.0005531588,0.000039195158,0.0019916748],"category_scores_gemma":[0.000052535637,0.00007238997,0.000023649913,0.00022356231,0.00021478695,0.00074763625,0.000009782465,0.00012673104,4.871476e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025986332,0.0000032465643,0.970888,0.0000020389004,0.000043275853,0.00013910387,0.00022284892,0.000933377,0.00062170957,0.0000016357744,0.0055900337,0.021528712],"study_design_scores_gemma":[0.00028698385,0.00026272068,0.94915223,0.000063178006,0.00005217016,0.0001368967,0.0012439186,0.0108568175,0.004365549,0.00071581785,0.032652266,0.0002114784],"about_ca_topic_score_codex":0.997278,"about_ca_topic_score_gemma":0.9970454,"teacher_disagreement_score":0.027062234,"about_ca_system_score_codex":0.000002277771,"about_ca_system_score_gemma":0.0016512291,"threshold_uncertainty_score":0.9989206},"labels":[],"label_agreement":null},{"id":"W2050945819","doi":"10.1139/e00-044","title":"Linking ocean and continental records of paleoclimate: determining accord and discord in the records","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Milankovitch cycles; Geology; Paleoclimatology; Climatology; Climate oscillation; Glacial period; Climate change; Oceanography; Interglacial; Physical geography; Paleontology; Global warming; Effects of global warming; Geography","score_opus":0.02604816357141778,"score_gpt":0.2480528023954721,"score_spread":0.2220046388240543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050945819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99266946,0.0015330409,7.087995e-7,0.00068697275,0.00015680038,0.000058124726,0.000008920372,0.0000010579234,0.004884914],"genre_scores_gemma":[0.9990646,0.00040307865,0.0003094675,0.00013491315,0.000040426978,8.903889e-8,0.0000015935688,9.752866e-7,0.000044803084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885,0.00018684246,0.00030535643,0.00013809887,0.00015829301,0.00036140863],"domain_scores_gemma":[0.99919623,0.00037940659,0.00012101056,0.000066386085,0.000029734469,0.00020725238],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017673757,0.000082294675,0.00019867462,0.00026215657,0.00032131557,0.00008899595,0.00032522902,0.000056276254,0.0006780754],"category_scores_gemma":[0.000098963144,0.00005289174,0.000028663968,0.00031136436,0.0011373968,0.00030430677,0.000004571581,0.00025832042,0.000004196921],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016290891,0.0000020840846,0.9849569,0.000007666775,0.0000029783412,0.00010628493,0.000722164,0.000031692434,9.1609905e-7,0.000013469171,0.000007192228,0.014132351],"study_design_scores_gemma":[0.00018602221,0.00042416132,0.9954876,0.00007243362,0.0000057127877,0.0009770871,0.001257979,0.00055930775,0.000006063625,0.00047551058,0.0004847061,0.000063472355],"about_ca_topic_score_codex":0.0034894857,"about_ca_topic_score_gemma":0.5195926,"teacher_disagreement_score":0.5161031,"about_ca_system_score_codex":1.8921926e-7,"about_ca_system_score_gemma":0.000318037,"threshold_uncertainty_score":0.74244505},"labels":[],"label_agreement":null},{"id":"W2050966333","doi":"10.1139/e00-033","title":"Mélanges in southern Mexico: geochemistry and metamorphism of Las Ollas complex (Guerrero terrane)","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Secretaría de Educación Pública","keywords":"Geology; Terrane; Geochemistry; Igneous rock; Metamorphism; Lawsonite; Subduction; Blueschist; Amphibole; Metamorphic rock; Quartz; Paleontology; Tectonics","score_opus":0.026732477959225197,"score_gpt":0.19986700160466128,"score_spread":0.17313452364543608,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050966333","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9858518,0.0018046855,0.0000014001346,0.0010923727,0.00003475399,0.000024594043,0.000046798315,0.000001758446,0.011141787],"genre_scores_gemma":[0.99900657,0.000055956567,0.0004246244,0.00019271039,0.00003879162,6.934116e-8,0.0000044866747,7.922808e-7,0.0002759884],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989468,0.000047374644,0.00032101126,0.00015327163,0.0002265475,0.0003050115],"domain_scores_gemma":[0.99925435,0.00008657269,0.00012226817,0.00006713685,0.000045702123,0.0004239746],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047750887,0.00009809527,0.00027097063,0.00016503215,0.00011178904,0.000043851054,0.00030626665,0.000049578117,0.029460175],"category_scores_gemma":[0.00006943783,0.00006586722,0.000074379815,0.00042839616,0.0007155917,0.000115692776,0.0000036559143,0.00013297262,0.00003049719],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009093171,0.0000056213034,0.9871372,0.0000065494623,0.000012836511,0.00005295231,0.0003132313,0.0017419334,0.0003348114,0.000008204259,0.00005370493,0.010323888],"study_design_scores_gemma":[0.00024032798,0.0001698788,0.98730767,0.000039948634,0.000024215396,0.00013012963,0.0008374112,0.0034397736,0.0004789026,0.004694176,0.0024870757,0.00015051136],"about_ca_topic_score_codex":0.06069501,"about_ca_topic_score_gemma":0.4888089,"teacher_disagreement_score":0.42811388,"about_ca_system_score_codex":7.621365e-7,"about_ca_system_score_gemma":0.00018762492,"threshold_uncertainty_score":0.971427},"labels":[],"label_agreement":null},{"id":"W2051005841","doi":"10.1139/e99-124","title":"Interaction among upper crustal, lower crustal, and mantle materials in the Port Mouton pluton, Meguma Lithotectonic Zone, southwest Nova Scotia","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Pluton; Geology; Geochemistry; Mafic; Zircon; Petrology; Mantle (geology); Crust; Nova scotia; Seismology; Tectonics","score_opus":0.014217333687910984,"score_gpt":0.2069904337616646,"score_spread":0.19277310007375362,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051005841","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99337834,0.00050166564,0.0000022787701,0.00090953166,0.00023505956,0.00006848021,0.000027671822,0.0000030082854,0.0048739477],"genre_scores_gemma":[0.9991342,0.000043098287,0.00012437586,0.00039511707,0.00009348977,1.4986708e-7,0.0000062367153,0.0000014475464,0.00020190734],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985666,0.000104151106,0.0003975678,0.0002146193,0.0002911118,0.0004259008],"domain_scores_gemma":[0.99927825,0.000089068206,0.00014604397,0.00009988626,0.000054415308,0.0003323504],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000982493,0.00013440354,0.00023702119,0.00024248566,0.00023914201,0.00035291302,0.00038107808,0.000067315115,0.060146816],"category_scores_gemma":[0.00007261001,0.000076512166,0.000075163414,0.0005663644,0.00066037546,0.0005177997,0.000005144685,0.00022931243,0.00012286784],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003380485,0.000012533817,0.99239576,0.0000053218932,0.000013207054,0.00019639096,0.0004959339,0.0017175322,0.00011358894,0.000017458286,0.00010126204,0.004897191],"study_design_scores_gemma":[0.00012691123,0.00020637497,0.99531764,0.000034818895,0.000018590075,0.00021165557,0.00084142346,0.00035136755,0.00027036297,0.00044342715,0.0020516736,0.00012573569],"about_ca_topic_score_codex":0.18980381,"about_ca_topic_score_gemma":0.7375219,"teacher_disagreement_score":0.54771805,"about_ca_system_score_codex":0.0000024069705,"about_ca_system_score_gemma":0.0002361616,"threshold_uncertainty_score":0.94071233},"labels":[],"label_agreement":null},{"id":"W2051087195","doi":"10.1139/e03-083","title":"What is a hot spring?","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Diet and metabolism studies","field":"Medicine","cited_by":97,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Spring (device); Hot spring; Term (time); Geology; Thermal; Core temperature; Environmental science; Climatology; Meteorology; Geography; Paleontology; Thermodynamics; Physics; Medicine","score_opus":0.03175542626855034,"score_gpt":0.26979006231315267,"score_spread":0.23803463604460234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051087195","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95313334,0.017269008,0.0000064947853,0.0026108772,0.0020974,0.000045143912,6.7520676e-7,0.000001956269,0.024835125],"genre_scores_gemma":[0.9944108,0.00071519025,0.0010221892,0.0018644446,0.00013758523,2.4289554e-7,1.9460206e-8,0.0000029082582,0.0018466365],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99929076,0.000015048532,0.00015696042,0.000079439946,0.00020078535,0.00025698822],"domain_scores_gemma":[0.9991662,0.000017846545,0.000075906304,0.00006313069,0.00013408782,0.00054283923],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005311318,0.000059097787,0.0001721744,0.0002285901,0.00017217446,0.0001138469,0.00009290907,0.000019617159,0.00038065788],"category_scores_gemma":[0.00019233274,0.00004148185,0.00007352457,0.0002816469,0.0002970804,0.0003410948,0.000002753019,0.000092943104,0.000024151394],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016876898,0.000028578217,0.9645818,0.000027196746,0.00010340036,0.00055038487,0.00542978,0.000008629016,0.0005802114,0.0100140525,0.008456538,0.010202556],"study_design_scores_gemma":[0.00032015875,0.00023404666,0.3391714,0.00014827293,0.000039803672,0.00015018845,0.0025626572,0.0000023373211,0.0010508084,0.00033604074,0.65591234,0.00007193585],"about_ca_topic_score_codex":0.00059155107,"about_ca_topic_score_gemma":0.014769204,"teacher_disagreement_score":0.6474558,"about_ca_system_score_codex":0.0000034615782,"about_ca_system_score_gemma":0.0017878301,"threshold_uncertainty_score":0.8241563},"labels":[],"label_agreement":null},{"id":"W2051125829","doi":"10.1139/e02-048","title":"An unusual new archosauromorph reptile from the Upper Triassic Wolfville Formation of Nova Scotia","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; University of Toronto","funders":"","keywords":"Geology; Paleontology; Nova scotia; Holotype; Rostrum; Skull; Taxonomy (biology); Biology; Genus; Zoology","score_opus":0.033757582297269266,"score_gpt":0.23191532274711246,"score_spread":0.1981577404498432,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051125829","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99079233,0.0022440017,0.00021334455,0.0008304946,0.0008881022,0.000054279786,0.000058152382,0.0000020659013,0.004917216],"genre_scores_gemma":[0.99804074,0.00001871745,0.0014564472,0.00029479913,0.00013115011,2.986622e-8,0.000010859783,7.951028e-7,0.000046484176],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99884766,0.00025418986,0.00031947106,0.00011855602,0.0001697841,0.00029035716],"domain_scores_gemma":[0.9989645,0.00022642383,0.00024473763,0.00011418258,0.0000686986,0.0003814462],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010096739,0.00007719633,0.00015581265,0.00015167256,0.00028523273,0.00003877491,0.00043081932,0.00006432506,0.00341911],"category_scores_gemma":[0.0002599612,0.0000478259,0.0000593433,0.00033314855,0.00070625293,0.0005787577,0.0000013931412,0.00015470835,0.00005568371],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016253367,0.0000036502402,0.9933628,7.6878473e-7,0.000008099985,0.000012350355,0.0005095998,0.0011265216,0.0000618464,0.00036944516,0.00097651756,0.0035521898],"study_design_scores_gemma":[0.00022428343,0.00041145075,0.98640823,0.000017379667,0.000011020337,0.00019548308,0.00073795515,0.00053975196,0.00018748647,0.0019189679,0.009278434,0.000069531656],"about_ca_topic_score_codex":0.064018324,"about_ca_topic_score_gemma":0.80894107,"teacher_disagreement_score":0.74492276,"about_ca_system_score_codex":0.0000016806615,"about_ca_system_score_gemma":0.0017776074,"threshold_uncertainty_score":0.9974919},"labels":[],"label_agreement":null},{"id":"W2051355872","doi":"10.1139/e00-112","title":"Quaternary stratigraphy and history of the Ootsa Lake - Cheslatta River area, Nechako Plateau, central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"British Geological Survey","keywords":"Geology; Outwash plain; Glacial period; Quaternary; Fluvial; Holocene; Geomorphology; Plateau (mathematics); Pleistocene; Paleontology; Geochemistry","score_opus":0.023783023438516602,"score_gpt":0.19596950439576982,"score_spread":0.17218648095725322,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051355872","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9860501,0.0049228324,0.0000020212524,0.00039647668,0.0007284461,0.0000618705,0.000033634722,0.000001785373,0.0078028077],"genre_scores_gemma":[0.9982002,0.00020404226,0.00013079285,0.00016220375,0.0000390851,9.3919354e-8,0.0000017128616,0.0000010034399,0.0012608799],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988077,0.00012255226,0.00024481182,0.00014234048,0.00023251126,0.00045005255],"domain_scores_gemma":[0.9991379,0.00010232969,0.00016677256,0.00008913072,0.0000691455,0.0004347287],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005938907,0.000066229106,0.00017587988,0.000117962554,0.00033553407,0.0000906068,0.00046030205,0.00008132413,0.0042218193],"category_scores_gemma":[0.00006858999,0.0000611571,0.00007114699,0.00025516545,0.0026362021,0.00027877183,0.0000061687315,0.00026457373,0.0000046211003],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005028033,0.000002159661,0.9970213,0.00000436173,0.0000117183645,0.00021764764,0.0002789105,0.00011824545,0.0000016207242,0.000008787643,0.0014906713,0.0008395205],"study_design_scores_gemma":[0.00015104325,0.0001583136,0.98645556,0.00004122093,0.000008769861,0.001486765,0.00014836085,0.00025882176,0.0000016386052,0.0010590641,0.010160949,0.000069507325],"about_ca_topic_score_codex":0.16984066,"about_ca_topic_score_gemma":0.99417514,"teacher_disagreement_score":0.82433444,"about_ca_system_score_codex":8.5086873e-7,"about_ca_system_score_gemma":0.001478908,"threshold_uncertainty_score":0.9966885},"labels":[],"label_agreement":null},{"id":"W2051734966","doi":"10.1139/e05-018","title":"Electromagnetic images of the Trans-Hudson orogen: the North American Central Plains anomaly revealed","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":94,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Manitoba; Geological Survey of Canada","funders":"","keywords":"Geology; Craton; Kimberlite; Lithosphere; Subduction; Mantle (geology); Magnetotellurics; Crust; Anomaly (physics); Geochemistry; Seismology; Paleontology; Geophysics; Tectonics; Electrical resistivity and conductivity","score_opus":0.010126383720505354,"score_gpt":0.2059601820335406,"score_spread":0.19583379831303524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051734966","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99104595,0.00081734505,0.000034389956,0.0064646993,0.0001791621,0.000095920004,0.000025755984,0.0000024348885,0.0013343428],"genre_scores_gemma":[0.9973269,0.000041138475,0.0017166777,0.00056543073,0.00022328804,1.7487491e-7,4.84344e-7,0.0000017432457,0.00012416118],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99823517,0.00026548692,0.00033223306,0.00014679656,0.00039206984,0.0006282509],"domain_scores_gemma":[0.99878633,0.00025071978,0.0002674441,0.00013445767,0.00008414825,0.00047692514],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00057633023,0.000118341755,0.00022861983,0.000110963374,0.0004728702,0.000082845,0.00088016543,0.000020534922,0.00043573912],"category_scores_gemma":[0.00017438391,0.000057512658,0.00016641732,0.0015063564,0.0009912954,0.00019105694,0.0000035561054,0.00027416204,0.000008998109],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012443193,0.00001021358,0.8772685,0.0000038178828,0.0000151175345,0.000007976314,0.00032660423,0.0032956786,0.0002214035,0.0000486448,0.00022285186,0.11856675],"study_design_scores_gemma":[0.00009081088,0.0007098644,0.9912797,0.000009121147,0.000021688904,0.000059291757,0.00008803928,0.00061198097,0.0008993535,0.00014812531,0.005996934,0.0000850922],"about_ca_topic_score_codex":0.017217608,"about_ca_topic_score_gemma":0.5291907,"teacher_disagreement_score":0.5119731,"about_ca_system_score_codex":0.000002578584,"about_ca_system_score_gemma":0.00096869905,"threshold_uncertainty_score":0.98932683},"labels":[],"label_agreement":null},{"id":"W2051845387","doi":"10.1139/e02-010","title":"Mesoproterozoic lamprophyres in the Labrieville Massif, Quebec: clues to the origin of alkalic anorthosites?","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Geology; Amphibole; Geochemistry; Massif; Dike; Biotite; Anorthosite; Mantle (geology); Incompatible element; Lithosphere; Partial melting; Plagioclase; Paleontology; Tectonics","score_opus":0.02756123235904956,"score_gpt":0.20746152976679938,"score_spread":0.17990029740774982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051845387","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98070455,0.0026892866,0.000007112568,0.012634292,0.00010585388,0.00009017494,0.000015840671,0.0000015007563,0.0037514074],"genre_scores_gemma":[0.9980487,0.000028986105,0.0002790526,0.0012882721,0.00009067416,4.833408e-7,9.95173e-7,7.060706e-7,0.0002620881],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986593,0.00015170347,0.00032198356,0.00013978835,0.00037826248,0.00034894596],"domain_scores_gemma":[0.9991977,0.00017299778,0.00014778101,0.00013067997,0.00007798179,0.0002728393],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009816994,0.00009386793,0.00018951054,0.0002041916,0.00026357724,0.00013030643,0.00088334497,0.000032440716,0.0053779487],"category_scores_gemma":[0.00022304234,0.000040942065,0.00009957189,0.0012712156,0.00047374962,0.00018088413,0.0000066265075,0.0001757754,0.00006699336],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000041055023,0.000007951346,0.9877937,0.0000036918943,0.000009805992,0.000045852878,0.001036459,0.003146882,0.000048531732,0.00018549919,0.00078865146,0.0069289035],"study_design_scores_gemma":[0.0000867195,0.00033642413,0.96058476,0.000030563122,0.000017043258,0.000046625435,0.00089890754,0.0013354843,0.00014291554,0.0017426701,0.03467017,0.00010771002],"about_ca_topic_score_codex":0.23536086,"about_ca_topic_score_gemma":0.9439807,"teacher_disagreement_score":0.70861983,"about_ca_system_score_codex":0.0000012983127,"about_ca_system_score_gemma":0.00015054768,"threshold_uncertainty_score":0.99553126},"labels":[],"label_agreement":null},{"id":"W2052911568","doi":"10.1139/e02-097","title":"Growth patterns and ontogenetic variation of the teeth and jaws of the Middle Jurassic sphenodontian <i>Cynosphenodon huizachalensis</i> (Reptilia: Rhynchocephalia)","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Hatchling; Biology; Anterior teeth; Anatomy; Symphysis; Dentition; Paleontology","score_opus":0.024923588244154866,"score_gpt":0.1894616032433739,"score_spread":0.16453801499921905,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052911568","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9890382,0.006022199,0.00002186638,0.0006790097,0.000534474,0.0000870238,0.00003220454,0.0000011016523,0.0035838783],"genre_scores_gemma":[0.9992036,0.00020696335,0.00028519236,0.000197947,0.000024624045,9.936068e-8,2.1236976e-7,0.0000014101448,0.000079908416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886733,0.00021434836,0.0003073713,0.00013602707,0.0002463368,0.00022857917],"domain_scores_gemma":[0.99910784,0.00011754859,0.0003574437,0.000109616594,0.00012687317,0.00018066961],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006915386,0.00009666375,0.00019370037,0.000076956305,0.00044656606,0.000032274686,0.00026348326,0.00004865298,0.00015726883],"category_scores_gemma":[0.00023179314,0.000054401316,0.00006140352,0.00031708466,0.0010480763,0.00014776136,0.0000074378154,0.00012279252,7.3981886e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000022228219,0.0000027567496,0.99795085,0.000014897259,0.000015057349,0.000001533699,0.0011315761,0.00012585046,0.000028589708,0.00030475328,0.00003836557,0.00038354893],"study_design_scores_gemma":[0.00015664025,0.00011411968,0.99708647,0.00006795044,0.00003501014,0.00009043427,0.0010917563,0.00009566749,0.00014078185,0.0005898371,0.00046988786,0.00006142717],"about_ca_topic_score_codex":0.016674064,"about_ca_topic_score_gemma":0.7158014,"teacher_disagreement_score":0.6991273,"about_ca_system_score_codex":0.0000015662026,"about_ca_system_score_gemma":0.0004444287,"threshold_uncertainty_score":0.989874},"labels":[],"label_agreement":null},{"id":"W2052929306","doi":"10.1139/e04-010","title":"Geology and UPb geochronology of the Kipawa Syenite Complex a thrust related alkaline pluton and adjacent rocks in the Grenville Province of western Quebec","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Geochemistry; Gneiss; Pluton; Anatexis; Zircon; Metasomatism; Geochronology; Titanite; Allochthon; Biotite; Shear zone; Schist; Metamorphic rock; Petrology; Partial melting; Quartz; Nappe; Crust; Mantle (geology); Tectonics; Paleontology","score_opus":0.014741970448358557,"score_gpt":0.19172260413256992,"score_spread":0.17698063368421135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052929306","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921084,0.0017062793,0.0000058488185,0.005488129,0.00004538075,0.00007183579,0.000014103558,7.1878753e-7,0.00055928726],"genre_scores_gemma":[0.99948955,0.000065385546,0.000112058835,0.00028193666,0.000013788056,1.1923655e-7,0.0000017130068,5.5257766e-7,0.0000349002],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99896806,0.00011417897,0.00035582497,0.00013720694,0.00016795211,0.00025679838],"domain_scores_gemma":[0.9993207,0.00012477126,0.00025943143,0.0000870445,0.000055105804,0.00015294163],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005463531,0.00008417718,0.00024086013,0.00013894767,0.00015472219,0.000022340124,0.0003858546,0.000058540812,0.0006234087],"category_scores_gemma":[0.0001111153,0.000040784817,0.00004951645,0.00040863772,0.0017842918,0.0000864777,0.000016910953,0.00018357733,0.0000018800644],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007934681,0.000007748627,0.9914891,0.000007492276,0.000010248686,0.000023382525,0.00037603604,0.006073642,0.0001105195,0.00015740521,0.0000060626444,0.0017304358],"study_design_scores_gemma":[0.0002613165,0.00027981162,0.99369824,0.00003283207,0.0000167044,0.00018584607,0.00048434644,0.0005486729,0.00008521693,0.0037446243,0.0006065085,0.000055897064],"about_ca_topic_score_codex":0.24630457,"about_ca_topic_score_gemma":0.95294505,"teacher_disagreement_score":0.7066405,"about_ca_system_score_codex":0.0000019255137,"about_ca_system_score_gemma":0.000462844,"threshold_uncertainty_score":0.7587144},"labels":[],"label_agreement":null},{"id":"W2052959767","doi":"10.1139/e05-089","title":"Global analyses of brachiopod faunas through the Ordovician and Silurian transition: reducing the role of the Lazarus effect","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Chinese Academy of Sciences; Smithsonian Institution","keywords":"Ordovician; Paleontology; Extinction event; Geology; Taxon; Fauna; Taphonomy; Population; Extinction (optical mineralogy); Range (aeronautics); Ecology; Biology; Biological dispersal; Demography","score_opus":0.013361063225455874,"score_gpt":0.23780493425605068,"score_spread":0.2244438710305948,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052959767","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94404906,0.018946957,0.000010685466,0.0016111534,0.00018340089,0.000081817416,0.00005036162,0.0000012353796,0.035065353],"genre_scores_gemma":[0.99969685,0.000018459146,0.00012954789,0.00007509724,0.000074659256,1.1059897e-7,3.5448468e-7,3.5797538e-7,0.0000045659035],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988144,0.00027523053,0.00030297806,0.00010720522,0.00025998743,0.00024021386],"domain_scores_gemma":[0.999208,0.0002366143,0.00028045452,0.00012414652,0.00005144982,0.00009936894],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008196235,0.0000928418,0.00018820632,0.00006113091,0.0008127989,0.00006930564,0.0005225812,0.000044964516,0.00007014559],"category_scores_gemma":[0.0000555773,0.000040063034,0.00013474766,0.0006430287,0.0020132626,0.0002437418,0.0000011932096,0.00013711923,3.1444736e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000120339955,0.0000032615053,0.9812037,0.0000050687886,0.000028608674,0.0000067145215,0.00060369406,0.0039390293,0.00008347802,0.0009763647,0.00002318687,0.013114889],"study_design_scores_gemma":[0.00010151744,0.00022832683,0.99271727,0.000040436476,0.000049138525,0.00015579702,0.0009290079,0.00030296494,0.00048155364,0.004608751,0.00033586725,0.000049389175],"about_ca_topic_score_codex":0.11509704,"about_ca_topic_score_gemma":0.7377183,"teacher_disagreement_score":0.62262124,"about_ca_system_score_codex":8.2345747e-7,"about_ca_system_score_gemma":0.00051295926,"threshold_uncertainty_score":0.8907956},"labels":[],"label_agreement":null},{"id":"W2053430433","doi":"10.1139/e05-041","title":"A new genus of rhizodontid (Sarcopterygii, Tetrapodomorpha) from the Lower Carboniferous Horton Bluff Formation of Nova Scotia, and the evolution of the lower jaws in this group","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Genus; Geology; Paleontology; Carboniferous; Anatomy; Biology; Zoology","score_opus":0.011294631554449553,"score_gpt":0.19097057726033756,"score_spread":0.17967594570588802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053430433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98544246,0.0102665825,0.000081914586,0.0017553214,0.000655369,0.00012846562,0.00005064618,8.228318e-7,0.0016184177],"genre_scores_gemma":[0.99930024,0.000081310434,0.00036377326,0.00013265293,0.00009397739,9.576433e-8,0.0000017790649,8.9193503e-7,0.000025278658],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99870074,0.00023053375,0.000472763,0.000112777256,0.00024154855,0.00024163943],"domain_scores_gemma":[0.99888027,0.00033921323,0.00044442352,0.00014040801,0.0000785944,0.00011712168],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012765129,0.000090342575,0.00023335464,0.00015198249,0.00017020741,0.000016209331,0.00052648736,0.00007934241,0.00050258334],"category_scores_gemma":[0.00015580274,0.00004440079,0.00008851178,0.0004270199,0.0017530319,0.0003635413,0.000008578967,0.00019811884,0.0000036029992],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011775938,0.000010010187,0.9930241,0.0000031518334,0.000014798757,0.0000037072891,0.0008677764,0.0010935871,0.00007463486,0.00022300467,0.00018128156,0.004386161],"study_design_scores_gemma":[0.00052454084,0.0003318338,0.9953614,0.000068916386,0.000023157629,0.000102905105,0.0004593902,0.0017951496,0.000090356276,0.0006166688,0.00057020865,0.00005549536],"about_ca_topic_score_codex":0.2861127,"about_ca_topic_score_gemma":0.9484808,"teacher_disagreement_score":0.66236806,"about_ca_system_score_codex":0.000006722956,"about_ca_system_score_gemma":0.000803761,"threshold_uncertainty_score":0.7186411},"labels":[],"label_agreement":null},{"id":"W2053608596","doi":"10.1139/e07-033","title":"McMurray Formation foraminifera within the lower Albian (Lower Cretaceous) Loon River shales of northern Alberta","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"BP (Canada); University of Calgary; University of Alberta","funders":"","keywords":"Geology; Microfauna; Paleontology; Foraminifera; Cretaceous; Outcrop; Biostratigraphy; Ecological succession; Oceanography; Ecology; Fauna","score_opus":0.018650682749788705,"score_gpt":0.21012168712288112,"score_spread":0.19147100437309242,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053608596","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9867171,0.00079705263,0.00031600823,0.00085316127,0.00058009784,0.00008552706,0.00001790026,0.0000024683638,0.010630685],"genre_scores_gemma":[0.99866563,0.00001826322,0.0006611424,0.0003668106,0.00008003355,9.460917e-8,0.0000041526882,0.0000014313338,0.00020245125],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986487,0.0000433338,0.0004974833,0.000102448386,0.000357277,0.00035073026],"domain_scores_gemma":[0.99858785,0.0002996116,0.0004118805,0.0001059798,0.00025145628,0.0003432121],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016468985,0.00010802702,0.00015950021,0.00023179158,0.00051213696,0.00012974645,0.00053483684,0.000060605667,0.0014243734],"category_scores_gemma":[0.00030664305,0.00005961272,0.00008478155,0.0005486663,0.0007671494,0.00091570255,0.000004740661,0.00016472705,0.00006126999],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037855996,0.000015391352,0.9688845,0.00002209902,0.000018095589,0.000037462287,0.0035742493,0.014287949,0.000009771005,0.00046861684,0.00015713033,0.012486851],"study_design_scores_gemma":[0.00019961092,0.0011420917,0.96597975,0.00008466029,0.000023810811,0.00024375043,0.0022668021,0.0030161862,0.00029040923,0.0026782844,0.023875032,0.00019959529],"about_ca_topic_score_codex":0.016139075,"about_ca_topic_score_gemma":0.8425401,"teacher_disagreement_score":0.82640105,"about_ca_system_score_codex":0.0000021592634,"about_ca_system_score_gemma":0.0006009774,"threshold_uncertainty_score":0.9994885},"labels":[],"label_agreement":null},{"id":"W2053630273","doi":"10.1139/e05-076","title":"Rostral structure in Thalattosauria (Reptilia, Diapsida)","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"College of Family Physicians of Canada","funders":"","keywords":"Premaxilla; Geology; Holotype; Rostrum; Anatomy; Vomer; Paleontology; Maxilla; Biology; Genus","score_opus":0.014499487079624599,"score_gpt":0.21177804470117634,"score_spread":0.19727855762155175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053630273","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98802805,0.0031580797,0.00000299549,0.0016034628,0.00065497437,0.00003394538,0.000043223456,0.0000023246514,0.0064729163],"genre_scores_gemma":[0.9981039,0.000025096904,0.001191628,0.00034266338,0.000253884,4.157845e-8,0.000003818439,7.047429e-7,0.00007822084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989407,0.00008177255,0.00026114532,0.00013821518,0.00013333114,0.0004448102],"domain_scores_gemma":[0.9993302,0.00007569062,0.00011221067,0.00006246844,0.000035161553,0.00038424018],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047842937,0.00008568027,0.00015505891,0.00033620262,0.00021925803,0.0000341471,0.00036633585,0.000096155985,0.0052617933],"category_scores_gemma":[0.0000879515,0.000064606924,0.000046371137,0.00032357877,0.00065295416,0.00045944608,0.0000018872634,0.00023925761,0.000051880186],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006338537,0.0000014957367,0.98799884,8.4569547e-7,0.0000032133714,0.000059365404,0.00015163168,0.004752371,0.000020953665,0.00010078874,0.00014176586,0.006762392],"study_design_scores_gemma":[0.00013649117,0.00015119981,0.98754567,0.000011194959,0.000002753938,0.00040980105,0.0001138976,0.0010751785,0.000030277899,0.000979497,0.009463917,0.00008011526],"about_ca_topic_score_codex":0.007425185,"about_ca_topic_score_gemma":0.92386866,"teacher_disagreement_score":0.91644347,"about_ca_system_score_codex":0.0000020840464,"about_ca_system_score_gemma":0.0010360932,"threshold_uncertainty_score":0.9991844},"labels":[],"label_agreement":null},{"id":"W2053815004","doi":"10.1139/e99-123","title":"Crustal evolution along a seismic section across the Grenville Province (western Quebec)","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University; University of British Columbia; Simon Fraser University; Université de Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Archean; Crust; Terrane; Proterozoic; Geochemistry; Orogeny; Mantle (geology); Continental crust; Paleontology; Seismology; Tectonics","score_opus":0.011115827511811298,"score_gpt":0.19596887800939733,"score_spread":0.18485305049758602,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053815004","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99404556,0.0008067716,0.000041440588,0.0024809302,0.00022723044,0.000051223138,0.000021029351,0.0000040727136,0.0023217688],"genre_scores_gemma":[0.9980153,0.000015819494,0.000058632417,0.00046741968,0.00025122977,1.5446086e-7,0.0000024168537,8.4041915e-7,0.0011881904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998755,0.000079176505,0.00026482673,0.00016370747,0.00029238,0.00044494247],"domain_scores_gemma":[0.99926007,0.00007080739,0.0001235566,0.0000830745,0.000068424175,0.0003940658],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000667342,0.000096345946,0.00014004821,0.00007626742,0.0007881365,0.00021107247,0.00042138514,0.0000664843,0.0064453124],"category_scores_gemma":[0.00006352185,0.000052786047,0.000107636864,0.0005273049,0.0007129042,0.0003443693,0.0000039085867,0.0002791116,0.00013382171],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000832013,0.000003335968,0.9523521,0.0000018236763,0.000008769268,0.000035715493,0.00019014918,0.028075889,0.000014777821,0.000009914657,0.00010783169,0.019191338],"study_design_scores_gemma":[0.000083621475,0.00015499287,0.978756,0.000014367542,0.00001172767,0.00018114653,0.00038187145,0.004744958,0.000034608827,0.001005353,0.014536027,0.00009529386],"about_ca_topic_score_codex":0.44073516,"about_ca_topic_score_gemma":0.9817728,"teacher_disagreement_score":0.5410376,"about_ca_system_score_codex":0.000004189663,"about_ca_system_score_gemma":0.000703889,"threshold_uncertainty_score":0.9944629},"labels":[],"label_agreement":null},{"id":"W2053968034","doi":"10.1139/e04-029","title":"Chemical variation in Al<sub>2</sub>O<sub>3</sub>CaONa<sub>2</sub>OK<sub>2</sub>O space: controls on the peraluminosity of the South Mountain Batholith","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Technical University of Nova Scotia; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Killam Trusts; Dalhousie University","keywords":"Batholith; Geology; Muscovite; Plagioclase; Mineralogy; Geochemistry; Fractionation; Chemical composition; Alkali feldspar; Feldspar; Analytical Chemistry (journal); Quartz; Chemistry","score_opus":0.011336865676293885,"score_gpt":0.18173622554616678,"score_spread":0.1703993598698729,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053968034","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9883345,0.0004835693,0.000036619123,0.009699048,0.0004111767,0.00039419282,0.00018631037,0.000015956884,0.0004386347],"genre_scores_gemma":[0.99666524,0.00011647353,0.00009063203,0.0027650695,0.0003252782,0.0000043329255,0.000018896024,0.0000095348505,0.000004546668],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99466676,0.0005063342,0.0011626399,0.0007704373,0.0015078742,0.0013859554],"domain_scores_gemma":[0.99646544,0.0006364098,0.0008854165,0.0004744633,0.00038775383,0.0011505303],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0029582886,0.0005331859,0.00086148735,0.0005136245,0.0009416747,0.00034750838,0.001480479,0.00027891292,0.00018797006],"category_scores_gemma":[0.001338246,0.00031934332,0.00055930176,0.0021739348,0.0018709544,0.00057879224,0.000059311897,0.0011642257,0.0001194504],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001350463,0.00010356806,0.2773624,0.000023937542,0.000102039645,0.00013516164,0.001409953,0.021915462,0.69356424,0.000670849,0.0001959299,0.004381434],"study_design_scores_gemma":[0.0008205001,0.00036681967,0.563039,0.0001677182,0.00009931583,0.00011056915,0.00059555355,0.0018387203,0.4245657,0.007833375,0.00011069311,0.00045201698],"about_ca_topic_score_codex":0.0054400237,"about_ca_topic_score_gemma":0.1444393,"teacher_disagreement_score":0.28567663,"about_ca_system_score_codex":0.000057095465,"about_ca_system_score_gemma":0.0017296573,"threshold_uncertainty_score":0.99992585},"labels":[],"label_agreement":null},{"id":"W2053992285","doi":"10.1139/e01-086","title":"The lower Proterozoic Fern Creek Formation, northern Michigan: mineral and bulk geochemical evidence for its glaciogenic origin","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Archean; Geochemistry; Proterozoic; Fern; Terrane; Gneiss; Provenance; Mineral; Weathering; Charnockite; Arenite; Sedimentary rock; Paleontology; Granulite; Clastic rock; Metamorphic rock","score_opus":0.04398139914295897,"score_gpt":0.23054744457515053,"score_spread":0.18656604543219157,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053992285","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920836,0.0047332165,0.000017992921,0.0025582386,0.00017070238,0.000115743715,0.000030307168,0.0000022770905,0.00028789433],"genre_scores_gemma":[0.998722,0.000100443125,0.00023819087,0.00015626465,0.00016055765,0.0000010183743,0.000003306434,0.0000012628363,0.00061694783],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99889416,0.000027995939,0.00029612624,0.00014387962,0.0002491149,0.00038871396],"domain_scores_gemma":[0.9990058,0.00017851432,0.00016524733,0.00007845814,0.00014445299,0.00042751673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006163029,0.00009681227,0.00012409792,0.00006736493,0.0008869065,0.00035639395,0.00038343633,0.000034029137,0.000858948],"category_scores_gemma":[0.00027548915,0.00006439329,0.00008663642,0.000266086,0.00032655857,0.0005853241,0.000004527038,0.00010217778,0.000026181402],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044991935,0.000013926556,0.9797776,0.00004449689,0.000057674122,0.00004202823,0.0009280052,0.0011995002,0.0013152758,0.0000150627375,0.0015684719,0.014992973],"study_design_scores_gemma":[0.0027602438,0.0053330567,0.50801474,0.00093973865,0.00046641508,0.0033799016,0.00523594,0.1883581,0.013411748,0.0037767554,0.26623854,0.002084844],"about_ca_topic_score_codex":0.002820355,"about_ca_topic_score_gemma":0.60413736,"teacher_disagreement_score":0.60131705,"about_ca_system_score_codex":0.0000022695829,"about_ca_system_score_gemma":0.00019109002,"threshold_uncertainty_score":0.9404878},"labels":[],"label_agreement":null},{"id":"W2054022285","doi":"10.1139/e00-098","title":"Sequence stratigraphy, biotic change, <sup>87</sup>Sr/<sup>86</sup>Sr record, paleoclimatic history, and sedimentation rate change across a regional late Cenozoic unconformity in Arctic Canada","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Unconformity; Paleontology; Tectonic uplift; Foraminifera; Cenozoic; Late Miocene; Tectonics; Structural basin; Oceanography; Benthic zone","score_opus":0.08982727073270419,"score_gpt":0.2390712226413775,"score_spread":0.14924395190867332,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054022285","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9917405,0.003540465,0.000004877218,0.0037657463,0.00033442592,0.00025889347,0.00004757516,0.000005436688,0.0003020329],"genre_scores_gemma":[0.9963446,0.0015085742,0.00020556705,0.0016825664,0.0001797649,0.0000032256653,0.00002082129,0.0000027374995,0.000052105133],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99780047,0.00015662609,0.00051119144,0.00031052573,0.00043660656,0.00078455504],"domain_scores_gemma":[0.99859965,0.00016245672,0.00032371396,0.00010320937,0.00013453381,0.0006764576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011140323,0.00021598369,0.000321936,0.00025372,0.0006071277,0.00015316531,0.00031342087,0.00007679714,0.0006096637],"category_scores_gemma":[0.00012401295,0.0001697706,0.00005831884,0.0007148254,0.0006227797,0.0011780409,0.00000928684,0.00026497353,0.000011506155],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019754516,0.0000056677563,0.98466206,0.000026947408,0.000011409546,0.00020184722,0.0026614945,0.0029294973,0.0000019303939,0.000027317137,0.00012703147,0.00932506],"study_design_scores_gemma":[0.00038350272,0.0005001375,0.96344465,0.00015192346,0.00001464199,0.0001631984,0.00403626,0.023284042,0.0000012992828,0.0006246382,0.007138804,0.00025691724],"about_ca_topic_score_codex":0.8305143,"about_ca_topic_score_gemma":0.9971708,"teacher_disagreement_score":0.16665646,"about_ca_system_score_codex":0.000047084635,"about_ca_system_score_gemma":0.0011443766,"threshold_uncertainty_score":0.69230443},"labels":[],"label_agreement":null},{"id":"W2054125042","doi":"10.1139/e99-111","title":"The Midway sequence: a Timiskaming-type, pull-apart basin deposit in the western Wawa subprovince, Minnesota","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Conglomerate; Archean; Clastic rock; Volcanic rock; Unconformity; Greenstone belt; Pyroclastic rock; Transpression; Siliciclastic; Tectonite; Syncline; Sequence (biology); Petrology; Sedimentary rock; Volcano; Geomorphology; Shear zone; Structural basin; Tectonics; Paleontology; Facies","score_opus":0.021415153244120605,"score_gpt":0.20734637694627037,"score_spread":0.18593122370214976,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054125042","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9786887,0.0018460734,0.0000013462345,0.008897844,0.0001526904,0.00006930745,0.000009865457,0.0000025884035,0.010331573],"genre_scores_gemma":[0.99676394,0.00019531065,0.00014308462,0.0020617272,0.0001117814,3.2417717e-7,0.000003161943,0.000001053967,0.00071960466],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998215,0.00019308469,0.00038076742,0.00019572605,0.0004301726,0.00058522815],"domain_scores_gemma":[0.998903,0.0003598414,0.000122061094,0.00015047063,0.00007915251,0.0003855207],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015724807,0.0001276926,0.00018996792,0.00012186698,0.00077005115,0.00037161185,0.0011585675,0.000053925214,0.0038219113],"category_scores_gemma":[0.00017558798,0.000058356345,0.00010178525,0.0011514944,0.0008966569,0.00031439002,0.000004381774,0.00029061412,0.0001678043],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012370734,0.0000052646824,0.98452926,0.0000019133413,0.0000073657184,0.00016464634,0.00020873042,0.0016900799,0.000012101721,0.00002242655,0.0004148335,0.012931021],"study_design_scores_gemma":[0.000107700216,0.00026920185,0.9207576,0.000029288467,0.000018256787,0.00034588896,0.00035078468,0.0014096969,0.0000606528,0.0018612375,0.07465035,0.00013937458],"about_ca_topic_score_codex":0.06586042,"about_ca_topic_score_gemma":0.7459231,"teacher_disagreement_score":0.6800627,"about_ca_system_score_codex":0.0000023481807,"about_ca_system_score_gemma":0.00051191566,"threshold_uncertainty_score":0.99708873},"labels":[],"label_agreement":null},{"id":"W2054223715","doi":"10.1139/e01-071","title":"Map symbology and analysis of box and polyclinal folds, with examples from the Rocky Mountain Foothills of northeastern British Columbia and the Liard Ranges of southeastern Yukon Territory and southwestern Northwest Territories","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Petro-Canada; BP (Canada); Geological Survey of Canada","funders":"","keywords":"Foothills; Geology; Fold (higher-order function); Hinge; Paleontology; Geologic map; Archaeology; Geomorphology; Cartography; Geography","score_opus":0.014344320764236465,"score_gpt":0.19347852947493852,"score_spread":0.17913420871070204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054223715","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9854966,0.01317925,0.000005555362,0.0006374936,0.00007462985,0.000099702054,0.0004569682,0.0000010823472,0.00004873771],"genre_scores_gemma":[0.999428,0.00030285303,0.00012126124,0.00005576533,0.000043725435,4.3118368e-7,0.0000075430767,0.0000019377633,0.00003850507],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99859965,0.00030388424,0.00037943185,0.00020404776,0.000233362,0.00027962885],"domain_scores_gemma":[0.99834555,0.0008704767,0.00033902936,0.0001152306,0.00010009016,0.00022961253],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00085585937,0.00010425208,0.00049878843,0.00016389179,0.0005114143,0.00020182587,0.0002777494,0.000074326046,0.00012588786],"category_scores_gemma":[0.000050711416,0.000071795585,0.000048803737,0.00021373839,0.005738945,0.00016767666,0.000016277754,0.00017491721,2.5894795e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005221784,0.0000042025067,0.9961301,0.000019032494,0.00018178433,0.000025519434,0.0026000156,0.000029904173,0.0000021946175,0.0000055747887,0.000002681163,0.00094673585],"study_design_scores_gemma":[0.0005836749,0.00041376145,0.9932051,0.00007876725,0.00023270935,0.00030840866,0.0043553906,0.000505507,0.0000036766785,0.00016109757,0.000076887576,0.00007506444],"about_ca_topic_score_codex":0.6074879,"about_ca_topic_score_gemma":0.99738926,"teacher_disagreement_score":0.38990134,"about_ca_system_score_codex":2.1215462e-7,"about_ca_system_score_gemma":0.00013931,"threshold_uncertainty_score":0.99696684},"labels":[],"label_agreement":null},{"id":"W2054246584","doi":"10.1139/e09-009","title":"Deep electrical structure of northern Alberta (Canada): implications for diamond exploration","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta; Western Canada Research Grid","keywords":"Geology; Kimberlite; Asthenosphere; Mantle (geology); Magnetotellurics; Lithosphere; Terrane; Subduction; Craton; Crust; Geochemistry; Diamond; Petrology; Geophysics; Paleontology; Electrical resistivity and conductivity; Tectonics","score_opus":0.017994438127207812,"score_gpt":0.23088705883367253,"score_spread":0.21289262070646472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054246584","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98647046,0.00074527966,0.003691376,0.007333572,0.00030013476,0.00018040907,0.00006253588,0.0000022342351,0.0012139821],"genre_scores_gemma":[0.9956418,0.000005819749,0.003849552,0.0003315831,0.00012714871,1.2482175e-7,0.0000060465177,0.0000010161039,0.000036883466],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9990119,0.000048065343,0.00028866023,0.00012743867,0.00019180702,0.0003321324],"domain_scores_gemma":[0.9987328,0.00033341217,0.00019747634,0.000074653544,0.00019933924,0.00046229744],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018625653,0.000083812105,0.00018354166,0.00014772631,0.0002622091,0.000049106657,0.00033230928,0.000039137405,0.0001547768],"category_scores_gemma":[0.00042665374,0.00005998027,0.0000679584,0.0007238363,0.00011606098,0.00026984687,9.153785e-7,0.00010805417,0.0000012820535],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031668118,0.000015649202,0.36927113,0.0000070872793,0.000020114265,0.0000043910386,0.00025690958,0.018514333,0.0006599515,0.0030378453,0.0004047096,0.6077762],"study_design_scores_gemma":[0.00010965885,0.0007993185,0.95463836,0.0000062713616,0.0000132159,0.00001749749,0.00003260358,0.0033098315,0.00060049165,0.037901428,0.002473452,0.00009784265],"about_ca_topic_score_codex":0.3139976,"about_ca_topic_score_gemma":0.9939511,"teacher_disagreement_score":0.6799535,"about_ca_system_score_codex":0.0000030058552,"about_ca_system_score_gemma":0.0019789287,"threshold_uncertainty_score":0.69057053},"labels":[],"label_agreement":null},{"id":"W2054701321","doi":"10.1139/e05-111","title":"Geochemical, <sup>40</sup>Ar/<sup>39</sup>Ar age, and isotopic data for crustal rocks of the Neyriz ophiolite, Iran","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Georgia State University","keywords":"Ophiolite; Geology; Basalt; Geochemistry; Metamorphism; Hornblende; Gabbro; Island arc; Pillow lava; Subduction; Volcanic rock; Paleontology; Biotite; Quartz","score_opus":0.029777140002775714,"score_gpt":0.21401755870826344,"score_spread":0.18424041870548774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054701321","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921326,0.0018954511,0.000037778973,0.0023513685,0.00009122173,0.00014376488,0.00046885497,0.000004625877,0.0028743376],"genre_scores_gemma":[0.99780184,0.000037677375,0.0010030022,0.0004320828,0.0002986126,4.982348e-7,0.00005633605,0.0000024441395,0.0003675211],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978893,0.00007758012,0.00057287345,0.00039065455,0.00043002318,0.00063960766],"domain_scores_gemma":[0.99835706,0.00028720658,0.0002767578,0.00033743226,0.00014278614,0.0005987743],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007565009,0.00019731904,0.00040125792,0.0001914942,0.000551023,0.000193035,0.0014360389,0.00011110255,0.0015981795],"category_scores_gemma":[0.00047167175,0.00011685345,0.00018047672,0.00071074476,0.0012821523,0.00042255636,0.000054174845,0.00026470152,0.000008177735],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028463532,0.000023905583,0.96784264,0.00003635003,0.00004456694,0.00005654649,0.0001743222,0.024624273,0.00019844674,0.00014946182,0.004048997,0.0027720036],"study_design_scores_gemma":[0.00086448964,0.0006005734,0.82638913,0.00013616607,0.00019044665,0.0002439683,0.001102695,0.07126262,0.00069246127,0.029267196,0.068692036,0.0005581933],"about_ca_topic_score_codex":0.042276904,"about_ca_topic_score_gemma":0.14955142,"teacher_disagreement_score":0.1414535,"about_ca_system_score_codex":0.0000024734584,"about_ca_system_score_gemma":0.00047184588,"threshold_uncertainty_score":0.9993145},"labels":[],"label_agreement":null},{"id":"W2054734224","doi":"10.1139/e05-110","title":"Provenance of fossiliferous clasts in Carboniferous conglomerate, Isle Madame, southern Cape Breton Island, Nova Scotia","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University; Government of Newfoundland and Labrador","funders":"Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Conglomerate; Geology; Carboniferous; Siltstone; Clastic rock; Paleozoic; Devonian; Paleontology; Provenance; Ordovician; Terrane; Nova scotia; Breccia; Paleocurrent; Laurentia; Facies; Sedimentary rock","score_opus":0.01250884297080878,"score_gpt":0.18796375854763758,"score_spread":0.1754549155768288,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054734224","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98660755,0.0023202398,0.000004788585,0.00044652983,0.00036734543,0.00008780533,0.00007238601,0.0000026859766,0.010090658],"genre_scores_gemma":[0.99915797,0.000010811626,0.00015602358,0.00010422309,0.00013282734,1.2145418e-7,0.0000021783428,0.0000015616282,0.00043426262],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984538,0.00006223042,0.00045015823,0.00019739453,0.00031570735,0.00052068796],"domain_scores_gemma":[0.999195,0.00010431961,0.0002524445,0.00007517393,0.00013001275,0.00024304377],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041987555,0.00014040348,0.00034018717,0.00018670764,0.00015278964,0.00007190899,0.0003522048,0.00005902062,0.0006813931],"category_scores_gemma":[0.00008482324,0.00009320941,0.000078360856,0.0006967107,0.0008366734,0.00019410196,0.0000066167895,0.00019120473,0.00010247364],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013574658,0.000012121526,0.99075854,0.000008539864,0.000005658888,0.000086224565,0.00018633896,0.0061029834,0.000030898547,0.00007130509,0.00008451786,0.0026392739],"study_design_scores_gemma":[0.00027627958,0.0005110381,0.99503964,0.000059162358,0.000006380856,0.00004822411,0.00037201372,0.00041976623,0.000117735784,0.0021530255,0.0008586291,0.00013811326],"about_ca_topic_score_codex":0.3655683,"about_ca_topic_score_gemma":0.9579772,"teacher_disagreement_score":0.5924089,"about_ca_system_score_codex":0.0000025313802,"about_ca_system_score_gemma":0.0005674506,"threshold_uncertainty_score":0.74607766},"labels":[],"label_agreement":null},{"id":"W2055061327","doi":"10.1139/e06-027","title":"Imaging the upper part of the Red Lake greenstone belt, northwestern Ontario, with 3-D traveltime tomography","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Greenstone belt; Archean; Fault (geology); Seismology; Shear zone; Unconformity; Inversion (geology); Paleontology; Geomorphology; Tectonics","score_opus":0.0078043413426699135,"score_gpt":0.159223723281647,"score_spread":0.15141938193897708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055061327","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.990119,0.0004895532,0.00000566123,0.0026632564,0.00013366142,0.000050792736,0.00002839683,0.0000018300108,0.0065078465],"genre_scores_gemma":[0.99905246,0.0000027319115,0.00021505113,0.00029555755,0.00007759493,1.3707968e-7,0.0000041327094,9.2038835e-7,0.00035139255],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99876326,0.000058102334,0.0003008933,0.00014216114,0.00038496472,0.0003505941],"domain_scores_gemma":[0.99920833,0.000075788936,0.00024090124,0.00012958024,0.00011789633,0.00022752432],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003968883,0.00010623992,0.00017963034,0.00012359097,0.00044838892,0.00008321648,0.0005974148,0.000023510362,0.0038695482],"category_scores_gemma":[0.00001412706,0.000043607033,0.00016626877,0.000778702,0.0012761307,0.00016989668,0.0000061104897,0.00019216485,0.0000052238065],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004864576,0.0000036580193,0.99717367,0.000001023219,0.000011604016,0.00002105296,0.00011659914,0.0015967359,0.000011192313,0.000020578,0.00008914034,0.00094990747],"study_design_scores_gemma":[0.00009343155,0.000089289286,0.99225295,0.000026183556,0.00003501098,0.00013198123,0.00014923674,0.00015113376,0.00007641013,0.0014103998,0.0055064666,0.0000775023],"about_ca_topic_score_codex":0.6419215,"about_ca_topic_score_gemma":0.99896246,"teacher_disagreement_score":0.35704094,"about_ca_system_score_codex":0.000001114832,"about_ca_system_score_gemma":0.0005251514,"threshold_uncertainty_score":0.99704105},"labels":[],"label_agreement":null},{"id":"W2055454765","doi":"10.1139/e06-100","title":"Late Ordovician - Early Silurian cryptospore occurrences on Anticosti Island (Île d'Anticosti), Quebec, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ordovician; Geology; Paleontology; Bay; Assemblage (archaeology); Glacial period; Oceanography","score_opus":0.01959074837896009,"score_gpt":0.23360716360950787,"score_spread":0.21401641523054776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055454765","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9845378,0.0010832163,0.000014894764,0.0027070236,0.001681389,0.000098228054,0.000051435512,0.0000050979434,0.00982094],"genre_scores_gemma":[0.99832875,0.000030082172,0.00019077839,0.000771748,0.00019028959,8.933266e-8,0.0000084132025,0.0000026282862,0.00047721918],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973937,0.00013109794,0.0004840618,0.00028570165,0.00057820266,0.0011272298],"domain_scores_gemma":[0.9976619,0.0005254311,0.00025609753,0.00015600167,0.00018738274,0.0012131698],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018038929,0.00019452622,0.0003232496,0.0005785122,0.0009637379,0.0001875227,0.0008143323,0.0001287646,0.0024315123],"category_scores_gemma":[0.0003830049,0.00014745448,0.00007400736,0.00078673195,0.0010728635,0.00037680296,0.0000063892185,0.00055605674,0.00012262305],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003100876,0.000004820793,0.99611944,0.0000060014067,0.00001607056,0.00094801234,0.00017654007,0.00064865994,0.0000019934482,0.000119845565,0.00061388983,0.0013136902],"study_design_scores_gemma":[0.00022583286,0.00037008902,0.98633933,0.000064915555,0.000011089471,0.00017208821,0.00029786138,0.00016207591,0.00005376058,0.00031196408,0.011806506,0.00018451198],"about_ca_topic_score_codex":0.8973271,"about_ca_topic_score_gemma":0.99995005,"teacher_disagreement_score":0.102622904,"about_ca_system_score_codex":0.0000027920996,"about_ca_system_score_gemma":0.0066092913,"threshold_uncertainty_score":0.9990223},"labels":[],"label_agreement":null},{"id":"W2055685507","doi":"10.1139/e08-029","title":"Elusive isotopic properties of deglacial meltwater spikes into the North Atlantic: example of the final drainage of Lake AgassizThis article is one of a series of papers published in the Special Issue on the theme <i>Polar Climate Stability Network</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Centre de Géomatique du Québec; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; University of Waterloo; Fonds Québécois de la Recherche sur la Nature et les Technologies; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Geology; Meltwater; Varve; Oceanography; Ostracod; Holocene; Glacial period; Salinity; Bay; Paleontology; Sediment","score_opus":0.04424662094728614,"score_gpt":0.2071382616665492,"score_spread":0.16289164071926304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055685507","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99225783,0.00031660032,2.3697574e-7,0.0046175984,0.00018829163,0.00024079054,0.000033737244,6.419631e-7,0.0023442707],"genre_scores_gemma":[0.99950695,0.000076178985,0.000043487937,0.00018902919,0.00015696906,8.510091e-7,0.0000011635929,0.0000013902999,0.000023974597],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976577,0.00066638924,0.0006065018,0.00014234782,0.00052268856,0.00040433108],"domain_scores_gemma":[0.9984634,0.00045629698,0.00049010414,0.00027800072,0.0002316323,0.000080549464],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0027334965,0.00010913453,0.00035093352,0.00011384446,0.0004965779,0.000024486406,0.0010671348,0.000060699727,0.00228474],"category_scores_gemma":[0.0004523375,0.000044808083,0.00012226377,0.0007191272,0.005166505,0.00024358316,0.000028848775,0.00030957823,0.0000018910006],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012076024,0.000021259983,0.9825342,0.00003605723,0.000018748588,0.0000068416075,0.016325133,0.0003994591,0.00010190118,0.00025835106,0.00007344192,0.00010382545],"study_design_scores_gemma":[0.0001734714,0.0004687381,0.989966,0.00007009196,0.000016558773,0.000035735076,0.0033570072,0.000060189166,0.0041788123,0.00064421876,0.0009775162,0.00005169602],"about_ca_topic_score_codex":0.017874917,"about_ca_topic_score_gemma":0.81243134,"teacher_disagreement_score":0.7945564,"about_ca_system_score_codex":9.924352e-7,"about_ca_system_score_gemma":0.00082625344,"threshold_uncertainty_score":0.9986273},"labels":[],"label_agreement":null},{"id":"W2056002148","doi":"10.1139/e06-074","title":"Geochemical and metallogenic relations in volcanic rocks of the southern Slave Province: implications for late Neoarchean tectonics","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Craton; Geochemistry; Subduction; Archean; Volcanic belt; Mantle (geology); Mantle wedge; Volcanic arc; Greenstone belt; Slab window; Tectonics; Volcanic rock; Earth science; Volcano; Paleontology; Oceanic crust","score_opus":0.013191370360435401,"score_gpt":0.19415714873464318,"score_spread":0.18096577837420777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056002148","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948171,0.0010292256,0.000059766197,0.0030767382,0.0000302061,0.000091906666,0.00008496815,0.0000013243751,0.0008087672],"genre_scores_gemma":[0.9991135,0.000005954344,0.00061161316,0.000065346685,0.000027829275,4.7007032e-7,0.000004304174,8.14306e-7,0.00017017865],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991826,0.000034729423,0.00030079705,0.00012503177,0.00011050227,0.00024635825],"domain_scores_gemma":[0.9993502,0.00016247114,0.00016706082,0.00007482974,0.00008257701,0.00016289008],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004351713,0.00006671312,0.00014782888,0.00012108938,0.00022341571,0.000033027292,0.00029515263,0.000045957622,0.00029550452],"category_scores_gemma":[0.00018184158,0.00003896841,0.00010259174,0.0004631949,0.0005256868,0.00008387957,0.0000069201365,0.00013100728,0.0000023941054],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000025027293,0.0000040164086,0.9930471,0.000002536215,0.000005919708,6.911451e-7,0.000047895566,0.0053604236,0.00057603774,0.0002144124,0.000019628163,0.0007187904],"study_design_scores_gemma":[0.00012594413,0.000074082964,0.93581,0.000012409197,0.0000285634,0.000019431649,0.00010782868,0.0032633203,0.0003699681,0.05962262,0.0004994896,0.00006630282],"about_ca_topic_score_codex":0.038228385,"about_ca_topic_score_gemma":0.83308715,"teacher_disagreement_score":0.79485875,"about_ca_system_score_codex":0.0000022203553,"about_ca_system_score_gemma":0.0006750249,"threshold_uncertainty_score":0.9681761},"labels":[],"label_agreement":null},{"id":"W2056062658","doi":"10.1139/e99-110","title":"Large-scale effects of subglacial meltwater flow in the southern Slave Province, Northwest Territories, Canada","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Meltwater; Geology; Drumlin; Bedrock; Geomorphology; Erosion; Geochemistry; Glacial period; Paleontology; Ice stream; Oceanography","score_opus":0.006268264525105432,"score_gpt":0.1884439308699326,"score_spread":0.18217566634482718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056062658","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99597853,0.00067143806,8.4233153e-7,0.0007769957,0.000397485,0.000106748805,0.00009277084,0.0000010006123,0.0019741727],"genre_scores_gemma":[0.9993198,0.00001495799,0.00009401699,0.00025558262,0.00010945811,3.423223e-7,0.0000102052345,0.0000011692774,0.00019447958],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984041,0.00025876542,0.00028274205,0.00013594376,0.00035927538,0.00055921637],"domain_scores_gemma":[0.99920666,0.00026632106,0.00009063958,0.00010494265,0.000059383725,0.00027207626],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001082624,0.00009684551,0.00020475425,0.00017248762,0.00035225015,0.000047797883,0.00064397964,0.000067022826,0.0015248469],"category_scores_gemma":[0.00007192242,0.000058717193,0.000045046087,0.00039249973,0.00063014333,0.00016670003,0.0000026822484,0.00028527458,0.000020803054],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000140343855,0.0000047039443,0.9959694,0.000010480559,0.0000053292943,0.00036015577,0.0020023405,0.0005398683,4.3402528e-7,0.0000045349693,0.0000708843,0.001017837],"study_design_scores_gemma":[0.00024097778,0.00020339924,0.9898309,0.000027162101,0.000006665911,0.00018279238,0.001000333,0.0002909399,0.00005059316,0.00012548665,0.007964172,0.000076589255],"about_ca_topic_score_codex":0.86187434,"about_ca_topic_score_gemma":0.99996644,"teacher_disagreement_score":0.13809209,"about_ca_system_score_codex":0.0000010863511,"about_ca_system_score_gemma":0.004321897,"threshold_uncertainty_score":0.9993879},"labels":[],"label_agreement":null},{"id":"W2056155717","doi":"10.1139/e01-096","title":"Arctic North American seasonal temperatures from the latest Miocene to the Early Pleistocene, based on mutual climatic range analysis of fossil beetle assemblages","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Maple Leaf Foods","funders":"National Science Foundation","keywords":"Arctic; Range (aeronautics); Holocene climatic optimum; Geology; Paleontology; Arctic vegetation; Fossil wood; Paleoclimatology; Permafrost; Neogene; Physical geography; Pleistocene; Latitude; Quaternary; Climate change; The arctic; Ecology; Oceanography; Geography; Biology; Tundra","score_opus":0.026071362239955223,"score_gpt":0.23379938519162513,"score_spread":0.20772802295166992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056155717","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98996437,0.0010490364,0.0000048279026,0.0079748705,0.00017394207,0.000107438835,0.00016464095,0.0000024575108,0.0005584065],"genre_scores_gemma":[0.99845517,0.000026226991,0.00024814962,0.0011309283,0.00008238825,7.4700506e-7,0.000008007902,0.0000019299237,0.000046474306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980309,0.00041040234,0.000320817,0.00021193425,0.00052140857,0.0005045624],"domain_scores_gemma":[0.99715436,0.0017261626,0.00024125591,0.00022800529,0.00016782299,0.00048240827],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010338852,0.00013658019,0.0003455054,0.00045596028,0.00077706156,0.00014428697,0.00094711524,0.000038574442,0.0016094893],"category_scores_gemma":[0.00059131393,0.00007218296,0.0001682947,0.002412772,0.0013538179,0.00012716676,0.0000064877054,0.00035620626,0.000081259874],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028028788,0.000008336,0.97554976,0.0000022157094,0.00009378056,0.000048137852,0.00048495524,0.0230683,5.867045e-7,0.000005442551,0.00027420738,0.00043625932],"study_design_scores_gemma":[0.00012376961,0.0006273351,0.9866977,0.000021726739,0.00012151004,0.000015904992,0.0002403425,0.011729992,0.000004786122,0.000015806972,0.00031430734,0.00008681611],"about_ca_topic_score_codex":0.024941402,"about_ca_topic_score_gemma":0.88917524,"teacher_disagreement_score":0.86423385,"about_ca_system_score_codex":0.0000013699845,"about_ca_system_score_gemma":0.0004367154,"threshold_uncertainty_score":0.99930316},"labels":[],"label_agreement":null},{"id":"W2056169670","doi":"10.1139/cjes-2012-0073","title":"Paleobotany and paleoecology of Gao Mine, a late Paleocene fossil locality near Red Deer, Alberta, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Paleoecology; Overbank; Paleobotany; Paleontology; Mesophyte; Floodplain; Range (aeronautics); Sedimentary depositional environment; Ecology; Deciduous; Biology; Structural basin","score_opus":0.013236368554423313,"score_gpt":0.16478171869524672,"score_spread":0.1515453501408234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056169670","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955992,0.0005219783,7.113993e-7,0.0028662276,0.0001934326,0.000058477162,0.000029551029,0.0000012327637,0.0007292066],"genre_scores_gemma":[0.99945956,0.000040361338,0.00009515393,0.00019294406,0.00004408534,3.1715643e-7,0.0000018409349,2.1789994e-7,0.00016553803],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99907684,0.00006033107,0.00022745221,0.00012691847,0.00018331749,0.00032516252],"domain_scores_gemma":[0.99898946,0.00016742056,0.00018510717,0.000025685784,0.0001449804,0.0004873141],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000306591,0.00007937097,0.00018123772,0.000026262167,0.00037192056,0.00006824516,0.00025839923,0.000057858404,0.00051702326],"category_scores_gemma":[0.00013320365,0.000035754587,0.00003985543,0.00027192262,0.00045456944,0.00024074406,0.000013470507,0.00009049499,0.0000046294476],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000056898784,0.000006086662,0.9927488,0.0000043725363,0.000009161293,0.000023377133,0.00007441075,0.000060096958,0.0022185526,0.000017276074,0.0018643737,0.002967814],"study_design_scores_gemma":[0.000091313224,0.0001940572,0.9903877,0.000021435502,0.00000831976,0.000056221328,0.00026251064,0.00022370461,0.000113620175,0.00018993918,0.008368612,0.000082603474],"about_ca_topic_score_codex":0.87548643,"about_ca_topic_score_gemma":0.9992404,"teacher_disagreement_score":0.12375401,"about_ca_system_score_codex":0.000008303941,"about_ca_system_score_gemma":0.00058744376,"threshold_uncertainty_score":0.56610423},"labels":[],"label_agreement":null},{"id":"W2056267841","doi":"10.1139/e04-096","title":"<i>Helmolepis cyphognathus</i>, sp. nov., a new platysiagid actinopterygian from the Lower Triassic Sulphur Mountain Formation (British Columbia, Canada)","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Royal Tyrrell Museum","funders":"Vedecká Grantová Agentúra MŠVVaŠ SR a SAV","keywords":"Early Triassic; Paleontology; Genus; Geology; Taxon; Tetrapod (structure); Actinopterygii; Fish fin; Permian; Biology; Fish <Actinopterygii>; Zoology","score_opus":0.013727731688010494,"score_gpt":0.18558633712877526,"score_spread":0.17185860544076476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056267841","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98328185,0.003323988,0.000035187844,0.0067971647,0.0013452632,0.00009956371,0.00023028934,0.0000050811914,0.0048815957],"genre_scores_gemma":[0.9954449,0.00006357571,0.0005716406,0.0026507762,0.0006858221,2.6119181e-7,0.00002478282,0.0000018510957,0.0005563731],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982838,0.00015331751,0.0004320802,0.00020077318,0.00035151292,0.00057851383],"domain_scores_gemma":[0.99849033,0.0003057431,0.00030229756,0.0001245935,0.00009217901,0.00068487256],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007681226,0.00011274223,0.00022574936,0.00008050737,0.0010085269,0.00034298957,0.0007004414,0.00010572007,0.005705525],"category_scores_gemma":[0.00021040638,0.00010600075,0.00008002074,0.0003640344,0.0005162484,0.00087169465,0.000005340591,0.00032098073,0.000059295842],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018392335,0.000004720597,0.9431473,0.000001011858,0.000019699315,0.00015077573,0.00017758158,0.0010738391,0.0000063625757,0.000009539116,0.02694716,0.0284436],"study_design_scores_gemma":[0.00033176053,0.00014977677,0.8682669,0.00003277977,0.000016008713,0.000692406,0.0003690726,0.0008536824,0.000009113116,0.00029700447,0.12884048,0.000141024],"about_ca_topic_score_codex":0.9839484,"about_ca_topic_score_gemma":0.999984,"teacher_disagreement_score":0.10189332,"about_ca_system_score_codex":0.000013466725,"about_ca_system_score_gemma":0.0063225348,"threshold_uncertainty_score":0.9993107},"labels":[],"label_agreement":null},{"id":"W2056553217","doi":"10.1139/e04-051","title":"Taxonomy, phylogeny, and paleoecology of<i>Eoseira wilsonii</i>gen. et sp. nov., a Middle Eocene diatom (Bacillariophyceae: Aulacoseiraceae) from lake sediments at Horsefly, British Columbia, Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Diatoms and Algae Research","field":"Materials Science","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta","keywords":"Diatom; Paleontology; Geology; Paleoecology; Cenozoic; Genus; Taxonomy (biology); Biostratigraphy; Ecology; Biology; Oceanography; Structural basin","score_opus":0.022987548174833807,"score_gpt":0.22346824640899224,"score_spread":0.20048069823415843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056553217","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99369615,0.0033815943,0.0000068861295,0.00062239775,0.000645084,0.00021098717,0.0006677217,0.000004721138,0.00076443824],"genre_scores_gemma":[0.9966934,0.00014895838,0.0016547008,0.000658359,0.00021383402,0.0000050800145,0.0000061839237,0.000012832848,0.00060665474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99720055,0.00016642068,0.00062293303,0.00041403848,0.000715697,0.00088036497],"domain_scores_gemma":[0.99771583,0.00019138496,0.00044293157,0.00019810647,0.00025056637,0.0012011902],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013125583,0.00016964343,0.00048760293,0.00015629822,0.0005950733,0.0006525198,0.00070287415,0.00010421577,0.002444006],"category_scores_gemma":[0.00016439892,0.00020174464,0.000087195745,0.00038091285,0.00093907944,0.00049229106,0.000104670326,0.00022678859,0.00001830367],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013978188,0.000043137614,0.9823384,0.000027106587,0.00004043025,0.0004438118,0.0002002375,0.00032388576,0.0065879915,0.000013652426,0.005580513,0.0043868143],"study_design_scores_gemma":[0.0010437565,0.00036944397,0.8049519,0.00019166738,0.000035238932,0.00034180123,0.0003345872,0.00014871432,0.0041345693,0.00009955398,0.1879366,0.0004121437],"about_ca_topic_score_codex":0.8983497,"about_ca_topic_score_gemma":0.9998487,"teacher_disagreement_score":0.18235609,"about_ca_system_score_codex":0.00007510017,"about_ca_system_score_gemma":0.0075262072,"threshold_uncertainty_score":0.9984679},"labels":[],"label_agreement":null},{"id":"W2056572874","doi":"10.1139/cjes-2013-0145","title":"A review of the inferred geodynamic evolution of the Dharwar craton over the ca. 3.5–2.5 Ga period, and possible implications for global tectonics","year":2013,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Dharwar Craton; Geochemistry; Archean; Craton; Gneiss; Metamorphism; Greenstone belt; Supercontinent; Metamorphic rock; Tectonics; Paleontology","score_opus":0.02748001932365823,"score_gpt":0.26128719866604455,"score_spread":0.23380717934238632,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056572874","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008397676,0.98854613,0.0000065548556,0.0015859421,0.00015935749,0.0004482741,0.000397798,8.354803e-7,0.00045740276],"genre_scores_gemma":[0.049515907,0.9500244,0.00009927002,0.0002469501,0.000048842543,0.0000038080157,0.00000736393,0.000001543656,0.00005188286],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99854064,0.00016525378,0.0006163252,0.00016923716,0.00022945511,0.00027911202],"domain_scores_gemma":[0.9982299,0.00018994207,0.00088496995,0.00024656588,0.000243011,0.00020558525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00080022716,0.00015670687,0.00059887377,0.00006518172,0.00048335662,0.00006667268,0.0010842782,0.00008453924,0.0007220781],"category_scores_gemma":[0.0005510093,0.000057672092,0.0005188197,0.0012227322,0.0011287265,0.00011279165,0.0000258083,0.0002070143,0.0000030256854],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000041366734,0.00002400631,0.48847008,0.012161454,0.00029207364,0.0000012861765,0.000085738124,0.00047177836,0.0000040592067,0.002528222,0.0026498258,0.49330732],"study_design_scores_gemma":[0.00010309959,0.00018243978,0.55744815,0.0135184,0.0009154363,0.00023389848,0.000072230025,0.0005674972,8.7728677e-7,0.011169565,0.41555357,0.0002348604],"about_ca_topic_score_codex":0.014192538,"about_ca_topic_score_gemma":0.18173234,"teacher_disagreement_score":0.49307248,"about_ca_system_score_codex":0.000008655134,"about_ca_system_score_gemma":0.0024555519,"threshold_uncertainty_score":0.99237204},"labels":[],"label_agreement":null},{"id":"W2056780974","doi":"10.1139/e04-014","title":"Endostromatolites from permafrost karst, Yukon, Canada: paleoclimatic proxies for the Holocene hypsithermal","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Resources Canada","keywords":"Permafrost; Geology; Holocene; Holocene climatic optimum; Radiocarbon dating; Calcite; Thermokarst; Tundra; Tufa; Karst; Carbonate; Geochemistry; Paleontology; Arctic; Oceanography","score_opus":0.02395756296315755,"score_gpt":0.2201707108413161,"score_spread":0.19621314787815855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056780974","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98605824,0.005874696,0.00003243793,0.005979168,0.00070147926,0.00019158599,0.00037503513,0.0000036876309,0.00078369136],"genre_scores_gemma":[0.9980401,0.000047862988,0.0011051184,0.00058010756,0.0001510755,0.0000014061602,0.000019313971,0.0000024413262,0.000052589454],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99832106,0.0000898003,0.0003460392,0.0001869966,0.00033056145,0.0007255394],"domain_scores_gemma":[0.9981096,0.00090656336,0.00019369999,0.00014212308,0.00015281928,0.0004952356],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008331239,0.00014143491,0.00025183012,0.00015803642,0.0012061299,0.00013760984,0.0008126456,0.00007055655,0.0008299426],"category_scores_gemma":[0.00037228686,0.00008668446,0.00008473173,0.00029876214,0.0012022223,0.0002738125,0.000006202475,0.0002633753,0.000026957297],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013436999,0.0000025576123,0.996095,0.0000066905895,0.000025232255,0.00010799188,0.00031118942,0.0030306873,0.0000036858805,0.00015346351,0.00010605617,0.00014403198],"study_design_scores_gemma":[0.00039511922,0.00020349253,0.99432373,0.0000374279,0.000024880492,0.0004505912,0.0010610527,0.0005137067,0.0001612886,0.0017927941,0.0009208575,0.00011504076],"about_ca_topic_score_codex":0.5323135,"about_ca_topic_score_gemma":0.9947843,"teacher_disagreement_score":0.46247083,"about_ca_system_score_codex":0.0000017396256,"about_ca_system_score_gemma":0.006774322,"threshold_uncertainty_score":0.99885637},"labels":[],"label_agreement":null},{"id":"W2057034445","doi":"10.1139/e06-006","title":"Structural evolution of the Cross Lake greenstone belt in the northwestern Superior Province, Manitoba: implications for relationship between vertical and horizontal tectonism","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Manitoba Hydro; University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Sinistral and dextral; Transpression; Pluton; Horizontal and vertical; Clockwise; Tectonics; Diapir; Greenstone belt; Archean; Paleontology; Geomorphology; Petrology; Fold (higher-order function); Geodesy","score_opus":0.023347230914934722,"score_gpt":0.22126083864490895,"score_spread":0.19791360772997424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057034445","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973651,0.000295689,0.00002104356,0.0018777602,0.00005377918,0.00011114963,0.00011878374,0.0000010656704,0.00015559388],"genre_scores_gemma":[0.99972063,7.112606e-7,0.00014311554,0.000031113614,0.00008600223,5.0203016e-7,0.000008610106,5.7671645e-7,0.000008709914],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991962,0.000052682855,0.0002716116,0.00010798943,0.00015297216,0.0002185676],"domain_scores_gemma":[0.999378,0.00029022695,0.000083869294,0.00006961458,0.00007127096,0.00010699493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041255617,0.00006300029,0.000116867195,0.00008799901,0.0004827972,0.00007889491,0.00032699446,0.00003991959,0.000035965997],"category_scores_gemma":[0.00012416305,0.000031398904,0.000068553694,0.00039930313,0.00084508926,0.0001768379,0.0000053650783,0.0001281907,7.568275e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000025948682,0.000001453527,0.99849075,0.0000024490519,0.0000020264574,9.252651e-7,0.000032769367,0.00039072058,0.000014575265,0.0006217242,0.000003116233,0.0004369241],"study_design_scores_gemma":[0.00010442357,0.000109647604,0.98158884,0.000007773377,0.00001705364,0.000034939803,0.000099925775,0.00020943096,0.000016061646,0.017710792,0.00005545513,0.000045673976],"about_ca_topic_score_codex":0.08379738,"about_ca_topic_score_gemma":0.9825113,"teacher_disagreement_score":0.8987139,"about_ca_system_score_codex":0.000002747185,"about_ca_system_score_gemma":0.00031274435,"threshold_uncertainty_score":0.9223037},"labels":[],"label_agreement":null},{"id":"W2057108875","doi":"10.1139/e06-132","title":"Neoproterozoic and Cambrian U–Pb (zircon) ages from Grand Manan Island, New Brunswick: implications for stratigraphy and northern Appalachian terrane correlations","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University","funders":"","keywords":"Geology; Zircon; Felsic; Bay; Terrane; Paleontology; Cove; Paleozoic; Nappe; Mesozoic; Geochemistry; Mafic; Tectonics; Geomorphology; Structural basin; Oceanography","score_opus":0.016268864730633128,"score_gpt":0.20659904569500734,"score_spread":0.1903301809643742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057108875","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9900845,0.0021761712,0.0031733578,0.0031775974,0.000100933335,0.00012544077,0.000102995604,0.0000038037692,0.0010551487],"genre_scores_gemma":[0.99545485,0.000043618045,0.0039964183,0.00022639657,0.00014969977,1.7153477e-7,0.000026394471,0.0000013400606,0.00010109485],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990133,0.000021971433,0.00030131862,0.00020963918,0.000115978626,0.00033775985],"domain_scores_gemma":[0.9986085,0.00021316795,0.0001562259,0.00007604374,0.000066909415,0.0008790976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039973564,0.00011456021,0.00019377349,0.0002393456,0.00053641695,0.0001755675,0.0002005143,0.000056919846,0.00040927343],"category_scores_gemma":[0.00007672669,0.00008082994,0.000077044366,0.0003557583,0.00047695878,0.0002366433,0.0000034689467,0.00012247342,0.000003550345],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007878953,0.000002292298,0.9897894,0.0000025582658,0.000018684215,0.0000049264377,0.0001564108,0.00007161875,0.00012930033,0.00018883134,0.000037726444,0.009590319],"study_design_scores_gemma":[0.00024574721,0.00019138484,0.97802794,0.000015420392,0.00004186725,0.00004487363,0.0002360251,0.00023957615,0.000028920116,0.019146949,0.0016681707,0.0001131238],"about_ca_topic_score_codex":0.15353253,"about_ca_topic_score_gemma":0.98930365,"teacher_disagreement_score":0.8357711,"about_ca_system_score_codex":7.8234245e-7,"about_ca_system_score_gemma":0.00040369632,"threshold_uncertainty_score":0.8521042},"labels":[],"label_agreement":null},{"id":"W2057138898","doi":"10.1139/e02-087","title":"Relationships between lithofacies belts and conodont faunas, Gun River Formation (Lower Silurian), Anticosti Island, Quebec: a statistical approach","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"","keywords":"Conodont; Facies; Siliciclastic; Geology; Paleontology; Carbonate; Carbonate rock; Carbonate platform; Sedimentary rock; Biostratigraphy","score_opus":0.04843406164012427,"score_gpt":0.21632360001848014,"score_spread":0.16788953837835588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057138898","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94832116,0.00792453,0.0028621773,0.0012287663,0.0003606822,0.00014273809,0.00028477094,0.000007862649,0.03886728],"genre_scores_gemma":[0.99466497,0.00005755785,0.004995892,0.000046519715,0.000082585924,1.7231666e-7,0.000006946865,6.77581e-7,0.00014467623],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998696,0.00017682809,0.0003547023,0.00016230722,0.00024185008,0.00036828322],"domain_scores_gemma":[0.9987735,0.00028515278,0.00018604014,0.00007310247,0.00006986054,0.00061231136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00086566224,0.00011959095,0.00021851034,0.0003091723,0.0008521197,0.00023338193,0.00022226585,0.00010157087,0.00047817733],"category_scores_gemma":[0.00023738612,0.00009174317,0.00004806244,0.00026444532,0.0012160513,0.0012719142,0.0000010839323,0.00030218644,0.000017009887],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000050559834,0.0000041387343,0.96900445,0.0000075202433,0.00001471362,0.000037461778,0.0012770662,0.00007814302,7.244137e-7,0.0005456716,0.0006617264,0.028363347],"study_design_scores_gemma":[0.00021123899,0.00020895964,0.99157745,0.00002422665,0.0000236379,0.00017542788,0.00042499346,0.0031028793,0.0000024692067,0.00085611845,0.0032685606,0.00012401733],"about_ca_topic_score_codex":0.012538632,"about_ca_topic_score_gemma":0.58344525,"teacher_disagreement_score":0.5709066,"about_ca_system_score_codex":0.0000017111277,"about_ca_system_score_gemma":0.00023057278,"threshold_uncertainty_score":0.994037},"labels":[],"label_agreement":null},{"id":"W2057302422","doi":"10.1139/e00-095","title":"Melting of heterogeneous mantle in a slab window environment: examples from the middle Tertiary Masset basalts, Queen Charlotte Islands, British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Geoscience BC","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Basalt; Geochemistry; Fractional crystallization (geology); Peridotite; Partial melting; Volcanic rock; Seamount; Andesites; Subduction; Mid-ocean ridge; Volcano; Andesite; Tectonics; Paleontology","score_opus":0.0187286804858305,"score_gpt":0.16593272727324399,"score_spread":0.1472040467874135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057302422","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953715,0.0026693959,0.0000061815113,0.0008589749,0.00007986606,0.00005687498,0.00016699091,0.0000019156307,0.0007882876],"genre_scores_gemma":[0.9986712,0.00027502282,0.0003342407,0.0004956644,0.00008926029,2.6598926e-7,0.00001649149,0.0000014591678,0.000116409654],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998561,0.00011434814,0.00040936194,0.00020101987,0.00030454132,0.0004096752],"domain_scores_gemma":[0.9991082,0.00022622674,0.0002133102,0.00010318844,0.000028407467,0.00032064394],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00061039574,0.00008581552,0.00024970848,0.00007243642,0.0002584164,0.00021934764,0.00054461154,0.000049395403,0.013171351],"category_scores_gemma":[0.00010713046,0.00007024972,0.00010299866,0.00033884184,0.0004590932,0.00018473905,0.000012021654,0.00016688772,0.000021754557],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003206197,0.000005664278,0.99516106,0.0000018626572,0.000013481713,0.00018413806,0.00014323811,0.0012823183,0.00005155861,6.003412e-7,0.00008803441,0.0030648196],"study_design_scores_gemma":[0.00016316105,0.000098239434,0.992809,0.000066344335,0.000016133574,0.0001133318,0.00034788772,0.0008719344,0.00006595955,0.0028003647,0.0025456836,0.000101991056],"about_ca_topic_score_codex":0.72289807,"about_ca_topic_score_gemma":0.9750438,"teacher_disagreement_score":0.2521457,"about_ca_system_score_codex":0.000002046905,"about_ca_system_score_gemma":0.00017083772,"threshold_uncertainty_score":0.98773074},"labels":[],"label_agreement":null},{"id":"W2057435446","doi":"10.1139/e01-045","title":"A condensed Lower to Middle Ordovician graptolite succession at Matane, Quebec, Canada","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ordovician; Fauna; Ecological succession; Paleontology; Geology; Biostratigraphy; Ecology; Biology","score_opus":0.02079984940020866,"score_gpt":0.21163838353231124,"score_spread":0.19083853413210258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057435446","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89429915,0.002652552,0.000009266552,0.0018672196,0.0008136554,0.00006835131,0.000029228599,0.000004367836,0.10025619],"genre_scores_gemma":[0.9963804,0.000016014643,0.000310639,0.0007240047,0.00007988692,1.4432815e-7,0.0000011850381,0.0000012394501,0.0024864692],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851525,0.00006906684,0.00030308086,0.00019175347,0.00034448673,0.0005763575],"domain_scores_gemma":[0.9982189,0.0000841042,0.00016471953,0.00011424447,0.00007933416,0.0013386948],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037830076,0.0001313478,0.00021110589,0.00037503667,0.00068875373,0.00011232637,0.00049829436,0.000059431077,0.0047656503],"category_scores_gemma":[0.00008044337,0.00010074287,0.00006405089,0.00067736453,0.0003748666,0.00028377454,0.0000013916246,0.0001330643,0.000039144034],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023755161,0.0000021934593,0.98987603,0.000002220331,0.0000092993305,0.0008308993,0.00011999083,0.00016025378,0.000022576496,0.000057360478,0.0022483144,0.006647126],"study_design_scores_gemma":[0.00013072565,0.00014078424,0.94409937,0.000049110735,0.000006346991,0.00032628555,0.00020906003,0.00006187169,0.000031506304,0.000098134675,0.054709326,0.00013746099],"about_ca_topic_score_codex":0.95490086,"about_ca_topic_score_gemma":0.9999872,"teacher_disagreement_score":0.10208125,"about_ca_system_score_codex":0.0000057783714,"about_ca_system_score_gemma":0.0032876916,"threshold_uncertainty_score":0.9961441},"labels":[],"label_agreement":null},{"id":"W2057487312","doi":"10.1139/e04-011","title":"Stratigraphy and tectono-sedimentary evolution of the Late Ordovician to Middle Devonian Gaspé Belt in northern New Brunswick: evidence from the Restigouche area","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Institut National de la Recherche Scientifique; Geological Survey of Canada","funders":"","keywords":"Geology; Unconformity; Devonian; Paleontology; Conglomerate; Ordovician; Group (periodic table); Sedimentary rock","score_opus":0.024547442061271487,"score_gpt":0.1931054567967242,"score_spread":0.1685580147354527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057487312","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9853012,0.004103941,0.000020430463,0.010195479,0.0001029963,0.0000795565,0.000013864432,0.0000014232985,0.00018113684],"genre_scores_gemma":[0.9986603,0.00003462113,0.00066329056,0.0005753207,0.000054408236,8.306967e-8,9.302402e-7,6.526215e-7,0.0000103587945],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885947,0.00007151216,0.00032521924,0.00015557022,0.00029671512,0.00029153033],"domain_scores_gemma":[0.9990168,0.00018237733,0.0001642047,0.00011852058,0.00006209656,0.00045600132],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005258144,0.00009757212,0.00016456633,0.00013951279,0.00028169036,0.00006906501,0.00059048436,0.000038135357,0.000380622],"category_scores_gemma":[0.00029734132,0.00004886167,0.00007840171,0.0011655494,0.00053490046,0.00022097821,0.000011221741,0.00019314088,0.000005382154],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057652337,0.000002637297,0.9826103,9.984191e-7,0.000007967273,0.000007090506,0.00043103614,0.015885077,0.00013521903,0.000026944097,0.00000811684,0.0008788722],"study_design_scores_gemma":[0.00009768758,0.00016260106,0.98685664,0.00017611554,0.000014007618,0.000009861778,0.0007186398,0.00015314325,0.00022026745,0.011405336,0.00011578697,0.00006992198],"about_ca_topic_score_codex":0.81020623,"about_ca_topic_score_gemma":0.9983791,"teacher_disagreement_score":0.18817286,"about_ca_system_score_codex":0.000005425317,"about_ca_system_score_gemma":0.0020623975,"threshold_uncertainty_score":0.4167544},"labels":[],"label_agreement":null},{"id":"W2057625494","doi":"10.1139/e08-058","title":"Continuous, diurnally fluctuating turbidity currents in Kluane Lake, Yukon Territory","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Pacific Insight Electronics (Canada); Queen's University","funders":"Arctic Institute of North America","keywords":"Sediment; Geology; Turbidity; Hydrology (agriculture); Turbidity current; Sedimentary rock; Glacier; Turbidite; STREAMS; Inflow; Current (fluid); Geomorphology; Sedimentary depositional environment; Oceanography; Geochemistry; Structural basin","score_opus":0.037410478360368385,"score_gpt":0.22490339539242732,"score_spread":0.18749291703205895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057625494","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98937416,0.0014080459,0.000024706173,0.000298034,0.00069234153,0.000045444824,0.00002529958,0.0000035741657,0.008128371],"genre_scores_gemma":[0.99860096,0.000065295164,0.0008743108,0.0001602297,0.00013810869,1.1186583e-7,0.0000049304335,9.0829116e-7,0.0001551275],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987146,0.00006695215,0.00042054648,0.00011549512,0.00030030002,0.00038209808],"domain_scores_gemma":[0.99909204,0.0001016494,0.00021481475,0.000054602257,0.00010460895,0.00043227515],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008735108,0.0000925251,0.00018122974,0.00033259712,0.00048439918,0.00009655492,0.00039554172,0.000046214456,0.0033210355],"category_scores_gemma":[0.00031596218,0.00006579226,0.00005033494,0.00046274494,0.00043279133,0.00070967124,0.0000038332896,0.00023790558,0.00006545962],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026128623,0.0000038824924,0.9918676,0.000004368502,0.0000019306892,0.000092686154,0.00031176684,0.003146818,0.0000024230526,0.000013618781,0.00026144992,0.0042908583],"study_design_scores_gemma":[0.00014574328,0.00021035793,0.9812272,0.00005238759,0.0000022051213,0.000376135,0.00021216499,0.0009894918,0.00002117696,0.0005147617,0.016149804,0.00009856344],"about_ca_topic_score_codex":0.010630653,"about_ca_topic_score_gemma":0.5731709,"teacher_disagreement_score":0.56254023,"about_ca_system_score_codex":0.0000015421134,"about_ca_system_score_gemma":0.0010533616,"threshold_uncertainty_score":0.99759007},"labels":[],"label_agreement":null},{"id":"W2057709601","doi":"10.1139/cjes-2015-0005","title":"Geology and paleoecology of a Middle Wisconsin fossil occurrence in Zorra Township, southwestern Ontario, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Guelph; Royal Ontario Museum; University of Waterloo; Geological Survey of Canada","funders":"","keywords":"Macrofossil; Geology; Taphonomy; Paleoecology; Tundra; Boreal; Paleontology; Glacial period; Wetland; Arctic; Physical geography; Ecology; Holocene; Oceanography; Geography","score_opus":0.06097749211421645,"score_gpt":0.23541185820737878,"score_spread":0.17443436609316232,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057709601","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99288034,0.0022409197,0.0000014928694,0.0008293611,0.00053717766,0.000059852126,0.000017809652,8.5959783e-7,0.003432173],"genre_scores_gemma":[0.9994924,0.000009245509,0.00021784587,0.00015368637,0.0000183187,1.9798614e-7,0.000002408393,6.1908173e-7,0.00010526966],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99848366,0.00021502089,0.0003708488,0.00017768514,0.00020557959,0.0005471874],"domain_scores_gemma":[0.99856657,0.0003148347,0.00019018183,0.00008580552,0.00013807815,0.0007045304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013520115,0.000100140816,0.00030909642,0.0003848263,0.00014074278,0.000026467143,0.0003895608,0.0001006619,0.0008573896],"category_scores_gemma":[0.0003460439,0.000080833306,0.000024503755,0.00031133866,0.0015832834,0.00018965219,0.00000943237,0.00034123415,0.000007789599],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018309676,0.0000027394858,0.99781954,0.000005694383,0.0000059128124,0.00033271586,0.0010128607,0.0004388204,3.7517233e-7,0.00003598821,0.00010289427,0.00022417336],"study_design_scores_gemma":[0.00033738255,0.00040299003,0.9951245,0.000022447499,0.0000046394343,0.0008048787,0.0012910259,0.00008276432,0.000006205376,0.0006441268,0.0011956824,0.00008335415],"about_ca_topic_score_codex":0.96128577,"about_ca_topic_score_gemma":0.9999938,"teacher_disagreement_score":0.038708057,"about_ca_system_score_codex":0.0000026362318,"about_ca_system_score_gemma":0.016146239,"threshold_uncertainty_score":0.9894313},"labels":[],"label_agreement":null},{"id":"W2057731022","doi":"10.1139/e06-062","title":"Tectonic evolution of the western Superior Province from NATMAP and Lithoprobe studies","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":253,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University; Geological Survey of Canada","funders":"","keywords":"Terrane; Geology; Metamorphism; Orogeny; Craton; Geochemistry; Fibrous joint; Seismology; Accretionary wedge; Basement; Accretion (finance); Continental crust; Paleontology; Geomorphology; Crust; Tectonics; Subduction","score_opus":0.012974401831354091,"score_gpt":0.18898940586054633,"score_spread":0.17601500402919223,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057731022","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9851464,0.012998169,0.000005264423,0.0011703752,0.0001303036,0.000037147773,0.000024914256,0.0000014421188,0.0004859578],"genre_scores_gemma":[0.9994077,0.00002485975,0.00030250297,0.00007031891,0.000069201924,7.22083e-8,5.8297644e-7,4.4408853e-7,0.00012428279],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991865,0.000050108094,0.00023606083,0.00011866949,0.0002092981,0.00019934587],"domain_scores_gemma":[0.9994464,0.00010101115,0.00015007505,0.00006117466,0.00009757126,0.00014376202],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032396606,0.00006859527,0.00016969419,0.00008022229,0.00026492067,0.000047018282,0.000273855,0.000028053268,0.0003661034],"category_scores_gemma":[0.00013056456,0.000034488025,0.000065634864,0.0003399631,0.00096739584,0.00016783222,0.000008670687,0.0000958744,0.0000044592402],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002047544,0.0000018723035,0.99843925,0.0000032316457,0.000008762328,0.000005587552,0.000048021386,0.0006003944,0.00014225539,0.000042458214,0.000025452679,0.00068063755],"study_design_scores_gemma":[0.00006556046,0.00009737723,0.9893783,0.000034318735,0.000020216072,0.000020765896,0.00022814423,0.00025191877,0.00045378107,0.008740777,0.00065656326,0.000052306874],"about_ca_topic_score_codex":0.12918405,"about_ca_topic_score_gemma":0.8425195,"teacher_disagreement_score":0.71333545,"about_ca_system_score_codex":0.0000020772563,"about_ca_system_score_gemma":0.00045519898,"threshold_uncertainty_score":0.8766148},"labels":[],"label_agreement":null},{"id":"W2057740222","doi":"10.1139/e06-102","title":"The Teton – Wind River domain: a 2.68–2.67 Ga active margin in the western Wyoming Province","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"University of Wyoming; National Park Service; National Science Foundation","keywords":"Geology; Gneiss; Batholith; Archean; Accretionary wedge; Geomorphology; Geochemistry; Dike; Back-arc basin; Paleontology; Subduction; Tectonics; Metamorphic rock","score_opus":0.010443134699826525,"score_gpt":0.18179153590771988,"score_spread":0.17134840120789335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057740222","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.983154,0.0011115406,0.000005981965,0.0038822063,0.00011085019,0.00007312492,0.000011268653,0.0000015649226,0.011649449],"genre_scores_gemma":[0.9990363,0.000018555913,0.00018953816,0.0003773053,0.00011838962,1.8415831e-7,0.0000015444309,7.202946e-7,0.0002574577],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986249,0.00014356531,0.00027805578,0.00015570379,0.00032784537,0.00046988527],"domain_scores_gemma":[0.99917084,0.00030059594,0.00017442313,0.000095056166,0.00005365151,0.00020542226],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011370821,0.000101622085,0.00014270408,0.00012685568,0.00060665974,0.00019759552,0.0007842521,0.000038138667,0.00066747103],"category_scores_gemma":[0.00008579168,0.00004556566,0.00009169487,0.0005829653,0.0010184428,0.00027406734,0.0000066729367,0.0002453331,0.00004465841],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011855341,0.0000053238805,0.99362797,0.000001230975,0.0000055655664,0.00012589584,0.00034879553,0.0010237566,0.0000106776615,0.00015168013,0.0001365737,0.0045506605],"study_design_scores_gemma":[0.000099701014,0.0001223375,0.9674822,0.000016276223,0.000008457929,0.000076508746,0.00073858374,0.00015904191,0.00004977631,0.012712775,0.01845154,0.00008280526],"about_ca_topic_score_codex":0.103242576,"about_ca_topic_score_gemma":0.85840297,"teacher_disagreement_score":0.7551604,"about_ca_system_score_codex":0.0000025777679,"about_ca_system_score_gemma":0.00048365217,"threshold_uncertainty_score":0.90272903},"labels":[],"label_agreement":null},{"id":"W2057758007","doi":"10.1139/e10-043","title":"Age and significance of Grenvillian and Silurian orogenic events in the Finnmarkian Caledonides, northern NorwayThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Nappe; Baltica; Metamorphism; Migmatite; Zircon; Laurentia; Geochemistry; Terrane; Metamorphic rock; Orogeny; Ordovician; Allochthon; Monazite; Titanite; Gneiss; Paleontology; Tectonics","score_opus":0.01883534978140121,"score_gpt":0.17727940986227764,"score_spread":0.15844406008087641,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057758007","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951605,0.00057548046,1.02060596e-7,0.0014902035,0.000032093456,0.00009768591,0.000045365014,3.0240778e-7,0.0025982433],"genre_scores_gemma":[0.9996222,0.00010801265,0.00012198038,0.00009818555,0.000026890952,3.8428965e-7,8.1251915e-7,8.9450384e-7,0.000020617064],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985925,0.00018319947,0.0005787168,0.00015010145,0.0002560382,0.00023942329],"domain_scores_gemma":[0.99906284,0.00023354811,0.00039558124,0.00011901435,0.00007102219,0.0001180046],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012233518,0.00009396068,0.00037222612,0.00023703612,0.000050570696,0.000008833876,0.00043861702,0.00005669868,0.006097822],"category_scores_gemma":[0.00030110969,0.000052297142,0.00006572744,0.00081356463,0.0013782282,0.00016775695,0.000011535354,0.0001778614,8.9500287e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005337816,0.000036907535,0.9914179,0.000017996921,0.000015205828,0.000015546433,0.004933294,0.00009185397,0.0006938913,0.00006806548,0.000009588981,0.002646382],"study_design_scores_gemma":[0.00022124071,0.0005365521,0.98621404,0.00008746085,0.00001337483,0.000008135525,0.002892052,0.00005285804,0.0067013167,0.003086697,0.00012637385,0.00005987034],"about_ca_topic_score_codex":0.09575112,"about_ca_topic_score_gemma":0.85395145,"teacher_disagreement_score":0.75820035,"about_ca_system_score_codex":0.0000019557708,"about_ca_system_score_gemma":0.00023908471,"threshold_uncertainty_score":0.99481076},"labels":[],"label_agreement":null},{"id":"W2057839912","doi":"10.1139/e05-010","title":"Darriwilian graptolites of the Hamburg succession (Dauphin Formation), Pennsylvania, and their geologic significance","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Marine and environmental studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Ordovician; Laurentia; Paleontology; Orogeny; Foreland basin; Biostratigraphy; Terrane; Ecological succession; Trilobite; Sedimentary depositional environment; Acritarch; Structural basin; Tectonics","score_opus":0.014152015701206923,"score_gpt":0.18067447916427978,"score_spread":0.16652246346307287,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057839912","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905536,0.0028988589,0.000014727196,0.0018561939,0.00014275413,0.00005625925,0.000019297839,0.0000013555872,0.0044569303],"genre_scores_gemma":[0.99907315,0.00022238008,0.00026197385,0.00025868247,0.00005782609,1.13113906e-7,7.336016e-7,7.177438e-7,0.00012439619],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992352,0.000046057485,0.00023494221,0.000088433895,0.00016224626,0.00023310955],"domain_scores_gemma":[0.9994179,0.00008256446,0.00019858827,0.00006717827,0.000024232992,0.0002095166],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00050622737,0.000079468315,0.0001307884,0.000090496746,0.00048625714,0.00005417546,0.00031864605,0.00002270825,0.0008493001],"category_scores_gemma":[0.00006675568,0.000040437306,0.000048288024,0.00021241825,0.00076675875,0.0004967271,0.000011500993,0.00009193843,0.0000061775113],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000022919166,0.0000019437286,0.9747668,0.000004489906,0.000003937022,0.0000016233869,0.00046032396,0.001380599,0.000051012335,0.000033919478,0.0001331081,0.023159977],"study_design_scores_gemma":[0.00007467906,0.00010963179,0.9770029,0.000026210788,0.0000044804237,0.000050117353,0.0009184017,0.0012357556,0.00064972637,0.0007522473,0.019111931,0.00006389959],"about_ca_topic_score_codex":0.010976477,"about_ca_topic_score_gemma":0.39463475,"teacher_disagreement_score":0.38365826,"about_ca_system_score_codex":0.0000017680417,"about_ca_system_score_gemma":0.00015916496,"threshold_uncertainty_score":0.9956095},"labels":[],"label_agreement":null},{"id":"W2058230419","doi":"10.1139/e05-024","title":"Record of Late Mississippian tectonics in the new Percé Group (Viséan) of eastern Gaspésie, Quebec","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Clastic rock; Structural basin; Paleontology; Carboniferous; Devonian; Group (periodic table); Alluvial fan; Geomorphology; Geochemistry","score_opus":0.023567731350219327,"score_gpt":0.2151656377233711,"score_spread":0.19159790637315177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058230419","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9873383,0.001718308,0.000029998037,0.0029314586,0.00013088364,0.00005090623,0.000010337765,0.0000011663408,0.007788647],"genre_scores_gemma":[0.9972383,0.00006979787,0.0021146345,0.00025004207,0.00006120653,5.5942326e-8,0.000001296094,7.31605e-7,0.00026393213],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988983,0.00006746881,0.00042677732,0.00008398654,0.000262591,0.0002608521],"domain_scores_gemma":[0.99918425,0.00012425055,0.0002618848,0.00008226922,0.00007408892,0.00027324967],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009870213,0.00007605151,0.00017164407,0.0002697048,0.00013681912,0.000073403804,0.0005925066,0.000041698397,0.0019968892],"category_scores_gemma":[0.00013363747,0.000043665346,0.00006224357,0.00065005996,0.0003325653,0.0004987285,0.0000031254979,0.00014778286,0.00001574917],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009196543,0.00000749988,0.87783706,0.000013346859,0.0000045903284,0.000010415198,0.0016195046,0.0056717624,0.000008883052,0.0001862109,0.00015877471,0.11447273],"study_design_scores_gemma":[0.0001511046,0.00040736794,0.9638778,0.00007951805,0.0000073032006,0.0000597986,0.0010571216,0.0020683403,0.000045061326,0.0011202702,0.03104558,0.00008073366],"about_ca_topic_score_codex":0.1276225,"about_ca_topic_score_gemma":0.93778604,"teacher_disagreement_score":0.81016356,"about_ca_system_score_codex":0.0000014338767,"about_ca_system_score_gemma":0.0011257422,"threshold_uncertainty_score":0.99891543},"labels":[],"label_agreement":null},{"id":"W2058375487","doi":"10.1139/cjes-2014-0078","title":"Corrigendum: Assessment of wavelets analysis for carrier-phase multipath mitigation","year":2014,"lang":"en","type":"erratum","venue":"Canadian Journal of Earth Sciences","topic":"Wireless Signal Modulation Classification","field":"Computer Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Geomatics; Library science; Engineering; Geology; Remote sensing; Computer science","score_opus":0.05408080946217915,"score_gpt":0.3162135102276662,"score_spread":0.26213270076548706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058375487","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0070132758,0.0004261164,0.9711829,0.0011214566,0.017894419,0.00037110155,0.00029968994,0.000011276784,0.0016798009],"genre_scores_gemma":[0.9574646,0.000017365204,0.038783032,0.00011936716,0.00054802373,0.00000871527,0.00009342143,0.000010133545,0.0029553436],"study_design_codex":"not_applicable","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9971312,0.00017526031,0.0009830708,0.00042909215,0.0008633005,0.0004180619],"domain_scores_gemma":[0.9952195,0.00016619438,0.0021654763,0.00042424575,0.0013608864,0.0006636871],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020163797,0.00022378165,0.000652958,0.0021553214,0.00039127455,0.0003503795,0.0016446458,0.00021874535,0.000049978727],"category_scores_gemma":[0.0003594246,0.00020112116,0.00040575807,0.0018909894,0.00037354257,0.0006189035,0.000022726175,0.00034573014,0.0000014490728],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033877004,0.0004123453,0.12231765,0.0008434028,0.0032429865,0.00016561348,0.0056492193,0.11676088,0.0035592695,0.10445272,0.5638215,0.07874055],"study_design_scores_gemma":[0.00066275714,0.0008634071,0.07507021,0.00022148648,0.000330982,0.000022476795,0.00009073361,0.8350976,0.00038527325,0.00096777425,0.085862294,0.0004249795],"about_ca_topic_score_codex":0.0010423161,"about_ca_topic_score_gemma":0.02849221,"teacher_disagreement_score":0.9504513,"about_ca_system_score_codex":0.0000584096,"about_ca_system_score_gemma":0.008885428,"threshold_uncertainty_score":0.99673325},"labels":[],"label_agreement":null},{"id":"W2058631794","doi":"10.1139/e05-069","title":"Diamond in the AtlinNakina region, British Columbia: insights from heavy minerals in stream sediments","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of British Columbia; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Detritus; Heavy mineral; Metamorphic rock; Massif; Bedrock; Volcanic rock; Kyanite; Diamond; Geomorphology; Paleontology; Volcano; Provenance","score_opus":0.013470293535485692,"score_gpt":0.1924750181671971,"score_spread":0.1790047246317114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058631794","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928049,0.0020984518,5.7144047e-7,0.001321001,0.00011577463,0.000052308256,0.00003895411,0.0000011482447,0.0035668812],"genre_scores_gemma":[0.9986376,0.00006132663,0.00014872715,0.00068020076,0.00017194315,2.8087985e-7,0.000015979416,9.219282e-7,0.00028300667],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99871975,0.00009327511,0.0003718106,0.00017118103,0.00030857453,0.0003353851],"domain_scores_gemma":[0.99937165,0.00008134244,0.0001431292,0.00008722672,0.000036559937,0.00028009634],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046806165,0.000073147654,0.00017045325,0.00013385004,0.00026568375,0.0004874475,0.00051209773,0.00004368903,0.0015547323],"category_scores_gemma":[0.00005843782,0.00006759754,0.000058995174,0.00075421616,0.00026046924,0.0004890249,0.0000035776084,0.00018370802,0.00001606878],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000221514,0.000010831611,0.9905767,0.0000012565224,0.0000055464548,0.00029955816,0.00041628222,0.0019518607,0.000010149538,0.0000010051766,0.0018584854,0.004866125],"study_design_scores_gemma":[0.0002466265,0.00008800923,0.982561,0.00007053831,0.000008316468,0.0001002355,0.0015075633,0.0006282276,0.000037583475,0.0007167054,0.013931881,0.00010331839],"about_ca_topic_score_codex":0.69780195,"about_ca_topic_score_gemma":0.9980324,"teacher_disagreement_score":0.30023047,"about_ca_system_score_codex":0.000004452262,"about_ca_system_score_gemma":0.00040286581,"threshold_uncertainty_score":0.999358},"labels":[],"label_agreement":null},{"id":"W2058678082","doi":"10.1139/e10-062","title":"Revision of the status of Saurolophus (Hadrosauridae) from California, USA","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Royal Ontario Museum; University of Alberta","funders":"Core Research for Evolutional Science and Technology; Natural Sciences and Engineering Research Council of Canada; Dinosaur Research Institute","keywords":"Taxon; Sister group; Paleontology; Clade; Geology; Phylogenetic tree; Geography; Biology","score_opus":0.013759573846815998,"score_gpt":0.21026774761636463,"score_spread":0.19650817376954863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058678082","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929753,0.0019692618,0.000007639368,0.00047799657,0.0012613354,0.00003896348,0.0002935872,7.6740895e-7,0.0029751637],"genre_scores_gemma":[0.9987315,0.000078289115,0.00094202394,0.00012703426,0.000092570466,1.9366409e-8,0.000003136466,6.031795e-7,0.000024847819],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988667,0.00010729041,0.00034246917,0.00010879726,0.00019618694,0.00037856773],"domain_scores_gemma":[0.9988198,0.00020341252,0.00035381762,0.00012675677,0.00010678953,0.00038937386],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00059952063,0.000069628884,0.00018622744,0.00013723726,0.00024251484,0.000011869049,0.0005311039,0.000086054155,0.0030956834],"category_scores_gemma":[0.00043135148,0.000040897805,0.00008351709,0.00029584824,0.0016244304,0.00014749229,0.000005225606,0.00025631988,0.000025536066],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010703557,0.0000022368845,0.994228,0.0000019812435,0.0000061729315,0.0000063558023,0.00008176692,0.00025775534,0.00038527852,0.00007048802,0.00013387967,0.004815395],"study_design_scores_gemma":[0.00009316815,0.00016097065,0.9694277,0.000018827339,0.000009581504,0.000055712586,0.00006298795,0.00021828024,0.00032178714,0.0007144297,0.028869517,0.00004700952],"about_ca_topic_score_codex":0.06300531,"about_ca_topic_score_gemma":0.7941107,"teacher_disagreement_score":0.73110545,"about_ca_system_score_codex":8.5306164e-7,"about_ca_system_score_gemma":0.0017659866,"threshold_uncertainty_score":0.9978156},"labels":[],"label_agreement":null},{"id":"W2058770701","doi":"10.1139/e08-068","title":"Subaqueous eruption and shallow-water reworking of a small-volume Surtseyan edifice at Kakanui, New Zealand","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lapilli; Geology; Pyroclastic rock; Breccia; Tephra; Geochemistry; Geomorphology; Volcano; Sedimentary depositional environment; Paleontology","score_opus":0.03514373312301869,"score_gpt":0.19520310224063508,"score_spread":0.1600593691176164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058770701","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952258,0.0015613429,0.000020184692,0.00081029866,0.00026039442,0.000041036703,0.000009374907,0.0000031010488,0.0020684719],"genre_scores_gemma":[0.99726135,0.00019558499,0.0010407694,0.00011054974,0.000108408385,5.4887757e-8,0.0000043039763,0.0000010913294,0.0012778857],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990111,0.000039045368,0.00030261956,0.000118061136,0.00020397476,0.0003252288],"domain_scores_gemma":[0.9990985,0.00006738998,0.00015298392,0.000056901248,0.000097209624,0.00052705733],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00054117845,0.00008565614,0.00016749336,0.00022340142,0.0004962744,0.00007361673,0.00022369121,0.000056130306,0.0020814592],"category_scores_gemma":[0.00007549862,0.000053928714,0.000042280833,0.00025135954,0.00044677538,0.0003627581,0.000006217918,0.00011190071,0.000028473767],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009176129,0.0000015749447,0.9945984,0.0000061115184,0.0000043317023,0.000040808787,0.0011455852,0.0013768566,0.000023656106,0.000008623618,0.00024476278,0.0025401271],"study_design_scores_gemma":[0.00014376974,0.0003707087,0.9752938,0.000040797866,0.000009015477,0.00091452576,0.00020044687,0.0005826879,0.00014693648,0.00062787207,0.021563318,0.000106104],"about_ca_topic_score_codex":0.030458283,"about_ca_topic_score_gemma":0.43697745,"teacher_disagreement_score":0.40651917,"about_ca_system_score_codex":0.0000016103994,"about_ca_system_score_gemma":0.00050397264,"threshold_uncertainty_score":0.9988308},"labels":[],"label_agreement":null},{"id":"W2058873732","doi":"10.1139/e04-047","title":"Phanerozoic vertical motions of Hudson Bay","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Devonian; Thermal subsidence; Paleozoic; Paleontology; Sedimentary basin; Lithosphere; Structural basin; Ordovician; Rift; Sedimentary rock; Cretaceous; Subsidence; Basin and range topography; Tectonic subsidence; Tectonics","score_opus":0.01810539976870911,"score_gpt":0.2121238993553354,"score_spread":0.1940184995866263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058873732","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948693,0.00036029893,0.00009575305,0.00048722443,0.0008680962,0.00003701331,0.00004295078,0.0000021115495,0.0032372805],"genre_scores_gemma":[0.9987946,0.000015075749,0.0009234699,0.00007620624,0.0001525845,5.1719024e-8,0.0000018496524,0.0000011553651,0.000035006713],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99906075,0.000034489964,0.00026788283,0.000095980984,0.00025290487,0.00028801887],"domain_scores_gemma":[0.99924856,0.000033282824,0.0000940458,0.00007399519,0.00009095845,0.00045916517],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004830411,0.00006940049,0.00016948789,0.00018183471,0.00020618546,0.00008295501,0.0003188847,0.00003331042,0.0015309654],"category_scores_gemma":[0.00008371492,0.000050957184,0.00006173887,0.00030285766,0.0004058859,0.00031119463,0.000002637241,0.00007198629,0.000053998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044341723,0.00009413733,0.73683316,0.00008989941,0.00014364943,0.0005270626,0.003788152,0.19597039,0.015832122,0.03526632,0.0008711505,0.010539605],"study_design_scores_gemma":[0.00042024264,0.000785094,0.9760332,0.00010508585,0.000032550444,0.00011521448,0.00024314331,0.00016930439,0.0075436807,0.008590573,0.0057837986,0.00017808753],"about_ca_topic_score_codex":0.01905255,"about_ca_topic_score_gemma":0.18119,"teacher_disagreement_score":0.23920004,"about_ca_system_score_codex":0.0000010131796,"about_ca_system_score_gemma":0.0012216651,"threshold_uncertainty_score":0.9993818},"labels":[],"label_agreement":null},{"id":"W2059028683","doi":"10.1139/cjes-2014-0012","title":"The mid-Cambrian (Series 3, Guzhangian; Marjuman) trilobite <i>Deiracephalus</i> Resser, 1935, from western Newfoundland","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Trilobite; Geology; Paleontology; Fauna; Bay; Oceanography; Biology; Ecology","score_opus":0.01685395388840618,"score_gpt":0.21288621061936971,"score_spread":0.19603225673096353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059028683","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9285106,0.017027345,0.00005060873,0.0026018713,0.0023068495,0.00009076102,0.00007072029,0.0000089678715,0.04933225],"genre_scores_gemma":[0.9981578,0.00019364814,0.00046611714,0.0002678672,0.0005006766,2.6098573e-7,0.0000030023073,0.0000013706581,0.0004092851],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980478,0.00026119789,0.0004395059,0.00023868069,0.00036914134,0.0006436276],"domain_scores_gemma":[0.99809456,0.0004985712,0.00033423182,0.00021305136,0.00010150548,0.00075806445],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0016149434,0.00017635558,0.00027409144,0.00021725731,0.001876299,0.0006323827,0.0009582063,0.00009372559,0.00028498625],"category_scores_gemma":[0.00023416556,0.000111817404,0.0001353808,0.00040883716,0.0015155899,0.0008490916,0.000001972501,0.000269506,0.00004174803],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003619816,0.000002055843,0.97086537,0.0000019834777,0.000024199582,0.00004606949,0.0003127768,0.00005741809,0.000021492791,0.00019289866,0.00030531824,0.028134225],"study_design_scores_gemma":[0.00026468447,0.00036469588,0.9356065,0.000038720882,0.00001882199,0.00013741148,0.0003125898,0.00010270514,0.000038501876,0.0021539612,0.060811058,0.00015036597],"about_ca_topic_score_codex":0.042271875,"about_ca_topic_score_gemma":0.9741758,"teacher_disagreement_score":0.9319039,"about_ca_system_score_codex":0.0000017063619,"about_ca_system_score_gemma":0.0008107155,"threshold_uncertainty_score":0.99942315},"labels":[],"label_agreement":null},{"id":"W2059375937","doi":"10.1139/e02-045","title":"Tectonic evolution and significance of Silurian Early Devonian hinterland-directed deformation in the internal Humber zone of the southern Quebec Appalachians","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; Geological Survey of Canada","funders":"","keywords":"Geology; Nappe; Devonian; Orogeny; Foreland basin; Metamorphism; Paleontology; Basement; Tectonics; Ordovician; Paleozoic; Laurentia; Obduction; Seismology; Subduction; Oceanic crust","score_opus":0.007909719560396846,"score_gpt":0.1728350968286561,"score_spread":0.16492537726825926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059375937","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99708366,0.00044897746,0.000072619056,0.00050405087,0.0000625403,0.00006075304,0.00001682945,0.0000010979784,0.0017494737],"genre_scores_gemma":[0.99968237,0.000004027665,0.00015733909,0.00004957602,0.000014220395,1.6811718e-7,5.885156e-7,5.6206176e-7,0.00009114365],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895453,0.00019211465,0.00032693436,0.000089439185,0.00023897612,0.0001980215],"domain_scores_gemma":[0.99937266,0.00009981773,0.00026108228,0.000072522555,0.00007634824,0.00011754708],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008818228,0.00006943018,0.00014830324,0.00013643703,0.00013611131,0.00004387619,0.0003477183,0.00003414769,0.0008602415],"category_scores_gemma":[0.00016638207,0.000033223205,0.00007252565,0.00060604664,0.0005881009,0.00015348158,0.0000031645686,0.00015596196,0.0000053866293],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000056456497,0.000004477896,0.99673414,0.000004333863,0.0000069308876,0.000002165658,0.0010392559,0.0011696973,0.000099000856,0.00011284122,0.000005814336,0.0008157067],"study_design_scores_gemma":[0.00011225012,0.000113317146,0.9947647,0.00004344116,0.000011875682,0.000039135113,0.001366346,0.0011745977,0.00020489164,0.0019021801,0.00021675372,0.000050518258],"about_ca_topic_score_codex":0.24390595,"about_ca_topic_score_gemma":0.92350256,"teacher_disagreement_score":0.6795966,"about_ca_system_score_codex":0.0000028683487,"about_ca_system_score_gemma":0.00033406247,"threshold_uncertainty_score":0.94190407},"labels":[],"label_agreement":null},{"id":"W2059376787","doi":"10.1139/e00-008","title":"Petrology of the Abloviak Aillikite dykes, New Québec: evidence for a Cambrian diamondiferous alkaline province in northeastern North America","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University; Université du Québec à Montréal","funders":"Université du Québec à Montréal","keywords":"Geology; Phlogopite; Ultramafic rock; Geochemistry; Phenocryst; Olivine; Gneiss; Ophiolite; Mantle (geology); Volcanic rock; Paleontology; Volcano; Metamorphic rock","score_opus":0.020729380788155786,"score_gpt":0.2073123740571106,"score_spread":0.1865829932689548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059376787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99247324,0.002184418,0.000026483527,0.0045576124,0.00010304606,0.0001194979,0.00004457159,0.0000019478744,0.00048920594],"genre_scores_gemma":[0.99774647,0.0000727686,0.00048672562,0.00071609503,0.00010153286,3.958935e-7,0.000002808647,0.0000013405814,0.0008718842],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984868,0.00008896733,0.00046896772,0.00021534528,0.00027024664,0.0004696464],"domain_scores_gemma":[0.9987057,0.0003010064,0.000261837,0.00013785169,0.00008482647,0.0005088189],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037695165,0.00012308206,0.00030919764,0.00017350918,0.00019616865,0.000047575384,0.00080535514,0.000041949712,0.0038986097],"category_scores_gemma":[0.00036939632,0.00007040078,0.00016395329,0.0008333231,0.00073616893,0.00025001002,0.0000064580913,0.00017224331,0.000029619809],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003336833,0.0000057081006,0.9636599,0.0000052928904,0.00000837058,0.000017172837,0.00014718139,0.012248527,0.000011709933,0.0000036073675,0.000062067425,0.023797132],"study_design_scores_gemma":[0.00018469075,0.00050379266,0.9833627,0.000050990864,0.000024163059,0.000043589625,0.00007310347,0.0032047515,0.000019442303,0.00045722342,0.011970271,0.00010533446],"about_ca_topic_score_codex":0.68181294,"about_ca_topic_score_gemma":0.99660563,"teacher_disagreement_score":0.3147927,"about_ca_system_score_codex":0.0000034092996,"about_ca_system_score_gemma":0.0024750058,"threshold_uncertainty_score":0.99701196},"labels":[],"label_agreement":null},{"id":"W2059428099","doi":"10.1139/e00-096","title":"W.G.E. Caldwell, B.Sc., Ph.D. (Glasgow), D.Sc. (Sask.), F.R.S.C. A Career Résumé","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University; Laurentian University","funders":"","keywords":"Library science; Honour; Geology; Management; Political science; Law","score_opus":0.04861661814452502,"score_gpt":0.21364969031350456,"score_spread":0.16503307216897956,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059428099","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.958092,0.0044538174,0.00010481254,0.0048015104,0.0014281048,0.000092692215,0.000022896347,0.000009923769,0.030994248],"genre_scores_gemma":[0.9974388,0.00035095046,0.00052395073,0.0008228372,0.00037506322,2.5986887e-7,0.0000046367963,0.0000019351676,0.00048160303],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99825174,0.00007052806,0.00036763446,0.00021314903,0.00043903722,0.0006579062],"domain_scores_gemma":[0.9985903,0.00010211972,0.0001865636,0.00010107373,0.0001770297,0.00084295246],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008114129,0.00014713767,0.0002385633,0.0002282047,0.0008475777,0.00023204784,0.00049554737,0.00007225694,0.005714718],"category_scores_gemma":[0.00021312495,0.000099647834,0.00010721068,0.00071194756,0.0005679579,0.000560087,0.000007730137,0.00020647908,0.00030830794],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012031927,0.000004811587,0.97497046,0.0000020979815,0.000013417769,0.00021866563,0.000391267,0.005574444,0.000007634164,0.00012120794,0.0033642913,0.0153197],"study_design_scores_gemma":[0.00019763173,0.00061620027,0.7540703,0.00002734663,0.00001395993,0.00023938711,0.0010565108,0.0010488417,0.000020456007,0.0014363019,0.24108332,0.0001897377],"about_ca_topic_score_codex":0.040174406,"about_ca_topic_score_gemma":0.6776896,"teacher_disagreement_score":0.6375152,"about_ca_system_score_codex":0.0000035867663,"about_ca_system_score_gemma":0.0006524961,"threshold_uncertainty_score":0.9951942},"labels":[],"label_agreement":null},{"id":"W2059640063","doi":"10.1139/e00-053","title":"The Margaree orthogneiss: an Ordovician, peri-Gondwanan, mafic-felsic igneous complex in southwestern Newfoundland","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Memorial University of Newfoundland","funders":"","keywords":"Geology; Metamorphism; Mafic; Geochemistry; Felsic; Pluton; Protolith; Hornblende; Metamorphic facies; Igneous rock; Petrology; Paleontology; Facies; Biotite","score_opus":0.024828982692341683,"score_gpt":0.21043045799607224,"score_spread":0.18560147530373056,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059640063","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9874821,0.0012061485,0.0000018922223,0.0016859908,0.00013520487,0.00005873948,0.000026617052,0.000004720354,0.009398587],"genre_scores_gemma":[0.99822694,0.00007457835,0.00022743037,0.0006428228,0.00013324195,2.1977078e-7,0.000009242347,0.0000017851431,0.0006837176],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99814004,0.00014523375,0.00044479116,0.00024053319,0.00035974628,0.000669682],"domain_scores_gemma":[0.9986612,0.00016245447,0.00013529947,0.00015446,0.00008501068,0.0008015369],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008696995,0.00015126726,0.0002519947,0.00020435582,0.0007956742,0.0004027169,0.0008639562,0.00005792018,0.024465699],"category_scores_gemma":[0.00008607618,0.00008574818,0.00011040652,0.0008617834,0.00082714745,0.00033440182,0.0000050564004,0.00024554972,0.00018996674],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013922117,0.0000058768373,0.9488813,0.0000013367436,0.000007324046,0.00014969365,0.00017326129,0.00433703,0.000011049278,0.000027493526,0.000026505633,0.046365153],"study_design_scores_gemma":[0.00013026774,0.000344461,0.9670109,0.000015490681,0.000012437651,0.00016609716,0.00044432416,0.0032318635,0.0000023050638,0.003538594,0.02495607,0.00014719891],"about_ca_topic_score_codex":0.12864327,"about_ca_topic_score_gemma":0.98321956,"teacher_disagreement_score":0.8545763,"about_ca_system_score_codex":0.0000030324877,"about_ca_system_score_gemma":0.00047490062,"threshold_uncertainty_score":0.97642606},"labels":[],"label_agreement":null},{"id":"W2060127319","doi":"10.1139/e02-008","title":"Geochemistry and age of the Aillik Group and associated plutonic rocks, Makkovik Bay area, Labrador: implications for tectonic development of the Makkovik Province","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; Acadia University; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University","keywords":"Felsic; Geology; Geochemistry; Volcanic rock; Zircon; Protolith; Archean; Metamorphism; Mafic; Petrology; Volcano","score_opus":0.018183454668329616,"score_gpt":0.18334089129059883,"score_spread":0.16515743662226923,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060127319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99557406,0.0019067302,0.000015560485,0.0015866364,0.000044379067,0.000100255886,0.000079579506,0.000001468164,0.00069131545],"genre_scores_gemma":[0.99914557,0.000035596615,0.00050664495,0.000114131486,0.000012442674,6.0333736e-7,0.0000028604159,8.924764e-7,0.00018128737],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99905616,0.000033680368,0.00032344743,0.00014865676,0.00017902182,0.00025901428],"domain_scores_gemma":[0.99914134,0.00014940544,0.00030964508,0.00010392053,0.00008198553,0.00021369173],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041991705,0.00008967278,0.0001893702,0.00005633509,0.00046057103,0.00004354526,0.00044095088,0.00005119425,0.000478049],"category_scores_gemma":[0.00025585492,0.00004586478,0.00008394244,0.00040468338,0.0007278443,0.00008497779,0.0000186284,0.00011973205,4.970799e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021817605,0.000010132621,0.9915443,0.000016065505,0.000026440302,0.0000010095846,0.00019943663,0.0002035642,0.0010226854,0.000034369335,0.000070259375,0.0068695606],"study_design_scores_gemma":[0.00013028656,0.0000668458,0.99390805,0.00004761952,0.000029909586,0.00002286771,0.00012476995,0.00095669733,0.0013349646,0.0018326133,0.001468133,0.00007723183],"about_ca_topic_score_codex":0.0024693338,"about_ca_topic_score_gemma":0.3601113,"teacher_disagreement_score":0.35764197,"about_ca_system_score_codex":0.0000035142612,"about_ca_system_score_gemma":0.00037689376,"threshold_uncertainty_score":0.651565},"labels":[],"label_agreement":null},{"id":"W2060169843","doi":"10.1139/e08-007","title":"The crustal structure of the southern Nain and Makkovik provinces of Labrador derived from refraction seismic data","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Crust; Seismology; Underplating; Seismometer; Orogeny; Submarine pipeline; Tectonics; Lithosphere; Geochemistry","score_opus":0.018921286631208265,"score_gpt":0.1878098659778066,"score_spread":0.16888857934659834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060169843","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958991,0.0017553099,0.0000053317904,0.001627041,0.00012287198,0.0000367312,0.00043228513,8.5338047e-7,0.00012048183],"genre_scores_gemma":[0.9994426,0.00006540619,0.00027963932,0.00009320395,0.000052307183,1.8155227e-8,0.0000053835565,5.73091e-7,0.00006087534],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990868,0.0000860027,0.00025294925,0.00012815616,0.0002734966,0.00017256907],"domain_scores_gemma":[0.9990949,0.00020238843,0.0003158569,0.00015371437,0.00007599934,0.00015716451],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030427013,0.0000668301,0.00014655078,0.00004988925,0.00043463625,0.000037877526,0.0007331439,0.000036275054,0.0005310084],"category_scores_gemma":[0.00026850248,0.000029066665,0.00004693881,0.0002726404,0.0014148566,0.00019101193,0.000019412888,0.0001431838,0.0000017038761],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014610029,0.0000024620524,0.98693675,0.0000032849225,0.000026508807,0.000008124951,0.00056776375,0.0008921791,0.002447673,0.000004844151,0.00006717281,0.009028639],"study_design_scores_gemma":[0.0000923281,0.000097787364,0.98756444,0.000018648732,0.000026599106,0.000056645677,0.0021407045,0.0042563016,0.00202702,0.0026113512,0.0010466799,0.000061503604],"about_ca_topic_score_codex":0.13462304,"about_ca_topic_score_gemma":0.7034614,"teacher_disagreement_score":0.56883836,"about_ca_system_score_codex":6.9373726e-7,"about_ca_system_score_gemma":0.0005230707,"threshold_uncertainty_score":0.8711396},"labels":[],"label_agreement":null},{"id":"W2060486998","doi":"10.1139/e09-069","title":"Structure of the Betts Cove Ophiolite Complex beneath the western margin of Notre Dame Bay, Newfoundland","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University; Geological Survey of Canada","funders":"","keywords":"Geology; Ophiolite; Outcrop; Cove; Bay; Ordovician; Paleontology; Series (stratigraphy); Geologic map; Carboniferous; Paleozoic; Diachronous; Geomorphology; Tectonics; Oceanography; Structural basin","score_opus":0.02098047916591802,"score_gpt":0.23485448587561616,"score_spread":0.21387400670969814,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060486998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960188,0.0002045199,0.0000123338295,0.0017703477,0.00063773757,0.00007900941,0.00016120181,0.0000010091715,0.0011150062],"genre_scores_gemma":[0.99843234,0.000004703142,0.00086205115,0.0003866001,0.00019118028,3.7057085e-8,0.0000015081159,0.0000014141362,0.0001201922],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99868375,0.00013759127,0.00031914894,0.0001249954,0.00040071266,0.00033377306],"domain_scores_gemma":[0.9986598,0.00034784028,0.00033425447,0.00017660874,0.00013860702,0.0003428885],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052608555,0.00010680638,0.00024219119,0.000101494385,0.0003182157,0.00008265291,0.0009669846,0.000054306267,0.0007684297],"category_scores_gemma":[0.00021438251,0.000048890437,0.00011878437,0.00068997685,0.0010459253,0.00016674536,0.000011027398,0.00037048545,0.0000035457276],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007981228,0.0000037170325,0.9865796,0.0000070918018,0.000011851255,0.0000043592663,0.0002445261,0.0011183535,0.0013890181,0.0002539998,0.00008726548,0.010292224],"study_design_scores_gemma":[0.00010794122,0.00021784318,0.9889919,0.000019236655,0.000014598147,0.0000559111,0.00005246053,0.0005439578,0.0005284651,0.003499861,0.0059004487,0.00006737431],"about_ca_topic_score_codex":0.029175375,"about_ca_topic_score_gemma":0.5956523,"teacher_disagreement_score":0.56647694,"about_ca_system_score_codex":8.800907e-7,"about_ca_system_score_gemma":0.0007272465,"threshold_uncertainty_score":0.97728944},"labels":[],"label_agreement":null},{"id":"W2060781149","doi":"10.1139/e05-048","title":"Iron oxide - copper - gold-type and related deposits in the Manitou Lake area, eastern Grenville Province, Quebec: variations in setting, composition, and style","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; Ministère des Ressources naturelles et des Forêts (Québec)","funders":"Université du Québec à Montréal","keywords":"Geology; Geochemistry; Allanite; Metasomatism; Cassiterite; Hypogene; Sphalerite; Sericite; Monazite; Uraninite; Pyrite; Molybdenite; Andradite; Marcasite; Ore genesis; Iron oxide copper gold ore deposits; Magnetite; Biotite; Fluid inclusions; Skarn; Hydrothermal circulation; Quartz; Zircon; Uranium","score_opus":0.00843111493796233,"score_gpt":0.17911625562501163,"score_spread":0.1706851406870493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060781149","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99262255,0.0010721374,0.000001432081,0.0037020026,0.00003607381,0.000057697263,0.000009275473,0.0000013566113,0.0024974588],"genre_scores_gemma":[0.99906945,0.000030087092,0.00032343625,0.00039903313,0.000025047035,1.477657e-7,0.0000065426875,6.163466e-7,0.00014565221],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991216,0.00009366961,0.00025485954,0.00013565194,0.00015841368,0.00023577109],"domain_scores_gemma":[0.9994934,0.00010837732,0.00010102316,0.00004643227,0.00004290859,0.00020784803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053996267,0.000075489465,0.0001239018,0.00019204548,0.00018559767,0.00014464268,0.00018330918,0.000041266012,0.00048560297],"category_scores_gemma":[0.000066632136,0.000045899866,0.00001979723,0.0005125488,0.0002779046,0.00025096742,0.000005275917,0.00016844393,0.0000101305095],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003599079,0.0000061755386,0.99509573,0.000002053358,0.0000031558745,0.000045658526,0.00039502175,0.0021681366,0.000031390602,0.00004865652,0.00006756374,0.0021328721],"study_design_scores_gemma":[0.00014293568,0.00007693124,0.99269104,0.000029367466,0.000010441198,0.00013025782,0.00043436128,0.005115252,0.000009913416,0.00044150013,0.00084655115,0.000071475675],"about_ca_topic_score_codex":0.065241314,"about_ca_topic_score_gemma":0.9831454,"teacher_disagreement_score":0.9179041,"about_ca_system_score_codex":0.0000019487002,"about_ca_system_score_gemma":0.00020202008,"threshold_uncertainty_score":0.9409833},"labels":[],"label_agreement":null},{"id":"W2060854164","doi":"10.1139/e03-082","title":"Late Wisconsinan buildup and wastage of the Innuitian Ice Sheet across southern Ellesmere Island, Nunavut","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta","funders":"","keywords":"Geology; Deglaciation; Ice sheet; Oceanography; Ice shelf; Ice field; Ice stream; Arctic ice pack; Bay; Glacier morphology; Fjord; Glacier; Sea ice; Paleontology; Cryosphere; Holocene","score_opus":0.017363902203073194,"score_gpt":0.23697986232392812,"score_spread":0.21961596012085494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060854164","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99358445,0.0012703787,0.0000034790944,0.0028419534,0.000288631,0.00006430115,0.00011763029,0.0000015454406,0.0018276125],"genre_scores_gemma":[0.9992255,0.000049976592,0.00016159948,0.00029356207,0.000039283193,7.672962e-8,0.0000011593645,0.0000014590009,0.00022739632],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987481,0.00012032443,0.00026012424,0.00014749235,0.00022460443,0.0004993445],"domain_scores_gemma":[0.9991291,0.000113768634,0.00018290915,0.0001196615,0.00009010578,0.00036441148],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010626045,0.00009791065,0.00019302359,0.000112421985,0.000722228,0.00007488272,0.0005340398,0.00008457484,0.00057210505],"category_scores_gemma":[0.0001302257,0.000059961738,0.0000602335,0.00039278695,0.0026307208,0.00020854497,0.000013280797,0.00030605472,0.000027578453],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008289188,0.0000022191823,0.9954144,0.000006003017,0.000009240616,0.00008023764,0.0018921565,0.002211801,0.0000074766613,0.00007219536,0.000016123378,0.0002798745],"study_design_scores_gemma":[0.00033161676,0.00020209943,0.9937478,0.000066614084,0.000007891593,0.0006695796,0.0026362243,0.00010121999,0.00012190197,0.0015157845,0.0005127334,0.000086556276],"about_ca_topic_score_codex":0.010302796,"about_ca_topic_score_gemma":0.93466675,"teacher_disagreement_score":0.924364,"about_ca_system_score_codex":4.7397e-7,"about_ca_system_score_gemma":0.001367933,"threshold_uncertainty_score":0.9962877},"labels":[],"label_agreement":null},{"id":"W2060867461","doi":"10.1139/e03-093","title":"Paleomagnetism and UPb geochronology of the 2.17 Ga Biscotasing dyke swarm, Ontario, Canada: evidence for vertical-axis crustal rotation across the Kapuskasing Zone","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; College of Family Physicians of Canada","funders":"","keywords":"Baddeleyite; Geology; Zircon; Clockwise; Paleomagnetism; Terrane; Geochronology; Rift; Precambrian; Swarm behaviour; Geochemistry; Seismology; Paleontology; Tectonics; Rotation (mathematics); Geometry","score_opus":0.028374264109860874,"score_gpt":0.2275266704033788,"score_spread":0.1991524062935179,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060867461","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99068964,0.002275148,0.00013088132,0.006369919,0.00025470654,0.0000996751,0.000024551395,0.0000011485604,0.00015432376],"genre_scores_gemma":[0.99869156,0.00002024487,0.0007510457,0.00042550187,0.000053171418,3.4429308e-7,0.0000012681112,8.776955e-7,0.000055987493],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987122,0.000055938774,0.00033510025,0.0001722425,0.00028792987,0.0004366074],"domain_scores_gemma":[0.99892426,0.00037533158,0.00016624382,0.00009966351,0.00013708083,0.00029740745],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00064779364,0.00010107626,0.00019406684,0.000051149946,0.00077329355,0.000101021666,0.0004319357,0.000045596247,0.00058055867],"category_scores_gemma":[0.00050615775,0.00005229376,0.00008634892,0.00036784136,0.0012374267,0.00022724828,0.000012963324,0.00018612677,0.0000010719956],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020662335,0.000004066199,0.9735383,0.0000097291095,0.000020158766,0.000018329249,0.0008693086,0.01854387,0.00022526394,0.00007821906,0.00006532664,0.0066068065],"study_design_scores_gemma":[0.00018525458,0.0002615555,0.9935306,0.000080708145,0.000034649795,0.000107962194,0.000602879,0.00070764124,0.0008687835,0.0026238668,0.0009078419,0.00008826014],"about_ca_topic_score_codex":0.97075653,"about_ca_topic_score_gemma":0.9997982,"teacher_disagreement_score":0.029041653,"about_ca_system_score_codex":0.0000120678405,"about_ca_system_score_gemma":0.0029185014,"threshold_uncertainty_score":0.6356711},"labels":[],"label_agreement":null},{"id":"W2061016685","doi":"10.1139/e05-037","title":"Tectonic significance of potential-field anomalies in western Canada: results from the Lithoprobe SNORCLE transect","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Lithosphere; Precambrian; Crust; Seismology; Tectonics; Mantle (geology); Gravity anomaly; Subduction; Terrane; Geophysics; Paleontology","score_opus":0.012003999488134196,"score_gpt":0.18852000359939314,"score_spread":0.17651600411125895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061016685","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99377,0.0010506815,0.000014951474,0.003262784,0.00050724973,0.00008017366,0.00034305238,0.0000013270612,0.0009697781],"genre_scores_gemma":[0.9990572,0.000035627236,0.00030147005,0.00032358203,0.0002245759,1.729543e-7,0.000003522239,0.0000015211032,0.000052377163],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986795,0.000105635525,0.00044005105,0.00014856542,0.0003035099,0.00032271657],"domain_scores_gemma":[0.9991045,0.00025559476,0.0002366269,0.00012286668,0.000062389605,0.00021802059],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00085711846,0.00009152959,0.00020989124,0.000087685396,0.00016976304,0.000101004814,0.0005533402,0.00003504094,0.00047351554],"category_scores_gemma":[0.00009579933,0.000059839465,0.000045409404,0.00029026065,0.00021036001,0.00026251198,0.000003244713,0.000121601945,0.000004649061],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020310322,0.0000206466,0.83850473,0.000022641916,0.00006514472,0.00030497074,0.0042155976,0.12113753,0.0035381408,0.00015186053,0.0018537458,0.029981906],"study_design_scores_gemma":[0.00030590573,0.00019435487,0.98056877,0.00007608596,0.000012691883,0.000017016933,0.00033970553,0.00040949322,0.00398268,0.0001816686,0.013788563,0.00012309203],"about_ca_topic_score_codex":0.9608619,"about_ca_topic_score_gemma":0.9992725,"teacher_disagreement_score":0.14206403,"about_ca_system_score_codex":0.000002794094,"about_ca_system_score_gemma":0.003054283,"threshold_uncertainty_score":0.5418167},"labels":[],"label_agreement":null},{"id":"W2061103892","doi":"10.1139/e00-117","title":"Imbricate architecture of the upper Paleozoic to Jurassic oceanic Cache Creek Terrane, central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Terrane; Subduction; Imbrication; Obduction; Geochemistry; Paleontology; Metamorphism; Petrology; Oceanic crust; Tectonics","score_opus":0.011672115962060706,"score_gpt":0.1765219230458026,"score_spread":0.16484980708374192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061103892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99222064,0.000730411,0.000015873407,0.0020514128,0.00024645147,0.000069774,0.000052907344,0.0000027859053,0.0046097147],"genre_scores_gemma":[0.99760807,0.000029077179,0.00037428766,0.000797033,0.00010648201,1.236669e-7,0.000002029585,0.0000012480459,0.0010816471],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984028,0.00008633992,0.0003463076,0.00019671505,0.0003832732,0.00058461545],"domain_scores_gemma":[0.9986693,0.00008233393,0.00017568345,0.00011994831,0.000098563076,0.000854138],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003909362,0.00008509054,0.00023777703,0.00007447924,0.00049972907,0.0003959068,0.00081880536,0.000048646478,0.01281107],"category_scores_gemma":[0.00023320447,0.00006767145,0.00020285824,0.0011056488,0.0006092122,0.00012015167,0.000011128687,0.0002320601,0.000016891943],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026702216,0.000004014472,0.9864854,0.0000026961113,0.000011583834,0.000052569023,0.000063514046,0.0017405852,0.000034969027,9.778037e-7,0.0011828617,0.010418149],"study_design_scores_gemma":[0.00008489986,0.0001671649,0.9894149,0.00004158203,0.00002267771,0.0003404781,0.00011878195,0.00016170446,0.000022395438,0.0021692668,0.00735335,0.00010282841],"about_ca_topic_score_codex":0.44732395,"about_ca_topic_score_gemma":0.9871528,"teacher_disagreement_score":0.53982884,"about_ca_system_score_codex":0.0000019023825,"about_ca_system_score_gemma":0.00048919837,"threshold_uncertainty_score":0.98809135},"labels":[],"label_agreement":null},{"id":"W2061150798","doi":"10.1139/e06-022","title":"Age of the Cabonga nepheline syenite, Grenville Province, western Quebec","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Pacific Institute for the Mathematical Sciences; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Zircon; Geochemistry; Geology; Anorthosite; Nepheline syenite; Granulite; Charnockite; Quartz monzonite; Migmatite; Terrane; Igneous rock; Metamorphic rock; Pluton; Baddeleyite; Gneiss; Plagioclase; Quartz; Geomorphology","score_opus":0.010094732106206235,"score_gpt":0.1727056864956383,"score_spread":0.16261095438943207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061150798","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.990912,0.0009546981,0.0000101241885,0.0014276003,0.00017349042,0.00004427043,0.000030498899,0.0000017526027,0.0064455336],"genre_scores_gemma":[0.9975867,0.000004590132,0.00025431928,0.00023960021,0.00013501252,6.1949336e-8,0.0000037586058,7.8184024e-7,0.0017751395],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987941,0.00006308071,0.00036296577,0.00013097642,0.0003282823,0.00032060678],"domain_scores_gemma":[0.9991904,0.00008055994,0.00024415465,0.00010457861,0.000101362086,0.0002789613],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042021487,0.00009308257,0.00020255761,0.00014049996,0.0002600771,0.000080210724,0.0005995384,0.00004113547,0.0024109753],"category_scores_gemma":[0.00009657943,0.000047974383,0.00012296811,0.000649134,0.00090923556,0.00014513276,0.000008347462,0.00014583253,0.000022871793],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002276726,0.0000043341383,0.99378234,0.000003575946,0.0000050340996,0.000038075803,0.000018639472,0.004592156,0.00016154713,0.000063310814,0.00016455396,0.0011641755],"study_design_scores_gemma":[0.00008027178,0.00009771466,0.9868263,0.00002074,0.00001795941,0.000038457896,0.000075218624,0.00030650813,0.00029884625,0.0018237323,0.010337405,0.0000768323],"about_ca_topic_score_codex":0.53851527,"about_ca_topic_score_gemma":0.99175096,"teacher_disagreement_score":0.45323572,"about_ca_system_score_codex":0.0000013367489,"about_ca_system_score_gemma":0.0007783177,"threshold_uncertainty_score":0.99850094},"labels":[],"label_agreement":null},{"id":"W2061221613","doi":"10.1139/e00-016","title":"The Abitibi-Grenville Lithoprobe transect part III: introduction","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Archean; Geochemistry; Geochronology; Tectonics; Transect; Petrology; Seismology","score_opus":0.013210067659032794,"score_gpt":0.1945380009028287,"score_spread":0.1813279332437959,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061221613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6560403,0.004129735,0.0050304397,0.19376574,0.004500563,0.00023386674,0.000004025352,0.00003609042,0.13625921],"genre_scores_gemma":[0.9919686,0.00008361691,0.0013871634,0.0002831352,0.00066301884,8.5144825e-7,1.5754742e-7,9.421837e-7,0.0056125456],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99892193,0.00005934264,0.00025026867,0.0001737677,0.00022079925,0.00037387887],"domain_scores_gemma":[0.9992168,0.000058489106,0.00010252478,0.0001921432,0.000117978,0.00031204027],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013444859,0.00007620572,0.00009888454,0.00007122488,0.00096397405,0.00034856467,0.0009622038,0.00003301068,0.00064949575],"category_scores_gemma":[0.00010405793,0.00004870555,0.0000666147,0.0004982283,0.00044146096,0.00033123154,0.000007423218,0.00016644427,0.000020161779],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044921733,0.00006802301,0.021337021,0.000037471884,0.0001109266,0.0005866905,0.009183816,0.037675817,0.0028436335,0.078519665,0.08113586,0.76845616],"study_design_scores_gemma":[0.00012108744,0.00014501075,0.0047970316,0.000020954525,0.0000032847115,0.0005479528,0.00013986732,0.0012352427,0.0010272755,0.004531139,0.98732775,0.00010341341],"about_ca_topic_score_codex":0.00076050265,"about_ca_topic_score_gemma":0.014408128,"teacher_disagreement_score":0.9061919,"about_ca_system_score_codex":0.000004713295,"about_ca_system_score_gemma":0.0007855689,"threshold_uncertainty_score":0.80400735},"labels":[],"label_agreement":null},{"id":"W2061639427","doi":"10.1139/e04-006","title":"Geochemistry of Wistarburgh glass (ca. 1739-1777): implications for batch recipes and distinction from other south Jersey wares","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Saint Mary's University","funders":"Luonnontieteiden ja Tekniikan Tutkimuksen Toimikunta","keywords":"Potash; Mineralogy; Confusion; Lime; Geology; Archaeology; Bottle; Lead glass; Glass production; Glass recycling; Geochemistry; Potassium; Metallurgy; Materials science; History","score_opus":0.01993358843686694,"score_gpt":0.20770462951195917,"score_spread":0.18777104107509224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061639427","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944322,0.0009616998,0.00035856676,0.0024128547,0.00008784428,0.000048169866,0.00046312498,0.0000027332803,0.0012328033],"genre_scores_gemma":[0.99704224,0.000016405667,0.0026317898,0.00013275795,0.000101951046,4.1905923e-7,0.00002034363,0.0000010241666,0.000053048487],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99913603,0.000015664926,0.00028095028,0.00017907238,0.00013372036,0.0002545677],"domain_scores_gemma":[0.999017,0.00013971036,0.00021218954,0.00007970238,0.00012967705,0.0004217158],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000283929,0.000090511094,0.00018996125,0.00009056469,0.00026078956,0.00006330507,0.00023983863,0.00005321412,0.0017135681],"category_scores_gemma":[0.00025572567,0.00006257183,0.00009090595,0.00027764548,0.0005781301,0.00014582097,0.0000040987115,0.00008577706,0.0000041074145],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013459023,0.0000061245682,0.9942995,0.0000063887373,0.000022975248,0.0000022370282,0.00019767131,0.0018799521,0.00073152967,0.0000832858,0.00007008463,0.0026868016],"study_design_scores_gemma":[0.00026311402,0.00019890988,0.93899715,0.000040829327,0.0000502655,0.00001644373,0.00064723607,0.00040401382,0.0018812985,0.054543674,0.0028216417,0.0001354508],"about_ca_topic_score_codex":0.048493598,"about_ca_topic_score_gemma":0.26049608,"teacher_disagreement_score":0.21200247,"about_ca_system_score_codex":0.0000019852334,"about_ca_system_score_gemma":0.00034593674,"threshold_uncertainty_score":0.999199},"labels":[],"label_agreement":null},{"id":"W2061710355","doi":"10.1139/e02-032","title":"Flank collapse at Mount Wrangell, Alaska, recorded by volcanic mass-flow deposits in the Copper River lowland","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Facies; Volcano; Debris flow; Mudflow; Geochemistry; Debris; Geomorphology; Volcanic rock; Pyroclastic rock; Landslide; Structural basin","score_opus":0.01014239365508985,"score_gpt":0.18702818690136583,"score_spread":0.17688579324627599,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061710355","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98699266,0.0014556905,0.000006546013,0.001878658,0.0003692609,0.000102447484,0.0000135060645,0.0000020733323,0.009179145],"genre_scores_gemma":[0.9968331,0.00027174232,0.00027418262,0.0006804526,0.00005086113,0.0000010312971,7.7437164e-7,0.000005148119,0.0018827171],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985916,0.00008774555,0.0002665355,0.00017786576,0.0004250825,0.00045116022],"domain_scores_gemma":[0.99928707,0.000056996156,0.00012992928,0.00011992495,0.000015157274,0.00039094026],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006390262,0.00011571908,0.00014885959,0.00009585293,0.00044093255,0.00012830654,0.00056085736,0.00007458328,0.0035434125],"category_scores_gemma":[0.000037041653,0.00006701397,0.00006457932,0.00054316246,0.00058683206,0.0002725519,0.000018726936,0.00021237308,0.00027279585],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011665799,0.000022159309,0.8957133,0.0000026347177,0.000013548048,0.0003662935,0.0023984218,0.004075603,0.00074260007,0.000008126517,0.094092995,0.0025526287],"study_design_scores_gemma":[0.001612534,0.00081600755,0.51192856,0.00012121061,0.000050497165,0.001056374,0.00078987103,0.014863206,0.0005288748,0.00023690765,0.4674553,0.0005406602],"about_ca_topic_score_codex":0.0065971236,"about_ca_topic_score_gemma":0.2868007,"teacher_disagreement_score":0.38378474,"about_ca_system_score_codex":0.00011153109,"about_ca_system_score_gemma":0.00009503347,"threshold_uncertainty_score":0.9973675},"labels":[],"label_agreement":null},{"id":"W2061721984","doi":"10.1139/e10-066","title":"U–Pb geochronology in Liverpool Land and Canning Land, East Greenland — the complex record of a polyphase Caledonian orogenyThis article is one of a series of papers published in this Special Issue on the theme of<i>Geochronology</i>in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Terrane; Geochemistry; Metamorphism; Gneiss; Geochronology; Proterozoic; Plutonism; Nappe; Paleontology; Magmatism; Metamorphic rock; Tectonics","score_opus":0.03255609186665125,"score_gpt":0.19554401938654106,"score_spread":0.1629879275198898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061721984","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943015,0.00056896143,4.7219638e-7,0.002077422,0.000051447023,0.00008703375,0.00008038303,5.737025e-7,0.0028322383],"genre_scores_gemma":[0.9994677,0.000073669165,0.0002909118,0.00009685874,0.00004903376,3.404799e-7,0.0000013955147,0.0000010541476,0.000019078441],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998543,0.0001871078,0.000608925,0.00015751451,0.00020280585,0.00030059295],"domain_scores_gemma":[0.9989544,0.00024150699,0.0004450191,0.00012134251,0.00009657329,0.00014115537],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010313507,0.00010409409,0.00046827254,0.00033262427,0.00006838096,0.000011879479,0.00041967243,0.000069956055,0.017058741],"category_scores_gemma":[0.00028709302,0.000057852863,0.000075243246,0.0007489486,0.0015880933,0.00015304371,0.000017967432,0.00021312298,0.0000016136445],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013698109,0.000031633743,0.99258685,0.000014327816,0.000024796831,0.000020851623,0.0030392245,0.00015509232,0.000493958,0.00004418857,0.000026917047,0.0034251735],"study_design_scores_gemma":[0.00042539454,0.00077876763,0.99132234,0.000093174844,0.000019077215,0.000026741898,0.002087505,0.0004222666,0.0032847326,0.0012432409,0.0002260627,0.00007071388],"about_ca_topic_score_codex":0.27632356,"about_ca_topic_score_gemma":0.8571416,"teacher_disagreement_score":0.58081806,"about_ca_system_score_codex":0.0000028727325,"about_ca_system_score_gemma":0.00034419468,"threshold_uncertainty_score":0.9838398},"labels":[],"label_agreement":null},{"id":"W2061790401","doi":"10.1139/e07-053","title":"Landform assemblages produced by the Laurentide Ice Sheet in northeastern British Columbia and adjacent Northwest Territories — constraints on glacial lakes and patterns of ice retreatThis article is one of a selection of papers published in this Special Issue on the theme <i>Geology of northeastern British Columbia and northwestern Alberta: diamonds, shallow gas, gravel, and glaciers</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Deglaciation; Ice sheet; Meltwater; Wisconsin glaciation; Ice stream; Glacial period; Ice shelf; Oceanography; Paleontology; Physical geography; Geomorphology; Sea ice; Cryosphere; Geography","score_opus":0.010691340491327864,"score_gpt":0.19312977680839624,"score_spread":0.18243843631706838,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061790401","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976924,0.00052087894,8.300362e-8,0.00067530404,0.00012225019,0.00023943618,0.0002000977,0.0000010637491,0.00054849265],"genre_scores_gemma":[0.99928945,0.00040476792,0.000007699149,0.00008900461,0.00007099267,0.0000013566744,0.000009650799,0.0000028825432,0.00012419716],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982921,0.00023989237,0.0005087451,0.00028080153,0.00031894853,0.00035954115],"domain_scores_gemma":[0.99871796,0.0005036704,0.00033900217,0.00010123691,0.00014300531,0.00019509277],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008650318,0.00010816744,0.00042633238,0.00010886711,0.00047310747,0.00028883226,0.0002317517,0.00010360167,0.0011354708],"category_scores_gemma":[0.00023024275,0.00010695723,0.000034845663,0.00033714526,0.0025577922,0.00027323762,0.000014966048,0.00028015464,2.796286e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005485557,0.000037585232,0.9953954,0.000043296997,0.000027784099,0.000039455936,0.0020616425,0.000007628956,0.000028024993,0.0000011627542,0.00006953655,0.0022336286],"study_design_scores_gemma":[0.0006088785,0.00079849875,0.9963563,0.00020117137,0.000016006454,0.0004300818,0.0011715655,0.000074335716,0.00011356875,0.000032516444,0.000104424966,0.00009267208],"about_ca_topic_score_codex":0.82586336,"about_ca_topic_score_gemma":0.99983776,"teacher_disagreement_score":0.17397445,"about_ca_system_score_codex":0.0000016982335,"about_ca_system_score_gemma":0.00030534202,"threshold_uncertainty_score":0.9997776},"labels":[],"label_agreement":null},{"id":"W2061995609","doi":"10.1139/e06-118","title":"Geology of the shear-hosted Brookbank gold prospect in the Beardmore–Geraldton belt, Wabigoon subprovince, Ontario","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Greenstone belt; Geochemistry; Shear zone; Greenschist; Archean; Ankerite; Pyrite; Sericite; Metamorphic rock; Quartz; Seismology; Paleontology; Siderite","score_opus":0.014089749392839704,"score_gpt":0.1893408875573568,"score_spread":0.1752511381645171,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061995609","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98464537,0.0005595172,0.0000034277584,0.0024395627,0.00021753067,0.0001065074,0.0000066238053,0.0000015996259,0.012019869],"genre_scores_gemma":[0.99860936,0.0000064916985,0.00021794844,0.0006988184,0.00007024493,1.4813548e-7,0.0000021838036,8.6336945e-7,0.00039393056],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982273,0.000112852074,0.00048101315,0.00018033982,0.00045042447,0.00054808066],"domain_scores_gemma":[0.9989976,0.00021355228,0.00025476233,0.00015347775,0.000104209634,0.00027638173],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0022505599,0.000116860865,0.00025157354,0.00022562876,0.00024189737,0.00006105325,0.0010045492,0.00007226436,0.0022344256],"category_scores_gemma":[0.00021043842,0.000054006847,0.00015938921,0.0011226834,0.0010753887,0.00016854942,0.000011586965,0.0004096695,0.000012798098],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012249341,0.0000076591905,0.9970946,0.0000025962056,0.0000067907927,0.00003887249,0.00037804514,0.00084457884,0.000049229286,0.00017196343,0.0000887629,0.0013046724],"study_design_scores_gemma":[0.00012432283,0.00028912546,0.9919649,0.0000202842,0.0000131116,0.00010179259,0.0002629208,0.000110609675,0.00025631717,0.003650656,0.0031263712,0.00007964022],"about_ca_topic_score_codex":0.6144605,"about_ca_topic_score_gemma":0.9948241,"teacher_disagreement_score":0.38036358,"about_ca_system_score_codex":0.0000061833357,"about_ca_system_score_gemma":0.0009178043,"threshold_uncertainty_score":0.9986777},"labels":[],"label_agreement":null},{"id":"W2062117964","doi":"10.1139/e10-069","title":"Introduction au numéro spécial sur<i>Albertosaurus</i>","year":2010,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology","score_opus":0.01779900496787494,"score_gpt":0.2077479395550375,"score_spread":0.18994893458716255,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062117964","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8277901,0.008398864,0.00002708516,0.0551488,0.08228101,0.00007707644,0.00010515577,0.000004374442,0.026167545],"genre_scores_gemma":[0.96970785,0.00017088618,0.0012486527,0.00056232803,0.023316817,1.8861701e-7,0.000011830358,0.0000028949553,0.0049785823],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99773294,0.00023142193,0.00049760204,0.00030331753,0.00025750627,0.0009772066],"domain_scores_gemma":[0.99784166,0.00024962504,0.00033785854,0.00014806094,0.00021699938,0.0012058063],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0020544496,0.00018880874,0.0003043267,0.00043987297,0.001127401,0.000120881596,0.00066706934,0.0003299151,0.02711585],"category_scores_gemma":[0.00078887865,0.00016239368,0.00014091165,0.00062526995,0.004234326,0.0010776774,0.0000062206177,0.0008652837,0.0005742379],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025908965,0.000013232477,0.93874115,0.0000089796,0.00002599218,0.00016521329,0.00034304644,0.0004787186,0.00017347373,0.0029173375,0.04307419,0.014032785],"study_design_scores_gemma":[0.00012802654,0.00035771946,0.4520525,0.000014418766,0.00001784401,0.002186664,0.000107462925,0.0002748432,0.00004523556,0.0013183451,0.5433677,0.00012926797],"about_ca_topic_score_codex":0.10005979,"about_ca_topic_score_gemma":0.9732413,"teacher_disagreement_score":0.8731815,"about_ca_system_score_codex":0.0000061601827,"about_ca_system_score_gemma":0.008013032,"threshold_uncertainty_score":0.99847555},"labels":[],"label_agreement":null},{"id":"W2062209062","doi":"10.1139/e00-079","title":"The conglomerate of Churn Creek: Late Cretaceous basin evolution along the InsularIntermontane superterrane boundary, southern British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Conglomerate; Cretaceous; Geochemistry; Canyon; Volcanic rock; Clastic rock; Paleontology; Structural basin; Volcano; Geomorphology","score_opus":0.014067160127463497,"score_gpt":0.18750831324871975,"score_spread":0.17344115312125624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062209062","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9898952,0.0058277682,0.000030851465,0.00096400274,0.00039933785,0.00008676386,0.00005842157,0.0000037339714,0.0027339193],"genre_scores_gemma":[0.99814314,0.00029354333,0.00006398727,0.00017998724,0.00006590111,2.6169252e-7,0.0000034374796,0.0000015462396,0.00124822],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99863136,0.000119346645,0.00042303393,0.00011348063,0.00031584248,0.0003969318],"domain_scores_gemma":[0.99894625,0.00016855702,0.0002467414,0.000107660155,0.0002495891,0.00028117799],"candidate_categories":["sts","scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013533945,0.00007359228,0.00016938795,0.000058965816,0.0018245172,0.001464022,0.00064986886,0.000046889665,0.002965025],"category_scores_gemma":[0.00021625434,0.000053249973,0.00008225652,0.0005174177,0.0013343324,0.00040963542,0.000006976709,0.00019580133,0.000025066092],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000072200783,0.0000029680675,0.9841999,0.0000039000042,0.000013232629,0.000077910845,0.00037194166,0.0006643256,0.0000036114182,0.0000062630716,0.0003113318,0.014337427],"study_design_scores_gemma":[0.00013746518,0.00032448166,0.9684741,0.00005238807,0.000013008631,0.0012622767,0.0017165665,0.0017286027,0.0000020843083,0.001453766,0.024748957,0.000086289205],"about_ca_topic_score_codex":0.61805654,"about_ca_topic_score_gemma":0.9946451,"teacher_disagreement_score":0.37658858,"about_ca_system_score_codex":0.0000026249677,"about_ca_system_score_gemma":0.0008996464,"threshold_uncertainty_score":0.9995726},"labels":[],"label_agreement":null},{"id":"W2062432606","doi":"10.1139/e09-051","title":"The Lower Triassic Sulphur Mountain Formation in the Wapiti Lake area: lithostratigraphy, conodont biostratigraphy, and a new biozonation for the lower Olenekian (Smithian)Earth Science Sector (ESS) Contribution 20080714.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta; Geological Survey of Canada","funders":"","keywords":"Conodont; Geology; Biostratigraphy; Paleontology; Ladinian; Cyclostratigraphy; Lithostratigraphy; Early Triassic; Dolomite; Group (periodic table); Sedimentary rock; Permian; Geochemistry","score_opus":0.025702534739080855,"score_gpt":0.23401832936712166,"score_spread":0.2083157946280408,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062432606","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9635937,0.016197668,0.0006915868,0.015656,0.00091748696,0.00075456727,0.0001279527,0.000007711069,0.0020533344],"genre_scores_gemma":[0.9988364,0.00030408963,0.0002640914,0.00044533584,0.00013246352,0.0000020231778,0.0000031800066,7.9493554e-7,0.000011649991],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99781597,0.00018974545,0.0005373619,0.00025013796,0.0005228968,0.0006838816],"domain_scores_gemma":[0.9980526,0.000750246,0.00037789685,0.00018013011,0.00024769444,0.00039145633],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.004509513,0.00019251632,0.00021454973,0.00046994342,0.002552126,0.001007223,0.00085904065,0.00009665917,0.000039105096],"category_scores_gemma":[0.0004226036,0.00009641747,0.00014169967,0.0013413617,0.0020859728,0.0014213971,0.0000012241899,0.00031980668,0.0000012230272],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051662093,0.00008411047,0.58720034,0.0000139995445,0.00007139461,0.0001120836,0.0043765088,0.0005759582,0.0004167702,0.022599548,0.0014438962,0.38258874],"study_design_scores_gemma":[0.00058713066,0.0013487181,0.98709553,0.000052005926,0.000021939404,0.00017557928,0.0012323557,0.0021822173,0.00013005047,0.0040969965,0.0029320316,0.00014544468],"about_ca_topic_score_codex":0.0029783936,"about_ca_topic_score_gemma":0.74756485,"teacher_disagreement_score":0.74458647,"about_ca_system_score_codex":0.0000032138864,"about_ca_system_score_gemma":0.0016937006,"threshold_uncertainty_score":0.9987464},"labels":[],"label_agreement":null},{"id":"W2062877836","doi":"10.1139/e00-081","title":"Integrated chitinozoan, conodont, and graptolite biostratigraphy from the upper part of the Cape Cormorant Formation (Middle Ordovician), western Newfoundland","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Geology; Conodont; Paleontology; Foreland basin; Biostratigraphy; Ordovician; Fauna; Paleocurrent; Turbidite; Clastic rock; Structural basin; Ecology","score_opus":0.028732270943607634,"score_gpt":0.20606549830794316,"score_spread":0.17733322736433552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062877836","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9845754,0.007649927,0.000017877861,0.0018159988,0.00046677003,0.000098761746,0.0001313732,0.0000025316476,0.0052413414],"genre_scores_gemma":[0.9993849,0.0001486163,0.00010738263,0.0002719332,0.00006823738,1.8219649e-7,0.0000032501362,5.842095e-7,0.000014928702],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883026,0.00014623134,0.0003828545,0.00012259302,0.00021705672,0.00030099635],"domain_scores_gemma":[0.9989974,0.00018946508,0.00033894618,0.000121053534,0.00008785868,0.00026531352],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005509115,0.000118493204,0.00019438438,0.00014980891,0.0007247112,0.00016690478,0.0004675454,0.000060895974,0.00017373338],"category_scores_gemma":[0.00006400784,0.000059698534,0.00009957659,0.00052042,0.0013660912,0.000518885,0.0000013295254,0.00020885064,0.0000017164621],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012427587,0.000002186536,0.99162066,0.0000017599052,0.00001688528,0.000010253608,0.0007124934,0.000023860488,0.000015695698,0.00012726625,0.000035475066,0.0074210633],"study_design_scores_gemma":[0.00018938683,0.00015919135,0.99255437,0.00007934782,0.000022014163,0.00020670812,0.0010747865,0.00033063663,0.000028142762,0.0007804267,0.0044943807,0.00008063915],"about_ca_topic_score_codex":0.062236585,"about_ca_topic_score_gemma":0.95585907,"teacher_disagreement_score":0.89362246,"about_ca_system_score_codex":8.0568344e-7,"about_ca_system_score_gemma":0.0005328642,"threshold_uncertainty_score":0.94400805},"labels":[],"label_agreement":null},{"id":"W2063321507","doi":"10.1139/e04-027","title":"Paleoenvironmental interpretation of the paleosols and sediments at the Stampede site (DjOn-26), Cypress Hills, Alberta","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Paleosol; Geology; Radiocarbon dating; Sequence (biology); Arid; Fluvial; Archaeology; Cypress; Pedogenesis; Period (music); Deposition (geology); Physical geography; Paleontology; Hydrology (agriculture); Geochemistry; Sediment; Loess; Soil water; Geography; Soil science; Ecology; Structural basin","score_opus":0.011068521385669126,"score_gpt":0.21131537982853218,"score_spread":0.20024685844286305,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2063321507","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937785,0.0018403156,0.000004218242,0.002355027,0.0002978597,0.00009907869,0.00002730894,8.265116e-7,0.0015968233],"genre_scores_gemma":[0.9994134,0.000075889206,0.000058446814,0.00027051452,0.000023130642,2.2053203e-7,0.0000025145193,0.0000012132783,0.00015467533],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99892384,0.00015296365,0.00022668947,0.00012765724,0.00026263105,0.00030624148],"domain_scores_gemma":[0.99918544,0.00025068573,0.00018446783,0.00011189405,0.00002740684,0.0002400797],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006818263,0.000081184655,0.0001279395,0.000092884715,0.00062468747,0.00004636186,0.00042162943,0.000051291412,0.00081543066],"category_scores_gemma":[0.00010667187,0.000042659332,0.00005449163,0.00018845148,0.0020362416,0.00021453567,0.000017789427,0.00018738773,0.000032017964],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011806494,0.0000024366311,0.9956996,0.0000036138729,0.000011955128,0.000009695607,0.0009732424,0.0029777181,0.000017792745,0.000022459342,0.00001971847,0.0002499849],"study_design_scores_gemma":[0.00020386832,0.00016590692,0.9975305,0.000037899128,0.000012533778,0.0002694129,0.00036718757,0.00024668174,0.00025916466,0.00036855988,0.00048615213,0.000052125342],"about_ca_topic_score_codex":0.012567955,"about_ca_topic_score_gemma":0.8286318,"teacher_disagreement_score":0.8160639,"about_ca_system_score_codex":0.0000010086394,"about_ca_system_score_gemma":0.00035085066,"threshold_uncertainty_score":0.99400747},"labels":[],"label_agreement":null},{"id":"W2063456955","doi":"10.1139/e09-072","title":"An overview of the Canadian Cordilleran lithospheric mantleThis article is one of a series of papers published in this Special Issue on the theme <i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Lithosphere; Xenolith; Mantle (geology); Craton; Geochemistry; Partial melting; Basalt; Olivine; Tectonics; Seismology","score_opus":0.017774908434866163,"score_gpt":0.1987538148758262,"score_spread":0.18097890644096004,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2063456955","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98212093,0.0011705824,2.818258e-7,0.011682839,0.00012455169,0.00013364274,0.000051538173,5.9853875e-7,0.0047150054],"genre_scores_gemma":[0.99920803,0.000095022726,0.00021461702,0.000365599,0.0000664906,4.550336e-7,6.3694335e-7,0.0000010071373,0.00004816038],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861276,0.00015913654,0.0004604097,0.00013654112,0.00038245952,0.00024868487],"domain_scores_gemma":[0.99865484,0.00024905993,0.00043704634,0.00017865673,0.00024493324,0.00023543357],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016044684,0.0000929035,0.00031800094,0.00010410319,0.00020389931,0.00005524745,0.0006109156,0.000056784098,0.012171957],"category_scores_gemma":[0.00068593794,0.00004070637,0.00009542343,0.0011722972,0.0025346181,0.00022639774,0.000008392404,0.00024473036,9.466683e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008035758,0.000024565288,0.99254143,0.00004817824,0.000033028875,0.0000024660203,0.002157961,0.00024863286,0.0006056586,0.0019392278,0.00016548575,0.0021530248],"study_design_scores_gemma":[0.0003722925,0.00044965761,0.97830427,0.00014418065,0.00005181285,0.000017799492,0.0020394798,0.00060480344,0.005059588,0.009975573,0.0028760382,0.000104524326],"about_ca_topic_score_codex":0.6472046,"about_ca_topic_score_gemma":0.98204017,"teacher_disagreement_score":0.33483556,"about_ca_system_score_codex":0.0000028563245,"about_ca_system_score_gemma":0.0010722259,"threshold_uncertainty_score":0.988731},"labels":[],"label_agreement":null},{"id":"W2063690622","doi":"10.1139/e04-104","title":"U/Pb geochronological constraints on Neoarchean tectonism: multiple compressional events in the northwestern Hearne Domain, Western Churchill Province, Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geoscience BC; Geological Survey of Canada","funders":"","keywords":"Geology; Metamorphism; Sinistral and dextral; Shear zone; Nappe; Geochemistry; Zircon; Plutonism; Shear (geology); Seismology; Greenstone belt; Geomorphology; Archean; Pluton; Petrology; Tectonics","score_opus":0.018115100987211634,"score_gpt":0.20459392745491495,"score_spread":0.1864788264677033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2063690622","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98836344,0.00025212736,0.000009200265,0.008481187,0.00012728624,0.00010904124,0.000061384904,0.0000028942097,0.0025934617],"genre_scores_gemma":[0.9965856,0.0000068084664,0.00044510784,0.00276168,0.00015236138,4.655071e-7,0.000011606066,0.0000011682424,0.000035208137],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997913,0.00017767443,0.00041645183,0.00025305047,0.0006186978,0.00062112766],"domain_scores_gemma":[0.9986809,0.00039137492,0.00017503943,0.00011847418,0.000060141963,0.0005740643],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00078854465,0.00016296675,0.0002616897,0.00017363424,0.00041006057,0.000067178466,0.0008299338,0.000059583384,0.0029087642],"category_scores_gemma":[0.00011996919,0.00008640412,0.0000924211,0.0003852852,0.00089038815,0.00017041466,0.000010994925,0.00045054223,0.000038415],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012255327,0.000019333856,0.98087245,0.0000018170699,0.0000076240453,0.00015568388,0.00011108883,0.008698011,0.000016427344,0.000020504036,0.00007513891,0.010009636],"study_design_scores_gemma":[0.0003225904,0.00028557083,0.9905431,0.00003776462,0.0000053325266,0.00018726556,0.0003228102,0.00064380514,0.00004632987,0.00079365476,0.006678042,0.00013368193],"about_ca_topic_score_codex":0.6856716,"about_ca_topic_score_gemma":0.9991539,"teacher_disagreement_score":0.31348225,"about_ca_system_score_codex":0.000009056791,"about_ca_system_score_gemma":0.0019979477,"threshold_uncertainty_score":0.9980027},"labels":[],"label_agreement":null},{"id":"W2064022009","doi":"10.1139/e09-065","title":"Provenance of North American Triassic strata from west-central and southeastern Yukon: correlations with coeval strata in the Western Canada Sedimentary Basin and Canadian Arctic Islands","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Pacific Institute for the Mathematical Sciences; University of British Columbia; Geological Survey of Canada","funders":"","keywords":"Geology; Terrane; Zircon; Provenance; Paleozoic; Sedimentary rock; Paleontology; Clastic rock; Geochemistry; Tectonics","score_opus":0.009443170046455519,"score_gpt":0.1741293099616916,"score_spread":0.1646861399152361,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064022009","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99569577,0.00018698789,0.0000023330317,0.0033488409,0.00009730054,0.000074309086,0.00039185295,6.349882e-7,0.0002019982],"genre_scores_gemma":[0.9992154,0.000010057335,0.00014250033,0.00054212176,0.000059969687,2.1087928e-7,0.000020573945,9.058455e-7,0.000008235235],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988492,0.000070675895,0.00025613853,0.00017529751,0.0002706106,0.00037808876],"domain_scores_gemma":[0.99882,0.00017209942,0.00017907147,0.00009271077,0.000055285564,0.00068085553],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030247387,0.00010880565,0.00021619558,0.00012299327,0.0002048356,0.00009989955,0.00032349236,0.00002094769,0.00025507074],"category_scores_gemma":[0.000058261114,0.00006158599,0.000022560102,0.00047931087,0.00084050803,0.000186923,0.0000037733862,0.0002996106,6.1983735e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010351299,0.0000030965045,0.99742657,0.0000022727738,0.000010726592,0.00006179274,0.00025486312,0.0003603784,0.0000013720429,0.0000062998256,0.000013269879,0.0018490015],"study_design_scores_gemma":[0.00019751024,0.00023218695,0.99718815,0.000019945557,0.000027909973,0.00007110321,0.00078226556,0.0009909037,0.0000033061604,0.0001278016,0.00026961713,0.00008928138],"about_ca_topic_score_codex":0.9970462,"about_ca_topic_score_gemma":0.9999946,"teacher_disagreement_score":0.0035196827,"about_ca_system_score_codex":0.0000025863096,"about_ca_system_score_gemma":0.0028428424,"threshold_uncertainty_score":0.50430804},"labels":[],"label_agreement":null},{"id":"W2064258460","doi":"10.1139/e01-015","title":"Apatite fission-track evidence of widespread Eocene heating and exhumation in the Yukon-Tanana Upland, interior Alaska","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Fission track dating; Geothermal gradient; Geochemistry; Metamorphic rock; Zircon; Paleontology","score_opus":0.03219095356592107,"score_gpt":0.23518311722858876,"score_spread":0.2029921636626677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064258460","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940205,0.0026436127,0.000019198776,0.002204764,0.00007005292,0.000041916297,0.000004554904,0.0000010892587,0.0009942901],"genre_scores_gemma":[0.9990986,0.00020857085,0.0003844481,0.00025432845,0.000036961243,1.2276173e-7,0.0000012201556,4.7489704e-7,0.000015272477],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99894786,0.00009626586,0.00034923843,0.00012116175,0.0002525206,0.00023294306],"domain_scores_gemma":[0.9990079,0.00044747218,0.00019590263,0.0000648921,0.0000590776,0.00022474595],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011857044,0.00007496727,0.00017361979,0.00019580254,0.00017658547,0.00008910497,0.0003300807,0.000031296564,0.0019047209],"category_scores_gemma":[0.0005578227,0.000040567567,0.000048416427,0.00062654633,0.0003624959,0.00038709256,0.0000047011185,0.00013143783,0.0000063746343],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008992524,0.0000021455076,0.988032,0.0000071195227,0.0000030601234,0.000030263383,0.00041963204,0.0010986082,0.00008433975,0.000012934509,0.000019008525,0.010281935],"study_design_scores_gemma":[0.000076228294,0.00026416974,0.99217206,0.00028911888,0.00001035021,0.00012866208,0.00071365933,0.0036653257,0.00015970832,0.002295958,0.00015807891,0.0000666884],"about_ca_topic_score_codex":0.025341898,"about_ca_topic_score_gemma":0.36783516,"teacher_disagreement_score":0.34249327,"about_ca_system_score_codex":0.0000011123036,"about_ca_system_score_gemma":0.0001748412,"threshold_uncertainty_score":0.9990077},"labels":[],"label_agreement":null},{"id":"W2064273578","doi":"10.1139/e02-030","title":"A multistage magmatic history for the genesis of the Orford ophiolite (Quebec, Canada): a study of the Mont Chagnon massif","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval","funders":"","keywords":"Geology; Massif; Ophiolite; Geochemistry; Oceanic crust; Island arc; Back-arc basin; Pillow lava; Subduction; Partial melting; Volcanic arc; Volcano; Felsic; Basalt; Magma; Volcanic rock; Paleontology; Tectonics","score_opus":0.029008646421114035,"score_gpt":0.17452170656660235,"score_spread":0.14551306014548832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064273578","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99179405,0.0038646942,0.000004046776,0.0031602748,0.00037785992,0.0002156222,0.00003400243,7.3589615e-7,0.0005486952],"genre_scores_gemma":[0.99872756,0.000020283904,0.00005574797,0.00031337232,0.00004298291,0.0000010225602,2.4163006e-7,0.0000010260356,0.0008377463],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99860907,0.00011250191,0.0003991006,0.0001236529,0.00046979423,0.00028590407],"domain_scores_gemma":[0.9987238,0.0003263589,0.00040762054,0.00019863507,0.00013032963,0.00021327876],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00054789806,0.0000975911,0.00022544907,0.00006711286,0.00039629696,0.00002421757,0.0010256158,0.000026081714,0.0025466154],"category_scores_gemma":[0.00030703572,0.000038523223,0.00016225473,0.0004465029,0.0006321795,0.00007916232,0.000012881127,0.00012323716,0.0000010079864],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000065809977,0.00002172024,0.98708797,0.000015174573,0.000044983146,0.000007500335,0.0011150289,0.0068780505,0.000039260987,0.00002398227,0.0020362465,0.0027235113],"study_design_scores_gemma":[0.00015732751,0.00014278025,0.9815677,0.00002268385,0.000068217225,0.000008795849,0.002354969,0.009797058,0.000049003786,0.00016909906,0.005596447,0.000065928856],"about_ca_topic_score_codex":0.94712484,"about_ca_topic_score_gemma":0.9993164,"teacher_disagreement_score":0.052191604,"about_ca_system_score_codex":0.000010295227,"about_ca_system_score_gemma":0.0008907153,"threshold_uncertainty_score":0.99836516},"labels":[],"label_agreement":null},{"id":"W2064622053","doi":"10.1139/e05-082","title":"The Edison magnetite deposits in the context of pre-, syn-, and post-orogenic metallogenesis in the Grenville Highlands of New Jersey","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Gneiss; Pegmatite; Rhyolite; Metamorphic rock; Feldspar; Country rock; Volcanic rock; Paleontology","score_opus":0.01171098872514988,"score_gpt":0.1899366619419657,"score_spread":0.17822567321681582,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064622053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9801742,0.011276845,8.125899e-7,0.007794332,0.00004424385,0.00006315553,0.00001057205,3.6038503e-7,0.00063547795],"genre_scores_gemma":[0.99901533,0.00029378582,0.0001021859,0.0004970631,0.00004617763,1.9929135e-7,0.0000010512326,4.8702117e-7,0.000043720884],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988461,0.0001540726,0.0003471773,0.00010285048,0.00029652787,0.00025324977],"domain_scores_gemma":[0.99911433,0.0004124509,0.00017002161,0.00009065627,0.00005265305,0.00015987859],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013193536,0.0000772275,0.00017996471,0.00012943576,0.00017092054,0.000060426,0.0006529741,0.000033890014,0.0003729402],"category_scores_gemma":[0.00018731506,0.000030889376,0.00008358694,0.0006054113,0.00055958075,0.00011115967,0.000006085544,0.00012562193,0.00000237586],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019495435,0.000007391136,0.97385186,0.000003202891,0.000012988665,0.000012350122,0.0016992551,0.0008581474,0.0001421247,0.00011137764,0.000053520595,0.023228275],"study_design_scores_gemma":[0.0001333368,0.0002918923,0.9932915,0.000014912839,0.000025078798,0.00006104547,0.0028724587,0.00040652996,0.0002247035,0.000520827,0.0021089092,0.000048821286],"about_ca_topic_score_codex":0.072112046,"about_ca_topic_score_gemma":0.9166859,"teacher_disagreement_score":0.84457386,"about_ca_system_score_codex":8.482304e-7,"about_ca_system_score_gemma":0.00025456707,"threshold_uncertainty_score":0.93406683},"labels":[],"label_agreement":null},{"id":"W2064751826","doi":"10.1139/e05-102","title":"Cenozoic ichthyolith biostratigraphy: Tofino Basin, British Columbia","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Luonnontieteiden ja Tekniikan Tutkimuksen Toimikunta; Natural Sciences and Engineering Research Council of Canada; Memorial University of Newfoundland; Shell Canada; University of Victoria","keywords":"Geology; Paleontology; Terrane; Unconformity; Cenozoic; Cretaceous; Biostratigraphy; Basement; Tectonics; Structural basin","score_opus":0.014372768731541054,"score_gpt":0.20565211370593692,"score_spread":0.19127934497439586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064751826","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9593576,0.003003576,0.000004488584,0.0007098699,0.00054894376,0.00006630555,0.00005015622,0.0000053516314,0.036253676],"genre_scores_gemma":[0.99793094,0.000039620467,0.0007023584,0.00027355223,0.00015743735,1.4514056e-7,0.000008140323,0.0000014787596,0.0008863433],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983226,0.00014949648,0.00033881777,0.00019699283,0.0002921819,0.00069992465],"domain_scores_gemma":[0.99889755,0.00014778224,0.00015322184,0.00009472567,0.00014822632,0.00055849383],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010211563,0.00008387864,0.00023134662,0.00025823957,0.0008762417,0.0005860912,0.0005217966,0.00010115481,0.0075809513],"category_scores_gemma":[0.0000964193,0.00009563653,0.00009938227,0.0006775922,0.0014882936,0.0003820224,0.000003024965,0.0002721026,0.00010150481],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002900236,0.0000037714885,0.99640065,0.0000041460958,0.000006983957,0.00045821225,0.000018238372,0.00012737447,0.0000011347641,0.000047274825,0.0023716956,0.00055761077],"study_design_scores_gemma":[0.00015316585,0.0003422759,0.9860892,0.000028321447,0.000007945611,0.0016490517,0.00008790038,0.00007281194,0.000009201036,0.0024980619,0.008948162,0.00011384463],"about_ca_topic_score_codex":0.47995955,"about_ca_topic_score_gemma":0.99712086,"teacher_disagreement_score":0.5171613,"about_ca_system_score_codex":3.4493658e-7,"about_ca_system_score_gemma":0.0016882455,"threshold_uncertainty_score":0.99332625},"labels":[],"label_agreement":null},{"id":"W2065419565","doi":"10.1139/e04-016","title":"A reevaluation of the enigmatic Permian synapsid<i>Watongia</i>and of its stratigraphic significance","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"University of California Museum of Paleontology","keywords":"Affinities; Geology; Permian; Paleontology; Vertebrate; Skull; Dentition; Biology","score_opus":0.023413133457216143,"score_gpt":0.21939604704051596,"score_spread":0.19598291358329983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065419565","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9925644,0.0045402353,0.00001575395,0.0011618608,0.00026042684,0.000077882825,0.000029943241,7.926476e-7,0.0013487048],"genre_scores_gemma":[0.99945205,0.00007877219,0.0003675687,0.00006166355,0.000022079548,1.2393421e-7,6.4294585e-7,4.5940644e-7,0.000016645949],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99911493,0.00012216109,0.00029952786,0.00009164353,0.0001846993,0.00018704162],"domain_scores_gemma":[0.99926406,0.000100552774,0.00029902023,0.00006869266,0.00010445448,0.0001631976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00088739005,0.00006085976,0.00015191673,0.00016828367,0.00023773964,0.000010915721,0.00030071673,0.000054010674,0.00017754585],"category_scores_gemma":[0.00021554613,0.000038103593,0.000052111125,0.00038427155,0.0012831524,0.00020049678,0.000002067586,0.00010824591,0.0000021882222],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006783546,0.000003215968,0.9912166,0.000015905487,0.000011759079,0.0000057250527,0.00047855068,0.005441542,0.00043008948,0.0014911755,0.000007806165,0.00089081883],"study_design_scores_gemma":[0.00013401256,0.0002884751,0.9945078,0.00006959927,0.0000137411735,0.00013988958,0.000262549,0.0004105952,0.0004338102,0.0036078638,0.000087090775,0.000044564684],"about_ca_topic_score_codex":0.00540704,"about_ca_topic_score_gemma":0.52529067,"teacher_disagreement_score":0.5198836,"about_ca_system_score_codex":0.0000011553248,"about_ca_system_score_gemma":0.0017502728,"threshold_uncertainty_score":0.8173863},"labels":[],"label_agreement":null},{"id":"W2065434841","doi":"10.1139/e06-030","title":"A new geological framework for the Middle Ordovician Carillon Formation (uppermost Beekmantown Group, Ottawa Embayment): onset of Taconic foreland deposition and tectonism within the Laurentian platform interior","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Geology; Paleontology; Foreland basin; Onlap; Graben; Ordovician; Siliciclastic; Sedimentary depositional environment; Carbonate platform; Passive margin; Facies; Rift; Structural basin","score_opus":0.019495323373834448,"score_gpt":0.2128993492577467,"score_spread":0.19340402588391226,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065434841","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9837778,0.0071555176,0.0056514572,0.001568624,0.0004017047,0.00023468198,0.000057877838,0.0000032723415,0.0011490496],"genre_scores_gemma":[0.9955482,0.000022249438,0.0042101606,0.00011019333,0.000091757975,8.821792e-7,0.000006156296,7.010001e-7,0.000009681233],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898386,0.000047916747,0.00037921584,0.000116020055,0.00018112079,0.00029185388],"domain_scores_gemma":[0.99901426,0.00031870254,0.00035344437,0.00008039449,0.000048272654,0.0001849504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007883592,0.00010522418,0.0001645013,0.00014366145,0.00095808494,0.00017026947,0.00034133543,0.000097346834,0.00008836344],"category_scores_gemma":[0.00007063939,0.000054896835,0.000087740285,0.00023080852,0.00071047165,0.00041676284,0.0000016534294,0.00020420624,5.640009e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007348734,0.000006239773,0.9538405,0.000020184407,0.00004977849,0.00002288873,0.0019054834,0.00051711843,0.000047107973,0.008795747,0.0002137238,0.034507763],"study_design_scores_gemma":[0.00023439825,0.00067901716,0.98008513,0.00008108772,0.000041968666,0.00038438835,0.0011085345,0.002725916,0.00010991786,0.014199513,0.0002714791,0.00007865621],"about_ca_topic_score_codex":0.028186623,"about_ca_topic_score_gemma":0.9073322,"teacher_disagreement_score":0.87914556,"about_ca_system_score_codex":0.0000018055873,"about_ca_system_score_gemma":0.00035036987,"threshold_uncertainty_score":0.9782848},"labels":[],"label_agreement":null},{"id":"W2065446319","doi":"10.1139/e00-034","title":"Taltson basement gneissic rocks: UPb and Nd isotopic constraints on the basement to the Paleoproterozoic Taltson magmatic zone, northeastern Alberta","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Terrane; Geochemistry; Gneiss; Archean; Basement; Magmatism; Mantle (geology); Craton; Petrology; Metamorphism; Crust; Continental crust; Metamorphic rock; Tectonics; Paleontology","score_opus":0.013134091557942444,"score_gpt":0.18592109733836198,"score_spread":0.17278700578041953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065446319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97312963,0.0005151972,0.000024589184,0.020178495,0.000113878545,0.00021481987,0.000023590672,0.0000019985982,0.0057978053],"genre_scores_gemma":[0.9954902,0.000026051874,0.00009482414,0.0035004632,0.000096561125,0.0000016851756,0.0000026957237,0.0000012723722,0.0007862381],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984038,0.00013583258,0.00034427946,0.00023198877,0.0004156236,0.00046846177],"domain_scores_gemma":[0.9987419,0.00025967637,0.000122069774,0.00015862029,0.000045914214,0.00067178014],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000832255,0.00015482954,0.00019875786,0.000119625096,0.0006597832,0.00023241004,0.0005378505,0.00003196063,0.042539604],"category_scores_gemma":[0.00010699569,0.000070649585,0.00008724982,0.0004411507,0.0005475168,0.00012152326,0.0000075196126,0.00019451992,0.00028670905],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015916388,0.000013699019,0.86570287,0.000008845509,0.000029690409,0.000038467857,0.00051604706,0.0044419505,0.000007083615,0.000047381393,0.00038969828,0.12878834],"study_design_scores_gemma":[0.0002062437,0.0009032251,0.9729962,0.00012581964,0.00004234198,0.00011524401,0.0008324094,0.005536434,0.00008556411,0.0010680851,0.017876673,0.0002117597],"about_ca_topic_score_codex":0.06207141,"about_ca_topic_score_gemma":0.76685476,"teacher_disagreement_score":0.7047833,"about_ca_system_score_codex":0.0000023858727,"about_ca_system_score_gemma":0.00020655358,"threshold_uncertainty_score":0.95833564},"labels":[],"label_agreement":null},{"id":"W2065753749","doi":"10.1139/e01-097","title":"Amphibole and mica <sup>40</sup>Ar/<sup>39</sup>Ar ages from the Kaipokok and Aillik domains, Makkovik Province, Labrador: towards a characterization of back-arc processes in the Paleoproterozoic","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University; Dalhousie University","funders":"","keywords":"Plutonism; Amphibole; Geology; Muscovite; Pluton; Geochemistry; Shear zone; Closure temperature; Mafic; Metamorphic rock; Petrology; Seismology; Tectonics; Paleontology","score_opus":0.01390066116936312,"score_gpt":0.17677408084614477,"score_spread":0.16287341967678165,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065753749","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887228,0.0033476779,0.0000062352183,0.006966346,0.00002758306,0.00018976984,0.00017591313,0.0000032022606,0.0005604502],"genre_scores_gemma":[0.9978532,0.0006765474,0.00029144177,0.00095525273,0.0001171445,0.0000012357403,0.000020902695,0.0000020589757,0.000082172875],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99821,0.00019631007,0.00044334325,0.00029494805,0.0004306914,0.0004246822],"domain_scores_gemma":[0.9988686,0.00027935964,0.00026159777,0.00014232883,0.0001111688,0.00033696726],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00066101534,0.00018333543,0.00031870953,0.00018178005,0.00038630495,0.00028024588,0.00063203886,0.000078792305,0.0020810578],"category_scores_gemma":[0.00029204067,0.00009274148,0.000066873785,0.0008884857,0.0011352182,0.00046271755,0.000017563192,0.00024453975,0.000016304371],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020342615,0.000022287384,0.97888654,0.000039882154,0.000027262267,0.00005159845,0.0029333092,0.0006059677,0.00021868786,0.000018760215,0.00011100921,0.017064359],"study_design_scores_gemma":[0.0002653522,0.0003080002,0.9834691,0.00010579994,0.000037739504,0.00007582022,0.0013154987,0.0061244657,0.00013295418,0.0013394996,0.0066539207,0.00017181678],"about_ca_topic_score_codex":0.025352178,"about_ca_topic_score_gemma":0.20934945,"teacher_disagreement_score":0.18399727,"about_ca_system_score_codex":0.0000020712132,"about_ca_system_score_gemma":0.00027862424,"threshold_uncertainty_score":0.99883115},"labels":[],"label_agreement":null},{"id":"W2065754740","doi":"10.1139/e05-058","title":"The thermal history of the Nares Strait, Kane Basin, and Smith Sound region in Canada and Greenland: constraints from apatite fission-track and (UThSm)/He dating","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"California Institute of Technology","keywords":"Geology; Fission track dating; Denudation; Rift; Orogeny; Paleontology; Thermochronology; Structural basin; Zircon; Tectonics","score_opus":0.024508950410743097,"score_gpt":0.1767794407316613,"score_spread":0.1522704903209182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065754740","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98998433,0.006552585,0.0000018531391,0.0026711016,0.00017718178,0.000044411056,0.00001810953,4.7209957e-7,0.00054995675],"genre_scores_gemma":[0.99936295,0.00020815305,0.000117379204,0.00022127638,0.000046887733,7.813757e-8,5.9210805e-7,5.896629e-7,0.000042122636],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99927914,0.00007514383,0.00020305939,0.00009842379,0.00016343418,0.00018077168],"domain_scores_gemma":[0.9993238,0.00025717876,0.00016686197,0.000043283733,0.00003255229,0.00017633801],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004100276,0.00006299194,0.000108756896,0.00003310814,0.00036090412,0.00005185808,0.00013735004,0.00002060357,0.000117806274],"category_scores_gemma":[0.00013364633,0.0000313231,0.000011785974,0.0000803904,0.0009199975,0.00019280521,0.00000755934,0.00011269057,1.8394759e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000043310365,5.256153e-7,0.9636602,0.0000017987749,0.0000037286736,0.0000069973935,0.0006335085,0.0004279749,0.0000031954537,0.000009058528,0.00026415227,0.034984533],"study_design_scores_gemma":[0.00010124686,0.00005958163,0.9921358,0.000039221293,0.000004404353,0.000029702518,0.0020921598,0.0010065478,0.0000028919023,0.00024197345,0.004240958,0.000045469096],"about_ca_topic_score_codex":0.8666907,"about_ca_topic_score_gemma":0.9985924,"teacher_disagreement_score":0.13190168,"about_ca_system_score_codex":0.000008074839,"about_ca_system_score_gemma":0.0010387533,"threshold_uncertainty_score":0.33897692},"labels":[],"label_agreement":null},{"id":"W2065888294","doi":"10.1139/e00-120","title":"Biostratigraphic and biogeographic constraints on the Carboniferous to Jurassic Cache Creek Terrane in central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Carboniferous; Permian; Paleontology; Terrane; Conodont; Sedimentary rock; Biostratigraphy; Tectonics; Structural basin","score_opus":0.01968242122907507,"score_gpt":0.20133449415544197,"score_spread":0.1816520729263669,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065888294","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9842268,0.0028374805,0.0000019032038,0.0017151433,0.00032395023,0.00013929405,0.000059391732,0.0000036039655,0.010692399],"genre_scores_gemma":[0.99926347,0.00013424746,0.00012393988,0.00040876653,0.00005112368,4.2894754e-7,6.926144e-7,7.2878066e-7,0.000016629685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984207,0.00014439793,0.00032031638,0.00022409679,0.0002534678,0.0006369768],"domain_scores_gemma":[0.9987966,0.00018056623,0.00011561382,0.000091050184,0.00004208619,0.00077409024],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008728815,0.000102240214,0.00020694578,0.00032764435,0.0006419271,0.00074722845,0.0004034294,0.00007807774,0.00073020725],"category_scores_gemma":[0.00012098906,0.00009924384,0.000073559415,0.0010297662,0.0019910154,0.00022294465,8.6647407e-7,0.0002929666,0.0000020417913],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004808283,0.0000038538333,0.94762826,0.0000014757584,0.000009434471,0.0005014076,0.00017590236,0.000028738152,0.0000064389374,0.0000177172,0.00013422099,0.05148775],"study_design_scores_gemma":[0.00017396499,0.000523525,0.9965719,0.000092240676,0.00000729678,0.0010154191,0.00054652477,0.000049698167,0.0000022494696,0.0006114667,0.00027922698,0.0001264806],"about_ca_topic_score_codex":0.45929456,"about_ca_topic_score_gemma":0.9984816,"teacher_disagreement_score":0.539187,"about_ca_system_score_codex":0.0000010611941,"about_ca_system_score_gemma":0.000706428,"threshold_uncertainty_score":0.79952574},"labels":[],"label_agreement":null},{"id":"W2065984890","doi":"10.1139/e00-113","title":"Enhanced resolution of geological structures from magnetic data: an example from the Abitibi Greenstone Belt of Northern Ontario","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"","keywords":"Geology; Greenstone belt; Archean; Fault (geology); Seismology; Normal fault; Sinistral and dextral; Felsic; Geochemistry; Geophysics; Tectonics","score_opus":0.06169604698171227,"score_gpt":0.24263314686680795,"score_spread":0.18093709988509568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065984890","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971845,0.0012641859,0.00039997604,0.0002110436,0.00024689757,0.000061916806,0.00011903463,0.000001924012,0.000510514],"genre_scores_gemma":[0.9956545,0.000018795894,0.003939199,0.00010953371,0.00019459658,6.3206166e-8,0.000040416366,0.0000011668917,0.000041675685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984028,0.00022141101,0.00040080727,0.00024962617,0.00039462783,0.0003307536],"domain_scores_gemma":[0.9984168,0.0004966563,0.0002906296,0.00028302922,0.00012880996,0.00038407554],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00068034057,0.00010694975,0.00028048977,0.000083443774,0.00023539885,0.00004781464,0.0010335427,0.0000610393,0.0026193282],"category_scores_gemma":[0.00017602612,0.00006161899,0.00005822765,0.0004459597,0.00081965793,0.00033462784,0.000014429177,0.0002345152,0.0000053535855],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000055703702,0.000012382643,0.8899093,0.0000010631796,0.0000147418505,0.000022319105,0.0008571136,0.0025807305,0.00045723602,0.000063365405,0.000028484374,0.10599754],"study_design_scores_gemma":[0.00016328147,0.00082845194,0.98712754,0.00001535913,0.000023153536,0.000012025359,0.0002167321,0.0009710278,0.00014969309,0.009879766,0.00053199596,0.00008094358],"about_ca_topic_score_codex":0.97487086,"about_ca_topic_score_gemma":0.9988148,"teacher_disagreement_score":0.1059166,"about_ca_system_score_codex":0.0000024760866,"about_ca_system_score_gemma":0.00086605974,"threshold_uncertainty_score":0.9982924},"labels":[],"label_agreement":null},{"id":"W2066079865","doi":"10.1139/cjes-2012-0149","title":"Framework geophysical modelling of granitoid versus supracrustal basement to the northeast Thelon Basin around the Kiggavik uranium camp, Nunavut","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; McMaster University","funders":"","keywords":"Geology; Basement; Geochemistry; Gneiss; Context (archaeology); Petrophysics; Structural basin; Fault (geology); Petrology; Uranium; Archean; Metamorphic rock; Geophysics; Geomorphology; Seismology; Paleontology","score_opus":0.027826875312807274,"score_gpt":0.20457532102349296,"score_spread":0.17674844571068568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066079865","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98654336,0.00042183322,0.00067264144,0.010648039,0.0004555927,0.00013444635,0.00003562009,0.000002455467,0.0010859859],"genre_scores_gemma":[0.99777246,0.00001990293,0.0011885496,0.00064701284,0.0003327344,8.433852e-7,0.0000026335363,0.0000015981242,0.000034279976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99825615,0.0001252078,0.00037226742,0.00019160354,0.00055417896,0.00050059037],"domain_scores_gemma":[0.998268,0.0005627415,0.00018796508,0.00018134779,0.00020942096,0.00059050636],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00079007796,0.00014077219,0.00023598135,0.000112726724,0.00064787245,0.00021615264,0.0008819366,0.000049400984,0.0039223875],"category_scores_gemma":[0.00020812036,0.000063698775,0.00018594113,0.00079243875,0.000656658,0.00025238178,0.000014280158,0.00033861605,0.00018816495],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000073961586,0.000027827358,0.7577212,0.0000075896173,0.0000831996,0.000024424582,0.0012896112,0.2302475,0.00003844336,0.0007944632,0.00045210574,0.00923967],"study_design_scores_gemma":[0.0003204512,0.0012509131,0.8844121,0.00009614587,0.000112511094,0.000048837166,0.006118213,0.07889905,0.00025838957,0.021875719,0.006240103,0.00036756793],"about_ca_topic_score_codex":0.16007785,"about_ca_topic_score_gemma":0.35753268,"teacher_disagreement_score":0.19745484,"about_ca_system_score_codex":0.0000026322607,"about_ca_system_score_gemma":0.00039800844,"threshold_uncertainty_score":0.9969882},"labels":[],"label_agreement":null},{"id":"W2066148377","doi":"10.1139/e04-087","title":"High-temperature, low-pressure metamorphism in the Kisseynew domain, Trans-Hudson orogen: crustal anatexis due to tectonic thickening?","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Anatexis; Metamorphism; Tectonics; Sedimentary rock; Metamorphic rock; Thickening; Petrology; Mantle (geology); Thermal; Crust; Terrane; Subduction; Seismology; Geochemistry; Partial melting; Thermodynamics","score_opus":0.009867780497104418,"score_gpt":0.19581354003815937,"score_spread":0.18594575954105497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066148377","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9786713,0.0035499686,0.000007858232,0.015990304,0.00018411828,0.00010417016,0.000041915155,0.0000046968357,0.0014456287],"genre_scores_gemma":[0.9945957,0.000028741148,0.0020771148,0.0029716743,0.00023585184,5.7665574e-7,0.0000049320097,0.0000018239903,0.000083605904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99788064,0.00018681774,0.00044094314,0.00028119585,0.0005529652,0.0006574183],"domain_scores_gemma":[0.99868983,0.00016263334,0.00012989934,0.00015022796,0.00011040772,0.00075698615],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015697826,0.00018378804,0.00035395575,0.00040150966,0.0004334853,0.0002702704,0.0010746806,0.00010192706,0.008187352],"category_scores_gemma":[0.00016831276,0.00010118301,0.00017767647,0.0016461682,0.00041537525,0.00038049355,0.0000064441015,0.0004746751,0.0000856615],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015855239,0.00011490277,0.74241585,0.00005104052,0.000278961,0.003111762,0.0074492022,0.21417207,0.0041932925,0.0034804924,0.004349955,0.020223955],"study_design_scores_gemma":[0.00058163516,0.0008585549,0.9311179,0.0001088569,0.00011050762,0.000684342,0.0024291095,0.00060012995,0.0032000097,0.011112684,0.04861488,0.00058137125],"about_ca_topic_score_codex":0.031847645,"about_ca_topic_score_gemma":0.7001567,"teacher_disagreement_score":0.66830903,"about_ca_system_score_codex":0.0000026228051,"about_ca_system_score_gemma":0.0005578406,"threshold_uncertainty_score":0.9927193},"labels":[],"label_agreement":null},{"id":"W2066439307","doi":"10.1139/e02-055","title":"Paleomagnetism of Carboniferous strata from the Stellarton Gap","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Geology; Carboniferous; Paleomagnetism; Paleontology; Clockwise; Graben; Thermal subsidence; Subsidence; Paleozoic; Structural basin; Seismology; Remanence; Fold (higher-order function); Magnetization","score_opus":0.052175802935093406,"score_gpt":0.22491700293305353,"score_spread":0.17274119999796012,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066439307","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9645363,0.011804365,0.0000022143327,0.0019442702,0.0004447295,0.000053228938,0.00004424081,0.0000016413921,0.021168975],"genre_scores_gemma":[0.9991553,0.0001842087,0.0002140774,0.00018687388,0.00009652344,6.3504515e-8,0.0000022122508,9.406106e-7,0.0001598277],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986846,0.00019874159,0.00029056374,0.00013006087,0.00029218593,0.0004038692],"domain_scores_gemma":[0.99874103,0.0004989484,0.00016785321,0.00014493612,0.00008686918,0.00036039183],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00083833374,0.00008345173,0.00018243173,0.00014500186,0.00037825372,0.00006343084,0.00075124565,0.00007517648,0.008891531],"category_scores_gemma":[0.00016347479,0.000051372106,0.00006257363,0.00035577407,0.0014700744,0.00018282585,0.0000044769486,0.00027399982,0.00009523718],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000030882748,0.000002271475,0.9977865,0.0000017384185,0.000010385895,0.00010071467,0.00033744806,0.00033043727,0.000004144767,0.000065557666,0.00023634314,0.0011213531],"study_design_scores_gemma":[0.0001325731,0.00036401572,0.99513304,0.000021164014,0.00001145366,0.00022738973,0.00041186062,0.00082001975,0.000045895566,0.000873957,0.0018928223,0.00006583453],"about_ca_topic_score_codex":0.017653497,"about_ca_topic_score_gemma":0.6940569,"teacher_disagreement_score":0.67640346,"about_ca_system_score_codex":1.8013637e-7,"about_ca_system_score_gemma":0.00045890507,"threshold_uncertainty_score":0.99201447},"labels":[],"label_agreement":null},{"id":"W2066837318","doi":"10.1139/e06-064","title":"Pressure–temperature–deformation paths of closely associated ultra-high-pressure (diamond-bearing) crustal and mantle rocks of the Kimi complex: implications for the tectonic history of the Rhodope Mountains, northern Greece","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Metamorphism; Eclogite; Zircon; Gneiss; Mantle (geology); Partial melting; Metamorphic rock; Protolith; Mantle wedge; Petrology; Subduction; Tectonics; Seismology","score_opus":0.014340606045857428,"score_gpt":0.18387645373034373,"score_spread":0.1695358476844863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066837318","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928917,0.004178983,0.000011113191,0.0015444345,0.00013998542,0.00016366826,0.00034055868,0.0000016223623,0.00072787923],"genre_scores_gemma":[0.9995516,0.000024101175,0.000057796733,0.00009243356,0.00003079254,6.5560283e-7,0.000007819428,0.0000012643765,0.00023351448],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989429,0.0000891953,0.00038402513,0.000110762434,0.00025819178,0.0002149158],"domain_scores_gemma":[0.9986756,0.0002379169,0.0005595736,0.00014800894,0.00028367797,0.00009525195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005785228,0.00009031817,0.00020766155,0.000068439855,0.00035597768,0.000028763376,0.0006172424,0.000059455357,0.0002455842],"category_scores_gemma":[0.0002248289,0.000041152107,0.00014574548,0.0003795143,0.0008226342,0.00014187492,0.00001131821,0.00015693036,3.7974158e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009551337,0.000012833314,0.9705139,0.000020271113,0.0000566515,2.0987406e-7,0.00023812879,0.025068726,0.002704362,0.00021719497,0.00039293017,0.00076523697],"study_design_scores_gemma":[0.00012963373,0.000086209155,0.99193716,0.000022568749,0.00010671635,0.0000084259,0.00014532963,0.0020192917,0.00088862656,0.0020999238,0.0024979156,0.00005819334],"about_ca_topic_score_codex":0.07419306,"about_ca_topic_score_gemma":0.49910095,"teacher_disagreement_score":0.4249079,"about_ca_system_score_codex":0.000004577673,"about_ca_system_score_gemma":0.0005321976,"threshold_uncertainty_score":0.93197197},"labels":[],"label_agreement":null},{"id":"W2066984514","doi":"10.1139/e00-030","title":"Some graptolites from the late Tremadoc and early Arenig of Yukon, Canada","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Biozone; Geology; Paleontology; Canyon; Group (periodic table); Range (aeronautics); Biostratigraphy; Geomorphology; Physics","score_opus":0.01821233026019961,"score_gpt":0.16945437853304607,"score_spread":0.15124204827284646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066984514","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9885035,0.007622499,5.230815e-7,0.0027388176,0.0001940539,0.000031132702,0.000046241814,9.1188224e-7,0.0008622804],"genre_scores_gemma":[0.9989555,0.00036568075,0.000079903795,0.00039234315,0.00010646977,5.5585144e-8,0.0000014568967,5.2272986e-7,0.00009806164],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992361,0.000043804488,0.00021200602,0.000078102035,0.00020741111,0.00022254635],"domain_scores_gemma":[0.99938726,0.00015181249,0.000103449056,0.00004852547,0.000046590958,0.00026238392],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00028583733,0.000063152605,0.00013532524,0.00003618483,0.00038809236,0.000075606964,0.00022901705,0.000019915635,0.0013237],"category_scores_gemma":[0.000056154466,0.000034161258,0.000029208646,0.00019925482,0.00041363676,0.00024385942,0.0000021027172,0.000079831785,0.0000050198746],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005092834,7.331679e-7,0.9853223,7.8345937e-7,0.000008101002,0.000012879825,0.00034749598,0.0012694579,0.0000021969984,0.000051006453,0.00041363572,0.012566342],"study_design_scores_gemma":[0.000067892644,0.00014309143,0.98553395,0.000014356485,0.0000063678676,0.0000076042575,0.0004409202,0.00016777524,0.000012592642,0.0026058098,0.010950185,0.000049440823],"about_ca_topic_score_codex":0.95619744,"about_ca_topic_score_gemma":0.9968321,"teacher_disagreement_score":0.040634632,"about_ca_system_score_codex":9.095878e-7,"about_ca_system_score_gemma":0.0005651643,"threshold_uncertainty_score":0.9995892},"labels":[],"label_agreement":null},{"id":"W2067279212","doi":"10.1139/e99-092","title":"Global water balance and atmospheric water vapour transport at last glacial maximum: climate simulations with the Canadian Climate Centre for Modelling and Analysis atmospheric general circulation model","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; University of Toronto","funders":"","keywords":"Glacial period; Climatology; Ice sheet; Atmospheric circulation; Water cycle; Northern Hemisphere; Last Glacial Maximum; Environmental science; Geology; Interglacial; Climate model; Atmospheric sciences; Ice-sheet model; Cryosphere; Climate change; Sea ice; Ice stream; Geomorphology; Oceanography","score_opus":0.014385710923090657,"score_gpt":0.2108883710871212,"score_spread":0.19650266016403053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067279212","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965813,0.00029206672,0.00042046246,0.0017159557,0.000054052354,0.00015323178,0.0001886509,0.0000034776897,0.00059079647],"genre_scores_gemma":[0.99657255,0.0000692415,0.0029461286,0.00020686192,0.00003945767,5.6536436e-7,0.000056269346,0.0000027305077,0.000106213294],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99829036,0.0000726072,0.00024789214,0.00026041217,0.00020312761,0.0009255881],"domain_scores_gemma":[0.9990691,0.000045039666,0.000058178983,0.00009057291,0.00010779073,0.000629315],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006302163,0.0001486016,0.00024304251,0.000040473733,0.0020924688,0.0001406158,0.00020327319,0.0000937144,0.0010814881],"category_scores_gemma":[0.000003507349,0.00008028362,0.00006744544,0.00038273208,0.0006507362,0.0003178127,0.0000034952232,0.00011976525,0.000009758966],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024335603,7.9257114e-7,0.511738,0.0000037767825,0.000026188794,0.00001491923,0.00026631367,0.4878016,4.1010597e-7,0.000011074981,0.0000017737192,0.00011078547],"study_design_scores_gemma":[0.00017663895,0.000047228365,0.4280989,0.000004165594,0.000077196906,0.00008300405,0.000043424978,0.57087886,0.0000015829557,0.000206347,0.00029766152,0.00008499906],"about_ca_topic_score_codex":0.041581,"about_ca_topic_score_gemma":0.9876588,"teacher_disagreement_score":0.9460778,"about_ca_system_score_codex":0.000004780564,"about_ca_system_score_gemma":0.0004479314,"threshold_uncertainty_score":0.9998317},"labels":[],"label_agreement":null},{"id":"W2067291633","doi":"10.1139/e06-091","title":"Precambrian history of the eastern Ferris Mountains and Bear Mountain, south-central Wyoming Province","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Archean; Mafic; Proterozoic; Metamorphism; Metamorphic rock; Dike; Sill; Pluton; Terrane; Craton; Lineation; Batholith; Gneiss; Precambrian; Paleontology; Tectonics","score_opus":0.012376591766570185,"score_gpt":0.16396790909390557,"score_spread":0.15159131732733538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067291633","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913556,0.0027789455,0.000011208275,0.0007340766,0.00024629128,0.000051142815,0.000021115547,0.000001943791,0.00479968],"genre_scores_gemma":[0.99856365,0.00000632262,0.00023870739,0.00018128351,0.00010838705,6.8447314e-8,0.0000011832673,9.549251e-7,0.00089944154],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883175,0.00006384235,0.00029878216,0.00014962332,0.00028091576,0.00037511412],"domain_scores_gemma":[0.9991991,0.000050608476,0.0002511007,0.000081952065,0.000075420474,0.00034182932],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039380335,0.00009489226,0.0001798064,0.00011978508,0.00019693476,0.000056911394,0.00040272952,0.00004099879,0.0008305465],"category_scores_gemma":[0.000090718124,0.000055109533,0.00009700615,0.00023902844,0.0009784283,0.00020422343,0.000009376451,0.00014513622,0.000005516644],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000042064394,0.000002842416,0.99714935,0.0000048681463,0.0000053617355,0.000011325043,0.0001715919,0.0016211095,0.00006300448,0.00009464866,0.00015455138,0.00071715453],"study_design_scores_gemma":[0.00010198039,0.00010051689,0.98788154,0.00002683487,0.000022232442,0.00004053716,0.00027021242,0.0032547193,0.00008642563,0.0010074448,0.0071191597,0.000088400426],"about_ca_topic_score_codex":0.12288527,"about_ca_topic_score_gemma":0.6940227,"teacher_disagreement_score":0.5711375,"about_ca_system_score_codex":0.0000075902103,"about_ca_system_score_gemma":0.0011100504,"threshold_uncertainty_score":0.90939015},"labels":[],"label_agreement":null},{"id":"W2067376134","doi":"10.1139/e00-051","title":"A reconstruction of Moorhead and Emerson Phase environments along the eastern margin of glacial Lake Agassiz, Rainy River basin, northwestern Ontario","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"The Scarborough Hospital; University of Waterloo; Geological Survey of Canada","funders":"Baosteel-Australia Joint Research and Development Centre","keywords":"Geology; Radiocarbon dating; Glacial period; Macrofossil; Fluvial; Alluvium; Marine transgression; Paleontology; Alluvial fan; Quaternary; Glacial lake; Structural basin; Holocene","score_opus":0.021021916815366762,"score_gpt":0.22158607262755015,"score_spread":0.2005641558121834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067376134","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99695927,0.00039646396,0.0000048778384,0.00030201828,0.0002043183,0.00007374672,0.000031674157,6.0253626e-7,0.0020270057],"genre_scores_gemma":[0.99920094,0.000053788208,0.0002206227,0.000059856095,0.000030629308,1.2666025e-7,0.0000032139055,9.256504e-7,0.0004299097],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988878,0.00015067264,0.00030899845,0.00013148959,0.00022498469,0.00029607373],"domain_scores_gemma":[0.9993273,0.00010083267,0.000197384,0.00008012624,0.00003062263,0.00026373233],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006990556,0.00008398092,0.00019968877,0.000183626,0.00028919138,0.000025932397,0.00026425242,0.00006174657,0.0061078086],"category_scores_gemma":[0.0000188996,0.00005726672,0.00005380981,0.0001698553,0.0021433944,0.00028616202,0.0000034938078,0.00019914753,0.000019048368],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047784946,0.000005886423,0.9809703,0.0000042094703,0.00001702493,0.00003584349,0.0015885811,0.00016165551,0.0000032061869,0.0000025160707,0.0000066610555,0.017156279],"study_design_scores_gemma":[0.0004581408,0.00040776323,0.9959568,0.000035001845,0.00001584089,0.00051432016,0.0003091934,0.0002843717,0.00003473504,0.000092926675,0.0018341913,0.00005671867],"about_ca_topic_score_codex":0.12900895,"about_ca_topic_score_gemma":0.9893713,"teacher_disagreement_score":0.86036235,"about_ca_system_score_codex":7.483078e-7,"about_ca_system_score_gemma":0.0006850891,"threshold_uncertainty_score":0.99480075},"labels":[],"label_agreement":null},{"id":"W2067383245","doi":"10.1139/e03-097","title":"Implications of the mineralogy and chemical composition of lead beads from Frobisher's assay site, Kodlunarn Island, Canada: prelude to Bre-X?","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Archaeology and ancient environmental studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval","funders":"","keywords":"Electron microprobe; Galena; Chemical composition; Microprobe; Mineralogy; Geology; Flux (metallurgy); Composition (language); Chemistry; Analytical Chemistry (journal); Metallurgy; Environmental chemistry; Materials science; Art","score_opus":0.00901853724653853,"score_gpt":0.17982500164947976,"score_spread":0.17080646440294123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067383245","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940501,0.0007254218,0.00008363603,0.003891051,0.00013999066,0.000053051306,0.00024656195,5.1818165e-7,0.0008096561],"genre_scores_gemma":[0.99881524,0.000011122082,0.00073295896,0.00038036855,0.000030457815,1.4574016e-7,0.0000058909936,7.5012866e-7,0.000023084318],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99934494,0.00003561576,0.00020057727,0.00010084049,0.00014468066,0.00017335317],"domain_scores_gemma":[0.99951714,0.000084425694,0.00013152206,0.00006185958,0.000028796463,0.00017623337],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018405609,0.00006011983,0.00014176487,0.00005360601,0.00022505282,0.000007282204,0.00023347083,0.000027868082,0.00012978469],"category_scores_gemma":[0.0000301913,0.000040205407,0.000029746252,0.00017472457,0.0008872426,0.000089043126,0.00001324386,0.00008146667,0.0000014690347],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045983256,0.0000033465092,0.9942305,0.0000016027453,0.000010778736,0.000002602058,0.000389126,0.001852675,0.002538674,0.00006238448,0.00018139121,0.0007223031],"study_design_scores_gemma":[0.000119502074,0.00008429866,0.99655294,0.000030225778,0.000012317617,0.000030332749,0.00016463922,0.000025569558,0.0019276247,0.0006388065,0.00036510327,0.000048629376],"about_ca_topic_score_codex":0.6673492,"about_ca_topic_score_gemma":0.99181473,"teacher_disagreement_score":0.3244655,"about_ca_system_score_codex":0.0000067820674,"about_ca_system_score_gemma":0.0005717871,"threshold_uncertainty_score":0.33486596},"labels":[],"label_agreement":null},{"id":"W2067507606","doi":"10.1139/e01-070","title":"Crustal velocity structure from SAREX, the Southern Alberta Refraction Experiment","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; University of British Columbia","funders":"","keywords":"Geology; Seismology; Crust; Archean; Tectonics; Seismometer; Structural basin; Mantle (geology); Underplating; Inversion (geology); Lithosphere; Geomorphology; Geochemistry","score_opus":0.01922209244486033,"score_gpt":0.18916137396746746,"score_spread":0.16993928152260712,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067507606","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9895534,0.0016454436,0.0000068545605,0.0033454597,0.00026445038,0.000028319842,0.00005892859,0.000001917972,0.0050952323],"genre_scores_gemma":[0.99860835,0.000012688141,0.00030102782,0.00052314973,0.00019976312,5.996601e-8,0.000004849759,7.2850526e-7,0.00034937114],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99899656,0.000064570435,0.00021642352,0.0001466364,0.000288819,0.0002869726],"domain_scores_gemma":[0.99914277,0.0001527877,0.00015192485,0.00008968965,0.000059876926,0.00040295382],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019782755,0.0000916504,0.00013679259,0.0000730946,0.0005067987,0.00015660468,0.00042415058,0.000049095124,0.06721733],"category_scores_gemma":[0.00015022467,0.000046663794,0.00009068948,0.00033069332,0.00042291055,0.00018981502,0.000004631986,0.0002070815,0.00015622753],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014774268,0.000010646253,0.9644751,0.0000015827013,0.000061087805,0.000056613455,0.0031932003,0.005685843,0.00037971724,0.000056647354,0.001248165,0.02481661],"study_design_scores_gemma":[0.00030194345,0.00041492126,0.91551894,0.000030667867,0.00007226314,0.00012299344,0.006446493,0.018987235,0.0015120724,0.01574992,0.040457506,0.00038506705],"about_ca_topic_score_codex":0.31603497,"about_ca_topic_score_gemma":0.82035273,"teacher_disagreement_score":0.50431776,"about_ca_system_score_codex":0.0000017198606,"about_ca_system_score_gemma":0.00011135111,"threshold_uncertainty_score":0.93363535},"labels":[],"label_agreement":null},{"id":"W2067637344","doi":"10.1139/e06-039","title":"Strike-slip juxtaposition of ca. 2.72 Ga juvenile arc and &gt;2.98 Ga continent margin sequences and its implications for Archean terrane accretion, western Superior Province, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Terrane; Geology; Continental crust; Subduction; Geochemistry; Paleontology; Continental margin; Continental arc; Transpression; Geomorphology; Crust; Structural basin; Sinistral and dextral","score_opus":0.015833001726695144,"score_gpt":0.20097424944480194,"score_spread":0.1851412477181068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067637344","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9914542,0.0016396759,0.000030578936,0.0059133708,0.00006712578,0.0001386943,0.0003626999,0.0000020266953,0.00039163046],"genre_scores_gemma":[0.99910945,0.00004245169,0.00042451802,0.0001470877,0.00007589354,0.0000011272156,0.000037869755,0.0000011869664,0.0001604066],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99880767,0.000042014686,0.00039287467,0.00020079604,0.00019746686,0.00035917162],"domain_scores_gemma":[0.99897206,0.00014301321,0.00021333192,0.000057820303,0.00018745115,0.00042635162],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004336736,0.00011101372,0.00025523992,0.00015124942,0.00035313205,0.00009553042,0.00021622014,0.000040191655,0.0004440761],"category_scores_gemma":[0.00008593365,0.00007922443,0.000050460945,0.0002638115,0.00043981016,0.0002298238,0.0000064802416,0.00008596311,8.8315016e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011587146,0.0000053957765,0.99603915,0.000024908952,0.000010848167,0.000007987603,0.000039612434,0.0006921512,0.0013220392,0.00016563077,0.00026202173,0.0014186375],"study_design_scores_gemma":[0.00018897613,0.00025229785,0.991861,0.000038544975,0.000033243312,0.00008380761,0.00013235901,0.001035627,0.0009255632,0.0025253096,0.002800876,0.00012240926],"about_ca_topic_score_codex":0.6273737,"about_ca_topic_score_gemma":0.99170053,"teacher_disagreement_score":0.36432683,"about_ca_system_score_codex":0.000004129055,"about_ca_system_score_gemma":0.0013071025,"threshold_uncertainty_score":0.48623222},"labels":[],"label_agreement":null},{"id":"W2067878503","doi":"10.1139/e01-049","title":"The occurrence of <i>Psittacosaurus xinjiangensis</i> Sereno and Chow, 1988 in the Urho area, Junggar Basin, Xinjiang, People's Republic of China","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Structural basin; China; Geology; Paleontology; Type locality; Range (aeronautics); Geography; Biology; Zoology; Archaeology; Taxonomy (biology)","score_opus":0.02180734090577117,"score_gpt":0.22263640463830575,"score_spread":0.2008290637325346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067878503","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96326345,0.017145291,0.000004632842,0.005432037,0.00043272102,0.00009305012,0.000058811183,0.0000017010973,0.013568316],"genre_scores_gemma":[0.9980502,0.0014437928,0.00008003151,0.00029245106,0.000046150886,2.0858792e-7,0.000001418002,8.1592884e-7,0.00008492904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99850196,0.00020744129,0.00042632993,0.00014981847,0.00032782246,0.00038662885],"domain_scores_gemma":[0.9987292,0.00039680864,0.00035893614,0.00015102685,0.0001389931,0.00022498809],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019394943,0.00011366182,0.00025783706,0.00026208264,0.0005423697,0.00008339884,0.0006172622,0.000047034402,0.00023635945],"category_scores_gemma":[0.00038702908,0.00006189947,0.000068193425,0.00094901235,0.0013421983,0.00028630457,0.000007171765,0.00021523751,0.0000030869546],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010353471,0.0000041635594,0.9925772,0.0000057422226,0.000010775356,0.000020622716,0.0015700054,0.00010087861,0.0000017606011,0.000115578376,0.0016345531,0.0039483965],"study_design_scores_gemma":[0.00014662892,0.00021779395,0.9758066,0.00004387759,0.00001335225,0.00028060834,0.0024121413,0.00019294719,0.000006094116,0.0002382752,0.020569727,0.00007197037],"about_ca_topic_score_codex":0.022099571,"about_ca_topic_score_gemma":0.9123265,"teacher_disagreement_score":0.8902269,"about_ca_system_score_codex":0.000001571171,"about_ca_system_score_gemma":0.0007706714,"threshold_uncertainty_score":0.9844124},"labels":[],"label_agreement":null},{"id":"W2067882887","doi":"10.1139/e02-060","title":"<i>Geosaurus vignaudi</i> n.sp. (Crocodyliformes: Thalattosuchia), first evidence of metriorhynchid crocodilians in the Late Jurassic (Tithonian) of central-east Mexico (State of Puebla)","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Consejo Nacional de Ciencia y Tecnología; Deutsche Forschungsgemeinschaft","keywords":"Holotype; Genus; Paleontology; Geology; Skull; Zoology; Biology","score_opus":0.03058300698945454,"score_gpt":0.21794848895589508,"score_spread":0.18736548196644054,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067882887","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.979599,0.014643619,0.000034073953,0.0018308661,0.00035194747,0.00014798524,0.0001329169,0.000002075599,0.0032575065],"genre_scores_gemma":[0.9984038,0.0009462984,0.00040202404,0.00015431817,0.000036641934,3.976574e-7,0.0000016560281,0.0000017263193,0.00005316523],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977302,0.000250535,0.0008113241,0.00018610305,0.00039694514,0.00062489987],"domain_scores_gemma":[0.99807435,0.00056356407,0.0007255421,0.00018044745,0.00014571265,0.00031037952],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014821508,0.00016133858,0.00044210235,0.0005563374,0.00027496702,0.000025338019,0.001035437,0.00008907071,0.0008798025],"category_scores_gemma":[0.00034341277,0.00010584367,0.00015362709,0.0012600615,0.0019366967,0.0005742201,0.0000070840897,0.00028322983,0.000016001155],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003334784,0.000019313884,0.9882221,0.000034143817,0.000020846644,0.000050221784,0.0017640005,0.005776922,0.0000944756,0.000035283687,0.00013564934,0.0038136917],"study_design_scores_gemma":[0.00023873182,0.0007499206,0.9943148,0.00030381492,0.000020580062,0.00022915925,0.00062923966,0.0016275966,0.00023953729,0.0003890548,0.001140795,0.000116767675],"about_ca_topic_score_codex":0.013247035,"about_ca_topic_score_gemma":0.677578,"teacher_disagreement_score":0.66433096,"about_ca_system_score_codex":0.0000041616267,"about_ca_system_score_gemma":0.00078582024,"threshold_uncertainty_score":0.99332386},"labels":[],"label_agreement":null},{"id":"W2068233941","doi":"10.1139/e03-012","title":"Reconnaissance sediment budgets for Lynn Valley, British Columbia: Holocene and contemporary time scales","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Soil erosion and sediment transport","field":"Agricultural and Biological Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Institute for Advanced Research; University of British Columbia","funders":"","keywords":"Geology; Landform; Debris; Alluvial fan; Debris flow; Sediment; Colluvium; Erosion; Sedimentary depositional environment; Sedimentary budget; Hydrology (agriculture); Geomorphology; Mass wasting; Ravine; Alluvium; STREAMS; Channel (broadcasting); Holocene; Pleistocene; Fluvial; Sediment transport; Structural basin; Archaeology; Oceanography; Paleontology","score_opus":0.03323531333828634,"score_gpt":0.20883025399902208,"score_spread":0.17559494066073575,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068233941","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935681,0.0027428593,0.0000023977782,0.0010421223,0.00029806036,0.00014231462,0.000041181538,0.000005866472,0.0021570686],"genre_scores_gemma":[0.9979604,0.000062726904,0.00029547044,0.00065788813,0.00008189896,0.000002320824,0.000003063341,7.8341697e-7,0.0009354877],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99901927,0.00004581129,0.00027351023,0.00018845178,0.00017855168,0.00029441688],"domain_scores_gemma":[0.99907315,0.00011003767,0.0001313396,0.000023274346,0.00012095331,0.000541247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00085085584,0.000073764284,0.00018919469,0.000020707103,0.000554444,0.00034610447,0.00019665205,0.00005510283,0.0005504604],"category_scores_gemma":[0.000091653055,0.00004539596,0.00007749921,0.00020081867,0.00039834954,0.00023038329,0.0000034664517,0.00007359017,0.00000394666],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019481411,0.00006770175,0.9343907,0.00001753996,0.00003460486,0.00023251845,0.00013806815,0.000012579661,0.004275062,0.00015803729,0.03272369,0.02792999],"study_design_scores_gemma":[0.0005328746,0.0010812513,0.8862177,0.00014172366,0.000010995108,0.0004101646,0.00039675663,0.000031656626,0.0005589462,0.00088268484,0.10948626,0.00024894718],"about_ca_topic_score_codex":0.009934774,"about_ca_topic_score_gemma":0.31018656,"teacher_disagreement_score":0.3002518,"about_ca_system_score_codex":0.0000041360404,"about_ca_system_score_gemma":0.00022465784,"threshold_uncertainty_score":0.99665815},"labels":[],"label_agreement":null},{"id":"W2068306410","doi":"10.1139/e05-047","title":"Structural testing of tectonic hypotheses by field-based analysis of distributed tangential shear: examples from major high-strain zones in the Grenville Province and other parts of the southern Canadian Shield","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Lineation; Shear zone; Archean; Shear (geology); Gneiss; Shearing (physics); Metamorphic rock; Migmatite; Indian Shield; Petrology; Simple shear; Schist; Geomorphology; Geochemistry; Seismology; Tectonics; Geotechnical engineering; Proterozoic","score_opus":0.021651176915031555,"score_gpt":0.18862948925010772,"score_spread":0.16697831233507618,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068306410","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99582326,0.00073300325,0.000009671849,0.0015031393,0.000026019969,0.000055124987,0.0017438731,6.551964e-7,0.0001052595],"genre_scores_gemma":[0.99919295,0.0000017820041,0.00053884246,0.00022585374,0.00002463937,1.6224276e-7,0.000009617031,8.2530164e-7,0.000005304917],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885905,0.0001193425,0.00036691062,0.00013476361,0.00026045172,0.000259503],"domain_scores_gemma":[0.9988091,0.0005462279,0.00028458034,0.00010699631,0.00005543535,0.00019763985],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047028763,0.00009146673,0.00026889524,0.00020811275,0.00015351902,0.000038437556,0.00047739298,0.000047685855,0.0021228031],"category_scores_gemma":[0.00037938688,0.0000465009,0.0001038428,0.001001497,0.000613226,0.00006136461,0.00000513861,0.0001187384,4.845261e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005313667,0.0000034032953,0.9878365,0.000003077483,0.00004384255,0.0000026406356,0.00021472207,0.009613879,0.0002055738,0.000013500129,0.000010330469,0.0020472363],"study_design_scores_gemma":[0.00010535765,0.00011646565,0.99090594,0.000028896542,0.00013133166,0.0000027921562,0.00072385604,0.006036903,0.0010841497,0.0006151305,0.00017488752,0.000074303985],"about_ca_topic_score_codex":0.8499557,"about_ca_topic_score_gemma":0.99400884,"teacher_disagreement_score":0.14405316,"about_ca_system_score_codex":0.0000021475707,"about_ca_system_score_gemma":0.00051242526,"threshold_uncertainty_score":0.99878937},"labels":[],"label_agreement":null},{"id":"W2068636340","doi":"10.1139/e06-120","title":"Reply to discussion by P.J. Barnett on \"Generation of heavy-mineral glacial indicator dispersal trains from a diabase sill, Nipigon Region, Northwestern Ontario\"","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Glacial period; Carbonate; Biological dispersal; Sill; Glacier; Paleontology; Geochemistry; Population","score_opus":0.024200234464966046,"score_gpt":0.2267209903191332,"score_spread":0.20252075585416715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068636340","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99367493,0.00023023697,0.000038427137,0.00444469,0.00051152194,0.0001155153,0.000103909384,0.000003085902,0.0008776729],"genre_scores_gemma":[0.9982527,0.000004409534,0.0002031775,0.0008068606,0.00027244538,5.261554e-7,0.00007819906,0.000002336754,0.0003793725],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99824905,0.0001760055,0.0004292643,0.00028137615,0.00038724043,0.00047703457],"domain_scores_gemma":[0.9988023,0.00010892932,0.00022312293,0.00013302955,0.00007257974,0.0006600519],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00057353685,0.00014045305,0.00026212266,0.0004092443,0.00042953057,0.00007715702,0.00038660003,0.000095436175,0.00095487834],"category_scores_gemma":[0.000067633475,0.000090606656,0.00008444856,0.000341934,0.0005976481,0.00029370442,0.000005204926,0.00027406932,0.000040350566],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000063632506,0.000014723793,0.9943327,0.0000016969905,0.0000079565925,0.00009453307,0.0009398505,0.0012371503,0.00008375788,0.000027176793,0.0027508624,0.00044600505],"study_design_scores_gemma":[0.0002972086,0.0009106694,0.99093246,0.000034639557,0.000011254061,0.000061875806,0.00021232267,0.00035789146,0.00042868196,0.00010378191,0.0065132556,0.00013593902],"about_ca_topic_score_codex":0.49122295,"about_ca_topic_score_gemma":0.9932494,"teacher_disagreement_score":0.50202644,"about_ca_system_score_codex":0.000003443052,"about_ca_system_score_gemma":0.0014925251,"threshold_uncertainty_score":0.9999584},"labels":[],"label_agreement":null},{"id":"W2068677550","doi":"10.1139/e06-011","title":"Diagenetic fluorapatite and aluminum phosphatesulphate in the Paleoproterozoic Thelon Formation and Hornby Bay Group, northwestern Canadian Shield","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University; Statistics Canada","funders":"","keywords":"Geology; Diagenesis; Geochemistry; Bay; Paragenesis; Fluorapatite; Geochronology; Paleontology; Metamorphic rock; Oceanography; Apatite","score_opus":0.00822766585795658,"score_gpt":0.1724133749489636,"score_spread":0.16418570909100702,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068677550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99469286,0.00305623,0.000005511155,0.0009826594,0.00006934449,0.00008179449,0.000035152963,0.0000010577305,0.0010753844],"genre_scores_gemma":[0.999321,0.00010794268,0.000114310555,0.00035403928,0.000057948575,5.0537375e-7,0.000016775764,9.887883e-7,0.000026520047],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990083,0.00005846556,0.00025522374,0.00012988338,0.00019121311,0.00035692364],"domain_scores_gemma":[0.99940443,0.00005010159,0.00011438578,0.0000653699,0.000025284518,0.00034041985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00077358243,0.00009891407,0.00011768118,0.00023984892,0.0004197751,0.00031119128,0.00023281107,0.000035821475,0.00024106333],"category_scores_gemma":[0.000015249344,0.00006551361,0.000030272462,0.00039840714,0.00027067005,0.00047323544,0.0000027219012,0.0001119031,0.00000548982],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000018452972,0.0000014855323,0.9911911,0.0000065494987,0.0000029214502,0.00005157383,0.00058016524,0.00033666557,0.000015317504,0.000008306222,0.000022820797,0.00778127],"study_design_scores_gemma":[0.00012568237,0.00012963712,0.9952929,0.000030829993,0.000012636768,0.00013124905,0.0011532797,0.0011735099,0.000128722,0.00043609217,0.0012910304,0.000094451265],"about_ca_topic_score_codex":0.6667315,"about_ca_topic_score_gemma":0.9982373,"teacher_disagreement_score":0.33150586,"about_ca_system_score_codex":0.0000024734968,"about_ca_system_score_gemma":0.00020789856,"threshold_uncertainty_score":0.3354878},"labels":[],"label_agreement":null},{"id":"W2068778666","doi":"10.1139/e04-004","title":"Variations in mixed-layer illite/smectite diagenesis in the rift and post-rift sediments of the Jeanne d'Arc Basin, Grand Banks offshore Newfoundland, Canada","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Clay minerals and soil interactions","field":"Materials Science","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University; Memorial University of Newfoundland","funders":"","keywords":"Geology; Illite; Diagenesis; Clay minerals; Geochemistry; Lithology; Structural basin; Rift; Denudation; Petrology; Geomorphology; Paleontology; Tectonics","score_opus":0.016049310255992964,"score_gpt":0.23236899413866927,"score_spread":0.2163196838826763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068778666","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99009204,0.0003337812,0.000008748751,0.008090284,0.0008249452,0.00010297729,0.00006420775,7.3171503e-7,0.00048229832],"genre_scores_gemma":[0.9989051,0.000020970823,0.00013194617,0.0008146433,0.00005804503,0.000001989551,6.834901e-7,0.0000033111266,0.00006326618],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873066,0.0001270386,0.00037735765,0.00013756765,0.00034020562,0.00028718682],"domain_scores_gemma":[0.9991729,0.00018473918,0.00018959474,0.00013291644,0.00014247844,0.00017736635],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009875912,0.00009430657,0.00016835153,0.0002211679,0.000351884,0.00015910188,0.0004292997,0.000033998822,0.00009256633],"category_scores_gemma":[0.00029499983,0.000055147553,0.00004562515,0.0006059698,0.00029432712,0.00032022406,0.000015322288,0.00015892988,8.922415e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003011654,0.000088741,0.94227415,0.000023118615,0.00002395674,0.00015879134,0.012933781,0.015685443,0.023779523,0.0032952684,0.0007174722,0.000989621],"study_design_scores_gemma":[0.00037224372,0.00008518263,0.9924225,0.00009931963,0.000012648142,0.00009939048,0.0010065206,0.000063922045,0.0012410859,0.000383193,0.004128044,0.00008592985],"about_ca_topic_score_codex":0.8982204,"about_ca_topic_score_gemma":0.99900717,"teacher_disagreement_score":0.10078675,"about_ca_system_score_codex":0.000042904794,"about_ca_system_score_gemma":0.0029447593,"threshold_uncertainty_score":0.5223877},"labels":[],"label_agreement":null},{"id":"W2068901787","doi":"10.1139/e06-077","title":"Giant dinosaur eggs from the Tiantai basin, Zhejiang Province, China","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Jurassic Foundation; U.S. Department of State","keywords":"Cretaceous; Geology; Eggshell; Paleontology; Structural basin; China; Archaeology; Geography","score_opus":0.01380666417666557,"score_gpt":0.21642072202004184,"score_spread":0.20261405784337627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068901787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9664188,0.0055867033,0.00020397885,0.0049431543,0.0015218145,0.000073782474,0.00007954377,0.000005188101,0.021167051],"genre_scores_gemma":[0.9973889,0.000049179114,0.0007418498,0.0011341893,0.00044727066,5.2833602e-8,0.000007274808,0.000001071098,0.00023019945],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99862057,0.000107148764,0.00031377244,0.00017386048,0.00021378795,0.000570888],"domain_scores_gemma":[0.9988007,0.0003249206,0.0001970278,0.000112451715,0.000055361914,0.0005095343],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017342427,0.00010962728,0.00016657673,0.00017205394,0.00086722476,0.00007183748,0.0007004912,0.00008792946,0.0022804476],"category_scores_gemma":[0.00018713294,0.00006387106,0.000077139615,0.00035262466,0.0012786184,0.0003719177,0.000004453491,0.00027973077,0.00009285108],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013436555,0.0000022303668,0.9896093,7.669067e-7,0.000011467994,0.00019944088,0.00017390249,0.00013125618,0.000015147307,0.00019232111,0.001437754,0.008212995],"study_design_scores_gemma":[0.00010320398,0.00018945865,0.9601554,0.000019038429,0.000009913897,0.00032781702,0.00031879495,0.00022592518,0.000027666314,0.0011458631,0.03738464,0.00009222988],"about_ca_topic_score_codex":0.05984276,"about_ca_topic_score_gemma":0.91254693,"teacher_disagreement_score":0.85270417,"about_ca_system_score_codex":0.0000025187771,"about_ca_system_score_gemma":0.0016033467,"threshold_uncertainty_score":0.9986316},"labels":[],"label_agreement":null},{"id":"W2068927737","doi":"10.1139/e04-053","title":"Braincase structure of the Middle Jurassic theropod dinosaur<i>Piatnitzkysaurus</i>","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Nature; Deutsche Forschungsgemeinschaft","keywords":"Geology; Autapomorphy; Paleontology; Theropoda; Anatomy; Synapomorphy; Fossa; Biology; Taxon; Phylogenetics","score_opus":0.02026952223073912,"score_gpt":0.19761884518535872,"score_spread":0.17734932295461958,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068927737","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99178445,0.0020324015,0.000008044179,0.002072637,0.0010620935,0.000051099774,0.000107795146,0.0000021136882,0.0028793437],"genre_scores_gemma":[0.99905026,0.000015151542,0.00031153127,0.00044610392,0.00011902689,2.9377983e-8,0.0000018805362,9.679317e-7,0.000055050143],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989703,0.00009988326,0.0002688266,0.00012278247,0.00019423355,0.00034393175],"domain_scores_gemma":[0.99917847,0.00008433598,0.00025422813,0.00011588053,0.000076975804,0.00029013483],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00033527418,0.00009402769,0.00016425725,0.00015194084,0.0005056541,0.00002516944,0.0006474806,0.000084285544,0.0009757127],"category_scores_gemma":[0.00014328682,0.0000531139,0.00009468715,0.00044086794,0.0016079883,0.00024561273,0.000004541324,0.00021642211,0.000013190618],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000072752186,0.0000034326229,0.9944774,0.000003708017,0.000012883273,0.000033011383,0.0003990861,0.0033416916,0.00027030436,0.00057736074,0.00008299846,0.0007908699],"study_design_scores_gemma":[0.00020078322,0.00022928859,0.98730963,0.00003521987,0.000010975288,0.0005901331,0.00026825603,0.000043805358,0.0003869728,0.008609018,0.0022398538,0.00007606102],"about_ca_topic_score_codex":0.011766618,"about_ca_topic_score_gemma":0.7248622,"teacher_disagreement_score":0.7130956,"about_ca_system_score_codex":0.000002372861,"about_ca_system_score_gemma":0.0020226103,"threshold_uncertainty_score":0.99993753},"labels":[],"label_agreement":null},{"id":"W2069206841","doi":"10.1139/e11-017","title":"Basal ornithopod (Dinosauria: Ornithischia) teeth from the Prince Creek Formation (early Maastrichtian) of Alaska","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Paleontology; Canyon; Cretaceous; Cheek teeth; Geomorphology","score_opus":0.03296144267496378,"score_gpt":0.19873276092910394,"score_spread":0.16577131825414015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069206841","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98918736,0.0015677623,0.00018173903,0.0004414909,0.00074124924,0.00006804727,0.000119142955,0.0000032376954,0.0076899775],"genre_scores_gemma":[0.9968593,0.000036553887,0.0026602868,0.00025015447,0.00013530627,1.6727562e-7,0.000006596049,0.0000010707453,0.000050576225],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987122,0.00020711552,0.00037892882,0.00013335154,0.00021552348,0.00035288878],"domain_scores_gemma":[0.99882925,0.00025365196,0.00036741755,0.00011573049,0.00012575866,0.00030820727],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009294838,0.00009428923,0.00017916887,0.00016636166,0.0004721758,0.000039115916,0.00066618103,0.00008936207,0.00236979],"category_scores_gemma":[0.00019792188,0.00006221107,0.00007045953,0.0003817321,0.0010646054,0.00066044775,0.0000057275715,0.00023201607,0.000064334534],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021866572,0.0000037469554,0.9965313,0.0000014604227,0.000014927558,0.00002645977,0.00087255513,0.00007893476,0.000008009604,0.000051158728,0.00028463086,0.002104926],"study_design_scores_gemma":[0.00014794074,0.00040692394,0.9950953,0.0000242667,0.00001834626,0.00012126409,0.0006009146,0.00013239686,0.000057982823,0.0019100406,0.0014064178,0.00007817015],"about_ca_topic_score_codex":0.03581912,"about_ca_topic_score_gemma":0.72201467,"teacher_disagreement_score":0.68619555,"about_ca_system_score_codex":0.0000016673396,"about_ca_system_score_gemma":0.0010512555,"threshold_uncertainty_score":0.9985422},"labels":[],"label_agreement":null},{"id":"W2069307107","doi":"10.1139/e03-016","title":"Paleoweathered surfaces on granitoids of southern Nova Scotia: paleoenvironmental implications of saprolites","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Saprolite; Geology; Weathering; Geochemistry; Batholith; Sedimentary rock; Clastic rock; Carboniferous; Biotite; Paleontology; Quartz","score_opus":0.01630251330936127,"score_gpt":0.19711794396605928,"score_spread":0.180815430656698,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069307107","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926499,0.00081011,0.0000050208237,0.00017697643,0.00008145163,0.00003943833,0.0002370983,9.235161e-7,0.005999076],"genre_scores_gemma":[0.99937016,0.000018481016,0.00048003384,0.000039306564,0.000019228346,4.5889337e-8,0.000005936372,0.0000011942293,0.00006559144],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998981,0.000052948315,0.00035276957,0.00012375946,0.00024823382,0.00024130782],"domain_scores_gemma":[0.99920225,0.000068223,0.00029747927,0.00010532555,0.00004930525,0.00027740968],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005217583,0.00009126306,0.00018810341,0.00015761112,0.00015556997,0.000027427184,0.00029644705,0.00003302219,0.0052995365],"category_scores_gemma":[0.000062975574,0.00006866624,0.00010685061,0.00039799206,0.0005910189,0.000112515714,0.0000017629068,0.00008228561,0.00003604752],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000038812314,0.000011447368,0.9946149,0.0000069557027,0.000020691283,0.0000028698114,0.00019400696,0.0031117373,0.0011449965,0.00003289434,0.000020045642,0.0008355729],"study_design_scores_gemma":[0.00017233312,0.00034998916,0.9848272,0.000045003926,0.00003130187,0.00003748069,0.0029309087,0.000042553096,0.01027734,0.0006622026,0.0005184971,0.00010515625],"about_ca_topic_score_codex":0.010609968,"about_ca_topic_score_gemma":0.22632268,"teacher_disagreement_score":0.21571271,"about_ca_system_score_codex":0.0000013898691,"about_ca_system_score_gemma":0.00028387742,"threshold_uncertainty_score":0.9959785},"labels":[],"label_agreement":null},{"id":"W2069344231","doi":"10.1139/e02-063","title":"<i>Archaeovenator hamiltonensis</i>, a new varanopid (Synapsida: Eupelycosauria) from the Upper Carboniferous of Kansas","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Amgen (Canada)","funders":"","keywords":"Carboniferous; Paleontology; Geology; Permian; Fauna; Tetrapod (structure); Genus; Taxon; Paleozoic; Amniote; Biology; Zoology; Vertebrate; Structural basin; Ecology","score_opus":0.019462128409066658,"score_gpt":0.20149823333009656,"score_spread":0.1820361049210299,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069344231","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97449124,0.0152303325,0.000060641272,0.0024536576,0.0014550867,0.00007037954,0.000085551175,0.0000030830086,0.0061500263],"genre_scores_gemma":[0.9972784,0.000108727945,0.0015941083,0.00072142354,0.00016738316,1.00514285e-7,0.0000037216957,0.0000015235689,0.00012464858],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984613,0.0002820706,0.0003749509,0.0001835678,0.00023745504,0.00046065255],"domain_scores_gemma":[0.9985639,0.00044791,0.00023513794,0.00015081378,0.00008983359,0.00051241566],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00090359617,0.00012459364,0.0002649834,0.00016156415,0.0003805988,0.000028114075,0.0005882576,0.00010413852,0.0016203888],"category_scores_gemma":[0.00039743225,0.000078213976,0.000112073016,0.00039351088,0.0014181422,0.00021907054,0.0000034810187,0.00024075595,0.000039127193],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015129725,0.0000030894057,0.9960934,0.0000011989583,0.00003233091,0.0000524059,0.00039087905,0.0005543583,0.000055055218,0.00094463537,0.0008441599,0.0010133922],"study_design_scores_gemma":[0.0002402765,0.00028135013,0.9584538,0.00002497195,0.000023636057,0.00033618996,0.00030322108,0.000107036736,0.00017320058,0.006043592,0.033904385,0.00010837699],"about_ca_topic_score_codex":0.070185386,"about_ca_topic_score_gemma":0.6379223,"teacher_disagreement_score":0.5677369,"about_ca_system_score_codex":0.0000020980758,"about_ca_system_score_gemma":0.003213263,"threshold_uncertainty_score":0.99929225},"labels":[],"label_agreement":null},{"id":"W2069385652","doi":"10.1139/e03-091","title":"Stratigraphy, geochronology, and geochemistry of the Georgie River area, northwest British Columbia, and implications for mineral exploration","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Clastic rock; Geochronology; Geochemistry; Pyroclastic rock; Zircon; Volcanic rock; Rhyolite; Facies; Volcano; Paleontology; Sedimentary rock; Structural basin","score_opus":0.017109276522682803,"score_gpt":0.19119296424075913,"score_spread":0.17408368771807634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069385652","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962882,0.0011380089,0.000029817784,0.0019381329,0.00004031946,0.00006148002,0.00018256105,0.0000012264676,0.00032025448],"genre_scores_gemma":[0.9988302,0.00006642778,0.0009345878,0.00010331066,0.000030747327,5.203715e-7,0.000009474325,4.7206765e-7,0.000024236777],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994058,0.00001235462,0.00019446375,0.00012571362,0.0000782702,0.0001833827],"domain_scores_gemma":[0.9993998,0.000057957528,0.0001400876,0.00005573439,0.000115589624,0.00023081989],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017789495,0.000049034847,0.00012353077,0.000038342532,0.00035847395,0.00013160807,0.0001801318,0.00004084689,0.00026695908],"category_scores_gemma":[0.000100107274,0.000041538384,0.000059036203,0.00023835707,0.0012241479,0.00020704254,0.000004822394,0.00007069951,2.4079768e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.919394e-7,0.0000033965896,0.9962267,0.0000045516326,0.000008189569,0.000001588276,0.00003829749,0.00052624353,0.0002072222,0.00004433714,0.000051623305,0.0028868343],"study_design_scores_gemma":[0.00014627737,0.00011495659,0.95221424,0.00001831506,0.000019601825,0.00008592497,0.00013303108,0.00008740964,0.0000897012,0.046814874,0.00022205913,0.000053633263],"about_ca_topic_score_codex":0.298863,"about_ca_topic_score_gemma":0.984792,"teacher_disagreement_score":0.685929,"about_ca_system_score_codex":7.9979435e-7,"about_ca_system_score_gemma":0.00033585314,"threshold_uncertainty_score":0.70580596},"labels":[],"label_agreement":null},{"id":"W2069532636","doi":"10.1139/e03-075","title":"Cyanobacteria associated with hot spring travertines","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Cyanobacteria; Hot spring; Photosynthesis; Geology; Microbial mat; Carbonate; Karst; Phototroph; Ecology; Spring (device); Deposition (geology); Botany; Biology; Paleontology; Chemistry; Sediment; Bacteria","score_opus":0.020776950791642657,"score_gpt":0.19898308431889652,"score_spread":0.17820613352725387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069532636","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94209445,0.0016446962,0.00003143246,0.00009224528,0.00035271153,0.00003113077,0.000008815904,0.000003532054,0.05574099],"genre_scores_gemma":[0.99884707,0.000009209727,0.0010226739,0.000058070138,0.00003071487,5.340452e-8,2.8848845e-7,5.0283575e-7,0.000031392254],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989816,0.000100700905,0.00021264947,0.00011889751,0.00019139546,0.00039478316],"domain_scores_gemma":[0.99910146,0.00010112795,0.00017916104,0.00005721931,0.000075984244,0.00048503402],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007945438,0.00009530933,0.0001623071,0.00022797768,0.00044189786,0.00010699188,0.00023138097,0.000050206276,0.00065882265],"category_scores_gemma":[0.00022896526,0.00006490672,0.00005459373,0.0004076308,0.000565042,0.0003867084,1.52169e-7,0.00013938145,0.000005648478],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000054352577,0.0000020431187,0.9973852,9.551114e-7,0.00001617582,0.000094004165,0.00012530044,0.00011452213,0.000024193274,0.00030233906,0.000010179364,0.0019196522],"study_design_scores_gemma":[0.00016470124,0.00033387067,0.997716,0.000039942297,0.0000107287815,0.00015945922,0.0001568064,0.000039009195,0.00021757337,0.0001911351,0.0008706034,0.000100161444],"about_ca_topic_score_codex":0.0045908894,"about_ca_topic_score_gemma":0.7129749,"teacher_disagreement_score":0.70838404,"about_ca_system_score_codex":7.956666e-7,"about_ca_system_score_gemma":0.0013834821,"threshold_uncertainty_score":0.7213646},"labels":[],"label_agreement":null},{"id":"W2069590943","doi":"10.1139/e03-096","title":"On the discovery of a unique terrestrial faunal assemblage in the classic Pennsylvanian section at Joggins, Nova Scotia","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Mollusks and Parasites Studies","field":"Agricultural and Biological Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Nova Scotia Department of Energy; Technical University of Nova Scotia; Bell (Canada)","funders":"","keywords":"Pennsylvanian; Tetrapod (structure); Geology; Paleontology; Assemblage (archaeology); Faunal assemblage; Nova scotia; Paleozoic; Fauna; Ecology; Biology; Oceanography; Structural basin","score_opus":0.04201579971139722,"score_gpt":0.24117099763790836,"score_spread":0.19915519792651115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069590943","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913058,0.00013637626,0.0000027493518,0.0062277215,0.00039379604,0.00010283863,0.000012925426,0.0000010501985,0.001816736],"genre_scores_gemma":[0.999256,0.0000143537145,0.000009961268,0.00039982374,0.00025931848,5.005718e-7,8.916836e-7,3.5891085e-7,0.000058785008],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990062,0.00012894807,0.0002359591,0.00011016478,0.00027835206,0.00024034658],"domain_scores_gemma":[0.9993584,0.00029436286,0.00018978721,0.00003859237,0.00003013558,0.0000887196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00094919204,0.000085507345,0.00013290482,0.000048766833,0.00042830664,0.00014626094,0.0004435011,0.000038257516,0.00010830979],"category_scores_gemma":[0.00014062446,0.000023184228,0.0000911339,0.0005544072,0.0003719538,0.00019598076,0.0000129954,0.00017596957,0.0000050466983],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014399197,0.00012041571,0.92705077,0.000008145799,0.00004343582,0.00018851433,0.0031577214,0.0031587994,0.044650897,0.016119162,0.0027708046,0.0025873655],"study_design_scores_gemma":[0.0001700821,0.00090418017,0.993188,0.00009640201,0.00000695752,0.00007489987,0.0008337171,0.00001143422,0.00065338175,0.0015063721,0.0024679126,0.000086609456],"about_ca_topic_score_codex":0.054884598,"about_ca_topic_score_gemma":0.9155975,"teacher_disagreement_score":0.8607129,"about_ca_system_score_codex":0.000017954853,"about_ca_system_score_gemma":0.00018942944,"threshold_uncertainty_score":0.951409},"labels":[],"label_agreement":null},{"id":"W2069599591","doi":"10.1139/e00-065","title":"Crustal geometry and tectonic evolution of the Archean crystalline basement beneath the southern Alberta Plains, from new seismic reflection and potential-field studies","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Archean; Proterozoic; Crust; Craton; Precambrian; Imbrication; Continental crust; Lithosphere; Basement; Terrane; Tectonics; Seismology; Paleontology; Geochemistry; Petrology","score_opus":0.014732954361153626,"score_gpt":0.2022603709082156,"score_spread":0.18752741654706198,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069599591","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9892671,0.0059758895,0.00002170231,0.0043045017,0.000065633096,0.00004459725,0.000020795498,0.0000010263585,0.00029874788],"genre_scores_gemma":[0.9990336,0.00018353123,0.00009604901,0.00024046043,0.00008051362,7.353806e-8,0.000001272711,6.4844136e-7,0.00036385475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99916065,0.00007589405,0.00021476534,0.00013256344,0.00021709336,0.00019903043],"domain_scores_gemma":[0.9993518,0.000200882,0.00011656949,0.000069197646,0.00004076147,0.0002207644],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042057835,0.000080886064,0.00014971611,0.0000812497,0.00041388746,0.000055984874,0.00020813818,0.00003324237,0.002069423],"category_scores_gemma":[0.00015099371,0.00003710908,0.0000624472,0.00035136787,0.00047708047,0.00009971174,0.000008751364,0.00014416165,0.000003057616],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000045376073,0.0000051621105,0.9538912,0.0000062339777,0.00008465833,0.0000065448608,0.0009992782,0.01565625,0.00022350831,0.000017380298,0.000113275215,0.028951105],"study_design_scores_gemma":[0.00033856294,0.0007767137,0.96225446,0.000082861174,0.00014731109,0.000080513135,0.0039289137,0.011692469,0.00048113844,0.0186826,0.0013776114,0.00015683257],"about_ca_topic_score_codex":0.34182867,"about_ca_topic_score_gemma":0.7024555,"teacher_disagreement_score":0.36062685,"about_ca_system_score_codex":0.0000024680367,"about_ca_system_score_gemma":0.0002312154,"threshold_uncertainty_score":0.99884284},"labels":[],"label_agreement":null},{"id":"W2069748752","doi":"10.1139/e05-035","title":"Tectonic evolution of the Manitoba-Saskatchewan segment of the Paleoproterozoic Trans-Hudson Orogen, Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":121,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Geology; Craton; Terrane; Supercontinent; Subduction; Tectonics; Continental margin; Geochemistry; Accretion (finance); Metamorphism; Paleontology; Island arc; Rift; Earth science","score_opus":0.009063292629885582,"score_gpt":0.160275268787909,"score_spread":0.1512119761580234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069748752","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994135,0.001425861,0.000010773839,0.003378308,0.00022549622,0.00007782727,0.000040291296,8.276892e-7,0.0007056179],"genre_scores_gemma":[0.9995005,0.0000074200243,0.0001849101,0.0001813239,0.000062144485,1.5334379e-7,4.4995346e-7,6.866843e-7,0.00006241539],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861515,0.00009074726,0.00037306556,0.000115664465,0.0005051875,0.00030018424],"domain_scores_gemma":[0.9991471,0.000055133256,0.00029660884,0.00013436103,0.00011453098,0.00025227785],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004689899,0.00008986907,0.00018187148,0.00006785037,0.0002855537,0.000020526655,0.0007694272,0.000036043246,0.0017408123],"category_scores_gemma":[0.0000704919,0.00004212397,0.00016074056,0.0007065225,0.0005797027,0.00010152275,0.0000068022327,0.000164023,0.0000020219563],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000034167726,0.0000043718787,0.9855824,0.0000061566266,0.000015233883,0.0000020572757,0.00012587823,0.010023448,0.000485389,0.000015696576,0.00006080266,0.0036751418],"study_design_scores_gemma":[0.000093887815,0.00009087845,0.98837805,0.00004193072,0.000031351326,0.000029419834,0.0010471985,0.00066777883,0.0072969412,0.00070089125,0.0015533093,0.00006838455],"about_ca_topic_score_codex":0.89057076,"about_ca_topic_score_gemma":0.99969685,"teacher_disagreement_score":0.10912605,"about_ca_system_score_codex":0.000010383187,"about_ca_system_score_gemma":0.0029897096,"threshold_uncertainty_score":0.99917173},"labels":[],"label_agreement":null},{"id":"W2070181883","doi":"10.1139/e01-014","title":"Depositional environments of Quaternary lacustrine travertines and stromatolites from high-altitude Andean lakes, northwestern Argentina","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Consejo Superior de Investigaciones Científicas","keywords":"Geology; Sedimentary depositional environment; Petrography; Facies; Tufa; Diagenesis; Geochemistry; Quaternary; Stromatolite; Paleontology; Fluvial; Structural basin; Geomorphology; Carbonate","score_opus":0.014920593411599247,"score_gpt":0.19794652315677302,"score_spread":0.1830259297451738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070181883","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934103,0.004931302,0.00004141344,0.0001649566,0.00019071039,0.00003759178,0.00013668765,0.0000016799522,0.0010853453],"genre_scores_gemma":[0.9987923,0.00016323247,0.0009114764,0.00003253566,0.000070735885,8.4479865e-8,0.000008916778,5.639946e-7,0.000020170395],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990018,0.000054429987,0.0003126636,0.00014208084,0.00022905633,0.0002599654],"domain_scores_gemma":[0.99922305,0.00008047726,0.00021302188,0.0000593946,0.000021020185,0.0004030196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022131963,0.00010050251,0.00019178048,0.00018784708,0.00022782075,0.00004917529,0.00021740925,0.00004679733,0.00041886815],"category_scores_gemma":[0.0000143100615,0.00007819129,0.0000508531,0.00013804286,0.000589406,0.00029807803,0.0000011338576,0.000094137766,0.0000028934887],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014956461,0.000005620576,0.9946061,0.0000024251242,0.00002367762,0.00016191168,0.00011423549,0.000086072025,0.00015493686,0.000049674967,0.0000057541433,0.004774682],"study_design_scores_gemma":[0.0002548174,0.00023400271,0.9979175,0.000036767004,0.000017049453,0.0002675146,0.00012569633,0.00017276633,0.00023547809,0.00043277472,0.0002223581,0.00008332645],"about_ca_topic_score_codex":0.03347507,"about_ca_topic_score_gemma":0.521441,"teacher_disagreement_score":0.48796594,"about_ca_system_score_codex":5.780853e-7,"about_ca_system_score_gemma":0.00022081172,"threshold_uncertainty_score":0.9729611},"labels":[],"label_agreement":null},{"id":"W2070434453","doi":"10.1139/e02-109","title":"The Prospect Rock thrust: western limit of the Taconian accretionary prism in the northern Green Mountain anticlinorium, Vermont","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Thrust fault; Imbrication; Dalradian; Fault (geology); Accretionary wedge; Metamorphism; Metamorphic rock; Geochemistry; Paleontology; Seismology; Subduction; Tectonics","score_opus":0.014746790637378897,"score_gpt":0.19363118816350341,"score_spread":0.1788843975261245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070434453","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98823273,0.0015960198,0.0000037763605,0.006815075,0.0001710983,0.00010333894,0.000008203227,0.0000011511387,0.0030685877],"genre_scores_gemma":[0.99926925,0.000042575633,0.000040090785,0.00044007768,0.000061177074,3.5417193e-7,7.1390366e-7,9.0584206e-7,0.00014484483],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99842495,0.00024114498,0.0003700179,0.00014009929,0.00044636067,0.0003774096],"domain_scores_gemma":[0.9990211,0.0002980466,0.00024265662,0.00016261174,0.000084925654,0.00019063531],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015449739,0.000101840764,0.00016480438,0.000077785466,0.00060916337,0.000116104195,0.0010413092,0.00004408017,0.00045746536],"category_scores_gemma":[0.00029798606,0.000039730945,0.00013375541,0.0007847576,0.0005623177,0.00016085122,0.000008053715,0.00027987745,0.000018152099],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004009392,0.0000050658814,0.99688756,0.0000015811418,0.000007975392,0.000018446604,0.00028976714,0.0015239059,0.000010800711,0.00011834954,0.000017005286,0.0011155494],"study_design_scores_gemma":[0.00008977634,0.00013855439,0.98872733,0.00001671957,0.00001435223,0.00007482395,0.000669198,0.0005872289,0.00007530305,0.0060305614,0.0035087955,0.000067381145],"about_ca_topic_score_codex":0.028403176,"about_ca_topic_score_gemma":0.7617446,"teacher_disagreement_score":0.73334146,"about_ca_system_score_codex":0.000002613886,"about_ca_system_score_gemma":0.0006032521,"threshold_uncertainty_score":0.97806674},"labels":[],"label_agreement":null},{"id":"W2070437686","doi":"10.1139/e09-052","title":"Extrapolating strong ground motion of the Silakhor earthquake (ML 6.1), Iran, using the empirical Green's function (EGF) approach based on a genetic algorithm","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Performance and Analysis","field":"Engineering","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Seismogram; Algorithm; Replicate; Geology; Spectral line; Aftershock; Function (biology); Genetic algorithm; Strong ground motion; Motion (physics); Ground motion; Synthetic data; Seismology; Computer science; Mathematics; Physics; Statistics; Artificial intelligence; Machine learning; Biology","score_opus":0.06312732004574056,"score_gpt":0.24630618132547508,"score_spread":0.1831788612797345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070437686","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94724417,0.00025726773,0.051614735,0.00021720574,0.00021138423,0.0000571835,0.0000032934909,0.000004904049,0.00038988114],"genre_scores_gemma":[0.99650633,0.0000050058356,0.003065979,0.00024115025,0.00016891726,2.6863066e-7,3.802677e-7,0.000004465046,0.000007477843],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989748,0.00005641446,0.00028436075,0.000097619515,0.00032889834,0.0002579064],"domain_scores_gemma":[0.9995146,0.000033043234,0.000121471654,0.00012712665,0.000067627,0.0001361813],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005998948,0.00009803992,0.00013829152,0.00034060105,0.0003702471,0.00008173298,0.0002661806,0.000040069594,0.000021350665],"category_scores_gemma":[0.000022666962,0.00005849596,0.00012580986,0.0009834582,0.00016236262,0.00021410063,0.0000026943349,0.00021043739,6.334149e-7],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000023425391,0.000006707997,0.013439882,0.0000066851203,0.0000139672975,0.0000024557944,0.00021581547,0.95026124,0.000360356,0.0000077987515,0.000024861618,0.035657868],"study_design_scores_gemma":[0.00009679581,0.0000971742,0.25494865,0.000045482906,0.000030583764,0.000021080557,0.00037847413,0.7440801,0.00009652534,0.00004297654,0.0001054807,0.000056645673],"about_ca_topic_score_codex":0.00067698536,"about_ca_topic_score_gemma":0.0011032863,"teacher_disagreement_score":0.24150875,"about_ca_system_score_codex":0.000014251083,"about_ca_system_score_gemma":0.0002383032,"threshold_uncertainty_score":0.28476787},"labels":[],"label_agreement":null},{"id":"W2070554573","doi":"10.1139/e03-087","title":"Emplacement, rapid burial, and exhumation of 90-Ma plutons in southeastern Alaska","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Pluton; Geology; Terrane; Geochemistry; Thrust fault; Magma; Seismology; Tectonics; Petrology; Volcano","score_opus":0.021303006116056643,"score_gpt":0.20410847855044686,"score_spread":0.18280547243439021,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070554573","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951939,0.0009558589,0.000019626737,0.0009719677,0.00009372009,0.000034589255,0.000015737558,0.0000011142963,0.0027135115],"genre_scores_gemma":[0.9993047,0.000036062404,0.00050877396,0.00009354401,0.000036894206,6.817638e-8,0.0000023055288,4.7596262e-7,0.000017155982],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99912596,0.000036256162,0.00030030255,0.0001108549,0.0001933494,0.00023328129],"domain_scores_gemma":[0.99937713,0.00005245591,0.00015628766,0.000044757693,0.000050314608,0.00031905336],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00055845606,0.00006733903,0.00017230547,0.00027210225,0.000111046706,0.000049615195,0.00018724336,0.0000331871,0.0034890794],"category_scores_gemma":[0.0001070045,0.000045664878,0.000047885973,0.00040060785,0.00041334453,0.00020797267,0.0000038641083,0.000089977046,0.000012992008],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008141302,0.0000055375226,0.9883344,0.0000051232705,0.0000070127053,0.00001791186,0.00042980709,0.0072949594,0.00009636369,0.00008761149,0.000005057814,0.0037080497],"study_design_scores_gemma":[0.0003275857,0.0003216885,0.99060154,0.00004970133,0.000010869034,0.00003639143,0.0007591218,0.00034028,0.0002549676,0.0069267736,0.00029168496,0.000079380516],"about_ca_topic_score_codex":0.02377704,"about_ca_topic_score_gemma":0.38689107,"teacher_disagreement_score":0.36311403,"about_ca_system_score_codex":9.3047265e-7,"about_ca_system_score_gemma":0.00031386415,"threshold_uncertainty_score":0.99742186},"labels":[],"label_agreement":null},{"id":"W2070700941","doi":"10.1139/e07-020","title":"Micro X-ray diffraction (µXRD): a versatile technique for characterization of Earth and planetary materials","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"X-ray Diffraction in Crystallography","field":"Materials Science","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Electron microprobe; Mineralogy; Geology; Diffraction; Thin section; Materials science; Mineral; Mosaicity; X-ray crystallography; Analytical Chemistry (journal); Optics; Chemistry; Physics; Metallurgy","score_opus":0.015259009866575335,"score_gpt":0.23678368004072622,"score_spread":0.2215246701741509,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070700941","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942669,0.00006137381,0.0040323967,0.0001430651,0.00096223224,0.00028106247,0.00014791936,0.000006488712,0.00009855406],"genre_scores_gemma":[0.98987484,0.000020919855,0.009800603,0.00009062318,0.00015768022,0.0000037156497,0.000008710731,0.0000074505706,0.000035432542],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9986744,0.000055247034,0.0005219111,0.00017835648,0.00023698615,0.00033312265],"domain_scores_gemma":[0.9986458,0.00014318818,0.0006265926,0.0000979499,0.00019599669,0.0002905076],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021128794,0.00011285689,0.0002328352,0.00063118694,0.0002699059,0.00014568532,0.00022528511,0.0000836841,0.0003828549],"category_scores_gemma":[0.00013029522,0.00009873797,0.000049970786,0.0002978177,0.00046493017,0.00070305995,0.000008913316,0.00007783342,0.000002695109],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035460638,0.0000086468135,0.012379815,0.000025951746,0.000005366715,0.0000060751595,0.0001708688,0.000018130857,0.987142,0.00006601014,0.000021589452,0.000120028664],"study_design_scores_gemma":[0.00022276228,0.00031460536,0.35413697,0.00007550398,0.000015007438,0.000102561506,0.00019821552,0.000005567026,0.63939506,0.00014189511,0.005287106,0.00010475587],"about_ca_topic_score_codex":0.0009612314,"about_ca_topic_score_gemma":0.004043795,"teacher_disagreement_score":0.34774703,"about_ca_system_score_codex":0.0000064340397,"about_ca_system_score_gemma":0.00044422262,"threshold_uncertainty_score":0.41919926},"labels":[],"label_agreement":null},{"id":"W2070887644","doi":"10.1139/e06-115","title":"Modèles d'astroblèmes d'après le déplacement des masses rocheuses : Charlevoix et le Ries","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Impact crater; Impact structure; Graben; Breccia; Classification of discontinuities; Seismology; Fault scarp; Fault (geology); Geomorphology; Tectonics","score_opus":0.03473137938259563,"score_gpt":0.23523293315790425,"score_spread":0.20050155377530862,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070887644","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94867176,0.0006444021,0.030705169,0.0008330927,0.00029897623,0.0000611128,0.00003666361,0.0000050486747,0.018743755],"genre_scores_gemma":[0.98850244,0.0000051062,0.010847932,0.000087046006,0.0001584875,3.7879005e-7,0.000003097282,0.000003935612,0.00039157222],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987398,0.00003952007,0.0002812351,0.00015494581,0.0002654749,0.0005190635],"domain_scores_gemma":[0.9989733,0.00009954137,0.00019610075,0.00008653887,0.000111480724,0.000533017],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012059248,0.00012627985,0.00016479289,0.0002405652,0.0006960338,0.00025242748,0.0004533529,0.000019565416,0.0003326123],"category_scores_gemma":[0.00002675066,0.00010303644,0.00007462677,0.0003120985,0.0007647553,0.00088274165,0.000014798528,0.00014390057,0.000012483848],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000062185386,0.000018900104,0.96439123,0.0000036221602,0.000021618893,0.000017529688,0.0007520349,0.0032242541,0.00059989974,0.026080122,0.00032835666,0.0045561986],"study_design_scores_gemma":[0.0004428306,0.0004213825,0.94524026,0.00011973063,0.000016586175,0.000050062114,0.013107923,0.0003024273,0.0062034037,0.005192305,0.02856989,0.00033317407],"about_ca_topic_score_codex":0.017398039,"about_ca_topic_score_gemma":0.06574745,"teacher_disagreement_score":0.048349407,"about_ca_system_score_codex":0.0000043206933,"about_ca_system_score_gemma":0.0025908514,"threshold_uncertainty_score":0.9891452},"labels":[],"label_agreement":null},{"id":"W2070899723","doi":"10.1139/e07-039","title":"The relative influence of Laurentide and local ice sheets during the last glacial maximum in the eastern Chic-Chocs Range, northern Gaspé Peninsula, Quebec","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université de Montréal; HEC Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Peninsula; Glacial period; Ice sheet; Plateau (mathematics); Glacier; Paleontology; Geomorphology; Oceanography; Meltwater; Archaeology; Geography","score_opus":0.01147910545985157,"score_gpt":0.2234187687277443,"score_spread":0.21193966326789274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070899723","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940063,0.0021165193,0.0000140392,0.0016292428,0.00015953927,0.00010999386,0.000005377773,0.0000011177693,0.0019579148],"genre_scores_gemma":[0.9996664,0.00005814689,0.000022393438,0.0001269326,0.000054055796,2.442488e-7,4.942985e-7,0.0000011890747,0.000070128284],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99829394,0.00032862372,0.00034191116,0.00013830302,0.00036909455,0.0005281405],"domain_scores_gemma":[0.9983352,0.0010126092,0.00020283838,0.000121472,0.000115480725,0.00021240118],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.003817343,0.00009961952,0.000151631,0.0001882772,0.0010414509,0.0001058392,0.0007781458,0.00006708885,0.00008860718],"category_scores_gemma":[0.0003162284,0.000047470083,0.000047812093,0.00052749505,0.0032051129,0.00034134547,0.000011852134,0.0005169207,0.000015784839],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042994023,0.0000022372985,0.9951451,0.0000040991886,0.000008799001,0.00012635984,0.0021937033,0.0016160923,0.0000017940501,0.00008162961,0.0000029100001,0.00077430095],"study_design_scores_gemma":[0.00020707215,0.00011178698,0.99520254,0.000032397875,0.000005460313,0.0004208476,0.0027488691,0.00023405248,0.000008940142,0.00054343883,0.00042770169,0.000056917717],"about_ca_topic_score_codex":0.038006347,"about_ca_topic_score_gemma":0.9927902,"teacher_disagreement_score":0.95478386,"about_ca_system_score_codex":0.0000012920061,"about_ca_system_score_gemma":0.0007465197,"threshold_uncertainty_score":0.9995076},"labels":[],"label_agreement":null},{"id":"W2070939036","doi":"10.1139/cjes-2014-0163","title":"Geodynamic setting, crustal architecture, and VMS metallogeny of ca. 2720 Ma greenstone belt assemblages of the northern Wawa subprovince, Superior Province","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geoscience BC; Geological Survey of Canada; Laurentian University","funders":"","keywords":"Greenstone belt; Geology; Metallogeny; Geochemistry; Basalt; Ultramafic rock; Mafic; Mantle plume; Rift; Island arc; Archean; Subduction; Tectonics; Paleontology; Lithosphere","score_opus":0.011352077525239628,"score_gpt":0.1878941474085649,"score_spread":0.17654206988332527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070939036","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955096,0.0018351176,0.000015039645,0.0009781375,0.0001273541,0.00008402718,0.00007579889,0.0000020497855,0.0013728457],"genre_scores_gemma":[0.9990961,0.00001237371,0.0006105819,0.000097792465,0.000043571974,1.3255075e-7,0.0000036572485,0.0000015870424,0.00013420988],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99840575,0.000117985895,0.00042708858,0.00019672014,0.00048020648,0.00037225927],"domain_scores_gemma":[0.9985804,0.000112732334,0.00037183496,0.00013283762,0.00022571711,0.0005764593],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009142336,0.00013877332,0.0003345328,0.00018725134,0.0002008041,0.00005066231,0.00061765226,0.000058349477,0.00043622637],"category_scores_gemma":[0.0003762355,0.000074497955,0.00014277599,0.0005274341,0.001564901,0.00017825665,0.0000248914,0.00020570612,0.0000037539726],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010279864,0.000006003764,0.9904975,0.0000126564455,0.000024315494,0.00002423148,0.00016840636,0.003491004,0.00052885315,0.000025353924,0.000015391866,0.0051959516],"study_design_scores_gemma":[0.00016340776,0.00039215942,0.993479,0.00003298441,0.000052947693,0.00015375686,0.0005487324,0.001737642,0.0007557012,0.0022090643,0.00035019685,0.00012440147],"about_ca_topic_score_codex":0.12751086,"about_ca_topic_score_gemma":0.91595346,"teacher_disagreement_score":0.7884426,"about_ca_system_score_codex":0.0000025069683,"about_ca_system_score_gemma":0.0011389874,"threshold_uncertainty_score":0.8782991},"labels":[],"label_agreement":null},{"id":"W2071000758","doi":"10.1139/e01-065","title":"New information on Cretaceous troodontids (Dinosauria, Theropoda) from the People's Republic of China","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":118,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature; Royal Tyrrell Museum","funders":"Natural Sciences and Engineering Research Council of Canada; North Carolina State University; Strong; American Museum of Natural History; Yale University","keywords":"Theropoda; Autapomorphy; Geology; Paleontology; Cretaceous; China; Geography; Phylogenetic tree; Biology; Archaeology","score_opus":0.013269162558670729,"score_gpt":0.19839635850956286,"score_spread":0.18512719595089214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2071000758","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97828144,0.0020163455,0.00014033067,0.005144566,0.0008594933,0.000052886444,0.00004218169,0.0000031671796,0.013459563],"genre_scores_gemma":[0.9987109,0.00009956371,0.0004077117,0.00048086283,0.00019997936,5.8763423e-8,0.000010213163,5.874139e-7,0.00009016257],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989722,0.00012516328,0.00031120033,0.000088854606,0.00021809943,0.00028448313],"domain_scores_gemma":[0.9990155,0.00021733578,0.00028022318,0.0001151156,0.00006496,0.00030682815],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00067171664,0.000083613384,0.00016357341,0.00019180756,0.0003796064,0.000060383758,0.0005463862,0.00007172888,0.0030866705],"category_scores_gemma":[0.00025631126,0.000049140384,0.00007051055,0.00041724037,0.0003731404,0.0006595952,0.0000027006818,0.00018212706,0.000055521916],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029183744,0.000001602498,0.98014915,5.430784e-7,0.000012261225,0.000008829316,0.00060740864,0.0011448957,0.0000020541438,0.00021170198,0.0013139141,0.016518444],"study_design_scores_gemma":[0.00015303846,0.0004586088,0.9731067,0.000014763415,0.0000084222,0.0001575801,0.00036461584,0.00042363076,0.0000071659183,0.0013508997,0.023895716,0.0000588933],"about_ca_topic_score_codex":0.061205275,"about_ca_topic_score_gemma":0.7562068,"teacher_disagreement_score":0.69500154,"about_ca_system_score_codex":0.0000016629017,"about_ca_system_score_gemma":0.001245175,"threshold_uncertainty_score":0.99782467},"labels":[],"label_agreement":null},{"id":"W2071073809","doi":"10.1139/e07-048","title":"Detrital zircon geochronology and provenance of Late Proterozoic and mid-Paleozoic successions outboard of the miogeocline, southeastern Canadian Cordillera","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta","keywords":"Geology; Paleozoic; Zircon; Proterozoic; Provenance; Craton; Basement; Geochronology; Paleontology; Geochemistry; Continental arc; Terrane; Continental crust; Island arc; Gneiss; Crust; Subduction; Metamorphic rock; Tectonics; Archaeology","score_opus":0.012834238946264804,"score_gpt":0.20094439176159598,"score_spread":0.18811015281533117,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2071073809","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956072,0.0013967134,0.0000072188855,0.0014462662,0.0001601743,0.00010290966,0.0000713208,0.0000010411287,0.0012071523],"genre_scores_gemma":[0.99929404,0.000024955712,0.00043431314,0.0001550433,0.000035158715,1.1948147e-7,0.0000015937893,0.0000010125899,0.000053779186],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987714,0.000052367082,0.0003993689,0.00016521622,0.00019968775,0.00041193218],"domain_scores_gemma":[0.99868554,0.00011545149,0.0002975996,0.000089172856,0.00015965427,0.0006525625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006391729,0.00010353203,0.00026737843,0.00028703318,0.00026104736,0.00003411023,0.00034226986,0.00007166234,0.0005307144],"category_scores_gemma":[0.00027111248,0.000058852318,0.00007156622,0.00049604924,0.001345124,0.00014454113,0.000011589839,0.00016978041,0.0000022778029],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000072794373,0.0000040861532,0.9966022,0.000011188196,0.00001144004,0.00000985851,0.0001179945,0.00007048752,0.00037313788,0.000017709737,0.0000057284806,0.0027689193],"study_design_scores_gemma":[0.00018158426,0.00025796317,0.995794,0.000061381535,0.000021929316,0.00002895938,0.0002028692,0.00016898215,0.0016882158,0.0010949539,0.00041933823,0.00007980378],"about_ca_topic_score_codex":0.26331505,"about_ca_topic_score_gemma":0.9703408,"teacher_disagreement_score":0.7070257,"about_ca_system_score_codex":0.0000013184256,"about_ca_system_score_gemma":0.0006418331,"threshold_uncertainty_score":0.7415906},"labels":[],"label_agreement":null},{"id":"W2071297460","doi":"10.1139/e05-015","title":"Lithological analysis of the Lower Devonian vertebrate-bearing beds at the MOTH locality, N.W.T., Canada: insights to taphonomy and depositional setting","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Sedimentary depositional environment; Paleontology; Trace fossil; Taphonomy; Devonian; Sedimentary rock; Sedimentary structures; Structural basin","score_opus":0.012413094024420993,"score_gpt":0.1990631086316683,"score_spread":0.18665001460724728,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2071297460","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99050474,0.001519122,0.000021837452,0.0054921852,0.00025456076,0.000045409022,0.0000413904,9.884868e-7,0.002119791],"genre_scores_gemma":[0.99808234,0.000007969586,0.00028390103,0.0015001808,0.00006560019,1.6159426e-7,0.0000025005088,5.5142596e-7,0.00005681977],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989442,0.00015515352,0.00026370285,0.00014618346,0.00020409482,0.00028662235],"domain_scores_gemma":[0.99918383,0.00019115032,0.00014213339,0.000089236695,0.00006998597,0.00032367633],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058040395,0.00007981859,0.0001718254,0.00017382941,0.0008454594,0.000032425392,0.00039406866,0.00005137257,0.00058361277],"category_scores_gemma":[0.00009374536,0.000041654297,0.000065285625,0.00070087274,0.00088774983,0.00013850529,0.000016613796,0.00014786996,0.0000037708019],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000073865194,0.0000020988914,0.98141664,7.2452406e-7,0.000047985053,0.000015263922,0.00014038805,0.017220626,0.000011113832,0.00011497356,0.00015704735,0.0008657316],"study_design_scores_gemma":[0.000048533046,0.00008846134,0.9906046,0.0000086892305,0.00004514207,0.00014037639,0.00015809556,0.004324381,0.000040046893,0.00007342876,0.004408933,0.000059313854],"about_ca_topic_score_codex":0.35133427,"about_ca_topic_score_gemma":0.9989466,"teacher_disagreement_score":0.64761233,"about_ca_system_score_codex":0.000013222542,"about_ca_system_score_gemma":0.0015774723,"threshold_uncertainty_score":0.6529853},"labels":[],"label_agreement":null},{"id":"W2071358817","doi":"10.1139/e01-048","title":"The first 20 years (1978-1979 to 1998–1999) of ice-wedge growth at the Illisarvik experimental drained lake site, western Arctic coast, Canada","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":136,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University; University of British Columbia","funders":"Natural Resources Canada; U.S. Department of Energy","keywords":"Ice wedge; Permafrost; Geology; Arctic; Geomorphology; Pressure ridge; Arctic ice pack; Antarctic sea ice; Oceanography","score_opus":0.03245751938815048,"score_gpt":0.21318195370728352,"score_spread":0.18072443431913304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2071358817","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9858876,0.0036179763,3.4026368e-7,0.0063367584,0.0010127042,0.00012825384,0.0011326965,0.0000020230755,0.0018816723],"genre_scores_gemma":[0.9968194,0.00009538918,0.00001372366,0.0019119768,0.00022846155,5.9974496e-7,0.000019950328,0.0000033034626,0.00090722094],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998344,0.00006125458,0.00034738332,0.00017056082,0.0005277493,0.00054907706],"domain_scores_gemma":[0.99851876,0.0003856102,0.0002017445,0.00016459524,0.0000802301,0.0006490659],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005435961,0.00014018436,0.00018895435,0.00012496734,0.0010366843,0.00020767987,0.0007369178,0.000034454413,0.0036826048],"category_scores_gemma":[0.00009194754,0.000083292616,0.00007817242,0.0005131014,0.0006101715,0.00023299496,0.000019776417,0.00014783996,0.00010462427],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015096181,0.0000054466886,0.97134405,0.000007154475,0.000016419735,0.000114321454,0.0037331122,0.00054062565,0.00006955576,0.000007441299,0.023627743,0.00051904196],"study_design_scores_gemma":[0.00023446394,0.00031044774,0.5526884,0.00005743951,0.000013653154,0.00017933206,0.002107506,0.0003533673,0.0001975892,0.000011399861,0.44366774,0.00017865309],"about_ca_topic_score_codex":0.81059575,"about_ca_topic_score_gemma":0.9999088,"teacher_disagreement_score":0.42004,"about_ca_system_score_codex":0.000013240622,"about_ca_system_score_gemma":0.0006161346,"threshold_uncertainty_score":0.99722815},"labels":[],"label_agreement":null},{"id":"W2071407440","doi":"10.1139/e05-019","title":"Stratigraphy, sedimentology, and environmental significance of late mid-Holocene dunes, Lauder Sand Hills, glacial Lake Hind Basin, southwestern Manitoba","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Holocene; Geology; Aeolian processes; Sedimentology; Geomorphology; Paleontology","score_opus":0.015914630391606257,"score_gpt":0.21156013837798254,"score_spread":0.19564550798637628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2071407440","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941486,0.0031976711,0.0000040693326,0.0010117927,0.00026631763,0.00008849212,0.00016737326,0.0000024284318,0.00111326],"genre_scores_gemma":[0.9990336,0.00014298117,0.0004266846,0.00022521272,0.000100832905,2.1081617e-7,0.00001335045,0.000001769393,0.000055372246],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998527,0.00015683226,0.00035148338,0.0002136729,0.000257125,0.00049390877],"domain_scores_gemma":[0.99902695,0.00014032355,0.00021210735,0.00008991796,0.000034306224,0.00049641286],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008037214,0.00013305427,0.00026509468,0.00032280904,0.0003561615,0.000058054404,0.0003414671,0.00011615265,0.0016972863],"category_scores_gemma":[0.00003183435,0.0001066537,0.000059928883,0.00019912542,0.0022032904,0.00034408382,0.0000067267047,0.00025296348,0.000024660314],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002223688,0.000008377774,0.9978722,0.000006563886,0.000021134305,0.000083248335,0.00027601246,0.00036703455,0.00003360648,0.00001352711,0.000037415815,0.0012586872],"study_design_scores_gemma":[0.00034694254,0.0003375825,0.9956548,0.00001778175,0.000016681792,0.00036229988,0.0005035327,0.00013322098,0.00048624116,0.00022740627,0.0018011081,0.00011238728],"about_ca_topic_score_codex":0.004014844,"about_ca_topic_score_gemma":0.8113692,"teacher_disagreement_score":0.80735433,"about_ca_system_score_codex":4.774693e-7,"about_ca_system_score_gemma":0.0005042092,"threshold_uncertainty_score":0.9992153},"labels":[],"label_agreement":null},{"id":"W2071541971","doi":"10.1139/e02-039","title":"The hind limb of<i>Captorhinus aguti</i>and the step cycle of basal amniotes","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Amphibian and Reptile Biology","field":"Environmental Science","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Canadian Museum of Nature","funders":"","keywords":"Anatomy; Postcrania; Femur; Geology; Tibia; Biology; Hindlimb; Cursorial; Paleontology; Tarsus (eyelids); Permian; Medicine; Structural basin","score_opus":0.007906432035149317,"score_gpt":0.19633497570790376,"score_spread":0.18842854367275444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2071541971","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9856214,0.001623074,0.000017891623,0.0009978147,0.0003266134,0.00006310515,0.0000031167933,6.0082976e-7,0.011346402],"genre_scores_gemma":[0.99911493,0.00010951874,0.00033502298,0.00015187605,0.000026176345,2.4482046e-7,2.9600253e-8,0.0000019878335,0.00026020885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990651,0.00014886187,0.0002594688,0.000092253875,0.00020177537,0.0002325617],"domain_scores_gemma":[0.999151,0.00025976895,0.00025133495,0.0001072578,0.000019009647,0.0002116364],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0015398504,0.00006351781,0.00014147328,0.00004208784,0.0003293215,0.000033816956,0.00039410568,0.000034492343,0.0002578179],"category_scores_gemma":[0.00029568071,0.000029374682,0.00006666176,0.00020217513,0.005020543,0.000101998194,0.000019178908,0.00010276251,0.0000064144983],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007499481,0.000028725412,0.95072466,0.000009130378,0.000060059738,0.000032744378,0.0034180377,0.0013791783,0.004913877,0.020865172,0.0027006357,0.015792768],"study_design_scores_gemma":[0.0014313804,0.0011058191,0.84457636,0.00007094577,0.000045578425,0.00040310816,0.0042704362,0.0006184844,0.009383844,0.007931984,0.12987132,0.00029072136],"about_ca_topic_score_codex":0.0032689762,"about_ca_topic_score_gemma":0.046687234,"teacher_disagreement_score":0.1271707,"about_ca_system_score_codex":0.0000057937336,"about_ca_system_score_gemma":0.00027846624,"threshold_uncertainty_score":0.9976872},"labels":[],"label_agreement":null},{"id":"W2072207454","doi":"10.1139/e02-067","title":"<i>Lariosaurus xingyiensis</i>(Reptilia: Sauropterygia) from the Triassic of China","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Chinese Academy of Sciences; National Science Foundation","keywords":"Paleontology; Geology; Genus; China; Cladistics; Sister group; Early Triassic; Taxon; Mesozoic; Geography; Archaeology; Permian; Zoology; Phylogenetic tree; Biology; Clade","score_opus":0.020911628983607766,"score_gpt":0.2022425284452477,"score_spread":0.18133089946163994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072207454","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97548074,0.0064826417,0.000041240834,0.0011776761,0.0013684883,0.000048640024,0.000060829232,0.0000022093782,0.015337528],"genre_scores_gemma":[0.9984442,0.00006370832,0.000933492,0.0003817615,0.000105747524,7.164875e-8,0.0000028552017,9.0264456e-7,0.00006726861],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986641,0.00029487972,0.00034628937,0.0001490158,0.00018805431,0.00035768942],"domain_scores_gemma":[0.9988562,0.00036728414,0.00027921228,0.00012674317,0.00007105509,0.00029949922],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012651547,0.000095978394,0.0002173768,0.0001363896,0.000469576,0.000033739518,0.00049688405,0.00007809324,0.002335809],"category_scores_gemma":[0.0005194047,0.00005762809,0.000099111014,0.00037880745,0.0013013263,0.00023575703,0.0000023744676,0.00022186474,0.000034706223],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010495257,0.0000028222885,0.9962902,8.393754e-7,0.00001745871,0.0000362674,0.00029840178,0.00059726764,0.000028133176,0.00037723835,0.00046213466,0.0018787114],"study_design_scores_gemma":[0.00017136667,0.0002271452,0.9808977,0.000017286255,0.00001717695,0.00020087749,0.0003616633,0.00012096938,0.00005405203,0.0022122224,0.015647702,0.00007181029],"about_ca_topic_score_codex":0.022241432,"about_ca_topic_score_gemma":0.5104611,"teacher_disagreement_score":0.48821965,"about_ca_system_score_codex":0.000001222888,"about_ca_system_score_gemma":0.0014216137,"threshold_uncertainty_score":0.99857616},"labels":[],"label_agreement":null},{"id":"W2072411362","doi":"10.1139/e10-040","title":"Chronology of transpression, magmatism, and sedimentation in the Thompson Nickel Belt (Manitoba, Canada) and timing of Trans-Hudson Orogen – Superior Province collisionThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université de Montréal; Université du Québec à Montréal","funders":"","keywords":"Geology; Craton; Archean; Zircon; Geochemistry; Terrane; Gneiss; Continental collision; Shear zone; Orogeny; Mafic; Transpression; Geochronology; Metamorphic rock; Paleontology; Tectonics; Subduction","score_opus":0.02037125181065283,"score_gpt":0.1835920328898054,"score_spread":0.16322078107915258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072411362","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99656904,0.00067180087,6.465755e-7,0.0017637929,0.000033631306,0.00012539527,0.000064636275,2.651857e-7,0.0007707913],"genre_scores_gemma":[0.99947774,0.000112379916,0.00032029895,0.0000682518,0.000014100961,4.466286e-7,0.0000013075436,7.890973e-7,0.000004661182],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99867606,0.0001646367,0.0005907365,0.00012270593,0.00026772518,0.00017812093],"domain_scores_gemma":[0.9991825,0.00023309873,0.00034923022,0.00007959089,0.00008216578,0.00007339642],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00087409036,0.000078746605,0.0003594028,0.00019073635,0.000047875885,0.0000065223758,0.0002981834,0.00005525847,0.0035777965],"category_scores_gemma":[0.00013568162,0.000044999713,0.000038898237,0.0004877025,0.0010234761,0.00019399972,0.000005601265,0.0001278434,7.033636e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013878185,0.000047532827,0.9739146,0.00006331411,0.000019926176,0.000008662949,0.010454152,0.00027713345,0.00883649,0.000106544976,0.000028344086,0.006104501],"study_design_scores_gemma":[0.00031533226,0.0006469205,0.9087898,0.00015107056,0.000021292297,0.0000075597286,0.007809653,0.00028022198,0.08130728,0.0005786169,0.00004159424,0.000050671166],"about_ca_topic_score_codex":0.64610046,"about_ca_topic_score_gemma":0.98916835,"teacher_disagreement_score":0.3430679,"about_ca_system_score_codex":0.0000033211609,"about_ca_system_score_gemma":0.0005995919,"threshold_uncertainty_score":0.99733305},"labels":[],"label_agreement":null},{"id":"W2072557782","doi":"10.1139/e06-103","title":"<i>Bearriverops</i>, a new Lower Ordovician trilobite genus from the Great Basin, western USA, and classification of the family Dimeropygidae","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Trilobite; Cladistics; Synonym (taxonomy); Genus; Paleontology; Geology; Taxon; Sister group; Ordovician; Type species; Clade; Zoology; Biology; Phylogenetics","score_opus":0.029358923957024254,"score_gpt":0.2227203917898833,"score_spread":0.19336146783285904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072557782","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98242223,0.007737197,0.000059662412,0.0013382166,0.0007073007,0.00007781048,0.00004558295,0.0000013953311,0.0076106275],"genre_scores_gemma":[0.998946,0.000058265454,0.00029760416,0.00048167977,0.00014437428,3.9991153e-8,4.826003e-7,6.524359e-7,0.0000709051],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988095,0.00011288883,0.00032783882,0.00015012875,0.00028769017,0.00031192295],"domain_scores_gemma":[0.9987675,0.000296788,0.0003016998,0.00014808806,0.00007036885,0.0004155543],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00095698645,0.00010356519,0.0001693006,0.00011999682,0.0005645288,0.0001033017,0.00058070786,0.00006964012,0.00016633164],"category_scores_gemma":[0.00009639119,0.00005538338,0.00008973188,0.0004522998,0.0012774145,0.00030585015,0.0000018281214,0.00021007491,0.0000065321383],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015531628,0.0000015564123,0.961193,7.81284e-7,0.000012885599,0.000014240115,0.00039986713,0.0000126401155,0.00013808583,0.00003242123,0.0001616846,0.03801727],"study_design_scores_gemma":[0.000158962,0.00016212407,0.99309903,0.000037627717,0.000023235909,0.000044406675,0.00035440185,0.00003591108,0.00005431365,0.00029347243,0.0056660282,0.000070462855],"about_ca_topic_score_codex":0.07040325,"about_ca_topic_score_gemma":0.8810229,"teacher_disagreement_score":0.8106196,"about_ca_system_score_codex":0.0000011507669,"about_ca_system_score_gemma":0.0009766185,"threshold_uncertainty_score":0.935787},"labels":[],"label_agreement":null},{"id":"W2072637895","doi":"10.1139/e01-087","title":"Step-pool and cascade morphology, Mosquito Creek, British Columbia: a test of four analytical techniques","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"Simon Fraser University","keywords":"Bedform; Revetment; Geology; Cascade; Channel (broadcasting); Wavelength; Fluvial; Geometry; Geomorphology; Hydrology (agriculture); Geotechnical engineering; Physics; Optics; Mathematics","score_opus":0.01756708657639885,"score_gpt":0.21346761333816497,"score_spread":0.19590052676176611,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072637895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99473614,0.00047090522,0.000040252933,0.00056866725,0.000060131733,0.00007015835,0.000018087314,0.000004985898,0.0040306784],"genre_scores_gemma":[0.99751717,0.00011575066,0.0013129245,0.00033170785,0.000033803582,0.0000010676983,2.2571919e-7,0.0000037965901,0.0006835436],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988772,0.00003141736,0.000318258,0.00019290326,0.00024035042,0.00033987215],"domain_scores_gemma":[0.9992091,0.0000837232,0.00014414957,0.00007585907,0.000027758822,0.00045939148],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00058542116,0.00006853004,0.00021041924,0.00007205395,0.0003003012,0.00013005912,0.00034380483,0.000093317205,0.006472094],"category_scores_gemma":[0.00016407119,0.00008406684,0.000046595975,0.00036934225,0.002262175,0.00036244502,0.000016690241,0.00018580104,0.000009477765],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.987874e-7,0.000022399414,0.98850626,0.0000057461507,0.000007504438,0.00041998771,0.00008646104,0.0000361144,0.0003475303,0.000003929587,0.0044457037,0.0061173607],"study_design_scores_gemma":[0.00029246887,0.0011258585,0.97216433,0.00008474924,0.00005309478,0.002726486,0.0001582839,0.0013976846,0.0005041803,0.00029618133,0.020980628,0.00021606492],"about_ca_topic_score_codex":0.08733456,"about_ca_topic_score_gemma":0.822808,"teacher_disagreement_score":0.7354735,"about_ca_system_score_codex":0.000008336703,"about_ca_system_score_gemma":0.00011612665,"threshold_uncertainty_score":0.99443614},"labels":[],"label_agreement":null},{"id":"W2072654212","doi":"10.1139/e01-038","title":"Stratigraphy and structure of a Late Wisconsinan salt collapse in the Saskatoon Low, south of Saskatoon, Saskatchewan, Canada: an update","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Glacial period; Pleistocene; Devonian; Paleontology; Geomorphology; Geochemistry; Evaporite; Sedimentary rock","score_opus":0.01106542772257537,"score_gpt":0.18934577332685423,"score_spread":0.17828034560427886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072654212","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973652,0.0010985591,0.0000039060033,0.00052673905,0.00011505471,0.000077642,0.00013296443,9.381936e-7,0.0006790022],"genre_scores_gemma":[0.99921566,0.000021410797,0.00042255785,0.00029692805,0.000020189567,6.1630594e-8,0.000005122145,9.361896e-7,0.00001714076],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99874425,0.00010739372,0.00042503476,0.000118884986,0.00031115534,0.00029326466],"domain_scores_gemma":[0.99907136,0.00008359746,0.00031573308,0.00010004743,0.00013239958,0.00029688224],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005987365,0.000105287014,0.00022430407,0.0002559291,0.00021272972,0.00009127188,0.00040539357,0.000047576847,0.0004000302],"category_scores_gemma":[0.000038633465,0.000062695115,0.00003156999,0.0009102037,0.00070772605,0.000495641,0.0000029134076,0.00015397296,3.574533e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014032622,0.000004803421,0.9912322,0.000019181816,0.000006670248,0.000041598516,0.0028222955,0.003647901,0.000025657731,0.00008900487,0.00009320468,0.0020034516],"study_design_scores_gemma":[0.00017753274,0.0005225705,0.98140293,0.000053969274,0.000010506641,0.00014916486,0.013786957,0.00041596623,0.0001118349,0.002176813,0.0010912087,0.00010053851],"about_ca_topic_score_codex":0.5624377,"about_ca_topic_score_gemma":0.9996491,"teacher_disagreement_score":0.4372114,"about_ca_system_score_codex":0.0000012999818,"about_ca_system_score_gemma":0.0037141237,"threshold_uncertainty_score":0.6588696},"labels":[],"label_agreement":null},{"id":"W2072887912","doi":"10.1139/e05-099","title":"Mapping subtle structures with light detection and ranging (LIDAR): flow units and phreatomagmatic rootless cones in the North Mountain Basalt, Nova Scotia","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University; St. Francis Xavier University; Nova Scotia Community College","funders":"Public Works and Government Services Canada; Natural Sciences and Engineering Research Council of Canada; Government of Canada","keywords":"Geology; Lidar; Digital elevation model; Phreatomagmatic eruption; Geomorphology; Ranging; Volcano; Remote sensing; Lava; Paleontology; Geodesy","score_opus":0.006941962268365713,"score_gpt":0.17953005094506802,"score_spread":0.1725880886767023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072887912","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982124,0.00041383924,0.000106105676,0.0003520852,0.00007374161,0.00007384896,0.0000022562886,0.0000017448368,0.0007639786],"genre_scores_gemma":[0.9995317,0.000009265149,0.000331166,0.000072050716,0.000034460176,2.3511579e-7,3.0469369e-7,0.0000032520445,0.000017561502],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992482,0.000048235695,0.00015944606,0.0001123465,0.00020052088,0.00023126364],"domain_scores_gemma":[0.9996798,0.000037117763,0.00009423394,0.00004936676,0.000015635242,0.00012385298],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004589219,0.00008278064,0.00010593444,0.0001592769,0.0003024312,0.0001810023,0.00014145274,0.000029483608,0.000060764796],"category_scores_gemma":[0.000016186881,0.000044365635,0.0000112387825,0.0006560852,0.00037629815,0.0002735565,0.0000093208055,0.00013512262,0.0000016451173],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005054542,0.0000020914997,0.9897816,0.0000060950483,0.000003974353,0.000071501614,0.0012055374,0.0066808844,0.00021123588,0.00003392942,0.000017255139,0.001980827],"study_design_scores_gemma":[0.00026961145,0.00008477542,0.99413794,0.000059009057,0.00000862245,0.0005196831,0.0012631617,0.0025180862,0.0001896232,0.0002720607,0.0005885819,0.00008885401],"about_ca_topic_score_codex":0.023803795,"about_ca_topic_score_gemma":0.7760434,"teacher_disagreement_score":0.75223964,"about_ca_system_score_codex":0.000012336781,"about_ca_system_score_gemma":0.000114528004,"threshold_uncertainty_score":0.9826968},"labels":[],"label_agreement":null},{"id":"W2073290345","doi":"10.1139/e10-046","title":"Catastrophic tidal expansion in the Bay of Fundy, CanadaEarth Sciences Sector (ESS) Contribution 20090423.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada; Canadian Hydrographic Service","funders":"","keywords":"Bay; Geology; Tidal range; Estuary; Oceanography; Holocene; Structural basin; Inlet; Barrier island; Sea level; Physical geography; Geomorphology; Shore; Geography","score_opus":0.02290111531526499,"score_gpt":0.23923331831377315,"score_spread":0.21633220299850817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073290345","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99438274,0.0006737336,0.0000055115465,0.0019486924,0.000778428,0.00010228346,0.00004335225,0.0000015070941,0.0020637377],"genre_scores_gemma":[0.9994226,0.000018531362,0.00024011568,0.00019407032,0.00009846206,3.1078415e-7,0.000005603586,9.2232995e-7,0.000019386513],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99803203,0.0002881646,0.0003699915,0.00018159636,0.00049400335,0.00063422846],"domain_scores_gemma":[0.99870145,0.00043711296,0.00021321687,0.00012743045,0.00017407494,0.00034668355],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.004138133,0.0001049,0.00022048478,0.000552767,0.0007068691,0.000109194916,0.00092663325,0.00010420566,0.0017989454],"category_scores_gemma":[0.00049767416,0.00006493417,0.00005686983,0.00097647525,0.0027178493,0.0004472033,0.0000056454905,0.0005921355,0.000025984724],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009365366,0.000004457782,0.99815893,0.0000034525829,0.0000032520732,0.0000845542,0.0002122893,0.00071959954,0.00006269381,0.00049581117,0.00006485149,0.00018074528],"study_design_scores_gemma":[0.00018838145,0.0004077633,0.9956554,0.000021955624,0.0000051615975,0.0005459305,0.00060228596,0.00057321176,0.00017872239,0.00058436464,0.0011597252,0.000077081975],"about_ca_topic_score_codex":0.040026885,"about_ca_topic_score_gemma":0.9754306,"teacher_disagreement_score":0.9354037,"about_ca_system_score_codex":6.2274876e-7,"about_ca_system_score_gemma":0.0036886544,"threshold_uncertainty_score":0.9999962},"labels":[],"label_agreement":null},{"id":"W2073545246","doi":"10.1139/e10-097","title":"Seismic reflection constraints on upper crustal structures in the volcanic-covered central Nechako basin, British Columbia<sup>1</sup>This article is one of a series of papers published in this Special Issue on the theme of <i>New insights in Cordilleran Intermontane geoscience: reducing exploration risk in the mountain pine beetle-affected area, British Columbia</i>.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Simon Fraser University","funders":"","keywords":"Geology; Cretaceous; Seismology; Volcanic rock; Structural basin; Volcano; Paleontology; Stratigraphy; Sedimentary basin; Tectonics","score_opus":0.01907524106760718,"score_gpt":0.19466251246504948,"score_spread":0.1755872713974423,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073545246","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961809,0.00011870785,0.000001745448,0.0006115696,0.00018369166,0.0003161279,0.00015219687,0.0000016562973,0.0024334334],"genre_scores_gemma":[0.9990623,0.00015551862,0.000059848317,0.0004974996,0.00013225802,0.000001128422,0.0000077032055,0.000003372761,0.0000803433],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997255,0.0005775779,0.0007894367,0.0002903486,0.0006492878,0.00043833986],"domain_scores_gemma":[0.99882793,0.00022821152,0.00050744164,0.00018371684,0.0001089715,0.00014371081],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019710616,0.000121274534,0.00041045982,0.00032054348,0.00026775326,0.0005788272,0.00067737466,0.00008926331,0.010531895],"category_scores_gemma":[0.0006486783,0.00010680667,0.000107735665,0.001956173,0.0010256651,0.00083241216,0.000008917297,0.0004658433,7.535234e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020339325,0.00012970896,0.9065423,0.000022200122,0.000040310304,0.00018485442,0.0441457,0.0120043885,0.00020696722,0.000026254274,0.0031609263,0.033333007],"study_design_scores_gemma":[0.0006591455,0.0012969178,0.96629316,0.00041615625,0.00001890596,0.00010260946,0.023496443,0.0056685936,0.00017010649,0.0015396638,0.00020233926,0.00013598106],"about_ca_topic_score_codex":0.9009104,"about_ca_topic_score_gemma":0.9896948,"teacher_disagreement_score":0.08878442,"about_ca_system_score_codex":0.000024614572,"about_ca_system_score_gemma":0.0007893601,"threshold_uncertainty_score":0.9903726},"labels":[],"label_agreement":null},{"id":"W2073568082","doi":"10.1139/e06-026","title":"Evidence for catastrophic volcanic debris flows in Pemberton Valley, British Columbia","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geoscience BC; Simon Fraser University; Geological Survey of Canada","funders":"","keywords":"Volcano; Geology; Debris; Debris flow; Volcanic hazards; Pyroclastic rock; Lahar; Landslide; Volcanic ash; Geomorphology; Volcanic plateau; Volcanic cone; Geochemistry; Volcanic rock","score_opus":0.0403878311175957,"score_gpt":0.24963941325752353,"score_spread":0.20925158213992784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073568082","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911079,0.0063646934,0.000019415149,0.0006905744,0.00045625964,0.00014530055,0.000035706136,0.0000027521446,0.0011774037],"genre_scores_gemma":[0.9981654,0.00009083264,0.0010076808,0.000109536166,0.00012489884,9.5157895e-7,0.000007297459,0.0000017916092,0.0004915687],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99833566,0.00013439411,0.00037127227,0.00022276523,0.00023374146,0.00070219644],"domain_scores_gemma":[0.99880207,0.00045453664,0.00013451187,0.000088993096,0.00014044726,0.0003794197],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016520186,0.000076665136,0.00022626341,0.0002455124,0.0005327427,0.0003428031,0.0005632371,0.000091519156,0.0024714363],"category_scores_gemma":[0.0004326473,0.00009084212,0.00007888555,0.000517724,0.00062828854,0.00045908827,0.000004451124,0.00024511994,0.00003764187],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008178816,0.000003405882,0.99578243,0.000008676382,0.000003391251,0.0002042597,0.000027010636,0.0022393048,0.0000031299016,0.000007381806,0.0010428615,0.00066998234],"study_design_scores_gemma":[0.00024706067,0.0003210594,0.99309283,0.00011771776,0.0000066765583,0.0008563332,0.00006998527,0.0021173381,0.000003589742,0.0013795963,0.0016855629,0.000102246544],"about_ca_topic_score_codex":0.58318293,"about_ca_topic_score_gemma":0.9996163,"teacher_disagreement_score":0.41643336,"about_ca_system_score_codex":0.0000013304505,"about_ca_system_score_gemma":0.0021200173,"threshold_uncertainty_score":0.99844044},"labels":[],"label_agreement":null},{"id":"W2073992409","doi":"10.1139/e07-037","title":"Distinct Taconic, Salinic, and Acadian deformation along the Iapetus suture zone, Newfoundland Appalachians","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Terrane; Mylonite; Overprinting; Ordovician; Paleontology; Devonian; Shear zone; Orogeny; Fibrous joint; Laurentia; Sinistral and dextral; Seismology; Tectonics","score_opus":0.012691811196037569,"score_gpt":0.20527756411804643,"score_spread":0.19258575292200886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073992409","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98849094,0.0019907851,0.000126856,0.0030101552,0.00024492302,0.00005079091,0.000017126536,0.0000036114182,0.0060648355],"genre_scores_gemma":[0.9986395,0.000043091164,0.00035344195,0.0006511676,0.00021143537,6.452497e-8,0.000006502578,9.306466e-7,0.000093850475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99871594,0.000053538526,0.00036255404,0.00014099019,0.00026677173,0.0004602178],"domain_scores_gemma":[0.99863327,0.0002762152,0.00019867318,0.00007703937,0.00007882706,0.00073595],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017522916,0.000108747634,0.00017140835,0.00017171598,0.00070178014,0.00021917782,0.00037931683,0.000065528526,0.0018871826],"category_scores_gemma":[0.00020515632,0.000056405923,0.00008565034,0.00050934055,0.0007354694,0.000335748,0.0000058649007,0.00027205024,0.00003619056],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000056577687,0.0000015012295,0.98955274,0.0000025125482,0.000009996013,0.000031073927,0.00019060321,0.00023260983,0.00000576291,0.00013994524,0.000049236172,0.009778347],"study_design_scores_gemma":[0.000100631725,0.0001266137,0.9871825,0.00001316143,0.000022771597,0.00022167101,0.00049935345,0.00075473863,0.000012482506,0.0017883516,0.009183744,0.00009398771],"about_ca_topic_score_codex":0.08707148,"about_ca_topic_score_gemma":0.96674997,"teacher_disagreement_score":0.8796785,"about_ca_system_score_codex":0.0000019746078,"about_ca_system_score_gemma":0.00033569284,"threshold_uncertainty_score":0.9990252},"labels":[],"label_agreement":null},{"id":"W2074109190","doi":"10.1139/e08-005","title":"Stable isotope record of the Eifelian–Givetian boundary Kačák–<i>otomari</i> Event (Middle Devonian) from Hungry Hollow, Ontario, Canada","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Conodont; Geology; Paleontology; Devonian; Chemostratigraphy; Biostratigraphy; Late Devonian extinction; Extinction event; Sedimentary rock; Facies; Isotopes of carbon; Structural basin; Total organic carbon","score_opus":0.021103097829026012,"score_gpt":0.18601103425791463,"score_spread":0.16490793642888862,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074109190","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9647309,0.0049485294,0.0000071671807,0.0006146073,0.001778222,0.000112481976,0.00018973419,0.000002591667,0.027615769],"genre_scores_gemma":[0.9982329,0.000046866196,0.0008078039,0.00036384046,0.00010459094,2.932405e-7,0.0000023247742,0.0000012646619,0.00044011325],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997883,0.00014941301,0.00055602734,0.00023719508,0.00058099616,0.0005933292],"domain_scores_gemma":[0.998321,0.0001595174,0.0004424655,0.00022470602,0.00013739376,0.00071489124],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004984947,0.00017706612,0.00033912028,0.00018767381,0.0013235381,0.00008053685,0.0010337107,0.00008961799,0.002194831],"category_scores_gemma":[0.000096321455,0.00012289608,0.00016980099,0.0005641711,0.001297517,0.00047188808,0.000003544115,0.0004015812,0.00000469681],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014944995,0.000004970791,0.99309707,0.0000025936436,0.000032259348,0.00022940434,0.0006532161,0.0002519274,0.000012317903,0.000010271005,0.0013157671,0.004375255],"study_design_scores_gemma":[0.0002018729,0.00020162656,0.9612114,0.00007560705,0.000016515241,0.00020303855,0.00040078015,0.00005676837,0.00014192422,0.0003351469,0.037001915,0.0001534316],"about_ca_topic_score_codex":0.9955586,"about_ca_topic_score_gemma":0.9999732,"teacher_disagreement_score":0.035686146,"about_ca_system_score_codex":0.000013508765,"about_ca_system_score_gemma":0.024052663,"threshold_uncertainty_score":0.9999766},"labels":[],"label_agreement":null},{"id":"W2074172465","doi":"10.1139/e10-005","title":"Faunal assemblages from the upper Horseshoe Canyon Formation, an early Maastrichtian cool-climate assemblage from Alberta, with special reference to the<i>Albertosaurus sarcophagus</i>bonebedThis article is one of a series of papers published in this Special Issue on the theme<i>Albertosaurus</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; University of Alberta","funders":"","keywords":"Canyon; Geology; Paleontology; Fauna; Taxon; Assemblage (archaeology); Faunal assemblage; Vertebrate; Ecology; Geomorphology; Biology","score_opus":0.013859436736015368,"score_gpt":0.20277361832691654,"score_spread":0.18891418159090118,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074172465","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9627704,0.00017228784,0.0000017757221,0.0119586475,0.0007964964,0.00023056683,0.00041382544,0.0000025692298,0.023653436],"genre_scores_gemma":[0.9966339,0.000040003302,0.00024593758,0.0014185555,0.0014528641,0.0000019113438,0.000024274756,0.000004149665,0.0001784282],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99745256,0.00039072198,0.0006511756,0.00031980796,0.0005653247,0.0006204024],"domain_scores_gemma":[0.9974318,0.0010894256,0.00050781405,0.00038759573,0.0001959929,0.00038736992],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012406365,0.00022858166,0.00038966787,0.00023794317,0.0007091641,0.00019647424,0.0013467929,0.00015507184,0.025695566],"category_scores_gemma":[0.00048743672,0.00011575601,0.00008333841,0.0008471208,0.0013133871,0.0011382332,0.00001947635,0.00062953786,0.00007524406],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044690925,0.00003309134,0.9852089,0.0000029780692,0.000047763035,0.000021057782,0.0067109726,0.00025217497,0.0012297676,0.0007372972,0.0032834148,0.0020256366],"study_design_scores_gemma":[0.00027604375,0.00086465565,0.97341573,0.000060680482,0.000032557135,0.000039026298,0.002132496,0.00012255457,0.0022246814,0.00045761635,0.020208115,0.00016582546],"about_ca_topic_score_codex":0.2944565,"about_ca_topic_score_gemma":0.9830515,"teacher_disagreement_score":0.68859494,"about_ca_system_score_codex":0.000006098875,"about_ca_system_score_gemma":0.0008019582,"threshold_uncertainty_score":0.97519505},"labels":[],"label_agreement":null},{"id":"W2074267546","doi":"10.1139/e09-022","title":"Geochemistry, geochronology, and geodynamic setting of Ni–Cu ± PGE mineral prospects hosted by mafic and ultramafic intrusions in the Portneuf–Mauricie Domain, Grenville Province, QuebecGéologie Québec Contribution 8439-2008-2009-5. Geological Survey of Canada Contribution 20080511.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval; Centre de Géomatique du Québec; Geological Survey of Canada","funders":"","keywords":"Geology; Pluton; Geochemistry; Mafic; Ultramafic rock; Zircon; Craton; Continental arc; Back-arc basin; Subduction; Geochronology; Laurentia; Terrane; Paleontology; Volcanic rock; Ordovician; Tectonics","score_opus":0.005871943170503157,"score_gpt":0.18232949054498418,"score_spread":0.17645754737448102,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074267546","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98827803,0.0046436316,0.000011291563,0.0062825372,0.000056388446,0.00017514531,0.00036933253,0.0000025610989,0.0001810516],"genre_scores_gemma":[0.9994469,0.000091348535,0.00008467957,0.00023801149,0.000020744546,4.970144e-7,0.0000978213,9.126709e-7,0.000019049354],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99782926,0.00028357562,0.0006493139,0.00028644913,0.0003373053,0.0006141107],"domain_scores_gemma":[0.99832076,0.00043197416,0.00050223246,0.00011054497,0.00028731374,0.00034718515],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019229664,0.00018269304,0.0004770156,0.00015402038,0.00033015333,0.000048435362,0.00038268487,0.0001359287,0.00033426782],"category_scores_gemma":[0.0013516552,0.00011275893,0.000051799714,0.0007155497,0.0011764276,0.00012594668,0.000012651668,0.00031486154,4.806713e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027186386,0.000019856057,0.9972024,0.0000065162817,0.00001119307,0.000051830448,0.0000592213,0.00042935135,0.0009437605,0.00004089655,0.0004514666,0.00075634645],"study_design_scores_gemma":[0.00036839634,0.00048403785,0.9953273,0.00002890766,0.000019851035,0.00016661524,0.0002562969,0.0017926099,0.00018318255,0.001094924,0.00013847103,0.00013938798],"about_ca_topic_score_codex":0.95949584,"about_ca_topic_score_gemma":0.99881357,"teacher_disagreement_score":0.03931776,"about_ca_system_score_codex":0.000016236052,"about_ca_system_score_gemma":0.0023783436,"threshold_uncertainty_score":0.45981756},"labels":[],"label_agreement":null},{"id":"W2074466617","doi":"10.1139/e01-031","title":"Paleomagnetism of the Upper Cretaceous Nanaimo Group, southwestern Canadian Cordillera","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; California Institute of Technology","keywords":"Geology; Paleomagnetism; Cretaceous; Paleontology; Structural basin; Conglomerate; Group (periodic table)","score_opus":0.020294202104928064,"score_gpt":0.21818187451066995,"score_spread":0.1978876724057419,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074466617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9593741,0.0029401544,0.0000020692817,0.0028079727,0.0008326728,0.00009209327,0.00003053767,0.0000020205384,0.03391833],"genre_scores_gemma":[0.9986796,0.000089025525,0.00014021351,0.0005140068,0.00007769773,1.8036746e-7,0.0000018139585,0.0000019609313,0.0004955112],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981665,0.00021400237,0.0003470776,0.00017244306,0.00034542833,0.00075455214],"domain_scores_gemma":[0.9983278,0.00016379231,0.00019276758,0.00018247316,0.0001492376,0.0009839089],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009259067,0.00012237878,0.00023901308,0.000484616,0.00080029445,0.00007778165,0.0009832925,0.00011906911,0.006125702],"category_scores_gemma":[0.00018025341,0.000078479505,0.00012011157,0.0007053276,0.0016532231,0.00023529006,0.000007037641,0.00035336587,0.00009857975],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005775697,0.0000021709873,0.99831736,0.0000034865902,0.000012980471,0.00021014488,0.0002634162,0.00028721296,0.0000030975032,0.000062992294,0.00011493346,0.0007164342],"study_design_scores_gemma":[0.00014862583,0.0002776491,0.987598,0.000036499263,0.000012303421,0.0012374751,0.0003924835,0.00021395968,0.000010848218,0.00032314076,0.009653367,0.0000956602],"about_ca_topic_score_codex":0.2641175,"about_ca_topic_score_gemma":0.9964169,"teacher_disagreement_score":0.7322994,"about_ca_system_score_codex":9.820683e-7,"about_ca_system_score_gemma":0.0028248543,"threshold_uncertainty_score":0.9947828},"labels":[],"label_agreement":null},{"id":"W2074695319","doi":"10.1139/e00-054","title":"A new ammonite and coccolith fauna from the lowermost Fernie Formation (Hettangian) in northwestern Alberta, Canada","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Intertek (Canada); University of Calgary","funders":"","keywords":"Ammonite; Geology; Paleontology; Outcrop; Biostratigraphy; Geochemistry; Siltstone; Coccolith; Carbonate; Structural basin; Cretaceous; Facies","score_opus":0.010348373153970188,"score_gpt":0.18471740314541524,"score_spread":0.17436902999144505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074695319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9811298,0.0044235857,0.0000049074183,0.0015213274,0.00019486566,0.000059027643,0.000051878542,9.688505e-7,0.012613586],"genre_scores_gemma":[0.9991804,0.00006262892,0.00016871908,0.00042517058,0.00006621064,8.239629e-8,0.0000025505196,4.2918495e-7,0.00009385317],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990321,0.000067038425,0.00025642014,0.00011463788,0.00020420225,0.00032561444],"domain_scores_gemma":[0.99910116,0.0002225094,0.0001050777,0.00007082148,0.000022975124,0.000477463],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00028232805,0.00009257236,0.00013873378,0.00009670462,0.0003537015,0.00014939762,0.00032278357,0.000040797502,0.0009923691],"category_scores_gemma":[0.000024968396,0.000060747254,0.00003023468,0.0002982538,0.00025925113,0.00054669735,4.754427e-7,0.00016598323,0.000006047606],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008136837,5.7369624e-7,0.86917603,6.948137e-7,0.0000046025816,0.000063963475,0.0007466363,0.00014490246,3.501212e-7,0.000008268554,0.00016642372,0.1296794],"study_design_scores_gemma":[0.00017982742,0.00007050146,0.9933896,0.000035457542,0.0000061542337,0.00011429833,0.00042676105,0.00047275503,0.000004184737,0.0002467678,0.0049726623,0.00008102842],"about_ca_topic_score_codex":0.99309504,"about_ca_topic_score_gemma":0.9999863,"teacher_disagreement_score":0.12959836,"about_ca_system_score_codex":0.000002462843,"about_ca_system_score_gemma":0.0024854017,"threshold_uncertainty_score":0.99992085},"labels":[],"label_agreement":null},{"id":"W2075009922","doi":"10.1139/e99-064","title":"A review of high-resolution seismic profiling across the Sudbury, Selbaie, Noranda, and Matagami mining camps","year":2000,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; Ministère des Ressources naturelles et des Forêts (Québec); Petrel Robertson Consulting (Canada); Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Vertical seismic profile; Borehole; Mineral exploration; High resolution; Synthetic seismogram; Seismic refraction; Geochemistry; Petrology; Geotechnical engineering; Remote sensing","score_opus":0.03540968059154257,"score_gpt":0.2758638061954338,"score_spread":0.24045412560389126,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075009922","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0013553948,0.9968016,0.000022614246,0.00032443716,0.00039258375,0.00026982627,0.00023352358,0.0000071265995,0.00059286284],"genre_scores_gemma":[0.00095840835,0.9961831,0.0015851383,0.0010202954,0.00012638076,7.435085e-7,0.000022113776,0.000005043597,0.00009875042],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99782985,0.00025893364,0.0008116439,0.0002521099,0.0003629386,0.0004845266],"domain_scores_gemma":[0.99827194,0.00024218713,0.00082763564,0.00018972505,0.00012198343,0.00034653905],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002832833,0.00024054282,0.00092671165,0.00031960485,0.0005923354,0.00017840012,0.00077336817,0.00010863336,0.00038247748],"category_scores_gemma":[0.00017447429,0.00013967793,0.00020586976,0.00077086844,0.0010163452,0.000350445,0.000010948948,0.000394966,0.000013326497],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000018756148,0.0000016823386,0.0007089583,0.0053999587,0.000022397251,0.000020014459,0.00013122821,0.000055617515,1.9139858e-8,0.000009778516,0.0043869973,0.98926145],"study_design_scores_gemma":[0.00005923608,0.00015678936,0.00018708479,0.04710062,0.00013134947,0.0007135477,0.00016324595,0.00037004883,0.0000023864027,0.00007149142,0.9508602,0.00018399156],"about_ca_topic_score_codex":0.034154013,"about_ca_topic_score_gemma":0.009097777,"teacher_disagreement_score":0.9890775,"about_ca_system_score_codex":0.0000050388244,"about_ca_system_score_gemma":0.002463921,"threshold_uncertainty_score":0.97227764},"labels":[],"label_agreement":null},{"id":"W2075063530","doi":"10.1139/e05-036","title":"Paleoproterozoic reworking of an Archean thrust fault in the Hearne domain, Western Churchill Province: UPb geochronological constraints","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Aboriginal Affairs Northern Dev Canada; Geological Survey of Canada","funders":"","keywords":"Geology; Metamorphism; Sinistral and dextral; Proterozoic; Archean; Shear zone; Transpression; Geochemistry; Seismology; Orogeny; Fault (geology); Geomorphology; Petrology; Tectonics","score_opus":0.025056885910010655,"score_gpt":0.2272185985257752,"score_spread":0.20216171261576454,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075063530","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913818,0.00067213736,0.000020372685,0.0038002566,0.000059003327,0.00010314014,0.000019395007,0.0000029197001,0.0039409506],"genre_scores_gemma":[0.99737316,0.0000223588,0.0017492629,0.00067171326,0.00016273373,3.0444943e-7,0.0000048624297,8.998649e-7,0.000014677831],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981193,0.00020086615,0.00047792724,0.00022254958,0.00040218292,0.0005771776],"domain_scores_gemma":[0.99896747,0.00016636604,0.00023605466,0.00013211956,0.000084469284,0.0004135192],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019207201,0.00012796663,0.00027932134,0.00022105633,0.000250233,0.00010517154,0.00083727774,0.00007791377,0.0028291848],"category_scores_gemma":[0.00019460326,0.00006869806,0.000086553424,0.00067209924,0.0018300243,0.0002995284,0.000008338241,0.000429413,0.000019429845],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013032957,0.000019782115,0.9337462,0.000005036038,0.000008611313,0.00010264033,0.0006249233,0.0032534979,0.00006788362,0.00010663685,0.0000093695335,0.062042344],"study_design_scores_gemma":[0.0002032416,0.0005773478,0.9900474,0.000048782666,0.000009244966,0.00024689996,0.0015497253,0.0007270289,0.000102192455,0.0050451607,0.0013188943,0.00012409447],"about_ca_topic_score_codex":0.011243833,"about_ca_topic_score_gemma":0.73884267,"teacher_disagreement_score":0.72759885,"about_ca_system_score_codex":0.0000026513853,"about_ca_system_score_gemma":0.00072085054,"threshold_uncertainty_score":0.99808234},"labels":[],"label_agreement":null},{"id":"W2075152868","doi":"10.1139/e05-049","title":"Multiple hydroclimatic controls over recent sedimentation in proglacial Mirror Lake, southern Selwyn Mountains, Northwest Territories","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Varve; Meltwater; Geology; Glacial period; Sediment; Sedimentation; Silt; Glacier; Snow; Sedimentology; Sedimentary rock; Glacial lake; Geomorphology; Physical geography; Geochemistry","score_opus":0.021017201902318126,"score_gpt":0.2507642199794636,"score_spread":0.22974701807714545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075152868","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99575245,0.00068103615,0.0000026098373,0.0021005266,0.00043303872,0.00016872391,0.00009741212,0.0000042706397,0.00075994234],"genre_scores_gemma":[0.99864155,0.000036434638,0.0007503845,0.00032316984,0.00014592275,0.0000010832072,0.00003220639,0.0000019476856,0.00006732509],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998334,0.00018042023,0.00041409067,0.00017428643,0.0003184717,0.00057871634],"domain_scores_gemma":[0.999004,0.00022013429,0.00018760955,0.0000744066,0.00009728004,0.00041655535],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011830091,0.00011926882,0.0002286657,0.00041779285,0.0003858102,0.0001131311,0.0003446496,0.00009126034,0.002185081],"category_scores_gemma":[0.00022563741,0.000094018134,0.00004938736,0.0004168924,0.0006174569,0.00052975403,0.0000038338794,0.00027711396,0.00012444358],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031190968,0.000009386136,0.99688387,0.0000055786577,0.00000877347,0.00006339893,0.0010996766,0.0010263228,0.000006237563,0.000013479136,0.0000123254285,0.00083976757],"study_design_scores_gemma":[0.000685248,0.00023702395,0.98673123,0.000028774413,0.000007521078,0.00011936567,0.0009043478,0.0027794004,0.00003585808,0.00014825915,0.0082104225,0.00011254768],"about_ca_topic_score_codex":0.030098079,"about_ca_topic_score_gemma":0.9959996,"teacher_disagreement_score":0.9659015,"about_ca_system_score_codex":0.0000022684255,"about_ca_system_score_gemma":0.0011569115,"threshold_uncertainty_score":0.9987271},"labels":[],"label_agreement":null},{"id":"W2075208671","doi":"10.1139/e01-098","title":"Geophysical correlations in the Ungava Bay area","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Université du Québec à Montréal","funders":"","keywords":"Geology; Bay; Batholith; Submarine pipeline; Tectonics; Shear zone; Magnetic anomaly; Paleontology; Terrane; Oceanography; Shoal; Seismology","score_opus":0.03860846828325177,"score_gpt":0.1929011636439308,"score_spread":0.15429269536067905,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075208671","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95666814,0.0010895265,0.0000083517725,0.00648314,0.000281617,0.000047947127,0.000009477124,0.0000019504462,0.035409864],"genre_scores_gemma":[0.99880743,0.0000269145,0.00008701907,0.0006203418,0.00012397475,1.4660395e-7,6.1061985e-7,4.004603e-7,0.00033315382],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990807,0.00007509557,0.00018303645,0.000097748634,0.00024685313,0.00031653847],"domain_scores_gemma":[0.9993076,0.00030278502,0.000071062306,0.000055368397,0.0000402815,0.00022291187],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003817645,0.00006974805,0.00012674178,0.00010153872,0.00044059756,0.00009455646,0.00040062473,0.000025264211,0.0028513202],"category_scores_gemma":[0.00016875376,0.00003525702,0.00006234202,0.0006370108,0.00056214345,0.00020387824,0.0000028286347,0.00020309581,0.00041318435],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.182639e-7,0.000008883845,0.99016064,6.052847e-7,0.000003382906,0.00006292362,0.0005362154,0.0023485192,3.4496964e-7,0.0005625177,0.00051753625,0.005797524],"study_design_scores_gemma":[0.000063611784,0.0002208519,0.98094887,0.000007748439,0.000004190757,0.000035759083,0.00042123435,0.0030843373,6.497098e-7,0.004101961,0.011054018,0.00005679167],"about_ca_topic_score_codex":0.010142235,"about_ca_topic_score_gemma":0.3817361,"teacher_disagreement_score":0.3715939,"about_ca_system_score_codex":6.431096e-7,"about_ca_system_score_gemma":0.00008362342,"threshold_uncertainty_score":0.9980602},"labels":[],"label_agreement":null},{"id":"W2075320242","doi":"10.1139/e06-067","title":"A statistical technique for determining the source area of glacially transported granite erratics in the Queen Elizabeth Islands, Nunavut","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"University of Toronto; University of Alberta; Washington State University","keywords":"Geology; Precambrian; Biological dispersal; Outcrop; Paleontology; Ice sheet; Geomorphology","score_opus":0.03267108596146497,"score_gpt":0.2684802518373675,"score_spread":0.23580916587590253,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075320242","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.983977,0.0002697778,0.012608672,0.00085762783,0.00014268752,0.00029153746,0.000053647294,0.0000015737966,0.0017974466],"genre_scores_gemma":[0.9979073,0.000011826079,0.0017709215,0.00024495358,0.00003540111,7.028981e-7,0.0000062925674,0.0000012577133,0.000021390526],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99867463,0.00015714685,0.00037657676,0.00010079805,0.00024407188,0.0004467946],"domain_scores_gemma":[0.998132,0.0013439495,0.00015197074,0.000083382445,0.00011856991,0.00017014383],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0047993218,0.0000787348,0.00017673562,0.00026112935,0.00038401628,0.00004036914,0.0005970542,0.00007810452,0.00014602451],"category_scores_gemma":[0.0003754323,0.000042271775,0.000050551294,0.00043029262,0.0011266605,0.000102681835,0.0000016670436,0.00029929326,0.0000015964567],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025574904,0.000004026854,0.9972885,0.000006974796,0.0000051214333,0.00004845863,0.001557978,0.00022115611,0.00000387402,0.00013585838,0.00003413306,0.00066832517],"study_design_scores_gemma":[0.00021118899,0.00038670585,0.9947124,0.000028172386,0.000012282153,0.00013671503,0.0012447181,0.0006167776,0.00003955758,0.0015110389,0.0010419807,0.000058447717],"about_ca_topic_score_codex":0.0020938907,"about_ca_topic_score_gemma":0.7114315,"teacher_disagreement_score":0.70933765,"about_ca_system_score_codex":4.18957e-7,"about_ca_system_score_gemma":0.000976039,"threshold_uncertainty_score":0.41512278},"labels":[],"label_agreement":null},{"id":"W2075423604","doi":"10.1139/e11-021","title":"Surface (sea floor) and near-surface (box cores) sediment mineralogy in Baffin Bay as a key to sediment provenance and ice sheet variations","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK; Canadian Foundation for Climate and Atmospheric Sciences; National Science Foundation","keywords":"Geology; Illite; Provenance; Dolomite; Sediment; Glacial period; Mineralogy; Geochemistry; Chlorite; Carbonate; Younger Dryas; Carbonate minerals; Clay minerals; Quartz; Geomorphology; Paleontology","score_opus":0.026697958290453096,"score_gpt":0.23686844461316534,"score_spread":0.21017048632271224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075423604","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99063474,0.0019458595,0.000015526524,0.0020003368,0.00027496731,0.00018485222,0.00002278417,0.000002762745,0.0049181813],"genre_scores_gemma":[0.99183124,0.00008581646,0.0073680365,0.00046958117,0.000021076881,4.451032e-7,0.0000020187267,0.0000018445724,0.00021992662],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99843043,0.00019830927,0.00030053864,0.00026373405,0.00021097873,0.0005960065],"domain_scores_gemma":[0.9987028,0.00016645176,0.00010168094,0.00009474211,0.0000992521,0.000835058],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015730072,0.0001238558,0.00022713067,0.00015552336,0.00047549736,0.00009758136,0.0002980749,0.0000848624,0.0010918132],"category_scores_gemma":[0.00020315153,0.00009999961,0.000022825952,0.00050643657,0.001005448,0.00032753657,0.000015106932,0.00024352068,0.00006719891],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003234068,0.000008059628,0.9936092,0.0000076238143,0.0000092256805,0.00016748958,0.0024974484,0.003054494,0.000015006227,0.00023253789,0.00008228315,0.0002843184],"study_design_scores_gemma":[0.0003218962,0.0007166369,0.9936125,0.000040435578,0.000007467228,0.00038267326,0.00039195913,0.0025762052,0.000051815492,0.00095702487,0.00082097156,0.00012041352],"about_ca_topic_score_codex":0.04057093,"about_ca_topic_score_gemma":0.69370407,"teacher_disagreement_score":0.6531331,"about_ca_system_score_codex":0.0000016316388,"about_ca_system_score_gemma":0.0012876131,"threshold_uncertainty_score":0.9998213},"labels":[],"label_agreement":null},{"id":"W2075572205","doi":"10.1139/e2012-048","title":"Stratigraphic restriction of stromatolites in a Middle and Upper Ordovician foreland-platform succession (Ottawa Embayment, eastern Ontario)","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Geology; Foreland basin; Onlap; Paleontology; Sedimentary depositional environment; Carbonate platform; Ordovician; Sedimentology; Geochemistry; Sedimentary rock; Unconformity; Tectonics","score_opus":0.03100566144419001,"score_gpt":0.22496765544732833,"score_spread":0.19396199400313832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075572205","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9792898,0.006430833,0.0000068165864,0.000068029854,0.00030811175,0.00006492341,0.000015470912,0.0000017035044,0.01381431],"genre_scores_gemma":[0.99926823,0.000049672097,0.0006024066,0.000018717838,0.000040343304,1.7904165e-7,0.0000014595583,5.227311e-7,0.000018467703],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987523,0.00005464364,0.00043344684,0.00011318065,0.0002152966,0.00043116545],"domain_scores_gemma":[0.9990333,0.000082209895,0.00028505392,0.00006334874,0.000039523027,0.0004965795],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00083051313,0.00010591716,0.00020906085,0.000661046,0.00024367087,0.00005900492,0.00020185583,0.00008293721,0.00020904567],"category_scores_gemma":[0.00003939259,0.00007862324,0.00005706871,0.00043007015,0.00050093397,0.0010771296,8.771833e-7,0.00019790015,0.000001214448],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010023874,0.0000070808223,0.9950093,0.000008639181,0.000007673273,0.000013797819,0.0010315542,0.000024142597,0.000010573818,0.00034452672,0.000006315389,0.0035263554],"study_design_scores_gemma":[0.00021749486,0.00032891583,0.9970562,0.00011715967,0.000009534959,0.00013174811,0.0009210082,0.00014546589,0.00002834876,0.00076923385,0.00018840707,0.000086480824],"about_ca_topic_score_codex":0.22042084,"about_ca_topic_score_gemma":0.98525816,"teacher_disagreement_score":0.7648373,"about_ca_system_score_codex":0.0000020239318,"about_ca_system_score_gemma":0.0006986862,"threshold_uncertainty_score":0.7847704},"labels":[],"label_agreement":null},{"id":"W2075704741","doi":"10.1139/cjes-2014-0093","title":"Petrochemistry, hydrothermal alteration, mineralogy, and sulfur isotope geochemistry of the Turgeon Cu–Zn volcanogenic massive sulfide deposit, northern New Brunswick, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval; Geological Survey of Canada","funders":"Université Laval","keywords":"Stockwork; Geology; Geochemistry; Pyrite; Volcanogenic massive sulfide ore deposit; Chalcopyrite; Basalt; Chlorite; Rhyolite; Breccia; Mafic; Sphalerite; Volcanic rock; Chemistry; Quartz; Volcano","score_opus":0.010797138972218937,"score_gpt":0.17633248681482985,"score_spread":0.16553534784261092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075704741","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99227893,0.0026404273,0.000008302562,0.0029140792,0.00017403197,0.000045387187,0.00002492184,0.0000016202466,0.0019123192],"genre_scores_gemma":[0.9986272,0.000010760494,0.00017917666,0.00036715443,0.00015113315,7.8554066e-8,0.0000069558664,0.0000015495597,0.0006560032],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985953,0.00005204655,0.00037582824,0.00019793567,0.00040486484,0.000374049],"domain_scores_gemma":[0.9982585,0.0000761858,0.00028601167,0.00012792205,0.00022974692,0.0010216822],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003089851,0.00014265857,0.00024190148,0.000056894027,0.00021704535,0.00007755624,0.0005365717,0.000057760157,0.00089541276],"category_scores_gemma":[0.00027954538,0.00008742465,0.00009175809,0.00040553996,0.00050329586,0.0001376084,0.000014165377,0.00018342078,0.0000027014978],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007881534,0.0000024456035,0.994536,0.0000053890603,0.000023094926,0.000029375835,0.000106273066,0.0029864737,0.0014279926,0.0000072258326,0.00042606,0.00044177767],"study_design_scores_gemma":[0.0003764081,0.00015158467,0.9695939,0.000048469425,0.00006965543,0.00035185786,0.00052416895,0.002413535,0.022591662,0.0014033234,0.0022283576,0.0002470648],"about_ca_topic_score_codex":0.9667644,"about_ca_topic_score_gemma":0.9992595,"teacher_disagreement_score":0.032495044,"about_ca_system_score_codex":0.00000914705,"about_ca_system_score_gemma":0.012413391,"threshold_uncertainty_score":0.9931853},"labels":[],"label_agreement":null},{"id":"W2075929381","doi":"10.1139/e04-021","title":"The Red Island Road Formation: Early Devonian terrestrial fill in the Anticosti Foreland Basin, western Newfoundland","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Petro-Canada; Memorial University of Newfoundland; Brandon University","funders":"","keywords":"Geology; Provenance; Foreland basin; Paleontology; Clastic rock; Siliciclastic; Terrane; Paleocurrent; Devonian; Conglomerate; Red beds; Structural basin; Facies; Tectonics","score_opus":0.018693139918930617,"score_gpt":0.20340318881695024,"score_spread":0.18471004889801962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075929381","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9864985,0.0005808867,0.000023174329,0.009840039,0.00024136725,0.000072135415,0.000012831345,0.0000015613265,0.0027295435],"genre_scores_gemma":[0.9992085,0.00004436928,0.0000828739,0.00044744916,0.00017507604,2.1343892e-7,0.0000037958093,6.616512e-7,0.000037058868],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987125,0.00009537017,0.0003456222,0.0001125093,0.00033531873,0.00039868522],"domain_scores_gemma":[0.9992368,0.00019654603,0.00015750718,0.00009363678,0.0000448643,0.00027063067],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010743754,0.00009393665,0.00014922653,0.0001252739,0.000669596,0.00047333437,0.0006366229,0.000043423428,0.00038448322],"category_scores_gemma":[0.00023488319,0.00004136189,0.00008443988,0.00056135753,0.0004556148,0.0004083892,0.000004287648,0.00021284382,0.00003065651],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014107456,0.0000027058402,0.9954564,8.226923e-7,0.0000051023007,0.00005796892,0.0003595736,0.0018871787,0.0000015873246,0.000022399227,0.00005276661,0.0021393758],"study_design_scores_gemma":[0.00036940468,0.00026753813,0.98420256,0.000023367485,0.000010018347,0.00015227044,0.00026254923,0.00030558472,0.000007260026,0.0078233145,0.006502116,0.00007403382],"about_ca_topic_score_codex":0.0929296,"about_ca_topic_score_gemma":0.96233046,"teacher_disagreement_score":0.86940086,"about_ca_system_score_codex":0.0000026657142,"about_ca_system_score_gemma":0.0003904487,"threshold_uncertainty_score":0.9131107},"labels":[],"label_agreement":null},{"id":"W2076029085","doi":"10.1139/e06-126","title":"Barite (BaSO<sub>4</sub>) biomineralization at Flybye Springs, a cold sulphur spring system in Canada's Northwest Territories","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"University of Saskatchewan","keywords":"Biomineralization; Chemosynthesis; Microbial mat; Pyrite; Geology; Extracellular polymeric substance; Barium; Mineralogy; Sulfur; Hydrothermal circulation; Chemocline; Geochemistry; Hydrothermal vent; Environmental chemistry; Chemistry; Cyanobacteria; Bacteria; Anoxic waters; Paleontology; Inorganic chemistry","score_opus":0.012673944426598227,"score_gpt":0.19870345462911107,"score_spread":0.18602951020251285,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076029085","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996444,0.00097064493,0.000014030713,0.000296778,0.0012028394,0.000094108196,0.00003678929,0.000004537243,0.00093627203],"genre_scores_gemma":[0.99956375,0.000027882803,0.00014428241,0.00010508817,0.00013018213,1.9705973e-7,0.0000075120092,0.000002514795,0.000018606575],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99792325,0.0001076421,0.000499308,0.00022186256,0.00041096105,0.000836942],"domain_scores_gemma":[0.9985286,0.00024037638,0.00021018361,0.00010841385,0.00015343355,0.0007590205],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019914408,0.00013994654,0.00026105827,0.0006699001,0.00058087555,0.00009726211,0.0004578019,0.00009395728,0.00009842262],"category_scores_gemma":[0.00015952167,0.00012125463,0.000045421464,0.00082167034,0.00046876454,0.0003514034,0.0000104903565,0.00026648058,0.000020552285],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014802542,0.0000015605216,0.9967631,0.000018907665,0.0000071633617,0.0008900116,0.0001159999,0.0016918834,0.00011050338,0.00017554795,0.00001730983,0.00019317574],"study_design_scores_gemma":[0.00020046122,0.00008517896,0.99480873,0.00008516818,0.0000055199125,0.000380191,0.0004950525,0.0007064702,0.0016040099,0.000011310056,0.0014826622,0.00013521571],"about_ca_topic_score_codex":0.9760435,"about_ca_topic_score_gemma":0.99999094,"teacher_disagreement_score":0.023947394,"about_ca_system_score_codex":0.000021494103,"about_ca_system_score_gemma":0.0049526324,"threshold_uncertainty_score":0.8785757},"labels":[],"label_agreement":null},{"id":"W2076165849","doi":"10.1139/e00-003","title":"Spatial distribution of surficial sediments in part of the Kingston basin of northeastern Lake Ontario, Canada","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada; Deutsche Forschungsgemeinschaft","keywords":"Geology; Winnowing; Structural basin; Slumping; Sediment; Sedimentary rock; Deposition (geology); Erosion; Channel (broadcasting); Geomorphology; Oceanography; Paleontology; Archaeology","score_opus":0.00792827425148638,"score_gpt":0.1675517179046802,"score_spread":0.15962344365319384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076165849","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99672914,0.000028391349,0.0000025347324,0.00017719249,0.00044033572,0.000048214406,0.0003500397,2.7933314e-7,0.0022238505],"genre_scores_gemma":[0.9996593,0.0000026615112,0.000015161912,0.000033635286,0.000029233517,3.101533e-8,0.000012451303,6.695534e-7,0.00024684877],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998951,0.00004478502,0.00037700197,0.000074880256,0.00035166263,0.0002006726],"domain_scores_gemma":[0.999428,0.000035881538,0.00024631142,0.000065435255,0.00007323787,0.00015118482],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003812508,0.00006285234,0.00017000368,0.00006872605,0.00007632502,0.000011614143,0.00029217743,0.000022906928,0.0020091527],"category_scores_gemma":[0.000033389402,0.00004338652,0.000050406492,0.00031477885,0.0002810624,0.00011757435,0.0000042278557,0.00010137509,4.2936747e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018070707,0.0000047104927,0.9795279,0.000004225926,0.0000036231668,0.0000071297086,0.0001521504,0.0055459915,0.0000021868818,0.000009470643,0.000037285157,0.014687265],"study_design_scores_gemma":[0.00013018011,0.00013184205,0.9885557,0.000055294,0.000006032635,0.000012751466,0.000077154014,0.00061898417,0.00006222434,0.00003828344,0.010267222,0.00004432634],"about_ca_topic_score_codex":0.9973137,"about_ca_topic_score_gemma":0.99999696,"teacher_disagreement_score":0.014642939,"about_ca_system_score_codex":0.000006717659,"about_ca_system_score_gemma":0.0048365425,"threshold_uncertainty_score":0.99890316},"labels":[],"label_agreement":null},{"id":"W2076336477","doi":"10.1139/e03-018","title":"Geology and geochemistry of the Clear Creek intrusion-related gold occurrences, Tintina Gold Province, Yukon, Canada","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon University","funders":"","keywords":"Geology; Geochemistry; Hornfels; Fluid inclusions; Greenschist; Quartz; Pyrite; Hydrothermal circulation; Arsenopyrite; Petrography; Metamorphic facies; Metamorphic rock; Mineralogy; Facies; Structural basin; Geomorphology; Biotite; Paleontology; Copper","score_opus":0.009443356303930612,"score_gpt":0.18558407942928307,"score_spread":0.17614072312535245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076336477","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96414906,0.00090402074,0.000058031535,0.0035795327,0.00068757375,0.00007526993,0.000004955064,0.000004325616,0.030537257],"genre_scores_gemma":[0.99725056,0.000011295539,0.0009514857,0.00022461973,0.000022628124,3.8334008e-7,1.751535e-7,0.000001043584,0.0015377863],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.998566,0.00009377343,0.00039984434,0.00023551045,0.00029418757,0.00041074102],"domain_scores_gemma":[0.9985953,0.00011073089,0.00043396314,0.0002364793,0.00025129417,0.00037222056],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009103711,0.00011266081,0.00019700396,0.00006954177,0.00027404213,0.00010328464,0.0011774632,0.00007386253,0.00012157033],"category_scores_gemma":[0.0008965187,0.00008307057,0.000049350303,0.00060352933,0.00082434283,0.00020064304,0.00007371367,0.00028931018,7.590961e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009186678,0.00005129952,0.89459354,0.0001854535,0.00008626767,0.0005435155,0.0011172065,0.002984493,0.003130538,0.042761397,0.041690867,0.012846232],"study_design_scores_gemma":[0.001420115,0.0008172286,0.31068107,0.0007508548,0.000055815122,0.006589019,0.0024652416,0.009643186,0.024521587,0.027586862,0.6142157,0.0012533553],"about_ca_topic_score_codex":0.18997367,"about_ca_topic_score_gemma":0.7713517,"teacher_disagreement_score":0.58391243,"about_ca_system_score_codex":0.000011933543,"about_ca_system_score_gemma":0.0076995036,"threshold_uncertainty_score":0.99792594},"labels":[],"label_agreement":null},{"id":"W2076431700","doi":"10.1139/e02-103","title":"Greenschist-facies metamorphism of the Burgess Shale and its implications for models of fossil formation and preservation","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Greenschist; Geology; Metamorphism; Geochemistry; Illite; Metamorphic facies; Chlorite; Facies; Clay minerals; Paleontology; Quartz; Structural basin","score_opus":0.056640767650635644,"score_gpt":0.21228231092507155,"score_spread":0.1556415432744359,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076431700","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99486154,0.0028224504,0.00023933085,0.0012357575,0.000032725406,0.00006927752,0.00005615003,5.4718345e-7,0.00068219495],"genre_scores_gemma":[0.9990695,0.000054985936,0.000785795,0.000035113153,0.0000069127573,3.293875e-7,0.0000011554815,3.2513367e-7,0.000045870307],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99946123,0.000031939766,0.00022171105,0.00006719111,0.00010122386,0.00011671033],"domain_scores_gemma":[0.9993182,0.000119844306,0.00020759788,0.000045072047,0.00017382552,0.00013547206],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044832742,0.00004383092,0.00011919986,0.00008381852,0.00020956193,0.000023411678,0.00014485446,0.000022810334,0.000099309415],"category_scores_gemma":[0.0002820447,0.000024864203,0.00004731338,0.00026510743,0.00027828067,0.0004274993,0.000003047784,0.000038146587,1.3677163e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000034384911,0.0000032586622,0.9853952,0.000022885115,0.0000118099115,1.1893249e-7,0.00023852345,0.0026324075,0.00069815695,0.008969403,0.00002321774,0.0020015643],"study_design_scores_gemma":[0.00009431589,0.00009559652,0.8897652,0.000016506026,0.000030408137,0.000021392183,0.00013186723,0.012744726,0.0018184336,0.09484944,0.00038531737,0.00004677924],"about_ca_topic_score_codex":0.002254136,"about_ca_topic_score_gemma":0.037680242,"teacher_disagreement_score":0.09563,"about_ca_system_score_codex":4.2878116e-7,"about_ca_system_score_gemma":0.00013658726,"threshold_uncertainty_score":0.97987956},"labels":[],"label_agreement":null},{"id":"W2076464878","doi":"10.1139/e02-107","title":"Lower Paleozoic configuration of the Quebec reentrant based on improved along-strike paleogeography","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Chicoutimi","funders":"","keywords":"Geology; Orogeny; Rift; Graben; Paleozoic; Ordovician; Paleontology; Tectonics; Fault (geology); Geomorphology; Palaeogeography","score_opus":0.01264808667277448,"score_gpt":0.18842655251561846,"score_spread":0.17577846584284398,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076464878","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98601866,0.0005968636,0.00023142733,0.00081629696,0.0007278958,0.00011255689,0.000038707512,0.0000024189753,0.011455173],"genre_scores_gemma":[0.99928033,0.000011493355,0.00027279512,0.00035849662,0.000022394725,1.554652e-7,0.0000019462354,6.86661e-7,0.00005169454],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989686,0.000099278215,0.00031376598,0.000096173026,0.00026929626,0.00025288598],"domain_scores_gemma":[0.9991045,0.00013642652,0.00025251764,0.000100108795,0.00015146357,0.000254979],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00072072214,0.00008302567,0.00012418983,0.00020489271,0.000378063,0.000095791256,0.0003279767,0.000044292407,0.0023866326],"category_scores_gemma":[0.0002734281,0.000045145676,0.000104736595,0.0006966974,0.0006116924,0.00023699,7.736731e-7,0.00012932494,0.000008551506],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010691984,0.0000075624025,0.9855974,0.000007851719,0.000005185821,0.0000054357774,0.00006957088,0.010285362,0.00002093426,0.0004232395,0.000051345563,0.003515421],"study_design_scores_gemma":[0.00020499954,0.0005299725,0.98809725,0.00005069663,0.000010709385,0.000018252551,0.00020219998,0.0017767525,0.00082310004,0.00052517623,0.0076707276,0.00009016869],"about_ca_topic_score_codex":0.015976014,"about_ca_topic_score_gemma":0.6061167,"teacher_disagreement_score":0.5901407,"about_ca_system_score_codex":8.439701e-7,"about_ca_system_score_gemma":0.0013722703,"threshold_uncertainty_score":0.9985253},"labels":[],"label_agreement":null},{"id":"W2076543482","doi":"10.1139/e05-007","title":"UPb zircon geochronology and Nd isotope geochemistry of Proterozoic granitoids in the western Churchill Province: intrusive age pattern and Archean source domains","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Nunavut Research Institute; Government of Nunavut; Geological Survey of Canada","funders":"","keywords":"Zircon; Geology; Geochemistry; Archean; Geochronology; Proterozoic; Igneous rock; Mafic; Plutonism; Crust; Pluton; Paleontology","score_opus":0.010379815642870906,"score_gpt":0.19399931053411387,"score_spread":0.18361949489124296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076543482","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99468035,0.0013776093,0.000036409507,0.0030934073,0.000026261654,0.00010235501,0.000018532108,0.0000014992095,0.0006636088],"genre_scores_gemma":[0.9989547,0.000051027477,0.00028422047,0.00056452985,0.000101096986,4.598621e-7,0.0000033608144,9.837079e-7,0.000039629802],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988284,0.000101829406,0.00031680975,0.00019483657,0.000200155,0.00035793707],"domain_scores_gemma":[0.99926853,0.00013622356,0.00017952142,0.00008700046,0.000040791874,0.0002879121],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00068933686,0.00011514589,0.00023868085,0.00016044741,0.00018194788,0.0000866478,0.00038771654,0.00006206137,0.000419288],"category_scores_gemma":[0.00010044011,0.00006795339,0.00004635453,0.0002383507,0.0013317539,0.00016998945,0.000013965103,0.0002678497,0.0000035252533],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000070154188,0.000007386399,0.97000647,0.000015526066,0.000008440634,0.000064047694,0.000816518,0.00024292599,0.00039384537,0.0000054135694,0.000016332468,0.028416099],"study_design_scores_gemma":[0.00028353574,0.00036071226,0.9926579,0.00004674983,0.000016889397,0.00031081238,0.0007666102,0.00065133977,0.00084489875,0.0015814588,0.002354692,0.00012438057],"about_ca_topic_score_codex":0.022193158,"about_ca_topic_score_gemma":0.6107035,"teacher_disagreement_score":0.5885104,"about_ca_system_score_codex":0.0000017001292,"about_ca_system_score_gemma":0.00024144229,"threshold_uncertainty_score":0.98431814},"labels":[],"label_agreement":null},{"id":"W2076949215","doi":"10.1139/e08-016","title":"Middle–Late Cambrian Rankenella–Girvanella reefs of the Mila Formation, northern Iran","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Reef; Geology; Paleontology; Ordovician; Stromatolite; Carbonate; Oceanography","score_opus":0.04099805110786572,"score_gpt":0.19777995782369423,"score_spread":0.1567819067158285,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076949215","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9638289,0.0043179053,0.000016502609,0.00053256535,0.00061901164,0.00007141866,0.000030189969,0.00000241948,0.030581089],"genre_scores_gemma":[0.999302,0.00006943724,0.00030872072,0.00010950403,0.000077080724,7.276174e-8,6.1394144e-7,6.306445e-7,0.00013190624],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998614,0.00012559404,0.00043744227,0.00011793506,0.00033736334,0.00036764046],"domain_scores_gemma":[0.9988684,0.00009023638,0.00037981741,0.00013984294,0.00013198283,0.00038969854],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006915709,0.000108959466,0.00020837184,0.00023604461,0.0008926434,0.00003892092,0.0006897134,0.00006644482,0.0002175403],"category_scores_gemma":[0.00010138202,0.000068101726,0.00016026685,0.0005512996,0.0014307363,0.0004280984,0.0000010347462,0.00018338746,0.000009462791],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000084138655,0.0000021935807,0.9949207,0.0000052142677,0.000010777719,0.000044394394,0.001095333,0.00075208425,0.000029960753,0.000028530088,0.000083062136,0.0030193867],"study_design_scores_gemma":[0.00019042812,0.00016005119,0.9968792,0.000044408982,0.000010743067,0.0005589114,0.00030581994,0.00032611194,0.00019310319,0.00034130472,0.0009021687,0.00008775134],"about_ca_topic_score_codex":0.01260334,"about_ca_topic_score_gemma":0.79705006,"teacher_disagreement_score":0.7844467,"about_ca_system_score_codex":0.0000011926061,"about_ca_system_score_gemma":0.0012000214,"threshold_uncertainty_score":0.9939718},"labels":[],"label_agreement":null},{"id":"W2077275603","doi":"10.1139/e01-013","title":"Ubiquity of anomalous fading in K-feldspars and the measurement and correction for it in optical dating","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1100,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Fading; Logarithm; Irradiation; Luminescence; Optically stimulated luminescence; Mineralogy; Thermoluminescence dating; Geology; Physics; Optics; Statistics; Mathematics; Nuclear physics","score_opus":0.06452201742207646,"score_gpt":0.26681085045603936,"score_spread":0.2022888330339629,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077275603","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949136,0.00086647103,0.000021288375,0.001288631,0.00017246521,0.00008743712,0.00000115796,3.5352312e-7,0.0026486015],"genre_scores_gemma":[0.99961066,0.000083178136,0.0002113951,0.000069777634,0.000014699809,2.802549e-7,2.0013168e-7,3.743675e-7,0.000009419495],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992553,0.00009365914,0.00020666326,0.0000852681,0.00012654772,0.00023255679],"domain_scores_gemma":[0.99930763,0.0004080175,0.00007463989,0.000028890676,0.000055236254,0.00012560004],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00396679,0.00004040632,0.00013672035,0.00023304916,0.00017615293,0.000030299298,0.00011805902,0.000037242207,0.000058934133],"category_scores_gemma":[0.0005855331,0.000026555519,0.000014701732,0.00023628614,0.0008355167,0.00013797886,0.000003216057,0.00014042531,4.3360555e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004671603,0.0000012990936,0.9962946,0.000004381715,0.0000021162557,0.000016410004,0.00043383084,0.0013404976,0.0000017519837,0.00008969566,0.000005693427,0.0017629995],"study_design_scores_gemma":[0.0004386279,0.00016598693,0.98151773,0.00004599172,0.000003052037,0.0002567811,0.0012092022,0.015598206,0.000010841058,0.00061577157,0.00010678801,0.000031042528],"about_ca_topic_score_codex":0.0061377226,"about_ca_topic_score_gemma":0.7603957,"teacher_disagreement_score":0.754258,"about_ca_system_score_codex":6.304911e-7,"about_ca_system_score_gemma":0.00036557644,"threshold_uncertainty_score":0.92784417},"labels":[],"label_agreement":null},{"id":"W2077298513","doi":"10.1139/e07-035","title":"Cessation of ice-wedge development during the 20th century in spruce forests of eastern Mackenzie Delta, Northwest Territories, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University; Aboriginal Affairs Northern Dev Canada","funders":"Natural Resources Canada; Aurora Research Institute","keywords":"Permafrost; Ice wedge; Geology; Tundra; Subarctic climate; Peat; Physical geography; Arctic; Snowmelt; Snow; Delta; Geomorphology; Ridge; Oceanography; Paleontology; Ecology; Geography","score_opus":0.023281196100461046,"score_gpt":0.21609954448192215,"score_spread":0.1928183483814611,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077298513","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970569,0.0012089141,0.000002716491,0.00013255543,0.00073095923,0.00006642376,0.00052482105,6.427453e-7,0.00027606593],"genre_scores_gemma":[0.999651,0.000042593303,0.000061409824,0.00005472331,0.00011527865,9.1491465e-8,0.000058483747,0.00000157091,0.000014842717],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99860495,0.000031229512,0.0004907199,0.00010076297,0.00040453422,0.0003677745],"domain_scores_gemma":[0.99905777,0.0001283725,0.0003202482,0.000076274315,0.00011996244,0.0002973587],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008815415,0.00009032028,0.00015917851,0.00024950056,0.00021131558,0.000039979182,0.0003961141,0.000032380456,0.00038005775],"category_scores_gemma":[0.000054914803,0.0000626866,0.000029312805,0.00048278223,0.00024067583,0.00025521356,0.000005872917,0.000115071976,9.156937e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012123264,0.0000025000945,0.996121,0.000020450845,0.0000042609036,0.000053875952,0.0012483922,0.00067515386,0.000017548493,0.000004122784,0.00001589187,0.0018246999],"study_design_scores_gemma":[0.00015282095,0.0000471116,0.99267584,0.000093302275,0.0000034200084,0.00003273741,0.0016714797,0.0000989676,0.00063578284,0.000009377599,0.0045049163,0.00007423073],"about_ca_topic_score_codex":0.97882223,"about_ca_topic_score_gemma":0.99999,"teacher_disagreement_score":0.021167753,"about_ca_system_score_codex":0.000013221202,"about_ca_system_score_gemma":0.0028777283,"threshold_uncertainty_score":0.5104966},"labels":[],"label_agreement":null},{"id":"W2077604873","doi":"10.1139/e02-080","title":"A review of nonmarine turtles from the Late Cretaceous of Alberta","year":2003,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":109,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"University of Alberta","keywords":"Cretaceous; Geology; Paleontology; Canyon; Turtle (robot); Cenomanian; Geomorphology; Ecology","score_opus":0.03862124284278584,"score_gpt":0.2549355386403446,"score_spread":0.2163142957975588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077604873","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0004264423,0.9915604,0.0000014359696,0.00025349145,0.0007054408,0.00014129169,0.00021837107,6.2614805e-7,0.006692519],"genre_scores_gemma":[0.00031838688,0.9987987,0.00019601568,0.00035474414,0.00008532495,2.631138e-7,0.000030162708,0.0000017618968,0.0002146229],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99797857,0.0004852626,0.0008666841,0.00016006727,0.00018548731,0.0003239342],"domain_scores_gemma":[0.9972028,0.0010450189,0.0011567725,0.00019532007,0.000120468336,0.00027961118],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013424701,0.00018843565,0.0011639259,0.00018836946,0.00018499022,0.000013511943,0.0009984836,0.00015635714,0.0037138825],"category_scores_gemma":[0.00052739284,0.00009981314,0.00035720022,0.00055230974,0.0014240922,0.00011814188,0.0000062207264,0.00031978017,0.000039861294],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010617039,0.000013090529,0.1963078,0.009349153,0.00044324054,0.00010434169,0.00023462035,0.00009213529,1.4189345e-7,0.00017004501,0.005021012,0.78825384],"study_design_scores_gemma":[0.00004113678,0.00016839111,0.01298172,0.016213281,0.00023774082,0.0003513686,0.000019308141,0.0000073351625,1.19140786e-7,0.00016630879,0.9697024,0.0001108816],"about_ca_topic_score_codex":0.042847898,"about_ca_topic_score_gemma":0.63443696,"teacher_disagreement_score":0.9646814,"about_ca_system_score_codex":0.0000016468007,"about_ca_system_score_gemma":0.0037286014,"threshold_uncertainty_score":0.99719685},"labels":[],"label_agreement":null},{"id":"W2077740530","doi":"10.1139/e10-015","title":"A new whitefish from the early Quaternary of Bluefish Basin, Yukon Territory, Canada, and its paleoenvironmental implications","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fish Ecology and Management Studies","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature; University of Ottawa; University of Waterloo; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta; University of Ottawa","keywords":"Geology; Paleontology; Concretion; Quaternary; Eemian; Interglacial","score_opus":0.008409389377827646,"score_gpt":0.1839394122753996,"score_spread":0.17553002289757194,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077740530","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98904157,0.00008431595,0.00000641234,0.007427876,0.00039397556,0.000075837255,0.000034173092,0.0000012200323,0.0029346044],"genre_scores_gemma":[0.9982459,0.000024677012,0.00029051598,0.0010445134,0.00007589217,0.0000010344163,5.6322864e-7,0.0000028064578,0.00031410306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992051,0.000029586156,0.00020592964,0.0001426944,0.00019055401,0.00022610788],"domain_scores_gemma":[0.99933755,0.00008314736,0.00017223049,0.000105706604,0.000007885831,0.00029348367],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00026785216,0.00007973228,0.00011459789,0.000037170925,0.0004284287,0.0000404125,0.00045357636,0.0000311174,0.0012246439],"category_scores_gemma":[0.00005439956,0.000057737197,0.00002708469,0.000115006536,0.00058962044,0.00026043862,0.00005860507,0.00015801536,0.000007443962],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001438179,0.0000034544937,0.9827589,5.77957e-7,0.000010923193,0.0000068626714,0.00033738508,0.00001717012,0.00028780143,0.000047156696,0.016041303,0.00048704635],"study_design_scores_gemma":[0.000100867095,0.000069698755,0.9865736,0.000006928334,0.00001572189,0.000015650718,0.00027805354,0.00001474914,0.00011911421,0.00033480616,0.012406728,0.00006409288],"about_ca_topic_score_codex":0.79947245,"about_ca_topic_score_gemma":0.99864787,"teacher_disagreement_score":0.19917543,"about_ca_system_score_codex":0.000012126655,"about_ca_system_score_gemma":0.00031253565,"threshold_uncertainty_score":0.9996884},"labels":[],"label_agreement":null},{"id":"W2077740754","doi":"10.1139/e06-085","title":"Nature and origin of sediments infilling poorly defined buried bedrock valleys adjacent to the Niagara Escarpment, southern Ontario, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University; University of Waterloo","funders":"","keywords":"Geology; Fluvial; Bedrock; Escarpment; Facies; Geomorphology; Colluvium; Sediment; Glacial period; Isopach map; Alluvium; Paleontology; Geochemistry; Structural basin","score_opus":0.0174130782943595,"score_gpt":0.22941295252394284,"score_spread":0.21199987422958333,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077740754","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926415,0.0014439966,0.000009238114,0.0021048046,0.00057984935,0.00010489365,0.000022171305,0.0000012347493,0.0030922892],"genre_scores_gemma":[0.9983164,0.0000096847125,0.00044526125,0.000777495,0.0000629326,1.15254046e-7,0.0000026958255,0.0000013894661,0.00038402266],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984754,0.00007606953,0.00031807163,0.0001599337,0.00041096107,0.0005596178],"domain_scores_gemma":[0.99867535,0.00024019225,0.00016252566,0.00009697308,0.00013534549,0.0006896321],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017065305,0.00010841448,0.00019563579,0.00024847322,0.0005094104,0.000048352642,0.00048007516,0.00009230384,0.0008961698],"category_scores_gemma":[0.0001309068,0.00006973589,0.00003609378,0.0003829581,0.0003604404,0.00010550445,0.000009058662,0.0004523836,0.0000118516045],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022666367,0.0000016827398,0.99721867,0.0000036760698,0.000020771882,0.00008056925,0.0010202012,0.00095727795,0.0000050544504,0.000035015906,0.0003570746,0.00027734277],"study_design_scores_gemma":[0.00018679143,0.00021526223,0.98142123,0.00003210086,0.000011884175,0.00017731616,0.0011774822,0.000059243244,0.000094297706,0.00012030984,0.016413176,0.000090884125],"about_ca_topic_score_codex":0.94034255,"about_ca_topic_score_gemma":0.99991286,"teacher_disagreement_score":0.059570327,"about_ca_system_score_codex":0.0000035631426,"about_ca_system_score_gemma":0.0044473037,"threshold_uncertainty_score":0.9812431},"labels":[],"label_agreement":null},{"id":"W2077745183","doi":"10.1139/e06-031","title":"Locomotion in derived dicynodonts (Synapsida, Anomodontia): a functional analysis of the pelvic girdle and hind limb of<i>Tetragonias njalilus</i>","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Hindlimb; Anatomy; Gait; Vertebral column; Geology; Biology; Paleontology","score_opus":0.013514699322062368,"score_gpt":0.18697615433355,"score_spread":0.17346145501148763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077745183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948608,0.002739997,0.00006348556,0.00047693984,0.00032073742,0.00004674754,0.00005405938,9.5295167e-7,0.0014362333],"genre_scores_gemma":[0.99964267,0.000025305293,0.00019011719,0.000056570505,0.000036170284,1.0089164e-7,0.0000069739976,6.379002e-7,0.000041465682],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99891627,0.00015557485,0.00037462715,0.00013396202,0.00017904113,0.00024055499],"domain_scores_gemma":[0.9992698,0.00014845052,0.00030031102,0.00007590369,0.00007957358,0.00012599393],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007168422,0.00007884784,0.00025284177,0.0006448322,0.00018224667,0.000015217731,0.000240868,0.000076575794,0.00043876717],"category_scores_gemma":[0.000078447,0.000053481777,0.0001056687,0.0010791556,0.0011442602,0.00021973786,0.0000045779025,0.00013631771,0.0000016441596],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017083656,0.000007321463,0.9849757,0.0000028491065,0.000035491987,0.0000085360125,0.000075226206,0.014132685,0.00018033455,0.00008385099,0.000038730068,0.00044220142],"study_design_scores_gemma":[0.0001672944,0.00016546737,0.9957915,0.000014948266,0.00006472274,0.00007203595,0.000112624046,0.0026314603,0.00009778886,0.00064903643,0.00017693883,0.000056172532],"about_ca_topic_score_codex":0.04955903,"about_ca_topic_score_gemma":0.894064,"teacher_disagreement_score":0.84450495,"about_ca_system_score_codex":0.000002748385,"about_ca_system_score_gemma":0.0006131493,"threshold_uncertainty_score":0.95677006},"labels":[],"label_agreement":null},{"id":"W2078184309","doi":"10.1139/cjes-2013-0001","title":"Age and growth in <i>Myledaphus bipartitus</i>, a Late Cretaceous freshwater guitarfish from Alberta, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Ichthyology and Marine Biology","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Royal Tyrrell Museum","funders":"","keywords":"Cretaceous; Biology; Geography; Ecology; Fishery; Paleontology","score_opus":0.006923049990537494,"score_gpt":0.17580163310770433,"score_spread":0.16887858311716683,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078184309","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98840505,0.0001892446,0.000001310658,0.0022252982,0.00031673317,0.00006322402,0.000007873214,0.0000010582751,0.008790179],"genre_scores_gemma":[0.9968777,0.000016292272,0.00039839398,0.0015940086,0.00003645878,0.0000015560325,9.817604e-7,0.0000029499477,0.0010717148],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898666,0.00006563811,0.00023349353,0.00017061303,0.00012464829,0.00041893413],"domain_scores_gemma":[0.9993114,0.00007879013,0.00007717885,0.00006739599,0.000013761357,0.00045146924],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024413678,0.00009511432,0.00016360459,0.00008851864,0.00015597326,0.000055043165,0.0003138453,0.00005727532,0.0070225224],"category_scores_gemma":[0.00011123358,0.00007203629,0.00002130085,0.00018007854,0.0007199906,0.0002932698,0.000041247375,0.00015030908,0.000092042144],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002658155,0.0000030586107,0.9929269,7.051475e-7,0.000005253897,0.00029903286,0.00026657357,0.00013229865,0.00026054765,0.00003176028,0.005648972,0.00042223802],"study_design_scores_gemma":[0.00017978,0.000096278774,0.95581627,0.00000844069,0.000004883045,0.0000690304,0.000065569344,0.00012887093,0.00018146509,0.001393088,0.041945033,0.00011129559],"about_ca_topic_score_codex":0.9939895,"about_ca_topic_score_gemma":0.99992496,"teacher_disagreement_score":0.037110634,"about_ca_system_score_codex":0.000022008462,"about_ca_system_score_gemma":0.00049555756,"threshold_uncertainty_score":0.9938852},"labels":[],"label_agreement":null},{"id":"W2078411808","doi":"10.1139/e02-059","title":"Analysis and reinterpretation of deformation features in the Rouge River valley, Scarborough, Ontario","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University; Geological Survey of Canada; Carleton University; Simon Fraser University","funders":"","keywords":"Geology; Bedrock; Geomorphology; Glacial period; Pleistocene; Ordovician; Borehole; Paleontology","score_opus":0.018088796083266596,"score_gpt":0.21955283899553005,"score_spread":0.20146404291226344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078411808","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99286044,0.001752893,0.000011547947,0.00054318627,0.000068388865,0.000050423598,0.0000027806525,5.059924e-7,0.004709842],"genre_scores_gemma":[0.9995353,0.000056669567,0.0002094204,0.000121064,0.000008716025,1.1530002e-7,0.0000016208431,2.8234308e-7,0.00006677707],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99915004,0.00018492213,0.0002105829,0.000075269636,0.00018668872,0.00019247146],"domain_scores_gemma":[0.9994486,0.00019498565,0.00013375258,0.00005936977,0.00005723389,0.0001060564],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001150929,0.00004947219,0.00015275538,0.0005526729,0.00017691727,0.000047453213,0.00026536512,0.000045763943,0.0006727052],"category_scores_gemma":[0.00010501027,0.000029869994,0.00005023381,0.00066907273,0.00059230725,0.00034234056,0.0000019967706,0.00018285173,0.000005941559],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000035968244,0.0000015297304,0.9928717,0.000009362834,0.000020510002,0.00001872504,0.0054879575,0.0013142746,2.9903066e-7,0.000044580946,0.000008522349,0.00021893096],"study_design_scores_gemma":[0.000074156254,0.00013504323,0.99626046,0.000027441432,0.00003754973,0.00011584737,0.0004725299,0.002483932,0.0000059659296,0.00032065282,0.00003328388,0.000033126307],"about_ca_topic_score_codex":0.10251734,"about_ca_topic_score_gemma":0.98848295,"teacher_disagreement_score":0.88596565,"about_ca_system_score_codex":6.0653673e-7,"about_ca_system_score_gemma":0.00018541096,"threshold_uncertainty_score":0.9034591},"labels":[],"label_agreement":null},{"id":"W2078560417","doi":"10.1139/e06-106","title":"Pre-, syn-, and post-imbrication deformation of carbonate slices along the southern Quebec Appalachian front – implications for hydrocarbon exploration","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"","keywords":"Imbrication; Geology; Echelon formation; Lithology; Carbonate; Seismology; Anticline; Bedding; Fold (higher-order function); Extensional definition; Hydrocarbon exploration; Extensional fault; Petrology; Sedimentary rock; Structural complexity; Structural geology; Thrust fault; Geomorphology; Paleontology; Tectonics","score_opus":0.014893939719646346,"score_gpt":0.22628295681491262,"score_spread":0.21138901709526628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078560417","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97200686,0.00091218203,0.023981398,0.0020352527,0.00013583676,0.00020132068,0.000016262935,0.000011324241,0.00069956755],"genre_scores_gemma":[0.9992935,0.000040501967,0.00048376145,0.000047019046,0.000065775705,0.0000054733355,0.000007809985,0.0000065190025,0.000049612972],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9991464,0.00001932896,0.00041599816,0.000080406186,0.00014885301,0.00018902037],"domain_scores_gemma":[0.99924225,0.000061177736,0.00021256189,0.00010262525,0.00019042693,0.00019095704],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009732595,0.00008221519,0.00012778166,0.00037287292,0.00024913566,0.00009348453,0.00020216245,0.000044178778,0.0000054926586],"category_scores_gemma":[0.00006208413,0.000057991238,0.000063179345,0.00032219288,0.00015746184,0.0005545308,0.00000403002,0.00007902716,0.0000011563515],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053052456,0.000038707294,0.17855494,0.00021965164,0.0003459053,0.0000031140105,0.07354516,0.6827963,0.022088898,0.005996879,0.00023173576,0.03612565],"study_design_scores_gemma":[0.00061814784,0.00034740748,0.5236891,0.00014364655,0.00019888116,0.000048358197,0.022810318,0.44102824,0.0045895707,0.0024970549,0.0035836892,0.00044558613],"about_ca_topic_score_codex":0.012231404,"about_ca_topic_score_gemma":0.6655311,"teacher_disagreement_score":0.6532997,"about_ca_system_score_codex":0.000017282164,"about_ca_system_score_gemma":0.00026768167,"threshold_uncertainty_score":0.99434626},"labels":[],"label_agreement":null},{"id":"W2078891611","doi":"10.1139/e04-031","title":"Late Holocene syngenetic ice-wedge polygons development, Bylot Island, Canadian Arctic Archipelago","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval; Center for Northern Studies","funders":"","keywords":"Geology; Ice wedge; Holocene; Sedimentary rock; Outwash plain; Geomorphology; Geochemistry; Last Glacial Maximum; Glacier; Archipelago; Permafrost; Paleontology; Oceanography","score_opus":0.027020760554935245,"score_gpt":0.2307331322480768,"score_spread":0.20371237169314155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078891611","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9863397,0.0026421037,0.000016035472,0.0024848105,0.0006781572,0.00010348913,0.000038749888,0.0000046386413,0.007692318],"genre_scores_gemma":[0.9975619,0.000058511367,0.001343273,0.00062127295,0.00009373442,4.0775546e-7,0.000012702386,0.000003414257,0.00030479828],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976678,0.00013433569,0.00039633195,0.00026428315,0.00030854772,0.0012287367],"domain_scores_gemma":[0.9973232,0.00013626997,0.00014565607,0.00014337547,0.00015645,0.002095047],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011896593,0.00017625245,0.00026403065,0.0010628765,0.0012317066,0.00015174094,0.00082679273,0.00013096002,0.0024521635],"category_scores_gemma":[0.00023087622,0.00014393806,0.00007513805,0.00073695544,0.0012359751,0.00027932102,0.0000069998005,0.00047564702,0.0006282817],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000068745903,0.0000034859272,0.9945478,0.000007635638,0.000021826532,0.0005020491,0.0006919619,0.0032086421,0.000001912585,0.00010767416,0.00003228918,0.0008678628],"study_design_scores_gemma":[0.00033720396,0.00023987437,0.99295014,0.000059520407,0.000012607218,0.0011467045,0.00023470451,0.00007115012,0.00008008488,0.0018468627,0.002829564,0.0001915613],"about_ca_topic_score_codex":0.376526,"about_ca_topic_score_gemma":0.9984812,"teacher_disagreement_score":0.6219552,"about_ca_system_score_codex":0.000004697547,"about_ca_system_score_gemma":0.013418727,"threshold_uncertainty_score":0.99845976},"labels":[],"label_agreement":null},{"id":"W2078949619","doi":"10.1139/e00-105","title":"Timing and tectonic setting of Stikine Terrane magmatism, Babine-Takla lakes area, central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Government of British Columbia","funders":"McMaster University","keywords":"Geology; Geochemistry; Terrane; Pluton; Quartz monzonite; Volcanic rock; Volcanic arc; Porphyritic; Andesite; Subduction; Paleontology; Volcano; Tectonics; Quartz","score_opus":0.014082677793586757,"score_gpt":0.18154589498623078,"score_spread":0.167463217192644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078949619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944635,0.0018360935,0.000016814303,0.0006517034,0.00010861728,0.00003769564,0.00003733833,0.0000033034955,0.0028449234],"genre_scores_gemma":[0.9983064,0.00010779034,0.0012076014,0.00012873342,0.00006370669,7.450505e-8,0.000004572519,0.0000010023871,0.00018010418],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987452,0.000041255214,0.00034943136,0.00016124893,0.00025216973,0.00045067922],"domain_scores_gemma":[0.9989566,0.000109750334,0.00020631656,0.00005325678,0.000089574394,0.0005845081],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004925287,0.00007599047,0.0002544519,0.00010789069,0.00030813614,0.0002806385,0.00026568666,0.000041992742,0.012095255],"category_scores_gemma":[0.0002251571,0.00007301488,0.00007566467,0.0005321243,0.0005179557,0.00025182695,0.0000061477476,0.00014335349,0.0000037856075],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000019817203,0.0000026538157,0.98084116,0.0000058606165,0.000009862771,0.000103670885,0.0000666591,0.00091392593,0.00008134165,0.0000018239095,0.0001376187,0.017833415],"study_design_scores_gemma":[0.0001368919,0.00016980796,0.99299055,0.00008469319,0.00002190183,0.000605458,0.00023213374,0.0029014114,0.000024915847,0.0018435107,0.00088794035,0.000100768695],"about_ca_topic_score_codex":0.29997998,"about_ca_topic_score_gemma":0.97886544,"teacher_disagreement_score":0.67888546,"about_ca_system_score_codex":0.0000012213735,"about_ca_system_score_gemma":0.00024582117,"threshold_uncertainty_score":0.9888078},"labels":[],"label_agreement":null},{"id":"W2079012167","doi":"10.1139/e99-104","title":"The simulated response of the climate system to changes in soil moisture parameterization under paleoclimatic boundary conditions at 6000 years before present","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; University of Toronto","funders":"","keywords":"Climatology; Northern Hemisphere; Paleoclimatology; Evapotranspiration; Anomaly (physics); Climate model; Context (archaeology); Environmental science; Latitude; Parametrization (atmospheric modeling); Geology; Forcing (mathematics); Atmospheric sciences; Climate change; Radiative transfer","score_opus":0.01703922598008667,"score_gpt":0.24494679373114744,"score_spread":0.22790756775106077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079012167","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99442714,0.0005405226,3.890512e-7,0.0038504142,0.00027338628,0.00018985017,0.000062327425,0.0000027810759,0.00065317436],"genre_scores_gemma":[0.99949205,0.000039011524,0.000022162929,0.00018496031,0.000024452364,7.248187e-7,0.0000043022424,0.0000016883229,0.00023062104],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981757,0.00062170747,0.00031125775,0.00013064023,0.00029026507,0.00047042253],"domain_scores_gemma":[0.9988198,0.00054399,0.00014623812,0.00016219761,0.000070997725,0.000256737],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018842757,0.000084882224,0.00017009571,0.00023276056,0.00091813126,0.00008767071,0.00053108664,0.00008271637,0.00066849816],"category_scores_gemma":[0.0001573607,0.000049045615,0.000052889824,0.0007242621,0.0010594437,0.00011638804,0.000010372263,0.00020603942,0.00005159139],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000083422245,0.0000023091104,0.9307003,0.000010372109,0.000008003314,0.000035244535,0.00061925757,0.068312235,0.0000075991074,0.00003230379,0.00002410304,0.0001648174],"study_design_scores_gemma":[0.00013876522,0.00024004196,0.9944222,0.00010131026,0.000008015961,0.00016464012,0.0006878309,0.0032323443,0.000029545894,0.0001532623,0.000768977,0.000053051608],"about_ca_topic_score_codex":0.0020162729,"about_ca_topic_score_gemma":0.7624253,"teacher_disagreement_score":0.76040906,"about_ca_system_score_codex":0.0000031517845,"about_ca_system_score_gemma":0.0007378491,"threshold_uncertainty_score":0.7319586},"labels":[],"label_agreement":null},{"id":"W2079081122","doi":"10.1139/e02-037","title":"Chronology of Devonian to early Carboniferous rifting and igneous activity in southern Magdalen Basin based on U-Pb (zircon) dating","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Saint Mary's University; Geological Survey of Canada; Bedford Institute of Oceanography; Acadia University; Memorial University of Newfoundland","funders":"Board of Research in Nuclear Sciences","keywords":"Geology; Tournaisian; Devonian; Zircon; Terrane; Late Devonian extinction; Carboniferous; Rhyolite; Geochemistry; Volcanic rock; Paleontology; Igneous rock; Structural basin; Volcano","score_opus":0.018231855252456537,"score_gpt":0.18604023445069998,"score_spread":0.16780837919824343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079081122","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99506056,0.00021133694,0.000027170208,0.0013118293,0.000057454236,0.000044964152,0.000026068134,0.000002147227,0.0032584856],"genre_scores_gemma":[0.9981375,0.000003367959,0.001492218,0.00029436394,0.00003728044,1.2307835e-7,4.9330004e-7,0.0000011412491,0.00003354514],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988489,0.0000987072,0.000264286,0.00019811235,0.00020404307,0.0003859261],"domain_scores_gemma":[0.99903786,0.00021335763,0.00015691578,0.00007652619,0.000049901028,0.00046544772],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005797997,0.00010044342,0.00025236743,0.00037972495,0.00014972675,0.0000552445,0.0002696544,0.00005327208,0.002769084],"category_scores_gemma":[0.0003128765,0.00007359791,0.00005167865,0.000565213,0.00034628247,0.00011252383,0.000005951426,0.00018539521,0.000025387615],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000084052135,0.0000068750314,0.97714615,0.000004261207,0.000004214339,0.00006913419,0.00036515063,0.0074677845,0.0004310708,0.000004392281,0.0000033287693,0.01448921],"study_design_scores_gemma":[0.00019750936,0.0008456489,0.97777694,0.00006275406,0.000009450392,0.000034325647,0.00036648347,0.019489296,0.0006659365,0.00030415173,0.000109264074,0.00013824271],"about_ca_topic_score_codex":0.09359944,"about_ca_topic_score_gemma":0.51686865,"teacher_disagreement_score":0.4232692,"about_ca_system_score_codex":0.0000024456133,"about_ca_system_score_gemma":0.0001565982,"threshold_uncertainty_score":0.99814254},"labels":[],"label_agreement":null},{"id":"W2079137925","doi":"10.1139/e05-020","title":"Global correlation of the radiolarian faunal change across the TriassicJurassic boundary","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology; Fauna; Sedimentary rock; Ridge; Biostratigraphy; Carbonate platform; Sedimentation; Facies; Sediment; Biology; Ecology; Structural basin","score_opus":0.029389565073967606,"score_gpt":0.24739714482193062,"score_spread":0.218007579747963,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079137925","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96835905,0.012322354,0.000048795184,0.004591538,0.0014732808,0.00011172686,0.00010078925,0.000002215844,0.012990226],"genre_scores_gemma":[0.9992154,0.000019844501,0.00015773691,0.00026614958,0.00031707928,1.7554095e-7,4.7920474e-7,3.280937e-7,0.000022759497],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987234,0.00017198481,0.0003167912,0.00010666256,0.00031926486,0.0003619148],"domain_scores_gemma":[0.9990944,0.000115630246,0.00034572536,0.0001170799,0.00007028121,0.00025685393],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013485175,0.000089613815,0.00015249582,0.00006391999,0.0012604762,0.00013995642,0.00073068443,0.000073453084,0.0002053493],"category_scores_gemma":[0.000118966374,0.00004564674,0.00014275828,0.00061642384,0.001707565,0.0005869186,0.0000014322679,0.00021186254,0.000004310419],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008610818,0.0000019175145,0.9061637,0.0000010957249,0.000010649772,0.0000052362575,0.0006845588,0.0004962346,0.000001281115,0.00022482136,0.00013188443,0.09226999],"study_design_scores_gemma":[0.00017277237,0.00012562318,0.9923947,0.000024283505,0.000012395577,0.00020359387,0.00044844957,0.001017968,0.000009545664,0.00053816644,0.0049937265,0.000058817845],"about_ca_topic_score_codex":0.009678326,"about_ca_topic_score_gemma":0.7225729,"teacher_disagreement_score":0.7128946,"about_ca_system_score_codex":0.0000025103902,"about_ca_system_score_gemma":0.0010605485,"threshold_uncertainty_score":0.9969163},"labels":[],"label_agreement":null},{"id":"W2079252222","doi":"10.1139/e07-008","title":"Rapid cold water formation and recrystallization of relict bryophyte tufa at the Fall Creek cold springs, Alberta, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Tufa; Calcite; Geology; Recrystallization (geology); Radiocarbon dating; Carbonate; Geochemistry; Diagenesis; Paleontology; Chemistry","score_opus":0.016956055850088428,"score_gpt":0.20227837529650392,"score_spread":0.18532231944641547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079252222","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99290925,0.0013319216,0.000017352915,0.0014239793,0.00029959457,0.00009186072,0.000008472316,8.8608556e-7,0.003916701],"genre_scores_gemma":[0.9988622,0.000108053275,0.00008883822,0.00032315208,0.000035481535,1.1617121e-7,0.000004597562,0.0000011123732,0.0005764382],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998797,0.00009150865,0.00031576594,0.00010436956,0.00026790783,0.00042343832],"domain_scores_gemma":[0.99896,0.00033116844,0.00015857867,0.00007906793,0.00013208164,0.00033909528],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017918593,0.000070812326,0.00013911109,0.0001566629,0.0006225231,0.000052224746,0.00026613683,0.000057371133,0.00067030016],"category_scores_gemma":[0.0001237215,0.00004439203,0.00002746016,0.00022764245,0.00065873546,0.00027945163,0.0000074540885,0.00015094537,0.000008602797],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013534173,9.0957286e-7,0.9984916,0.000009138551,0.000006836508,0.000032153304,0.0002870995,0.00041004986,0.00006638623,0.000055618253,0.00037846973,0.00024820995],"study_design_scores_gemma":[0.00017589475,0.00022629787,0.9442055,0.000026350564,0.000009229713,0.00030492418,0.00034126538,0.00038002836,0.0024997087,0.0000683062,0.051681515,0.0000809844],"about_ca_topic_score_codex":0.8255871,"about_ca_topic_score_gemma":0.9998384,"teacher_disagreement_score":0.1742513,"about_ca_system_score_codex":0.0000021302017,"about_ca_system_score_gemma":0.0009462526,"threshold_uncertainty_score":0.73393166},"labels":[],"label_agreement":null},{"id":"W2079254238","doi":"10.1139/e07-066","title":"Palynostratigraphy and lithostratigraphy of Carboniferous Upper Codroy Group and Barachois Group, southwestern Newfoundland","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada","funders":"","keywords":"Carboniferous; Geology; Lithostratigraphy; Group (periodic table); Pennsylvanian; Paleontology; Coal measures; Paleozoic; Biostratigraphy; Bay; Outcrop; Structural basin; Oceanography","score_opus":0.021353714926253643,"score_gpt":0.21729587860882787,"score_spread":0.19594216368257422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079254238","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9895184,0.008054297,0.000008461985,0.0002570348,0.00017944029,0.00007607209,0.000028668474,0.0000027256845,0.0018749028],"genre_scores_gemma":[0.9986565,0.00043416096,0.00074716564,0.000095799114,0.000043817214,1.9073319e-7,0.0000033635745,0.0000014964094,0.000017486209],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861336,0.0001500138,0.0003412537,0.00020843421,0.0002499331,0.00043697868],"domain_scores_gemma":[0.9987419,0.00024333409,0.00017673602,0.00009151238,0.00007359375,0.0006729118],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0007534437,0.00013299691,0.00029171375,0.00055297505,0.00054745196,0.00006987637,0.00025511207,0.000107053354,0.00017014991],"category_scores_gemma":[0.000059976166,0.000100556375,0.00006635091,0.00042802803,0.0029834488,0.00035578947,0.0000047211743,0.00026198573,0.0000028630907],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015863772,0.0000039364877,0.9986653,0.0000121639405,0.000020479994,0.00017289005,0.0006746046,0.000014293282,0.000011120018,0.00013412256,0.000007340459,0.00026790192],"study_design_scores_gemma":[0.0002762693,0.0008080207,0.99541676,0.000028327877,0.000013992833,0.0021379015,0.00036500258,0.00009709637,0.000007963755,0.00055672164,0.0001850977,0.0001068461],"about_ca_topic_score_codex":0.023224628,"about_ca_topic_score_gemma":0.7559574,"teacher_disagreement_score":0.73273283,"about_ca_system_score_codex":1.757073e-7,"about_ca_system_score_gemma":0.00044113165,"threshold_uncertainty_score":0.9997299},"labels":[],"label_agreement":null},{"id":"W2079340903","doi":"10.1139/e08-050","title":"Arctic vs. North Atlantic water mass exchanges in Fram Strait from Pb isotopes in sedimentsThis article is one of a series of papers published in this Special Issue on the theme <i>Polar Climate Stability Network</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Fonds Québécois de la Recherche sur la Nature et les Technologies","keywords":"Geology; Radiogenic nuclide; Oceanography; Arctic; Geochemistry; Trace element; Provenance; Mantle (geology)","score_opus":0.02778204316324777,"score_gpt":0.20666273839640137,"score_spread":0.17888069523315359,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079340903","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9925673,0.00030601383,1.2424742e-7,0.0043600206,0.00025396212,0.00016330605,0.000049835777,0.0000012099197,0.0022982007],"genre_scores_gemma":[0.9990914,0.00022392442,0.0001585572,0.0003307434,0.0001631458,8.0923314e-7,0.000006172502,0.0000017766976,0.000023471963],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976595,0.00048217602,0.00055840483,0.00022096017,0.0003832555,0.00069567177],"domain_scores_gemma":[0.9989309,0.0004569364,0.00017241936,0.00015884021,0.00007839534,0.00020252865],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0024592334,0.00012291112,0.00038540162,0.00034149262,0.00020162668,0.000039674902,0.0005285843,0.00009466213,0.036560107],"category_scores_gemma":[0.00023246011,0.000075976,0.00005975665,0.00068197644,0.0014142917,0.0004343073,0.000012913935,0.00045089156,0.000024747213],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001506473,0.000022265589,0.99446106,0.000016327102,0.000011340212,0.000098007746,0.0042265607,0.00083867816,0.000031146046,0.000013850402,0.00006688688,0.00006323805],"study_design_scores_gemma":[0.0003119241,0.00038517016,0.9960142,0.00008534061,0.000004737872,0.000019534886,0.000852418,0.00015225964,0.0009104263,0.00068023463,0.0004999096,0.00008387575],"about_ca_topic_score_codex":0.051044196,"about_ca_topic_score_gemma":0.8910083,"teacher_disagreement_score":0.83996415,"about_ca_system_score_codex":0.0000027006436,"about_ca_system_score_gemma":0.00049725425,"threshold_uncertainty_score":0.9643206},"labels":[],"label_agreement":null},{"id":"W2079469534","doi":"10.1139/e02-070","title":"Geochemistry of the late Archean Banting Group, Yellowknife greenstone belt, Slave Province, Canada: simultaneous melting of the upper mantle and juvenile mafic crust","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Northwest Territories; Carleton University","funders":"University of Ottawa","keywords":"Felsic; Geology; Geochemistry; Mafic; Volcanic rock; Archean; Greenstone belt; Basalt; Igneous rock; Petrology; Volcano","score_opus":0.010824938531063057,"score_gpt":0.16271576219481176,"score_spread":0.1518908236637487,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079469534","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936696,0.0012315625,0.0000011331831,0.0013562558,0.00012501552,0.00005363059,0.00005082657,0.0000011704749,0.0035107855],"genre_scores_gemma":[0.999006,0.000017006298,0.00015616133,0.00016656856,0.00004644244,6.2805846e-8,9.886994e-7,0.0000012780037,0.0006054919],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861026,0.000063949636,0.00040288147,0.00014499344,0.00041117496,0.00036673667],"domain_scores_gemma":[0.99884295,0.00024680555,0.00039309336,0.0001270051,0.00009985814,0.00029028088],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000466969,0.00010964519,0.00024222322,0.000057841444,0.00042380908,0.000034189685,0.0005723327,0.0000445896,0.001490522],"category_scores_gemma":[0.0004219509,0.000056543966,0.00011153525,0.00046524455,0.0010411006,0.00008456849,0.000024934456,0.00023680876,0.000001228442],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026293515,0.00000520502,0.9905766,0.000021844697,0.00001673928,0.000029498078,0.00017853512,0.004309445,0.00089426537,0.000011778142,0.000084615924,0.0038688155],"study_design_scores_gemma":[0.00018693853,0.00011511474,0.95833004,0.0001603664,0.0000643346,0.00018308658,0.0008885669,0.033394977,0.004531832,0.0005926297,0.0013556173,0.0001964761],"about_ca_topic_score_codex":0.64612204,"about_ca_topic_score_gemma":0.9834028,"teacher_disagreement_score":0.33728075,"about_ca_system_score_codex":0.000003703312,"about_ca_system_score_gemma":0.0007240411,"threshold_uncertainty_score":0.99942225},"labels":[],"label_agreement":null},{"id":"W2079564903","doi":"10.1139/e02-065","title":"A new baphetid (stem tetrapod) from the Upper Carboniferous of Tyne and Wear, U.K., and the evolution of the tetrapod occiput","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Natural Environment Research Council","keywords":"Tetrapod (structure); Geology; Anatomy; Skull; Occiput; Carboniferous; Stapes; Paleontology; Biology; Middle ear","score_opus":0.010701201837360941,"score_gpt":0.1794306999207299,"score_spread":0.16872949808336896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079564903","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96622473,0.028244548,0.000021511973,0.0021640058,0.0005224511,0.00008449747,0.000036103687,9.3722423e-7,0.002701236],"genre_scores_gemma":[0.9993125,0.00016648814,0.00025194132,0.00013807895,0.00005190809,9.285521e-8,3.5233268e-7,7.699273e-7,0.0000778773],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886173,0.0003391342,0.00027057156,0.000121701305,0.00017313684,0.00023375226],"domain_scores_gemma":[0.99892515,0.00049131503,0.00022414011,0.000118452546,0.000052315274,0.00018862632],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010632679,0.00008376513,0.00018691832,0.000080756035,0.00043842164,0.000025091067,0.00037388684,0.000066488356,0.00018974385],"category_scores_gemma":[0.00019083459,0.00003673393,0.000063908294,0.00033189304,0.002543035,0.00013150209,0.0000051139514,0.00018268752,0.0000014076261],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001753736,0.0000013165511,0.9960875,0.0000015259284,0.000018444047,0.0000020120483,0.00051008305,0.0001275007,0.000022264325,0.0018061119,0.00008574462,0.0013199542],"study_design_scores_gemma":[0.00033826596,0.00014119601,0.9921234,0.000029033634,0.00002622558,0.00023588073,0.0013857748,0.00020451933,0.000033894503,0.0036316095,0.0018018329,0.000048326874],"about_ca_topic_score_codex":0.057910606,"about_ca_topic_score_gemma":0.50556064,"teacher_disagreement_score":0.44765002,"about_ca_system_score_codex":0.0000021623289,"about_ca_system_score_gemma":0.0013363853,"threshold_uncertainty_score":0.9483628},"labels":[],"label_agreement":null},{"id":"W2079701702","doi":"10.1139/e05-094","title":"The record of Glacial Lake Champagne in Kusawa Lake, southwestern Yukon Territory","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Glacier; Glacial period; Glacial lake; Shelf ice; Facies; Deglaciation; Sedimentary rock; Geomorphology; Pleistocene; Structural basin; Oceanography; Paleontology; Arctic","score_opus":0.023508511165700623,"score_gpt":0.2355978715725823,"score_spread":0.21208936040688167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079701702","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9872315,0.0015645461,0.000001956709,0.0022987744,0.00067500956,0.00005859742,0.0000226988,0.0000016141706,0.008145302],"genre_scores_gemma":[0.9991152,0.00008894099,0.00018939178,0.00013569393,0.00019665413,1.9433733e-7,0.0000021409896,0.0000010957535,0.0002706803],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985222,0.00019223386,0.0003890557,0.00012701073,0.000250658,0.00051882735],"domain_scores_gemma":[0.9989932,0.00030636945,0.00018824193,0.0000995413,0.00007450515,0.00033814984],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019674185,0.00008473663,0.00018978944,0.00034578732,0.00041121853,0.000058662616,0.00060224545,0.00008229887,0.0017579937],"category_scores_gemma":[0.00016623906,0.000055103006,0.000061058636,0.0003442395,0.0013332521,0.00028122892,0.000005563345,0.0003169666,0.00006981383],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017472963,0.0000030487515,0.99302226,0.0000026661203,0.0000046655896,0.000048390262,0.00034392378,0.00046080863,0.0000010232152,0.000026975773,0.000071149,0.005997604],"study_design_scores_gemma":[0.00017930251,0.00023983324,0.9571339,0.000024881996,0.000002809854,0.00014100235,0.00032624992,0.00026557693,0.000015902364,0.00026185927,0.041345775,0.00006290898],"about_ca_topic_score_codex":0.004214656,"about_ca_topic_score_gemma":0.99626553,"teacher_disagreement_score":0.9920509,"about_ca_system_score_codex":4.5258375e-7,"about_ca_system_score_gemma":0.0012098479,"threshold_uncertainty_score":0.9991545},"labels":[],"label_agreement":null},{"id":"W2079742949","doi":"10.1139/e05-072","title":"Ice-wedge casts in Late Wisconsinan glaciofluvial deposits, southern Ontario, Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Baosteel-Australia Joint Research and Development Centre","keywords":"Geology; Ice wedge; Permafrost; Geomorphology; Wedge (geometry); Thermokarst; Physical geography; Geochemistry; Oceanography; Geometry","score_opus":0.019660780809920095,"score_gpt":0.2120252478236744,"score_spread":0.19236446701375431,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079742949","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987381,0.00130416,0.0000011104738,0.0021285282,0.0005202909,0.00006215452,0.000014518149,0.0000017533089,0.00858653],"genre_scores_gemma":[0.9977709,0.000008525649,0.00035519453,0.00046649761,0.0000947961,1.2380266e-7,0.0000027133897,0.000001486266,0.0012997302],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983464,0.00013837968,0.00033935375,0.00017785413,0.0002820874,0.0007159163],"domain_scores_gemma":[0.9988916,0.00013562557,0.00012594047,0.00008903074,0.00007533183,0.0006824704],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00086629967,0.00011685454,0.00021966312,0.00035182823,0.00042570996,0.00007677973,0.00048437278,0.00008276279,0.0037342343],"category_scores_gemma":[0.00008213715,0.00009449477,0.00004298715,0.00036913098,0.00057394936,0.00030774652,0.000005150427,0.0004399473,0.00013408676],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013239159,0.0000024493208,0.99272925,0.0000020581272,0.000006545753,0.0006238682,0.0011326508,0.0042491923,0.0000013407418,0.000012219986,0.00017197587,0.0010551863],"study_design_scores_gemma":[0.00026377456,0.00011133597,0.98979294,0.000025418276,0.000005164391,0.0005765466,0.00036497,0.00052820804,0.000030471845,0.00011965462,0.008062432,0.000119104465],"about_ca_topic_score_codex":0.9884924,"about_ca_topic_score_gemma":0.9999992,"teacher_disagreement_score":0.012688614,"about_ca_system_score_codex":0.00000546445,"about_ca_system_score_gemma":0.0126940785,"threshold_uncertainty_score":0.99717647},"labels":[],"label_agreement":null},{"id":"W2080047436","doi":"10.1139/e03-013","title":"The CambrianOrdovician successions along the ancient continental margin of Laurentia recent advances","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"GDG Environnement; Institut National de la Recherche Scientifique; Geological Survey of Canada","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Laurentia; Ordovician; Geology; Paleontology; Margin (machine learning); Continental margin; Tectonics","score_opus":0.014816568810814282,"score_gpt":0.22532681510090175,"score_spread":0.21051024629008747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080047436","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8258616,0.120183885,0.000025666379,0.0020547416,0.0022364606,0.000116817275,0.00003775301,0.0000024129495,0.04948068],"genre_scores_gemma":[0.99873245,0.00079225196,0.00026057218,0.000110333596,0.000047962003,2.4789895e-7,5.632271e-7,5.150117e-7,0.000055127868],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99848163,0.00023255179,0.00039205817,0.00012482044,0.00032268406,0.00044623413],"domain_scores_gemma":[0.9987599,0.00028243472,0.00034690034,0.00012410161,0.00012701054,0.00035964994],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0017384528,0.000100415644,0.00015968713,0.0001379913,0.0015341804,0.0001297216,0.0006463186,0.000039580405,0.00045461368],"category_scores_gemma":[0.00030006203,0.000049498984,0.000101921745,0.0005684874,0.0016757295,0.00034148502,9.595177e-7,0.00019887488,0.0000036851118],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000067215706,0.0000034471427,0.9651787,0.000001887413,0.000011989385,0.00001799735,0.00018313628,0.0001644008,0.000011682182,0.0010608401,0.0003359214,0.033023257],"study_design_scores_gemma":[0.00011385238,0.00016554262,0.904777,0.000029311183,0.00001167836,0.00010765848,0.0014271168,0.00004827751,0.0001047983,0.00038015755,0.092769064,0.00006553019],"about_ca_topic_score_codex":0.0047160494,"about_ca_topic_score_gemma":0.8695511,"teacher_disagreement_score":0.8648351,"about_ca_system_score_codex":0.0000010258793,"about_ca_system_score_gemma":0.001377598,"threshold_uncertainty_score":0.9997657},"labels":[],"label_agreement":null},{"id":"W2080089730","doi":"10.1139/e03-004","title":"Structural evolution of the Hemlo greenstone belt in the vicinity of the world-class Hemlo gold deposit","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Sinistral and dextral; Greenstone belt; Shear zone; Dike; Geochemistry; Metamorphism; Shear (geology); Seismology; Transpression; Mylonite; Archean; Fault (geology); Petrology; Tectonics","score_opus":0.014042121818303725,"score_gpt":0.18902847960006494,"score_spread":0.17498635778176122,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080089730","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.991271,0.0011638594,0.0000014887678,0.0020606297,0.00022598827,0.000064497064,0.000013472556,6.156773e-7,0.0051984168],"genre_scores_gemma":[0.99949247,0.000006078563,0.0001037658,0.00027953796,0.000027745898,8.9748674e-8,3.9224255e-7,5.2383825e-7,0.000089393136],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99853563,0.00027193455,0.0003611068,0.00011165665,0.00043495366,0.0002847217],"domain_scores_gemma":[0.9991216,0.00018208694,0.00029315785,0.00015045976,0.00009951425,0.0001531475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009816627,0.000086598964,0.00018451532,0.00012813689,0.00028169926,0.00003310565,0.0008713086,0.000035487792,0.0007660069],"category_scores_gemma":[0.000330362,0.000034305765,0.00015808952,0.0017566651,0.0010565736,0.0001308153,0.000008257579,0.00025599566,0.0000022625397],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000030254528,0.0000029970797,0.99518716,0.0000029284977,0.000005945241,0.0000029953756,0.00012200114,0.0034125105,0.00011612661,0.00048370936,0.00003770346,0.0006228655],"study_design_scores_gemma":[0.00008147867,0.00006735227,0.9905634,0.00003012089,0.000018619712,0.000055007415,0.00038855514,0.00057160476,0.0008503783,0.007034079,0.00028817958,0.000051259987],"about_ca_topic_score_codex":0.09471025,"about_ca_topic_score_gemma":0.9232423,"teacher_disagreement_score":0.82853204,"about_ca_system_score_codex":0.0000038903586,"about_ca_system_score_gemma":0.0004399309,"threshold_uncertainty_score":0.9113181},"labels":[],"label_agreement":null},{"id":"W2080122259","doi":"10.1139/e04-043","title":"Redescription of <i>Ankylosaurus magniventris </i>Brown 1908 (Ankylosauridae) from the Upper Cretaceous of the Western Interior of North America","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":94,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Core Research for Evolutional Science and Technology; American Museum of Natural History","keywords":"Geology; Paleontology; Cretaceous; Armour; Skull; Archaeology; Geography","score_opus":0.014299650992687506,"score_gpt":0.19494795365093381,"score_spread":0.1806483026582463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080122259","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99183357,0.0042445445,0.000035238307,0.0021221514,0.0006832841,0.000081118946,0.0003572915,0.0000013531699,0.00064145616],"genre_scores_gemma":[0.9990566,0.00012895385,0.00039090659,0.00030628065,0.000076104356,1.3490052e-7,0.000007106075,0.0000011283313,0.0000328179],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986724,0.00018052207,0.0004889965,0.00013627874,0.00024891642,0.00027288342],"domain_scores_gemma":[0.9987538,0.00016484392,0.00060465746,0.00017099794,0.00013768082,0.00016801899],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038606738,0.00010058775,0.0002644998,0.0001257482,0.00023153394,0.000014387838,0.0008065181,0.00005020978,0.0004798461],"category_scores_gemma":[0.00016215371,0.00005522508,0.00014848394,0.00042758786,0.0024276334,0.0002181778,0.000010413411,0.00018545937,0.000008306399],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003316602,0.0000055636947,0.99466825,0.0000043312225,0.000023896282,0.000011754934,0.00064230745,0.0015404907,0.000117594784,0.000013591246,0.000076505574,0.0028625536],"study_design_scores_gemma":[0.00018639932,0.000405715,0.9930666,0.00007624776,0.00002914022,0.000102989216,0.00034124326,0.00004704723,0.0002785886,0.00039699595,0.0050083348,0.000060671155],"about_ca_topic_score_codex":0.05439604,"about_ca_topic_score_gemma":0.56842816,"teacher_disagreement_score":0.5140321,"about_ca_system_score_codex":0.0000034733018,"about_ca_system_score_gemma":0.0011207993,"threshold_uncertainty_score":0.95190084},"labels":[],"label_agreement":null},{"id":"W2080274563","doi":"10.1139/e99-114","title":"Hurricanes Pauline and Nora rainwater chemical composition","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Rainwater harvesting; Chemical composition; Hydrology (agriculture); Environmental science; Sampling (signal processing); Geology; Seawater; Oceanography; Chemistry","score_opus":0.010418890608790624,"score_gpt":0.19170776712568668,"score_spread":0.18128887651689607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080274563","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9922366,0.00057800906,0.0000062022023,0.00081735133,0.00008293915,0.000022660814,0.000015235186,0.0000027482738,0.006238243],"genre_scores_gemma":[0.9978209,0.00003118382,0.0014093476,0.0003197673,0.0001631061,4.2262386e-8,0.0000041270214,8.919164e-7,0.00025061262],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993101,0.000019383835,0.00017533058,0.00010945585,0.00014750642,0.00023823243],"domain_scores_gemma":[0.99934196,0.00004052672,0.00006091247,0.000042580254,0.00003144878,0.00048255455],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002458078,0.00007219822,0.000116004936,0.000015573261,0.00023345056,0.00012250898,0.00017516664,0.000033424236,0.008174041],"category_scores_gemma":[0.000014814493,0.000052198047,0.000031748204,0.00018298051,0.0004884168,0.00025687984,0.0000013182791,0.000099765224,0.0000312401],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037592563,0.000010639196,0.91996807,0.00001625859,0.000019472775,0.00031860397,0.00065421796,0.003297909,0.0046082838,0.000024550789,0.00083959574,0.07020478],"study_design_scores_gemma":[0.0011441394,0.0007135265,0.8910301,0.00021888918,0.000052987976,0.002730634,0.00088372896,0.0042002345,0.016646782,0.0014535829,0.08011734,0.0008080852],"about_ca_topic_score_codex":0.0029133658,"about_ca_topic_score_gemma":0.008258725,"teacher_disagreement_score":0.07927775,"about_ca_system_score_codex":7.250248e-7,"about_ca_system_score_gemma":0.00025579613,"threshold_uncertainty_score":0.99273264},"labels":[],"label_agreement":null},{"id":"W2080479546","doi":"10.1139/e00-087","title":"Age, chemo- and biostratigraphy of Haiti spherule-rich deposits: a multi-event KT scenario","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft; National Science Foundation","keywords":"Geology; Unconformity; Outcrop; Basalt; Anomaly (physics); Volcano; Paleontology; Geochemistry; Escarpment; Platinum group; Biostratigraphy; Chronostratigraphy; Sedimentary rock; Platinum; Chemistry","score_opus":0.021078901752707345,"score_gpt":0.20688292403661407,"score_spread":0.18580402228390672,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080479546","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924459,0.0029251208,0.00005042122,0.00076385867,0.00009547432,0.000040734194,0.000012769501,0.0000025223762,0.0036631941],"genre_scores_gemma":[0.9962108,0.00012569012,0.003304523,0.00019179597,0.000044117205,8.0357715e-8,0.0000023521714,7.7973704e-7,0.00011985566],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988228,0.000042510976,0.00034933604,0.0001708001,0.00025719014,0.00035735333],"domain_scores_gemma":[0.9988816,0.00007102264,0.00019367607,0.00006879472,0.00010436644,0.0006805608],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041770883,0.00011016601,0.00024549945,0.00022172615,0.00022656498,0.00009428779,0.0003140527,0.00005249115,0.001844695],"category_scores_gemma":[0.000117899086,0.00007238627,0.0001057061,0.00084261486,0.00076172,0.00020965496,0.0000050965723,0.00014049414,0.000009598478],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005527905,0.000009352246,0.99454737,0.000005103924,0.000017323797,0.000112637754,0.000095384654,0.00058061146,0.00019017604,0.00002179351,0.000031086714,0.0043836087],"study_design_scores_gemma":[0.0001790311,0.0002961689,0.9951715,0.000036295074,0.0000259147,0.00018532545,0.00027383468,0.0009214461,0.0007460965,0.0010794667,0.0009703582,0.00011457404],"about_ca_topic_score_codex":0.031348273,"about_ca_topic_score_gemma":0.7292906,"teacher_disagreement_score":0.6979423,"about_ca_system_score_codex":7.448987e-7,"about_ca_system_score_gemma":0.00029358608,"threshold_uncertainty_score":0.9990678},"labels":[],"label_agreement":null},{"id":"W2080588529","doi":"10.1139/e03-101","title":"A reappraisal of the ornithischian dinosaur <i>Amtosaurus magnus</i> Kurzanov and Tumanova 1978, with comments on the status of <i>A. archibaldi</i> Averianov 2002","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Nomen dubium; Holotype; Geology; Paleontology; Genus; Autapomorphy; Taxon; Zoology; Biology","score_opus":0.01727440543204066,"score_gpt":0.20565293247762773,"score_spread":0.18837852704558705,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080588529","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97840714,0.0011009984,0.0000068251657,0.0035311922,0.00042498807,0.00011330547,0.00016192206,0.000001718273,0.01625192],"genre_scores_gemma":[0.99861515,0.000077154866,0.00032625778,0.00087909476,0.0000473118,2.4177993e-7,0.000001976455,0.0000013542577,0.00005143907],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985423,0.00017051274,0.00032766792,0.00015514286,0.00028279447,0.0005215984],"domain_scores_gemma":[0.9987823,0.00024131073,0.00036939606,0.00015750571,0.0000807201,0.00036881582],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00058318797,0.00012669605,0.00022277408,0.00016025602,0.00050372904,0.000026177202,0.0005391295,0.000056855075,0.0003688499],"category_scores_gemma":[0.00016212801,0.00006143215,0.000056660312,0.0004373432,0.0030620985,0.00017156011,0.000008826002,0.0002708177,0.0000070524707],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007937272,0.000012635541,0.99488735,0.000006470874,0.000026602891,0.000023665581,0.0004635688,0.0013590773,0.000074302305,0.0020107408,0.00027103123,0.0007851962],"study_design_scores_gemma":[0.00043211054,0.0010833127,0.98520523,0.000098305965,0.000017724513,0.00033677198,0.0004327116,0.000031036117,0.00021887715,0.0005171176,0.011539708,0.00008708254],"about_ca_topic_score_codex":0.015604772,"about_ca_topic_score_gemma":0.48583972,"teacher_disagreement_score":0.47023496,"about_ca_system_score_codex":0.0000019975785,"about_ca_system_score_gemma":0.0017819166,"threshold_uncertainty_score":0.999651},"labels":[],"label_agreement":null},{"id":"W2080614096","doi":"10.1139/e08-019","title":"The origin of the Variscan upper allochthons in the Ortegal Complex, northwestern Iberia: Sm–Nd isotopic constraints on the closure of the Rheic Ocean","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"Ophiolite; Geology; Paleozoic; Devonian; Metamorphism; Geochemistry; Massif; Orogeny; Ordovician; Mafic; Fibrous joint; Paleontology; Protolith; Petrology; Tectonics","score_opus":0.031416265156654716,"score_gpt":0.20576487470285404,"score_spread":0.17434860954619932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080614096","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97938097,0.00031229536,7.332746e-7,0.015643328,0.00024243022,0.00012907402,0.000047271576,9.369114e-7,0.004242949],"genre_scores_gemma":[0.99853027,0.000029903244,0.0000208649,0.001216664,0.000063192834,2.4523845e-7,0.0000010248415,0.0000010125516,0.00013682248],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99806243,0.00038720807,0.00043928105,0.00014443102,0.00058639265,0.0003802655],"domain_scores_gemma":[0.9984484,0.0006771482,0.00034056173,0.00027351239,0.00010128726,0.00015910508],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013313018,0.00012617654,0.00021619748,0.00006653378,0.0010303406,0.0000722289,0.0018051807,0.00004764737,0.0015423936],"category_scores_gemma":[0.00022531458,0.000038376034,0.00022942829,0.00081980077,0.0038819243,0.00008172628,0.000017197684,0.00040634788,0.00000673571],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004738143,0.00000800555,0.99685746,0.0000014651694,0.000018545374,0.0000096934455,0.00065102923,0.0011325574,0.000013415764,0.00046774544,0.00041924394,0.00041612575],"study_design_scores_gemma":[0.000097344375,0.000118618445,0.9915975,0.000026942073,0.00002009793,0.00012816767,0.0011602985,0.00021183837,0.00006747738,0.0025571785,0.0039542955,0.000060259255],"about_ca_topic_score_codex":0.029349588,"about_ca_topic_score_gemma":0.6065919,"teacher_disagreement_score":0.5772423,"about_ca_system_score_codex":0.0000021997748,"about_ca_system_score_gemma":0.00076539017,"threshold_uncertainty_score":0.99937034},"labels":[],"label_agreement":null},{"id":"W2080639740","doi":"10.1139/e02-074","title":"Late Archaean clastic sedimentary rocks (Shamvaian Group) of the Zimbabwe craton: first observations from the Bindura-Shamva greenstone belt","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Deutscher Akademischer Austauschdienst","keywords":"Geology; Conglomerate; Clastic rock; Sedimentary rock; Foreland basin; Archean; Siliciclastic; Facies; Geochemistry; Geomorphology; Paleontology; Petrology; Structural basin","score_opus":0.04596071138450371,"score_gpt":0.1917025786962699,"score_spread":0.1457418673117662,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080639740","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98307836,0.0021163523,0.000042158237,0.0121920705,0.000584778,0.00009656251,0.00019871801,0.0000037671043,0.001687217],"genre_scores_gemma":[0.9979588,0.00008514358,0.00037207804,0.0013080563,0.00013852252,3.2717168e-7,0.000010731871,0.0000015493922,0.00012482368],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986454,0.00008361222,0.00040522165,0.00013245933,0.0003908844,0.00034241387],"domain_scores_gemma":[0.998703,0.00039332936,0.0002993986,0.00015859069,0.00011848897,0.0003272156],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046441075,0.00011629494,0.0001602909,0.00011315886,0.0013112731,0.00012258958,0.00091775024,0.000051121766,0.004583998],"category_scores_gemma":[0.00018781562,0.000058806345,0.000097550685,0.0008623788,0.0009143673,0.00049547356,0.000014599472,0.00025887467,0.000036146066],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002267199,0.000005826887,0.9863106,0.0000042248857,0.00001376203,0.000007931268,0.0008338031,0.009622843,0.000004118928,0.0000572768,0.0009318702,0.0022054976],"study_design_scores_gemma":[0.0001226955,0.00019358734,0.9806639,0.00006711745,0.000020195595,0.00003778186,0.0005350448,0.0056451396,0.00001729927,0.00163675,0.010970402,0.00009009981],"about_ca_topic_score_codex":0.08878393,"about_ca_topic_score_gemma":0.84688616,"teacher_disagreement_score":0.75810224,"about_ca_system_score_codex":0.0000022169702,"about_ca_system_score_gemma":0.00024988028,"threshold_uncertainty_score":0.9999889},"labels":[],"label_agreement":null},{"id":"W2081205386","doi":"10.1139/e08-027","title":"Late Pleistocene northward-dispersing Bison antiquus from the Bighill Creek Formation, Gallelli Gravel Pit, Alberta, Canada, and the fate of Bison occidentalis","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Pleistocene-Era Hominins and Archaeology","field":"Social Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Douglas College; University of Calgary","funders":"Luonnontieteiden ja Tekniikan Tutkimuksen Toimikunta; Natural Environment Research Council; Royal Society","keywords":"Beringia; Bison bison; Pleistocene; Geology; Biological dispersal; Younger Dryas; Paleontology; Archaeology; Geography; Glacial period; Ecology; Population; Biology","score_opus":0.024224678726643214,"score_gpt":0.23348789982861642,"score_spread":0.2092632211019732,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081205386","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987867,0.0012805667,0.00003865462,0.009136713,0.00042422366,0.00013337148,0.00005056049,0.0000018607458,0.0010670692],"genre_scores_gemma":[0.9982185,0.0005636134,0.00023980653,0.0006238246,0.00014722436,8.2580215e-7,0.0000020124905,0.0000046341706,0.00019955533],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99818474,0.0002745115,0.00044778007,0.0001497703,0.0004911978,0.00045200982],"domain_scores_gemma":[0.9982893,0.00052978273,0.0004524594,0.000121298326,0.00019333397,0.00041381485],"candidate_categories":["sts"],"consensus_categories":["sts"],"category_scores_codex":[0.0011425775,0.000113692535,0.00027847823,0.00013112163,0.002369429,0.00009814497,0.00066053576,0.000050012153,0.00008418471],"category_scores_gemma":[0.00034706053,0.000071965216,0.00008527336,0.0004716086,0.0043105106,0.00039682738,0.000026218215,0.00017746203,0.0000011061437],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024818106,0.000004847115,0.9660419,0.0000026113173,0.00002576934,0.00005002696,0.03053017,0.00022225578,0.000024932673,0.0011910596,0.0011981628,0.0006834113],"study_design_scores_gemma":[0.0005392547,0.0000964416,0.97909063,0.000054622993,0.000023692235,0.000086619686,0.006208237,0.00032633878,0.00013666575,0.00076329353,0.012538979,0.00013519639],"about_ca_topic_score_codex":0.99114245,"about_ca_topic_score_gemma":0.9999579,"teacher_disagreement_score":0.024321932,"about_ca_system_score_codex":0.000033568776,"about_ca_system_score_gemma":0.00426686,"threshold_uncertainty_score":0.9989293},"labels":[],"label_agreement":null},{"id":"W2081206520","doi":"10.1139/e00-085","title":"U-Pb ages of granitoid rocks in the northwestern Makkovik Province, Labrador: evidence for 175 million years of episodic synorogenic and postorogenic plutonism","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University; Acadia University; Memorial University of Newfoundland","funders":"","keywords":"Plutonism; Geology; Terrane; Pluton; Geochemistry; Orogeny; Zircon; Crust; Batholith; Mafic; Continental crust; Archean; Isochron; Paleontology; Tectonics","score_opus":0.02850550986679434,"score_gpt":0.22463054194602985,"score_spread":0.1961250320792355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081206520","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9902233,0.008869656,0.0000171921,0.000599821,0.00006796354,0.00011478048,0.00003396602,0.0000011245505,0.0000722228],"genre_scores_gemma":[0.99901587,0.00045193502,0.00034553825,0.00012435162,0.000033982633,4.1065275e-7,0.000002625853,0.0000010159862,0.000024258969],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99877834,0.000082102655,0.00038973495,0.00015877407,0.00029196552,0.00029907704],"domain_scores_gemma":[0.9989157,0.0004186066,0.00026254987,0.000093039234,0.00009140577,0.00021874347],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009374552,0.000089790075,0.0002438654,0.00025233912,0.00012786464,0.000044337976,0.0005009548,0.00004780074,0.00021672176],"category_scores_gemma":[0.00021612298,0.000056542616,0.00012074626,0.0005764494,0.00058028,0.00024824962,0.0000066355624,0.00011459343,0.000002586866],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020614521,0.0000069387474,0.9887785,0.000016969756,0.000010872995,0.000040783892,0.00032471863,0.00065676565,0.00024573578,0.00001155266,0.0000102140575,0.009876374],"study_design_scores_gemma":[0.00016898029,0.00054240937,0.99576294,0.00008879089,0.000034102926,0.00014177132,0.0004754498,0.00038418447,0.0002979644,0.0013988711,0.0006198164,0.000084686304],"about_ca_topic_score_codex":0.057965558,"about_ca_topic_score_gemma":0.7258423,"teacher_disagreement_score":0.6678767,"about_ca_system_score_codex":0.0000016435246,"about_ca_system_score_gemma":0.00038688094,"threshold_uncertainty_score":0.9483075},"labels":[],"label_agreement":null},{"id":"W2081222747","doi":"10.1139/e03-040","title":"Distinguishing between Archean and Paleoproterozoic tectonism, and evolution of the Isortoq fault zone, Eqe Bay area, north-central Baffin Island, Canada","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"ARC Resources (Canada); University of Regina","funders":"","keywords":"Geology; Plutonism; Archean; Metamorphism; Geochemistry; Metamorphic rock; Felsic; Gneiss; Greenstone belt; Geochronology; Petrology; Paleontology; Volcanism; Mafic; Tectonics","score_opus":0.012205152632090066,"score_gpt":0.16982545943225438,"score_spread":0.1576203068001643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081222747","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99710596,0.0011744141,0.000055340974,0.0005817772,0.00011967962,0.00005428128,0.00006797599,0.0000010798124,0.000839474],"genre_scores_gemma":[0.9995693,0.0000124811795,0.00026755568,0.00007430935,0.000040038307,9.0692595e-8,0.0000021555868,7.917811e-7,0.00003326803],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987591,0.00009113512,0.00028884917,0.00016171955,0.00030406873,0.00039511945],"domain_scores_gemma":[0.9989806,0.00014670711,0.00019921134,0.00007008661,0.00007566288,0.000527769],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000443423,0.00010236801,0.00020915599,0.00008510213,0.0004291818,0.00007798984,0.00025705912,0.000035964982,0.00038811838],"category_scores_gemma":[0.00048414362,0.00005901499,0.000050877472,0.00044124608,0.0005983209,0.00012219393,0.000007389656,0.00020227248,4.1511345e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000014428863,0.0000011536206,0.99731165,0.000005703474,0.000009095917,0.000009684597,0.00008488535,0.0006497437,0.000007946462,0.000024301906,0.000016427939,0.0018779786],"study_design_scores_gemma":[0.000097639175,0.00007718488,0.9968788,0.00002786347,0.00002286578,0.000041854255,0.00027924063,0.00056225114,0.00006289553,0.0011604606,0.00070363854,0.0000852939],"about_ca_topic_score_codex":0.7502135,"about_ca_topic_score_gemma":0.999062,"teacher_disagreement_score":0.24884848,"about_ca_system_score_codex":0.000004289819,"about_ca_system_score_gemma":0.001103788,"threshold_uncertainty_score":0.4249624},"labels":[],"label_agreement":null},{"id":"W2081384689","doi":"10.1139/e01-053","title":"Origin of vertical shafts in bedrock along the Eramosa River valley near Guelph, southern Ontario","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Waterloo; Canadian Natural Resources","funders":"","keywords":"Geology; Bedrock; Precambrian; Clastic rock; Geomorphology; Lithology; Dolomite; Basement; Geochemistry; Paleontology; Structural basin; Archaeology","score_opus":0.04094436590736624,"score_gpt":0.2347410874022207,"score_spread":0.19379672149485444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081384689","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926896,0.001274938,0.0000020423875,0.0014708876,0.0002696953,0.00006402721,0.000007502672,0.0000013789345,0.0042199357],"genre_scores_gemma":[0.9990667,0.000021736483,0.0002584438,0.00018985629,0.00003492543,1.3957076e-7,8.952897e-7,0.0000011598385,0.00042611882],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984721,0.00018862201,0.00034220016,0.00014683545,0.0003133658,0.0005368974],"domain_scores_gemma":[0.9990358,0.00029584725,0.00008584891,0.00011614278,0.00007880315,0.00038755598],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011629205,0.00009375115,0.00021225453,0.00021928598,0.00040210006,0.00006493064,0.00065484096,0.000088559194,0.008910562],"category_scores_gemma":[0.0001721975,0.000059002607,0.0000717055,0.00043546612,0.001940245,0.00021181896,0.000006917606,0.00045964852,0.00026726455],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008967098,0.000005358743,0.993691,0.0000026155126,0.000009593629,0.00016192529,0.0036648756,0.0020258087,9.405487e-7,0.000048196664,0.00010315997,0.00027751655],"study_design_scores_gemma":[0.00020363415,0.00021807857,0.99353015,0.00002697052,0.000007186756,0.00026211148,0.0004800414,0.0027466174,0.000006794488,0.00042072695,0.002025902,0.000071779614],"about_ca_topic_score_codex":0.29252613,"about_ca_topic_score_gemma":0.9938794,"teacher_disagreement_score":0.70135325,"about_ca_system_score_codex":0.0000014055884,"about_ca_system_score_gemma":0.0012171358,"threshold_uncertainty_score":0.99199545},"labels":[],"label_agreement":null},{"id":"W2081630810","doi":"10.1139/e07-046","title":"A new family, genus, and species of crab (Crustacea, Decapoda, Brachyura) from the upper Cretaceous (Campanian) of Manitoba, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Crustacean biology and ecology","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Brandon University","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Carapace; Cretaceous; Genus; Decapoda; Paleontology; Taxon; Geology; Extinction (optical mineralogy); Crustacean; Zoology; Biology","score_opus":0.01704988004782522,"score_gpt":0.19941344393983546,"score_spread":0.18236356389201025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081630810","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935669,0.0017258032,0.00008177439,0.0010067791,0.00040631567,0.0000715418,0.00003282966,9.775857e-7,0.0031071021],"genre_scores_gemma":[0.99767905,0.00006790931,0.0012384927,0.00062813034,0.0000871449,1.02728286e-7,6.4320795e-7,0.0000035476767,0.00029500396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998739,0.000047110698,0.0003869407,0.0001602301,0.0002648827,0.00040180748],"domain_scores_gemma":[0.9987749,0.00030638612,0.0003079415,0.00013209271,0.000031469623,0.00044723978],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007761547,0.000107477106,0.00022937701,0.00007808802,0.00027664652,0.000025733721,0.0005319714,0.00006946446,0.0018988787],"category_scores_gemma":[0.00016008543,0.000074072515,0.000050446477,0.0002817154,0.0013505948,0.00016208798,0.000045063232,0.00017168227,0.000006870865],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015816027,0.0000037554678,0.9900436,0.0000013960451,0.000014953653,0.000056648594,0.0004735352,0.00016020097,0.0011768931,0.00011313285,0.005943097,0.001996964],"study_design_scores_gemma":[0.00015173835,0.0001496252,0.9505051,0.000014048369,0.000015675174,0.00007253665,0.0038432535,0.000018297242,0.0007910653,0.00025253065,0.04410457,0.00008155413],"about_ca_topic_score_codex":0.82696605,"about_ca_topic_score_gemma":0.9986686,"teacher_disagreement_score":0.17170253,"about_ca_system_score_codex":0.00003875777,"about_ca_system_score_gemma":0.0014010458,"threshold_uncertainty_score":0.99901354},"labels":[],"label_agreement":null},{"id":"W2081927336","doi":"10.1139/e07-031","title":"Multimedia exploration strategies for PGEs: insights from the Surficial Geochemistry Case Studies Project, Lake Nipigon Region Geoscience Initiative, northwestern Ontario","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Geochemistry; Sill; Mafic; Ultramafic rock; Bedrock; Geomorphology","score_opus":0.10439521792980366,"score_gpt":0.2819626380263793,"score_spread":0.1775674200965756,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081927336","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95149356,0.0005111786,0.044100456,0.0013496581,0.0009742855,0.00022296989,0.000011225178,0.000013305563,0.0013233324],"genre_scores_gemma":[0.9933778,0.000010680028,0.005878992,0.00024425818,0.00029163287,0.0000044664307,0.0000031761276,0.0000016014377,0.00018738332],"study_design_codex":"qualitative","study_design_gemma":"qualitative","domain_scores_codex":[0.9984598,0.00005303913,0.00042643707,0.00032140155,0.0003063457,0.00043298103],"domain_scores_gemma":[0.9978845,0.00058535323,0.00043170562,0.00020740094,0.00065704226,0.0002339985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010432395,0.00016049366,0.00019820026,0.00013778085,0.0010426316,0.00046022845,0.00091439625,0.000070079586,0.0000073671454],"category_scores_gemma":[0.00035521953,0.00010743081,0.00007663237,0.0005456152,0.00072503183,0.0016622052,0.000047064463,0.00022780681,0.000001111045],"study_design_candidate":"qualitative","study_design_consensus":"qualitative","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014918335,0.00019585149,0.2072398,0.00016382399,0.00033717413,0.02109336,0.7153878,0.0086317,0.0024833742,0.010775175,0.0047824346,0.028760297],"study_design_scores_gemma":[0.003747252,0.0030669195,0.101066425,0.0014496355,0.00019674072,0.013791229,0.5154985,0.024484681,0.023789957,0.14460316,0.16533144,0.0029740504],"about_ca_topic_score_codex":0.033408616,"about_ca_topic_score_gemma":0.9719853,"teacher_disagreement_score":0.93857664,"about_ca_system_score_codex":0.000027992763,"about_ca_system_score_gemma":0.0043089106,"threshold_uncertainty_score":0.973028},"labels":[],"label_agreement":null},{"id":"W2082006506","doi":"10.1139/e01-066","title":"Seawater composition during deposition of Viséan evaporites in the Moncton Subbasin of New Brunswick as inferred from the fluid inclusion study of halite","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"PotashCorp (Canada)","funders":"Uniwersytet Marii Curie-Skłodowskiej; National Academy of Sciences of Ukraine","keywords":"Evaporite; Halite; Geology; Geochemistry; Anhydrite; Diagenesis; Fluid inclusions; Seawater; Potash; Inclusion (mineral); Mineralogy; Structural basin; Paleontology; Gypsum; Sedimentary rock; Hydrothermal circulation; Chemistry; Oceanography; Potassium","score_opus":0.020136239903902245,"score_gpt":0.2129758381935235,"score_spread":0.19283959828962127,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082006506","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997876,0.0008991823,0.0000032092062,0.0004901664,0.00010397231,0.00014686733,0.000011546448,9.576795e-7,0.00046813485],"genre_scores_gemma":[0.9997484,0.000024353873,0.000069067086,0.00007211187,0.000061071776,1.0440519e-7,0.000006491342,0.0000012339024,0.000017147586],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985956,0.00017120418,0.00046365688,0.000111203226,0.00046603242,0.00019229196],"domain_scores_gemma":[0.99925524,0.00011577055,0.00027597978,0.0001326253,0.000084465006,0.00013592355],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007142652,0.00008692493,0.00018415235,0.00012721606,0.0002917423,0.00006284296,0.00050470507,0.000035315108,0.0004138452],"category_scores_gemma":[0.000035289177,0.000049378843,0.000054283868,0.000413173,0.00022429673,0.00034230162,0.000016121527,0.00012580155,0.0000023782545],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023171628,0.000028649954,0.9782178,0.000009449311,0.00000938341,0.000020083438,0.013925688,0.0015965959,0.005400737,0.0000025181005,0.000019784018,0.000746137],"study_design_scores_gemma":[0.00039165904,0.00048635236,0.9777274,0.00012191053,0.000017023494,0.000046055007,0.0033635157,0.0007984288,0.016760446,0.00019417555,0.000033176406,0.000059858663],"about_ca_topic_score_codex":0.37769872,"about_ca_topic_score_gemma":0.5177853,"teacher_disagreement_score":0.14008659,"about_ca_system_score_codex":0.000002838672,"about_ca_system_score_gemma":0.0003253534,"threshold_uncertainty_score":0.62644523},"labels":[],"label_agreement":null},{"id":"W2082185807","doi":"10.1139/e10-013","title":"An Ordovician “Lost City” — venting serpentinite and life oases on Iapetus seafloor","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Regina; Geological Survey of Canada","funders":"","keywords":"Ordovician; Geology; Micrite; Carbonate; Calcite; Geochemistry; Diagenesis; Seafloor spreading; Paleontology; Carbonate minerals; Hydrothermal vent; Precambrian; Hydrothermal circulation","score_opus":0.023170105411622233,"score_gpt":0.23629025844239976,"score_spread":0.21312015303077753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082185807","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96647537,0.001153418,0.000003626055,0.00050515775,0.00085815316,0.000046068046,0.000038655035,0.00000439249,0.03091516],"genre_scores_gemma":[0.9985627,0.000014731801,0.0008276048,0.0003458732,0.00022889038,6.7890326e-8,0.0000013651508,7.296682e-7,0.000018022633],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988198,0.00007384143,0.00025620006,0.00019352292,0.00022857878,0.00042805122],"domain_scores_gemma":[0.99831027,0.00013873554,0.00018413804,0.000106759595,0.00007065371,0.0011894453],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009543133,0.00011577039,0.0001736271,0.0003858615,0.0008058683,0.000283342,0.00039205223,0.00007566486,0.0011008984],"category_scores_gemma":[0.00022744699,0.000090458554,0.00005817481,0.00032357062,0.00083422277,0.00063340965,7.721204e-7,0.000367876,0.00001648517],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008402039,0.000004782932,0.97511786,0.0000025932682,0.000007811019,0.00008642866,0.00020166617,0.000044743352,0.00006441573,0.00016665901,0.000016918784,0.024277745],"study_design_scores_gemma":[0.00013131274,0.0005123452,0.995963,0.000025123274,0.0000102056665,0.00015612938,0.00040279084,0.0003393969,0.000056452856,0.00036132144,0.0019256674,0.000116263625],"about_ca_topic_score_codex":0.007779289,"about_ca_topic_score_gemma":0.7811787,"teacher_disagreement_score":0.7733994,"about_ca_system_score_codex":2.6958787e-7,"about_ca_system_score_gemma":0.00085455354,"threshold_uncertainty_score":0.99981225},"labels":[],"label_agreement":null},{"id":"W2082508448","doi":"10.1139/e00-022","title":"Petrology, geochemistry, and diabase-granophyre relations of a thick basaltic sill emplaced into wet sediments, western Montana","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Sill; Geochemistry; Hornblende; Sedimentary rock; Igneous rock; Mafic; Petrology; Basalt; Metamorphism; Quartz; Biotite; Paleontology","score_opus":0.010170704363741342,"score_gpt":0.196474484356486,"score_spread":0.18630377999274467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082508448","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916338,0.0017653161,0.000004025382,0.002317739,0.000054147178,0.00003709938,0.000040808085,0.0000030337726,0.0041440553],"genre_scores_gemma":[0.99859065,0.000051550967,0.0005986284,0.00028122374,0.000046288453,1.6917033e-7,0.000008621264,0.0000010459008,0.00042180353],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988178,0.000062663836,0.0003538017,0.00019244984,0.00024743422,0.0003258397],"domain_scores_gemma":[0.9988796,0.00015798508,0.00015921489,0.00009134084,0.00008326237,0.0006285893],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046477516,0.00011360965,0.00025455325,0.000159538,0.0002887368,0.00005249557,0.00029696012,0.00007056629,0.013363911],"category_scores_gemma":[0.00013174841,0.00008008907,0.000078543715,0.00043742263,0.0008249985,0.00020695916,0.000005090838,0.0001910414,0.000040001807],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011050386,0.0000056410904,0.99553883,0.000006710275,0.000019892563,0.000030660856,0.00015423293,0.0015644021,0.00016970914,0.000006377861,0.00010211325,0.0023903775],"study_design_scores_gemma":[0.00026242554,0.00042628488,0.98963225,0.000032806838,0.000056681307,0.00010089128,0.00026693594,0.0027469294,0.0003106755,0.003627161,0.0023901023,0.00014686931],"about_ca_topic_score_codex":0.05336007,"about_ca_topic_score_gemma":0.4313168,"teacher_disagreement_score":0.37795672,"about_ca_system_score_codex":0.0000015899961,"about_ca_system_score_gemma":0.0003427314,"threshold_uncertainty_score":0.987538},"labels":[],"label_agreement":null},{"id":"W2082613013","doi":"10.1139/e99-105","title":"Structural setting, textures, and timing of hydrothermal vein systems in the Val d'Or camp, Abitibi, Canada: implications for the evolution of transcrustal, second- and third-order fault zones and gold mineralization","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Vale (Canada)","funders":"Australian Research Council","keywords":"Geology; Tourmaline; Quartz; Greenstone belt; Geochemistry; Shear zone; Vein; Hydrothermal circulation; Sinistral and dextral; Mineralization (soil science); Archean; Shear (geology); Fluid inclusions; Tectonics; Petrology; Mineralogy; Seismology; Paleontology","score_opus":0.014722071254180838,"score_gpt":0.2032030652006131,"score_spread":0.18848099394643225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082613013","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993255,0.0045393943,0.000020883806,0.001669923,0.000025468757,0.00010785489,0.000096497286,4.938024e-7,0.0002844569],"genre_scores_gemma":[0.9996307,0.000049347298,0.00013021375,0.00009513286,0.0000245833,4.788445e-7,0.0000029947066,5.729023e-7,0.000066009314],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999366,0.000048929593,0.00023147122,0.00009070981,0.00011138577,0.00015154645],"domain_scores_gemma":[0.9994655,0.00022429657,0.0001115058,0.000040003186,0.00006114624,0.00009753493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033935768,0.000059558795,0.00012922882,0.000061640785,0.00019610819,0.000046778125,0.00013711446,0.000027242428,0.00027440523],"category_scores_gemma":[0.00006191624,0.000028295095,0.000019589907,0.0002549756,0.0003666598,0.000117085736,0.0000013856813,0.00006266285,3.3841008e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029365028,0.0000038277867,0.95234394,0.00005772442,0.000027114329,0.0000037799684,0.0014068573,0.032602817,0.000339776,0.0007671266,0.00021279987,0.012204881],"study_design_scores_gemma":[0.00012692537,0.00011068569,0.9708638,0.000021145188,0.00002162589,0.00008882173,0.0012253169,0.026346454,0.000011182626,0.0006187425,0.0005154299,0.00004984121],"about_ca_topic_score_codex":0.71616733,"about_ca_topic_score_gemma":0.99119943,"teacher_disagreement_score":0.2750321,"about_ca_system_score_codex":0.0000018141523,"about_ca_system_score_gemma":0.0003984291,"threshold_uncertainty_score":0.3004545},"labels":[],"label_agreement":null},{"id":"W2082687610","doi":"10.1139/e06-073","title":"Nass River on the move: radar facies analysis of glaciofluvial sedimentation and its response to sea-level change in northwestern British Columbia","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical Methods and Applications","field":"Engineering","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; AXYS Technologies (Canada)","funders":"","keywords":"Geology; Bedrock; Sea level; Fjord; Facies; Ridge; Sedimentary depositional environment; Geomorphology; Glacial period; Delta; Buttress; Paleontology; Bathymetry; Oceanography; Archaeology","score_opus":0.03244003273904369,"score_gpt":0.2555434217931908,"score_spread":0.2231033890541471,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082687610","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991692,0.00008718311,0.0000692724,0.0003890621,0.00004557513,0.00008126793,0.0001134006,0.0000016646221,0.000043423515],"genre_scores_gemma":[0.99915123,0.000004945838,0.00067911705,0.000084006955,0.000029850371,0.0000032224598,7.6307856e-7,0.0000021767198,0.00004469852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994701,0.000046518,0.00015382346,0.000066883695,0.00013516197,0.00012751807],"domain_scores_gemma":[0.9996381,0.00011358334,0.00004435825,0.000041680483,0.00004681134,0.0001154854],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004165838,0.000037665788,0.0001114554,0.00017995114,0.00010123844,0.00010423559,0.00010983958,0.000015589574,0.000030547842],"category_scores_gemma":[0.000032990916,0.000038902785,0.00003273533,0.00084561395,0.00008823181,0.00011383521,0.0000039308643,0.00005538017,0.0000010943096],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027283462,0.000039970862,0.91690177,0.000020510155,0.00013379674,0.00005520785,0.005200387,0.026350638,0.01887031,0.00049276906,0.00038286042,0.03152447],"study_design_scores_gemma":[0.00006479038,0.00004760005,0.9973584,0.00002013587,0.000017649752,0.0000023694101,0.00012634067,0.0015685781,0.0002666275,0.000114275455,0.00036947333,0.00004379831],"about_ca_topic_score_codex":0.108414575,"about_ca_topic_score_gemma":0.82549256,"teacher_disagreement_score":0.717078,"about_ca_system_score_codex":0.000007985017,"about_ca_system_score_gemma":0.0000649181,"threshold_uncertainty_score":0.89752257},"labels":[],"label_agreement":null},{"id":"W2082701485","doi":"10.1139/e10-071","title":"Neoarchean high-potassium granites of the Boothia mainland area, Rae domain, Churchill Province: U–Pb zircon and Sm–Nd whole rock isotopic constraintsThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Government of Newfoundland and Labrador; Geological Survey of Canada","funders":"","keywords":"Geology; Zircon; Geochemistry; Plutonism; Metamorphism; Archean; Craton; Terrane; Pluton; Petrology; Paleontology; Tectonics","score_opus":0.013911504142756013,"score_gpt":0.1662130745584227,"score_spread":0.1523015704156667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082701485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893151,0.0003271387,0.0000011400796,0.0039016563,0.00007245757,0.0001307861,0.00010417258,6.9532445e-7,0.006146842],"genre_scores_gemma":[0.9993145,0.00003510902,0.00038398494,0.00015089827,0.000047710022,3.357416e-7,0.0000012323233,0.0000011551076,0.00006506616],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984414,0.000175994,0.0006230048,0.00016730528,0.0003002645,0.0002920451],"domain_scores_gemma":[0.9988195,0.00023143715,0.00052610354,0.0001481007,0.00012305484,0.00015185517],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010426355,0.00011501003,0.00043631168,0.00023410312,0.00009141857,0.000017831091,0.00051221164,0.000074630516,0.011549999],"category_scores_gemma":[0.0003253128,0.00006206601,0.00009977727,0.0006211425,0.0023209746,0.00018960719,0.000020179888,0.0002397764,0.0000012341332],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010321641,0.000057882295,0.9829555,0.00003977334,0.000035811707,0.000009836293,0.0038625682,0.00016714973,0.009398627,0.0005968885,0.00012951632,0.0026432301],"study_design_scores_gemma":[0.00044033394,0.0007504692,0.9170656,0.00015705456,0.00002425521,0.00001569197,0.0029406,0.00007242292,0.06249978,0.015542131,0.00039961794,0.00009200866],"about_ca_topic_score_codex":0.032711484,"about_ca_topic_score_gemma":0.29987672,"teacher_disagreement_score":0.26716524,"about_ca_system_score_codex":0.0000026272164,"about_ca_system_score_gemma":0.0004813933,"threshold_uncertainty_score":0.9893536},"labels":[],"label_agreement":null},{"id":"W2082822768","doi":"10.1139/e02-016","title":"Age of volcanic rocks and syndepositional iron formations, Marquette Range Supergroup: implications for the tectonic setting of Paleoproterozoic iron formations of the Lake Superior region","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":141,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Ironwood Pharmaceuticals, Incorporated","keywords":"Geology; Zircon; Geochemistry; Provenance; Terrane; Rift; Continental arc; Paleontology; Rhyolite; Passive margin; Archean; Continental margin; Subduction; Volcanic rock; Tectonics; Volcano","score_opus":0.01734673085921407,"score_gpt":0.18935234831609798,"score_spread":0.17200561745688392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082822768","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9917704,0.0012901102,0.00027974445,0.005859889,0.000043285698,0.000148483,0.00023020111,0.0000013441753,0.00037655613],"genre_scores_gemma":[0.99946404,0.000077914236,0.0002916957,0.00010754496,0.000019972018,0.0000019561141,0.000011635882,7.118061e-7,0.00002455085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990836,0.000046253448,0.0004160857,0.00008324486,0.000176185,0.00019462482],"domain_scores_gemma":[0.99907273,0.00026428865,0.0003004005,0.00010579387,0.00013212835,0.0001246388],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039326216,0.00007141007,0.00016186554,0.00011979772,0.00049073226,0.000033823104,0.00034202728,0.000037089023,0.0004917901],"category_scores_gemma":[0.00014942512,0.000038102113,0.00012953368,0.0004362296,0.00050928514,0.00026649883,0.000008132302,0.00009749448,8.296652e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045484944,0.000008220857,0.9926897,0.000042171556,0.000016622982,5.3402226e-7,0.0004509827,0.0027034802,0.00039061025,0.00016218961,0.00007789142,0.0034530356],"study_design_scores_gemma":[0.00013771889,0.00015143186,0.9931842,0.000045422497,0.000052945812,0.00007966059,0.00031575628,0.004112384,0.00015250526,0.0012756237,0.00043578583,0.000056572484],"about_ca_topic_score_codex":0.0027187364,"about_ca_topic_score_gemma":0.3306107,"teacher_disagreement_score":0.32789195,"about_ca_system_score_codex":0.0000015445904,"about_ca_system_score_gemma":0.00010010407,"threshold_uncertainty_score":0.6816039},"labels":[],"label_agreement":null},{"id":"W2082929728","doi":"10.1139/e02-066","title":"A new microsaur (Tetrapoda: Lepospondyli) from the Lower Permian of Richards Spur (Fort Sill), Oklahoma","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Amgen (Canada)","funders":"McGill University","keywords":"Geology; Permian; Paleontology; Ridge","score_opus":0.016362173193956924,"score_gpt":0.20561154546175064,"score_spread":0.18924937226779373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082929728","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97946346,0.008679969,0.00006185415,0.0014311968,0.0016856747,0.000059303697,0.00011189053,0.0000026204439,0.008504042],"genre_scores_gemma":[0.99743706,0.00006467206,0.001493961,0.00048127843,0.00018007123,7.264162e-8,0.0000049035,0.0000013869005,0.0003366024],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986077,0.00016576026,0.00036653478,0.00018212145,0.00022249058,0.0004554078],"domain_scores_gemma":[0.9987409,0.00025865063,0.00024239444,0.00013841476,0.00009099548,0.00052861945],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00087978976,0.00012434875,0.00023587502,0.00016957194,0.0004854378,0.000046617373,0.00062379095,0.000106160915,0.0053455173],"category_scores_gemma":[0.0002698082,0.00007778934,0.00012467615,0.00046560125,0.0010104092,0.00028354366,0.0000029454393,0.0002414625,0.00005515686],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016218873,0.000004460574,0.994708,0.0000010400719,0.000022398717,0.000077201024,0.0003045662,0.00022415943,0.00008553285,0.00028433994,0.0015191517,0.0027529227],"study_design_scores_gemma":[0.0001983385,0.0003927627,0.9384378,0.00002018094,0.000016714961,0.0004186759,0.00035420424,0.000056954053,0.00010886002,0.0014090288,0.058484823,0.000101645936],"about_ca_topic_score_codex":0.045541268,"about_ca_topic_score_gemma":0.6612384,"teacher_disagreement_score":0.61569715,"about_ca_system_score_codex":0.0000023599398,"about_ca_system_score_gemma":0.003197828,"threshold_uncertainty_score":0.99556375},"labels":[],"label_agreement":null},{"id":"W2082938432","doi":"10.1139/e03-034","title":"Geochemistry and petrogenesis of Ordovician arc-related mafic volcanic rocks in the Popelogan Inlier, northern New Brunswick","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Geochemistry; Mafic; Basalt; Andesites; Pyroclastic rock; Partial melting; Andesite; Volcanic rock; Petrogenesis; Mantle wedge; Mantle plume; Petrology; Volcanic arc; Subduction; Volcano; Lithosphere; Paleontology","score_opus":0.010947012577588214,"score_gpt":0.181243026636685,"score_spread":0.1702960140590968,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082938432","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9899268,0.004031968,0.000003871821,0.0010115838,0.00006370621,0.000036045414,0.000005694292,0.0000013156855,0.004919005],"genre_scores_gemma":[0.9994058,0.00006059435,0.0001576281,0.00022608812,0.00002579126,4.353843e-8,0.0000023395648,9.663319e-7,0.00012073182],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987383,0.00009749608,0.0003744832,0.0001655135,0.00026417858,0.00036006398],"domain_scores_gemma":[0.99904543,0.00013011348,0.00019590238,0.00009728627,0.00006923808,0.0004620393],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007863564,0.00010933114,0.0002258846,0.0001881972,0.00018791176,0.00006182271,0.0004489693,0.000062755775,0.0026774989],"category_scores_gemma":[0.00031342136,0.0000647069,0.00008628039,0.00095569866,0.00044314464,0.00011892923,0.000003925799,0.00020365434,0.000012073455],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002511805,0.000004754955,0.99659413,0.0000033086742,0.000010163981,0.000034988774,0.0002202475,0.0011167384,0.0000495403,0.000048737013,0.000017714718,0.0018971483],"study_design_scores_gemma":[0.0001796098,0.00015915695,0.9903315,0.000022667673,0.000025044337,0.0001854862,0.0012240137,0.00028324907,0.00026583706,0.0058344943,0.0013781636,0.000110827204],"about_ca_topic_score_codex":0.1304366,"about_ca_topic_score_gemma":0.94881207,"teacher_disagreement_score":0.81837547,"about_ca_system_score_codex":0.0000015951338,"about_ca_system_score_gemma":0.0015028864,"threshold_uncertainty_score":0.9982342},"labels":[],"label_agreement":null},{"id":"W2083328074","doi":"10.1139/e2012-055","title":"Cf.<i>Wortmania</i>from the early Paleocene of Montana and an evaluation of the fossil record of the initial diversification of the Taeniodonta (Mammalia)","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"University of California Museum of Paleontology","keywords":"Fossil Record; Range (aeronautics); Fauna; Population; Geology; Mammal; Paleontology; Geography; Structural basin; Archaeology; Ecology; Biology; Demography","score_opus":0.06941088524378779,"score_gpt":0.25347980272631476,"score_spread":0.18406891748252696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083328074","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99323,0.0018862884,0.0000021618816,0.0023436358,0.0005662448,0.00018728431,0.00007053979,5.6164765e-7,0.001713314],"genre_scores_gemma":[0.99974614,0.000045977667,0.00005521419,0.00007747818,0.00004944987,3.3188033e-7,4.961541e-7,7.6605136e-7,0.00002412414],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984048,0.00044143526,0.00036639304,0.00010140551,0.00053837564,0.00014759923],"domain_scores_gemma":[0.99837697,0.00020166977,0.00071872526,0.0002080297,0.00040384562,0.00009076744],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013448725,0.000071412054,0.00015875617,0.000055754484,0.00046113555,0.00002610669,0.0007136701,0.00003992124,0.00023094841],"category_scores_gemma":[0.0002868262,0.00003131354,0.00008325937,0.00038563798,0.0018021836,0.00028049486,0.000013934639,0.0001189474,7.4966437e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000060974157,0.0000033222423,0.9929652,0.00000264226,0.000017670129,1.2010206e-7,0.001476852,0.0002083909,0.00008161177,0.00004868562,0.00013491602,0.005054481],"study_design_scores_gemma":[0.00015776698,0.00012680604,0.9955698,0.00005313341,0.00006160434,0.000005470013,0.00197916,0.0008116764,0.0003001505,0.0007465945,0.00015049224,0.000037339556],"about_ca_topic_score_codex":0.12305206,"about_ca_topic_score_gemma":0.8926415,"teacher_disagreement_score":0.7695894,"about_ca_system_score_codex":0.0000022989968,"about_ca_system_score_gemma":0.0007020797,"threshold_uncertainty_score":0.8827876},"labels":[],"label_agreement":null},{"id":"W2083831910","doi":"10.1139/e01-036","title":"A new species of <i>Chasmosaurus</i> (Dinosauria: Ceratopsia) from the Dinosaur Park Formation of southern Alberta","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; Canadian Museum of Nature","funders":"","keywords":"Paleontology; Biology; Genus; French horn; Geology; Anatomy; Zoology; Physics","score_opus":0.021598372879661727,"score_gpt":0.19763548273551623,"score_spread":0.1760371098558545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083831910","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98328894,0.0029050417,0.00022748529,0.0030861823,0.00052655226,0.00005822926,0.00013383973,0.0000015222741,0.009772219],"genre_scores_gemma":[0.9985997,0.00009279607,0.00047824177,0.00023383246,0.00020464766,6.901466e-8,0.000011018626,8.6564665e-7,0.0003788062],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998866,0.0001199459,0.00041213864,0.0001078453,0.00020483966,0.00028920046],"domain_scores_gemma":[0.99876755,0.0003871466,0.0003906409,0.00010755757,0.000087009175,0.0002600724],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005036456,0.000092742775,0.00021938872,0.00012946944,0.00027260353,0.000025730791,0.00053510733,0.00007601109,0.0030731307],"category_scores_gemma":[0.00016287343,0.00005747421,0.00008908074,0.00037389368,0.0008677923,0.00034086008,0.0000041438325,0.00013633588,0.000044356104],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029161152,0.0000027397934,0.9943751,0.0000017572696,0.000015097389,0.000011658971,0.0011549139,0.0005546186,0.00009130122,0.00025732533,0.0014397101,0.0020665897],"study_design_scores_gemma":[0.00020893507,0.0002357599,0.9750239,0.000039837614,0.000020902407,0.00015062877,0.0018468278,0.00039934856,0.0002063932,0.0021834776,0.019600788,0.00008319857],"about_ca_topic_score_codex":0.112119995,"about_ca_topic_score_gemma":0.8527534,"teacher_disagreement_score":0.74063337,"about_ca_system_score_codex":0.0000013887473,"about_ca_system_score_gemma":0.00091196515,"threshold_uncertainty_score":0.9978382},"labels":[],"label_agreement":null},{"id":"W2084076600","doi":"10.1139/e09-024","title":"Geologist-controlled trends versus computer-controlled trends: introducing a high-resolution approach to subsurface structural mapping using well-log data, trend surface analysis, and geospatial analysisA companion paper to Mei, S. 2009. New insights on faults in the Peace River Arch region, northwest Alberta, based on existing well-log data and refined trend surface analysis. Canadian Journal of Earth Sciences, <b>46</b>(1): 41–65.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Residual; Geology; Kriging; Polynomial; Variogram; Data mining; Remote sensing; Algorithm; Computer science; Mathematics","score_opus":0.04853423576249651,"score_gpt":0.2654000998846114,"score_spread":0.21686586412211487,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084076600","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9698943,0.0008688304,0.020195391,0.00722632,0.00039015713,0.00029041368,0.00007743467,0.0000111463905,0.0010460042],"genre_scores_gemma":[0.96753246,0.000016601472,0.031451497,0.0005171347,0.00023724366,6.309438e-7,0.00011770957,0.000005776831,0.00012091916],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9934221,0.0010008162,0.001590888,0.0015701979,0.0011719707,0.0012440529],"domain_scores_gemma":[0.99445355,0.0010124288,0.0014197379,0.0013569553,0.00028918337,0.0014681394],"candidate_categories":["metaepi_narrow","sts","scholarly_communication"],"consensus_categories":[],"category_scores_codex":[0.00561642,0.0005932854,0.0017412094,0.004272252,0.0016645731,0.0010570321,0.0039177705,0.0001747941,0.000036019133],"category_scores_gemma":[0.00076439604,0.0004228881,0.00028387015,0.01076211,0.00071150716,0.0013139833,0.00018422704,0.0006934489,8.357212e-7],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003509633,0.000039481463,0.04640465,0.0000051758448,0.0003603418,0.00011487886,0.002376061,0.94726306,0.00007578877,0.00014695812,0.0003134686,0.0025491551],"study_design_scores_gemma":[0.0041695694,0.00069216604,0.24856108,0.00008407652,0.0006044659,0.000087578366,0.0005253109,0.74389595,0.000011106228,0.000030191906,0.0009241608,0.0004143547],"about_ca_topic_score_codex":0.24370421,"about_ca_topic_score_gemma":0.9109352,"teacher_disagreement_score":0.66723096,"about_ca_system_score_codex":0.00008297466,"about_ca_system_score_gemma":0.0019142155,"threshold_uncertainty_score":0.99998},"labels":[],"label_agreement":null},{"id":"W2084362152","doi":"10.1139/e2012-067","title":"U–Pb and Hf isotopic data from Franklinian Basin strata: insights into the nature of Crockerland and the timing of accretion, Canadian Arctic Islands","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Calgary","funders":"University of Calgary; Washington State University","keywords":"Geology; Zircon; Devonian; Provenance; Laurentia; Clastic rock; Foreland basin; Late Devonian extinction; Population; Paleontology; Geochemistry; Terrane; Structural basin; Paleozoic; Tectonics; Carboniferous","score_opus":0.02070208117842458,"score_gpt":0.21477510031114114,"score_spread":0.19407301913271655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084362152","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9808622,0.014781154,0.0000061180654,0.0033250772,0.00013749271,0.000047137823,0.000070545255,5.596353e-7,0.0007697238],"genre_scores_gemma":[0.99890816,0.0002191334,0.00028033135,0.0004327409,0.000127064,7.418001e-8,0.00001592316,6.985437e-7,0.00001589937],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99902743,0.00010556968,0.000273131,0.00013262397,0.00020995318,0.00025129254],"domain_scores_gemma":[0.9986813,0.00038641674,0.00017920583,0.0001627287,0.00009514709,0.00049519655],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008820128,0.00008504941,0.000220745,0.00013010726,0.0003894472,0.000082035214,0.0005852866,0.0000721424,0.001137749],"category_scores_gemma":[0.00037284076,0.000038425445,0.000037757363,0.0003465456,0.0012585289,0.0003431925,0.00001745069,0.0002546651,0.0000019942772],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007738637,0.000001567856,0.99679387,0.0000052890455,0.000025061196,0.000003211406,0.0015310426,0.000025923542,0.000013169624,0.000107852946,0.00006532669,0.0014199311],"study_design_scores_gemma":[0.00018412269,0.000056120716,0.9873136,0.000033494438,0.00005428426,0.000019303145,0.0011174288,0.0013437414,0.00006572538,0.006134523,0.003614387,0.00006324627],"about_ca_topic_score_codex":0.66079444,"about_ca_topic_score_gemma":0.9774372,"teacher_disagreement_score":0.31664273,"about_ca_system_score_codex":0.0000010486957,"about_ca_system_score_gemma":0.00045262225,"threshold_uncertainty_score":0.99977535},"labels":[],"label_agreement":null},{"id":"W2084564364","doi":"10.1139/e00-099","title":"Structure of the Lac Nominingue Mont-Laurier region, Central Metasedimentary Belt, Quebec Grenville Province","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Gneiss; Metamorphism; Terrane; Shear zone; Granulite; Geochemistry; Metamorphic rock; Orogeny; Fold (higher-order function); Petrology; Tectonics; Geomorphology; Facies; Seismology; Structural basin","score_opus":0.011041914152940719,"score_gpt":0.17557597339706796,"score_spread":0.16453405924412723,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084564364","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933215,0.0012554257,0.000005256318,0.003904688,0.0003119454,0.000054636042,0.000049341284,0.0000015106756,0.0010957316],"genre_scores_gemma":[0.9986017,0.000018839133,0.00032969055,0.000591503,0.00012357662,4.069323e-8,0.0000045427205,9.320074e-7,0.0003292027],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986733,0.000077942466,0.000329879,0.00016189802,0.00033144775,0.00042550912],"domain_scores_gemma":[0.99892855,0.00007111471,0.00027637524,0.00012201508,0.00008671081,0.0005152271],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022385147,0.00011142218,0.0002179051,0.00011960248,0.0003227503,0.00005564589,0.0006379562,0.00004765972,0.004650231],"category_scores_gemma":[0.00012624107,0.000058390266,0.00015230454,0.00059053366,0.0008324471,0.00019467797,0.000009681197,0.00018530755,0.0000043596538],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008102903,0.000003790364,0.9938217,0.0000023994198,0.000020820296,0.00005534683,0.00009518389,0.0033183892,0.0000999481,0.00005131962,0.00052978686,0.0019932184],"study_design_scores_gemma":[0.00012242915,0.00012736661,0.98630804,0.000024042758,0.000042894255,0.00014580572,0.00026605558,0.0004698636,0.00088334363,0.0020959368,0.009410385,0.00010384072],"about_ca_topic_score_codex":0.33485627,"about_ca_topic_score_gemma":0.9669668,"teacher_disagreement_score":0.63211054,"about_ca_system_score_codex":0.0000027354429,"about_ca_system_score_gemma":0.00094071135,"threshold_uncertainty_score":0.9962596},"labels":[],"label_agreement":null},{"id":"W2084714346","doi":"10.1139/e09-004","title":"Provenance of the Meguma terrane, Nova Scotia: rifted margin of early Paleozoic Gondwana","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":129,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University; Saint Mary's University; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Gondwana; Geology; Terrane; Paleozoic; Paleontology; Provenance; Rift; Proterozoic; Passive margin; Ordovician; Structural basin; Tectonics","score_opus":0.01600710535459211,"score_gpt":0.19248820256188365,"score_spread":0.17648109720729155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084714346","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98985946,0.001305135,0.000006669464,0.0020206128,0.00018407627,0.000059322392,0.000028458255,0.0000014551613,0.006534832],"genre_scores_gemma":[0.99902767,0.000011564837,0.0005909132,0.00023879299,0.000044787896,2.2488296e-8,8.898113e-7,6.001114e-7,0.000084746134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986174,0.00006624768,0.00044166629,0.0001438612,0.00039203203,0.00033879798],"domain_scores_gemma":[0.99892294,0.000059785412,0.00039865647,0.00013167644,0.00016329039,0.00032364903],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000552989,0.000101904225,0.0002809018,0.00017456104,0.00013468508,0.00003653633,0.00075186254,0.00004979942,0.0027848126],"category_scores_gemma":[0.00020408402,0.000054509088,0.00018101673,0.0011135072,0.00083852286,0.00019575183,0.0000048417332,0.00017363434,0.000013048277],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000849626,0.000008598188,0.99301267,0.000005661485,0.000012270739,0.000011293707,0.0001101203,0.0009458949,0.0005440137,0.0001530761,0.00008205669,0.0051058666],"study_design_scores_gemma":[0.00011255849,0.00044738036,0.9911219,0.00006286358,0.000020621848,0.00002719658,0.00007028523,0.00022791808,0.0016294798,0.0059136213,0.0002909027,0.000075275355],"about_ca_topic_score_codex":0.035396736,"about_ca_topic_score_gemma":0.3680875,"teacher_disagreement_score":0.33269075,"about_ca_system_score_codex":9.1677805e-7,"about_ca_system_score_gemma":0.00053052383,"threshold_uncertainty_score":0.9981268},"labels":[],"label_agreement":null},{"id":"W2085022874","doi":"10.1139/e06-075","title":"The Wyoming Province: a distinctive Archean craton in Laurentian North America","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":138,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Terrane; Archean; Geology; Craton; Laurentia; Zircon; Geochemistry; Mafic; Proterozoic; Continental crust; Crust; Magmatism; Provenance; Paleontology; Paleozoic; Tectonics","score_opus":0.009145289986727364,"score_gpt":0.18066925386092217,"score_spread":0.1715239638741948,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2085022874","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99012876,0.0010876455,0.000027502016,0.0019044108,0.00011647921,0.000045289467,0.000016924676,0.00000226671,0.0066707097],"genre_scores_gemma":[0.99932307,0.000013751722,0.0002963428,0.00012659632,0.00010544057,1.7000498e-7,0.000006165505,6.809506e-7,0.00012780329],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99876416,0.000076919125,0.00030006058,0.00014777205,0.0002569129,0.00045415544],"domain_scores_gemma":[0.9991994,0.00018680973,0.00016716804,0.00006520945,0.000065401444,0.0003160271],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047019243,0.00008789294,0.00015029672,0.00015555984,0.00052986795,0.00017523006,0.00044170252,0.0000232508,0.0010455785],"category_scores_gemma":[0.00016487272,0.000047316895,0.00008049469,0.000761205,0.0008754524,0.00017665874,0.0000052600712,0.00020447305,0.000026997968],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005225047,0.000003665842,0.98396444,0.0000010997749,0.000003433298,0.000057395548,0.000052511143,0.004442613,0.000004366241,0.000053698306,0.00010152748,0.011310027],"study_design_scores_gemma":[0.00006848084,0.0001214562,0.9787677,0.000011049617,0.0000067092583,0.000017475568,0.00033602092,0.0023253774,0.000023947012,0.005810928,0.0124291275,0.00008170952],"about_ca_topic_score_codex":0.14234965,"about_ca_topic_score_gemma":0.9873767,"teacher_disagreement_score":0.8450271,"about_ca_system_score_codex":0.0000022895856,"about_ca_system_score_gemma":0.0006487371,"threshold_uncertainty_score":0.9998676},"labels":[],"label_agreement":null},{"id":"W2085274161","doi":"10.1139/e10-006","title":"Detrital zircon characteristics of the Lower Cretaceous Isachsen Formation, Sverdrup Basin: source constraints from age and Hf isotope data","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Norges Forskningsråd","keywords":"Zircon; Geology; Sverdrup; Precambrian; Geochemistry; Arctic; Cretaceous; Population; Paleontology; Basement; Structural basin; Oceanography","score_opus":0.01826439203194495,"score_gpt":0.1903193924943634,"score_spread":0.17205500046241845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2085274161","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964554,0.00024923842,0.000081328246,0.0011060638,0.0003748978,0.000041937987,0.0004506304,0.0000016384846,0.0012388707],"genre_scores_gemma":[0.99836457,0.000017367884,0.0011031625,0.00033424766,0.00010236027,3.0924014e-8,0.000019515985,7.6500976e-7,0.000057992776],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989852,0.000047508755,0.00032006606,0.00014903511,0.00026311976,0.00023508816],"domain_scores_gemma":[0.99888533,0.00018541323,0.00025720417,0.0001861618,0.00009573774,0.00039013466],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005456804,0.00008627273,0.00019988237,0.00008789799,0.00026861575,0.00014105727,0.0007894732,0.000057301877,0.004112476],"category_scores_gemma":[0.0005846113,0.00004938206,0.00005959291,0.00026295276,0.0014966474,0.0003905471,0.000026251071,0.00024856403,0.000013366633],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006673184,0.000006453936,0.9808892,0.0000036117256,0.00001616786,0.000048312857,0.00016435982,0.000021541573,0.0015958383,0.000016009119,0.00015998805,0.017071865],"study_design_scores_gemma":[0.00012963604,0.00013324861,0.98279375,0.000023696404,0.000039384468,0.0001318319,0.00025947683,0.0014149388,0.0008195218,0.0011785293,0.012964753,0.00011125401],"about_ca_topic_score_codex":0.011951034,"about_ca_topic_score_gemma":0.2845956,"teacher_disagreement_score":0.27264458,"about_ca_system_score_codex":4.950743e-7,"about_ca_system_score_gemma":0.00028917135,"threshold_uncertainty_score":0.9967979},"labels":[],"label_agreement":null},{"id":"W2086283574","doi":"10.1139/e08-049","title":"Correlation of Grassy Lake and Cedar Lake ambers using infrared spectroscopy, stable isotopes, and palaeoentomology","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fossil Insects in Amber","field":"Agricultural and Biological Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Cretaceous; Geology; Fauna; Context (archaeology); Paleontology; Arthropod; Ecology; Biology","score_opus":0.029551049336582154,"score_gpt":0.22750522195845396,"score_spread":0.19795417262187182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086283574","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99676055,0.0007130323,0.0000073956385,0.0002085478,0.00022457198,0.000057011577,0.000027094728,0.0000024952367,0.0019993111],"genre_scores_gemma":[0.9987072,0.00010515868,0.0008764833,0.00008492166,0.00006787595,1.8337704e-7,0.000001344791,5.5082086e-7,0.0001563236],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991206,0.000059582548,0.00024177037,0.00013311594,0.00017891843,0.00026600057],"domain_scores_gemma":[0.99926823,0.00009288573,0.00022255933,0.00002620638,0.000097740005,0.00029238756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039465533,0.00008202066,0.00017185659,0.00007302917,0.00037142218,0.00005366324,0.0001417709,0.000058179845,0.00034223855],"category_scores_gemma":[0.0001097999,0.000037590376,0.000029755645,0.00038825866,0.0009933757,0.0003202187,0.000014568787,0.00011192627,8.265216e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011783719,0.000008960756,0.98328876,0.0000046987475,0.000010120409,0.00008557076,0.0003948738,0.00020903618,0.01469259,0.00029264073,0.00040530408,0.0005956685],"study_design_scores_gemma":[0.00019420289,0.00056128355,0.98564786,0.000046847363,0.000011655841,0.0010691469,0.00037275563,0.0005539524,0.0012007403,0.00067646307,0.009537119,0.00012796538],"about_ca_topic_score_codex":0.0039066025,"about_ca_topic_score_gemma":0.432832,"teacher_disagreement_score":0.4289254,"about_ca_system_score_codex":0.0000046228474,"about_ca_system_score_gemma":0.00022348033,"threshold_uncertainty_score":0.590564},"labels":[],"label_agreement":null},{"id":"W2086308446","doi":"10.1139/e03-046","title":"Pleistocene magmatism in a lithospheric transition area: petrogenesis of alkaline and peralkaline lavas from the BaringoBogoria Basin, central Kenya Rift","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Craton; Petrogenesis; Basalt; Rift; Peralkaline rock; Phenocryst; Fractional crystallization (geology); Large igneous province; Volcanic rock; Petrology; Magmatism; Volcano; Geomorphology; Structural basin; Tectonics; Paleontology","score_opus":0.012312396422048849,"score_gpt":0.18027921193803864,"score_spread":0.1679668155159898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086308446","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942122,0.0037059167,0.00008283288,0.0014003044,0.00010966809,0.00004512179,0.00006057845,0.0000015262798,0.00038185046],"genre_scores_gemma":[0.9969254,0.00014418847,0.0025526527,0.00030545145,0.000048585956,1.4749794e-7,0.0000070544866,0.0000010120968,0.00001550784],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99880093,0.00012862925,0.00035532622,0.00015951566,0.00022734645,0.0003282311],"domain_scores_gemma":[0.9991612,0.00017926184,0.00014426411,0.000072405724,0.00006785288,0.0003750076],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00063486793,0.00010364364,0.00025379768,0.000088263034,0.00016974808,0.000060470207,0.00023213263,0.000044956036,0.0044223797],"category_scores_gemma":[0.0002134425,0.00006142171,0.00008692068,0.0006137099,0.00043523387,0.00017201332,0.000002527511,0.00013375655,0.0000035565945],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011021057,0.000007872914,0.99293023,0.0000033976648,0.000014696324,0.000031402575,0.0004201645,0.003552837,0.00012666974,0.000085848806,0.000023494,0.0027923547],"study_design_scores_gemma":[0.00021246306,0.00015350671,0.9907669,0.00003369398,0.000029099658,0.00004262993,0.00054380903,0.002489448,0.00028568378,0.004399268,0.00095300144,0.00009052854],"about_ca_topic_score_codex":0.16276382,"about_ca_topic_score_gemma":0.66900694,"teacher_disagreement_score":0.5062431,"about_ca_system_score_codex":0.0000016976898,"about_ca_system_score_gemma":0.00029830704,"threshold_uncertainty_score":0.99648774},"labels":[],"label_agreement":null},{"id":"W2086692354","doi":"10.1139/cjes-2013-0018","title":"Genesis of dispersal plumes in till","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Ottawa; Geoscience BC","funders":"","keywords":"Geology; Meltwater; Geomorphology; Ice sheet; Debris; Glacier; Plume; Ice divide; Ice shelf; Geochemistry; Sea ice; Oceanography; Cryosphere","score_opus":0.02341515087464269,"score_gpt":0.20271635513867672,"score_spread":0.17930120426403404,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086692354","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99378294,0.0024289258,0.000010709257,0.0007441937,0.00030242698,0.000044620392,0.000009839284,8.9495524e-7,0.0026754416],"genre_scores_gemma":[0.99858,0.00007557458,0.0010810953,0.00012761472,0.000050001745,1.2602938e-7,4.6694686e-7,7.2932096e-7,0.00008438915],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99926645,0.000020664213,0.0002466857,0.000073234856,0.00016317373,0.00022979332],"domain_scores_gemma":[0.9994379,0.000082482795,0.000116848285,0.000048163303,0.000084667045,0.00022990757],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00028371607,0.000052564857,0.00013314217,0.00012573777,0.00013265593,0.000050469695,0.00024029615,0.000019771383,0.0038366523],"category_scores_gemma":[0.00010074889,0.00003755212,0.00004352791,0.00049729453,0.00031104812,0.00031933066,0.0000024846065,0.000055606102,0.000026103675],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[6.471581e-7,0.0000014962759,0.9914489,0.0000018553615,0.0000033944716,0.0000054022294,0.00039193733,0.002084867,0.000007427697,0.000054020784,0.00029682677,0.0057032583],"study_design_scores_gemma":[0.00006664403,0.000097642784,0.99253124,0.000017055583,0.0000027554331,0.000008597477,0.0019357078,0.0018992734,0.000012092704,0.00018783388,0.0031931512,0.000048012374],"about_ca_topic_score_codex":0.24520928,"about_ca_topic_score_gemma":0.76314646,"teacher_disagreement_score":0.5179372,"about_ca_system_score_codex":0.0000010983277,"about_ca_system_score_gemma":0.00050499325,"threshold_uncertainty_score":0.99707395},"labels":[],"label_agreement":null},{"id":"W2086778250","doi":"10.1139/e08-006","title":"Inception of a Devonian subduction zone along the southwestern Gondwana margin: <sup>40</sup>Ar–<sup>39</sup>Ar dating of eclogite–amphibolite assemblages in blueschist boulders from the Coastal Range of Chile (41°S)","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Metamorphism; Blueschist; Eclogite; Geochemistry; Metamorphic facies; Hornblende; Subduction; Petrology; Paleontology; Facies; Tectonics; Biotite","score_opus":0.02084335206982822,"score_gpt":0.19885817926362587,"score_spread":0.17801482719379766,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086778250","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964486,0.0014952093,0.000045983972,0.0012050035,0.00007664335,0.00011690151,0.00024929736,0.0000034061472,0.00035896117],"genre_scores_gemma":[0.99910975,0.00013023677,0.00040897424,0.00014927663,0.00013289113,5.004414e-7,0.000035457644,0.000002679631,0.000030260851],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975225,0.00030726375,0.0008315556,0.00026923203,0.00061168155,0.00045780165],"domain_scores_gemma":[0.99822205,0.00041488835,0.0006636738,0.00020588459,0.00019350459,0.0003000244],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013680268,0.00018726478,0.00046628277,0.00029288992,0.00044128788,0.00006094056,0.0007689094,0.00009328131,0.0015983909],"category_scores_gemma":[0.000365875,0.000106846215,0.00021658815,0.001157814,0.0019311379,0.00043182768,0.000025126266,0.0003391577,0.0000078859],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033772012,0.000016049067,0.9527901,0.000009786335,0.000031597658,0.000017988204,0.0025549002,0.04264286,0.00024881362,0.000009820101,0.00003116187,0.0016131514],"study_design_scores_gemma":[0.0003205124,0.0002184211,0.983907,0.00011183194,0.000043720895,0.00006200078,0.006034467,0.00810549,0.00034287144,0.0005312671,0.00018955691,0.00013285765],"about_ca_topic_score_codex":0.21866861,"about_ca_topic_score_gemma":0.60957867,"teacher_disagreement_score":0.39091003,"about_ca_system_score_codex":0.000004091499,"about_ca_system_score_gemma":0.0005161141,"threshold_uncertainty_score":0.9993143},"labels":[],"label_agreement":null},{"id":"W2086990102","doi":"10.1139/e09-046","title":"Nature and evolution of the Slave Province subcontinental lithospheric mantleThis article is one of a series of papers published in this Special Issue on the theme <i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Craton; Geology; Eclogite; Lithosphere; Peridotite; Kimberlite; Geochemistry; Xenolith; Metasomatism; Mantle (geology); Mafic; Obduction; Crust; Subduction; Oceanic crust; Ultramafic rock; Earth science; Petrology; Tectonics; Paleontology","score_opus":0.004769447125360053,"score_gpt":0.16394706001771375,"score_spread":0.1591776128923537,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086990102","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9884497,0.0014077566,9.945708e-7,0.008126321,0.00010714267,0.00014569011,0.000032930984,7.253769e-7,0.0017287647],"genre_scores_gemma":[0.99945486,0.000043530108,0.00024060265,0.00010829705,0.000065713844,4.137281e-7,3.9549346e-7,8.0093724e-7,0.00008541546],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988475,0.00010613594,0.00038511257,0.0001364661,0.00034238258,0.00018242694],"domain_scores_gemma":[0.9988651,0.00026450417,0.0004705024,0.00011316531,0.00018982822,0.0000968497],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011575458,0.000085633204,0.0002589764,0.00007231246,0.00013105999,0.00003832337,0.00036024864,0.00007111616,0.0019435014],"category_scores_gemma":[0.0008694305,0.000036941572,0.00007326869,0.0007697196,0.002461922,0.00022785821,0.000015348769,0.00031260733,3.4890044e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011506982,0.000017304985,0.9945819,0.000039572566,0.00002080585,0.000001214356,0.0009481804,0.00005189658,0.0021573915,0.0013766319,0.000097066615,0.0005929649],"study_design_scores_gemma":[0.00036231417,0.00030389638,0.97569203,0.00010634484,0.00004092791,0.000020710693,0.0019148666,0.0005380723,0.012377484,0.008043876,0.00052959396,0.000069871916],"about_ca_topic_score_codex":0.037590224,"about_ca_topic_score_gemma":0.35603112,"teacher_disagreement_score":0.31844088,"about_ca_system_score_codex":0.0000027336682,"about_ca_system_score_gemma":0.00050929416,"threshold_uncertainty_score":0.99896884},"labels":[],"label_agreement":null},{"id":"W2087061602","doi":"10.1139/e04-079","title":"Early Carboniferous deformation and mineralization in the Cobequid shear zone, Nova Scotia: an <sup>40</sup>Ar/<sup>39</sup>Ar geochronology study","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Dalhousie University; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University","keywords":"Geology; Pluton; Shear zone; Geochemistry; Gabbro; Mafic; Mylonite; Geochronology; Carboniferous; Igneous rock; Devonian; Hornblende; Plutonism; Biotite; Geomorphology; Seismology; Paleontology; Tectonics","score_opus":0.017300172973327473,"score_gpt":0.20892524383043365,"score_spread":0.19162507085710617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087061602","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967173,0.00062226015,0.000051648716,0.001699475,0.00007740174,0.00017703066,0.000016318041,0.000005654408,0.0006329076],"genre_scores_gemma":[0.9989566,0.000020180545,0.0003660526,0.00050211174,0.00012268337,4.2705747e-7,0.000015542262,0.0000019160464,0.000014488882],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997955,0.00023174129,0.00051797193,0.00028437088,0.00044531544,0.0005655996],"domain_scores_gemma":[0.99895567,0.00009204366,0.00018471414,0.00014739814,0.00013604254,0.0004841589],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013675676,0.00017954863,0.00030355956,0.00044476532,0.00038910419,0.0002921325,0.0005681104,0.00009660463,0.0008147212],"category_scores_gemma":[0.0001603148,0.00010998308,0.00006650458,0.0010928207,0.00063543743,0.0008586076,0.000011048002,0.00030155267,0.000044176166],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015571954,0.000031875767,0.79881227,0.0000040020896,0.000013362835,0.000097876175,0.0031060607,0.19664106,0.000010727733,0.00009336656,0.000009712476,0.0011641303],"study_design_scores_gemma":[0.0005353155,0.0016851191,0.97491455,0.000022806418,0.00003726846,0.00025955425,0.004903048,0.015270342,0.000013600801,0.0020539155,0.00012744615,0.00017701487],"about_ca_topic_score_codex":0.28839305,"about_ca_topic_score_gemma":0.79829615,"teacher_disagreement_score":0.5099031,"about_ca_system_score_codex":0.0000076176325,"about_ca_system_score_gemma":0.0004970753,"threshold_uncertainty_score":0.8920626},"labels":[],"label_agreement":null},{"id":"W2087197105","doi":"10.1139/e01-005","title":"Eocambrian granite clasts in southern British Columbia shed light on Cordilleran hinterland crust","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Vernon Jubilee Hospital; Geological Survey of Canada; University of Alberta","funders":"","keywords":"Geology; Schist; Geochemistry; Proterozoic; Pluton; Zircon; Clastic rock; Biotite; Gneiss; Paleozoic; Continental crust; Petrology; Crust; Metamorphic rock; Paleontology; Quartz; Sedimentary rock; Tectonics","score_opus":0.011156012344376652,"score_gpt":0.17693457545205504,"score_spread":0.16577856310767838,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087197105","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9801929,0.0004601842,0.0000029228568,0.0011903612,0.00026430044,0.000048105852,0.000037783564,0.0000040423706,0.017799376],"genre_scores_gemma":[0.9979779,0.00003581732,0.000074580166,0.00066849316,0.00013085267,1.4294112e-7,0.0000046470645,0.000001517007,0.00110603],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851674,0.00007927265,0.00036430353,0.0002247441,0.00030939223,0.000505533],"domain_scores_gemma":[0.9989096,0.0000752073,0.00013978987,0.00007854502,0.00007903036,0.0007178526],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005568527,0.00009690919,0.00026437393,0.0002101038,0.00032033236,0.00052794174,0.0004349613,0.0000623651,0.02312134],"category_scores_gemma":[0.00015016165,0.00009068528,0.00012104564,0.0008005651,0.0003790805,0.00019161723,0.000004108553,0.00024712083,0.00014555104],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010445634,0.000007957452,0.9857534,0.0000014052978,0.0000072004955,0.00056571345,0.0001223076,0.00077218964,0.000011142934,0.0000021381238,0.00039521768,0.012350847],"study_design_scores_gemma":[0.00028795007,0.00039237083,0.98819095,0.00007835676,0.000008584386,0.00029135603,0.00046996662,0.0008950478,0.0000039428883,0.0014431124,0.007788598,0.00014978956],"about_ca_topic_score_codex":0.55539507,"about_ca_topic_score_gemma":0.99702597,"teacher_disagreement_score":0.4416309,"about_ca_system_score_codex":0.0000023896675,"about_ca_system_score_gemma":0.00025953376,"threshold_uncertainty_score":0.97777164},"labels":[],"label_agreement":null},{"id":"W2087271787","doi":"10.1139/e05-050","title":"Temporal evolution and nature of TiFeP mineralization in the anorthositemangeritecharnockitegranite (AMCG) suites of the south-central Grenville Province, Saguenay Lac St. Jean area, Quebec, Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Ministère des Ressources naturelles et des Forêts (Québec)","funders":"","keywords":"Anorthosite; Geochemistry; Charnockite; Geology; Quartz monzonite; Mafic; Pluton; Petrology; Igneous rock; Iron oxide copper gold ore deposits; Plagioclase; Granulite; Geomorphology; Structural basin; Facies","score_opus":0.006355076480370384,"score_gpt":0.16249045190877037,"score_spread":0.15613537542839998,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087271787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933528,0.0027798663,0.000004291181,0.003453033,0.000078908364,0.000078348785,0.00006792816,7.368981e-7,0.00018412324],"genre_scores_gemma":[0.99950314,0.000014519958,0.00008480143,0.00022968951,0.000054218883,1.3123064e-7,0.000008449976,7.2811514e-7,0.000104347055],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988173,0.00010562792,0.00032545763,0.000121960926,0.0003630686,0.0002665602],"domain_scores_gemma":[0.9992546,0.00011886062,0.00027388133,0.00008478953,0.00009571212,0.00017214617],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045477293,0.00009168165,0.0001771549,0.0001384603,0.00016888251,0.00004096199,0.0003856782,0.00005709036,0.00031639138],"category_scores_gemma":[0.000209643,0.00004526641,0.00006475137,0.00072764856,0.00042407104,0.00013410537,0.000006152951,0.0001987909,2.6571172e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000047523426,0.0000041319736,0.9955676,0.000006508811,0.000005533487,0.00000554254,0.0001810543,0.0032341492,0.000052465122,0.00006160439,0.000122022975,0.000754618],"study_design_scores_gemma":[0.00009171086,0.00004992363,0.99473804,0.00003971585,0.000015475054,0.0000125840925,0.00044515595,0.0021066489,0.00012569896,0.00022184577,0.0020879267,0.000065247936],"about_ca_topic_score_codex":0.9190221,"about_ca_topic_score_gemma":0.99987537,"teacher_disagreement_score":0.08085327,"about_ca_system_score_codex":0.0000048839765,"about_ca_system_score_gemma":0.00085353956,"threshold_uncertainty_score":0.3464264},"labels":[],"label_agreement":null},{"id":"W2087302749","doi":"10.1139/e02-088","title":"Late Wisconsinan stratigraphy and chronology of southern St. George's Bay, Newfoundland: a re-appraisal: Discussion","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"York University","funders":"","keywords":"Geology; Chronology; Glacial period; Stratigraphy; Bay; Paleontology; George (robot); Archaeology; Oceanography; Geography","score_opus":0.027654964971308482,"score_gpt":0.24337820367041174,"score_spread":0.21572323869910326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087302749","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98722893,0.003175839,0.000007270085,0.0032205128,0.00031091427,0.000054042186,0.000050863746,0.0000030715757,0.005948563],"genre_scores_gemma":[0.99905795,0.00012512786,0.00038997902,0.00007534945,0.00004615319,1.01038864e-7,0.000002372103,0.0000014693306,0.0003014766],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986862,0.00018374305,0.00030690499,0.000177587,0.00018554866,0.00046002644],"domain_scores_gemma":[0.9989263,0.00021849573,0.00020406517,0.00010072277,0.00007133007,0.00047911613],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008036868,0.00010578796,0.00025194927,0.00045932963,0.0003733875,0.000057170742,0.0003183414,0.00010641464,0.0047360724],"category_scores_gemma":[0.00014649073,0.00006330662,0.00005862581,0.00036934685,0.0021640449,0.00024571817,0.0000057869665,0.00026131852,0.000043160166],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008237382,0.000003904006,0.9972869,0.000007973602,0.000013973624,0.00007619496,0.00060097914,0.00014285363,0.0000065421664,0.00009147417,0.00008623567,0.0016747048],"study_design_scores_gemma":[0.00028069678,0.0006646933,0.9904294,0.00004009411,0.000012180891,0.00041458462,0.001029877,0.0013259063,0.000008435795,0.0016114138,0.00407497,0.00010775383],"about_ca_topic_score_codex":0.008444006,"about_ca_topic_score_gemma":0.84832823,"teacher_disagreement_score":0.8398842,"about_ca_system_score_codex":2.5892618e-7,"about_ca_system_score_gemma":0.00041068386,"threshold_uncertainty_score":0.9981589},"labels":[],"label_agreement":null},{"id":"W2087519825","doi":"10.1139/e03-014","title":"Geochemistry and SrNd isotopic composition of Eocene lamphrophyre dykes, southeastern British Columbia","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Social Sciences and Humanities Research Council; Natural Sciences and Engineering Research Council of Canada; BP (Canada)","funders":"","keywords":"Geology; Geochemistry; Mantle (geology); Plagioclase; Partial melting; Incompatible element; Mafic; Mineralogy; Quartz; Paleontology","score_opus":0.008929472536361126,"score_gpt":0.16764281217502455,"score_spread":0.15871333963866344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087519825","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993011,0.0019699263,0.000009136331,0.00013828756,0.00007879171,0.000026968943,0.000045333043,0.0000015700217,0.004719013],"genre_scores_gemma":[0.9989862,0.000037151767,0.00067373645,0.00009650932,0.000034903274,6.104053e-8,0.0000043189907,6.568709e-7,0.00016648266],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99913466,0.000045303528,0.00024895012,0.00013470065,0.0001903387,0.0002460603],"domain_scores_gemma":[0.9992244,0.000049213773,0.00014944031,0.000051537216,0.00009625755,0.00042913563],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031820947,0.000058685993,0.00018722854,0.000050035746,0.00022625693,0.00018187732,0.00017270375,0.000045581222,0.006952607],"category_scores_gemma":[0.00008130858,0.00005942938,0.00006281271,0.000273505,0.0005915223,0.00012975326,0.0000029309724,0.00010203452,0.0000055832634],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001452246,0.000004123259,0.9979233,0.000008489716,0.000008265676,0.00003500894,0.000028289094,0.00010918853,0.00022183132,0.000008632655,0.000051705887,0.0015997181],"study_design_scores_gemma":[0.00018026626,0.00016713378,0.99196696,0.000053469586,0.000021642,0.00043131757,0.00022913865,0.00027362272,0.00055632857,0.0051039485,0.00091028045,0.000105904095],"about_ca_topic_score_codex":0.13165067,"about_ca_topic_score_gemma":0.769243,"teacher_disagreement_score":0.6375923,"about_ca_system_score_codex":5.418486e-7,"about_ca_system_score_gemma":0.00024872398,"threshold_uncertainty_score":0.9939552},"labels":[],"label_agreement":null},{"id":"W2087971375","doi":"10.1139/e06-133","title":"A new hexactinellid sponge from the Cretaceous of Devon Island, Canadian High Arctic","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Office of Polar Programs","keywords":"Sponge spicule; Geology; Paleontology; Cretaceous; Arctic; Sponge; Genus; Context (archaeology); Biology; Oceanography; Zoology","score_opus":0.01811155693005585,"score_gpt":0.21158714673699378,"score_spread":0.19347558980693794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087971375","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96921057,0.014286535,0.00013429027,0.0015174245,0.0010046099,0.000073764015,0.0002650866,0.0000016577225,0.013506057],"genre_scores_gemma":[0.9979797,0.000042312793,0.0014045553,0.00024978592,0.000260228,2.8928286e-8,0.00000599551,7.81958e-7,0.000056592937],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99850357,0.000079591904,0.00038400324,0.00015402566,0.0002958505,0.00058293884],"domain_scores_gemma":[0.99776465,0.00047564416,0.00026069765,0.00013218613,0.00009733557,0.0012694631],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013634876,0.00012184441,0.00022000703,0.00035181575,0.0005082943,0.00009684096,0.0006848414,0.000088048575,0.0053068036],"category_scores_gemma":[0.00020196468,0.00007910978,0.00010159859,0.0005484157,0.00060546485,0.00028923957,6.6696646e-7,0.00027287568,0.000014434558],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001728643,0.0000011131649,0.9668272,0.0000014857533,0.000022536853,0.00020142624,0.000517797,0.00012817756,0.000006432144,0.000084547624,0.00040991144,0.03178208],"study_design_scores_gemma":[0.0001529576,0.00022931476,0.98627913,0.00003996378,0.000021430324,0.00018592556,0.0005128747,0.0000429567,0.00007482209,0.001491328,0.010869418,0.000099857265],"about_ca_topic_score_codex":0.95988417,"about_ca_topic_score_gemma":0.9998455,"teacher_disagreement_score":0.03996134,"about_ca_system_score_codex":0.0000028885813,"about_ca_system_score_gemma":0.004154586,"threshold_uncertainty_score":0.9956025},"labels":[],"label_agreement":null},{"id":"W2088083669","doi":"10.1139/e04-058","title":"Holocene tree line, permafrost, and climate dynamics in the Nenets Region, East European Arctic","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Macrofossil; Permafrost; Holocene; Tundra; Mire; Peat; Geology; Tree line; Physical geography; Chronology; Arctic; Taiga; Aggradation; Climate change; Oceanography; Geomorphology; Forestry; Paleontology; Archaeology; Geography","score_opus":0.028712263028669503,"score_gpt":0.22838830099197882,"score_spread":0.19967603796330932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088083669","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98203975,0.0017666186,0.000007063531,0.0069731683,0.0001847456,0.000057712543,0.000016519894,0.0000018855515,0.008952507],"genre_scores_gemma":[0.9988855,0.00022535675,0.0001840397,0.00061966217,0.000061082705,9.347247e-8,0.000005582108,0.0000014293073,0.000017220455],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986386,0.0002747682,0.0002416197,0.00015242322,0.00018151866,0.0005111071],"domain_scores_gemma":[0.999285,0.0001161914,0.0001054148,0.000098412325,0.00006218388,0.00033278804],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019299805,0.00009046795,0.0001394869,0.00031751557,0.0005068943,0.00012533471,0.0005224545,0.000045675362,0.00008557498],"category_scores_gemma":[0.00015365139,0.000057348367,0.000034965167,0.00045641343,0.0012096508,0.0002450979,0.0000063187895,0.00034007474,0.00003890576],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007303371,0.000003009349,0.9960412,0.0000053417843,0.0000025739341,0.0008160097,0.00052216277,0.0015430456,1.4418204e-7,0.00042054107,0.000006746548,0.0006319581],"study_design_scores_gemma":[0.00025434568,0.00028719197,0.99291205,0.00004414233,0.0000050382946,0.0032588104,0.0014270257,0.0006902735,9.293645e-7,0.0009453688,0.00010508085,0.00006975986],"about_ca_topic_score_codex":0.0038284338,"about_ca_topic_score_gemma":0.78884894,"teacher_disagreement_score":0.78502053,"about_ca_system_score_codex":0.0000011533034,"about_ca_system_score_gemma":0.000562226,"threshold_uncertainty_score":0.5787472},"labels":[],"label_agreement":null},{"id":"W2088491583","doi":"10.1139/e03-089","title":"Large Holocene landslides from Pylon Peak, southwestern British Columbia","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; Geological Survey of Canada; Squamish Nation","funders":"University of Washington","keywords":"Geology; Landslide; Pyroclastic rock; Massif; Volcano; Debris; Holocene; Geochemistry; Geomorphology; Stratovolcano; Rockfall; Explosive eruption; Tephra; Paleontology; Oceanography","score_opus":0.008145686584842592,"score_gpt":0.19275420805075388,"score_spread":0.18460852146591128,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088491583","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99473894,0.00046323033,0.000058195168,0.0003041192,0.00045251998,0.000045644836,0.00006002454,0.0000061343594,0.0038711787],"genre_scores_gemma":[0.99825644,0.000049474937,0.0006628726,0.00036607138,0.00012369307,3.4496696e-7,0.0000022301158,0.000006768966,0.00053210946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998701,0.000026713125,0.00026348667,0.00019339361,0.00034679528,0.00046860988],"domain_scores_gemma":[0.9990495,0.000019396351,0.00015421343,0.00009673881,0.000021829206,0.00065832405],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048742373,0.000077917626,0.00016391223,0.0000482232,0.0005429505,0.0006466401,0.00044632837,0.000077301265,0.004266181],"category_scores_gemma":[0.000053167496,0.00008032095,0.00008504278,0.00031652264,0.00044504207,0.00040702207,0.0000309392,0.00019509652,0.00014834924],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000019045406,0.000014049504,0.99521536,0.0000010124769,0.000010507063,0.00047429567,0.00064003,0.0014922734,0.00007437777,0.0000072197545,0.0008478474,0.0012211081],"study_design_scores_gemma":[0.00063841254,0.00018299709,0.9793191,0.000097198135,0.00001651923,0.00031377698,0.0004976682,0.00003083223,0.000059047008,0.001876236,0.016808713,0.00015949247],"about_ca_topic_score_codex":0.3922119,"about_ca_topic_score_gemma":0.9526049,"teacher_disagreement_score":0.560393,"about_ca_system_score_codex":0.00002625336,"about_ca_system_score_gemma":0.0003970293,"threshold_uncertainty_score":0.9966441},"labels":[],"label_agreement":null},{"id":"W2088517302","doi":"10.1139/e00-088","title":"Late 18th century drought-induced sand dune activity, Great Sand Hills, Saskatchewan","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Regina; Mount Allison University; Université de Montréal; Simon Fraser University; Geological Survey of Canada","funders":"","keywords":"Sand dune stabilization; Foothills; Geology; Physical geography; Quaternary; Precipitation; Climate change; Geomorphology; Geography; Paleontology; Oceanography","score_opus":0.01796335227210349,"score_gpt":0.21687091369632533,"score_spread":0.19890756142422183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088517302","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98619264,0.0020849055,0.000024176876,0.0011197287,0.001077283,0.00009288411,0.000030726984,0.000008966461,0.009368699],"genre_scores_gemma":[0.9982673,0.0002273229,0.0002784665,0.00038768316,0.00039210796,1.4839684e-7,0.0000035837375,0.0000043858786,0.00043899944],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99813116,0.00008542993,0.00028959694,0.00027031044,0.00045183746,0.00077166304],"domain_scores_gemma":[0.998177,0.000108516084,0.00025960372,0.00013647205,0.00010759865,0.0012107919],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007865845,0.00019966213,0.00030275737,0.000342459,0.0007078205,0.0003647703,0.00053589774,0.00009333039,0.0023268757],"category_scores_gemma":[0.00008703634,0.00014773628,0.000095707524,0.0008489919,0.00037188362,0.0010160678,0.000007805725,0.00028597467,0.00008954997],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000051297277,0.000012000204,0.9186985,0.000025885409,0.000035361852,0.00095888134,0.0011785543,0.003082708,0.0003595365,0.000012589761,0.00080758426,0.074777134],"study_design_scores_gemma":[0.0006587182,0.0012351273,0.95949125,0.00017603001,0.00004136306,0.0011424796,0.0007470094,0.003926667,0.001116513,0.0008992008,0.030085297,0.00048033567],"about_ca_topic_score_codex":0.048864324,"about_ca_topic_score_gemma":0.532821,"teacher_disagreement_score":0.48395666,"about_ca_system_score_codex":0.0000047567123,"about_ca_system_score_gemma":0.0020048933,"threshold_uncertainty_score":0.9985851},"labels":[],"label_agreement":null},{"id":"W2089111355","doi":"10.1139/cjes-2013-0106","title":"Evidence for an Early Pleistocene glaciation in the Okanagan Valley, southern British Columbia","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Thompson Rivers University; University of British Columbia, Okanagan Campus; University of Northern British Columbia; Simon Fraser University; Kelowna General Hospital; University of Lethbridge; Agriculture and Agri-Food Canada; Okanagan University College","funders":"","keywords":"Geology; Pleistocene; Glacial period; Paleontology; Lithology; Basalt; Paleosol; Outcrop; Sedimentary depositional environment; Quaternary; Fluvial; Geomorphology; Structural basin; Loess","score_opus":0.06372391487986603,"score_gpt":0.2600115797161299,"score_spread":0.1962876648362639,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089111355","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99638635,0.0010897813,0.000012472615,0.0011580775,0.00020800589,0.000251208,0.000014026652,0.0000020141865,0.00087803754],"genre_scores_gemma":[0.9988966,0.00002383515,0.00036641743,0.0003590389,0.00007837901,0.0000020301009,0.000002887066,0.0000011939171,0.00026962173],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986452,0.00024880562,0.0002513977,0.00015313302,0.0002373993,0.0004641034],"domain_scores_gemma":[0.99884635,0.00046604156,0.00012656636,0.000092953436,0.00015831739,0.00030975556],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002276904,0.000055001285,0.0001343569,0.00013598183,0.0006298093,0.0007323592,0.00072343514,0.000068839014,0.0018349051],"category_scores_gemma":[0.00046079708,0.00005072745,0.00004755286,0.00036947313,0.0005726067,0.0007776481,0.0000023705575,0.00019947764,0.00007958715],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000040884224,0.00000278567,0.996351,0.00000331629,0.0000028246186,0.000023012628,0.00061274105,0.00018565486,8.652771e-7,0.00000643862,0.0002552406,0.0025520097],"study_design_scores_gemma":[0.00013406923,0.00063296757,0.99475104,0.000041219006,0.0000042362067,0.0001856668,0.0011557558,0.00078516075,5.8524097e-7,0.0020515,0.00019122272,0.000066553024],"about_ca_topic_score_codex":0.54224443,"about_ca_topic_score_gemma":0.99804765,"teacher_disagreement_score":0.45580322,"about_ca_system_score_codex":6.7407854e-7,"about_ca_system_score_gemma":0.0009255976,"threshold_uncertainty_score":0.99907756},"labels":[],"label_agreement":null},{"id":"W2089125195","doi":"10.1139/e09-018","title":"Modeling topographical density for geoid determinationThis article is one of a series of papers published in this Special Issue on the theme<i>GEODESY</i>.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Geoid; Geodesy; Geology; Terrain; Gravitational field; Undulation of the geoid; Gravity of Earth; Series (stratigraphy); Geophysics; Computation; Physics; Classical mechanics; Geography; Mathematics; Algorithm","score_opus":0.03064039287640072,"score_gpt":0.21399202697908998,"score_spread":0.18335163410268926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089125195","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915771,0.00006630296,0.000009632302,0.0040156464,0.00020875834,0.00011044857,0.000024499066,7.925064e-7,0.0039868127],"genre_scores_gemma":[0.99887097,0.000012107859,0.0004228261,0.000442873,0.00021506671,1.5951373e-7,8.266195e-7,8.5809853e-7,0.000034305373],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988468,0.00004895843,0.0003271702,0.000115774805,0.0004114792,0.00024978572],"domain_scores_gemma":[0.9992818,0.00008096034,0.00016170922,0.00009366087,0.00021031107,0.00017152399],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012968119,0.00007346371,0.00018362812,0.00022333516,0.0002048183,0.00008377507,0.00031691615,0.00003556946,0.002003327],"category_scores_gemma":[0.00026068607,0.000049552407,0.00009139227,0.0004737466,0.00025089004,0.0003494813,0.0000021041735,0.000114955255,0.0000018615842],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002888154,0.00014918935,0.87549055,0.000039308343,0.000062599334,0.000023598974,0.0077213002,0.02277521,0.0022744,0.0038784193,0.0010820174,0.0862146],"study_design_scores_gemma":[0.00056647125,0.0018949715,0.9331142,0.00017760988,0.000029870003,0.000013072626,0.0013211477,0.018277612,0.009174233,0.032925006,0.0022865236,0.00021929717],"about_ca_topic_score_codex":0.0082146935,"about_ca_topic_score_gemma":0.19044833,"teacher_disagreement_score":0.18223365,"about_ca_system_score_codex":0.0000018302027,"about_ca_system_score_gemma":0.00039291568,"threshold_uncertainty_score":0.998909},"labels":[],"label_agreement":null},{"id":"W2089205495","doi":"10.1139/e05-071","title":"Cordierite-gedrite rocks from the Central Metasedimentary Belt boundary thrust zone (Grenville Province, Ontario): Mesoproterozoic metavolcanic rocks with affinities to the Composite Arc Belt","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Protolith; Metamorphism; Volcanic rock; Petrology; Zircon; Felsic; Mafic; Volcano","score_opus":0.012236339773038557,"score_gpt":0.17741118117991167,"score_spread":0.1651748414068731,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089205495","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97670627,0.004716552,0.00015477944,0.015376968,0.00028613704,0.00025087633,0.0002785934,0.0000069492517,0.0022228777],"genre_scores_gemma":[0.9916708,0.000030984993,0.002118411,0.0052902647,0.0004174736,0.0000016454392,0.000055441284,0.000003354893,0.000411652],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99737906,0.00017822564,0.00048662795,0.0003544356,0.0007486895,0.0008529791],"domain_scores_gemma":[0.9981234,0.00028057082,0.0002690188,0.00024407862,0.00012280661,0.00096011534],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007623949,0.00027260216,0.0004127206,0.0001570286,0.0016791685,0.00050841563,0.0012523315,0.000054896333,0.011293777],"category_scores_gemma":[0.000040781782,0.00012507376,0.0002015096,0.0006433762,0.00097300485,0.00042384551,0.000033738375,0.00052986096,0.000070847396],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009094073,0.000021850436,0.96052134,0.0000026457135,0.00022665443,0.00009967605,0.001526532,0.023547098,0.00005778987,0.000010750315,0.0016442582,0.012250447],"study_design_scores_gemma":[0.00037717656,0.0008611178,0.85506815,0.00006771983,0.00026717642,0.00015261273,0.0016495892,0.00088623527,0.000437123,0.0005153954,0.13936007,0.00035761646],"about_ca_topic_score_codex":0.7260624,"about_ca_topic_score_gemma":0.99726176,"teacher_disagreement_score":0.27119938,"about_ca_system_score_codex":0.000015971904,"about_ca_system_score_gemma":0.0015857809,"threshold_uncertainty_score":0.9996205},"labels":[],"label_agreement":null},{"id":"W2089309076","doi":"10.1139/e04-026","title":"The Lower Devonian Compton Formation in southern Quebec: from delta front to pro-delta sedimentation","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Université du Québec à Montréal","keywords":"Geology; Devonian; Delta; Facies; Paleontology; Sedimentary rock; Conglomerate; Front (military); Geochemistry; Oceanography","score_opus":0.0189872018897052,"score_gpt":0.2167042674132621,"score_spread":0.1977170655235569,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089309076","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940169,0.00054384436,0.00051958836,0.0034964918,0.00033956463,0.00011139921,0.000057545163,0.0000029824027,0.00091169175],"genre_scores_gemma":[0.9978518,0.00001171255,0.0015617943,0.00045259984,0.000057262787,4.7496076e-7,0.000013845592,8.637895e-7,0.00004966333],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990259,0.000039754523,0.0003157899,0.00008949906,0.00024712682,0.0002819439],"domain_scores_gemma":[0.9993224,0.00007455873,0.00014117944,0.000058859347,0.00009623063,0.0003067612],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005553115,0.00007430007,0.0000935023,0.00017468922,0.00053760654,0.00032057226,0.00034825626,0.000033307064,0.0007412593],"category_scores_gemma":[0.00008546852,0.000044098466,0.000030228352,0.00035062747,0.0001597148,0.0007502705,0.0000033782978,0.00010844678,0.00015232632],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007096076,0.000025269426,0.6325572,0.000010224888,0.000015894284,0.000058899208,0.021971108,0.26263377,0.000032461776,0.000391099,0.00043982491,0.08179329],"study_design_scores_gemma":[0.000511805,0.0007408529,0.95422834,0.00013488483,0.000008606733,0.000050022205,0.0137916645,0.0035220643,0.00025448267,0.009230688,0.017295193,0.00023141602],"about_ca_topic_score_codex":0.38499132,"about_ca_topic_score_gemma":0.9892892,"teacher_disagreement_score":0.60429794,"about_ca_system_score_codex":0.0000071921318,"about_ca_system_score_gemma":0.0006561467,"threshold_uncertainty_score":0.811627},"labels":[],"label_agreement":null},{"id":"W2089512180","doi":"10.1139/e04-078","title":"High-resolution stratigraphy of the deep-water lower Cloridorme Formation (Ordovician), Gaspé Peninsula, based on K-bentonite and megaturbidite correlations","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Geological Society of America","keywords":"Geology; Stratigraphy; Ordovician; Paleontology; Foreland basin; Turbidite; Sedimentary rock; Subdivision; Lithostratigraphy; Structural basin; Tectonics; Archaeology","score_opus":0.013052178722278217,"score_gpt":0.18725364970726363,"score_spread":0.17420147098498542,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089512180","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942283,0.00036531614,0.0005711151,0.0018245543,0.00051611033,0.00008971154,0.000035554778,0.0000027632746,0.002366577],"genre_scores_gemma":[0.99856484,0.000021188933,0.0010481941,0.00030141795,0.000040572835,2.1253376e-7,0.000008244154,7.995732e-7,0.0000145342965],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9990771,0.00004177758,0.00028933858,0.000081950515,0.00027738637,0.00023245413],"domain_scores_gemma":[0.99934286,0.000059925842,0.00018547293,0.00007381281,0.00013166484,0.00020625912],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042833155,0.0000820791,0.00010546766,0.00027818943,0.0006086104,0.00011783596,0.00021474886,0.000046300986,0.0005011001],"category_scores_gemma":[0.00006610763,0.00004344643,0.000059651953,0.00046647838,0.00039352718,0.0007125825,0.0000025841414,0.0001417466,0.000011714889],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023738445,0.000013076411,0.2432088,0.000015571499,0.000007523445,0.0000068370546,0.0005974969,0.7513168,0.000038883587,0.003212703,0.000039201543,0.0015193698],"study_design_scores_gemma":[0.0003822525,0.0007437474,0.96193403,0.00009969388,0.000017431525,0.000052659827,0.00031495973,0.023141127,0.00064110284,0.010127476,0.0024188727,0.00012663496],"about_ca_topic_score_codex":0.004954026,"about_ca_topic_score_gemma":0.18494911,"teacher_disagreement_score":0.7281757,"about_ca_system_score_codex":0.0000022489376,"about_ca_system_score_gemma":0.00036574877,"threshold_uncertainty_score":0.82992345},"labels":[],"label_agreement":null},{"id":"W2089710398","doi":"10.1139/e00-057","title":"Mantle flow mechanisms of epeirogeny and their possible role in the evolution of the Western Canada Sedimentary Basin","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Craton; Subduction; Mantle (geology); Sedimentary rock; Paleontology; Sedimentary basin; Ocean surface topography; Tectonics","score_opus":0.00634513744990845,"score_gpt":0.15403019161838027,"score_spread":0.14768505416847183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089710398","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954801,0.0011193275,0.0000047227995,0.0020422277,0.000057460064,0.000037640115,0.0000529134,3.3061735e-7,0.0012052632],"genre_scores_gemma":[0.9993269,0.000013094195,0.0001132418,0.0004778386,0.000016249794,7.0118105e-8,0.000001000073,3.946044e-7,0.000051217183],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991808,0.000093503666,0.00022222397,0.000083494415,0.00022758055,0.00019242679],"domain_scores_gemma":[0.99957734,0.00008065826,0.00010203271,0.000071943454,0.000031765016,0.00013627115],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005546334,0.0000617723,0.0001381499,0.00006641305,0.00014323845,0.000020368903,0.00040656634,0.000022000484,0.0017124102],"category_scores_gemma":[0.000022506947,0.000027431968,0.00005047348,0.0004548221,0.00030288735,0.00009800499,0.000003928769,0.00009504684,0.0000011110968],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004493416,0.0000037646264,0.99259084,0.0000026694038,0.0000058962783,0.000005825348,0.00021812602,0.0039949603,0.00010178063,0.000029719658,0.000044482797,0.0029974359],"study_design_scores_gemma":[0.000072692346,0.00009899743,0.98554254,0.000022591317,0.000009306804,0.00004644729,0.0014097864,0.0023278687,0.001187283,0.008706288,0.0005317467,0.000044435255],"about_ca_topic_score_codex":0.92062443,"about_ca_topic_score_gemma":0.9943661,"teacher_disagreement_score":0.07374168,"about_ca_system_score_codex":0.0000027766612,"about_ca_system_score_gemma":0.000771577,"threshold_uncertainty_score":0.99920017},"labels":[],"label_agreement":null},{"id":"W2089967163","doi":"10.1139/e03-060","title":"Microbes and mineral precipitation, Miette Hot Springs, Jasper National Park, Alberta, Canada","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Mine drainage and remediation techniques","field":"Environmental Science","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Waterloo; University of Alberta; Parks Canada","keywords":"Calcite; Hot spring; Microbial mat; Geology; Algal mat; Gypsum; Chemosynthesis; Lyngbya; Cyanobacteria; Algae; Mineral; Mineralogy; Geochemistry; Environmental chemistry; Botany; Chemistry; Hydrothermal vent; Ecology; Biology; Paleontology; Bacteria","score_opus":0.008146145953823713,"score_gpt":0.20014918660780814,"score_spread":0.19200304065398444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089967163","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97368634,0.00021342188,0.000041208517,0.001483767,0.00020632587,0.000058204045,0.00000461873,0.0000015393417,0.024304556],"genre_scores_gemma":[0.99428815,0.000013621756,0.0026881625,0.00090587523,0.000041005183,8.163307e-7,5.977333e-7,0.0000028953648,0.0020588725],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99910885,0.00003958616,0.00020033002,0.000121009376,0.000316736,0.00021347468],"domain_scores_gemma":[0.9994026,0.000060682458,0.00012123182,0.000040031995,0.00004976685,0.0003257028],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005044963,0.00007284679,0.00008387159,0.0000945426,0.00023315815,0.00006804818,0.00015937773,0.000025895366,0.0012281737],"category_scores_gemma":[0.00032163397,0.00005878687,0.000022690116,0.00022065426,0.00031433874,0.00029700832,0.000007232381,0.00007498326,0.000007544893],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005841748,0.000023477178,0.82013,0.000012319425,0.00002766481,0.00008086786,0.0028039487,0.0014534044,0.01698759,0.0036723202,0.15310185,0.0017006979],"study_design_scores_gemma":[0.0003071968,0.0001609358,0.341445,0.000038068436,0.000010013357,0.00029305724,0.0006077425,0.00016114138,0.015644861,0.0024435725,0.6385557,0.0003326786],"about_ca_topic_score_codex":0.5635711,"about_ca_topic_score_gemma":0.98991835,"teacher_disagreement_score":0.48545387,"about_ca_system_score_codex":0.000032022283,"about_ca_system_score_gemma":0.0011282342,"threshold_uncertainty_score":0.9996848},"labels":[],"label_agreement":null},{"id":"W2090061715","doi":"10.1139/e01-020","title":"Lithospheric structure across the craton-Cordilleran transition of northeastern British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Saskatchewan; University of Victoria; University of British Columbia","funders":"","keywords":"Geology; Foreland basin; Craton; Crust; Terrane; Underplating; Lithosphere; Rift; Seismology; Passive margin; Seismic refraction; Tectonics; Paleontology","score_opus":0.008955699986798415,"score_gpt":0.19308262647727573,"score_spread":0.18412692649047732,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090061715","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99638224,0.0014265949,0.000059984937,0.00055954594,0.00033179933,0.000044827095,0.0002071887,0.000001775243,0.0009860626],"genre_scores_gemma":[0.99888617,0.00008594862,0.00019050212,0.00042176803,0.00014686726,3.8404565e-8,0.000004646254,0.0000016852217,0.00026237773],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988355,0.000062087274,0.0003178353,0.0001275759,0.0003113212,0.00034567626],"domain_scores_gemma":[0.9991985,0.000049075206,0.00020857842,0.000091116985,0.00012364326,0.00032908743],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00049314083,0.00006774829,0.00019170113,0.000035071982,0.0010247845,0.00092225417,0.00042854465,0.00003969121,0.0039060533],"category_scores_gemma":[0.000028618313,0.000057945508,0.00012370296,0.00075617124,0.0006248819,0.0003226115,0.0000015539515,0.00013795291,0.0000042775478],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000034855145,0.0000023156426,0.95213217,0.0000036759764,0.000019986437,0.00009176757,0.0005608966,0.010201254,0.000007892517,0.0000011247066,0.0001732729,0.036802176],"study_design_scores_gemma":[0.0001341705,0.00017840187,0.9821124,0.000047474383,0.000019897365,0.00055775855,0.0029664726,0.0041390867,0.000004970783,0.00039674708,0.009348274,0.00009436027],"about_ca_topic_score_codex":0.5830493,"about_ca_topic_score_gemma":0.9929747,"teacher_disagreement_score":0.40992537,"about_ca_system_score_codex":0.0000010909515,"about_ca_system_score_gemma":0.00048402173,"threshold_uncertainty_score":0.9970045},"labels":[],"label_agreement":null},{"id":"W2090246508","doi":"10.1139/e99-120","title":"The Lithoprobe Abitibi-Grenville transect: two billion years of crust formation and recycling in the Precambrian Shield of Canada","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":129,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Crust; Archean; Precambrian; Orogeny; Accretion (finance); Geochemistry; Proterozoic; Lithosphere; Tectonics; Subduction; Earth science; Petrology; Paleontology","score_opus":0.012220125720302455,"score_gpt":0.18169289133717356,"score_spread":0.1694727656168711,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090246508","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9925735,0.0011902923,0.0000021467863,0.0019173336,0.00004221229,0.00004316748,0.000012711574,3.3196525e-7,0.0042183227],"genre_scores_gemma":[0.999551,0.00015313961,0.00009637661,0.00015306498,0.00002233288,9.3701345e-8,8.949127e-7,3.6256384e-7,0.00002275586],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990924,0.000083524064,0.00030602244,0.00006939584,0.0002457417,0.00020291068],"domain_scores_gemma":[0.99938595,0.00026056523,0.00012349269,0.000054985303,0.000034786844,0.00014024615],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010768536,0.00004789858,0.000120465236,0.0000784339,0.00018283866,0.000040105864,0.00027284032,0.000020970196,0.0007405284],"category_scores_gemma":[0.00010505073,0.00002439301,0.00003980875,0.0004744809,0.0003362869,0.00012342825,0.0000012776131,0.00011323323,6.3065556e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003950851,0.000008028178,0.7277406,0.00001702465,0.000015358652,0.000036423247,0.0018195807,0.018493062,0.00014672868,0.00020399921,0.00012085018,0.25135884],"study_design_scores_gemma":[0.00012845505,0.0001597777,0.9914385,0.0000434202,0.000010066773,0.00004613759,0.0009619195,0.0025963234,0.0001941502,0.0019051966,0.002459751,0.000056301586],"about_ca_topic_score_codex":0.8111276,"about_ca_topic_score_gemma":0.9974487,"teacher_disagreement_score":0.26369792,"about_ca_system_score_codex":0.0000011368747,"about_ca_system_score_gemma":0.00039746147,"threshold_uncertainty_score":0.81082666},"labels":[],"label_agreement":null},{"id":"W2090562651","doi":"10.1139/e04-022","title":"The effects of strike-slip motion along the Cobequid - Chedabucto - southwest Grand Banks fault system on the Cretaceous-Tertiary evolution of Atlantic Canada","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Saint Mary's University","funders":"","keywords":"Geology; Cretaceous; Fault (geology); Rift; Strike-slip tectonics; Paleontology; Structural basin; Seismology; Tectonics; Plate tectonics; Echelon formation; Transform fault","score_opus":0.006902355256008108,"score_gpt":0.16312588947942544,"score_spread":0.15622353422341734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090562651","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935357,0.002782517,0.00003315903,0.002782888,0.0003556954,0.0001207709,0.000022929718,0.0000019094743,0.0003644132],"genre_scores_gemma":[0.9997411,0.000027880193,0.000012888761,0.0001294354,0.00007013185,3.6640324e-7,0.0000023896794,0.0000010446329,0.000014767116],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99839264,0.00016116085,0.00040702792,0.00013307204,0.0005580238,0.00034805713],"domain_scores_gemma":[0.9983187,0.0007619568,0.0003663924,0.00014796307,0.00015106177,0.00025397673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010147145,0.00011526708,0.00021077468,0.00008111393,0.0007366966,0.000072144976,0.0006607511,0.000043142823,0.00013322158],"category_scores_gemma":[0.00045890146,0.00004548642,0.00012335833,0.00055245374,0.00081413484,0.00010071485,0.000006726991,0.00020544526,0.000004422027],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028155942,0.00000826475,0.9703064,0.00005315762,0.00006678863,0.0000553493,0.00033884944,0.026456473,0.0002152364,0.00089988403,0.00011924145,0.0014521973],"study_design_scores_gemma":[0.00020425713,0.00035073675,0.99406505,0.00019203467,0.00006685196,0.000070261376,0.0011459814,0.0012095737,0.0012070814,0.0010360464,0.00036019276,0.00009196065],"about_ca_topic_score_codex":0.836848,"about_ca_topic_score_gemma":0.98983467,"teacher_disagreement_score":0.15298663,"about_ca_system_score_codex":0.000012172786,"about_ca_system_score_gemma":0.0012371622,"threshold_uncertainty_score":0.5666149},"labels":[],"label_agreement":null},{"id":"W2090656147","doi":"10.1139/e03-009","title":"First Middle Ordovician biota from southern New Brunswick: stratigraphic and tectonic implications for the evolution of the Avalon continent","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ordovician; Geology; Laurentia; Trilobite; Baltica; Paleontology; Paleozoic; Precambrian; Devonian; Outcrop; Gondwana; Tectonics","score_opus":0.025648455247468276,"score_gpt":0.20926919114038267,"score_spread":0.1836207358929144,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090656147","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9606541,0.032003153,0.00032147625,0.0041500125,0.000349161,0.0001773917,0.000102233855,0.0000018330956,0.002240658],"genre_scores_gemma":[0.99916846,0.000056963556,0.00065689214,0.00004350247,0.000044172368,2.0241959e-7,3.5648253e-7,5.10159e-7,0.000028952929],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99923027,0.00006152749,0.00024309666,0.000119328644,0.00011260873,0.00023315579],"domain_scores_gemma":[0.99903786,0.00030109138,0.00023864003,0.00012567558,0.000065966065,0.00023078096],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005130369,0.0000790726,0.00012303832,0.000114371804,0.00091617915,0.000074151765,0.00038751148,0.000049392045,0.000084254934],"category_scores_gemma":[0.00012676243,0.000043050823,0.00009765946,0.00038520567,0.00084102247,0.00013013631,5.942437e-7,0.00011239804,7.3826277e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000033591946,0.00000184938,0.9938991,0.0000019172735,0.000017330862,3.044801e-7,0.00036429192,0.00016562053,0.000025395406,0.002936596,0.000024910874,0.0025593275],"study_design_scores_gemma":[0.00015247178,0.00011918838,0.9924045,0.000031737094,0.000030200912,0.000024313864,0.0011220989,0.00020553316,0.000027974542,0.004910299,0.0009162015,0.000055457134],"about_ca_topic_score_codex":0.1472914,"about_ca_topic_score_gemma":0.9810629,"teacher_disagreement_score":0.83377147,"about_ca_system_score_codex":0.0000012075955,"about_ca_system_score_gemma":0.0028359746,"threshold_uncertainty_score":0.8583869},"labels":[],"label_agreement":null},{"id":"W2090697157","doi":"10.1139/e05-104","title":"A preliminary radiolarian biozonation for the Lower Silurian of the Cape Phillips Formation, Nunavut, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University","funders":"Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; St. Francis Xavier University","keywords":"Biozone; Assemblage (archaeology); Geology; Paleontology; Biostratigraphy; Radiolaria; Ordovician; Stratigraphy; Cape; Tectonics; Archaeology; Geography","score_opus":0.012654220825008907,"score_gpt":0.1871622618552972,"score_spread":0.17450804103028827,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090697157","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9694389,0.010333561,0.00022275676,0.008606036,0.0019757769,0.00028747102,0.00018341166,0.0000021621909,0.008949887],"genre_scores_gemma":[0.99941224,0.0000092188475,0.0002605478,0.00013509978,0.00014220986,4.2801003e-7,0.0000015775402,4.880039e-7,0.000038178547],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898416,0.000067381116,0.00032468888,0.00008495167,0.00026933232,0.00026946884],"domain_scores_gemma":[0.99902934,0.00027024912,0.0003207901,0.00010047323,0.00013583497,0.00014332341],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007623652,0.000079738165,0.000117952906,0.000111817935,0.00091049605,0.00006362144,0.0005582618,0.000046769066,0.000094196126],"category_scores_gemma":[0.00011658729,0.000042469754,0.00009485869,0.00036275835,0.00056101225,0.000353251,7.066104e-7,0.00012161014,3.5892938e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000045674857,0.000009283981,0.96359897,0.000016502072,0.00003360601,0.000017756658,0.0004687724,0.008991227,0.000034691526,0.001637563,0.0053654546,0.019780476],"study_design_scores_gemma":[0.00014145818,0.00021510154,0.9875783,0.000023852384,0.000018369288,0.00010625384,0.00030927296,0.0026858975,0.00012304979,0.0011294554,0.0076074298,0.0000616127],"about_ca_topic_score_codex":0.61883986,"about_ca_topic_score_gemma":0.99841774,"teacher_disagreement_score":0.37957785,"about_ca_system_score_codex":0.000002743295,"about_ca_system_score_gemma":0.0030019318,"threshold_uncertainty_score":0.70028913},"labels":[],"label_agreement":null},{"id":"W2091086103","doi":"10.1139/e02-024","title":"Geochronologic and thermobarometric constraints on the metamorphic history of the Fairbanks Mining District, western Yukon-Tanana terrane, Alaska","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Biotite; Geochemistry; Metamorphic rock; Terrane; Metamorphic facies; Eclogite; Metamorphism; Closure temperature; Schist; Amphibole; Geochronology; Geomorphology; Subduction; Facies; Quartz; Paleontology; Tectonics","score_opus":0.041798909509512566,"score_gpt":0.1758854613378856,"score_spread":0.13408655182837304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091086103","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9772362,0.006313634,0.0000035580003,0.0029129954,0.00023677884,0.000052392144,0.000019663874,0.0000021824026,0.013222608],"genre_scores_gemma":[0.9988888,0.00007238868,0.00004781247,0.0005876309,0.000036833324,1.6022688e-7,4.9601806e-7,8.9761517e-7,0.0003649983],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99872243,0.00013118131,0.00030987925,0.00016925596,0.0003392318,0.00032802],"domain_scores_gemma":[0.9987858,0.00043348275,0.0002962122,0.00013334202,0.00005952381,0.00029166945],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00064006756,0.000120370365,0.00023410463,0.000246975,0.00026446447,0.000049623377,0.00065570924,0.000050296745,0.012670768],"category_scores_gemma":[0.00043053704,0.00005269431,0.00013077183,0.0008053705,0.0024246462,0.000115428105,0.00001038599,0.00022235893,0.000019648778],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002455182,0.000007892925,0.9782269,0.000003881055,0.000032731925,0.000030029305,0.00030140197,0.00043077834,0.000027016527,0.000072505856,0.00047089046,0.020393506],"study_design_scores_gemma":[0.0000917244,0.00025881795,0.9955684,0.00002857115,0.000039744824,0.00010100926,0.00033694936,0.001134409,0.00003854906,0.00050930574,0.0017980896,0.000094435665],"about_ca_topic_score_codex":0.004065078,"about_ca_topic_score_gemma":0.061494514,"teacher_disagreement_score":0.057429437,"about_ca_system_score_codex":0.000005290956,"about_ca_system_score_gemma":0.00022874986,"threshold_uncertainty_score":0.9882318},"labels":[],"label_agreement":null},{"id":"W2091432342","doi":"10.1139/e04-082","title":"Relations between air and surface temperature in discontinuous permafrost terrain near Mayo, Yukon Territory","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Permafrost; Air temperature; Snow; Taiga; Atmospheric sciences; Geology; Vegetation (pathology); Boreal; Environmental science; Snow cover; Hydrology (agriculture); Terrain; Geomorphology; Geography; Oceanography","score_opus":0.02193101346446833,"score_gpt":0.22554401608334304,"score_spread":0.20361300261887472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091432342","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916677,0.002134558,0.0000011321773,0.0031846857,0.00035000156,0.00007615471,0.0012199315,0.0000032744117,0.0013625863],"genre_scores_gemma":[0.9990296,0.000047508533,0.00026022302,0.00026511523,0.00020448447,8.9109285e-8,0.00007461672,0.0000028325614,0.000115523995],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99884015,0.000060754897,0.00029931744,0.00017736151,0.000213741,0.0004086896],"domain_scores_gemma":[0.99914116,0.000082134575,0.0001167496,0.00007735409,0.000037952457,0.00054464873],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006481701,0.00012342508,0.000203053,0.00022769319,0.00051134144,0.00026120676,0.00025337783,0.00008342964,0.0007216375],"category_scores_gemma":[0.000051936895,0.0000968584,0.00004752946,0.00037702126,0.00059172366,0.0006696068,0.000005134475,0.00029783737,0.000027317867],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000023825658,0.0000020598077,0.99417716,0.000004752954,0.0000030292913,0.000092487215,0.001960895,0.0033265902,0.00009339884,0.000010844625,0.00008787622,0.000238533],"study_design_scores_gemma":[0.00026889486,0.00017232954,0.9931182,0.00011247503,0.0000068382647,0.00012593485,0.0014032386,0.00008343957,0.000040874787,0.00024366568,0.0042893803,0.00013471194],"about_ca_topic_score_codex":0.0715869,"about_ca_topic_score_gemma":0.8760615,"teacher_disagreement_score":0.80447465,"about_ca_system_score_codex":0.000005908767,"about_ca_system_score_gemma":0.0009726334,"threshold_uncertainty_score":0.93459547},"labels":[],"label_agreement":null},{"id":"W2091763392","doi":"10.1139/e06-014","title":"Middle Turonian dinosaur paleoenvironments in the Upper Cretaceous Kaskapau Formation, northeast British Columbia","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Peace Arch Hospital; Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Jurassic Foundation","keywords":"Geology; Paleontology; Cretaceous; Outcrop; Foreland basin; Siltstone; Structural basin; Facies","score_opus":0.011890619707235641,"score_gpt":0.17315939964301347,"score_spread":0.16126877993577782,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091763392","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9880322,0.0029871727,0.000009355516,0.0007640168,0.00033668758,0.00007607018,0.00006432307,0.0000020302366,0.007728107],"genre_scores_gemma":[0.9990007,0.00004104081,0.00015828242,0.00041273786,0.00012819655,3.4830336e-7,0.000015243867,8.6445544e-7,0.00024254849],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99874675,0.00016156102,0.00031920333,0.0001294402,0.00020328343,0.00043976353],"domain_scores_gemma":[0.99949145,0.00007962191,0.00014713754,0.00007555838,0.000027879187,0.00017837071],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007424604,0.00006824844,0.00013152139,0.000112383,0.00064642215,0.0002207185,0.0004744292,0.000065468754,0.0015857435],"category_scores_gemma":[0.000041712196,0.0000629033,0.00005344214,0.00028708542,0.0007578458,0.00046723743,0.000002241104,0.00018200373,0.0000554145],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000017689919,0.000004982178,0.9967222,0.0000016161873,0.0000021198891,0.0001468084,0.00013008018,0.0007017717,7.423155e-7,0.0000073531023,0.0008810873,0.0013994443],"study_design_scores_gemma":[0.00013940809,0.00014269754,0.9780234,0.000019907067,0.000004744579,0.001577146,0.00040847235,0.00033706613,3.9184397e-7,0.00082363636,0.018442307,0.00008081389],"about_ca_topic_score_codex":0.20840804,"about_ca_topic_score_gemma":0.99697685,"teacher_disagreement_score":0.78856885,"about_ca_system_score_codex":0.000003179476,"about_ca_system_score_gemma":0.00038314876,"threshold_uncertainty_score":0.99932694},"labels":[],"label_agreement":null},{"id":"W2091772994","doi":"10.1139/e04-086","title":"MesozoicCenozoic paleomagnetism of the Intermontane and YukonTanana terranes, Canadian Cordillera","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon Department of Environment; Yukon University; University of Windsor","funders":"","keywords":"Terrane; Geology; Paleomagnetism; Craton; Clockwise; Cretaceous; Paleontology; North American Plate; Apparent polar wander; Cenozoic; Mesozoic; Tectonics; Seismology; Fold (higher-order function); Plate tectonics; Structural basin","score_opus":0.012023827897950073,"score_gpt":0.17750149374710478,"score_spread":0.16547766584915471,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091772994","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9758631,0.003835182,0.0000010335756,0.006274077,0.00017250703,0.000048275913,0.000033737208,0.0000014273081,0.013770677],"genre_scores_gemma":[0.99857485,0.00006404438,0.0003360148,0.0007731059,0.00008694551,7.781387e-8,0.0000013568638,9.614191e-7,0.00016262771],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987979,0.000058777434,0.00033216245,0.00014781035,0.00025827897,0.00040507244],"domain_scores_gemma":[0.99865264,0.00006771499,0.00017059872,0.000104821906,0.000094440846,0.0009097632],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00039441924,0.00010699015,0.00022451371,0.00023609624,0.00034211122,0.00007255823,0.0005618641,0.00005086184,0.008162362],"category_scores_gemma":[0.00013189827,0.000059627448,0.000102486665,0.00050329743,0.00085122674,0.00019918093,0.0000071319905,0.00017481038,0.00001324628],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000029830576,0.000002630218,0.9800851,0.0000034215368,0.00001579577,0.000035949135,0.00016177482,0.00051654957,0.00006249975,0.00006879326,0.00016795019,0.018876582],"study_design_scores_gemma":[0.00010687171,0.00018437166,0.98765564,0.000035229405,0.000027649065,0.00021602113,0.00020004532,0.0012673034,0.00016225845,0.0008696501,0.009174794,0.000100173165],"about_ca_topic_score_codex":0.56222445,"about_ca_topic_score_gemma":0.99619126,"teacher_disagreement_score":0.43396682,"about_ca_system_score_codex":0.0000028136449,"about_ca_system_score_gemma":0.00081615685,"threshold_uncertainty_score":0.9927443},"labels":[],"label_agreement":null},{"id":"W2091790896","doi":"10.1139/e02-012","title":"Evolution of Precambrian continental lithosphere in Western Canada: results from Lithoprobe studies in Alberta and beyond","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Lithosphere; Imbrication; Subduction; Precambrian; Crust; Magmatism; Archean; Proterozoic; Continental crust; Seismology; Geochemistry; Earth science; Tectonics","score_opus":0.021375911786130835,"score_gpt":0.19685350396700144,"score_spread":0.1754775921808706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091790896","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98811096,0.008005909,3.4908132e-7,0.0018751881,0.00012905177,0.00003862452,0.00006516583,5.1780995e-7,0.0017742076],"genre_scores_gemma":[0.99937606,0.000103722865,0.00021135072,0.000086814354,0.000034385335,9.3007884e-8,0.0000026416633,5.463628e-7,0.0001843963],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99884546,0.00006897736,0.00044535194,0.00017068106,0.00020465847,0.000264881],"domain_scores_gemma":[0.9991542,0.00026937688,0.00018281632,0.000054020646,0.00006117756,0.00027841906],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041581102,0.000084491745,0.00026835364,0.00013365797,0.00007086811,0.000026037713,0.00019604473,0.000036259822,0.0005094858],"category_scores_gemma":[0.0004432709,0.000058748246,0.00003121913,0.00049488706,0.00043266374,0.000199443,0.000006609016,0.00012523288,0.000002387045],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010334373,0.000004313721,0.9972499,0.0000033319993,0.000007746207,0.00005204035,0.0005149192,0.00080299564,0.0000066181224,0.000011064384,0.00005907936,0.0012776454],"study_design_scores_gemma":[0.00031976477,0.000114176466,0.99468786,0.00007410756,0.000007712368,0.000017864715,0.0012450032,0.0019726532,0.00003200064,0.0010756927,0.0003755911,0.000077588484],"about_ca_topic_score_codex":0.9863538,"about_ca_topic_score_gemma":0.99993694,"teacher_disagreement_score":0.013583138,"about_ca_system_score_codex":0.0000066632047,"about_ca_system_score_gemma":0.00034922114,"threshold_uncertainty_score":0.5578512},"labels":[],"label_agreement":null},{"id":"W2091796605","doi":"10.1139/e01-062","title":"Deformation of Upper Carboniferous coal measures in the Sydney Basin: evidence for late Alleghanian tectonism in Atlantic Canada","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Geological Survey of Canada; Dalhousie University","funders":"Scheme for Promotion of Academic and Research Collaboration; Natural Sciences and Engineering Research Council of Canada; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Geology; Carboniferous; Paleontology; Fold (higher-order function); Paleozoic; Mesozoic; Bedding; Subsidence; Permian; Tectonics; Fission track dating; Coal measures; Structural basin; Seismology","score_opus":0.04337864438333695,"score_gpt":0.20544372067868685,"score_spread":0.16206507629534989,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091796605","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99362314,0.0013670399,0.0000063358048,0.0037817704,0.00010336074,0.000083824634,0.000011632831,6.9268316e-7,0.0010222136],"genre_scores_gemma":[0.9992626,0.000056015753,0.00015254914,0.00047861706,0.000029311303,3.9927917e-7,0.0000015625715,5.7539694e-7,0.00001837873],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987524,0.00007188079,0.0003710998,0.000107946275,0.00035882552,0.0003378608],"domain_scores_gemma":[0.9992421,0.00026158823,0.00015058977,0.000065582426,0.0000777766,0.00020234915],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010856282,0.000079724756,0.00019332216,0.00019997731,0.00013458233,0.000055214103,0.00045484313,0.000034727655,0.0007099499],"category_scores_gemma":[0.0003771796,0.00004525602,0.00006245327,0.00054461387,0.0002089093,0.0002313531,0.0000024838976,0.00013986281,0.00000263148],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000059757162,0.000003228792,0.9922242,0.0000070820543,0.0000038895814,0.000028993105,0.00030254098,0.006403819,0.000009112153,0.000025918436,0.00006777281,0.0009174347],"study_design_scores_gemma":[0.00013266389,0.00016351111,0.98360205,0.00007624335,0.000010518545,0.000049237173,0.0004214301,0.013654481,0.000051243573,0.0008404196,0.000919483,0.0000787253],"about_ca_topic_score_codex":0.92058975,"about_ca_topic_score_gemma":0.99862295,"teacher_disagreement_score":0.07803321,"about_ca_system_score_codex":0.0000049978357,"about_ca_system_score_gemma":0.000613961,"threshold_uncertainty_score":0.77734536},"labels":[],"label_agreement":null},{"id":"W2091935193","doi":"10.1139/e05-083","title":"Mesoproterozoic deep K-magmatism recorded in a megacryst- and xenolith-bearing minette dyke, western Grenville Province","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université Laval; Geological Survey of Canada; Institut National de la Recherche Scientifique","funders":"","keywords":"Xenolith; Geology; Geochemistry; Partial melting; Pyroxene; Phenocryst; Fractional crystallization (geology); Phlogopite; Mafic; Igneous differentiation; Magmatism; Mantle (geology); Olivine; Volcanic rock; Paleontology","score_opus":0.012296394752150011,"score_gpt":0.1879459626897134,"score_spread":0.17564956793756337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091935193","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9914999,0.0026507904,0.000023242248,0.0031325452,0.00007802699,0.000072490126,0.000006538743,0.0000029673338,0.0025334938],"genre_scores_gemma":[0.9960688,0.000049670252,0.0031322862,0.0004677392,0.00010281095,3.0940532e-7,0.0000013248272,0.0000012563381,0.00017582356],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861634,0.00006402214,0.00038310004,0.00022185076,0.00024266168,0.00047200546],"domain_scores_gemma":[0.9990308,0.00008576523,0.00016710126,0.000078210825,0.00004761368,0.0005904676],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00066609046,0.00012379402,0.00025382006,0.0003253999,0.00019717717,0.00015926136,0.00035013916,0.000053353222,0.0019553283],"category_scores_gemma":[0.00014172978,0.00008568538,0.000056200395,0.00046044245,0.00039656364,0.00038612718,0.000010025927,0.00020926046,0.000037549096],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004888784,0.0000037943464,0.96530235,0.0000060327757,0.0000063009343,0.00007130835,0.0001494369,0.0020027831,0.00005786102,0.000015885067,0.000013888354,0.032365456],"study_design_scores_gemma":[0.00021206909,0.00018645679,0.98580813,0.00005229674,0.000010970737,0.00015728515,0.00013090302,0.006772388,0.00012702383,0.0017229338,0.0046652965,0.00015426136],"about_ca_topic_score_codex":0.038942136,"about_ca_topic_score_gemma":0.93099844,"teacher_disagreement_score":0.8920563,"about_ca_system_score_codex":0.0000027739015,"about_ca_system_score_gemma":0.00027961022,"threshold_uncertainty_score":0.99895704},"labels":[],"label_agreement":null},{"id":"W2091974012","doi":"10.1139/cjes-2014-0036","title":"A POSSIBLE ORIGIN OF THE HAWAIIAN ISLANDS","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Lava; Seamount; Volcano; Submarine; Paleontology; Geophysics; Precambrian; Series (stratigraphy); Continental drift; Volcanism; Convection; Seismology; Shear (geology); Earth science; Tectonics; Oceanography; Meteorology","score_opus":0.020457296842908246,"score_gpt":0.19820555860791259,"score_spread":0.17774826176500433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091974012","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95661014,0.00019690733,0.000008241725,0.0014137122,0.00061431923,0.000025913176,0.0000089058785,0.0000012761807,0.04112059],"genre_scores_gemma":[0.99897766,0.00000434422,0.00019893286,0.00024523868,0.00013092581,3.604182e-8,1.8671197e-7,4.1255186e-7,0.00044225718],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99922544,0.000049705963,0.00017714017,0.00007988927,0.00022007243,0.00024776146],"domain_scores_gemma":[0.9993602,0.00011129428,0.00013505486,0.000068583584,0.000071968585,0.00025289448],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005113268,0.000059933594,0.00014005232,0.00006644516,0.00034320296,0.000048450536,0.00046864498,0.000021349091,0.0009964282],"category_scores_gemma":[0.00020419729,0.000027977787,0.00008225117,0.00042122373,0.000755876,0.00011102407,0.0000052122364,0.000113112364,0.000048737034],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001451911,0.0000017821283,0.99251825,0.0000020444938,0.0000039809647,0.0000019401296,0.00009650095,0.0004605072,0.000006092243,0.00087822357,0.00012393683,0.0059052636],"study_design_scores_gemma":[0.000065403205,0.00024128852,0.9752558,0.000014261639,0.0000048246607,0.000017192939,0.000100569356,0.00034524853,0.00005417099,0.0060855467,0.017769828,0.00004586864],"about_ca_topic_score_codex":0.014117785,"about_ca_topic_score_gemma":0.36495706,"teacher_disagreement_score":0.3508393,"about_ca_system_score_codex":2.7244718e-7,"about_ca_system_score_gemma":0.00032377036,"threshold_uncertainty_score":0.9999168},"labels":[],"label_agreement":null},{"id":"W2092175852","doi":"10.1139/e01-078","title":"A peculiar new fossil shrew (Lipotyphla, Soricidae) from the High Arctic of Canada","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Bat Biology and Ecology Studies","field":"Agricultural and Biological Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature","funders":"","keywords":"Shrew; Neogene; Geology; Coronoid process; Paleontology; Extant taxon; Biology; Anatomy; Evolutionary biology; Structural basin","score_opus":0.02685085991693494,"score_gpt":0.17629240563091955,"score_spread":0.1494415457139846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092175852","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.970179,0.004470048,5.351665e-7,0.023554076,0.00074418116,0.000042640848,0.0000305474,0.000001607508,0.0009773448],"genre_scores_gemma":[0.99795574,0.000079368285,0.000079520505,0.00093113177,0.00034972338,3.7735586e-7,6.347425e-7,3.0952697e-7,0.00060321396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999017,0.00007175282,0.00025519342,0.00012954777,0.00016868381,0.00035782473],"domain_scores_gemma":[0.9989177,0.00042534593,0.00020870708,0.00003965148,0.00009879052,0.00030983365],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00033667614,0.00009110692,0.00019752288,0.000016501843,0.00069854816,0.000032928157,0.0005647109,0.000058270416,0.0031788165],"category_scores_gemma":[0.00029335686,0.000029477229,0.00006529265,0.00035579837,0.0005779798,0.00010039354,0.00001698133,0.00015882993,0.000008359982],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013435984,0.000020729678,0.91227216,0.0000026123366,0.00011144483,0.000081612845,0.0007733409,0.00007824231,0.0017124083,0.0010095251,0.06900036,0.014924159],"study_design_scores_gemma":[0.00008933511,0.00026895813,0.95114017,0.000022881202,0.000018027851,0.000027759666,0.00080011017,0.000016109123,0.0002099987,0.0013932319,0.045926183,0.00008726549],"about_ca_topic_score_codex":0.8903806,"about_ca_topic_score_gemma":0.99817526,"teacher_disagreement_score":0.107794635,"about_ca_system_score_codex":0.000010786547,"about_ca_system_score_gemma":0.0005325834,"threshold_uncertainty_score":0.9977324},"labels":[],"label_agreement":null},{"id":"W2092258196","doi":"10.1139/e11-038","title":"<i>Climacograptus pungens</i>Ruedemann, 1904 and the definition of the Darriwilian (Ordovician) graptolite genus<i>Archiclimacograptus</i>Mitchell, 1987","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Biozone; Ordovician; Paleontology; Genus; Geology; Taxon; Cladistics; Phylogenetic tree; Biology; Biostratigraphy; Zoology","score_opus":0.03223198028237208,"score_gpt":0.20325725398095829,"score_spread":0.17102527369858622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092258196","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8744767,0.024203364,0.000018448383,0.0010375418,0.00080818665,0.00019443408,0.000097772354,0.000004926587,0.09915864],"genre_scores_gemma":[0.9978671,0.00044693853,0.0011453689,0.00045841705,0.00006829743,5.864267e-7,9.231474e-7,0.0000013794164,0.000010961567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99798477,0.00033690728,0.0005363764,0.00021555196,0.00037875178,0.0005476421],"domain_scores_gemma":[0.99840885,0.00027323613,0.0004928445,0.0002098321,0.00012943578,0.00048582448],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0018632568,0.00017897961,0.00031402594,0.0003432496,0.0011779576,0.00009554279,0.0008708209,0.000089866975,0.00026252342],"category_scores_gemma":[0.00013383623,0.000096069896,0.0002753789,0.000838567,0.005572194,0.0003796037,0.0000042998786,0.00035868507,0.0000032702487],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052536332,0.0000060584744,0.9812372,0.000009284121,0.00004739143,0.000020954121,0.0016972272,0.000008053648,0.00001807906,0.0041044056,0.000046361933,0.012752467],"study_design_scores_gemma":[0.0004571157,0.00022576479,0.979299,0.000056329583,0.000075946264,0.00024534785,0.0008489863,0.0000536303,0.000086599575,0.017687606,0.00084003067,0.00012361583],"about_ca_topic_score_codex":0.023871979,"about_ca_topic_score_gemma":0.5720234,"teacher_disagreement_score":0.5481514,"about_ca_system_score_codex":6.892591e-7,"about_ca_system_score_gemma":0.0006822566,"threshold_uncertainty_score":0.9971341},"labels":[],"label_agreement":null},{"id":"W2092436156","doi":"10.1139/e10-038","title":"Birthdate for the Coronation paleocean: age of initial rifting in Wopmay orogen, CanadaThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Terrane; Zircon; Craton; Geochronology; Felsic; Paleontology; Passive margin; Precambrian; Geochemistry; Continental margin; Rift; Mafic; Structural basin; Tectonics","score_opus":0.036281744312475696,"score_gpt":0.2126319438512091,"score_spread":0.1763501995387334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092436156","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937235,0.00029161046,0.0000010952058,0.0015641737,0.00008984423,0.0001145274,0.00009860789,4.608961e-7,0.0041161813],"genre_scores_gemma":[0.9994722,0.000046688045,0.00027812892,0.00012738051,0.000054970653,5.026812e-7,0.0000027864064,9.938152e-7,0.000016365972],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99849224,0.00011977923,0.000708634,0.00012819689,0.00028607377,0.0002650876],"domain_scores_gemma":[0.9986719,0.00043168335,0.00053758785,0.000105939485,0.00015540633,0.00009747178],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017387728,0.00008520618,0.00035550105,0.0003053338,0.000064260465,0.000011495688,0.00050194835,0.000056389676,0.011046465],"category_scores_gemma":[0.00076664076,0.000048417536,0.00008818285,0.0009400184,0.0010046334,0.00021594497,0.00001055806,0.00016420883,6.676024e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013495573,0.000043259417,0.98690575,0.000025180061,0.000028693363,0.000013622159,0.0044721127,0.0009468795,0.001228554,0.00043449653,0.000051305742,0.0057151713],"study_design_scores_gemma":[0.0003954552,0.0006878462,0.9457073,0.00011683711,0.000021574639,0.000005991288,0.0041567115,0.0006269888,0.04386386,0.0038696637,0.00046323775,0.00008448999],"about_ca_topic_score_codex":0.18153772,"about_ca_topic_score_gemma":0.90126884,"teacher_disagreement_score":0.71973115,"about_ca_system_score_codex":0.0000031578104,"about_ca_system_score_gemma":0.0005471946,"threshold_uncertainty_score":0.98985755},"labels":[],"label_agreement":null},{"id":"W2092468831","doi":"10.1139/e2012-037","title":"The Wood Lake, Ontario, H4 ordinary chondrite, a new Canadian meteorite","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Robarts Clinical Trials; Geological Survey of Canada; Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Ordinary chondrite; Meteorite; Chondrite; Geology; Pyroxene; Olivine; Petrography; Weathering; Plagioclase; Mineralogy; Geochemistry; Andradite; Lithic fragment; Shock metamorphism; Silicate; Feldspar; Carbonaceous chondrite; Chondrule; Sedimentary rock; Clastic rock; Chemistry; Astrobiology; Quartz; Skarn; Fluid inclusions","score_opus":0.012274227653133523,"score_gpt":0.18990177237501532,"score_spread":0.1776275447218818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092468831","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9348955,0.0004192848,0.000110883426,0.004214455,0.001566153,0.00015975018,0.000041119274,0.0000027970884,0.05859007],"genre_scores_gemma":[0.98665285,0.0000019065541,0.0013092118,0.00025195876,0.00035161132,8.2804445e-7,0.0000025791094,0.000003400578,0.011425638],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986568,0.000038282757,0.00024762654,0.00014657737,0.00023731177,0.00067339593],"domain_scores_gemma":[0.9976381,0.00008058368,0.00014199076,0.00013542802,0.000108708686,0.0018951816],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00045907355,0.000118364456,0.00013882178,0.00020918138,0.0010851842,0.00054219406,0.00078001234,0.000024277995,0.0068329596],"category_scores_gemma":[0.000014831094,0.00007738469,0.000080946615,0.00042889,0.00034921677,0.0007420653,0.000008902781,0.0002778821,0.00016332643],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000014220601,0.00000293934,0.935754,5.693037e-7,0.000025590982,0.000027498822,0.00072845427,0.0003349868,0.00003246857,0.0015651347,0.034357984,0.027168937],"study_design_scores_gemma":[0.00011094983,0.00014243502,0.49819484,0.00001969815,0.000008402967,0.000037076887,0.0005701401,0.00009759874,0.000014272056,0.001175862,0.49950138,0.00012733974],"about_ca_topic_score_codex":0.9750913,"about_ca_topic_score_gemma":0.99942094,"teacher_disagreement_score":0.46514338,"about_ca_system_score_codex":0.000013004934,"about_ca_system_score_gemma":0.011301446,"threshold_uncertainty_score":0.9943036},"labels":[],"label_agreement":null},{"id":"W2092769284","doi":"10.1139/e01-082","title":"Cranial morphology of <i>Sinornithosaurus millenii </i>Xu et al. 1999 (Dinosauria: Theropoda: Dromaeosauridae) from the Yixian Formation of Liaoning, China","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Theropoda; Quadrate bone; Premaxilla; Geology; Anatomy; Skull; Paleontology; Yixian Formation; Biology; Maxilla; Mesozoic; Cretaceous","score_opus":0.01589218438520516,"score_gpt":0.2160997145868645,"score_spread":0.20020753020165935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092769284","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98155385,0.0059033777,0.000107915395,0.0073749577,0.0009515681,0.00008159906,0.00017468352,0.0000034839911,0.0038485369],"genre_scores_gemma":[0.9971976,0.0004502823,0.0007399354,0.0014407352,0.0001197291,2.0995414e-7,0.000022493163,0.0000017597965,0.000027216169],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99826896,0.00034528927,0.0005501959,0.00017144953,0.00025498832,0.00040912168],"domain_scores_gemma":[0.9985994,0.00032065425,0.0005673383,0.00015077552,0.000110491565,0.00025132915],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012107097,0.00013658794,0.00031555508,0.00022116805,0.0004161344,0.000024834928,0.0007019259,0.000112932226,0.001559235],"category_scores_gemma":[0.0001931147,0.00008734304,0.0001193209,0.00040605396,0.0014990565,0.00046991307,0.000008058712,0.00028329028,0.000021319189],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006044502,0.000009358036,0.9935039,0.0000026122286,0.000025419235,0.00006905479,0.0008401043,0.0008353151,0.00035355552,0.00011299216,0.002415557,0.0017716556],"study_design_scores_gemma":[0.000308121,0.0005486929,0.9816633,0.00004088165,0.000022520851,0.0006821673,0.00046712792,0.0005424604,0.00014805756,0.0011293537,0.014348086,0.00009923819],"about_ca_topic_score_codex":0.06279494,"about_ca_topic_score_gemma":0.5723593,"teacher_disagreement_score":0.5095644,"about_ca_system_score_codex":0.0000025303204,"about_ca_system_score_gemma":0.00089270796,"threshold_uncertainty_score":0.99935347},"labels":[],"label_agreement":null},{"id":"W2092864930","doi":"10.1139/cjes-2014-0007","title":"John Tuzo Wilson: a Canadian who revolutionized Earth Sciences","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor","funders":"","keywords":"Continental drift; Plate tectonics; Honour; Geology; Tectonics; Earth science; Solid earth; Paleontology; Geophysics; History; Archaeology","score_opus":0.016517447711671716,"score_gpt":0.19036992523571483,"score_spread":0.17385247752404312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092864930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90986466,0.002070773,0.00007111733,0.006661508,0.0005400326,0.00007825066,0.000038404618,0.000009601968,0.08066567],"genre_scores_gemma":[0.9952974,0.000051823426,0.0022835813,0.0016267465,0.00030055633,2.373438e-7,0.000004372021,0.0000017554582,0.00043353398],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973563,0.00018276075,0.00047774767,0.0003585815,0.0005876353,0.0010369541],"domain_scores_gemma":[0.99689037,0.00020454786,0.00024221046,0.00014439314,0.00022116251,0.0022973425],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0022843312,0.00019294325,0.0003872454,0.00073601026,0.0015442909,0.00040462177,0.001012623,0.00009487041,0.012141965],"category_scores_gemma":[0.00077147526,0.00013098617,0.0001945745,0.0017836373,0.0018444683,0.00056040875,0.000008461951,0.00028956222,0.0002916916],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000050921317,0.000003921737,0.9861055,0.000004824652,0.000017525626,0.000052955358,0.00010274271,0.003704373,0.00002337992,0.0015895817,0.0008796507,0.0075104255],"study_design_scores_gemma":[0.0002633564,0.00072890456,0.8478434,0.0000764727,0.00003741832,0.00021815852,0.00025253804,0.0142046185,0.00011255587,0.018022323,0.11786402,0.00037623785],"about_ca_topic_score_codex":0.634224,"about_ca_topic_score_gemma":0.98989165,"teacher_disagreement_score":0.35566765,"about_ca_system_score_codex":0.0000037112522,"about_ca_system_score_gemma":0.0027428924,"threshold_uncertainty_score":0.99975556},"labels":[],"label_agreement":null},{"id":"W2093484769","doi":"10.1139/e03-036","title":"Discussion of \"Analysis and reinterpretation of deformation features in the Rouge River valley, Scarborough, Ontario\"","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"The Scarborough Hospital","funders":"","keywords":"Reinterpretation; Geology; Archaeology; Deformation (meteorology); River valley; Geography; Oceanography; Art","score_opus":0.005518177590624087,"score_gpt":0.1997924966717626,"score_spread":0.1942743190811385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093484769","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99625474,0.00017155662,0.00008875753,0.00018397582,0.000050252547,0.000046718582,0.0000011031024,2.5750876e-7,0.0032026295],"genre_scores_gemma":[0.99937236,0.000022733653,0.00048685115,0.000036590915,0.000002547596,2.0426093e-7,2.6313683e-7,7.939365e-7,0.000077680445],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992941,0.00008224272,0.00022568021,0.000060208138,0.00023315055,0.000104631144],"domain_scores_gemma":[0.99962115,0.000027748887,0.00020561818,0.00005525423,0.000014600504,0.00007560755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008816596,0.000043313823,0.00012124373,0.00016640553,0.00008497722,0.00002466692,0.00015172815,0.000030339865,0.00016225818],"category_scores_gemma":[0.000057921054,0.000019052895,0.00005766039,0.00053962524,0.00033117077,0.00029318128,0.000005741091,0.00008984496,5.5635877e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057766074,0.0000072510684,0.9740677,0.000011812736,0.000026645614,0.00000567054,0.014576789,0.010208689,0.00018271642,0.00027179372,0.000020553307,0.0006146439],"study_design_scores_gemma":[0.000107380954,0.00011302615,0.996879,0.000085740256,0.00007355158,0.000025451687,0.00097259553,0.00040588478,0.00042056534,0.0007191946,0.00015807163,0.000039549326],"about_ca_topic_score_codex":0.05943595,"about_ca_topic_score_gemma":0.73781514,"teacher_disagreement_score":0.6783792,"about_ca_system_score_codex":0.000015573809,"about_ca_system_score_gemma":0.00013138175,"threshold_uncertainty_score":0.94682735},"labels":[],"label_agreement":null},{"id":"W2093547966","doi":"10.1139/e00-074","title":"Tectonique et venues volcaniques en contexte de collision, exemple du massif néogène du Siroua (Atlas Marocain) : effets combinés d'une transformante et de la suture panafricaine","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies Worldwide","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Subduction; Massif; Seismology; Fibrous joint; Volcano; Lithosphere; Collision zone; Fault (geology); Tectonics; Geomorphology; Geochemistry","score_opus":0.007077322362078748,"score_gpt":0.2188898947783457,"score_spread":0.21181257241626694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093547966","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9719768,0.00096922624,0.00035624584,0.017203698,0.00018770457,0.00012176621,0.000053144126,0.000014745252,0.009116673],"genre_scores_gemma":[0.99593353,0.0008482075,0.0006105213,0.0021890176,0.0001778495,0.0000012126995,0.0000066236285,0.0000036208323,0.00022944341],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978744,0.0006172231,0.0003335331,0.00020708988,0.00030489097,0.00066290604],"domain_scores_gemma":[0.9978205,0.0010746393,0.00016412996,0.000084048086,0.00011712759,0.00073957705],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002610377,0.00019252884,0.00034758108,0.00014612316,0.0006441565,0.00021378891,0.0005246495,0.00009762266,0.00044169393],"category_scores_gemma":[0.0005345775,0.00013068585,0.0001365221,0.00064027676,0.0007752172,0.00036702753,0.000011376149,0.00041565785,0.000019761554],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006045443,0.00003109459,0.98436993,0.000011317131,0.000031565334,0.0008228273,0.002809433,0.0028859782,0.00007633693,0.00082299765,0.0022763622,0.005801711],"study_design_scores_gemma":[0.0003457759,0.00066276605,0.8698812,0.00007233688,0.000016418906,0.00038522668,0.00039139553,0.00062141113,0.000090707465,0.0057014334,0.12166411,0.00016719097],"about_ca_topic_score_codex":0.055832393,"about_ca_topic_score_gemma":0.39955127,"teacher_disagreement_score":0.34371886,"about_ca_system_score_codex":0.000009494906,"about_ca_system_score_gemma":0.00088664115,"threshold_uncertainty_score":0.9504549},"labels":[],"label_agreement":null},{"id":"W2093978818","doi":"10.1139/e08-053","title":"Holocene and Last Interglacial cloudiness in eastern Baffin Island, Arctic CanadaThis article is one of a series of papers published in this Special Issue on the theme<i>Polar Climate Stability Network</i>.GEOTOP Publication 2008-0027.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université de Montréal; Université du Québec à Montréal","funders":"","keywords":"Tundra; Interglacial; Holocene; Vegetation (pathology); Arctic; Biome; Geology; Physical geography; Climatology; Shrub; Oceanography; Glacial period; Geography; Ecology; Ecosystem; Paleontology","score_opus":0.03648297414009228,"score_gpt":0.2110410091136368,"score_spread":0.17455803497354452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093978818","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99175596,0.000341347,1.6327202e-7,0.0035656914,0.00036053968,0.00013212909,0.00035327295,0.00000123704,0.0034896454],"genre_scores_gemma":[0.9987463,0.00028922322,0.000021932077,0.00043795657,0.0004496469,5.801834e-7,0.00001573349,0.0000023583298,0.00003628976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983446,0.00014827277,0.0005350448,0.00018994484,0.00034538237,0.0004367777],"domain_scores_gemma":[0.9989721,0.00017530733,0.00030489336,0.00014228444,0.00016150394,0.000243864],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016316324,0.00011814617,0.00028742442,0.00026581984,0.0002201033,0.00010045679,0.00036056206,0.00005508792,0.020428874],"category_scores_gemma":[0.0003028902,0.00008274702,0.00004432286,0.00089954404,0.000771306,0.00063501747,0.000014180968,0.00021232564,0.0000064212054],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000070449576,0.000014713862,0.99408406,0.000017093129,0.000004992851,0.00001495235,0.0037267369,0.00018434474,0.000027443062,0.000021320084,0.0008082793,0.0010256309],"study_design_scores_gemma":[0.00028791124,0.0002820521,0.9934012,0.000113679,0.0000054599036,0.000040710973,0.0015453085,0.00040706946,0.000242254,0.00008390797,0.0034903565,0.00010006619],"about_ca_topic_score_codex":0.14216764,"about_ca_topic_score_gemma":0.98584455,"teacher_disagreement_score":0.8436769,"about_ca_system_score_codex":0.00000895718,"about_ca_system_score_gemma":0.0006321926,"threshold_uncertainty_score":0.9804666},"labels":[],"label_agreement":null},{"id":"W2094374504","doi":"10.1139/e06-078","title":"Permian exhumation of the Buffalo Pitts orogenic peridotite massif, northern Cordillera, Yukon","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Victoria","funders":"","keywords":"Geology; Massif; Terrane; Geochemistry; Metamorphism; Rift; Zircon; Migmatite; Eclogite; Peridotite; Metamorphic rock; Petrology; Mantle (geology); Gneiss; Subduction; Paleontology; Tectonics","score_opus":0.016864797005372825,"score_gpt":0.19419312272400308,"score_spread":0.17732832571863025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094374504","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9856645,0.0009985028,0.000019662146,0.00085904053,0.0003323263,0.000044320426,0.000012396978,0.0000021491621,0.012067093],"genre_scores_gemma":[0.999377,0.000015935857,0.00021994926,0.00018674815,0.00010741072,4.2982144e-8,0.0000020884145,9.691637e-7,0.00008981373],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99863213,0.00005597263,0.00038703124,0.0001326849,0.0004278668,0.00036429],"domain_scores_gemma":[0.99887276,0.00010086169,0.00028966926,0.00010727835,0.0001911942,0.0004382521],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009361904,0.000094977695,0.00019197023,0.00017093758,0.0003783679,0.00006079045,0.0005521715,0.00004880855,0.0093917595],"category_scores_gemma":[0.00021515644,0.000051606385,0.00017412727,0.0007358966,0.00063634565,0.00018951963,0.000006804975,0.0001629922,0.000035226414],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000052326604,0.0000043623836,0.9907248,0.0000036413164,0.000013094319,0.00001421857,0.00020040562,0.0015678307,0.0002305285,0.000045524142,0.000018267834,0.00717211],"study_design_scores_gemma":[0.000085901695,0.00014239174,0.99555665,0.000026625115,0.000021295167,0.0000417573,0.0006050643,0.00057678885,0.0007157373,0.00096278643,0.0011822089,0.00008276128],"about_ca_topic_score_codex":0.01774774,"about_ca_topic_score_gemma":0.7070264,"teacher_disagreement_score":0.68927866,"about_ca_system_score_codex":0.0000024938383,"about_ca_system_score_gemma":0.00046476594,"threshold_uncertainty_score":0.9915138},"labels":[],"label_agreement":null},{"id":"W2094468904","doi":"10.1139/e03-038","title":"Structure of the crust and upper mantle of the Great Slave Lake shear zone, northwestern Canada, from teleseismic analysis and gravity modelling","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Shear zone; Seismology; Lithosphere; Crust; Shear wave splitting; Shear (geology); Mantle (geology); Receiver function; Gravity anomaly; Geophysics; Petrology; Tectonics; Paleontology","score_opus":0.008146625900337245,"score_gpt":0.16826840997737313,"score_spread":0.1601217840770359,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094468904","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99809426,0.00048194797,0.000040993247,0.00011263689,0.00030931205,0.000050257197,0.00080914807,3.4128993e-7,0.00010112571],"genre_scores_gemma":[0.99960214,0.000020009948,0.0002359286,0.00006621375,0.000027490156,2.4431644e-8,0.0000019065121,0.000001187478,0.000045099274],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99908847,0.00009378152,0.00023187418,0.00012127967,0.00027507884,0.00018950288],"domain_scores_gemma":[0.99931014,0.000060789163,0.00023571345,0.00012710999,0.00007182795,0.00019444125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023060889,0.00008503187,0.00023128504,0.000086859865,0.00027938996,0.000070103175,0.00027625918,0.000031987773,0.00029712467],"category_scores_gemma":[0.000018488363,0.000044757442,0.000057031386,0.0003893868,0.00035623388,0.0001239686,0.0000071825652,0.00008785961,1.3997936e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000020228122,7.1732615e-7,0.9593716,0.0000050273843,0.000043985045,0.000003126258,0.00029203805,0.03989463,0.00013824011,0.000040809024,0.0000122910415,0.00019547896],"study_design_scores_gemma":[0.000074596195,0.00002569175,0.99446917,0.000025240939,0.00011403254,0.000012936657,0.00020102615,0.0019269281,0.0013621994,0.0006378916,0.0010834101,0.000066901826],"about_ca_topic_score_codex":0.8949585,"about_ca_topic_score_gemma":0.99816996,"teacher_disagreement_score":0.103211455,"about_ca_system_score_codex":0.0000010287284,"about_ca_system_score_gemma":0.0009730951,"threshold_uncertainty_score":0.32533067},"labels":[],"label_agreement":null},{"id":"W2094698597","doi":"10.1139/e08-035","title":"Holocene tephras in lake cores from northern British Columbia, Canada","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; University of Calgary; University of Alberta; University of Northern British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia; University of Northern British Columbia; Geological Society of America","keywords":"Tephra; Geology; Holocene; Volcano; Period (music); Preboreal; Geochemistry; Paleontology; Archaeology; Geomorphology; Oceanography; Younger Dryas; Geography","score_opus":0.01915483941627709,"score_gpt":0.194925294781405,"score_spread":0.17577045536512792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094698597","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99328583,0.002157066,6.179794e-7,0.00047720663,0.0005148779,0.000050729734,0.00016441052,0.00000204319,0.0033472336],"genre_scores_gemma":[0.9989524,0.00011853645,0.00014894817,0.00040111403,0.00007407446,1.5476155e-7,0.000012396954,0.000001412812,0.00029096534],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99850523,0.00012512933,0.00029952507,0.00017903802,0.00031866244,0.0005723847],"domain_scores_gemma":[0.9988563,0.0002339575,0.000115914256,0.000082188366,0.00010711955,0.00060453045],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005060941,0.00007013297,0.00022598822,0.00014076034,0.000608411,0.00011980729,0.0005299422,0.00007619642,0.005923111],"category_scores_gemma":[0.00022735252,0.00008277302,0.000037498703,0.00046183149,0.0010815967,0.00022471536,0.000004383444,0.0003191148,0.00003554806],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000032184041,0.0000023825364,0.9946644,0.0000012170657,0.0000062889803,0.003444306,0.00009692669,0.0005156805,1.1091539e-7,6.4871404e-7,0.00073469663,0.00053017965],"study_design_scores_gemma":[0.00020412893,0.000093174574,0.9938582,0.000025273546,0.000002533872,0.0012675211,0.00019037006,0.00009988563,0.0000020929224,0.0002424528,0.0039175916,0.00009677917],"about_ca_topic_score_codex":0.9969829,"about_ca_topic_score_gemma":0.99999976,"teacher_disagreement_score":0.008431427,"about_ca_system_score_codex":0.0000012103258,"about_ca_system_score_gemma":0.008432638,"threshold_uncertainty_score":0.9971886},"labels":[],"label_agreement":null},{"id":"W2094717584","doi":"10.1139/e01-094","title":"Late Ordovician brachiopod communities of southeast China","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Ordovician; Geology; Facies; Paleontology; Siliciclastic; Carbonate platform; Structural basin","score_opus":0.028028621190775493,"score_gpt":0.2075321216671738,"score_spread":0.17950350047639832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094717584","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.84728634,0.0077861096,0.000006229591,0.0006832459,0.00026953116,0.000028820288,0.000049862305,0.0000027712954,0.14388709],"genre_scores_gemma":[0.9991806,0.000053824835,0.0006126555,0.00004979265,0.00004837982,3.684361e-8,6.0270486e-7,4.935892e-7,0.00005358041],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989605,0.00011362684,0.00031226515,0.00007101558,0.00020914049,0.00033344145],"domain_scores_gemma":[0.9991213,0.000078269295,0.00024137902,0.00010196532,0.000057002795,0.00040005104],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005628574,0.00009285902,0.00020758314,0.0003907253,0.00055676705,0.000069823356,0.00054658647,0.00005307782,0.0021222555],"category_scores_gemma":[0.000032283002,0.000070554874,0.00009665987,0.00038139263,0.0016040895,0.0003802789,7.3520545e-7,0.00021354566,0.000014075206],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002887235,0.0000046372515,0.97826314,0.0000037200139,0.000012088667,0.00002589176,0.0015351,0.0002623558,0.0000018850689,0.0003244709,0.00002747452,0.019536324],"study_design_scores_gemma":[0.0001127823,0.00036978038,0.9954847,0.00003992478,0.000009191775,0.00009795414,0.0012045561,0.0011249352,0.000007848598,0.0009086303,0.00055637007,0.00008329556],"about_ca_topic_score_codex":0.02479069,"about_ca_topic_score_gemma":0.8102306,"teacher_disagreement_score":0.7854399,"about_ca_system_score_codex":3.5508208e-7,"about_ca_system_score_gemma":0.0002931364,"threshold_uncertainty_score":0.99878997},"labels":[],"label_agreement":null},{"id":"W2095054336","doi":"10.1139/e05-070","title":"Polymetamorphism of marbles in the Morin terrane, Grenville Province, Quebec","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Colgate University; University of Wisconsin-Madison; National Science Foundation","keywords":"Granulite; Anorthosite; Terrane; Geology; Metamorphism; Geochemistry; Massif; Metamorphic rock; Orogeny; Metamorphic facies; Hornblende; Pluton; Petrology; Facies; Shear zone; Plagioclase; Geomorphology; Biotite; Seismology; Tectonics; Paleontology; Quartz","score_opus":0.015272766810575154,"score_gpt":0.18581333084555515,"score_spread":0.17054056403498,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095054336","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98409826,0.0020489283,0.000003148262,0.0049259732,0.00007405222,0.000041589148,0.000012803033,9.4357216e-7,0.008794334],"genre_scores_gemma":[0.99864805,0.000024068999,0.0005481369,0.0004488083,0.00010000473,1.1188554e-7,0.0000014080255,5.2134465e-7,0.00022890996],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988355,0.00008158642,0.00034384904,0.00011663413,0.00031088814,0.0003115305],"domain_scores_gemma":[0.99934226,0.00012203176,0.0001690728,0.000084456275,0.000041704832,0.0002404441],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00087445154,0.00008240804,0.00019151717,0.00026583593,0.00013752391,0.00005888992,0.0006315331,0.0000346756,0.0038240305],"category_scores_gemma":[0.000101916696,0.00004248448,0.00009861675,0.0006316118,0.00060969254,0.00020128471,0.0000039365764,0.00015093332,0.000025824307],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057911207,0.000010473938,0.9770557,0.0000036381825,0.000007793109,0.00005064822,0.00021414466,0.003991736,0.00008590284,0.0004204891,0.00013696532,0.01801668],"study_design_scores_gemma":[0.00011313002,0.0001575331,0.98404574,0.000020025947,0.000012888064,0.000067946145,0.00043638388,0.0011329567,0.0003082802,0.0015000369,0.01211961,0.0000854872],"about_ca_topic_score_codex":0.2738124,"about_ca_topic_score_gemma":0.97797126,"teacher_disagreement_score":0.70415884,"about_ca_system_score_codex":0.0000012895106,"about_ca_system_score_gemma":0.0006070804,"threshold_uncertainty_score":0.9970866},"labels":[],"label_agreement":null},{"id":"W2095096485","doi":"10.1139/e10-030","title":"Palaeopathological changes in a population of <i>Albertosaurus sarcophagus</i> from the Upper Cretaceous Horseshoe Canyon Formation of Alberta, CanadaThis article is one of a series of papers published in this Special Issue on the theme <i>Albertosaurus</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Canyon; Horseshoe (symbol); Geology; Cretaceous; Phalanx; Paleontology; Population; Anatomy; Medicine; Geomorphology","score_opus":0.013281037707308964,"score_gpt":0.19573386070460086,"score_spread":0.1824528229972919,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095096485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98455304,0.0005037101,2.4500252e-7,0.009342972,0.00045758596,0.00014354633,0.00015760244,7.0628596e-7,0.004840607],"genre_scores_gemma":[0.9991167,0.00006737221,0.00011942366,0.00044993174,0.00018523127,7.915194e-7,0.000013144498,0.0000014641678,0.000045921428],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983329,0.0002693452,0.0006126202,0.00015593576,0.00031705404,0.00031210994],"domain_scores_gemma":[0.9982948,0.0007377342,0.00056149275,0.00017334807,0.0001042858,0.00012836927],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012024381,0.000117129355,0.000356263,0.00025415383,0.00013896871,0.000016752005,0.0005230774,0.00013711546,0.008747897],"category_scores_gemma":[0.0008065377,0.00006776352,0.000069191396,0.0005848923,0.0011271343,0.00037993025,0.000008806341,0.00031109565,0.0000026649861],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010821102,0.000018350069,0.99284166,0.0000070625047,0.000008913709,0.000007694527,0.0033698585,0.00014993887,0.0014871196,0.00026440763,0.00033282358,0.0014039569],"study_design_scores_gemma":[0.00021232496,0.00044764677,0.9909963,0.00006599091,0.000012997063,0.000041282015,0.0008931767,0.0002863847,0.0039497493,0.00088978285,0.0021283363,0.000076050776],"about_ca_topic_score_codex":0.4718862,"about_ca_topic_score_gemma":0.99458057,"teacher_disagreement_score":0.52269435,"about_ca_system_score_codex":0.000004613205,"about_ca_system_score_gemma":0.0005514248,"threshold_uncertainty_score":0.99215823},"labels":[],"label_agreement":null},{"id":"W2095334462","doi":"10.1139/e06-063","title":"The Western Superior Province Lithoprobe and NATMAP transects: introduction and summary","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Queen's University; Geological Survey of Canada","funders":"","keywords":"Geology; Prospectivity mapping; Archean; Transect; Craton; Geochemistry; Crust; Greenstone belt; Continental crust; Structural basin; Earth science; Paleontology; Tectonics","score_opus":0.006591248083523481,"score_gpt":0.1650886486339224,"score_spread":0.1584974005503989,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095334462","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9818339,0.007670101,0.000008541157,0.009555648,0.00013021068,0.000037710648,0.0000074851705,0.000002258269,0.0007541498],"genre_scores_gemma":[0.9988466,0.00014102708,0.00024480376,0.00014493146,0.000256276,9.2631005e-8,0.0000014523285,5.593375e-7,0.00036428586],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99922305,0.000045407352,0.00018961955,0.00013814954,0.00015343314,0.0002503352],"domain_scores_gemma":[0.99947774,0.00009611223,0.000068646594,0.00004368895,0.000051144776,0.00026267124],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056083634,0.00007016261,0.00011181742,0.000075885415,0.0005530379,0.00024075585,0.00015948947,0.00002791488,0.00020106662],"category_scores_gemma":[0.000062939136,0.000036838075,0.00003246499,0.00021822732,0.0008774946,0.0002519602,0.0000029424305,0.00011389578,0.000003499685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006216075,0.0000015144251,0.99041486,0.0000036849704,0.0000043865193,0.000018820376,0.000038172806,0.00019132362,0.000064962354,0.00009740764,0.00016292749,0.008995728],"study_design_scores_gemma":[0.000083405,0.00020497531,0.9624717,0.000010034272,0.000013665166,0.00020308372,0.00012368205,0.00038912328,0.00012594946,0.004393408,0.031901903,0.00007902025],"about_ca_topic_score_codex":0.0310738,"about_ca_topic_score_gemma":0.7323929,"teacher_disagreement_score":0.7013191,"about_ca_system_score_codex":6.4390423e-7,"about_ca_system_score_gemma":0.00021993139,"threshold_uncertainty_score":0.97537833},"labels":[],"label_agreement":null},{"id":"W2095429551","doi":"10.1139/e10-029","title":"Quantifying tooth variation within a single population of<i>Albertosaurus sarcophagus</i>(Theropoda: Tyrannosauridae) and implications for identifying isolated teeth of tyrannosauridsThis article is one of a series of papers published in this Special Issue on the theme<i>Albertosaurus</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Peace Arch Hospital; University of Calgary; University of Alberta","funders":"","keywords":"Theropoda; Population; Juvenile; Permanent teeth; Morphometrics; Geology; Orthodontics; Biology; Cretaceous; Paleontology; Zoology; Medicine; Ecology","score_opus":0.033668481495254206,"score_gpt":0.24373177692066944,"score_spread":0.21006329542541524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095429551","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99403495,0.0004527069,0.00002110041,0.0033491042,0.00048563402,0.00021288697,0.00013635699,0.0000019112956,0.0013053776],"genre_scores_gemma":[0.9981505,0.000027395146,0.0015275877,0.00010162995,0.00015246856,9.684882e-7,0.000009289819,0.000002551545,0.00002758465],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984697,0.00013608803,0.0007581368,0.00018740623,0.00019174966,0.00025688295],"domain_scores_gemma":[0.9981461,0.00053390866,0.000824136,0.00015219755,0.00022377085,0.00011985841],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014286208,0.000113139795,0.00034140935,0.0003903586,0.00025059367,0.00003219631,0.00032709024,0.00012398335,0.0017032466],"category_scores_gemma":[0.0007301344,0.00008245139,0.00007831345,0.0006674602,0.000901195,0.00055070646,0.000006319539,0.00020298288,0.0000010412182],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001904181,0.0000417273,0.9459294,0.000042280026,0.000040541436,0.0000010656339,0.0036707814,0.0003352303,0.0446419,0.0029762436,0.000086911146,0.0020434908],"study_design_scores_gemma":[0.00032437925,0.00062134844,0.9870303,0.00009268004,0.000029480881,0.000031899028,0.00040895274,0.0006625534,0.0071408586,0.0032627643,0.000303893,0.00009086625],"about_ca_topic_score_codex":0.020886885,"about_ca_topic_score_gemma":0.44319692,"teacher_disagreement_score":0.42231005,"about_ca_system_score_codex":0.0000031702982,"about_ca_system_score_gemma":0.00044837274,"threshold_uncertainty_score":0.99920934},"labels":[],"label_agreement":null},{"id":"W2095467023","doi":"10.1139/e10-027","title":"Sediment sources and dispersion as revealed by single-grain <sup>40</sup>Ar/<sup>39</sup>Ar ages of detrital muscovite from Carboniferous and Cretaceous rocks in mainland Nova ScotiaGeological Survey of Canada contribution 20090289.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Bedford Institute of Oceanography; Geological Survey of Canada; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University; Transport Canada","keywords":"Geology; Terrane; Carboniferous; Muscovite; Geochemistry; Cretaceous; Metamorphic rock; Detritus; Zircon; Batholith; Paleontology; Structural basin; Tectonics; Quartz","score_opus":0.009413836220599556,"score_gpt":0.1811955255798993,"score_spread":0.17178168935929974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095467023","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942272,0.004040318,0.000008252201,0.0008649911,0.00008720696,0.00010926914,0.0005148726,0.000002237884,0.0001456758],"genre_scores_gemma":[0.99943936,0.00007222725,0.00018881299,0.00015099296,0.00004350997,1.8367427e-7,0.00006330928,0.0000019044635,0.000039725914],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99768716,0.000255243,0.00061913865,0.00035256858,0.00051990914,0.0005659792],"domain_scores_gemma":[0.9978138,0.0006953307,0.0003379067,0.0001094479,0.00020822044,0.00083525985],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014816511,0.00020949838,0.00057579,0.00024719397,0.00022568929,0.000091734575,0.00034600313,0.00015507084,0.00093371293],"category_scores_gemma":[0.0013387593,0.00014501694,0.00007035669,0.000623869,0.0010418736,0.0002041109,0.000023798368,0.0003752631,0.0000013803901],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058384696,0.000017820024,0.99452376,0.0000075190646,0.000024048995,0.00008906975,0.00015471043,0.0033392464,0.00078858226,0.0000019540603,0.00009630492,0.0008986129],"study_design_scores_gemma":[0.00054598076,0.00063372107,0.9907312,0.000059686532,0.00003541942,0.00007815948,0.00044054468,0.0057723275,0.0007414911,0.0004806143,0.00027991692,0.00020096167],"about_ca_topic_score_codex":0.9188538,"about_ca_topic_score_gemma":0.9886131,"teacher_disagreement_score":0.06975928,"about_ca_system_score_codex":0.000007230363,"about_ca_system_score_gemma":0.0006712941,"threshold_uncertainty_score":0.99997956},"labels":[],"label_agreement":null},{"id":"W2095561639","doi":"10.1139/e09-035","title":"Paleomagnetism of the mid-Cretaceous gem-bearing pegmatite dikes of San Diego County, California, USA","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"","keywords":"Geology; Batholith; Dike; Paleomagnetism; Cretaceous; Paleontology; Clockwise; Geochemistry; Tectonics; Neogene; Seismology; Fold (higher-order function)","score_opus":0.01278026776200807,"score_gpt":0.18894251850233837,"score_spread":0.1761622507403303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095561639","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9899257,0.002529015,0.000009001822,0.00090342446,0.00015252354,0.000043204138,0.00007048003,0.0000014800916,0.0063651693],"genre_scores_gemma":[0.9991366,0.000038472215,0.00042712173,0.00025637215,0.000054358083,4.0501554e-8,0.0000014673774,6.548782e-7,0.000084885105],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985357,0.00006849254,0.00045254684,0.0001369237,0.0004567083,0.00034964585],"domain_scores_gemma":[0.99888074,0.00010411014,0.00036864128,0.00012363459,0.00014390313,0.00037894773],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00059402565,0.00010737629,0.00028720638,0.00016149411,0.00024833856,0.000053882166,0.0006874011,0.00004867606,0.0054037645],"category_scores_gemma":[0.00024034716,0.000058930622,0.00018181601,0.0006769001,0.0008369203,0.00015477143,0.00000785002,0.00016384572,0.000015184554],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004275188,0.000005570814,0.9905208,0.0000065642857,0.000009613227,0.000013738852,0.0000932053,0.003717615,0.0006826859,0.000041347303,0.0000869371,0.004817681],"study_design_scores_gemma":[0.0000865132,0.00030144234,0.9907682,0.00005489947,0.000029807165,0.000049158956,0.00011800144,0.0009026926,0.0011791266,0.004819653,0.0016028841,0.000087627115],"about_ca_topic_score_codex":0.020191532,"about_ca_topic_score_gemma":0.4905496,"teacher_disagreement_score":0.47035807,"about_ca_system_score_codex":0.0000011529606,"about_ca_system_score_gemma":0.00035569977,"threshold_uncertainty_score":0.99550545},"labels":[],"label_agreement":null},{"id":"W2095977674","doi":"10.1139/e03-071","title":"Late Pleistocene coastal paleogeography of the Queen Charlotte Islands, British Columbia, Canada, and its implications for terrestrial biogeography and early postglacial human occupation","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"","keywords":"Pleistocene; Geology; Holocene; Palaeogeography; Land bridge; Biogeography; Quaternary; Glacial period; Oceanography; Paleontology; Archaeology; Geography","score_opus":0.01573049892000915,"score_gpt":0.22139650190658294,"score_spread":0.20566600298657378,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095977674","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975696,0.0008889428,0.0000016996268,0.0003788295,0.00025396544,0.00019787913,0.0004345614,0.000001149383,0.00027336154],"genre_scores_gemma":[0.99975294,0.00003724773,0.00005788411,0.000067058536,0.00003583068,8.8037416e-7,0.0000071747395,0.0000012617103,0.000039714974],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990167,0.00011650605,0.00025935026,0.00014618455,0.00014017777,0.00032104956],"domain_scores_gemma":[0.99919385,0.00013091679,0.0001940532,0.00006143403,0.000121392106,0.00029838146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006062531,0.00006376727,0.0001702986,0.0001504482,0.0010042656,0.00014796616,0.0002205051,0.00006246158,0.00008371518],"category_scores_gemma":[0.0001453747,0.00006220525,0.0000555654,0.00036717133,0.0007688432,0.00015512767,0.000004248381,0.00012508758,1.6462234e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000064024866,0.0000019589947,0.9996083,0.0000054154775,0.000013884567,0.0000036388633,0.000051229712,0.0000063088346,0.0000058063993,0.0000409385,0.00007609609,0.00018004864],"study_design_scores_gemma":[0.00034044037,0.0002798794,0.9977497,0.00002014491,0.000015712902,0.00011752693,0.00004558156,0.00001411473,0.000011871072,0.00084358925,0.0004913358,0.00007011447],"about_ca_topic_score_codex":0.89133567,"about_ca_topic_score_gemma":0.9997944,"teacher_disagreement_score":0.1084588,"about_ca_system_score_codex":3.351028e-7,"about_ca_system_score_gemma":0.0013255713,"threshold_uncertainty_score":0.7724101},"labels":[],"label_agreement":null},{"id":"W2096049795","doi":"10.1139/e10-082","title":"U–Pb Neoproterozoic–Ordovician protolith age constraints for high- to medium-pressure rocks thrust over low-grade metamorphic rocks in theIxcamilpa area, Acatlán Complex, southern Mexico","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Universidad Nacional Autónoma de México; Consejo Nacional de Ciencia y Tecnología","keywords":"Geology; Laurentia; Geochemistry; Ordovician; Protolith; Blueschist; Zircon; Provenance; Metamorphism; Volcanic rock; Orogeny; Geochronology; Craton; Gondwana; Metamorphic rock; Nappe; Petrology; Subduction; Paleontology; Eclogite; Tectonics; Volcano","score_opus":0.02453768330522016,"score_gpt":0.2213965349263192,"score_spread":0.19685885162109903,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096049795","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99278945,0.00017832482,0.00021609299,0.0037559196,0.0003518649,0.0006142502,0.00033106652,0.000009108647,0.001753899],"genre_scores_gemma":[0.9963802,0.0000030787028,0.0017755944,0.0014300601,0.00022530176,0.000007250798,0.000023672748,0.000004188746,0.00015061517],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99745005,0.00008833067,0.0006009984,0.0004272403,0.00052237953,0.0009110064],"domain_scores_gemma":[0.99778116,0.00021533895,0.0002870844,0.00020669625,0.00015115624,0.0013585732],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011355074,0.00026858426,0.0005487859,0.0004923265,0.000454922,0.00025837746,0.0011278496,0.00016186574,0.013756146],"category_scores_gemma":[0.00045840163,0.00017499876,0.000200863,0.00083732174,0.0009784166,0.0002516284,0.000019668492,0.0005816841,0.00005456813],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003380822,0.00002537694,0.9881626,0.00001530557,0.00005385294,0.00012381712,0.0005340243,0.005205721,0.0017896012,0.0000719183,0.00015758001,0.0038264107],"study_design_scores_gemma":[0.00067529286,0.0005177643,0.9725216,0.000088835644,0.00007525242,0.00009363001,0.0008397057,0.0020039168,0.0014731489,0.01402185,0.0072268015,0.00046218382],"about_ca_topic_score_codex":0.062295366,"about_ca_topic_score_gemma":0.87894374,"teacher_disagreement_score":0.81664836,"about_ca_system_score_codex":0.0000025106483,"about_ca_system_score_gemma":0.00067527493,"threshold_uncertainty_score":0.9871454},"labels":[],"label_agreement":null},{"id":"W2097026661","doi":"10.1139/e04-019","title":"<i>Arcticanodon dawsonae</i>, a primitive new palaeanodont from the lower Eocene of Ellesmere Island, Canadian High Arctic","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Incertae sedis; Paleontology; Arctic; Geology; Taxon; Genus; The arctic; Paleogene; Group (periodic table); Oceanography; Zoology; Biology; Structural basin","score_opus":0.019707369560075644,"score_gpt":0.205999625286918,"score_spread":0.18629225572684235,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097026661","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9668681,0.004975263,0.000036246125,0.01912515,0.0013944481,0.00012714889,0.0005757206,0.0000031061745,0.0068948315],"genre_scores_gemma":[0.9962556,0.00018496462,0.00077914004,0.0023408118,0.00024455192,1.3466747e-7,0.000012656956,0.0000024360947,0.00017972733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984597,0.00007095476,0.000372732,0.0002004786,0.00034154177,0.0005546058],"domain_scores_gemma":[0.9981282,0.00025303516,0.00025864466,0.00014543887,0.00018791092,0.0010267849],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00053403556,0.00015438239,0.0002811845,0.00021472231,0.0006481881,0.00008061206,0.0005963427,0.00007468464,0.0034276089],"category_scores_gemma":[0.00023271966,0.0000990404,0.000109040695,0.00047088673,0.0011250156,0.00025497974,0.0000050302956,0.0002646828,0.000045392113],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014775105,0.0000048621587,0.9941211,0.0000018229059,0.00004969189,0.000082142484,0.0010500847,0.0016038879,0.0000031236616,0.00049998506,0.0011237978,0.0014447493],"study_design_scores_gemma":[0.00040620274,0.0003929538,0.9768443,0.00009516311,0.000036655194,0.000079814825,0.0011952124,0.000024625451,0.000031434844,0.0023406069,0.018421838,0.00013117913],"about_ca_topic_score_codex":0.9623674,"about_ca_topic_score_gemma":0.999864,"teacher_disagreement_score":0.037496567,"about_ca_system_score_codex":0.00001201239,"about_ca_system_score_gemma":0.005916005,"threshold_uncertainty_score":0.9997195},"labels":[],"label_agreement":null},{"id":"W2097278890","doi":"10.1139/e06-098","title":"Paleoenvironmental and basin analysis of the late Neoproterozoic (Ediacaran) upper Conception and St. John's groups, west Conception Bay, Newfoundland","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"","keywords":"Geology; Turbidite; Turbidity current; Outcrop; Structural basin; Paleontology; Pyroclastic rock; Siliciclastic; Lithostratigraphy; Marine transgression; Geomorphology; Volcano; Geochemistry; Facies; Sedimentary depositional environment","score_opus":0.013717864350940377,"score_gpt":0.22443869759771232,"score_spread":0.21072083324677193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097278890","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969876,0.0013917326,0.000025141593,0.0005332727,0.00023017297,0.00008813666,0.00003375946,0.0000011599102,0.0007090613],"genre_scores_gemma":[0.9994263,0.00015924386,0.00011917899,0.00016085511,0.000053595057,1.1317302e-7,0.000006247669,9.857566e-7,0.00007349811],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883425,0.00015754184,0.00027846248,0.00014591974,0.00024193693,0.00034187312],"domain_scores_gemma":[0.99915767,0.00018319655,0.0001973062,0.00008024046,0.00003858797,0.00034299176],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015111197,0.0000912701,0.00022853448,0.00039219216,0.00045262312,0.000060155347,0.00021174854,0.00008593893,0.0013260946],"category_scores_gemma":[0.00005706855,0.00006022244,0.00006938053,0.00054670277,0.0029190436,0.0002859731,0.00000817487,0.00020657065,0.0000065114864],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001468192,0.0000020373077,0.99817204,0.0000035099313,0.000043833446,0.000014523943,0.00044498907,0.00029834447,0.000016838565,0.000050428996,0.0000049949076,0.000933771],"study_design_scores_gemma":[0.00021318674,0.00019204577,0.9975437,0.00001530766,0.000084350664,0.00010339926,0.0006560776,0.0006078423,0.000016735352,0.00016606646,0.00033429282,0.00006699457],"about_ca_topic_score_codex":0.0057329047,"about_ca_topic_score_gemma":0.71965015,"teacher_disagreement_score":0.7139172,"about_ca_system_score_codex":0.0000010404839,"about_ca_system_score_gemma":0.00017515756,"threshold_uncertainty_score":0.9997944},"labels":[],"label_agreement":null},{"id":"W2097279722","doi":"10.1139/e10-010","title":"Palaeocope ostracods from the Silurian Wenlock Series of Arctic Canada","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ostracod; Geology; Trilobite; Paleontology; Arctic; Biozone; Fauna; Biostratigraphy; Oceanography; Ecology; Ordovician; Biology","score_opus":0.017445335089109604,"score_gpt":0.17763414738928215,"score_spread":0.16018881230017254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097279722","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98821765,0.0005773133,0.000002723894,0.007945705,0.0013066367,0.000044826615,0.00005400053,0.0000010811608,0.0018500759],"genre_scores_gemma":[0.99888563,0.000028641985,0.00045646168,0.00035947387,0.00021654328,9.460195e-8,0.000003083191,6.7943995e-7,0.000049395036],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99908406,0.000043729957,0.00024734868,0.00009380171,0.00027156525,0.00025951548],"domain_scores_gemma":[0.99915034,0.00017855174,0.00016069534,0.00008119183,0.00012069233,0.00030853],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048166973,0.00007246883,0.00013527661,0.00003593595,0.00050099235,0.00008315469,0.00042654664,0.000031287655,0.0028043576],"category_scores_gemma":[0.00031998332,0.000039255803,0.00003923112,0.0002535151,0.00057831046,0.00025666147,0.0000044349604,0.00019989173,0.000008884594],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004775756,0.0000010412206,0.99402875,0.0000014124399,0.000008067243,0.000018946896,0.00022462086,0.0017260001,0.00002559139,0.00008161431,0.0005449594,0.0033342184],"study_design_scores_gemma":[0.000057400273,0.0001597199,0.968591,0.0000120393925,0.0000069525004,0.000027271595,0.0012198325,0.00015677142,0.00009492213,0.00091674156,0.028697891,0.00005948743],"about_ca_topic_score_codex":0.96948117,"about_ca_topic_score_gemma":0.999888,"teacher_disagreement_score":0.030406883,"about_ca_system_score_codex":0.0000010668194,"about_ca_system_score_gemma":0.0017671272,"threshold_uncertainty_score":0.9981072},"labels":[],"label_agreement":null},{"id":"W2097564358","doi":"10.1139/e04-083","title":"Taconian mélanges in the parautochthonous zone of the Quebec Appalachians revisited: implications for foreland basin and thrust belt evolution","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Cegep de Sainte Foy; Université Laval; Ministère des Ressources naturelles et des Forêts (Québec); Institut National de la Recherche Scientifique; Centre de Géomatique du Québec","funders":"","keywords":"Foreland basin; Geology; Allochthon; Paleontology; Ordovician; Imbrication; Sequence (biology); Flysch; Nappe; Group (periodic table); Lithology; Structural basin; Tectonics","score_opus":0.016279957638082165,"score_gpt":0.2086832662581911,"score_spread":0.19240330862010896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097564358","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9809643,0.0017674924,0.00024146677,0.016028749,0.00004418953,0.00013696203,0.00006707867,0.0000010586562,0.0007486727],"genre_scores_gemma":[0.9990121,0.000025868723,0.0005598946,0.00033376995,0.000041149426,7.3234287e-7,0.00000391864,5.423244e-7,0.00002202286],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99927384,0.00005230454,0.0002251857,0.000107670436,0.00012044229,0.00022055832],"domain_scores_gemma":[0.99941623,0.00014530121,0.0001485114,0.000086221226,0.00006235264,0.00014141036],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006684811,0.0000641244,0.000139455,0.000109593195,0.0003373156,0.000060018905,0.00036673172,0.000035501933,0.00009737116],"category_scores_gemma":[0.00015252166,0.000030339303,0.00007534475,0.0005401836,0.0005388265,0.00011953231,0.0000036837728,0.00010749428,0.0000011472354],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000032061648,0.0000048904376,0.99236536,0.0000052304626,0.000005309524,0.0000013589938,0.00026399153,0.002458427,0.000023163115,0.002268999,0.000027799115,0.0025722426],"study_design_scores_gemma":[0.00013121613,0.000116612166,0.97604054,0.000028830977,0.000019338153,0.000049048867,0.00043738674,0.00016436112,0.000016488584,0.022269726,0.0006807923,0.00004562971],"about_ca_topic_score_codex":0.15568684,"about_ca_topic_score_gemma":0.9266453,"teacher_disagreement_score":0.7709584,"about_ca_system_score_codex":0.0000026664509,"about_ca_system_score_gemma":0.00039451686,"threshold_uncertainty_score":0.84993553},"labels":[],"label_agreement":null},{"id":"W2097616268","doi":"10.1139/e01-068","title":"Sediment transfer by shallow landsliding in the Queen Charlotte Islands, British Columbia","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":149,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia; Ministry of Forests; Government of British Columbia; University of Calgary","funders":"","keywords":"Geology; Landslide; Bedrock; Debris; Colluvium; Sediment; Erosion; Geomorphology; Weathering; Hydrology (agriculture); Oceanography; Geotechnical engineering; Alluvium","score_opus":0.010100931246130908,"score_gpt":0.18046865966799272,"score_spread":0.17036772842186182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097616268","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9824769,0.0007049615,0.000011116253,0.0018069382,0.00020912268,0.00008159221,0.000015017066,0.0000022467675,0.014692094],"genre_scores_gemma":[0.9973719,0.0002019243,0.00004414391,0.0008039914,0.00005053216,0.000001002903,5.764732e-7,0.000003846308,0.0015220958],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99882305,0.000059220696,0.00023427195,0.00013732068,0.00037073236,0.0003754188],"domain_scores_gemma":[0.9995798,0.000030378365,0.000046569854,0.00006746376,0.000008149765,0.00026765722],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00082778226,0.000062901956,0.00012391797,0.00004196231,0.00037205007,0.00047666338,0.00047183727,0.00005072289,0.007088459],"category_scores_gemma":[0.00001870322,0.000051890056,0.000058020913,0.0003818019,0.0002707939,0.00028613358,0.000007793551,0.00021555573,0.000037924954],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001086287,0.000020136758,0.9473671,0.0000018919765,0.000007455344,0.0002683899,0.0021169328,0.00031811526,0.000084963875,0.00000612361,0.046381585,0.0034262585],"study_design_scores_gemma":[0.0010326861,0.00050089805,0.66138405,0.00016367201,0.000025450214,0.00083417544,0.0013465884,0.0012557439,0.000045522567,0.00023642338,0.3328338,0.0003410265],"about_ca_topic_score_codex":0.11218231,"about_ca_topic_score_gemma":0.7701465,"teacher_disagreement_score":0.65796417,"about_ca_system_score_codex":0.000016590096,"about_ca_system_score_gemma":0.00006109782,"threshold_uncertainty_score":0.9938192},"labels":[],"label_agreement":null},{"id":"W2098391751","doi":"10.1139/e02-098","title":"Robert Lynn Carroll an appreciation","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature; Royal Ontario Museum","funders":"","keywords":"Honour; Vertebrate paleontology; Geology; Environmental ethics; Paleontology; Classics; History; Philosophy; Archaeology","score_opus":0.024907530249350666,"score_gpt":0.22588433323726884,"score_spread":0.20097680298791817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2098391751","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.87584484,0.004835621,0.000082873616,0.0005036234,0.0014143995,0.000049589573,0.000012368491,0.0000049937476,0.11725168],"genre_scores_gemma":[0.9978909,0.0000344325,0.0013742009,0.00032754714,0.000091510294,6.795634e-8,0.0000013195887,7.9237157e-7,0.00027924613],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99902976,0.00014125826,0.00021109822,0.0001157128,0.00019191303,0.0003102418],"domain_scores_gemma":[0.99912596,0.00007037681,0.0001351673,0.000063769876,0.00010642421,0.00049831124],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00096806925,0.0000737503,0.00013120192,0.00023514495,0.00053992384,0.00008207195,0.00022026713,0.00004330546,0.001483587],"category_scores_gemma":[0.00023364193,0.00005608026,0.00004573954,0.0003333264,0.00036072772,0.00047575225,6.5369653e-7,0.00010812886,0.000048818845],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000016050681,0.0000016594685,0.9955012,9.0982974e-7,0.0000057904213,0.000013255548,0.00033058843,0.0017156353,0.0000024576964,0.000574639,0.00024795887,0.0016042691],"study_design_scores_gemma":[0.00011935197,0.00023799278,0.9521755,0.000007860831,0.000007505428,0.00013221486,0.0007778739,0.0003971102,0.000019095012,0.00086116756,0.045178443,0.00008591173],"about_ca_topic_score_codex":0.010409449,"about_ca_topic_score_gemma":0.929906,"teacher_disagreement_score":0.91949654,"about_ca_system_score_codex":0.0000013889351,"about_ca_system_score_gemma":0.0009844038,"threshold_uncertainty_score":0.99942917},"labels":[],"label_agreement":null},{"id":"W2099013251","doi":"10.1139/e06-111","title":"<i>Boreameryx</i>, an unusual new artiodactyl (Mammalia) from the Pliocene of Arctic Canada and endemism in Arctic fossil mammals","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature","funders":"Core Research for Evolutional Science and Technology","keywords":"Arctic; Endemism; Paleontology; Geology; Theria; Ecology; Biology; Cenozoic; Structural basin; Oceanography; Phanerozoic","score_opus":0.02741090740933717,"score_gpt":0.22892002623203486,"score_spread":0.2015091188226977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099013251","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98795956,0.008439689,0.00001702344,0.0016113846,0.0004966185,0.000055160835,0.000035584813,0.0000014714651,0.0013834941],"genre_scores_gemma":[0.99867,0.00009381913,0.00041634386,0.00060717855,0.00014042894,6.1136944e-8,0.0000020019265,0.00000130866,0.00006885135],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851894,0.0001064487,0.0004326167,0.00016843172,0.00032194884,0.00045163912],"domain_scores_gemma":[0.9981925,0.0006784737,0.0002532635,0.00010283819,0.00009321847,0.00067972444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013815454,0.00011388973,0.00023620678,0.00018509333,0.00030929578,0.00005361901,0.00036170543,0.000050359213,0.0002742484],"category_scores_gemma":[0.0004346643,0.000077072495,0.000034731453,0.0004608905,0.0008033054,0.0002829565,0.0000043724185,0.00022124127,0.0000016429348],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012705755,0.0000023120238,0.99269843,0.0000028503837,0.000013312646,0.000060203813,0.00065253576,0.00032744557,0.000008083996,0.00005983514,0.00013955671,0.00602271],"study_design_scores_gemma":[0.0002258658,0.0001591608,0.99431026,0.00005040597,0.0000142491235,0.0000867208,0.001888284,0.00008665905,0.00005289157,0.00086696545,0.002166067,0.00009245799],"about_ca_topic_score_codex":0.9831889,"about_ca_topic_score_gemma":0.9999546,"teacher_disagreement_score":0.016765704,"about_ca_system_score_codex":0.0000071695295,"about_ca_system_score_gemma":0.0033669819,"threshold_uncertainty_score":0.59728813},"labels":[],"label_agreement":null},{"id":"W2099274919","doi":"10.1139/e03-055","title":"Tectonic implications of magnetic fabrics and remanence in the Cooper Mountain pluton, North Cascade Mountains, Washington","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Geological Survey; Geological Society of America; Western Washington University; National Science Foundation","keywords":"Pluton; Geology; Paleomagnetism; Lineation; Transpression; Remanence; Dike; Seismology; Geochemistry; Tectonics; Paleontology; Geophysics; Sinistral and dextral; Magnetization","score_opus":0.015190775041731334,"score_gpt":0.2020292546534888,"score_spread":0.18683847961175748,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099274919","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99202234,0.0032726906,0.000011101416,0.0015011639,0.000034365286,0.00005995749,0.000017211747,0.0000011077236,0.003080081],"genre_scores_gemma":[0.999025,0.00013554681,0.00037164747,0.00042011213,0.000012254933,2.6923547e-7,0.0000019629827,6.757141e-7,0.000032543594],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99888724,0.00011782353,0.00031470758,0.00014615117,0.00022217634,0.00031189906],"domain_scores_gemma":[0.99920833,0.00020790927,0.00013957839,0.000099377765,0.000088776884,0.00025599988],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009443216,0.00008454372,0.00016669331,0.0002031934,0.0002324351,0.000079358804,0.0004388998,0.000035570156,0.0007511548],"category_scores_gemma":[0.0003557617,0.000048244365,0.000045739536,0.001104463,0.0006367365,0.00017083452,0.000003695219,0.00018789363,0.0000053290137],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000015588997,0.0000042668003,0.9957474,0.00000354289,0.0000025698653,0.000013156533,0.00024324656,0.0022156439,0.000048208483,0.00058938365,0.000027263179,0.0011037616],"study_design_scores_gemma":[0.00007537259,0.0002176217,0.99173677,0.000011949476,0.000012823876,0.00014978473,0.0005878409,0.0004323259,0.000053241718,0.0044895518,0.0021587992,0.000073944706],"about_ca_topic_score_codex":0.028239585,"about_ca_topic_score_gemma":0.686213,"teacher_disagreement_score":0.6579734,"about_ca_system_score_codex":0.000001979971,"about_ca_system_score_gemma":0.00044354057,"threshold_uncertainty_score":0.97823143},"labels":[],"label_agreement":null},{"id":"W2099392746","doi":"10.1139/e04-063","title":"Seismicity in the vicinity of the SNORCLE corridors of the northern Canadian Cordillera","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Induced seismicity; Geology; Seismology; Magnitude (astronomy); Epicenter; Tectonics; Lithosphere; Active fault; Moment magnitude scale; Focal mechanism; Earthquake swarm; Thrust fault; Volcano; Plate tectonics; Intraplate earthquake","score_opus":0.020474565906313275,"score_gpt":0.20088307000821898,"score_spread":0.1804085041019057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099392746","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97931004,0.00095052575,4.6786545e-7,0.0055359905,0.00042679708,0.000116566924,0.000054231285,7.4848265e-7,0.013604638],"genre_scores_gemma":[0.9984543,0.000024657706,0.00003150032,0.0013514438,0.00007689132,1.2927543e-7,2.7389643e-7,0.0000012978719,0.000059548187],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985344,0.00018580466,0.0003705124,0.000105247804,0.00042162355,0.000382418],"domain_scores_gemma":[0.9989538,0.00020300741,0.00029427098,0.00020424824,0.00012693251,0.00021772162],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012238774,0.000096165466,0.00019442885,0.00017087697,0.00060900435,0.000042147134,0.0011562153,0.000038201215,0.0006064063],"category_scores_gemma":[0.0002572785,0.00004383522,0.00012348604,0.00094178406,0.001056801,0.00016074051,0.00000843389,0.00027721832,0.000007666818],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021369815,0.0000034770476,0.9858697,0.0000025965903,0.000008220225,0.000004363008,0.0016250357,0.0068736332,0.0000025179427,0.000026788948,0.00017773286,0.005403774],"study_design_scores_gemma":[0.00010840731,0.00008711376,0.98988354,0.000050453298,0.000010577803,0.000042378804,0.0017697028,0.0005240976,0.00011962864,0.00013554169,0.007210609,0.000057935078],"about_ca_topic_score_codex":0.7442704,"about_ca_topic_score_gemma":0.9988413,"teacher_disagreement_score":0.25457087,"about_ca_system_score_codex":0.00000598849,"about_ca_system_score_gemma":0.0031208189,"threshold_uncertainty_score":0.6639724},"labels":[],"label_agreement":null},{"id":"W2099695915","doi":"10.1139/cjes-2014-0162","title":"Investigation of regional seismicity before and after hydraulic fracturing in the Horn River Basin, northeast British Columbia","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; British Columbia Oil and Gas Commission; U.S. Department of Energy","keywords":"Induced seismicity; Geology; Seismology; Seismogram; Seismometer; Tectonics; Hydraulic fracturing; Structural basin; Drainage basin; Magnitude (astronomy); French horn; Geomorphology; Geotechnical engineering; Geography","score_opus":0.0244524218907891,"score_gpt":0.19316413553802486,"score_spread":0.16871171364723575,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099695915","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99652076,0.0014954635,0.0000020264436,0.0010341954,0.00012090882,0.00005606579,0.000018651024,0.0000011612921,0.00075077027],"genre_scores_gemma":[0.9987437,0.00003052471,0.00020655002,0.00091433694,0.00007283931,2.0395449e-7,0.0000012147481,9.585114e-7,0.00002965541],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99907327,0.00008296176,0.00022169767,0.000107020416,0.00029942446,0.00021563472],"domain_scores_gemma":[0.99937576,0.000073161886,0.00013434111,0.000053431908,0.00009294514,0.00027033055],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009994935,0.000054252116,0.00013647067,0.000106698266,0.00020074777,0.00018866174,0.00019593973,0.000031266616,0.00012413431],"category_scores_gemma":[0.00008894561,0.000047558126,0.000032726264,0.00032112576,0.00093610963,0.00036787768,0.0000039715665,0.00014068377,0.0000026375542],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002374034,8.6152716e-7,0.99257237,0.0000030321362,0.0000038622334,0.00005445899,0.0018973282,0.00012162744,1.2448653e-7,0.0000024503147,0.00023544428,0.005106069],"study_design_scores_gemma":[0.00013818311,0.00018390648,0.99380434,0.00006671056,0.000005908306,0.00027779955,0.0009980062,0.00016837579,0.0000020034342,0.0014722476,0.0028291165,0.0000533858],"about_ca_topic_score_codex":0.4615619,"about_ca_topic_score_gemma":0.98680633,"teacher_disagreement_score":0.5252445,"about_ca_system_score_codex":0.000001682024,"about_ca_system_score_gemma":0.0006959907,"threshold_uncertainty_score":0.5420236},"labels":[],"label_agreement":null},{"id":"W2099979921","doi":"10.1139/e03-005","title":"Geology of Denman and Hornby islands, British Columbia: implications for Nanaimo Basin evolution and formal definition of the Geoffrey and Spray formations, Upper Cretaceous Nanaimo Group","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Simon Fraser University","keywords":"Geology; Cretaceous; Paleontology; Stratigraphy; Structural basin; Diachronous; Ecological succession; Paleomagnetism; Group (periodic table); Tectonics","score_opus":0.016272600106213893,"score_gpt":0.21156913696223026,"score_spread":0.19529653685601636,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099979921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930344,0.004351152,0.00012791937,0.0005283346,0.0001018266,0.0001609127,0.000098168384,0.0000010051306,0.0015962528],"genre_scores_gemma":[0.9983532,0.00021956708,0.0013049825,0.00007544967,0.000010297124,0.0000010954055,0.000004216132,0.0000010604989,0.000030171093],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99906427,0.00013520026,0.00028479568,0.000114945185,0.00009172779,0.00030908696],"domain_scores_gemma":[0.99912876,0.00025948457,0.0002074311,0.00006721423,0.00014746212,0.00018966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010849664,0.000055376426,0.00017426527,0.00014190486,0.0008295641,0.00007278213,0.00014295585,0.00008804933,0.000094138704],"category_scores_gemma":[0.00032292123,0.000051704832,0.000036307258,0.00022006105,0.0014061513,0.00038347923,0.000006598049,0.00011810511,4.572692e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045898387,0.0000028214815,0.9973549,0.000020552592,0.0000092381315,0.0000012815185,0.000094321236,0.000010093892,0.0000063421153,0.001982791,0.000117523465,0.00039551716],"study_design_scores_gemma":[0.00028622046,0.00030892124,0.9849653,0.000028074011,0.00001962159,0.0014865247,0.00041425737,0.0001172331,0.0000089426485,0.011801561,0.00050881103,0.000054481057],"about_ca_topic_score_codex":0.011637532,"about_ca_topic_score_gemma":0.8789989,"teacher_disagreement_score":0.8673613,"about_ca_system_score_codex":6.8802797e-7,"about_ca_system_score_gemma":0.0004605805,"threshold_uncertainty_score":0.99494404},"labels":[],"label_agreement":null},{"id":"W2100014424","doi":"10.1139/e06-033","title":"A possible egg of the dromaeosaur<i>Deinonychus antirrhopus</i>: phylogenetic and biological implications","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"American Museum of Natural History; Geological Society of America; National Science Foundation","keywords":"Taphonomy; Subaerial; Context (archaeology); Paleontology; Sedimentary depositional environment; Geology; Biology; Evolutionary biology","score_opus":0.019394848143323554,"score_gpt":0.2104522241388167,"score_spread":0.19105737599549316,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100014424","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9874151,0.004857351,0.00001528518,0.0012767797,0.00026616183,0.000048138154,0.000052368327,0.0000016368245,0.0060672252],"genre_scores_gemma":[0.9991673,0.00005037523,0.0005194796,0.00013485074,0.00006700209,1.2416814e-7,0.0000020210493,4.6922835e-7,0.000058364232],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99921554,0.00009289383,0.00023678617,0.000117849304,0.00007867884,0.00025827612],"domain_scores_gemma":[0.99942434,0.000107218555,0.00017063027,0.00008078685,0.000057763886,0.00015925893],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003746484,0.00006576498,0.00013110058,0.0001262716,0.00043618394,0.00002122796,0.0003511957,0.00006638158,0.00023447767],"category_scores_gemma":[0.000059890437,0.000037764046,0.00005116876,0.0003512457,0.0017852151,0.00009109202,0.0000044797066,0.00009780937,0.000005007491],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026136004,0.000002814746,0.9974645,0.0000011434017,0.0000035555413,0.0000040859077,0.000020027968,0.00026890833,0.00028102598,0.00093316904,0.000087222485,0.0009309536],"study_design_scores_gemma":[0.000077562945,0.00019198074,0.99277085,0.000008400993,0.000005232995,0.00045157774,0.000042790027,0.00011051193,0.00006713444,0.0049638045,0.0012601479,0.000049987637],"about_ca_topic_score_codex":0.009623005,"about_ca_topic_score_gemma":0.3068667,"teacher_disagreement_score":0.2972437,"about_ca_system_score_codex":6.655801e-7,"about_ca_system_score_gemma":0.0005906674,"threshold_uncertainty_score":0.996972},"labels":[],"label_agreement":null},{"id":"W2100084802","doi":"10.1139/e2012-021","title":"Rock denudation rates and organic carbon exports along a latitudinal gradient in the Hudson, James, and Ungava bays watershed","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Bayer Canada","keywords":"Denudation; Dissolved organic carbon; Geology; Total organic carbon; Lithology; Sedimentary rock; Geochemistry; Hydrology (agriculture); Environmental chemistry; Oceanography; Chemistry","score_opus":0.016180079042377598,"score_gpt":0.1974723889823941,"score_spread":0.18129230994001652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100084802","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955576,0.0031565004,0.000004203572,0.000462324,0.00017736049,0.000053705084,0.0000029708608,0.0000011994794,0.00058415096],"genre_scores_gemma":[0.99961066,0.000059807695,0.000081029764,0.00012123073,0.0000993447,1.8297999e-7,0.0000036922538,0.0000010748977,0.000022982545],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991194,0.000062047584,0.00019587866,0.00010465734,0.0001734219,0.00034457035],"domain_scores_gemma":[0.9994598,0.000050662406,0.00008587634,0.00005347321,0.000029104716,0.00032108958],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010687074,0.00008254417,0.000108377804,0.00012958953,0.00023497277,0.0001798026,0.00015653526,0.000030499572,0.00017677175],"category_scores_gemma":[0.000049802515,0.000050244755,0.000015365855,0.00022570905,0.00015747335,0.00045448754,0.0000041928265,0.00012053444,0.0000025147992],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000020418315,0.0000019578465,0.9970541,0.0000047152075,0.000002708052,0.000022699185,0.002186337,0.000033976492,0.00008579689,0.000008232011,0.00003645859,0.0005609672],"study_design_scores_gemma":[0.00011080959,0.00008840116,0.9953506,0.000022378725,0.000008497355,0.00048493146,0.0022083647,0.0003400097,0.00041854475,0.00015472714,0.0007355226,0.0000772367],"about_ca_topic_score_codex":0.017875534,"about_ca_topic_score_gemma":0.20179792,"teacher_disagreement_score":0.1839224,"about_ca_system_score_codex":0.0000019500392,"about_ca_system_score_gemma":0.00021049162,"threshold_uncertainty_score":0.9886645},"labels":[],"label_agreement":null},{"id":"W2100768227","doi":"10.1139/e01-034","title":"Lower Jurassic Amaltheidae (Ammonitina) in North America: paleobiogeography and tectonic implications","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of British Columbia","funders":"","keywords":"Terrane; Fauna; Geology; Craton; Paleontology; Biological dispersal; Tectonics; Geography; Ecology; Population","score_opus":0.017318958164002488,"score_gpt":0.2185864799896859,"score_spread":0.20126752182568342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100768227","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97193575,0.0087483805,0.000011898291,0.0014308727,0.0001893151,0.000062488376,0.000030277733,0.000003661088,0.017587356],"genre_scores_gemma":[0.9988793,0.00046505546,0.0004592124,0.00014312922,0.000043243588,3.7321843e-7,0.000001227949,5.2029765e-7,0.0000079529145],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989155,0.00006570715,0.00026813522,0.00017313409,0.00012947441,0.00044806],"domain_scores_gemma":[0.9990527,0.00011497731,0.00016440498,0.00008839502,0.000054439894,0.00052507926],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035175902,0.00010441793,0.00017972854,0.0006538413,0.00044207863,0.00010570177,0.0003212181,0.000047442438,0.00023861516],"category_scores_gemma":[0.00005159252,0.000082729974,0.00006756897,0.0013026588,0.0011245644,0.0003892575,7.7217925e-7,0.0002245319,0.0000064851642],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000050341437,0.000003522305,0.9234216,0.000001265364,0.0000055510263,0.00007651219,0.00010474463,0.000063149535,0.0000026303924,0.000033638964,0.000015373504,0.076266974],"study_design_scores_gemma":[0.00012550323,0.00028791695,0.995521,0.000017067969,0.0000063731773,0.00026899166,0.00024740392,0.00005833072,0.0000018161825,0.0004782416,0.0028852564,0.00010211766],"about_ca_topic_score_codex":0.010443306,"about_ca_topic_score_gemma":0.8881635,"teacher_disagreement_score":0.8777202,"about_ca_system_score_codex":7.900125e-7,"about_ca_system_score_gemma":0.00069087953,"threshold_uncertainty_score":0.99614626},"labels":[],"label_agreement":null},{"id":"W2100942156","doi":"10.1139/cjes-2013-0185","title":"The first substantive evidence of <i>Utatsusaurus</i> (Ichthyopterygia) from the Sulphur Mountain Formation (Lower–Middle Triassic) of British Columbia, Canada: a skull roof description in comparison with other early taxa","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Vedecká Grantová Agentúra MŠVVaŠ SR a SAV; University of Sydney","keywords":"Geology; Paleontology; Early Triassic; Siltstone; Taxon; Permian; Structural basin; Facies","score_opus":0.031338040251606525,"score_gpt":0.195964933754507,"score_spread":0.16462689350290047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100942156","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99384946,0.004304009,0.00010581719,0.0007829369,0.00035271305,0.00012409649,0.00015727202,0.0000012027808,0.00032251378],"genre_scores_gemma":[0.9995465,0.000051301657,0.0001465132,0.00016615164,0.00004905803,6.2392826e-7,0.000003315146,0.0000013130034,0.000035170964],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984126,0.00029903447,0.0005134078,0.00013461597,0.00031118732,0.00032916502],"domain_scores_gemma":[0.99807847,0.00087961665,0.00061267597,0.0001104881,0.0001741919,0.00014454352],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016653535,0.00007671934,0.00025711113,0.000062562474,0.00044419756,0.0001025587,0.0005373914,0.000059425238,0.00010671365],"category_scores_gemma":[0.00025245597,0.000058278045,0.0000422725,0.00041718848,0.0011060851,0.00065521355,0.0000040614777,0.0001888308,0.0000016608534],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000083220526,0.0000043197856,0.9959244,0.0000042808624,0.000012690592,0.000009822022,0.00045586968,0.0011655822,0.0000063697207,0.000017450282,0.0003156795,0.002000304],"study_design_scores_gemma":[0.00027328223,0.00059831934,0.99251634,0.00025911798,0.000014571119,0.000050139333,0.0012230588,0.0017508813,0.000010513227,0.0002508634,0.00297743,0.000075477255],"about_ca_topic_score_codex":0.9865354,"about_ca_topic_score_gemma":0.9999867,"teacher_disagreement_score":0.013451383,"about_ca_system_score_codex":0.0000121480425,"about_ca_system_score_gemma":0.0016392242,"threshold_uncertainty_score":0.40754166},"labels":[],"label_agreement":null},{"id":"W2101509673","doi":"10.1139/e03-067","title":"Partitioning of bacterial communities between travertine depositional facies at Mammoth Hot Springs, Yellowstone National Park, U.S.A.","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Microbial Community Ecology and Physiology","field":"Environmental Science","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"American Chemical Society Petroleum Research Fund; National Science Foundation","keywords":"Sedimentary depositional environment; Facies; Geology; Hot spring; Mammoth; Tufa; Spring (device); Geochemistry; Paleontology; Carbonate; Chemistry","score_opus":0.03204501400924425,"score_gpt":0.2297162474127601,"score_spread":0.19767123340351583,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101509673","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913738,0.00005297235,0.000030327874,0.00013514499,0.00017850644,0.000036884023,0.000043534572,0.000001627386,0.008147255],"genre_scores_gemma":[0.9986476,0.0000099685885,0.0009951146,0.00013372292,0.000039495986,4.472227e-7,0.000015335905,0.000002809087,0.00015552052],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989273,0.0002518952,0.00030540788,0.00006976723,0.00019561386,0.00025004498],"domain_scores_gemma":[0.9992856,0.00017950995,0.00022215827,0.00007175187,0.000047192378,0.0001937892],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008705204,0.00008195807,0.00017333745,0.000110343564,0.000691657,0.000024876126,0.00034000078,0.00005518774,0.0143512655],"category_scores_gemma":[0.000094026436,0.00007615737,0.000060839408,0.00018291666,0.0021947436,0.0002467393,0.000033116383,0.0001734533,0.00004007583],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003461596,0.000039546416,0.9502221,0.000009187917,0.00004653919,0.000009203902,0.0034364215,0.0043611177,0.036774285,0.0026051265,0.0023565523,0.000105330466],"study_design_scores_gemma":[0.0003753464,0.00039988777,0.9477214,0.000041900967,0.000018615543,0.00014903369,0.0009916245,0.000025734298,0.0138124265,0.0024470894,0.03383143,0.0001854958],"about_ca_topic_score_codex":0.003721512,"about_ca_topic_score_gemma":0.20656995,"teacher_disagreement_score":0.20284845,"about_ca_system_score_codex":0.000031297994,"about_ca_system_score_gemma":0.000346779,"threshold_uncertainty_score":0.98654974},"labels":[],"label_agreement":null},{"id":"W2101716389","doi":"10.1139/cjes-2014-0178","title":"What lies beneath: geophysical mapping of a concealed Precambrian intrusive complex along the Iowa–Minnesota border","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Precambrian; Geology; Mafic; Ultramafic rock; Magnetic anomaly; Geophysics; Seismology; Geochemistry","score_opus":0.05642846878412286,"score_gpt":0.26937772112606156,"score_spread":0.2129492523419387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101716389","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9903233,0.0021187104,0.00009315738,0.0037648536,0.0010349784,0.00012816337,0.000021040014,0.000003982751,0.0025118203],"genre_scores_gemma":[0.9964831,0.000048081456,0.0024673683,0.00048021972,0.00038544083,3.26209e-7,0.0000028550562,0.0000022092777,0.00013039385],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99804336,0.00027017717,0.0004440672,0.00019348296,0.00052286556,0.00052606856],"domain_scores_gemma":[0.99778193,0.00055621134,0.00032792895,0.0001399256,0.0003490239,0.0008449848],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012561801,0.00014871567,0.0003623475,0.00020538934,0.00035827834,0.00030206444,0.0007299085,0.00005188964,0.0007182308],"category_scores_gemma":[0.0005876728,0.000087686116,0.0001278827,0.0011106757,0.0011773747,0.00083745585,0.000013189335,0.00025661162,0.000033960267],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000114539085,0.00005767158,0.49092552,0.000048093927,0.00016359083,0.00018784846,0.010800872,0.0094970735,0.00037579364,0.0031123138,0.0024575708,0.48225912],"study_design_scores_gemma":[0.00030624613,0.0008800084,0.96588326,0.00009301989,0.000023732991,0.00009646512,0.0052226726,0.00423457,0.0001786614,0.004962146,0.017937157,0.0001820586],"about_ca_topic_score_codex":0.02943258,"about_ca_topic_score_gemma":0.1462984,"teacher_disagreement_score":0.48207706,"about_ca_system_score_codex":0.0000027134306,"about_ca_system_score_gemma":0.0014829098,"threshold_uncertainty_score":0.9770305},"labels":[],"label_agreement":null},{"id":"W2101796088","doi":"10.1139/e11-016","title":"Evidence for seamount accretion to a peri-Laurentian arc during closure of Iapetus <sup>1</sup>This article is one of a series of papers published in <i>CJES Special Issue: In honour of Ward Neale</i> on the theme of Appalachian and Grenvillian geology.<sup>2</sup> Geological Survey of Canada Contribution 20100465.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seamount; Accretionary wedge; Subduction; Ordovician; Accretion (finance); Laurentia; Paleontology; Seafloor spreading; Sedimentary rock; Mylonite; Volcanic arc; Basalt; Geochemistry; Tectonics; Shear zone","score_opus":0.02565363131649465,"score_gpt":0.20835477165973526,"score_spread":0.18270114034324061,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101796088","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947876,0.00073956524,0.000002102769,0.0038418022,0.00005883628,0.00019834434,0.00024030451,7.2912746e-7,0.00013072252],"genre_scores_gemma":[0.9995606,0.000073677984,0.00016190733,0.000082289414,0.000087066495,0.0000010750979,0.000009988504,0.0000014842725,0.000021922222],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976345,0.00031944318,0.00088201975,0.00020625189,0.00047250112,0.000485343],"domain_scores_gemma":[0.9979557,0.00058321445,0.00058819674,0.00013791141,0.0003847708,0.0003502013],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002724424,0.00014348175,0.00063285994,0.0002720209,0.00010370656,0.00001639319,0.00042569917,0.00009942506,0.0048196665],"category_scores_gemma":[0.0022191885,0.00009261534,0.00011015392,0.0009151204,0.0010397437,0.00032930402,0.000022867267,0.00019875151,4.583748e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002597225,0.00003549344,0.98877734,0.00005671965,0.000030729556,0.00000225853,0.0011762287,0.008392436,0.00075015024,0.00006770383,0.00010242067,0.000348773],"study_design_scores_gemma":[0.0003284522,0.0006634642,0.9891318,0.0001630101,0.000026974112,0.000009784464,0.0014276807,0.0011530138,0.0066015236,0.00027422232,0.00012468139,0.0000954066],"about_ca_topic_score_codex":0.43350592,"about_ca_topic_score_gemma":0.9046817,"teacher_disagreement_score":0.47117573,"about_ca_system_score_codex":0.0000089616005,"about_ca_system_score_gemma":0.0006290681,"threshold_uncertainty_score":0.99609005},"labels":[],"label_agreement":null},{"id":"W2101809863","doi":"10.1139/e10-054","title":"Structural and kinematic analysis of the Shagawa Lake shear zone, Superior Province, northern Minnesota: implications for the role of vertical versus horizontal tectonics in the Archean","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"College of Science and Engineering, University of Minnesota; University of Minnesota Duluth; University of Minnesota; Geological Society of America; McKnight Foundation","keywords":"Geology; Tectonite; Shear zone; Lineation; Sinistral and dextral; Shear (geology); Transpression; Population; Overprinting; Seismology; Simple shear; Geomorphology; Paleontology; Tectonics","score_opus":0.013331611114724763,"score_gpt":0.20925460605210006,"score_spread":0.1959229949373753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101809863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960598,0.00039581777,0.00000555531,0.003057427,0.00007435527,0.00011664314,0.00009002178,6.1250614e-7,0.00019978419],"genre_scores_gemma":[0.9996361,0.000005949621,0.0002786457,0.000042902026,0.000028961338,7.1324246e-7,0.0000030924757,6.563763e-7,0.0000029793578],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910367,0.00005415839,0.0003010896,0.00011180162,0.00020244546,0.00022683918],"domain_scores_gemma":[0.9988674,0.0006392637,0.00011192253,0.00014349984,0.00009792737,0.00014001934],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006814673,0.00007318754,0.00020348441,0.00013535455,0.00029139218,0.000052530577,0.00063744874,0.000035764602,0.00025789023],"category_scores_gemma":[0.0003774642,0.000029650166,0.00016227872,0.0009908198,0.0010745347,0.000096760574,0.000009183562,0.0001921728,4.1175736e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013044156,0.000003915187,0.9941417,0.000003196989,0.000050194583,5.595053e-7,0.00024323401,0.0018623646,0.00025156268,0.00052875094,0.0000016065998,0.002899862],"study_design_scores_gemma":[0.00011084746,0.00015351624,0.9804671,0.0000044488056,0.00019149046,0.000012254415,0.00074200274,0.016336916,0.000064707325,0.0015902565,0.0002824969,0.000043953387],"about_ca_topic_score_codex":0.014039368,"about_ca_topic_score_gemma":0.95877063,"teacher_disagreement_score":0.9447313,"about_ca_system_score_codex":8.434418e-7,"about_ca_system_score_gemma":0.00038379285,"threshold_uncertainty_score":0.99252623},"labels":[],"label_agreement":null},{"id":"W2101917694","doi":"10.1139/e10-050","title":"Holocene temperature records show millennial-scale periodicity","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Holocene; Geology; Pleistocene; Climatology; Forcing (mathematics); Holocene climatic optimum; Quaternary; Paleoclimatology; Climate change; Paleontology; Physical geography; Oceanography; Geography","score_opus":0.016145307272946566,"score_gpt":0.23023830111882018,"score_spread":0.2140929938458736,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101917694","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9831345,0.0010638016,0.0000012162534,0.0027425794,0.0020475243,0.00005486994,0.000023580127,0.0000047393787,0.010927162],"genre_scores_gemma":[0.99786305,0.000061300125,0.0010155846,0.00042139526,0.00027326428,1.415916e-7,0.0000030742315,0.0000015448788,0.00036064122],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985417,0.00011967367,0.00025642657,0.00019946134,0.0002687022,0.0006140476],"domain_scores_gemma":[0.99856114,0.0001179846,0.000120026605,0.00013500445,0.00017527734,0.0008905633],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015474698,0.00011664902,0.00022204594,0.00038132683,0.0009214167,0.0001626345,0.0006792062,0.00019148248,0.00687817],"category_scores_gemma":[0.0002764504,0.00008435826,0.00008382752,0.00047902163,0.0018301251,0.0003416099,0.0000051518614,0.00086460693,0.00017091376],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009049194,0.0000026485484,0.9986555,0.0000037355671,0.0000053510093,0.00013814733,0.00018350748,0.00006924856,0.000046068104,0.000029925983,0.00037202664,0.0004848002],"study_design_scores_gemma":[0.0001432367,0.00027628735,0.9919013,0.000013792666,0.000006254686,0.0012057377,0.00024253356,0.0001273818,0.00022136435,0.00032005596,0.005431375,0.00011069924],"about_ca_topic_score_codex":0.00523295,"about_ca_topic_score_gemma":0.77372295,"teacher_disagreement_score":0.76849,"about_ca_system_score_codex":2.41404e-7,"about_ca_system_score_gemma":0.002046487,"threshold_uncertainty_score":0.9940297},"labels":[],"label_agreement":null},{"id":"W2102056066","doi":"10.1139/e04-080","title":"Seasonal isotopic imprint in moonmilk from Caverne de l'Ours (Quebec, Canada): implications for climatic reconstruction","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Karst Systems and Hydrogeology","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Calcite; Geology; Cave; Bedrock; Dissolution; Precipitation; Geochemistry; Spring (device); Speleothem; Mineralogy; Geomorphology; Chemistry; Archaeology","score_opus":0.016281878683086004,"score_gpt":0.20928457388930993,"score_spread":0.19300269520622393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102056066","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99346757,0.00059640355,0.00024803812,0.0043880674,0.000578158,0.0001122512,0.00010337261,0.0000018235368,0.00050428894],"genre_scores_gemma":[0.9975645,0.000012982612,0.001970379,0.00026931366,0.00013696482,9.601049e-7,0.0000057910743,0.0000014720308,0.000037641395],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99899304,0.00003613577,0.00031764488,0.00013895449,0.0001200673,0.0003941691],"domain_scores_gemma":[0.9991361,0.000098174416,0.00018036808,0.00007359229,0.00006183968,0.0004499277],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004361173,0.00007784368,0.00017024111,0.00017609105,0.00025936775,0.00007308791,0.00026975665,0.000048441147,0.00042970767],"category_scores_gemma":[0.000074744945,0.00006653076,0.000047461584,0.00021760678,0.00020568434,0.00022052579,0.0000020045377,0.00011403172,0.0000045327592],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026415823,0.000001644217,0.981542,0.0000038006515,0.0000061505734,0.000012863419,0.00016563719,0.01090455,0.000019567351,0.0004338869,0.00004900104,0.0068582804],"study_design_scores_gemma":[0.00025904764,0.000062865685,0.9892292,0.000046331785,0.000006512565,0.00017843339,0.00037507105,0.0010717063,0.000037416627,0.0074388543,0.0012125603,0.00008199657],"about_ca_topic_score_codex":0.9834197,"about_ca_topic_score_gemma":0.9999391,"teacher_disagreement_score":0.016519416,"about_ca_system_score_codex":0.000034791683,"about_ca_system_score_gemma":0.009160087,"threshold_uncertainty_score":0.99645704},"labels":[],"label_agreement":null},{"id":"W2102176733","doi":"10.1139/e00-037","title":"Periodically forced self-organization in the long-term evolution of planktic foraminifera","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada; American Chemical Society Petroleum Research Fund","keywords":"Extinction event; Geology; Foraminifera; Extinction (optical mineralogy); Paleontology; Impact crater; Oceanography; Physics","score_opus":0.01744580101922377,"score_gpt":0.22989556184629562,"score_spread":0.21244976082707184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102176733","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99606323,0.0006640403,0.000055384266,0.001073764,0.00016922486,0.00007387948,0.0000035810779,0.0000018482885,0.0018950343],"genre_scores_gemma":[0.99962753,0.000044623474,0.00014673804,0.00011940876,0.00003344779,9.616912e-8,0.000004167243,7.686708e-7,0.000023235567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989064,0.00017122742,0.00026333777,0.00009355042,0.00024374272,0.00032174136],"domain_scores_gemma":[0.9992851,0.00018793691,0.00013084082,0.00007333159,0.00014680637,0.00017599737],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012886748,0.000060372255,0.00013005805,0.0003584377,0.00031040097,0.00005843614,0.00049105,0.00006880932,0.00091693393],"category_scores_gemma":[0.0002830257,0.00003902093,0.000026912676,0.0010198933,0.00055606675,0.0002519359,0.000002575167,0.00018789373,0.000025998403],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000065263935,0.000004607325,0.99843097,0.00000485517,0.0000040775026,0.00012809537,0.0006208584,0.0005027977,0.0000022170716,0.00014115583,0.000010997414,0.00014284406],"study_design_scores_gemma":[0.00015323349,0.0002766893,0.99741143,0.00002017782,0.0000056974654,0.0009924172,0.00039597164,0.00036300498,0.000010142088,0.0002599145,0.00006711744,0.000044191023],"about_ca_topic_score_codex":0.0017544063,"about_ca_topic_score_gemma":0.44417834,"teacher_disagreement_score":0.44242394,"about_ca_system_score_codex":9.3353583e-7,"about_ca_system_score_gemma":0.0015481903,"threshold_uncertainty_score":0.99999636},"labels":[],"label_agreement":null},{"id":"W2102246845","doi":"10.1139/e11-002","title":"Retro-arc extension and continental rifting: a model for the Paleoproterozoic Baker Lake Basin, Nunavut<sup>1</sup>Geological Survey of Canada Contribution 20100436.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Carleton University","funders":"Northwestern University","keywords":"Geology; Siliciclastic; Rift; Structural basin; Pull apart basin; Basin and range topography; Volcanic rock; Paleontology; Transtension; Geomorphology; Tectonics; Sedimentary basin; Facies; Geochemistry; Volcano","score_opus":0.03626160990353531,"score_gpt":0.19661090510478885,"score_spread":0.16034929520125354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102246845","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99684215,0.0011097307,0.00036857126,0.0009100608,0.00010137381,0.00014006572,0.00025944316,0.0000020184443,0.0002665914],"genre_scores_gemma":[0.9987835,0.000033198838,0.000668295,0.00039998099,0.000036436886,5.8483647e-7,0.00001676854,0.0000011094182,0.000060107257],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984575,0.00012176512,0.0004242084,0.00021673532,0.00031216798,0.00046760603],"domain_scores_gemma":[0.998225,0.00043870494,0.00027123312,0.00010002959,0.00045346902,0.0005116088],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0020533374,0.00012854108,0.00031713452,0.00008477875,0.0004602584,0.00004632961,0.00036518977,0.00007029058,0.0016238857],"category_scores_gemma":[0.0014031942,0.00006877763,0.00008980694,0.0003347813,0.0008048183,0.00015196543,0.000010821696,0.00017965178,0.0000015241585],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004898884,0.000005250338,0.99487317,0.0000035990022,0.000018212695,0.000012435669,0.000108668915,0.003977192,0.000013425079,0.0000397854,0.00024989445,0.0006493598],"study_design_scores_gemma":[0.00019727976,0.00022688345,0.84766835,0.000016608215,0.000026454394,0.000040125462,0.00014413349,0.14982939,0.00006245341,0.0014587691,0.00024032201,0.00008920951],"about_ca_topic_score_codex":0.6627714,"about_ca_topic_score_gemma":0.9950457,"teacher_disagreement_score":0.33227435,"about_ca_system_score_codex":0.0000019764884,"about_ca_system_score_gemma":0.0009317339,"threshold_uncertainty_score":0.99928874},"labels":[],"label_agreement":null},{"id":"W2102488445","doi":"10.1139/e05-056","title":"A comparison of Eastern North America and Coastal New England magma suites: implications for subcontinental mantle evolution and the broad-terrane hypothesis","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Division of Mathematical Sciences; Centre National d’Etudes Spatiales; Brigham Young University","keywords":"Geology; Basalt; Geochemistry; Magmatism; Mantle plume; Flood basalt; Mantle (geology); Trace element; Terrane; Subduction; Incompatible element; Rift; Earth science; Paleontology; Partial melting; Structural basin; Volcanism; Tectonics; Lithosphere","score_opus":0.028492286687555296,"score_gpt":0.22594673056845263,"score_spread":0.19745444388089733,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102488445","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99202335,0.0023440097,0.00019841855,0.005022002,0.000028577755,0.000071382216,0.00007125547,0.0000013071352,0.00023967266],"genre_scores_gemma":[0.99829876,0.000042407548,0.0013607752,0.00011294524,0.00009234075,2.6173097e-7,0.000005072543,6.5745695e-7,0.000086750115],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992942,0.000035424804,0.0002540251,0.00011154084,0.000105592815,0.00019916867],"domain_scores_gemma":[0.9990188,0.00036626833,0.00018219955,0.000047974332,0.00006193117,0.00032286314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021643324,0.00006965857,0.00021090252,0.000099038494,0.00023952727,0.000065152526,0.00017672456,0.000020138694,0.00032341044],"category_scores_gemma":[0.00017674996,0.00003940071,0.00006248971,0.00022716566,0.0007929734,0.00014548018,0.0000053597687,0.000062504136,0.0000031940324],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002516396,0.0000036957704,0.9599376,0.0000028584361,0.0000107573605,3.3154126e-7,0.00027464065,0.00038449187,0.00002927462,0.000031945972,0.000050510487,0.039248735],"study_design_scores_gemma":[0.0005082759,0.00018930541,0.9885895,0.000008340299,0.000038341906,0.000031157604,0.0003503822,0.0057832203,0.000027003463,0.0013253452,0.0030916245,0.000057482215],"about_ca_topic_score_codex":0.022826698,"about_ca_topic_score_gemma":0.6507508,"teacher_disagreement_score":0.6279241,"about_ca_system_score_codex":7.218531e-7,"about_ca_system_score_gemma":0.00014976629,"threshold_uncertainty_score":0.98368037},"labels":[],"label_agreement":null},{"id":"W2102547300","doi":"10.1139/e05-045","title":"Mississippian volcanic assemblage conformably overlying Cordilleran miogeoclinal strata, Turnagain River area, northern British Columbia, is not part of an accreted terrane","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Government of British Columbia; University of Alberta","funders":"","keywords":"Geology; Terrane; Geochemistry; Zircon; Volcanic rock; Volcanic arc; Outcrop; Volcano; Continental arc; Sedimentary rock; Paleontology; Subduction; Tectonics","score_opus":0.025454795767413368,"score_gpt":0.21015890390994016,"score_spread":0.1847041081425268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102547300","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99532574,0.00057720754,0.000007303941,0.00066602946,0.00017356906,0.000078398785,0.0003097225,0.000006296455,0.002855711],"genre_scores_gemma":[0.9975273,0.000042567688,0.00072457566,0.0010147518,0.0001863294,1.9239532e-7,0.000029238847,0.000002676397,0.000472352],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997558,0.000095900796,0.0007522257,0.00030770263,0.0006107537,0.0006754421],"domain_scores_gemma":[0.99759966,0.000105393236,0.00049840583,0.00016272771,0.00028631708,0.0013474743],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009013987,0.00016436241,0.00046347847,0.00018278924,0.00054324075,0.0005165012,0.0007709825,0.00010839534,0.02571483],"category_scores_gemma":[0.00015520277,0.00016246592,0.00023430029,0.000640441,0.0009230581,0.0009274376,0.000008862073,0.00030351282,0.000031985564],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017684299,0.00001679755,0.94990355,0.000007831164,0.000045996498,0.00016443344,0.0002717749,0.0019384909,0.0002047106,0.0000012260028,0.0003755164,0.047052],"study_design_scores_gemma":[0.00044235398,0.0007196554,0.9774187,0.00010294456,0.000059708942,0.00030926126,0.0005297724,0.009188859,0.00033113488,0.00042112602,0.010175595,0.00030085252],"about_ca_topic_score_codex":0.40606797,"about_ca_topic_score_gemma":0.98933494,"teacher_disagreement_score":0.583267,"about_ca_system_score_codex":0.0000043475743,"about_ca_system_score_gemma":0.00094127096,"threshold_uncertainty_score":0.9751758},"labels":[],"label_agreement":null},{"id":"W2102547420","doi":"10.1139/e04-085","title":"Early Proterozoic orogeny and exhumation of Wernecke Supergroup revealed by vent facies of Wernecke Breccia, Yukon, Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Breccia; Geology; Geochemistry; Supergroup; Orogeny; Proterozoic; Facies; Clastic rock; Volcanic rock; Metamorphism; Paleontology; Sedimentary rock; Volcano; Structural basin; Tectonics","score_opus":0.00987488440841499,"score_gpt":0.17139390252158773,"score_spread":0.16151901811317274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102547420","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945692,0.002968651,0.000006290755,0.0012758193,0.00007853727,0.000056181972,0.000099599194,0.0000014371959,0.00094428274],"genre_scores_gemma":[0.99918455,0.00005912985,0.00043787537,0.00013187651,0.00004252319,2.2996481e-7,0.0000064935207,0.0000010238149,0.00013631431],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985627,0.00005874235,0.0004941264,0.00015552074,0.00041870883,0.0003102076],"domain_scores_gemma":[0.99888957,0.00007630415,0.00031517856,0.00007696086,0.00016322573,0.00047879491],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005049654,0.0001096247,0.00029769153,0.00014578066,0.00015896403,0.00004389889,0.00032632326,0.00004576697,0.0033711486],"category_scores_gemma":[0.00013899145,0.00007675271,0.00006959641,0.0003834052,0.00048035203,0.00027391498,0.0000065421636,0.00011521956,0.000004260363],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008770477,0.0000070822352,0.9881252,0.000016725151,0.000021564132,0.000008376116,0.00020504193,0.00062618905,0.0005656653,0.000028489996,0.0003417105,0.010045183],"study_design_scores_gemma":[0.00018045744,0.0003633545,0.9911231,0.000054748096,0.00002509748,0.00003552767,0.00030125096,0.00072533666,0.0021061082,0.00040095008,0.0045549786,0.00012913281],"about_ca_topic_score_codex":0.7731697,"about_ca_topic_score_gemma":0.9807265,"teacher_disagreement_score":0.2075568,"about_ca_system_score_codex":0.0000040851264,"about_ca_system_score_gemma":0.00074067904,"threshold_uncertainty_score":0.9975399},"labels":[],"label_agreement":null},{"id":"W2102783673","doi":"10.1139/e03-058","title":"Travertine mounds of the Cave and Basin National Historic Site, Banff National Park","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Banff Centre; BP (Canada); Geological Survey of Canada","funders":"Parks Canada","keywords":"Cave; Geology; Spring (device); National park; Karst; Structural basin; Gypsum; Calcite; Archaeology; Paleontology; Geography","score_opus":0.026771106859653795,"score_gpt":0.22746221335016853,"score_spread":0.20069110649051475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102783673","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9606658,0.0013730741,0.0000037348157,0.0010021245,0.00040354382,0.000037712263,0.00002455161,7.362828e-7,0.036488704],"genre_scores_gemma":[0.99891645,0.00001822851,0.00028019736,0.00025694465,0.0000352774,9.59491e-8,0.0000013498159,6.295744e-7,0.00049079995],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883056,0.00016450285,0.00021652895,0.00010086263,0.0004478047,0.00023972234],"domain_scores_gemma":[0.99904245,0.0002679958,0.00013752899,0.000039799932,0.0002745473,0.00023770425],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017281707,0.000060437604,0.000119643046,0.0002485202,0.00043732376,0.000028877841,0.00023509593,0.000052618907,0.0014653765],"category_scores_gemma":[0.00074601005,0.00003950733,0.000043649212,0.00043855488,0.0010347054,0.00017068868,0.0000023431505,0.00017161165,0.0000096161475],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003432293,0.000002143955,0.99760747,0.0000026324499,0.000006195878,0.0000063910716,0.00014689127,0.00055115664,0.0000051697743,0.0012652052,0.00035282358,0.00005047528],"study_design_scores_gemma":[0.00013916715,0.0000910504,0.98749214,0.000009960639,0.0000040320765,0.00044056916,0.0000828397,0.00029294722,0.00004790629,0.0029037064,0.008447849,0.00004784698],"about_ca_topic_score_codex":0.0016646823,"about_ca_topic_score_gemma":0.19540288,"teacher_disagreement_score":0.19373819,"about_ca_system_score_codex":0.0000015176435,"about_ca_system_score_gemma":0.0025553342,"threshold_uncertainty_score":0.9994474},"labels":[],"label_agreement":null},{"id":"W2102816136","doi":"10.1139/e01-032","title":"Early Proterozoic magmatism in Yukon, Canada: constraints on the evolution of northwestern Laurentia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon University; University of British Columbia; University of Alberta; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Laurentia; Geology; Proterozoic; Orogeny; Rodinia; Craton; Zircon; Supergroup; Geochemistry; Supercontinent; Metamorphism; Rift; Gondwana; Paleontology; Paleozoic; Tectonics","score_opus":0.012973257257894503,"score_gpt":0.1746683153507142,"score_spread":0.1616950580928197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102816136","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99405485,0.00037559768,0.000012462301,0.0017350815,0.0001274244,0.000062237996,0.000021390091,8.728495e-7,0.0036101006],"genre_scores_gemma":[0.9996667,0.0000070762244,0.000059037455,0.0001903438,0.000031600317,1.7477902e-7,0.0000012094579,5.233835e-7,0.000043332704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886566,0.00007717521,0.0003156456,0.00011199899,0.00032956692,0.00029995345],"domain_scores_gemma":[0.99927175,0.000114226415,0.00018498584,0.000071214694,0.00008224292,0.00027556822],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000533774,0.00007770092,0.00015865813,0.00017149355,0.00014243198,0.000041782605,0.0003809443,0.000029555273,0.004986249],"category_scores_gemma":[0.000108591536,0.00004316655,0.000052688898,0.0006310919,0.00057632045,0.00012653672,0.0000029908642,0.0001624202,0.000013010789],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004111058,0.0000030994127,0.99547803,0.0000016970573,0.0000055365176,0.00005645285,0.000059450616,0.001550649,0.000011950819,0.00014962802,0.000035370922,0.0026439982],"study_design_scores_gemma":[0.00007665517,0.00014431363,0.9964276,0.000043193042,0.000005820206,0.00004056523,0.00030287978,0.00042927702,0.000039669787,0.002198966,0.0002340434,0.000056993526],"about_ca_topic_score_codex":0.954696,"about_ca_topic_score_gemma":0.9995989,"teacher_disagreement_score":0.04490291,"about_ca_system_score_codex":0.0000055863866,"about_ca_system_score_gemma":0.001463255,"threshold_uncertainty_score":0.99592334},"labels":[],"label_agreement":null},{"id":"W2102821614","doi":"10.1139/e09-060","title":"Heckethornia, a new genus of dimeropygid trilobites from the Lower Ordovician (Ibexian; Tulean and Blackhillsian) of the Great Basin, western USA","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Genus; Ordovician; Geology; Paleontology; Cladistics; SPINE (molecular biology); Holotype; Zoology; Biology; Phylogenetic tree","score_opus":0.02080287032203511,"score_gpt":0.2184656398347977,"score_spread":0.19766276951276257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102821614","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98112273,0.009125695,0.000009315611,0.0038276084,0.00037400163,0.000083657826,0.00007793754,0.0000013253087,0.005377731],"genre_scores_gemma":[0.9987779,0.000074071315,0.00045034007,0.0004848309,0.0001388543,2.9489712e-8,4.515158e-7,6.245713e-7,0.00007289536],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99865085,0.00016871642,0.00039679825,0.00016039732,0.000303204,0.00032003148],"domain_scores_gemma":[0.9986961,0.00026836572,0.0003717934,0.00017508578,0.00007199089,0.00041665026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00065626734,0.00012966285,0.00027999372,0.00013857153,0.00040259486,0.00007986188,0.0007217611,0.0000726858,0.00036408126],"category_scores_gemma":[0.00013803474,0.00006870443,0.00013818854,0.00049018353,0.0014464782,0.00028398924,0.0000018711621,0.00021553862,0.0000031427144],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001877117,0.0000041799112,0.9469496,0.0000014154828,0.000017188684,0.000016534928,0.0006544327,0.00003930909,0.000039586816,0.000033333115,0.0001639239,0.05206171],"study_design_scores_gemma":[0.00018798426,0.00054587994,0.99543005,0.0000812831,0.000032236167,0.00006931691,0.00024058534,0.000039984803,0.00020239955,0.0012328663,0.0018540046,0.000083436185],"about_ca_topic_score_codex":0.04144825,"about_ca_topic_score_gemma":0.6925091,"teacher_disagreement_score":0.6510608,"about_ca_system_score_codex":7.9234746e-7,"about_ca_system_score_gemma":0.0010250835,"threshold_uncertainty_score":0.9649348},"labels":[],"label_agreement":null},{"id":"W2102844373","doi":"10.1139/cjes-2012-0150","title":"A new high-resolution radiocarbon Bayesian age model of the Holocene and Late Pleistocene from core MD02-2494 and others, Effingham Inlet, British Columbia, Canada; with an application to the paleoseismic event chronology of the Cascadia Subduction Zone","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia; Royal Roads University; Geological Survey of Canada","funders":"","keywords":"Geology; Radiocarbon dating; Holocene; Pleistocene; Paleontology; Turbidite; Foraminifera; Varve; Chronology; Deglaciation; Oceanography; Structural basin; Sediment","score_opus":0.009437212522260706,"score_gpt":0.18333221684713763,"score_spread":0.17389500432487692,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102844373","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99548405,0.0011719427,0.0003851519,0.0024378716,0.00014065545,0.00030046928,0.000048883838,0.0000012629428,0.000029691615],"genre_scores_gemma":[0.99898636,0.00003913875,0.0006089888,0.00023036177,0.000038108068,0.0000013120944,0.0000033022889,0.0000020571645,0.00009039028],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998958,0.00015436209,0.00022968397,0.0001803943,0.00019481417,0.00028275073],"domain_scores_gemma":[0.9991447,0.000081016355,0.00022807137,0.00016747865,0.000079975805,0.000298782],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045056042,0.0000739055,0.00018024718,0.00006069533,0.0005107896,0.000069321504,0.00042183444,0.00007027059,0.00008236797],"category_scores_gemma":[0.000043033066,0.000050041057,0.000021862294,0.00031202473,0.0009786173,0.00011639188,0.000011295483,0.00020205762,4.5867137e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011734877,0.0000018517981,0.97598153,0.000003898662,0.000012572931,0.00000402519,0.00027850165,0.01862127,0.000021563541,0.000008866616,0.000089970694,0.0049641947],"study_design_scores_gemma":[0.00020240062,0.00023201476,0.9716493,0.000037487975,0.00001772323,0.00017711302,0.00017500561,0.026811218,0.000025325007,0.00055587856,0.00005660552,0.00005991136],"about_ca_topic_score_codex":0.9817981,"about_ca_topic_score_gemma":0.9997903,"teacher_disagreement_score":0.017992157,"about_ca_system_score_codex":0.0000033313845,"about_ca_system_score_gemma":0.0018869303,"threshold_uncertainty_score":0.39286324},"labels":[],"label_agreement":null},{"id":"W2103031558","doi":"10.1139/cjes-2014-0138","title":"Protolith of ultramafic rocks in the Kluane Schist, Yukon, and implications for arc collisions in the northern Cordillera","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Victoria","funders":"","keywords":"Geology; Schist; Ultramafic rock; Geochemistry; Zircon; Forearc; Olivine; Peridotite; Metamorphism; Protolith; Ophiolite; Metamorphic rock; Basalt; Subduction; Paleontology; Tectonics","score_opus":0.04038356351064095,"score_gpt":0.23776278771195247,"score_spread":0.19737922420131152,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2103031558","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9877799,0.00066055864,0.000013210884,0.009546878,0.000026406067,0.00023007058,0.000040312414,5.683385e-7,0.0017020665],"genre_scores_gemma":[0.999341,0.000013931029,0.00024425617,0.00035403518,0.000027674396,0.0000029283049,0.000003497651,4.314621e-7,0.000012237271],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991376,0.000094019604,0.0002628201,0.00010333902,0.00017985604,0.00022240053],"domain_scores_gemma":[0.9991127,0.00034170705,0.000120916695,0.000084686544,0.00012682585,0.00021314714],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013831862,0.00005912337,0.00014041868,0.00015029561,0.00018458562,0.00006752649,0.00049401243,0.000026878555,0.00009543678],"category_scores_gemma":[0.00047143514,0.000026767508,0.00004436789,0.0007444779,0.00043072697,0.00010503326,0.0000026130792,0.00013101056,0.0000016660034],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000058934475,0.000009131165,0.9947245,0.0000021593826,0.0000025104603,0.000003555704,0.0008133287,0.0025070454,0.000005334051,0.000110612884,0.000051948868,0.0017639599],"study_design_scores_gemma":[0.0001542501,0.00027937826,0.98299605,0.000016551592,0.0000083999585,0.000054648608,0.0028749444,0.0007831176,0.000007872065,0.0110312,0.0017473451,0.00004626138],"about_ca_topic_score_codex":0.03237522,"about_ca_topic_score_gemma":0.74747413,"teacher_disagreement_score":0.7150989,"about_ca_system_score_codex":0.0000012247616,"about_ca_system_score_gemma":0.00051389687,"threshold_uncertainty_score":0.9740683},"labels":[],"label_agreement":null},{"id":"W2103373488","doi":"10.1139/e01-079","title":"Holocene deltaic sedimentation along an emerging coast: Nastapoka River delta, eastern Hudson Bay, Quebec","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Rimouski; Université Laval","funders":"Université Laval","keywords":"Geology; Delta; Fluvial; Post-glacial rebound; Quaternary; Geomorphology; River delta; Holocene; Bay; Sea level; Facies; Glacial period; Oceanography; Erosion; Submarine pipeline; Paleontology; Structural basin","score_opus":0.04180092653507674,"score_gpt":0.2598912139088724,"score_spread":0.21809028737379563,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2103373488","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948078,0.0017054862,0.0000568484,0.0010959371,0.00060141546,0.00007193886,0.000018224833,0.000006446425,0.0016359],"genre_scores_gemma":[0.9982589,0.000047232254,0.00081711804,0.00037116735,0.00012869899,2.2622267e-7,0.000011814615,0.0000024941746,0.00036233175],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99810165,0.0002418927,0.00035043445,0.00023756221,0.00037838542,0.0006900533],"domain_scores_gemma":[0.9985553,0.0001180401,0.00019473974,0.000114575734,0.00015599554,0.0008613284],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010885757,0.00013665676,0.00020678974,0.00051805895,0.00079773384,0.00015398744,0.0005340181,0.00009630374,0.006646296],"category_scores_gemma":[0.000088866844,0.00011350156,0.000064131425,0.00047276588,0.0010263462,0.0010755297,0.000006199745,0.00030237783,0.0003581062],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000075418625,0.0000058952546,0.9908204,0.0000042350575,0.000011675401,0.0002520184,0.0013051616,0.0023019747,0.0000020081277,0.000031914107,0.00013325037,0.005123918],"study_design_scores_gemma":[0.0002864737,0.0004272756,0.9815406,0.000028073839,0.000013506674,0.0005403571,0.0013697658,0.014679312,0.000039257735,0.00019370932,0.0007345201,0.00014714217],"about_ca_topic_score_codex":0.08891154,"about_ca_topic_score_gemma":0.9361998,"teacher_disagreement_score":0.84728825,"about_ca_system_score_codex":0.0000013405305,"about_ca_system_score_gemma":0.00061980984,"threshold_uncertainty_score":0.99426174},"labels":[],"label_agreement":null},{"id":"W2103558929","doi":"10.1139/e00-091","title":"Controls on the distribution of thermal springs in the southern Canadian Cordillera","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":113,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Parks Canada","keywords":"Geology; Hydrothermal circulation; Meteoric water; Geochemistry; Fault (geology); Thermal; Petrology; Geomorphology; Paleontology","score_opus":0.016603638263822815,"score_gpt":0.18081794020338818,"score_spread":0.16421430193956538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2103558929","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9795536,0.00026638724,0.0000017889015,0.010212813,0.000062232015,0.00005550417,0.00005116028,7.036411e-7,0.009795809],"genre_scores_gemma":[0.99872583,0.000009986368,0.000008309689,0.0011609531,0.00005792662,1.7833871e-7,0.000003594977,4.7202536e-7,0.00003272691],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99893177,0.00011604283,0.00023554728,0.00009234831,0.00027373477,0.00035057846],"domain_scores_gemma":[0.9991499,0.00026409715,0.00012372929,0.000084743675,0.0000696194,0.00030788],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011426132,0.00007308176,0.00014099422,0.00011562757,0.00029415978,0.00007694963,0.0005938454,0.00003300966,0.0049347477],"category_scores_gemma":[0.0002704416,0.000031562024,0.000085964835,0.0006129426,0.00048506234,0.00007913817,0.0000018423067,0.00019449186,0.000043694738],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007126463,0.0000036648082,0.9947597,5.281572e-7,0.0000067979695,0.00004653603,0.00021925273,0.003040024,0.000017528684,0.00032835727,0.000056917175,0.0015136003],"study_design_scores_gemma":[0.00008293651,0.0001683634,0.992167,0.000016676537,0.000008728006,0.000026274207,0.0010527327,0.001085585,0.00002952192,0.0014918528,0.0038157473,0.000054596923],"about_ca_topic_score_codex":0.6078701,"about_ca_topic_score_gemma":0.97905946,"teacher_disagreement_score":0.37118933,"about_ca_system_score_codex":0.0000022181002,"about_ca_system_score_gemma":0.0004876748,"threshold_uncertainty_score":0.9959749},"labels":[],"label_agreement":null},{"id":"W2103699438","doi":"10.1139/e11-008","title":"Les pseudotachylites en conditions granulitiques de la zone de cisaillement paléoprotérozoïque de Tikachitine, terrane d’In Ouzzal (Bouclier Touareg, Algérie)","year":2011,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies Worldwide","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Terrane; Geomorphology; Seismology; Tectonics","score_opus":0.03226155933331592,"score_gpt":0.24706577818012668,"score_spread":0.21480421884681075,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2103699438","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94591266,0.007426028,0.00019787082,0.00713274,0.0004205155,0.00017277867,0.00020004854,0.00000874455,0.0385286],"genre_scores_gemma":[0.99022084,0.0005496239,0.0058892113,0.0008807667,0.00036390813,0.0000036428742,0.000007063754,0.0000048327324,0.0020801139],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9965306,0.0009048985,0.0005820907,0.00029728553,0.00030825497,0.0013768954],"domain_scores_gemma":[0.99749357,0.0007208447,0.00023153436,0.00011159574,0.000103579805,0.0013388554],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002828178,0.00026326845,0.00041067362,0.0002997285,0.0007491206,0.00019756352,0.0006501974,0.0001750915,0.011961361],"category_scores_gemma":[0.00045045555,0.00020845723,0.00019287158,0.00057787524,0.002411439,0.00035926735,0.000021084432,0.0006264961,0.00006631041],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021557817,0.00006772863,0.9699666,0.000030101819,0.00003776475,0.001066896,0.006250467,0.0008873515,0.000029352104,0.0051694675,0.0009471254,0.015525576],"study_design_scores_gemma":[0.00032592792,0.000814319,0.93589383,0.00022065394,0.000037833623,0.0005626046,0.0024194645,0.00045367525,0.00014728149,0.019707626,0.039151054,0.00026572705],"about_ca_topic_score_codex":0.3009377,"about_ca_topic_score_gemma":0.65302193,"teacher_disagreement_score":0.35208425,"about_ca_system_score_codex":0.000029964327,"about_ca_system_score_gemma":0.0015701603,"threshold_uncertainty_score":0.98894185},"labels":[],"label_agreement":null},{"id":"W2103974001","doi":"10.1139/e05-113","title":"Early Paleozoic development of the Maine-Quebec Boundary Mountains region","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Université du Québec","funders":"National Science Foundation","keywords":"Geology; Massif; Paleozoic; Pluton; Ordovician; Devonian; Ophiolite; Craton; Paleontology; Terrane; Geochemistry; Carboniferous; Orogeny; Geomorphology; Tectonics","score_opus":0.013590550174835785,"score_gpt":0.17724970569248935,"score_spread":0.16365915551765356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2103974001","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926286,0.00074158533,0.00003448833,0.0010361602,0.00017739648,0.000034710705,0.0000057494217,0.0000018423666,0.005339513],"genre_scores_gemma":[0.99846464,0.0000032990222,0.0007968107,0.00014838255,0.00008298001,7.9221216e-8,0.0000017860589,6.63321e-7,0.00050135574],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998795,0.000051205694,0.00037669129,0.00011960811,0.0003359668,0.00032154706],"domain_scores_gemma":[0.999252,0.00005792691,0.00024199288,0.00008337485,0.00010756037,0.00025713418],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004488353,0.00008609643,0.00016037747,0.0001486,0.0004900965,0.0000914929,0.00051940675,0.000039126935,0.001201664],"category_scores_gemma":[0.00006681254,0.00004620548,0.00011502819,0.0006499991,0.00078342203,0.00017403996,0.000006656932,0.00013031687,0.000018193963],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026955138,0.0000035138794,0.99575895,0.0000023522148,0.000007431569,0.000017790848,0.00010404951,0.00094714464,0.000048086196,0.00014063143,0.000105384315,0.0028619969],"study_design_scores_gemma":[0.00006509261,0.000054004046,0.9856226,0.000020265032,0.000010388975,0.00003596968,0.0001153623,0.00010564299,0.0004429134,0.0051238905,0.008331508,0.000072394774],"about_ca_topic_score_codex":0.1619651,"about_ca_topic_score_gemma":0.9410698,"teacher_disagreement_score":0.7791047,"about_ca_system_score_codex":0.000002685837,"about_ca_system_score_gemma":0.0014326259,"threshold_uncertainty_score":0.9997114},"labels":[],"label_agreement":null},{"id":"W2104389935","doi":"10.1139/e02-090","title":"Geochemistry and tectonic significance of alkalic mafic magmatism in the Yukon-Tanana terrane, Finlayson Lake region, Yukon","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Geological Survey of Canada; Yukon University; University of British Columbia","funders":"","keywords":"Geology; Mafic; Felsic; Geochemistry; Magmatism; Terrane; Basalt; Volcanic rock; Mantle (geology); Island arc; Petrology; Subduction; Tectonics; Volcano; Paleontology","score_opus":0.022199479450004136,"score_gpt":0.18501854411370838,"score_spread":0.16281906466370424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104389935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9843975,0.00496435,0.0000056638833,0.0033547524,0.000058714766,0.00005538161,0.000018756262,0.000001773821,0.0071431403],"genre_scores_gemma":[0.99915373,0.00020161584,0.00017207867,0.00031333513,0.00004473523,2.931805e-7,0.0000021969943,8.666956e-7,0.00011116743],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99871016,0.00008434959,0.0003639525,0.0001830893,0.00029742485,0.00036101913],"domain_scores_gemma":[0.9991309,0.00018257383,0.00022090929,0.000119098215,0.000058555397,0.00028795536],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006522863,0.00011163603,0.0002341522,0.00018337955,0.00018803094,0.000075646356,0.00052288914,0.000057826957,0.004890066],"category_scores_gemma":[0.00017654776,0.00006597423,0.000077192344,0.0008093844,0.00078159577,0.00017622177,0.000004479351,0.00021877258,0.000012943946],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005664389,0.000013580104,0.98445064,0.000026126445,0.000012926491,0.00020973131,0.00061714085,0.0013169021,0.00017848473,0.000062932406,0.0007198081,0.012386054],"study_design_scores_gemma":[0.00019737163,0.00025002356,0.98412275,0.00007878283,0.000024370582,0.00037004307,0.0007234193,0.005622877,0.0002738019,0.0051439977,0.0030245339,0.0001680544],"about_ca_topic_score_codex":0.0151213715,"about_ca_topic_score_gemma":0.51473176,"teacher_disagreement_score":0.49961036,"about_ca_system_score_codex":0.0000011794845,"about_ca_system_score_gemma":0.00013006834,"threshold_uncertainty_score":0.9960196},"labels":[],"label_agreement":null},{"id":"W2104426698","doi":"10.1139/e99-098","title":"The role of fluids during formation and evolution of the southern Superior Province lithosphere: an overview","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Geology; Greenstone belt; Geochemistry; Hydrothermal circulation; Archean; Provenance; Volcano; Volcanic rock; Lithosphere; Paleontology; Tectonics","score_opus":0.00904315933492286,"score_gpt":0.17354776820228357,"score_spread":0.1645046088673607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104426698","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98838335,0.010545406,9.640203e-7,0.00029660494,0.000025285137,0.000036094425,0.00001569598,8.1217627e-7,0.00069580734],"genre_scores_gemma":[0.99964947,0.00014569069,0.000087553475,0.000017573162,0.000021523465,6.103158e-8,3.4551366e-7,3.841094e-7,0.000077393815],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992876,0.000064756605,0.00022940715,0.00006522262,0.00019351038,0.00015949296],"domain_scores_gemma":[0.9995548,0.00003754508,0.00011943438,0.000068961774,0.000061362436,0.0001578871],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00043424027,0.000047776477,0.0000985589,0.000028128801,0.00036355955,0.000045218323,0.00029523333,0.000021992275,0.0011767313],"category_scores_gemma":[0.0000526788,0.00002183699,0.00005421039,0.00028416712,0.00052454695,0.0002690713,0.0000035236308,0.00006652816,0.0000035919193],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000754863,0.000002252164,0.97425884,0.000006587956,0.000004160939,7.2059356e-7,0.00027843504,0.000977267,0.00045171875,0.00010848675,0.0000010968552,0.023902897],"study_design_scores_gemma":[0.000053974505,0.0001275353,0.9879681,0.00003215304,0.0000117834925,0.000029122855,0.0012083784,0.003518152,0.00116565,0.005041072,0.0008032991,0.000040771658],"about_ca_topic_score_codex":0.025893653,"about_ca_topic_score_gemma":0.4071063,"teacher_disagreement_score":0.38121265,"about_ca_system_score_codex":0.0000012270204,"about_ca_system_score_gemma":0.00025512435,"threshold_uncertainty_score":0.9997363},"labels":[],"label_agreement":null},{"id":"W2104441139","doi":"10.1139/cjes-2015-0048","title":"Topographic features of the sub-Athabasca Group unconformity surface in the southeastern Athabasca Basin and their relationship to uranium ore deposits","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Government of Saskatchewan; University of Regina","funders":"","keywords":"Geology; Unconformity; Structural basin; Fault scarp; Uranium ore; Geomorphology; Geochemistry; Fault (geology); Paleontology; Uranium","score_opus":0.02677168054835739,"score_gpt":0.21454136721169265,"score_spread":0.18776968666333527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104441139","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98742473,0.00048514415,0.0006633609,0.009222459,0.00021347955,0.0000981698,0.0000035340734,0.0000024584388,0.0018866633],"genre_scores_gemma":[0.9988215,0.0000018164644,0.00077637634,0.00031588224,0.00002749961,4.820841e-7,1.2526986e-7,8.7005566e-7,0.000055435143],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989216,0.00017335356,0.00023213346,0.00014589977,0.0002678525,0.00025917153],"domain_scores_gemma":[0.9989895,0.00017951883,0.00016937758,0.00022311014,0.00015402991,0.00028441512],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023038168,0.000094327734,0.00013330794,0.00012390249,0.00027864098,0.000187108,0.001271956,0.000045788907,0.0000018173524],"category_scores_gemma":[0.0003887427,0.000048401,0.000062165054,0.0010174457,0.0003101074,0.00032841208,0.00005868864,0.00022779139,6.9555404e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000028956717,0.0000051347824,0.98808306,0.0000060797624,0.000003351598,0.000009620145,0.0072813416,0.00072266243,0.000053409014,0.0032752738,0.00009528338,0.00046189688],"study_design_scores_gemma":[0.00012155963,0.00010821246,0.9917752,0.00007870877,0.000002813332,0.0002473108,0.0028695762,0.00031009852,0.0005762499,0.0029151815,0.00091898313,0.00007607784],"about_ca_topic_score_codex":0.0043571307,"about_ca_topic_score_gemma":0.19184163,"teacher_disagreement_score":0.1874845,"about_ca_system_score_codex":0.000004056153,"about_ca_system_score_gemma":0.0006298841,"threshold_uncertainty_score":0.8229052},"labels":[],"label_agreement":null},{"id":"W2104708484","doi":"10.1139/e02-033","title":"U-Pb ages of plutonism, wollastonite formation, and deformation in the central part of the Lac-Saint-Jean anorthosite suite","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Université du Québec à Chicoutimi","funders":"","keywords":"Pluton; Geology; Geochemistry; Anorthosite; Shear zone; Gabbro; Zircon; Metamorphism; Plutonism; Petrology; Igneous rock; Tectonics; Plagioclase; Seismology","score_opus":0.016314672532485624,"score_gpt":0.17259171849164423,"score_spread":0.15627704595915862,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104708484","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953317,0.0010011751,0.000007456853,0.0027073664,0.00007008672,0.000049789393,0.000022556056,7.0940445e-7,0.00080918096],"genre_scores_gemma":[0.99952275,0.000092378235,0.000101655714,0.0002253875,0.000023352179,8.9942496e-8,0.0000018916763,3.5759086e-7,0.00003215309],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989855,0.00009685487,0.00034909789,0.00006459172,0.00026511474,0.00023883997],"domain_scores_gemma":[0.9993257,0.00012353878,0.00026226923,0.000068280046,0.00007178463,0.00014840593],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006628939,0.00006196518,0.0001339069,0.00013618363,0.0001920684,0.00005344304,0.00033571248,0.000027121787,0.00071072654],"category_scores_gemma":[0.0001422418,0.000029282037,0.000064016764,0.00068114453,0.00051342294,0.0003441084,0.0000050755284,0.00010566937,0.0000028033473],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001939006,0.0000036555045,0.990338,0.000006612081,0.00000387984,0.000002767225,0.001016238,0.0050838753,0.00002980337,0.000087627624,0.00004416468,0.0033814132],"study_design_scores_gemma":[0.000092689785,0.0001076369,0.988279,0.000035178815,0.000012663617,0.000038989205,0.00059636467,0.0068874112,0.0002996159,0.0008600651,0.002741884,0.000048504993],"about_ca_topic_score_codex":0.022632109,"about_ca_topic_score_gemma":0.44208446,"teacher_disagreement_score":0.41945234,"about_ca_system_score_codex":0.0000012238451,"about_ca_system_score_gemma":0.00006148991,"threshold_uncertainty_score":0.9838763},"labels":[],"label_agreement":null},{"id":"W2104769192","doi":"10.1139/cjes-2014-0157","title":"Lu–Hf zircon and Sm–Nd whole-rock isotope constraints on the extent of juvenile arc crust in Avalonia: examples from Newfoundland and Nova Scotia, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University; Memorial University of Newfoundland; Mount Royal University","funders":"Natural Sciences and Engineering Research Council of Canada; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Geology; Zircon; Geochemistry; Continental crust; Crust; Igneous rock; Craton; Mantle (geology); Proterozoic; Partial melting; Felsic; Anatexis; Continental arc; Petrology; Volcanic rock; Mafic; Paleontology; Volcano; Tectonics","score_opus":0.03441855735802415,"score_gpt":0.20148497718600428,"score_spread":0.16706641982798012,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104769192","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921144,0.0018046901,0.0000047620656,0.0036985478,0.00015917931,0.000055145778,0.000101804064,7.759943e-7,0.0020606595],"genre_scores_gemma":[0.99918544,0.000015719434,0.00018169048,0.0005266215,0.00004613388,7.450329e-8,0.0000041290314,8.293826e-7,0.00003933419],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987898,0.00007977053,0.00032316233,0.00018131261,0.0003276019,0.0002983817],"domain_scores_gemma":[0.99873626,0.00029348047,0.00016856033,0.00007627504,0.000087545624,0.00063790305],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000655617,0.000108204,0.00026576745,0.00012599965,0.0001287484,0.00009957531,0.00027036984,0.000038721202,0.0019371359],"category_scores_gemma":[0.00031417023,0.00006204462,0.00003163927,0.00029749714,0.0006923284,0.00013345739,0.000009271449,0.00017774117,0.0000064624955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009993487,0.0000038438557,0.99445564,0.0000025064744,0.0000108441245,0.00005406293,0.00017818417,0.0011627378,0.00007101044,0.000043526125,0.0003449585,0.0036626754],"study_design_scores_gemma":[0.0002609155,0.00023500664,0.992338,0.000059733735,0.0000146721595,0.00004580669,0.0018896703,0.0008514279,0.00011872072,0.0028259186,0.0012550427,0.00010511251],"about_ca_topic_score_codex":0.9691599,"about_ca_topic_score_gemma":0.999396,"teacher_disagreement_score":0.030236103,"about_ca_system_score_codex":0.000004806292,"about_ca_system_score_gemma":0.0014148938,"threshold_uncertainty_score":0.9989752},"labels":[],"label_agreement":null},{"id":"W2104917285","doi":"10.1139/e99-069","title":"Tectono-thermal evolution of deep crust in a Mesoproterozoic continental collision setting: the Manicouagan example","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Crust; Mantle (geology); Lithosphere; Continental crust; Continental collision; Mantle plume; Metamorphic core complex; Craton; Petrology; Geochemistry; Seismology; Geophysics; Tectonics; Extensional definition","score_opus":0.011090658330872959,"score_gpt":0.1836063888153291,"score_spread":0.17251573048445612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104917285","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942252,0.0010959362,0.0000088978095,0.00086385844,0.00007163512,0.0000694657,0.000010221485,0.0000017286351,0.0036530704],"genre_scores_gemma":[0.9994827,0.0000102407275,0.0002671262,0.00012328669,0.000057113855,2.0455964e-7,0.0000019117417,7.5674376e-7,0.00005669619],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99880475,0.00009536247,0.00036164885,0.00013685515,0.00027601336,0.0003253529],"domain_scores_gemma":[0.99934244,0.00011081736,0.0001577334,0.000077647346,0.00006119955,0.00025015266],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008849032,0.00008401184,0.00017932896,0.00017083775,0.00023369431,0.000058675847,0.00043493064,0.000042007137,0.012909269],"category_scores_gemma":[0.000093532144,0.0000470976,0.00009107357,0.0007070702,0.00050604943,0.0001976254,0.0000039325123,0.00016439284,0.000030842493],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016082084,0.0000071986865,0.9733155,0.0000025353975,0.00000645518,0.000024809478,0.00020253696,0.015192329,0.00027288924,0.00003589331,0.000017628196,0.010906157],"study_design_scores_gemma":[0.00016783246,0.0002143955,0.98845196,0.000024619421,0.0000105839845,0.000050624596,0.00048582864,0.007870412,0.0004236752,0.0012777008,0.00094699906,0.000075349555],"about_ca_topic_score_codex":0.1120803,"about_ca_topic_score_gemma":0.57624805,"teacher_disagreement_score":0.46416774,"about_ca_system_score_codex":0.0000031469178,"about_ca_system_score_gemma":0.0002766893,"threshold_uncertainty_score":0.98799306},"labels":[],"label_agreement":null},{"id":"W2104977894","doi":"10.1139/e02-056","title":"Physical and chemical properties of the Sulphur Mountain thermal springs, Banff National Park, and implications for endangered snails","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Aquatic Invertebrate Ecology and Behavior","field":"Environmental Science","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Banff Centre; Geological Survey of Canada; Natural Resources Canada","funders":"Parks Canada; World Wildlife Fund","keywords":"Spring (device); Snowmelt; Endangered species; Geology; Hydrology (agriculture); Weathering; Population; Ecology; Elevation (ballistics); Environmental science; Habitat; Oceanography; Snow; Geomorphology; Biology","score_opus":0.03689971236010938,"score_gpt":0.22606729129254063,"score_spread":0.18916757893243125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104977894","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971127,0.00008781233,0.0000048917586,0.0022745926,0.000035479483,0.000083997096,0.000007689212,6.589801e-7,0.00039220782],"genre_scores_gemma":[0.99948543,0.0000027031233,0.00024687033,0.00014332544,0.000028955505,0.0000028842103,7.845492e-8,0.0000015603042,0.000088174405],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995328,0.000020156043,0.00011778423,0.00008259256,0.00010783761,0.0001388142],"domain_scores_gemma":[0.9996977,0.0000383497,0.000087928245,0.000037307436,0.000023235389,0.00011551578],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027032246,0.00004550618,0.00007536479,0.00002559007,0.00024863632,0.000024175002,0.00016490923,0.000024214673,0.00023785744],"category_scores_gemma":[0.00009969263,0.000027744123,0.000026182544,0.00009567022,0.0012407206,0.00016671917,0.00001862702,0.00005799798,0.0000035020532],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045283095,0.000036673595,0.85508543,0.0000061105766,0.000008738609,8.0924974e-7,0.0020284383,0.000075777185,0.13715225,0.0015813239,0.00071435294,0.003305567],"study_design_scores_gemma":[0.00018683565,0.0000884574,0.97609174,0.000014544103,0.000014738778,0.000047633628,0.000166431,0.0016283814,0.020216238,0.0010345468,0.00043987817,0.00007059925],"about_ca_topic_score_codex":0.00029002022,"about_ca_topic_score_gemma":0.004804394,"teacher_disagreement_score":0.12100629,"about_ca_system_score_codex":0.000010407231,"about_ca_system_score_gemma":0.00009828043,"threshold_uncertainty_score":0.4571487},"labels":[],"label_agreement":null},{"id":"W2105107985","doi":"10.1139/e99-067","title":"Convergent margin on southeastern Laurentia during the Mesoproterozoic: tectonic implications","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":203,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Orogeny; Laurentia; Geochemistry; Continental margin; Continental crust; Continental arc; Quartz monzonite; Back-arc basin; Crust; Island arc; Metamorphism; Subduction; Petrology; Volcanic rock; Pluton; Paleontology; Tectonics; Ordovician; Volcano","score_opus":0.014501552898901595,"score_gpt":0.1915978508767153,"score_spread":0.1770962979778137,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105107985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987207,0.00057444826,0.0000027861242,0.0047735986,0.00009790065,0.000054594195,0.0000284792,0.0000035513694,0.0072576706],"genre_scores_gemma":[0.9987022,0.000027453636,0.00006397386,0.00042132247,0.00009202907,3.4775724e-7,0.0000019760687,8.2949316e-7,0.0006898544],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990084,0.00005566323,0.0002271916,0.00014556905,0.00021643683,0.0003467199],"domain_scores_gemma":[0.9992673,0.00005651597,0.00009106124,0.00011512,0.00004555872,0.00042445314],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034658378,0.00008761192,0.00012272065,0.00011135644,0.00057788496,0.00012060667,0.00052262424,0.000028363584,0.056597345],"category_scores_gemma":[0.00003493702,0.000045258992,0.00011187635,0.00044067425,0.00039567758,0.00010932424,0.0000028390953,0.00016744559,0.00045066743],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008314057,0.000004669031,0.9878509,0.000002037777,0.000016777969,0.000014243634,0.00009404456,0.004803896,0.000048690257,0.00006436436,0.000053759377,0.0070382757],"study_design_scores_gemma":[0.00008218331,0.00011568132,0.9906133,0.000013323501,0.000012737865,0.00006711532,0.00009620774,0.00035593825,0.00016040317,0.0022374925,0.0061705923,0.000075072974],"about_ca_topic_score_codex":0.010102564,"about_ca_topic_score_gemma":0.26224107,"teacher_disagreement_score":0.25213853,"about_ca_system_score_codex":9.552523e-7,"about_ca_system_score_gemma":0.0002027542,"threshold_uncertainty_score":0.9964892},"labels":[],"label_agreement":null},{"id":"W2105122419","doi":"10.1139/e2012-032","title":"Biostratigraphic, strontium isotopic, and geologic constraints on the landward movement and fragmentation of terranes within the Tofino Basin, British Columbia","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Terrane; Paleontology; Cenozoic; Sedimentary depositional environment; Chronostratigraphy; Structural basin; Subduction; Outcrop; Accretionary wedge; Neogene; North American Plate; Tectonics","score_opus":0.023280113843224304,"score_gpt":0.21820388484737765,"score_spread":0.19492377100415334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105122419","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942974,0.0015195231,0.0000022374882,0.0023154889,0.00022271568,0.000108155116,0.000020787527,8.9164587e-7,0.0015128214],"genre_scores_gemma":[0.9991672,0.00009095323,0.00010532659,0.000553015,0.000031462692,3.6666523e-7,0.0000011683587,4.7320847e-7,0.00005000822],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99917257,0.00015868555,0.00018166723,0.000080981175,0.00015494059,0.00025116073],"domain_scores_gemma":[0.99931407,0.0002699465,0.00013300769,0.00005187357,0.000042682997,0.00018839852],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014240877,0.000049163453,0.00011437444,0.000061104205,0.00051909004,0.00013743716,0.00017586863,0.00004294782,0.0012063626],"category_scores_gemma":[0.000097481396,0.000032854325,0.00002269249,0.00011955552,0.0024534424,0.00015527767,0.0000037696273,0.00015601613,0.0000021543071],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003710474,0.0000025398679,0.99864984,0.0000041814014,0.0000102400345,0.000007859957,0.00031986128,0.000026415397,0.000002665543,0.00018040015,0.000096821714,0.0006954441],"study_design_scores_gemma":[0.000103769875,0.00031694252,0.9967321,0.000023760565,0.0000075422145,0.00022165838,0.0016247767,0.0000729748,0.000022858609,0.0007234215,0.00011157659,0.000038607406],"about_ca_topic_score_codex":0.031913575,"about_ca_topic_score_gemma":0.85896444,"teacher_disagreement_score":0.82705086,"about_ca_system_score_codex":1.7745062e-7,"about_ca_system_score_gemma":0.00020532266,"threshold_uncertainty_score":0.9997067},"labels":[],"label_agreement":null},{"id":"W2105296157","doi":"10.1139/e2012-053","title":"A multispectral geological study of the Schrödinger impact basin","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Impact crater; Geology; Impact structure; Structural basin; Ejecta; Terrain; Meteor (satellite); Regolith; Orbiter; Geology of the Moon; Basalt; Geochemistry; Geomorphology; Astrobiology","score_opus":0.026605057969332508,"score_gpt":0.24261768506417422,"score_spread":0.2160126270948417,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105296157","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987094,0.000018143424,0.000022079746,0.0003338755,0.0001611385,0.00008874613,0.0000036437805,5.7211184e-7,0.00066243357],"genre_scores_gemma":[0.9997453,1.9843746e-7,0.0001069918,0.000031862724,0.00007629602,5.1448495e-7,3.5082388e-7,7.8499704e-7,0.000037717542],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993589,0.000045390505,0.0001635324,0.00006719251,0.00017042637,0.00019456552],"domain_scores_gemma":[0.999516,0.00002511415,0.00013626536,0.00006389142,0.00006735749,0.00019133913],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030152913,0.0000497934,0.00009513823,0.000089834146,0.00022188661,0.0000916791,0.0003292606,0.000009582496,0.0007429261],"category_scores_gemma":[0.000018128701,0.000025405008,0.000055011056,0.00029725124,0.00021994341,0.0005148667,0.0000066668663,0.0000936751,0.000026126494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[6.070114e-7,0.000015166595,0.9965463,1.5832315e-7,0.0000051000543,0.0000012217611,0.00052122347,0.0020470533,0.00020576786,0.00010201224,0.00019895918,0.00035643004],"study_design_scores_gemma":[0.000109441375,0.0003392792,0.9953752,0.000007507956,0.0000043354416,0.0000052850587,0.0023527755,0.00091766746,0.00011316021,0.0006429331,0.0000955756,0.00003681688],"about_ca_topic_score_codex":0.031478588,"about_ca_topic_score_gemma":0.020506976,"teacher_disagreement_score":0.010971612,"about_ca_system_score_codex":0.0000022191782,"about_ca_system_score_gemma":0.0005501579,"threshold_uncertainty_score":0.9973662},"labels":[],"label_agreement":null},{"id":"W2105451018","doi":"10.1139/cjes-2013-0152","title":"New geophysical models for subsurface velocity structure in the Nechako–Chilcotin plateau from 2.5-D waveform tomography","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Seismology; Inversion (geology); Seismic vibrator; Seismic tomography; Geophysics; Tectonics; Volcano; Mantle (geology)","score_opus":0.015537679250536564,"score_gpt":0.1996977196063098,"score_spread":0.18416004035577324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105451018","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99021685,0.00038970265,0.003924288,0.0029728848,0.00049402827,0.00012396068,0.00009372181,0.000008274236,0.0017763082],"genre_scores_gemma":[0.9864614,0.000008704982,0.011372151,0.0019077815,0.00021350068,1.08708626e-7,0.000008149488,0.0000018807443,0.0000263157],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988515,0.00007435322,0.00024023952,0.00016770844,0.00029247458,0.00037372028],"domain_scores_gemma":[0.99912703,0.00023283262,0.00014016338,0.00011521655,0.000053356307,0.00033137764],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000857588,0.00011228634,0.00017834082,0.0002452616,0.00032770177,0.00018990377,0.0007204464,0.000057562356,0.00023011939],"category_scores_gemma":[0.000073901116,0.00006864143,0.00009534734,0.00044655724,0.0002405678,0.00050177635,0.0000031917966,0.00024120921,0.0000043754007],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009363301,0.000018003204,0.5449802,0.00002048081,0.000048001057,0.000042608164,0.00856481,0.04556131,0.000117411466,0.0045198794,0.033657867,0.36237577],"study_design_scores_gemma":[0.00065809605,0.00076616474,0.4441098,0.00010973354,0.000024875577,0.000067196124,0.0014194741,0.26080626,0.0013920529,0.24834122,0.041915428,0.00038969752],"about_ca_topic_score_codex":0.1589157,"about_ca_topic_score_gemma":0.16636306,"teacher_disagreement_score":0.36198607,"about_ca_system_score_codex":0.0000020444786,"about_ca_system_score_gemma":0.00062064,"threshold_uncertainty_score":0.84884864},"labels":[],"label_agreement":null},{"id":"W2105598443","doi":"10.1139/e03-054","title":"Early Archean to Mesoproterozoic evolution of the Wyoming Province: Archean origins to modern lithospheric architecture","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":132,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Archean; Geology; Magmatism; Proterozoic; Craton; Mafic; Geochemistry; Rift; Lithosphere; Crust; Tectonics; Paleontology","score_opus":0.01260366972922443,"score_gpt":0.19189305019117653,"score_spread":0.17928938046195209,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105598443","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993714,0.00041881573,0.0015008674,0.0020857234,0.00017400013,0.00015850815,0.000016947466,0.0000029838075,0.00192816],"genre_scores_gemma":[0.99287695,0.0000013430437,0.0065572476,0.0003471598,0.00006068398,4.189893e-7,3.3615515e-7,0.000001556256,0.00015428032],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99834085,0.00014413163,0.0003355088,0.00022292449,0.00044759078,0.0005090229],"domain_scores_gemma":[0.9985711,0.00007756857,0.00015638598,0.00015275514,0.00012172241,0.00092045934],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00088108674,0.00012539641,0.00022524947,0.00019964034,0.00034639947,0.00008172963,0.0006844477,0.00004383511,0.0007744263],"category_scores_gemma":[0.0004985496,0.0000704763,0.00014283234,0.0012432277,0.00037302208,0.00012484615,0.000010884164,0.0002484384,0.00002266155],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012181575,0.0000069483767,0.94673663,0.000007727982,0.000013091844,0.000011190325,0.00076747435,0.041892167,0.0006824127,0.00047287723,0.00002611584,0.009371152],"study_design_scores_gemma":[0.000098905104,0.00054425414,0.967171,0.00006801098,0.000020018942,0.000053445467,0.00026268733,0.0008449089,0.0015112972,0.025397377,0.0038617966,0.00016629172],"about_ca_topic_score_codex":0.04068928,"about_ca_topic_score_gemma":0.40205562,"teacher_disagreement_score":0.36136636,"about_ca_system_score_codex":0.000009068039,"about_ca_system_score_gemma":0.0012956253,"threshold_uncertainty_score":0.96569884},"labels":[],"label_agreement":null},{"id":"W2105696285","doi":"10.1139/e10-078","title":"Volcanic ash in the Lower Cretaceous Chaswood Formation of Nova Scotia: source and implicationsGeological Survey of Canada Contribution 20100082.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Coal and Its By-products","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Bedford Institute of Oceanography; Geological Survey of Canada","funders":"","keywords":"Geology; Terrigenous sediment; Geochemistry; Volcanic ash; Authigenic; Volcanic rock; Rhyolite; Illite; Volcanic glass; Lapilli; Igneous rock; Diagenesis; Silicic; Basalt; Volcano; Sedimentary rock; Clay minerals","score_opus":0.01931293688584423,"score_gpt":0.20593933027901015,"score_spread":0.18662639339316592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105696285","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968701,0.0006179614,0.000024983527,0.0015904537,0.00037038242,0.00008548187,0.00006866493,5.825725e-7,0.000371416],"genre_scores_gemma":[0.9997701,0.000012376238,0.00005307356,0.00010444489,0.000037017802,5.2787136e-8,0.000007122627,5.6432947e-7,0.000015250045],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989901,0.0000985627,0.00032284297,0.000094915886,0.00026133074,0.00023219983],"domain_scores_gemma":[0.99895406,0.00020756619,0.00026027806,0.00009289537,0.0003140471,0.00017118255],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002088175,0.00006254692,0.00014861426,0.00013281521,0.00014253329,0.000040675408,0.00032501607,0.00003956908,0.00023996833],"category_scores_gemma":[0.00085388025,0.00003846436,0.000017951439,0.00054299406,0.0004182372,0.00026698393,0.000004249829,0.00018803976,0.0000017322913],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000104575465,0.000006426805,0.99597436,0.000005032011,0.0000027263961,0.0000052233563,0.000190666,0.00041972677,0.0001982763,0.00006882958,0.00043238015,0.002685874],"study_design_scores_gemma":[0.00010641041,0.00022776892,0.99685,0.000011311457,0.00000383367,0.00013459304,0.00015278699,0.0006551276,0.00029401417,0.00010649659,0.0014091006,0.00004856665],"about_ca_topic_score_codex":0.85525125,"about_ca_topic_score_gemma":0.99957716,"teacher_disagreement_score":0.14432594,"about_ca_system_score_codex":0.0000017594732,"about_ca_system_score_gemma":0.0020432353,"threshold_uncertainty_score":0.36246118},"labels":[],"label_agreement":null},{"id":"W2105930694","doi":"10.1139/e02-036","title":"Stratigraphy, structure, and geochronology of the Anyox Pendant, northwest British Columbia, and implications for mineral exploration","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Geochronology; Zircon; Geochemistry; Pyroclastic rock; Greenschist; Volcanic rock; Facies; Siltstone; Mafic; Basalt; Volcano; Paleontology; Metamorphism","score_opus":0.02044018695979276,"score_gpt":0.1893670062368356,"score_spread":0.16892681927704284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105930694","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962444,0.0017369027,0.000010712671,0.0014129139,0.00005495517,0.000059771297,0.00024324165,8.7397234e-7,0.00023626807],"genre_scores_gemma":[0.9991457,0.000084688676,0.0005891894,0.000107963584,0.00003346165,2.2284682e-7,0.0000045496963,4.238262e-7,0.000033803597],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99944574,0.000024017243,0.00018564344,0.00010876037,0.00007045687,0.0001653927],"domain_scores_gemma":[0.99947023,0.0000684541,0.00012989795,0.00004632203,0.00008740665,0.00019767864],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001214061,0.00004183999,0.00011776135,0.000050685467,0.0003495088,0.0001467352,0.00016059623,0.0000307595,0.0010112975],"category_scores_gemma":[0.00008018459,0.000033922224,0.000044240584,0.00026223995,0.00074104924,0.00020686274,0.0000032940727,0.00006141794,2.2951346e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[4.473346e-7,0.0000017113356,0.9922023,0.0000028853335,0.000005803013,8.4470236e-7,0.00003150054,0.00011098134,0.00009218183,0.000047609854,0.00012631313,0.0073774266],"study_design_scores_gemma":[0.00008336656,0.00015978202,0.98210216,0.0000073300744,0.0000152095945,0.00010096141,0.000074951335,0.00063399196,0.00002071157,0.016312389,0.00044424422,0.000044886543],"about_ca_topic_score_codex":0.16906986,"about_ca_topic_score_gemma":0.9918154,"teacher_disagreement_score":0.82274556,"about_ca_system_score_codex":3.2410435e-7,"about_ca_system_score_gemma":0.000084570405,"threshold_uncertainty_score":0.9999019},"labels":[],"label_agreement":null},{"id":"W2106172314","doi":"10.1139/e06-094","title":"Gradual encroachment of a rocky shoreline by an invasive sea during the Mississippian at the southeastern margin of the Maritimes Basin, Nova Scotia, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Nova Scotia Department of Energy; Technical University of Nova Scotia; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Evaporite; Onlap; Fluvial; Paleontology; Clastic rock; Structural basin; Marine transgression; Sedimentary depositional environment; Geochemistry; Geomorphology","score_opus":0.012166244245279578,"score_gpt":0.18349230788717513,"score_spread":0.17132606364189557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2106172314","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920042,0.0017017162,0.0000055995956,0.0042319577,0.00020757935,0.000097274555,0.00030270705,9.2776105e-7,0.0014480406],"genre_scores_gemma":[0.99925774,0.000011025819,0.000065146625,0.00028165738,0.000055769513,1.2641831e-7,0.000008952374,0.0000012769921,0.00031832952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99858433,0.00010878062,0.0004028954,0.00011039495,0.00047943625,0.00031414462],"domain_scores_gemma":[0.99899715,0.0001616983,0.00033028855,0.00014281303,0.00014510627,0.00022291853],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00065014855,0.00010541915,0.00015820476,0.00006792983,0.0006748527,0.000085158914,0.00079523725,0.00002972487,0.0017990038],"category_scores_gemma":[0.00008988825,0.000045521734,0.00006530106,0.0004410793,0.0007675383,0.00020534256,0.000015190947,0.00014012576,0.000002931761],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007782735,0.0000050302533,0.98943233,0.0000141808105,0.000008568379,0.000005102189,0.00023958467,0.008470454,0.000033324788,0.000021134754,0.0011491951,0.00061331515],"study_design_scores_gemma":[0.00011420247,0.00012740871,0.99254334,0.00004961181,0.000015294132,0.00011656118,0.001746519,0.0004095182,0.0014617529,0.00024955647,0.003085397,0.00008085818],"about_ca_topic_score_codex":0.9060806,"about_ca_topic_score_gemma":0.9986393,"teacher_disagreement_score":0.092558704,"about_ca_system_score_codex":0.000004091566,"about_ca_system_score_gemma":0.001844618,"threshold_uncertainty_score":0.9991135},"labels":[],"label_agreement":null},{"id":"W2106180230","doi":"10.1139/cjes-2013-0215","title":"The 5.2 magnitude earthquake near Ladysmith, Quebec, 17 May 2013: implications for the seismotectonics of the Ottawa–Bonnechere Graben","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismotectonics; Magnitude (astronomy); Seismology; Graben; Earthquake magnitude; Tectonics; Geometry","score_opus":0.02324281401113725,"score_gpt":0.22943651726530268,"score_spread":0.20619370325416542,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2106180230","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8826958,0.016265705,0.00037432404,0.088664725,0.0019682082,0.0007024631,0.00019157991,0.000013566458,0.009123634],"genre_scores_gemma":[0.99725884,0.000253725,0.0005559381,0.000668508,0.00017256885,0.0000019108218,0.0000010565527,0.0000040340365,0.0010834136],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983402,0.00016352725,0.00044427786,0.00017921187,0.0003256639,0.00054713426],"domain_scores_gemma":[0.99696463,0.001698371,0.00041887778,0.0003710905,0.00029077992,0.00025623234],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0024159017,0.00015065547,0.00021471114,0.00007567145,0.0032240856,0.00033675937,0.0013861776,0.00006167413,0.00019001823],"category_scores_gemma":[0.0007044521,0.000067207315,0.0002216334,0.0005646142,0.0017566332,0.00019970634,0.000015932057,0.00028225812,0.000015435584],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013836244,0.000008933423,0.8032868,0.000015820891,0.0001208626,0.0000017798441,0.0008454336,0.012119313,0.0000099261015,0.005809474,0.015764331,0.1620035],"study_design_scores_gemma":[0.00013504949,0.00014787594,0.72342706,0.000023970666,0.00003169197,0.000030896103,0.0003545924,0.0012732289,0.000027481396,0.0017230457,0.2727441,0.00008101229],"about_ca_topic_score_codex":0.07711798,"about_ca_topic_score_gemma":0.9458574,"teacher_disagreement_score":0.8687394,"about_ca_system_score_codex":0.000003032895,"about_ca_system_score_gemma":0.0016006948,"threshold_uncertainty_score":0.9980736},"labels":[],"label_agreement":null},{"id":"W2106604767","doi":"10.1139/cjes-2014-0040","title":"Origin and tectonometamorphic history of the Repulse Bay block, Melville Peninsula, Nunavut: exotic terrane or deeper level of the Rae craton?","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of New Brunswick","funders":"","keywords":"Geology; Zircon; Geochemistry; Craton; Archean; Gneiss; Terrane; Granulite; Metamorphism; Charnockite; Orogeny; Metamorphic facies; Laurentia; Supercontinent; Shear zone; Petrology; Metamorphic rock; Facies; Geomorphology; Paleontology; Paleozoic; Tectonics","score_opus":0.06533099404024009,"score_gpt":0.20032932904241518,"score_spread":0.1349983350021751,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2106604767","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940134,0.0018873964,0.000006653307,0.001235359,0.00038274328,0.000056060686,0.000021018934,0.0000011465114,0.002396218],"genre_scores_gemma":[0.998295,0.000019145333,0.00027044982,0.0003028989,0.000048496575,1.4207905e-7,3.6596052e-7,0.0000011414459,0.0010623422],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986562,0.0001515127,0.00040256538,0.0001672122,0.00034828216,0.00027418556],"domain_scores_gemma":[0.9988059,0.0002078322,0.0003535026,0.0001856438,0.000121218036,0.00032593455],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000978551,0.00011023617,0.00029335366,0.00014165125,0.00021741311,0.000025803936,0.0006992558,0.00004824634,0.004871037],"category_scores_gemma":[0.0006253155,0.00004664924,0.00015692934,0.00055899855,0.0016021975,0.0001304587,0.000017002672,0.00018436449,0.000004643876],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010435151,0.000006755064,0.99593025,0.000012102015,0.000019676854,0.0000064447613,0.00021907956,0.0015455274,0.00037188022,0.00007501775,0.00014754527,0.0016552848],"study_design_scores_gemma":[0.00015810138,0.00018127807,0.9883487,0.000046092322,0.000052510295,0.00012682518,0.0001406157,0.0013733475,0.0004727836,0.0015722947,0.0074342275,0.00009319487],"about_ca_topic_score_codex":0.020020206,"about_ca_topic_score_gemma":0.5988808,"teacher_disagreement_score":0.5788606,"about_ca_system_score_codex":0.000004346586,"about_ca_system_score_gemma":0.0009418708,"threshold_uncertainty_score":0.9960387},"labels":[],"label_agreement":null},{"id":"W2106679376","doi":"10.1139/e05-053","title":"Introduction to special issue of <i>Canadian Journal of Earth Sciences</i>: The Trans-Hudson Orogen Transect of Lithoprobe","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Saskatchewan; Geological Survey of Canada; University of Saskatchewan","funders":"","keywords":"Laurentia; Craton; Archean; Geology; Tectonics; Terrane; Earth science; Transect; Yilgarn Craton; Paleontology; Geochemistry","score_opus":0.015283020611727748,"score_gpt":0.19487611692147663,"score_spread":0.17959309630974887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2106679376","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9677597,0.0013141326,0.000061005027,0.02496906,0.00064885576,0.000098539145,0.00005890135,0.000001299814,0.005088476],"genre_scores_gemma":[0.9937294,0.00007994448,0.0027717897,0.0004099475,0.0028781793,1.0851401e-7,0.0000013814954,0.0000017494777,0.00012747667],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975639,0.00015366869,0.0008401375,0.00021378622,0.0006682836,0.0005602232],"domain_scores_gemma":[0.9977843,0.0001285526,0.00046697387,0.00012527376,0.0004088365,0.0010860605],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002649462,0.00015320705,0.00043468468,0.0011137766,0.00047317287,0.0001139347,0.0010455935,0.000074431686,0.017263655],"category_scores_gemma":[0.00033589423,0.00009019868,0.0002763168,0.002876482,0.0016599593,0.00046307617,0.00000354226,0.00028806413,0.00002558252],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011480597,0.00005550513,0.8036898,0.00004191397,0.00014992525,0.0000696551,0.0063775885,0.10543242,0.0042578736,0.00076619524,0.0076005924,0.07144377],"study_design_scores_gemma":[0.000550861,0.0034498246,0.50921756,0.00012787462,0.00018606395,0.000634798,0.0023390092,0.00078458857,0.027923431,0.0028827405,0.4514894,0.0004138644],"about_ca_topic_score_codex":0.07905601,"about_ca_topic_score_gemma":0.8894285,"teacher_disagreement_score":0.81037253,"about_ca_system_score_codex":0.00000257522,"about_ca_system_score_gemma":0.0022617695,"threshold_uncertainty_score":0.9836347},"labels":[],"label_agreement":null},{"id":"W2106704051","doi":"10.1139/e02-081","title":"\"Without a leg to stand on\": on the evolution and development of axial elongation and limblessness in tetrapods","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"McGill University","keywords":"Anatomy; Tetrapod (structure); Appendicular skeleton; Context (archaeology); Axial skeleton; Appendage; Biology; Forelimb; Permian; Osteology; Numerical digit; Skeleton (computer programming); Paleontology; Evolutionary biology","score_opus":0.02775934167750455,"score_gpt":0.22741969329711975,"score_spread":0.1996603516196152,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2106704051","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960554,0.00091311947,0.000064396016,0.0004838754,0.00018515902,0.00005915906,0.000005594093,6.0155105e-7,0.0022326908],"genre_scores_gemma":[0.9991628,0.000015049272,0.0006962902,0.00009616433,0.00001470688,1.9954847e-7,3.6651747e-7,4.1507334e-7,0.0000140419625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99932003,0.000117732685,0.00017775121,0.00009871875,0.00010830782,0.00017746212],"domain_scores_gemma":[0.999542,0.00014316378,0.00007554251,0.00003324906,0.00003396486,0.00017207173],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010998507,0.00005472877,0.00010153279,0.0002623041,0.00028235087,0.000018439876,0.00009486542,0.000038593134,0.00007577711],"category_scores_gemma":[0.00018015945,0.00003405061,0.000008802677,0.00022169213,0.00038177476,0.000100249155,0.0000011237579,0.000090501846,0.000003044302],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021360505,0.000002725534,0.99451303,0.0000022316979,0.0000028801926,0.0000042232227,0.0006162848,0.00059773115,0.0000151695285,0.0013485356,0.000007858474,0.0028679662],"study_design_scores_gemma":[0.00011805446,0.00035735,0.996588,0.000042284013,0.000001381801,0.00004203984,0.00091311545,0.00011199627,0.000059386017,0.0005633018,0.0011573578,0.00004573989],"about_ca_topic_score_codex":0.0013161459,"about_ca_topic_score_gemma":0.45810452,"teacher_disagreement_score":0.45678836,"about_ca_system_score_codex":0.0000037669913,"about_ca_system_score_gemma":0.0010605487,"threshold_uncertainty_score":0.5517837},"labels":[],"label_agreement":null},{"id":"W2106830333","doi":"10.1139/e05-040","title":"Genesis of the Olden wollastonite skarn, Sharbot Lake domain, Central Metasedimentary Belt, Grenville Province, southeastern Ontario, Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Skarn; Hornblende; Pyroxene; Gabbro; Diorite; Metamorphic rock; Pluton; Zircon; Metamorphism; Magma; Igneous rock; Olivine; Biotite; Hydrothermal circulation; Quartz; Fluid inclusions","score_opus":0.008157766712730968,"score_gpt":0.15810894464545946,"score_spread":0.1499511779327285,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2106830333","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915282,0.0010672495,0.0000026113933,0.0027864657,0.00030732137,0.00007382639,0.0001931916,0.0000014611036,0.004039634],"genre_scores_gemma":[0.9978098,0.000005172566,0.00065657415,0.0009121286,0.0001416703,1.658495e-7,0.000007418677,0.0000014447011,0.00046561557],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99809754,0.00008061025,0.00044641757,0.00019864524,0.00059243984,0.00058435655],"domain_scores_gemma":[0.99864554,0.000067498666,0.00030572238,0.00013807311,0.000092290466,0.00075086445],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042385794,0.00014878256,0.00027787118,0.00012584086,0.00039000143,0.00006324961,0.00080378796,0.000040314055,0.015788922],"category_scores_gemma":[0.000038262093,0.00008413342,0.00017647354,0.00048852403,0.00046010912,0.0001712112,0.000016081032,0.00020055173,0.000010356264],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000075300113,0.0000057979123,0.99125934,0.0000029021314,0.000035504385,0.000025362628,0.00017288717,0.0068490743,0.000028621791,0.000018571904,0.00031645462,0.0012779546],"study_design_scores_gemma":[0.00016129606,0.00009997197,0.970361,0.00002406525,0.00005184591,0.000050198396,0.00038174732,0.0002643415,0.00022158626,0.00049102295,0.027761389,0.00013155772],"about_ca_topic_score_codex":0.98566186,"about_ca_topic_score_gemma":0.99998593,"teacher_disagreement_score":0.027444933,"about_ca_system_score_codex":0.0000092228665,"about_ca_system_score_gemma":0.004775735,"threshold_uncertainty_score":0.98511076},"labels":[],"label_agreement":null},{"id":"W2106928330","doi":"10.1139/e2012-069","title":"Variations in salt expulsion style within the Sable Canopy Complex, central Scotian margin<sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of<i>Mesozoic–Cenozoic geology of the Scotian Basin</i>.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Petroleum Research Newfoundland and Labrador","funders":"Offshore Energy Research Association","keywords":"Geology; Canopy; Salt tectonics; Paleontology; Geomorphology; Tectonics; Geography; Archaeology","score_opus":0.020335616898203485,"score_gpt":0.20128196726603131,"score_spread":0.18094635036782783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2106928330","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98315305,0.0004237731,0.0000018756632,0.006597423,0.00035873626,0.00018940364,0.00008497924,0.0000011765213,0.009189578],"genre_scores_gemma":[0.99890137,0.0000460837,0.0003672267,0.0004236311,0.00014273706,5.2041145e-7,0.0000026965822,0.0000018194553,0.00011389784],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998,0.0003142155,0.0006968043,0.00011598943,0.00042820835,0.00044477903],"domain_scores_gemma":[0.9985323,0.00036506695,0.00056235184,0.00019518733,0.00015575181,0.00018932833],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018811182,0.000115854586,0.00031091657,0.00025444975,0.00029531855,0.000056629826,0.000738476,0.00006483318,0.024232924],"category_scores_gemma":[0.00059988507,0.000057824207,0.00008202253,0.0012709575,0.001384251,0.00066551013,0.00001863717,0.00024007249,0.000006445252],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003679907,0.000040257484,0.97466475,0.000022328322,0.000012742491,8.809061e-7,0.012853234,0.008821451,0.00012766746,0.0020767485,0.00090052537,0.000442623],"study_design_scores_gemma":[0.00022249923,0.00033528556,0.9831269,0.00013037682,0.000014849703,0.0000176409,0.0066043637,0.0014111903,0.002672882,0.0017127474,0.003663118,0.0000881714],"about_ca_topic_score_codex":0.060898174,"about_ca_topic_score_gemma":0.3429135,"teacher_disagreement_score":0.28201532,"about_ca_system_score_codex":0.000006016077,"about_ca_system_score_gemma":0.00091016246,"threshold_uncertainty_score":0.97665906},"labels":[],"label_agreement":null},{"id":"W2106972202","doi":"10.1139/cjes-2015-0028","title":"A new Gorstian radiolarian fauna from the upper Silurian of the Cape Phillips Formation, Cornwallis and Bathurst islands, Canadian Arctic","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"Université de Lille","keywords":"Paleontology; Geology; Fauna; Arctic; Taxon; Biostratigraphy; Genus; Cape; Sensu; Biozone; Structural basin; Oceanography; Ecology; Biology; Geography; Archaeology","score_opus":0.0225493618804409,"score_gpt":0.19491933407458414,"score_spread":0.17236997219414324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2106972202","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9550956,0.01662187,0.00003894316,0.011993223,0.001322993,0.0001609718,0.00024246462,0.0000027330045,0.014521204],"genre_scores_gemma":[0.99883956,0.00003862218,0.00046155317,0.00041669907,0.00020542246,1.09885356e-7,0.000002835529,8.800795e-7,0.000034312656],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99859935,0.00016908468,0.0003350701,0.00014129315,0.0003064809,0.00044874958],"domain_scores_gemma":[0.99783534,0.0001859559,0.00025307917,0.0001646647,0.00013243456,0.0014285295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010316571,0.00012673065,0.00020076272,0.00020102096,0.000764858,0.00019553515,0.0007602143,0.00008930274,0.00032184346],"category_scores_gemma":[0.00037406405,0.00006973867,0.00008463724,0.00046326665,0.00083767093,0.00056318153,0.00000176798,0.0002758761,0.0000050245544],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006153043,8.5026056e-7,0.9871617,0.0000017866283,0.000018772365,0.00001475123,0.0035280383,0.000087106346,0.0000024026424,0.00021637435,0.0012111536,0.007750893],"study_design_scores_gemma":[0.00024083295,0.00013978954,0.9862265,0.00005549677,0.00002766985,0.00022504828,0.0020346118,0.00039013606,0.000012008832,0.003158817,0.0073918845,0.0000971813],"about_ca_topic_score_codex":0.798494,"about_ca_topic_score_gemma":0.99738425,"teacher_disagreement_score":0.19889024,"about_ca_system_score_codex":0.0000052667597,"about_ca_system_score_gemma":0.005722566,"threshold_uncertainty_score":0.99991405},"labels":[],"label_agreement":null},{"id":"W2107011014","doi":"10.1139/cjes-2012-0058","title":"Thermochronological constraints on the Eocene exhumation of the Grand Forks complex, British Columbia, based on <sup>40</sup>Ar/<sup>39</sup>Ar and apatite fission track geochronology","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University; University of Calgary","funders":"","keywords":"Geology; Hornblende; Closure temperature; Biotite; Fission track dating; Metamorphic facies; Thermochronology; Metamorphic rock; Greenschist; Geochronology; Granulite; Geochemistry; Terrane; Zircon; Facies; Quartz; Paleontology; Tectonics","score_opus":0.019749766115997894,"score_gpt":0.18547416901600045,"score_spread":0.16572440290000257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107011014","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9900647,0.00025927433,0.000019069146,0.0048495857,0.000057303656,0.0002094152,0.000068565314,0.000005008698,0.004467118],"genre_scores_gemma":[0.9982908,0.000028545259,0.00016845035,0.001386261,0.00005893767,0.0000012736647,0.000009014934,0.0000018391428,0.00005487572],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99805975,0.00027914022,0.0004450789,0.00027859054,0.00046845226,0.00046898852],"domain_scores_gemma":[0.99844295,0.00050920155,0.00028885304,0.00016418935,0.00018702181,0.00040776428],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008452482,0.00014457188,0.00032892547,0.00010270914,0.0007987648,0.0003362928,0.0006069612,0.00013298915,0.03862679],"category_scores_gemma":[0.000527592,0.00008830177,0.00015381246,0.00042967833,0.0027269816,0.00019174941,0.000013544704,0.00036003583,0.0000321456],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032716176,0.00005870068,0.8278513,0.000020575744,0.00004757119,0.000037335547,0.00029763862,0.03974061,0.00013165845,0.00007465606,0.0030353097,0.12867196],"study_design_scores_gemma":[0.00031734552,0.0006442528,0.9212756,0.000112688336,0.000021446676,0.00007076572,0.00034288035,0.07290081,0.000046725192,0.0036678032,0.00046934254,0.00013030395],"about_ca_topic_score_codex":0.048553046,"about_ca_topic_score_gemma":0.2254609,"teacher_disagreement_score":0.17690787,"about_ca_system_score_codex":0.0000052192813,"about_ca_system_score_gemma":0.00031959248,"threshold_uncertainty_score":0.999987},"labels":[],"label_agreement":null},{"id":"W2107106881","doi":"10.1139/cjes-2015-0087","title":"Glacier velocities and dynamic discharge from the ice masses of Baffin Island and Bylot Island, Nunavut, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Glacier; Archipelago; Arctic; Glacier morphology; Physical geography; Geomorphology; Climatology; Geodesy; Oceanography; Arctic ice pack; Antarctic sea ice; Geography","score_opus":0.0204927206216936,"score_gpt":0.19958917005786353,"score_spread":0.17909644943616992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107106881","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98532194,0.010798485,0.000019996149,0.002438572,0.00041200558,0.000043654683,0.00035172453,8.6163664e-7,0.0006127556],"genre_scores_gemma":[0.9988616,0.00023619694,0.00034546375,0.0003371617,0.00006759293,1.1511513e-7,0.00000419708,0.0000012438821,0.00014642475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991882,0.000038222483,0.00020261384,0.000104183324,0.00024873452,0.00021803705],"domain_scores_gemma":[0.999115,0.00027368971,0.00013666667,0.00006115896,0.000092345465,0.00032115425],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038839757,0.00008149863,0.00015584122,0.00003159667,0.00037995272,0.000115415656,0.00020937908,0.000019477124,0.00024867954],"category_scores_gemma":[0.00016251105,0.000048353275,0.000018450692,0.00022275202,0.0005175266,0.00022030975,0.000008018998,0.00008549898,8.54324e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000040210753,7.4039855e-7,0.99527293,0.000002385763,0.000013445767,0.000009362787,0.0009956476,0.00032545766,0.0000013896894,0.00003674536,0.0019691328,0.0013687339],"study_design_scores_gemma":[0.00015913283,0.000090722846,0.96472716,0.000023636343,0.000013909004,0.000028801385,0.008130315,0.0016713446,0.0000030595038,0.0003756595,0.02470379,0.000072457595],"about_ca_topic_score_codex":0.8881395,"about_ca_topic_score_gemma":0.9997897,"teacher_disagreement_score":0.11165019,"about_ca_system_score_codex":0.0000028942775,"about_ca_system_score_gemma":0.001898819,"threshold_uncertainty_score":0.33684233},"labels":[],"label_agreement":null},{"id":"W2107148493","doi":"10.1139/e00-093","title":"New UPb and Ar/Ar isotopic age constraints on the timing of Eocene magmatism, Fort Fraser and Nechako River map areas, central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Geological Survey of Canada","funders":"","keywords":"Magmatism; Geology; Felsic; Plutonism; Igneous rock; Geochemistry; Volcanic rock; Pluton; Group (periodic table); Plateau (mathematics); Paleontology; Volcano; Tectonics","score_opus":0.015000031049643639,"score_gpt":0.1778333911643219,"score_spread":0.16283336011467825,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107148493","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952556,0.0009479301,0.000028131344,0.0014771641,0.000096418815,0.000055881752,0.000028576325,0.0000017844441,0.0021085169],"genre_scores_gemma":[0.99823385,0.00015501022,0.00075113936,0.00049332075,0.00006217771,7.0041295e-8,0.0000024319568,7.904014e-7,0.00030122354],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99904025,0.000038468635,0.00022408752,0.00014763536,0.00021376892,0.00033581303],"domain_scores_gemma":[0.9990498,0.00012124209,0.00012435621,0.00005478199,0.000040461808,0.0006093653],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00030557008,0.000071561764,0.0001869803,0.00006236882,0.00028665274,0.00024723305,0.00021156555,0.000041551495,0.011716476],"category_scores_gemma":[0.00009935765,0.000056076355,0.000053261178,0.00024387919,0.0010249641,0.00015362757,0.000006503707,0.00013156145,0.0000052657683],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021118306,0.0000021258468,0.92737156,0.0000034232137,0.000010602773,0.0001578811,0.00006064037,0.00007008102,0.0000061557153,0.000020269903,0.0009634702,0.07133169],"study_design_scores_gemma":[0.00014990535,0.00014347356,0.9901169,0.0000722427,0.000017625536,0.00014582547,0.00018827143,0.00041174373,0.000020338337,0.0064185862,0.0022360205,0.00007906631],"about_ca_topic_score_codex":0.21692972,"about_ca_topic_score_gemma":0.8442641,"teacher_disagreement_score":0.62733436,"about_ca_system_score_codex":9.618774e-7,"about_ca_system_score_gemma":0.0001986795,"threshold_uncertainty_score":0.98918694},"labels":[],"label_agreement":null},{"id":"W2107248173","doi":"10.1139/e09-071","title":"Kennetcook thrust system: late Paleozoic transpression near the southern margin of the Maritimes Basin, Nova Scotia","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; University of Alberta; Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Geology; Evaporite; Flysch; Paleontology; Graben; Carboniferous; Group (periodic table); Thrust fault; Pennsylvanian; Seismology; Geomorphology; Fault (geology); Structural basin","score_opus":0.010787522510362432,"score_gpt":0.17597352020946785,"score_spread":0.1651859976991054,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107248173","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9890284,0.0006739575,0.0000052514065,0.0028036141,0.0005746422,0.00006972925,0.000063055355,0.0000030490673,0.006778314],"genre_scores_gemma":[0.9991988,0.00000570443,0.00027824347,0.00024769738,0.00010266075,6.336082e-8,0.0000014383041,0.0000013119528,0.00016411275],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986255,0.00011966374,0.0003533383,0.00015100703,0.00038383238,0.00036663434],"domain_scores_gemma":[0.9989407,0.00017019671,0.00024658075,0.00017209182,0.00011942915,0.0003509675],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010287729,0.000115305374,0.00021811982,0.000078334095,0.0006332405,0.0001806308,0.0009776708,0.000070272894,0.013066309],"category_scores_gemma":[0.00012686073,0.00004860608,0.0001999698,0.0005929729,0.0018198447,0.00014279777,0.000008309654,0.00038092092,0.000083311104],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000060092875,0.0000034779127,0.99504405,0.000010867179,0.000014507257,0.000012344524,0.00026021228,0.0021094778,0.00035289922,0.00005919997,0.00011494987,0.002011978],"study_design_scores_gemma":[0.000114258015,0.00008290731,0.992233,0.00008186388,0.000048050486,0.0000761413,0.00055412273,0.002849116,0.0005082661,0.0009119243,0.0024375347,0.000102819],"about_ca_topic_score_codex":0.08186455,"about_ca_topic_score_gemma":0.7255703,"teacher_disagreement_score":0.6437057,"about_ca_system_score_codex":6.9587776e-7,"about_ca_system_score_gemma":0.00056543073,"threshold_uncertainty_score":0.9878359},"labels":[],"label_agreement":null},{"id":"W2107380103","doi":"10.1139/e10-074","title":"<i>Eudaemonema webbi</i> sp. nov. (Mammalia, Mixodectidae) from the late Paleocene of western Canada: the youngest known mixodectid","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"Princeton University","keywords":"Geology; Paleontology; Genus; Range (aeronautics); Paleogene; Zoology; Biology; Structural basin","score_opus":0.017743796790117384,"score_gpt":0.2025573935210509,"score_spread":0.1848135967309335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107380103","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9769209,0.005400334,0.0000044263406,0.008267306,0.0030471147,0.00009636247,0.00015075579,0.000003558382,0.0061092135],"genre_scores_gemma":[0.99774396,0.000117289135,0.00013548984,0.0012424935,0.00037403367,2.992583e-7,0.000002747841,0.000002516668,0.0003811647],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99814093,0.00020804137,0.00045895617,0.00018391939,0.0004943799,0.00051374955],"domain_scores_gemma":[0.9978072,0.00089643616,0.0004033564,0.00024621584,0.00021750001,0.00042927757],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015428452,0.00017231092,0.00029337849,0.00010076614,0.0011050231,0.00011776939,0.0010813633,0.00007437494,0.0008560412],"category_scores_gemma":[0.00037216066,0.00009086636,0.00009764218,0.00048535955,0.0016459381,0.00022547114,0.000010924557,0.00052048115,0.000022760936],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010093516,0.0000025936051,0.9958424,0.000002115116,0.00003638801,0.000033355802,0.00052566105,0.00024904145,0.000040277348,0.000024149975,0.002024893,0.0012090347],"study_design_scores_gemma":[0.00015852576,0.00007722149,0.96078366,0.00002826504,0.000032902233,0.00013863467,0.0009394185,0.00011639988,0.00007637671,0.000109307286,0.037421186,0.00011810355],"about_ca_topic_score_codex":0.9076553,"about_ca_topic_score_gemma":0.9999639,"teacher_disagreement_score":0.09230862,"about_ca_system_score_codex":0.000002867548,"about_ca_system_score_gemma":0.003498502,"threshold_uncertainty_score":0.9373051},"labels":[],"label_agreement":null},{"id":"W2107498297","doi":"10.1139/e02-077","title":"Reappraisal of the Beekmantown Group sedimentology and stratigraphy, Montréal area, southwestern Quebec: implications for understanding the depositional evolution of the Lower-Middle Ordovician Laurentian passive margin of eastern Canada","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Centre de Géomatique du Québec; Institut National de la Recherche Scientifique","funders":"Institut national de la recherche scientifique; University of Victoria","keywords":"Geology; Paleontology; Ordovician; Sedimentary depositional environment; Group (periodic table); Sedimentology; Carbonate platform; Conodont; Biostratigraphy; Shoal; Laurentia; Stratigraphy; Structural basin; Geomorphology; Tectonics","score_opus":0.023470837738972204,"score_gpt":0.2037262051532558,"score_spread":0.18025536741428358,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107498297","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99039394,0.0036574956,0.0010700728,0.0017686876,0.0004914893,0.00019624928,0.0003192586,7.3905414e-7,0.002102091],"genre_scores_gemma":[0.99978197,0.000005515241,0.00015029282,0.00003645281,0.000015165143,6.7430227e-7,0.0000010667853,6.0812977e-7,0.000008255461],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895144,0.00014167005,0.0003448325,0.000113779395,0.00021384828,0.00023444483],"domain_scores_gemma":[0.9989057,0.00024926453,0.0004902371,0.00012018368,0.00009604875,0.00013855743],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037586704,0.000088257,0.00016335891,0.00010356341,0.00060426816,0.000028754717,0.00038233836,0.00004990667,0.000023954968],"category_scores_gemma":[0.00006413563,0.000047990226,0.0001065186,0.000335237,0.0013169337,0.00014685998,0.0000016938994,0.00011451376,2.1040785e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010502337,0.0000064858928,0.983595,0.000007404706,0.000036724286,9.659385e-7,0.00028850528,0.00020542296,0.00006321369,0.0152324075,0.000036096015,0.0005172762],"study_design_scores_gemma":[0.00017188289,0.00016965604,0.9917501,0.000057848734,0.000039078277,0.000061293445,0.00277342,0.00016282687,0.00004184442,0.004653955,0.00006627965,0.000051803083],"about_ca_topic_score_codex":0.6869522,"about_ca_topic_score_gemma":0.99970675,"teacher_disagreement_score":0.3127546,"about_ca_system_score_codex":0.000004354706,"about_ca_system_score_gemma":0.0022224388,"threshold_uncertainty_score":0.4852297},"labels":[],"label_agreement":null},{"id":"W2107762566","doi":"10.1139/e11-073","title":"A Paleogene flora from the upper Bonnet Plume Formation of northeast Yukon Territory, Canada","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon Department of Tourism and Culture; Royal Tyrrell Museum; Royal Ontario Museum","funders":"","keywords":"Macrofossil; Paleogene; Geology; Paleontology; Archipelago; Flora (microbiology); Arctic; Cretaceous; Assemblage (archaeology); Taxon; Structural basin; Oceanography; Holocene","score_opus":0.021201148701485387,"score_gpt":0.16312545937673248,"score_spread":0.14192431067524708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107762566","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99615145,0.0007991676,0.00000186711,0.0019153658,0.000496588,0.00003185782,0.00021109988,0.000001062273,0.00039155874],"genre_scores_gemma":[0.99935466,0.000015294076,0.000036425638,0.00021197168,0.00035416905,1.2773332e-7,0.000010613987,1.4861412e-7,0.000016608084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992741,0.000046679324,0.00015429955,0.000049137263,0.0002356128,0.00024019407],"domain_scores_gemma":[0.9994237,0.000077187535,0.0001491535,0.000021582013,0.000057985606,0.00027041836],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036100438,0.00005102981,0.00008441153,0.000017158973,0.00038308225,0.000037493315,0.000297797,0.0000276506,0.0002747188],"category_scores_gemma":[0.000038782608,0.000018122088,0.000041820174,0.00016795279,0.00013046921,0.0004499962,0.000008742114,0.00006749701,0.000003921298],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008347638,0.000006373078,0.9897193,0.0000013423717,0.0000064702017,0.0000043388322,0.00042147515,0.000052470066,0.0020381252,0.00003402241,0.003749799,0.0039579463],"study_design_scores_gemma":[0.000039848546,0.00005936379,0.95472324,0.000024361518,0.000008029439,0.000027144268,0.0015661932,0.00008428031,0.00046248958,0.000029037012,0.042923357,0.000052674743],"about_ca_topic_score_codex":0.74427176,"about_ca_topic_score_gemma":0.9949549,"teacher_disagreement_score":0.25068313,"about_ca_system_score_codex":0.000011826748,"about_ca_system_score_gemma":0.00029937434,"threshold_uncertainty_score":0.3007978},"labels":[],"label_agreement":null},{"id":"W2107819840","doi":"10.1139/e08-026","title":"Classification of the Late Cambrian (Steptoean) trilobite genera <i>Cheilocephalus</i> Berkey, 1898 and <i>Oligometopus</i> Resser, 1936 from Laurentia","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Laurentia; Trilobite; Polyphyly; Paleontology; Geology; Genus; Ordovician; Zoology; Biology; Phylogenetics","score_opus":0.025293636451302805,"score_gpt":0.2073085219175936,"score_spread":0.1820148854662908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107819840","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.974291,0.013708635,0.000010763673,0.0006496242,0.0007114314,0.00007607475,0.00013470318,0.000003185096,0.010414551],"genre_scores_gemma":[0.99876976,0.00029762083,0.0005239393,0.00015639258,0.000115322546,1.6026817e-7,0.0000029888333,9.770321e-7,0.00013281839],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985558,0.00017106783,0.0004279435,0.00018139782,0.00032740764,0.0003363945],"domain_scores_gemma":[0.99873,0.00013992043,0.00041749256,0.00016425095,0.0001068302,0.0004414979],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006320027,0.00013009323,0.0002523283,0.0002279718,0.0007670769,0.00007204882,0.000567111,0.000093677954,0.00015626462],"category_scores_gemma":[0.00009018094,0.0000870249,0.0001158467,0.0005704494,0.001614432,0.0004373058,0.0000022162026,0.00022734705,0.0000031527281],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012369141,0.0000038832814,0.9945073,0.0000030733663,0.000022256085,0.00002125358,0.0005337786,0.000063478634,0.0005457639,0.00007433752,0.00038077193,0.0038317463],"study_design_scores_gemma":[0.0002455082,0.0001189119,0.9956056,0.00003860325,0.000026759832,0.00014090288,0.00022156523,0.00022819322,0.0006343258,0.00039014532,0.0022455729,0.00010389722],"about_ca_topic_score_codex":0.01910175,"about_ca_topic_score_gemma":0.42704278,"teacher_disagreement_score":0.40794104,"about_ca_system_score_codex":0.0000010627751,"about_ca_system_score_gemma":0.0010291121,"threshold_uncertainty_score":0.98743016},"labels":[],"label_agreement":null},{"id":"W2107843523","doi":"10.1139/e10-014","title":"Mineralogical, geochronological, and geochemical characterization of Early Devonian aquamarine-bearing dykes of the Zealand Station beryl and molybdenite deposit, west central New Brunswick","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; University of New Brunswick","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Pegmatite; Geology; Geochemistry; Batholith; Isochron; Zircon; Molybdenite; Allanite; Monazite; Gneiss; Quartz; Metamorphic rock; Fluid inclusions; Paleontology; Tectonics","score_opus":0.009430700626251176,"score_gpt":0.17991614695885597,"score_spread":0.1704854463326048,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107843523","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99852836,0.00018911263,0.000011693337,0.00094651146,0.000098625715,0.0000541001,0.000017987426,0.000001945934,0.00015165542],"genre_scores_gemma":[0.99906003,0.000048088816,0.0006999617,0.000074655065,0.000064890526,5.3094492e-8,0.0000072388266,9.2954485e-7,0.000044123575],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895376,0.000038832855,0.00034728198,0.00016058645,0.00021318979,0.0002863706],"domain_scores_gemma":[0.99899447,0.00010052435,0.00027577893,0.00007217252,0.00008772017,0.00046935197],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000245272,0.00010171133,0.00022178434,0.000115950315,0.00017964629,0.000091294045,0.0002262605,0.000082594495,0.0007336533],"category_scores_gemma":[0.00019283626,0.00005805664,0.000061619605,0.00034544975,0.00088970514,0.0002260397,0.00001646464,0.00022337116,0.0000011622698],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009816312,0.0000050775934,0.95510536,0.0000056410986,0.00000839631,0.000005821458,0.0001313271,0.000050248582,0.042432632,0.000056435485,0.000003749335,0.0021854877],"study_design_scores_gemma":[0.00013812435,0.00020778115,0.99330777,0.000021763364,0.000022241857,0.00009361972,0.000032991684,0.00044544367,0.004457496,0.0010696613,0.00012743147,0.00007565913],"about_ca_topic_score_codex":0.10159359,"about_ca_topic_score_gemma":0.50377756,"teacher_disagreement_score":0.40218395,"about_ca_system_score_codex":8.2032193e-7,"about_ca_system_score_gemma":0.00038593655,"threshold_uncertainty_score":0.90438896},"labels":[],"label_agreement":null},{"id":"W2108071412","doi":"10.1139/cjes-2013-0094","title":"Making faults run backwards: the Wilson Cycle and ore deposits","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Mesothermal; Subduction; Tectonics; Geochemistry; Base metal; Rift; Period (music); Seismology; Hydrothermal circulation; Fluid inclusions","score_opus":0.019704704923468992,"score_gpt":0.202969937895742,"score_spread":0.183265232972273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108071412","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98736876,0.0019209309,0.000010372744,0.0040843454,0.000120131896,0.000045605615,0.000004588978,0.0000024781643,0.0064428034],"genre_scores_gemma":[0.9981975,0.00002953948,0.00067045545,0.00095016963,0.000087333035,1.4817022e-7,7.5511946e-7,6.396275e-7,0.00006344725],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99905044,0.000055043096,0.00020061416,0.00012983195,0.00022420535,0.0003398764],"domain_scores_gemma":[0.9991833,0.000120572826,0.000112734924,0.00006336592,0.000086031774,0.0004340094],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00043674518,0.000082221944,0.00013352642,0.00009625648,0.0005099452,0.0002192596,0.00037330517,0.000034472152,0.0043380638],"category_scores_gemma":[0.00014003395,0.00004050419,0.000059377115,0.0003858738,0.0005583867,0.00032579643,0.000007001209,0.00014883572,0.000091673195],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000012933332,0.0000012819829,0.9833057,0.0000019905533,0.0000086209275,0.000018699282,0.00012556363,0.0009776801,0.000024358324,0.00006009821,0.00013310692,0.015341626],"study_design_scores_gemma":[0.000052941326,0.00011357055,0.98657644,0.000021378191,0.000012297841,0.00012736492,0.0004079758,0.0035168717,0.000052736308,0.007285424,0.0017555658,0.000077443976],"about_ca_topic_score_codex":0.033047646,"about_ca_topic_score_gemma":0.42279792,"teacher_disagreement_score":0.38975027,"about_ca_system_score_codex":6.338212e-7,"about_ca_system_score_gemma":0.00017165711,"threshold_uncertainty_score":0.9965721},"labels":[],"label_agreement":null},{"id":"W2108191880","doi":"10.1139/e01-058","title":"Saddle reef auriferous veins in a conical fold termination (Oldham anticline, Meguma terrane, Nova Scotia, Canada): reconciliation of structural and age data","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University","funders":"St. Francis Xavier University","keywords":"Geology; Fold (higher-order function); Anticline; Metamorphism; Crenulation; Geochemistry; Terrane; Metamorphic rock; Seismology; Tectonics; Shear zone","score_opus":0.054789061086553445,"score_gpt":0.2260972782762736,"score_spread":0.17130821718972017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108191880","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99575573,0.0010802038,0.0000030310032,0.001688487,0.00017869573,0.00004677585,0.000118916876,0.0000012242937,0.0011269461],"genre_scores_gemma":[0.9990197,0.000023319873,0.00064430194,0.00019166147,0.000050325365,2.6391083e-8,0.00001804872,7.931658e-7,0.00005184743],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99866015,0.00006374367,0.00044739805,0.0002071614,0.00033145017,0.0002901226],"domain_scores_gemma":[0.9990676,0.00015352262,0.0002156642,0.00012647286,0.00008046611,0.00035624488],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00059070264,0.00009396731,0.00026119826,0.00019481142,0.000107363674,0.000062969564,0.00045644512,0.000050657673,0.0028150268],"category_scores_gemma":[0.00049471547,0.000065794666,0.00003232964,0.00045426175,0.00041651953,0.00038246138,0.000011594644,0.00015594455,0.0000033083031],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000046979217,0.000004747924,0.9910355,0.000006750372,0.000007913909,0.00010466924,0.000095300486,0.0003726092,0.000066269975,0.00001744698,0.00016900545,0.008115051],"study_design_scores_gemma":[0.00020270284,0.00020474686,0.9733092,0.00003085258,0.000014712342,0.000082957995,0.0001271024,0.025072139,0.0000911872,0.00046529106,0.00030587456,0.000093211085],"about_ca_topic_score_codex":0.81473845,"about_ca_topic_score_gemma":0.99898756,"teacher_disagreement_score":0.18424912,"about_ca_system_score_codex":0.0000040143523,"about_ca_system_score_gemma":0.00049874326,"threshold_uncertainty_score":0.9980965},"labels":[],"label_agreement":null},{"id":"W2108238859","doi":"10.1139/e04-020","title":"Reconstruction of Taconian and Acadian paleostress regimes in the Quebec and northern New Brunswick Appalachians","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Centre de Géomatique du Québec; Institut National de la Recherche Scientifique","funders":"","keywords":"Sinistral and dextral; Geology; Orogeny; Seismology; Shear (geology); Shear zone; Compression (physics); Transpression; Tectonics; Fault (geology); Brittleness; Paleontology","score_opus":0.011097567590768976,"score_gpt":0.1823488406117701,"score_spread":0.17125127302100113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108238859","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99108684,0.0022292556,0.000005340122,0.0053648567,0.000055845205,0.000036421865,0.0000045755532,8.8944705e-7,0.0012160036],"genre_scores_gemma":[0.9991728,0.000091646434,0.00045450055,0.00018920821,0.00004925029,2.8832988e-8,8.014636e-7,4.6847902e-7,0.000041293075],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992582,0.000046886158,0.00022339931,0.000117481504,0.00014161922,0.00021238482],"domain_scores_gemma":[0.99935997,0.000071411865,0.00013133365,0.000049481394,0.000033182187,0.00035462872],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041402402,0.00007039759,0.00014982137,0.00018231847,0.00015262044,0.00007935267,0.00021452807,0.000041614512,0.00025028648],"category_scores_gemma":[0.00008486055,0.00004032072,0.000037758204,0.00040252012,0.0007609665,0.00020387024,0.0000024942117,0.00014600738,0.0000024180592],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000027414962,0.0000014854526,0.9756339,0.0000028099996,0.0000042277143,0.000016121408,0.0005839232,0.0007261865,0.0000056430167,0.00016429232,0.0000028753689,0.022855775],"study_design_scores_gemma":[0.0001475326,0.0001278374,0.9901279,0.00003834845,0.000010218347,0.00020378524,0.0014169674,0.00006837796,0.000034100423,0.0074545816,0.00031270244,0.000057628626],"about_ca_topic_score_codex":0.6864975,"about_ca_topic_score_gemma":0.9975744,"teacher_disagreement_score":0.3110769,"about_ca_system_score_codex":9.866098e-7,"about_ca_system_score_gemma":0.0010360084,"threshold_uncertainty_score":0.31559014},"labels":[],"label_agreement":null},{"id":"W2108317937","doi":"10.1139/e07-073","title":"Assessing the role of orogen-parallel faulting in post-orogenic exhumation: low-temperature thermochronology across the Norumbega Fault System, Maine","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Oregon State University; Yale University; U.S. Department of Energy; National Science Foundation","keywords":"Geology; Thermochronology; Fault (geology); Mesozoic; Paleozoic; Seismology; Orogeny; Paleontology; Fission track dating; Tectonics; Structural basin","score_opus":0.013706034821430667,"score_gpt":0.22460203630127226,"score_spread":0.21089600147984158,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108317937","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923307,0.004443383,0.000003321097,0.0014046727,0.0001277703,0.00007492207,0.000017523364,0.0000032102582,0.0015945382],"genre_scores_gemma":[0.9994105,0.000027572696,0.00020011814,0.00023746298,0.00009785022,4.3043352e-7,0.000004313176,0.0000013006941,0.000020418423],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99834734,0.00019868459,0.00048146863,0.00016737847,0.00032151706,0.0004836187],"domain_scores_gemma":[0.9988779,0.0002470307,0.00032579456,0.00013205038,0.00020133522,0.00021589658],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001189107,0.00012125826,0.000259738,0.00010603774,0.00092986604,0.00013997676,0.0007609898,0.000079164245,0.0012572706],"category_scores_gemma":[0.00021253104,0.000056540724,0.00013783625,0.00079829205,0.0010720992,0.00034526092,0.000013018685,0.00031532152,0.0000226323],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012355206,0.000009451553,0.96242166,0.000011176092,0.000040605162,0.00012584514,0.0022366317,0.027069954,0.0029619143,0.00013750304,0.000012491317,0.004960428],"study_design_scores_gemma":[0.00018456319,0.00014554661,0.9794685,0.00006018903,0.000015071399,0.0007914335,0.013441158,0.0037842542,0.0013198999,0.0004497018,0.00022076548,0.000118882825],"about_ca_topic_score_codex":0.01800185,"about_ca_topic_score_gemma":0.302253,"teacher_disagreement_score":0.28425115,"about_ca_system_score_codex":0.0000041498483,"about_ca_system_score_gemma":0.00067068957,"threshold_uncertainty_score":0.9996557},"labels":[],"label_agreement":null},{"id":"W2108400645","doi":"10.1139/cjes-2014-0041","title":"Microfacies and microstructures of subglacial and deglacial sediments from the Pingualuit Crater Lake (Ungava Peninsula, Canada)","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Center for Northern Studies; Institut National de la Recherche Scientifique; Université du Québec à Rimouski; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Glacial period; Glacier; Sedimentary depositional environment; Meltwater; Ice sheet; Facies; Geomorphology; Geochemistry; Paleontology; Structural basin","score_opus":0.012022477992517792,"score_gpt":0.2045781360392716,"score_spread":0.1925556580467538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108400645","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99526006,0.0021492068,0.0000021891956,0.001457022,0.0004417131,0.000045177134,0.00008353202,7.789244e-7,0.00056030316],"genre_scores_gemma":[0.99919105,0.000030012898,0.00017513623,0.00046270437,0.000097434044,5.8239447e-8,0.0000046944283,9.949069e-7,0.00003789585],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989292,0.0001747152,0.00021180841,0.00013749443,0.00021907555,0.00032772156],"domain_scores_gemma":[0.99908763,0.00033142534,0.00013279935,0.000066382454,0.00008200706,0.00029978278],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007629275,0.0000900248,0.00018796136,0.00010192837,0.0005970116,0.000087611115,0.00031143727,0.000060612696,0.00057887187],"category_scores_gemma":[0.0002048829,0.000056663797,0.000022381211,0.00013797815,0.0016609116,0.00013265922,0.000009806256,0.00018771146,0.0000021747676],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001322293,5.0951263e-7,0.9987758,0.0000032944963,0.000012173546,0.00001816156,0.00043223327,0.000021316555,0.000073045245,0.000030753294,0.00015315966,0.00046632226],"study_design_scores_gemma":[0.00018397562,0.00011618748,0.99340445,0.000014437457,0.00001096541,0.0001633395,0.00031457952,0.00008674833,0.00035428896,0.00064783904,0.0046365205,0.0000666755],"about_ca_topic_score_codex":0.37261876,"about_ca_topic_score_gemma":0.9982603,"teacher_disagreement_score":0.6256415,"about_ca_system_score_codex":3.1028148e-7,"about_ca_system_score_gemma":0.001513406,"threshold_uncertainty_score":0.63382405},"labels":[],"label_agreement":null},{"id":"W2108547825","doi":"10.1139/e10-025","title":"Large igneous provinces (LIPs), giant dyke swarms, and mantle plumes: significance for breakup events within Canada and adjacent regions from 2.5 Ga to the PresentThis article is one of a selection of papers published in this Special Issue on the the theme <i>Lithoprobe—parameters, processes, and the evolution of a continent</i>.Lithoprobe Contribution 1482. Geological Survey of Canada Contribution 20100072.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":397,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Frontier Geosciences (Canada); Geological Survey of Canada","funders":"","keywords":"Geology; Craton; Large igneous province; Mantle plume; Breakup; Flood basalt; Paleontology; Rift; Magmatism; Intraplate earthquake; Precambrian; Passive margin; Igneous rock; Lithosphere; Seismology; Tectonics; Volcanism","score_opus":0.008347476082540883,"score_gpt":0.1808518798287816,"score_spread":0.1725044037462407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108547825","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98553574,0.00072351197,0.00003429961,0.012309067,0.00012387396,0.00056773116,0.000651534,8.184695e-7,0.000053396147],"genre_scores_gemma":[0.9995481,0.000047155685,0.00006694105,0.00022950156,0.000059697082,0.000004685088,0.000009177978,0.0000011037863,0.00003363051],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998229,0.00030139642,0.0005212385,0.00020793226,0.00043943978,0.00030095936],"domain_scores_gemma":[0.9972871,0.0012911839,0.00057230884,0.000115099516,0.0005563853,0.00017793525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027807408,0.00011344495,0.000337353,0.000058817215,0.00031964586,0.00004428619,0.00032727123,0.000055234308,0.0006277355],"category_scores_gemma":[0.0031286243,0.000048763482,0.000036848596,0.00058885745,0.000868339,0.00011241628,0.00001664375,0.00021553351,7.905365e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006652747,0.00004240689,0.9937572,0.00003196074,0.000083387706,0.0000022545476,0.0012892267,0.0008095828,0.00072973006,0.00073940185,0.0013263678,0.0005232379],"study_design_scores_gemma":[0.00069063884,0.0003800057,0.98459375,0.000070156515,0.000060378818,0.000012968266,0.0012660634,0.005264126,0.0036097234,0.0029324605,0.0010248624,0.00009488294],"about_ca_topic_score_codex":0.98492026,"about_ca_topic_score_gemma":0.9997241,"teacher_disagreement_score":0.014803814,"about_ca_system_score_codex":0.000012770535,"about_ca_system_score_gemma":0.0019087035,"threshold_uncertainty_score":0.6873264},"labels":[],"label_agreement":null},{"id":"W2108638216","doi":"10.1139/e09-048","title":"Holmograptus spinosus and the Middle Ordovician (Darriwilian) graptolite biostratigraphy at Les Méchins (Quebec, Canada)","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University","funders":"Deutsche Forschungsgemeinschaft","keywords":"Biozone; Conodont; Paleontology; Biostratigraphy; Geology; Fauna; Ordovician; Group (periodic table); Trilobite; Ecology; Biology","score_opus":0.019390422236393513,"score_gpt":0.19587752995738483,"score_spread":0.17648710772099133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108638216","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93058145,0.036001816,0.000005117545,0.008743284,0.00046078765,0.00010767377,0.00004761109,0.0000048144875,0.024047444],"genre_scores_gemma":[0.9987335,0.00017100743,0.00023850852,0.0007051833,0.00008937091,1.4578039e-7,0.0000013077205,6.4405805e-7,0.000060312334],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99823576,0.00016203313,0.00039229819,0.0002206293,0.0003932975,0.00059597957],"domain_scores_gemma":[0.99851054,0.00017639234,0.0002631689,0.00013956348,0.000082802704,0.0008275235],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0007705085,0.00018676148,0.00029343014,0.00036886492,0.0018380537,0.00022494429,0.00057213183,0.00008140835,0.0001911611],"category_scores_gemma":[0.000089649504,0.000115047565,0.00014014178,0.00067526265,0.0024461495,0.0003544027,0.0000010636373,0.0002838395,0.0000010828257],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039110048,0.000002643498,0.96335655,0.0000037694017,0.00002490945,0.000152089,0.00043368238,0.000052210762,0.0000064569263,0.0019409882,0.0002509375,0.03373668],"study_design_scores_gemma":[0.00040468664,0.00021895922,0.99226946,0.000034629003,0.0000220856,0.00027778323,0.0006295908,0.00008398282,0.00001920203,0.0016024652,0.0042813537,0.00015577636],"about_ca_topic_score_codex":0.85297453,"about_ca_topic_score_gemma":0.99990594,"teacher_disagreement_score":0.14693141,"about_ca_system_score_codex":0.0000024601966,"about_ca_system_score_gemma":0.0023352208,"threshold_uncertainty_score":0.9994614},"labels":[],"label_agreement":null},{"id":"W2108921525","doi":"10.1139/e11-050","title":"Large fossil birds from a Late Cretaceous marine turbidite sequence on Hornby Island (British Columbia)","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal British Columbia Museum","funders":"","keywords":"Cretaceous; Paleontology; Geology; Turbidite; Mesozoic; Sequence (biology); Autapomorphy; Sedimentary rock; Structural basin; Biology","score_opus":0.030757223696543975,"score_gpt":0.20591265211473375,"score_spread":0.17515542841818976,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108921525","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9711144,0.002231696,0.000014474113,0.00015799525,0.0011143677,0.000054489155,0.00047695948,0.0000077494315,0.024827888],"genre_scores_gemma":[0.99780905,0.00013189205,0.0006606846,0.00044140252,0.00017372421,2.2924964e-7,0.0000147494275,0.0000018459929,0.0007664196],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99855393,0.00013342025,0.00028669956,0.00024967646,0.00019639188,0.00057986536],"domain_scores_gemma":[0.9988988,0.00011382233,0.00019163545,0.000110930756,0.0000836338,0.00060115865],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006477214,0.000099166675,0.00022633685,0.0001427965,0.00065017154,0.0001629176,0.0005212053,0.0001199415,0.016861733],"category_scores_gemma":[0.00014307693,0.00010623205,0.000075385076,0.00029833114,0.00080829643,0.00035764923,0.0000069080056,0.0002709089,0.00014929082],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015697013,0.000006733146,0.99306905,0.000001318652,0.000016915412,0.00077816244,0.00021229331,0.000046192115,0.000007181605,0.00001245692,0.00078300125,0.005051024],"study_design_scores_gemma":[0.00022711548,0.00066837994,0.98023635,0.00003458737,0.000011886605,0.0005244416,0.00010808563,0.0004992338,0.0000048399797,0.0041838693,0.013359516,0.00014170332],"about_ca_topic_score_codex":0.41059884,"about_ca_topic_score_gemma":0.99643016,"teacher_disagreement_score":0.58583134,"about_ca_system_score_codex":0.0000027463527,"about_ca_system_score_gemma":0.00097241416,"threshold_uncertainty_score":0.984037},"labels":[],"label_agreement":null},{"id":"W2109030467","doi":"10.1139/e10-058","title":"The Pikwitonei Granulite Domain, Manitoba: a giant Neoarchean high-grade terrane in the northwest Superior ProvinceThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.N. Machado, T.E. Krogh, and W. Weber are deceased.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; University of Alberta; University of Toronto; Geological Survey of Canada","funders":"","keywords":"Granulite; Geology; Terrane; Zircon; Geochemistry; Archean; Metamorphic rock; Protolith; Gneiss; Migmatite; Mafic; Orogeny; Metamorphism; Charnockite; Facies; Petrology; Paleontology; Tectonics","score_opus":0.018646234796686072,"score_gpt":0.1804556654695672,"score_spread":0.16180943067288114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109030467","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9872794,0.00085726054,1.9332664e-7,0.010068627,0.000073300864,0.00017395652,0.00007855749,8.6755267e-7,0.001467829],"genre_scores_gemma":[0.9991869,0.00016634689,0.00025182232,0.00029541936,0.00007936132,0.0000012684563,0.0000017989473,0.0000015532802,0.000015549236],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979843,0.00031290774,0.00069098163,0.00019996252,0.0004049346,0.0004069256],"domain_scores_gemma":[0.99871933,0.00040016024,0.0004218058,0.00018806574,0.00010463172,0.00016602749],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019126958,0.00014049016,0.00042604725,0.00026848333,0.0001643998,0.00004537818,0.00076308934,0.00007356786,0.004118299],"category_scores_gemma":[0.00031565854,0.00006642209,0.000103616716,0.000987077,0.0026113146,0.00024158637,0.000018740024,0.0003486364,0.00000194722],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000166095,0.00007018435,0.98855716,0.000022090515,0.000023454626,0.00005031811,0.006257917,0.00007029956,0.00062506733,0.00030071937,0.000060591075,0.003796097],"study_design_scores_gemma":[0.00036099125,0.0007105574,0.97620493,0.0001177108,0.000018872182,0.000028295346,0.011280734,0.000061027513,0.004343257,0.006363832,0.00042007153,0.00008969275],"about_ca_topic_score_codex":0.18986438,"about_ca_topic_score_gemma":0.93944365,"teacher_disagreement_score":0.74957925,"about_ca_system_score_codex":0.0000042980755,"about_ca_system_score_gemma":0.00034173636,"threshold_uncertainty_score":0.9967921},"labels":[],"label_agreement":null},{"id":"W2109059085","doi":"10.1139/e03-032","title":"Thermal annealing of fission tracks in fluorapatite, chlorapatite, manganoanapatite, and Durango apatite: experimental results","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Nuclear Materials and Properties","field":"Materials Science","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Dalhousie University","keywords":"Fluorapatite; Apatite; Fission track dating; Mineralogy; Anisotropy; Isotropic etching; Materials science; Annealing (glass); Etching (microfabrication); Isotropy; Crystallography; Analytical Chemistry (journal); Geology; Chemistry; Composite material; Optics","score_opus":0.023795050981875156,"score_gpt":0.2349222310133182,"score_spread":0.21112718003144304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109059085","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99571097,0.0016476497,0.000002407078,0.00011515489,0.00044059756,0.00008522701,0.000027385715,0.000003354199,0.001967226],"genre_scores_gemma":[0.99800456,0.000036668207,0.001803244,0.000071142116,0.000042960495,8.875892e-7,5.896809e-7,0.000007749522,0.000032229775],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9985397,0.00015285496,0.0005651878,0.00017683332,0.00025751186,0.0003079106],"domain_scores_gemma":[0.9991664,0.000055620654,0.0003165516,0.00010312014,0.00009374338,0.00026451063],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013802083,0.00011984447,0.00025578772,0.0003315546,0.00020496754,0.0001552652,0.00023541723,0.00005601713,0.000477949],"category_scores_gemma":[0.0002307339,0.0000890483,0.000038195347,0.00029375916,0.0004739049,0.000569363,0.000012109632,0.000084444815,0.0000056712643],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008351677,0.000025461357,0.030392714,0.000031938966,0.000003988811,0.00004908542,0.004347801,0.000583483,0.96324414,0.00042767703,0.00008100685,0.0007291839],"study_design_scores_gemma":[0.0010162683,0.000921677,0.11278447,0.00040349382,0.000007690074,0.00007493879,0.002015924,0.0001941413,0.8790801,0.00015289671,0.0030760881,0.0002722809],"about_ca_topic_score_codex":0.004047261,"about_ca_topic_score_gemma":0.0106625995,"teacher_disagreement_score":0.08416401,"about_ca_system_score_codex":0.000007886273,"about_ca_system_score_gemma":0.00040773666,"threshold_uncertainty_score":0.61182755},"labels":[],"label_agreement":null},{"id":"W2109069297","doi":"10.1139/e09-047","title":"Enhancing base-metal exploration with seismic imagingThis article is one of a series of papers published in this Special Issue on the theme<i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; University of Calgary; Bedford Institute of Oceanography; University of Toronto; Geological Survey of Canada; Cegep de Sainte Foy","funders":"","keywords":"Geology; Felsic; Lithology; Mineral exploration; Borehole; Base metal; Series (stratigraphy); Mafic; Mining engineering; Geochemistry; Seismology; Paleontology; Engineering","score_opus":0.010499608409967666,"score_gpt":0.18451161885359602,"score_spread":0.17401201044362835,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109069297","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98536533,0.00024996794,0.00005421453,0.010914009,0.00016302467,0.00015080246,0.000014687352,0.000002625342,0.0030853143],"genre_scores_gemma":[0.99794936,0.000033770328,0.0014357453,0.00044269089,0.00008295229,5.927249e-7,5.933025e-7,0.0000015720838,0.000052744308],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9989372,0.000093774994,0.00034681588,0.00011864854,0.0003283345,0.00017520878],"domain_scores_gemma":[0.9989752,0.00021530305,0.0004047157,0.000109106666,0.00020549567,0.00009013647],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019012745,0.000079821504,0.00020120731,0.0002414547,0.0001517413,0.000078264624,0.00026626838,0.000026789841,0.0013612082],"category_scores_gemma":[0.00045970763,0.000041382336,0.00003544109,0.00061129656,0.0015365604,0.0008118535,0.000004710596,0.00019662932,8.961864e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012788377,0.000121372774,0.88408136,0.00031651868,0.00013570586,0.000025578696,0.051198788,0.0014941168,0.019409481,0.0034723135,0.0062281387,0.032237787],"study_design_scores_gemma":[0.0028410752,0.0031652688,0.09782463,0.0014780896,0.00014587816,0.0002352436,0.047318317,0.018307228,0.79911673,0.013608827,0.01539831,0.0005604113],"about_ca_topic_score_codex":0.04763572,"about_ca_topic_score_gemma":0.077888034,"teacher_disagreement_score":0.78625673,"about_ca_system_score_codex":0.0000025047011,"about_ca_system_score_gemma":0.0008197022,"threshold_uncertainty_score":0.99955165},"labels":[],"label_agreement":null},{"id":"W2109185299","doi":"10.1139/e00-059","title":"Dimorphism and a new record of<i>Barroisiceras</i>De Grossouvre (Ammonoidea) from the Coniacian of Bagh, central India","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Ammonoidea; Ammonite; Cretaceous; Paleontology; Geology; Sexual dimorphism; Intraspecific competition; Subfamily; Mesozoic; Biology; Zoology","score_opus":0.01701638057274423,"score_gpt":0.19924143535664146,"score_spread":0.18222505478389722,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109185299","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9785377,0.009727012,0.000007206877,0.00091380073,0.00027275048,0.00005119765,0.00011251783,0.0000015420038,0.01037627],"genre_scores_gemma":[0.99837357,0.00022301933,0.0010804944,0.00015926069,0.000118307114,4.6861143e-8,9.352126e-7,5.724793e-7,0.000043769596],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885213,0.00010494361,0.00034233602,0.00012988034,0.00019414055,0.00037654958],"domain_scores_gemma":[0.9987822,0.00023641711,0.00024235072,0.00009316545,0.000036146906,0.0006096962],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00053425547,0.00009756095,0.00023371668,0.00011417081,0.00029826796,0.000067901594,0.0004418656,0.00006856261,0.0014856317],"category_scores_gemma":[0.00007068969,0.000065574255,0.00008690007,0.00030468273,0.0011935943,0.0003034198,6.9841025e-7,0.00018529766,0.0000022117877],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019379999,0.0000017902494,0.90558136,0.0000017816424,0.000018185256,0.00002489957,0.0014256161,0.00008158053,0.000027336759,0.000059984006,0.00018630785,0.09257176],"study_design_scores_gemma":[0.00020051963,0.0002464553,0.99419624,0.000048727838,0.000019112293,0.000062300394,0.0003926317,0.00009053584,0.00009518091,0.0020591435,0.002513953,0.00007520719],"about_ca_topic_score_codex":0.12590909,"about_ca_topic_score_gemma":0.60045236,"teacher_disagreement_score":0.47454327,"about_ca_system_score_codex":8.541238e-7,"about_ca_system_score_gemma":0.0015679573,"threshold_uncertainty_score":0.99942714},"labels":[],"label_agreement":null},{"id":"W2109261219","doi":"10.1139/e09-075","title":"A revised late-Quaternary vegetation history of the unglaciated southwestern Yukon Territory, Canada, from Antifreeze and Eikland ponds","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Macrofossil; Glacial period; Geology; Vegetation (pathology); Holocene; Stadial; Physical geography; Radiocarbon dating; Paleontology; Geography","score_opus":0.015008751871006936,"score_gpt":0.19606194875769098,"score_spread":0.18105319688668403,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109261219","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99396837,0.0019371532,6.406411e-7,0.00075314124,0.0017865931,0.000051716077,0.000027672033,0.0000013170647,0.0014733857],"genre_scores_gemma":[0.99942654,0.0000145648755,0.000058746595,0.00017142067,0.00006689884,8.291945e-8,0.0000039311294,0.0000012534819,0.00025657107],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989534,0.00014125688,0.0002553314,0.00013181762,0.0002493152,0.0002688969],"domain_scores_gemma":[0.9990828,0.00017100893,0.00022916822,0.00011111363,0.0000882082,0.00031772585],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006474064,0.00008202307,0.00017219677,0.00015300083,0.00021115212,0.00003010279,0.00041866192,0.00008004578,0.00039318437],"category_scores_gemma":[0.00013503262,0.000053616885,0.000036320573,0.00013461054,0.0010217724,0.00017885298,0.0000062157037,0.00033044253,0.0000042848837],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008463709,0.0000013013223,0.9990727,0.000006423999,0.000009780659,0.000049292827,0.0003387649,0.00008271705,0.00018230763,0.00000746219,0.00008378835,0.00015705358],"study_design_scores_gemma":[0.00017837377,0.000073666255,0.9965709,0.00004104361,0.000011946065,0.00008781003,0.000069186746,0.00096246734,0.00007001303,0.00018866568,0.0016828866,0.00006306425],"about_ca_topic_score_codex":0.7169028,"about_ca_topic_score_gemma":0.9990189,"teacher_disagreement_score":0.28211612,"about_ca_system_score_codex":0.0000015951927,"about_ca_system_score_gemma":0.0043506157,"threshold_uncertainty_score":0.7717805},"labels":[],"label_agreement":null},{"id":"W2109472225","doi":"10.1139/cjes-2012-0100","title":"A new species of osteostracan from the Lochkovian (Early Devonian) of the Mackenzie Mountains, with comments on body size, growth, and geographic distribution in the genus <i>Machairaspis</i>","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"University of Alberta","keywords":"Devonian; Genus; Paleontology; Fauna; Laurentia; Subfamily; Range (aeronautics); Terrane; Geology; Biology; Zoology; Ecology; Paleozoic","score_opus":0.009002341658044158,"score_gpt":0.17829676584602983,"score_spread":0.16929442418798568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109472225","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9919209,0.001247137,0.0000069704397,0.0056689195,0.00014932365,0.00014004753,0.00020800738,7.603319e-7,0.0006579524],"genre_scores_gemma":[0.99927497,0.000055439832,0.00005324151,0.0005450764,0.000049639868,3.394247e-7,0.000008448684,7.4230604e-7,0.000012079727],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99891406,0.00022646684,0.00024993345,0.000112981535,0.00023263726,0.00026389357],"domain_scores_gemma":[0.99898857,0.00045633892,0.00024016669,0.000105140425,0.000058051286,0.00015174592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048595114,0.00009251639,0.00014941093,0.000065986176,0.00034614268,0.000046685975,0.0005884035,0.00005243975,0.00023244106],"category_scores_gemma":[0.00010235729,0.000040592746,0.00004362739,0.00041342984,0.0014993566,0.00020224914,0.000005406342,0.00021887923,0.0000025752686],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018663108,0.000004094968,0.9982786,0.0000016285354,0.000011921581,0.0000061359037,0.00034388236,0.00005588153,0.0000135630025,0.00021804724,0.00016695188,0.00088060857],"study_design_scores_gemma":[0.00020147761,0.00052267336,0.9965301,0.000044257806,0.000011201442,0.000053280222,0.00090481556,0.000045880268,0.000035994162,0.0010311662,0.0005678341,0.000051333],"about_ca_topic_score_codex":0.2287508,"about_ca_topic_score_gemma":0.7274764,"teacher_disagreement_score":0.49872565,"about_ca_system_score_codex":0.0000017741844,"about_ca_system_score_gemma":0.0005060388,"threshold_uncertainty_score":0.776385},"labels":[],"label_agreement":null},{"id":"W2109717386","doi":"10.1139/e04-050","title":"<sup>40</sup>Ar/<sup>39</sup>Ar dating in the LochaberMulgrave area, northern mainland Nova Scotia: implications for timing of regional metamorphism and sediment provenance in the Late Devonian Early Carboniferous Horton Group","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Mount Saint Vincent University; Acadia University; Dalhousie University","funders":"","keywords":"Geology; Metamorphism; Provenance; Muscovite; Terrane; Geochemistry; Late Devonian extinction; Devonian; Zircon; Paleontology; Carboniferous; Quartz; Tectonics","score_opus":0.03014294618620149,"score_gpt":0.21494114621537075,"score_spread":0.18479820002916925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109717386","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905993,0.0010151899,0.0000634918,0.0076429984,0.000022507917,0.000256162,0.000052972577,0.0000016467072,0.0003457625],"genre_scores_gemma":[0.9982622,0.000024152545,0.0010561085,0.0005716084,0.00005982449,0.0000022864808,0.00001259053,0.0000020290574,0.000009175602],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983306,0.00010265875,0.0004884803,0.00025223277,0.00033262218,0.0004934313],"domain_scores_gemma":[0.9989236,0.0003336205,0.00026187787,0.00015187818,0.000100023135,0.0002290166],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016289641,0.00015621824,0.00028189266,0.0002366996,0.00031233116,0.0001306637,0.00063740596,0.00006182328,0.000088844616],"category_scores_gemma":[0.00014837756,0.00008530842,0.000102711594,0.0008328582,0.00058197003,0.00022613676,0.000010050147,0.000271011,0.0000025279755],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011922599,0.000015679798,0.9389477,0.000008527921,0.000017423725,0.00002370165,0.0021888618,0.057112858,0.00003263262,0.00028896626,0.000007846917,0.0013439127],"study_design_scores_gemma":[0.00036683318,0.00035509508,0.9760234,0.000086718144,0.00003698959,0.00012580885,0.0018555912,0.0060546556,0.00001968645,0.014781314,0.00015390206,0.0001400275],"about_ca_topic_score_codex":0.09896221,"about_ca_topic_score_gemma":0.63803446,"teacher_disagreement_score":0.5390723,"about_ca_system_score_codex":0.0000070838837,"about_ca_system_score_gemma":0.0003751509,"threshold_uncertainty_score":0.90703785},"labels":[],"label_agreement":null},{"id":"W2109782966","doi":"10.1139/e00-080","title":"Geochemistry and Nd isotopes of the François Lake plutonic suite, Endako batholith: host and progenitor to the Endako molybdenum camp, central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Batholith; Geochemistry; Pluton; Mafic; Diorite; Felsic; Zircon; Paleontology; Tectonics","score_opus":0.0075025709496132804,"score_gpt":0.17029267080010058,"score_spread":0.16279009985048729,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109782966","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99280703,0.0039868853,0.0000013738987,0.0021728587,0.00015138045,0.000100092104,0.0001926755,0.0000020684618,0.00058563484],"genre_scores_gemma":[0.9986284,0.00013803209,0.000121691184,0.00038178437,0.00012304423,4.2396908e-7,0.0000022211273,0.0000011945326,0.00060323114],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986885,0.00005953601,0.00027621016,0.00020081791,0.00030878448,0.00046611213],"domain_scores_gemma":[0.99888366,0.00010923007,0.00014209525,0.0001051826,0.00010303047,0.0006567897],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047747753,0.00009173152,0.00020445335,0.000042957854,0.0005512849,0.0003684367,0.0004880681,0.000053490247,0.0035834494],"category_scores_gemma":[0.0003006005,0.000062368345,0.000087577864,0.00054098497,0.00097010034,0.00014687331,0.000021290043,0.00019185102,0.0000037777004],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000029001192,0.000003215392,0.9949568,0.000005221621,0.000011766138,0.000037206926,0.00019648457,0.00007800752,0.00015911851,0.0000012849948,0.00041707128,0.004130903],"study_design_scores_gemma":[0.00009807737,0.00009861133,0.98042107,0.000038021368,0.00002430213,0.00055652205,0.00032398422,0.00010909575,0.00030888684,0.00035222602,0.017574273,0.000094953946],"about_ca_topic_score_codex":0.15864249,"about_ca_topic_score_gemma":0.96921813,"teacher_disagreement_score":0.81057566,"about_ca_system_score_codex":0.0000013846384,"about_ca_system_score_gemma":0.0003889521,"threshold_uncertainty_score":0.9973274},"labels":[],"label_agreement":null},{"id":"W2109786456","doi":"10.1139/e10-108","title":"Where is the Iapetus suture in northern New England? A study of the Ammonoosuc Volcanics, Bronson Hill terrane, New Hampshire<sup>1</sup>This article is one of a series of papers published in this <i>CJES Special Issue: In honour of Ward Neale</i> on the theme of Appalachian and Grenvillian geology.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Division of Mathematical Sciences; National Science Foundation","keywords":"Geology; Terrane; Volcanic rock; Orogeny; Fibrous joint; Paleontology; Metamorphism; Geochemistry; Subduction; Ordovician; Laurentia; Provenance; Igneous rock; Island arc; Ophiolite; Volcano; Tectonics","score_opus":0.013490794761973717,"score_gpt":0.1786649736568214,"score_spread":0.1651741788948477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109786456","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98428243,0.0017424091,1.2075374e-7,0.012518046,0.000080040096,0.00019869184,0.000036241137,7.6373385e-7,0.0011412522],"genre_scores_gemma":[0.99923277,0.0001447951,0.00004860677,0.0002756391,0.00014474966,3.7220607e-7,8.497211e-7,0.0000020015298,0.00015019468],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978128,0.00037965653,0.00076585123,0.00019132187,0.00044445597,0.0004059363],"domain_scores_gemma":[0.9985253,0.00032673602,0.0005534248,0.0002259503,0.00008853382,0.00028005237],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015997522,0.00015889977,0.0005285348,0.00021970789,0.00010762324,0.000028719205,0.0007559536,0.0000897697,0.0066157635],"category_scores_gemma":[0.00041805473,0.0000764391,0.00012717505,0.001162255,0.0009500777,0.00028863284,0.000028788825,0.00038411244,0.000001635131],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008690799,0.000067838155,0.9717738,0.000016503807,0.00002950701,0.000003105417,0.02246031,0.0009377535,0.00008825416,0.000018700806,0.00035563917,0.004161692],"study_design_scores_gemma":[0.00064045703,0.00062287867,0.9821605,0.00012488637,0.00003333693,0.000013380428,0.012489244,0.00028869015,0.000767221,0.0007657657,0.001996402,0.00009719895],"about_ca_topic_score_codex":0.24124348,"about_ca_topic_score_gemma":0.92887825,"teacher_disagreement_score":0.68763477,"about_ca_system_score_codex":0.0000044774915,"about_ca_system_score_gemma":0.00042414747,"threshold_uncertainty_score":0.9942923},"labels":[],"label_agreement":null},{"id":"W2110252548","doi":"10.1139/e08-069","title":"Regional characterization of the Paskapoo bedrock aquifer system, southern AlbertaGeological Survey of Canada Contribution 2008-0479.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Aquifer; Groundwater recharge; Foreland basin; Geochemistry; Bedrock; Siltstone; Fluvial; Groundwater; Geomorphology; Population; Groundwater flow; Facies; Geotechnical engineering; Structural basin","score_opus":0.02063112527305647,"score_gpt":0.1859688359240503,"score_spread":0.16533771065099384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110252548","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99846447,0.00014878389,0.0005187427,0.0002913071,0.00026159786,0.000057051395,0.000055051474,0.0000024781048,0.000200549],"genre_scores_gemma":[0.99976796,0.000016152793,0.000010217275,0.000036566264,0.00003472731,6.2055693e-7,0.0000072796415,0.0000031798013,0.00012327176],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989101,0.0001100976,0.0003934108,0.000064707776,0.00033396494,0.00018771764],"domain_scores_gemma":[0.9991287,0.00004924679,0.00021844167,0.00008507851,0.00030810933,0.00021045038],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048084132,0.00007142694,0.00020742767,0.00013070581,0.00018394961,0.00001165031,0.00026273975,0.000045738157,0.000061611594],"category_scores_gemma":[0.00015131258,0.0000460717,0.000066398774,0.0005685349,0.00023682108,0.00010905768,0.000005004892,0.00009363871,0.0000011033742],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000124849,0.000010789209,0.8013311,0.000031679538,0.000110538094,0.00003280185,0.000940381,0.19180016,0.004684719,0.00017862284,0.0008070949,0.000059642098],"study_design_scores_gemma":[0.0002101138,0.000046546742,0.956265,0.00008088311,0.000019131494,0.00009241431,0.0003397755,0.03897602,0.0024047946,0.0000069804414,0.0014424975,0.00011585903],"about_ca_topic_score_codex":0.3024077,"about_ca_topic_score_gemma":0.95374304,"teacher_disagreement_score":0.6513353,"about_ca_system_score_codex":0.000024537394,"about_ca_system_score_gemma":0.0018627632,"threshold_uncertainty_score":0.7022376},"labels":[],"label_agreement":null},{"id":"W2110265041","doi":"10.1139/e07-038","title":"Geophysical modeling of Devonian plutons in the southern Gulf of St. Lawrence: implications for Appalachian terrane boundaries in Maritime Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Acadia University","funders":"Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; Acadia University","keywords":"Terrane; Geology; Pluton; Basement; Devonian; Paleozoic; Magnetic anomaly; Seismology; Sedimentary rock; Paleontology; Fault (geology); Geophysics; Tectonics; Archaeology","score_opus":0.019515603942602072,"score_gpt":0.21391356420296964,"score_spread":0.19439796026036757,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110265041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99554116,0.00029654865,0.00024640202,0.0025971108,0.000051028946,0.00007446617,0.00021069114,5.928072e-7,0.0009820277],"genre_scores_gemma":[0.99900734,0.0000028544137,0.0007726546,0.00016223181,0.00003361631,3.3038057e-7,0.000008330603,7.354386e-7,0.000011895167],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987929,0.000039994407,0.0004612333,0.00011920235,0.00022507239,0.00036163966],"domain_scores_gemma":[0.9991889,0.0002583974,0.00015643018,0.00008249826,0.00010562956,0.000208168],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011489143,0.000076198405,0.00022154847,0.00019597763,0.00021029435,0.00004671222,0.00050525303,0.000035537098,0.00027909793],"category_scores_gemma":[0.00017769866,0.000047475212,0.00007302188,0.00070135045,0.0006482624,0.00009730276,0.000003991878,0.0001443615,5.909153e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000109989205,0.000009776905,0.97913927,0.0000072956227,0.000006213285,0.000006734305,0.0006185581,0.01796957,0.000028629482,0.0004816229,0.000017060034,0.0017042732],"study_design_scores_gemma":[0.00016395487,0.0001414936,0.963486,0.000034184646,0.000012328098,0.000016458589,0.0028058023,0.013190553,0.000037830523,0.019365948,0.00065269443,0.00009272851],"about_ca_topic_score_codex":0.90471905,"about_ca_topic_score_gemma":0.99945086,"teacher_disagreement_score":0.09473185,"about_ca_system_score_codex":0.0000034603818,"about_ca_system_score_gemma":0.0019867285,"threshold_uncertainty_score":0.35243714},"labels":[],"label_agreement":null},{"id":"W2110407283","doi":"10.1139/e01-051","title":"A new ankylosaurid (Dinosauria: Ankylosauria) from the Lower Cretaceous of China, with comments on ankylosaurian relationships","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Universiteit Leiden","keywords":"Postcrania; Paleontology; Geology; Cretaceous; Sister group; Taxon; China; Phylogenetic tree; Geography; Biology; Archaeology; Clade","score_opus":0.028121859878815034,"score_gpt":0.21507650926173535,"score_spread":0.18695464938292033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110407283","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9771218,0.0033957327,0.00010154941,0.008872951,0.0008592614,0.00012505222,0.00018624245,0.000005623181,0.009331809],"genre_scores_gemma":[0.99755424,0.00007341313,0.0011782795,0.0006561025,0.00036203003,2.190674e-7,0.00002333416,0.0000024993403,0.00014990839],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99809563,0.00037005602,0.00043626878,0.00024293084,0.00036044102,0.0004946708],"domain_scores_gemma":[0.9980838,0.00062487205,0.0003789654,0.00023277465,0.00009257586,0.0005870703],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010201811,0.00017579018,0.00029373777,0.00024044204,0.00080441695,0.00006238024,0.00076100125,0.00012597232,0.0028984454],"category_scores_gemma":[0.00026004648,0.000103767765,0.000094564006,0.0006158993,0.0009779617,0.00037806178,0.0000052936934,0.00047031956,0.000051359842],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016631337,0.000013322484,0.99287707,0.0000011182321,0.000045025587,0.00016538503,0.00038961344,0.0019558512,0.0000049182386,0.00031491168,0.0017538144,0.0023126532],"study_design_scores_gemma":[0.00044420455,0.0013099927,0.97223973,0.0000682477,0.000032887805,0.00038392012,0.0002987333,0.00025291173,0.00001092383,0.002542491,0.022282908,0.00013305996],"about_ca_topic_score_codex":0.030793265,"about_ca_topic_score_gemma":0.6394106,"teacher_disagreement_score":0.60861737,"about_ca_system_score_codex":0.000003982094,"about_ca_system_score_gemma":0.0015026404,"threshold_uncertainty_score":0.998013},"labels":[],"label_agreement":null},{"id":"W2110548795","doi":"10.1139/e06-018","title":"Geology, geochronology, and geochemistry of basaltic flows of the Cat Hills, Cat Mesa, Wind Mesa, Cerro Verde, and Mesita Negra, central New Mexico","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Geology; Basalt; Geochemistry; Mantle (geology); Geochronology; Volcano; Trace element; Radiogenic nuclide; Magma chamber; Partial melting; Cape verde; Magma","score_opus":0.007998830023493903,"score_gpt":0.17371709370700264,"score_spread":0.16571826368350873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110548795","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99020934,0.004994104,0.000004281211,0.002992672,0.00015216104,0.00006540198,0.0000506091,0.000001931599,0.001529523],"genre_scores_gemma":[0.99875486,0.00008966202,0.00074599974,0.0001387997,0.00008721416,7.292914e-8,0.0000070871947,0.0000013799837,0.00017495027],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99844426,0.00006946041,0.0004611361,0.00024388343,0.00026675942,0.0005144994],"domain_scores_gemma":[0.99870896,0.0001460433,0.00034046735,0.00014358452,0.00010374471,0.000557203],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004009123,0.00016066375,0.00038711703,0.00014302683,0.00024639015,0.000040459217,0.00049849716,0.00011801469,0.0018929907],"category_scores_gemma":[0.00013801498,0.000096854084,0.00012099476,0.0004347478,0.001831259,0.00016540915,0.000025938461,0.00015709414,0.0000024710453],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001233527,0.000007341059,0.99573004,0.00001437631,0.00002536632,0.000014027983,0.00008601048,0.0020492084,0.000821586,0.000059939248,0.00041153928,0.0007682302],"study_design_scores_gemma":[0.00032437837,0.00016336393,0.9864391,0.000033104512,0.000069793656,0.00016820733,0.00021818632,0.0019855993,0.0039628455,0.0057191732,0.0007877924,0.00012844823],"about_ca_topic_score_codex":0.21814363,"about_ca_topic_score_gemma":0.5879912,"teacher_disagreement_score":0.36984757,"about_ca_system_score_codex":0.0000031953093,"about_ca_system_score_gemma":0.00097206247,"threshold_uncertainty_score":0.99901944},"labels":[],"label_agreement":null},{"id":"W2110739540","doi":"10.1139/e05-063","title":"A multi-proxy lithostratigraphic record of Late Glacial and Holocene climate variability from Piper Lake, Nova Scotia","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Preboreal; Holocene; Geology; Younger Dryas; Glacial period; Glacial lake; Greenland ice sheet; Varve; Physical geography; Paleontology; Glacier; Sediment; Geography","score_opus":0.029339817567612773,"score_gpt":0.25072136185044286,"score_spread":0.22138154428283008,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110739540","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99575895,0.0010800229,0.000018488267,0.0008888365,0.00038094315,0.00008436316,0.00012298909,0.000003185006,0.0016622208],"genre_scores_gemma":[0.9907868,0.000102075595,0.008844946,0.0001472368,0.000091023125,8.142422e-8,0.0000055441315,0.0000013787363,0.000020921829],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99833834,0.00025300126,0.0004331133,0.00024042773,0.00020726406,0.00052786246],"domain_scores_gemma":[0.99867266,0.00029219993,0.00021959218,0.00012117412,0.00014020962,0.00055417477],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0021433705,0.00012049423,0.00029580432,0.00032418207,0.00029401112,0.000069323156,0.00037590467,0.00012692114,0.0030708208],"category_scores_gemma":[0.0002725407,0.00009266862,0.000066138775,0.0004313988,0.0017089199,0.00042270057,0.000007923276,0.0003214306,0.000044762484],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002789228,0.000008553667,0.9977635,0.000008086397,0.000013794523,0.000036001635,0.00020108826,0.00017253293,0.000014243528,0.00001766028,0.000010089982,0.001726525],"study_design_scores_gemma":[0.0003285355,0.00025961586,0.9962126,0.000035348683,0.000014526136,0.00009304817,0.00006750619,0.002209037,0.000061606406,0.00028850808,0.0003310594,0.00009861956],"about_ca_topic_score_codex":0.015404641,"about_ca_topic_score_gemma":0.9230635,"teacher_disagreement_score":0.9076589,"about_ca_system_score_codex":3.3370915e-7,"about_ca_system_score_gemma":0.0008614985,"threshold_uncertainty_score":0.9978405},"labels":[],"label_agreement":null},{"id":"W2110740618","doi":"10.1139/e01-018","title":"Paleomagnetic reconnaissance of early Mesozoic carbonates from Williston Lake, northeastern British Columbia, Canada: evidence for late Mesozoic remagnetization","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Canadian Society of Petroleum Geologists","keywords":"Geology; Mesozoic; Paleontology; Paleomagnetism; Cretaceous; Cenozoic; Trias; Magnetostratigraphy; Polarity (international relations); Red beds; Phanerozoic; Structural basin","score_opus":0.023117360354466217,"score_gpt":0.22649897881680664,"score_spread":0.20338161846234043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110740618","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96821153,0.029666783,0.000044961853,0.0003140459,0.0005671814,0.00020941925,0.00018935549,0.0000021893093,0.0007945467],"genre_scores_gemma":[0.9954436,0.0012123616,0.000568661,0.00014695944,0.00022751612,0.0000068248182,0.000017269644,0.000012463755,0.0023643686],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983083,0.00007774632,0.0005274674,0.0003345833,0.00029700113,0.00045490466],"domain_scores_gemma":[0.9985321,0.000096500444,0.00040107252,0.00019154533,0.0004143582,0.00036440935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041420848,0.00014538494,0.00030673007,0.00006740301,0.00048399184,0.00026860068,0.00047776452,0.00009081783,0.00015118536],"category_scores_gemma":[0.00043058136,0.00018525627,0.000103321574,0.00028849862,0.00053341634,0.000039036837,0.00002291626,0.000089743975,7.161467e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028267481,0.00000800784,0.9904341,0.000023843331,0.000029450777,0.0000585669,0.00010253787,0.00023230075,0.0027164046,0.000002065978,0.0013618212,0.0050026085],"study_design_scores_gemma":[0.0004827266,0.00168763,0.97543293,0.00030374626,0.00005206454,0.0001022922,0.00010554647,0.00006856142,0.0003678145,0.00021201209,0.02093017,0.00025453325],"about_ca_topic_score_codex":0.88234967,"about_ca_topic_score_gemma":0.9998216,"teacher_disagreement_score":0.11747195,"about_ca_system_score_codex":0.000006298052,"about_ca_system_score_gemma":0.0020487679,"threshold_uncertainty_score":0.75545317},"labels":[],"label_agreement":null},{"id":"W2111008068","doi":"10.1139/e10-001","title":"Insights into the metamorphic evolution of the Belt–Purcell basin; evidence from Lu–Hf garnet geochronology","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Washington State University; National Science Foundation","keywords":"Schist; Geology; Metamorphic rock; Geochronology; Kyanite; Geochemistry; Proterozoic; Butte; Metamorphic core complex; Staurolite; Basement; Metamorphism; Paleontology; Archaeology; Tectonics","score_opus":0.01559247428990062,"score_gpt":0.18652980416315626,"score_spread":0.17093732987325563,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111008068","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98749787,0.005228244,0.000023346678,0.0055152946,0.000655532,0.000053069605,0.000008644846,0.000002141394,0.0010158318],"genre_scores_gemma":[0.99893457,0.000046930872,0.00047641856,0.00029863146,0.00016931257,1.792447e-7,0.000001531202,8.279829e-7,0.00007161908],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985589,0.00019421078,0.0003626427,0.00019673395,0.0003809308,0.00030657343],"domain_scores_gemma":[0.998456,0.00048152235,0.000327467,0.00022047223,0.00017280238,0.00034176372],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00074958557,0.000111616144,0.00022756206,0.00014375568,0.00055894273,0.00007491404,0.0012600323,0.00008378447,0.0051422203],"category_scores_gemma":[0.00080346636,0.000049272887,0.00017057803,0.0008245351,0.0020971736,0.00028918637,0.000020190535,0.00045209433,0.00004006654],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000056242484,0.0000042907022,0.9917676,0.0000020866971,0.000021816093,0.000008455597,0.0004578173,0.0017246339,0.0032109835,0.00032096356,0.00009989362,0.0023758556],"study_design_scores_gemma":[0.000058161433,0.0001274128,0.96305186,0.000026896834,0.000049632286,0.000021975142,0.00037073594,0.0020975778,0.0019443297,0.029096378,0.0030738642,0.00008116566],"about_ca_topic_score_codex":0.27240694,"about_ca_topic_score_gemma":0.90816057,"teacher_disagreement_score":0.63575363,"about_ca_system_score_codex":0.0000022899521,"about_ca_system_score_gemma":0.0008995257,"threshold_uncertainty_score":0.99576724},"labels":[],"label_agreement":null},{"id":"W2111461451","doi":"10.1139/e2012-045","title":"Upper-crustal, basement-involved folding in the East Range of the Sudbury Basin, Ontario, inferred from paleomagnetic data and spatial analysis of mafic dykes","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Anticline; Basement; Mafic; Fold (higher-order function); Paleomagnetism; Archean; Seismology; Pluton; Geochemistry; Proterozoic; Sedimentary rock; Petrology; Geomorphology; Paleontology; Structural basin; Tectonics","score_opus":0.037544513895719014,"score_gpt":0.21126921780909258,"score_spread":0.17372470391337358,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111461451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965117,0.0018623719,0.000014393785,0.0005629628,0.00009080117,0.000053314103,0.00015858446,5.92675e-7,0.0007452852],"genre_scores_gemma":[0.99955094,0.000018210934,0.00020581149,0.00014764257,0.000035742425,1.0426472e-7,0.000019076631,6.163311e-7,0.000021875621],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985975,0.0001542068,0.00040478454,0.00015151662,0.00038533943,0.00030666596],"domain_scores_gemma":[0.9989196,0.0002654906,0.00027381297,0.00023020437,0.000056177898,0.00025469935],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013242243,0.00009701791,0.0003040346,0.00028562444,0.00016351372,0.000058676094,0.0008770042,0.00003861072,0.0059734974],"category_scores_gemma":[0.00020412463,0.000048678205,0.000120797384,0.0009904683,0.0006728125,0.00028885796,0.000026454867,0.00015298321,0.0000014442626],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006258635,0.000008676472,0.99665326,0.0000024232438,0.00005810932,0.0000032100004,0.00070179463,0.00038681313,0.000023001801,0.000011642569,0.00001563628,0.0021291857],"study_design_scores_gemma":[0.00011206668,0.00007638508,0.99235123,0.00002357011,0.0002896542,0.0000027624314,0.0012840265,0.0050669014,0.000024228615,0.00042037852,0.00028410472,0.00006471368],"about_ca_topic_score_codex":0.673838,"about_ca_topic_score_gemma":0.9887823,"teacher_disagreement_score":0.31494427,"about_ca_system_score_codex":0.0000022135068,"about_ca_system_score_gemma":0.0003686591,"threshold_uncertainty_score":0.99493515},"labels":[],"label_agreement":null},{"id":"W2111548193","doi":"10.1139/cjes-2012-0054","title":"Hierarchical clustering of pit crater chains on Venus","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Frontier Geosciences (Canada); Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Impact crater; Geology; Graben; Volcano; Pyroclastic rock; Tectonics; Paleontology; Astrobiology","score_opus":0.022819813357794344,"score_gpt":0.21666465067573293,"score_spread":0.19384483731793858,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111548193","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99540126,0.000017962677,0.00039496284,0.00084320956,0.00024350994,0.00003239655,0.000006669064,6.324372e-7,0.003059392],"genre_scores_gemma":[0.9993509,5.982204e-7,0.00030825206,0.000096984884,0.00013999817,3.6410415e-7,0.0000017142596,0.0000011248561,0.000100031466],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994705,0.000017214588,0.00014353471,0.00006134638,0.00013413513,0.00017330867],"domain_scores_gemma":[0.99957234,0.000019549965,0.00009069732,0.000045536504,0.000046989997,0.0002248863],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019789189,0.0000422089,0.00007891348,0.00014606888,0.0001272133,0.00007272196,0.00018723137,0.000009960129,0.0003871839],"category_scores_gemma":[0.000007974719,0.000031188036,0.00003103334,0.00014772423,0.0001739825,0.00039339004,0.000003701871,0.00007869428,0.0000740843],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001200618,0.00004357266,0.90255094,0.000010296029,0.000036639845,0.000034360346,0.0041457,0.037694447,0.00601185,0.0084687155,0.0026885262,0.03830296],"study_design_scores_gemma":[0.00053592265,0.0017227468,0.9364813,0.0002432552,0.000014759535,0.000034838744,0.0023237364,0.030517926,0.004008148,0.011996377,0.0117460145,0.00037500449],"about_ca_topic_score_codex":0.0026204754,"about_ca_topic_score_gemma":0.0038912557,"teacher_disagreement_score":0.03792796,"about_ca_system_score_codex":0.0000015099306,"about_ca_system_score_gemma":0.00037772316,"threshold_uncertainty_score":0.42393923},"labels":[],"label_agreement":null},{"id":"W2111672313","doi":"10.1139/e06-066","title":"2480 Ma mafic magmatism in the northern Black Hills, South Dakota: a new link connecting the Wyoming and Superior cratons","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Craton; Mafic; Geochemistry; Precambrian; Sill; Magmatism; Zircon; Rift; Paleontology; Tectonics","score_opus":0.014974310779778123,"score_gpt":0.18239945132348484,"score_spread":0.16742514054370672,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111672313","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98480946,0.0019577642,0.000011124371,0.010905837,0.00008149439,0.000057337445,0.000017546816,0.0000022491524,0.0021571994],"genre_scores_gemma":[0.99883026,0.000014058983,0.0002844946,0.00056320586,0.00021696654,9.952686e-8,0.000002952862,0.0000010553327,0.00008689461],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987879,0.0001071335,0.00030571665,0.00015891757,0.000247808,0.00039255715],"domain_scores_gemma":[0.99917144,0.00029326443,0.00013798391,0.00008720068,0.000043155705,0.00026697514],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010057628,0.00010604034,0.00017189207,0.00013397489,0.0005444703,0.0003508853,0.00049405353,0.000041027415,0.001332381],"category_scores_gemma":[0.00019016255,0.00004978669,0.00007416947,0.00062091544,0.0005801761,0.00018808633,0.0000072427865,0.0002589332,0.00003155372],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021850678,0.0000017665545,0.9856359,0.0000020904567,0.0000050651483,0.00006196648,0.0011651183,0.0028889074,0.000018165883,0.00006433422,0.000066804125,0.010087695],"study_design_scores_gemma":[0.00013773634,0.000090696594,0.9816327,0.00002749621,0.000020178779,0.0001643424,0.0036214513,0.0023208593,0.00002244609,0.0076696556,0.004184511,0.000107938366],"about_ca_topic_score_codex":0.14189921,"about_ca_topic_score_gemma":0.92277247,"teacher_disagreement_score":0.7808733,"about_ca_system_score_codex":0.0000013267764,"about_ca_system_score_gemma":0.00032449735,"threshold_uncertainty_score":0.99958056},"labels":[],"label_agreement":null},{"id":"W2111685163","doi":"10.1139/e10-083","title":"An istiodactylid pterosaur from the Upper Cretaceous Nanaimo Group, Hornby Island, British Columbia, Canada","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta","keywords":"Rostrum; Cretaceous; Paleontology; Geology; Genus; Group (periodic table); Biology; Zoology","score_opus":0.007705539979860705,"score_gpt":0.1812532573092633,"score_spread":0.1735477173294026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111685163","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9898659,0.002198571,0.000010094579,0.0013891886,0.002784669,0.000059080023,0.00063998083,0.0000037310917,0.0030488002],"genre_scores_gemma":[0.99732137,0.00003336114,0.0003983933,0.0015571788,0.0004750888,2.2683507e-7,0.00003189218,0.0000016832086,0.00018078939],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985572,0.00015640135,0.00028579496,0.00022551639,0.00025292623,0.00052212947],"domain_scores_gemma":[0.99863,0.0002488022,0.00017271489,0.00016013297,0.00009434346,0.00069400045],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00070698577,0.00009465557,0.00019052648,0.00004793328,0.0013211421,0.0004074364,0.0008944876,0.000111712034,0.008686243],"category_scores_gemma":[0.00017907219,0.00008554433,0.00005723274,0.00021817209,0.0011675556,0.00041341857,0.0000035970488,0.00045860303,0.000022877733],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004302289,0.0000025031263,0.98848903,5.0569975e-7,0.000011287957,0.00019392514,0.000060222763,0.000063559404,0.000021364056,0.000009645196,0.006890087,0.0042535374],"study_design_scores_gemma":[0.00012459485,0.00018189628,0.91680294,0.000009467516,0.000010529828,0.0008045394,0.00024327314,0.00030881236,0.0000015498698,0.00048804752,0.08090659,0.0001177474],"about_ca_topic_score_codex":0.99648845,"about_ca_topic_score_gemma":0.9999992,"teacher_disagreement_score":0.074016504,"about_ca_system_score_codex":0.0000028778607,"about_ca_system_score_gemma":0.0034574682,"threshold_uncertainty_score":0.999979},"labels":[],"label_agreement":null},{"id":"W2112294167","doi":"10.1139/e11-014","title":"Upper-crustal orogenic lid and mid-crustal core complexes: signature of a collapsed orogenic plateau in the hinterland of the Grenville Province <sup>1</sup>This article is one of a series of papers published in <i>CJES Special Issue: In honour of Ward Neale</i> on the theme of Appalachian and Grenvillian geology.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":136,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Crust; Metamorphism; Granulite; Geochemistry; Terrane; Tectonics; Metamorphic facies; Shear zone; Petrology; Metamorphic core complex; Continental crust; Seismology; Paleontology; Facies; Extensional definition","score_opus":0.0134929751897213,"score_gpt":0.18429442432565915,"score_spread":0.17080144913593784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112294167","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953356,0.0015181674,8.369561e-8,0.002105517,0.000041017687,0.00019489757,0.00014056446,4.5937088e-7,0.00066371064],"genre_scores_gemma":[0.99964535,0.00008838836,0.000080025115,0.00012277125,0.00003965078,4.7669033e-7,0.0000021735352,0.0000015644044,0.000019596115],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99816805,0.00023106272,0.0007079903,0.00016237593,0.00038455895,0.0003459759],"domain_scores_gemma":[0.9986972,0.00035036853,0.0005499071,0.00015034791,0.00009422429,0.00015790902],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012927193,0.0001391857,0.00052260363,0.00023347641,0.000087229404,0.000018109353,0.00056526106,0.00009134923,0.0022032782],"category_scores_gemma":[0.0003401268,0.00006854131,0.00012343643,0.00094315154,0.002351061,0.00019751191,0.000030119398,0.00028914268,3.447598e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015337863,0.000058832513,0.9884176,0.000049420014,0.000033193133,0.0000044452695,0.0077992566,0.00080556545,0.0018547334,0.00010577432,0.000042884698,0.00067489175],"study_design_scores_gemma":[0.00064075494,0.00079355296,0.97177225,0.00019352543,0.000039160703,0.000048282673,0.015716545,0.00079188956,0.00865848,0.0009910518,0.00024353435,0.000110988796],"about_ca_topic_score_codex":0.020131834,"about_ca_topic_score_gemma":0.31791374,"teacher_disagreement_score":0.2977819,"about_ca_system_score_codex":0.000003229439,"about_ca_system_score_gemma":0.00034055483,"threshold_uncertainty_score":0.99870884},"labels":[],"label_agreement":null},{"id":"W2112341657","doi":"10.1139/e09-014","title":"Near real-time water vapor distribution surface rendering using Ordinary KrigingThis article is one of a series of papers published in this Special Issue on the theme<i> GEODESY</i>.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"GNSS positioning and interference","field":"Engineering","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Changjiang Scholar Program of Chinese Ministry of Education; Natural Sciences and Engineering Research Council of Canada; Li Ka Shing Foundation","keywords":"Kriging; Variogram; Gaussian; Interpolation (computer graphics); Geodesy; Global Positioning System; Geology; Mathematics; Statistics; Algorithm; Applied mathematics; Computer science","score_opus":0.016927526227203893,"score_gpt":0.20867143968706267,"score_spread":0.19174391345985878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112341657","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98485374,0.000044401277,0.000010729206,0.001079825,0.00017313243,0.000041019008,0.000013448428,0.0000051148677,0.013778612],"genre_scores_gemma":[0.999252,0.00001947076,0.00047297674,0.000040290353,0.000119193035,1.2982073e-7,9.628684e-7,0.0000038200374,0.00009114108],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990776,0.00003555965,0.0003205253,0.000087956134,0.00020681597,0.0002715284],"domain_scores_gemma":[0.9995742,0.000031996973,0.00009034498,0.00009877754,0.00008614801,0.00011854325],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005770641,0.00008391488,0.0001714974,0.00009484529,0.00015148337,0.00011675512,0.00022197372,0.000035780435,0.0018395404],"category_scores_gemma":[0.00006375865,0.000057324203,0.000047508333,0.0003192346,0.00024082177,0.00044258806,0.000005880464,0.00014921905,0.0000042207166],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013514873,0.00009869187,0.0148118995,0.0000734885,0.000097074924,0.00007195489,0.022157613,0.361522,0.58681256,0.0015084285,0.008871851,0.0038393098],"study_design_scores_gemma":[0.00052754115,0.0014840022,0.03633411,0.001345904,0.000044034943,0.0001366549,0.0016755027,0.051921632,0.89586467,0.0013359835,0.008879138,0.00045084435],"about_ca_topic_score_codex":0.002424356,"about_ca_topic_score_gemma":0.001285167,"teacher_disagreement_score":0.30960035,"about_ca_system_score_codex":0.000027229167,"about_ca_system_score_gemma":0.00019614535,"threshold_uncertainty_score":0.9990729},"labels":[],"label_agreement":null},{"id":"W2112369736","doi":"10.1139/cjes-2015-0110","title":"Dynamic cause of marginal lithospheric thinning and implications for craton destruction: a comparison of the North China, Superior, and Yilgarn cratons","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Craton; Geology; Lithosphere; Subduction; Yilgarn Craton; Mantle (geology); Tectonics; Earth science; Geochemistry; Paleontology; Seismology","score_opus":0.028487502626142264,"score_gpt":0.24109212118033538,"score_spread":0.2126046185541931,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112369736","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957706,0.0023169755,0.000074791096,0.0015114532,0.00007326117,0.00005579602,0.00004262683,0.0000010830092,0.0001534139],"genre_scores_gemma":[0.9971235,0.000021005482,0.002790106,0.000034038123,0.000013152615,2.2989767e-7,0.0000018333396,6.562191e-7,0.000015472819],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992995,0.000033724296,0.00026138072,0.00010576548,0.00012505693,0.00017455271],"domain_scores_gemma":[0.99917394,0.000072755036,0.00020673493,0.00006503195,0.00014269506,0.00033886937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003208999,0.000065722474,0.00019218914,0.00006512875,0.00025727207,0.000044405035,0.00020390852,0.000027622731,0.00008276125],"category_scores_gemma":[0.00016142201,0.000038340157,0.000049581646,0.00045440873,0.0007812746,0.00015023703,0.0000074430814,0.0000901198,2.5304053e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000050120166,0.0000028629356,0.99584526,0.0000061064075,0.000008960968,4.9622935e-7,0.00030707073,0.0013867317,0.000034273962,0.00007596435,0.000013701574,0.0023135343],"study_design_scores_gemma":[0.000099201236,0.00023669247,0.98979986,0.000015612777,0.00003325643,0.000058599504,0.00049724785,0.0052520507,0.000052586653,0.0037241261,0.00018146796,0.00004927228],"about_ca_topic_score_codex":0.010896613,"about_ca_topic_score_gemma":0.3947979,"teacher_disagreement_score":0.3839013,"about_ca_system_score_codex":0.0000011746164,"about_ca_system_score_gemma":0.00041278818,"threshold_uncertainty_score":0.9956899},"labels":[],"label_agreement":null},{"id":"W2112474875","doi":"10.1139/e09-011","title":"Paleomagnetism and U–Pb geochronology of the Clarence Head dykes, Arctic Canada: orthogonal emplacement of mafic dykes in a large igneous province","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto","keywords":"Baddeleyite; Geology; Mafic; Geochronology; Geochemistry; Paleomagnetism; Zircon; Igneous rock; Precambrian; Devonian; Apparent polar wander; Magmatism; Paleozoic; Paleontology; Tectonics","score_opus":0.00916397766332664,"score_gpt":0.18339570391348842,"score_spread":0.17423172625016178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112474875","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9925997,0.0039022348,0.000004942239,0.0026329947,0.00009620999,0.000069075446,0.00005446293,7.626171e-7,0.0006396003],"genre_scores_gemma":[0.99930024,0.000050504925,0.00025871725,0.0003281819,0.00001910283,1.08193554e-7,0.0000018834627,4.9534356e-7,0.000040767016],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99857855,0.00009191427,0.00042501913,0.00017028139,0.00032739903,0.00040681372],"domain_scores_gemma":[0.9991346,0.00011268822,0.00026982476,0.000094337986,0.00009490068,0.00029362665],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005224587,0.0001018738,0.00027566365,0.00014954599,0.00015296125,0.000021166094,0.00042596646,0.00004665262,0.0014329358],"category_scores_gemma":[0.00019257526,0.000061210136,0.000058029113,0.0004963728,0.0006050899,0.00009891302,0.000009392756,0.00018460111,8.97509e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009201276,0.000009134047,0.99443907,0.000009860121,0.000005480288,0.000056354846,0.000060597355,0.0012615991,0.00007831357,0.00016664875,0.000021383108,0.0038823497],"study_design_scores_gemma":[0.00016213807,0.00045962632,0.99493384,0.00006513362,0.0000122619595,0.000111146335,0.00017530032,0.00058818486,0.00013723418,0.0028167805,0.00046134405,0.00007700825],"about_ca_topic_score_codex":0.6452927,"about_ca_topic_score_gemma":0.998725,"teacher_disagreement_score":0.35343227,"about_ca_system_score_codex":0.0000045633055,"about_ca_system_score_gemma":0.0024456908,"threshold_uncertainty_score":0.9994799},"labels":[],"label_agreement":null},{"id":"W2112573964","doi":"10.1139/e04-002","title":"Peat-forming history of the ancestral Souris mire (Palaeocene), Ravenscrag Formation, southern Saskatchewan, Canada","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Regina","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mire; Peat; Geology; Paleontology; Ecological succession; Physical geography; Geochemistry; Ecology; Geography; Biology","score_opus":0.021900382154165114,"score_gpt":0.19570470462944137,"score_spread":0.17380432247527625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112573964","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912518,0.00225629,0.000012688602,0.0023557276,0.0009645575,0.00006415582,0.000034105982,0.0000016951983,0.0030589318],"genre_scores_gemma":[0.9985062,0.00000971932,0.00026408123,0.00029982365,0.00006261595,1.2211139e-7,0.0000020107034,0.000001358161,0.0008540916],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985912,0.00009574277,0.00034800524,0.00011079133,0.00037614425,0.00047812387],"domain_scores_gemma":[0.99897736,0.00008251174,0.00030089967,0.00011776451,0.00014918143,0.00037226998],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007711371,0.000098109085,0.00018590127,0.00016116953,0.00042180152,0.00002168991,0.00066327804,0.00006506843,0.00066435983],"category_scores_gemma":[0.00010836687,0.000058565496,0.000080251026,0.0002936711,0.0011350256,0.0002907525,0.0000055217915,0.0002767182,0.000012008216],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000050659964,0.0000015030357,0.9922485,0.000009623343,0.0000073002607,0.000049697006,0.0019490005,0.0050273947,0.000003744357,0.000019472844,0.00032564963,0.0003530837],"study_design_scores_gemma":[0.00033124222,0.0001454586,0.9805753,0.000083629,0.000014206255,0.00077647605,0.0076078954,0.00019959228,0.00017692284,0.0009101497,0.009044987,0.00013409882],"about_ca_topic_score_codex":0.7466916,"about_ca_topic_score_gemma":0.999578,"teacher_disagreement_score":0.2528864,"about_ca_system_score_codex":0.00000888728,"about_ca_system_score_gemma":0.019118492,"threshold_uncertainty_score":0.9864422},"labels":[],"label_agreement":null},{"id":"W2113045564","doi":"10.1139/e02-105","title":"K-Ar dating constraints on the tectonothermal evolution of the external Humber zone, southern Quebec Appalachians","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"","keywords":"Nappe; Geology; Metamorphism; Imbrication; Ordovician; Geochemistry; Outcrop; Paleontology; Metamorphic rock; Orogeny; Devonian; Geochronology; Tectonics","score_opus":0.01369995627512812,"score_gpt":0.18015005971577647,"score_spread":0.16645010344064834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113045564","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98216295,0.00027406812,0.00013258634,0.0007670823,0.00016675191,0.00004792332,0.000026329823,0.00000149675,0.016420802],"genre_scores_gemma":[0.9991689,0.000001459677,0.00024886357,0.00028823825,0.000050903534,1.037095e-7,2.8596696e-7,8.7042326e-7,0.00024039643],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99878937,0.00018341374,0.00027779205,0.00012031965,0.00033363467,0.00029545897],"domain_scores_gemma":[0.99915504,0.00019200899,0.00025391814,0.00010745594,0.00007445993,0.00021713207],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009771693,0.00008855645,0.00013660945,0.00008093124,0.00046431454,0.00006890595,0.0005047368,0.00003627926,0.014046413],"category_scores_gemma":[0.0003654842,0.000039484705,0.00013455791,0.00045014525,0.0013771448,0.00009311717,0.0000038145504,0.00021632473,0.000043678156],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000029952655,0.0000047808344,0.98964643,0.0000015907597,0.000011931277,0.0000058085107,0.00019595535,0.0042348024,0.0002548479,0.0021671136,0.00002626021,0.0034474954],"study_design_scores_gemma":[0.00012907562,0.00012886223,0.9877568,0.00007286506,0.000024991696,0.00008708324,0.0024150661,0.00091241865,0.00089141703,0.00649347,0.00096815923,0.00011977704],"about_ca_topic_score_codex":0.093299106,"about_ca_topic_score_gemma":0.6980165,"teacher_disagreement_score":0.60471743,"about_ca_system_score_codex":0.0000027622946,"about_ca_system_score_gemma":0.00072180416,"threshold_uncertainty_score":0.9868549},"labels":[],"label_agreement":null},{"id":"W2113378460","doi":"10.1139/cjes-2014-0034","title":"Geochemical constraints on magmatic and metallogenic processes: Iskut River Formation, volcanogenic massive sulfide-hosting basalts, NW British Columbia, Canada","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Geological Survey of Canada; Dalhousie University","funders":"","keywords":"Basalt; Geology; Geochemistry; Rift; Flood basalt; Rhyolite; Mantle (geology); Volcanic rock; Partial melting; Volcano; Structural basin; Geomorphology; Volcanism; Paleontology; Tectonics","score_opus":0.008784851794690463,"score_gpt":0.16803093038669883,"score_spread":0.15924607859200837,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113378460","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99593383,0.00082163187,0.00004450865,0.0007098258,0.00012923758,0.00007344112,0.00008151607,0.0000041702506,0.002201847],"genre_scores_gemma":[0.9980242,0.000037109032,0.0006934785,0.0010582183,0.000077590696,3.8749153e-7,0.000013240377,0.0000016623618,0.000094117335],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99826664,0.000086773995,0.0004494631,0.0002418256,0.00044076698,0.00051455543],"domain_scores_gemma":[0.99806845,0.00038504673,0.0002887008,0.00007748245,0.00027668802,0.00090365316],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006539134,0.000120264325,0.00030392242,0.000096153955,0.00052852917,0.0003886164,0.0003838473,0.000057076857,0.007800946],"category_scores_gemma":[0.0015763646,0.000116120915,0.00007025255,0.00052672107,0.000974929,0.00030675414,0.000008877981,0.00020746824,0.00001795176],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045079482,0.000006629406,0.97343683,0.0000528483,0.00004373432,0.00013037423,0.00012174871,0.0011776694,0.00006170362,0.000015105149,0.0011426866,0.023806175],"study_design_scores_gemma":[0.00056564296,0.0005265839,0.97222936,0.0002895856,0.00012380352,0.0009430622,0.0008615239,0.0073668296,0.00037359746,0.011959122,0.004227487,0.00053341966],"about_ca_topic_score_codex":0.8837134,"about_ca_topic_score_gemma":0.9993424,"teacher_disagreement_score":0.11562891,"about_ca_system_score_codex":0.0000064798214,"about_ca_system_score_gemma":0.0020645529,"threshold_uncertainty_score":0.99310607},"labels":[],"label_agreement":null},{"id":"W2113390173","doi":"10.1139/cjes-2014-0057","title":"Isotopic characterization of organic matter from the Danek Bonebed (Edmonton, Alberta, Canada) with special reference to amber","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fossil Insects in Amber","field":"Agricultural and Biological Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Saskatchewan Museum; University of Alberta","funders":"","keywords":"Geology; Paleontology; Stable isotope ratio; Earth science; Physics","score_opus":0.012352202812902785,"score_gpt":0.17520821887868634,"score_spread":0.16285601606578357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113390173","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9886409,0.00001192884,0.0000042308,0.0052590934,0.00027602393,0.00007202144,0.000023612303,0.0000010388133,0.005711144],"genre_scores_gemma":[0.9970024,0.0000015159794,0.000073806754,0.0018003902,0.0005582484,6.556998e-7,0.000003853039,7.955227e-7,0.000558302],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989326,0.00007624351,0.00024389426,0.00014645072,0.0003448416,0.0002559453],"domain_scores_gemma":[0.9990861,0.00018194626,0.00021840434,0.000063423904,0.00015117343,0.00029898525],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00026574655,0.00009368538,0.00015710187,0.00002067919,0.00025189482,0.00010440096,0.00049949123,0.00003477935,0.0031067017],"category_scores_gemma":[0.00010321118,0.000031165568,0.000023180914,0.00041207412,0.00022603916,0.00019873767,0.000013182295,0.00010887086,0.000017970578],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030798117,0.000012084395,0.8879243,0.0000029203843,0.000020245814,0.000015060204,0.000745236,0.00002807996,0.10210413,0.00045587946,0.003658464,0.0050028213],"study_design_scores_gemma":[0.000048246053,0.00019203662,0.9239943,0.000038503025,0.000006272653,0.000015869116,0.00012535349,0.0000061168653,0.0017193713,0.000055487217,0.07371502,0.00008338914],"about_ca_topic_score_codex":0.76260656,"about_ca_topic_score_gemma":0.9990909,"teacher_disagreement_score":0.23648433,"about_ca_system_score_codex":0.000012692439,"about_ca_system_score_gemma":0.0005609568,"threshold_uncertainty_score":0.9978046},"labels":[],"label_agreement":null},{"id":"W2113480760","doi":"10.1139/e07-044","title":"Llandovery (Early Silurian) orthide brachiopod associations from Anticosti Island, eastern CanadaThis article is one of a series of papers published in this Special Issue on the theme <i>The dynamic reef and shelly communities of the Paleozoic. This Special is in honour of our colleague and friend Paul Copper</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Brandon University; The Arctic Eider Society","funders":"","keywords":"Geology; Jaccard index; Storm; Paleontology; Series (stratigraphy); Reef; Oceanography; Cluster analysis","score_opus":0.01685254966380468,"score_gpt":0.19544351764513887,"score_spread":0.1785909679813342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113480760","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9813259,0.0011866216,1.220595e-7,0.004908148,0.00026306836,0.00014313374,0.00088783517,6.4455264e-7,0.011284475],"genre_scores_gemma":[0.9992704,0.00027925003,0.000052043,0.00017621162,0.00013738363,2.876478e-7,0.0000016213033,0.000001217178,0.00008162015],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981898,0.00036098552,0.00061565853,0.00012814041,0.00043690714,0.00026847943],"domain_scores_gemma":[0.9984014,0.0005845969,0.00059989584,0.00017948763,0.000106377345,0.00012821898],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011443445,0.00012347166,0.00039735957,0.00022350023,0.00047487815,0.00005961319,0.0005289448,0.000085280524,0.0011564458],"category_scores_gemma":[0.0003134577,0.000074394375,0.00007957441,0.0005440314,0.0015139496,0.00037613284,0.00000725661,0.00031858223,4.6097927e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006974801,0.000015850688,0.98036677,0.0000060987613,0.000037012076,0.000012658477,0.017975237,0.000023922821,0.00005196448,0.000037184916,0.00056653074,0.0008370135],"study_design_scores_gemma":[0.0004115665,0.00029427477,0.9887026,0.00012542059,0.000018909308,0.000027110222,0.009251941,0.00013565575,0.00025454367,0.00041976632,0.00027918076,0.00007901012],"about_ca_topic_score_codex":0.21201235,"about_ca_topic_score_gemma":0.97795326,"teacher_disagreement_score":0.7659409,"about_ca_system_score_codex":0.0000037027198,"about_ca_system_score_gemma":0.0009927395,"threshold_uncertainty_score":0.99975663},"labels":[],"label_agreement":null},{"id":"W2113744727","doi":"10.1139/e00-023","title":"Early Devonian eurypterids from the Northwest Territories of Arctic Canada","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Leverhulme Trust","keywords":"Telson; Devonian; Geology; Paleontology; Fauna; Arctic; Carapace; Oceanography; Ecology; Crustacean; Biology","score_opus":0.01052061499186643,"score_gpt":0.17959371646007358,"score_spread":0.16907310146820714,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113744727","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99245554,0.0022566128,0.000001089059,0.0016304671,0.0008785188,0.000028730074,0.00032621686,0.0000011939022,0.0024216077],"genre_scores_gemma":[0.999102,0.000036127003,0.00018504288,0.00037590423,0.00022534373,7.0339695e-8,0.000010509341,7.204276e-7,0.00006426359],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990224,0.00010572049,0.00026761708,0.00010859562,0.00018640996,0.00030922567],"domain_scores_gemma":[0.99918497,0.00022078761,0.00012715765,0.00009177361,0.000069981346,0.00030531586],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000321516,0.000079902464,0.00015150369,0.00005882842,0.00043725828,0.00003323724,0.0005525225,0.000043006738,0.0052121915],"category_scores_gemma":[0.00006921262,0.000049697086,0.000041990384,0.00023681541,0.0010854965,0.00021665369,0.0000016139257,0.00014641533,0.000013525197],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001021254,9.967839e-7,0.99551696,8.5118376e-7,0.000011268992,0.00004573867,0.00019693769,0.00039637779,0.0000014670295,0.00002235203,0.00012121846,0.0036756422],"study_design_scores_gemma":[0.00007136621,0.00017289614,0.9698469,0.000018325394,0.00000754474,0.00010870053,0.00017024882,0.00005388276,0.0000070473334,0.00034864913,0.029133594,0.000060835722],"about_ca_topic_score_codex":0.99459195,"about_ca_topic_score_gemma":0.999937,"teacher_disagreement_score":0.029012375,"about_ca_system_score_codex":0.0000026157823,"about_ca_system_score_gemma":0.0033991898,"threshold_uncertainty_score":0.9956972},"labels":[],"label_agreement":null},{"id":"W2113772257","doi":"10.1139/e06-131","title":"Devonian–Carboniferous paleogeography and orogenesis, northern Yukon and adjacent Arctic Alaska","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Northwestern University","keywords":"Geology; Carboniferous; Devonian; Orogeny; Paleontology; Paleozoic; Late Devonian extinction; Thrust fault; Fault (geology); Geomorphology; Tectonics; Structural basin","score_opus":0.0171905352737955,"score_gpt":0.19086286364736763,"score_spread":0.17367232837357213,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113772257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9869092,0.010847024,0.000035116536,0.00068815914,0.0002617418,0.00005456256,0.0000044938342,0.0000022631984,0.0011974386],"genre_scores_gemma":[0.9987631,0.00046364646,0.00045311826,0.00021984005,0.000084541534,7.816086e-8,0.0000010322632,9.928807e-7,0.000013652233],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99903494,0.000029534353,0.00021983447,0.00014603444,0.00019204132,0.00037762354],"domain_scores_gemma":[0.99906814,0.000083020095,0.00011365032,0.00004121715,0.00008597652,0.00060798833],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00082698604,0.00009212475,0.00013899656,0.00018143597,0.0005108929,0.00012360621,0.00012296511,0.0000388265,0.00025366113],"category_scores_gemma":[0.000069131085,0.000062754036,0.000034266337,0.00032539736,0.00052701763,0.00020313213,0.0000048128445,0.000088662244,0.000012075971],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008950941,0.0000016290323,0.98263,0.0000036096535,0.000007773246,0.000035679182,0.00020106221,0.0002342334,0.000003543066,0.000015941801,0.000006244791,0.01685133],"study_design_scores_gemma":[0.00014488514,0.00038162275,0.99571043,0.00001756165,0.000008737352,0.00013779012,0.0008721699,0.00006810029,0.000017717333,0.00032876738,0.0022246165,0.00008758657],"about_ca_topic_score_codex":0.014294321,"about_ca_topic_score_gemma":0.7774048,"teacher_disagreement_score":0.76311046,"about_ca_system_score_codex":0.0000012013892,"about_ca_system_score_gemma":0.00015494703,"threshold_uncertainty_score":0.9922696},"labels":[],"label_agreement":null},{"id":"W2113810164","doi":"10.1139/e07-006","title":"A new species of mosasaur (Squamata: Mosasauridae) from the Pierre Shale (lower Campanian) of Manitoba","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Amphibian and Reptile Biology","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature; Carleton University","funders":"American Museum of Natural History","keywords":"Quadrate bone; Geology; Anatomy; Paleontology; Foramen; Squamata; Genus; Biology; Zoology","score_opus":0.017973895058904867,"score_gpt":0.21297987581285416,"score_spread":0.1950059807539493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113810164","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9837517,0.000709355,0.00021904586,0.00048980565,0.0006217464,0.00007164008,0.000026021322,0.0000017782975,0.0141089065],"genre_scores_gemma":[0.9967725,0.000029531788,0.0017219323,0.00020897218,0.00022468739,1.0537276e-7,6.746986e-7,0.0000042364413,0.0010373159],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99862236,0.000042002353,0.00044736027,0.00015967096,0.00036411875,0.00036447513],"domain_scores_gemma":[0.99880606,0.0001429029,0.00038462735,0.00018037585,0.00003097619,0.00045508164],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008409148,0.00010761759,0.00022053796,0.00008654518,0.00018165885,0.000029959223,0.00079004647,0.00006729086,0.004294999],"category_scores_gemma":[0.000115250616,0.00006556746,0.0001095571,0.00041898724,0.0015616441,0.00021659124,0.000042178188,0.00014413336,0.000045478213],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020431155,0.000015346468,0.97733486,0.0000022852626,0.00001879841,0.00006302474,0.0015531935,0.0001922834,0.006847848,0.00023882746,0.008039868,0.0056732623],"study_design_scores_gemma":[0.00016762971,0.0002491382,0.95526683,0.000043000313,0.000013114191,0.00004414586,0.002896804,0.000015523143,0.0030256987,0.00036870953,0.03781374,0.00009564058],"about_ca_topic_score_codex":0.048179105,"about_ca_topic_score_gemma":0.5300742,"teacher_disagreement_score":0.48189506,"about_ca_system_score_codex":0.000019572299,"about_ca_system_score_gemma":0.0005267811,"threshold_uncertainty_score":0.99661523},"labels":[],"label_agreement":null},{"id":"W2113869969","doi":"10.1139/e08-038","title":"Late Quaternary paleoproductivity history on the Vancouver Island margin, western Canada: a multiproxy geochemical studyThis article is one of a series of papers published in this Special Issue on the theme <i>Polar Climate Stability Network</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Geology; Stadial; Oceanography; Terrigenous sediment; Upwelling; Sedimentary rock; Younger Dryas; Glacial period; Holocene; Geochemistry; Paleontology","score_opus":0.02967458563792869,"score_gpt":0.19837505508720954,"score_spread":0.16870046944928085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113869969","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9847181,0.0005009732,7.1003626e-8,0.0064081987,0.0007791035,0.00019108286,0.000059649567,0.0000015194423,0.0073413067],"genre_scores_gemma":[0.998677,0.00009542364,0.00002448207,0.0006657948,0.0003167519,8.933825e-7,0.0000011617877,0.0000021452447,0.000216329],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975777,0.0005294073,0.0004667035,0.00025470206,0.0005742685,0.0005972204],"domain_scores_gemma":[0.99831885,0.0007234191,0.00030960722,0.00027362435,0.00014575664,0.00022872687],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0029780623,0.00014311096,0.00035723363,0.00012364058,0.00040034184,0.000019866628,0.0006361973,0.00007654753,0.01598104],"category_scores_gemma":[0.000495843,0.000081778955,0.00007124674,0.00037976573,0.0021919538,0.00026838057,0.00001706497,0.00054872426,0.000009199856],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001699033,0.000027206142,0.9913574,0.000011768709,0.000022296095,0.00007580338,0.0020658555,0.00041873302,0.000018562201,0.000018195185,0.005759186,0.00005510761],"study_design_scores_gemma":[0.00023844358,0.00042117955,0.9895,0.000052087675,0.000008818169,0.00004448225,0.00063468475,0.00017590562,0.00078793935,0.00019281686,0.0078382995,0.00010534237],"about_ca_topic_score_codex":0.28733313,"about_ca_topic_score_gemma":0.9949574,"teacher_disagreement_score":0.70762426,"about_ca_system_score_codex":0.000008598232,"about_ca_system_score_gemma":0.0022416047,"threshold_uncertainty_score":0.9849185},"labels":[],"label_agreement":null},{"id":"W2113899004","doi":"10.1139/e05-052","title":"Styles of Proterozoic crustal growth on the southeast margin of Laurentia: evidence from the central Grenville Province northwest of Lac St.-Jean, Quebec","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"","keywords":"Geology; Terrane; Laurentia; Continental arc; Proterozoic; Subduction; Archean; Gneiss; Continental crust; Continental margin; Island arc; Passive margin; Geochemistry; Craton; Volcanic arc; Back-arc basin; Diachronous; Paleontology; Crust; Tectonics; Ordovician; Metamorphic rock; Rift","score_opus":0.016728168189551546,"score_gpt":0.18225898186725015,"score_spread":0.1655308136776986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113899004","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9894877,0.0017738428,0.00000886024,0.00796599,0.00006190396,0.000119642464,0.0002916042,0.0000012237235,0.00028923652],"genre_scores_gemma":[0.9994293,0.000044696302,0.00024224637,0.00012128933,0.000105001265,2.6736274e-7,0.000004569663,0.0000011069304,0.000051509385],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983174,0.00015802252,0.00048153847,0.00016808743,0.0005262654,0.0003486838],"domain_scores_gemma":[0.9983177,0.0005771973,0.00050369906,0.00014917064,0.00017412569,0.00027807968],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007305775,0.00012165136,0.00027161246,0.00009737504,0.00019656426,0.000044351415,0.00088402716,0.00004208887,0.0039252653],"category_scores_gemma":[0.0004795477,0.00005557383,0.00016800317,0.00046297937,0.0014106592,0.00020595735,0.000013303867,0.00019750024,0.000008547716],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029546089,0.000015547803,0.993272,0.0000091298425,0.000027192902,0.0000059764,0.0002820178,0.0032500436,0.0002096411,0.0002050103,0.000109737055,0.0025841275],"study_design_scores_gemma":[0.00009278265,0.00033082705,0.9944672,0.0001789828,0.000036541,0.000004984416,0.0010127696,0.0007785542,0.0020558925,0.00055053475,0.00041054896,0.00008036439],"about_ca_topic_score_codex":0.4466982,"about_ca_topic_score_gemma":0.9757155,"teacher_disagreement_score":0.5290173,"about_ca_system_score_codex":0.000002222447,"about_ca_system_score_gemma":0.000772869,"threshold_uncertainty_score":0.99698526},"labels":[],"label_agreement":null},{"id":"W2114058398","doi":"10.1139/e99-091","title":"Reconstruction of sea-surface temperature, salinity, and sea-ice cover in the northern North Atlantic during the last glacial maximum based on dinocyst assemblages","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":146,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"University of Cambridge; Université du Québec à Montréal","keywords":"Geology; Dinocyst; Glacial period; Oceanography; Meltwater; Sea ice; Thermohaline circulation; Paleontology","score_opus":0.015165766107219794,"score_gpt":0.21818751266711947,"score_spread":0.20302174655989969,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114058398","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960758,0.00025450805,2.6335636e-7,0.001052848,0.00017026,0.00009417349,0.000023992527,0.0000014989444,0.0023266433],"genre_scores_gemma":[0.99961907,0.00005842291,0.000038402377,0.0001922173,0.00005668625,1.5060319e-7,0.0000032920154,0.0000012149495,0.000030520216],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99859047,0.0003914074,0.00024096292,0.00014516253,0.00029306498,0.00033890555],"domain_scores_gemma":[0.9991051,0.00044636527,0.00011361773,0.000103971084,0.00006520444,0.00016573964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012960561,0.00009589418,0.00016530516,0.00016466991,0.000620538,0.00010573221,0.00041658516,0.000068801586,0.00071665196],"category_scores_gemma":[0.000096385455,0.00005288666,0.000042619435,0.0005177806,0.0009895188,0.00020303769,0.0000028934576,0.00040487724,0.000025272908],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039695726,0.0000040667683,0.9838208,0.000008449025,0.0000053586145,0.000086317355,0.00023463699,0.015327935,0.0000036569945,0.000002003223,0.000009960378,0.00045714612],"study_design_scores_gemma":[0.0002210842,0.00020262753,0.9970508,0.000038169437,0.0000064409855,0.00057437643,0.0002917549,0.0013380138,0.000024002205,0.00005951718,0.00013075753,0.00006240576],"about_ca_topic_score_codex":0.00973671,"about_ca_topic_score_gemma":0.8924327,"teacher_disagreement_score":0.882696,"about_ca_system_score_codex":8.503599e-7,"about_ca_system_score_gemma":0.0006445136,"threshold_uncertainty_score":0.9968575},"labels":[],"label_agreement":null},{"id":"W2114066521","doi":"10.1139/e02-040","title":"<i>Captorhinus magnus</i>, a new captorhinid (Amniota: Eureptilia) from the Lower Permian of Oklahoma, with new evidence on the homology of the astragalus","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"University of Oklahoma","keywords":"Geology; Anatomy; Paleontology; Anticline; Permian; Biology; Structural basin","score_opus":0.04017983041214497,"score_gpt":0.20303855053251518,"score_spread":0.16285872012037023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114066521","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96887827,0.008572295,0.0000118476655,0.01774667,0.0010672616,0.00011971868,0.000053847194,0.00000220033,0.0035478636],"genre_scores_gemma":[0.9978067,0.00009364478,0.00019290681,0.0010620344,0.0002523148,1.6006412e-7,6.59693e-7,0.0000018164394,0.000589761],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998343,0.00030037508,0.0003732916,0.00021289583,0.00036153276,0.00040890783],"domain_scores_gemma":[0.9977563,0.0010420493,0.00043491466,0.00031563494,0.00009600662,0.00035509357],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007749694,0.00014911412,0.0002581067,0.00009168141,0.00050394685,0.000035322446,0.0014248805,0.00009487679,0.0049063056],"category_scores_gemma":[0.00048407415,0.000063350475,0.0001180765,0.0004899889,0.0025702515,0.00023718996,0.000009604709,0.0003932044,0.000035758963],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005599848,0.0000092623695,0.9864467,0.000001734157,0.00003544257,0.000041905507,0.0010204815,0.0012858914,0.00005905666,0.00017335617,0.007754415,0.0031157865],"study_design_scores_gemma":[0.00017217483,0.0010978709,0.9925485,0.00011713589,0.000031640237,0.00041129813,0.00038478407,0.00018628617,0.000090647365,0.00057235063,0.004300836,0.00008647957],"about_ca_topic_score_codex":0.075119175,"about_ca_topic_score_gemma":0.7053391,"teacher_disagreement_score":0.63021994,"about_ca_system_score_codex":0.0000032771472,"about_ca_system_score_gemma":0.0019281221,"threshold_uncertainty_score":0.9960033},"labels":[],"label_agreement":null},{"id":"W2114244687","doi":"10.1139/e01-077","title":"Comparison of diagenetic fluids in the Proterozoic Thelon and Athabasca Basins, Canada: implications for protracted fluid histories in stable intracratonic basins","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Cameco (Canada); Queen's University","funders":"Cameco","keywords":"Diagenesis; Geology; Illite; Geochemistry; Structural basin; Cementation (geology); Quartz; Uranium ore; Mineralogy; Paleontology; Uranium; Clay minerals; Cement","score_opus":0.03712104104241066,"score_gpt":0.22958500129676154,"score_spread":0.1924639602543509,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114244687","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9899869,0.0043070805,0.000013541893,0.0048766388,0.00005552739,0.00024052156,0.00010271077,8.9915784e-7,0.00041616033],"genre_scores_gemma":[0.999252,0.00004407309,0.00050488394,0.00014622268,0.000022780221,0.0000036083268,0.0000041693943,8.692586e-7,0.000021342334],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99887234,0.00008244571,0.0004056642,0.00014142209,0.0001775808,0.0003205375],"domain_scores_gemma":[0.99924356,0.0002359413,0.000150792,0.00008362533,0.000085662185,0.00020039584],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005919477,0.00008662208,0.00023328181,0.00017569418,0.00020736198,0.00005539405,0.0003570221,0.000035633737,0.0005098476],"category_scores_gemma":[0.0002704008,0.000052822445,0.000037510566,0.00070212845,0.00034002197,0.00015586564,0.0000033822716,0.00014082878,6.506899e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000358547,0.000013130658,0.9954563,0.000009688125,0.000003430054,0.0000038848157,0.0004777189,0.0005846442,0.00011749531,0.00006750498,0.00013000146,0.003132662],"study_design_scores_gemma":[0.0001145334,0.00024805503,0.99032193,0.00002281213,0.000009601855,0.0000154478,0.0005062695,0.0038458433,0.00025567086,0.0009132833,0.0036732813,0.000073291776],"about_ca_topic_score_codex":0.47232187,"about_ca_topic_score_gemma":0.9978633,"teacher_disagreement_score":0.5255414,"about_ca_system_score_codex":0.0000073667206,"about_ca_system_score_gemma":0.0007278419,"threshold_uncertainty_score":0.5582474},"labels":[],"label_agreement":null},{"id":"W2114696605","doi":"10.1139/e09-037","title":"Early Pliocene fish remains from Arctic Canada support a pre-Pleistocene dispersal of percids (Teleostei: Perciformes)","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fish Ecology and Management Studies","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Sander; Pleistocene; Early Pleistocene; Pike; Geology; Perciformes; Arctic; Paleontology; Biological dispersal; Genus; Teleostei; Geography; Fish <Actinopterygii>; Ecology; Fishery; Oceanography; Biology; Population","score_opus":0.008187626334121869,"score_gpt":0.19632392978994348,"score_spread":0.1881363034558216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114696605","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98579174,0.00003788351,0.000016273378,0.0036456008,0.00032065334,0.00010525006,0.000036715242,0.0000028671134,0.01004303],"genre_scores_gemma":[0.9969335,0.000022342832,0.0004383803,0.0020477232,0.000056486057,8.0077467e-7,0.0000015370548,0.000003910816,0.0004952977],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984293,0.000038766517,0.00037829802,0.00022156077,0.00043459644,0.0004974632],"domain_scores_gemma":[0.9990771,0.00005304473,0.00023303252,0.00014239346,0.000038136495,0.00045632012],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004496839,0.00013880966,0.00026918165,0.00012608604,0.00042740782,0.00004289201,0.0005689006,0.000047194513,0.003032822],"category_scores_gemma":[0.00015584701,0.00011672126,0.00007058734,0.00037844575,0.00072764326,0.00042347735,0.000035324854,0.00016001127,0.000010864197],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016323922,0.000015243534,0.9858817,0.0000035097223,0.000020581994,0.00011928366,0.0008521514,0.0003493084,0.000048121023,0.000067948386,0.011986403,0.00063941063],"study_design_scores_gemma":[0.00020863411,0.0006864218,0.994323,0.000027451766,0.0000279052,0.000025857664,0.0005742407,0.000057477602,0.00009513951,0.00020907474,0.0036334144,0.00013138357],"about_ca_topic_score_codex":0.6876314,"about_ca_topic_score_gemma":0.99718416,"teacher_disagreement_score":0.30955273,"about_ca_system_score_codex":0.00008758974,"about_ca_system_score_gemma":0.0009960153,"threshold_uncertainty_score":0.99787855},"labels":[],"label_agreement":null},{"id":"W2115116446","doi":"10.1139/e05-107","title":"New eocrinoids from the Burgess Shale, southern British Columbia, Canada, and the Spence Shale, northern Utah, USA","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum","funders":"","keywords":"Geology; Oil shale; Paratype; Holotype; Paleontology; Genus; Geochemistry; Biology; Zoology","score_opus":0.008977134667619126,"score_gpt":0.17028192155033867,"score_spread":0.16130478688271954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115116446","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9713652,0.015241194,0.000015040871,0.0012884564,0.0005359925,0.000096420714,0.00023631864,0.000002367867,0.011218997],"genre_scores_gemma":[0.9981724,0.00004069036,0.0001911596,0.0003368243,0.00034474826,2.1043311e-7,0.0000019561603,9.978789e-7,0.0009110077],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99838614,0.00014841273,0.0003462045,0.00021447356,0.00041455825,0.00049023045],"domain_scores_gemma":[0.99864095,0.00042648785,0.00023446768,0.00013667486,0.000079158424,0.00048227204],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007233491,0.00011215041,0.000230951,0.00004091454,0.0013090901,0.0008973409,0.0008527608,0.000054864893,0.0014604853],"category_scores_gemma":[0.00008880526,0.00008354771,0.000080174614,0.00032596858,0.0016999973,0.000283447,0.0000024174092,0.00028388525,0.0000062527793],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000053847043,9.095225e-7,0.97186106,8.206979e-7,0.000012587623,0.00016611666,0.00020824005,0.00004803308,5.406369e-7,0.000020957865,0.0013242272,0.026351113],"study_design_scores_gemma":[0.00030258516,0.00004595909,0.9944773,0.000033568493,0.000020051533,0.00037544552,0.00063852506,0.00011516905,0.0000012055754,0.0025053283,0.0013627019,0.00012219652],"about_ca_topic_score_codex":0.99970937,"about_ca_topic_score_gemma":0.9999987,"teacher_disagreement_score":0.026807193,"about_ca_system_score_codex":0.0000021208882,"about_ca_system_score_gemma":0.0039452394,"threshold_uncertainty_score":0.99999106},"labels":[],"label_agreement":null},{"id":"W2115228923","doi":"10.1139/e06-025","title":"A new abelisauroid theropod from northwestern Patagonia","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Cretaceous; Paleontology; Cenomanian; Fluvial; Theropoda; Structural basin","score_opus":0.014041621506853376,"score_gpt":0.19456972060607589,"score_spread":0.18052809909922252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115228923","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98082453,0.006131553,0.00016004038,0.000800334,0.0010160966,0.00003189618,0.00009460122,0.000004869164,0.010936091],"genre_scores_gemma":[0.99657834,0.000020806965,0.002337507,0.00025406972,0.0005090095,3.5525233e-8,0.000017258628,0.0000010107632,0.00028194976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898,0.000072359144,0.00025819588,0.00015400493,0.00015309408,0.00038235023],"domain_scores_gemma":[0.99916285,0.000107106396,0.00015871829,0.00008161872,0.00004773272,0.00044198526],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029903222,0.00009504856,0.00015602222,0.00018258163,0.00034948508,0.00006514317,0.0004383786,0.00007292374,0.00368866],"category_scores_gemma":[0.000017849925,0.00006945715,0.00006114592,0.00024006529,0.0004802968,0.00033854818,0.000002264127,0.00014518134,0.0001926662],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006747477,0.000001612529,0.9934833,3.6870784e-7,0.000006542801,0.0000850374,0.000082926344,0.0007397208,0.000019418592,0.00009800874,0.0008220926,0.004654211],"study_design_scores_gemma":[0.00015122109,0.00017895362,0.97066414,0.000009714455,0.000007980406,0.00016106995,0.00009910445,0.0001589396,0.000017747565,0.0035655391,0.024895549,0.00009001499],"about_ca_topic_score_codex":0.45743683,"about_ca_topic_score_gemma":0.979825,"teacher_disagreement_score":0.5223882,"about_ca_system_score_codex":0.000001257085,"about_ca_system_score_gemma":0.0016821447,"threshold_uncertainty_score":0.9972221},"labels":[],"label_agreement":null},{"id":"W2115444762","doi":"10.1139/e03-008","title":"Validity and composition of the Silurian trilobite genera <i>Borealarges</i> and <i>Dicranogmus</i>, with new species from the Canadian Arctic","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Arctic; Trilobite; Monophyly; Taxon; Genus; Paleontology; Range (aeronautics); Geology; Group (periodic table); Phylogenetic tree; Ecology; Geography; Biology; Clade; Chemistry; Ordovician","score_opus":0.028984077556118343,"score_gpt":0.16680293959584674,"score_spread":0.1378188620397284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115444762","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923047,0.00046467246,0.0000014758923,0.0062991534,0.00012829422,0.000057863843,0.00012317699,9.239392e-7,0.0006197642],"genre_scores_gemma":[0.99916524,0.00006824144,0.00007577197,0.0005454437,0.00008877443,7.7695795e-8,0.0000030485044,2.5024346e-7,0.000053154894],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99932283,0.00009677182,0.00011033009,0.000095825526,0.00017619468,0.00019803636],"domain_scores_gemma":[0.9992763,0.00011686069,0.00011542483,0.000028410152,0.000070304224,0.00039269534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040303235,0.00006534475,0.000100656245,0.000022424429,0.000987385,0.0001369478,0.0002084448,0.000035638324,0.000078557634],"category_scores_gemma":[0.00005485137,0.000020659507,0.000030943047,0.000283106,0.0005301908,0.00017878917,0.0000065594386,0.00010446894,5.765929e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008371743,0.000003828754,0.9913093,0.000001571201,0.0000088817005,0.000008276839,0.00034442297,0.000033460383,0.0059064836,0.0007495047,0.0012432311,0.0003827033],"study_design_scores_gemma":[0.000105446474,0.00012950212,0.9761364,0.000043356846,0.000021136822,0.00008327959,0.00032171028,0.000008196889,0.0009153816,0.00066484214,0.021511849,0.00005889447],"about_ca_topic_score_codex":0.5243467,"about_ca_topic_score_gemma":0.98812693,"teacher_disagreement_score":0.46378022,"about_ca_system_score_codex":0.0000111915015,"about_ca_system_score_gemma":0.00050610525,"threshold_uncertainty_score":0.7594267},"labels":[],"label_agreement":null},{"id":"W2115818748","doi":"10.1139/cjes-2012-0189","title":"The Late Cambrian (Furongian) trilobite<i>Tangshanaspis</i>Zhou and Zhang, 1978, in North America","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Trilobite; Fauna; Geology; Paleontology; Biostratigraphy; Ecology; Ordovician; Biology","score_opus":0.01327028547445499,"score_gpt":0.19545820876104347,"score_spread":0.18218792328658848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115818748","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9646899,0.011703192,0.000003058625,0.0018423926,0.0003648524,0.00010426592,0.000020696802,0.0000028430247,0.0212688],"genre_scores_gemma":[0.99911076,0.0002355593,0.00020578978,0.00025634805,0.00006444771,4.5553597e-7,8.506804e-7,5.677572e-7,0.00012523658],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99868786,0.000109395616,0.00031726327,0.00014045143,0.00020200301,0.000542999],"domain_scores_gemma":[0.9988414,0.00020115433,0.0001881223,0.000093488175,0.000060425882,0.0006154296],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005520974,0.00011511443,0.00018428541,0.00030106964,0.0007027529,0.00030353997,0.0004516711,0.000048129725,0.00030019315],"category_scores_gemma":[0.00011845185,0.00007246504,0.000057441193,0.0006618929,0.0012485698,0.00059807254,0.0000012849331,0.00022855798,0.00002639494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000036306042,0.0000012689835,0.919335,0.0000014890968,0.000006719987,0.000045348977,0.00034318186,0.000068322595,0.0000035583055,0.00003960476,0.0001438664,0.080007985],"study_design_scores_gemma":[0.00013567349,0.00023937749,0.99248254,0.000015961077,0.0000046860764,0.00007756872,0.00067375664,0.00038264395,0.0000037599052,0.00035162552,0.0055329646,0.00009944406],"about_ca_topic_score_codex":0.05694871,"about_ca_topic_score_gemma":0.94211274,"teacher_disagreement_score":0.885164,"about_ca_system_score_codex":0.0000011113318,"about_ca_system_score_gemma":0.0006411392,"threshold_uncertainty_score":0.94933116},"labels":[],"label_agreement":null},{"id":"W2115874487","doi":"10.1139/e00-104","title":"The influence of mantle plume in the genesis of the Cache Creek oceanic igneous rocks: implications for the geodynamic evolution of the inner accreted terranes of the Canadian Cordillera","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Geochemistry; Mafic; Basalt; Terrane; Mantle plume; Igneous rock; Ultramafic rock; Volcanic rock; Oceanic crust; Permian; Large igneous province; Gabbro; Petrogenesis; Subduction; Paleontology; Volcano; Tectonics; Lithosphere; Magmatism","score_opus":0.0145059726464029,"score_gpt":0.19920234033878342,"score_spread":0.18469636769238051,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115874487","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9875993,0.0014930294,0.000005863688,0.009994153,0.00010355908,0.0002607042,0.0001244011,6.7749016e-7,0.00041829716],"genre_scores_gemma":[0.9995376,0.000074509444,0.000016701826,0.00027641925,0.000025754003,0.0000017071538,0.0000010626566,0.0000013824674,0.0000649007],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99838793,0.00021747957,0.0005195114,0.00013176484,0.00037975656,0.00036357876],"domain_scores_gemma":[0.99792904,0.0007117664,0.0005499293,0.00036910572,0.00030762993,0.00013251565],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011725024,0.000103334285,0.00020243619,0.00009704305,0.001105955,0.000052485106,0.0022409388,0.0000588117,0.00019955412],"category_scores_gemma":[0.00066743995,0.000035425495,0.00023079524,0.0015857844,0.001780729,0.000101268735,0.000022486642,0.00020302592,7.1627954e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000071955064,0.0000053736403,0.95898634,0.000005483394,0.000024932075,5.2566355e-7,0.00038915905,0.03916929,0.00029016804,0.00011669877,0.00006585623,0.00093899557],"study_design_scores_gemma":[0.00007708126,0.00007476677,0.9901153,0.00003951324,0.00005814526,0.00003983204,0.0015151203,0.004462852,0.00008782303,0.00300631,0.00047119224,0.000052062474],"about_ca_topic_score_codex":0.7021116,"about_ca_topic_score_gemma":0.9891717,"teacher_disagreement_score":0.28706008,"about_ca_system_score_codex":0.000010331945,"about_ca_system_score_gemma":0.0015021643,"threshold_uncertainty_score":0.8506223},"labels":[],"label_agreement":null},{"id":"W2115880590","doi":"10.1139/e11-006","title":"Crustal velocity structure of the southern Nechako basin, British Columbia, from wide-angle seismic traveltime inversion<sup>1</sup>This article is one of a series of papers published in this Special Issue on the theme of <i>New insights in Cordilleran Intermontane geoscience: reducing exploration risk in the mountain pine beetle-affected area, British Columbia</i>.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Sedimentary rock; Sedimentary basin; Seismic refraction; Seismology; Structural basin; Crust; Inversion (geology); Basin and range topography; Paleontology","score_opus":0.013474800837395383,"score_gpt":0.16118956574691515,"score_spread":0.14771476490951976,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115880590","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997764,0.00016047532,0.0000014086156,0.0007272062,0.000084886975,0.00021106991,0.00037574137,0.0000014322787,0.0006738007],"genre_scores_gemma":[0.999285,0.000043955653,0.00017093064,0.0003113719,0.00006368378,4.741368e-7,0.0000074250543,0.000002079882,0.00011511848],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977459,0.0003707017,0.00072574377,0.00025894275,0.0005915727,0.0003071768],"domain_scores_gemma":[0.99864954,0.00024213888,0.0005843383,0.00018365234,0.00017794888,0.00016236998],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009253164,0.00010396252,0.0004421227,0.00013299505,0.0002236115,0.0002097338,0.0008525164,0.00009608003,0.031487163],"category_scores_gemma":[0.00089266984,0.00008465632,0.00013042994,0.0017306313,0.0013293588,0.0004964958,0.000023769087,0.00037973054,0.0000011944753],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005625221,0.00006492353,0.9689877,0.000010286468,0.000024317786,0.00003092331,0.02089327,0.0018308662,0.00060889707,0.0000016101033,0.0008620912,0.0066288384],"study_design_scores_gemma":[0.00042696876,0.00046254162,0.9740502,0.00029644067,0.000026446281,0.000016935533,0.01297239,0.0043090074,0.0011684711,0.0060769934,0.000078289035,0.00011529413],"about_ca_topic_score_codex":0.96059585,"about_ca_topic_score_gemma":0.9940142,"teacher_disagreement_score":0.033418357,"about_ca_system_score_codex":0.000010018296,"about_ca_system_score_gemma":0.0005221507,"threshold_uncertainty_score":0.9693982},"labels":[],"label_agreement":null},{"id":"W2116097273","doi":"10.1139/e10-073","title":"New information on olenelline trilobites from the Cambrian Sekwi Formation in northwestern Canada","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Aurora Research Institute; National Science Foundation","keywords":"Trilobite; Laurentia; Paleontology; Geology; Facies; Structural basin; Stage (stratigraphy); Series (stratigraphy); Paleozoic; Ordovician","score_opus":0.012964209934788421,"score_gpt":0.18258792977098595,"score_spread":0.16962371983619753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116097273","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942248,0.000118778036,0.0000752753,0.0025440038,0.0006777519,0.000060731207,0.00006573244,0.00000185451,0.002231107],"genre_scores_gemma":[0.9981393,0.000014509312,0.00047131916,0.0011861142,0.0001333109,1.0268909e-7,0.00002657024,4.900383e-7,0.000028251516],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909145,0.000029090483,0.00033291653,0.00005508484,0.000264805,0.0002266569],"domain_scores_gemma":[0.99913806,0.00020162921,0.00019416708,0.000070433765,0.00008170119,0.00031401557],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041732792,0.00007432929,0.000095510804,0.00015030826,0.00029540653,0.00022071622,0.00038233638,0.00003756264,0.0012436868],"category_scores_gemma":[0.00016022063,0.00004261925,0.000024142944,0.00042168144,0.00008668944,0.0012942012,0.000002097427,0.00023647214,0.00003821395],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000064995315,8.8188307e-7,0.96882814,0.0000017609864,0.0000017492948,0.000007194807,0.00044548672,0.0057954676,0.0000022955937,0.000109995686,0.000559363,0.024241189],"study_design_scores_gemma":[0.00014250778,0.000100656536,0.9626433,0.000020688842,0.0000025497939,0.00003509649,0.0005754933,0.001652341,0.000055369062,0.0005216334,0.034182422,0.00006793721],"about_ca_topic_score_codex":0.96451324,"about_ca_topic_score_gemma":0.99986124,"teacher_disagreement_score":0.03534797,"about_ca_system_score_codex":0.0000022939128,"about_ca_system_score_gemma":0.0022643749,"threshold_uncertainty_score":0.9996693},"labels":[],"label_agreement":null},{"id":"W2116394802","doi":"10.1139/e06-045","title":"Uniformitarianism as a guide to rocky-shore ecosystems in the geological record","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Rocky shore; Shore; Paleontology; Precambrian; Intertidal zone; Neogene; Geologic record; Pleistocene; Sedimentary rock; Taphonomy; Oceanography","score_opus":0.023793114122115037,"score_gpt":0.25032198609747774,"score_spread":0.2265288719753627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116394802","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9365251,0.00054593576,0.000013797757,0.007832543,0.00041318746,0.000120216035,0.000007239776,0.000002345314,0.054539658],"genre_scores_gemma":[0.9979355,0.000010486641,0.0005838751,0.0009057166,0.00015213796,5.496379e-7,0.0000031885259,8.854696e-7,0.0004076847],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99823195,0.0002861056,0.00038835692,0.00017025707,0.00029328908,0.00063006254],"domain_scores_gemma":[0.99900055,0.0003404497,0.000101744685,0.00011339851,0.00008267607,0.0003611672],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0027540824,0.00009808528,0.00019509392,0.00045258785,0.0004413758,0.000121512916,0.0009084227,0.00009966813,0.0019594654],"category_scores_gemma":[0.00029116645,0.00005739559,0.0000573076,0.0007249531,0.00042629597,0.00021026054,0.0000057975208,0.00032609713,0.00039306848],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007637733,0.000003027109,0.9952187,0.0000016954552,0.0000022989427,0.0005352444,0.00018442633,0.001933515,7.8685963e-7,0.00077921746,0.0010785222,0.00025491437],"study_design_scores_gemma":[0.000121569894,0.00050738384,0.9468024,0.000019018102,0.0000032234132,0.0015119173,0.0009831757,0.00034541942,0.000005270475,0.00427953,0.04533625,0.000084856976],"about_ca_topic_score_codex":0.094954334,"about_ca_topic_score_gemma":0.9756377,"teacher_disagreement_score":0.88068336,"about_ca_system_score_codex":8.5972323e-7,"about_ca_system_score_gemma":0.0012353634,"threshold_uncertainty_score":0.99895287},"labels":[],"label_agreement":null},{"id":"W2116429473","doi":"10.1139/e08-059","title":"Last glacial maximum (LGM) primary productivity in the northern North Atlantic OceanThis article is one of a series of papers published in this Special Issue on the theme <i>Polar Climate Stability Network</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Fonds Québécois de la Recherche sur la Nature et les Technologies; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Last Glacial Maximum; Geology; Glacial period; Oceanography; Northern Hemisphere; Dinocyst; Climatology; Bay; Physical geography; Geography; Paleontology; Ecology","score_opus":0.025305007045329314,"score_gpt":0.2016407950476494,"score_spread":0.17633578800232008,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116429473","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9833977,0.0002526122,1.2722626e-7,0.0055109398,0.00029354385,0.00021353853,0.000034383338,0.0000015028107,0.010295614],"genre_scores_gemma":[0.9991527,0.00010223185,0.000046420188,0.00030812007,0.00036936064,5.3221686e-7,0.0000033641043,0.000001745406,0.000015531294],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974331,0.0006507445,0.0005182382,0.0002284233,0.0005296118,0.000639849],"domain_scores_gemma":[0.9986595,0.00051676086,0.00029002476,0.00023464527,0.00013781601,0.00016126978],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0040932572,0.00012648889,0.00035753503,0.00022175342,0.0004888502,0.0000443613,0.00076867366,0.00007271635,0.005945919],"category_scores_gemma":[0.0005004279,0.000072768,0.00008177452,0.001213925,0.0031149657,0.00045037892,0.000014735379,0.0005255765,0.000017725315],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001349482,0.00003709324,0.9947429,0.000018474771,0.000010334431,0.00007006085,0.004067431,0.0004750475,0.00000580611,0.00003544097,0.00018109792,0.00022137316],"study_design_scores_gemma":[0.00018669802,0.00040007188,0.99685454,0.00003321628,0.0000063271236,0.000116200674,0.0007346631,0.00004325335,0.000099745725,0.00041246423,0.001036014,0.00007680359],"about_ca_topic_score_codex":0.008627535,"about_ca_topic_score_gemma":0.9095146,"teacher_disagreement_score":0.9008871,"about_ca_system_score_codex":0.0000022991524,"about_ca_system_score_gemma":0.0012939478,"threshold_uncertainty_score":0.99959797},"labels":[],"label_agreement":null},{"id":"W2116549710","doi":"10.1139/e06-109","title":"High-resolution organic carbon isotope record across the Cretaceous–Tertiary boundary in south-central Alberta: implications for the post-impact recovery rate of terrestrial ecosystems and use of δ<sup>13</sup>C as a boundary marker","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Royal Tyrrell Museum","funders":"Natural Sciences and Engineering Research Council of Canada; University of Waterloo","keywords":"Geology; Context (archaeology); Terrestrial ecosystem; Excursion; Isotopes of carbon; Paleontology; Cretaceous; Boundary (topology); Sedimentary rock; Carbon cycle; Total organic carbon; Ecosystem; Chemistry; Ecology; Environmental chemistry","score_opus":0.020588887198032292,"score_gpt":0.25484116268946483,"score_spread":0.23425227549143254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116549710","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944318,0.0023728674,0.000021388065,0.0021024938,0.00046523707,0.0003855904,0.00015016667,0.0000014103352,0.000069027425],"genre_scores_gemma":[0.9994771,0.000111545975,0.00008310712,0.00015945119,0.000100289035,0.0000011558119,0.000011289522,0.0000030642504,0.000052984247],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980172,0.00034388673,0.0005987065,0.00019184334,0.00015025762,0.0006981067],"domain_scores_gemma":[0.9967022,0.0022906617,0.00038070226,0.00018224226,0.0001401786,0.00030401757],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003543159,0.000131047,0.00028782824,0.00026047276,0.00068216823,0.00016701376,0.00047165938,0.00012722115,0.00017577091],"category_scores_gemma":[0.0010077253,0.000076592056,0.00010683129,0.00048413535,0.0015005626,0.00039716088,0.000014073501,0.00032049516,0.0000023995813],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035303325,0.000005297,0.9954167,0.000009593189,0.00004166716,0.00001182548,0.0013550337,0.0016685104,0.000026364187,0.000007170337,0.000039082548,0.0010657042],"study_design_scores_gemma":[0.00042344138,0.000601684,0.99253076,0.000046502955,0.000022276525,0.00028417507,0.000833978,0.0035561766,0.00002211129,0.0003083095,0.0012864652,0.00008409715],"about_ca_topic_score_codex":0.10625699,"about_ca_topic_score_gemma":0.92066234,"teacher_disagreement_score":0.8144053,"about_ca_system_score_codex":0.0000040888085,"about_ca_system_score_gemma":0.0024215456,"threshold_uncertainty_score":0.8996945},"labels":[],"label_agreement":null},{"id":"W2116636505","doi":"10.1139/e06-013","title":"Reconstructing sea-level change from the internal architecture of stromatolite reefs: an example from the Mesoproterozoic Sulky Formation, Dismal Lakes Group, arctic Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Reef; Geology; Subaerial; Stromatolite; Paleontology; Aggradation; Sea level; Carbonate platform; Marine transgression; Oceanography; Arctic; Evaporite; Sedimentary depositional environment; Sedimentary rock; Structural basin; Carbonate; Fluvial","score_opus":0.045397053270912466,"score_gpt":0.20028056529765492,"score_spread":0.15488351202674244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116636505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9922456,0.004168578,0.00012345833,0.0013671416,0.000545539,0.000114032824,0.0007082148,0.0000026840623,0.0007247243],"genre_scores_gemma":[0.9982357,0.000008373233,0.0010979325,0.00021934605,0.00040889115,5.710349e-7,0.000024821524,9.671428e-7,0.0000034194188],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99840206,0.0002198594,0.00045734213,0.00017041028,0.00036314857,0.00038719128],"domain_scores_gemma":[0.9984956,0.0005199891,0.0004600571,0.00016953454,0.00008339235,0.000271455],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007187963,0.00013625939,0.00021249207,0.00009058416,0.00075917505,0.00017519348,0.00086198974,0.000050887757,0.00027039353],"category_scores_gemma":[0.00006709051,0.00007571743,0.00007690012,0.00026714598,0.00079002604,0.0006429295,0.0000023016064,0.00030409775,5.487821e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011652894,0.0000016878618,0.98158723,0.0000023977964,0.000017777944,0.000024643014,0.0013555438,0.00008792819,0.000013849541,0.00007429498,0.00009244371,0.016730541],"study_design_scores_gemma":[0.00016531136,0.00010641353,0.99263716,0.00009168001,0.000017759903,0.0001697293,0.002554938,0.0006650596,0.000047055455,0.0030073,0.00044279438,0.000094805386],"about_ca_topic_score_codex":0.9925557,"about_ca_topic_score_gemma":0.9998564,"teacher_disagreement_score":0.016635735,"about_ca_system_score_codex":0.0000034003358,"about_ca_system_score_gemma":0.000981427,"threshold_uncertainty_score":0.58390373},"labels":[],"label_agreement":null},{"id":"W2116910270","doi":"10.1139/cjes-2014-0159","title":"Neogene strontium isotope stratigraphy, foraminifer biostratigraphy, and lithostratigraphy from offshore wells, Queen Charlotte Basin, British Columbia, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Luonnontieteiden ja Tekniikan Tutkimuksen Toimikunta; Social Sciences and Humanities Research Council of Canada; Natural Sciences and Engineering Research Council of Canada; Memorial University of Newfoundland; University of Victoria; Commonwealth Scientific and Industrial Research Organisation; Shell Canada","keywords":"Geology; Neogene; Paleontology; Anticline; Biostratigraphy; Chronostratigraphy; Sedimentary rock; Sedimentary depositional environment; Outcrop; Stratigraphy; Structural basin; Tectonics","score_opus":0.018680199030386407,"score_gpt":0.20416135199854502,"score_spread":0.18548115296815862,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116910270","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98443973,0.007205706,0.000005077301,0.0012430742,0.00073283986,0.00016528256,0.0004762143,0.000005619371,0.005726457],"genre_scores_gemma":[0.99822223,0.00016804162,0.00084009283,0.00042675753,0.0001396611,5.775041e-7,0.000031011507,0.000003157821,0.00016847701],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975705,0.00024426254,0.0004893747,0.00036333213,0.0005356093,0.00079688086],"domain_scores_gemma":[0.9973476,0.00015770286,0.00022354303,0.0001624772,0.000281184,0.001827515],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009355376,0.0001733387,0.00040723983,0.00025344163,0.0006184645,0.0007796343,0.00062060467,0.00015208634,0.0014203406],"category_scores_gemma":[0.00011478397,0.0001951231,0.000094316936,0.0006625231,0.0014577407,0.0005552774,0.00000722876,0.00041063255,0.0000060326483],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011303107,0.0000046589935,0.9942338,0.0000054927223,0.00004987641,0.00044542973,0.00008645928,0.000039916144,9.118961e-7,0.000021077733,0.0045750006,0.0005260996],"study_design_scores_gemma":[0.000355309,0.00066545204,0.98928964,0.00005002226,0.000026982934,0.0003908072,0.0012482117,0.00012292656,0.000018022462,0.0008894063,0.0067240843,0.00021911008],"about_ca_topic_score_codex":0.989421,"about_ca_topic_score_gemma":0.9999602,"teacher_disagreement_score":0.013782494,"about_ca_system_score_codex":0.0000010249483,"about_ca_system_score_gemma":0.007749903,"threshold_uncertainty_score":0.9994925},"labels":[],"label_agreement":null},{"id":"W2116931427","doi":"10.1139/e11-034","title":"Lithostratigraphic and tectonic framework of Jurassic and Cretaceous Intermontane sedimentary basins of south-central British Columbia<sup>1</sup>This article is one of a series of papers published in this Special Issue on the theme of <i>New insights in Cordilleran Intermontane geoscience: reducing exploration risk in the mountain pine beetle-affected area, British Columbia</i>.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of British Columbia","funders":"","keywords":"Geology; Paleontology; Cretaceous; Clastic rock; Sedimentary rock; Sedimentary basin; Volcanic rock; Unconformity; Volcano; Stratigraphy; Tectonics","score_opus":0.017919233963586165,"score_gpt":0.19773807296071755,"score_spread":0.17981883899713139,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116931427","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99732804,0.001241526,0.000001029874,0.0003434433,0.00009253229,0.00029996954,0.00010073807,0.0000011344083,0.00059157395],"genre_scores_gemma":[0.99913985,0.00048493443,0.0002443115,0.0000681918,0.000032681735,0.0000011911919,0.0000028933027,0.0000022028808,0.000023727538],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977648,0.00048685275,0.0007549411,0.00024021961,0.00038215262,0.0003710205],"domain_scores_gemma":[0.9986323,0.00040637626,0.0005082893,0.00015056672,0.00012928115,0.00017319541],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017493863,0.00009594174,0.0004643693,0.00029638546,0.00017470778,0.0001433564,0.00045961956,0.00012194495,0.003897865],"category_scores_gemma":[0.0006360989,0.00009581086,0.00005713059,0.0011935105,0.002686643,0.0005566018,0.000015689935,0.00049225823,1.8802324e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008487403,0.00004377456,0.9742939,0.00002976904,0.000019885949,0.00008910372,0.022814149,0.00006630125,0.00006538387,0.0000045317142,0.00007411765,0.0024142158],"study_design_scores_gemma":[0.00049446966,0.0016717832,0.9840792,0.0006988158,0.000017847924,0.00021303343,0.011053503,0.0005280861,0.00020860715,0.00093721994,0.000012255337,0.00008518028],"about_ca_topic_score_codex":0.5387204,"about_ca_topic_score_gemma":0.98735386,"teacher_disagreement_score":0.44863343,"about_ca_system_score_codex":0.0000029378837,"about_ca_system_score_gemma":0.00064204715,"threshold_uncertainty_score":0.99701273},"labels":[],"label_agreement":null},{"id":"W2117623996","doi":"10.1139/e06-125","title":"Limnology, sedimentology, and hydrology of a jökulhlaup into a meromictic High Arctic lake","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"National Science Foundation","keywords":"Geology; Sill; Shelf ice; Halite; Hydrology (agriculture); Limnology; Sedimentology; Chemocline; Shore; Structural basin; Arctic; Oceanography; Geomorphology; Geochemistry; Water column; Arctic ice pack","score_opus":0.02611282994967158,"score_gpt":0.2368216681287287,"score_spread":0.2107088381790571,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117623996","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99410564,0.0027315703,0.000010525061,0.001507818,0.0007043703,0.000052242005,0.00009849682,0.0000020443217,0.0007873142],"genre_scores_gemma":[0.9987165,0.00012863577,0.0004803838,0.0005133736,0.00011942976,6.8074236e-8,0.000014466586,0.0000016579983,0.000025490146],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988194,0.00005690331,0.0003619677,0.00015365059,0.00015337208,0.00045469357],"domain_scores_gemma":[0.9988037,0.0002664302,0.00024044252,0.00007979655,0.00008777301,0.0005218643],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001353796,0.00010113625,0.00025479042,0.0005225662,0.00023150312,0.00003905312,0.00028288644,0.00009008289,0.0033851801],"category_scores_gemma":[0.000126725,0.00007889585,0.00004568341,0.00035498184,0.0013825468,0.00022738037,0.000007021531,0.00017197784,0.000017594008],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001944752,0.0000035590747,0.99658424,0.000012320105,0.000014419656,0.00011393916,0.0008303808,0.00005976752,0.00018358277,0.00014275305,0.00005035634,0.0019852594],"study_design_scores_gemma":[0.00028204554,0.0009225343,0.9894477,0.000035633777,0.00002473048,0.0008141223,0.0007569376,0.00016695613,0.00016636935,0.001898319,0.0053808438,0.00010381443],"about_ca_topic_score_codex":0.094501615,"about_ca_topic_score_gemma":0.9689161,"teacher_disagreement_score":0.8744145,"about_ca_system_score_codex":0.0000017283031,"about_ca_system_score_gemma":0.0004372191,"threshold_uncertainty_score":0.9975259},"labels":[],"label_agreement":null},{"id":"W2117801945","doi":"10.1139/e01-075","title":"The Early Permian floras of Prince Edward Island, Canada: differentiating global from local effects of climate change","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Dalhousie University; University of Chicago; National Science Foundation","keywords":"Permian; Carboniferous; Pangaea; Paleontology; Geology; Subtropics; Laurasia; Structural basin; Paleozoic; Earth science; Ecology; Gondwana","score_opus":0.017525245599296316,"score_gpt":0.17054125452454946,"score_spread":0.15301600892525313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117801945","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973821,0.00095555914,0.0000032126572,0.0007088793,0.00039467553,0.000048217884,0.00019471622,0.0000011589125,0.00031150042],"genre_scores_gemma":[0.99967235,0.00012823507,0.000016346152,0.000058452046,0.00011355444,1.9711644e-7,0.0000014369274,1.745603e-7,0.000009240453],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991159,0.000057139485,0.00018565726,0.00008583388,0.0002773258,0.00027815727],"domain_scores_gemma":[0.999295,0.00016040137,0.00022524825,0.000024605526,0.00007377858,0.00022096057],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019169612,0.0000642636,0.00013707332,0.000013425533,0.0004468169,0.00004251218,0.00037156983,0.000033965673,0.0000682343],"category_scores_gemma":[0.000069312424,0.000024422037,0.000054346554,0.00025115995,0.00028697008,0.00016917933,0.00001939644,0.00007300406,0.0000018618385],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011615339,0.000011113156,0.9525185,0.000011199176,0.000017718477,0.000044783177,0.00033506812,0.000022909626,0.0008563837,0.0002042686,0.00032073585,0.04564569],"study_design_scores_gemma":[0.00007164822,0.00019264626,0.9973953,0.00009457738,0.000011329105,0.0000095354735,0.00039858205,0.00025898064,0.00025699908,0.00006823232,0.0011859369,0.000056234476],"about_ca_topic_score_codex":0.6354362,"about_ca_topic_score_gemma":0.99453896,"teacher_disagreement_score":0.35910276,"about_ca_system_score_codex":0.00001667625,"about_ca_system_score_gemma":0.00011602125,"threshold_uncertainty_score":0.36699146},"labels":[],"label_agreement":null},{"id":"W2117850564","doi":"10.1139/e09-023","title":"Assessment of wavelets analysis for carrier-phase multipath mitigationThis article is one of a series of papers published in this Special Issue on the theme <i>GEODESY</i>.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"GNSS positioning and interference","field":"Engineering","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Multipath propagation; Multipath mitigation; Wavelet; Computer science; Global Positioning System; Multipath interference; Algorithm; Remote sensing; Electronic engineering; Telecommunications; Geology; Artificial intelligence; Engineering","score_opus":0.02071137455044434,"score_gpt":0.256707834153724,"score_spread":0.23599645960327967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117850564","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9885027,0.000058972564,0.000116345596,0.001065537,0.00012577239,0.00008236494,0.00008993705,0.0000018421161,0.009956524],"genre_scores_gemma":[0.9986879,0.000010709928,0.0011072933,0.000081548285,0.00007540843,0.0000012035968,0.0000011752603,0.000001987076,0.000032772314],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9990871,0.000029720408,0.00040486708,0.00007831365,0.00023053496,0.00016948274],"domain_scores_gemma":[0.99932396,0.0000814988,0.00018158271,0.000101802674,0.00019019748,0.0001209518],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00057952106,0.000068593916,0.00023425889,0.00036698757,0.000070956565,0.000046804475,0.00022474818,0.00002889621,0.001262919],"category_scores_gemma":[0.00016705992,0.000050673978,0.00010572301,0.0006769144,0.0002123842,0.0002523296,0.0000023368034,0.00009551693,2.371237e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024419226,0.0007912681,0.25576043,0.00028255014,0.001748779,0.000038147668,0.07072322,0.33956942,0.26154912,0.024800435,0.011684312,0.032808144],"study_design_scores_gemma":[0.0016371219,0.0037018205,0.46099666,0.00067914656,0.0002613178,0.000011155933,0.0047810045,0.06373918,0.45931113,0.0015060118,0.003015394,0.00036008056],"about_ca_topic_score_codex":0.00090216595,"about_ca_topic_score_gemma":0.01012779,"teacher_disagreement_score":0.27583024,"about_ca_system_score_codex":0.000014334917,"about_ca_system_score_gemma":0.00031674426,"threshold_uncertainty_score":0.99965006},"labels":[],"label_agreement":null},{"id":"W2117958821","doi":"10.1139/e11-031","title":"U–Pb ages, geochemistry, and tectonomagmatic history of the Cambro-Ordovician Annidale Group: a remnant of the Penobscot arc system in southern New Brunswick?<sup>1</sup>This article is one of a series of papers published in this <i>CJES Special Issue: In honour of Ward Neale</i> on the theme of Appalachian and Grenvillian geology.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Geological Survey of Canada","funders":"Northwestern University","keywords":"Geology; Ordovician; Andesites; Geochemistry; Magmatism; Basalt; Felsic; Paleozoic; Island arc; Group (periodic table); Forearc; Volcanic rock; Back-arc basin; Continental arc; Volcanic arc; Paleontology; Mafic; Tectonics; Andesite; Subduction; Volcano","score_opus":0.011122029740652016,"score_gpt":0.16025290864683897,"score_spread":0.14913087890618695,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117958821","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99238324,0.0021655096,1.7435595e-7,0.0017781281,0.00006499955,0.00013754009,0.000037755377,6.981156e-7,0.0034319495],"genre_scores_gemma":[0.99952644,0.00004509709,0.00012391013,0.00008082823,0.000052195624,3.192693e-7,8.7160385e-7,0.0000018157748,0.00016850827],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981331,0.0002313063,0.0007873884,0.00016283226,0.00035573592,0.00032960423],"domain_scores_gemma":[0.9985561,0.00021927686,0.0007425466,0.00020944916,0.00007390298,0.00019873437],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014337761,0.00013605533,0.0005391547,0.00019980497,0.00006608225,0.000011598374,0.0005677819,0.0000813908,0.002056439],"category_scores_gemma":[0.00036189958,0.00007052293,0.000118851305,0.0007002332,0.0019461134,0.00016591877,0.000033094228,0.00025031148,6.129648e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043252716,0.00003433818,0.98762107,0.0001224385,0.00002046146,0.000001999589,0.008604805,0.000315887,0.0023612804,0.00007181144,0.00006469459,0.00073797815],"study_design_scores_gemma":[0.0003356537,0.00023565162,0.9845827,0.0004360785,0.00003586617,0.000022698294,0.0096711125,0.0005812055,0.0032663196,0.00040117322,0.00033492214,0.00009659419],"about_ca_topic_score_codex":0.2165011,"about_ca_topic_score_gemma":0.5463617,"teacher_disagreement_score":0.3298606,"about_ca_system_score_codex":0.000010816318,"about_ca_system_score_gemma":0.000633215,"threshold_uncertainty_score":0.9988558},"labels":[],"label_agreement":null},{"id":"W2118435528","doi":"10.1139/e10-072","title":"On gregarious behavior in<i>Albertosaurus</i>This article is one of a series of papers published in this Special Issue on the theme<i>Albertosaurus</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; University of Alberta","funders":"","keywords":"Assemblage (archaeology); Canyon; Geology; Paleontology; Taphonomy; Cretaceous; Archaeology; Taxon; History; Geomorphology","score_opus":0.013104181781925378,"score_gpt":0.2030748165405815,"score_spread":0.1899706347586561,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118435528","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93976986,0.00017444302,7.224796e-8,0.0057412074,0.0010882715,0.00012153082,0.000052108357,0.0000014766354,0.053051002],"genre_scores_gemma":[0.9982741,0.000028919274,0.00012331552,0.00086187193,0.00031677485,8.8608255e-7,0.000002394729,0.0000018654085,0.0003898596],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983149,0.00015950672,0.0005315769,0.00021387788,0.00032448777,0.00045560434],"domain_scores_gemma":[0.998681,0.00047566945,0.00031395818,0.00019008727,0.00008420562,0.0002550478],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012354533,0.00013647349,0.00031944038,0.00049491914,0.00021086859,0.000043496482,0.0006620578,0.00014959254,0.055953894],"category_scores_gemma":[0.0006542289,0.000089421046,0.00009003644,0.00071150693,0.0014933744,0.00040589808,0.000006666459,0.0005515356,0.00004668629],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013268698,0.000050015322,0.9905643,0.0000044361736,0.000011045236,0.000059200996,0.0018965779,0.00010831717,0.00062720274,0.0013022507,0.0018423904,0.0034016045],"study_design_scores_gemma":[0.00030497188,0.00096560316,0.9819814,0.00004706917,0.000010666834,0.000093443705,0.00044912583,0.00006437918,0.0015097078,0.0016295753,0.012825425,0.00011865063],"about_ca_topic_score_codex":0.032595437,"about_ca_topic_score_gemma":0.9140634,"teacher_disagreement_score":0.881468,"about_ca_system_score_codex":0.0000033735869,"about_ca_system_score_gemma":0.0008889944,"threshold_uncertainty_score":0.9738466},"labels":[],"label_agreement":null},{"id":"W2118440258","doi":"10.1139/cjes-2014-0188","title":"Preliminary study on the pore characterization of lacustrine shale reservoirs using low pressure nitrogen adsorption and field emission scanning electron microscopy methods: a case study of the Upper Jurassic Emuerhe Formation, Mohe basin, northeastern China","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"China Geological Survey; National Science Foundation","keywords":"Oil shale; Geology; Characterization (materials science); Adsorption; Scanning electron microscope; Mineralogy; Pore water pressure; Green River Formation; Geotechnical engineering; Chemistry; Materials science; Paleontology","score_opus":0.03184907825861568,"score_gpt":0.28946335770903864,"score_spread":0.257614279450423,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118440258","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99864125,0.00014665586,0.000535878,0.00027429228,0.00008803713,0.0002806088,0.0000052046607,0.0000034188547,0.000024633093],"genre_scores_gemma":[0.9998225,0.0000040105933,0.00010021756,0.00001674159,0.000032102336,0.000002208839,9.948756e-7,0.0000065559375,0.000014673891],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987851,0.0002944151,0.0003869138,0.000094373274,0.00028738752,0.00015180366],"domain_scores_gemma":[0.999197,0.000044041408,0.00027188478,0.00015291211,0.00017548043,0.00015864873],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001101226,0.000100075005,0.00018300024,0.000265812,0.00022201095,0.00006954643,0.00022362053,0.00003657962,0.0000075246808],"category_scores_gemma":[0.00013711328,0.00005741732,0.00004576699,0.0005869419,0.00006789243,0.00037928927,0.000019693578,0.00017510273,1.05356186e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009554742,0.00017291294,0.7491214,0.00008019829,0.00020929093,0.00007364658,0.05137143,0.134873,0.06318683,0.000004377248,0.000055199085,0.0007561197],"study_design_scores_gemma":[0.0015980342,0.004067123,0.12580314,0.00073228334,0.00051822135,0.0009182433,0.12894402,0.62663066,0.110198356,0.00008067827,0.000112247304,0.00039697648],"about_ca_topic_score_codex":0.0015761739,"about_ca_topic_score_gemma":0.0046518897,"teacher_disagreement_score":0.6233183,"about_ca_system_score_codex":0.000011975826,"about_ca_system_score_gemma":0.0002361612,"threshold_uncertainty_score":0.25958636},"labels":[],"label_agreement":null},{"id":"W2118464834","doi":"10.1139/e01-067","title":"Sequence stratigraphy, paleoclimate patterns, and vertebrate fossil preservation in JurassicCretaceous strata of the Junggar Basin, Xinjiang Autonomous Region, People's Republic of China","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":122,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Geographic Society","keywords":"Geology; Paleontology; Unconformity; Cretaceous; Structural basin; Sedimentary rock; Tectonic uplift; Paleoclimatology; Tectonics; Stratigraphy; Climate change; Oceanography","score_opus":0.027481254781438227,"score_gpt":0.21614404954311764,"score_spread":0.1886627947616794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118464834","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954075,0.0015821208,0.000030437543,0.0014610811,0.0001236441,0.0000832408,0.000031872954,0.0000019414297,0.0012781438],"genre_scores_gemma":[0.9993936,0.00038249098,0.00013437032,0.000048569927,0.00001529601,2.0399229e-7,0.0000022021984,8.449004e-7,0.000022455417],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988711,0.000091188245,0.00043828515,0.00012294416,0.00022675643,0.0002497624],"domain_scores_gemma":[0.9991806,0.00006948682,0.00032355686,0.000117528994,0.00012366798,0.0001851619],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00068117987,0.00008766277,0.00018774057,0.00023831794,0.00022083506,0.00011263561,0.0004327064,0.000045640976,0.00019510339],"category_scores_gemma":[0.00017418432,0.000054017433,0.00004621704,0.00089969,0.0003992518,0.001002112,0.0000064043697,0.00013359862,5.3494074e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004432606,0.0000033160277,0.99505407,0.000028222872,0.0000033655722,0.000011805947,0.00038573556,0.0012544795,0.000006915498,0.00020068309,0.0000121318835,0.0030348264],"study_design_scores_gemma":[0.00010229858,0.00021393281,0.9933962,0.00010863426,0.000006159863,0.0001602104,0.0004927634,0.0038175585,0.00004328814,0.0013784077,0.00021556673,0.00006493648],"about_ca_topic_score_codex":0.027244428,"about_ca_topic_score_gemma":0.66480887,"teacher_disagreement_score":0.6375644,"about_ca_system_score_codex":0.00000116097,"about_ca_system_score_gemma":0.0009473516,"threshold_uncertainty_score":0.97923326},"labels":[],"label_agreement":null},{"id":"W2118492269","doi":"10.1139/e08-046","title":"Holocene fluctuations in Arctic sea-ice cover: dinocyst-based reconstructions for the eastern Chukchi SeaThis article is one of a series of papers published in this Special Issue on the theme <i>Polar Climate Stability Network</i>.GEOTOP Publication 2008-0023.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Dinocyst; Geology; Holocene; Oceanography; Sea ice; Terrigenous sediment; Arctic ice pack; Arctic; Palynology; Ice core; Physical geography; Paleontology; Sediment; Pollen; Geography","score_opus":0.0374810286320764,"score_gpt":0.22934441740250416,"score_spread":0.19186338877042777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118492269","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9767573,0.00034853464,0.0000057821285,0.018075874,0.00033208635,0.00034353617,0.00015552746,0.0000020076984,0.003979369],"genre_scores_gemma":[0.99889666,0.000102741215,0.00029698916,0.00044928206,0.00017691475,0.0000039912534,0.0000085374195,0.0000017719428,0.00006309349],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99818015,0.00032249134,0.0005253029,0.00018822849,0.0003038093,0.0004799961],"domain_scores_gemma":[0.997825,0.0011596468,0.00031287404,0.00021464603,0.00031234862,0.00017548433],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0029454306,0.00009926373,0.0002452942,0.00029019348,0.0006768633,0.00006384443,0.00050989614,0.00007864249,0.013710228],"category_scores_gemma":[0.0010827259,0.000063104984,0.000081697566,0.001139463,0.001946916,0.0004866516,0.000007289773,0.00032008346,0.000016859423],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007996239,0.00001843576,0.99478525,0.000012619038,0.000012559017,0.0000032793446,0.00082878064,0.0034957048,0.000005163213,0.00015595197,0.00036345955,0.0002388393],"study_design_scores_gemma":[0.000330789,0.00029604044,0.9904147,0.00004480897,0.00001165881,0.000053256306,0.00077483413,0.0056676087,0.00025757405,0.00050365285,0.0015745744,0.000070516304],"about_ca_topic_score_codex":0.009530727,"about_ca_topic_score_gemma":0.30433792,"teacher_disagreement_score":0.2948072,"about_ca_system_score_codex":0.0000036252982,"about_ca_system_score_gemma":0.0014044639,"threshold_uncertainty_score":0.9970649},"labels":[],"label_agreement":null},{"id":"W2118644610","doi":"10.1139/e00-090","title":"Oxygen isotope systematics of the Precambrian basement of Alberta: implications for Paleoproterozoic and Phanerozoic tectonics in northwestern Alberta","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Precambrian; Basement; Geochemistry; Amphibole; Isotopes of oxygen; Sedimentary rock; Paleontology; Quartz","score_opus":0.01580755466199743,"score_gpt":0.20364723991987235,"score_spread":0.18783968525787492,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118644610","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99648243,0.000586949,0.000008945585,0.001379327,0.00004373148,0.00021497835,0.000040779003,4.0493737e-7,0.0012424479],"genre_scores_gemma":[0.9993523,0.000030628686,0.00030085514,0.0000918793,0.000017324974,0.000001370204,0.000002557696,8.5849877e-7,0.00020225433],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989554,0.000055932214,0.00048726035,0.0001264816,0.00014346019,0.00023143011],"domain_scores_gemma":[0.9990584,0.00026839087,0.00025705315,0.00011987281,0.000081667895,0.00021459848],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046624214,0.000082020146,0.0002493169,0.000115463794,0.00013064087,0.00003056633,0.00039691495,0.000036331327,0.0008898935],"category_scores_gemma":[0.00012618872,0.000046362835,0.000094239316,0.0004707323,0.00033589595,0.00011047258,0.0000049114037,0.00006900313,0.00000220021],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004916807,0.0000072257462,0.9944042,0.000042197385,0.000012885857,4.2045588e-7,0.00021756269,0.001929251,0.00004750188,0.000053874024,0.0000057414277,0.0032742347],"study_design_scores_gemma":[0.00016202535,0.00020279204,0.99540436,0.00011521769,0.000030413661,0.000022538712,0.00012655201,0.0017374026,0.00018488515,0.001314762,0.00063308206,0.00006597249],"about_ca_topic_score_codex":0.16064602,"about_ca_topic_score_gemma":0.96107286,"teacher_disagreement_score":0.80042684,"about_ca_system_score_codex":0.0000013292009,"about_ca_system_score_gemma":0.0002832082,"threshold_uncertainty_score":0.974371},"labels":[],"label_agreement":null},{"id":"W2118963723","doi":"10.1139/e01-085","title":"Magnetostratigraphic and biostratigraphic correlation of late Campanian and Maastrichtian marine and continental strata from the Red Deer Valley to the Cypress Hills, Alberta, Canada","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; University of Alberta","funders":"","keywords":"Geology; Biostratigraphy; Paleontology; Palynology; Magnetostratigraphy; Chronostratigraphy; Paleomagnetism; Pollen; Sedimentary rock","score_opus":0.01149576125556157,"score_gpt":0.17104328099524377,"score_spread":0.1595475197396822,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118963723","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9827374,0.008151654,0.0000030919061,0.0059531378,0.00021363082,0.0001290327,0.00017080051,0.0000011300691,0.0026400788],"genre_scores_gemma":[0.99928063,0.00025448977,0.00018416872,0.00020596368,0.000043468237,2.2659941e-7,0.0000039090596,7.4475844e-7,0.000026388861],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99887913,0.00011194647,0.0003131569,0.00018310464,0.00023327289,0.00027940518],"domain_scores_gemma":[0.9988235,0.000353807,0.00019782908,0.000107758344,0.000052379986,0.00046470467],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003534706,0.00013154041,0.0001864625,0.00013673468,0.00055846863,0.00015389449,0.0002962531,0.000054495442,0.00032142978],"category_scores_gemma":[0.00008752083,0.00007715647,0.000030274887,0.0003670894,0.00082668266,0.00025595727,0.0000028993397,0.00019424033,3.9271472e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008157509,0.0000015987653,0.98603463,0.0000023352413,0.000022264932,0.00001855978,0.0005152966,0.00006243615,0.000011625276,0.000057198537,0.00034660948,0.012919256],"study_design_scores_gemma":[0.00018892092,0.0002508086,0.9960176,0.000028702625,0.0000306039,0.00011908907,0.0005765265,0.0016882728,0.000011297071,0.00018357045,0.00080861745,0.000096035714],"about_ca_topic_score_codex":0.9031941,"about_ca_topic_score_gemma":0.99960566,"teacher_disagreement_score":0.09641151,"about_ca_system_score_codex":5.792766e-7,"about_ca_system_score_gemma":0.00034935915,"threshold_uncertainty_score":0.42953455},"labels":[],"label_agreement":null},{"id":"W2119189144","doi":"10.1139/e07-062","title":"The Eocene–Oligocene magmatic hiatus in the south-central Canadian Cordillera: a capture of the Kula Plate by the Pacific Plate?","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University; Victoria Park; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University","keywords":"Geology; Subduction; Magmatism; Pacific Plate; Forearc; Basalt; Paleontology; Andesite; Convergent boundary; Continental margin; Volcanic arc; Oceanic crust; Continental crust; Paleogene; Volcanic rock; Plate tectonics; Neogene; Crust; Volcano; Tectonics; Structural basin","score_opus":0.012217423308245719,"score_gpt":0.16674250649326358,"score_spread":0.15452508318501787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119189144","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9767582,0.0040504597,0.0000011884027,0.013704889,0.0002856598,0.00015879972,0.00008844815,0.0000015053104,0.0049508912],"genre_scores_gemma":[0.99872345,0.00010743786,0.000023707464,0.00091993355,0.0000702575,6.637222e-7,0.0000026291625,0.0000014881392,0.00015042309],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99768543,0.00024964687,0.00043634296,0.00016818424,0.00064345653,0.000816947],"domain_scores_gemma":[0.9985216,0.00031317322,0.00027206665,0.00022190258,0.00011349993,0.0005577236],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0012123393,0.0001554483,0.00023271251,0.00011436143,0.001592859,0.00015505144,0.0015749931,0.00007156734,0.00089973945],"category_scores_gemma":[0.0003331055,0.00005486894,0.00017936413,0.0011657992,0.0017499148,0.0001271065,0.0000091139045,0.00048043186,0.000016158829],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008205795,0.0000056045806,0.99146587,0.0000031505715,0.00002427069,0.000071893235,0.0022978391,0.0028207938,0.000010029911,0.00006959635,0.0023697908,0.00085298216],"study_design_scores_gemma":[0.00015178522,0.00008184239,0.9833858,0.000037126323,0.000025599214,0.00030239555,0.0036706375,0.002044261,0.00003973199,0.0013525855,0.008786144,0.00012207722],"about_ca_topic_score_codex":0.45648897,"about_ca_topic_score_gemma":0.9652697,"teacher_disagreement_score":0.5087807,"about_ca_system_score_codex":0.000007256026,"about_ca_system_score_gemma":0.0017382633,"threshold_uncertainty_score":0.9997069},"labels":[],"label_agreement":null},{"id":"W2119202286","doi":"10.1139/cjes-2014-0030","title":"Quartz arenites of the Cambro–Ordovician Kamouraska Formation, Quebec Appalachians, Canada: II. Eolian sands in deep-sea sedimentary gravity-flow deposits","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Arenite; Submarine canyon; Aeolian processes; Abyssal plain; Geochemistry; Quartz; Micrite; Canyon; Geomorphology; Sedimentary rock; Paleontology; Clastic rock; Sediment; Structural basin; Facies","score_opus":0.016674356934488425,"score_gpt":0.20979893109279013,"score_spread":0.1931245741583017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119202286","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99046654,0.0025013585,0.000004596398,0.005068762,0.0006954049,0.00011657357,0.000060849365,0.0000018605447,0.0010840886],"genre_scores_gemma":[0.9989957,0.00001617229,0.00022817479,0.00056028174,0.000058434907,5.147797e-7,0.000010431989,0.0000017009559,0.00012856715],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980056,0.00030174473,0.00046671776,0.00014780748,0.00049580913,0.0005822785],"domain_scores_gemma":[0.9985641,0.0001462076,0.00026045166,0.00013418008,0.0001961232,0.00069889025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011983947,0.00013077701,0.00026041773,0.0003973852,0.0006087267,0.000051413474,0.0007705924,0.00008622706,0.000248612],"category_scores_gemma":[0.00017489205,0.00008893804,0.00006254956,0.00085009105,0.00076768803,0.00044962965,0.000013148494,0.00037704306,0.0000059531494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011930752,0.0000052892156,0.9919443,0.000009432487,0.000010360846,0.00004948854,0.0013686846,0.005492871,0.0000014474166,0.000030017392,0.00051726674,0.0005589037],"study_design_scores_gemma":[0.0002850701,0.00016203763,0.99303484,0.0000592388,0.000012230123,0.00022734403,0.0023925162,0.0023026569,0.00008015975,0.0002755122,0.0010620637,0.00010635738],"about_ca_topic_score_codex":0.9462324,"about_ca_topic_score_gemma":0.9999843,"teacher_disagreement_score":0.05375194,"about_ca_system_score_codex":0.000007705885,"about_ca_system_score_gemma":0.00960568,"threshold_uncertainty_score":0.99600893},"labels":[],"label_agreement":null},{"id":"W2119355617","doi":"10.1139/e03-043","title":"Paleotopographic reconstructions of the eastern outlets of glacial Lake Agassiz","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Smithsonian Institution","keywords":"Geology; Glacial lake; Glacial period; Shelf ice; Drainage basin; Geomorphology; Oceanography; Structural basin; Stage (stratigraphy); Hydrology (agriculture); Physical geography; Paleontology; Ice stream; Sea ice; Cryosphere; Geography","score_opus":0.02655579095285133,"score_gpt":0.22602348805782974,"score_spread":0.19946769710497841,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119355617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9808246,0.0006153294,0.000004804621,0.00040330793,0.00093047903,0.000053385225,0.000023503007,8.026702e-7,0.017143792],"genre_scores_gemma":[0.99952614,0.000021231754,0.00027594122,0.000044598746,0.000024749434,8.535331e-8,4.3970812e-7,6.7113143e-7,0.000106142244],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988302,0.00023930513,0.0003151475,0.000094499286,0.00022279599,0.00029806074],"domain_scores_gemma":[0.99909717,0.00014223157,0.00026298512,0.00010736623,0.0001420644,0.000248159],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010265312,0.00006483506,0.00017868889,0.0003261961,0.00033883762,0.0000189971,0.0004363545,0.00006576598,0.0021329431],"category_scores_gemma":[0.00030893137,0.000041196345,0.00011125667,0.0006614117,0.0024193688,0.00013974957,0.0000028309667,0.00020896463,0.000011437004],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003140369,0.0000023772286,0.9989139,0.000004926749,0.000010934934,0.000009049012,0.000119066506,0.00022057763,0.0000031571262,0.00039108805,0.0000144460655,0.00030736264],"study_design_scores_gemma":[0.00012112351,0.0001393452,0.995423,0.000029869352,0.000009669478,0.0004253532,0.00033988772,0.000047105335,0.00015867446,0.0015514354,0.0017094036,0.000045115765],"about_ca_topic_score_codex":0.0011736053,"about_ca_topic_score_gemma":0.75224304,"teacher_disagreement_score":0.7510694,"about_ca_system_score_codex":1.2654057e-7,"about_ca_system_score_gemma":0.0014488068,"threshold_uncertainty_score":0.99877924},"labels":[],"label_agreement":null},{"id":"W2119382708","doi":"10.1139/e10-031","title":"Uplift of the Tug Hill Plateau in northern New York State","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Shell (Canada); Effigis (Canada)","funders":"U.S. Geological Survey; New York State Energy Research and Development Authority","keywords":"Geology; Plateau (mathematics); Precambrian; Escarpment; Colorado plateau; Volcanic plateau; Basement; Paleontology; Geomorphology; Tectonics; Shear zone; Geochemistry; Archaeology; Geography","score_opus":0.014751685957043,"score_gpt":0.1779107421071599,"score_spread":0.16315905615011692,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119382708","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944398,0.00044787172,0.0000017713182,0.0019854663,0.00042355896,0.0000313418,0.000016053931,0.0000011146985,0.0026530558],"genre_scores_gemma":[0.9992931,0.000006320342,0.00029864415,0.00017610432,0.00007011863,2.6401384e-8,7.866799e-7,6.218323e-7,0.00015425959],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895734,0.000044975735,0.00032083783,0.00011429229,0.00025462813,0.0003079321],"domain_scores_gemma":[0.9990246,0.00010869286,0.00019832891,0.00009520827,0.000060353148,0.00051280414],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00074052386,0.00007532507,0.00016819948,0.00015227428,0.00013853263,0.00004850136,0.00064538606,0.000040032224,0.003289491],"category_scores_gemma":[0.000276078,0.000039225877,0.00010357145,0.0007552651,0.0005264611,0.0001267608,0.000005878189,0.00031192476,0.000028820277],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000027157575,0.000002198327,0.9905734,0.0000012273525,0.000003865077,0.000007616878,0.00014285237,0.0038709806,0.00012334637,0.000028292348,0.000067137385,0.005176384],"study_design_scores_gemma":[0.00008794688,0.00006971808,0.98467606,0.000015590667,0.0000057190045,0.000026929998,0.000104841485,0.00062900264,0.0003302077,0.010458223,0.0035310048,0.00006473336],"about_ca_topic_score_codex":0.17364939,"about_ca_topic_score_gemma":0.98590523,"teacher_disagreement_score":0.81225586,"about_ca_system_score_codex":6.3573106e-7,"about_ca_system_score_gemma":0.0009663544,"threshold_uncertainty_score":0.99762166},"labels":[],"label_agreement":null},{"id":"W2119419485","doi":"10.1139/e09-019","title":"Dolomitization of the Lower Ordovician Watts Bight Formation of the St. George Group, western Newfoundland: evidence of hydrothermal fluid alterationGeological Survey of Canada Contribution 20080544.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Government of Newfoundland and Labrador; Memorial University of Newfoundland","funders":"Natural Resources Canada","keywords":"Dolomitization; Dolomite; Geology; Calcite; Diagenesis; Petrography; Ordovician; Geochemistry; Hydrothermal circulation; Carbonate; Fluid inclusions; Seawater; Meteoric water; Mineralogy; Unconformity; Anhydrite; Paleontology; Sedimentary rock; Facies; Oceanography; Chemistry","score_opus":0.02299985655730894,"score_gpt":0.22110053915048059,"score_spread":0.19810068259317165,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119419485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99584156,0.002147465,0.00019447993,0.0006444097,0.00039540904,0.0001477442,0.00010865681,6.242779e-7,0.000519634],"genre_scores_gemma":[0.9998284,0.000025413095,0.000039850158,0.00007302441,0.000022227574,1.2822552e-7,0.0000030541166,3.272746e-7,0.000007584177],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99831444,0.00038879437,0.000578168,0.00008907422,0.0004055011,0.00022401898],"domain_scores_gemma":[0.99841464,0.00023597656,0.0007533356,0.000118586904,0.0003487437,0.00012870421],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001503578,0.00008349258,0.0002332802,0.00011070133,0.00027092407,0.00001926263,0.00048399586,0.00006341404,0.00009866341],"category_scores_gemma":[0.00041254974,0.000046011177,0.00007558819,0.000535858,0.00064210675,0.0004913437,0.0000016282715,0.00010908419,1.1709225e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037727954,0.0000076559,0.9961136,0.000007316324,0.0000068161717,0.0000016697543,0.000113091475,0.0020291437,0.0005318206,0.00012193499,0.000021056192,0.0010081572],"study_design_scores_gemma":[0.00014630082,0.00045051277,0.9968196,0.00012820083,0.000011641886,0.000028048351,0.000027737819,0.00090305397,0.0012075978,0.00019861848,0.000028487066,0.000050190927],"about_ca_topic_score_codex":0.40525895,"about_ca_topic_score_gemma":0.99678344,"teacher_disagreement_score":0.5915245,"about_ca_system_score_codex":0.0000043660466,"about_ca_system_score_gemma":0.0016560076,"threshold_uncertainty_score":0.5987015},"labels":[],"label_agreement":null},{"id":"W2119853945","doi":"10.1139/cjes-2014-0108","title":"Characterization and dispersal of indicator minerals associated with the Pine Point Mississippi Valley-type (MVT) district, Northwest Territories, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Sphalerite; Geology; Bedrock; Pyrite; Galena; Geochemistry; Jarosite; Clastic rock; Mineralogy; Geomorphology; Sedimentary rock","score_opus":0.014981027598899702,"score_gpt":0.19232134346122418,"score_spread":0.17734031586232446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119853945","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9867334,0.00018521262,0.00043757874,0.011903124,0.00029877204,0.000047466692,0.000023129462,0.0000028628845,0.00036844905],"genre_scores_gemma":[0.99927646,0.0000036219194,0.00022023908,0.00016637568,0.00006313202,3.247236e-7,0.000006740319,0.0000010306021,0.00026205392],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990651,0.00005115741,0.00021007628,0.00012752537,0.00032211503,0.0002240472],"domain_scores_gemma":[0.9986914,0.00005866243,0.00035112016,0.000111028436,0.00030952462,0.00047831086],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058162474,0.000084540545,0.00014736195,0.000087790795,0.00020229965,0.0001240653,0.0005648772,0.000028913124,0.000011378713],"category_scores_gemma":[0.0004125626,0.00005061764,0.000015717796,0.00064272236,0.00029833993,0.0002889684,0.000024465098,0.000101182166,1.1340676e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001222688,0.000022982045,0.9898253,0.000015054021,0.00005991133,0.00017503863,0.0026075873,0.00040474252,0.0022418217,0.0010888942,0.002198883,0.0013475487],"study_design_scores_gemma":[0.0005560377,0.0006828096,0.89671546,0.00014605635,0.000025784819,0.00028036037,0.0009792543,0.0030185452,0.0022473165,0.00011090706,0.09494945,0.00028803572],"about_ca_topic_score_codex":0.33211765,"about_ca_topic_score_gemma":0.9384159,"teacher_disagreement_score":0.6062982,"about_ca_system_score_codex":0.000019040903,"about_ca_system_score_gemma":0.0051907706,"threshold_uncertainty_score":0.9208204},"labels":[],"label_agreement":null},{"id":"W2119931126","doi":"10.1139/e02-061","title":"A new Late Cretaceous (Turonian) basal euteleostean fish from Lac des Bois of the Northwest Territories of Canada","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Muséum National d'Histoire Naturelle","keywords":"Cretaceous; Geology; Paleontology; Basal (medicine); Genus; Biology; Zoology","score_opus":0.014883313738942139,"score_gpt":0.17498544901995874,"score_spread":0.1601021352810166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119931126","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891178,0.0035849237,0.0000040079044,0.0025592537,0.0014605989,0.000037701036,0.0005115853,0.0000013221701,0.0027228098],"genre_scores_gemma":[0.9985334,0.000045305154,0.00055945234,0.0003246672,0.00018768356,4.1261952e-8,0.000004703079,0.0000010232202,0.00034367607],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988525,0.00011055988,0.00033554446,0.000119110104,0.00023059023,0.000351686],"domain_scores_gemma":[0.99891365,0.00016915106,0.00028851733,0.00010798267,0.00011212009,0.0004085971],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002594322,0.0000949125,0.0002121855,0.00009700675,0.0003801054,0.000021154814,0.000600278,0.00006215281,0.0024949322],"category_scores_gemma":[0.00018487945,0.00006220431,0.00006778064,0.00032934366,0.0011169171,0.00022262007,0.000005390561,0.00015554059,0.0000027501444],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000069007124,0.0000017329181,0.99399966,0.0000026407222,0.000016940932,0.00003254905,0.00041432356,0.00068538723,0.0000069885677,0.000009578879,0.002217566,0.0026057144],"study_design_scores_gemma":[0.00011782458,0.00018235685,0.97886115,0.00003296033,0.0000129850805,0.000071291186,0.0001883669,0.0002667233,0.000094545234,0.00032664035,0.019773364,0.00007176947],"about_ca_topic_score_codex":0.96807265,"about_ca_topic_score_gemma":0.9999186,"teacher_disagreement_score":0.03184597,"about_ca_system_score_codex":0.0000045536085,"about_ca_system_score_gemma":0.003015704,"threshold_uncertainty_score":0.9984169},"labels":[],"label_agreement":null},{"id":"W2119977944","doi":"10.1139/e03-039","title":"Contractional uplift of deep crustal rocks along the Legs Lake shear zone, western Churchill Province, Canadian Shield","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Granulite; Shear zone; Metamorphism; Mylonite; Geochemistry; Zircon; Orogeny; Metamorphic rock; Metamorphic facies; Geochronology; Craton; Eclogite; Petrology; Geomorphology; Facies; Subduction; Tectonics; Seismology","score_opus":0.011265958973228768,"score_gpt":0.18651698833915922,"score_spread":0.17525102936593046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119977944","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9727641,0.0013235766,0.00009275716,0.0027060614,0.00033367565,0.00008857317,0.00008262892,0.000002712152,0.022605928],"genre_scores_gemma":[0.99851805,0.000019499465,0.00025456914,0.00079914846,0.00010340933,2.2252249e-7,0.0000061474016,0.000001484817,0.00029745413],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99827373,0.00010231858,0.00042397596,0.00019302066,0.00041370507,0.00059326226],"domain_scores_gemma":[0.99817646,0.00022267838,0.00022931526,0.00011087648,0.00015562307,0.001105052],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009249758,0.00013606243,0.00025530995,0.00028250276,0.0005879506,0.00013777995,0.0005355234,0.0000759955,0.012734663],"category_scores_gemma":[0.0003298571,0.00008012733,0.00015396753,0.00057062134,0.0007784429,0.00031936355,0.0000038536136,0.00032117203,0.00004647125],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004908189,0.000004854933,0.99029887,0.0000031836425,0.00002270784,0.000067632136,0.000095109135,0.007396609,0.000008057637,0.0002685568,0.00010723513,0.0017222948],"study_design_scores_gemma":[0.00015089782,0.00022886254,0.94946724,0.000021796048,0.00003198278,0.00025556918,0.0005083057,0.00072402385,0.0001234008,0.0012923698,0.047036003,0.00015954088],"about_ca_topic_score_codex":0.5541327,"about_ca_topic_score_gemma":0.9988175,"teacher_disagreement_score":0.44468483,"about_ca_system_score_codex":0.0000030980955,"about_ca_system_score_gemma":0.0024663417,"threshold_uncertainty_score":0.9881678},"labels":[],"label_agreement":null},{"id":"W2120203875","doi":"10.1139/e07-055","title":"Ductile strain partitioning in micritic limestones, Calabria, Italy: the roles and mechanisms of intracrystalline and intercrystalline deformation","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Geology; Calcite; Mineralogy; Deformation (meteorology); Dynamic recrystallization; Grain size; Strain partitioning; Grain boundary; Grain Boundary Sliding; Strain (injury); Microstructure; Materials science; Composite material; Tectonics","score_opus":0.01085902303162583,"score_gpt":0.19572843883478103,"score_spread":0.1848694158031552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120203875","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966695,0.0012225457,0.0006276057,0.0011648262,0.000044704615,0.000034711855,0.000019711915,0.0000010947383,0.00021529853],"genre_scores_gemma":[0.9987479,0.000038325725,0.0010482647,0.00012432587,0.000028836806,6.07213e-8,0.0000041566173,5.2985007e-7,0.000007625493],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999182,0.000037126716,0.00033014765,0.00008757643,0.00014250218,0.00022068789],"domain_scores_gemma":[0.9994136,0.00014551084,0.0001152392,0.00003407292,0.00006430854,0.00022725693],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014436018,0.00006245131,0.00013804417,0.00018208279,0.00013856501,0.000059541417,0.0001287317,0.00003082655,0.00040269582],"category_scores_gemma":[0.00016917118,0.00003709092,0.000028119726,0.00032204005,0.0005049676,0.00025402088,0.000005094307,0.00011756462,9.107928e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032208285,0.000018005368,0.9549564,0.00003410184,0.000026400596,0.00009765303,0.0018455904,0.004822076,0.007159899,0.0040747835,0.000010678938,0.026922205],"study_design_scores_gemma":[0.0001791447,0.0003423938,0.90359557,0.00007836891,0.000021898088,0.0002791524,0.004302898,0.005210858,0.0015800912,0.08417125,0.00013001496,0.00010835069],"about_ca_topic_score_codex":0.010149107,"about_ca_topic_score_gemma":0.6395786,"teacher_disagreement_score":0.62942946,"about_ca_system_score_codex":0.0000010402291,"about_ca_system_score_gemma":0.00010801987,"threshold_uncertainty_score":0.9964424},"labels":[],"label_agreement":null},{"id":"W2120237817","doi":"10.1139/e03-099","title":"A new stratigraphic framework for the Gaspé Belt in southern Quebec: implications for the pre-Acadian Appalachians of eastern Canada","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Natural Resources Canada; Université du Québec à Montréal","keywords":"Geology; Conglomerate; Ordovician; Orogeny; Devonian; Paleontology; Facies; Transgressive; Paleozoic; Group (periodic table); Ecological succession; Sequence (biology); Marine transgression; Conodont; Peninsula; Period (music); Sedimentary rock; Biostratigraphy; Structural basin; Archaeology; Geography","score_opus":0.019973851259058217,"score_gpt":0.21574095168486998,"score_spread":0.19576710042581177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120237817","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93806595,0.003581212,0.009532112,0.047820795,0.00020865655,0.00035478463,0.0002910002,0.0000018473206,0.00014366406],"genre_scores_gemma":[0.99673975,0.000020218195,0.0024914339,0.0005562686,0.000109122455,0.0000020075129,0.000003465278,0.0000011527593,0.00007660861],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99900067,0.000021775699,0.0003166067,0.00013215016,0.00016744425,0.00036134102],"domain_scores_gemma":[0.99855447,0.00066695415,0.00019422252,0.00011965617,0.00008636775,0.00037831656],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004654762,0.00009075697,0.00016265993,0.00009789376,0.00042043973,0.00008255788,0.0007133479,0.000045158464,0.00030772644],"category_scores_gemma":[0.00025235664,0.000045184606,0.00012672874,0.00060169253,0.00036274278,0.00008808615,0.000002812183,0.00016206277,0.0000010219394],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009804601,0.0000035816188,0.93867886,0.000005259892,0.000030119138,0.0000014012572,0.00063988747,0.046450496,0.0000074208156,0.0030215438,0.00007715655,0.01107444],"study_design_scores_gemma":[0.00017226141,0.00014842063,0.9243496,0.000036218975,0.000032807075,0.0000105419995,0.0021734617,0.0013115251,0.00001786305,0.06983943,0.0018206047,0.00008725424],"about_ca_topic_score_codex":0.987743,"about_ca_topic_score_gemma":0.9999495,"teacher_disagreement_score":0.06681789,"about_ca_system_score_codex":0.0000032845983,"about_ca_system_score_gemma":0.0037650354,"threshold_uncertainty_score":0.6679011},"labels":[],"label_agreement":null},{"id":"W2120390340","doi":"10.1139/e2012-008","title":"Timing of fault reactivation in the upper crust of the St. Lawrence rift system, Canada, by K–Ar dating of illite-rich fault rocks<sup>1</sup>GEOTOP Contribution 2012-0002.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Agence Nationale de Sécurité Sanitaire de l’Alimentation, de l’Environnement et du Travail","keywords":"Geology; Isochron; Fault (geology); Basement; Rift; Paleozoic; Devonian; Ordovician; Paleontology; Tectonics; Geochemistry","score_opus":0.01400265777348687,"score_gpt":0.19623836074326317,"score_spread":0.18223570296977631,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120390340","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99567527,0.00160699,0.000030344738,0.00071821664,0.00009555236,0.000093649,0.00020204681,9.216636e-7,0.0015770332],"genre_scores_gemma":[0.99967635,0.000014600042,0.00009115535,0.00012441791,0.000046749148,4.356293e-7,0.000013977281,8.414603e-7,0.0000314911],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980524,0.00021768587,0.00060499844,0.00012194089,0.0006064446,0.00039652042],"domain_scores_gemma":[0.99835914,0.00038349925,0.00063203566,0.0001289612,0.00027544022,0.00022091101],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017500884,0.00010492222,0.00028677756,0.00012212501,0.00023769237,0.000028011802,0.0006077746,0.000058138605,0.00075840944],"category_scores_gemma":[0.00068331725,0.000054366727,0.00008090646,0.00094155595,0.0003743141,0.00042149087,0.000009714148,0.00021102055,0.00000136334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005323077,0.000009143691,0.9835697,0.000019077988,0.000012046789,0.0000015836121,0.0003998171,0.0142419515,0.0003047611,0.00008962939,0.00046076396,0.0008862334],"study_design_scores_gemma":[0.00019649294,0.00013082389,0.9713721,0.00023331682,0.000051148825,0.000037539667,0.005784909,0.014452775,0.003777676,0.00015767492,0.0036584039,0.00014712544],"about_ca_topic_score_codex":0.70755637,"about_ca_topic_score_gemma":0.8169326,"teacher_disagreement_score":0.10937621,"about_ca_system_score_codex":0.000007782574,"about_ca_system_score_gemma":0.00066736573,"threshold_uncertainty_score":0.8304052},"labels":[],"label_agreement":null},{"id":"W2120521345","doi":"10.1139/e11-069","title":"The skull and appendicular skeleton of <i>Gryposaurus latidens</i>, a saurolophine hadrosaurid (Dinosauria: Ornithopoda) from the early Campanian (Cretaceous) of Montana, USA","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Premaxilla; Geology; Anatomy; Paleontology; Autapomorphy; Context (archaeology); Biology; Maxilla","score_opus":0.013072106375315251,"score_gpt":0.1991985290970434,"score_spread":0.18612642272172814,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120521345","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96895325,0.027537687,0.000014868196,0.0015856553,0.0006748006,0.00009736538,0.0001479574,0.0000017846415,0.0009866422],"genre_scores_gemma":[0.99881613,0.0003540372,0.00036103427,0.00021359148,0.0002145711,2.347324e-7,0.00000480716,0.0000018371668,0.000033776323],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982449,0.00029179134,0.00047082404,0.00015060918,0.00030116754,0.00054071244],"domain_scores_gemma":[0.99804205,0.0007624473,0.00047296155,0.00017369924,0.00010326084,0.00044561314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016199428,0.00014008656,0.00029893263,0.00012555669,0.00074434216,0.00004230408,0.0006326856,0.000104737,0.00042051345],"category_scores_gemma":[0.00027647146,0.00007526222,0.00009501864,0.00033090083,0.0022230227,0.0003712594,0.000011634262,0.00027876644,0.000015786762],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003329167,0.000003956412,0.99748594,0.0000024425958,0.000039393028,0.000022193028,0.00048099353,0.00013213026,0.00010179831,0.0001641931,0.00018257264,0.001351084],"study_design_scores_gemma":[0.00017180775,0.00035749224,0.98897296,0.000023970719,0.000038738144,0.0003153669,0.0004196004,0.00016848149,0.00007643591,0.00066478667,0.008700582,0.00008977065],"about_ca_topic_score_codex":0.04448199,"about_ca_topic_score_gemma":0.7046554,"teacher_disagreement_score":0.6601734,"about_ca_system_score_codex":0.0000019250774,"about_ca_system_score_gemma":0.00057574414,"threshold_uncertainty_score":0.96188086},"labels":[],"label_agreement":null},{"id":"W2120648387","doi":"10.1139/e01-052","title":"A new crocodylian (Archosauria) from the basal Paleocene of the Red Deer River Valley, southern Alberta","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology; Cretaceous; Basal (medicine); Biology","score_opus":0.01917171721231934,"score_gpt":0.20007322455969664,"score_spread":0.1809015073473773,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120648387","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97699046,0.0023198114,0.000043084903,0.011520256,0.00089344574,0.00007018168,0.0000597212,0.0000015480939,0.008101519],"genre_scores_gemma":[0.9974316,0.000042161766,0.00058542745,0.0007059562,0.00029152216,8.930506e-8,0.0000028336774,0.000001215112,0.0009391942],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875647,0.00020869424,0.00027904205,0.00014919613,0.00022626808,0.00038030313],"domain_scores_gemma":[0.9987807,0.0003940921,0.0002284043,0.00016005783,0.00006680232,0.0003699267],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00057307316,0.00009957087,0.00016447573,0.000081177284,0.0005407687,0.00003375117,0.001001261,0.000082674575,0.0043300292],"category_scores_gemma":[0.00022188605,0.000050880306,0.00011301047,0.0003790849,0.0012990024,0.00017644225,0.000007790735,0.00021784875,0.00006008575],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002568668,0.0000017720081,0.9949678,4.2847466e-7,0.000019187835,0.000016109623,0.00090741203,0.00052270514,0.000014217716,0.000030921747,0.0009783714,0.0025153584],"study_design_scores_gemma":[0.00018323647,0.00010397992,0.97124267,0.000024950526,0.000015981912,0.00010984205,0.00039326248,0.00024488024,0.000010478069,0.003211941,0.024388937,0.00006986024],"about_ca_topic_score_codex":0.25817883,"about_ca_topic_score_gemma":0.9573538,"teacher_disagreement_score":0.69917494,"about_ca_system_score_codex":0.0000014277348,"about_ca_system_score_gemma":0.0015752396,"threshold_uncertainty_score":0.9965801},"labels":[],"label_agreement":null},{"id":"W2120807294","doi":"10.1139/e07-004","title":"Correlation of physical surfaces, bentonites, and biozones in the Cretaceous Colorado Group from the Alberta Foothills to southwest Saskatchewan, and a revision of the Belle Fourche - Second White Specks formational boundary","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Conglomerate; Cretaceous; Cenomanian; Outcrop; Paleontology; Stratotype; Group (periodic table); Lithology; Archaeology; Structural basin; Geography","score_opus":0.012460322050630433,"score_gpt":0.2044276991295984,"score_spread":0.19196737707896797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120807294","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954271,0.0019770863,0.00005871847,0.001631303,0.00008272367,0.00013465813,0.000090879716,4.985976e-7,0.0005970896],"genre_scores_gemma":[0.9992388,0.000020933676,0.00040992693,0.0002620154,0.000036878184,8.1821106e-8,0.0000066134944,7.083291e-7,0.000024064206],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99908733,0.00008765961,0.00030570556,0.000081914266,0.00026842408,0.00016898697],"domain_scores_gemma":[0.99857354,0.0009187267,0.00023787821,0.000071517694,0.00007623516,0.0001220893],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013837833,0.00007173262,0.00013315836,0.00009236137,0.00055701,0.000096473224,0.00030590597,0.000035276797,0.00022483527],"category_scores_gemma":[0.00016397233,0.00003250931,0.000034271132,0.00048471056,0.0005692959,0.00032636823,0.000014149745,0.00014542553,0.0000014808064],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016134469,0.0000054916004,0.97669387,0.000009137299,0.00000480753,0.0000012065462,0.016740223,0.0020617251,0.000012344367,0.00011063365,0.000048193055,0.004296241],"study_design_scores_gemma":[0.00010701144,0.00029330933,0.97969985,0.00006605909,0.000009084884,0.000032975207,0.008081898,0.0014890607,0.000023832275,0.0011837,0.008964014,0.000049184073],"about_ca_topic_score_codex":0.01822994,"about_ca_topic_score_gemma":0.8086087,"teacher_disagreement_score":0.79037875,"about_ca_system_score_codex":0.0000013075326,"about_ca_system_score_gemma":0.000280517,"threshold_uncertainty_score":0.9883078},"labels":[],"label_agreement":null},{"id":"W2120963076","doi":"10.1139/e07-047","title":"Conodont biostratigraphy of the latest Cambrian - Early Ordovician upper McKay Group, southeastern British Columbia","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Conodont; Geology; Biostratigraphy; Paleontology; Ordovician; Group (periodic table)","score_opus":0.012467056537457503,"score_gpt":0.19406458058690004,"score_spread":0.18159752404944254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120963076","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9681597,0.0031434349,0.00001489069,0.0002459444,0.0008605699,0.00010149414,0.00011546816,0.0000036537979,0.027354892],"genre_scores_gemma":[0.99929917,0.000011789272,0.0003754382,0.00013209203,0.000099892364,7.805203e-8,7.029258e-7,0.0000010339492,0.00007982432],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982959,0.00009998529,0.0005158551,0.00018163033,0.00034086622,0.0005657675],"domain_scores_gemma":[0.998611,0.00012874149,0.00038306115,0.00013877619,0.00011779549,0.00062064966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001442628,0.00010554669,0.00024557597,0.00020786597,0.00078050885,0.00036452044,0.0007432797,0.00010380083,0.00047054107],"category_scores_gemma":[0.00007805554,0.00009628148,0.00020481799,0.0007064893,0.0018332276,0.00039966265,0.0000014395418,0.00026510397,0.0000045205275],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000049689297,0.0000047295316,0.99110407,0.000003539701,0.000018381324,0.00007165195,0.00027523158,0.000008703744,0.000027555561,0.00004203884,0.00004295697,0.008396183],"study_design_scores_gemma":[0.00018308764,0.0003635697,0.9972619,0.000086320884,0.000016256017,0.00029265898,0.00057747425,0.00001621836,0.000023232964,0.00043592215,0.000621861,0.00012153356],"about_ca_topic_score_codex":0.47396898,"about_ca_topic_score_gemma":0.998289,"teacher_disagreement_score":0.52432,"about_ca_system_score_codex":7.2307216e-7,"about_ca_system_score_gemma":0.0007912606,"threshold_uncertainty_score":0.67546034},"labels":[],"label_agreement":null},{"id":"W2121005752","doi":"10.1139/e01-072","title":"Organic substances in cave drip waters: studies from Marengo Cave, Indiana","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Karst Systems and Hydrogeology","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Cave; Calcite; Speleothem; Spring (device); Geology; Organic matter; Hydrology (agriculture); Geochemistry; Environmental chemistry; Oceanography; Archaeology; Chemistry; Geography","score_opus":0.04162166415687395,"score_gpt":0.2120201556376091,"score_spread":0.17039849148073516,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121005752","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9677735,0.02744683,0.0000017055986,0.00080019975,0.0012351772,0.000066885426,0.000039726936,0.0000038869084,0.0026320808],"genre_scores_gemma":[0.9985788,0.00047160118,0.00018287577,0.000287833,0.00022551007,2.1446556e-7,0.0000024750939,0.0000025205807,0.0002482014],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99826884,0.00012276645,0.00048580382,0.0002318303,0.0002987138,0.00059202383],"domain_scores_gemma":[0.9988684,0.00017567916,0.00023742695,0.00011072977,0.00008660746,0.00052116107],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007235388,0.0001476409,0.0003666773,0.00055312424,0.00032444615,0.0001387258,0.0005159507,0.000074753465,0.005069555],"category_scores_gemma":[0.00013970477,0.00010667944,0.00006283879,0.0006681927,0.000634415,0.0005271054,0.0000049498562,0.00021808581,0.00020153983],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002096888,0.0000025915567,0.99258333,0.0000042496054,0.00002196705,0.00037774243,0.0039956747,0.00042587746,0.000009738009,0.000022506967,0.0004431176,0.0021110892],"study_design_scores_gemma":[0.0003499905,0.00032340045,0.9807902,0.00014533347,0.000014543969,0.00019429336,0.006110176,0.0007681088,0.0000944898,0.0011152185,0.0098451115,0.00024913458],"about_ca_topic_score_codex":0.06840861,"about_ca_topic_score_gemma":0.9138877,"teacher_disagreement_score":0.8454791,"about_ca_system_score_codex":0.000006790879,"about_ca_system_score_gemma":0.0003135098,"threshold_uncertainty_score":0.99583995},"labels":[],"label_agreement":null},{"id":"W2121011434","doi":"10.1139/e10-084","title":"A new species of <i>Sorbinichthys</i> (Teleostei: Clupeomorpha: Ellimmichthyiformes) from the Late Cretaceous of Morocco","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Cenomanian; Cretaceous; Genus; Teleostei; Paleontology; Taxon; Geology; Mediterranean sea; Mediterranean climate; Type species; Ecology; Biology; Fish <Actinopterygii>; Fishery","score_opus":0.01647011395094644,"score_gpt":0.20087473425813668,"score_spread":0.18440462030719024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121011434","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9815446,0.004646324,0.000031214768,0.0013272889,0.0014477556,0.00006062604,0.00011548697,0.00000221721,0.010824448],"genre_scores_gemma":[0.997558,0.00014758339,0.001355226,0.00024573557,0.00023504542,5.8871194e-8,0.0000066144485,0.000001316688,0.00045039962],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99869645,0.00008838309,0.0004791833,0.0001296386,0.0002392101,0.00036713647],"domain_scores_gemma":[0.9983665,0.00049475004,0.0004578181,0.00016022255,0.00012862387,0.0003921224],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007885526,0.000116469215,0.000301623,0.00015489486,0.0002729276,0.000026991102,0.0008596267,0.00011391031,0.005400214],"category_scores_gemma":[0.00023670102,0.000071669674,0.00011978023,0.00036671603,0.0016372845,0.00028450572,0.00000673305,0.00032826548,0.000059781953],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030619918,0.0000032729138,0.9939658,0.000002165515,0.000030139525,0.000021958303,0.0003980543,0.00045537762,0.0011892968,0.00018466936,0.00086190517,0.0028567412],"study_design_scores_gemma":[0.00021008454,0.00036122644,0.9715823,0.000021719778,0.000026916965,0.0001489469,0.0004094112,0.00018240153,0.000792185,0.0015999223,0.024575606,0.00008928642],"about_ca_topic_score_codex":0.034441557,"about_ca_topic_score_gemma":0.73625827,"teacher_disagreement_score":0.7018167,"about_ca_system_score_codex":7.813809e-7,"about_ca_system_score_gemma":0.0020141148,"threshold_uncertainty_score":0.99550897},"labels":[],"label_agreement":null},{"id":"W2121084722","doi":"10.1139/e04-055","title":"Description of a new enantiornithine bird from the Early Cretaceous of Hebei, northern China","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Cretaceous; Claw; China; Phalanx; Geology; Paleontology; Climb; Geography; Biology; Ecology; Anatomy; Archaeology; Engineering; Aerospace engineering","score_opus":0.02220606570394254,"score_gpt":0.19733939532287736,"score_spread":0.17513332961893482,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121084722","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909851,0.006210916,0.00013646692,0.0013767325,0.0005255308,0.000046022367,0.000048710725,0.0000026967698,0.00066783256],"genre_scores_gemma":[0.99875516,0.000060882456,0.00092520687,0.00009293527,0.00012270072,3.6873775e-8,0.0000023812713,0.0000011281131,0.00003955145],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990642,0.00007779054,0.00032908426,0.00010635984,0.00017986764,0.00024270004],"domain_scores_gemma":[0.99915177,0.00008800114,0.00032210752,0.00009071748,0.00008490533,0.00026252007],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005316025,0.00007826001,0.00018834292,0.0001434139,0.00023722154,0.000020851243,0.00045252702,0.000066182496,0.00047319554],"category_scores_gemma":[0.00015060983,0.00004661199,0.000078863566,0.00033615626,0.0009387747,0.00028158628,0.0000028142626,0.00015161805,0.000023501862],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002072521,0.0000031184097,0.9930072,0.000001239288,0.000016060545,0.000017946562,0.0009443364,0.0034386439,0.00009275223,0.000047388894,0.0000306286,0.002379965],"study_design_scores_gemma":[0.00021408657,0.0005153272,0.99296254,0.000039983235,0.000015426554,0.00011435441,0.00022046479,0.000057156212,0.00007297616,0.005148984,0.0005844945,0.000054214393],"about_ca_topic_score_codex":0.28802168,"about_ca_topic_score_gemma":0.947326,"teacher_disagreement_score":0.6593043,"about_ca_system_score_codex":0.0000018635636,"about_ca_system_score_gemma":0.0018924435,"threshold_uncertainty_score":0.71671945},"labels":[],"label_agreement":null},{"id":"W2121156519","doi":"10.1139/e00-041","title":"Petrology of a supra-subduction zone ophiolite (Elaz1g, Turkey)","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Ophiolite; Geochemistry; Schist; Metamorphic rock; Gabbro; Volcanic rock; Massif; Greenschist; Sedimentary rock; Basalt; Petrology; Seismology; Volcano; Tectonics","score_opus":0.012773199058291844,"score_gpt":0.18424866527510503,"score_spread":0.17147546621681317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121156519","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9844844,0.0013675878,0.000009697815,0.0014482304,0.0001820624,0.000024336849,0.000019710938,0.0000025613233,0.012461468],"genre_scores_gemma":[0.9984621,0.00008362484,0.00068376155,0.00022251456,0.0001346251,6.631623e-8,0.0000039148326,6.97528e-7,0.00040868693],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987963,0.00007422575,0.00036034448,0.00015304811,0.00024611043,0.00036997662],"domain_scores_gemma":[0.99904585,0.00008297541,0.00015907234,0.00007890721,0.00010678748,0.00052642555],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005720418,0.00008994529,0.00024717,0.00025893564,0.00019033071,0.00004061882,0.0003716977,0.000056564564,0.051246542],"category_scores_gemma":[0.00010321967,0.00005965217,0.0001312251,0.0006957831,0.0007610843,0.00024292324,0.0000022637635,0.00015781446,0.000119626035],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028320906,0.00001030559,0.9689356,0.0000053696535,0.000023797764,0.00006742276,0.00015046936,0.016148347,0.0002555105,0.00017153293,0.00024564832,0.013957687],"study_design_scores_gemma":[0.00021677386,0.0008325424,0.96529436,0.000021036547,0.000038241407,0.00035299992,0.00017240904,0.002067911,0.0005997276,0.007849724,0.02239837,0.00015593371],"about_ca_topic_score_codex":0.042173535,"about_ca_topic_score_gemma":0.22823635,"teacher_disagreement_score":0.18606281,"about_ca_system_score_codex":8.773995e-7,"about_ca_system_score_gemma":0.00035602468,"threshold_uncertainty_score":0.9642047},"labels":[],"label_agreement":null},{"id":"W2121497783","doi":"10.1139/e11-039","title":"Revision of the position of the Ordovician–Silurian boundary in southern Ontario: regional chronostratigraphic implications of δ<sup>13</sup>C chemostratigraphy of the Manitoulin Formation and associated strata","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ordovician; Geology; Chemostratigraphy; Paleontology; Peninsula; Excursion; Bay; Laurentia; Sedimentary depositional environment; Isotopes of carbon; Oceanography; Archaeology; Geography; Structural basin; Isotope","score_opus":0.026835495891183662,"score_gpt":0.20396612971030503,"score_spread":0.17713063381912136,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121497783","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941673,0.0014278231,0.0000038380363,0.0005819177,0.00007735879,0.00017803459,0.00013622314,7.5684363e-7,0.0034266985],"genre_scores_gemma":[0.99977237,0.000023673705,0.00015121316,0.000035194746,0.000009384283,1.919715e-7,0.000001751954,6.088638e-7,0.0000056385365],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99859995,0.00020333682,0.0006149786,0.00010789694,0.0002885472,0.00018531116],"domain_scores_gemma":[0.9985401,0.000081697995,0.0009389503,0.00018630747,0.00015580398,0.000097121854],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008278887,0.00009719221,0.00021093967,0.00020599412,0.00036243905,0.000022052098,0.0006289802,0.00008893919,0.000067079396],"category_scores_gemma":[0.00006757291,0.00005373041,0.00016008264,0.0008159731,0.0016999226,0.00034282746,0.0000030163885,0.00023324808,1.0286078e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012197982,0.000013228343,0.99295205,0.000013634438,0.000016732658,4.678392e-7,0.0042479984,0.00008391373,0.00018236553,0.00027049042,0.00001419595,0.00219273],"study_design_scores_gemma":[0.00017190156,0.0002009357,0.9941667,0.00025640277,0.000027527129,0.000031222768,0.002090335,0.00011216215,0.0006239307,0.0022460336,0.000019649136,0.000053246535],"about_ca_topic_score_codex":0.12528645,"about_ca_topic_score_gemma":0.97208226,"teacher_disagreement_score":0.84679586,"about_ca_system_score_codex":0.0000027018443,"about_ca_system_score_gemma":0.0015599872,"threshold_uncertainty_score":0.88053834},"labels":[],"label_agreement":null},{"id":"W2121597755","doi":"10.1139/e10-067","title":"High-precision U–Pb age and geochemistry of the mineralized (Ni–Cu–Co) Suwar intrusion, YemenThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Okanagan University College; University of British Columbia, Okanagan Campus; Kelowna General Hospital; University of Toronto","funders":"","keywords":"Geology; Geochemistry; Mafic; Archean; Zircon; Gabbro; Mantle (geology); Hornblende; Craton; Basalt; Ultramafic rock; Plagioclase; Tectonics; Biotite; Paleontology","score_opus":0.016842160476414045,"score_gpt":0.18623104188761092,"score_spread":0.16938888141119687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121597755","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9907513,0.00031406965,1.8890502e-7,0.0020591994,0.000089058805,0.00007288123,0.000052802596,5.4386186e-7,0.0066599525],"genre_scores_gemma":[0.999262,0.00008798099,0.0004080075,0.00011275346,0.000048962742,2.2627488e-7,0.0000014445626,9.1350324e-7,0.00007773927],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99843806,0.00013296436,0.00068570825,0.00015441467,0.00035627838,0.00023259028],"domain_scores_gemma":[0.9988397,0.000176307,0.0005556783,0.00016484196,0.00013355231,0.00012997183],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011218874,0.000101389116,0.00042197114,0.00019368924,0.00006660118,0.000012710018,0.00056668214,0.00007390136,0.031693373],"category_scores_gemma":[0.00059092505,0.00005360328,0.000098737204,0.0007772489,0.0013807133,0.00016689011,0.000025668436,0.00017827823,0.0000012239027],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018104118,0.00007645907,0.95356697,0.00003615228,0.000037900252,0.000014098396,0.0034961954,0.00016794917,0.0387328,0.00018788656,0.0005544326,0.00294812],"study_design_scores_gemma":[0.0003793902,0.00046412725,0.749661,0.00015498624,0.00002333121,0.000006731277,0.0016052626,0.00006320148,0.24127346,0.005943711,0.00034622865,0.00007852062],"about_ca_topic_score_codex":0.06779477,"about_ca_topic_score_gemma":0.2243346,"teacher_disagreement_score":0.20390591,"about_ca_system_score_codex":0.0000022171698,"about_ca_system_score_gemma":0.000241722,"threshold_uncertainty_score":0.9691918},"labels":[],"label_agreement":null},{"id":"W2121707475","doi":"10.1139/e04-035","title":"The Pelican Thrust Zone: basal detachment between the Archean Sask Craton and Paleoproterozoic Flin Flon Glennie Complex, western Trans-Hudson Orogen","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Alberta; University of Regina; Government of Saskatchewan; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Northwestern University","keywords":"Geology; Archean; Mylonite; Lineation; Shear zone; Geochemistry; Charnockite; Gneiss; Migmatite; Anatexis; Terrane; Petrology; Craton; Thrust fault; Imbrication; Tectonite; Crust; Geomorphology; Seismology; Tectonics; Metamorphic rock; Granulite; Partial melting; Facies; Structural basin","score_opus":0.031002930039263858,"score_gpt":0.2269790436514242,"score_spread":0.19597611361216036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121707475","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9742044,0.0027358495,0.000059688613,0.021970412,0.00007701562,0.00011485921,0.00003823488,0.000004196122,0.00079534925],"genre_scores_gemma":[0.9981553,0.00014011309,0.00044983154,0.000833282,0.0003429387,5.1180234e-7,0.0000055580786,0.0000016282987,0.00007084709],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99815196,0.00017002653,0.0004152762,0.0002251742,0.00044413013,0.0005934259],"domain_scores_gemma":[0.99852616,0.00032900265,0.00017323765,0.00013785831,0.00007230073,0.0007614404],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014210576,0.00015954621,0.00024911467,0.00009695824,0.0012302338,0.0003445857,0.0007539787,0.0000513178,0.0016455114],"category_scores_gemma":[0.00005669493,0.0000744852,0.00012403062,0.00038926554,0.0012944752,0.00020916203,0.000010687222,0.0003089188,0.000031197473],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000075581142,0.0000031741513,0.9321764,0.0000025745119,0.000024651481,0.000008950561,0.00030906187,0.00057848555,0.000035948266,0.000009958802,0.000074936695,0.06676828],"study_design_scores_gemma":[0.00014859696,0.00028016575,0.97479707,0.00001600015,0.000043114276,0.000039730698,0.00047339022,0.0013278744,0.00020310887,0.0009814051,0.021559792,0.00012972335],"about_ca_topic_score_codex":0.015448038,"about_ca_topic_score_gemma":0.7470613,"teacher_disagreement_score":0.7316133,"about_ca_system_score_codex":0.0000027998326,"about_ca_system_score_gemma":0.00029924276,"threshold_uncertainty_score":0.9992671},"labels":[],"label_agreement":null},{"id":"W2121970773","doi":"10.1139/e06-097","title":"Determination of alteration facies using the normative mineral alteration index: Selbaie Cu–Zn deposit, northern Abitibi greenstone belt, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; Université du Québec","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Sericite; Greenschist; Greenstone belt; Pyrophyllite; Archean; Hypogene; Covellite; Stockwork; Pyrite; Ankerite; Orthoclase; Siderite; Mineralogy; Hydrothermal circulation; Sphalerite; Plagioclase; Metamorphism; Quartz; Chalcopyrite; Copper; Chemistry","score_opus":0.014212625787277229,"score_gpt":0.20886174708212268,"score_spread":0.19464912129484546,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121970773","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9152003,0.00012937603,0.0819065,0.0014902713,0.00029436967,0.000069886475,0.0000054575867,0.0000028375646,0.0009010312],"genre_scores_gemma":[0.9953521,0.0000010183436,0.004304768,0.00013592394,0.000105416475,5.425526e-7,0.0000021297749,0.0000010710853,0.000097045944],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987737,0.000080715625,0.00039228852,0.00013300017,0.00036719043,0.0002530943],"domain_scores_gemma":[0.99876744,0.00006450956,0.00044075144,0.00012082968,0.00048263618,0.00012381341],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005077248,0.0000999349,0.00013202206,0.00014039683,0.00056983466,0.0002027008,0.0005121041,0.000033460303,0.000008054715],"category_scores_gemma":[0.000084025276,0.00007313333,0.00004145267,0.00044644822,0.00023470065,0.0007770049,0.000020010126,0.00011605508,2.6100162e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000064184524,0.00002156215,0.7465417,0.000043977965,0.000020392026,0.0001433868,0.0044231084,0.21983448,0.017835433,0.0023664073,0.00037985918,0.008383311],"study_design_scores_gemma":[0.00030270673,0.00017755988,0.44035542,0.00013338646,0.000016145781,0.0006912386,0.0006740791,0.5422593,0.012180174,0.0022436718,0.0006840895,0.00028221286],"about_ca_topic_score_codex":0.7689971,"about_ca_topic_score_gemma":0.9932594,"teacher_disagreement_score":0.32242483,"about_ca_system_score_codex":0.000036702844,"about_ca_system_score_gemma":0.002065076,"threshold_uncertainty_score":0.4382765},"labels":[],"label_agreement":null},{"id":"W2121998315","doi":"10.1139/e10-047","title":"Chilliwack composite terrane in northwest Washington: Neoproterozoic–Silurian passive margin basement, Ordovician–Silurian arc inception","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Terrane; Geology; Paleozoic; Ordovician; Basement; Devonian; Zircon; Paleontology; Island arc; Volcanic arc; Volcanic rock; Laurentia; Geochemistry; Subduction; Volcano; Tectonics; Archaeology","score_opus":0.01039370279698856,"score_gpt":0.1937530526904946,"score_spread":0.18335934989350602,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121998315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909078,0.00016040671,0.000014812373,0.0049039843,0.0005480333,0.00011845703,0.000060090115,0.000006189725,0.0032802296],"genre_scores_gemma":[0.9971666,0.000017317421,0.0016690542,0.0007478217,0.0002932006,6.495199e-7,0.000033749024,0.0000023025525,0.00006931865],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99790967,0.00010617299,0.0005582224,0.0003195506,0.0004296699,0.0006767332],"domain_scores_gemma":[0.99834526,0.00009992517,0.0003100855,0.00015331834,0.000120973615,0.0009704578],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00082011573,0.00020061027,0.00033958652,0.0005497901,0.00045846868,0.000260616,0.0007341616,0.000107695785,0.011198347],"category_scores_gemma":[0.00015968492,0.0001420964,0.00014558545,0.0010212681,0.0007089833,0.0005376896,0.000012219745,0.00062173605,0.000116681076],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001135533,0.000013164934,0.98968154,0.0000045343822,0.000009990811,0.00013365193,0.00017692512,0.0012414218,0.000640506,0.000047131954,0.000029719555,0.008010038],"study_design_scores_gemma":[0.00028385912,0.00024929427,0.9899793,0.00004660406,0.00001559284,0.000097626886,0.00019878037,0.0015929427,0.00029429724,0.0026690834,0.0043654074,0.00020716667],"about_ca_topic_score_codex":0.17829803,"about_ca_topic_score_gemma":0.9815845,"teacher_disagreement_score":0.80328643,"about_ca_system_score_codex":0.0000037016696,"about_ca_system_score_gemma":0.0004915776,"threshold_uncertainty_score":0.98970556},"labels":[],"label_agreement":null},{"id":"W2122267141","doi":"10.1139/e01-017","title":"Geochemistry and oxygen isotopic composition of the Canton Saint-Onge wollastonite deposit, central Grenville Province, Canada","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université de Montréal; Polytechnique Montréal; Université du Québec à Montréal; Université du Québec à Chicoutimi","funders":"Université de Montréal; Université du Québec à Chicoutimi; Université du Québec à Montréal","keywords":"Wollastonite; Skarn; Geology; Geochemistry; Metasomatism; Pluton; Country rock; Mineral; Diopside; Metamorphism; Titanite; Metamorphic rock; Mineralogy; Fluid inclusions; Hydrothermal circulation; Chemistry; Tectonics","score_opus":0.0064504064410420515,"score_gpt":0.15734324427410898,"score_spread":0.15089283783306692,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122267141","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949857,0.0012520137,0.000003444545,0.0012994761,0.00014804275,0.000043820837,0.000032743694,9.5054725e-7,0.0022338273],"genre_scores_gemma":[0.99942327,0.00003451536,0.00013012231,0.00025729695,0.000058711204,7.119392e-8,0.0000026890175,6.4151953e-7,0.00009265914],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99896836,0.00004073221,0.00024458178,0.00012732043,0.00027502814,0.00034394593],"domain_scores_gemma":[0.99916935,0.000050344417,0.00017273617,0.00007303341,0.000073022224,0.00046149263],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001706897,0.00008711499,0.00016015055,0.000057689715,0.00031089215,0.000049869675,0.0003304142,0.00003496739,0.00092436303],"category_scores_gemma":[0.00004710514,0.00005142754,0.00005873324,0.0003560704,0.00045249175,0.00008366376,0.000008435908,0.00012934151,8.680968e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000047285107,0.0000022852803,0.9972134,0.0000057564394,0.000009409872,0.000036103076,0.000023652401,0.00074651,0.00047769866,0.0000121519115,0.00009121451,0.001377043],"study_design_scores_gemma":[0.000089674395,0.00006238325,0.9936763,0.000031803007,0.000019096544,0.00022410873,0.00012354914,0.0014255006,0.0019093766,0.0002499519,0.0021107337,0.00007752033],"about_ca_topic_score_codex":0.9212848,"about_ca_topic_score_gemma":0.9973814,"teacher_disagreement_score":0.07609663,"about_ca_system_score_codex":0.000006652626,"about_ca_system_score_gemma":0.0012215913,"threshold_uncertainty_score":0.9999889},"labels":[],"label_agreement":null},{"id":"W2122322481","doi":"10.1139/e2012-051","title":"New multituberculate mammal from the Early Cretaceous of eastern North America","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Cretaceous; Paleontology; Yixian Formation; Cusp (singularity); Facies; Geology; Mesozoic; Aptian; Mammal; Dentition; Geometry","score_opus":0.02124971150347292,"score_gpt":0.2029378403647961,"score_spread":0.18168812886132318,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122322481","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9878441,0.004691705,0.00007614423,0.0018704423,0.0005340967,0.00006984348,0.00003201079,0.0000025466727,0.004879089],"genre_scores_gemma":[0.99757963,0.000053423177,0.0014610991,0.00041639904,0.00015210269,9.522993e-8,0.0000017053377,0.0000010258672,0.00033450904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99896306,0.000081181264,0.00028630905,0.000116126546,0.00024239051,0.00031095237],"domain_scores_gemma":[0.9988882,0.00019806146,0.00023381808,0.00009809578,0.00011874577,0.0004631133],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017962581,0.00009247227,0.00018537542,0.000103817074,0.0003394521,0.00009656689,0.0004966413,0.00003163048,0.0035773157],"category_scores_gemma":[0.000098075194,0.000054249907,0.000078224555,0.00030924156,0.0007611358,0.0003324783,0.000004620551,0.00014696458,0.00027590737],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000029205682,8.5631547e-7,0.98409176,6.6078616e-7,0.000021545951,0.000011722846,0.0009855763,0.00094860006,0.0000024658775,0.0000041395106,0.00079024397,0.013139508],"study_design_scores_gemma":[0.00010927035,0.00016493123,0.9881626,0.00001531321,0.00001321246,0.00002044527,0.0006592821,0.0008353835,0.0000034824072,0.00014925183,0.009798374,0.00006849888],"about_ca_topic_score_codex":0.38865438,"about_ca_topic_score_gemma":0.94292045,"teacher_disagreement_score":0.55426604,"about_ca_system_score_codex":8.2507756e-7,"about_ca_system_score_gemma":0.0006991617,"threshold_uncertainty_score":0.9973335},"labels":[],"label_agreement":null},{"id":"W2122829605","doi":"10.1139/e10-008","title":"An articulated embolomere skeleton (Amphibia: Anthracosauria) from the Lower Pennsylvanian (Bashkirian) of Nova Scotia","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University; Canadian Museum of Nature","funders":"","keywords":"Pennsylvanian; Tetrapod (structure); Paleontology; Nova scotia; Geology; Synapomorphy; Paleozoic; Type locality; Taxon; Carboniferous; Taxonomy (biology); Phylogenetic tree; Zoology; Biology","score_opus":0.015210125020876897,"score_gpt":0.22693951951193075,"score_spread":0.21172939449105385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122829605","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923297,0.0009140068,0.000013614359,0.0020173292,0.002494266,0.00006542836,0.00011224744,0.0000041267285,0.0020492768],"genre_scores_gemma":[0.99845743,0.000013789608,0.0008458521,0.00036407638,0.000290695,4.3994106e-8,0.000013248768,0.0000016463491,0.000013200903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99858665,0.0001669353,0.00038299966,0.00020694271,0.00021621665,0.0004402213],"domain_scores_gemma":[0.99857545,0.00026201445,0.00028992438,0.00020851557,0.00014983854,0.0005142612],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010266816,0.0001240278,0.0002354388,0.00017262754,0.0004091027,0.00006134774,0.0008053019,0.00014633653,0.0076069976],"category_scores_gemma":[0.0002242251,0.000078001074,0.0000854239,0.00043233132,0.0019875225,0.00050906406,0.0000041059884,0.0003989455,0.00010612675],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021988979,0.000011901795,0.9952801,9.678062e-7,0.00001801561,0.00005516889,0.00017129272,0.00048614858,0.0016784034,0.0001442918,0.00021212848,0.0019196152],"study_design_scores_gemma":[0.00016790602,0.000529595,0.99321127,0.000017552426,0.000018748904,0.0001808292,0.00025293507,0.0007308972,0.00020596318,0.0007951737,0.003781662,0.00010745783],"about_ca_topic_score_codex":0.07944328,"about_ca_topic_score_gemma":0.96738553,"teacher_disagreement_score":0.88794225,"about_ca_system_score_codex":9.985122e-7,"about_ca_system_score_gemma":0.0012685359,"threshold_uncertainty_score":0.9933002},"labels":[],"label_agreement":null},{"id":"W2122908316","doi":"10.1139/e08-010","title":"High-resolution seismo-stratigraphy and sedimentological properties of late- and postglacial sediments in Lac Guillaume-Delisle Estuary and Nastapoka Sound, eastern Hudson Bay","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Center for Northern Studies; Centre de Géomatique du Québec; Université du Québec à Rimouski; Geological Survey of Canada","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Fonds Québécois de la Recherche sur la Nature et les Technologies; ArcticNet; Université Laval","keywords":"Geology; Deglaciation; Bay; Fluvial; Estuary; Sedimentary rock; Moraine; Glacial period; Geomorphology; Oceanography; Paleontology; Structural basin","score_opus":0.03675864397511147,"score_gpt":0.22312383002883385,"score_spread":0.18636518605372238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122908316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99293363,0.0056070657,0.0000022673053,0.0008819022,0.00015012894,0.00008767627,0.000010366129,0.0000018958269,0.00032503874],"genre_scores_gemma":[0.9993035,0.00019431312,0.00032578598,0.00012212945,0.000027084998,2.3622881e-7,0.0000016755084,9.967857e-7,0.000024263847],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987853,0.00016410899,0.00029076976,0.00018326999,0.00021067161,0.00036585],"domain_scores_gemma":[0.99935144,0.00007521358,0.00011782213,0.000049232647,0.000063344305,0.00034292432],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007190567,0.00010481623,0.00024080378,0.00038000304,0.00036061517,0.000042596577,0.00014795746,0.00010098941,0.000087221095],"category_scores_gemma":[0.00007435428,0.000074753174,0.00002252585,0.00024467488,0.0021434627,0.00033783837,0.000010447537,0.00020385472,0.0000026780888],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000050361945,0.000005264258,0.99877995,0.0000113097785,0.000009812007,0.000102382175,0.00063675526,0.00017471502,0.000026682153,0.00004983076,0.000009632667,0.00014332098],"study_design_scores_gemma":[0.00040411795,0.00062099355,0.99553096,0.000036819674,0.000006481452,0.0006192924,0.00042139672,0.0016026202,0.00007480555,0.0005390022,0.000058006834,0.00008548519],"about_ca_topic_score_codex":0.008270094,"about_ca_topic_score_gemma":0.24059793,"teacher_disagreement_score":0.23232783,"about_ca_system_score_codex":4.4376418e-7,"about_ca_system_score_gemma":0.000346459,"threshold_uncertainty_score":0.99833393},"labels":[],"label_agreement":null},{"id":"W2122957524","doi":"10.1139/e01-056","title":"Nature of the basement to Quesnel Terrane near Christina Lake, southeastern British Columbia","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Calgary","funders":"","keywords":"Terrane; Diorite; Geology; Paleontology; Basement; Accretion (finance); Paleozoic; Conglomerate; Assemblage (archaeology); Sedimentary rock; Archaeology; Zircon; Geography","score_opus":0.013010193298533184,"score_gpt":0.1736628308787266,"score_spread":0.16065263758019344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122957524","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99138254,0.0010552738,0.000003151713,0.0022694923,0.0002551688,0.00005578931,0.000103108934,0.0000019082368,0.0048735566],"genre_scores_gemma":[0.9975535,0.000010180369,0.00040572174,0.0009879535,0.00007541075,1.1395713e-7,0.0000013125914,8.3651366e-7,0.00096491736],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988056,0.00005859166,0.00028486882,0.00014819686,0.00037675974,0.0003259851],"domain_scores_gemma":[0.99902713,0.000047669393,0.00015280428,0.000099188735,0.000116025345,0.00055716775],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041915977,0.00006630922,0.00018421478,0.000051242114,0.0004001193,0.00028723682,0.0006107106,0.000054340588,0.031809527],"category_scores_gemma":[0.00021022435,0.000050672425,0.00012813226,0.0006383572,0.00050501426,0.000106591375,0.0000096803715,0.00022480106,0.000045695084],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.973551e-7,0.0000049887753,0.9945447,0.0000031911145,0.0000069714224,0.00002506431,0.00010040304,0.000547614,0.000007920118,0.0000017078995,0.0015829998,0.0031734537],"study_design_scores_gemma":[0.000076417964,0.00017446947,0.98094654,0.00006106133,0.000014235178,0.00008609268,0.00012679817,0.0010936719,0.000024212273,0.0005201232,0.016795315,0.00008108086],"about_ca_topic_score_codex":0.29986006,"about_ca_topic_score_gemma":0.9903993,"teacher_disagreement_score":0.69053924,"about_ca_system_score_codex":6.743675e-7,"about_ca_system_score_gemma":0.0001629563,"threshold_uncertainty_score":0.9690755},"labels":[],"label_agreement":null},{"id":"W2123323237","doi":"10.1139/e11-044","title":"Fluid inclusion and stable isotope constraints on the origin of Wernecke Breccia and associated iron oxide – copper – gold mineralization, Yukon","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; Yukon University","funders":"","keywords":"Breccia; Geology; Iron oxide copper gold ore deposits; Geochemistry; Fluid inclusions; Meteoric water; Mineralization (soil science); Clastic rock; Carbonate; Isotope geochemistry; Dolomite; Mineralogy; Sedimentary rock; Hydrothermal circulation; Chemistry; Isotope; Paleontology","score_opus":0.024968034118480777,"score_gpt":0.19521884934636374,"score_spread":0.17025081522788296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2123323237","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9903259,0.00059501984,0.000002793311,0.00085521705,0.000058108428,0.000044156906,0.000029791277,0.0000015887243,0.008087376],"genre_scores_gemma":[0.99913824,0.00007874205,0.00017892262,0.00044753333,0.000014011338,7.514688e-8,0.0000029954851,7.145967e-7,0.0001387886],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991228,0.00007972303,0.00023342576,0.00012308898,0.00021961519,0.00022133575],"domain_scores_gemma":[0.99922603,0.00013336922,0.00016996032,0.00005012171,0.000109203545,0.00031129838],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00081834465,0.00008058164,0.00016482871,0.00011773779,0.00032555076,0.000044215474,0.00020759842,0.000043664797,0.003578304],"category_scores_gemma":[0.0003027161,0.00004360315,0.000033467553,0.00034516872,0.0008475344,0.00014940504,0.000015206578,0.00009338915,0.000005062336],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008055153,0.0000064012547,0.9968408,0.0000029045343,0.000010396832,0.000010143594,0.0003387065,0.00016508174,0.00038877287,0.00053399144,0.00029673023,0.0013980665],"study_design_scores_gemma":[0.00013492527,0.0003187185,0.9922716,0.00004583635,0.00002048458,0.000021990427,0.00030064952,0.0010940811,0.0006890457,0.0042636893,0.0007489953,0.000089967354],"about_ca_topic_score_codex":0.041531723,"about_ca_topic_score_gemma":0.27986103,"teacher_disagreement_score":0.23832932,"about_ca_system_score_codex":0.0000013037544,"about_ca_system_score_gemma":0.00019087867,"threshold_uncertainty_score":0.9973326},"labels":[],"label_agreement":null},{"id":"W2123660838","doi":"10.1139/e2012-014","title":"Reply to the discussion by Rajesh and Knoper on “New zircon shock phenomena and their use for dating and reconstruction of large impact structures revealed by electron nanobeam (EBSD, CL, EDS) and isotopic U–Pb and (U–Th)/He analysis of the Vredefort dome”<sup>1</sup>Appears in Canadian Journal of Earth Sciences, 2012, <b>49</b>(7): this issue [doi: 10.1139/e2012-003].","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Zircon; Impact crater; Geology; Shock (circulatory); Electron backscatter diffraction; Geochemistry; Mineralogy; Microstructure; Materials science; Physics; Metallurgy; Astrobiology","score_opus":0.008717956035096994,"score_gpt":0.22903356319377166,"score_spread":0.22031560715867465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2123660838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960441,0.0024356097,0.00006624857,0.0007417012,0.00009274285,0.0002216291,0.00030709725,5.3896247e-7,0.00009033911],"genre_scores_gemma":[0.9990566,0.0000678096,0.0004466648,0.00010355913,0.00010394838,6.3973084e-7,0.000004548922,0.000004382799,0.00021187021],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984274,0.0001366461,0.00045632385,0.00022545905,0.00022107373,0.00053312536],"domain_scores_gemma":[0.998429,0.00015178001,0.0004757593,0.00013070376,0.00007561537,0.00073713716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018817488,0.00017438884,0.0003827028,0.00047050355,0.0006388581,0.00022361733,0.00027136185,0.000041765987,0.00016338512],"category_scores_gemma":[0.00008508908,0.00008672735,0.00006418396,0.0006785057,0.0006716488,0.0009668461,0.000024368543,0.00020920216,1.250399e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028879535,0.000007228748,0.9804608,0.000008204534,0.00007556054,2.7869535e-7,0.0023652946,0.0004136143,0.0017212837,0.000081855935,0.0012436877,0.013593317],"study_design_scores_gemma":[0.0010919134,0.0017843544,0.9491159,0.0003085022,0.00023842549,0.0001233015,0.0069510345,0.002559487,0.00197988,0.00028466998,0.035178997,0.0003835834],"about_ca_topic_score_codex":0.056604106,"about_ca_topic_score_gemma":0.106823064,"teacher_disagreement_score":0.050218955,"about_ca_system_score_codex":0.000011129185,"about_ca_system_score_gemma":0.00095528027,"threshold_uncertainty_score":0.94967806},"labels":[],"label_agreement":null},{"id":"W2123747158","doi":"10.1139/e05-109","title":"Paleobathymetry of a Silurian shelf based on brachiopod assemblages: an oxygen isotope test","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Marine Biology and Ecology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Brock University; Western University; Laurentian University; Carleton University; Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research","keywords":"Geology; Taphonomy; Carbonate; Isotopes of oxygen; Benthic zone; Paleontology; Petrography; Water mass; Oceanography; Geochemistry; Chemistry","score_opus":0.0179214149713997,"score_gpt":0.23344476454483337,"score_spread":0.21552334957343366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2123747158","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9706433,0.0002624427,0.000007648342,0.0007731362,0.0002653204,0.000079160076,0.000036286154,0.000003822564,0.027928876],"genre_scores_gemma":[0.99875605,0.000005583752,0.00047777352,0.0003338186,0.00017163064,1.9053373e-7,0.000011536303,0.0000019064495,0.00024151187],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984535,0.00017561334,0.00035899918,0.00020610177,0.0002958378,0.00050995935],"domain_scores_gemma":[0.99853516,0.0004572867,0.00021277614,0.00014984827,0.0001135517,0.0005313762],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017786745,0.00011726458,0.00023188296,0.0006184941,0.00041984918,0.00008441571,0.000662913,0.00010846511,0.0035246967],"category_scores_gemma":[0.00040469106,0.00008634022,0.000078994846,0.0005629848,0.00073723734,0.00030757976,0.000004321994,0.0002569996,0.000048061516],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015986338,0.000022707276,0.99485475,0.000005008506,0.0000042476404,0.00007889235,0.000021433323,0.0031489448,0.000041650273,0.00006920371,0.0001604051,0.001576787],"study_design_scores_gemma":[0.00020885619,0.0019566102,0.9906684,0.000020100904,0.0000062118384,0.00005464188,0.000109316876,0.0040756078,0.0001369482,0.00032437398,0.0023368946,0.00010200022],"about_ca_topic_score_codex":0.025602888,"about_ca_topic_score_gemma":0.72044104,"teacher_disagreement_score":0.6948381,"about_ca_system_score_codex":0.0000020490675,"about_ca_system_score_gemma":0.0017073136,"threshold_uncertainty_score":0.9973862},"labels":[],"label_agreement":null},{"id":"W2123924732","doi":"10.1139/e10-037","title":"Comparison of structures in zircons from lunar and terrestrial impactitesThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Office of Research and Development","keywords":"Zircon; Baddeleyite; Geology; Breccia; Impact crater; Ejecta; Geochemistry; Geochronology; Shock metamorphism; Impact structure; Shock (circulatory); Astrobiology","score_opus":0.0385799102365715,"score_gpt":0.23986872626585168,"score_spread":0.20128881602928017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2123924732","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99784154,0.000072587754,9.4499336e-7,0.00038323668,0.000101011065,0.00006453753,0.000062862855,2.0437577e-7,0.0014730998],"genre_scores_gemma":[0.9996476,0.000005610783,0.00025068884,0.000014633395,0.000075443444,2.571177e-7,0.0000018355883,0.0000010959121,0.0000027978701],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990861,0.00006786294,0.00046352905,0.00008452752,0.00015529126,0.00014268272],"domain_scores_gemma":[0.9992806,0.000091942595,0.0004423878,0.000079001766,0.00003803107,0.00006809392],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000457981,0.000060289836,0.00028846387,0.00026636003,0.000029592076,0.000013850218,0.00023416782,0.000028081358,0.0016730479],"category_scores_gemma":[0.00006275307,0.000042563068,0.000031148644,0.00037212094,0.0006215428,0.00045018215,0.000008490658,0.00012459283,3.549331e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007223838,0.00004356644,0.97427106,0.0000033463207,0.0000113659125,0.0000013366257,0.014226316,0.00029405367,0.009310966,0.000576233,0.00010229386,0.0010872453],"study_design_scores_gemma":[0.00048320444,0.0006060013,0.86827826,0.00012272788,0.000008668309,0.000001028201,0.011885025,0.00017704042,0.113852575,0.0044232584,0.00010306377,0.000059154336],"about_ca_topic_score_codex":0.055152785,"about_ca_topic_score_gemma":0.13321903,"teacher_disagreement_score":0.10599279,"about_ca_system_score_codex":0.0000037118539,"about_ca_system_score_gemma":0.0005504913,"threshold_uncertainty_score":0.99923956},"labels":[],"label_agreement":null},{"id":"W2124087833","doi":"10.1139/cjes-2015-0059","title":"Introduction to the Special Issue commemorating the 30th anniversary of the Royal Tyrrell Museum of Palaeontology, with a summary of the museum’s early history and its research contributions","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Paleontology; Geology; Archaeology; History","score_opus":0.03768170944471368,"score_gpt":0.24184173559369956,"score_spread":0.20416002614898587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124087833","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9431431,0.004510653,0.000004281417,0.04664665,0.0016313819,0.00020422251,0.000082453225,9.97045e-7,0.0037762325],"genre_scores_gemma":[0.99875766,0.000017287362,0.000039734045,0.0001383409,0.0008097235,3.1989833e-7,9.078837e-7,8.616329e-7,0.00023518426],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982578,0.0007593093,0.00026389648,0.00012572775,0.0003095542,0.00028368365],"domain_scores_gemma":[0.9985853,0.00030750738,0.00028057577,0.00017044538,0.00047287077,0.0001832884],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0029010202,0.0000715736,0.00017254402,0.00012331591,0.0008354579,0.000017144375,0.00074027904,0.00006203449,0.00015691156],"category_scores_gemma":[0.0007158798,0.000030362171,0.000044860608,0.00049375,0.0034121452,0.00014317725,0.000022275257,0.00036224318,0.0000033476952],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010725749,0.000008907085,0.94559526,0.000005728081,0.00002982278,0.0000057722464,0.003939592,0.0041386345,0.000035771034,0.00050964823,0.045086566,0.00053700904],"study_design_scores_gemma":[0.00017520536,0.00060080684,0.91590744,0.000032701337,0.00001878149,0.000092901406,0.0034298007,0.0004895886,0.000051146333,0.00013873035,0.07901828,0.00004459667],"about_ca_topic_score_codex":0.024223872,"about_ca_topic_score_gemma":0.616619,"teacher_disagreement_score":0.5923951,"about_ca_system_score_codex":0.000011029918,"about_ca_system_score_gemma":0.0021809165,"threshold_uncertainty_score":0.9993},"labels":[],"label_agreement":null},{"id":"W2124162192","doi":"10.1139/e10-075","title":"The Duck Pond and Boundary Cu–Zn deposits, Newfoundland: new insights into the ages of host rocks and the timing of VHMS mineralization","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Newfoundland and Labrador; Royal Roads University; Teck (Canada); Geological Survey of Canada","funders":"","keywords":"Felsic; Geology; Geochemistry; Mafic; Zircon; Mineralization (soil science); Volcanic rock; Volcanogenic massive sulfide ore deposit; Pyroclastic rock; Sedimentary rock; Volcano; Sphalerite","score_opus":0.009632516193034069,"score_gpt":0.19197219079967795,"score_spread":0.18233967460664388,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124162192","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9849943,0.009347891,0.000016270078,0.0047747702,0.00014938693,0.000046031237,0.0000019155054,7.7035224e-7,0.00066865195],"genre_scores_gemma":[0.99900544,0.00037779624,0.00019482082,0.00019455806,0.00008689434,6.9218785e-8,0.0000011305685,6.177141e-7,0.00013865661],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999196,0.000069812195,0.00025616615,0.00009555104,0.0002161166,0.00016635693],"domain_scores_gemma":[0.99894816,0.00041800077,0.00021762804,0.00008367984,0.00009109335,0.00024146917],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000645069,0.000072704854,0.00015883516,0.000074465104,0.0007354227,0.00019434506,0.00036038418,0.000034589437,0.00018288216],"category_scores_gemma":[0.00029975927,0.000027249305,0.00004953603,0.00033824996,0.0018458263,0.0001764843,0.000011414567,0.0001607474,8.652766e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002237152,0.0000019981194,0.9833873,0.0000050926856,0.000024015913,0.000004373881,0.0024339592,0.00032590755,0.00074900466,0.00044918386,0.00010473824,0.012492044],"study_design_scores_gemma":[0.00022742222,0.00013543703,0.977328,0.000019626146,0.000043688844,0.000059119397,0.0006456237,0.002684437,0.0003304763,0.013438265,0.005020975,0.00006692722],"about_ca_topic_score_codex":0.19140653,"about_ca_topic_score_gemma":0.94307226,"teacher_disagreement_score":0.7516657,"about_ca_system_score_codex":4.3287966e-7,"about_ca_system_score_gemma":0.00029109122,"threshold_uncertainty_score":0.81397796},"labels":[],"label_agreement":null},{"id":"W2124279925","doi":"10.1139/cjes-2014-0029","title":"Lobal affinity of Late Wisconsin tills at St. Marys in southwestern Ontario, Canada","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Waterloo; Western University","funders":"","keywords":"Geology; Unconformity; Subaerial; Moraine; Geomorphology; Deposition (geology); Bedrock; Sediment; Meltwater; Geochemistry; Facies; Ice stream; Glacier; Varve; Structural basin; Paleontology; Oceanography; Cryosphere","score_opus":0.020101308490831298,"score_gpt":0.18583826566666742,"score_spread":0.1657369571758361,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124279925","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947987,0.0003509398,0.0000033774857,0.0005578409,0.0005979409,0.0000406127,0.000098493176,9.302335e-7,0.0035511407],"genre_scores_gemma":[0.9987841,0.000008647992,0.00037767692,0.00033974147,0.000044245284,5.5325092e-8,0.000003344504,0.0000010666289,0.00044107737],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988655,0.000049785504,0.00034236777,0.00011998429,0.00028362664,0.00033874146],"domain_scores_gemma":[0.99912125,0.00014429478,0.00021285801,0.00008232926,0.000077359546,0.00036193256],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00059760653,0.000087684064,0.00021183284,0.000080887476,0.00024863592,0.000042718282,0.00029259408,0.000027618791,0.003531327],"category_scores_gemma":[0.00011075179,0.000068844216,0.000042456515,0.00036361613,0.00029723736,0.00017335673,0.0000076143824,0.00011546031,0.000004850304],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000039845863,0.0000015556952,0.9915204,0.0000023524722,0.0000051885013,0.000022518438,0.0003025904,0.0061199833,0.0000013006722,0.00001999518,0.00066451717,0.0013355884],"study_design_scores_gemma":[0.00014561861,0.00010024907,0.9689,0.000030341858,0.0000052530563,0.00001786454,0.000279925,0.0004007584,0.0000066134467,0.00014911525,0.02988436,0.00007989934],"about_ca_topic_score_codex":0.99581695,"about_ca_topic_score_gemma":0.9999969,"teacher_disagreement_score":0.029219843,"about_ca_system_score_codex":0.000017008017,"about_ca_system_score_gemma":0.0041234633,"threshold_uncertainty_score":0.9973796},"labels":[],"label_agreement":null},{"id":"W2124345640","doi":"10.1139/e00-018","title":"Geology of the Matthew Creek metamorphic zone, southeast British Columbia: a window into Middle Proterozoic metamorphism in the Purcell Basin","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Metamorphism; Metamorphic rock; Geochemistry; Lineation; Metamorphic core complex; Shear zone; Schist; Sill; Sillimanite; Proterozoic; Metamorphic facies; Mafic; Isograd; Biotite; Quartz; Geomorphology; Paleontology; Structural basin; Facies; Tectonics","score_opus":0.01549849072240182,"score_gpt":0.1694543115677261,"score_spread":0.1539558208453243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124345640","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9919239,0.0015793201,0.0000033775354,0.002981783,0.00009845209,0.00016857735,0.00003075741,0.000002053439,0.0032117588],"genre_scores_gemma":[0.99770874,0.000029738916,0.00037230534,0.00087972457,0.000062911124,0.0000011435432,0.0000019374115,0.0000015381453,0.00094194204],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978708,0.0003979238,0.00052627927,0.00022960195,0.00046158256,0.0005138085],"domain_scores_gemma":[0.99898577,0.00016854324,0.00024765392,0.00018428073,0.00008958285,0.00032416006],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017025115,0.000107971704,0.00037055253,0.00010960277,0.0004886496,0.00033907147,0.0012917125,0.00007514882,0.03089352],"category_scores_gemma":[0.00016493042,0.00007423154,0.00023707749,0.0012437789,0.0016426451,0.00020731323,0.000010107051,0.0003547559,0.0000552493],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000048263278,0.000014928921,0.9931341,0.000007238692,0.000016402973,0.00008667048,0.00025212052,0.0012372455,0.000021152384,0.000007664936,0.00012842625,0.0050892225],"study_design_scores_gemma":[0.0001789204,0.00019871123,0.9866008,0.000048355112,0.000041511244,0.00040786614,0.00062271743,0.0003579766,0.00001810758,0.0074286647,0.0039887885,0.00010756571],"about_ca_topic_score_codex":0.7602943,"about_ca_topic_score_gemma":0.99130446,"teacher_disagreement_score":0.23101012,"about_ca_system_score_codex":0.0000017294997,"about_ca_system_score_gemma":0.0005025398,"threshold_uncertainty_score":0.9699924},"labels":[],"label_agreement":null},{"id":"W2124495327","doi":"10.1139/e10-093","title":"Eocene rotation of the Coast Plutonic Complex and Intermontane Belt: paleomagnetism of Eocene plutons along the Klondike Highway","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor","funders":"","keywords":"Geology; Pluton; Terrane; Paleomagnetism; Felsic; Mafic; Outcrop; Geochemistry; Clockwise; Seismology; Tectonics; Geomorphology; Fold (higher-order function); Paleontology","score_opus":0.023460330682345668,"score_gpt":0.2186115963306319,"score_spread":0.19515126564828622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124495327","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916572,0.0054643294,0.000038073482,0.00045600088,0.00026017,0.00011742543,0.000046853427,9.1503813e-7,0.001959039],"genre_scores_gemma":[0.99890566,0.00031579498,0.00049984816,0.00010044045,0.000050936847,0.0000015073123,0.0000021196454,0.000004841884,0.00011882796],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989601,0.000087874425,0.00036519373,0.00014759469,0.00018742349,0.00025181947],"domain_scores_gemma":[0.9991003,0.00002997046,0.00036512007,0.00018441942,0.00016817541,0.00015198204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004265197,0.00011821816,0.00018819432,0.000090792535,0.00028657535,0.00002176557,0.00048555623,0.000054617925,0.00007950037],"category_scores_gemma":[0.00009279294,0.00007128148,0.00008851656,0.00020723294,0.0015238957,0.000015561101,0.000060648217,0.00009521273,4.2161216e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010183323,0.00006739736,0.7770642,0.00008604577,0.0001799969,0.000039385046,0.00862164,0.00014843202,0.19229513,0.0016772479,0.00120532,0.01851338],"study_design_scores_gemma":[0.00032793448,0.0009620213,0.97815704,0.000058862446,0.000036556274,0.00014318386,0.00083944714,0.000018827113,0.018189177,0.00018816002,0.0009879189,0.000090839676],"about_ca_topic_score_codex":0.0045725163,"about_ca_topic_score_gemma":0.21660006,"teacher_disagreement_score":0.21202755,"about_ca_system_score_codex":0.0000016805268,"about_ca_system_score_gemma":0.00047338038,"threshold_uncertainty_score":0.7976949},"labels":[],"label_agreement":null},{"id":"W2124583084","doi":"10.1139/cjes-2014-0064","title":"Histologic growth dynamic study of <i>Edmontosaurus regalis</i> (Dinosauria: Hadrosauridae) from a bonebed assemblage of the Upper Cretaceous Horseshoe Canyon Formation, Edmonton, Alberta, Canada","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Paleontology; Horseshoe (symbol); Canyon; Cretaceous; Assemblage (archaeology); Geomorphology","score_opus":0.007829958678337948,"score_gpt":0.18373126570003584,"score_spread":0.1759013070216979,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124583084","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915768,0.0021758717,0.000023531553,0.0014568422,0.001181914,0.0001774545,0.00010849662,0.0000025342397,0.003296576],"genre_scores_gemma":[0.99933696,0.000024909914,0.00012221301,0.00032689192,0.00006022197,6.028712e-7,0.000010338508,0.000002244022,0.00011560903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99756736,0.00049526413,0.00075464026,0.00024368841,0.0004522932,0.0004867474],"domain_scores_gemma":[0.99785167,0.0004402831,0.0008306864,0.0002507577,0.00025705088,0.00036953492],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00086822594,0.00018771233,0.00047295156,0.00022204815,0.00053798064,0.000027956252,0.0009940356,0.00012154223,0.0003274055],"category_scores_gemma":[0.00058066985,0.00012311449,0.000107775675,0.0004822145,0.0007597331,0.0004804837,0.000012099261,0.00026635666,0.0000030705557],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033762924,0.000017574079,0.9965027,0.00000741383,0.00003406875,0.00002543611,0.00075050764,0.0011479955,0.000113612696,0.00006621666,0.0009851998,0.00031551786],"study_design_scores_gemma":[0.00042250688,0.0006515368,0.9920207,0.00003649155,0.000054789423,0.00014990865,0.0011974563,0.0019455191,0.000116921765,0.0005306357,0.0027241562,0.00014934434],"about_ca_topic_score_codex":0.96864194,"about_ca_topic_score_gemma":0.9998842,"teacher_disagreement_score":0.031242263,"about_ca_system_score_codex":0.000017561944,"about_ca_system_score_gemma":0.0029289697,"threshold_uncertainty_score":0.5195866},"labels":[],"label_agreement":null},{"id":"W2124950699","doi":"10.1139/e05-084","title":"Brittle faulting in the ThorOdin culmination, Monashee complex, southern Canadian Cordillera: constraints on geometry and kinematics","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Geology; Sinistral and dextral; Lineament; Echelon formation; Strike-slip tectonics; Seismology; Culmination; Fault (geology); Normal fault; Tectonics","score_opus":0.02856878422596771,"score_gpt":0.22050044194888618,"score_spread":0.19193165772291848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124950699","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9788545,0.00033115296,0.000005300895,0.0070488085,0.00004630038,0.000054149183,0.00004940503,0.000001439715,0.013608966],"genre_scores_gemma":[0.99756646,0.000012177811,0.0007329574,0.001564144,0.00008806986,1.2929948e-7,0.000005546394,7.9779034e-7,0.000029742143],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988454,0.00008078832,0.00028281313,0.00013426006,0.00028110528,0.00037562835],"domain_scores_gemma":[0.9990137,0.00023111091,0.00011304903,0.00006229638,0.00007668074,0.0005031525],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009903539,0.00009227282,0.00016534403,0.00035901967,0.00038571993,0.0001643422,0.00035974316,0.00004141509,0.0062760683],"category_scores_gemma":[0.00035478795,0.000054609915,0.000046120047,0.0006030728,0.0006468742,0.00012757326,0.0000027958924,0.00019851212,0.000052422798],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000020797343,0.0000070470683,0.9620826,0.0000039150164,0.000008836638,0.000067646804,0.0009139614,0.0062679932,0.000013601197,0.00020322211,0.00020605841,0.03022303],"study_design_scores_gemma":[0.00012758981,0.00011849955,0.98367244,0.000032961823,0.0000101726955,0.00011902553,0.003090608,0.0090869265,0.0000127952635,0.0014373779,0.0021794438,0.0001121832],"about_ca_topic_score_codex":0.23446268,"about_ca_topic_score_gemma":0.9759807,"teacher_disagreement_score":0.74151796,"about_ca_system_score_codex":0.0000032786231,"about_ca_system_score_gemma":0.00036944836,"threshold_uncertainty_score":0.9946323},"labels":[],"label_agreement":null},{"id":"W2125136201","doi":"10.1139/e2012-075","title":"Widespread erosion and mass failure from the ∼51 Ma Montagnais marine bolide impact off southwestern Nova Scotia, Canada <sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of <i>Mesozoic–Cenozoic geology of the Scotian Basin</i>. <sup>2</sup>Earth Sciences Sector Contribution 20120241.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Petroleum Research Newfoundland and Labrador","funders":"","keywords":"Geology; Debris; Paleontology; Fault scarp; Impact crater; Cretaceous; Impact structure; Abyssal plain; Erosion; Seamount; Continental margin; Tectonics; Oceanography; Sediment","score_opus":0.01419778120702564,"score_gpt":0.20895452560370179,"score_spread":0.19475674439667615,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125136201","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98780596,0.0013278467,6.2226485e-7,0.008485286,0.00036934562,0.0002847751,0.00037957812,0.0000016526052,0.0013449349],"genre_scores_gemma":[0.99908596,0.000075037846,0.00010103012,0.00039430108,0.00024045557,5.341668e-7,0.0000074150907,0.000003776395,0.00009149378],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9966316,0.0007451185,0.00075400627,0.00027892285,0.00076803734,0.00082226424],"domain_scores_gemma":[0.99704796,0.0013550421,0.0006381325,0.00031541422,0.00028052714,0.00036292608],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0030072492,0.00022835295,0.0005948772,0.0002969542,0.0004648514,0.00008232855,0.0010573202,0.00015776581,0.018466108],"category_scores_gemma":[0.0009895144,0.00012050259,0.00013631416,0.0010289678,0.0044122646,0.0006842221,0.00005532199,0.00049116416,0.000008714136],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012390246,0.000019673831,0.9937071,0.0000154209,0.00005387111,0.0000067591313,0.0029541762,0.0017970386,0.00025195887,0.00007791938,0.00077551196,0.00021663743],"study_design_scores_gemma":[0.00042705177,0.0005508422,0.9890522,0.00016232855,0.000037897662,0.000071244656,0.003470902,0.00083111477,0.004146578,0.00029647458,0.0008287555,0.00012461134],"about_ca_topic_score_codex":0.7241674,"about_ca_topic_score_gemma":0.9838122,"teacher_disagreement_score":0.2596448,"about_ca_system_score_codex":0.000005918922,"about_ca_system_score_gemma":0.0025301508,"threshold_uncertainty_score":0.99829715},"labels":[],"label_agreement":null},{"id":"W2125251532","doi":"10.1139/e09-016","title":"Paleomagnetic dating of the northern Alberta kimberlites","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Paleomagnetism; Kimberlite; Geology; Cenozoic; Mesozoic; Paleontology; Absolute dating; Apparent polar wander; Ultramafic rock; Radiogenic nuclide; Geochronology; Geochemistry; Radiocarbon dating; Mantle (geology)","score_opus":0.011177570854021268,"score_gpt":0.17824323221484709,"score_spread":0.16706566136082582,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125251532","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97684675,0.00087446306,0.0000019897125,0.0025173381,0.00010719619,0.000024321851,0.000005634212,8.7319785e-7,0.019621447],"genre_scores_gemma":[0.9990087,0.000006633111,0.0003594259,0.00037703675,0.000053500673,1.6864254e-8,8.032365e-7,3.3817102e-7,0.00019355024],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99907196,0.00004966178,0.0002768369,0.00009946086,0.00024244943,0.00025961592],"domain_scores_gemma":[0.99916226,0.00014812325,0.0002046149,0.00008908019,0.00009615534,0.00029974835],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00036762204,0.00006906368,0.00014822728,0.00008741072,0.00023155336,0.000051609488,0.0005617457,0.000026659638,0.0050127287],"category_scores_gemma":[0.00041213768,0.00003505429,0.00011679419,0.0006066739,0.0004358733,0.00012768149,0.0000033304757,0.00011245408,0.00001792151],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011804506,0.000002362925,0.98950964,0.0000011552075,0.000003638064,0.000004179716,0.00007931015,0.001961732,0.00008390599,0.000057109897,0.00002177092,0.008273998],"study_design_scores_gemma":[0.000047815745,0.00022066866,0.9907272,0.000022220673,0.000013779069,0.00003280664,0.0001168508,0.00074734475,0.0002659087,0.006783875,0.0009644954,0.00005701856],"about_ca_topic_score_codex":0.043509055,"about_ca_topic_score_gemma":0.80383635,"teacher_disagreement_score":0.7603273,"about_ca_system_score_codex":4.3598607e-7,"about_ca_system_score_gemma":0.00032969422,"threshold_uncertainty_score":0.9958968},"labels":[],"label_agreement":null},{"id":"W2125686038","doi":"10.1139/e07-002","title":"A new paraclupeid fish (Clupeomorpha, Ellimmichthyiformes) from a muddy marine pro-delta environment: middle Cenomanian Dunvegan Formation, Alberta, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fish Ecology and Management Studies","field":"Environmental Science","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Delta; Oceanography; Salinity; Estuary; Brackish water; Cenomanian; Paleontology; Cretaceous","score_opus":0.011758485731056256,"score_gpt":0.17749020864902137,"score_spread":0.16573172291796512,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125686038","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9426762,0.00010187062,0.00058130204,0.00607504,0.0006211085,0.00030297777,0.000031645857,0.000005908866,0.04960394],"genre_scores_gemma":[0.9895126,0.000057560945,0.002653033,0.0036210853,0.0001369631,0.0000019399897,0.000011416763,0.000009681357,0.0039956723],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979922,0.00003444141,0.00052557606,0.00026147868,0.00045285292,0.0007334086],"domain_scores_gemma":[0.99853075,0.00011620385,0.00034554632,0.00016811541,0.000016510403,0.00082288287],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007076481,0.00019076875,0.00023818332,0.00012236519,0.00076386466,0.00008426089,0.0006616708,0.00005979397,0.008786399],"category_scores_gemma":[0.00009388969,0.00016871108,0.000059753173,0.00033600524,0.00043805296,0.00081765733,0.00010708452,0.00018493844,0.00013849938],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018683922,0.000019226474,0.9116326,0.0000055258106,0.000044923196,0.00021465191,0.0010325045,0.000741929,0.00002456485,0.00011890408,0.083982885,0.0021636242],"study_design_scores_gemma":[0.00035732804,0.00015672189,0.71703637,0.000016815307,0.000029550798,0.000052793035,0.0007849114,0.00012160682,0.00022877281,0.0004664725,0.28054905,0.00019960268],"about_ca_topic_score_codex":0.89899415,"about_ca_topic_score_gemma":0.9997885,"teacher_disagreement_score":0.19656615,"about_ca_system_score_codex":0.00012757795,"about_ca_system_score_gemma":0.0006723717,"threshold_uncertainty_score":0.9921197},"labels":[],"label_agreement":null},{"id":"W2125733368","doi":"10.1139/e03-019","title":"Dike swarms on Seward Peninsula, Alaska, and their implications for the kinematics of Cretaceous extension in the Bering Strait region","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation","keywords":"Dike; Geology; Geochemistry; Mafic; Metamorphism; Magmatism; Felsic; Pluton; Seismology; Petrology; Tectonics","score_opus":0.06468647182634617,"score_gpt":0.2324369834311171,"score_spread":0.16775051160477095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125733368","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909239,0.0017441433,0.00052685704,0.0058125565,0.00012269105,0.0001593762,0.000009612556,8.495743e-7,0.00070005865],"genre_scores_gemma":[0.9991943,0.00017410464,0.00033574126,0.00025884516,0.000026356942,6.835181e-7,7.3374053e-7,6.425212e-7,0.0000085812335],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99941564,0.00005353803,0.0001948541,0.00008079906,0.00008266962,0.00017252356],"domain_scores_gemma":[0.9991684,0.00048344105,0.0001331273,0.00006927662,0.00006198669,0.00008379253],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008586316,0.000058506183,0.00010463407,0.00006520018,0.00045039336,0.00006219011,0.00018848716,0.000021096446,0.000023629445],"category_scores_gemma":[0.0002892227,0.0000251385,0.000036713976,0.00022821833,0.0002700451,0.000099112614,0.0000018125202,0.00007758138,7.226992e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019577175,0.000014635467,0.8711018,0.000018551706,0.000018262861,0.000007771105,0.0053434214,0.08849183,0.00004606325,0.0036753984,0.00036810525,0.030894589],"study_design_scores_gemma":[0.00010440677,0.00047164218,0.9824592,0.000029633653,0.000007229473,0.000075742886,0.005065616,0.0022983828,0.000024892934,0.006300257,0.0031128537,0.00005015225],"about_ca_topic_score_codex":0.0012837015,"about_ca_topic_score_gemma":0.0739187,"teacher_disagreement_score":0.11135739,"about_ca_system_score_codex":8.539448e-7,"about_ca_system_score_gemma":0.000111098554,"threshold_uncertainty_score":0.9429799},"labels":[],"label_agreement":null},{"id":"W2126424023","doi":"10.1139/cjes-2013-0076","title":"The Flin Flon paleosol revisited","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"","keywords":"Geology; Chlorite; Geochemistry; Albite; Weathering; Mafic; Petrography; Epidote; Greenstone belt; Mineralogy; Calcite; Mineral; Quartz; Archean; Chemistry","score_opus":0.011387499115861649,"score_gpt":0.18600203179409333,"score_spread":0.17461453267823168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126424023","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97793037,0.0027397212,0.000009866189,0.0031303284,0.00027519028,0.000056315952,0.000011161498,0.0000025309603,0.01584452],"genre_scores_gemma":[0.9987266,0.00007006527,0.00022244622,0.00026169585,0.00013892204,1.4455973e-7,0.0000028750944,6.2051305e-7,0.000576636],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990025,0.000045606685,0.0002545296,0.0000966981,0.00024656797,0.0003540538],"domain_scores_gemma":[0.9990607,0.000093095645,0.00014237767,0.00008761987,0.00010887876,0.000507311],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007266142,0.000070935355,0.000102861595,0.00009092968,0.00089257705,0.00038948163,0.00048569363,0.000024456087,0.007848106],"category_scores_gemma":[0.00011939426,0.00003933217,0.00008062135,0.00046658522,0.0003875379,0.00033855808,0.0000027364272,0.00011836655,0.00027719935],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000015056287,0.0000011614071,0.9813026,0.000002626981,0.000015173455,0.000016498107,0.00007334306,0.0006983802,0.000053053715,0.000026711747,0.0017339354,0.016074985],"study_design_scores_gemma":[0.000097278345,0.00016568716,0.9470674,0.000033203334,0.00001829883,0.0001095485,0.0010688913,0.0029482024,0.00037674044,0.001525721,0.046457577,0.00013145042],"about_ca_topic_score_codex":0.02015668,"about_ca_topic_score_gemma":0.31027338,"teacher_disagreement_score":0.2901167,"about_ca_system_score_codex":5.731017e-7,"about_ca_system_score_gemma":0.00036328813,"threshold_uncertainty_score":0.99305886},"labels":[],"label_agreement":null},{"id":"W2126483052","doi":"10.1139/cjes-2012-0023","title":"A comparative geochemical study of Mars and Earth basalt petrogenesis","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of British Columbia, Okanagan Campus","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mars Exploration Program; Geology; Basalt; Martian; Meteorite; Mantle (geology); Geochemistry; Astrobiology; Trace element; Achondrite; Chondrite","score_opus":0.026778763605279074,"score_gpt":0.21355066302414455,"score_spread":0.18677189941886546,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126483052","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967744,0.00085666706,0.0000024308488,0.00036191204,0.000061542654,0.000085906555,0.000011251692,0.0000018769823,0.0018440608],"genre_scores_gemma":[0.9991388,0.000012673927,0.00066357764,0.00010140477,0.00003625079,3.04301e-7,0.0000013254722,6.3000545e-7,0.000045083954],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99879456,0.000081392136,0.00034376813,0.00017208935,0.00029690823,0.00031129387],"domain_scores_gemma":[0.99873304,0.00015976094,0.00018404062,0.00007280531,0.0001790943,0.00067128375],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003712508,0.0001047107,0.00033191577,0.00021899404,0.00019021243,0.00008500884,0.00030697437,0.00003444653,0.007328263],"category_scores_gemma":[0.00009927585,0.00006658931,0.000069424445,0.0005296295,0.0006202717,0.00024773693,0.000008727799,0.00012562079,0.000037154972],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000043096825,0.000017201459,0.99768156,0.0000026621676,0.000025118308,0.000013073154,0.00033492915,0.0004043052,0.00024086519,0.000010998214,0.00005817752,0.0012067757],"study_design_scores_gemma":[0.00018138846,0.0007944792,0.9924485,0.000010766946,0.000027347176,0.00004166375,0.002646839,0.001415187,0.00070559286,0.0014114812,0.00021924502,0.00009748742],"about_ca_topic_score_codex":0.0683257,"about_ca_topic_score_gemma":0.32805145,"teacher_disagreement_score":0.25972575,"about_ca_system_score_codex":5.0010345e-7,"about_ca_system_score_gemma":0.00022355537,"threshold_uncertainty_score":0.99357915},"labels":[],"label_agreement":null},{"id":"W2126556271","doi":"10.1139/cjes-2015-0071","title":"Cenozoic uplift of the Central Andes in northern Chile and Bolivia—reconciling paleoaltimetry with the geological evolution","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Subduction; Lithosphere; Cenozoic; Crust; Asthenosphere; Mantle (geology); Mountain formation; Back-arc basin; Crustal recycling; Geomorphology; Tectonics; Paleontology; Structural basin","score_opus":0.015835760711266734,"score_gpt":0.17514115781857267,"score_spread":0.15930539710730593,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126556271","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99463177,0.002498145,0.00001066807,0.0015837201,0.00007363935,0.000043559437,0.0000064749224,0.0000010459304,0.0011509814],"genre_scores_gemma":[0.99968266,0.000011778036,0.00011961609,0.0001248998,0.000046339974,7.7412e-8,5.465646e-7,4.5532516e-7,0.0000136505],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990586,0.000091456925,0.00019194697,0.00011104756,0.0002463451,0.00030058337],"domain_scores_gemma":[0.9992648,0.00010751482,0.00014372644,0.000062237435,0.0000832467,0.0003385176],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00074209506,0.000071256756,0.00015225737,0.000083177285,0.00018959788,0.000043050546,0.00028389273,0.00003439188,0.0003320894],"category_scores_gemma":[0.00019992043,0.000028330076,0.00004552806,0.0005555145,0.0010455622,0.00012561382,0.000007698287,0.00016706173,0.0000025799357],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000071369464,0.00000275775,0.9907528,0.0000012944805,0.0000046773735,0.0000075310945,0.00016602794,0.008274228,0.0000057107873,0.000022177506,0.000008502143,0.0007471305],"study_design_scores_gemma":[0.00012098908,0.00018114284,0.995232,0.000017540557,0.000010589495,0.00006789318,0.0008001283,0.0016529368,0.00003038446,0.0016878815,0.00014863754,0.000049871822],"about_ca_topic_score_codex":0.027601972,"about_ca_topic_score_gemma":0.85189146,"teacher_disagreement_score":0.82428944,"about_ca_system_score_codex":0.0000021896994,"about_ca_system_score_gemma":0.00053438876,"threshold_uncertainty_score":0.9788733},"labels":[],"label_agreement":null},{"id":"W2126639688","doi":"10.1139/cjes-2014-0015","title":"The Cora Lake shear zone, Athabasca granulite terrane, an intraplate response to far-field orogenic processes during the amalgamation of Laurentia","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Granulite; Shear zone; Lineation; Mafic; Geochemistry; Felsic; Shear (geology); Terrane; Metamorphic rock; Transtension; Sinistral and dextral; Transpression; Petrology; Geomorphology; Tectonics; Seismology; Facies","score_opus":0.009473432805051838,"score_gpt":0.1951979347080358,"score_spread":0.18572450190298395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126639688","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99549043,0.0005975146,0.00010419392,0.0032750007,0.00013324716,0.0000664512,0.000019374704,0.0000035819908,0.00031022896],"genre_scores_gemma":[0.99922913,0.00003279014,0.00022262517,0.00035994753,0.00007163281,3.5702803e-7,0.0000024120402,0.0000010983846,0.000079985744],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986079,0.00020326591,0.00034840623,0.00015065078,0.00034094893,0.00034887643],"domain_scores_gemma":[0.99852484,0.0004961553,0.00019760596,0.00013708326,0.00019439313,0.00044988902],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017757581,0.00009735165,0.00016422186,0.00014841321,0.0007249181,0.0001997758,0.00070491934,0.000038744263,0.0012721128],"category_scores_gemma":[0.0009221395,0.000046729056,0.00008200572,0.00085690396,0.0003948956,0.0002693234,0.000007863374,0.00015510536,0.000021393336],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035416975,0.000010763864,0.97127664,0.000025567824,0.00003592105,0.000018646637,0.001297669,0.0066605043,0.0014829666,0.00008284741,0.00008028784,0.018674005],"study_design_scores_gemma":[0.00012726829,0.00084120536,0.98314714,0.000037824808,0.00002558201,0.00006538968,0.00047239277,0.0012982053,0.002148834,0.0010836481,0.010640224,0.00011230987],"about_ca_topic_score_codex":0.0074568912,"about_ca_topic_score_gemma":0.7823527,"teacher_disagreement_score":0.7748958,"about_ca_system_score_codex":8.301651e-7,"about_ca_system_score_gemma":0.0003302778,"threshold_uncertainty_score":0.9996409},"labels":[],"label_agreement":null},{"id":"W2127225893","doi":"10.1139/cjes-2014-0141","title":"Stratigraphy, thickness, tectonic environment, and economic implications of the giant Suwar – Wadi Qutabah layered mafic complex in northwestern Yemen","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Kelowna General Hospital; University of British Columbia, Okanagan Campus","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey","keywords":"Mafic; Geology; Geochemistry; Plagioclase; Norite; Gabbro; Basalt; Paleontology","score_opus":0.03410247220135227,"score_gpt":0.20341062613113337,"score_spread":0.1693081539297811,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127225893","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954179,0.00078371185,0.000004894857,0.0019820977,0.000053415853,0.000052812666,0.000057400528,9.526168e-7,0.0016468106],"genre_scores_gemma":[0.9995566,0.00004397143,0.00025587698,0.00010493892,0.00001984387,1.9379782e-7,0.0000030394658,6.200145e-7,0.000014895113],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99914795,0.000058952006,0.00029082797,0.00013504771,0.00013225879,0.0002349729],"domain_scores_gemma":[0.99927366,0.000058189285,0.00017793808,0.00009971118,0.000020258387,0.0003702363],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046830688,0.00007601459,0.00016713771,0.00013681425,0.00013405734,0.000050316496,0.0003888324,0.000031062533,0.00088836666],"category_scores_gemma":[0.000025691352,0.00004497399,0.000062139865,0.000252533,0.00070405554,0.00015460164,0.00000888125,0.00011254129,0.000011558581],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000019592367,0.0000030298258,0.9943353,0.0000014132663,0.000006352802,0.0000025110721,0.000099059085,0.0045213923,0.00010334795,0.00009891298,0.000019118661,0.0008076134],"study_design_scores_gemma":[0.000120005934,0.00009998949,0.9913069,0.000008483753,0.000009175838,0.000037277157,0.00033547485,0.0009790299,0.000047601254,0.0062409434,0.0007528868,0.000062220686],"about_ca_topic_score_codex":0.07875408,"about_ca_topic_score_gemma":0.89167166,"teacher_disagreement_score":0.81291753,"about_ca_system_score_codex":0.000002551468,"about_ca_system_score_gemma":0.0005054472,"threshold_uncertainty_score":0.9726992},"labels":[],"label_agreement":null},{"id":"W2127306684","doi":"10.1139/cjes-2013-0119","title":"Paleomagnetic dating of magmatic phases at the Cantung tungsten deposit, Northwest Territories, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Dike; Geochemistry; Paleomagnetism; Pyrrhotite; Skarn; Proterozoic; Paleontology; Pyrite; Fluid inclusions; Hydrothermal circulation","score_opus":0.008014730958914541,"score_gpt":0.19660270214569558,"score_spread":0.18858797118678106,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127306684","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98800147,0.009173822,0.0000047863905,0.0006034167,0.00046552453,0.00011937942,0.00007303224,8.287294e-7,0.0015577518],"genre_scores_gemma":[0.99858147,0.0001107006,0.00030804356,0.00020102935,0.00017386212,0.000003839158,0.000011061039,0.000005490984,0.00060450495],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987744,0.00005928862,0.00037641343,0.00015522918,0.00026243163,0.00037221677],"domain_scores_gemma":[0.9989979,0.000054678156,0.00026658407,0.000180021,0.00019927854,0.00030151557],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023526812,0.00013236223,0.00017875031,0.00006515989,0.00045998342,0.00006929926,0.00047162914,0.000037803256,0.00027430497],"category_scores_gemma":[0.00017121085,0.000089505884,0.00005769564,0.000185292,0.00059261534,0.000017577755,0.000043857443,0.00007631934,0.0000014473395],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004394828,0.0000069135376,0.9738479,0.000029821593,0.000038216232,0.00003688995,0.00023632229,0.0001853856,0.016854625,0.000010395854,0.0062313876,0.0025177218],"study_design_scores_gemma":[0.00030920343,0.0009129264,0.9671245,0.000083512714,0.000044383327,0.0003650694,0.0012218216,0.00004526593,0.010126725,0.000027198588,0.019525109,0.00021425622],"about_ca_topic_score_codex":0.91554356,"about_ca_topic_score_gemma":0.99887216,"teacher_disagreement_score":0.083328635,"about_ca_system_score_codex":0.000006869786,"about_ca_system_score_gemma":0.002023804,"threshold_uncertainty_score":0.3649944},"labels":[],"label_agreement":null},{"id":"W2127306758","doi":"10.1139/cjes-2015-0125","title":"Connemara: its position and role in the Grampian Orogeny","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Orogeny; Dalradian; Ophiolite; Terrane; Accretionary wedge; Paleontology; Metamorphism; Nappe; Back-arc basin; Ordovician; Trough (economics); Island arc; Geosyncline; Geochemistry; Geomorphology; Paleozoic; Subduction; Structural basin; Tectonics","score_opus":0.025320108798979595,"score_gpt":0.19971074115462967,"score_spread":0.17439063235565008,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127306758","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.985353,0.002888021,0.0000020987457,0.004411489,0.00006865665,0.000028432089,0.000006698168,9.3571464e-7,0.0072406917],"genre_scores_gemma":[0.9990266,0.000016112446,0.00014240881,0.00074259925,0.00005255144,7.289135e-8,0.0000017889921,2.7686843e-7,0.000017566983],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99926066,0.00007981787,0.00015385299,0.000086848064,0.00020080611,0.00021798864],"domain_scores_gemma":[0.99933106,0.000076128264,0.00006457169,0.00003642926,0.00006572655,0.00042610738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001022685,0.00005245661,0.000099826044,0.00012635734,0.00014042965,0.00011569022,0.0002558911,0.000026053143,0.0007041928],"category_scores_gemma":[0.0001834928,0.000027324095,0.00003112767,0.0004339731,0.00026859462,0.00020441112,0.0000023753034,0.00010630296,0.000026733203],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000036883819,0.0000026900595,0.9961199,9.4504423e-7,0.0000030914766,0.00008102179,0.00043265973,0.0007400615,0.000019203211,0.00034591954,0.000064575004,0.0021862574],"study_design_scores_gemma":[0.00014293213,0.0002993942,0.96708834,0.000011342508,0.000010268474,0.00035961543,0.0019002738,0.0017819963,0.000077008284,0.025650773,0.002600486,0.00007758359],"about_ca_topic_score_codex":0.018739311,"about_ca_topic_score_gemma":0.48130196,"teacher_disagreement_score":0.46256268,"about_ca_system_score_codex":6.5778653e-7,"about_ca_system_score_gemma":0.00027661843,"threshold_uncertainty_score":0.987795},"labels":[],"label_agreement":null},{"id":"W2127682214","doi":"10.1139/e05-112","title":"Origin and orogenic role of the Chain Lakes massif, Maine and Quebec","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Massif; Geology; Devonian; Laurentia; Ordovician; Paleozoic; Geochemistry; Paleontology; Monazite; Sedimentary rock; Metamorphic rock; Precambrian; Zircon","score_opus":0.007578589957196074,"score_gpt":0.16544177982827063,"score_spread":0.15786318987107456,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127682214","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99233174,0.004020291,0.0000017299577,0.0014908845,0.00005165143,0.000023276974,0.000015414684,9.785387e-7,0.0020640392],"genre_scores_gemma":[0.9993734,0.000020262403,0.00020191465,0.00010177665,0.000052782478,3.9558294e-8,7.5305996e-7,4.1690734e-7,0.00024865748],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99930906,0.000039765157,0.00018659339,0.00009709974,0.00016187252,0.00020558148],"domain_scores_gemma":[0.99949306,0.000069238245,0.00011655011,0.000046739802,0.00004255735,0.00023187046],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00036910363,0.000062143314,0.00013563746,0.00008969282,0.00020527349,0.00005885034,0.00020033342,0.000027501046,0.0011145602],"category_scores_gemma":[0.00006038855,0.000031927124,0.00004921632,0.00034281085,0.00080505287,0.000110819536,0.0000055216697,0.00008047465,0.00000239794],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000015816053,0.0000014320367,0.9964796,0.0000019370623,0.0000042751303,0.000004998123,0.00003257754,0.00030483375,0.00025701683,0.00046879967,0.00002279393,0.0024201693],"study_design_scores_gemma":[0.00006695507,0.0000629816,0.98151416,0.000012139886,0.000013698548,0.000054388034,0.00020930968,0.00086020125,0.00043424076,0.013128757,0.0035901929,0.000052965886],"about_ca_topic_score_codex":0.22282793,"about_ca_topic_score_gemma":0.9545476,"teacher_disagreement_score":0.7317196,"about_ca_system_score_codex":5.7690283e-7,"about_ca_system_score_gemma":0.000258694,"threshold_uncertainty_score":0.99979854},"labels":[],"label_agreement":null},{"id":"W2127867400","doi":"10.1139/e00-002","title":"A U-Pb and <sup>40</sup>Ar/<sup>39</sup>Ar time scale for the Jurassic","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":187,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Paleontology; Radiometric dating; Stage (stratigraphy); Ammonite; Cretaceous; Geochronology; Orogeny; Boundary (topology); Tectonics","score_opus":0.01154429532316867,"score_gpt":0.1819033023326346,"score_spread":0.17035900700946593,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127867400","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9848888,0.0023399778,0.000020047779,0.0071952203,0.0000553919,0.00012164806,0.000097443204,0.0000068049217,0.0052746646],"genre_scores_gemma":[0.9950453,0.00012866828,0.0008742184,0.0011179039,0.00026261536,8.488337e-7,0.0000072357047,0.00000231228,0.0025608856],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99822736,0.00007734513,0.00038066527,0.00026439675,0.0003712339,0.0006789935],"domain_scores_gemma":[0.99823016,0.00046067676,0.0001253083,0.00013987946,0.00010883675,0.000935162],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010032168,0.00017913664,0.00031619475,0.00017478011,0.00097239146,0.0003162928,0.0006845697,0.00008045696,0.023428695],"category_scores_gemma":[0.00017040917,0.00009859727,0.00019305995,0.00066986564,0.001146555,0.00037142562,0.000007887693,0.00023147621,0.0002660794],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000102671234,0.000028749133,0.7052442,0.0000220054,0.00011973306,0.00009077677,0.0013995003,0.1205414,0.00008183254,0.00007657112,0.005697923,0.16659467],"study_design_scores_gemma":[0.0007513625,0.0012317871,0.5584432,0.0000878686,0.0002169527,0.0004945313,0.0016013812,0.23502871,0.00016695261,0.012268914,0.1890818,0.0006265249],"about_ca_topic_score_codex":0.0115681635,"about_ca_topic_score_gemma":0.07264485,"teacher_disagreement_score":0.18338388,"about_ca_system_score_codex":0.000002162635,"about_ca_system_score_gemma":0.00044200782,"threshold_uncertainty_score":0.9950139},"labels":[],"label_agreement":null},{"id":"W2128008645","doi":"10.1139/cjes-2014-0079","title":"Three-dimensional unified geological model of the Milk River Transboundary Aquifer (Alberta, Canada – Montana, USA)","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Modeling and Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Institut National de la Recherche Scientifique; Geological Survey of Canada","funders":"U.S. Geological Survey","keywords":"Aquifer; Geology; Hydrogeology; Groundwater; Hydrology (agriculture); Geochemistry; Geomorphology","score_opus":0.044889506326609,"score_gpt":0.20107960914900788,"score_spread":0.15619010282239887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128008645","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931279,0.0006681007,0.00025696174,0.0031060001,0.00041878514,0.00004408765,0.000050224924,0.0000012280007,0.0023267441],"genre_scores_gemma":[0.99755234,0.000004110971,0.0013158711,0.00071683276,0.000057237754,8.388946e-8,0.0000022354538,0.0000012349124,0.0003500658],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9982281,0.00008280671,0.00038815307,0.0001845711,0.00069677667,0.0004196338],"domain_scores_gemma":[0.99846727,0.00012849977,0.00019695604,0.00013545882,0.00023834486,0.00083347206],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00080018595,0.00012738946,0.0002690264,0.00012545937,0.0003959838,0.000046785713,0.0007333587,0.00006981934,0.0008909167],"category_scores_gemma":[0.0002326051,0.000069345966,0.00013523259,0.00046915203,0.0009303978,0.00018409643,0.000008157442,0.00023230976,0.000010483654],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000074377917,0.0000026517698,0.42340824,9.987306e-7,0.0000107254655,0.000017233753,0.00006977013,0.57550293,0.0000021893745,0.000073925185,0.00053751766,0.00036639412],"study_design_scores_gemma":[0.00023981727,0.00021114039,0.47974533,0.000027198126,0.00004257658,0.000075088596,0.00014094188,0.5122819,0.000026862077,0.005315554,0.0017290349,0.00016454948],"about_ca_topic_score_codex":0.9714006,"about_ca_topic_score_gemma":0.9996813,"teacher_disagreement_score":0.06322101,"about_ca_system_score_codex":0.0000056047584,"about_ca_system_score_gemma":0.0076083154,"threshold_uncertainty_score":0.9980176},"labels":[],"label_agreement":null},{"id":"W2128310247","doi":"10.1139/e02-003","title":"Variation in plagioclase clouding intensity in Matachewan dykes: evidence for the exhumation history of the northern margin of the Sudbury Igneous Complex","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Plagioclase; Geochemistry; Archean; Igneous rock; Gneiss; Metamorphism; Mafic; Anorthosite; Petrology; Crust; Metamorphic rock; Paleontology; Quartz","score_opus":0.08716620699508419,"score_gpt":0.2155769017009599,"score_spread":0.12841069470587568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128310247","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950112,0.0018425746,0.000022118607,0.002437165,0.00024164723,0.0001088944,0.000011705417,6.461543e-7,0.0003240191],"genre_scores_gemma":[0.99957347,0.00002383469,0.00010695717,0.00020260026,0.000026945325,2.8970737e-7,4.834147e-7,5.841266e-7,0.00006484064],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990054,0.000097107666,0.00036373793,0.00009944988,0.00024925036,0.000185088],"domain_scores_gemma":[0.99890715,0.0004442206,0.00033970326,0.00011141504,0.00012019484,0.00007732286],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011266139,0.00006274209,0.00015927054,0.00011094281,0.00014034112,0.000018323084,0.0005890105,0.000032736047,0.0010395168],"category_scores_gemma":[0.0007021982,0.000028951845,0.00010277139,0.0005051502,0.00056733936,0.00014921458,0.000009335714,0.00014466592,0.0000018334943],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000114622335,0.000005977218,0.9752403,0.000009671415,0.000005311184,0.0000021034666,0.0015152089,0.021175636,0.000213036,0.00002627432,0.000105137246,0.0016899077],"study_design_scores_gemma":[0.0000813343,0.000052574356,0.9554862,0.00008965743,0.000013148428,0.000012053646,0.00050850614,0.04232348,0.000053726817,0.0011106295,0.00022807912,0.00004061511],"about_ca_topic_score_codex":0.07492764,"about_ca_topic_score_gemma":0.7415144,"teacher_disagreement_score":0.66658676,"about_ca_system_score_codex":0.00001449432,"about_ca_system_score_gemma":0.00029555126,"threshold_uncertainty_score":0.9998737},"labels":[],"label_agreement":null},{"id":"W2128333994","doi":"10.1139/e01-091","title":"Augmented and reassessed U–Pb geochronological data from the Labradorian–Grenvillian front in the Smokey archipelago, eastern Labrador","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; St. Mary's University; Government of Newfoundland and Labrador; Royal Ontario Museum","funders":"","keywords":"Geology; Metamorphism; Pegmatite; Geochemistry; Gneiss; Monazite; Rodinia; Mafic; Outcrop; Metamorphic rock; Felsic; Laurentia; Zircon; Geomorphology; Craton; Paleontology; Paleozoic; Tectonics","score_opus":0.06292754168688236,"score_gpt":0.22100636723288497,"score_spread":0.1580788255460026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128333994","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9793012,0.004239753,0.000012675636,0.014339058,0.00015326907,0.0000704662,0.00015562691,0.00000285859,0.0017250564],"genre_scores_gemma":[0.9976081,0.00012861444,0.0005050725,0.0014981547,0.00018170617,2.2408089e-7,0.000024891078,9.323469e-7,0.000052299394],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998322,0.00024865105,0.00033249275,0.0002918575,0.00037075309,0.0004342141],"domain_scores_gemma":[0.99854463,0.00060495734,0.00015268155,0.00029330075,0.00003437365,0.00037005643],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011231581,0.0001321116,0.0002190167,0.00009711114,0.0003971109,0.00029141834,0.0017081434,0.00005742702,0.010601038],"category_scores_gemma":[0.00042504322,0.00005834934,0.000054119606,0.00044063435,0.0009464095,0.00032478283,0.000031186384,0.000354556,0.000095034295],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006782747,0.000012312925,0.983347,0.0000013950067,0.000018277606,0.00013737084,0.00057596585,0.00013032054,0.000013249373,0.000039044484,0.0009463561,0.014771916],"study_design_scores_gemma":[0.0001920644,0.00014481887,0.97677726,0.000024721789,0.000024787496,0.000056604888,0.0013711775,0.00961628,0.0000056160625,0.004536455,0.007147972,0.0001022572],"about_ca_topic_score_codex":0.1515286,"about_ca_topic_score_gemma":0.8667003,"teacher_disagreement_score":0.7151717,"about_ca_system_score_codex":0.0000012734238,"about_ca_system_score_gemma":0.00012778421,"threshold_uncertainty_score":0.9903034},"labels":[],"label_agreement":null},{"id":"W2128405974","doi":"10.1139/e09-068","title":"A flowline map of glaciated Canada based on remote sensing dataThis paper is accompanied by a large foldout map entitled <i>A flowline map of glaciated Canada based on remote sensing</i> <i>data</i> (see pocket on back cover).","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Drumlin; Landform; Glacial landform; Moraine; Ice sheet; Terrain; Remote sensing; Glacier; Glaciology; Geomorphology; Shuttle Radar Topography Mission; Ice stream; Cryosphere; Paleontology; Digital elevation model; Oceanography; Cartography; Sea ice; Stratigraphy; Geography","score_opus":0.01746526616988905,"score_gpt":0.22731621722400241,"score_spread":0.20985095105411336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128405974","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9738231,0.0003765915,0.00016466586,0.014826394,0.0032724238,0.00041882513,0.004623389,0.000011357476,0.0024832692],"genre_scores_gemma":[0.9875518,0.0000078585745,0.0026136625,0.008551897,0.000113562855,2.153312e-8,0.00061456475,0.000012623462,0.0005340243],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9953351,0.00048593082,0.0009597071,0.0006610641,0.0013066815,0.0012515206],"domain_scores_gemma":[0.9958841,0.00094310625,0.0006977339,0.0008255591,0.00049943326,0.001150023],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0025400273,0.00040367458,0.00081261405,0.0005278203,0.000606498,0.00009496582,0.0011959313,0.00024565254,0.009063649],"category_scores_gemma":[0.00066001277,0.0003385329,0.000119777724,0.0007355764,0.00065900286,0.00026574248,0.000027786235,0.0010411204,0.000111951944],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017514224,0.000101954916,0.66063166,0.00032432846,0.0002662038,0.0026791256,0.00027529214,0.01508579,0.0018377427,0.000009344603,0.31395647,0.0030806526],"study_design_scores_gemma":[0.003539763,0.0011717032,0.0390138,0.000734381,0.000097202275,0.00015684219,0.00018295537,0.78878736,0.0041971067,0.00008953197,0.16121906,0.0008102723],"about_ca_topic_score_codex":0.9530765,"about_ca_topic_score_gemma":0.9995696,"teacher_disagreement_score":0.7737016,"about_ca_system_score_codex":0.000016244687,"about_ca_system_score_gemma":0.014958351,"threshold_uncertainty_score":0.99990666},"labels":[],"label_agreement":null},{"id":"W2129016148","doi":"10.1139/e03-053","title":"Little Ice Age glacial activity in the Mt. Waddington area, British Columbia Coast Mountains, Canada","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Inter-American Institute for Global Change Research","keywords":"Moraine; Glacier; Glacial period; Geology; Physical geography; Glacier morphology; Climate change; Geomorphology; Climatology; Geography; Oceanography; Cryosphere; Ice stream; Sea ice","score_opus":0.02029865486434565,"score_gpt":0.21651968096957833,"score_spread":0.19622102610523268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129016148","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98342264,0.0006515359,0.000001938038,0.0006520477,0.00054190744,0.00008353644,0.00004170781,0.0000013406992,0.014603331],"genre_scores_gemma":[0.9989917,0.000030905514,0.00006125948,0.0005134978,0.00004809786,3.389366e-7,0.0000032394482,0.0000011484838,0.00034979882],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981434,0.00043385458,0.00022075415,0.00017035476,0.0003828749,0.00064876635],"domain_scores_gemma":[0.9989343,0.0003793355,0.000114654475,0.000096254706,0.00007319898,0.0004022537],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0021811018,0.00007718828,0.00019294758,0.000115636714,0.0008704322,0.00040805375,0.00059587276,0.00007497801,0.0026268656],"category_scores_gemma":[0.00049511046,0.00007454783,0.000042547654,0.00061462435,0.0007624748,0.00028473482,0.0000032878527,0.00045538734,0.000009659407],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000038851613,0.0000039101274,0.9960354,0.0000029553012,0.000004361304,0.0012362205,0.0001665205,0.00021282225,9.666594e-7,0.00001912182,0.0018102762,0.0005035627],"study_design_scores_gemma":[0.00016470454,0.000121493766,0.9792612,0.000021417709,0.0000040604973,0.0011158341,0.0009173679,0.000101551894,0.000004896129,0.00035144648,0.017844765,0.000091222566],"about_ca_topic_score_codex":0.98501426,"about_ca_topic_score_gemma":0.99999684,"teacher_disagreement_score":0.016774159,"about_ca_system_score_codex":0.000002734524,"about_ca_system_score_gemma":0.005971667,"threshold_uncertainty_score":0.99966353},"labels":[],"label_agreement":null},{"id":"W2129081636","doi":"10.1139/e00-123","title":"Kilometre-scale folding in the Teslin zone, northern Canadian Cordillera, and its tectonic implications for the accretion of the Yukon-Tanana terrane to North America: Discussion","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Lineation; Tectonite; Shear zone; Terrane; Paleontology; Fold (higher-order function); Tectonics","score_opus":0.022387087741512077,"score_gpt":0.2195641191866157,"score_spread":0.19717703144510362,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129081636","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95955753,0.00085386675,0.00004363519,0.03869783,0.00007778302,0.00020602896,0.00007291957,0.0000010501495,0.00048933644],"genre_scores_gemma":[0.9988239,0.00007168149,0.000107736305,0.0008829206,0.000053650114,0.0000019472739,0.0000039999486,0.0000011273052,0.000053031952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989282,0.000067332476,0.0002804231,0.00015497116,0.0001980475,0.00037105748],"domain_scores_gemma":[0.998944,0.00027689728,0.00015285659,0.00013112943,0.00010837419,0.00038677503],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005046766,0.000091452566,0.00016212625,0.00024113161,0.00073410885,0.00008191609,0.00070445705,0.000029031775,0.00055509293],"category_scores_gemma":[0.0002942667,0.000033967663,0.00009180774,0.0018677121,0.00029928892,0.00012438951,0.000007927215,0.00014663606,0.0000048165966],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004501857,0.0000035578744,0.97324294,0.0000018242582,0.000007249378,0.0000017762405,0.00040093827,0.005251632,0.000049145143,0.0000110957835,0.000048249203,0.020977085],"study_design_scores_gemma":[0.00006542873,0.00013970908,0.991205,0.000020151349,0.000023456365,0.000025969583,0.001023645,0.0024531672,0.00001674676,0.00033504138,0.004625579,0.00006613631],"about_ca_topic_score_codex":0.27473456,"about_ca_topic_score_gemma":0.99551606,"teacher_disagreement_score":0.7207815,"about_ca_system_score_codex":0.000005169971,"about_ca_system_score_gemma":0.0004612355,"threshold_uncertainty_score":0.730095},"labels":[],"label_agreement":null},{"id":"W2129084534","doi":"10.1139/cjes-2014-0062","title":"Taphonomy of the Danek Bonebed: a monodominant <i>Edmontosaurus</i> (Hadrosauridae) bonebed from the Horseshoe Canyon Formation, Alberta","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"University of Texas at El Paso","keywords":"Geology; Taphonomy; Canyon; Paleontology; Horseshoe (symbol); Assemblage (archaeology); Geomorphology","score_opus":0.009904284647334576,"score_gpt":0.17862971474204567,"score_spread":0.16872543009471108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129084534","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9834535,0.0023045249,0.00010599842,0.005733496,0.0012025675,0.000115617724,0.00008736445,0.000002149599,0.0069947736],"genre_scores_gemma":[0.99834794,0.000038639195,0.00030924892,0.0009921391,0.00018167715,4.4031307e-7,0.000007967953,0.0000014430966,0.00012051044],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998395,0.00031743248,0.0004716484,0.00016062811,0.00023223406,0.0004230251],"domain_scores_gemma":[0.9982927,0.000617056,0.0004731085,0.00021825619,0.000100037745,0.0002988378],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001167927,0.00012936788,0.0002452841,0.00010916767,0.00080627826,0.000054637047,0.0009886547,0.00008683502,0.0005292007],"category_scores_gemma":[0.00039653605,0.00006697162,0.00012416017,0.0003726986,0.001429381,0.00062726147,0.000009783877,0.00022843892,0.000030001855],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020454227,0.0000036753725,0.9931353,0.0000024396847,0.000016351813,0.000004690263,0.0008155095,0.0010169087,0.000079641555,0.00038744533,0.002191104,0.0023265253],"study_design_scores_gemma":[0.00021622582,0.00016654578,0.9345108,0.000037580605,0.000023778506,0.00015526492,0.00045621855,0.0021089383,0.00018631417,0.0017017344,0.06033411,0.00010248563],"about_ca_topic_score_codex":0.22077426,"about_ca_topic_score_gemma":0.949221,"teacher_disagreement_score":0.7284467,"about_ca_system_score_codex":0.0000032192138,"about_ca_system_score_gemma":0.0011237217,"threshold_uncertainty_score":0.78441465},"labels":[],"label_agreement":null},{"id":"W2129109111","doi":"10.1139/e06-046","title":"The basal unconformity of the Nanaimo Group, southwestern British Columbia: a Late Cretaceous storm-swept rocky shoreline","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Simon Fraser University","keywords":"Geology; Cove; Unconformity; Marine transgression; Facies; Shore; Cretaceous; Paleontology; Rocky shore; Intertidal zone; Geomorphology; Structural basin; Oceanography","score_opus":0.009742226143963976,"score_gpt":0.1776963052017958,"score_spread":0.16795407905783183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129109111","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99169946,0.0029354845,0.000023347922,0.00068713224,0.00054062105,0.000081320904,0.00008546087,0.0000031159557,0.003944062],"genre_scores_gemma":[0.99878156,0.000053351832,0.00012414106,0.00024907803,0.0000996086,1.9593394e-7,0.000003028981,0.0000012073083,0.0006878546],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986498,0.00006625745,0.000433583,0.00010146641,0.00037236037,0.0003765405],"domain_scores_gemma":[0.9989926,0.00015185087,0.00032187634,0.00010354255,0.00019428141,0.00023581028],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009957306,0.00007470386,0.00015496035,0.000052274216,0.001363686,0.00065114826,0.00072918716,0.00005237916,0.0011088772],"category_scores_gemma":[0.00015605826,0.000048897222,0.000102996746,0.00052163546,0.00086963567,0.00038813648,0.0000096322265,0.00019339497,0.0000122215915],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000022592396,0.000003259332,0.98369205,0.000005298015,0.000005773788,0.000013772754,0.00008073944,0.004510183,0.000001100038,0.000019049417,0.0014282905,0.010238218],"study_design_scores_gemma":[0.000107198044,0.00019945152,0.96463764,0.000035198726,0.000010457288,0.00014222218,0.0003589767,0.0009008141,0.000005202073,0.0026684247,0.03085384,0.00008060701],"about_ca_topic_score_codex":0.41949737,"about_ca_topic_score_gemma":0.9971399,"teacher_disagreement_score":0.5776425,"about_ca_system_score_codex":0.0000018526637,"about_ca_system_score_gemma":0.0007481125,"threshold_uncertainty_score":0.9999364},"labels":[],"label_agreement":null},{"id":"W2129137579","doi":"10.1139/e07-041","title":"A revision of the stratigraphic nomenclature of the Cambrian–Ordovician strata of the Philipsburg tectonic slice, southern Quebec","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Regina","funders":"","keywords":"Ordovician; Unconformity; Geology; Paleontology; Group (periodic table); Tectonics","score_opus":0.014006380932419515,"score_gpt":0.2114211832417547,"score_spread":0.1974148023093352,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129137579","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.983762,0.0062335785,0.000004833359,0.00073386764,0.000580232,0.00015882764,0.00012744787,0.0000012050174,0.008398009],"genre_scores_gemma":[0.9996718,0.00002101235,0.00009505615,0.000075317104,0.000057115336,4.00932e-8,2.5751174e-7,8.1835253e-7,0.00007857491],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99808097,0.0002029291,0.0006179409,0.00015144338,0.0005480257,0.00039871715],"domain_scores_gemma":[0.99820685,0.0001741564,0.00088375923,0.00034658742,0.00015716071,0.00023146415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020032625,0.00013382798,0.00027091606,0.00021541477,0.0005679412,0.000036431848,0.0015738698,0.00011360338,0.00017768962],"category_scores_gemma":[0.00017449379,0.000060876573,0.00029153947,0.0015343935,0.0024659778,0.00020878151,0.000004478903,0.00041909708,4.9914684e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010960816,0.00000582822,0.9898535,0.00001505704,0.000022393713,0.0000034097911,0.00090867694,0.00009344763,0.0003522762,0.0003792864,0.000031987296,0.008323172],"study_design_scores_gemma":[0.00012139742,0.00014587345,0.996269,0.00022232547,0.000029432002,0.000046500438,0.0015639275,0.00003079119,0.00050634454,0.0004886908,0.00050489925,0.00007085919],"about_ca_topic_score_codex":0.06986082,"about_ca_topic_score_gemma":0.97746134,"teacher_disagreement_score":0.9076005,"about_ca_system_score_codex":0.0000017152081,"about_ca_system_score_gemma":0.0026497138,"threshold_uncertainty_score":0.93633306},"labels":[],"label_agreement":null},{"id":"W2129452725","doi":"10.1139/e2012-065","title":"Geochronology and geochemistry of the enderbite series in the Lapland Granulite Belt: generation, tectonic setting, and correlation of the belt<sup>1</sup>NORDSIM Publication No. 322.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Suomen Kulttuurirahasto","keywords":"Zircon; Geology; Geochemistry; Granulite; Archean; Metamorphic rock; Igneous rock; Anatexis; Geochronology; Diorite; Felsic; Mafic; Crust; Partial melting; Facies; Geomorphology","score_opus":0.010047091982603914,"score_gpt":0.1813428397091292,"score_spread":0.17129574772652528,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129452725","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99212265,0.0022739707,0.0000039078122,0.00437559,0.00007864348,0.00006329234,0.000028193386,7.894711e-7,0.0010529347],"genre_scores_gemma":[0.9994447,0.000053262527,0.00010526495,0.00025364157,0.00007617879,3.5098216e-7,0.00000929666,5.7008134e-7,0.000056722078],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990421,0.00013619395,0.00028865683,0.00010295922,0.0002043174,0.00022576546],"domain_scores_gemma":[0.9992372,0.00013516254,0.0002699852,0.00010630133,0.00013070139,0.00012066374],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010005846,0.0000749877,0.00013129284,0.00007454437,0.00031779657,0.000052492927,0.00031224886,0.00005821605,0.00035582567],"category_scores_gemma":[0.00044285433,0.000034460558,0.0000462459,0.00043556085,0.000886745,0.000299639,0.000012930437,0.00017435517,0.000001149271],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000025789363,0.0000036034994,0.99713594,0.0000071067693,0.000005934327,3.1940112e-7,0.0006207237,0.00093426154,0.00021923134,0.00008693394,0.00010854707,0.0008748331],"study_design_scores_gemma":[0.000092632064,0.00005660051,0.99214095,0.000017507702,0.0000202381,0.00009424442,0.00040209788,0.004174529,0.0004544891,0.0011370388,0.0013595214,0.00005018163],"about_ca_topic_score_codex":0.007820746,"about_ca_topic_score_gemma":0.113997065,"teacher_disagreement_score":0.10617632,"about_ca_system_score_codex":0.0000014467354,"about_ca_system_score_gemma":0.00021842305,"threshold_uncertainty_score":0.9987863},"labels":[],"label_agreement":null},{"id":"W2129565623","doi":"10.1139/e05-080","title":"The electrical resistivity structure of Archean to Tertiary lithosphere along 3200 km of SNORCLE profiles, northwestern Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Terrane; Magnetotellurics; Archean; Lithosphere; Craton; Shear zone; Crust; Transect; Basement; Subduction; Fault (geology); Seismology; North American Plate; Tectonics; Electrical resistivity and conductivity; Geochemistry; Archaeology","score_opus":0.01015931342128221,"score_gpt":0.21406422789664722,"score_spread":0.20390491447536502,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129565623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962305,0.0012003622,0.000034035955,0.0018622251,0.00018355857,0.00009606732,0.000095686744,0.0000014811795,0.00029612548],"genre_scores_gemma":[0.99631524,0.000010379131,0.003141901,0.0002626848,0.00016321515,1.08179705e-7,0.0000015603655,0.0000018143867,0.00010308249],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99813527,0.0001835839,0.00045132983,0.000167856,0.000535167,0.0005267854],"domain_scores_gemma":[0.9981746,0.0005046457,0.00024872262,0.00013314885,0.00017771631,0.00076117006],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000645592,0.0001167444,0.00025887717,0.000101066,0.00034215776,0.00005499116,0.00064941234,0.00004246106,0.00022785297],"category_scores_gemma":[0.00036876678,0.00006988442,0.00007585585,0.0009046711,0.00034527128,0.0001638773,0.0000075738194,0.00025852962,0.0000025630977],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023922848,0.0000062471254,0.69852877,0.0000090337535,0.000014291757,0.00001853812,0.00013107753,0.0029928095,0.0001808106,0.00007030368,0.00038607547,0.29763812],"study_design_scores_gemma":[0.000075065764,0.0003353054,0.98796046,0.000027187016,0.00000936467,0.000028140563,0.00006644482,0.0006988592,0.0029545878,0.0004927848,0.007257002,0.000094805066],"about_ca_topic_score_codex":0.7972728,"about_ca_topic_score_gemma":0.9976217,"teacher_disagreement_score":0.29754332,"about_ca_system_score_codex":0.0000064256474,"about_ca_system_score_gemma":0.0039134757,"threshold_uncertainty_score":0.6942338},"labels":[],"label_agreement":null},{"id":"W2129681004","doi":"10.1139/e03-069","title":"Siliceous shrubs in hot springs from Yellowstone National Park, Wyoming, U.S.A.","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Park Service; Johnson Space Center; National Aeronautics and Space Administration","keywords":"Geology; Hot spring; Precipitation; Microbial mat; Cyanobacteria; Carbonate; Geochemistry; Paleontology; Chemistry; Bacteria","score_opus":0.03103496068236712,"score_gpt":0.24455795475401715,"score_spread":0.21352299407165004,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129681004","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9694755,0.0021378503,0.0000050646217,0.00044085688,0.00050080277,0.000047073907,0.00001515919,0.0000020393707,0.02737565],"genre_scores_gemma":[0.99844843,0.00004070979,0.00090221287,0.00032515157,0.00005611934,1.7858605e-7,0.0000029853059,0.0000012276323,0.00022297754],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99845,0.0001930185,0.0003010427,0.00018743526,0.00035143818,0.00051708973],"domain_scores_gemma":[0.99884546,0.00036167554,0.00012382142,0.00006755155,0.000109773704,0.0004917486],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018438584,0.00009435355,0.00019102979,0.00051933125,0.00030289264,0.00006661234,0.00041626365,0.00009197846,0.0050881454],"category_scores_gemma":[0.0006255413,0.000078574114,0.000052452404,0.0005111191,0.0011011945,0.00031010105,0.0000027639985,0.0003365867,0.0002117362],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000095170135,0.0000036362615,0.99750173,0.0000013788961,0.000006387547,0.00020997795,0.00027671043,0.0014816382,0.0000066392877,0.00028367332,0.00009488437,0.00012384176],"study_design_scores_gemma":[0.0002281085,0.000115010065,0.98741657,0.000020739673,0.0000032528853,0.00026810414,0.00040729297,0.00040404117,0.00008526957,0.0025906807,0.008361142,0.00009981734],"about_ca_topic_score_codex":0.019068316,"about_ca_topic_score_gemma":0.8166068,"teacher_disagreement_score":0.7975385,"about_ca_system_score_codex":0.0000011342747,"about_ca_system_score_gemma":0.0023175876,"threshold_uncertainty_score":0.99582136},"labels":[],"label_agreement":null},{"id":"W2129729715","doi":"10.1139/cjes-2012-0151","title":"Late Holocene glacial activity at Bromley Glacier, Cambria Icefield, northern British Columbia Coast Mountains, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Holocene; Geology; Glacier; Ice field; Glacial period; Radiocarbon dating; Physical geography; Glacier mass balance; Geomorphology; Oceanography; Paleontology; Geography","score_opus":0.0122987498181486,"score_gpt":0.1980718824730323,"score_spread":0.1857731326548837,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129729715","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934007,0.00075252267,0.0000015494204,0.0011251939,0.00097037066,0.00013650321,0.00008495341,0.0000049825708,0.0035232236],"genre_scores_gemma":[0.996926,0.00004718176,0.00007272032,0.00053516706,0.00013125966,6.38409e-7,0.00000907946,0.0000029167768,0.0022750287],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99780816,0.00020940597,0.00031820597,0.00027097104,0.00045783585,0.0009354159],"domain_scores_gemma":[0.99802125,0.00020775237,0.00021857324,0.00013504497,0.00027147075,0.0011458839],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007659862,0.00012611695,0.00030678525,0.00012012874,0.001504302,0.00049432635,0.0006591303,0.00013824069,0.009121648],"category_scores_gemma":[0.0002228319,0.00014316477,0.000073819036,0.000430162,0.0010331881,0.0005339126,0.000016421382,0.00042751856,0.00014166704],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007391203,0.0000035744536,0.9939345,0.000005815209,0.000015418449,0.00044314118,0.000058547535,0.00030950177,0.0000050666636,8.751549e-7,0.002968288,0.0022478902],"study_design_scores_gemma":[0.0002531975,0.0001905795,0.99475056,0.000021123971,0.000008668746,0.001115467,0.0001507955,0.0004056422,0.000011730945,0.00011962201,0.0028046712,0.00016791609],"about_ca_topic_score_codex":0.9966135,"about_ca_topic_score_gemma":0.99999666,"teacher_disagreement_score":0.008979981,"about_ca_system_score_codex":0.0000060021152,"about_ca_system_score_gemma":0.0061716586,"threshold_uncertainty_score":0.9997956},"labels":[],"label_agreement":null},{"id":"W2129777455","doi":"10.1139/e02-089","title":"Kimberlites from the Wawa area, Ontario","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; Stornoway Diamond (Canada)","funders":"","keywords":"Kimberlite; Geology; Enstatite; Geochemistry; Pyrope; Xenolith; Olivine; Augite; Ilmenite; Mantle (geology); Diopside; Eclogite; Mineralogy; Meteorite; Plagioclase; Subduction; Chondrite","score_opus":0.029713585867412972,"score_gpt":0.16701064667371526,"score_spread":0.1372970608063023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129777455","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9657545,0.0027640846,0.0000044603626,0.004595597,0.00023137755,0.00002239329,0.000022061293,0.00000231926,0.026603224],"genre_scores_gemma":[0.99740344,0.000024452538,0.0004573515,0.0011407111,0.00013601338,5.3829783e-8,0.0000029679104,4.8808255e-7,0.000834541],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989764,0.00004519539,0.00023272753,0.00013557223,0.0002734164,0.0003366873],"domain_scores_gemma":[0.9989259,0.00027765473,0.000117955315,0.00009197829,0.000069145295,0.0005173124],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00036170316,0.00008651702,0.00015064247,0.000072059214,0.0004319987,0.00018249267,0.0005982852,0.000034948014,0.13452037],"category_scores_gemma":[0.0001709902,0.00004257749,0.00011784054,0.0003921204,0.0005439366,0.00020843327,0.0000041764806,0.00020812653,0.0002615917],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.763131e-7,0.0000020934337,0.9946461,1.8852757e-7,0.000010580956,0.000032732703,0.00031747838,0.0006212731,0.0000047925237,0.000023858292,0.0012111737,0.0031287759],"study_design_scores_gemma":[0.00005880489,0.000101937265,0.94345844,0.0000110035235,0.000017568485,0.000032626845,0.00019529747,0.0012101014,0.000029995614,0.0075978558,0.047206018,0.0000803832],"about_ca_topic_score_codex":0.67652786,"about_ca_topic_score_gemma":0.99431163,"teacher_disagreement_score":0.31778377,"about_ca_system_score_codex":0.0000015247325,"about_ca_system_score_gemma":0.0002521013,"threshold_uncertainty_score":0.8662708},"labels":[],"label_agreement":null},{"id":"W2129935800","doi":"10.1139/e10-081","title":"<i>Blasisaurus canudoi</i>gen. et sp. nov., a new lambeosaurine dinosaur (Hadrosauridae) from the Latest Cretaceous of Arén (Huesca, Spain)","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Koninklijk Belgisch Instituut voor Natuurwetenschappen; Ministerio de Ciencia e Innovación; Eusko Jaurlaritza","keywords":"Paleontology; Cretaceous; Biological dispersal; Geology; Synonym (taxonomy); Archipelago; Zoology; Biology; Genus; Population; Demography","score_opus":0.01597295008321991,"score_gpt":0.2140124816037703,"score_spread":0.19803953152055037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129935800","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9769316,0.00407541,0.000018942717,0.008954243,0.0019419973,0.000094309275,0.00024257529,0.0000069788393,0.007733943],"genre_scores_gemma":[0.99630475,0.00010693365,0.0014623916,0.0013332817,0.0005288287,1.9598761e-7,0.00001955634,0.0000027908238,0.00024128727],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981361,0.00019078319,0.00049729756,0.0002619172,0.0003133341,0.0006005368],"domain_scores_gemma":[0.99784166,0.0006255133,0.00040031952,0.00023649284,0.00012779671,0.000768212],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013084322,0.00019050202,0.00033869303,0.00020468386,0.0004935024,0.000082938175,0.001030593,0.0001635493,0.0035961089],"category_scores_gemma":[0.00044898136,0.0001229072,0.0001389201,0.0004669605,0.0016471721,0.0003978139,0.000011559268,0.0006210742,0.0000891548],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023623956,0.0000063635357,0.9941495,0.000002325246,0.000028880379,0.00010453746,0.00031139355,0.0008718643,0.00028330824,0.00021299117,0.0021941292,0.0018110581],"study_design_scores_gemma":[0.00025246487,0.00029359598,0.94331175,0.00003021335,0.000027115493,0.00047585712,0.00014828685,0.00033515677,0.00012351717,0.0015086484,0.05334118,0.00015222676],"about_ca_topic_score_codex":0.15926632,"about_ca_topic_score_gemma":0.9616199,"teacher_disagreement_score":0.8023536,"about_ca_system_score_codex":0.000001920514,"about_ca_system_score_gemma":0.0033987176,"threshold_uncertainty_score":0.99731475},"labels":[],"label_agreement":null},{"id":"W2130130348","doi":"10.1139/e07-069","title":"Quaternary stratigraphy and glacial history of the Peace River valley, northeast British ColumbiaThis article is one of a selection of papers published in this Special Issue on the theme <i>Geology of northeastern British Columbia and northwestern Alberta: diamonds, shallow gas, gravel, and glaciers</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Glacial period; Wisconsin glaciation; Quaternary; Ice sheet; Fluvial; Paleontology; Landform; Pleistocene; Glacial landform; Geomorphology; Moraine; Ice stream; Oceanography; Structural basin; Cryosphere","score_opus":0.012899624166487551,"score_gpt":0.1781230180304157,"score_spread":0.16522339386392815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130130348","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944161,0.0018005648,1.587389e-7,0.00042839517,0.00020738573,0.00015633415,0.00003782484,7.635646e-7,0.0029524632],"genre_scores_gemma":[0.99892133,0.0004434632,0.000038013328,0.000106673855,0.00006526937,5.029078e-7,0.0000012245807,0.0000020904533,0.0004214218],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99840945,0.0002738481,0.00046847813,0.00021369505,0.00032619474,0.00030836152],"domain_scores_gemma":[0.9988843,0.0002630004,0.000388223,0.00009995257,0.00016022865,0.00020429646],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00074593467,0.00008725648,0.00036000015,0.00013824119,0.0003317962,0.00006375124,0.0003124084,0.00009978803,0.0031602404],"category_scores_gemma":[0.00012289944,0.00008510026,0.000067761954,0.00037105312,0.0046781283,0.00025108556,0.000013680765,0.00026589737,5.4856434e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003960652,0.000021741791,0.99540484,0.000025044941,0.000028735987,0.000029406168,0.0031785003,0.00001425044,0.0000213971,0.0000046059718,0.0003246065,0.0009072426],"study_design_scores_gemma":[0.00040746288,0.00058170187,0.9969078,0.00009076493,0.00001633386,0.0006199502,0.0005200802,0.00018900126,0.000022676262,0.0001695062,0.00039971387,0.000075060714],"about_ca_topic_score_codex":0.6460389,"about_ca_topic_score_gemma":0.9975668,"teacher_disagreement_score":0.3515279,"about_ca_system_score_codex":0.0000018395738,"about_ca_system_score_gemma":0.000799223,"threshold_uncertainty_score":0.99803054},"labels":[],"label_agreement":null},{"id":"W2130292590","doi":"10.1139/e05-055","title":"Early Silurian (Wenlockian) δ<sup>13</sup>C profiles from the Cape Phillips Formation, Arctic Canada and their relation to biotic events","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University; University of Saskatchewan","funders":"Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; Geological Society of America; National Science Foundation","keywords":"Geology; Carbonate; Paleontology; Extinction event; Excursion; Arctic; Devonian; Weathering; Oceanography","score_opus":0.013964056824356232,"score_gpt":0.18478688756133557,"score_spread":0.17082283073697935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130292590","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9882225,0.0032450608,0.000024825724,0.0066796583,0.00021635447,0.00012601756,0.000106420965,0.000002932417,0.0013762489],"genre_scores_gemma":[0.9988389,0.000021945918,0.00043623828,0.00047368527,0.00020542271,2.9386504e-7,0.0000034875143,8.185636e-7,0.00001921856],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987579,0.0001226451,0.00032701358,0.00015793015,0.0002579013,0.00037660412],"domain_scores_gemma":[0.99878025,0.00024041696,0.00017974997,0.00010464797,0.000086779415,0.00060813845],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000584613,0.00012768744,0.00015751013,0.00016544771,0.0008660224,0.00014564156,0.0004068728,0.000054713968,0.00025336788],"category_scores_gemma":[0.00013690324,0.000078098135,0.00004454324,0.00036393575,0.00028233288,0.00076156703,0.0000014059681,0.00019888664,0.000009083715],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006445802,0.00000140042,0.97019005,0.000002076664,0.000014622468,0.000008345859,0.0022219045,0.002892574,0.0000036945992,0.000027148271,0.00021286926,0.0244189],"study_design_scores_gemma":[0.00011487825,0.00013148552,0.99356145,0.00005407168,0.000009944961,0.00007415288,0.001070591,0.002480534,0.000022901168,0.00067684386,0.0016961398,0.00010698307],"about_ca_topic_score_codex":0.7593147,"about_ca_topic_score_gemma":0.99791116,"teacher_disagreement_score":0.23859645,"about_ca_system_score_codex":0.0000050921203,"about_ca_system_score_gemma":0.001538314,"threshold_uncertainty_score":0.66608316},"labels":[],"label_agreement":null},{"id":"W2130513728","doi":"10.1139/e07-005","title":"Origin of iron-oxide and silicate melt rocks in Paleogene sediments of southern Ellesmere Island, Canadian Arctic Archipelago, Nunavut","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Paleontology","score_opus":0.021960427617597762,"score_gpt":0.21251952467890237,"score_spread":0.1905590970613046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130513728","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965646,0.0014080022,0.000013542181,0.00045979224,0.00011729612,0.000068190995,0.00008100634,7.198487e-7,0.0012868472],"genre_scores_gemma":[0.99948114,0.00010127822,0.00022990302,0.00012038107,0.000033686698,8.9714426e-8,0.000004089282,0.0000012004941,0.000028236458],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987553,0.00004355274,0.0004026772,0.00013595785,0.00022990706,0.00043260306],"domain_scores_gemma":[0.9989339,0.000097181604,0.00021291357,0.00006075026,0.00008702936,0.00060823985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010404561,0.0000938424,0.0002172051,0.00036213268,0.00018051619,0.000024259576,0.00022890698,0.000049008424,0.00069680007],"category_scores_gemma":[0.00010872302,0.00006809426,0.000040915696,0.00039761967,0.00043546327,0.00012463784,0.0000044943104,0.00012731813,0.000009703553],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013617372,0.0000029638302,0.9882482,0.000007674435,0.0000065606573,0.000029949328,0.00091624376,0.0028803207,0.000028576607,0.000009020042,0.00001275966,0.007844062],"study_design_scores_gemma":[0.00020439677,0.0002711326,0.99398,0.000051426123,0.000008030855,0.000027126942,0.0034006047,0.00030668802,0.0001814044,0.00048425715,0.0009958289,0.00008914234],"about_ca_topic_score_codex":0.70190984,"about_ca_topic_score_gemma":0.9987882,"teacher_disagreement_score":0.2968783,"about_ca_system_score_codex":0.0000043895116,"about_ca_system_score_gemma":0.00064530614,"threshold_uncertainty_score":0.7629472},"labels":[],"label_agreement":null},{"id":"W2130667048","doi":"10.1139/e04-040","title":"The PotsdamBeekmantown Group boundary, Nepean Formation type section (Ottawa, Ontario): a cryptic sequence boundary, not a conformable transition","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; BP (Canada); Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Ordovician; Unconformity; Geology; Paleontology; Diachronous; Group (periodic table); Section (typography); Conformable matrix; Sequence (biology); Type (biology); Facies; Conodont; Boundary (topology); Laurentia; Biostratigraphy; Sedimentary rock; Tectonics; Structural basin","score_opus":0.024892844444458963,"score_gpt":0.2122741623235173,"score_spread":0.18738131787905835,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130667048","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9868277,0.0007598852,0.00076883106,0.0021300076,0.001205301,0.0001393737,0.000018520523,0.000010954484,0.008139463],"genre_scores_gemma":[0.9981975,0.00007982272,0.00087545096,0.000578326,0.00011327982,4.0447168e-7,0.000017401448,0.0000014375838,0.00013638215],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9985788,0.00004885974,0.0004313687,0.00011482814,0.0003727179,0.00045346664],"domain_scores_gemma":[0.9989894,0.00006763705,0.0002552658,0.00008515313,0.00023064378,0.00037191567],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012657887,0.00011925186,0.0001351152,0.00020605949,0.0024719762,0.00090857234,0.00037266646,0.00006153574,0.0010027713],"category_scores_gemma":[0.000084927764,0.00007545285,0.0000679312,0.0005789429,0.00064556446,0.0023547139,0.0000027754586,0.0002660922,0.00007815257],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010899872,0.00011623996,0.232246,0.00032552058,0.00023428323,0.0007867561,0.06273792,0.5006346,0.0007680177,0.019816337,0.0037288773,0.17751548],"study_design_scores_gemma":[0.0010891929,0.003950853,0.51555693,0.0002169729,0.0000556141,0.0029832446,0.003853831,0.0065628625,0.0002988941,0.022610117,0.44227114,0.000550338],"about_ca_topic_score_codex":0.17590007,"about_ca_topic_score_gemma":0.9593028,"teacher_disagreement_score":0.78340274,"about_ca_system_score_codex":0.000020231408,"about_ca_system_score_gemma":0.0028547111,"threshold_uncertainty_score":0.9999105},"labels":[],"label_agreement":null},{"id":"W2130842457","doi":"10.1139/cjes-2012-0103","title":"Holocene environmental history of the Aishihik Region, Yukon, Canada","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; Arctic Institute of North America","keywords":"Deglaciation; Tundra; Holocene; Geology; Physical geography; Vegetation (pathology); Sediment; Loss on ignition; Climate change; Oceanography; Arctic; Geography; Geomorphology","score_opus":0.025481180089142838,"score_gpt":0.18667891997120892,"score_spread":0.1611977398820661,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130842457","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97985786,0.009016847,0.0000010459739,0.0011411044,0.0018235291,0.000038100585,0.000010798342,6.6370194e-7,0.008110027],"genre_scores_gemma":[0.99862015,0.00003490363,0.000049538616,0.0004620643,0.00008097642,6.421867e-8,9.781959e-7,9.0801916e-7,0.00075042807],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99879074,0.00015202991,0.00022210712,0.000079399244,0.0002904199,0.00046533212],"domain_scores_gemma":[0.9990513,0.00011969041,0.00018976956,0.00011010161,0.000029343695,0.00049984007],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007648016,0.000069386544,0.00013571797,0.00011346593,0.00024650645,0.000008042142,0.00055529753,0.00005151588,0.0018315576],"category_scores_gemma":[0.00011664652,0.000044260858,0.000051065428,0.00015892954,0.0015023237,0.0002332542,0.000006063082,0.00021931587,0.00001462018],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000030338722,0.0000022506708,0.99616486,0.0000022957972,0.00000596117,0.000022238277,0.00021923514,0.00013937747,0.0000014322032,0.000036580586,0.003242912,0.00015981834],"study_design_scores_gemma":[0.00006885447,0.00005507467,0.9751626,0.000009236458,0.0000063115504,0.0005390787,0.00027011885,0.00003109442,0.00004222491,0.000048965594,0.023714412,0.000051987266],"about_ca_topic_score_codex":0.39651284,"about_ca_topic_score_gemma":0.9763384,"teacher_disagreement_score":0.5798256,"about_ca_system_score_codex":0.0000045730512,"about_ca_system_score_gemma":0.0052756974,"threshold_uncertainty_score":0.9990809},"labels":[],"label_agreement":null},{"id":"W2130909494","doi":"10.1139/e10-048","title":"Magmatic and tectonic emplacement of the Pukaskwa batholith, Superior Province, Ontario, CanadaThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; University of Waterloo; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Batholith; Felsic; Geochemistry; Greenstone belt; Subduction; Lithosphere; Partial melting; Mantle (geology); Tectonics; Archean; Geochronology; Petrology; Seismology; Mafic","score_opus":0.01558789187133144,"score_gpt":0.16782433326287566,"score_spread":0.1522364413915442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130909494","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891219,0.0002722056,1.0543245e-7,0.0013957607,0.00007061993,0.0001224492,0.000050090457,3.939606e-7,0.00896644],"genre_scores_gemma":[0.9994898,0.000024133786,0.00024301777,0.00010388021,0.000020825406,3.9305357e-7,5.086258e-7,8.6263367e-7,0.000116581345],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99848694,0.00012292092,0.0006465103,0.00013927984,0.00033840374,0.00026595552],"domain_scores_gemma":[0.9990282,0.00013522338,0.00044284403,0.00015146214,0.000106718275,0.0001355335],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010719144,0.00009764286,0.00040028346,0.00021844957,0.00007078972,0.000013509171,0.00050719595,0.00004932387,0.029251598],"category_scores_gemma":[0.00028000938,0.000051547224,0.00008561057,0.0006590281,0.0014541113,0.00019010017,0.00001977811,0.00019228137,8.3113133e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000579662,0.000038090817,0.9925285,0.000031474323,0.000024100797,0.000006088492,0.0047403635,0.00014629355,0.0010139125,0.00017835706,0.00005451503,0.0011803259],"study_design_scores_gemma":[0.00021793995,0.00065313606,0.96776843,0.00013592717,0.000025372336,0.000013416786,0.002656359,0.000075813296,0.026384588,0.0015701164,0.00043121644,0.00006769283],"about_ca_topic_score_codex":0.6011069,"about_ca_topic_score_gemma":0.985877,"teacher_disagreement_score":0.3847701,"about_ca_system_score_codex":0.0000068241125,"about_ca_system_score_gemma":0.0013784578,"threshold_uncertainty_score":0.9716358},"labels":[],"label_agreement":null},{"id":"W2131521223","doi":"10.1139/e06-135","title":"Late Holocene vegetation and climate change at Moraine Bog, Tiedemann Glacier, southern Coast Mountains, British Columbia","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; Nunavut Research Institute","funders":"","keywords":"Geology; Holocene; Moraine; Bog; Glacier; Vegetation (pathology); Tsuga; Physical geography; Paleoclimatology; Pollen; Oceanography; Climate change; Peat; Geomorphology; Ecology; Geography; Archaeology","score_opus":0.024241381653364907,"score_gpt":0.23303256503487488,"score_spread":0.20879118338150998,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131521223","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9922077,0.005224292,0.0000037112757,0.00040449126,0.0003452387,0.000104986255,0.00005705716,0.0000054928423,0.0016470215],"genre_scores_gemma":[0.99854344,0.00030564843,0.00023464116,0.00045498676,0.00012727515,2.6243742e-7,0.000011785368,0.000002501993,0.00031948654],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983572,0.000100844736,0.00030774926,0.00020659302,0.00026550182,0.000762137],"domain_scores_gemma":[0.9987411,0.0001460496,0.00018619491,0.000072403265,0.00012553704,0.0007287274],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026455417,0.00008870452,0.00020709325,0.00021256202,0.0010807085,0.0002839557,0.0002709483,0.00011007583,0.0007543249],"category_scores_gemma":[0.000111789595,0.000099677694,0.000043920383,0.0003635735,0.0011629385,0.00037183514,0.00001161717,0.00022030884,0.00007717571],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010808792,0.0000025193171,0.9957612,0.000013097332,0.000006947672,0.00047891968,0.00056318723,0.000061081686,0.0000020958423,0.0000063554676,0.000049283193,0.0030444628],"study_design_scores_gemma":[0.00027067066,0.00026822396,0.9957183,0.000053572614,0.000009702353,0.0014515511,0.00050997635,0.00046837764,0.0000045547044,0.00026269554,0.0008691451,0.000113219205],"about_ca_topic_score_codex":0.083375014,"about_ca_topic_score_gemma":0.99278426,"teacher_disagreement_score":0.9094092,"about_ca_system_score_codex":0.0000012708815,"about_ca_system_score_gemma":0.00029078778,"threshold_uncertainty_score":0.9227289},"labels":[],"label_agreement":null},{"id":"W2131601499","doi":"10.1139/e08-015","title":"The Spi Lake Formation of the central Hearne domain, western Churchill Province, Canada: an axial intracratonic continental tholeiite trough above the cogenetic Kaminak dyke swarmGeological Survey of Canada Contribution 20070462.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geoscience BC; Geological Survey of Canada","funders":"","keywords":"Geology; Geochemistry; Basalt; Continental crust; Mantle (geology); Conglomerate; Sedimentary rock","score_opus":0.011468207235509606,"score_gpt":0.1773337429821646,"score_spread":0.16586553574665497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131601499","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950263,0.0010226427,0.000016909506,0.0028645953,0.00034345666,0.00015796452,0.0003733472,0.0000012425131,0.00019353167],"genre_scores_gemma":[0.99943227,0.000051475177,0.000022326063,0.00034247685,0.00006845493,3.3579673e-7,0.000025998997,0.0000010985201,0.000055585282],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974913,0.00042982504,0.0006166372,0.00015552218,0.00068980735,0.00061692],"domain_scores_gemma":[0.99815106,0.00034598642,0.0005550682,0.00015394016,0.00036886288,0.00042509483],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012899705,0.00014131531,0.00029417282,0.00004208949,0.0010117947,0.000053458258,0.000829661,0.00005120787,0.00027139462],"category_scores_gemma":[0.00047976655,0.000061694474,0.000094000854,0.0005712423,0.001592107,0.00019460551,0.000015551717,0.00025766215,6.829495e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033509685,0.000007924169,0.995802,0.0000024470469,0.000014666484,0.000023037303,0.00009392398,0.0033282894,0.000024831335,0.000042926924,0.00023410637,0.00039233576],"study_design_scores_gemma":[0.00019993773,0.00023057018,0.9943065,0.000013600661,0.000016930693,0.00016600851,0.00024769938,0.0011686367,0.00042355104,0.00020870529,0.0029287841,0.00008907562],"about_ca_topic_score_codex":0.98554045,"about_ca_topic_score_gemma":0.99998385,"teacher_disagreement_score":0.014443419,"about_ca_system_score_codex":0.000014871336,"about_ca_system_score_gemma":0.0067104297,"threshold_uncertainty_score":0.9989206},"labels":[],"label_agreement":null},{"id":"W2131852128","doi":"10.1139/e09-007","title":"Structural analysis of the Velardeña mining district, Mexico: a faulted Au–Ag-rich hydrothermal system","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Breccia; Hydrothermal circulation; Structural basin; Geochemistry; Carbonate; Volcano; Fault (geology); Extensional definition; Basin and Range Province; Intrusion; Tectonics; Seismology; Geomorphology","score_opus":0.013896475974430238,"score_gpt":0.19514740299301395,"score_spread":0.1812509270185837,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131852128","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942031,0.0005376587,0.000013875999,0.00073349435,0.00017068749,0.00003982308,0.000054927652,0.000003400938,0.0042430284],"genre_scores_gemma":[0.99949116,0.0000021453113,0.00022791777,0.0001742191,0.000058106045,5.1958164e-8,0.000004404789,6.1895935e-7,0.00004138567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99839354,0.000109479035,0.0004491846,0.00017217263,0.0004590325,0.0004165678],"domain_scores_gemma":[0.99880475,0.00011034215,0.00036870773,0.00012973815,0.00012671383,0.00045972932],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005723827,0.000121040095,0.00036851404,0.00039614568,0.00048238155,0.00008627967,0.0007434572,0.000052550207,0.001540349],"category_scores_gemma":[0.00017491839,0.000063148495,0.0003094813,0.0027096872,0.0004459041,0.00017122076,0.000005642811,0.0001477878,0.000005190075],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004638412,0.000001901645,0.9612163,0.0000023230666,0.000097856486,0.000017722537,0.00020294127,0.036357947,0.00004379013,0.00009047508,0.000013200455,0.0019509081],"study_design_scores_gemma":[0.00007689002,0.00014059024,0.9673054,0.000021557084,0.00026155182,0.000036551897,0.00047024174,0.031062363,0.00021560524,0.0002254969,0.000092762486,0.00009094272],"about_ca_topic_score_codex":0.023843868,"about_ca_topic_score_gemma":0.2461808,"teacher_disagreement_score":0.22233693,"about_ca_system_score_codex":0.000004541197,"about_ca_system_score_gemma":0.00050872995,"threshold_uncertainty_score":0.99937236},"labels":[],"label_agreement":null},{"id":"W2132122505","doi":"10.1139/e04-084","title":"The McAbee flora of British Columbia and its relation to the Early-Middle Eocene Okanagan Highlands flora of the Pacific Northwest","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Western Washington University; Harvard University; National Science Foundation","keywords":"Flora (microbiology); Pollen; Pinaceae; Gymnosperm; Betulaceae; Botany; Taxon; Paleobotany; Genus; Phytogeography; Geography; Ecology; Biology; Paleontology","score_opus":0.016754466907854974,"score_gpt":0.15988816638798442,"score_spread":0.14313369948012944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132122505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943814,0.0005925807,2.9602694e-7,0.004269428,0.00022876395,0.000075228694,0.00013372504,0.0000013662898,0.00031717616],"genre_scores_gemma":[0.99930024,0.00009465315,0.0000150616415,0.000068081245,0.000128817,2.3490288e-7,0.0000013005415,2.5529505e-7,0.0003913622],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99922794,0.000061521714,0.00018787745,0.000086227774,0.000246205,0.0001902504],"domain_scores_gemma":[0.99939775,0.00009902874,0.00017451496,0.000033849945,0.00013031768,0.00016450488],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006752247,0.0000411149,0.0000905635,0.000015192903,0.0009387782,0.00017871732,0.00042404098,0.00003515305,0.00004345851],"category_scores_gemma":[0.000085722095,0.00001691173,0.000050402366,0.0004772051,0.0002823298,0.0002452844,0.00002268388,0.00009215131,0.0000028560548],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011212344,0.000011897249,0.9762006,0.000003751166,0.000014236793,0.0000055176697,0.0007144083,0.0004726703,0.0018713025,0.00014007786,0.0033122764,0.017242078],"study_design_scores_gemma":[0.00004661799,0.0001419114,0.98368984,0.000049365797,0.000008170926,0.000035158617,0.0007537511,0.000103254155,0.000070417336,0.00007174855,0.014988054,0.000041724667],"about_ca_topic_score_codex":0.05219219,"about_ca_topic_score_gemma":0.946224,"teacher_disagreement_score":0.89403176,"about_ca_system_score_codex":0.0000059196664,"about_ca_system_score_gemma":0.00009883733,"threshold_uncertainty_score":0.9541193},"labels":[],"label_agreement":null},{"id":"W2132230386","doi":"10.1139/e06-001","title":"A record of post-glacial moraine deposition and tephra stratigraphy from Otokomi Lake, Rose Basin, Glacier National Park, Montana","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Acadia University; University of Calgary","funders":"Northwestern University","keywords":"Younger Dryas; Moraine; Geology; Deglaciation; Glacier; Sedimentary rock; Glacial period; Glacial lake; Tephra; Geomorphology; Structural basin; Physical geography; Glacier mass balance; Paleontology; Volcano","score_opus":0.01540944344219282,"score_gpt":0.217416035735339,"score_spread":0.20200659229314616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132230386","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911556,0.0011034334,0.000017429058,0.00082618307,0.00021032682,0.00006996948,0.00022650427,0.0000021365306,0.0063883862],"genre_scores_gemma":[0.9975655,0.000027760814,0.0020252727,0.00019054311,0.00011720064,2.3420274e-7,0.000037807822,0.0000011185747,0.00003453475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99869895,0.00014034261,0.00033771875,0.00016285005,0.00033932738,0.00032079013],"domain_scores_gemma":[0.99894065,0.00022918254,0.0001992155,0.00005382612,0.00026417949,0.00031293507],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007779316,0.00009598163,0.00020324242,0.00043146734,0.00034791906,0.000078645455,0.00022818988,0.00008989334,0.0014368172],"category_scores_gemma":[0.00012481074,0.0000776396,0.000063341424,0.00039178977,0.0009994525,0.00039917874,0.0000031067955,0.00019016257,0.000009871549],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003473055,0.0000059037857,0.9985922,0.0000034253699,0.000012577844,0.00007389835,0.00008246491,0.00023292667,0.000049521637,0.0001694014,0.00011903093,0.0006239274],"study_design_scores_gemma":[0.00024475795,0.00033329136,0.9934285,0.00002142744,0.000010506544,0.00018411307,0.00014181284,0.00059015816,0.000102415645,0.0043074,0.0005523184,0.00008329792],"about_ca_topic_score_codex":0.04052042,"about_ca_topic_score_gemma":0.9550022,"teacher_disagreement_score":0.91448176,"about_ca_system_score_codex":4.7585362e-7,"about_ca_system_score_gemma":0.0010757961,"threshold_uncertainty_score":0.999476},"labels":[],"label_agreement":null},{"id":"W2132259680","doi":"10.1139/e03-031","title":"A new species of catfish (Claroteidae, <i>Chrysichthys</i>) from an Eocene crater lake in East Africa","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fish biology, ecology, and behavior","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta; Canadian Museum of Nature","funders":"National Geographic Society","keywords":"Catfish; Barbel; Genus; Fauna; Biology; Actinopterygii; Paleontology; Range (aeronautics); Zoology; Ecology; Fish <Actinopterygii>; Fishery","score_opus":0.02584019983726404,"score_gpt":0.2190812931800491,"score_spread":0.19324109334278505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132259680","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9860178,0.00015172608,0.000013553889,0.0005097216,0.0003803252,0.00006664445,0.000023903769,0.0000019836366,0.012834337],"genre_scores_gemma":[0.9968384,0.000008463747,0.0022205042,0.00022947237,0.000063062835,6.5106263e-7,0.0000010500859,0.000004364546,0.00063401175],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986481,0.000115438284,0.00036055836,0.00022034542,0.00021239833,0.00044315634],"domain_scores_gemma":[0.99904096,0.000032789743,0.0001953248,0.00013296092,0.00002295059,0.00057501305],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006201364,0.00011711484,0.00024034883,0.0001691839,0.00013586316,0.0000563098,0.00049546285,0.00008656191,0.012328742],"category_scores_gemma":[0.00010435919,0.00009452296,0.00005835777,0.000518415,0.00089584134,0.00044981783,0.000016380865,0.00017008629,0.000049819086],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004081961,0.000025804595,0.99114966,6.511345e-7,0.0000029955513,0.000058517093,0.00060173974,0.00015487829,0.0061095078,0.000048356676,0.0014741182,0.0003697127],"study_design_scores_gemma":[0.0002448168,0.00033263408,0.97540575,0.000014666781,0.000009385037,0.000026447333,0.00056499086,0.0000066129173,0.0017666261,0.0007575563,0.02075404,0.00011649355],"about_ca_topic_score_codex":0.011279839,"about_ca_topic_score_gemma":0.8007635,"teacher_disagreement_score":0.78948367,"about_ca_system_score_codex":0.00002039584,"about_ca_system_score_gemma":0.0006176415,"threshold_uncertainty_score":0.9953041},"labels":[],"label_agreement":null},{"id":"W2132316325","doi":"10.1139/cjes-2014-0120","title":"Evidence of an Asia to North America dispersal of palynomorphs in the Late Cretaceous","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Pollen; Cretaceous; Geology; Biological dispersal; Paleontology; Genus; China; Geography; Archaeology; Ecology; Biology; Population","score_opus":0.05148499140944309,"score_gpt":0.2548405475609078,"score_spread":0.2033555561514647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132316325","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9878146,0.005946699,0.00001589171,0.0006912092,0.00017654712,0.00006600568,0.000022806522,8.5397954e-7,0.0052653616],"genre_scores_gemma":[0.9990887,0.000025421348,0.0007466394,0.000107325184,0.000025584706,1.0921786e-7,4.2554103e-7,3.2622555e-7,0.000005469465],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875873,0.00019273337,0.0003291712,0.0001008733,0.00034417515,0.0002743238],"domain_scores_gemma":[0.99883556,0.0001761092,0.00022858597,0.00011620421,0.000107931985,0.0005355886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010889587,0.000076039774,0.0002095019,0.00031007585,0.00010465782,0.00004243281,0.0007558247,0.000030413883,0.00008200435],"category_scores_gemma":[0.00030011815,0.000047642458,0.000054194323,0.0008049205,0.00084682996,0.00044726505,8.9954e-7,0.00013562197,0.000003270524],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028047845,0.00000475463,0.9740103,0.0000031263019,0.000005364534,0.00007798545,0.003788721,0.0036033874,0.000012634081,0.00001409138,0.0000375736,0.01841402],"study_design_scores_gemma":[0.00008045778,0.001367014,0.99460316,0.00005597179,0.000008814999,0.000071616814,0.00271325,0.0006504245,0.000027571426,0.00011378278,0.000247385,0.000060533424],"about_ca_topic_score_codex":0.030226449,"about_ca_topic_score_gemma":0.84357256,"teacher_disagreement_score":0.81334615,"about_ca_system_score_codex":7.3434495e-7,"about_ca_system_score_gemma":0.0013851089,"threshold_uncertainty_score":0.97623134},"labels":[],"label_agreement":null},{"id":"W2132389935","doi":"10.1139/e06-082","title":"The tonalite–trondhjemite–granodiorite (TTG) to granodiorite–granite (GG) transition in the late Archean plutonic rocks of the central Wyoming Province","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Department of Energy; National Science Foundation","keywords":"Geology; Geochemistry; Archean; Continental crust; Partial melting; Gneiss; Crust; Petrology; Metamorphic rock","score_opus":0.009423414348767051,"score_gpt":0.17982104989096823,"score_spread":0.17039763554220116,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132389935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98729426,0.0015998164,0.000049983715,0.009160508,0.00020096825,0.00015395535,0.00004527581,0.0000024043743,0.0014928055],"genre_scores_gemma":[0.9990221,0.000021639456,0.00009341746,0.0006112537,0.00012510433,4.781513e-7,0.000003564625,0.0000014582424,0.00012096589],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978549,0.00020309196,0.00051705656,0.00017541183,0.0005773136,0.00067222683],"domain_scores_gemma":[0.99893755,0.00031288058,0.00020625164,0.00016112071,0.000097957054,0.000284218],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001616977,0.00014128622,0.00022041658,0.00015945997,0.0007598974,0.00019132985,0.0010625519,0.000050155868,0.00020236448],"category_scores_gemma":[0.00012742991,0.00006311172,0.00022210454,0.0012307572,0.000755535,0.00020448935,0.00000802279,0.00032796973,0.0000075491002],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002765373,0.000013203104,0.9613429,0.00000795173,0.000011619364,0.000029821014,0.001190828,0.03256991,0.00043769862,0.00029456118,0.000103665865,0.0039701853],"study_design_scores_gemma":[0.0001753579,0.00015496029,0.9863776,0.00005899135,0.000028943114,0.00005954482,0.00080511783,0.0013983522,0.0004003342,0.0063639395,0.0040537417,0.00012310506],"about_ca_topic_score_codex":0.08167909,"about_ca_topic_score_gemma":0.7946392,"teacher_disagreement_score":0.7129601,"about_ca_system_score_codex":0.0000050989306,"about_ca_system_score_gemma":0.0005925441,"threshold_uncertainty_score":0.9244361},"labels":[],"label_agreement":null},{"id":"W2132460632","doi":"10.1139/cjes-2014-0132","title":"Climate change and recent sedimentation in Nastapoka Sound, eastern coast of Hudson Bay","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Rimouski; Université Laval; Center for Northern Studies","funders":"Natural Sciences and Engineering Research Council of Canada; ArcticNet; Université Laval","keywords":"Bay; Geology; Sound (geography); Oceanography; Sedimentation; Climate change; Physical geography; Sediment; Geomorphology; Geography","score_opus":0.1020633466410953,"score_gpt":0.28434917682463706,"score_spread":0.18228583018354177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132460632","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99493426,0.0020492529,0.0000028843976,0.0010093466,0.0003547749,0.00006899709,0.000014439308,9.520741e-7,0.0015650763],"genre_scores_gemma":[0.9993556,0.00019428131,0.00026461645,0.00013069146,0.000041108306,2.1060382e-7,0.0000031571562,7.872922e-7,0.000009538551],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989571,0.00014141799,0.0002397704,0.00010647571,0.00020897541,0.00034626346],"domain_scores_gemma":[0.9991688,0.00008177614,0.00014267168,0.000044935387,0.000110759516,0.0004510503],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016722273,0.00006264016,0.00015594308,0.00038489792,0.000114308095,0.00003712423,0.00017787193,0.000050869377,0.00027650956],"category_scores_gemma":[0.000103596576,0.00004931993,0.000017052627,0.00034448018,0.0005687571,0.00036642415,0.000005451163,0.0001392453,0.00002023069],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024925272,0.0000028652744,0.9965659,0.0000067788933,0.000002428089,0.000055822195,0.00107908,0.00010290838,8.092365e-7,0.00004779006,0.000007984798,0.0021027215],"study_design_scores_gemma":[0.00032913315,0.0004931713,0.9948147,0.00003996305,0.0000036581457,0.00021841226,0.0025043404,0.0005854329,0.000022601043,0.0006438657,0.0002902559,0.000054450193],"about_ca_topic_score_codex":0.0046970462,"about_ca_topic_score_gemma":0.8010791,"teacher_disagreement_score":0.796382,"about_ca_system_score_codex":5.734996e-7,"about_ca_system_score_gemma":0.0004972336,"threshold_uncertainty_score":0.710056},"labels":[],"label_agreement":null},{"id":"W2132662653","doi":"10.1139/e07-024","title":"The Late Ordovician Dawson Point Formation (Timiskaming outlier, Ontario): key to a new regional synthesis of Richmondian–Hirnantian carbonate and siliciclastic magnafacies across the central Canadian craton","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada; Institut national de la recherche scientifique","keywords":"Siliciclastic; Geology; Ordovician; Craton; Foreland basin; Paleontology; Carbonate; Carbonate platform; Marine transgression; Facies; Structural basin; Tectonics","score_opus":0.016333497769017474,"score_gpt":0.21626999927820018,"score_spread":0.1999365015091827,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132662653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9861233,0.0029461302,0.00004084352,0.0040614945,0.00048310758,0.00012936711,0.000038998365,0.0000025567783,0.006174193],"genre_scores_gemma":[0.99913156,0.000049065846,0.00033330382,0.00028064236,0.00007923918,2.1081442e-7,7.138139e-7,0.0000011247542,0.00012413083],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99810445,0.00007953591,0.00045437375,0.00014409944,0.00032119994,0.0008963447],"domain_scores_gemma":[0.9977738,0.00043452953,0.00026819174,0.00011964881,0.00009257553,0.0013112087],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00173312,0.0001478023,0.00020238031,0.000301559,0.001663137,0.00027129657,0.00054710096,0.00007523667,0.00006497031],"category_scores_gemma":[0.0002407374,0.00008821375,0.00008542456,0.0004972498,0.0008569518,0.00046540736,0.0000022924858,0.00024372413,0.0000025212887],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003172926,0.0000016902039,0.8959436,0.000004423468,0.000022975606,0.000057652658,0.011405156,0.00060386333,0.000021992626,0.000110438836,0.00014327109,0.09165326],"study_design_scores_gemma":[0.00009233251,0.0001806966,0.9886507,0.00006390959,0.000017617462,0.00015919007,0.0040092054,0.00029598965,0.00011745643,0.00028906605,0.006008916,0.00011495786],"about_ca_topic_score_codex":0.92078984,"about_ca_topic_score_gemma":0.9999075,"teacher_disagreement_score":0.09270711,"about_ca_system_score_codex":0.000012939468,"about_ca_system_score_gemma":0.0027514403,"threshold_uncertainty_score":0.9996366},"labels":[],"label_agreement":null},{"id":"W2133299498","doi":"10.1139/e08-057","title":"Taphonomy and ontogeny of a multibranched Ediacaran fossil: <i>Bradgatia</i> from the Avalon Peninsula of Newfoundland","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"","keywords":"Petal; Ontogeny; Paleontology; Taphonomy; Geology; Biology; Botany","score_opus":0.025352207113534763,"score_gpt":0.20577722962487935,"score_spread":0.1804250225113446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133299498","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9715027,0.022146402,0.000022250451,0.00026844043,0.00039220686,0.00007230381,0.00009242718,0.0000014630647,0.0055018044],"genre_scores_gemma":[0.99821407,0.00017095203,0.0014439069,0.000051830135,0.00010952075,1.08762315e-7,0.0000010286105,5.751332e-7,0.000007984729],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988427,0.00010837068,0.00039869625,0.00013888096,0.00024954887,0.0002617582],"domain_scores_gemma":[0.9986581,0.0003989294,0.0003704617,0.000108955755,0.00011130295,0.00035221895],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055969507,0.000105876265,0.0002854924,0.00015121822,0.0004288771,0.000033864442,0.00042882885,0.00006215942,0.00016978897],"category_scores_gemma":[0.000154318,0.00006727051,0.000099384546,0.00030345665,0.0021792874,0.000345567,0.000001207045,0.00015730482,0.0000010590813],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019802575,0.0000032315168,0.9917731,0.0000030875804,0.000024039791,0.000024395644,0.0016138292,0.000059798087,0.00012477918,0.000033474043,0.00007412302,0.0062462976],"study_design_scores_gemma":[0.0003570121,0.00025943434,0.9971366,0.000036865844,0.000018151046,0.00011633753,0.00030313557,0.00025890398,0.00032654023,0.00043285594,0.00067674514,0.00007745344],"about_ca_topic_score_codex":0.12160614,"about_ca_topic_score_gemma":0.70762724,"teacher_disagreement_score":0.5860211,"about_ca_system_score_codex":5.792362e-7,"about_ca_system_score_gemma":0.0011329423,"threshold_uncertainty_score":0.88424313},"labels":[],"label_agreement":null},{"id":"W2133304691","doi":"10.1139/e00-014","title":"Paleomagnetic evidence for multiple Late Pliocene - Early Pleistocene glaciations in the Klondike area, Yukon Territory","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Lethbridge; University of Calgary","funders":"","keywords":"Geology; Glacial period; Paleontology; Aggradation; Pleistocene; Interglacial; Fluvial; Loess; Early Pleistocene; Paleomagnetism; Outwash plain; Glacier; Magnetostratigraphy; Geomorphology; Structural basin","score_opus":0.06042747892030949,"score_gpt":0.266712236780457,"score_spread":0.20628475786014755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133304691","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99144214,0.0036407292,0.000006339781,0.0023321519,0.00025928963,0.00020625704,0.00002668333,0.0000025938757,0.0020838035],"genre_scores_gemma":[0.998723,0.00009109937,0.00039800795,0.0003467854,0.000087824425,0.000002154154,0.0000038471144,0.000001351319,0.0003459353],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984721,0.00020494671,0.0003153833,0.00017937373,0.00025715883,0.0005710708],"domain_scores_gemma":[0.9982566,0.0011383928,0.000104282946,0.00012522355,0.00007255322,0.0003029059],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018222718,0.00010063783,0.00017143028,0.00035238775,0.00067373307,0.00012563422,0.0007401225,0.000079703364,0.0021862679],"category_scores_gemma":[0.00040096947,0.00006799813,0.00007365961,0.00049339473,0.00075495476,0.00042386202,0.0000020532057,0.00026505356,0.00006775685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033038374,0.0000045158336,0.99441487,0.0000045982583,0.000004001581,0.00006518733,0.0005603476,0.0029066375,0.0000015987782,0.000010946687,0.00008270309,0.001911557],"study_design_scores_gemma":[0.000255478,0.0006186973,0.9942891,0.000053344178,0.000008436554,0.0001447036,0.00015472631,0.0022624554,0.000006029916,0.00059851137,0.001523783,0.0000847331],"about_ca_topic_score_codex":0.011436054,"about_ca_topic_score_gemma":0.83291763,"teacher_disagreement_score":0.8214816,"about_ca_system_score_codex":9.284358e-7,"about_ca_system_score_gemma":0.0009796456,"threshold_uncertainty_score":0.9987259},"labels":[],"label_agreement":null},{"id":"W2133424978","doi":"10.1139/cjes-2012-0166","title":"Ants from the Miocene Totolapa amber (Chiapas, Mexico), with the first record of the genus<i>Forelius</i>(Hymenoptera, Formicidae)","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Insect and Arachnid Ecology and Behavior","field":"Biochemistry, Genetics and Molecular Biology","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Universidad Nacional Autónoma de México; Consejo Nacional de Ciencia y Tecnología","keywords":"Hymenoptera; Genus; Lagerstätte; Biota; Geology; Paleontology; Ecology; Biology","score_opus":0.009374041683133535,"score_gpt":0.20097367035133742,"score_spread":0.1915996286682039,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133424978","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99450755,0.00051558367,0.000010893469,0.003942247,0.0003479047,0.00013660382,0.000014376232,5.8768126e-7,0.0005242472],"genre_scores_gemma":[0.9975096,0.000030011874,0.00013601307,0.0018747213,0.00017107246,0.0000035561554,0.0000015582235,0.0000042103193,0.00026924582],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99927914,0.00004329428,0.00018535802,0.00010999654,0.00012713131,0.00025507968],"domain_scores_gemma":[0.99935764,0.000029493462,0.00021239767,0.00018570249,0.00010957956,0.00010520827],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027030133,0.00009329758,0.00010649723,0.000024159279,0.00062146364,0.000056338682,0.00060803624,0.00006078472,0.00021989208],"category_scores_gemma":[0.000027440352,0.000037674476,0.00007811391,0.00013000457,0.00068529206,0.000019708077,0.000025955727,0.00014115838,0.0000055883215],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020330042,0.000014666663,0.97688067,0.00000170962,0.00003775179,0.000004782818,0.0003387575,0.00005259822,0.012286928,0.00003721354,0.008746319,0.0015782979],"study_design_scores_gemma":[0.0003738449,0.00072751095,0.8620178,0.00005334716,0.000055113556,0.000115688556,0.00065315346,0.00002692419,0.06953714,0.00013609983,0.06614138,0.00016198336],"about_ca_topic_score_codex":0.005445474,"about_ca_topic_score_gemma":0.23424603,"teacher_disagreement_score":0.22880057,"about_ca_system_score_codex":0.0000026299756,"about_ca_system_score_gemma":0.000520403,"threshold_uncertainty_score":0.8231964},"labels":[],"label_agreement":null},{"id":"W2133532939","doi":"10.1139/e05-023","title":"Current tectonics of the northern Canadian Cordillera","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"ASL Environmental Sciences (Canada); University of Victoria; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Lithosphere; Terrane; Crust; Thrust fault; Seismology; Craton; Mountain formation; North American Plate; Tectonics; Collision zone; Plate tectonics; Geomorphology; Paleontology","score_opus":0.016042266431334013,"score_gpt":0.19234881848236923,"score_spread":0.1763065520510352,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133532939","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9841805,0.003167947,0.0000017624343,0.003760337,0.00030228827,0.000037522597,0.000035561843,0.0000012465823,0.008512825],"genre_scores_gemma":[0.9992804,0.00003557738,0.00019282148,0.0003260735,0.00011753533,5.2567227e-8,0.0000011661804,7.131438e-7,0.00004564585],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885035,0.000046822537,0.0002944321,0.00011303917,0.00030186513,0.0003935169],"domain_scores_gemma":[0.99868965,0.000057551642,0.00017931359,0.000102732556,0.0001669794,0.00080378825],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041412425,0.00008426021,0.00016841611,0.00019791431,0.00035864837,0.00005210661,0.000691277,0.00003426273,0.008085064],"category_scores_gemma":[0.00018782179,0.000044959535,0.00014460835,0.00072210614,0.0005724045,0.00013975211,0.000004844402,0.00020421717,0.000052884363],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000010371042,0.0000027845483,0.97190076,0.0000016999579,0.000007942707,0.000003999946,0.00007083143,0.006519584,0.000009869144,0.000038544615,0.00009031627,0.021352623],"study_design_scores_gemma":[0.00007143697,0.00009046448,0.95299125,0.000030087836,0.000019978661,0.000034724682,0.00010351582,0.0019229462,0.00024459805,0.0010576722,0.04333921,0.000094135416],"about_ca_topic_score_codex":0.43501264,"about_ca_topic_score_gemma":0.99794054,"teacher_disagreement_score":0.5629279,"about_ca_system_score_codex":0.0000036313447,"about_ca_system_score_gemma":0.002244546,"threshold_uncertainty_score":0.9928217},"labels":[],"label_agreement":null},{"id":"W2133587517","doi":"10.1139/cjes-2014-0172","title":"A reassessment of the horned dinosaur <i>Judiceratops tigris</i> (Ornithischia: Ceratopsidae) from the Upper Cretaceous (Campanian) of Montana, USA","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Autapomorphy; Paleontology; Geology; Taxon; Cretaceous; Section (typography); Skull; Anatomy; Biology; Phylogenetic tree","score_opus":0.013410976664227546,"score_gpt":0.2022314126331279,"score_spread":0.18882043596890036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133587517","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.984977,0.0029094156,0.00003306677,0.0027336231,0.000930005,0.0000869067,0.000118280936,0.0000016730376,0.008210051],"genre_scores_gemma":[0.99865824,0.000061720464,0.0003892654,0.0006412951,0.00016900989,2.6363853e-7,0.0000028708116,0.0000013937723,0.00007593126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99823654,0.00045478676,0.00045813684,0.00017753299,0.00031232872,0.00036067207],"domain_scores_gemma":[0.9983495,0.00051832077,0.00048195967,0.00022665545,0.00014567435,0.00027788396],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012239089,0.00012541407,0.00029101936,0.00010202462,0.00058420876,0.000036518843,0.00093288743,0.00010037888,0.0010677148],"category_scores_gemma":[0.00028215285,0.00006515269,0.00013677447,0.00041062527,0.0015493251,0.00022146614,0.000010639132,0.00029453522,0.000017880126],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001642161,0.0000040068844,0.9963953,0.0000021852206,0.00002853694,0.000006549376,0.00024719202,0.000522743,0.00006257213,0.00027748608,0.00058552966,0.0018515054],"study_design_scores_gemma":[0.00016567536,0.00027043343,0.98757124,0.000043447177,0.000033218614,0.000116964075,0.0003676814,0.00042506115,0.00012016741,0.0013619345,0.009443396,0.00008078824],"about_ca_topic_score_codex":0.047380917,"about_ca_topic_score_gemma":0.7634659,"teacher_disagreement_score":0.716085,"about_ca_system_score_codex":0.000003361409,"about_ca_system_score_gemma":0.0019275037,"threshold_uncertainty_score":0.99984545},"labels":[],"label_agreement":null},{"id":"W2133849236","doi":"10.1139/e10-101","title":"Laterally extensive modified placer gold deposits in the Paleoproterozoic Mississagi Formation, Clement and Pardo Townships, Ontario","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Conglomerate; Pebble; Pyrite; Geochemistry; Diagenesis; Archean; Sedimentary depositional environment; Clastic rock; Residuum; Geomorphology; Outcrop; Metamorphism; Bedrock; Fluvial; Weathering; Placer mining; Greenstone belt; Sedimentary rock","score_opus":0.04649341122023779,"score_gpt":0.19403869324150583,"score_spread":0.14754528202126804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133849236","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918832,0.0005985473,0.000011164971,0.0012191312,0.000065733424,0.00007751426,0.0000042762413,0.0000012825589,0.006139129],"genre_scores_gemma":[0.99843526,0.00001671752,0.00057542376,0.0008448599,0.000024727531,3.906892e-7,0.0000021341846,4.7577282e-7,0.00010001724],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895746,0.000083281935,0.00029430923,0.00012642675,0.00022618884,0.00031235293],"domain_scores_gemma":[0.99933743,0.0000587682,0.00012924781,0.000065809574,0.0000761898,0.00033256237],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00072235486,0.000089926594,0.00014531305,0.00014434998,0.00019943925,0.00012293154,0.00033824163,0.0000363907,0.0018646519],"category_scores_gemma":[0.000056550365,0.000047866506,0.000048824793,0.0002692231,0.00024068276,0.00032279934,0.0000047679514,0.00017550224,0.000011680083],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010872398,0.0000041211338,0.99409556,0.000002613854,0.0000065438403,0.00008156662,0.0029163596,0.00026491954,0.00000666988,0.00004619076,0.00008005012,0.0024845002],"study_design_scores_gemma":[0.00012410722,0.00020620419,0.9927616,0.000020659547,0.000013204202,0.00011611222,0.0007027905,0.00031524352,0.00007804655,0.0049062176,0.0006769922,0.00007879566],"about_ca_topic_score_codex":0.24093568,"about_ca_topic_score_gemma":0.98368996,"teacher_disagreement_score":0.7427543,"about_ca_system_score_codex":0.0000021103217,"about_ca_system_score_gemma":0.00026147222,"threshold_uncertainty_score":0.99904776},"labels":[],"label_agreement":null},{"id":"W2133903695","doi":"10.1139/e04-089","title":"Geochemistry of the active layer and near-surface permafrost, Mackenzie delta region, Northwest Territories, Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":126,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Permafrost; Active layer; Geology; Aggradation; Soil water; Silt; Delta; Alluvium; Soil horizon; Thermokarst; River delta; Geomorphology; Hydrology (agriculture); Oceanography; Soil science; Layer (electronics); Fluvial; Chemistry","score_opus":0.02452788567753827,"score_gpt":0.21102356182885595,"score_spread":0.18649567615131768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133903695","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9895063,0.001635461,2.481834e-7,0.00295891,0.00047069706,0.000045775756,0.004503503,0.0000010584498,0.00087804586],"genre_scores_gemma":[0.99900335,0.00007531421,0.000060133396,0.0004862458,0.00022918737,5.497748e-8,0.000068821944,0.0000018683603,0.00007504313],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989543,0.00002659352,0.00024830102,0.0001345833,0.00030830968,0.00032791912],"domain_scores_gemma":[0.99899095,0.00007458792,0.00021667259,0.00011897619,0.0001371636,0.00046167124],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022406838,0.00010796777,0.00015751885,0.000026843038,0.00051722524,0.0001142281,0.00042152434,0.00004442593,0.0011228389],"category_scores_gemma":[0.000051695184,0.000071852686,0.000044263226,0.00028579315,0.00067350524,0.00030445654,0.000008818585,0.00016981499,0.0000010576681],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005786285,0.0000014775335,0.9960935,0.0000064009037,0.000006242846,0.000025594807,0.00051960564,0.00066995266,0.000054208354,0.00000266068,0.0016219242,0.0009926539],"study_design_scores_gemma":[0.000118770215,0.000049617644,0.932766,0.00004724754,0.00001119824,0.00030258083,0.0009363755,0.00048814336,0.0012138563,0.000020721753,0.06394214,0.000103344675],"about_ca_topic_score_codex":0.9731929,"about_ca_topic_score_gemma":0.99989545,"teacher_disagreement_score":0.06332749,"about_ca_system_score_codex":0.0000070535407,"about_ca_system_score_gemma":0.0036727535,"threshold_uncertainty_score":0.99979025},"labels":[],"label_agreement":null},{"id":"W2133956049","doi":"10.1139/e98-088","title":"Teleseismic studies of the lithosphere below the Abitibi-Grenville Lithoprobe transect","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université de Montréal; Université du Québec à Montréal; Polytechnique Montréal; Geological Survey of Canada; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Polytechnique Montréal; New Mexico State University","keywords":"Geology; Lithosphere; Receiver function; Seismology; Crust; Archean; Anisotropy; Magnetotellurics; Mantle (geology); Seismic anisotropy; Geophysics; Transect; Tectonics; Petrology; Paleontology; Electrical resistivity and conductivity","score_opus":0.019262946180558255,"score_gpt":0.21343484969406734,"score_spread":0.19417190351350908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133956049","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987356,0.005472031,0.0000015723167,0.0017355862,0.0007435166,0.000102317565,0.00008298209,0.0000017820784,0.004504231],"genre_scores_gemma":[0.9985311,0.00026576422,0.00016546181,0.00028054137,0.00017943064,2.262358e-7,4.8343475e-7,0.0000019191089,0.0005750801],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987229,0.00014697542,0.00033430624,0.00012465156,0.00033479242,0.00033635864],"domain_scores_gemma":[0.9991919,0.00016538972,0.00018243451,0.00015950363,0.000100268226,0.00020050751],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010453622,0.00010832634,0.00023439249,0.000047993974,0.0006811195,0.00013649589,0.0007734066,0.00003341485,0.0033115875],"category_scores_gemma":[0.00007313088,0.00004983615,0.00012134017,0.0004306435,0.0010755905,0.00022507593,0.00000403372,0.00012921261,0.000026596052],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009448899,0.000042830958,0.6210497,0.0001664251,0.00043813736,0.00016374992,0.023349622,0.07428963,0.001549981,0.0017590823,0.0071965875,0.2698998],"study_design_scores_gemma":[0.00023316074,0.00041499687,0.908341,0.00019711851,0.000056686706,0.00012727873,0.0016248316,0.00020304827,0.0011966809,0.0032839926,0.08412769,0.00019353814],"about_ca_topic_score_codex":0.025089772,"about_ca_topic_score_gemma":0.27145776,"teacher_disagreement_score":0.2872913,"about_ca_system_score_codex":0.0000010325854,"about_ca_system_score_gemma":0.0007938227,"threshold_uncertainty_score":0.99759954},"labels":[],"label_agreement":null},{"id":"W2134474332","doi":"10.1139/e09-020","title":"Stratigraphy of the Upper Cretaceous Wapiti Formation, west-central Alberta, Canada","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Paleontological Society","keywords":"Geology; Facies; Paleontology; Outcrop; Subaerial; Stratigraphy; Cretaceous; Sedimentary depositional environment; Westphalian sovereignty; Stratigraphic unit; Unconformity; Fluvial; Coal measures; Tectonics; Structural basin; Carboniferous","score_opus":0.010437127144372454,"score_gpt":0.1792284115918368,"score_spread":0.16879128444746436,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134474332","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9758151,0.0012817925,0.000016644724,0.00370806,0.0003755402,0.000056276273,0.000031936397,0.0000010553482,0.018713558],"genre_scores_gemma":[0.99886525,0.000025593925,0.00022940729,0.0007541408,0.000037356716,3.5598095e-8,0.0000018680382,3.6802166e-7,0.000086007174],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998974,0.00003852086,0.00031165383,0.00006256696,0.00029926156,0.0003139925],"domain_scores_gemma":[0.9991718,0.00007339945,0.00021582784,0.00007019549,0.00013260396,0.00033620014],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024118634,0.00007238288,0.00011554236,0.00010457409,0.00040689346,0.00008610487,0.0004583341,0.000027912412,0.0017622913],"category_scores_gemma":[0.00012322947,0.000040139785,0.000062652565,0.00050308387,0.00024070362,0.0005121734,0.0000013373057,0.00010895593,0.0000037855139],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000037304667,0.0000034217271,0.9801183,0.0000076135684,0.0000059704007,0.00000776176,0.00045565935,0.010361662,0.000003875482,0.001021428,0.0013751497,0.0066354447],"study_design_scores_gemma":[0.00006337294,0.0001833625,0.9826821,0.000024427361,0.0000062752033,0.00010797693,0.00041747294,0.0006272408,0.00015022149,0.0021079266,0.013564441,0.00006515314],"about_ca_topic_score_codex":0.69756,"about_ca_topic_score_gemma":0.9977304,"teacher_disagreement_score":0.30017036,"about_ca_system_score_codex":0.0000015707425,"about_ca_system_score_gemma":0.0029124538,"threshold_uncertainty_score":0.9991502},"labels":[],"label_agreement":null},{"id":"W2134661554","doi":"10.1139/e09-063","title":"Morphopédologie et anomalie géochimique","year":2009,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies Worldwide","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Humanities; Philosophy","score_opus":0.048581806489650665,"score_gpt":0.23346733226569874,"score_spread":0.18488552577604808,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134661554","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.66244745,0.044018265,0.000078884776,0.19996841,0.0035162515,0.00013456901,0.00008282095,0.00000959674,0.089743786],"genre_scores_gemma":[0.98087686,0.0008385742,0.0027023214,0.008884295,0.0005520373,1.0481924e-7,0.000002878385,0.0000016078318,0.006141315],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99761766,0.0002662893,0.00048368864,0.00027272012,0.00035894237,0.0010006861],"domain_scores_gemma":[0.9977941,0.00033588582,0.0002812267,0.00011195799,0.0001609714,0.0013158765],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014607058,0.00022256812,0.00040707953,0.00022809552,0.0006756119,0.00028111064,0.00075816404,0.000119276825,0.006595173],"category_scores_gemma":[0.0005482994,0.00015724455,0.00021025313,0.00089758146,0.0016590563,0.0005948234,0.000010277169,0.0004874998,0.00040673383],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000045761626,0.00009387669,0.6298392,0.000028316412,0.000073092735,0.0020602606,0.00065033033,0.020129953,0.000048872138,0.033194184,0.035085283,0.2787509],"study_design_scores_gemma":[0.00013372253,0.0018175256,0.7289161,0.00007248049,0.000016774997,0.00018977498,0.0001339367,0.0002113289,0.000027559912,0.022845766,0.24544615,0.00018885148],"about_ca_topic_score_codex":0.025011295,"about_ca_topic_score_gemma":0.35817552,"teacher_disagreement_score":0.33316424,"about_ca_system_score_codex":0.000003804489,"about_ca_system_score_gemma":0.0016092608,"threshold_uncertainty_score":0.99431294},"labels":[],"label_agreement":null},{"id":"W2134694696","doi":"10.1139/e04-102","title":"Cosmogenic exposure dating in arctic glacial landscapes: implications for the glacial history of northeastern Baffin Island, Arctic Canada","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; American Alpine Club; U.S. Department of Energy","keywords":"Geology; Ice sheet; Glacial period; Deglaciation; Glacial landform; Foreland basin; Surface exposure dating; Seabed gouging by ice; Physical geography; Arctic; Last Glacial Maximum; Glacier; Meltwater; Paleontology; Arctic ice pack; Geomorphology; Moraine; Antarctic sea ice; Oceanography; Geography; Structural basin","score_opus":0.026900503535080517,"score_gpt":0.23210178844919904,"score_spread":0.20520128491411851,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134694696","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9898368,0.0045057414,0.000023385704,0.0037280398,0.0005826339,0.00015208827,0.000054937005,0.0000010304996,0.0011153152],"genre_scores_gemma":[0.9992292,0.000023356992,0.00018323533,0.0002624254,0.00016146076,0.0000013241669,0.0000064520586,0.0000015012438,0.00013102412],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99877185,0.000106584965,0.00037025975,0.00013616178,0.00018096926,0.00043418835],"domain_scores_gemma":[0.9986124,0.00067654334,0.00020889248,0.00010853257,0.00014995741,0.00024365187],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001078237,0.00008478738,0.00018710652,0.00021891456,0.00030504592,0.000022859802,0.00054387114,0.00005233616,0.00091422285],"category_scores_gemma":[0.00035217285,0.000059496757,0.000058165333,0.00026296644,0.00044689415,0.00017584057,0.0000037687817,0.0002251682,0.0000051479515],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018450262,0.0000031326665,0.9923702,0.000010265824,0.000010751101,0.000006363615,0.0003707603,0.0044784565,0.0000017232417,0.000051527968,0.00015997572,0.0025184276],"study_design_scores_gemma":[0.0002920759,0.00014592364,0.98806447,0.000024279781,0.0000128427055,0.00015202853,0.00039492664,0.0018720273,0.0000024554602,0.0001308146,0.008836503,0.00007166708],"about_ca_topic_score_codex":0.44921902,"about_ca_topic_score_gemma":0.9998755,"teacher_disagreement_score":0.55065644,"about_ca_system_score_codex":0.000008437666,"about_ca_system_score_gemma":0.0076460135,"threshold_uncertainty_score":0.9999991},"labels":[],"label_agreement":null},{"id":"W2134775120","doi":"10.1139/e07-021","title":"Introduction to Special Issue of <i>Canadian Journal of Earth Sciences</i>: the Lake Nipigon Region Geoscience Initiative","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Northern Ontario Academic Medicine Association; Lakehead University","funders":"","keywords":"Geology; Earth science; Mineral exploration; Mineral resource classification; Geochemistry; Government (linguistics); Geochronology; Library science","score_opus":0.029472701946313223,"score_gpt":0.23175074330217418,"score_spread":0.20227804135586097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134775120","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6454854,0.00091285503,0.053133827,0.18615401,0.016363623,0.0005247338,0.000019711624,0.000014549016,0.09739132],"genre_scores_gemma":[0.9844699,0.000020953259,0.009028522,0.0011540963,0.004610221,3.4031538e-7,2.0323186e-7,0.0000022500087,0.00071354466],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9973859,0.00012366354,0.00072721805,0.0002986845,0.0007218892,0.0007426353],"domain_scores_gemma":[0.99665207,0.0001783539,0.0008422599,0.0002509914,0.0010372377,0.0010390731],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0065995893,0.00015115456,0.00027197978,0.001595114,0.0010976634,0.00037665808,0.0024849123,0.00007260206,0.00025458436],"category_scores_gemma":[0.0016820743,0.00010605316,0.000116133546,0.004561921,0.0020282045,0.0011748071,0.00004838151,0.00036769372,0.000010838048],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016594982,0.0002293721,0.29876134,0.00015276398,0.00019176131,0.0034999796,0.090769276,0.06318194,0.012683855,0.15876228,0.24379867,0.1278028],"study_design_scores_gemma":[0.0002416212,0.0012199144,0.07064668,0.0001506261,0.000013259298,0.0019321407,0.0025168182,0.00028189787,0.012905186,0.0038712372,0.9059592,0.00026143258],"about_ca_topic_score_codex":0.0042423257,"about_ca_topic_score_gemma":0.3912086,"teacher_disagreement_score":0.6621605,"about_ca_system_score_codex":0.000013515407,"about_ca_system_score_gemma":0.006080486,"threshold_uncertainty_score":0.9995541},"labels":[],"label_agreement":null},{"id":"W2135318274","doi":"10.1139/e11-026","title":"Ordovician A-type plutons in the Antigonish Highlands, Nova Scotia<sup>1</sup>This article is one of a series of papers published in <i>CJES Special Issue: In honour of Ward Neale</i> on the theme of Appalachian and Grenvillian geology.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; St. Francis Xavier University; Acadia University","funders":"Natural Sciences and Engineering Research Council of Canada; Acadia University","keywords":"Geology; Pluton; Zircon; Geochemistry; Gabbro; Mafic; Amphibole; Quartz monzonite; Ordovician; Alkali feldspar; Hornblende; Feldspar; Petrology; Igneous rock; Quartz; Biotite; Tectonics; Paleontology","score_opus":0.017453793176147713,"score_gpt":0.19194511977587075,"score_spread":0.17449132659972305,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135318274","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9865511,0.0006084259,1.1315702e-7,0.0077177677,0.00008707039,0.00008607477,0.000031885433,6.084712e-7,0.004916953],"genre_scores_gemma":[0.9992725,0.00008729822,0.00013401954,0.00037344793,0.00010809765,1.3077207e-7,0.00000210314,0.0000011094322,0.000021275422],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982994,0.00023649288,0.0005895817,0.0001420789,0.0003282678,0.00040414347],"domain_scores_gemma":[0.9989493,0.00032981535,0.0003166195,0.0001308652,0.00008158947,0.00019182426],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0020719587,0.0001127233,0.00040741594,0.00033927924,0.0000788381,0.000029162145,0.0005195206,0.00006990635,0.007520968],"category_scores_gemma":[0.00046326895,0.00006049399,0.00007597509,0.001465357,0.0013962052,0.00030424737,0.000013396336,0.00026594757,0.0000039308557],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048472117,0.000041182255,0.9942936,0.0000130939125,0.000012911399,0.0000058316514,0.0034902373,0.0009279415,0.00013596879,0.00019006224,0.000092359995,0.0007483413],"study_design_scores_gemma":[0.000218358,0.00038922884,0.99199075,0.000075613934,0.000013905772,0.000014778871,0.0042537753,0.0002523148,0.00090996706,0.0010240017,0.00078237714,0.00007492244],"about_ca_topic_score_codex":0.06940558,"about_ca_topic_score_gemma":0.62466204,"teacher_disagreement_score":0.5552564,"about_ca_system_score_codex":0.0000018504328,"about_ca_system_score_gemma":0.00025236243,"threshold_uncertainty_score":0.99338627},"labels":[],"label_agreement":null},{"id":"W2135386591","doi":"10.1139/e10-099","title":"Integrating ice-flow history, geochronology, geology, and geophysics to trace mineralized glacial erratics to their bedrock source: An example from south-central British Columbia<sup>1</sup>This article is one of a series of papers published in this Special Issue on the theme of <i>New insights in Cordilleran Intermontane geoscience: reducing exploration risk in the mountain pine beetle-affected area, British Columbia</i>.<sup>2</sup>Earth Sciences Sector Contribution Number: 20100079.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Bedrock; Geochronology; Batholith; Zircon; Geochemistry; Geomorphology; Paleontology; Tectonics","score_opus":0.028623176293066786,"score_gpt":0.2057185655375756,"score_spread":0.1770953892445088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135386591","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99770606,0.00031982895,0.000023364502,0.00050653884,0.00022484553,0.0005656228,0.00013720231,0.000004525618,0.00051203894],"genre_scores_gemma":[0.99862784,0.000058977785,0.0007733292,0.00023705169,0.00015697931,0.00000518551,0.000017357359,0.000004348444,0.00011893455],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99642855,0.0010257999,0.0008773593,0.00048043297,0.0004636191,0.0007242354],"domain_scores_gemma":[0.99816054,0.0005226703,0.0004915355,0.00021504189,0.00026027774,0.00034991044],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0027397154,0.00017061394,0.0006348358,0.00029315377,0.0005250905,0.00032997437,0.00085075625,0.00019807949,0.007490822],"category_scores_gemma":[0.0010987645,0.00016989833,0.00007428956,0.0012678305,0.002651259,0.0009518475,0.00003258573,0.00063769775,0.0000028853967],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014230351,0.000064368694,0.91786444,0.000007601691,0.00001798034,0.000037615515,0.07583417,0.0024970046,0.00011269492,0.000011652906,0.0005691464,0.0028410093],"study_design_scores_gemma":[0.0011423262,0.0023539905,0.9534495,0.00026752442,0.000019854437,0.00012797955,0.02693742,0.013883439,0.00009439961,0.0011579018,0.0003424584,0.00022323972],"about_ca_topic_score_codex":0.8693937,"about_ca_topic_score_gemma":0.99456555,"teacher_disagreement_score":0.12517181,"about_ca_system_score_codex":0.000015018333,"about_ca_system_score_gemma":0.0013149387,"threshold_uncertainty_score":0.9934165},"labels":[],"label_agreement":null},{"id":"W2135578166","doi":"10.1139/cjes-2012-0128","title":"Colombian-style emerald mineralization in the northern Canadian Cordillera: integration into a regional Paleozoic fluid flow regime","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Northwest Territories; University of Alberta; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Dolomite; Geochemistry; Fluid inclusions; Carbonate; Dolostone; Quartz; Pyrite; Meteoric water; Emerald; Metamorphism; Proterozoic; Paleozoic; Mineralization (soil science); Carbonate rock; Galena; Sedimentary rock; Mineralogy; Hydrothermal circulation; Sphalerite; Paleontology; Chemistry","score_opus":0.016677202309352553,"score_gpt":0.19177116518424103,"score_spread":0.1750939628748885,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135578166","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9748229,0.0006390537,0.000015582842,0.020515125,0.0001310164,0.00012393306,0.000008828975,0.0000024941394,0.0037410585],"genre_scores_gemma":[0.99514204,0.000028527582,0.00056979735,0.0039683925,0.000114848764,0.0000013047598,0.00003098324,0.000001246217,0.00014288203],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851257,0.00014959449,0.0003624162,0.0001832694,0.00035010072,0.00044205584],"domain_scores_gemma":[0.9987785,0.00010988297,0.00014387051,0.00010296439,0.00023775427,0.000627007],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00064052915,0.00012293577,0.00018694336,0.00040279567,0.00042573834,0.00025581688,0.0005648327,0.00006847288,0.008183664],"category_scores_gemma":[0.00024630976,0.000071257025,0.00009042023,0.001127306,0.00039230322,0.0004460169,0.0000026408304,0.00020804175,0.0001386247],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000044855783,0.000008178483,0.9778732,0.0000030508154,0.000012369399,0.00005281427,0.0013876138,0.005738497,0.00008169162,0.00009329841,0.0035590774,0.011185725],"study_design_scores_gemma":[0.00012767373,0.00028092804,0.955962,0.000039662853,0.000014486184,0.00007680749,0.0012956043,0.028304186,0.000023541263,0.007231019,0.0064674304,0.00017664008],"about_ca_topic_score_codex":0.92333275,"about_ca_topic_score_gemma":0.9992176,"teacher_disagreement_score":0.07588486,"about_ca_system_score_codex":0.0000070302144,"about_ca_system_score_gemma":0.00093356485,"threshold_uncertainty_score":0.992723},"labels":[],"label_agreement":null},{"id":"W2135863806","doi":"10.1139/e03-098","title":"Pleistocene volcanic damming of Yukon River and the maximum age of the Reid Glaciation, west-central Yukon","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Lethbridge; Simon Fraser University; Yukon Department of Environment; Yukon University","funders":"Simon Fraser University","keywords":"Geology; Glacial period; Outwash plain; Pleistocene; Tephra; Subaerial; Pillow lava; Paleontology; Stage (stratigraphy); Basalt; Breccia; Volcano; Pyroclastic rock; Volcanic rock; Geomorphology; Geochemistry","score_opus":0.016290298431592853,"score_gpt":0.21091905385922602,"score_spread":0.19462875542763317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135863806","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937516,0.0017849499,0.00001772081,0.0023896678,0.00036142033,0.00009584425,0.000011103201,8.811258e-7,0.0015868441],"genre_scores_gemma":[0.9995041,0.000080752805,0.00020217357,0.00013079587,0.000038089056,1.0950101e-7,0.0000011509458,8.910147e-7,0.000041962834],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998783,0.00017731849,0.00030420913,0.00010697556,0.0002739999,0.00035450215],"domain_scores_gemma":[0.9990908,0.0002015859,0.00027655304,0.00011069412,0.000103268314,0.00021707955],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0013987946,0.00007317931,0.00019746198,0.00015012568,0.00046085942,0.000030509651,0.00052151934,0.000057292866,0.00026611966],"category_scores_gemma":[0.00032110722,0.00003908986,0.00006935049,0.00040394053,0.0035788752,0.00018295555,0.000009143459,0.00022214529,0.00000464647],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027004095,0.0000022609536,0.9951334,0.0000074389154,0.000011055359,0.000020048139,0.0009360077,0.0026357789,0.0000066271086,0.0008484632,0.0000070617994,0.00036485516],"study_design_scores_gemma":[0.0005054302,0.00015792594,0.992682,0.00004206631,0.0000148598265,0.00019093373,0.00034727625,0.00016060272,0.00010588559,0.0055544563,0.00019393128,0.000044653247],"about_ca_topic_score_codex":0.026193395,"about_ca_topic_score_gemma":0.7211588,"teacher_disagreement_score":0.6949654,"about_ca_system_score_codex":0.0000010358208,"about_ca_system_score_gemma":0.0013114983,"threshold_uncertainty_score":0.9991328},"labels":[],"label_agreement":null},{"id":"W2136228559","doi":"10.1139/e10-051","title":"A revised life table and survivorship curve for <i>Albertosaurus sarcophagus</i> based on the Dry Island mass death assemblageThis article is one of a series of papers published in this Special Issue on the theme <i>Albertosaurus</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Dinosaur Research Institute; Florida State University","keywords":"Survivorship curve; Population; Demography; Life expectancy; Geography; Table (database); Archaeology; Ecology; Biology","score_opus":0.020832668889285297,"score_gpt":0.2094028989500421,"score_spread":0.1885702300607568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136228559","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9492257,0.0005288713,0.000004843502,0.023137696,0.0007118235,0.00028828206,0.00019748427,0.0000020051455,0.025903266],"genre_scores_gemma":[0.9967284,0.00004090857,0.00033077097,0.0022796905,0.0003907256,0.0000018826618,0.00000407316,0.0000025788095,0.00022094372],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982607,0.00033287192,0.00044824803,0.00022570889,0.00029326958,0.00043920995],"domain_scores_gemma":[0.9967613,0.0022774937,0.00035038317,0.0002029306,0.00012943745,0.00027845454],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0032217992,0.00014810548,0.0003352746,0.00022826756,0.00041876195,0.00007915947,0.0005625812,0.0001325114,0.011178727],"category_scores_gemma":[0.0020383343,0.000082508064,0.0000851892,0.00051791925,0.0012635436,0.00032543414,0.00000518267,0.00039834602,0.000006677726],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026762742,0.000021486625,0.99337006,0.000017980205,0.000022429433,0.000007808761,0.0007094681,0.00021193492,0.00075233914,0.0014461573,0.002716229,0.00045647478],"study_design_scores_gemma":[0.00080816966,0.0016652709,0.95714855,0.00014914466,0.000034392382,0.00002628024,0.0007406167,0.0033154837,0.0037506623,0.0041901,0.027932098,0.00023923638],"about_ca_topic_score_codex":0.017917922,"about_ca_topic_score_gemma":0.68060064,"teacher_disagreement_score":0.6626827,"about_ca_system_score_codex":0.0000021844276,"about_ca_system_score_gemma":0.0011453404,"threshold_uncertainty_score":0.9897252},"labels":[],"label_agreement":null},{"id":"W2136461485","doi":"10.1139/e05-004","title":"Correlation Chart of the evolution of the Trans-Hudson Orogen ManitobaSaskatchewan segment","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saskatchewan Disease Control Laboratory; Manitoba Hydro; University of Saskatchewan; University of Alberta; Saskatchewan Research Council (Canada); Geological Survey of Canada; Université du Québec à Montréal","funders":"","keywords":"Chart; Geology; Tectonics; Archean; Craton; Bounding overwatch; Geochronology; Paleontology; Geochemistry; Archaeology; Statistics; Geography","score_opus":0.011091172002503463,"score_gpt":0.1715629962039847,"score_spread":0.16047182420148126,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136461485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937948,0.0007345811,0.00005346514,0.0031756386,0.00022013199,0.00005519252,0.000021423775,8.921108e-7,0.0019438969],"genre_scores_gemma":[0.9994947,0.0000074082727,0.0002037755,0.00011849021,0.00006735791,6.684435e-8,6.440592e-7,4.8164117e-7,0.00010711156],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898565,0.000076972094,0.00030627707,0.00008536901,0.0003557928,0.00018992188],"domain_scores_gemma":[0.9993205,0.000049432136,0.0002713918,0.000091102156,0.000103214355,0.0001643597],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005359474,0.00006269948,0.00013108959,0.00007543825,0.0002324848,0.000017433342,0.00048145064,0.000036197,0.0019606974],"category_scores_gemma":[0.00007037528,0.000029299981,0.00015844344,0.0005905621,0.0005264598,0.00014321589,0.000004512122,0.00011677006,0.000006944845],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000028335915,0.0000046565115,0.97290516,0.0000027504218,0.000008681756,3.7485538e-7,0.0002488571,0.023966935,0.00034671364,0.00008441029,0.00004171599,0.0023869374],"study_design_scores_gemma":[0.00007960631,0.00008963705,0.98943824,0.00003244351,0.0000301052,0.000016361104,0.00085590244,0.00399065,0.002878484,0.0014657158,0.0010755794,0.00004729758],"about_ca_topic_score_codex":0.030048722,"about_ca_topic_score_gemma":0.6426957,"teacher_disagreement_score":0.612647,"about_ca_system_score_codex":0.0000042845804,"about_ca_system_score_gemma":0.00058261503,"threshold_uncertainty_score":0.9989517},"labels":[],"label_agreement":null},{"id":"W2136666184","doi":"10.1139/e10-100","title":"Late Wisconsinan glacial history in the Bonaparte Lake map area, south-central British Columbia: implications for glacial transport and mineral exploration<sup>1</sup>This article is one of a series of papers published in this Special Issue on the theme of<i>New insights in Cordilleran Intermontane geoscience: reducing exploration risk in the mountain pine beetle-affected area, British Columbia</i>.<sup>2</sup>Earth Sciences Sector Contribution Number: 20100093.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Stantec (Canada); Thompson Rivers University; Geological Survey of Canada","funders":"","keywords":"Geology; Glacial period; Plateau (mathematics); Ice sheet; Glacier; Sedimentology; Geomorphology; Glacial landform; Moraine; Physical geography; Geography","score_opus":0.03018174698976463,"score_gpt":0.2096751179453424,"score_spread":0.17949337095557777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136666184","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961149,0.0003289297,0.000004504947,0.0015599949,0.00015889067,0.0007020853,0.00023948694,0.0000026129226,0.00088857673],"genre_scores_gemma":[0.9992693,0.000109996385,0.00013859729,0.00016509659,0.00013141167,0.000012630634,0.000027024867,0.0000029386497,0.00014301689],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972701,0.00059707015,0.00080004305,0.0003433649,0.00042355526,0.00056588225],"domain_scores_gemma":[0.99868095,0.00036624604,0.00042059482,0.00015649547,0.00021083362,0.00016489375],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.003257147,0.00012557884,0.00041926533,0.00026256387,0.00054175034,0.00025848488,0.0006162057,0.0001308635,0.0051418715],"category_scores_gemma":[0.0005854086,0.00011921001,0.000081081205,0.0011329583,0.0028217551,0.0012673716,0.000008982057,0.0004341677,0.0000015578568],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010042002,0.00005526369,0.96840364,0.000011243244,0.000009549494,0.000032322714,0.029056251,0.00069684867,0.00002059782,0.000030526808,0.00085779687,0.00072553765],"study_design_scores_gemma":[0.0009598498,0.00077354244,0.98686934,0.0001856127,0.000017746925,0.00010847232,0.0068262215,0.0019195161,0.000015751808,0.001542798,0.000648043,0.00013311561],"about_ca_topic_score_codex":0.31134623,"about_ca_topic_score_gemma":0.993813,"teacher_disagreement_score":0.68246675,"about_ca_system_score_codex":0.000009571361,"about_ca_system_score_gemma":0.0014897952,"threshold_uncertainty_score":0.999892},"labels":[],"label_agreement":null},{"id":"W2137414555","doi":"10.1139/e00-107","title":"Geochronology of mid-Cretaceous to Eocene magmatism, Babine porphyry copper district, central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Government of British Columbia","funders":"McMaster University","keywords":"Geology; Rhyolite; Geochronology; Cretaceous; Geochemistry; Volcanic rock; Andesites; Magmatism; Porphyry copper deposit; Basalt; Zircon; Volcano; Paleontology; Andesite; Fluid inclusions; Hydrothermal circulation; Tectonics","score_opus":0.00969338878651019,"score_gpt":0.18150682121199227,"score_spread":0.17181343242548208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137414555","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918831,0.002092051,0.000034902325,0.0015708586,0.0002988988,0.000061138955,0.000117590724,0.0000041859294,0.003937298],"genre_scores_gemma":[0.99765146,0.00011215934,0.0012212343,0.00046121303,0.000109647095,1.5338122e-7,0.000011941674,0.0000013834198,0.00043080255],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99826294,0.00006307857,0.00046192048,0.0002202981,0.00031928378,0.0006724921],"domain_scores_gemma":[0.9982946,0.00009203514,0.00020688526,0.00009868517,0.00016439338,0.0011433876],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038100974,0.000098355515,0.00035010834,0.00015593563,0.00026483502,0.00020815375,0.00054363074,0.00006753937,0.028684469],"category_scores_gemma":[0.00027232897,0.00009758207,0.00013941704,0.0009671737,0.000641452,0.00020061887,0.000010339568,0.0001590708,0.000056976845],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000060838915,0.000007538581,0.9736885,0.000003974023,0.000015985866,0.00032673823,0.000031082323,0.0021074608,0.0000607758,0.0000034811078,0.001837997,0.021910395],"study_design_scores_gemma":[0.00015518327,0.00043685443,0.98574615,0.000031977586,0.00002314442,0.00068644685,0.000089537534,0.00028512138,0.00007027615,0.0015090285,0.010832582,0.00013370861],"about_ca_topic_score_codex":0.42995074,"about_ca_topic_score_gemma":0.9730027,"teacher_disagreement_score":0.54305196,"about_ca_system_score_codex":0.000003123692,"about_ca_system_score_gemma":0.00055675226,"threshold_uncertainty_score":0.97220343},"labels":[],"label_agreement":null},{"id":"W2137466239","doi":"10.1139/e03-059","title":"Hot spring sinters: keys to understanding Earth's earliest life forms","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":138,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Alberta","funders":"","keywords":"Archean; Geology; Hot spring; Mineralization (soil science); Extant taxon; Microbial mat; Earth (classical element); Paleontology; Geothermal gradient; Earth science; Taphonomy; Astrobiology; Biology; Evolutionary biology; Bacteria; Cyanobacteria","score_opus":0.05501655257359877,"score_gpt":0.23051778109380622,"score_spread":0.17550122852020744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137466239","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8557409,0.0026544956,0.00086637936,0.0008206699,0.0009908618,0.00008288441,0.000011558247,0.000006610876,0.13882564],"genre_scores_gemma":[0.9972941,0.00001656848,0.0022383153,0.000330163,0.00006988884,1.15658985e-7,1.785966e-7,9.528889e-7,0.00004969072],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99846405,0.00008322396,0.0003335286,0.00019309891,0.0002927602,0.00063337],"domain_scores_gemma":[0.998141,0.00013615623,0.00015343634,0.00010009023,0.000045940105,0.0014233645],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011529776,0.00013597378,0.00021931948,0.00055419275,0.00076089386,0.0002968854,0.00041867341,0.000066210865,0.0008241129],"category_scores_gemma":[0.000344828,0.00010562847,0.0001083993,0.00058252655,0.0005285572,0.00068159366,8.607664e-7,0.00022093071,0.000043036554],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000109434,0.0000025699467,0.98997027,0.000003862039,0.000019521294,0.000106470674,0.00049103494,0.0007657227,0.000016029602,0.006399075,0.000098128956,0.0021163845],"study_design_scores_gemma":[0.00016889047,0.00048044318,0.9906107,0.000066250774,0.000009044705,0.00014990782,0.001974626,0.000082726096,0.00011564729,0.002051019,0.0041155587,0.00017516343],"about_ca_topic_score_codex":0.006108048,"about_ca_topic_score_gemma":0.6456707,"teacher_disagreement_score":0.63956267,"about_ca_system_score_codex":0.000002932028,"about_ca_system_score_gemma":0.0017240375,"threshold_uncertainty_score":0.9233582},"labels":[],"label_agreement":null},{"id":"W2137788276","doi":"10.1139/e07-068","title":"Internal structure and the thermal and hydrological regime of a typical lithalsa: significance for permafrost growth and decay","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université Laval; Center for Northern Studies","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Permafrost; Geology; Aggradation; Thermokarst; Frost heaving; Groundwater; Context (archaeology); Geomorphology; Ice wedge; Hydrology (agriculture); Geotechnical engineering; Paleontology; Structural basin","score_opus":0.034186590831262735,"score_gpt":0.22405339539986358,"score_spread":0.18986680456860083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137788276","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99320424,0.004246955,0.000006679611,0.0014578663,0.00012231356,0.00009430213,0.00050538074,9.571439e-7,0.0003613354],"genre_scores_gemma":[0.99900734,0.0003818273,0.00016309084,0.00029304836,0.00012967983,2.1203887e-7,0.0000054310194,0.0000013319965,0.000018030014],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992276,0.00006314918,0.00020381268,0.00013503764,0.00013868403,0.00023171799],"domain_scores_gemma":[0.9990848,0.00036313196,0.00013538256,0.000044898832,0.000055901382,0.0003159431],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004460465,0.00008797871,0.00020635231,0.00008923545,0.00038170206,0.000073416726,0.00018620488,0.000049123657,0.00029488883],"category_scores_gemma":[0.00010598829,0.000047038935,0.000036725778,0.00011170852,0.0024756615,0.00019369832,0.0000073109545,0.00012876478,3.5356652e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012916785,0.0000012482886,0.9973495,0.0000103502025,0.000007889929,0.000027363014,0.0012817063,0.000019125073,0.0002693872,0.0002638305,0.00004253199,0.0005979122],"study_design_scores_gemma":[0.0005475922,0.0003925869,0.99541706,0.000025030053,0.000013048873,0.0010760126,0.00027440267,0.0008928541,0.00022227105,0.00067973405,0.00038556402,0.000073846204],"about_ca_topic_score_codex":0.0055659516,"about_ca_topic_score_gemma":0.08233417,"teacher_disagreement_score":0.07676821,"about_ca_system_score_codex":4.9141397e-7,"about_ca_system_score_gemma":0.00021356938,"threshold_uncertainty_score":0.93441087},"labels":[],"label_agreement":null},{"id":"W2138351677","doi":"10.1139/e05-026","title":"The Sask Craton and Hearne Province margin: seismic reflection studies in the western Trans-Hudson Orogen","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of British Columbia; Geological Survey of Canada; University of Regina","funders":"Natural Sciences and Engineering Research Council of Canada; University of Saskatchewan","keywords":"Geology; Craton; Terrane; Tectonics; Archean; Seismology; Paleontology; Subduction; Crust; Continental margin","score_opus":0.037895660862384085,"score_gpt":0.2496206674922107,"score_spread":0.21172500662982663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138351677","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96721303,0.01052324,0.0000041713465,0.021282485,0.00009194247,0.00006139529,0.0000033879269,0.0000017046648,0.00081863033],"genre_scores_gemma":[0.99828565,0.00047429564,0.00008739808,0.0008791227,0.000112262,2.9227957e-7,5.087259e-7,5.5471725e-7,0.00015990139],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895006,0.00014764475,0.0002321532,0.00012899522,0.00023420242,0.00030692015],"domain_scores_gemma":[0.999365,0.0002525801,0.00009196176,0.00006043771,0.000046686215,0.00018337094],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015109357,0.0000828335,0.0001437536,0.00009493272,0.0005750938,0.0001547397,0.000322464,0.000028665292,0.00012478304],"category_scores_gemma":[0.000109288114,0.000035487028,0.000048428443,0.0004308683,0.0007385676,0.00023959322,0.000003125586,0.00018865714,0.000009731144],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013696409,0.000003097774,0.95939535,0.00000488385,0.000013980894,0.000033861554,0.00085880025,0.0034686986,0.000020464186,0.00002106936,0.0001621388,0.036003962],"study_design_scores_gemma":[0.00022495103,0.0007156097,0.9217148,0.00004561578,0.00003316156,0.0003404269,0.0025881894,0.0030580682,0.00022068176,0.0033000808,0.06760697,0.00015149254],"about_ca_topic_score_codex":0.010654876,"about_ca_topic_score_gemma":0.87241685,"teacher_disagreement_score":0.861762,"about_ca_system_score_codex":0.0000022363693,"about_ca_system_score_gemma":0.00023431997,"threshold_uncertainty_score":0.99593323},"labels":[],"label_agreement":null},{"id":"W2138791978","doi":"10.1139/cjes-2014-0069","title":"Stratigraphy of the Danek Bonebed (Upper Cretaceous Horseshoe Canyon Formation, central Alberta) and correlations with strata in the Drumheller and Grande Prairie regions","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Geology; Canyon; Paleontology; Stratigraphy; Cretaceous; Assemblage (archaeology); Geomorphology; Tectonics","score_opus":0.011043804457913007,"score_gpt":0.18505009609302794,"score_spread":0.17400629163511494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138791978","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9902819,0.0013995359,0.000076054515,0.0028771462,0.000115339964,0.00008876397,0.000017562945,6.8490425e-7,0.0051430217],"genre_scores_gemma":[0.9995874,0.00004684425,0.0001654198,0.00015160811,0.000018409404,2.1159121e-7,0.0000025576142,4.8343406e-7,0.000027056365],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99921924,0.00017728962,0.00018711107,0.000085580614,0.00010821835,0.00022256986],"domain_scores_gemma":[0.9993795,0.0002130676,0.00014669668,0.00007246779,0.000037747075,0.00015050893],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046602925,0.00006522139,0.00010341347,0.0001269143,0.00042598398,0.000031383126,0.00020985438,0.00004322032,0.000045955883],"category_scores_gemma":[0.00008071255,0.000032498945,0.000022992243,0.00029206954,0.001379589,0.00036125103,0.00000173176,0.00014622687,4.6510834e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009833261,0.0000021456603,0.9953768,0.0000022614893,0.0000049823097,0.0000029542846,0.0013190049,0.00045700392,0.0000013307766,0.002452691,0.00010110666,0.0002698655],"study_design_scores_gemma":[0.00015577878,0.00024743914,0.9926345,0.000023921659,0.0000133085205,0.0004699969,0.0012906062,0.0011631973,0.0000021155904,0.0022177182,0.0017338702,0.000047571204],"about_ca_topic_score_codex":0.019371783,"about_ca_topic_score_gemma":0.96676546,"teacher_disagreement_score":0.94739366,"about_ca_system_score_codex":5.584842e-7,"about_ca_system_score_gemma":0.0004186115,"threshold_uncertainty_score":0.9871583},"labels":[],"label_agreement":null},{"id":"W2138833544","doi":"10.1139/e07-032","title":"Ontogeny of <i>Parabolinella</i> <i>panosa</i> (Olenidae, Trilobita) from the uppermost Furongian (Upper Cambrian) of northwestern Canada, with discussion of olenid protaspides","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"University of Alberta","keywords":"Ontogeny; Paleontology; Geology; Monophyly; Period (music); Biology; Phylogenetics; Clade","score_opus":0.011594351886498523,"score_gpt":0.1986134843249364,"score_spread":0.18701913243843787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138833544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887865,0.004987364,0.000035016026,0.00062075665,0.00044014555,0.00017986397,0.0004494324,0.0000015976751,0.0044992873],"genre_scores_gemma":[0.9989365,0.000037283924,0.00077244214,0.00010733937,0.00010555263,1.914412e-7,0.0000041112207,0.0000016512416,0.000034958408],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977088,0.00012219152,0.0008169696,0.00021034987,0.0006321935,0.0005095262],"domain_scores_gemma":[0.99773324,0.00036412085,0.00085498625,0.00021618596,0.00029970836,0.00053175533],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011074902,0.00018751783,0.00046653193,0.00021270382,0.0002964526,0.00002959368,0.00078806526,0.00008181708,0.000140612],"category_scores_gemma":[0.0001164905,0.00008717657,0.00013327337,0.0006092915,0.0015205743,0.0003074786,0.000002438194,0.00022846204,6.2243225e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010673285,0.0000090108615,0.9852611,0.000011529144,0.00004378764,0.000049057468,0.00054007175,0.00021694032,0.00030095872,0.000021750671,0.00008933502,0.013349767],"study_design_scores_gemma":[0.00035463416,0.0006019593,0.9920214,0.0002114203,0.000045167668,0.00006662631,0.0017691741,0.00002707755,0.004134835,0.00007280944,0.0005591328,0.0001357785],"about_ca_topic_score_codex":0.84383625,"about_ca_topic_score_gemma":0.99920017,"teacher_disagreement_score":0.15536393,"about_ca_system_score_codex":0.0000026336936,"about_ca_system_score_gemma":0.004570253,"threshold_uncertainty_score":0.8107433},"labels":[],"label_agreement":null},{"id":"W2138975848","doi":"10.1139/e05-046","title":"Geology and juxtaposition history of the Yukon-Tanana, Slide Mountain, and Cassiar terranes in the Glenlyon area of central Yukon","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; University of British Columbia; Ministry of Energy, Northern Development and Mines; Yukon University; Geological Survey of Canada","funders":"","keywords":"Geology; Terrane; Batholith; Clastic rock; Geochemistry; Pluton; Paleozoic; Paleontology; Petrology; Geomorphology; Tectonics; Sedimentary rock","score_opus":0.016121241998354997,"score_gpt":0.17773415603626305,"score_spread":0.16161291403790806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138975848","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9888612,0.005284274,0.00000263966,0.0039236248,0.00007856091,0.000038802635,0.000008158446,5.146131e-7,0.0018022135],"genre_scores_gemma":[0.9992609,0.00009573841,0.00012954706,0.00042871456,0.000035406265,8.194836e-8,9.289758e-7,4.063142e-7,0.000048284703],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909836,0.00010775269,0.00026917824,0.00010337479,0.00018635804,0.0002349548],"domain_scores_gemma":[0.99941653,0.00012785477,0.00018520659,0.00006389014,0.00004511364,0.00016138237],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005632649,0.000068496156,0.0001716429,0.00013043593,0.00009955148,0.000016307677,0.0002746831,0.00004121142,0.0006011079],"category_scores_gemma":[0.000098443095,0.000033771747,0.00005158052,0.00023275572,0.0010737072,0.00015282915,0.000005469577,0.00012934845,6.295817e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007917407,0.0000049223054,0.99396306,0.000006024973,0.0000057009584,0.000010795412,0.00072895456,0.0016302526,0.00011879882,0.00010020131,0.000102738624,0.0033206127],"study_design_scores_gemma":[0.0001024895,0.00015049224,0.99334615,0.000023080185,0.000018125771,0.00012813743,0.00064995914,0.0021937673,0.00010193141,0.0015320665,0.0017042788,0.000049521084],"about_ca_topic_score_codex":0.053219113,"about_ca_topic_score_gemma":0.63093275,"teacher_disagreement_score":0.57771367,"about_ca_system_score_codex":0.000004181566,"about_ca_system_score_gemma":0.0002850554,"threshold_uncertainty_score":0.9530856},"labels":[],"label_agreement":null},{"id":"W2139144132","doi":"10.1139/e05-011","title":"Geochemistry of metasedimentary rocks of the Proterozoic Xingxingxia complex: implications for provenance and tectonic setting of the eastern segment of the Central Tianshan Tectonic Zone, northwestern China","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Proterozoic; Provenance; Felsic; Geochemistry; Archean; Sedimentary rock; Continental margin; Continental crust; Greenschist; Tectonics; Petrology; Mafic; Crust; Metamorphism; Paleontology","score_opus":0.011720142001623825,"score_gpt":0.2043541699526141,"score_spread":0.19263402795099027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139144132","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969182,0.00055550766,0.000024581213,0.0016787647,0.00006118384,0.00024750677,0.0003652199,6.8795e-7,0.00014831849],"genre_scores_gemma":[0.9995248,0.00000621127,0.00033472056,0.000053680662,0.00003280949,0.0000011999816,0.0000044786148,0.000001530766,0.000040596125],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988008,0.000046611276,0.00048217675,0.00013576828,0.00026048243,0.00027412103],"domain_scores_gemma":[0.99872094,0.000045772376,0.0008151015,0.00020360979,0.000088038716,0.00012652326],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045456225,0.00010268585,0.00020975676,0.00004639781,0.00034472966,0.000021558955,0.000705229,0.00002741055,0.00010996946],"category_scores_gemma":[0.000034190358,0.000054111748,0.00017811148,0.00040533065,0.0005728863,0.00012328284,0.00002571235,0.00011240805,1.0225163e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005626406,0.000011259745,0.9828673,0.00007318364,0.000039890172,9.942755e-8,0.00040078326,0.0038949854,0.0104665505,0.0000025647892,0.000012382283,0.002225387],"study_design_scores_gemma":[0.00017883767,0.000079670834,0.92112386,0.00018039875,0.00007582714,0.00003062758,0.00040186848,0.001956951,0.075691685,0.00008364669,0.00013607532,0.0000605781],"about_ca_topic_score_codex":0.01543237,"about_ca_topic_score_gemma":0.20046653,"teacher_disagreement_score":0.18503417,"about_ca_system_score_codex":0.0000053426643,"about_ca_system_score_gemma":0.0006092353,"threshold_uncertainty_score":0.991124},"labels":[],"label_agreement":null},{"id":"W2139267204","doi":"10.1139/cjes-2013-0220","title":"Brown bear (<i>Ursus arctos</i>) (9880 ± 35 BP) from late-glacial Champlain Sea deposits at Saint-Nicolas, Quebec, Canada, and the dispersal history of brown bears","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Wildlife Ecology and Conservation","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Musée de la Civilisation; Canadian Museum of Nature","funders":"University of California, Irvine","keywords":"Ursus; Radiocarbon dating; Geology; Fauna; Quaternary; Biological dispersal; Glacial period; Paleontology; Archaeology; Accelerator mass spectrometry; Oceanography; Geography; Ecology; Biology","score_opus":0.007709717685060931,"score_gpt":0.168218236599544,"score_spread":0.16050851891448306,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139267204","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931048,0.000509721,0.000018427832,0.0038701133,0.00081346027,0.00009192431,0.000014334629,0.0000021641672,0.001575028],"genre_scores_gemma":[0.9962402,0.000013709607,0.00011970892,0.0021369478,0.00010294363,0.0000012453914,0.0000017126991,0.0000051119964,0.0013784036],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984554,0.00021357599,0.00032724807,0.00020181586,0.00044198343,0.0003599484],"domain_scores_gemma":[0.99878395,0.00028873072,0.000300728,0.00013130342,0.00003317861,0.00046210352],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010159555,0.000120973746,0.00022413356,0.0000706968,0.00042876636,0.00003913915,0.0004462598,0.00007092476,0.00081353454],"category_scores_gemma":[0.0002669463,0.000090127374,0.000056344914,0.00015869566,0.0021878595,0.0002817517,0.000045416728,0.00019405453,0.000010169044],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004500156,0.000004320072,0.9859051,0.0000020823798,0.00001537472,0.000017656954,0.0008931753,0.00047526383,0.00020747249,0.0001816225,0.011002669,0.0012502422],"study_design_scores_gemma":[0.00052400515,0.000075608245,0.9453795,0.000022096243,0.000021592137,0.000024741375,0.00010391541,0.00077298214,0.00006863128,0.00015104542,0.05274153,0.00011433256],"about_ca_topic_score_codex":0.97173667,"about_ca_topic_score_gemma":0.9998535,"teacher_disagreement_score":0.04173886,"about_ca_system_score_codex":0.00038781314,"about_ca_system_score_gemma":0.0019919246,"threshold_uncertainty_score":0.8907633},"labels":[],"label_agreement":null},{"id":"W2139564898","doi":"10.1139/e07-067","title":"Protolith age and timing of Precambrian magmatic and metamorphic events in the Priest River complex, northern Rockies","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"University of Wyoming; National Science Foundation","keywords":"Zircon; Geology; Gneiss; Metamorphic rock; Geochemistry; Precambrian; Metamorphism; Archean; Geochronology; Protolith","score_opus":0.046592818761233216,"score_gpt":0.20697281976455048,"score_spread":0.16038000100331726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139564898","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99743074,0.00077310344,0.000002720498,0.0006271948,0.000018752133,0.000097474374,0.0000072691896,7.6473816e-7,0.0010419927],"genre_scores_gemma":[0.9992539,0.000036615787,0.0005510096,0.00011284776,0.000016721717,3.0974704e-7,0.0000013232262,4.9259995e-7,0.000026740416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991415,0.00009336974,0.00023930366,0.00010188893,0.0002169807,0.00020694722],"domain_scores_gemma":[0.99944025,0.00012010207,0.0001359178,0.000050018843,0.000043852197,0.00020986561],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005667205,0.00007154506,0.00019240878,0.0001452908,0.00024163851,0.000024762168,0.000239096,0.000022353262,0.00033284648],"category_scores_gemma":[0.00013748943,0.000037948434,0.00003586725,0.00034969626,0.0009922951,0.00016374979,0.000005763504,0.00010579342,0.000002481862],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002959825,0.0000032091264,0.99786496,0.000008572271,0.000006299832,0.00006284453,0.0009691967,0.00018630744,0.000009996728,0.000020018315,0.0000032691053,0.0008623577],"study_design_scores_gemma":[0.00009557372,0.00013205726,0.9937447,0.000025555186,0.00001178414,0.00021934016,0.00041084812,0.0008903805,0.00001134979,0.0042598695,0.00014604653,0.000052516774],"about_ca_topic_score_codex":0.030361453,"about_ca_topic_score_gemma":0.6022425,"teacher_disagreement_score":0.57188106,"about_ca_system_score_codex":5.4444433e-7,"about_ca_system_score_gemma":0.00015538617,"threshold_uncertainty_score":0.97609544},"labels":[],"label_agreement":null},{"id":"W2139726675","doi":"10.1139/e05-065","title":"A midge-based late-glacial temperature reconstruction from southwestern Nova Scotia","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Macrofossil; Nova scotia; Younger Dryas; Glacial period; Geology; Physical geography; Midge; Last Glacial Maximum; Climate change; Holocene; Oceanography; Paleontology; Geography; Ecology; Gall","score_opus":0.02237606911911826,"score_gpt":0.22805403555686862,"score_spread":0.20567796643775035,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139726675","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924106,0.0009557179,0.000007249719,0.0025799382,0.0011722869,0.000053063348,0.000053332456,0.0000048425636,0.0027629856],"genre_scores_gemma":[0.9972485,0.0000061690957,0.0017450918,0.00052353035,0.0003775255,4.9114263e-8,0.00001063117,0.0000015202237,0.00008701919],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99866235,0.00014348615,0.00028694043,0.00019312323,0.00023703068,0.00047708652],"domain_scores_gemma":[0.9989199,0.00015398559,0.00014913552,0.0000936562,0.00012331278,0.0005600095],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007261316,0.00011228537,0.0001963716,0.0004059151,0.0004104788,0.00015694859,0.00041448456,0.00014981475,0.0082535185],"category_scores_gemma":[0.0001124829,0.00008665244,0.00007711378,0.00039198558,0.00095919764,0.0004363779,0.0000025147065,0.00039506014,0.0005407202],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018017043,0.0000023819252,0.9945005,0.0000017804925,0.0000098465935,0.00007766061,0.00015559592,0.0031783525,0.000029330504,0.000006428381,0.000060832193,0.0019592554],"study_design_scores_gemma":[0.0003054983,0.00017701981,0.99612683,0.00003939613,0.000010460263,0.00034529142,0.00015428665,0.0011515347,0.00021668083,0.0002087186,0.0011511861,0.000113078524],"about_ca_topic_score_codex":0.013030151,"about_ca_topic_score_gemma":0.9349846,"teacher_disagreement_score":0.92195445,"about_ca_system_score_codex":7.762243e-7,"about_ca_system_score_gemma":0.0020054386,"threshold_uncertainty_score":0.9935422},"labels":[],"label_agreement":null},{"id":"W2139807024","doi":"10.1139/e09-043","title":"Insights from geodynamical modeling on possible fates of continental mantle lithosphere: collision, removal, and overturnThis article is one of a series of papers published in this Special Issue on the theme <i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto; Geological Survey of Canada; Dalhousie University","funders":"","keywords":"Lithosphere; Geology; Mantle (geology); Subduction; Hotspot (geology); Crust; Obduction; Craton; Geophysics; Collision zone; Eclogitization; Crustal recycling; Continental collision; Continental margin; Continental crust; Oceanic crust; Tectonics; Seismology","score_opus":0.008690936344850438,"score_gpt":0.17552268013368402,"score_spread":0.1668317437888336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139807024","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938934,0.00090696645,0.000002406761,0.0031640334,0.00006889384,0.000098280405,0.00005668212,7.6228804e-7,0.0018086141],"genre_scores_gemma":[0.99916613,0.00008388262,0.00055984815,0.000100455094,0.00005285909,2.7195114e-7,0.000001655015,9.646053e-7,0.00003390441],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99881274,0.00007823318,0.00046360155,0.00015520453,0.00033365385,0.00015657378],"domain_scores_gemma":[0.9987915,0.00045072075,0.00033991327,0.000098370285,0.00018659655,0.00013287092],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005405194,0.00009102117,0.0003323541,0.00011431614,0.000109820816,0.000051208088,0.0002604999,0.000057150562,0.002480693],"category_scores_gemma":[0.00073233363,0.00004379941,0.00006158744,0.0006005987,0.0013729451,0.00022060184,0.000012001409,0.00018816868,6.019115e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013073657,0.00014293102,0.96967584,0.00008514036,0.00012495072,0.000015495792,0.004670662,0.0040980075,0.012555293,0.005363037,0.00019272813,0.0017685647],"study_design_scores_gemma":[0.003228347,0.002314359,0.68420196,0.0009343382,0.00020487657,0.00005704717,0.011242937,0.12059564,0.06845606,0.10741681,0.0008903502,0.00045726396],"about_ca_topic_score_codex":0.0568338,"about_ca_topic_score_gemma":0.21705219,"teacher_disagreement_score":0.28547385,"about_ca_system_score_codex":0.0000014899452,"about_ca_system_score_gemma":0.00022383724,"threshold_uncertainty_score":0.99843115},"labels":[],"label_agreement":null},{"id":"W2140043134","doi":"10.1139/cjes-2014-0065","title":"Implications of finding a ceratopsian horncore in the Danek bonebed","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Paleontology; Canyon; Geomorphology","score_opus":0.029566296999247548,"score_gpt":0.23463214913419067,"score_spread":0.20506585213494313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140043134","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.972685,0.0007640908,0.00006873111,0.003383988,0.00022238259,0.000039924547,0.000016982174,9.701608e-7,0.022817926],"genre_scores_gemma":[0.99912864,0.000011733649,0.0004490447,0.00033523235,0.000057771744,1.4633352e-7,0.000002401851,3.6569335e-7,0.0000146681705],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99920857,0.0001578021,0.00022423896,0.000082379105,0.00008949844,0.00023752726],"domain_scores_gemma":[0.9993598,0.0002402425,0.00014146758,0.00007677252,0.000038710295,0.00014303917],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012967364,0.000048691807,0.00011426545,0.00023914693,0.00026437626,0.000021289012,0.0004508166,0.000042244028,0.00031457236],"category_scores_gemma":[0.00017487668,0.000030261828,0.00003634596,0.00041677593,0.0006304122,0.00019232543,0.000001354792,0.00012761164,0.00001049402],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002355275,0.0000017177067,0.9939168,0.0000013002141,0.0000020053956,0.0000057528896,0.00035028323,0.0005576619,0.0000120116065,0.0023896643,0.00009241334,0.0026680399],"study_design_scores_gemma":[0.00007061494,0.00017492003,0.9899747,0.000011590206,0.0000032189241,0.00022343945,0.0003892133,0.00041191065,0.000004774911,0.0049164644,0.0037814637,0.000037710353],"about_ca_topic_score_codex":0.0069068978,"about_ca_topic_score_gemma":0.7067318,"teacher_disagreement_score":0.69982487,"about_ca_system_score_codex":8.482164e-7,"about_ca_system_score_gemma":0.0005648382,"threshold_uncertainty_score":0.9997062},"labels":[],"label_agreement":null},{"id":"W2140286229","doi":"10.1139/e11-071","title":"Probing the composition of unexposed basement, South Portuguese Zone, southern Iberia: implications for the connections between the Appalachian and Variscan orogens","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of British Columbia; St. Francis Xavier University","funders":"","keywords":"Geology; Terrane; Batholith; Zircon; Devonian; Carboniferous; Paleozoic; Geochemistry; Continental crust; Basement; Late Devonian extinction; Detritus; Crust; Paleontology; Orogeny; Tectonics","score_opus":0.03228985423032123,"score_gpt":0.21907423518097588,"score_spread":0.18678438095065464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140286229","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.985769,0.0012557891,0.000805271,0.011321284,0.00009379066,0.00018305508,0.00023355402,0.0000021954002,0.00033610908],"genre_scores_gemma":[0.9992909,0.000012404947,0.00025933693,0.00024335436,0.00015858332,0.000001569991,0.000009573553,9.957739e-7,0.00002331702],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991628,0.00008096779,0.0002574536,0.00008902084,0.00012651448,0.0002832351],"domain_scores_gemma":[0.99869615,0.0005510536,0.00024289169,0.000103672,0.000098104734,0.00030812132],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012337392,0.00007375147,0.00012640985,0.00006652954,0.0011350769,0.00007232408,0.00033899472,0.00002622974,0.00040707152],"category_scores_gemma":[0.000103972045,0.000029965751,0.00009252963,0.00039381647,0.0007391505,0.00011785042,0.0000068363993,0.00011766375,0.0000035046316],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002390887,0.0000035863948,0.9950873,0.0000021223152,0.000041952117,1.2671951e-7,0.001118197,0.0007021091,0.000069205875,0.0003859939,0.00003574076,0.0025512208],"study_design_scores_gemma":[0.00008205672,0.00009231619,0.99232244,0.000007834471,0.00013072554,0.000020587235,0.0035456624,0.0005231539,0.00008173055,0.002191082,0.0009451156,0.000057289784],"about_ca_topic_score_codex":0.012285977,"about_ca_topic_score_gemma":0.10394256,"teacher_disagreement_score":0.09165658,"about_ca_system_score_codex":0.0000010512919,"about_ca_system_score_gemma":0.00019230526,"threshold_uncertainty_score":0.9942913},"labels":[],"label_agreement":null},{"id":"W2140421150","doi":"10.1139/e09-003","title":"Soft lodgement till deposition and syndepositional deformation, Anielinek, the Polish Lowlands","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Glacier; Geomorphology; Glacial period; Deposition (geology); Geochemistry; Debris; Sediment; Intrusion; Oceanography","score_opus":0.015273562359315823,"score_gpt":0.2258052350182606,"score_spread":0.2105316726589448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140421150","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9847022,0.0015848245,0.0001311174,0.0076753674,0.00021685504,0.000055737586,0.000009734252,0.0000025170707,0.005621641],"genre_scores_gemma":[0.9981566,0.00004767246,0.00036784587,0.0012865615,0.00009345173,9.147714e-8,0.0000067483948,4.3597092e-7,0.000040592502],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99912333,0.00008458934,0.00020203958,0.00008668792,0.00020981817,0.00029350226],"domain_scores_gemma":[0.99933994,0.0001040248,0.00009533418,0.000051286414,0.00011480886,0.00029461368],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008811742,0.00006328866,0.00009126139,0.00018689033,0.00076744054,0.00013491664,0.0002354761,0.000047028818,0.00048340042],"category_scores_gemma":[0.00007269014,0.000038416132,0.000030353049,0.0002273453,0.00047797387,0.00036992173,0.00000221744,0.00016582545,0.000029933795],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006303103,0.000001924272,0.9975368,0.0000017262945,0.000004864366,0.000031093092,0.00015130013,0.00065122853,0.0000019825309,0.00032893757,0.00021978214,0.0010640721],"study_design_scores_gemma":[0.00011151812,0.00031991975,0.9924261,0.000015806556,0.0000075151775,0.0012788101,0.00016601708,0.0029949092,0.000023028602,0.001963732,0.00063933415,0.000053287247],"about_ca_topic_score_codex":0.00090056076,"about_ca_topic_score_gemma":0.081146896,"teacher_disagreement_score":0.08024633,"about_ca_system_score_codex":4.2753584e-7,"about_ca_system_score_gemma":0.0004867456,"threshold_uncertainty_score":0.9356198},"labels":[],"label_agreement":null},{"id":"W2140563828","doi":"10.1139/e04-072","title":"Systematics and phytogeography of selected Eocene Okanagan Highlands plants","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Disjunct; Phytogeography; Betulaceae; Taxon; Fagaceae; Geography; Ecology; Botany; Biology","score_opus":0.018195970238479714,"score_gpt":0.1738716860909848,"score_spread":0.1556757158525051,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140563828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99831945,0.00058315846,0.0000012977306,0.0004961381,0.000082452854,0.000028986482,0.00006468394,0.0000024106155,0.00042141165],"genre_scores_gemma":[0.999603,0.000063964566,0.00017500372,0.00004554022,0.000090822745,5.6567014e-8,0.000002860257,1.2980738e-7,0.000018634457],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99939877,0.00002999185,0.00016775719,0.000067354806,0.00015971452,0.00017639462],"domain_scores_gemma":[0.9994462,0.0000566533,0.00015604764,0.000013115586,0.00009067842,0.00023727876],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034208238,0.00005052845,0.00013002133,0.00007282438,0.00023140584,0.00004336754,0.00017919259,0.00003507712,0.00005738864],"category_scores_gemma":[0.000037119862,0.000020565143,0.00003285821,0.0004077553,0.00016954239,0.00020817338,0.0000061749774,0.000052728497,0.0000019989477],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014221325,0.000019372843,0.97982365,0.000026378695,0.000028520966,0.000022891236,0.00033580806,0.000121198755,0.01193314,0.0002726597,0.0010701616,0.0063319956],"study_design_scores_gemma":[0.00009152923,0.00026850356,0.9936588,0.0001136582,0.000011332355,0.0001324523,0.0004725702,0.00020496477,0.0010405489,0.000076184544,0.0038549567,0.00007449408],"about_ca_topic_score_codex":0.0018310489,"about_ca_topic_score_gemma":0.11603347,"teacher_disagreement_score":0.114202425,"about_ca_system_score_codex":0.0000023760263,"about_ca_system_score_gemma":0.00007759909,"threshold_uncertainty_score":0.9000966},"labels":[],"label_agreement":null},{"id":"W2140609040","doi":"10.1139/cjes-2014-0131","title":"Slipstream: an early Holocene slump and turbidite record from the frontal ridge of the Cascadia accretionary wedge off western Canada and paleoseismic implications","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Camosun College","funders":"","keywords":"Geology; Slumping; Turbidity current; Turbidite; Abyssal plain; Sedimentary rock; Geomorphology; Subduction; Sedimentary structures; Paleontology; Seismology; Oceanography; Sediment; Sedimentary depositional environment; Tectonics","score_opus":0.03002568712453857,"score_gpt":0.2084643318653791,"score_spread":0.17843864474084054,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140609040","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99340373,0.0028433308,0.0000029438502,0.0025834432,0.0002951369,0.00006366573,0.00042206526,0.0000014151747,0.00038425694],"genre_scores_gemma":[0.9991689,0.00009308679,0.00017105773,0.00043502182,0.00007647039,2.3667607e-7,0.000011509526,9.585366e-7,0.000042773347],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99921423,0.000084013125,0.00022018078,0.00010903668,0.00018182417,0.0001906975],"domain_scores_gemma":[0.9989885,0.00014910815,0.00017540352,0.000103976476,0.00011489194,0.0004681249],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038015854,0.00007682965,0.00011480183,0.000050037685,0.00042524212,0.0001189596,0.00039854826,0.00003433278,0.00012202018],"category_scores_gemma":[0.00009995753,0.00004001791,0.00002149794,0.00023432457,0.0005182715,0.00043449536,0.000009569268,0.00012730899,0.0000021366313],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000037033046,0.0000011715434,0.99210536,0.0000010930122,0.0000041828544,0.0000025465104,0.00036828467,0.0001358212,0.0000013764791,0.000011077005,0.0003365317,0.0070288586],"study_design_scores_gemma":[0.00009020799,0.0001328442,0.9924923,0.0000158283,0.000010594333,0.000087891916,0.0007486259,0.00025736183,0.000009163648,0.0007328298,0.0053630644,0.000059276812],"about_ca_topic_score_codex":0.87522405,"about_ca_topic_score_gemma":0.9942712,"teacher_disagreement_score":0.119047165,"about_ca_system_score_codex":0.0000022443705,"about_ca_system_score_gemma":0.0016872851,"threshold_uncertainty_score":0.32706615},"labels":[],"label_agreement":null},{"id":"W2140859058","doi":"10.1139/e05-096","title":"UPb constraints on the thermotectonic evolution of the Vernon antiform and the age of the Aberdeen gneiss complex, southeastern Canadian Cordillera","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Vernon Jubilee Hospital; University of British Columbia; Geological Survey of Canada; University of Alberta","funders":"","keywords":"Geology; Anticline; Gneiss; Metamorphism; Geochemistry; Metamorphic rock; Zircon; Shear zone; Metamorphic core complex; Orogeny; Geomorphology; Paleontology; Tectonics; Extensional definition","score_opus":0.015130448210235717,"score_gpt":0.17160911439574858,"score_spread":0.15647866618551287,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140859058","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97682065,0.00051619485,0.0000024380656,0.006318439,0.00013477827,0.00012016886,0.000080652324,8.8616054e-7,0.01600577],"genre_scores_gemma":[0.99945694,0.0000070701967,0.0000116459305,0.00040653886,0.000043276534,1.4371894e-7,0.0000011890431,9.4908427e-7,0.00007227391],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987032,0.00019102618,0.00030917904,0.00011623184,0.00036129614,0.000319086],"domain_scores_gemma":[0.9990264,0.00026235505,0.00027901414,0.00016931743,0.00008940449,0.00017348985],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009308873,0.00010132939,0.00020373044,0.000085439526,0.0007106345,0.00006765119,0.0008193825,0.00004125234,0.0021916514],"category_scores_gemma":[0.00014710761,0.000034629196,0.00015831197,0.00054135435,0.004093746,0.000058780995,0.00001203535,0.00021762514,0.0000059768645],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013691243,0.000004418422,0.9937421,0.00000442083,0.000026505071,0.000004775611,0.0002342296,0.002041787,0.00015271649,0.0018490701,0.00006253934,0.0018637639],"study_design_scores_gemma":[0.0001695043,0.0000662694,0.9910771,0.00004543114,0.00002875539,0.00002822075,0.0005242429,0.0015150917,0.00011841047,0.0059233257,0.00044940735,0.000054222306],"about_ca_topic_score_codex":0.58622485,"about_ca_topic_score_gemma":0.96206075,"teacher_disagreement_score":0.37583587,"about_ca_system_score_codex":0.000003863978,"about_ca_system_score_gemma":0.0007301771,"threshold_uncertainty_score":0.99872047},"labels":[],"label_agreement":null},{"id":"W2140998181","doi":"10.1139/cjes-2014-0211","title":"Modelling seabed shear stress, sediment mobility, and sediment transport in the Bay of Fundy","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Saint Mary's University; Bedford Institute of Oceanography; Fisheries and Oceans Canada; Geological Survey of Canada","funders":"Government of Canada","keywords":"Bay; Geology; Seabed; Oceanography; Sediment; Sediment transport; Bay mud; Current (fluid); Geomorphology","score_opus":0.03404890499561797,"score_gpt":0.21475443125872426,"score_spread":0.1807055262631063,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140998181","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99301887,0.004543493,0.00017543965,0.00055149995,0.00017672624,0.000082211634,0.00002281001,0.0000014529379,0.0014274733],"genre_scores_gemma":[0.9983649,0.00010188783,0.001334333,0.00013778744,0.000044667646,1.2874145e-7,0.000001508045,0.000001026597,0.0000137451625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987923,0.000059754107,0.0003090938,0.00012816269,0.00043413712,0.0002765418],"domain_scores_gemma":[0.9992295,0.000073656985,0.00012928911,0.00007256813,0.00008400115,0.0004109909],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017790175,0.00008620007,0.00016687841,0.000080667596,0.0001313843,0.000056189834,0.00034653742,0.000031181855,0.00012877549],"category_scores_gemma":[0.00002251408,0.000052432355,0.000037424597,0.000543032,0.00052849425,0.00033944505,0.0000022377953,0.00013007526,0.0000011245861],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006727583,0.00000844999,0.86529213,0.000011699848,0.0000047205394,0.000022517264,0.0015426545,0.13252413,4.230245e-7,0.000037269856,0.000020471542,0.0005288021],"study_design_scores_gemma":[0.0005853077,0.0010789309,0.9212228,0.00017301795,0.000031038973,0.0000955154,0.0137713775,0.05692252,0.000079550926,0.0028623145,0.00296264,0.00021500206],"about_ca_topic_score_codex":0.015644634,"about_ca_topic_score_gemma":0.1094893,"teacher_disagreement_score":0.09384467,"about_ca_system_score_codex":0.0000014351419,"about_ca_system_score_gemma":0.0012415773,"threshold_uncertainty_score":0.9909103},"labels":[],"label_agreement":null},{"id":"W2141277794","doi":"10.1139/e08-030","title":"Determining the post-glacial evolution of a northeast Pacific coastal fjord using a multiproxy geochemical approachThis article is one of a series of papers published in this Special Issue on the theme <i>Polar Climate Stability Network</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; University of British Columbia; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Geology; Holocene; Meltwater; Deglaciation; Greenland ice sheet; Oceanography; Glacial period; Fjord; Younger Dryas; Biogenic silica; Anoxic waters; Sedimentary rock; Ice sheet; Holocene climatic optimum; Marine transgression; Geochemistry; Paleontology; Sediment; Structural basin","score_opus":0.03599307876442754,"score_gpt":0.21681224183902278,"score_spread":0.18081916307459525,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141277794","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945112,0.00016204442,0.0000010814246,0.0010089405,0.0002027003,0.00016876201,0.000075153235,0.0000012670175,0.0038688884],"genre_scores_gemma":[0.99943924,0.000019410907,0.00026543066,0.000054507836,0.0002103753,4.0373052e-7,0.0000026899386,0.0000017717207,0.00000616861],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978827,0.00038870465,0.00056860334,0.00018050375,0.0004467271,0.0005327122],"domain_scores_gemma":[0.99854165,0.0004399908,0.00039546323,0.00016882879,0.00027036716,0.00018371717],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0025813042,0.00011389677,0.00032754068,0.0001907699,0.00053103035,0.000028951083,0.0004938173,0.00009447474,0.0040518017],"category_scores_gemma":[0.0006325277,0.000068628244,0.00010450276,0.0007302669,0.0034562023,0.0003538546,0.00001821279,0.000381619,0.0000032838595],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001745697,0.000025156285,0.9958138,0.000014195115,0.000013426462,0.0000102052245,0.003085501,0.0004990863,0.00012509758,0.0000448974,0.000019929428,0.00017414818],"study_design_scores_gemma":[0.00027308843,0.00048337763,0.9924404,0.00005400258,0.000012159033,0.00011028003,0.002945165,0.0025379967,0.0008086662,0.00015981366,0.00009839704,0.00007666673],"about_ca_topic_score_codex":0.006639863,"about_ca_topic_score_gemma":0.2960828,"teacher_disagreement_score":0.28944296,"about_ca_system_score_codex":0.0000024174171,"about_ca_system_score_gemma":0.0012672666,"threshold_uncertainty_score":0.999975},"labels":[],"label_agreement":null},{"id":"W2141398750","doi":"10.1139/e05-062","title":"An expanded record of Early Cambrian carbon cycling from the Anti-Atlas Margin, Morocco","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":226,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Geochronology; Carbonate; Zircon; Paleontology; Context (archaeology); Carbon cycle; Total organic carbon; Phanerozoic; Geochemistry; Isotopes of carbon; Geologic record; Cenozoic; Structural basin","score_opus":0.021907798259276245,"score_gpt":0.2271010714359063,"score_spread":0.20519327317663005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141398750","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.981357,0.0056026066,0.000007902115,0.0004998911,0.00062206713,0.000054131036,0.000042710155,0.0000033851702,0.0118103195],"genre_scores_gemma":[0.9980478,0.000054029977,0.0013720333,0.00010819153,0.00040353587,9.132618e-8,0.0000011922616,7.9149953e-7,0.000012278287],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99858016,0.00015531079,0.00039162932,0.0001539616,0.00028151652,0.00043743988],"domain_scores_gemma":[0.9986891,0.0002075229,0.00030885547,0.0001480724,0.00007301597,0.0005734424],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00096523593,0.000115737435,0.00023632994,0.00019952991,0.00040864316,0.00011427524,0.00067883375,0.0000747763,0.00022490602],"category_scores_gemma":[0.00008136985,0.00007584028,0.00009426123,0.00034204978,0.00072316785,0.00065633183,7.732031e-7,0.00022815692,0.0000037063028],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008949722,0.0000036513331,0.97133726,8.257118e-7,0.000014542415,0.000016090009,0.0007334684,0.00025735583,0.00010919204,0.00002237677,0.00002579221,0.027470496],"study_design_scores_gemma":[0.00014017646,0.0002898386,0.99711937,0.00003622358,0.00001573199,0.000042866875,0.00066619506,0.0007058205,0.0002878,0.00018397615,0.0004108914,0.000101139965],"about_ca_topic_score_codex":0.12743783,"about_ca_topic_score_gemma":0.81023633,"teacher_disagreement_score":0.6827985,"about_ca_system_score_codex":0.0000010716769,"about_ca_system_score_gemma":0.0008388071,"threshold_uncertainty_score":0.8783726},"labels":[],"label_agreement":null},{"id":"W2141592070","doi":"10.1139/e00-116","title":"On the possibility of anisotropic heat flow in the inner core","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Alexander von Humboldt-Stiftung","keywords":"Anisotropy; Thermal conductivity; Materials science; Condensed matter physics; Inner core; Electrical resistivity and conductivity; Conductivity; Atmospheric temperature range; Thermodynamics; Composite material; Chemistry; Physics; Optics","score_opus":0.028413774839814342,"score_gpt":0.22124807501887558,"score_spread":0.19283430017906125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141592070","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99433345,0.00016535555,0.0000025116099,0.0013746774,0.00037758125,0.000068959846,0.00008785496,7.089538e-7,0.0035889123],"genre_scores_gemma":[0.9992927,0.000013655113,0.00007893489,0.0004815749,0.00009366688,1.4613246e-7,0.0000019472955,6.764606e-7,0.00003670937],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999051,0.00012200023,0.00022909825,0.00009087666,0.00026967234,0.00023737043],"domain_scores_gemma":[0.9993038,0.00029312668,0.00009142509,0.00013026239,0.000052880467,0.00012846077],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012527178,0.00006466672,0.00012970946,0.000098101875,0.00023555577,0.00010308493,0.0005579861,0.000023593928,0.0042247586],"category_scores_gemma":[0.00016120568,0.000029083489,0.000043885582,0.00041549103,0.00039442175,0.00014758222,0.0000025528448,0.00010729842,0.000021209227],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003787892,0.00002157345,0.9683859,0.000009388091,0.0000139206495,0.00016783908,0.002798634,0.016815545,0.00017757008,0.0038297477,0.004003025,0.0037390012],"study_design_scores_gemma":[0.000089882866,0.00034504375,0.98384994,0.000036522324,0.0000043960654,0.00004008755,0.00047851785,0.0007615922,0.00005753962,0.006669378,0.0076102833,0.00005683115],"about_ca_topic_score_codex":0.027788946,"about_ca_topic_score_gemma":0.3746604,"teacher_disagreement_score":0.34687147,"about_ca_system_score_codex":8.405881e-7,"about_ca_system_score_gemma":0.0005082826,"threshold_uncertainty_score":0.9966855},"labels":[],"label_agreement":null},{"id":"W2141618095","doi":"10.1139/e02-076","title":"Regional metamorphism of the Appalachian Humber zone of Gaspé Peninsula: <sup>40</sup>Ar/<sup>39</sup>Ar evidence for crustal thickening during the Taconian orogeny","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"GDG Environnement; Institut National de la Recherche Scientifique","funders":"","keywords":"Geology; Metamorphism; Hornblende; Metamorphic rock; Orogeny; Muscovite; Ophiolite; Geochemistry; Ordovician; Metamorphic facies; Paleontology; Facies; Biotite; Tectonics","score_opus":0.03916878290368606,"score_gpt":0.22441311532889313,"score_spread":0.18524433242520708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141618095","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99257547,0.0033213673,0.000055236575,0.0028321508,0.000116301424,0.00018770796,0.000057001005,0.000003656464,0.00085108215],"genre_scores_gemma":[0.9976598,0.00006657591,0.0014601941,0.0003520876,0.00013285705,0.0000012489551,0.0000023559592,0.0000036362724,0.00032121906],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970768,0.0002928358,0.0007729421,0.00034381583,0.0008035193,0.0007100774],"domain_scores_gemma":[0.9974802,0.0006882836,0.00060994783,0.0002801055,0.00034861563,0.0005928498],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0021477824,0.00023345536,0.00048412938,0.00023374354,0.0010045655,0.00011705047,0.0012443357,0.00010437606,0.003108755],"category_scores_gemma":[0.0012413403,0.00012308317,0.00049768825,0.001169545,0.0019202915,0.000454111,0.000023805449,0.0004091277,0.000012312149],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004524939,0.000014625407,0.9239784,0.000032625256,0.00010106593,0.000024738247,0.0010512958,0.07320076,0.00044645907,0.0005544484,0.00012527706,0.0004250693],"study_design_scores_gemma":[0.00075198145,0.00059476,0.955246,0.00038331407,0.00027740566,0.0005979059,0.004316185,0.01941864,0.0034693056,0.0064471946,0.007988827,0.000508482],"about_ca_topic_score_codex":0.014219819,"about_ca_topic_score_gemma":0.06712604,"teacher_disagreement_score":0.05378212,"about_ca_system_score_codex":0.000005878099,"about_ca_system_score_gemma":0.0011516648,"threshold_uncertainty_score":0.99780256},"labels":[],"label_agreement":null},{"id":"W2141701613","doi":"10.1139/e99-103","title":"Late Laramide dolomite recrystallization of the Husky Rainbow \"A\" hydrocarbon Devonian reservoir, northwestern Alberta, Canada: paleomagnetic and geochemical evidence","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Terrafix Geosynthetics (Canada); University of Windsor","funders":"Natural Sciences and Engineering Research Council of Canada; American Academy of Sleep Medicine","keywords":"Dolomite; Geology; Devonian; Sedimentary rock; Petrography; Diagenesis; Geochemistry; Paleomagnetism; Dolomitization; Carbonate rock; Mineralogy; Paleontology; Facies; Structural basin","score_opus":0.011697448739810047,"score_gpt":0.2058741987352121,"score_spread":0.19417674999540205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141701613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9901238,0.0073074033,0.0000016781067,0.0013306726,0.00014122904,0.00009628727,0.000014994798,6.9802417e-7,0.0009832265],"genre_scores_gemma":[0.9974228,0.000798833,0.0001277131,0.00024506115,0.000080113015,0.0000013358252,0.0000022022427,0.0000055071127,0.0013164126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987864,0.00009787113,0.0003280716,0.00021057503,0.0002488101,0.000328298],"domain_scores_gemma":[0.99918526,0.00006126205,0.00017733226,0.00018528714,0.000114284136,0.00027659003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003349251,0.00013225926,0.00017343657,0.000057991587,0.00025497656,0.000045002846,0.0004102794,0.00007257973,0.00008816293],"category_scores_gemma":[0.00021982721,0.000098056764,0.00005626744,0.00023912465,0.00055950787,0.000020274816,0.000031406995,0.00010663282,5.99159e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037702168,0.000007776695,0.9760736,0.000035051533,0.000029516465,0.000027450258,0.0005171097,0.0014151377,0.019067187,0.00001059958,0.0005580958,0.0022207468],"study_design_scores_gemma":[0.00035441865,0.00070072326,0.96786475,0.00025011253,0.000038299866,0.00019000345,0.00013868479,0.00016130423,0.006164179,0.00010330284,0.023805672,0.0002285523],"about_ca_topic_score_codex":0.4120689,"about_ca_topic_score_gemma":0.9922227,"teacher_disagreement_score":0.5801538,"about_ca_system_score_codex":0.0000046410714,"about_ca_system_score_gemma":0.0016799687,"threshold_uncertainty_score":0.59184617},"labels":[],"label_agreement":null},{"id":"W2141723640","doi":"10.1139/e01-054","title":"Seismic refraction profiles in the Gulf of Saint Lawrence and implications for extent of continuous Grenville lower crust","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Crust; Terrane; Craton; Seismology; Seismic refraction; Continental crust; Lithosphere; Reflection (computer programming); Block (permutation group theory); Geophysics; Tectonics; Geometry","score_opus":0.02518363599935532,"score_gpt":0.2144095343937354,"score_spread":0.18922589839438006,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141723640","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99400115,0.0014081179,0.000055292683,0.0036051176,0.00004724157,0.00007291957,0.00003937733,4.748265e-7,0.0007702943],"genre_scores_gemma":[0.99922323,0.00008254328,0.00051404577,0.00012732869,0.00002222558,4.952336e-7,0.0000012747478,3.51664e-7,0.0000285318],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993382,0.000035864523,0.00026187307,0.00009129041,0.00011224574,0.00016049511],"domain_scores_gemma":[0.999342,0.00018442272,0.00019676094,0.00005941484,0.0000963953,0.00012099759],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00050995767,0.000048432437,0.0001413163,0.000118810894,0.00011595677,0.00002439663,0.00022283325,0.000024797155,0.0006728448],"category_scores_gemma":[0.0001814382,0.000026951599,0.00005404246,0.00032895795,0.00045197815,0.00009193588,0.0000023905063,0.00006882798,0.00000169538],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005424627,0.000014009974,0.9825427,0.0000070446267,0.0000057652505,0.0000021688843,0.00018582151,0.0033721812,0.00018960043,0.00025111463,0.00011193289,0.013312263],"study_design_scores_gemma":[0.00009221775,0.00034646242,0.98722965,0.000022997905,0.000012760443,0.00003440668,0.0004359277,0.0046666632,0.00013308006,0.004855419,0.0021235354,0.00004685451],"about_ca_topic_score_codex":0.0174025,"about_ca_topic_score_gemma":0.12726264,"teacher_disagreement_score":0.10986014,"about_ca_system_score_codex":9.4932204e-7,"about_ca_system_score_gemma":0.00006813834,"threshold_uncertainty_score":0.9891407},"labels":[],"label_agreement":null},{"id":"W2142138633","doi":"10.1139/e06-057","title":"Stress in western Canada from regional moment tensor analysis","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Thrust fault; Crust; Fault (geology); Tension (geology); Pacific Plate; Induced seismicity; Compression (physics); Subduction; Tectonics; Paleontology","score_opus":0.025433769843875777,"score_gpt":0.21828784540912874,"score_spread":0.19285407556525297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142138633","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942983,0.0025508502,0.000035099478,0.00083885266,0.00035690508,0.00003522764,0.00008347222,0.0000015424798,0.001799797],"genre_scores_gemma":[0.9989736,0.000038853857,0.00031128133,0.0004330696,0.00012083637,5.1891245e-8,0.0000060162893,0.0000010384828,0.00011523175],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99845016,0.000040620285,0.0003790726,0.00017160145,0.0004719852,0.0004865739],"domain_scores_gemma":[0.9989027,0.00023020162,0.00017266205,0.00008736,0.000079473175,0.0005276044],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008411127,0.00010225347,0.00025002065,0.0005984784,0.00023137838,0.000076509954,0.00035295225,0.000032032793,0.0012195361],"category_scores_gemma":[0.0000458448,0.00007737576,0.000075268625,0.0011497996,0.00024131351,0.0001891831,0.0000033603424,0.00015300469,0.000007816028],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000041871826,0.0000020756554,0.9917616,8.302226e-7,0.000057920286,0.00029719964,0.00021258621,0.004316163,9.628073e-7,0.000008812216,0.00010041758,0.003237239],"study_design_scores_gemma":[0.00012589963,0.00007108916,0.99085903,0.000022916418,0.00003183485,0.000013707625,0.000962861,0.00018385556,0.000036490255,0.00006563326,0.0075271246,0.00009955602],"about_ca_topic_score_codex":0.9816731,"about_ca_topic_score_gemma":0.9999752,"teacher_disagreement_score":0.018302087,"about_ca_system_score_codex":0.000007774892,"about_ca_system_score_gemma":0.0023576298,"threshold_uncertainty_score":0.9996935},"labels":[],"label_agreement":null},{"id":"W2142200108","doi":"10.1139/cjes-2014-0021","title":"Syndepositional architecture of the northern Athabasca Oil Sands Deposit, northeastern Alberta","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Chevron (Canada)","funders":"","keywords":"Geology; Evaporite; Devonian; Oil sands; Cretaceous; Fault scarp; Halite; Escarpment; Paleontology; Geochemistry; Sedimentary rock; Geomorphology; Fault (geology); Asphalt; Structural basin; Archaeology","score_opus":0.008680425987606363,"score_gpt":0.17740982880726244,"score_spread":0.1687294028196561,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142200108","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9795619,0.00046167584,0.00013235836,0.001224682,0.00029030215,0.000020672092,0.000019527097,0.0000013819055,0.018287504],"genre_scores_gemma":[0.99901724,0.0000064330916,0.0004267524,0.0002587778,0.00008402361,9.8176045e-8,0.0000024001756,0.0000010023488,0.00020325196],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990132,0.00007432694,0.0002717583,0.0000918447,0.00030637853,0.00024249459],"domain_scores_gemma":[0.99911004,0.0001721842,0.00021468975,0.00009122963,0.0001268578,0.00028497353],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041337204,0.00008292753,0.00013289423,0.00012233706,0.00046472062,0.00008615439,0.0005624649,0.000038631173,0.000752732],"category_scores_gemma":[0.00015917073,0.000044074688,0.00009407975,0.00038140424,0.00045392624,0.00020403604,0.000005817889,0.00014222827,0.000019786567],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000034631157,0.0000023890952,0.975002,0.000009916682,0.0000057786533,0.0000018437094,0.00022787813,0.011088968,0.000003861369,0.000104004954,0.000009740719,0.013540154],"study_design_scores_gemma":[0.00009172934,0.00022841508,0.99215883,0.0000707891,0.000010889598,0.00032877215,0.000089658395,0.0013122994,0.00009461771,0.0011263998,0.004408698,0.000078876496],"about_ca_topic_score_codex":0.049251378,"about_ca_topic_score_gemma":0.8997494,"teacher_disagreement_score":0.850498,"about_ca_system_score_codex":7.785176e-7,"about_ca_system_score_gemma":0.00052609365,"threshold_uncertainty_score":0.95707977},"labels":[],"label_agreement":null},{"id":"W2142386865","doi":"10.1139/e2012-056","title":"A new ceratopsid from the Foremost Formation (middle Campanian) of Alberta","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature; Royal Ontario Museum; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Taxon; Paleontology; Geology; Sister group; Genus; Phylogenetic tree; Zoology; Biology; Clade","score_opus":0.03032206481677161,"score_gpt":0.20347157428307683,"score_spread":0.17314950946630522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142386865","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98213655,0.0057022767,0.00015583397,0.0013642015,0.00094110105,0.000044481592,0.000034981476,0.0000011152466,0.0096194595],"genre_scores_gemma":[0.9981465,0.000022621793,0.0010874778,0.00032779927,0.00029618468,4.5013756e-8,0.000007119284,5.521219e-7,0.00011174022],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991766,0.00008380373,0.00023635545,0.000060272356,0.00012270594,0.00032024554],"domain_scores_gemma":[0.9989995,0.00028578562,0.00019847888,0.00007169291,0.000046586443,0.00039799575],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00053662015,0.00006229061,0.000119958175,0.0000848986,0.00032395872,0.000023255516,0.00035778733,0.000053890526,0.0022728695],"category_scores_gemma":[0.00016343006,0.000036673733,0.000049537615,0.00023020567,0.00037611567,0.00068872125,0.0000024643498,0.00010505133,0.00006276456],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006692082,0.000001186317,0.99416924,8.369838e-7,0.000007145137,0.0000016361878,0.0012593042,0.00013337325,0.000008515872,0.00032176968,0.0007116692,0.0033786376],"study_design_scores_gemma":[0.00009117608,0.00010939951,0.9791689,0.000014947654,0.000008685384,0.00015063505,0.0006814135,0.00026509183,0.000052257557,0.0010155124,0.018391717,0.000050274983],"about_ca_topic_score_codex":0.12073522,"about_ca_topic_score_gemma":0.89441544,"teacher_disagreement_score":0.7736802,"about_ca_system_score_codex":0.0000012955942,"about_ca_system_score_gemma":0.00084990053,"threshold_uncertainty_score":0.99863917},"labels":[],"label_agreement":null},{"id":"W2142748826","doi":"10.1139/e07-003","title":"Spindle-shaped Ediacara fossils from the Mistaken Point assemblage, Avalon Zone, Newfoundland","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":112,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Terrane; Assemblage (archaeology); Geology; Paleontology; Photic zone; Tectonics; Biology","score_opus":0.02867244163784422,"score_gpt":0.23868432083286412,"score_spread":0.2100118791950199,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142748826","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92864,0.012171766,0.000503108,0.0013585654,0.0014488614,0.00009713973,0.000057145884,0.000006386254,0.055717044],"genre_scores_gemma":[0.99759114,0.000041032676,0.0013178764,0.0004077085,0.0005779047,9.583512e-8,0.0000026470243,9.802822e-7,0.000060619364],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980103,0.00012176264,0.000480568,0.00022967494,0.00045432276,0.0007033899],"domain_scores_gemma":[0.9978757,0.0006499961,0.00032703517,0.00016613807,0.00010928626,0.0008718521],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0025882362,0.0001680893,0.0002550723,0.0002508921,0.0010061009,0.0003403145,0.00085856917,0.00011685595,0.00087354303],"category_scores_gemma":[0.00022818705,0.00010512219,0.0001593078,0.0005193701,0.0010447507,0.0005812274,0.0000012052805,0.0003788416,0.000032229986],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020988391,0.0000033855697,0.9699007,0.0000013361813,0.000025459241,0.00022201461,0.0005747601,0.000040409715,0.000050499068,0.0001035311,0.0003117517,0.028745156],"study_design_scores_gemma":[0.00023570165,0.00026601242,0.991828,0.000036951955,0.00002213237,0.00015905329,0.0008447456,0.00017037483,0.00004295639,0.0009931002,0.005253729,0.00014723185],"about_ca_topic_score_codex":0.102321714,"about_ca_topic_score_gemma":0.9496781,"teacher_disagreement_score":0.84735644,"about_ca_system_score_codex":0.0000025969136,"about_ca_system_score_gemma":0.0014608216,"threshold_uncertainty_score":0.95646834},"labels":[],"label_agreement":null},{"id":"W2143095943","doi":"10.1139/cjes-2014-0166","title":"Middle Cenomanian (Late Cretaceous) molluscs of the Shaftesbury Formation, Birch Mountains, northeastern Alberta, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Stantec (Canada)","funders":"","keywords":"Cenomanian; Fauna; Geology; Cretaceous; Paleontology; Oil shale; Invertebrate; Ecology","score_opus":0.027124059375183397,"score_gpt":0.19737871030597534,"score_spread":0.17025465093079195,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143095943","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9590919,0.004100517,0.000009974684,0.0015547663,0.00069440226,0.000075871154,0.0000768843,0.0000013990245,0.0343943],"genre_scores_gemma":[0.9993901,0.000009221257,0.00014901452,0.00019805065,0.00005846403,1.0161902e-7,0.0000012999574,7.2022596e-7,0.00019297429],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984617,0.00011590413,0.00045377322,0.00012045159,0.0004493777,0.00039877425],"domain_scores_gemma":[0.99847776,0.000107039414,0.00038254014,0.00014615896,0.00019525751,0.0006912748],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00080930936,0.00011338094,0.00019628688,0.00017729317,0.00041537065,0.00007289484,0.00074579846,0.00005264593,0.00008518561],"category_scores_gemma":[0.00018264313,0.00007311534,0.00007930358,0.00048302946,0.00056462974,0.0004946281,0.0000019709616,0.00017127655,0.0000039578285],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001286956,0.0000021707187,0.99187815,0.000006129632,0.000013588717,0.000032568627,0.0010531124,0.0033953742,0.0000021865828,0.00004540875,0.0003155263,0.0032429264],"study_design_scores_gemma":[0.00022027662,0.00017395135,0.9893465,0.000044275122,0.000013075741,0.00021152447,0.0010142538,0.0020060362,0.00007147465,0.00033458066,0.006459447,0.00010460964],"about_ca_topic_score_codex":0.9123164,"about_ca_topic_score_gemma":0.99979705,"teacher_disagreement_score":0.08748069,"about_ca_system_score_codex":0.000004716929,"about_ca_system_score_gemma":0.006940035,"threshold_uncertainty_score":0.9986897},"labels":[],"label_agreement":null},{"id":"W2143306226","doi":"10.1139/e09-015","title":"Pilot study of fossil evidence of onshore-directed storm events in estuarine sediments: Chezzetcook Inlet, Nova ScotiaNatural Resources Canada Climate Change Impacts and Adaptation Program SST 20090027.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Dalhousie University","funders":"","keywords":"Inlet; Sedimentary depositional environment; Storm; Geology; Estuary; Oceanography; Foraminifera; Coring; Benthic zone; Sediment; Barrier island; Hydrology (agriculture); Paleontology; Structural basin; Shore","score_opus":0.0748789269557606,"score_gpt":0.291518101081956,"score_spread":0.21663917412619543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143306226","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99101764,0.007653739,1.5039912e-7,0.0005547916,0.00024071695,0.00038157386,0.0000103918255,0.0000034316465,0.00013754742],"genre_scores_gemma":[0.999447,0.00016624268,0.00028172374,0.00006865963,0.0000250268,6.7499053e-7,0.0000019721597,0.0000014208605,0.0000072928706],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979328,0.00025444647,0.00054989284,0.00020648494,0.0004881154,0.00056828803],"domain_scores_gemma":[0.99860084,0.0002363254,0.00040833588,0.00010693762,0.00020293682,0.00044461992],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015939188,0.0001388225,0.00034852582,0.00057905656,0.00021827537,0.000026228901,0.00040443087,0.000043808348,0.00011615425],"category_scores_gemma":[0.00039192842,0.00010853453,0.000023342882,0.0009220788,0.00044203302,0.00052770873,0.000008681648,0.0003049368,0.0000013071311],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012339969,0.000051557032,0.99344623,0.000023482196,0.000012841135,0.00008475419,0.0017030733,0.0002936634,0.0000062988233,0.0000012106887,0.000011827569,0.0042416616],"study_design_scores_gemma":[0.00048820002,0.0067756167,0.98908556,0.00032496965,0.000014473869,0.0000929484,0.0019869732,0.0010728383,0.000017768376,0.00002417993,0.000018468518,0.000098036595],"about_ca_topic_score_codex":0.69331706,"about_ca_topic_score_gemma":0.9993994,"teacher_disagreement_score":0.30608237,"about_ca_system_score_codex":0.000004137817,"about_ca_system_score_gemma":0.0015337084,"threshold_uncertainty_score":0.44259095},"labels":[],"label_agreement":null},{"id":"W2143745478","doi":"10.1139/e02-901","title":"A comparative <sup>40</sup>Ar/<sup>39</sup>Ar conventional and laserprobe study of muscovite from Port Mouton Pluton, southwest Nova Scotia: Erratum","year":2002,"lang":"en","type":"erratum","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Pluton; Muscovite; Geology; Geochemistry; Monazite; Nova scotia; Zircon; Closure temperature; Orogeny; Terrane; Metamorphic rock; Mineralogy; Paleontology; Tectonics; Quartz","score_opus":0.029454632515339706,"score_gpt":0.2230679541914235,"score_spread":0.1936133216760838,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143745478","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9809899,0.00552125,0.0000061476203,0.0006033774,0.0016077033,0.00031435452,0.0011871347,0.000010258243,0.009759904],"genre_scores_gemma":[0.992969,0.00008019699,0.00033381474,0.00028598862,0.0007359029,8.111679e-7,0.00033198536,0.000007249128,0.0052550766],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99515015,0.00030543635,0.001368156,0.0008728923,0.0013552784,0.00094811467],"domain_scores_gemma":[0.9961401,0.00030132913,0.00114222,0.00030681663,0.0005482512,0.0015612552],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010117246,0.0006038008,0.0015625166,0.0008922666,0.00058220275,0.00038565922,0.0012110982,0.00039589996,0.016833156],"category_scores_gemma":[0.0002301912,0.00043891143,0.0004012781,0.0013659715,0.0019375702,0.000566194,0.00004748187,0.001376172,0.00015593445],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006126229,0.00016633223,0.93345654,0.0000468112,0.00047301824,0.00048575463,0.0032893636,0.025215203,0.0000061371506,0.000016921778,0.03643991,0.00034274912],"study_design_scores_gemma":[0.0014016648,0.0028459586,0.9311298,0.00054893445,0.00066439353,0.0002020699,0.011394129,0.025916258,0.000014854965,0.0024346455,0.022346523,0.0011007602],"about_ca_topic_score_codex":0.23852801,"about_ca_topic_score_gemma":0.75438255,"teacher_disagreement_score":0.51585454,"about_ca_system_score_codex":0.000009574062,"about_ca_system_score_gemma":0.0018526319,"threshold_uncertainty_score":0.9998063},"labels":[],"label_agreement":null},{"id":"W2144097136","doi":"10.1139/e08-039","title":"High-resolution paleomagnetic secular variation and relative paleointensity records from the western Canadian Arctic: implication for Holocene stratigraphy and geomagnetic field behaviourThis article is one of a series of papers published in this Special Issue on the theme <i>Polar Climate Stability Network</i>.GEOTOP Contribution 2008-0024.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Rimouski; Université du Québec à Montréal","funders":"University of Florida","keywords":"Geology; Paleomagnetism; Secular variation; Earth's magnetic field; Holocene; Declination; Geomagnetic secular variation; Paleontology; Chronostratigraphy; Stratigraphy; Arctic; Magnetic declination; Geophysics; Oceanography; Structural basin; Tectonics","score_opus":0.017862458022409267,"score_gpt":0.20497069483771468,"score_spread":0.18710823681530542,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2144097136","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98728234,0.00087797525,0.0000069166085,0.010913841,0.00016168572,0.00034408763,0.00019694775,0.0000012485582,0.00021496808],"genre_scores_gemma":[0.99901325,0.00028159094,0.00023488073,0.00032488612,0.00012231154,0.0000015693157,0.000014490193,0.0000012285983,0.0000057887178],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99856085,0.00031148348,0.00037548016,0.00019019913,0.0001884932,0.0003734994],"domain_scores_gemma":[0.99831754,0.0007809685,0.00025779635,0.00013672127,0.00029659746,0.00021037653],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016895535,0.00009594306,0.00022606706,0.00012987325,0.00056911696,0.000047654812,0.00018903971,0.00010855784,0.0017138527],"category_scores_gemma":[0.00064032257,0.00006397656,0.000044014414,0.00036005367,0.0010504408,0.00031001683,0.000005715746,0.0002497413,0.0000012048146],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009060178,0.0000067829365,0.99778306,0.000005842668,0.000013612352,0.0000050814524,0.001510354,0.00008584532,0.000022845807,0.00020313864,0.000103122016,0.00016970953],"study_design_scores_gemma":[0.00028070543,0.0009119241,0.99526244,0.00004087186,0.000027455671,0.00004224402,0.0002994135,0.0003519556,0.00026433446,0.0023565183,0.00009774967,0.00006438534],"about_ca_topic_score_codex":0.32562295,"about_ca_topic_score_gemma":0.94789785,"teacher_disagreement_score":0.62227494,"about_ca_system_score_codex":0.0000025466986,"about_ca_system_score_gemma":0.0004837476,"threshold_uncertainty_score":0.99919873},"labels":[],"label_agreement":null},{"id":"W2144638561","doi":"10.1139/e08-013","title":"Mountain permafrost probability mapping using the BTS method in two climatically dissimilar locations, northwest Canada","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"International Permafrost Association","keywords":"Permafrost; Geology; Summit; Physical geography; Elevation (ballistics); Mountain range (options); Range (aeronautics); Snow; Climatology; Geomorphology; Geography; Oceanography","score_opus":0.08475256406202049,"score_gpt":0.2865677729630479,"score_spread":0.20181520890102744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2144638561","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949553,0.00074032444,0.0001352663,0.0021367562,0.00037135268,0.00014636417,0.0007879762,0.0000019108213,0.00072472583],"genre_scores_gemma":[0.99613744,0.000043662247,0.0027813963,0.0008316051,0.00013518777,3.5855334e-7,0.000052084004,0.0000024974854,0.000015787293],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998127,0.0002165592,0.0004942495,0.00018909592,0.00042599798,0.0005471154],"domain_scores_gemma":[0.99867827,0.0003282275,0.0002010592,0.00015173006,0.00013244554,0.0005082517],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017108348,0.00013387571,0.00022287444,0.00021864264,0.0010269517,0.00013174592,0.00053556665,0.00002894801,0.0011455192],"category_scores_gemma":[0.00019887903,0.00008896722,0.0000547638,0.0007915895,0.00055390625,0.00041760708,0.0000075223925,0.00025596577,0.0000053309172],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000027864571,0.000003180327,0.98220766,0.0000074539457,0.0000035013543,0.00013286,0.0010654883,0.016060866,0.000018146653,0.00002809272,0.00007292716,0.00039701356],"study_design_scores_gemma":[0.00014170844,0.00003722187,0.974353,0.00005626691,0.0000065401846,0.0005925692,0.0020228745,0.019700529,0.000012281169,0.00025361642,0.0026906081,0.00013277779],"about_ca_topic_score_codex":0.95944667,"about_ca_topic_score_gemma":0.9998686,"teacher_disagreement_score":0.040421885,"about_ca_system_score_codex":0.000022538006,"about_ca_system_score_gemma":0.006597177,"threshold_uncertainty_score":0.99976754},"labels":[],"label_agreement":null},{"id":"W2144663013","doi":"10.1139/e05-025","title":"Tectonic framework of a Paleoproterozoic arc-continent to continent-continent collisional zone, Trans-Hudson Orogen, from geological and seismic reflection studies","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Health Canada; University of Saskatchewan; Statistics Canada; PotashCorp (Canada); Geological Survey of Canada","funders":"","keywords":"Geology; Craton; Foreland basin; Tectonics; Batholith; Seismology; Archean; Crust; Shear zone; Passive margin; Paleontology; Geologic map; Rift","score_opus":0.02525004267403231,"score_gpt":0.2441314995391732,"score_spread":0.2188814568651409,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2144663013","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9812757,0.006522151,0.0003415464,0.011260905,0.00021128377,0.00013807151,0.000050515904,0.000005852992,0.00019397582],"genre_scores_gemma":[0.9930545,0.00027168752,0.00577456,0.0006133141,0.0002171291,0.0000012237613,0.0000047586923,0.0000016199604,0.00006118502],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980121,0.000120360484,0.0006133597,0.0003370386,0.00043758264,0.0004795434],"domain_scores_gemma":[0.9983018,0.00036360015,0.0002715433,0.00010159902,0.0002175864,0.00074387033],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008464735,0.00019181211,0.0005306387,0.00028778714,0.0002967394,0.0000795142,0.00036209685,0.000106531596,0.0025573508],"category_scores_gemma":[0.0004999713,0.00012022261,0.00015989928,0.00066815113,0.00064858346,0.00019511113,0.0000134032725,0.00028607468,0.000021752492],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008771661,0.000016745193,0.9777699,0.000008608481,0.000082126935,0.000027936932,0.00045948473,0.008988897,0.00068550615,0.000039598024,0.00008216062,0.01175133],"study_design_scores_gemma":[0.0004588484,0.0015827151,0.9748631,0.00019748532,0.00010503196,0.0000804851,0.0006038875,0.003380881,0.0031529376,0.0046187476,0.0106724985,0.0002833427],"about_ca_topic_score_codex":0.014464188,"about_ca_topic_score_gemma":0.31326413,"teacher_disagreement_score":0.29879996,"about_ca_system_score_codex":0.000004090819,"about_ca_system_score_gemma":0.00021418797,"threshold_uncertainty_score":0.99835443},"labels":[],"label_agreement":null},{"id":"W2144761084","doi":"10.1139/cjes-2014-0220","title":"First record of the tritylodontid cynodont <i>Oligokyphus</i> and cynodont postcranial bones from the McCoy Brook Formation of Nova Scotia, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Postcrania; Geology; Paleontology; Nova scotia; Taxon","score_opus":0.022454268162338028,"score_gpt":0.18922056325820585,"score_spread":0.16676629509586782,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2144761084","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9869476,0.0042192284,0.000020415993,0.0055419207,0.0015020191,0.00008887537,0.0002434638,0.0000010549991,0.0014354354],"genre_scores_gemma":[0.9990694,0.000042942804,0.00030631866,0.00043162704,0.00011889741,6.060934e-8,0.0000041126764,9.4455686e-7,0.000025677627],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987437,0.00016833631,0.00042003955,0.000112463604,0.00028495846,0.00027046463],"domain_scores_gemma":[0.99869674,0.00029615362,0.0004160253,0.000120434874,0.00017655073,0.00029406813],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000923683,0.000095063246,0.00022785722,0.00008013164,0.00031488496,0.000025629039,0.00055515755,0.000065411434,0.00014367874],"category_scores_gemma":[0.0003208355,0.000052439376,0.000056276538,0.00026229335,0.0010628974,0.00033352067,0.000009662081,0.00016026538,0.0000027297535],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003819598,0.000002399117,0.9957061,0.0000039573374,0.000010862491,0.000007702818,0.0003718294,0.0005472735,0.000016345075,0.00004094573,0.0021444634,0.0011099374],"study_design_scores_gemma":[0.00027175498,0.00022679454,0.9873766,0.000049392445,0.000019347726,0.00017130008,0.00066670444,0.0007093388,0.000089885434,0.0005022399,0.0098469,0.00006974775],"about_ca_topic_score_codex":0.9679749,"about_ca_topic_score_gemma":0.9998563,"teacher_disagreement_score":0.031881362,"about_ca_system_score_codex":0.0000057720736,"about_ca_system_score_gemma":0.002950614,"threshold_uncertainty_score":0.52342623},"labels":[],"label_agreement":null},{"id":"W2145145283","doi":"10.1139/e08-021","title":"A new specimen of <i>Suzhousaurus megatherioides</i> (Dinosauria: Therizinosauroidea) from the Early Cretaceous of northwestern China","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Fisheries Research and Development Corporation","keywords":"Geology; Cretaceous; Autapomorphy; Paleontology; Postcrania; Anatomy; Taxon; Biology; Phylogenetic tree","score_opus":0.018884906469852438,"score_gpt":0.1945534904235942,"score_spread":0.17566858395374177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145145283","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9846514,0.00996562,0.000044928718,0.0008217771,0.0005999916,0.00007418842,0.00013517556,0.0000030546196,0.0037039062],"genre_scores_gemma":[0.9980487,0.000212263,0.0011955659,0.00019085695,0.00021303512,8.0029906e-8,0.000004124676,0.000001986865,0.00013337519],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99850595,0.00016495533,0.0004883535,0.00017346669,0.00029014781,0.00037712426],"domain_scores_gemma":[0.99856466,0.00030178062,0.0004828385,0.00017376669,0.00008693019,0.0003899945],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005006988,0.00013550775,0.0003373357,0.00014053995,0.00037853557,0.000019174184,0.00085424,0.000093783645,0.0014761974],"category_scores_gemma":[0.0000862981,0.000084537554,0.00013439302,0.0003919324,0.0015205429,0.00029037613,0.0000070231945,0.00022039813,0.000024305042],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000036375357,0.000003932356,0.9950774,0.000001203587,0.000037634883,0.00009117935,0.0015327999,0.00042383396,0.00024188733,0.000033782977,0.0003261058,0.0021938635],"study_design_scores_gemma":[0.00023009254,0.0005701695,0.9926793,0.000025345067,0.000019722638,0.0003829375,0.00021231371,0.000045843495,0.0002531778,0.0007874738,0.004700333,0.00009330904],"about_ca_topic_score_codex":0.18367282,"about_ca_topic_score_gemma":0.6998361,"teacher_disagreement_score":0.5161633,"about_ca_system_score_codex":0.0000016197506,"about_ca_system_score_gemma":0.0020580592,"threshold_uncertainty_score":0.9994366},"labels":[],"label_agreement":null},{"id":"W2145521854","doi":"10.1139/e2012-004","title":"Discussion of “Geochemical signature of Ordovician Mn-rich sedimentary rocks on the Avalonian shelf”<sup>1</sup>Appears in Canadian Journal of Earth Sciences, 2011, <b>48</b>(4): 703–718 [doi: 10.1139/e10-092].","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Ordovician; Geology; Sedimentary rock; Geochemistry; Supergroup; Turbidite; Pyrite","score_opus":0.011448127256250133,"score_gpt":0.2037438878453448,"score_spread":0.19229576058909467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145521854","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98851705,0.0024855128,0.0000022303345,0.0034409391,0.0003917082,0.00012121215,0.00023547316,0.0000018255231,0.004804069],"genre_scores_gemma":[0.9985419,0.000041254716,0.00029205967,0.00034906255,0.0002688365,3.242837e-7,0.000018085546,0.000004907413,0.00048358183],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9961176,0.00025319468,0.0010529957,0.0002820191,0.0011000589,0.0011941642],"domain_scores_gemma":[0.9967468,0.00021428501,0.0008135267,0.00023030596,0.0002481221,0.0017469641],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0037362487,0.00028684677,0.00054861093,0.0010006616,0.0007530526,0.00013708929,0.00143358,0.0001680158,0.011144161],"category_scores_gemma":[0.0003124877,0.00016595333,0.0002645814,0.0016266307,0.0015734868,0.0008234915,0.000020588359,0.00069621205,0.000044628923],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003359408,0.00003939335,0.9828376,0.000023307815,0.000050640254,0.000053647338,0.0015126327,0.011139378,0.0004656505,0.00003139663,0.0023441575,0.0014686136],"study_design_scores_gemma":[0.0015333331,0.002761666,0.8844825,0.0013387544,0.00031748,0.00075902767,0.023273056,0.006059083,0.026747977,0.0012195342,0.050314765,0.0011928126],"about_ca_topic_score_codex":0.18320894,"about_ca_topic_score_gemma":0.69834757,"teacher_disagreement_score":0.5151386,"about_ca_system_score_codex":0.000018068798,"about_ca_system_score_gemma":0.0041018254,"threshold_uncertainty_score":0.9897598},"labels":[],"label_agreement":null},{"id":"W2145600823","doi":"10.1139/e03-086","title":"Early Tertiary Anaconda Metamorphic Core Complex, southwestern Montana","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Geological Survey; Montana State University","keywords":"Mylonite; Geology; Detachment fault; Metamorphic core complex; Breccia; Metamorphic rock; Geochemistry; Sedimentary rock; Fault (geology); Conglomerate; Country rock; Seismology; Shear zone; Petrology; Tectonics","score_opus":0.03784196111443932,"score_gpt":0.20646610824961872,"score_spread":0.1686241471351794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145600823","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99422055,0.0009679826,0.000041832875,0.0017396966,0.0002004703,0.000041652318,0.000040627147,0.0000059956064,0.0027411587],"genre_scores_gemma":[0.99757344,0.000011822974,0.0013130013,0.00092386414,0.00011360396,9.501027e-8,0.0000066440066,0.0000013418096,0.00005616417],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99850667,0.000036703594,0.00037290584,0.0002066438,0.00036805612,0.0005090241],"domain_scores_gemma":[0.9985316,0.00006023597,0.00019430617,0.00010415416,0.000113007125,0.0009966947],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048882986,0.00013973366,0.00026994117,0.0002947876,0.00038898134,0.00016952948,0.0006133169,0.00005418391,0.007389071],"category_scores_gemma":[0.00009154795,0.00009110095,0.00017586564,0.00066286325,0.0007256154,0.00037827657,0.000006551794,0.00021333754,0.00019762173],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000037812545,0.0000041910394,0.9935479,0.0000020588316,0.000021944345,0.00021340183,0.0001511231,0.004549326,0.00012593674,0.00012101435,0.000026054873,0.0012332277],"study_design_scores_gemma":[0.0001970792,0.00026155644,0.98102576,0.000019078736,0.00003164151,0.00014236696,0.00019377313,0.00029827017,0.000073517,0.016776986,0.00084071496,0.00013927359],"about_ca_topic_score_codex":0.12818696,"about_ca_topic_score_gemma":0.71116775,"teacher_disagreement_score":0.5829808,"about_ca_system_score_codex":0.0000020820767,"about_ca_system_score_gemma":0.0006164276,"threshold_uncertainty_score":0.9935183},"labels":[],"label_agreement":null},{"id":"W2145768529","doi":"10.1139/cjes-2014-0218","title":"Early Cretaceous (?early late Albian) echinoderms from northeastern British Columbia, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Echinoderm; Cretaceous; Paleontology; Crinoid; Boreal; Oceanography; Facies; Structural basin","score_opus":0.017935682569604185,"score_gpt":0.1854090456596807,"score_spread":0.16747336309007652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145768529","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9653914,0.007934651,0.000008933683,0.00028402204,0.001365586,0.00006607512,0.0002302299,0.0000057004945,0.024713408],"genre_scores_gemma":[0.998732,0.000014427988,0.00042423763,0.00022748928,0.0001718399,1.2253615e-7,0.0000031970915,0.0000013569229,0.00042535932],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980642,0.0001222312,0.0003984743,0.00024356227,0.00054710946,0.0006244274],"domain_scores_gemma":[0.99758154,0.000102847815,0.0002541865,0.00012673454,0.0001677669,0.0017668956],"candidate_categories":["scholarly_communication"],"consensus_categories":[],"category_scores_codex":[0.00058711146,0.00012122714,0.00028794762,0.0000959228,0.00092574477,0.0016081571,0.00070621213,0.000090366615,0.0005807434],"category_scores_gemma":[0.00011196261,0.00014053905,0.00008576392,0.0003464871,0.00061614136,0.00067825144,0.0000015120642,0.0003026896,0.000016831233],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000051552333,0.0000018530038,0.9738997,0.0000010164666,0.000021540836,0.000976725,0.0002940739,0.00018161275,8.378553e-7,9.215896e-7,0.00060414,0.024012383],"study_design_scores_gemma":[0.0002780579,0.0003112599,0.9942725,0.00004220584,0.000015584796,0.00029280467,0.00025743523,0.0002462316,0.0000026157707,0.00096885883,0.0031282026,0.00018427873],"about_ca_topic_score_codex":0.99926883,"about_ca_topic_score_gemma":0.9999964,"teacher_disagreement_score":0.033340577,"about_ca_system_score_codex":0.0000039059023,"about_ca_system_score_gemma":0.0073102517,"threshold_uncertainty_score":0.9994283},"labels":[],"label_agreement":null},{"id":"W2145847068","doi":"10.1139/e01-026","title":"Crustal structure of the Grenville Province in southeastern Labrador from refraction seismic data: evidence for a high-velocity lower crustal wedge","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Terrane; Crust; Underplating; Seismology; Seismic refraction; Rift; Continental crust; Geomorphology; Tectonics; Paleontology; Subduction","score_opus":0.037856850610870414,"score_gpt":0.23208091663694988,"score_spread":0.19422406602607947,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145847068","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996264,0.00069896743,0.00008126229,0.001857438,0.00038254904,0.00010763455,0.0005050213,0.0000014338175,0.00010168465],"genre_scores_gemma":[0.9988763,0.000018264911,0.0006475495,0.00020641561,0.00014548392,1.1127791e-7,0.000012573944,0.0000011071317,0.00009221722],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99868643,0.00007849866,0.00035555765,0.00024977897,0.00030937,0.00032033934],"domain_scores_gemma":[0.9989244,0.00024121211,0.00030187776,0.00019298689,0.000099951576,0.00023961792],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00044508936,0.00010597693,0.00021999248,0.000121160054,0.00022054694,0.00007822304,0.0009271392,0.00006500786,0.0017574194],"category_scores_gemma":[0.0005237264,0.000060037124,0.00007733745,0.00054438773,0.00049503613,0.0004919831,0.000022927507,0.00021531628,0.0000061620517],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000064842716,0.000007878578,0.987539,0.0000066824905,0.000012818045,0.000025431302,0.000101201025,0.004954551,0.00033500014,0.000016875698,0.000058681406,0.0068770405],"study_design_scores_gemma":[0.00021440008,0.00016558744,0.9799391,0.00009562833,0.000028120117,0.000030858046,0.00038153643,0.013523179,0.00029564102,0.0036569356,0.0015572127,0.00011177821],"about_ca_topic_score_codex":0.20937972,"about_ca_topic_score_gemma":0.896865,"teacher_disagreement_score":0.6874853,"about_ca_system_score_codex":0.000002923061,"about_ca_system_score_gemma":0.0010056123,"threshold_uncertainty_score":0.9991551},"labels":[],"label_agreement":null},{"id":"W2145886102","doi":"10.1139/e04-098","title":"MazatzalLabradorian-age (1.71.6 Ga) ductile deformation of the South Range Sudbury impact structure at the Thayer Lindsley mine, Ontario","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University; Ministry of Energy, Northern Development and Mines; University of Toronto; Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Shear zone; Orogeny; Titanite; Lineation; Metamorphic rock; Shear (geology); Geochemistry; Fold (higher-order function); Seismology; Geomorphology; Tectonics; Paleontology","score_opus":0.012780351447592932,"score_gpt":0.18689611069417844,"score_spread":0.1741157592465855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145886102","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958807,0.0005826284,0.000002957333,0.0015165644,0.00037824965,0.00007507004,0.00008716295,0.0000017494559,0.0014748874],"genre_scores_gemma":[0.999125,0.0000053046897,0.00015482506,0.00027546598,0.0001195783,8.571657e-8,0.000008322668,0.0000011092034,0.00031031604],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986328,0.000047848458,0.00034080702,0.00013895094,0.00045810983,0.00038150014],"domain_scores_gemma":[0.9989705,0.000052034815,0.0003273891,0.00015959599,0.000112430156,0.00037802962],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004923647,0.00013161787,0.00021366919,0.000120477926,0.0005287922,0.000107224885,0.00069633895,0.00006841463,0.012900917],"category_scores_gemma":[0.00010698608,0.00005443991,0.00023617175,0.0006666972,0.0007345424,0.0002794604,0.000013961003,0.0002732058,0.000022921045],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000112418475,0.000002479326,0.96764463,0.0000026103803,0.000020311501,0.000012040184,0.001510916,0.030285597,0.0000796308,0.000018233253,0.000092010305,0.0003203104],"study_design_scores_gemma":[0.00018004107,0.00014537232,0.9932334,0.000020277703,0.000034865585,0.000099865334,0.00043962736,0.00007786212,0.0006367127,0.003920691,0.0011204779,0.00009085056],"about_ca_topic_score_codex":0.39377508,"about_ca_topic_score_gemma":0.98619324,"teacher_disagreement_score":0.59241813,"about_ca_system_score_codex":0.000013300596,"about_ca_system_score_gemma":0.0011465852,"threshold_uncertainty_score":0.9880014},"labels":[],"label_agreement":null},{"id":"W2145893092","doi":"10.1139/e11-045","title":"Paleomagnetic study of the late Neoproterozoic Bull Arm and Crown Hill formations (Musgravetown Group) of eastern Newfoundland: implications for Avalonia and West Gondwana paleogeography<sup>1</sup>This article is one of a series of papers published in <i>CJES Special Issue: In honour of Ward Neale</i> on the theme of Appalachian and Grenvillian geology.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University; Geological Survey of Canada; Government of Newfoundland and Labrador; Memorial University of Newfoundland; Western University","funders":"Natural Sciences and Engineering Research Council of Canada; European Commission","keywords":"Geology; Gondwana; Paleomagnetism; Paleontology; Subaerial; Remanence; Supercontinent; Fold (higher-order function); Craton; Tectonics; Magnetization","score_opus":0.01659001696532306,"score_gpt":0.2047148875939899,"score_spread":0.18812487062866684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145893092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99529237,0.0016101287,0.0000011045558,0.0014341492,0.00005400218,0.0003946277,0.00014035507,6.034605e-7,0.0010726675],"genre_scores_gemma":[0.99967873,0.00009175891,0.00016432455,0.000028189676,0.00002727128,0.0000021186922,8.6726806e-7,9.710408e-7,0.000005782586],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985746,0.00020169061,0.00067105796,0.0001181312,0.0001721996,0.00026228058],"domain_scores_gemma":[0.9987079,0.00027365738,0.00061491143,0.00015099013,0.00009265239,0.00015990148],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012907694,0.00011140443,0.00037413972,0.00036064693,0.00019185392,0.000024015955,0.0003012598,0.000060525635,0.00017015834],"category_scores_gemma":[0.0001281668,0.000070404014,0.00006929769,0.0005251116,0.0017267106,0.0003466466,0.0000057563593,0.00015130993,6.635153e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006495984,0.000063595595,0.9834151,0.000046996596,0.00002968989,2.9245567e-7,0.011035378,0.00006977879,0.00013932891,0.00013001912,0.0000056329072,0.00499923],"study_design_scores_gemma":[0.0005703668,0.0013977491,0.9913499,0.0000812845,0.000032258704,0.000017167995,0.0055470928,0.00014617392,0.00008722351,0.0006716532,0.000035966805,0.00006319665],"about_ca_topic_score_codex":0.01859136,"about_ca_topic_score_gemma":0.5636726,"teacher_disagreement_score":0.54508126,"about_ca_system_score_codex":8.4255043e-7,"about_ca_system_score_gemma":0.00013721606,"threshold_uncertainty_score":0.98794395},"labels":[],"label_agreement":null},{"id":"W2146462471","doi":"10.1139/e09-021","title":"Structural history and granite emplacement in the Rottenstone Domain during closure of the Trans-Hudson Orogen, Davin Lake, northern Saskatchewan","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University","keywords":"Geology; Transpression; Stockwork; Batholith; Geochemistry; Shear zone; Pluton; Pegmatite; Archean; Leucogranite; Gneiss; Magma; Metallogeny; Petrology; Geomorphology; Seismology; Metamorphic rock; Tectonics; Volcano","score_opus":0.01139769065423741,"score_gpt":0.17430035210157366,"score_spread":0.16290266144733626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146462471","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99500346,0.0016121385,9.054389e-7,0.0027820328,0.00008790727,0.0000636775,0.000016907614,9.811723e-7,0.00043199243],"genre_scores_gemma":[0.99942636,0.000011750807,0.00012214306,0.00037018576,0.000038067323,8.156628e-8,0.0000013361034,5.3541925e-7,0.000029537716],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99889046,0.000119345896,0.00027837872,0.00012427357,0.00031430964,0.00027320586],"domain_scores_gemma":[0.99947554,0.000048684553,0.00014915381,0.00008583634,0.00004640809,0.00019437706],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006383324,0.00009212948,0.0001706682,0.00010756621,0.00023551853,0.000031899013,0.00044655168,0.000034747693,0.00084841694],"category_scores_gemma":[0.000033250533,0.00004382178,0.00009235971,0.00038560815,0.0005529646,0.00012165177,0.0000027623403,0.00019187536,0.000001112016],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008073467,0.0000029261926,0.9957012,0.0000030202384,0.000005294611,0.000020039855,0.0019809755,0.0011281247,0.000198741,0.000011829066,0.0000113186115,0.00092845166],"study_design_scores_gemma":[0.00016606138,0.00015889299,0.995221,0.000019955638,0.000013499057,0.0000859892,0.0018444167,0.00005631064,0.000078159304,0.001677795,0.00061155274,0.00006633048],"about_ca_topic_score_codex":0.016790543,"about_ca_topic_score_gemma":0.9444488,"teacher_disagreement_score":0.92765826,"about_ca_system_score_codex":0.000003179134,"about_ca_system_score_gemma":0.00031089073,"threshold_uncertainty_score":0.98975676},"labels":[],"label_agreement":null},{"id":"W2146731604","doi":"10.1139/e07-028","title":"Nucularcidae: a new family of palaeotaxodont Ordovician pelecypods (Mollusca) from North America and Australia","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Ordovician; Synonym (taxonomy); Paleontology; Genus; Geology; Baltica; Type species; Dentition; Biostratigraphy; Biozone; Zoology; Biology","score_opus":0.030744468983330067,"score_gpt":0.23656121793613244,"score_spread":0.2058167489528024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146731604","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9857439,0.007379641,0.00021974079,0.00023810359,0.00037640403,0.000053544347,0.000064853855,0.0000026804646,0.005921136],"genre_scores_gemma":[0.9945978,0.000054884043,0.0050606686,0.00012101993,0.00012490773,2.7685303e-8,0.0000020114228,6.8635404e-7,0.00003801836],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99855304,0.000057313904,0.00042154646,0.0001830093,0.00030465296,0.00048043995],"domain_scores_gemma":[0.99830925,0.00014750451,0.00030759248,0.000097409524,0.00007495769,0.0010632823],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048756727,0.00013047886,0.00028368118,0.0003735577,0.0002875117,0.00007405969,0.00040189107,0.00007221634,0.0003324911],"category_scores_gemma":[0.00008462318,0.000103185295,0.00009243881,0.00059873256,0.0011008095,0.00026569673,0.000001160499,0.00021001537,0.0000055324713],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014078858,0.0000024343133,0.9176316,0.0000021066562,0.000019616613,0.0001210535,0.00042668075,0.0000627301,0.00005385311,0.00002331199,0.000066356595,0.08157617],"study_design_scores_gemma":[0.0001903318,0.00041138474,0.9957256,0.000029601988,0.000020460804,0.00005578625,0.0005612528,0.000064565334,0.000041127932,0.00041987278,0.0023596757,0.00012038093],"about_ca_topic_score_codex":0.18629685,"about_ca_topic_score_gemma":0.9477526,"teacher_disagreement_score":0.7614558,"about_ca_system_score_codex":9.948855e-7,"about_ca_system_score_gemma":0.0011165664,"threshold_uncertainty_score":0.81912166},"labels":[],"label_agreement":null},{"id":"W2146756787","doi":"10.1139/e01-088","title":"Correlation chart of the Proterozoic assembly of the northeastern Canadian - Greenland Shield","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University; Geological Survey of Canada; Memorial University of Newfoundland; Government of Newfoundland and Labrador","funders":"","keywords":"Geology; Proterozoic; Shield; Baltic Shield; Paleontology; Precambrian; Chart; Geochemistry; Physical geography; Tectonics; Geography","score_opus":0.03646368793638599,"score_gpt":0.18515597236945563,"score_spread":0.14869228443306964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146756787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98914707,0.0005343915,0.000009743391,0.0043138596,0.00064320426,0.00012498087,0.000022389779,6.6783275e-7,0.005203672],"genre_scores_gemma":[0.99951196,0.00001735117,0.000030608975,0.00020121026,0.00005750731,1.6486045e-7,4.3896654e-7,7.0196427e-7,0.00018008224],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990766,0.0000739386,0.00025945058,0.00007818155,0.00027424263,0.00023760952],"domain_scores_gemma":[0.9992637,0.00004628715,0.000269299,0.00009144003,0.00009293558,0.00023636088],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043718406,0.00006317717,0.00011967921,0.000089325935,0.00047442457,0.000037322683,0.00042544494,0.00003819583,0.00085071294],"category_scores_gemma":[0.00013548558,0.000030374755,0.00007347274,0.00044610776,0.0004051148,0.00019277913,0.000005067722,0.00012210445,0.0000127690355],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000012294933,0.0000014179337,0.9914692,0.0000026613625,0.0000043217597,0.000001648164,0.00045245758,0.004991011,0.0000039057636,0.00003054892,0.00011331517,0.0029283073],"study_design_scores_gemma":[0.00006511816,0.00016413789,0.9911215,0.00004182336,0.000007278218,0.00002042014,0.0003539049,0.0052813804,0.000035611185,0.00016098958,0.0027047761,0.000043106764],"about_ca_topic_score_codex":0.38931683,"about_ca_topic_score_gemma":0.98785675,"teacher_disagreement_score":0.5985399,"about_ca_system_score_codex":0.0000021104286,"about_ca_system_score_gemma":0.00036182202,"threshold_uncertainty_score":0.931471},"labels":[],"label_agreement":null},{"id":"W2146773444","doi":"10.1139/e06-088","title":"Origin, age, and paleoenvironmental significance of carbonate precipitates from a granitic environment, Akshayuk Pass, southern Baffin Island, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto","keywords":"Calcite; Geology; Geochemistry; Precambrian; Weathering; Carbonate; Strontium; Isotopes of strontium; δ18O; Mineralogy; Stable isotope ratio; Chemistry","score_opus":0.015329973475445435,"score_gpt":0.1989763638993372,"score_spread":0.18364639042389178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146773444","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945806,0.0028859328,0.000009694766,0.00024980263,0.0002325331,0.00008280333,0.00024535038,0.0000011756475,0.0017120888],"genre_scores_gemma":[0.9992886,0.00009366652,0.00031754002,0.00010521173,0.000052167088,1.8985403e-7,0.0000118319995,0.0000020741666,0.00012871333],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99849004,0.00011019089,0.00034145813,0.00020267829,0.00032912396,0.0005265047],"domain_scores_gemma":[0.9986896,0.000436342,0.00020050026,0.0000920149,0.00002156771,0.0005600012],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00085307914,0.00012427829,0.0002399697,0.00017424823,0.00028578172,0.000035047666,0.00034930639,0.00006725941,0.0018138365],"category_scores_gemma":[0.00006501252,0.00009929659,0.0000376812,0.0001506454,0.0014405705,0.00013069369,0.000006512813,0.00023158213,0.000017661167],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018290231,0.000003139491,0.9980026,0.0000046310543,0.000019880303,0.00047880187,0.00039655276,0.00038736497,0.000031170362,0.000009353339,0.000033379623,0.0006148269],"study_design_scores_gemma":[0.00023545696,0.00017472186,0.99548095,0.000019834833,0.000015410074,0.00009520751,0.0012447995,0.0001506366,0.000090099806,0.00048584165,0.0018938839,0.00011317607],"about_ca_topic_score_codex":0.7073027,"about_ca_topic_score_gemma":0.99881417,"teacher_disagreement_score":0.29151148,"about_ca_system_score_codex":0.0000018370578,"about_ca_system_score_gemma":0.00096529885,"threshold_uncertainty_score":0.99909866},"labels":[],"label_agreement":null},{"id":"W2146874305","doi":"10.1139/e03-064","title":"Diagenetic transformations (opal-A to quartz) of low- and mid-temperature microbial textures in siliceous hot-spring deposits, Taupo Volcanic Zone, New Zealand","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Subaerial; Diagenesis; Geology; Quartz; Volcano; Geochemistry; Chalcedony; Mineralogy; Hydrothermal circulation; Sedimentary depositional environment; Hot spring; Microbial mat; Dissolved silica; Geomorphology; Paleontology; Chemistry","score_opus":0.006624819221961694,"score_gpt":0.17790821010483268,"score_spread":0.17128339088287098,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146874305","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99600875,0.0027397745,0.0000122236725,0.0007514122,0.00009530758,0.0000678331,0.000016447219,0.0000015942497,0.0003066577],"genre_scores_gemma":[0.9987722,0.00007098839,0.0007345008,0.00027517238,0.000035234098,1.3308829e-7,0.0000016980523,0.0000010582434,0.00010903611],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99889076,0.000065158,0.0003533229,0.00015533743,0.0001793411,0.000356107],"domain_scores_gemma":[0.99895996,0.000082523555,0.00009440749,0.00006214683,0.000056771914,0.0007442118],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033814218,0.00011024499,0.00023499811,0.00033257977,0.0001625448,0.000100633726,0.00023695927,0.000058501475,0.0006432816],"category_scores_gemma":[0.00012750833,0.00007813452,0.000069673806,0.0007751673,0.00017616195,0.00017108972,0.0000024804551,0.00016477652,0.00000845692],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014274335,0.000009467313,0.97553754,0.00001624459,0.000014511145,0.000051162275,0.0013069033,0.01490192,0.005874771,0.000024481593,0.00014600722,0.0021026938],"study_design_scores_gemma":[0.00027197125,0.00029600726,0.990092,0.00008849844,0.00002153935,0.00012103812,0.00036930968,0.00012774633,0.006224863,0.00045589387,0.001772255,0.00015891243],"about_ca_topic_score_codex":0.041533843,"about_ca_topic_score_gemma":0.92734545,"teacher_disagreement_score":0.8858116,"about_ca_system_score_codex":0.0000017538688,"about_ca_system_score_gemma":0.0005213515,"threshold_uncertainty_score":0.96484864},"labels":[],"label_agreement":null},{"id":"W2147053648","doi":"10.1139/e05-051","title":"Metallogeny of the Grenville Province revisited","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Medicago (Canada); Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Université du Québec à Montréal","keywords":"Geology; Geochemistry; Iron oxide copper gold ore deposits; Metallogeny; Terrane; Magmatism; Ore genesis; Chromite; Crust; Partial melting; Mafic; Mineralization (soil science); Pyrite; Sphalerite; Fluid inclusions; Paleontology; Quartz; Tectonics","score_opus":0.014421029571943382,"score_gpt":0.183311494371199,"score_spread":0.16889046479925562,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147053648","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98404044,0.002297327,0.00000639543,0.0030301376,0.0000941655,0.000036061872,0.0000167164,0.0000010731032,0.010477692],"genre_scores_gemma":[0.99828976,0.000016537666,0.0009709643,0.00043532441,0.00008190818,2.9468573e-8,5.776688e-7,4.3400323e-7,0.0002044651],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990512,0.00005859991,0.0002809106,0.00010084249,0.00026779284,0.0002406283],"domain_scores_gemma":[0.999229,0.000064545784,0.00021592506,0.00009120474,0.00009229187,0.00030703525],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005751777,0.00006576789,0.00016488797,0.000108013075,0.0002126797,0.00003701901,0.00059791235,0.000028146973,0.00730542],"category_scores_gemma":[0.00022886488,0.000032125005,0.00014534526,0.0005930002,0.00061217905,0.0001327899,0.0000064187043,0.00011499069,0.00003180202],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000023404832,0.0000033830117,0.9879973,0.000002901278,0.000013313967,0.000006502993,0.00003519052,0.0039908797,0.0002271528,0.00020326047,0.00012941484,0.007388371],"study_design_scores_gemma":[0.00007866481,0.00013223274,0.9678159,0.000022500048,0.000030914776,0.000058507292,0.00007135786,0.0014952467,0.0016668349,0.0023161585,0.026227128,0.000084555504],"about_ca_topic_score_codex":0.008875013,"about_ca_topic_score_gemma":0.42505777,"teacher_disagreement_score":0.41618276,"about_ca_system_score_codex":7.711655e-7,"about_ca_system_score_gemma":0.00045913708,"threshold_uncertainty_score":0.99772495},"labels":[],"label_agreement":null},{"id":"W2147219539","doi":"10.1139/e06-021","title":"Finite element modeling of transient saline hydrothermal fluids in multifaulted sedimentary basins: implications for ore-forming processes","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geothermal gradient; Convection; Hydrothermal circulation; Sedimentary rock; Structural basin; Sedimentary basin; Sink (geography); Fluid dynamics; Salinity; Geochemistry; Petrology; Convection cell; Mineralogy; Geomorphology; Natural convection; Geophysics; Combined forced and natural convection; Mechanics; Oceanography","score_opus":0.02220192744455705,"score_gpt":0.2416847433883788,"score_spread":0.21948281594382177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147219539","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95787257,0.00030731346,0.040121265,0.0010644812,0.0000685684,0.00019239368,0.00004356312,0.000002247203,0.00032762566],"genre_scores_gemma":[0.9961784,0.000009097538,0.0035635333,0.00012515044,0.000029783721,0.000009664987,0.0000033174638,0.0000036882136,0.00007737402],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9990102,0.00001584144,0.00042157227,0.00012528374,0.00017361011,0.00025346826],"domain_scores_gemma":[0.9996134,0.00005031911,0.00011803709,0.000051426956,0.000064307125,0.00010250147],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048083416,0.00007846338,0.00013182056,0.00017549805,0.00022000162,0.00002937435,0.00020333914,0.000019160472,0.00007769411],"category_scores_gemma":[0.000035477075,0.000063902095,0.000041647716,0.00040662813,0.00020287503,0.00035118987,0.000008964497,0.000044542998,0.0000012481968],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016707365,0.000076620185,0.4558279,0.000034235436,0.000014545371,0.0000047755693,0.0021913517,0.52517444,0.0062057786,0.00015240858,0.00012754959,0.010173682],"study_design_scores_gemma":[0.0026600566,0.00089961995,0.6285303,0.00034123397,0.00007104369,0.000042292577,0.003868165,0.3222902,0.0149683785,0.0011626862,0.024587246,0.000578749],"about_ca_topic_score_codex":0.010252093,"about_ca_topic_score_gemma":0.24904363,"teacher_disagreement_score":0.23879154,"about_ca_system_score_codex":0.000029114977,"about_ca_system_score_gemma":0.00023945855,"threshold_uncertainty_score":0.9963387},"labels":[],"label_agreement":null},{"id":"W2147317765","doi":"10.1139/e02-075","title":"Marine reptiles from the Nanaimo Group (Upper Cretaceous) of Vancouver Island","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"North Island College; Royal Tyrrell Museum","funders":"","keywords":"Fauna; Cretaceous; Geology; Paleontology; Pacific Plate; Genus; Group (periodic table); Ecology; Biology; Subduction; Tectonics","score_opus":0.016255502807478176,"score_gpt":0.1865756281161238,"score_spread":0.17032012530864563,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147317765","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95291096,0.008107547,0.000018175428,0.0012123275,0.0013137734,0.000045303703,0.00009705483,0.0000023889206,0.036292475],"genre_scores_gemma":[0.99813396,0.00019610443,0.00068256,0.00038831317,0.00018604496,7.888421e-8,0.0000027640738,8.4975704e-7,0.00040934593],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990051,0.00012008787,0.00027686002,0.00013169777,0.0001678531,0.00029844526],"domain_scores_gemma":[0.9990887,0.0003031309,0.00020303958,0.00010930378,0.000060472066,0.00023537672],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00051178003,0.00008324015,0.00017341235,0.000118532036,0.00037735936,0.000025690235,0.00048774394,0.00006722485,0.014975046],"category_scores_gemma":[0.00014743653,0.00004830857,0.000075457036,0.00024600653,0.0011731782,0.0002481832,0.0000050457634,0.00016226879,0.000050543473],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000070597443,0.0000027389117,0.98592633,9.285082e-7,0.00001592766,0.00003535113,0.00021756286,0.0002693756,0.000005653674,0.0000528476,0.008989121,0.0044771163],"study_design_scores_gemma":[0.00011917481,0.00023216415,0.94765025,0.000014486657,0.000012255896,0.00009757079,0.00028824768,0.0012611611,0.000005476256,0.0013217101,0.04893047,0.000067001936],"about_ca_topic_score_codex":0.034930583,"about_ca_topic_score_gemma":0.96114504,"teacher_disagreement_score":0.92621446,"about_ca_system_score_codex":0.0000010427982,"about_ca_system_score_gemma":0.00020514466,"threshold_uncertainty_score":0.9859254},"labels":[],"label_agreement":null},{"id":"W2147467540","doi":"10.1139/e03-068","title":"Experimental studies on New Zealand hot spring sinters: rates of growth and textural development","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Microbial Community Ecology and Physiology","field":"Environmental Science","cited_by":123,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Calcite; Hot spring; Supersaturation; Geology; Mineralogy; Precipitation; Quartz; Growth rate; Evaporation; Chemistry; Paleontology","score_opus":0.039751387336295296,"score_gpt":0.26580059523633504,"score_spread":0.22604920790003974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147467540","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99819326,0.00042327985,0.00000127514,0.00013016585,0.00018240626,0.000028292821,3.9016533e-7,6.4678085e-7,0.0010402784],"genre_scores_gemma":[0.99875504,0.00001123646,0.00093793904,0.00016801016,0.000009915758,1.5137198e-7,7.6649684e-8,0.0000014303984,0.000116196316],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994435,0.00007545091,0.00017234156,0.00007709595,0.00006447542,0.00016714906],"domain_scores_gemma":[0.99957836,0.000075188866,0.00011069687,0.00003902998,0.000008921052,0.00018783075],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033464143,0.00006392505,0.00012869584,0.00007171703,0.0002487771,0.000016357635,0.00016620176,0.00002130652,0.00046757862],"category_scores_gemma":[0.00009903716,0.000048072572,0.000019292802,0.000101934114,0.000706644,0.00013051016,0.00002128938,0.000091827766,0.000007426276],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046373585,0.000045935416,0.86994404,0.000009039999,0.000065929584,0.00003397732,0.019644007,0.0006977715,0.10547794,0.0013152399,0.0021790653,0.00054071716],"study_design_scores_gemma":[0.0005313704,0.0013155214,0.5835078,0.000111843154,0.000008762435,0.00012311728,0.0055287,0.0000059892022,0.4009227,0.0008699767,0.0068513784,0.00022288386],"about_ca_topic_score_codex":0.0022320307,"about_ca_topic_score_gemma":0.069746256,"teacher_disagreement_score":0.29544473,"about_ca_system_score_codex":0.0000122246765,"about_ca_system_score_gemma":0.00024087404,"threshold_uncertainty_score":0.94722843},"labels":[],"label_agreement":null},{"id":"W2147822729","doi":"10.1139/e02-018","title":"Mesozoic thermal history and timing of structural events for the Yukon-Tanana Upland, east-central Alaska: <sup>40</sup>Ar/<sup>39</sup>Ar data from metamorphic and plutonic rocks","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Metamorphism; Metamorphic rock; Hornblende; Plutonism; Geochemistry; Pluton; Cretaceous; Assemblage (archaeology); Paleontology; Biotite","score_opus":0.0511554759180611,"score_gpt":0.20133830917179316,"score_spread":0.15018283325373205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147822729","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9721626,0.025494765,0.000028390848,0.0015073552,0.00014007333,0.00011278334,0.00036132213,0.0000034750437,0.00018925716],"genre_scores_gemma":[0.998767,0.00018686964,0.0004541766,0.00025366785,0.00017696663,3.5832923e-7,0.000031834006,0.0000028472043,0.00012628913],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980276,0.00010108993,0.00046068258,0.00038030767,0.00040813684,0.0006221791],"domain_scores_gemma":[0.99828494,0.0004101743,0.00028876544,0.00023662692,0.000068605616,0.00071091566],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006576503,0.00020804764,0.0004099905,0.00017349239,0.00049675035,0.00009035522,0.0009618318,0.00008133591,0.0077317907],"category_scores_gemma":[0.00023134434,0.00012047495,0.00012239261,0.00027118088,0.00087579293,0.000539152,0.000037320995,0.00025948713,0.0000085421625],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041626285,0.000008239315,0.9553505,0.000015583655,0.00018532596,0.000035239038,0.0011015383,0.030724088,0.0000310556,0.000015188848,0.00064873096,0.011842842],"study_design_scores_gemma":[0.00047949346,0.00023844525,0.55284417,0.000042234176,0.00024350741,0.0000931649,0.0006614564,0.43966976,0.000019583204,0.0010651946,0.0044153323,0.00022768266],"about_ca_topic_score_codex":0.02218272,"about_ca_topic_score_gemma":0.09788956,"teacher_disagreement_score":0.40894568,"about_ca_system_score_codex":0.0000064512046,"about_ca_system_score_gemma":0.00030674355,"threshold_uncertainty_score":0.99317527},"labels":[],"label_agreement":null},{"id":"W2147851311","doi":"10.1139/e09-055","title":"Lithoprobe’s impact on the Canadian diamond-exploration industryThis article is one of a series of papers published in this Special Issue on the theme <i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.Earth Sciences Sector Contribution 20070261; Lithoprobe Contribution 1479.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Craton; Kimberlite; Geology; Terrane; Archean; Eclogite; Precambrian; Diamond; Crust; Proterozoic; Mantle (geology); Geochemistry; Earth science; Paleontology; Tectonics","score_opus":0.015276946897895417,"score_gpt":0.19966943584636954,"score_spread":0.18439248894847413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147851311","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97179437,0.00049951015,0.000004130516,0.024815872,0.00018853435,0.0004045228,0.00018857101,0.0000026091438,0.0021019015],"genre_scores_gemma":[0.999177,0.000060328635,0.00008653962,0.00040369752,0.00021513671,0.0000033046788,0.0000071545483,0.0000018946835,0.0000449756],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99748355,0.00034028292,0.0006806304,0.00027120224,0.00070065615,0.0005237016],"domain_scores_gemma":[0.99730146,0.0007772282,0.0007129333,0.00019082979,0.0006528533,0.00036467405],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.004574886,0.00019000661,0.00043817624,0.00034791115,0.00067806296,0.00025488855,0.0005826056,0.00014523178,0.006795928],"category_scores_gemma":[0.0038700432,0.0000850292,0.00014008992,0.0020188699,0.0033848083,0.0006696817,0.000012566395,0.0005471638,0.0000051818397],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042476147,0.00006976147,0.9824557,0.000024081899,0.00008780354,0.0000069672483,0.0023031305,0.0015788144,0.0015297466,0.009537614,0.0005459097,0.0014357668],"study_design_scores_gemma":[0.0015134161,0.00258908,0.91236264,0.00035720534,0.00013506175,0.000043880475,0.0035077105,0.0039915983,0.031092336,0.04063501,0.0033773798,0.00039467105],"about_ca_topic_score_codex":0.36826167,"about_ca_topic_score_gemma":0.92359996,"teacher_disagreement_score":0.55533826,"about_ca_system_score_codex":0.000013962427,"about_ca_system_score_gemma":0.0020564515,"threshold_uncertainty_score":0.9993274},"labels":[],"label_agreement":null},{"id":"W2148185714","doi":"10.1139/e03-084","title":"New reptile material from the Lower Triassic of Madagascar: implications for the PermianTriassic extinction event","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Muséum National d'Histoire Naturelle; University of Oxford","keywords":"Amniote; Tetrapod (structure); Permian; Extinction event; Paleontology; Geology; Permian–Triassic extinction event; Early Triassic; Extinction (optical mineralogy); Fauna; Vertebrate; Ecology; Biological dispersal; Biology; Population","score_opus":0.02754176653348678,"score_gpt":0.23875981275397173,"score_spread":0.21121804622048496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148185714","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9683071,0.00448534,0.0019320761,0.020393066,0.0035470084,0.0002233457,0.0004318784,0.0000033643662,0.0006768638],"genre_scores_gemma":[0.9982634,0.000066627654,0.00082153676,0.00021723156,0.0005558897,6.7225665e-7,0.000010385762,8.874506e-7,0.00006336012],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992004,0.000067203495,0.00028801605,0.00011379748,0.00009538519,0.00023521365],"domain_scores_gemma":[0.9989289,0.00044895944,0.00024952728,0.00012011635,0.000071157425,0.0001813154],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007207657,0.000067048175,0.00012594742,0.00006526555,0.000645095,0.000041241914,0.00047122306,0.0000557761,0.0012884621],"category_scores_gemma":[0.00019702189,0.000034298053,0.00010073503,0.00020462657,0.00052492315,0.00017520381,0.000002704889,0.0000902183,0.000009606679],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032289664,0.000021970729,0.8667266,0.0000037689297,0.00012659853,0.000012624338,0.0012217335,0.0224947,0.00040411207,0.0021106976,0.008266282,0.09828802],"study_design_scores_gemma":[0.0003049595,0.0003114326,0.9750425,0.00001314262,0.000029602461,0.00009133166,0.0002627742,0.000091502305,0.00004867335,0.00780092,0.015955217,0.00004790096],"about_ca_topic_score_codex":0.023687199,"about_ca_topic_score_gemma":0.52262884,"teacher_disagreement_score":0.49894166,"about_ca_system_score_codex":0.000002886179,"about_ca_system_score_gemma":0.0020036618,"threshold_uncertainty_score":0.9996245},"labels":[],"label_agreement":null},{"id":"W2148220487","doi":"10.1139/e04-017","title":"Detrital ooids of Holocene age in glaciomarine Champlain Sea sediments, Gatineau, Quebec, Canada","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Sedimentary rock; Ooid; Diagenesis; Holocene; Geochemistry; Oceanography; Geomorphology; Paleontology; Sedimentary depositional environment; Structural basin","score_opus":0.01727328163534382,"score_gpt":0.22256129402133526,"score_spread":0.20528801238599143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148220487","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99392295,0.0011668178,0.000005812931,0.0017080931,0.00040600705,0.00007040431,0.000028109056,0.000001431675,0.00269037],"genre_scores_gemma":[0.99904525,0.000025551568,0.0005544502,0.00019812524,0.00004274201,1.5758599e-7,0.000009876016,0.0000013764848,0.00012245023],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983591,0.000106842424,0.00040547966,0.00016166143,0.00037059945,0.0005963146],"domain_scores_gemma":[0.99892116,0.00015845434,0.00016952633,0.00009370559,0.00009557131,0.00056156487],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010533729,0.00010992456,0.0002705622,0.00052255247,0.00021834517,0.000034983423,0.00050243037,0.000077545315,0.0008779859],"category_scores_gemma":[0.00023845756,0.00008984576,0.000044533546,0.0008185933,0.0008652142,0.00023768106,0.0000072634675,0.00029757968,0.000011587601],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012063682,0.000005392235,0.9945392,0.0000081653325,0.000008971798,0.0011586418,0.00013910566,0.003656863,0.0000045457673,0.000066088585,0.000053986467,0.00034695983],"study_design_scores_gemma":[0.00047210293,0.00021024274,0.9973071,0.000040637384,0.0000036599467,0.0003147163,0.00031444998,0.000067861176,0.00025121294,0.00048915297,0.00043374475,0.000095078474],"about_ca_topic_score_codex":0.96508974,"about_ca_topic_score_gemma":0.99995,"teacher_disagreement_score":0.034860242,"about_ca_system_score_codex":0.0000040965633,"about_ca_system_score_gemma":0.007832738,"threshold_uncertainty_score":0.99779195},"labels":[],"label_agreement":null},{"id":"W2148277585","doi":"10.1139/e10-003","title":"Protracted continental collision — evidence from the Grenville OrogenThis article is one of a series of papers published in this Special Issue on the theme <i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":192,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"McGill University; Memorial University of Newfoundland","funders":"","keywords":"Geology; Laurentia; Metamorphism; Craton; Terrane; Orogeny; Rodinia; Subduction; Continental collision; Granulite; Lithosphere; Continental crust; Geochemistry; Collision zone; Supercontinent; Proterozoic; Continental margin; Metamorphic facies; Diachronous; Paleontology; Crust; Ordovician; Facies; Tectonics; Structural basin","score_opus":0.014250217791429242,"score_gpt":0.18774192531287334,"score_spread":0.1734917075214441,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148277585","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97855306,0.0010988029,7.289204e-7,0.018872265,0.00011084339,0.0002531332,0.000056041466,8.493343e-7,0.0010542773],"genre_scores_gemma":[0.9993033,0.0001024588,0.00023218177,0.00021037452,0.00011350931,0.0000013213486,0.0000011783773,8.350245e-7,0.000034831148],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984831,0.00019467945,0.00050921814,0.00015525859,0.00045249678,0.00020521198],"domain_scores_gemma":[0.99774337,0.0012247893,0.0005208326,0.00013484794,0.00024394722,0.00013221284],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0020097385,0.00009488635,0.00032851775,0.00008032359,0.00018456006,0.00008217826,0.00052201346,0.000049472543,0.009784459],"category_scores_gemma":[0.002702003,0.000038093873,0.00009654849,0.000829158,0.0030570254,0.00028219377,0.000014164988,0.00024861156,0.0000022531349],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00070362695,0.00003134624,0.9922212,0.000016915377,0.000044581648,0.00000321409,0.0026595618,0.00015609378,0.0025263978,0.0005291866,0.00025943262,0.0008484786],"study_design_scores_gemma":[0.0017605211,0.00057687034,0.94669807,0.00039117387,0.0001083249,0.000022214223,0.004389839,0.0014445778,0.03241523,0.010339351,0.0016986872,0.00015514925],"about_ca_topic_score_codex":0.11155908,"about_ca_topic_score_gemma":0.44860652,"teacher_disagreement_score":0.33704746,"about_ca_system_score_codex":0.0000016575715,"about_ca_system_score_gemma":0.0004142471,"threshold_uncertainty_score":0.9996561},"labels":[],"label_agreement":null},{"id":"W2148685400","doi":"10.1139/cjes-2014-0170","title":"Review of Stagodontidae (Mammalia, Marsupialia) from the Judithian (Late Cretaceous) Belly River Group of southeastern Alberta, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Royal Tyrrell Museum","funders":"Core Research for Evolutional Science and Technology","keywords":"Nomen dubium; Genus; Paleontology; Holotype; Geology; Cretaceous; Archaeology; Dentition; Zoology; Geography; Biology; Taxon","score_opus":0.03251762595909242,"score_gpt":0.21846147304376107,"score_spread":0.18594384708466866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148685400","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.85286623,0.12836513,0.000016037075,0.0057791653,0.0018084694,0.00015519426,0.0003452869,0.0000018135709,0.01066269],"genre_scores_gemma":[0.9960272,0.0012900763,0.0003174264,0.0017503406,0.000119481956,1.4798361e-7,0.000006915288,0.000001969884,0.0004864998],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99826133,0.00023622741,0.00054268574,0.00014656915,0.0004784439,0.00033474836],"domain_scores_gemma":[0.99815035,0.00031072824,0.00055908295,0.00015484946,0.00029133182,0.0005336676],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012733233,0.00012500396,0.00037964192,0.00008755774,0.00023613489,0.000024241297,0.0006441371,0.000041403342,0.0006897527],"category_scores_gemma":[0.00040614334,0.00007869647,0.00009374668,0.00034468103,0.0011100457,0.00019428534,0.000008420163,0.00015980031,0.000012281308],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009536334,0.0000018652638,0.9933536,0.000039380517,0.00004050056,0.0000187153,0.0008990027,0.00014840404,8.164183e-7,0.00002990305,0.0042850943,0.0011731513],"study_design_scores_gemma":[0.00020837755,0.00020655198,0.8850931,0.0008065478,0.000055765548,0.000032605047,0.0012103113,0.00015556064,0.0000052906807,0.00020912784,0.11190337,0.00011342206],"about_ca_topic_score_codex":0.97348493,"about_ca_topic_score_gemma":0.99989825,"teacher_disagreement_score":0.14316092,"about_ca_system_score_codex":0.0000026927678,"about_ca_system_score_gemma":0.0035820338,"threshold_uncertainty_score":0.7552308},"labels":[],"label_agreement":null},{"id":"W2149238852","doi":"10.1139/e03-102","title":"Little Ice Age glacial activity in Strathcona Provincial Park, Vancouver Island, British Columbia, Canada","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Moraine; Glacier; Geology; Physical geography; Climate change; Glacial period; Terminal moraine; Landform; Ice field; Geomorphology; Archaeology; Geography; Oceanography","score_opus":0.013094946020289858,"score_gpt":0.20518681121140983,"score_spread":0.19209186519111998,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149238852","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98852813,0.00035607748,0.00000353003,0.0003429745,0.0010966684,0.00009825829,0.0000841391,0.0000019059931,0.009488334],"genre_scores_gemma":[0.9990661,0.00001417328,0.00011841526,0.00022023548,0.0001346784,3.1097838e-7,0.0000025670713,0.0000014543026,0.00044205307],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983609,0.0001314833,0.00025981775,0.00020488353,0.00036186198,0.0006810592],"domain_scores_gemma":[0.99902153,0.00012149362,0.00012510743,0.0000733325,0.000081050726,0.0005774879],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00089632004,0.00008315306,0.00023365757,0.00013704374,0.0005179391,0.0002573505,0.00044898107,0.00010069738,0.0020493914],"category_scores_gemma":[0.0002108337,0.0000987702,0.000045602348,0.00046250355,0.0007598855,0.0004154382,0.000005335692,0.00044308542,0.000014045222],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009937347,0.0000056974955,0.99451166,0.0000053316385,0.000005222567,0.0026411114,0.00009214013,0.000943854,0.0000012795226,0.0000057115494,0.0006609,0.0011171686],"study_design_scores_gemma":[0.00042839834,0.00020283702,0.994641,0.000032403907,0.0000037183922,0.0003735647,0.00021156488,0.00004296256,0.000008548023,0.00075669884,0.0031782086,0.00012007248],"about_ca_topic_score_codex":0.99581695,"about_ca_topic_score_gemma":0.9999999,"teacher_disagreement_score":0.015691558,"about_ca_system_score_codex":0.0000050086946,"about_ca_system_score_gemma":0.015696567,"threshold_uncertainty_score":0.99886286},"labels":[],"label_agreement":null},{"id":"W2149391817","doi":"10.1139/e01-080","title":"Depth migration of deep seismic reflection profiles: crustal thickness variations in Alberta","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Crust; Mantle (geology); Seismology; Discontinuity (linguistics); Tectonics; Seismic refraction; Lithosphere; Metamorphic rock; Petrology; Geochemistry","score_opus":0.022241853115986355,"score_gpt":0.209387499922507,"score_spread":0.18714564680652063,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149391817","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891426,0.0003950233,0.00016568889,0.0019010294,0.00013385552,0.000044871267,0.00000587458,0.000001481175,0.008209598],"genre_scores_gemma":[0.9990523,0.000022377686,0.0006181104,0.00013128434,0.000047452002,1.9943184e-7,0.0000039000533,5.924995e-7,0.00012378462],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999025,0.00008029795,0.00032597716,0.000120157834,0.00021353301,0.00023502295],"domain_scores_gemma":[0.9992855,0.00013951353,0.00018557583,0.000052319265,0.00009390968,0.00024317321],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004437428,0.000071045666,0.00016310453,0.00033561108,0.00015999931,0.000048959613,0.00021449993,0.0000523102,0.0050846105],"category_scores_gemma":[0.0002850747,0.000048378435,0.00006830378,0.0009839021,0.00023775468,0.00031880208,0.0000021508322,0.00013732549,0.000031095493],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000034545596,0.0000063469147,0.9806946,0.0000037658754,0.000005517852,0.000007937991,0.00035588813,0.014533335,0.000061218336,0.00007256464,0.000026911915,0.004228462],"study_design_scores_gemma":[0.00013958481,0.00034494718,0.86725885,0.000024128713,0.000018409104,0.00006205676,0.000245822,0.12728249,0.0003256022,0.0034976196,0.00070246117,0.000098026016],"about_ca_topic_score_codex":0.17509855,"about_ca_topic_score_gemma":0.9551822,"teacher_disagreement_score":0.78008366,"about_ca_system_score_codex":0.0000020084608,"about_ca_system_score_gemma":0.00014598372,"threshold_uncertainty_score":0.9958249},"labels":[],"label_agreement":null},{"id":"W2149492956","doi":"10.1139/e02-108","title":"A new characiform fish (Teleostei: Ostariophysi) from the Eocene of Tanzania","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fish biology, ecology, and behavior","field":"Environmental Science","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Teleostei; Characiformes; Tanzania; Fish <Actinopterygii>; Paleontology; Genus; Actinopterygii; Geology; Biology; Zoology; Geography; Fishery","score_opus":0.018267895173278155,"score_gpt":0.2146247457826979,"score_spread":0.19635685060941976,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149492956","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929281,0.00017326501,0.000011672498,0.0014671643,0.00055628945,0.000073797135,0.000025308513,0.0000016741328,0.004762759],"genre_scores_gemma":[0.99784434,0.000017084474,0.0010408575,0.0008511806,0.00007341054,4.5090545e-7,4.7352978e-7,0.0000032067924,0.00016902173],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988858,0.000065527754,0.00028803071,0.00015151803,0.000258354,0.00035074027],"domain_scores_gemma":[0.99911433,0.000074261974,0.00024620615,0.00013208367,0.00003052046,0.00040259305],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00072159566,0.00009509914,0.0001744013,0.000052775573,0.00028188722,0.00004473414,0.0005828331,0.00006307806,0.006389117],"category_scores_gemma":[0.00020632113,0.000060878287,0.00007779121,0.0003634899,0.00091081625,0.00025010633,0.000017171422,0.00016038696,0.000056159246],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000054214765,0.000014544224,0.98164123,8.46373e-7,0.0000090119975,0.000031050426,0.00044629746,0.00004854217,0.0073517114,0.00016719972,0.0061931172,0.004090997],"study_design_scores_gemma":[0.00016420311,0.00027182486,0.9685576,0.000013336968,0.000014187816,0.000048104783,0.00035416335,0.0000058367727,0.0021873296,0.0007830015,0.027518779,0.000081610946],"about_ca_topic_score_codex":0.024037717,"about_ca_topic_score_gemma":0.5445774,"teacher_disagreement_score":0.5205397,"about_ca_system_score_codex":0.000022581344,"about_ca_system_score_gemma":0.0008554499,"threshold_uncertainty_score":0.9945192},"labels":[],"label_agreement":null},{"id":"W2149500426","doi":"10.1139/e02-101","title":"Early rhinocerotids (Mammalia: Perissodactyla) from South Asia and a review of the Holarctic Paleogene rhinocerotid record","year":2003,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Wenner-Gren Foundation","keywords":"Paleogene; Holarctic; Cenozoic; Plateau (mathematics); Paleontology; Geology; Biochronology; Subtropics; Neogene; Mammal; Geography; Proboscidea; Structural basin; Biostratigraphy; Ecology; Genus","score_opus":0.05146497683649396,"score_gpt":0.25960120167901346,"score_spread":0.2081362248425195,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149500426","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0035607321,0.9907876,0.000002091171,0.00032725235,0.0012934533,0.00036020545,0.0002359216,0.0000028994925,0.0034297951],"genre_scores_gemma":[0.00508824,0.9939333,0.0002840769,0.0003232333,0.00012643234,0.0000010540135,0.000005060767,0.000005360233,0.00023321144],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99694383,0.00071055925,0.0010138811,0.00035153827,0.00047178203,0.0005084054],"domain_scores_gemma":[0.99723494,0.00029471258,0.001382032,0.0002737778,0.00020509587,0.00060942746],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015703433,0.00035140268,0.0014765688,0.00031008376,0.0006548107,0.000117771066,0.00091839075,0.00018505508,0.0017997524],"category_scores_gemma":[0.00056981074,0.0002045806,0.000488976,0.0008784563,0.0014354088,0.00024888682,0.000013975484,0.000623947,0.000029435188],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000035265666,0.0000041459716,0.7845829,0.004673711,0.00020574756,0.00004419218,0.00035616846,0.0000022459812,3.2382477e-8,0.000019731402,0.00070398336,0.20940359],"study_design_scores_gemma":[0.00012046237,0.00023218515,0.27997577,0.027456237,0.00056897214,0.00035273738,0.00015821602,0.000003016693,2.3572598e-7,0.000054946093,0.69078517,0.00029202676],"about_ca_topic_score_codex":0.008236898,"about_ca_topic_score_gemma":0.3027893,"teacher_disagreement_score":0.6900812,"about_ca_system_score_codex":0.000005274839,"about_ca_system_score_gemma":0.0032495765,"threshold_uncertainty_score":0.9991127},"labels":[],"label_agreement":null},{"id":"W2149931535","doi":"10.1139/e00-045","title":"The Climate System History and Dynamics Program - CSHD: Introduction","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Paleoclimatology; Climatology; Climate system; Last Glacial Maximum; Proxy (statistics); Holocene; Coupled model intercomparison project; Climate change; Climate model; Earth system science; Holocene climatic optimum; Physical geography; Geology; Cenozoic; Glacial period; Geography; Oceanography; Paleontology; Computer science","score_opus":0.013140158469068608,"score_gpt":0.21126578415367375,"score_spread":0.19812562568460515,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149931535","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97270185,0.0062555275,9.2415894e-7,0.0026072708,0.000931715,0.00008604564,0.000005848232,0.0000072441535,0.017403552],"genre_scores_gemma":[0.99876803,0.0003177832,0.00024402683,0.00005276743,0.00017114716,3.2576557e-7,0.0000023059076,8.979288e-7,0.00044271015],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99892855,0.00015210595,0.00019926688,0.00012292384,0.0001590094,0.00043815415],"domain_scores_gemma":[0.99930537,0.00012506652,0.00008563476,0.000078586694,0.00006216481,0.0003431564],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016345159,0.000065026805,0.000111122696,0.00013715542,0.0009451749,0.000098923374,0.00028883148,0.000057912002,0.0011000186],"category_scores_gemma":[0.000057398356,0.00004019099,0.000030144214,0.0001785485,0.0015885488,0.00022549895,0.0000021471171,0.00023429385,0.00007316172],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010846159,0.000001124847,0.975264,0.0000064569444,0.0000053285853,0.000039334445,0.00008276867,0.0002118059,8.6840856e-8,0.00078823545,0.00022242147,0.02336758],"study_design_scores_gemma":[0.000099653065,0.00041770583,0.88337266,0.000016065353,0.000009309769,0.0017817974,0.00069129636,0.008161619,0.0000010246144,0.00014175687,0.10523162,0.00007551167],"about_ca_topic_score_codex":0.0022289723,"about_ca_topic_score_gemma":0.51381475,"teacher_disagreement_score":0.51158583,"about_ca_system_score_codex":0.0000020813288,"about_ca_system_score_gemma":0.00069958373,"threshold_uncertainty_score":0.99981314},"labels":[],"label_agreement":null},{"id":"W2150063945","doi":"10.1139/e2012-007","title":"The Cabot Head Archipelago: evidence of glacial Lake Algonquin on the Northern Bruce Peninsula, Ontario","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Waterloo; Queen's University; Golder Associates (Canada); Trent University","funders":"Parks Canada","keywords":"Geology; Bedrock; Shore; Glacial period; Archipelago; Shelf ice; Bay; Head (geology); Glacial lake; Oceanography; Geomorphology; Paleontology; Arctic","score_opus":0.062055128610260565,"score_gpt":0.2684745023806677,"score_spread":0.20641937377040714,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150063945","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9873524,0.0032521,0.0000028319116,0.003601515,0.0008544603,0.00009731257,0.000008647358,0.0000015192919,0.0048292414],"genre_scores_gemma":[0.99908674,0.000044481483,0.000067439425,0.00026079826,0.0001536186,3.366602e-7,8.1753086e-7,0.0000013424941,0.00038444722],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997961,0.00039227842,0.00032938612,0.00012351987,0.00045280327,0.0007410099],"domain_scores_gemma":[0.99722433,0.0017073561,0.00023100787,0.00018268639,0.00013868028,0.000515955],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0039433455,0.000110365385,0.00018322855,0.00015747698,0.0012647042,0.000089280635,0.0010197437,0.00006434306,0.0016104677],"category_scores_gemma":[0.00069082883,0.000055329314,0.000093017996,0.00036110915,0.0022953998,0.00032258537,0.000009449715,0.0005212704,0.00015192345],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041121028,0.0000036701733,0.9965345,0.0000023179882,0.000012223924,0.000018347588,0.0018442969,0.00027161473,0.0000019736867,0.0002854962,0.00005307487,0.0009313068],"study_design_scores_gemma":[0.000076098986,0.0004207346,0.9925963,0.000053930424,0.000008410456,0.00022806584,0.00076558156,0.000060500934,0.000042951262,0.0004752151,0.0052021546,0.0000700101],"about_ca_topic_score_codex":0.09639398,"about_ca_topic_score_gemma":0.9983694,"teacher_disagreement_score":0.9019754,"about_ca_system_score_codex":0.0000012507015,"about_ca_system_score_gemma":0.002783144,"threshold_uncertainty_score":0.9993022},"labels":[],"label_agreement":null},{"id":"W2151421046","doi":"10.1139/e10-077","title":"Tungsten in Archean banded iron formation of the former Sherman and Adams mines, Ontario: possible mineralization processes","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University; University of Sudbury","funders":"","keywords":"Tungsten; Archean; Geology; Geochemistry; Mineralization (soil science); Metamorphic rock; Metamorphism; Hydrothermal circulation; Banded iron formation; Wolframite; Silicate; Chemistry; Paleontology; Metallurgy; Materials science","score_opus":0.013230893384128098,"score_gpt":0.18553389762687633,"score_spread":0.17230300424274825,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151421046","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961682,0.00018852626,0.000004169932,0.0007251047,0.00008081985,0.00004339184,0.000004960638,7.207871e-7,0.002784135],"genre_scores_gemma":[0.99940395,0.000007743972,0.00028877254,0.000096548465,0.0000215848,1.1172003e-7,0.0000035625312,4.2628028e-7,0.00017728197],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993166,0.0000214468,0.00023408605,0.00007701273,0.00017270834,0.0001781898],"domain_scores_gemma":[0.999498,0.000041745327,0.00014797403,0.000044374865,0.000090172914,0.00017771717],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035642568,0.000057482604,0.000110933805,0.00013610513,0.00013793899,0.000053310912,0.00021567062,0.00003478273,0.0009520085],"category_scores_gemma":[0.00014460941,0.000030695886,0.000031587504,0.00048185186,0.0003082921,0.00039448286,0.000004095837,0.0001158681,0.0000010967317],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000034302939,0.0000027836725,0.9974142,0.00001154242,0.0000012549707,0.0000015850734,0.00049742195,0.00051207555,0.00042926855,0.000019247727,0.000019167883,0.0010880546],"study_design_scores_gemma":[0.00010062657,0.000079033096,0.99464476,0.000025772419,0.000007968603,0.000035582736,0.00017352808,0.0013427621,0.0007838514,0.0021675637,0.00058803085,0.00005051685],"about_ca_topic_score_codex":0.24475338,"about_ca_topic_score_gemma":0.99732256,"teacher_disagreement_score":0.7525692,"about_ca_system_score_codex":0.0000011455054,"about_ca_system_score_gemma":0.0004937358,"threshold_uncertainty_score":0.99996126},"labels":[],"label_agreement":null},{"id":"W2151462099","doi":"10.1139/cjes-2012-0120","title":"A new genus and species of polychelid lobster (Crustacea, Decapoda, Eryonidae) from the Early Jurassic (Hettangian) of British Columbia","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Crustacean biology and ecology","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Decapoda; Crustacean; Genus; Terrane; Shrimp; Geology; Paleontology; Geography; Biology; Fishery; Zoology","score_opus":0.010339642927222023,"score_gpt":0.18120754468288905,"score_spread":0.17086790175566702,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151462099","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959951,0.0009741519,0.00001875001,0.0007961642,0.00026745722,0.00009298384,0.000034535522,0.0000011963331,0.0018196298],"genre_scores_gemma":[0.9962099,0.00004826298,0.0009908726,0.0002807887,0.000059954673,3.8052107e-7,3.6777507e-7,0.000003281743,0.002406194],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989738,0.00005323775,0.00032802724,0.00015300843,0.00017573193,0.00031621437],"domain_scores_gemma":[0.9990661,0.0001542075,0.0002729935,0.00011397952,0.00003118013,0.00036154897],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034158907,0.00006759013,0.00020496806,0.000040484072,0.00019721623,0.00013595572,0.0004471706,0.00007439401,0.012972371],"category_scores_gemma":[0.00010087415,0.000063845204,0.000061489874,0.00024127681,0.0018565009,0.0003348404,0.00004291699,0.00013505494,0.000049178518],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000023605023,0.0000047038766,0.9745793,0.0000011130089,0.000012363577,0.000014841321,0.0005777358,0.000018081144,0.00067777414,0.000009631281,0.01917906,0.0049230624],"study_design_scores_gemma":[0.00016055597,0.00021337088,0.99124426,0.000025597432,0.000012616013,0.00006457182,0.0009244091,0.000016002763,0.00009971246,0.00052730995,0.0066394215,0.00007217128],"about_ca_topic_score_codex":0.45515084,"about_ca_topic_score_gemma":0.90381473,"teacher_disagreement_score":0.4486639,"about_ca_system_score_codex":0.000011649888,"about_ca_system_score_gemma":0.0003296234,"threshold_uncertainty_score":0.9879299},"labels":[],"label_agreement":null},{"id":"W2151533434","doi":"10.1139/cjes-2014-0197","title":"Taphonomy, age, and paleoecological implication of a new <i>Pachyrhinosaurus</i> (Dinosauria: Ceratopsidae) bonebed from the Upper Cretaceous (Campanian) Wapiti Formation of Alberta, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Taphonomy; Paleontology; Cretaceous; Canyon; Sedimentary depositional environment; Paleoecology; Structural basin; Geomorphology","score_opus":0.0217732895035943,"score_gpt":0.20690052123436614,"score_spread":0.18512723173077184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151533434","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9908249,0.0038014106,0.000035952875,0.0029516187,0.00036262267,0.000088917295,0.00007802003,0.0000012144832,0.0018553851],"genre_scores_gemma":[0.99883014,0.000053678472,0.0005413042,0.0004114267,0.00009760219,2.1310092e-7,0.000019131969,8.1474155e-7,0.00004570081],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886006,0.00013927619,0.00040527663,0.00013139329,0.00019039075,0.00027362775],"domain_scores_gemma":[0.9985447,0.00038190294,0.00036075214,0.00009846372,0.00012200274,0.0004921574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051412405,0.000097285316,0.00023977057,0.00008701458,0.0002101159,0.000027727081,0.00034926386,0.00008760789,0.0003100968],"category_scores_gemma":[0.0002842275,0.00006182789,0.000042588385,0.00021925545,0.0006192482,0.00038042458,0.0000059456056,0.00014225669,0.000004077517],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026571703,0.0000026673758,0.9942654,0.000002213076,0.000012737509,0.000019781866,0.0009586872,0.00033200026,0.000032999218,0.00011352719,0.002698778,0.0015346713],"study_design_scores_gemma":[0.00025509723,0.00027064467,0.9859674,0.000013933895,0.00001868247,0.00019711402,0.0010907139,0.0003577217,0.00009548392,0.0016354914,0.010022385,0.00007535143],"about_ca_topic_score_codex":0.86699766,"about_ca_topic_score_gemma":0.9982175,"teacher_disagreement_score":0.13121988,"about_ca_system_score_codex":0.000005299255,"about_ca_system_score_gemma":0.003700698,"threshold_uncertainty_score":0.65648794},"labels":[],"label_agreement":null},{"id":"W2151549408","doi":"10.1139/e05-031","title":"Unusual tetrapod teeth from the Upper Triassic Chinle Formation, Arizona, USA","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"American Museum of Natural History","keywords":"Amniote; Tetrapod (structure); Dentition; Affinities; Basal (medicine); Paleontology; Geology; Vertebrate; Biology","score_opus":0.02307948876235159,"score_gpt":0.21873893567893046,"score_spread":0.19565944691657888,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151549408","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97468674,0.004745519,0.000091824135,0.007860217,0.0008938907,0.000055922214,0.00009085506,0.0000033888423,0.01157162],"genre_scores_gemma":[0.9967289,0.000056458375,0.0011472028,0.0013193144,0.0005757958,1.4610883e-7,0.000010626581,8.020786e-7,0.00016072924],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998817,0.00015550264,0.0003128849,0.00012770397,0.00019500786,0.00039190054],"domain_scores_gemma":[0.99898565,0.000327541,0.00018256775,0.000091614245,0.0000633498,0.0003492877],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009293164,0.00009483051,0.00014682011,0.00016549022,0.0008659585,0.00008011007,0.000586432,0.00007801347,0.003938405],"category_scores_gemma":[0.00018278156,0.000054789132,0.00007603667,0.000330108,0.0008660767,0.000757845,0.0000029210971,0.0002409251,0.00027828192],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009840756,0.0000026984821,0.98113453,4.046167e-7,0.000010814964,0.000010144684,0.0003460239,0.0011307814,0.000005918085,0.00022224718,0.0018000675,0.015326506],"study_design_scores_gemma":[0.00017737107,0.00016110345,0.9205013,0.000009807806,0.000009220193,0.00019764311,0.0003133577,0.0014383672,0.000019548148,0.0010728809,0.07602198,0.00007742903],"about_ca_topic_score_codex":0.015386269,"about_ca_topic_score_gemma":0.84083194,"teacher_disagreement_score":0.82544565,"about_ca_system_score_codex":0.0000026440125,"about_ca_system_score_gemma":0.0011101636,"threshold_uncertainty_score":0.99697214},"labels":[],"label_agreement":null},{"id":"W2151600986","doi":"10.1139/e06-029","title":"Evidence for a second species of the ichthyosaur <i>Platypterygius</i> in North America: a new record from the Loon River Formation (Lower Cretaceous) of northwestern Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Cretaceous; Paleontology; Geology; Taxon; Geography","score_opus":0.027010719662904106,"score_gpt":0.19596857263263825,"score_spread":0.16895785296973415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151600986","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938836,0.0033280237,0.00006748195,0.0012157871,0.0006729294,0.00011510489,0.000255233,6.4513966e-7,0.00046118573],"genre_scores_gemma":[0.99900466,0.000035222733,0.0003128095,0.0003868062,0.000116920164,2.3724154e-7,0.0000077274135,7.973046e-7,0.00013478938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99893457,0.0000972507,0.00041357276,0.00011024134,0.00018507811,0.00025929353],"domain_scores_gemma":[0.9986764,0.00056423026,0.0004478799,0.00010812725,0.00009074122,0.00011260727],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003039193,0.000084252606,0.00019299144,0.000083474326,0.00019929372,0.000017130102,0.00054226053,0.00003991321,0.00045907914],"category_scores_gemma":[0.000119440796,0.00004812814,0.00007104353,0.000383621,0.000728494,0.00044861276,0.0000050664403,0.000121135454,0.0000018424416],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037376143,0.0000018961035,0.9943539,0.0000036603928,0.000006411026,0.0000063949788,0.00031052285,0.0023990737,0.000016459959,0.000006936708,0.0014075586,0.0014497925],"study_design_scores_gemma":[0.00014304952,0.00016004067,0.98149836,0.000056851204,0.00001143034,0.000025280446,0.00025927575,0.00042707165,0.000037149224,0.0003293027,0.016994108,0.000058067104],"about_ca_topic_score_codex":0.89808995,"about_ca_topic_score_gemma":0.9999425,"teacher_disagreement_score":0.10185252,"about_ca_system_score_codex":0.0000060410152,"about_ca_system_score_gemma":0.0027239237,"threshold_uncertainty_score":0.5026595},"labels":[],"label_agreement":null},{"id":"W2151609727","doi":"10.1139/e04-095","title":"Regional and local vegetation community dynamics of the Eocene Okanagan Highlands (British Columbia Washington State) from palynology","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":97,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Brandon University","funders":"Australian Research Council; Natural Sciences and Engineering Research Council of Canada; University of Wisconsin-Madison","keywords":"Palynology; Macrofossil; Vegetation (pathology); Ecology; Edaphic; Betulaceae; Geography; Geology; Deciduous; Phytogeography; Disjunct; Taxon; Pollen; Paleontology; Biology; Population","score_opus":0.01723353231093637,"score_gpt":0.17201991336104805,"score_spread":0.15478638105011167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151609727","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974239,0.00027973167,0.00000788082,0.0019440238,0.000112267924,0.000024184856,0.00007916836,0.0000017870873,0.00012707118],"genre_scores_gemma":[0.9996373,0.00005185383,0.00006477928,0.00015480588,0.000047378137,6.026592e-8,0.000008176561,1.7839197e-7,0.000035448145],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993607,0.00011500554,0.00014170619,0.000062519655,0.00017467554,0.00014543951],"domain_scores_gemma":[0.9994991,0.000091439644,0.0001472845,0.000021392705,0.00009946435,0.00014134849],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046237957,0.000035573536,0.000093249146,0.000014971574,0.0006930257,0.00011956292,0.00029769237,0.000044128,0.000060500603],"category_scores_gemma":[0.000052726435,0.000019851692,0.000034771547,0.00018828733,0.0005888867,0.00022887441,0.000019324234,0.00015763225,7.677831e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008626774,0.000023058556,0.9305965,0.00000420013,0.000015737258,0.0000098363025,0.0004993623,0.000520269,0.0010365129,0.000097830954,0.001040934,0.06614717],"study_design_scores_gemma":[0.0000787562,0.00011815849,0.9946463,0.000054405733,0.000007077565,0.000052020645,0.00078427413,0.0010071141,0.00003966802,0.001452199,0.0017144387,0.000045593904],"about_ca_topic_score_codex":0.30979463,"about_ca_topic_score_gemma":0.99550945,"teacher_disagreement_score":0.68571484,"about_ca_system_score_codex":0.000015450589,"about_ca_system_score_gemma":0.00012328781,"threshold_uncertainty_score":0.6948015},"labels":[],"label_agreement":null},{"id":"W2151832387","doi":"10.1139/e10-061","title":"The parabasisphenoid complex in Mesozoic turtles and the evolution of the testudinate basicranium","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Agencia Nacional de Promoción Científica y Tecnológica; Consejo Nacional de Investigaciones Científicas y Técnicas; Fondation Simone et Cino Del Duca; Deutsche Forschungsgemeinschaft; Ministerio de Ciencia, Tecnología e Innovación Productiva; Centre National de la Recherche Scientifique; Deutscher Akademischer Austauschdienst","keywords":"Endochondral ossification; Turtle (robot); Anatomy; Paleontology; Skull; Geology; Ossification; Internal carotid artery; Biology; Cartilage","score_opus":0.013605715681933424,"score_gpt":0.20194773652178014,"score_spread":0.18834202083984672,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151832387","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9845926,0.0039886367,0.0000031175848,0.0069769146,0.0008063951,0.00007490155,0.00001168936,8.1567254e-7,0.0035448996],"genre_scores_gemma":[0.9996274,0.000050521598,0.000100617406,0.000120454926,0.000060301998,2.1433078e-7,2.5977613e-7,4.631028e-7,0.000039762068],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990784,0.00022472869,0.00022988638,0.00008625641,0.00012748381,0.00025327923],"domain_scores_gemma":[0.9989788,0.0005807208,0.0001795402,0.00009443621,0.00005974552,0.00010676644],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0019797217,0.000062006104,0.0001253326,0.00007619802,0.00088410545,0.00003203781,0.0005338179,0.000044280438,0.00011709048],"category_scores_gemma":[0.00036195797,0.000024914825,0.000046274003,0.00032701794,0.00459753,0.00012513857,0.0000065334034,0.00027440913,0.0000033685458],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016726086,0.000001209837,0.9954964,9.4998654e-7,0.000004932648,0.0000022324077,0.00013842572,0.0002015284,0.000053657797,0.0031206084,0.000068785106,0.00089456997],"study_design_scores_gemma":[0.00022023644,0.000057030313,0.98926073,0.000007667429,0.000006529611,0.00016028389,0.0005206927,0.0011646847,0.000008847858,0.0062084896,0.0023499413,0.000034863002],"about_ca_topic_score_codex":0.02094347,"about_ca_topic_score_gemma":0.9089764,"teacher_disagreement_score":0.88803285,"about_ca_system_score_codex":0.0000014883691,"about_ca_system_score_gemma":0.00074840104,"threshold_uncertainty_score":0.99811137},"labels":[],"label_agreement":null},{"id":"W2152087115","doi":"10.1139/cjes-2013-0026","title":"Detrital zircon geochronology of Ediacaran to Cambrian deep-water strata of the Franklinian basin, northern Ellesmere Island, Nunavut: implications for regional stratigraphic correlations","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Zircon; Provenance; Paleontology; Geochronology; Sedimentary rock; Sedimentary depositional environment; Passive margin; Craton; Structural basin; Geochemistry; Tectonics; Rift","score_opus":0.01725825224774137,"score_gpt":0.20176687491959275,"score_spread":0.18450862267185136,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152087115","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9884804,0.000243345,0.00030945783,0.009855772,0.00015072656,0.00018494777,0.00021817118,0.0000014151368,0.0005557643],"genre_scores_gemma":[0.99851906,0.0000084195735,0.001057999,0.00028244068,0.000076688244,0.0000014402061,0.000018169629,0.0000012008479,0.000034558667],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988231,0.000053067728,0.00045165748,0.00016206852,0.00017545807,0.0003346362],"domain_scores_gemma":[0.9987055,0.00018942256,0.00021858912,0.000135842,0.0003646569,0.0003859906],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029910798,0.00009905657,0.0002322045,0.00022969348,0.0003325141,0.00004150727,0.0005584573,0.000073143456,0.002142167],"category_scores_gemma":[0.00013715298,0.000054473774,0.00019681518,0.0005515698,0.0007329213,0.00017978603,0.000006752553,0.00013470423,0.000015429116],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000041083554,0.0000078545,0.9946508,0.000003713092,0.000023631135,5.99092e-7,0.00016386634,0.0026713852,0.0007994388,0.00021543098,0.0001262795,0.0013329291],"study_design_scores_gemma":[0.000137716,0.0002809133,0.99085164,0.000016749385,0.00003195497,0.000027369773,0.0003839575,0.0003987402,0.0006081979,0.0066115065,0.0005682425,0.00008300583],"about_ca_topic_score_codex":0.026254708,"about_ca_topic_score_gemma":0.91424817,"teacher_disagreement_score":0.88799345,"about_ca_system_score_codex":0.0000013518239,"about_ca_system_score_gemma":0.00051730516,"threshold_uncertainty_score":0.99877},"labels":[],"label_agreement":null},{"id":"W2152899562","doi":"10.1139/e08-044","title":"Stratigraphy and geochemistry of the Lac-Brompton ophiolite, Canada: evidence for extensive forearc magmatism and mantle exhumation in the Southern Quebec Ophiolite Belt","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Ophiolite; Geology; Forearc; Geochemistry; Obduction; Ultramafic rock; Basalt; Oceanic crust; Gabbro; Mantle (geology); Petrology; Subduction; Tectonics; Paleontology","score_opus":0.031053430650776703,"score_gpt":0.2074127018281698,"score_spread":0.17635927117739308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152899562","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935862,0.0033797433,0.0000037467237,0.0023941554,0.000036997273,0.00008922326,0.00006317329,5.3993324e-7,0.00044620936],"genre_scores_gemma":[0.9994068,0.00008776427,0.0001674255,0.0002676298,0.000030957646,4.6376925e-7,0.0000025782583,5.598833e-7,0.00003577692],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99908674,0.000058504902,0.00025431666,0.00012645285,0.00024927862,0.00022468985],"domain_scores_gemma":[0.99911225,0.0003490569,0.00017745953,0.00007800908,0.00011086408,0.00017235843],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004957077,0.00007975705,0.00015629845,0.00006801785,0.0003146868,0.000045306286,0.00030334803,0.00003275015,0.0002297488],"category_scores_gemma":[0.0002965408,0.00004028582,0.000052026047,0.00031787145,0.00072474784,0.00016022213,0.000005524735,0.000112082154,2.4172272e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009674787,0.0000027620117,0.9963194,0.000024737485,0.000009866636,0.000019039586,0.0007968528,0.00037413192,0.00018567777,0.00012404624,0.00028227604,0.001851494],"study_design_scores_gemma":[0.00008807068,0.00006184097,0.992388,0.00006283142,0.000012220673,0.00010507867,0.0011374553,0.00089578895,0.00018511647,0.004892858,0.00011140403,0.00005931181],"about_ca_topic_score_codex":0.8722465,"about_ca_topic_score_gemma":0.9969222,"teacher_disagreement_score":0.1246757,"about_ca_system_score_codex":0.0000017135255,"about_ca_system_score_gemma":0.0007882111,"threshold_uncertainty_score":0.26703635},"labels":[],"label_agreement":null},{"id":"W2153116299","doi":"10.1139/e02-044","title":"Stratigraphy, depositional setting, and diagenetic history of the Saint-Jules Formation (Upper Devonian or Mississippian), a newly identified post-Acadian red clastic unit in the southern Gaspé Peninsula, Quebec","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Devonian; Clastic rock; Paleontology; Sedimentary rock; Diagenesis; Arenite; SAINT; Sedimentary depositional environment; Late Devonian extinction; Structural basin; Carboniferous","score_opus":0.02643167696332559,"score_gpt":0.19469443956139323,"score_spread":0.16826276259806763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153116299","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.992772,0.0029884307,0.00001337558,0.0023973845,0.00014400779,0.00010193962,0.0000398216,0.0000016988364,0.0015413365],"genre_scores_gemma":[0.9988408,0.00003913595,0.00033741625,0.00043973202,0.000029862818,4.7776325e-7,0.0000039054526,0.0000011033686,0.00030756096],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988332,0.00016828983,0.00036405158,0.000096135824,0.00028945305,0.00024890265],"domain_scores_gemma":[0.9991698,0.00017859112,0.00025163664,0.00007976193,0.00010292593,0.00021723202],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005732726,0.00009333011,0.000116181975,0.00026692584,0.00039918264,0.00015737824,0.0004276751,0.000048402497,0.0022482763],"category_scores_gemma":[0.00022276319,0.000047982125,0.000055431672,0.00042575388,0.00058238214,0.0004710529,0.0000036893423,0.00016412516,0.0000082455945],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012927391,0.000009078931,0.9789213,0.000029464929,0.000008139024,0.00002476778,0.011963802,0.0019429001,0.000036694477,0.00016257136,0.0003228115,0.0065655294],"study_design_scores_gemma":[0.00014327635,0.00016977642,0.98611456,0.00007796196,0.000010093898,0.00022099956,0.0057514827,0.0034145492,0.000008865858,0.0004938609,0.0035142316,0.000080361904],"about_ca_topic_score_codex":0.053193834,"about_ca_topic_score_gemma":0.88353026,"teacher_disagreement_score":0.83033645,"about_ca_system_score_codex":0.0000050134295,"about_ca_system_score_gemma":0.0007884418,"threshold_uncertainty_score":0.9986638},"labels":[],"label_agreement":null},{"id":"W2153151264","doi":"10.1139/e09-034","title":"A late-glacial – Holocene palaeoecological record from Pye Lake on the eastern shore of Nova Scotia, CanadaGeological Survey of Canada Contribution 20080395.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval; Center for Northern Studies; University of British Columbia, Okanagan Campus; Douglas College; Geological Survey of Canada","funders":"","keywords":"Younger Dryas; Tundra; Holocene; Vegetation (pathology); Geology; Physical geography; Glacial period; Radiocarbon dating; Oceanography; Geography; Arctic; Paleontology","score_opus":0.043320192653126074,"score_gpt":0.2410254034921043,"score_spread":0.19770521083897824,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153151264","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99362856,0.00045245487,0.0000042263982,0.0036880195,0.00057856145,0.000107158274,0.00033082106,0.0000015116586,0.0012087079],"genre_scores_gemma":[0.9991821,0.000014676495,0.000053407504,0.0006237829,0.000054279582,7.330458e-8,0.000028534914,8.973023e-7,0.000042224405],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975869,0.00060901965,0.00050887687,0.00020507285,0.00046678897,0.00062332704],"domain_scores_gemma":[0.9974861,0.0011686828,0.00034753923,0.00012924927,0.00036834984,0.0005000509],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002333484,0.00013574393,0.00041013837,0.00016889599,0.0002912224,0.000028766004,0.000718767,0.00015383921,0.004993787],"category_scores_gemma":[0.0014988873,0.00008121805,0.00006511883,0.0005220781,0.0012238105,0.00009821235,0.000006622363,0.0004244198,0.000013607072],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008884702,0.000008459361,0.99801004,0.0000011756644,0.000016591799,0.00016378771,0.000042780757,0.0008133295,0.0000024062522,0.00006763292,0.00046559225,0.00031934635],"study_design_scores_gemma":[0.00020195848,0.00092819595,0.9974365,0.00002562136,0.000008367681,0.000042132666,0.000080622835,0.0004936875,0.000061281884,0.0004659247,0.00016755509,0.000088114415],"about_ca_topic_score_codex":0.91501087,"about_ca_topic_score_gemma":0.99992406,"teacher_disagreement_score":0.08491321,"about_ca_system_score_codex":0.00000234166,"about_ca_system_score_gemma":0.005110797,"threshold_uncertainty_score":0.9959158},"labels":[],"label_agreement":null},{"id":"W2153224972","doi":"10.1139/e00-106","title":"A new species of <i>Dimetrodon</i> (Synapsida: Sphenacodontidae) from the Lower Permian of Germany records first occurrence of genus outside of North America","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Geographic Society","keywords":"Permian; Genus; Paleontology; Autapomorphy; Holotype; Geology; Type locality; Ecology; Predation; Taphonomy; Geography; Biology; Structural basin; Phylogenetics","score_opus":0.019001853001945335,"score_gpt":0.20183855934312345,"score_spread":0.1828367063411781,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153224972","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98923063,0.004799338,0.0000953002,0.0007025159,0.00078138965,0.00006377234,0.00043731494,0.0000014383213,0.003888326],"genre_scores_gemma":[0.99792045,0.0004815266,0.0012365762,0.00009906476,0.00011656384,7.788116e-8,0.000008769383,0.0000010801612,0.00013590867],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983701,0.00012700775,0.00068342104,0.00017261678,0.0002937852,0.00035304905],"domain_scores_gemma":[0.99796563,0.00046452417,0.00087616785,0.00018767027,0.0001953749,0.00031059937],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048914476,0.00012826468,0.00044950118,0.00021984066,0.0001766289,0.000009567666,0.0008480641,0.00006368809,0.0031833122],"category_scores_gemma":[0.00027257987,0.00008529831,0.00015738302,0.00075067393,0.0022002533,0.0002467587,0.000009902948,0.0001771416,0.000010974797],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054269836,0.000010580494,0.9895741,0.000006101944,0.000035168418,0.000025144049,0.000465057,0.0011602972,0.00003331557,0.000010977347,0.0013896937,0.0072353277],"study_design_scores_gemma":[0.00015437532,0.00072603853,0.979837,0.000058778754,0.000030074934,0.000053414038,0.00036679744,0.00013554949,0.000082255094,0.00009974118,0.018370485,0.00008547366],"about_ca_topic_score_codex":0.10862515,"about_ca_topic_score_gemma":0.81184155,"teacher_disagreement_score":0.7032164,"about_ca_system_score_codex":0.0000024303527,"about_ca_system_score_gemma":0.0015746026,"threshold_uncertainty_score":0.99772793},"labels":[],"label_agreement":null},{"id":"W2153227769","doi":"10.1139/e00-061","title":"Late Maastrichtian age of spherule deposits in northeastern Mexico: implication for Chicxulub scenario","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Marl; Geology; Slumping; Pelagic zone; Cretaceous; Siliciclastic; Paleontology; Deposition (geology); Overprinting; Geochemistry; Sedimentary depositional environment; Structural basin; Oceanography","score_opus":0.019068863499314997,"score_gpt":0.2078207682321167,"score_spread":0.1887519047328017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153227769","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954675,0.0008749086,0.0001305793,0.0009817204,0.00009122004,0.00007217745,0.000017018476,0.0000016468028,0.0023632227],"genre_scores_gemma":[0.99850565,0.000031868614,0.001195563,0.00011482435,0.00004943877,2.5884282e-7,0.0000089667155,9.076874e-7,0.00009251158],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99892837,0.000031643816,0.00036561457,0.00014513954,0.00018546828,0.00034378748],"domain_scores_gemma":[0.99918115,0.00006656951,0.00019520968,0.000069685084,0.00009678839,0.00039060146],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046675946,0.00008215699,0.00020765566,0.00023164105,0.00012859362,0.000054286615,0.00035621185,0.000044727236,0.00092189934],"category_scores_gemma":[0.00010093755,0.000057252582,0.000097338096,0.00074819865,0.00023142363,0.00018870785,0.0000035263968,0.00009937931,0.00001206362],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010807166,0.000006087795,0.98507774,0.0000037194998,0.0000061833075,0.00002981545,0.00006968506,0.006660829,0.00020913551,0.00001675338,0.000006280498,0.007902959],"study_design_scores_gemma":[0.0001687612,0.00023836056,0.99126756,0.000025446185,0.000012207185,0.000042891596,0.00008687223,0.0025601462,0.00034998092,0.0033326796,0.0018353002,0.000079783706],"about_ca_topic_score_codex":0.029515853,"about_ca_topic_score_gemma":0.84614205,"teacher_disagreement_score":0.8166262,"about_ca_system_score_codex":0.0000014771405,"about_ca_system_score_gemma":0.00028510002,"threshold_uncertainty_score":0.9999914},"labels":[],"label_agreement":null},{"id":"W2153565394","doi":"10.1139/e10-109","title":"Geological significance of high-resolution magnetic data in the Quesnel terrane, Central British Columbia<sup>1</sup>This article is one of a series of papers published in this Special Issue on the theme of <i>New insights in Cordilleran Intermontane geoscience: reducing exploration risk in the mountain pine beetle-affected area, British Columbia</i>.<sup>2</sup>Geological Survey of Canada Contribution No. 20100225.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"British Geological Survey","keywords":"Geology; Terrane; Batholith; Pluton; Volcano; Geologic map; Basement; Sedimentary rock; Geochemistry; Volcanic rock; Paleontology; Diapir; Tectonics; Archaeology","score_opus":0.025718240969322112,"score_gpt":0.1838020107644242,"score_spread":0.15808376979510208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153565394","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974712,0.0004331841,0.0000032247185,0.0006160793,0.00007887422,0.0003925187,0.0005454779,0.0000014234116,0.00045802625],"genre_scores_gemma":[0.9993488,0.0002131543,0.000111514026,0.00015579203,0.00006109019,0.0000024630165,0.000059960308,0.0000016700471,0.000045562952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9957348,0.0013442951,0.0012139437,0.0003773843,0.0007942301,0.000535362],"domain_scores_gemma":[0.9977393,0.00072957936,0.0006880084,0.0002961443,0.00036323362,0.00018369587],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.004354536,0.00013284283,0.0006397409,0.00014663245,0.00017502031,0.0001468873,0.0013564273,0.00013218152,0.012964111],"category_scores_gemma":[0.0038620546,0.00010555041,0.00007173188,0.0019390394,0.0018136287,0.0005565789,0.000037394395,0.0004958077,6.535506e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014373595,0.00013616028,0.9880023,0.000014903307,0.000012556863,0.00006477746,0.0025493724,0.0055128704,0.00010675625,0.000008073965,0.0013159123,0.002132574],"study_design_scores_gemma":[0.0005344052,0.0012931479,0.9846826,0.00020272085,0.000018457356,0.000028221975,0.0023785974,0.009325621,0.00008848573,0.0012755323,0.00005245358,0.00011974629],"about_ca_topic_score_codex":0.9966832,"about_ca_topic_score_gemma":0.99965864,"teacher_disagreement_score":0.012963457,"about_ca_system_score_codex":0.00002020936,"about_ca_system_score_gemma":0.0010215282,"threshold_uncertainty_score":0.98793817},"labels":[],"label_agreement":null},{"id":"W2153612910","doi":"10.1139/e00-048","title":"The significance of multiple causes and coincidence in the geological record: from clam clusters to Cretaceous catastrophe","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Extinction event; Geology; Cretaceous; Paleontology; Geologic record; Extinction (optical mineralogy); Benthic zone; Permian–Triassic extinction event; Range (aeronautics); Oceanography; Population","score_opus":0.02910988079385374,"score_gpt":0.2294464986036818,"score_spread":0.20033661780982806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153612910","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99009126,0.0060945605,0.00003217402,0.002046391,0.00022427854,0.000103785416,0.000028527744,0.0000010643789,0.0013779493],"genre_scores_gemma":[0.99881405,0.00018662562,0.00072622794,0.00021903911,0.00004466222,4.1831373e-7,3.731192e-7,2.8373276e-7,0.000008315976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998838,0.00019879246,0.00028606332,0.0001390122,0.00021458458,0.00032354184],"domain_scores_gemma":[0.99837095,0.001057042,0.00015684534,0.00010043816,0.000046148965,0.00026860175],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010912091,0.00007992632,0.00015154883,0.000112159694,0.0004675684,0.00009781103,0.00062337064,0.00004164685,0.00006874932],"category_scores_gemma":[0.0003992596,0.000041228443,0.00003728862,0.0003762201,0.0012568493,0.00019071174,0.0000015277875,0.00018591399,0.0000022384743],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027551005,0.0000017088421,0.98356545,6.59214e-7,0.0000040536543,0.00014641783,0.0005838214,0.00057025574,0.000016992133,0.000014976398,0.00006599308,0.015002147],"study_design_scores_gemma":[0.00009281349,0.00035145416,0.99471897,0.000020222522,0.0000048880133,0.00017540736,0.0018026285,0.00043407577,0.000015227433,0.00042696946,0.0019016571,0.000055699835],"about_ca_topic_score_codex":0.06851983,"about_ca_topic_score_gemma":0.94407797,"teacher_disagreement_score":0.87555814,"about_ca_system_score_codex":8.4902297e-7,"about_ca_system_score_gemma":0.00044097856,"threshold_uncertainty_score":0.937683},"labels":[],"label_agreement":null},{"id":"W2153786885","doi":"10.1139/e09-025","title":"Stratigraphy of the Fort Selkirk Volcanogenic Complex in central Yukon and its paleoclimatic significance: Ar/Ar and paleomagnetic data","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Lethbridge","funders":"","keywords":"Geology; Paleomagnetism; Basalt; Volcanic rock; Pleistocene; Paleontology; Glacial period; Quaternary; Lava; Magnetic declination; Volcano; Earth's magnetic field","score_opus":0.05293196102280164,"score_gpt":0.2560582303858308,"score_spread":0.20312626936302916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153786885","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98908013,0.008142275,0.000001167682,0.0012371404,0.00012841937,0.0001423821,0.00006749008,0.0000012193178,0.0011997746],"genre_scores_gemma":[0.99918735,0.0003643683,0.00024666078,0.00015500133,0.000023448769,1.06808734e-7,0.000004069561,7.5499855e-7,0.000018246179],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985178,0.00018527183,0.00034666804,0.0002052965,0.00024279498,0.00050217053],"domain_scores_gemma":[0.99903744,0.00019171262,0.0001727812,0.00016426238,0.000051092014,0.0003827215],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010509001,0.00010262414,0.00023539858,0.00029905207,0.000295419,0.00005907214,0.0006930193,0.00006474865,0.00027632076],"category_scores_gemma":[0.00015184414,0.00006831368,0.000032851465,0.0005457286,0.0010497537,0.00030403453,0.000009855033,0.00024580545,0.0000019046779],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007868371,0.000004064133,0.9987843,0.000015682777,0.000005917365,0.000029996478,0.00017795955,0.00016574853,0.000037872644,0.000088276414,0.000020793625,0.0006615404],"study_design_scores_gemma":[0.0002142172,0.0003649903,0.9933021,0.000047344798,0.0000125672495,0.00023209584,0.0002983045,0.00422603,0.00002933199,0.0011160413,0.00008074561,0.0000762471],"about_ca_topic_score_codex":0.0011084288,"about_ca_topic_score_gemma":0.5990651,"teacher_disagreement_score":0.59795666,"about_ca_system_score_codex":2.793128e-7,"about_ca_system_score_gemma":0.00085199263,"threshold_uncertainty_score":0.40825093},"labels":[],"label_agreement":null},{"id":"W2153924069","doi":"10.1139/e06-007","title":"A second enantiornithean (Aves: Ornithothoraces) wing from the Early Cretaceous Xiagou Formation near Changma, Gansu Province, People's Republic of China","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Chinese Academy of Geological Sciences; China Geological Survey; Ministry of Land and Resources of the People's Republic of China; Chinese Academy of Sciences","keywords":"Manus; Geology; Cretaceous; Paleontology; Humerus; Ulna; Phalanx; Anatomy; Biology","score_opus":0.010931374155145796,"score_gpt":0.1909824682372609,"score_spread":0.1800510940821151,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153924069","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98971504,0.0035341433,0.0000887833,0.0011918492,0.0004768697,0.00011571916,0.0001661182,0.0000058141113,0.0047056396],"genre_scores_gemma":[0.99876094,0.00002501348,0.0007028559,0.00014118897,0.00021928853,3.0504617e-7,0.000021440153,0.00000189811,0.00012704602],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984438,0.0002357792,0.00045769944,0.00017437564,0.00024219563,0.0004461533],"domain_scores_gemma":[0.99879754,0.000232431,0.00048686954,0.00013633117,0.000113030605,0.00023380136],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012012197,0.000126161,0.00024001896,0.0002198832,0.00088901067,0.00014676523,0.00056286715,0.000096488846,0.0016198223],"category_scores_gemma":[0.00012955828,0.0000798478,0.000089513254,0.0005156232,0.00092548947,0.0009234516,0.0000051044553,0.00023884604,0.00002999091],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019051458,0.000004266705,0.9954494,0.0000055586643,0.000011371047,0.000027640554,0.0009426902,0.00075710216,0.00004294331,0.000071988245,0.00031831418,0.0023496437],"study_design_scores_gemma":[0.00015222824,0.0003062948,0.98853517,0.000039835504,0.00001575634,0.00029994172,0.00045797916,0.0013783601,0.000064436725,0.0010288549,0.0076176436,0.00010350201],"about_ca_topic_score_codex":0.04397393,"about_ca_topic_score_gemma":0.90822893,"teacher_disagreement_score":0.864255,"about_ca_system_score_codex":0.00000320619,"about_ca_system_score_gemma":0.0014030818,"threshold_uncertainty_score":0.99929285},"labels":[],"label_agreement":null},{"id":"W2154097498","doi":"10.1139/e05-001","title":"Taphonomic variations in Eocene fish-bearing varves at Horsefly, British Columbia, reveal 10 000 years of environmental change","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Directorate for Biological Sciences","keywords":"Taphonomy; Varve; Geology; Disarticulation; Water column; Paleontology; Dominance (genetics); Paleoecology; Ecology; Oceanography; Biology; Sediment","score_opus":0.022118711531000382,"score_gpt":0.20740410284748315,"score_spread":0.18528539131648275,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154097498","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968293,0.0009912498,4.6316626e-7,0.00036884236,0.00018281573,0.00007731314,0.00014299067,0.0000015350346,0.0014055322],"genre_scores_gemma":[0.99843717,0.000116218034,0.00041232535,0.00013609281,0.000093226125,4.2954687e-7,0.000008812072,0.0000015907345,0.00079416635],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987847,0.00011152563,0.00032782942,0.0001590661,0.0001846051,0.0004322678],"domain_scores_gemma":[0.9992749,0.00013243804,0.00016027957,0.00007624537,0.000016655647,0.00033948064],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009204257,0.00005690401,0.00019854272,0.00026413662,0.00028427137,0.00009392649,0.00035888643,0.000083005805,0.010051537],"category_scores_gemma":[0.000066748566,0.00007736375,0.000053331336,0.00026410035,0.0007250465,0.0004212151,0.000011029559,0.00018939844,0.0000812696],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000041673597,0.000006518786,0.99606305,0.000002810786,0.0000063057423,0.00008315976,0.0002640894,0.00032499584,0.000009708354,0.0000013834498,0.0001505778,0.003083249],"study_design_scores_gemma":[0.00020270687,0.00014610196,0.99664307,0.000029051233,0.0000047980493,0.000305153,0.00011062415,0.00058663206,0.000010537134,0.000057875786,0.0018263522,0.00007712007],"about_ca_topic_score_codex":0.12398164,"about_ca_topic_score_gemma":0.9871175,"teacher_disagreement_score":0.86313593,"about_ca_system_score_codex":0.0000030657468,"about_ca_system_score_gemma":0.00034117492,"threshold_uncertainty_score":0.9908534},"labels":[],"label_agreement":null},{"id":"W2154167055","doi":"10.1139/cjes-2014-0177","title":"A GIS-based method for depicting the characteristics of mesoscale eddies: a case study in the Northern South China Sea","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"National Science Foundation","keywords":"Eddy; Mesoscale meteorology; Geology; Climatology; Meteorology; Oceanography; Geography; Turbulence","score_opus":0.03955720474977436,"score_gpt":0.2652806236914333,"score_spread":0.22572341894165893,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154167055","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970344,0.0005781043,0.0010968081,0.0005725497,0.00021521059,0.00022255209,0.000046957095,0.0000018823723,0.00023154911],"genre_scores_gemma":[0.99633104,0.0000018959645,0.0033576805,0.00020159273,0.00009634602,7.921923e-7,8.995929e-7,0.0000018518417,0.0000078831845],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986976,0.00020448823,0.0003577068,0.000121943776,0.00031712986,0.00030115008],"domain_scores_gemma":[0.99868566,0.00045928932,0.00033661965,0.000109950844,0.00016328055,0.00024518505],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0040063364,0.000098516204,0.00020351943,0.00008141627,0.00042354446,0.00013378181,0.00056379795,0.000025158688,0.000030653002],"category_scores_gemma":[0.0005664398,0.000048815742,0.00006988797,0.00079524756,0.0003400471,0.00017663601,0.0000032880057,0.0001542647,7.702394e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011047196,0.000010600454,0.97855216,0.0000075175863,0.000008424799,0.00019975024,0.011960848,0.00249771,1.3215899e-7,0.0000029601965,0.000014277637,0.0067345444],"study_design_scores_gemma":[0.000541837,0.001375572,0.84553295,0.00004795728,0.00005002896,0.00068857596,0.1283107,0.022264175,0.0000062861827,0.00028117036,0.0007659727,0.0001347768],"about_ca_topic_score_codex":0.045410782,"about_ca_topic_score_gemma":0.6983605,"teacher_disagreement_score":0.6529497,"about_ca_system_score_codex":0.0000015083791,"about_ca_system_score_gemma":0.0018431025,"threshold_uncertainty_score":0.9609459},"labels":[],"label_agreement":null},{"id":"W2154211501","doi":"10.1139/e10-042","title":"High-precision U–Pb zircon ID–TIMS dating of two regionally extensive bentonites: Cenomanian Stage, Western Canada Foreland BasinThis article is one of a series of papers published in this Special Issue on the theme of<i>Geochronology</i>in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Cenomanian; Geology; Foreland basin; Zircon; Cretaceous; Paleontology; Geochronology; Bentonite; Marine transgression; Structural basin; Geochemistry","score_opus":0.024319762614598384,"score_gpt":0.19583739624626936,"score_spread":0.17151763363167097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154211501","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939155,0.00023808263,0.0000020942887,0.0012381107,0.00011857835,0.00008542378,0.00015139378,6.051051e-7,0.0042502023],"genre_scores_gemma":[0.9985566,0.000040499417,0.0011010072,0.00015946093,0.000062325,2.0233777e-7,0.000004599659,0.0000014367067,0.000073843155],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99808156,0.00014342266,0.00081270223,0.00018940456,0.0004638598,0.00030902168],"domain_scores_gemma":[0.9981875,0.00038215276,0.0007963555,0.0001585879,0.00028454696,0.00019084952],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001041901,0.0001198389,0.0004906832,0.00030555166,0.00007695011,0.000016475411,0.00056846184,0.00005578196,0.022552527],"category_scores_gemma":[0.0004978881,0.00007484796,0.00008842983,0.0007414653,0.0008744486,0.00028123282,0.00001864484,0.00019566734,0.0000013857572],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012550614,0.00004038294,0.99058133,0.000024263192,0.00004276815,0.000032997064,0.0021267105,0.0017131293,0.0023854072,0.00034137277,0.00014971741,0.0024363918],"study_design_scores_gemma":[0.00044759962,0.0009640108,0.93528235,0.0002812063,0.000030466546,0.000013232388,0.0039051026,0.00026347386,0.05486767,0.0033387144,0.00047614655,0.0001300027],"about_ca_topic_score_codex":0.75606424,"about_ca_topic_score_gemma":0.9826337,"teacher_disagreement_score":0.22656946,"about_ca_system_score_codex":0.000005870383,"about_ca_system_score_gemma":0.00091388676,"threshold_uncertainty_score":0.978341},"labels":[],"label_agreement":null},{"id":"W2154307385","doi":"10.1139/e99-115","title":"New UPb zircon ages integrated with ammonite biochronology from the Jurassic of the Canadian Cordillera","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of British Columbia","funders":"","keywords":"Ammonite; Zircon; Geology; Paleontology; Terrane; Biochronology; Radiometric dating; Biostratigraphy; Geochemistry; Cretaceous; Tectonics","score_opus":0.01177181300684238,"score_gpt":0.17204546726278022,"score_spread":0.16027365425593784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154307385","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98289484,0.001309672,0.0000048464453,0.008997157,0.00014544475,0.000052499756,0.00008028682,0.0000020113675,0.0065132333],"genre_scores_gemma":[0.9980976,0.000034158333,0.00048478285,0.00092089904,0.000087907,8.464421e-8,0.000006609298,0.0000010707581,0.00036687028],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99879867,0.000106780615,0.00026275797,0.00015836337,0.00026458886,0.00040886956],"domain_scores_gemma":[0.99872965,0.00015939535,0.00015958797,0.000146068,0.0001035276,0.00070176774],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002791786,0.00011619142,0.00021374533,0.00011940893,0.00058063417,0.00012220025,0.0008951102,0.0000626614,0.036248095],"category_scores_gemma":[0.00008567444,0.00004731768,0.00009847682,0.00097355567,0.0011992706,0.0001382296,0.000003590362,0.00027528673,0.00005580877],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000089224395,0.0000020173438,0.95634377,6.795534e-7,0.00004136377,0.000027926779,0.00016556974,0.0025183735,0.000053143453,0.000025055046,0.00068694184,0.04012622],"study_design_scores_gemma":[0.00012027887,0.00021485795,0.9811659,0.000040055183,0.000039615585,0.000040838324,0.00023377781,0.0003286797,0.00046475537,0.0012601032,0.015997121,0.00009402502],"about_ca_topic_score_codex":0.9520945,"about_ca_topic_score_gemma":0.9987924,"teacher_disagreement_score":0.046697915,"about_ca_system_score_codex":0.0000038641083,"about_ca_system_score_gemma":0.002928512,"threshold_uncertainty_score":0.9646329},"labels":[],"label_agreement":null},{"id":"W2154399930","doi":"10.1139/e07-036","title":"Late Holocene sea-level change around Newfoundland","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Agrisearch; Geological Society of America; National Science Foundation","keywords":"Geology; Deglaciation; Sea level; Holocene; Post-glacial rebound; Oceanography; Shore; Glacial period; Physical geography; Ice sheet; Climate change; Peninsula; Paleontology; Geography; Archaeology","score_opus":0.08994096924953172,"score_gpt":0.2767641603151919,"score_spread":0.1868231910656602,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154399930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98233265,0.002199378,0.000038843373,0.0013513723,0.0008930062,0.000067671775,0.000025551648,0.00000386392,0.013087666],"genre_scores_gemma":[0.99794704,0.00005894352,0.00069061876,0.00062345684,0.00031280366,8.85281e-8,0.0000049725636,0.0000015024772,0.0003605811],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983822,0.00008278763,0.00028206495,0.00016299318,0.00029016126,0.00079976924],"domain_scores_gemma":[0.9984791,0.0002518432,0.0001436082,0.00009352739,0.00012967654,0.00090222235],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0028618737,0.00010539568,0.00019287331,0.0005530241,0.00061850273,0.000106358304,0.00051209744,0.00010738816,0.0013680141],"category_scores_gemma":[0.00015086622,0.000079405494,0.000061600054,0.00058031495,0.0010589064,0.00047146078,0.0000046503474,0.00031467932,0.0002091584],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013123102,0.0000021445524,0.99724346,0.000003345635,0.000009118966,0.00047791118,0.00020731881,0.00011509957,9.969527e-7,0.00007191504,0.00004966008,0.0018058957],"study_design_scores_gemma":[0.00017724208,0.00028388447,0.994433,0.000018155153,0.000006307204,0.0007972666,0.00018199468,0.00022976931,0.000019507395,0.00075684563,0.0029966608,0.00009938175],"about_ca_topic_score_codex":0.02844534,"about_ca_topic_score_gemma":0.9017858,"teacher_disagreement_score":0.8733404,"about_ca_system_score_codex":7.340572e-7,"about_ca_system_score_gemma":0.0009644462,"threshold_uncertainty_score":0.99954486},"labels":[],"label_agreement":null},{"id":"W2154466700","doi":"10.1139/e09-041","title":"Eocene and Neogene volcanic rocks in the southeastern Nechako Basin, British Columbia: interpretation of the Canadian Hunter seismic reflection surveys using first-arrival tomography","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; Geological Survey of Canada","funders":"","keywords":"Geology; Outcrop; Neogene; Volcanic rock; Sedimentary rock; Seismic tomography; Cretaceous; Volcano; Seismology; Paleontology; Bedrock; Structural basin; Petrology; Mantle (geology)","score_opus":0.015785827431473068,"score_gpt":0.21080532493714002,"score_spread":0.19501949750566694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154466700","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996491,0.0005756228,0.00016711337,0.0014745841,0.0003392949,0.00010277181,0.000031355357,0.000002880262,0.0008153907],"genre_scores_gemma":[0.99800897,0.000017881548,0.00012106707,0.0017725448,0.000043943757,9.358666e-8,0.0000012886903,0.0000015836051,0.000032656753],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873364,0.00030295865,0.00027256095,0.00013813234,0.00025398564,0.00029874875],"domain_scores_gemma":[0.99935234,0.000058156864,0.00018148345,0.00009341599,0.00008881426,0.00022577737],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020255912,0.00007440772,0.00014916265,0.0003015651,0.00065833604,0.00045732758,0.0004035027,0.00005307782,0.00011155757],"category_scores_gemma":[0.0000907558,0.00006169653,0.000069649825,0.0007096356,0.000340792,0.0003471404,0.0000030379017,0.00020474775,6.629376e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000025479333,0.0000015241167,0.97527677,0.0000030082751,0.000003166441,0.000013024391,0.00052490446,0.0013854133,0.0000038005035,6.6944557e-7,0.00022677491,0.02255837],"study_design_scores_gemma":[0.00012007528,0.00033429186,0.95954174,0.00018486446,0.000012015134,0.00040967183,0.0006144182,0.03714098,0.000055730925,0.0007210252,0.00077585963,0.00008933331],"about_ca_topic_score_codex":0.9590787,"about_ca_topic_score_gemma":0.9987121,"teacher_disagreement_score":0.039633423,"about_ca_system_score_codex":0.000007418893,"about_ca_system_score_gemma":0.0008793394,"threshold_uncertainty_score":0.5063455},"labels":[],"label_agreement":null},{"id":"W2154680514","doi":"10.1139/e05-005","title":"The systematic position of the Late Jurassic alleged dinosaur<i>Macelognathus</i>(Crocodylomorpha: Sphenosuchia)","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Université Claude Bernard Lyon 1; Deutsche Forschungsgemeinschaft","keywords":"Postcrania; Paleontology; Geology; Mandibular symphysis; Tetrapod (structure); Osteology; Symphysis; Taxon; Geography; Archaeology","score_opus":0.01205481115898095,"score_gpt":0.19645677505255343,"score_spread":0.1844019638935725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154680514","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.978534,0.008716922,0.000016594884,0.0067231017,0.0010474012,0.00016158333,0.00002895312,0.0000029437715,0.004768537],"genre_scores_gemma":[0.9990375,0.00008367165,0.0001577968,0.0003541275,0.000115823175,3.716377e-7,0.0000012031958,9.414722e-7,0.00024857232],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99853367,0.0003142941,0.00043833817,0.000099080215,0.0002454951,0.00036910092],"domain_scores_gemma":[0.998759,0.00034954966,0.00043259756,0.00013081775,0.00010099445,0.00022704017],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013709905,0.00009561476,0.0002096829,0.000102916536,0.001129147,0.000050298062,0.00076486054,0.000066297514,0.00024399733],"category_scores_gemma":[0.00018952275,0.00004657751,0.00010806007,0.00033978312,0.0013916793,0.00026378562,0.0000054214233,0.00019798106,0.000036550668],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019246447,0.000007064262,0.988692,0.000079759266,0.00005160805,0.000019489175,0.00043280603,0.007248673,0.00018145575,0.001316502,0.00072677404,0.0012246346],"study_design_scores_gemma":[0.00014968833,0.00018451121,0.99268615,0.00024172601,0.000033543827,0.00046942258,0.00035755488,0.0023042993,0.000113051465,0.001008416,0.002365858,0.00008575716],"about_ca_topic_score_codex":0.001904667,"about_ca_topic_score_gemma":0.5540013,"teacher_disagreement_score":0.5520966,"about_ca_system_score_codex":0.0000032570908,"about_ca_system_score_gemma":0.00096698746,"threshold_uncertainty_score":0.86846},"labels":[],"label_agreement":null},{"id":"W2154878812","doi":"10.1139/cjes-2014-0239","title":"SHRIMP U–Pb and REE data pertaining to the origins of xenotime in Belt Supergroup rocks: evidence for ages of deposition, hydrothermal alteration, and metamorphism","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Zircon; Geology; Metamorphism; Geochemistry; Diagenesis; Metamorphic rock; Monazite; Sedimentary rock; Radiometric dating; Cretaceous; Paleontology","score_opus":0.10317231347636757,"score_gpt":0.2721130270046236,"score_spread":0.16894071352825601,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154878812","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99195814,0.0045670923,0.0003601185,0.0028766906,0.000046203982,0.00006374362,0.00004816357,6.667083e-7,0.00007916159],"genre_scores_gemma":[0.996339,0.00004320633,0.0033414604,0.0002120592,0.00004589299,2.7730505e-7,0.0000063185566,6.409687e-7,0.00001110097],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991211,0.00006225654,0.00029208206,0.00015069227,0.00019354382,0.00018032131],"domain_scores_gemma":[0.9990488,0.0002766967,0.00011880061,0.000100416815,0.00012887824,0.0003263507],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014099181,0.00006384709,0.00018388724,0.00015208819,0.00013313032,0.000059008133,0.00039873057,0.00002289652,0.00011175319],"category_scores_gemma":[0.0007579269,0.00003660225,0.000024444726,0.0003513525,0.00031374776,0.00044522868,0.0000148972795,0.00006113434,7.66068e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002412975,0.000003913934,0.9856678,0.000009649594,0.000015099375,0.000008407906,0.0008292849,0.008016679,0.00042440518,0.00016136825,0.00006953214,0.00476972],"study_design_scores_gemma":[0.00041150805,0.0013783908,0.9284911,0.00021703611,0.000086523585,0.00014800375,0.0013023409,0.0593932,0.0014634283,0.004437524,0.0024672982,0.00020364673],"about_ca_topic_score_codex":0.07792867,"about_ca_topic_score_gemma":0.5500311,"teacher_disagreement_score":0.47210246,"about_ca_system_score_codex":0.0000015063372,"about_ca_system_score_gemma":0.0003302983,"threshold_uncertainty_score":0.9282115},"labels":[],"label_agreement":null},{"id":"W2154891313","doi":"10.1139/cjes-2013-0147","title":"Mapping crustal structure of the Nechako–Chilcotin plateau using teleseismic receiver function analysis<sup>,</sup>","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Natural Resources Canada; University of Victoria","funders":"","keywords":"Geology; Seismology; Receiver function; Crust; Volcano; Plateau (mathematics); Magnetotellurics; Inversion (geology); Tectonics; Geophysics","score_opus":0.014462697993928532,"score_gpt":0.19037836425131718,"score_spread":0.17591566625738866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154891313","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99745053,0.0003002117,0.0008085928,0.0003103263,0.00034612443,0.000044055305,0.000061882296,0.0000023435434,0.00067592866],"genre_scores_gemma":[0.99849564,0.000008577138,0.0008456349,0.0003655721,0.00020588738,1.1682774e-8,0.0000047388176,0.0000021758203,0.00007179296],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99837554,0.00016108139,0.00043820086,0.00019891185,0.00044216213,0.00038413095],"domain_scores_gemma":[0.99880236,0.00009296671,0.00045953464,0.00016618619,0.0001289915,0.00034997705],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007732563,0.00013412604,0.00031952083,0.0007883755,0.0005974863,0.00014572972,0.0005552849,0.00007034482,0.001536412],"category_scores_gemma":[0.0001327404,0.000083575214,0.00028318987,0.0023528745,0.0004376228,0.0003596408,0.0000074987224,0.00023657246,0.0000044810668],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000034570085,0.0000011405996,0.44198275,0.0000035485232,0.00009600275,0.0000027863161,0.00025630742,0.5548966,0.000107238935,0.000036499452,0.000035320696,0.0025783563],"study_design_scores_gemma":[0.00012579755,0.000102180464,0.6127303,0.000046749647,0.00021575522,0.000046943278,0.0016935903,0.38037485,0.000085730346,0.0011290972,0.003313115,0.00013587248],"about_ca_topic_score_codex":0.037566006,"about_ca_topic_score_gemma":0.100337476,"teacher_disagreement_score":0.17452173,"about_ca_system_score_codex":0.0000041060066,"about_ca_system_score_gemma":0.00068759866,"threshold_uncertainty_score":0.9993763},"labels":[],"label_agreement":null},{"id":"W2154934314","doi":"10.1139/e07-016","title":"Alpine glacial geology of the Tablelands, Gros Morne National Park, Newfoundland","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University; Acadia University; University of Calgary","funders":"Purdue University","keywords":"Geology; Moraine; Cirque; Glacier; Glacial period; Geomorphology; Paleontology","score_opus":0.02644611345466862,"score_gpt":0.2488535552838838,"score_spread":0.22240744182921518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154934314","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97360194,0.0009011053,0.000027092912,0.0014107089,0.0008752146,0.000056283,0.000014044896,0.0000012765224,0.023112312],"genre_scores_gemma":[0.9989646,0.000017561704,0.00024897777,0.0002995115,0.0001678935,6.273031e-8,0.0000026832151,8.272217e-7,0.00029787526],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99857444,0.000113208545,0.00032892654,0.00011688773,0.00038022306,0.00048634064],"domain_scores_gemma":[0.99881554,0.00032573554,0.00021391227,0.00007293084,0.00023879032,0.0003330936],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0027830654,0.00007652601,0.00017722369,0.0003166449,0.00048032615,0.00002837234,0.00057219557,0.00009288702,0.0022946773],"category_scores_gemma":[0.00042238383,0.000047283083,0.00006822048,0.000556958,0.0017314398,0.00018561377,0.0000073490323,0.0002701845,0.000033661836],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019237577,0.000002901546,0.99809337,0.0000029430935,0.000011096558,0.000037588088,0.000100023826,0.00077070366,0.0000070956107,0.0006128175,0.0001540686,0.00018816929],"study_design_scores_gemma":[0.00021675117,0.00018062496,0.99240774,0.000010405124,0.00000523498,0.0006622331,0.00009700858,0.00020289658,0.000045939203,0.0021461681,0.003970703,0.000054310316],"about_ca_topic_score_codex":0.009289376,"about_ca_topic_score_gemma":0.87268513,"teacher_disagreement_score":0.86339575,"about_ca_system_score_codex":7.738823e-7,"about_ca_system_score_gemma":0.0021360146,"threshold_uncertainty_score":0.99861735},"labels":[],"label_agreement":null},{"id":"W2155186423","doi":"10.1139/e99-062","title":"Geoscience impact: a synthesis of studies of the Sudbury Structure","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Igneous rock; Archean; Metamorphism; Context (archaeology); Sedimentary rock; Geochemistry; Meteorite; Impact structure; Geophysics; Paleontology; Astrobiology; Impact crater","score_opus":0.017835896870112868,"score_gpt":0.2173838054908378,"score_spread":0.19954790862072494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155186423","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948511,0.003008434,6.5446915e-7,0.00061018637,0.00010928885,0.000028032513,0.00006495678,8.4118926e-7,0.0013264986],"genre_scores_gemma":[0.99939924,0.00008029559,0.00031676533,0.00009079687,0.000032408207,3.9063817e-8,2.1226877e-7,4.6557847e-7,0.000079790036],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99877656,0.000070589595,0.00037576302,0.000117961725,0.00037394487,0.0002851862],"domain_scores_gemma":[0.99893135,0.00024967772,0.000268074,0.00010835109,0.00015965803,0.00028290335],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005933692,0.00008768035,0.0002802526,0.00013526434,0.00023905122,0.000026088257,0.0007184169,0.0000341126,0.011318841],"category_scores_gemma":[0.00059600285,0.000039830364,0.00018876145,0.0010274493,0.0018918583,0.00017840332,0.0000059253607,0.00011471974,0.000004979758],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005506887,0.0000028978645,0.9807369,0.000007970582,0.000025859485,0.0000056488147,0.0001703009,0.0070972843,0.00019420695,0.000019305971,0.00003828705,0.011695799],"study_design_scores_gemma":[0.000037842983,0.00015551261,0.99073035,0.00006197374,0.00003142728,0.000045295656,0.0003290511,0.00037703916,0.00264054,0.0052534705,0.00027374452,0.000063742424],"about_ca_topic_score_codex":0.029920416,"about_ca_topic_score_gemma":0.2519903,"teacher_disagreement_score":0.22206986,"about_ca_system_score_codex":0.0000011814794,"about_ca_system_score_gemma":0.0005851589,"threshold_uncertainty_score":0.9895849},"labels":[],"label_agreement":null},{"id":"W2155290904","doi":"10.1139/e01-100","title":"A gravity profile across southern Saganash Lake fault: implications for the origin of the Kapuskasing Structural Zone","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Sinistral and dextral; Shear zone; Fault (geology); Seismology; Extensional definition; Shear (geology); Geodesy; Paleontology; Tectonics","score_opus":0.04497946212561604,"score_gpt":0.2609300213901272,"score_spread":0.21595055926451118,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155290904","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.991837,0.002853075,0.000036599096,0.0033131598,0.0004937324,0.00018658164,0.00057328213,0.0000029244234,0.0007036299],"genre_scores_gemma":[0.9989706,0.000027253805,0.00037388573,0.00014907631,0.0001247696,6.6256695e-7,0.0000011314384,0.0000017490662,0.00035082674],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989738,0.000044272725,0.00026789462,0.000120693134,0.00020280933,0.0003905244],"domain_scores_gemma":[0.99897176,0.00029468426,0.00026403432,0.00015358739,0.00014781319,0.00016811806],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00061894226,0.00009151471,0.0001518798,0.0000481953,0.0015870397,0.00012651068,0.0006210478,0.000030260784,0.00072371494],"category_scores_gemma":[0.0001890881,0.000044934943,0.00012939927,0.0004945241,0.0009376035,0.0001647723,0.0000073884935,0.00014027604,0.000010652316],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026164496,0.0000017181204,0.9627859,0.000005012623,0.000023566337,0.0000011382955,0.0022117675,0.00093965034,0.000012982786,0.00013052602,0.00027663267,0.033608485],"study_design_scores_gemma":[0.00014134118,0.00009529395,0.98598236,0.00002326106,0.000017901233,0.00006512006,0.0018310915,0.0011715878,0.00004490759,0.00057840906,0.009975697,0.00007304764],"about_ca_topic_score_codex":0.009995453,"about_ca_topic_score_gemma":0.85141957,"teacher_disagreement_score":0.8414241,"about_ca_system_score_codex":0.0000014804309,"about_ca_system_score_gemma":0.00034073714,"threshold_uncertainty_score":0.99971277},"labels":[],"label_agreement":null},{"id":"W2155294938","doi":"10.1139/e07-012","title":"Geochemistry of Sainte-Marguerite volcanic rocks: implications for the evolution of Silurian–Devonian volcanism in the Gaspé Peninsula","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Devonian; Volcanic arc; Volcanic rock; Peninsula; Volcano; Paleontology; Subduction; Volcanism; Igneous rock; Geochemistry; Tectonics; Archaeology","score_opus":0.021062512925616287,"score_gpt":0.2108922179672505,"score_spread":0.1898297050416342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155294938","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99073774,0.0025387174,0.0002683818,0.00443553,0.00007454023,0.000106531916,0.00009971635,0.0000012070013,0.0017376372],"genre_scores_gemma":[0.9993725,0.00006429814,0.00030839563,0.0001335933,0.0000684097,9.2539653e-7,0.000004846657,8.215169e-7,0.000046247438],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998845,0.000056338176,0.00042777654,0.00013394466,0.0002305006,0.00030644008],"domain_scores_gemma":[0.99868804,0.00046080988,0.00030399064,0.00014795852,0.00020923336,0.00018995236],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009116,0.00008810054,0.00020169158,0.00013991108,0.00038472156,0.000023611583,0.00081130926,0.000046310535,0.0008038284],"category_scores_gemma":[0.00046479938,0.00004591726,0.00016220758,0.0007915736,0.0008955209,0.00012427065,0.0000057910984,0.00015073584,0.00000290856],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008624747,0.0000099169365,0.9938249,0.0000067837473,0.00001389194,0.0000042850584,0.00030818896,0.0042443234,0.00055789703,0.00024566308,0.00020138561,0.0005741284],"study_design_scores_gemma":[0.00013630584,0.00018424194,0.9836628,0.000020930393,0.000020463453,0.0001231757,0.0010938372,0.0033555252,0.00035280315,0.009538931,0.0014395227,0.000071506875],"about_ca_topic_score_codex":0.061149854,"about_ca_topic_score_gemma":0.413213,"teacher_disagreement_score":0.35206315,"about_ca_system_score_codex":0.0000044446274,"about_ca_system_score_gemma":0.00092449604,"threshold_uncertainty_score":0.94510204},"labels":[],"label_agreement":null},{"id":"W2155326290","doi":"10.1139/e04-041","title":"An unusually large <i>Aulocopella winnipegensis</i> and associated demosponges from the Upper Ordovician Beaverfoot Formation, southeastern British Columbia","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Sponge spicule; Ordovician; Geology; Paleontology; Sponge","score_opus":0.01141903523736468,"score_gpt":0.19755999043471642,"score_spread":0.18614095519735174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155326290","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99030423,0.0059066443,0.000055525335,0.0007657518,0.00029377948,0.00008838855,0.0003657964,0.0000062371882,0.0022136203],"genre_scores_gemma":[0.9987716,0.000053302585,0.00037389534,0.0006781552,0.000097229306,1.3913744e-7,0.0000083595505,9.172682e-7,0.000016396374],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986062,0.00015539449,0.00032026262,0.00017834255,0.00027930518,0.0004604907],"domain_scores_gemma":[0.9988679,0.00011835657,0.00022517826,0.000100408906,0.00012778526,0.00056032476],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0010687024,0.000096869524,0.00019143161,0.000071119895,0.0014286258,0.0009011937,0.0004734084,0.00009310735,0.00030193277],"category_scores_gemma":[0.00011227541,0.00008976536,0.00006250194,0.00033703685,0.00067248463,0.00083648827,0.0000013227911,0.00021589857,0.000006539943],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000033573613,0.00000568539,0.9895444,9.870232e-7,0.000017049031,0.00006424405,0.0009221846,0.00010542066,0.000005051631,0.000011904929,0.000072826384,0.009246895],"study_design_scores_gemma":[0.00037527652,0.0002734385,0.99477065,0.000066370565,0.000022072338,0.00018704771,0.001590924,0.00021044063,0.000006492991,0.0015600756,0.0008129381,0.00012427906],"about_ca_topic_score_codex":0.29710597,"about_ca_topic_score_gemma":0.99838865,"teacher_disagreement_score":0.7012827,"about_ca_system_score_codex":0.0000014558639,"about_ca_system_score_gemma":0.00091714965,"threshold_uncertainty_score":0.9998714},"labels":[],"label_agreement":null},{"id":"W2155633713","doi":"10.1139/e06-130","title":"Fluid chemistry and evolution of hydrothermal fluids in an Archaean transcrustal fault zone network: the case of the Cadillac Tectonic Zone, Abitibi greenstone belt, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Hydrothermal circulation; Geology; Shear zone; Greenstone belt; Geochemistry; Fluid inclusions; Quartz; Archean; Mineralogy; Shear (geology); Mineralization (soil science); Tectonics; Petrology; Seismology","score_opus":0.007641142181726508,"score_gpt":0.18463577983876492,"score_spread":0.1769946376570384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155633713","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99602705,0.0025119067,0.000044863526,0.0005542061,0.00007901029,0.00006474086,0.000048344245,9.69027e-7,0.0006689132],"genre_scores_gemma":[0.99966294,0.0000139199565,0.00012998453,0.000087633016,0.000072855386,8.806631e-8,0.0000017942789,0.0000011874315,0.000029579036],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99858034,0.00008099536,0.00044037253,0.00015302116,0.00028627028,0.00045902582],"domain_scores_gemma":[0.99904126,0.00013937554,0.00018719496,0.00011916258,0.00009829672,0.00041468907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012758716,0.00010901044,0.00022698873,0.00006577488,0.00030524132,0.000018857969,0.00040229032,0.00005576324,0.0005532628],"category_scores_gemma":[0.000064961874,0.000059182363,0.000077091514,0.00082448765,0.0013626937,0.00012519964,0.000007912922,0.00024008773,2.0293326e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020159045,0.000005940704,0.9719883,0.000010950022,0.000013067206,0.0002814124,0.00021188175,0.020026822,0.0016351292,0.000062426654,0.000011541581,0.005732327],"study_design_scores_gemma":[0.00017843682,0.00015096182,0.9884855,0.000036869747,0.000022606446,0.0009761526,0.0011499826,0.007548912,0.00090757944,0.00037110454,0.0000738619,0.000098034405],"about_ca_topic_score_codex":0.96803916,"about_ca_topic_score_gemma":0.9996969,"teacher_disagreement_score":0.031657763,"about_ca_system_score_codex":0.000008008873,"about_ca_system_score_gemma":0.001249337,"threshold_uncertainty_score":0.605784},"labels":[],"label_agreement":null},{"id":"W2155708066","doi":"10.1139/e06-019","title":"Rocky shores and development of the Pliocene-Pleistocene Arroyo Blanco Basin on Isla Carmen in the Gulf of California, Mexico","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"American Chemical Society Petroleum Research Fund; Williams College","keywords":"Geology; Unconformity; Paleontology; Conglomerate; Structural basin; Pleistocene; Andesite; Early Pleistocene; Neogene; Geomorphology; Volcano; Volcanic rock","score_opus":0.020865015704598453,"score_gpt":0.22313241229292488,"score_spread":0.20226739658832643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155708066","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932099,0.00095767924,0.0000037111986,0.0011980243,0.00013229236,0.0000816999,0.000030896474,5.20865e-7,0.004385301],"genre_scores_gemma":[0.9995,0.0000134624215,0.000274674,0.00015344862,0.00002288053,2.6163963e-7,0.0000019932595,8.109227e-7,0.000032472224],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987164,0.00019249896,0.00034309216,0.00011231538,0.0003142943,0.00032136374],"domain_scores_gemma":[0.999237,0.00031588777,0.0001733804,0.000096603646,0.000061927916,0.00011520628],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015993173,0.00007976642,0.00018441727,0.00025320455,0.00032849697,0.000024740464,0.0005444763,0.000055224606,0.00019518331],"category_scores_gemma":[0.00011652007,0.000041821222,0.000034994402,0.00039129562,0.0010123744,0.00006830711,0.0000065622985,0.00019589593,0.0000061397263],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011585551,0.0000053911895,0.9970572,0.0000062497575,0.0000045202823,0.000017239061,0.0005432186,0.0016198958,0.000004996148,0.000062722684,0.00010879602,0.00055815774],"study_design_scores_gemma":[0.00014204187,0.0001452649,0.9963201,0.000039741808,0.000003587878,0.00009157757,0.00055951753,0.000117040545,0.00042037052,0.000526393,0.0015855927,0.000048759583],"about_ca_topic_score_codex":0.010575304,"about_ca_topic_score_gemma":0.7794899,"teacher_disagreement_score":0.7689145,"about_ca_system_score_codex":9.05615e-7,"about_ca_system_score_gemma":0.0013643737,"threshold_uncertainty_score":0.99601334},"labels":[],"label_agreement":null},{"id":"W2155721249","doi":"10.1139/e04-088","title":"Heat flow, thermal regime, and elastic thickness of the lithosphere in the Trans-Hudson Orogen","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Institut national des sciences de l'Univers; Conseil National de la Recherche Scientifique","keywords":"Geology; Lithosphere; Crust; Radiogenic nuclide; Archean; Basement; Heat flow; Petrology; Heat generation; Paleozoic; High heat; Geochemistry; Craton; Geophysics; Geomorphology; Tectonics; Thermal; Seismology; Mantle (geology)","score_opus":0.011806604109622401,"score_gpt":0.18278005961672747,"score_spread":0.17097345550710508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155721249","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98605776,0.002532028,0.0000072392363,0.00819855,0.000078310935,0.00004370554,0.000009477098,8.059347e-7,0.0030721151],"genre_scores_gemma":[0.9989817,0.000035783265,0.00035946557,0.0005177647,0.000067638844,1.05280016e-7,4.0717822e-7,5.363673e-7,0.000036574373],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990069,0.00012375857,0.00023907915,0.00010596153,0.00026842247,0.0002558608],"domain_scores_gemma":[0.9994445,0.00018171058,0.000056993962,0.00008056712,0.000045159617,0.0001911059],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00086114125,0.00007521999,0.00015004967,0.000056776364,0.00022142315,0.000059052287,0.0005420583,0.000039531922,0.0021762378],"category_scores_gemma":[0.000108727545,0.000031902302,0.0000801661,0.0005685066,0.0006706723,0.00016432849,0.0000037478333,0.00019101112,0.0000047889125],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005850979,0.000005335402,0.9721709,0.0000040993245,0.0000071602976,0.00000977344,0.0007929523,0.01836548,0.000085918706,0.00005758583,0.00003626216,0.008458718],"study_design_scores_gemma":[0.000111164525,0.00011669871,0.98986274,0.00003414384,0.000020162024,0.00009457535,0.0006915718,0.005422583,0.00022815238,0.00096937496,0.0023834002,0.00006542588],"about_ca_topic_score_codex":0.014186643,"about_ca_topic_score_gemma":0.5466503,"teacher_disagreement_score":0.5324636,"about_ca_system_score_codex":7.400902e-7,"about_ca_system_score_gemma":0.0002718799,"threshold_uncertainty_score":0.9987359},"labels":[],"label_agreement":null},{"id":"W2155783924","doi":"10.1139/e04-066","title":"The problematic fossil<i>Triplicatella</i>from the Early Cambrian of Greenland, Canada, and Siberia","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Vetenskapsrådet","keywords":"Laurentia; Gondwana; Paleontology; Geology; Genus; Ordovician; Taxonomy (biology); Ecology; Structural basin; Biology","score_opus":0.013586407121614739,"score_gpt":0.18901344914609647,"score_spread":0.17542704202448173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155783924","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97935355,0.012704234,0.000007728572,0.0036822308,0.00031857766,0.00009203983,0.000048702863,0.0000011201855,0.0037918119],"genre_scores_gemma":[0.9995131,0.00007471264,0.0002456543,0.000086358654,0.00006143432,1.8703692e-7,3.3061997e-7,4.9150776e-7,0.000017723063],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988543,0.000084878884,0.0003363941,0.00011715966,0.00027452732,0.00033278228],"domain_scores_gemma":[0.9987672,0.0003931328,0.00027859153,0.00012232343,0.00006857625,0.0003701934],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007957063,0.0000942438,0.00016800589,0.00005678815,0.00091538706,0.00014228032,0.00057656533,0.000037912316,0.000037955782],"category_scores_gemma":[0.00010618788,0.00004705695,0.00004849755,0.0002873703,0.0012833863,0.00018170859,0.0000012230064,0.00016579145,0.0000010693942],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000076039782,9.741423e-7,0.9866269,0.000002734928,0.00002026345,0.000026950649,0.00043437592,0.000113009235,0.000015749725,0.0003023535,0.000075156466,0.012373878],"study_design_scores_gemma":[0.00016298388,0.00016248965,0.99227685,0.000041179952,0.0000138782525,0.000089783156,0.00035521036,0.000026379774,0.000048838323,0.0061325524,0.0006251475,0.00006471996],"about_ca_topic_score_codex":0.9470935,"about_ca_topic_score_gemma":0.99965155,"teacher_disagreement_score":0.05255807,"about_ca_system_score_codex":0.0000015080744,"about_ca_system_score_gemma":0.0034091398,"threshold_uncertainty_score":0.70405096},"labels":[],"label_agreement":null},{"id":"W2155799428","doi":"10.1139/e05-064","title":"Mapping lithology in Canada's Arctic: application of hyperspectral data using the minimum noise fraction transformation and matched filtering","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":106,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"McMaster University","keywords":"Hyperspectral imaging; Geology; Remote sensing; Lithology; Geologic map; Arctic; Permafrost; Vegetation (pathology); Mineralogy; Geochemistry; Geomorphology","score_opus":0.03532831991893331,"score_gpt":0.2426109338348771,"score_spread":0.2072826139159438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155799428","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94113946,0.00020567965,0.05007252,0.008157656,0.000082300234,0.0000536856,0.0000024303777,0.0000012983742,0.00028495933],"genre_scores_gemma":[0.9867501,0.000008702477,0.013097416,0.000101753176,0.000037544865,3.15369e-7,4.762431e-7,5.015447e-7,0.0000031410775],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99930227,0.000034571753,0.00024874616,0.00011562923,0.0001228777,0.00017590515],"domain_scores_gemma":[0.9994516,0.000052241543,0.00018221678,0.00015333584,0.00006706329,0.00009357496],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00075361104,0.00004832903,0.00009628486,0.00011840175,0.00013937504,0.00005123539,0.00058920163,0.000020907313,0.000005986623],"category_scores_gemma":[0.000072721,0.000037422065,0.000010698011,0.00031702348,0.00011138148,0.0006230617,0.00002239993,0.00010766917,1.3454711e-7],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021455853,0.000039410592,0.5214487,0.00022259654,0.000049897968,0.00009467017,0.027159892,0.18202293,0.12214221,0.0054737595,0.00009289179,0.14123164],"study_design_scores_gemma":[0.0002508498,0.000042195767,0.20642228,0.000102117236,0.0000064324236,0.00075032306,0.005637473,0.7758815,0.0048545348,0.001116394,0.004785187,0.00015069128],"about_ca_topic_score_codex":0.40427125,"about_ca_topic_score_gemma":0.9002884,"teacher_disagreement_score":0.5938586,"about_ca_system_score_codex":0.000030903735,"about_ca_system_score_gemma":0.0014248329,"threshold_uncertainty_score":0.59969574},"labels":[],"label_agreement":null},{"id":"W2156095713","doi":"10.1139/e02-029","title":"Proterozoic evolution of the northeastern Canadian Shield: Lithoprobe Eastern Canadian Shield Onshore-Offshore Transect (ECSOOT), introduction and summary","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Government of Newfoundland and Labrador","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Transect; Shield; Geology; Submarine pipeline; Archean; Proterozoic; Craton; Accretion (finance); Oceanography; Paleontology; Tectonics","score_opus":0.024674352311078694,"score_gpt":0.18326062360005657,"score_spread":0.15858627128897787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156095713","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9760547,0.0030790363,0.000017936569,0.016161693,0.0009384455,0.00024878886,0.00006506222,0.0000030406554,0.0034312638],"genre_scores_gemma":[0.9989876,0.00008151137,0.00010055255,0.0002761556,0.0003332599,7.946238e-7,0.0000034818574,0.0000024179592,0.00021421403],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983981,0.00012208801,0.00036523133,0.00022806767,0.00030069659,0.00058581965],"domain_scores_gemma":[0.99848914,0.000038634425,0.00016894109,0.00013092106,0.00011581155,0.0010565253],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006748444,0.00014639425,0.00020947678,0.00039820097,0.0009132488,0.00014010245,0.00039327503,0.00009699185,0.0010475968],"category_scores_gemma":[0.00012965615,0.00009556549,0.00008063328,0.0006463903,0.0006191226,0.0004321842,0.0000048572583,0.00026753335,0.000018132007],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000050352164,0.00000247933,0.98623496,0.000008894402,0.00001120751,0.000015780943,0.00116426,0.0013569708,0.0000028924387,0.00007063657,0.00031444346,0.010812442],"study_design_scores_gemma":[0.00013735276,0.0004943038,0.97624075,0.000070019065,0.00002198701,0.00014271893,0.0018025257,0.0038552312,0.000011997655,0.00046781718,0.01658816,0.00016712767],"about_ca_topic_score_codex":0.9520875,"about_ca_topic_score_gemma":0.99983543,"teacher_disagreement_score":0.047747944,"about_ca_system_score_codex":0.000018892875,"about_ca_system_score_gemma":0.001162829,"threshold_uncertainty_score":0.9998656},"labels":[],"label_agreement":null},{"id":"W2156767567","doi":"10.1139/cjes-2014-0060","title":"Quantitative diagenetic analyses of<i>Edmontosaurus regalis</i>(Dinosauria: Hadrosauridae) postcranial elements from the Danek Bonebed, Upper Cretaceous Horseshoe Canyon Formation, Edmonton, Alberta, Canada: implications for allometric studies of fossil organisms","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Core Research for Evolutional Science and Technology","keywords":"Geology; Canyon; Paleontology; Diagenesis; Cretaceous; Horseshoe (symbol); Postcrania; Vertebrate; Taxon; Geomorphology; Biology","score_opus":0.05095981147568393,"score_gpt":0.2876454669592376,"score_spread":0.23668565548355366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156767567","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9739958,0.019687828,0.00047644202,0.0036696377,0.00066779467,0.00023569002,0.00084577606,0.000002181107,0.0004188551],"genre_scores_gemma":[0.9967297,0.00028759046,0.0024638108,0.000320035,0.000111322865,0.0000021907636,0.000046875717,0.000002779873,0.000035709058],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979006,0.00026988654,0.00084299536,0.00022957186,0.0002900103,0.0004669295],"domain_scores_gemma":[0.9960528,0.002005661,0.0008478667,0.0001954289,0.0005952861,0.00030295525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010116418,0.0001780916,0.000479121,0.00032988907,0.0007588773,0.0000357329,0.0007027559,0.00007990076,0.0001511792],"category_scores_gemma":[0.0018997062,0.00011811734,0.00012279776,0.00080700475,0.0010030004,0.00041167723,0.000009117758,0.0001290334,0.0000022292213],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058071822,0.000009622803,0.9917674,0.000014120951,0.00021332389,0.0000040233317,0.0010147515,0.0017427577,0.0008805763,0.0004719492,0.0024269356,0.001396443],"study_design_scores_gemma":[0.0003503327,0.00075490796,0.98996896,0.000035931942,0.00014790946,0.00005036528,0.0016049357,0.0007893516,0.00048377644,0.0017470596,0.0039187847,0.00014771298],"about_ca_topic_score_codex":0.78646964,"about_ca_topic_score_gemma":0.9985227,"teacher_disagreement_score":0.21205306,"about_ca_system_score_codex":0.000013772733,"about_ca_system_score_gemma":0.0026985286,"threshold_uncertainty_score":0.5836748},"labels":[],"label_agreement":null},{"id":"W2156855697","doi":"10.1139/e10-022","title":"Upper mantle thermochemical structure from seismic–geodynamic flow models: constraints from the Lithoprobe initiativeThis article is one of a series of papers published in this Special Issue on the theme <i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Mantle (geology); Geophysics; Mantle convection; Transition zone; Geodynamics; Geoid; Mantle plume; Craton; Seismic tomography; Lithosphere; Tectonics; Seismology","score_opus":0.009903632176611782,"score_gpt":0.1810299918179349,"score_spread":0.1711263596413231,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156855697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99204445,0.0003641916,0.000009026896,0.004189859,0.0003168969,0.0002099857,0.0009840039,0.0000012388873,0.0018803363],"genre_scores_gemma":[0.9986883,0.000038531434,0.00074970955,0.00025902517,0.00024423123,7.252219e-7,0.000006384113,0.0000024760889,0.000010654207],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986259,0.00018543882,0.00043256895,0.00017124075,0.00036157997,0.00022331641],"domain_scores_gemma":[0.99847317,0.0006237009,0.00043461306,0.00018114195,0.00017854302,0.00010882444],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00097207027,0.00012180401,0.00031991935,0.00006717,0.00016501537,0.00012325842,0.0005314239,0.00007487723,0.006599397],"category_scores_gemma":[0.00036199612,0.00005731948,0.000058676535,0.00031541425,0.002541243,0.00038642652,0.000014427132,0.0002745363,0.0000011354138],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003438249,0.00028507138,0.54090065,0.00033913882,0.0011903888,0.00005641687,0.1878112,0.014109503,0.18694752,0.035243142,0.0041960767,0.02548266],"study_design_scores_gemma":[0.0041435673,0.0010092108,0.51635975,0.0011672758,0.0003293174,0.000062945095,0.023499208,0.027953645,0.11669381,0.30451542,0.0034799997,0.00078584964],"about_ca_topic_score_codex":0.05239807,"about_ca_topic_score_gemma":0.13254872,"teacher_disagreement_score":0.26927227,"about_ca_system_score_codex":0.000002008618,"about_ca_system_score_gemma":0.00075982,"threshold_uncertainty_score":0.9943087},"labels":[],"label_agreement":null},{"id":"W2157074599","doi":"10.1139/e04-005","title":"Linearized quantities in transversely isotropic media","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Slowness; Transverse isotropy; Wavefront; Isotropy; Mathematical analysis; Phase velocity; Physics; Dimensionless quantity; Mathematics; Optics; Mechanics","score_opus":0.02811010272419587,"score_gpt":0.2151393214002727,"score_spread":0.18702921867607683,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157074599","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893294,0.0012500962,0.00027795337,0.002651014,0.00077696587,0.00004423309,0.000015097726,0.000010111813,0.0056451056],"genre_scores_gemma":[0.99397194,0.00009055161,0.0049275504,0.00089500507,0.00007422101,5.015177e-8,0.0000014123561,0.0000012366585,0.000038001126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99905485,0.000037566384,0.00025373016,0.000104904975,0.00023412125,0.00031482146],"domain_scores_gemma":[0.9994285,0.00006107623,0.00008901483,0.0000558185,0.000050669238,0.00031492146],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006001007,0.00007675735,0.00015110758,0.0005803173,0.00017404658,0.00010269749,0.00034230156,0.000039110862,0.00094599416],"category_scores_gemma":[0.00011747758,0.000059696627,0.00005750459,0.00046819926,0.0004964416,0.00047834087,0.00000121972,0.00017633263,0.000042121697],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029074727,0.000013585406,0.95309633,0.000015054707,0.000012964031,0.0005941299,0.005161136,0.013434192,0.0000725355,0.0017528008,0.0012039777,0.024614228],"study_design_scores_gemma":[0.002229813,0.0011560867,0.8742062,0.00044907568,0.0000223122,0.00052985153,0.0071777273,0.0051112194,0.0036019247,0.024492169,0.08043899,0.0005846544],"about_ca_topic_score_codex":0.11760452,"about_ca_topic_score_gemma":0.3112632,"teacher_disagreement_score":0.19365868,"about_ca_system_score_codex":0.000003141435,"about_ca_system_score_gemma":0.0015405262,"threshold_uncertainty_score":0.9999673},"labels":[],"label_agreement":null},{"id":"W2157353435","doi":"10.1139/cjes-2012-0185","title":"Dinosaur biostratigraphy of the Edmonton Group (Upper Cretaceous), Alberta, Canada: evidence for climate influence","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; Royal Tyrrell Museum","funders":"","keywords":"Geology; Macrofossil; Paleontology; Cretaceous; Biostratigraphy; Faunal assemblage; Assemblage (archaeology); Pangaea; Canyon; Fauna; Structural basin; Permian; Geomorphology; Ecology; Holocene","score_opus":0.019567762602125234,"score_gpt":0.21541410839596617,"score_spread":0.19584634579384094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157353435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9904247,0.0042419387,0.0000062977174,0.0032731795,0.0006953063,0.00017215162,0.000058677335,0.0000011538344,0.0011265762],"genre_scores_gemma":[0.99883795,0.00008572955,0.0003944131,0.0005751639,0.000060340157,9.748945e-7,0.000001536516,9.121406e-7,0.000043011147],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99866927,0.00010281192,0.00036489157,0.0001600455,0.00020532812,0.00049767084],"domain_scores_gemma":[0.99843794,0.00059624144,0.0003099772,0.00012302365,0.00018089908,0.0003519412],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005645886,0.00010684904,0.00019021782,0.00013307443,0.0005592432,0.000041556792,0.0007252599,0.00006918501,0.0005489176],"category_scores_gemma":[0.00048282338,0.000064560736,0.000100575606,0.0003612553,0.0010902934,0.0006086558,0.0000047068224,0.00013543866,0.000006834509],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007385592,0.0000014256847,0.99799746,0.0000094376555,0.000009444661,0.0000026632106,0.000059609076,0.0006032646,0.00008573536,0.00014951234,0.0005227141,0.00055135495],"study_design_scores_gemma":[0.00007747518,0.0002563656,0.9947082,0.00007299655,0.000011872442,0.00008841045,0.00013457301,0.00049750775,0.000060219474,0.00048646648,0.0035196915,0.000086255975],"about_ca_topic_score_codex":0.9202801,"about_ca_topic_score_gemma":0.9993959,"teacher_disagreement_score":0.07911578,"about_ca_system_score_codex":0.0000029747243,"about_ca_system_score_gemma":0.0027764286,"threshold_uncertainty_score":0.6010263},"labels":[],"label_agreement":null},{"id":"W2157450508","doi":"10.1139/e05-038","title":"Anatomy of the Early Cretaceous bird <i>Eoenantiornis buhleri</i> (Aves: Enantiornithes) from China","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Anatomy; Skull; Cretaceous; Geology; Paleontology; Articulation (sociology); Numerical digit; Biology; Mathematics","score_opus":0.01107487765607005,"score_gpt":0.20601671034610702,"score_spread":0.19494183269003698,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157450508","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98694474,0.0051049064,0.000021059286,0.0026133528,0.00082265446,0.000059275182,0.00010127211,0.000005515703,0.0043272385],"genre_scores_gemma":[0.99851435,0.000093043884,0.0008244288,0.00025448448,0.00021644059,1.0540198e-7,0.0000014073278,0.0000019739618,0.00009374362],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986069,0.00017214153,0.00038967773,0.00016954496,0.00023910213,0.0004226151],"domain_scores_gemma":[0.9989497,0.00013439504,0.0003516253,0.00014880908,0.00006818715,0.00034728154],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00062200363,0.000118804724,0.00023306855,0.0002104,0.0005310398,0.000043055603,0.00080735487,0.00009621812,0.0015121907],"category_scores_gemma":[0.00012283363,0.00007016856,0.00013467587,0.00046397673,0.0015214491,0.00040261608,0.0000063279526,0.00023749443,0.00008626106],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010273003,0.0000038023725,0.9935908,0.0000013370351,0.000017179145,0.00001719151,0.00029151895,0.00089773687,0.000049874718,0.00007984627,0.00012947911,0.0049109645],"study_design_scores_gemma":[0.00014938113,0.00018301596,0.97663677,0.000033292064,0.000017035629,0.00016163182,0.00011859503,0.000325447,0.00017605687,0.0007555286,0.021349385,0.00009387948],"about_ca_topic_score_codex":0.031109873,"about_ca_topic_score_gemma":0.64925694,"teacher_disagreement_score":0.6181471,"about_ca_system_score_codex":0.0000020324637,"about_ca_system_score_gemma":0.0011703172,"threshold_uncertainty_score":0.99940056},"labels":[],"label_agreement":null},{"id":"W2157637895","doi":"10.1139/e03-052","title":"Cycles and trends in the recent eruptive behaviour of Mount Etna (Italy)","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate variability and models","field":"Environmental Science","cited_by":116,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Flank; Mount; Volcano; Geology; Summit; Lateral eruption; Earth science; Seismology; Physical geography; Magma; Geography","score_opus":0.03791652300292799,"score_gpt":0.25888047192048025,"score_spread":0.22096394891755225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157637895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9894531,0.00017049148,0.000006191735,0.00084691227,0.00007362691,0.000033410422,0.000006212752,4.4618722e-7,0.009409648],"genre_scores_gemma":[0.99945825,0.000047899634,0.0003278042,0.0001314651,0.000005878642,4.399865e-7,1.4131531e-7,0.0000013126677,0.000026783298],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991935,0.00008958815,0.00020564682,0.00010181203,0.0002121671,0.00019730588],"domain_scores_gemma":[0.99959284,0.000055026037,0.00010097133,0.00007199538,0.000012173693,0.00016700877],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015120312,0.00005439315,0.00009602536,0.00013711253,0.00012775214,0.000041097264,0.00021989383,0.000024850646,0.0008116787],"category_scores_gemma":[0.000096996955,0.00003510354,0.000028615104,0.0004771414,0.00069917366,0.00022963186,0.000008841405,0.000096575975,0.00000214644],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004397471,0.000044253953,0.9778975,0.000002164449,0.0000034730065,0.000032672055,0.0062263156,0.004529796,0.0004886564,0.0036539016,0.00014120858,0.0069756266],"study_design_scores_gemma":[0.0001685847,0.00021309618,0.98922426,0.000015402253,0.000010243413,0.00008870147,0.0026973828,0.00020526683,0.00024285857,0.0024672723,0.004584888,0.0000820257],"about_ca_topic_score_codex":0.0071983184,"about_ca_topic_score_gemma":0.16754816,"teacher_disagreement_score":0.16034985,"about_ca_system_score_codex":0.000020066525,"about_ca_system_score_gemma":0.00011178361,"threshold_uncertainty_score":0.99941283},"labels":[],"label_agreement":null},{"id":"W2157728345","doi":"10.1139/e06-136","title":"Overburden geochemical signature of the Lac des Iles platinum group element deposit, northwestern Ontario, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Overburden; Biological dispersal; Geochemistry; Intrusion; Platinum group; Horizon; Placer mining; Geomorphology; Paleontology; Platinum","score_opus":0.010373318963280476,"score_gpt":0.18975358365051875,"score_spread":0.17938026468723828,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157728345","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99309045,0.0002697389,0.001380471,0.0008524269,0.00043554185,0.000053522424,0.0000035260093,0.0000024652531,0.003911855],"genre_scores_gemma":[0.9957655,0.0000010657566,0.0035887614,0.00025126923,0.000081845865,2.2933244e-7,3.682296e-7,9.563163e-7,0.00030997852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985803,0.000026790003,0.00034787282,0.00016301734,0.00044496177,0.0004370522],"domain_scores_gemma":[0.99887544,0.000093820236,0.00028392966,0.0001851614,0.00018983631,0.00037179055],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007616704,0.0001047748,0.00014597531,0.00006915766,0.00035188964,0.00008568902,0.0013262508,0.000053089912,0.00008695089],"category_scores_gemma":[0.00007664151,0.00007064906,0.000070312,0.00039074634,0.00035145582,0.00021834692,0.00006683637,0.0002600297,2.8198474e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004446912,0.000011461511,0.98770183,0.000020169029,0.000024353008,0.00020486211,0.002723281,0.0019272498,0.0031205742,0.00085325853,0.0012250071,0.002183481],"study_design_scores_gemma":[0.00033622314,0.00020651748,0.89085406,0.00026958503,0.000016903645,0.0005993018,0.0011549677,0.0006229932,0.052692853,0.0024223777,0.05051491,0.00030933612],"about_ca_topic_score_codex":0.93186814,"about_ca_topic_score_gemma":0.9996184,"teacher_disagreement_score":0.096847825,"about_ca_system_score_codex":0.00005466789,"about_ca_system_score_gemma":0.0035186838,"threshold_uncertainty_score":0.6241994},"labels":[],"label_agreement":null},{"id":"W2157927928","doi":"10.1139/cjes-2015-0038","title":"Geological setting of vertebrate microfossil localities across the Cretaceous–Paleogene boundary in southwestern Saskatchewan, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Geology; Paleontology; Cretaceous; Paleogene; Lithology; Vertebrate; Clastic rock; Sequence (biology); Archaeology; Geography; Sedimentary rock","score_opus":0.029973681319692795,"score_gpt":0.23255942428057144,"score_spread":0.20258574296087864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157927928","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97311234,0.021490568,0.000007871431,0.0020083932,0.0007024048,0.000052614476,0.00007342766,0.0000019523386,0.0025504085],"genre_scores_gemma":[0.9989316,0.000022715074,0.00014657572,0.0006076402,0.000072892864,1.6545324e-7,0.0000015924728,0.0000010720522,0.00021573203],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983673,0.00019783614,0.00043038928,0.0001390748,0.0003336527,0.00053176127],"domain_scores_gemma":[0.9988673,0.0002066337,0.00025022897,0.00009089035,0.00016773707,0.00041721298],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016898504,0.00011502174,0.00026273608,0.0000963814,0.0004651904,0.00008507378,0.0004969227,0.00005531263,0.00019293505],"category_scores_gemma":[0.00020524734,0.00007106818,0.000049371585,0.0003885503,0.0015251593,0.00018663089,0.000009312663,0.00022369258,0.0000057931884],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012148043,0.0000014655257,0.99094546,0.0000041295343,0.0000108937,0.00007954297,0.004081955,0.0028692824,0.0000014630637,0.00000204703,0.00048732432,0.0015042947],"study_design_scores_gemma":[0.00021573265,0.00013820328,0.9445725,0.000029352923,0.000006020526,0.00018435791,0.04237557,0.0005462164,0.000026222255,0.00014814278,0.011663302,0.00009437949],"about_ca_topic_score_codex":0.74862504,"about_ca_topic_score_gemma":0.9999675,"teacher_disagreement_score":0.25134248,"about_ca_system_score_codex":0.0000067383644,"about_ca_system_score_gemma":0.0075017847,"threshold_uncertainty_score":0.9981248},"labels":[],"label_agreement":null},{"id":"W2157950369","doi":"10.1139/e99-094","title":"A seismic-based cross-section of the Grenville Orogen in southern Ontario and western Quebec","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University; Polytechnique Montréal; Carleton University; Geological Survey of Canada","funders":"","keywords":"Geology; Laurentia; Orogeny; Seismology; Tectonics; Shear zone; Paleontology","score_opus":0.012818017420237545,"score_gpt":0.1846531523552305,"score_spread":0.17183513493499294,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157950369","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99754477,0.0003635186,9.824195e-7,0.00067899685,0.00006879355,0.000028383602,0.000012456287,7.0297517e-7,0.0013013713],"genre_scores_gemma":[0.9987153,0.000006075959,0.000049414353,0.0002388182,0.000026754295,5.7841625e-8,7.3815795e-7,4.6638658e-7,0.000962405],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99925894,0.000045690143,0.00022418016,0.00010488933,0.00016658744,0.00019969254],"domain_scores_gemma":[0.9995584,0.00004223121,0.00009748918,0.00005536606,0.000037508067,0.0002090377],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035927343,0.000061499384,0.00013046936,0.00009740272,0.0001552873,0.00006796424,0.00023949397,0.00003753499,0.009359513],"category_scores_gemma":[0.00003243484,0.000034000095,0.00005956789,0.0003849745,0.0005549572,0.0000849998,0.0000023404782,0.00012955235,0.0000126031],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006472803,0.0000026511275,0.9741904,0.000001251,0.000002848863,0.0000052773175,0.00032911662,0.022066455,0.000010007284,7.010802e-7,0.0000034751774,0.003381311],"study_design_scores_gemma":[0.00012305197,0.00008081139,0.9944259,0.000015451202,0.000005895893,0.000020409565,0.0001304173,0.00134777,0.000064888955,0.00038539397,0.0033509315,0.000049092916],"about_ca_topic_score_codex":0.9208373,"about_ca_topic_score_gemma":0.9993587,"teacher_disagreement_score":0.07852145,"about_ca_system_score_codex":0.000002561484,"about_ca_system_score_gemma":0.00088164175,"threshold_uncertainty_score":0.9915461},"labels":[],"label_agreement":null},{"id":"W2158171625","doi":"10.1139/e06-108","title":"Trace element constraints on mantle sources during mid-Proterozoic magmatism: evidence for a link between the Gardar (South Greenland) and Abitibi (Canadian Shield) mafic rocks","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Mantle plume; Mantle (geology); Geochemistry; Basalt; Primitive mantle; Trace element; Incompatible element; Mafic; Partial melting; Proterozoic; Petrology; Lithosphere; Paleontology; Tectonics","score_opus":0.03553364889908556,"score_gpt":0.23316356943593602,"score_spread":0.19762992053685047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158171625","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99199617,0.0014140875,0.00018219251,0.0052453536,0.00013359883,0.00019167029,0.00009183205,0.0000036239146,0.00074145145],"genre_scores_gemma":[0.99855363,0.000028198201,0.00059842324,0.00034985744,0.0003930492,5.217329e-7,0.0000031915727,0.0000018913452,0.000071239425],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998212,0.000060879862,0.000410646,0.00025996938,0.00033508588,0.00072145555],"domain_scores_gemma":[0.99793744,0.0005197687,0.00020855092,0.00010643713,0.00008191064,0.0011458924],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018189872,0.00015618431,0.00024640627,0.00031723653,0.0009052678,0.00022932069,0.0004965276,0.000073457835,0.0021474522],"category_scores_gemma":[0.00033882432,0.00009259133,0.00011486124,0.00035754062,0.0008023209,0.00019057271,0.0000065908353,0.00025611377,0.000023848681],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017959537,0.0000012159626,0.9701513,0.00001565093,0.000024059598,0.000045113473,0.0004152939,0.00057553704,0.00002637281,0.0000143220805,0.000027778651,0.028685376],"study_design_scores_gemma":[0.00020742357,0.00040143155,0.9949423,0.00014293526,0.00004198452,0.00006964563,0.0009048256,0.00024210413,0.00047704467,0.0014803037,0.0009282625,0.00016175772],"about_ca_topic_score_codex":0.08675704,"about_ca_topic_score_gemma":0.891259,"teacher_disagreement_score":0.80450195,"about_ca_system_score_codex":0.0000046425716,"about_ca_system_score_gemma":0.00041877135,"threshold_uncertainty_score":0.9987647},"labels":[],"label_agreement":null},{"id":"W2158251849","doi":"10.1139/cjes-2014-0168","title":"Dinosaur trackways from the Upper Cretaceous Oldman and Dinosaur Park formations (Belly River Group) of southern Alberta, Canada, reveal novel ichnofossil preservation style","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Royal Tyrrell Museum","funders":"","keywords":"Geology; Sedimentary depositional environment; Trace fossil; Carbonate; Paleontology; Cretaceous; Geochemistry; Siderite; Clastic rock; Groundwater; Sedimentary rock; Calcite; Structural basin","score_opus":0.024736824814096434,"score_gpt":0.19878386404285558,"score_spread":0.17404703922875914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158251849","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9907415,0.0028063396,0.00007522861,0.002770384,0.0003920733,0.00007964352,0.00042251495,0.0000018110317,0.0027105045],"genre_scores_gemma":[0.9987316,0.000016071352,0.00057128613,0.00034491825,0.000113675436,2.877018e-7,0.00002547016,0.0000012309262,0.00019546419],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883443,0.00010580257,0.00033770787,0.00014080729,0.0002567919,0.0003244457],"domain_scores_gemma":[0.9986845,0.00036314531,0.00027744132,0.00010715036,0.00013181352,0.00043592256],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006673068,0.00010439721,0.00017838436,0.00009293903,0.00049185,0.000044029006,0.00044141765,0.000075655626,0.00022386046],"category_scores_gemma":[0.00028693693,0.000067189576,0.000039571434,0.00022245149,0.0008881983,0.000520652,0.000006662377,0.00016769777,0.000008184487],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014516812,0.000003597916,0.9954488,0.000002017632,0.000017322483,0.000006549264,0.0015655262,0.00071694504,0.000011208856,0.00010975534,0.0013515998,0.00075210433],"study_design_scores_gemma":[0.00023264367,0.00016335526,0.98306113,0.000020270842,0.000019632984,0.00008567338,0.0017706862,0.0022962946,0.000005754663,0.0007922937,0.011462465,0.00008978824],"about_ca_topic_score_codex":0.922384,"about_ca_topic_score_gemma":0.99913347,"teacher_disagreement_score":0.07674944,"about_ca_system_score_codex":0.000004766519,"about_ca_system_score_gemma":0.0017618125,"threshold_uncertainty_score":0.37829626},"labels":[],"label_agreement":null},{"id":"W2158294981","doi":"10.1139/e08-066","title":"The Hamilton Bar Fauna: evidence for a Hypsithermal age","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Pleistocene-Era Hominins and Archaeology","field":"Social Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; University of Waterloo","funders":"McMaster University; Ministry of Natural Resources","keywords":"Fauna; Glacial period; Geology; Radiocarbon dating; Holocene climatic optimum; Paleontology; Fish <Actinopterygii>; Ecology; Holocene; Biology; Fishery","score_opus":0.09947997764633788,"score_gpt":0.32011383011006284,"score_spread":0.22063385246372497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158294981","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98778427,0.002140958,0.00010506986,0.00547934,0.0008498165,0.00012813114,0.0000043679242,0.0000036792896,0.0035043508],"genre_scores_gemma":[0.99639744,0.0005159654,0.0010749202,0.0004001105,0.0004304286,0.0000027530823,8.261832e-8,0.000003386245,0.0011749452],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99858326,0.00014869272,0.0002470569,0.00012363025,0.00031749625,0.00057984533],"domain_scores_gemma":[0.99831903,0.00068757625,0.00018251078,0.00008512601,0.00017663739,0.0005491176],"candidate_categories":["sts"],"consensus_categories":["sts"],"category_scores_codex":[0.0022724855,0.00007251427,0.0001409446,0.00012860412,0.0040962677,0.000108662636,0.0008293744,0.000046734338,0.000057228488],"category_scores_gemma":[0.0011227973,0.000048208527,0.000104830295,0.00029668424,0.0042112586,0.00040163225,0.000009820412,0.00012627739,0.000006970871],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057574158,0.000015004284,0.8819195,0.0000067824394,0.000035189947,0.0007231123,0.058660217,0.000263255,0.00032483664,0.044286046,0.0055162627,0.008192222],"study_design_scores_gemma":[0.0003085735,0.00054794,0.5544106,0.000087395754,0.000012503304,0.00020480632,0.005098331,0.000076383796,0.00017266232,0.0030974536,0.43578938,0.0001939883],"about_ca_topic_score_codex":0.003222772,"about_ca_topic_score_gemma":0.6390475,"teacher_disagreement_score":0.63582474,"about_ca_system_score_codex":0.000016954422,"about_ca_system_score_gemma":0.004548466,"threshold_uncertainty_score":0.99849874},"labels":[],"label_agreement":null},{"id":"W2158337840","doi":"10.1139/e11-065","title":"Mafic and ultrapotassic rocks from the Canyon domain (central Grenville Province): geochemistry and tectonic implications","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mafic; Geology; Geochemistry; Orogeny; Metamorphism; Petrogenesis; Magmatism; Continental arc; Petrology; Archean; Incompatible element; Basalt; Partial melting; Tectonics; Volcanic rock; Paleontology","score_opus":0.010641542048716575,"score_gpt":0.17980424763629957,"score_spread":0.169162705587583,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158337840","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9862218,0.0084696775,0.000012429961,0.003422234,0.00007889132,0.000040273997,0.00007944753,0.0000019549254,0.0016733006],"genre_scores_gemma":[0.9991015,0.00008871507,0.00031788,0.0003005757,0.00015831462,2.075704e-7,0.0000063431153,7.390527e-7,0.000025688567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990633,0.000040285813,0.0001794248,0.00013575553,0.00013911707,0.000442097],"domain_scores_gemma":[0.9988593,0.00016523706,0.00010950422,0.00007801939,0.00002986078,0.00075810635],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034462506,0.00008934991,0.00012887317,0.00004547733,0.0005108511,0.0001194223,0.0002533999,0.000041819643,0.0021088657],"category_scores_gemma":[0.00008920188,0.00004906338,0.00004462365,0.00022942173,0.00069183833,0.00016674805,0.000007154514,0.00016196856,0.0000066436805],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000017044613,0.000002389934,0.99543136,0.0000013557296,0.0000095228515,0.000002744282,0.00011727688,0.00004756371,0.00025464979,0.00003210319,0.00009513245,0.004004175],"study_design_scores_gemma":[0.000069304515,0.000043464162,0.99097025,0.000010286401,0.00002167117,0.00009395826,0.00039696117,0.00011672741,0.00020092199,0.0041188006,0.003876948,0.00008067645],"about_ca_topic_score_codex":0.04750391,"about_ca_topic_score_gemma":0.41788822,"teacher_disagreement_score":0.37038434,"about_ca_system_score_codex":0.0000016634388,"about_ca_system_score_gemma":0.0003141099,"threshold_uncertainty_score":0.9988033},"labels":[],"label_agreement":null},{"id":"W2158372422","doi":"10.1139/e05-077","title":"Mineral chemistry, petrogenesis, and tectonic setting of the Wateranga layered intrusion, southeast Queensland, Australia","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Gabbro; Layered intrusion; Olivine; Fractional crystallization (geology); Mafic; Norite; Anorthosite; Plagioclase; Magma chamber; Petrogenesis; Magma; Petrography; Pyroxene; Basalt; Petrology; Quartz","score_opus":0.013610713304994413,"score_gpt":0.19540899993759736,"score_spread":0.18179828663260295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158372422","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958249,0.0006531353,0.0000016755931,0.0028019112,0.000064641106,0.000024251738,0.000026090382,0.0000013150525,0.0006021232],"genre_scores_gemma":[0.99917954,0.000009153162,0.0004308413,0.00007740005,0.000118618686,5.82772e-8,0.0000015672805,6.606221e-7,0.0001821539],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99907607,0.00004227675,0.0002685352,0.000120129,0.00020994416,0.00028306546],"domain_scores_gemma":[0.9993147,0.00004370986,0.00016370341,0.00006852226,0.000075664844,0.00033370385],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000440193,0.00008461986,0.000163864,0.000060919414,0.0002486681,0.000057331406,0.00032650106,0.00003887919,0.0033521175],"category_scores_gemma":[0.00010036236,0.000043706546,0.00009153795,0.00033036375,0.0004314344,0.0000844713,0.000008847068,0.00012313706,0.000008663835],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000033177341,0.0000018871073,0.994867,0.0000046553796,0.0000082589095,0.0000032907599,0.00009838249,0.0019478665,0.0012738683,0.0000053483673,0.000028704917,0.0017573978],"study_design_scores_gemma":[0.00011963723,0.000048877515,0.993125,0.000024160196,0.000017120543,0.00012069778,0.00023052808,0.0011935867,0.0032985471,0.00041026232,0.0013294914,0.00008209348],"about_ca_topic_score_codex":0.019954158,"about_ca_topic_score_gemma":0.40194824,"teacher_disagreement_score":0.38199407,"about_ca_system_score_codex":9.3922375e-7,"about_ca_system_score_gemma":0.00019593938,"threshold_uncertainty_score":0.99755895},"labels":[],"label_agreement":null},{"id":"W2158642524","doi":"10.1139/cjes-2014-0182","title":"Quaternary stratigraphy and evidence for multiple glacial episodes in the north Okanagan Valley, British Columbia","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ministry of Forests; Geoscience BC; Penn West Exploration (Canada); University of British Columbia, Okanagan Campus","funders":"Natural Sciences and Engineering Research Council of Canada; Ministry of Environment","keywords":"Geology; Quaternary; Bedrock; Glacial period; Interglacial; Pleistocene; Alluvium; Paleontology; Stratigraphy; Geochemistry; Geomorphology; Stratigraphic unit; Sedimentary rock; Tectonics","score_opus":0.08253322207637476,"score_gpt":0.27306022336966,"score_spread":0.19052700129328526,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158642524","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933785,0.0047076335,0.000011542676,0.0009425168,0.00024958726,0.00015233642,0.000018225823,0.000001522541,0.0005381446],"genre_scores_gemma":[0.9989494,0.000089459565,0.00061021297,0.00023225052,0.00007523377,8.4204777e-7,0.0000021025483,8.4836165e-7,0.000039667233],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99874836,0.00022182902,0.00023383014,0.00015494533,0.00023158918,0.00040941592],"domain_scores_gemma":[0.9986258,0.00068163156,0.0000994314,0.00006679818,0.00010829491,0.0004180437],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022979418,0.0000594423,0.00015283375,0.00014811134,0.0004563585,0.00042355002,0.0005159852,0.000052290015,0.000107133106],"category_scores_gemma":[0.0007457386,0.000053831016,0.000042926913,0.00037030602,0.0010386826,0.00045090876,0.0000037081857,0.00019352701,0.000004618846],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013428789,0.0000022410563,0.9979184,0.0000069437697,0.0000044957033,0.0001626364,0.0004430956,0.00021598389,1.3794657e-7,0.000009116768,0.00031270698,0.00091080007],"study_design_scores_gemma":[0.00027019207,0.0005073038,0.99393886,0.000045802815,0.000005251155,0.0006033028,0.00092484336,0.0010149847,4.3170698e-7,0.0021412938,0.00047879634,0.00006892954],"about_ca_topic_score_codex":0.2501692,"about_ca_topic_score_gemma":0.99914855,"teacher_disagreement_score":0.7489794,"about_ca_system_score_codex":3.440088e-7,"about_ca_system_score_gemma":0.0011753187,"threshold_uncertainty_score":0.754824},"labels":[],"label_agreement":null},{"id":"W2158973468","doi":"10.1139/cjes-2014-0010","title":"Neoarchean continental crust formation and Paleoproterozoic deformation of the central Rae craton, Committee Bay belt, Nunavut","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Nunavut Research Institute; Government of Nunavut; Geological Survey of Canada","funders":"","keywords":"Geology; Geochemistry; Craton; Metamorphism; Greenstone belt; Plutonism; Metamorphic facies; Mafic; Diorite; Orogeny; Geochronology; Continental crust; Archean; Crust; Ultramafic rock; Pluton; Paleontology; Zircon; Facies; Tectonics","score_opus":0.010693683438893287,"score_gpt":0.1761466774710581,"score_spread":0.16545299403216482,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158973468","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99613273,0.00026065024,0.00007575233,0.0018133244,0.00013905994,0.00005605851,0.000012988721,0.0000015632069,0.0015078954],"genre_scores_gemma":[0.9993771,0.000010334218,0.0002510603,0.00028541315,0.000054983117,9.563784e-8,0.000004598984,4.866538e-7,0.000015941874],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99903744,0.0000692322,0.00031187703,0.00007655037,0.00023709386,0.0002678114],"domain_scores_gemma":[0.9992293,0.0000569579,0.0002458944,0.00006269295,0.000082971485,0.00032217993],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00062398426,0.000072345276,0.00014766712,0.00009912475,0.00033475133,0.000079633326,0.0002911922,0.000034198903,0.0006631026],"category_scores_gemma":[0.0001293759,0.00003910616,0.00007592339,0.0002946299,0.0005892324,0.00039027364,0.0000069991206,0.00012221413,0.000005025208],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000035050864,0.000002023441,0.9919199,0.000006883091,0.0000039031443,7.4520085e-7,0.00024369435,0.0005158196,0.000070239665,0.00008359227,0.00003831563,0.0071113836],"study_design_scores_gemma":[0.00013603723,0.00013565454,0.9866388,0.00002703863,0.00001246664,0.000045395514,0.00031177537,0.008220058,0.00072727364,0.0028248338,0.0008635028,0.000057154863],"about_ca_topic_score_codex":0.01207237,"about_ca_topic_score_gemma":0.6238536,"teacher_disagreement_score":0.6117813,"about_ca_system_score_codex":0.0000011828719,"about_ca_system_score_gemma":0.00012705525,"threshold_uncertainty_score":0.9945063},"labels":[],"label_agreement":null},{"id":"W2159774630","doi":"10.1139/e10-086","title":"The evolutionary significance of a Lower Cambrian trace-fossil assemblage from the Meguma terrane, Nova Scotia","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University; University of Alberta","funders":"","keywords":"Trace fossil; Geology; Paleontology; Assemblage (archaeology); Tetrapod (structure)","score_opus":0.02068583479017823,"score_gpt":0.2150809541310413,"score_spread":0.19439511934086307,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159774630","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9853297,0.0037724227,0.000026469326,0.0034801909,0.0014126826,0.00007908178,0.00008741892,0.0000024631938,0.005809603],"genre_scores_gemma":[0.998773,0.000030154302,0.00078458793,0.00012170982,0.00018516197,1.3398801e-7,0.0000014789247,0.0000010206903,0.000102761944],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99879766,0.00007538327,0.0003491994,0.00011340457,0.00034418362,0.00032014737],"domain_scores_gemma":[0.99847865,0.0006185333,0.00027454327,0.00014623805,0.00018246085,0.00029958843],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011380719,0.00009192523,0.00013159345,0.000075944976,0.0008636752,0.00022273613,0.00090831146,0.0000541018,0.0027569553],"category_scores_gemma":[0.00042563968,0.000043256885,0.000077134035,0.00048141705,0.0013366512,0.0004584164,0.000004646426,0.00030579168,0.000051490482],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027726881,0.000009385275,0.9764932,0.0000051344095,0.000021536534,0.000031690997,0.0005504364,0.0014590458,0.0003499653,0.0009385545,0.0021404324,0.017972924],"study_design_scores_gemma":[0.0000747837,0.0001926845,0.95370394,0.000020125046,0.000009039529,0.00007392711,0.00061334885,0.0006747335,0.000090462454,0.001994743,0.042477056,0.00007513833],"about_ca_topic_score_codex":0.06665839,"about_ca_topic_score_gemma":0.8556502,"teacher_disagreement_score":0.7889918,"about_ca_system_score_codex":8.720859e-7,"about_ca_system_score_gemma":0.0014088775,"threshold_uncertainty_score":0.99815464},"labels":[],"label_agreement":null},{"id":"W2160073758","doi":"10.1139/e06-117","title":"Further refinement to the timing of Mesoproterozoic magmatism, Lake Nipigon region, Ontario","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":103,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Magmatism; Mafic; Rift; Geology; Geochemistry; Flood basalt; Basalt; Ultramafic rock; Precambrian; Earth science; Paleontology; Volcanism; Tectonics","score_opus":0.02807146760485609,"score_gpt":0.20541578381976253,"score_spread":0.17734431621490643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160073758","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9850985,0.00039852379,0.00021256403,0.005642885,0.00020536732,0.00006795158,0.0000059850927,0.000001719941,0.0083665205],"genre_scores_gemma":[0.9970101,0.000004238009,0.0015980719,0.00081672875,0.00008714927,1.0721741e-7,0.0000014302676,7.4279797e-7,0.00048143804],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987536,0.000035314235,0.00037577003,0.00012965604,0.0003371792,0.00036848674],"domain_scores_gemma":[0.99899334,0.00008726927,0.00019817398,0.00010412531,0.00012215793,0.0004949478],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014016327,0.00008573624,0.00017163283,0.00020424515,0.00022944543,0.00005498268,0.00049610186,0.000032373217,0.010253301],"category_scores_gemma":[0.00011556192,0.000045293345,0.00009292855,0.00057858607,0.00027958333,0.00011201782,0.000007020851,0.00014699766,0.000048467587],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010588976,0.0000039048823,0.9824383,0.0000027043445,0.000014788038,0.000048958856,0.0009874338,0.0021244008,0.000030855153,0.000047427468,0.00055543776,0.013735195],"study_design_scores_gemma":[0.0000669267,0.00027397458,0.9607792,0.000032240667,0.000016271,0.000057983027,0.0003933495,0.00009299561,0.00028873328,0.0014192389,0.03650033,0.00007876793],"about_ca_topic_score_codex":0.24976385,"about_ca_topic_score_gemma":0.9969488,"teacher_disagreement_score":0.74718493,"about_ca_system_score_codex":0.00000247045,"about_ca_system_score_gemma":0.00039551457,"threshold_uncertainty_score":0.9906515},"labels":[],"label_agreement":null},{"id":"W2160074718","doi":"10.1139/cjes-2013-0051","title":"Variation and taxonomy of Asiamerican eutherian mammal<i>Paranyctoides</i>","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"University of California Museum of Paleontology; Russian Foundation for Basic Research","keywords":"Autapomorphy; Synapomorphy; Monophyly; Taxon; Sister group; Cladistics; Taxonomy (biology); Biology; Zoology; Clade; Paleontology; Phylogenetic tree","score_opus":0.027120354908017855,"score_gpt":0.2002293691605603,"score_spread":0.17310901425254244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160074718","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9727837,0.0023358515,0.00010187047,0.0012731778,0.00033786733,0.00009705804,0.000013352845,0.000002328626,0.023054838],"genre_scores_gemma":[0.99700415,0.000053710253,0.0025694207,0.00021569469,0.000054741573,3.4838695e-7,4.839915e-7,6.9565743e-7,0.00010076067],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992624,0.00006345355,0.00024135421,0.000092006405,0.00012469561,0.00021609924],"domain_scores_gemma":[0.9992178,0.00008891956,0.00023055541,0.00004465826,0.000106699445,0.00031138686],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041336843,0.00006663999,0.0001618015,0.00019859395,0.00023655887,0.00005626983,0.00016778494,0.000029141394,0.0015253699],"category_scores_gemma":[0.00008184879,0.000049555718,0.00003235396,0.00026014665,0.0008021893,0.00034873057,0.0000019058218,0.000074415344,0.000025806969],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000017823716,0.0000011507914,0.99287426,0.0000026899284,0.000010350216,0.0000035864318,0.00035799984,0.00016264316,0.000024960907,0.0001107669,0.00017281578,0.0062770015],"study_design_scores_gemma":[0.000096864256,0.00018501052,0.99111295,0.000012850966,0.0000069105336,0.000062538995,0.00066844915,0.0004008136,0.000011695012,0.0003512638,0.007032521,0.000058113154],"about_ca_topic_score_codex":0.058466494,"about_ca_topic_score_gemma":0.5132626,"teacher_disagreement_score":0.45479614,"about_ca_system_score_codex":7.0362285e-7,"about_ca_system_score_gemma":0.00042446767,"threshold_uncertainty_score":0.9993874},"labels":[],"label_agreement":null},{"id":"W2160356530","doi":"10.1139/e07-019","title":"Glacier fluctuations during the past millennium in Garibaldi Provincial Park, southern Coast Mountains, British Columbia","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Glacier; Moraine; Geology; Little ice age; Radiocarbon dating; Glacier morphology; Holocene; Chronology; Physical geography; Ice sheet; Dendrochronology; Northern Hemisphere; Climatology; Archaeology; Geography; Paleontology; Oceanography; Cryosphere; Ice stream; Sea ice","score_opus":0.011713264102914477,"score_gpt":0.21279029230617597,"score_spread":0.20107702820326148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160356530","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953305,0.0011453069,0.000008247305,0.00061995693,0.00041648504,0.00012308118,0.00005105723,0.0000029974883,0.002302347],"genre_scores_gemma":[0.99872154,0.00003225703,0.00011193257,0.00017382416,0.0001829602,3.4553386e-7,0.0000038340486,0.0000017857516,0.0007715315],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982429,0.00015230196,0.00036429235,0.00017274526,0.0003178341,0.0007499055],"domain_scores_gemma":[0.99898046,0.0002217252,0.00013918288,0.0000932233,0.00012359663,0.00044182673],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0027160372,0.00007625496,0.00016313692,0.00022623203,0.0012278088,0.00035517296,0.0005638222,0.00009472248,0.0018931675],"category_scores_gemma":[0.00022547736,0.0000718528,0.000058322577,0.00063326187,0.0013138644,0.00025030528,0.0000080335785,0.00043480252,0.00006394223],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008278652,0.000003654652,0.9980612,0.0000044833237,0.0000056044896,0.00036447644,0.0005554784,0.00034344438,0.0000029936566,0.000004646063,0.00014006165,0.00050570455],"study_design_scores_gemma":[0.0002214901,0.0000945887,0.9938587,0.000024720592,0.0000045201673,0.0009920332,0.0026210428,0.000110779554,0.0000023360362,0.00015820199,0.0018232524,0.000088335495],"about_ca_topic_score_codex":0.2764639,"about_ca_topic_score_gemma":0.99937665,"teacher_disagreement_score":0.7229127,"about_ca_system_score_codex":0.0000018687807,"about_ca_system_score_gemma":0.001390694,"threshold_uncertainty_score":0.99901927},"labels":[],"label_agreement":null},{"id":"W2160448013","doi":"10.1139/e02-026","title":"The Ketilidian orogen of South Greenland: geochronology, tectonics, magmatism, and fore-arc accretion during Palaeoproterozoic oblique convergence","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":144,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Transpression; Batholith; Geochemistry; Craton; Metamorphism; Sinistral and dextral; Geochronology; Archean; Shear zone; Orogeny; Foreland basin; Subduction; Paleontology; Tectonics","score_opus":0.014471132963497153,"score_gpt":0.18007772542944514,"score_spread":0.165606592465948,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160448013","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932486,0.004411892,0.000013970147,0.0015000004,0.000112877286,0.0000655826,0.000023861732,0.000002882681,0.00062037323],"genre_scores_gemma":[0.9991558,0.00037298675,0.000299211,0.000068606554,0.000042908763,3.0578585e-7,0.0000013075186,9.908728e-7,0.000057866917],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99880105,0.000082534294,0.00034402264,0.00016398246,0.00021549204,0.0003929436],"domain_scores_gemma":[0.99899966,0.0001265733,0.00025360956,0.00009904911,0.00010285637,0.0004182307],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006156182,0.00010307371,0.0001980592,0.00015603,0.000517941,0.000083721025,0.0004125647,0.000060864822,0.003887813],"category_scores_gemma":[0.00023496868,0.000059204223,0.00008028254,0.000388336,0.0011849474,0.00019337259,0.000010964903,0.0001748622,0.00002277328],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005799933,0.000001768228,0.99325526,0.000008467275,0.000015343623,0.000019466846,0.00023746715,0.00026387602,0.00009724937,0.00006088294,0.000013388627,0.0060210587],"study_design_scores_gemma":[0.00014094045,0.0002303605,0.9901429,0.00002819539,0.000017219229,0.00012137892,0.00038443776,0.0036313774,0.00076799485,0.003997013,0.0004401433,0.000098029515],"about_ca_topic_score_codex":0.013538721,"about_ca_topic_score_gemma":0.41434768,"teacher_disagreement_score":0.40080896,"about_ca_system_score_codex":0.0000015123949,"about_ca_system_score_gemma":0.00014551064,"threshold_uncertainty_score":0.99702275},"labels":[],"label_agreement":null},{"id":"W2160519692","doi":"10.1139/cjes-2015-0040","title":"R.A. Daly’s early model of seafloor generation 40 years before the Vine–Matthews hypothesis: an outstanding theoretical achievement inspired by field work on St. Helena in 1921–1922","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Continental drift; Geology; Seafloor spreading; Lithosphere; Plate tectonics; Continental crust; Crust; Paleontology; Geophysics; Tectonics","score_opus":0.04588294179241281,"score_gpt":0.21334333739824243,"score_spread":0.16746039560582962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160519692","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99541354,0.00022215738,0.000078439785,0.0032827395,0.00011557514,0.00006430687,0.000037451122,0.0000022389313,0.0007835423],"genre_scores_gemma":[0.99869466,0.000007494405,0.0004936462,0.00066051487,0.00009482981,4.2008807e-7,0.000005282753,0.0000014529276,0.000041712447],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985923,0.00012429115,0.00034780355,0.00017241822,0.0004370045,0.00032618074],"domain_scores_gemma":[0.9990768,0.00009714233,0.0001502995,0.00011688756,0.0000638627,0.00049503334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001258512,0.00010452165,0.00020502569,0.00017121456,0.00013759533,0.00010471503,0.0004901555,0.00005927587,0.0006308151],"category_scores_gemma":[0.00024702537,0.000058702422,0.000074952244,0.0004866535,0.00042128685,0.00021824312,0.0000071167383,0.00019367044,0.000009831199],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008521606,0.00003866945,0.880573,0.0000032314952,0.000024072477,0.000022397284,0.0016751614,0.10069037,0.00012587594,0.001427392,0.0004284823,0.014906165],"study_design_scores_gemma":[0.0010463209,0.0054263915,0.680019,0.0001659664,0.00009439703,0.00001974729,0.0038206512,0.21524504,0.0023300904,0.09049604,0.0007774498,0.00055887434],"about_ca_topic_score_codex":0.0065091727,"about_ca_topic_score_gemma":0.17107937,"teacher_disagreement_score":0.20055394,"about_ca_system_score_codex":0.0000045146953,"about_ca_system_score_gemma":0.00028987302,"threshold_uncertainty_score":0.9839965},"labels":[],"label_agreement":null},{"id":"W2160553249","doi":"10.1139/e10-104","title":"Buried bedrock valleys and glacial and subglacial meltwater erosion in southern Ontario, Canada","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Bedrock; Geology; Glacial period; Meltwater; Geomorphology; Paleontology","score_opus":0.011792034627185076,"score_gpt":0.17368320760528172,"score_spread":0.16189117297809663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160553249","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99439144,0.00009203292,0.0000019479469,0.00017794363,0.00021431374,0.00004008649,0.0000019237684,8.390103e-7,0.0050794827],"genre_scores_gemma":[0.99914503,0.000008826519,0.00020419438,0.00012710382,0.000031816755,2.2178456e-7,1.5962726e-7,0.0000028724744,0.00047979207],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99915886,0.00002566827,0.00018912526,0.00013774954,0.0002059555,0.0002826563],"domain_scores_gemma":[0.9994171,0.000009943374,0.00007592822,0.000042286618,0.000009909842,0.00044479105],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003678752,0.00007942474,0.00011855535,0.000073334646,0.00022868265,0.00005425581,0.00015347879,0.000048686725,0.0019723598],"category_scores_gemma":[0.000016387277,0.000054115884,0.00001721637,0.00012625344,0.0003556547,0.00021229271,0.00002547795,0.00015234145,0.000004828132],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011903265,0.000002950334,0.99183905,9.340201e-7,0.0000028155198,0.00010585723,0.006801506,0.000030865085,0.00011444199,0.000011707689,0.00016671255,0.00091122766],"study_design_scores_gemma":[0.0003217185,0.0001323018,0.99339217,0.000023475506,0.000007959898,0.00010912022,0.0008777874,0.000052858162,0.00015033994,0.0004175727,0.0043969085,0.000117778436],"about_ca_topic_score_codex":0.99306667,"about_ca_topic_score_gemma":0.99994123,"teacher_disagreement_score":0.0068745525,"about_ca_system_score_codex":0.000040079227,"about_ca_system_score_gemma":0.0008832637,"threshold_uncertainty_score":0.99894},"labels":[],"label_agreement":null},{"id":"W2160772685","doi":"10.1139/e05-108","title":"Reservoir-induced earthquakes at Sainte-Marguerite-3, Quebec, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Collège de Maisonneuve; Hydro-Québec; Natural Resources Canada","funders":"Natural Resources Canada; Hydro-Québec","keywords":"Geology; Seismometer; Seismology; Magnitude (astronomy); Induced seismicity; Seismic zone","score_opus":0.020022620956771715,"score_gpt":0.20127193416369493,"score_spread":0.18124931320692322,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160772685","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96346086,0.0037699025,0.0000022166655,0.0024193586,0.0011002674,0.00007771408,0.000050752744,0.000007607441,0.029111302],"genre_scores_gemma":[0.99594194,0.000023968656,0.00020589992,0.0004083435,0.00034818414,2.0525778e-7,0.000008349267,0.0000038058981,0.00305929],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99766815,0.00010219805,0.0005073397,0.0002569515,0.0006478953,0.00081748614],"domain_scores_gemma":[0.99844337,0.00026651303,0.00027586904,0.00016550724,0.00019546723,0.0006532507],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007453306,0.0001988338,0.00031730466,0.00031203585,0.0010530562,0.00020177849,0.00058293453,0.000063098196,0.003663952],"category_scores_gemma":[0.00020711553,0.00015292114,0.00011226877,0.00064706133,0.00046669526,0.00040095998,0.000010837132,0.0002325123,0.000073506635],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012836193,0.000003696159,0.9780636,0.000007043221,0.000022289281,0.00044033775,0.00010710512,0.0023122688,0.000044766213,0.00017875877,0.014479772,0.0043275184],"study_design_scores_gemma":[0.00020180235,0.0001521266,0.8845349,0.00003943914,0.000010817418,0.00013098458,0.00034971008,0.00014230417,0.0003081245,0.00027391038,0.11365322,0.00020267793],"about_ca_topic_score_codex":0.9952846,"about_ca_topic_score_gemma":0.9999932,"teacher_disagreement_score":0.09917345,"about_ca_system_score_codex":0.000018220533,"about_ca_system_score_gemma":0.0055222446,"threshold_uncertainty_score":0.99724686},"labels":[],"label_agreement":null},{"id":"W2161015798","doi":"10.1139/e10-059","title":"Taphonomy, pathology, and paleoecology of the terminal Pleistocene Marmes Rockshelter (45FR50) “big elk” (<i>Cervus elaphus</i>), southeastern Washington State, USA","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Wildlife Ecology and Conservation","field":"Environmental Science","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Taphonomy; Pleistocene; Geology; Archaeology; Holocene; Radiocarbon dating; Cervus elaphus; Antler; Cervus; Paleoecology; Paleontology; Geography; Ecology; Biology","score_opus":0.00939210761618874,"score_gpt":0.19948963304582706,"score_spread":0.19009752542963831,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161015798","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960972,0.00004200242,0.000017774206,0.0013372805,0.001014179,0.00009185485,0.000009986285,0.0000016247816,0.001388063],"genre_scores_gemma":[0.998134,0.0000059682993,0.000471036,0.0007702642,0.000065342814,0.0000017041589,2.179709e-7,0.0000038851704,0.00054757897],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988584,0.00010640738,0.00033111867,0.00018738306,0.00016519912,0.0003515273],"domain_scores_gemma":[0.99910724,0.00009493116,0.00034634245,0.0001410927,0.000031669977,0.00027872386],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000799944,0.00010977964,0.00017588174,0.00010964595,0.00042497183,0.00004634774,0.00053068856,0.00009315853,0.0008771893],"category_scores_gemma":[0.00013241476,0.0000759579,0.000058615766,0.00021620661,0.0022164155,0.000271025,0.000064366075,0.00032691535,0.000028111972],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008177269,0.0000068506642,0.9950196,0.0000023979812,0.00000426432,0.000041516672,0.00041590378,0.00008035628,0.00081976346,0.000018926581,0.00017974933,0.0034024604],"study_design_scores_gemma":[0.00018288515,0.00022045561,0.9946147,0.000010967742,0.0000119680235,0.0007349673,0.00018200847,0.000038292656,0.00037716873,0.0007761171,0.0027636362,0.00008680002],"about_ca_topic_score_codex":0.0023097598,"about_ca_topic_score_gemma":0.7357998,"teacher_disagreement_score":0.73349,"about_ca_system_score_codex":0.000006829625,"about_ca_system_score_gemma":0.00046804847,"threshold_uncertainty_score":0.9604608},"labels":[],"label_agreement":null},{"id":"W2161031575","doi":"10.1139/cjes-2014-0136","title":"Assessing the age of the Late Cretaceous Danek Bonebed with U–Pb geochronology","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geochronology; Geology; Zircon; Cretaceous; Paleontology; Precambrian; Provenance; Archean; Detritus; Geochemistry","score_opus":0.0162663504705699,"score_gpt":0.20196279270742215,"score_spread":0.18569644223685225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161031575","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98822933,0.0005507106,0.00009359637,0.0036108103,0.00015029122,0.0000332305,0.000003806092,0.0000017788117,0.007326464],"genre_scores_gemma":[0.9986811,0.0000069918574,0.00052335754,0.0005948462,0.00005804713,6.6261606e-8,0.0000010559279,7.52728e-7,0.00013375905],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99889016,0.00016039984,0.00024221852,0.00010804871,0.00027133877,0.00032785957],"domain_scores_gemma":[0.99907,0.00024924037,0.0002478036,0.00013011615,0.00008971954,0.00021313979],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008901225,0.00008512401,0.00019677731,0.00008518128,0.00046445255,0.00014002233,0.00068908616,0.00003708509,0.0014396176],"category_scores_gemma":[0.0002466945,0.000032936823,0.00009275717,0.00055144046,0.0016390455,0.00022474083,0.000008411769,0.00020331593,0.000011529691],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000034850432,0.0000025947218,0.98358506,0.000003101371,0.000018503315,0.000024727815,0.00014949308,0.0117384605,0.0002515749,0.000113103786,0.000032537715,0.0040773787],"study_design_scores_gemma":[0.00009484657,0.0002352658,0.98637056,0.00002599306,0.000034079316,0.00012018348,0.00029037765,0.00213432,0.00037471324,0.0046282117,0.005616563,0.000074860654],"about_ca_topic_score_codex":0.01567478,"about_ca_topic_score_gemma":0.42613178,"teacher_disagreement_score":0.41045702,"about_ca_system_score_codex":8.308294e-7,"about_ca_system_score_gemma":0.00043188455,"threshold_uncertainty_score":0.9994732},"labels":[],"label_agreement":null},{"id":"W2161155643","doi":"10.1139/cjes-2014-0061","title":"Microconchid tubeworms (Class Tentaculita) from the Joggins Formation (Pennsylvanian), Nova Scotia, Canada","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Marine Biology and Ecology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Uniwersytet Śląski w Katowicach; Eesti Teadusagentuur; Eesti Teadusfondi","keywords":"Pennsylvanian; Carboniferous; Nova scotia; Geology; Paleontology; Polychaete; Brackish water; Oceanography; Ecology; Biology; Salinity; Structural basin","score_opus":0.019238084089857756,"score_gpt":0.21033157341997336,"score_spread":0.1910934893301156,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161155643","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9835716,0.0004380262,0.000022812967,0.008010819,0.0011803773,0.000082913015,0.00005110442,0.0000022828704,0.0066400818],"genre_scores_gemma":[0.99715,0.000011230066,0.0002160707,0.0021608118,0.00029996145,9.490549e-8,0.000016718766,0.000001337931,0.00014379584],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99859554,0.00016976071,0.00029897472,0.00014768842,0.0002672204,0.0005208025],"domain_scores_gemma":[0.99870235,0.00041830126,0.000155754,0.00012172407,0.00010166272,0.0005001847],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013571662,0.00010394428,0.00016730995,0.00011623569,0.00075184385,0.00014671928,0.0008173479,0.000064740794,0.0045242384],"category_scores_gemma":[0.00030529685,0.000060367576,0.000051447452,0.00028887315,0.0005802605,0.00040820046,0.000009701576,0.0003095158,0.00013689561],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006146899,0.0000011649438,0.98926765,0.0000017640457,0.000011113407,0.000018267605,0.000107951746,0.00024536604,0.00001347097,0.00006238215,0.0056864093,0.004578306],"study_design_scores_gemma":[0.00014475938,0.00016934174,0.9266331,0.000014966997,0.000006872165,0.000109077366,0.0003384464,0.0017372739,0.00007189896,0.0003724528,0.07031435,0.0000874461],"about_ca_topic_score_codex":0.9534281,"about_ca_topic_score_gemma":0.99990374,"teacher_disagreement_score":0.06462794,"about_ca_system_score_codex":0.0000073134693,"about_ca_system_score_gemma":0.0029350528,"threshold_uncertainty_score":0.99638575},"labels":[],"label_agreement":null},{"id":"W2161161879","doi":"10.1139/e02-014","title":"A new occurrence of <i>Archaeoscyphia pulchra </i>(Bassler) from the Ordovician of western Canada","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Ordovician; Geology; Paleontology; Head (geology)","score_opus":0.02773901831440433,"score_gpt":0.20416764047251787,"score_spread":0.17642862215811353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161161879","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97183776,0.01811666,0.000033224675,0.002017163,0.0007101144,0.00005934805,0.0003950749,0.0000013835479,0.006829243],"genre_scores_gemma":[0.9990438,0.00007466827,0.00057667156,0.00019580418,0.00008367456,4.6251472e-8,0.0000011716209,3.9000247e-7,0.000023721841],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985821,0.00010221926,0.00042777762,0.00013336824,0.00040559057,0.00034892323],"domain_scores_gemma":[0.99850315,0.00033362317,0.000400189,0.0001404066,0.000093536604,0.0005291228],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00045088472,0.000106369516,0.00025269683,0.00013522181,0.00026108287,0.00003497257,0.00088896847,0.000045489985,0.0012405787],"category_scores_gemma":[0.00012259193,0.00006907899,0.000079513484,0.00050978805,0.0008818932,0.0002591683,0.0000014716896,0.0001981264,0.0000025118604],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003889671,0.0000017625416,0.9704933,0.0000024838066,0.000014115624,0.00003028322,0.0005180082,0.00010803747,0.000007950974,0.000028670365,0.0011124115,0.027679078],"study_design_scores_gemma":[0.00012645347,0.00018505672,0.9950103,0.000061282044,0.0000146501825,0.00003881357,0.00033349014,0.0001672261,0.00007285676,0.00028166786,0.0036290013,0.000079190315],"about_ca_topic_score_codex":0.9415821,"about_ca_topic_score_gemma":0.99956465,"teacher_disagreement_score":0.05798259,"about_ca_system_score_codex":0.000001170025,"about_ca_system_score_gemma":0.003304429,"threshold_uncertainty_score":0.9996724},"labels":[],"label_agreement":null},{"id":"W2161766640","doi":"10.1139/e10-085","title":"Cyclic sedimentation in the Eocene Allenby Formation of south-central British Columbia and the origin of the Princeton Chert fossil beds","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Western Washington University","keywords":"Geology; Geochemistry; Conglomerate; Volcanic ash; Pyroclastic rock; Sedimentary rock; Volcano; Geomorphology; Paleontology","score_opus":0.017110792099158716,"score_gpt":0.22752929037756967,"score_spread":0.21041849827841094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161766640","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99623203,0.0005974336,0.0000023189439,0.0018351133,0.00027958959,0.0001289129,0.000011060656,4.907794e-7,0.00091303803],"genre_scores_gemma":[0.9997095,0.00005005595,0.00007382887,0.000114602386,0.000029389246,3.4945052e-7,8.273657e-7,4.8392064e-7,0.000020968364],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99891967,0.00023365632,0.00025618973,0.00006769091,0.0002811334,0.00024168451],"domain_scores_gemma":[0.9993457,0.00019005533,0.00021453926,0.00007758612,0.000077640885,0.00009447814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0025631266,0.00003921455,0.00012007107,0.000061633014,0.00036040976,0.000106217136,0.000458351,0.00005081932,0.00021475666],"category_scores_gemma":[0.00021729627,0.000024183862,0.00003916095,0.00030632873,0.0018609128,0.00023454957,0.000004756107,0.00028295701,0.0000011051908],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000778772,0.0000020249781,0.9969763,0.0000059632002,0.000003185053,0.000004148227,0.0019171165,0.00007466429,0.00001265444,0.00005286279,0.000036323305,0.00090692716],"study_design_scores_gemma":[0.00038329628,0.00006631214,0.9962928,0.000022740938,0.000006669377,0.00024359729,0.0012410078,0.0005994542,0.00005405861,0.0007110989,0.00035093172,0.000028022549],"about_ca_topic_score_codex":0.05956061,"about_ca_topic_score_gemma":0.96818686,"teacher_disagreement_score":0.90862626,"about_ca_system_score_codex":4.2261507e-7,"about_ca_system_score_gemma":0.0006272361,"threshold_uncertainty_score":0.9467019},"labels":[],"label_agreement":null},{"id":"W2161973685","doi":"10.1139/e11-025","title":"Age determinations for glacial Lake Agassiz shorelines west of Fargo, North Dakota, USA","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Ohio State University; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Geology; Glacial lake; Glacial period; Shore; Oceanography; Archaeology; Physical geography; Paleontology; Geography","score_opus":0.06771218057569436,"score_gpt":0.26459449004058755,"score_spread":0.19688230946489318,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161973685","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99030966,0.000325786,0.00005975162,0.00021200269,0.0005855985,0.000098893164,0.00011182055,0.0000018543046,0.008294612],"genre_scores_gemma":[0.9972152,0.000023034665,0.0023661358,0.0000815019,0.00009525641,5.1222895e-7,0.000010761092,0.0000013839774,0.00020622525],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987833,0.00008099305,0.00035205184,0.00014257262,0.00019111928,0.00044998463],"domain_scores_gemma":[0.99881023,0.00022592153,0.00020331146,0.00008999832,0.00023344252,0.0004370822],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00085750996,0.000092350645,0.00021817937,0.00043361075,0.00046499283,0.000035404733,0.0005623723,0.0000767887,0.004523869],"category_scores_gemma":[0.00032646666,0.00007053436,0.000094335905,0.00037864497,0.0013359801,0.0002830072,0.0000045569723,0.00015809071,0.000052746353],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015243673,0.000005330361,0.9980936,0.000009029512,0.0000099143,0.00008568448,0.00040785954,0.00010993561,0.000001402698,0.000108496504,0.00006960817,0.001083893],"study_design_scores_gemma":[0.00015631912,0.00048382947,0.99565417,0.000017324372,0.000013895547,0.00016592101,0.00018015646,0.00025796157,0.000060147777,0.00062560063,0.0023042972,0.00008040115],"about_ca_topic_score_codex":0.0033398743,"about_ca_topic_score_gemma":0.97793525,"teacher_disagreement_score":0.9745954,"about_ca_system_score_codex":2.4767942e-7,"about_ca_system_score_gemma":0.0012279779,"threshold_uncertainty_score":0.9963861},"labels":[],"label_agreement":null},{"id":"W2162064893","doi":"10.1139/e00-047","title":"A calcareous foraminiferal faunule from the upper Albian Viking Formation of the Giroux Lake and Kaybob North fields, northwestern Alberta: implications for regional biostratigraphic correlation","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Foraminifera; Facies; Calcareous; Paleontology; Transgressive; Structural basin; Geochemistry; Oceanography; Benthic zone","score_opus":0.02395992629309789,"score_gpt":0.20800287148089022,"score_spread":0.18404294518779232,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162064893","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935929,0.0004488944,0.00022803736,0.0047377804,0.00010718865,0.00014135009,0.00021376296,0.0000014526981,0.0005286139],"genre_scores_gemma":[0.999023,0.000051225747,0.00027306785,0.000511436,0.000054321536,8.9055504e-7,0.0000351636,8.201346e-7,0.00005005466],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993015,0.000035055833,0.00027951124,0.00008447863,0.00012497183,0.00017451147],"domain_scores_gemma":[0.9991782,0.0003202323,0.0001886518,0.00008053955,0.00010414657,0.00012823996],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019862648,0.00006932874,0.0000932129,0.000064867476,0.00073844934,0.00012203943,0.00028429172,0.00004197145,0.00028540072],"category_scores_gemma":[0.000057989728,0.000036734593,0.00006338952,0.0003090332,0.00031910764,0.0004977394,0.000002394894,0.00009412305,0.0000022818158],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000047157323,0.0000017611032,0.98350686,0.0000033666856,0.0000042255183,1.83794e-7,0.00083532685,0.0025991271,5.633553e-7,0.00014142385,0.00007650439,0.012825945],"study_design_scores_gemma":[0.000095098076,0.00012682102,0.9857355,0.0000247131,0.000013794326,0.00004719924,0.00030332562,0.0026904766,0.0000058376336,0.0023462086,0.00855734,0.000053728054],"about_ca_topic_score_codex":0.024360692,"about_ca_topic_score_gemma":0.93814486,"teacher_disagreement_score":0.9137842,"about_ca_system_score_codex":6.8061007e-7,"about_ca_system_score_gemma":0.00028326808,"threshold_uncertainty_score":0.9821362},"labels":[],"label_agreement":null},{"id":"W2162442859","doi":"10.1139/e05-073","title":"Rediscovery of the Mattawa Anorthosite Massif, Grenville Province, Quebec","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Anorthosite; Geology; Geochemistry; Pluton; Massif; Plagioclase; Xenolith; Layered intrusion; Petrology; Basalt; Mafic; Tectonics; Paleontology","score_opus":0.009751063786965445,"score_gpt":0.17467521311742856,"score_spread":0.16492414933046312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162442859","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97804594,0.0008591784,0.000007389877,0.0041899434,0.000193739,0.000040867544,0.000028192884,0.0000014920442,0.016633268],"genre_scores_gemma":[0.99780816,0.00001614204,0.0006425619,0.00042564323,0.0001370141,5.8875802e-8,0.0000011766864,7.2118974e-7,0.00096852507],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998806,0.00005930407,0.00033992066,0.0001310613,0.0003442466,0.0003194699],"domain_scores_gemma":[0.99910414,0.00006880705,0.0002656123,0.000110859415,0.00008141198,0.00036918945],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004758169,0.00008842625,0.00018512098,0.00014166556,0.00027865055,0.000076128155,0.0006143482,0.000040097493,0.0052244635],"category_scores_gemma":[0.00011719307,0.000045379176,0.00016278631,0.00058654504,0.00083373644,0.000272319,0.000009366995,0.00015066763,0.000035471807],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000031051777,0.000003989912,0.98791796,0.0000030213323,0.000008619388,0.000009203169,0.000043949767,0.005025308,0.00007899391,0.00012379422,0.00032660327,0.006455439],"study_design_scores_gemma":[0.00007548124,0.00009675282,0.9744891,0.000028155908,0.000018509576,0.000042653504,0.00012064521,0.00081401033,0.0007535995,0.0011167674,0.022358049,0.000086274],"about_ca_topic_score_codex":0.11249658,"about_ca_topic_score_gemma":0.959517,"teacher_disagreement_score":0.8470204,"about_ca_system_score_codex":0.0000018852398,"about_ca_system_score_gemma":0.0010683407,"threshold_uncertainty_score":0.9956849},"labels":[],"label_agreement":null},{"id":"W2162766179","doi":"10.1139/e10-028","title":"A new Lower Cretaceous (lower Albian) ichthyosaur genus from the Clearwater Formation, Alberta, Canada","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Killam Trusts","keywords":"Premaxilla; Cretaceous; Paleontology; Geology; Genus; Sister group; Pectoral girdle; Skull; Tetrapod (structure); Anatomy; Biology; Maxilla; Phylogenetic tree; Zoology; Clade","score_opus":0.009226137587746938,"score_gpt":0.18092721224392921,"score_spread":0.17170107465618228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162766179","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97515005,0.0013770948,0.000040041272,0.008809831,0.004695681,0.00006193795,0.000064138316,0.0000024982733,0.009798732],"genre_scores_gemma":[0.9955744,0.00001448441,0.00073337473,0.0023621782,0.0005296379,1.11948424e-7,0.000009441741,0.000001484869,0.00077484257],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873805,0.00008560516,0.00029887914,0.00015460898,0.00023486956,0.00048796192],"domain_scores_gemma":[0.99858755,0.00032600653,0.00017355046,0.0001456594,0.0000916584,0.00067558076],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00044917312,0.00011851651,0.00015704871,0.00008380822,0.00070183707,0.000097678996,0.0007162543,0.000098271616,0.010925486],"category_scores_gemma":[0.00021327946,0.00007135578,0.0000640119,0.00021959185,0.0005036085,0.00047557277,0.00000470868,0.00038118046,0.00015229087],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003099485,0.0000021986907,0.96164894,9.0216673e-7,0.000025238649,0.00018100192,0.00039657188,0.000539008,0.000026520618,0.00007818521,0.029756224,0.00731422],"study_design_scores_gemma":[0.00009848549,0.00010301156,0.6417025,0.00000567534,0.0000096754875,0.000367614,0.00010893214,0.00037232524,0.000011708692,0.00039285995,0.3567426,0.00008461004],"about_ca_topic_score_codex":0.9689225,"about_ca_topic_score_gemma":0.9999574,"teacher_disagreement_score":0.32698637,"about_ca_system_score_codex":0.000002869148,"about_ca_system_score_gemma":0.005079596,"threshold_uncertainty_score":0.9899787},"labels":[],"label_agreement":null},{"id":"W2162808162","doi":"10.1139/e99-107","title":"Late Holocene diatom biostratigraphy and sea-level changes in the southeastern Beaufort Sea","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Université Laval","keywords":"Geology; Holocene; Diatom; Radiocarbon dating; Marine transgression; Thermokarst; Sea level; Oceanography; Macrofossil; Paleontology; Beaufort sea; Sea ice; Arctic; Structural basin","score_opus":0.03782742706420658,"score_gpt":0.23606165336931909,"score_spread":0.1982342263051125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162808162","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98778445,0.0022052883,5.6174815e-7,0.004943348,0.000106451254,0.00006990663,0.00006281207,0.0000016695063,0.0048255264],"genre_scores_gemma":[0.9988704,0.0002141072,0.00010555455,0.00065051136,0.00005390201,2.4670905e-7,0.0000035711996,8.8419637e-7,0.00010087973],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99879813,0.00018440888,0.00017604225,0.00014362096,0.00021449437,0.00048330566],"domain_scores_gemma":[0.9993183,0.0001715615,0.00006189774,0.00008114856,0.000032212403,0.00033486626],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015054382,0.000090673435,0.0001503057,0.00034682231,0.00040695324,0.00011409351,0.00044451313,0.0000701615,0.0014309748],"category_scores_gemma":[0.000034951332,0.00005517964,0.00003388178,0.0005152046,0.0010678801,0.00019768583,0.0000021181868,0.00027050974,0.000043701362],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007723927,0.0000020634761,0.9964214,0.0000030789981,0.00000494222,0.00015648796,0.0007251154,0.00015299066,2.860146e-7,0.000014286401,0.00002369369,0.002487927],"study_design_scores_gemma":[0.0001355366,0.00023633486,0.9969367,0.00001825843,0.0000047491317,0.000457377,0.0005239015,0.00034886,0.000008141494,0.0004883462,0.00077233504,0.000069480084],"about_ca_topic_score_codex":0.009882795,"about_ca_topic_score_gemma":0.8382925,"teacher_disagreement_score":0.8284097,"about_ca_system_score_codex":1.10164926e-7,"about_ca_system_score_gemma":0.0004590627,"threshold_uncertainty_score":0.99948186},"labels":[],"label_agreement":null},{"id":"W2162816360","doi":"10.1139/cjes-2013-0028","title":"Pyroclastic kimberlite deposits from the Victor Northwest pipe (Ontario, Canada): the transition from phreatomagmatic to magmatic explosivity","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Kimberlite; Phreatomagmatic eruption; Geology; Pyroclastic rock; Geochemistry; Lapilli; Diatreme; Maar; Xenolith; Explosive eruption; Petrology; Volcano; Basalt; Mantle (geology)","score_opus":0.009716301547391915,"score_gpt":0.15993450466177603,"score_spread":0.1502182031143841,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162816360","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98473704,0.0005434562,0.00009350223,0.013543017,0.00029038414,0.00014722648,0.00010711008,0.0000035241408,0.0005347373],"genre_scores_gemma":[0.99596703,0.0000045891093,0.0004504485,0.003351142,0.0001559004,0.0000015499432,0.000020595946,0.0000015497457,0.000047193036],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982683,0.00013514547,0.00039371455,0.00020953164,0.0005383313,0.0004549901],"domain_scores_gemma":[0.99794626,0.0007329977,0.0001626306,0.00016901958,0.00013853508,0.00085056794],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029496267,0.00015974474,0.00024767342,0.000063767526,0.000717171,0.00035359056,0.00081213913,0.00003775295,0.016294425],"category_scores_gemma":[0.00016790106,0.00007498605,0.00010531648,0.0005315518,0.00032873312,0.0003272638,0.000007637193,0.00024835003,0.00014976703],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005276894,0.000005169484,0.99117476,0.000002085945,0.00004137896,0.000038302598,0.0013938723,0.00393925,0.00009912836,0.000005842383,0.0008942348,0.0024007093],"study_design_scores_gemma":[0.00007811876,0.000085292275,0.99217314,0.000042477146,0.00006341612,0.000017798911,0.00068837695,0.0019692266,0.0001226065,0.0033640333,0.0012710243,0.00012451784],"about_ca_topic_score_codex":0.99823326,"about_ca_topic_score_gemma":0.99998593,"teacher_disagreement_score":0.01614466,"about_ca_system_score_codex":0.000010353732,"about_ca_system_score_gemma":0.0016276648,"threshold_uncertainty_score":0.98460484},"labels":[],"label_agreement":null},{"id":"W2163014424","doi":"10.1139/e03-017","title":"Échanges napperivière en vallée alpine : quantification et modélisation (Vallée d'Aoste, Italie)","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Aquifer; Geology; Water table; Hydrology (agriculture); Context (archaeology); Groundwater; Alluvial fan; Alluvium; Geomorphology; Sedimentary rock; Structural basin; Geochemistry; Paleontology; Geotechnical engineering","score_opus":0.030034862963787223,"score_gpt":0.22794072246683308,"score_spread":0.19790585950304587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163014424","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97688,0.0015174738,0.00044886887,0.0014337621,0.0007386803,0.000090332534,0.000030044379,0.0000073895726,0.01885344],"genre_scores_gemma":[0.9979448,0.00006246301,0.0011124491,0.00027605996,0.000100493795,3.3194777e-7,0.000016338794,0.0000025702,0.0004845408],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986383,0.00015361153,0.00030212116,0.00019479792,0.00033604872,0.00037513155],"domain_scores_gemma":[0.9990403,0.00008483557,0.00017613122,0.00012186792,0.00012547855,0.00045135763],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015800208,0.00012435525,0.00015824867,0.00023310367,0.00032564637,0.00029542609,0.00036237485,0.00006903677,0.0015844249],"category_scores_gemma":[0.00023952122,0.000097994845,0.00006731552,0.00037389822,0.00024300265,0.00070704095,0.0000026898865,0.00016594729,0.00006154095],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009223884,0.0000127293215,0.97281003,0.000028658083,0.000028177874,0.0000577269,0.0028439227,0.011394713,0.0013184288,0.001591777,0.000588315,0.009316306],"study_design_scores_gemma":[0.0004127485,0.0004855303,0.9078979,0.00010486877,0.000029816374,0.0005712012,0.003363674,0.003235027,0.0055891727,0.0027143368,0.075150385,0.0004453663],"about_ca_topic_score_codex":0.006030908,"about_ca_topic_score_gemma":0.16638461,"teacher_disagreement_score":0.16035369,"about_ca_system_score_codex":0.0000035864891,"about_ca_system_score_gemma":0.00096579536,"threshold_uncertainty_score":0.99932826},"labels":[],"label_agreement":null},{"id":"W2163250458","doi":"10.1139/cjes-2014-0167","title":"Redescription of UALVP 40, an unusual specimen of <i>Chasmosaurus</i> Lambe, 1914 (Ceratopsidae: Chasmosaurinae) bearing long postorbital horns, and its implications for ontogeny and alpha taxonomy of the genus","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Anatomy; Skull; Biology; Geology; Genus; Paleontology; Zoology","score_opus":0.06478676194562602,"score_gpt":0.24262440235811683,"score_spread":0.1778376404124908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163250458","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930585,0.0050497614,0.000052146253,0.00057897717,0.00026975654,0.00016676533,0.0002246606,0.0000012902035,0.0005981532],"genre_scores_gemma":[0.9991239,0.000046229212,0.0006873221,0.00004410684,0.00006487576,5.1624266e-7,0.000006944441,0.0000012954141,0.000024860934],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990932,0.00008110099,0.00033366666,0.00014633963,0.00011448892,0.00023124354],"domain_scores_gemma":[0.9989008,0.00007476518,0.00040979314,0.000090519316,0.0002005491,0.0003236237],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007884029,0.00008450378,0.00020874267,0.0001544564,0.00023291382,0.000016927654,0.0002705677,0.00007235822,0.000022802938],"category_scores_gemma":[0.00012901016,0.00006222463,0.00004297046,0.00020594752,0.0009487092,0.00038335484,0.000009013134,0.00008876207,3.577617e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046646335,0.000007723803,0.9957759,0.000010980187,0.000017054084,0.0000019213735,0.00030533492,0.00018429491,0.00069649983,0.0008682392,0.000053973206,0.0020314506],"study_design_scores_gemma":[0.00026050518,0.0007389516,0.9953461,0.00002506874,0.00002153211,0.00027869496,0.00040361425,0.00030525943,0.0007808623,0.00038719265,0.0013817399,0.00007045135],"about_ca_topic_score_codex":0.0044975653,"about_ca_topic_score_gemma":0.17448208,"teacher_disagreement_score":0.16998452,"about_ca_system_score_codex":0.0000030911633,"about_ca_system_score_gemma":0.00083556346,"threshold_uncertainty_score":0.8405815},"labels":[],"label_agreement":null},{"id":"W2163250751","doi":"10.1139/e02-001","title":"Early Eocene Leptictida, Pantolesta, Creodonta, Carnivora, and Mesonychidae (Mammalia) from the Eureka Sound Group, Ellesmere Island, Nunavut","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Land bridge; Sound (geography); Geology; Group (periodic table); Biological dispersal; Paleontology; Oceanography; Archaeology; Geography","score_opus":0.02905016262139728,"score_gpt":0.2049978750190997,"score_spread":0.1759477123977024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163250751","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9625874,0.021961858,0.000026870677,0.003670827,0.0007215928,0.000081657956,0.00014861024,0.0000063070697,0.01079486],"genre_scores_gemma":[0.9974713,0.00059733976,0.00024963965,0.00093771995,0.00031114495,2.598074e-7,0.0000035084763,0.0000028392803,0.00042628424],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998323,0.0001951192,0.00034412497,0.00025159016,0.00034602947,0.0005401287],"domain_scores_gemma":[0.9985636,0.00039833575,0.00023440844,0.00014031981,0.00009067236,0.00057270535],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006521213,0.0001801173,0.00027496502,0.00015404422,0.0013491308,0.00028473765,0.0005079261,0.00008135303,0.0024741376],"category_scores_gemma":[0.0001291708,0.00011566843,0.00008850088,0.00033124164,0.001392205,0.00042319324,0.000008068587,0.00032799522,0.000092842674],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000061908067,0.0000032371065,0.99288845,0.000001626635,0.000034358563,0.00008840387,0.0017371732,0.000077476434,0.0000014631488,0.00009484238,0.002691446,0.0023753478],"study_design_scores_gemma":[0.00026761426,0.00026125388,0.97762585,0.00003297853,0.00003639772,0.00018881143,0.0019173993,0.00058424094,0.0000014303848,0.00046867543,0.01845823,0.00015711102],"about_ca_topic_score_codex":0.06988318,"about_ca_topic_score_gemma":0.987839,"teacher_disagreement_score":0.9179558,"about_ca_system_score_codex":0.0000023779016,"about_ca_system_score_gemma":0.00019759167,"threshold_uncertainty_score":0.999951},"labels":[],"label_agreement":null},{"id":"W2163274926","doi":"10.1139/cjes-2014-0133","title":"A new crocodylian (Eusuchia) from the uppermost Cretaceous of Alberta, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; Canadian Museum of Nature","funders":"","keywords":"Cretaceous; Paleontology; Premaxilla; Mandibular symphysis; Geology; Range (aeronautics); Genus; Sister group; Geography; Phylogenetic tree; Biology; Zoology; Clade; Symphysis; Anatomy","score_opus":0.02155881604342835,"score_gpt":0.2021345656008483,"score_spread":0.18057574955741995,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163274926","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9658447,0.007794519,0.000026419251,0.00738526,0.0015315654,0.0000524453,0.00008729566,0.0000012484295,0.017276527],"genre_scores_gemma":[0.9979084,0.000015344343,0.0006666622,0.0007809163,0.00021725481,4.5943853e-8,0.00000641821,8.4336654e-7,0.00040409097],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988941,0.000117497955,0.00027912724,0.0001221655,0.00024178109,0.00034533607],"domain_scores_gemma":[0.998403,0.0003514861,0.00020689974,0.00010536393,0.00010261731,0.0008306142],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048633755,0.00008807994,0.00018308495,0.00007598291,0.00028249342,0.000030226227,0.00068179105,0.00005749865,0.0016181194],"category_scores_gemma":[0.00033642928,0.000054330078,0.000046534333,0.00028081186,0.00060912,0.00018452009,0.0000038038154,0.00016011519,0.000023254768],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000145318645,8.0822014e-7,0.9859853,4.8738474e-7,0.000013703149,0.00004463326,0.00038741776,0.0011315013,0.0000026870607,0.000061893785,0.009153152,0.0032038763],"study_design_scores_gemma":[0.00015607556,0.00019176806,0.8828187,0.000013743059,0.000011168556,0.00020482075,0.00071797974,0.00029523476,0.000016292523,0.00097020593,0.11453202,0.00007200341],"about_ca_topic_score_codex":0.99334794,"about_ca_topic_score_gemma":0.99995,"teacher_disagreement_score":0.10537887,"about_ca_system_score_codex":0.0000035779967,"about_ca_system_score_gemma":0.016185803,"threshold_uncertainty_score":0.9992945},"labels":[],"label_agreement":null},{"id":"W2163619769","doi":"10.1139/e00-092","title":"Middle Pleistocene to Holocene palynostratigraphy of Ocean Drilling Program Site 887 in the Gulf of Alaska, northeastern North Pacific","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Public Works and Government Services Canada","funders":"","keywords":"Dinocyst; Pleistocene; Geology; Paleontology; Palynology; Early Pleistocene; Holocene; Oceanography; Pollen; Ecology","score_opus":0.03513873010084726,"score_gpt":0.24146441912027528,"score_spread":0.20632568901942802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163619769","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99592286,0.00093099615,0.0000063399843,0.0008217506,0.00016040239,0.00020644446,0.00003292279,0.0000021174133,0.0019161379],"genre_scores_gemma":[0.999257,0.000057795514,0.00052211777,0.000090383735,0.000039178023,3.7744715e-7,0.0000062112313,0.000001490331,0.000025415668],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99815524,0.00020361811,0.0005070524,0.00018092287,0.000390803,0.0005623769],"domain_scores_gemma":[0.9987605,0.0002586568,0.00024744126,0.0001605721,0.00017086012,0.00040195367],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014959534,0.0001178537,0.00029167096,0.0007111439,0.00023998668,0.00004783147,0.0007275801,0.00006641203,0.00022690186],"category_scores_gemma":[0.00013425859,0.000077948614,0.00009672239,0.001613192,0.0010233389,0.00019865093,0.000004949499,0.00026528968,0.000014756197],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031971962,0.000016284954,0.99218726,0.000011003327,0.00000930427,0.00013504545,0.0018167979,0.0041046236,0.0000010354842,0.000008862168,0.000016007514,0.0016617888],"study_design_scores_gemma":[0.00015612478,0.0010985305,0.99576783,0.00005745822,0.000007717545,0.0002647393,0.0017537012,0.0003317849,0.000020575095,0.00009671513,0.00036343682,0.00008135634],"about_ca_topic_score_codex":0.007003958,"about_ca_topic_score_gemma":0.77054596,"teacher_disagreement_score":0.763542,"about_ca_system_score_codex":3.893362e-7,"about_ca_system_score_gemma":0.00070901663,"threshold_uncertainty_score":0.9996085},"labels":[],"label_agreement":null},{"id":"W2163620328","doi":"10.1139/cjes-2013-0096","title":"Late Quaternary glacial history and meltwater discharges along the Northeastern Newfoundland Shelf","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Rimouski; Geological Survey of Canada; Université Laval; Natural Resources Canada; Bedford Institute of Oceanography; Dalhousie University; Université du Québec à Montréal; Center for Northern Studies","funders":"","keywords":"Geology; Meltwater; Glacial period; Last Glacial Maximum; Quaternary; Turbidite; Geomorphology; Ice shelf; Ice sheet; Paleontology; Sedimentary rock; Radiocarbon dating; Oceanography; Sea ice; Cryosphere","score_opus":0.023007624993945035,"score_gpt":0.2139263104728135,"score_spread":0.19091868547886845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163620328","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98668945,0.004116474,0.0000027089072,0.00497465,0.0007302205,0.00008036769,0.000003788368,0.0000024834255,0.003399878],"genre_scores_gemma":[0.9984085,0.00006997486,0.00008036218,0.00042676993,0.00013237177,3.8236084e-7,0.0000015939193,0.0000014009668,0.0008786274],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988117,0.00016240079,0.00022087098,0.00014299159,0.00020293646,0.00045910754],"domain_scores_gemma":[0.99909717,0.00016311267,0.000105852916,0.000085126114,0.00007511109,0.00047361944],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008464832,0.000096541124,0.00015304884,0.00019405581,0.000523332,0.00013526979,0.00042870577,0.000057609257,0.005358305],"category_scores_gemma":[0.00005344732,0.000052906147,0.000042635176,0.0001079908,0.0015341472,0.0005265325,0.0000080337995,0.0002517419,0.00026079873],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000051574393,0.0000011185,0.99824095,0.000003402329,0.000010419152,0.0000621823,0.0006347908,0.000090578505,0.0000023793398,0.000037192425,0.00009707805,0.0008147438],"study_design_scores_gemma":[0.000112883296,0.00013893843,0.992094,0.00001318351,0.000006859113,0.00045615077,0.00018357378,0.00084667915,0.0000022814654,0.00076103956,0.0053087906,0.00007562564],"about_ca_topic_score_codex":0.08357656,"about_ca_topic_score_gemma":0.87743825,"teacher_disagreement_score":0.7938617,"about_ca_system_score_codex":8.1559153e-7,"about_ca_system_score_gemma":0.0006632766,"threshold_uncertainty_score":0.99555093},"labels":[],"label_agreement":null},{"id":"W2163631523","doi":"10.1139/e00-076","title":"A Cretaceous back-arc basin in the Coast Belt of the northern Canadian Cordillera: evidence from geochemical and neodymium isotope characteristics of the Kluane metamorphic assemblage, southwest Yukon","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon University; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Terrane; Metamorphic rock; Geochemistry; Provenance; Cretaceous; SLATES; Sedimentary rock; Gneiss; Back-arc basin; Paleontology; Subduction; Tectonics","score_opus":0.02415555104153365,"score_gpt":0.19836630835643287,"score_spread":0.1742107573148992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163631523","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98792243,0.0015472232,0.0000014181084,0.009512446,0.00015552375,0.00011288029,0.00017518416,7.327531e-7,0.00057216664],"genre_scores_gemma":[0.9986813,0.00012836451,0.00006731886,0.0010008645,0.00006894848,2.8417955e-7,0.0000040305013,0.000001602768,0.000047264915],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99806094,0.00024809252,0.00051892153,0.00021453806,0.00052023306,0.00043729172],"domain_scores_gemma":[0.99827737,0.00045219803,0.00039224676,0.00024364516,0.00019123573,0.00044330626],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00095258077,0.00015362252,0.00036496526,0.00013834816,0.00033049233,0.00009815586,0.0012153585,0.00008127767,0.0022718175],"category_scores_gemma":[0.00066327426,0.00006998926,0.00016596113,0.0010623054,0.0011912218,0.00016511585,0.000023096389,0.00036962712,0.000008444432],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009271665,0.000006299802,0.9977735,0.0000040507207,0.000016744387,0.00003077323,0.00055454014,0.00014192748,0.00025553445,0.000003750208,0.00004522612,0.0011583776],"study_design_scores_gemma":[0.00009517422,0.00009812174,0.99633276,0.00012364094,0.00005760373,0.00009305862,0.00062251865,0.000808473,0.00029715718,0.00055977335,0.0008152892,0.00009644218],"about_ca_topic_score_codex":0.7547981,"about_ca_topic_score_gemma":0.9926141,"teacher_disagreement_score":0.23781593,"about_ca_system_score_codex":0.000004306538,"about_ca_system_score_gemma":0.0011122585,"threshold_uncertainty_score":0.99864024},"labels":[],"label_agreement":null},{"id":"W2163751192","doi":"10.1139/e04-074","title":"Late-glacial lakes in the Thompson Basin, British Columbia: paleogeography and evolution","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Simon Fraser University","keywords":"Geology; Glacial period; Ice sheet; Post-glacial rebound; Plateau (mathematics); Glacial lake; Sedimentology; Meltwater; Geomorphology; Paleontology; Palaeogeography; Structural basin; Shelf ice; Oceanography; Physical geography; Ice stream; Cryosphere; Sea ice; Tectonics","score_opus":0.012867174178479808,"score_gpt":0.20684634356589665,"score_spread":0.19397916938741686,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163751192","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98947203,0.0030372227,0.0000041388034,0.0018021881,0.00029467707,0.000071438604,0.000012731864,0.0000014748205,0.0053040828],"genre_scores_gemma":[0.9993613,0.00010192789,0.00014472975,0.00027559962,0.00006461856,2.1892419e-7,0.0000017590819,6.4683195e-7,0.000049206054],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99889994,0.00016968469,0.00018990498,0.00013100397,0.00020507803,0.00040437139],"domain_scores_gemma":[0.99944884,0.00012938802,0.000074294745,0.000053564192,0.000055133914,0.00023879096],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015526314,0.00005266835,0.00013741062,0.00021442238,0.0006748169,0.00034947225,0.00034182752,0.00007435559,0.00085779245],"category_scores_gemma":[0.00012435026,0.00004864497,0.00004265139,0.0006250507,0.0013187194,0.00030144208,0.0000026401158,0.00027378256,0.000022143464],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000334772,0.0000029210323,0.99854195,0.0000030617093,0.000003138297,0.0002104062,0.00022868461,0.0004676884,4.3691819e-7,0.000041536794,0.000043501157,0.0004533038],"study_design_scores_gemma":[0.0002267301,0.00027053873,0.99364626,0.00003539981,0.000004119912,0.0010086802,0.00052905304,0.000027470851,8.3167816e-7,0.003565105,0.0006265265,0.000059309525],"about_ca_topic_score_codex":0.12429824,"about_ca_topic_score_gemma":0.9966929,"teacher_disagreement_score":0.8723947,"about_ca_system_score_codex":4.3363593e-7,"about_ca_system_score_gemma":0.0007916101,"threshold_uncertainty_score":0.9392226},"labels":[],"label_agreement":null},{"id":"W2163755738","doi":"10.1139/e03-088","title":"The timing of Proterozoic magmatism in the Pinware terrane of southeast Labrador, easternmost Quebec and northwest Newfoundland","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec)","funders":"","keywords":"Geology; Terrane; Mafic; Baddeleyite; Geochemistry; Magmatism; Proterozoic; Anorthosite; Crust; Gabbro; Geochronology; Zircon; Tectonics; Paleontology; Plagioclase; Igneous rock; Quartz","score_opus":0.016808070058509508,"score_gpt":0.196493551726126,"score_spread":0.1796854816676165,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163755738","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99553406,0.0013478522,0.000009915205,0.0023699133,0.00005235363,0.00006805147,0.000023744038,6.208205e-7,0.00059348874],"genre_scores_gemma":[0.9996277,0.000025777741,0.00020638778,0.000088015135,0.000028359655,1.8087525e-7,0.0000016064273,5.7357704e-7,0.000021390893],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990084,0.00006751879,0.00032770465,0.000094983385,0.0002664059,0.00023499888],"domain_scores_gemma":[0.99933827,0.00013745028,0.00021302351,0.00007822873,0.000060569528,0.00017244925],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007547434,0.000075049276,0.00016938437,0.000110791945,0.00024823943,0.00008749093,0.00043132392,0.00002698089,0.00026356796],"category_scores_gemma":[0.00010726825,0.00003412548,0.000052916894,0.00043041894,0.00089810725,0.00015701742,0.000005494841,0.0001300062,0.0000029641972],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006980083,0.0000043759865,0.98919207,0.000009545118,0.0000065815775,0.000018008846,0.0013151718,0.0013297393,0.000028075081,0.000077202334,0.0000017233332,0.008010516],"study_design_scores_gemma":[0.0001592243,0.00017395482,0.9938223,0.00007685108,0.000010202447,0.000072324205,0.0023925733,0.00024033553,0.00003282849,0.0028235547,0.00014654562,0.000049300917],"about_ca_topic_score_codex":0.56669074,"about_ca_topic_score_gemma":0.9929166,"teacher_disagreement_score":0.4262258,"about_ca_system_score_codex":0.0000011764575,"about_ca_system_score_gemma":0.00036148404,"threshold_uncertainty_score":0.4361947},"labels":[],"label_agreement":null},{"id":"W2163913131","doi":"10.1139/e09-039","title":"Globally significant Early Permian crinoids from the Mount Mark Formation in Strathcona Provincial Park, Vancouver Island, British Columbia — preliminary analysis of a disappearing fauna","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ministry of Forests; Geological Survey of Canada","funders":"","keywords":"Fauna; Crinoid; Permian; Paleozoic; Geology; Terrane; Paleontology; Mount; Archaeology; Geography; Ecology; Structural basin; Biology; Tectonics","score_opus":0.012593234691993058,"score_gpt":0.2026688730941983,"score_spread":0.19007563840220523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163913131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99383694,0.0012548433,0.00004138832,0.00030392097,0.0002515127,0.000110945824,0.0002446905,0.0000024262113,0.0039533535],"genre_scores_gemma":[0.99941707,0.00004380772,0.00019467466,0.00021601062,0.00006355494,2.546248e-7,0.000006392204,7.613122e-7,0.000057454792],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985328,0.00013314177,0.00046692998,0.00016069712,0.00036280428,0.00034364482],"domain_scores_gemma":[0.9991837,0.00012464575,0.00027899572,0.000088206114,0.00010615343,0.00021829414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00070087996,0.00008408812,0.00027455253,0.00017950195,0.0004200167,0.00031043668,0.0004389161,0.000055276214,0.0004385588],"category_scores_gemma":[0.00011628036,0.000076493525,0.000114968185,0.00085039734,0.00044569917,0.00052702636,0.0000043536143,0.0001762462,0.0000025996255],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016800699,0.000006429171,0.99074143,0.0000019629847,0.00004078626,0.000068433976,0.00094697415,0.0020428668,0.0000050048247,0.000011941614,0.00074035046,0.0053769904],"study_design_scores_gemma":[0.0001710289,0.0003926213,0.99314195,0.000050199844,0.00008555484,0.000017727914,0.001963955,0.0034066222,0.0000013378423,0.00031841462,0.000355698,0.000094918134],"about_ca_topic_score_codex":0.6287084,"about_ca_topic_score_gemma":0.9996735,"teacher_disagreement_score":0.37096503,"about_ca_system_score_codex":0.000008572001,"about_ca_system_score_gemma":0.00056585064,"threshold_uncertainty_score":0.48019114},"labels":[],"label_agreement":null},{"id":"W2163956624","doi":"10.1139/e10-065","title":"Introduction to<i>Albertosaurus</i>Special Issue","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Geochemistry","score_opus":0.00892600679723247,"score_gpt":0.20300478509642608,"score_spread":0.19407877829919362,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163956624","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9220389,0.00020560058,0.000016867123,0.02182749,0.011917838,0.00005340916,0.000020422549,0.0000038825674,0.043915566],"genre_scores_gemma":[0.9787006,0.0000072857706,0.0020784526,0.0007933102,0.017695053,9.9471e-8,0.0000035745563,8.590419e-7,0.00072079664],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99908775,0.000050482446,0.0002088162,0.00015594442,0.00013454774,0.00036243827],"domain_scores_gemma":[0.9990422,0.000066024055,0.00009355089,0.00008183864,0.00008837208,0.00062801724],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00073362095,0.000074525386,0.00012732352,0.00032620755,0.00045268144,0.000050840565,0.0003776531,0.00008095099,0.023727162],"category_scores_gemma":[0.00033308927,0.00005722649,0.000043531687,0.0003837514,0.0006435547,0.00032342464,0.0000022311676,0.00027303494,0.00072092446],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016386302,0.0000029157418,0.9395145,0.000001110124,0.0000068093777,0.000040619838,0.00021144461,0.00059626624,0.00021148154,0.00066960684,0.04121085,0.01751798],"study_design_scores_gemma":[0.00003999974,0.00017421854,0.5060137,0.0000016526186,0.0000026262312,0.00035659273,0.000053287527,0.000041347044,0.000043227326,0.00044291533,0.49277943,0.00005100685],"about_ca_topic_score_codex":0.0070709772,"about_ca_topic_score_gemma":0.8564539,"teacher_disagreement_score":0.84938294,"about_ca_system_score_codex":7.450943e-7,"about_ca_system_score_gemma":0.00088486675,"threshold_uncertainty_score":0.99954104},"labels":[],"label_agreement":null},{"id":"W2164103536","doi":"10.1139/e01-008","title":"Ammonoid faunas from the Cardium Formation (TuronianConiacian; Upper Cretaceous) and contiguous units, Alberta, Canada: II. Collignoniceratidae and Placenticeratidae","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Alberta Bone and Joint Health Institute","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Ammonite; Biozone; Cretaceous; Paleontology; Geology; Biostratigraphy; Fauna; Structural basin; Biology; Ecology","score_opus":0.013122951692425716,"score_gpt":0.18606440223843085,"score_spread":0.17294145054600513,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164103536","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9600637,0.02285921,0.000017417844,0.003043572,0.00044976533,0.000117224656,0.00008589285,0.0000022590239,0.013360943],"genre_scores_gemma":[0.99874896,0.00033217712,0.00019062805,0.0005093119,0.000110030414,3.18963e-7,0.0000032445212,9.0423725e-7,0.00010442123],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99872947,0.00013514134,0.00031267141,0.0001710554,0.00024500804,0.00040666224],"domain_scores_gemma":[0.998724,0.0003373611,0.00019563184,0.000094993455,0.00011522349,0.00053282524],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00048413387,0.00014489483,0.00022945472,0.000102645645,0.001617132,0.00030630882,0.00027570289,0.000069194604,0.00018889259],"category_scores_gemma":[0.00013284363,0.00009742909,0.000032565025,0.00031798903,0.0006564728,0.0006513003,0.000002207487,0.00021822401,0.000001533191],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017839884,0.0000012720623,0.98604715,0.0000024114872,0.000031279083,0.0000944226,0.0011238743,0.00014151819,0.000005465231,0.00015485093,0.0010404186,0.011339477],"study_design_scores_gemma":[0.00026552274,0.00018393635,0.9701331,0.00003125426,0.000029559402,0.0004887096,0.0015636119,0.0011332203,0.000029468147,0.00018233941,0.025825346,0.00013389256],"about_ca_topic_score_codex":0.8605754,"about_ca_topic_score_gemma":0.9996979,"teacher_disagreement_score":0.13912255,"about_ca_system_score_codex":0.0000037301506,"about_ca_system_score_gemma":0.0027928988,"threshold_uncertainty_score":0.9996826},"labels":[],"label_agreement":null},{"id":"W2164191885","doi":"10.1139/cjes-2013-0062","title":"Improving Bayesian maximum entropy and ordinary Kriging methods for estimating precipitations in a large watershed: a new cluster-based approach","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrology and Drought Analysis","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of British Columbia, Okanagan Campus; University of British Columbia","funders":"","keywords":"Watershed; Kriging; Principle of maximum entropy; Environmental science; Bayesian probability; Entropy (arrow of time); Statistics; Precipitation; Spatial variability; Spatial analysis; Cluster analysis; Computer science; Mathematics; Meteorology; Machine learning; Geography","score_opus":0.01566689502306166,"score_gpt":0.27341655053404057,"score_spread":0.2577496555109789,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164191885","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.32372534,0.000090429116,0.67405593,0.0013270315,0.00008288591,0.00017504793,0.0000014836878,0.0000028105023,0.0005390592],"genre_scores_gemma":[0.4998959,3.561783e-7,0.4998463,0.0001816075,0.000023750923,0.0000041650674,6.383585e-7,0.000002591675,0.000044654033],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99888355,0.00012231115,0.0002756818,0.00019260905,0.00010176004,0.00042410157],"domain_scores_gemma":[0.99917126,0.00016011635,0.00015519357,0.00006881207,0.000014731874,0.00042989408],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001570101,0.00008992552,0.00016823727,0.00026932714,0.00040286517,0.0001379056,0.00022817565,0.000045792058,0.00045843833],"category_scores_gemma":[0.00026215738,0.0000713998,0.000056413806,0.0004054709,0.00026138517,0.0006260772,0.000019989224,0.00012151015,0.0000047674025],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020212585,0.000052257026,0.6841147,0.000037571477,0.00003246275,0.000019659094,0.005398862,0.18484871,0.0025611694,0.00023311576,0.0006151411,0.122066125],"study_design_scores_gemma":[0.00044426168,0.00016035108,0.013790376,0.000018046556,0.000022072678,0.000030459618,0.0005285635,0.9805026,0.000092909155,0.0037630626,0.0005341871,0.00011310555],"about_ca_topic_score_codex":0.0116347475,"about_ca_topic_score_gemma":0.029705785,"teacher_disagreement_score":0.7956539,"about_ca_system_score_codex":0.000017433564,"about_ca_system_score_gemma":0.00030001043,"threshold_uncertainty_score":0.99494684},"labels":[],"label_agreement":null},{"id":"W2164245304","doi":"10.1139/cjes-2015-0061","title":"A new elasmobranch assemblage from the early Eocene (Ypresian) Fishburne Formation of Berkeley County, South Carolina, USA","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Ichthyology and Marine Biology","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Assemblage (archaeology); Geology; Paleontology; Faunal assemblage; Oceanography; Archaeology; Geography; Fauna; Ecology; Biology","score_opus":0.02039598472094081,"score_gpt":0.216956818827464,"score_spread":0.1965608341065232,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164245304","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911044,0.00020368144,0.00035170582,0.0011137795,0.0004250507,0.00006528889,0.000017706794,0.0000016979213,0.0067166477],"genre_scores_gemma":[0.99844384,0.000007365837,0.0008292177,0.0003596702,0.00012003691,4.0678694e-7,0.000001323657,0.0000027054298,0.0002354593],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989094,0.0001026324,0.0002918638,0.000118925105,0.00027622416,0.00030097034],"domain_scores_gemma":[0.9991037,0.000076529584,0.00019920956,0.000125688,0.00004366202,0.00045115664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00094544893,0.00008868238,0.000162642,0.00006791925,0.0001902282,0.00004143534,0.00060763437,0.000076639764,0.0007563776],"category_scores_gemma":[0.00018891662,0.000058167872,0.000053347863,0.00028486474,0.0006040586,0.0005075326,0.000042069034,0.00015950449,0.00009334605],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017486218,0.0000044093836,0.9903526,8.9590986e-7,0.000007656924,0.000015665246,0.0024756996,0.0007165739,0.00042490914,0.00013742619,0.004569089,0.0012776218],"study_design_scores_gemma":[0.00035208365,0.00037468618,0.9849529,0.000014976354,0.00001924844,0.00006599034,0.0003876099,0.00014940514,0.0011675744,0.0016322152,0.010791893,0.0000913969],"about_ca_topic_score_codex":0.08614163,"about_ca_topic_score_gemma":0.40416992,"teacher_disagreement_score":0.31802827,"about_ca_system_score_codex":0.000019263247,"about_ca_system_score_gemma":0.00073643174,"threshold_uncertainty_score":0.9199438},"labels":[],"label_agreement":null},{"id":"W2164387178","doi":"10.1139/e02-043","title":"A three-dimensional model to simulate joint networks in layered rocks","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Classification of discontinuities; Joint (building); Geology; Discontinuity (linguistics); Position (finance); Fracture (geology); Fractal; Stochastic modelling; Geometry; Geotechnical engineering; Mathematics; Structural engineering; Mathematical analysis; Engineering","score_opus":0.038197214908526005,"score_gpt":0.21742472574165292,"score_spread":0.1792275108331269,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164387178","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9815523,0.00020609697,0.014868982,0.0014658904,0.00017766256,0.00006959147,0.000001619674,0.000002405348,0.0016554322],"genre_scores_gemma":[0.9975093,0.0000024339247,0.00093557505,0.00078518264,0.000028375563,0.0000010282486,7.3321694e-8,0.0000028759225,0.00073518377],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99896973,0.000017337903,0.0002488288,0.00014413845,0.0002793764,0.00034056048],"domain_scores_gemma":[0.99943024,0.000021022315,0.00007161153,0.000063880754,0.000022888471,0.0003903627],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004307538,0.00008071573,0.00013327984,0.00017216397,0.00024332294,0.000068009555,0.00022663824,0.000027050333,0.0008794639],"category_scores_gemma":[0.000037581027,0.000063763175,0.000042105934,0.00041447947,0.00018299313,0.0002784509,0.00003400785,0.000107630854,0.00008577947],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001330241,0.000006014095,0.08022103,2.9187348e-7,0.0000021434096,0.000033077347,0.00038479108,0.9142777,0.00006977144,0.000014620482,0.0007818647,0.0042074095],"study_design_scores_gemma":[0.00022643995,0.00013077042,0.18398836,0.000029981977,0.0000032487435,0.000029665121,0.000076473574,0.8120492,0.00004390441,0.00027341684,0.0030128593,0.00013569393],"about_ca_topic_score_codex":0.0050906264,"about_ca_topic_score_gemma":0.40526125,"teacher_disagreement_score":0.40017062,"about_ca_system_score_codex":0.000026326587,"about_ca_system_score_gemma":0.00006013122,"threshold_uncertainty_score":0.96295136},"labels":[],"label_agreement":null},{"id":"W2164526185","doi":"10.1139/e06-124","title":"Paleomagnetism, U–Pb geochronology, and geochemistry of Lac Esprit and other dyke swarms, James Bay area, Quebec, and implications for Paleoproterozoic deformation of the Superior Province","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec en Abitibi-Témiscamingue; Carleton University; University of Toronto; Geological Survey of Canada","funders":"Natural Resources Canada; Public Works and Government Services Canada; Government of Canada; Canadian Natural Resources Limited","keywords":"Paleomagnetism; Geology; Clockwise; Bay; Magnetic declination; Paleontology; Geochronology; Declination; Terrane; Rift; Swarm behaviour; Seismology; Sinistral and dextral; Rotation (mathematics); Fault (geology); Tectonics; Geometry; Earth's magnetic field; Oceanography","score_opus":0.01158383437624103,"score_gpt":0.1990025048339265,"score_spread":0.18741867045768548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164526185","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99378115,0.0034687903,0.000065038046,0.002176164,0.000026261618,0.0001039777,0.000074285104,0.0000011730684,0.0003031492],"genre_scores_gemma":[0.99887764,0.00005652274,0.0008790534,0.00012368754,0.000020760504,4.080308e-7,0.0000019951015,6.649605e-7,0.000039274393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992796,0.000014684516,0.0002849422,0.000120855635,0.00009112967,0.000208741],"domain_scores_gemma":[0.999292,0.00011968559,0.0002109795,0.00007041098,0.00008947046,0.00021741609],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005071694,0.00007497871,0.0001653323,0.00008531101,0.00019218748,0.00003672398,0.00017878077,0.000054951917,0.00022712254],"category_scores_gemma":[0.000116670526,0.000044033237,0.00004259183,0.00017350352,0.0011589495,0.00014009507,0.000008981523,0.00007487703,2.280743e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000065572453,0.0000026627956,0.9895445,0.000024518173,0.0000074327695,5.237987e-7,0.00011657164,0.000026245109,0.0011248813,0.000048118047,0.000013186325,0.009084801],"study_design_scores_gemma":[0.00012553451,0.00014338284,0.9927247,0.000029790526,0.000021086114,0.000056473516,0.0003295313,0.00024789557,0.0028308695,0.0024417427,0.0009889859,0.00006000377],"about_ca_topic_score_codex":0.033339646,"about_ca_topic_score_gemma":0.76557344,"teacher_disagreement_score":0.7322338,"about_ca_system_score_codex":9.4981385e-7,"about_ca_system_score_gemma":0.00022712308,"threshold_uncertainty_score":0.97309744},"labels":[],"label_agreement":null},{"id":"W2164811954","doi":"10.1139/e05-016","title":"Electromagnetic image of the Trans-Hudson orogen THO94 transect","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Magnetotellurics; Anomaly (physics); Archean; Baltic Shield; Paleozoic; Seismology; Geophysics; Paleontology; Crust; Electrical resistivity and conductivity","score_opus":0.013635129887023856,"score_gpt":0.21534143885923013,"score_spread":0.20170630897220626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164811954","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887434,0.0014383737,0.00012453881,0.0033021998,0.00022085819,0.00007598859,0.00001677651,0.0000025098832,0.006075335],"genre_scores_gemma":[0.9933036,0.000023125916,0.006101445,0.00025891737,0.00015661617,9.421325e-8,2.9933358e-7,0.0000015007716,0.0001543853],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9985912,0.00017670153,0.00030832068,0.00012762063,0.00035233892,0.0004438494],"domain_scores_gemma":[0.99908674,0.00016566551,0.00014134834,0.00009554965,0.00008298,0.0004277049],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007720976,0.000099639146,0.00020045851,0.00014423099,0.00026802858,0.000062332525,0.000647081,0.000040319046,0.0019402219],"category_scores_gemma":[0.0001226058,0.00005648792,0.00017681142,0.00093196234,0.00053690624,0.00025841186,0.0000014386691,0.00021893873,0.000018466995],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058794594,0.000054606062,0.20499916,0.000040819406,0.00006181347,0.000045420293,0.0020068076,0.006303749,0.019157974,0.0009222609,0.0006088851,0.7657397],"study_design_scores_gemma":[0.00022144365,0.001141729,0.9669766,0.00003055659,0.000032489188,0.00012573536,0.000080649945,0.0013863571,0.015805313,0.002696307,0.011358629,0.00014420826],"about_ca_topic_score_codex":0.00617759,"about_ca_topic_score_gemma":0.15398066,"teacher_disagreement_score":0.7655955,"about_ca_system_score_codex":0.0000013249505,"about_ca_system_score_gemma":0.0009328361,"threshold_uncertainty_score":0.9989721},"labels":[],"label_agreement":null},{"id":"W2164887764","doi":"10.1139/e99-097","title":"Spatial and temporal trends in carbon storage of peatlands of continental western Canada through the Holocene","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":396,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Peat; Holocene; Carbon sink; Deglaciation; Subarctic climate; Geology; Permafrost; Carbon cycle; Continental shelf; Oceanography; Physical geography; Environmental science; Carbon fibers; Boreal; Climate change; Ecosystem; Ecology; Geography; Paleontology; Archaeology","score_opus":0.010184912357425064,"score_gpt":0.20903726938971726,"score_spread":0.1988523570322922,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164887764","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99327725,0.00015406561,0.0000010575667,0.00069320266,0.00009462991,0.000027093427,0.000013769534,4.101946e-7,0.0057385266],"genre_scores_gemma":[0.9996038,0.000018026461,0.000029823908,0.00008487301,0.000028266113,2.5834134e-7,0.0000013566558,0.0000020391744,0.00023152688],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999136,0.000050898372,0.00028074,0.000100767356,0.00020696734,0.00022467054],"domain_scores_gemma":[0.99959135,0.00003111347,0.00015711946,0.00006585591,0.000008570731,0.00014600946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034341955,0.00007092395,0.00019026706,0.00007171837,0.000069019385,0.000013831366,0.00024598214,0.000028298637,0.0006965907],"category_scores_gemma":[0.000011780261,0.000045416014,0.000026318025,0.00026707246,0.0006562102,0.0001084112,0.000012953182,0.00009191919,1.984685e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009451829,0.000005388312,0.9966221,0.0000010914465,0.0000028884006,0.000044306395,0.00042087983,0.0004677247,0.000027160848,0.0000026745934,0.00011963991,0.0022766807],"study_design_scores_gemma":[0.00032737537,0.00024576846,0.99630535,0.000014100407,0.000005312137,0.000079637204,0.00018169793,0.0002967554,0.0000943766,0.000022034928,0.0023731827,0.000054419143],"about_ca_topic_score_codex":0.9293051,"about_ca_topic_score_gemma":0.9964291,"teacher_disagreement_score":0.06712399,"about_ca_system_score_codex":0.000016262335,"about_ca_system_score_gemma":0.00035716363,"threshold_uncertainty_score":0.76271796},"labels":[],"label_agreement":null},{"id":"W2165053760","doi":"10.1139/e07-040","title":"Detrital zircon constraints on terrane ages and affinities and timing of orogenic events in the San Juan Islands and North Cascades, Washington","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Nappe; Zircon; Terrane; Metamorphism; Orogeny; Geochemistry; Plutonism; Geochronology; Precambrian; Population; Paleontology; Magmatism; Structural basin; Tectonics","score_opus":0.030854017960631898,"score_gpt":0.21464058467491914,"score_spread":0.18378656671428725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2165053760","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99686515,0.0017022137,0.000002425462,0.00031468974,0.000037121496,0.000034028428,0.000016773296,7.572393e-7,0.0010268631],"genre_scores_gemma":[0.99952114,0.000100356854,0.00017805344,0.00016493667,0.000026813486,3.7423302e-8,0.0000020907264,5.1208207e-7,0.000006067417],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991825,0.000045745815,0.00022394022,0.00011502902,0.0001882587,0.0002444825],"domain_scores_gemma":[0.9992834,0.00031275646,0.00010254554,0.000034493747,0.000025149004,0.0002417063],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00093994924,0.000077186516,0.00015852849,0.00019568365,0.00017511245,0.00004705751,0.0001518882,0.00003354497,0.00028776965],"category_scores_gemma":[0.00013953714,0.0000437617,0.000028318243,0.00027546723,0.0008429692,0.0001441786,0.00000462578,0.00014232904,6.2582933e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007329684,0.0000029648525,0.9879421,0.000005411987,0.000006701726,0.000054908975,0.00091768795,0.00003172825,0.00005162817,0.000016548274,0.000004059309,0.0109589035],"study_design_scores_gemma":[0.00014463549,0.00031643844,0.9960875,0.00003725017,0.000013351894,0.00022363098,0.0021149258,0.00008638704,0.00023188826,0.0006373601,0.00004433649,0.00006228335],"about_ca_topic_score_codex":0.0076292665,"about_ca_topic_score_gemma":0.6040948,"teacher_disagreement_score":0.5964656,"about_ca_system_score_codex":6.135671e-7,"about_ca_system_score_gemma":0.00007930034,"threshold_uncertainty_score":0.99897903},"labels":[],"label_agreement":null},{"id":"W2165134975","doi":"10.1139/cjes-2014-0184","title":"Hadrosaurid (<i>Edmontosaurus</i>) bonebeds from the Horseshoe Canyon Formation (Horsethief Member) at Drumheller, Alberta, Canada: geology, preliminary taphonomy, and significance","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; Royal Ontario Museum","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Taphonomy; Canyon; Overbank; Paleontology; Debris; Geomorphology; Fluvial; Oceanography","score_opus":0.021877538135810982,"score_gpt":0.19836415180359776,"score_spread":0.17648661366778678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2165134975","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9671622,0.0135702435,0.000015591604,0.01081322,0.0014844527,0.00013073419,0.00015293976,0.000003616126,0.0066669825],"genre_scores_gemma":[0.99732244,0.00013195805,0.00027409528,0.0016681417,0.00021794603,9.1552005e-7,0.00003824538,0.0000019242518,0.00034432008],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982625,0.00026425262,0.00040216383,0.00024212037,0.00026692176,0.00056200085],"domain_scores_gemma":[0.9980111,0.000568521,0.00031431892,0.00014702472,0.00012346046,0.00083553465],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009959385,0.0001683319,0.00026205712,0.00011870232,0.00088079757,0.00005548084,0.00054280605,0.0001299584,0.0004606516],"category_scores_gemma":[0.00029334243,0.00011356917,0.000045886984,0.00025488442,0.0015486248,0.00052918814,0.000015798843,0.0002867827,0.000026144771],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007669041,0.000002900823,0.9727664,0.0000025156007,0.00002233611,0.00009112465,0.00083332387,0.0017367892,0.000010764512,0.000084355284,0.022926403,0.0014464005],"study_design_scores_gemma":[0.0002586571,0.00038743793,0.8590519,0.000017885493,0.000022343183,0.00064540945,0.0010646504,0.0019777743,0.000042895645,0.0006125109,0.13575429,0.00016429147],"about_ca_topic_score_codex":0.9735436,"about_ca_topic_score_gemma":0.9998592,"teacher_disagreement_score":0.11371454,"about_ca_system_score_codex":0.000019912588,"about_ca_system_score_gemma":0.0051005865,"threshold_uncertainty_score":0.9048221},"labels":[],"label_agreement":null},{"id":"W2165240154","doi":"10.1139/cjes-2014-0072","title":"Multivariate analysis of isolated tyrannosaurid teeth from the Danek Bonebed, Horseshoe Canyon Formation, Alberta, Canada","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Ministerio de Economía y Competitividad","keywords":"Canyon; Geology; Horseshoe (symbol); Paleontology; Cretaceous; Multivariate statistics; Geomorphology; Mathematics; Statistics","score_opus":0.010259171587326001,"score_gpt":0.19301361994182398,"score_spread":0.18275444835449797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2165240154","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99267274,0.0010884042,0.00030523076,0.0022967847,0.00064167025,0.00005004993,0.00024247337,0.000001617728,0.0027010464],"genre_scores_gemma":[0.99893355,0.000018045084,0.00023617287,0.0006309194,0.000078031946,1.1788672e-7,0.00004612248,8.4670893e-7,0.000056185985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99859405,0.00025896652,0.00043039795,0.00014107826,0.0002211447,0.00035435997],"domain_scores_gemma":[0.99827933,0.00072368496,0.00038109566,0.00013218986,0.0001475353,0.00033616624],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00082202186,0.00010392861,0.0002872089,0.0002680566,0.00049530476,0.000031611533,0.00054916675,0.00006699858,0.0011476689],"category_scores_gemma":[0.0003609296,0.00006469947,0.000086941574,0.0009069152,0.00057335175,0.00035685382,0.0000034364837,0.00016413111,0.000007770655],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001721196,0.0000017542112,0.9825067,0.0000011527278,0.00013250319,0.000009368155,0.00040167308,0.015315681,0.000015465905,0.00010376264,0.0005457412,0.00094901887],"study_design_scores_gemma":[0.00012271538,0.00012066783,0.94772,0.000010974215,0.00013189614,0.000031032643,0.0003026901,0.041370366,0.000013618113,0.0001940107,0.009897757,0.00008430877],"about_ca_topic_score_codex":0.9909921,"about_ca_topic_score_gemma":0.99995023,"teacher_disagreement_score":0.034786705,"about_ca_system_score_codex":0.0000043045047,"about_ca_system_score_gemma":0.0022468248,"threshold_uncertainty_score":0.9997654},"labels":[],"label_agreement":null},{"id":"W2165925059","doi":"10.1139/e99-074","title":"Geologic transect across the Grenville orogen of Ontario and New York","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":257,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Geology; Laurentia; Pluton; Geochemistry; Continental arc; Thrust fault; Tectonics; Crust; Shear zone; Volcanic rock; Seismology; Volcano","score_opus":0.029577876772751005,"score_gpt":0.1923371509907609,"score_spread":0.1627592742180099,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2165925059","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9876242,0.0036004118,0.0000020649638,0.0018520909,0.00005975362,0.00002867626,0.000012182684,0.0000010927075,0.0068195076],"genre_scores_gemma":[0.99829656,0.00007489023,0.00030141123,0.0003957353,0.00004851687,3.5069508e-8,0.0000010080972,4.3333102e-7,0.00088139076],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99908435,0.00003929388,0.00024073159,0.00012038777,0.00019244346,0.00032279314],"domain_scores_gemma":[0.99923694,0.00008909582,0.000090744434,0.000065202665,0.000036687787,0.00048130582],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005246706,0.00007891383,0.00018059203,0.000047200756,0.00032277612,0.00006511073,0.0003864649,0.000039204293,0.04631504],"category_scores_gemma":[0.00004160558,0.000039401944,0.00008339467,0.00039375556,0.00087078614,0.00008950632,0.0000022973554,0.00014464537,0.000025536698],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000086277605,0.0000019135139,0.96135527,0.0000010252201,0.000013108246,0.000015764621,0.0009726939,0.0024176452,0.000011398361,0.00001454673,0.00008252071,0.035105497],"study_design_scores_gemma":[0.00011057332,0.00028409786,0.95449764,0.000008224314,0.00001802576,0.00011874839,0.00023473796,0.00012754629,0.00010410875,0.0048199114,0.03960446,0.000071946546],"about_ca_topic_score_codex":0.6400493,"about_ca_topic_score_gemma":0.9873617,"teacher_disagreement_score":0.34731245,"about_ca_system_score_codex":0.0000012618303,"about_ca_system_score_gemma":0.001026294,"threshold_uncertainty_score":0.95455676},"labels":[],"label_agreement":null},{"id":"W2166087016","doi":"10.1139/e01-050","title":"Anatomy of<i>Sinosauropteryx prima</i>from Liaoning, northeastern China","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":171,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Cretaceous; Paleontology; Feather; Geology; Tetrapod (structure); Yixian Formation; Mesozoic","score_opus":0.014042466653876495,"score_gpt":0.21738449391801956,"score_spread":0.20334202726414308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166087016","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9771615,0.0043344595,0.00007658563,0.0008714638,0.0008708567,0.000036958332,0.000052501502,0.0000034766258,0.01659219],"genre_scores_gemma":[0.99852234,0.00009690605,0.00085597043,0.00020649045,0.00017704976,5.5670533e-8,0.000007291486,0.0000010962482,0.00013278723],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987943,0.00010505913,0.00034039994,0.00016450095,0.00018864754,0.00040705],"domain_scores_gemma":[0.9990017,0.00009128001,0.0002687923,0.00010041609,0.00007611388,0.00046170535],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048969337,0.000105077626,0.00022538942,0.0002970045,0.00031086407,0.000031302687,0.000506733,0.00007530134,0.0022729693],"category_scores_gemma":[0.000078893936,0.00007956632,0.00008150727,0.0003795934,0.0010085352,0.00038208824,0.000003890191,0.00017597618,0.000056808763],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014611822,0.0000035472353,0.9924638,0.0000013403335,0.000013764946,0.00015903058,0.00016792458,0.00081759517,0.0000148826475,0.000071085415,0.00006000079,0.0062123714],"study_design_scores_gemma":[0.00014177996,0.00031646166,0.9831073,0.00002807649,0.000010735504,0.0005272474,0.00011233007,0.0009564049,0.000021531785,0.0006665703,0.014017511,0.000093999544],"about_ca_topic_score_codex":0.045357447,"about_ca_topic_score_gemma":0.6467041,"teacher_disagreement_score":0.6013466,"about_ca_system_score_codex":0.0000013284014,"about_ca_system_score_gemma":0.0010635224,"threshold_uncertainty_score":0.9986391},"labels":[],"label_agreement":null},{"id":"W2166240011","doi":"10.1139/e03-079","title":"Geodynamic evolution of the Pan-African belt in central Africa with special reference to Cameroon","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":587,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Craton; Geology; Archean; Tectonics; Shear zone; Terrane; Paleontology; Geochemistry; Earth science","score_opus":0.01232680330854427,"score_gpt":0.17328318621454694,"score_spread":0.16095638290600267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166240011","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9892914,0.00019424531,0.000022529568,0.0016617719,0.00010948392,0.000053432228,0.000021958673,0.0000010504832,0.0086441105],"genre_scores_gemma":[0.99936056,0.000004363591,0.0004491251,0.00006741671,0.00008028212,1.10723704e-7,8.827007e-7,5.788992e-7,0.000036650323],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988123,0.000043802233,0.0002518835,0.00014075544,0.00033237113,0.00041888884],"domain_scores_gemma":[0.99926245,0.000036243066,0.00014576934,0.000078988625,0.00007897022,0.00039759793],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030117383,0.00008108765,0.00017020154,0.00021257237,0.00016300804,0.000035789642,0.0004896936,0.000031800253,0.00085146877],"category_scores_gemma":[0.00011512447,0.00004232489,0.00005659066,0.0013918715,0.00049231725,0.00014008037,0.000006414112,0.00016638168,0.000010611616],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015998286,0.0000070725673,0.95247185,0.000001756454,0.000004843692,0.000019123441,0.0003503657,0.045328673,0.00007105564,0.00042665724,0.0000107552805,0.001291841],"study_design_scores_gemma":[0.00011645862,0.0003350219,0.99272263,0.00004148145,0.000008982795,0.000022453187,0.00052275666,0.00012676136,0.00008672452,0.005253918,0.00069084374,0.000071942166],"about_ca_topic_score_codex":0.13394763,"about_ca_topic_score_gemma":0.9293383,"teacher_disagreement_score":0.7953906,"about_ca_system_score_codex":0.000010409361,"about_ca_system_score_gemma":0.0010973623,"threshold_uncertainty_score":0.9322986},"labels":[],"label_agreement":null},{"id":"W2166414655","doi":"10.1139/e04-034","title":"A geothermally influenced wetland containing unconsolidated geochemical sediments","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Natural Environment Research Council; National Park Service","keywords":"Geology; Wetland; Geochemistry; Subaerial; Sediment; Sedimentary depositional environment; Organic matter; Hot spring; Dissolved silica; Geomorphology; Structural basin; Ecology; Paleontology","score_opus":0.010947986957228519,"score_gpt":0.22349889898382988,"score_spread":0.21255091202660137,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166414655","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9908859,0.00005344728,0.000039682294,0.0007168632,0.0001821535,0.000049607977,0.0000044805547,0.0000040611217,0.008063813],"genre_scores_gemma":[0.99834895,0.0000054160473,0.00074185786,0.00079226866,0.000052680014,7.238102e-7,0.0000010692735,0.0000036887866,0.00005333645],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988648,0.00002738099,0.00026813385,0.0001562125,0.0002317669,0.000451688],"domain_scores_gemma":[0.99911094,0.000031350435,0.00016068596,0.000076057906,0.0000232674,0.00059772434],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00050121796,0.000098283475,0.00016405263,0.00011617401,0.00027843623,0.00008145013,0.00039554283,0.00005827351,0.0014657878],"category_scores_gemma":[0.00009582582,0.000075615586,0.00004890754,0.000298033,0.00067365944,0.0003161453,0.000024753936,0.00015037194,0.00007574082],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013601763,0.000010832583,0.9843325,0.0000010032244,0.0000112524995,0.00021012985,0.0004291392,0.006799662,0.00757149,0.000090938105,0.00017158514,0.0003578497],"study_design_scores_gemma":[0.002277031,0.0011670582,0.9683984,0.000083804945,0.000023899252,0.00087813474,0.00038215154,0.00018403391,0.005406821,0.0029135342,0.01793236,0.0003527716],"about_ca_topic_score_codex":0.0098159285,"about_ca_topic_score_gemma":0.11399563,"teacher_disagreement_score":0.104179695,"about_ca_system_score_codex":0.000033053275,"about_ca_system_score_gemma":0.0006732407,"threshold_uncertainty_score":0.999447},"labels":[],"label_agreement":null},{"id":"W2166881647","doi":"10.1139/e07-071","title":"Dendroglaciological evidence for Holocene glacial advances in the Todd Icefield area, northern British Columbia Coast Mountains","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Geology; Holocene; Ice field; Glacial period; Glacier; Subfossil; Radiocarbon dating; Physical geography; Deglaciation; Westerlies; Archaeology; Paleontology; Oceanography; Geography","score_opus":0.0699041588278397,"score_gpt":0.27804131841328833,"score_spread":0.20813715958544865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166881647","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98721546,0.010017704,0.000025548661,0.0010899924,0.00034378894,0.00016615428,0.000027362075,0.0000028072106,0.0011111699],"genre_scores_gemma":[0.99798554,0.00090494787,0.00024942541,0.0006315665,0.0001297667,0.00000181717,0.000003724879,0.0000011608455,0.00009206865],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99830943,0.0002351259,0.0003251335,0.00021337488,0.00028647497,0.0006304514],"domain_scores_gemma":[0.9981712,0.0011477132,0.00014156112,0.00009304699,0.00014831393,0.00029816074],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018687573,0.00008405733,0.00023199224,0.0001256231,0.0011393428,0.00018890401,0.0008463742,0.00011320365,0.0009665478],"category_scores_gemma":[0.0010684539,0.00007210618,0.000087268476,0.00044075155,0.0017131539,0.00057027815,0.0000054723587,0.00036158503,0.000014769804],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019929923,0.0000055092896,0.9969233,0.0000044073035,0.0000029895994,0.00060711725,0.00027607256,0.0006077954,2.181604e-7,0.000006906026,0.00029552338,0.0012501794],"study_design_scores_gemma":[0.00021370461,0.0006510077,0.9914555,0.000046529865,0.0000051431703,0.003499151,0.00062428764,0.0002026345,0.0000012229916,0.00075937493,0.0024458459,0.00009557494],"about_ca_topic_score_codex":0.05940191,"about_ca_topic_score_gemma":0.9961752,"teacher_disagreement_score":0.9367733,"about_ca_system_score_codex":0.0000010151634,"about_ca_system_score_gemma":0.0013561909,"threshold_uncertainty_score":0.9999467},"labels":[],"label_agreement":null},{"id":"W2167099566","doi":"10.1139/e08-017","title":"Delineation of isograds in siliceous dolomitic marbles along the Sharbot Lake – Frontenac terrane boundary of the Grenville Province, southeastern Ontario","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Diopside; Tremolite; Geology; Calcite; Dolomite; Metamorphism; Geochemistry; Isograd; Petrography; Forsterite; Metamorphic facies; Quartz; Mineral; Metamorphic rock; Terrane; Mineralogy; Facies; Geomorphology; Paleontology; Chemistry","score_opus":0.02018535233454696,"score_gpt":0.17723568911056045,"score_spread":0.1570503367760135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2167099566","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996145,0.001098416,0.000007500823,0.001250466,0.00013642097,0.00007522691,0.000033584598,8.850151e-7,0.0012524955],"genre_scores_gemma":[0.9993185,0.000017152654,0.00015909103,0.0001627277,0.000038055223,1.7734982e-7,0.0000026040464,8.245557e-7,0.00030086222],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986983,0.000095442556,0.00046150413,0.00012739042,0.000340818,0.0002765757],"domain_scores_gemma":[0.9992008,0.000119444834,0.00028868348,0.000114660426,0.00009811359,0.00017824852],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00060426205,0.000092157454,0.00023090851,0.00014793717,0.0002777985,0.000028471342,0.00059131585,0.00004091058,0.0020742612],"category_scores_gemma":[0.00013743718,0.00004327959,0.00013768762,0.0004568106,0.001274896,0.00012450412,0.000010171346,0.00019430305,0.0000049045266],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011099122,0.0000068410445,0.9949929,0.0000042700044,0.000008978155,0.000018014412,0.0005187239,0.0032779959,0.000034871915,0.0000062345894,0.000018983585,0.0011010495],"study_design_scores_gemma":[0.00013170873,0.0001512514,0.9957233,0.00004551917,0.000016878683,0.00009040375,0.00037050134,0.0014218804,0.00009865306,0.00050386344,0.0013847487,0.00006130373],"about_ca_topic_score_codex":0.461793,"about_ca_topic_score_gemma":0.9978897,"teacher_disagreement_score":0.5360967,"about_ca_system_score_codex":0.0000021728852,"about_ca_system_score_gemma":0.0013880472,"threshold_uncertainty_score":0.998838},"labels":[],"label_agreement":null},{"id":"W2167174059","doi":"10.1139/e06-096","title":"Magnetic fabric studies of the Nipissing sill province and Senneterre dykes, Canadian Shield, and implications for emplacement","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Carleton University; Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Sill; Paleomagnetism; Geochemistry; Outcrop; Paleontology","score_opus":0.023552937615194117,"score_gpt":0.26621362322737707,"score_spread":0.24266068561218296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2167174059","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9643492,0.032235056,0.000049968836,0.0024627666,0.00016500379,0.00017036815,0.000038286693,4.8391826e-7,0.00052886794],"genre_scores_gemma":[0.9981855,0.00037932646,0.0008889675,0.00023139315,0.00006327755,0.0000016029852,7.6895526e-7,0.0000030886029,0.00024606736],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99929684,0.000019352108,0.00020429226,0.00013467907,0.00006354469,0.0002812921],"domain_scores_gemma":[0.9993676,0.000041052106,0.00011494175,0.000089894165,0.00011274628,0.00027378573],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047929218,0.000081461454,0.00011611865,0.000110173474,0.00046713656,0.000035819972,0.00015806935,0.000037466656,0.0000031707305],"category_scores_gemma":[0.00015227016,0.000058010126,0.000033583474,0.00010291864,0.0006857431,0.000008971254,0.00002319936,0.000043654076,7.4903994e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019395977,0.000009629086,0.9344736,0.00009580981,0.00007051658,0.000008793962,0.0017528898,0.00005700046,0.022174472,0.0008384199,0.002259013,0.038240507],"study_design_scores_gemma":[0.00029428402,0.0011970191,0.9615592,0.00006529173,0.000040479907,0.00016792738,0.0022161666,0.000008877603,0.0018865126,0.0004920556,0.031930484,0.00014173932],"about_ca_topic_score_codex":0.0099236965,"about_ca_topic_score_gemma":0.85751975,"teacher_disagreement_score":0.84759605,"about_ca_system_score_codex":0.000003857183,"about_ca_system_score_gemma":0.0008135983,"threshold_uncertainty_score":0.9966693},"labels":[],"label_agreement":null},{"id":"W2167352413","doi":"10.1139/cjes-2015-0090","title":"Modelled nearshore sediment transport in open-water conditions, central north shore of Prince Edward Island, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; University of Guelph; Geological Survey of Canada","funders":"Deltares","keywords":"Sediment transport; Shore; Bed load; Geology; Submarine pipeline; Storm; Current (fluid); Oceanography; Deposition (geology); Suspended load; Longshore drift; Sediment; Erosion; Prevailing winds; Winter storm; Hydrology (agriculture); Geomorphology; Geotechnical engineering","score_opus":0.0168095998076107,"score_gpt":0.20104785383808313,"score_spread":0.18423825403047242,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2167352413","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945931,0.000120431636,0.000031552652,0.00071887724,0.0004802944,0.00012274325,0.0002839001,0.0000010251417,0.0036481204],"genre_scores_gemma":[0.99930006,0.000013340834,0.0002341638,0.00015878455,0.000042240616,2.0991034e-7,0.000053192212,0.0000016544931,0.00019633361],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985984,0.000039356124,0.00038352277,0.00014280966,0.00037970574,0.0004562372],"domain_scores_gemma":[0.9988642,0.00002569065,0.00010723512,0.000082192266,0.00011484381,0.00080586143],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048347382,0.00010310273,0.00022724367,0.00017304366,0.000108594955,0.000060546994,0.0005856592,0.000026711537,0.0005964762],"category_scores_gemma":[0.0000247322,0.000070877104,0.00003856018,0.0002932835,0.0002331657,0.0004131837,0.00001170222,0.00014361035,0.0000024619108],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001910617,0.0000050722224,0.8608656,0.000004575055,0.0000057110847,0.00015059512,0.0005618927,0.1372801,0.0000010175527,0.000022872751,0.00015616971,0.00092731294],"study_design_scores_gemma":[0.0005969955,0.00032371053,0.9681429,0.000047287547,0.000012003697,0.00008214223,0.0010878397,0.018312203,0.000035910627,0.0004030547,0.010772681,0.00018321787],"about_ca_topic_score_codex":0.92026657,"about_ca_topic_score_gemma":0.99988043,"teacher_disagreement_score":0.118967906,"about_ca_system_score_codex":0.000010537653,"about_ca_system_score_gemma":0.0073500266,"threshold_uncertainty_score":0.99827737},"labels":[],"label_agreement":null},{"id":"W2167711755","doi":"10.1139/e06-092","title":"Archean crustal growth by lateral accretion of juvenile supracrustal belts in the south-central Wyoming Province","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Terrane; Pluton; Geochemistry; Plutonism; Archean; Accretion (finance); Magmatism; Basement; Zircon; Continental crust; Crust; Paleontology; Tectonics","score_opus":0.010087767318337515,"score_gpt":0.18106366808598814,"score_spread":0.17097590076765062,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2167711755","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99543226,0.00047921416,0.000016430044,0.00151624,0.00007981791,0.000052652693,0.000058155427,0.0000016030666,0.0023636438],"genre_scores_gemma":[0.99947006,0.000004794835,0.00024268421,0.00013242409,0.00008857496,1.1379753e-7,0.00001385398,7.6503085e-7,0.00004673889],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99855465,0.0001033577,0.00039156785,0.00014171764,0.0003426679,0.00046602704],"domain_scores_gemma":[0.99933666,0.00010433758,0.00021194463,0.000055072625,0.00006392796,0.00022808221],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00083096506,0.00009250624,0.00018807636,0.00016489431,0.0001943341,0.00009855563,0.00045917195,0.00004312629,0.0010153466],"category_scores_gemma":[0.0001231215,0.0000540758,0.000096910604,0.0005072276,0.00055995904,0.00029814703,0.0000049899854,0.00020393229,0.0000059515733],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009774748,0.000008999609,0.9971257,0.0000044500903,0.0000029269354,0.000044348384,0.00025364992,0.0014680382,0.00018277287,0.00014495425,0.00028390737,0.0004705169],"study_design_scores_gemma":[0.00017084072,0.00022610526,0.9923997,0.000021793749,0.000011701428,0.000050861465,0.000708818,0.0015024984,0.0005839452,0.0034208293,0.000801074,0.00010184214],"about_ca_topic_score_codex":0.09786032,"about_ca_topic_score_gemma":0.56164825,"teacher_disagreement_score":0.4637879,"about_ca_system_score_codex":0.0000021457952,"about_ca_system_score_gemma":0.00050661876,"threshold_uncertainty_score":0.99989784},"labels":[],"label_agreement":null},{"id":"W2168053637","doi":"10.1139/e02-004","title":"The southeastern Churchill Province: synthesis of a Paleoproterozoic transpressional orogen","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Memorial University of Newfoundland; Government of Newfoundland and Labrador","funders":"","keywords":"Craton; Geology; Transpression; Subduction; Archean; Sinistral and dextral; Tectonics; Baltic Shield; Crust; Seismology; Paleontology; Geochemistry","score_opus":0.017974605961886055,"score_gpt":0.1774660151523314,"score_spread":0.15949140919044535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168053637","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9885205,0.0031657522,0.000010267563,0.00225982,0.00011048079,0.00005382167,0.000045034565,0.0000020633952,0.0058322633],"genre_scores_gemma":[0.99938345,0.00005625945,0.00025202177,0.00008985039,0.00006952738,2.692328e-7,4.620306e-7,7.876669e-7,0.0001473641],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987124,0.00008934098,0.0003432862,0.00012918506,0.00037561124,0.00035012848],"domain_scores_gemma":[0.99886465,0.0003025449,0.00020525584,0.000090603615,0.00008425296,0.0004527081],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006433288,0.00009019404,0.00018083263,0.0001120681,0.00044977432,0.00007571416,0.0006243587,0.000037261452,0.0075666793],"category_scores_gemma":[0.00023934628,0.00004376238,0.00015066088,0.00032391248,0.0008861884,0.00014053998,0.0000035995681,0.0001360975,0.000047476806],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000073456895,0.0000058107157,0.97840416,0.000005321125,0.000020607238,0.000022495089,0.00013281591,0.0007491745,0.00004806024,0.000044797915,0.000039371138,0.020520013],"study_design_scores_gemma":[0.00014309087,0.00033220407,0.9837076,0.00008731777,0.000047340247,0.00010720078,0.00041834728,0.004934256,0.0012940313,0.0044748825,0.0042876843,0.00016604792],"about_ca_topic_score_codex":0.0061778952,"about_ca_topic_score_gemma":0.26719666,"teacher_disagreement_score":0.26101875,"about_ca_system_score_codex":4.116059e-7,"about_ca_system_score_gemma":0.00022801905,"threshold_uncertainty_score":0.99334055},"labels":[],"label_agreement":null},{"id":"W2168097570","doi":"10.1139/e06-099","title":"Tempestite frequency curves: a key to Late Ordovician and Early Silurian subsidence, sea-level change, and orbital forcing in the Anticosti foreland basin, Quebec, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":97,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Foreland basin; Ordovician; Paleontology; Subsidence; Orbital forcing; Sedimentary rock; Geomorphology; Glacial period; Structural basin","score_opus":0.036160113896778145,"score_gpt":0.21757060488484983,"score_spread":0.1814104909880717,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168097570","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9895701,0.0037799336,0.000025360803,0.0048815715,0.00016210662,0.00015172073,0.00004548137,0.0000016855595,0.0013820843],"genre_scores_gemma":[0.99720997,0.00010441822,0.00055799074,0.0020216666,0.00006165315,3.5150612e-7,0.0000022605952,0.000001221902,0.00004045573],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987437,0.000048481907,0.00032061877,0.00013948133,0.0002914456,0.0004562781],"domain_scores_gemma":[0.99890256,0.0002596673,0.00012041099,0.000061126746,0.00009815694,0.0005580837],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015536335,0.00010799241,0.00016683241,0.00030259253,0.0004755689,0.0002469353,0.0003019539,0.00003768535,0.00010822023],"category_scores_gemma":[0.00033529595,0.00006638376,0.000017866807,0.0008031266,0.00024708323,0.0007546652,0.000005305016,0.00017271155,0.000002536079],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000033400197,0.000001048626,0.9962581,0.000016755055,0.0000020872005,0.000144467,0.00089859543,0.000057262674,7.5349914e-7,0.00007690105,0.00008015884,0.0024605652],"study_design_scores_gemma":[0.00008783111,0.00018076964,0.9961371,0.00020452167,0.0000058426176,0.00019107379,0.0008891069,0.000085705535,0.0000030290914,0.0005205832,0.0015889781,0.00010544971],"about_ca_topic_score_codex":0.975984,"about_ca_topic_score_gemma":0.9999127,"teacher_disagreement_score":0.0239287,"about_ca_system_score_codex":0.0000036290035,"about_ca_system_score_gemma":0.0012016322,"threshold_uncertainty_score":0.36577395},"labels":[],"label_agreement":null},{"id":"W2168120787","doi":"10.1139/e05-066","title":"Turonian (Upper Cretaceous) lithostratigraphy and biochronology, southern Gulf Islands, British Columbia, and northern San Juan Islands, Washington State","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Conglomerate; Siltstone; Cretaceous; Paleontology; Clastic rock; Outcrop; Thrust fault; Lithostratigraphy; Facies; Marine transgression; Structural basin; Fault (geology)","score_opus":0.008343911571882058,"score_gpt":0.1844778448324464,"score_spread":0.17613393326056434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168120787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98622686,0.010542173,0.000016302598,0.0008037528,0.000118787306,0.00006905349,0.00017918971,0.0000068306877,0.0020370318],"genre_scores_gemma":[0.9979401,0.00041269374,0.0009418995,0.00032204765,0.00009701875,1.973327e-7,0.000006866884,0.000002149661,0.00027697696],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883074,0.000057434347,0.00030393276,0.00019706,0.00018156241,0.00042926642],"domain_scores_gemma":[0.99904656,0.000069357935,0.0001661484,0.000066734094,0.000097618795,0.0005535768],"candidate_categories":["scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00054005533,0.000105123356,0.00019415212,0.0001611824,0.00075405894,0.0011204673,0.0002560774,0.000068030364,0.0020710153],"category_scores_gemma":[0.00006868654,0.00009959745,0.000043424556,0.00029188217,0.0008312421,0.00060453994,0.000006236326,0.00019658683,0.00002060307],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000024883002,0.0000025266825,0.94292665,0.000006724581,0.000009640054,0.000019435538,0.0010992074,0.00015507003,0.000001633737,0.0000019702586,0.00017514173,0.055599537],"study_design_scores_gemma":[0.00022892767,0.0004699815,0.9732879,0.00004714097,0.0000137748875,0.00062456925,0.0016588593,0.00058102026,0.0000046386817,0.0012247848,0.021683276,0.00017512744],"about_ca_topic_score_codex":0.11577225,"about_ca_topic_score_gemma":0.9920291,"teacher_disagreement_score":0.8762569,"about_ca_system_score_codex":0.0000011583975,"about_ca_system_score_gemma":0.00051928253,"threshold_uncertainty_score":0.9999165},"labels":[],"label_agreement":null},{"id":"W2168232570","doi":"10.1139/e05-115","title":"Geochemical evidence for the origin of late Quaternary loess in central Alaska","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":123,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Loess; Geology; Quaternary; Aeolian processes; Katabatic wind; Glacial period; Glacier; Silt; Geochemistry; Geomorphology; Weathering; Climatology; Paleontology","score_opus":0.054299458702354045,"score_gpt":0.28416887293900644,"score_spread":0.22986941423665241,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168232570","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929851,0.0037868614,0.000025906367,0.0022247862,0.00037069037,0.00008857346,0.00001303546,9.4967305e-7,0.0005040864],"genre_scores_gemma":[0.9993673,0.00006157466,0.00029599754,0.00007293034,0.00008496368,3.1221578e-7,0.0000015559593,7.4540486e-7,0.00011460492],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99882394,0.000086617474,0.00029461106,0.00011407629,0.00018475926,0.00049598725],"domain_scores_gemma":[0.99857664,0.000955297,0.0001308193,0.00007300246,0.00007747462,0.00018674893],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013352891,0.000066167864,0.00015657653,0.00019782047,0.00019855735,0.0000363233,0.0005521755,0.00005837963,0.00044522216],"category_scores_gemma":[0.00022770454,0.00004069317,0.00006170949,0.00032041565,0.0010264347,0.00022996047,0.0000035330982,0.00018619382,0.0000092241735],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025625312,0.0000025246147,0.9935407,0.0000075639277,0.0000039884126,0.000045536945,0.0000816742,0.005917655,0.000013439199,0.00010732712,0.00007833776,0.00017561845],"study_design_scores_gemma":[0.00015332866,0.00014220671,0.9937574,0.00005534271,0.000005866239,0.00010541523,0.00008586416,0.0030258114,0.00023845195,0.0017640465,0.00061612076,0.00005009692],"about_ca_topic_score_codex":0.023051102,"about_ca_topic_score_gemma":0.6135658,"teacher_disagreement_score":0.5905147,"about_ca_system_score_codex":5.940811e-7,"about_ca_system_score_gemma":0.0011548576,"threshold_uncertainty_score":0.98345447},"labels":[],"label_agreement":null},{"id":"W2168578219","doi":"10.1139/e09-013","title":"Provenance of detrital muscovite in Cambrian Avalonia of Maritime Canada: <sup>40</sup>Ar/<sup>39</sup>Ar ages and chemical compositions","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Mount Saint Vincent University; Acadia University; Dalhousie University","funders":"","keywords":"Geology; Muscovite; Clastic rock; Provenance; Conglomerate; Detritus; Metamorphic rock; Nova scotia; Geochemistry; Andalusite; Mineralogy; Paleontology; Sedimentary rock; Quartz; Oceanography","score_opus":0.008051280185025655,"score_gpt":0.1777925010704612,"score_spread":0.16974122088543556,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168578219","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939391,0.0018733436,0.0000045159636,0.002817107,0.00003304665,0.00008240971,0.00016769757,0.0000023176126,0.0010804342],"genre_scores_gemma":[0.9985098,0.0000420034,0.0010109046,0.00032122488,0.000056575715,2.0446383e-7,0.000013170615,0.000001392893,0.000044679266],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99808484,0.000076882076,0.0006109529,0.00025998926,0.00044173255,0.0005255755],"domain_scores_gemma":[0.9986186,0.00015128082,0.000252879,0.00011142446,0.00015594772,0.0007098691],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005133652,0.00016590694,0.0004729392,0.00032451612,0.00017065737,0.000060294402,0.0004613483,0.00008210713,0.00053214916],"category_scores_gemma":[0.00024965993,0.00012627205,0.00010873795,0.00093797466,0.00072641624,0.0003005973,0.000010502178,0.00026583005,0.0000028462662],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027563432,0.00002760906,0.9843708,0.000023143974,0.000020592594,0.0001797369,0.00019315431,0.01057006,0.00097367016,0.000122061116,0.00013978181,0.0033518232],"study_design_scores_gemma":[0.00033981883,0.00044749165,0.98637646,0.00015514718,0.000032035256,0.00014993658,0.00032837875,0.008463024,0.001152807,0.0019635456,0.0003851922,0.00020616082],"about_ca_topic_score_codex":0.61426467,"about_ca_topic_score_gemma":0.9215804,"teacher_disagreement_score":0.30731574,"about_ca_system_score_codex":0.000007711071,"about_ca_system_score_gemma":0.0012898966,"threshold_uncertainty_score":0.58266604},"labels":[],"label_agreement":null},{"id":"W2168678027","doi":"10.1139/e04-039","title":"Stratigraphic evidence for multiple Holocene advances of Lillooet Glacier, southern Coast Mountains, British Columbia","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Geological Society of America; Simon Fraser University; National Science Foundation","keywords":"Moraine; Geology; Holocene; Glacier; Radiocarbon dating; Landform; Physical geography; Paleontology; Stratigraphy; Glacier mass balance; Paleosol; Geomorphology; Rock glacier; Loess; Geography","score_opus":0.0382047785131436,"score_gpt":0.2604663381037823,"score_spread":0.22226155959063867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168678027","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9844697,0.014286212,0.000072124625,0.0003266365,0.00030831812,0.0001659408,0.00018760515,0.000003742066,0.00017972007],"genre_scores_gemma":[0.9973034,0.00039485955,0.0020275053,0.00010867561,0.0000632347,7.8480844e-7,0.0000056007757,0.0000020073742,0.00009390913],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983982,0.00009405427,0.00040981444,0.00021790792,0.00030301645,0.0005770092],"domain_scores_gemma":[0.99835277,0.0004609927,0.00028300876,0.00010422211,0.0002882616,0.0005107738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014382283,0.00009116293,0.00028313432,0.00020327898,0.0006737935,0.00020649025,0.0006254563,0.00009792089,0.0005352037],"category_scores_gemma":[0.0008067853,0.0000997163,0.000115436495,0.00052802684,0.0018358001,0.0006040226,0.000004427006,0.00021030578,0.000011751998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018702518,0.000006419146,0.99499637,0.000025660824,0.000012313515,0.00006748324,0.00019897065,0.003496429,0.000006476949,0.000014224668,0.000033698143,0.0011232703],"study_design_scores_gemma":[0.0005572123,0.000923865,0.99303705,0.00021009977,0.000014256502,0.000529791,0.0012927616,0.00019563345,0.000046508987,0.0025586297,0.00050596514,0.00012820827],"about_ca_topic_score_codex":0.17397992,"about_ca_topic_score_gemma":0.99411094,"teacher_disagreement_score":0.820131,"about_ca_system_score_codex":7.6513135e-7,"about_ca_system_score_gemma":0.002314107,"threshold_uncertainty_score":0.8315206},"labels":[],"label_agreement":null},{"id":"W2168720074","doi":"10.1139/e08-012","title":"Paleomagnetism and counterclockwise tectonic rotation of the Upper Oligocene Sooke Formation, southern Vancouver Island, British Columbia","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Redlen Technologies (Canada)","funders":"California Institute of Technology; American Physical Therapy Association; American Chemical Society Petroleum Research Fund; National Science Foundation","keywords":"Clockwise; Geology; Paleomagnetism; Paleontology; Peninsula; Bay; Basement; Volcanic rock; Tectonics; Volcano; Fold (higher-order function); Seismology; Oceanography; Archaeology","score_opus":0.010982485689446818,"score_gpt":0.1871882379720257,"score_spread":0.17620575228257887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168720074","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99517304,0.0019533092,0.0000071167974,0.00018706537,0.0003333153,0.00008105456,0.00004850496,0.0000014825943,0.002215097],"genre_scores_gemma":[0.9988776,0.000157509,0.00012778168,0.0001244996,0.000030221076,2.2586536e-7,0.0000013344367,0.0000010522542,0.00067977194],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990273,0.00010432123,0.00025394853,0.00009778713,0.00023329303,0.0002833501],"domain_scores_gemma":[0.999314,0.000088982095,0.00017070957,0.00006990787,0.00014954404,0.00020687403],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000519896,0.000052995492,0.0001396922,0.00009550542,0.00076423684,0.000083801235,0.00028579557,0.000061592546,0.0018270729],"category_scores_gemma":[0.00009981325,0.000047129106,0.00004628987,0.00026575266,0.001324688,0.00030605748,0.0000049178116,0.0001624119,0.00001409699],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000028695279,0.0000017117327,0.99804497,0.0000065955646,0.0000046875552,0.00003184612,0.0005498104,0.00017644916,0.0000018923265,0.0000015977198,0.0006162906,0.0005612601],"study_design_scores_gemma":[0.00022195707,0.00015648773,0.9958191,0.000039464067,0.000006475763,0.0014571673,0.0005397412,0.0004757903,0.000010862034,0.00038177846,0.0008335545,0.00005764218],"about_ca_topic_score_codex":0.058312867,"about_ca_topic_score_gemma":0.9928422,"teacher_disagreement_score":0.93452936,"about_ca_system_score_codex":4.5585583e-7,"about_ca_system_score_gemma":0.00077274104,"threshold_uncertainty_score":0.99908537},"labels":[],"label_agreement":null},{"id":"W2169626674","doi":"10.1139/cjes-2014-0050","title":"<i>Albertosaurus</i> (Dinosauria: Theropoda) material from an <i>Edmontosaurus</i> bonebed (Horseshoe Canyon Formation) near Edmonton: clarification of palaeogeographic distribution","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Canyon; Geology; Horseshoe (symbol); Paleontology; Theropoda; Cretaceous; Geomorphology","score_opus":0.010243385891071986,"score_gpt":0.19821799009208219,"score_spread":0.1879746042010102,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2169626674","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99397975,0.00073626026,0.0005189043,0.0010885611,0.0012019585,0.00010719079,0.00079589785,0.000009441072,0.0015620309],"genre_scores_gemma":[0.99787706,0.000058666043,0.00083115755,0.0002672468,0.00038008846,5.9618765e-7,0.0005735666,0.0000024018993,0.0000092333175],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979262,0.00042433053,0.00061892613,0.00024817282,0.00030645833,0.0004759358],"domain_scores_gemma":[0.998382,0.0001436879,0.00055656105,0.0002012173,0.00018722474,0.0005293366],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012768266,0.00017080338,0.00032700528,0.00020138735,0.0007445575,0.00011110385,0.00057782215,0.0002117624,0.00090361846],"category_scores_gemma":[0.0001512878,0.00013683997,0.00010691991,0.00044433394,0.001182125,0.0013670161,0.000004810922,0.000220652,0.000019466088],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009015886,0.000017876251,0.99139893,0.000007683575,0.00002506782,0.00001080193,0.00030553454,0.0008948595,0.0008652092,0.0011551644,0.00039972615,0.004828989],"study_design_scores_gemma":[0.00030671712,0.0006865667,0.97586954,0.00003231782,0.000036672525,0.00009468016,0.00019974705,0.00386069,0.0006606361,0.0031603985,0.014911623,0.00018040591],"about_ca_topic_score_codex":0.053463716,"about_ca_topic_score_gemma":0.6763477,"teacher_disagreement_score":0.622884,"about_ca_system_score_codex":0.0000043076425,"about_ca_system_score_gemma":0.0007504359,"threshold_uncertainty_score":0.98939884},"labels":[],"label_agreement":null},{"id":"W2169642074","doi":"10.1139/e03-044","title":"Experimental study of iron and silica immobilization by bacteria in mixed Fe-Si systems: implications for microbial silicification in hot springs","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Bacteria; Iron bacteria; Precipitation; Chemistry; Sorption; Chemical engineering; Environmental chemistry; Inorganic chemistry; Adsorption; Geology; Organic chemistry","score_opus":0.01713470042674893,"score_gpt":0.22433722325537214,"score_spread":0.20720252282862323,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2169642074","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988435,0.0006966975,0.000010945481,0.00006236494,0.00007483981,0.00018691643,0.000038652746,7.1427667e-7,0.00008537903],"genre_scores_gemma":[0.9998398,0.000008701622,0.00010440134,0.000010349608,0.00000950651,0.0000018766689,0.000011805354,9.555919e-7,0.00001263319],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991952,0.000060535145,0.00035006457,0.00014267922,0.00007903133,0.00017245744],"domain_scores_gemma":[0.99954355,0.00004253006,0.00017427134,0.00005760801,0.000041561467,0.0001405105],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005701886,0.00006477721,0.00013879563,0.00019345628,0.00012703793,0.000061762184,0.0001330562,0.00002667107,0.000051185372],"category_scores_gemma":[0.000051635572,0.000057754456,0.000021293805,0.00037763722,0.0001097167,0.00025195576,0.0000016722615,0.0000422021,4.027134e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001285305,0.000057871952,0.9095097,0.00001114774,0.0000041457706,7.3385473e-7,0.0006842098,0.0020462335,0.08740322,0.000026439415,0.000018804403,0.00022461184],"study_design_scores_gemma":[0.00050325657,0.00051247625,0.975342,0.000024319765,0.000010506378,0.000017295486,0.010252003,0.0006864586,0.012182281,0.000025851421,0.0003451849,0.000098411794],"about_ca_topic_score_codex":0.01676432,"about_ca_topic_score_gemma":0.20964469,"teacher_disagreement_score":0.19288036,"about_ca_system_score_codex":0.0000052186697,"about_ca_system_score_gemma":0.00017578014,"threshold_uncertainty_score":0.9897831},"labels":[],"label_agreement":null},{"id":"W2169982338","doi":"10.1139/e04-067","title":"Composition, age, and origin of granitoid rocks in the Davin Lake area, Rottenstone Domain, Trans-Hudson Orogen, northern Saskatchewan","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Batholith; Pluton; Mafic; Pegmatite; Volcanic rock; Porphyritic; Xenolith; Tectonics; Petrology; Mantle (geology); Volcano; Seismology; Paleontology; Quartz","score_opus":0.014234612112160056,"score_gpt":0.19667501860006248,"score_spread":0.1824404064879024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2169982338","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936949,0.0011521352,0.000038196507,0.0037272864,0.000044404518,0.000058435948,0.000040742518,0.000001643398,0.0012422247],"genre_scores_gemma":[0.998527,0.000031505806,0.00080529886,0.00054063887,0.00006464395,1.9349842e-7,0.00000825089,8.3915586e-7,0.000021645023],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99879336,0.00009501035,0.00035325036,0.00014539885,0.00030461192,0.00030838576],"domain_scores_gemma":[0.9992677,0.00011115941,0.00014292015,0.00007524593,0.000085924476,0.00031703155],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00077022205,0.000104116174,0.00023098986,0.00018595204,0.0002359182,0.00006925789,0.00039743367,0.000045164717,0.0014245801],"category_scores_gemma":[0.000028346054,0.000059626804,0.000082809216,0.00060232665,0.00064359495,0.0001875704,0.000002568431,0.00018551866,0.000006425684],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000908384,0.000011125734,0.98968,0.000003262881,0.000009212655,0.00009640295,0.0013336672,0.004586182,0.00017818341,0.000012908317,0.000036730165,0.004043245],"study_design_scores_gemma":[0.00026495883,0.00024927274,0.9859608,0.000036182577,0.000022887356,0.00018766327,0.002886918,0.00036480068,0.00019930337,0.0031512396,0.006546388,0.00012961919],"about_ca_topic_score_codex":0.037285604,"about_ca_topic_score_gemma":0.98437446,"teacher_disagreement_score":0.94708884,"about_ca_system_score_codex":0.0000012872586,"about_ca_system_score_gemma":0.0002762254,"threshold_uncertainty_score":0.99948823},"labels":[],"label_agreement":null},{"id":"W2170337777","doi":"10.1139/cjes-2015-0113","title":"A revision of the Late Cretaceous–Paleocene eutherian mammal <i>Cimolestes</i> Marsh, 1889","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Paleogene; Paleontology; Cretaceous; Monophyly; Geology; Mammal; Dentition; Taxon; Range (aeronautics); Zoology; Biology; Phylogenetic tree; Clade","score_opus":0.036396692742065175,"score_gpt":0.2291882286006845,"score_spread":0.19279153585861933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2170337777","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.961628,0.009291969,0.00001217761,0.002618837,0.0011877535,0.00007349077,0.000029260707,0.0000032078804,0.025155311],"genre_scores_gemma":[0.9982868,0.000073457995,0.0005163992,0.0004242239,0.00009876981,3.7022353e-8,6.049473e-7,0.0000013760659,0.0005983474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986841,0.00017450607,0.00034154818,0.00011014404,0.00035390278,0.0003357678],"domain_scores_gemma":[0.99876446,0.000084765496,0.00031467873,0.00012460221,0.00019476713,0.00051671994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013160018,0.00010159091,0.00021632298,0.00015573397,0.00035866216,0.000059167316,0.0005643573,0.000053562755,0.00038122202],"category_scores_gemma":[0.00028243568,0.000060348513,0.000096620504,0.0005105466,0.0010148787,0.00023069525,0.000007904968,0.00016294011,0.000031968175],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009483613,0.0000019594368,0.9943833,0.000004408914,0.000009806749,0.00001814787,0.00059062435,0.0011268856,0.0000054726193,0.000052544474,0.0008019102,0.002995492],"study_design_scores_gemma":[0.0002577545,0.00030288275,0.9292599,0.00009823176,0.000020138903,0.00019605097,0.001406624,0.00032898586,0.000054286265,0.0003539042,0.067613356,0.00010788221],"about_ca_topic_score_codex":0.0053847125,"about_ca_topic_score_gemma":0.6068988,"teacher_disagreement_score":0.6015141,"about_ca_system_score_codex":0.0000018947313,"about_ca_system_score_gemma":0.0014605663,"threshold_uncertainty_score":0.81401104},"labels":[],"label_agreement":null},{"id":"W2170770444","doi":"10.1139/cjes-2013-0027","title":"Evidence of discharging saline formation water to the Athabasca River in the oil sands mining region, northern Alberta","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Alberta Innovates; Alberta Environment and Protected Areas; University of Calgary; University of Victoria","funders":"Suncor Energy Incorporated; Canadian Natural Resources Limited","keywords":"Geology; Tributary; Hydrology (agriculture); Oil sands; Groundwater; Saline water; Sedimentary rock; Halite; Geochemistry; Geomorphology; Structural basin; Salinity; Oceanography","score_opus":0.0263458524935124,"score_gpt":0.2188446906451428,"score_spread":0.1924988381516304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2170770444","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9894316,0.0003618558,0.00047313015,0.008973808,0.00009132162,0.000035320976,2.9380521e-7,0.0000014626711,0.0006311713],"genre_scores_gemma":[0.9995533,0.000045399003,0.000077894976,0.0001652944,0.000053822663,0.0000023194993,3.3911596e-7,0.0000028298855,0.00009875339],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992521,0.00004094888,0.00026522644,0.00005285674,0.00020422469,0.00018465861],"domain_scores_gemma":[0.99957097,0.00006321738,0.000054254717,0.00010418794,0.000083825405,0.00012353834],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006645043,0.00005622985,0.00009351948,0.00024314674,0.00013556637,0.000106616455,0.00043094103,0.000016491538,0.000050899293],"category_scores_gemma":[0.00009801659,0.000025341902,0.00004855117,0.00045723858,0.00009100322,0.00067894463,0.000007293753,0.00008175374,0.000016416501],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003854643,0.0000054214656,0.13627325,0.000036613546,0.000030448813,0.000014137365,0.114867955,0.742125,0.00070056197,0.00006333534,0.0011849084,0.0046945377],"study_design_scores_gemma":[0.0005646815,0.00037739973,0.11440877,0.0018946348,0.00008337633,0.00024425454,0.04302097,0.8178486,0.004573756,0.0004815651,0.015892059,0.00060994044],"about_ca_topic_score_codex":0.011243361,"about_ca_topic_score_gemma":0.5415442,"teacher_disagreement_score":0.53030086,"about_ca_system_score_codex":0.0000074255045,"about_ca_system_score_gemma":0.000075882526,"threshold_uncertainty_score":0.9953409},"labels":[],"label_agreement":null},{"id":"W2170880857","doi":"10.1139/e99-102","title":"<i>Amia</i>cf.<i>pattersoni</i>from the Paleocene Paskapoo Formation of Alberta","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fish Ecology and Management Studies","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Fauna; Geology; Paleontology; Genus; Sensu; Range (aeronautics); Fish <Actinopterygii>; Paleogene; Assemblage (archaeology); Freshwater fish; Ecology; Cretaceous; Biology; Fishery","score_opus":0.009706479825706568,"score_gpt":0.18415471151325574,"score_spread":0.17444823168754917,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2170880857","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9462861,0.000101238686,0.000023071458,0.007082504,0.00017098506,0.000063588544,0.0000054654497,0.000001235169,0.046265848],"genre_scores_gemma":[0.9965001,0.000067856185,0.00019736342,0.0025344677,0.000038834132,7.8880225e-7,5.206123e-7,0.0000017763272,0.00065830717],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99922454,0.000047227746,0.0002174026,0.00009172182,0.00018746819,0.00023163385],"domain_scores_gemma":[0.9995154,0.00011302593,0.00015019962,0.00008829104,0.000010377115,0.00012271793],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00043282213,0.00006606762,0.00010716015,0.00004050107,0.0004198488,0.000033322514,0.00041838878,0.000023364246,0.005519573],"category_scores_gemma":[0.000047263344,0.00004297228,0.00004531282,0.00025931862,0.0007796015,0.00047611268,0.000018445826,0.00008015774,0.00011419053],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000060116663,0.000010207452,0.9511598,0.000002563237,0.0000148991985,0.000012761199,0.0024067366,0.0014397863,0.00004510797,0.00008736643,0.040197603,0.0046171537],"study_design_scores_gemma":[0.00014618305,0.00012336101,0.9469824,0.000022149507,0.000018366616,0.000014363683,0.0006063647,0.00015017182,0.00020052271,0.0005985728,0.051065914,0.00007162703],"about_ca_topic_score_codex":0.01604319,"about_ca_topic_score_gemma":0.7196209,"teacher_disagreement_score":0.7035777,"about_ca_system_score_codex":0.000007484179,"about_ca_system_score_gemma":0.000060508064,"threshold_uncertainty_score":0.9953895},"labels":[],"label_agreement":null},{"id":"W2171125516","doi":"10.1139/e09-005","title":"Evidence for prolonged mid-Paleozoic plutonism and ages of crustal sources in east-central Alaska from SHRIMP U–Pb dating of syn-magmatic, inherited, and detrital zircon","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Zircon; Geology; Batholith; Geochemistry; Plutonism; Devonian; Laurentia; Paleozoic; Precambrian; Gneiss; Pluton; Paleontology; Metamorphic rock; Tectonics","score_opus":0.03804391914886961,"score_gpt":0.22932606505530734,"score_spread":0.19128214590643772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171125516","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.990785,0.008239589,0.000039083232,0.0006600538,0.00004868346,0.00009310528,0.000053688902,0.0000014955313,0.000079321115],"genre_scores_gemma":[0.9948468,0.00009665618,0.004938478,0.00006733914,0.000040644754,1.7550913e-7,0.0000035490727,7.549023e-7,0.0000055618984],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998739,0.000059570863,0.0004498724,0.00018659474,0.00022365247,0.00034131025],"domain_scores_gemma":[0.9987653,0.0004237412,0.00029537606,0.00005539926,0.000081154234,0.0003790284],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000601034,0.000105814914,0.00032874485,0.00023148111,0.0001258757,0.00008818436,0.00024481316,0.000054807402,0.00028341432],"category_scores_gemma":[0.0008342807,0.00007515502,0.000064069434,0.0003710504,0.0006376848,0.0003922593,0.000006728138,0.000120200304,3.8950375e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002704553,0.0000073224674,0.98542404,0.000019897656,0.000010720011,0.000015108352,0.00060540927,0.00062486745,0.003929709,0.000007277969,0.0000033651932,0.009325217],"study_design_scores_gemma":[0.00028046832,0.0006273626,0.990014,0.00024963613,0.000028902316,0.00002423657,0.000916499,0.002254968,0.0027948222,0.0026876654,0.000020595418,0.000100801895],"about_ca_topic_score_codex":0.01134881,"about_ca_topic_score_gemma":0.12519678,"teacher_disagreement_score":0.11384798,"about_ca_system_score_codex":0.0000012260417,"about_ca_system_score_gemma":0.0002406117,"threshold_uncertainty_score":0.9952347},"labels":[],"label_agreement":null},{"id":"W2171230052","doi":"10.1139/e09-042","title":"Paleomagnetism and U–Pb geochronology of Franklin dykes in High Arctic Canada and Greenland: a revised age and paleomagnetic pole constraining block rotations in the Nares Strait regionThis is a companion paper to Denyszyn, S.W., Davis, D.W., and Halls, H.C. Paleomagnetism and U–Pb geochronology of the Clarence Head dykes, Arctic Canada: orthogonal emplacement of mafic dykes in a large igneous province. Canadian Journal of Earth Sciences, <b>46</b>(3): 155–167.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Paleomagnetism; Geology; Apparent polar wander; Paleontology; Arctic; Geochronology; Oceanography","score_opus":0.011129254383947152,"score_gpt":0.19629671371114304,"score_spread":0.1851674593271959,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171230052","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9776482,0.016354699,0.0000025781342,0.0053914804,0.00005854685,0.0002824718,0.00019750319,7.2652705e-7,0.000063809064],"genre_scores_gemma":[0.99824786,0.0004664565,0.00065845315,0.0005902096,0.000019096038,0.0000011514159,0.0000046843656,0.0000021253657,0.00000993639],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99718934,0.00035970798,0.0009409777,0.00037019333,0.0004749463,0.0006648431],"domain_scores_gemma":[0.99814874,0.0004514486,0.00052515045,0.00013826668,0.00016560731,0.00057078147],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012182348,0.00023784403,0.0006613012,0.00056197494,0.00034240406,0.00008621215,0.00044726455,0.00010625678,0.00029198872],"category_scores_gemma":[0.0003751992,0.0001601927,0.000043680906,0.00081127736,0.0021980177,0.00018832003,0.000024092591,0.0003993561,6.961653e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023523997,0.000015638678,0.9934207,0.000062202256,0.000014292419,0.0003236441,0.0011242074,0.000613126,0.00014270676,0.00013100942,0.000019345116,0.004109601],"study_design_scores_gemma":[0.00080019934,0.0013254439,0.9922534,0.0004580842,0.000042830437,0.00094366755,0.00211638,0.00048317754,0.000018382223,0.0012235338,0.00016154947,0.00017332424],"about_ca_topic_score_codex":0.98419404,"about_ca_topic_score_gemma":0.99995935,"teacher_disagreement_score":0.020599702,"about_ca_system_score_codex":0.000014763008,"about_ca_system_score_gemma":0.0051803985,"threshold_uncertainty_score":0.9189805},"labels":[],"label_agreement":null},{"id":"W2171350220","doi":"10.1139/cjes-2014-0209","title":"Controlling factors and genesis of hydrocarbons with complex phase state in the Upper Ordovician of the Tazhong Area, Tarim Basin, China","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Key Research and Development Program of China; PetroChina Company Limited; National Natural Science Foundation of China","keywords":"Ordovician; Geology; Source rock; Hydrocarbon; Tarim basin; Geochemistry; Natural gas; Structural basin; Petrology; Geomorphology","score_opus":0.031396804790988136,"score_gpt":0.23257963215713096,"score_spread":0.20118282736614282,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171350220","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99808294,0.0004290176,0.0004598434,0.00040044714,0.000057137262,0.000059100268,0.000010723355,0.0000016049947,0.00049918937],"genre_scores_gemma":[0.99980015,0.00001833823,0.00011245843,0.000046268215,0.00001227468,3.9971712e-7,4.3531816e-7,0.00000401599,0.000005635329],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99915165,0.00006995809,0.0002759113,0.0000612865,0.00027043468,0.00017077141],"domain_scores_gemma":[0.9994702,0.00004581687,0.00012813509,0.000093899085,0.000055061984,0.00020692618],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058523216,0.00008234712,0.00021547668,0.00027966942,0.00009383378,0.00004748405,0.00028515773,0.000018553135,0.000011741405],"category_scores_gemma":[0.00006514201,0.00003956525,0.00005338462,0.0006719975,0.0003349518,0.00016325808,0.000004541266,0.00010847488,1.08759835e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009709869,0.0000143920115,0.70422685,0.000008321789,0.00006102335,0.000014536376,0.01116041,0.28337654,0.00081753806,0.000043213135,0.00003652128,0.00023094354],"study_design_scores_gemma":[0.0021922996,0.0005496271,0.66029567,0.0001940766,0.000124395,0.000054157023,0.020219903,0.31215298,0.0022607055,0.00057332654,0.0010927017,0.00029012823],"about_ca_topic_score_codex":0.012797191,"about_ca_topic_score_gemma":0.24131317,"teacher_disagreement_score":0.22851598,"about_ca_system_score_codex":0.000007230569,"about_ca_system_score_gemma":0.00042144782,"threshold_uncertainty_score":0.9937767},"labels":[],"label_agreement":null},{"id":"W2171458074","doi":"10.1139/e00-102","title":"Quaternary geology of the Babine porphyry copper district: implications for geochemical exploration","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Glacial period; Quaternary; Bedrock; Geochemistry; Glacier; Interglacial; Paleontology; Geomorphology","score_opus":0.05010639261786816,"score_gpt":0.26770536079425683,"score_spread":0.21759896817638869,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171458074","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98408836,0.0005857819,0.0001219919,0.012718504,0.00033460438,0.00010040835,0.0000318993,0.0000014668465,0.0020169977],"genre_scores_gemma":[0.9992379,0.000052758234,0.00031698222,0.00018623946,0.00006888798,7.986356e-7,0.000008978641,8.306219e-7,0.00012664207],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991361,0.00007993453,0.00025888876,0.00010818159,0.00010658588,0.0003103334],"domain_scores_gemma":[0.9990855,0.0002558465,0.00016996714,0.00010590899,0.00016211242,0.000220685],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006122108,0.000060083967,0.0001358302,0.00015369142,0.0003928826,0.00002004364,0.0004882894,0.00006923592,0.00047957833],"category_scores_gemma":[0.00025761602,0.000038025453,0.00007381269,0.00036968425,0.0010244894,0.00021631055,0.000005320667,0.00013491229,0.000012539651],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011599175,0.0000035251435,0.99832475,0.0000028156167,0.000005463489,0.0000046489013,0.00006484553,0.0005294276,0.000038432427,0.0003579523,0.000319425,0.0003371294],"study_design_scores_gemma":[0.00013630358,0.00018235584,0.990669,0.000008205542,0.000007440183,0.0004046178,0.00010591776,0.00043408468,0.00012314184,0.0051499535,0.002733458,0.000045525914],"about_ca_topic_score_codex":0.0018671007,"about_ca_topic_score_gemma":0.1616364,"teacher_disagreement_score":0.1597693,"about_ca_system_score_codex":4.3235957e-7,"about_ca_system_score_gemma":0.00084303506,"threshold_uncertainty_score":0.85366154},"labels":[],"label_agreement":null},{"id":"W2171580743","doi":"10.1139/e11-030","title":"Laurentia-derived detritus in the Badger Group of central Newfoundland: deposition during closing of the Iapetus Ocean<sup>1</sup>This article is one of a series of papers published in <i>CJES Special Issue: In honour of Ward Neale</i> on the theme of Appalachian and Grenvillian geology.<sup>2</sup>Geological Survey of Canada Contribution 20110273.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta","funders":"","keywords":"Laurentia; Terrane; Geology; Paleozoic; Zircon; Paleontology; Detritus; Ordovician; Baltica; Paleomagnetism; Tectonics","score_opus":0.010869977290223341,"score_gpt":0.1713450715788229,"score_spread":0.16047509428859955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171580743","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99736506,0.0007183732,9.5014974e-7,0.0013738628,0.000059457074,0.00014210407,0.000116626645,4.881457e-7,0.00022310049],"genre_scores_gemma":[0.99973303,0.00008119123,0.000054944598,0.00007110819,0.00004614318,2.7059832e-7,0.000008068252,0.0000012257402,0.000004013124],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974146,0.00061907026,0.00088350475,0.00015166843,0.00047768076,0.00045349935],"domain_scores_gemma":[0.9983504,0.00049795205,0.0006724706,0.00013510819,0.00017546982,0.00016860673],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0020678707,0.00013043151,0.00054488453,0.0002037823,0.00010821196,0.000015472555,0.00046266435,0.00008874447,0.00132781],"category_scores_gemma":[0.0007685691,0.000069556474,0.00010657362,0.001043921,0.0013608041,0.00025479187,0.000022067306,0.00025669657,1.3645845e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014468581,0.000061167164,0.9911482,0.000032251042,0.000026305415,0.0000033105337,0.0017616203,0.005541541,0.0010033629,0.000059648737,0.000019642554,0.00019826875],"study_design_scores_gemma":[0.0004204581,0.00027432552,0.9904189,0.00012016346,0.000025983463,0.000015191442,0.001773126,0.000996431,0.0055818046,0.0002877845,0.000015198192,0.000070644375],"about_ca_topic_score_codex":0.630511,"about_ca_topic_score_gemma":0.94191074,"teacher_disagreement_score":0.31139973,"about_ca_system_score_codex":0.000009027928,"about_ca_system_score_gemma":0.00035984983,"threshold_uncertainty_score":0.9995851},"labels":[],"label_agreement":null},{"id":"W2171649256","doi":"10.1139/cjes-2014-0101","title":"<i>Aceroryctes dulcis</i>, a new palaeoryctid (Mammalia, Eutheria) from the early Eocene of the Wasatch Formation of southwestern Wyoming, USA","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Paleontology; Geology; Genus; Monophyly; Paleogene; Mammal; Biostratigraphy; Paleosol; Zoology; Clade; Biology; Structural basin; Phylogenetic tree","score_opus":0.02788583009589518,"score_gpt":0.2086175366272174,"score_spread":0.18073170653132223,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171649256","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99268293,0.0015445807,0.00009762865,0.0018140402,0.0007384911,0.0000456789,0.000049308677,0.0000017773091,0.003025564],"genre_scores_gemma":[0.99888575,0.00004209733,0.0003925537,0.0003020986,0.00016261313,1.0102108e-7,0.0000010663117,0.0000013744791,0.00021235521],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99866027,0.00022482102,0.00041293292,0.000108179425,0.00032683392,0.00026694],"domain_scores_gemma":[0.99857575,0.00035579244,0.00056144735,0.00015572371,0.00013094976,0.0002203111],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010245725,0.00010206239,0.00022015281,0.000091041824,0.00042030573,0.00005857385,0.00067250006,0.00005075264,0.00040539293],"category_scores_gemma":[0.00026556393,0.0000543831,0.00011177245,0.00033688097,0.0009103344,0.00032284547,0.0000082217975,0.00014562611,0.000018226285],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007737336,0.0000015155376,0.9926957,0.0000036035824,0.00001358746,7.112453e-7,0.0026210817,0.00030601828,0.00004783646,0.00005392135,0.00025745467,0.003990853],"study_design_scores_gemma":[0.00019557506,0.00014525536,0.9929275,0.00007580244,0.000024408202,0.0000129482705,0.0013628639,0.00030850386,0.0002756245,0.0005805262,0.0040237317,0.00006726329],"about_ca_topic_score_codex":0.1053719,"about_ca_topic_score_gemma":0.9402487,"teacher_disagreement_score":0.83487684,"about_ca_system_score_codex":0.0000014326248,"about_ca_system_score_gemma":0.00056866504,"threshold_uncertainty_score":0.90058553},"labels":[],"label_agreement":null},{"id":"W2171675931","doi":"10.1139/cjes-2015-0142","title":"Two garnet growth events in polymetamorphic rocks in southwest Spitsbergen, Norway: insight in the history of Neoproterozoic and early Paleozoic metamorphism in the High Arctic","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Narodowym Centrum Nauki","keywords":"Geology; Metamorphism; Geochemistry; Metamorphic facies; Greenschist; Schist; Metamorphic rock; Orogeny; Gneiss; Basement; Facies; Paleontology; Tectonics","score_opus":0.025902306422482452,"score_gpt":0.1908907342747766,"score_spread":0.16498842785229414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171675931","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905405,0.0066611385,0.0000010513106,0.001813899,0.00018279419,0.00012165735,0.0000055670957,6.311023e-7,0.00067275675],"genre_scores_gemma":[0.9993531,0.00004573784,0.000066152556,0.0004482997,0.000042283824,0.0000012441977,0.0000020389857,0.0000012065758,0.000039923452],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978225,0.00046978393,0.000568009,0.00021851674,0.0004817933,0.00043937075],"domain_scores_gemma":[0.9990729,0.0002224513,0.00023132876,0.00012033546,0.00006199216,0.00029100425],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027932227,0.00014371243,0.00035158507,0.000763521,0.00005328133,0.000035303343,0.0007476143,0.000057753485,0.00047956395],"category_scores_gemma":[0.00034857242,0.00007632653,0.00006885922,0.0014226849,0.0005172469,0.00031478796,0.000010160211,0.00043244474,0.000009821653],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011443065,0.000016037287,0.9957641,0.0000048645325,0.000004009973,0.00013311344,0.0027637572,0.0009719476,0.000009010165,0.000047574773,0.000009732,0.0002644532],"study_design_scores_gemma":[0.0004361894,0.0002534843,0.98870444,0.00004701806,0.000012568749,0.000054607608,0.00091474946,0.00020432695,0.0000059433155,0.009094243,0.00017162802,0.00010081399],"about_ca_topic_score_codex":0.56378955,"about_ca_topic_score_gemma":0.94946456,"teacher_disagreement_score":0.38567504,"about_ca_system_score_codex":0.000011453548,"about_ca_system_score_gemma":0.000666719,"threshold_uncertainty_score":0.5250889},"labels":[],"label_agreement":null},{"id":"W2171910288","doi":"10.1139/e03-074","title":"Lake Terrell upland glacial resurgences and implications for late-glacial history, northwestern Washington State, U.S.A.","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Glacial period; Deglaciation; Moraine; Paleontology; Ridge; Last Glacial Maximum; Post-glacial rebound; Geomorphology; Sediment; Physical geography; Oceanography","score_opus":0.03651521537100114,"score_gpt":0.249854633564126,"score_spread":0.21333941819312485,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171910288","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.990122,0.002375272,0.000028514734,0.00085665815,0.0009315105,0.00012120594,0.000078150784,0.0000036470522,0.0054829917],"genre_scores_gemma":[0.9987818,0.00010386802,0.0004665252,0.00017554655,0.000066622866,7.513227e-7,0.000010102933,0.000001814503,0.00039294513],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99871427,0.0001306662,0.00029726507,0.0002050098,0.00013812314,0.0005146399],"domain_scores_gemma":[0.9987305,0.00032807194,0.00016855051,0.00008021664,0.00012248327,0.00057019095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013899998,0.00010696001,0.000197528,0.00032474435,0.00062813243,0.00008799644,0.0003022292,0.00008012289,0.0008703654],"category_scores_gemma":[0.00022753845,0.00008460281,0.000054726566,0.00019781277,0.0010088144,0.00034199987,0.0000028839681,0.00018379059,0.000016893517],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014715161,0.0000026474795,0.9981674,0.0000058755377,0.000008867721,0.000016381277,0.0003974704,0.00022664914,0.0000025253448,0.00023000625,0.0002292626,0.00069820095],"study_design_scores_gemma":[0.00021399396,0.00028151364,0.92870915,0.000011343275,0.000009497044,0.00023330134,0.000098399105,0.000094878844,0.000010114242,0.0021778017,0.06805264,0.000107351974],"about_ca_topic_score_codex":0.0023077757,"about_ca_topic_score_gemma":0.9199034,"teacher_disagreement_score":0.9175956,"about_ca_system_score_codex":0.0000010457918,"about_ca_system_score_gemma":0.0019140058,"threshold_uncertainty_score":0.9529891},"labels":[],"label_agreement":null},{"id":"W2172120032","doi":"10.1139/e08-047","title":"<sup>210</sup>Pb–<sup>226</sup>Ra–<sup>230</sup>Th systematics in very low sedimentation rate sediments from the Mendeleev Ridge (Arctic Ocean)This article is one of a series of papers published in this Special Issue on the theme<i> Polar Climate Stability Network</i>.GEOTOP Publication 2008-0031.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Office of Polar Programs; Canadian Foundation for Climate and Atmospheric Sciences; National Science Foundation","keywords":"Geology; Sediment; Water column; Benthic zone; Arctic; Oceanography; Ridge; Seafloor spreading; Radionuclide; Sedimentation; Paleontology","score_opus":0.017968454483265655,"score_gpt":0.2043814428392184,"score_spread":0.18641298835595277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2172120032","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9895973,0.00031030696,0.000003003516,0.005031618,0.00022764174,0.00074024854,0.00013889726,0.000006349006,0.003944602],"genre_scores_gemma":[0.99785984,0.00025833215,0.00033965695,0.0009912938,0.0003521944,0.000009186145,0.000017583396,0.00001759742,0.00015434258],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99500865,0.00096900604,0.0015084464,0.00047523994,0.0011868321,0.00085184566],"domain_scores_gemma":[0.9973181,0.0005772751,0.0009900762,0.0005231301,0.0001612053,0.00043020505],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.005603272,0.00031390897,0.0005923482,0.00024679594,0.0006362338,0.00023005405,0.0010148841,0.00015267295,0.018853115],"category_scores_gemma":[0.0005636003,0.00020305326,0.00015535639,0.0019960913,0.001395416,0.0015604296,0.00009557822,0.00060125167,0.00006813288],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002791324,0.00040313756,0.64171857,0.000146565,0.00018618107,0.000043806755,0.060794145,0.2822495,0.001484528,0.00035692635,0.011951026,0.00038646758],"study_design_scores_gemma":[0.010275751,0.0050508957,0.5276248,0.0046252464,0.0006283122,0.00025819364,0.0864321,0.29082146,0.038920276,0.006895226,0.025482612,0.0029851196],"about_ca_topic_score_codex":0.01653472,"about_ca_topic_score_gemma":0.007517338,"teacher_disagreement_score":0.11409377,"about_ca_system_score_codex":0.00021100127,"about_ca_system_score_gemma":0.00058333535,"threshold_uncertainty_score":0.99001426},"labels":[],"label_agreement":null},{"id":"W2172279583","doi":"10.1139/e02-017","title":"Dextral strike-slip faulting in the Cariboo Mountains, British Columbia: a natural example of wrench tectonics in relation to Cordilleran tectonics","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Sinistral and dextral; Strike-slip tectonics; Seismology; Fault scarp; Fault (geology); Transform fault; Tectonics; Neotectonics; Slip (aerodynamics)","score_opus":0.022030203442943486,"score_gpt":0.194838467973019,"score_spread":0.1728082645300755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2172279583","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995995,0.0018432972,0.00000482799,0.0005399046,0.000118014126,0.00009766719,0.00002211318,0.0000018080098,0.0013773979],"genre_scores_gemma":[0.9990286,0.00003625851,0.0005949122,0.0002476346,0.00003466358,3.6714587e-7,0.0000041671638,9.496205e-7,0.000052427768],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984095,0.000115768235,0.0004703356,0.00018677903,0.00037355462,0.0004440401],"domain_scores_gemma":[0.99916905,0.00023315418,0.00016696147,0.00008342897,0.00009249503,0.00025493314],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011113307,0.00007847334,0.00023507663,0.0002225401,0.00023681056,0.0002341103,0.0005060389,0.000060682185,0.0021707655],"category_scores_gemma":[0.00046041104,0.00006733556,0.0000837182,0.0016417064,0.00028049946,0.00023635644,0.0000064755645,0.0003691705,0.0000062998115],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000020560526,0.0000072007115,0.97917503,0.0000028823824,0.0000037455768,0.00006880621,0.00040117628,0.010858744,0.000021467686,0.000007140567,0.00007056526,0.009381163],"study_design_scores_gemma":[0.00017432627,0.0002061301,0.9830259,0.000051093986,0.0000070414635,0.00010519083,0.0007239559,0.014169263,0.000007965064,0.0006123431,0.00081793335,0.000098841185],"about_ca_topic_score_codex":0.69936615,"about_ca_topic_score_gemma":0.9939505,"teacher_disagreement_score":0.29458436,"about_ca_system_score_codex":0.0000062508925,"about_ca_system_score_gemma":0.00022544072,"threshold_uncertainty_score":0.9987414},"labels":[],"label_agreement":null},{"id":"W2172405935","doi":"10.1139/cjes-2012-0162","title":"Contrasting changes in surface waters and barrens over the past 60 years for a subarctic forest–tundra site in northern Manitoba based on remote sensing imagery","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"St. Olaf College; National Science Foundation","keywords":"Tundra; Permafrost; Subarctic climate; Arctic; Physical geography; Tree line; Environmental science; Edaphic; Surface water; Thermokarst; Taiga; Geology; Hydrology (agriculture); Soil water; Climate change; Oceanography; Geography; Soil science; Forestry","score_opus":0.0290114487304696,"score_gpt":0.21181676556207485,"score_spread":0.18280531683160525,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2172405935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965612,0.00021655852,0.000010499183,0.0025858409,0.00027836958,0.00018075306,0.00007946291,0.0000016173288,0.000085680476],"genre_scores_gemma":[0.99870807,0.000019505318,0.00025781992,0.00088257226,0.00010996684,9.1068614e-8,0.000009687887,0.000003162209,0.000009153494],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989714,0.00006713386,0.00019656184,0.00014693274,0.00016807482,0.00044992237],"domain_scores_gemma":[0.99909574,0.00044016598,0.000106955435,0.0000656202,0.00005095118,0.00024057255],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00081468385,0.00009987301,0.00015452736,0.00025961644,0.00021130631,0.0002807328,0.0001438427,0.000034504585,0.00013295953],"category_scores_gemma":[0.00009745484,0.00006774969,0.00003250845,0.00027578263,0.00026014898,0.0002449036,0.0000033104252,0.00014967863,0.00000860718],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009232972,8.6194575e-7,0.988953,0.000008576179,0.0000015051011,0.00009298312,0.0007684641,0.0050950623,0.000063657906,2.4726614e-7,0.000040979674,0.0049654427],"study_design_scores_gemma":[0.0002475182,0.0001363708,0.91422474,0.00012872666,0.0000038310827,0.000034350425,0.0013296875,0.08348111,0.000006935618,0.00008173763,0.00023592332,0.000089058776],"about_ca_topic_score_codex":0.16965225,"about_ca_topic_score_gemma":0.991254,"teacher_disagreement_score":0.82160175,"about_ca_system_score_codex":0.0000058969645,"about_ca_system_score_gemma":0.00021444914,"threshold_uncertainty_score":0.8358771},"labels":[],"label_agreement":null},{"id":"W2172576306","doi":"10.1139/e11-015","title":"The quest for chron E23r at Partridge Island, Bay of Fundy, Canada: CAMP emplacement postdates the end-Triassic extinction event at the North American craton","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Bay; Basalt; Paleontology; Baltica; Sedimentary rock; Structural basin; Conodont; Geochemistry; Flood basalt; Paleomagnetism; Oceanography; Biostratigraphy; Volcanism; Ordovician; Tectonics","score_opus":0.02556628337196257,"score_gpt":0.21850484136376663,"score_spread":0.19293855799180407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2172576306","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98784536,0.00580205,0.000015204896,0.0021293717,0.00089581084,0.00022702652,0.00022618138,0.0000016154302,0.0028573587],"genre_scores_gemma":[0.9994355,0.00014695476,0.000030892912,0.00014978959,0.00009458651,0.0000020492191,0.000005083475,0.0000010008395,0.00013413305],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99831533,0.00020791778,0.00042057218,0.0001698814,0.00037213013,0.00051414105],"domain_scores_gemma":[0.9982354,0.0005593409,0.0005821152,0.00017932674,0.00012166505,0.0003221246],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0015390246,0.00013689954,0.00019843582,0.000081605904,0.0024450324,0.00006802817,0.0006391787,0.00002748112,0.0004186287],"category_scores_gemma":[0.00011179682,0.00006173497,0.000114790455,0.00036300314,0.0019147852,0.00015924442,0.0000037706643,0.00015232328,0.0000027791166],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000758881,0.0000031554416,0.98410416,0.000002774982,0.00003808765,0.000009442856,0.00054803345,0.00013325896,0.0000051408156,0.00003204712,0.0017996057,0.01324843],"study_design_scores_gemma":[0.00015033064,0.0006402073,0.975492,0.000010461072,0.000030908705,0.00007986189,0.0008421324,0.00018904204,0.0001976752,0.000045036566,0.022234652,0.0000877001],"about_ca_topic_score_codex":0.5927643,"about_ca_topic_score_gemma":0.99992305,"teacher_disagreement_score":0.40715873,"about_ca_system_score_codex":0.000014087194,"about_ca_system_score_gemma":0.0025917373,"threshold_uncertainty_score":0.9988536},"labels":[],"label_agreement":null},{"id":"W2172591798","doi":"10.1139/e10-064","title":"Harvey-Cardiff domain and its relationship to the Composite Arc Belt, Grenville Province: insights from U–Pb geochronology and geochemistryThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto; Geological Survey of Canada","funders":"","keywords":"Geology; Geochronology; Zircon; Monazite; Geochemistry; Gneiss; Diorite; Pluton; Titanite; Metamorphic rock; Closure temperature; Pegmatite; Hornblende; Terrane; Biotite; Seismology; Paleontology; Tectonics; Quartz","score_opus":0.018749468798603584,"score_gpt":0.17743824480221534,"score_spread":0.15868877600361175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2172591798","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9902818,0.0011599147,7.4862874e-7,0.0036510895,0.00004899353,0.000105594656,0.000086145956,6.9308277e-7,0.004664974],"genre_scores_gemma":[0.99918026,0.000054853645,0.0005216284,0.00014716932,0.00006239468,5.164042e-7,0.0000027278827,9.802435e-7,0.000029481971],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986919,0.00017101159,0.00050051656,0.00018837808,0.00021902387,0.00022915653],"domain_scores_gemma":[0.99891704,0.0003577965,0.00033075397,0.00012871138,0.000096643795,0.00016906035],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006880402,0.000103339116,0.0003653554,0.00020002451,0.000118005715,0.000019719635,0.00038503116,0.00007974227,0.0058609103],"category_scores_gemma":[0.00035353875,0.000058348935,0.000057775756,0.00056309276,0.0011487046,0.00016597057,0.000026240114,0.00022408318,0.0000026276282],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010513951,0.00003251256,0.9871391,0.000015820058,0.00003608931,0.000012393386,0.00450593,0.0002016823,0.0060591134,0.00048118134,0.00006208847,0.001348944],"study_design_scores_gemma":[0.00022907612,0.00039524958,0.956234,0.0000758887,0.000019022264,0.000011616542,0.0014048305,0.0000953637,0.030658424,0.010464793,0.00033748933,0.0000742433],"about_ca_topic_score_codex":0.037153967,"about_ca_topic_score_gemma":0.42780635,"teacher_disagreement_score":0.39065236,"about_ca_system_score_codex":0.0000027501922,"about_ca_system_score_gemma":0.000254311,"threshold_uncertainty_score":0.99504787},"labels":[],"label_agreement":null},{"id":"W2173385447","doi":"10.1139/cjes-2015-0068","title":"Geochemistry, geochronology, and fluid inclusion study of the Late Cretaceous Newton epithermal gold deposit, British Columbia","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Becton Dickinson (Canada); University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Molybdenite; Felsic; Fluid inclusions; Pyrite; Zircon; Diorite; Magmatic water; Volcanic rock; Arsenopyrite; Sericite; Marcasite; Quartz; Sphalerite; Mafic; Chalcopyrite; Volcano; Paleontology","score_opus":0.013169619440825966,"score_gpt":0.1872108462866979,"score_spread":0.17404122684587192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2173385447","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994902,0.0030297395,8.629614e-7,0.0006711052,0.00015319421,0.00007098474,0.00001777048,0.0000023883194,0.0011519261],"genre_scores_gemma":[0.9994004,0.000026612171,0.00006933145,0.00012903441,0.000049014026,1.2797211e-7,0.0000013766588,9.373526e-7,0.00032319533],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99877286,0.00012133219,0.00031026284,0.00015654684,0.00033453025,0.00030448573],"domain_scores_gemma":[0.9989069,0.000059001028,0.00020437085,0.000102331884,0.00014801287,0.00057939754],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00076809607,0.00007726253,0.00022670829,0.000049676863,0.00048406093,0.00018298972,0.0005528506,0.000059378504,0.0011457005],"category_scores_gemma":[0.00022262627,0.00006093951,0.000064562075,0.00041937732,0.00074906944,0.00014483077,0.00006953828,0.00016972973,0.0000032515156],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003831349,0.000013245078,0.9920552,0.0000029400644,0.0000143536245,0.000057965644,0.00031683428,0.0010849941,0.00013221202,2.6139006e-7,0.00030175154,0.0060164356],"study_design_scores_gemma":[0.00029251436,0.0005845587,0.99441916,0.000025957102,0.000036609337,0.00027822296,0.0007707853,0.0011882627,0.00017941777,0.0013366981,0.0007961903,0.00009163364],"about_ca_topic_score_codex":0.6177864,"about_ca_topic_score_gemma":0.9793573,"teacher_disagreement_score":0.36157086,"about_ca_system_score_codex":0.0000020921925,"about_ca_system_score_gemma":0.00041180622,"threshold_uncertainty_score":0.99976736},"labels":[],"label_agreement":null},{"id":"W2174072160","doi":"10.1139/cjes-2013-0019","title":"A petrological and geochronological study of a 360 Ma metallogenic event in Maritime Canada with implications for lithophile-metal mineralization in the Canadian Appalachians","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University; University of Alberta; Parks Canada; Laurentian University","funders":"","keywords":"Geology; Biotite; Greisen; Geochemistry; Molybdenite; Mineralization (soil science); Muscovite; Skarn; Pyrite; Terrane; Partial melting; Magmatism; Crust; Tectonics; Hydrothermal circulation; Quartz; Fluid inclusions","score_opus":0.01620072027474012,"score_gpt":0.19952780162776243,"score_spread":0.1833270813530223,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2174072160","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99300915,0.00033857214,0.0000075401513,0.005955688,0.000022069184,0.00029784872,0.000034646073,7.081555e-7,0.00033375694],"genre_scores_gemma":[0.9992522,0.0000053108474,0.00031608157,0.00037937638,0.000018132228,0.0000063642397,0.000008553702,7.4631157e-7,0.000013261479],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987968,0.000115758434,0.00034373012,0.0001806965,0.00018305649,0.0003799576],"domain_scores_gemma":[0.99914247,0.00019070717,0.00012152136,0.00007675687,0.00010195062,0.00036658553],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006396478,0.000098132165,0.00023897746,0.00027201147,0.00021772445,0.000070945716,0.0003590123,0.00004489467,0.00064458826],"category_scores_gemma":[0.00016880216,0.000050982275,0.000039955066,0.000703469,0.0003210095,0.00012642125,0.000004266476,0.00014774821,8.656212e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000053230697,0.000018600176,0.9958359,0.0000021794372,0.000010691939,0.000019240133,0.0001149473,0.003309688,0.000008140136,0.00011130882,0.000016160811,0.0005478396],"study_design_scores_gemma":[0.00025533,0.00080084166,0.9941292,0.0000061066276,0.000020206648,0.00007309144,0.0008919196,0.0013493481,0.0000010688299,0.0022584593,0.00014050183,0.00007396956],"about_ca_topic_score_codex":0.9937471,"about_ca_topic_score_gemma":0.99999034,"teacher_disagreement_score":0.006243206,"about_ca_system_score_codex":0.000007806088,"about_ca_system_score_gemma":0.0013260439,"threshold_uncertainty_score":0.7057789},"labels":[],"label_agreement":null},{"id":"W2174156564","doi":"10.1139/cjes-2015-0107","title":"A hydrological approach to estimating daily glacier ablation","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Meltwater; Ablation; Glacier; Ablation zone; Snow; Geology; Environmental science; Hydrology (agriculture); Atmospheric sciences; Climatology; Geomorphology; Medicine","score_opus":0.07671950886005083,"score_gpt":0.2412365209472813,"score_spread":0.16451701208723046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2174156564","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9721901,0.0005572979,0.0033717281,0.0011111542,0.0007779258,0.000074385774,0.000008292152,0.000005133254,0.021904014],"genre_scores_gemma":[0.9269339,0.0000014366983,0.07212106,0.0006053307,0.0002238175,1.908675e-7,0.000001740216,9.0296913e-7,0.00011161249],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990558,0.000033873872,0.00021942279,0.00012219962,0.00027903242,0.00028964845],"domain_scores_gemma":[0.9988596,0.00006528844,0.00010265581,0.00005667094,0.0001303717,0.0007854226],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009835178,0.00006777587,0.00012405663,0.00009846053,0.00037811787,0.00015013167,0.00026621146,0.00002713885,0.00021824273],"category_scores_gemma":[0.00046351954,0.0000474324,0.000036126887,0.00063315406,0.00018547037,0.00030077738,0.000004479896,0.00008875065,0.000044585537],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003637138,0.0000029325317,0.77829146,0.0000011478264,0.0000046537707,0.00000952636,0.00076139055,0.2154677,0.000001036482,0.0001588178,0.0012077487,0.0040899287],"study_design_scores_gemma":[0.00012591247,0.0003424397,0.88640046,0.000010992877,0.0000067977967,0.000074876494,0.0017130546,0.08671362,0.0000017268643,0.000690449,0.023819312,0.00010036977],"about_ca_topic_score_codex":0.008369806,"about_ca_topic_score_gemma":0.08029397,"teacher_disagreement_score":0.1287541,"about_ca_system_score_codex":0.0000024390956,"about_ca_system_score_gemma":0.0007559344,"threshold_uncertainty_score":0.99823356},"labels":[],"label_agreement":null},{"id":"W2174740111","doi":"10.1139/e11-042","title":"Preservation of terranes during the assembly of the Annieopsquotch Accretionary Tract: Inferences from the provenance of a Middle Ordovician ophiolite to arc transition, central Newfoundland Appalachians<sup>1</sup>Geological Survey of Canada Contribution 20100463.<sup>2</sup>This article is one of a series of papers published in this <i>CJES Special Issue: In honour of Ward Neale</i> on the theme of Appalachian and Grenvillian geology.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Memorial University of Newfoundland","funders":"","keywords":"Geology; Zircon; Ophiolite; Provenance; Geochemistry; Terrane; Volcanic rock; Conglomerate; Basement; Ordovician; Volcanic arc; Island arc; Accretionary wedge; Basalt; Clastic rock; Population; Petrology; Paleontology; Subduction; Sedimentary rock; Volcano; Archaeology; Tectonics","score_opus":0.017350694127087733,"score_gpt":0.18255592913876134,"score_spread":0.1652052350116736,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2174740111","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99115396,0.0005679669,0.0000015090708,0.0071516843,0.00004889123,0.0002654817,0.00051654363,6.229355e-7,0.0002933276],"genre_scores_gemma":[0.9996445,0.00008227551,0.00005163857,0.00013213919,0.000059497965,0.0000013415631,0.000013570418,0.0000014665699,0.000013544615],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973612,0.0005674021,0.0009869509,0.00017139407,0.00054026966,0.0003728221],"domain_scores_gemma":[0.99768114,0.0007964945,0.0008276787,0.00018713842,0.00034877856,0.00015875263],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019453265,0.00014437023,0.000568532,0.00012884356,0.00014140563,0.000015290014,0.00064745586,0.00008960567,0.0013960566],"category_scores_gemma":[0.0010160845,0.0000699226,0.000111468995,0.0010510606,0.0014999982,0.00035512936,0.000022766684,0.00024102569,1.3010154e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021521395,0.000065185595,0.9819684,0.000045052686,0.000037022633,7.606873e-7,0.0059014214,0.010604079,0.0008498101,0.00010004221,0.00002945096,0.0001835772],"study_design_scores_gemma":[0.0002917144,0.0003157828,0.99136174,0.00020168342,0.000028962735,0.0000049026185,0.002476104,0.0013741822,0.003002705,0.0008072185,0.000062422616,0.00007258535],"about_ca_topic_score_codex":0.6623967,"about_ca_topic_score_gemma":0.90291417,"teacher_disagreement_score":0.24051748,"about_ca_system_score_codex":0.0000068233835,"about_ca_system_score_gemma":0.00063626893,"threshold_uncertainty_score":0.9995168},"labels":[],"label_agreement":null},{"id":"W2175480519","doi":"10.1139/cjes-2014-0183","title":"A wide-gauge, large-mammal trackway from the upper Paleocene of Alberta, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Geology; Paleontology; Siltstone; Manus; Overprinting; Range (aeronautics); Mammal; Tectonics; Facies","score_opus":0.025225904748000696,"score_gpt":0.21099753147595002,"score_spread":0.18577162672794933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2175480519","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9655157,0.0076589067,0.000009925952,0.005900251,0.0012663333,0.000049888884,0.00016297851,0.000001324365,0.019434724],"genre_scores_gemma":[0.9980183,0.00003289742,0.00024722272,0.0012594678,0.00014495665,9.671737e-8,0.0000044781614,0.0000011094384,0.0002914684],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986045,0.00012666671,0.0003331859,0.0001272619,0.00039934387,0.00040904141],"domain_scores_gemma":[0.9982473,0.0005882916,0.00023212355,0.0001050356,0.00019370194,0.0006335298],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00085221307,0.000103142986,0.00022005691,0.00008914621,0.00038520966,0.000045848472,0.0005233062,0.000041963536,0.0011788929],"category_scores_gemma":[0.00064668595,0.00006177743,0.00006215467,0.00032912852,0.0006142691,0.00021797966,0.000004202709,0.00016588664,0.000017291515],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000074883533,0.0000019493825,0.9879086,9.413241e-7,0.000020314137,0.00002694645,0.00080412504,0.00032913437,3.0808957e-7,0.00009588414,0.010336401,0.00046790083],"study_design_scores_gemma":[0.00020830144,0.0001125519,0.90578324,0.000020176689,0.000014492053,0.000037383437,0.0026691146,0.00019970673,0.000010173416,0.00030239983,0.09056513,0.000077345656],"about_ca_topic_score_codex":0.9769476,"about_ca_topic_score_gemma":0.9999799,"teacher_disagreement_score":0.08212539,"about_ca_system_score_codex":0.0000031647592,"about_ca_system_score_gemma":0.005939128,"threshold_uncertainty_score":0.99973416},"labels":[],"label_agreement":null},{"id":"W2175942927","doi":"10.1139/cjes-2012-0031","title":"Rapidly changing styles of subsidence revealed by high-resolution mudstone allostratigraphy: Coniacian of Sweetgrass Arch area, southern Alberta and northern Montana","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Arch; Subsidence; Geomorphology; Ground subsidence; Resolution (logic); Geochemistry; Paleontology; Mining engineering; Archaeology; Structural basin","score_opus":0.016611297118198334,"score_gpt":0.20084057278505812,"score_spread":0.1842292756668598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2175942927","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920284,0.0064285244,0.00006001044,0.00030910224,0.00009368072,0.000066024586,0.00009512584,0.0000015781272,0.00091754925],"genre_scores_gemma":[0.99919343,0.000095971816,0.00056270766,0.00004232113,0.00003291675,1.9395135e-7,0.000006682696,0.0000012542132,0.000064507025],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987685,0.00006706598,0.00038893582,0.000100368234,0.0002694959,0.00040563464],"domain_scores_gemma":[0.99878687,0.00017775844,0.00038387266,0.00006977639,0.0001527631,0.0004289444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00094690867,0.00010261871,0.00022989776,0.00033559112,0.00027375936,0.000036396446,0.00025874915,0.000051022096,0.0004014026],"category_scores_gemma":[0.00013954216,0.000073273004,0.000052053874,0.00054856995,0.0007818357,0.00054413674,0.0000042712873,0.00010335919,0.0000038146345],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009010924,0.0000050822737,0.9957813,0.00001670328,0.000011534972,0.0000016420439,0.0017517165,0.00054542575,0.00011456341,0.00010679133,0.000016468273,0.0016397592],"study_design_scores_gemma":[0.00016701847,0.0004350522,0.9915846,0.000117392316,0.00002313991,0.000060719325,0.0056808167,0.0005923391,0.0005056811,0.0003941897,0.0002968346,0.00014221879],"about_ca_topic_score_codex":0.14984658,"about_ca_topic_score_gemma":0.75166184,"teacher_disagreement_score":0.6018153,"about_ca_system_score_codex":0.0000011171439,"about_ca_system_score_gemma":0.00031907455,"threshold_uncertainty_score":0.85581464},"labels":[],"label_agreement":null},{"id":"W2177183019","doi":"10.1139/cjes-2013-0123","title":"Long-term dynamics of a palsa in the sporadic permafrost zone of northwestern Quebec (Canada)","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval; Center for Northern Studies","funders":"Natural Sciences and Engineering Research Council of Canada; University of California, Irvine","keywords":"Permafrost; Geology; Term (time); Physical geography; Geomorphology; Earth science; Oceanography; Geography","score_opus":0.023073584839193063,"score_gpt":0.21595848620424318,"score_spread":0.19288490136505013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2177183019","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99620503,0.000588861,0.000011258725,0.00087964436,0.00029242848,0.000062740575,0.00078707864,5.9656327e-7,0.0011723621],"genre_scores_gemma":[0.99945384,0.00005337099,0.000023566889,0.0002878567,0.00008063696,7.992902e-8,0.00005573746,0.0000017828645,0.000043097436],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985716,0.0000874079,0.0004415171,0.000113782655,0.0004636745,0.00032205041],"domain_scores_gemma":[0.998907,0.00023342844,0.00035115605,0.00013692201,0.00009720284,0.00027425133],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010518186,0.000103624036,0.00025565104,0.00026297438,0.0001386304,0.00006090016,0.00064991805,0.00003951243,0.0013155283],"category_scores_gemma":[0.000053864314,0.00006855381,0.00006365899,0.00044840365,0.00056297774,0.00022420168,0.0000040644372,0.00015393355,0.0000028607017],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000061249807,0.0000036668553,0.9959235,0.000017886745,0.0000031089812,0.000059465707,0.0007064248,0.00045025337,0.000014415235,0.000071785544,0.000025141866,0.0027181788],"study_design_scores_gemma":[0.00014947019,0.00016894647,0.996817,0.000095319825,0.000008934499,0.00009529128,0.0010169989,0.001048429,0.000019417634,0.000048325765,0.0004493159,0.000082554056],"about_ca_topic_score_codex":0.9591668,"about_ca_topic_score_gemma":0.9999909,"teacher_disagreement_score":0.040824044,"about_ca_system_score_codex":0.00000411826,"about_ca_system_score_gemma":0.001626371,"threshold_uncertainty_score":0.99959743},"labels":[],"label_agreement":null},{"id":"W2177737943","doi":"10.1139/cjes-2015-0129","title":"Propagation of a strike-slip plate boundary within an extensional environment: the westward propagation of the North Anatolian Fault","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":99,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Subduction; North Anatolian Fault; Plate tectonics; Seismology; North American Plate; Eurasian Plate; African Plate; Lithosphere; Shear zone; Trough (economics); Slab; Shear (geology); Fault (geology); Structural basin; Strike-slip tectonics; Pleistocene; Tectonics; Paleontology","score_opus":0.03388487881580114,"score_gpt":0.21342184876437226,"score_spread":0.1795369699485711,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2177737943","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970509,0.00092599925,0.000025136556,0.0006975243,0.00036824433,0.00016047168,0.000049139227,0.0000020749162,0.00072050147],"genre_scores_gemma":[0.9994063,0.000021978305,0.00034344103,0.000100478355,0.00006957142,2.9418084e-7,0.000003762958,0.0000019062832,0.000052298223],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983258,0.00016068575,0.00042926552,0.0001420956,0.00069619046,0.00024591322],"domain_scores_gemma":[0.99872744,0.000073008705,0.0005576928,0.00015793448,0.00018703175,0.00029691306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013152555,0.00010527708,0.00018240289,0.0001465452,0.00049518986,0.00006811647,0.0004904386,0.000035836045,0.00013803877],"category_scores_gemma":[0.00021191349,0.000053580745,0.000068557005,0.00036880476,0.0013118692,0.00046112042,0.000009513896,0.00018272336,0.0000071253303],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020905254,0.0000067969595,0.9688684,0.0000074547843,0.000020043344,0.000011053776,0.0022382785,0.021499438,0.00002223197,0.00022190441,0.000068048364,0.007015442],"study_design_scores_gemma":[0.00019833763,0.0005239748,0.99186856,0.00005104635,0.000020821893,0.000087653534,0.0014372332,0.0037362042,0.00037330302,0.0006733394,0.00094877835,0.00008076145],"about_ca_topic_score_codex":0.008748618,"about_ca_topic_score_gemma":0.30166247,"teacher_disagreement_score":0.29291385,"about_ca_system_score_codex":0.000003783626,"about_ca_system_score_gemma":0.0022987651,"threshold_uncertainty_score":0.9978522},"labels":[],"label_agreement":null},{"id":"W2178860130","doi":"10.1139/cjes-2015-0100","title":"Re-evaluation of the historic Canadian fossil <i>Bathygnathus borealis</i> from the Early Permian of Prince Edward Island","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; Carleton University; University of Toronto","funders":"","keywords":"Autapomorphy; Paleontology; Cladistics; Taxon; Holotype; Permian; Sister group; Dentition; Phylogenetic tree; Snout; Geology; Clade; Zoology; Biology; Taxonomy (biology); Structural basin","score_opus":0.03906673402919655,"score_gpt":0.22931048892330716,"score_spread":0.1902437548941106,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2178860130","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9689421,0.0091107385,0.0000039788974,0.0029849384,0.0014294385,0.00010198429,0.00035070686,0.0000010758567,0.017075023],"genre_scores_gemma":[0.99946135,0.000021932796,0.00008986175,0.00021383121,0.00015268144,2.3728562e-7,0.0000062126514,9.85592e-7,0.00005287821],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99835676,0.00038974857,0.00032818766,0.00013201727,0.00047596384,0.00031731089],"domain_scores_gemma":[0.99841064,0.00017083106,0.00035402703,0.00018011965,0.00038503562,0.00049933675],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0025901427,0.00008707614,0.00017619831,0.00015142547,0.00039385824,0.000023233768,0.00082614424,0.00008615426,0.00030727946],"category_scores_gemma":[0.00060914457,0.000048241865,0.000073414136,0.00044012573,0.0012376911,0.00022916122,0.0000045953047,0.00018372961,0.00000582612],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008307068,0.0000016842951,0.9925195,8.884663e-7,0.000011408623,0.0000059366216,0.0015048526,0.0013756853,0.000003814877,0.0000649652,0.0023576631,0.0021453223],"study_design_scores_gemma":[0.00018783179,0.00017000208,0.9771854,0.000024399733,0.000033268785,0.00003608142,0.0007624431,0.0006347613,0.000016838492,0.0014760653,0.01941216,0.00006072421],"about_ca_topic_score_codex":0.8564194,"about_ca_topic_score_gemma":0.9991015,"teacher_disagreement_score":0.14268212,"about_ca_system_score_codex":0.000016786775,"about_ca_system_score_gemma":0.009512741,"threshold_uncertainty_score":0.9961024},"labels":[],"label_agreement":null},{"id":"W2179543705","doi":"10.1139/cjes-2015-0126","title":"Plate-tectonic evolution of the Earth: bottom-up and top-down mantle circulation","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Japan Society for the Promotion of Science; Ministry of Education, Culture, Sports, Science and Technology","keywords":"Geology; Mantle (geology); Earth's internal heat budget; Plate tectonics; Mantle convection; Subduction; Lithosphere; Hadean; Continental crust; Oceanic crust; Crust; Convergent boundary; Mid-ocean ridge; Geophysics; Petrology; Paleontology; Tectonics","score_opus":0.021593418945646946,"score_gpt":0.1922614234600144,"score_spread":0.17066800451436745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2179543705","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947103,0.001721914,0.000027046986,0.00086603925,0.00029912862,0.00003425445,0.000010024143,0.000001628305,0.002329616],"genre_scores_gemma":[0.99954385,0.00000973676,0.00022937311,0.00006837831,0.000051477688,4.516333e-8,8.800246e-7,4.91908e-7,0.00009576646],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99911046,0.00006024684,0.00022122022,0.00010774363,0.00028386075,0.00021645725],"domain_scores_gemma":[0.99919033,0.0000553529,0.00016433482,0.00006991125,0.00012238903,0.0003976581],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00064826827,0.00006338781,0.00013476062,0.0001274245,0.00019297743,0.0000519538,0.00025085016,0.00004138317,0.0009591015],"category_scores_gemma":[0.0002368886,0.000035303332,0.00006614488,0.00052259705,0.00050226465,0.00021307157,0.000006525308,0.00012587688,0.000014478439],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000037303864,0.0000014819644,0.9946869,0.0000021002659,0.0000059622653,0.000003406663,0.000094228955,0.003637362,0.00012336395,0.00016971676,0.000036540685,0.0012351848],"study_design_scores_gemma":[0.00011912559,0.00011702835,0.98373073,0.000017054694,0.000016339654,0.00006214082,0.0002714792,0.004425365,0.00034515234,0.010056086,0.00078088674,0.0000585865],"about_ca_topic_score_codex":0.027429895,"about_ca_topic_score_gemma":0.20877792,"teacher_disagreement_score":0.18134803,"about_ca_system_score_codex":0.0000019463214,"about_ca_system_score_gemma":0.0006046214,"threshold_uncertainty_score":0.99995416},"labels":[],"label_agreement":null},{"id":"W2179856397","doi":"10.1139/cjes-2015-0103","title":"An Upper Jurassic ichthyosaur (Ichthyosauria: Ophthalmosauridae) from the Bowser Basin, British Columbia","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; Royal Tyrrell Museum; Geological Survey of Canada; University of Alberta","funders":"Simon Fraser University","keywords":"Geology; Paleontology; Structural basin; Sedimentary depositional environment","score_opus":0.025971280048457255,"score_gpt":0.2199874180137385,"score_spread":0.19401613796528125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2179856397","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98087484,0.006338793,0.0000117000045,0.002546551,0.002251618,0.00008247219,0.00023362548,0.000008106784,0.0076522715],"genre_scores_gemma":[0.99653286,0.000035416873,0.0008883107,0.0015088537,0.0007088625,3.5356092e-7,0.000028351087,0.0000026177343,0.00029434974],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979616,0.0003933471,0.0003884555,0.00028237322,0.0003559226,0.0006183284],"domain_scores_gemma":[0.99793804,0.00025143937,0.00022779014,0.00019676643,0.00020714708,0.0011788163],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016239253,0.00012114349,0.00027040133,0.00008582796,0.0009628795,0.000585268,0.0010908374,0.00014682233,0.005304243],"category_scores_gemma":[0.0003285407,0.000107566215,0.000096039264,0.00042132958,0.0015402047,0.00091156445,0.000006319627,0.00033140392,0.00015871496],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012365475,0.000006360601,0.9822316,6.1363545e-7,0.00001879049,0.00030003328,0.00018139106,0.00031926387,0.0000038581416,0.00001370323,0.0142613575,0.002650639],"study_design_scores_gemma":[0.00024310061,0.000573659,0.95504826,0.000024636387,0.000021481295,0.0014613089,0.0006674625,0.00040742703,0.0000019900353,0.002559856,0.038839262,0.00015157975],"about_ca_topic_score_codex":0.5148677,"about_ca_topic_score_gemma":0.9858115,"teacher_disagreement_score":0.47094378,"about_ca_system_score_codex":0.000004259602,"about_ca_system_score_gemma":0.0029469323,"threshold_uncertainty_score":0.99560505},"labels":[],"label_agreement":null},{"id":"W2180303840","doi":"10.1139/e2012-059","title":"Investigation of three Fe–Ti oxide deposits associated with Grenvillian anorthosite massifs as potential source for lunar analogue ilmenite","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Canadian Space Agency","funders":"","keywords":"Ilmenite; Hematite; Magnetite; Spinel; Geology; Anorthosite; Electron microprobe; Mineralogy; Geochemistry; Plagioclase; Quartz","score_opus":0.019174447493536067,"score_gpt":0.19010955832886242,"score_spread":0.17093511083532636,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2180303840","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940073,0.000039513794,0.005030672,0.0005082581,0.00008969673,0.00014378985,0.000026847792,0.000002207799,0.00015173308],"genre_scores_gemma":[0.99830127,6.457768e-7,0.0013974264,0.00008654299,0.00007056663,0.0000023679381,0.000050233397,0.0000037552957,0.00008719173],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99905366,0.000032468164,0.00025435275,0.00012763953,0.0002455736,0.000286312],"domain_scores_gemma":[0.99890834,0.000035920886,0.00037959966,0.00006434966,0.00023038546,0.0003813833],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034230397,0.000093191746,0.00015017668,0.00021807573,0.00034678745,0.00016545945,0.00023397732,0.000027512946,0.000051064537],"category_scores_gemma":[0.000020069592,0.00007120088,0.000056267996,0.00041202147,0.00030815075,0.0010350307,0.000004462002,0.000082968734,0.000012339364],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000434627,0.000003925995,0.98803335,0.0000022288118,0.000031428903,0.0000033332703,0.00027542605,0.0066857375,0.003650516,0.00017162353,0.00014108025,0.0009970154],"study_design_scores_gemma":[0.0003555129,0.0005517842,0.9831618,0.00010619447,0.00004611782,0.000014542945,0.0007846441,0.0077665183,0.0034706169,0.0033357108,0.00023090703,0.00017564319],"about_ca_topic_score_codex":0.009250132,"about_ca_topic_score_gemma":0.085415125,"teacher_disagreement_score":0.07616499,"about_ca_system_score_codex":0.0000057830202,"about_ca_system_score_gemma":0.0008626601,"threshold_uncertainty_score":0.99734735},"labels":[],"label_agreement":null},{"id":"W2181434454","doi":"10.1139/cjes-2015-0082","title":"Determining the provenance of Triassic sedimentary rocks in northeastern British Columbia and western Alberta using detrital zircon geochronology, with implications for regional tectonics","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta; Government of British Columbia; University of British Columbia","funders":"","keywords":"Geology; Zircon; Terrane; Provenance; Geochronology; Foreland basin; Sedimentary rock; Geochemistry; Volcanic rock; Structural basin; Paleontology; Tectonics; Volcano","score_opus":0.03880620899944952,"score_gpt":0.22232279586988116,"score_spread":0.18351658687043165,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2181434454","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99803543,0.0006852908,0.00007493668,0.0009462035,0.000038184182,0.0001031755,0.00002974154,6.8658636e-7,0.00008632207],"genre_scores_gemma":[0.9986368,0.000007074982,0.0011310718,0.00015905629,0.000030420302,6.108372e-7,0.000003504527,9.1745557e-7,0.000030564337],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99925345,0.000031184172,0.00023921805,0.00013325177,0.00010948663,0.00023343174],"domain_scores_gemma":[0.9992072,0.00018285163,0.00019306266,0.000052482676,0.00012283145,0.00024159928],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036679182,0.000053778913,0.00016717856,0.000060099865,0.00027270673,0.00018218851,0.00022614082,0.000031779484,0.000042939497],"category_scores_gemma":[0.00011368256,0.000041169245,0.000035806996,0.00029876444,0.00055330095,0.00020093338,0.000005860815,0.00008859492,3.1231903e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006609068,0.0000048038496,0.99452215,0.0000027540402,0.0000071506693,0.0000033168888,0.00006147061,0.001520225,0.000012157995,9.673827e-7,0.000012427433,0.003845991],"study_design_scores_gemma":[0.0004563812,0.0004975478,0.99488044,0.000051486695,0.000021623333,0.00021644168,0.00026286088,0.0018823448,0.000013528639,0.0012449283,0.00040082433,0.00007161232],"about_ca_topic_score_codex":0.41332066,"about_ca_topic_score_gemma":0.99336034,"teacher_disagreement_score":0.5800397,"about_ca_system_score_codex":0.0000026089244,"about_ca_system_score_gemma":0.0006434439,"threshold_uncertainty_score":0.5905861},"labels":[],"label_agreement":null},{"id":"W2181947216","doi":"10.1139/e08-036","title":"Low- and high-frequency climate variability in eastern Beringia during the past 25 000 yearsThis article is one of a series of papers published in this Special Issue on the theme <i>Polar Climate Stability Network</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Beringia; Holocene; Glacial period; Precipitation; Climate change; Series (stratigraphy); Climatology; Geology; Pollen; Physical geography; Geography; Paleontology; Oceanography; Meteorology","score_opus":0.01765879094546258,"score_gpt":0.19995270142775343,"score_spread":0.18229391048229085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2181947216","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9903914,0.00022222298,1.2700968e-7,0.0026250856,0.00022415497,0.00014553274,0.000052298812,0.0000015349633,0.0063376776],"genre_scores_gemma":[0.9993993,0.00020841596,0.00008925487,0.0001163663,0.00016666531,5.928465e-7,8.5951973e-7,0.0000016817162,0.000016851813],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977779,0.00056025793,0.00052601757,0.00021006922,0.00031393138,0.0006118326],"domain_scores_gemma":[0.9987196,0.0005598857,0.00023136963,0.00021211416,0.00008480213,0.0001922679],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0048481305,0.00011058433,0.00030503844,0.0001742919,0.00043009256,0.000049378687,0.0004973556,0.000080557,0.011541089],"category_scores_gemma":[0.00038494254,0.000067225265,0.00005062186,0.0006865814,0.0023191515,0.0003949662,0.000022974393,0.0004150356,0.000010128854],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006825086,0.000014899924,0.9972638,0.000032691383,0.000007912717,0.000035830093,0.0019852086,0.000307331,0.000026492427,0.0001520804,0.000012569537,0.000092942886],"study_design_scores_gemma":[0.00020665005,0.00018997453,0.9977193,0.0000708346,0.0000043358855,0.000065850654,0.0004927078,0.00014395615,0.00030167348,0.0006566018,0.00008124404,0.00006689718],"about_ca_topic_score_codex":0.009420623,"about_ca_topic_score_gemma":0.3758133,"teacher_disagreement_score":0.3663927,"about_ca_system_score_codex":0.0000023022199,"about_ca_system_score_gemma":0.0003789148,"threshold_uncertainty_score":0.99717575},"labels":[],"label_agreement":null},{"id":"W2183358173","doi":"10.1139/e11-019","title":"Paleoenvironmental and chronological constraints on the Mount Tatlow succession, British Columbia: first recognition of radiolarian and foraminiferal faunas in the Intermontane Cretaceous back-arc basins of western Canada<sup>1</sup>This article is one of a series of papers published in this Special Issue on the theme of <i>New insights in Cordilleran Intermontane geoscience: reducing exploration risk in the mountain pine beetle-affected area, British Columbia</i>.<sup>2</sup>Geological Survey of Canada Contribution 20100279.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; Carleton University; Geological Survey of Canada","funders":"University of Wisconsin-Eau Claire; University of Arizona","keywords":"Geology; Paleontology; Cretaceous; Ecological succession; Cenomanian; Sedimentary rock; Conglomerate; Stratigraphy; Structural basin; Foreland basin; Tectonics","score_opus":0.024968114960899655,"score_gpt":0.19085716773815317,"score_spread":0.16588905277725352,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2183358173","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99758154,0.0002914194,7.2662846e-7,0.0008993002,0.000055010725,0.0004728544,0.00046124135,5.0522834e-7,0.00023742487],"genre_scores_gemma":[0.99951875,0.00027866967,0.000020914173,0.00012717438,0.000017175114,0.0000025643112,0.000022145134,0.0000017807251,0.0000108171425],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9966761,0.0013789122,0.0008500571,0.00024839916,0.00048333892,0.0003632113],"domain_scores_gemma":[0.9979581,0.0010736216,0.0005472974,0.00014501247,0.00015059242,0.00012537432],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0035207556,0.00011352546,0.0005026083,0.00013152779,0.00023156444,0.000091818096,0.00052521046,0.00013119019,0.0034291556],"category_scores_gemma":[0.0013885368,0.0000870535,0.000035968525,0.00062763086,0.0032615715,0.0003268898,0.00002129757,0.00050796225,1.4554098e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016480283,0.000061571445,0.9935373,0.000015967325,0.000014962476,0.000111787405,0.004430302,0.00023049497,0.00002006432,0.0000029486598,0.00016055253,0.0012492305],"study_design_scores_gemma":[0.0007491537,0.0013908988,0.98680276,0.0003631526,0.000010176288,0.0002541456,0.008802006,0.0012783513,0.00008607686,0.00016535557,0.000014117117,0.00008381743],"about_ca_topic_score_codex":0.9905038,"about_ca_topic_score_gemma":0.9999521,"teacher_disagreement_score":0.009448275,"about_ca_system_score_codex":0.000019339499,"about_ca_system_score_gemma":0.0011635943,"threshold_uncertainty_score":0.999451},"labels":[],"label_agreement":null},{"id":"W2184039327","doi":"10.1139/e11-037","title":"Ophiolite obduction in the Quebec Appalachians, Canada — <sup>40</sup>Ar/<sup>39</sup>Ar age constraints and evidence for syn-tectonic erosion and sedimentation<sup>1</sup>Geological Survey of Canada Contribution 20100430.<sup>2</sup>GEOTOP (Centre de recherche en géochimie et géodynamique) Contribution 2011-0002.<sup>3</sup>This article is one of a series of papers published in this <i>CJES Special Issue: In honour of Ward Neale</i> on the theme of Appalachian and Grenvillian geology.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Université du Québec à Montréal","funders":"","keywords":"Obduction; Geology; Ophiolite; Massif; Allochthon; Laurentia; Orogeny; Paleontology; Geochemistry; Paleozoic; Subduction; Nappe; Oceanic crust; Tectonics","score_opus":0.03970736146749457,"score_gpt":0.2436947089911691,"score_spread":0.20398734752367453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2184039327","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9870387,0.0017260645,0.000013238565,0.009848016,0.00004512565,0.0006277566,0.0005810848,0.0000028459954,0.00011721986],"genre_scores_gemma":[0.99834806,0.00068992336,0.00022669324,0.00051692856,0.000085122,0.000005757733,0.00008022812,0.0000046325285,0.000042670385],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99436736,0.0024274096,0.0012551253,0.00044708225,0.00065202586,0.00085101154],"domain_scores_gemma":[0.9951912,0.0029721372,0.00072681,0.0002292292,0.0004013888,0.00047920362],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00876506,0.00032801245,0.0009099118,0.00031776482,0.0002654272,0.000069374706,0.00053295575,0.00030910445,0.0021643622],"category_scores_gemma":[0.0040071076,0.00021695116,0.00011577552,0.0009836025,0.0020529574,0.0006754745,0.000040631436,0.00073260476,7.6720335e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041361572,0.00007863766,0.96307105,0.00010195355,0.000068396934,0.000015532918,0.0052107368,0.028754795,0.00029700925,0.00029466787,0.00048328566,0.0012103012],"study_design_scores_gemma":[0.0013100826,0.0005953892,0.95766795,0.0004159246,0.00009114962,0.000071145,0.008647761,0.028195564,0.001175538,0.0013271209,0.00021648458,0.0002858698],"about_ca_topic_score_codex":0.93356985,"about_ca_topic_score_gemma":0.98727846,"teacher_disagreement_score":0.05370865,"about_ca_system_score_codex":0.000098246244,"about_ca_system_score_gemma":0.0023719121,"threshold_uncertainty_score":0.99874777},"labels":[],"label_agreement":null},{"id":"W2184740541","doi":"10.1139/e2012-073","title":"Initial rifting and breakup between Nova Scotia and Morocco: insight from new magnetic models <sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of <i>Mesozoic–Cenozoic geology of the Scotian Basin</i>. <sup>2</sup>Earth Sciences Sector Contribution 20120024.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Rift; Magnetic anomaly; Continental margin; Basement; Seafloor spreading; Paleontology; Passive margin; Magmatism; Continental crust; Volcanism; Oceanic crust; Crust; Seismology; Tectonics; Subduction","score_opus":0.0231031033482788,"score_gpt":0.19861375261496503,"score_spread":0.17551064926668622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2184740541","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99106836,0.0020125369,0.0000025563288,0.0032711728,0.0001110607,0.00015258354,0.00016706539,0.0000018387608,0.0032128112],"genre_scores_gemma":[0.9988014,0.000058776972,0.00036945828,0.00030999933,0.00040159785,1.768144e-7,0.0000038731987,0.0000022098016,0.00005248333],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975576,0.00028661592,0.0007654086,0.00026585438,0.00057934556,0.0005451727],"domain_scores_gemma":[0.9980479,0.00064549234,0.0005301872,0.00016150303,0.00019901608,0.00041590031],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014651845,0.00018722337,0.00059204013,0.00030195442,0.00024257136,0.00008615289,0.00057648076,0.000117206466,0.020185633],"category_scores_gemma":[0.00065321516,0.00010589409,0.00012093015,0.0011674878,0.0032476159,0.00081651023,0.000043574175,0.0002750473,0.000005129797],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043920896,0.000023629897,0.99089855,0.000013783647,0.00003707453,0.0000017705693,0.0034495948,0.0029081255,0.00034679,0.00021101169,0.00013262525,0.0019331088],"study_design_scores_gemma":[0.0005715519,0.00089996995,0.9740777,0.00019706402,0.00010624499,0.000023082575,0.001825149,0.0051160865,0.00996852,0.0064284415,0.0005888731,0.00019729785],"about_ca_topic_score_codex":0.1313921,"about_ca_topic_score_gemma":0.13026813,"teacher_disagreement_score":0.020180503,"about_ca_system_score_codex":0.0000027895712,"about_ca_system_score_gemma":0.0005454503,"threshold_uncertainty_score":0.999465},"labels":[],"label_agreement":null},{"id":"W2184977037","doi":"10.1139/cjes-2014-0232","title":"Pinwarian to Grenvillian magmatic evolution in the central Grenville Province: new constraints from ID–TIMS U–Pb ages and coupled Lu–Hf S–MC–ICP–MS data","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland; Ministère des Ressources naturelles et des Forêts (Québec); Université du Québec à Montréal","funders":"","keywords":"Geology; Geochemistry; Orogeny; Metamorphism; Zircon; Gneiss; Pluton; Magmatism; Continental arc; Subduction; Continental crust; Metamorphic rock; Mantle (geology); Crust; Back-arc basin; Petrology; Tectonics; Volcanic rock; Paleontology","score_opus":0.03733343792351142,"score_gpt":0.21532133030328005,"score_spread":0.17798789237976864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2184977037","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98719126,0.001705965,0.0001369717,0.009224054,0.00025471463,0.00013355365,0.00020079334,0.0000030375932,0.0011496635],"genre_scores_gemma":[0.99731195,0.000019560166,0.0016422365,0.00077245675,0.00015809402,1.521044e-7,0.000045167337,9.3524704e-7,0.000049461378],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982263,0.00012919301,0.0003623839,0.0002917019,0.00046223166,0.0005281839],"domain_scores_gemma":[0.9980795,0.00015894228,0.0001525067,0.00020155076,0.000051105097,0.0013563955],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011750677,0.00013646467,0.00025070796,0.00019563768,0.0002265505,0.0002777564,0.0010250629,0.000057660054,0.0020467513],"category_scores_gemma":[0.0005665383,0.00007930636,0.000039819708,0.0005582796,0.0007342059,0.00038557523,0.000023184988,0.000205256,0.000055450884],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010263502,0.000006597843,0.99039304,0.0000026341636,0.000012995172,0.00009416439,0.00053799624,0.0013142196,0.000029588116,0.00005781813,0.001195,0.006345661],"study_design_scores_gemma":[0.0002800652,0.00022209641,0.98297995,0.00003880617,0.000029418823,0.000079061676,0.0015889389,0.006201973,0.0000061153096,0.005907333,0.0025186804,0.00014753913],"about_ca_topic_score_codex":0.28614053,"about_ca_topic_score_gemma":0.88676167,"teacher_disagreement_score":0.6006211,"about_ca_system_score_codex":0.0000051575053,"about_ca_system_score_gemma":0.0013084405,"threshold_uncertainty_score":0.9988655},"labels":[],"label_agreement":null},{"id":"W2185503559","doi":"10.1139/e11-022","title":"Interpretation of structures in the southeastern Nechako Basin, British Columbia, from seismic reflection, well log, and potential field data<sup>1</sup>This article is one of a series of papers published in this Special Issue on the theme of <i>New insights in Cordilleran Intermontane geoscience: reducing exploration risk in the mountain pine beetle-affected area, British Columbia</i>.<sup>2</sup>Geological Survey of Canada Contribution 20100002.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; Geological Survey of Canada","funders":"Northwestern University","keywords":"Geology; Transtension; Pull apart basin; Structural basin; Cretaceous; Paleontology; Neogene; Volcanic rock; Basin and range topography; Tectonics; Fault (geology); Pyroclastic rock; Seismology; Forearc; Sinistral and dextral; Sedimentary basin; Volcano; Subduction","score_opus":0.01753141820067775,"score_gpt":0.18669643329588856,"score_spread":0.1691650150952108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2185503559","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99834436,0.00021173501,0.000011086036,0.0005420308,0.00006394533,0.00021728278,0.00036642948,8.119857e-7,0.00024231226],"genre_scores_gemma":[0.9995643,0.00009272331,0.000051143204,0.00019126869,0.000041186253,8.1446206e-7,0.00003976922,0.0000012314697,0.000017594091],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973948,0.0008150307,0.00081373233,0.00025810208,0.00046975206,0.00024856615],"domain_scores_gemma":[0.9984653,0.00051013345,0.0005316936,0.0001744701,0.00022102684,0.00009736665],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0023346588,0.00009073551,0.00043460308,0.00013764799,0.0001270644,0.0001519475,0.00063283107,0.00009134583,0.00611005],"category_scores_gemma":[0.0016745987,0.00007268947,0.00004648897,0.001128953,0.0007207598,0.00047429302,0.000023505627,0.00032706803,1.8192999e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017196333,0.00004406803,0.98445374,0.000009832669,0.000016983266,0.00002523185,0.0058089136,0.0045436798,0.000090234644,0.0000016944472,0.00045563694,0.0043780524],"study_design_scores_gemma":[0.00040787467,0.0008274806,0.9725284,0.00018573493,0.000020161739,0.000023894941,0.005114621,0.018330913,0.00022836831,0.0022318768,0.000021649366,0.00007904034],"about_ca_topic_score_codex":0.9961199,"about_ca_topic_score_gemma":0.99959743,"teacher_disagreement_score":0.013787234,"about_ca_system_score_codex":0.000007512692,"about_ca_system_score_gemma":0.00049110333,"threshold_uncertainty_score":0.9947985},"labels":[],"label_agreement":null},{"id":"W2185943624","doi":"10.1139/cjes-2013-0073","title":"Chronostratigraphy of Eocene volcanism, central British Columbia","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Pacific Institute for the Mathematical Sciences; Government of British Columbia; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Society of Economic Geologists Canada Foundation; Society of Economic Geologists Foundation","keywords":"Geology; Felsic; Rhyolite; Dacite; Chronostratigraphy; Plateau (mathematics); Volcanic plateau; Volcanic rock; Volcanism; Geochemistry; Andesite; Pyroclastic rock; Paleontology; Subduction; Phenocryst; Volcano; Tectonics","score_opus":0.008892539185734455,"score_gpt":0.16180898016513706,"score_spread":0.1529164409794026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2185943624","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923431,0.0011443777,0.000009151446,0.00041299485,0.00018135554,0.000050166815,0.00003749864,0.0000022678682,0.0058190525],"genre_scores_gemma":[0.9983843,0.00003493762,0.0011752384,0.0001919196,0.00007592867,1.1692772e-7,0.0000035673775,6.5309143e-7,0.00013335868],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99878114,0.000037965423,0.00034225135,0.00013342538,0.00026265072,0.0004425344],"domain_scores_gemma":[0.9987273,0.000056393314,0.00019086637,0.000060073966,0.00016295206,0.0008023732],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025176068,0.000063555526,0.00021310891,0.00009505068,0.00022232768,0.00034367322,0.0004061158,0.000042686705,0.052495603],"category_scores_gemma":[0.00010160626,0.00006155839,0.00013873585,0.0005840227,0.0007781353,0.00034046234,0.000002982113,0.00011918597,0.000033387],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[6.1819804e-7,0.0000032427567,0.991132,0.0000031273432,0.000011266382,0.0000205328,0.000023579612,0.00033866958,0.000057687583,0.000007187965,0.0010271857,0.007374857],"study_design_scores_gemma":[0.00008741531,0.0002470779,0.99131256,0.000022945113,0.0000115284065,0.00006721574,0.00013212344,0.0003644458,0.0001179904,0.006635576,0.0009172109,0.000083909574],"about_ca_topic_score_codex":0.75740147,"about_ca_topic_score_gemma":0.9780106,"teacher_disagreement_score":0.22060914,"about_ca_system_score_codex":6.5942567e-7,"about_ca_system_score_gemma":0.00055546284,"threshold_uncertainty_score":0.9483705},"labels":[],"label_agreement":null},{"id":"W2186097838","doi":"10.1139/e2012-054","title":"Late Paleocene radiolarian fauna from Tibet and its geological implications","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"China Geological Survey; National Science Foundation","keywords":"Geology; Paleontology; Oceanic crust; Radiolaria; Subduction; Foreland basin; Fauna; Abyssal plain; Oceanic basin; Fibrous joint; Abyssal zone; Structural basin; Bathyal zone; Basalt; Tectonics; Oceanography","score_opus":0.04621146837349764,"score_gpt":0.2538926961515885,"score_spread":0.20768122777809084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2186097838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9811777,0.010668443,0.000009625979,0.0027937137,0.00035099292,0.00005133449,0.00004555939,0.0000034061513,0.0048992336],"genre_scores_gemma":[0.9987246,0.00014675905,0.00053536287,0.0003375286,0.0001663026,1.8262348e-7,0.000007797297,9.1755135e-7,0.00008057574],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99877554,0.00015940676,0.00021005161,0.0001348163,0.00012935085,0.00059084635],"domain_scores_gemma":[0.9984528,0.00029965557,0.000102850165,0.00007531613,0.00006771843,0.001001704],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010740847,0.000085855194,0.00017546528,0.0002112961,0.0005753543,0.00006536067,0.00034204818,0.00011542578,0.0027947421],"category_scores_gemma":[0.00021653154,0.00006168403,0.000036565845,0.000266996,0.00065525377,0.0004440003,0.000006439053,0.00028511442,0.00015205525],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000036607557,0.000002434942,0.99882376,0.0000012411524,0.000009884724,0.000018756102,0.00016596966,0.00007080941,0.000009624899,0.00037790305,0.00003941385,0.00047656242],"study_design_scores_gemma":[0.00010960303,0.00010906176,0.9954085,0.0000073797937,0.000009832517,0.000344023,0.000083011924,0.00022825615,0.00002612595,0.0015121255,0.0020845956,0.00007748586],"about_ca_topic_score_codex":0.002231568,"about_ca_topic_score_gemma":0.14286399,"teacher_disagreement_score":0.14063242,"about_ca_system_score_codex":2.7592148e-7,"about_ca_system_score_gemma":0.00043377452,"threshold_uncertainty_score":0.99811685},"labels":[],"label_agreement":null},{"id":"W2187229674","doi":"10.1139/e11-041","title":"The Salinic Orogeny in northern New Brunswick: geochronological constraints and implications for Silurian stratigraphic nomenclature<sup>1</sup>This article is one of a series of papers published in this CJES Special Issue: In honour of Ward Neale on the theme of Appalachian and Grenvillian geology.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Geological Survey of Canada","funders":"","keywords":"Unconformity; Geology; Ordovician; Paleontology; Devonian; Orogeny; Conglomerate; Sedimentary rock; Structural basin","score_opus":0.01968047184414674,"score_gpt":0.2077125110947815,"score_spread":0.18803203925063477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2187229674","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9872323,0.0012766479,6.595606e-7,0.010238682,0.000029091128,0.00014194692,0.00003896843,6.369424e-7,0.0010410472],"genre_scores_gemma":[0.9993711,0.00017644346,0.0002641101,0.0001015094,0.00006319998,5.42426e-7,0.0000018902962,9.0586497e-7,0.000020315416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986621,0.00011007063,0.0005710918,0.00014834752,0.00014802773,0.00036033892],"domain_scores_gemma":[0.9987421,0.00051119324,0.00032102203,0.000106999214,0.00007133379,0.0002473736],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013251737,0.00010008734,0.00033674156,0.00021495124,0.00012290805,0.000026437529,0.00032630409,0.000084538384,0.0029419186],"category_scores_gemma":[0.00049027,0.00005439584,0.00007604167,0.0006510352,0.0022701067,0.00019101426,0.000010405204,0.00020580362,6.995841e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003663449,0.000023724495,0.9913402,0.000008272544,0.000018051616,7.7216106e-7,0.001535191,0.00016881566,0.0001412415,0.0009795884,0.000022925347,0.005724545],"study_design_scores_gemma":[0.0002568121,0.00038548364,0.98790026,0.000035558376,0.000012695457,0.000011144684,0.0019019742,0.00015900192,0.00029882335,0.0087294355,0.0002472519,0.00006157836],"about_ca_topic_score_codex":0.028586458,"about_ca_topic_score_gemma":0.80814105,"teacher_disagreement_score":0.7795546,"about_ca_system_score_codex":0.0000020777068,"about_ca_system_score_gemma":0.0005493219,"threshold_uncertainty_score":0.9979695},"labels":[],"label_agreement":null},{"id":"W2187648898","doi":"10.1139/e11-049","title":"A paleogeographical review of the peri-Gondwanan realm of the Appalachian orogen<sup>1</sup>This article is one of a series of papers published in this <i>CJES Special Issue: In honour of Ward Neale</i> on the theme of Appalachian and Grenvillian geology.","year":2012,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":135,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Mount Royal University","funders":"","keywords":"Laurentia; Geology; Paleozoic; Gondwana; Paleontology; Orogeny; Devonian; Ordovician; Pangaea; Laurasia; Terrane; Carboniferous; Accretion (finance); Permian; Tectonics; Physics; Astrophysics","score_opus":0.02348929662092163,"score_gpt":0.20861571426929662,"score_spread":0.18512641764837498,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2187648898","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.29981282,0.68927586,5.555388e-8,0.0048776963,0.00012988034,0.00048335537,0.00028242267,0.0000010074729,0.0051368824],"genre_scores_gemma":[0.5565825,0.44292656,0.000081094615,0.000246791,0.00010271222,0.0000016591615,0.0000048095612,0.0000036664062,0.000050235245],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99584824,0.00084630324,0.0017828875,0.00029573368,0.0007399712,0.0004868377],"domain_scores_gemma":[0.9966459,0.00046962968,0.0019377086,0.00043137174,0.00020965727,0.00030572733],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0031418032,0.00029258805,0.001886491,0.00041120418,0.00014021763,0.00001984189,0.0015080819,0.00020149522,0.012207667],"category_scores_gemma":[0.00085984246,0.00013125864,0.00074685906,0.002769495,0.0041715475,0.00017816902,0.000060707047,0.00063541456,0.0000015555829],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034926205,0.00009209154,0.9265973,0.005299778,0.00017877712,0.0000050467856,0.0015719136,0.00006773639,0.000012890793,0.0003215345,0.00019175434,0.06562625],"study_design_scores_gemma":[0.00067900534,0.0016359474,0.75038767,0.04177641,0.0014954483,0.00018682553,0.0028403832,0.000110406516,0.0004500257,0.0028785476,0.19683194,0.0007274074],"about_ca_topic_score_codex":0.02067166,"about_ca_topic_score_gemma":0.1515944,"teacher_disagreement_score":0.2567697,"about_ca_system_score_codex":0.0000036885344,"about_ca_system_score_gemma":0.000877535,"threshold_uncertainty_score":0.99853855},"labels":[],"label_agreement":null},{"id":"W2187829405","doi":"10.1139/cjes-2015-0131","title":"A 2169 Ma U–Pb baddeleyite age for the Otish Gabbro, Quebec: implications for correlation of Proterozoic magmatic events and sedimentary sequences in the eastern Superior Province","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Toronto","funders":"University of Otago","keywords":"Sill; Geology; Geochemistry; Supergroup; Baddeleyite; Gabbro; Proterozoic; Sedimentary rock; Large igneous province; Precambrian; Paleontology; Magmatism; Igneous rock; Zircon; Tectonics","score_opus":0.03381529134165104,"score_gpt":0.2304896432623564,"score_spread":0.19667435192070537,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2187829405","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9895874,0.001056207,0.0005193356,0.008029552,0.00010878688,0.00051472406,0.00007754119,0.0000011817907,0.00010526938],"genre_scores_gemma":[0.99802995,0.000009771038,0.0014349823,0.00035861033,0.00004719021,0.000006726147,0.000009883378,8.056869e-7,0.000102113],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990946,0.000069297654,0.0003030398,0.00012388319,0.00017972488,0.00022946051],"domain_scores_gemma":[0.99907947,0.00036163547,0.00018325036,0.000074564705,0.000105127714,0.00019598295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011731482,0.000074927586,0.00014720931,0.000100628415,0.00022721618,0.00010135088,0.00040856405,0.000028650877,0.00007769869],"category_scores_gemma":[0.00022963807,0.000037038804,0.00006236487,0.00030117526,0.00041703036,0.00030322987,0.0000047497338,0.00008006492,0.0000015504772],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001326935,0.0000055889213,0.9921024,0.000014472718,0.000009756775,0.0000024702965,0.0005330528,0.0020627733,0.000028054093,0.00009384684,0.00010596965,0.00502837],"study_design_scores_gemma":[0.00026905676,0.00044412792,0.9658602,0.00005042288,0.00004247024,0.000047639343,0.0016004201,0.015169296,0.000025967647,0.0151462965,0.0012633164,0.000080809165],"about_ca_topic_score_codex":0.07195963,"about_ca_topic_score_gemma":0.7914207,"teacher_disagreement_score":0.7194611,"about_ca_system_score_codex":0.0000026317903,"about_ca_system_score_gemma":0.00054786756,"threshold_uncertainty_score":0.93422025},"labels":[],"label_agreement":null},{"id":"W2188524188","doi":"10.1139/e11-023","title":"A partial articulated acanthodian from the Silurian of New Brunswick, Canada","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology; Devonian; Taxon; Chondrichthyes; Late Devonian extinction; Anatomy; Biology; Carboniferous; Zoology","score_opus":0.036144629650857775,"score_gpt":0.20080735951808873,"score_spread":0.16466272986723096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2188524188","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9910321,0.0021222804,0.00002234291,0.0017445097,0.001002224,0.00004259623,0.000045233977,0.0000016426052,0.0039870264],"genre_scores_gemma":[0.99861354,0.00001497051,0.00067524577,0.00046654552,0.00016662723,2.3159844e-8,0.0000035187545,7.795687e-7,0.00005878114],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99889666,0.00013512147,0.00031137848,0.00011947059,0.00016871344,0.00036865417],"domain_scores_gemma":[0.9988644,0.00016977079,0.00021984117,0.00010043007,0.00006354383,0.00058201846],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048106207,0.00008361077,0.00016915837,0.00007659978,0.00031427355,0.000016243332,0.0005336126,0.00006148749,0.0041140607],"category_scores_gemma":[0.00018473939,0.00005130351,0.00005160361,0.00029047366,0.00079847546,0.00017696606,0.0000029534729,0.00017387989,0.000015799527],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017375269,0.0000014656649,0.9965991,4.4479717e-7,0.000018618091,0.00006378976,0.0005178127,0.00023601558,0.0000071291192,0.00022081273,0.00084365794,0.0014737947],"study_design_scores_gemma":[0.00012090725,0.00015291007,0.98958516,0.000013847125,0.000015668566,0.00008982792,0.00040740267,0.00029405518,0.0001315576,0.0007839331,0.0083364835,0.00006822832],"about_ca_topic_score_codex":0.995184,"about_ca_topic_score_gemma":0.9999493,"teacher_disagreement_score":0.020447003,"about_ca_system_score_codex":0.000001957269,"about_ca_system_score_gemma":0.020448959,"threshold_uncertainty_score":0.9967963},"labels":[],"label_agreement":null},{"id":"W2189065366","doi":"10.1139/e11-057","title":"Middle Ordovician (late Dapingian–Darriwilian) conodonts from the Cow Head Group and Lower Head Formation, western Newfoundland, Canada<sup>1</sup>This article is one of a series of papers published in<i>CJES Special Issue: In honour of Ward Neale</i>on the theme of Appalachian and Grenvillian geology.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Memorial University of Newfoundland","keywords":"Conodont; Geology; Paleontology; Ordovician; Head (geology); Fauna; Bay; Group (periodic table); Biostratigraphy; Oceanography; Biology; Ecology","score_opus":0.022326293370663216,"score_gpt":0.19808876806757156,"score_spread":0.17576247469690834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2189065366","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9894301,0.003045892,8.105519e-7,0.003985764,0.0001970044,0.00012802593,0.0001328357,6.964612e-7,0.0030788304],"genre_scores_gemma":[0.9994193,0.00010862063,0.00010067354,0.00025630303,0.00009793305,3.1704442e-7,0.000002000701,0.0000010477933,0.000013861407],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984501,0.0002013735,0.0005864424,0.00013066003,0.00026057704,0.00037084435],"domain_scores_gemma":[0.99880904,0.00030988906,0.00042813705,0.000130886,0.0000652607,0.0002567872],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011477554,0.000125922,0.00037395742,0.00018147708,0.00020527924,0.000041855616,0.0003460793,0.00007289139,0.0006820642],"category_scores_gemma":[0.00013398529,0.000079322446,0.000047625243,0.0003619853,0.0014693195,0.0007232183,0.0000042350903,0.0002145553,4.157574e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000078106554,0.000012623297,0.988147,0.00001552019,0.000024003142,0.0000052165874,0.0078669675,0.0001024945,0.00002343369,0.00008438724,0.00003645637,0.0036037983],"study_design_scores_gemma":[0.00038752487,0.00032178377,0.99291795,0.00015722918,0.000012831137,0.000024043451,0.0045461683,0.00021940566,0.0000538747,0.00027379085,0.0010042627,0.00008114891],"about_ca_topic_score_codex":0.64417464,"about_ca_topic_score_gemma":0.9985613,"teacher_disagreement_score":0.3543867,"about_ca_system_score_codex":0.0000036793617,"about_ca_system_score_gemma":0.0005418647,"threshold_uncertainty_score":0.74681246},"labels":[],"label_agreement":null},{"id":"W2191709205","doi":"10.1139/cjes-2015-0099","title":"Frontal bones of non-avian theropod dinosaurs from the Upper Cretaceous (Santonian–?Campanian) Bostobe Formation of the northeastern Aral Sea region, Kazakhstan","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Core Research for Evolutional Science and Technology","keywords":"Geology; Paleontology; Cretaceous; Cenomanian; Fossa","score_opus":0.02316005880617511,"score_gpt":0.2084324194993599,"score_spread":0.18527236069318478,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2191709205","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9899261,0.0035766782,0.00008102964,0.0032697963,0.0010199654,0.000099975034,0.00014087181,0.0000019770978,0.0018836161],"genre_scores_gemma":[0.999336,0.00003105002,0.00021062144,0.00024562457,0.000120028875,1.6903391e-7,0.000007644728,0.0000015045154,0.000047379544],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99859196,0.00022217138,0.0004117373,0.0001286903,0.0003097998,0.00033562686],"domain_scores_gemma":[0.99872714,0.00013689206,0.00047896407,0.00017551518,0.00017033315,0.00031114143],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006823807,0.000116205854,0.00022979725,0.000109991866,0.00039213712,0.000031610773,0.0007906828,0.00008715351,0.0001633575],"category_scores_gemma":[0.0001283758,0.000060440718,0.00011473424,0.00029231448,0.0015415109,0.00046867243,0.000008855327,0.00019323626,0.000014806348],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003746352,0.000004106443,0.99546784,0.0000019509434,0.000014092464,0.000011884474,0.0019243958,0.00082320214,0.000016513772,0.00002459128,0.0002852861,0.0013886817],"study_design_scores_gemma":[0.00021734287,0.0003078673,0.9909895,0.000049506747,0.00002120189,0.00029434526,0.0031900082,0.0020460414,0.00005655302,0.0007114988,0.0020372379,0.00007889224],"about_ca_topic_score_codex":0.044680927,"about_ca_topic_score_gemma":0.77272654,"teacher_disagreement_score":0.7280456,"about_ca_system_score_codex":0.000004447267,"about_ca_system_score_gemma":0.0012656294,"threshold_uncertainty_score":0.96168065},"labels":[],"label_agreement":null},{"id":"W2193852902","doi":"10.1139/e2012-050","title":"Facies architecture in depositional systems resulting from the interaction of acidic springs, alkaline springs, and acidic lakes: case study of Lake Roto-a-Tamaheke, Rotorua, New Zealand","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Alberta","funders":"","keywords":"Facies; Geology; Sedimentary depositional environment; Hot spring; Spring (device); Geochemistry; Volcano; Hydrology (agriculture); Structural basin; Geomorphology; Paleontology; Geotechnical engineering","score_opus":0.031248525083068225,"score_gpt":0.2559997900808779,"score_spread":0.2247512649978097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2193852902","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970476,0.0018846464,0.000006161759,0.00034108158,0.00032451923,0.00022102393,0.000044802382,0.0000015925216,0.00012856213],"genre_scores_gemma":[0.99970156,0.000021972719,0.000111077745,0.000023824405,0.000114163486,6.521541e-7,0.000004038142,0.0000014599449,0.000021227637],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984724,0.00030362286,0.00045096912,0.00013718805,0.00027555472,0.0003602946],"domain_scores_gemma":[0.99859864,0.00055978575,0.000326886,0.00009681356,0.000075851814,0.00034203762],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015101458,0.000103168946,0.00025518844,0.00033635958,0.00026968602,0.000055075216,0.00027168766,0.00006912719,0.00021469388],"category_scores_gemma":[0.00024750372,0.00006772319,0.00003571553,0.00034626783,0.0007580561,0.0003357107,0.000009654749,0.00037116464,0.0000031289785],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033390595,0.000012380891,0.989135,0.000009278655,0.000022360988,0.00021025242,0.0059917863,0.004313835,0.000021661164,0.000007785349,0.000009781765,0.00023244113],"study_design_scores_gemma":[0.00043477325,0.00035034423,0.9707589,0.00012029808,0.000016776406,0.0028851954,0.024613725,0.0003866772,0.000066966764,0.0000543018,0.0002409775,0.00007102186],"about_ca_topic_score_codex":0.15869601,"about_ca_topic_score_gemma":0.93891764,"teacher_disagreement_score":0.78022164,"about_ca_system_score_codex":7.854434e-7,"about_ca_system_score_gemma":0.0004282606,"threshold_uncertainty_score":0.8469063},"labels":[],"label_agreement":null},{"id":"W2196833702","doi":"10.1139/e2012-011","title":"Copula-based interpretation of continuous rainfall–runoff simulations of a watershed in northern Iran","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Environmental science; Copula (linguistics); Watershed; Surface runoff; Hydrology (agriculture); Joint probability distribution; Water content; Soil science; Geology; Statistics; Mathematics; Geotechnical engineering; Computer science","score_opus":0.015744671664706923,"score_gpt":0.23010311738753308,"score_spread":0.21435844572282617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2196833702","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974457,0.00006977967,0.00023009983,0.00049111387,0.00013208773,0.00007462244,0.0000036155934,0.0000010824068,0.0015518932],"genre_scores_gemma":[0.9994792,0.0000014412685,0.0003516803,0.00012756877,0.000011376704,4.9401297e-7,7.824854e-7,0.0000020757493,0.000025433925],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991523,0.000064440814,0.00031255756,0.00007072941,0.00016044486,0.00023953647],"domain_scores_gemma":[0.999527,0.000054857243,0.00021004459,0.00005925258,0.00001911333,0.00012974985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007206594,0.000061210725,0.00016265032,0.00022272978,0.000091294256,0.000008108101,0.00019465924,0.000028118351,0.0002602528],"category_scores_gemma":[0.000090677466,0.000047635527,0.000043880766,0.00029677435,0.0006609727,0.00030901592,0.0000142646495,0.000063722684,0.00000791633],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011271499,0.000015317384,0.92567074,0.0000041356975,0.0000070243227,0.000002657822,0.0025398168,0.071102664,0.00027955516,0.000019190678,0.000022224402,0.0003253976],"study_design_scores_gemma":[0.0003930349,0.00022797093,0.9915369,0.000043192016,0.000016113734,0.0000028160202,0.0005611536,0.0053183683,0.00091517356,0.00021111307,0.00069244247,0.00008173184],"about_ca_topic_score_codex":0.005318968,"about_ca_topic_score_gemma":0.27300772,"teacher_disagreement_score":0.26768875,"about_ca_system_score_codex":0.0000104788405,"about_ca_system_score_gemma":0.000059309143,"threshold_uncertainty_score":0.80407244},"labels":[],"label_agreement":null},{"id":"W2198744282","doi":"10.1139/e10-091","title":"Evolution of early crust in chondritic or non-chondritic Earth inferred from U–Pb and Lu–Hf data for chemically abraded zircon from the Itsaq Gneiss Complex, West GreenlandThis article is one of a series of papers published in this Special Issue on the theme of <i>Geochronology</i> in honour of Tom Krogh.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Protolith; Zircon; Geochemistry; Geology; Mafic; Hadean; Gneiss; Mantle (geology); Silicate; Planetary differentiation; Crust; Archean; Mantle wedge; Mineralogy; Metamorphic rock; Chemistry; Subduction","score_opus":0.050426933542015086,"score_gpt":0.21364344523436557,"score_spread":0.1632165116923505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2198744282","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962375,0.00043957273,0.000004483488,0.0015398335,0.00008463732,0.00017864932,0.00073749793,8.565048e-7,0.0007769566],"genre_scores_gemma":[0.9984975,0.00005570175,0.0012027214,0.00012146526,0.000083904815,7.973199e-7,0.000020271938,0.0000017995708,0.00001584477],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981523,0.00014191735,0.00084070605,0.00025207712,0.00030112904,0.00031186495],"domain_scores_gemma":[0.9981787,0.0007800454,0.0004758158,0.0002633,0.0001467185,0.00015542188],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000879825,0.00013054613,0.00056999794,0.00023943506,0.00006664309,0.000025239216,0.00087854714,0.00009586926,0.011689179],"category_scores_gemma":[0.0009358944,0.0000752408,0.0000771547,0.00083169626,0.001484992,0.00041681874,0.00003420583,0.00023676819,0.0000016196954],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034902594,0.00007705883,0.97527176,0.00002656641,0.00003871909,0.000007201509,0.0027812952,0.00008375909,0.02001851,0.00007609218,0.0000994883,0.0011705464],"study_design_scores_gemma":[0.00067686057,0.0006354096,0.9738487,0.00022706989,0.000034740307,0.000003862163,0.0022097633,0.0009105622,0.017582906,0.003695954,0.00008264819,0.000091525515],"about_ca_topic_score_codex":0.22957572,"about_ca_topic_score_gemma":0.7173388,"teacher_disagreement_score":0.48776305,"about_ca_system_score_codex":0.0000037660254,"about_ca_system_score_gemma":0.0004790587,"threshold_uncertainty_score":0.98921424},"labels":[],"label_agreement":null},{"id":"W2202932032","doi":"10.1139/cjes-2015-0008","title":"Geophysical models of the Montresor metasedimentary belt and its environs, central Nunavut, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Breccia; Igneous rock; Geochemistry; Geophysics; Magnetic anomaly; Lithology; Shear zone; Seismology; Tectonics","score_opus":0.01888416498207517,"score_gpt":0.16877990082145528,"score_spread":0.1498957358393801,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2202932032","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99200493,0.0037569827,0.0000019079052,0.0029103062,0.00018229072,0.00003643269,0.000097155535,7.119543e-7,0.0010093043],"genre_scores_gemma":[0.9992692,0.000019204206,0.0001287281,0.00045191363,0.00005811887,6.076162e-8,0.000002800751,5.958421e-7,0.00006936176],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988639,0.000069228736,0.00020864418,0.00011961277,0.00040832817,0.0003303072],"domain_scores_gemma":[0.99876535,0.00007434558,0.000135473,0.00006445474,0.000065456974,0.0008949214],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003011088,0.00008395709,0.00018706672,0.000054251348,0.00017313,0.000029788065,0.000382177,0.000024104178,0.00058305386],"category_scores_gemma":[0.00009888856,0.000045001616,0.00006792923,0.00028763103,0.00038304215,0.000203225,0.000010415107,0.00012739339,0.0000018612774],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000072153043,0.000006439174,0.9671573,0.0000035269975,0.000031424144,0.00003913618,0.00011865662,0.030490562,0.000040618783,0.00019620168,0.0009890132,0.0009198801],"study_design_scores_gemma":[0.00021220044,0.00018018419,0.960379,0.000017747036,0.00006240792,0.00005632493,0.00044525779,0.026612794,0.00075386197,0.00889227,0.002258442,0.00012953315],"about_ca_topic_score_codex":0.8781462,"about_ca_topic_score_gemma":0.9937224,"teacher_disagreement_score":0.11557622,"about_ca_system_score_codex":0.0000028260438,"about_ca_system_score_gemma":0.0016690074,"threshold_uncertainty_score":0.63840306},"labels":[],"label_agreement":null},{"id":"W2207387824","doi":"10.1139/cjes-2015-0140","title":"Aeronian (Llandovery, Silurian) conodonts from the Densmore Creek Phosphate Bed and the Budd Road Phosphate Bed, Clinton Group, western New York State","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Phosphate; Oil shale; Phosphorite; Geochemistry; Paleontology; Chemistry","score_opus":0.03294256833229024,"score_gpt":0.22100695184680416,"score_spread":0.18806438351451393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2207387824","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9295983,0.062387325,0.000021383616,0.0036228562,0.0014528936,0.00018362622,0.000090563226,0.0000068996196,0.0026361952],"genre_scores_gemma":[0.99803025,0.00029415617,0.0004250668,0.00077809533,0.0003030294,3.8210794e-7,0.0000039024726,0.000001931631,0.00016316786],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978138,0.00030743435,0.00050062436,0.000289377,0.000451593,0.0006371221],"domain_scores_gemma":[0.99750304,0.00047596186,0.00044185045,0.0002042046,0.00009341327,0.0012815285],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00221377,0.00021252315,0.00038582127,0.00009389222,0.0009108787,0.00077246345,0.0009388884,0.0000881447,0.00021789562],"category_scores_gemma":[0.00020115665,0.00011902884,0.00012606892,0.0003187809,0.0021825708,0.00059833424,0.000004604313,0.0003667388,0.000022594442],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016395052,0.0000024335689,0.9479761,0.0000014239223,0.00005224923,0.00007579287,0.002487817,0.00012771295,7.1479786e-7,0.0000461113,0.0010169969,0.048048686],"study_design_scores_gemma":[0.0018213096,0.00037725756,0.98434144,0.000056904617,0.000047430254,0.00014997683,0.0010307436,0.00041936064,0.000015049437,0.0036537796,0.007909196,0.00017753991],"about_ca_topic_score_codex":0.38707593,"about_ca_topic_score_gemma":0.96684015,"teacher_disagreement_score":0.5797642,"about_ca_system_score_codex":0.0000024891185,"about_ca_system_score_gemma":0.0015306998,"threshold_uncertainty_score":0.80417734},"labels":[],"label_agreement":null},{"id":"W2208973677","doi":"10.1139/cjes-2015-0118","title":"Neo-Tethys geodynamics and mantle convection: from extension to compression in Africa and a conceptual model for obduction","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Institut Universitaire de France; Agence Nationale de la Recherche","keywords":"Geology; Obduction; Mantle convection; Subduction; Geodynamics; Mantle plume; Mantle (geology); Transition zone; Plate tectonics; Geophysics; Oceanic crust; Paleontology; Lithosphere; Tectonics","score_opus":0.06200835366443721,"score_gpt":0.22087254390954503,"score_spread":0.1588641902451078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2208973677","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964986,0.0010178498,0.00085034576,0.0011406866,0.00013946672,0.00005660193,0.000030538555,0.0000016906138,0.00026421776],"genre_scores_gemma":[0.9952153,0.00002062664,0.004491203,0.00016937745,0.000050994488,2.2393822e-7,0.0000044159524,5.9262925e-7,0.000047251935],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993181,0.000028374108,0.00016700978,0.00015571596,0.00013210274,0.00019869792],"domain_scores_gemma":[0.99912405,0.00008298531,0.00006461816,0.000034414577,0.00009426758,0.0005996882],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038748077,0.00006239938,0.00014431306,0.00013823956,0.00013805093,0.00006147309,0.0000923225,0.00003836964,0.00014684738],"category_scores_gemma":[0.00015710368,0.000042864027,0.000022046666,0.00021635846,0.00029588744,0.00018798586,0.0000059840304,0.0000776833,0.0000029150058],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008317084,0.000009266699,0.8355048,0.000004315839,0.000009658137,0.00002572527,0.0033506397,0.1481391,0.00038431436,0.0001790162,0.00034391656,0.011966099],"study_design_scores_gemma":[0.00034958893,0.00039330169,0.32117903,0.000027056003,0.0000136354865,0.000032961692,0.0024908069,0.64901924,0.00004916003,0.0254194,0.00090940885,0.00011639079],"about_ca_topic_score_codex":0.017621458,"about_ca_topic_score_gemma":0.27054137,"teacher_disagreement_score":0.51432574,"about_ca_system_score_codex":0.0000016435558,"about_ca_system_score_gemma":0.00018135944,"threshold_uncertainty_score":0.9889203},"labels":[],"label_agreement":null},{"id":"W2209372662","doi":"10.1139/cjes-2014-0180","title":"Macroflora, paleogeography, and paleoecology of the Upper Cretaceous (Turonian?–Santonian) Saanich Member of the Comox Formation, Saanich Peninsula, British Columbia, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; Royal British Columbia Museum","funders":"","keywords":"Geology; Cretaceous; Paleontology; Paleoecology; Macrofossil; Sedimentary rock; Fluvial; Biostratigraphy; Stratigraphic unit; Structural basin; Holocene","score_opus":0.015560297388116191,"score_gpt":0.1679787495930653,"score_spread":0.15241845220494912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2209372662","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958067,0.0011615262,3.224242e-7,0.0014245289,0.00052358035,0.00009160093,0.00015904092,9.682942e-7,0.0008317385],"genre_scores_gemma":[0.99941087,0.000049336024,0.000021863121,0.00024126554,0.00003889961,2.823002e-7,0.0000015943128,3.443443e-7,0.0002355515],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989004,0.00012400321,0.00026783824,0.00010231497,0.0003398685,0.00026556908],"domain_scores_gemma":[0.9990128,0.00008027429,0.00031525607,0.000046990117,0.0002744952,0.00027012822],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00050757674,0.00006167493,0.00016876517,0.000018655139,0.0005810145,0.00011085281,0.0005642884,0.00005665419,0.00025509493],"category_scores_gemma":[0.00013140023,0.000030203038,0.00007603011,0.0005072387,0.00061315595,0.00023209985,0.000043866163,0.0001237715,8.853465e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000027181843,0.000005022024,0.9926782,0.0000037649395,0.000008556541,0.000006324813,0.00012615482,0.000028714183,0.00043262058,0.000010747227,0.0060274927,0.0006696867],"study_design_scores_gemma":[0.00012519203,0.00012486747,0.9746938,0.000042864496,0.000016657836,0.0003108202,0.0010997396,0.000025285866,0.000177846,0.00012207958,0.02319239,0.00006845939],"about_ca_topic_score_codex":0.7801652,"about_ca_topic_score_gemma":0.99966305,"teacher_disagreement_score":0.21949783,"about_ca_system_score_codex":0.000015209878,"about_ca_system_score_gemma":0.0009252764,"threshold_uncertainty_score":0.44687524},"labels":[],"label_agreement":null},{"id":"W2210407539","doi":"10.1139/cjes-2013-0223","title":"Paleobotanical evidence for the post-Miocene uplift of the Cascade Range","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Botany, Ecology, and Taxonomy Studies","field":"Agricultural and Biological Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Neogene; Paleontology; Late Miocene; Range (aeronautics); Sequoia; Physical geography; Structural basin; Geography","score_opus":0.07487205737385143,"score_gpt":0.25356086102044784,"score_spread":0.1786888036465964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2210407539","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9710633,0.0028755867,0.0000087052,0.02490973,0.0006739908,0.00016570857,0.00001322161,0.0000017609035,0.0002880004],"genre_scores_gemma":[0.99844635,0.00007970553,0.00012331289,0.00090982567,0.00035243735,0.0000030515564,2.7853414e-8,3.6392768e-7,0.0000849577],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990472,0.000091501526,0.00026693332,0.000121490586,0.00017394514,0.000298907],"domain_scores_gemma":[0.99763453,0.001660856,0.00025388532,0.000054029046,0.00021894403,0.00017774072],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015011259,0.00007914448,0.0001717779,0.000013430528,0.000880886,0.000058098798,0.00080485945,0.00004467884,0.00009022421],"category_scores_gemma":[0.0015535612,0.00002067514,0.0001670321,0.00029603567,0.00094385596,0.00013165995,0.000025169309,0.00011432914,0.000002160254],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002330472,0.000013758276,0.986354,0.000007087313,0.000035574656,0.0000021759938,0.00008184577,0.000050273997,0.0028910679,0.00045377135,0.0010817826,0.009005335],"study_design_scores_gemma":[0.00007046328,0.0004314054,0.97179073,0.000040349503,0.000021479835,0.000025356949,0.00041453203,0.000059936767,0.0002415437,0.0002405497,0.026608102,0.00005555646],"about_ca_topic_score_codex":0.00082972366,"about_ca_topic_score_gemma":0.43118447,"teacher_disagreement_score":0.43035474,"about_ca_system_score_codex":0.000004350835,"about_ca_system_score_gemma":0.00017853368,"threshold_uncertainty_score":0.67751515},"labels":[],"label_agreement":null},{"id":"W2213317492","doi":"10.1139/cjes-2015-0083","title":"Peridotite and pyroxenite xenoliths from the Muskox kimberlite, northern Slave craton, Canada","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Hudbay Minerals (Canada); University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Peridotite; Geology; Kimberlite; Geochemistry; Xenolith; Mantle (geology); Metasomatism; Olivine; Craton; Enstatite; Asthenosphere; Amphibole; Pyrope; Petrology; Lithosphere; Chondrite; Meteorite; Paleontology","score_opus":0.017223903060183746,"score_gpt":0.17307770620714763,"score_spread":0.1558538031469639,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2213317492","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9850402,0.004125198,0.000004306032,0.005401442,0.00029986358,0.00003314646,0.00009299235,0.0000022218053,0.0050006355],"genre_scores_gemma":[0.9979578,0.000022253402,0.0002279001,0.0014583488,0.00020545023,9.119986e-8,0.0000066639877,0.000001070654,0.00012041161],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987016,0.00007980345,0.0002610777,0.00017515043,0.00040127756,0.00038109173],"domain_scores_gemma":[0.99819577,0.00021545298,0.00014200718,0.00010122333,0.0002046361,0.0011408958],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00053390575,0.000115490875,0.00019124767,0.00006526566,0.00036620634,0.00020075701,0.00047174608,0.000035528934,0.0021512574],"category_scores_gemma":[0.00034104445,0.000061054496,0.000054092852,0.00044649397,0.0006157199,0.00020666096,0.000009082961,0.00018691587,0.000022915123],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003833879,0.000001036936,0.9951531,5.9068424e-7,0.0000137676425,0.00006983402,0.0002603692,0.00079358916,0.0000042898346,0.000017549291,0.0005468248,0.003135178],"study_design_scores_gemma":[0.00013239164,0.00013116219,0.9592627,0.000013407921,0.000024337349,0.00006929213,0.001355871,0.001197405,0.000032593965,0.004336734,0.03331665,0.0001274449],"about_ca_topic_score_codex":0.9759951,"about_ca_topic_score_gemma":0.9997707,"teacher_disagreement_score":0.035890426,"about_ca_system_score_codex":0.0000033764284,"about_ca_system_score_gemma":0.0025973665,"threshold_uncertainty_score":0.99876094},"labels":[],"label_agreement":null},{"id":"W2216912618","doi":"10.1139/cjes-2015-0007","title":"Cape St. Marys shear zone and the Halifax Group – Rockville Notch Group disconformity, southwestern Nova Scotia: structural development and tectonic significance","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Shear zone; Unconformity; Lineation; Shear (geology); Terrane; Metamorphism; Pressure solution; Clockwise; Metamorphic rock; Nappe; Quartz; Simple shear; Schist; Fold (higher-order function); Geochemistry; Seismology; Tectonics; Paleontology","score_opus":0.020686187355895676,"score_gpt":0.19705247265057213,"score_spread":0.17636628529467646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2216912618","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99424183,0.0027820189,0.000057545032,0.0016401153,0.00020968974,0.00008744964,0.000027987155,0.0000034813572,0.0009498798],"genre_scores_gemma":[0.99802685,0.00001822264,0.001475082,0.0003181368,0.000084211606,1.9524578e-7,0.000008010984,0.0000013706331,0.00006792266],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99849695,0.00007928425,0.00035142637,0.00022918332,0.00039617665,0.00044698815],"domain_scores_gemma":[0.9986407,0.0001336889,0.00017741803,0.00008293011,0.00008487455,0.0008803501],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011549676,0.00015383004,0.00028798482,0.00013348114,0.00042665092,0.00028945532,0.00038905218,0.000049637183,0.00086322194],"category_scores_gemma":[0.00011298444,0.000079120306,0.00005498141,0.00039169422,0.0014138989,0.0003685872,0.00002439218,0.00021752148,0.000019786148],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003573212,0.0000026319133,0.98674524,0.000007749607,0.000029209577,0.00004077305,0.00078407576,0.0005719564,0.000012959617,0.00018572627,0.00004610937,0.011537853],"study_design_scores_gemma":[0.00074492826,0.00023760664,0.9885999,0.00003054195,0.0000339316,0.00029370302,0.001899274,0.00196035,0.0000455902,0.0032675567,0.0026653127,0.00022129601],"about_ca_topic_score_codex":0.104227886,"about_ca_topic_score_gemma":0.85300523,"teacher_disagreement_score":0.74877733,"about_ca_system_score_codex":0.0000030855929,"about_ca_system_score_gemma":0.00046060662,"threshold_uncertainty_score":0.9451675},"labels":[],"label_agreement":null},{"id":"W2224993797","doi":"10.1139/cjes-2015-0076","title":"Secondary migration of hydrocarbons in the Zhujiang Formation in the Huixi half-graben, Pearl River Mouth Basin, South China Sea","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science and Technology Major Project; China National Offshore Oil Corporation; University of Cambridge","keywords":"Geology; Graben; Source rock; Structural basin; Geochemistry; Permeability (electromagnetism); Geomorphology; River mouth; Petrology","score_opus":0.01355213105168767,"score_gpt":0.20065514952030897,"score_spread":0.1871030184686213,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2224993797","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993043,0.00031726103,0.000620461,0.0037117945,0.00008705069,0.00007452578,0.000009793244,0.0000030705614,0.002133011],"genre_scores_gemma":[0.9997122,0.00003659349,0.000059172657,0.00012214806,0.000044189404,0.0000016830566,0.0000014957737,0.0000034815216,0.000019026967],"study_design_codex":"qualitative","study_design_gemma":"observational","domain_scores_codex":[0.9989424,0.00014201501,0.0003421399,0.00006700206,0.0003002388,0.00020620863],"domain_scores_gemma":[0.9995991,0.00005832201,0.00010985842,0.00011114321,0.000025388345,0.00009620725],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011681414,0.000078684374,0.00013023149,0.0005442936,0.00011097673,0.00007631148,0.0003920208,0.000036497313,0.00002961452],"category_scores_gemma":[0.00006847641,0.000038514463,0.00007546094,0.0008191982,0.00018789424,0.0006276964,0.0000033793433,0.00016029707,0.0000043468904],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030115005,0.000081395505,0.4091422,0.000104929284,0.00013687526,0.00031244048,0.41307718,0.14682092,0.0051765046,0.0021465009,0.002814598,0.020156356],"study_design_scores_gemma":[0.0013843246,0.00028074882,0.81692576,0.00044311868,0.00006510531,0.00016360013,0.039088577,0.13153149,0.0022074077,0.0033791312,0.004084555,0.00044615002],"about_ca_topic_score_codex":0.004074066,"about_ca_topic_score_gemma":0.28804746,"teacher_disagreement_score":0.4077836,"about_ca_system_score_codex":0.000014800299,"about_ca_system_score_gemma":0.00023583173,"threshold_uncertainty_score":0.7249438},"labels":[],"label_agreement":null},{"id":"W2228821361","doi":"10.1139/cjes-2014-0155","title":"Evolution of the Hazelton arc near Terrace, British Columbia: stratigraphic, geochronological, and geochemical constraints on a Late Triassic – Early Jurassic arc and Cu–Au porphyry belt","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Pacific Institute for the Mathematical Sciences; Saint Mary's University; Geological Survey of Canada; Dalhousie University","funders":"","keywords":"Geology; Zircon; Terrane; Early Triassic; Geochemistry; Conglomerate; Paleozoic; Volcanic arc; Paleontology; Island arc; Basement; Craton; Volcanic rock; Geochronology; Subduction; Volcano; Sedimentary rock; Permian; Structural basin; Tectonics; Archaeology","score_opus":0.018462685307375392,"score_gpt":0.1884783168544824,"score_spread":0.17001563154710703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2228821361","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960402,0.0011907113,0.0000033051203,0.0011154164,0.0001398578,0.00008734096,0.00006705195,0.0000035812507,0.0013525018],"genre_scores_gemma":[0.9994613,0.000031567684,0.0002680505,0.00012958665,0.00005737566,2.9124382e-7,0.000002746823,0.0000010895112,0.000047984126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99844664,0.00011517965,0.00037733634,0.00025599755,0.0003899171,0.00041495526],"domain_scores_gemma":[0.9985512,0.000139739,0.00027414953,0.00009396481,0.00013675378,0.0008041985],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0007977932,0.00011283467,0.00030709087,0.0000934356,0.0004505343,0.00035505905,0.00033259837,0.00010793532,0.0008473929],"category_scores_gemma":[0.0003877259,0.00008517635,0.0001032933,0.0005304345,0.0041210083,0.00022465743,0.000015094653,0.00030938492,0.0000036306217],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011367817,0.000011044957,0.9893306,0.000004683733,0.00001669951,0.000036581987,0.000082846025,0.00013330241,0.00013705195,0.000030262085,0.00017100344,0.010034583],"study_design_scores_gemma":[0.00034330584,0.0006474007,0.9845786,0.000070739065,0.000031076688,0.00019077156,0.00026220825,0.00075771805,0.000041853094,0.012800415,0.00016013715,0.00011574369],"about_ca_topic_score_codex":0.2609125,"about_ca_topic_score_gemma":0.8880451,"teacher_disagreement_score":0.62713253,"about_ca_system_score_codex":0.0000049397613,"about_ca_system_score_gemma":0.0011047313,"threshold_uncertainty_score":0.9985892},"labels":[],"label_agreement":null},{"id":"W2231561449","doi":"10.1139/cjes-2015-0193","title":"Recovery brachiopod associations from the lower Silurian of South China and their paleoecological implications","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Paleoecology; Paleontology; Geology; Extinction event; Ordovician; Marine transgression; Transgressive; Fauna; Extinction (optical mineralogy); Section (typography); Biostratigraphy; China; Ecology; Sedimentary depositional environment; Archaeology; Geography; Structural basin; Biology","score_opus":0.01883226315081635,"score_gpt":0.2073536104486851,"score_spread":0.18852134729786876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2231561449","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9355923,0.0002771061,0.0070807426,0.05197139,0.0002626867,0.000054788394,0.00006672299,0.000005107954,0.0046891645],"genre_scores_gemma":[0.99828863,0.00001144048,0.0012882671,0.00023533551,0.000060090668,5.7319073e-7,2.4928354e-7,5.1888344e-7,0.00011487942],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992943,0.000067438035,0.00021227173,0.00013560326,0.000093147784,0.00019728448],"domain_scores_gemma":[0.9988258,0.00043546944,0.0002695152,0.00016408284,0.0001105639,0.00019456897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00070166256,0.00006172131,0.0001143165,0.000053171854,0.00038856114,0.00010163906,0.00076829636,0.000041808536,0.00008476623],"category_scores_gemma":[0.0007614026,0.00002879596,0.000057961974,0.00024349135,0.00037939587,0.0002704934,0.000037266884,0.00008639483,0.0000023346056],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002568552,0.000027991864,0.9534229,0.0000018512145,0.000043047592,0.000008881723,0.0025313594,0.00014750264,0.0023709915,0.016816206,0.000689766,0.023936955],"study_design_scores_gemma":[0.00008187663,0.000111366615,0.96877724,0.000023080516,0.000003121217,0.00002038065,0.00014000277,0.000050557992,0.000249379,0.02698808,0.0035016867,0.000053246058],"about_ca_topic_score_codex":0.00034648983,"about_ca_topic_score_gemma":0.010124899,"teacher_disagreement_score":0.06269635,"about_ca_system_score_codex":0.0000044451735,"about_ca_system_score_gemma":0.00061029295,"threshold_uncertainty_score":0.56499314},"labels":[],"label_agreement":null},{"id":"W2232396884","doi":"10.1139/cjes-2015-0122","title":"Olympia Interstadial: vegetation, landscape history, and paleoclimatic implications of a mid-Wisconsinan (MIS3) nonglacial sequence from southwest British Columbia, Canada","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of the Fraser Valley; University of Victoria; Western University; Royal British Columbia Museum","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Stadial; Geology; Tsuga; Interglacial; Vegetation (pathology); Glacial period; Beringia; Macrofossil; Peat; Holocene; Physical geography; Paleontology; Ecology; Archaeology; Geography","score_opus":0.02353869758998567,"score_gpt":0.2108508509175043,"score_spread":0.18731215332751863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2232396884","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99357766,0.0026616622,0.000013488288,0.0013209893,0.0005135822,0.00007040892,0.00018768762,0.0000022904812,0.0016522091],"genre_scores_gemma":[0.99921864,0.00006530063,0.00034449098,0.00017753863,0.000050653096,4.4169605e-7,0.000006976945,0.0000017334187,0.00013422561],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998732,0.00012917937,0.00036998373,0.00019161997,0.0002003122,0.0003769091],"domain_scores_gemma":[0.99846965,0.00045175003,0.00026132766,0.00010603791,0.00017904495,0.0005321608],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00050511095,0.00007631099,0.00023528987,0.00013993068,0.0003211776,0.000089148605,0.0003710608,0.000065854925,0.0021507915],"category_scores_gemma":[0.00032826586,0.00007333986,0.000038194565,0.00019295426,0.0015826839,0.00028405277,0.0000057807424,0.000115175455,0.000008634273],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000354315,0.0000019496615,0.9974547,0.000007844002,0.000013136768,0.00006978878,0.00024730625,0.000010634162,0.000021662525,0.0000111679265,0.00039549873,0.0017627805],"study_design_scores_gemma":[0.00026511843,0.000123666,0.99654555,0.000110898836,0.0000147613,0.00038099353,0.00025618382,0.000044540637,0.0000087863355,0.0007756161,0.0013782583,0.00009563065],"about_ca_topic_score_codex":0.93436134,"about_ca_topic_score_gemma":0.99995494,"teacher_disagreement_score":0.065593645,"about_ca_system_score_codex":0.0000039441343,"about_ca_system_score_gemma":0.0064357216,"threshold_uncertainty_score":0.9991969},"labels":[],"label_agreement":null},{"id":"W2236316817","doi":"10.1139/cjes-2015-0183","title":"Paleolatitudinal morpho-gradient of the early Silurian brachiopod <i>Pentameroides</i> in Laurentia","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; Western University","funders":"National Geographic Society","keywords":"Laurentia; Geology; Paleontology; Baltica; Equator; Oceanography; Latitude; Ordovician","score_opus":0.015213649195205068,"score_gpt":0.20089798476831552,"score_spread":0.18568433557311045,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2236316817","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9860028,0.0030377698,0.00001199596,0.0012668391,0.00059364096,0.00006384396,0.00003970072,0.0000013650686,0.008982062],"genre_scores_gemma":[0.9995865,0.000019444873,0.0002504283,0.000067035595,0.000042561194,1.125142e-7,1.6120467e-7,4.9747433e-7,0.000033227563],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986525,0.00013196688,0.00039378266,0.00014347858,0.00029039462,0.00038787554],"domain_scores_gemma":[0.99906164,0.00013304497,0.00030168024,0.00011993982,0.000053171454,0.00033049058],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00079814455,0.00010015995,0.00019560469,0.0002986263,0.00026404348,0.000043451313,0.00065756624,0.00005299965,0.0005211312],"category_scores_gemma":[0.000100482575,0.000051434057,0.00012611692,0.0005195269,0.0012352451,0.00053687394,0.0000015101164,0.00015732295,0.0000061322244],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008200576,0.0000040225746,0.991932,0.0000019561126,0.000009043921,0.00002962848,0.00015987486,0.000041132258,0.00017495318,0.00024058198,0.00004657813,0.0073520243],"study_design_scores_gemma":[0.00025128396,0.00022678998,0.9973614,0.000108454995,0.000009063578,0.00009239383,0.00010354617,0.000026131416,0.00032751632,0.0010310517,0.00038572063,0.00007665453],"about_ca_topic_score_codex":0.015186529,"about_ca_topic_score_gemma":0.819211,"teacher_disagreement_score":0.80402446,"about_ca_system_score_codex":0.000001303379,"about_ca_system_score_gemma":0.0008296067,"threshold_uncertainty_score":0.99137145},"labels":[],"label_agreement":null},{"id":"W2238014226","doi":"10.1139/cjes-2015-0135","title":"<sup>10</sup>Be ages of flood deposits west of Lake Nipigon, Ontario: evidence for eastward meltwater drainage during the early Holocene Epoch","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"Lawrence Livermore National Laboratory; Dartmouth College; Comer Science and Education Foundation","keywords":"Meltwater; Deglaciation; Geology; Bedrock; Holocene; Geomorphology; Surface exposure dating; Glacial lake; Glacial period; Paleontology; Oceanography; Hydrology (agriculture); Moraine","score_opus":0.0424403011068503,"score_gpt":0.24783049732078088,"score_spread":0.2053901962139306,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2238014226","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99562395,0.0010498384,0.000018044202,0.002192828,0.00019231407,0.00016746184,0.00005475032,0.0000026068876,0.00069818454],"genre_scores_gemma":[0.998266,0.000036261412,0.0004290384,0.00006690017,0.00006015164,9.841965e-7,0.00000147083,0.0000025244108,0.0011366977],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980544,0.00019863759,0.0004874402,0.00022860049,0.00037810754,0.0006528058],"domain_scores_gemma":[0.9979232,0.0008468285,0.00031015647,0.00019330243,0.00031923645,0.00040727813],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019242925,0.00014004129,0.00032450157,0.00032992213,0.000532047,0.000060261238,0.00094614003,0.00010419738,0.0023234168],"category_scores_gemma":[0.000580104,0.0000744422,0.00013645209,0.00033430543,0.0017673511,0.00055965804,0.000015384432,0.00019665231,0.00002783238],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000077657394,0.000004646885,0.99792284,0.000027464268,0.000032153326,0.000059150287,0.0008926938,0.00049156207,0.00007276542,0.00003666903,0.000038308866,0.00034407002],"study_design_scores_gemma":[0.0003656261,0.0006456143,0.99571353,0.00020382112,0.00002537227,0.0003161013,0.00019855284,0.000036781206,0.001706639,0.00037487625,0.0003123873,0.00010069166],"about_ca_topic_score_codex":0.028818985,"about_ca_topic_score_gemma":0.9384809,"teacher_disagreement_score":0.90966195,"about_ca_system_score_codex":0.0000015617516,"about_ca_system_score_gemma":0.001467652,"threshold_uncertainty_score":0.9985886},"labels":[],"label_agreement":null},{"id":"W2239744666","doi":"10.1139/cjes-2015-0052","title":"Neoproterozoic Jiangnan Orogeny in southeast Guizhou, South China: evidence from U–Pb ages for detrital zircons from the Sibao Group and Xiajiang Group","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"China Geological Survey; National Natural Science Foundation of China","keywords":"Zircon; Geology; Orogeny; Rodinia; Supercontinent; Provenance; Geochemistry; Sedimentary depositional environment; Continental arc; Basement; Pluton; Craton; Paleontology; Structural basin; Volcanic rock; Tectonics","score_opus":0.025506628716749215,"score_gpt":0.20067776350739708,"score_spread":0.17517113479064786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2239744666","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9892017,0.00556478,0.0003272894,0.004086173,0.00019520859,0.00013587749,0.00039712002,0.0000044699386,0.00008733741],"genre_scores_gemma":[0.99712044,0.00007143076,0.002264875,0.00024756286,0.00025960212,0.000001241831,0.0000071951126,0.0000021482301,0.000025516752],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983281,0.00011567401,0.00038929956,0.00034137265,0.00029000684,0.00053553144],"domain_scores_gemma":[0.9980741,0.0009228582,0.00021272694,0.00014056591,0.000050703704,0.000599026],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00089171197,0.00016522538,0.00028978023,0.00016048494,0.00043441384,0.00022733616,0.0006874472,0.00007455078,0.0017063726],"category_scores_gemma":[0.00067145133,0.00007834481,0.00013927644,0.00045475204,0.00085575343,0.00050087663,0.000017096902,0.00016153534,0.000027172211],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017705634,0.0000035830583,0.98856497,0.0000020839627,0.00001712679,0.000030643685,0.00059725967,0.000036457477,0.00066068966,0.00002908396,0.000024700106,0.010015678],"study_design_scores_gemma":[0.0002997043,0.00026109006,0.9842695,0.00023171828,0.00003202719,0.00001652085,0.0012187532,0.00024590155,0.00020822506,0.012745467,0.00031187513,0.00015919146],"about_ca_topic_score_codex":0.13256195,"about_ca_topic_score_gemma":0.8124449,"teacher_disagreement_score":0.67988294,"about_ca_system_score_codex":0.0000029060905,"about_ca_system_score_gemma":0.00020224009,"threshold_uncertainty_score":0.9992062},"labels":[],"label_agreement":null},{"id":"W2245523782","doi":"10.1139/e11-040","title":"Tectono-stratigraphic setting of the Moreton’s Harbour Group and its implications for the evolution of the Laurentian margin: Notre Dame Bay, Newfoundland<sup>1</sup>This article is one of a series of papers published in this <i>CJES Special Issue: In honour of Ward Neale</i> on the theme of Appalachian and Grenvillian geology.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Carleton University","funders":"","keywords":"Geology; Felsic; Ophiolite; Pillow lava; Continental margin; Ordovician; Paleontology; Andesites; Geochemistry; Tectonics; Volcanic rock; Andesite","score_opus":0.012220468777023982,"score_gpt":0.18671238675897306,"score_spread":0.17449191798194907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2245523782","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9836705,0.001161817,0.0000012902237,0.01410877,0.00005486054,0.00019309399,0.00012364543,5.469766e-7,0.00068547396],"genre_scores_gemma":[0.999654,0.0000737975,0.00009709358,0.00008860423,0.000060349936,0.000001195738,0.0000013660206,0.0000011930119,0.000022387458],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99868387,0.00015614895,0.0005306671,0.0001273375,0.0002372123,0.0002647627],"domain_scores_gemma":[0.9986816,0.00036712945,0.00056636805,0.00015780803,0.000112754,0.00011432568],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012833787,0.000099209145,0.00030232698,0.00015277702,0.00019119498,0.000019537327,0.00049465906,0.000060417075,0.0012510334],"category_scores_gemma":[0.0003601876,0.000045334462,0.0001237157,0.00092947506,0.0013444779,0.00022602343,0.000021131227,0.00018617137,1.5054273e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025310408,0.000020265881,0.9948614,0.000029121304,0.000026825095,8.584736e-8,0.001957926,0.0006011075,0.00089205866,0.00089605636,0.000042206644,0.00064763456],"study_design_scores_gemma":[0.0001789655,0.00016859497,0.9920712,0.00008309884,0.000040552623,0.000007167933,0.002271309,0.0012197,0.0010073209,0.002739913,0.0001616642,0.000050517967],"about_ca_topic_score_codex":0.031013085,"about_ca_topic_score_gemma":0.48903546,"teacher_disagreement_score":0.45802236,"about_ca_system_score_codex":0.0000030475019,"about_ca_system_score_gemma":0.00021643672,"threshold_uncertainty_score":0.999662},"labels":[],"label_agreement":null},{"id":"W2253204942","doi":"10.1139/cjes-2015-0115","title":"Geochemical characterization and dating of R tephra, a postglacial marker bed in Mount Rainier National Park, Washington, USA","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Yukon University; University of Calgary","funders":"University of California, Irvine; U.S. Geological Survey; University of Calgary","keywords":"Tephra; Geology; Lapilli; Geochemistry; Rhyolite; Radiocarbon dating; Tephrochronology; Conglomerate; Sedimentary rock; Geomorphology; Pyroclastic rock; Paleontology; Volcano; Volcanic rock","score_opus":0.023246073082501085,"score_gpt":0.24221991531187465,"score_spread":0.21897384222937355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2253204942","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970726,0.00012235399,0.0000119630795,0.0012923873,0.00014254889,0.0000434586,0.000036116326,7.124691e-7,0.0012778738],"genre_scores_gemma":[0.9994313,0.000026105334,0.0003011544,0.00012085596,0.00005301779,1.6292923e-7,0.0000060730613,7.7774797e-7,0.000060522892],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989175,0.000119790995,0.00029119663,0.00012684205,0.00024995883,0.0002946683],"domain_scores_gemma":[0.99911946,0.00031014884,0.00015760989,0.00003718233,0.00013958185,0.00023603502],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016707478,0.00006314911,0.0001485151,0.00036055123,0.00014470876,0.000033388325,0.00020655188,0.00007213095,0.0016358735],"category_scores_gemma":[0.00072468835,0.000041640513,0.000023716146,0.00026471316,0.0008044068,0.00040297865,0.000005812455,0.00012469133,0.0000127049625],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019329858,0.0000022610163,0.9975276,0.0000037489062,0.0000043433547,0.00001758183,0.00015496234,0.000009426734,0.0010501656,0.00011620982,0.000008814647,0.0010855368],"study_design_scores_gemma":[0.0002370848,0.00008763617,0.99771833,0.000049732633,0.0000020889652,0.00013862517,0.000059722257,0.00042903543,0.0002570348,0.00038850796,0.0005766211,0.00005555314],"about_ca_topic_score_codex":0.0012742946,"about_ca_topic_score_gemma":0.123496525,"teacher_disagreement_score":0.12222224,"about_ca_system_score_codex":0.0000011327201,"about_ca_system_score_gemma":0.0010150213,"threshold_uncertainty_score":0.99927676},"labels":[],"label_agreement":null},{"id":"W2257373820","doi":"10.1139/cjes-2015-0191","title":"A 1300 year reconstruction of paleofloods using oxbow lake sediments in temperate southwestern Quebec, Canada","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; University of Ottawa","keywords":"Temperate climate; Flood myth; Geology; Radiocarbon dating; Arid; Physical geography; Proxy (statistics); Climate change; Hydrology (agriculture); Archaeology; Geography; Oceanography; Paleontology; Ecology","score_opus":0.024957305701815674,"score_gpt":0.2268352692486249,"score_spread":0.20187796354680923,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2257373820","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974966,0.00027959025,0.0000046402183,0.00055815774,0.00061992777,0.00004440544,0.000037438138,9.165744e-7,0.0009583416],"genre_scores_gemma":[0.9994784,0.000015367266,0.00027931336,0.000060800707,0.000042222302,7.0498686e-8,9.1773165e-7,0.0000010563921,0.00012185839],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99876446,0.00015125354,0.0003232185,0.00013165723,0.00022383199,0.00040555897],"domain_scores_gemma":[0.9992123,0.0001198939,0.00017762707,0.000071906026,0.000093558476,0.00032471662],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007797849,0.00007782981,0.00018937515,0.00037365372,0.00015704762,0.000026450827,0.00027328008,0.000064538326,0.0017410574],"category_scores_gemma":[0.00011153553,0.0000513333,0.00003209667,0.00035324087,0.0006614543,0.00030054405,0.000003456954,0.00013093864,0.000011394274],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012622724,0.0000012513359,0.99853486,0.0000036383158,0.000008023872,0.00006543307,0.00009557534,0.00025490945,0.000027061145,0.0000060329226,0.0000108657905,0.0009797123],"study_design_scores_gemma":[0.0002850984,0.00008935039,0.99831414,0.000093726485,0.000004478019,0.00023723063,0.00034304318,0.00009654771,0.00013343105,0.00008917764,0.00024316859,0.00007060516],"about_ca_topic_score_codex":0.76172984,"about_ca_topic_score_gemma":0.99993896,"teacher_disagreement_score":0.23820916,"about_ca_system_score_codex":0.0000019623599,"about_ca_system_score_gemma":0.0055068517,"threshold_uncertainty_score":0.9991715},"labels":[],"label_agreement":null},{"id":"W2259098866","doi":"10.1139/cjes-2015-0094","title":"A shale gas resource potential assessment of Devonian Horn River strata using a well-performance method","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Geology; Resource (disambiguation); Devonian; Oil shale; Shale gas; Structural basin; Unconventional oil; Mining engineering; Petroleum engineering; Hydrology (agriculture); Geochemistry; Paleontology; Geotechnical engineering","score_opus":0.03856401954911044,"score_gpt":0.27965682263490643,"score_spread":0.241092803085796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2259098866","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9746333,0.00027790078,0.019699141,0.00013036137,0.00021180608,0.0000355348,0.0000047351195,0.0000057002685,0.0050015356],"genre_scores_gemma":[0.979215,0.000015070959,0.020614095,0.000023974497,0.00008376189,2.2418516e-7,6.118381e-7,0.0000059419162,0.00004131251],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989249,0.000060858838,0.0003125435,0.000088280845,0.00036712585,0.00024625604],"domain_scores_gemma":[0.99907863,0.000012634208,0.00011664892,0.00009988874,0.00013216554,0.0005600362],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009980018,0.000084675696,0.00018812787,0.00046031937,0.000120550765,0.00008023448,0.00030457668,0.00003911731,0.00008904104],"category_scores_gemma":[0.000025406,0.00007021559,0.00007267152,0.0006107687,0.00018460647,0.00038635204,0.000008609444,0.00014770211,0.000002846024],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000016668068,0.000003770655,0.011013482,0.000009778986,0.00003637183,0.000039001246,0.0004885877,0.9868327,0.0008774139,0.00003216961,0.00012893233,0.00053616666],"study_design_scores_gemma":[0.00020738512,0.00012499359,0.0039323308,0.000055934204,0.000034811525,0.00009935571,0.0013514525,0.9897978,0.0013359741,0.000050431372,0.0028967834,0.000112771755],"about_ca_topic_score_codex":0.0010640026,"about_ca_topic_score_gemma":0.008156467,"teacher_disagreement_score":0.0070924642,"about_ca_system_score_codex":0.000022990022,"about_ca_system_score_gemma":0.0012441206,"threshold_uncertainty_score":0.45515},"labels":[],"label_agreement":null},{"id":"W2260569831","doi":"10.1139/cjes-2015-0177","title":"A review of paleobotanical studies of the Early Eocene Okanagan (Okanogan) Highlands floras of British Columbia, Canada, and Washington, USA","year":2016,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; Brandon University","funders":"Natural Sciences and Engineering Research Council of Canada; National Geographic Society","keywords":"Geology; Archaeology; Assemblage (archaeology); Paleontology; Palynology; Geological survey; Geography; Ecology; Biology","score_opus":0.046016463408741486,"score_gpt":0.23157122822567835,"score_spread":0.18555476481693686,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2260569831","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.17492643,0.8236787,3.4107273e-8,0.00020058708,0.0002928442,0.00011318864,0.00071863626,5.7765334e-7,0.000069024376],"genre_scores_gemma":[0.03197022,0.9676895,0.0000118317475,0.00007782944,0.00008059296,4.071747e-7,0.000002047378,5.773777e-7,0.00016697883],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99828064,0.00018439005,0.0006918575,0.00016993041,0.00041292267,0.00026025545],"domain_scores_gemma":[0.9979477,0.00032139392,0.001086099,0.000055977765,0.00032623362,0.00026261204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010040852,0.00011382875,0.0010285052,0.000027499984,0.0002467306,0.000041547795,0.0007313342,0.000087608685,0.000119159056],"category_scores_gemma":[0.00041492758,0.000050725062,0.00024050903,0.000571698,0.0009027397,0.00015434262,0.00005843734,0.00015349248,4.8012885e-7],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006505414,0.000038072318,0.21447898,0.025199572,0.0004725311,0.00012892917,0.00012818236,6.860961e-7,0.00005570329,0.00005485729,0.029125854,0.73031014],"study_design_scores_gemma":[0.00008948366,0.00036078546,0.1883841,0.1406212,0.00032939127,0.00029105015,0.00015112376,2.118403e-7,0.0000033519852,0.000060005066,0.6694861,0.00022319867],"about_ca_topic_score_codex":0.7910071,"about_ca_topic_score_gemma":0.9984066,"teacher_disagreement_score":0.7300869,"about_ca_system_score_codex":0.000019752382,"about_ca_system_score_gemma":0.0015149763,"threshold_uncertainty_score":0.3326182},"labels":[],"label_agreement":null},{"id":"W2261729205","doi":"10.1139/cjes-2015-0203","title":"The two-stage Aegean extension, from localized to distributed, a result of slab rollback acceleration","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":113,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Agence Nationale de la Recherche","keywords":"Geology; Seismology; Subduction; Metamorphic rock; Sedimentary rock; Neogene; Mantle (geology); Metamorphic core complex; Detachment fault; Accretionary wedge; Sedimentary basin; Paleontology; Tectonics; Structural basin","score_opus":0.03269920616654275,"score_gpt":0.24138717212855296,"score_spread":0.2086879659620102,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2261729205","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99114007,0.0018755642,0.00037771263,0.004107463,0.0005877643,0.000100499085,0.00034862498,0.0000039794872,0.0014583416],"genre_scores_gemma":[0.9987317,0.00013516804,0.0005521259,0.00022333924,0.0001278559,2.106781e-7,0.0000030676933,0.0000016595479,0.0002249167],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985151,0.0001037604,0.00043450747,0.00017727213,0.000383702,0.0003856284],"domain_scores_gemma":[0.9982924,0.00054438104,0.00025689352,0.00017042524,0.00026413478,0.00047178188],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011021617,0.000105869054,0.00020531504,0.0001433872,0.00065038144,0.00014057211,0.00048159002,0.000030755295,0.00096024305],"category_scores_gemma":[0.00078156893,0.00005077992,0.00007633575,0.0004903952,0.0005597832,0.00031418516,0.0000086750815,0.00008465194,0.00006667402],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000158948,0.000007555281,0.863277,0.0000035166754,0.00006683889,0.00011811133,0.0008141957,0.003129246,0.00081345165,0.00056036963,0.0034623404,0.12758844],"study_design_scores_gemma":[0.00075821835,0.000522404,0.9252047,0.000127467,0.000016834587,0.000026259124,0.0009311973,0.00035649212,0.0016859351,0.0013154895,0.068893515,0.00016152296],"about_ca_topic_score_codex":0.028930115,"about_ca_topic_score_gemma":0.69119793,"teacher_disagreement_score":0.6622678,"about_ca_system_score_codex":0.000002736269,"about_ca_system_score_gemma":0.0008540569,"threshold_uncertainty_score":0.99995303},"labels":[],"label_agreement":null},{"id":"W2262291041","doi":"10.1139/cjes-2015-0136","title":"Tectono-metamorphic evolution of the pre-Athabasca basement within the Wollaston–Mudjatik Transition Zone, Saskatchewan","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Basement; Geochemistry; Metamorphic rock; Orogeny; Lithology; Metallogeny; Drilling; Petrology; Geomorphology; Fault (geology); Tectonics; Structural basin; Seismology","score_opus":0.008793837590798163,"score_gpt":0.17039418389330394,"score_spread":0.16160034630250578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2262291041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905025,0.0006489702,0.00064104475,0.0071266,0.0002895524,0.00008103904,0.000043406453,0.0000023705627,0.00066455925],"genre_scores_gemma":[0.9992257,0.0000064607157,0.0002857746,0.00021462268,0.00008047965,3.2122094e-7,6.6268234e-7,8.790692e-7,0.00018512236],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985732,0.00015699265,0.0003829112,0.00014910099,0.00045259026,0.0002852004],"domain_scores_gemma":[0.998968,0.00015954742,0.00031837742,0.00013857838,0.00013323146,0.00028226944],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012369828,0.00010071779,0.00017195819,0.00013076777,0.00042026394,0.000046734152,0.00060883706,0.000041590913,0.003325689],"category_scores_gemma":[0.00016787031,0.000037019712,0.00017988578,0.0007505121,0.0010192078,0.00022571927,0.0000060694933,0.00013239497,0.000016806638],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022205853,0.000011240184,0.9830494,0.000006682868,0.000041168518,0.0000070382953,0.00084965414,0.0076308977,0.0018730848,0.00028172228,0.00011992663,0.006106968],"study_design_scores_gemma":[0.00017167006,0.00029105443,0.9862171,0.000081275204,0.000052615236,0.00004906238,0.0012535356,0.0012014803,0.0033376357,0.006568592,0.00067555084,0.00010047274],"about_ca_topic_score_codex":0.069044605,"about_ca_topic_score_gemma":0.78729284,"teacher_disagreement_score":0.71824825,"about_ca_system_score_codex":0.0000046439645,"about_ca_system_score_gemma":0.0010034969,"threshold_uncertainty_score":0.9975854},"labels":[],"label_agreement":null},{"id":"W2262410969","doi":"10.1139/cjes-2015-0141","title":"Geologic interpretation of aeromagnetic and chemical data from the Oaks Belt, Wabigoon subprovince, Minnesota: implications for Au-rich VMS deposit exploration","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Minnesota Department of Natural Resources","keywords":"Geology; Interpretation (philosophy); Geochemistry; Geologic map; Paleontology; Seismology; Geophysics","score_opus":0.06156220944203463,"score_gpt":0.23760541898879917,"score_spread":0.17604320954676453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2262410969","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99109834,0.0017349408,0.00078233995,0.005684085,0.00012717673,0.00009109287,0.00015196152,0.0000021460896,0.00032789572],"genre_scores_gemma":[0.99694276,0.000028114751,0.0026393211,0.00016455166,0.00009299659,7.5485906e-7,0.00011471052,7.7563885e-7,0.000016000819],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99908125,0.000055383203,0.00030453101,0.00019478612,0.00015303178,0.00021104261],"domain_scores_gemma":[0.9987481,0.00037172245,0.00020842577,0.00015598071,0.00017901503,0.00033674267],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066308305,0.000078444624,0.00016392645,0.000070481896,0.00018978662,0.000078526566,0.0006332348,0.000044954744,0.00012759815],"category_scores_gemma":[0.0006906648,0.00004462522,0.000037890994,0.00033249278,0.00056177704,0.00047627412,0.000018909821,0.0000822915,0.0000041567296],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017551762,0.000006009067,0.9911123,0.000003376057,0.000013174626,0.0000013135026,0.0003219072,0.00078330014,0.00040353346,0.000068273315,0.00035639666,0.006912901],"study_design_scores_gemma":[0.00022346985,0.00040933516,0.9417472,0.000023917373,0.000088432105,0.000030542036,0.0007681394,0.027433816,0.0005514494,0.027935285,0.0006697473,0.00011869735],"about_ca_topic_score_codex":0.036300138,"about_ca_topic_score_gemma":0.48677877,"teacher_disagreement_score":0.45047864,"about_ca_system_score_codex":0.0000021211554,"about_ca_system_score_gemma":0.00041457108,"threshold_uncertainty_score":0.9701172},"labels":[],"label_agreement":null},{"id":"W2262893100","doi":"10.1139/cjes-2015-0190","title":"Biotic processes in the Okanagan Highlands floras: possible evidence of hybridization in plants adapting to a temperate forest","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Botanical Studies and Applications","field":"Agricultural and Biological Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Arizona State University","keywords":"Anacardiaceae; Flora (microbiology); Taxon; Biology; Ecology; Rosaceae; Temperate climate; Botany; Plant evolution; Paleontology","score_opus":0.05427301362922255,"score_gpt":0.24907262836174707,"score_spread":0.19479961473252452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2262893100","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.990142,0.0004611191,0.00000781884,0.00919159,0.000034249173,0.00008956391,0.000007752199,0.0000010723336,0.00006482139],"genre_scores_gemma":[0.99959457,0.000113576505,0.000063257765,0.00015959525,0.000058207515,0.0000021588812,1.4853931e-7,2.482758e-7,0.000008208659],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992458,0.000039104194,0.00024867195,0.00010338265,0.00015751836,0.00020549053],"domain_scores_gemma":[0.9993336,0.00032786402,0.00011075108,0.000024433006,0.00008488345,0.0001184747],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007065952,0.00005072398,0.00010404153,0.000023521357,0.00017747929,0.000060325303,0.00038222127,0.000017573333,0.000026062953],"category_scores_gemma":[0.00045508458,0.000014231367,0.000019256651,0.0010275828,0.00012273033,0.00020157368,0.000011117786,0.00004333388,0.000002424575],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009462185,0.00001590343,0.9743731,0.0000075327403,0.00000216573,0.000009162317,0.00040781588,0.00022103506,0.00966643,0.00016057344,0.000058741512,0.015068062],"study_design_scores_gemma":[0.000059712933,0.00031577377,0.9959937,0.00053198566,0.0000018194908,0.000012130518,0.0011809478,0.000026148964,0.00063513377,0.0002236795,0.0009601585,0.00005882627],"about_ca_topic_score_codex":0.0064698253,"about_ca_topic_score_gemma":0.7267765,"teacher_disagreement_score":0.7203067,"about_ca_system_score_codex":0.0000053550852,"about_ca_system_score_gemma":0.00010976618,"threshold_uncertainty_score":0.9780484},"labels":[],"label_agreement":null},{"id":"W2265351268","doi":"10.1139/cjes-2015-0155","title":"Role of metalliferous mudstones and detrital shales in the localization, genesis, and paleoenvironment of volcanogenic massive sulphide deposits of the Tally Pond volcanic belt, central Newfoundland, Canada","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Nuclear Laboratories; Teck (Canada); Memorial University of Newfoundland","funders":"","keywords":"Geology; Geochemistry; Ordovician; Felsic; Base metal; Hydrothermal circulation; Mineralization (soil science); Paleontology; Volcano; Oil shale","score_opus":0.005329141069059995,"score_gpt":0.15779014633251845,"score_spread":0.15246100526345846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2265351268","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940957,0.0052387505,0.000007664172,0.00042551852,0.000039404506,0.00005596635,0.0000817791,2.0263998e-7,0.000055021075],"genre_scores_gemma":[0.99966747,0.00021079957,0.000037313108,0.00004949193,0.000016004285,1.3817166e-7,0.0000020201344,9.0314444e-7,0.000015884512],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989306,0.00007000444,0.00033934007,0.00010687915,0.00033377868,0.00021939696],"domain_scores_gemma":[0.9993135,0.0000982979,0.0002866575,0.000078099016,0.000045353587,0.0001781408],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033273263,0.00008169234,0.00017385553,0.00007915281,0.00014937283,0.000020351072,0.0003122702,0.000023467815,0.000111336885],"category_scores_gemma":[0.00006201917,0.000040866515,0.00004503615,0.00030088832,0.00059310417,0.00013429887,0.000009040828,0.000042330663,9.375391e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000070568203,0.000003811143,0.9952133,0.000009214881,0.000023494264,0.00000661512,0.00023982512,0.0012471267,0.0019684564,0.000010696306,0.0000068462887,0.0012635269],"study_design_scores_gemma":[0.00015335999,0.00010783547,0.99382454,0.00004576792,0.000042634052,0.000069305504,0.0015445689,0.00015684796,0.0038013796,0.0001171169,0.00008106564,0.000055602464],"about_ca_topic_score_codex":0.5870896,"about_ca_topic_score_gemma":0.99749094,"teacher_disagreement_score":0.41040134,"about_ca_system_score_codex":0.000005320694,"about_ca_system_score_gemma":0.00069530547,"threshold_uncertainty_score":0.41566},"labels":[],"label_agreement":null},{"id":"W2266015492","doi":"10.1139/cjes-2015-0163","title":"Paleoenvironment of the Quilchena flora, British Columbia, during the Early Eocene Climatic Optimum","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal British Columbia Museum; Brandon University; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; National Geographic Society","keywords":"Taxodium; Temperate climate; Holocene climatic optimum; Ecology; Biology; Botany; Climate change","score_opus":0.012352213174072865,"score_gpt":0.14778968007149945,"score_spread":0.13543746689742658,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2266015492","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977696,0.00019166974,7.098138e-7,0.0014906073,0.00020700155,0.00005206109,0.00005979185,0.0000012553659,0.00022733182],"genre_scores_gemma":[0.99934345,0.000059516085,0.000022074648,0.000063376916,0.000076551776,2.1897168e-7,1.6072899e-7,1.914668e-7,0.00043443078],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99922454,0.00005918908,0.00016198012,0.00008109236,0.0002421474,0.00023104953],"domain_scores_gemma":[0.99953586,0.00007559945,0.00016571664,0.0000336045,0.00003337342,0.00015582146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043929453,0.000038254508,0.00008469953,0.000009177792,0.0007235407,0.00014225017,0.000523226,0.00002731999,0.00050746504],"category_scores_gemma":[0.0000623268,0.000013303093,0.000077255594,0.00019906642,0.0005475853,0.00021662893,0.00002565853,0.00006110067,0.000007968193],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000018498633,0.0000056364497,0.98828816,0.0000019612698,0.000005429498,0.000009138505,0.00007441485,0.000023209746,0.00831993,0.000006736867,0.0002800733,0.0029834684],"study_design_scores_gemma":[0.00006365973,0.00009495391,0.99783015,0.00008987098,0.000006271099,0.00006977196,0.00024389756,0.0000049856194,0.0001811337,0.0001454266,0.0012267382,0.000043138214],"about_ca_topic_score_codex":0.03783096,"about_ca_topic_score_gemma":0.6802398,"teacher_disagreement_score":0.64240885,"about_ca_system_score_codex":0.000009289202,"about_ca_system_score_gemma":0.00006324853,"threshold_uncertainty_score":0.9685762},"labels":[],"label_agreement":null},{"id":"W2268068135","doi":"10.1139/cjes-2015-0150","title":"A revised depositional setting for Halton sediments in the Oak Ridges Moraine area, Ontario","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Sedimentary depositional environment; Geomorphology; Sedimentology; Sedimentary rock; Facies; Sedimentary basin analysis; Geochemistry; Paleontology; Structural basin","score_opus":0.037047929846036394,"score_gpt":0.24991864373943826,"score_spread":0.21287071389340187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2268068135","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9839945,0.0004864523,0.000046456084,0.012060516,0.00024084644,0.00013101853,0.00003408171,0.0000011628341,0.003004996],"genre_scores_gemma":[0.9980676,0.000008306369,0.00080033846,0.0008451338,0.00006952104,9.3054405e-7,0.000005194704,7.364252e-7,0.00020224038],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988219,0.00014254091,0.0002395471,0.0001294836,0.00022499837,0.00044152775],"domain_scores_gemma":[0.9988268,0.0006854795,0.00011662173,0.00006621811,0.00008017113,0.00022470987],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0023215495,0.00007245902,0.00013095363,0.0002526381,0.00045425346,0.00006449227,0.0004452025,0.000049743958,0.0011496037],"category_scores_gemma":[0.00026250843,0.000036754253,0.000054849756,0.00021563975,0.0005176583,0.00026423542,0.000002560473,0.00015124033,0.000022633694],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016742577,0.0000025410716,0.99844915,0.0000025764864,0.000005855965,0.000072214454,0.00031190575,0.00010056118,0.0000074808404,0.00008453883,0.00037843292,0.0005679879],"study_design_scores_gemma":[0.00033814512,0.00027189765,0.992593,0.00006538909,0.0000053048307,0.00039631812,0.00015398418,0.00011049884,0.00002587809,0.0012087444,0.004771574,0.000059278],"about_ca_topic_score_codex":0.018705651,"about_ca_topic_score_gemma":0.9479611,"teacher_disagreement_score":0.9292554,"about_ca_system_score_codex":0.0000015281283,"about_ca_system_score_gemma":0.0017496021,"threshold_uncertainty_score":0.9997635},"labels":[],"label_agreement":null},{"id":"W2268772219","doi":"10.1139/e2012-040","title":"Characterization of green clay concretions from the Tonggao Formation, South China: Mineralogy, petrogenesis and paleoenvironmental implications<sup>1</sup>National Natural Science Foundation of China 40825006.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Clay minerals and soil interactions","field":"Materials Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geology; Concretion; Diagenesis; Geochemistry; Clay minerals; Glauconite; Calcite; Sedimentary rock; Dolomite; Mineral; Marl; Mineralogy; Paleontology; Structural basin; Chemistry","score_opus":0.017669527907523897,"score_gpt":0.24249768996119167,"score_spread":0.22482816205366776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2268772219","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975291,0.0001923549,0.00022259222,0.001218292,0.00028830097,0.0001042801,0.00019961863,0.0000025288252,0.0002429334],"genre_scores_gemma":[0.9989952,0.000021460339,0.00063113356,0.00008539292,0.00018668718,0.000003206819,0.000028884715,0.0000037303435,0.000044325498],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9986676,0.00007305243,0.00047659653,0.00013368507,0.0003975609,0.0002515103],"domain_scores_gemma":[0.9987952,0.00007211347,0.00054408493,0.00011406947,0.00025815054,0.00021636164],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010558497,0.00009628051,0.00015617264,0.00025015653,0.0007000921,0.00012769799,0.0003614514,0.000031598112,0.0002646305],"category_scores_gemma":[0.0002077807,0.00006911442,0.00005684321,0.00042279824,0.0014402969,0.0018441717,0.000027142562,0.00008910088,0.000005197407],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000070920555,0.00001813736,0.22660705,0.0000054373,0.000007946455,2.1707372e-7,0.0049097994,0.0004195089,0.76437306,0.003091428,0.000032897846,0.00052740914],"study_design_scores_gemma":[0.00013839421,0.000058309575,0.97741795,0.000028749646,0.000022187587,0.00006345424,0.0006886921,0.0015663713,0.01933512,0.00022399922,0.00037514337,0.00008160827],"about_ca_topic_score_codex":0.004099771,"about_ca_topic_score_gemma":0.003821839,"teacher_disagreement_score":0.7508109,"about_ca_system_score_codex":0.000029774988,"about_ca_system_score_gemma":0.0006434035,"threshold_uncertainty_score":0.61976546},"labels":[],"label_agreement":null},{"id":"W2270369109","doi":"10.1139/cjes-2015-0153","title":"Upper Llandovery (Telychian) graptolites of the <i>Oktavites spiralis</i> Biozone from the Long Dai Formation, at Lam Thuy village, Quang Binh Province, central Vietnam","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Japan Society for the Promotion of Science; Leverhulme Trust; Vietnam Academy of Science and Technology","keywords":"Biozone; Geology; Paleontology; Paleozoic; Assemblage (archaeology); Ordovician; Biostratigraphy","score_opus":0.010864098173009476,"score_gpt":0.1750989923854203,"score_spread":0.1642348942124108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2270369109","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9872984,0.0026221464,0.00001962541,0.008199414,0.0003543742,0.00009458042,0.00027025607,0.0000038571,0.0011373339],"genre_scores_gemma":[0.99838865,0.00011615557,0.00014875666,0.0009784886,0.00016393849,2.249977e-7,0.000007965249,0.000001477161,0.00019435996],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981987,0.00017530065,0.0004627335,0.00018397506,0.00046484667,0.0005144434],"domain_scores_gemma":[0.9984401,0.0004441565,0.00039403068,0.00018393876,0.0001258031,0.0004119826],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00070959784,0.00014537234,0.00024341328,0.00010410258,0.0008410573,0.00012111293,0.00089560467,0.000056604935,0.0035748277],"category_scores_gemma":[0.00035936642,0.00005362702,0.00024672245,0.00062724773,0.0010972051,0.0004951146,0.000024354911,0.00015789313,0.000041599702],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009906833,0.0000045262886,0.9962632,0.0000032369119,0.000017701586,0.0000100645675,0.00012983018,0.00015805586,0.00050355645,0.00010635038,0.0004767344,0.0023168412],"study_design_scores_gemma":[0.00020701473,0.00011545197,0.9835597,0.000087954526,0.000033402597,0.000055252178,0.00021489516,0.00014546482,0.0028600618,0.003659243,0.008938357,0.00012315578],"about_ca_topic_score_codex":0.01830342,"about_ca_topic_score_gemma":0.59743536,"teacher_disagreement_score":0.5791319,"about_ca_system_score_codex":0.000003944485,"about_ca_system_score_gemma":0.00038834542,"threshold_uncertainty_score":0.99733603},"labels":[],"label_agreement":null},{"id":"W2272160786","doi":"10.1139/cjes-2015-0029","title":"Reconstruction and evolution of Archean intracaldera facies: the Rouyn–Pelletier Caldera Complex of the Blake River Group, Abitibi greenstone belt, Canada","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University; Université du Québec à Chicoutimi","funders":"","keywords":"Geology; Caldera; Archean; Facies; Felsic; Geochemistry; Greenstone belt; Volcano; Mafic; Magma chamber; Outcrop; Volcanic rock; Magma; Geomorphology; Structural basin","score_opus":0.014360323838286138,"score_gpt":0.16815252483887536,"score_spread":0.1537922010005892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2272160786","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99189156,0.0005579423,0.00006946442,0.0065448475,0.0001812441,0.000052364707,0.00007346665,8.630057e-7,0.0006282294],"genre_scores_gemma":[0.99943715,0.00003384198,0.00024245458,0.00017642701,0.000048838418,7.630825e-8,9.1311404e-7,6.7131816e-7,0.0000596316],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987917,0.000114258735,0.0003523635,0.00013129761,0.00034516942,0.0002652101],"domain_scores_gemma":[0.9989778,0.00022421531,0.0002856174,0.00009675726,0.00014497658,0.00027063093],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00053745793,0.000087720364,0.0001966882,0.00008438935,0.00035574465,0.000021107995,0.0003616944,0.00003712117,0.0013615969],"category_scores_gemma":[0.00019385232,0.000036223475,0.00007984415,0.00038436882,0.00273444,0.00014708379,0.000010548371,0.00012809562,0.0000011444617],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006123972,0.0000023023879,0.9827306,0.0000046186174,0.000016398819,0.0000037165382,0.00010301239,0.0002636505,0.00047646507,0.00026519696,0.00014845098,0.015979448],"study_design_scores_gemma":[0.00011684585,0.000104202256,0.9920465,0.00004226725,0.000019396512,0.00012841824,0.00040192727,0.00046778287,0.00015414105,0.005721772,0.00073338737,0.00006337297],"about_ca_topic_score_codex":0.8794759,"about_ca_topic_score_gemma":0.99681324,"teacher_disagreement_score":0.117337346,"about_ca_system_score_codex":0.000005915852,"about_ca_system_score_gemma":0.0007757947,"threshold_uncertainty_score":0.99997956},"labels":[],"label_agreement":null},{"id":"W2274660795","doi":"10.1139/cjes-2015-0194","title":"Carbon isotope (δ<sup>13</sup>C<sub>carb</sub>) and facies variability at the Wenlock–Ludlow boundary (Silurian) of the Midland Platform, UK","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Natural England","keywords":"Geology; Diachronous; Paleontology; Sedimentary depositional environment; Carbonate; Isotopes of carbon; Facies; Unconformity; Phanerozoic; Biozone; Baltica; Excursion; Boundary (topology); Ordovician; Sedimentary rock; Isotope; Biostratigraphy; Structural basin; Cenozoic; Chemistry; Physics","score_opus":0.013572520414128196,"score_gpt":0.1899446662964684,"score_spread":0.17637214588234018,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2274660795","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97959644,0.005532476,0.0000050517674,0.0020766775,0.00044212618,0.00013783232,0.00012094749,0.0000029417995,0.012085502],"genre_scores_gemma":[0.9995541,0.0001305799,0.00004407056,0.00009883116,0.000085777414,3.8797288e-7,3.8482727e-7,9.383338e-7,0.00008494687],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982197,0.0002203816,0.00042419424,0.00023681963,0.00039993253,0.0004989591],"domain_scores_gemma":[0.9983479,0.0005668098,0.00031652546,0.00024031702,0.000094921066,0.00043355225],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0019289711,0.0001694133,0.0002750787,0.00015586597,0.0011186724,0.00012257133,0.00070531777,0.00010789373,0.00024892756],"category_scores_gemma":[0.00031817224,0.00007494441,0.00013763967,0.00036662535,0.00351528,0.00036184103,0.0000071647332,0.00022015664,0.0000028257425],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020593192,0.0000023407495,0.9837003,0.000006281385,0.000024388379,0.000012541962,0.00070168945,0.00009073296,0.0003104699,0.000068130495,0.00008834692,0.01497421],"study_design_scores_gemma":[0.0002493952,0.00023083335,0.99367297,0.000066395325,0.000024894476,0.0002241856,0.0002959682,0.00021011395,0.001099723,0.0019997754,0.0018045738,0.0001211692],"about_ca_topic_score_codex":0.010030292,"about_ca_topic_score_gemma":0.62568736,"teacher_disagreement_score":0.6156571,"about_ca_system_score_codex":0.0000037517275,"about_ca_system_score_gemma":0.0013415694,"threshold_uncertainty_score":0.9991966},"labels":[],"label_agreement":null},{"id":"W2275258172","doi":"10.1139/cjes-2015-0230","title":"Relations between basalts and adakitic–felsic intrusive bodies in a soft-substrate environment: the South Ouessant Visean basin in the Variscan belt, Armorican Massif, France","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Mafic; Felsic; Massif; Partial melting; Petrology; Orogeny; Basalt; Geomorphology; Structural basin","score_opus":0.016204037209263344,"score_gpt":0.1833219126285041,"score_spread":0.16711787541924078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2275258172","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9835435,0.0013797435,0.00005098062,0.013722759,0.000038194732,0.00007151879,0.000049821927,0.0000014022679,0.0011420669],"genre_scores_gemma":[0.9992944,0.00006371451,0.00015211356,0.00035261989,0.00007257406,5.085788e-7,0.0000017580398,9.614877e-7,0.0000613406],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986145,0.00019318146,0.0003104453,0.00019217681,0.00028885005,0.0004008703],"domain_scores_gemma":[0.998912,0.0005113208,0.00016947987,0.00009800102,0.000022472988,0.0002867515],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011480566,0.00010866788,0.00019559312,0.00016299299,0.00036780303,0.00010587157,0.00047353527,0.00003953853,0.0014743494],"category_scores_gemma":[0.00019292596,0.000046545516,0.00005543951,0.00038574074,0.0011626345,0.00022352113,0.000008882815,0.00023021775,0.000029940727],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000023877542,0.0000029831006,0.9925241,0.0000010506848,0.0000060065636,0.000031555523,0.001168201,0.00038314797,0.0000048468123,0.00004722644,0.000019220886,0.0058092875],"study_design_scores_gemma":[0.00015541258,0.000101972204,0.97802424,0.000037522954,0.00001594066,0.000013463183,0.0013432305,0.00031201495,0.000008788025,0.0191618,0.0007404404,0.00008519763],"about_ca_topic_score_codex":0.020129858,"about_ca_topic_score_gemma":0.35089108,"teacher_disagreement_score":0.33076122,"about_ca_system_score_codex":0.0000027835622,"about_ca_system_score_gemma":0.00022794353,"threshold_uncertainty_score":0.99943846},"labels":[],"label_agreement":null},{"id":"W2276097866","doi":"10.1139/cjes-2015-0189","title":"Restudy of the Llandovery conodont biostratigraphy in the Xiushan area, Chongqing City, China","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China; Ohio State University","keywords":"Conodont; Geology; Biostratigraphy; Paleontology; China; Palaeogeography; Archaeology; Geography","score_opus":0.02718687324917258,"score_gpt":0.21589369917138257,"score_spread":0.18870682592221,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2276097866","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96796626,0.0027581109,0.000005915624,0.0026472348,0.0004186922,0.000089784546,0.000030976717,0.0000011440767,0.026081873],"genre_scores_gemma":[0.99973965,0.00004034809,0.000058675178,0.00009909942,0.00004788669,1.598203e-7,1.00267165e-7,3.1894695e-7,0.000013787767],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99870956,0.00020406955,0.00033715626,0.00012320255,0.0003004366,0.00032557367],"domain_scores_gemma":[0.99908787,0.00028065822,0.00027028855,0.0001430987,0.00003960338,0.0001784681],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016198745,0.00009396446,0.00017337373,0.00027093926,0.0003958507,0.000074100666,0.00091199065,0.000047618953,0.00019812472],"category_scores_gemma":[0.00017724783,0.000037995742,0.00012742289,0.0006123554,0.0012498932,0.00031408903,0.0000012585797,0.00016618673,0.000001046401],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006977582,0.0000036837005,0.99277174,0.0000013809822,0.000007721174,0.000023029574,0.0004855786,0.00002180668,0.00003599102,0.00016829094,0.00008052155,0.0063932524],"study_design_scores_gemma":[0.00021102015,0.0002276432,0.9967149,0.00009064674,0.0000066123425,0.000100273675,0.00046014923,0.00001575439,0.00010586092,0.0017646968,0.00023956748,0.000062895895],"about_ca_topic_score_codex":0.015436189,"about_ca_topic_score_gemma":0.8068878,"teacher_disagreement_score":0.79145163,"about_ca_system_score_codex":6.7038474e-7,"about_ca_system_score_gemma":0.00075025583,"threshold_uncertainty_score":0.9911201},"labels":[],"label_agreement":null},{"id":"W2276946064","doi":"10.1139/cjes-2015-0119","title":"Further studies on the focal mechanism and source rupture process of the 2012 Haida Gwaii, Canada, 7.8 moment magnitude earthquake","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Geology; Seismology; Seismic moment; Slip (aerodynamics); Moment magnitude scale; Thrust fault; Focal mechanism; Tsunami earthquake; Aftershock; Subduction; Magnitude (astronomy); Thrust; Fault (geology); Tectonics; Geometry","score_opus":0.021755816192150206,"score_gpt":0.21459137861809982,"score_spread":0.19283556242594962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2276946064","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97909975,0.004974368,0.000010203558,0.014110344,0.0006764087,0.00012615592,0.000037655493,0.0000023053103,0.00096278393],"genre_scores_gemma":[0.9982361,0.00012228926,0.000029432524,0.00087887916,0.00010162932,6.157734e-7,9.6077756e-8,0.0000026229195,0.00062829535],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984169,0.000111697926,0.00031378222,0.00017289932,0.00057999,0.00040474258],"domain_scores_gemma":[0.99870604,0.0004172953,0.00028439425,0.00014734991,0.00017796172,0.00026698143],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00095544994,0.00015293427,0.00023367447,0.000098581964,0.000678536,0.000055845627,0.0005033998,0.000036882037,0.0003368102],"category_scores_gemma":[0.00026482562,0.000058696478,0.00006629217,0.00030251904,0.0010224595,0.00019193653,0.000013906212,0.00016610381,0.0000059246004],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038117752,0.000014579213,0.9274093,0.000041138854,0.00029044374,0.00006978827,0.007134046,0.0011827305,0.000053215434,0.008517744,0.0022834437,0.05296544],"study_design_scores_gemma":[0.00033388878,0.0006079518,0.96967304,0.00029338643,0.000042772353,0.00012080694,0.009138111,0.000078952486,0.0008704862,0.005181494,0.01344298,0.00021613933],"about_ca_topic_score_codex":0.1142762,"about_ca_topic_score_gemma":0.9816876,"teacher_disagreement_score":0.8674114,"about_ca_system_score_codex":0.000004489176,"about_ca_system_score_gemma":0.0017849242,"threshold_uncertainty_score":0.8916219},"labels":[],"label_agreement":null},{"id":"W2277242164","doi":"10.1139/cjes-2015-0209","title":"Early Telychian (Silurian) marine siliciclastic red beds in the Eastern Yangtze Platform, South China: distribution pattern and controlling factors","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Key Research and Development Program of China; China Geological Survey; National Natural Science Foundation of China; University of Cincinnati","keywords":"Siliciclastic; Red beds; Geology; Paleontology; Oceanography; Monsoon; Sedimentary rock; Sedimentary depositional environment; Structural basin","score_opus":0.01741303878147534,"score_gpt":0.19757915519363767,"score_spread":0.18016611641216232,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2277242164","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959432,0.0006499221,0.00018330064,0.0012496733,0.00030138757,0.00008076328,0.00008766262,0.0000028011502,0.0015013181],"genre_scores_gemma":[0.99981815,0.000013243965,0.000029692066,0.000043843524,0.000080310725,1.8474344e-7,0.0000018737411,6.195916e-7,0.000012076782],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987703,0.000100865254,0.00030736031,0.0001570169,0.00023646533,0.00042799482],"domain_scores_gemma":[0.99911654,0.0002282375,0.00019240781,0.00008003864,0.000031137602,0.00035163027],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008572373,0.00012534612,0.00019426076,0.00020920075,0.00041246033,0.000161617,0.00036880083,0.0000657185,0.000119784614],"category_scores_gemma":[0.00014656491,0.000062103965,0.00006277595,0.00026548895,0.000624504,0.00052135036,0.0000013997791,0.00018049264,0.0000034693346],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013408957,0.0000019306221,0.9725996,0.000001851777,0.00000737443,0.00004378229,0.0009367579,0.00001742291,0.000004735055,0.000042357748,0.0000036228769,0.026327105],"study_design_scores_gemma":[0.00040322094,0.00037127853,0.9973024,0.000053228698,0.000010482992,0.00006973375,0.0005532429,0.00032055995,0.000006874261,0.00072461966,0.000088605506,0.000095754585],"about_ca_topic_score_codex":0.018786611,"about_ca_topic_score_gemma":0.5387116,"teacher_disagreement_score":0.519925,"about_ca_system_score_codex":0.0000015256271,"about_ca_system_score_gemma":0.0002939496,"threshold_uncertainty_score":0.9877474},"labels":[],"label_agreement":null},{"id":"W2281323752","doi":"10.1139/cjes-2015-0138","title":"Apatite fission-track evidence for regional exhumation in the subtropical Eocene, block faulting, and localized fluid flow in east-central Alaska","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Fission track dating; Paleogene; Cretaceous; Thermochronology; Paleontology; Fault (geology); Subduction; Dike; Geomorphology; Geochemistry; Zircon; Tectonics","score_opus":0.07033447253597688,"score_gpt":0.2510301818564795,"score_spread":0.18069570932050263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2281323752","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98732024,0.0013685481,0.00027806405,0.01065063,0.00016798975,0.00013423825,0.0000065198174,0.0000013709126,0.00007240709],"genre_scores_gemma":[0.99828666,0.0002504661,0.0010017436,0.00034958223,0.000096586846,9.390588e-7,0.0000012531932,6.7183123e-7,0.000012080166],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99891025,0.00010150756,0.0002814426,0.00014042533,0.00022961685,0.0003367741],"domain_scores_gemma":[0.9991659,0.00042155612,0.000107837266,0.000043781165,0.000058628873,0.00020227897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009095965,0.000073225536,0.0001252732,0.000116497504,0.0002591082,0.000093337694,0.00021584128,0.00003930305,0.00018868025],"category_scores_gemma":[0.000696277,0.0000350884,0.000035132973,0.00024728206,0.00031835298,0.0004515997,0.0000032173718,0.000075092765,0.0000047703247],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000340934,0.0000036470071,0.9757982,0.0000041678686,0.0000015449373,0.000011402339,0.00066194194,0.002096019,0.000013021961,0.000049760576,0.00030091117,0.021025293],"study_design_scores_gemma":[0.00033594394,0.00030610323,0.98658514,0.00017222446,0.0000026663013,0.000032368007,0.00053600007,0.008314778,0.000006893351,0.00073247956,0.0029103165,0.0000650619],"about_ca_topic_score_codex":0.003157738,"about_ca_topic_score_gemma":0.27261457,"teacher_disagreement_score":0.26945683,"about_ca_system_score_codex":0.000003689616,"about_ca_system_score_gemma":0.00026577854,"threshold_uncertainty_score":0.74065834},"labels":[],"label_agreement":null},{"id":"W2282207731","doi":"10.1139/cjes-2015-0222","title":"Late Ordovician jaw-bearing polychaetes from Anticosti Island, eastern Canada, and their biogeographic significance","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"Eesti Teadusagentuur; Grantová Agentura České Republiky","keywords":"Ordovician; Laurentia; Paleontology; Geology; Baltica; Fauna; Polychaete; Bay; Trilobite; Orogeny; Conodont; Gondwana; Biological dispersal; Trace fossil; Biostratigraphy; Ecology; Oceanography; Population; Structural basin; Biology","score_opus":0.014673337025713619,"score_gpt":0.1851521521082613,"score_spread":0.1704788150825477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2282207731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9864547,0.008876082,0.000038068098,0.0013388479,0.00060257316,0.000044852706,0.00027152157,0.0000033125887,0.002370021],"genre_scores_gemma":[0.9994029,0.00012691088,0.00018212582,0.00016547993,0.000087292385,9.577231e-8,7.8365224e-7,8.438916e-7,0.000033585085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987925,0.00007007499,0.0002670151,0.00021143508,0.00018523919,0.00047370285],"domain_scores_gemma":[0.9987388,0.0002513665,0.0001857064,0.00009603162,0.00005556186,0.0006724938],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038083963,0.00014097842,0.00021889943,0.00027344454,0.00047194882,0.000119173645,0.0003889602,0.00005694682,0.00028039693],"category_scores_gemma":[0.00006886905,0.00008104774,0.000055217577,0.0003065504,0.0008606294,0.0003892663,0.0000013843487,0.0001237294,0.0000034125987],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006360571,8.973425e-7,0.94979817,0.0000013409502,0.000019298011,0.000060722643,0.00010117007,0.0000065555123,0.00016176442,0.00001709888,0.00002151049,0.049805127],"study_design_scores_gemma":[0.00016537461,0.00013952909,0.99681,0.000083122264,0.0000075896482,0.00004314435,0.0001648119,0.00013919699,0.00014502982,0.0009694336,0.0011965213,0.00013623187],"about_ca_topic_score_codex":0.92851573,"about_ca_topic_score_gemma":0.9997083,"teacher_disagreement_score":0.07119256,"about_ca_system_score_codex":0.0000013533361,"about_ca_system_score_gemma":0.0015576172,"threshold_uncertainty_score":0.36298963},"labels":[],"label_agreement":null},{"id":"W2283172874","doi":"10.1139/cjes-2015-0210","title":"Paleo-ocean redox environments of the Upper Ordovician Wufeng and the first member in lower Silurian Longmaxi formations in the Jiaoshiba area, Sichuan Basin","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Pyrite; Geology; Anoxic waters; Ordovician; Oil shale; Bottom water; Redox; Geochemistry; Upwelling; Paleontology; Oceanography; Chemistry","score_opus":0.010948288331942335,"score_gpt":0.1900996313534,"score_spread":0.17915134302145766,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2283172874","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9831768,0.00029490082,0.00007840512,0.013532985,0.0001554387,0.0001059942,0.0000065588106,0.0000014232155,0.0026474523],"genre_scores_gemma":[0.9995155,0.0000910858,0.000021161693,0.00028472545,0.000027947575,0.0000013803392,1.6835844e-7,0.000003676186,0.000054398046],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99905485,0.000089023386,0.00032842136,0.00006877495,0.0002485175,0.00021040595],"domain_scores_gemma":[0.99950653,0.00012191691,0.00009167857,0.00015579062,0.000015351421,0.00010874727],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010237651,0.00007983668,0.00013771126,0.0002406017,0.00020385042,0.000068954774,0.00043093972,0.00003324721,0.000095905765],"category_scores_gemma":[0.000114693845,0.000032240547,0.00007298042,0.0005307241,0.0004883631,0.00028746243,0.000010779362,0.00013709579,0.0000024443973],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012323609,0.00002140875,0.90722895,0.000014076794,0.000050761362,0.000029876574,0.01517594,0.07424315,0.00013605352,0.0014328007,0.0005974284,0.0010572062],"study_design_scores_gemma":[0.0015172348,0.00007294593,0.9298648,0.00035760956,0.000044695065,0.00004968169,0.006664792,0.022528432,0.0002966487,0.0013517359,0.037010208,0.00024118234],"about_ca_topic_score_codex":0.00090130715,"about_ca_topic_score_gemma":0.3924232,"teacher_disagreement_score":0.3915219,"about_ca_system_score_codex":0.000013715107,"about_ca_system_score_gemma":0.0001179538,"threshold_uncertainty_score":0.6186635},"labels":[],"label_agreement":null},{"id":"W2286282697","doi":"10.1139/cjes-2015-0197","title":"New data on Hirnantian (latest Ordovician) postglacial carbonate rocks and fossils in northern Guizhou, Southwest China","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"State Key Laboratory of Palaeobiology and Stratigraphy; National Natural Science Foundation of China","keywords":"Geology; Ordovician; Paleontology; Stratotype; Glacial period; Fauna; Carbonate; Global Boundary Stratotype Section and Point; Biostratigraphy; Stage (stratigraphy); Ecology","score_opus":0.03721737763222068,"score_gpt":0.2394216151831291,"score_spread":0.2022042375509084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2286282697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9516981,0.006847443,0.00000846705,0.0015618869,0.0007262811,0.000072045455,0.00007694358,0.0000043217556,0.03900448],"genre_scores_gemma":[0.99909943,0.000023240062,0.0005156283,0.00009898204,0.00022918379,4.601804e-8,0.000004415403,0.0000010580769,0.0000280388],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99844426,0.000092912655,0.0003522742,0.00028344517,0.0003179111,0.00050917454],"domain_scores_gemma":[0.99822205,0.00007295972,0.00020196174,0.00019434009,0.0000554824,0.0012531952],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011172604,0.00015545698,0.0002556243,0.0004815969,0.00031290267,0.00020676175,0.00083869026,0.00009305042,0.00006779138],"category_scores_gemma":[0.00024175768,0.00011895435,0.000037448408,0.0004893287,0.00045559864,0.000681164,0.0000036023944,0.00029771094,0.000011110983],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021181058,0.0000030225756,0.9572113,0.0000013700176,0.0000074874933,0.0002406289,0.00076208,0.00042398172,0.0000010321435,0.000024375484,0.000082639206,0.041220896],"study_design_scores_gemma":[0.0004052862,0.00048186217,0.99518645,0.000050562394,0.000009842868,0.00020755702,0.00043857945,0.0008988114,0.000003257661,0.0008530592,0.001314103,0.00015063718],"about_ca_topic_score_codex":0.20252286,"about_ca_topic_score_gemma":0.99125534,"teacher_disagreement_score":0.78873247,"about_ca_system_score_codex":0.0000020934888,"about_ca_system_score_gemma":0.0033440515,"threshold_uncertainty_score":0.8027876},"labels":[],"label_agreement":null},{"id":"W2286864048","doi":"10.1139/cjes-2015-0223","title":"Biochemostratigraphy of the Eramosa Formation in southwestern Ontario, Canada","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Università degli Studi di Cagliari; Ohio State University; National Science Foundation","keywords":"Conodont; Geology; Dolostone; Baltica; Paleontology; Chemostratigraphy; Laurentia; Biostratigraphy; Carbonate; Ordovician; Sedimentary rock; Paleozoic; Stratigraphy; Isotopes of carbon; Carbonate rock; Geochemistry; Isotope","score_opus":0.015520047452146135,"score_gpt":0.1853891566097726,"score_spread":0.16986910915762646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2286864048","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891642,0.0007913169,0.00000772144,0.00086990563,0.00039811578,0.000042236185,0.000031572443,5.315717e-7,0.00869445],"genre_scores_gemma":[0.9997838,0.0000046222917,0.00010288681,0.00006645135,0.00001607043,6.051783e-8,1.6564475e-7,1.9103565e-7,0.000025733092],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991087,0.00005624707,0.00029497014,0.000074156946,0.00022381908,0.00024214968],"domain_scores_gemma":[0.99937767,0.00007713084,0.0002231559,0.000073973206,0.00005031264,0.00019773204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037568595,0.000064934604,0.00011817232,0.00016774925,0.00016367044,0.000025083238,0.0003845748,0.000036179183,0.00030843072],"category_scores_gemma":[0.00004809875,0.000032756114,0.000057089685,0.00033616016,0.00046906632,0.00035742795,4.969069e-7,0.000095887575,5.640425e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000033779063,8.842215e-7,0.9908009,0.0000016258795,0.0000031939285,0.000013666699,0.00024676917,0.000028632521,0.00005740128,0.00003908992,0.00007020342,0.00873426],"study_design_scores_gemma":[0.0001368236,0.00007638452,0.9978277,0.00006592064,0.0000029626494,0.000067532455,0.0001776654,0.000011608722,0.0007887063,0.0004140387,0.00037998662,0.000050688835],"about_ca_topic_score_codex":0.9754756,"about_ca_topic_score_gemma":0.9999919,"teacher_disagreement_score":0.024516303,"about_ca_system_score_codex":0.0000029644573,"about_ca_system_score_gemma":0.004203667,"threshold_uncertainty_score":0.74571246},"labels":[],"label_agreement":null},{"id":"W2286998524","doi":"10.1139/e2012-061","title":"The provenance of Middle Jurassic sandstones in the Scotian Basin: petrographic evidence of passive margin tectonics <sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of <i>Mesozoic–Cenozoic geology of the Scotian Basin</i>. <sup>2</sup>Geological Survey of Canada Contribution 20110319.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Saint Mary's University","funders":"","keywords":"Geology; Terrane; Provenance; Zircon; Rift; Paleontology; Cretaceous; Geochemistry; Sedimentary rock; Tectonics","score_opus":0.023857068296790563,"score_gpt":0.2049015547851889,"score_spread":0.18104448648839833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2286998524","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98931175,0.0033623858,0.0000012015477,0.005670656,0.00018647984,0.00032977227,0.00021412285,8.879911e-7,0.0009227336],"genre_scores_gemma":[0.9993055,0.00037219282,0.000062149455,0.000171137,0.00005317439,0.0000017461005,0.000003032913,0.0000021663002,0.000028926665],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99628586,0.0009680059,0.0012094734,0.0001755263,0.00080290466,0.00055820943],"domain_scores_gemma":[0.99525166,0.0021512192,0.0014258038,0.00032040343,0.00069529505,0.00015561651],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0051575387,0.00018061645,0.0006305535,0.00025684008,0.00027491772,0.0000328992,0.0012568345,0.0001096003,0.0024784198],"category_scores_gemma":[0.003639372,0.0000839632,0.00014390372,0.0020643699,0.0036668214,0.0005738651,0.000030474876,0.0003383847,7.092971e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015344925,0.000056997098,0.99142015,0.00007984249,0.000029092866,0.0000013522077,0.0026804188,0.0036632235,0.00005512378,0.00075075164,0.00040232693,0.0007073003],"study_design_scores_gemma":[0.0002546551,0.0008710232,0.98768646,0.00043071705,0.00002502518,0.000019381929,0.0044592647,0.0006499658,0.0041745086,0.00055476406,0.00077781884,0.000096400596],"about_ca_topic_score_codex":0.3966114,"about_ca_topic_score_gemma":0.86166596,"teacher_disagreement_score":0.4650546,"about_ca_system_score_codex":0.000009777045,"about_ca_system_score_gemma":0.0022946158,"threshold_uncertainty_score":0.99904466},"labels":[],"label_agreement":null},{"id":"W2287876505","doi":"10.1139/cjes-2015-0228","title":"Earth evolution and dynamics—a tribute to Kevin Burke","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Mantle (geology); Plate tectonics; Mantle convection; Mantle plume; Hotspot (geology); Lithosphere; Subduction; Kimberlite; Geophysics; Tectonophysics; Tectonics; Paleontology","score_opus":0.00969521518978276,"score_gpt":0.19201112239451693,"score_spread":0.18231590720473417,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2287876505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931967,0.00038040642,0.00055323367,0.0034810891,0.00090369105,0.00007118765,0.00019687651,0.0000037544107,0.0012130651],"genre_scores_gemma":[0.9982435,0.000022268903,0.000679363,0.00012656605,0.00019751627,1.262407e-7,0.000001359545,0.0000015351799,0.0007277433],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998964,0.000056924826,0.00023177048,0.00015283324,0.00021993698,0.00037449677],"domain_scores_gemma":[0.99886245,0.00008159387,0.0001172994,0.00008002405,0.00009519818,0.0007634665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000828029,0.00008878683,0.00016719465,0.00024458722,0.00028880587,0.00018495828,0.0002679261,0.0000353211,0.0008544452],"category_scores_gemma":[0.00013917898,0.000053506286,0.000035536646,0.0002749368,0.00024879377,0.00043914065,0.0000058679043,0.000046839774,0.00009756027],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038106067,0.0000061351852,0.9385183,0.000014608592,0.00003225003,0.00011485699,0.00038340682,0.0010698974,0.0029837252,0.0042759497,0.002233497,0.05032927],"study_design_scores_gemma":[0.00017985987,0.0004959932,0.9500504,0.00008967806,0.000011704031,0.00008103265,0.000098529825,0.00028193888,0.00036317224,0.0028757893,0.045304332,0.00016756625],"about_ca_topic_score_codex":0.015228979,"about_ca_topic_score_gemma":0.41995525,"teacher_disagreement_score":0.4047263,"about_ca_system_score_codex":0.0000022642723,"about_ca_system_score_gemma":0.0006698614,"threshold_uncertainty_score":0.9913287},"labels":[],"label_agreement":null},{"id":"W2288631080","doi":"10.1139/cjes-2015-0219","title":"Sequence stratigraphic model for repeated “butter shale” Lagerstätten in the Ordovician (Katian) of the Cincinnati, Ohio region, USA","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"American Chemical Society Petroleum Research Fund","keywords":"Geology; Paleontology; Oil shale; Siliciclastic; Ordovician; Sedimentary depositional environment; Fauna; Outcrop; Turbidity current; Geochemistry; Structural basin","score_opus":0.06951735647902335,"score_gpt":0.2603125769562136,"score_spread":0.19079522047719027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2288631080","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98374325,0.0002911059,0.00012038927,0.013554818,0.00016224383,0.00017116773,0.000031690273,0.0000010466823,0.0019242739],"genre_scores_gemma":[0.99867153,0.000026724087,0.0002405545,0.0008110285,0.000029733472,8.733429e-7,7.821543e-7,0.0000011272915,0.00021763764],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99849147,0.00025923084,0.00035612396,0.00016317701,0.00027599029,0.00045398567],"domain_scores_gemma":[0.99874866,0.00047932283,0.00023622478,0.00019149862,0.00016802187,0.00017627445],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020574846,0.000091981085,0.00017132393,0.00030064714,0.0004393623,0.000042222946,0.0010834468,0.00008183271,0.0002086345],"category_scores_gemma":[0.00039921535,0.000039992596,0.00008970724,0.0006777275,0.001585812,0.000305392,0.0000045131915,0.00020403942,0.000006504409],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000096087315,0.0000022466734,0.9974891,0.000004728163,0.0000057484685,0.000031520223,0.0005699318,0.0009659171,0.000017462993,0.0004653284,0.000093797025,0.00034463548],"study_design_scores_gemma":[0.00020771787,0.00017187533,0.98900205,0.000069971225,0.0000072776147,0.0002533961,0.000318144,0.005034753,0.000038080452,0.004646334,0.00018193698,0.0000684889],"about_ca_topic_score_codex":0.0032034107,"about_ca_topic_score_gemma":0.8527414,"teacher_disagreement_score":0.84953797,"about_ca_system_score_codex":7.6103663e-7,"about_ca_system_score_gemma":0.001564677,"threshold_uncertainty_score":0.584299},"labels":[],"label_agreement":null},{"id":"W2288665748","doi":"10.1139/e02-025","title":"The High Pressure belt in the Grenville Province: architecture, timing, and exhumation","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":124,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Granulite; Terrane; Crust; Geochemistry; Mafic; Metamorphic facies; Foreland basin; Tectonics; Eclogite; Petrology; Metamorphism; Seismology; Facies; Geomorphology; Subduction; Structural basin","score_opus":0.01822243421977823,"score_gpt":0.18063387362504243,"score_spread":0.1624114394052642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2288665748","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9801237,0.005810426,0.0000050370472,0.008124113,0.00007987293,0.000055724813,0.000006830528,0.0000010578779,0.005793252],"genre_scores_gemma":[0.9992069,0.000094449286,0.00015382002,0.00033521475,0.000059987226,1.6705562e-7,7.823966e-7,3.6294495e-7,0.0001483282],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991652,0.000090633876,0.00017216499,0.00009530224,0.00023305204,0.00024368089],"domain_scores_gemma":[0.99943197,0.00021597663,0.00009581665,0.00006171532,0.000028797718,0.00016572762],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007574594,0.000059922102,0.000087291795,0.00008738308,0.0005437454,0.00018616888,0.00038884406,0.000025250585,0.0020750826],"category_scores_gemma":[0.00017225022,0.00002505484,0.00003326757,0.00031729013,0.00054401776,0.00010084053,0.000003617138,0.00017027093,0.000010412958],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000050347003,0.0000066797893,0.8977843,0.000006319471,0.000014887775,0.0000521433,0.00093436684,0.010132487,0.000008950099,0.0006613239,0.00070191093,0.089691624],"study_design_scores_gemma":[0.0000869142,0.00017510119,0.9623365,0.000013787884,0.000014312278,0.000090864894,0.00033356436,0.004919919,0.000013450636,0.010864946,0.021079618,0.00007105246],"about_ca_topic_score_codex":0.016303122,"about_ca_topic_score_gemma":0.55545676,"teacher_disagreement_score":0.53915364,"about_ca_system_score_codex":3.709914e-7,"about_ca_system_score_gemma":0.00007410756,"threshold_uncertainty_score":0.9988372},"labels":[],"label_agreement":null},{"id":"W2288836266","doi":"10.1139/cjes-2015-0165","title":"Determining the paleoclimate and elevation of the late Eocene Florissant flora: support from the coexistence approach","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Paleoclimatology; Temperate climate; Flora (microbiology); Geology; Elevation (ballistics); Subtropics; Paleontology; Taxon; Physical geography; Ecology; Climate change; Oceanography; Geography; Biology","score_opus":0.042894262916586746,"score_gpt":0.1898472149305248,"score_spread":0.14695295201393807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2288836266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956345,0.00009396115,0.0000035341407,0.0036276875,0.00019544382,0.000044040513,0.00007200069,0.0000011344105,0.00032771373],"genre_scores_gemma":[0.99961203,0.000054631644,0.000035254237,0.0001691449,0.00008866747,1.8124129e-7,0.000001032709,1.5335452e-7,0.00003892033],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993885,0.000066241344,0.00013265104,0.00007141464,0.00018310579,0.0001580864],"domain_scores_gemma":[0.99942225,0.00021760339,0.00017436128,0.000031647476,0.00006837299,0.00008578514],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066822016,0.00004733725,0.00007205411,0.000009339541,0.0006591758,0.000061441366,0.00043141414,0.000024458903,0.000052159718],"category_scores_gemma":[0.0001228682,0.000009793533,0.00003901071,0.00019302261,0.0005305075,0.00021340474,0.000023214372,0.00005912116,0.0000018162685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004470456,0.0000028482348,0.9890403,8.1976196e-7,0.0000048606576,0.0000013364149,0.00038700536,0.000011826515,0.0051054386,0.00009903682,0.00025522985,0.0050868164],"study_design_scores_gemma":[0.000053913882,0.00006830348,0.99666435,0.000032696622,0.000009112505,0.000012746793,0.0007924347,0.00007415471,0.0003014717,0.0002211693,0.0017348172,0.000034808392],"about_ca_topic_score_codex":0.0013461414,"about_ca_topic_score_gemma":0.029605797,"teacher_disagreement_score":0.028259655,"about_ca_system_score_codex":0.0000028981262,"about_ca_system_score_gemma":0.000081155325,"threshold_uncertainty_score":0.98810136},"labels":[],"label_agreement":null},{"id":"W2289751185","doi":"10.1139/e06-089","title":"Recent climate and stable isotopes in modern surface waters of northernmost Ungava Peninsula, Canada","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval; Center for Northern Studies","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Peninsula; Geology; Precipitation; Physical geography; Period (music); Isotopes of oxygen; Stable isotope ratio; Climate change; Isotope; Surface water; Oceanography; Geochemistry; Environmental science; Geography; Archaeology","score_opus":0.019808351457194853,"score_gpt":0.22240669550654454,"score_spread":0.20259834404934968,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2289751185","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99230766,0.0037578752,0.0000032776347,0.00073569483,0.0002479519,0.000061954124,0.00003094696,8.770128e-7,0.0028537603],"genre_scores_gemma":[0.9990824,0.00042995746,0.00030340816,0.00011688659,0.0000130324115,2.8452563e-8,0.0000024964963,0.0000012004506,0.00005061647],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99850094,0.00009825705,0.00035106178,0.00014136168,0.00025982878,0.0006485762],"domain_scores_gemma":[0.998977,0.0002236707,0.00014158548,0.00006880703,0.00011278178,0.0004761439],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023848636,0.00008580676,0.00021582274,0.00022831772,0.00029897763,0.000031860713,0.00029511945,0.000055062654,0.00042255656],"category_scores_gemma":[0.00009833463,0.00006577534,0.000019005805,0.0003957908,0.00060876337,0.00020868101,0.000006371334,0.00021178962,0.0000033679494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024847568,0.0000020442278,0.9936068,0.0000083856685,0.0000052280493,0.00021534192,0.00033193,0.004461983,0.0000118604075,0.000014267485,0.000016152102,0.0013011333],"study_design_scores_gemma":[0.0001858439,0.00013762372,0.99542236,0.000027658058,0.0000034043494,0.00017243128,0.0011252266,0.001125548,0.0002051617,0.00012291553,0.0013922857,0.0000795494],"about_ca_topic_score_codex":0.69053787,"about_ca_topic_score_gemma":0.9994925,"teacher_disagreement_score":0.3089546,"about_ca_system_score_codex":0.0000016527205,"about_ca_system_score_gemma":0.002555193,"threshold_uncertainty_score":0.4626698},"labels":[],"label_agreement":null},{"id":"W2294097789","doi":"10.1139/cjes-2015-0186","title":"Is the Lomagundi Event present on the Rae craton? A case study from the Murmac Bay Group","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Geology; Craton; Carbonate; Geochemistry; Metamorphic rock; Dolomite; Carbonate rock; Bay; Carbonate minerals; Sedimentary rock; Calcite; Paleontology; Oceanography; Tectonics","score_opus":0.03725898059505075,"score_gpt":0.24968931896327565,"score_spread":0.2124303383682249,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2294097789","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9704906,0.0034350387,0.000012683761,0.02083191,0.0006756871,0.00023592604,0.000074674805,0.0000026365308,0.0042408793],"genre_scores_gemma":[0.998607,0.000027453552,0.000020071026,0.0010280776,0.00024846938,0.0000010199477,1.302606e-7,6.924147e-7,0.00006708751],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99810284,0.0005232497,0.00030620996,0.00020002865,0.000445396,0.00042228002],"domain_scores_gemma":[0.99743897,0.0016561914,0.00020753795,0.0002721583,0.000057107234,0.00036804233],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0021525046,0.00013593357,0.00014777959,0.00008964624,0.0018874193,0.000245075,0.0010487844,0.00003918811,0.001548204],"category_scores_gemma":[0.00014393948,0.00004326648,0.00013393229,0.0003373896,0.0013156162,0.0002738934,0.0000025886231,0.00025412798,0.00003580612],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011236705,0.000010457213,0.9601139,3.167495e-7,0.00004568358,0.0008371073,0.0022217885,0.000026574337,0.000003225569,0.00011541837,0.0015128085,0.03510152],"study_design_scores_gemma":[0.00019077431,0.00058460754,0.9877201,0.000029215986,0.000024644041,0.000656338,0.0056155263,0.00009748513,0.000015650288,0.0009905465,0.0039934646,0.00008165405],"about_ca_topic_score_codex":0.0823526,"about_ca_topic_score_gemma":0.9216602,"teacher_disagreement_score":0.8393076,"about_ca_system_score_codex":0.0000015677564,"about_ca_system_score_gemma":0.00062390923,"threshold_uncertainty_score":0.999412},"labels":[],"label_agreement":null},{"id":"W2295142572","doi":"10.1139/cjes-2015-0226","title":"A Late Ordovician age for the Whirlpool and Power Glen formations, New York","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Eesti Teadusagentuur","keywords":"Ordovician; Geology; Acritarch; Paleontology; Palynology; Assemblage (archaeology); Pollen; Ecology","score_opus":0.035461734044689885,"score_gpt":0.24075157022116797,"score_spread":0.20528983617647809,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2295142572","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9684427,0.0050674104,0.0002872386,0.020927042,0.00046715388,0.00016916668,0.000025782978,0.000003378143,0.0046101427],"genre_scores_gemma":[0.9977009,0.000072957075,0.0006104726,0.0005255095,0.00006996773,2.8895312e-7,6.602529e-7,8.7690034e-7,0.0010183511],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999163,0.00005450924,0.00017968976,0.000092650414,0.00012945778,0.00038069245],"domain_scores_gemma":[0.9987728,0.00055736594,0.000093687064,0.00007413334,0.000058931044,0.00044309397],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010457438,0.000063365886,0.000109633685,0.0001806506,0.00061939616,0.00011631381,0.00037307866,0.000051130355,0.0011044849],"category_scores_gemma":[0.00026752625,0.000029771792,0.00004118698,0.00020335932,0.0007468029,0.00034975956,0.000003443579,0.00009953416,0.000051713494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008503244,5.160521e-7,0.9943744,0.0000015412966,0.00000943797,0.000011208938,0.00034005204,0.000042871863,0.0000016000537,0.00037189494,0.00085218047,0.0039858227],"study_design_scores_gemma":[0.00023667622,0.00025755542,0.9363089,0.00002525698,0.00000873512,0.00018882692,0.00028066552,0.00015360581,0.0000072271228,0.0039350316,0.058536764,0.00006073627],"about_ca_topic_score_codex":0.0025882388,"about_ca_topic_score_gemma":0.62571585,"teacher_disagreement_score":0.62312764,"about_ca_system_score_codex":2.8323646e-7,"about_ca_system_score_gemma":0.001025791,"threshold_uncertainty_score":0.99980867},"labels":[],"label_agreement":null},{"id":"W2295462978","doi":"10.1139/cjes-2015-0145","title":"Isotopic evidence for a lithospheric origin of alkaline rocks and carbonatites: an example from southern Africa","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Carbonatite; Geology; Magmatism; Geochemistry; Nepheline; Mantle (geology); Lithosphere; Rift; Subduction; Nepheline syenite; Igneous rock; Petrology; Paleontology; Tectonics","score_opus":0.07499936181145551,"score_gpt":0.23559075545656674,"score_spread":0.1605913936451112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2295462978","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954042,0.003166618,0.0004784623,0.0004983879,0.000075839256,0.000049082366,0.00007382384,0.0000021668143,0.00025142133],"genre_scores_gemma":[0.9963179,0.000051534676,0.0032961755,0.00007719753,0.00009473285,2.9400303e-7,0.0000014899248,8.5002625e-7,0.00015981428],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99906975,0.000041925465,0.00026574376,0.00018170882,0.00018315033,0.0002577383],"domain_scores_gemma":[0.99861765,0.0005159325,0.00017724335,0.0000810122,0.00012558147,0.0004825537],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048181368,0.000081215636,0.00020816359,0.00008210407,0.00012931145,0.000046485726,0.0003161585,0.00003740981,0.0036125702],"category_scores_gemma":[0.00027712047,0.000042405758,0.00006496384,0.0002803573,0.00040517567,0.0002726967,0.0000042937368,0.00004675433,0.0000065724935],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017257733,0.0000039712754,0.9865727,0.0000040145,0.0000144083,0.0000060466937,0.0005654769,0.00016942873,0.0007621976,0.000036464044,0.000021493293,0.011826564],"study_design_scores_gemma":[0.0008583754,0.002222608,0.90242755,0.0003407759,0.00012330427,0.000030331808,0.002304007,0.006295508,0.0012422156,0.06732317,0.016399318,0.00043281127],"about_ca_topic_score_codex":0.22094366,"about_ca_topic_score_gemma":0.5523458,"teacher_disagreement_score":0.33140215,"about_ca_system_score_codex":9.813575e-7,"about_ca_system_score_gemma":0.0003188513,"threshold_uncertainty_score":0.99729824},"labels":[],"label_agreement":null},{"id":"W2295493479","doi":"10.1139/cjes-2015-0156","title":"Chemical weathering east and west of the emerging Caledonides in the Silurian – Early Devonian, with implications for climate","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Tallinna Tehnikaülikool","keywords":"Geology; Provenance; Weathering; Authigenic; Glacial period; Geochemistry; Illite; Devonian; Sedimentary rock; Earth science; Structural basin; Arid; Paleontology; Clay minerals","score_opus":0.022854910722510797,"score_gpt":0.2206835149879017,"score_spread":0.1978286042653909,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2295493479","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916172,0.0009601958,0.000026652451,0.0050575994,0.00004748455,0.00007803767,0.000040343555,7.7330446e-7,0.0021716985],"genre_scores_gemma":[0.9994725,0.000014236396,0.00044385542,0.000037460206,0.000026919522,5.5539795e-7,6.837354e-8,3.8670467e-7,0.000004032278],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993753,0.000040369538,0.00016797567,0.0000857364,0.00008815321,0.00024251091],"domain_scores_gemma":[0.9994696,0.00017372509,0.00012458143,0.00007064375,0.000038444563,0.00012300139],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006115558,0.00005586392,0.000094578296,0.00008844445,0.00032273188,0.000044601013,0.00034996227,0.000025268513,0.00003413898],"category_scores_gemma":[0.000060499915,0.00002291931,0.00003634395,0.00023012488,0.00083291426,0.00020494775,7.9339384e-7,0.00006543014,3.9160142e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006037845,0.0000012053295,0.9869858,0.000002893439,0.0000036726485,0.0000016134504,0.0005375444,0.000011424004,0.00018698454,0.0002828956,0.0000033091524,0.011976639],"study_design_scores_gemma":[0.00013604843,0.000101984595,0.99841803,0.00006825909,0.000005989768,0.00009834874,0.0003750021,0.000017534447,0.00006792585,0.000467101,0.00020251046,0.000041239713],"about_ca_topic_score_codex":0.001910415,"about_ca_topic_score_gemma":0.36390162,"teacher_disagreement_score":0.3619912,"about_ca_system_score_codex":5.54974e-7,"about_ca_system_score_gemma":0.00032329556,"threshold_uncertainty_score":0.64770555},"labels":[],"label_agreement":null},{"id":"W2296305985","doi":"10.1139/cjes-2015-0172","title":"A primitive clupeomorph from the Albian Loon River Formation (Northwest Territories, Canada)","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Incertae sedis; Paleontology; Taxon; Cretaceous; Geology; Ammonite","score_opus":0.014622593512406008,"score_gpt":0.18008534289455097,"score_spread":0.16546274938214497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2296305985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.985729,0.001533174,0.00007148093,0.008213055,0.0015939013,0.000056707227,0.00068631175,0.0000024825217,0.0021139155],"genre_scores_gemma":[0.99861616,0.000043472173,0.00019046466,0.00076299865,0.0003143321,1.549838e-7,0.000018895054,6.979343e-7,0.000052817068],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989726,0.00012901751,0.00022724566,0.00011580746,0.00021363935,0.00034169733],"domain_scores_gemma":[0.9989257,0.0003720604,0.00018070654,0.000080085374,0.00009803314,0.00034342468],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004243925,0.00008314604,0.000120186414,0.00007055892,0.00062407396,0.00003439024,0.00044538855,0.000054336517,0.0009950761],"category_scores_gemma":[0.00017520315,0.000041170348,0.00003617822,0.00016759294,0.0010870527,0.0005394585,0.0000030817819,0.00010788185,0.000021960976],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009395338,7.971192e-7,0.9927992,3.9486795e-7,0.000009239589,0.000046154666,0.0002094588,0.000038647442,0.000007022365,0.000095335046,0.001226367,0.0055579804],"study_design_scores_gemma":[0.00013406984,0.00011803262,0.9378743,0.000026771917,0.00000770401,0.0001488991,0.00030832068,0.00006316246,0.00002684888,0.000627924,0.060593694,0.00007025136],"about_ca_topic_score_codex":0.96297115,"about_ca_topic_score_gemma":0.9999429,"teacher_disagreement_score":0.059367325,"about_ca_system_score_codex":0.000008090656,"about_ca_system_score_gemma":0.0037944368,"threshold_uncertainty_score":0.99991816},"labels":[],"label_agreement":null},{"id":"W2298331322","doi":"10.1139/cjes-2015-0164","title":"Early extensional detachments in a contractional orogen: coherent, map-scale, submarine slides (mass transport complexes) on the outer slope of an Ediacaran collisional foredeep, eastern Kaoko belt, Namibia","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"McGill University; University of Victoria","funders":"","keywords":"Geology; Paleontology; Submarine landslide; Facies; Diachronous; Stratigraphy; Passive margin; Extensional tectonics; Continental margin; Continental shelf; Tectonics; Structural basin; Geomorphology; Rift; Landslide","score_opus":0.02125706235330632,"score_gpt":0.21226091878095227,"score_spread":0.19100385642764595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2298331322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99566245,0.00017595255,0.000038219572,0.0026264533,0.00025954502,0.00011272534,0.00024181946,0.0000025067213,0.0008803542],"genre_scores_gemma":[0.9987458,0.000011102958,0.00050717616,0.0004462252,0.00012036672,8.338602e-7,0.000018549894,0.0000019803201,0.00014795389],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99779844,0.00013327028,0.0005805975,0.0002705326,0.00074913853,0.00046804696],"domain_scores_gemma":[0.9983805,0.00037845032,0.0002763151,0.00011943075,0.00021060808,0.00063469727],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010249728,0.0001684821,0.0003423236,0.00025530605,0.00025597092,0.000057532186,0.0005791888,0.00007017578,0.00796857],"category_scores_gemma":[0.00008411955,0.00008139918,0.0001793173,0.00040019592,0.0008019539,0.00040578275,0.0000059447366,0.00019551812,0.000038814174],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000090895206,0.000027376622,0.995984,0.000002407809,0.000025245869,0.00007646158,0.000044053144,0.000765255,0.00044825042,0.00017603471,0.000042840602,0.0023171343],"study_design_scores_gemma":[0.00044770978,0.0005103769,0.99195653,0.00007580918,0.000019434783,0.00004665732,0.00008919101,0.0008386096,0.00034503752,0.004598092,0.0009433248,0.00012924692],"about_ca_topic_score_codex":0.017459767,"about_ca_topic_score_gemma":0.4669534,"teacher_disagreement_score":0.44949365,"about_ca_system_score_codex":0.0000045917927,"about_ca_system_score_gemma":0.00045147954,"threshold_uncertainty_score":0.9929383},"labels":[],"label_agreement":null},{"id":"W2298543957","doi":"10.1139/cjes-2015-0205","title":"Upper Middle to lower Upper Ordovician chitinozoans and conodonts from the Bliudziai-150 core, southern Lithuania","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"University of California, San Diego; Landesverteidigungsakademie; Eesti Teadusagentuur; Geocenter Danmark","keywords":"Conodont; Geology; Biozone; Ordovician; Paleontology; Facies; Biostratigraphy; Sedimentary depositional environment; Trilobite; Waves and shallow water; Oceanography","score_opus":0.029327572345261767,"score_gpt":0.2114699217318444,"score_spread":0.18214234938658264,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2298543957","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9767212,0.004244241,0.000020511798,0.004587053,0.00067891495,0.00008240468,0.00031447015,0.0000042210763,0.013346939],"genre_scores_gemma":[0.9979989,0.000032722226,0.00060400023,0.0009660171,0.00020913813,2.2088933e-7,6.473898e-7,0.0000011647122,0.00018717583],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99866635,0.00008285455,0.00028501058,0.0002261164,0.00023996281,0.00049972784],"domain_scores_gemma":[0.99846727,0.0003428234,0.000143783,0.00014043359,0.000073946794,0.00083176425],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00065588113,0.00014049899,0.00020063893,0.000184368,0.00069184764,0.00018702631,0.00057779043,0.00007336559,0.0016077373],"category_scores_gemma":[0.00017511188,0.00007002577,0.00008403855,0.0002768768,0.0010948095,0.00034314123,0.0000022118993,0.00014611366,0.00009440658],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000149396365,0.0000020738098,0.97003704,6.0266524e-7,0.000016278143,0.000035070043,0.00091630564,0.0000042725005,0.000038763326,0.00014892184,0.00016912854,0.02861662],"study_design_scores_gemma":[0.00019538606,0.00028795266,0.98910975,0.00008517797,0.000012960779,0.000074519754,0.00095073786,0.000020603678,0.00001997638,0.001169661,0.007943297,0.00012997397],"about_ca_topic_score_codex":0.03074952,"about_ca_topic_score_gemma":0.7938743,"teacher_disagreement_score":0.7631248,"about_ca_system_score_codex":0.0000011157631,"about_ca_system_score_gemma":0.000655886,"threshold_uncertainty_score":0.99930495},"labels":[],"label_agreement":null},{"id":"W2299185555","doi":"10.1139/cjes-2016-0013","title":"Camel fossils from gravel pits near Edmonton and Vauxhall, and a review of the Quaternary camelid record of Alberta","year":2016,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"Pleistocene-Era Hominins and Archaeology","field":"Social Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Alberta Museum","funders":"","keywords":"Quaternary; Radiocarbon dating; Pleistocene; Megafauna; Geology; Deglaciation; Last Glacial Maximum; Archaeology; Paleontology; Glacial period; Holocene; Geography","score_opus":0.045649236112439616,"score_gpt":0.31232952638615724,"score_spread":0.26668029027371765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2299185555","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.018220503,0.9779471,0.0000014747379,0.001386388,0.00053006655,0.0002703236,0.000086429995,8.289106e-7,0.0015568618],"genre_scores_gemma":[0.0031909514,0.99587286,0.00029140443,0.00016330258,0.0001648612,0.000002238412,5.4625104e-7,0.0000071516415,0.00030667277],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99761605,0.0005404249,0.0008291378,0.0002481885,0.000374094,0.00039211538],"domain_scores_gemma":[0.9970306,0.0006184534,0.0014335901,0.00018736898,0.00017336539,0.0005566157],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0016971964,0.00019751007,0.001226051,0.00018455597,0.0004755059,0.000055827488,0.0009466804,0.00014574961,0.00016970004],"category_scores_gemma":[0.00092143944,0.000109763416,0.00024597388,0.00038893236,0.0041252635,0.00021221364,0.000066790366,0.00022502219,0.000001883375],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000039123424,0.000009420019,0.030880947,0.0037227548,0.00009704597,0.000033761342,0.0042462386,6.9077444e-8,0.0000020782704,0.0014339072,0.0006989904,0.9588709],"study_design_scores_gemma":[0.00010867595,0.00018225606,0.006790648,0.05533237,0.00014944744,0.000058906415,0.00019071932,7.560659e-7,0.0000014617063,0.00071539404,0.9362975,0.00017190573],"about_ca_topic_score_codex":0.07091839,"about_ca_topic_score_gemma":0.7555546,"teacher_disagreement_score":0.958699,"about_ca_system_score_codex":0.000019967305,"about_ca_system_score_gemma":0.008172611,"threshold_uncertainty_score":0.9985849},"labels":[],"label_agreement":null},{"id":"W2300188916","doi":"10.1139/cjes-2015-0220","title":"Architecture of the Canadian portion of the High Arctic Large Igneous Province and implications for magmatic Ni–Cu potential","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Sill; Orogeny; Igneous rock; Geochemistry; Arctic; Magma; Archipelago; Volcano; Paleontology; Rift; Sverdrup; Dike; Structural basin; Oceanography","score_opus":0.007346757321238862,"score_gpt":0.17688800117366993,"score_spread":0.16954124385243108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2300188916","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9822112,0.00028256423,0.00008605239,0.016749928,0.0001318911,0.00011515399,0.00024004167,6.3789037e-7,0.00018256778],"genre_scores_gemma":[0.99934644,0.0000061118762,0.00030252236,0.00020941874,0.000033474334,3.01643e-7,0.0000012318999,6.621704e-7,0.00009986761],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991946,0.000046925987,0.00024345114,0.00009992003,0.0001570008,0.00025807112],"domain_scores_gemma":[0.9991131,0.000091447,0.0002537793,0.00010495622,0.00013842474,0.00029831514],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040427837,0.000060234877,0.0001271082,0.00009917558,0.00042134785,0.000028692833,0.00041473052,0.000034543802,0.0005204712],"category_scores_gemma":[0.00033093066,0.000023938403,0.000092440765,0.000299578,0.0006703034,0.00007141366,0.0000066299053,0.00007049165,9.946956e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000029531145,0.0000028167124,0.9939213,0.000011187128,0.000010279461,0.0000011032228,0.000043862194,0.0004911002,0.00034081182,0.00062929746,0.000040984167,0.0045042955],"study_design_scores_gemma":[0.00008447785,0.000085632324,0.9663385,0.00004266435,0.000028583485,0.00005320515,0.000032165095,0.00011259485,0.00017091434,0.032647967,0.00036192243,0.000041367355],"about_ca_topic_score_codex":0.36668238,"about_ca_topic_score_gemma":0.99173325,"teacher_disagreement_score":0.62505084,"about_ca_system_score_codex":0.000002775082,"about_ca_system_score_gemma":0.0011758176,"threshold_uncertainty_score":0.6375349},"labels":[],"label_agreement":null},{"id":"W2303208212","doi":"10.1139/cjes-2015-0238","title":"A new species of the basal plesiadapiform <i>Purgatorius</i> (Mammalia, Primates) from the early Paleocene Ravenscrag Formation, Cypress Hills, southwest Saskatchewan, Canada: further taxonomic and dietary diversity in the earliest primates","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Primate Behavior and Ecology","field":"Psychology","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Royal Tyrrell Museum","funders":"Office of International Science and Engineering; National Science Foundation","keywords":"Paleogene; Paleontology; Geology; Cretaceous; Range (aeronautics); Insectivore; Genus; Biology; Zoology","score_opus":0.03175791315449505,"score_gpt":0.21610102488154684,"score_spread":0.18434311172705178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2303208212","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909513,0.00066402403,0.000017270186,0.0065343054,0.0007712291,0.00018153274,0.0002083519,0.0000022555116,0.0006697256],"genre_scores_gemma":[0.99897754,0.000025106643,0.000067824454,0.0005805433,0.0001355883,0.0000018733588,0.0000013491093,0.0000055579626,0.00020458875],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99848753,0.00017008853,0.0004167365,0.00016796692,0.0002995527,0.00045815067],"domain_scores_gemma":[0.9986827,0.00033997578,0.00039811747,0.00026610537,0.000080039965,0.00023306036],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007730876,0.00015081312,0.00024956916,0.00008412152,0.000552871,0.00008366993,0.0011368712,0.00007250102,0.00049076945],"category_scores_gemma":[0.000058034544,0.00006950823,0.00007275792,0.00021545793,0.00075869146,0.0003365577,0.00009606299,0.00019348264,0.0000055274563],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024255784,0.000008230789,0.985149,0.000002930621,0.000018986333,0.000026411188,0.010232503,0.0000041016347,0.00017778907,0.00015254685,0.003487205,0.0007160262],"study_design_scores_gemma":[0.00047138068,0.00008392245,0.98409,0.00004203364,0.000035434943,0.000045901754,0.012423375,0.000001188603,0.00021553932,0.00032352214,0.0021673793,0.00010035059],"about_ca_topic_score_codex":0.82089525,"about_ca_topic_score_gemma":0.99362016,"teacher_disagreement_score":0.17272492,"about_ca_system_score_codex":0.000047317317,"about_ca_system_score_gemma":0.0022794397,"threshold_uncertainty_score":0.53735816},"labels":[],"label_agreement":null},{"id":"W2305686837","doi":"10.1139/cjes-2016-0003","title":"A high-resolution, continuous δ<sup>13</sup>C record spanning the Ordovician–Silurian boundary on Anticosti Island, eastern Canada","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"","keywords":"Geology; Ordovician; Paleontology; Chemostratigraphy; Excursion; Bay; Laurentia; Isotopes of carbon; Oceanography; Chemistry; Total organic carbon","score_opus":0.014399352751158993,"score_gpt":0.19708974906477078,"score_spread":0.18269039631361178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2305686837","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.975404,0.003107333,0.00008151351,0.008375959,0.0014430889,0.0001003132,0.00013764577,0.000005484003,0.011344629],"genre_scores_gemma":[0.9984372,0.000036347876,0.00023876435,0.0007113867,0.00033220762,2.656815e-7,0.0000010382903,0.000001394631,0.00024135676],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997965,0.00018923295,0.00042870818,0.00024370363,0.00045403143,0.0007193199],"domain_scores_gemma":[0.99834824,0.00037290942,0.0003021071,0.00017434916,0.0001287253,0.00067364326],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0009554859,0.0001812557,0.00027900634,0.0002602422,0.0013816972,0.00023739223,0.0007597252,0.0000753853,0.0007149316],"category_scores_gemma":[0.00028227127,0.000095979936,0.00009228006,0.00040552398,0.0010840239,0.00042064532,0.0000016966243,0.00026621966,0.000025572834],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029405473,0.0000027048798,0.92704123,0.0000021019946,0.000025211639,0.00024237669,0.0001893825,0.0006025573,0.0000028703455,0.00011277512,0.001990898,0.069758505],"study_design_scores_gemma":[0.0003327057,0.0004906846,0.96516716,0.00014448151,0.000016226764,0.00021906075,0.00042201683,0.0005648314,0.000009025621,0.0005918151,0.03187322,0.0001687532],"about_ca_topic_score_codex":0.805279,"about_ca_topic_score_gemma":0.9990254,"teacher_disagreement_score":0.19374636,"about_ca_system_score_codex":0.000006087937,"about_ca_system_score_gemma":0.004816675,"threshold_uncertainty_score":0.99991834},"labels":[],"label_agreement":null},{"id":"W2308758292","doi":"10.1139/cjes-2015-0173","title":"Taphocoenoses and diversification patterns of calcimicrobes and calcareous algae, Ordovician, Tarim Basin, China","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université Laval; Geological Survey of Canada","funders":"","keywords":"Geology; Paleontology; Ordovician; Paleoecology; Algae; Carbonate; Hermatypic coral; Reef; Ecology; Biology; Oceanography","score_opus":0.015828783149559822,"score_gpt":0.2072982664126617,"score_spread":0.19146948326310187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2308758292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.991736,0.005006218,0.000077506076,0.0008681588,0.00017704457,0.000043952194,0.000114074,0.0000018374436,0.0019751897],"genre_scores_gemma":[0.999223,0.00030493815,0.00037219672,0.000049407092,0.000029440813,5.536969e-8,4.8738406e-7,4.159561e-7,0.000020066891],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992262,0.000058379563,0.00021442767,0.00013619073,0.00013098937,0.00023378902],"domain_scores_gemma":[0.99921775,0.00011920392,0.00017916677,0.00005870838,0.00006422482,0.00036096998],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037874727,0.00008233491,0.00016455752,0.00025857688,0.00031591166,0.00004911992,0.00019517426,0.000049835384,0.00017217272],"category_scores_gemma":[0.00008609687,0.000051160343,0.000036449113,0.00014315502,0.00089444936,0.0003662713,0.0000012945382,0.000066744586,0.0000010515806],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005779708,0.0000016074273,0.94219804,0.0000053312624,0.000008995094,0.00002253906,0.0002988628,0.000003090931,0.0001410981,0.000100775775,0.000024969508,0.057188887],"study_design_scores_gemma":[0.00015874793,0.00027194177,0.99781317,0.00006451032,0.000012778155,0.00015768658,0.00027639905,0.000017888548,0.00038587698,0.00034831546,0.00041800083,0.000074666495],"about_ca_topic_score_codex":0.03640738,"about_ca_topic_score_gemma":0.4449106,"teacher_disagreement_score":0.4085032,"about_ca_system_score_codex":7.0492626e-7,"about_ca_system_score_gemma":0.0003608413,"threshold_uncertainty_score":0.97000927},"labels":[],"label_agreement":null},{"id":"W2312336295","doi":"10.1139/cjes-2013-0163","title":"Are Wilson Cycles preserved in Archean cratons? A comparison of the North China and Slave cratons","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Craton; Geology; Archean; Subduction; Lithosphere; Terrane; Paleontology; Mantle (geology); Tectonics; Geochemistry; Rift; Earth science; Seismology","score_opus":0.03051316254116193,"score_gpt":0.21918073535284777,"score_spread":0.18866757281168584,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2312336295","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944486,0.0010320178,0.0000014006611,0.0032598514,0.00006805314,0.000070315866,0.000017945498,0.0000012302736,0.0011005718],"genre_scores_gemma":[0.9995897,0.000012929483,0.0001822342,0.00014655963,0.000029656343,2.3516758e-7,9.2996197e-7,6.4504917e-7,0.000037150134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99887365,0.00010227203,0.0003362665,0.00013504633,0.00024215666,0.000310619],"domain_scores_gemma":[0.9990089,0.000110656845,0.00030798255,0.00008887779,0.00007346203,0.00041012146],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000328953,0.00008909532,0.00025166204,0.00016220189,0.00022459969,0.00009212152,0.0004588133,0.00003652926,0.0017637679],"category_scores_gemma":[0.00028681583,0.000047465808,0.00007732962,0.00064459624,0.00081526226,0.00024194882,0.000012626591,0.00021452784,0.000009688415],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000018676893,0.000006331011,0.99631107,0.0000048333395,0.0000055527316,0.000004556118,0.00022131362,0.0019938806,0.000022123982,0.000008490831,0.00010265589,0.001317322],"study_design_scores_gemma":[0.00007919773,0.00008853561,0.99100804,0.00003677178,0.000008262766,0.000009134554,0.00062089023,0.004670022,0.00016484347,0.0030642643,0.00018437565,0.00006566017],"about_ca_topic_score_codex":0.09476415,"about_ca_topic_score_gemma":0.90693307,"teacher_disagreement_score":0.8121689,"about_ca_system_score_codex":9.56854e-7,"about_ca_system_score_gemma":0.00022193842,"threshold_uncertainty_score":0.9991487},"labels":[],"label_agreement":null},{"id":"W2312404339","doi":"10.1139/e2012-036","title":"Canadian meteorites: a brief review","year":2012,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University; Geological Survey of Canada","funders":"","keywords":"Meteorite; Chondrite; Enstatite; Achondrite; Astrobiology; Geology; Meteoroid; Geochemistry; Mars Exploration Program; Earth science; Impact crater; Physics","score_opus":0.05359246399486398,"score_gpt":0.27991192875867205,"score_spread":0.22631946476380807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2312404339","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00000487287,0.98185885,0.000016142207,0.00015262607,0.00092609075,0.00019618253,0.0002714533,0.0000015018375,0.01657228],"genre_scores_gemma":[0.00039435187,0.9971774,0.0005417407,0.00026731746,0.0008503646,0.0000022225383,0.00003072782,0.0000107750475,0.0007250871],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9977429,0.00015042695,0.0006647126,0.00022637271,0.00031393816,0.0009016732],"domain_scores_gemma":[0.9962553,0.000107116975,0.00062232104,0.00020629229,0.000113232294,0.0026957442],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016112742,0.00029169762,0.0010629314,0.0006148964,0.00045163863,0.00018690937,0.0011962213,0.00006692016,0.0052477005],"category_scores_gemma":[0.0000338484,0.00020991759,0.0004275476,0.0009884589,0.00031486727,0.0005002824,0.0000106417865,0.0004815375,0.00023819425],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[7.904168e-8,0.0000027186616,0.0041327556,0.0010283429,0.00005273855,0.000036842066,0.000040258124,0.0000022975164,1.2963291e-8,0.0008299402,0.0033287841,0.9905452],"study_design_scores_gemma":[0.000021341517,0.000044486034,0.00015901546,0.011113481,0.00029911773,0.00012386324,0.000025763313,0.0000011447756,4.3778797e-8,0.000030179099,0.9879587,0.00022283106],"about_ca_topic_score_codex":0.39754656,"about_ca_topic_score_gemma":0.6229778,"teacher_disagreement_score":0.9903224,"about_ca_system_score_codex":0.000022033448,"about_ca_system_score_gemma":0.020996569,"threshold_uncertainty_score":0.9956616},"labels":[],"label_agreement":null},{"id":"W2312598670","doi":"10.1139/cjes-2014-0090","title":"New age data refine extent and duration of Paleozoic and Neoproterozoic plutonism at Ganderia–Avalonia boundary, Newfoundland","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Newfoundland and Labrador; Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Geology; Plutonism; Zircon; Geochemistry; Paleozoic; Devonian; Hornblende; Pluton; Provenance; Geochronology; Orogeny; Paleontology; Biotite; Tectonics","score_opus":0.026243646832550798,"score_gpt":0.21262218271200797,"score_spread":0.18637853587945719,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2312598670","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943668,0.002711958,0.00013534642,0.0017514145,0.0001272353,0.000044441764,0.000023858356,0.0000020964383,0.00083680917],"genre_scores_gemma":[0.99707097,0.00012895347,0.0023011162,0.00016548841,0.00009940335,4.6390582e-8,0.00001841735,9.311529e-7,0.00021465999],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988779,0.0000592859,0.0003304819,0.00022840676,0.00024258718,0.00026133674],"domain_scores_gemma":[0.99883145,0.000088886445,0.00021812634,0.00014543998,0.00004787459,0.0006682139],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000781025,0.00010408773,0.00024503085,0.00013943297,0.00033231193,0.00018067448,0.00034361755,0.000044293196,0.0012926254],"category_scores_gemma":[0.00021382073,0.00006577082,0.0000327156,0.00023421322,0.0005337418,0.00032464927,0.00002478319,0.00009859629,0.000007042645],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013548641,0.0000020315754,0.97968537,0.000009976478,0.000013094606,0.00002268215,0.00010444157,0.00011298933,0.0003491655,0.000050666582,0.000101753125,0.019534305],"study_design_scores_gemma":[0.00026040434,0.00041214123,0.98069507,0.00003331986,0.000032878466,0.00017170112,0.000040122544,0.0036663453,0.000095965275,0.006434625,0.008048981,0.00010842986],"about_ca_topic_score_codex":0.05182662,"about_ca_topic_score_gemma":0.784961,"teacher_disagreement_score":0.7331343,"about_ca_system_score_codex":0.0000013189743,"about_ca_system_score_gemma":0.0002933614,"threshold_uncertainty_score":0.9996203},"labels":[],"label_agreement":null},{"id":"W2312904110","doi":"10.1139/e2012-013","title":"Deep transverse basement structural control of mineral systems in the southeastern Canadian Cordillera<sup>1</sup>Geological Survey of Canada Contribution 20110294.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Sedimentary rock; Archean; Mineralization (soil science); Carbonatite; Geochemistry; Basement; Facies; Proterozoic; Geomorphology; Paleontology; Structural basin; Tectonics; Mantle (geology)","score_opus":0.01661556144060724,"score_gpt":0.18431585045353854,"score_spread":0.1677002890129313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2312904110","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99575824,0.002309022,0.000023679246,0.0007355109,0.00020547204,0.00012706564,0.00039452608,6.6370984e-7,0.00044581725],"genre_scores_gemma":[0.9996395,0.00000635267,0.000024071118,0.00023261686,0.00006146657,3.4927433e-7,0.000025321513,8.35302e-7,0.000009485256],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99758077,0.00047604775,0.0005906865,0.00012878262,0.0005035039,0.00072021555],"domain_scores_gemma":[0.99807155,0.00040669768,0.0002667977,0.00009696457,0.0002755718,0.0008823876],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0022588335,0.0001356291,0.00041690332,0.0002072379,0.00019862021,0.000036831025,0.0005176658,0.00006663024,0.0026263988],"category_scores_gemma":[0.00044220823,0.00007483033,0.000090496615,0.00056788354,0.00047705864,0.00017706373,0.0000025117324,0.0001936024,0.000002926446],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019159736,0.000004496544,0.95562553,0.0000049548908,0.000021200345,0.000020202833,0.00021608979,0.043831587,0.000007157674,0.00005532701,0.000041160652,0.00015311492],"study_design_scores_gemma":[0.00029951023,0.00017296016,0.96092427,0.000018702362,0.000026517164,0.000042308304,0.0012009352,0.036909338,0.000010517691,0.000056951198,0.00024055807,0.00009740335],"about_ca_topic_score_codex":0.9969843,"about_ca_topic_score_gemma":0.99984086,"teacher_disagreement_score":0.006922248,"about_ca_system_score_codex":0.000008273591,"about_ca_system_score_gemma":0.0018533309,"threshold_uncertainty_score":0.99828535},"labels":[],"label_agreement":null},{"id":"W2313324982","doi":"10.1139/cjes-2012-0184","title":"Species composition of the Late Cretaceous eutherian mammal<i>Paranyctoides</i>Fox","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; University of Alberta","funders":"","keywords":"Cretaceous; Taxon; Mesozoic; Genus; Mammal; Paleontology; Synonym (taxonomy); Range (aeronautics); Fauna; Geography; Geology; Zoology; Ecology; Biology","score_opus":0.023674278181494934,"score_gpt":0.20139141384164838,"score_spread":0.17771713566015346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2313324982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96301645,0.0032729073,0.000008227661,0.002801127,0.0008151401,0.00008478784,0.000022997774,0.000002695736,0.029975658],"genre_scores_gemma":[0.9982987,0.00004264709,0.00023064732,0.00038886463,0.000060830876,1.4624875e-7,6.9842304e-7,9.966667e-7,0.0009764842],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989822,0.00011329258,0.0002937188,0.00008375223,0.0002358028,0.0002912286],"domain_scores_gemma":[0.99919516,0.00009623551,0.00025748194,0.0000911011,0.00015074507,0.00020927149],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041333243,0.00008661489,0.00017649944,0.0001463885,0.00053920137,0.00008361356,0.0004405667,0.000039328363,0.0028213365],"category_scores_gemma":[0.00005772683,0.000051506897,0.00009202742,0.00035443492,0.0012589619,0.00029593118,0.0000042937118,0.00013356851,0.00007545287],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000028088607,0.0000018044343,0.9967858,0.000003298381,0.000013230964,0.0000059562253,0.00047268576,0.0011997748,0.00015518087,0.0001026223,0.00052406336,0.0007327718],"study_design_scores_gemma":[0.00009921822,0.000108250555,0.9893518,0.000032727155,0.000009962968,0.00009038227,0.00059894886,0.00030146766,0.00014883692,0.00045190318,0.008739746,0.00006675345],"about_ca_topic_score_codex":0.014746601,"about_ca_topic_score_gemma":0.52869135,"teacher_disagreement_score":0.51394475,"about_ca_system_score_codex":0.0000013759162,"about_ca_system_score_gemma":0.0004310891,"threshold_uncertainty_score":0.9980902},"labels":[],"label_agreement":null},{"id":"W2314234888","doi":"10.1139/cjes-2012-0165","title":"Pore-water extraction from the unsaturated and saturated zones","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Alberta Innovates; University of Waterloo","funders":"","keywords":"Pore water pressure; Soil water; Water content; Silt; Geology; Sediment; Vadose zone; Moisture; Capillary fringe; Water table; Tailings; Groundwater; Soil science; Mineralogy; Environmental chemistry; Geotechnical engineering; Chemistry; Geomorphology","score_opus":0.013714557673939308,"score_gpt":0.20329346866738557,"score_spread":0.18957891099344626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2314234888","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944588,0.00022307702,0.00011539407,0.0042048614,0.00027549232,0.000055556364,0.0000018643643,0.0000023851906,0.0006625595],"genre_scores_gemma":[0.99844736,0.000012436485,0.00021605965,0.00043596883,0.00004767525,0.0000010233509,0.0000012551864,0.0000018302852,0.0008364143],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99935114,0.000043393225,0.0001485596,0.00009659743,0.00016838289,0.00019191283],"domain_scores_gemma":[0.99963087,0.0000472777,0.00006797145,0.00004958346,0.000036659763,0.00016763291],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002651287,0.00006340818,0.00007368698,0.000039780236,0.00048120116,0.00025346657,0.00016817954,0.000022890286,0.0016309066],"category_scores_gemma":[0.000027876651,0.000030377387,0.000019943496,0.00015307564,0.00053140975,0.00065588934,0.000015683701,0.00008907282,0.00009601793],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006521956,0.000010973938,0.8895043,0.0000014504432,0.00004090613,0.000054667118,0.0064514303,0.00021514438,0.030904803,0.0001037767,0.0078107477,0.064895265],"study_design_scores_gemma":[0.00008719145,0.00004961517,0.96516806,0.000008117916,0.0000073159968,0.000048554288,0.001354108,0.0001244351,0.0016428812,0.00036725512,0.031076988,0.00006546851],"about_ca_topic_score_codex":0.03561117,"about_ca_topic_score_gemma":0.10178947,"teacher_disagreement_score":0.07566376,"about_ca_system_score_codex":0.0000074936784,"about_ca_system_score_gemma":0.000044887678,"threshold_uncertainty_score":0.99928176},"labels":[],"label_agreement":null},{"id":"W2314342400","doi":"10.1139/e2012-071","title":"Plate tectonic reconstructions and paleogeographic maps of the central and North Atlantic oceans<sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of<i>Mesozoic–Cenozoic geology of the Scotian Basin</i>.<sup>2</sup>Earth Sciences Sector Contribution 20120172.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies Worldwide","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography","funders":"","keywords":"Geology; Cretaceous; Paleontology; Rift; Magnetic anomaly; Continental margin; Aptian; Tectonics","score_opus":0.011594104836122922,"score_gpt":0.17106597635803403,"score_spread":0.1594718715219111,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2314342400","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934757,0.0010519356,2.4946158e-7,0.003533776,0.00024783946,0.00021321738,0.00016294955,0.0000014914589,0.0013128474],"genre_scores_gemma":[0.99935764,0.00024145872,0.000057680758,0.00013602074,0.00015494305,4.0609757e-7,0.0000012944707,0.0000015659743,0.000048984224],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978857,0.00029586858,0.00060464314,0.00020114989,0.00044390248,0.0005687303],"domain_scores_gemma":[0.99840516,0.00046132682,0.0005697995,0.0001647247,0.00016764106,0.00023137503],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001140878,0.00015755603,0.0004607168,0.0001952214,0.00052596256,0.000042826443,0.0005298676,0.000066465975,0.0029203913],"category_scores_gemma":[0.00050795736,0.00007743687,0.00014737897,0.0013381145,0.0064588482,0.00040477703,0.00003758682,0.00025580265,0.0000015594084],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003852594,0.000024533068,0.9956677,0.000020070089,0.000036650763,7.680768e-7,0.0015898164,0.001061839,0.000048668408,0.00047231422,0.000100369725,0.0009387707],"study_design_scores_gemma":[0.00027733526,0.0005116276,0.9943491,0.00014079659,0.00003710268,0.00003371269,0.0013831868,0.0003123826,0.00072582904,0.0010284889,0.0011082577,0.000092158116],"about_ca_topic_score_codex":0.016694399,"about_ca_topic_score_gemma":0.14978068,"teacher_disagreement_score":0.13308628,"about_ca_system_score_codex":0.0000023982493,"about_ca_system_score_gemma":0.0003674542,"threshold_uncertainty_score":0.9979911},"labels":[],"label_agreement":null},{"id":"W2315343977","doi":"10.1139/cjes-2012-0129","title":"A reevaluation of<i>Sigilmassasaurus brevicollis</i>(Dinosauria) from the Cretaceous of Morocco","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Holotype; Cretaceous; Paleontology; Geology; Dorsum; Taxon; Margin (machine learning); Anatomy; Biology; Taxonomy (biology); Zoology; Computer science","score_opus":0.029346544146393205,"score_gpt":0.22168251374766434,"score_spread":0.19233596960127114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2315343977","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.983323,0.010279028,0.00003056137,0.0018622794,0.0005832526,0.0001064232,0.00007517201,0.0000015282227,0.0037387793],"genre_scores_gemma":[0.99860245,0.00009613095,0.00089521677,0.00024275853,0.00011442671,2.8169728e-7,0.000005870233,7.5471945e-7,0.00004212651],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987447,0.00022841105,0.00040868268,0.000116630006,0.00024527806,0.0002562498],"domain_scores_gemma":[0.9985578,0.00048401934,0.00040038963,0.00011539246,0.00022049854,0.00022188101],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010205426,0.000079614045,0.0002189057,0.00013906157,0.00024078549,0.000026237438,0.0005452604,0.00007480117,0.0031259404],"category_scores_gemma":[0.00034860437,0.000048593618,0.000082162165,0.00034530228,0.0010368808,0.000349271,0.0000037475913,0.00013277003,0.000044614248],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008487959,0.0000027329245,0.99184704,0.0000023311238,0.000019423293,0.0000057640204,0.00025905512,0.0015525308,0.00016764995,0.00008134849,0.00072052435,0.005333107],"study_design_scores_gemma":[0.0001227973,0.0002824682,0.99142575,0.000029521705,0.000019980782,0.00006520291,0.00039795134,0.0015459134,0.00010525588,0.002453985,0.0034932357,0.00005796454],"about_ca_topic_score_codex":0.044923652,"about_ca_topic_score_gemma":0.42086643,"teacher_disagreement_score":0.37594277,"about_ca_system_score_codex":0.0000013024228,"about_ca_system_score_gemma":0.0010360355,"threshold_uncertainty_score":0.99778533},"labels":[],"label_agreement":null},{"id":"W2315384596","doi":"10.1139/cjes-2013-0170","title":"In situ LA–ICP–MS dating of monazite from aluminous gneisses: insights on the tectono-metamorphic history of a granulite-facies domain in the central Grenville Province","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University","keywords":"Geology; Granulite; Metamorphism; Monazite; Geochemistry; Gneiss; Metamorphic rock; Orogeny; Zircon; Facies; Geomorphology","score_opus":0.014685582314239259,"score_gpt":0.1697105233877836,"score_spread":0.15502494107354436,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2315384596","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98998356,0.0016522459,0.0000050292533,0.0011117175,0.00011120669,0.000069478,0.000014666593,8.131262e-7,0.007051283],"genre_scores_gemma":[0.99931747,0.000020475614,0.00020104849,0.00038443482,0.000042748034,3.260361e-7,0.0000025569534,8.109405e-7,0.000030114286],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99834883,0.0003766001,0.00043404376,0.00016370504,0.00036388193,0.00031290768],"domain_scores_gemma":[0.99848026,0.0008754469,0.0003017105,0.00013224046,0.00004326606,0.00016709139],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013304296,0.0001074357,0.00027194511,0.0002471266,0.00010238429,0.00003480712,0.0007238358,0.000045327124,0.00096359005],"category_scores_gemma":[0.00043338598,0.00005161544,0.00009616076,0.00054179784,0.0010534222,0.00015890943,0.0000073743713,0.00024761396,0.0000052067053],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021031385,0.00002842914,0.987425,0.000010757915,0.000013791291,0.00006291367,0.0040651592,0.0036044258,0.0017630208,0.00087390107,0.00010698631,0.002024558],"study_design_scores_gemma":[0.00016805776,0.00029869002,0.9780526,0.00007806225,0.00001282674,0.0000136604895,0.0013024793,0.0012287354,0.0004532314,0.0127853025,0.0055052163,0.00010112778],"about_ca_topic_score_codex":0.10841688,"about_ca_topic_score_gemma":0.69472235,"teacher_disagreement_score":0.58630544,"about_ca_system_score_codex":0.0000058592254,"about_ca_system_score_gemma":0.0005309728,"threshold_uncertainty_score":0.9999497},"labels":[],"label_agreement":null},{"id":"W2315786691","doi":"10.1139/e2012-010","title":"Tree macrofossils of Younger Dryas age from Cohoes, New York State, USA","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Younger Dryas; Macrofossil; Abies balsamea; Black spruce; Allerød oscillation; Geology; Radiocarbon dating; Picea engelmannii; Fossil wood; Juniper; Dendroclimatology; Dendrochronology; Taiga; Balsam; Paleontology; Physical geography; Forestry; Geography; Glacial period; Botany; Holocene; Pinus contorta; Biology","score_opus":0.04292613520020167,"score_gpt":0.23803276058412937,"score_spread":0.1951066253839277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2315786691","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9819897,0.0093670525,0.000022232465,0.00024593386,0.0014985604,0.000063891166,0.00020792913,0.0000050374747,0.0065997075],"genre_scores_gemma":[0.99580365,0.00006829418,0.0028335063,0.000116750634,0.0003399673,6.530443e-8,0.00000482924,0.0000034466138,0.0008295154],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979739,0.00012456757,0.0004722604,0.00016337605,0.00050878926,0.0007570725],"domain_scores_gemma":[0.99751204,0.00035243167,0.0003683521,0.00015242294,0.0000651562,0.0015495901],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010319506,0.00015717569,0.00031170837,0.00041664665,0.00026195144,0.00019145914,0.0006609524,0.000059552578,0.005646856],"category_scores_gemma":[0.0002226854,0.00011793251,0.00010786374,0.00059807923,0.0006681961,0.00096338656,0.0000059901704,0.00018350728,0.00016356063],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022805776,0.0000048227594,0.9819371,0.0000044123676,0.00001968138,0.000053344,0.00084559503,0.0002609495,0.00018843162,0.000029639385,0.0015922488,0.015040957],"study_design_scores_gemma":[0.00019083284,0.00019091544,0.97725034,0.00007318199,0.000018936982,0.0000717706,0.00038785438,0.000043801076,0.0006098642,0.00026477975,0.02075131,0.00014643665],"about_ca_topic_score_codex":0.21822533,"about_ca_topic_score_gemma":0.71272415,"teacher_disagreement_score":0.49449885,"about_ca_system_score_codex":0.000003617407,"about_ca_system_score_gemma":0.0020715343,"threshold_uncertainty_score":0.99526215},"labels":[],"label_agreement":null},{"id":"W2315921687","doi":"10.1139/cjes-2013-0116","title":"Emplacement of metabreccia along the Whistle offset dike, Sudbury: implications for post-impact modification of the Sudbury impact structure","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"","keywords":"Dike; Geology; Impact structure; Impact crater; Geochemistry; Mineralogy; Astrobiology","score_opus":0.02537271652810586,"score_gpt":0.25253356029944185,"score_spread":0.227160843771336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2315921687","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99473023,0.0006848939,0.00011003977,0.0033810234,0.0001126573,0.00012796691,0.0006247583,0.0000011097313,0.00022729071],"genre_scores_gemma":[0.99950945,0.000009960449,0.00025473625,0.00012980448,0.000044260833,3.8569715e-7,0.000025615236,0.0000010889097,0.000024674762],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988626,0.000101765836,0.00039572036,0.00012668627,0.00023758583,0.00027559875],"domain_scores_gemma":[0.9984048,0.00031813013,0.0004796523,0.00019454713,0.0003399091,0.000262953],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00092778367,0.00010105105,0.0002350975,0.00012580972,0.0003691807,0.000051203628,0.00069847546,0.000044324428,0.0016913598],"category_scores_gemma":[0.00042632874,0.00004267875,0.00028073415,0.000627933,0.0005258281,0.00015136716,0.0000071711593,0.00011573436,0.0000016792205],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000119069455,0.0000050915132,0.9802598,0.0000053756935,0.00003921183,7.371768e-8,0.00010945664,0.013840815,0.0010127758,0.00023561419,0.00026142556,0.0042184526],"study_design_scores_gemma":[0.000087571076,0.0002870048,0.98898226,0.000011990669,0.000059181988,0.000013957485,0.00011706666,0.0024811255,0.0006319376,0.0064761513,0.00079228,0.000059489215],"about_ca_topic_score_codex":0.07458738,"about_ca_topic_score_gemma":0.35303625,"teacher_disagreement_score":0.27844885,"about_ca_system_score_codex":0.0000034651277,"about_ca_system_score_gemma":0.00059759803,"threshold_uncertainty_score":0.9992212},"labels":[],"label_agreement":null},{"id":"W2316362674","doi":"10.1139/e2012-025","title":"Environmental and seasonal controls on riverine dissolved uranium in the Hudson, James, and Ungava bays region, Canada","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Radioactive contamination and transfer","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Manitoba; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Hydro-Québec","keywords":"Snowmelt; Baseflow; Hydrology (agriculture); Sedimentary rock; Geology; Streamflow; Drainage basin; STREAMS; Environmental science; Sampling (signal processing); Physical geography; Oceanography; Geochemistry; Snow; Geomorphology; Geography","score_opus":0.009153259486388742,"score_gpt":0.18450245228002268,"score_spread":0.17534919279363395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2316362674","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945579,0.00052388647,0.000019469107,0.0029575224,0.00010940478,0.000077333054,0.00000973643,5.298287e-7,0.0017442276],"genre_scores_gemma":[0.99872124,0.00004789874,0.000033079825,0.0011057209,0.000037230002,8.465282e-7,3.694381e-7,0.0000022886238,0.00005130287],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99914515,0.000079845246,0.00013021304,0.00010139223,0.00027513568,0.00026823627],"domain_scores_gemma":[0.9994095,0.00009222094,0.000053064912,0.000049094207,0.0000034997565,0.0003926221],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048764504,0.00007914052,0.00009536442,0.000049792015,0.0002318877,0.000049366237,0.0001579245,0.000019249439,0.0003140166],"category_scores_gemma":[0.000027752183,0.000052469484,0.000016893524,0.0001009512,0.00057044555,0.0003361764,0.0000062494128,0.00012578609,0.0000028708937],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007191819,0.000009727102,0.99565613,7.237276e-7,0.0000038143016,0.00003885381,0.00070443074,0.00003446397,0.00018020411,0.00043744242,0.00048220143,0.0024448303],"study_design_scores_gemma":[0.00030677626,0.000087302615,0.9723393,0.00000822071,0.0000053772237,0.0001545264,0.000871564,0.00007330719,0.00005520362,0.000028990067,0.026002437,0.000067048284],"about_ca_topic_score_codex":0.1431176,"about_ca_topic_score_gemma":0.8779348,"teacher_disagreement_score":0.7348172,"about_ca_system_score_codex":0.000047530895,"about_ca_system_score_gemma":0.00015135985,"threshold_uncertainty_score":0.86258847},"labels":[],"label_agreement":null},{"id":"W2316426598","doi":"10.1139/e11-058","title":"<i>Procteria</i> (<i>Pachyprocteria</i>) <i>vermifera</i> n. sp., an unusual <i>Hicetes-</i>bearing species of tabulate coral from the lower Eifelian of the Gaspé Sandstones Group, Rimouski County (Quebec, Canada)","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Marine Biology and Ecology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Centre de Géomatique du Québec","funders":"","keywords":"Coral; Geology; Group (periodic table); Paleontology; Scleractinia; Oceanography","score_opus":0.03008129365699034,"score_gpt":0.20254043462937169,"score_spread":0.17245914097238135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2316426598","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99381715,0.00059796084,0.000002081094,0.00051598967,0.001754262,0.00014765869,0.00023504393,0.0000033079025,0.0029265382],"genre_scores_gemma":[0.9986924,0.00004931714,0.000108804445,0.0006718478,0.00025590204,4.6965266e-7,0.000011556965,0.0000044658027,0.00020524126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99762225,0.0003007895,0.00060789404,0.00027488085,0.0005301958,0.00066397793],"domain_scores_gemma":[0.9981543,0.00027396917,0.0005340946,0.00031617086,0.00023646237,0.00048504747],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013694296,0.00020683391,0.0004036627,0.00012974789,0.00073761656,0.00008597223,0.0016196092,0.00011640797,0.002224243],"category_scores_gemma":[0.00018341502,0.00011585233,0.0001206177,0.00051738654,0.0023955398,0.00047074462,0.000041158997,0.00039275378,0.0000047863555],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010054753,0.00001626,0.99769586,0.000007180904,0.00003420666,0.000035376077,0.0004321449,0.00008079485,0.00056399434,0.00008359588,0.00055342616,0.00039659062],"study_design_scores_gemma":[0.0002398096,0.00045789653,0.9927414,0.00004587282,0.000024985577,0.000055179727,0.0005763806,0.000089304296,0.0013409734,0.00026965924,0.0040108967,0.00014765996],"about_ca_topic_score_codex":0.90865546,"about_ca_topic_score_gemma":0.9988516,"teacher_disagreement_score":0.090196155,"about_ca_system_score_codex":0.000008425457,"about_ca_system_score_gemma":0.0039814794,"threshold_uncertainty_score":0.99868786},"labels":[],"label_agreement":null},{"id":"W2317049644","doi":"10.1139/e11-067","title":"Tectonic evolution of Pliocene–Pleistocene wedge-top basins of the southern Apennines: new constraints from magnetic fabric analysis","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies Worldwide","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Università degli Studi di Napoli Federico II","keywords":"Geology; Foreland basin; Tectonic subsidence; Structural basin; Tectonics; Paleontology; Inversion (geology); Neogene; Accretionary wedge; Geomorphology; Sedimentary basin; Subduction","score_opus":0.01387468437160965,"score_gpt":0.18708484304214226,"score_spread":0.1732101586705326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2317049644","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99119675,0.0054686074,0.00008638179,0.00048919534,0.00034982248,0.00006543899,0.00013537682,0.0000018337673,0.00220662],"genre_scores_gemma":[0.99916476,0.000013604707,0.0003720523,0.00006850775,0.0001302885,8.372862e-8,0.0000016561122,0.0000010057872,0.0002480564],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99860966,0.0000908394,0.00039445996,0.00013053659,0.00035499161,0.00041949045],"domain_scores_gemma":[0.99870163,0.00019633064,0.000366534,0.00012150704,0.000107858585,0.000506155],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004170889,0.00011272734,0.00032986823,0.00022895249,0.00025076285,0.000025548372,0.0005243934,0.00004236088,0.0063119084],"category_scores_gemma":[0.00020685577,0.000063647676,0.00023125374,0.0018335959,0.0013269895,0.00014860954,0.000012168857,0.00013361116,0.00004485024],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000056705467,0.000007851419,0.98642683,0.0000025006727,0.000049394148,0.0000014616281,0.00024662146,0.0019487808,0.000031646825,0.00005066364,0.00004577309,0.011182818],"study_design_scores_gemma":[0.00012869021,0.00017414681,0.9968586,0.0000240186,0.0001452056,0.0000062540516,0.000754549,0.00030303167,0.000080688595,0.000911053,0.0005339231,0.00007982791],"about_ca_topic_score_codex":0.11499451,"about_ca_topic_score_gemma":0.4174983,"teacher_disagreement_score":0.3025038,"about_ca_system_score_codex":0.0000040832165,"about_ca_system_score_gemma":0.000727559,"threshold_uncertainty_score":0.9945965},"labels":[],"label_agreement":null},{"id":"W2317101316","doi":"10.1139/cjes-2012-0143","title":"Holocene sediments from a coastal lake on northern Devon Island, Nunavut, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"","keywords":"Varve; Geology; Holocene; Permafrost; Sediment; Deposition (geology); Arctic; Sedimentation; Oceanography; Structural basin; Plateau (mathematics); Stratigraphy; Physical geography; Geomorphology; Paleontology","score_opus":0.015578637621145332,"score_gpt":0.20653488030513523,"score_spread":0.1909562426839899,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2317101316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909787,0.000451288,0.0000023804694,0.0015143249,0.00076493336,0.00007945444,0.00032421426,0.000002049625,0.0058826637],"genre_scores_gemma":[0.99854034,0.000011239241,0.00012043278,0.0008702953,0.000111220834,3.1997234e-7,0.000041198382,0.0000017329544,0.0003032382],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99843204,0.00012245575,0.00025588612,0.00018761079,0.00039870472,0.00060328847],"domain_scores_gemma":[0.9985634,0.00024224105,0.00013842781,0.00010462459,0.00014173066,0.0008095909],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000391989,0.000120947705,0.0001989735,0.00020189013,0.00047488505,0.00010344992,0.0005250256,0.0000742619,0.018023638],"category_scores_gemma":[0.0001239061,0.00008783189,0.000043581545,0.00027952096,0.0005148888,0.00025572052,0.0000051170814,0.0003105709,0.00042010672],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008282457,0.0000028295096,0.99680066,0.0000012987706,0.00001578327,0.0002669339,0.000086608954,0.00087918394,6.790006e-7,0.0000039467664,0.0015321475,0.0004016641],"study_design_scores_gemma":[0.00022098901,0.00027154936,0.9947851,0.000021807307,0.000005262471,0.00014812386,0.0002601078,0.00036481154,0.000030977084,0.0003328188,0.0034538908,0.00010461446],"about_ca_topic_score_codex":0.9435292,"about_ca_topic_score_gemma":0.99998444,"teacher_disagreement_score":0.056455273,"about_ca_system_score_codex":0.0000010030877,"about_ca_system_score_gemma":0.004225371,"threshold_uncertainty_score":0.98287404},"labels":[],"label_agreement":null},{"id":"W2317164286","doi":"10.1139/cjes-2012-0115","title":"Paleobotanical and environmental implications of a buried forest bed in northern Lower Michigan, USA","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Conservation Service; University of Wisconsin-Madison","keywords":"Geology; Hydrology (agriculture); Physical geography; Geotechnical engineering; Geography","score_opus":0.022191282526167637,"score_gpt":0.23416710917260353,"score_spread":0.21197582664643588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2317164286","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963518,0.0017528349,0.0000028395027,0.00067353126,0.00013672184,0.000051682655,0.00001900331,5.351828e-7,0.0010110617],"genre_scores_gemma":[0.999611,0.000045812387,0.00020688768,0.00007347565,0.00004169633,1.8798643e-7,0.0000027644824,8.027597e-7,0.000017375054],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909,0.00007831873,0.00023526486,0.00009007767,0.000117657575,0.00038866603],"domain_scores_gemma":[0.9991443,0.00020522108,0.0001008895,0.00006712809,0.00001672314,0.00046574764],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007333418,0.00006154361,0.00014392073,0.00020250426,0.00016590524,0.00001612853,0.00022563212,0.00005912557,0.0006476879],"category_scores_gemma":[0.000091666625,0.000047614685,0.000031727322,0.00019237975,0.0010945122,0.0002269994,0.000004882508,0.00016022923,0.000024025305],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007319395,0.000007877687,0.99936634,0.0000022350234,0.000004624609,0.000011152932,0.00025414175,0.00011215552,0.000020165224,0.000054161468,0.0000032743055,0.00015655474],"study_design_scores_gemma":[0.00013520541,0.00014973879,0.9985376,0.000009828538,0.00000469268,0.00025341587,0.0002713117,0.00005782858,0.000019543491,0.00027190946,0.00023825999,0.000050665076],"about_ca_topic_score_codex":0.002210261,"about_ca_topic_score_gemma":0.9362687,"teacher_disagreement_score":0.9340584,"about_ca_system_score_codex":3.284984e-7,"about_ca_system_score_gemma":0.0003699657,"threshold_uncertainty_score":0.7091728},"labels":[],"label_agreement":null},{"id":"W2317289056","doi":"10.1139/cjes-2014-0112","title":"Landform signature of the Laurentide and Cordilleran ice sheets across Alberta during the last glaciation","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Landform; Digital elevation model; Glacial period; Ice sheet; Glacier; Remote sensing; Glacial landform; Lidar; Physical geography; Geomorphology; Moraine; Geography","score_opus":0.009084088792587514,"score_gpt":0.21498597120697455,"score_spread":0.20590188241438703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2317289056","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99306595,0.0006158046,0.0000014249548,0.0018077946,0.00035148702,0.00004995373,0.000008301801,7.5695687e-7,0.0040985215],"genre_scores_gemma":[0.99955726,0.000020626581,0.000022512091,0.00015482133,0.00005767862,8.578852e-8,8.508375e-7,7.136909e-7,0.00018546295],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991021,0.00014347544,0.00016868058,0.00009028346,0.0001913658,0.00030407638],"domain_scores_gemma":[0.99917245,0.0003392589,0.00015555501,0.000087981585,0.00007273339,0.00017203846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011452049,0.00006078438,0.00011660305,0.000068477115,0.0008781904,0.000065349785,0.00043143434,0.000058770504,0.00042052916],"category_scores_gemma":[0.00029029563,0.000029886329,0.000041738323,0.0002781865,0.0010100274,0.00017870693,0.000008725013,0.00024977056,0.000007733064],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005893484,7.8986835e-7,0.998379,0.0000060650978,0.000006133107,0.0000024410297,0.0006327928,0.0005529839,0.000008488104,0.00005119428,0.000026695207,0.00032753006],"study_design_scores_gemma":[0.00013591794,0.000072263676,0.9967835,0.000022268023,0.000004569294,0.00016467768,0.00035267705,0.0004416125,0.000087974186,0.00018440493,0.0017114615,0.00003869145],"about_ca_topic_score_codex":0.006152602,"about_ca_topic_score_gemma":0.87240845,"teacher_disagreement_score":0.8662559,"about_ca_system_score_codex":2.7427762e-7,"about_ca_system_score_gemma":0.00025305408,"threshold_uncertainty_score":0.93009347},"labels":[],"label_agreement":null},{"id":"W2317304264","doi":"10.1139/e2012-078","title":"An igneous-textured clast in the Peace River meteorite: insights into accretion and metamorphism of asteroids in the early solar system","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Science and Technology Facilities Council","keywords":"Geology; Parent body; Metamorphism; Geochemistry; Meteorite; Breccia; Shock metamorphism; Chondrite; Igneous rock; Metamorphic rock; Petrography; Astrobiology","score_opus":0.008978985538858975,"score_gpt":0.19567092869143465,"score_spread":0.18669194315257567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2317304264","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99851,0.00037615976,0.00023130522,0.00024247747,0.00009875972,0.00011878122,0.0000042607217,5.6443247e-7,0.0004177004],"genre_scores_gemma":[0.99942327,0.000001628191,0.0004385412,0.000051843563,0.000072839764,0.0000012146976,0.0000012298377,0.0000014532606,0.000007994654],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989164,0.00026544085,0.00024364109,0.00011491017,0.000255629,0.0002039683],"domain_scores_gemma":[0.9994334,0.00009005218,0.0001633398,0.000110185116,0.000055236313,0.000147785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010405075,0.000080925325,0.0001402185,0.00021130363,0.00022877591,0.0002474757,0.00059145596,0.000021842856,0.000045287226],"category_scores_gemma":[0.000007825425,0.00004300417,0.000031229218,0.00041261234,0.0004775274,0.00078103406,0.0000057800985,0.00019081506,0.0000043425944],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000052958135,0.000018225608,0.9476283,0.00000865476,0.000011323103,0.000031377538,0.039751567,0.0007642821,0.001922318,0.0033715551,0.000084360516,0.0064027184],"study_design_scores_gemma":[0.00013715427,0.00029964754,0.9830351,0.000049527884,0.000008325624,0.000024356996,0.013514292,0.0019181907,0.000054977205,0.00038408686,0.00050680886,0.0000675175],"about_ca_topic_score_codex":0.044970363,"about_ca_topic_score_gemma":0.0404575,"teacher_disagreement_score":0.03540679,"about_ca_system_score_codex":0.0000034851398,"about_ca_system_score_gemma":0.0003190697,"threshold_uncertainty_score":0.9770517},"labels":[],"label_agreement":null},{"id":"W2317371219","doi":"10.1139/cjes-2013-0200","title":"Petroleum generation and expulsion characteristics of Lower and Middle Jurassic source rocks on the southern margin of Junggar Basin, northwest China: implications for unconventional gas potential","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Lawrence Livermore National Laboratory; National Natural Science Foundation of China","keywords":"Source rock; Geology; Kerogen; Petroleum; Structural basin; Geochemistry; Cretaceous; Paleogene; Natural gas; Paleontology","score_opus":0.014899145819457777,"score_gpt":0.19565838185135528,"score_spread":0.1807592360318975,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2317371219","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98585993,0.00009531911,0.012695052,0.0010865299,0.00011883932,0.00004400085,0.000038595823,0.0000017691908,0.000059947626],"genre_scores_gemma":[0.9996426,0.000027377984,0.00014284636,0.00002770488,0.00009915444,0.0000013538574,0.0000058963324,0.000004467782,0.000048592454],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994659,0.000026846805,0.00023252954,0.00006647226,0.000109614695,0.000098679026],"domain_scores_gemma":[0.999555,0.00003362508,0.00013491734,0.00006214413,0.000089690926,0.0001246256],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003454033,0.000058719088,0.00012487767,0.00016528569,0.00017831956,0.000044867036,0.00009316236,0.000026133093,0.000023204151],"category_scores_gemma":[0.00005536036,0.00004048857,0.000053460688,0.00011384042,0.00014242328,0.000082728075,0.0000039610345,0.000055275774,4.4625358e-7],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000083496765,0.00012859385,0.3384106,0.00029795797,0.00040312484,0.000005576332,0.00517692,0.56248575,0.06182045,0.004984984,0.00093185937,0.0252707],"study_design_scores_gemma":[0.00066373957,0.0006584748,0.3386231,0.00019603812,0.00013353501,0.00004792516,0.0010015353,0.65215266,0.0021424543,0.0008552475,0.0032624225,0.00026285692],"about_ca_topic_score_codex":0.00027966025,"about_ca_topic_score_gemma":0.010608467,"teacher_disagreement_score":0.0896669,"about_ca_system_score_codex":0.0000036900854,"about_ca_system_score_gemma":0.00009239948,"threshold_uncertainty_score":0.59197736},"labels":[],"label_agreement":null},{"id":"W2317736492","doi":"10.1139/cjes-2012-0092","title":"Stratigraphy and geochemistry of the igneous rocks in the Elu Link between Hope Bay and Elu greenstone belts, northeast Slave craton: tectonic setting and implications for gold mineralization","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Vancouver Native Health Society; University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Felsic; Andesites; Greenstone belt; Basalt; Fractional crystallization (geology); Mafic; Craton; Volcanic rock; Igneous rock; Archean; Petrology; Andesite; Tectonics; Volcano; Paleontology","score_opus":0.014354216369545753,"score_gpt":0.20761149987665625,"score_spread":0.1932572835071105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2317736492","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912386,0.003311419,0.000021406162,0.004824161,0.000020970636,0.00008131721,0.00007326101,8.6113675e-7,0.00042803556],"genre_scores_gemma":[0.9993611,0.000052616346,0.000297281,0.00017359888,0.000099705816,5.0988825e-7,0.0000061105256,6.658065e-7,0.000008415211],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99925834,0.000045508823,0.00023032869,0.00011046124,0.00011210134,0.00024324696],"domain_scores_gemma":[0.9992742,0.00020721617,0.00015938355,0.000067696885,0.00006360234,0.00022793251],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00062135677,0.000076761244,0.00013788343,0.00008117418,0.0002819423,0.000063057465,0.00019360721,0.000044160544,0.000046708345],"category_scores_gemma":[0.00012594565,0.0000402877,0.000042426116,0.00040536223,0.00048270152,0.00014427383,0.0000065583426,0.000112280584,1.3756794e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011759266,0.0000016773364,0.9898257,0.000007792765,0.000006329862,3.8348756e-7,0.00018392004,0.00007819391,0.00014334335,0.000033579097,0.000010745133,0.009707137],"study_design_scores_gemma":[0.00007912911,0.00007262825,0.99672854,0.00002207569,0.000029760253,0.00005717937,0.00029173374,0.00032618013,0.00010589655,0.002001453,0.00022733775,0.000058063775],"about_ca_topic_score_codex":0.006622818,"about_ca_topic_score_gemma":0.37214136,"teacher_disagreement_score":0.36551857,"about_ca_system_score_codex":6.0871133e-7,"about_ca_system_score_gemma":0.00011432203,"threshold_uncertainty_score":0.9999922},"labels":[],"label_agreement":null},{"id":"W2319075953","doi":"10.1139/cjes-2012-0063","title":"First record of<i>Porolepis</i>(Sarcopterygii; Porolepiformes) from eastern Gondwana","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Gondwana; Devonian; Geology; Paleontology; Fauna; Genus; Southern Hemisphere; Northern Hemisphere; Physical geography; Geography; Ecology; Climatology; Tectonics; Biology","score_opus":0.01664685461490201,"score_gpt":0.1915483254822511,"score_spread":0.17490147086734908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2319075953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98036444,0.0031805479,0.000054017164,0.001479689,0.0010853802,0.00006734481,0.0000662877,0.0000036238796,0.013698682],"genre_scores_gemma":[0.9975196,0.00006600041,0.0017750736,0.00029732139,0.00017273732,2.6256285e-7,0.000008011772,0.0000013411777,0.00015962149],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99863964,0.000084529,0.00045644538,0.00017801306,0.00018255075,0.000458816],"domain_scores_gemma":[0.9986412,0.00019137183,0.00034440254,0.00011891486,0.00012775537,0.00057634665],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046705882,0.00012110737,0.000275693,0.00028860357,0.00032405055,0.000047241367,0.000591864,0.0001033683,0.009398553],"category_scores_gemma":[0.0001093144,0.00009052782,0.00010291434,0.0002802784,0.0009618222,0.0006488391,0.0000049016976,0.00017670517,0.0004220262],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008618772,0.0000032253881,0.98752105,0.0000027800145,0.000017590686,0.000025791316,0.00012839455,0.0003390832,0.000011675449,0.000028826686,0.00051265967,0.011400275],"study_design_scores_gemma":[0.00015324051,0.00029926526,0.9819867,0.00003563466,0.000010532375,0.000092419985,0.00026136648,0.0016500398,0.000019245417,0.0024925906,0.01289055,0.00010838764],"about_ca_topic_score_codex":0.1547388,"about_ca_topic_score_gemma":0.7314662,"teacher_disagreement_score":0.5767274,"about_ca_system_score_codex":0.0000016559941,"about_ca_system_score_gemma":0.00096715527,"threshold_uncertainty_score":0.991507},"labels":[],"label_agreement":null},{"id":"W2319287491","doi":"10.1139/e2012-022","title":"<sup>40</sup>Ar–<sup>39</sup>Ar ages for detrital white mica in Meguma terrane, Nova Scotia, Canada: implications for provenance of the Goldenville and Halifax groups","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Technical University of Nova Scotia; Acadia University; Nova Scotia Department of Energy; Dalhousie University","funders":"Northwestern University","keywords":"Geology; Terrane; Precambrian; Provenance; Mica; Geochemistry; Nova scotia; Geochronology; Rift; Paleozoic; Mineralogy; Paleontology; Tectonics","score_opus":0.0201872050385719,"score_gpt":0.20223227759316567,"score_spread":0.18204507255459376,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2319287491","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9881236,0.002459677,0.00004245554,0.007873878,0.00011564841,0.0002816702,0.00052171724,0.0000018696975,0.00057948957],"genre_scores_gemma":[0.99762523,0.000017501194,0.0016998613,0.00040057118,0.00013299147,0.000002109738,0.000013948779,0.0000024779324,0.00010530684],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983262,0.000053913314,0.0004752922,0.00023081964,0.00024634774,0.00066743226],"domain_scores_gemma":[0.9985375,0.00031761877,0.00025850997,0.00014254964,0.0001533322,0.0005904896],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000681567,0.00015448027,0.0003251954,0.0001838961,0.00034842937,0.00007057378,0.0005888715,0.00006975932,0.0004410108],"category_scores_gemma":[0.0004636505,0.00009558617,0.00014087615,0.0007092462,0.00062168477,0.0003590532,0.000014361905,0.00015535158,0.0000019990748],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001161166,0.000011361068,0.99280256,0.000020698424,0.00001656947,0.000001473853,0.00024092675,0.004015874,0.000076246615,0.00018478303,0.0007263292,0.0018915603],"study_design_scores_gemma":[0.00028375312,0.00017143096,0.9900866,0.00005196357,0.000035917426,0.00005641535,0.00057922164,0.0025787426,0.00018121318,0.002191741,0.0036232832,0.0001596849],"about_ca_topic_score_codex":0.48476315,"about_ca_topic_score_gemma":0.98387706,"teacher_disagreement_score":0.49911392,"about_ca_system_score_codex":0.000008384028,"about_ca_system_score_gemma":0.00087084464,"threshold_uncertainty_score":0.5186679},"labels":[],"label_agreement":null},{"id":"W2319465987","doi":"10.1139/cjes-2013-0151","title":"The electrical resistivity of Canada’s lithosphere and correlation with other parameters: contributions from Lithoprobe and other programmes","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Polytechnique Montréal; University of Manitoba; Geological Survey of Canada","funders":"","keywords":"Lithosphere; Geology; Asthenosphere; Tectonics; Shield; North American Plate; Magnetotellurics; Plate tectonics; Physical geography; Seismology; Paleontology; Geography; Electrical resistivity and conductivity","score_opus":0.010082297210256913,"score_gpt":0.20854287342502367,"score_spread":0.19846057621476676,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2319465987","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938688,0.0022581096,0.0011983279,0.0016101224,0.00008806798,0.00009148711,0.000048146558,0.0000019749161,0.0008349575],"genre_scores_gemma":[0.99530095,0.0000092501205,0.0044110734,0.00016557073,0.000044131124,2.396145e-7,4.4903126e-7,0.0000011796103,0.000067173634],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99900275,0.00019130614,0.00017800096,0.000121332145,0.00021943869,0.0002871645],"domain_scores_gemma":[0.9983248,0.00097099895,0.00016117503,0.000058618127,0.00009544229,0.00038898125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008153954,0.00007523632,0.0001589585,0.00003619527,0.00043924685,0.00011399412,0.00013299387,0.000032592634,0.000043756194],"category_scores_gemma":[0.0005982106,0.000039259958,0.000020676656,0.00030600993,0.0005633773,0.000102605605,0.0000022124564,0.00014156137,4.6529306e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000036792037,0.0000041716717,0.828076,0.0000024454075,0.000018436354,0.0000027973233,0.000080454876,0.000278191,0.000005062688,0.0012884088,0.00007153198,0.1701357],"study_design_scores_gemma":[0.00014691892,0.0006143304,0.968626,0.000025694539,0.000017102562,0.00001691402,0.00006776665,0.0048990822,0.00006476229,0.00611659,0.019329878,0.00007490892],"about_ca_topic_score_codex":0.72865933,"about_ca_topic_score_gemma":0.9825373,"teacher_disagreement_score":0.25387797,"about_ca_system_score_codex":0.0000019719428,"about_ca_system_score_gemma":0.0010654359,"threshold_uncertainty_score":0.3378376},"labels":[],"label_agreement":null},{"id":"W2319483927","doi":"10.1139/cjes-2012-0158","title":"Field relationships, petrology, age, and tectonic setting of the Late Cambrian–Ordovician West Barneys River Plutonic Suite, southern Antigonish Highlands, Nova Scotia, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick; University of Toronto; St. Francis Xavier University; Acadia University","funders":"Natural Sciences and Engineering Research Council of Canada; Acadia University","keywords":"Geology; Geochemistry; Felsic; Mafic; Zircon; Alkali feldspar; Hornblende; Petrology; Augite; Quartz monzonite; Plagioclase; Pluton; Biotite; Quartz; Tectonics","score_opus":0.011515431416226917,"score_gpt":0.17518395280885757,"score_spread":0.16366852139263066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2319483927","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99118525,0.000781784,0.0000022426539,0.005773026,0.00024477058,0.00006657234,0.000036912883,0.0000022020577,0.0019072258],"genre_scores_gemma":[0.9988055,0.000010066682,0.00019571064,0.0006389153,0.00005414725,9.28659e-8,0.0000029835176,0.0000013304217,0.00029124974],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986557,0.00015177325,0.00035176467,0.00015574064,0.00026633244,0.00041868887],"domain_scores_gemma":[0.9985871,0.00048722205,0.00026440993,0.00011320036,0.00011635032,0.0004317389],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00066587667,0.00011443914,0.00023193014,0.0001316569,0.0004633085,0.000098934004,0.00046556912,0.00006970123,0.0043890094],"category_scores_gemma":[0.0006242226,0.00006734701,0.00007989225,0.00059542916,0.0006358388,0.00018369932,0.000015135932,0.0003539549,0.0000257248],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000019931872,0.0000014757477,0.99820596,0.0000039910806,0.000014950714,0.000016247912,0.0001424522,0.0007809782,0.000028792543,0.000018527155,0.00014621219,0.0006383906],"study_design_scores_gemma":[0.000099527475,0.00009501012,0.9970212,0.000027306918,0.000024403069,0.000042571024,0.00046503526,0.0008367938,0.000027972179,0.00083412044,0.00043161918,0.00009446495],"about_ca_topic_score_codex":0.9711054,"about_ca_topic_score_gemma":0.9995486,"teacher_disagreement_score":0.028443243,"about_ca_system_score_codex":0.0000030139736,"about_ca_system_score_gemma":0.0011843289,"threshold_uncertainty_score":0.9965211},"labels":[],"label_agreement":null},{"id":"W2319601662","doi":"10.1139/e2012-026","title":"Obducted nappe sequence in the San Juan Islands – northwest Cascades thrust system, Washington and British Columbia","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nappe; Geology; Metamorphism; Terrane; Geochemistry; Zircon; Obduction; Paleontology; Geomorphology; Subduction; Tectonics; Oceanic crust","score_opus":0.019177624067605765,"score_gpt":0.19495929578093624,"score_spread":0.17578167171333048,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2319601662","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911017,0.0033641767,8.998773e-7,0.00037171587,0.00019268332,0.000053114505,0.000050797153,0.000003469722,0.0048614587],"genre_scores_gemma":[0.99928796,0.000059574282,0.00015245908,0.00028594062,0.00015514312,2.4195967e-7,0.00000871087,9.010821e-7,0.00004907925],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99860513,0.00012758042,0.00029003585,0.00014778892,0.00030217413,0.0005273156],"domain_scores_gemma":[0.9990461,0.00014371147,0.0001368808,0.000073309166,0.00006094975,0.0005390713],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013432523,0.00008150808,0.00020155704,0.000098244906,0.00052200677,0.0006254727,0.00045595103,0.000053998727,0.0018683168],"category_scores_gemma":[0.00013074231,0.00006169064,0.000057831887,0.00074205047,0.0006291504,0.0004961332,0.000005873245,0.0002328865,0.000011986579],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[9.556906e-7,0.0000033972124,0.9967846,0.000007655845,0.0000054820857,0.00007590946,0.00033137447,0.00006641307,0.000007598994,0.000021355536,0.000089457346,0.0026057796],"study_design_scores_gemma":[0.0000794869,0.0000992398,0.9939318,0.00006593147,0.000017994531,0.0008644944,0.0021234858,0.00030632282,0.0000052460173,0.0003181414,0.0020860804,0.00010177813],"about_ca_topic_score_codex":0.67140335,"about_ca_topic_score_gemma":0.9925959,"teacher_disagreement_score":0.32119256,"about_ca_system_score_codex":0.0000021644375,"about_ca_system_score_gemma":0.00023877075,"threshold_uncertainty_score":0.9990441},"labels":[],"label_agreement":null},{"id":"W2320291295","doi":"10.1139/cjes-2012-0161","title":"Geon 12 crustal extension in the central Grenville Province, implications for the orogenic architecture, and potential influence on the emplacement of anorthosites","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec); Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Mafic; Geochemistry; Felsic; Orogeny; Metamorphism; Granulite; Anorthosite; Magmatism; Petrology; Geomorphology; Facies; Tectonics; Paleontology; Plagioclase","score_opus":0.014101398159273712,"score_gpt":0.19347921626652725,"score_spread":0.17937781810725353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2320291295","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98750466,0.000649237,0.000041230694,0.01134257,0.00003555168,0.00022807883,0.000024437248,6.166742e-7,0.00017359208],"genre_scores_gemma":[0.99903846,0.00003381988,0.000157233,0.0007219402,0.000031890282,0.0000018840452,0.000001644809,5.0926604e-7,0.000012621382],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99915594,0.00006650141,0.000212105,0.00011418589,0.00017348577,0.00027775916],"domain_scores_gemma":[0.9991248,0.0004349998,0.00012785112,0.00009755422,0.00007056232,0.00014422297],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005519222,0.00006982275,0.000097721204,0.000078806865,0.00044808816,0.00010107935,0.0004208187,0.00002129935,0.00042740273],"category_scores_gemma":[0.00018167525,0.000025962601,0.00006854221,0.00025798232,0.00060441304,0.000085260675,0.000006667574,0.00011936871,0.0000024743265],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010846369,0.000008203136,0.9709077,0.0000031758236,0.000011534005,0.0000021264223,0.00025572232,0.019866683,0.00031451488,0.00042468111,0.00010154759,0.008093307],"study_design_scores_gemma":[0.00006241542,0.00022913392,0.9911664,0.000010241974,0.000014636613,0.00003065913,0.00043650882,0.0013379154,0.00006367043,0.0060944,0.00051276514,0.00004122134],"about_ca_topic_score_codex":0.023530122,"about_ca_topic_score_gemma":0.32649657,"teacher_disagreement_score":0.30296645,"about_ca_system_score_codex":8.976984e-7,"about_ca_system_score_gemma":0.0001993742,"threshold_uncertainty_score":0.98297226},"labels":[],"label_agreement":null},{"id":"W2320404971","doi":"10.1139/e2012-066","title":"Metamorphism and deformation of the Grand Forks complex: implications for the exhumation history of the Shuswap core complex, southern British Columbia","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Metamorphism; Metamorphic facies; Geochemistry; Greenschist; Metamorphic rock; Sillimanite; Hornblende; Granulite; Biotite; Geomorphology; Quartz; Facies; Paleontology","score_opus":0.06036900328923893,"score_gpt":0.20450899102549594,"score_spread":0.14413998773625702,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2320404971","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995038,0.0021113276,0.00006481744,0.001491249,0.0001865178,0.0001440629,0.00013863613,9.669067e-7,0.00082444446],"genre_scores_gemma":[0.99933,0.000014405536,0.00020839235,0.00024207302,0.000037411013,6.406176e-7,0.0000047986136,6.549041e-7,0.0001616644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99929,0.000036232046,0.00027673127,0.000058192807,0.00016025518,0.00017858317],"domain_scores_gemma":[0.9991192,0.0001554865,0.00035827822,0.000090985865,0.00013962806,0.00013640951],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00069183,0.000044533503,0.00013197755,0.000029435449,0.00049588754,0.00005415549,0.00039482437,0.00002713288,0.001388552],"category_scores_gemma":[0.000118710625,0.000024864235,0.00011799367,0.00022617004,0.0010390858,0.00016763435,0.000008140465,0.000075415286,9.3189794e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000013973565,0.0000032869439,0.99462104,0.000006178211,0.000012379202,2.8442603e-8,0.00039575773,0.00026135807,0.00008648752,0.00007147273,0.0016213509,0.0029192579],"study_design_scores_gemma":[0.00008210336,0.000032767708,0.9874069,0.000013491152,0.000049244398,0.000029800467,0.00033622657,0.0019468865,0.000007359734,0.0042541465,0.0058043175,0.0000367197],"about_ca_topic_score_codex":0.075077824,"about_ca_topic_score_gemma":0.76759976,"teacher_disagreement_score":0.692522,"about_ca_system_score_codex":0.0000032091802,"about_ca_system_score_gemma":0.00020460182,"threshold_uncertainty_score":0.9995243},"labels":[],"label_agreement":null},{"id":"W2321050042","doi":"10.1139/e2012-074","title":"Gondwanatheria and ?Multituberculata (Mammalia) from the Late Cretaceous of Madagascar","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Stony Brook University","keywords":"Cheek teeth; Incertae sedis; Paleontology; Theria; Gondwana; Dentition; Cretaceous; Biology; Clade; Taxon; Eutheria; Biochronology; Zoology; Geology; Biostratigraphy; Phylogenetic tree; Phanerozoic; Structural basin; Cenozoic","score_opus":0.02380484155397836,"score_gpt":0.20958181180459154,"score_spread":0.18577697025061318,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2321050042","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9787789,0.013819062,0.0000062288236,0.002431746,0.0003760265,0.000059603208,0.00003753433,0.0000017605435,0.004489165],"genre_scores_gemma":[0.9987222,0.00017148678,0.000520071,0.0003387337,0.00006267508,1.0204839e-7,0.0000011214886,8.478004e-7,0.00018275122],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992135,0.000082457766,0.00022458407,0.000090164416,0.00016189313,0.0002273728],"domain_scores_gemma":[0.9991712,0.00022455389,0.00015696889,0.000083468054,0.000098567674,0.00026526727],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00043398843,0.00007477519,0.00015979774,0.00007868368,0.00035721282,0.000081886894,0.00031923453,0.00003663968,0.0018560998],"category_scores_gemma":[0.00012628404,0.00004331251,0.000044250624,0.00018015025,0.001073567,0.00026305212,0.0000047026774,0.00010772832,0.000035024797],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000017696755,7.5289836e-7,0.99542326,0.000001223605,0.000020389003,0.0000069553453,0.00059281505,0.0002233628,0.000019622828,0.000038580212,0.00053739524,0.0031338886],"study_design_scores_gemma":[0.00009673221,0.00008481744,0.9897906,0.000018716011,0.000013186337,0.000040626255,0.0011673763,0.00082585774,0.00001387457,0.0007292852,0.0071624075,0.00005651692],"about_ca_topic_score_codex":0.1179452,"about_ca_topic_score_gemma":0.8646466,"teacher_disagreement_score":0.7467014,"about_ca_system_score_codex":5.9493203e-7,"about_ca_system_score_gemma":0.00031450787,"threshold_uncertainty_score":0.99905634},"labels":[],"label_agreement":null},{"id":"W2321104306","doi":"10.1139/cjes-2013-0068","title":"Reassessment of<i>Ischnacanthus</i>?<i>scheii</i>Spjeldnaes (Acanthodii, Ischnacanthiformes) from the latest Silurian or earliest Devonian of Ellesmere Island, arctic Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Devonian; Arctic; Geology; Paleontology; Archipelago; The arctic; Oceanography","score_opus":0.02087504873322401,"score_gpt":0.2010151665923952,"score_spread":0.1801401178591712,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2321104306","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9853098,0.0011506604,0.000020668718,0.009357023,0.00064150366,0.00019125383,0.00030735295,0.0000025448317,0.003019226],"genre_scores_gemma":[0.99811506,0.00031654348,0.0006729237,0.0006516423,0.00014360106,9.610258e-7,0.0000113484175,0.0000027053652,0.000085215754],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99798185,0.00010274279,0.000645229,0.00019917214,0.00055405236,0.0005169533],"domain_scores_gemma":[0.9979985,0.0005122849,0.0005542875,0.00014966489,0.00029379796,0.00049149815],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00067489315,0.00017832463,0.0003810079,0.00009725575,0.0005995509,0.00011152789,0.0006881551,0.00006626678,0.005853567],"category_scores_gemma":[0.0003657052,0.000092874536,0.00008804827,0.0005184592,0.001005015,0.00043687125,0.0000166225,0.0002531955,0.000015552067],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019573165,0.000006890352,0.9874173,0.000010170109,0.00004533778,0.000025926114,0.0004009676,0.0014527682,0.000014720372,0.000093680515,0.0034734244,0.0070392466],"study_design_scores_gemma":[0.0002113946,0.0005006761,0.977697,0.000113711525,0.000027638707,0.000029495242,0.005073169,0.00034996436,0.00014658013,0.0005925119,0.015102244,0.00015558326],"about_ca_topic_score_codex":0.97150606,"about_ca_topic_score_gemma":0.99909943,"teacher_disagreement_score":0.027593374,"about_ca_system_score_codex":0.0000075454686,"about_ca_system_score_gemma":0.0038539942,"threshold_uncertainty_score":0.9950552},"labels":[],"label_agreement":null},{"id":"W2321213299","doi":"10.1139/cjes-2013-0020","title":"Characterizing heterogeneity in a glaciofluvial deposit using architectural elements, Limehouse, Ontario, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"McMaster University; Ministry of Natural Resources","keywords":"Facies; Outcrop; Geology; Fluvial; Sedimentary rock; Alluvial fan; Alluvium; Sedimentary depositional environment; Sedimentary structures; Geomorphology; Geochemistry; Delta; Structural basin","score_opus":0.026305567364791376,"score_gpt":0.203882292776015,"score_spread":0.17757672541122363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2321213299","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99812126,0.0002750527,0.000012415783,0.0002749903,0.0003303934,0.000075112854,0.000009911793,0.0000016816521,0.0008991578],"genre_scores_gemma":[0.99779165,0.0000032814446,0.0016811701,0.00045614646,0.000043411703,1.9805377e-7,0.0000026922548,9.546877e-7,0.00002051372],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988143,0.000045961446,0.0003611937,0.000108789856,0.00023226939,0.00043750516],"domain_scores_gemma":[0.99923074,0.00004378763,0.00016055256,0.00005036818,0.00006868798,0.00044587717],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003267551,0.000093111674,0.00014696871,0.00020867691,0.00034937583,0.0002230265,0.0003203682,0.000028572515,0.0030323316],"category_scores_gemma":[0.000049907532,0.00006714337,0.000033412103,0.00032011143,0.00013373642,0.0006126942,0.0000048065767,0.00017568126,0.000010095878],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002084041,0.0000012879908,0.99428576,0.0000033045806,0.0000034613265,0.000027235088,0.00020863177,0.002545733,0.00003436329,0.0000033095919,0.000011004756,0.0028738403],"study_design_scores_gemma":[0.00009057713,0.000105548206,0.995555,0.00002828053,0.0000030488068,0.00021153376,0.00015216322,0.0020028807,0.00016213176,0.00012246036,0.0014705682,0.00009580617],"about_ca_topic_score_codex":0.997664,"about_ca_topic_score_gemma":0.99997044,"teacher_disagreement_score":0.0033763724,"about_ca_system_score_codex":0.000012321649,"about_ca_system_score_gemma":0.003388694,"threshold_uncertainty_score":0.997879},"labels":[],"label_agreement":null},{"id":"W2321410251","doi":"10.1139/cjes-2012-0099","title":"Paleoenvironmental analysis of Ediacaran strata in the Catalina Dome, Bonavista Peninsula, Newfoundland","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Newfoundland and Labrador; Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Peninsula; Paleontology; Outcrop; Dome (geology); Ecological succession; Volcano; Tectonic uplift; Pyroclastic rock; Bay; Structural basin; Geochemistry; Archaeology; Oceanography","score_opus":0.02110915288772412,"score_gpt":0.23637289707306958,"score_spread":0.21526374418534547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2321410251","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944386,0.0012226707,0.0000022748077,0.00080116163,0.00013045788,0.000089356145,0.00003757013,6.1429694e-7,0.003277333],"genre_scores_gemma":[0.9996511,0.000045386852,0.000100975085,0.00011172874,0.000030543437,2.9665907e-7,0.000017499902,6.6745633e-7,0.000041852956],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99856853,0.00021067604,0.00034560644,0.00014003449,0.00032747744,0.00040767677],"domain_scores_gemma":[0.9990563,0.0003196203,0.0001671987,0.0001373695,0.000040547835,0.0002789551],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013941996,0.00008456457,0.0002508383,0.00070250867,0.00024785363,0.000093754286,0.0007373112,0.00006019761,0.003851789],"category_scores_gemma":[0.00007960462,0.000052570675,0.00009685298,0.0011681985,0.0013114366,0.00034031106,0.000004526543,0.00024589887,0.000054252418],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000040070213,0.0000049487935,0.9979247,0.000002279158,0.000038689286,0.0000811247,0.00043425147,0.0013049602,0.00000322694,0.00004459411,0.00003393523,0.00012330373],"study_design_scores_gemma":[0.00012760598,0.0001762072,0.9968277,0.000006358286,0.000046758403,0.00012972218,0.0011457488,0.0010439721,0.0000034586133,0.000244745,0.00018837198,0.000059340386],"about_ca_topic_score_codex":0.061461985,"about_ca_topic_score_gemma":0.8748366,"teacher_disagreement_score":0.81337464,"about_ca_system_score_codex":5.722653e-7,"about_ca_system_score_gemma":0.00048684955,"threshold_uncertainty_score":0.9970588},"labels":[],"label_agreement":null},{"id":"W2321777915","doi":"10.1139/cjes-2016-0004","title":"Late-glacial and Holocene evolution as a driver of diversity and complexity of the northeastern North American alpine landscapes: a synthesis","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Glacial period; Geology; Physical geography; Deglaciation; Holocene; Pleistocene; Earth science; Climate change; Geomorphology; Paleontology; Geography; Oceanography","score_opus":0.03251782844104242,"score_gpt":0.21884076586511714,"score_spread":0.1863229374240747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2321777915","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99832493,0.00025097025,0.0000055510395,0.0010063343,0.00007171806,0.000041552983,0.000045249337,7.955337e-7,0.0002529126],"genre_scores_gemma":[0.99981815,0.000055025343,0.000064875334,0.000029511877,0.000015385447,4.64545e-8,2.1388323e-7,4.956271e-7,0.000016273663],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992033,0.00013965668,0.00015716608,0.00010320016,0.0001824069,0.00021427356],"domain_scores_gemma":[0.9992058,0.00020073155,0.00020355485,0.00006379934,0.000093380004,0.00023271835],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00046588978,0.000058825153,0.00018632402,0.00015885598,0.00052633724,0.000008547314,0.0002608066,0.000026189708,0.00017668668],"category_scores_gemma":[0.00019166917,0.000031128173,0.00003492456,0.00027593478,0.0039253198,0.00014650436,0.00003178357,0.00007718447,0.0000029118655],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026002443,0.0000023660286,0.99846673,0.0000053628037,0.000012195124,0.000008455095,0.00029967818,0.000029483997,0.0000037308473,0.000037457627,0.0000018017676,0.0011067162],"study_design_scores_gemma":[0.0001350203,0.00023555815,0.99877256,0.000029669665,0.000013847269,0.00010001797,0.00015372333,0.00014468096,0.00003448999,0.00032344987,0.000016610828,0.00004034142],"about_ca_topic_score_codex":0.020779563,"about_ca_topic_score_gemma":0.75505507,"teacher_disagreement_score":0.7342755,"about_ca_system_score_codex":4.4903973e-7,"about_ca_system_score_gemma":0.00034942638,"threshold_uncertainty_score":0.99878544},"labels":[],"label_agreement":null},{"id":"W2322021109","doi":"10.1139/e2012-001","title":"Lake- and channel-bottom temperatures in the Mackenzie Delta, Northwest Territories<sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of <i>Fundamental and applied research on permafrost in Canada</i>.<sup>2</sup>Polar Continental Shelf Project Contribution 03511.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Aboriginal Affairs Northern Dev Canada; Carleton University","funders":"","keywords":"Delta; Geology; River delta; Hydrology (agriculture); Channel (broadcasting); Alluvium; Nile delta; Series (stratigraphy); Physical geography; Geomorphology; Geography; Paleontology; Environmental science; Physics","score_opus":0.032173919578415776,"score_gpt":0.2452103871903672,"score_spread":0.2130364676119514,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2322021109","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98925436,0.000737184,6.9216415e-9,0.0027049347,0.00013083988,0.00035669567,0.0059350366,7.759231e-7,0.0008801606],"genre_scores_gemma":[0.99888426,0.00016395784,0.000007056992,0.00038739128,0.00039972895,0.0000026092907,0.00014132075,0.0000033431445,0.000010339823],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976849,0.00028540936,0.00052157097,0.00019821555,0.0007194201,0.0005904863],"domain_scores_gemma":[0.9988599,0.0004770269,0.00019328545,0.00013326488,0.000115165676,0.00022139947],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0026257425,0.00015948186,0.00035281028,0.00045566043,0.0002838046,0.00016048766,0.00038441445,0.00006725379,0.002456167],"category_scores_gemma":[0.00020128173,0.00009875503,0.00003818968,0.0008707155,0.0010119847,0.0005201357,0.000016842288,0.00045847706,0.0000010006078],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001737536,0.000034688444,0.9785446,0.000022857734,0.000009658196,0.000016523,0.019852586,0.00009239245,0.00016904384,0.000098445205,0.0008454748,0.00013997321],"study_design_scores_gemma":[0.0006324402,0.0005438606,0.9465797,0.00018871206,0.000008137769,0.000044034543,0.045580085,0.00030669646,0.0014258235,0.00004156797,0.0045182854,0.00013065264],"about_ca_topic_score_codex":0.8835046,"about_ca_topic_score_gemma":0.99765253,"teacher_disagreement_score":0.11414789,"about_ca_system_score_codex":0.000023510249,"about_ca_system_score_gemma":0.0011229288,"threshold_uncertainty_score":0.9984557},"labels":[],"label_agreement":null},{"id":"W2322638569","doi":"10.1139/cjes-2014-0027","title":"Additions and refinements to<i>Sycodes</i><i>glabra</i>(Shumard, 1858), a poorly known Late Cretaceous (Campanian) marine gastropod from the northeast Pacific: taxonomic and biostratigraphic implications","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Marine Biology and Ecology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal British Columbia Museum","funders":"","keywords":"Geology; Ammonite; Paleontology; Cretaceous; Type locality; Genus; Zoology; Biology","score_opus":0.017016634779817564,"score_gpt":0.21004123941188482,"score_spread":0.19302460463206725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2322638569","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98679924,0.0002708092,0.000018202094,0.008375671,0.00018448556,0.00014896908,0.00034836397,0.0000043355267,0.003849921],"genre_scores_gemma":[0.9978061,0.000115245246,0.0011262116,0.0006360349,0.00014306429,0.000001820511,0.00004312499,0.000002057748,0.00012637577],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987465,0.00015781302,0.00027761896,0.0002523937,0.000118361495,0.0004472973],"domain_scores_gemma":[0.9985618,0.00032882227,0.00013579303,0.00015828636,0.000083181796,0.0007321186],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007854193,0.00012162655,0.00018497171,0.00023734957,0.0011722199,0.00023224883,0.00040936758,0.00005832937,0.002359099],"category_scores_gemma":[0.00017900574,0.00008389121,0.000040233128,0.0003432986,0.0009908134,0.00021258715,0.00002199763,0.0002444426,0.0000631817],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011955922,0.0000032652752,0.9880597,0.00000144137,0.000018042276,0.000004727193,0.000075962824,0.00002340142,0.000014173941,0.00014515436,0.0007394283,0.010902749],"study_design_scores_gemma":[0.00016277425,0.00045120344,0.969423,0.000013626846,0.000014918966,0.00011172221,0.0002011522,0.00029576645,0.0000023592193,0.001028795,0.028201286,0.00009339812],"about_ca_topic_score_codex":0.018742513,"about_ca_topic_score_gemma":0.7705204,"teacher_disagreement_score":0.7517779,"about_ca_system_score_codex":0.0000016788381,"about_ca_system_score_gemma":0.00047005602,"threshold_uncertainty_score":0.99855286},"labels":[],"label_agreement":null},{"id":"W2323735825","doi":"10.1139/cjes-2014-0052","title":"An early Late Cretaceous (Cenomanian) sturgeon (Acipenseriformes) from the Dunvegan Formation, northwestern Alberta, Canada","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fish Ecology and Management Studies","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Cenomanian; Cretaceous; Geology; Sturgeon; Paleontology; Fish <Actinopterygii>; Fishery","score_opus":0.006816661725537953,"score_gpt":0.17546013320820442,"score_spread":0.16864347148266645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2323735825","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98675555,0.0000303923,0.000045679142,0.0032263729,0.0004276126,0.00008351775,0.0000070567917,0.0000025774189,0.009421242],"genre_scores_gemma":[0.99587345,0.000010165543,0.00011579885,0.003355639,0.0000619464,0.0000011996525,0.0000017285339,0.000003986146,0.00057606946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988608,0.000084935426,0.0002550832,0.00015162877,0.00026740078,0.0003801487],"domain_scores_gemma":[0.99914205,0.00012392183,0.0002123374,0.00015792166,0.000023956996,0.00033981437],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005190815,0.00010893824,0.00013803065,0.000036135094,0.0009795619,0.00013753003,0.00068640907,0.000029671452,0.0009768697],"category_scores_gemma":[0.00007029012,0.00007267908,0.00003277527,0.00019865678,0.0004597102,0.00082892954,0.00003333641,0.00012580103,0.000066120825],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002914167,0.0000028549573,0.99296796,8.0131144e-7,0.000010740163,0.00001699113,0.0012118383,0.0012826088,0.0000061799847,0.000050976094,0.003921968,0.00052413426],"study_design_scores_gemma":[0.00010822383,0.0001612802,0.9309024,0.0000080012705,0.0000141742,0.0000109628745,0.00054835185,0.0006178245,0.000019779876,0.00022072755,0.067290366,0.0000978648],"about_ca_topic_score_codex":0.9253297,"about_ca_topic_score_gemma":0.9999408,"teacher_disagreement_score":0.07461111,"about_ca_system_score_codex":0.000028731683,"about_ca_system_score_gemma":0.00027033046,"threshold_uncertainty_score":0.9999364},"labels":[],"label_agreement":null},{"id":"W2323906791","doi":"10.1139/e2012-046","title":"Reassessment of the problematic Burgess Shale sponge <i>Takakkawia lineata</i> Walcott, 1920","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Marine Sponges and Natural Products","field":"Biochemistry, Genetics and Molecular Biology","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Sponge spicule; Paleontology; Sponge; Geology","score_opus":0.017983341471819694,"score_gpt":0.24943199631226518,"score_spread":0.23144865484044547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2323906791","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99416596,0.0020586269,0.0000073448205,0.0010646424,0.00065340253,0.00010119525,0.000009107701,6.408445e-7,0.0019390701],"genre_scores_gemma":[0.99824077,0.000051069615,0.0004410051,0.00016922169,0.00034900074,6.878178e-7,0.0000018415362,0.000004222173,0.00074220495],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991004,0.00005233997,0.00025119103,0.000102532766,0.0001949031,0.00029863202],"domain_scores_gemma":[0.9991466,0.000010409585,0.00024156088,0.00017843451,0.00014286548,0.00028013618],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008472451,0.00008388279,0.00012708969,0.00007057437,0.000140129,0.000025889716,0.0004187149,0.000045160265,0.00007816678],"category_scores_gemma":[0.00016558322,0.00004961346,0.00008718981,0.00022814215,0.00024606468,0.000019749301,0.000039590588,0.00010513986,0.0000014738475],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031855376,0.00008612745,0.87547314,0.0001758341,0.000087922876,0.000010617808,0.00035773986,0.00010573941,0.105131485,0.0015229727,0.0064045186,0.010612051],"study_design_scores_gemma":[0.0003930138,0.00051738834,0.81550276,0.00020750196,0.000049201597,0.00037684583,0.0002157733,0.00003054502,0.11580544,0.0002599432,0.066370465,0.00027111854],"about_ca_topic_score_codex":0.00063698855,"about_ca_topic_score_gemma":0.004116667,"teacher_disagreement_score":0.05997037,"about_ca_system_score_codex":0.0000032359567,"about_ca_system_score_gemma":0.00077628536,"threshold_uncertainty_score":0.22971968},"labels":[],"label_agreement":null},{"id":"W2323989458","doi":"10.1139/cjes-2014-0109","title":"Late Wisconsin ice-flow history in the Buffalo Head Hills kimberlite field, north-central Alberta","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Deglaciation; Ice stream; Outcrop; Kimberlite; Ice sheet; Drumlin; Bedrock; Glacial period; Geomorphology; Head (geology); Seabed gouging by ice; Paleontology; Oceanography; Cryosphere; Sea ice; Mantle (geology)","score_opus":0.02375731989137817,"score_gpt":0.22175634625779841,"score_spread":0.19799902636642025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2323989458","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.970047,0.002691924,0.00000751272,0.0064538782,0.0008625349,0.00007137208,0.0000055445066,0.0000016674588,0.019858548],"genre_scores_gemma":[0.99655885,0.00004964433,0.00022238377,0.0027056925,0.00012076086,2.1391861e-7,0.0000045471347,0.0000012002713,0.0003366865],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99809587,0.0004359193,0.0003061691,0.00017647681,0.00026227295,0.00072330004],"domain_scores_gemma":[0.99824375,0.0009684668,0.0001270428,0.00014709691,0.00005780676,0.0004558487],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016877305,0.00010979149,0.00020597807,0.0003173595,0.00031847556,0.0000688652,0.0007453793,0.00008904211,0.0022996545],"category_scores_gemma":[0.0004918149,0.00007144947,0.000072536575,0.00033620972,0.00091420737,0.0003068054,0.0000044014173,0.00046960558,0.00012290922],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009659683,0.0000035683577,0.9945845,0.0000035866271,0.0000049167747,0.00010672604,0.0010523654,0.0016136435,3.1506627e-7,0.00011522399,0.0011537166,0.001351759],"study_design_scores_gemma":[0.00017790434,0.00028409637,0.92508894,0.00002180916,0.0000054959337,0.00031503133,0.000112126465,0.0022869923,0.0000019895194,0.0003681537,0.071248665,0.00008880859],"about_ca_topic_score_codex":0.076577954,"about_ca_topic_score_gemma":0.98544735,"teacher_disagreement_score":0.9088694,"about_ca_system_score_codex":0.0000015976028,"about_ca_system_score_gemma":0.0013960896,"threshold_uncertainty_score":0.9986124},"labels":[],"label_agreement":null},{"id":"W2324085609","doi":"10.1139/e2012-044","title":"First mammals from the Paleocene Porcupine Hills Formation of southwestern Alberta, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Royal Tyrrell Museum","funders":"","keywords":"Fauna; Geology; Mammal; Paleontology; Porcupine; Stratigraphic unit; Taxon; Genus; Archaeology; Geography; Ecology; Sedimentary rock; Biology","score_opus":0.016627911968573505,"score_gpt":0.18292768512761884,"score_spread":0.16629977315904534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2324085609","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9841988,0.0025743362,0.00002089477,0.0073691076,0.00060781726,0.00008108536,0.0001045977,0.0000011460302,0.0050422247],"genre_scores_gemma":[0.9987888,0.00005297847,0.00018179626,0.0007455111,0.00009852805,2.0910825e-7,0.0000060203183,7.8852884e-7,0.00012537914],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99897337,0.000060284616,0.00034621314,0.00008626068,0.00025491105,0.0002789453],"domain_scores_gemma":[0.99877226,0.00040214113,0.00030127278,0.000086515414,0.00014957726,0.00028821945],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003138175,0.00008479158,0.00016827557,0.00008022254,0.00044696458,0.0000622106,0.0003899317,0.000031064796,0.0023515504],"category_scores_gemma":[0.0001713365,0.00004985755,0.000045700355,0.00022249753,0.00042191424,0.00039923372,0.0000031930983,0.00009582398,0.00003258932],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001456194,7.653597e-7,0.9954454,0.0000023792534,0.0000102297945,0.0000047931735,0.0005450191,0.0007917394,0.0000012213742,0.000016931586,0.0023637216,0.00081640005],"study_design_scores_gemma":[0.0001006162,0.0000672275,0.98762584,0.00003503424,0.000009581578,0.00003302832,0.0013856373,0.0006918392,0.0000177647,0.00018656324,0.00978266,0.0000642404],"about_ca_topic_score_codex":0.9906344,"about_ca_topic_score_gemma":0.9999817,"teacher_disagreement_score":0.014589999,"about_ca_system_score_codex":0.000002289062,"about_ca_system_score_gemma":0.0012077794,"threshold_uncertainty_score":0.9985604},"labels":[],"label_agreement":null},{"id":"W2324552471","doi":"10.1139/cjes-2014-0156","title":"Hirnantian strata identified in major intracratonic basins of central North America: implications for uppermost Ordovician stratigraphy","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Research Manitoba; University of Manitoba","funders":"","keywords":"Ordovician; Geology; Paleontology; Excursion; Conodont; Paleozoic; Structural basin; Stratigraphy; Chemostratigraphy; Subaerial; Biostratigraphy; Tectonics; Isotopes of carbon; Total organic carbon","score_opus":0.019295957354992163,"score_gpt":0.23222233885893476,"score_spread":0.2129263815039426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2324552471","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9885236,0.0016477853,0.00044454186,0.0009846386,0.00039498988,0.0001713358,0.00049188203,0.0000033954827,0.0073378333],"genre_scores_gemma":[0.9975272,0.00004349469,0.0022345898,0.00009637753,0.00008140749,6.593214e-7,0.000010766401,9.915578e-7,0.0000045064608],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983431,0.00009817679,0.0005775125,0.0002156634,0.00016507714,0.00060043106],"domain_scores_gemma":[0.9985978,0.00019193442,0.00038782958,0.00015129511,0.0001191812,0.00055197184],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005677129,0.00013437633,0.0002998538,0.0005968258,0.00040020203,0.000112747286,0.00063915807,0.00006905455,0.00012834926],"category_scores_gemma":[0.00014555431,0.00011246997,0.00014346099,0.0009531798,0.0009533817,0.00050388376,8.087762e-7,0.00018447761,0.0000015883429],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010040876,0.000008797763,0.9487044,0.000008620595,0.00001474998,0.000005126138,0.00020297439,0.0003172566,0.00004368663,0.0010861476,0.000035454126,0.049562752],"study_design_scores_gemma":[0.00026365096,0.00043174482,0.9953298,0.00003375074,0.000017960538,0.000030999843,0.00039021345,0.0004930434,0.000050683717,0.0019869432,0.0008459799,0.00012525369],"about_ca_topic_score_codex":0.012761393,"about_ca_topic_score_gemma":0.9678063,"teacher_disagreement_score":0.9550449,"about_ca_system_score_codex":0.0000013876934,"about_ca_system_score_gemma":0.0015174004,"threshold_uncertainty_score":0.99381274},"labels":[],"label_agreement":null},{"id":"W2325146523","doi":"10.1139/cjes-2014-0008","title":"An integrated technique for delineating groundwater contaminated zones using geophysical and remote sensing techniques: a case study of Al-Quway’iyah, central Saudi Arabia","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Groundwater; Lineament; Water table; Groundwater flow; Bedrock; Remote sensing; Aquifer; Tectonics; Mining engineering; Hydrology (agriculture); Geomorphology; Seismology; Geotechnical engineering","score_opus":0.023167705153068808,"score_gpt":0.25281661112886267,"score_spread":0.22964890597579385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2325146523","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9105371,0.0000482084,0.08879684,0.00010518786,0.00013627089,0.00030617858,0.000011661604,0.00001941545,0.000039089733],"genre_scores_gemma":[0.88159627,0.0000039561824,0.11799298,0.00032332027,0.00007013757,1.2432957e-7,0.000002885005,0.0000046644773,0.0000056727963],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99842894,0.0002136982,0.00047644516,0.00024546916,0.0002099675,0.00042548598],"domain_scores_gemma":[0.99867016,0.0001498141,0.00032773154,0.00012641556,0.00032474592,0.00040111266],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016383788,0.00016220915,0.00032302688,0.0004709111,0.0005199069,0.00016760336,0.00022467895,0.000064265456,0.000020769188],"category_scores_gemma":[0.00018337579,0.00012341116,0.00005609411,0.00038941024,0.00048039522,0.0005035392,0.0000058105393,0.00020528762,2.3004374e-7],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012175313,0.00009775071,0.17392808,0.0000954143,0.000077556906,0.0016103126,0.006320732,0.0014235692,0.01161381,0.000027981292,0.0002945827,0.80438846],"study_design_scores_gemma":[0.0007190976,0.0069799754,0.00975769,0.00061229395,0.00009869635,0.010665751,0.01749538,0.9268438,0.023109939,0.0008186606,0.0023533814,0.00054530083],"about_ca_topic_score_codex":0.2802023,"about_ca_topic_score_gemma":0.0737566,"teacher_disagreement_score":0.9254203,"about_ca_system_score_codex":0.0000062717163,"about_ca_system_score_gemma":0.0004103397,"threshold_uncertainty_score":0.9431449},"labels":[],"label_agreement":null},{"id":"W2325160388","doi":"10.1139/cjes-2012-0146","title":"Summary of fossil vertebrate taxa named by Richard C. Fox, with an annotated list of taxa named between 1962 and 2012 and new photographs for non-mammalian therapsid and mammalian holotypes erected between 1968 and 1994","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"University of Alberta","keywords":"Vertebrate paleontology; Vertebrate; Cretaceous; Taxon; Paleontology; Mammal; Geology; Fauna; Archaeology; Geography; Biology; Ecology","score_opus":0.027895965167053928,"score_gpt":0.23764512488885617,"score_spread":0.20974915972180225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2325160388","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97633636,0.021992765,0.000026525702,0.0004618467,0.00011678443,0.00021654196,0.0005109777,0.000004191575,0.00033400816],"genre_scores_gemma":[0.9979394,0.00031504384,0.0014269175,0.00008043421,0.0000845369,7.055549e-7,0.00002065819,0.0000044429457,0.00012783824],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99852633,0.00012670082,0.00039180234,0.00023846152,0.00020717537,0.0005095402],"domain_scores_gemma":[0.9981332,0.00025653478,0.00044059232,0.00008910697,0.00010542833,0.00097513234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008542176,0.00020482315,0.00050491095,0.00035990044,0.00044521544,0.000080642974,0.00018714195,0.00010319503,0.000059975948],"category_scores_gemma":[0.00006557109,0.00014729846,0.000036732068,0.0004087267,0.001994985,0.0007276439,0.00000779377,0.00015074028,2.7508696e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000669819,0.0000049310474,0.9882026,0.000030931944,0.00007989237,0.0000029318196,0.001491095,0.0000014552286,0.00007476705,0.0000047723843,0.00047107643,0.009568594],"study_design_scores_gemma":[0.0009078215,0.0015118202,0.9908869,0.00007645471,0.00009643576,0.000045841534,0.00095056073,0.000066839726,0.00022190766,0.000110899695,0.004930331,0.00019416184],"about_ca_topic_score_codex":0.026631627,"about_ca_topic_score_gemma":0.42005017,"teacher_disagreement_score":0.39341855,"about_ca_system_score_codex":0.0000017654737,"about_ca_system_score_gemma":0.00045711515,"threshold_uncertainty_score":0.9798501},"labels":[],"label_agreement":null},{"id":"W2325211438","doi":"10.1139/e2012-012","title":"Influence of snow on near-surface ground temperatures in upland and alluvial environments of the outer Mackenzie Delta, Northwest Territories<sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of <i>Fundamental and applied research on permafrost in Canada</i>.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Aboriginal Affairs Northern Dev Canada; Carleton University","funders":"","keywords":"Alluvium; Permafrost; Geology; Snow; Alluvial plain; Alluvial fan; Hydrology (agriculture); Active layer; Bedrock; Geomorphology; Oceanography","score_opus":0.02795741511806026,"score_gpt":0.22676105807023766,"score_spread":0.1988036429521774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2325211438","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99615294,0.00020788623,2.3715558e-9,0.000776659,0.00009039004,0.00016753473,0.0020716195,1.9054278e-7,0.00053276407],"genre_scores_gemma":[0.99959296,0.000097137185,0.000011020137,0.00018014833,0.00008816458,4.6238483e-7,0.000014922826,0.0000024359601,0.000012776254],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982459,0.00014717982,0.0004642644,0.00014770788,0.0006451676,0.00034979772],"domain_scores_gemma":[0.9990601,0.0003598605,0.00022855734,0.00013782903,0.00003932979,0.00017435248],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011416486,0.00011605447,0.00028828395,0.00015630334,0.00013752062,0.00005206688,0.00034125487,0.000047803704,0.001586584],"category_scores_gemma":[0.00009588135,0.000071964845,0.000026795187,0.00045375293,0.0013264893,0.00030440287,0.000021102818,0.00027051067,4.9700196e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016712946,0.00002725422,0.9859002,0.00002231102,0.0000075765865,0.0000046477994,0.010211211,0.0022824323,0.0011055545,0.000028818564,0.00010341976,0.00013940124],"study_design_scores_gemma":[0.0003463908,0.00037352394,0.98552746,0.00020758164,0.00000411735,0.000008442059,0.005683258,0.00007302128,0.007070133,0.000024473928,0.0006121253,0.000069489186],"about_ca_topic_score_codex":0.8447664,"about_ca_topic_score_gemma":0.9925453,"teacher_disagreement_score":0.14777894,"about_ca_system_score_codex":0.000017927356,"about_ca_system_score_gemma":0.0006419922,"threshold_uncertainty_score":0.9993261},"labels":[],"label_agreement":null},{"id":"W2325560029","doi":"10.1139/cjes-2014-0039","title":"Geochemical characteristics of glacial Lake Agassiz sediments and new ages for the Moorhead Phase at Fargo, North Dakota, USA","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"North Dakota State University","keywords":"Geology; Glacial lake; Aeolian processes; Glacial period; Fluvial; Sediment; Structural basin; Geochemistry; Geomorphology","score_opus":0.03771440854323119,"score_gpt":0.2674639506827945,"score_spread":0.2297495421395633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2325560029","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99691594,0.0005752345,0.000052548952,0.0013096868,0.00041043127,0.00009043834,0.0000983415,0.0000011147396,0.0005462933],"genre_scores_gemma":[0.99898803,0.00005344882,0.0003107085,0.00021602695,0.00017328879,2.4042643e-7,0.000014313341,0.000001169693,0.00024279728],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998893,0.00007694369,0.00027568318,0.00014010865,0.00020573655,0.00040851402],"domain_scores_gemma":[0.99850345,0.0005786835,0.00019698615,0.00008661454,0.00009288717,0.00054136006],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009194155,0.00009126212,0.00021856437,0.00013529586,0.0005445645,0.000051755087,0.00038948495,0.00006651878,0.0012721438],"category_scores_gemma":[0.00040446283,0.000058067937,0.000055225733,0.00016862153,0.0011767966,0.00014217102,0.0000090186595,0.00016384458,0.00002003136],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004157545,0.0000038060548,0.99502313,0.000007918974,0.000014581361,0.000009687459,0.00012909301,0.000037870203,0.000011931772,0.00002692567,0.0003421788,0.0043512885],"study_design_scores_gemma":[0.00049108797,0.00048373768,0.98207724,0.000014909782,0.000020538897,0.00013981693,0.000032092186,0.0012147675,0.000109327404,0.00018930774,0.015158966,0.00006821162],"about_ca_topic_score_codex":0.0016605947,"about_ca_topic_score_gemma":0.653648,"teacher_disagreement_score":0.6519874,"about_ca_system_score_codex":3.956885e-7,"about_ca_system_score_gemma":0.00062636385,"threshold_uncertainty_score":0.9996408},"labels":[],"label_agreement":null},{"id":"W2325777086","doi":"10.1139/cjes-2013-0064","title":"Regional and local ice-flow history in the vicinity of the Izok Lake Zn–Cu–Pb–Ag deposit, Nunavut","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University; Geological Survey of Canada","funders":"","keywords":"Geology; Glacial period; Geomorphology; Landform; Glacier; Biological dispersal; Terrain; Ice stream; Physical geography; Geochemistry; Paleontology; Cryosphere; Oceanography; Sea ice","score_opus":0.02920302871995954,"score_gpt":0.2135644706569079,"score_spread":0.18436144193694837,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2325777086","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98607767,0.0039641107,0.000009513943,0.0041647074,0.00030966918,0.00009343075,0.000005328386,0.0000010720305,0.005374521],"genre_scores_gemma":[0.99856675,0.000047794263,0.00016345759,0.0010918344,0.000038833343,3.503647e-7,8.3486435e-7,7.383898e-7,0.00008940887],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986523,0.00033944537,0.000244501,0.00011974566,0.00028926288,0.00035474205],"domain_scores_gemma":[0.9990343,0.00038291098,0.0001344047,0.00011293944,0.00008778154,0.00024770416],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013872207,0.00007697832,0.00015295004,0.0001919377,0.0003385144,0.000036348614,0.0006738868,0.00007377105,0.0011973899],"category_scores_gemma":[0.000110804154,0.000040510204,0.000050558836,0.0002982914,0.0028344428,0.0002477384,0.000007215447,0.00038231755,0.000026215084],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000047112776,0.0000031595662,0.9971236,0.00000534269,0.0000043592254,0.0000294154,0.0007178205,0.00030979616,0.0000022219042,0.00006627644,0.0009959559,0.00073731877],"study_design_scores_gemma":[0.000117424635,0.00013576896,0.99219364,0.000027290534,0.000005167662,0.0005753255,0.0007206534,0.0017318625,0.0000059064178,0.0006235849,0.0038136402,0.00004972431],"about_ca_topic_score_codex":0.025212841,"about_ca_topic_score_gemma":0.9330754,"teacher_disagreement_score":0.9078626,"about_ca_system_score_codex":0.0000011830136,"about_ca_system_score_gemma":0.0012770928,"threshold_uncertainty_score":0.9998793},"labels":[],"label_agreement":null},{"id":"W2325876585","doi":"10.1139/cjes-2013-0218","title":"Implications of metallic iron for diamonds and nitrogen in the sublithospheric mantle","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mantle (geology); Diamond; Kimberlite; Mineral redox buffer; Geology; Lithosphere; Metal; Geochemistry; Mantle plume; Transition zone; Materials science; Tectonics; Metallurgy; Paleontology","score_opus":0.0174132832002935,"score_gpt":0.21551800874832255,"score_spread":0.19810472554802905,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2325876585","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99716085,0.0005649811,0.000050139937,0.00074006803,0.00012397331,0.00007463537,0.0000402542,5.748414e-7,0.001244517],"genre_scores_gemma":[0.9988647,0.00001861948,0.00093056395,0.00011085955,0.000059202725,5.1231683e-7,0.0000020000043,7.935911e-7,0.000012709644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994377,0.000053265085,0.0001735585,0.00007152048,0.00009378011,0.00017018232],"domain_scores_gemma":[0.999497,0.00014836108,0.00012007783,0.000066359826,0.00004239059,0.00012579054],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010659193,0.000045245397,0.00011718215,0.000075237986,0.00014390927,0.00008465241,0.00027947186,0.00001715281,0.00013615175],"category_scores_gemma":[0.00006402839,0.000027239592,0.000029772213,0.00021268107,0.000201679,0.00016216702,0.0000018562737,0.000032975007,0.0000018222238],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005742453,0.000005736635,0.9820945,0.000020839865,0.000008649845,0.0000017208264,0.000849464,0.00057021255,0.000529225,0.008906924,0.0002072037,0.006799726],"study_design_scores_gemma":[0.00011798335,0.00024721966,0.9606376,0.00001067694,0.0000144803,0.000016638163,0.00022188938,0.00027292207,0.00022861092,0.026190009,0.0119838165,0.000058108977],"about_ca_topic_score_codex":0.008964264,"about_ca_topic_score_gemma":0.12835518,"teacher_disagreement_score":0.11939091,"about_ca_system_score_codex":2.9727832e-7,"about_ca_system_score_gemma":0.00019956652,"threshold_uncertainty_score":0.9976351},"labels":[],"label_agreement":null},{"id":"W2326006077","doi":"10.1139/e11-070","title":"Provenance variations in northern Appalachian Avalonia based on detrital zircon age patterns in Ediacaran and Cambrian sedimentary rocks, New Brunswick and Nova Scotia, Canada","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Mount Saint Vincent University; University of Toronto; Acadia University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Zircon; Provenance; Geology; Laurentia; Gondwana; Ordovician; Craton; Sedimentary depositional environment; Amazonian; Paleontology; Sedimentary rock; Paleozoic; Clastic rock; Geochemistry; Rodinia; Structural basin; Amazon rainforest","score_opus":0.009777721805436242,"score_gpt":0.17887733404358486,"score_spread":0.16909961223814862,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2326006077","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99572486,0.0009740518,0.000024547435,0.002491442,0.0002124487,0.00007540646,0.00002839039,0.0000011701145,0.0004676839],"genre_scores_gemma":[0.9986277,0.000009344728,0.00040207827,0.0008175166,0.00011151614,7.368578e-8,0.000008818099,0.0000012657496,0.000021663474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99877626,0.000061309715,0.00027596432,0.00017314467,0.0002471256,0.00046619252],"domain_scores_gemma":[0.99885696,0.00011067913,0.00010599127,0.00005829539,0.000022157736,0.00084590283],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004533991,0.00011546906,0.00020101998,0.00027996604,0.000115338094,0.000070305156,0.00017040069,0.000042170534,0.0003730981],"category_scores_gemma":[0.00009607864,0.00008710967,0.000028467839,0.00047880266,0.00012511796,0.00026730826,0.0000046911214,0.00021209609,0.0000037424763],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000056034346,0.0000071706068,0.9963089,0.0000045181155,0.0000034710586,0.000062664396,0.00011068102,0.0015500903,0.000009536273,0.000008606677,0.000024094681,0.0019046701],"study_design_scores_gemma":[0.000285136,0.00012495562,0.9975871,0.000049085604,0.000007939669,0.000021530419,0.00016768528,0.0012160796,0.000031923355,0.00012159552,0.00027144165,0.00011555615],"about_ca_topic_score_codex":0.99132574,"about_ca_topic_score_gemma":0.99996996,"teacher_disagreement_score":0.008644272,"about_ca_system_score_codex":0.000008889,"about_ca_system_score_gemma":0.0020798345,"threshold_uncertainty_score":0.40851626},"labels":[],"label_agreement":null},{"id":"W2326120462","doi":"10.1139/e11-055","title":"The Campbellton Formation, New Brunswick, Canada: paleoenvironments in an important Early Devonian terrestrial locality","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University; Geological Society of America","keywords":"Geology; Siltstone; Conglomerate; Facies; Outcrop; Alluvium; Cobble; Fluvial; Alluvial fan; Geochemistry; Paleontology; Overbank; Geomorphology; Sedimentary rock; Structural basin","score_opus":0.032721204369031504,"score_gpt":0.20026022634708915,"score_spread":0.16753902197805765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2326120462","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99673843,0.00070784835,0.000031299838,0.0003756304,0.00040540044,0.00007178871,0.000008629399,0.0000015242786,0.001659463],"genre_scores_gemma":[0.9993809,0.00005740295,0.00028774972,0.00015622235,0.00006420777,7.241532e-8,0.0000027487572,8.1317063e-7,0.000049871313],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986674,0.00007497315,0.00047340686,0.000097836295,0.00029115533,0.00039522495],"domain_scores_gemma":[0.9989101,0.000057671623,0.0002436417,0.000090232425,0.00003280501,0.0006655459],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00073263387,0.00008677041,0.00011285991,0.00010412275,0.00056786207,0.00015580788,0.00052381237,0.000037552327,0.000903874],"category_scores_gemma":[0.00010402799,0.000051071904,0.000027014768,0.00032374836,0.0002913524,0.00090093235,0.000003323817,0.00015090735,0.000009809304],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008691449,0.0000019202712,0.9951176,9.427917e-7,0.0000017897677,0.000025435902,0.000540739,0.00035535265,2.0383587e-7,0.000068538364,0.00006321127,0.003815591],"study_design_scores_gemma":[0.00012248116,0.00025046978,0.9904119,0.000010108531,0.0000028621187,0.000039766073,0.0006340118,0.0005186382,0.000021969696,0.0013085708,0.006601293,0.00007792345],"about_ca_topic_score_codex":0.96848494,"about_ca_topic_score_gemma":0.99989516,"teacher_disagreement_score":0.031410217,"about_ca_system_score_codex":0.0000049858154,"about_ca_system_score_gemma":0.0075579584,"threshold_uncertainty_score":0.9980683},"labels":[],"label_agreement":null},{"id":"W2327086661","doi":"10.1139/cjes-2014-0025","title":"New structural, metamorphic, and U–Pb geochronological constraints on the Blezardian Orogeny and Yavapai Orogeny in the Southern Province, Sudbury, Canada","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University; University of Regina","funders":"","keywords":"Orogeny; Geology; Geochemistry; Craton; Metamorphism; Archean; Zircon; Dike; Overprinting; Metamorphic rock; Proterozoic; Pluton; Paleontology; Tectonics","score_opus":0.014207739714630132,"score_gpt":0.1764062490790466,"score_spread":0.16219850936441646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2327086661","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98617727,0.00095969054,0.0000059379977,0.01094762,0.00007843035,0.000079368896,0.000028576562,0.0000016328474,0.001721469],"genre_scores_gemma":[0.9975719,0.000019193323,0.00025715833,0.0020264983,0.00008662823,1.676774e-7,0.0000016734729,8.6005207e-7,0.00003592452],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985999,0.00018821165,0.0002541178,0.00020861372,0.0003304853,0.0004187119],"domain_scores_gemma":[0.9987041,0.00049509853,0.00012687172,0.00010467261,0.00003968745,0.00052956986],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011457782,0.00013585559,0.00022381995,0.00009327602,0.00044917065,0.00020264777,0.00051192846,0.000050325474,0.0035773434],"category_scores_gemma":[0.0003639451,0.000057797406,0.00005013292,0.00032910978,0.001141842,0.00009692162,0.000009145803,0.00028557933,0.000008879754],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008976791,0.000002014631,0.9565863,0.0000034909465,0.000025484764,0.000103038765,0.0002329946,0.00040510445,0.000034568606,0.0013353426,0.00049311144,0.040769592],"study_design_scores_gemma":[0.00016433823,0.00028034413,0.98196775,0.000016849017,0.000026290647,0.00025925715,0.0010961464,0.00081572303,0.00006462315,0.010619001,0.0045426795,0.00014701809],"about_ca_topic_score_codex":0.77983147,"about_ca_topic_score_gemma":0.99681866,"teacher_disagreement_score":0.21698716,"about_ca_system_score_codex":0.000002352272,"about_ca_system_score_gemma":0.001335105,"threshold_uncertainty_score":0.9973335},"labels":[],"label_agreement":null},{"id":"W2327518324","doi":"10.1139/cjes-2013-0120","title":"Structural setting and age of the Partridge Island block, southern New Brunswick, Canada: a link to the Cobequid Highlands of northern mainland Nova Scotia","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University; Technical University of Nova Scotia; University of Toronto; University of New Brunswick; Dalhousie University; Nova Scotia Department of Energy","funders":"Natural Sciences and Engineering Research Council of Canada; Acadia University; U.S. Department of Energy","keywords":"Geology; Zircon; Carboniferous; Terrane; Devonian; Volcanic rock; Geochemistry; Sedimentary rock; Paleontology; Volcano; Tectonics; Structural basin","score_opus":0.01131033378022501,"score_gpt":0.17415468274673118,"score_spread":0.16284434896650618,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2327518324","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98869556,0.0005441666,0.0000034501593,0.009961504,0.00017020911,0.00009011783,0.000055389322,7.7606813e-7,0.0004788523],"genre_scores_gemma":[0.9991615,0.0000030925128,0.0001500311,0.00042019694,0.00011389035,3.164269e-8,0.0000020961606,0.0000011066855,0.00014809181],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99876606,0.00006633566,0.00035340915,0.00013514276,0.00034359784,0.000335424],"domain_scores_gemma":[0.9988472,0.00015645259,0.00024690284,0.00011331322,0.00013415268,0.0005019932],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042060995,0.00010719715,0.00023683919,0.00007493887,0.000226838,0.00007574858,0.00054126926,0.000034808334,0.0017732244],"category_scores_gemma":[0.00020369244,0.00004751148,0.000074484946,0.0004992291,0.00043765805,0.00008155943,0.000017094237,0.00015669357,0.000008166643],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003457396,5.617346e-7,0.99434644,0.0000038238777,0.00001626419,0.000006537712,0.00037827113,0.0033585432,0.00005151655,0.000007882924,0.00019876713,0.0016279088],"study_design_scores_gemma":[0.00011344401,0.00010902554,0.99704725,0.000027949018,0.000023113816,0.0000468173,0.00043088768,0.00079574704,0.00010001585,0.00042551884,0.00080303114,0.00007722461],"about_ca_topic_score_codex":0.9775113,"about_ca_topic_score_gemma":0.99983567,"teacher_disagreement_score":0.022324381,"about_ca_system_score_codex":0.0000018246575,"about_ca_system_score_gemma":0.0025654219,"threshold_uncertainty_score":0.9991393},"labels":[],"label_agreement":null},{"id":"W2328225848","doi":"10.1139/cjes-2012-0177","title":"Insights into the Phanerozoic tectonic evolution of the northern Laurentian margin: detrital apatite and zircon (U–Th)/He ages from Devonian strata of the Franklinian Basin, Canadian Arctic Islands","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Calgary","funders":"","keywords":"Geology; Laurentia; Zircon; Devonian; Paleontology; Orogeny; Terrane; Sedimentary depositional environment; Paleozoic; Late Devonian extinction; Structural basin; Tectonics; Carboniferous","score_opus":0.011027649019080191,"score_gpt":0.17198894148317673,"score_spread":0.16096129246409654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2328225848","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9897693,0.003926978,0.000010069846,0.0051288926,0.0005070735,0.00017271379,0.000040659605,0.00000125017,0.00044310014],"genre_scores_gemma":[0.9995535,0.000075605014,0.000082185135,0.00017441667,0.00008696374,5.572149e-7,0.0000036894921,0.0000016821109,0.000021423297],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99868953,0.00016419597,0.00034118025,0.00015476948,0.00034207953,0.00030821993],"domain_scores_gemma":[0.9988857,0.00013690753,0.00030003174,0.0001623702,0.00020266153,0.00031232636],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038001468,0.00011819199,0.00018237479,0.00013481037,0.0009851049,0.00013757592,0.00067365967,0.00006452542,0.00053826306],"category_scores_gemma":[0.00021152197,0.00005284874,0.00008650524,0.00064101326,0.0010928111,0.00034630997,0.000016112239,0.00022204814,0.000009101149],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002067598,0.0000024119058,0.9952902,0.0000050859876,0.000020667649,0.0000017267763,0.0015871336,0.00043322277,0.000058219357,0.00003846375,0.000048103913,0.002512664],"study_design_scores_gemma":[0.00011593944,0.00015771472,0.99285305,0.00006316209,0.000022906843,0.000007810631,0.0021814294,0.0005326238,0.00009310076,0.0026273136,0.001270584,0.00007438224],"about_ca_topic_score_codex":0.8916044,"about_ca_topic_score_gemma":0.9991013,"teacher_disagreement_score":0.107496895,"about_ca_system_score_codex":0.000011118061,"about_ca_system_score_gemma":0.0010082386,"threshold_uncertainty_score":0.757673},"labels":[],"label_agreement":null},{"id":"W2328490207","doi":"10.1139/cjes-2012-0083","title":"Barrovian metamorphism in the central Kootenay Arc, British Columbia: petrology and isograd geometry","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Metamorphism; Sillimanite; Isograd; Metamorphic rock; Andalusite; Kyanite; Metamorphic facies; Staurolite; Pyrope; Geochemistry; Biotite; Fault (geology); Doming; Cretaceous; Petrology; Facies; Paleontology; Tectonics; Quartz","score_opus":0.008965507953859284,"score_gpt":0.16131881914727314,"score_spread":0.15235331119341386,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2328490207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99095094,0.0025206031,0.0000034108105,0.004581489,0.00014179444,0.000060032482,0.0000133888625,0.0000017228022,0.0017266182],"genre_scores_gemma":[0.9979866,0.00007268193,0.0003354524,0.0013982318,0.00008125566,3.4292862e-7,0.0000023857503,6.8967535e-7,0.0001223284],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99860746,0.00012409851,0.00028028272,0.00017394662,0.00024183976,0.00057238626],"domain_scores_gemma":[0.99901175,0.00016852084,0.00010551113,0.000067166526,0.000059829825,0.0005871932],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00074530876,0.000072532,0.00021514004,0.00016501536,0.00033216667,0.00062914065,0.00049292,0.000053248037,0.014336413],"category_scores_gemma":[0.0002273635,0.000054643137,0.00008266592,0.0007349886,0.00090093084,0.00030856155,0.000005767041,0.0002514475,0.000033099448],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[5.580575e-7,0.0000033685528,0.99207604,0.0000014675164,0.000006749897,0.000105343686,0.00006316193,0.00011174426,0.000006597723,0.000009482812,0.0004958828,0.007119618],"study_design_scores_gemma":[0.000103377875,0.00017700106,0.9876184,0.000007799367,0.000012539304,0.00043787094,0.00044735058,0.00045733587,0.0000015090394,0.007863327,0.0027940325,0.00007944204],"about_ca_topic_score_codex":0.7308689,"about_ca_topic_score_gemma":0.98784614,"teacher_disagreement_score":0.25697726,"about_ca_system_score_codex":9.2840065e-7,"about_ca_system_score_gemma":0.00021607266,"threshold_uncertainty_score":0.98656464},"labels":[],"label_agreement":null},{"id":"W2328566270","doi":"10.1139/cjes-2013-0172","title":"Tuzo Wilson and the acceptance of pre-Mesozoic continental drift","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Center for the Environment, Harvard University; Australian National University","keywords":"Continental drift; Geology; Paleontology; Mesozoic; Paleomagnetism; Continental shelf; Continental margin; Geologic time scale; Craton; Continental crust; Mantle (geology); Oceanography; Tectonics; Sedimentary rock; Structural basin","score_opus":0.007832457195139997,"score_gpt":0.18208107311001498,"score_spread":0.17424861591487498,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2328566270","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9904125,0.0017029217,0.000030698415,0.0022015048,0.000127859,0.000034609424,0.0000072223147,0.000001279067,0.0054814043],"genre_scores_gemma":[0.99913585,0.00003862261,0.00032633907,0.00033542936,0.00007389949,6.888896e-8,8.0424996e-7,4.487406e-7,0.00008856065],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910855,0.00008655283,0.00025305361,0.00010737207,0.00021548041,0.0002290035],"domain_scores_gemma":[0.9991046,0.00024673023,0.00019421641,0.00006452091,0.000070670496,0.00031921855],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010326016,0.00006933936,0.00021139836,0.00008815751,0.00021159371,0.00007290329,0.00036881238,0.000027388427,0.0020440642],"category_scores_gemma":[0.00034771545,0.000034044857,0.00008321062,0.00031024995,0.0015363827,0.00017091112,0.00000539404,0.0001135359,0.0000073138963],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018524648,0.0000018217971,0.9908014,0.000003095286,0.000009697067,0.0000029586556,0.00015160015,0.0005036155,0.00003068535,0.0007507313,0.000063140506,0.00766271],"study_design_scores_gemma":[0.00029744732,0.0001783972,0.9837057,0.000017569913,0.000019239937,0.000039803468,0.0001697076,0.0043902127,0.00019408324,0.007620265,0.003303382,0.00006421283],"about_ca_topic_score_codex":0.02042518,"about_ca_topic_score_gemma":0.27189773,"teacher_disagreement_score":0.25147256,"about_ca_system_score_codex":2.914515e-7,"about_ca_system_score_gemma":0.0001349873,"threshold_uncertainty_score":0.9988682},"labels":[],"label_agreement":null},{"id":"W2329082921","doi":"10.1139/cjes-2017-0164","title":"Corrigendum: Geothermobarometry of spinel peridotites from southern British Columbia: implications for the thermal conditions in the upper mantle","year":2017,"lang":"en","type":"erratum","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia; University of Calgary","funders":"","keywords":"Olivine; Geology; Pyroxene; Peridotite; Spinel; Xenolith; Lithosphere; Mantle (geology); Geochemistry; Kimberlite; Basalt; Amphibole; Tectonics; Quartz; Seismology","score_opus":0.027913292312814444,"score_gpt":0.22294905684153765,"score_spread":0.1950357645287232,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2329082921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94970614,0.014954257,0.000015681439,0.0051087965,0.004357764,0.000371279,0.008826798,0.0000035921107,0.016655711],"genre_scores_gemma":[0.9902906,0.0002027465,0.00011577082,0.00046372294,0.00064602064,0.0000031771417,0.00017976708,0.0000031711468,0.008095054],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99862766,0.00007668047,0.00041534632,0.00021889606,0.00027044403,0.0003909526],"domain_scores_gemma":[0.9984306,0.00038161097,0.0005322854,0.00026163482,0.00017759104,0.00021628861],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007390717,0.000121846475,0.00034540312,0.000121587465,0.00110513,0.000654175,0.0018002196,0.00014314792,0.012685382],"category_scores_gemma":[0.00039940226,0.00008087415,0.00028766593,0.0003512431,0.0014243723,0.00013704716,0.000009551285,0.0004399456,0.00001993529],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001576005,0.00000898933,0.9481637,0.0000068909735,0.000048259088,0.000011962542,0.00016324529,0.00019977799,0.000008156473,0.000011484724,0.04925086,0.002125109],"study_design_scores_gemma":[0.00008710602,0.00009229792,0.9601792,0.00007636786,0.00008130223,0.000035812882,0.0008206876,0.0003069248,9.071695e-7,0.0056154453,0.032590475,0.00011349137],"about_ca_topic_score_codex":0.6191983,"about_ca_topic_score_gemma":0.9815683,"teacher_disagreement_score":0.36236995,"about_ca_system_score_codex":0.0000018196079,"about_ca_system_score_gemma":0.0009965162,"threshold_uncertainty_score":0.9882172},"labels":[],"label_agreement":null},{"id":"W2329183081","doi":"10.1139/cjes-2014-0175","title":"Corrigendum: A low-relief hill in eastern Ontario, Canada, covered by the easily erodible Queenston Formation and derived sediments — probably the result of Quaternary tectonic uplift","year":2014,"lang":"en","type":"erratum","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Shell (Canada)","funders":"","keywords":"Geology; Quaternary; Tectonics; Geochemistry; Paleontology; Tectonic uplift; Geomorphology","score_opus":0.01742263999198586,"score_gpt":0.1918738231017286,"score_spread":0.17445118310974272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2329183081","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9733297,0.0068395315,0.000025271798,0.00236342,0.0055923443,0.00042995563,0.0003202549,0.0000029568441,0.011096518],"genre_scores_gemma":[0.993949,0.00019275556,0.000044144577,0.00060551043,0.00008821692,0.0000011333093,0.00007615554,0.0000027255335,0.0050403713],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978636,0.00019291307,0.0007343503,0.00018311501,0.00057393947,0.00045207984],"domain_scores_gemma":[0.99834234,0.0001304563,0.00086429506,0.00015256078,0.0001892552,0.00032110536],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015525261,0.00020027028,0.00032513228,0.000202601,0.0005465058,0.00020659085,0.0008049369,0.00013676679,0.00050024624],"category_scores_gemma":[0.00018113802,0.000105179926,0.00005369705,0.00039190534,0.00052112725,0.00045147102,0.00001323961,0.00061734417,0.0000062565355],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006904186,0.000014172212,0.71654886,0.0001818154,0.00005019985,0.000042532527,0.0030212952,0.0056371544,0.000008764487,0.000029727764,0.2689354,0.005460991],"study_design_scores_gemma":[0.0005044829,0.0007898756,0.70421904,0.0007080897,0.000042124386,0.00024846615,0.0011403507,0.009129828,0.000053510408,0.00053774973,0.28227058,0.00035591138],"about_ca_topic_score_codex":0.98531884,"about_ca_topic_score_gemma":0.99974346,"teacher_disagreement_score":0.02061924,"about_ca_system_score_codex":0.000020619696,"about_ca_system_score_gemma":0.0072835754,"threshold_uncertainty_score":0.9983442},"labels":[],"label_agreement":null},{"id":"W2329193866","doi":"10.1139/e2012-016","title":"Age and structure of the Crevice pluton: overlapping orogens in west-central Idaho?","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"University of Texas at Dallas; Washington State University","keywords":"Geology; Pluton; Overprinting; Shear zone; Transpression; Mylonite; Sinistral and dextral; Terrane; Geochemistry; Zircon; Cretaceous; Leucogranite; Batholith; Plutonism; Paleontology; Tectonics; Metamorphic rock","score_opus":0.014632869914881766,"score_gpt":0.18774142112957437,"score_spread":0.1731085512146926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2329193866","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99491674,0.0030529604,9.91057e-7,0.0005991681,0.00017956573,0.00002819126,0.000017813638,6.462051e-7,0.0012039454],"genre_scores_gemma":[0.99940634,0.000024742647,0.00023179977,0.00024502512,0.000075068645,1.4959102e-8,6.273729e-7,4.406781e-7,0.00001597206],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990715,0.000055706256,0.00022004539,0.00008073417,0.0001927426,0.00037927297],"domain_scores_gemma":[0.9992868,0.00006917195,0.00013236418,0.00005473108,0.000030460687,0.000426489],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031514952,0.0000678337,0.00016122012,0.00010131824,0.00013956222,0.000039467053,0.00028035868,0.00003656765,0.0025402238],"category_scores_gemma":[0.00014891078,0.000035973593,0.00006052409,0.0005331421,0.00046931137,0.0002230747,0.0000069618814,0.00014845504,0.0000023147823],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001324225,0.0000016619957,0.99774617,0.0000039561464,0.0000045228257,0.000009413271,0.00023739558,0.0007142994,0.00026194123,0.000091118265,0.000007066628,0.00092114473],"study_design_scores_gemma":[0.00005878728,0.000034792272,0.9970215,0.000025207906,0.000010922562,0.00005681531,0.00023583506,0.00018596408,0.00023240666,0.001165207,0.00092021277,0.000052325788],"about_ca_topic_score_codex":0.022381982,"about_ca_topic_score_gemma":0.52592516,"teacher_disagreement_score":0.5035432,"about_ca_system_score_codex":0.0000011247281,"about_ca_system_score_gemma":0.00021646444,"threshold_uncertainty_score":0.9983716},"labels":[],"label_agreement":null},{"id":"W2329281336","doi":"10.1139/cjes-2012-0025","title":"Giant Upper Triassic bivalves of Wrangellia, Vancouver Island, Canada","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"University of Montana; National Science Foundation","keywords":"Terrane; Geology; Bay; Biota; Paleontology; Genus; Oceanography; Ecology; Tectonics","score_opus":0.01411073401081913,"score_gpt":0.19345665506408793,"score_spread":0.1793459210532688,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2329281336","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94499916,0.0067042974,0.00002738219,0.00060114864,0.0015584392,0.00008410369,0.000056729074,0.0000017018199,0.045967028],"genre_scores_gemma":[0.998639,0.000020885065,0.0009251248,0.0001073942,0.00008592653,1.5825006e-7,5.8468976e-7,5.657276e-7,0.00022040101],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986505,0.0000788651,0.00038679742,0.00012863748,0.00033885066,0.0004163547],"domain_scores_gemma":[0.9987357,0.0001627565,0.00026958596,0.00009662762,0.00013774452,0.00059754204],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048315176,0.00010947717,0.00025162505,0.00027612704,0.000286879,0.00006460725,0.000455097,0.00005743924,0.0037226065],"category_scores_gemma":[0.000105523104,0.0000760715,0.00010164898,0.000385235,0.00070841715,0.0004515003,6.092203e-7,0.00016516526,0.000011756027],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000062591507,0.0000027713543,0.95579827,0.0000068709865,0.000026105265,0.000034369255,0.00018757416,0.00017396848,0.00003705965,0.00004963648,0.012131349,0.03154577],"study_design_scores_gemma":[0.00017911376,0.00016371273,0.99271387,0.00003253583,0.000011123871,0.000045966055,0.00034325855,0.00014172721,0.000111919944,0.0007474792,0.00540322,0.0001060887],"about_ca_topic_score_codex":0.909924,"about_ca_topic_score_gemma":0.9998469,"teacher_disagreement_score":0.0899229,"about_ca_system_score_codex":0.0000015243853,"about_ca_system_score_gemma":0.0042021605,"threshold_uncertainty_score":0.99718815},"labels":[],"label_agreement":null},{"id":"W2330601677","doi":"10.1139/cjes-2014-0001","title":"Fault zone migration by footwall shortcut and recumbent folding along an inverted fault: example from the Mosha Fault, Central Alborz, Northern Iran","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Fault (geology); Seismology; Normal fault","score_opus":0.029548825917799202,"score_gpt":0.2116782938699169,"score_spread":0.1821294679521177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2330601677","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99372953,0.0036090468,0.00021094616,0.0011689073,0.00045457907,0.00012251758,0.00009078589,0.0000095025225,0.0006041647],"genre_scores_gemma":[0.9984288,0.00021264568,0.00036492612,0.0006471079,0.00025904606,4.4779395e-7,0.000034344597,0.0000041492594,0.000048502727],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980344,0.00018145032,0.00041178727,0.00031245308,0.00044570217,0.00061416277],"domain_scores_gemma":[0.998485,0.00028621205,0.0002404062,0.0001666298,0.00010453978,0.00071715924],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009556146,0.00019007552,0.00026609408,0.00012067755,0.001067553,0.00040568598,0.00048568283,0.00006949781,0.00039119972],"category_scores_gemma":[0.00016733057,0.00012457796,0.000072273506,0.0003535908,0.00052010454,0.00063726737,0.000008864219,0.00023875608,0.000010820386],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000794842,0.000004581047,0.9428818,0.0000018358386,0.000031094296,0.000012587457,0.0029417912,0.0011374706,0.000051336203,0.000020624408,0.00062871195,0.05228018],"study_design_scores_gemma":[0.000357278,0.0004625929,0.9603269,0.00005398686,0.0000345242,0.000045758265,0.0026153936,0.015276199,0.00011048769,0.00028883448,0.020206466,0.00022155441],"about_ca_topic_score_codex":0.49178606,"about_ca_topic_score_gemma":0.9883994,"teacher_disagreement_score":0.49661332,"about_ca_system_score_codex":0.0000046904834,"about_ca_system_score_gemma":0.0003830929,"threshold_uncertainty_score":0.8210862},"labels":[],"label_agreement":null},{"id":"W2331176462","doi":"10.1139/cjes-2015-0198","title":"Unusual preservation of the trace fossil <i>Conostichus</i> in middle Silurian carbonate facies of Indiana, USA","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Paleontological Society","keywords":"Paleozoic; Siliciclastic; Geology; Carbonate; Paleontology; Trace fossil; Facies; Carbonate rock; Devonian; Sedimentary rock; Ordovician; Pennsylvanian; Carbonate platform; Taphonomy; Geochemistry","score_opus":0.03350179906039887,"score_gpt":0.20303031729239293,"score_spread":0.16952851823199405,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2331176462","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932084,0.0011100593,0.000013246729,0.0013820609,0.0002116621,0.000057614507,0.00006952366,7.153451e-7,0.0039467146],"genre_scores_gemma":[0.9995809,0.00003414419,0.00018422028,0.000040824598,0.000019645682,1.2933145e-7,2.991526e-7,5.557807e-7,0.0001392569],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990124,0.000066997505,0.00038026855,0.00007765153,0.00023949218,0.00022316766],"domain_scores_gemma":[0.9990899,0.00023383215,0.00031238992,0.00007394908,0.00012746308,0.00016247993],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00072380574,0.0000639822,0.00014610328,0.00021835588,0.00013803494,0.000032659424,0.00047546902,0.000041580926,0.0005370356],"category_scores_gemma":[0.00052256824,0.00003116777,0.000049413597,0.00062719506,0.00066076993,0.0006411168,0.0000048616835,0.00007460655,0.0000045535357],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004434367,0.0000029419962,0.99263704,0.000010699885,0.0000029514883,0.0000022598583,0.00047180417,0.0024991252,0.00006972229,0.00026276606,0.000018583341,0.0040176576],"study_design_scores_gemma":[0.0001373809,0.00018508804,0.9926214,0.00010355996,0.000004205269,0.000013613859,0.00037052156,0.0002132317,0.0013107378,0.0022215494,0.0027662308,0.00005244677],"about_ca_topic_score_codex":0.021220144,"about_ca_topic_score_gemma":0.54479355,"teacher_disagreement_score":0.5235734,"about_ca_system_score_codex":0.0000013976993,"about_ca_system_score_gemma":0.0009368408,"threshold_uncertainty_score":0.9852976},"labels":[],"label_agreement":null},{"id":"W2331225384","doi":"10.1139/cjes-2015-0206","title":"Paleoenvironments revealed by rare-earth element systematics in vertebrate bioapatite from the Lower Devonian of Svalbard","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Sedimentary depositional environment; Diagenesis; Taphonomy; Devonian; Paleontology; Vertebrate; Rare-earth element; Stromatolite; Structural basin; Carbonate; Biology; Rare earth; Earth science; Chemistry","score_opus":0.010056379994683819,"score_gpt":0.17941443210813235,"score_spread":0.16935805211344854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2331225384","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965736,0.0010237653,0.000032342345,0.0011989725,0.0001855702,0.000077965844,0.00028835438,9.912604e-7,0.00061839796],"genre_scores_gemma":[0.9992385,0.00009737701,0.00022803304,0.00019188508,0.00003870151,2.779595e-7,0.0000072313037,0.0000013695397,0.00019660903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998429,0.00012023789,0.00054113864,0.00015501544,0.00041326557,0.00034131698],"domain_scores_gemma":[0.99901277,0.00014229005,0.000349897,0.00013163242,0.000036031506,0.00032735892],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009640907,0.00011239087,0.00023585426,0.00010037659,0.00018522295,0.00006209368,0.00049015484,0.00003592391,0.0055901967],"category_scores_gemma":[0.00008844288,0.000058027636,0.00008374982,0.0003424245,0.00039255712,0.00025804827,0.0000068833,0.00008183102,0.000052832373],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000059754125,0.0000072941457,0.99686086,0.000007480837,0.00002456258,0.000017922592,0.00012505626,0.00019478338,0.0003529966,0.0000021581347,0.0003065818,0.002094321],"study_design_scores_gemma":[0.00052542024,0.00034274132,0.98810035,0.0005220889,0.000041609357,0.000016731185,0.0009858487,0.00087354425,0.0028209647,0.000285303,0.0052949134,0.00019049672],"about_ca_topic_score_codex":0.0126297595,"about_ca_topic_score_gemma":0.2524052,"teacher_disagreement_score":0.23977543,"about_ca_system_score_codex":0.0000039051106,"about_ca_system_score_gemma":0.0002867547,"threshold_uncertainty_score":0.99531883},"labels":[],"label_agreement":null},{"id":"W2331885488","doi":"10.1139/cjes-2012-0040","title":"Hydrocarbon fluid inclusions in the Argo salt, offshore Canadian Atlantic margin","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Fluid inclusions; Geology; Petroleum; Eutectic system; Mineralogy; Geochemistry; Salt dome; Quartz; Chemistry; Crystallography; Microstructure","score_opus":0.01362934198924304,"score_gpt":0.2082422692548761,"score_spread":0.19461292726563306,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2331885488","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9806089,0.0007684046,0.000039302577,0.0049681505,0.000287413,0.000106893895,0.0000030167262,0.0000066907496,0.013211264],"genre_scores_gemma":[0.99914014,0.00007248022,0.00008937261,0.00052452565,0.00010128949,0.000003057063,0.0000018060833,0.000007144791,0.00006020055],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987538,0.000068917674,0.00032219244,0.00009638934,0.00028669523,0.000472003],"domain_scores_gemma":[0.9989512,0.000047182024,0.000046108125,0.00013853873,0.000060911967,0.00075608765],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066578726,0.000109868015,0.00016893589,0.0009872696,0.00031152193,0.00022621146,0.0006246102,0.00005628062,0.0004338595],"category_scores_gemma":[0.00008389435,0.0000732513,0.00007778818,0.0011886416,0.00017448049,0.00035135268,0.0000070339097,0.0002567449,0.0000673439],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002564754,0.000025876903,0.43886262,0.000042046304,0.0001302066,0.00089441973,0.013847184,0.5150677,0.0017662647,0.0018319278,0.024723347,0.0028058102],"study_design_scores_gemma":[0.00061077275,0.00024942757,0.3247385,0.00028312232,0.00006620867,0.00040771515,0.008597451,0.5607299,0.00034861494,0.0028275875,0.100316346,0.000824296],"about_ca_topic_score_codex":0.4016043,"about_ca_topic_score_gemma":0.98642117,"teacher_disagreement_score":0.5848169,"about_ca_system_score_codex":0.000033656906,"about_ca_system_score_gemma":0.001225829,"threshold_uncertainty_score":0.6023805},"labels":[],"label_agreement":null},{"id":"W2332749167","doi":"10.1139/e2012-003","title":"Discussion of “New zircon shock phenomena and their use for dating and reconstruction of large impact structures revealed by electron nanobeam (EBSD, CL, EDS) and isotopic U–Pb and (U–Th)/He analysis of the Vredefort dome”<sup>1</sup>Appears in Canadian Journal of Earth Sciences, 2011, <b>48</b>(2): 117–139 [doi: dx.doi.org/10.1139/e11-011].","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Pegmatite; Impact structure; Geology; Spodumene; Zircon; Geochemistry; Breccia; Baddeleyite; Gneiss; Mineralogy; Metamorphic rock; Chemistry; Ceramic","score_opus":0.013750943592925394,"score_gpt":0.2210062316433541,"score_spread":0.2072552880504287,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2332749167","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931036,0.0060498924,0.000015581569,0.00033813625,0.000077672754,0.0001394555,0.00018876066,8.4394935e-7,0.00008603444],"genre_scores_gemma":[0.998854,0.00033145677,0.0006058467,0.00004092722,0.0000625644,2.1482037e-7,0.000006867745,0.0000022588802,0.00009586288],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99786836,0.00015915495,0.0007499666,0.00024332464,0.00033943672,0.0006397703],"domain_scores_gemma":[0.9977938,0.00020649983,0.0007800469,0.00011539323,0.00018362323,0.0009206246],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022378261,0.0001966622,0.00064536737,0.00082985475,0.0004343336,0.00011368858,0.00032780523,0.00009983765,0.0008792697],"category_scores_gemma":[0.0004184219,0.00009924076,0.00016022235,0.0011125682,0.0012709562,0.0007933253,0.000020476578,0.00024472905,2.1140346e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030497447,0.0000067384167,0.9913548,0.0000206925,0.00010171612,8.1797026e-7,0.0006739375,0.00074226945,0.0015508522,0.000025060428,0.00006544815,0.0054271375],"study_design_scores_gemma":[0.00045644783,0.0006532749,0.990114,0.00010033214,0.000214934,0.00008019627,0.0017289774,0.003176194,0.001486398,0.0011777316,0.00064643106,0.00016509567],"about_ca_topic_score_codex":0.13932876,"about_ca_topic_score_gemma":0.57204705,"teacher_disagreement_score":0.4327183,"about_ca_system_score_codex":0.000007955842,"about_ca_system_score_gemma":0.0010574897,"threshold_uncertainty_score":0.96273863},"labels":[],"label_agreement":null},{"id":"W2332995183","doi":"10.1139/cjes-2015-0215","title":"An overview of Chinese Silurian acritarch research","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Acritarch; Paleontology; Geology; Ordovician; China; Taxon; Archaeology; History","score_opus":0.11399624090069986,"score_gpt":0.351108168597301,"score_spread":0.2371119276966011,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2332995183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96669114,0.015466522,0.000011098049,0.0009594516,0.00034999984,0.00004848113,0.000045155433,0.0000021123537,0.016426032],"genre_scores_gemma":[0.9988592,0.00022344371,0.00073798996,0.000029151186,0.0001229118,9.039423e-8,2.7468622e-7,5.2170833e-7,0.000026377744],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99819964,0.00031651964,0.0003316947,0.00016239937,0.00047518715,0.0005145624],"domain_scores_gemma":[0.9983007,0.000370141,0.00013823347,0.00015338683,0.00024703244,0.0007905561],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0032660544,0.00008681979,0.00021014323,0.00064684806,0.00045082977,0.000063400286,0.00081843097,0.000065332395,0.0012408728],"category_scores_gemma":[0.00032752132,0.000047105405,0.000084480336,0.00077926466,0.0018671119,0.00078256556,9.262887e-7,0.00017524404,0.000014272767],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009961345,0.0000043264645,0.9447573,0.000005488522,0.000007101761,0.00004943928,0.00031374226,0.000012014149,0.0002598005,0.00047434785,0.000038701317,0.05406782],"study_design_scores_gemma":[0.00014455999,0.0008267472,0.9901654,0.000072511764,0.0000025428985,0.0000952974,0.00016550609,0.000035013243,0.00011916353,0.0073900344,0.0009122466,0.000070976865],"about_ca_topic_score_codex":0.013947691,"about_ca_topic_score_gemma":0.6505331,"teacher_disagreement_score":0.6365854,"about_ca_system_score_codex":9.065785e-7,"about_ca_system_score_gemma":0.001836629,"threshold_uncertainty_score":0.9996721},"labels":[],"label_agreement":null},{"id":"W2333617463","doi":"10.1139/e11-063","title":"An unusual stone circle, Chilcotin Range, British Columbia, Canada","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Island Health","funders":"","keywords":"Geology; Deglaciation; Lithology; Glacial period; Geomorphology; Glacier; Ice sheet; Meltwater; Outcrop; Moraine; Paleontology; Ice shelf; Cryosphere; Oceanography; Sea ice","score_opus":0.023304636996220828,"score_gpt":0.2121391492411773,"score_spread":0.18883451224495648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2333617463","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98331994,0.0011060587,0.000003993835,0.000172094,0.0008158533,0.00006447575,0.000056051904,0.0000038392195,0.01445768],"genre_scores_gemma":[0.9986748,0.000023311102,0.00044109745,0.00042279036,0.00009520694,1.5886039e-7,0.0000050728195,0.0000019251338,0.00033564947],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99826545,0.0001992178,0.00029696577,0.0002074327,0.00033574956,0.0006951721],"domain_scores_gemma":[0.99830973,0.00008964838,0.00014401675,0.00011845416,0.00015510965,0.0011830609],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011695056,0.00007557031,0.00021797561,0.0001565536,0.0008322545,0.00022039388,0.00076684257,0.000082583334,0.009934387],"category_scores_gemma":[0.00013430382,0.00009587993,0.000044677698,0.00045462366,0.0010814968,0.0004367784,0.0000036616307,0.00031960022,0.00003660222],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000044282033,0.0000047644257,0.9964299,0.0000028802565,0.000009599583,0.0008275199,0.00015218768,0.000058489437,4.5278097e-7,0.0000061028604,0.00045872608,0.0020449182],"study_design_scores_gemma":[0.00017942328,0.00038690126,0.995624,0.000018549852,0.0000072402204,0.001690859,0.0004266547,0.00009163396,0.000009076564,0.00030686476,0.0011372513,0.00012151448],"about_ca_topic_score_codex":0.9946643,"about_ca_topic_score_gemma":0.9999953,"teacher_disagreement_score":0.0153548345,"about_ca_system_score_codex":8.9526014e-7,"about_ca_system_score_gemma":0.0066998196,"threshold_uncertainty_score":0.9989313},"labels":[],"label_agreement":null},{"id":"W2333884617","doi":"10.1139/e11-007","title":"Imaging the Nechako Basin, British Columbia, using ambient seismic noise<sup>1</sup>This article is one of a series of papers published in this Special Issue on the theme of <i>New insights in Cordilleran Intermontane geoscience: reducing exploration risk in the mountain pine beetle-affected area, British Columbia</i>.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Manitoba; University of Alberta","funders":"British Geological Survey; National Research Council Canada; University of Manitoba","keywords":"Geology; Seismic noise; Seismology; Structural basin; Volcano; Microseism; Passive seismic; Rayleigh wave; Ambient noise level; Outcrop; Sedimentary basin; Lithosphere; Surface wave; Sedimentary rock; Mantle (geology); Geophysics; Tectonics; Geomorphology; Paleontology","score_opus":0.019912696031034766,"score_gpt":0.18947611572917164,"score_spread":0.16956341969813687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2333884617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99677336,0.0004002338,0.0000072909797,0.00094441423,0.0001802698,0.000269648,0.00008791512,0.0000018837572,0.0013349607],"genre_scores_gemma":[0.9987162,0.0002124076,0.00018662582,0.0006001412,0.00014315997,7.0997896e-7,0.0000035602282,0.0000041230605,0.0001330996],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997328,0.00041727282,0.0008755248,0.0002927105,0.0006515235,0.00043500742],"domain_scores_gemma":[0.99856275,0.00020129968,0.00065211306,0.00022786364,0.00017979465,0.00017619091],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0025806688,0.00011555345,0.00042667935,0.00029836892,0.0004237473,0.0007649952,0.00084637525,0.00005160474,0.0076135146],"category_scores_gemma":[0.00051399355,0.000105821084,0.00012338719,0.0023387182,0.0011118249,0.0011005418,0.000018168776,0.00035655094,0.0000010821049],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004297311,0.00008420986,0.93747777,0.000017808983,0.000030544674,0.00015277782,0.028193869,0.0124930935,0.000316356,0.000005589601,0.0018935907,0.019291416],"study_design_scores_gemma":[0.00049320195,0.00045562533,0.9164631,0.00074415875,0.000036238092,0.00013112096,0.026775233,0.05282881,0.00020424426,0.0011776298,0.000515635,0.00017503675],"about_ca_topic_score_codex":0.95764935,"about_ca_topic_score_gemma":0.98266715,"teacher_disagreement_score":0.04033572,"about_ca_system_score_codex":0.000019055868,"about_ca_system_score_gemma":0.00084846746,"threshold_uncertainty_score":0.99329364},"labels":[],"label_agreement":null},{"id":"W2334020599","doi":"10.1139/cjes-2013-0212","title":"A constrained potential field data interpretation of the deep geometry of the Sudbury structure","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"","keywords":"Geology; Seismology; Basement; Basalt; Borehole; Fold (higher-order function); Igneous rock; Petrology; Geochemistry; Paleontology","score_opus":0.009656393745717974,"score_gpt":0.19039156330016516,"score_spread":0.18073516955444718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2334020599","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964531,0.00023869275,0.0002165239,0.0016318725,0.00032771792,0.00002850888,0.00006165113,5.5662315e-7,0.0010413886],"genre_scores_gemma":[0.99928075,0.0000035117346,0.00031547557,0.000336007,0.000048750764,1.0613352e-8,0.0000027038168,3.3998143e-7,0.000012475532],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99913955,0.00008931856,0.0002552635,0.000097796656,0.00026494823,0.00015313216],"domain_scores_gemma":[0.9991576,0.00015861039,0.00027388424,0.00018113636,0.000091274655,0.00013747474],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004919458,0.000054187552,0.0001381997,0.00008633918,0.00015105493,0.000030233461,0.0011376383,0.00003834304,0.0026633572],"category_scores_gemma":[0.0008067536,0.000023889253,0.000089736124,0.0005521408,0.0007202932,0.00013359392,0.000022220222,0.00014249783,0.0000010698695],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007457669,0.0000023477744,0.97197574,0.000007318099,0.00001932858,0.0000014345962,0.000099632496,0.010435369,0.00034440702,0.000089786576,0.00006896961,0.016948232],"study_design_scores_gemma":[0.0000899057,0.00014388876,0.94887966,0.000038175447,0.00004277797,0.00004177962,0.00023627712,0.041329626,0.0016138196,0.007170723,0.00035540856,0.00005797601],"about_ca_topic_score_codex":0.012895749,"about_ca_topic_score_gemma":0.32479247,"teacher_disagreement_score":0.3118967,"about_ca_system_score_codex":3.6744945e-7,"about_ca_system_score_gemma":0.00027706052,"threshold_uncertainty_score":0.99824834},"labels":[],"label_agreement":null},{"id":"W2334422452","doi":"10.1139/cjes-2012-0057","title":"A reexamination of Pleistocene tunnel valley distribution on the central Scotian Shelf","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Saint Mary's University","funders":"","keywords":"Geology; Canyon; Meltwater; Meander (mathematics); Geomorphology; Channel (broadcasting); Pleistocene; Continental shelf; Oceanography; Paleontology; Glacial period; Geometry","score_opus":0.026101124986476047,"score_gpt":0.21835692023708456,"score_spread":0.1922557952506085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2334422452","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911551,0.0002731381,0.000019079393,0.004290176,0.0003830025,0.00010861952,0.000024732428,0.0000015553177,0.0037445945],"genre_scores_gemma":[0.99960613,0.00001816682,0.0000652292,0.00015052187,0.000050130417,2.8612612e-7,0.000008514661,7.2685185e-7,0.00010027345],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987865,0.00018476091,0.00024063143,0.00010571079,0.0002658989,0.0004164764],"domain_scores_gemma":[0.99893,0.00031069238,0.00016580707,0.00008945365,0.00016245892,0.00034163968],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010615567,0.000070370304,0.00012844389,0.00016118621,0.00042922463,0.00006304079,0.00043920832,0.00005913108,0.0036412294],"category_scores_gemma":[0.00040957186,0.000042214997,0.000053130625,0.00035724294,0.0010199274,0.00025097685,0.0000030485996,0.00020575544,0.000110542125],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005383776,0.0000034870359,0.9970767,0.0000030780202,0.0000062340855,0.000010118592,0.00012884983,0.0007175535,0.0000048963216,0.0009563995,0.00041745548,0.00066982745],"study_design_scores_gemma":[0.00008421356,0.00042860856,0.99593556,0.000027679585,0.000004212585,0.00008149166,0.00029826045,0.0011302483,0.000074728196,0.001524482,0.00036312517,0.000047418605],"about_ca_topic_score_codex":0.013243373,"about_ca_topic_score_gemma":0.35935915,"teacher_disagreement_score":0.34611577,"about_ca_system_score_codex":8.668606e-7,"about_ca_system_score_gemma":0.00077837374,"threshold_uncertainty_score":0.9972696},"labels":[],"label_agreement":null},{"id":"W2334445825","doi":"10.1139/cjes-2012-0163","title":"Sedimentary and metamorphic lithofacies of the Lower Negaunee Iron Formation, Marquette District, Michigan, USA","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Siderite; Geochemistry; Banded iron formation; Clastic rock; Metamorphic rock; Diagenesis; Greenschist; Archean; Sedimentary rock; Pyrite","score_opus":0.008913833745926861,"score_gpt":0.16861495160697035,"score_spread":0.1597011178610435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2334445825","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99537975,0.00076446397,0.000005433893,0.0022918608,0.00019323581,0.000055076845,0.00006889326,8.494018e-7,0.0012404373],"genre_scores_gemma":[0.99917006,0.000032118318,0.00020297151,0.00035532334,0.00003584118,1.6660101e-7,0.000005013263,5.55728e-7,0.000197917],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99908984,0.00004146338,0.00028860205,0.000091316935,0.00025570774,0.00023308519],"domain_scores_gemma":[0.99928117,0.000051465846,0.00022143363,0.00008390382,0.00007224316,0.0002897805],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035923815,0.00008328807,0.00013256709,0.00010794506,0.0003646995,0.000121201985,0.0003294602,0.000024090145,0.0044766567],"category_scores_gemma":[0.000048732112,0.000048807222,0.00007608869,0.00041221493,0.0005192854,0.0006752631,0.00000787698,0.00009570702,0.000018202174],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000017245603,0.000003810488,0.99682236,0.000012962211,0.0000147376395,0.000003510609,0.000181238,0.00056256726,0.00035040546,0.000008505999,0.000715137,0.0013230486],"study_design_scores_gemma":[0.00009701439,0.00011904381,0.9933821,0.000028672357,0.000036607464,0.000086609994,0.0008380988,0.0005166529,0.0018576739,0.00047289097,0.0024820142,0.00008264344],"about_ca_topic_score_codex":0.028787987,"about_ca_topic_score_gemma":0.21963689,"teacher_disagreement_score":0.1908489,"about_ca_system_score_codex":0.0000010756153,"about_ca_system_score_gemma":0.00024290822,"threshold_uncertainty_score":0.9964334},"labels":[],"label_agreement":null},{"id":"W2335465793","doi":"10.1139/e2012-002","title":"Factors influencing permafrost temperatures across tree line in the uplands east of the Mackenzie Delta, 2004–2010<sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of <i>Fundamental and applied research on permafrost in Canada</i>.<sup>2</sup>Polar Continental Shelf Contribution 03611.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University; Aboriginal Affairs Northern Dev Canada","funders":"","keywords":"Tundra; Subarctic climate; Permafrost; Tree line; Taiga; Snow; Physical geography; Vegetation (pathology); Geology; Boreal; Shrub; Delta; Snow line; Plateau (mathematics); Growing season; Arctic; Environmental science; Climatology; Climate change; Snow cover; Geomorphology; Oceanography; Geography; Ecology; Forestry","score_opus":0.04443563474611053,"score_gpt":0.25359824336009335,"score_spread":0.2091626086139828,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2335465793","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9860841,0.0006971149,1.3017266e-8,0.0021562504,0.00015896338,0.0003178034,0.009895925,7.721814e-7,0.0006890428],"genre_scores_gemma":[0.99918437,0.00006936347,0.0000029270723,0.00037286556,0.00023843916,0.0000014339497,0.00010780071,0.0000044892327,0.0000183364],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99698395,0.00033932168,0.000760134,0.00020620458,0.0009821376,0.00072825205],"domain_scores_gemma":[0.99840647,0.00060208765,0.0003540354,0.00021650137,0.00016978502,0.00025113384],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.003074441,0.0002021781,0.0004542665,0.00035438876,0.00037935073,0.000138545,0.00071122486,0.00008864465,0.0039046376],"category_scores_gemma":[0.00035172456,0.00010914563,0.00008221637,0.001125939,0.0013545293,0.00053526927,0.00003071047,0.00059054466,0.0000014301203],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001786205,0.00004007239,0.96120894,0.000023109968,0.000013248889,0.0000058694695,0.035003036,0.00089216017,0.0018180148,0.000050598093,0.00065249676,0.00011382902],"study_design_scores_gemma":[0.00063400785,0.00030923213,0.9135484,0.0002266437,0.000008969219,0.00001894926,0.07698659,0.00035127052,0.007041079,0.000018160737,0.0007408601,0.000115827155],"about_ca_topic_score_codex":0.66298306,"about_ca_topic_score_gemma":0.98571247,"teacher_disagreement_score":0.32272938,"about_ca_system_score_codex":0.000040942574,"about_ca_system_score_gemma":0.0011475311,"threshold_uncertainty_score":0.99700594},"labels":[],"label_agreement":null},{"id":"W2335823011","doi":"10.1139/cjes-2016-0011","title":"Southern continuation of the Wakeham Group and Robe-Noire mafic suite (eastern Grenville Province) from hydrocarbon-targeted seismic reflection data on Anticosti Island, Quebec, Canada","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Mafic; Geology; Sill; Paleozoic; Metallogeny; Basement; Geochemistry; Reflection (computer programming); Group (periodic table); Seismology; Paleontology; Archaeology; Geography","score_opus":0.015089020245666305,"score_gpt":0.18080337488597611,"score_spread":0.1657143546403098,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2335823011","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995693,0.00056414347,0.000022862641,0.0027366064,0.0002675989,0.000066382396,0.00033406945,0.0000016796533,0.00031360675],"genre_scores_gemma":[0.99930155,0.000014017646,0.00003674051,0.00022077492,0.00008302285,7.7970874e-8,0.000018437393,0.0000013299883,0.0003240414],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987277,0.000108583,0.00029325584,0.00023823927,0.00036594225,0.00026629108],"domain_scores_gemma":[0.9990205,0.00017242826,0.0002887363,0.0001830301,0.000051674466,0.00028363033],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040819598,0.000111468034,0.00020239921,0.00008822694,0.00024340878,0.000065345965,0.00054075907,0.0000447531,0.0008472489],"category_scores_gemma":[0.00020248991,0.00005168721,0.000043915326,0.00027428666,0.00038476702,0.00019177982,0.0000163282,0.0001125541,0.000006675398],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019070458,0.0000028449917,0.98404235,0.0000026379212,0.000016800888,0.000010361381,0.00005235427,0.00038530407,0.00050698564,0.0000035918538,0.000146081,0.014811611],"study_design_scores_gemma":[0.00036225634,0.00027502826,0.9841965,0.00013193279,0.000051190313,0.000015311109,0.00021938814,0.009644058,0.00056392676,0.0010710516,0.003310325,0.00015905975],"about_ca_topic_score_codex":0.9572277,"about_ca_topic_score_gemma":0.9997519,"teacher_disagreement_score":0.0425242,"about_ca_system_score_codex":0.000005208982,"about_ca_system_score_gemma":0.0008030211,"threshold_uncertainty_score":0.9276781},"labels":[],"label_agreement":null},{"id":"W2336361093","doi":"10.1139/cjes-2015-0244","title":"An unusual sponge – microbe – synsedimentary cement framework in a Late Ordovician reef, Southampton Island (Nunavut, Canada)","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec); University of Ottawa","funders":"Natural Resources Canada","keywords":"Ordovician; Subaerial; Geology; Reef; Paleontology; Facies; Devonian; Sponge; Aragonite; Calcite; Geochemistry; Oceanography; Structural basin","score_opus":0.01360374853426304,"score_gpt":0.2155389457714879,"score_spread":0.20193519723722486,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2336361093","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9885239,0.002454395,0.00006011366,0.0016628837,0.00083314115,0.00007846001,0.00015757873,0.000003150114,0.006226357],"genre_scores_gemma":[0.99862814,0.000033704728,0.0006909827,0.00047713186,0.00013082597,2.2423177e-7,0.0000013583716,0.0000010960916,0.00003654473],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99814653,0.00015005526,0.0004078764,0.00025059193,0.0003707762,0.0006741498],"domain_scores_gemma":[0.9985636,0.00018908046,0.00020522306,0.00013984783,0.000054309996,0.00084796915],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00097417197,0.00015925075,0.00024270243,0.0004306427,0.00042350168,0.00009246928,0.00059202994,0.0000978759,0.00091624673],"category_scores_gemma":[0.000076063785,0.000105529245,0.00005729657,0.00045413908,0.0005640556,0.00051771116,0.0000012297904,0.00023655122,0.0000055158253],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025467836,0.000005395103,0.98351586,0.0000023471634,0.000012816357,0.00052775687,0.0004628278,0.00014029087,0.000056553064,0.00006185287,0.00010760481,0.015081237],"study_design_scores_gemma":[0.00026993704,0.00044392922,0.99592465,0.00014012613,0.000008350165,0.00009584207,0.0004241372,0.000116496376,0.0000848139,0.0012150164,0.0011022801,0.00017444014],"about_ca_topic_score_codex":0.6685296,"about_ca_topic_score_gemma":0.9997881,"teacher_disagreement_score":0.33125848,"about_ca_system_score_codex":0.00000789081,"about_ca_system_score_gemma":0.004122469,"threshold_uncertainty_score":0.9999971},"labels":[],"label_agreement":null},{"id":"W2336479949","doi":"10.1139/e2012-015","title":"Geomorphology of a thermo-erosion gully, Bylot Island, Nunavut, Canada<sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of <i>Fundamental and applied research on permafrost in Canada</i>.<sup>2</sup>Polar Continental Shelf Project Contribution 043-11.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Center for Northern Studies; HEC Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Gully erosion; Sinkhole; Erosion; Geomorphology; Hydrology (agriculture); Channel (broadcasting); Glacier; Bedrock; Karst; Physical geography; Paleontology; Geography; Geotechnical engineering","score_opus":0.037018018182135085,"score_gpt":0.24126704261650125,"score_spread":0.20424902443436616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2336479949","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9882136,0.000496302,3.888238e-8,0.0019523653,0.00015583458,0.0003596831,0.006317869,7.1240584e-7,0.002503613],"genre_scores_gemma":[0.9991669,0.0001118457,0.000009220737,0.00034799852,0.0002177586,0.0000015550817,0.000097547694,0.0000047236035,0.000042445674],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971104,0.00030457746,0.000731291,0.00022637217,0.0009058068,0.00072152005],"domain_scores_gemma":[0.998431,0.0005029665,0.0003878639,0.00017065412,0.00019733065,0.00031015152],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0023562538,0.00017953166,0.0005187275,0.00046723787,0.00022624395,0.000055131604,0.00044871832,0.00008301608,0.016641228],"category_scores_gemma":[0.00023243763,0.00012502194,0.000056160996,0.00081348995,0.0011080266,0.00035507052,0.000024493702,0.0003507446,0.0000022882143],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031622435,0.000045775058,0.9847919,0.00003187537,0.000017236787,0.00001923766,0.0071304217,0.00031622435,0.003145195,0.00010328042,0.0039060994,0.0001765696],"study_design_scores_gemma":[0.0012627513,0.0010595694,0.9441795,0.00030064062,0.0000193028,0.000075210824,0.03239392,0.0007097141,0.013204685,0.000038524387,0.006541409,0.00021481495],"about_ca_topic_score_codex":0.9911366,"about_ca_topic_score_gemma":0.9997668,"teacher_disagreement_score":0.040612403,"about_ca_system_score_codex":0.000060227205,"about_ca_system_score_gemma":0.0037081032,"threshold_uncertainty_score":0.9842577},"labels":[],"label_agreement":null},{"id":"W2337116877","doi":"10.1139/cjes-2015-0160","title":"Paleoclimate and precipitation seasonality of the Early Eocene McAbee megaflora, Kamloops Group, British Columbia","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; Brandon University","funders":"Natural Sciences and Engineering Research Council of Canada; National Geographic Society","keywords":"Geology; Paleoclimatology; Monsoon; Seasonality; Physical geography; Climate change; Outcrop; Cenozoic; Precipitation; Population; Paleontology; Climatology; Geography; Ecology; Structural basin; Oceanography","score_opus":0.017524283876328362,"score_gpt":0.17086629852597668,"score_spread":0.1533420146496483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2337116877","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99808764,0.0002258009,0.0000014858045,0.001064888,0.00018681523,0.000045277193,0.00015385447,0.0000018074978,0.00023243632],"genre_scores_gemma":[0.9996438,0.00005886043,0.000047229383,0.00005360839,0.0000548818,1.6858864e-7,7.0856447e-7,1.6382418e-7,0.00014060554],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99931014,0.00007359849,0.00014023964,0.00009495288,0.00019997309,0.0001811191],"domain_scores_gemma":[0.9994178,0.00010187112,0.00016236698,0.000018586194,0.00010411015,0.00019530987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058884895,0.000036119138,0.00009050383,0.0000067783662,0.00046381736,0.00016825003,0.0002424974,0.00003508936,0.00019416778],"category_scores_gemma":[0.00013037864,0.000015687712,0.000047786605,0.00023293024,0.00044277645,0.00039402058,0.000015763895,0.00004530731,0.0000018074373],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000027003564,0.0000039231068,0.9855885,0.0000018911031,0.0000034325433,0.0000035907537,0.00004182127,7.483461e-7,0.004438353,0.000045674624,0.0002888181,0.00958056],"study_design_scores_gemma":[0.000078052966,0.00014360818,0.9969594,0.00009409156,0.0000068333434,0.000045048473,0.00010329167,0.0000041019666,0.000073578674,0.0009715797,0.0014743354,0.000046080993],"about_ca_topic_score_codex":0.061854966,"about_ca_topic_score_gemma":0.8975392,"teacher_disagreement_score":0.83568424,"about_ca_system_score_codex":0.000004420397,"about_ca_system_score_gemma":0.000079262056,"threshold_uncertainty_score":0.9443922},"labels":[],"label_agreement":null},{"id":"W2338230958","doi":"10.1139/e11-024","title":"The Dog Bay – Liberty Line and its significance for Silurian tectonics of the northern Appalachian orogen<sup>1</sup>This article is one of a series of papers published in this <i>CJES Special Issue: In honour of Ward Neale</i> on the theme of Appalachian and Grenvillian geology.<sup>2</sup>Geological Survey of Canada Contribution 20100257.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Forearc; Terrane; Subduction; Paleontology; Lithosphere; Volcanic arc; Ordovician; Passive margin; Seismology; Trough (economics); Rift; Tectonics","score_opus":0.013708990824906531,"score_gpt":0.18409594945266144,"score_spread":0.1703869586277549,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2338230958","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915833,0.0015710247,8.53518e-7,0.0057572257,0.00006587808,0.00026234414,0.00035935745,7.48698e-7,0.00039930205],"genre_scores_gemma":[0.99950516,0.00016949062,0.00006355454,0.00013410031,0.000060931867,0.0000012852242,0.0000057525704,0.0000020083305,0.000057737936],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975169,0.00045455477,0.00090149464,0.00020160222,0.00043258478,0.00049286656],"domain_scores_gemma":[0.997261,0.001152448,0.0007620976,0.00017849781,0.00037242493,0.0002735236],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0032704026,0.00016520452,0.0006190264,0.00012605867,0.00021343284,0.000020000418,0.0005964833,0.0001123908,0.0015279845],"category_scores_gemma":[0.0019480076,0.00008080841,0.00011442586,0.000889302,0.0018624194,0.00019179014,0.000029504019,0.0002756864,3.2349436e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014508303,0.000039122948,0.99368775,0.000031405965,0.000043831024,0.0000010222136,0.0011026985,0.0035039275,0.00024202884,0.00014689993,0.000071625,0.0009845997],"study_design_scores_gemma":[0.0004083669,0.0005473685,0.9865462,0.000076397075,0.00003528318,0.000008647245,0.0012137591,0.0038854403,0.00579821,0.00075947266,0.0006117667,0.00010905016],"about_ca_topic_score_codex":0.3401555,"about_ca_topic_score_gemma":0.955072,"teacher_disagreement_score":0.61491644,"about_ca_system_score_codex":0.000006407198,"about_ca_system_score_gemma":0.0008200125,"threshold_uncertainty_score":0.99938476},"labels":[],"label_agreement":null},{"id":"W2338263796","doi":"10.1139/e2012-018","title":"Degradation of permafrost beneath a road embankment enhanced by heat advected in groundwater<sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of <i>Fundamental and applied research on permafrost in Canada</i>.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":117,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université de Montréal; Université Laval; Center for Northern Studies; HEC Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Transport Canada","keywords":"Permafrost; Geology; Groundwater; Levee; Geotechnical engineering; Water table; Groundwater flow; Hydrology (agriculture); Geomorphology; Aquifer; Oceanography","score_opus":0.04187096089558434,"score_gpt":0.2436831660029281,"score_spread":0.20181220510734377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2338263796","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99235255,0.00043787292,4.4313143e-8,0.0012025961,0.00010765016,0.00023418652,0.0015107954,5.234354e-7,0.0041537955],"genre_scores_gemma":[0.99944675,0.00016323649,0.000015541622,0.00016281367,0.000095266245,0.0000016101328,0.000058352052,0.000003284663,0.00005317116],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99760795,0.00018918686,0.0006520344,0.00018361353,0.00084655226,0.00052066956],"domain_scores_gemma":[0.99901116,0.00025804315,0.00021782618,0.00013475152,0.00012509723,0.00025310772],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001902788,0.00013620958,0.00037673392,0.0005524801,0.00012890682,0.00005435336,0.00033381692,0.000054102322,0.011451478],"category_scores_gemma":[0.00011430533,0.00009666888,0.000037832655,0.0009898309,0.0006476357,0.00048495055,0.000014327704,0.0002537028,0.0000019530069],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021508285,0.00007302907,0.9633387,0.000037538175,0.000010670011,0.0000036870372,0.016244952,0.00043208172,0.017811222,0.000048845217,0.00063684245,0.0011474048],"study_design_scores_gemma":[0.00056954066,0.00068494695,0.92810816,0.00026291658,0.0000058935993,0.0000066051775,0.02166291,0.00030844755,0.04762448,0.000028058545,0.00061749393,0.00012055803],"about_ca_topic_score_codex":0.82738477,"about_ca_topic_score_gemma":0.9892711,"teacher_disagreement_score":0.16188633,"about_ca_system_score_codex":0.000048817707,"about_ca_system_score_gemma":0.0011662103,"threshold_uncertainty_score":0.9894522},"labels":[],"label_agreement":null},{"id":"W2338287126","doi":"10.1139/e2012-072","title":"Detrital zircon geochronology and polycyclic sediment sources, Upper Jurassic – Lower Cretaceous of the Scotian Basin, southeastern Canada <sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of <i>Mesozoic–Cenozoic geology of the Scotian Basin</i>.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Saint Mary's University; Bedford Institute of Oceanography","funders":"Offshore Energy Research Association","keywords":"Zircon; Geology; Geochronology; Provenance; Terrane; Paleozoic; Cretaceous; Paleontology; Rift; Structural basin; Detritus; Sediment; Source rock; Geochemistry; Tectonics","score_opus":0.00832213811564098,"score_gpt":0.1670289137026846,"score_spread":0.15870677558704363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2338287126","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9846405,0.0014334919,3.6993615e-7,0.010652764,0.00035170215,0.0001340819,0.00010171742,8.6930703e-7,0.002684538],"genre_scores_gemma":[0.99893206,0.000027031178,0.00006824878,0.0006254703,0.00016578853,3.0550103e-7,0.0000011233992,0.0000025368283,0.00017743609],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99759257,0.0003088622,0.0007543474,0.00020487326,0.00059178675,0.00054757285],"domain_scores_gemma":[0.9982392,0.00036224123,0.00069465855,0.00027096536,0.00013332255,0.00029961183],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009780605,0.00017800629,0.00055972213,0.00021038676,0.00018610466,0.000026090804,0.0008120819,0.00010183311,0.017483583],"category_scores_gemma":[0.00047018356,0.0000881543,0.00018961217,0.00086656015,0.0030158919,0.00022718195,0.000046214012,0.00028156556,0.0000026221544],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052830765,0.000040243547,0.99523836,0.000019700532,0.000054917553,0.0000026898138,0.0019470537,0.0004309968,0.0009474559,0.000050926395,0.0003107697,0.00090404454],"study_design_scores_gemma":[0.00034108284,0.00056529866,0.95892113,0.00014053272,0.00008305743,0.00004743416,0.0042104255,0.0002064579,0.03100826,0.00054576364,0.0037855394,0.00014501074],"about_ca_topic_score_codex":0.49335623,"about_ca_topic_score_gemma":0.87693715,"teacher_disagreement_score":0.38358095,"about_ca_system_score_codex":0.0000067367355,"about_ca_system_score_gemma":0.0010276464,"threshold_uncertainty_score":0.9996973},"labels":[],"label_agreement":null},{"id":"W2338737908","doi":"10.1139/cjes-2015-0207","title":"Siltstone: a key to cyclicity in mixed siliciclastic–carbonate successions: example from Upper Ordovician Kope Formation (Ohio, Indiana, Kentucky)","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Siltstone; Siliciclastic; Geology; Silt; Ordovician; Sedimentary depositional environment; Carbonate; Paleontology; Lithology; Geochemistry; Sedimentary rock; Facies","score_opus":0.022759044285679916,"score_gpt":0.22511684171208063,"score_spread":0.2023577974264007,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2338737908","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9815073,0.0013142191,0.00012856188,0.0017522592,0.00071562116,0.00012955723,0.000083948915,0.000006176494,0.014362371],"genre_scores_gemma":[0.99818754,0.000038677015,0.0013119992,0.00033375446,0.00009328073,7.81106e-7,0.0000018896318,0.0000011229661,0.0000309284],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99801767,0.00018314598,0.0005553493,0.0002605182,0.00035163778,0.0006316978],"domain_scores_gemma":[0.9981241,0.00042264647,0.00025945087,0.00014455449,0.000083862935,0.00096538174],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009970637,0.0001608107,0.00028954414,0.0008883056,0.00042962952,0.00012881853,0.00063311326,0.0001102698,0.0007007753],"category_scores_gemma":[0.00040549645,0.00010429878,0.0000859281,0.0008450402,0.00043559255,0.0011370053,0.000002718479,0.00019389235,0.00004346249],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027073149,0.0000054247803,0.94838834,0.0000018009198,0.0000080442105,0.00007671883,0.0008306344,0.00015081388,0.0002463242,0.00008873387,0.00009957217,0.05007652],"study_design_scores_gemma":[0.0003621305,0.00024708503,0.9948095,0.00016923585,0.000007817476,0.000027763224,0.0004160827,0.0002596303,0.00022723713,0.0017153262,0.0015901559,0.0001680501],"about_ca_topic_score_codex":0.12686256,"about_ca_topic_score_gemma":0.9647042,"teacher_disagreement_score":0.8378417,"about_ca_system_score_codex":0.000006223801,"about_ca_system_score_gemma":0.0009079298,"threshold_uncertainty_score":0.8789517},"labels":[],"label_agreement":null},{"id":"W2338869545","doi":"10.1139/cjes-2015-0227","title":"Widespread Late Devonian marine anoxia in eastern North America: a case study of the Kettle Point Formation black shale, southwestern Ontario","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Western University","funders":"","keywords":"Geology; Oil shale; Devonian; Sedimentary depositional environment; Green River Formation; Deposition (geology); Anoxic waters; Sedimentary rock; Geochemistry; Lithology; Authigenic; Paleontology; Sediment; Structural basin; Oceanography","score_opus":0.02441889947658789,"score_gpt":0.21115922868030285,"score_spread":0.18674032920371494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2338869545","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962366,0.0001084646,0.000012361648,0.00024676975,0.00023645697,0.00013580853,0.00002138535,0.0000015553245,0.0030005523],"genre_scores_gemma":[0.99976003,0.0000032617131,0.00009053838,0.00004212736,0.000020047426,2.2710505e-7,2.7949906e-7,5.715754e-7,0.00008293218],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99876213,0.00013448305,0.00041892644,0.00013396658,0.00023132427,0.00031916547],"domain_scores_gemma":[0.999085,0.00009888696,0.00034611922,0.00012828798,0.000066260385,0.00027543164],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045502832,0.000105751635,0.00019600871,0.0002888867,0.00022773271,0.00005655363,0.00040058672,0.000034941662,0.0003271865],"category_scores_gemma":[0.00004984195,0.000056681285,0.00006542032,0.00042011368,0.0006089137,0.0006508814,0.0000033776212,0.00014748942,0.00000799035],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011741751,0.000010921559,0.9720521,0.0000024201252,0.000009398908,0.0005322933,0.007276717,0.00024273306,0.000003879548,9.876888e-7,0.0000043634445,0.019852418],"study_design_scores_gemma":[0.00038588003,0.00056013785,0.99475205,0.000052165517,0.000010280711,0.0006324859,0.0032143933,0.0001672282,0.000009018135,0.00008555164,0.00005013324,0.00008064791],"about_ca_topic_score_codex":0.48822954,"about_ca_topic_score_gemma":0.9993779,"teacher_disagreement_score":0.5111484,"about_ca_system_score_codex":0.0000042914285,"about_ca_system_score_gemma":0.00085385103,"threshold_uncertainty_score":0.5151784},"labels":[],"label_agreement":null},{"id":"W2339417835","doi":"10.1139/cjes-2016-0019","title":"Early magmatism in the greater Red Sea rift: timing and significance","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":149,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Rift; Dike; Magmatism; Mantle plume; Volcanism; Flood basalt; Paleontology; Plate tectonics; East African Rift; Lithosphere; Geochemistry; Seismology; Tectonics","score_opus":0.02369614935496591,"score_gpt":0.19114734293733007,"score_spread":0.16745119358236416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2339417835","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98870325,0.0003839841,0.0000130712715,0.007496291,0.000055665085,0.000030824132,0.000010471716,0.000001167622,0.0033052587],"genre_scores_gemma":[0.9991738,0.000023018927,0.00028456087,0.0003845514,0.00004696327,1.3164515e-7,2.767329e-7,4.3088224e-7,0.00008624828],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991346,0.000078565354,0.00018876669,0.00012111199,0.00019362257,0.00028335926],"domain_scores_gemma":[0.99939066,0.00017430223,0.000081767255,0.000057212335,0.000033288597,0.00026278695],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00079720106,0.000064939275,0.00011766935,0.00013624977,0.00017430047,0.00010149724,0.00032550708,0.000027130482,0.002263582],"category_scores_gemma":[0.00013095784,0.000026773954,0.00003797374,0.00034630537,0.00049508177,0.00024575266,0.0000028929985,0.00008843856,0.000027883138],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000030653164,7.9249907e-7,0.9918618,9.907186e-7,0.0000024343638,0.000056783458,0.00016248635,0.000041152365,0.000048081394,0.000041859064,0.000044965727,0.0077355807],"study_design_scores_gemma":[0.00008843167,0.00012999709,0.99177,0.00002666712,0.000005201423,0.000053383104,0.00009902631,0.00012037118,0.000060590348,0.006665522,0.000923877,0.000056876124],"about_ca_topic_score_codex":0.024780769,"about_ca_topic_score_gemma":0.34282625,"teacher_disagreement_score":0.31804547,"about_ca_system_score_codex":6.3117466e-7,"about_ca_system_score_gemma":0.0001316802,"threshold_uncertainty_score":0.99864846},"labels":[],"label_agreement":null},{"id":"W2339921190","doi":"10.1139/cjes-2015-0240","title":"U–Pb and Hf isotopic analyses of detrital zircons from the Taku terrane, southeast Alaska","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Terrane; Geology; Paleozoic; Permian; Volcanic rock; Carboniferous; Igneous rock; Geochemistry; Paleontology; Pluton; Zircon; Petrology; Volcano; Structural basin","score_opus":0.03696247031457689,"score_gpt":0.21958612713846049,"score_spread":0.1826236568238836,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2339921190","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920178,0.0022959656,0.00005828504,0.0036998917,0.00010933864,0.000026534064,0.00011909882,0.0000015767846,0.0016714969],"genre_scores_gemma":[0.9991086,0.000049644736,0.0005011235,0.00017858535,0.000099281926,6.326397e-8,0.0000013644377,5.9711465e-7,0.000060748465],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990179,0.00006663842,0.0002791797,0.0001415569,0.00023134108,0.00026337765],"domain_scores_gemma":[0.9988232,0.00042708882,0.00017110442,0.00008692962,0.00007767142,0.0004139564],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037325366,0.0000856957,0.00020511959,0.00012362865,0.0002278991,0.00006477344,0.0003972561,0.000036499474,0.0069647464],"category_scores_gemma":[0.00030050377,0.000035339086,0.00010401436,0.00038056364,0.0011492863,0.00018861286,0.0000070641827,0.00008315928,0.000022794702],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003424545,0.0000020029893,0.9939886,9.119679e-7,0.00002294232,0.000011746134,0.00008251311,0.000045089833,0.0012616152,0.000022923316,0.00006569001,0.004492595],"study_design_scores_gemma":[0.00014068723,0.00015630774,0.99079585,0.000037049875,0.000041193965,0.000031834057,0.000738021,0.00006470348,0.0017721914,0.005356434,0.0007876687,0.00007803285],"about_ca_topic_score_codex":0.040663444,"about_ca_topic_score_gemma":0.3254791,"teacher_disagreement_score":0.28481567,"about_ca_system_score_codex":5.4985134e-7,"about_ca_system_score_gemma":0.000252978,"threshold_uncertainty_score":0.99394304},"labels":[],"label_agreement":null},{"id":"W2340659794","doi":"10.1139/cjes-2015-0195","title":"Magnetic susceptibility mapping of the Sudbury area, Ontario, Canada: evaluating pollution distributions decades later","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor","funders":"Ontario Innovation Trust","keywords":"Magnetic susceptibility; Magnetic mineralogy; Geology; Magnetite; Environmental magnetism; Mineralogy; Greigite; In situ; Ferrimagnetism; Remanence; Magnetization; Pyrite; Chemistry; Magnetic field","score_opus":0.022265376323254052,"score_gpt":0.2324883343857343,"score_spread":0.21022295806248026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2340659794","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956282,0.0017163312,0.000066980305,0.0014619982,0.0003753744,0.00007197661,0.000075453885,5.7265135e-7,0.0006031234],"genre_scores_gemma":[0.9987959,0.00002214701,0.00024398194,0.00007661573,0.000060581326,9.3284274e-7,0.0000013105108,0.0000022585166,0.00079626567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99897444,0.00007550755,0.00028736025,0.00014625456,0.00022233844,0.00029407244],"domain_scores_gemma":[0.9992618,0.000025348232,0.00018276731,0.00015306455,0.00019973022,0.00017728792],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054795516,0.000089547204,0.00011939116,0.000052996456,0.0003492752,0.000021105889,0.00031397812,0.000044771026,0.00025243216],"category_scores_gemma":[0.00031535327,0.000051198902,0.000074297146,0.00016182187,0.0005969448,0.000011499115,0.000033311364,0.00006599173,5.0768193e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000516676,0.0000042807687,0.93441945,0.000004805047,0.000012008201,0.000003551851,0.00012912977,0.0000529185,0.061824724,0.00003409955,0.0012574082,0.0022524768],"study_design_scores_gemma":[0.0001721739,0.0003514733,0.9840604,0.00006397413,0.000014235037,0.00004019964,0.00016771292,0.000003473253,0.0071104984,0.00015415171,0.007781172,0.000080502876],"about_ca_topic_score_codex":0.6391596,"about_ca_topic_score_gemma":0.99854934,"teacher_disagreement_score":0.35938975,"about_ca_system_score_codex":0.000021964139,"about_ca_system_score_gemma":0.00500719,"threshold_uncertainty_score":0.888254},"labels":[],"label_agreement":null},{"id":"W2340828404","doi":"10.1139/e11-066","title":"A new depositional model for glaciogenic Neoproterozoic iron formation: insights from the chemostratigraphy and basin configuration of the Rapitan iron formation<sup>1</sup>Northwest Territories Geoscience Office Contribution 0052.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"","keywords":"Geology; Banded iron formation; Geochemistry; Structural basin; Water column; Sedimentary depositional environment; Diamictite; Sedimentary rock; Chemostratigraphy; Paleontology; Clastic rock; Total organic carbon; Oceanography; Isotopes of carbon","score_opus":0.010331642286774122,"score_gpt":0.18441531813919226,"score_spread":0.17408367585241813,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2340828404","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915489,0.0012168459,0.005233515,0.0012994946,0.00012855562,0.00017978063,0.0003256826,0.000001962665,0.00006524726],"genre_scores_gemma":[0.9985571,0.000017744567,0.00092216925,0.00019881103,0.00017558997,0.0000010909209,0.00011416922,8.785126e-7,0.000012436156],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988743,0.00005356545,0.00036620934,0.000103763065,0.00034503307,0.00025709724],"domain_scores_gemma":[0.99903756,0.00011044966,0.0003399267,0.00008974231,0.00013980693,0.00028251493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004181295,0.000104514715,0.00012916485,0.00007599173,0.0009583117,0.0001819551,0.00031208002,0.000045176115,0.000115816205],"category_scores_gemma":[0.00007161915,0.00006184617,0.000095561074,0.00034810425,0.00043247224,0.0017440551,0.000004803388,0.000089269015,0.0000011925289],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011307015,0.000020017631,0.9507585,0.000041623556,0.000040841187,0.0000011961486,0.0075017656,0.03202884,0.002279235,0.001009591,0.00033044067,0.005874841],"study_design_scores_gemma":[0.0004957174,0.00025010094,0.8698068,0.000081044294,0.00009877812,0.00008988024,0.0026767654,0.11339176,0.010293667,0.0016778724,0.00094635587,0.0001912296],"about_ca_topic_score_codex":0.016758908,"about_ca_topic_score_gemma":0.24182937,"teacher_disagreement_score":0.22507045,"about_ca_system_score_codex":0.0000054407574,"about_ca_system_score_gemma":0.00046490371,"threshold_uncertainty_score":0.9897886},"labels":[],"label_agreement":null},{"id":"W2341017821","doi":"10.1139/cjes-2015-0231","title":"Geology and age of the Morrison porphyry Cu–Au–Mo deposit, Babine Lake area, British Columbia","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Molybdenite; Geochemistry; Sericite; Pyrite; Sphalerite; Arsenopyrite; Porphyry copper deposit; Meteoric water; Chalcopyrite; Fluid inclusions; Galena; Dolomite; Isochron; Vein; Magmatic water; Mineralogy; Quartz; Chemistry; Copper","score_opus":0.010198930870779612,"score_gpt":0.16315174568406748,"score_spread":0.15295281481328787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2341017821","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956461,0.00088105677,0.00001321798,0.0011721955,0.00014957329,0.000035628374,0.00005106864,0.0000016548595,0.0020494938],"genre_scores_gemma":[0.9987761,0.000052342144,0.00019941041,0.0002601046,0.000059694008,9.3892105e-8,0.0000013569044,7.157931e-7,0.00065020885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989352,0.000066936824,0.00028293967,0.00015597475,0.00021550362,0.0003433981],"domain_scores_gemma":[0.99907017,0.00013362175,0.00018419868,0.00007234334,0.00008552275,0.0004541659],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00043727463,0.000065664935,0.00022242163,0.0000626002,0.00031919687,0.00011084082,0.0004151229,0.000052730808,0.005905078],"category_scores_gemma":[0.0002623921,0.00004100679,0.00009675846,0.00035530684,0.0014368792,0.00015683296,0.000012410201,0.000100525656,0.0000066387556],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000017549182,0.0000028071709,0.9915898,0.0000023540963,0.000009256311,0.00005852871,0.000022484088,0.00004355479,0.00017038305,0.0000057833113,0.0002140192,0.007879291],"study_design_scores_gemma":[0.00011848977,0.00017071114,0.99252605,0.00004625293,0.000017033786,0.00029878734,0.00004751349,0.00008676402,0.000063516956,0.0044179307,0.0021361595,0.000070765986],"about_ca_topic_score_codex":0.46194768,"about_ca_topic_score_gemma":0.99578875,"teacher_disagreement_score":0.5338411,"about_ca_system_score_codex":0.0000010995343,"about_ca_system_score_gemma":0.00028587968,"threshold_uncertainty_score":0.99500364},"labels":[],"label_agreement":null},{"id":"W2341262636","doi":"10.1139/cjes-2015-0157","title":"Preservation of mandibular zinc in a beetle from the Eocene Kishenehn Formation of Montana, USA","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fossil Insects in Amber","field":"Agricultural and Biological Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Museum of Natural History","keywords":"Extant taxon; Insect; Geology; Homogeneous; Paleontology; Taphonomy; Biology; Botany; Evolutionary biology","score_opus":0.03359706112615599,"score_gpt":0.2145244593385895,"score_spread":0.1809273982124335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2341262636","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99666905,0.0003648854,0.000011785423,0.002104485,0.00011589458,0.000055165867,0.000030675605,7.061369e-7,0.0006473743],"genre_scores_gemma":[0.9996592,0.000026824326,0.0001583125,0.00005858244,0.000062766005,4.889314e-7,5.163258e-7,2.4571614e-7,0.000033056902],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991053,0.00006535775,0.00031372046,0.00007092651,0.00029040413,0.00015434242],"domain_scores_gemma":[0.9992313,0.00019012736,0.00028758156,0.000038112546,0.00015648438,0.00009638683],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008122935,0.000048856135,0.0001127482,0.000037027465,0.00009263101,0.000027679702,0.00038786203,0.000035144032,0.0003532015],"category_scores_gemma":[0.0002880077,0.000014099148,0.00004261904,0.00038117715,0.00029036298,0.0005809775,0.000010959203,0.000047402013,0.0000024991834],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023367413,0.000019960147,0.83580005,0.0000051685774,0.000008350841,0.000010683525,0.0006616894,0.00013815003,0.13707866,0.0007256285,0.0006505483,0.024877753],"study_design_scores_gemma":[0.0001012117,0.00019113452,0.98344755,0.00013582822,0.000003334325,0.000006119897,0.00021459295,0.000087699606,0.011518424,0.0021921357,0.0020598834,0.000042088628],"about_ca_topic_score_codex":0.03929987,"about_ca_topic_score_gemma":0.6626837,"teacher_disagreement_score":0.6233839,"about_ca_system_score_codex":0.00001051153,"about_ca_system_score_gemma":0.00014237214,"threshold_uncertainty_score":0.9670975},"labels":[],"label_agreement":null},{"id":"W2342662352","doi":"10.1139/e2012-041","title":"Buried-valley aquifers in the Canadian Prairies: geology, hydrogeology, and origin<sup>1</sup>Earth Science Sector (ESS) Contribution 20120131.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Geoscience BC","funders":"","keywords":"Geology; Aquifer; Bedrock; Groundwater; Hydrogeology; Anticline; Groundwater recharge; Fluvial; Geomorphology; Geochemistry; Quaternary; Groundwater flow; Paleontology; Structural basin; Geotechnical engineering","score_opus":0.0273630017183814,"score_gpt":0.25618794976392434,"score_spread":0.22882494804554293,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2342662352","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98025763,0.003925378,0.000004148092,0.008650804,0.0005910907,0.00021674899,0.00002703144,0.0000045383103,0.006322604],"genre_scores_gemma":[0.9983607,0.000071797556,0.00021293377,0.0010559368,0.00021598165,0.0000013380572,0.000008041487,0.0000022656302,0.00007100673],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99640983,0.00049632567,0.00040998933,0.00030475593,0.00048255484,0.0018965345],"domain_scores_gemma":[0.9971332,0.0005422334,0.0001810677,0.00019940683,0.00025266604,0.0016914163],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["sts"],"category_scores_codex":[0.008015315,0.00019516303,0.00033627695,0.0012540013,0.0021150962,0.00023275247,0.0010951452,0.00021920812,0.0010796778],"category_scores_gemma":[0.0010070285,0.00013328128,0.000056572946,0.0013316132,0.009013905,0.0012352369,0.000015652711,0.00074424816,0.00014624548],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011373928,0.000004903205,0.9950237,0.000003947159,0.000009753523,0.00009374109,0.0013221073,0.00086878106,0.0000017010649,0.002398346,0.00014349887,0.00011812029],"study_design_scores_gemma":[0.00030210495,0.00027565227,0.97747004,0.000018454193,0.000012058302,0.0020289263,0.0012945244,0.0014769846,0.000014465524,0.00074954686,0.016190268,0.000166991],"about_ca_topic_score_codex":0.38581496,"about_ca_topic_score_gemma":0.9904802,"teacher_disagreement_score":0.6046652,"about_ca_system_score_codex":0.000005375316,"about_ca_system_score_gemma":0.006908694,"threshold_uncertainty_score":0.99983346},"labels":[],"label_agreement":null},{"id":"W2342848403","doi":"10.1139/cjes-2016-0043","title":"Eocene paleontology and geology of western North America","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Brandon University","funders":"Natural Sciences and Engineering Research Council of Canada; Geological Society of America","keywords":"Geology; Biota; Geologic record; Paleontology; Mammal; Cenozoic; Temperate climate; Climate change; Archaeology; Physical geography; Ecology; Geography; Oceanography; Structural basin","score_opus":0.022614177755911163,"score_gpt":0.23157035417378982,"score_spread":0.20895617641787867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2342848403","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924939,0.0021224378,0.000050754905,0.0026559443,0.000250967,0.000034741293,0.000016414939,0.0000016052829,0.002373201],"genre_scores_gemma":[0.9990627,0.00021676887,0.0003422563,0.00018356963,0.00003778618,8.959164e-8,7.2866396e-7,7.5405785e-7,0.00015535884],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988607,0.00015518622,0.00027003625,0.00014373587,0.00012946238,0.00044083362],"domain_scores_gemma":[0.99875283,0.00041387187,0.00019647821,0.00008065414,0.000110361914,0.0004458122],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004930846,0.00007789834,0.00025312786,0.0003510058,0.00019029342,0.000013457317,0.0003511016,0.00007144973,0.0013508492],"category_scores_gemma":[0.00021348539,0.000046047313,0.00003485424,0.00024741484,0.0030760823,0.00020054751,0.0000058573437,0.00011694717,0.00004918476],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000124476355,0.0000016538147,0.9938492,0.000003981966,0.000010919966,0.00009328475,0.000122255,0.000029704694,0.0000040922896,0.000058071844,0.000012951086,0.0058014384],"study_design_scores_gemma":[0.00019015087,0.00055860274,0.99546504,0.000014051334,0.000005920471,0.00070385926,0.000088130386,0.000022129887,0.00001613661,0.00055575947,0.0023207378,0.00005946763],"about_ca_topic_score_codex":0.0036195198,"about_ca_topic_score_gemma":0.8242521,"teacher_disagreement_score":0.8206326,"about_ca_system_score_codex":1.7128393e-7,"about_ca_system_score_gemma":0.0007607786,"threshold_uncertainty_score":0.99963695},"labels":[],"label_agreement":null},{"id":"W2342850532","doi":"10.1139/cjes-2015-0217","title":"Conodont faunal dynamics across the Middle and Upper Ordovician boundary in the Yichang area, western Hubei Province, South China","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Conodont; Fauna; Geology; Ordovician; Paleontology; Section (typography); Biostratigraphy; Ecology; Biology","score_opus":0.023156774275792484,"score_gpt":0.21815678880325698,"score_spread":0.1950000145274645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2342850532","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98431724,0.0040527987,0.000035100653,0.0043848096,0.00031220316,0.000104383544,0.000107017244,0.000002143808,0.006684277],"genre_scores_gemma":[0.99938655,0.00003383368,0.00005539579,0.00035836035,0.0000779943,3.351434e-7,5.724221e-7,6.7336754e-7,0.000086260516],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986609,0.00014922064,0.00026444648,0.00016656246,0.0002397113,0.00051911065],"domain_scores_gemma":[0.99920267,0.0002006059,0.00017442537,0.00011767998,0.000033262215,0.00027137325],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013903755,0.00011887163,0.00016413885,0.00014737887,0.0010978928,0.00033599263,0.0006646672,0.00006072214,0.00007411641],"category_scores_gemma":[0.000078671816,0.000050740582,0.00006137256,0.0002667043,0.0019926508,0.00048077365,0.0000022290744,0.00022499048,0.0000043199116],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008226341,0.00000192934,0.97054887,0.0000019484823,0.000006522906,0.00006597897,0.003505405,0.000015075145,0.0000010036613,0.00013783657,0.000012071688,0.025695141],"study_design_scores_gemma":[0.00017860594,0.0002149057,0.9934352,0.00006128998,0.0000059945496,0.0002833919,0.0037598321,0.00026137274,0.0000014518746,0.0007453605,0.0009612906,0.00009132789],"about_ca_topic_score_codex":0.012312789,"about_ca_topic_score_gemma":0.9451954,"teacher_disagreement_score":0.9328826,"about_ca_system_score_codex":0.0000022029142,"about_ca_system_score_gemma":0.00081283634,"threshold_uncertainty_score":0.9942643},"labels":[],"label_agreement":null},{"id":"W2344134623","doi":"10.1139/cjes-2016-0002","title":"Upper Ordovician – Upper Silurian conodont biostratigraphy, Devon Island and southern Ellesmere Island, Canadian Arctic Islands, with implications for regional stratigraphy, eustasy, and thermal maturation","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada; Government of Nunavut; Nunavut Research Institute","funders":"Natural Sciences and Engineering Research Council of Canada; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Conodont; Geology; Paleontology; Biostratigraphy; Ordovician; Facies; Laurentia; Stratigraphy; Baltica; Glacial period; Range (aeronautics); Tectonics; Structural basin","score_opus":0.015259379167776923,"score_gpt":0.209430643625329,"score_spread":0.1941712644575521,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2344134623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9804485,0.0038116002,0.00011199948,0.010092224,0.00013093167,0.0002743137,0.0016709353,0.0000046175846,0.003454892],"genre_scores_gemma":[0.99850786,0.000102507525,0.000925157,0.00029993866,0.00011024173,0.000001927317,0.000016740027,0.000002360945,0.000033266908],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985798,0.000077243276,0.00031908142,0.00030199336,0.00015352898,0.0005683284],"domain_scores_gemma":[0.9983627,0.00020461892,0.000211291,0.00011953434,0.00017907805,0.0009227493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045267786,0.00020650617,0.00023888756,0.0005626692,0.0010219892,0.00025014865,0.00025270542,0.00012379995,0.00030018398],"category_scores_gemma":[0.000040660158,0.00012316942,0.00007943576,0.0002853356,0.0012207549,0.00054902164,8.075204e-7,0.00014233436,0.0000016817743],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000045952296,0.000002848896,0.98161,0.000006987033,0.000044458942,0.0000096801605,0.0004828726,0.000008460541,0.000061085884,0.0012902725,0.0001399551,0.016297441],"study_design_scores_gemma":[0.00055827986,0.00061572477,0.99292916,0.00009117266,0.0000362552,0.000318874,0.0008794786,0.00005826456,0.000012996481,0.0021051413,0.00217742,0.0002172096],"about_ca_topic_score_codex":0.15437695,"about_ca_topic_score_gemma":0.9982027,"teacher_disagreement_score":0.8438257,"about_ca_system_score_codex":0.0000026617442,"about_ca_system_score_gemma":0.0018543018,"threshold_uncertainty_score":0.8512541},"labels":[],"label_agreement":null},{"id":"W2344219290","doi":"10.1139/cjes-2015-0188","title":"The Homerian (late Wenlock, Silurian) carbon isotope excursion from Perunica: Does dolomite control the magnitude of the carbon isotope excursion?","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Česká geologická služba; Grantová Agentura České Republiky","keywords":"Dolomite; Calcite; Geology; Isotopes of carbon; Diagenesis; Carbonate; Geochemistry; Isotopes of oxygen; Excursion; Mineralogy; Stable isotope ratio; Carbon fibers; Carbonate minerals; Isotope; Chemistry; Total organic carbon; Environmental chemistry; Materials science","score_opus":0.009831397558293271,"score_gpt":0.19508953082338792,"score_spread":0.18525813326509466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2344219290","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96129185,0.012532673,0.0000027726285,0.015257576,0.002074035,0.00023490633,0.00010292554,0.0000044920694,0.008498763],"genre_scores_gemma":[0.99894476,0.0004026875,0.000053234795,0.00018553251,0.00023363036,9.305663e-7,3.3036167e-7,0.0000017696798,0.00017710614],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973964,0.0006084861,0.0005546002,0.0002678197,0.0005352005,0.00063745986],"domain_scores_gemma":[0.99736786,0.0010144822,0.00060289283,0.00040383174,0.00016074802,0.00045016513],"candidate_categories":["sts"],"consensus_categories":["sts"],"category_scores_codex":[0.0018745655,0.00020848784,0.00033099516,0.00014698475,0.0013566669,0.00017298528,0.0017820399,0.00011903446,0.00022728278],"category_scores_gemma":[0.00036788662,0.000070834394,0.0002193578,0.00043851498,0.00317269,0.00029455964,0.00000641612,0.00033608824,0.00000389409],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000072082024,0.000005171684,0.9675874,0.0000023338102,0.0000553662,0.000023149629,0.00059938215,0.00007753423,0.00079877273,0.000112294016,0.000055732686,0.030610798],"study_design_scores_gemma":[0.00051495555,0.0002717986,0.9922628,0.00012261904,0.000050681705,0.000032814627,0.000647569,0.00035244468,0.0004484111,0.0019984546,0.0031558522,0.0001416137],"about_ca_topic_score_codex":0.043738935,"about_ca_topic_score_gemma":0.6706072,"teacher_disagreement_score":0.6268683,"about_ca_system_score_codex":0.0000035237285,"about_ca_system_score_gemma":0.0011837396,"threshold_uncertainty_score":0.99994344},"labels":[],"label_agreement":null},{"id":"W2345450468","doi":"10.1139/cjes-2016-0039","title":"Crustal accretion of thick mafic crust in Iceland: implications for volcanic rifted margins","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"University at Albany; State University of New York; National Science Foundation","keywords":"Geology; Crust; Mafic; Rift; Seafloor spreading; Continental crust; Underplating; Oceanic crust; Petrology; Geochemistry; Igneous rock; Seismology; Geophysics; Tectonics; Subduction","score_opus":0.025145246028018944,"score_gpt":0.22320747319409803,"score_spread":0.19806222716607907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2345450468","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993049,0.00040828367,0.00020504916,0.0049161366,0.000098893295,0.000069407455,0.000118195225,0.0000026801,0.0011323137],"genre_scores_gemma":[0.99918,0.000038776023,0.00053855975,0.000120212506,0.000051043564,4.6523527e-7,0.0000042650668,0.0000010273048,0.00006565866],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999038,0.000037247075,0.00033783633,0.00013939674,0.00013553213,0.0003119987],"domain_scores_gemma":[0.99901086,0.00023520447,0.00019490953,0.00007314617,0.00014780971,0.0003380696],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00058792497,0.00007268918,0.00018382796,0.00029747759,0.00012689605,0.00003235649,0.0003412354,0.000052128104,0.002126838],"category_scores_gemma":[0.0003383101,0.00004042685,0.00010145332,0.00056993036,0.00039498028,0.00022313537,0.0000034952704,0.00007512154,0.0000099644485],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010688271,0.0000048823354,0.99320453,0.0000036789663,0.0000065218446,0.0000034330408,0.00003993732,0.00032998165,0.00076836575,0.00036501113,0.00008292016,0.0051800166],"study_design_scores_gemma":[0.00020684898,0.00021399673,0.9838006,0.000032832522,0.000011446051,0.000016404021,0.00009639423,0.00031157443,0.00020780995,0.013216578,0.0018146578,0.000070890346],"about_ca_topic_score_codex":0.017723715,"about_ca_topic_score_gemma":0.63725376,"teacher_disagreement_score":0.61953,"about_ca_system_score_codex":0.0000022810038,"about_ca_system_score_gemma":0.0005435397,"threshold_uncertainty_score":0.9987854},"labels":[],"label_agreement":null},{"id":"W2345931547","doi":"10.1139/cjes-2015-0137","title":"Alignment of fluvio-tidal point bars in the middle McMurray Formation: implications for structural architecture of the Lower Cretaceous Athabasca Oil Sands Deposit, northern Alberta","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Chevron (Canada)","funders":"","keywords":"Geology; Cretaceous; Devonian; Fluvial; Oil sands; Paleontology; Geomorphology; Geochemistry; Petrology; Asphalt; Structural basin","score_opus":0.01870598358356964,"score_gpt":0.20490361223749226,"score_spread":0.18619762865392261,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2345931547","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99193037,0.00060186564,0.00022356166,0.0054418817,0.00015979861,0.00009571944,0.00011128413,7.425803e-7,0.0014347974],"genre_scores_gemma":[0.99923164,0.000018478768,0.00050221244,0.00016334798,0.000031872976,0.0000010294756,0.0000024605736,8.972033e-7,0.000048066362],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990503,0.000063211875,0.0003738504,0.000080465405,0.0002002562,0.0002318963],"domain_scores_gemma":[0.9990212,0.00031980366,0.00028068936,0.00012491783,0.00012951992,0.00012390336],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051593885,0.000078562676,0.00012827726,0.00011049211,0.00032659207,0.00004683125,0.00062779547,0.00003355683,0.00024495507],"category_scores_gemma":[0.00017566375,0.000031354044,0.0000990799,0.00035171057,0.00038334535,0.00029375698,0.0000053529398,0.00007117733,0.0000017265237],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002033608,0.000007729901,0.96775305,0.000030444777,0.000010933017,0.0000011024886,0.0031545714,0.0055668335,0.000075742035,0.00036724165,0.000071906696,0.022940088],"study_design_scores_gemma":[0.000253237,0.00047753353,0.9897057,0.000117343705,0.000014931085,0.00020686757,0.00084715337,0.000265951,0.0005277806,0.0044263005,0.0030669244,0.00009029144],"about_ca_topic_score_codex":0.0066874274,"about_ca_topic_score_gemma":0.590927,"teacher_disagreement_score":0.5842396,"about_ca_system_score_codex":0.0000026552707,"about_ca_system_score_gemma":0.00038988946,"threshold_uncertainty_score":0.9999271},"labels":[],"label_agreement":null},{"id":"W2345978558","doi":"10.1139/cjes-2016-0006","title":"Earliest occurrence of <i>Hydrocynus</i> (Characiformes, Alestidae) from Eocene continental deposits of Méridja Hamada, northwestern Sahara, Algeria","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fish biology, ecology, and behavior","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Royal Tyrrell Museum; University of Alberta","funders":"Université de Poitiers; University of Tlemcen; Northwestern University","keywords":"Geology; Paleontology; Characiformes; Biological dispersal; Taxon; Fish <Actinopterygii>; Biology; Population; Fishery","score_opus":0.015077448886587798,"score_gpt":0.21627208974217135,"score_spread":0.20119464085558356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2345978558","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99768233,0.0003121896,0.000020064603,0.00031098584,0.000647544,0.00009697833,0.0003392525,0.000003255871,0.00058740197],"genre_scores_gemma":[0.99919826,0.00006049683,0.00048258415,0.000118683274,0.000057686728,0.0000011659134,0.0000037989412,0.000004581257,0.000072773546],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982525,0.00006662666,0.00062854885,0.00026671484,0.00031725378,0.0004683282],"domain_scores_gemma":[0.99850476,0.0001291879,0.0006363591,0.00016624981,0.00005848547,0.00050495414],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047172335,0.00016478788,0.00036501006,0.00013891105,0.0001713767,0.000028210006,0.00075059023,0.00008652536,0.0015325914],"category_scores_gemma":[0.00009362723,0.000111765905,0.0001122215,0.00028552217,0.002366586,0.0005133183,0.000054837838,0.000117193245,0.00006351138],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012672195,0.000027266668,0.93758345,0.0000033013678,0.000008479209,0.00003401165,0.00012241896,0.0000119289925,0.05965411,0.000005066951,0.0003264519,0.002210824],"study_design_scores_gemma":[0.00040728025,0.00043477947,0.9764559,0.000099409976,0.000022588054,0.000092301176,0.00012320292,0.000006466687,0.020886388,0.000054880788,0.0012696488,0.00014714239],"about_ca_topic_score_codex":0.0155825475,"about_ca_topic_score_gemma":0.5280813,"teacher_disagreement_score":0.51249874,"about_ca_system_score_codex":0.000024285991,"about_ca_system_score_gemma":0.000481591,"threshold_uncertainty_score":0.9993802},"labels":[],"label_agreement":null},{"id":"W2346421272","doi":"10.1139/e2012-064","title":"Lateral variation in sandstone lithofacies from conventional core, Scotian Basin: implications for reservoir quality and connectivity <sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of <i>Mesozoic–Cenozoic geology of the Scotian Basin</i>. <sup>2</sup>Geological Survey of Canada Contribution 20120021.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Saint Mary's University","funders":"","keywords":"Geology; Outcrop; Facies; Turbidite; Sedimentary depositional environment; Diagenesis; Transgressive; Conglomerate; Structural basin; Delta; Geomorphology; Paleontology; Petrology","score_opus":0.04395961324848086,"score_gpt":0.2452669211970293,"score_spread":0.20130730794854845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2346421272","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99183625,0.00038035357,0.000010214771,0.00547291,0.00012929772,0.0002429294,0.0014665027,8.8066014e-7,0.00046065944],"genre_scores_gemma":[0.999498,0.000033049728,0.00017761627,0.00017658096,0.000059972874,0.0000013660774,0.000027673612,0.0000012609969,0.000024456864],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978303,0.0005371635,0.00084094604,0.00014735541,0.0003192918,0.00032499532],"domain_scores_gemma":[0.9969299,0.0015035683,0.0007177639,0.0001500042,0.00054114894,0.00015760682],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0037265634,0.00011180364,0.00044857827,0.00016816321,0.000209619,0.000026667363,0.00035806533,0.00009520534,0.005170676],"category_scores_gemma":[0.002812125,0.00006835616,0.000067903144,0.0007146265,0.0012956553,0.00053942925,0.000017330347,0.00015794279,4.256045e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012604245,0.000043569482,0.99376345,0.000028261726,0.000020616202,1.6790314e-7,0.0014207542,0.002429273,0.00006565789,0.0017193506,0.00025539042,0.00012747402],"study_design_scores_gemma":[0.00038591755,0.0002900074,0.99312824,0.000064757165,0.000012915031,0.0000052391238,0.00062689866,0.00088117603,0.0008696086,0.003266802,0.00039708999,0.00007132534],"about_ca_topic_score_codex":0.6401978,"about_ca_topic_score_gemma":0.88087547,"teacher_disagreement_score":0.24067768,"about_ca_system_score_codex":0.000010029428,"about_ca_system_score_gemma":0.001239262,"threshold_uncertainty_score":0.99573874},"labels":[],"label_agreement":null},{"id":"W2346706211","doi":"10.1139/cjes-2015-0242","title":"Refining 2 km of Ordovician chronostratigraphy beneath Anticosti Island utilizing integrated chemostratigraphy","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université du Québec; GDG Environnement; Institut National de la Recherche Scientifique; University of Ottawa","funders":"U.S. Geological Survey","keywords":"Geology; Chemostratigraphy; Ordovician; Chronostratigraphy; Paleontology; Conodont; Biostratigraphy; Cyclostratigraphy; Unconformity; Biozone; Geochemistry; Isotopes of carbon; Sedimentary rock; Isotope","score_opus":0.021938540744631096,"score_gpt":0.20468402753501272,"score_spread":0.18274548679038163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2346706211","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98616475,0.0013293631,0.000055825127,0.0008661165,0.00017127059,0.000026613401,0.00010502063,0.000004287292,0.01127677],"genre_scores_gemma":[0.99798703,0.00005163199,0.001736008,0.00013362436,0.000058227826,7.886063e-8,0.000004593723,0.0000011389516,0.000027681292],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851596,0.000055667337,0.00048530014,0.00020306422,0.00030060104,0.0004394229],"domain_scores_gemma":[0.9986413,0.00017531379,0.00031437402,0.0001024952,0.00019298062,0.00057351775],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00059469795,0.00014201005,0.00031079416,0.0004382075,0.00024478356,0.000075142816,0.00046663734,0.000064565524,0.006148778],"category_scores_gemma":[0.00027665606,0.00007459482,0.0001822136,0.0011806894,0.00090737134,0.00034097224,0.0000037176817,0.00014154648,0.000013284004],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007746694,0.000004466294,0.981499,0.0000038594403,0.000023530742,0.000024237539,0.00006597356,0.00008740788,0.0015422759,0.000092747476,0.0000373061,0.016611436],"study_design_scores_gemma":[0.00021677767,0.000569583,0.98960245,0.00015862873,0.00003093415,0.000046158784,0.00036107347,0.00020385341,0.0039332686,0.0023603772,0.002353451,0.00016345557],"about_ca_topic_score_codex":0.022975817,"about_ca_topic_score_gemma":0.5721412,"teacher_disagreement_score":0.54916537,"about_ca_system_score_codex":9.391101e-7,"about_ca_system_score_gemma":0.00060589396,"threshold_uncertainty_score":0.99475974},"labels":[],"label_agreement":null},{"id":"W2363980641","doi":"10.1139/e2012-062","title":"Detrital muscovite geochronology and the Cretaceous tectonics of the inner Scotian Shelf, southeastern Canada <sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of <i>Mesozoic–Cenozoic geology of the Scotian Basin</i>. <sup>2</sup>Geological Survey of Canada Contribution 20120142.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada; Saint Mary's University; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Offshore Energy Research Association","keywords":"Geology; Cretaceous; Terrane; Muscovite; Aptian; Paleontology; Geochronology; Detritus; Structural basin; Mesozoic; Provenance; Tectonics","score_opus":0.009683002836931357,"score_gpt":0.16926044543498156,"score_spread":0.1595774425980502,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2363980641","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9876835,0.0017359859,7.5100525e-7,0.008631009,0.00022331177,0.00021885855,0.0004240355,8.153783e-7,0.0010817482],"genre_scores_gemma":[0.9992839,0.000046465895,0.000027648772,0.00046831358,0.000092919945,5.651077e-7,0.000004482709,0.0000024056026,0.000073268944],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9963664,0.000980307,0.0010488745,0.00022424202,0.00073892093,0.0006412812],"domain_scores_gemma":[0.9965681,0.001314602,0.0010069803,0.0003381353,0.0004969279,0.0002752728],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0029852274,0.00020747885,0.0008206125,0.00015916118,0.00024197731,0.000022447524,0.001090694,0.00013925818,0.008573062],"category_scores_gemma":[0.0028106284,0.00009260242,0.00017680644,0.0012141779,0.0049483436,0.00020427558,0.000071060786,0.00040183685,8.357569e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014393935,0.00003069338,0.9930331,0.000023057753,0.000079779755,0.000002464513,0.0012213439,0.0044576963,0.00011000966,0.00018972163,0.0003511074,0.0003570465],"study_design_scores_gemma":[0.0005892601,0.00037923336,0.98876256,0.00009117743,0.000075903714,0.00003446123,0.002248514,0.0015586752,0.0043202266,0.0007021288,0.0011087928,0.00012906754],"about_ca_topic_score_codex":0.96379787,"about_ca_topic_score_gemma":0.99738234,"teacher_disagreement_score":0.03358448,"about_ca_system_score_codex":0.000012899307,"about_ca_system_score_gemma":0.002797265,"threshold_uncertainty_score":0.99775964},"labels":[],"label_agreement":null},{"id":"W2368180547","doi":"10.1139/cjes-2015-0167","title":"A window into mid-latitudinal Early Eocene environmental variability: a high-resolution palynological analysis of the Falkland site, Okanagan Highlands, British Columbia, Canada","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Brandon University; Canadian Museum of Nature","funders":"Natural Sciences and Engineering Research Council of Canada; University of Queensland","keywords":"Geology; Palynology; Tephra; Volcano; Vegetation (pathology); Physical geography; Period (music); Holocene; Environmental change; Pollen; Paleontology; Climate change; Oceanography; Ecology; Geography","score_opus":0.0091654592451683,"score_gpt":0.18071305804777787,"score_spread":0.17154759880260959,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2368180547","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974262,0.000411035,0.000015270407,0.0011824343,0.0003410045,0.00008128687,0.00027501764,0.0000017836269,0.0002659679],"genre_scores_gemma":[0.99951595,0.000034120978,0.00013899938,0.00010106563,0.000041141233,3.2174097e-7,0.000007628082,0.0000011433272,0.00015964474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998019,0.0003706915,0.00039106436,0.00024868222,0.00046818756,0.00050237094],"domain_scores_gemma":[0.99864733,0.00042359543,0.000251865,0.00016318008,0.00006701098,0.00044704555],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001199179,0.00009188398,0.0003428647,0.00019687782,0.00069207075,0.00010807839,0.00059082964,0.00010814244,0.0040419023],"category_scores_gemma":[0.00031362058,0.000066183326,0.000121274,0.00085629994,0.0018092109,0.00021451732,0.000016752501,0.00020405444,0.0000060625625],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001007589,0.00000619201,0.9985237,0.0000026781934,0.000113567636,0.00009647966,0.000057458812,0.0004031426,0.0000150750075,0.0000078542935,0.000079422985,0.00068436895],"study_design_scores_gemma":[0.00026412,0.00020532018,0.99814034,0.000024285093,0.00011067639,0.00013367979,0.000057357163,0.00016408734,0.0000137817415,0.00045343937,0.00034001138,0.00009288825],"about_ca_topic_score_codex":0.96329635,"about_ca_topic_score_gemma":0.9999036,"teacher_disagreement_score":0.03660727,"about_ca_system_score_codex":0.000005646175,"about_ca_system_score_gemma":0.0019573516,"threshold_uncertainty_score":0.99686855},"labels":[],"label_agreement":null},{"id":"W2389513146","doi":"10.1139/cjes-2016-0023","title":"Lithological, structural, and geochemical characteristics of the Mesoarchean Târtoq greenstone belt, southern West Greenland, and the Chugach – Prince William accretionary complex, southern Alaska: evidence for uniformitarian plate-tectonic processes","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"","keywords":"Geology; Felsic; Geochemistry; Accretionary wedge; Archean; Subduction; Greenstone belt; Oceanic crust; Craton; Continental crust; Adakite; Zircon; Pillow lava; Petrology; Crust; Mafic; Paleontology; Volcanic rock; Tectonics","score_opus":0.035419388457327415,"score_gpt":0.23017060830511143,"score_spread":0.194751219847784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2389513146","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99098563,0.0017805978,0.000028225986,0.0066459426,0.000051188963,0.00013737005,0.00030084013,0.000003365865,0.0000668613],"genre_scores_gemma":[0.9989605,0.00019924906,0.00048589348,0.00018261258,0.00008597129,9.250611e-7,0.0000052860055,0.0000018757505,0.000077700955],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985721,0.00009272635,0.0004133983,0.00024511694,0.00029925047,0.00037740733],"domain_scores_gemma":[0.99786925,0.0010752318,0.00036941044,0.00012949202,0.00021431809,0.00034227734],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00088979735,0.00015839146,0.00033809134,0.00007186064,0.0006037497,0.00008610191,0.00062692375,0.000074488365,0.0007166758],"category_scores_gemma":[0.0011693069,0.000059823433,0.00010159742,0.00031069005,0.0041226163,0.0002125217,0.00003606523,0.00016893007,0.0000031833413],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000084552725,0.000002561786,0.9945469,0.000027997152,0.00002097272,0.0000043374316,0.00030423826,0.000018132081,0.00020961584,0.000059821705,0.000006138203,0.0047147456],"study_design_scores_gemma":[0.00043152156,0.00019528715,0.9899674,0.00015001341,0.000056809135,0.00017621464,0.00042121575,0.00034206267,0.000084919375,0.007775566,0.0002699898,0.00012898761],"about_ca_topic_score_codex":0.0050493064,"about_ca_topic_score_gemma":0.15038705,"teacher_disagreement_score":0.14533775,"about_ca_system_score_codex":0.0000021812798,"about_ca_system_score_gemma":0.0004247031,"threshold_uncertainty_score":0.9985876},"labels":[],"label_agreement":null},{"id":"W2392977100","doi":"10.1139/e09-010","title":"Preliminary results on the sensitivity of atmospheric bending angles retrieved from COSMIC radio occultations to Doppler frequency shift and satellite velocity variationsThis article is one of a series of papers published in this Special Issue on the theme <i>GEODESY</i>.","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"York University","funders":"University Corporation for Atmospheric Research","keywords":"Doppler effect; Radio occultation; Geodesy; Satellite; Global Positioning System; COSMIC cancer database; Physics; Bending; Geology; Remote sensing; Computer science; Astrophysics; Telecommunications; Astronomy","score_opus":0.012000239455033167,"score_gpt":0.20586292078650173,"score_spread":0.19386268133146856,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2392977100","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98273367,0.00005677697,0.00004729922,0.0064873523,0.000097323384,0.00016181693,0.00017200035,0.0000012188551,0.010242556],"genre_scores_gemma":[0.99779737,0.00001335004,0.0017248228,0.0002432608,0.0001617038,7.687017e-7,0.0000029256416,0.00000295563,0.00005283531],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99890673,0.0001409971,0.0004054216,0.00013775735,0.00022679998,0.00018231344],"domain_scores_gemma":[0.9987928,0.00046599918,0.00035328718,0.0001403298,0.00013248454,0.00011507702],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00087818614,0.000095874144,0.0002072879,0.000023978122,0.0001972823,0.00006854653,0.00018475109,0.000029771238,0.0012178001],"category_scores_gemma":[0.0002235067,0.00006344149,0.0000578963,0.00064378296,0.00029024985,0.00027645886,0.000009020392,0.00015237453,0.0000011638734],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002156207,0.00089141546,0.41356176,0.000042434516,0.0004943045,0.00004736575,0.18080138,0.014578215,0.022514801,0.23310193,0.00874679,0.123063385],"study_design_scores_gemma":[0.00053454394,0.0014276704,0.9656379,0.0002496262,0.000036130616,0.000002582182,0.0066303182,0.0012154569,0.007843827,0.015074212,0.0011661912,0.00018151251],"about_ca_topic_score_codex":0.011593296,"about_ca_topic_score_gemma":0.01823455,"teacher_disagreement_score":0.55207616,"about_ca_system_score_codex":0.000011753301,"about_ca_system_score_gemma":0.00046099655,"threshold_uncertainty_score":0.99969524},"labels":[],"label_agreement":null},{"id":"W2406945125","doi":"10.1139/e2012-063","title":"Early Cretaceous volcanism in the Scotian Basin <sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of <i>Mesozoic–Cenozoic geology of the Scotian Basin</i>.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Saint Mary's University","funders":"Fisheries and Oceans Canada","keywords":"Geology; Aptian; Cretaceous; Basalt; Volcanic rock; Paleontology; Basement; Flood basalt; Geochemistry; Sedimentary rock; Outcrop; Graben; Volcano; Volcanism; Structural basin","score_opus":0.014558450255301988,"score_gpt":0.18559852780289657,"score_spread":0.1710400775475946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2406945125","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9713095,0.00068534754,2.9174277e-7,0.013266351,0.0002108674,0.00014584366,0.00005213079,0.0000011072194,0.014328564],"genre_scores_gemma":[0.99835914,0.00004116066,0.00011688884,0.0010392613,0.00023919289,4.3752448e-7,0.0000011637011,0.0000021190788,0.00020065435],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99723005,0.0004901084,0.00080285023,0.000195414,0.0006923937,0.00058918435],"domain_scores_gemma":[0.9981676,0.0005494863,0.0005627312,0.00028989284,0.00016692012,0.00026339162],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0025590758,0.00016826557,0.0005247188,0.0003123314,0.00018171396,0.00005475241,0.0012586904,0.00010214901,0.036910757],"category_scores_gemma":[0.0008809262,0.00008004891,0.00022637715,0.0016469288,0.0025468073,0.0004199875,0.000025768473,0.00037898566,0.000014439535],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043691267,0.00005279632,0.9901999,0.000014263872,0.00002620274,0.0000058955125,0.0066019143,0.00083447987,0.00030535064,0.00034476686,0.00059908605,0.00097165344],"study_design_scores_gemma":[0.00022299467,0.00055492326,0.9820938,0.000101746016,0.000038042228,0.000026186286,0.003951709,0.00022995083,0.006103666,0.0025873587,0.0039756084,0.000114027454],"about_ca_topic_score_codex":0.09028711,"about_ca_topic_score_gemma":0.28623152,"teacher_disagreement_score":0.1959444,"about_ca_system_score_codex":0.00000425602,"about_ca_system_score_gemma":0.0005104809,"threshold_uncertainty_score":0.96396965},"labels":[],"label_agreement":null},{"id":"W2408469476","doi":"10.1139/e11-060","title":"The chronostratigraphy of Holocene sediments from four Lake Superior sub-basins<sup>1</sup>Laboratory for Stable Isotope Science (LSIS) Contribution 264.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Varve; Geology; Glacial period; Carbonate; Chronostratigraphy; Radiocarbon dating; Geochemistry; Calcite; Sediment; Detritus; Paleontology; Sedimentary rock","score_opus":0.027181886838874736,"score_gpt":0.22625595238744092,"score_spread":0.1990740655485662,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2408469476","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99494857,0.0025894558,0.00003839411,0.00040078702,0.00048533644,0.00022129812,0.00046356083,0.0000035583093,0.0008490392],"genre_scores_gemma":[0.99892664,0.0001023174,0.0007549873,0.00011945359,0.00006861771,0.0000013493018,0.0000087587805,0.0000018678901,0.000015997264],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978872,0.00016708738,0.00043565294,0.0002550495,0.00043435255,0.0008206686],"domain_scores_gemma":[0.99783605,0.00041503154,0.000268755,0.00017936829,0.00069144316,0.0006093533],"candidate_categories":["sts"],"consensus_categories":["sts"],"category_scores_codex":[0.0033133542,0.00013365538,0.00026285456,0.00039493793,0.001759145,0.00013622906,0.0010108278,0.0000965685,0.00073839317],"category_scores_gemma":[0.00056446047,0.0000900155,0.00009099661,0.0009636024,0.004737306,0.0007390158,0.000008643968,0.00023427838,0.000021132344],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005349425,0.000006425095,0.9986394,0.0000040105,0.000021764108,0.000021384,0.00032125236,0.00019623422,0.00007116991,0.00017619629,0.00007067594,0.00041801334],"study_design_scores_gemma":[0.0004199714,0.0007232412,0.9883475,0.00003271052,0.00002008549,0.000039731352,0.00063131057,0.0010520517,0.0056955316,0.0010161574,0.0019043925,0.0001173727],"about_ca_topic_score_codex":0.0033047257,"about_ca_topic_score_gemma":0.30602345,"teacher_disagreement_score":0.30271873,"about_ca_system_score_codex":0.0000014464305,"about_ca_system_score_gemma":0.004692059,"threshold_uncertainty_score":0.99954045},"labels":[],"label_agreement":null},{"id":"W2413872372","doi":"10.1139/cjes-2016-0020","title":"The structural evolution of the Albula Pass region, Graubünden, eastern Switzerland: the origin of the various vergences in the structure of the Alps","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Nappe; Geology; Paleontology; Metamorphic rock; Permian; Basement; Cretaceous; Allochthon; Tectonics; Seismology","score_opus":0.011267299470572038,"score_gpt":0.18595609753605666,"score_spread":0.17468879806548462,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2413872372","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98268086,0.0014974565,0.0000048583306,0.014825157,0.0005918522,0.00012487323,0.00003759075,7.311581e-7,0.0002366049],"genre_scores_gemma":[0.9995492,0.000042472944,0.000010311626,0.00019516604,0.000077676625,1.7793263e-7,2.291792e-7,9.3855044e-7,0.00012382722],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978361,0.0004731051,0.00048060273,0.00014580353,0.0007216386,0.0003427451],"domain_scores_gemma":[0.9982456,0.00049557845,0.0006437861,0.00034222176,0.00016820851,0.00010460878],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009977656,0.00012469977,0.00019688062,0.000057054884,0.0007600429,0.000058547317,0.002597978,0.00005851861,0.00027181522],"category_scores_gemma":[0.00042699906,0.000028197164,0.0002309875,0.001125207,0.0025619867,0.00014040527,0.000032093816,0.00026962295,0.0000013097057],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009096526,0.0000017476787,0.99542594,0.0000025884667,0.000017204338,0.0000011991701,0.0004304524,0.0016005641,0.0001921326,0.0007006198,0.00013205262,0.0014863812],"study_design_scores_gemma":[0.00009643985,0.00007521806,0.96142834,0.000054413846,0.000032468364,0.00005823483,0.0010786065,0.00040195262,0.00041146923,0.035129912,0.0011778568,0.000055067976],"about_ca_topic_score_codex":0.048727017,"about_ca_topic_score_gemma":0.64216536,"teacher_disagreement_score":0.5934384,"about_ca_system_score_codex":0.000004513707,"about_ca_system_score_gemma":0.0006563649,"threshold_uncertainty_score":0.95760757},"labels":[],"label_agreement":null},{"id":"W2418057795","doi":"10.1139/cjes-2015-0168","title":"Freshwater molluscan fauna from the Florissant Formation, Colorado: paleohydrologic reconstruction of a latest Eocene lake","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Park Service; University of Washington","keywords":"Geology; Conglomerate; Paleontology; Aragonite; Geochemistry; Calcite; Sedimentary rock","score_opus":0.024645842429283103,"score_gpt":0.21179409755570416,"score_spread":0.18714825512642105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2418057795","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913048,0.00089373795,0.00002821608,0.0056817727,0.0006577721,0.00007031167,0.00017802804,0.0000028174022,0.0011825096],"genre_scores_gemma":[0.9992206,0.000102924,0.0003735081,0.00015200238,0.00009591443,2.6791608e-7,0.0000054188104,9.1652566e-7,0.000048447066],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987233,0.0002118704,0.00035319646,0.00012476723,0.00020920012,0.0003776156],"domain_scores_gemma":[0.9987187,0.00049323705,0.00025492505,0.000110343026,0.00014990807,0.00027292344],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011592333,0.00008583073,0.0001871652,0.00016138174,0.00043516225,0.00004293829,0.0005028606,0.00008652402,0.0052134036],"category_scores_gemma":[0.00025405933,0.000040162704,0.00006128123,0.00031449675,0.00156694,0.00043944153,0.00000533863,0.00015125058,0.000078695244],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001595242,0.0000014857,0.99757093,0.0000017239919,0.000011716194,0.000026693604,0.00018576666,0.00015450842,0.00003309735,0.000029180423,0.00020091154,0.0017680362],"study_design_scores_gemma":[0.00023232303,0.00028588326,0.9917555,0.000048843565,0.000010389504,0.0004443266,0.0002224612,0.00044414037,0.00037937815,0.0027226259,0.0033853822,0.000068748894],"about_ca_topic_score_codex":0.0046018055,"about_ca_topic_score_gemma":0.90475243,"teacher_disagreement_score":0.90015066,"about_ca_system_score_codex":5.0929594e-7,"about_ca_system_score_gemma":0.00059628324,"threshold_uncertainty_score":0.99569595},"labels":[],"label_agreement":null},{"id":"W2418998566","doi":"10.1139/e2012-006","title":"Reply to the discussion by J.W.F. Waldron and C.E. White on “Geochemical signature of Ordovician Mn-rich sedimentary rocks on the Avalonian shelf”<sup>1</sup>Appears in Canadian Journal of Earth Sciences, 2012, <b>49</b>(6): 772–774 [doi: 10.1139/e2012-004].","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ordovician; Geology; Sedimentary rock; Nova scotia; Zircon; Geochemistry; Paleontology; Fibrous joint; Baltica; Oceanography","score_opus":0.008653146352990375,"score_gpt":0.19720306299547857,"score_spread":0.18854991664248819,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2418998566","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96817553,0.0023759073,0.0000019214258,0.02540902,0.0003085917,0.00017254586,0.0002364253,0.0000020563587,0.0033179861],"genre_scores_gemma":[0.99622035,0.000041019215,0.00012290676,0.0025286775,0.0002723011,6.165461e-7,0.00001617939,0.0000050999943,0.0007928211],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99658,0.00025315722,0.00074033195,0.000323327,0.0009608373,0.0011423286],"domain_scores_gemma":[0.9970575,0.0002063289,0.00048146475,0.0002480578,0.00013427401,0.0018723689],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0038822636,0.0002824001,0.00039924352,0.00063795905,0.0011394499,0.0002596346,0.00120315,0.00012065668,0.0038473094],"category_scores_gemma":[0.0003061247,0.00014281532,0.00015260816,0.0015080645,0.0009841202,0.0007367443,0.00002264109,0.00073563185,0.000042718064],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005704277,0.00003546468,0.95826465,0.000013365118,0.000044153025,0.00004114527,0.0025585224,0.012371635,0.00022631518,0.000017341034,0.02316596,0.0032043832],"study_design_scores_gemma":[0.000943816,0.0032032153,0.61506027,0.0009190948,0.00017165531,0.00052311446,0.015022645,0.0023400388,0.0059917783,0.00037941453,0.3545523,0.0008926688],"about_ca_topic_score_codex":0.12587406,"about_ca_topic_score_gemma":0.6516091,"teacher_disagreement_score":0.5257351,"about_ca_system_score_codex":0.000019247334,"about_ca_system_score_gemma":0.0018161745,"threshold_uncertainty_score":0.99706334},"labels":[],"label_agreement":null},{"id":"W2461000102","doi":"10.1139/cjes-2016-0017","title":"The Coulon deposit: quantifying alteration in volcanogenic massive sulphide systems modified by amphibolite-facies metamorphism","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Paul University; Université du Québec à Chicoutimi; Hudbay Minerals (Canada)","funders":"","keywords":"Metamorphism; Geology; Geochemistry; Metasomatism; Muscovite; Context (archaeology); Metamorphic facies; Metamorphic rock; Biotite; Greenschist; Chlorite; Facies; Quartz; Geomorphology; Paleontology; Mantle (geology)","score_opus":0.03209914912027217,"score_gpt":0.21682378385885692,"score_spread":0.18472463473858475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2461000102","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9864894,0.009401285,0.00015840957,0.0030372315,0.00028151437,0.00006688879,0.000039943658,0.0000032123287,0.0005220862],"genre_scores_gemma":[0.99929434,0.00025095852,0.00007180056,0.00010756301,0.00005646665,5.438428e-7,0.0000031976083,0.0000010730096,0.00021407465],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983796,0.00015490237,0.00044574408,0.00018576879,0.00035393515,0.00048007397],"domain_scores_gemma":[0.9987153,0.00039890193,0.00023954891,0.00009182917,0.00012687333,0.00042759],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001097541,0.00011558868,0.00021579354,0.00019787098,0.0005630506,0.00032174285,0.00045995766,0.000050625575,0.00038928387],"category_scores_gemma":[0.00031252473,0.000052291984,0.00009551822,0.00054198684,0.00058912055,0.00041759832,0.000005123267,0.00011769139,0.000030489542],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016028804,0.0000032605672,0.9788234,0.0000046473633,0.000031046293,0.000058319896,0.000120538585,0.012300017,0.00402357,0.00074740424,0.0003458877,0.0035258788],"study_design_scores_gemma":[0.00062597916,0.000427508,0.9508799,0.00022252878,0.000065553046,0.00016280766,0.0009820438,0.023906115,0.004565121,0.009257983,0.008426154,0.00047834232],"about_ca_topic_score_codex":0.064276874,"about_ca_topic_score_gemma":0.5561559,"teacher_disagreement_score":0.49187905,"about_ca_system_score_codex":0.0000062740824,"about_ca_system_score_gemma":0.00036389954,"threshold_uncertainty_score":0.9419542},"labels":[],"label_agreement":null},{"id":"W2461353620","doi":"10.1139/cjes-2016-0030","title":"Stratigraphy and structure of the Drake Point Anticline, Sabine Peninsula, Canadian Arctic Islands","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Institut national de la recherche scientifique; Suncor Energy Incorporated","keywords":"Anticline; Geology; Graben; Paleontology; Cretaceous; Paleozoic; Sill; Devonian; Syncline; Permian; Carboniferous; Geomorphology; Structural basin; Geochemistry","score_opus":0.013580319987454278,"score_gpt":0.18220736625489062,"score_spread":0.16862704626743635,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2461353620","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99189806,0.00076485856,0.000007501553,0.0057009878,0.0003509406,0.000052065272,0.00007948115,8.640092e-7,0.0011452162],"genre_scores_gemma":[0.99941415,0.000063874606,0.00018011508,0.00024313886,0.00006975862,2.9131188e-8,6.9386874e-7,6.8802626e-7,0.000027527029],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991526,0.00004483266,0.00022397755,0.0001045633,0.000186137,0.00028786325],"domain_scores_gemma":[0.99914384,0.00007249391,0.0001465701,0.00006814937,0.000119453856,0.0004495234],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029486933,0.000076237586,0.00013582243,0.00014348234,0.00041182915,0.00006179911,0.0002484671,0.00003619172,0.0010620604],"category_scores_gemma":[0.00021204994,0.000033200846,0.000048856728,0.0003520595,0.0006890903,0.0002400968,0.0000034593847,0.00008066739,0.000002662838],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000024532414,5.9638916e-7,0.9963013,0.0000026172713,0.000006196282,0.0000061484443,0.00013416838,0.00010268483,0.00008651353,0.00022574925,0.00008693271,0.0030446332],"study_design_scores_gemma":[0.00012387524,0.0002417735,0.9938625,0.000039171824,0.000007625478,0.000052036532,0.00030861882,0.000098799566,0.00008273528,0.0039055005,0.001218534,0.00005880175],"about_ca_topic_score_codex":0.2859104,"about_ca_topic_score_gemma":0.9898179,"teacher_disagreement_score":0.7039075,"about_ca_system_score_codex":0.0000017166931,"about_ca_system_score_gemma":0.00072971237,"threshold_uncertainty_score":0.9998511},"labels":[],"label_agreement":null},{"id":"W2461374265","doi":"10.1139/cjes-2012-0142","title":"Reply to the discussion of the reply by R.L. Romer and U. Kroner on “Geochemical signature of Ordovician Mn-rich sedimentary rocks on the Avalonian shelf” <sup>1</sup>Appears in the Canadian Journal of Earth Sciences, <b>49</b>(11): 1372–1377 [doi:10.1139/e2012-049].","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Zircon; Geology; Ordovician; Sedimentary rock; Paleontology; Argumentation theory; Geochemistry; Epistemology","score_opus":0.013908795362229522,"score_gpt":0.21385168347082634,"score_spread":0.1999428881085968,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2461374265","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9502937,0.004946205,0.0000014946105,0.037052028,0.0004973298,0.00027504237,0.00014701398,0.0000014748954,0.0067857173],"genre_scores_gemma":[0.9959208,0.000026041704,0.000102222235,0.0036387835,0.00018941295,7.761168e-7,0.0000018362887,0.0000025882227,0.00011753372],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.996374,0.0006903526,0.00073813106,0.00027838015,0.0010540831,0.0008650489],"domain_scores_gemma":[0.99744254,0.0005882057,0.00061956514,0.00036003714,0.00014583829,0.0008437912],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00573232,0.00025091693,0.00037719888,0.00052809954,0.0016354896,0.00019702598,0.0018620612,0.00013686455,0.0004459805],"category_scores_gemma":[0.0005439383,0.00009848916,0.00018064864,0.0014344379,0.0025792634,0.0005136801,0.000008967321,0.0009336382,0.0000057813895],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047137924,0.00002722755,0.97644216,0.0000072887215,0.000032361415,0.000024489123,0.006024198,0.0018038319,0.00008006145,0.00014871196,0.011588676,0.003773844],"study_design_scores_gemma":[0.00023137796,0.00089185324,0.9601881,0.00023300684,0.000037402035,0.00021764683,0.0044870004,0.0001500932,0.0004984445,0.00022797885,0.032665137,0.00017197827],"about_ca_topic_score_codex":0.09152127,"about_ca_topic_score_gemma":0.76659703,"teacher_disagreement_score":0.6750757,"about_ca_system_score_codex":0.000007959194,"about_ca_system_score_gemma":0.0024259612,"threshold_uncertainty_score":0.99966425},"labels":[],"label_agreement":null},{"id":"W2463599799","doi":"10.1139/cjes-2015-0169","title":"Geochemistry and diagenetic history of the Ordovician Lower Head Formation sandstones, western Newfoundland, Canada","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Brock University; Government of Newfoundland and Labrador; Memorial University of Newfoundland","funders":"","keywords":"Geology; Calcite; Diagenesis; Petrography; Cementation (geology); Geochemistry; Fluid inclusions; Authigenic; Arenite; Mineralogy; Quartz; Clastic rock; Sedimentary rock; Cement; Paleontology","score_opus":0.012204467784874933,"score_gpt":0.18762662739900943,"score_spread":0.1754221596141345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2463599799","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950779,0.0019896093,0.00015187215,0.0008432841,0.00047598904,0.000019341685,0.000004759632,0.0000016827021,0.0014355605],"genre_scores_gemma":[0.9993795,0.00006735424,0.000017018085,0.000079049874,0.000036966743,2.628718e-7,1.4804269e-7,0.0000024747087,0.00041723347],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99948466,0.000013690843,0.00017541753,0.000041430038,0.00016025556,0.00012455124],"domain_scores_gemma":[0.9995962,0.000019191168,0.00007108051,0.0000697804,0.000047227277,0.00019656878],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013140777,0.000049740705,0.000090202244,0.000078362296,0.000059722668,0.000015839792,0.00015692587,0.000020400455,0.00007214995],"category_scores_gemma":[0.000031407544,0.000027720853,0.000029628674,0.0001225391,0.0001591126,0.00015802837,0.0000040589143,0.00004543884,5.6878054e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007698627,0.000008869478,0.9410685,0.00010248741,0.000093001705,0.000058478174,0.0021666202,0.022122422,0.017893324,0.000045944496,0.0065525854,0.009880112],"study_design_scores_gemma":[0.0011547116,0.00017743127,0.52481675,0.0006310533,0.00009834662,0.0002492882,0.00082949264,0.015819112,0.0048275087,0.00017827321,0.45065692,0.00056113227],"about_ca_topic_score_codex":0.16081963,"about_ca_topic_score_gemma":0.99577206,"teacher_disagreement_score":0.8349524,"about_ca_system_score_codex":0.00006931723,"about_ca_system_score_gemma":0.0014569437,"threshold_uncertainty_score":0.8447685},"labels":[],"label_agreement":null},{"id":"W2466311310","doi":"10.1139/cjes-2015-0161","title":"Wenlock–Ludlow boundary interval revisited: new insights from the offshore facies of the Prague Synform, Czech Republic","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Grantová Agentura České Republiky","keywords":"Biozone; Conodont; Geology; Paleontology; Biostratigraphy; Baltica; Stratotype; Facies; Unconformity; Global Boundary Stratotype Section and Point; Stratigraphic unit; Ordovician; Sedimentary rock; Structural basin; Stage (stratigraphy)","score_opus":0.02339232516755222,"score_gpt":0.21387429066373667,"score_spread":0.19048196549618446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2466311310","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9587488,0.018599657,0.00005812276,0.006684157,0.001018424,0.00010364321,0.00011650881,0.0000041795465,0.014666499],"genre_scores_gemma":[0.998998,0.00009152849,0.00023256139,0.00030746238,0.00018253068,1.05840066e-7,7.4504567e-7,7.018133e-7,0.00018634851],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998431,0.0001746913,0.0004567792,0.00017411835,0.00041174892,0.00035164415],"domain_scores_gemma":[0.99835825,0.0004074783,0.00043089822,0.00024782008,0.00011616511,0.00043940314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000682858,0.00013372899,0.00024146537,0.00017568539,0.0007717336,0.00020045899,0.0013369019,0.00008304902,0.0006454322],"category_scores_gemma":[0.0004538588,0.00005360845,0.00018649019,0.00055205246,0.0019149494,0.00080911675,0.000004314656,0.00023519786,0.000008688868],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011509979,0.0000019843985,0.93835586,0.0000024722704,0.000034671437,0.000020468002,0.0007868802,0.000012901648,0.000040130788,0.0005078205,0.0026821804,0.057543114],"study_design_scores_gemma":[0.00014333417,0.00019241219,0.9740718,0.00017269078,0.000016850796,0.00009050026,0.00052387,0.00002284849,0.00021196534,0.0035861789,0.020878581,0.00008893834],"about_ca_topic_score_codex":0.015587998,"about_ca_topic_score_gemma":0.5404465,"teacher_disagreement_score":0.52485853,"about_ca_system_score_codex":0.0000018644442,"about_ca_system_score_gemma":0.0028229365,"threshold_uncertainty_score":0.9909673},"labels":[],"label_agreement":null},{"id":"W2467812658","doi":"10.1139/cjes-2016-0083","title":"Early–Middle Paleozoic ecosystem evolution and revolution (Part 1 of 2): an introduction","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University; Western University","funders":"","keywords":"Ordovician; Devonian; Paleozoic; Paleontology; Geology; Excursion; Peninsula; Extinction event; Archaeology; Geography; Law","score_opus":0.019515784587684937,"score_gpt":0.19635624679804334,"score_spread":0.1768404622103584,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2467812658","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99333555,0.0030857178,0.00012452467,0.00063409307,0.00078667677,0.00004990345,0.000038823684,0.0000032255728,0.0019415055],"genre_scores_gemma":[0.99913806,0.000036232108,0.00049470074,0.0000058664295,0.00030014786,9.764974e-8,4.633863e-7,4.0888824e-7,0.00002399793],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895567,0.00013533123,0.00031081348,0.00015608645,0.00018722375,0.00025490613],"domain_scores_gemma":[0.9990915,0.000057766334,0.00026737544,0.00008594394,0.000108742366,0.0003886779],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010979291,0.0000756505,0.00015835189,0.00033695647,0.0002942315,0.00003743974,0.0001856808,0.00006198895,0.0002017972],"category_scores_gemma":[0.00011466251,0.00004868859,0.00004380105,0.00026381487,0.000585169,0.00095022924,4.8815537e-7,0.000071960756,0.0000036780104],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000138457635,0.000002594331,0.97117513,0.000006730101,0.000008222728,0.000007640534,0.000107555075,0.000032735,0.00017124884,0.0007770991,0.000045406985,0.027651792],"study_design_scores_gemma":[0.0001554401,0.0006631068,0.9963102,0.00006061499,0.0000103146895,0.0001959613,0.00014206347,0.00011717774,0.00011859202,0.0013919972,0.0007641773,0.000070360875],"about_ca_topic_score_codex":0.0033292188,"about_ca_topic_score_gemma":0.45978585,"teacher_disagreement_score":0.45645663,"about_ca_system_score_codex":0.0000018656976,"about_ca_system_score_gemma":0.00051156426,"threshold_uncertainty_score":0.55007166},"labels":[],"label_agreement":null},{"id":"W2468359785","doi":"10.1139/e11-061","title":"Malley diabase dykes of the Slave craton, Canadian Shield: U–Pb age, paleomagnetism, and implications for continental reconstructions in the early Paleoproterozoic<sup>1</sup>Geological Survey of Canada Contribution 20110114.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Craton; Apparent polar wander; Paleomagnetism; Overprinting; Remanence; Geochemistry; Baddeleyite; Mafic; Archean; Clockwise; Paleontology; Fold (higher-order function); Zircon; Tectonics; Metamorphic rock; Magnetization","score_opus":0.020818250918294395,"score_gpt":0.20265409262503478,"score_spread":0.1818358417067404,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2468359785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939562,0.0010837283,0.00001273546,0.003462884,0.000115670475,0.00020830681,0.0006834233,6.913306e-7,0.00047634603],"genre_scores_gemma":[0.9994292,0.000023320526,0.00020033184,0.00026567772,0.00004070583,0.0000021068745,0.000018526347,8.189501e-7,0.000019292018],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985144,0.00023236338,0.0004391966,0.0001333618,0.00018210516,0.00049858034],"domain_scores_gemma":[0.9983653,0.00052633096,0.0002442341,0.00011528325,0.00021050862,0.0005383792],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014792217,0.00010559699,0.0002590382,0.0001435576,0.00040909232,0.000043994714,0.00043636144,0.00006701974,0.00067271927],"category_scores_gemma":[0.00085288665,0.000057340974,0.00007974975,0.0005928623,0.0009038618,0.00016969668,0.0000065786576,0.00017437102,7.018318e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000054166976,0.000005009624,0.99859357,0.0000029246432,0.000008804141,0.0000023325865,0.00013993248,0.0003058682,0.000020333782,0.0001931186,0.0001388686,0.0005838335],"study_design_scores_gemma":[0.00013909973,0.00013125179,0.9975863,0.000015699145,0.000020303776,0.00005379245,0.0003682198,0.00019364413,0.000060520535,0.0010240354,0.00033084166,0.00007629836],"about_ca_topic_score_codex":0.9758048,"about_ca_topic_score_gemma":0.9997506,"teacher_disagreement_score":0.023945818,"about_ca_system_score_codex":0.000004701783,"about_ca_system_score_gemma":0.001286501,"threshold_uncertainty_score":0.7365804},"labels":[],"label_agreement":null},{"id":"W2469151188","doi":"10.1139/e2012-019","title":"Recent changes in climate and permafrost temperatures at forested and polar desert sites in northern Canada<sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of<i>Fundamental and applied research on permafrost in Canada</i>.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa; Geological Survey of Canada","funders":"University of Ottawa","keywords":"Permafrost; Taiga; Boreal; Arctic; Climatology; Climate change; Hindcast; Snow; Environmental science; Physical geography; Forcing (mathematics); Tundra; Atmospheric sciences; Geology; Geography; Oceanography; Geomorphology","score_opus":0.045658323150439994,"score_gpt":0.24012211324869617,"score_spread":0.19446379009825618,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2469151188","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9900635,0.0022909485,3.5208342e-10,0.004105525,0.00007146111,0.0002047487,0.0019815513,4.0253528e-7,0.0012818835],"genre_scores_gemma":[0.99820817,0.0012368655,0.0000062186923,0.00039643527,0.000096751355,0.0000012056698,0.00003459705,0.0000037303707,0.000016015381],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980859,0.00016841735,0.00041527016,0.00019387674,0.0005329305,0.0006035735],"domain_scores_gemma":[0.998964,0.0003935918,0.00015169807,0.000104524115,0.00007110085,0.00031508916],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016025027,0.00014153915,0.00034138266,0.0005202667,0.00018912047,0.00007584494,0.00022419797,0.000050524042,0.00343819],"category_scores_gemma":[0.00014500943,0.00009921852,0.000014893117,0.00077254494,0.0006258947,0.0002901526,0.000026489162,0.00029366286,6.0347077e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015563091,0.000014604366,0.9883955,0.00003325794,0.000004929099,0.000021213242,0.009436496,0.00008848916,0.001072756,0.000019380419,0.0002960888,0.00046164406],"study_design_scores_gemma":[0.00037439927,0.00022110387,0.9775704,0.00018439653,0.0000031391353,0.000021535183,0.017615287,0.00011688066,0.0018423944,0.000015540192,0.0019295193,0.00010540319],"about_ca_topic_score_codex":0.975277,"about_ca_topic_score_gemma":0.9999889,"teacher_disagreement_score":0.024711862,"about_ca_system_score_codex":0.000056592355,"about_ca_system_score_gemma":0.0013580538,"threshold_uncertainty_score":0.9974728},"labels":[],"label_agreement":null},{"id":"W2471201622","doi":"10.1139/cjes-2016-0034","title":"Modelling the spatial distribution of permafrost in Labrador–Ungava using the temperature at the top of permafrost","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; Memorial University of Newfoundland; Parks Canada; Association of Canadian Universities for Northern Studies; University of Ottawa","keywords":"Permafrost; Subarctic climate; Geology; Snow; Land cover; Spatial distribution; Physical geography; Snow cover; Climatology; Geomorphology; Land use; Remote sensing; Geography; Oceanography","score_opus":0.04123899046393023,"score_gpt":0.23380532590047876,"score_spread":0.19256633543654852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2471201622","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9877209,0.0025597382,0.000055975474,0.002885085,0.00045396903,0.000109285844,0.0061145253,8.164206e-7,0.00009971755],"genre_scores_gemma":[0.9993921,0.00016267244,0.00001174904,0.00013034984,0.00018459526,1.5259135e-7,0.00005143683,0.0000021220528,0.000064847314],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985794,0.00015800256,0.00039096273,0.00012832867,0.00038720734,0.00035610114],"domain_scores_gemma":[0.9988592,0.0003763077,0.0002876764,0.0001749659,0.00014180387,0.00015999246],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013750612,0.000111915935,0.00018254478,0.00009912235,0.0006340047,0.00008883248,0.00061713293,0.000056213565,0.001686811],"category_scores_gemma":[0.00009237279,0.00004247225,0.00009534741,0.000482699,0.0011710905,0.00025672547,0.00001414849,0.00018105023,0.0000049612904],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023502478,0.0000030902365,0.9656587,0.0000063757298,0.0000065456347,0.000010249644,0.0020867193,0.02865251,0.0021308253,0.000053189644,0.0001581615,0.0012100777],"study_design_scores_gemma":[0.0003145449,0.00015841746,0.97018516,0.00023853332,0.000026161279,0.00013580367,0.002921177,0.019975252,0.0013529646,0.00013200383,0.0044129924,0.00014697935],"about_ca_topic_score_codex":0.083799966,"about_ca_topic_score_gemma":0.71349716,"teacher_disagreement_score":0.6296972,"about_ca_system_score_codex":0.000007842165,"about_ca_system_score_gemma":0.00066134497,"threshold_uncertainty_score":0.9992258},"labels":[],"label_agreement":null},{"id":"W2473015746","doi":"10.1139/e11-013","title":"Late stage rifting of the Laurentian continent: evidence from the geochemistry of greenstone and amphibolite in the central Vermont Appalachians<sup>1</sup>This article is one of a series of papers published in <i>CJES Special Issue: In honour of Ward Neale</i> on the theme of Appalachian and Grenvillian geology.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Memorial University of Newfoundland","keywords":"Geology; Greenschist; Geochemistry; Greenstone belt; Basalt; Metamorphic facies; Rift; Mafic; Igneous rock; Blueschist; Archean; Metamorphism; Petrology; Subduction; Tectonics; Eclogite; Facies; Paleontology","score_opus":0.014488506512233209,"score_gpt":0.1826898289054008,"score_spread":0.1682013223931676,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2473015746","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912637,0.0020660686,1.9420747e-7,0.0059361486,0.000039528502,0.000110768204,0.00011443697,4.175818e-7,0.0004687381],"genre_scores_gemma":[0.99951226,0.00020712285,0.000061594066,0.00013662587,0.00006373623,3.1782028e-7,0.0000021216636,0.0000011242932,0.000015087429],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998136,0.00029822983,0.00068714883,0.00014786399,0.00038160925,0.00034916413],"domain_scores_gemma":[0.9984358,0.00055736816,0.0006160491,0.00017756058,0.000076858596,0.00013636035],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018566693,0.00011891459,0.00041278475,0.000102496786,0.000089657835,0.000020926558,0.00060027326,0.000062772844,0.0016722293],"category_scores_gemma":[0.0005749932,0.00005576692,0.00009939607,0.00071884756,0.0020923,0.00023684063,0.000029661787,0.00027115512,2.0366863e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058827354,0.000027963173,0.9881796,0.000031534695,0.000021285912,0.0000019857289,0.008376002,0.0008088396,0.0016891765,0.00004584428,0.000019967747,0.00073892914],"study_design_scores_gemma":[0.00023475543,0.00011799651,0.98680264,0.0002621715,0.00002725683,0.000004240577,0.005507042,0.0006455791,0.005763752,0.00047258398,0.00010295019,0.000059011236],"about_ca_topic_score_codex":0.09087432,"about_ca_topic_score_gemma":0.34513378,"teacher_disagreement_score":0.25425947,"about_ca_system_score_codex":0.0000018854629,"about_ca_system_score_gemma":0.0001483976,"threshold_uncertainty_score":0.9992404},"labels":[],"label_agreement":null},{"id":"W2475279772","doi":"10.1139/cjes-2015-0229","title":"Different styles of modern and ancient non-collisional orogens and implications for crustal growth: a Gondwanaland perspective","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Terrane; Accretionary wedge; Forearc; Accretion (finance); Continental margin; Paleontology; Convergent boundary; Passive margin; Subduction; Plate tectonics; Cretaceous; Tectonics; Earth science; Oceanic crust; Rift","score_opus":0.017350439169270922,"score_gpt":0.21368621096047727,"score_spread":0.19633577179120634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2475279772","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99335605,0.001811351,0.00042707718,0.0037101163,0.000029415052,0.00006081287,0.0002503191,9.383194e-7,0.00035391047],"genre_scores_gemma":[0.9991067,0.000084366584,0.00066426833,0.00008084223,0.000033548687,4.0566837e-7,0.0000012727904,6.5425803e-7,0.000027943877],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99927616,0.000017015034,0.0001937536,0.00016048852,0.00012648088,0.00022607988],"domain_scores_gemma":[0.99888605,0.00024034994,0.00012050939,0.00004185987,0.00024192984,0.00046930622],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002371987,0.00007589121,0.00017982785,0.0001583184,0.00022562905,0.000041435564,0.00014643476,0.000028547733,0.00028794497],"category_scores_gemma":[0.0002158642,0.000037798643,0.00006706643,0.00017757474,0.0006846852,0.00013956826,0.000006568299,0.0000393402,7.3138705e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010549955,0.000005665511,0.9942144,0.0000037092432,0.00001818971,0.0000016025177,0.00012007939,0.00004756632,0.0011547767,0.0012559044,0.000032915454,0.003134626],"study_design_scores_gemma":[0.00018818757,0.0002864532,0.9577562,0.00002052722,0.000023493789,0.000035364304,0.00025256406,0.0006388117,0.0003727656,0.04027041,0.00008958175,0.00006564643],"about_ca_topic_score_codex":0.0037844393,"about_ca_topic_score_gemma":0.13399497,"teacher_disagreement_score":0.13021053,"about_ca_system_score_codex":0.0000018641953,"about_ca_system_score_gemma":0.00024836912,"threshold_uncertainty_score":0.8818074},"labels":[],"label_agreement":null},{"id":"W2481487517","doi":"10.1139/cjes-2016-0026","title":"Precambrian to Early Cretaceous rocks of the Strandja Massif (northwestern Turkey): evolution of a long lasting magmatic arc","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Massif; Carboniferous; Devonian; Nappe; Paleontology; Paleozoic; Ordovician; Precambrian; Geochemistry; Basement; Permian; Cretaceous; Tectonics; Structural basin","score_opus":0.01235733786223421,"score_gpt":0.1822230361326197,"score_spread":0.1698656982703855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2481487517","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99693066,0.00037905452,0.00041542578,0.00087629736,0.00015553774,0.00006657487,0.000044168442,0.0000017661936,0.0011305051],"genre_scores_gemma":[0.9994099,0.0000037917619,0.00031395376,0.000036776015,0.000049108963,1.2098808e-7,2.9505284e-7,9.3204136e-7,0.00018513594],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986365,0.00008418813,0.00042628654,0.00013949923,0.0003871628,0.00032638042],"domain_scores_gemma":[0.9987746,0.00017433339,0.00033105596,0.000108203,0.0001638934,0.00044794916],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005515344,0.00009251058,0.00023024052,0.00019057166,0.00016628856,0.000040098017,0.00054832455,0.000039342845,0.001282566],"category_scores_gemma":[0.00028396092,0.000042794905,0.00014344063,0.000634091,0.0004499897,0.00020761383,0.000010204102,0.000087975815,0.000014410576],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008457519,0.0000029912162,0.9880157,0.00000812353,0.000011955767,0.000008263793,0.0001373128,0.0026587616,0.00046254758,0.000008943426,0.000005909951,0.008671029],"study_design_scores_gemma":[0.000117205294,0.00029127207,0.9963513,0.00017852282,0.000025233745,0.00003859543,0.00014548466,0.00033747838,0.001059593,0.0012978194,0.00008608422,0.00007141325],"about_ca_topic_score_codex":0.04275959,"about_ca_topic_score_gemma":0.70154244,"teacher_disagreement_score":0.6587829,"about_ca_system_score_codex":0.000002952539,"about_ca_system_score_gemma":0.00050047546,"threshold_uncertainty_score":0.9996304},"labels":[],"label_agreement":null},{"id":"W2481840238","doi":"10.1139/cjes-2016-0032","title":"U–Pb zircon geochronology from the Alexander terrane, southeast Alaska: implications for the Greens Creek massive sulphide deposit","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Zircon; Geology; Geochemistry; Geochronology; Metamorphism; Mafic; Terrane; Permian; Unconformity; Rhyolite; Mineralization (soil science); Metamorphic rock; Volcanic rock; Paleontology; Sedimentary rock; Volcano; Structural basin; Tectonics","score_opus":0.028784706900124826,"score_gpt":0.2095326464568343,"score_spread":0.18074793955670948,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2481840238","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8897602,0.002545371,0.0044085914,0.101220526,0.00031954423,0.0001621515,0.00044466005,0.0000054651337,0.0011334933],"genre_scores_gemma":[0.9976468,0.000054241904,0.00078333967,0.0010262894,0.00027454057,0.0000014542629,0.000005847971,0.0000013361437,0.00020615062],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99884385,0.000070704504,0.00028434774,0.00020301316,0.00015075604,0.0004473236],"domain_scores_gemma":[0.99770576,0.0014155016,0.000194473,0.00017014422,0.00014230644,0.00037179285],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000463314,0.00010464417,0.00017363673,0.00006263112,0.00095310336,0.00013287932,0.00084352045,0.000055217686,0.0055064186],"category_scores_gemma":[0.00032762092,0.000041277824,0.00016490181,0.00027927646,0.0012023221,0.00016767213,0.000009152167,0.000118913194,0.000056467143],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008084009,0.000002523735,0.9847347,6.6473604e-7,0.00004836073,0.00000499667,0.000088411194,0.00033406593,0.00043607515,0.00013930423,0.0008542865,0.013348514],"study_design_scores_gemma":[0.00017325756,0.00014019915,0.9766841,0.000015723686,0.000060045797,0.000048063448,0.0003815217,0.00020616349,0.00019364733,0.015623187,0.00638601,0.00008809487],"about_ca_topic_score_codex":0.07889545,"about_ca_topic_score_gemma":0.86663073,"teacher_disagreement_score":0.7877353,"about_ca_system_score_codex":0.0000019730599,"about_ca_system_score_gemma":0.00037762537,"threshold_uncertainty_score":0.9954027},"labels":[],"label_agreement":null},{"id":"W2488560262","doi":"10.1139/cjes-2016-0053","title":"A new hesperornithiform (Aves) specimen from the Late Cretaceous Canadian High Arctic with comments on high-latitude hesperornithiform diet","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature","funders":"Office of Polar Programs; University of Colorado Boulder; National Science Foundation","keywords":"Cretaceous; Arctic; High latitude; Geology; Latitude; Paleontology; Trophic level; Stage (stratigraphy); Oceanography","score_opus":0.017398258882546737,"score_gpt":0.19556925278220197,"score_spread":0.17817099389965524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2488560262","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9732848,0.0008401064,0.000044159642,0.021368537,0.0009018219,0.00013233903,0.0004123262,0.0000059427657,0.003009985],"genre_scores_gemma":[0.99534714,0.00007100116,0.0011146036,0.002573903,0.00033503064,3.5528902e-7,0.000019373192,0.0000035096102,0.0005351041],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981338,0.00014060618,0.0003325068,0.00024784784,0.0003329553,0.00081230886],"domain_scores_gemma":[0.99756366,0.00049143034,0.00023399832,0.0002180155,0.00009325266,0.001399657],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00062570215,0.00021217047,0.0002761816,0.00027494517,0.0010028108,0.00011056606,0.00088448887,0.000118798685,0.00910029],"category_scores_gemma":[0.0001245669,0.00010017357,0.00006339134,0.0003355642,0.0010318203,0.0004548197,0.0000058035703,0.0003061856,0.0004601393],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012217811,0.0000032106398,0.9930604,9.5153905e-7,0.00006052766,0.00017330397,0.00026982164,0.00106101,0.0000035085334,0.00033251903,0.00104529,0.003867272],"study_design_scores_gemma":[0.0005106489,0.0013556144,0.9624441,0.000112308495,0.000024803738,0.00015008134,0.00015665479,0.000051953364,0.0000148040735,0.0029225214,0.032071907,0.00018456552],"about_ca_topic_score_codex":0.77200294,"about_ca_topic_score_gemma":0.9976893,"teacher_disagreement_score":0.22568639,"about_ca_system_score_codex":0.000024641482,"about_ca_system_score_gemma":0.003457364,"threshold_uncertainty_score":0.99180555},"labels":[],"label_agreement":null},{"id":"W2494206980","doi":"10.1139/cjes-2015-0184","title":"Redox conditions of the Late Cretaceous Western Interior Seaway recorded by rare earth elements of Bearpaw molluscan fossils","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University; Queen's University; University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey","keywords":"Geology; Cretaceous; Brackish water; Ammonite; Fauna; Nekton; Paleontology; Benthic zone; Sedimentary rock; Water column; Oceanography; Ecology; Biology; Estuary; Salinity","score_opus":0.011424475373432434,"score_gpt":0.20856171281753014,"score_spread":0.1971372374440977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2494206980","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99550426,0.00044247898,0.000009869491,0.0011934119,0.0002446016,0.000064711385,0.0006537527,0.000001655314,0.0018852449],"genre_scores_gemma":[0.99743915,0.000037210466,0.00010964129,0.00009181451,0.000031969976,2.0832819e-7,0.000006214974,0.000001530938,0.0022822453],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99858105,0.00008313425,0.0005156105,0.00013270372,0.00035499796,0.00033251802],"domain_scores_gemma":[0.9987491,0.000069786816,0.00052530196,0.0001497883,0.00013241192,0.0003736434],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00055639097,0.000108120774,0.00023543191,0.00013853738,0.00029608788,0.000053104843,0.0006107668,0.000038906506,0.0046046823],"category_scores_gemma":[0.000097794255,0.00005966355,0.00015091144,0.00044889483,0.0007623376,0.00031132804,0.000010754568,0.000090297995,0.000012010925],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000098599185,0.0000050674207,0.98594683,0.000010133763,0.00004607027,0.000008201987,0.0001771149,0.000115597104,0.008499698,0.0000028148909,0.0005250322,0.0046535544],"study_design_scores_gemma":[0.0006782196,0.0006917505,0.912927,0.00047840498,0.00009393534,0.00010768765,0.0012037734,0.00016705482,0.06814001,0.0004623771,0.014791481,0.00025831634],"about_ca_topic_score_codex":0.00737637,"about_ca_topic_score_gemma":0.22039913,"teacher_disagreement_score":0.21302277,"about_ca_system_score_codex":0.0000025734662,"about_ca_system_score_gemma":0.0006128051,"threshold_uncertainty_score":0.9992336},"labels":[],"label_agreement":null},{"id":"W2495304870","doi":"10.1139/cjes-2015-0213","title":"<i>Lesleya</i> Lesquereux from the Pennsylvanian of the Iberian Massif: part of a dryland megaflora from the Variscan orogen, northwestern Portugal","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada; Česká geologická služba; Ministério da Ciência, Tecnologia e Ensino Superior; Grantová Agentura České Republiky","keywords":"Pennsylvanian; Carboniferous; Geology; Massif; Paleontology; Permian; Paleozoic; Fluvial; Structural basin; Coal measures; Oil shale","score_opus":0.026955319481670976,"score_gpt":0.17039585365194354,"score_spread":0.14344053417027255,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2495304870","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98610634,0.00039512236,0.000002520786,0.011582024,0.00046436256,0.000073105075,0.0010625517,0.0000018439159,0.00031211923],"genre_scores_gemma":[0.99912757,0.000057703608,0.00002109136,0.00041292096,0.00029462972,2.8701632e-7,0.00000461315,4.9114095e-7,0.00008068945],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998763,0.00016161204,0.0002970188,0.00014265481,0.00037511287,0.00026058647],"domain_scores_gemma":[0.9987196,0.000439976,0.0004216223,0.000095026466,0.00011266829,0.0002111415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006203759,0.00009737698,0.00017159128,0.000013847054,0.00058080524,0.000075186006,0.0011841921,0.000056465364,0.00050618174],"category_scores_gemma":[0.00009849284,0.000022505626,0.0001392056,0.00031140252,0.00080116745,0.000251438,0.00004818931,0.0001133095,0.000006964984],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015779466,0.000009066935,0.98255676,5.8930704e-7,0.00002687404,0.000008256036,0.0004921465,0.000009541968,0.01115718,0.00010003259,0.0019709852,0.0036527829],"study_design_scores_gemma":[0.00011742936,0.000112292015,0.96172464,0.000110301364,0.000030745756,0.000016119504,0.0012524386,0.000004965128,0.0012974648,0.00069969374,0.034562,0.00007192691],"about_ca_topic_score_codex":0.09166088,"about_ca_topic_score_gemma":0.8201374,"teacher_disagreement_score":0.72847646,"about_ca_system_score_codex":0.000007744389,"about_ca_system_score_gemma":0.00034015422,"threshold_uncertainty_score":0.9143878},"labels":[],"label_agreement":null},{"id":"W2502013307","doi":"10.1139/cjes-2016-0066","title":"The pattern and style of deglaciation at the Late Wisconsinan Laurentide and Cordilleran ice sheet limits in northeastern British Columbia","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of British Columbia; University of the Fraser Valley; Geological Survey of Canada","funders":"","keywords":"Geology; Deglaciation; Meltwater; Moraine; Ice sheet; Wisconsin glaciation; Glacial period; Glacier; Geomorphology; Glacial landform; Ice stream; Crevasse; Plateau (mathematics); Glacier morphology; Paleontology; Physical geography; Cryosphere; Oceanography; Sea ice; Geography","score_opus":0.015002570789413125,"score_gpt":0.20608816783676553,"score_spread":0.1910855970473524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2502013307","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937057,0.0031992206,0.0000013533585,0.0022363823,0.00016078002,0.00006472631,0.000019626048,6.5182724e-7,0.00061156385],"genre_scores_gemma":[0.9986995,0.0003773145,0.000007779507,0.00007724041,0.000012499415,1.6979557e-7,7.2151073e-7,7.7479e-7,0.0008240264],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991157,0.00017898776,0.00020341593,0.00009481118,0.00012840588,0.0002786665],"domain_scores_gemma":[0.99910045,0.00049281656,0.00013137683,0.00006057894,0.000060250506,0.00015450406],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012191123,0.000043449047,0.000112865935,0.000054597127,0.0009075376,0.00024558432,0.00020196993,0.000037692385,0.00036537275],"category_scores_gemma":[0.00014448751,0.000027246318,0.000018621326,0.00014924679,0.0016105893,0.00018251127,0.000007631979,0.000099414414,0.000006057402],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004776433,8.7392834e-7,0.97796774,0.0000024365675,0.0000049139476,0.00002300089,0.00014824864,0.000017356124,0.0000046704836,9.947144e-7,0.0000628803,0.021762101],"study_design_scores_gemma":[0.00021132077,0.00012446837,0.997945,0.00005794921,0.000003901359,0.0003201217,0.00024641154,0.00013849081,0.00000681904,0.00011926431,0.0007870328,0.000039219376],"about_ca_topic_score_codex":0.09393533,"about_ca_topic_score_gemma":0.99853736,"teacher_disagreement_score":0.90460205,"about_ca_system_score_codex":4.5796023e-7,"about_ca_system_score_gemma":0.00027524063,"threshold_uncertainty_score":0.9120982},"labels":[],"label_agreement":null},{"id":"W2504130073","doi":"10.1139/cjes-2015-0212","title":"Transtensional origin of multi-order cross-folds in a high-grade gneiss complex, southwestern Grenville Province: formation during post-peak gravitational collapse","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"TD Bank Group; Memorial University of Newfoundland; BP (Canada); University of Toronto","funders":"","keywords":"Geology; Lineation; Metamorphism; Gneiss; Transtension; Hinge; Shear zone; Metamorphic core complex; Petrology; Fold (higher-order function); Seismology; Metamorphic rock; Extensional definition; Physics; Tectonics","score_opus":0.024862292170890643,"score_gpt":0.22824385252915913,"score_spread":0.2033815603582685,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2504130073","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977574,0.0001891016,0.000045799337,0.0015467755,0.00011177933,0.000073321346,0.00020610043,0.0000022332563,0.000067505054],"genre_scores_gemma":[0.9979105,0.00000842763,0.0018238347,0.000113939976,0.00003917992,2.965735e-7,0.000014499484,0.0000012334829,0.000088078625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984793,0.00007055384,0.0005153725,0.00017146707,0.00039569504,0.00036758147],"domain_scores_gemma":[0.9988739,0.00013612914,0.00024949072,0.00006187732,0.00028929362,0.00038932645],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048014274,0.00011456307,0.00024429298,0.00038038843,0.00021821301,0.000061803505,0.00031587007,0.000054831093,0.0024682633],"category_scores_gemma":[0.0001537939,0.000066330605,0.00009608926,0.00058702554,0.00064724934,0.00045034278,0.0000048775078,0.00009432926,0.000024325589],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002750504,0.0000144437745,0.9904281,0.000012044104,0.000008494226,0.000039378334,0.00017125411,0.004235338,0.0043792375,0.000074251446,0.0000038060396,0.00060614065],"study_design_scores_gemma":[0.0007530902,0.00018217694,0.9958552,0.000060405087,0.000008425779,0.000068719724,0.0002099199,0.0009654491,0.00057855796,0.0010922278,0.000112564514,0.00011323841],"about_ca_topic_score_codex":0.01958009,"about_ca_topic_score_gemma":0.6479327,"teacher_disagreement_score":0.6283526,"about_ca_system_score_codex":0.000004586216,"about_ca_system_score_gemma":0.000655829,"threshold_uncertainty_score":0.9984436},"labels":[],"label_agreement":null},{"id":"W2505501905","doi":"10.1139/cjes-2015-0196","title":"<sup>40</sup>Ar/<sup>39</sup>Ar thermochronology of the Thor-Odin – Pinnacles area, southeastern British Columbia: tectonic implications of cooling and exhumation patterns","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University; Cape Breton University","funders":"Forskningsrådet om Hälsa, Arbetsliv och Välfärd; Natural Sciences and Engineering Research Council of Canada; Queen's University","keywords":"Thermochronology; Geology; Geochronology; Dome (geology); Biotite; Hornblende; Closure temperature; Muscovite; Zircon; Basement; Geochemistry; Metamorphic rock; Foreland basin; Cretaceous; Tectonics; Paleontology; Quartz","score_opus":0.017125355300827372,"score_gpt":0.19041192531322562,"score_spread":0.17328657001239825,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2505501905","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962361,0.00087430887,0.0000906871,0.0018535388,0.00004173197,0.00008881412,0.00023117675,0.000003543973,0.0005801139],"genre_scores_gemma":[0.9994977,0.00010138528,0.00012812475,0.0001194935,0.000051190622,6.224445e-7,0.0000033029003,0.0000018592996,0.00009628442],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985382,0.00012220907,0.000489214,0.00022521423,0.00024729874,0.0003778864],"domain_scores_gemma":[0.99871594,0.00022808276,0.000381875,0.00015949484,0.00019594765,0.00031868412],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005744135,0.00010154189,0.0003004314,0.0001253099,0.00037959547,0.00012120313,0.0005790452,0.0000815374,0.0060049235],"category_scores_gemma":[0.0002406687,0.00006852193,0.00013285263,0.00042537446,0.0011886068,0.00022990037,0.000020974037,0.0001368628,0.0000080855325],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000041044445,0.000006313756,0.97766715,0.000008781208,0.00002229217,0.000003519174,0.00018320522,0.0015102638,0.0002637389,0.000014504571,0.00003126794,0.020284882],"study_design_scores_gemma":[0.00017602308,0.00016917047,0.9933017,0.00015059116,0.00003534963,0.00012946148,0.0006156954,0.0016945924,0.00014051133,0.0033311234,0.00015399113,0.00010178503],"about_ca_topic_score_codex":0.08737419,"about_ca_topic_score_gemma":0.67677015,"teacher_disagreement_score":0.58939594,"about_ca_system_score_codex":0.0000027992508,"about_ca_system_score_gemma":0.00038812216,"threshold_uncertainty_score":0.99490374},"labels":[],"label_agreement":null},{"id":"W2508974167","doi":"10.1139/cjes-2016-0098","title":"Depositional timing of Neoarchean turbidites of the Slave craton—recommended nomenclature and type localities","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto; Government of Northwest Territories; University of Calgary; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Turbidite; Zircon; Craton; Sedimentary depositional environment; Geochemistry; Felsic; Banded iron formation; Sedimentary rock; Population; Paleontology; Mafic; Structural basin; Tectonics","score_opus":0.024874203483333662,"score_gpt":0.1996541502259749,"score_spread":0.17477994674264125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2508974167","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99389446,0.0010518616,0.000013327279,0.0032290842,0.00011554729,0.000020142097,0.000036744612,7.161855e-7,0.001638105],"genre_scores_gemma":[0.9990858,0.000027780092,0.00060595997,0.00016567545,0.000039909315,2.8110342e-8,7.5335834e-7,4.5001164e-7,0.000073681236],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99927634,0.00005107532,0.00022018398,0.000082245395,0.0001940527,0.0001761211],"domain_scores_gemma":[0.99922484,0.00022115205,0.00016492739,0.000051265386,0.00012443459,0.00021340283],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003300204,0.000058905443,0.00014446513,0.00009530759,0.00014192135,0.000020705778,0.00024741914,0.00003341704,0.0029306274],"category_scores_gemma":[0.00017866908,0.000025725778,0.000064280655,0.00030564918,0.0008290248,0.00012752676,0.000007711918,0.00007625263,0.0000023090636],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007227882,0.0000026372911,0.99363154,0.0000061184937,0.000015504178,0.000003596335,0.000132133,0.00009963964,0.0010830422,0.00029520644,0.00009689941,0.0046264315],"study_design_scores_gemma":[0.0001149244,0.00025185023,0.96748245,0.00009421465,0.000020615693,0.000055569093,0.00027653849,0.0002730164,0.007055057,0.023715433,0.0005858494,0.00007448678],"about_ca_topic_score_codex":0.0047824536,"about_ca_topic_score_gemma":0.088088095,"teacher_disagreement_score":0.08330564,"about_ca_system_score_codex":8.214695e-7,"about_ca_system_score_gemma":0.00032393835,"threshold_uncertainty_score":0.99798083},"labels":[],"label_agreement":null},{"id":"W2510985717","doi":"10.1139/cjes-2015-0236","title":"Holocene glacier history of Frank Mackie Glacier, northern British Columbia Coast Mountains","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Ministry of Environment; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Glacier; Geology; Moraine; Holocene; Radiocarbon dating; Physical geography; Glacier mass balance; Tidewater glacier cycle; Archaeology; Geomorphology; Oceanography; Paleontology; Geography; Ice calving","score_opus":0.02015450103049895,"score_gpt":0.20742675101754227,"score_spread":0.1872722499870433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2510985717","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.988686,0.0050619454,0.000015590464,0.00046357486,0.0010109473,0.000067590976,0.00008084147,0.000004052465,0.0046094414],"genre_scores_gemma":[0.9958496,0.00017984267,0.00019245537,0.00020999789,0.00008320599,2.2245739e-7,0.0000025706477,0.0000025339307,0.0034795525],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981734,0.00017263502,0.00040581822,0.00021863921,0.00037843155,0.00065106334],"domain_scores_gemma":[0.99833894,0.00024268647,0.00026460798,0.00013922085,0.00029743157,0.00071711687],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013463598,0.00009445101,0.0002973736,0.00023269634,0.0003277577,0.000081409664,0.0006935303,0.00012280342,0.010342498],"category_scores_gemma":[0.00031253032,0.00008666242,0.00010553704,0.00028619013,0.0029673162,0.00040137637,0.000008060261,0.00021663842,0.000109654124],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000090522935,0.000005473821,0.99427783,0.0000069968214,0.000015924143,0.00026933342,0.00013498556,0.000039032828,0.000009269,0.0000089189825,0.0014479364,0.0037752464],"study_design_scores_gemma":[0.00035401844,0.00035210577,0.9848586,0.0000658303,0.000010152634,0.00091242377,0.00013355834,0.000035763947,0.00001098974,0.0004261827,0.012720967,0.00011941631],"about_ca_topic_score_codex":0.171853,"about_ca_topic_score_gemma":0.9875617,"teacher_disagreement_score":0.8157087,"about_ca_system_score_codex":0.000004460462,"about_ca_system_score_gemma":0.0042635994,"threshold_uncertainty_score":0.999746},"labels":[],"label_agreement":null},{"id":"W2513227079","doi":"10.1139/cjes-2016-0109","title":"The provenance of Jurassic and Lower Cretaceous clastic sediments offshore southwestern Nova Scotia","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada; Natural Resources Canada; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Provenance; Clastic rock; Terrane; Geochemistry; Sedimentary rock; Cretaceous; Heavy mineral; Ultramafic rock; Paleontology; Tectonics","score_opus":0.011664054981260046,"score_gpt":0.19638440690194608,"score_spread":0.18472035192068603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2513227079","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959015,0.0013709922,0.0000150802025,0.0009193908,0.00032276852,0.00003482498,0.000038003123,0.000001007584,0.0013963936],"genre_scores_gemma":[0.9994625,0.000035408986,0.00008131699,0.000053520806,0.00005714106,3.790173e-8,5.701326e-7,9.0753366e-7,0.0003086077],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990374,0.000028347384,0.00026199094,0.00012048359,0.00025554726,0.0002962462],"domain_scores_gemma":[0.9991684,0.00011929196,0.00022650795,0.000080412065,0.00007724454,0.00032815392],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005040423,0.000080856196,0.00013081434,0.00007510221,0.00026395518,0.000087919616,0.00031445257,0.000025114852,0.000689847],"category_scores_gemma":[0.00008887113,0.000038277445,0.000053584637,0.00023167544,0.0008362896,0.0002387837,0.0000053254253,0.000063344676,0.000022419577],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009596797,0.0000022456857,0.9867157,0.000005075883,0.000018964682,0.000019119998,0.000093473915,0.000088831745,0.0002927951,0.000009190014,0.00008122295,0.012663804],"study_design_scores_gemma":[0.00026596355,0.00045684315,0.99118024,0.00017027787,0.000039509712,0.00012754666,0.00058566296,0.0002300516,0.0015866631,0.00060537853,0.004617205,0.0001346322],"about_ca_topic_score_codex":0.0033556477,"about_ca_topic_score_gemma":0.2940051,"teacher_disagreement_score":0.29064944,"about_ca_system_score_codex":0.0000013501715,"about_ca_system_score_gemma":0.00044084678,"threshold_uncertainty_score":0.7553341},"labels":[],"label_agreement":null},{"id":"W2513434176","doi":"10.1139/cjes-2016-0073","title":"Age and tectonic setting of granitoid plutons in the Chéticamp belt, western Cape Breton Island, Nova Scotia, Canada","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Technical University of Nova Scotia; Cape Breton University; Nova Scotia Department of Energy; Acadia University","funders":"Natural Sciences and Engineering Research Council of Canada; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; Cape Breton University","keywords":"Pluton; Geology; Zircon; Geochemistry; Terrane; Ordovician; Petrography; Devonian; Metamorphic rock; Metamorphism; Continental arc; Volcanic rock; Paleontology; Tectonics; Volcano","score_opus":0.01181784564642138,"score_gpt":0.18485983995886102,"score_spread":0.17304199431243963,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2513434176","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932392,0.0008068307,0.000004867724,0.004615066,0.00011275408,0.00003950586,0.00004578282,7.55198e-7,0.0011352418],"genre_scores_gemma":[0.99945366,0.000019951638,0.000075687094,0.00037080306,0.00004659464,5.1073506e-8,0.0000013708327,7.061743e-7,0.00003119222],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988076,0.00008066781,0.00030022726,0.0001376319,0.00030882526,0.00036504038],"domain_scores_gemma":[0.99909884,0.00033034786,0.00015204301,0.0000773774,0.000051869298,0.00028954295],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00075823074,0.000089264475,0.00020402788,0.00014889894,0.00014463803,0.00005487101,0.00042744167,0.00003172542,0.0012524725],"category_scores_gemma":[0.0002051152,0.0000413303,0.000046786507,0.0005163893,0.0005258551,0.00014515968,0.000006126162,0.00013296433,0.0000049169835],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000259989,0.0000017398229,0.99634725,0.0000035432743,0.0000056433946,0.00009770865,0.00015209896,0.00012398303,0.00012221691,0.000012596351,0.000048191552,0.0030824412],"study_design_scores_gemma":[0.00013975191,0.00011758893,0.9974618,0.000055111188,0.000011482072,0.000113146976,0.0003515363,0.00008063297,0.00010227247,0.0008447058,0.00064411847,0.000077862736],"about_ca_topic_score_codex":0.93048614,"about_ca_topic_score_gemma":0.9998938,"teacher_disagreement_score":0.069407634,"about_ca_system_score_codex":0.0000024235121,"about_ca_system_score_gemma":0.00089881197,"threshold_uncertainty_score":0.9996605},"labels":[],"label_agreement":null},{"id":"W2517601114","doi":"10.1139/cjes-2016-0129","title":"Theorems in pure mathematics can be proved right but the models used in applied mathematics, natural and social science, as well as in engineering, can at most be “not yet proved wrong”","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Philosophy and History of Science","field":"Arts and Humanities","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Division of Mathematical Sciences","keywords":"Mathematics; Publication; Natural (archaeology); Universe; Property (philosophy); Mathematics education; Pure mathematics; Epistemology; Physics; Philosophy; Geology; Law; Political science","score_opus":0.02748581518476849,"score_gpt":0.20125107314727347,"score_spread":0.17376525796250497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2517601114","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.959721,0.000089466506,0.0000018398913,0.0071455436,0.00034159733,0.0002867685,0.000031392432,0.000005344151,0.03237704],"genre_scores_gemma":[0.9981769,0.0000057483276,0.00014831034,0.0004654837,0.00009182413,0.0000062080308,3.5216289e-7,0.000007832655,0.0010973589],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9981998,0.000021784934,0.0004302224,0.00024495966,0.0005444513,0.00055878854],"domain_scores_gemma":[0.9991905,0.00011623196,0.0002391137,0.00012059736,0.00008553894,0.0002479804],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0016022216,0.00017198607,0.00027642708,0.000714418,0.0008043426,0.00033904344,0.000801937,0.00004544349,0.00018520915],"category_scores_gemma":[0.00012016495,0.0000995491,0.000038988113,0.00031343964,0.0040574083,0.00057292235,0.000039825893,0.00025430435,0.000004086422],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000114275135,0.00003546046,0.00033010196,0.00003417846,0.0000049576565,0.000049244474,0.09662849,0.000108813605,0.003750364,0.89878595,0.00009938812,0.00016162694],"study_design_scores_gemma":[0.0067017023,0.0014603228,0.0067935726,0.002285284,0.00007821852,0.000558326,0.11264964,0.031512376,0.011395213,0.75557953,0.06785274,0.003133042],"about_ca_topic_score_codex":0.004001932,"about_ca_topic_score_gemma":0.49766785,"teacher_disagreement_score":0.49366593,"about_ca_system_score_codex":0.00012567837,"about_ca_system_score_gemma":0.001824318,"threshold_uncertainty_score":0.998653},"labels":[],"label_agreement":null},{"id":"W2520135906","doi":"10.1139/cjes-2016-0080","title":"Latest Cretaceous eggshell assemblage from the Willow Creek Formation (upper Maastrichtian – lower Paleocene) of Alberta, Canada, reveals higher dinosaur diversity than represented by skeletal remains","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; University of Alberta; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; University of Calgary","keywords":"Willow; Cretaceous; Geology; Paleontology; Eggshell; Assemblage (archaeology); Taxon; Ecology; Biology","score_opus":0.013040629245473154,"score_gpt":0.18910552031417832,"score_spread":0.17606489106870515,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2520135906","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98780835,0.0016588805,0.000025910915,0.005706621,0.0008800006,0.00007820328,0.00047586276,0.000002491984,0.0033636973],"genre_scores_gemma":[0.99839693,0.00007791074,0.00007222041,0.0003931835,0.00011764113,1.2474193e-7,0.000022062133,0.0000014783457,0.0009184526],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99836445,0.00024292184,0.00037072052,0.00020811903,0.00033597965,0.0004777898],"domain_scores_gemma":[0.9981658,0.0007158521,0.00038025962,0.00017110286,0.00012739633,0.00043961502],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005904543,0.00013016381,0.00023758454,0.000095780095,0.0007450997,0.000037719925,0.00069383124,0.0001039295,0.0022357325],"category_scores_gemma":[0.00027195175,0.000076434495,0.00009164862,0.00028653062,0.00074767397,0.0005806015,0.000017316554,0.00015174664,0.00001998379],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001530742,0.000003927357,0.9881578,0.0000017650045,0.000024563305,0.00006348677,0.00010348719,0.00004073107,0.00007793119,0.000010362493,0.011013925,0.00048670836],"study_design_scores_gemma":[0.00020649529,0.00019371994,0.98224723,0.00004979003,0.000021702506,0.0000825395,0.00014822997,0.000072677736,0.000040347826,0.00022430008,0.016598284,0.000114674374],"about_ca_topic_score_codex":0.88783735,"about_ca_topic_score_gemma":0.9991498,"teacher_disagreement_score":0.111312464,"about_ca_system_score_codex":0.000008731548,"about_ca_system_score_gemma":0.0009792981,"threshold_uncertainty_score":0.99867636},"labels":[],"label_agreement":null},{"id":"W2522379810","doi":"10.1139/cjes-2016-0099","title":"Landscape evolution in Africa during the Cenozoic and Quaternary—the legacy and limitations of Lester C. King","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Ice sheet; Quaternary; Global cooling; Glacial period; Paleontology; Plate tectonics; Antarctic ice sheet; Cenozoic; Tectonics; Climatology; Oceanography; Climate change; Cryosphere; Sea ice","score_opus":0.04361623503154942,"score_gpt":0.22474434125387008,"score_spread":0.18112810622232067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2522379810","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912894,0.002837455,0.0000052284095,0.004452786,0.00008910384,0.000036830006,0.000002727648,5.582071e-7,0.0012859529],"genre_scores_gemma":[0.99967116,0.00016729576,0.000039773215,0.000022113141,0.000021842998,1.3294269e-7,9.447258e-8,4.516838e-7,0.00007712045],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99933565,0.00012500351,0.00014475173,0.00007163125,0.00010036106,0.00022258596],"domain_scores_gemma":[0.99912095,0.00060751033,0.00007683332,0.00004651153,0.000035281286,0.0001128957],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00088088564,0.000039865525,0.000076181546,0.00018962745,0.00034268806,0.00004732904,0.00017989916,0.000026403477,0.000078898534],"category_scores_gemma":[0.00022049023,0.000017506989,0.000013951454,0.00020114466,0.00094238314,0.0003047472,0.0000048837924,0.00009690303,0.0000040032437],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005219231,6.3108143e-7,0.9984968,0.000002464715,0.0000027357241,0.000012771129,0.0005694476,0.00008523284,0.0000151192735,0.000119232405,0.0000034112572,0.00068695605],"study_design_scores_gemma":[0.00012692747,0.00007524079,0.99747646,0.00003224839,0.0000028258103,0.00024318048,0.0008045055,0.00021170391,0.000010027088,0.00072335853,0.00026692462,0.000026589107],"about_ca_topic_score_codex":0.0021010716,"about_ca_topic_score_gemma":0.5051086,"teacher_disagreement_score":0.50300753,"about_ca_system_score_codex":3.1496856e-7,"about_ca_system_score_gemma":0.00024834104,"threshold_uncertainty_score":0.5039219},"labels":[],"label_agreement":null},{"id":"W2523946309","doi":"10.1139/cjes-2016-0059","title":"Parentage of Archean basement within a Paleoproterozoic orogen and implications for on-craton diamond preservation: Slave craton and Wopmay orogen, northwest Canada","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"ARC Resources (Canada); Carleton University; Geological Survey of Canada; Yukon Agricultural Association; Government of Northwest Territories; University of Calgary","funders":"","keywords":"Craton; Geology; Archean; Geochemistry; Terrane; Basement; Kimberlite; Rift; Petrology; Mantle (geology); Paleontology; Tectonics","score_opus":0.025711712692261048,"score_gpt":0.21043738099672543,"score_spread":0.18472566830446438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2523946309","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930222,0.00061952963,0.000047542224,0.0055745193,0.000058634127,0.00013357378,0.00036210768,0.000001310799,0.00018059798],"genre_scores_gemma":[0.99902254,0.00003890732,0.00053252047,0.00031576576,0.000040235307,0.0000018390772,0.000009657265,0.000001086037,0.00003746172],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99896216,0.000038793954,0.00033322466,0.00019847834,0.00019396096,0.00027337988],"domain_scores_gemma":[0.9987134,0.00024502186,0.0002212522,0.00009132172,0.00013838518,0.0005906152],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044150586,0.00010230978,0.00019128578,0.00011094844,0.00027542273,0.0000506399,0.00021424421,0.000030198937,0.00044994475],"category_scores_gemma":[0.00018930642,0.00005717717,0.000042284475,0.0002418395,0.00040906892,0.0001879574,0.0000064976243,0.000058481666,7.397525e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009926498,0.000003863629,0.99352777,0.000008507731,0.000016884234,0.000003859332,0.00006666956,0.000094531366,0.00020794333,0.0001740169,0.00006294306,0.005823083],"study_design_scores_gemma":[0.00021601301,0.0003923528,0.9914434,0.00004214874,0.000022041473,0.000016538906,0.00014423982,0.00019931697,0.0018218019,0.004405296,0.0011977076,0.00009913459],"about_ca_topic_score_codex":0.48307753,"about_ca_topic_score_gemma":0.9964288,"teacher_disagreement_score":0.5133513,"about_ca_system_score_codex":0.0000032108649,"about_ca_system_score_gemma":0.00094019924,"threshold_uncertainty_score":0.5203647},"labels":[],"label_agreement":null},{"id":"W2526845342","doi":"10.1139/cjes-2015-0224","title":"Petroleum generation modeling of the organic-rich shales of Late Jurassic – Early Cretaceous succession from Mintaq-01 well in the Wadi Hajar sub-basin, Yemen","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Source rock; Cretaceous; Oil shale; Kerogen; Maturity (psychological); Paleontology; Total organic carbon; Window (computing); Organic matter; Geochemistry; Structural basin","score_opus":0.01820897503911835,"score_gpt":0.20265275552238732,"score_spread":0.18444378048326898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2526845342","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958989,0.0006691548,0.0015389039,0.0013441483,0.00019521148,0.000038927905,0.000006360394,0.000002439715,0.00030596188],"genre_scores_gemma":[0.99967194,0.000095288706,0.00007608728,0.000038197228,0.00006983613,5.25854e-7,5.878289e-7,0.0000056613635,0.000041862277],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99891454,0.00009761336,0.00038888515,0.00009074189,0.00032943848,0.00017878733],"domain_scores_gemma":[0.9994597,0.00005515871,0.00014874162,0.00013693505,0.00008782044,0.00011165356],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006075979,0.000081827515,0.00016807861,0.00025693246,0.00010830936,0.000060562692,0.0004799413,0.00004394664,0.00012591864],"category_scores_gemma":[0.000071060575,0.000039136197,0.000076982535,0.00050419493,0.00014025996,0.0003028495,0.000008380767,0.000107244254,0.0000036977492],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000067753,0.000012479987,0.109592155,0.000013348005,0.000057863836,0.000016897362,0.003356423,0.7658179,0.11996093,0.000043196094,0.0002112588,0.0009108027],"study_design_scores_gemma":[0.00045577204,0.0001181879,0.036801033,0.00029723282,0.00006586029,0.000008497212,0.0009181444,0.87927336,0.080914505,0.00033088445,0.0006189877,0.00019754608],"about_ca_topic_score_codex":0.00222508,"about_ca_topic_score_gemma":0.14567906,"teacher_disagreement_score":0.14345397,"about_ca_system_score_codex":0.000016595744,"about_ca_system_score_gemma":0.000372633,"threshold_uncertainty_score":0.86991006},"labels":[],"label_agreement":null},{"id":"W2527567882","doi":"10.1139/cjes-2016-0117","title":"An arborescent lycopsid stem fragment from the Palliser Formation (Famennian) carbonate platform, southwestern Alberta, Canada, and its paleogeographic and paleoclimatic significance","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Geology; Paleontology; Carbonate; Paleoclimatology; Late Devonian extinction; Salt marsh; Carboniferous; Oceanography; Structural basin; Climate change","score_opus":0.019555888733699133,"score_gpt":0.1704016931160355,"score_spread":0.15084580438233638,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2527567882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99676526,0.00063677935,0.0000014778544,0.0021581629,0.0001280328,0.00008320761,0.00017436265,0.0000018556907,0.00005088062],"genre_scores_gemma":[0.9994372,0.00020658226,0.000010295891,0.0002578759,0.000065649896,5.771589e-7,0.00000358922,3.4539428e-7,0.000017900858],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991139,0.00005457928,0.00018417006,0.00013504535,0.00024438594,0.0002679275],"domain_scores_gemma":[0.9991339,0.00021581246,0.0001657761,0.000030166268,0.000057258843,0.0003971102],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029870102,0.0000906364,0.00011109177,0.000025332676,0.00046797752,0.00013346142,0.0002513389,0.000036674828,0.000050696384],"category_scores_gemma":[0.000020391202,0.000029502622,0.000023621957,0.00014201584,0.00016934844,0.00055741734,0.000011313941,0.000065381544,0.0000017898329],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000113812785,0.0000041519784,0.9916288,0.000003831345,0.000009789303,0.000015245336,0.0004842663,0.00001587256,0.003646041,0.00007004458,0.000042949818,0.004067628],"study_design_scores_gemma":[0.00011486998,0.00014627376,0.9966187,0.000107578264,0.0000129738755,0.00001951333,0.0011436519,0.00026147804,0.00018092508,0.0001456818,0.0011509963,0.00009738621],"about_ca_topic_score_codex":0.52884007,"about_ca_topic_score_gemma":0.9977959,"teacher_disagreement_score":0.46895584,"about_ca_system_score_codex":0.0000106945645,"about_ca_system_score_gemma":0.00015442802,"threshold_uncertainty_score":0.47429746},"labels":[],"label_agreement":null},{"id":"W2528606768","doi":"10.1139/cjes-2016-0074","title":"Structure and kinematic evolution of the Duke River fault, southwestern Yukon","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of British Columbia; Yukon University","funders":"","keywords":"Geology; Terrane; Fault (geology); Greenschist; Metamorphism; Thrust fault; Cretaceous; Paleontology; Seismology; Geomorphology; Tectonics","score_opus":0.008988583106514701,"score_gpt":0.17014807279580108,"score_spread":0.16115948968928637,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2528606768","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99739635,0.00059780164,0.000031980137,0.0013523602,0.00012988765,0.000025224452,0.000039093284,8.88179e-7,0.00042643404],"genre_scores_gemma":[0.9995213,0.0000072286357,0.00028076797,0.00007535543,0.000041298168,1.8703501e-8,2.3027972e-7,3.7718866e-7,0.00007341359],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992727,0.00004600084,0.00019659719,0.00009111638,0.00020864091,0.00018492913],"domain_scores_gemma":[0.9993614,0.00008379626,0.000174096,0.00006259527,0.000073219366,0.0002448934],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023243144,0.00006038194,0.00012716059,0.00009370462,0.00015971708,0.000027025846,0.0002805397,0.000031768523,0.0019558785],"category_scores_gemma":[0.00017643644,0.000023443788,0.00006150651,0.00029446365,0.000889659,0.00016019504,0.000005864306,0.000063127285,0.000006898975],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000016538264,7.118373e-7,0.9968461,0.0000032607004,0.0000055370183,0.0000025948777,0.00008272492,0.0004088181,0.0004122203,0.00009695945,0.000010726421,0.0021286996],"study_design_scores_gemma":[0.00008189363,0.0000764324,0.9834521,0.00004429108,0.000015537576,0.000041880136,0.00009675202,0.00030064644,0.00027893836,0.015403042,0.0001635352,0.00004496795],"about_ca_topic_score_codex":0.013252688,"about_ca_topic_score_gemma":0.3071169,"teacher_disagreement_score":0.2938642,"about_ca_system_score_codex":0.0000010455326,"about_ca_system_score_gemma":0.00021764223,"threshold_uncertainty_score":0.99895644},"labels":[],"label_agreement":null},{"id":"W2528756148","doi":"10.1139/cjes-2016-0001","title":"Geological significance of <sup>40</sup>Ar/<sup>39</sup>Ar mica dates across a mid-crustal continental plate margin, Connemara (Grampian orogeny, Irish Caledonides), and implications for the evolution of lithospheric collisions","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Metamorphism; Orogeny; Metamorphic rock; Magmatism; Geochemistry; Lithosphere; Paleontology; Tectonics","score_opus":0.019477403058838504,"score_gpt":0.231442104375892,"score_spread":0.2119647013170535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2528756148","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98962706,0.0027943114,0.00055306125,0.005327092,0.00007144896,0.00027738695,0.001196413,0.0000056927706,0.00014753631],"genre_scores_gemma":[0.99786466,0.00017424545,0.001601078,0.00011911283,0.000077163524,0.00000393359,0.000013165572,0.0000026526109,0.00014401443],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978855,0.00010827768,0.0007003925,0.00035983705,0.00029067506,0.0006553181],"domain_scores_gemma":[0.99695754,0.0013430477,0.00046593402,0.00019563733,0.00038982747,0.0006480012],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009637354,0.00019742525,0.0004639321,0.0001046392,0.00069656613,0.00009466166,0.0007317473,0.000117959964,0.0012732147],"category_scores_gemma":[0.0008812782,0.000100795056,0.00022754654,0.00077031046,0.0029961828,0.00031077664,0.00003030127,0.00016024573,0.000007443785],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000077416444,0.000024299326,0.9878734,0.000014173275,0.00006206434,0.000007697473,0.00022603624,0.0066931346,0.0012405987,0.00020455969,0.0003212062,0.0032554483],"study_design_scores_gemma":[0.0006163523,0.0006704266,0.97532064,0.00007863126,0.00009401768,0.00013002135,0.0023121908,0.011773507,0.0006308789,0.0042762975,0.0038669147,0.00023009746],"about_ca_topic_score_codex":0.021028925,"about_ca_topic_score_gemma":0.06404775,"teacher_disagreement_score":0.043018825,"about_ca_system_score_codex":0.000008280577,"about_ca_system_score_gemma":0.00061610556,"threshold_uncertainty_score":0.9997171},"labels":[],"label_agreement":null},{"id":"W2528969322","doi":"10.1139/cjes-2016-0115","title":"Seismic velocity model of the crust in the northern Canadian Cordillera from Rayleigh wave dispersion data","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"","keywords":"Geology; Crust; Seismology; Rayleigh wave; Receiver function; Upper crust; Mantle (geology); Azimuth; Shear (geology); Surface wave; Geodesy; Geophysics; Lithosphere; Tectonics; Paleontology; Geometry","score_opus":0.0582941266709383,"score_gpt":0.21351073744481233,"score_spread":0.15521661077387403,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2528969322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.988379,0.0010731461,0.000016425634,0.0055269017,0.00035272617,0.00008762502,0.00070339674,0.0000011347253,0.0038596403],"genre_scores_gemma":[0.99903315,0.00010570157,0.00013021957,0.00057683495,0.00007701523,1.1035413e-7,0.0000034258792,0.0000016798158,0.000071863025],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99856305,0.00012071511,0.00029787124,0.0001928553,0.00040972512,0.00041580744],"domain_scores_gemma":[0.9987804,0.00028186454,0.00018463214,0.00035292184,0.000083459316,0.00031670555],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009723166,0.00010766485,0.00018471609,0.00018521793,0.0005420657,0.00007035314,0.0014742459,0.000045726716,0.0007214854],"category_scores_gemma":[0.00026669842,0.000045930108,0.000065264525,0.00040978516,0.00076442497,0.00037421155,0.000018333334,0.00017672272,0.000016524356],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000046365567,0.0000027892136,0.9769572,0.0000013736168,0.000015010282,0.000019428218,0.0009128438,0.0027348807,0.000014256931,0.000018239825,0.00035239384,0.018966943],"study_design_scores_gemma":[0.00019106646,0.00006629074,0.9751112,0.0000870256,0.000014733471,0.00002033546,0.0009767658,0.020785756,0.000038692247,0.000537748,0.0020745879,0.0000958229],"about_ca_topic_score_codex":0.7322583,"about_ca_topic_score_gemma":0.99762976,"teacher_disagreement_score":0.26537144,"about_ca_system_score_codex":0.0000066088646,"about_ca_system_score_gemma":0.0033627457,"threshold_uncertainty_score":0.7899759},"labels":[],"label_agreement":null},{"id":"W2532750073","doi":"10.1139/cjes-2016-0042","title":"Application of biomarkers to petroleum migration in the Linyi fault area, Huimin Depression, Bohai Bay Basin, China","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Maturity (psychological); Fault (geology); Geochemistry; Source rock; Petroleum; Structural basin; Dominance (genetics); Bay; Petrology; Seismology; Geomorphology; Paleontology; Oceanography","score_opus":0.009975339905553722,"score_gpt":0.21644967655122224,"score_spread":0.20647433664566853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2532750073","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96835196,0.00027690027,0.024404483,0.0057165846,0.00012374391,0.00007475502,0.000006536286,0.0000045820007,0.0010404462],"genre_scores_gemma":[0.9995045,0.00003889556,0.0002904702,0.00009589694,0.000038155176,0.0000031949346,6.448094e-7,0.0000033182391,0.000024888006],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991876,0.000047348854,0.0002872202,0.00008182409,0.0002336736,0.00016231512],"domain_scores_gemma":[0.9994956,0.000044232085,0.000082547136,0.00011239591,0.00006152045,0.00020366718],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00067681755,0.000064759704,0.000113974165,0.00050074345,0.000085880485,0.000044121138,0.00032192538,0.000032590484,0.0000395984],"category_scores_gemma":[0.00011652949,0.00003469008,0.00005493247,0.000706414,0.00009166757,0.0002396147,0.000003389926,0.000060422866,0.000005296191],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015144892,0.000024494944,0.52484506,0.00001945034,0.000062937695,0.000020694855,0.0043460466,0.41514134,0.021969417,0.00017854616,0.00395106,0.029425789],"study_design_scores_gemma":[0.00058514375,0.00022516762,0.7372832,0.0003143758,0.000041489704,0.000042242064,0.0027494158,0.20693484,0.010506386,0.0004899095,0.040491097,0.00033674706],"about_ca_topic_score_codex":0.0019669489,"about_ca_topic_score_gemma":0.23220018,"teacher_disagreement_score":0.23023322,"about_ca_system_score_codex":0.000011256643,"about_ca_system_score_gemma":0.00018025744,"threshold_uncertainty_score":0.78181016},"labels":[],"label_agreement":null},{"id":"W2535970380","doi":"10.1139/cjes-2016-0135","title":"Mantle influence of syn- to late-Grenvillian alkaline magmatism in the Grenville Province: causes and implications","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec); Université du Québec à Montréal","funders":"Ministère de l'Énergie et des Ressources Naturelles","keywords":"Geology; Magmatism; Orogeny; Geochemistry; Pluton; Terrane; Subduction; Metamorphism; Laurentia; Mantle (geology); Paleozoic; Paleontology; Tectonics","score_opus":0.013407826039083618,"score_gpt":0.20622306615500294,"score_spread":0.19281524011591933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2535970380","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.988915,0.00038749777,0.000010146063,0.009847696,0.000023320477,0.00005834619,0.00004717396,8.791246e-7,0.00070994],"genre_scores_gemma":[0.99899495,0.00006267385,0.00038869894,0.00047926797,0.000018744637,3.0342795e-7,6.150213e-7,4.9956896e-7,0.00005425043],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99916476,0.00005044201,0.00025963536,0.00012124396,0.00016672943,0.00023719542],"domain_scores_gemma":[0.99924767,0.00018912695,0.00011492478,0.00008760662,0.00006398299,0.0002967141],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005610693,0.00006528461,0.00013838096,0.00018353925,0.00013755809,0.000040072573,0.00039703422,0.000025583973,0.00088723964],"category_scores_gemma":[0.00024854037,0.000029346418,0.000032725595,0.0005023797,0.00049009436,0.00016052465,0.0000067310853,0.000062961444,0.00002484768],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002041637,0.0000029775824,0.9919919,0.0000028372533,0.0000034036345,0.000011738779,0.000112967806,0.0012263199,0.000681409,0.00021380832,0.000046081273,0.005704541],"study_design_scores_gemma":[0.000060181326,0.00014068706,0.9917956,0.00004170588,0.0000064970427,0.0000353624,0.000105631196,0.000041042345,0.00017511648,0.005527481,0.0020156025,0.000055073644],"about_ca_topic_score_codex":0.024469906,"about_ca_topic_score_gemma":0.6356162,"teacher_disagreement_score":0.6111463,"about_ca_system_score_codex":9.3373603e-7,"about_ca_system_score_gemma":0.00023279192,"threshold_uncertainty_score":0.9820262},"labels":[],"label_agreement":null},{"id":"W2536020535","doi":"10.1139/cjes-2016-0179","title":"Discussion of “Glacier velocities and dynamic discharge from the ice masses of Baffin Island and Bylot Island, Nunavut, Canada”","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Glacier; Geology; Arctic; Iceberg; Physical geography; Ice caps; Oceanography; Glacier morphology; Ice calving; Tidewater glacier cycle; Ice sheet; Geomorphology; Arctic ice pack; Antarctic sea ice; Geography","score_opus":0.012145670557023083,"score_gpt":0.19216488322212627,"score_spread":0.18001921266510318,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2536020535","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99015796,0.0040373737,0.000045893128,0.0046863314,0.00025131533,0.000043680026,0.00056804274,6.018021e-7,0.00020881197],"genre_scores_gemma":[0.99894845,0.00047098516,0.00021236467,0.0001097909,0.000039857256,1.057468e-7,0.0000018104502,0.0000012006501,0.00021542406],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99920374,0.00003805409,0.00024146291,0.000102911996,0.00022152101,0.00019229317],"domain_scores_gemma":[0.9991254,0.00036989662,0.000193222,0.000066345965,0.00006630485,0.00017882162],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029588028,0.00007737549,0.00016941897,0.000036143403,0.00032568094,0.000042372285,0.00019617498,0.0000199236,0.00047745966],"category_scores_gemma":[0.0001345015,0.00003118183,0.000024722483,0.00017968385,0.0006670317,0.00021152617,0.000008613167,0.000051587613,4.1506866e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000534665,0.0000010057475,0.9929616,0.0000042708048,0.000013088125,0.000003371566,0.0005466823,0.000038409256,0.00003854699,0.00004093636,0.0005048108,0.0058419583],"study_design_scores_gemma":[0.00015892806,0.00009057116,0.9882939,0.00008691742,0.000013514447,0.000011319775,0.0030450707,0.00028271807,0.000026106773,0.00034676556,0.0075827623,0.00006143203],"about_ca_topic_score_codex":0.6137754,"about_ca_topic_score_gemma":0.9990924,"teacher_disagreement_score":0.38531703,"about_ca_system_score_codex":0.000002126859,"about_ca_system_score_gemma":0.0009216828,"threshold_uncertainty_score":0.5227848},"labels":[],"label_agreement":null},{"id":"W2539051818","doi":"10.1139/cjes-2016-0060","title":"The thermal structure of the central Nova Scotia Slope (eastern Canada): seafloor heat flow and thermal maturation models","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Diapir; Lithosphere; Seafloor spreading; Salt dome; Borehole; Thermal; Rift; Heat transfer; Geomorphology; Petrology; Tectonics; Heat flow; Sediment; Geophysics; Seismology; Paleontology; Mechanics; Meteorology","score_opus":0.009652775216858554,"score_gpt":0.17874488557046095,"score_spread":0.1690921103536024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2539051818","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950413,0.00062584714,0.00018936332,0.0029643064,0.00058035116,0.00004483219,0.000017507067,0.000002051354,0.0005344109],"genre_scores_gemma":[0.99971783,0.000019368035,0.000053777243,0.00006148745,0.00008927239,7.8630954e-8,1.8173246e-7,0.000004496105,0.00005349167],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99917346,0.000042480555,0.00020360759,0.00006263781,0.00027631436,0.00024147822],"domain_scores_gemma":[0.999518,0.00002983313,0.0000551583,0.00009717473,0.000074900134,0.00022497047],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015362285,0.00007711593,0.0000999911,0.000060126797,0.00021313396,0.0000893648,0.0003023651,0.000028405168,0.00008017457],"category_scores_gemma":[0.000022295975,0.000032135104,0.000042844982,0.00020970275,0.0002445843,0.00029929142,0.000007721813,0.00008853399,4.6683908e-7],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009382021,0.0000013692803,0.036346305,0.000009660281,0.00007344152,0.000008746345,0.00087774807,0.9420395,0.015349952,0.0002753693,0.00032252588,0.00468602],"study_design_scores_gemma":[0.00060621457,0.000084840045,0.2856874,0.0002177697,0.00006604526,0.00009001604,0.0012465417,0.6918163,0.01741953,0.00045142535,0.001977056,0.00033688545],"about_ca_topic_score_codex":0.072650485,"about_ca_topic_score_gemma":0.9706583,"teacher_disagreement_score":0.8980078,"about_ca_system_score_codex":0.000015465945,"about_ca_system_score_gemma":0.0010504683,"threshold_uncertainty_score":0.9335248},"labels":[],"label_agreement":null},{"id":"W2539331834","doi":"10.1139/cjes-2016-0159","title":"<i>Arctosaurus osborni</i>, a Late Triassic archosauromorph reptile from the Canadian Arctic Archipelago","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology; Archipelago; Arctic; Fossil Record; Oceanography","score_opus":0.027400879360069255,"score_gpt":0.2088865520146048,"score_spread":0.18148567265453552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2539331834","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9706242,0.0028437602,0.000024039338,0.01912901,0.0015832167,0.00010366849,0.00043631296,0.0000059846675,0.005249799],"genre_scores_gemma":[0.9971202,0.00008178365,0.00038972113,0.0017666694,0.00039007174,4.6833307e-7,0.000009820802,0.0000023089763,0.00023894841],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99782884,0.00038276907,0.00039348291,0.0002749579,0.00027211301,0.0008478143],"domain_scores_gemma":[0.9971598,0.0009867984,0.00023802446,0.00021397446,0.00012365919,0.0012777848],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014655871,0.00015722112,0.00024070503,0.00031906329,0.0012705907,0.0001092959,0.0010217031,0.00011621935,0.004902261],"category_scores_gemma":[0.0006921399,0.0000808139,0.00012079639,0.0004106206,0.0022705568,0.00035990542,0.0000058904657,0.00032280793,0.00037066825],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023972972,0.0000019985835,0.9825609,9.388575e-7,0.000026158721,0.00022273144,0.00035481973,0.000113872666,0.000036682955,0.00022545327,0.00088917644,0.015543332],"study_design_scores_gemma":[0.00027742446,0.00024745762,0.95076877,0.00006028669,0.00001722802,0.00028919143,0.00010949278,0.00010159433,0.000010259432,0.009613437,0.038370483,0.00013438563],"about_ca_topic_score_codex":0.76131874,"about_ca_topic_score_gemma":0.9991961,"teacher_disagreement_score":0.2378774,"about_ca_system_score_codex":0.000011407122,"about_ca_system_score_gemma":0.0061300118,"threshold_uncertainty_score":0.9995043},"labels":[],"label_agreement":null},{"id":"W2540997622","doi":"10.1139/cjes-2016-0110","title":"A basal ceratopsid (Centrosaurinae: Nasutoceratopsini) from the Oldman Formation (Campanian) of Alberta, Canada","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; University of Toronto; Canadian Museum of Nature; University of Alberta","funders":"","keywords":"Taxon; Paleontology; Clade; Geology; Geography; Phylogenetic tree; Biology","score_opus":0.012902805745535288,"score_gpt":0.1830966508358399,"score_spread":0.1701938450903046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2540997622","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9873773,0.0010491,0.0000482098,0.0063547916,0.0009307369,0.000057716537,0.00017070778,0.0000013036279,0.0040101344],"genre_scores_gemma":[0.99867415,0.000029671513,0.00016505462,0.0008590675,0.00015951775,1.425865e-7,0.0000051970915,9.071968e-7,0.00010627702],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988282,0.00014246439,0.00033992968,0.00011877146,0.00021335715,0.0003573293],"domain_scores_gemma":[0.9987036,0.0004988793,0.00026957574,0.00010350658,0.000106115054,0.0003183393],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00043168513,0.00009135705,0.0001671206,0.00008134697,0.0004069872,0.000027980463,0.00050000416,0.000055170993,0.002496605],"category_scores_gemma":[0.00023403173,0.000046421646,0.00005057001,0.00021350574,0.0006786505,0.00044360335,0.000003566363,0.00009849691,0.00002050124],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016073256,0.0000015260492,0.99473304,0.0000012476149,0.000011948334,0.000021328304,0.00017104024,0.0000958099,0.00003152652,0.00024141121,0.0021276004,0.002547465],"study_design_scores_gemma":[0.00019893509,0.00014016953,0.9711598,0.000031788804,0.0000072328426,0.00011405106,0.00022776953,0.00019356507,0.00015971021,0.0008112524,0.026880706,0.000074997726],"about_ca_topic_score_codex":0.88529724,"about_ca_topic_score_gemma":0.9996631,"teacher_disagreement_score":0.11436589,"about_ca_system_score_codex":0.000005803165,"about_ca_system_score_gemma":0.0036587075,"threshold_uncertainty_score":0.99841523},"labels":[],"label_agreement":null},{"id":"W2546569839","doi":"10.1139/cjes-2016-0199","title":"Tracking low-temperature tectonism of the St. Lawrence Platform and Humber Zone, southern Quebec Appalachians, through apatite and zircon (U–Th)/He thermochronology","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"","keywords":"Geology; Thermochronology; Zircon; Ordovician; Devonian; Outcrop; Paleontology; Closure temperature; Siliciclastic; Monocline; Basement; Geochemistry; Structural basin; Sedimentary depositional environment","score_opus":0.01584830459915086,"score_gpt":0.2012557989569313,"score_spread":0.18540749435778042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2546569839","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99438995,0.0015565325,0.000008145788,0.0021450517,0.00015443975,0.000050139628,0.000049267204,0.0000018459939,0.0016446165],"genre_scores_gemma":[0.9991918,0.000067407804,0.00027877107,0.00022051687,0.00006587371,1.1335511e-7,0.0000012865122,0.0000011545962,0.00017306626],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990129,0.000045702698,0.00024364993,0.00018878923,0.00020448556,0.00030447636],"domain_scores_gemma":[0.99910015,0.000087392844,0.00033053473,0.00016109837,0.00007879665,0.00024205005],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042877256,0.00011707054,0.00023517081,0.00005953935,0.0009903606,0.00027004714,0.00058333867,0.0000897564,0.0011200226],"category_scores_gemma":[0.0001569245,0.000062164414,0.000074291944,0.00014003237,0.0022008256,0.00043041306,0.000020333613,0.00026461744,0.000004503089],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000063637763,0.0000037240914,0.9881669,0.0000121356625,0.00002517829,0.00001637358,0.000933064,0.00015612939,0.0012866264,0.00021166774,0.000018608485,0.009163222],"study_design_scores_gemma":[0.0001609078,0.00010780793,0.9912546,0.00007725213,0.000029041239,0.0000788961,0.00074477046,0.00018670576,0.0015126748,0.005017691,0.0007138897,0.000115720875],"about_ca_topic_score_codex":0.18000354,"about_ca_topic_score_gemma":0.9207938,"teacher_disagreement_score":0.7407902,"about_ca_system_score_codex":0.0000011683354,"about_ca_system_score_gemma":0.00032172023,"threshold_uncertainty_score":0.9997931},"labels":[],"label_agreement":null},{"id":"W2548318053","doi":"10.1139/cjes-2016-0090","title":"Provenance analysis reveals mountain uplift in the midsection of the Altyn Tagh Fault during the Middle Miocene","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Provenance; Zircon; Clastic rock; Conglomerate; Sedimentary rock; Geochemistry; Plateau (mathematics); Tectonics; Structural basin; Paleontology; Fault (geology); Paleocurrent; Geomorphology","score_opus":0.017749030142987697,"score_gpt":0.19081721454565112,"score_spread":0.17306818440266342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2548318053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912528,0.00078489777,0.000011486026,0.006862622,0.000095628995,0.00007226805,0.00002399191,0.0000010321836,0.0008953142],"genre_scores_gemma":[0.999308,0.000039715975,0.00004931644,0.00031925944,0.00006270815,4.3450544e-7,4.6667145e-7,5.708048e-7,0.0002195259],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99856514,0.00020008226,0.00036700116,0.0001502409,0.00038600873,0.00033152942],"domain_scores_gemma":[0.9990292,0.00026125507,0.00030270003,0.00016861013,0.00009341484,0.00014480592],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015320622,0.00008687937,0.00019626264,0.0001855236,0.00040277094,0.00006376822,0.0009002916,0.00003600122,0.0010177564],"category_scores_gemma":[0.0003778158,0.000027730734,0.00020297813,0.0021005822,0.00069549633,0.00018422845,0.000007926867,0.0001457519,0.0000075708567],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004974869,0.0000038744665,0.99430996,0.0000029229275,0.000025632156,0.0000058345368,0.00020112329,0.004407891,0.0002901165,0.000058971942,0.000020284748,0.00066840654],"study_design_scores_gemma":[0.000083911546,0.000060732225,0.9943205,0.000034906134,0.000048608723,0.000023283821,0.00047989265,0.00038693473,0.0005210532,0.00353729,0.0004475294,0.00005534656],"about_ca_topic_score_codex":0.030618994,"about_ca_topic_score_gemma":0.57762784,"teacher_disagreement_score":0.5470088,"about_ca_system_score_codex":0.000003159739,"about_ca_system_score_gemma":0.00021093871,"threshold_uncertainty_score":0.99989545},"labels":[],"label_agreement":null},{"id":"W2548892109","doi":"10.1139/cjes-2016-0052","title":"Intensified aridity in the Qaidam Basin during the Middle Miocene: constraints from ostracod, stable isotope, and weathering records","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"China University of Geosciences; State Key Laboratory of Biogeology and Environmental Geology; China Postdoctoral Science Foundation","keywords":"Ostracod; Geology; Aridification; Structural basin; Paleoclimatology; Cenozoic; Tectonic uplift; Weathering; Paleontology; Plateau (mathematics); Late Miocene; Sedimentology; Sedimentary rock; Denudation; Arid; Tectonics; Climate change; Oceanography","score_opus":0.04484605213352104,"score_gpt":0.2228724098855342,"score_spread":0.17802635775201314,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2548892109","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99139196,0.0009785923,0.000005342432,0.0045211804,0.00028261653,0.00008074284,0.000042499127,0.0000016502923,0.002695393],"genre_scores_gemma":[0.9992638,0.0001308276,0.00014376354,0.00026962982,0.00006714076,3.0853627e-7,6.153939e-7,0.0000010211784,0.00012288764],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986703,0.00029225595,0.00023571191,0.00015948177,0.00018439176,0.0004578859],"domain_scores_gemma":[0.9987186,0.00077694835,0.000104102895,0.00011016353,0.00006228388,0.00022789289],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0020835304,0.00008725475,0.00015608981,0.00015410045,0.00057131605,0.00011881726,0.0005313727,0.000062095445,0.0016260456],"category_scores_gemma":[0.00033293344,0.000039172133,0.000033576955,0.00026951393,0.0019394528,0.00029685252,0.0000073342158,0.00028406977,0.000029362913],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012640876,0.0000016842941,0.99773693,0.0000021101862,0.0000063144807,0.00012372207,0.00054933137,0.000025135922,0.000026187621,0.000029198463,0.00002476406,0.0014619979],"study_design_scores_gemma":[0.00021279606,0.0000829749,0.9952903,0.00006411228,0.000004007326,0.00043349172,0.0019876203,0.000048485657,0.00008860454,0.0008339503,0.00089140097,0.00006224763],"about_ca_topic_score_codex":0.017891435,"about_ca_topic_score_gemma":0.6880745,"teacher_disagreement_score":0.6701831,"about_ca_system_score_codex":7.680762e-7,"about_ca_system_score_gemma":0.0006144173,"threshold_uncertainty_score":0.9992866},"labels":[],"label_agreement":null},{"id":"W2550206991","doi":"10.1139/cjes-2016-0181","title":"Remnants of Early Mesozoic basalt of the Central Atlantic Magmatic Province in Cape Breton Island, Nova Scotia, Canada","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University; Laurentian University; Nova Scotia Department of Energy; Technical University of Nova Scotia","funders":"Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Geology; Basalt; Mesozoic; Nova scotia; Geochemistry; Flood basalt; Cape; Deccan Traps; Paleontology; Structural basin; Tectonics; Oceanography; Volcanism; Archaeology; Geography","score_opus":0.010116489661936111,"score_gpt":0.17289594704627267,"score_spread":0.16277945738433655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2550206991","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967252,0.00036318816,0.0000041318085,0.0016808073,0.00026201687,0.00006028878,0.00004817613,5.657113e-7,0.00085563783],"genre_scores_gemma":[0.9996647,0.000010360361,0.00007996182,0.00010802251,0.00003050141,2.7541622e-8,5.776413e-7,8.349144e-7,0.00010501449],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99840766,0.00009094129,0.00047473758,0.00013697696,0.00044681138,0.00044288475],"domain_scores_gemma":[0.99892193,0.00018451405,0.00033881457,0.00011292547,0.000097789874,0.0003440002],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004930593,0.00009457996,0.00027183694,0.0001413263,0.0000742311,0.000020594814,0.00063814863,0.000035708497,0.0030808526],"category_scores_gemma":[0.0003240306,0.000043130898,0.000086728025,0.00065122964,0.0005987264,0.00016500312,0.00000837124,0.000107160435,0.0000061245546],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006773297,0.0000032088915,0.99811697,0.000010881537,0.0000068985773,0.00002401906,0.00004934952,0.000345161,0.0001921876,0.000018087107,0.000087558314,0.0011389231],"study_design_scores_gemma":[0.0001516219,0.00012511665,0.99739563,0.00016976718,0.000012505056,0.000025058476,0.000063651896,0.00020543726,0.00092828064,0.00071203377,0.00013900881,0.00007187105],"about_ca_topic_score_codex":0.9721773,"about_ca_topic_score_gemma":0.99982387,"teacher_disagreement_score":0.027646538,"about_ca_system_score_codex":0.0000053329545,"about_ca_system_score_gemma":0.003258689,"threshold_uncertainty_score":0.99783045},"labels":[],"label_agreement":null},{"id":"W2556046142","doi":"10.1139/cjes-2016-0088","title":"Investigating the Paleozoic–Mesozoic low-temperature thermal history of the southwestern Canadian Arctic: insights from (U–Th)/He thermochronology","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Ottawa","funders":"","keywords":"Geology; Thermochronology; Paleontology; Devonian; Cretaceous; Rift; Craton; Paleozoic; Unconformity; Mesozoic; Late Devonian extinction; Laurentia; Zircon; Sedimentary rock; Structural basin; Tectonics; Carboniferous","score_opus":0.022847959004645514,"score_gpt":0.17467432571178737,"score_spread":0.15182636670714186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2556046142","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9843933,0.0037331446,0.0000015274501,0.008486932,0.0013905882,0.00008042456,0.000030152065,0.0000022551694,0.001881691],"genre_scores_gemma":[0.99824417,0.000036731275,0.0000463759,0.0012485418,0.00024350082,3.4997538e-7,0.0000013924608,0.000001870322,0.00017705568],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986449,0.00022348968,0.00030748209,0.00016477883,0.00026362354,0.00039576576],"domain_scores_gemma":[0.9987071,0.00024591506,0.0002947135,0.00016124676,0.00014421539,0.00044678256],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041171204,0.00012346097,0.00018036536,0.00010449087,0.0006271233,0.000057898007,0.0007669701,0.000085782645,0.001562669],"category_scores_gemma":[0.0003259865,0.00004784113,0.00009070536,0.0002496687,0.0017815792,0.00026814602,0.000010956583,0.00022246329,0.00003339954],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002944485,0.0000018149067,0.9894765,0.0000027695867,0.000026069858,0.000013430423,0.0030348457,0.00057136326,0.0010516812,0.00011359667,0.0003499855,0.0053549823],"study_design_scores_gemma":[0.000118799246,0.00012081819,0.9898327,0.000081529266,0.000013271175,0.000013738507,0.00091231294,0.000050183953,0.00013468965,0.0013738762,0.0072593605,0.000088706896],"about_ca_topic_score_codex":0.51344055,"about_ca_topic_score_gemma":0.9901033,"teacher_disagreement_score":0.47666278,"about_ca_system_score_codex":0.000021332198,"about_ca_system_score_gemma":0.0028522916,"threshold_uncertainty_score":0.99935},"labels":[],"label_agreement":null},{"id":"W2556247702","doi":"10.1139/cjes-2016-0132","title":"Gravity and magnetic modelling of layered mafic–ultramafic intrusions in large igneous province plume centre regions: case studies from the 1.27 Ga Mackenzie, 1.38 Ga Kunene–Kibaran, 0.06 Ga Deccan, and 0.13–0.08 Ga High Arctic events","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Mafic; Ultramafic rock; Geology; Plume; Geochemistry; Igneous rock; Crust; Mantle plume; Layered intrusion; Flood basalt; Geophysics; Magnetic anomaly; Petrology; Seismology; Tectonics; Lithosphere","score_opus":0.034239969171673094,"score_gpt":0.2101358937360218,"score_spread":0.1758959245643487,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2556247702","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98313075,0.012155992,0.00010008165,0.0038928096,0.00024993139,0.00020454175,0.00023627152,0.0000035637054,0.000026065078],"genre_scores_gemma":[0.9960679,0.0031178372,0.00051567116,0.00015962325,0.00006691844,7.2659697e-7,0.0000052546775,0.0000026767843,0.00006340368],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982341,0.0001968038,0.00046148052,0.00029905036,0.0002918791,0.0005167164],"domain_scores_gemma":[0.9984929,0.0005556407,0.0002655147,0.00012575384,0.00015827635,0.00040189052],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008119796,0.00017496714,0.0003324038,0.00014062377,0.0007165609,0.000081222024,0.00026258983,0.00006272149,0.00025349698],"category_scores_gemma":[0.00037158455,0.00009435066,0.00004998173,0.00033501987,0.0007820094,0.0003307515,0.000025820395,0.00016890118,0.000007545306],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003807079,0.000015683181,0.9886478,0.000017676313,0.00002527604,0.0005518757,0.0016303902,0.005443159,0.000013544447,0.00013020672,0.00013702182,0.0033492914],"study_design_scores_gemma":[0.0013899617,0.00093334226,0.9531477,0.00068116136,0.00007724469,0.0009904752,0.013248649,0.00800586,0.00001923582,0.019002633,0.002088993,0.0004147224],"about_ca_topic_score_codex":0.082108125,"about_ca_topic_score_gemma":0.8297367,"teacher_disagreement_score":0.74762857,"about_ca_system_score_codex":0.000008201682,"about_ca_system_score_gemma":0.00030677713,"threshold_uncertainty_score":0.9240042},"labels":[],"label_agreement":null},{"id":"W2556840055","doi":"10.1139/cjes-2016-0144","title":"Age and origin of the Cannon Point syenite, Essex County, New York: southernmost expression of Monteregian Hills magmatism?","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Washington State University","keywords":"Geology; Sill; Geochemistry; Sanidine; Rift; Zircon; Silicic; Phenocryst; Igneous rock; Paleozoic; Magmatism; Quartz monzonite; Pluton; Paleontology; Volcanic rock; Basalt; Plagioclase; Tectonics; Quartz; Volcano","score_opus":0.02064441708662331,"score_gpt":0.19286761369384783,"score_spread":0.17222319660722452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2556840055","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99447906,0.0011832647,0.000027805743,0.0016646024,0.00012970011,0.00004179131,0.00010429307,0.0000012550031,0.0023682176],"genre_scores_gemma":[0.9990479,0.000029929775,0.00039638154,0.00010733231,0.000045372948,4.3521688e-8,7.327747e-7,8.734076e-7,0.000371446],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99892896,0.00006253155,0.00032413143,0.00012669394,0.00031057218,0.00024708922],"domain_scores_gemma":[0.99892306,0.00012871793,0.00031956716,0.00010542153,0.00007867846,0.00044453293],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042697697,0.00008991315,0.00022232503,0.00011803069,0.00014687756,0.0000384981,0.0004474154,0.000042595784,0.0024811686],"category_scores_gemma":[0.00015342819,0.000038141407,0.00008540725,0.0003486935,0.0007783236,0.00017000182,0.000010880815,0.000080522695,0.0000040811615],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000104375185,0.0000041738604,0.98579866,0.000009423368,0.000010814788,0.000026922633,0.0003611752,0.0001976654,0.0037691153,0.00011178379,0.0004431842,0.009256632],"study_design_scores_gemma":[0.00026983066,0.00023358472,0.98018026,0.00033830898,0.000027934006,0.0000680062,0.0006200393,0.0001083276,0.0065419804,0.008659481,0.002824264,0.00012800073],"about_ca_topic_score_codex":0.08268579,"about_ca_topic_score_gemma":0.448072,"teacher_disagreement_score":0.36538622,"about_ca_system_score_codex":0.0000013321484,"about_ca_system_score_gemma":0.00042851077,"threshold_uncertainty_score":0.99843067},"labels":[],"label_agreement":null},{"id":"W2558650658","doi":"10.1139/cjes-2016-0118","title":"Origin and evolution of ore-forming fluids, and genesis of the Duhuangling and Jiusangou gold deposits in eastern Yanbian, northeast China","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Geology; Pyrite; Geochemistry; Sericite; Fluid inclusions; Quartz; Arsenopyrite; Chalcopyrite; Mineralization (soil science); Sphalerite; Calcite; Mineralogy; Copper; Metallurgy; Materials science","score_opus":0.012729832872084259,"score_gpt":0.1847764557086052,"score_spread":0.17204662283652095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2558650658","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99536943,0.0037471573,0.000013211223,0.0005987448,0.000046298108,0.000031059724,0.000012196541,6.184076e-7,0.00018129904],"genre_scores_gemma":[0.9996275,0.000102887665,0.0002037157,0.000018531438,0.000021470029,5.363446e-8,1.3943043e-7,5.470341e-7,0.000025210045],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999273,0.000039141833,0.00024057717,0.000111002344,0.0001514372,0.00018483837],"domain_scores_gemma":[0.9994692,0.00007076581,0.00014470771,0.000045978413,0.00004617664,0.00022313016],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004004589,0.000064659405,0.00016240167,0.00015875007,0.00010301196,0.000023273375,0.00015217156,0.000030597126,0.00007183374],"category_scores_gemma":[0.0001114,0.00003094729,0.000031733718,0.00035326998,0.000596183,0.00019363547,0.0000102507465,0.000053378324,4.700447e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004429305,0.0000013952231,0.985798,0.0000071483237,0.000004317785,0.0000036691174,0.00011638237,0.000065905944,0.0006402175,0.000040737385,0.0000010487713,0.013316748],"study_design_scores_gemma":[0.00011428155,0.00009185625,0.99706334,0.00010075752,0.000012081244,0.000053916792,0.00021461376,0.0008566175,0.00037851316,0.0010251696,0.000040446645,0.000048435246],"about_ca_topic_score_codex":0.047990177,"about_ca_topic_score_gemma":0.49913996,"teacher_disagreement_score":0.4511498,"about_ca_system_score_codex":0.000001301217,"about_ca_system_score_gemma":0.0001427875,"threshold_uncertainty_score":0.95834935},"labels":[],"label_agreement":null},{"id":"W2559337127","doi":"10.1139/cjes-2016-0193","title":"Reply to the discussion by Ommanney on “Glacier velocities and dynamic discharge from the ice masses of Baffin Island and Bylot Island, Nunavut, Canada”","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; University of Ottawa","funders":"","keywords":"Geology; Glacier; Ice caps; Oceanography; Physical geography; Climatology; Geomorphology; Geography","score_opus":0.01123511070050507,"score_gpt":0.19382403700910478,"score_spread":0.1825889263085997,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2559337127","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9392534,0.0025236874,0.00004019743,0.056728266,0.00033311325,0.00007733469,0.0008101371,9.592401e-7,0.00023291627],"genre_scores_gemma":[0.99690634,0.00028460246,0.00007807979,0.0020531893,0.0000679107,3.4416288e-7,0.0000027234353,0.0000016424063,0.0006051964],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910617,0.000054112195,0.0002046078,0.00014036625,0.00025897633,0.00023579758],"domain_scores_gemma":[0.9990035,0.00047376973,0.00012866914,0.00010220592,0.000049426064,0.00024237728],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040648555,0.00009166022,0.00013632649,0.000028656737,0.00070029986,0.00010423649,0.0002849305,0.00001618358,0.00031383638],"category_scores_gemma":[0.00020242922,0.000031878997,0.000022258559,0.00020294174,0.0004002416,0.00016182724,0.000010818073,0.000072576055,0.0000018895277],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013872101,0.0000016897669,0.95831263,0.0000022869006,0.000017281724,0.00000500616,0.0011799936,0.00013387071,0.00001939633,0.000044139102,0.029777398,0.010492415],"study_design_scores_gemma":[0.00011255598,0.00014064791,0.8493495,0.000066731336,0.000008983756,0.0000085469765,0.0028968472,0.00018456607,0.00001256115,0.00013775505,0.14701366,0.00006765762],"about_ca_topic_score_codex":0.63048387,"about_ca_topic_score_gemma":0.99860936,"teacher_disagreement_score":0.36812553,"about_ca_system_score_codex":0.000003579768,"about_ca_system_score_gemma":0.0005987948,"threshold_uncertainty_score":0.5386211},"labels":[],"label_agreement":null},{"id":"W2559464502","doi":"10.1139/cjes-2016-0096","title":"The Devonian Horn River Group and the basal Imperial Formation of the central Mackenzie Plain, N.W.T., Canada: multiproxy stratigraphic framework of a black shale basin","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Aboriginal Affairs and Northern Development Canada","keywords":"Geology; Oil shale; Canyon; Dolomite; Unconformity; Devonian; Paleontology; Geochemistry; Facies; Sedimentary rock; Geomorphology; Structural basin","score_opus":0.009695356979013981,"score_gpt":0.18845079072736914,"score_spread":0.17875543374835517,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2559464502","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9925527,0.0025504532,0.00006524602,0.0030984671,0.0006231465,0.00014304933,0.00013115538,9.1259335e-7,0.0008348667],"genre_scores_gemma":[0.99946296,0.00013887539,0.00022254299,0.00009009963,0.00007824549,2.520617e-7,2.860343e-7,5.753282e-7,0.0000061723676],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984958,0.00024589195,0.0004043789,0.00010569707,0.0003592134,0.00038900584],"domain_scores_gemma":[0.9984348,0.0006718269,0.0004168295,0.00013050844,0.000083530096,0.00026254554],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0011089437,0.0001045642,0.00018899007,0.000078220066,0.0007897522,0.00006670716,0.0006198125,0.00006531294,0.000060443814],"category_scores_gemma":[0.00030284232,0.00004063423,0.000101031765,0.00030396302,0.0047381097,0.0003342977,0.0000022622996,0.00017179982,1.7731514e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008693539,0.0000022271793,0.9855353,0.0000064373867,0.000022339247,0.000006588811,0.0013268584,0.00003473392,0.00003462152,0.002877809,0.00016131418,0.009904801],"study_design_scores_gemma":[0.000419489,0.0001320361,0.9938092,0.00007954046,0.000015094355,0.00003728652,0.0006658793,0.00037189736,0.00019751383,0.0038326737,0.00037631072,0.00006303028],"about_ca_topic_score_codex":0.38706943,"about_ca_topic_score_gemma":0.9942955,"teacher_disagreement_score":0.607226,"about_ca_system_score_codex":0.0000023764924,"about_ca_system_score_gemma":0.0018525845,"threshold_uncertainty_score":0.9979704},"labels":[],"label_agreement":null},{"id":"W2559763970","doi":"10.1139/cjes-2016-0177","title":"Coastal retreat rates and sediment input to the Minas Basin, Nova Scotia","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Sediment; Structural basin; Bay; Nova scotia; Geology; Erosion; Oceanography; Grain size; Dredging; Current (fluid); Hydrology (agriculture); Geomorphology; Geotechnical engineering","score_opus":0.013401989559317018,"score_gpt":0.20444959824894038,"score_spread":0.19104760868962337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2559763970","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9831295,0.00031964318,0.00007166556,0.011634877,0.0007193592,0.0000715305,0.00008269905,0.0000021913756,0.00396851],"genre_scores_gemma":[0.99780023,0.000024562782,0.00042457914,0.0006834242,0.00013617262,4.2575333e-8,0.0000010535571,0.0000013174854,0.0009286094],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99908435,0.00004020419,0.00018340889,0.00013615488,0.00022664841,0.00032922896],"domain_scores_gemma":[0.9990029,0.0001289605,0.000081251346,0.000080017264,0.000082210594,0.0006246939],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00067220704,0.000090815345,0.00011801487,0.00017747395,0.00026311682,0.00017085392,0.00030971752,0.00002172269,0.0010952272],"category_scores_gemma":[0.00013829318,0.000042187847,0.000036210593,0.0003241014,0.000447626,0.0002936027,0.000015376414,0.00006997453,0.00007567318],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009295548,0.0000015087628,0.9285464,0.0000018981924,0.000005913303,0.00004247322,0.00017351881,0.000117487165,0.000028734767,0.0000825378,0.0013212606,0.06966893],"study_design_scores_gemma":[0.00015089741,0.0005153738,0.94848955,0.00005915752,0.000008346133,0.00026820507,0.00029464441,0.00019913242,0.00011245433,0.00031165985,0.049483873,0.000106736545],"about_ca_topic_score_codex":0.06623901,"about_ca_topic_score_gemma":0.93975186,"teacher_disagreement_score":0.87351286,"about_ca_system_score_codex":0.0000015862286,"about_ca_system_score_gemma":0.00065873394,"threshold_uncertainty_score":0.9998179},"labels":[],"label_agreement":null},{"id":"W2560145442","doi":"10.1139/cjes-2016-0111","title":"Focal depth distribution of the 1982 Miramichi earthquake sequence determined by modelling depth phases","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aftershock; Geology; Seismology; Foreshock; Magnitude (astronomy); Focal mechanism; Geodesy; Tectonics","score_opus":0.04261974297062024,"score_gpt":0.2346072955795724,"score_spread":0.19198755260895217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2560145442","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99348015,0.0021079609,0.0014329161,0.00074224774,0.00048213024,0.00008652597,0.00030690254,0.0000049211585,0.0013562719],"genre_scores_gemma":[0.9992354,0.00012440576,0.00030616514,0.00010608317,0.000076464916,2.167626e-7,0.0000038431017,0.0000022181555,0.00014523577],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983657,0.000095315336,0.00042393405,0.0001938275,0.000427502,0.0004937378],"domain_scores_gemma":[0.9987354,0.00027738317,0.0003314174,0.00014924716,0.00014627079,0.0003602535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006680028,0.00014409338,0.00023395203,0.00010827855,0.0005355323,0.00007444649,0.0005919527,0.000052896477,0.00029373038],"category_scores_gemma":[0.00023545684,0.00007393692,0.00014082236,0.00046221336,0.0011657315,0.0004278597,0.000008272243,0.00012854366,0.000012611779],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015827316,0.00000758524,0.9177239,0.0000064760397,0.000026912154,0.000024185169,0.00017180356,0.003557382,0.00029175292,0.00011910883,0.0004333008,0.07762176],"study_design_scores_gemma":[0.00069006946,0.0008027274,0.9710566,0.00034952036,0.000049229424,0.00027004586,0.00031128697,0.005527354,0.005331285,0.0013909582,0.013881613,0.00033935788],"about_ca_topic_score_codex":0.0141139375,"about_ca_topic_score_gemma":0.41472116,"teacher_disagreement_score":0.40060723,"about_ca_system_score_codex":0.0000039749625,"about_ca_system_score_gemma":0.0010747329,"threshold_uncertainty_score":0.9924512},"labels":[],"label_agreement":null},{"id":"W2561516476","doi":"10.1139/cjes-2016-0058","title":"Carbonic fluids in the Hamadi gold deposit, Sudan: origin and contribution to gold mineralization","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"China Geological Survey; National Natural Science Foundation of China; University of Regina","keywords":"Fluid inclusions; Geology; Quartz; Pyrite; Geochemistry; Mineralization (soil science); Partial melting; Mineralogy; Metamorphic rock; Mantle (geology)","score_opus":0.013398873524820054,"score_gpt":0.19898796342227879,"score_spread":0.18558908989745873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2561516476","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99035454,0.001095632,0.000055612858,0.0074895336,0.00010272802,0.000053247615,0.000011945585,0.0000015168587,0.0008352664],"genre_scores_gemma":[0.9988395,0.000049460745,0.00015231616,0.0007914477,0.0000722232,2.304008e-7,0.0000017176125,4.6179755e-7,0.00009264787],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990593,0.00008436959,0.00021660952,0.0001304697,0.00020585244,0.00030338758],"domain_scores_gemma":[0.9993002,0.00014219564,0.00006319857,0.0000561808,0.00007270248,0.0003655246],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00079682475,0.00007118701,0.00013049056,0.00018729837,0.000103967155,0.0001062985,0.00027792077,0.000034034012,0.0003891382],"category_scores_gemma":[0.00028576827,0.000032149444,0.00003863612,0.0006628429,0.00023466304,0.00020220858,0.000003310388,0.00006715471,0.00001734209],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000042745282,0.0000016948318,0.99580294,8.831241e-7,0.0000029394857,0.000025636902,0.000066449,0.0002818061,0.0004899318,0.000527543,0.00013689465,0.0026590193],"study_design_scores_gemma":[0.00014320874,0.0002163828,0.99071777,0.00003176167,0.000009794597,0.00006621083,0.00006294151,0.0005602869,0.00020584809,0.0026741885,0.005234668,0.00007692437],"about_ca_topic_score_codex":0.046538487,"about_ca_topic_score_gemma":0.72738516,"teacher_disagreement_score":0.6808467,"about_ca_system_score_codex":0.0000024996102,"about_ca_system_score_gemma":0.00016810892,"threshold_uncertainty_score":0.9598107},"labels":[],"label_agreement":null},{"id":"W2569212530","doi":"10.1139/cjes-2016-0175","title":"Evidence for Early Pleistocene glaciation from borecore stratigraphy in north-central Alberta, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Lethbridge; Alberta Energy","funders":"","keywords":"Geology; Pleistocene; Paleontology; Quaternary; Glacial period; Wisconsin glaciation; Sedimentology; Early Pleistocene; Outwash plain; Ice sheet; Sedimentary rock; Outcrop; Magnetostratigraphy; Geochronology; Paleomagnetism; Geomorphology; Ice stream; Oceanography","score_opus":0.05569489974717593,"score_gpt":0.259250840415088,"score_spread":0.20355594066791208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2569212530","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99529743,0.0010985907,0.0000070938436,0.0015830263,0.0007967648,0.00012098415,0.00007461375,7.4847105e-7,0.0010207304],"genre_scores_gemma":[0.99932355,0.000040028233,0.00036167106,0.0001151522,0.000107758926,5.352576e-7,0.000008603367,0.0000010542843,0.000041640844],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99862844,0.00007327681,0.0002878696,0.00018532542,0.00023664991,0.00058843615],"domain_scores_gemma":[0.99834377,0.0005845819,0.0002832038,0.00014878748,0.00010900926,0.0005306641],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005600475,0.00009397947,0.00019375126,0.00019671286,0.0008799416,0.0002026394,0.00082393974,0.00006539455,0.00048950984],"category_scores_gemma":[0.0008970084,0.000078058474,0.000054168937,0.00016898848,0.0005515979,0.0007091116,0.0000034638717,0.00020980569,0.000005860591],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033871285,0.0000013712267,0.998013,0.0000032875523,0.0000079456195,0.00006451928,0.00015514492,0.0004486778,3.466514e-7,0.00002708683,0.00008846437,0.0011562741],"study_design_scores_gemma":[0.00022518504,0.00021652954,0.9977435,0.000048435177,0.000006447742,0.000017615022,0.00008487778,0.0006960925,0.000013201556,0.00047295354,0.00038469242,0.000090458954],"about_ca_topic_score_codex":0.9854433,"about_ca_topic_score_gemma":0.9999971,"teacher_disagreement_score":0.014553772,"about_ca_system_score_codex":0.0000020440998,"about_ca_system_score_gemma":0.0062611806,"threshold_uncertainty_score":0.9993724},"labels":[],"label_agreement":null},{"id":"W2570600800","doi":"10.1139/e10-080","title":"The thickness of Neogene and Quaternary cover across the central Interior Plateau, British Columbia: analysis of water-well drill records and implications for mineral exploration potential<sup>1</sup>This article is one of a series of papers published in this Special Issue on the theme of <i>New insights in Cordilleran Intermontane geoscience: reducing exploration risk in the mountain pine beetle-affected area, British Columbia</i>. <sup>2</sup>Geological Survey of Canada (GSC) Contribution 20100036; Mineral Deposit Research Unit (MDRU, Department of Earh and Ocean Sciences, The University of British Columbia) Contribution p-261.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; University of British Columbia; Natural Resources Canada; Geological Survey of Canada","funders":"Ministry of Environment","keywords":"Geology; Neogene; Bedrock; Quaternary; Plateau (mathematics); Lithology; Geochemistry; Basalt; Geomorphology; Paleontology; Structural basin","score_opus":0.029110379364600435,"score_gpt":0.2258772139353258,"score_spread":0.19676683457072539,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2570600800","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973957,0.00045115277,0.000009185807,0.00058273814,0.000048224632,0.0005947013,0.0008859955,6.433723e-7,0.00003166219],"genre_scores_gemma":[0.999181,0.0006619487,0.000031626834,0.000017516093,0.000013250414,0.000001802349,0.000043904685,0.0000016550779,0.000047338744],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99679494,0.0013498703,0.00075687165,0.00024318138,0.00044755533,0.00040756344],"domain_scores_gemma":[0.9975114,0.0008509354,0.000565372,0.0001605291,0.00080267334,0.000109103246],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0059972354,0.00007664029,0.00046840738,0.00013132076,0.00063898193,0.00016550475,0.0005482231,0.00010046437,0.000338555],"category_scores_gemma":[0.0008196173,0.00006686131,0.000058902984,0.001330429,0.004414032,0.00047592333,0.000046002173,0.00025473116,3.332915e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022783637,0.000046035464,0.9921731,0.000019024586,0.000061726154,0.000010148987,0.004774251,0.0015681966,0.0002391721,0.0000042610354,0.00030873698,0.0005675436],"study_design_scores_gemma":[0.0006950522,0.0010137324,0.98255265,0.00015136956,0.000049165214,0.000064353015,0.0076568904,0.0072491937,0.00024334576,0.0002436271,0.000017304697,0.000063334206],"about_ca_topic_score_codex":0.9808833,"about_ca_topic_score_gemma":0.9995224,"teacher_disagreement_score":0.018639077,"about_ca_system_score_codex":0.000010585114,"about_ca_system_score_gemma":0.00074659,"threshold_uncertainty_score":0.99829537},"labels":[],"label_agreement":null},{"id":"W2572133168","doi":"10.1139/cjes-2016-0155","title":"The mid-Cambrian (Series 3, Drumian–Guzhangian; Marjuman) trilobite <i>Holmdalia</i> Robison, 1988, in western Newfoundland and its biostratigraphic significance","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Tenaga Nasional Berhad; National Science Foundation","keywords":"Trilobite; Bay; Paleontology; Taxon; Genus; Geology; Biostratigraphy; Type (biology); Type species; Ecological succession; Zoology; Biology; Oceanography; Ecology","score_opus":0.02361187100387803,"score_gpt":0.23144207168879682,"score_spread":0.2078302006849188,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2572133168","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9639461,0.019436572,0.000002105618,0.0041317996,0.0008841293,0.00014204426,0.000047205824,0.0000037023522,0.011406349],"genre_scores_gemma":[0.9987463,0.0006333197,0.000093768824,0.00009517956,0.000132075,5.6650873e-7,6.347427e-7,0.00000116348,0.00029701227],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982585,0.00013954217,0.0004311308,0.00025770126,0.0002643218,0.00064885756],"domain_scores_gemma":[0.9984551,0.0001722247,0.00045436807,0.00021939419,0.000081270475,0.00061762566],"candidate_categories":["sts","scholarly_communication"],"consensus_categories":[],"category_scores_codex":[0.0015292417,0.0001825611,0.0002776441,0.00032217518,0.0027047822,0.0011528404,0.0010176774,0.00009955687,0.000047236063],"category_scores_gemma":[0.00020216202,0.00012336159,0.0000857187,0.0002870874,0.0021398745,0.0014420399,0.0000027229642,0.00029758294,0.0000061971496],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029804729,0.0000021709166,0.9906768,0.0000057233237,0.0000127666935,0.0001455731,0.0002499438,0.000017271777,0.00003794508,0.00032429953,0.00003171835,0.0084659355],"study_design_scores_gemma":[0.00033269485,0.00032882649,0.9941293,0.00007841503,0.000010289987,0.00024341585,0.00030382225,0.00007452081,0.000052163803,0.0008120767,0.0034685957,0.00016586263],"about_ca_topic_score_codex":0.02669258,"about_ca_topic_score_gemma":0.9842459,"teacher_disagreement_score":0.9575533,"about_ca_system_score_codex":0.000001781242,"about_ca_system_score_gemma":0.0010020656,"threshold_uncertainty_score":0.99988407},"labels":[],"label_agreement":null},{"id":"W2572477845","doi":"10.1139/cjes-2016-0170","title":"U–Pb zircon geochronology and depositional history of the Montresor group, Rae Province, Nunavut, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Geological Survey of Canada","funders":"","keywords":"Zircon; Geology; Geochronology; Provenance; Geochemistry; Sedimentary depositional environment; Igneous rock; Paleontology; Structural basin","score_opus":0.010311042669534594,"score_gpt":0.16072770249142448,"score_spread":0.1504166598218899,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2572477845","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.985838,0.003109366,0.0000071226955,0.0029298337,0.000480061,0.00003788937,0.000033082404,8.0209105e-7,0.0075638513],"genre_scores_gemma":[0.9988898,0.000019824462,0.0003270641,0.00035595085,0.00006632684,9.106027e-8,0.0000012878895,5.518039e-7,0.00033909606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990974,0.000048186976,0.00022210092,0.00012966689,0.00024363576,0.00025898704],"domain_scores_gemma":[0.9990377,0.000080717735,0.00033145168,0.00012486565,0.00007677634,0.00034853318],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002966352,0.00007616214,0.00017224973,0.0000663107,0.0004923311,0.0000495806,0.0006336996,0.000037691087,0.001676495],"category_scores_gemma":[0.00021204507,0.00004352049,0.00006284184,0.000065076514,0.0015011022,0.00019175952,0.000013697193,0.00013578561,0.0000019282581],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000038602284,0.0000022573413,0.99641067,0.0000040805867,0.000011572815,0.000036440197,0.000023707027,0.00026079486,0.00018285924,0.00015262728,0.00073656894,0.0021745434],"study_design_scores_gemma":[0.000102116814,0.00009205653,0.9873759,0.000016782313,0.000016242739,0.000079305675,0.00004618172,0.0005100252,0.0001804239,0.0017103719,0.009806687,0.000063865176],"about_ca_topic_score_codex":0.9264376,"about_ca_topic_score_gemma":0.99949104,"teacher_disagreement_score":0.073053434,"about_ca_system_score_codex":0.000008432974,"about_ca_system_score_gemma":0.0033483026,"threshold_uncertainty_score":0.9992361},"labels":[],"label_agreement":null},{"id":"W2575348785","doi":"10.1139/cjes-2016-0007","title":"The geology, petrology, and geochronology of the Archean Côté Gold large-tonnage, low-grade intrusion-related Au(–Cu) deposit, Swayze greenstone belt, Ontario, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Laurentian University","funders":"Natural Resources Canada; IAMGOLD","keywords":"Diorite; Geology; Geochemistry; Greenstone belt; Geochronology; Archean; Zircon; Mafic; Felsic; Batholith; Hornblende; Skarn; Petrology; Fluid inclusions; Quartz; Biotite; Tectonics; Paleontology","score_opus":0.009767576593120763,"score_gpt":0.18811368963983616,"score_spread":0.17834611304671538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2575348785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9780761,0.0020541574,0.0000013379945,0.016291447,0.0007827465,0.00006336719,0.000027140712,0.000002034629,0.0027016804],"genre_scores_gemma":[0.9988295,0.00004656062,0.000065751374,0.00036989927,0.000082406856,2.1801489e-7,0.0000031625846,0.0000014541793,0.00060109],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982079,0.00013189475,0.0004350617,0.00024276203,0.00028623673,0.0006961042],"domain_scores_gemma":[0.9984119,0.000247799,0.00042975458,0.0002829346,0.000102010476,0.0005256304],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["sts"],"category_scores_codex":[0.0010200399,0.00015327298,0.0003087599,0.00010869338,0.0019059262,0.00012973485,0.001330877,0.00010744576,0.0010975007],"category_scores_gemma":[0.0003624904,0.000075452765,0.00012020989,0.00019005044,0.0037968964,0.0001482886,0.00007263608,0.00054246624,0.000006489245],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007689421,0.0000030409358,0.9959141,0.000003796527,0.000046379762,0.000077631346,0.00016001813,0.00028480717,0.00003099825,0.0002875395,0.00025503465,0.0029289646],"study_design_scores_gemma":[0.00016434611,0.00015721492,0.9875813,0.000023905599,0.00004383672,0.00028005915,0.0001755035,0.001065545,0.00004797588,0.0069063012,0.0034536216,0.00010040195],"about_ca_topic_score_codex":0.99669003,"about_ca_topic_score_gemma":0.99998885,"teacher_disagreement_score":0.020753369,"about_ca_system_score_codex":0.000011732668,"about_ca_system_score_gemma":0.0028154869,"threshold_uncertainty_score":0.99981564},"labels":[],"label_agreement":null},{"id":"W2575585937","doi":"10.1139/cjes-2016-0120","title":"Geophysical, geological, and hydrogeological characterization of a tributary buried bedrock valley in southern Ontario","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Guelph","funders":"Ontario Water Consortium","keywords":"Bedrock; Geology; Geomorphology; Aquifer; Electrical resistivity tomography; Tributary; Alluvium; Quaternary; Fluvial; Borehole; Hydrogeology; Groundwater; Groundwater flow; Paleontology; Structural basin","score_opus":0.028219766458761234,"score_gpt":0.22793143372742647,"score_spread":0.19971166726866524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2575585937","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99781156,0.0000962946,0.000031573334,0.00083768455,0.00012769985,0.00006859693,0.000019528094,0.000001807419,0.0010052815],"genre_scores_gemma":[0.9987426,0.000009998746,0.00083115074,0.000103751605,0.000090197704,1.9480383e-7,0.0000031936281,9.824618e-7,0.00021794454],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987637,0.000110334506,0.00033835022,0.000188905,0.00022450178,0.00037420815],"domain_scores_gemma":[0.998886,0.00013822931,0.00034424642,0.000114821865,0.000071078495,0.0004456461],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006803621,0.00010981323,0.00033290405,0.0001595284,0.00041314578,0.00013068941,0.00048731235,0.00007831493,0.00067771546],"category_scores_gemma":[0.00034353486,0.00007311437,0.00007017706,0.00019531763,0.0008691083,0.0003303974,0.000013185783,0.00024938595,0.000014586323],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027975811,0.000016226371,0.9819313,0.0000040595605,0.0000069462744,0.00006189947,0.00045126094,0.00016424178,0.0003368538,0.00012064609,0.000002856769,0.016875682],"study_design_scores_gemma":[0.00021599456,0.00070169027,0.9896827,0.00002469914,0.000008003064,0.000028067196,0.00006426422,0.0008333233,0.00011223199,0.007599137,0.0006343941,0.00009553866],"about_ca_topic_score_codex":0.2771823,"about_ca_topic_score_gemma":0.6726492,"teacher_disagreement_score":0.3954669,"about_ca_system_score_codex":0.0000019272377,"about_ca_system_score_gemma":0.0006077361,"threshold_uncertainty_score":0.7420509},"labels":[],"label_agreement":null},{"id":"W2576810053","doi":"10.1139/e11-074","title":"Vein assemblages and fluid evolution in <sup>18</sup>O-depleted Neoproterozoic igneous rocks of the Mira terrane, Cape Breton Island, Nova Scotia<sup>1</sup>This article is one of a series of papers published in <i>CJES Special Issue: In honour of Ward Neale</i> on the theme of Appalachian and Grenvillian geology.<sup>2</sup>Laboratory for Stable Isotope Science (LSIS) Contribution 251.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University; Western University","funders":"","keywords":"Epidote; Geology; Calcite; Quartz; Fluid inclusions; Geochemistry; Vein; Terrane; Igneous rock; Albite; Petrography; Pyrite; Mineralogy; Chlorite; Paleontology","score_opus":0.012081561850751245,"score_gpt":0.20048101266794008,"score_spread":0.18839945081718884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2576810053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943132,0.0027894066,0.0000063732264,0.0010963624,0.00010553176,0.0005024416,0.00021667825,0.0000016131903,0.0009684063],"genre_scores_gemma":[0.99963486,0.00006551124,0.00014633228,0.00006740414,0.00007247583,0.0000018133951,0.0000019722304,0.0000021569494,0.0000074484014],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973617,0.00036600258,0.0008765395,0.00027961968,0.00048298074,0.0006331365],"domain_scores_gemma":[0.99832577,0.0003300474,0.00062396144,0.00021008057,0.00026826476,0.00024188565],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0033962538,0.00019613534,0.00058637897,0.00069758826,0.00027661506,0.000053845153,0.00057592965,0.00015520028,0.00040503588],"category_scores_gemma":[0.0007225269,0.00013421406,0.00008492358,0.0014651703,0.0032826273,0.0010726562,0.000010978702,0.0003077958,3.7954297e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023387103,0.00004983145,0.9858264,0.000061425024,0.000021083015,0.0000033944093,0.0065501044,0.002847879,0.0027266948,0.00012160318,0.000060959857,0.0014967807],"study_design_scores_gemma":[0.0008761364,0.00092027034,0.9797683,0.00029160062,0.000023030303,0.000035532772,0.005111599,0.004419101,0.008007534,0.0003297014,0.00007885621,0.00013838559],"about_ca_topic_score_codex":0.029578846,"about_ca_topic_score_gemma":0.3153622,"teacher_disagreement_score":0.28578335,"about_ca_system_score_codex":0.0000113597935,"about_ca_system_score_gemma":0.0010806095,"threshold_uncertainty_score":0.9994299},"labels":[],"label_agreement":null},{"id":"W2578542971","doi":"10.1139/cjes-2016-0160","title":"The pre-Late Wisconsin stratigraphy of southern Simcoe County, Ontario: implications for ice sheet buildup, decay, and Great Lakes drainage evolution","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Subaerial; Glacial period; Stratigraphy; Radiocarbon dating; Unconformity; Paleontology; Sedimentary rock; Ice sheet; Sediment; Paleosol; Geomorphology; Geochemistry; Loess","score_opus":0.028465993202947137,"score_gpt":0.2596896211206548,"score_spread":0.23122362791770767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2578542971","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893257,0.0017236727,0.00004827806,0.0026963428,0.00018433972,0.00015223424,0.00016241214,0.0000014632683,0.0057055727],"genre_scores_gemma":[0.9992916,0.000029838728,0.00031691743,0.000031895044,0.000028681712,7.2828095e-7,0.0000026520515,0.0000010230706,0.00029668782],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99906063,0.00007249815,0.0002362171,0.00014065517,0.00012687096,0.00036314942],"domain_scores_gemma":[0.9986596,0.00038861815,0.0002994667,0.00018441018,0.00018017612,0.00028772518],"candidate_categories":["sts"],"consensus_categories":["sts"],"category_scores_codex":[0.0013828545,0.000081173086,0.0001521614,0.00014802146,0.0025406736,0.00025041023,0.00062642223,0.00006640338,0.00010905887],"category_scores_gemma":[0.0001948997,0.00005271242,0.000057947047,0.00009879067,0.002748097,0.00032874072,0.0000066023094,0.00015782032,0.0000031819443],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016901493,0.0000015157401,0.99688435,0.000004874493,0.000016229404,0.0000035218268,0.0003232905,0.00022584235,0.000008352324,0.0020099012,0.000047931077,0.00045731457],"study_design_scores_gemma":[0.00015594813,0.00022850327,0.97945637,0.000019161229,0.000016598655,0.00009369356,0.00031067908,0.0003046124,0.0000090129015,0.018264854,0.0010805953,0.000059953167],"about_ca_topic_score_codex":0.111020125,"about_ca_topic_score_gemma":0.99541104,"teacher_disagreement_score":0.88439095,"about_ca_system_score_codex":8.1729195e-7,"about_ca_system_score_gemma":0.0017488606,"threshold_uncertainty_score":0.99996585},"labels":[],"label_agreement":null},{"id":"W2580545760","doi":"10.1139/cjes-2016-0126","title":"Geochronological constraints on magmatism and polyphase deformation and metamorphism in the southern Omineca Belt, British Columbia","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Metamorphism; Monazite; Zircon; Geochemistry; Kyanite; Sillimanite; Pluton; Magmatism; Plutonism; Cretaceous; Terrane; Metamorphic rock; Paleontology; Tectonics","score_opus":0.017950841760687685,"score_gpt":0.19817529361812528,"score_spread":0.1802244518574376,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2580545760","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99406147,0.0006591293,0.0000024153208,0.0021776822,0.000054153097,0.000046377558,0.00004659681,0.0000011314787,0.0029510532],"genre_scores_gemma":[0.9992157,0.000043301774,0.0002092839,0.00045517695,0.000033667962,1.5866613e-7,0.000002485,3.8967292e-7,0.000039802766],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992173,0.000055882545,0.00019839601,0.000120311604,0.00017172012,0.00023643536],"domain_scores_gemma":[0.9993593,0.000107861626,0.0001642374,0.000073461495,0.000030140405,0.00026497466],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008623416,0.00005716366,0.0001510383,0.00006341912,0.00078641716,0.00096360914,0.00033763534,0.00004253398,0.0028071136],"category_scores_gemma":[0.00033302163,0.000040767365,0.000034799934,0.000087991706,0.001613304,0.00026726807,0.0000064443184,0.00015646337,0.000010590243],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000022418965,0.000003995494,0.89405566,0.000002042701,0.0000051758498,0.00013886593,0.00015810208,0.00002917082,0.000008031334,0.000033769382,0.00005952608,0.10550342],"study_design_scores_gemma":[0.00017282653,0.00018070012,0.99119353,0.000024092571,0.000009975605,0.00040459447,0.00048441044,0.00048217032,0.0000028885959,0.006770614,0.00021231135,0.00006190106],"about_ca_topic_score_codex":0.33694074,"about_ca_topic_score_gemma":0.98220164,"teacher_disagreement_score":0.64526093,"about_ca_system_score_codex":6.8995837e-7,"about_ca_system_score_gemma":0.0001097714,"threshold_uncertainty_score":0.99810445},"labels":[],"label_agreement":null},{"id":"W2580563375","doi":"10.1139/cjes-2016-0201","title":"Lillooet Glacier basalts, southwestern British Columbia, Canada: products of Quaternary glaciovolcanism","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Basalt; Geology; Pillow lava; Geochemistry; Breccia; Phenocryst; Basaltic andesite; Andesite; Flood basalt; Mafic; Plagioclase; Magma; Olivine; Quaternary; Volcanic rock; Volcano; Paleontology; Volcanism; Quartz","score_opus":0.01715127084405115,"score_gpt":0.18487717937140052,"score_spread":0.16772590852734937,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2580563375","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942906,0.0008891298,0.0000022259635,0.0013998826,0.00058757677,0.000052977444,0.00013855936,0.000002065066,0.0026370045],"genre_scores_gemma":[0.9982394,0.000028932269,0.0003711292,0.00026501817,0.00016841589,1.1855059e-7,0.000005122393,0.0000015581487,0.00092030794],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99829435,0.000051904262,0.00042547204,0.0002409557,0.00049840065,0.00048893737],"domain_scores_gemma":[0.99815756,0.000055259177,0.00052471634,0.00022264499,0.00028052472,0.00075931026],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006631011,0.000098396835,0.00032648086,0.00007105919,0.00085216045,0.00062033837,0.0011081072,0.0000503201,0.004558306],"category_scores_gemma":[0.00053061766,0.00009635879,0.00009693672,0.00021144607,0.0010105507,0.00040604192,0.000016104732,0.00017481795,0.00001300381],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000022927145,0.0000037347054,0.99595505,0.00000879298,0.000017556396,0.0002395127,0.000037313806,0.00011990994,0.000027829848,0.0000033580015,0.00040839726,0.0031762223],"study_design_scores_gemma":[0.00012880539,0.00016027021,0.992194,0.000051916162,0.000021785572,0.00015905133,0.00013397797,0.00018299127,0.00011449567,0.0011935841,0.005523208,0.00013590093],"about_ca_topic_score_codex":0.9980482,"about_ca_topic_score_gemma":0.9999615,"teacher_disagreement_score":0.005114811,"about_ca_system_score_codex":0.0000029410182,"about_ca_system_score_gemma":0.003391614,"threshold_uncertainty_score":0.99635166},"labels":[],"label_agreement":null},{"id":"W2582739005","doi":"10.1139/cjes-2016-0123","title":"Flux of methane release and carbon dioxide sequestration at Winterhouse Canyon, Gros Morne, Newfoundland, Canada: a site of continental serpentinization","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Canyon; Methane; Carbon sequestration; Flux (metallurgy); Carbon dioxide; Atmosphere (unit); Geology; Oceanography; Environmental science; Earth science; Geomorphology; Ecology; Chemistry; Geography; Meteorology","score_opus":0.00883989735729157,"score_gpt":0.19668585901606866,"score_spread":0.1878459616587771,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2582739005","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982724,0.000080157646,0.00006673611,0.00017107472,0.00015591207,0.000073454954,0.0000119606475,9.931017e-7,0.0011672917],"genre_scores_gemma":[0.9984609,0.000027083284,0.0009005475,0.000040785493,0.000019997886,3.569885e-7,0.0000016463758,0.000005435021,0.0005432376],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989788,0.000032240627,0.00032371256,0.00014282561,0.00031445405,0.00020796583],"domain_scores_gemma":[0.99889547,0.000018319264,0.0005821565,0.0001421056,0.000017783934,0.00034414572],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003139004,0.00009706859,0.0001884904,0.000020216503,0.00020395665,0.00003105255,0.000249466,0.000034877718,0.00016727175],"category_scores_gemma":[0.00009063695,0.000084947475,0.000033406337,0.00008293154,0.0009887379,0.00034221224,0.000052276802,0.00006957853,8.107117e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012178305,0.0000055687656,0.98506457,0.0000053309477,0.000007117063,0.0000268256,0.00019775225,0.0064219986,0.007830928,0.000012991016,0.000021753634,0.00039296414],"study_design_scores_gemma":[0.0002821475,0.0001827506,0.9927725,0.00003846648,0.00002260947,0.00007213595,0.00019013678,0.0034350497,0.0025012172,0.000028857288,0.0003784985,0.00009559316],"about_ca_topic_score_codex":0.89733547,"about_ca_topic_score_gemma":0.9915247,"teacher_disagreement_score":0.09418922,"about_ca_system_score_codex":0.00009596938,"about_ca_system_score_gemma":0.00041743452,"threshold_uncertainty_score":0.3643046},"labels":[],"label_agreement":null},{"id":"W2584665131","doi":"10.1139/cjes-2016-0119","title":"A large onychodontiform (Osteichthyes: Sarcopterygii) apex predator from the Eifelian-aged Dundee Formation of Ontario, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; University of Toronto","funders":"Pioneers in Health Care Innovation Fund, University of Twente","keywords":"Devonian; Paleontology; Geology; Apex (geometry); Vertebrate; Dentition; Anatomy; Biology","score_opus":0.022950322531346393,"score_gpt":0.21301023676509295,"score_spread":0.19005991423374657,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2584665131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98626065,0.0013887576,0.000041297135,0.0016027794,0.0014337298,0.00008114264,0.0003487585,0.0000015238778,0.008841364],"genre_scores_gemma":[0.99888283,0.00001934878,0.00030147083,0.0004174964,0.00013877515,1.9602956e-7,0.000019028439,9.1721677e-7,0.00021990889],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99872845,0.00009283847,0.00036882135,0.00013406818,0.00025984002,0.00041596097],"domain_scores_gemma":[0.99857545,0.00019499833,0.0005614352,0.00023416309,0.00010030827,0.00033362952],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009814894,0.000103597595,0.00020771551,0.00008918347,0.0015308162,0.000109345936,0.0010776999,0.000073018746,0.0020952332],"category_scores_gemma":[0.00028289304,0.00006542983,0.00006531659,0.00008851333,0.00069101463,0.0008283088,0.000008817859,0.00022368281,0.000014838341],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020133713,0.000002181012,0.9962844,0.0000020576751,0.000016143074,0.00003147144,0.0007185174,0.000097681346,0.000007251482,0.000042895204,0.0018412169,0.00093604653],"study_design_scores_gemma":[0.00023684588,0.00013891733,0.9663768,0.000035913952,0.000014618677,0.00008287109,0.00047635337,0.0003007176,0.0000345486,0.00048227826,0.031739876,0.000080302605],"about_ca_topic_score_codex":0.98977804,"about_ca_topic_score_gemma":0.9999928,"teacher_disagreement_score":0.029907648,"about_ca_system_score_codex":0.000014547717,"about_ca_system_score_gemma":0.008252293,"threshold_uncertainty_score":0.99976903},"labels":[],"label_agreement":null},{"id":"W2586856274","doi":"10.1139/cjes-2016-0151","title":"Lithostratigraphic and allostratigraphic framework of the Cambrian–Ordovician Potsdam Group and correlations across Early Paleozoic southern Laurentia","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Ottawa","funders":"","keywords":"Siliciclastic; Geology; Marine transgression; Unconformity; Graben; Paleontology; Ordovician; Paleozoic; Progradation; Rift; Sedimentary depositional environment; Sedimentary rock; Structural basin","score_opus":0.017676896075085137,"score_gpt":0.2347388481425175,"score_spread":0.21706195206743237,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2586856274","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9872546,0.008225457,0.000020061967,0.00059564743,0.00053512485,0.00009696121,0.00012579066,0.0000025726767,0.0031437625],"genre_scores_gemma":[0.99917495,0.00008958157,0.00060339767,0.000042522362,0.00006882855,2.1001422e-7,4.3199913e-7,9.1724905e-7,0.000019150928],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99869573,0.00011129821,0.00035067165,0.00019622136,0.00025376148,0.00039232668],"domain_scores_gemma":[0.9985246,0.00016134091,0.0005443582,0.0002417885,0.000065314496,0.00046257646],"candidate_categories":["sts"],"consensus_categories":["sts"],"category_scores_codex":[0.0008202666,0.00014158737,0.00023095695,0.00016987225,0.00247932,0.00046139932,0.00067119405,0.00013818007,0.000055141],"category_scores_gemma":[0.0002048409,0.00009502198,0.00011176658,0.00026155115,0.0037067623,0.00050224946,0.0000033544245,0.00036889725,8.54345e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000055218497,0.0000027845701,0.9910892,0.000005893348,0.000023800494,0.0000135470755,0.0011947686,0.000005406037,0.00001171252,0.0010272701,0.00000305122,0.006617023],"study_design_scores_gemma":[0.00014728309,0.00025658074,0.99454355,0.00012486886,0.000027562923,0.00010456889,0.0009810694,0.000077186756,0.000004421649,0.0035718756,0.00005043219,0.0001106199],"about_ca_topic_score_codex":0.031166006,"about_ca_topic_score_gemma":0.9152581,"teacher_disagreement_score":0.8840921,"about_ca_system_score_codex":2.696603e-7,"about_ca_system_score_gemma":0.00039276914,"threshold_uncertainty_score":0.9990046},"labels":[],"label_agreement":null},{"id":"W2587189918","doi":"10.1139/cjes-2016-0146","title":"Hydrothermally altered volcanic rocks metamorphosed at granulite-facies conditions: an example from the Grenville Province","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Gneiss; Granulite; Geology; Geochemistry; Protolith; Sillimanite; Metamorphic rock; Felsic; Volcanic rock; Mafic; Facies; Biotite; Quartz; Volcano; Geomorphology","score_opus":0.04238839019482654,"score_gpt":0.21602145320884203,"score_spread":0.1736330630140155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2587189918","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931185,0.0012539219,0.00001546381,0.002132186,0.00026835952,0.00008131993,0.00016968865,0.000004032155,0.0029564768],"genre_scores_gemma":[0.9985505,0.000025286758,0.00022251073,0.00062442524,0.0002028297,4.208457e-7,0.00002329313,0.0000014805202,0.00034925088],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851835,0.000108559885,0.0003202525,0.00026240182,0.0003552904,0.00043514208],"domain_scores_gemma":[0.9982889,0.00020337562,0.0003954632,0.00033327035,0.000097177006,0.0006817947],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00069408613,0.00014026246,0.00025035182,0.000080870734,0.002499557,0.00052923197,0.0014830201,0.00004926581,0.018120494],"category_scores_gemma":[0.00020021446,0.00007631942,0.00014374046,0.00014705326,0.0013923857,0.00055761694,0.000019002728,0.00017634362,0.00010556105],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013191131,0.000006053212,0.9954498,0.0000012034868,0.000035505793,0.00006297808,0.00025401375,0.0016227294,0.00046526614,0.00005352521,0.00029848912,0.0017372346],"study_design_scores_gemma":[0.00021669209,0.00020997487,0.9780909,0.00001772152,0.00004392855,0.000047681995,0.0002976011,0.0019644739,0.00048539718,0.007422389,0.011048743,0.00015453371],"about_ca_topic_score_codex":0.49581698,"about_ca_topic_score_gemma":0.9675186,"teacher_disagreement_score":0.47170165,"about_ca_system_score_codex":0.0000025694185,"about_ca_system_score_gemma":0.0005535289,"threshold_uncertainty_score":0.998799},"labels":[],"label_agreement":null},{"id":"W2587853641","doi":"10.1139/cjes-2016-0104","title":"Geology, U–Pb zircon geochronology, and geochemistry of PGE-bearing Neoarchean and Paleoproterozoic gabbroic rocks of the Peter Lake domain, southern Hearne craton, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Government of Saskatchewan","funders":"Natural Resources Canada","keywords":"Geology; Zircon; Geochemistry; Craton; Gabbro; Layered intrusion; Continental arc; Geochronology; Precambrian; Mafic; Mantle plume; Igneous rock; Volcanic rock; Paleontology; Lithosphere","score_opus":0.011515956819226947,"score_gpt":0.18570795244713628,"score_spread":0.17419199562790932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2587853641","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99501276,0.0012684789,0.000007939033,0.0019860514,0.00009698378,0.000049835628,0.000058870995,0.0000010069059,0.0015180978],"genre_scores_gemma":[0.99938923,0.00002516188,0.0003007276,0.00015321009,0.000050655086,1.5704617e-7,0.0000016643236,0.0000011303473,0.00007804751],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987893,0.00006163154,0.00034173098,0.00020053342,0.00022851682,0.00037828865],"domain_scores_gemma":[0.99871725,0.000096116724,0.00045573123,0.000202992,0.00011684398,0.00041106908],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005516627,0.00012244859,0.0003082336,0.00007406435,0.00059004046,0.000069702925,0.00061275926,0.000076842574,0.0011483232],"category_scores_gemma":[0.0002777134,0.00007420089,0.00007224071,0.00011432256,0.00266508,0.00012145726,0.00004210297,0.00024418402,0.0000011083256],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000067399847,0.0000020577752,0.99719626,0.00001759446,0.000019547377,0.000017675708,0.000107661195,0.00012849376,0.0010897161,0.000007307964,0.000022584833,0.0013843377],"study_design_scores_gemma":[0.00019383381,0.00012285703,0.9922164,0.000049210998,0.000022206612,0.00014963285,0.0004875261,0.00017433657,0.002660387,0.0032225684,0.00060051354,0.000100530706],"about_ca_topic_score_codex":0.78960645,"about_ca_topic_score_gemma":0.99738497,"teacher_disagreement_score":0.20777847,"about_ca_system_score_codex":0.0000015853487,"about_ca_system_score_gemma":0.0009053145,"threshold_uncertainty_score":0.99976474},"labels":[],"label_agreement":null},{"id":"W2590310259","doi":"10.1139/cjes-2016-0163","title":"Evidence for voluminous bimodal pyroclastic volcanism during rifting of a Paleoproterozoic arc at Snow Lake, Manitoba","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada; Society of Economic Geologists Canada Foundation; Society of Economic Geologists Foundation","keywords":"Geology; Pyroclastic rock; Felsic; Geochemistry; Rift; Sequence stratigraphy; Petrology; Volcano; Geomorphology; Structural basin; Sedimentary depositional environment","score_opus":0.05908908923233342,"score_gpt":0.23440177646660484,"score_spread":0.17531268723427143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2590310259","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971854,0.0008787556,0.00004555696,0.0006789963,0.00030136105,0.00010098464,0.000050014103,0.0000029439982,0.0007559774],"genre_scores_gemma":[0.99835134,0.000030904794,0.0011914717,0.000053686905,0.00020922285,5.941794e-7,0.0000019658135,0.0000015698583,0.00015925016],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99842644,0.00003547321,0.00041471337,0.00024008485,0.00034609923,0.0005371727],"domain_scores_gemma":[0.9980875,0.00031412698,0.00059015467,0.00018235589,0.00020801848,0.00061783363],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000732864,0.00013154239,0.00030558207,0.00019941309,0.001386009,0.00022290836,0.0009519045,0.000057704943,0.001930837],"category_scores_gemma":[0.0020181106,0.000092509894,0.00018550431,0.0001782877,0.0009818051,0.0004982116,0.000021645672,0.00014143005,0.000024666908],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022709959,0.0000030466724,0.99581975,0.00002573235,0.000015449288,0.000047315796,0.00007517508,0.00092940626,0.0005189759,0.0000103741195,0.000015281434,0.002516777],"study_design_scores_gemma":[0.00019318153,0.00035545623,0.9929773,0.00022244059,0.000036165173,0.000089876026,0.00011205286,0.0019415345,0.0018409558,0.0018745571,0.00022328681,0.00013318774],"about_ca_topic_score_codex":0.029879536,"about_ca_topic_score_gemma":0.90675735,"teacher_disagreement_score":0.8768778,"about_ca_system_score_codex":0.0000030124681,"about_ca_system_score_gemma":0.00044214394,"threshold_uncertainty_score":0.99991405},"labels":[],"label_agreement":null},{"id":"W2591687417","doi":"10.1139/cjes-2016-0127","title":"Cambrian detrital zircon signatures of the northern Cordilleran passive margin, Liard area, Canada: evidence of sediment recycling, non-Laurentian ultimate sources, and basement denudation","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Government of British Columbia; Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Geology; Zircon; Basement; Provenance; Laurentia; Proterozoic; Precambrian; Paleontology; Geochemistry; Clastic rock; Conglomerate; Sedimentary rock; Unconformity; Paleozoic; Archaeology; Tectonics","score_opus":0.016576182645511466,"score_gpt":0.20178428079898947,"score_spread":0.185208098153478,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2591687417","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958785,0.0017144708,0.000016624277,0.0016130682,0.0003000656,0.000082137994,0.00005118963,6.8408394e-7,0.00034323885],"genre_scores_gemma":[0.9994466,0.000058096426,0.00028876666,0.00010702584,0.0000487457,1.9209043e-7,0.0000027132494,9.877509e-7,0.00004690938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986357,0.000058225552,0.00038113567,0.00017081901,0.0004768975,0.00027721075],"domain_scores_gemma":[0.99833405,0.0001366527,0.0007496797,0.00016633859,0.00022906286,0.00038422632],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005448833,0.000112010304,0.00025236787,0.000086002095,0.0006087745,0.000102544764,0.00066063134,0.000044604767,0.0008295029],"category_scores_gemma":[0.0004645588,0.00006542023,0.000092419825,0.00017738083,0.0007549536,0.00023579164,0.000019368019,0.00015586537,8.516854e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010547283,0.0000034661875,0.993997,0.00001292744,0.000025625584,0.000014963521,0.00010704021,0.0019529642,0.00069451187,0.000002696025,0.00008249383,0.0030957973],"study_design_scores_gemma":[0.00014201736,0.00017355042,0.99244857,0.00024017978,0.000046533773,0.000010624476,0.00035097057,0.0015304261,0.004545366,0.00017499646,0.00024356759,0.000093182236],"about_ca_topic_score_codex":0.859565,"about_ca_topic_score_gemma":0.9979135,"teacher_disagreement_score":0.13834849,"about_ca_system_score_codex":0.0000049944824,"about_ca_system_score_gemma":0.001151607,"threshold_uncertainty_score":0.9082475},"labels":[],"label_agreement":null},{"id":"W2592848396","doi":"10.1139/cjes-2016-0195","title":"Diagenetic apatite character and in situ ion microprobe U–Pb age, Keeseville Formation, Potsdam Group, New York State","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Laurentian University; Geological Survey of Canada; University of Ottawa","funders":"University of Ottawa","keywords":"Fluorapatite; Geology; Cementation (geology); Geochemistry; Diagenesis; Mineralogy; Apatite; Cement; Materials science; Composite material","score_opus":0.019589915413292216,"score_gpt":0.2019645279913238,"score_spread":0.1823746125780316,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2592848396","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99551183,0.0010949802,0.000014806842,0.00084193604,0.00021022206,0.000047596466,0.000016711832,0.0000012711163,0.002260625],"genre_scores_gemma":[0.9986122,0.00012687499,0.0006042233,0.00016055505,0.000105412386,1.06595266e-7,0.000009017145,0.0000010554995,0.00038053843],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99906594,0.00002878883,0.00027149206,0.00013363284,0.00018387519,0.0003162926],"domain_scores_gemma":[0.9990572,0.000020770767,0.00026518732,0.000110007495,0.000031666994,0.00051517354],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005246293,0.000091777896,0.00015062542,0.00018795281,0.0006205552,0.0005165749,0.0003790034,0.000028662631,0.0006144572],"category_scores_gemma":[0.00006177916,0.000071473354,0.00004328997,0.00016225607,0.0002810516,0.0007599966,0.00000760325,0.00010935406,0.000023571194],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007635849,0.0000031054255,0.98019695,0.000013316591,0.000008081633,0.000068109126,0.00061614206,0.00044042905,0.0016132947,0.0000030686494,0.00032482663,0.01670505],"study_design_scores_gemma":[0.00018592789,0.00009102008,0.9915442,0.00006505237,0.000008628356,0.000064536944,0.00022085883,0.0002570508,0.0012400283,0.00042849666,0.005787011,0.00010719051],"about_ca_topic_score_codex":0.032942116,"about_ca_topic_score_gemma":0.76269895,"teacher_disagreement_score":0.72975683,"about_ca_system_score_codex":0.000002266354,"about_ca_system_score_gemma":0.00025153396,"threshold_uncertainty_score":0.9734976},"labels":[],"label_agreement":null},{"id":"W2592935224","doi":"10.1139/cjes-2016-0108","title":"Secondary migration of petroleum along syncline axes: a case study of the southern Kuqa Foreland Basin","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"PetroChina Company Limited; National Natural Science Foundation of China; National Science Foundation","keywords":"Foreland basin; Syncline; Geology; Petroleum; Structural basin; Sedimentary rock; Maturity (psychological); Sedimentary basin; Mesozoic; Geochemistry; Basin modelling; Paleontology; Petrology; Geomorphology","score_opus":0.01956559790069262,"score_gpt":0.23271036040664225,"score_spread":0.21314476250594963,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2592935224","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987724,0.00018720476,0.00007977458,0.00026178747,0.00020122484,0.000049745944,0.000013612978,0.0000016992885,0.00043257544],"genre_scores_gemma":[0.9998216,0.000006466523,0.000043981774,0.0000117495965,0.000045495406,4.5184697e-7,1.7870913e-7,0.0000039853658,0.000066061446],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992237,0.000042722626,0.0003370652,0.00006069913,0.00021182746,0.00012397303],"domain_scores_gemma":[0.9992664,0.000023663682,0.00026710637,0.00018852064,0.000096436626,0.00015790264],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005675347,0.00006379953,0.00017421677,0.00021866917,0.00034707747,0.00008432229,0.00036334567,0.000026186615,0.00005225738],"category_scores_gemma":[0.00009622342,0.000040216655,0.000088767374,0.00015523029,0.00021663742,0.00024281666,0.000009016821,0.000119269054,0.0000010079801],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045704423,0.000029505512,0.8525582,0.000029052766,0.00012320915,0.000374491,0.014113898,0.13107371,0.00047266172,0.000012171211,0.00013094833,0.0010775852],"study_design_scores_gemma":[0.002852362,0.0014043346,0.5080954,0.00043288158,0.00039508787,0.0017387713,0.17212102,0.30602217,0.0034221646,0.00028337826,0.0026913923,0.000541043],"about_ca_topic_score_codex":0.031777598,"about_ca_topic_score_gemma":0.84253097,"teacher_disagreement_score":0.81075335,"about_ca_system_score_codex":0.0000046320565,"about_ca_system_score_gemma":0.00039332628,"threshold_uncertainty_score":0.9746699},"labels":[],"label_agreement":null},{"id":"W2595918084","doi":"10.1139/cjes-2016-0106","title":"Occurrence, origin, and significance of melagranites in the South Mountain Batholith, Nova Scotia","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Batholith; Geology; Geochemistry; Mafic; Porphyritic; Mineral; Mineralogy; Quartz; Tectonics; Paleontology","score_opus":0.03324824422166902,"score_gpt":0.2316174156122318,"score_spread":0.19836917139056276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2595918084","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99487877,0.00089238764,0.000003772153,0.000947173,0.00010859365,0.000041962965,0.000079841724,6.339753e-7,0.0030468446],"genre_scores_gemma":[0.9995343,0.000018360139,0.00022199574,0.00017597877,0.000037373946,5.143717e-8,0.0000016423568,2.5716056e-7,0.000010052623],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990327,0.00006432964,0.00025124568,0.00013311063,0.00024560592,0.00027305153],"domain_scores_gemma":[0.9991232,0.00015949465,0.00027816396,0.00012400246,0.00008071175,0.00023438701],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012306705,0.00007926819,0.00018836591,0.00016500444,0.00032856304,0.00021070562,0.00077941286,0.000027101514,0.0011215329],"category_scores_gemma":[0.00041706758,0.0000422326,0.000053244024,0.0002979633,0.0014254331,0.00027992306,0.0000057304833,0.00016008808,0.00001531455],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000031967334,0.0000023370208,0.9978862,0.0000038694598,0.0000033542144,0.000026629825,0.000371466,0.0002371129,0.000018540934,0.00012293927,0.000024797064,0.001299602],"study_design_scores_gemma":[0.00009076285,0.00012326264,0.9940913,0.000023199755,0.000011583198,0.000031320415,0.0008124929,0.00024209083,0.00007406984,0.0037857327,0.00064611726,0.000068081274],"about_ca_topic_score_codex":0.078289345,"about_ca_topic_score_gemma":0.64440656,"teacher_disagreement_score":0.5661172,"about_ca_system_score_codex":5.04477e-7,"about_ca_system_score_gemma":0.0003297409,"threshold_uncertainty_score":0.99979156},"labels":[],"label_agreement":null},{"id":"W2596326137","doi":"10.1139/cjes-2016-0168","title":"Tectonic and chemical implications of cathodoluminescent microstructures in quartz, Parry Sound domain, Ontario, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"University of Maine; National Science Foundation","keywords":"Geology; Quartz; Shear zone; Metamorphism; Metamorphic facies; Facies; Greenschist; Shearing (physics); Geochemistry; Fluid inclusions; Mineralogy; Tectonics; Paleontology","score_opus":0.018422130642050373,"score_gpt":0.21129223497219346,"score_spread":0.1928701043301431,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2596326137","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996147,0.0006937186,0.0000016039461,0.0018332371,0.00010115039,0.00003481449,0.000030571344,5.5873704e-7,0.0011573903],"genre_scores_gemma":[0.9991662,0.000008272267,0.00064042583,0.00013004204,0.000030632502,1.1894566e-7,0.0000025321995,5.8902674e-7,0.000021207055],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99906546,0.000025241417,0.00029619518,0.00015068032,0.00016384346,0.00029855725],"domain_scores_gemma":[0.9990248,0.00007901269,0.00025246842,0.00013147177,0.00007764225,0.0004346086],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035828355,0.00008406212,0.00021980936,0.00010000924,0.00034497233,0.00011832772,0.0004957852,0.000039728944,0.0014028051],"category_scores_gemma":[0.00018962387,0.00005865427,0.00004713681,0.0001348262,0.00082988624,0.00013734528,0.000009520399,0.00015367374,9.199273e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000037357252,0.0000018553471,0.9985406,0.0000031277202,0.0000052347364,0.000016693019,0.00014439874,0.000066820605,0.00048012135,0.000046215566,0.000051671508,0.0006395733],"study_design_scores_gemma":[0.00010826483,0.000046351634,0.9874709,0.000015036677,0.000008069982,0.00007300838,0.00014140469,0.0000225176,0.00049264205,0.010712313,0.00083289307,0.00007659431],"about_ca_topic_score_codex":0.9917854,"about_ca_topic_score_gemma":0.99994725,"teacher_disagreement_score":0.011069648,"about_ca_system_score_codex":0.000006487427,"about_ca_system_score_gemma":0.0020824075,"threshold_uncertainty_score":0.99951005},"labels":[],"label_agreement":null},{"id":"W2599938587","doi":"10.1139/cjes-2016-0133","title":"Great Plains polygonal fault system as expressed in Saskatchewan: Late Cretaceous fault initiation and graben formation","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Graben; Cretaceous; Fault (geology); Paleontology; Isopach map; Tectonics; Seismology; Facies; Structural basin","score_opus":0.02040582348195725,"score_gpt":0.22491175364789043,"score_spread":0.2045059301659332,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2599938587","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9901944,0.00045136528,0.00007820032,0.001098235,0.00032172722,0.00007456873,0.00003730498,0.000009744718,0.0077344514],"genre_scores_gemma":[0.99887085,0.000045524124,0.0005639625,0.00034014165,0.000060439896,2.1959576e-7,0.0000048103966,0.0000016080962,0.00011245851],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898183,0.000062660205,0.00027342353,0.00013178565,0.00026519384,0.00028509158],"domain_scores_gemma":[0.9991022,0.000051977942,0.00032356157,0.00010997097,0.00008019748,0.00033210852],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008337481,0.000095128285,0.00015632767,0.00038404323,0.00081286696,0.000516709,0.00038575375,0.000049252983,0.00013112527],"category_scores_gemma":[0.0001377233,0.00007579777,0.0000352538,0.000114823444,0.00034946596,0.0015841342,0.0000061632845,0.00015451857,0.000016396425],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000050813476,0.0000061055234,0.90500534,0.00007227877,0.00001645034,0.0006130488,0.0059194863,0.0028789085,0.00024147193,0.00017215808,0.0015179993,0.08350593],"study_design_scores_gemma":[0.0012536732,0.000867433,0.80921406,0.0009783257,0.000031538988,0.0015829069,0.015726859,0.14220594,0.0053495937,0.002735859,0.019470511,0.00058333203],"about_ca_topic_score_codex":0.07539772,"about_ca_topic_score_gemma":0.17530131,"teacher_disagreement_score":0.13932702,"about_ca_system_score_codex":0.0000062211816,"about_ca_system_score_gemma":0.0006324342,"threshold_uncertainty_score":0.9307593},"labels":[],"label_agreement":null},{"id":"W2604275651","doi":"10.1139/cjes-2016-0197","title":"Cenozoic tectonic and thermal history of the Nenana basin, central interior Alaska: new constraints from seismic reflection data, fracture history, and apatite fission-track analyses","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Air Force Office of Scientific Research; U.S. Air Force; ConocoPhillips","keywords":"Geology; Graben; Subduction; Seismology; Fission track dating; Pull apart basin; Structural basin; Tectonics; Intraplate earthquake; Thermal subsidence; Fault (geology); Rift; Paleontology; Sedimentary basin","score_opus":0.05014305328133397,"score_gpt":0.24535878628604493,"score_spread":0.19521573300471096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2604275651","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891295,0.007062394,0.000012256926,0.0021065648,0.0005505784,0.00003892526,0.000052801093,0.0000017898789,0.0010451779],"genre_scores_gemma":[0.9988425,0.00009019167,0.00024535749,0.00044460339,0.00011307127,3.1677796e-8,0.000005935539,0.000001087626,0.00025722658],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989515,0.00008216598,0.00025971857,0.00022759452,0.00021625312,0.00026278326],"domain_scores_gemma":[0.9986472,0.00009948739,0.0004384483,0.00024307086,0.000048610633,0.00052316603],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003240153,0.000114542556,0.00024975344,0.00010046094,0.00033087647,0.00008657441,0.00072623044,0.00006342523,0.0044899173],"category_scores_gemma":[0.00034068027,0.00006225756,0.000071123504,0.000074555195,0.0018888552,0.00045471775,0.000026626794,0.0002262378,0.0000026427988],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013394872,0.0000021702501,0.9794042,0.0000043711466,0.000032371543,0.000014181209,0.00030673525,0.00024284399,0.0008423144,0.0000011804946,0.0017911829,0.017345032],"study_design_scores_gemma":[0.0001432588,0.00011697793,0.9745728,0.000055574736,0.000070066126,0.000031348634,0.000087543594,0.0017808336,0.00025303045,0.00031620148,0.02248461,0.000087775246],"about_ca_topic_score_codex":0.13893563,"about_ca_topic_score_gemma":0.2959231,"teacher_disagreement_score":0.15698749,"about_ca_system_score_codex":0.000011957176,"about_ca_system_score_gemma":0.0013117827,"threshold_uncertainty_score":0.9964201},"labels":[],"label_agreement":null},{"id":"W2605233595","doi":"10.1139/cjes-2016-0161","title":"Subsurface heterogeneity in the geological and hydraulic properties of the hummocky Paris Moraine, Guelph, Ontario","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University; University of Guelph","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Moraine; Geology; Outwash plain; Permeameter; Geomorphology; Hydraulic conductivity; Sediment; Sedimentary rock; Hydrogeology; Hydrology (agriculture); Geochemistry; Glacial period; Soil science","score_opus":0.030813862693670944,"score_gpt":0.21928280750119827,"score_spread":0.18846894480752732,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2605233595","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99313647,0.00036335268,5.9301686e-7,0.0027722393,0.00012672888,0.00006904014,9.841507e-7,4.450303e-7,0.0035301307],"genre_scores_gemma":[0.9995892,0.000031538482,0.00005754738,0.00018675662,0.000013284359,3.798022e-7,2.3724906e-8,0.0000012313095,0.00012004275],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99919516,0.00005646565,0.00018271968,0.00010137831,0.0002493274,0.00021492512],"domain_scores_gemma":[0.9994679,0.000016333903,0.00019829099,0.00017504407,0.000010890816,0.00013153657],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009713607,0.00006416982,0.00011363464,0.000025191885,0.0007167801,0.00014006995,0.0008214507,0.000043917273,0.00014368034],"category_scores_gemma":[0.00008530497,0.000025790127,0.00004682484,0.000089157256,0.0018497331,0.00022138859,0.00006130277,0.00020190964,0.0000030008885],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000027690373,0.000004765105,0.9969458,0.0000010165744,0.000002825116,0.000014542419,0.0011925588,0.0013153655,0.00026832646,0.000021961483,0.00006156768,0.00016851752],"study_design_scores_gemma":[0.00009998112,0.00008263289,0.9954333,0.000028468105,0.0000058614555,0.0000846388,0.00020723815,0.00012101862,0.0005828082,0.00018529169,0.0031238603,0.000044903725],"about_ca_topic_score_codex":0.24752356,"about_ca_topic_score_gemma":0.9244462,"teacher_disagreement_score":0.6769227,"about_ca_system_score_codex":0.000012766845,"about_ca_system_score_gemma":0.00024536127,"threshold_uncertainty_score":0.75748724},"labels":[],"label_agreement":null},{"id":"W2606283455","doi":"10.1139/cjes-2016-0216","title":"Lithogeochemical characterization of the Middle–Upper Devonian Road River Group and Canol and Imperial formations on Trail River, east Richardson Mountains, Yukon: age constraints and a depositional model for fine-grained strata in the Lower Paleozoic Richardson trough","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon University; Geological Survey of Canada","funders":"","keywords":"Geology; Sedimentary depositional environment; Siliciclastic; Outcrop; Lithology; Turbidite; Turbidity current; Devonian; Geochemistry; Paleontology; Deposition (geology); Group (periodic table); Marine transgression; Conodont; Oil shale; Sedimentary rock; Structural basin; Biostratigraphy","score_opus":0.0284512704173739,"score_gpt":0.22349334240049987,"score_spread":0.19504207198312595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2606283455","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99716353,0.00038823485,0.000082432976,0.0010034383,0.00014356276,0.00020817446,0.0006025733,0.0000010447302,0.0004070309],"genre_scores_gemma":[0.9991695,0.000034430333,0.0006343309,0.00008598568,0.00005916234,0.00000160393,0.000010318976,7.485347e-7,0.000003908649],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990685,0.00007330277,0.00025359823,0.00015433654,0.00019848242,0.00025180355],"domain_scores_gemma":[0.99934036,0.000075158285,0.00025404824,0.000100141275,0.000048078702,0.00018219934],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052952545,0.00011447596,0.00017095589,0.00012083547,0.0009256114,0.000202431,0.0003118987,0.0000767344,0.000013240413],"category_scores_gemma":[0.000100920945,0.00007055016,0.00005480052,0.00008662623,0.0020512806,0.0005626911,0.000002512361,0.00015194563,8.517022e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019461023,0.000030666746,0.96253145,0.000030727406,0.000034490622,0.000033184995,0.010404243,0.00006265495,0.0013489736,0.0015942247,0.000013194059,0.023721566],"study_design_scores_gemma":[0.0005982283,0.00032724088,0.98830706,0.00007243036,0.000017648443,0.0001369333,0.0002907459,0.009113158,0.000025564601,0.001007172,0.000018426492,0.00008542093],"about_ca_topic_score_codex":0.0014678678,"about_ca_topic_score_gemma":0.17724961,"teacher_disagreement_score":0.17578174,"about_ca_system_score_codex":0.0000018079579,"about_ca_system_score_gemma":0.0003722046,"threshold_uncertainty_score":0.8377634},"labels":[],"label_agreement":null},{"id":"W2606508048","doi":"10.1139/cjes-2016-0189","title":"Seismic and gravity constraints on the crustal architecture of the Intermontane terranes, central Yukon","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon University; Geological Survey of Canada; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Terrane; Allochthon; Cretaceous; Clastic rock; Crust; Paleontology; Sedimentary rock; Basement; North American Plate; Volcanic rock; Imbrication; Lithology; Igneous rock; Tectonics; Volcano; Nappe; Plate tectonics","score_opus":0.017368657678364163,"score_gpt":0.19298004045207265,"score_spread":0.1756113827737085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2606508048","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98679554,0.000169648,0.000005308488,0.009247214,0.00019302305,0.00003980503,0.00003777263,6.7921627e-7,0.0035109886],"genre_scores_gemma":[0.99947274,0.000009113006,0.000041574905,0.00038526382,0.000048480295,3.762721e-8,4.4226792e-7,4.1437673e-7,0.000041934993],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992055,0.00006245371,0.00016430004,0.00010325548,0.00020804661,0.000256405],"domain_scores_gemma":[0.99921095,0.00010707815,0.00022767068,0.00013385022,0.000039572522,0.0002808832],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041331974,0.000074426775,0.00013657236,0.0000496478,0.0007350231,0.00013852815,0.0007195042,0.00002968628,0.0014967143],"category_scores_gemma":[0.00032136246,0.000030366497,0.00009238831,0.00009124537,0.0029371302,0.00008366861,0.000011714297,0.00021714927,0.0000026575995],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008271685,0.0000027203243,0.9845976,0.000002609787,0.000012204596,0.00002072343,0.00017955193,0.0010846197,0.00006118677,0.00014421572,0.000043471617,0.013842784],"study_design_scores_gemma":[0.00006307294,0.00012257801,0.9916035,0.000035419034,0.0000122100455,0.00011937254,0.00018663879,0.0007431158,0.0002569057,0.006412512,0.00039770725,0.00004698882],"about_ca_topic_score_codex":0.021530764,"about_ca_topic_score_gemma":0.34825987,"teacher_disagreement_score":0.3267291,"about_ca_system_score_codex":6.8904313e-7,"about_ca_system_score_gemma":0.0002297196,"threshold_uncertainty_score":0.9997763},"labels":[],"label_agreement":null},{"id":"W2606810677","doi":"10.1139/e10-070","title":"Ediacaran body and trace fossils in Miette Group (Windermere Supergroup) near Salient Mountain, British Columbia, CanadaRevision of the paper was carried out by Dr. Guy Narbonne following the passing away of both Hans Hofmann (<sup>†</sup>deceased May 19, 2010) and Eric Mountjoy (<sup>†</sup>deceased June 18, 2010) after manuscript submission.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Parks Canada","keywords":"Trace fossil; Macrofossil; Geology; Laurentia; Paleontology; Siliciclastic; Group (periodic table); Assemblage (archaeology); Ichnology; Trilobite; Supergroup; Paleozoic; Sedimentary depositional environment; Ordovician; Structural basin; Holocene","score_opus":0.011166801844636585,"score_gpt":0.202074428958306,"score_spread":0.1909076271136694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2606810677","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97475034,0.020265697,0.0000062376917,0.0028551156,0.0009964016,0.00035156848,0.00035979316,0.00000536876,0.00040950617],"genre_scores_gemma":[0.9986907,0.00016287962,0.00032333864,0.00045979532,0.00012546207,0.0000030065328,0.000007344849,0.0000064795404,0.00022098365],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9962267,0.00046127776,0.0009542547,0.0005387681,0.0008726065,0.00094637764],"domain_scores_gemma":[0.99761605,0.00033514496,0.00045567754,0.00036222587,0.0001239545,0.001106946],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":["sts"],"category_scores_codex":[0.002170271,0.00032408524,0.000682238,0.00023955687,0.0015751736,0.0007681549,0.00084021804,0.00027031972,0.0004300509],"category_scores_gemma":[0.00029826214,0.00026074483,0.00026099297,0.0006834019,0.0027362444,0.0009658973,0.000012060211,0.0008190624,5.3297487e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000045374203,0.000022731168,0.9845838,0.00003887541,0.000050751343,0.00017106882,0.0018867112,0.00015624698,0.0009168694,0.0000044350004,0.0056402534,0.0064829006],"study_design_scores_gemma":[0.00096485927,0.00025033831,0.98845375,0.00029762567,0.000087160566,0.00015398471,0.0024955897,0.0027005016,0.000051244926,0.00018748817,0.004029573,0.00032786388],"about_ca_topic_score_codex":0.41737878,"about_ca_topic_score_gemma":0.95537263,"teacher_disagreement_score":0.53799385,"about_ca_system_score_codex":0.000011011996,"about_ca_system_score_gemma":0.0015860101,"threshold_uncertainty_score":0.9999845},"labels":[],"label_agreement":null},{"id":"W2608228557","doi":"10.1139/cjes-2016-0164","title":"Hydraulic properties of the Paskapoo Formation in west-central Alberta","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta; Petroleum Technology Alliance Canada","keywords":"Hydraulic conductivity; Geology; Porosity; Siltstone; Aquifer; Cementation (geology); Sedimentary rock; Geomorphology; Mineralogy; Geochemistry; Petrology; Geotechnical engineering; Facies; Groundwater; Cement; Soil science; Structural basin; Soil water; Archaeology","score_opus":0.023342502946669536,"score_gpt":0.20372389948960729,"score_spread":0.18038139654293775,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2608228557","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99290156,0.00007480734,0.00001985533,0.002569953,0.00023120762,0.000049708047,5.489559e-7,3.241635e-7,0.004152018],"genre_scores_gemma":[0.9990478,0.000005032078,0.00002646095,0.00010324004,0.000015993643,6.209867e-7,2.5240588e-8,0.0000010552934,0.00079976994],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993499,0.000027310252,0.00018322411,0.00005630846,0.00019802403,0.00018524833],"domain_scores_gemma":[0.9995702,0.000008827563,0.00021160328,0.0001019666,0.000015364012,0.00009201879],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028678664,0.000044244065,0.00007824923,0.00004822504,0.0004888644,0.00010027957,0.0005254903,0.000014332856,0.00010941705],"category_scores_gemma":[0.000118249794,0.000025164942,0.000034820117,0.00009020483,0.00073866674,0.00076963735,0.00003462287,0.000055871493,0.000010903746],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000016599248,0.0000050089334,0.9896165,0.0000030185618,0.000002149773,0.0000033574631,0.003280228,0.00031787227,0.0013515675,0.00007328191,0.000106907995,0.005238447],"study_design_scores_gemma":[0.00010574427,0.00003337095,0.98892003,0.000047770616,0.0000027694555,0.000019222678,0.00048712408,0.00018099148,0.0045690574,0.00005534763,0.005540117,0.000038461563],"about_ca_topic_score_codex":0.040346853,"about_ca_topic_score_gemma":0.7323658,"teacher_disagreement_score":0.6920189,"about_ca_system_score_codex":0.000014786616,"about_ca_system_score_gemma":0.00010827298,"threshold_uncertainty_score":0.96604353},"labels":[],"label_agreement":null},{"id":"W2610115869","doi":"10.1139/cjes-2017-0013","title":"A new Early Devonian (Emsian) arthrodire from the Northwest Territories, Canada, and its significance for paleogeographic reconstruction","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature","funders":"Tallinna Tehnikaülikool; Aurora Research Institute","keywords":"Geology; Devonian; Paleontology; Archipelago; Fauna; Arctic; Genus; Oceanography","score_opus":0.017015876230566503,"score_gpt":0.19840195681182465,"score_spread":0.18138608058125816,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2610115869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9856144,0.007321294,0.000019199688,0.0036946854,0.0022903145,0.00009624694,0.0005472067,0.0000019127792,0.00041472047],"genre_scores_gemma":[0.9985296,0.0000925489,0.0006048786,0.00015975203,0.0005514775,4.0466853e-7,0.000009193631,0.0000010082065,0.00005114259],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990825,0.00005357016,0.00021280437,0.00018112859,0.0001259667,0.00034403664],"domain_scores_gemma":[0.99879754,0.00020761552,0.00029077017,0.00012561675,0.00009170339,0.00048673086],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0003896581,0.00009762544,0.00015401708,0.00006805711,0.0021638405,0.00017870817,0.0005552535,0.00006812668,0.00024853882],"category_scores_gemma":[0.0002355358,0.000066251196,0.000040687155,0.0000897447,0.00083093275,0.0004750371,0.0000032651428,0.0001465752,0.000001957084],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011401432,3.7925577e-7,0.9797573,0.0000010582368,0.000013685205,0.000016420472,0.00008998855,0.000018584062,0.0000021053131,0.00007146528,0.00013738376,0.01988022],"study_design_scores_gemma":[0.00015664392,0.00015801139,0.9829066,0.000025946096,0.000011796921,0.00014673574,0.0001358622,0.0001305234,0.00000756099,0.0011464471,0.015083795,0.000090079964],"about_ca_topic_score_codex":0.9850646,"about_ca_topic_score_gemma":0.99997675,"teacher_disagreement_score":0.01979014,"about_ca_system_score_codex":0.0000022551383,"about_ca_system_score_gemma":0.004179002,"threshold_uncertainty_score":0.9991352},"labels":[],"label_agreement":null},{"id":"W2611925948","doi":"10.1139/cjes-2016-0226","title":"Secondary rock structures and the regional hydrogeology of claystone-rich cretaceous strata, Williston Basin, Saskatchewan, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; Mosaic Company","keywords":"Geology; Cretaceous; Sedimentary rock; Structural basin; Fault (geology); Paleontology; Hydrogeology; Sequence stratigraphy; Denudation; Geomorphology; Facies; Tectonics; Geotechnical engineering","score_opus":0.015401641147576143,"score_gpt":0.20867810258718403,"score_spread":0.1932764614396079,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2611925948","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9790329,0.010887402,0.0000034134455,0.0033099381,0.0005696027,0.00007147292,0.000067259294,0.0000013855052,0.0060566654],"genre_scores_gemma":[0.9988377,0.000121824225,0.00014725202,0.0005491558,0.000118200456,1.2853047e-7,0.0000017694983,0.0000017614313,0.00022217764],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986463,0.00009591363,0.00034476945,0.00017491925,0.0003587169,0.00037935644],"domain_scores_gemma":[0.9984928,0.00029241672,0.0005226451,0.00020987178,0.00013869764,0.0003436125],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00075884804,0.00013377021,0.00033931565,0.000116882504,0.0015201243,0.00015320342,0.0007272411,0.00005293094,0.00073624565],"category_scores_gemma":[0.00021252771,0.00008085102,0.00006331908,0.00010951056,0.0021503426,0.00030193306,0.000013388836,0.00026304837,0.0000016040148],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046961326,0.0000015249908,0.983263,0.000014327686,0.00007414283,0.0001588288,0.0009280307,0.0010636859,0.0000038526655,0.00051334046,0.0021330426,0.011799252],"study_design_scores_gemma":[0.00051091396,0.00017567149,0.9807488,0.00002432252,0.000025933572,0.0005628869,0.0022413842,0.00021632695,0.00007557534,0.0021771875,0.0131268455,0.00011417328],"about_ca_topic_score_codex":0.88259006,"about_ca_topic_score_gemma":0.9992937,"teacher_disagreement_score":0.11670364,"about_ca_system_score_codex":0.0000026271493,"about_ca_system_score_gemma":0.0061204555,"threshold_uncertainty_score":0.99977976},"labels":[],"label_agreement":null},{"id":"W2613291825","doi":"10.1139/cjes-2016-0225","title":"Three-dimensional gravity modelling applied to the exploration of uranium unconformity-related basement-hosted deposits: the Contact prospect case study, Kiggavik, northeast Thelon region (Nunavut, Canada)","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Areva","keywords":"Geology; Unconformity; Drilling; Inversion (geology); Basement; Geochemistry; Mineral exploration; Structural basin; Petrophysics; Geophysics; Geomorphology; Petrology","score_opus":0.04146062426232911,"score_gpt":0.2377610683265661,"score_spread":0.196300444064237,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2613291825","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99438995,0.0001349954,0.00105668,0.0030140385,0.0004703761,0.000525232,0.00001970416,0.0000027969886,0.0003862472],"genre_scores_gemma":[0.99936426,0.0000019642405,0.00030474656,0.00020871924,0.00009392393,0.0000015690991,0.0000016298253,0.0000025138397,0.000020694704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99811506,0.00014285478,0.00045457637,0.00021707633,0.00065970916,0.00041072312],"domain_scores_gemma":[0.9982046,0.00026273046,0.0005092258,0.0002996241,0.00024582684,0.00047797553],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0015842926,0.00015711346,0.00026400722,0.00010644787,0.0024544466,0.00026117067,0.000777924,0.00003821303,0.00004659044],"category_scores_gemma":[0.0001455605,0.00007934355,0.000076302225,0.00045832386,0.0002657023,0.0004497865,0.000015287447,0.00031277223,0.000004867484],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017828481,0.00005703081,0.68039566,0.00001334017,0.00011480489,0.0012098365,0.0021320232,0.23006038,0.000029035378,0.0006776393,0.00017541507,0.08495654],"study_design_scores_gemma":[0.0004930268,0.0013219311,0.9467781,0.000060118076,0.00007462893,0.0006198136,0.002220074,0.04538016,0.00020623613,0.0023322874,0.00027290365,0.0002406741],"about_ca_topic_score_codex":0.8958036,"about_ca_topic_score_gemma":0.9984146,"teacher_disagreement_score":0.2663825,"about_ca_system_score_codex":0.000007917487,"about_ca_system_score_gemma":0.0017471691,"threshold_uncertainty_score":0.9988442},"labels":[],"label_agreement":null},{"id":"W2615985275","doi":"10.1139/cjes-2016-0158","title":"Ore characteristics of the sandstone-type Daying uranium deposit in the Ordos Basin, northwestern China","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Radioactive element chemistry and processing","field":"Chemistry","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Uranium; Geology; Uranium ore; Structural basin; Geochemistry; Electron microprobe; Mineralization (soil science); Mineralogy; Coal; Mining engineering; Geomorphology; Soil science; Metallurgy","score_opus":0.022685543744293896,"score_gpt":0.25628767885218084,"score_spread":0.23360213510788694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2615985275","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99013484,0.00020179975,0.0000046644645,0.0008183351,0.00023664795,0.000022676792,0.000010622295,8.679888e-7,0.008569542],"genre_scores_gemma":[0.9995572,0.000015260886,0.00004613728,0.000104469786,0.00017793864,3.0031737e-7,5.3948645e-7,0.000003721362,0.00009440567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990816,0.00002518639,0.00028377472,0.000105878134,0.00026574827,0.00023781875],"domain_scores_gemma":[0.99890137,0.00005073058,0.0005817556,0.00025467487,0.00008632011,0.00012514913],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00057975133,0.00009172989,0.00015269034,0.00004283657,0.0009419269,0.00031652008,0.0012699891,0.000043367847,0.00011512118],"category_scores_gemma":[0.00020017223,0.00005308615,0.00006204356,0.00014133466,0.00052992214,0.00032967512,0.00001871479,0.0002856557,5.5360937e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000078876055,0.0000066375587,0.98715204,0.00003758639,0.000009035165,0.000040122955,0.0011342871,0.000013690098,0.009594074,0.000010125224,0.000019642572,0.0019749],"study_design_scores_gemma":[0.00019322908,0.000027663664,0.9484073,0.0003402505,0.00002131594,0.00019873552,0.00076280994,0.0000546146,0.04789835,0.00005711077,0.0019418141,0.00009682228],"about_ca_topic_score_codex":0.0025970652,"about_ca_topic_score_gemma":0.020052094,"teacher_disagreement_score":0.038744725,"about_ca_system_score_codex":0.000010087077,"about_ca_system_score_gemma":0.0008559495,"threshold_uncertainty_score":0.9978294},"labels":[],"label_agreement":null},{"id":"W2617174137","doi":"10.1139/e11-020","title":"Public geoscience to reduce exploration risk: new methods to characterize the basement beneath geological cover and to address community engagement in the Cariboo-Chilcotin region of British Columbia<sup>1</sup>This article introduces a series of papers published in this Special Issue on the theme of <i>New insights in Cordilleran Intermontane geoscience: reducing exploration risk in the mountain pine beetle-affected area, British Columbia</i>. James Haggart is the Special Issue guest editor.<sup>2</sup>Geological Survey of Canada Contribution 20100476.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Golder Associates (Canada); Geological Survey of Canada","funders":"","keywords":"Mountain pine beetle; Mineral exploration; Geology; Earth science; Glacial period; Pleistocene; Environmental resource management; Archaeology; Geography; Paleontology; Geochemistry; Environmental science","score_opus":0.041656789326017796,"score_gpt":0.22952812142034779,"score_spread":0.18787133209433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2617174137","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9919684,0.0000578061,0.000034121575,0.0052214507,0.0006603039,0.001675439,0.00014406885,0.0000024402568,0.00023600194],"genre_scores_gemma":[0.9983006,0.000078963305,0.00017668547,0.00061637326,0.0006911352,0.00004596964,0.000007926353,0.0000062126114,0.0000761227],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9903755,0.00641221,0.0011319384,0.00044710492,0.0010706775,0.0005625799],"domain_scores_gemma":[0.9968133,0.0014027071,0.0007752603,0.0004805824,0.00024635062,0.00028179077],"candidate_categories":["metaresearch","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.018980335,0.00018681513,0.0005482042,0.00017594117,0.0006937268,0.00057469186,0.001691043,0.000099173616,0.0012948381],"category_scores_gemma":[0.009568492,0.00013884937,0.000055861627,0.0026335092,0.0012489022,0.0010990967,0.00019664064,0.000759917,0.0000011127481],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032334292,0.0004397994,0.72646487,0.000021308335,0.000028679171,0.00006512615,0.12030857,0.005991643,0.00093601405,0.00001870326,0.12083999,0.02456196],"study_design_scores_gemma":[0.00048162125,0.0014878109,0.97554064,0.00027131688,0.000012793535,0.00003846792,0.015764918,0.0013811759,0.00043426614,0.00009222214,0.0043287924,0.00016595986],"about_ca_topic_score_codex":0.98999757,"about_ca_topic_score_gemma":0.99840266,"teacher_disagreement_score":0.24907579,"about_ca_system_score_codex":0.00021109487,"about_ca_system_score_gemma":0.0008787578,"threshold_uncertainty_score":0.9996181},"labels":[],"label_agreement":null},{"id":"W2617761419","doi":"10.1139/cjes-2017-0061","title":"An Eocene brontothere and tillodonts (Mammalia) from British Columbia, and their paleoenvironments","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Brandon University","funders":"Natural Sciences and Engineering Research Council of Canada; Simon Fraser University; National Geographic Society","keywords":"Geology; Paleontology; Range (aeronautics); Paleosol","score_opus":0.0211796978960646,"score_gpt":0.20903282552563132,"score_spread":0.1878531276295667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2617761419","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98752487,0.007936494,0.000005088145,0.00035523184,0.00033053878,0.000039575745,0.00015151994,0.0000020894945,0.0036545696],"genre_scores_gemma":[0.99854726,0.00051332987,0.00032792537,0.00024269267,0.00009705116,8.3460144e-8,0.0000021377396,0.0000012843374,0.0002682133],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992282,0.00005542106,0.0001572108,0.00017832471,0.00011656773,0.0002642872],"domain_scores_gemma":[0.9990588,0.00004735317,0.00019010874,0.00011587666,0.000025892177,0.0005620026],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037454895,0.000070907394,0.0001727463,0.000038785845,0.0016674139,0.00092595135,0.00033515925,0.00004893102,0.0010062255],"category_scores_gemma":[0.00006868019,0.00007270485,0.000023557612,0.000027907574,0.0014726644,0.0006264974,0.0000056790495,0.0000941463,0.0000053598524],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000016329348,0.0000016794544,0.9745946,0.0000011160602,0.0000117020245,0.00003764655,0.00022403452,0.000007145133,0.000003769918,0.0000011434911,0.00024082647,0.0248747],"study_design_scores_gemma":[0.00020068049,0.00017722421,0.9920749,0.00002821429,0.0000071259506,0.00011799334,0.0006027554,0.00019974614,0.000001743763,0.0004340807,0.006062816,0.000092692266],"about_ca_topic_score_codex":0.52171034,"about_ca_topic_score_gemma":0.99885833,"teacher_disagreement_score":0.477148,"about_ca_system_score_codex":8.864831e-7,"about_ca_system_score_gemma":0.00015373009,"threshold_uncertainty_score":0.999907},"labels":[],"label_agreement":null},{"id":"W2618615128","doi":"10.1139/cjes-2016-0233","title":"A late Campanian euselachian assemblage from the Bearpaw Formation of Alberta, Canada: some notable range extensions","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Ichthyology and Marine Biology","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Geology; Assemblage (archaeology); Fauna; Benthic zone; Paleontology; Range (aeronautics); Faunal assemblage; Pelagic zone; Oceanography; Ecology; Biology","score_opus":0.015159641655891488,"score_gpt":0.20963795609881578,"score_spread":0.1944783144429243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2618615128","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.988316,0.0000977731,0.000011196166,0.005572545,0.00055412896,0.00006127522,0.000016147314,7.657375e-7,0.0053701955],"genre_scores_gemma":[0.9983819,0.00001331558,0.00017647175,0.0007763872,0.000075396296,5.373556e-7,0.0000010870797,0.0000025068941,0.0005723823],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991109,0.00007100183,0.00023239484,0.00010624241,0.00017539217,0.00030406547],"domain_scores_gemma":[0.9990343,0.0001246644,0.00032890757,0.00022088732,0.000025090143,0.0002661601],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00057831395,0.00007675583,0.00015076935,0.00003783549,0.0011575375,0.000058293517,0.00080490456,0.000049240236,0.0007512808],"category_scores_gemma":[0.00035906496,0.000048904323,0.000043776035,0.00007222207,0.0008735073,0.0006127185,0.00005771413,0.00014558437,0.00003124869],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001117055,0.000007915494,0.98984116,0.0000016572881,0.000015132756,0.00005290402,0.0011079377,0.00067443436,0.0013951394,0.00058200996,0.005012866,0.0012976854],"study_design_scores_gemma":[0.0001469879,0.000077127115,0.9768747,0.000015156388,0.000014742651,0.000035757836,0.00017430059,0.00023812971,0.0003735309,0.00056669296,0.021413539,0.00006935316],"about_ca_topic_score_codex":0.9810654,"about_ca_topic_score_gemma":0.99965084,"teacher_disagreement_score":0.01858545,"about_ca_system_score_codex":0.0000226,"about_ca_system_score_gemma":0.00093886844,"threshold_uncertainty_score":0.8902959},"labels":[],"label_agreement":null},{"id":"W2618618196","doi":"10.1139/cjes-2017-0015","title":"New <i>Saurorhynchus</i> (Actinopterygii: Saurichthyidae) material from the Early Jurassic of Alberta, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"University of Alberta","keywords":"Actinopterygii; Paleontology; Geology; Permian; Tetrapod (structure); Range (aeronautics); Canyon; Genus; Biostratigraphy; Invertebrate; Structural basin; Fish <Actinopterygii>; Ecology; Biology; Fishery; Geomorphology","score_opus":0.013999171892482808,"score_gpt":0.19454638693992787,"score_spread":0.18054721504744506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2618618196","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98088264,0.0006884664,0.000006993428,0.0039330414,0.002934696,0.00004319914,0.00015884059,0.0000010358823,0.011351102],"genre_scores_gemma":[0.9985888,0.000017975142,0.00032356937,0.00034013027,0.00044323268,6.175568e-8,0.0000058332053,0.0000011363746,0.00027926572],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99881756,0.000096435746,0.00032042604,0.00015085087,0.00022771912,0.00038698094],"domain_scores_gemma":[0.9983841,0.00033657116,0.0005102022,0.00022491925,0.00006914177,0.00047502478],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004106802,0.00010919146,0.00021902243,0.00006247741,0.001040574,0.0001331683,0.0012595901,0.000069192654,0.0030358708],"category_scores_gemma":[0.00027235795,0.00006805311,0.000060255283,0.00008812755,0.0009121329,0.00043049268,0.0000078955345,0.00016520922,0.000017488399],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020319181,8.624768e-7,0.99245816,8.0610243e-7,0.000018876835,0.000042698546,0.00013277405,0.00006936468,0.000023209117,0.000049502258,0.003113108,0.00407031],"study_design_scores_gemma":[0.00013498434,0.00014192464,0.97732246,0.000020152855,0.000016558142,0.00007864985,0.00009190504,0.000031414653,0.00013641476,0.0004960514,0.021445751,0.00008372931],"about_ca_topic_score_codex":0.994851,"about_ca_topic_score_gemma":0.99981695,"teacher_disagreement_score":0.018332643,"about_ca_system_score_codex":0.0000027542933,"about_ca_system_score_gemma":0.0060127527,"threshold_uncertainty_score":0.9996222},"labels":[],"label_agreement":null},{"id":"W2619561264","doi":"10.1139/cjes-2017-0096","title":"Best Paper Award 2016","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Metallurgy and Material Science","field":"Materials Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry","score_opus":0.03914902322321542,"score_gpt":0.26749659147573335,"score_spread":0.22834756825251792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2619561264","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96677184,0.00028649927,0.00006715606,0.0024197793,0.0045439615,0.000043374173,0.000007856005,0.0000035887338,0.025855953],"genre_scores_gemma":[0.9958428,0.000028086062,0.0016666474,0.0002757346,0.0003124732,4.905379e-7,6.761322e-8,0.0000030926974,0.0018706045],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987123,0.00004896487,0.0002711012,0.0001745741,0.00033761837,0.00045546138],"domain_scores_gemma":[0.9984637,0.000029844507,0.00039160348,0.00026999513,0.00013861895,0.00070624653],"candidate_categories":["sts","scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002091785,0.00009013392,0.00017241613,0.00012595029,0.0017708875,0.0011012367,0.0015941678,0.00004269661,0.0043080165],"category_scores_gemma":[0.0005534416,0.00006175576,0.000060020793,0.000081256854,0.0015552439,0.001757914,0.000037630638,0.00007626756,0.00056970265],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002974699,0.000038839633,0.035830557,0.000025272604,0.000014580695,0.0006649931,0.0009868926,0.00032118207,0.9233099,0.023969254,0.0062838066,0.008524936],"study_design_scores_gemma":[0.00065666076,0.0009331263,0.15684018,0.0004123992,0.00003792325,0.00063408865,0.0004931442,0.00005470105,0.14082578,0.009766872,0.68868876,0.0006563999],"about_ca_topic_score_codex":0.009834929,"about_ca_topic_score_gemma":0.062669456,"teacher_disagreement_score":0.7824842,"about_ca_system_score_codex":0.0000052698056,"about_ca_system_score_gemma":0.0020195355,"threshold_uncertainty_score":0.9999357},"labels":[],"label_agreement":null},{"id":"W2621692749","doi":"10.1139/cjes-2016-0224","title":"Evaluating the groundwater resource potential of the Dundas buried bedrock valley, southwestern Ontario: an integrated geological and hydrogeological case study","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Baosteel-Australia Joint Research and Development Centre; McMaster University","keywords":"Bedrock; Geology; Aquifer; Groundwater; Hydrogeology; Borehole; Resource (disambiguation); Hydrology (agriculture); Sediment; Geochemistry; Geomorphology; Paleontology; Geotechnical engineering","score_opus":0.057825565870326626,"score_gpt":0.28732514449141766,"score_spread":0.22949957862109105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2621692749","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99847806,0.000026075582,0.000069195856,0.00079035654,0.00016607692,0.00016923169,0.0000014044795,0.0000019657243,0.00029762526],"genre_scores_gemma":[0.9987882,4.2125794e-7,0.00013581236,0.00011261577,0.00003857751,0.0000021386834,1.4362635e-7,0.0000025795878,0.0009195247],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99843717,0.00029840457,0.00032410043,0.00021548329,0.0004411181,0.00028374454],"domain_scores_gemma":[0.99907863,0.000054622185,0.00034448516,0.00025864295,0.000051568924,0.00021205077],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0019224606,0.0001196877,0.00018339764,0.000042273263,0.002678735,0.0003694676,0.0008595366,0.000042389,0.0003265902],"category_scores_gemma":[0.00014430296,0.000054326214,0.00006290937,0.000090729816,0.002408436,0.00037926694,0.00021576413,0.000235539,0.0000036193198],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010800934,0.000031198822,0.98805434,5.710751e-7,0.000016416989,0.00033082702,0.0071963626,0.0005979725,0.00012336958,0.000009332,0.000008600172,0.003620185],"study_design_scores_gemma":[0.00032349955,0.0012335606,0.983329,0.000010006416,0.000042760013,0.0016290064,0.01180228,0.00046971018,0.000026104226,0.00012297533,0.000927109,0.00008401981],"about_ca_topic_score_codex":0.3231539,"about_ca_topic_score_gemma":0.9142098,"teacher_disagreement_score":0.59105587,"about_ca_system_score_codex":0.000020534077,"about_ca_system_score_gemma":0.00019640212,"threshold_uncertainty_score":0.9986196},"labels":[],"label_agreement":null},{"id":"W2624992773","doi":"10.1139/cjes-2017-0004","title":"Sedimentary exhalative origin for magnetite deposits of the New Jersey Highlands","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Ore genesis; Banded iron formation; Magnetite; Skarn; Quartz; Gneiss; Genetic model; Mineral; Sedimentary rock; Fluid inclusions; Metamorphic rock","score_opus":0.025067005102125044,"score_gpt":0.22201375585829927,"score_spread":0.19694675075617424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2624992773","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9880417,0.0006962352,0.000027571215,0.0060742022,0.0004213838,0.000062927975,0.000034066303,9.97116e-7,0.00464094],"genre_scores_gemma":[0.9977436,0.000012334972,0.0012974465,0.00028108893,0.00014939111,7.974021e-8,0.0000015532946,5.829896e-7,0.00051390275],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991907,0.000024284192,0.00021103109,0.00011069108,0.0002125243,0.000250805],"domain_scores_gemma":[0.9989612,0.000096057185,0.00031144483,0.00012296563,0.00008983125,0.00041849524],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035312743,0.00007298647,0.00016071244,0.00007640928,0.0006574913,0.00010984425,0.00079570385,0.00003173079,0.0017610898],"category_scores_gemma":[0.00020348748,0.00003792423,0.00013846929,0.00015306007,0.0005900933,0.00024256276,0.000008548064,0.00008781564,0.000006854764],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000069507314,0.0000016880717,0.99568784,0.0000025664863,0.000013533693,0.000004941834,0.00006426805,0.0005390677,0.000058056008,0.000098702825,0.0005425934,0.0029797636],"study_design_scores_gemma":[0.00018000601,0.00024572902,0.9829982,0.000028286808,0.000031982567,0.000017222183,0.00007589211,0.00041183832,0.0013371265,0.007168363,0.007438731,0.00006664787],"about_ca_topic_score_codex":0.04703381,"about_ca_topic_score_gemma":0.57020897,"teacher_disagreement_score":0.5231751,"about_ca_system_score_codex":8.61389e-7,"about_ca_system_score_gemma":0.00059342437,"threshold_uncertainty_score":0.9991514},"labels":[],"label_agreement":null},{"id":"W2626344581","doi":"10.1139/cjes-2016-0015","title":"The effects of shale composition and pore structure on gas adsorption potential in highly mature marine shales, Lower Paleozoic, central Yangtze, China","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Sorption; Oil shale; Methane; Organic matter; Geology; Clay minerals; Adsorption; Mineralogy; Illite; Ordovician; Porosity; Environmental chemistry; Geochemistry; Chemistry; Organic chemistry","score_opus":0.004055068391500252,"score_gpt":0.1895614199051829,"score_spread":0.18550635151368267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2626344581","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979502,0.00042502914,0.00002336652,0.00060698617,0.00054037286,0.00005272868,0.0000067820674,0.0000026057962,0.00039194713],"genre_scores_gemma":[0.99959993,0.00020077458,0.000054964188,0.000017091046,0.00009627842,2.8257696e-7,0.0000028477727,0.000003947501,0.000023888117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99934566,0.000027307196,0.00017289395,0.00007412285,0.00018366206,0.00019633272],"domain_scores_gemma":[0.9995287,0.00001777653,0.00011616452,0.0001080729,0.000032335596,0.00019694866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014452258,0.000078079596,0.00012814096,0.00018435623,0.00026958456,0.00018627381,0.00023943846,0.000050671126,0.000025123309],"category_scores_gemma":[0.0000406261,0.000051447823,0.000047406473,0.000110982815,0.00021050678,0.00024142937,0.000008708462,0.00018026763,4.1605642e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020240524,0.00007154461,0.53317654,0.0004361262,0.00032119767,0.001417995,0.0032202902,0.3660637,0.06751183,0.002753161,0.0011750181,0.02365018],"study_design_scores_gemma":[0.0003969533,0.00016700335,0.9721489,0.00016918509,0.000021639791,0.00004974072,0.000070596216,0.023546597,0.0025678219,0.0005151574,0.00023887191,0.00010755001],"about_ca_topic_score_codex":0.0007581981,"about_ca_topic_score_gemma":0.07520644,"teacher_disagreement_score":0.43897235,"about_ca_system_score_codex":0.000008774614,"about_ca_system_score_gemma":0.00008782221,"threshold_uncertainty_score":0.9416686},"labels":[],"label_agreement":null},{"id":"W2628586923","doi":"10.1139/cjes-2017-0024","title":"Mineralogy, geochronology, and genesis of the Andrew Lake uranium deposit, Thelon Basin, Nunavut, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Manitoba","funders":"Natural Resources Canada","keywords":"Uraninite; Geology; Illite; Geochronology; Geochemistry; Uranium ore; Mineralization (soil science); Uranium; Structural basin; Zircon; Authigenic; Carbonate; Mineralogy; Sedimentary rock; Paleontology; Clay minerals; Chemistry","score_opus":0.012538961918845428,"score_gpt":0.18425165987026204,"score_spread":0.1717126979514166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2628586923","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.988601,0.002156846,0.0000021337414,0.0058219475,0.00033241685,0.000035427296,0.00006339014,8.627645e-7,0.0029859552],"genre_scores_gemma":[0.99907947,0.00006268814,0.0002125685,0.00047363908,0.00007211855,6.9606266e-8,0.0000012192874,7.364258e-7,0.00009749295],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990125,0.00006075482,0.00024780855,0.0001455009,0.0002155456,0.00031792012],"domain_scores_gemma":[0.9989402,0.00009240577,0.00030739902,0.00017022934,0.00010099718,0.00038872406],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038301363,0.00009534782,0.00022817748,0.00006810746,0.00085937703,0.00010732132,0.0007980102,0.000049003473,0.0014146318],"category_scores_gemma":[0.00026774182,0.000051065606,0.00007873421,0.0001492729,0.001398736,0.00017155592,0.000017776785,0.00013198744,0.0000020951295],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000031512911,0.0000014128442,0.99698603,0.000003956329,0.000014522336,0.000025069294,0.000028835993,0.00021422382,0.0000710809,0.000027587786,0.00026697872,0.0023571504],"study_design_scores_gemma":[0.000095855954,0.000081604856,0.9946834,0.000019538527,0.00002875546,0.00013126271,0.000097914635,0.00030088625,0.0005172556,0.000880175,0.003089365,0.00007400079],"about_ca_topic_score_codex":0.95602506,"about_ca_topic_score_gemma":0.99977005,"teacher_disagreement_score":0.04374498,"about_ca_system_score_codex":0.0000013874909,"about_ca_system_score_gemma":0.0011130386,"threshold_uncertainty_score":0.9994982},"labels":[],"label_agreement":null},{"id":"W2680866755","doi":"10.1139/cjes-2017-0002","title":"Sedimentation in isolated glaciomarine embayments during glacio-isostatically induced relative sea level fall (northern Champlain Sea basin)","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université Laval; Center for Northern Studies; Geological Survey of Canada","funders":"","keywords":"Geology; Oceanography; Deglaciation; Sedimentation; Sediment; Post-glacial rebound; Bioturbation; Structural basin; Sea level; Sea ice; Geomorphology; Paleontology; Holocene","score_opus":0.05094481585664067,"score_gpt":0.2780676515666917,"score_spread":0.22712283571005104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2680866755","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923914,0.00015554538,0.000021093494,0.0023890866,0.0003909485,0.0001399149,0.000059419264,0.0000034093132,0.004449151],"genre_scores_gemma":[0.99922746,0.000016968064,0.00034056275,0.00011505819,0.000043247048,6.690424e-7,0.000013753077,0.0000026858181,0.00023960872],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980143,0.00029839855,0.00041607168,0.00024735395,0.00035115515,0.0006727254],"domain_scores_gemma":[0.9985316,0.00021280242,0.00033240675,0.00017169147,0.00016233303,0.0005891589],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017558767,0.00014814784,0.00026199425,0.0005481796,0.00118668,0.00020970109,0.00064391614,0.00012962591,0.00079403596],"category_scores_gemma":[0.0005745341,0.000123871,0.000057967754,0.00029261372,0.00080634793,0.001106043,0.000016114598,0.0004712304,0.00011819402],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011666094,0.0000068114605,0.9978135,0.0000070291003,0.000021547861,0.0006662913,0.0006117415,0.00023852279,0.000009822846,0.000022454919,0.000003289688,0.0004822762],"study_design_scores_gemma":[0.000653943,0.0003813539,0.99595326,0.000054580025,0.000008224997,0.00025295,0.0002919391,0.0015975374,0.0000439785,0.00057910813,0.000048073252,0.00013505974],"about_ca_topic_score_codex":0.04626856,"about_ca_topic_score_gemma":0.9604252,"teacher_disagreement_score":0.9141566,"about_ca_system_score_codex":0.000003089731,"about_ca_system_score_gemma":0.0013831438,"threshold_uncertainty_score":0.9600824},"labels":[],"label_agreement":null},{"id":"W2729948314","doi":"10.1139/cjes-2018-0268","title":"Rock and age relationships within the Talkeetna forearc accretionary complex in the Nelchina area, southern Alaska","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Geology; Accretionary wedge; Subduction; Forearc; Pillow lava; Paleontology; Terrane; Island arc; Dike; Petrography; Geochemistry; Tectonics; Volcanic rock; Volcano","score_opus":0.039930134849923166,"score_gpt":0.1995089465993803,"score_spread":0.15957881174945712,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2729948314","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9884241,0.0005461402,0.000005092161,0.005310932,0.00006654683,0.000072015515,0.00001804559,0.0000014504598,0.0055556605],"genre_scores_gemma":[0.99896866,0.000006989685,0.0001490523,0.0006530528,0.0000417074,1.704543e-7,0.0000067894503,6.4387615e-7,0.00017291996],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99896157,0.00017375343,0.00023177692,0.00012524486,0.00027221712,0.0002354453],"domain_scores_gemma":[0.9991659,0.00037664935,0.000127668,0.00008837168,0.000036618836,0.00020480255],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014834658,0.00007776434,0.0001308361,0.00012010537,0.000464345,0.000157911,0.00048682795,0.000035057987,0.0027710604],"category_scores_gemma":[0.00018677437,0.00003437934,0.000057915182,0.0005219275,0.00036959103,0.00017677383,0.0000066644025,0.00031264906,0.00007462356],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000035986957,0.0000017727823,0.9916835,0.0000011636167,0.000004239896,0.000022755363,0.0009519678,0.0068160794,0.0000069283883,0.0001800621,0.00007136159,0.00025659718],"study_design_scores_gemma":[0.000075813005,0.00009913487,0.9677419,0.0000124958515,0.000007962472,0.00010199497,0.0038682935,0.0067973337,0.0000018559858,0.020549402,0.0006844133,0.000059391765],"about_ca_topic_score_codex":0.013757953,"about_ca_topic_score_gemma":0.4767414,"teacher_disagreement_score":0.46298346,"about_ca_system_score_codex":8.3668266e-7,"about_ca_system_score_gemma":0.00019198206,"threshold_uncertainty_score":0.9981405},"labels":[],"label_agreement":null},{"id":"W2734815613","doi":"10.1139/cjes-2017-0100","title":"A middle Holocene steppe bison and paleoenvironments from the Versleuce Meadows, Whitehorse, Yukon, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature; University of Alberta; Simon Fraser University; Yukon Department of Tourism and Culture","funders":"University of California, Irvine","keywords":"Holocene; Beringia; Macrofossil; Pleistocene; Steppe; Ecology; Bison bison; Population; Geology; Geography; Paleontology; Biology","score_opus":0.039500482650639934,"score_gpt":0.217566391244296,"score_spread":0.17806590859365606,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2734815613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98585045,0.0038465208,0.0000013462044,0.0057810694,0.00066080317,0.00006158295,0.00007046792,0.0000010706226,0.0037266654],"genre_scores_gemma":[0.9989102,0.00016169937,0.00014053746,0.0005378032,0.000088431945,1.5053092e-7,0.000003474853,0.0000012847424,0.00015643885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986631,0.00013367728,0.00020121448,0.00018850452,0.00032694417,0.00048651604],"domain_scores_gemma":[0.9986452,0.00026315017,0.00022461926,0.00022992893,0.00004970834,0.000587397],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008522508,0.00010476837,0.0001760619,0.000077416495,0.002105707,0.0003027811,0.0010115145,0.00006744658,0.0010428135],"category_scores_gemma":[0.00035578688,0.00006663481,0.000030381689,0.000090144305,0.0017176114,0.00042185507,0.000015978263,0.0002940761,0.000028161126],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008547061,0.0000011169697,0.9982674,0.00000146856,0.000015031801,0.0001549373,0.00014771552,0.000119939774,6.4513e-7,0.000011447634,0.00041878707,0.0008529254],"study_design_scores_gemma":[0.00019537909,0.00009782539,0.9937733,0.000026237589,0.000011689945,0.00012381625,0.0005341544,0.00022967567,0.000014979751,0.00026323172,0.004647855,0.0000818912],"about_ca_topic_score_codex":0.807134,"about_ca_topic_score_gemma":0.99860334,"teacher_disagreement_score":0.1914694,"about_ca_system_score_codex":9.429314e-7,"about_ca_system_score_gemma":0.0018085344,"threshold_uncertainty_score":0.99987036},"labels":[],"label_agreement":null},{"id":"W2734948953","doi":"10.1139/cjes-2017-0053","title":"Landscape antiquity and Cenozoic drainage development of southern Yukon, through restoration modeling of the Tintina Fault","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Fault (geology); Cenozoic; Tectonics; Paleontology; Neogene; Drainage basin; Cretaceous; Drainage; River terraces; Sinistral and dextral; Geomorphology; Fluvial; Structural basin","score_opus":0.056356068534920756,"score_gpt":0.2342039993208428,"score_spread":0.17784793078592204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2734948953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943771,0.000496159,0.00021110527,0.00069324876,0.00016781352,0.00004185398,0.000008594515,7.143208e-7,0.0040034414],"genre_scores_gemma":[0.9985584,0.0000235547,0.0013400094,0.000025375093,0.000033003424,4.989758e-8,5.464652e-7,5.113654e-7,0.000018546227],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99927837,0.00003254924,0.00023947828,0.00007707528,0.00022539872,0.00014712328],"domain_scores_gemma":[0.9993413,0.000021960226,0.00035248217,0.00007725057,0.00012211336,0.00008487361],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007504012,0.000051180505,0.00011784552,0.00003622215,0.001018607,0.00007942441,0.00029387022,0.000026271488,0.00006902961],"category_scores_gemma":[0.00022136117,0.000028494136,0.00002799241,0.00008284683,0.00037903563,0.00027964736,0.000012242764,0.00006443199,0.0000021405617],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000073705623,0.0000029842818,0.97447395,0.000012028222,0.000008095481,0.0000029545201,0.0039022872,0.015118116,0.000050717717,0.000119052514,0.000022866207,0.0062795877],"study_design_scores_gemma":[0.00012614873,0.00013245293,0.97495365,0.000069094334,0.000008082306,0.000010369088,0.0036361853,0.018082159,0.00015721328,0.0019843113,0.00076825736,0.00007205235],"about_ca_topic_score_codex":0.007891695,"about_ca_topic_score_gemma":0.334227,"teacher_disagreement_score":0.32633528,"about_ca_system_score_codex":6.984196e-7,"about_ca_system_score_gemma":0.00036403254,"threshold_uncertainty_score":0.99871486},"labels":[],"label_agreement":null},{"id":"W2735300118","doi":"10.1139/cjes-2017-0034","title":"A new species of troodontid theropod (Dinosauria: Maniraptora) from the Horseshoe Canyon Formation (Maastrichtian) of Alberta, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; University of Toronto","funders":"","keywords":"Canyon; Horseshoe (symbol); Autapomorphy; Geology; Paleontology; Cretaceous; Horseshoe crab; Taxon; Biology; Geomorphology; Phylogenetic tree","score_opus":0.020409230480078606,"score_gpt":0.19726490700771293,"score_spread":0.17685567652763431,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2735300118","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98288184,0.0022042973,0.000054941313,0.0033940456,0.0011436032,0.000062973566,0.0001240187,6.953157e-7,0.010133571],"genre_scores_gemma":[0.9988601,0.000046396628,0.0004522066,0.00010946834,0.00019066899,5.5291327e-8,0.0000062692643,8.274572e-7,0.00033397367],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989386,0.00008766957,0.00035276855,0.00010287716,0.0002378133,0.00028023083],"domain_scores_gemma":[0.99853635,0.00021310923,0.00069556426,0.00018315506,0.00009914916,0.00027268424],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004040498,0.00009183771,0.00022486788,0.000096056276,0.0006243486,0.00004654561,0.00093952595,0.000059158836,0.0014673319],"category_scores_gemma":[0.000270951,0.000057311197,0.00006503418,0.00012358377,0.0007488737,0.00046362253,0.0000060300376,0.00013186572,0.0000048499496],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017575392,0.0000013882909,0.99430794,0.0000020105583,0.000022734614,0.0000121519515,0.00034624254,0.00020744636,0.000036153593,0.0001822096,0.002577008,0.0022871313],"study_design_scores_gemma":[0.00016710049,0.00018504105,0.9858268,0.00002929222,0.000020092033,0.000042764514,0.00080034457,0.00022533663,0.0001494691,0.00039196742,0.012097991,0.00006380723],"about_ca_topic_score_codex":0.9834737,"about_ca_topic_score_gemma":0.99988383,"teacher_disagreement_score":0.016410137,"about_ca_system_score_codex":0.0000042203474,"about_ca_system_score_gemma":0.0041871546,"threshold_uncertainty_score":0.99944544},"labels":[],"label_agreement":null},{"id":"W2737550034","doi":"10.1139/cjes-2016-0167","title":"Sources and accumulation of sediment and particulate organic carbon in a subarctic fjard estuary: <sup>210</sup>Pb, <sup>137</sup>Cs, and δ<sup>13</sup>C records from Lake Melville, Labrador","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada; University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Excellence Research Chairs, Government of Canada; ArcticNet; University of Manitoba","keywords":"Geology; Sediment; Tributary; Bay; Total organic carbon; Hydrology (agriculture); Mars Exploration Program; Particulates; Oceanography; Estuary; Deposition (geology); TRACER; Geomorphology; Environmental chemistry","score_opus":0.03381864144157677,"score_gpt":0.25664395746942686,"score_spread":0.2228253160278501,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2737550034","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936039,0.0035677939,0.000002322629,0.0020291086,0.0001094937,0.00019776686,0.000051808805,0.0000051092616,0.00043273557],"genre_scores_gemma":[0.9989048,0.00047546084,0.0003200636,0.000117361706,0.0000996299,9.208836e-7,0.000010612121,0.0000052804107,0.00006587443],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99752456,0.00034464573,0.00055890146,0.00044601227,0.00040059056,0.00072531373],"domain_scores_gemma":[0.9979384,0.0005240647,0.0003617166,0.00023973417,0.00012942923,0.0008066619],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019002393,0.00024013022,0.0005377245,0.00051165314,0.00086940575,0.00032090786,0.0004768865,0.00020345881,0.0007194448],"category_scores_gemma":[0.00059665873,0.00019373471,0.000052203213,0.00031191317,0.0020121592,0.0007137945,0.00004353343,0.00044474035,0.000009802562],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005024634,0.0000084335015,0.9892118,0.000025686637,0.000038997798,0.00014612409,0.0028248015,0.0060743443,0.000008433555,0.000011633959,0.000014812891,0.0015846954],"study_design_scores_gemma":[0.00078496255,0.00045171694,0.92315507,0.00012023776,0.000045521425,0.00023793495,0.0018187582,0.072141625,0.00004872641,0.00073586387,0.00026515874,0.0001944434],"about_ca_topic_score_codex":0.049327876,"about_ca_topic_score_gemma":0.66175866,"teacher_disagreement_score":0.61243075,"about_ca_system_score_codex":0.0000024925666,"about_ca_system_score_gemma":0.0007530852,"threshold_uncertainty_score":0.95700276},"labels":[],"label_agreement":null},{"id":"W2737715837","doi":"10.1139/cjes-2017-0052","title":"Employing contact metamorphism to assess the conditions of pluton emplacement and timing of recrystallization in southwestern Kellys Mountain, Cape Breton Island, Nova Scotia","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick; Acadia University","funders":"Acadia University","keywords":"Geology; Metamorphism; Metamorphic rock; Geochemistry; Sillimanite; Andalusite; Pluton; Diorite; Gneiss; Zircon; Metamorphic facies; Monazite; Recrystallization (geology); Isograd; Facies; Geomorphology; Petrology; Biotite; Paleontology","score_opus":0.06349295624067085,"score_gpt":0.2676940110513306,"score_spread":0.20420105481065975,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2737715837","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978535,0.00023534129,0.00009011849,0.0008784202,0.000102497455,0.000075010066,0.00005306089,6.6896877e-7,0.0007113568],"genre_scores_gemma":[0.99955624,0.000013394602,0.00026662217,0.00010723307,0.000026421949,1.1309259e-7,0.00000469849,8.21804e-7,0.000024436305],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99900824,0.00006111579,0.0003544241,0.00012585019,0.00023551998,0.00021485945],"domain_scores_gemma":[0.9990249,0.0001339602,0.00037799843,0.000109011446,0.00012537578,0.00022870202],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008963581,0.0000784983,0.00022765635,0.00021413881,0.000294199,0.00012455927,0.00038497263,0.00003191671,0.0016123417],"category_scores_gemma":[0.00025628693,0.000047802976,0.00005256205,0.00023052041,0.00038528556,0.0002651286,0.000012088041,0.000097368466,0.0000040810423],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006470705,0.000003188001,0.9940646,0.000005845221,0.000014911586,0.000008720624,0.00033308862,0.004313869,0.0008306984,0.000054421158,0.000012492687,0.00035164956],"study_design_scores_gemma":[0.00014283287,0.00019966101,0.99564,0.000079459656,0.000031184085,0.000016750555,0.0006075966,0.0015420574,0.0006829913,0.0008711498,0.00011669814,0.000069619404],"about_ca_topic_score_codex":0.11733344,"about_ca_topic_score_gemma":0.864512,"teacher_disagreement_score":0.7471786,"about_ca_system_score_codex":0.0000020418129,"about_ca_system_score_gemma":0.0002396029,"threshold_uncertainty_score":0.9993003},"labels":[],"label_agreement":null},{"id":"W2742202778","doi":"10.1139/cjes-2017-0023","title":"Hirnantian (Ordovician) through Wenlock (Silurian) conodont biostratigraphy, bioevents, and integration with graptolite biozones, Cape Phillips Formation slope facies, Cornwallis Island, Canadian Arctic Islands","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; Government of Nunavut; Schlumberger (Canada); Nunavut Research Institute","funders":"","keywords":"Conodont; Geology; Paleontology; Biozone; Ordovician; Biostratigraphy; Facies; Chemostratigraphy; Devonian; Trilobite; Isotopes of carbon","score_opus":0.02354904309561742,"score_gpt":0.220166122676906,"score_spread":0.19661707958128857,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2742202778","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9538003,0.009623187,0.00027075963,0.004521364,0.0010148154,0.00032316742,0.0006540929,0.000009716047,0.029782584],"genre_scores_gemma":[0.9980489,0.00045716562,0.0011010044,0.00021472972,0.00011752452,6.87571e-7,0.000025353467,0.0000020192492,0.000032640484],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99808663,0.000100926336,0.0004715059,0.00029828126,0.00031966955,0.00072296744],"domain_scores_gemma":[0.99789405,0.00006244783,0.000598629,0.00025277,0.00022011853,0.00097201264],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00069779786,0.0002647633,0.00034708623,0.0006471929,0.003004515,0.0009768056,0.0007042039,0.00013155479,0.0002889186],"category_scores_gemma":[0.00010812163,0.00018802805,0.000090618094,0.0003491552,0.0017493891,0.002512634,0.0000019383333,0.00031624624,0.000007928743],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033425553,0.000004967319,0.96937686,0.000014108224,0.000044678956,0.00012269669,0.0011081557,0.000020583433,0.000015949132,0.00078972254,0.00011871687,0.028350132],"study_design_scores_gemma":[0.0004897313,0.0009888567,0.9894484,0.00018283499,0.000040981657,0.00056923804,0.0010335866,0.00037054977,0.00006887534,0.0014449246,0.005081043,0.0002809485],"about_ca_topic_score_codex":0.6751473,"about_ca_topic_score_gemma":0.99936956,"teacher_disagreement_score":0.3242223,"about_ca_system_score_codex":0.0000059513063,"about_ca_system_score_gemma":0.001941006,"threshold_uncertainty_score":0.99829346},"labels":[],"label_agreement":null},{"id":"W2742325356","doi":"10.1139/cjes-2017-0031","title":"Troodontids (Theropoda) from the Dinosaur Park Formation, Alberta, with a description of a unique new taxon: implications for deinonychosaur diversity in North America","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Paleontology; Taxon; Theropoda; Crania; Biology; Anatomy","score_opus":0.04339006236083708,"score_gpt":0.2233700916510632,"score_spread":0.1799800292902261,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2742325356","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99137104,0.00042342168,0.0018496503,0.0051454417,0.00014703856,0.0001320912,0.00011851836,0.0000010832752,0.00081171474],"genre_scores_gemma":[0.99783665,0.000044925397,0.0017732185,0.0002230634,0.000064035594,5.9660437e-7,0.000015664538,6.3760945e-7,0.000041185485],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993111,0.000066633795,0.00020209777,0.00010894543,0.00008211122,0.00022913872],"domain_scores_gemma":[0.9989695,0.00020449229,0.0003856034,0.00014654109,0.00009179485,0.00020207267],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027150929,0.000069642076,0.00014730323,0.00009948178,0.0012111325,0.000051394996,0.0006695916,0.00004251237,0.000103532846],"category_scores_gemma":[0.00016258551,0.000043276046,0.00004621654,0.00016643164,0.0008213239,0.0006684449,0.00000704254,0.00009804278,0.0000032386808],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032216252,0.0000029091696,0.9955792,0.0000013177291,0.00001035592,0.0000016621136,0.00055719836,0.0005477126,0.000003831633,0.00007316627,0.00033443602,0.0028559878],"study_design_scores_gemma":[0.00023987214,0.00029669653,0.99368316,0.000020283986,0.000014165844,0.000024618254,0.0002689245,0.00037676888,0.0000038740895,0.0013446221,0.003668864,0.00005817803],"about_ca_topic_score_codex":0.2737263,"about_ca_topic_score_gemma":0.9930366,"teacher_disagreement_score":0.7193103,"about_ca_system_score_codex":0.0000029985072,"about_ca_system_score_gemma":0.00081733405,"threshold_uncertainty_score":0.9315174},"labels":[],"label_agreement":null},{"id":"W2742727699","doi":"10.1139/cjes-2017-0103","title":"Major geological events in the late Guadalupian and carbon–strontium isotope responses in the Yangtze platform, South China","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Chengdu University; National Natural Science Foundation of China","keywords":"Geology; Sedimentary rock; Large igneous province; Geochemistry; Earth science; Basalt; Isotopes of strontium; Isotopes of carbon; Volcano; Carbonate; Paleontology; Strontium; Total organic carbon; Magmatism; Tectonics; Ecology","score_opus":0.030993038242047407,"score_gpt":0.2394548565982794,"score_spread":0.20846181835623198,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2742727699","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97655284,0.00225919,6.5000916e-7,0.0037169638,0.00022186628,0.00010466657,0.000012557178,9.48292e-7,0.017130325],"genre_scores_gemma":[0.9996506,0.000025559844,0.00006533355,0.00016479268,0.000053737236,3.9448472e-7,2.847107e-7,3.4093455e-7,0.000038955808],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998699,0.0002540666,0.00024527265,0.0001307322,0.0002519471,0.00041895921],"domain_scores_gemma":[0.999269,0.00016370404,0.00020465418,0.00016872725,0.000015840898,0.00017808915],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0029356447,0.000102282494,0.00016629559,0.00022157782,0.0009565954,0.0002140834,0.0011590004,0.00006905501,0.000057322533],"category_scores_gemma":[0.00030362603,0.000050684495,0.000048015587,0.00016715306,0.0011178496,0.0004040975,0.0000022615068,0.00035793844,0.000001479395],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025002038,0.0000025803486,0.9952119,0.0000012201903,0.0000033520505,0.00017535996,0.0025274563,0.000036898666,7.929732e-7,0.000089581845,0.0000074261734,0.001918439],"study_design_scores_gemma":[0.00023836821,0.00025526987,0.9953926,0.0000246152,0.000005577884,0.00017501505,0.0017773317,0.0002950829,0.000001219788,0.0016171698,0.00014561969,0.00007208341],"about_ca_topic_score_codex":0.039955933,"about_ca_topic_score_gemma":0.8195035,"teacher_disagreement_score":0.7795476,"about_ca_system_score_codex":7.4493687e-7,"about_ca_system_score_gemma":0.00045893173,"threshold_uncertainty_score":0.9664371},"labels":[],"label_agreement":null},{"id":"W2743294795","doi":"10.1139/cjes-2017-0101","title":"Systematics and biogeography of some early Cambrian (Series 2) bradoriids (Arthropoda) from Laurentia (Greenland)","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Laurentia; Paleontology; Geology; Series (stratigraphy); Trilobite; Baltica; Ordovician; Systematics; Biogeography; Ecological succession; Ecology; Taxonomy (biology); Biology","score_opus":0.018401978016508048,"score_gpt":0.2158402375646629,"score_spread":0.19743825954815483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2743294795","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9794412,0.014706562,0.000011293906,0.0003809155,0.0008812605,0.00006183828,0.00018832026,0.0000026192522,0.0043259463],"genre_scores_gemma":[0.99836504,0.00014472094,0.0013179774,0.000018633213,0.0001345941,8.6310706e-8,0.0000012731658,7.1357897e-7,0.000016962607],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99876785,0.00007935424,0.00039208418,0.00015997999,0.00027784705,0.00032285758],"domain_scores_gemma":[0.99849695,0.000091204776,0.00059109466,0.00020408662,0.00009048366,0.0005261651],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006436056,0.00012587172,0.00033936306,0.00033401485,0.0010879047,0.00035950248,0.0006346109,0.00008706789,0.00015252849],"category_scores_gemma":[0.00011677317,0.000094117895,0.00010950221,0.00013612799,0.0026034438,0.001225043,0.0000021754493,0.0001430773,0.0000026608589],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000092669725,0.0000020125253,0.9947514,0.000015547552,0.000043206903,0.00005323019,0.0002919016,0.0000034273992,0.000015762902,0.00058041484,0.000024113051,0.004209749],"study_design_scores_gemma":[0.00019371667,0.0004284596,0.99512875,0.00015422668,0.000032616546,0.00007130245,0.00038562837,0.000045354795,0.00007898592,0.0032045906,0.00016513615,0.00011123038],"about_ca_topic_score_codex":0.059654687,"about_ca_topic_score_gemma":0.6776831,"teacher_disagreement_score":0.6180284,"about_ca_system_score_codex":3.2185858e-7,"about_ca_system_score_gemma":0.00049380143,"threshold_uncertainty_score":0.9592497},"labels":[],"label_agreement":null},{"id":"W2744554591","doi":"10.1139/cjes-2016-0192","title":"Analysis of the charging process of the lacustrine tight oil reservoir in the Triassic Chang 6 Member in the southwest Ordos Basin, China","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Specialized Research Fund for the Doctoral Program of Higher Education of China; National Natural Science Foundation of China","keywords":"Tight oil; Geology; Quartz; Feldspar; Fluid inclusions; Oil shale; Petrography; Structural basin; Calcite; Tight gas; Homogenization (climate); Geochemistry; Shale oil; Green River Formation; Mineralogy; Petrology; Paleontology; Hydraulic fracturing","score_opus":0.030586635225361168,"score_gpt":0.2606186625762384,"score_spread":0.23003202735087722,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2744554591","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887703,0.00022762024,0.0000088353845,0.0078936005,0.00015289421,0.00006760775,0.000010394538,0.0000012814687,0.0028674412],"genre_scores_gemma":[0.9997042,0.000039136776,0.0000064377064,0.00009710048,0.000057546204,0.000002941304,3.6533524e-7,0.0000041044705,0.000088174325],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99846023,0.00021990864,0.00042977865,0.00009837216,0.00053956633,0.00025211409],"domain_scores_gemma":[0.99893606,0.000084627936,0.00036356255,0.00045048643,0.00008381477,0.00008143604],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026644012,0.000101477446,0.0002834056,0.00055156363,0.00045390267,0.0001661212,0.0021033746,0.000041052735,0.00006277832],"category_scores_gemma":[0.0004073325,0.000040694402,0.00021772401,0.0027323088,0.00042279944,0.00029163554,0.000021719532,0.00031907565,5.740209e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005753554,0.000020085019,0.5239039,0.00003522984,0.0001835927,0.000017852533,0.020304129,0.4547993,0.00011084358,0.0001369874,0.000090193265,0.00039213296],"study_design_scores_gemma":[0.00033933652,0.000025455547,0.9079202,0.00018531585,0.00021079666,0.000009722257,0.0077864467,0.08184197,0.00053608924,0.000091584596,0.00094329857,0.00010982946],"about_ca_topic_score_codex":0.0069543035,"about_ca_topic_score_gemma":0.4916794,"teacher_disagreement_score":0.48472512,"about_ca_system_score_codex":0.000011570252,"about_ca_system_score_gemma":0.00043505462,"threshold_uncertainty_score":0.99965847},"labels":[],"label_agreement":null},{"id":"W2747739868","doi":"10.1139/cjes-2017-0074","title":"Spatial and temporal distributions of the late Mesozoic volcanic successions and their controlling effects on the Changling fault depression of the Songliao Basin, northeast China","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Geology; Partial melting; Volcano; Geochemistry; Volcanic rock; Fault (geology); Fractional crystallization (geology); Magma; Crust; Structural basin; Seismology; Paleontology","score_opus":0.011046485188372734,"score_gpt":0.19394606103329842,"score_spread":0.1828995758449257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2747739868","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99387634,0.00068971986,0.000019547113,0.0047944575,0.00019991472,0.00008465315,0.000077499666,7.990445e-7,0.00025705178],"genre_scores_gemma":[0.9998042,0.000025276546,0.000012188577,0.000081457845,0.0000550606,2.1486456e-7,8.194892e-7,7.003545e-7,0.000020063379],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99915415,0.00012626305,0.00020616513,0.00010460162,0.0001988926,0.00020992459],"domain_scores_gemma":[0.9988952,0.0002629885,0.00040631506,0.00016466437,0.000071744325,0.0001990833],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00065469334,0.00008958758,0.00019431482,0.000043535103,0.0017375055,0.0001029002,0.0005928176,0.000036038527,0.00012582386],"category_scores_gemma":[0.000674727,0.000030782816,0.0001061809,0.00016732966,0.0010830914,0.00011761948,0.000028155222,0.00019145662,4.1341252e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000061498426,0.000002626867,0.9956859,0.0000042007237,0.000010512391,0.0000012322289,0.00012929241,0.00024109618,0.00013904384,0.000038796054,0.000004562865,0.0037366075],"study_design_scores_gemma":[0.00012476635,0.00007982866,0.98944473,0.00014826343,0.000024326098,0.000009033553,0.00013225255,0.0057492736,0.001893696,0.0022570714,0.0000918625,0.000044912373],"about_ca_topic_score_codex":0.037045732,"about_ca_topic_score_gemma":0.38848773,"teacher_disagreement_score":0.35144198,"about_ca_system_score_codex":8.2161614e-7,"about_ca_system_score_gemma":0.000182033,"threshold_uncertainty_score":0.9995621},"labels":[],"label_agreement":null},{"id":"W2748958359","doi":"10.1139/cjes-2017-0069","title":"Geochemistry of volcanic and plutonic rocks from the Nahlin ophiolite with implications for a Permo–Triassic arc in the Cache Creek terrane, northwestern British Columbia","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Ophiolite; Geology; Terrane; Geochemistry; Volcanic rock; Basalt; Ultramafic rock; Peridotite; Island arc; Petrology; Subduction; Volcano; Paleontology; Tectonics","score_opus":0.024400062041605605,"score_gpt":0.20912567042576136,"score_spread":0.18472560838415575,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2748958359","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99428874,0.0013073158,0.0000104865185,0.003498568,0.000031433203,0.000101020305,0.0003240228,9.147058e-7,0.00043747385],"genre_scores_gemma":[0.9993366,0.000053749223,0.00014383122,0.00031700972,0.000073770454,0.0000014772055,0.000012344946,9.4338924e-7,0.000060274237],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990787,0.000042242176,0.00025662055,0.00017720101,0.00016425161,0.00028097557],"domain_scores_gemma":[0.9988545,0.00033897132,0.0002873238,0.00019414375,0.00009863869,0.00022643112],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000597035,0.00006748043,0.00019166144,0.00002496726,0.00088428817,0.0007449639,0.00091261,0.00004082184,0.00056066073],"category_scores_gemma":[0.00022026317,0.000044809836,0.00007453642,0.00016788409,0.00095401326,0.00017214281,0.000009170268,0.00016300024,7.64449e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004199122,0.000003932861,0.9964025,0.000003104181,0.000012426903,0.000010173082,0.00016878682,0.00010647355,0.0000305506,0.0000013344284,0.00013083678,0.003125661],"study_design_scores_gemma":[0.0002185659,0.00013489688,0.9938647,0.000049050224,0.000033504806,0.00010386972,0.0005217533,0.0004687641,0.000008315623,0.0038514994,0.0006737824,0.000071282746],"about_ca_topic_score_codex":0.7661119,"about_ca_topic_score_gemma":0.9984873,"teacher_disagreement_score":0.23237537,"about_ca_system_score_codex":0.0000012905434,"about_ca_system_score_gemma":0.0005189611,"threshold_uncertainty_score":0.71837044},"labels":[],"label_agreement":null},{"id":"W2750075651","doi":"10.1139/cjes-2016-0187","title":"Neoglacial history of Robson Glacier, British Columbia","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Brock University","keywords":"Glacier; Geology; Subfossil; Physical geography; Holocene; Rock glacier; Glacier mass balance; Glacial period; Geomorphology; Archaeology; Paleontology; Geography","score_opus":0.0327532437126104,"score_gpt":0.2295014378889396,"score_spread":0.1967481941763292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2750075651","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95983046,0.003416962,0.0000025755667,0.00031765003,0.0018568458,0.00004322684,0.000016925867,0.0000016358571,0.034513738],"genre_scores_gemma":[0.9959242,0.00006215913,0.00031996198,0.00009337209,0.00010590605,7.611576e-8,0.0000013187345,0.0000010566453,0.0034919968],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998744,0.00009320034,0.0002707435,0.00013905775,0.00025407175,0.0004988953],"domain_scores_gemma":[0.99862796,0.00009295509,0.0003589229,0.00015960813,0.00016138588,0.00059915625],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001483329,0.000056061373,0.00022501804,0.00013553658,0.0008600076,0.00026636288,0.0009713133,0.00008993662,0.0075663286],"category_scores_gemma":[0.0006043991,0.00006684848,0.00008071825,0.00008332817,0.0031043147,0.00048645207,0.000007497665,0.00023327455,0.00004046607],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004335905,0.0000023748457,0.99579173,0.000005492689,0.000007525366,0.00023275363,0.00011266229,0.00004961192,0.0000021574076,0.000012455494,0.0017042831,0.0020745955],"study_design_scores_gemma":[0.000173125,0.00024222641,0.978915,0.00003298396,0.0000068862123,0.0005605881,0.000081495025,0.0001365114,0.000003877278,0.0005014515,0.019274382,0.00007149448],"about_ca_topic_score_codex":0.3252389,"about_ca_topic_score_gemma":0.9937908,"teacher_disagreement_score":0.66855186,"about_ca_system_score_codex":0.0000013963672,"about_ca_system_score_gemma":0.0043366686,"threshold_uncertainty_score":0.99960864},"labels":[],"label_agreement":null},{"id":"W2750164606","doi":"10.1139/cjes-2016-0162","title":"Petrography and phase equilibria modeling of mid-pressure aluminous gneisses derived from hydrothermally altered protoliths, Grenville Province, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Sillimanite; Geology; Protolith; Gneiss; Geochemistry; Metamorphic rock; Granulite; Cordierite; Felsic; Metamorphism; Petrography; Migmatite; Partial melting; Andalusite; Anatexis; Plagioclase; Petrology; Biotite; Mafic; Quartz; Facies; Crust; Geomorphology; Paleontology","score_opus":0.020187270534041356,"score_gpt":0.21363631313205345,"score_spread":0.1934490425980121,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2750164606","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99494153,0.0026808102,0.000011553438,0.0005962308,0.00016601726,0.00011765726,0.00016540533,0.0000018200208,0.0013189786],"genre_scores_gemma":[0.9989863,0.000024885847,0.0007831913,0.00007438823,0.00009425521,4.0494442e-7,0.000004898323,0.0000015165697,0.000030177198],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99864906,0.00005135053,0.00035864217,0.0002265222,0.00032454767,0.0003898687],"domain_scores_gemma":[0.99856794,0.000057330755,0.00038806547,0.00017576005,0.000115713476,0.00069517584],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029395448,0.00013533075,0.00032296215,0.00013560014,0.00057532574,0.00020001801,0.00073246955,0.00004455193,0.0014272064],"category_scores_gemma":[0.00019530096,0.000092593364,0.0000873928,0.00013047086,0.00075109303,0.00030642023,0.00001536667,0.00013618948,0.0000012371296],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003221424,0.000010088039,0.9905316,0.000015339101,0.0000647164,0.00009662586,0.00007209699,0.004233496,0.0013771018,0.0000072271923,0.000026951615,0.0035325235],"study_design_scores_gemma":[0.00110969,0.00077893364,0.81326205,0.00015720572,0.00015335753,0.00009666785,0.00040007333,0.17517167,0.0028333946,0.0037330743,0.0018869529,0.00041694596],"about_ca_topic_score_codex":0.93496716,"about_ca_topic_score_gemma":0.99255526,"teacher_disagreement_score":0.1772696,"about_ca_system_score_codex":0.000001070584,"about_ca_system_score_gemma":0.001703122,"threshold_uncertainty_score":0.9994856},"labels":[],"label_agreement":null},{"id":"W2750453590","doi":"10.1139/cjes-2017-0133","title":"Fractured latest Devonian granites of the West Moose River pluton along the Cobequid Shear Zone, Nova Scotia: implications for regional mineralization","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University; Bedford Institute of Oceanography; Geological Survey of Canada; Natural Resources Canada; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Pluton; Mineralization (soil science); Biotite; Hydrothermal circulation; Shear zone; Tourmaline; Quartz; Tectonics; Paleontology","score_opus":0.032800702925036715,"score_gpt":0.2351308924361303,"score_spread":0.2023301895110936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2750453590","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9747135,0.0007062455,0.00008807769,0.023410536,0.00021420004,0.00010857328,0.000093139824,0.0000015464794,0.0006641936],"genre_scores_gemma":[0.9986274,0.000017254219,0.0006355335,0.00050284894,0.00011589672,2.439099e-7,0.000008632273,0.0000011112568,0.00009107373],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990973,0.000040373252,0.00027095235,0.00013305679,0.00019906965,0.0002592366],"domain_scores_gemma":[0.998706,0.00019564274,0.00041355318,0.00020092307,0.00025187162,0.00023203973],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000497912,0.000087176835,0.0001518338,0.00008285221,0.001199131,0.00017171548,0.0009619698,0.00004710923,0.001109085],"category_scores_gemma":[0.00044703408,0.000041772837,0.0001429775,0.0002797981,0.0014884869,0.00027801652,0.00001020027,0.00011547552,0.000011202965],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000044678773,0.00000410804,0.9953095,0.0000028997736,0.000012913149,0.00000102778,0.00014638116,0.0029195573,0.000119112665,0.00042607938,0.00042585543,0.0006281181],"study_design_scores_gemma":[0.00010556083,0.00007878797,0.98879516,0.000025179968,0.000029408237,0.0000225832,0.000043034957,0.00096522784,0.00013964069,0.004325638,0.0054061306,0.000063622174],"about_ca_topic_score_codex":0.10439009,"about_ca_topic_score_gemma":0.84207535,"teacher_disagreement_score":0.73768526,"about_ca_system_score_codex":0.0000014482976,"about_ca_system_score_gemma":0.0004253933,"threshold_uncertainty_score":0.999804},"labels":[],"label_agreement":null},{"id":"W2754304616","doi":"10.1139/cjes-2017-0025","title":"A multi-century estimate of suspended sediment yield from Lillooet Lake, southern Coast Mountains, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Northern British Columbia; Simon Fraser University","funders":"","keywords":"Sediment; Sedimentary budget; Watershed; Geology; Hydrology (agriculture); Glacier; Drainage basin; Varve; Sedimentation; Physical geography; Oceanography; Sediment transport; Geomorphology; Geography","score_opus":0.03840973530073489,"score_gpt":0.23187329753784622,"score_spread":0.19346356223711134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2754304616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942162,0.0017892182,0.000018776824,0.0011036112,0.0012135385,0.00006888591,0.0008510269,0.000001971841,0.00073677656],"genre_scores_gemma":[0.9972836,0.000064163876,0.0021738329,0.0002326632,0.000112443326,1.3796577e-7,0.00000814469,0.0000019885867,0.00012303711],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987857,0.00002202777,0.0003267684,0.00014667303,0.00036572755,0.0003531443],"domain_scores_gemma":[0.99862325,0.000114373404,0.0004622773,0.0001842173,0.00014197273,0.0004739032],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00036482414,0.00011159633,0.00022815327,0.000050490115,0.0010582512,0.00018101156,0.0006767231,0.000032367632,0.0023499802],"category_scores_gemma":[0.00030082063,0.000084154584,0.00005991058,0.000118554664,0.0004271909,0.000252178,0.0000127136855,0.00012193221,0.000008022381],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005503703,0.0000042881293,0.99418396,0.000002896674,0.000026772936,0.000060948365,0.0004716668,0.0022904286,0.000010488598,0.000010547792,0.00083508715,0.0020974034],"study_design_scores_gemma":[0.0002525933,0.00009357008,0.9752118,0.00006261285,0.000018086237,0.000009880891,0.0031473532,0.002152398,0.000028160577,0.000053499178,0.018858155,0.000111891706],"about_ca_topic_score_codex":0.98304415,"about_ca_topic_score_gemma":0.999926,"teacher_disagreement_score":0.01897217,"about_ca_system_score_codex":0.0000045171296,"about_ca_system_score_gemma":0.0029339558,"threshold_uncertainty_score":0.998562},"labels":[],"label_agreement":null},{"id":"W2754899066","doi":"10.1139/cjes-2017-0006","title":"Ice-marginal sedimentation and processes of diamicton deposition in large proglacial lakes, Lake Erie, Ontario, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Waterloo; Laurentian University","funders":"","keywords":"Geology; Glacier; Geomorphology; Debris; Debris flow; Shelf ice; Moraine; Glacial period; Ice stream; Glacial lake; Sedimentation; Sediment; Oceanography; Sea ice; Cryosphere","score_opus":0.016688680248363928,"score_gpt":0.21308986631043983,"score_spread":0.1964011860620759,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2754899066","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965387,0.00066863035,0.000009062642,0.00051880657,0.0003490005,0.00007109686,0.00010260194,7.036266e-7,0.0017413847],"genre_scores_gemma":[0.99936604,0.00004034982,0.00038013174,0.00007890375,0.000053668246,2.8527108e-7,0.000008574886,8.473796e-7,0.00007119641],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992227,0.000015580548,0.00022182043,0.000099161494,0.00021568213,0.00022504211],"domain_scores_gemma":[0.99933845,0.000043074186,0.00027064446,0.000054804637,0.00011228989,0.00018075267],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031980753,0.00006481951,0.00013029792,0.00006119375,0.00065071194,0.00013114112,0.0001931343,0.000021259746,0.0005136008],"category_scores_gemma":[0.00013121437,0.000053303855,0.000014863894,0.00015197661,0.00021862608,0.0005194672,0.0000043568625,0.00008207791,3.7808763e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006891622,0.0000028037007,0.99754006,0.000011206704,0.000004423322,0.000024246232,0.0005360918,0.0002401181,0.0000024733197,0.000021588108,0.00009848281,0.0015115918],"study_design_scores_gemma":[0.00020804348,0.00012579618,0.98801804,0.00005342843,0.0000072186967,0.00001916578,0.0006722589,0.00019197934,0.000029791623,0.000058772897,0.010553804,0.0000617046],"about_ca_topic_score_codex":0.96405464,"about_ca_topic_score_gemma":0.9999985,"teacher_disagreement_score":0.035943873,"about_ca_system_score_codex":0.0000064553974,"about_ca_system_score_gemma":0.0044005783,"threshold_uncertainty_score":0.78064364},"labels":[],"label_agreement":null},{"id":"W2756949389","doi":"10.1139/cjes-2017-0016","title":"Borehole geophysical log signatures and stratigraphic assessment in a glacial basin, southern Ontario","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Baosteel-Australia Joint Research and Development Centre","keywords":"Geology; Borehole; Glacial period; Provenance; Context (archaeology); Suite; Geomorphology; Geophysics; Paleontology; Archaeology","score_opus":0.024026338113745896,"score_gpt":0.2569086154603192,"score_spread":0.2328822773465733,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2756949389","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9899039,0.0004098881,0.0000016629731,0.0014077206,0.0002580803,0.00005357004,0.00001183957,0.0000010935172,0.007952209],"genre_scores_gemma":[0.9993122,0.000010817667,0.0003413705,0.00011595116,0.00006556062,1.5190388e-7,0.000001374487,7.899961e-7,0.00015176991],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99890304,0.00010698154,0.00019232255,0.00016436959,0.00021195253,0.00042132055],"domain_scores_gemma":[0.9991612,0.00010441733,0.0001511823,0.00011265208,0.00005177493,0.000418807],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010178407,0.00008882345,0.00019692582,0.00028046456,0.0009055999,0.00027457994,0.00050895597,0.00009052602,0.0008896581],"category_scores_gemma":[0.00009997497,0.00006638969,0.00004398774,0.00010463366,0.0016437325,0.0003582712,0.000006957892,0.0005370155,0.00001478461],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000884581,0.0000036331744,0.9983764,0.000002223509,0.0000061823594,0.0002540163,0.00052646827,0.000108545006,0.0000021354158,0.00021572552,0.000015641976,0.00048013],"study_design_scores_gemma":[0.00021858733,0.00026627732,0.99568063,0.00002191665,0.00000454358,0.00009358433,0.00035854572,0.00026445522,0.0000034169698,0.0026354077,0.00037608654,0.00007656978],"about_ca_topic_score_codex":0.33199948,"about_ca_topic_score_gemma":0.9981029,"teacher_disagreement_score":0.6661034,"about_ca_system_score_codex":6.7479226e-7,"about_ca_system_score_gemma":0.0027262,"threshold_uncertainty_score":0.9741132},"labels":[],"label_agreement":null},{"id":"W2758058656","doi":"10.1139/cjes-2016-0198","title":"Quaternary geology of part of the McLeod Lake map area (NTS 093J), central British Columbia: lithostratigraphy, glacial history, and chronology","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of British Columbia; Golder Associates (Canada); University of the Fraser Valley; Simon Fraser University","funders":"","keywords":"Geology; Deglaciation; Outwash plain; Meltwater; Glacial period; Glacier; Geomorphology; Ice sheet; Paleontology; Physical geography","score_opus":0.02520398002224215,"score_gpt":0.21519364490762183,"score_spread":0.1899896648853797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2758058656","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911795,0.0029643816,0.000001012694,0.001156771,0.0016857407,0.00007678187,0.000055937406,0.000001211293,0.0028786082],"genre_scores_gemma":[0.9992972,0.000121156016,0.00009801646,0.00007764884,0.00007375179,1.9716808e-7,0.000001789351,0.0000010879003,0.00032916327],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99858314,0.0001928701,0.0003484086,0.00017396917,0.00019148037,0.00051013153],"domain_scores_gemma":[0.9987645,0.000114008166,0.00046642422,0.00019075845,0.00011892461,0.0003453795],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00075288006,0.00007530782,0.0002963764,0.00011149672,0.0006965386,0.000081448234,0.0008930967,0.00013567471,0.003033159],"category_scores_gemma":[0.0002390562,0.00007066524,0.00008565008,0.000076080774,0.006845729,0.00025218117,0.000017919516,0.00027150425,0.0000036509211],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010094958,0.000004358798,0.99831694,0.000013416801,0.000018187566,0.00011669588,0.00014905556,0.00001830444,0.0000030651497,0.00002320654,0.00074778486,0.00057889795],"study_design_scores_gemma":[0.0002410342,0.00037926383,0.9921806,0.000049435694,0.0000124838325,0.00071384123,0.00009719546,0.00006978674,0.000011535599,0.000736115,0.0054416587,0.00006705044],"about_ca_topic_score_codex":0.13228258,"about_ca_topic_score_gemma":0.99441636,"teacher_disagreement_score":0.8621338,"about_ca_system_score_codex":7.544102e-7,"about_ca_system_score_gemma":0.0018071623,"threshold_uncertainty_score":0.9978782},"labels":[],"label_agreement":null},{"id":"W2758252753","doi":"10.1139/cjes-2016-0112","title":"Using a multiple variogram approach to improve the accuracy of subsurface geological models","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Modeling and Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Guelph","funders":"","keywords":"Geology; Hydrogeology; Bedrock; Context (archaeology); Groundwater; Variogram; Geologic map; Earth science; Kriging; Geomorphology; Paleontology; Computer science; Geotechnical engineering","score_opus":0.1161453974687744,"score_gpt":0.26786244894113403,"score_spread":0.15171705147235964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2758252753","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9847091,0.00047553476,0.009882228,0.0008205783,0.00024161798,0.00008731822,0.000024945904,0.0000023886282,0.0037562903],"genre_scores_gemma":[0.98222715,0.000014229273,0.01748417,0.0001520876,0.000079603175,1.3747311e-7,7.173516e-7,0.0000010226698,0.000040860603],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99867874,0.00008151926,0.0003205462,0.00019537123,0.0003165324,0.0004072938],"domain_scores_gemma":[0.9984687,0.00018291168,0.00039760087,0.00025046567,0.00017441482,0.00052592263],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001533188,0.00010265027,0.0002447589,0.00015913056,0.0012014934,0.0003232982,0.001310434,0.000057996072,0.00013938877],"category_scores_gemma":[0.0010759373,0.000054139728,0.000139898,0.0002682653,0.0007037301,0.0004170967,0.000017858178,0.00018681306,0.000007973275],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000047001345,0.000004829465,0.33070105,0.0000018505847,0.00001043488,0.00000579822,0.000147324,0.6654313,0.000017306855,0.00007968933,0.000010766403,0.003584927],"study_design_scores_gemma":[0.00009552189,0.00018379024,0.21582182,0.000016531665,0.000023371344,0.000033643282,0.00033031552,0.7812598,0.000025179066,0.0018151788,0.00030140718,0.00009348425],"about_ca_topic_score_codex":0.107238784,"about_ca_topic_score_gemma":0.15834181,"teacher_disagreement_score":0.115828425,"about_ca_system_score_codex":0.0000011230303,"about_ca_system_score_gemma":0.0005597235,"threshold_uncertainty_score":0.92410374},"labels":[],"label_agreement":null},{"id":"W2758433351","doi":"10.1139/cjes-2017-0130","title":"Scimitar cat (<i>Homotherium serum</i> Cope) from southwestern Alberta, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Alberta Historical Resources Foundation","keywords":"Accelerator mass spectrometry; Radiocarbon dating; Geology; Context (archaeology); Archaeology; Dentition; Range (aeronautics); Physical geography; Geography; Paleontology","score_opus":0.024273623018119007,"score_gpt":0.21001189472656656,"score_spread":0.18573827170844756,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2758433351","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9503251,0.0015682307,0.0000046854548,0.0046275915,0.0023728302,0.000046795576,0.000186242,0.0000022379738,0.040866304],"genre_scores_gemma":[0.99726117,0.000033905886,0.00033777693,0.0011291354,0.00024497721,8.743056e-8,0.000002378299,0.0000018945788,0.0009886777],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986803,0.000062051455,0.00027641878,0.0001914479,0.0003090102,0.00048077633],"domain_scores_gemma":[0.9984221,0.00016909193,0.0003511607,0.0002188711,0.00011564102,0.0007231593],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00040406652,0.00013439888,0.00024032679,0.00010134349,0.0019593316,0.00031589827,0.0009810603,0.000051717176,0.0021974803],"category_scores_gemma":[0.00025715647,0.00010189338,0.00006058159,0.00009153614,0.0010240749,0.00048353255,0.0000075941534,0.00013606976,0.00007933861],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000035687558,9.172035e-7,0.99668264,0.0000014045726,0.000019664742,0.00009717694,0.0003569372,0.00017937097,0.0000017402612,0.000017548335,0.0014856016,0.0011534347],"study_design_scores_gemma":[0.00017350906,0.0000746364,0.9589356,0.000029786888,0.000013701387,0.00006141677,0.00071812596,0.00022422678,0.000012935049,0.00014483523,0.039479993,0.00013119938],"about_ca_topic_score_codex":0.9952352,"about_ca_topic_score_gemma":0.9999965,"teacher_disagreement_score":0.046936084,"about_ca_system_score_codex":0.0000045747506,"about_ca_system_score_gemma":0.004703141,"threshold_uncertainty_score":0.99934},"labels":[],"label_agreement":null},{"id":"W2759263710","doi":"10.1139/cjes-2017-0106","title":"Soft-sediment deformation structures induced by rapid sedimentation in Early Cretaceous turbidites, Lingshan Island, eastern China","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China; National Science Foundation","keywords":"Geology; Paleocurrent; Turbidite; Clastic rock; Sedimentary rock; Geomorphology; Cretaceous; Sedimentary structures; Sediment; Petrology; Paleontology; Structural basin; Sedimentary depositional environment","score_opus":0.02186968929927371,"score_gpt":0.2299827117616401,"score_spread":0.20811302246236638,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2759263710","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953308,0.0010457917,0.000049776136,0.00066812255,0.00051393715,0.00008561981,0.000039007682,0.000002996632,0.0022639623],"genre_scores_gemma":[0.9994187,0.00003313529,0.00027529022,0.00013605156,0.000085417785,2.745475e-7,0.000015852873,0.0000012228037,0.000034068766],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988713,0.000044317745,0.00034527646,0.000117679716,0.00030081815,0.00032056373],"domain_scores_gemma":[0.9990492,0.000036523033,0.00042026426,0.00009598689,0.000076410375,0.0003216183],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00066091673,0.00010638192,0.0001462101,0.00025799245,0.0008230073,0.000682846,0.00050716486,0.00006354991,0.0011792019],"category_scores_gemma":[0.00016476148,0.000074488555,0.00003902477,0.00016449732,0.00016073114,0.0015674033,0.000005755143,0.00018115867,0.000033683482],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012055163,0.0000037015602,0.9653116,0.000009681278,0.0000065027634,0.000012177691,0.0014026699,0.0019506181,0.00004279556,0.000026144933,0.00012776502,0.03109431],"study_design_scores_gemma":[0.0002685213,0.0004518605,0.991803,0.000038867427,0.0000055883743,0.000037320016,0.00029889212,0.0029015306,0.00041640666,0.0017457607,0.001912055,0.000120220684],"about_ca_topic_score_codex":0.02907997,"about_ca_topic_score_gemma":0.19946548,"teacher_disagreement_score":0.17038551,"about_ca_system_score_codex":0.0000031145776,"about_ca_system_score_gemma":0.00041957412,"threshold_uncertainty_score":0.99973387},"labels":[],"label_agreement":null},{"id":"W2760432947","doi":"10.1139/cjes-2017-0145","title":"Upper Ordovician conodont biostratigraphy and revised lithostratigraphy and geological map, Akpatok Island, Ungava Bay, Nunavut","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Nunavut; Nunavut Research Institute","funders":"Natural Resources Canada; Universidad Nacional de Córdoba","keywords":"Conodont; Geology; Biostratigraphy; Paleontology; Lithostratigraphy; Bay; Ordovician; Range (aeronautics); Outcrop; Trilobite; Sedimentary rock; Oceanography","score_opus":0.02834940756845808,"score_gpt":0.2198918479522866,"score_spread":0.19154244038382853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2760432947","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9825231,0.006219392,0.000016769967,0.006257782,0.0003086355,0.000100356585,0.000037553727,0.0000036385297,0.0045327903],"genre_scores_gemma":[0.9977399,0.00069036987,0.0009970807,0.00041992657,0.00011487564,2.630369e-7,0.000002473436,0.000001020639,0.00003407568],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988343,0.00006859339,0.0002886606,0.00022807192,0.00018902359,0.00039132783],"domain_scores_gemma":[0.9988029,0.000087942084,0.00026924416,0.00011668556,0.00008672027,0.0006364914],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0007414753,0.000139813,0.0002524184,0.0001607729,0.0018191175,0.0006760477,0.00033371977,0.00007751027,0.0006144441],"category_scores_gemma":[0.00018990817,0.000088354085,0.000064252985,0.00012383919,0.001680604,0.00057831913,0.000010527603,0.00017408871,0.000011585621],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008461729,0.0000020664245,0.9945037,0.0000053506024,0.000010663039,0.000044757533,0.00014125147,0.000024439609,0.0000032469686,0.00031545424,0.00012821954,0.0048124385],"study_design_scores_gemma":[0.00019667186,0.0006672395,0.9857711,0.00004022786,0.000012769071,0.00007141605,0.0005299392,0.00028464265,0.0000064032,0.0027014252,0.009586933,0.00013119774],"about_ca_topic_score_codex":0.01364139,"about_ca_topic_score_gemma":0.71070945,"teacher_disagreement_score":0.69706804,"about_ca_system_score_codex":5.510056e-7,"about_ca_system_score_gemma":0.00020025985,"threshold_uncertainty_score":0.99948037},"labels":[],"label_agreement":null},{"id":"W2761387547","doi":"10.1139/cjes-2017-0092","title":"Provenance of the Early Triassic in the southwestern Sichuan Basin, Upper Yangtze, and its implications for tectonic evolution","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Provenance; Large igneous province; Craton; Clastic rock; Sedimentary rock; Permian; Paleontology; Geochemistry; Precambrian; Structural basin; Paleozoic; Basalt; Mesozoic; Early Triassic; Gondwana; Tectonics; Magmatism","score_opus":0.028057894660485607,"score_gpt":0.2256925448464574,"score_spread":0.1976346501859718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2761387547","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896229,0.0008234094,0.000010366126,0.008478655,0.0000797816,0.000117352894,0.00004584029,5.4902154e-7,0.0008211508],"genre_scores_gemma":[0.9996913,0.000008464001,0.00007613165,0.00013521449,0.000041030667,7.947379e-7,4.748745e-7,4.558883e-7,0.00004614487],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993298,0.00004626923,0.00019450574,0.00010349527,0.0001201309,0.00020581696],"domain_scores_gemma":[0.9992771,0.00013038002,0.00026310756,0.00012755743,0.00008546331,0.00011640394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007271461,0.000054323296,0.00011838085,0.000070965674,0.0006257082,0.00012396357,0.00068705616,0.000027986074,0.00007136548],"category_scores_gemma":[0.00044840857,0.000024813355,0.0000786433,0.00021011925,0.0004635192,0.00022563577,0.000005059709,0.00009473535,0.0000019636907],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003193813,0.0000023579403,0.9975642,0.0000025627867,0.0000031230618,4.350821e-7,0.00012587273,0.000088201785,0.0000737766,0.00061299425,0.000008988544,0.0015143121],"study_design_scores_gemma":[0.00011437916,0.00010951771,0.98614544,0.000021647029,0.000012864909,0.000011775488,0.00012830702,0.00035437674,0.000074213356,0.012677935,0.00031152583,0.00003802015],"about_ca_topic_score_codex":0.014049399,"about_ca_topic_score_gemma":0.32176363,"teacher_disagreement_score":0.30771422,"about_ca_system_score_codex":0.0000010372676,"about_ca_system_score_gemma":0.00030219086,"threshold_uncertainty_score":0.99251616},"labels":[],"label_agreement":null},{"id":"W2762072572","doi":"10.1139/cjes-2017-0140","title":"U–Pb baddeleyite crystallization age for a Corson diabase intrusion: possible Midcontinent Rift magmatism in eastern South Dakota","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"South Dakota School of Mines and Technology","keywords":"Geology; Craton; Baddeleyite; Rift; Geochemistry; Laurentia; Sill; Proterozoic; Terrane; Magmatism; Precambrian; Geochronology; Basement; Paleontology; Paleozoic; Tectonics; Zircon; Archaeology","score_opus":0.027386298966022248,"score_gpt":0.22300538373547976,"score_spread":0.19561908476945752,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2762072572","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99434173,0.00044279822,0.00046907165,0.0017476985,0.00029615025,0.0001068696,0.000059966642,0.0000026987495,0.0025330242],"genre_scores_gemma":[0.99684167,0.000015531934,0.0024493227,0.00022698702,0.00013561315,5.051889e-7,0.00001343953,0.0000014046223,0.0003155317],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986896,0.000044483353,0.00036623757,0.0002087222,0.00025995434,0.000431008],"domain_scores_gemma":[0.99872094,0.00007932434,0.00037194288,0.00014511512,0.000112846195,0.00056980766],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008046559,0.00011751013,0.0002515529,0.00026477347,0.0006307941,0.00051035587,0.00063934154,0.000056914138,0.0026530894],"category_scores_gemma":[0.00051852554,0.000080750826,0.00011209245,0.00023177125,0.00042479602,0.00052852044,0.000012101519,0.0001325813,0.000028152826],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012874343,0.0000052884684,0.99314183,0.000008652264,0.000006718278,0.000095362,0.00025208862,0.0018975352,0.00009593082,0.000055206172,0.00005944177,0.00436907],"study_design_scores_gemma":[0.00038540622,0.00024972344,0.9760131,0.00009735014,0.000018903733,0.000022049142,0.00025951286,0.014743736,0.00019291803,0.005589697,0.0022679772,0.00015962847],"about_ca_topic_score_codex":0.027656432,"about_ca_topic_score_gemma":0.6412296,"teacher_disagreement_score":0.6135732,"about_ca_system_score_codex":0.0000017996972,"about_ca_system_score_gemma":0.00031906052,"threshold_uncertainty_score":0.99825865},"labels":[],"label_agreement":null},{"id":"W2763108616","doi":"10.1139/cjes-2017-0036","title":"Spatially overlapping episodes of deformation, metamorphism, and magmatism in the southern Omineca Belt, southeastern British Columbia","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Metamorphism; Geology; Cretaceous; Metamorphic rock; Greenschist; Magmatism; Geochemistry; Metamorphic facies; Staurolite; Paleontology; Kyanite; Petrology; Facies; Tectonics","score_opus":0.015992245488647156,"score_gpt":0.18835213188776767,"score_spread":0.1723598863991205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2763108616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99619496,0.00079283456,0.000015217891,0.0010056843,0.00006695969,0.000045966884,0.000054609365,8.721133e-7,0.0018228801],"genre_scores_gemma":[0.9993065,0.000025301637,0.00040507712,0.00014681932,0.000042908243,1.3353119e-7,0.0000022374782,6.343999e-7,0.0000704128],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990044,0.00007039355,0.00033109842,0.000103395876,0.0002546902,0.00023601965],"domain_scores_gemma":[0.99915636,0.00009379997,0.00036481718,0.000104191364,0.0000785951,0.00020226822],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011794963,0.000058296704,0.00020318232,0.00007877106,0.0005781376,0.00066657166,0.0006015298,0.000033217133,0.0015014806],"category_scores_gemma":[0.0003148577,0.000044735654,0.000064512205,0.0001464722,0.00076386,0.00038194118,0.000008770957,0.00011558246,0.0000074658424],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011583561,0.000002155497,0.99069893,0.000005177214,0.000006649934,0.00002402088,0.00049825135,0.00022345324,0.000011075873,0.000010694221,0.000013807631,0.008504613],"study_design_scores_gemma":[0.00011588217,0.000079141,0.99031186,0.00005316005,0.000015184801,0.000106556174,0.0008752017,0.0014769022,0.00000451035,0.0067354995,0.00016288874,0.00006320727],"about_ca_topic_score_codex":0.68069965,"about_ca_topic_score_gemma":0.9944436,"teacher_disagreement_score":0.31374395,"about_ca_system_score_codex":4.3660484e-7,"about_ca_system_score_gemma":0.00018185635,"threshold_uncertainty_score":0.9994113},"labels":[],"label_agreement":null},{"id":"W2765840185","doi":"10.1139/cjes-2017-0059","title":"Spines of the stem chondrichthyan <i>Doliodus latispinosus</i> (Whiteaves) comb. nov. from the Lower Devonian of eastern Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick; Hôpital du Sacré-Cœur de Montréal","funders":"","keywords":"Devonian; SPINE (molecular biology); Fish fin; Paleontology; Geology; Biology; Peninsula; Anatomy; Holotype; Taxonomy (biology); Zoology; Fish <Actinopterygii>; Ecology; Fishery","score_opus":0.021623498640433884,"score_gpt":0.2025161150538894,"score_spread":0.1808926164134555,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2765840185","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9868451,0.002403873,0.000004661623,0.003763454,0.0025492988,0.00006427972,0.0002532604,8.024722e-7,0.0041153217],"genre_scores_gemma":[0.99917924,0.000023911345,0.000077738776,0.0003376355,0.00014362407,8.609626e-8,0.0000015537532,0.0000011117462,0.00023511032],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987509,0.00013333076,0.0003655398,0.00013668419,0.00028471247,0.00032880605],"domain_scores_gemma":[0.9984751,0.00017725451,0.000676404,0.0002821951,0.00013689464,0.0002521788],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005014202,0.00010718545,0.00023965762,0.000059642407,0.000979691,0.000050690287,0.0015463507,0.00006351756,0.00043206807],"category_scores_gemma":[0.00016941896,0.00005628929,0.00008165007,0.00017072793,0.0019947274,0.00024430276,0.000015087451,0.00018870748,0.000005080225],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009813391,0.000002726462,0.99700177,0.0000022170755,0.000020293292,0.000019321127,0.00011679538,0.00031716665,0.000015999078,0.00004855272,0.0005576154,0.0018877102],"study_design_scores_gemma":[0.00014552557,0.00014770236,0.99060583,0.000058538986,0.000014822894,0.000068017005,0.00026014665,0.00029635144,0.00006706214,0.00015764647,0.008108667,0.000069698435],"about_ca_topic_score_codex":0.85872513,"about_ca_topic_score_gemma":0.99881154,"teacher_disagreement_score":0.14008641,"about_ca_system_score_codex":0.000002784976,"about_ca_system_score_gemma":0.0033406839,"threshold_uncertainty_score":0.75350904},"labels":[],"label_agreement":null},{"id":"W2766783616","doi":"10.1139/cjes-2017-0019","title":"Competence and lithostratigraphy of host rocks govern kimberlite pipe morphology","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Stornoway Diamond (Canada); University of British Columbia","funders":"","keywords":"Kimberlite; Diatreme; Geology; Petrology; Impact crater; Sedimentary rock; Lithology; Country rock; Breccia; Geochemistry","score_opus":0.016565241016225304,"score_gpt":0.20270781135172855,"score_spread":0.18614257033550324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2766783616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98871547,0.0016547478,0.000019103576,0.0014979065,0.00014536553,0.000024008146,0.00003940857,0.0000012215601,0.007902776],"genre_scores_gemma":[0.99870193,0.000084870495,0.00094396353,0.00016244348,0.000051946747,4.0838213e-8,9.775996e-7,4.9618325e-7,0.000053328367],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990444,0.00003729066,0.00026597633,0.00015311198,0.00021037883,0.00028882126],"domain_scores_gemma":[0.9987503,0.00009776682,0.00036542251,0.00013688508,0.000112783935,0.0005367865],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046992736,0.00008694363,0.00024835652,0.00013023715,0.0005192459,0.00015697851,0.0006264695,0.00004643215,0.0017499677],"category_scores_gemma":[0.0002800534,0.000057149562,0.000086056796,0.00016884123,0.0017422196,0.00031451075,0.000009556162,0.0001360451,0.000009272892],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045006245,0.000002257768,0.9965144,0.000003595466,0.000009484002,0.000044168486,0.000045662506,0.00007139226,0.0002636252,0.000083798,0.000020477755,0.0029366794],"study_design_scores_gemma":[0.00009648699,0.0002842869,0.9941589,0.000022684935,0.000014687648,0.00009930663,0.000116879644,0.00024596573,0.0004526407,0.003412598,0.0010190862,0.00007645379],"about_ca_topic_score_codex":0.07782284,"about_ca_topic_score_gemma":0.554709,"teacher_disagreement_score":0.47688618,"about_ca_system_score_codex":3.3262398e-7,"about_ca_system_score_gemma":0.00026643116,"threshold_uncertainty_score":0.99916255},"labels":[],"label_agreement":null},{"id":"W2766797477","doi":"10.1139/cjes-2017-0070","title":"Recent sedimentation in three adjacent fjord-lakes on the Québec North Shore (eastern Canada): facies analysis, laminae preservation, and potential for varve formation","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Center for Northern Studies; Bedford Institute of Oceanography; Université du Québec à Rimouski; Institut National de la Recherche Scientifique; Geological Survey of Canada","funders":"","keywords":"Varve; Geology; Facies; Fjord; Shore; Sediment; Transect; Structural basin; Sedimentation; Geomorphology; Oceanography; Radiocarbon dating; Paleontology; Geochemistry","score_opus":0.04128877538690845,"score_gpt":0.24540069106979723,"score_spread":0.20411191568288878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2766797477","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9839575,0.0005578955,0.000075032796,0.014748961,0.0002067925,0.0001630929,0.000037850852,8.0614734e-7,0.00025203306],"genre_scores_gemma":[0.9995647,0.000091074515,0.000048807557,0.0001931643,0.000033825883,0.0000012003861,0.000016461263,7.3252073e-7,0.000050051694],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990417,0.00008244914,0.0002327602,0.000120905395,0.0002322764,0.00028992456],"domain_scores_gemma":[0.99909973,0.00021899166,0.00023403681,0.0001129419,0.00015125636,0.00018303511],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00090543745,0.000075282136,0.00013900799,0.00023333027,0.0011224264,0.00019797085,0.0004060947,0.000035109708,0.00020779583],"category_scores_gemma":[0.0003474051,0.000048523652,0.00003298771,0.00019911058,0.00044818313,0.00054441777,0.000005723825,0.00012937943,0.000002153048],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020707841,0.0000018087798,0.99094707,0.0000041105213,0.00002401832,0.000012561392,0.0003148344,0.0067217327,2.585046e-7,0.00005848348,0.00006640984,0.0018279958],"study_design_scores_gemma":[0.00015202958,0.000148428,0.9773439,0.000011059482,0.000025033367,0.000013350619,0.0006086152,0.02033464,0.000010139988,0.00025228274,0.0010457237,0.00005479356],"about_ca_topic_score_codex":0.66220486,"about_ca_topic_score_gemma":0.99996394,"teacher_disagreement_score":0.33775905,"about_ca_system_score_codex":0.0000028250172,"about_ca_system_score_gemma":0.0018494396,"threshold_uncertainty_score":0.86329097},"labels":[],"label_agreement":null},{"id":"W2767091401","doi":"10.1139/cjes-2017-0179","title":"A new occurrence of the Early Jurassic brachiopod <i>Anarhynchia</i> from the Canadian Cordillera confirms its membership in chemosynthesis-based ecosystems","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Chemosynthesis; Geology; Cold seep; Siliciclastic; Carbonate; Paleontology; Conglomerate; Petroleum seep; Sedimentary rock; Hydrothermal vent; Sedimentary depositional environment; Ecology; Structural basin","score_opus":0.03736743493262395,"score_gpt":0.22957410373785134,"score_spread":0.19220666880522738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767091401","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9555268,0.0032156145,0.0000015981132,0.0057939924,0.0010325154,0.00016408744,0.00032009144,0.0000018502243,0.03394345],"genre_scores_gemma":[0.9995144,0.00000850062,0.000106052525,0.00024782447,0.00010208778,2.7843834e-7,0.0000011111158,8.435325e-7,0.000018923689],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981713,0.00021040172,0.00043513425,0.00021347567,0.00041465648,0.00055501703],"domain_scores_gemma":[0.9976316,0.00041488215,0.0006519664,0.00036808487,0.00009421661,0.0008392132],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0011910056,0.00016002658,0.0003063111,0.00020537495,0.0018004159,0.00044411625,0.0022814106,0.000112120346,0.0008098619],"category_scores_gemma":[0.0005211958,0.000091930546,0.00015166716,0.00032937503,0.0011291774,0.00047738303,0.0000021867074,0.00041333924,0.000008342108],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008695361,0.0000021115482,0.99143577,0.0000032643975,0.00001566854,0.000032667398,0.00035408768,0.000106357205,0.000009131955,0.000098685145,0.00021522166,0.007718351],"study_design_scores_gemma":[0.00023624899,0.00009646177,0.99688333,0.00018977023,0.000018508454,0.000022282633,0.00015773515,0.0005423288,0.00027173656,0.00027149695,0.0011883995,0.000121699886],"about_ca_topic_score_codex":0.8756683,"about_ca_topic_score_gemma":0.99963385,"teacher_disagreement_score":0.123965584,"about_ca_system_score_codex":0.000004716104,"about_ca_system_score_gemma":0.009492713,"threshold_uncertainty_score":0.9994991},"labels":[],"label_agreement":null},{"id":"W2767169518","doi":"10.1139/cjes-2017-0152","title":"Criteria for the recognition of Archean calc-alkaline lamprophyres: examples from the Abitibi Subprovince","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec); Université du Québec à Chicoutimi","funders":"Ministère de l'Énergie et des Ressources Naturelles","keywords":"Geology; Archean; Geochemistry; Greenstone belt; Mafic; Diorite; Biotite; Phlogopite; Layered intrusion; Plagioclase; Petrology; Zircon; Paleontology; Mantle (geology); Quartz","score_opus":0.0800167381496218,"score_gpt":0.2542413694010549,"score_spread":0.17422463125143312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767169518","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909445,0.0009860902,0.00012705296,0.0064048753,0.00035103908,0.00008981566,0.00036113165,0.0000013961976,0.0007340915],"genre_scores_gemma":[0.99804145,0.000052517957,0.0011870237,0.00034185877,0.00030436646,4.0135438e-7,0.0000119535325,8.44455e-7,0.000059555812],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990471,0.00006332071,0.0002719744,0.00013566419,0.00021513794,0.00026683044],"domain_scores_gemma":[0.9982292,0.00083296024,0.0003390012,0.00018377208,0.00018224778,0.00023278699],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011034395,0.0000792463,0.00016700578,0.000045874553,0.0012655284,0.00025517173,0.001016805,0.00003336433,0.002913933],"category_scores_gemma":[0.0011758349,0.00003490301,0.00013241816,0.000111002155,0.0014448095,0.00021980239,0.000009431763,0.00012008274,0.00001307579],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004755288,0.000008489627,0.93605053,0.000009721639,0.000052215284,0.000014523482,0.0004118732,0.00036790286,0.00090321066,0.00012345471,0.0007753781,0.061235134],"study_design_scores_gemma":[0.00014182563,0.00023557433,0.95794064,0.000040053055,0.000047477923,0.000010457339,0.00050794706,0.0022401111,0.0007652343,0.03139294,0.0065942192,0.00008354144],"about_ca_topic_score_codex":0.27746266,"about_ca_topic_score_gemma":0.83332366,"teacher_disagreement_score":0.555861,"about_ca_system_score_codex":6.855569e-7,"about_ca_system_score_gemma":0.0003562974,"threshold_uncertainty_score":0.9979975},"labels":[],"label_agreement":null},{"id":"W2767186580","doi":"10.1139/cjes-2017-0126","title":"Eemian estuarine record forced by glacio-isostasy (southern Iceland)—link with Greenland and deep sea records","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Deglaciation; Geology; Eemian; Glacial period; Interglacial; Tephra; Marine transgression; Glacier; Paleontology; Oceanography; Younger Dryas; Ice sheet; Sedimentary rock; Volcano","score_opus":0.018702324526025202,"score_gpt":0.2297745034694686,"score_spread":0.21107217894344338,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767186580","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9849104,0.0011348967,0.000031780666,0.0033761158,0.00030630972,0.00008733667,0.000039079197,0.0000036055424,0.010110435],"genre_scores_gemma":[0.9978348,0.00014523945,0.00083966786,0.00016617675,0.00011189794,2.7375447e-7,0.000007810611,0.0000027313124,0.00089141174],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985392,0.000110952016,0.00024710677,0.00024402754,0.00024627175,0.00061243435],"domain_scores_gemma":[0.998326,0.00017037573,0.0002975533,0.00020743957,0.000121472985,0.0008771707],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011783681,0.00014555619,0.00026953925,0.00022802687,0.0017438083,0.00033274805,0.00069967733,0.000111740286,0.0013191621],"category_scores_gemma":[0.00020787229,0.000097539254,0.00003972663,0.00014123216,0.0017962239,0.0004714092,0.000011264388,0.0003740235,0.000061155144],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005074369,0.0000014771223,0.99064577,0.000006555044,0.000018741111,0.0002613993,0.00021189121,0.000027729644,0.0000011348117,0.0000099906465,0.00010981991,0.008654725],"study_design_scores_gemma":[0.0005126864,0.0008780782,0.9899256,0.0000384129,0.000016460812,0.0006836376,0.0003803871,0.0008035225,0.000010278156,0.0004221602,0.0061729467,0.00015579267],"about_ca_topic_score_codex":0.0544797,"about_ca_topic_score_gemma":0.93160295,"teacher_disagreement_score":0.87712324,"about_ca_system_score_codex":5.873516e-7,"about_ca_system_score_gemma":0.00074729125,"threshold_uncertainty_score":0.9995938},"labels":[],"label_agreement":null},{"id":"W2767627061","doi":"10.1139/cjes-2017-0146","title":"The Pele Offset Dykes, Sudbury impact structure, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Wallbridge Mining (Canada); Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Mitacs; Ontario Centres of Excellence","keywords":"Geology; Igneous rock; Geochemistry; Lithology; Archean; Electron microprobe; Petrology; Mineralogy","score_opus":0.01601641982677679,"score_gpt":0.23274892620140256,"score_spread":0.21673250637462577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767627061","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99490005,0.00033104137,0.000045322628,0.0014303119,0.0010643649,0.00003197656,0.00014301181,6.8178986e-7,0.002053258],"genre_scores_gemma":[0.99947894,0.0000038200114,0.000038953738,0.000040495564,0.00029019732,9.755162e-8,0.000008788493,0.0000013024662,0.00013739405],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99928504,0.000018877274,0.00013126696,0.00007333149,0.00021631879,0.00027515995],"domain_scores_gemma":[0.99926,0.000047113535,0.00016536702,0.0001324634,0.0000618305,0.0003332317],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00035356233,0.000059875063,0.000073511466,0.000049537517,0.0021150631,0.00091378985,0.0006653351,0.0000097315,0.00025363395],"category_scores_gemma":[0.000030149853,0.00003395747,0.00003767822,0.00008081248,0.00031247456,0.00090912357,0.000005242816,0.00010569317,0.0000040113496],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000030523115,0.0000013702919,0.9481488,0.0000010012207,0.000026908323,0.0000395956,0.0001547578,0.002548998,0.00010569901,0.0023787187,0.023258448,0.023332682],"study_design_scores_gemma":[0.0001049591,0.00010605262,0.8235725,0.000028180268,0.000008032221,0.000036596724,0.000633125,0.0028714123,0.00025171167,0.003411724,0.1688325,0.00014316579],"about_ca_topic_score_codex":0.8744082,"about_ca_topic_score_gemma":0.9917044,"teacher_disagreement_score":0.14557405,"about_ca_system_score_codex":0.000008141131,"about_ca_system_score_gemma":0.0085834665,"threshold_uncertainty_score":0.9991841},"labels":[],"label_agreement":null},{"id":"W2767640694","doi":"10.1139/cjes-2017-0046","title":"Water budget, performance of evapotranspiration formulations, and their impact on hydrological modeling of a small boreal peatland-dominated watershed","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Institut National de la Recherche Scientifique; Université Laval","funders":"","keywords":"Evapotranspiration; Environmental science; Watershed; Water balance; Hydrology (agriculture); Eddy covariance; Peat; Ecohydrology; Streamflow; Geology; Ecosystem; Geography; Ecology; Drainage basin","score_opus":0.023270050484319783,"score_gpt":0.2326004079939904,"score_spread":0.2093303575096706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767640694","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99817365,0.000018264713,0.000063472246,0.00023150892,0.000040830946,0.000056344197,0.000007118888,9.1328207e-7,0.0014078764],"genre_scores_gemma":[0.99980575,0.000019051738,0.00011723542,0.00002283187,0.000017982456,4.4602763e-7,0.000002878841,0.000002055969,0.000011793352],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992711,0.000028028708,0.00025072473,0.000106776235,0.00010576441,0.00023760385],"domain_scores_gemma":[0.9995001,0.000021248932,0.00016691066,0.000099300465,0.000025362851,0.0001870769],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00065409834,0.00008533178,0.00018863277,0.00010201552,0.0003644469,0.00004342062,0.0002714288,0.00004875441,0.000103183724],"category_scores_gemma":[0.000028421828,0.00004112082,0.000055151286,0.00004118707,0.00045908618,0.00029508438,0.000016359536,0.0000799853,0.0000012422032],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005598778,0.000009352844,0.9359811,0.000003891833,0.0000076067195,0.000004355749,0.0005669442,0.059299227,0.0030748865,0.00001079721,0.0000033988258,0.0009824777],"study_design_scores_gemma":[0.00036090202,0.001233453,0.74663836,0.000022117552,0.000007947711,0.00003241496,0.000020798414,0.24755688,0.0038065126,0.00023403813,0.000023360693,0.000063200474],"about_ca_topic_score_codex":0.0048975237,"about_ca_topic_score_gemma":0.024795175,"teacher_disagreement_score":0.1893427,"about_ca_system_score_codex":0.00000904382,"about_ca_system_score_gemma":0.00007640331,"threshold_uncertainty_score":0.9929998},"labels":[],"label_agreement":null},{"id":"W2767699940","doi":"10.1139/cjes-2017-0086","title":"A missing link in the peri-Gondwanan terrane collage: the Precambrian basement of the Moroccan Meseta and its lower Paleozoic cover","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies Worldwide","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Geology; Paleontology; Terrane; Precambrian; Gondwana; Paleozoic; Basement; Siliciclastic; Ordovician; Unconformity; Craton; Sedimentary depositional environment; Graben; Detritus; Sedimentary rock; Provenance; Rift; Structural basin; Tectonics","score_opus":0.02725488959807996,"score_gpt":0.22045850818868193,"score_spread":0.19320361859060198,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767699940","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9455958,0.0017659769,6.7843536e-7,0.04442732,0.00036567057,0.00014131021,0.000018624174,6.135988e-7,0.007683984],"genre_scores_gemma":[0.9984767,0.000044226945,0.000021615913,0.0009911045,0.000110367764,3.3331804e-7,2.4464367e-7,7.548469e-7,0.00035464737],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987999,0.00015870057,0.00023774836,0.00013166838,0.00034417192,0.00032778707],"domain_scores_gemma":[0.99909425,0.00020941993,0.00026008658,0.00018509249,0.000058075886,0.00019307596],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0012310348,0.000096652286,0.00017087533,0.000045616205,0.0015951302,0.00028901655,0.0010947505,0.000025598063,0.0005108789],"category_scores_gemma":[0.00038804306,0.00003704236,0.00007424843,0.00023583697,0.0011581022,0.00019529946,0.000023436873,0.00019463917,0.000006421063],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001723787,0.000008948955,0.9684627,0.000010439841,0.000017605427,0.00005352026,0.0013488156,0.000803577,0.000026507663,0.0001592306,0.00037211078,0.028719323],"study_design_scores_gemma":[0.00013985089,0.00019315696,0.98555744,0.00005380879,0.000012407161,0.000025858082,0.00040931883,0.00088819495,0.000021627313,0.0005949691,0.012043455,0.000059906026],"about_ca_topic_score_codex":0.01829139,"about_ca_topic_score_gemma":0.5016686,"teacher_disagreement_score":0.48337716,"about_ca_system_score_codex":0.0000013516362,"about_ca_system_score_gemma":0.00033832883,"threshold_uncertainty_score":0.99970466},"labels":[],"label_agreement":null},{"id":"W2768336539","doi":"10.1139/cjes-2017-0077","title":"Three-dimensional hydrostratigraphy of the Orangeville Moraine area, southwestern Ontario, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Baosteel-Australia Joint Research and Development Centre; Northwestern University","keywords":"Geology; Moraine; Terminal moraine; Bedrock; Geomorphology; Aquifer; Glacial period; Geochemistry; Groundwater; Geotechnical engineering","score_opus":0.030180834290855454,"score_gpt":0.2163647138504677,"score_spread":0.18618387955961224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2768336539","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905763,0.0005265092,0.0000013938646,0.002085953,0.00074940175,0.000058554448,0.00004380836,6.2606614e-7,0.0059574186],"genre_scores_gemma":[0.99945945,0.000001740606,0.00015408153,0.00017379507,0.000028456674,9.17642e-8,0.0000013512141,8.0500854e-7,0.00018021277],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988129,0.000050557508,0.00025012,0.00012582443,0.00038150395,0.00037908464],"domain_scores_gemma":[0.9987954,0.0001108321,0.00034381685,0.00023754351,0.00013351641,0.00037889264],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00072130875,0.000089928944,0.00019433143,0.00011849672,0.0013493231,0.00007984467,0.0010915712,0.000054823857,0.0030072979],"category_scores_gemma":[0.00015262685,0.000053786684,0.00008088746,0.00013553229,0.0017649535,0.00021558527,0.000010764,0.00027632038,0.000005487678],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000065405065,0.0000014409817,0.9984292,0.0000023263701,0.000013176923,0.00007610467,0.000089499794,0.0009888732,0.0000016057278,0.000025759966,0.00028884914,0.00007665029],"study_design_scores_gemma":[0.00014022703,0.00010566819,0.9975123,0.000034618053,0.000008240631,0.00019861541,0.000059622307,0.00032433617,0.000033412394,0.0005532643,0.0009665529,0.00006314127],"about_ca_topic_score_codex":0.988795,"about_ca_topic_score_gemma":0.9999965,"teacher_disagreement_score":0.0112015,"about_ca_system_score_codex":8.523407e-7,"about_ca_system_score_gemma":0.009087508,"threshold_uncertainty_score":0.99995077},"labels":[],"label_agreement":null},{"id":"W2768383108","doi":"10.1139/cjes-2017-0168","title":"The vesicular Sainte-Sophie dykes: a chemically distinct, near-surface facies of the Grenville Dyke Swarm?","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Chicoutimi","funders":"","keywords":"Geology; Plagioclase; Geochemistry; Pyroxene; Phenocryst; Olivine; Basalt; Facies; Intrusion; Igneous rock; Geomorphology; Paleontology; Volcano; Volcanic rock","score_opus":0.016138899154871322,"score_gpt":0.19603869319497091,"score_spread":0.1798997940400996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2768383108","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98339856,0.0014234319,0.0000051957154,0.008599573,0.00032522337,0.000053455617,0.000032992106,0.0000017765254,0.00615979],"genre_scores_gemma":[0.999162,0.00003857725,0.00029209044,0.00014886793,0.000073305826,1.02692574e-7,8.369129e-7,0.0000011161502,0.0002830817],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99847543,0.00007159014,0.0003690835,0.00017205572,0.00046270312,0.00044911687],"domain_scores_gemma":[0.99831957,0.00023482248,0.00050249405,0.00032424383,0.00016643247,0.0004524286],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["sts"],"category_scores_codex":[0.00096136826,0.00012699822,0.00023561339,0.000024401295,0.002552966,0.00045037328,0.002001843,0.000051244828,0.0011341011],"category_scores_gemma":[0.0012931544,0.000055615277,0.00023760802,0.00026686315,0.003943339,0.00017524631,0.00003358989,0.00024372486,0.000029527344],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007859726,0.000004124192,0.99440366,0.000004162696,0.000026896343,0.00001875126,0.00010979173,0.0023975712,0.00026026068,0.00013545723,0.00020209553,0.0024293545],"study_design_scores_gemma":[0.000108877975,0.00012626298,0.97246224,0.000040745144,0.000031051924,0.000042320957,0.000286729,0.0016415365,0.0015739583,0.0068780812,0.016688414,0.000119782904],"about_ca_topic_score_codex":0.025665656,"about_ca_topic_score_gemma":0.32449812,"teacher_disagreement_score":0.29883245,"about_ca_system_score_codex":0.0000018829288,"about_ca_system_score_gemma":0.000594968,"threshold_uncertainty_score":0.999779},"labels":[],"label_agreement":null},{"id":"W2768768849","doi":"10.1139/cjes-2017-0131","title":"Underwater faunal assemblages: radiocarbon dates and late Quaternary vertebrates from Cold Lake, Alberta and Saskatchewan, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Pleistocene-Era Hominins and Archaeology","field":"Social Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Alberta Museum","funders":"","keywords":"Quaternary; Geology; Holocene; Radiocarbon dating; Pleistocene; Biota; Last Glacial Maximum; Paleontology; Glacial period; Range (aeronautics); Ecology; Biology","score_opus":0.020935602361555065,"score_gpt":0.2489269047046684,"score_spread":0.22799130234311335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2768768849","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9898312,0.0006861207,0.000004113168,0.006639814,0.0005568246,0.00005777473,0.000028701246,0.0000019069855,0.0021935566],"genre_scores_gemma":[0.9978102,0.00012294432,0.00019550645,0.00045937725,0.0001900385,5.7993856e-7,0.0000011620251,0.0000050285416,0.0012151597],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987081,0.0001122201,0.00023029189,0.00021354474,0.00026406604,0.00047173706],"domain_scores_gemma":[0.99849665,0.0002206492,0.00025544857,0.00012846463,0.000068093854,0.0008307088],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0006398138,0.0001200571,0.00024227469,0.00010830853,0.0020384297,0.00049109926,0.00058366347,0.00006804171,0.000120581186],"category_scores_gemma":[0.0001925028,0.00009814703,0.00002729181,0.00006773956,0.0021719306,0.00059060036,0.00004409159,0.00014827399,0.0000012321192],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000047650974,0.0000022537047,0.9951312,0.0000022260344,0.000021089687,0.00018886915,0.0033153484,0.000009365664,0.00023937684,0.00040800255,0.00025063765,0.00042689312],"study_design_scores_gemma":[0.0003930672,0.00013865615,0.96368086,0.000081021004,0.000023372042,0.000036783982,0.005753651,0.000257049,0.0006265276,0.0026250563,0.026148751,0.00023519936],"about_ca_topic_score_codex":0.96208984,"about_ca_topic_score_gemma":0.99997836,"teacher_disagreement_score":0.037888493,"about_ca_system_score_codex":0.000016236505,"about_ca_system_score_gemma":0.0044479617,"threshold_uncertainty_score":0.9992608},"labels":[],"label_agreement":null},{"id":"W2770367252","doi":"10.1139/cjes-2017-0195","title":"Dinosaur eggshells from the lower Maastrichtian St. Mary River Formation of southern Alberta, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Eggshell; Cretaceous; Assemblage (archaeology); Geology; Paleontology; Fauna; Range (aeronautics); Ecology; Biology","score_opus":0.014419067952885223,"score_gpt":0.19060406775267136,"score_spread":0.17618499979978614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2770367252","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9866213,0.00093446067,0.000017045266,0.003034429,0.0011595926,0.00004308845,0.0005103223,6.658647e-7,0.007679075],"genre_scores_gemma":[0.99910027,0.000017859422,0.00012686555,0.00037100018,0.00014763269,5.928502e-8,0.0000111638865,6.9701383e-7,0.00022443727],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990931,0.00008455472,0.00024713142,0.000099854726,0.00019063246,0.0002847291],"domain_scores_gemma":[0.99885553,0.00024909308,0.00039964708,0.00016032455,0.00007591739,0.000259483],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042240703,0.00007865458,0.00014259726,0.000064503096,0.0009191558,0.000055665678,0.0008423072,0.00005516887,0.0021140254],"category_scores_gemma":[0.00019767127,0.00004788977,0.00004997442,0.0000778495,0.001046467,0.00041282165,0.0000058132077,0.00013902977,0.0000366024],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011938966,0.0000015953792,0.99468684,8.906799e-7,0.000010627062,0.000030731004,0.00024238235,0.0003730735,0.0000031139177,0.00001880785,0.0019134893,0.0027064984],"study_design_scores_gemma":[0.000105003215,0.000104911065,0.98147285,0.000020475245,0.000011295017,0.000054617678,0.0004527503,0.0005857388,0.000012630287,0.0005135456,0.01660256,0.00006363557],"about_ca_topic_score_codex":0.980122,"about_ca_topic_score_gemma":0.99979633,"teacher_disagreement_score":0.019674296,"about_ca_system_score_codex":0.0000028691902,"about_ca_system_score_gemma":0.0021006735,"threshold_uncertainty_score":0.9987982},"labels":[],"label_agreement":null},{"id":"W2771996787","doi":"10.1139/cjes-2017-0079","title":"U–Pb geochronology and trace element composition of zircon from the Horseshoe Lake greenstone belt, Superior Province, Canada: implications for the tectonic and metamorphic history","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick; Geological Survey of Canada; Natural Resources Canada; University of Ottawa","funders":"Natural Resources Canada; Goldcorp","keywords":"Zircon; Geology; Geochemistry; Metamorphism; Geochronology; Greenstone belt; Archean; Metasomatism; Greenschist; Metamorphic rock; Mantle (geology)","score_opus":0.024186957128426896,"score_gpt":0.20134917970656352,"score_spread":0.17716222257813663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2771996787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9702051,0.009389478,0.000060760638,0.019707767,0.00012482402,0.00011795391,0.00023497049,8.4250456e-7,0.0001582953],"genre_scores_gemma":[0.9990854,0.00013074875,0.00041793208,0.00027626794,0.000054516924,9.049523e-7,0.000007150597,6.648271e-7,0.000026378839],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99929875,0.000037692265,0.00020850822,0.00013491494,0.00011266209,0.00020747812],"domain_scores_gemma":[0.9990105,0.0003224283,0.00024693448,0.00013639146,0.00008715514,0.00019657607],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004467209,0.000072589035,0.00016958533,0.000040353127,0.0009163583,0.00005976341,0.00043176155,0.000027709473,0.00058871973],"category_scores_gemma":[0.00011404185,0.00003693746,0.000045030312,0.000053580356,0.0014265879,0.00013273701,0.0000099913095,0.00010231634,3.717976e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010031417,0.000003477308,0.9828684,0.0000044675535,0.000050926308,0.0000043373943,0.00008468041,0.00023231762,0.00090975565,0.00028778723,0.00039491712,0.015148924],"study_design_scores_gemma":[0.00011228117,0.0001274183,0.98704904,0.000008637857,0.000072311195,0.000029536579,0.00011409771,0.0005722088,0.00011942202,0.001017343,0.010723999,0.000053699958],"about_ca_topic_score_codex":0.8236206,"about_ca_topic_score_gemma":0.9993472,"teacher_disagreement_score":0.17572655,"about_ca_system_score_codex":0.0000045477004,"about_ca_system_score_gemma":0.0012667949,"threshold_uncertainty_score":0.70479804},"labels":[],"label_agreement":null},{"id":"W2772509336","doi":"10.1139/cjes-2017-0160","title":"Late Ordovician (Hirnantian) diploporitan fauna of Anticosti Island, Quebec, Canada: implications for evolutionary and biogeographic patterns","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Geographic Society; National Science Foundation","keywords":"Ordovician; Crinoid; Paleontology; Geology; Echinoderm; Fauna; Biogeography; Trilobite; Conodont; Paleoecology; Taxon; Ecology; Biostratigraphy; Biology","score_opus":0.02063039804023565,"score_gpt":0.231301919540356,"score_spread":0.21067152150012036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2772509336","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98753095,0.0057931407,0.000054977692,0.0032716913,0.00047415748,0.000097863885,0.00071022613,0.000001536878,0.0020654604],"genre_scores_gemma":[0.99925846,0.00013049282,0.00045295936,0.000055745437,0.00007385906,2.938985e-7,0.0000042656025,6.7676626e-7,0.000023265266],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990524,0.000028449946,0.0002933258,0.00015197914,0.00013622305,0.00033761424],"domain_scores_gemma":[0.9987647,0.00010583162,0.00039926264,0.00015314524,0.00014580782,0.00043125276],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00035715202,0.00009710516,0.00020420768,0.00025129298,0.0014122088,0.0001228796,0.00051523617,0.000054141085,0.000060704435],"category_scores_gemma":[0.00013378468,0.00007745767,0.000070700175,0.00013677916,0.0009267253,0.00043781224,0.0000015522445,0.00009657805,2.3062991e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004835132,0.0000020963034,0.98524326,0.000008206632,0.000019771061,0.000011307774,0.00004982124,0.000016953089,0.000010597088,0.00024695828,0.0001136402,0.014272582],"study_design_scores_gemma":[0.00016142013,0.00012751878,0.9967449,0.00004829546,0.000020970316,0.00004899823,0.00011318178,0.00012248554,0.000010853531,0.0013983089,0.0011064926,0.000096625765],"about_ca_topic_score_codex":0.91928196,"about_ca_topic_score_gemma":0.9999118,"teacher_disagreement_score":0.08062981,"about_ca_system_score_codex":0.0000014028926,"about_ca_system_score_gemma":0.0025931215,"threshold_uncertainty_score":0.9998878},"labels":[],"label_agreement":null},{"id":"W2775043799","doi":"10.1139/cjes-2017-0184","title":"Mineralogy and genesis of the Ni–Co lateritic regolith deposit of the Çaldağ area (Manisa, western Anatolia), Turkey","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Macquarie University; Commonwealth Scientific and Industrial Research Organisation; Türkiye Bilimsel ve Teknolojik Araştırma Kurumu; Texas Tech University","keywords":"Geology; Saprolite; Ultramafic rock; Weathering; Pyrite; Geochemistry; Mineralogy; Clay minerals; Laterite; Olivine; Kaolinite; Nickel; Chemistry","score_opus":0.020920024290684434,"score_gpt":0.2030110698342937,"score_spread":0.18209104554360928,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2775043799","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946437,0.00092315883,0.0000010605988,0.0023688492,0.00019495103,0.000036999594,0.00003146763,6.248979e-7,0.0017992029],"genre_scores_gemma":[0.99946755,0.000038177175,0.000086944776,0.00019608687,0.000035331403,6.7768326e-8,4.582267e-7,7.2370625e-7,0.00017467594],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99903035,0.00007044926,0.0002773649,0.00012572839,0.00024549433,0.00025062222],"domain_scores_gemma":[0.9989984,0.00006139121,0.00036255136,0.00021295302,0.00010532414,0.00025935107],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035004623,0.00008440407,0.00022435641,0.00007074832,0.00054522953,0.00009826345,0.0009605422,0.000043731547,0.00047058662],"category_scores_gemma":[0.00019088743,0.000038558534,0.00010183259,0.00019177147,0.0016494278,0.00016370136,0.000020950813,0.00010318702,0.000002226507],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002781128,0.0000022017073,0.99883616,0.00000741198,0.000013606955,0.0000092050805,0.00009877026,0.00021710995,0.00029567454,0.00002488305,0.000035042296,0.00045713838],"study_design_scores_gemma":[0.00007442396,0.000079631725,0.9960488,0.000044201908,0.000036429712,0.00010427525,0.0000930591,0.0002984766,0.0014966321,0.00143118,0.00023708997,0.00005576894],"about_ca_topic_score_codex":0.14171597,"about_ca_topic_score_gemma":0.61485267,"teacher_disagreement_score":0.4731367,"about_ca_system_score_codex":8.7531015e-7,"about_ca_system_score_gemma":0.0002386023,"threshold_uncertainty_score":0.8639994},"labels":[],"label_agreement":null},{"id":"W2779340447","doi":"10.1139/cjes-2017-0186","title":"Real-time monitoring for structural health, public safety, and risk management of mine tailings dams","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Tailings Management and Properties","field":"Engineering","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"BC Innovation Council; National Research Council Canada","funders":"","keywords":"Tailings; Work (physics); Stakeholder; Risk analysis (engineering); Stakeholder engagement; Business; Environmental planning; Engineering; Environmental economics; Environmental science","score_opus":0.0269823124079209,"score_gpt":0.25076913895093256,"score_spread":0.22378682654301166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2779340447","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99463654,0.0018217074,0.000070502254,0.0004424885,0.00057888747,0.000116123425,0.000010139803,0.0000071328086,0.0023164672],"genre_scores_gemma":[0.99157584,0.0019634997,0.006083784,0.0000034854806,0.00010660475,6.4094667e-7,3.6464488e-7,0.000006506148,0.00025930192],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99921465,0.000010151426,0.00026957018,0.00008592606,0.0001345388,0.00028517505],"domain_scores_gemma":[0.9992829,0.0000198438,0.0002573766,0.00011650729,0.0000633248,0.00026004633],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007355039,0.00008099435,0.00017083794,0.00018815155,0.000675297,0.00026653794,0.0003815761,0.000019021758,0.000017088723],"category_scores_gemma":[0.000045324065,0.00006611005,0.000038912844,0.00006865138,0.00022905723,0.0004997755,0.000019860972,0.000065088294,7.542533e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005100594,0.000005364678,0.6820398,0.000922208,0.0004262852,0.000038645856,0.0025271217,0.012225762,0.000648949,0.0032869903,0.00066692557,0.29716092],"study_design_scores_gemma":[0.0019350986,0.0011320773,0.9069739,0.0011445102,0.00013745249,0.000046334957,0.003158486,0.029077908,0.0018501248,0.002961431,0.050886102,0.00069658784],"about_ca_topic_score_codex":0.003026896,"about_ca_topic_score_gemma":0.0064707333,"teacher_disagreement_score":0.29646432,"about_ca_system_score_codex":0.000009745141,"about_ca_system_score_gemma":0.00010971717,"threshold_uncertainty_score":0.51939064},"labels":[],"label_agreement":null},{"id":"W2781969447","doi":"10.1139/cjes-2017-0067","title":"Geoelectric structure of the Great Slave Lake shear zone in northwest Alberta: implications for structure and tectonic history","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; China Scholarship Council; Helmholtz-Alberta Initiative; Western Canada Research Grid; Compute Canada","keywords":"Geology; Terrane; Precambrian; Tectonics; Basement; Magnetotellurics; Shear zone; Metamorphic rock; Seismology; Lithosphere; Shear (geology); Sedimentary rock; Fault (geology); Geophysics; Geomorphology; Petrology; Paleontology; Electrical resistivity and conductivity","score_opus":0.014142391783985728,"score_gpt":0.21781055148879763,"score_spread":0.2036681597048119,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2781969447","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99721265,0.00097072584,0.000044985278,0.00092178583,0.000341277,0.00013113345,0.000120078585,0.000001030569,0.00025635515],"genre_scores_gemma":[0.998162,0.000009052006,0.0013556771,0.00019776289,0.00014224564,1.6848816e-7,0.0000023501427,0.0000016576023,0.000129138],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99904007,0.00007009417,0.000245333,0.0001622364,0.00013557446,0.00034668125],"domain_scores_gemma":[0.99904656,0.0002603284,0.00017686035,0.00010633176,0.00013338569,0.00027650592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021568598,0.00009658448,0.0001941911,0.00023524683,0.00025597203,0.000030679472,0.00036825018,0.00005954202,0.00054271566],"category_scores_gemma":[0.00025705283,0.00005750686,0.00006054571,0.00083070644,0.0007167114,0.00015836267,0.0000044585613,0.00018035754,9.951632e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013039312,0.0000033527406,0.9337971,0.00001043398,0.000009661002,0.0000012196414,0.0003034716,0.00029295572,0.00040252294,0.0004023754,0.00012461275,0.06463924],"study_design_scores_gemma":[0.00013629338,0.00047221262,0.9820396,0.000013975245,0.000012567831,0.000056493354,0.00001449735,0.00039731327,0.00030734146,0.0051531782,0.011320664,0.00007586707],"about_ca_topic_score_codex":0.03488627,"about_ca_topic_score_gemma":0.9346283,"teacher_disagreement_score":0.899742,"about_ca_system_score_codex":0.000005123347,"about_ca_system_score_gemma":0.0010820244,"threshold_uncertainty_score":0.9715405},"labels":[],"label_agreement":null},{"id":"W2782552157","doi":"10.1139/cjes-2017-0176","title":"Tectonostratigraphic and petrogenetic setting of late Mississippian volcanism in eastern Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Volcanism; Geochemistry; Paleontology; Earth science; Tectonics","score_opus":0.011500778641253307,"score_gpt":0.1826230526595908,"score_spread":0.1711222740183375,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2782552157","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952201,0.0010610445,0.0000016230733,0.0009780203,0.00007959445,0.000022461527,0.000012131348,7.0210814e-7,0.0026242954],"genre_scores_gemma":[0.9993558,0.000011406118,0.00039334022,0.0001733066,0.00003680643,3.281372e-8,6.650054e-7,5.3966795e-7,0.000028080567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990428,0.000043152784,0.0002906217,0.00012558288,0.00020204877,0.00029580592],"domain_scores_gemma":[0.99917996,0.00006380912,0.00014978932,0.00004818236,0.000078532175,0.00047971468],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00039839259,0.00007508659,0.00017635305,0.0002155261,0.00014073917,0.000040838717,0.00023138801,0.00002786295,0.001434425],"category_scores_gemma":[0.00010796615,0.000052064854,0.000034551027,0.00058442703,0.0005196635,0.00009320229,0.0000035390437,0.000099327255,0.0000021726214],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021117316,9.960529e-7,0.9968069,0.0000034245484,0.0000051395473,0.000025468684,0.000073190895,0.00023054199,0.00009620952,0.000010176205,0.000007522122,0.002738295],"study_design_scores_gemma":[0.00007895924,0.00020094082,0.99491364,0.000032640964,0.000007629444,0.000035798705,0.00020392639,0.0022607392,0.0005028796,0.0013206145,0.00037294987,0.000069286325],"about_ca_topic_score_codex":0.89688945,"about_ca_topic_score_gemma":0.99948967,"teacher_disagreement_score":0.102600254,"about_ca_system_score_codex":9.649004e-7,"about_ca_system_score_gemma":0.0011949328,"threshold_uncertainty_score":0.9994784},"labels":[],"label_agreement":null},{"id":"W2782669930","doi":"10.1139/cjes-2016-0152","title":"In situ geochemical characterization of pyrite crystals in burial dolomites of St. George Group carbonates","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Pyrite; Dolomite; Geology; Geochemistry; Mineralogy; Sulfide; Fluid inclusions; Mineralization (soil science); Sulfate; Sphalerite; Quartz; Chemistry; Paleontology","score_opus":0.012102853639116607,"score_gpt":0.19719112806836833,"score_spread":0.18508827442925171,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2782669930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997935,0.00024227159,0.0000035134367,0.00051953795,0.00016265316,0.00004206933,0.000051387142,9.802609e-7,0.0010426086],"genre_scores_gemma":[0.99949735,0.000022856291,0.000235952,0.00009164779,0.00012267288,1.0745017e-7,0.000013503277,7.7797955e-7,0.000015147828],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986705,0.00007194423,0.0005414582,0.0001517215,0.00025177945,0.00031259898],"domain_scores_gemma":[0.999157,0.00012583884,0.00027841367,0.00006264282,0.00012849945,0.00024761996],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008346787,0.000088683795,0.00031279956,0.00044743053,0.00004936012,0.000024941997,0.00033174755,0.00006942517,0.0028829554],"category_scores_gemma":[0.00029622935,0.00006360868,0.000074686555,0.0009164198,0.0008610875,0.0002989743,0.000007669759,0.00012504644,0.0000043210753],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024268471,0.000011623576,0.91027963,0.0000073529104,0.0000053959343,0.000017843715,0.00016758095,0.00008312805,0.088868454,0.000063965825,0.0000071161467,0.00046364017],"study_design_scores_gemma":[0.00023840624,0.0003467404,0.9662593,0.000058912086,0.0000083052055,0.000013302299,0.00011040384,0.00078722904,0.02669595,0.004978606,0.00040780296,0.00009506013],"about_ca_topic_score_codex":0.030398635,"about_ca_topic_score_gemma":0.4536406,"teacher_disagreement_score":0.42324197,"about_ca_system_score_codex":0.000001745671,"about_ca_system_score_gemma":0.00023939628,"threshold_uncertainty_score":0.9980285},"labels":[],"label_agreement":null},{"id":"W2783355937","doi":"10.1139/cjes-2017-0094","title":"Magnetization age from paleomagnetism of the Copper Harbor red beds, Northern Michigan, USA, and its Keweenawan geologic consequences","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Paleomagnetism; Apparent polar wander; Polar wander; Zircon; Red beds; Volcanic rock; Clockwise; Sedimentary rock; Volcano; Geochemistry; Conglomerate; Plate tectonics; Paleontology; Geomorphology; Tectonics; Fold (higher-order function)","score_opus":0.016514639795984033,"score_gpt":0.1847945237540913,"score_spread":0.16827988395810728,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2783355937","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9908726,0.0027848424,0.0000026281746,0.0026754946,0.00023737155,0.00005819202,0.00006198259,0.0000019874842,0.0033048831],"genre_scores_gemma":[0.99877673,0.00007959985,0.00044410236,0.0004207448,0.00011903758,1.2071929e-7,0.00000335764,8.74077e-7,0.0001554343],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99879104,0.000113001435,0.00032904,0.00019235212,0.00027791108,0.00029664484],"domain_scores_gemma":[0.99893296,0.00014787292,0.0002686694,0.00009193404,0.00019606827,0.00036251126],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038520707,0.000109406246,0.00021540611,0.00011245908,0.00038381582,0.000077420125,0.00050901144,0.00006382878,0.0076636216],"category_scores_gemma":[0.00036319895,0.000059713544,0.000074346965,0.00049657596,0.0022888142,0.00016738247,0.000011772024,0.00012275341,0.00003238012],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000054270195,0.000002499407,0.9975457,0.000002359324,0.000010122526,0.00001865679,0.0001462458,0.00010743184,0.0013739376,0.00004259344,0.0000384535,0.0007065609],"study_design_scores_gemma":[0.000105013336,0.00038250562,0.9905078,0.000031755986,0.000029380559,0.000021947502,0.00012948619,0.00056311314,0.0015039883,0.0055950014,0.0010362037,0.00009382201],"about_ca_topic_score_codex":0.044877756,"about_ca_topic_score_gemma":0.91272193,"teacher_disagreement_score":0.86784416,"about_ca_system_score_codex":6.49199e-7,"about_ca_system_score_gemma":0.00043850648,"threshold_uncertainty_score":0.9932435},"labels":[],"label_agreement":null},{"id":"W2783417082","doi":"10.1139/cjes-2017-0150","title":"Influence of a large debris flow fan on the late Holocene evolution of Squamish River, southwest British Columbia, Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geoscience BC; Simon Fraser University","funders":"","keywords":"Overbank; Geology; Alluvial fan; Aggradation; Floodplain; Debris; Holocene; Hydrology (agriculture); Debris flow; Tributary; Moraine; Geomorphology; Glacier; Radiocarbon dating; Fluvial; Oceanography; Paleontology; Geography","score_opus":0.004840515482833636,"score_gpt":0.1779710576682168,"score_spread":0.17313054218538318,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2783417082","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982625,0.00008569355,0.000008178896,0.00017809359,0.00018739785,0.00006499115,0.000088935296,0.0000012096608,0.0011229737],"genre_scores_gemma":[0.9993873,0.000011353513,0.00009259414,0.00022491794,0.00003322289,2.7616122e-7,4.0179995e-7,0.0000035160942,0.00024642004],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873775,0.000051825067,0.00029460367,0.000117330856,0.00046648935,0.0003319946],"domain_scores_gemma":[0.99914837,0.0000444756,0.00028327724,0.000114539944,0.00010809956,0.00030124508],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006565533,0.0000627413,0.00014710377,0.000042232605,0.00044734307,0.00007020591,0.00048343735,0.000048166585,0.00080750114],"category_scores_gemma":[0.0001765336,0.000053881144,0.000050848976,0.00048680464,0.0013692091,0.00018825861,0.000025695022,0.00013764336,0.000007114205],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000035066282,0.000011552802,0.99170125,0.0000025578522,0.000009348524,0.000022826001,0.00032303596,0.0045127636,0.00006464535,0.000013740169,0.0025821456,0.00075262616],"study_design_scores_gemma":[0.00020161009,0.000288938,0.99628466,0.000095196134,0.000010823423,0.000039782295,0.00018354726,0.0003889113,0.00019115038,0.00014546051,0.0020939163,0.00007598243],"about_ca_topic_score_codex":0.97659457,"about_ca_topic_score_gemma":0.9990723,"teacher_disagreement_score":0.022477781,"about_ca_system_score_codex":0.000057610458,"about_ca_system_score_gemma":0.0013381,"threshold_uncertainty_score":0.8841571},"labels":[],"label_agreement":null},{"id":"W2783464756","doi":"10.1139/cjes-2017-0115","title":"Late Cretaceous radiolarians from a bentonite-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Regina","funders":"","keywords":"Cretaceous; Geology; Paleontology; Foraminifera; Microfauna; Assemblage (archaeology); Radiolaria; Structural basin; Sverdrup; Subaerial; Fauna; Oceanography; Benthic zone; Ecology","score_opus":0.013551601478427525,"score_gpt":0.18764511384391316,"score_spread":0.17409351236548565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2783464756","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.991751,0.00388754,0.000020450832,0.002421989,0.00025914557,0.000092290786,0.00042155792,0.0000013154702,0.0011446947],"genre_scores_gemma":[0.99953544,0.000020696387,0.00012457515,0.00022473486,0.00006103578,2.611147e-7,0.0000036053025,6.199235e-7,0.000029002274],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99893564,0.00012484966,0.00032362834,0.00013324109,0.0002177201,0.00026492192],"domain_scores_gemma":[0.9990757,0.00013283633,0.00030168178,0.00015523263,0.00004788447,0.00028662695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038695295,0.000103265476,0.0001407225,0.00009299351,0.0010269808,0.0000832433,0.00049903087,0.000046097775,0.00027902442],"category_scores_gemma":[0.000029756227,0.000058092264,0.00006385257,0.00029863656,0.0018995513,0.0003043673,0.0000035022238,0.00014762967,0.0000015043355],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005794723,0.0000016037134,0.99495804,0.0000015389124,0.000019723091,0.0000050800586,0.0016243419,0.000025165748,0.00016312343,0.000007855433,0.00011794561,0.0030697612],"study_design_scores_gemma":[0.00011775466,0.00013804685,0.99602073,0.0000198647,0.000026301623,0.00013920596,0.0021890204,0.00013671852,0.0005039166,0.00025433308,0.00038297722,0.00007109742],"about_ca_topic_score_codex":0.44637483,"about_ca_topic_score_gemma":0.99946225,"teacher_disagreement_score":0.5530874,"about_ca_system_score_codex":0.000002923255,"about_ca_system_score_gemma":0.0012267011,"threshold_uncertainty_score":0.789881},"labels":[],"label_agreement":null},{"id":"W2783486932","doi":"10.1139/cjes-2017-0154","title":"Understanding fluid behavior through ion and isotope data from the Yitong Basin, Northeast China","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China; Jilin University; National Youth Science Foundation","keywords":"Geology; Weathering; Geochemistry; Plagioclase; Meteoric water; Structural basin; Mineralogy; Groundwater; Quartz; Geomorphology; Paleontology","score_opus":0.10221702288510084,"score_gpt":0.24710574477468739,"score_spread":0.14488872188958654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2783486932","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99256045,0.0010076879,0.00020893598,0.0011561533,0.0008244358,0.00008256124,0.00020693536,0.000003335439,0.0039495234],"genre_scores_gemma":[0.9985148,0.00005208467,0.0004674736,0.00030020226,0.0005970619,9.943786e-8,0.000023942795,0.000001909306,0.000042469517],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988683,0.00005650647,0.00022969526,0.00022768341,0.0002718633,0.0003459793],"domain_scores_gemma":[0.9991676,0.00008850698,0.00011803193,0.00024360057,0.000047614063,0.0003346327],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00072089076,0.000106094376,0.0001370796,0.000052966592,0.0010379626,0.00047968247,0.00088493567,0.00004099333,0.0021445635],"category_scores_gemma":[0.00007685815,0.00006452818,0.000029016688,0.0002465165,0.001109117,0.0009664315,0.000021861493,0.00014977262,0.000028453775],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004028838,0.0000018306665,0.9977747,0.0000019798313,0.0000064346873,0.000026885227,0.0006228075,0.00000935108,0.00005094125,0.000021574504,0.00069340126,0.0007860459],"study_design_scores_gemma":[0.00014365811,0.00018085496,0.98978955,0.00011088272,0.000027601458,0.00020947297,0.002142179,0.00054043526,0.00024774647,0.00083034806,0.005645616,0.00013163927],"about_ca_topic_score_codex":0.08309141,"about_ca_topic_score_gemma":0.60665727,"teacher_disagreement_score":0.5235658,"about_ca_system_score_codex":0.0000025424765,"about_ca_system_score_gemma":0.0006926525,"threshold_uncertainty_score":0.9987676},"labels":[],"label_agreement":null},{"id":"W2784488663","doi":"10.1139/cjes-2017-0173","title":"Internal fabric of giant domes in the Mesoarchean Steep Rock carbonate platform, Superior Province, Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada; Lakehead University","keywords":"Calcite; Geology; Dolomite; Carbonate; Archean; Quartz; Geochemistry; Aragonite; Subaerial; Mineralogy; Paleontology; Materials science","score_opus":0.018198146793034106,"score_gpt":0.2122141379743315,"score_spread":0.1940159911812974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2784488663","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96111846,0.0026034187,0.000010896196,0.0006225697,0.00051878946,0.00007955934,0.000039094823,0.0000010741379,0.035006147],"genre_scores_gemma":[0.99951684,0.000012741762,0.00017897812,0.00016084207,0.00009957279,1.3587687e-7,4.643693e-7,5.2335605e-7,0.000029896659],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99849445,0.000103747196,0.0004000751,0.000136565,0.00040901193,0.0004561367],"domain_scores_gemma":[0.9991142,0.00016684685,0.00020673605,0.000099426754,0.00008907586,0.0003236758],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001132889,0.0001088865,0.0002170582,0.00033206152,0.00031533043,0.00007386204,0.0008586819,0.000044904093,0.0002563451],"category_scores_gemma":[0.00009818462,0.00006584112,0.00006294561,0.0004928903,0.0009882221,0.0003486742,0.0000014102221,0.00022915463,0.0000017050614],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021905307,0.0000033564045,0.983897,0.0000065267755,0.000014280808,0.00023450865,0.0010782,0.00017223018,0.000023867417,0.00024983034,0.00018769305,0.014110617],"study_design_scores_gemma":[0.00016577668,0.0004885138,0.99472463,0.00004490438,0.0000065820127,0.0002806566,0.0016803468,0.00097165606,0.00012590319,0.00039509998,0.001029168,0.00008675331],"about_ca_topic_score_codex":0.87113637,"about_ca_topic_score_gemma":0.999617,"teacher_disagreement_score":0.12848063,"about_ca_system_score_codex":0.000003271333,"about_ca_system_score_gemma":0.0063953,"threshold_uncertainty_score":0.99923754},"labels":[],"label_agreement":null},{"id":"W2784963041","doi":"10.1139/cjes-2017-0180","title":"Converging ice streams: a new paradigm for reconstructions of the Laurentide Ice Sheet in southern Ontario and deposition of the Oak Ridges Moraine","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"The Scarborough Hospital","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Deglaciation; Moraine; Ice stream; Meltwater; Ice sheet; STREAMS; Glacier; Escarpment; Geomorphology; Outwash plain; Glacier morphology; Antarctic sea ice; Drumlin; Glacial period; Arctic ice pack; Lineation; Sea ice; Cryosphere; Oceanography; Paleontology","score_opus":0.02351769466723181,"score_gpt":0.20602870224433265,"score_spread":0.18251100757710084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2784963041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963352,0.00059063965,0.0000361259,0.0020486861,0.00046019678,0.000094786075,0.000069847185,6.128196e-7,0.00036391077],"genre_scores_gemma":[0.9985916,0.000020747771,0.0010315654,0.00012910871,0.00007379247,1.7480797e-7,7.754923e-7,8.602744e-7,0.0001514001],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99938977,0.000028803364,0.00023223751,0.00007777289,0.00012063537,0.00015078578],"domain_scores_gemma":[0.99941254,0.000104252525,0.00023015124,0.00006951337,0.000080909325,0.00010262515],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030125046,0.000052382205,0.00011168734,0.0000486809,0.00039267968,0.00003679907,0.00021467784,0.000018859999,0.00026492923],"category_scores_gemma":[0.0000967407,0.000030348208,0.000046752837,0.00039224382,0.0006442476,0.00014531954,0.00000510358,0.00006777037,4.3032463e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000049394134,0.0000016363996,0.991553,0.0000033024012,0.0000096259855,3.4096388e-7,0.0026832197,0.00092688395,0.000012225176,0.00010538072,0.00016829206,0.004531148],"study_design_scores_gemma":[0.00017386249,0.000110441666,0.9898245,0.000078351426,0.00001861306,0.000027864739,0.004634413,0.0008862959,0.00006534118,0.0009090946,0.0032293166,0.00004195146],"about_ca_topic_score_codex":0.45791098,"about_ca_topic_score_gemma":0.99485856,"teacher_disagreement_score":0.5369476,"about_ca_system_score_codex":0.0000035499502,"about_ca_system_score_gemma":0.0011771471,"threshold_uncertainty_score":0.5456988},"labels":[],"label_agreement":null},{"id":"W2785497349","doi":"10.1139/cjes-2017-0273","title":"The first record of dinosaur eggshell from the Horseshoe Canyon Formation (Maastrichtian) of Alberta, Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Dinosaur Research Institute; Alberta Innovates; Alberta Historical Resources Foundation","keywords":"Canyon; Eggshell; Horseshoe (symbol); Geology; Cretaceous; Paleontology; Prospecting; Geochemistry; Geomorphology","score_opus":0.013195857414957162,"score_gpt":0.18870307498358113,"score_spread":0.17550721756862397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2785497349","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98714197,0.0017701443,0.000014562002,0.0043609845,0.0013795113,0.000052917916,0.000091638634,5.997448e-7,0.0051876795],"genre_scores_gemma":[0.9992957,0.00006092202,0.0000956079,0.00029601168,0.00017865706,1.0360997e-7,0.0000042316083,6.0217263e-7,0.00006817783],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989696,0.0000971545,0.00036466625,0.000086206186,0.00019349727,0.00028887167],"domain_scores_gemma":[0.9985305,0.00062756514,0.00038964138,0.000110765184,0.00015965854,0.00018185112],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058989506,0.000071878814,0.0001410096,0.00006873717,0.0007526523,0.000021426302,0.00063255563,0.0000472628,0.0006386964],"category_scores_gemma":[0.00027729865,0.00003770856,0.00004442587,0.00031775836,0.0013559678,0.00022825216,0.0000041213757,0.00011581358,0.000008221158],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015881817,0.0000010073161,0.9917671,0.0000014586329,0.000012538992,0.000003718966,0.00034484363,0.000143281,0.0000035623768,0.00006287717,0.0035373685,0.004106343],"study_design_scores_gemma":[0.00007354675,0.00026187336,0.9228849,0.000021770558,0.000010415172,0.000041347983,0.00069702516,0.0007584156,0.00007747251,0.00034272828,0.074783415,0.00004709341],"about_ca_topic_score_codex":0.9748037,"about_ca_topic_score_gemma":0.9999699,"teacher_disagreement_score":0.07124604,"about_ca_system_score_codex":0.000003893658,"about_ca_system_score_gemma":0.0027261565,"threshold_uncertainty_score":0.69932777},"labels":[],"label_agreement":null},{"id":"W2786725920","doi":"10.1139/cjes-2017-0167","title":"Temporal and spatial evolution of Northern Cascade Arc magmatism revealed by LA–ICP–MS U–Pb zircon dating","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Agence Nationale de la Recherche","keywords":"Batholith; Geology; Magmatism; Zircon; Pluton; Geochemistry; Caldera; Volcano; Paleontology; Tectonics","score_opus":0.010754265963443385,"score_gpt":0.19216863558157574,"score_spread":0.18141436961813234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2786725920","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943953,0.0009865726,0.0005273435,0.00062915037,0.00010052364,0.000034641555,0.000039617833,0.0000023184978,0.0032845119],"genre_scores_gemma":[0.99797535,0.000012479922,0.0017268045,0.000085004394,0.00012637548,6.306042e-8,0.000005209014,8.999919e-7,0.00006784045],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988803,0.0000918046,0.0003321794,0.00015413866,0.00025852805,0.0002830053],"domain_scores_gemma":[0.9989835,0.000107842105,0.00027148123,0.00006125754,0.00013214431,0.00044377518],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007812451,0.00008877772,0.00020349,0.00015257706,0.00026864107,0.00006757261,0.00025421203,0.000053980588,0.002556819],"category_scores_gemma":[0.00023133076,0.000060238697,0.000055312445,0.00036051014,0.0010903912,0.00023160715,0.0000064856254,0.00012761595,0.000016044718],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000052218234,0.0000026792081,0.9907442,0.0000049480236,0.000008940093,0.000010521418,0.000114188806,0.000081933336,0.0012456842,0.000018443305,0.00013416502,0.0076290923],"study_design_scores_gemma":[0.00017064523,0.00048343596,0.9873405,0.00005236103,0.00002343081,0.00010421734,0.0002753864,0.0036978784,0.0013020007,0.0045072604,0.0019156936,0.00012720353],"about_ca_topic_score_codex":0.24472888,"about_ca_topic_score_gemma":0.84188664,"teacher_disagreement_score":0.5971578,"about_ca_system_score_codex":0.0000019674953,"about_ca_system_score_gemma":0.00036172962,"threshold_uncertainty_score":0.998355},"labels":[],"label_agreement":null},{"id":"W2787306563","doi":"10.1139/cjes-2017-0129","title":"Déformations tardi-grenvilliennes dans la ceinture parautochtone (Province de Grenville centrale) : contraintes géochronologiques par couplage de méthodes U–Pb de haute résolution spatiale et de haute précision","year":2018,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec); Université du Québec à Montréal; Polytechnique Montréal","funders":"Ministère de l'Énergie et des Ressources Naturelles","keywords":"Geology; Humanities; Geomorphology; Philosophy","score_opus":0.017442498574328728,"score_gpt":0.23431492203896956,"score_spread":0.21687242346464083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2787306563","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.947055,0.0062633855,0.03193165,0.011045557,0.00038733167,0.0001444355,0.0002735016,0.0000182874,0.0028808767],"genre_scores_gemma":[0.9564222,0.0018863655,0.039861564,0.0011477274,0.00039469753,0.0000013095726,0.000020515876,0.000004938578,0.00026068618],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99595463,0.0011197268,0.00064897205,0.00036419596,0.00037056042,0.001541885],"domain_scores_gemma":[0.99668235,0.0008262979,0.00050907076,0.00018680662,0.00024766795,0.0015478217],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0053623165,0.00030469513,0.00047738594,0.00028762722,0.0010974148,0.00043375551,0.0008239871,0.00037042555,0.0036357485],"category_scores_gemma":[0.0018843183,0.00023603125,0.00026447096,0.00065360504,0.0037532686,0.00072481146,0.000027971539,0.0006723981,0.00005782361],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034487046,0.00006748317,0.9185349,0.000052757103,0.000106742445,0.0004289007,0.004137671,0.056378614,0.0042410158,0.0049844184,0.0018420737,0.009190969],"study_design_scores_gemma":[0.0003251146,0.0010214683,0.8313646,0.0003680834,0.0001660092,0.0012672504,0.001701475,0.1082875,0.006337867,0.023851987,0.024866067,0.00044257857],"about_ca_topic_score_codex":0.09458615,"about_ca_topic_score_gemma":0.6698164,"teacher_disagreement_score":0.57523024,"about_ca_system_score_codex":0.00007161531,"about_ca_system_score_gemma":0.005185249,"threshold_uncertainty_score":0.99895793},"labels":[],"label_agreement":null},{"id":"W2787618982","doi":"10.1139/cjes-2017-0208","title":"On estimation of stopping criteria for iterative solutions of gravity downward continuation","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Grantová Agentura České Republiky; Západočeská Univerzita v Plzni","keywords":"Tikhonov regularization; Regularization (linguistics); Conjugate gradient method; Geoid; Mathematics; Continuation; Applied mathematics; Iterative method; Inverse problem; Mathematical optimization; Algorithm; Computer science; Geology; Mathematical analysis; Geophysics","score_opus":0.06488001230493348,"score_gpt":0.2780663105040435,"score_spread":0.21318629819911003,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2787618982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99487853,0.00006331704,0.0033920112,0.0001773239,0.00050114584,0.00010230177,0.00012879724,8.2493284e-7,0.0007557676],"genre_scores_gemma":[0.9969662,8.3023065e-7,0.0029060072,0.00004195987,0.00006361141,1.5262243e-7,0.000005874401,6.8086297e-7,0.000014686242],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992189,0.000046847337,0.000252715,0.00007895077,0.00022956639,0.00017304743],"domain_scores_gemma":[0.9989917,0.00007432703,0.00030199988,0.000051982355,0.00043676473,0.0001432226],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010653612,0.000053392152,0.00013371596,0.00021022686,0.0002849032,0.000046722955,0.0001485485,0.000021425245,0.00016556491],"category_scores_gemma":[0.00027306934,0.00004273591,0.000053653574,0.00023462315,0.00037288526,0.0002787347,0.0000013488108,0.00004109009,0.0000039016736],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031185008,0.00012817596,0.7063996,0.00017768935,0.0001551519,0.000009073035,0.013438383,0.05225202,0.010939475,0.026243018,0.0026519676,0.18729356],"study_design_scores_gemma":[0.0003825856,0.0023099862,0.9399675,0.0002069984,0.000025074105,0.000006195625,0.00031282566,0.024906274,0.003590108,0.027784703,0.00039296565,0.00011478356],"about_ca_topic_score_codex":0.005077517,"about_ca_topic_score_gemma":0.07636286,"teacher_disagreement_score":0.23356786,"about_ca_system_score_codex":0.0000015301696,"about_ca_system_score_gemma":0.0005169902,"threshold_uncertainty_score":0.9404911},"labels":[],"label_agreement":null},{"id":"W2788553056","doi":"10.1139/cjes-2017-0205","title":"Correlation of the Aptian Naskapi Member of the Scotian Basin and its regional implications","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada; Natural Resources Canada; Saint Mary's University","funders":"","keywords":"Geology; Aptian; Sedimentary depositional environment; Canyon; Geochemistry; Paleontology; Structural basin; Tectonics; Deposition (geology); Sediment; Geomorphology","score_opus":0.03301342909452394,"score_gpt":0.23118908677619807,"score_spread":0.1981756576816741,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2788553056","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9801051,0.002034031,0.000009083619,0.002960978,0.0004726584,0.00006177386,0.000027982791,6.577909e-7,0.014327734],"genre_scores_gemma":[0.99965006,0.000011700928,0.0001388386,0.000107833315,0.000052141142,5.4205138e-8,1.5597469e-7,2.7526e-7,0.000038947113],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99928904,0.00008799479,0.00022035916,0.0000797159,0.0001721546,0.00015073737],"domain_scores_gemma":[0.9992343,0.000090308204,0.00028762862,0.00009259487,0.00013703223,0.00015813737],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004945102,0.00005162923,0.00009664804,0.00010338746,0.0005168954,0.00002239177,0.0003900096,0.000041674975,0.00018918597],"category_scores_gemma":[0.00009990811,0.00002778632,0.000063611646,0.00041883462,0.0017216271,0.00020348871,0.0000013568193,0.00010087546,0.0000012460685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026780742,0.0000014125893,0.9957452,0.000002086259,0.0000067449582,3.1676316e-7,0.00044487364,0.00007054354,0.000053296837,0.0010292737,0.00013519416,0.002508422],"study_design_scores_gemma":[0.000060750575,0.00009508807,0.99713564,0.0000416489,0.000010380124,0.000086327695,0.00021938393,0.00039673055,0.00023679658,0.001177996,0.0005058625,0.000033413424],"about_ca_topic_score_codex":0.0043787593,"about_ca_topic_score_gemma":0.5192622,"teacher_disagreement_score":0.51488346,"about_ca_system_score_codex":5.099322e-7,"about_ca_system_score_gemma":0.00089096563,"threshold_uncertainty_score":0.66194034},"labels":[],"label_agreement":null},{"id":"W2789822966","doi":"10.1139/cjes-2017-0260","title":"Geochronology, geochemistry, and tectonic implications of upper Silurian – Lower Devonian meta-sedimentary rocks from the Jiangyu Group in eastern Jilin Province, Northeast China","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Northwest University; Ministry of Land and Resources of the People's Republic of China; National Natural Science Foundation of China","keywords":"Geology; Zircon; Protolith; Devonian; Craton; Geochemistry; Geochronology; Sedimentary rock; Provenance; Paleozoic; Gondwana; Continental arc; Paleontology; Subduction; Tectonics","score_opus":0.014196000706849295,"score_gpt":0.20169507475880136,"score_spread":0.18749907405195207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2789822966","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9890674,0.0026544502,0.000017918284,0.006269276,0.00009901041,0.00007745926,0.00014369658,0.0000023737352,0.0016684347],"genre_scores_gemma":[0.9988582,0.000020843354,0.00052260875,0.00041199187,0.00013647504,6.826111e-7,0.00001358174,0.0000013361416,0.000034245193],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986948,0.00007381758,0.0003931117,0.0002574389,0.00019045532,0.0003903891],"domain_scores_gemma":[0.99901557,0.00013604504,0.00022181582,0.00016440231,0.00008021527,0.000381942],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00051788834,0.00013924576,0.00030020918,0.0001380018,0.0003116663,0.00006670667,0.0005959502,0.00006721832,0.008236368],"category_scores_gemma":[0.00009553003,0.00007797194,0.00012747738,0.00047562804,0.0015321475,0.00019177163,0.00002013329,0.00021168338,0.000019156423],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009378338,0.000010121537,0.9969793,0.0000020949701,0.00006632704,0.000008730876,0.00010559823,0.000085438674,0.00010098011,0.00001359414,0.00004543844,0.0025730296],"study_design_scores_gemma":[0.0001412276,0.00026239018,0.9918213,0.000018117264,0.00009858329,0.000040613886,0.00018900662,0.0005950724,0.0002318685,0.0047306283,0.0017680586,0.00010312756],"about_ca_topic_score_codex":0.1892445,"about_ca_topic_score_gemma":0.88030076,"teacher_disagreement_score":0.69105625,"about_ca_system_score_codex":0.0000026645346,"about_ca_system_score_gemma":0.00047995258,"threshold_uncertainty_score":0.99267024},"labels":[],"label_agreement":null},{"id":"W2789887662","doi":"10.1139/cjes-2017-0149","title":"Biogeochemistry of U, Ni, and As in two meromictic pit lakes at the Cluff Lake uranium mine, northern Saskatchewan","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Mine drainage and remediation techniques","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta; Areva","keywords":"Chemocline; Water column; Anoxic waters; Environmental chemistry; Geology; Sulfide; Uranium; Halite; Hydrology (agriculture); Oceanography; Chemistry; Geomorphology","score_opus":0.007163994263247773,"score_gpt":0.22331504269031344,"score_spread":0.21615104842706567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2789887662","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923294,0.00020514813,0.0000039891406,0.00095943466,0.00008240079,0.000051953903,0.000008063555,0.0000018050133,0.0063577592],"genre_scores_gemma":[0.9989086,0.000015055288,0.00019776764,0.00018277211,0.000062923675,5.608823e-7,5.443292e-7,0.0000026456323,0.0006291799],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992118,0.000031558764,0.00022684524,0.0001171172,0.00021201393,0.00020066206],"domain_scores_gemma":[0.99946505,0.00003998214,0.0001771781,0.00009505232,0.00002907672,0.00019364695],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00066939363,0.00007038224,0.000108597524,0.000081949394,0.00018549975,0.000031761163,0.00029513196,0.000027081627,0.0013589268],"category_scores_gemma":[0.000091761365,0.000045188146,0.000030889354,0.00030988353,0.0015537038,0.00015471935,0.000030284222,0.00008110576,0.000017664683],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006574637,0.000008897168,0.95150065,0.000004716984,0.000005079106,0.000025424979,0.003528664,0.000026020401,0.042727366,0.000011655155,0.00073948724,0.0014154328],"study_design_scores_gemma":[0.0009466899,0.00094699743,0.58718044,0.00018433132,0.00004061106,0.00061902084,0.008950848,0.0002599127,0.35779983,0.0029005841,0.03967599,0.000494747],"about_ca_topic_score_codex":0.022017458,"about_ca_topic_score_gemma":0.9548217,"teacher_disagreement_score":0.9328042,"about_ca_system_score_codex":0.000012860422,"about_ca_system_score_gemma":0.00025021014,"threshold_uncertainty_score":0.999554},"labels":[],"label_agreement":null},{"id":"W2790473514","doi":"10.1139/cjes-2017-0223","title":"The variability of Baffin Bay seafloor sediment mineralogy: the identification of discrete glacial sediment sources and application to Late Quaternary downcore analysis","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Bengbu Medical College","keywords":"Geology; Bay; Sediment; Seafloor spreading; Bedrock; Fjord; Quaternary; Outcrop; Continental shelf; Glacial period; Oceanography; Fluvial; Geochemistry; Geomorphology; Paleontology","score_opus":0.01191729427611602,"score_gpt":0.2476803862828822,"score_spread":0.23576309200676618,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790473514","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949031,0.0003274423,0.0002623817,0.003796857,0.00018454876,0.00014383878,0.000027176759,0.0000010816793,0.0003535893],"genre_scores_gemma":[0.9996213,0.00002302812,0.00015678146,0.0000688533,0.00006503752,9.266878e-7,0.0000037353834,6.9721455e-7,0.000059646998],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99855435,0.00030733313,0.0004475339,0.00016331275,0.00027085296,0.00025660812],"domain_scores_gemma":[0.9987072,0.00035952142,0.00032890908,0.00017235207,0.0002076819,0.00022433903],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0043481425,0.00007133843,0.00017877854,0.0002310683,0.00062932906,0.000054321055,0.0004954226,0.00004579058,0.00016952038],"category_scores_gemma":[0.000174206,0.00003773238,0.000060855014,0.0007314903,0.0020097424,0.00011628946,0.00001230225,0.00010648185,0.000009618924],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028631945,0.000002812694,0.99533486,0.0000041439894,0.000057629484,0.0000011939553,0.00078044494,0.0027415422,0.0001246717,0.00011854618,0.000013885782,0.00079161377],"study_design_scores_gemma":[0.00007112937,0.00025162476,0.9896201,0.0000057453344,0.00006358909,0.000012849327,0.0003560649,0.007830381,0.0005231898,0.00086060405,0.00036124766,0.00004347371],"about_ca_topic_score_codex":0.006709536,"about_ca_topic_score_gemma":0.38274243,"teacher_disagreement_score":0.3760329,"about_ca_system_score_codex":7.837816e-7,"about_ca_system_score_gemma":0.0003818552,"threshold_uncertainty_score":0.9999049},"labels":[],"label_agreement":null},{"id":"W2790473882","doi":"10.1139/cjes-2017-0270","title":"Origin of the Piché Structural Complex and implications for the early evolution of the Archean crustal-scale Cadillac – Larder Lake Fault Zone, Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec); Université du Québec à Chicoutimi","funders":"","keywords":"Geology; Greenstone belt; Archean; Geochemistry; Ultramafic rock; Volcanic rock; Lithology; Fault (geology); Volcanic belt; Felsic; Outcrop; Volcano; Petrology; Paleontology","score_opus":0.02152265056481815,"score_gpt":0.21739094025110248,"score_spread":0.19586828968628434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790473882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896234,0.00041232124,0.00004270093,0.008872047,0.00016160673,0.00009305154,0.00026013952,6.094687e-7,0.0005340929],"genre_scores_gemma":[0.99945563,0.0000034803597,0.00021570563,0.0001653086,0.00007084833,2.2005928e-7,0.0000012321938,6.077111e-7,0.00008696061],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991899,0.000049947772,0.00022785361,0.000097047734,0.0002074388,0.00022777327],"domain_scores_gemma":[0.99908465,0.00017365336,0.00020512113,0.00012047567,0.00023771556,0.00017836172],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031669706,0.00006413849,0.00012529407,0.000038762788,0.00068817363,0.000033602137,0.000543627,0.00002417887,0.00058517786],"category_scores_gemma":[0.00013356139,0.000026176134,0.00007840257,0.00045765244,0.0015985065,0.00006744147,0.000011191827,0.00009549357,4.4582922e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000033515764,7.5366944e-7,0.99732184,0.00000266608,0.000011412873,1.05843476e-7,0.000111026115,0.00084444135,0.00010134403,0.0002634836,0.000389027,0.00095055904],"study_design_scores_gemma":[0.000067018875,0.0000636433,0.9876922,0.000008226816,0.000024325105,0.000015679763,0.0003470707,0.001870389,0.00011522955,0.0029226379,0.0068330695,0.00004054892],"about_ca_topic_score_codex":0.69091165,"about_ca_topic_score_gemma":0.9982096,"teacher_disagreement_score":0.30729795,"about_ca_system_score_codex":0.0000029129685,"about_ca_system_score_gemma":0.0011143085,"threshold_uncertainty_score":0.6407287},"labels":[],"label_agreement":null},{"id":"W2791040140","doi":"10.1139/cjes-2017-0081","title":"Stratigraphic analysis of Late Wisconsin and Holocene glaciolacustrine deposits exposed along the Nottawasaga River, southern Ontario, Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Baosteel-Australia Joint Research and Development Centre; McMaster University","keywords":"Geology; Deglaciation; Outcrop; Silt; Fluvial; Sedimentary rock; Meltwater; Geomorphology; Glacial period; Groundwater flow; Pleistocene; Groundwater; Outwash plain; Geochemistry; Structural basin; Paleontology; Aquifer","score_opus":0.02241026099597711,"score_gpt":0.21062791505209796,"score_spread":0.18821765405612084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791040140","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967426,0.0013247519,0.000003661448,0.00075134175,0.00017049939,0.000054521537,0.00003740019,0.000001134306,0.0009140679],"genre_scores_gemma":[0.99946386,0.000017738455,0.00015449805,0.00018256107,0.000029990884,7.6621745e-8,0.0000035882044,8.908805e-7,0.000146821],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986449,0.00017192056,0.00032664923,0.0001625754,0.00028077664,0.00041318292],"domain_scores_gemma":[0.9987937,0.0002571106,0.00022461406,0.000121981604,0.00018438109,0.00041820313],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010343498,0.00010311237,0.00027441597,0.00045994893,0.00062301743,0.000057012843,0.0004354852,0.000061654966,0.0012284153],"category_scores_gemma":[0.00008886476,0.00006464135,0.00006380831,0.0010521701,0.0026527226,0.00015116412,0.0000060359894,0.0002463092,0.0000040280165],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012633068,0.0000014742155,0.99769443,0.0000019151826,0.00014045276,0.00008621942,0.000980664,0.00069966604,0.000003930284,0.000016277367,0.00003125367,0.0003310954],"study_design_scores_gemma":[0.00014147075,0.00024933228,0.99773157,0.00001341919,0.00011883987,0.00011770661,0.00051180104,0.0007517153,0.00007672764,0.00009178234,0.00012154759,0.00007407791],"about_ca_topic_score_codex":0.9760026,"about_ca_topic_score_gemma":0.999992,"teacher_disagreement_score":0.023989428,"about_ca_system_score_codex":0.0000010520234,"about_ca_system_score_gemma":0.004534878,"threshold_uncertainty_score":0.9996846},"labels":[],"label_agreement":null},{"id":"W2791123016","doi":"10.1139/cjes-2017-0266","title":"The stratigraphic position and the age of the Ordovician organic-rich intervals in the northern Hudson Bay, Hudson Strait, and Foxe basins—evidence from graptolites","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"GDG Environnement; Institut National de la Recherche Scientifique; Government of Nunavut; Nunavut Research Institute","funders":"","keywords":"Geology; Bay; Ordovician; Paleontology; Structural basin; Oceanography","score_opus":0.018760155552017755,"score_gpt":0.22073070298931574,"score_spread":0.20197054743729798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791123016","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.975668,0.01590388,0.000010628922,0.006087162,0.000249208,0.000156732,0.0000361317,0.0000014403089,0.0018867776],"genre_scores_gemma":[0.99922746,0.00028746176,0.00010732807,0.00028660087,0.00008547336,3.948776e-7,4.7623723e-7,7.2442054e-7,0.0000040725267],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99824864,0.0005857368,0.0003707478,0.00016583696,0.00031811986,0.00031090845],"domain_scores_gemma":[0.99820095,0.0011005509,0.00029165545,0.00017735,0.00009539853,0.00013406295],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0024438177,0.00012271764,0.0001885097,0.00012643388,0.0012911333,0.00034575808,0.0009014616,0.000060911287,0.000056524765],"category_scores_gemma":[0.00031527987,0.00004952812,0.000073314375,0.00065644074,0.0046131406,0.00039826208,0.0000034859627,0.00029457093,6.66481e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024785391,0.000002344071,0.98596376,0.0000024471237,0.00001541298,0.000011621498,0.004049676,0.000004565944,0.00008419877,0.00037135708,0.000012220618,0.009457582],"study_design_scores_gemma":[0.0001878627,0.00030378476,0.9897336,0.00012440063,0.00002501858,0.00008854871,0.0030368727,0.00015216968,0.00006708209,0.0061234804,0.00009085921,0.000066347275],"about_ca_topic_score_codex":0.03033413,"about_ca_topic_score_gemma":0.9830301,"teacher_disagreement_score":0.95269597,"about_ca_system_score_codex":9.0590186e-7,"about_ca_system_score_gemma":0.00046751017,"threshold_uncertainty_score":0.99809575},"labels":[],"label_agreement":null},{"id":"W2792411277","doi":"10.1139/cjes-2017-0226","title":"Petrogenesis and tectonic implications of Late Jurassic – Early Cretaceous granitic magmatism in the Xing’an Block, Northeast China: geochronological, geochemical, and Hf isotopic evidence","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Institute of Geology and Geophysics, Chinese Academy of Sciences; Chinese Academy of Sciences","keywords":"Geology; Zircon; Geochemistry; Petrogenesis; Magmatism; Diorite; Partial melting; Geochronology; Continental arc; Cretaceous; Magma; Petrology; Mantle (geology); Tectonics; Paleontology","score_opus":0.022423336206165136,"score_gpt":0.22159143491845737,"score_spread":0.19916809871229224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2792411277","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929938,0.0037600796,0.000004841978,0.0027410956,0.00003525998,0.00007439234,0.000022325698,0.000002852488,0.00036537647],"genre_scores_gemma":[0.99919486,0.00019475899,0.00035950658,0.00018596782,0.000054047207,6.5259263e-7,0.0000013827608,0.0000010043509,0.000007829515],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99877393,0.00010697481,0.00033574842,0.00022508824,0.00020160853,0.00035664617],"domain_scores_gemma":[0.9990025,0.0002360885,0.00017866868,0.0001340463,0.000102467224,0.0003462333],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007029992,0.000115784984,0.0002341941,0.00019416853,0.00039994373,0.0001353938,0.00048568554,0.000057078047,0.0006770917],"category_scores_gemma":[0.00026927952,0.000066505,0.000054893037,0.0006196298,0.0018603939,0.0002856743,0.000011996487,0.00017643513,0.0000058824735],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004284306,0.000007272929,0.99435663,0.000006491332,0.0000074377317,0.0000137843135,0.0003108186,0.000047602425,0.00048940524,0.000059691676,0.0000044519848,0.004692143],"study_design_scores_gemma":[0.00007952946,0.0005737304,0.9908914,0.000046539815,0.000029789075,0.000189709,0.00015391246,0.00043015502,0.00015173158,0.0072782338,0.00008479544,0.00009044844],"about_ca_topic_score_codex":0.021068567,"about_ca_topic_score_gemma":0.3564949,"teacher_disagreement_score":0.33542633,"about_ca_system_score_codex":0.0000015180575,"about_ca_system_score_gemma":0.00022794954,"threshold_uncertainty_score":0.9854502},"labels":[],"label_agreement":null},{"id":"W2792462953","doi":"10.1139/cjes-2017-0170","title":"Palynomorphs from a lacustrine sequence provide evidence for palaeoenvironmental changes during the early Miocene in Central Anatolia, Turkey","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Vegetation (pathology); Deciduous; Mediterranean climate; Paleontology; Late Miocene; Range (aeronautics); Physical geography; Geography; Ecology; Structural basin; Archaeology","score_opus":0.06569133848599588,"score_gpt":0.22157644837693236,"score_spread":0.15588510989093646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2792462953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959469,0.00036327273,0.0000011044333,0.0031728337,0.00020892391,0.00011989369,0.00016055236,0.0000023355099,0.0000241823],"genre_scores_gemma":[0.99929696,0.00006238006,0.000094567586,0.00013746001,0.00035022834,0.0000011247657,0.000003021313,3.1342591e-7,0.000053947064],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990768,0.000048597292,0.00014379108,0.00015351489,0.00018277533,0.0003945131],"domain_scores_gemma":[0.9994073,0.00015388068,0.0001277199,0.00002755226,0.000037907193,0.00024563842],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037836493,0.00007563439,0.000104972816,0.000037504735,0.0005244846,0.00010647075,0.00044058764,0.000039067963,0.00017733569],"category_scores_gemma":[0.0001226568,0.000029890642,0.000044574135,0.0002814061,0.0004983678,0.00037201846,0.000019045376,0.00009375932,0.000007157798],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004784372,0.000007162786,0.963489,0.000002468162,0.0000060634266,0.000040117007,0.000452721,0.000038713933,0.033238262,0.000018289424,0.0001303306,0.0025290134],"study_design_scores_gemma":[0.00011110058,0.00032207087,0.9927653,0.00009790665,0.000006450564,0.000028329068,0.0005278507,0.00014991406,0.0032488722,0.00010407522,0.0025601543,0.00007799131],"about_ca_topic_score_codex":0.044114854,"about_ca_topic_score_gemma":0.5611139,"teacher_disagreement_score":0.516999,"about_ca_system_score_codex":0.000026529919,"about_ca_system_score_gemma":0.00011639972,"threshold_uncertainty_score":0.9622505},"labels":[],"label_agreement":null},{"id":"W2794107568","doi":"10.1139/cjes-2017-0197","title":"The Geon 14 arc-related mafic rocks from the central Grenville Province","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Memorial University of Newfoundland; Strong","keywords":"Mafic; Geology; Laurentia; Geochemistry; Continental arc; Gneiss; Rodinia; Metamorphism; Archean; Granulite; Back-arc basin; Geochronology; Petrology; Craton; Metamorphic rock; Subduction; Volcanic rock; Ordovician; Geomorphology; Tectonics; Paleontology; Facies; Structural basin","score_opus":0.010016962203975363,"score_gpt":0.16964541719862514,"score_spread":0.15962845499464978,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794107568","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98172826,0.0026589339,0.000012799475,0.008056623,0.00061906176,0.000051545492,0.000030840063,0.0000031699087,0.0068387766],"genre_scores_gemma":[0.9985785,0.000046189216,0.00009971043,0.0005870759,0.00031273728,8.623347e-8,0.0000032335156,8.426533e-7,0.00037161517],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851304,0.00010491343,0.00029810154,0.00016986948,0.00034043958,0.00057364383],"domain_scores_gemma":[0.9986865,0.00034580112,0.00018600003,0.00013024642,0.00011290247,0.0005385533],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007140363,0.000101364625,0.00013549443,0.000050827937,0.0014660708,0.0002706838,0.0009413904,0.000047230267,0.007818343],"category_scores_gemma":[0.0003242338,0.0000424657,0.00011177157,0.00048402787,0.0017564782,0.00013952883,0.000009884145,0.00023217559,0.00018947366],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007956739,0.0000022171248,0.9857768,3.822595e-7,0.000021812131,0.000024080458,0.00016675449,0.0005836472,0.000019842448,0.000084558385,0.0010049867,0.012307007],"study_design_scores_gemma":[0.000085965534,0.00022190312,0.9380453,0.000014988654,0.000020980293,0.00003381314,0.00035142055,0.0023037314,0.00011626099,0.01290508,0.045806926,0.00009358666],"about_ca_topic_score_codex":0.10473231,"about_ca_topic_score_gemma":0.8879915,"teacher_disagreement_score":0.7832592,"about_ca_system_score_codex":0.0000016454661,"about_ca_system_score_gemma":0.000651116,"threshold_uncertainty_score":0.9998339},"labels":[],"label_agreement":null},{"id":"W2794128397","doi":"10.1139/cjes-2017-0178","title":"Geochronology and geochemistry of the Cuihongshan Fe-polymetallic deposit, northeastern China: implications for ore genesis and tectonic setting","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochronology; Geochemistry; Zircon; Skarn; Isochron; Molybdenite; Mineralization (soil science); Radiometric dating; Metallogeny; Isochron dating; Hydrothermal circulation; Fluid inclusions; Sphalerite; Paleontology; Pyrite","score_opus":0.011720809692782039,"score_gpt":0.20220537056987634,"score_spread":0.1904845608770943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794128397","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939216,0.0027256587,0.000033473323,0.0027176172,0.000057944573,0.00005456784,0.000052134037,0.000001653176,0.00043538748],"genre_scores_gemma":[0.9989997,0.000027453787,0.00073558843,0.00012176382,0.00008213724,3.8518348e-7,0.0000021704766,9.084905e-7,0.00002987369],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99923575,0.000026800451,0.00022387692,0.00016006565,0.0000841976,0.0002693061],"domain_scores_gemma":[0.999259,0.00009106831,0.00018950201,0.00008833146,0.00009970251,0.00027240027],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028226833,0.000081027654,0.00016205045,0.00007750606,0.00050636777,0.000053373074,0.0003071644,0.00004544996,0.00035072825],"category_scores_gemma":[0.00014783372,0.00004692565,0.00006952682,0.00029502803,0.0011887096,0.00009275837,0.0000137182815,0.00007593932,0.0000012525005],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000025166657,0.0000018389934,0.9887224,0.000008421649,0.00001545678,6.817788e-7,0.00007081167,0.000028728988,0.001581059,0.000025944095,0.000008925743,0.0095332395],"study_design_scores_gemma":[0.00008126804,0.00015673935,0.9922225,0.000018202812,0.0000391424,0.00014993834,0.000097851305,0.0011315225,0.002522447,0.003267859,0.00024779045,0.000064739244],"about_ca_topic_score_codex":0.015462164,"about_ca_topic_score_gemma":0.31268102,"teacher_disagreement_score":0.29721886,"about_ca_system_score_codex":8.222837e-7,"about_ca_system_score_gemma":0.00024995566,"threshold_uncertainty_score":0.99109393},"labels":[],"label_agreement":null},{"id":"W2796124521","doi":"10.1139/cjes-2019-0223","title":"Sequence stratigraphy of the late Carboniferous Clifton Formation, New Brunswick","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; University of New Brunswick","funders":"","keywords":"Cyclothems; Geology; Pennsylvanian; Carboniferous; Paleontology; Transgressive; Sequence stratigraphy; Sequence (biology); Stratigraphic unit; Cyclostratigraphy; Structural basin; Interglacial; Westphalian sovereignty; Sedimentary depositional environment; Quaternary","score_opus":0.04163889919053037,"score_gpt":0.21316543178768327,"score_spread":0.1715265325971529,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2796124521","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9878273,0.0011913155,0.000111912006,0.0049629775,0.00020377571,0.00005728174,0.000015783538,0.0000027736367,0.0056268675],"genre_scores_gemma":[0.9984806,0.000037623435,0.00059538987,0.00078660075,0.000054495453,1.840232e-8,0.000001024237,5.126016e-7,0.000043694825],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99913615,0.00004117801,0.00031504285,0.000060414688,0.00024478772,0.00020245508],"domain_scores_gemma":[0.99907047,0.00004711987,0.00025993935,0.000055256372,0.00010972557,0.0004574979],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029304886,0.00006480317,0.00011558509,0.00008481369,0.00027430314,0.0000940682,0.00050850294,0.00003066355,0.00068678806],"category_scores_gemma":[0.0001503499,0.000036378453,0.000066560526,0.0007932907,0.00034247382,0.00060052867,0.000003034516,0.000124449,0.0000123820755],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000047918866,0.0000012805688,0.9795854,0.000017908053,0.000005978489,0.0000056636827,0.0014163471,0.013743813,0.000037741556,0.001077569,0.00025632494,0.0038471895],"study_design_scores_gemma":[0.00013138713,0.0004971311,0.98063207,0.000049003305,0.0000124295075,0.00007481792,0.0007274942,0.0043210774,0.000543336,0.005020082,0.007882275,0.00010891552],"about_ca_topic_score_codex":0.02867802,"about_ca_topic_score_gemma":0.41933164,"teacher_disagreement_score":0.3906536,"about_ca_system_score_codex":4.916117e-7,"about_ca_system_score_gemma":0.0027330755,"threshold_uncertainty_score":0.9777901},"labels":[],"label_agreement":null},{"id":"W2796715589","doi":"10.1139/cjes-2018-0038","title":"Geology, geochemistry, and geochronology of the Laozuoshan gold deposit, Heilongjiang Province, Northeast China: implications for multiple gold mineralization events and geodynamic setting","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geochronology; Geology; Diorite; Zircon; Geochemistry; Sericite; Massif; Mineralization (soil science); Subduction; Cretaceous; Hydrothermal circulation; Paleontology; Tectonics; Soil water","score_opus":0.008905143932902888,"score_gpt":0.20008921814615796,"score_spread":0.19118407421325506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2796715589","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957939,0.000721842,0.00008939734,0.0026968939,0.00007611826,0.0001101796,0.00007919091,0.0000022932531,0.00043021943],"genre_scores_gemma":[0.99864745,0.00002055695,0.0010339987,0.00012343684,0.00008194874,6.5812327e-7,0.000011760502,0.0000011755747,0.000078997706],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99912167,0.000040365423,0.00026977283,0.00018707316,0.00008533043,0.0002957872],"domain_scores_gemma":[0.9991794,0.00010514721,0.0002487263,0.00008988824,0.0001383171,0.00023848121],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032591217,0.00009314035,0.0001674144,0.00009312882,0.00034488505,0.000034471665,0.0002901145,0.00006103948,0.00010268773],"category_scores_gemma":[0.0002741225,0.000058248785,0.000057412817,0.00027264154,0.0010322917,0.00012828277,0.000017732289,0.00008559498,8.997838e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004888868,0.0000035869753,0.995989,0.000011276437,0.000011968154,6.461918e-7,0.000042287407,0.00019432316,0.0005807791,0.0000656362,0.00003594471,0.0030596338],"study_design_scores_gemma":[0.00015072298,0.00017513201,0.98571604,0.000022879543,0.000025144653,0.000104152896,0.000057840673,0.009967178,0.00023662862,0.0032382903,0.00023264515,0.00007336011],"about_ca_topic_score_codex":0.030778147,"about_ca_topic_score_gemma":0.69324744,"teacher_disagreement_score":0.6624693,"about_ca_system_score_codex":0.0000016969065,"about_ca_system_score_gemma":0.00024922146,"threshold_uncertainty_score":0.975676},"labels":[],"label_agreement":null},{"id":"W2796986408","doi":"10.1139/cjes-2017-0196","title":"U–Pb (zircon) ages and provenance of the White Rock Formation of the Rockville Notch Group, Meguma terrane, Nova Scotia, Canada: evidence for the “Sardian gap” and West African origin","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University; Nova Scotia Department of Energy; Technical University of Nova Scotia","funders":"Northwestern University","keywords":"Terrane; Geology; Zircon; Felsic; Geochemistry; Ordovician; Provenance; Mafic; Plutonism; Devonian; Paleozoic; Paleontology; Pluton","score_opus":0.03702568175645161,"score_gpt":0.21602880051421705,"score_spread":0.17900311875776545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2796986408","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9839877,0.0022068345,0.00011120564,0.012565964,0.0002888372,0.00018248362,0.00006183977,8.334638e-7,0.00059429655],"genre_scores_gemma":[0.9992153,0.000034128054,0.00025734326,0.0003569883,0.0000772682,3.0446813e-7,5.3281235e-7,8.606237e-7,0.000057258178],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989223,0.00006169895,0.00030441658,0.00013076885,0.00031299394,0.00026785687],"domain_scores_gemma":[0.99886626,0.00027361506,0.0003518268,0.00012529404,0.00018417292,0.00019882018],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00067047664,0.00009193222,0.00018553363,0.00005629804,0.0004930596,0.00006313171,0.0005576985,0.000028972021,0.00027439755],"category_scores_gemma":[0.00041138296,0.000038611088,0.00007234525,0.00053779857,0.00090107304,0.00029285028,0.000016947877,0.00010504424,7.9202624e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000141667215,0.000002555986,0.9946112,0.00002808115,0.00001642003,0.0000010361703,0.0005056367,0.00085843675,0.0004447953,0.000088595174,0.00047330972,0.0029557736],"study_design_scores_gemma":[0.00010499172,0.00021268084,0.9909636,0.00013332168,0.00004225917,0.000040953706,0.0006987099,0.0028511537,0.0016859991,0.0008885984,0.002300287,0.00007747867],"about_ca_topic_score_codex":0.5971411,"about_ca_topic_score_gemma":0.9965743,"teacher_disagreement_score":0.39943323,"about_ca_system_score_codex":0.000003167431,"about_ca_system_score_gemma":0.0006611697,"threshold_uncertainty_score":0.40554163},"labels":[],"label_agreement":null},{"id":"W2797512617","doi":"10.1139/cjes-2017-0277","title":"Surface-wave images of western Canada: lithospheric variations across the Cordillera–craton boundary","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; University of Manitoba","funders":"","keywords":"Geology; Craton; Lithosphere; Asthenosphere; Mantle (geology); Seismology; Archean; Low-velocity zone; Geophysics; Slab; Paleontology; Tectonics","score_opus":0.017931920173655403,"score_gpt":0.22092494760656003,"score_spread":0.20299302743290462,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2797512617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935993,0.0006960364,0.000039434486,0.00088474475,0.0017353249,0.00007241784,0.00032639896,0.0000020563982,0.0026442683],"genre_scores_gemma":[0.99866986,0.000019295241,0.0004993132,0.00024794685,0.00031072582,8.951337e-8,0.000002644543,0.0000021610674,0.0002479725],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986363,0.000100622296,0.00034378452,0.00013020264,0.00037793466,0.00041113736],"domain_scores_gemma":[0.998766,0.00012938527,0.00032275825,0.0001435564,0.00029994422,0.00033837993],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009114759,0.00010314259,0.00021486907,0.000033114997,0.0008968038,0.00029985473,0.00047562894,0.000031660245,0.0019814437],"category_scores_gemma":[0.00008148565,0.00006432133,0.000045236786,0.00040626508,0.00097094756,0.0003344559,0.000008999209,0.00009633458,0.00001477275],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026671303,0.000012698949,0.9785436,0.000025605716,0.000108317705,0.000120687444,0.003771279,0.003952381,0.001062854,0.00020932055,0.00609882,0.0060677826],"study_design_scores_gemma":[0.00010524698,0.00027479682,0.9670214,0.000035619414,0.000016775935,0.000049622147,0.0005299544,0.00031696225,0.0014941801,0.00024161336,0.029796548,0.00011730291],"about_ca_topic_score_codex":0.8540863,"about_ca_topic_score_gemma":0.994103,"teacher_disagreement_score":0.14001672,"about_ca_system_score_codex":0.0000027839708,"about_ca_system_score_gemma":0.0050562373,"threshold_uncertainty_score":0.9989309},"labels":[],"label_agreement":null},{"id":"W2799459395","doi":"10.1139/cjes-2018-0007","title":"Detrital zircon U–Pb dating of Late Triassic Wenbinshan Formation in southwestern Fujian, South China, and its geological significance","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Zircon; Geology; Provenance; Paleozoic; Geochemistry; Sedimentary rock; Mesozoic; Volcanic rock; Paleontology; Structural basin; Volcano","score_opus":0.029806046607652226,"score_gpt":0.2092757374716115,"score_spread":0.17946969086395925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2799459395","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976918,0.00051855715,0.00009280105,0.00035523297,0.000098950564,0.00005632996,0.000028809249,0.0000023856774,0.001155102],"genre_scores_gemma":[0.99909776,0.000012809634,0.0006830909,0.00007960078,0.000085295236,1.3291638e-7,0.000003479873,7.2109714e-7,0.000037102476],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987369,0.00008499391,0.00043672824,0.00016712335,0.0002263162,0.00034791647],"domain_scores_gemma":[0.99906623,0.000095919284,0.00031110152,0.00005178735,0.00009947392,0.000375505],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00083310576,0.000098035525,0.00024798806,0.00029548744,0.00019579074,0.000074175754,0.00028581673,0.000059637925,0.0017928283],"category_scores_gemma":[0.00032025002,0.00006451712,0.000057401085,0.00065585796,0.000561511,0.000546001,0.000008896565,0.00015591338,0.00002276459],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001825599,0.0000049905284,0.99302745,0.000009327186,0.0000061318988,0.000032411474,0.00070905517,0.00085298857,0.0018352314,0.00005204546,0.0000041236217,0.0034479748],"study_design_scores_gemma":[0.00029023472,0.0006321335,0.98419225,0.000053689997,0.0000127249605,0.000045551536,0.0005296217,0.0077851308,0.003153416,0.0031222936,0.00006125894,0.00012170112],"about_ca_topic_score_codex":0.0062320544,"about_ca_topic_score_gemma":0.25365132,"teacher_disagreement_score":0.24741927,"about_ca_system_score_codex":0.0000014132462,"about_ca_system_score_gemma":0.00016593587,"threshold_uncertainty_score":0.99911964},"labels":[],"label_agreement":null},{"id":"W2799905322","doi":"10.1139/cjes-2017-0185","title":"The Ferguson Lake deposit: an example of Ni–Cu–Co–PGE mineralization emplaced in a back-arc basin setting?","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Northwest Territories; Government of Newfoundland and Labrador; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Ultramafic rock; Archean; Greenstone belt; Mafic; Basalt; Rift; Gabbro; Structural basin; Proterozoic; Tectonics; Igneous rock; Geomorphology; Paleontology","score_opus":0.025009144884891168,"score_gpt":0.2192291439091039,"score_spread":0.19421999902421272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2799905322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951095,0.0002881427,0.00003324279,0.0011546868,0.00015625318,0.000046012352,0.000018250703,0.0000018559284,0.0031920332],"genre_scores_gemma":[0.9986359,0.00001590094,0.0007681871,0.00027697854,0.00011073818,1.1194479e-7,0.0000090557105,0.0000010246875,0.00018211683],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986054,0.00015769737,0.00038501728,0.00017194705,0.00028936283,0.00039059832],"domain_scores_gemma":[0.9989625,0.00014682293,0.00021019629,0.00010646203,0.00016086527,0.0004131225],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012829787,0.00009289731,0.00018224616,0.00020469003,0.0003810235,0.00012780358,0.00048455602,0.00004775176,0.00373633],"category_scores_gemma":[0.00021768217,0.000053765467,0.00006247373,0.00081407116,0.000602504,0.00029163697,0.0000048128336,0.0001136782,0.000032475113],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012054434,0.0000047070507,0.99630463,0.0000023670084,0.000005176491,0.0000096689955,0.0002625708,0.00055400917,0.0001304836,0.0000488402,0.00020950017,0.002455983],"study_design_scores_gemma":[0.0001293558,0.0004592058,0.9889037,0.000024743718,0.000007519235,0.000033698096,0.00026384156,0.00447216,0.00037287653,0.0015004649,0.003742461,0.00008999136],"about_ca_topic_score_codex":0.37176448,"about_ca_topic_score_gemma":0.9920826,"teacher_disagreement_score":0.6203181,"about_ca_system_score_codex":0.000002151217,"about_ca_system_score_gemma":0.0003403102,"threshold_uncertainty_score":0.9971744},"labels":[],"label_agreement":null},{"id":"W2800453510","doi":"10.1139/cjes-2018-0019","title":"Volcaniclastic lithostratigraphy and paleoenvironment of the lower Eocene McAbee fossil beds, Kamloops Group, British Columbia, Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; Brandon University","funders":"Natural Sciences and Engineering Research Council of Canada; Society for Sedimentary Geology; Paleontological Society","keywords":"Taphonomy; Geology; Paleontology; Sedimentary depositional environment; Facies; Pyroclastic rock; Lithology; Lithostratigraphy; Trace fossil; Biostratigraphy; Bioturbation; Sedimentary rock; Volcano; Sediment","score_opus":0.009403912975468574,"score_gpt":0.1802563709743872,"score_spread":0.17085245799891863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2800453510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937581,0.0030897707,0.0000023616212,0.00046290844,0.00076566817,0.00007775063,0.000057266785,9.606421e-7,0.0017852129],"genre_scores_gemma":[0.9992932,0.00006942421,0.00016461604,0.00023127967,0.00007449523,1.8167943e-7,7.7340883e-7,0.0000011855835,0.0001648479],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985986,0.00014066644,0.00028679366,0.00017255564,0.00034169914,0.00045972317],"domain_scores_gemma":[0.9989574,0.00016566495,0.0001794442,0.00011469949,0.00008666666,0.00049615174],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007149147,0.00007514582,0.00018662382,0.00007263452,0.0007908009,0.00014137446,0.0004956074,0.00006420781,0.002061716],"category_scores_gemma":[0.00014836424,0.00006839283,0.000048545953,0.00038220044,0.0030963474,0.00015816555,0.000009119312,0.00021809309,0.0000036934298],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000037546863,0.0000040124914,0.99825376,0.000005474372,0.000012720005,0.00006674508,0.000060804552,0.000018847575,0.0000026461519,0.0000066716775,0.0004900891,0.0010744932],"study_design_scores_gemma":[0.00014279377,0.00053862814,0.9956004,0.00004976044,0.000011980505,0.00051186996,0.0002068111,0.00009520898,0.000012517182,0.00026465787,0.0024870906,0.000078258076],"about_ca_topic_score_codex":0.9157348,"about_ca_topic_score_gemma":0.99994075,"teacher_disagreement_score":0.08420595,"about_ca_system_score_codex":8.2827523e-7,"about_ca_system_score_gemma":0.001802679,"threshold_uncertainty_score":0.9996167},"labels":[],"label_agreement":null},{"id":"W2801495793","doi":"10.1139/cjes-2017-0113","title":"Geological framework of the Laurentian trough aquifer system, southern Ontario","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Unconformity; Bedrock; Glacial period; Interglacial; Geomorphology; Outwash plain; Subaerial; Geochemistry; Paleontology; Structural basin","score_opus":0.027372256324739466,"score_gpt":0.23058920801122684,"score_spread":0.20321695168648737,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2801495793","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98505133,0.00049975293,0.000023706836,0.00089549465,0.001137182,0.00006057898,0.0000126077875,0.0000024710544,0.012316897],"genre_scores_gemma":[0.9984138,0.0000018955037,0.0006692082,0.00017736302,0.0001619122,9.711639e-8,6.889566e-7,9.3366566e-7,0.0005741166],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99856395,0.0002222177,0.00030121687,0.0001417003,0.00030247643,0.00046845622],"domain_scores_gemma":[0.99894613,0.00018199012,0.00020906255,0.00015173598,0.00016592951,0.0003451382],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011884742,0.00008786756,0.00020716288,0.00015987232,0.0006578386,0.000049398528,0.00087746046,0.00013755847,0.00801496],"category_scores_gemma":[0.00020771878,0.000048241964,0.00010179252,0.00041075688,0.0030391198,0.00012045149,0.0000099862455,0.00040013492,0.00019384277],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010721144,0.0000020692446,0.997821,0.000004174626,0.000012438129,0.000026724549,0.0012470761,0.000116162,8.271347e-7,0.00061551435,0.00007989182,0.00006343365],"study_design_scores_gemma":[0.00008989545,0.00035556158,0.99362826,0.00006905655,0.000012510336,0.0003754741,0.0012643827,0.00011137,0.000031189087,0.001478652,0.0025205656,0.00006308803],"about_ca_topic_score_codex":0.103746906,"about_ca_topic_score_gemma":0.98667485,"teacher_disagreement_score":0.88292795,"about_ca_system_score_codex":9.451672e-7,"about_ca_system_score_gemma":0.0019999202,"threshold_uncertainty_score":0.999674},"labels":[],"label_agreement":null},{"id":"W2802696279","doi":"10.1139/cjes-2017-0231","title":"Further studies on the 1988 <i>M</i><sub>W</sub> 5.9 Saguenay, Quebec, earthquake sequence","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Carleton University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Aftershock; Geology; Seismology; Graben; Seismometer; Sequence (biology); Focal mechanism; Foreshock; Hypocenter; Seismic moment; Induced seismicity; Fault (geology); Tectonics","score_opus":0.05448337184608769,"score_gpt":0.24795690265393325,"score_spread":0.19347353080784557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2802696279","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98035026,0.0040224767,0.0000038419157,0.0058050985,0.0017273427,0.00012227597,0.000023520117,0.000011683228,0.007933516],"genre_scores_gemma":[0.9964754,0.00026733088,0.00009062038,0.002305448,0.0006513036,6.0275266e-7,7.621519e-7,0.0000044534963,0.00020407612],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977328,0.0001896977,0.00046770874,0.00029378443,0.0005913431,0.0007246371],"domain_scores_gemma":[0.9979803,0.000618062,0.00032994553,0.00023721506,0.00035316258,0.00048130768],"candidate_categories":["sts"],"consensus_categories":["sts"],"category_scores_codex":[0.0018949176,0.00023039365,0.00031688312,0.00031631187,0.0014761256,0.00025799745,0.00074739475,0.000060107992,0.0008587859],"category_scores_gemma":[0.0006756328,0.00013016805,0.00014475109,0.0008389117,0.0032783605,0.0004176698,0.000012373672,0.00031748496,0.0006433634],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007354808,0.000024162222,0.81986773,0.00002651166,0.00043391262,0.0005654332,0.015608736,0.0015284134,0.00084556366,0.003564779,0.014247703,0.1432135],"study_design_scores_gemma":[0.0003266004,0.0019210448,0.9512326,0.00030779524,0.000049513652,0.00028977907,0.008219518,0.00023023757,0.0081256665,0.0034228344,0.025382414,0.00049196323],"about_ca_topic_score_codex":0.019572336,"about_ca_topic_score_gemma":0.923804,"teacher_disagreement_score":0.90423167,"about_ca_system_score_codex":0.000005058948,"about_ca_system_score_gemma":0.0015434065,"threshold_uncertainty_score":0.9998238},"labels":[],"label_agreement":null},{"id":"W2803021066","doi":"10.1139/cjes-2017-0258","title":"Provenance constraints on the Xishanyao Formation, southern Yili Basin, northwest China: evidence from petrology, geochemistry, and detrital zircon U–Pb geochronology","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Provenance; Zircon; Petrography; Geochemistry; Geochronology; Felsic; Trace element; Continental crust; Volcanic rock; Petrology; Crust; Mafic; Volcano","score_opus":0.017178729561090324,"score_gpt":0.19444705382284289,"score_spread":0.17726832426175257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2803021066","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98895615,0.0011306424,0.00010358127,0.0069526173,0.00016826589,0.000060640916,0.00014696791,0.000004468883,0.00247666],"genre_scores_gemma":[0.9983961,0.00004423448,0.00058360887,0.00069879333,0.0002367022,3.6707493e-7,0.000007696677,0.0000010718472,0.000031453048],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986745,0.000090558446,0.00031629895,0.0002473964,0.00023512237,0.00043613266],"domain_scores_gemma":[0.99863595,0.00039142524,0.00025788337,0.0001277411,0.00017462461,0.00041238632],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006856762,0.00013839646,0.00022493972,0.00010923558,0.0006204266,0.00014840989,0.0005276595,0.000080090555,0.00978194],"category_scores_gemma":[0.00092865067,0.00007816854,0.000074128686,0.00034633817,0.0034397289,0.00037646876,0.000012205805,0.0002456869,0.00010950709],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026451675,0.0000073466913,0.98917973,0.0000049172736,0.000027432354,0.000048474118,0.00052648113,0.00010456646,0.0011976034,0.00008782391,0.0002545846,0.008534559],"study_design_scores_gemma":[0.00022482517,0.00094710273,0.9776065,0.00011450359,0.000035759524,0.00025717955,0.0010474909,0.0015297937,0.005787683,0.010953373,0.0012808152,0.00021501635],"about_ca_topic_score_codex":0.04497103,"about_ca_topic_score_gemma":0.5724772,"teacher_disagreement_score":0.5275062,"about_ca_system_score_codex":0.0000025766037,"about_ca_system_score_gemma":0.00041652602,"threshold_uncertainty_score":0.99927235},"labels":[],"label_agreement":null},{"id":"W2803119005","doi":"10.1139/cjes-2018-0020","title":"Platform drowning leading to cool-water carbonate deposition: evolution of a Late Ordovician (Turinian–Chatfieldian) mixed-sediment platform within the Taconic orogen (Long Point Group, Newfoundland Appalachians)","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta","keywords":"Geology; Siliciclastic; Carbonate; Ordovician; Carbonate platform; Paleontology; Foreland basin; Geochemistry; Facies; Tectonics; Structural basin","score_opus":0.01687178511817334,"score_gpt":0.2096267045335733,"score_spread":0.19275491941539996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2803119005","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9922195,0.00064124295,0.00059610285,0.0009463131,0.0008073614,0.00015872827,0.000015344347,0.000006717812,0.0046087024],"genre_scores_gemma":[0.99829596,0.00000950722,0.00096680643,0.00044755457,0.00020210262,8.3807413e-7,0.000006426153,0.0000026202765,0.00006819777],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983437,0.000040259816,0.00053394784,0.00017940195,0.00037332505,0.00052936404],"domain_scores_gemma":[0.99882025,0.00009129752,0.00026709336,0.00012031647,0.0001911505,0.0005099129],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014118173,0.00015240833,0.00022250495,0.00036128328,0.0010486251,0.00025579683,0.00051414093,0.00007665332,0.0008520829],"category_scores_gemma":[0.00007303238,0.00008493322,0.00007824258,0.00058829185,0.0005148258,0.0009032626,0.000015060697,0.00021531183,0.00008599445],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011110831,0.000014445624,0.94481015,0.00004926166,0.00008097507,0.00007119477,0.009361443,0.03173423,0.00019926715,0.0023631535,0.000059202663,0.011145556],"study_design_scores_gemma":[0.0005491354,0.0028082908,0.9661463,0.0003746656,0.00007048378,0.00056643,0.004908651,0.013008883,0.0017844641,0.006646031,0.0026677009,0.0004689617],"about_ca_topic_score_codex":0.031141143,"about_ca_topic_score_gemma":0.7632874,"teacher_disagreement_score":0.73214626,"about_ca_system_score_codex":0.000013602715,"about_ca_system_score_gemma":0.0005828786,"threshold_uncertainty_score":0.97531056},"labels":[],"label_agreement":null},{"id":"W2803224269","doi":"10.1139/cjes-2017-0209","title":"Correcting airborne gravity data for overburden thickness: a case study from the Nechako interior plateau, British Columbia","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Polytechnique Montréal; Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Bedrock; Overburden; Geology; Plateau (mathematics); Bouguer anomaly; Borehole; Seismology; Geomorphology; Gravity anomaly; Mining engineering; Geotechnical engineering; Paleontology","score_opus":0.05077064759826158,"score_gpt":0.2784401057287491,"score_spread":0.22766945813048753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2803224269","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966419,0.00039017567,0.00032523694,0.00037820445,0.0014835022,0.00025119705,0.00039241204,0.0000054956217,0.00013187694],"genre_scores_gemma":[0.9955753,0.0000025267886,0.0029799324,0.0004154161,0.0008815468,5.272577e-7,0.000006957514,0.0000025381453,0.00013523977],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99831694,0.0002477106,0.00034703457,0.0003299716,0.00028224275,0.00047607312],"domain_scores_gemma":[0.99770355,0.0010828678,0.00022926196,0.0002671554,0.00020805027,0.0005091184],"candidate_categories":["sts","scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0024311426,0.0000964636,0.00025274296,0.00005089246,0.0015038495,0.0012164743,0.0012010135,0.000046459438,0.0011014419],"category_scores_gemma":[0.0015057218,0.000080381695,0.00006635678,0.0006212989,0.000599915,0.0004974688,0.000029188861,0.0002739841,0.00001613328],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016972625,0.00001583499,0.47531044,0.0000028762831,0.00003757418,0.00098535,0.0011155623,0.000039764018,0.0000044008752,0.0000011519808,0.0024994304,0.51997066],"study_design_scores_gemma":[0.00044265413,0.002399153,0.9668734,0.00007760795,0.000068089255,0.0042291866,0.007443669,0.007283015,0.00000912834,0.0027625842,0.008186347,0.00022515851],"about_ca_topic_score_codex":0.8990557,"about_ca_topic_score_gemma":0.99604297,"teacher_disagreement_score":0.51974547,"about_ca_system_score_codex":0.000002007637,"about_ca_system_score_gemma":0.00086566637,"threshold_uncertainty_score":0.99982035},"labels":[],"label_agreement":null},{"id":"W2803540597","doi":"10.1139/cjes-2018-0039","title":"Monazite U–Th–Pb geochronology of the Central Metasedimentary Belt Boundary Zone (CMBbz), Grenville Province, Ontario Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Monazite; Geology; Metamorphism; Gneiss; Geochronology; Geochemistry; Shear zone; Tectonics; Zircon; Paleontology; Metamorphic rock","score_opus":0.008750703726597609,"score_gpt":0.1642406910895493,"score_spread":0.1554899873629517,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2803540597","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99102914,0.0011512643,0.000007813514,0.0026751999,0.00084068836,0.00006813151,0.00010135114,0.000001479271,0.0041249353],"genre_scores_gemma":[0.9977056,0.0000077798195,0.0005807966,0.0010406263,0.0001668557,1.1841315e-7,0.000008747922,0.0000011356698,0.00048836647],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981623,0.000088782836,0.00042547763,0.00021099819,0.00046885078,0.0006435806],"domain_scores_gemma":[0.99866927,0.000080145015,0.0003060708,0.00015280601,0.00014743123,0.0006442762],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041419192,0.00014003292,0.0002910924,0.00012975799,0.0006084131,0.000055459874,0.00081651664,0.000052387102,0.017959932],"category_scores_gemma":[0.000076501805,0.00008005477,0.0001400725,0.0005257862,0.001989216,0.00016906732,0.000019959165,0.00024471484,0.000012258797],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011949603,0.000006462358,0.99549484,0.0000032302428,0.00004578022,0.000049040726,0.00010923898,0.00057643733,0.00009513507,0.00003654179,0.0016360322,0.0019353231],"study_design_scores_gemma":[0.00014552576,0.00035910797,0.9327892,0.00001927486,0.000050265404,0.000089784575,0.00015132423,0.00022841369,0.0013179957,0.0010116746,0.06371513,0.00012231903],"about_ca_topic_score_codex":0.9964027,"about_ca_topic_score_gemma":0.99998343,"teacher_disagreement_score":0.06270565,"about_ca_system_score_codex":0.000016915246,"about_ca_system_score_gemma":0.009793421,"threshold_uncertainty_score":0.9958201},"labels":[],"label_agreement":null},{"id":"W2806124000","doi":"10.1139/cjes-2017-0237","title":"Mineral composition of host sediments influences the fossilization of soft tissues","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Chlorite; Kaolinite; Geology; Clay minerals; Mineralization (soil science); Mineralogy; Geochemistry; Sediment; Weathering; Dissolution; Mineral; Environmental chemistry; Chemistry; Quartz; Soil water; Soil science; Geomorphology; Paleontology","score_opus":0.014603814855276516,"score_gpt":0.2241257981452362,"score_spread":0.2095219832899597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2806124000","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970177,0.00051893375,0.000023169387,0.00031703123,0.00017836028,0.000027483859,0.000030326923,7.8487017e-7,0.0018862208],"genre_scores_gemma":[0.9994812,0.000008475214,0.00029357043,0.00006826536,0.000100369645,4.0492377e-8,0.000004792492,4.4911155e-7,0.000042848827],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991773,0.000038918548,0.00028247022,0.00007226154,0.00027289332,0.00015620822],"domain_scores_gemma":[0.99928516,0.000042150623,0.00028990753,0.000057119527,0.0001816036,0.00014405505],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048067153,0.0000552204,0.00011692802,0.00011658865,0.0002747966,0.00004265918,0.00030397266,0.000021241674,0.0013312359],"category_scores_gemma":[0.000038449773,0.00003398679,0.000048750768,0.00045219393,0.00096978445,0.0002744272,0.0000029974044,0.00004365552,0.000006497739],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006930135,0.0000038969833,0.99268997,0.000007099773,0.000017482867,0.0000022066824,0.0005037687,0.0016084504,0.003135122,0.00001671912,0.00010677999,0.0019015888],"study_design_scores_gemma":[0.00011202403,0.00049541227,0.9645964,0.00007231589,0.00003290168,0.000029118852,0.0010643676,0.002264096,0.029784549,0.00030995574,0.0011683608,0.000070489376],"about_ca_topic_score_codex":0.01630507,"about_ca_topic_score_gemma":0.11126262,"teacher_disagreement_score":0.09495755,"about_ca_system_score_codex":7.8441843e-7,"about_ca_system_score_gemma":0.00028663987,"threshold_uncertainty_score":0.9995817},"labels":[],"label_agreement":null},{"id":"W2807652684","doi":"10.1139/cjes-2018-0006","title":"Lithostratigraphy of the upper Turinian – lower Chatfieldian (Upper Ordovician) foreland succession, and a U–Pb ID–TIMS date for the Millbrig volcanic ash bed in the Ottawa Embayment","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Carleton University","funders":"","keywords":"Geology; Foreland basin; Laurentia; Paleontology; Onlap; Facies; Sedimentary depositional environment; Marine transgression; Lithostratigraphy; Trilobite; Carbonate platform; Ordovician; Stratotype; Diachronous; Siliciclastic; Fault block; Stage (stratigraphy); Sedimentary rock; Structural basin","score_opus":0.014677471978177772,"score_gpt":0.22159239603101982,"score_spread":0.20691492405284206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2807652684","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9858379,0.0018252819,0.000029296101,0.009207012,0.00048164657,0.0002384892,0.000061146835,0.0000012120313,0.0023180614],"genre_scores_gemma":[0.9981985,0.000077166165,0.0003023768,0.0012593573,0.000111196736,0.0000012968318,0.0000018534354,0.0000010927022,0.00004712538],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99888486,0.0000806344,0.00032793175,0.00012324651,0.0002541368,0.00032918618],"domain_scores_gemma":[0.99906117,0.00029999294,0.00020276444,0.00013996144,0.00012334088,0.00017276611],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013852566,0.00010014821,0.00013564019,0.00014853939,0.0008592715,0.00020333311,0.0007391287,0.000051156898,0.0006835705],"category_scores_gemma":[0.00015620787,0.000039057228,0.00007176519,0.00059313665,0.0009028667,0.00034199713,0.000007662403,0.00015581276,0.000003521209],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010846198,0.0000051973443,0.9923171,0.000009157315,0.00000942804,0.0000022906324,0.0016762365,0.00010779679,0.0000042136367,0.00040998645,0.00042872748,0.005019016],"study_design_scores_gemma":[0.00015696856,0.0005123447,0.9510018,0.000056444253,0.000014046264,0.000047300913,0.0017588038,0.0005949364,0.000057841546,0.0017592394,0.043966375,0.000073892435],"about_ca_topic_score_codex":0.01124789,"about_ca_topic_score_gemma":0.7340288,"teacher_disagreement_score":0.72278094,"about_ca_system_score_codex":6.235946e-7,"about_ca_system_score_gemma":0.00047955938,"threshold_uncertainty_score":0.9953363},"labels":[],"label_agreement":null},{"id":"W2809944106","doi":"10.1139/cjes-2018-0088","title":"Magnetic hysteresis of 0.6–110 μm magnetites across the Verwey transition","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Japan Society for the Promotion of Science; University of Minnesota; Earth Sciences Division; National Science Foundation","keywords":"Remanence; Coercivity; Materials science; Hysteresis; Condensed matter physics; Charge ordering; Saturation (graph theory); Magnetic hysteresis; Analytical Chemistry (journal); Magnetite; Hardening (computing); Magnetization; Nuclear magnetic resonance; Mineralogy; Charge (physics); Chemistry; Physics; Nanotechnology; Magnetic field; Metallurgy","score_opus":0.012053249973611919,"score_gpt":0.23485916917133717,"score_spread":0.22280591919772524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2809944106","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98868555,0.007121962,0.000045706354,0.0010230379,0.00038692905,0.00007222562,0.000045797322,0.0000011026985,0.0026176989],"genre_scores_gemma":[0.99835116,0.00017669499,0.00040999043,0.0002747219,0.00033564403,0.0000010880707,0.0000016704338,0.000004753021,0.00044425085],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989892,0.00006773356,0.000272153,0.00014890727,0.0001855232,0.00033643414],"domain_scores_gemma":[0.99924725,0.000024977311,0.00014700355,0.0001571791,0.00024098653,0.0001825819],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051330525,0.000105390114,0.0001405307,0.000076522,0.00040250405,0.00006143839,0.00042277476,0.00005854137,0.00021031339],"category_scores_gemma":[0.00009608799,0.00007255826,0.00009098717,0.00023204084,0.0017004526,0.000013563385,0.000019817955,0.00006660483,0.000009478771],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032098583,0.00012633065,0.3515243,0.00020069712,0.00023735268,0.00014791719,0.022873769,0.0005193638,0.5082916,0.00076658983,0.021428326,0.0935628],"study_design_scores_gemma":[0.0010653598,0.013362656,0.8066364,0.00015261133,0.000084935804,0.00043147363,0.0049870224,0.00008203201,0.071598314,0.0006181236,0.10052807,0.00045303514],"about_ca_topic_score_codex":0.001247527,"about_ca_topic_score_gemma":0.08974827,"teacher_disagreement_score":0.45511207,"about_ca_system_score_codex":0.0000010885096,"about_ca_system_score_gemma":0.00040330732,"threshold_uncertainty_score":0.92686146},"labels":[],"label_agreement":null},{"id":"W2810139144","doi":"10.1139/cjes-2018-0060","title":"Zircon provenance of the Carboniferous Mattson delta complex, western Laurentian margin, Canada: record of a Greenland-sourced pancontinental river system","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Geological Survey of Canada","funders":"","keywords":"Geology; Laurentia; Provenance; Zircon; Detritus; Paleontology; Carboniferous; Pennsylvanian; Paleozoic; Clastic rock; Diamictite; Sedimentary rock; Structural basin","score_opus":0.014744132934076061,"score_gpt":0.17639486988478537,"score_spread":0.1616507369507093,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2810139144","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968642,0.00032579093,0.000012824229,0.00068406767,0.00039663486,0.00007515288,0.00011225201,0.0000018929874,0.0015271647],"genre_scores_gemma":[0.9993822,0.0000034858183,0.00026719572,0.00013709912,0.000105697625,1.3085096e-7,0.0000035235498,0.0000013063917,0.00009934139],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985093,0.000090718844,0.00046880453,0.0001623703,0.0004114997,0.00035729725],"domain_scores_gemma":[0.9987139,0.000060317117,0.00052320695,0.00013156344,0.00022689956,0.00034412782],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038952217,0.00011551396,0.00033402359,0.00010116735,0.00022189539,0.000030508387,0.000665448,0.00004060356,0.0009044512],"category_scores_gemma":[0.000065734865,0.00006551099,0.00012064497,0.0005226971,0.0010258964,0.0001044082,0.000013408298,0.00012143641,0.000004056234],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012385636,0.000003113213,0.9982539,0.000019836809,0.000020943182,0.000015163622,0.000109858374,0.00014421753,0.00022204699,0.000019387298,0.00018846325,0.0009906924],"study_design_scores_gemma":[0.00016921703,0.00023709553,0.99415535,0.0001294821,0.00003502179,0.000075586366,0.00036499705,0.0013389314,0.0009855891,0.00014460624,0.0022664804,0.00009764333],"about_ca_topic_score_codex":0.9262671,"about_ca_topic_score_gemma":0.99851054,"teacher_disagreement_score":0.07224345,"about_ca_system_score_codex":0.000005143828,"about_ca_system_score_gemma":0.0010101349,"threshold_uncertainty_score":0.9903106},"labels":[],"label_agreement":null},{"id":"W2810797743","doi":"10.1139/cjes-2018-0029","title":"Early gold-bearing quartz veins within the Rivière-Héva fault zone, Abitibi subprovince, Quebec, Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Ministère des Ressources naturelles et des Forêts (Québec); Université du Québec à Chicoutimi","funders":"","keywords":"Geology; Geochemistry; Diorite; Greenstone belt; Vein; Felsic; Lineation; Mafic; Zircon; Shear zone; Quartz; Fault (geology); Mylonite; Archean; Seismology; Tectonics; Paleontology","score_opus":0.010617584300872509,"score_gpt":0.1784610584612718,"score_spread":0.1678434741603993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2810797743","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9861346,0.0005217177,0.000023617351,0.0034897611,0.00066339644,0.000061699466,0.000027595315,0.0000053856684,0.009072222],"genre_scores_gemma":[0.99690616,0.000004988696,0.00028479827,0.0010888337,0.0004152771,1.8763129e-7,0.0000027287078,0.0000018907441,0.0012951271],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979096,0.00010561559,0.00045525265,0.0002606917,0.0006140103,0.000654807],"domain_scores_gemma":[0.9981695,0.0001916032,0.00029179786,0.0001722127,0.00025396602,0.0009209455],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009175303,0.0001682941,0.00025917718,0.00016593302,0.0008162681,0.00033001823,0.0009958752,0.000059332593,0.0032810904],"category_scores_gemma":[0.00028573038,0.00009341786,0.0001123725,0.00092950277,0.0014305196,0.00037644536,0.00001234194,0.00032774894,0.00010099151],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010109127,0.000005629787,0.9927106,0.0000034588372,0.000027605267,0.000120671575,0.00035527645,0.0019215809,0.000054347915,0.00030569194,0.0015894785,0.002895587],"study_design_scores_gemma":[0.00011529455,0.0003723311,0.9819977,0.000030289373,0.000025409883,0.00006674839,0.0006994433,0.0020093273,0.00028439108,0.0013252024,0.012873245,0.00020059901],"about_ca_topic_score_codex":0.99533874,"about_ca_topic_score_gemma":0.9999789,"teacher_disagreement_score":0.011283767,"about_ca_system_score_codex":0.0000075295407,"about_ca_system_score_gemma":0.0037283797,"threshold_uncertainty_score":0.99763006},"labels":[],"label_agreement":null},{"id":"W2811135113","doi":"10.1139/cjes-2018-0065","title":"Karstic spring wetlands of the Persepolis Basin, southwest Iran: unique sediment archives of Holocene environmental change and human impacts","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Agence Nationale de la Recherche","keywords":"Wetland; Karst; Geology; Spring (device); Structural basin; Groundwater; Hydrology (agriculture); Alluvial plain; Aquifer; Cave; Ecology; Paleontology; Geography; Archaeology","score_opus":0.0379519863889369,"score_gpt":0.23517378634142316,"score_spread":0.19722179995248626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2811135113","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971048,0.0006952981,0.0000012967707,0.00045468603,0.00018767217,0.00006457796,0.000033781977,7.6516733e-7,0.0014570808],"genre_scores_gemma":[0.9996523,0.000048237318,0.00011779388,0.000082921186,0.00007614724,1.10201604e-7,9.551572e-7,0.000001116659,0.000020407624],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99904686,0.00012978642,0.00021561522,0.000108193264,0.00018043768,0.00031909795],"domain_scores_gemma":[0.99925065,0.00014167631,0.00018503975,0.000092053044,0.000018420142,0.00031217685],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0005955339,0.00007688283,0.00017019927,0.00024328982,0.0004084051,0.000019230076,0.00033257907,0.00004527977,0.00046455237],"category_scores_gemma":[0.0000615604,0.000048745573,0.00005072408,0.00016068647,0.0034972467,0.00012882566,0.000012620931,0.00014904681,0.0000038771777],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000765918,0.0000035480482,0.9979572,0.000008865062,0.000010179101,0.000011796168,0.001668386,0.000011230438,0.0001257967,0.000056025263,0.0000025213646,0.00013677456],"study_design_scores_gemma":[0.00015358496,0.0005245494,0.9970109,0.00006202074,0.000011433841,0.00016124453,0.0006909394,0.000099074416,0.0009701742,0.00017514336,0.00009030247,0.000050654446],"about_ca_topic_score_codex":0.01342837,"about_ca_topic_score_gemma":0.27875224,"teacher_disagreement_score":0.26532388,"about_ca_system_score_codex":4.182474e-7,"about_ca_system_score_gemma":0.0002757414,"threshold_uncertainty_score":0.99921465},"labels":[],"label_agreement":null},{"id":"W2826414899","doi":"10.1139/cjes-2018-0082","title":"Allochthonous sources of iodine and organic carbon in an eastern Ontario aquifer","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Ottawa","funders":"","keywords":"Geology; Aquifer; Glacial period; Bedrock; Organic matter; Total organic carbon; Geochemistry; Groundwater; Sedimentary rock; Sedimentary organic matter; Dissolved organic carbon; Oceanography; Geomorphology; Environmental chemistry","score_opus":0.016709604907612606,"score_gpt":0.19203659495933242,"score_spread":0.1753269900517198,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2826414899","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99566334,0.0004042163,0.0000018836243,0.000083727515,0.00021133166,0.000030537703,0.000004046806,0.0000012245706,0.003599679],"genre_scores_gemma":[0.9993929,0.000004320385,0.00022040353,0.000066515386,0.00011108466,3.4259358e-8,0.0000010159654,0.0000012343547,0.00020246506],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990992,0.000032397358,0.00026906416,0.00013536896,0.00017567733,0.00028832007],"domain_scores_gemma":[0.9992891,0.000019848023,0.00012200442,0.0000758719,0.000081688115,0.0004114659],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00054003287,0.000081780876,0.00016129254,0.00020815311,0.000114133436,0.000104533174,0.0002902169,0.00004005571,0.0013121045],"category_scores_gemma":[0.000026873739,0.00006220141,0.00002094599,0.00022786409,0.0006113426,0.00029115521,0.000004730235,0.00011182624,0.0000043748237],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000075104595,0.000002701254,0.9965492,0.0000033876518,0.00000282137,0.000030417808,0.002047376,0.000029055986,0.0003112073,0.0000014685038,0.0000028119773,0.0010120403],"study_design_scores_gemma":[0.00017917494,0.0006843995,0.99502546,0.00003916726,0.000005729656,0.00018697159,0.0007042827,0.0006907498,0.0016220008,0.00015746403,0.00061228,0.00009233326],"about_ca_topic_score_codex":0.36209455,"about_ca_topic_score_gemma":0.9897466,"teacher_disagreement_score":0.62765205,"about_ca_system_score_codex":0.0000025095292,"about_ca_system_score_gemma":0.0011060007,"threshold_uncertainty_score":0.9996008},"labels":[],"label_agreement":null},{"id":"W2841446990","doi":"10.1139/cjes-2018-0025","title":"Carbon isotopes, stratigraphy, and environmental change: the Middle–Upper Cambrian Positive Excursion (SPICE) in Port au Port Group, western Newfoundland, Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Universidade Federal do Rio Grande do Sul; Shell Brasil; University of Aberdeen; Natural Environment Research Council; Sight Research UK","keywords":"Geology; Cove; Grainstone; Sedimentary depositional environment; Stratigraphy; Paleontology; Excursion; Diagenesis; Isochron; Geochemistry; Geomorphology; Structural basin","score_opus":0.020486999981370303,"score_gpt":0.20286786444033622,"score_spread":0.18238086445896592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2841446990","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9829023,0.005036247,0.0000011075944,0.00091229286,0.00061812316,0.00014011093,0.00007146142,0.000001399717,0.010316985],"genre_scores_gemma":[0.9992223,0.00006803563,0.000060546445,0.0003471985,0.00026874262,4.4694565e-7,0.0000045270967,9.399246e-7,0.000027284173],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99852693,0.00011178376,0.00029926316,0.0002169433,0.0003271707,0.0005179368],"domain_scores_gemma":[0.9990863,0.00007114213,0.00018679345,0.000098863144,0.000022054888,0.0005348092],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00068834674,0.00015044978,0.00019652929,0.0002399909,0.00058827613,0.00010319158,0.0003487592,0.000068416375,0.00009917361],"category_scores_gemma":[0.000015132942,0.00010136864,0.00004588442,0.00025406206,0.0013802311,0.00041850735,0.000001917077,0.00022751588,8.50834e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001347154,0.0000031186198,0.990332,0.0000017669232,0.000010685684,0.00017102588,0.0009055209,0.0000018814667,0.000007880341,0.000028909602,0.0000089820005,0.008514775],"study_design_scores_gemma":[0.00019516522,0.0005289731,0.99595803,0.00005014506,0.000012423292,0.0003976279,0.0017219896,0.00015938192,0.0000072563175,0.00008097714,0.0007546781,0.00013332914],"about_ca_topic_score_codex":0.96113324,"about_ca_topic_score_gemma":0.99993384,"teacher_disagreement_score":0.038800623,"about_ca_system_score_codex":0.000008184878,"about_ca_system_score_gemma":0.0016487224,"threshold_uncertainty_score":0.5085519},"labels":[],"label_agreement":null},{"id":"W2847573868","doi":"10.1139/cjes-2018-0022","title":"Phylogenetic relationships among the Rangeomorpha: the importance of outgroup selection and implications for their diversification","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto; Queen's University","funders":"Northwestern University","keywords":"Clade; Taxon; Phylogenetic tree; Biology; Evolutionary biology; Ecology; Paleontology","score_opus":0.05078112249337184,"score_gpt":0.23229923028019855,"score_spread":0.1815181077868267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2847573868","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99205524,0.0032700785,0.0003894392,0.0021757975,0.00012879098,0.00013065575,0.000038453953,0.0000012794042,0.0018102681],"genre_scores_gemma":[0.9994837,0.000028592049,0.00035871897,0.000042685373,0.000077779165,6.75124e-7,8.042599e-7,2.9878902e-7,0.0000067519286],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999454,0.000079215635,0.00017569549,0.00008255912,0.000065070715,0.00014344527],"domain_scores_gemma":[0.99912727,0.00032556072,0.0002311749,0.00006963781,0.00014162557,0.00010471503],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0010922226,0.000047514844,0.00007104631,0.00008840908,0.0013895386,0.000046813537,0.00025265914,0.000032259795,0.000038348087],"category_scores_gemma":[0.0001395983,0.000024897494,0.000037938917,0.00030845526,0.0014816019,0.00017268492,5.153269e-7,0.00008512387,4.818879e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000038026253,7.941414e-7,0.99228925,0.0000010254527,0.000007947774,7.907965e-8,0.00045424234,0.000036676138,0.00002843244,0.0005798833,0.000053985128,0.0065438724],"study_design_scores_gemma":[0.00006457495,0.00016678656,0.9945956,0.000006174193,0.000015033326,0.000028244054,0.00055062905,0.0006327982,0.00005974562,0.0036016728,0.00024680258,0.000031981064],"about_ca_topic_score_codex":0.00185144,"about_ca_topic_score_gemma":0.59933424,"teacher_disagreement_score":0.5974828,"about_ca_system_score_codex":5.60373e-7,"about_ca_system_score_gemma":0.00027817514,"threshold_uncertainty_score":0.99991053},"labels":[],"label_agreement":null},{"id":"W2858637132","doi":"10.1139/cjes-2017-0172","title":"Conceptual hydrogeological model of the Yonge Street Aquifer, south-central Ontario: a glaciofluvial channel–fan setting","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Toronto and Region Conservation Authority; Geological Survey of Canada","funders":"","keywords":"Geology; Aquifer; Bedrock; Hydrogeology; Channel (broadcasting); Geomorphology; Channelized; Facies; Groundwater; Geochemistry; Petrology; Hydrology (agriculture); Geotechnical engineering; Structural basin","score_opus":0.03197990028168924,"score_gpt":0.2066628218833441,"score_spread":0.17468292160165486,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2858637132","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941472,0.00018838336,0.00016271876,0.00068350515,0.00073950435,0.00006930766,0.00004403021,0.0000076925735,0.003957654],"genre_scores_gemma":[0.9973187,0.0000033971892,0.0011295442,0.0011890283,0.00019398861,9.276787e-8,0.0000012741154,0.0000016390255,0.0001623587],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984717,0.000089640205,0.00033754937,0.00017161338,0.00039858202,0.0005309545],"domain_scores_gemma":[0.9989671,0.00005208746,0.00028484745,0.00012205908,0.00013144877,0.0004424662],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00081367214,0.00011823886,0.00018881208,0.0001620229,0.00056528917,0.0000697294,0.00075752934,0.000065145956,0.0011489032],"category_scores_gemma":[0.0001457774,0.000072890536,0.00012038917,0.00027749565,0.002754287,0.00031577857,0.000014291955,0.0002558705,0.000010348305],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012129565,0.0000044161143,0.9895866,0.0000017129066,0.000009748763,0.000010260503,0.0051855748,0.002369186,0.00003085887,0.00020623302,0.0011968111,0.0013864908],"study_design_scores_gemma":[0.0011873572,0.0031235393,0.6728485,0.00037419907,0.000087183995,0.00032302024,0.012103266,0.26885968,0.011837451,0.007889821,0.0205393,0.0008266255],"about_ca_topic_score_codex":0.19679697,"about_ca_topic_score_gemma":0.67039037,"teacher_disagreement_score":0.4735934,"about_ca_system_score_codex":0.0000060964007,"about_ca_system_score_gemma":0.0024775185,"threshold_uncertainty_score":0.99995965},"labels":[],"label_agreement":null},{"id":"W2876850239","doi":"10.1139/cjes-2018-0040","title":"Borehole magnetic surveys in weakly magnetic sediments (Chicxulub impact crater) versus strongly magnetic volcanics (Bathurst mining camp)","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Brock University; University of Toronto; McMaster University","funders":"","keywords":"Borehole; Geology; Geophysics; Magnetic anomaly; Magnetometer; Impact crater; Remanence; Paleomagnetism; Seismology; Magnetic field; Magnetization; Paleontology; Physics","score_opus":0.018340241237958715,"score_gpt":0.25470805004314245,"score_spread":0.23636780880518374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2876850239","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9768594,0.016249195,0.000022695735,0.00018635123,0.001503991,0.00017616256,0.0000833942,0.0000042243605,0.0049145925],"genre_scores_gemma":[0.9971878,0.00025308275,0.0009300322,0.0000882622,0.0005244465,0.0000041707535,0.000012129031,0.000022017257,0.0009780821],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99700356,0.00037053786,0.00060302013,0.00047447416,0.00040871298,0.0011397267],"domain_scores_gemma":[0.99829185,0.000056530425,0.0002442987,0.00031592057,0.0002946781,0.0007967339],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017439615,0.00034497722,0.00036458066,0.00047381583,0.00040114496,0.0002151149,0.0007601415,0.00016505724,0.0009559033],"category_scores_gemma":[0.00029304132,0.0003063544,0.00014947349,0.0006365308,0.0012326429,0.000042797416,0.000075538665,0.00021752651,0.000051990355],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001748377,0.00008577804,0.948473,0.000029160978,0.00006108927,0.0003139508,0.0014854454,0.00048813023,0.01995514,0.000015533613,0.0046221297,0.024295824],"study_design_scores_gemma":[0.0017944266,0.018851364,0.9656293,0.000085586755,0.000044828706,0.00014566016,0.0009053153,0.00019816562,0.0010624593,0.00004140074,0.010780297,0.00046118963],"about_ca_topic_score_codex":0.0039177155,"about_ca_topic_score_gemma":0.29577687,"teacher_disagreement_score":0.29185915,"about_ca_system_score_codex":0.000018955458,"about_ca_system_score_gemma":0.00199624,"threshold_uncertainty_score":0.9999574},"labels":[],"label_agreement":null},{"id":"W2882976539","doi":"10.1139/cjes-2018-0089","title":"Distinguishing cryoseisms from earthquakes in Alberta, Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Magnitude (astronomy); Seismology; Geology; Seismic noise; Ground motion; Maximum magnitude; Induced seismicity","score_opus":0.014035588199021605,"score_gpt":0.1958877994090164,"score_spread":0.1818522112099948,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2882976539","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9862688,0.00047284635,0.000015080536,0.0016559765,0.0009392455,0.000024024752,0.00007265891,0.0000012601228,0.010550083],"genre_scores_gemma":[0.9975301,0.000008668486,0.0007329046,0.0010033597,0.00047792928,2.927922e-8,0.000006716173,0.0000016828358,0.00023860065],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986295,0.000058608133,0.00034917548,0.00017937327,0.00033038142,0.00045293834],"domain_scores_gemma":[0.9988118,0.00024229697,0.0001801919,0.00009375171,0.00009125145,0.00058070064],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005170303,0.00010313217,0.00020692914,0.000253792,0.00036175217,0.00021501051,0.0004883581,0.00003400097,0.0031172764],"category_scores_gemma":[0.0003871929,0.00007965141,0.00005452258,0.00064288324,0.00040296087,0.0003193381,0.0000034693132,0.00014752032,0.00003060167],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026466178,0.000001109225,0.9932199,8.3544353e-7,0.000008706438,0.00011022467,0.00026236274,0.0016294147,0.0000027203268,0.000044169956,0.00061072333,0.0041071856],"study_design_scores_gemma":[0.00011300973,0.00010580746,0.9407204,0.00005615942,0.000009376454,0.000019081337,0.00081439514,0.006850215,0.00002708539,0.0011306069,0.050017487,0.00013636837],"about_ca_topic_score_codex":0.99866927,"about_ca_topic_score_gemma":0.9999741,"teacher_disagreement_score":0.052499495,"about_ca_system_score_codex":0.000004384181,"about_ca_system_score_gemma":0.0036393942,"threshold_uncertainty_score":0.99779403},"labels":[],"label_agreement":null},{"id":"W2883028490","doi":"10.1139/cjes-2017-0242","title":"Early thrusting and folding in the Snow Lake camp, Manitoba: tectonic implications and effects on volcanogenic massive sulfide deposits","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Archean; Geochemistry; Accretion (finance); Paleontology; Batholith; Mafic; Fault (geology); Precambrian; Tectonics; Geomorphology","score_opus":0.015181633322749338,"score_gpt":0.2016428779610213,"score_spread":0.18646124463827196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2883028490","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99564916,0.00084770925,0.0000075455764,0.0019952245,0.00008564484,0.00006514186,0.0000071039303,0.0000018273629,0.0013406279],"genre_scores_gemma":[0.99901396,0.000029442524,0.00023467936,0.00056376366,0.00014944113,3.787343e-7,8.780219e-7,7.438836e-7,0.0000067206884],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991194,0.00007723366,0.00017271905,0.00016293766,0.00015222748,0.00031547147],"domain_scores_gemma":[0.9990044,0.00048727143,0.00010088682,0.00006427536,0.000057394143,0.0002857347],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005466503,0.00008402364,0.00012978344,0.0001837813,0.0005414955,0.00018027375,0.00026537225,0.00003439366,0.00017130275],"category_scores_gemma":[0.00030951094,0.00004722447,0.000034866927,0.00054065057,0.0004774602,0.00015591807,0.000006266602,0.00015730676,0.000011567719],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000025985826,0.0000014074953,0.98834413,0.000002301274,0.000005999817,0.000025599144,0.00022667852,0.000058562084,0.00009995318,0.000083729974,0.000015974301,0.011133091],"study_design_scores_gemma":[0.00008703017,0.0003782411,0.99422467,0.000045842637,0.000016455673,0.000087139095,0.00028783234,0.00023358976,0.00023509566,0.0041640038,0.00017096577,0.000069113834],"about_ca_topic_score_codex":0.013652025,"about_ca_topic_score_gemma":0.8810789,"teacher_disagreement_score":0.8674269,"about_ca_system_score_codex":0.0000013859986,"about_ca_system_score_gemma":0.00014753854,"threshold_uncertainty_score":0.99291617},"labels":[],"label_agreement":null},{"id":"W2884220437","doi":"10.1139/cjes-2018-0046","title":"Applying laterally varying density corrections to ground gravity and airborne gravity gradiometry data: a case study from the Bathurst Mining Camp","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Brock University; McMaster University","funders":"","keywords":"Geology; Terrain; Density contrast; Bouguer anomaly; Geodesy; Gravity anomaly; Geophysics; Gemology; Geomorphology; Seismology; Engineering geology; Paleontology; Tectonics; Volcanism","score_opus":0.05764372167907488,"score_gpt":0.2823302898546924,"score_spread":0.2246865681756175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2884220437","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975876,0.00023671286,0.0003924997,0.0003765765,0.0009988401,0.00022742776,0.0000780439,0.0000057835823,0.000096471886],"genre_scores_gemma":[0.9947053,0.00000286236,0.004292524,0.00046062106,0.0005098756,6.6643645e-7,0.000003146875,0.0000021110304,0.000022851453],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99820584,0.00031130618,0.00028831736,0.00036357975,0.00032981692,0.0005011461],"domain_scores_gemma":[0.99774414,0.00078876223,0.0001454398,0.00024816752,0.00014021691,0.00093324354],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0022031907,0.00014176841,0.00025265044,0.0002432884,0.001934677,0.00049675035,0.0006413983,0.00003761893,0.00014371342],"category_scores_gemma":[0.00061632047,0.0000901884,0.000040927018,0.0015511012,0.0005318812,0.0005354104,0.00003701733,0.000279456,0.000021580365],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012719433,0.0000132660125,0.91628474,0.0000012603472,0.000022595368,0.00060269644,0.0015016582,0.00007665825,0.000016870536,0.000003566539,0.000083743806,0.08138025],"study_design_scores_gemma":[0.00013745672,0.0008808862,0.9920443,0.000020144813,0.00004330407,0.000921124,0.002511848,0.0017994442,0.000011791607,0.00073056604,0.00075824634,0.00014088734],"about_ca_topic_score_codex":0.34808716,"about_ca_topic_score_gemma":0.83183557,"teacher_disagreement_score":0.4837484,"about_ca_system_score_codex":0.000003628333,"about_ca_system_score_gemma":0.00048171773,"threshold_uncertainty_score":0.9993647},"labels":[],"label_agreement":null},{"id":"W2884482673","doi":"10.1139/cjes-2018-0072","title":"Ordovician mafic magmatism in an Ediacaran arc complex, Sibak, northeastern Iran: the eastern tip of the Rheic Ocean","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Plutonism; Gondwana; Zircon; Paleozoic; Magmatism; Rift; Mafic; Paleontology; Precambrian; Ordovician; Geochemistry; Gabbro; Terrane; Basalt; Structural basin; Tectonics","score_opus":0.03481652762309678,"score_gpt":0.2164258782635101,"score_spread":0.1816093506404133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2884482673","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99135095,0.00030923713,0.0000062439613,0.0036629161,0.00029106185,0.00007401291,0.000028794868,0.0000019331144,0.004274836],"genre_scores_gemma":[0.9987557,0.000005349117,0.00013158088,0.0008143922,0.00020147422,7.794115e-8,0.000002435183,0.0000013807793,0.00008759615],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99833137,0.00019760344,0.00043251208,0.00017837617,0.00041910942,0.00044100967],"domain_scores_gemma":[0.9988888,0.000111400426,0.00025972314,0.00019461759,0.00012800262,0.0004174538],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00092306326,0.00012282217,0.0002404228,0.00018677948,0.00041709453,0.00011306563,0.0012033039,0.00004484405,0.004165239],"category_scores_gemma":[0.000101869104,0.000057518086,0.00012537887,0.00095350936,0.0018496682,0.00024508155,0.000014399392,0.0002257978,0.00005085145],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057996954,0.00000570508,0.9954895,0.000002797336,0.0000061209403,0.000006462478,0.00045274492,0.00071422796,0.000027455571,0.000040066647,0.00003309398,0.0032160638],"study_design_scores_gemma":[0.00011354895,0.00028114516,0.9837155,0.000037419333,0.000014253788,0.000037235994,0.0006486106,0.009798311,0.000032331754,0.003643782,0.0015907994,0.00008707334],"about_ca_topic_score_codex":0.05438373,"about_ca_topic_score_gemma":0.934471,"teacher_disagreement_score":0.8800873,"about_ca_system_score_codex":0.0000015404785,"about_ca_system_score_gemma":0.0003403878,"threshold_uncertainty_score":0.9967451},"labels":[],"label_agreement":null},{"id":"W2885080132","doi":"10.1139/cjes-2018-0024","title":"Estimating basin-wide air temperature by partial integration of remote sensing data","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Urban Heat Island Mitigation","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Remote sensing; Interpolation (computer graphics); Structural basin; Satellite; Meteorology; Geology; Air temperature; Environmental science; Climatology; Computer science; Geography; Geomorphology","score_opus":0.02450517422589342,"score_gpt":0.24548399373675522,"score_spread":0.2209788195108618,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2885080132","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99093974,0.00005191912,0.0058666277,0.0009296566,0.00051393226,0.00005214683,0.000028592347,0.0000028277877,0.0016145599],"genre_scores_gemma":[0.9355926,0.0000013292344,0.06382065,0.00030523958,0.00016261921,1.4316192e-8,0.0000044135995,0.0000033126885,0.000109827],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990035,0.000055188568,0.00027588406,0.00016104533,0.00028746706,0.00021686654],"domain_scores_gemma":[0.99927694,0.000055207853,0.00020428616,0.00017004978,0.00004650709,0.0002470171],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009486735,0.00007028462,0.0001111897,0.0000801113,0.000291326,0.00006429647,0.00037489706,0.00004055494,0.00027248685],"category_scores_gemma":[0.00059005216,0.000055301327,0.00002284024,0.00032431597,0.00076672697,0.00071656005,0.000027795548,0.00011615517,0.000018829296],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003400518,0.000022779497,0.23786984,0.000019608035,0.000036196972,0.00008712214,0.006967809,0.0027842843,0.37063822,0.000060400038,0.12773944,0.25374028],"study_design_scores_gemma":[0.0009095891,0.001685725,0.1767258,0.0009464805,0.00009790929,0.0006537227,0.0017669415,0.3614073,0.37787873,0.0018768291,0.07525765,0.0007933209],"about_ca_topic_score_codex":0.010517186,"about_ca_topic_score_gemma":0.09590916,"teacher_disagreement_score":0.35862303,"about_ca_system_score_codex":0.000016818862,"about_ca_system_score_gemma":0.0003259942,"threshold_uncertainty_score":0.9960719},"labels":[],"label_agreement":null},{"id":"W2885212109","doi":"10.1139/cjes-2018-0030","title":"Salt tectonism and distribution of brackish-water trace fossils in the Cretaceous McMurray Formation, Athabasca Oil Sands, Alberta Foreland Basin","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Golder Associates (Canada)","funders":"","keywords":"Geology; Fluvial; Foreland basin; Cretaceous; Paleontology; Sedimentary depositional environment; Oil sands; Trace fossil; Brackish water; Structural basin; Oceanography; Salinity","score_opus":0.014098580269914443,"score_gpt":0.20596584815079436,"score_spread":0.1918672678808799,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2885212109","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915774,0.0013093567,0.0001119355,0.0018947115,0.00012935384,0.00004237925,0.000042271888,0.0000011667313,0.0048914533],"genre_scores_gemma":[0.99950534,0.000075364966,0.00015509584,0.0001420279,0.00005368623,2.2817223e-7,0.0000117205345,6.191529e-7,0.000055899873],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99902207,0.00007399579,0.00032454493,0.000085914806,0.00020818737,0.00028526966],"domain_scores_gemma":[0.9993189,0.00016697968,0.0001441957,0.000063031766,0.00013202503,0.00017486697],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011412784,0.00007725756,0.00013406896,0.00013591324,0.00045265205,0.00017785095,0.00028851032,0.000046799603,0.00062202115],"category_scores_gemma":[0.00019654329,0.000038715163,0.000033878434,0.00034994088,0.0006277545,0.0007813268,0.0000031333227,0.000111521076,0.000013057984],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025145779,0.000009474298,0.9600447,0.000039888208,0.000006528102,0.00001443505,0.006107945,0.0003891933,0.000020091731,0.00024306239,0.000516321,0.03258325],"study_design_scores_gemma":[0.00022061937,0.00058397744,0.95481396,0.000059170416,0.0000098583905,0.00039324642,0.0010003576,0.0013584037,0.000620113,0.0018510617,0.03899053,0.000098729186],"about_ca_topic_score_codex":0.015352646,"about_ca_topic_score_gemma":0.5181432,"teacher_disagreement_score":0.5027906,"about_ca_system_score_codex":0.0000012594187,"about_ca_system_score_gemma":0.00024791976,"threshold_uncertainty_score":0.9912042},"labels":[],"label_agreement":null},{"id":"W2885474322","doi":"10.1139/cjes-2018-0090","title":"Geology and geochemistry of pillow basalt in the Huilvshan region (west Junggar, China): implications for magma source and tectonic setting","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Basalt; Petrogenesis; Pillow lava; Magma; Plagioclase; Mantle (geology); Partial melting; Petrology; Volcanic rock; Quartz; Volcano; Paleontology","score_opus":0.015251386008132861,"score_gpt":0.21424994806070718,"score_spread":0.19899856205257432,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2885474322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9898173,0.0010548033,0.00006276383,0.007882425,0.000029396868,0.0000543926,0.000011545617,0.0000011858947,0.0010861846],"genre_scores_gemma":[0.99898374,0.000039108203,0.0005780014,0.00029217982,0.00007422093,3.6352594e-7,0.0000028248232,6.265953e-7,0.000028924678],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992489,0.000042309264,0.00021786086,0.00014549472,0.00008133987,0.00026407326],"domain_scores_gemma":[0.99927896,0.00021528733,0.00015654777,0.000072652816,0.00007737168,0.00019916907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007095187,0.000068635854,0.0001450193,0.00011931251,0.00031687153,0.000047663212,0.00027579942,0.000043557386,0.00024961669],"category_scores_gemma":[0.0003008424,0.000040853254,0.000039813818,0.0003357714,0.0011763488,0.00009596045,0.0000068383392,0.000104708364,9.956976e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000044874605,0.0000024874792,0.993242,0.0000076499555,0.0000042119377,0.0000024183946,0.00019241919,0.00006941128,0.00018614062,0.000062974075,0.000056749403,0.006169052],"study_design_scores_gemma":[0.00010682015,0.00026271242,0.98956674,0.000017685841,0.00001228231,0.00020907607,0.00035211435,0.0013357162,0.00016930653,0.0069623557,0.0009464129,0.000058794743],"about_ca_topic_score_codex":0.01076703,"about_ca_topic_score_gemma":0.25191996,"teacher_disagreement_score":0.24115293,"about_ca_system_score_codex":6.989129e-7,"about_ca_system_score_gemma":0.00018459214,"threshold_uncertainty_score":0.99582034},"labels":[],"label_agreement":null},{"id":"W2886917623","doi":"10.1139/cjes-2017-0234","title":"Lithostratigraphy and sedimentary environment of the Precambrian Kushk Series of central Iran","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"College of Family Physicians of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto Mississauga; Geological Survey and Mineral Exploration of Iran; University of Toronto; Islamic Azad University","keywords":"Geology; Precambrian; Paleontology; Lithostratigraphy; Marine transgression; Gondwana; Sedimentology; Sedimentary rock; Series (stratigraphy); Ecological succession; Rift; Biota; Stromatolite; Structural basin; Carbonate","score_opus":0.016247002747381188,"score_gpt":0.19043952712563744,"score_spread":0.17419252437825625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2886917623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98606527,0.0038409024,0.00000464061,0.0005267225,0.00038955818,0.000060950497,0.000043096104,7.735727e-7,0.0090680905],"genre_scores_gemma":[0.99888027,0.00006134847,0.0009391831,0.0000416395,0.00006376532,4.953973e-8,2.568287e-7,3.2537818e-7,0.000013155249],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99905825,0.00008434129,0.00028489417,0.00010230303,0.00021305846,0.00025713543],"domain_scores_gemma":[0.9992981,0.000045014145,0.000251032,0.000087159635,0.000023042941,0.0002956403],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0004352083,0.000078132165,0.00015444309,0.00014037541,0.00030568257,0.000026570553,0.00031535164,0.000040594943,0.0002584459],"category_scores_gemma":[0.000023298304,0.000049207338,0.00007608982,0.00021719183,0.0033567152,0.00031256807,0.0000012064027,0.00009248775,4.777436e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011048399,0.000002808274,0.9920429,0.00000425676,0.000017420547,0.0000039550846,0.0007070464,0.000013475434,0.00012447867,0.000102245285,0.000037499678,0.006932878],"study_design_scores_gemma":[0.000102837526,0.0007092747,0.99518216,0.00003988503,0.000015320795,0.00008056759,0.0005378499,0.000026681058,0.002112349,0.0005139181,0.00062527007,0.00005388999],"about_ca_topic_score_codex":0.007881568,"about_ca_topic_score_gemma":0.3468978,"teacher_disagreement_score":0.33901626,"about_ca_system_score_codex":3.944847e-7,"about_ca_system_score_gemma":0.00042629166,"threshold_uncertainty_score":0.99935555},"labels":[],"label_agreement":null},{"id":"W2886929440","doi":"10.1139/cjes-2018-0055","title":"Geological origins of seismic bright spot reflections in the Ordovician strata in the Halahatang area of the Tarim Basin, western China","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Ordovician; Karst; Tectonics; Paleontology; Volcano; Volcanism; Volcanic rock; Tarim basin; Paleozoic; Carbonate rock; Structural basin; Geochemistry; Seismology; Sedimentary rock","score_opus":0.03751300207978396,"score_gpt":0.25571084514996606,"score_spread":0.21819784307018208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2886929440","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9858443,0.00020262088,0.000032920296,0.00727147,0.00028380894,0.00009298912,0.000026867749,0.0000020179662,0.006243013],"genre_scores_gemma":[0.9976374,0.00002132342,0.00019915368,0.0020325491,0.000070511225,1.6926498e-7,0.0000010814573,9.0649183e-7,0.000036893704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99868184,0.00026953535,0.00032890565,0.00011744727,0.00032982632,0.0002724439],"domain_scores_gemma":[0.99930006,0.00014761412,0.0002158631,0.00018909537,0.00006439667,0.00008294685],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020187243,0.000082066595,0.00014984024,0.0002752812,0.0003470194,0.000077916724,0.0012197971,0.000036201072,0.0002809733],"category_scores_gemma":[0.00012944193,0.00003602298,0.00006289654,0.0010622003,0.0014413053,0.00027655793,0.000006661387,0.000295766,0.0000037639152],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000048922207,0.000009086366,0.99462885,0.0000024500362,0.0000026635555,0.000019384192,0.0019430468,0.00036994374,0.000014501538,0.00021887533,0.0006264545,0.0021598646],"study_design_scores_gemma":[0.00007779353,0.00024984486,0.9724689,0.00007289105,0.000006308759,0.00017468042,0.0020259477,0.0015436074,0.0003127521,0.0015398798,0.02147335,0.000054060078],"about_ca_topic_score_codex":0.22795324,"about_ca_topic_score_gemma":0.60374266,"teacher_disagreement_score":0.3757894,"about_ca_system_score_codex":0.0000051311654,"about_ca_system_score_gemma":0.00084295444,"threshold_uncertainty_score":0.7771879},"labels":[],"label_agreement":null},{"id":"W2887357510","doi":"10.1139/cjes-2018-0015","title":"Late Wisconsinan Cordilleran and Laurentide glaciation of the Peace River Valley east of the Rocky Mountains, British Columbia","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Lethbridge; Simon Fraser University; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Ice sheet; Wisconsin glaciation; Glacial period; Paleontology; Geomorphology; Ice stream; Oceanography; Cryosphere; Sea ice","score_opus":0.014146578309108655,"score_gpt":0.20337997663917623,"score_spread":0.18923339833006758,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2887357510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99571365,0.0010256714,0.0000017445163,0.0007891231,0.0004693911,0.0000777913,0.000027219829,7.993912e-7,0.0018946176],"genre_scores_gemma":[0.9992056,0.000048310154,0.00008531625,0.00011184346,0.00004089224,6.0545574e-8,6.2099474e-7,8.596244e-7,0.0005065043],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989629,0.00020328723,0.00023043605,0.000105315026,0.0002401518,0.00025792085],"domain_scores_gemma":[0.9991911,0.000085313695,0.00025603245,0.00010032364,0.00020118449,0.00016604649],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00086121145,0.00004876359,0.00014802026,0.00006582762,0.0007438208,0.00008474673,0.00045464665,0.000053474465,0.0007877753],"category_scores_gemma":[0.00020039864,0.000036989364,0.00005565942,0.00036877574,0.0037210255,0.00017914784,0.0000129768005,0.0001640545,0.0000044015974],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004059172,0.0000019752406,0.9986058,0.0000051470115,0.000009791229,0.0000054097127,0.00041356476,0.00008812678,0.0000076104034,0.00001116012,0.0003306342,0.0005167547],"study_design_scores_gemma":[0.00014633877,0.00015387964,0.9972725,0.00006730348,0.000010932374,0.00024113125,0.0002908812,0.0003562774,0.000032633852,0.00049365975,0.00089226704,0.000042224143],"about_ca_topic_score_codex":0.10742109,"about_ca_topic_score_gemma":0.9856886,"teacher_disagreement_score":0.8782675,"about_ca_system_score_codex":4.869716e-7,"about_ca_system_score_gemma":0.00092736445,"threshold_uncertainty_score":0.9989903},"labels":[],"label_agreement":null},{"id":"W2887472087","doi":"10.1139/cjes-2018-0034","title":"Revealing rangeomorph species characters using spatial analyses","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Newnham College, University of Cambridge; Natural Environment Research Council; Sight Research UK; Natural England; Cambridge Philosophical Society","keywords":"Intraspecific competition; Spatial distribution; Biology; Ecology; Branching (polymer chemistry); Evolutionary biology; Geography; Chemistry","score_opus":0.10370885334715592,"score_gpt":0.2876872258136097,"score_spread":0.18397837246645382,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2887472087","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97866535,0.002417242,0.0002568443,0.00025193175,0.0011342642,0.00003595221,0.000025730398,0.0000033366737,0.017209355],"genre_scores_gemma":[0.997438,0.000017378343,0.0017823786,0.00012368301,0.00060821004,2.2229479e-8,7.5984616e-7,5.214036e-7,0.000029040253],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987891,0.00008968147,0.0003047871,0.00014488824,0.00025116513,0.0004204152],"domain_scores_gemma":[0.9989419,0.000081920225,0.00025668918,0.00007753213,0.00014008088,0.00050189707],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00080953207,0.00010444781,0.00021070923,0.00046632538,0.0008183401,0.00016840684,0.00038794865,0.000054843553,0.0011973486],"category_scores_gemma":[0.000123817,0.00007904431,0.00010202349,0.00047180854,0.0016059797,0.0005032684,6.564892e-7,0.00014152913,0.000014369481],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012215972,0.0000015314703,0.99044716,0.0000023630184,0.000023225302,0.00009918876,0.00036328542,0.00015584852,0.00048455532,0.000046339217,0.00004938895,0.008314891],"study_design_scores_gemma":[0.0001052265,0.00027097165,0.9963762,0.000041722036,0.000021026615,0.00021302163,0.0002829772,0.0010683218,0.0006791169,0.0002482228,0.0005863315,0.000106823965],"about_ca_topic_score_codex":0.037793007,"about_ca_topic_score_gemma":0.6394662,"teacher_disagreement_score":0.6016732,"about_ca_system_score_codex":0.0000011083376,"about_ca_system_score_gemma":0.0010987782,"threshold_uncertainty_score":0.9997157},"labels":[],"label_agreement":null},{"id":"W2887529059","doi":"10.1139/cjes-2018-0056","title":"S-type granites in the western Superior Province: a marker of Archean collision zones","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor; University of Manitoba; Manitoba Hydro","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Zircon; Partial melting; Terrane; Granulite; Pluton; Metamorphism; Migmatite; Anatexis; Felsic; Petrology; Archean; Mafic; Crust; Metamorphic rock; Gneiss; Tectonics; Facies; Geomorphology","score_opus":0.0221425208466447,"score_gpt":0.21576584029761872,"score_spread":0.19362331945097402,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2887529059","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956405,0.00070665305,0.000003869681,0.0015752636,0.00012413546,0.000047971065,0.000009056212,9.567734e-7,0.0018915863],"genre_scores_gemma":[0.99912566,0.000019336683,0.0003494001,0.00035016172,0.000091263726,6.2436605e-8,0.0000012072153,5.356642e-7,0.000062352185],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99893963,0.00010711571,0.0002755941,0.00011223917,0.000289655,0.00027576377],"domain_scores_gemma":[0.99930966,0.00014626379,0.000114677365,0.000074968964,0.0001406226,0.00021383283],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011170738,0.000070828035,0.00016385267,0.00020407772,0.00019089397,0.00007421793,0.0005231252,0.00003249603,0.0015017827],"category_scores_gemma":[0.00025819804,0.000035787423,0.000060620754,0.0008391762,0.0010807358,0.00017817067,0.000004751574,0.00011748751,0.000027723196],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013857445,0.0000048731767,0.9978824,0.0000033893996,0.0000034094608,0.000025576617,0.00033344777,0.00013238669,0.000049694227,0.000022135791,0.000049288392,0.0014795375],"study_design_scores_gemma":[0.00007966398,0.0006183493,0.9935067,0.000036569374,0.000008444896,0.000050384653,0.0005011072,0.00049766264,0.00020619422,0.0019300408,0.0025056452,0.00005919909],"about_ca_topic_score_codex":0.033874396,"about_ca_topic_score_gemma":0.7486656,"teacher_disagreement_score":0.7147912,"about_ca_system_score_codex":6.8186716e-7,"about_ca_system_score_gemma":0.00054273906,"threshold_uncertainty_score":0.999411},"labels":[],"label_agreement":null},{"id":"W2887789178","doi":"10.1139/cjes-2018-0041","title":"Origin of Late Triassic mafic–ultramafic intrusions in the Hongqiling Ni–Cu sulfide deposit, Northeast China: evidence from trace element and Sr–Nd isotope geochemistry","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Mafic; Ultramafic rock; Partial melting; Mantle (geology); Trace element; Petrology; Layered intrusion","score_opus":0.021510734308172956,"score_gpt":0.22128735220449716,"score_spread":0.1997766178963242,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2887789178","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99286276,0.0042086006,0.000017095645,0.002267172,0.00013230438,0.00006988803,0.000040547977,0.0000019551437,0.00039969262],"genre_scores_gemma":[0.9987922,0.00017972253,0.0007142526,0.00013423669,0.00014098185,2.9840675e-7,0.0000032156809,0.0000010154423,0.0000341103],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99840415,0.000121377416,0.00047697462,0.0002405067,0.00036564202,0.00039133773],"domain_scores_gemma":[0.99880165,0.0003373661,0.00024772916,0.00013099755,0.00009332463,0.0003889223],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012258141,0.00013069723,0.00026662022,0.00015333854,0.0003592156,0.00013691548,0.00062830205,0.000054931304,0.0023282194],"category_scores_gemma":[0.00035295123,0.000075030766,0.000081102444,0.0007729541,0.0008714299,0.00026414223,0.000010250621,0.00025336267,0.000010455113],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017772607,0.000007855933,0.9930716,0.0000049957853,0.000011318417,0.00004043759,0.000729883,0.00044386173,0.0008561495,0.0000054501083,0.000034851993,0.004775809],"study_design_scores_gemma":[0.00016446225,0.00024911843,0.9923861,0.0001399743,0.000032950586,0.000046197154,0.00077557744,0.0028823956,0.0011155625,0.0018414585,0.0002540004,0.00011217537],"about_ca_topic_score_codex":0.15302247,"about_ca_topic_score_gemma":0.7367925,"teacher_disagreement_score":0.58377004,"about_ca_system_score_codex":0.0000023783682,"about_ca_system_score_gemma":0.00037797767,"threshold_uncertainty_score":0.9985838},"labels":[],"label_agreement":null},{"id":"W2887959252","doi":"10.1139/cjes-2018-0049","title":"Geological interpretation of the northern flank of the Matagami camp, Quebec, using gravity and magnetic inversions","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Polytechnique Montréal","funders":"","keywords":"Geology; Anticline; Flank; Magnetic anomaly; Geophysics; Volcano; Outcrop; Prospectivity mapping; Mafic; Inversion (geology); Gravity anomaly; Seismology; Paleontology; Tectonics","score_opus":0.019616909381058707,"score_gpt":0.2246336842115613,"score_spread":0.2050167748305026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2887959252","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984431,0.00027146706,0.00005549059,0.000540394,0.00028538454,0.000049343336,0.000010272298,5.8507163e-7,0.00034395355],"genre_scores_gemma":[0.9990794,0.000003126843,0.0006880168,0.00013078302,0.000044836317,2.3734065e-8,1.2370222e-7,4.98463e-7,0.000053174263],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991668,0.000186125,0.00019281669,0.000080981496,0.00020177776,0.00017153901],"domain_scores_gemma":[0.9993105,0.00014856372,0.00018944108,0.00007853426,0.00010619846,0.0001667551],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004599069,0.00005414551,0.00012240079,0.00006751044,0.00027970938,0.000027664715,0.00036695288,0.00003032431,0.00023944216],"category_scores_gemma":[0.0003135842,0.000024962032,0.000061561506,0.00052701676,0.0015691563,0.00010704621,0.000012214191,0.00011603678,0.000002502112],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007589858,0.0000032109774,0.97388816,0.000004725553,0.000003795686,0.0000012765671,0.0004217267,0.0006842325,0.00023949248,0.0000671283,0.000013833335,0.024664834],"study_design_scores_gemma":[0.00004971315,0.00025634008,0.9884503,0.000035250698,0.000013163417,0.00002266353,0.00014490237,0.007696234,0.0004627121,0.0026520079,0.00018047598,0.00003627419],"about_ca_topic_score_codex":0.081450686,"about_ca_topic_score_gemma":0.70629114,"teacher_disagreement_score":0.62484044,"about_ca_system_score_codex":0.0000012970356,"about_ca_system_score_gemma":0.00051236874,"threshold_uncertainty_score":0.924666},"labels":[],"label_agreement":null},{"id":"W2888010473","doi":"10.1139/cjes-2018-0111","title":"Solar activity expressed in a modern varve thickness sequence","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"National Centers for Environmental Information; National Oceanic and Atmospheric Administration; California Polytechnic State University, San Luis Obispo","keywords":"Varve; Forcing (mathematics); Geology; Atmospheric sciences; Meltwater; Climate change; Climatology; Sediment; Glacial period; Environmental science; Geomorphology; Oceanography","score_opus":0.057148970069036215,"score_gpt":0.273816570892242,"score_spread":0.21666760082320577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888010473","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905776,0.00036392917,0.000111602545,0.0009950915,0.0004461346,0.000057307105,0.000015454805,0.00000293606,0.007429969],"genre_scores_gemma":[0.999018,0.00001935954,0.0005850427,0.0001973256,0.00009562385,1.9489194e-7,7.8500915e-7,0.0000011300477,0.00008249644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984738,0.00025539877,0.00020859786,0.00019616276,0.00025520337,0.000610818],"domain_scores_gemma":[0.99891406,0.0002235508,0.00012066182,0.0001135031,0.00014780223,0.00048041105],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001922079,0.00009386452,0.0001956175,0.00046527974,0.00047015082,0.00009147786,0.0006262959,0.00010597001,0.0014499177],"category_scores_gemma":[0.00029612854,0.0000730414,0.000042988602,0.00058101193,0.0019641859,0.0005998604,0.0000062559297,0.0003723241,0.00011226546],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001835511,0.000003169636,0.99669456,0.00000355427,0.000004067676,0.00020324133,0.00055049424,0.0004256713,0.00008942668,0.000038515474,0.000017717093,0.0019511952],"study_design_scores_gemma":[0.00017879838,0.0003400674,0.98719215,0.000037014695,0.0000031162008,0.00042397456,0.0002107687,0.0067666294,0.0004146778,0.0038426614,0.00048490617,0.00010522743],"about_ca_topic_score_codex":0.012272656,"about_ca_topic_score_gemma":0.82662,"teacher_disagreement_score":0.8143473,"about_ca_system_score_codex":6.74895e-7,"about_ca_system_score_gemma":0.0022800048,"threshold_uncertainty_score":0.9994629},"labels":[],"label_agreement":null},{"id":"W2888197475","doi":"10.1139/cjes-2018-0047","title":"Evaluation of mineral exploration targets defined by airborne gravity gradiometry through gravity and magnetic modelling: vicinity of the Iron Range Fault, Purcell anticlinorium, southern Canadian Cordillera","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"College of the Rockies; Geological Survey of Canada","funders":"Monash University","keywords":"Geology; Gradiometer; Gravity anomaly; Magnetic anomaly; Sill; Fault (geology); Anticline; Mineralization (soil science); Geophysics; Geochemistry; Seismology; Tectonics; Magnetometer; Paleontology; Magnetic field","score_opus":0.04909875877537331,"score_gpt":0.25405170780442826,"score_spread":0.20495294902905495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888197475","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99601614,0.0017558102,0.0002709322,0.0006243844,0.00037032546,0.00016880158,0.00013108955,0.0000016418624,0.00066088384],"genre_scores_gemma":[0.9979063,0.00002552304,0.0018156111,0.00010451592,0.000108852786,2.8731455e-7,0.000004876175,0.0000023057405,0.000031716456],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977879,0.00046962328,0.00040574552,0.00020113417,0.000743195,0.0003923831],"domain_scores_gemma":[0.9982814,0.00014544468,0.0003249075,0.00013304019,0.00062031794,0.00049484137],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023118735,0.00013432126,0.00028171943,0.00022719344,0.00040604462,0.00005662362,0.00034541875,0.00007195285,0.0003208604],"category_scores_gemma":[0.00040905477,0.00008835842,0.000082112034,0.0011332121,0.0009520362,0.00032701166,0.0000053165045,0.00017918798,0.0000055499804],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000066719695,0.000081302336,0.87657595,0.000049727052,0.00004512229,0.000007056979,0.003975636,0.019975968,0.001440508,0.00014407861,0.00035833745,0.09727958],"study_design_scores_gemma":[0.00061997754,0.0016426495,0.8808154,0.000050388284,0.00015460166,0.000017160588,0.0005020987,0.0972756,0.001804731,0.016423283,0.00046123433,0.00023286903],"about_ca_topic_score_codex":0.523541,"about_ca_topic_score_gemma":0.80474645,"teacher_disagreement_score":0.28120553,"about_ca_system_score_codex":0.0000068561812,"about_ca_system_score_gemma":0.0011278064,"threshold_uncertainty_score":0.47963184},"labels":[],"label_agreement":null},{"id":"W2888289926","doi":"10.1139/cjes-2018-0096","title":"Genesis of the Changlingzi Zn–Pb deposit in the southern Great Xing’an Range, northeastern China: constraints from fluid inclusions and H–O–S–Pb isotope systematics","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Skarn; Geochemistry; Fluid inclusions; Mineralization (soil science); Magmatic water; Meteoric water; Hydrothermal circulation; Ore genesis; δ34S; Vein; Sulfide; Pyrite; Mineralogy; Chemistry; Paleontology","score_opus":0.018680080945003157,"score_gpt":0.1961148663696301,"score_spread":0.17743478542462696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888289926","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966695,0.0011392235,0.000041474657,0.0010310668,0.00014426462,0.00009655484,0.000085306114,0.0000015599541,0.0007910963],"genre_scores_gemma":[0.99903756,0.000017536617,0.00045316693,0.00033876862,0.00013315122,2.4245958e-7,0.0000018331111,0.0000011331476,0.000016619562],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861294,0.00021953299,0.0003746155,0.00015797817,0.000351363,0.00028354392],"domain_scores_gemma":[0.99907,0.00015907364,0.00022604296,0.00015096278,0.00009918362,0.00029476627],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009538307,0.0001098953,0.00024802712,0.00013027892,0.00055124686,0.0001067023,0.00074605894,0.000051579966,0.0010675231],"category_scores_gemma":[0.0001578211,0.000050116832,0.000083231454,0.0005422522,0.001341971,0.00013048941,0.000020352267,0.00013206758,0.000012700941],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000044754606,0.000005104936,0.9944388,0.000007267719,0.000011998593,0.00001628589,0.0033149917,0.0002083964,0.000133351,0.000013830616,0.0000042737224,0.001841202],"study_design_scores_gemma":[0.00015737253,0.00022919224,0.9873348,0.00015552412,0.000053087315,0.00009610436,0.004478105,0.00488253,0.0002192947,0.0022297027,0.000058097045,0.00010620207],"about_ca_topic_score_codex":0.16127588,"about_ca_topic_score_gemma":0.8367993,"teacher_disagreement_score":0.67552346,"about_ca_system_score_codex":0.000001259443,"about_ca_system_score_gemma":0.00021054829,"threshold_uncertainty_score":0.9998456},"labels":[],"label_agreement":null},{"id":"W2888315153","doi":"10.1139/cjes-2018-0103","title":"Reprocessing legacy three-dimensional seismic data from the Halfmile Lake and Brunswick No. 6 volcanogenic massive sulphide deposits, New Brunswick, Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Prestack; Context (archaeology); Mineral exploration; Mineralogy; Geochemistry; Paleontology","score_opus":0.02725484711179018,"score_gpt":0.2212646744625092,"score_spread":0.194009827350719,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888315153","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98109037,0.0061687934,0.00019518395,0.009719923,0.0014228692,0.000093390896,0.0001209124,0.000013143241,0.0011754438],"genre_scores_gemma":[0.9873603,0.00003674908,0.0032691823,0.00815608,0.0008190179,2.9733426e-8,0.00003349533,0.000004643461,0.0003204838],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99818707,0.00007546733,0.00035992436,0.00038597637,0.0005013287,0.0004902563],"domain_scores_gemma":[0.9981093,0.0002646842,0.00029660485,0.0003589935,0.00023209187,0.00073832145],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00081542926,0.00016667943,0.00020989009,0.00013140979,0.0011571383,0.0005026741,0.0012594517,0.00005247301,0.0012979113],"category_scores_gemma":[0.00038779658,0.00011143987,0.0000368217,0.0003955659,0.00096930756,0.0011230252,0.000038243674,0.00027853658,0.000041325045],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018819743,0.0000020852576,0.8151881,0.000003689464,0.000031468757,0.00012027641,0.00018063566,0.00024280006,0.00001771151,0.000014225909,0.15468107,0.029499076],"study_design_scores_gemma":[0.00030784536,0.00024135903,0.6454333,0.00022654647,0.000049363225,0.00039476235,0.00042965144,0.08526,0.00046217415,0.0007167826,0.2661556,0.00032262542],"about_ca_topic_score_codex":0.993586,"about_ca_topic_score_gemma":0.99978834,"teacher_disagreement_score":0.16975485,"about_ca_system_score_codex":0.000006301936,"about_ca_system_score_gemma":0.0322226,"threshold_uncertainty_score":0.999615},"labels":[],"label_agreement":null},{"id":"W2888842235","doi":"10.1139/cjes-2018-0027","title":"Pseudocryptic species of the Middle Cambrian trilobite <i>Eodiscus</i> Hartt, in Walcott, 1884, from Avalonian and Laurentian Newfoundland","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Trilobite; Baltica; Bay; Siliciclastic; Paleontology; Geology; Invertebrate; Fauna; Ecology; Biology; Sedimentary depositional environment; Oceanography; Ordovician","score_opus":0.026290786571363654,"score_gpt":0.20527361597960067,"score_spread":0.178982829408237,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888842235","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9696348,0.00470076,0.000004832385,0.0008183467,0.0008417263,0.00007139437,0.000078917474,0.0000017196825,0.023847539],"genre_scores_gemma":[0.9991355,0.00004072819,0.0003969329,0.00011931223,0.00018268693,8.645588e-8,9.357075e-7,7.2823406e-7,0.00012310948],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99866503,0.0001394069,0.0003748882,0.00017861681,0.00025173812,0.00039029503],"domain_scores_gemma":[0.9990587,0.000117979194,0.0002472702,0.00013249724,0.000068088375,0.00037544259],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006427489,0.00012006928,0.0002484781,0.00028970078,0.00046502418,0.00013914134,0.0005153204,0.00006529933,0.0006632582],"category_scores_gemma":[0.00009874409,0.000075129654,0.000086815926,0.0005175647,0.0023160458,0.00038929266,0.0000023531954,0.00019289112,0.0000063552297],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012479086,0.0000031213476,0.9962606,0.0000032811488,0.0000115815565,0.000024249895,0.0010636882,0.000012503882,0.00006463181,0.00013970387,0.00012848445,0.002275721],"study_design_scores_gemma":[0.00028949112,0.0002427532,0.9949533,0.0000971527,0.000015501999,0.00007003289,0.00051724486,0.00017521612,0.00010402603,0.0011563004,0.0022821128,0.000096919815],"about_ca_topic_score_codex":0.073991224,"about_ca_topic_score_gemma":0.9802711,"teacher_disagreement_score":0.9062799,"about_ca_system_score_codex":0.000001576596,"about_ca_system_score_gemma":0.0008605502,"threshold_uncertainty_score":0.93217516},"labels":[],"label_agreement":null},{"id":"W2889746742","doi":"10.1139/cjes-2018-0035","title":"New occurrences of <i>Palaeopascichnus</i> from the Stáhpogieddi Formation, Arctic Norway, and their bearing on the age of the Varanger Ice Age","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland","funders":"Norges Forskningsråd","keywords":"Baltica; Geology; Paleontology; Arctic; Peninsula; Range (aeronautics); Glacier; Ice age; Physical geography; Ordovician; Glacial period; Oceanography; Archaeology; Geography","score_opus":0.030118530087952036,"score_gpt":0.21107976613052556,"score_spread":0.18096123604257353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2889746742","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98219025,0.004018332,0.00004729383,0.0022519208,0.00051102316,0.00009411471,0.000059740432,0.000001273115,0.010826078],"genre_scores_gemma":[0.9992947,0.00004610063,0.00017547407,0.0003363278,0.00012928933,1.0962691e-7,4.673309e-7,4.4308624e-7,0.000017064473],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989234,0.00016722282,0.00029870227,0.00011021523,0.0002583236,0.00024212577],"domain_scores_gemma":[0.99853927,0.00072310294,0.00033045208,0.0001648727,0.00008517347,0.00015711541],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010277733,0.00010033659,0.00016675163,0.000085808104,0.00074476836,0.00010477577,0.0008768481,0.000040956173,0.00023921177],"category_scores_gemma":[0.0002064404,0.000040783227,0.000084824715,0.0004251261,0.0022529485,0.00030555236,0.0000035218695,0.00019867794,0.0000026116372],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016325277,0.0000031158208,0.96795416,0.00000616859,0.00003093847,0.000006478735,0.0061151087,0.000057224544,0.00013517606,0.000457046,0.00066923373,0.024549011],"study_design_scores_gemma":[0.00008412738,0.00022120978,0.9928599,0.00011631936,0.000013783221,0.000023926337,0.001326959,0.00010711822,0.0005503047,0.0032261522,0.001415357,0.0000548627],"about_ca_topic_score_codex":0.026804557,"about_ca_topic_score_gemma":0.6340353,"teacher_disagreement_score":0.6072307,"about_ca_system_score_codex":6.7568e-7,"about_ca_system_score_gemma":0.00058163214,"threshold_uncertainty_score":0.979676},"labels":[],"label_agreement":null},{"id":"W2889781170","doi":"10.1139/cjes-2018-0123","title":"Petrographic and geochemical characteristics of organic-rich shale and tuff of the Upper Triassic Yanchang Formation, Ordos Basin, China: implications for lacustrine fertilization by volcanic ash","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Petrography; Oil shale; Volcanic ash; Total organic carbon; Organic matter; Sedimentation; Volcano; Organic geochemistry; Sediment; Source rock; Structural basin; Geomorphology; Paleontology","score_opus":0.014815640516051881,"score_gpt":0.21671887995820366,"score_spread":0.20190323944215177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2889781170","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99620485,0.0019338941,0.00021754469,0.00095855456,0.00011923397,0.00010629536,0.00016986833,0.0000012962502,0.000288432],"genre_scores_gemma":[0.99960244,0.00007679942,0.00022927049,0.00003516875,0.00004344271,3.734809e-7,0.0000040852397,5.9545266e-7,0.000007823002],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992959,0.000038543112,0.00029750803,0.00009426705,0.000098020944,0.00017574494],"domain_scores_gemma":[0.99917483,0.00009644209,0.0003058626,0.00006947589,0.00018461354,0.00016878231],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004256793,0.00006712027,0.00015878101,0.00015331872,0.00035503585,0.000037905415,0.00019501659,0.000050186794,0.000054534354],"category_scores_gemma":[0.00023508698,0.00004532526,0.000039128212,0.00044017626,0.00084799743,0.0002590871,0.0000016309684,0.000068108115,1.2943002e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000879069,0.0000034712507,0.99368143,0.000011327821,0.000008264378,1.1531356e-7,0.00017681535,3.7153416e-7,0.0006194941,0.00010004382,0.00012534847,0.0052645435],"study_design_scores_gemma":[0.00018874841,0.00027390028,0.99715257,0.000028720931,0.000023280325,0.000047298465,0.00011148352,0.00023066504,0.0010749011,0.0006176768,0.00020152309,0.000049214508],"about_ca_topic_score_codex":0.0005468837,"about_ca_topic_score_gemma":0.08346259,"teacher_disagreement_score":0.08291571,"about_ca_system_score_codex":7.533185e-7,"about_ca_system_score_gemma":0.00031297305,"threshold_uncertainty_score":0.9332618},"labels":[],"label_agreement":null},{"id":"W2890773639","doi":"10.1139/cjes-2018-0167","title":"Deglacial and postglacial paleoseismological archives in mass movement deposits of lakes of south-central Québec","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Center for Northern Studies","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Bathymetry; Mass movement; Marine transgression; Deglaciation; Seismology; Landslide; Oceanography; Paleontology; Holocene; Structural basin","score_opus":0.01943956893493758,"score_gpt":0.22297802654726853,"score_spread":0.20353845761233094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2890773639","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996289,0.0010630897,0.00002279191,0.00045531776,0.00020230978,0.000057554524,0.000012232971,8.673279e-7,0.0018968363],"genre_scores_gemma":[0.99913156,0.000024878953,0.00066453806,0.000092523784,0.00006282275,9.134882e-8,8.608222e-7,6.910277e-7,0.000022055243],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987628,0.00015650003,0.00034302095,0.00012996022,0.0001814768,0.00042626003],"domain_scores_gemma":[0.99918807,0.00019542626,0.00017184332,0.000052280535,0.000060097147,0.00033230727],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0005719322,0.000077882745,0.00023545591,0.00037164244,0.00017230316,0.000018999393,0.0002996337,0.00006711496,0.00039634248],"category_scores_gemma":[0.00018183546,0.000057215155,0.0000450253,0.00025558085,0.0031445855,0.00011530686,0.000006278126,0.0001611761,0.0000037542557],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000059696526,0.0000049594805,0.99733263,0.0000076191573,0.000008620726,0.00006239347,0.0014305982,0.00009597709,0.000073578805,0.000106929816,0.000002109083,0.00081489567],"study_design_scores_gemma":[0.00023460874,0.0009017186,0.99639314,0.000030588,0.000005586436,0.00007522314,0.00045407368,0.00037344778,0.00048592236,0.0009316109,0.000056163004,0.00005791937],"about_ca_topic_score_codex":0.014754417,"about_ca_topic_score_gemma":0.9184513,"teacher_disagreement_score":0.9036969,"about_ca_system_score_codex":3.417008e-7,"about_ca_system_score_gemma":0.001401371,"threshold_uncertainty_score":0.9995683},"labels":[],"label_agreement":null},{"id":"W2891105393","doi":"10.1139/cjes-2018-0071","title":"Late Tortonian – Piacenzian multi-proxy record of Asian southwest monsoon intensification: evidence from Coastal Makran, southeast Iran","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Weathering; Monsoon; East Asian Monsoon; Oceanography; Paleoclimatology; Climatology; Paleontology; Climate change","score_opus":0.07399253174189552,"score_gpt":0.27322658961974927,"score_spread":0.19923405787785375,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2891105393","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929954,0.00085472397,0.00008661294,0.0024220333,0.0010034468,0.00011471233,0.00014990894,0.00000609347,0.0023670774],"genre_scores_gemma":[0.99551165,0.00003404902,0.003929552,0.00012414271,0.00021792982,2.753839e-7,0.000008892509,0.000003020375,0.00017047746],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99797446,0.0002558997,0.0005283474,0.0003000818,0.00033807365,0.00060314726],"domain_scores_gemma":[0.9979763,0.00022331672,0.00037379438,0.00022801317,0.0004212073,0.00077738386],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012540489,0.00015618707,0.00032697464,0.00044444145,0.0006166169,0.000099401695,0.0008180151,0.00013532014,0.0027776998],"category_scores_gemma":[0.00050091546,0.00012343192,0.00010154815,0.0005973232,0.0030175992,0.0004789057,0.000011167639,0.00034250328,0.00030492066],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047393845,0.0000053171566,0.99616,0.0000058765777,0.000018723542,0.0000626485,0.0022118578,0.000053078238,0.00005346765,0.000012165736,0.000035185873,0.001334338],"study_design_scores_gemma":[0.00022253091,0.0005874584,0.99273646,0.00016560777,0.000018710542,0.0001294763,0.0032027222,0.0016736197,0.00018719782,0.00018763324,0.0007514067,0.00013715086],"about_ca_topic_score_codex":0.05293985,"about_ca_topic_score_gemma":0.9282063,"teacher_disagreement_score":0.8752665,"about_ca_system_score_codex":8.160559e-7,"about_ca_system_score_gemma":0.0014191724,"threshold_uncertainty_score":0.9996956},"labels":[],"label_agreement":null},{"id":"W2891245622","doi":"10.1139/cjes-2017-0274","title":"Effects of bioturbation on carbon and sulfur cycling across the Ediacaran–Cambrian transition at the GSSP in Newfoundland, Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada; Queen's University; Pennsylvania State University; University of Pennsylvania; NASA Astrobiology Institute; National Aeronautics and Space Administration; National Science Foundation","keywords":"Bioturbation; Geology; Paleontology; Benthic zone; Global Boundary Stratotype Section and Point; Phanerozoic; Ordovician; Sulfur cycle; Carbon cycle; Isotopes of carbon; Pyrite; Carbonate; Extinction event; Total organic carbon; Sediment; Geochemistry; Oceanography; Ecosystem; Ecology; Environmental chemistry; Biostratigraphy; Chemistry","score_opus":0.009426018837044931,"score_gpt":0.2101745058162659,"score_spread":0.20074848697922096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2891245622","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99139476,0.003028407,0.0000019874942,0.0014774831,0.000613572,0.00008406935,0.000015869802,6.8698574e-7,0.0033831606],"genre_scores_gemma":[0.99962044,0.000035103025,0.000014569867,0.00019041085,0.00012969071,1.4962811e-7,4.909688e-7,3.871637e-7,0.000008789187],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990746,0.00012899605,0.00020383672,0.00010437591,0.00022053976,0.00026766665],"domain_scores_gemma":[0.9992214,0.00037432802,0.00014137593,0.00005865805,0.0000426974,0.00016154043],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00088377524,0.00007329684,0.00012217902,0.000089913694,0.00056639075,0.000052001415,0.00020906543,0.00004228243,0.000019064644],"category_scores_gemma":[0.00008594004,0.000039757113,0.000030202094,0.0002985602,0.0010170065,0.000120206525,6.0870843e-7,0.00014115144,3.797702e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031601554,0.000001441812,0.9831227,0.0000063396224,0.0000077846225,0.000026548018,0.001843725,0.00020681936,0.00012225215,0.000037045116,0.000017458051,0.014576307],"study_design_scores_gemma":[0.00018631031,0.00029993127,0.99777114,0.000048760037,0.0000069887865,0.000045600584,0.00038855235,0.0004984311,0.00043801244,0.00010916595,0.00015688421,0.000050222054],"about_ca_topic_score_codex":0.8538348,"about_ca_topic_score_gemma":0.9997921,"teacher_disagreement_score":0.14595732,"about_ca_system_score_codex":0.0000041332814,"about_ca_system_score_gemma":0.00094151055,"threshold_uncertainty_score":0.4356277},"labels":[],"label_agreement":null},{"id":"W2891980837","doi":"10.1139/cjes-2018-0059","title":"Carbon-isotope stratigraphy of the Furongian Berry Head Formation (Port au Port Group) and Tremadocian Watts Bight Formation (St. George Group), western Newfoundland, and the correlative significance","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Cove; Paleontology; Ordovician; Conodont; Group (periodic table); Stratigraphy; Bay; Chemostratigraphy; Biostratigraphy; Isotopes of carbon; Oceanography; Geomorphology; Total organic carbon; Tectonics","score_opus":0.017687158663902667,"score_gpt":0.21525668089595199,"score_spread":0.19756952223204932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2891980837","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9801065,0.0019493755,0.0001430822,0.0007975538,0.00044705567,0.00026575988,0.00003718997,0.0000024912451,0.016251026],"genre_scores_gemma":[0.99959904,0.000050479437,0.00013282805,0.00008997886,0.0001059942,8.627645e-7,0.000002410129,8.528057e-7,0.000017554006],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99853295,0.00020814479,0.00045303858,0.00015182236,0.0003080718,0.00034595185],"domain_scores_gemma":[0.99877,0.00014966686,0.0005805625,0.00011548891,0.00008967972,0.00029460367],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0014518211,0.00013979783,0.0002490571,0.0002289411,0.00090205274,0.00013179683,0.0003294163,0.0000646896,0.000028129034],"category_scores_gemma":[0.000044084278,0.0000766682,0.00008186568,0.00044204592,0.0036693327,0.0010207479,0.000002476392,0.0002033856,5.473218e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038242626,0.0000027540088,0.98709935,0.000009231298,0.00001613772,0.0000058807013,0.0023974534,0.000008828568,0.000015458598,0.0005955057,0.000007738883,0.009803432],"study_design_scores_gemma":[0.00041501955,0.00048471507,0.99457884,0.000055036406,0.000029118777,0.00024597865,0.0012011272,0.00094185735,0.000022796088,0.0015814853,0.00034252784,0.00010147555],"about_ca_topic_score_codex":0.04814267,"about_ca_topic_score_gemma":0.97248214,"teacher_disagreement_score":0.9243395,"about_ca_system_score_codex":0.0000031673737,"about_ca_system_score_gemma":0.00038204173,"threshold_uncertainty_score":0.9990421},"labels":[],"label_agreement":null},{"id":"W2892240099","doi":"10.1139/cjes-2018-0105","title":"Iron mineralogy characteristics of the desert sediments of the Tarim Basin and its provenance implications","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Iron oxide chemistry and applications","field":"Energy","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China","keywords":"Provenance; Geology; Aeolian processes; Tarim basin; Hematite; Desert (philosophy); Geochemistry; Sediment; Structural basin; Mineralogy; Geomorphology","score_opus":0.019538141425797826,"score_gpt":0.23752438666457654,"score_spread":0.21798624523877871,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2892240099","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99368036,0.0000713123,0.0000049794457,0.0026752804,0.000114310395,0.000049053313,0.000025093714,5.7052955e-7,0.0033790225],"genre_scores_gemma":[0.99920523,0.000005765617,0.00013213442,0.0001610585,0.00007007727,0.0000011768241,2.8254095e-7,0.0000019697936,0.00042228008],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99950415,0.000020757738,0.00019991871,0.000066156514,0.0000880443,0.000120946956],"domain_scores_gemma":[0.9993269,0.00002721518,0.00027243272,0.00013003433,0.0001476756,0.00009577201],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016681089,0.00004330726,0.000080699516,0.000026728621,0.00022961505,0.00001326549,0.0003800829,0.000025542418,0.000048723447],"category_scores_gemma":[0.00011720659,0.000025180963,0.000031071344,0.0002356935,0.00064975664,0.00006601982,0.000016123919,0.00006216917,9.084351e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000071925665,0.000037959817,0.28305534,0.00004253227,0.00002014946,8.6508044e-7,0.0010279715,0.000090867674,0.6548552,0.05668832,0.001001842,0.003171776],"study_design_scores_gemma":[0.00008499958,0.000047044363,0.8467791,0.00005237454,0.000012885892,0.000034081255,0.000065055174,0.000050579143,0.13444287,0.0010076643,0.017378064,0.000045280936],"about_ca_topic_score_codex":0.0012709583,"about_ca_topic_score_gemma":0.010072431,"teacher_disagreement_score":0.56372374,"about_ca_system_score_codex":0.0000047775716,"about_ca_system_score_gemma":0.00055348367,"threshold_uncertainty_score":0.56206524},"labels":[],"label_agreement":null},{"id":"W2893276969","doi":"10.1139/cjes-2018-0014","title":"Petrology, mineral chemistry, and geochemistry of Late Triassic Ni–Cu ore-bearing mafic–ultramafic intrusions, Hongqiling, northeastern China: petrogenesis and tectonic implications","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"China Geological Survey; National Natural Science Foundation of China","keywords":"Geology; Geochemistry; Ultramafic rock; Mafic; Olivine; Layered intrusion; Petrogenesis; Gabbro; Magma; Fractional crystallization (geology); Chromite; Petrology; Basalt; Volcano","score_opus":0.01180085847302016,"score_gpt":0.20309041061956895,"score_spread":0.1912895521465488,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2893276969","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955659,0.0017345716,0.000008750821,0.001345922,0.00006960297,0.00003493608,0.00004515101,0.000004049188,0.0011911457],"genre_scores_gemma":[0.9990044,0.00009305468,0.000581478,0.000065252134,0.000131187,2.745218e-7,0.0000068430872,0.0000016186008,0.000115861454],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99879265,0.00003422396,0.0003704345,0.0002567043,0.00016607642,0.00037990027],"domain_scores_gemma":[0.9988375,0.00008119497,0.00025240466,0.00011590469,0.0001287117,0.0005843011],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004714837,0.00013540893,0.00028142487,0.00011535618,0.0003951871,0.000083959596,0.00032255778,0.000077005905,0.0020851546],"category_scores_gemma":[0.0001930379,0.000096053904,0.000077012184,0.00044759206,0.0015011535,0.00012701082,0.00001848269,0.00017013945,0.0000050855947],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001028977,0.0000051935376,0.9890347,0.0000116004285,0.000021313255,0.000007594351,0.000076209544,0.000090732436,0.0062740296,0.000006243647,0.000013285639,0.0044488143],"study_design_scores_gemma":[0.00020085719,0.00019672059,0.99340737,0.000025103975,0.00004858323,0.00022830085,0.00015440506,0.0019495577,0.0021618062,0.0013154862,0.00018765463,0.00012414527],"about_ca_topic_score_codex":0.01782242,"about_ca_topic_score_gemma":0.1348388,"teacher_disagreement_score":0.11701639,"about_ca_system_score_codex":0.0000016295653,"about_ca_system_score_gemma":0.00032962416,"threshold_uncertainty_score":0.9988271},"labels":[],"label_agreement":null},{"id":"W2893707435","doi":"10.1139/cjes-2018-0192","title":"Musings in tectonics","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Plate tectonics; Tectonics; Context (archaeology); Precambrian; Ophiolite; Lithosphere; Paleontology; Earth science","score_opus":0.019500877057036656,"score_gpt":0.19773171833130257,"score_spread":0.17823084127426592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2893707435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9775165,0.00048826134,0.000008897294,0.0010425079,0.00020652862,0.000015510414,0.000003610365,0.0000015845188,0.020716617],"genre_scores_gemma":[0.99820375,0.000008665055,0.0011076615,0.000506153,0.00012472048,1.9365567e-8,5.1336923e-7,3.9108932e-7,0.000048104317],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991523,0.000029047562,0.00021243354,0.00010779796,0.00017369656,0.00032473158],"domain_scores_gemma":[0.99932456,0.000054662345,0.00008557361,0.000047257992,0.0000911492,0.00039677607],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00061110465,0.00005800465,0.0001266656,0.00028187316,0.00018045685,0.000072723655,0.00032610638,0.000032317574,0.0120486915],"category_scores_gemma":[0.00021127817,0.000037494487,0.000052386993,0.00086679304,0.00075578166,0.0001895223,0.0000028372435,0.00011719127,0.00012502357],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000022723016,0.0000015688137,0.99537826,6.6825726e-7,0.0000021764238,0.000038549522,0.00007745643,0.00033668705,0.00003252976,0.00006662998,0.00005040493,0.0040128212],"study_design_scores_gemma":[0.00007921871,0.00028098174,0.9797024,0.000016323416,0.000004418826,0.000059899136,0.00013137107,0.0018024441,0.00027641526,0.009937431,0.0076321717,0.000076889526],"about_ca_topic_score_codex":0.0459533,"about_ca_topic_score_gemma":0.8494406,"teacher_disagreement_score":0.8034873,"about_ca_system_score_codex":8.001378e-7,"about_ca_system_score_gemma":0.00047334272,"threshold_uncertainty_score":0.9888544},"labels":[],"label_agreement":null},{"id":"W2894455335","doi":"10.1139/cjes-2017-0244","title":"Provenance analysis of the Dezadeash Formation (Jurassic–Cretaceous), Yukon, Canada: implications regarding a linkage between the Wrangellia composite terrane and the western margin of Laurasia","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon Agricultural Association; Yukon University","funders":"","keywords":"Geology; Provenance; Terrane; Geochemistry; Detritus; Laurasia; Paleocurrent; Forearc; Siliciclastic; Flysch; Volcanic arc; Back-arc basin; Paleontology; Sedimentary rock; Clastic rock; Subduction; Sedimentary depositional environment; Structural basin; Gondwana","score_opus":0.016879531980452712,"score_gpt":0.2017465619348189,"score_spread":0.18486702995436619,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2894455335","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9862557,0.0009845579,0.0000865008,0.011538708,0.000054513934,0.000098340395,0.000094296425,9.790186e-7,0.0008863767],"genre_scores_gemma":[0.99948066,0.000026663878,0.00009004682,0.0003009756,0.000056217254,3.3897564e-7,0.000004131888,7.0419327e-7,0.0000402835],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99878913,0.00014500687,0.0004238657,0.00011161337,0.0003029285,0.0002274729],"domain_scores_gemma":[0.9985186,0.0003239508,0.00061938114,0.0001629704,0.0002027269,0.00017235625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009234291,0.00008448596,0.0002908074,0.00012183349,0.0005555349,0.00006742682,0.0006560065,0.00003005106,0.00014465259],"category_scores_gemma":[0.00015894973,0.000034338715,0.00013831089,0.0013394372,0.0015794461,0.0001592238,0.0000137880415,0.00014066997,8.478205e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000061839623,0.0000010335621,0.99723357,0.0000044696485,0.000089635614,5.982506e-7,0.0002626433,0.00078954594,0.00004910226,0.00003390919,0.00006721716,0.0014620658],"study_design_scores_gemma":[0.000116924944,0.000044879376,0.9944297,0.00002940615,0.00031484623,0.000013199606,0.00016051545,0.0030124611,0.00032583915,0.00067578116,0.0008262843,0.00005015697],"about_ca_topic_score_codex":0.36555514,"about_ca_topic_score_gemma":0.9791425,"teacher_disagreement_score":0.6135874,"about_ca_system_score_codex":0.0000030807598,"about_ca_system_score_gemma":0.00042773015,"threshold_uncertainty_score":0.63866967},"labels":[],"label_agreement":null},{"id":"W2894490852","doi":"10.1139/cjes-2018-0122","title":"Paleomagnetism of the Mn wad deposit at Niimi hot springs, Hokkaido, Japan","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Paleomagnetism; Pyroclastic rock; Coercivity; Magnetite; Natural remanent magnetization; Geochemistry; Diagenesis; Manganese; Volcano; Mineralogy; Remanence; Apparent polar wander; Magnetization; Paleontology; Materials science","score_opus":0.01129932965013478,"score_gpt":0.21080895379433232,"score_spread":0.19950962414419754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2894490852","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9859926,0.0054771462,0.000012720375,0.0005805801,0.00076992565,0.00007730192,0.000023214892,0.0000013739336,0.0070651304],"genre_scores_gemma":[0.99705666,0.0001707822,0.00048027793,0.00027481443,0.00033503634,9.2922244e-7,0.0000010369419,0.000006458333,0.001673999],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987797,0.00006148268,0.0003060305,0.00020160132,0.00025020476,0.00040098545],"domain_scores_gemma":[0.9989976,0.000015114883,0.00025225227,0.00023989622,0.00019687548,0.00029824933],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037017436,0.00013484381,0.00017130897,0.000102727456,0.0005533064,0.000044357286,0.0006684517,0.00008012817,0.00017191857],"category_scores_gemma":[0.00013361195,0.000094274525,0.0001309035,0.0002502267,0.0016603434,0.000012182413,0.00008776278,0.000089303605,0.000011127957],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025637471,0.000013393005,0.8719058,0.000017452921,0.000042912685,0.000016955233,0.00062674953,0.000026796677,0.11837639,0.00014532692,0.0061459825,0.0026566198],"study_design_scores_gemma":[0.00030026227,0.0018043345,0.8629462,0.00006048106,0.000028026248,0.00025788904,0.00018551925,0.0000069236603,0.07585411,0.00008358432,0.058308028,0.00016465386],"about_ca_topic_score_codex":0.0016364797,"about_ca_topic_score_gemma":0.19877322,"teacher_disagreement_score":0.19713674,"about_ca_system_score_codex":0.0000031592344,"about_ca_system_score_gemma":0.0005153426,"threshold_uncertainty_score":0.8158471},"labels":[],"label_agreement":null},{"id":"W2895173106","doi":"10.1139/cjes-2018-0053","title":"Reappraisal of the Permian dissorophid <i>Fayella chickashaensis</i>","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Holotype; Postcrania; Paleontology; Geology; Neurocranium; Permian; Taxon; Biology; Taxonomy (biology); Zoology; Skull","score_opus":0.017960235434634753,"score_gpt":0.22256929199047948,"score_spread":0.20460905655584471,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2895173106","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9527629,0.0011068167,0.000006529145,0.001957995,0.0018381245,0.000036731784,0.000035453657,0.0000018128181,0.042253643],"genre_scores_gemma":[0.99887097,0.000017724544,0.0002957155,0.00035585312,0.00031257587,3.5813688e-8,9.1758824e-7,7.769559e-7,0.00014542417],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898547,0.00012960802,0.0002597489,0.00011957144,0.00017449683,0.00033110997],"domain_scores_gemma":[0.99913025,0.00010683447,0.00021911063,0.00011628108,0.00013422537,0.00029330372],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006653078,0.00007643114,0.00015218796,0.00013885749,0.00057094207,0.000019556603,0.00061780657,0.00006739617,0.0015428254],"category_scores_gemma":[0.00023839693,0.00004418146,0.0000825536,0.00041075246,0.0035860564,0.00018002366,0.000004913287,0.00014781421,0.000037139107],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009211536,0.0000018449707,0.9971495,0.0000015224979,0.000007541611,0.0000110045,0.00020402083,0.000086059255,0.00007266212,0.00039614202,0.00048658033,0.0015739107],"study_design_scores_gemma":[0.00007846146,0.00034481465,0.9724296,0.00002028337,0.000008231947,0.00042923685,0.00015742944,0.00018289995,0.00017161215,0.0005737234,0.02554418,0.000059547212],"about_ca_topic_score_codex":0.0080139525,"about_ca_topic_score_gemma":0.61849356,"teacher_disagreement_score":0.61047965,"about_ca_system_score_codex":5.435818e-7,"about_ca_system_score_gemma":0.0012909769,"threshold_uncertainty_score":0.9993699},"labels":[],"label_agreement":null},{"id":"W2895379507","doi":"10.1139/cjes-2018-0144","title":"Geochemistry of carbonate formations of the Chhattisgarh Supergroup, central India: implications for Mesoproterozoic global events","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Proterozoic; Supergroup; Carbonate; Siliciclastic; Sedimentary depositional environment; Geochemistry; Sedimentary rock; Archean; Radiogenic nuclide; Craton; Riphean; Paleontology; Structural basin; Tectonics","score_opus":0.017293218426257195,"score_gpt":0.2344746020111627,"score_spread":0.21718138358490552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2895379507","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9802775,0.001156126,0.00005235491,0.0007268585,0.00034167292,0.000094079565,0.00039532824,0.0000011663905,0.016954942],"genre_scores_gemma":[0.9991619,0.000007716825,0.00073071674,0.0000306842,0.00005688006,4.708599e-7,0.0000017806235,2.911015e-7,0.000009572933],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99912614,0.000032739954,0.0003188329,0.00008500953,0.00014126627,0.00029599643],"domain_scores_gemma":[0.99913955,0.000051658855,0.00029649792,0.000105678795,0.00016776503,0.00023882354],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035599933,0.00006768816,0.000137332,0.00007629438,0.00040582454,0.000019112622,0.00053405005,0.000054475175,0.00011081408],"category_scores_gemma":[0.000099211065,0.000045892233,0.000117109405,0.0003763613,0.0010398008,0.00024225935,0.000001295223,0.000069884714,5.07224e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045162788,0.0000032648347,0.9952967,0.0000074386653,0.000015193342,3.218239e-7,0.0001461516,0.000018893996,0.000083297964,0.0004451135,0.000043111504,0.003936],"study_design_scores_gemma":[0.00013278988,0.00019962442,0.99466246,0.000030729727,0.00001575795,0.00004385055,0.0001236341,0.00010723554,0.00078364415,0.003673242,0.00018004331,0.00004695907],"about_ca_topic_score_codex":0.0036663816,"about_ca_topic_score_gemma":0.18405743,"teacher_disagreement_score":0.18039104,"about_ca_system_score_codex":0.0000016981961,"about_ca_system_score_gemma":0.0012859424,"threshold_uncertainty_score":0.8308314},"labels":[],"label_agreement":null},{"id":"W2895847231","doi":"10.1139/cjes-2018-0162","title":"Description of a partial <i>Dromiceiomimus</i> (Dinosauria: Theropoda) skeleton with comments on the validity of the genus","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Taxon; Anatomy; Femur; Scapula; Paleontology; Tibia; Biology; Genus; Geology; Zoology","score_opus":0.044998742953257974,"score_gpt":0.21961138578448894,"score_spread":0.17461264283123096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2895847231","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993753,0.00016999347,0.000019625828,0.002058776,0.000754834,0.00007527408,0.000037393987,0.0000010050984,0.0031301002],"genre_scores_gemma":[0.9992787,0.000011032784,0.00008840033,0.00046213012,0.00013279032,1.3944675e-7,8.235635e-7,7.5191946e-7,0.000025185647],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99893165,0.00027967367,0.00023298297,0.000098122764,0.0002150292,0.0002425265],"domain_scores_gemma":[0.99912655,0.00017767538,0.00032968444,0.00012451038,0.00011151902,0.00013006838],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010203765,0.000074192634,0.0001439471,0.000084463885,0.00048901263,0.000016166072,0.00052941014,0.000051043455,0.00055759907],"category_scores_gemma":[0.00010382408,0.000033657743,0.00005821693,0.0002923774,0.002497505,0.00014105129,0.0000041784206,0.00014080541,0.000010081285],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044227974,0.000006377128,0.998212,0.0000017975657,0.000015634665,0.000003318119,0.00024336943,0.00023004436,0.00011712727,0.00022675634,0.00039806045,0.0005012897],"study_design_scores_gemma":[0.00015365637,0.0012200787,0.9926494,0.000039014067,0.00001644997,0.000083595,0.00022935079,0.0003506243,0.001035342,0.00048983673,0.0036845438,0.000048113554],"about_ca_topic_score_codex":0.006315282,"about_ca_topic_score_gemma":0.32521883,"teacher_disagreement_score":0.31890357,"about_ca_system_score_codex":0.0000019453892,"about_ca_system_score_gemma":0.0006982451,"threshold_uncertainty_score":0.954686},"labels":[],"label_agreement":null},{"id":"W2896484939","doi":"10.1139/cjes-2018-0170","title":"Southeast Anatolian Orogenic Belt revisited (geology and evolution)","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Nappe; Metamorphism; Imbrication; Subduction; Volcanic arc; Ophiolite; Massif; Geochemistry; Foreland basin; Paleontology; Metamorphic rock; Tectonics; Geomorphology","score_opus":0.01275894740577435,"score_gpt":0.19530226297969247,"score_spread":0.18254331557391812,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2896484939","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9884222,0.0023946844,0.000029678415,0.0017421914,0.00014975079,0.000026471473,0.000015176816,0.0000035258481,0.0072162943],"genre_scores_gemma":[0.99872464,0.000018491668,0.00063312566,0.00035125235,0.00019056324,4.3323272e-8,0.0000026077682,6.749866e-7,0.00007861512],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99894214,0.00006520972,0.00024880443,0.00017312753,0.0001792181,0.00039151552],"domain_scores_gemma":[0.9988191,0.000060356113,0.00012727919,0.00007080084,0.00017701508,0.0007454094],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005502222,0.000088246445,0.00018940264,0.00026486986,0.00046969933,0.00007793056,0.0003057951,0.000051885927,0.008603827],"category_scores_gemma":[0.00022337023,0.00005793029,0.00006840914,0.0007088682,0.0015841126,0.00019509002,0.000006509654,0.00012303809,0.0001415526],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000038862618,9.1971333e-7,0.99747086,0.0000015551323,0.00001042323,0.000021835758,0.000056081324,0.000031332158,0.000018975321,0.0007301668,0.00005671498,0.0015972267],"study_design_scores_gemma":[0.00009124169,0.00032953397,0.98101884,0.000013132807,0.000018679933,0.00027158586,0.0002952327,0.0009915454,0.000039205257,0.014248121,0.0025871822,0.000095686286],"about_ca_topic_score_codex":0.021010315,"about_ca_topic_score_gemma":0.5168281,"teacher_disagreement_score":0.49581778,"about_ca_system_score_codex":9.704263e-7,"about_ca_system_score_gemma":0.0003997241,"threshold_uncertainty_score":0.9923024},"labels":[],"label_agreement":null},{"id":"W2896928644","doi":"10.1139/cjes-2018-0172","title":"Preferred orientation of ferromagnetic phases in rock-forming minerals: insights from magnetic anisotropy of single crystals","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Ferrimagnetism; Silicate; Anisotropy; Mineralogy; Paleomagnetism; Olivine; Silicate minerals; Remanence; Pyroxene; Magnetic mineralogy; Magnetic anisotropy; Magnetization; Magnetic field; Geophysics; Chemistry; Optics","score_opus":0.022393867349683592,"score_gpt":0.2456379313285063,"score_spread":0.2232440639788227,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2896928644","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9894224,0.008520615,0.00007487401,0.00005992395,0.00026827876,0.00008708817,0.00003372073,8.811868e-7,0.00153222],"genre_scores_gemma":[0.99764764,0.000108029046,0.0018706291,0.000036537585,0.00015596616,0.0000011370681,0.000006606224,0.000005039993,0.00016841678],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9988213,0.00006201781,0.00048341876,0.00018323338,0.00020811691,0.0002418871],"domain_scores_gemma":[0.9991239,0.000030577856,0.00030864053,0.00012700171,0.00024325088,0.00016667214],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017068385,0.000117445685,0.00023364554,0.00027618583,0.00009824793,0.000026846456,0.00028987648,0.00006442171,0.00014629691],"category_scores_gemma":[0.0001887694,0.00010178209,0.000060747978,0.0003103408,0.00051229127,0.000028412183,0.000023472803,0.000045517278,0.0000012626583],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052550608,0.000048994232,0.06257456,0.000017275039,0.000015869817,0.000017289143,0.001355919,0.0003270351,0.9341368,0.0000417051,0.00023709705,0.001174871],"study_design_scores_gemma":[0.0023942844,0.021691259,0.5037436,0.00040540547,0.00008124069,0.00008042738,0.0034640792,0.00038984756,0.45648223,0.0014621933,0.009332684,0.00047275057],"about_ca_topic_score_codex":0.0034577884,"about_ca_topic_score_gemma":0.09610772,"teacher_disagreement_score":0.4776546,"about_ca_system_score_codex":0.0000029928228,"about_ca_system_score_gemma":0.00047150388,"threshold_uncertainty_score":0.92038596},"labels":[],"label_agreement":null},{"id":"W2897489080","doi":"10.1139/cjes-2018-0174","title":"Timeline of the South Tibet – Himalayan belt: the geochronological record of subduction, collision, and underthrusting from zircon and monazite U–Pb ages","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochronology; Zircon; Subduction; Tectonics; Monazite; Collision; Fibrous joint; Paleontology; Thermochronology; Geochemistry; Radiometric dating; Seismology","score_opus":0.019792333048124906,"score_gpt":0.19114707383297652,"score_spread":0.1713547407848516,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2897489080","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99516535,0.001477585,0.000021194275,0.0026703475,0.00014096264,0.00004062132,0.000048521408,0.000001349352,0.00043405095],"genre_scores_gemma":[0.9985747,0.000060649498,0.0010356593,0.00015456395,0.00012821115,5.511828e-8,0.0000019933982,6.360387e-7,0.000043556025],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990389,0.00008380845,0.0003176093,0.0001503803,0.00020492933,0.00020439165],"domain_scores_gemma":[0.9989854,0.000244974,0.0002995721,0.0000897394,0.00017170719,0.00020856853],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00063874864,0.000081328246,0.0002003867,0.00007660146,0.00041590582,0.000048733982,0.00031697363,0.00004924033,0.0014703211],"category_scores_gemma":[0.00040640304,0.000036553643,0.000056594265,0.00042225874,0.0023690534,0.00011697064,0.000018936262,0.00013342494,0.0000036406689],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008419007,0.0000024250248,0.99491185,0.0000023211628,0.000014250842,0.0000020741136,0.0002318378,0.00021197704,0.0007288005,0.000028457162,0.00006562711,0.0037919555],"study_design_scores_gemma":[0.000098739256,0.00030877593,0.98764694,0.000033999357,0.000033401164,0.000023525392,0.00067428313,0.0010567184,0.0019331658,0.007564838,0.00056533824,0.000060265862],"about_ca_topic_score_codex":0.038599793,"about_ca_topic_score_gemma":0.26455715,"teacher_disagreement_score":0.22595735,"about_ca_system_score_codex":7.582676e-7,"about_ca_system_score_gemma":0.00016947834,"threshold_uncertainty_score":0.99944246},"labels":[],"label_agreement":null},{"id":"W2899198137","doi":"10.1139/cjes-2018-0181","title":"Geochemistry of Late Ordovician dalmanelloid brachiopods from Laurentia: testing the effects of paleolatitudinal gradient","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University; Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Laurentia; Geology; Ordovician; Baltica; Diagenesis; Upwelling; Oil shale; Geochemistry; Craton; Paleontology; Oceanography","score_opus":0.01827992566515666,"score_gpt":0.2141609821246535,"score_spread":0.19588105645949686,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2899198137","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97655886,0.0065157856,0.000016931715,0.00010776921,0.0006438746,0.000050676193,0.000037681908,0.000002010879,0.016066382],"genre_scores_gemma":[0.9985884,0.000014423121,0.0011825435,0.000035809353,0.0001657107,8.173771e-8,0.0000013072494,5.502898e-7,0.00001118474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883115,0.000086658,0.00036829003,0.00014161601,0.00025737897,0.00031488328],"domain_scores_gemma":[0.9984588,0.0005204333,0.0004498089,0.00012497917,0.00015838555,0.00028756223],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00061749935,0.00010547232,0.0002270545,0.00014811159,0.00045225243,0.00003901573,0.0005712948,0.00006135213,0.00024475425],"category_scores_gemma":[0.00038798476,0.00006795059,0.00009027466,0.00047682846,0.0020738468,0.00019521033,0.0000018073598,0.00019003963,0.0000026321989],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000066219272,0.0000044482863,0.9910148,0.000014495154,0.000030856507,0.000028549564,0.00048747868,0.00003779713,0.0010630847,0.000018462992,0.000017060902,0.00727638],"study_design_scores_gemma":[0.00013209044,0.0005470233,0.99518406,0.00013916279,0.000035817928,0.000043445245,0.00018274673,0.0004717775,0.002002521,0.0011103962,0.00007673018,0.00007422942],"about_ca_topic_score_codex":0.016465966,"about_ca_topic_score_gemma":0.6082885,"teacher_disagreement_score":0.59182256,"about_ca_system_score_codex":5.981659e-7,"about_ca_system_score_gemma":0.00069147465,"threshold_uncertainty_score":0.99008346},"labels":[],"label_agreement":null},{"id":"W2899552179","doi":"10.1139/cjes-2018-0129","title":"A revised stratigraphic framework for Cretaceous sedimentary and igneous rocks at Mokka Fiord, Axel Heiberg Island, Nunavut, with implications for the Cretaceous Normal Superchron","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; Geological Survey of Canada","funders":"","keywords":"Geology; Igneous rock; Paleontology; Paleomagnetism; Cretaceous; Sedimentary rock; Magmatism; Large igneous province; Volcanic rock; Geochemistry; Volcano","score_opus":0.027795237367743014,"score_gpt":0.23320197476138443,"score_spread":0.20540673739364143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2899552179","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96557003,0.011633972,0.008442213,0.012525401,0.00037253936,0.00067574804,0.0003156333,0.0000070269134,0.0004574076],"genre_scores_gemma":[0.9936102,0.0003550579,0.004706258,0.0008942178,0.00034880228,0.00000656955,0.000012156391,0.000002766564,0.00006394585],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886614,0.00003522898,0.00025937354,0.00021517804,0.00016717348,0.00045689882],"domain_scores_gemma":[0.99860567,0.0005555167,0.00015885322,0.00011150508,0.00020141176,0.00036706976],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0005296818,0.0001356567,0.00018828566,0.00008785667,0.0021956037,0.00019419898,0.00030264613,0.00006260292,0.00042605784],"category_scores_gemma":[0.00014001438,0.0000745745,0.000072615214,0.0002811505,0.0008577397,0.00025490555,0.0000069969487,0.0001181683,0.0000041854896],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021583473,0.000008747551,0.9801923,0.000021443095,0.00008137723,0.000011723152,0.00100655,0.0037268947,0.000016103957,0.00027017147,0.0021699555,0.012278917],"study_design_scores_gemma":[0.00088245026,0.008507037,0.90925765,0.000114151284,0.00015306867,0.00064392126,0.0022587809,0.0074120355,0.000047082827,0.013423107,0.056906946,0.00039376027],"about_ca_topic_score_codex":0.0029515815,"about_ca_topic_score_gemma":0.6863833,"teacher_disagreement_score":0.6834317,"about_ca_system_score_codex":0.0000036185547,"about_ca_system_score_gemma":0.00034110088,"threshold_uncertainty_score":0.9991034},"labels":[],"label_agreement":null},{"id":"W2899868611","doi":"10.1139/cjes-2018-0169","title":"Testing of Permian – Lower Triassic stratigraphic data in a half-graben/tilt-block system: evidence for the initial rifting phase in Antalya Nappes","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology; Rift; Graben; Nappe; Clastic rock; Permian; Passive margin; Sedimentary rock; Facies; Tectonics; Structural basin","score_opus":0.16277705676966805,"score_gpt":0.31809016349547875,"score_spread":0.1553131067258107,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2899868611","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951255,0.0029624568,0.000013453234,0.0007488149,0.00023867494,0.00015942419,0.000055376157,0.0000020721245,0.0006942656],"genre_scores_gemma":[0.99897015,0.000011410753,0.0007530922,0.00006445995,0.0001925245,5.0885524e-7,0.0000035473106,0.0000010328948,0.000003284085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99818325,0.00013560985,0.0006138808,0.00025958105,0.00036653902,0.00044113587],"domain_scores_gemma":[0.9977413,0.0012412384,0.00033852886,0.00019565134,0.00020157958,0.00028171245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003781015,0.00011343493,0.00029170007,0.00037381335,0.00030564747,0.00012499871,0.0011309476,0.000049760976,0.00035158213],"category_scores_gemma":[0.0027584,0.00006577875,0.00007609626,0.0015460973,0.0009147952,0.000515879,0.000014959231,0.00019038252,0.0000041764324],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000045659235,0.000014713949,0.9860337,0.000028369479,0.000013789683,0.00005605256,0.0001788976,0.0009995907,0.00012305583,0.000021076212,0.000020465295,0.012464666],"study_design_scores_gemma":[0.0011163898,0.0014866486,0.7496129,0.0009991435,0.00009594225,0.00014622447,0.0030081396,0.24161707,0.0003252426,0.0009942732,0.00035662056,0.00024137531],"about_ca_topic_score_codex":0.084093876,"about_ca_topic_score_gemma":0.82758695,"teacher_disagreement_score":0.743493,"about_ca_system_score_codex":0.0000025098493,"about_ca_system_score_gemma":0.0010612637,"threshold_uncertainty_score":0.92200524},"labels":[],"label_agreement":null},{"id":"W2900499765","doi":"10.1139/cjes-2018-0205","title":"Forearc strike-slip displacement as an alternative to subduction erosion, with examples from Mexico and California (sinistral Nacimiento fault)","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Forearc; Batholith; Subduction; Sinistral and dextral; Seismology; Paleontology; Fault (geology); Tectonics","score_opus":0.02463369531785407,"score_gpt":0.2318961725086887,"score_spread":0.20726247719083465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900499765","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974956,0.0001159498,0.00020563538,0.0012324884,0.00015050842,0.00006436454,0.00014998605,0.0000033170506,0.00058215676],"genre_scores_gemma":[0.9971056,0.0000083679115,0.002162201,0.0004377812,0.00021710501,2.568007e-7,0.000020274523,0.0000012236005,0.000047195346],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99868834,0.00005981932,0.00022992247,0.000270676,0.0003773977,0.000373824],"domain_scores_gemma":[0.99836725,0.000060479226,0.00012745967,0.00007842624,0.0001790492,0.0011873393],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00039046173,0.000121372555,0.00017704788,0.00017547737,0.00047147574,0.00021681532,0.00029270287,0.000033875043,0.0042679883],"category_scores_gemma":[0.00010254501,0.00007196357,0.00003632798,0.00040636427,0.00075772015,0.0003382829,0.000007591535,0.000103374805,0.000060870098],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006649068,0.000007848917,0.99457484,0.0000011303572,0.00001910619,0.000026847243,0.00046408369,0.0012981304,0.00017532782,0.00009172339,0.00007817956,0.0031963056],"study_design_scores_gemma":[0.0002500602,0.0032189256,0.97692055,0.000041043004,0.000035462377,0.000072833274,0.0015949176,0.00257541,0.0024342407,0.007771714,0.0048813988,0.00020347048],"about_ca_topic_score_codex":0.16111587,"about_ca_topic_score_gemma":0.82546246,"teacher_disagreement_score":0.6643466,"about_ca_system_score_codex":0.0000029794517,"about_ca_system_score_gemma":0.0002991066,"threshold_uncertainty_score":0.99664223},"labels":[],"label_agreement":null},{"id":"W2900575634","doi":"10.1139/cjes-2018-0168","title":"Geochemical characteristics of Upper Jurassic – Lower Cretaceous platform carbonates in Hazine Mağara, Gümüşhane (northeast Turkey): implications for dolomitization and recrystallization","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"Natural Sciences and Engineering Research Council of Canada; Türkiye Bilimsel ve Teknolojik Araştırma Kurumu; Karadeniz Teknik Üniversitesi","keywords":"Geology; Dolomitization; Dolomite; Geochemistry; Petrography; Diagenesis; Cretaceous; Recrystallization (geology); Mineralization (soil science); Carbonate; Pyrite; Facies; Paleontology","score_opus":0.015322520083522627,"score_gpt":0.21970026390708153,"score_spread":0.2043777438235589,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900575634","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99790984,0.00030707015,0.0001266023,0.00073896395,0.000111481946,0.00007555672,0.00016387529,0.0000015892196,0.00056500244],"genre_scores_gemma":[0.99897075,0.000041156425,0.000705851,0.00006192814,0.00010316843,4.72095e-7,0.00006902218,0.0000014807875,0.00004616951],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99913675,0.0000140071,0.00036525476,0.00013463656,0.000116292445,0.00023306512],"domain_scores_gemma":[0.9992042,0.00007271334,0.00023204515,0.00006203533,0.00019442629,0.0002345547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004107471,0.00008106631,0.00017157305,0.00019727107,0.00018679738,0.000060220253,0.00015719226,0.000049301176,0.00035277032],"category_scores_gemma":[0.00015984212,0.00006628796,0.00004178831,0.00038593024,0.00042079482,0.0002915148,0.0000035774003,0.000060444945,0.0000015392145],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021086797,0.0000062328604,0.9943618,0.000013998235,0.000009502442,0.000001918518,0.00013212764,0.00015763083,0.0012560653,0.000049150265,0.000037607846,0.0039528897],"study_design_scores_gemma":[0.00021475149,0.00031097373,0.98937786,0.00006285447,0.00002757194,0.00007882143,0.00020823131,0.005506646,0.0013465493,0.0014470373,0.0013029362,0.00011574825],"about_ca_topic_score_codex":0.0023099026,"about_ca_topic_score_gemma":0.0696647,"teacher_disagreement_score":0.0673548,"about_ca_system_score_codex":0.0000032248718,"about_ca_system_score_gemma":0.00033946344,"threshold_uncertainty_score":0.9473115},"labels":[],"label_agreement":null},{"id":"W2900871422","doi":"10.1139/cjes-2018-0091","title":"Geology, lithogeochemistry, and significance of porphyry intrusions associated with gold mineralization within the Timmins–Porcupine gold camp, Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Geological Survey of Canada","funders":"","keywords":"Geology; Geochemistry; Mafic; Mineralization (soil science); Partial melting; Metallogeny; Sericite; Carbonate; Crust; Hydrothermal circulation; Sphalerite; Pyrite; Chemistry; Paleontology","score_opus":0.01091680922967953,"score_gpt":0.17954545523625604,"score_spread":0.1686286460065765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900871422","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99521637,0.0004468299,0.000008139161,0.001963194,0.00010946976,0.000047695696,0.000058557365,0.0000019242384,0.0021478243],"genre_scores_gemma":[0.99888635,0.000009739239,0.00024578682,0.00042685602,0.00008736979,1.8555185e-7,0.000016687798,0.000001051499,0.00032597684],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99887836,0.0000681825,0.00031596865,0.00016418415,0.00029043565,0.0002828894],"domain_scores_gemma":[0.99866873,0.00016819796,0.0003754706,0.000090995454,0.00030914572,0.00038748005],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005918155,0.00010734089,0.00021062794,0.00007956242,0.00023764944,0.000044604454,0.00034736606,0.000047546502,0.0010212797],"category_scores_gemma":[0.0005450625,0.000056555968,0.0000331361,0.00073440175,0.0016321847,0.00010775287,0.000007799715,0.00014190428,0.0000024170697],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009498803,0.0000037813359,0.9972188,0.0000033050521,0.00002660976,0.000025947436,0.00008920714,0.001287239,0.000435382,0.00008039576,0.0005198053,0.00030001588],"study_design_scores_gemma":[0.000160069,0.00043388375,0.9917781,0.00004977096,0.000043558928,0.00009514585,0.00045833315,0.0030999198,0.0011076066,0.0011898763,0.001441611,0.00014216115],"about_ca_topic_score_codex":0.7546747,"about_ca_topic_score_gemma":0.9969107,"teacher_disagreement_score":0.24223603,"about_ca_system_score_codex":0.0000028632867,"about_ca_system_score_gemma":0.0015824492,"threshold_uncertainty_score":0.99989194},"labels":[],"label_agreement":null},{"id":"W2900904559","doi":"10.1139/cjes-2018-0201","title":"Microsedimentological evidence of vertical fluctuations in subglacial stress from the northwest sector of the Laurentide Ice Sheet, Northwest Territories, Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Brock University; Geological Survey of Canada; University of Waterloo","funders":"","keywords":"Geology; Geomorphology; Lineation; Bedrock; Quaternary; Aggradation; Ice sheet; Geochemistry; Paleontology; Tectonics; Fluvial","score_opus":0.028159511316323042,"score_gpt":0.22385760941411997,"score_spread":0.19569809809779692,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900904559","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948657,0.0014727594,0.000004578876,0.0018137918,0.0013129114,0.00007636063,0.0003830698,7.426348e-7,0.00007009182],"genre_scores_gemma":[0.9993054,0.00002657331,0.00015164405,0.00022299694,0.00027905905,2.3368014e-7,0.000005769546,9.669183e-7,0.0000073154147],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987047,0.000088457906,0.00040792875,0.00012372284,0.0004094635,0.00026576623],"domain_scores_gemma":[0.9987186,0.0005849188,0.00017516383,0.00013285335,0.00021326562,0.00017515259],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036521794,0.00008356365,0.00017209223,0.00003216434,0.00047038196,0.00004885111,0.0006981001,0.00003062329,0.00070337765],"category_scores_gemma":[0.0005339618,0.000045314373,0.0000543328,0.0007034307,0.0012490265,0.0001846,0.000013690649,0.00013904182,8.006101e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007933057,0.000004204717,0.9983998,0.000002041921,0.0000093713015,0.0000048293496,0.0005026242,0.0005759345,0.000025265701,0.000030408297,0.00021208276,0.0002255082],"study_design_scores_gemma":[0.00008734416,0.00012093254,0.9955355,0.000092576636,0.000015158372,0.0000041536637,0.0010595169,0.00021348345,0.00016657206,0.000049486414,0.0026009337,0.000054358647],"about_ca_topic_score_codex":0.9892841,"about_ca_topic_score_gemma":0.99998564,"teacher_disagreement_score":0.010701529,"about_ca_system_score_codex":0.000008336371,"about_ca_system_score_gemma":0.0033914363,"threshold_uncertainty_score":0.7701492},"labels":[],"label_agreement":null},{"id":"W2901148753","doi":"10.1139/cjes-2018-0160","title":"Geochemical characteristics and geological significance of the bedded chert during the Ordovician and Silurian transition in the Shizhu area, Chongqing, South China","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Ordovician; Terrigenous sediment; Geochemistry; Sedimentary rock; Petrography; Paleontology","score_opus":0.01049930930805407,"score_gpt":0.18200381113721886,"score_spread":0.1715045018291648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2901148753","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99656856,0.00017069896,0.0000027124167,0.0026212675,0.000058442798,0.00005856139,0.000031038773,7.684149e-7,0.00048794833],"genre_scores_gemma":[0.9995871,0.000013695194,0.00003645005,0.0002347097,0.00010880614,2.2490936e-7,0.0000015601618,6.1682806e-7,0.000016837883],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991404,0.00008259717,0.0002273094,0.000119508026,0.00019972933,0.00023048547],"domain_scores_gemma":[0.99953717,0.00005865302,0.00015214093,0.00008324329,0.00003453803,0.00013427623],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007896898,0.00007780953,0.00012470839,0.000050311064,0.00054521905,0.0000942703,0.00036937126,0.000036764453,0.0003745826],"category_scores_gemma":[0.000097811644,0.000035611425,0.00004047454,0.0003428482,0.0013854727,0.00011396404,0.0000058791234,0.00018454975,8.2353955e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009438318,0.0000032160724,0.9953378,0.0000064209553,0.0000061561354,0.00000845354,0.0033524346,0.00006520056,0.00060697016,0.000008938553,0.000004912505,0.000590092],"study_design_scores_gemma":[0.00008898862,0.00008220942,0.99527156,0.000031968095,0.000014970085,0.00008167975,0.0024135543,0.000894621,0.0006681187,0.00027270208,0.0001266085,0.000053025793],"about_ca_topic_score_codex":0.005576223,"about_ca_topic_score_gemma":0.13474706,"teacher_disagreement_score":0.12917084,"about_ca_system_score_codex":0.0000012955088,"about_ca_system_score_gemma":0.00014243976,"threshold_uncertainty_score":0.8810415},"labels":[],"label_agreement":null},{"id":"W2901299007","doi":"10.1139/cjes-2018-0196","title":"A New Year’s Day icebreaker: icequakes on lakes in Alberta, Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University; Geological Survey of Canada; University of Alberta","funders":"","keywords":"Geology; Brittleness; Epicenter; Seismology; Geotechnical engineering","score_opus":0.007723964561645761,"score_gpt":0.19750191771728143,"score_spread":0.18977795315563567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2901299007","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9156966,0.000059238508,0.0000066744465,0.0032242208,0.00078563986,0.000046528243,0.000003428082,0.0000010751602,0.08017658],"genre_scores_gemma":[0.9956044,0.000007446766,0.0002539752,0.0006982867,0.0001632647,1.7582994e-7,1.7040576e-7,0.000003963066,0.003268337],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99887526,0.000034970373,0.0002156687,0.00014717615,0.00034363952,0.00038326645],"domain_scores_gemma":[0.999081,0.000064275046,0.000102324884,0.00009126207,0.000014196175,0.0006469245],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00045089104,0.00008707447,0.0001226655,0.00011184222,0.0002062747,0.00007500862,0.000391033,0.000044153418,0.0045646997],"category_scores_gemma":[0.00010329919,0.000059566624,0.000033130927,0.00045528088,0.00034082177,0.00015851864,0.000012372451,0.00015488043,0.00014168781],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018217444,0.000010562355,0.9345596,0.000001814059,0.000013223931,0.00024712726,0.0016583228,0.0025047197,0.00011866404,0.000779948,0.047169115,0.012918695],"study_design_scores_gemma":[0.00036765327,0.00049925724,0.5772952,0.00008817864,0.0000073605706,0.00008170548,0.00032234192,0.00023430603,0.00033497435,0.0005036942,0.42007208,0.00019326551],"about_ca_topic_score_codex":0.96372443,"about_ca_topic_score_gemma":0.9998211,"teacher_disagreement_score":0.37290296,"about_ca_system_score_codex":0.00004861844,"about_ca_system_score_gemma":0.002416788,"threshold_uncertainty_score":0.9963453},"labels":[],"label_agreement":null},{"id":"W2901497151","doi":"10.1139/cjes-2018-0233","title":"Genesis of the Wuxing Pt–Pd-rich Cu–Ni sulfide deposit in the eastern Central Asian Orogenic Belt: evidences from geochronology, elemental geochemistry, and Sr–Nd–Hf isotopic data","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Zircon; Hornblende; Fractional crystallization (geology); Underplating; Mantle (geology); Biotite; Subduction; Tectonics; Quartz","score_opus":0.028367198356818293,"score_gpt":0.22164756616401132,"score_spread":0.19328036780719304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2901497151","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9901772,0.005439435,0.0000043119553,0.0034299875,0.00020950277,0.00007033372,0.000102554644,0.0000015923549,0.0005650585],"genre_scores_gemma":[0.9989535,0.00009717693,0.00031555915,0.00038915183,0.00020805893,2.2889674e-7,0.000014192505,0.0000010306842,0.000021055972],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981922,0.00016580985,0.00045460544,0.00030265065,0.00037879395,0.000505944],"domain_scores_gemma":[0.9989126,0.00018385031,0.00027137218,0.00027790695,0.00006488621,0.00028939496],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008570961,0.00013497465,0.00023683382,0.000080344704,0.00043278348,0.00014329249,0.0018095431,0.00006705098,0.0018423777],"category_scores_gemma":[0.00028562002,0.00007096639,0.00007232761,0.00055548764,0.0014441484,0.00030627556,0.00006051658,0.0002093731,0.000008843756],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005449486,0.0000055088335,0.9940923,0.0000040226655,0.000023295275,0.00001844967,0.00046119027,0.000025982163,0.00028407108,0.000004084228,0.000067222245,0.005008417],"study_design_scores_gemma":[0.00012976218,0.00013364057,0.9923136,0.00005112522,0.00005381377,0.00008598837,0.0021897287,0.002212454,0.0013470087,0.00095820474,0.0004216845,0.00010294524],"about_ca_topic_score_codex":0.22802468,"about_ca_topic_score_gemma":0.882991,"teacher_disagreement_score":0.65496635,"about_ca_system_score_codex":0.0000031095292,"about_ca_system_score_gemma":0.0003853621,"threshold_uncertainty_score":0.99907005},"labels":[],"label_agreement":null},{"id":"W2901526321","doi":"10.1139/cjes-2018-0127","title":"Aeolian activity during Late Glacial time, with an example from Mongo, Indiana, USA","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Ohio State University; U.S. Geological Survey; North Dakota State University","keywords":"Geology; Outwash plain; Stadial; Deglaciation; Meltwater; Glacial period; Aeolian processes; Younger Dryas; Geomorphology; Sand dune stabilization; Glacial lake; Last Glacial Maximum; Moraine; Ice sheet; Physical geography; Geography","score_opus":0.032783571912295355,"score_gpt":0.23427995618799347,"score_spread":0.2014963842756981,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2901526321","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99074864,0.00010289889,0.000006275531,0.00027026847,0.00026515732,0.00006045699,0.000022147764,0.00000449743,0.008519673],"genre_scores_gemma":[0.9987784,0.000005555635,0.00053472945,0.000104164654,0.00029353393,1.4869373e-7,0.0000041429644,0.0000019755973,0.00027733407],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99844074,0.00017187289,0.00018589635,0.00025581077,0.0002876363,0.0006580631],"domain_scores_gemma":[0.9984941,0.000116226554,0.00015824877,0.0001486865,0.00012583513,0.0009569398],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00076675275,0.00012307093,0.00022421175,0.0003703972,0.0010323768,0.00013774757,0.0005758087,0.00010057316,0.011548284],"category_scores_gemma":[0.000042366042,0.00008976897,0.000038130922,0.00048081577,0.0020578385,0.000816171,0.000006317462,0.00030009766,0.00038613172],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007557242,0.0000035486828,0.99823296,0.0000011862414,0.000015535887,0.00021286952,0.000723779,0.0001717749,0.000033743854,0.000007953135,0.000013595647,0.0005074899],"study_design_scores_gemma":[0.00028722116,0.00080849114,0.9964237,0.000017569824,0.00000892663,0.00021270465,0.00016089862,0.000799672,0.0004547797,0.000336509,0.00036262366,0.00012689822],"about_ca_topic_score_codex":0.1245358,"about_ca_topic_score_gemma":0.96048653,"teacher_disagreement_score":0.83595073,"about_ca_system_score_codex":7.6556813e-7,"about_ca_system_score_gemma":0.0013750755,"threshold_uncertainty_score":0.98935527},"labels":[],"label_agreement":null},{"id":"W2901614156","doi":"10.1139/cjes-2018-0068","title":"The history of the core dynamos of Mars and the Moon inferred from their crustal magnetization: a brief review","year":2018,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Dynamo; Geology; Geophysics; Mars Exploration Program; Mantle (geology); Martian; Dynamo theory; Outer core; Crust; Inner core; Core–mantle boundary; Astrobiology; Physics; Magnetic field","score_opus":0.04782648731019908,"score_gpt":0.241843735176572,"score_spread":0.19401724786637292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2901614156","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00036632695,0.9970613,0.000012586111,0.00035612468,0.0007203431,0.0002495431,0.00011203496,4.3538103e-7,0.0011212692],"genre_scores_gemma":[0.004126715,0.9950926,0.00003196306,0.00011687834,0.00020090547,0.0000028524566,0.000019931013,0.0000040996197,0.0004040571],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9988038,0.00017636469,0.00051406136,0.000111760266,0.00023983333,0.00015420638],"domain_scores_gemma":[0.9982787,0.00022037675,0.0010449737,0.00020567176,0.00013547104,0.00011480566],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011148633,0.00012196663,0.00047576864,0.00005930519,0.0002724849,0.00005364051,0.0007738543,0.000028527502,0.00015781175],"category_scores_gemma":[0.00007051539,0.000048645827,0.00019573212,0.00031734773,0.0021264968,0.00020546492,0.00002257276,0.00016466518,0.000002966706],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013074374,0.000014889628,0.0048288396,0.0014390503,0.00022090701,0.0000036063955,0.0025538742,0.00004971999,0.0000015674,0.00537176,0.038452264,0.94705045],"study_design_scores_gemma":[0.0000786346,0.000050518604,0.0004577836,0.005217743,0.00012807501,0.000008723803,0.00018124396,0.00009763541,2.5077395e-7,0.0007472253,0.9929657,0.000066438166],"about_ca_topic_score_codex":0.0034393612,"about_ca_topic_score_gemma":0.013055931,"teacher_disagreement_score":0.9545135,"about_ca_system_score_codex":0.000010842862,"about_ca_system_score_gemma":0.003997841,"threshold_uncertainty_score":0.7835166},"labels":[],"label_agreement":null},{"id":"W2902328840","doi":"10.1139/cjes-2018-0131","title":"U–Pb geochronology, Nd–Sm geochemistry, structural setting, and tectonic significance of Late Devonian and Paleogene intrusions in northern Yukon and northeastern Alaska","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia; Geological Survey of Canada","funders":"","keywords":"Geology; Geochemistry; Zircon; Underplating; Geochronology; Devonian; Rhyolite; Late Devonian extinction; Felsic; Batholith; Crust; Rift; Magmatism; Mafic; Petrology; Volcanic rock; Paleontology; Carboniferous; Tectonics; Volcano; Lithosphere; Structural basin","score_opus":0.008701555970844984,"score_gpt":0.19600176698216495,"score_spread":0.18730021101131997,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902328840","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960397,0.0023263996,0.000002793766,0.0008515693,0.000055265606,0.000049063496,0.00002950836,0.0000018709407,0.00064383773],"genre_scores_gemma":[0.99925655,0.000069153226,0.00051720964,0.00007885938,0.00005760148,1.5168803e-7,0.0000025989461,0.0000010870596,0.000016775393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99891615,0.000047771682,0.00030552386,0.00023518478,0.00014057706,0.0003547821],"domain_scores_gemma":[0.99910265,0.00009054177,0.00019154967,0.00007148137,0.000095624964,0.00044814384],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038792752,0.000119197066,0.00024075827,0.00017129074,0.00024512038,0.00005709746,0.00019774644,0.000065823646,0.001226861],"category_scores_gemma":[0.00013231645,0.000083104926,0.000031179672,0.00031796691,0.0018924372,0.00013606889,0.000017229184,0.00015727279,0.0000026696596],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012413439,0.0000014232243,0.98793465,0.000008431884,0.00000906077,0.000018618417,0.00021527788,0.00012652393,0.0005828594,0.0000022450465,0.0000012235918,0.011087301],"study_design_scores_gemma":[0.0002250585,0.00028229106,0.9935434,0.000034617213,0.000013996968,0.00013709604,0.00025340228,0.0023671254,0.0011023292,0.001821758,0.0001075639,0.00011136227],"about_ca_topic_score_codex":0.018166678,"about_ca_topic_score_gemma":0.8687285,"teacher_disagreement_score":0.8505618,"about_ca_system_score_codex":0.0000014428138,"about_ca_system_score_gemma":0.00029657676,"threshold_uncertainty_score":0.9996862},"labels":[],"label_agreement":null},{"id":"W2902422169","doi":"10.1139/cjes-2018-0061","title":"Origin and <sup>87</sup>Rb–<sup>87</sup>Sr age of porewaters in low permeability Ordovician sediments on the eastern flank of the Michigan Basin, Tiverton, Ontario, Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Statistics Canada; Nuclear Waste Management Organization; University of Ottawa","funders":"Nuclear Waste Management Organization; University of Ottawa","keywords":"Geology; Radiogenic nuclide; Strontium; Geochemistry; Ordovician; Isotopes of strontium; Seawater; Carbonate; Carbonate rock; Mineralogy; Diagenesis; Dolomite; Sedimentary rock; Mantle (geology); Chemistry; Oceanography","score_opus":0.013169316896627961,"score_gpt":0.18143344303292244,"score_spread":0.1682641261362945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902422169","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99472517,0.00010077099,7.668602e-7,0.0029492034,0.00012268146,0.0001102662,0.00006980912,0.0000012036971,0.0019201576],"genre_scores_gemma":[0.99847513,0.0000055162914,0.00005295749,0.0011892631,0.000058584803,2.2233722e-7,0.0000049735518,0.0000016117315,0.0002117403],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99794906,0.0002014734,0.0005069573,0.00027230717,0.00056998426,0.00050023623],"domain_scores_gemma":[0.99869,0.00021150002,0.0002586639,0.00020688566,0.0001552132,0.00047771353],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00095855223,0.00017702553,0.00035830925,0.00015804678,0.00036655567,0.00006377362,0.0007959824,0.00006132807,0.003211465],"category_scores_gemma":[0.0002155604,0.00008893777,0.0001102411,0.00067735225,0.0017850955,0.00016232033,0.000021582484,0.00029875312,0.000006852617],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021575666,0.000010923864,0.9946467,0.000007384293,0.000021462321,0.000029029316,0.0015399727,0.0031976355,0.00002249588,0.000019521385,0.00008716875,0.0003961006],"study_design_scores_gemma":[0.00018775127,0.000325606,0.98926395,0.000104169805,0.00002395213,0.000018404406,0.0015782376,0.00450096,0.00032498117,0.000971315,0.0025719383,0.00012872489],"about_ca_topic_score_codex":0.9723608,"about_ca_topic_score_gemma":0.9994547,"teacher_disagreement_score":0.027093852,"about_ca_system_score_codex":0.000014150418,"about_ca_system_score_gemma":0.0020030031,"threshold_uncertainty_score":0.99769974},"labels":[],"label_agreement":null},{"id":"W2902521471","doi":"10.1139/cjes-2018-0048","title":"The Bathurst Mining Camp, New Brunswick: data integration, geophysical modelling, and implications for exploration","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; McMaster University; Brock University","funders":"Natural Resources Canada","keywords":"Geology; Geophysics; Felsic; Ophiolite; Inversion (geology); Magnetic anomaly; Volcano; Mafic; Exploration geophysics; Mineral exploration; Bouguer anomaly; Gravity anomaly; Geologic map; Section (typography); Electromagnetics; Interpretation (philosophy); Seismology; Geochemistry; Paleontology; Tectonics","score_opus":0.09864650523932321,"score_gpt":0.2918428595418514,"score_spread":0.19319635430252818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902521471","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6517974,0.002977187,0.3149106,0.026424406,0.0013443683,0.0003767259,0.00009340037,0.000012409092,0.0020635014],"genre_scores_gemma":[0.96597886,0.000054402128,0.03242276,0.0002421728,0.0009351066,2.4864616e-7,0.00001170562,0.0000018301258,0.00035291497],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99910605,0.000051751947,0.00022122239,0.00017804412,0.00012696789,0.00031593945],"domain_scores_gemma":[0.9985299,0.0004974977,0.00013241533,0.0001518919,0.00018611498,0.0005021688],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008805108,0.00007393244,0.00010685267,0.00008202093,0.0011113017,0.0003284162,0.000537823,0.000028147004,0.000046285186],"category_scores_gemma":[0.00045591957,0.000043738968,0.000029945955,0.00041090764,0.00051611406,0.00069015496,0.0000068100444,0.00008804258,0.000012735565],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030604428,0.00000815115,0.05766699,0.000003598214,0.000022135911,0.0000013918152,0.001093778,0.0026325008,0.000036986537,0.011174717,0.0056335875,0.92169553],"study_design_scores_gemma":[0.00023954996,0.001397798,0.5666641,0.00003567297,0.000038009297,0.000041238578,0.00059011206,0.2358321,0.00012756084,0.110122055,0.084688246,0.00022354041],"about_ca_topic_score_codex":0.016896164,"about_ca_topic_score_gemma":0.47947034,"teacher_disagreement_score":0.921472,"about_ca_system_score_codex":9.763035e-7,"about_ca_system_score_gemma":0.0020021426,"threshold_uncertainty_score":0.9896504},"labels":[],"label_agreement":null},{"id":"W2902857456","doi":"10.1139/cjes-2018-0095","title":"Provenance and depositional environment of organic-rich calcareous black shale of the Late Ordovician Macasty Formation, western Anticosti Basin, eastern Canada","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"","keywords":"Geology; Ordovician; Geochemistry; Provenance; Detritus; Diagenesis; Pyrite; Sedimentary depositional environment; Paleontology; Structural basin","score_opus":0.007722453727863114,"score_gpt":0.1654621747052675,"score_spread":0.15773972097740438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902857456","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982972,0.00019447553,0.000021072994,0.0006441277,0.00008603661,0.000042918626,0.00008793413,4.07598e-7,0.0006258342],"genre_scores_gemma":[0.9995455,0.000012921365,0.00010242938,0.00016535795,0.000040145664,4.6586205e-8,0.0000032214398,8.752815e-7,0.00012946884],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990906,0.000031815965,0.00028723906,0.00008299597,0.00031242974,0.00019492082],"domain_scores_gemma":[0.9993374,0.000025024083,0.0002829682,0.00007487875,0.00007254014,0.00020721616],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002208295,0.00007000061,0.00012813263,0.000050928462,0.00024620688,0.00003310155,0.00026234813,0.000020131463,0.00053319643],"category_scores_gemma":[0.000026285856,0.000046329395,0.000030608146,0.00023147016,0.00059956615,0.00019176865,0.000008666248,0.00006245431,0.000003330216],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000034734603,0.0000026854702,0.9981567,0.000012096266,0.000010908921,0.000006015312,0.00025183795,0.00043672565,0.00030921347,0.000002002861,0.00003038068,0.00077795907],"study_design_scores_gemma":[0.00010031765,0.00013900764,0.9897603,0.00006147554,0.000023822684,0.00009450334,0.00064146984,0.0013894899,0.00692201,0.000060867384,0.0007389472,0.00006779277],"about_ca_topic_score_codex":0.2681221,"about_ca_topic_score_gemma":0.96996385,"teacher_disagreement_score":0.7018417,"about_ca_system_score_codex":0.0000043625355,"about_ca_system_score_gemma":0.00081300206,"threshold_uncertainty_score":0.7367515},"labels":[],"label_agreement":null},{"id":"W2903215382","doi":"10.1139/cjes-2018-0254","title":"LA-ICP-MS zircon U–Pb and sericite <sup>40</sup>Ar/<sup>39</sup>Ar ages of the Songjianghe gold deposit in southeastern Jilin Province, Northeast China, and their geological significance","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Metamorphism; Zircon; Geochemistry; Greenschist; Sericite; Permian; Geochronology; Metamorphic rock; Subduction; Facies; Metamorphic facies; Paleontology; Quartz; Structural basin; Tectonics","score_opus":0.009862348960662083,"score_gpt":0.17645108308173554,"score_spread":0.16658873412107347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2903215382","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948656,0.0015834526,0.000031004725,0.001765658,0.000049670994,0.00013987711,0.00007183997,0.000004944817,0.001487984],"genre_scores_gemma":[0.9989595,0.000067812776,0.00036833456,0.00031205764,0.00012795668,6.004683e-7,0.0000025437648,0.00000261332,0.00015860614],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979097,0.00027861807,0.0005012561,0.00038876839,0.00032334853,0.00059825624],"domain_scores_gemma":[0.9986094,0.00023389932,0.00027358337,0.00016528893,0.00010665877,0.0006111185],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0010614237,0.00023534284,0.00043670167,0.00021989146,0.00036718574,0.00017298604,0.0006830668,0.00013059199,0.000605115],"category_scores_gemma":[0.00021038459,0.00012268446,0.00012069697,0.00076180947,0.0028663096,0.00036719965,0.00004087803,0.0003842027,0.000012430821],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029114388,0.0000120173945,0.98932576,0.000014473242,0.00001642598,0.000036091238,0.0009648034,0.0037735559,0.00016578227,0.0000324793,0.000012660483,0.0056168595],"study_design_scores_gemma":[0.00022665941,0.00047675663,0.97956526,0.00009914177,0.000022512862,0.00014931419,0.0013521571,0.014876639,0.00030958332,0.0018012929,0.0009284816,0.00019220327],"about_ca_topic_score_codex":0.04005695,"about_ca_topic_score_gemma":0.3806427,"teacher_disagreement_score":0.34058577,"about_ca_system_score_codex":0.000002566095,"about_ca_system_score_gemma":0.0003639637,"threshold_uncertainty_score":0.9998473},"labels":[],"label_agreement":null},{"id":"W2903223694","doi":"10.1139/cjes-2018-0184","title":"Conditions and timing of low-pressure – high-temperature metamorphism in the Montresor Belt, Rae Province, Nunavut","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Andalusite; Geology; Metamorphism; Monazite; Staurolite; Geochemistry; Sillimanite; Biotite; Plagioclase; Muscovite; Metamorphic rock; Grossular; Felsic; Geochronology; Quartz; Kyanite; Mineralogy; Zircon; Mafic; Paleontology","score_opus":0.011152904587850138,"score_gpt":0.19423698834266542,"score_spread":0.18308408375481527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2903223694","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938145,0.0017269497,8.329363e-7,0.002356905,0.00009634541,0.00005497787,0.00006305479,0.000001208614,0.0018852093],"genre_scores_gemma":[0.9990796,0.000021361795,0.00028381927,0.0004177369,0.000103388156,1.6814766e-7,0.000004755798,5.8266676e-7,0.000088593886],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99903077,0.000091437556,0.00024963266,0.00013275568,0.00023807057,0.000257325],"domain_scores_gemma":[0.9992738,0.00015567437,0.00014208762,0.00007689616,0.00010579372,0.00024578796],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006697682,0.00008126414,0.00019182882,0.0002027345,0.00030318295,0.00008930189,0.00040344254,0.000047643724,0.0028070512],"category_scores_gemma":[0.0001750854,0.000042834425,0.000055502736,0.0005611657,0.0011179486,0.00022879016,0.0000053825966,0.0001707823,0.0000075761104],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008472176,0.000011643229,0.9955228,0.000013224008,0.000031181487,0.00008581618,0.00048155957,0.0010929446,0.00065933395,0.0005492073,0.00069804164,0.00084575993],"study_design_scores_gemma":[0.00012780304,0.00024772758,0.99096704,0.000040899864,0.000035964502,0.00006061371,0.00049905694,0.0007957062,0.0005587212,0.005582141,0.0010066136,0.000077720186],"about_ca_topic_score_codex":0.02965979,"about_ca_topic_score_gemma":0.6927972,"teacher_disagreement_score":0.66313744,"about_ca_system_score_codex":4.5652678e-7,"about_ca_system_score_gemma":0.0003284468,"threshold_uncertainty_score":0.9981045},"labels":[],"label_agreement":null},{"id":"W2903480432","doi":"10.1139/cjes-2018-0085","title":"Strontium isotope geochemistry of modern and ancient archives: tracer of secular change in ocean chemistry","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University; University of New Brunswick; Brock University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seawater; Geology; Isotopes of strontium; Halite; Strontium; Diagenesis; Radiogenic nuclide; Calcite; Geochemistry; Oceanography; Mineralogy; Paleontology; Chemistry; Gypsum; Mantle (geology)","score_opus":0.022855595606693303,"score_gpt":0.23402893017684354,"score_spread":0.21117333457015022,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2903480432","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99157786,0.0036766448,0.0000070087026,0.00020891339,0.000080139915,0.000049490263,0.000023758865,6.99733e-7,0.0043754806],"genre_scores_gemma":[0.9995377,0.000050712988,0.00027435506,0.00003825554,0.0000530579,9.710422e-8,0.000001934863,8.9056573e-7,0.000042994994],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990222,0.000051298353,0.00026502245,0.00014026446,0.00017126545,0.0003499734],"domain_scores_gemma":[0.9992959,0.00006703907,0.00016226975,0.000085612504,0.000074016716,0.00031518648],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00065441383,0.00007442176,0.0002056584,0.00017960063,0.00010743193,0.000014455119,0.0003125376,0.000067295354,0.0009297723],"category_scores_gemma":[0.000081569226,0.000060383714,0.000038531136,0.00023519756,0.0021405588,0.00014475867,0.0000071169807,0.00017271069,0.0000016990019],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015517606,0.0000047483186,0.9979443,0.000032565575,0.000006205621,0.000032159813,0.0010760042,0.00007240321,0.00033240186,0.00000553947,0.000008470606,0.00046968774],"study_design_scores_gemma":[0.00020711498,0.0002240373,0.98955494,0.00007330444,0.000005258313,0.00021192332,0.00043122927,0.004677849,0.0040192194,0.0004085145,0.000119564655,0.00006706904],"about_ca_topic_score_codex":0.0020962558,"about_ca_topic_score_gemma":0.10777173,"teacher_disagreement_score":0.105675474,"about_ca_system_score_codex":2.897748e-7,"about_ca_system_score_gemma":0.00066862797,"threshold_uncertainty_score":0.9999835},"labels":[],"label_agreement":null},{"id":"W2903549063","doi":"10.1139/cjes-2018-0069","title":"Deep mineral exploration using multi-scale electromagnetic geophysics: the Lalor massive sulphide deposit case study","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Borehole; Drilling; Geophysics; Geophysical imaging; Mineralogy; Geotechnical engineering","score_opus":0.04469027954365932,"score_gpt":0.26782527691620533,"score_spread":0.22313499737254602,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2903549063","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969034,0.00029479712,0.00164877,0.00033197523,0.0004627143,0.00017277325,0.0000036223157,0.0000041113817,0.00017784427],"genre_scores_gemma":[0.9883305,0.0000025292695,0.010838108,0.00020152642,0.00056351034,4.6372318e-7,5.9897314e-7,0.0000025393786,0.00006025901],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99831843,0.00030218135,0.0003137666,0.00021108719,0.00032240068,0.00053215434],"domain_scores_gemma":[0.9987535,0.00019069009,0.0001953191,0.00012202501,0.00022919923,0.0005093008],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000698338,0.00013855768,0.00019692795,0.00018526662,0.0010984424,0.0002826015,0.0003994998,0.000035196237,0.00024917108],"category_scores_gemma":[0.00014438752,0.00008322928,0.00008147498,0.0010338366,0.00058004825,0.0005774707,0.000006201057,0.00021875453,0.000041528623],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006739179,0.00015390456,0.8105294,0.0000120240375,0.0000954651,0.004590408,0.011534903,0.013505596,0.002807627,0.000047482354,0.00007503579,0.15658073],"study_design_scores_gemma":[0.00049411185,0.005535398,0.8265803,0.000020401189,0.00009328836,0.0021882632,0.007052964,0.15553643,0.00057096273,0.0014587804,0.00017164428,0.0002974996],"about_ca_topic_score_codex":0.09899956,"about_ca_topic_score_gemma":0.706349,"teacher_disagreement_score":0.60734946,"about_ca_system_score_codex":0.0000034033792,"about_ca_system_score_gemma":0.000506037,"threshold_uncertainty_score":0.9070003},"labels":[],"label_agreement":null},{"id":"W2905106246","doi":"10.1139/cjes-2018-0087","title":"Makran continental margin sedimentation during the Late Holocene","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Marine and environmental studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Mass wasting; Holocene; Sedimentation; Sediment; Clastic rock; Continental margin; Contourite; Geochemistry; Turbidity current; Turbidite; Geomorphology; Oceanography; Paleontology; Tectonics; Sedimentary rock; Sedimentary depositional environment","score_opus":0.012891155999353266,"score_gpt":0.19044244041108424,"score_spread":0.177551284411731,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2905106246","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98630804,0.00039521285,0.0000031304728,0.0010812908,0.0004744515,0.000041953583,0.000011098551,0.0000019824715,0.011682819],"genre_scores_gemma":[0.99851626,0.000039080544,0.00012985409,0.0003244213,0.00024205299,7.962207e-8,0.0000011459705,0.0000010097717,0.0007460647],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99927557,0.000030625102,0.00016109468,0.000076034616,0.00019871836,0.0002579792],"domain_scores_gemma":[0.99960256,0.000026703758,0.000101160476,0.000047705482,0.000021244638,0.00020061208],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000398482,0.0000655376,0.00008124175,0.000086093045,0.0007791493,0.00010012448,0.00023633767,0.000015248624,0.0030888754],"category_scores_gemma":[0.000019988234,0.00003913484,0.00003665729,0.00019441682,0.00077259436,0.00025220736,0.0000060716416,0.00007363744,0.00009268601],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057079797,0.0000010751032,0.99622625,0.0000013555432,0.000007762308,0.000016410775,0.00033285865,0.00021235569,0.000033575718,0.0000072344405,0.00018683198,0.0029685718],"study_design_scores_gemma":[0.00013301436,0.00017246798,0.9916383,0.000009443723,0.00000571452,0.000072237795,0.0007310992,0.00023471747,0.00036998067,0.00007111295,0.006505603,0.00005631585],"about_ca_topic_score_codex":0.017974624,"about_ca_topic_score_gemma":0.22644919,"teacher_disagreement_score":0.20847458,"about_ca_system_score_codex":0.0000018715709,"about_ca_system_score_gemma":0.000102849444,"threshold_uncertainty_score":0.99782246},"labels":[],"label_agreement":null},{"id":"W2905571073","doi":"10.1139/cjes-2017-0239","title":"Sediment distribution pattern of the South Caspian Sea: possible hydroclimatic implications","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Marine and environmental studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Terrigenous sediment; Geology; Sediment; Sedimentary rock; Fluvial; Continental margin; Structural basin; Oceanography; Geochemistry; Tectonics; Paleontology","score_opus":0.019092526530030813,"score_gpt":0.20016700160798087,"score_spread":0.18107447507795005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2905571073","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.992971,0.00018569661,0.00007214486,0.0012314903,0.00027695444,0.000055955446,0.00012010389,0.0000011176955,0.00508551],"genre_scores_gemma":[0.9995925,0.000009023069,0.00006447671,0.00017367577,0.000087208544,1.3522667e-7,0.000003428361,7.072746e-7,0.00006884809],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992873,0.000028629827,0.0002032227,0.00007983766,0.00018580555,0.00021519503],"domain_scores_gemma":[0.9994811,0.000023571305,0.00017430521,0.00008852479,0.000035491666,0.00019699874],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003097804,0.000058127647,0.000091802794,0.000048960177,0.0005728799,0.00004185525,0.00029871234,0.000016697219,0.0009399789],"category_scores_gemma":[0.00003016328,0.000034322646,0.000051465668,0.00027635973,0.0007168417,0.0001354734,0.000009599729,0.000060387665,0.00003164635],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[6.2887244e-7,0.0000018753112,0.9945649,0.0000025493703,0.0000058504033,8.5362484e-7,0.00033339113,0.00018255472,0.000005568558,0.000012152033,0.0001982282,0.004691462],"study_design_scores_gemma":[0.000054902946,0.00017247882,0.9962596,0.000020531796,0.0000106965135,0.00002593937,0.00047640788,0.0004883284,0.00016968796,0.00023026412,0.0020466645,0.000044482666],"about_ca_topic_score_codex":0.022729773,"about_ca_topic_score_gemma":0.35068354,"teacher_disagreement_score":0.32795376,"about_ca_system_score_codex":0.000002943354,"about_ca_system_score_gemma":0.00024815407,"threshold_uncertainty_score":0.9999733},"labels":[],"label_agreement":null},{"id":"W2907822770","doi":"10.1139/cjes-2018-0128","title":"A new approach to the opening of the eastern Mediterranean Sea and the origin of the Hellenic Subduction Zone. Part 1: The eastern Mediterranean Sea","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Transform fault; Subduction; Mediterranean sea; Mediterranean climate; Fault (geology); Seismology; Paleontology; Tectonics; Geography; Archaeology","score_opus":0.049107408149788805,"score_gpt":0.2275456644606543,"score_spread":0.1784382563108655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2907822770","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97448874,0.0032869799,0.000033372413,0.013523328,0.0024537456,0.0004930739,0.000028611219,0.0000023590717,0.005689821],"genre_scores_gemma":[0.99753445,0.00007777808,0.000068624286,0.00058695354,0.00046677855,8.4178004e-7,6.64643e-7,0.0000035537369,0.0012603408],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99771696,0.00041783415,0.00044475985,0.00021936162,0.00078770774,0.0004133862],"domain_scores_gemma":[0.9983845,0.0004018858,0.00043585556,0.00040761643,0.000108872795,0.0002612741],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0028931785,0.00016577046,0.00029654652,0.00010251371,0.00090121705,0.00018666223,0.0016350106,0.000043503736,0.0003931271],"category_scores_gemma":[0.00018386212,0.000056968867,0.00016947069,0.0007706297,0.0013787214,0.00026440216,0.00005220327,0.00035558312,0.000024628167],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000059222824,0.000004828564,0.95270294,0.000021041535,0.000089795576,0.0000022401914,0.014577588,0.004351568,0.0000061479614,0.00016636982,0.0018894976,0.026128743],"study_design_scores_gemma":[0.0014705731,0.00048631165,0.8770111,0.00046040025,0.0001709281,0.0005239961,0.018805344,0.02594583,0.00015228543,0.00047127611,0.0741851,0.00031684132],"about_ca_topic_score_codex":0.041396104,"about_ca_topic_score_gemma":0.30607262,"teacher_disagreement_score":0.2646765,"about_ca_system_score_codex":0.000002806112,"about_ca_system_score_gemma":0.0009570956,"threshold_uncertainty_score":0.96498734},"labels":[],"label_agreement":null},{"id":"W2909032402","doi":"10.1139/cjes-2018-0227","title":"Mesozoic C-cycle perturbations and climate: evidence for increased resilience of the Cretaceous biosphere to greenhouse pulses","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Extinction event; Paleontology; Large igneous province; Carbon cycle; Biosphere; Cretaceous; Earth science; Mesozoic; Volcano; Biota; Ecosystem; Ecology; Biological dispersal; Tectonics; Magmatism","score_opus":0.025141683650328067,"score_gpt":0.245838913584122,"score_spread":0.22069722993379393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909032402","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9888294,0.008160761,0.000015759668,0.0009773829,0.0003047364,0.00019426494,0.00006576258,0.0000019627275,0.0014500059],"genre_scores_gemma":[0.998265,0.00005264897,0.001467429,0.00015755314,0.000027814842,3.6832188e-7,2.0787454e-7,5.912264e-7,0.000028382638],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99900585,0.00007645006,0.0002511608,0.00015552629,0.00020483635,0.00030615536],"domain_scores_gemma":[0.9987112,0.0005067835,0.00018502961,0.00012557504,0.00011279276,0.00035856824],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00078981416,0.00008180822,0.00016711857,0.00013253286,0.0004565566,0.00007770717,0.0004995177,0.000044504082,0.00021021225],"category_scores_gemma":[0.0005708325,0.000051497947,0.000069368056,0.00043008724,0.00059159764,0.00041385062,0.0000021064045,0.00009025885,0.0000035392325],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021615671,0.0000016515814,0.99244094,0.000012970084,0.000004955864,0.000002751551,0.00021641275,0.0009813651,0.00012480325,0.00011296531,0.000037773043,0.006041768],"study_design_scores_gemma":[0.00011300088,0.00047132093,0.9972995,0.00011110766,0.000013824127,0.000055752105,0.00033143003,0.00072978885,0.0002185739,0.000364541,0.00021929995,0.000071846145],"about_ca_topic_score_codex":0.010127222,"about_ca_topic_score_gemma":0.5260228,"teacher_disagreement_score":0.51589555,"about_ca_system_score_codex":9.1566915e-7,"about_ca_system_score_gemma":0.00090862886,"threshold_uncertainty_score":0.99646443},"labels":[],"label_agreement":null},{"id":"W2909261623","doi":"10.1139/cjes-2018-0156","title":"Enigmatic massive sulphide mineralization in the High Arctic Large Igneous Province, Nunavut, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; Geological Survey of Canada; Memorial University of Newfoundland","funders":"","keywords":"Geology; Geochemistry; Mineralization (soil science); Sphalerite; Metallogeny; Pyrite; Pyrrhotite; Large igneous province; Igneous rock; Anhydrite; Galena; Bornite; Mafic; Chalcopyrite; Magmatism; Paleontology","score_opus":0.006623818273555746,"score_gpt":0.16696329399252416,"score_spread":0.16033947571896842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909261623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935071,0.00045949698,0.000006270008,0.0034028674,0.00023466846,0.000091940004,0.000028898603,0.0000011219963,0.0022676536],"genre_scores_gemma":[0.9982047,0.000008774634,0.00013489116,0.0013742722,0.0000568035,1.933073e-7,0.0000113737815,7.657766e-7,0.00020824325],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986044,0.000115851246,0.00029886718,0.0001426679,0.0004169241,0.00042127224],"domain_scores_gemma":[0.9991626,0.00021196595,0.00016962901,0.00009065851,0.000086878266,0.0002782792],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006964617,0.00009329502,0.00018389213,0.00016108884,0.000181259,0.00010809801,0.00052679767,0.000031382664,0.006609437],"category_scores_gemma":[0.00023591098,0.000050845953,0.000051723608,0.00071935775,0.00014362666,0.00019142556,0.0000037605525,0.0001665566,0.000038248643],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002754157,0.0000036066226,0.98621255,0.0000075715943,0.000005028712,0.00013982404,0.00009474965,0.0127471965,0.000006157514,0.00038682894,0.00018278434,0.00021092923],"study_design_scores_gemma":[0.00016074812,0.00016256045,0.98560935,0.000038340255,0.0000128066295,0.00007699889,0.0007305799,0.0051722657,0.000016136013,0.004889975,0.0030174274,0.000112792724],"about_ca_topic_score_codex":0.931736,"about_ca_topic_score_gemma":0.99970055,"teacher_disagreement_score":0.067964554,"about_ca_system_score_codex":0.000005278782,"about_ca_system_score_gemma":0.0019604263,"threshold_uncertainty_score":0.99429864},"labels":[],"label_agreement":null},{"id":"W2909263492","doi":"10.1139/cjes-2018-0187","title":"Petrography, geochemistry, and Nd isotope systematics of metaconglomerates and matrix-rich metasedimentary rocks: implications for the provenance and tectonic setting of the Labrador Trough, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; Ministère des Ressources naturelles et des Forêts (Québec); Université Laval","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Craton; Arenite; Provenance; Felsic; Terrane; Petrography; Terrigenous sediment; Mafic; Proterozoic; Metamorphism; Archean; Sedimentary rock; Paleontology; Tectonics; Clastic rock","score_opus":0.00695441376231965,"score_gpt":0.19854887712156977,"score_spread":0.19159446335925012,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909263492","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98768914,0.0101227425,0.000004268744,0.0016061187,0.000057583373,0.00017361762,0.0002689672,4.5950162e-7,0.00007708704],"genre_scores_gemma":[0.99947834,0.00006246386,0.00034486287,0.00005316342,0.000014866472,9.3506185e-7,0.0000029377468,9.385227e-7,0.000041512347],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99924517,0.00002772621,0.00029002034,0.00011260542,0.00014866269,0.00017580239],"domain_scores_gemma":[0.9990971,0.000248544,0.0003382184,0.00009827605,0.000086400454,0.00013146376],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005620436,0.00007834328,0.00019816593,0.000045876062,0.00031792678,0.000058486745,0.00023630325,0.000017019436,0.000061900326],"category_scores_gemma":[0.000061571016,0.0000424875,0.000045466313,0.0003327544,0.00026389136,0.00012175689,0.000008901353,0.000064005115,5.1164662e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002871887,0.00000170936,0.9973749,0.0001762145,0.00007825441,3.1326178e-7,0.000109299865,0.00048845867,0.0009776183,0.0000143836005,0.00006991112,0.00070609665],"study_design_scores_gemma":[0.00033214997,0.0001956105,0.97806466,0.00018326948,0.0003240498,0.00014446558,0.005751812,0.0035239547,0.010188825,0.00035807188,0.00078745384,0.00014566087],"about_ca_topic_score_codex":0.24550256,"about_ca_topic_score_gemma":0.78686386,"teacher_disagreement_score":0.54136133,"about_ca_system_score_codex":0.0000017508722,"about_ca_system_score_gemma":0.0005735328,"threshold_uncertainty_score":0.7595217},"labels":[],"label_agreement":null},{"id":"W2909289743","doi":"10.1139/cjes-2018-0183","title":"Magnetic characterisation of magnetite and hematite from the Blötberget apatite – iron oxide deposits (Bergslagen), south-central Sweden","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Iron Ore Company (Canada)","funders":"","keywords":"Hematite; Magnetite; Magnetic susceptibility; Iron oxide; Magnetic mineralogy; Mineralogy; Geology; Apatite; Geochemistry; Materials science; Chemistry; Magnetization; Metallurgy; Remanence; Crystallography; Magnetic field","score_opus":0.007902762434408434,"score_gpt":0.1922124637500934,"score_spread":0.18430970131568497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909289743","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98890114,0.009775135,0.0000286461,0.00030802598,0.00027733733,0.00012873199,0.00006460521,0.0000011238648,0.00051523605],"genre_scores_gemma":[0.9984124,0.0003021301,0.0006036969,0.0001866973,0.000113502465,0.000001109933,0.000011331755,0.000005213529,0.00036397603],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989688,0.00006942194,0.00029805786,0.00018900742,0.00018674314,0.0002879621],"domain_scores_gemma":[0.9992645,0.000036624962,0.00024671652,0.00016057458,0.00008589075,0.00020572444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026558558,0.00012292952,0.00019378976,0.00010071242,0.00014961309,0.00007554621,0.00028139143,0.000063569416,0.00016087644],"category_scores_gemma":[0.000060876562,0.000089069676,0.00008142219,0.00019911469,0.0003381248,0.000021376052,0.000032585238,0.00007602286,0.000006979695],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014099072,0.0000049834575,0.9311313,0.00001453435,0.00004124668,0.0000057921466,0.00093062257,0.00014320611,0.066841215,0.000032190983,0.00012524505,0.0007155824],"study_design_scores_gemma":[0.00024883868,0.0006149463,0.9931605,0.000036452864,0.00007312266,0.000021894075,0.000289881,0.000044772893,0.0032607208,0.000037407426,0.0021001147,0.00011134566],"about_ca_topic_score_codex":0.0023416504,"about_ca_topic_score_gemma":0.06308511,"teacher_disagreement_score":0.06358049,"about_ca_system_score_codex":0.0000015031975,"about_ca_system_score_gemma":0.0002463307,"threshold_uncertainty_score":0.95401114},"labels":[],"label_agreement":null},{"id":"W2909328254","doi":"10.1139/cjes-2018-0239","title":"Pargasite-bearing vein in spinel lherzolite from the mantle lithosphere of the North America Cordillera","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia; University of Calgary","funders":"","keywords":"Geology; Amphibole; Peridotite; Geochemistry; Mafic; Lithosphere; Mantle (geology); Xenolith; Olivine; Petrology; Tectonics; Paleontology","score_opus":0.011848715711475177,"score_gpt":0.1765500060496676,"score_spread":0.16470129033819245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909328254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9914697,0.001516989,0.0000018501654,0.001607046,0.00018713633,0.000053777418,0.000034244844,0.0000011058498,0.005128142],"genre_scores_gemma":[0.9989283,0.00003232727,0.0002042999,0.0006605706,0.00005573884,7.9987814e-8,0.000002516025,7.893719e-7,0.00011536134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99890417,0.00008039411,0.00029039508,0.00013984628,0.00028830138,0.00029687813],"domain_scores_gemma":[0.9991995,0.0001794384,0.00020900137,0.00014221059,0.000060192935,0.0002096602],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00028899065,0.000083178384,0.00020535846,0.000052278232,0.00015542927,0.000065154716,0.00076790876,0.000028674242,0.011065054],"category_scores_gemma":[0.00013393733,0.000038074362,0.00011418804,0.0008780858,0.0004512893,0.00014150314,0.000013682937,0.00022077243,0.00007578797],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000037427367,0.000003174656,0.9903996,0.000001548565,0.000008690533,0.000007135528,0.00017363166,0.006759613,0.000028630813,0.0000073849897,0.00004872719,0.0025581315],"study_design_scores_gemma":[0.0000807923,0.00008323586,0.99374115,0.000038626087,0.000009128087,0.00000482989,0.00048457703,0.0016579562,0.00006287676,0.0007238177,0.0030524768,0.000060557915],"about_ca_topic_score_codex":0.13651395,"about_ca_topic_score_gemma":0.6447655,"teacher_disagreement_score":0.50825155,"about_ca_system_score_codex":0.000001347901,"about_ca_system_score_gemma":0.00034771717,"threshold_uncertainty_score":0.98983896},"labels":[],"label_agreement":null},{"id":"W2909620987","doi":"10.1139/cjes-2018-0246","title":"Late Pleistocene age, size, and paleoenvironment of a caribou antler from Haida Gwaii, British Columbia","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Pleistocene-Era Hominins and Archaeology","field":"Social Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Antler; Radiocarbon dating; Pleistocene; Geology; Woodland caribou; Archaeology; Glacial period; Woodland; Paleontology; Marine isotope stage; Geography; Interglacial; Ecology; Predation","score_opus":0.013675722316805562,"score_gpt":0.22452789453372002,"score_spread":0.21085217221691446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909620987","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942847,0.0011308733,0.0000037258935,0.0004344401,0.00047722633,0.00011895659,0.000083996536,0.0000023684868,0.003463751],"genre_scores_gemma":[0.99683625,0.0002503744,0.0008450845,0.00021161702,0.0001056566,6.9735887e-7,9.4508584e-7,0.000004446682,0.0017449146],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861187,0.00011782333,0.00031961314,0.00019412837,0.0003380771,0.000418498],"domain_scores_gemma":[0.9988189,0.00018049203,0.00026000247,0.00009031751,0.000059703878,0.0005906083],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008252166,0.00007034828,0.00028705652,0.000077783996,0.00047131686,0.00021685069,0.00038118052,0.00007336617,0.0021083036],"category_scores_gemma":[0.00017746986,0.000087587534,0.0000642557,0.00022383427,0.0022415728,0.0002663295,0.00002652316,0.00013611862,0.0000049070727],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003070267,0.000006990775,0.99492687,0.0000028006675,0.000012253016,0.000111470596,0.0020308143,0.000029308494,0.00016665441,0.000110523586,0.00020888969,0.0023903516],"study_design_scores_gemma":[0.00028809076,0.00022404431,0.98389834,0.00006716902,0.000010313005,0.000017799575,0.0011540799,0.000014332519,0.000025071891,0.0011117238,0.013082443,0.00010661221],"about_ca_topic_score_codex":0.38440266,"about_ca_topic_score_gemma":0.99084383,"teacher_disagreement_score":0.60644114,"about_ca_system_score_codex":0.000015496702,"about_ca_system_score_gemma":0.0010294089,"threshold_uncertainty_score":0.9988039},"labels":[],"label_agreement":null},{"id":"W2909744272","doi":"10.1139/cjes-2018-0142","title":"Nd isotope mapping of the Grenvillian Allochthon Boundary Thrust in Algonquin Park, Ontario","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"McMaster University; Ontario Ministry of Natural Resources and Forestry; Ministry of Natural Resources","keywords":"Allochthon; Geology; Boundary (topology); Tectonics; Paleontology; Geomorphology; Nappe","score_opus":0.01826356226396309,"score_gpt":0.18081665352668422,"score_spread":0.16255309126272113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909744272","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9820295,0.00085620483,0.0000020159828,0.0011938545,0.00036115118,0.00006625237,0.000009417036,9.547521e-7,0.015480661],"genre_scores_gemma":[0.99874204,0.00001037986,0.0003474286,0.00034152504,0.000035135,7.6087275e-8,0.0000014929535,7.39541e-7,0.00052117667],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99868053,0.00007458343,0.0003785021,0.00016277721,0.00032463582,0.00037898618],"domain_scores_gemma":[0.9992076,0.000082242404,0.00022216517,0.00011925572,0.00006154026,0.00030720927],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00080935133,0.00009697902,0.00024394202,0.0002039706,0.00016846764,0.00007573809,0.0006645009,0.000051233394,0.017842654],"category_scores_gemma":[0.00008239111,0.000054381853,0.00013548114,0.0007547958,0.000560481,0.00022640455,0.000010982557,0.00026864847,0.000056999972],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003377703,0.0000032448436,0.99543256,0.0000035733146,0.000007149312,0.00001341387,0.00037000992,0.0023854354,0.00007870422,0.000023167458,0.000047651258,0.0016316989],"study_design_scores_gemma":[0.000110336914,0.00012215025,0.987523,0.000059656093,0.0000065847953,0.000027765285,0.0003938361,0.00038154254,0.00016024013,0.0022407244,0.008889527,0.00008464655],"about_ca_topic_score_codex":0.3825767,"about_ca_topic_score_gemma":0.98073035,"teacher_disagreement_score":0.59815365,"about_ca_system_score_codex":0.0000042753486,"about_ca_system_score_gemma":0.0011703674,"threshold_uncertainty_score":0.9830552},"labels":[],"label_agreement":null},{"id":"W2911151763","doi":"10.1139/cjes-2018-0210","title":"Partitioned tectonic shortening, with emphasis on outcrop-scale folding and flattening, Pindos fold-and-thrust belt, Peloponnese, Greece","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Outcrop; Geology; Fold (higher-order function); Flattening; Cretaceous; Tectonics; Nappe; Paleontology","score_opus":0.012403368541324728,"score_gpt":0.19098960681566163,"score_spread":0.1785862382743369,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2911151763","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99316084,0.0009145393,0.00001807559,0.0011595165,0.00010541768,0.00007309449,0.000011837952,0.0000056766726,0.004550971],"genre_scores_gemma":[0.9983821,0.000044420587,0.0009582447,0.00035381995,0.00005999324,2.9642888e-7,0.000003435058,0.0000020051632,0.00019570706],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99859554,0.000048284488,0.00026438024,0.00029324665,0.0003370088,0.00046156356],"domain_scores_gemma":[0.9988125,0.00013055369,0.00016390969,0.00009065826,0.00009016767,0.00071223633],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005173636,0.00015320322,0.00029067844,0.00027506275,0.00045438018,0.00019703181,0.00024287692,0.000055492223,0.0045429],"category_scores_gemma":[0.000058545098,0.0000935111,0.0000686594,0.0005219637,0.000502715,0.00031740047,0.000008493189,0.00020199042,0.000044379773],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016890363,0.000003338426,0.98993635,0.0000049151913,0.00002180178,0.000041794436,0.0001317042,0.0011023174,0.00006887081,0.000030190695,0.000021717191,0.008620125],"study_design_scores_gemma":[0.0002997505,0.0011274599,0.9922109,0.000091251044,0.000050500814,0.0002678943,0.00056343176,0.0029039069,0.0003538756,0.0007163912,0.0011912985,0.00022328722],"about_ca_topic_score_codex":0.010256737,"about_ca_topic_score_gemma":0.27989176,"teacher_disagreement_score":0.26963502,"about_ca_system_score_codex":0.000001999288,"about_ca_system_score_gemma":0.00023193727,"threshold_uncertainty_score":0.9963671},"labels":[],"label_agreement":null},{"id":"W2911408026","doi":"10.1139/cjes-2018-0207","title":"Baffin Bay/Nares Strait surface (seafloor) sediment mineralogy: further investigations and methods to elucidate spatial variations in provenance","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Provenance; Sediment; Seafloor spreading; Heavy mineral; Facies; Geochemistry; Spatial distribution; Bay; Mineralogy; Plagioclase; Compositional data; Geomorphology; Oceanography; Paleontology; Remote sensing; Structural basin","score_opus":0.023149012176876215,"score_gpt":0.2778537779976242,"score_spread":0.25470476582074797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2911408026","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9897526,0.00069299765,0.00020864133,0.00615303,0.00039530566,0.00019845659,0.000027373815,0.0000025237377,0.0025691073],"genre_scores_gemma":[0.9745222,0.000013641723,0.024755482,0.00042760887,0.00003420464,5.0152806e-7,0.0000038242842,0.000001537587,0.00024104535],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99855775,0.00032731198,0.00028462536,0.00021350502,0.00017026499,0.00044656053],"domain_scores_gemma":[0.99887735,0.00029631797,0.000105312334,0.00009649297,0.00008204025,0.0005424615],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018634261,0.00009639046,0.00020197961,0.000374441,0.00021632871,0.000085998785,0.0003104189,0.00007380726,0.0015737195],"category_scores_gemma":[0.00024200793,0.00007735889,0.000027420987,0.00054600835,0.00043639168,0.00030247698,0.0000084096955,0.00023798774,0.00008179254],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006547422,0.000003034512,0.98710436,0.000004807295,0.0000069799257,0.000020646728,0.00059563864,0.010982839,0.00007722174,0.000320972,0.000035713074,0.0008412159],"study_design_scores_gemma":[0.00020174256,0.0002899452,0.9923705,0.000031273947,0.000004740711,0.00007779593,0.00030527735,0.0035616122,0.00008632296,0.0015590088,0.0014149327,0.00009687574],"about_ca_topic_score_codex":0.014164957,"about_ca_topic_score_gemma":0.79206175,"teacher_disagreement_score":0.7778968,"about_ca_system_score_codex":9.75247e-7,"about_ca_system_score_gemma":0.0013419866,"threshold_uncertainty_score":0.999339},"labels":[],"label_agreement":null},{"id":"W2911763842","doi":"10.1139/cjes-2018-0042","title":"Significance of the metasomatized lithospheric mantle in the formation of early basalts and Cu – platinum group element sulfide mineralization in the Coldwell Complex, Midcontinent Rift, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Geology; Gabbro; Geochemistry; Lithophile; Basalt; Mantle (geology); Mantle plume; Partial melting; Rift; Magmatism; Fractional crystallization (geology); Incompatible element; Metasomatism; Pillow lava; Trace element; Lithosphere; Volcanic rock; Paleontology; Volcano; Tectonics","score_opus":0.014202389642383979,"score_gpt":0.18255764255988013,"score_spread":0.16835525291749615,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2911763842","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99718267,0.0003913314,0.000009859584,0.0015601416,0.000057825626,0.00016933477,0.000022205233,2.8668757e-7,0.00060632516],"genre_scores_gemma":[0.99941546,0.000012724303,0.00020048805,0.0003409986,0.000009469357,4.728148e-7,0.000004144152,4.2515927e-7,0.000015806409],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987755,0.00020314792,0.00039162353,0.00008102318,0.0003670886,0.0001816506],"domain_scores_gemma":[0.99925816,0.00023524252,0.00030814097,0.00008147291,0.000051906485,0.00006509827],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010940358,0.0000644224,0.00016867992,0.000057521283,0.0000855617,0.000039504117,0.00043161557,0.000016809043,0.00040603356],"category_scores_gemma":[0.00007426846,0.000028236045,0.000039888815,0.00071445166,0.00017886856,0.00015140758,0.000004727117,0.00008756245,6.5534107e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000067570277,0.0000046832765,0.9947576,0.000010942662,0.000003251734,0.000002227475,0.00061428157,0.00393652,0.00020888644,0.00012002959,0.00007467604,0.0002601263],"study_design_scores_gemma":[0.00017419977,0.00010773887,0.9886883,0.000028003573,0.000008962114,0.0000065616337,0.0014904279,0.008157299,0.00013215009,0.0006196426,0.0005456576,0.000041090196],"about_ca_topic_score_codex":0.8121195,"about_ca_topic_score_gemma":0.9945583,"teacher_disagreement_score":0.18243876,"about_ca_system_score_codex":0.0000024621413,"about_ca_system_score_gemma":0.00021696443,"threshold_uncertainty_score":0.4445783},"labels":[],"label_agreement":null},{"id":"W2911778962","doi":"10.1139/cjes-2018-0304","title":"Introduction to “Advances in low-temperature geochemistry, diagenesis, and seawater and climate evolution through the Earth’s history: a tribute to Ján Veizer”","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; University of Windsor","funders":"","keywords":"Geology; Diagenesis; Earth history; Earth (classical element); Seawater; Tribute; Geochemistry; Early Earth; Earth science; Oceanography; Paleontology; Archaeology","score_opus":0.007438322799173859,"score_gpt":0.19729473300643668,"score_spread":0.18985641020726282,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2911778962","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9642726,0.026688792,0.0000053334456,0.006879978,0.00072809536,0.00012664017,0.000018834038,0.0000023893979,0.0012773473],"genre_scores_gemma":[0.9988593,0.00030418177,0.00030624715,0.00023428559,0.00021446576,5.6870465e-7,0.0000011645468,6.440792e-7,0.000079160076],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989619,0.00007377571,0.00020189301,0.00023115733,0.00016379361,0.00036746036],"domain_scores_gemma":[0.9993944,0.00005409867,0.00008409246,0.00008987225,0.000052428484,0.00032510207],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00071492244,0.00010457635,0.00016938719,0.00017004467,0.00026672488,0.000096722026,0.00019337745,0.000059613445,0.00018956096],"category_scores_gemma":[0.00007397188,0.00006954779,0.00002901728,0.00030134353,0.0003212636,0.0006265943,0.0000021862716,0.00016559116,0.000009313892],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004706412,0.0000030165745,0.989864,0.000020562367,0.000006168216,0.000023317094,0.0012156569,0.000975922,0.0008565708,0.00008941528,0.0008301307,0.006068202],"study_design_scores_gemma":[0.00013948721,0.00025497944,0.9650892,0.000048491744,0.0000053272056,0.00011823191,0.00045744245,0.00006141975,0.0003023368,0.00016016583,0.03325849,0.000104436396],"about_ca_topic_score_codex":0.004060744,"about_ca_topic_score_gemma":0.3987242,"teacher_disagreement_score":0.39466345,"about_ca_system_score_codex":0.000004541086,"about_ca_system_score_gemma":0.00037319554,"threshold_uncertainty_score":0.6138657},"labels":[],"label_agreement":null},{"id":"W2912400917","doi":"10.1139/cjes-2018-0232","title":"Crustal density structure of the northwestern Iranian Plateau","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Institute for Advanced Studies in Basic Sciences; Chinese Academy of Sciences","keywords":"Geology; Crust; Plateau (mathematics); Fibrous joint; Seismology; Tectonics; Continental crust; Fault (geology); Gravity anomaly; Receiver function; Structural basin; Geophysics; Geomorphology; Lithosphere; Paleontology","score_opus":0.008292054269181512,"score_gpt":0.1779468789565308,"score_spread":0.1696548246873493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2912400917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967307,0.00011537939,0.0000015104699,0.00013720697,0.0017840863,0.00006945254,0.0001286371,0.000001189284,0.0010318767],"genre_scores_gemma":[0.99954313,0.0000026837297,0.00011290688,0.00010759407,0.000114743634,8.508326e-9,0.0000013564644,0.0000012804958,0.00011630836],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999065,0.000052662108,0.00023037083,0.00010492851,0.00029060195,0.0002564528],"domain_scores_gemma":[0.9992519,0.000037547507,0.0002473505,0.00012537757,0.000089901376,0.00024794944],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002749331,0.00008043044,0.00018039232,0.00009255629,0.00020200356,0.00010324011,0.0005324686,0.00004042644,0.0019054104],"category_scores_gemma":[0.00002119509,0.00004632951,0.00007106107,0.00024170795,0.00028065775,0.0002687191,0.0000069288653,0.000106676736,0.00002814823],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004872401,0.0000010234298,0.9939717,0.00000808048,0.000008905015,0.000009581939,0.00043750167,0.0028717655,0.0022321464,0.000102343845,0.000036764835,0.00031529812],"study_design_scores_gemma":[0.000104372586,0.00011751058,0.99422324,0.00003302826,0.000009370295,0.00005256452,0.00016519339,0.00006442221,0.0027287544,0.00053074607,0.0019004773,0.00007030304],"about_ca_topic_score_codex":0.042449497,"about_ca_topic_score_gemma":0.5962536,"teacher_disagreement_score":0.5538041,"about_ca_system_score_codex":7.250707e-7,"about_ca_system_score_gemma":0.0008995779,"threshold_uncertainty_score":0.999007},"labels":[],"label_agreement":null},{"id":"W2913045111","doi":"10.1139/cjes-2018-0226","title":"Fluid compartmentalization of Devonian and Mississippian dolostones, Western Canada Sedimentary Basin: petrologic and geochemical evidence from fracture mineralization","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Dolomite; Devonian; Calcite; Fluid inclusions; Geochemistry; Petrography; Diagenesis; Mineralogy; Sedimentary rock; Hydrothermal circulation; Paleontology","score_opus":0.016476348173387712,"score_gpt":0.2123408079424194,"score_spread":0.1958644597690317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2913045111","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98410666,0.013611684,0.000014838731,0.0015308061,0.00023008918,0.00006468893,0.00006240882,0.000001313539,0.0003775143],"genre_scores_gemma":[0.99887407,0.00010406824,0.00048449202,0.0004812312,0.000035737205,6.215693e-8,0.000010440395,4.9637214e-7,0.000009426275],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990829,0.000086954,0.00025265632,0.000161528,0.00021543105,0.0002005275],"domain_scores_gemma":[0.99916375,0.0001585286,0.00019959461,0.00006017665,0.000049919938,0.00036805717],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027818783,0.000097916905,0.00020864127,0.000121540914,0.00016507378,0.000052482297,0.00016891964,0.000059118105,0.0004032072],"category_scores_gemma":[0.000038025824,0.000075355776,0.000022811631,0.00015433034,0.00039053062,0.00040244692,0.0000013165225,0.000092308015,5.324377e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001495096,0.0000016155544,0.99841136,0.000007851325,0.000012318031,0.000022967819,0.00018786639,0.00021727939,0.00021500015,0.0000044033577,0.00017744777,0.000726935],"study_design_scores_gemma":[0.00016174342,0.0002167928,0.997063,0.000090206035,0.000016188831,0.00009666444,0.00022075485,0.0007343259,0.00046403546,0.000081082166,0.0007712195,0.00008398087],"about_ca_topic_score_codex":0.7375284,"about_ca_topic_score_gemma":0.9787536,"teacher_disagreement_score":0.24122527,"about_ca_system_score_codex":0.0000022510405,"about_ca_system_score_gemma":0.00093177386,"threshold_uncertainty_score":0.44148362},"labels":[],"label_agreement":null},{"id":"W2913563750","doi":"10.1139/cjes-2018-0272","title":"Late Pleistocene records of felids from Medicine Hat, Alberta, including the first Canadian record of the sabre-toothed cat <i>Smilodon fatalis</i>","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Wildlife Ecology and Conservation","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; University of Toronto","funders":"Florida Museum of Natural History","keywords":"Panthera; Cave; Pleistocene; Interglacial; Range (aeronautics); Paleontology; Geography; Geology; Zoology; Archaeology; Biology; Predation","score_opus":0.018228588774442757,"score_gpt":0.20980068232887966,"score_spread":0.1915720935544369,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2913563750","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9717645,0.000097265605,0.0000032143616,0.017731655,0.0010989862,0.0001399625,0.000019200226,9.778828e-7,0.009144245],"genre_scores_gemma":[0.9962327,0.000022144466,0.00014975743,0.0027337722,0.000081484606,9.492608e-7,0.0000011776342,0.000005211595,0.00077281403],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998666,0.000095734336,0.00044370533,0.00016629904,0.0003033204,0.0003249246],"domain_scores_gemma":[0.99862844,0.00028995887,0.0004950913,0.00024838775,0.0000414051,0.00029670462],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001011674,0.000109922374,0.00023120266,0.00011713976,0.00049188227,0.000021107699,0.0009746252,0.00007166572,0.00275368],"category_scores_gemma":[0.00026548997,0.00006395876,0.00007387857,0.0005948432,0.0012739068,0.00028749113,0.000042176798,0.00016444435,0.000028976494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000779517,0.000002324856,0.99477845,0.0000025598051,0.00001072952,0.0000026154705,0.00095131644,0.0006103974,0.00018574184,0.000052715768,0.002476514,0.0009188469],"study_design_scores_gemma":[0.00019344829,0.00018544406,0.9635241,0.00011409307,0.000020627374,0.000013005527,0.00034336254,0.00033149673,0.00026716586,0.0006586759,0.034268335,0.00008024247],"about_ca_topic_score_codex":0.9286563,"about_ca_topic_score_gemma":0.99777263,"teacher_disagreement_score":0.06911639,"about_ca_system_score_codex":0.00007056999,"about_ca_system_score_gemma":0.0009376244,"threshold_uncertainty_score":0.9981579},"labels":[],"label_agreement":null},{"id":"W2914103155","doi":"10.1139/cjes-2018-0299","title":"Rare metal indicator minerals in bedrock and till at the Strange Lake peralkaline complex, Quebec and Labrador, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Kellogg's (Canada); Geological Survey of Canada","funders":"","keywords":"Geology; Peralkaline rock; Geochemistry; Monazite; Zircon; Allanite; Rare-earth element; Mineral; Mineralogy; Carbonate minerals; Silicate; Rare earth; Chemistry; Dolomite; Volcano","score_opus":0.013582662927547179,"score_gpt":0.18366544108452673,"score_spread":0.17008277815697956,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914103155","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99065554,0.002731907,9.7963806e-8,0.005486886,0.0000748743,0.00005374598,0.00011303509,8.839334e-7,0.00088302244],"genre_scores_gemma":[0.99809396,0.000035213314,0.000057649984,0.0010256756,0.00003397997,9.097809e-8,0.000011024026,7.127996e-7,0.00074169756],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990211,0.000060552124,0.00022169236,0.00015829386,0.00023770133,0.0003006407],"domain_scores_gemma":[0.9992194,0.00013291872,0.00010193526,0.0000586976,0.000030768817,0.00045627035],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003842803,0.000092922026,0.00021126874,0.000111004556,0.00020133545,0.00007842371,0.0002353993,0.000030763997,0.010738104],"category_scores_gemma":[0.000053249383,0.000050213323,0.00003410311,0.0003012885,0.00040970644,0.00015650365,0.000010059644,0.0001376955,0.000010144424],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004098385,0.0000012236258,0.99800473,0.0000039720076,0.0000075479293,0.000039286617,0.00009126262,0.0002956709,0.000066854875,0.000019113331,0.00027804545,0.0011881819],"study_design_scores_gemma":[0.0001480117,0.00007705616,0.9792335,0.000009811143,0.0000102869,0.00006704827,0.00028402937,0.00061494636,0.000028271883,0.00019168413,0.01925178,0.000083596344],"about_ca_topic_score_codex":0.9490004,"about_ca_topic_score_gemma":0.9999668,"teacher_disagreement_score":0.05096636,"about_ca_system_score_codex":0.0000025636305,"about_ca_system_score_gemma":0.0006294316,"threshold_uncertainty_score":0.9901662},"labels":[],"label_agreement":null},{"id":"W2914137553","doi":"10.1139/cjes-2018-0098","title":"First high-precision U–Pb CA–ID–TIMS age for the Battle Formation (Upper Cretaceous), Red Deer River valley, Alberta, Canada: implications for ages, correlations, and dinosaur biostratigraphy of the Scollard, Frenchman, and Hell Creek formations","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Royal Tyrrell Museum","funders":"Government of Alberta","keywords":"Geology; Cretaceous; Radiometric dating; Paleontology; Unconformity; Geochronology; Horizon; Geochemistry; Tectonics","score_opus":0.013113307428519067,"score_gpt":0.19569077954155137,"score_spread":0.1825774721130323,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914137553","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9817809,0.0037776243,0.0010375238,0.010261244,0.0010295503,0.0006509008,0.0008209947,0.0000017664007,0.00063953275],"genre_scores_gemma":[0.9980822,0.00014895631,0.001387501,0.00014918535,0.000036701604,0.0000032683213,0.00004721243,0.0000011807334,0.00014379038],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99917567,0.000049452752,0.0003036279,0.000121793484,0.0001125165,0.0002369122],"domain_scores_gemma":[0.99790746,0.0014191034,0.00025658953,0.000119581695,0.00013906392,0.00015820989],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004367195,0.00008441784,0.00014403496,0.000119586555,0.0011749094,0.00006241677,0.00028366037,0.00007102948,0.00014283448],"category_scores_gemma":[0.00025271357,0.00005240042,0.000055216413,0.00022726785,0.000548345,0.0004557831,0.00000603022,0.000090256355,0.0000013001729],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010173929,0.000002262116,0.9915762,0.000012709471,0.000020488515,2.867227e-7,0.00024449587,0.002889206,0.0000143450525,0.00052018027,0.0040952717,0.0006143934],"study_design_scores_gemma":[0.00022985517,0.00016662215,0.9656475,0.000026568843,0.000032504595,0.00006236451,0.00020402213,0.0058294185,0.000007733828,0.0015615204,0.02616105,0.00007080343],"about_ca_topic_score_codex":0.3611379,"about_ca_topic_score_gemma":0.9970508,"teacher_disagreement_score":0.63591295,"about_ca_system_score_codex":0.0000043106966,"about_ca_system_score_gemma":0.0007379035,"threshold_uncertainty_score":0.90365726},"labels":[],"label_agreement":null},{"id":"W2914154071","doi":"10.1139/cjes-2018-0260","title":"Evolution of migrating transform faults in anisotropic oceanic crust: examples from Iceland","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation","keywords":"Transform fault; Geology; Seismology; Plate tectonics; Hotspot (geology); Fault (geology); Rift; Strike-slip tectonics; Mid-ocean ridge; Ridge; Tectonics; Rift zone; Seafloor spreading; Extensional definition; Paleontology; Basalt","score_opus":0.017753102009896816,"score_gpt":0.2028390283221711,"score_spread":0.18508592631227427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914154071","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893128,0.0052683936,0.000016672917,0.0001244217,0.0003701708,0.00007734788,0.000046151592,0.00000210733,0.0047819237],"genre_scores_gemma":[0.99931616,0.00007660866,0.0004679239,0.00003209176,0.000059577942,6.105752e-8,0.0000020751852,0.000001312075,0.000044175886],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885327,0.000047600864,0.0003700179,0.0001446941,0.00026314464,0.0003212482],"domain_scores_gemma":[0.99930525,0.00018003,0.00018783697,0.00007363515,0.000061442595,0.00019179907],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000466103,0.000092559196,0.00023708043,0.00031817134,0.00014263522,0.000038030194,0.00027334774,0.000044390996,0.0013676672],"category_scores_gemma":[0.0000744641,0.0000695881,0.00006670994,0.0004601834,0.00021876974,0.0003772592,0.000002237949,0.000140839,0.000026560376],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006351999,0.0000022722231,0.99427,0.0000059228437,0.000007838426,0.000017310489,0.0006610128,0.0012467771,0.000054347038,0.00007604272,0.000010741389,0.003641374],"study_design_scores_gemma":[0.00030921563,0.000339436,0.9940273,0.00010673177,0.0000071028694,0.000015860847,0.001996013,0.001404011,0.00011670599,0.00082412193,0.00076904485,0.00008443334],"about_ca_topic_score_codex":0.15361711,"about_ca_topic_score_gemma":0.85016763,"teacher_disagreement_score":0.6965505,"about_ca_system_score_codex":0.000003874528,"about_ca_system_score_gemma":0.00093048514,"threshold_uncertainty_score":0.9995452},"labels":[],"label_agreement":null},{"id":"W2914275246","doi":"10.1139/cjes-2018-0248","title":"New U–Pb age constraints on the geological history of the Ganderian Bras d’Or terrane, Cape Breton Island, Nova Scotia","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Nova Scotia Department of Energy; Acadia University; Cape Breton University","funders":"Natural Sciences and Engineering Research Council of Canada; Cape Breton University","keywords":"Terrane; Geology; Gondwana; Zircon; Provenance; Geochemistry; Craton; Pluton; Protolith; Volcanic rock; Metamorphism; Paleontology; Structural basin; Volcano; Tectonics","score_opus":0.03054954731970327,"score_gpt":0.19105022680004075,"score_spread":0.16050067948033747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914275246","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95378053,0.0004463196,0.000008661608,0.004073738,0.0008609472,0.00008761564,0.000017681175,0.0000020450955,0.04072244],"genre_scores_gemma":[0.99563867,0.000008074879,0.00013980005,0.0017090963,0.00009588521,3.221035e-8,0.000001526769,9.571592e-7,0.0024059857],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998596,0.00011962693,0.00032677618,0.00018407164,0.00039813935,0.00037535946],"domain_scores_gemma":[0.9988007,0.00030430517,0.00024813812,0.00016007248,0.000061000854,0.00042578072],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006616257,0.00012529087,0.00025944333,0.00010904648,0.00013723515,0.000052263564,0.0008669406,0.000070426875,0.12329087],"category_scores_gemma":[0.00027714905,0.000049488684,0.00017208603,0.00039631722,0.0015413394,0.00010788804,0.000010377177,0.0002877379,0.000186974],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033618177,0.000007055268,0.98961014,0.000005204255,0.000026749403,0.00006567617,0.00031661,0.0013931813,0.0003170523,0.0003095514,0.0044454327,0.0034697063],"study_design_scores_gemma":[0.00025307926,0.000606539,0.980999,0.000066783345,0.000027878283,0.00016834258,0.00037896176,0.00030839263,0.00028041264,0.0023473273,0.014411438,0.00015184334],"about_ca_topic_score_codex":0.047851797,"about_ca_topic_score_gemma":0.7175017,"teacher_disagreement_score":0.6696499,"about_ca_system_score_codex":0.000004857226,"about_ca_system_score_gemma":0.0015511374,"threshold_uncertainty_score":0.95848864},"labels":[],"label_agreement":null},{"id":"W2914327947","doi":"10.1139/cjes-2018-0033","title":"The role of magma injection and crystal sorting in the formation of early gabbros at the Coldwell Complex, Ontario, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor; Western University","funders":"","keywords":"Geology; Olivine; Gabbro; Augite; Geochemistry; Magma; Magma chamber; Plagioclase; Layered intrusion; Fractional crystallization (geology); Phenocryst; Ultramafic rock; Petrography; Petrogenesis; Mafic; Igneous rock; Volcanic rock; Basalt; Quartz; Volcano","score_opus":0.010013962341087704,"score_gpt":0.16607572156618633,"score_spread":0.15606175922509863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914327947","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99487954,0.0004832952,7.6010406e-7,0.0006807988,0.000054762568,0.00006115305,0.000009352375,2.6176355e-7,0.0038300469],"genre_scores_gemma":[0.9997677,0.00000634162,0.0000192199,0.00011749832,0.000010864052,9.528512e-8,0.0000015048493,2.853281e-7,0.000076457785],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991346,0.000073453004,0.00027537474,0.00006074354,0.0002731543,0.00018269237],"domain_scores_gemma":[0.99929786,0.00024150097,0.00025230457,0.00005829702,0.00006249814,0.000087550725],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008519905,0.00004782798,0.00010630701,0.00004806429,0.00030069618,0.000050898318,0.00028201705,0.000016834612,0.00096586125],"category_scores_gemma":[0.000056907636,0.00002019045,0.000036363796,0.0002876668,0.00032559875,0.00014018752,0.000006193711,0.000112197034,0.0000015200009],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007427661,9.125936e-7,0.99507046,0.0000019260485,0.000002868606,0.0000011336211,0.0005661271,0.0027432812,0.00018832575,0.00003896095,0.000039830804,0.0013387585],"study_design_scores_gemma":[0.000059205027,0.00016780013,0.9899783,0.000010117134,0.0000059981276,0.000033399534,0.0026576726,0.0024593074,0.0001928981,0.0015417901,0.0028613165,0.000032203905],"about_ca_topic_score_codex":0.98133767,"about_ca_topic_score_gemma":0.9998963,"teacher_disagreement_score":0.018558616,"about_ca_system_score_codex":0.0000045763054,"about_ca_system_score_gemma":0.0005532515,"threshold_uncertainty_score":0.99994737},"labels":[],"label_agreement":null},{"id":"W2914681700","doi":"10.1139/cjes-2018-0083","title":"Geochemical, isotopic, and U–Pb zircon study of the central and southern portions of the 780 Ma Gunbarrel Large Igneous Province in western Laurentia","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Zircon; Large igneous province; Craton; Geochemistry; Mantle plume; Igneous rock; Sill; Flood basalt; Plume; Crust; Basalt; Continental crust; Laurentia; Mantle (geology); Magma; Volcano; Paleozoic; Magmatism; Paleontology; Tectonics; Volcanism","score_opus":0.0072973230012343005,"score_gpt":0.17605992047665325,"score_spread":0.16876259747541894,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914681700","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99825627,0.0005558393,0.0000012952738,0.000631689,0.00009711887,0.00012139088,0.000035125868,6.389333e-7,0.0003006248],"genre_scores_gemma":[0.9997468,0.000008129001,0.00002624725,0.000076064505,0.000015166143,9.731656e-8,4.796175e-7,5.736659e-7,0.00012643595],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990668,0.0000680893,0.00027961252,0.00012671063,0.0002176143,0.00024116877],"domain_scores_gemma":[0.9994244,0.000055184548,0.0002082714,0.00009885542,0.00004437724,0.00016890373],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031786846,0.000068661655,0.00017201234,0.00006503062,0.00012149745,0.00003366467,0.00034416924,0.000031926276,0.0005277928],"category_scores_gemma":[0.00007228855,0.000033335393,0.000053626514,0.00028009815,0.0003359816,0.00008283794,0.000020388185,0.00013456118,0.0000016435837],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003229895,0.00001525085,0.99856347,0.0000059259787,0.0000070742294,0.0000035572325,0.00052916666,0.00035771754,0.00030086524,0.000017572072,0.0000044198914,0.00019173934],"study_design_scores_gemma":[0.00020061954,0.00015665313,0.99635696,0.00003414692,0.000018813462,0.000022052931,0.0016012138,0.0003405909,0.00030140422,0.00080361037,0.000115053466,0.000048871116],"about_ca_topic_score_codex":0.026672434,"about_ca_topic_score_gemma":0.71864504,"teacher_disagreement_score":0.6919726,"about_ca_system_score_codex":8.263809e-7,"about_ca_system_score_gemma":0.00023095155,"threshold_uncertainty_score":0.97980905},"labels":[],"label_agreement":null},{"id":"W2914879532","doi":"10.1139/cjes-2018-0267","title":"Early Eocene (Ypresian) birds from the Okanagan Highlands, British Columbia (Canada) and Washington State (USA)","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; Royal British Columbia Museum","funders":"","keywords":"Geology; Paleontology; Canyon; Taxon; Paleogene; Taphonomy; Geography; Structural basin","score_opus":0.008045606274943875,"score_gpt":0.16875572593943136,"score_spread":0.16071011966448748,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914879532","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9917072,0.0032525952,0.0000025890124,0.0011258237,0.0010889053,0.000064408465,0.00022406678,0.0000026447997,0.0025317615],"genre_scores_gemma":[0.99833703,0.000118473174,0.00014178788,0.00066931336,0.000121146295,8.65964e-8,0.0000065240406,0.0000014558454,0.0006041831],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99876946,0.00012932363,0.00023327595,0.00019555118,0.00024095266,0.00043144854],"domain_scores_gemma":[0.9989539,0.00027146674,0.00015703881,0.00009762056,0.000060905917,0.0004590768],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000587849,0.0000778949,0.00018336778,0.00005112845,0.0006294199,0.00034733023,0.000491376,0.000060249648,0.0029260665],"category_scores_gemma":[0.00007991442,0.00006989807,0.000033471373,0.00022116241,0.00064792926,0.0003675299,0.0000060312045,0.00021927427,0.000027445496],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000053519557,8.593562e-7,0.99408525,0.0000012750619,0.000013821864,0.00008735898,0.000085217245,0.000108887376,0.000004453017,0.0000061410574,0.0014878989,0.0041135033],"study_design_scores_gemma":[0.00016419559,0.00019804879,0.98508394,0.000029068457,0.000007631704,0.00020734947,0.00012945206,0.00019516643,0.000002123947,0.0008070461,0.013074295,0.00010166781],"about_ca_topic_score_codex":0.99355227,"about_ca_topic_score_gemma":0.9999802,"teacher_disagreement_score":0.011586396,"about_ca_system_score_codex":0.0000026976684,"about_ca_system_score_gemma":0.0021409811,"threshold_uncertainty_score":0.9979854},"labels":[],"label_agreement":null},{"id":"W2915724217","doi":"10.1139/cjes-2016-0107","title":"Early–Middle Paleozoic ecosystem evolution and revolution (Part 2 of 2): an introduction","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University; Western University","funders":"","keywords":"Paleozoic; Geology; Peninsula; Stratigraphy; Paleontology; Excursion; Devonian; Archaeology; Geography; Tectonics","score_opus":0.02647378186472681,"score_gpt":0.18348195894159347,"score_spread":0.15700817707686665,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2915724217","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99625486,0.0008284155,0.00020600125,0.0016074103,0.0006810574,0.000050477774,0.000019060415,0.0000028430306,0.0003498674],"genre_scores_gemma":[0.99914396,0.00007274116,0.00033855197,0.000013560278,0.00038635844,1.2744582e-7,0.0000012531574,6.667132e-7,0.000042798136],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991151,0.00008506355,0.0002680036,0.00013353626,0.00018376959,0.00021453836],"domain_scores_gemma":[0.9992767,0.00003915489,0.00021462911,0.00005871694,0.00013180844,0.00027899147],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008807493,0.00006175458,0.00013067925,0.00015423821,0.0002994727,0.0000391531,0.000121915764,0.00003727653,0.00040253781],"category_scores_gemma":[0.00015791753,0.000035512625,0.000028802959,0.00024082932,0.00029788795,0.0007536897,0.000002627096,0.000045696,0.000013898405],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015399486,0.0000035887974,0.9816545,0.000007751987,0.0000070465453,0.0000044203407,0.00015097465,0.0005997854,0.00011656949,0.0008283993,0.00014629388,0.016465249],"study_design_scores_gemma":[0.00013513833,0.0009177221,0.9902809,0.000042352345,0.000007655829,0.000055463268,0.0003493945,0.00034821546,0.000058120022,0.0018328415,0.005905845,0.00006629532],"about_ca_topic_score_codex":0.0049758963,"about_ca_topic_score_gemma":0.33949387,"teacher_disagreement_score":0.33451796,"about_ca_system_score_codex":0.000003227181,"about_ca_system_score_gemma":0.00018386447,"threshold_uncertainty_score":0.75220996},"labels":[],"label_agreement":null},{"id":"W2916855787","doi":"10.1139/cjes-2018-0067","title":"New constraints on the genesis and geodynamic setting of the Wulong gold deposit, Liaodong Peninsula, northeast China: evidence from geology, geochemistry, fluid inclusions, and C–H–O–S–Pb isotopes","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"China Geological Survey; National Natural Science Foundation of China","keywords":"Geology; Fluid inclusions; Geochemistry; Meteoric water; Quartz; Magmatic water; Pyrite; Mineralization (soil science); Craton; Isotope geochemistry; Overprinting; Mineralogy; Metamorphic rock; Isotope; Hydrothermal circulation; Tectonics; Paleontology","score_opus":0.009310943122804846,"score_gpt":0.18505321530885427,"score_spread":0.17574227218604943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2916855787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9892906,0.004364895,0.0000097544635,0.005405199,0.00012917726,0.000092450566,0.000033499313,0.0000020326013,0.0006724168],"genre_scores_gemma":[0.9989274,0.0001633852,0.0004952974,0.00029073557,0.000060092316,1.4082295e-7,0.0000018622544,0.0000012434361,0.000059836493],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99868774,0.0001176738,0.00032305848,0.0002480357,0.00030235457,0.0003211209],"domain_scores_gemma":[0.9985209,0.000590207,0.00026233136,0.00015594841,0.0000669341,0.00040368325],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000684948,0.00013912006,0.00025337012,0.00007838061,0.00046157316,0.000106270534,0.0006105582,0.00006552932,0.0027672136],"category_scores_gemma":[0.00045070233,0.00006930009,0.00009059564,0.00036727017,0.0009907869,0.00017021789,0.000054274627,0.00023278892,0.00000914349],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000073186925,0.0000017801799,0.99186736,0.0000055764644,0.000017771219,0.000007832563,0.0002240845,0.00063123903,0.0014519822,0.000016986112,0.000032527536,0.0057355496],"study_design_scores_gemma":[0.00008836975,0.00010517893,0.9914596,0.00015875336,0.00003152578,0.000094534946,0.00045234477,0.0056142444,0.0007619003,0.0011006158,0.0000358122,0.0000971371],"about_ca_topic_score_codex":0.18310897,"about_ca_topic_score_gemma":0.32168138,"teacher_disagreement_score":0.13857242,"about_ca_system_score_codex":0.0000019064032,"about_ca_system_score_gemma":0.0004132291,"threshold_uncertainty_score":0.9981444},"labels":[],"label_agreement":null},{"id":"W2917369889","doi":"10.1139/cjes-2018-0289","title":"Continental collisions and the origin of subcrustal continental earthquakes","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Lithosphere; Subduction; Mantle (geology); Continental crust; Oceanic crust; Continental shelf; Crust; Seismology; Seafloor spreading; Plate tectonics; Continental collision; Geophysics; Tectonics; Oceanography","score_opus":0.016578233207938702,"score_gpt":0.21634411420927874,"score_spread":0.19976588100134005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2917369889","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9831357,0.0044493056,0.0000027084964,0.0008819208,0.0006256578,0.00013908594,0.00005012909,0.0000023879575,0.010713099],"genre_scores_gemma":[0.9992411,0.00012027235,0.00016340696,0.00013317564,0.000067809684,1.2781845e-7,0.0000013310754,0.0000015624846,0.00027117977],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988026,0.000082669605,0.00035007513,0.00013285308,0.00031369994,0.0003180739],"domain_scores_gemma":[0.9988735,0.00041455255,0.00024779383,0.0000896611,0.00010704152,0.00026746004],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010447451,0.000106533065,0.0003041069,0.00018957777,0.00034312817,0.000106067855,0.0003061168,0.000033722004,0.0014865301],"category_scores_gemma":[0.00015539222,0.000060349994,0.00010461634,0.00034685148,0.0016279982,0.00028248865,0.000008012341,0.00015139263,0.00003440034],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030799558,0.000002252229,0.9959594,0.0000044665335,0.00002241941,0.00001388764,0.0004413259,0.00013240379,0.000014173014,0.0013584666,0.00008252042,0.001937908],"study_design_scores_gemma":[0.0011026525,0.00035677003,0.9873338,0.000046967332,0.000019264533,0.00016748074,0.002432605,0.00055424345,0.00011219294,0.00026577833,0.0075121373,0.00009611774],"about_ca_topic_score_codex":0.019090638,"about_ca_topic_score_gemma":0.21973568,"teacher_disagreement_score":0.20064504,"about_ca_system_score_codex":7.5354296e-7,"about_ca_system_score_gemma":0.0005668818,"threshold_uncertainty_score":0.99942625},"labels":[],"label_agreement":null},{"id":"W2919918154","doi":"10.1139/cjes-2018-0309","title":"Preservation of carbon isotopes in kerogen from thermally altered Mesoproterozoic lacustrine microbialites","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Lakehead University","funders":"","keywords":"Geology; Kerogen; Mafic; Geochemistry; Sill; Sedimentary rock; Carbonate; Precambrian; Metamorphism; Isotopes of carbon; Igneous rock; Mineralogy; Total organic carbon; Paleontology; Source rock; Chemistry; Environmental chemistry","score_opus":0.016375727623184778,"score_gpt":0.20732762618621378,"score_spread":0.190951898563029,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2919918154","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973976,0.0007225,0.000024566054,0.00024572696,0.00018985858,0.00007820338,0.000008522994,0.0000038581343,0.0013291568],"genre_scores_gemma":[0.99955213,0.000030935622,0.00025043054,0.000031070515,0.0000548666,7.0936727e-7,0.0000022060199,0.0000051285783,0.00007252357],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992043,0.00004100506,0.000343428,0.00007989429,0.00016271966,0.00016864699],"domain_scores_gemma":[0.99956965,0.000026401269,0.00010268315,0.00009420182,0.000066656714,0.00014037735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033721578,0.000072388255,0.00019075516,0.00040343666,0.000022557379,0.00004832686,0.00028103794,0.000040109582,0.00021980282],"category_scores_gemma":[0.00003508902,0.000058835525,0.00005437629,0.00047979673,0.000065183536,0.00031550252,0.0000060903385,0.00010170233,0.0000045760958],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008129666,0.000009037966,0.59767526,0.000028067443,0.00007552441,0.000014011989,0.0016703638,0.27819276,0.12173054,0.000051751947,0.00005052953,0.0004940446],"study_design_scores_gemma":[0.0020291652,0.0004627972,0.49602005,0.00068853464,0.0000740998,0.000019540394,0.0018321546,0.2690742,0.21969953,0.0011571861,0.0082598375,0.00068289146],"about_ca_topic_score_codex":0.010921691,"about_ca_topic_score_gemma":0.121438645,"teacher_disagreement_score":0.11051696,"about_ca_system_score_codex":0.000009039783,"about_ca_system_score_gemma":0.00027596252,"threshold_uncertainty_score":0.99566466},"labels":[],"label_agreement":null},{"id":"W2920515251","doi":"10.1139/cjes-2018-0177","title":"Up, down, or sideways: emplacement of magmatic Fe–Ni–Cu–PGE sulfide melts in large igneous provinces","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Laurentian University","funders":"","keywords":"Geology; Sill; Sulfide; Igneous rock; Lava; Geochemistry; Silicate; Volcano; Basalt; Mineralization (soil science); Dike; Partial melting; Volcanogenic massive sulfide ore deposit; Mineralogy; Chemistry; Materials science; Metallurgy; Pyrite","score_opus":0.01515646230848441,"score_gpt":0.20387718820654305,"score_spread":0.18872072589805863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2920515251","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929665,0.0010272998,0.000005179562,0.0007911361,0.00034216026,0.00013199617,0.000047988393,0.0000029808928,0.004684782],"genre_scores_gemma":[0.99838465,0.000038597675,0.00050450774,0.00028615992,0.000040821036,2.9799293e-7,0.000005037101,0.0000013072615,0.0007385883],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979203,0.00010215182,0.0006333435,0.00023748487,0.0005034946,0.00060326786],"domain_scores_gemma":[0.99863666,0.00023279153,0.00034482966,0.00012747993,0.00012006492,0.0005381446],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013098392,0.00014711404,0.0004222804,0.0004163202,0.00014196361,0.00009255948,0.0006256056,0.000061215316,0.01921643],"category_scores_gemma":[0.00033065965,0.00008591,0.0001155816,0.00091683416,0.00033261973,0.00032385247,0.000012628818,0.0001857727,0.00015025772],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003082486,0.000012789462,0.99577737,0.000024849342,0.000014091719,0.000090313864,0.00024963412,0.0018739518,0.000081771104,0.00006676723,0.00010422887,0.0016734084],"study_design_scores_gemma":[0.00053088856,0.0011129675,0.9869267,0.00015624297,0.00002742671,0.00010980487,0.0019521815,0.00326657,0.00031752564,0.0037904927,0.0015745204,0.0002346764],"about_ca_topic_score_codex":0.09277507,"about_ca_topic_score_gemma":0.90975845,"teacher_disagreement_score":0.8169834,"about_ca_system_score_codex":0.0000040506075,"about_ca_system_score_gemma":0.0010733886,"threshold_uncertainty_score":0.98168015},"labels":[],"label_agreement":null},{"id":"W2920970626","doi":"10.1139/cjes-2018-0198","title":"Geochronology and geochemistry of igneous rocks in the southeastern Lesser Xing’an Range, northeastern China: petrogenesis and implications for the early Mesozoic tectonic evolution","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Petrogenesis; Geochemistry; Diorite; Igneous rock; Geochronology; Partial melting; Crust; Petrology; Zircon; Basalt","score_opus":0.011558198772276975,"score_gpt":0.2001651759783678,"score_spread":0.18860697720609082,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2920970626","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928889,0.0046628057,0.000059211343,0.0019983216,0.00003837723,0.000103148166,0.000037235506,0.0000011688472,0.00021082685],"genre_scores_gemma":[0.9997777,0.000035634504,0.00006850615,0.000055088498,0.000037622664,9.3642205e-7,0.0000022421978,9.112831e-7,0.000021412481],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99920976,0.00005261906,0.0002169961,0.00015606079,0.00011178246,0.00025277244],"domain_scores_gemma":[0.9993095,0.00021628382,0.00014508347,0.00011146718,0.000065179855,0.00015250164],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00059006206,0.000080398284,0.00016185605,0.00010207141,0.0002403256,0.000062419305,0.0003729973,0.000045314286,0.00023400714],"category_scores_gemma":[0.00006367951,0.000041140076,0.00005558775,0.00025805217,0.00042620723,0.000120031415,0.0000068098902,0.000109639426,0.0000024508508],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008283577,0.0000035359635,0.9959089,0.0000065083127,0.00000894552,0.0000011349118,0.00025587715,0.00093412725,0.00012737208,0.00003665403,8.7924303e-7,0.0027077545],"study_design_scores_gemma":[0.0001418923,0.00023896371,0.992516,0.00001209371,0.000027202339,0.00011084277,0.00077364634,0.002458625,0.000037523827,0.003574682,0.00005137838,0.000057154375],"about_ca_topic_score_codex":0.03715745,"about_ca_topic_score_gemma":0.42914605,"teacher_disagreement_score":0.3919886,"about_ca_system_score_codex":9.695924e-7,"about_ca_system_score_gemma":0.00019132919,"threshold_uncertainty_score":0.9692542},"labels":[],"label_agreement":null},{"id":"W2921825641","doi":"10.1139/cjes-2018-0023","title":"Revised stratigraphy of the middle Simcoe Group (Ordovician, upper Sandbian–Katian) in its type area: an integrated approach","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Geographic Society","keywords":"Paleontology; Geology; Unconformity; Ordovician; Chemostratigraphy; Sequence (biology); Global Boundary Stratotype Section and Point; Conodont; Group (periodic table); Biostratigraphy; Stratigraphic unit; Trilobite; Sequence stratigraphy; Diachronous; Radiometric dating; Facies; Isotopes of carbon; Tectonics; Structural basin","score_opus":0.03945428841194634,"score_gpt":0.21757335958402674,"score_spread":0.1781190711720804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2921825641","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95632684,0.006025524,0.0000074377253,0.00013822906,0.0004957774,0.00016779455,0.00003355223,0.0000024659016,0.03680237],"genre_scores_gemma":[0.99892294,0.00003425977,0.00085990864,0.000108686676,0.00003124558,1.697657e-7,0.0000028128106,8.976089e-7,0.00003905694],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99841064,0.00022908015,0.00044471526,0.0002096613,0.0003012822,0.00040459484],"domain_scores_gemma":[0.9989455,0.00008921284,0.00030026544,0.00017347267,0.0001294351,0.00036215244],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010405568,0.00014170671,0.00029634958,0.00045810538,0.000219732,0.00008894017,0.0007904418,0.00010421295,0.0006020214],"category_scores_gemma":[0.00010315099,0.00008768247,0.00012296371,0.0014582209,0.0005808269,0.00062909845,0.0000011334106,0.00033159836,0.0000053986723],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016999133,0.000011119874,0.99390656,0.0000121460325,0.000011561166,0.000008833245,0.00049246114,0.0007072307,0.000053899348,0.00036405,0.000019774603,0.004395347],"study_design_scores_gemma":[0.00022032823,0.00048921513,0.9949758,0.00012709369,0.00000913623,0.000040503317,0.0015165986,0.001726087,0.0000420237,0.00035162873,0.00038607037,0.00011548845],"about_ca_topic_score_codex":0.010108223,"about_ca_topic_score_gemma":0.67006004,"teacher_disagreement_score":0.6599518,"about_ca_system_score_codex":0.0000013601119,"about_ca_system_score_gemma":0.0012160176,"threshold_uncertainty_score":0.99648356},"labels":[],"label_agreement":null},{"id":"W2921908685","doi":"10.1139/cjes-2018-0171","title":"Paleoproterozoic Iron Oxide Apatite (IOA) and Iron Oxide-Copper-Gold (IOCG) mineralization in the East Arm Basin, Northwest Territories, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Iron oxide copper gold ore deposits; Geology; Geochemistry; Mineralization (soil science); Uraninite; Craton; Skarn; Hydrothermal circulation; Paleontology; Uranium; Fluid inclusions","score_opus":0.009121209890608278,"score_gpt":0.16808584974576948,"score_spread":0.1589646398551612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2921908685","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99497724,0.00074663013,0.0000012446495,0.002748515,0.00023896225,0.000103254075,0.000059320395,0.0000018545581,0.0011229684],"genre_scores_gemma":[0.9984619,0.000031130505,0.00016990706,0.0011056982,0.00008996357,4.0959546e-7,0.000026959618,0.0000013560525,0.00011264442],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984211,0.00010682531,0.00035443762,0.00022714464,0.00045442773,0.00043607972],"domain_scores_gemma":[0.99909157,0.000109185276,0.00017942782,0.00011579039,0.00007587228,0.00042813312],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006285294,0.00014396672,0.00022903811,0.00017424051,0.0001989173,0.00018559801,0.00046833296,0.000052214076,0.00088121725],"category_scores_gemma":[0.00012031175,0.00008561226,0.000050788483,0.0006544478,0.00029774732,0.00031727005,0.000006674152,0.00020505983,0.000010031976],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000048331376,0.0000040783616,0.9963117,0.00000890703,0.0000031364534,0.000042615546,0.00013191433,0.0026165647,0.000043358683,0.000028234625,0.00011582191,0.00068878714],"study_design_scores_gemma":[0.0001386232,0.00016374898,0.99258745,0.00003691031,0.00001137842,0.00006627496,0.0005869619,0.00086045027,0.000028607947,0.0002762269,0.005110887,0.00013247371],"about_ca_topic_score_codex":0.9769165,"about_ca_topic_score_gemma":0.9997822,"teacher_disagreement_score":0.022865696,"about_ca_system_score_codex":0.0000057269062,"about_ca_system_score_gemma":0.0007718459,"threshold_uncertainty_score":0.96487105},"labels":[],"label_agreement":null},{"id":"W2922265995","doi":"10.1139/cjes-2018-0141","title":"Distinct sulfur saturation histories within the Palaeogene Magilligan Sill, Northern Ireland: implications for Ni – Cu – platinum group element mineralisation in the North Atlantic Igneous Province","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"University of Exeter; Natural Environment Research Council; Sight Research UK","keywords":"Sill; Geology; Geochemistry; Pyrrhotite; Gabbro; Mafic; Igneous rock; Olivine; Pentlandite; Large igneous province; Layered intrusion; Pyrite; Paleontology; Magmatism","score_opus":0.013868626393063981,"score_gpt":0.19050973893141848,"score_spread":0.1766411125383545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2922265995","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99082494,0.0003430033,0.000024641438,0.007980682,0.00019580401,0.00026416418,0.000055316697,0.0000025453255,0.0003088997],"genre_scores_gemma":[0.99911946,0.0000052884184,0.00023429352,0.00037625618,0.000105484374,0.0000022283102,0.00007515684,0.0000012262021,0.00008060665],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885225,0.000087507295,0.00037319944,0.00017483973,0.000235793,0.00027641858],"domain_scores_gemma":[0.9990717,0.00025477976,0.00029923982,0.00012277669,0.00010938096,0.00014211822],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008070842,0.00010500836,0.0001476034,0.000094708856,0.0004421272,0.00014597492,0.0004778464,0.00002985436,0.00019997978],"category_scores_gemma":[0.00018570526,0.00004972323,0.00007429325,0.00044497292,0.0002831187,0.00019192061,0.000004027985,0.00012882845,0.000010758125],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007544773,0.0000047873227,0.99448824,0.0000042747697,0.000005973671,0.0000032664184,0.00044198206,0.0039248606,0.00006574248,0.00030210093,0.00004437764,0.0007068271],"study_design_scores_gemma":[0.00010722955,0.0002424182,0.9927722,0.000008997113,0.000019398818,0.00003266766,0.00044661475,0.0017002408,0.000007801228,0.003281791,0.0012927469,0.00008789075],"about_ca_topic_score_codex":0.052543808,"about_ca_topic_score_gemma":0.97902477,"teacher_disagreement_score":0.926481,"about_ca_system_score_codex":0.000006330982,"about_ca_system_score_gemma":0.00035548166,"threshold_uncertainty_score":0.9537654},"labels":[],"label_agreement":null},{"id":"W2923621790","doi":"10.1139/cjes-2018-0315","title":"A new approach to the opening of the eastern Mediterranean Sea and the origin of the Hellenic subduction zone. Part 2: The Hellenic subduction zone","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Subduction; Lithosphere; Seismology; Accretionary wedge; Transform fault; Trough (economics); Paleontology; Fault (geology); Tectonics","score_opus":0.03807487843882709,"score_gpt":0.2164341174955975,"score_spread":0.1783592390567704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2923621790","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9782048,0.0046046567,0.000055839308,0.011522241,0.0022321162,0.00045152282,0.000014863836,0.0000021827364,0.0029117616],"genre_scores_gemma":[0.99732894,0.00018278771,0.00008534183,0.0003099929,0.0003762862,8.2208976e-7,4.7469513e-7,0.0000029494788,0.0017124158],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99803996,0.00037402063,0.00040088216,0.0002040156,0.00062428816,0.00035681893],"domain_scores_gemma":[0.99861705,0.00031490662,0.00041271417,0.00035975777,0.00010716104,0.0001884317],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027478784,0.0001415953,0.00025610594,0.000102148,0.0009953665,0.0001457583,0.0011551452,0.000040618354,0.00038368924],"category_scores_gemma":[0.00016254428,0.000050077473,0.00015665745,0.00087031996,0.0011793787,0.00025971417,0.00003789473,0.00032163726,0.000021112148],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014480371,0.0000124421385,0.9073006,0.000038748047,0.00018618847,0.000002487672,0.021217268,0.018036595,0.000047151858,0.000825979,0.0036834665,0.048504256],"study_design_scores_gemma":[0.0013748737,0.00052798196,0.88774735,0.00034661658,0.00018611817,0.0006465522,0.022014812,0.009381136,0.0004225165,0.0006016153,0.076448165,0.00030224037],"about_ca_topic_score_codex":0.039214335,"about_ca_topic_score_gemma":0.29445708,"teacher_disagreement_score":0.25524274,"about_ca_system_score_codex":0.0000034027405,"about_ca_system_score_gemma":0.00091035,"threshold_uncertainty_score":0.9671836},"labels":[],"label_agreement":null},{"id":"W2924090640","doi":"10.1139/cjes-2018-0118","title":"Research on the fracture structure and activity of the Qinling Mountains thrust nappe system in western Hubei","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Nappe; Outcrop; Fault (geology); Active fault; Quaternary; Pleistocene; Thrust fault; Paleontology; Tectonics","score_opus":0.04078378779502766,"score_gpt":0.2678025888430302,"score_spread":0.22701880104800254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2924090640","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937231,0.0010259395,5.4474793e-7,0.0014438687,0.00031442294,0.00013426453,0.000022858738,0.0000011280148,0.003333866],"genre_scores_gemma":[0.9996894,0.000023055065,0.0000113864435,0.00015354852,0.00006207028,9.211518e-8,1.3847155e-7,0.0000013565887,0.000058958994],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99862325,0.00022391808,0.00017784527,0.00014097807,0.00049317343,0.00034081994],"domain_scores_gemma":[0.998961,0.0005234408,0.00014718038,0.00014772918,0.0000865261,0.00013416968],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016998126,0.00008403068,0.00017352143,0.00022739201,0.00050301995,0.00011458773,0.0004882672,0.000052447336,0.0002788779],"category_scores_gemma":[0.000104631166,0.000038936272,0.000041722415,0.0006287698,0.00060085196,0.00018848543,0.000011755805,0.00052618457,0.000007444092],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007257261,0.0000012363705,0.99368966,0.000012982841,0.000008013232,0.000008232391,0.00068963075,0.0038600382,0.000017801738,0.00018767813,0.000017128395,0.001500345],"study_design_scores_gemma":[0.00009542582,0.00018711576,0.99420244,0.00019337791,0.0000030001258,0.000036992365,0.0034266207,0.00046298612,0.00026928596,0.00013272223,0.0009405763,0.000049485767],"about_ca_topic_score_codex":0.02172542,"about_ca_topic_score_gemma":0.49808386,"teacher_disagreement_score":0.47635844,"about_ca_system_score_codex":0.0000043840946,"about_ca_system_score_gemma":0.0007418038,"threshold_uncertainty_score":0.984789},"labels":[],"label_agreement":null},{"id":"W2924333267","doi":"10.1139/cjes-2018-0329","title":"Analysis of geological hiatus surfaces across Africa in the Cenozoic and implications for the timescales of convectively-maintained topography","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Hiatus; Cenozoic; Pleistocene; Elevation (ballistics); Paleontology; Geologic map; Geologic time scale; Mantle (geology); Period (music); Sedimentary rock; Structural basin","score_opus":0.02036863292089754,"score_gpt":0.22879278536166128,"score_spread":0.20842415244076373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2924333267","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938591,0.0023749904,0.000026043423,0.002982492,0.00003554021,0.00010374476,0.000102123966,7.3230655e-7,0.00051523757],"genre_scores_gemma":[0.99960375,0.000058175145,0.00020922114,0.00009802204,0.000009586439,4.3495933e-7,0.000003446816,3.6807486e-7,0.000016992384],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999067,0.00008167946,0.00030467886,0.00013082373,0.00015007635,0.00026570534],"domain_scores_gemma":[0.9981897,0.001232516,0.00022255444,0.00009728475,0.00013141525,0.00012654209],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013058925,0.00006921737,0.00027573554,0.00021557178,0.00019126377,0.000040771225,0.00048442316,0.000037834154,0.0005646289],"category_scores_gemma":[0.00020015899,0.000030810017,0.00018230938,0.0017546589,0.0010482451,0.000085844054,0.0000068178533,0.00009377439,0.0000010268719],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008745886,0.000005737898,0.99215364,0.0000028446057,0.00007491894,5.481011e-7,0.00038528265,0.0058666756,0.000030929248,0.0005234782,0.000008792944,0.00093841716],"study_design_scores_gemma":[0.00008608959,0.00023188068,0.98878515,0.000004614304,0.000108484266,0.000005518856,0.0016403564,0.003459664,0.000016850949,0.0052045155,0.0004123139,0.000044539316],"about_ca_topic_score_codex":0.0123772845,"about_ca_topic_score_gemma":0.27805385,"teacher_disagreement_score":0.2656766,"about_ca_system_score_codex":6.304691e-7,"about_ca_system_score_gemma":0.00015093306,"threshold_uncertainty_score":0.9941994},"labels":[],"label_agreement":null},{"id":"W2924451021","doi":"10.1139/cjes-2018-0253","title":"Further detrital zircon evidence for peri-Gondwanan blocks in the central Appalachian Piedmont Province, USA","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Zircon; Laurentia; Geology; Gondwana; Terrane; Geochemistry; Provenance; Schist; Paleontology; Metamorphic rock; Ordovician; Structural basin; Tectonics","score_opus":0.027087611580813135,"score_gpt":0.21586855678133812,"score_spread":0.188780945200525,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2924451021","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916184,0.0014195461,0.00003799702,0.0030715214,0.0002670188,0.00020247782,0.000019395164,0.0000017007602,0.0033619436],"genre_scores_gemma":[0.99821043,0.000016870952,0.0008267896,0.00060219824,0.00013003143,5.5568586e-7,0.0000022241047,0.0000010449202,0.00020982896],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983914,0.00008237869,0.0003249257,0.00022358702,0.00035153318,0.0006261857],"domain_scores_gemma":[0.99887455,0.00035965518,0.00015507423,0.00011434968,0.00007279355,0.00042360902],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012099893,0.00012030259,0.00021708399,0.00021871206,0.00022307484,0.00020047183,0.0008144668,0.000052695585,0.0043720226],"category_scores_gemma":[0.00029806446,0.0000653044,0.00015674622,0.0006087946,0.00037846118,0.00038767085,0.0000050671133,0.00020402916,0.00005173941],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013573756,0.000005596811,0.9940841,0.000005623618,0.0000060568436,0.000024928304,0.00029299816,0.0016125407,0.00012004493,0.00007319812,0.00005840384,0.0037029437],"study_design_scores_gemma":[0.00017995694,0.0005945859,0.9892307,0.000055312204,0.00001703651,0.000059768394,0.0010299648,0.0015592691,0.00015787735,0.0018420029,0.005130369,0.00014314975],"about_ca_topic_score_codex":0.032554634,"about_ca_topic_score_gemma":0.7867231,"teacher_disagreement_score":0.75416845,"about_ca_system_score_codex":0.0000029594448,"about_ca_system_score_gemma":0.0008585036,"threshold_uncertainty_score":0.9965381},"labels":[],"label_agreement":null},{"id":"W2925656992","doi":"10.1139/cjes-2018-0157","title":"The theory of undercurrent from the Austrian alpine geologist Otto Ampferer (1875–1947): first conceptual ideas on the way to plate tectonics","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Plate tectonics; Seafloor spreading; Tectonics; Geologist; Crust; Continental drift; Paleontology; Geophysics","score_opus":0.03173894996924441,"score_gpt":0.20623214774391554,"score_spread":0.17449319777467115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2925656992","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97820294,0.0016230431,0.000016650414,0.014652961,0.00048436318,0.00014994269,0.00007602567,0.0000027422923,0.0047913203],"genre_scores_gemma":[0.9985626,0.00006967314,0.000052504885,0.0010263186,0.00009578047,4.494607e-7,0.0000035488001,0.0000013094296,0.00018785888],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981897,0.0002708216,0.00039227973,0.00021205825,0.000460188,0.00047498025],"domain_scores_gemma":[0.99602723,0.0029290533,0.000257609,0.00025489993,0.00011816862,0.00041301403],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0020965547,0.00014775858,0.00023973313,0.00006915119,0.0007993742,0.00015958035,0.0012932067,0.000056517612,0.009205805],"category_scores_gemma":[0.0012016264,0.000054154476,0.00016352367,0.0005907184,0.0017755228,0.0000897599,0.000018767701,0.00035573874,0.0002279735],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008433735,0.000010937118,0.9417213,0.0000020880234,0.00010119725,0.000015657843,0.00080950273,0.023062758,0.000024946034,0.025845846,0.0010211548,0.007300257],"study_design_scores_gemma":[0.00022769452,0.0007125688,0.8918779,0.00006815276,0.000042734064,0.000014083724,0.004765115,0.0006213621,0.0002792095,0.052007373,0.04920158,0.00018223526],"about_ca_topic_score_codex":0.029334176,"about_ca_topic_score_gemma":0.5595204,"teacher_disagreement_score":0.53018624,"about_ca_system_score_codex":0.000003345446,"about_ca_system_score_gemma":0.00039199652,"threshold_uncertainty_score":0.99169993},"labels":[],"label_agreement":null},{"id":"W2935865199","doi":"10.1139/cjes-2018-0306","title":"Quaternary evolution of the Suluova Basin: implications on tectonics and palaeonvironments of the Central North Anatolian Shear Zone","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Structural basin; Quaternary; Sinistral and dextral; Paleontology; Transtension; Pull apart basin; Graben; Shear zone; Tectonics; Early Pleistocene; Fault (geology); Geomorphology; Pleistocene; Sedimentary basin","score_opus":0.01215424588129474,"score_gpt":0.18797478377612498,"score_spread":0.17582053789483024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2935865199","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957878,0.0009250859,0.0000037828236,0.0012020643,0.00039418502,0.00011411517,0.000063347536,9.104176e-7,0.001508722],"genre_scores_gemma":[0.9996664,0.00008281491,0.000059694954,0.00009533637,0.000022628168,8.8826454e-8,4.3390415e-7,0.0000012871673,0.00007133664],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990203,0.0000685041,0.00025041396,0.000116081916,0.0002854491,0.000259263],"domain_scores_gemma":[0.9992881,0.00007685892,0.00026255252,0.00017274897,0.000043654243,0.00015608972],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002841767,0.0000778116,0.00014824672,0.00010181826,0.00031487245,0.00002317908,0.00040989975,0.000027548676,0.00021075575],"category_scores_gemma":[0.0000507723,0.0000418033,0.00007876929,0.0004128433,0.00066083873,0.00013271166,0.0000113448195,0.00012850971,0.000005948708],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003472698,0.0000027872914,0.9958015,0.0000048551155,0.000011171639,7.1307835e-7,0.0001768263,0.0014433117,0.000016783186,0.00015355166,0.000021515074,0.0023635065],"study_design_scores_gemma":[0.00012335967,0.00018368542,0.9978678,0.000052850904,0.0000113801725,0.000028427809,0.00026461142,0.00028428758,0.00014237747,0.00017315228,0.00081878883,0.000049265527],"about_ca_topic_score_codex":0.017550388,"about_ca_topic_score_gemma":0.21384145,"teacher_disagreement_score":0.19629106,"about_ca_system_score_codex":0.0000048586867,"about_ca_system_score_gemma":0.00061790587,"threshold_uncertainty_score":0.98899186},"labels":[],"label_agreement":null},{"id":"W2936120123","doi":"10.1139/cjes-2018-0277","title":"Multichannel systems in an ancient river-dominated delta: case study of the lower Yanchang Formation, southwest Ordos Basin, China","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Sedimentology; Facies; Delta; Sinuosity; Fluvial; Structural basin; Channel (broadcasting); Geomorphology; Mouth bar; Geochemistry; Paleontology; Petrology; Sedimentary structures","score_opus":0.021797916868944042,"score_gpt":0.21813607877210686,"score_spread":0.19633816190316283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2936120123","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99824136,0.0003635345,0.000013810616,0.000078870915,0.0007857274,0.0002804951,0.00003660108,0.0000019154286,0.00019770593],"genre_scores_gemma":[0.9998342,0.0000034171285,0.00006174064,0.000054280703,0.000025410054,4.250912e-7,0.0000015854272,0.0000010139283,0.000017932025],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987534,0.00013831462,0.000421169,0.00011427614,0.00028494786,0.00028784704],"domain_scores_gemma":[0.9990332,0.00006099588,0.0003055951,0.000119022414,0.00022276747,0.00025839498],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010476601,0.00009062027,0.00018420473,0.0003178672,0.00035186153,0.0001267681,0.00040880963,0.000037569233,0.00029999285],"category_scores_gemma":[0.000097901466,0.000051637395,0.000036747828,0.00090977695,0.00020471368,0.0009851226,0.0000067392466,0.00013464408,0.0000138664855],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000059694803,0.000029620252,0.92602223,0.000013665697,0.0000029724788,0.00011206456,0.005889545,0.0674136,0.0000030633594,0.000009061794,0.000008083738,0.0004901473],"study_design_scores_gemma":[0.00038624657,0.0011868549,0.93771625,0.00006423888,0.0000078942785,0.00075490307,0.030958856,0.028610721,0.000012917456,0.00003798941,0.00017242605,0.00009070149],"about_ca_topic_score_codex":0.12201288,"about_ca_topic_score_gemma":0.719652,"teacher_disagreement_score":0.59763914,"about_ca_system_score_codex":0.000002958252,"about_ca_system_score_gemma":0.0004372384,"threshold_uncertainty_score":0.8838337},"labels":[],"label_agreement":null},{"id":"W2936308053","doi":"10.1139/cjes-2018-0262","title":"The northern termination of the Cache Creek terrane in Yukon: Middle Triassic arc activity and Jurassic–Cretaceous structural imbrication","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon University; Geological Survey of Canada; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Simon Fraser University","keywords":"Geology; Terrane; Imbrication; Geochemistry; Back-arc basin; Cretaceous; Ultramafic rock; Paleontology; Petrology; Subduction; Tectonics","score_opus":0.01742592887399728,"score_gpt":0.1955516309640684,"score_spread":0.17812570209007114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2936308053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996118,0.0006853637,0.0000011817534,0.0021415094,0.00014730328,0.00007147461,0.00000787939,7.8476415e-7,0.0008264984],"genre_scores_gemma":[0.9997221,0.000016638844,0.000042562726,0.000043337495,0.000026738257,1.2225253e-7,7.5987356e-7,5.2584005e-7,0.00014719598],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991239,0.000108662476,0.00021415639,0.00011238561,0.00023653502,0.00020441719],"domain_scores_gemma":[0.99924105,0.00021621375,0.00024428533,0.00008720316,0.00006787115,0.00014337132],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006265115,0.00006296574,0.00014023708,0.00007561497,0.0002557919,0.00009149078,0.00034276806,0.00003208732,0.0003539159],"category_scores_gemma":[0.00018702596,0.000030384495,0.000063365456,0.00044477393,0.00048540166,0.00019043824,0.000006578856,0.00014964724,0.0000038192534],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000073693927,0.0000013451329,0.9707818,0.0000028263557,0.0000042566544,0.0000020164457,0.00012817315,0.0007473413,0.0002202235,0.000006116934,0.0000022900847,0.028096255],"study_design_scores_gemma":[0.00011175851,0.00010393668,0.99139744,0.000015960713,0.000008574507,0.000027575792,0.00023561518,0.005843071,0.00022313163,0.0018321944,0.00015397336,0.000046764322],"about_ca_topic_score_codex":0.033513915,"about_ca_topic_score_gemma":0.84343565,"teacher_disagreement_score":0.80992174,"about_ca_system_score_codex":0.000002382675,"about_ca_system_score_gemma":0.00028086692,"threshold_uncertainty_score":0.972922},"labels":[],"label_agreement":null},{"id":"W2937441154","doi":"10.1139/cjes-2019-0009","title":"Geophysical inversion contributions to mineral exploration: lessons from the Footprints project","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Memorial University of Newfoundland; University of British Columbia; Polytechnique Montréal; Western University; University of Saskatchewan; TechnoRem (Canada); Laurentian University; McMaster University","funders":"","keywords":"Geology; Petrophysics; Inversion (geology); Geophysics; Mineral exploration; Mineral resource classification; Mineralogy; Geochemistry; Seismology; Porosity","score_opus":0.04403699384400893,"score_gpt":0.2820776530539482,"score_spread":0.23804065920993928,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2937441154","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97977626,0.00013643244,0.00022423737,0.016989863,0.00073362637,0.00015856918,0.00009844365,0.000003670537,0.0018788985],"genre_scores_gemma":[0.9970201,0.0000044949225,0.0013406987,0.001012385,0.00038331898,3.6682388e-7,0.0000045809184,0.000001060534,0.00023298727],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987927,0.00016330884,0.0001973193,0.00016885612,0.0003165482,0.00036124565],"domain_scores_gemma":[0.9986691,0.00049624545,0.000093491195,0.00010858682,0.00015351463,0.00047906808],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005327513,0.000088466215,0.00016554035,0.00011776614,0.00038894996,0.00017161091,0.0004802231,0.00003539861,0.00069121],"category_scores_gemma":[0.00048466955,0.00005068928,0.00008771944,0.00089172507,0.00017952148,0.0003577721,0.000007798146,0.00020344662,0.00042105798],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000086847635,0.000038210135,0.79580665,0.000006012429,0.00006030264,0.000064786705,0.0020115897,0.009481554,0.0010304264,0.005520667,0.009915114,0.17597787],"study_design_scores_gemma":[0.00015197042,0.00062040566,0.95207727,0.000033999404,0.0000117203035,0.000008449294,0.00036438604,0.0021474937,0.00024350965,0.0067296284,0.03748877,0.0001223784],"about_ca_topic_score_codex":0.048347265,"about_ca_topic_score_gemma":0.12870266,"teacher_disagreement_score":0.17585549,"about_ca_system_score_codex":0.0000027437222,"about_ca_system_score_gemma":0.0010718673,"threshold_uncertainty_score":0.9579899},"labels":[],"label_agreement":null},{"id":"W2937787567","doi":"10.1139/cjes-2018-0307","title":"A mid-Cretaceous alkaline volcano in the Davis Strait","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Nationale Geologiske Undersøgelser for Danmark og Grønland","keywords":"Geology; Zircon; Basalt; Geochemistry; Volcano; Volcanic rock; Andesite","score_opus":0.015618086683291742,"score_gpt":0.19850583525199444,"score_spread":0.1828877485687027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2937787567","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9827368,0.0009665103,0.0000021260703,0.0024610786,0.00017954923,0.000050737573,0.000016899205,0.0000014517213,0.013584836],"genre_scores_gemma":[0.9984442,0.00001655956,0.0002364569,0.0009849332,0.000072696756,7.568356e-8,0.0000033345202,5.536537e-7,0.00024119676],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987993,0.00008539607,0.0002663849,0.00014272427,0.000326234,0.0003799168],"domain_scores_gemma":[0.99925476,0.0001623257,0.000115594376,0.00009302608,0.000055905504,0.00031841287],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010473895,0.0000785955,0.00017742302,0.00017246546,0.0001479802,0.00017744242,0.00069405674,0.000037541875,0.02137301],"category_scores_gemma":[0.00013065193,0.000043877822,0.000098777695,0.00080858724,0.00031274484,0.00019864863,0.0000033502085,0.00020826695,0.00022803468],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000027678334,0.000003301453,0.9946001,0.000001997279,0.000005011075,0.00008037184,0.00013838333,0.0026482528,0.00004914605,0.00003369263,0.000109485,0.0023274885],"study_design_scores_gemma":[0.00014106561,0.0003072638,0.9721607,0.000018309187,0.000010696489,0.00014159786,0.00071793544,0.0011785192,0.00004261332,0.0055167973,0.019662386,0.000102124926],"about_ca_topic_score_codex":0.08170004,"about_ca_topic_score_gemma":0.8581028,"teacher_disagreement_score":0.7764028,"about_ca_system_score_codex":8.598191e-7,"about_ca_system_score_gemma":0.00042827052,"threshold_uncertainty_score":0.9795216},"labels":[],"label_agreement":null},{"id":"W2938190979","doi":"10.1139/cjes-2018-0308","title":"Spatio-temporal behaviour of continental transform faults: implications from the late Quaternary slip history of the North Anatolian Fault, Turkey","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"North Anatolian Fault; Geology; Quaternary; Seismology; Slip (aerodynamics); Geodetic datum; Shear (geology); Shear zone; Fault (geology); Tectonics; Geodesy; Paleontology","score_opus":0.019209395409923533,"score_gpt":0.20616830059460775,"score_spread":0.18695890518468422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2938190979","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99173206,0.0025467528,0.000002080844,0.0015383532,0.00084844814,0.00015003116,0.0003662852,0.0000022425345,0.0028137588],"genre_scores_gemma":[0.9992861,0.000053679913,0.0000638008,0.00016033794,0.00004946197,2.6498077e-7,0.000011188981,0.0000021131816,0.00037301777],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987846,0.00006890493,0.0004369947,0.00012357043,0.0003262315,0.00025967273],"domain_scores_gemma":[0.99893683,0.00014614213,0.00042277455,0.00018598154,0.0001278876,0.00018040292],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037816443,0.000109000925,0.00023102714,0.00010708888,0.0002110473,0.00002159657,0.00073586416,0.00003641898,0.0009244934],"category_scores_gemma":[0.000039675735,0.000059437483,0.00015920123,0.00030087036,0.0007390345,0.00025445202,0.000006786299,0.00017934194,0.00001294828],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000072335292,0.000003296166,0.99610245,0.0000032338514,0.000021174235,0.000002598527,0.0015048839,0.00043472552,0.000009485747,0.000027936232,0.00027846172,0.0016045371],"study_design_scores_gemma":[0.00020422334,0.00014794982,0.9921925,0.000049806495,0.000024980369,0.000016699498,0.00090753374,0.00022115532,0.00006209391,0.00014169954,0.0059548533,0.00007647535],"about_ca_topic_score_codex":0.21556297,"about_ca_topic_score_gemma":0.8132645,"teacher_disagreement_score":0.59770155,"about_ca_system_score_codex":0.0000066154435,"about_ca_system_score_gemma":0.0014303342,"threshold_uncertainty_score":0.9999888},"labels":[],"label_agreement":null},{"id":"W2941001062","doi":"10.1139/cjes-2018-0216","title":"West Asian climate during the last millennium according to the EC-Earth model","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Supercomputer Centre, Linköpings Universitet; European Centre for Medium-Range Weather Forecasts; Vetenskapsrådet; National Science Council","keywords":"Precipitation; Climatology; Climate change; Sea surface temperature; Forcing (mathematics); Climate model; Environmental science; Geology; Geography; Oceanography; Meteorology","score_opus":0.02046961338317733,"score_gpt":0.23011963097175298,"score_spread":0.20965001758857565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2941001062","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9723805,0.0008405052,0.000007901425,0.008635843,0.0007808063,0.00015831266,0.000022376584,0.0000040081786,0.017169705],"genre_scores_gemma":[0.9984678,0.00007636492,0.00022941231,0.0007033314,0.00013074599,4.2732088e-7,0.000001118677,0.0000023228233,0.00038848733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981488,0.00017100874,0.0002722344,0.00020555168,0.00033531376,0.00086711976],"domain_scores_gemma":[0.998816,0.00020651286,0.00012778748,0.00021276086,0.0000954995,0.00054141355],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0019936024,0.00012243992,0.0001904281,0.00030247425,0.0015052023,0.00023080263,0.0011660472,0.00006679799,0.0013964084],"category_scores_gemma":[0.0001236813,0.00006382068,0.00008545781,0.0005994365,0.0005879319,0.00034486994,0.000021813597,0.0004567671,0.0010541454],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010814591,0.0000011010208,0.95992386,0.0000054162106,0.000007885522,0.0000311934,0.0004571024,0.03915015,0.000009063783,0.00010147464,0.000071279224,0.0002306738],"study_design_scores_gemma":[0.00012677995,0.00016373074,0.9867917,0.000032526983,0.0000063252905,0.00048017997,0.0023053645,0.0060756966,0.000033816836,0.00008251156,0.0037993968,0.00010202502],"about_ca_topic_score_codex":0.0015228259,"about_ca_topic_score_gemma":0.62332064,"teacher_disagreement_score":0.6217978,"about_ca_system_score_codex":6.706613e-7,"about_ca_system_score_gemma":0.00094277685,"threshold_uncertainty_score":0.9997947},"labels":[],"label_agreement":null},{"id":"W2941193009","doi":"10.1139/cjes-2018-0166","title":"Three-dimensional stochastic assimilation of gravity data in Lalor volcanogenic massive sulphide, Manitoba, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Soil Geostatistics and Mapping","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval; Institut National de la Recherche Scientifique","funders":"Fonds de recherche du Québec – Nature et technologies","keywords":"Geology; Grid; Geophysics; Gravity anomaly; Data assimilation; Workflow; Stochastic modelling; Geodesy; Computer science; Meteorology","score_opus":0.02733578637684127,"score_gpt":0.22219429095225898,"score_spread":0.1948585045754177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2941193009","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981881,0.00007366947,0.00030049213,0.00031699988,0.0005209874,0.00009408025,0.00010429248,6.5418016e-7,0.00040074027],"genre_scores_gemma":[0.99869967,9.630891e-7,0.0011281288,0.000111549576,0.000024379979,2.6875915e-7,0.0000057086827,0.0000030786605,0.000026251999],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873275,0.000024659555,0.0003015501,0.00018289927,0.00048005272,0.00027808492],"domain_scores_gemma":[0.9991412,0.00011574617,0.00025366765,0.00018027927,0.000037526068,0.00027156185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006626494,0.00007746139,0.0001531163,0.000124645,0.00010150206,0.000028307559,0.00054295996,0.00002542238,0.0006255891],"category_scores_gemma":[0.00020665144,0.00006779469,0.000019118295,0.0003784175,0.0002518123,0.0002902658,0.00006212942,0.00011837488,0.000013212629],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004968011,0.0000061665532,0.93662304,0.00000449913,0.0000066210946,0.00004083415,0.000058630132,0.060056813,0.00032639902,0.00013804488,0.0012959574,0.001438027],"study_design_scores_gemma":[0.00018117588,0.00006790086,0.97434646,0.00004917818,0.0000068989248,0.000021720236,0.0001618203,0.023662861,0.00003241284,0.00080643845,0.0005701561,0.00009298042],"about_ca_topic_score_codex":0.8976124,"about_ca_topic_score_gemma":0.99933994,"teacher_disagreement_score":0.10172757,"about_ca_system_score_codex":0.000059251888,"about_ca_system_score_gemma":0.002252385,"threshold_uncertainty_score":0.6849762},"labels":[],"label_agreement":null},{"id":"W2945075984","doi":"10.1139/cjes-2018-0251","title":"Geochemistry, zircon geochronology, and isotopic systematics of the Zhanbuzhale granites in the East Kunlun, Qinghai Province, northwestern China: implications for the tectonic setting","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Chinese Academy of Geological Sciences","keywords":"Zircon; Geology; Geochemistry; Geochronology; Subduction; Petrography; Feldspar; Alkali feldspar; Isotope geochemistry; Petrology; Tectonics; Isotope; Paleontology; Quartz","score_opus":0.011417041687665497,"score_gpt":0.1956396796650427,"score_spread":0.1842226379773772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2945075984","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911274,0.0015451378,0.000024548768,0.0062129945,0.000083014325,0.00025350513,0.00004137326,0.0000011973631,0.0007108448],"genre_scores_gemma":[0.99959296,0.000013570789,0.00013996809,0.00016326722,0.00004061945,0.0000015227728,0.0000020892187,7.740815e-7,0.000045199526],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910533,0.00006535674,0.00030489228,0.0001275786,0.0001379277,0.00025888698],"domain_scores_gemma":[0.99898267,0.00042787887,0.0002721349,0.00015934886,0.000070479546,0.000087476765],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00089912786,0.00008208357,0.00016877457,0.00006455684,0.00036079955,0.00006979058,0.0007188297,0.000039057984,0.0001654268],"category_scores_gemma":[0.00017148576,0.000034269025,0.00008768396,0.00037386184,0.00055342074,0.00009603372,0.000012120201,0.00015920405,0.0000023662192],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000012858158,0.0000030386484,0.99764794,0.00003817475,0.000009584981,6.4895994e-7,0.00025339212,0.0009484373,0.0001818402,0.00013810323,0.000009503685,0.00076803105],"study_design_scores_gemma":[0.00010070024,0.000091815964,0.9929823,0.000067023815,0.000028803888,0.00007877103,0.0012322627,0.002453035,0.00010998791,0.0024570627,0.00034276478,0.000055435776],"about_ca_topic_score_codex":0.011335655,"about_ca_topic_score_gemma":0.4442414,"teacher_disagreement_score":0.43290576,"about_ca_system_score_codex":0.0000017086675,"about_ca_system_score_gemma":0.00037091132,"threshold_uncertainty_score":0.99524796},"labels":[],"label_agreement":null},{"id":"W2946049759","doi":"10.1139/cjes-2018-0178","title":"Pleistocene mammals from Extinction Cave, Belize","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Toronto Zoo; University of Toronto","funders":"","keywords":"Cave; Panthera; Pleistocene; Jaguar; Fauna; Extinction (optical mineralogy); Equus; Geography; Eutheria; Ecology; Geology; Archaeology; Biology; Paleontology; Predation; Cenozoic; Phanerozoic","score_opus":0.023506862282381406,"score_gpt":0.21528297493133267,"score_spread":0.19177611264895125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946049759","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95116246,0.00448528,0.00001579601,0.0006911925,0.0018467044,0.000055793913,0.000039733546,0.0000043842324,0.04169865],"genre_scores_gemma":[0.99790806,0.0000595273,0.0007595221,0.00041266903,0.00017460564,7.082042e-8,0.0000033029692,0.0000010320923,0.00068120105],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898136,0.00006658296,0.00025484973,0.00014855368,0.0002276681,0.00032096467],"domain_scores_gemma":[0.9991119,0.00014022778,0.00018324825,0.000079831385,0.000094877534,0.00038992174],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005151685,0.00008751251,0.00018224605,0.00022139234,0.00035262376,0.000076825054,0.00028619575,0.000051504077,0.009813349],"category_scores_gemma":[0.00009568816,0.00006657683,0.00006391701,0.00027984832,0.00035083923,0.00033768982,0.000002469023,0.0001387778,0.00048869324],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007265549,0.0000010740675,0.99481225,0.0000013060854,0.0000121349185,0.000019244979,0.00016334535,0.00061001553,0.000011039324,0.000048059574,0.00044019957,0.0038740397],"study_design_scores_gemma":[0.00015897494,0.00023629788,0.9698399,0.000019578916,0.000008662708,0.000054605836,0.00050662487,0.0003723597,0.00002004017,0.00047350416,0.028222539,0.00008694876],"about_ca_topic_score_codex":0.066302195,"about_ca_topic_score_gemma":0.9232465,"teacher_disagreement_score":0.85694426,"about_ca_system_score_codex":0.0000019149718,"about_ca_system_score_gemma":0.0006105624,"threshold_uncertainty_score":0.9910918},"labels":[],"label_agreement":null},{"id":"W2946692482","doi":"10.1139/cjes-2019-0003","title":"Geochemistry, geochronology and Sr–Nd–Hf isotopes of two types of Early Cretaceous granite porphyry dykes in the Sulu orogenic belt, eastern China","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Zircon; Geochemistry; Geochronology; Tectonics; Cretaceous; Isotope; Rare-earth element; Trace element; Petrology; Rare earth; Mineralogy; Paleontology","score_opus":0.009862259779370811,"score_gpt":0.19397455670942124,"score_spread":0.18411229693005043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946692482","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99069184,0.006016782,0.0000019714887,0.0006638542,0.00007432503,0.000059633043,0.000030233115,0.0000011581743,0.0024602122],"genre_scores_gemma":[0.99960846,0.00007980281,0.00011596932,0.00008639148,0.000035258032,1.3123163e-7,0.000003855631,9.480434e-7,0.00006919189],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99877954,0.00010292767,0.00037094866,0.00017106763,0.00025129586,0.00032422366],"domain_scores_gemma":[0.99918,0.0001506628,0.00026531727,0.000116020536,0.00008142782,0.00020654626],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007726886,0.000110135756,0.0003148765,0.00019138049,0.00008919386,0.000043594584,0.0005446847,0.000054492688,0.0024336353],"category_scores_gemma":[0.00009346815,0.00006465501,0.00009791902,0.00049142475,0.0007876008,0.0001567656,0.0000109114935,0.00018364798,0.00001487205],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000100533425,0.0000063282796,0.99534434,0.000013131709,0.000017464985,0.00002565314,0.00036097216,0.00072069984,0.0005347878,0.000030912255,0.0000069103044,0.0029287485],"study_design_scores_gemma":[0.00022893213,0.0005076323,0.992259,0.000039108676,0.00002820317,0.00012952345,0.00039671655,0.0008393248,0.00089621334,0.004320097,0.00025586312,0.00009933756],"about_ca_topic_score_codex":0.052949317,"about_ca_topic_score_gemma":0.33565232,"teacher_disagreement_score":0.28270298,"about_ca_system_score_codex":8.735723e-7,"about_ca_system_score_gemma":0.00029367514,"threshold_uncertainty_score":0.9984783},"labels":[],"label_agreement":null},{"id":"W2946701303","doi":"10.1139/cjes-2019-0036","title":"Assessment of a seismo-neotectonic origin for the New Liskeard–Thornloe scarp, Timiskaming graben, northeastern Ontario","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Fault scarp; Geology; Bedrock; Graben; Fault (geology); Geomorphology; Half-graben; Neotectonics; River terraces; Seismology; Shore; Structural basin; Fluvial; Oceanography","score_opus":0.035812742992884304,"score_gpt":0.2720692499739326,"score_spread":0.2362565069810483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946701303","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99111325,0.0012814744,0.0002020585,0.0014326054,0.0009279726,0.00024121,0.000014459905,0.0000021170467,0.004784861],"genre_scores_gemma":[0.99642926,0.000020439513,0.001513013,0.00015693385,0.00008874923,3.7234406e-7,0.0000026631071,0.0000019508414,0.0017866102],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99849606,0.0001032351,0.00033509437,0.00018452563,0.00032914535,0.00055194995],"domain_scores_gemma":[0.9984027,0.00059338735,0.00024272276,0.00016516531,0.00015007901,0.00044592566],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001848859,0.000113132664,0.0002698937,0.00028240719,0.00042629335,0.00009214528,0.00074204523,0.00008000485,0.0030629504],"category_scores_gemma":[0.0000810239,0.000071012924,0.00013270724,0.00034210374,0.0005179602,0.00024640508,0.000007482314,0.00036774136,0.00004750645],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010922681,0.000002245209,0.9901083,0.00000923351,0.000029235258,0.00001255748,0.00034447145,0.008243232,0.0000032116332,0.00015522922,0.00009341892,0.0009879468],"study_design_scores_gemma":[0.00030657838,0.0005736812,0.9786506,0.00004476853,0.000022647553,0.00017795849,0.00029720194,0.005715342,0.000016057513,0.00039093225,0.013715393,0.0000888285],"about_ca_topic_score_codex":0.13873588,"about_ca_topic_score_gemma":0.96421134,"teacher_disagreement_score":0.82547545,"about_ca_system_score_codex":0.0000021356861,"about_ca_system_score_gemma":0.007808833,"threshold_uncertainty_score":0.9978484},"labels":[],"label_agreement":null},{"id":"W2947131279","doi":"10.1139/cjes-2018-0283","title":"Reconstructing the deformation of the North Anatolian Fault Zone through restoring the Oligo–Miocene exhumation pattern of the Almacık Block (northwestern Turkey) based on the apatite (U–Th)/He ages","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Block (permutation group theory); Fault (geology); Tectonics; Seismology; North Anatolian Fault; Neogene; Paleontology; Structural basin","score_opus":0.024015422171736307,"score_gpt":0.20470261234638573,"score_spread":0.18068719017464943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2947131279","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924221,0.0004295896,0.000008821404,0.0037339523,0.00089014415,0.00026760658,0.000033521876,0.0000027557996,0.002211492],"genre_scores_gemma":[0.9992353,0.00004909444,0.000036159112,0.00054384454,0.00008859181,6.6151165e-7,0.0000010961669,0.000002813709,0.00004248557],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981334,0.00024389834,0.0004931247,0.00014105045,0.0006629804,0.00032555065],"domain_scores_gemma":[0.9979985,0.00052607537,0.0008458831,0.00038802522,0.00016651244,0.00007502121],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013607386,0.0001443831,0.00019921396,0.00009128149,0.0012607955,0.00012122438,0.0010901378,0.000038913466,0.00021602405],"category_scores_gemma":[0.0001584211,0.00005226716,0.00015967587,0.000753921,0.00081408804,0.0003479836,0.00002044148,0.00034099215,0.000008526233],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000034803272,0.0000017842364,0.96671695,0.0000108133145,0.000021008715,7.630053e-7,0.0026477813,0.023620775,0.000004449114,0.000033429544,0.000029956262,0.006908809],"study_design_scores_gemma":[0.00013096578,0.000110350724,0.9893764,0.00021175752,0.000025936904,0.00003568092,0.0032072696,0.0056865853,0.0003787611,0.000090102265,0.00066860166,0.00007758885],"about_ca_topic_score_codex":0.03865705,"about_ca_topic_score_gemma":0.4490426,"teacher_disagreement_score":0.41038555,"about_ca_system_score_codex":0.000005893811,"about_ca_system_score_gemma":0.0005361385,"threshold_uncertainty_score":0.96971476},"labels":[],"label_agreement":null},{"id":"W2947340396","doi":"10.1139/cjes-2018-0312","title":"Geomorphic diversity and complexity of the inner shelf, Canadian Arctic Archipelago, based on LiDAR and multibeam sonar surveys","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Geological Survey of Canada","funders":"","keywords":"Geology; Glacial period; Oceanography; Seabed gouging by ice; Seafloor spreading; Arctic; Iceberg; Archipelago; Bathymetry; Continental shelf; Glacial landform; Paleontology; Geomorphology; Moraine; Sea ice; Arctic ice pack; Drift ice","score_opus":0.029543622725026673,"score_gpt":0.19795897688439054,"score_spread":0.16841535415936387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2947340396","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967039,0.00010337896,0.0000040312857,0.000926987,0.00019060413,0.000106308566,0.000024208091,7.665461e-7,0.0019397953],"genre_scores_gemma":[0.99931794,0.000008730961,0.00022231713,0.00032894316,0.000010657034,1.08706736e-7,3.6721758e-7,0.000002878457,0.0001080377],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988613,0.00021530449,0.00016660245,0.00016169137,0.00028798555,0.00030712347],"domain_scores_gemma":[0.99893695,0.00009116003,0.0001422763,0.00011737445,0.000023851526,0.00068836357],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015357399,0.000091246424,0.00015125891,0.0001439383,0.0007835617,0.000037790698,0.00035231875,0.000042752745,0.001109709],"category_scores_gemma":[0.00006271582,0.000058708825,0.000038674163,0.00032142331,0.0016900585,0.00013467466,0.00008142266,0.00021927383,0.000012552017],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000027257524,0.00000487824,0.9954277,0.0000064559467,0.0000048128636,0.00000851581,0.0006617142,0.0031520715,0.00009382047,0.0000888138,0.00001359003,0.0005348905],"study_design_scores_gemma":[0.00022249884,0.00019060979,0.9951219,0.00005263286,0.00000785803,0.0000238527,0.00016863002,0.0028284593,0.000061744664,0.00076517055,0.00047286286,0.000083809646],"about_ca_topic_score_codex":0.5497438,"about_ca_topic_score_gemma":0.88155544,"teacher_disagreement_score":0.33181167,"about_ca_system_score_codex":0.000027171964,"about_ca_system_score_gemma":0.00040996936,"threshold_uncertainty_score":0.9998034},"labels":[],"label_agreement":null},{"id":"W2947534168","doi":"10.1139/cjes-2018-0321","title":"Active transform faults in the Gulf of Guinea: insights from geophysical data and implications for seismic hazard assessment","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Transform fault; Seismic hazard; Tectonics; Transtension; Seismotectonics; Active fault; Fault (geology); Strain partitioning; Induced seismicity; Plate tectonics; Rift","score_opus":0.036828523129992935,"score_gpt":0.27119562085918136,"score_spread":0.23436709772918843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2947534168","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99298495,0.0009868216,0.00007595432,0.0027154405,0.00014738213,0.000188291,0.00048648944,8.646482e-7,0.0024138321],"genre_scores_gemma":[0.999026,0.000069873226,0.00063783687,0.00018112878,0.000055780783,4.9212343e-7,0.000016723452,9.2591836e-7,0.00001125251],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99922997,0.000038851234,0.00022478208,0.00015863402,0.00015783936,0.00018994605],"domain_scores_gemma":[0.99908674,0.0004538289,0.00012120309,0.00016216366,0.000059414764,0.00011666763],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003662388,0.00007087249,0.00017701607,0.00012470008,0.00018808633,0.000046960155,0.0005647742,0.000025244652,0.000067805006],"category_scores_gemma":[0.00004556603,0.000042116033,0.000035661382,0.00025205,0.00027723835,0.00038659034,0.0000058127985,0.00011150504,0.0000029630662],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015463549,0.000011160193,0.9492346,0.000008408948,0.00003704899,0.000004286459,0.0021608823,0.0007067569,0.000036424335,0.0004924755,0.00016121664,0.047131248],"study_design_scores_gemma":[0.00026027873,0.00028329826,0.9857875,0.000026376261,0.000013627561,0.000009355368,0.0015210976,0.0034877185,0.000021274655,0.0041387556,0.0043938947,0.000056823872],"about_ca_topic_score_codex":0.016583689,"about_ca_topic_score_gemma":0.48695213,"teacher_disagreement_score":0.47036844,"about_ca_system_score_codex":0.000001336285,"about_ca_system_score_gemma":0.0007617917,"threshold_uncertainty_score":0.98996496},"labels":[],"label_agreement":null},{"id":"W2948014132","doi":"10.1139/cjes-2018-0311","title":"Distribution and morphology of inner-shelf sand bodies off southwest Newfoundland based on merged multibeam sonar and LiDAR data","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Geology; Seafloor spreading; Bedrock; Bathymetry; Submarine pipeline; Oceanography; Marine transgression; Submarine canyon; Canyon; Continental shelf; Sonar; Channel (broadcasting); Geomorphology; Shoal; Seabed; Structural basin","score_opus":0.02488941715286607,"score_gpt":0.22200170968782182,"score_spread":0.19711229253495574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2948014132","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956376,0.0022126415,0.000028179405,0.0006257321,0.00016460047,0.000055729597,0.0005546407,0.0000017747245,0.000719105],"genre_scores_gemma":[0.99899054,0.0001521592,0.0006165737,0.00012208491,0.000026220085,5.6298365e-8,0.000058499285,7.4047625e-7,0.000033111755],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991972,0.000048534763,0.00022795325,0.0001484089,0.0001675908,0.0002103416],"domain_scores_gemma":[0.99920595,0.00017768829,0.00016729778,0.00010142781,0.00008186406,0.00026575307],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006769503,0.0000806974,0.00017482297,0.00014946723,0.00024879284,0.00009139894,0.0002608569,0.00004759456,0.00066899235],"category_scores_gemma":[0.00016617497,0.000053686777,0.000016747092,0.00016690628,0.0005320773,0.0004299367,0.000008923069,0.00010456639,0.000011018532],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014591612,0.0000030905712,0.99470675,0.00001286824,0.0000041854814,0.0000059035815,0.000102173006,0.0010451801,0.000015772326,0.00003472162,0.0000416335,0.004013117],"study_design_scores_gemma":[0.00025645594,0.00061680365,0.98621243,0.000036601363,0.0000098016335,0.000057360878,0.00027635987,0.0060242717,0.0000282061,0.00021382199,0.006189713,0.00007815],"about_ca_topic_score_codex":0.012507049,"about_ca_topic_score_gemma":0.16152038,"teacher_disagreement_score":0.14901333,"about_ca_system_score_codex":8.1062495e-7,"about_ca_system_score_gemma":0.00038521126,"threshold_uncertainty_score":0.99406874},"labels":[],"label_agreement":null},{"id":"W2948216840","doi":"10.1139/cjes-2018-0338","title":"Interpreting basal sediments and plant fossils in kettle lakes: insights from Silver Lake, Michigan, USA","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"University of Minnesota; National Science Foundation","keywords":"Macrofossil; Geology; Holocene; Deglaciation; Radiocarbon dating; Kettle (birds); Physical geography; Paleontology; Pleistocene; Pollen; Chronology; Paleoecology; Archaeology; Ecology; Geography","score_opus":0.016557090898110437,"score_gpt":0.2216437799405561,"score_spread":0.20508668904244565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2948216840","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905075,0.0017716646,0.0000010751097,0.00037006655,0.0006321047,0.00006863186,0.00004530763,0.0000014748011,0.006602177],"genre_scores_gemma":[0.9992206,0.000028808243,0.00020508692,0.0003766967,0.00004270469,1.1482139e-7,0.0000069552234,0.0000011266517,0.00011792586],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987856,0.00014544137,0.00026203564,0.00019721877,0.00019941926,0.0004102966],"domain_scores_gemma":[0.99891627,0.0004566137,0.00011146329,0.00007437017,0.000035426256,0.0004058441],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005861149,0.00009688788,0.00021021387,0.00038918376,0.00019148749,0.000094586656,0.00034035573,0.000087886,0.0029726864],"category_scores_gemma":[0.00013101046,0.00007224071,0.000031306954,0.0002601365,0.0004946213,0.0003875102,0.000007731743,0.0003032995,0.00017476025],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015291933,0.0000021902156,0.99861753,0.0000043098207,0.000008242076,0.00014640285,0.000821002,0.00021955532,0.000028148386,0.000020796104,0.000028823144,0.00008768287],"study_design_scores_gemma":[0.00027221383,0.00018931263,0.9957337,0.00010922131,0.000003406108,0.000087325374,0.0005585855,0.0010790866,0.00009068154,0.00072923326,0.0010548928,0.000092341295],"about_ca_topic_score_codex":0.007065061,"about_ca_topic_score_gemma":0.95128316,"teacher_disagreement_score":0.9442181,"about_ca_system_score_codex":2.9944377e-7,"about_ca_system_score_gemma":0.0007572884,"threshold_uncertainty_score":0.999547},"labels":[],"label_agreement":null},{"id":"W2948822093","doi":"10.1139/cjes-2019-0022","title":"Sedimentological signatures and identification of Paleocene sedimentary facies in the Lishui Sag, East China Sea Shelf Basin","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"China National Offshore Oil Corporation","keywords":"Geology; Facies; Delta; Sedimentary rock; Mouth bar; Ichnofacies; Sedimentary structures; Paleontology; Trace fossil; Geomorphology; Fluvial; Continental shelf; Structural basin; Oceanography","score_opus":0.01401699432437281,"score_gpt":0.2045894217046909,"score_spread":0.1905724273803181,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2948822093","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938136,0.0022698804,0.000006368425,0.0017888772,0.00019963695,0.000087373424,0.00004236629,0.0000014118225,0.0017905262],"genre_scores_gemma":[0.99938786,0.00006517338,0.00017245168,0.00031585674,0.000025907555,1.6195445e-7,0.000006593511,4.682177e-7,0.000025500794],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990231,0.00009287711,0.00030550815,0.00010467168,0.00026568898,0.00020817964],"domain_scores_gemma":[0.99945086,0.00011838493,0.00017834129,0.00006207983,0.00005093475,0.00013939204],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012159655,0.00007184959,0.00013755295,0.00020078897,0.00017723757,0.00013396433,0.00035543,0.000044397068,0.001214104],"category_scores_gemma":[0.00009162196,0.000039364542,0.00003262645,0.00043028686,0.00038302437,0.00049207546,0.0000041198073,0.00015033674,0.000010982065],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000048390425,0.0000044381773,0.9949115,0.000010786594,0.000002611542,0.0000060918583,0.0007087173,0.0024804422,0.00002167664,0.00013565604,0.00005864448,0.0016545918],"study_design_scores_gemma":[0.00009399134,0.0002545483,0.9946307,0.000022588332,0.0000047952685,0.000046884194,0.0016015501,0.0009177025,0.000084920444,0.0010170009,0.0012703361,0.000054978016],"about_ca_topic_score_codex":0.0054107546,"about_ca_topic_score_gemma":0.033605646,"teacher_disagreement_score":0.028194891,"about_ca_system_score_codex":7.7839826e-7,"about_ca_system_score_gemma":0.00022121822,"threshold_uncertainty_score":0.99969894},"labels":[],"label_agreement":null},{"id":"W2949406804","doi":"10.1139/cjes-2018-0332","title":"Zircon U–Pb chronology, geochemistry, and petrogenesis of the high Nb–Ta alkaline rhyolites at the Tuohe Tree Farm, northern Volcanic Belt, Great Xing’an Range, China","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Partial melting; Mantle plume; Petrogenesis; Rhyolite; Zircon; Primitive mantle; Basalt; Mantle (geology); Mafic; Fractional crystallization (geology); Volcanic rock; Volcano; Tectonics; Lithosphere; Paleontology","score_opus":0.008314048965867902,"score_gpt":0.17740172292974726,"score_spread":0.16908767396387936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2949406804","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99186796,0.0034874254,0.0000021166331,0.002849467,0.0001894124,0.000077276374,0.00007764842,0.0000029885216,0.0014456868],"genre_scores_gemma":[0.9989819,0.00008726451,0.00008710809,0.00024472727,0.00010881789,2.5965687e-7,0.000010476441,0.0000019532663,0.00047752023],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99849945,0.00011399673,0.00034776574,0.0002660803,0.0003335332,0.00043916836],"domain_scores_gemma":[0.99875593,0.00015295018,0.00031233794,0.00024545,0.00011234295,0.00042101045],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00066483836,0.00016295884,0.00031142568,0.000098481876,0.00048323255,0.00007634069,0.000841863,0.000076274184,0.006812686],"category_scores_gemma":[0.00015289897,0.00007774654,0.00016435189,0.00051862904,0.0013167567,0.00016361417,0.000033364027,0.00019504454,0.00002782064],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012334501,0.000004754556,0.9922274,0.00000808062,0.000030551742,0.0000074153763,0.00010279708,0.00089336577,0.0031859223,0.000017490369,0.00002825948,0.0034816419],"study_design_scores_gemma":[0.00025207127,0.0002836149,0.9905131,0.000023973194,0.00006241228,0.00016124758,0.00023052872,0.00081454543,0.0042533665,0.0016103771,0.0016586018,0.00013617857],"about_ca_topic_score_codex":0.08332892,"about_ca_topic_score_gemma":0.8888794,"teacher_disagreement_score":0.8055505,"about_ca_system_score_codex":0.0000043407117,"about_ca_system_score_gemma":0.00037396516,"threshold_uncertainty_score":0.9940952},"labels":[],"label_agreement":null},{"id":"W2955826766","doi":"10.1139/cjes-2018-0182","title":"The sources of metamorphic heat during collisional orogeny: the Barrovian enigma","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Metamorphism; Lithosphere; Ophiolite; Metamorphic rock; Orogeny; Crust; Geochemistry; Petrology; Metamorphic core complex; Back-arc basin; Overprinting; Subduction; Geophysics; Tectonics; Seismology","score_opus":0.010673436667737369,"score_gpt":0.17276095400383296,"score_spread":0.16208751733609558,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2955826766","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9901708,0.0042090868,9.897329e-7,0.0033163263,0.00024393015,0.000053315667,0.000016402382,0.0000014894599,0.0019876682],"genre_scores_gemma":[0.9993097,0.000056289136,0.00007420528,0.00018647393,0.00007911246,1.0878958e-7,8.215102e-7,7.892798e-7,0.00029246378],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986035,0.000102701815,0.00033417213,0.00013177095,0.00045668907,0.0003711693],"domain_scores_gemma":[0.99879265,0.00042062413,0.00015946866,0.00012452272,0.00012489365,0.00037784482],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011564364,0.000091337635,0.00019646993,0.00010962399,0.0007659907,0.00013740604,0.0008396227,0.000033746008,0.00573761],"category_scores_gemma":[0.00020299056,0.00003770075,0.00017355075,0.00062710285,0.0009091793,0.0001666207,0.000010127636,0.00017762734,0.00007086922],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008026805,0.0000016360809,0.99170125,0.0000024069957,0.00002271055,0.000011083888,0.00008609745,0.007444211,0.00019533097,0.00014655493,0.000028843557,0.00035188007],"study_design_scores_gemma":[0.00009966619,0.00016226205,0.9891039,0.000016565733,0.000022091095,0.0001086178,0.0007142098,0.0012642083,0.0011428958,0.002562625,0.0047258707,0.00007704787],"about_ca_topic_score_codex":0.016274795,"about_ca_topic_score_gemma":0.284788,"teacher_disagreement_score":0.26851323,"about_ca_system_score_codex":9.83925e-7,"about_ca_system_score_gemma":0.0005156525,"threshold_uncertainty_score":0.9951713},"labels":[],"label_agreement":null},{"id":"W2956272617","doi":"10.1139/cjes-2018-0313","title":"Petrochemistry and U–Pb (zircon) age of porphyry dykes at the McKenzie Gulch porphyry–skarn Cu–Ag–Au deposit, north-central New Brunswick, Canada: implications for emplacement age, tectonic setting, and mineralization potential","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Zircon; Plagioclase; Hornblende; Felsic; Adakite; Mafic; Partial melting; Andesite; Fractional crystallization (geology); Petrology; Subduction; Crust; Mantle (geology); Biotite; Quartz; Tectonics; Oceanic crust; Volcanic rock; Seismology","score_opus":0.008997052496774093,"score_gpt":0.18803329038519662,"score_spread":0.17903623788842252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2956272617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945519,0.0016709388,0.00012948443,0.0029212637,0.0001262042,0.00012968265,0.00008233371,0.000001919904,0.00038628402],"genre_scores_gemma":[0.998331,0.00005266186,0.0006192452,0.0003095443,0.00009769163,2.6969792e-7,0.000077012395,0.0000017696225,0.0005108217],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99871314,0.000031779124,0.00035266054,0.00023075377,0.00023162812,0.00044005847],"domain_scores_gemma":[0.9988156,0.000108639906,0.00027398602,0.000109839966,0.000099164004,0.00059275056],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025798383,0.00013212353,0.00023043515,0.00008209992,0.0004247927,0.00009179923,0.00029335657,0.00004523807,0.00060032454],"category_scores_gemma":[0.00009133311,0.0000857344,0.00007975526,0.0002956476,0.0003885116,0.00013079376,0.000015906036,0.00010571622,0.0000013513279],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010651345,0.0000031341892,0.9936252,0.000017191549,0.000027657548,0.00001036621,0.00007053822,0.0020193537,0.003092942,0.000035322984,0.00040771646,0.0006798932],"study_design_scores_gemma":[0.00023184206,0.00013942158,0.99608195,0.000019879664,0.000057124336,0.00011268881,0.00014949132,0.00041749902,0.00081213407,0.00034757177,0.0015111165,0.00011928556],"about_ca_topic_score_codex":0.7624302,"about_ca_topic_score_gemma":0.9977311,"teacher_disagreement_score":0.23530091,"about_ca_system_score_codex":0.00001059915,"about_ca_system_score_gemma":0.0026781014,"threshold_uncertainty_score":0.6573133},"labels":[],"label_agreement":null},{"id":"W2958583059","doi":"10.1139/cjes-2018-0213","title":"Geochemistry and mineralogy of Quaternary sediments in the northern Bohai Bay Basin, North China: implications for provenance and climate change","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Provenance; Geochemistry; Sedimentary rock; Quaternary; Weathering; Igneous rock; Plagioclase; Feldspar; Quartz; Paleontology","score_opus":0.014773548136693144,"score_gpt":0.21284264288452098,"score_spread":0.19806909474782783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2958583059","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99622494,0.00084122946,8.92832e-7,0.0021345415,0.000045493933,0.00011166509,0.0001594002,5.3073927e-7,0.00048128708],"genre_scores_gemma":[0.99952483,0.000075094445,0.00013778282,0.00018702558,0.00004078421,0.0000011393053,0.000013061327,7.8195797e-7,0.000019488682],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99935406,0.000019267916,0.00019562429,0.00012017636,0.000087636894,0.00022322254],"domain_scores_gemma":[0.9995645,0.00004656723,0.00015320358,0.00006876096,0.000036419005,0.0001305078],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039431427,0.00006528377,0.0001286283,0.000067458815,0.00014775908,0.000039942322,0.00020723921,0.000021375317,0.00007087435],"category_scores_gemma":[0.000020065101,0.00004260996,0.00003106805,0.00019966425,0.00018846495,0.00019152256,0.000004540204,0.000060841197,9.893441e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005097207,0.0000036208542,0.99733245,0.000022955528,0.000005206166,0.0000021844228,0.0003558531,0.000057134483,0.00009390849,0.000009647849,0.000015125529,0.0020968108],"study_design_scores_gemma":[0.00014686574,0.00013388498,0.99799496,0.00002539369,0.000010496607,0.00005255888,0.0003601352,0.0005165504,0.00007724409,0.00019389564,0.00043492057,0.000053068386],"about_ca_topic_score_codex":0.009056078,"about_ca_topic_score_gemma":0.34312254,"teacher_disagreement_score":0.33406648,"about_ca_system_score_codex":9.628554e-7,"about_ca_system_score_gemma":0.00012205981,"threshold_uncertainty_score":0.9975427},"labels":[],"label_agreement":null},{"id":"W2960284623","doi":"10.1139/cjes-2019-0065","title":"Principles of structural geology on rocky planets","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Planet; Tectonics; Plate tectonics; Astrobiology; Mars Exploration Program; Venus; Landform; Terrestrial planet; Geophysics; Paleontology; Astronomy","score_opus":0.018927675140799204,"score_gpt":0.19391836936690718,"score_spread":0.17499069422610797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2960284623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97525936,0.0004806694,0.000001069856,0.00050912384,0.00028775836,0.00003173709,0.000018423898,0.0000015888463,0.023410236],"genre_scores_gemma":[0.99910843,0.00000629488,0.00033668336,0.00023288395,0.00005389217,2.1892568e-8,0.0000042065963,5.2349606e-7,0.00025706922],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99897695,0.000042176318,0.00029096,0.00013450925,0.0002468317,0.00030859574],"domain_scores_gemma":[0.99911547,0.00014542528,0.00021327652,0.00007676395,0.00007365826,0.00037543027],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003346267,0.000082246275,0.00022519844,0.00021672732,0.00010824526,0.000028122791,0.00041478957,0.0000465737,0.018090995],"category_scores_gemma":[0.00012169547,0.0000493732,0.00008395718,0.00030475412,0.00036399803,0.00011826062,0.000004416425,0.00013864272,0.00013808282],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000088824245,0.0000012371241,0.97892433,0.0000031307784,0.0000100143725,0.000016997334,0.00003473624,0.019426938,0.000046145335,0.0005918973,0.000011950918,0.00092374475],"study_design_scores_gemma":[0.00010032963,0.0006125877,0.99061745,0.000014686873,0.0000075866556,0.00006412325,0.0000889524,0.0022441973,0.00036233437,0.0027611793,0.0030504942,0.000076096105],"about_ca_topic_score_codex":0.016655823,"about_ca_topic_score_gemma":0.23002152,"teacher_disagreement_score":0.2133657,"about_ca_system_score_codex":6.3536106e-7,"about_ca_system_score_gemma":0.00032944468,"threshold_uncertainty_score":0.98989236},"labels":[],"label_agreement":null},{"id":"W2960851734","doi":"10.1139/cjes-2019-0114","title":"Observations: What for?","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Test (biology); USable; Paleontology; Computer science; Multimedia","score_opus":0.049550418144802155,"score_gpt":0.2313222734391691,"score_spread":0.18177185529436696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2960851734","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.87394994,0.003095313,0.037779134,0.057686035,0.0056876973,0.00030367982,0.0000029313983,0.000019571948,0.021475663],"genre_scores_gemma":[0.9743962,0.000014001926,0.023066565,0.0008107751,0.00007260319,7.28265e-7,1.9922302e-7,5.6017245e-7,0.0016383161],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99938756,0.000012306211,0.00015059327,0.00010818324,0.000120835655,0.00022050411],"domain_scores_gemma":[0.9992519,0.00008203862,0.00011768906,0.000118003816,0.00022127447,0.00020906866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006738143,0.00004426429,0.00008044193,0.00010408024,0.00017859384,0.00042905167,0.0008130303,0.000024406108,0.00006316762],"category_scores_gemma":[0.00018343414,0.000035535148,0.000047813333,0.00032813346,0.00008329849,0.0014514296,0.000013060421,0.00005805961,0.000012764159],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005246417,0.000023367933,0.48722756,0.00008420346,0.000043308424,0.00008142717,0.0036180487,0.019706268,0.004095827,0.4407416,0.006899372,0.037473764],"study_design_scores_gemma":[0.00046235393,0.00054847397,0.08811168,0.0002779961,0.0000056974022,0.0002848495,0.0016721823,0.022668071,0.0033619339,0.07405518,0.80823517,0.00031641696],"about_ca_topic_score_codex":0.00011064289,"about_ca_topic_score_gemma":0.0018784973,"teacher_disagreement_score":0.8013358,"about_ca_system_score_codex":0.0000026820396,"about_ca_system_score_gemma":0.0010773791,"threshold_uncertainty_score":0.4137355},"labels":[],"label_agreement":null},{"id":"W2961762386","doi":"10.1139/cjes-2019-0126","title":"Introduction to the Special issue of the <i>Canadian Journal of Earth Sciences</i>, “Magmatic and metallogenic processes associated with large igneous provinces”","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Metallogeny; Igneous rock; Geology; Geochemistry; Mineral exploration; Session (web analytics); Plenary session; Scope (computer science); Large igneous province; Earth science; Felsic; Library science; Mafic; Tectonics; Paleontology; Computer science","score_opus":0.007026142852900496,"score_gpt":0.1738097169359643,"score_spread":0.16678357408306382,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2961762386","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98732036,0.00093838753,0.0000051766547,0.0089973435,0.0004962374,0.0001557647,0.0000339893,0.0000011473564,0.0020516117],"genre_scores_gemma":[0.9982345,0.000014270728,0.0002400418,0.00046109152,0.0007261639,1.6317868e-7,0.0000010753392,0.0000014750857,0.000321201],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99807906,0.00015382757,0.00044565854,0.00019382309,0.0006448683,0.0004827875],"domain_scores_gemma":[0.9980726,0.00017566945,0.0005661017,0.00011245503,0.00048663636,0.000586501],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0022522572,0.00013036809,0.00032251872,0.00030852586,0.00080830936,0.00026086104,0.000882847,0.000051837804,0.0043515237],"category_scores_gemma":[0.0012483359,0.000058060592,0.00009692785,0.0019259696,0.0011970752,0.0003652647,0.0000113374645,0.00026017666,0.000022795071],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015137872,0.000011435421,0.9878706,0.000019172941,0.00006150853,0.00001872913,0.0008008679,0.009210814,0.0000746784,0.00009266595,0.00078434346,0.0010400792],"study_design_scores_gemma":[0.00037241477,0.0021526208,0.9523283,0.00017044532,0.00016719174,0.00049764477,0.0018942644,0.00066261855,0.0009469795,0.002233467,0.038316388,0.0002576483],"about_ca_topic_score_codex":0.027580531,"about_ca_topic_score_gemma":0.96741545,"teacher_disagreement_score":0.9398349,"about_ca_system_score_codex":0.000003581024,"about_ca_system_score_gemma":0.004112292,"threshold_uncertainty_score":0.9965586},"labels":[],"label_agreement":null},{"id":"W2963148930","doi":"10.1139/cjes-2018-0325","title":"The Kanaka Creek fossil flora (Huntingdon Formation), British Columbia, Canada — paleoenvironment and evidence for Paleocene age using palynology and macroflora","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Brandon University; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Macrofossil; Palynology; Geology; Paleogene; Paleontology; Beringia; Paleobotany; Range (aeronautics); Flora (microbiology); Pleistocene; Ecology; Cretaceous; Pollen; Holocene; Biology","score_opus":0.03620431815694286,"score_gpt":0.1913981750777942,"score_spread":0.15519385692085133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2963148930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99536806,0.0034343817,0.000004882903,0.00075485767,0.0002490657,0.00011284312,0.000044922665,0.0000012778015,0.000029693623],"genre_scores_gemma":[0.99916774,0.00035703715,0.00013138859,0.00014466693,0.000057286128,4.4774768e-7,0.00000149266,2.773209e-7,0.00013964543],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99921983,0.000043563243,0.00016321139,0.00012307781,0.00015889503,0.00029144515],"domain_scores_gemma":[0.99932134,0.00023603268,0.00015400325,0.000021803799,0.000045919594,0.0002209222],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005998393,0.0000476874,0.00010850864,0.000010743275,0.0012831152,0.00063224573,0.00019603419,0.00003543986,0.000056641213],"category_scores_gemma":[0.00010838992,0.000029599827,0.000025942732,0.00011791475,0.0002883777,0.00041507624,0.000018968485,0.00007049349,5.4660137e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057047837,0.0000018776465,0.97733563,0.000010247912,0.0000070570204,0.00003235494,0.000052676252,0.000030982705,0.0012518342,0.0000068370596,0.0006552858,0.020609522],"study_design_scores_gemma":[0.00009726731,0.0001712313,0.98172045,0.000091200745,0.00001138449,0.00019698766,0.000837992,0.00067017163,0.000014382398,0.00014142042,0.01596384,0.00008367097],"about_ca_topic_score_codex":0.8667488,"about_ca_topic_score_gemma":0.99936855,"teacher_disagreement_score":0.13261975,"about_ca_system_score_codex":0.000015500524,"about_ca_system_score_gemma":0.00020173144,"threshold_uncertainty_score":0.9868815},"labels":[],"label_agreement":null},{"id":"W2963320608","doi":"10.1139/cjes-2019-0050","title":"U–Pb dating of detrital zircons in the eastern Guangdong Basin, South China, and constraints on the tectonic transformation from the Early to Middle Jurassic","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Zircon; Foreland basin; Paleontology; Structural basin; Tectonics; Sedimentary rock; Mesozoic; Provenance; Paleozoic; Geochemistry","score_opus":0.024023348652465065,"score_gpt":0.18601044005705292,"score_spread":0.16198709140458786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2963320608","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915622,0.00017660465,0.000016916787,0.0049505336,0.000066709974,0.00010194747,0.00005421185,7.7448175e-7,0.0030701323],"genre_scores_gemma":[0.99926966,0.0000028333768,0.000076859826,0.00061175815,0.000027186099,1.7455235e-7,0.0000016835646,4.946095e-7,0.000009338209],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990752,0.000119060074,0.00023592351,0.00009229536,0.00026078624,0.0002167352],"domain_scores_gemma":[0.9991456,0.00048259407,0.00011783625,0.00008249894,0.000031563646,0.0001398834],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010059356,0.0000703152,0.00012864152,0.00009193495,0.00021648567,0.00013347011,0.0004584257,0.000024484609,0.00156537],"category_scores_gemma":[0.00019574985,0.000028336328,0.000056061777,0.0004899486,0.0004829192,0.00016270563,0.0000039121983,0.00018658003,0.000030071735],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045709935,0.000002059757,0.99071693,0.000001422715,0.000006561109,0.000002915188,0.0035061908,0.000581498,0.00006978261,0.00010778752,0.0000055223036,0.0049947584],"study_design_scores_gemma":[0.00008971227,0.00019900865,0.99103874,0.000055902878,0.000009432709,0.000011094131,0.0065448526,0.0008564812,0.00013669119,0.00093960925,0.00006962715,0.000048872294],"about_ca_topic_score_codex":0.029854024,"about_ca_topic_score_gemma":0.20011489,"teacher_disagreement_score":0.17026086,"about_ca_system_score_codex":8.5551744e-7,"about_ca_system_score_gemma":0.00015332786,"threshold_uncertainty_score":0.9993473},"labels":[],"label_agreement":null},{"id":"W2963470757","doi":"10.1139/cjes-2019-0076","title":"A younger glacial Lake Iroquois in the Lake Ontario basin, Ontario and New York: re-examination of pollen stratigraphy and radiocarbon dating","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Geological Survey of Canada","funders":"","keywords":"Varve; Geology; Radiocarbon dating; Glacial lake; Glacial period; Structural basin; Pollen; Detritus; Physical geography; Vegetation (pathology); Shelf ice; Paleontology; Oceanography; Sediment; Arctic; Geography; Ecology","score_opus":0.03526127653332789,"score_gpt":0.22150992714686132,"score_spread":0.18624865061353343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2963470757","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97931725,0.0007434198,6.803061e-7,0.0006371375,0.00017510238,0.00010541405,0.0000078381345,8.0265875e-7,0.019012349],"genre_scores_gemma":[0.9991806,0.000024065806,0.00028091558,0.00016238997,0.000029740013,1.00642666e-7,0.000004398343,7.41471e-7,0.0003170137],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99887437,0.00017805838,0.0002546154,0.00015016815,0.00023903247,0.00030373238],"domain_scores_gemma":[0.99928457,0.00022070091,0.00014766927,0.00007671039,0.000043149677,0.00022719605],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019210178,0.00008366344,0.00019295681,0.00036471203,0.00019660169,0.00009081148,0.00026459407,0.00007448234,0.0023667251],"category_scores_gemma":[0.00006229838,0.000057265075,0.000027825994,0.00034704804,0.0005234077,0.00035281238,0.000003915362,0.0003255449,0.0000031898112],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000148416775,0.000002088664,0.99334997,0.0000042850975,0.000006928788,0.000025372496,0.0052464795,0.000052068935,0.0000011129127,0.00007195463,0.00003773129,0.0011871777],"study_design_scores_gemma":[0.00027924485,0.00037188924,0.9947096,0.00003092838,0.0000081813405,0.0001881755,0.0011164541,0.000057388082,0.0000031490474,0.0003037379,0.0028682973,0.00006295839],"about_ca_topic_score_codex":0.41605276,"about_ca_topic_score_gemma":0.99992466,"teacher_disagreement_score":0.5838719,"about_ca_system_score_codex":9.3366265e-7,"about_ca_system_score_gemma":0.0022947558,"threshold_uncertainty_score":0.9985452},"labels":[],"label_agreement":null},{"id":"W2963891871","doi":"10.1139/cjes-2019-0004","title":"Hydrochronology of a proposed deep geological repository for low- and intermediate-level nuclear waste in southern Ontario from U–Pb dating of secondary minerals: response to Silurian and Cretaceous events","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Nuclear Waste Management Organization; University of Ottawa; Natural Resources Canada; University of Toronto","funders":"","keywords":"Geology; Calcite; Ordovician; Paleozoic; Carbonate; Devonian; Outcrop; Geochemistry; Paleontology; Sedimentary rock; Carbonate rock; Cretaceous","score_opus":0.01519270548034096,"score_gpt":0.1984707356012397,"score_spread":0.18327803012089874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2963891871","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988397,0.00040955836,0.000012159035,0.00017583206,0.00012054433,0.00013620405,0.000059780417,0.0000010061096,0.00024524293],"genre_scores_gemma":[0.9969102,0.0000032838598,0.002875229,0.000075076896,0.00001653111,1.8583576e-7,0.000002871928,0.0000011328203,0.00011545086],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990668,0.00008791642,0.00038545352,0.0001421894,0.00010834589,0.00020926673],"domain_scores_gemma":[0.9991288,0.00027604855,0.00023540028,0.000057767218,0.00007099294,0.00023094416],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007195584,0.00007588922,0.0002374051,0.00022554967,0.00009733847,0.000031538646,0.00021184947,0.00006182831,0.0006167],"category_scores_gemma":[0.0002582572,0.000053413794,0.000027649072,0.00013090849,0.00028795618,0.00021106264,0.000012031647,0.000113428876,0.0000032395865],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031642278,0.0000066956454,0.9865731,0.00003576651,0.000010934991,0.0000160485,0.006614491,0.0018401764,0.0013481127,0.000006303341,0.0000046303394,0.003227318],"study_design_scores_gemma":[0.000533761,0.0022420487,0.9870868,0.00015555229,0.000008350465,0.000069558024,0.005594913,0.0030268638,0.0002696052,0.0006085911,0.00029865326,0.000105317406],"about_ca_topic_score_codex":0.056046166,"about_ca_topic_score_gemma":0.68551296,"teacher_disagreement_score":0.6294668,"about_ca_system_score_codex":0.0000026879054,"about_ca_system_score_gemma":0.0006309321,"threshold_uncertainty_score":0.9502397},"labels":[],"label_agreement":null},{"id":"W2964708789","doi":"10.1139/cjes-2018-0256","title":"A major hydrobiological change in Dasht-e Arjan Wetland (southwestern Iran) during the late glacial – early Holocene transition revealed by subfossil chironomids","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Centre National de la Recherche Scientifique; Agence Nationale de la Recherche; Deutsche Forschungsgemeinschaft","keywords":"Holocene; Subfossil; Geology; Glacial period; Younger Dryas; Profundal zone; Varve; Wetland; Physical geography; Paleontology; Oceanography; Littoral zone; Ecology; Geography; Sediment","score_opus":0.022647181302613374,"score_gpt":0.2221536488121919,"score_spread":0.19950646750957854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2964708789","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961013,0.0010235684,8.3430774e-7,0.001578689,0.00033928268,0.00019266833,0.00004372314,0.0000035373776,0.0007163535],"genre_scores_gemma":[0.999462,0.00004166619,0.000020720634,0.00022904125,0.00009898191,8.4257397e-7,0.000007713975,0.0000017216701,0.0001372958],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99840915,0.00027902945,0.00030458806,0.00020114,0.00017485385,0.0006312382],"domain_scores_gemma":[0.999274,0.00012207216,0.00013032016,0.00010448566,0.00002979562,0.00033930817],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012799838,0.00012648599,0.0002514567,0.00027854313,0.0004145496,0.00009916038,0.00052305625,0.00013565786,0.0013614991],"category_scores_gemma":[0.000032662447,0.00007916839,0.000072212155,0.00037879104,0.00076332124,0.00037323718,0.000005364388,0.0004256579,0.00015389013],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005480327,0.0000037250331,0.9980777,0.000006575866,0.0000068757886,0.00007883443,0.0014025734,0.00019258665,0.000043855114,0.0000037361863,0.0000034569205,0.00012529622],"study_design_scores_gemma":[0.000544763,0.00035931313,0.99806076,0.000033910757,0.0000054150278,0.00021724297,0.00022362616,0.00025795415,0.000027764125,0.00007593931,0.00008645347,0.000106827174],"about_ca_topic_score_codex":0.011150724,"about_ca_topic_score_gemma":0.45700222,"teacher_disagreement_score":0.4458515,"about_ca_system_score_codex":0.0000013196279,"about_ca_system_score_gemma":0.00026025693,"threshold_uncertainty_score":0.9995514},"labels":[],"label_agreement":null},{"id":"W2964861330","doi":"10.1139/cjes-2018-0191","title":"Comment on “Converging ice streams: a new paradigm for reconstructions of the Laurentide Ice Sheet in southern Ontario and deposition of the Oak Ridges Moraine”","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Geological Survey of Canada","funders":"","keywords":"Moraine; Geology; Ice sheet; STREAMS; Geomorphology; Ice stream; Deposition (geology); Glacier; Earth science; Ice core; Physical geography; Paleontology; Cryosphere; Sea ice; Oceanography; Sediment","score_opus":0.02085547986785932,"score_gpt":0.21980217418525366,"score_spread":0.19894669431739434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2964861330","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896617,0.00026949387,0.0000027351573,0.008647172,0.000339811,0.00014434125,0.00003634098,4.6531164e-7,0.0008979629],"genre_scores_gemma":[0.99932015,0.000010906811,0.00018562899,0.00033505438,0.000014472611,2.0368127e-7,0.0000013098299,6.777813e-7,0.00013162052],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992502,0.00011278015,0.00021055566,0.000092914896,0.00013257732,0.00020097927],"domain_scores_gemma":[0.9993075,0.00025663487,0.00018573558,0.000090165966,0.00003945312,0.00012047026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00060949946,0.00005604008,0.00013559982,0.00013985627,0.0002175881,0.000023118711,0.00029454156,0.000039936796,0.0003525889],"category_scores_gemma":[0.00006581095,0.00003238209,0.000049400056,0.0002311324,0.0005059265,0.0001067034,0.0000051624356,0.00017467108,0.0000027318044],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014764177,0.0000026312312,0.99627054,0.0000066573334,0.000008741169,0.0000011004084,0.0010443784,0.001852189,0.0000043635514,0.00021144286,0.00005902049,0.0005241826],"study_design_scores_gemma":[0.00028969184,0.00019601618,0.99452615,0.00010643823,0.000010628074,0.000097444135,0.0018379882,0.0005866794,0.000115837436,0.0013448603,0.00084624806,0.000041999152],"about_ca_topic_score_codex":0.13318142,"about_ca_topic_score_gemma":0.9748557,"teacher_disagreement_score":0.8416743,"about_ca_system_score_codex":0.0000014690893,"about_ca_system_score_gemma":0.0012414391,"threshold_uncertainty_score":0.8725908},"labels":[],"label_agreement":null},{"id":"W2965615177","doi":"10.1139/cjes-2018-0080","title":"Salt anomalies in potash beds of the Esterhazy Member, Devonian Prairie Evaporite Formation, Saskatchewan, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"PotashCorp (Canada)","funders":"","keywords":"Evaporite; Geology; Halite; Devonian; Potash; Geochemistry; Carbonate; Anhydrite; Sedimentary rock; Paleontology; Gypsum; Potassium","score_opus":0.009338246620728118,"score_gpt":0.1828582361387798,"score_spread":0.17351998951805167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2965615177","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918348,0.0005117577,0.0000025586623,0.0010312666,0.00068981946,0.000088490255,0.000046021432,0.0000010780701,0.005794159],"genre_scores_gemma":[0.9987735,0.0000030887047,0.00018327658,0.00031029776,0.000046590758,1.2081404e-7,0.000003583186,0.0000014385635,0.0006781095],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99864113,0.00005795707,0.00040934468,0.0001157191,0.0004046329,0.00037123496],"domain_scores_gemma":[0.99913794,0.000058746144,0.00025831893,0.00014026165,0.00011716607,0.00028757425],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00064579846,0.00010099747,0.0001843792,0.00013387554,0.00016779952,0.000096718424,0.0006109078,0.000040223043,0.0008865078],"category_scores_gemma":[0.00005054765,0.00006611581,0.000053220927,0.0004922343,0.0002504448,0.0005584362,0.000007682033,0.00016103078,0.000007235392],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000029471894,0.0000014645302,0.9963857,0.00001717534,0.000003891689,0.000013818276,0.0006325953,0.0015966075,0.00005809263,0.000006976396,0.00036822565,0.0009125362],"study_design_scores_gemma":[0.00019295,0.00008831434,0.978404,0.00009071995,0.000005002895,0.00016399602,0.0030854058,0.0004724225,0.0016503916,0.00017272662,0.015561466,0.00011263597],"about_ca_topic_score_codex":0.80120397,"about_ca_topic_score_gemma":0.99947625,"teacher_disagreement_score":0.19827232,"about_ca_system_score_codex":0.000008417307,"about_ca_system_score_gemma":0.0061259223,"threshold_uncertainty_score":0.99950844},"labels":[],"label_agreement":null},{"id":"W2967192487","doi":"10.1139/cjes-2017-0251","title":"Paleomagnetism of the native copper mineralization, Keweenaw Peninsula, Michigan","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"","keywords":"Geology; Hematite; Paleomagnetism; Geochemistry; Magnetite; Sedimentary rock; Mineralization (soil science); Basalt; Bedding; Apparent polar wander; Mineralogy; Paleontology","score_opus":0.008422424969439712,"score_gpt":0.21012672322028875,"score_spread":0.20170429825084904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2967192487","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9856943,0.00384554,0.000007790403,0.0006147808,0.0006042734,0.00010550786,0.000018405752,6.871492e-7,0.009108722],"genre_scores_gemma":[0.99621433,0.00008766252,0.0002801784,0.00024171927,0.000098730685,6.648903e-7,0.0000017197486,0.0000046708014,0.0030702988],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990924,0.00006861877,0.00025456035,0.00014373299,0.00020641393,0.00023429828],"domain_scores_gemma":[0.9992108,0.000017224045,0.00022229069,0.00015596188,0.00024143668,0.00015228271],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028974595,0.000099123274,0.00014701723,0.0000990535,0.00017554924,0.00003157436,0.00043495646,0.00005506963,0.0001399499],"category_scores_gemma":[0.00012624275,0.000067054825,0.00009563423,0.00026590918,0.00054280757,0.000012422726,0.00003061862,0.00007258963,0.000005388378],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000070964006,0.0000074382365,0.95227706,0.000011695192,0.000023110788,0.0000037778084,0.0005559545,0.00035770284,0.044547964,0.00042378466,0.0016422626,0.00014217148],"study_design_scores_gemma":[0.00040466018,0.0010067876,0.94604886,0.000056031196,0.000017361648,0.00007615609,0.0005089229,0.000019254814,0.012935754,0.00015659705,0.038628183,0.00014145914],"about_ca_topic_score_codex":0.0009848304,"about_ca_topic_score_gemma":0.06373763,"teacher_disagreement_score":0.0627528,"about_ca_system_score_codex":6.934799e-7,"about_ca_system_score_gemma":0.0007532176,"threshold_uncertainty_score":0.9533467},"labels":[],"label_agreement":null},{"id":"W2967423011","doi":"10.1139/cjes-2018-0263","title":"Analysis of factors influencing the interpretation of a digitally examined fluvial meanderbelt system: Joggins Formation, Nova Scotia","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Modeling and Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Dalhousie University","keywords":"Geology; Outcrop; Fluvial; Permeameter; Channelized; Remote sensing; Mineralogy; Geomorphology; Soil science; Structural basin","score_opus":0.02055768410070642,"score_gpt":0.20522003804874003,"score_spread":0.18466235394803363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2967423011","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99665624,0.00021843213,0.001049924,0.000076768156,0.00019951591,0.000049914186,0.000032830125,0.0000022930803,0.0017140947],"genre_scores_gemma":[0.9997851,0.000003218747,0.00013448863,0.00003288474,0.000017499224,2.2370775e-8,0.0000081220205,7.6611275e-7,0.000017890288],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986693,0.000084729676,0.0005538722,0.00010792903,0.0003806836,0.00020346532],"domain_scores_gemma":[0.9987074,0.00017869905,0.0005443008,0.00010873701,0.0002784138,0.00018242218],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00095655455,0.00008388733,0.00032216642,0.0007357484,0.0001224788,0.000093237846,0.00042719615,0.000035938956,0.0004679381],"category_scores_gemma":[0.000192712,0.000046589,0.00019699315,0.0014464161,0.00022120192,0.0005355658,0.000004301371,0.00008944928,0.000011300234],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004133777,0.0000012736809,0.67222637,0.000011371738,0.00008492638,9.402119e-7,0.0010478229,0.32613134,0.000022809734,0.00002061759,0.0000025718305,0.00044582563],"study_design_scores_gemma":[0.00007186949,0.0001926265,0.7412578,0.00007666427,0.00020127326,0.0000064138917,0.0041490453,0.2538557,0.0000830177,0.000031250092,0.0000142356475,0.00006013194],"about_ca_topic_score_codex":0.037168816,"about_ca_topic_score_gemma":0.4475116,"teacher_disagreement_score":0.4103428,"about_ca_system_score_codex":0.0000030591445,"about_ca_system_score_gemma":0.00040777912,"threshold_uncertainty_score":0.96924275},"labels":[],"label_agreement":null},{"id":"W2968196643","doi":"10.1139/cjes-2019-0048","title":"Evidence for early glaciation of southeastern Beringia","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Glacial period; Pleistocene; Plateau (mathematics); Cirque; Glacier; Beringia; Paleontology; Deglaciation; Moraine; Geomorphology; Ice sheet; Lithology; Outwash plain; Physical geography; Geography","score_opus":0.06481439551916236,"score_gpt":0.2719653615731788,"score_spread":0.20715096605401645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2968196643","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99592936,0.0012986893,0.00004871207,0.00036747972,0.00048367155,0.00010347926,0.000011578853,0.000001170332,0.0017558665],"genre_scores_gemma":[0.9990333,0.000013280473,0.0006502449,0.000043306365,0.000042074622,1.3058711e-7,8.521982e-7,7.9474916e-7,0.00021603251],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991168,0.00006217414,0.0002292342,0.00010502036,0.00018249963,0.00030427662],"domain_scores_gemma":[0.9989418,0.0004084462,0.00018325639,0.00007111293,0.00015723422,0.00023817796],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013024036,0.000054317148,0.00015381142,0.00026400908,0.00014423385,0.0000376316,0.00035680563,0.00005335286,0.0011397249],"category_scores_gemma":[0.00027945059,0.00004173506,0.00006245451,0.00023224135,0.00034213,0.0003586285,0.000002435408,0.000102521895,0.000102433085],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020476004,8.634521e-7,0.9985773,0.00001314757,0.000006298681,0.000003991613,0.00026246562,0.0006815957,0.000013597132,0.000084494946,0.000004408075,0.000331361],"study_design_scores_gemma":[0.00013201323,0.0005706259,0.99729806,0.00007535126,0.0000057104303,0.00004938521,0.00016525203,0.00082892505,0.00009311153,0.00054063066,0.00019322659,0.000047719455],"about_ca_topic_score_codex":0.0029604738,"about_ca_topic_score_gemma":0.22715499,"teacher_disagreement_score":0.22419451,"about_ca_system_score_codex":1.3774388e-7,"about_ca_system_score_gemma":0.0009123808,"threshold_uncertainty_score":0.9997734},"labels":[],"label_agreement":null},{"id":"W2968880354","doi":"10.1139/cjes-2018-0291","title":"Paleomagnetism and rock magnetism of East and West Clearwater Lake impact structures","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"Agence Nationale de la Recherche","keywords":"Geology; Impact structure; Radiometric dating; Paleomagnetism; Basement; Earth's magnetic field; Geochemistry; Breccia; Drilling; Paleontology; Seismology; Petrology; Impact crater; Magnetic field","score_opus":0.010652236688216658,"score_gpt":0.20226156120897112,"score_spread":0.19160932452075446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2968880354","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99836683,0.0002644151,0.0000186966,0.00017809974,0.00012152337,0.000037738846,0.0000346305,5.5520803e-7,0.0009774787],"genre_scores_gemma":[0.9996289,0.000006341132,0.00018436066,0.00002534173,0.000057573943,7.661923e-8,0.0000036851875,0.000001449311,0.00009228432],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99947333,0.000016411064,0.00013595837,0.000087253204,0.00011600728,0.00017105043],"domain_scores_gemma":[0.999552,0.000013196007,0.000101754165,0.000044301934,0.000035453235,0.0002532806],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001720344,0.0000613473,0.00011138334,0.00013137938,0.00009833459,0.000104469524,0.00011236921,0.000014961163,0.0009622027],"category_scores_gemma":[0.00000323095,0.000042759813,0.000023514633,0.000109111,0.00012774885,0.0005323604,0.000006187944,0.00006542795,0.000013619099],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000024099616,0.0000013260923,0.99553263,0.0000025898303,0.0000047706135,0.0000026075293,0.00047657988,0.0006473343,0.0006537508,0.0003525906,0.00006365549,0.0022597383],"study_design_scores_gemma":[0.00014533274,0.00040589183,0.99552196,0.000019687322,0.000005373983,0.00003236585,0.00054369913,0.00054350623,0.000066675035,0.0014327277,0.0012171805,0.00006557116],"about_ca_topic_score_codex":0.002305848,"about_ca_topic_score_gemma":0.021594066,"teacher_disagreement_score":0.01928822,"about_ca_system_score_codex":6.027148e-7,"about_ca_system_score_gemma":0.00026642953,"threshold_uncertainty_score":0.99995106},"labels":[],"label_agreement":null},{"id":"W2969042580","doi":"10.1139/cjes-2019-0016","title":"Reply to the comment by H.A.J. Russell on “Converging ice streams: a new paradigm for reconstructions of the Laurentide Ice Sheet in southern Ontario and deposition of the Oak Ridges Moraine”","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"The Scarborough Hospital","funders":"","keywords":"Geology; Ice sheet; STREAMS; Deposition (geology); Geomorphology; Ice stream; Greenland ice sheet; Paleontology; Oceanography; Physical geography; Sea ice; Cryosphere; Sediment","score_opus":0.01680868467421404,"score_gpt":0.2166436778631448,"score_spread":0.19983499318893078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2969042580","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9700965,0.00034038114,0.00000436901,0.028217401,0.00033064708,0.00022331103,0.000064449174,5.4700814e-7,0.0007223449],"genre_scores_gemma":[0.99821997,0.000012607067,0.00012360081,0.0013336095,0.000017295975,4.4581313e-7,0.0000017555075,8.912498e-7,0.0002898491],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99912125,0.00014587231,0.00023181784,0.000115146286,0.00015824758,0.00022767087],"domain_scores_gemma":[0.9991802,0.00031619464,0.000183305,0.00013480734,0.000042046697,0.00014347266],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008591693,0.00006413721,0.00013518082,0.000110640634,0.00030748933,0.00003439954,0.00042673454,0.00003383245,0.0002610628],"category_scores_gemma":[0.00008726993,0.000032632073,0.00004938053,0.00029585988,0.00042012916,0.00009299119,0.0000074800546,0.00019369966,0.0000046710625],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019296229,0.0000028566824,0.9945296,0.000004563485,0.0000093647905,7.363052e-7,0.0016581832,0.0024233947,0.0000073374913,0.00009219953,0.00068711396,0.0005653631],"study_design_scores_gemma":[0.0003036905,0.00032694198,0.98531795,0.00011924408,0.000015742198,0.00011634495,0.0034022538,0.0005399335,0.00023404634,0.00072902895,0.008831279,0.000063544474],"about_ca_topic_score_codex":0.18954898,"about_ca_topic_score_gemma":0.96356857,"teacher_disagreement_score":0.7740196,"about_ca_system_score_codex":0.0000018973142,"about_ca_system_score_gemma":0.000985543,"threshold_uncertainty_score":0.8158479},"labels":[],"label_agreement":null},{"id":"W2969740865","doi":"10.1139/cjes-2019-0006","title":"Geochronology, geochemistry, and Pb–Hf isotopes of mineralization-related magmatism in the Dongyang gold deposit, Fujian Province, southeastern China","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"China Geological Survey","keywords":"Geology; Geochemistry; Diorite; Rhyolite; Zircon; Mineralization (soil science); Geochronology; Magmatism; Volcanic rock; Volcano; Tectonics","score_opus":0.00640753233374789,"score_gpt":0.1751319624923464,"score_spread":0.1687244301585985,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2969740865","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98958975,0.00195347,0.00000549105,0.0013680038,0.00007606255,0.00008294339,0.000019246609,0.0000016760854,0.006903371],"genre_scores_gemma":[0.99936897,0.000033427412,0.00025447743,0.00012821284,0.0000241675,1.6111098e-7,0.0000067471324,8.551786e-7,0.00018298892],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99890774,0.00007941166,0.00035360243,0.00016153946,0.00020649606,0.00029122597],"domain_scores_gemma":[0.999361,0.00008401531,0.00021195176,0.00009441331,0.000047456455,0.00020121105],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00056180207,0.00010064598,0.00021770253,0.00017312057,0.00009652441,0.00008010809,0.00044584085,0.000063740976,0.0019276715],"category_scores_gemma":[0.0000780191,0.000057521913,0.000060723716,0.00047403967,0.0005097565,0.00018875234,0.000008272269,0.00016626889,0.000017490103],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003393366,0.0000052139494,0.99632007,0.00001329663,0.00000908157,0.00002145901,0.00033570244,0.0012470367,0.00027072497,0.00009532991,0.000021967635,0.0016567046],"study_design_scores_gemma":[0.0001735344,0.0001858901,0.9921725,0.000052376265,0.000015032518,0.00013066563,0.0005217235,0.003666066,0.00019661471,0.0025167742,0.00027901217,0.00008984115],"about_ca_topic_score_codex":0.080733664,"about_ca_topic_score_gemma":0.6088816,"teacher_disagreement_score":0.52814794,"about_ca_system_score_codex":8.5567154e-7,"about_ca_system_score_gemma":0.0002396697,"threshold_uncertainty_score":0.9989847},"labels":[],"label_agreement":null},{"id":"W2969926702","doi":"10.1139/cjes-2019-0014","title":"Zircon U–Pb and molybdenite Re–Os dating and geological implications of the Shimadong porphyry molybdenum deposit in eastern Yanbian, northeastern China","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Zircon; Porphyritic; Molybdenite; Geology; Geochemistry; Craton; Mineralization (soil science); Diorite; Lithophile; Titanite; Crust; Partial melting; Geochronology; Underplating; Isochron; Subduction; Tectonics; Quartz; Fluid inclusions","score_opus":0.01599358585819971,"score_gpt":0.1961095029469626,"score_spread":0.1801159170887629,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2969926702","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995023,0.0008425848,0.000014922551,0.0019467531,0.0000690494,0.00008655127,0.000015883994,0.0000013764087,0.0019998795],"genre_scores_gemma":[0.9993509,0.000021559263,0.00023852359,0.0002729048,0.000022611623,1.5635803e-7,0.0000017054841,9.454628e-7,0.000090695234],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989136,0.00007921327,0.00033003875,0.00020055639,0.00018996077,0.00028667113],"domain_scores_gemma":[0.9992202,0.00011946505,0.00021269098,0.000112666385,0.000047252255,0.00028771712],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00044107233,0.000096899385,0.00022428803,0.00015069061,0.00015362343,0.00007894714,0.00037147914,0.000051367973,0.00094272115],"category_scores_gemma":[0.00009504655,0.000056256435,0.000058530135,0.00045905646,0.00043421754,0.00026690817,0.000025516878,0.00019549034,0.00001086067],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003868581,0.000003186097,0.9958172,0.000007626993,0.000005558242,0.0000061861056,0.00011524044,0.0015629004,0.00056926307,0.00003882715,0.0000017270933,0.0018684329],"study_design_scores_gemma":[0.00012562373,0.00013018724,0.99452734,0.000050464652,0.000011230216,0.000092172246,0.00025664805,0.0028709609,0.00021558709,0.0015945033,0.000047745092,0.00007755541],"about_ca_topic_score_codex":0.02690326,"about_ca_topic_score_gemma":0.314116,"teacher_disagreement_score":0.28721276,"about_ca_system_score_codex":0.0000011387947,"about_ca_system_score_gemma":0.00014159032,"threshold_uncertainty_score":0.99997056},"labels":[],"label_agreement":null},{"id":"W2969948016","doi":"10.1139/cjes-2018-0179","title":"Petrophysical constraints on magnetic anomalies associated with metamorphic reactions in northern Saskatchewan, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Petrography; Hornblende; Mylonite; Geochemistry; Natural remanent magnetization; Shear zone; Paleomagnetism; Magnetite; Magnetic anomaly; Petrology; Mineralogy; Remanence; Geophysics; Magnetization; Seismology; Biotite; Magnetic field; Paleontology","score_opus":0.007475027974284002,"score_gpt":0.18721307439691054,"score_spread":0.17973804642262653,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2969948016","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948311,0.00057942595,0.000001937703,0.00038193003,0.00025140832,0.00007591418,0.000023096714,9.495251e-7,0.003854264],"genre_scores_gemma":[0.9984543,0.000011200434,0.00007203544,0.00018322591,0.000049754373,0.0000012625384,0.00000414248,0.0000055076407,0.0012186072],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99900216,0.00006147271,0.00020473472,0.00017921525,0.00022196301,0.00033044812],"domain_scores_gemma":[0.999391,0.0000348126,0.00013084563,0.00010655356,0.00011279071,0.0002240046],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020787423,0.00011941159,0.00017948767,0.0001233393,0.0001261827,0.00003711735,0.00020220477,0.000043725395,0.00012302956],"category_scores_gemma":[0.00008625527,0.00009328992,0.000040487113,0.00024336371,0.00045137716,0.000009568579,0.000008432242,0.00013300867,0.0000050735466],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021556545,0.000021109681,0.99267066,0.000005530201,0.000034539302,0.00015761668,0.00014729623,0.0013978418,0.0039016267,0.000034016157,0.00024525545,0.001362982],"study_design_scores_gemma":[0.0005055154,0.002406926,0.9911764,0.00007197152,0.000012396706,0.00008264368,0.001603022,0.0000144651685,0.0005306947,0.00001969791,0.0034023288,0.00017394083],"about_ca_topic_score_codex":0.18132004,"about_ca_topic_score_gemma":0.9987471,"teacher_disagreement_score":0.8174271,"about_ca_system_score_codex":0.000010561842,"about_ca_system_score_gemma":0.0038385333,"threshold_uncertainty_score":0.8241316},"labels":[],"label_agreement":null},{"id":"W2972469354","doi":"10.1139/cjes-2018-0326","title":"New embolomerous tetrapod material and a faunal overview of the Mississippian-aged Point Edward locality, Nova Scotia, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Tetrapod (structure); Postcrania; Paleontology; Carboniferous; Taxon; Fauna; Vertebrate; Geology; Geography; Biology; Ecology; Structural basin","score_opus":0.020547401941322038,"score_gpt":0.2173152513785238,"score_spread":0.19676784943720177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2972469354","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9898344,0.0036582726,0.0000063659995,0.001903216,0.0022151864,0.0000759617,0.000091632275,0.0000011722958,0.0022137424],"genre_scores_gemma":[0.9989378,0.0000242826,0.0002686816,0.00052343233,0.000096910786,1.7377635e-8,0.0000020483947,9.80455e-7,0.00014583493],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987797,0.00014477599,0.00032190923,0.00015593231,0.00023861788,0.00035906813],"domain_scores_gemma":[0.99904084,0.00009374306,0.00022657153,0.000109578774,0.000051249037,0.00047802113],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00058841065,0.00010413102,0.00025038174,0.000110967194,0.00021122933,0.000036526304,0.00047599076,0.000069432754,0.004505102],"category_scores_gemma":[0.00007619132,0.000065147615,0.000055911147,0.00029748253,0.00059618236,0.0001929913,0.000008480557,0.00016545934,0.000011171736],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016307331,0.00000137272,0.9969327,0.000011357789,0.000014826189,0.000020100255,0.00006676549,0.00028433892,0.000054037155,0.00007273258,0.0009231019,0.001602345],"study_design_scores_gemma":[0.00018058847,0.00020283592,0.995206,0.00005633015,0.000011814258,0.0004842776,0.00016796224,0.00008330366,0.00009502068,0.00038489187,0.003041623,0.00008533434],"about_ca_topic_score_codex":0.9106319,"about_ca_topic_score_gemma":0.998422,"teacher_disagreement_score":0.08779009,"about_ca_system_score_codex":0.000003978634,"about_ca_system_score_gemma":0.0052311104,"threshold_uncertainty_score":0.9964049},"labels":[],"label_agreement":null},{"id":"W2972569833","doi":"10.1139/cjes-2019-0121","title":"Syn-accretionary multistage assembly of an Early Jurassic Alaskan-type intrusion in the Canadian Cordillera: U–Pb and <sup>40</sup>Ar/<sup>39</sup>Ar geochronology of the Turnagain ultramafic–mafic intrusive complex, Yukon–Tanana terrane","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Pacific Institute for the Mathematical Sciences","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochronology; Zircon; Mafic; Geochemistry; Phlogopite; Ultramafic rock; Terrane; Hornblende; Paleontology; Biotite; Mantle (geology); Tectonics","score_opus":0.015498111273280336,"score_gpt":0.20688669002052887,"score_spread":0.19138857874724854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2972569833","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99381256,0.0006549644,0.0000021051471,0.00325216,0.00014995005,0.00024315438,0.00014032151,0.0000031211637,0.001741675],"genre_scores_gemma":[0.99878997,0.000050083298,0.00030230638,0.00067889795,0.000075523356,5.018122e-7,0.000030665473,0.0000037040675,0.00006836948],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971072,0.000466402,0.0007235141,0.0003851589,0.0005935419,0.00072414614],"domain_scores_gemma":[0.9978465,0.0004201114,0.00044880153,0.00030551132,0.000270559,0.0007085536],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012385838,0.00025252238,0.0005721915,0.00056218146,0.00054261537,0.0001455518,0.001248147,0.00017888332,0.004001427],"category_scores_gemma":[0.00037270915,0.00014449852,0.00015082805,0.0013928756,0.0016782563,0.00042903642,0.000026933425,0.0005566357,0.000021131771],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006138994,0.000028451579,0.9627291,0.000026696005,0.000055413653,0.00012582369,0.0019481037,0.02883602,0.0010648037,0.00018851874,0.00013509112,0.004800586],"study_design_scores_gemma":[0.00035308633,0.0008534653,0.96537244,0.000084771986,0.000040055977,0.00016255768,0.0026572002,0.028476467,0.00015854332,0.0007623583,0.0008746855,0.00020438814],"about_ca_topic_score_codex":0.48948866,"about_ca_topic_score_gemma":0.92200017,"teacher_disagreement_score":0.4325115,"about_ca_system_score_codex":0.000016664504,"about_ca_system_score_gemma":0.0014481673,"threshold_uncertainty_score":0.996909},"labels":[],"label_agreement":null},{"id":"W2973273762","doi":"10.1139/cjes-2019-0102","title":"Introduction for the David W. Strangway Special Issue","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Contemporary Sociological Theory and Practice","field":"Social Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"","keywords":"Geology; Geochemistry","score_opus":0.0529419004747352,"score_gpt":0.3161407387425987,"score_spread":0.2631988382678635,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2973273762","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4163878,0.0021525214,0.00028203387,0.26850682,0.022105958,0.0008271616,0.00002218595,0.000011911816,0.2897036],"genre_scores_gemma":[0.9722434,0.00005787949,0.00020290822,0.00059405004,0.017780581,7.97288e-7,3.4430627e-7,0.0000019643248,0.009118065],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990579,0.00023371009,0.00016311514,0.00009796091,0.00020364445,0.00024367654],"domain_scores_gemma":[0.9985463,0.0008584589,0.00016655131,0.00006626919,0.00013862048,0.00022380428],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.005029032,0.000046902318,0.00009807667,0.000065544904,0.0011660759,0.00019829317,0.0004365403,0.00004741295,0.0065312344],"category_scores_gemma":[0.0012390118,0.00002939951,0.000082096376,0.00026604292,0.0008092961,0.000635381,0.0000037164186,0.00015911461,0.00009220284],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018021719,0.00002878486,0.03995816,0.000012797551,0.00008745143,0.00002398497,0.044871192,0.00081183587,0.00018439839,0.7258578,0.11499491,0.07298844],"study_design_scores_gemma":[0.00007938169,0.00017852122,0.0031849835,0.000004650446,0.000007303637,0.0000052097485,0.009767292,0.000006652671,0.000015723712,0.0067901597,0.9799137,0.00004638355],"about_ca_topic_score_codex":0.0019343933,"about_ca_topic_score_gemma":0.047814112,"teacher_disagreement_score":0.8649188,"about_ca_system_score_codex":0.000008080709,"about_ca_system_score_gemma":0.0015063119,"threshold_uncertainty_score":0.99437696},"labels":[],"label_agreement":null},{"id":"W2973678622","doi":"10.1139/cjes-2019-0083","title":"My lifelong dear friend David Strangway","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Nursing Education, Practice, and Leadership","field":"Nursing","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Archaeology; Geochemistry; History","score_opus":0.0357974905428483,"score_gpt":0.2940351052937346,"score_spread":0.2582376147508863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2973678622","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9642286,0.0009917347,0.000013324227,0.018201921,0.0068769846,0.000075726864,0.0000027657507,0.000005808873,0.009603176],"genre_scores_gemma":[0.99681616,0.000003175315,0.00094790384,0.0009143581,0.0005675912,1.9617175e-7,7.0428536e-7,0.000007903562,0.0007419807],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987385,0.00010095325,0.00024505227,0.00015383011,0.00034015122,0.00042149666],"domain_scores_gemma":[0.9987623,0.00014583797,0.00022355725,0.0001310852,0.00014632486,0.0005909037],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011975267,0.00009079351,0.00014144416,0.00037981183,0.00036331633,0.00033737934,0.00041456133,0.000053232736,0.0006738173],"category_scores_gemma":[0.00024237807,0.00007912939,0.00006473752,0.00043020953,0.0003360673,0.00089996273,0.0000012005706,0.00027073914,0.00018098399],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008822056,0.00006469499,0.92529076,0.000056512625,0.000040891653,0.00006315113,0.04421832,0.00054789655,0.0018161699,0.0021083641,0.013573084,0.012131921],"study_design_scores_gemma":[0.0006322148,0.0011167006,0.53563976,0.0003583344,0.000062951236,0.0005766953,0.02859172,0.00010473908,0.0021955387,0.0017100031,0.42861655,0.00039480365],"about_ca_topic_score_codex":0.0029112657,"about_ca_topic_score_gemma":0.02971055,"teacher_disagreement_score":0.41504347,"about_ca_system_score_codex":0.000018218296,"about_ca_system_score_gemma":0.001932909,"threshold_uncertainty_score":0.98799473},"labels":[],"label_agreement":null},{"id":"W2979592242","doi":"10.1139/cjes-2019-0089","title":"A taphonomic analysis of a multitaxic bonebed from the St. Mary River Formation (uppermost Campanian to lowermost Maastrichtian) of Alberta, dominated by cf. <i>Edmontosaurus regalis</i> (Ornithischia: Hadrosauridae), with significant remains of <i>Pachyrhinosaurus canadensis</i> (Ornithischia: Ceratopsidae)","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University; University of Calgary","funders":"","keywords":"Taphonomy; Geology; Paleontology; Butte; Subaerial; Cretaceous; Fauna; Ecology","score_opus":0.005736289154418194,"score_gpt":0.17570437663534663,"score_spread":0.16996808748092843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979592242","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99281156,0.001364061,0.000072217954,0.0016195779,0.0003374588,0.00033265,0.0024337294,0.0000031828101,0.0010255818],"genre_scores_gemma":[0.99830884,0.000035934205,0.0008391138,0.0005119322,0.000035945355,9.670629e-7,0.00016790775,0.0000049584323,0.00009439559],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971612,0.0003774639,0.0010063048,0.0003718874,0.00047254926,0.0006105996],"domain_scores_gemma":[0.99691105,0.0006001239,0.0011960672,0.00036313894,0.0003410377,0.0005885779],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009942522,0.00027724274,0.0008646101,0.0007943335,0.00033890828,0.000041658368,0.00087782094,0.00017723853,0.00091849867],"category_scores_gemma":[0.00019351803,0.00018415108,0.00021725197,0.0020593766,0.0013180078,0.0006512691,0.000014948915,0.00034626422,0.000018142497],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030444108,0.000020873156,0.9861714,0.000011979395,0.0004017552,0.000035239,0.0020160426,0.0066393246,0.0026877222,0.00003054749,0.0014148544,0.00026579213],"study_design_scores_gemma":[0.0006869083,0.00085414265,0.9912356,0.00010745713,0.00039646812,0.00008677005,0.001776373,0.002142269,0.0009811466,0.000034210578,0.0014499913,0.00024862625],"about_ca_topic_score_codex":0.4054191,"about_ca_topic_score_gemma":0.9544128,"teacher_disagreement_score":0.5489937,"about_ca_system_score_codex":0.000017630642,"about_ca_system_score_gemma":0.0021073418,"threshold_uncertainty_score":0.9999948},"labels":[],"label_agreement":null},{"id":"W2979872101","doi":"10.1139/cjes-2019-0019","title":"High-precision U–Pb CA–ID–TIMS dating and chronostratigraphy of the dinosaur-rich Horseshoe Canyon Formation (Upper Cretaceous, Campanian–Maastrichtian), Red Deer River valley, Alberta, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Royal Tyrrell Museum","funders":"Government of Alberta","keywords":"Geology; Paleontology; Chronostratigraphy; Cretaceous; Marine transgression; Canyon; Zircon; Geomorphology; Structural basin","score_opus":0.007812715335659543,"score_gpt":0.1794614403365904,"score_spread":0.17164872500093084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979872101","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936311,0.0016600173,0.000019362771,0.0010146878,0.0011405477,0.00013539725,0.00009462527,0.0000014057453,0.0023028112],"genre_scores_gemma":[0.9989173,0.00005539189,0.00063579064,0.00018484323,0.00006622599,2.0241936e-7,0.000014960877,0.0000014980185,0.00012381721],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99848574,0.00017191132,0.00041585974,0.00019278769,0.00031507222,0.00041861617],"domain_scores_gemma":[0.9987347,0.0002777774,0.00039237362,0.00014110017,0.00011901369,0.00033499746],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005411674,0.00013907066,0.00024651518,0.00021982194,0.00050207344,0.00004230074,0.0004641509,0.00009852512,0.0013810524],"category_scores_gemma":[0.00016235355,0.00009034181,0.000053330863,0.0004539314,0.00056442455,0.0005711753,0.000009384885,0.00022267268,0.0000091373095],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011709319,0.0000017327832,0.99493444,0.0000073775395,0.000015802947,0.000008017938,0.00022792399,0.0027157778,0.000082855615,0.000044295157,0.0008231227,0.0011269592],"study_design_scores_gemma":[0.00019740079,0.00023101583,0.9925531,0.000049229297,0.000019409135,0.00022109301,0.00038298772,0.0019161865,0.00012338813,0.00017135283,0.0040151854,0.00011963288],"about_ca_topic_score_codex":0.8213877,"about_ca_topic_score_gemma":0.99778295,"teacher_disagreement_score":0.17639525,"about_ca_system_score_codex":0.000008559121,"about_ca_system_score_gemma":0.0024041794,"threshold_uncertainty_score":0.9995318},"labels":[],"label_agreement":null},{"id":"W2980895292","doi":"10.1139/cjes-2019-0100","title":"Localisation of the brittle Bathurst fault on pre-existing fabrics: a case for structural inheritance in the northeastern Slave craton, western Nunavut, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Queen's University","funders":"","keywords":"Geology; Hornblende; Craton; Zircon; Fault (geology); Geochemistry; Geochronology; Shear zone; Batholith; Basement; Tectonics; Seismology; Quartz; Biotite; Paleontology; Archaeology","score_opus":0.02074874625112035,"score_gpt":0.21527924835027204,"score_spread":0.19453050209915168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980895292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974922,0.0002518871,0.000008566297,0.0012700191,0.00024309527,0.00013301507,0.000074327894,6.726288e-7,0.0005262125],"genre_scores_gemma":[0.9992583,0.0000015262533,0.00006829862,0.00056157605,0.000055135148,3.2018565e-7,0.0000023781477,8.878541e-7,0.000051580748],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99884343,0.00008334205,0.0003097452,0.0001383318,0.0003261674,0.0002990005],"domain_scores_gemma":[0.99910456,0.00028120112,0.00023591421,0.00010553289,0.00011152876,0.00016126728],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005699792,0.00008758359,0.00016416075,0.00006344109,0.00022655749,0.00007372171,0.00048044152,0.000029532739,0.00029120134],"category_scores_gemma":[0.00021141462,0.00004339233,0.00007227483,0.00044798394,0.00023256686,0.00013239673,0.0000044869294,0.00015395496,0.0000020629484],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008193212,0.0000015891756,0.9749572,0.000007920772,0.0000044982817,0.000046476678,0.00037233296,0.022222763,0.00000757202,0.000020742458,0.000015236469,0.002335454],"study_design_scores_gemma":[0.0001654202,0.00018793855,0.98063594,0.00005794809,0.0000110395595,0.0003309617,0.0014035315,0.015377218,0.000082399034,0.0010005232,0.00065659714,0.00009046909],"about_ca_topic_score_codex":0.77829427,"about_ca_topic_score_gemma":0.99911034,"teacher_disagreement_score":0.22081608,"about_ca_system_score_codex":0.0000049477044,"about_ca_system_score_gemma":0.0008344069,"threshold_uncertainty_score":0.31884506},"labels":[],"label_agreement":null},{"id":"W2981093131","doi":"10.1139/cjes-2019-0031","title":"Cretaceous flora and fauna of the Sustut Group near the Sustut River, northern British Columbia, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Royal Tyrrell Museum; Royal Ontario Museum; Royal British Columbia Museum","funders":"","keywords":"Geology; Paleontology; Genus; Fauna; Outcrop; Type locality; Vertebrate; Cretaceous; Range (aeronautics); Turtle (robot); Taxon; Ecology; Biology","score_opus":0.006040536870615965,"score_gpt":0.15968512314314182,"score_spread":0.15364458627252586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981093131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893833,0.00617197,9.338612e-7,0.0009310005,0.0012251085,0.00010334751,0.00007689966,0.0000012124201,0.0021062305],"genre_scores_gemma":[0.99890053,0.00005442179,0.000045093486,0.00041564266,0.00006157485,1.0805449e-7,0.0000018011139,0.000001075222,0.00051973603],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99884665,0.00015669774,0.00023979765,0.00014616865,0.0002371272,0.00037353806],"domain_scores_gemma":[0.9991293,0.00018229285,0.00020316041,0.00012040509,0.00010565155,0.000259167],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00063057884,0.00006973244,0.00017842857,0.00003215061,0.0010305697,0.00016260541,0.0006186445,0.000059314323,0.00084988395],"category_scores_gemma":[0.0001145905,0.000052208557,0.0000528609,0.0002803833,0.0024503013,0.00018914363,0.000009733101,0.00020991212,0.000006452278],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000035672726,0.0000012255259,0.99622875,0.0000034259588,0.000013004055,0.000040985364,0.00015183284,0.0005380327,0.0000016311842,0.000011696682,0.0005533411,0.002452507],"study_design_scores_gemma":[0.0001295379,0.00016636934,0.97197276,0.000020960668,0.000010562886,0.0006569383,0.00062227075,0.0004491516,6.646843e-7,0.00025852956,0.02564079,0.000071470895],"about_ca_topic_score_codex":0.9875038,"about_ca_topic_score_gemma":0.9999813,"teacher_disagreement_score":0.025087448,"about_ca_system_score_codex":0.0000043199116,"about_ca_system_score_gemma":0.004303619,"threshold_uncertainty_score":0.93056333},"labels":[],"label_agreement":null},{"id":"W2981651832","doi":"10.1139/cjes-2019-0073","title":"Cranial variation in <i>Gryposaurus</i> and biostratigraphy of hadrosaurines (Ornithischia: Hadrosauridae) from the Dinosaur Park Formation of Alberta, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; University of Toronto","funders":"","keywords":"Biostratigraphy; Paleontology; Morphometrics; Skull; Biology; Ontogeny; Geology; Taxon; Zoology","score_opus":0.0071791645983303246,"score_gpt":0.17121316957615795,"score_spread":0.16403400497782764,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981651832","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99536735,0.0011641624,0.000010980327,0.0015466855,0.0005355194,0.000083504296,0.000120496334,5.7106456e-7,0.0011707594],"genre_scores_gemma":[0.9995064,0.000044457214,0.00020768994,0.00017509724,0.00004682142,1.0103429e-7,0.000009786914,6.550378e-7,0.00000895889],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895626,0.0001288554,0.00040829688,0.00011158754,0.00017865223,0.0002163157],"domain_scores_gemma":[0.9989419,0.00043654875,0.00034430993,0.00007639505,0.000068608286,0.00013221907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005110075,0.00008290279,0.0002042446,0.00015722086,0.000141492,0.000017847015,0.00027311634,0.00006424645,0.00027790194],"category_scores_gemma":[0.00010709442,0.000054914704,0.000036025638,0.0003217483,0.00044169487,0.0003902332,0.000003020282,0.00013328345,0.0000019988731],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002020611,0.0000023860287,0.9981483,0.0000059125928,0.000007803639,0.0000037498803,0.00040112808,0.0006642125,0.0001466108,0.00015729053,0.00009709949,0.00034530592],"study_design_scores_gemma":[0.0002245919,0.00017136967,0.9964811,0.000038693943,0.000008983993,0.000043886936,0.0003133507,0.0011138109,0.00011134624,0.00047983197,0.0009503952,0.00006263951],"about_ca_topic_score_codex":0.92974347,"about_ca_topic_score_gemma":0.999453,"teacher_disagreement_score":0.06970953,"about_ca_system_score_codex":0.0000018213246,"about_ca_system_score_gemma":0.0015848444,"threshold_uncertainty_score":0.30428314},"labels":[],"label_agreement":null},{"id":"W2982099614","doi":"10.1139/cjes-2019-0088","title":"Early–Middle Permian post-collisional granitoids in the northern Beishan orogen, northwestern China: evidence from U–Pb ages and Sr–Nd–Hf isotopes","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China; National Science Foundation","keywords":"Zircon; Geology; Geochemistry; Crust; Lithophile; Paleozoic; Partial melting; Pluton; Permian; Paleontology; Tectonics","score_opus":0.01836980449331271,"score_gpt":0.19462499625150467,"score_spread":0.17625519175819196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982099614","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99268186,0.0043075727,0.0000015782316,0.0022676205,0.00018465453,0.00010491628,0.00007781481,0.0000027766807,0.00037118173],"genre_scores_gemma":[0.99895215,0.00010461136,0.00018279674,0.00055552274,0.0001240644,3.6397145e-7,0.000010079621,0.0000016225441,0.00006878623],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99825567,0.00014865772,0.0003556251,0.0002916064,0.0005051205,0.00044334796],"domain_scores_gemma":[0.9987343,0.00037732365,0.0001691323,0.00013837148,0.00011634102,0.0004645112],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008443426,0.00015885824,0.00027172122,0.00021101738,0.00034884395,0.00033283717,0.0008232951,0.0000662809,0.0027563218],"category_scores_gemma":[0.00018413429,0.00008772382,0.0001159201,0.00061832217,0.0004996447,0.0005981424,0.000014211568,0.0002937594,0.000112344984],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010657055,0.0000052356286,0.9951834,0.0000032378834,0.000009926047,0.00008447134,0.0011009476,0.00067142386,0.000078349876,0.0000067196033,0.0000063902758,0.0028392118],"study_design_scores_gemma":[0.00012735838,0.00038630926,0.9960334,0.000093357135,0.000016972568,0.000061805215,0.00086010003,0.00037759735,0.00003877151,0.0015283859,0.00033745397,0.0001384924],"about_ca_topic_score_codex":0.29250047,"about_ca_topic_score_gemma":0.9512347,"teacher_disagreement_score":0.6587342,"about_ca_system_score_codex":0.0000021226483,"about_ca_system_score_gemma":0.00038249366,"threshold_uncertainty_score":0.9981553},"labels":[],"label_agreement":null},{"id":"W2983064582","doi":"10.1139/cjes-2019-0143","title":"Appreciation of A.M. Celâl Şengör","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Marine and environmental studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Phanerozoic; Rift; Paleontology; Mantle (geology); Continental margin; Continental drift; Earth science; Geophysics; Tectonics; Cenozoic; Structural basin","score_opus":0.012093078183939412,"score_gpt":0.16739752241497619,"score_spread":0.1553044442310368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2983064582","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9377355,0.00066283817,0.0000057958587,0.00017708738,0.00041120948,0.000034713346,0.0000090325575,8.095152e-7,0.06096302],"genre_scores_gemma":[0.99905384,0.000047068905,0.00035164054,0.00007482027,0.00005010802,2.1956993e-8,0.0000010490237,6.0893194e-7,0.0004208397],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999354,0.000020934674,0.0001788925,0.000069576294,0.0002024985,0.0001740883],"domain_scores_gemma":[0.99956393,0.000044162072,0.0001454839,0.000046366895,0.000022205277,0.00017787785],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004034908,0.000048649228,0.00011660365,0.00013038209,0.00010520129,0.00002700435,0.00018821281,0.000018758876,0.004679377],"category_scores_gemma":[0.000031325148,0.00003533247,0.000042842657,0.00019501716,0.00018214458,0.0002389492,0.000003149287,0.000058396785,0.0000974273],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000018084697,0.0000011502045,0.98971415,0.0000035207197,0.000004800448,0.0000028222269,0.00012281473,0.0023886461,0.000017279654,0.000035268495,0.00013627624,0.0075714434],"study_design_scores_gemma":[0.000077485194,0.00023443256,0.98268634,0.000013571015,0.0000038090784,0.000014450518,0.00036478092,0.00037341897,0.0001305546,0.00023733276,0.015815776,0.00004804948],"about_ca_topic_score_codex":0.015550678,"about_ca_topic_score_gemma":0.18231395,"teacher_disagreement_score":0.16676326,"about_ca_system_score_codex":9.5280166e-7,"about_ca_system_score_gemma":0.00020722237,"threshold_uncertainty_score":0.9962305},"labels":[],"label_agreement":null},{"id":"W2984196254","doi":"10.1139/cjes-2019-0054","title":"The nature and origin of furrows in lake-bed sediments: Okanagan Lake, British Columbia, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia, Okanagan Campus; Okanagan University College; Okanagan College","funders":"","keywords":"Geology; Sediment; Deposition (geology); Structural basin; Geomorphology; Sediment transport; Beach morphodynamics; Waves and shallow water; Tension (geology); Paleontology; Sonar; Oceanography","score_opus":0.007510293351919106,"score_gpt":0.18381055190395693,"score_spread":0.17630025855203782,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2984196254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911047,0.0026215848,2.3614281e-7,0.0005129989,0.0004626557,0.00006459564,0.00010470429,7.984316e-7,0.0051276907],"genre_scores_gemma":[0.99907863,0.000103697756,0.000082172206,0.0002983039,0.000022399125,9.27088e-8,0.0000034430911,6.189514e-7,0.00041063924],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99911416,0.000038669878,0.00024823318,0.00008796936,0.0002469487,0.00026403513],"domain_scores_gemma":[0.99931765,0.00014274554,0.00014362783,0.000052172516,0.00009492866,0.00024885804],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00063547946,0.000047059293,0.00012809341,0.00006151479,0.000281033,0.00028867074,0.00030913658,0.00004515451,0.0021032752],"category_scores_gemma":[0.00011916715,0.00003879511,0.000019015391,0.00044108805,0.0002642014,0.00030968827,0.000003676332,0.00019663859,0.0000031034226],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000014391085,9.0767844e-7,0.9954307,0.0000066291454,0.000003060413,0.000019308576,0.00003778156,0.00036585264,4.1740049e-7,0.000026944193,0.0004983607,0.0036086028],"study_design_scores_gemma":[0.00011529242,0.00011166944,0.8944369,0.00004245526,0.0000021534638,0.000077923985,0.0004469074,0.00018069195,0.0000031764598,0.00043931385,0.10408864,0.00005489462],"about_ca_topic_score_codex":0.92368627,"about_ca_topic_score_gemma":0.9999916,"teacher_disagreement_score":0.10359028,"about_ca_system_score_codex":0.0000013613698,"about_ca_system_score_gemma":0.0020253467,"threshold_uncertainty_score":0.9988089},"labels":[],"label_agreement":null},{"id":"W2984226741","doi":"10.1139/cjes-2018-0206","title":"Petrogenesis and tectonic setting of the Huhetaoergai granitic pluton in the northern Ya-Gan Fault zone, northern Alxa, China: constraints from whole-rock geochemistry, zircon U–Pb ages, and Hf isotope compositions","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Pluton; Geology; Zircon; Geochemistry; Biotite; Petrogenesis; Partial melting; Feldspar; Crust; Fractional crystallization (geology); Petrology; Tectonics; Mantle (geology); Quartz; Seismology; Paleontology","score_opus":0.006823259015022951,"score_gpt":0.173755297559067,"score_spread":0.16693203854404404,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2984226741","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995208,0.0015556555,0.0000074511186,0.0020675047,0.000066232744,0.000092776696,0.00017944498,0.0000018394949,0.00082108215],"genre_scores_gemma":[0.99960583,0.000026678954,0.00009482304,0.00019921908,0.000035501995,2.9136308e-7,0.0000132196365,0.0000014633177,0.000022977913],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987365,0.000116143005,0.00032462523,0.00020905797,0.00029329426,0.0003203649],"domain_scores_gemma":[0.99913263,0.00020653012,0.00022631328,0.00012631417,0.00007479265,0.00023339278],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004818105,0.00013179099,0.00025268874,0.00009676614,0.0003687728,0.000117192314,0.00046985102,0.00005528427,0.00080601854],"category_scores_gemma":[0.00008785085,0.0000719383,0.00009371182,0.00044782137,0.0006771618,0.0001567164,0.000012639688,0.00024626375,0.000008474804],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000032470443,0.0000058415067,0.9938923,0.0000074017894,0.000017256107,0.0000128451875,0.0004691967,0.0018088039,0.0021975504,0.000005173775,0.0000032398812,0.0015771084],"study_design_scores_gemma":[0.00019741834,0.00009458126,0.99489784,0.00006942942,0.000038898506,0.00011274301,0.0011810124,0.0015587118,0.00068389985,0.0009399071,0.00011716698,0.00010841206],"about_ca_topic_score_codex":0.06225097,"about_ca_topic_score_gemma":0.7443833,"teacher_disagreement_score":0.6821323,"about_ca_system_score_codex":0.0000025338886,"about_ca_system_score_gemma":0.0002716972,"threshold_uncertainty_score":0.94399357},"labels":[],"label_agreement":null},{"id":"W2985231621","doi":"10.1139/cjes-2019-0175","title":"Ali Mehmet Celâl Şengör: A geologist who unravels the histories of continents and oceans","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"","keywords":"Geologist; Geology; Plate tectonics; Tectonics; Paleontology; Earth science","score_opus":0.014174244156426919,"score_gpt":0.18404817020228678,"score_spread":0.16987392604585985,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2985231621","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98743284,0.002355881,0.0000083656605,0.0040613925,0.00023506797,0.000046500445,0.000029813224,0.000001558429,0.005828579],"genre_scores_gemma":[0.99882954,0.000053560874,0.00019343007,0.00031669225,0.000038401024,4.8251295e-8,0.0000016490147,6.1717253e-7,0.00056606304],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895716,0.00006627014,0.0002836534,0.00013984159,0.00026127684,0.00029178115],"domain_scores_gemma":[0.9990217,0.00020251816,0.00022576028,0.00008920362,0.00012630488,0.00033453232],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00078117155,0.00008988002,0.00025220768,0.00012748888,0.00021228669,0.00006640862,0.00042444424,0.000039712144,0.0039031394],"category_scores_gemma":[0.00022266597,0.00004635636,0.00008439382,0.000398921,0.0012403781,0.00017171567,0.0000084522935,0.00013508815,0.000014844505],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004709924,0.0000018974912,0.9979712,0.0000040411933,0.000014144399,0.000009127073,0.00021944729,0.00038140969,0.000041380856,0.00038702218,0.00016230629,0.0008033163],"study_design_scores_gemma":[0.00013805226,0.00034849206,0.9732828,0.000018755849,0.000027953753,0.000053058808,0.0007042228,0.0006867202,0.00026027445,0.004487783,0.019892711,0.00009916843],"about_ca_topic_score_codex":0.033213798,"about_ca_topic_score_gemma":0.23461843,"teacher_disagreement_score":0.20140463,"about_ca_system_score_codex":9.403163e-7,"about_ca_system_score_gemma":0.00028006246,"threshold_uncertainty_score":0.9970074},"labels":[],"label_agreement":null},{"id":"W2988310985","doi":"10.1139/cjes-2018-0322","title":"Geochemistry of the Eocene clastic sediments (Suonahu Formation) in the North Qiangtang Basin, Tibet: implications for paleoclimate conditions, provenance and tectonic setting","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"China Geological Survey; China Scholarship Council; National Natural Science Foundation of China","keywords":"Clastic rock; Geology; Provenance; Terrigenous sediment; Sedimentary rock; Geochemistry; Felsic; Paleoclimatology; Diagenesis; Weathering; Mafic; Oceanography","score_opus":0.0095725929262015,"score_gpt":0.20758162271295658,"score_spread":0.19800902978675508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2988310985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964311,0.00035854644,0.000006960092,0.0018643056,0.000055530254,0.00013371147,0.00020500383,7.600249e-7,0.00094407774],"genre_scores_gemma":[0.999612,0.000013231337,0.00012577964,0.00019070873,0.000022182101,0.0000011198671,0.000014859109,6.8981143e-7,0.000019428046],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992584,0.000027187181,0.00024942917,0.00009236595,0.00016074324,0.00021188939],"domain_scores_gemma":[0.9993869,0.00010855186,0.00024519442,0.000089302244,0.00008193758,0.00008813435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005604174,0.00006103731,0.00009955248,0.000060907318,0.00033035505,0.00005957506,0.00030892185,0.00001955071,0.00014502375],"category_scores_gemma":[0.00008787158,0.00003580095,0.000051427065,0.0003759009,0.00018692177,0.00025195605,0.0000042422157,0.00008430112,0.0000023345833],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000016369519,0.000002739873,0.99806315,0.000030807572,0.0000053743647,6.1562673e-7,0.00014876202,0.0008103861,0.0003340558,0.00001964976,0.000055121516,0.00052772363],"study_design_scores_gemma":[0.00013420243,0.000047232697,0.9958093,0.000073714924,0.000016434917,0.00006280771,0.0008024798,0.0012725048,0.0007600752,0.0005879389,0.00038183545,0.000051437397],"about_ca_topic_score_codex":0.0007219483,"about_ca_topic_score_gemma":0.05704418,"teacher_disagreement_score":0.056322232,"about_ca_system_score_codex":0.00000281606,"about_ca_system_score_gemma":0.0003119802,"threshold_uncertainty_score":0.9601623},"labels":[],"label_agreement":null},{"id":"W2988846979","doi":"10.1139/cjes-2019-0111","title":"Northward subglacial drainage during the Mackinaw Interstade in the Cayuga basin, central New York, USA","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Shelf ice; Trough (economics); Geomorphology; Drainage; Structural basin; Sedimentary rock; Deglaciation; Paleontology; Ice stream; Oceanography; Glacial period; Cryosphere","score_opus":0.026407727621635766,"score_gpt":0.22209799000793076,"score_spread":0.195690262386295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2988846979","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98162353,0.0007012757,0.0000020202983,0.005178963,0.00082094996,0.00013290638,0.000007715951,0.0000014687557,0.011531187],"genre_scores_gemma":[0.998477,0.000016206288,0.00005357885,0.000659162,0.00016194183,1.4566923e-7,0.0000015140715,0.0000012608141,0.0006292338],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99810827,0.00032352924,0.00026763589,0.00016777444,0.00033537412,0.0007973897],"domain_scores_gemma":[0.9990099,0.00030301267,0.00012069706,0.00014769945,0.000037195394,0.00038145963],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016153442,0.00010785137,0.0001770027,0.0002880073,0.00051959767,0.00019278676,0.0011813818,0.00007034094,0.0034239125],"category_scores_gemma":[0.00012669714,0.000058107034,0.000083928506,0.0006241357,0.0008759516,0.00029951002,0.000007892934,0.0005558309,0.00024960714],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019751682,0.000001801845,0.99613655,0.000004463328,0.0000057913767,0.00020437229,0.0022560384,0.00085386954,0.0000017891439,0.00018846669,0.00013762004,0.00018946706],"study_design_scores_gemma":[0.0002187524,0.00016366591,0.9909721,0.000022001965,0.000004230657,0.0006415592,0.002253335,0.00012193775,0.000013283537,0.0003960122,0.005116103,0.000076995835],"about_ca_topic_score_codex":0.02960271,"about_ca_topic_score_gemma":0.93770546,"teacher_disagreement_score":0.90810275,"about_ca_system_score_codex":0.0000014453134,"about_ca_system_score_gemma":0.0016531164,"threshold_uncertainty_score":0.99748707},"labels":[],"label_agreement":null},{"id":"W2989142667","doi":"10.1139/cjes-2019-0112","title":"Petrogenesis of early Permian granitic dykes in the Wulanhuduge area, central Inner Mongolia, North China: constraints from geochronology, geochemistry, and Sr–Nd–Pb isotopes","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Geochronology; Zircon; Petrogenesis; Partial melting; Mafic; Fractional crystallization (geology); Lithophile; Permian; Radiogenic nuclide; Magma; Crust; Petrography; Pluton; Isotope geochemistry; Continental arc; Volcanic rock; Isotope; Mantle (geology); Tectonics; Volcano; Geomorphology","score_opus":0.01040883722688142,"score_gpt":0.17612882833721924,"score_spread":0.1657199911103378,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2989142667","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99591887,0.0015707156,0.0000020118125,0.00075000606,0.000099004224,0.00007054841,0.00022849896,0.0000018767358,0.0013584764],"genre_scores_gemma":[0.99955606,0.00005543854,0.0001334192,0.00015873897,0.00005572748,2.4953198e-7,0.000017619162,0.0000011372964,0.000021610578],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99855584,0.00008677634,0.00036001237,0.00023000239,0.0002740781,0.00049327355],"domain_scores_gemma":[0.99907655,0.0001688526,0.00019507673,0.00012044354,0.00006611215,0.00037298008],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035406614,0.00014279195,0.00031898744,0.00017453899,0.00015842519,0.00009471299,0.00057142705,0.000069710506,0.0056507387],"category_scores_gemma":[0.00012330097,0.000085888,0.000105077095,0.00045237725,0.0013684619,0.00018740185,0.000009175142,0.00022590319,0.000013435534],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007062363,0.0000071204604,0.99685174,0.00000571268,0.00001801804,0.000057403056,0.00050396734,0.0003579902,0.00017061818,0.000015738819,0.000014079861,0.001990561],"study_design_scores_gemma":[0.0001895132,0.00019842036,0.99611676,0.000029413577,0.000026117608,0.000071228686,0.00088412134,0.00043181056,0.00031053092,0.0014870942,0.00013868675,0.00011628522],"about_ca_topic_score_codex":0.106537856,"about_ca_topic_score_gemma":0.55113155,"teacher_disagreement_score":0.44459367,"about_ca_system_score_codex":0.0000019350286,"about_ca_system_score_gemma":0.00037237094,"threshold_uncertainty_score":0.9952582},"labels":[],"label_agreement":null},{"id":"W2990114137","doi":"10.1139/cjes-2019-0120","title":"Biological mats in siliciclastic sediments of the Paleoproterozoic Gunflint Formation, northwestern Ontario, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Lakehead University","funders":"","keywords":"Stromatolite; Geology; Siliciclastic; Precambrian; Microbial mat; Paleontology; Sedimentary depositional environment; Algal mat; Phanerozoic; Bedding; Period (music); Geochemistry; Carbonate; Cenozoic; Ecology","score_opus":0.01891619712626525,"score_gpt":0.19418945554144426,"score_spread":0.17527325841517902,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2990114137","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936962,0.0005959552,0.0000024790143,0.0001876408,0.0006718391,0.00010727587,0.000018493938,6.5629365e-7,0.004719466],"genre_scores_gemma":[0.99976814,0.0000031621291,0.0000758584,0.00011164073,0.000015532181,1.3525343e-7,6.4520435e-7,2.436504e-7,0.000024667026],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989135,0.000077357756,0.00036622942,0.00010007449,0.0002518259,0.00029096953],"domain_scores_gemma":[0.99931693,0.000085164065,0.00024689652,0.00008669357,0.00005375232,0.00021053314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044632578,0.00008032785,0.00017149119,0.00014176691,0.00014375124,0.000029244322,0.0004659729,0.000047154917,0.0006125551],"category_scores_gemma":[0.000028209472,0.00004712466,0.000053058397,0.0002970806,0.00029897425,0.00025332204,0.0000013214858,0.00018293176,0.0000034108784],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005578296,0.0000018414001,0.99734473,0.0000037898246,0.0000041393837,0.000015059049,0.00044292564,0.0008573343,0.00001799998,0.000011495173,0.0000145914555,0.0012804889],"study_design_scores_gemma":[0.00015252836,0.0001758619,0.9984807,0.00005453353,0.0000027311582,0.000064559375,0.00031403327,0.00018234547,0.00008195336,0.00015827321,0.0002735145,0.000059013055],"about_ca_topic_score_codex":0.9719362,"about_ca_topic_score_gemma":0.9999713,"teacher_disagreement_score":0.02803509,"about_ca_system_score_codex":0.0000052658884,"about_ca_system_score_gemma":0.0033957579,"threshold_uncertainty_score":0.67070484},"labels":[],"label_agreement":null},{"id":"W2990748495","doi":"10.1139/cjes-2019-0137","title":"Contact-style magmatic sulphide mineralisation in the Labrador Trough, northern Quebec, Canada: implications for regional prospectivity","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"NOSM University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Sill; Geochemistry; Mafic; Magma; Petrology; Volcano","score_opus":0.020135662178575216,"score_gpt":0.2035209739540636,"score_spread":0.1833853117754884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2990748495","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9714733,0.00029806938,0.0000110194715,0.027301693,0.00009234604,0.00016690172,0.000047755384,0.0000012391561,0.00060767756],"genre_scores_gemma":[0.998436,0.0000035716466,0.00018695203,0.00111272,0.00006796038,0.0000013370776,0.000014164687,7.5568215e-7,0.00017659091],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99905217,0.00006331476,0.00025284514,0.0001390311,0.00020608956,0.00028654854],"domain_scores_gemma":[0.9990888,0.0003425191,0.00016537934,0.00008965439,0.00011838063,0.00019526857],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058801874,0.00007774195,0.00016197961,0.00009967562,0.0002009414,0.00009063036,0.00039254,0.00002693335,0.0007545214],"category_scores_gemma":[0.00017634292,0.000044476106,0.00007177492,0.00045903496,0.00013149093,0.00022539729,0.0000018458192,0.000109603076,0.000008901536],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000044948088,0.000003906169,0.9968994,0.0000040285004,0.0000051789007,0.0000029013793,0.00015840228,0.001290667,0.00003782215,0.00045004155,0.0003093989,0.00083375216],"study_design_scores_gemma":[0.0001349457,0.00008366989,0.9902845,0.000010166392,0.000008793719,0.000020348449,0.00047552527,0.0009123714,0.000010485376,0.0051922924,0.0027968101,0.00007008821],"about_ca_topic_score_codex":0.9625915,"about_ca_topic_score_gemma":0.9999606,"teacher_disagreement_score":0.037369054,"about_ca_system_score_codex":0.000008245743,"about_ca_system_score_gemma":0.001655231,"threshold_uncertainty_score":0.826148},"labels":[],"label_agreement":null},{"id":"W2991081402","doi":"10.1139/cjes-2019-0140","title":"New insights into the geologic evolution of the Grenvillian Trenton Prong inlier, Central Appalachian Piedmont, USA","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Hornblende; Orogeny; Rodinia; Laurentia; Felsic; Mafic; Metamorphic facies; Granulite; Metamorphism; Metamorphic rock; Biotite; Continental arc; Diorite; Partial melting; Basalt; Petrology; Zircon; Geomorphology; Craton; Facies; Ordovician; Volcanic rock; Paleontology; Tectonics; Structural basin","score_opus":0.009612127550393854,"score_gpt":0.17292996872320818,"score_spread":0.16331784117281434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2991081402","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98907214,0.002609845,0.000028377219,0.0026555613,0.0005098599,0.00009856388,0.0000032284586,0.0000017400295,0.005020697],"genre_scores_gemma":[0.9989368,0.000030398998,0.00022989867,0.0001824951,0.00010914477,1.0012728e-7,0.0000013949305,7.717705e-7,0.0005090288],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985556,0.00011921683,0.00033463727,0.00017548948,0.000396552,0.00041851276],"domain_scores_gemma":[0.99892706,0.000084802865,0.00028487027,0.00015445474,0.000070814574,0.0004780131],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041207473,0.000115414616,0.0002032558,0.00013991933,0.000380894,0.0000710989,0.0009207603,0.00005902851,0.0046516773],"category_scores_gemma":[0.00011434703,0.000049186965,0.00017521577,0.00089420343,0.0006702456,0.00023772348,0.000013571289,0.00024067092,0.000055980752],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000047113567,0.0000030543752,0.9868328,0.0000029033251,0.000011018138,0.0000026108587,0.00042192408,0.008754358,0.000057711204,0.00037097192,0.000068900605,0.003469015],"study_design_scores_gemma":[0.000105974395,0.00020351342,0.98114693,0.000025090105,0.000021219323,0.000014735678,0.00039462303,0.0020178626,0.00016260381,0.01114395,0.004682112,0.0000813609],"about_ca_topic_score_codex":0.13773891,"about_ca_topic_score_gemma":0.8239134,"teacher_disagreement_score":0.6861745,"about_ca_system_score_codex":0.000004991231,"about_ca_system_score_gemma":0.0009482777,"threshold_uncertainty_score":0.9962582},"labels":[],"label_agreement":null},{"id":"W2992773998","doi":"10.1139/cjes-2018-0161","title":"Geology, mineralogy, S and Sr isotope geochemistry, and fluid inclusion analysis of barite associated with the Lemarchant Zn–Pb–Cu–Ag–Au-rich volcanogenic massive sulphide deposit, Newfoundland, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University; Government of Newfoundland and Labrador; Memorial University of Newfoundland","funders":"","keywords":"Geology; Fluid inclusions; Geochemistry; Seawater; Hydrothermal circulation; Mineralogy; Metamorphism; Inclusion (mineral); Metamorphic rock; Ore genesis; Isotope geochemistry; Isotope","score_opus":0.007038216850210257,"score_gpt":0.17692453445895312,"score_spread":0.16988631760874287,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2992773998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927851,0.0022764076,0.0000061130645,0.003970301,0.000061521874,0.000062840656,0.00008036238,0.0000015574336,0.0007557939],"genre_scores_gemma":[0.99906653,0.00008084633,0.00008904228,0.000488072,0.000032215095,2.6073266e-7,0.00003066631,0.0000014097633,0.00021095652],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983447,0.000120337514,0.00035233668,0.0002784177,0.00041361645,0.0004905857],"domain_scores_gemma":[0.9983333,0.0004242797,0.0003320191,0.00012721446,0.00021830019,0.0005648821],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007791741,0.00016608185,0.00047199373,0.00026907906,0.0005926811,0.0000657784,0.00044021607,0.000077191646,0.001187569],"category_scores_gemma":[0.0001785021,0.000091053065,0.00008620088,0.0012583898,0.00096314756,0.00013141362,0.000057845104,0.0002095965,0.0000011872226],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001740461,0.000003409241,0.995756,0.000005655004,0.00030484566,0.000047065874,0.0001597419,0.0024094214,0.0008314335,0.000010355895,0.000055764776,0.00039890522],"study_design_scores_gemma":[0.00022616034,0.0002765112,0.98831195,0.000023781273,0.0003938887,0.00006130498,0.0003554177,0.009448302,0.000176134,0.00020676554,0.00037348195,0.00014633438],"about_ca_topic_score_codex":0.93472695,"about_ca_topic_score_gemma":0.9993395,"teacher_disagreement_score":0.06461255,"about_ca_system_score_codex":0.000011014485,"about_ca_system_score_gemma":0.0013942698,"threshold_uncertainty_score":0.99972546},"labels":[],"label_agreement":null},{"id":"W2993948233","doi":"10.1139/cjes-2018-0255","title":"Zircons to the front: accretionary history of the Rheno-Hercynian active margin (Variscides, Germany)","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Devonian; Zircon; Carboniferous; Geochemistry; Orogeny; Ophiolite; Accretionary wedge; Paleontology; Paleozoic; Ordovician; Foreland basin; Accretion (finance); Island arc; Rift; Terrane; Late Devonian extinction; Subduction; Tectonics; Structural basin","score_opus":0.014121066760438136,"score_gpt":0.17763755564904898,"score_spread":0.16351648888861084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2993948233","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9607829,0.0017189814,0.0000071988025,0.008707598,0.00085640344,0.000098156524,0.000040462804,0.000001699002,0.027786627],"genre_scores_gemma":[0.996013,0.000010865499,0.00020517263,0.001181209,0.00007641023,1.8585943e-7,0.0000013098048,8.98766e-7,0.0025109488],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988091,0.000110931454,0.000258662,0.00015228809,0.00036281266,0.00030619217],"domain_scores_gemma":[0.9989833,0.00016225815,0.00020202153,0.00015960574,0.000109907814,0.00038286104],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00062498194,0.00009064851,0.00018291458,0.00014038953,0.00020333062,0.00003298523,0.0009374784,0.000040947652,0.020090148],"category_scores_gemma":[0.00015342284,0.00004234986,0.00015352597,0.00040782505,0.00057817757,0.00018530128,0.000015079373,0.00021841862,0.00021887463],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015050973,0.0000057703655,0.98190576,0.0000041300023,0.000028696255,0.000010619833,0.0009074648,0.0072895987,0.00030213242,0.00017403043,0.0045174584,0.0048392834],"study_design_scores_gemma":[0.000054724936,0.000120917815,0.90216863,0.000020877356,0.000017049779,0.00002792204,0.000348639,0.00046637558,0.000100034034,0.0015381373,0.095061734,0.000074957105],"about_ca_topic_score_codex":0.03232814,"about_ca_topic_score_gemma":0.38218164,"teacher_disagreement_score":0.3498535,"about_ca_system_score_codex":0.0000081519365,"about_ca_system_score_gemma":0.0012809468,"threshold_uncertainty_score":0.98080564},"labels":[],"label_agreement":null},{"id":"W2994777939","doi":"10.1139/cjes-2019-0166","title":"An Early Cretaceous (Berriasian) fossil-bearing locality from the Rocky Mountains of Alberta, yielding the oldest dinosaur skeletal remains from western Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; University of Calgary","funders":"Dinosaur Research Institute","keywords":"Geology; Paleontology; Cretaceous; Sedimentary depositional environment; Range (aeronautics); Fauna; Vertebrate; Ecology; Structural basin","score_opus":0.013565541963971446,"score_gpt":0.20497541181792717,"score_spread":0.19140986985395572,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2994777939","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99296397,0.0019634096,0.000031117896,0.0018654752,0.0011630016,0.000098294884,0.00016248476,0.0000022563343,0.0017500172],"genre_scores_gemma":[0.999012,0.000014657064,0.00008385325,0.0005235114,0.00025798843,1.8104194e-7,0.000011707709,0.0000019704075,0.00009411697],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99819845,0.000320348,0.00040374868,0.0002495884,0.00032661346,0.00050125323],"domain_scores_gemma":[0.997937,0.0009761404,0.00032806623,0.0002661275,0.000080301026,0.00041235247],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007770255,0.00014781722,0.0002729863,0.000069846916,0.00069866754,0.00010215359,0.0011532395,0.0001001524,0.00093792344],"category_scores_gemma":[0.00015861879,0.000084364816,0.00008091739,0.00024965778,0.0007955351,0.00045375002,0.000009735358,0.0003618362,0.000022769496],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012204355,0.0000025149725,0.9953606,0.0000012597858,0.000030067651,0.000031129974,0.0006652255,0.0029562379,0.000039152877,0.000041175124,0.00005534827,0.00080510014],"study_design_scores_gemma":[0.00013528808,0.00021559007,0.9933268,0.00003593966,0.000021307402,0.000059511243,0.0014684149,0.0014085078,0.000031451018,0.00035221933,0.0028284658,0.00011650478],"about_ca_topic_score_codex":0.98379546,"about_ca_topic_score_gemma":0.9998794,"teacher_disagreement_score":0.01608399,"about_ca_system_score_codex":0.000008678142,"about_ca_system_score_gemma":0.0028636246,"threshold_uncertainty_score":0.9999754},"labels":[],"label_agreement":null},{"id":"W2995056177","doi":"10.1139/cjes-2018-0163","title":"First evidence for the conifer <i>Pinus</i>, as <b><i>Pinuxylon selmeierianum</i></b> sp. nov., during the Paleogene on Wootton Peninsula, northern Ellesmere Island, Nunavut, Canada","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Plant Diversity and Evolution","field":"Agricultural and Biological Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Paleogene; Geology; Fossil wood; Peninsula; Paleontology; Arctic; Vegetation (pathology); Extant taxon; Ecology; Oceanography; Biology; Cretaceous","score_opus":0.023501443248755555,"score_gpt":0.19285890020025112,"score_spread":0.16935745695149557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2995056177","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9847484,0.000979657,9.921426e-7,0.012621965,0.0008114275,0.00025264433,0.00016330168,0.000003435573,0.0004181338],"genre_scores_gemma":[0.99776095,0.00014742122,0.000007847647,0.0011489585,0.00032291454,0.0000019128736,0.0000033976412,9.334109e-7,0.00060564536],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985943,0.000059265356,0.00022571388,0.00021605994,0.0004305783,0.00047412273],"domain_scores_gemma":[0.9985221,0.0007259508,0.0002249427,0.00007987158,0.00015877491,0.00028837819],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0006936051,0.00014089273,0.00016424544,0.000027910166,0.0019113949,0.0002012264,0.0008955008,0.00005681588,0.0006650071],"category_scores_gemma":[0.00018614932,0.000047629466,0.00011331751,0.0003583148,0.0002303346,0.00026414846,0.000023421071,0.0001986857,0.000038116144],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003088136,0.000018487697,0.9770522,0.00002429263,0.00006438989,0.00011503016,0.00062793086,0.007198263,0.0062256795,0.0001187519,0.0066420855,0.0016040382],"study_design_scores_gemma":[0.0003014271,0.00053097226,0.888448,0.00022931506,0.0000301833,0.00024395924,0.0019857984,0.00033688435,0.0014083603,0.00004228492,0.106197,0.000245804],"about_ca_topic_score_codex":0.33852202,"about_ca_topic_score_gemma":0.9980276,"teacher_disagreement_score":0.6595056,"about_ca_system_score_codex":0.0000416839,"about_ca_system_score_gemma":0.0009061052,"threshold_uncertainty_score":0.999388},"labels":[],"label_agreement":null},{"id":"W2995312363","doi":"10.1139/cjes-2019-0081","title":"Directions of lithosphere interactions in the Pamir – Hindu Kush junction inferred from anisotropic tomography","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Institute of Population and Public Health; King Saud University; National Natural Science Foundation of China; National Science Foundation","keywords":"Geology; Lithosphere; Seismology; Seismic tomography; Induced seismicity; Subduction; Anisotropy; Fibrous joint; Seismic anisotropy; Crust; Continental crust; Geophysics; Tectonics; Mantle (geology)","score_opus":0.014306391820668545,"score_gpt":0.21225535235364218,"score_spread":0.19794896053297364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2995312363","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923553,0.0005962019,0.000011556873,0.00033597354,0.0020665105,0.000080697595,0.00006187384,0.0000021259534,0.0044897553],"genre_scores_gemma":[0.99938715,0.000033783956,0.00027550774,0.000082033715,0.00012931622,2.6864117e-7,0.0000053651297,0.0000011170096,0.00008543699],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991165,0.00010522006,0.0002652748,0.00010624432,0.00021633224,0.0001904448],"domain_scores_gemma":[0.99936485,0.00013596739,0.00019497826,0.000104843675,0.00006888416,0.00013047957],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004290858,0.000070372145,0.00015480717,0.00020107588,0.00016543738,0.00013208773,0.0003165253,0.000024994682,0.002496695],"category_scores_gemma":[0.0000370988,0.000045446868,0.00006941365,0.00057632854,0.00014952091,0.000462598,0.0000028785216,0.00012501169,0.00003619674],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006906038,0.000008713134,0.9940906,0.000003886932,0.000015252194,0.000007966166,0.0010728338,0.0013649982,0.0002904651,0.00022830938,0.00028344,0.0026266216],"study_design_scores_gemma":[0.00010740729,0.0001478381,0.9680853,0.00004904865,0.00001074644,0.000010618367,0.0011415153,0.00015394976,0.00013653371,0.00062985043,0.029467924,0.000059288897],"about_ca_topic_score_codex":0.14652058,"about_ca_topic_score_gemma":0.62415695,"teacher_disagreement_score":0.47763637,"about_ca_system_score_codex":0.0000011794517,"about_ca_system_score_gemma":0.0003914303,"threshold_uncertainty_score":0.9984152},"labels":[],"label_agreement":null},{"id":"W2995427450","doi":"10.1139/cjes-2019-0021","title":"Converging ice streams: an unreasonable hypothesis for deposition of the Oak Ridges Moraine, southern Ontario","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Lineation; Moraine; Meltwater; Geomorphology; STREAMS; Landform; Bedrock; Sediment; Sedimentary rock; Glacier; Ice stream; Paleontology; Sea ice; Oceanography; Cryosphere","score_opus":0.027035941667798345,"score_gpt":0.19636530818887318,"score_spread":0.16932936652107483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2995427450","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99722564,0.00042082302,0.000026604932,0.00055132183,0.00045344912,0.00011945089,0.00009841426,0.0000015850123,0.0011026822],"genre_scores_gemma":[0.99701303,0.0000067100564,0.0019474287,0.00023199752,0.00006359839,2.5652557e-7,0.0000024261763,0.0000016443349,0.0007329311],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99922633,0.000030461373,0.00020550942,0.00010584122,0.0001957151,0.00023612396],"domain_scores_gemma":[0.99920505,0.00017296801,0.00021672466,0.00009491828,0.00013190371,0.00017841304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043436346,0.00007058268,0.00013845386,0.000049629205,0.0004264917,0.00008015713,0.00033344672,0.000024544797,0.00091052765],"category_scores_gemma":[0.00007876126,0.000044913962,0.00008076592,0.0002698044,0.00020019298,0.0002945068,0.0000031499515,0.00006650942,0.000008129418],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005967459,0.0000029487426,0.98712635,0.000005272152,0.000012232893,0.0000010676582,0.0010950842,0.0078089186,0.00002426997,0.000059764992,0.00009472641,0.0037634259],"study_design_scores_gemma":[0.00015241827,0.00023632757,0.985081,0.000044855686,0.00001953826,0.000014081335,0.005877083,0.002952191,0.00008642739,0.0002996077,0.005163201,0.000073241594],"about_ca_topic_score_codex":0.417749,"about_ca_topic_score_gemma":0.97182107,"teacher_disagreement_score":0.5540721,"about_ca_system_score_codex":0.000004664096,"about_ca_system_score_gemma":0.0011858908,"threshold_uncertainty_score":0.9969639},"labels":[],"label_agreement":null},{"id":"W2996825467","doi":"10.1139/cjes-2019-0011","title":"<i>Polypleuraspis</i> (Arthropoda, Trilobita) from the middle Cambrian (Miaolingian Series) around Kane Basin (Nunavut and Greenland)","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Trilobite; Geology; Paleontology; Series (stratigraphy); Structural basin; Cape; Oceanography; Archaeology; Ordovician; Geography","score_opus":0.022163307979023165,"score_gpt":0.20075207512433463,"score_spread":0.17858876714531147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2996825467","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9666464,0.011857751,0.0000063205343,0.0024594963,0.0012174984,0.00011427017,0.00014177193,0.0000050038234,0.0175515],"genre_scores_gemma":[0.99835765,0.00010897013,0.0005904392,0.0004917865,0.00028123127,1.3582553e-7,0.0000029164908,0.0000012820497,0.00016559742],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983862,0.00016085568,0.00035737883,0.00025495075,0.0003126192,0.00052798516],"domain_scores_gemma":[0.9984863,0.0003786061,0.00024361566,0.0001739413,0.00006774474,0.00064978434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009295422,0.00017135969,0.00029651393,0.0001742866,0.0007726812,0.00031713003,0.0005698277,0.0000966361,0.00084783306],"category_scores_gemma":[0.0001115423,0.00011029359,0.00010331491,0.00039129858,0.001268363,0.00076975307,0.0000020533348,0.0003133483,0.000038969494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022824726,0.0000019508964,0.99279493,0.0000030605613,0.00002315836,0.00007449434,0.0004922024,0.00004420704,0.000023535786,0.00012925419,0.00014584887,0.0062445304],"study_design_scores_gemma":[0.00032303957,0.00045075576,0.9913581,0.000059937276,0.000020572465,0.00038148602,0.0015415711,0.000199431,0.00004371686,0.0011550025,0.004306023,0.00016035522],"about_ca_topic_score_codex":0.060076736,"about_ca_topic_score_gemma":0.856661,"teacher_disagreement_score":0.79658425,"about_ca_system_score_codex":0.0000013274342,"about_ca_system_score_gemma":0.001065218,"threshold_uncertainty_score":0.9461823},"labels":[],"label_agreement":null},{"id":"W2999271645","doi":"10.1139/cjes-2018-0189","title":"Ancient DNA reveals northwest range extension of Richardson’s ground squirrel (<i>Urocitellus richardsonii</i>) into northeastern British Columbia, Canada, during the Late Pleistocene","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Genetic diversity and population structure","field":"Biochemistry, Genetics and Molecular Biology","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"Social Sciences and Humanities Research Council of Canada; Simon Fraser University","keywords":"Pleistocene; Ground squirrel; Range (aeronautics); Mitochondrial DNA; Archaeology; Vegetation (pathology); Glacial period; Geology; Ancient DNA; Geography; Paleontology; Ecology; Squirrel monkey; Biology","score_opus":0.01178288704291492,"score_gpt":0.19250600852097766,"score_spread":0.18072312147806274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2999271645","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99739003,0.0013728618,0.000023841973,0.00055496895,0.00036268213,0.00009964448,0.00011037099,0.000001098471,0.00008451944],"genre_scores_gemma":[0.99824667,0.00004869915,0.00012540269,0.000988157,0.00016517987,4.1385294e-7,0.0000066251914,0.000005703072,0.00041314782],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988456,0.000058901333,0.00029974672,0.00018568785,0.000342731,0.000267347],"domain_scores_gemma":[0.9988438,0.00000971987,0.00028447027,0.00012245406,0.00027568202,0.00046387754],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002600674,0.0000871309,0.00017530618,0.000030495314,0.00075996167,0.00022636415,0.00041666403,0.000055556953,0.00008458244],"category_scores_gemma":[0.00009916697,0.00009241126,0.00008232223,0.0002533351,0.0002643535,0.000015654556,0.00004215029,0.00010698319,0.0000012480235],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026820639,0.000006050562,0.976517,0.00004265079,0.000038858816,0.00010543295,0.0007451114,0.0020367114,0.017424589,0.0000017799013,0.0018109692,0.0012440045],"study_design_scores_gemma":[0.0002807566,0.00019076039,0.9863377,0.000032790602,0.000018231956,0.00011760923,0.00043756486,0.000032227188,0.00055761606,0.000011911295,0.011867637,0.00011514438],"about_ca_topic_score_codex":0.8366303,"about_ca_topic_score_gemma":0.9980532,"teacher_disagreement_score":0.16142292,"about_ca_system_score_codex":0.000011807411,"about_ca_system_score_gemma":0.001328007,"threshold_uncertainty_score":0.5845087},"labels":[],"label_agreement":null},{"id":"W2999276319","doi":"10.1139/cjes-2013-0037","title":"Geothermobarometry of spinel peridotites from southern British Columbia: implications for the thermal conditions in the upper mantle","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Olivine; Pyroxene; Geology; Peridotite; Xenolith; Spinel; Lithosphere; Mantle (geology); Geochemistry; Basalt; Kimberlite; Tectonics; Seismology","score_opus":0.015197678040498232,"score_gpt":0.19657886987477885,"score_spread":0.18138119183428061,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2999276319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934788,0.0011976016,0.000015013971,0.0037178241,0.000058620997,0.00012007248,0.00037798067,0.0000011206747,0.0010330123],"genre_scores_gemma":[0.99899477,0.000016638334,0.00025907785,0.000550142,0.00007308554,0.0000024299436,0.000010294419,8.247837e-7,0.000092746915],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99927163,0.00004344112,0.00023343593,0.00009871574,0.00012613647,0.00022665932],"domain_scores_gemma":[0.9990945,0.0004569007,0.00012281738,0.00008919624,0.00010161581,0.00013498486],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037692688,0.000047299996,0.00012392807,0.000056881338,0.00038772315,0.0002747792,0.0005804465,0.000029327506,0.018661238],"category_scores_gemma":[0.00015321428,0.00002969882,0.00010715714,0.00042745026,0.0006221991,0.00013957951,0.000003430901,0.00010009635,0.000028445418],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[4.0723438e-7,0.0000049482805,0.99670196,0.000001003295,0.000010553341,0.0000011119442,0.00012958975,0.0006094251,0.000099112774,0.000018163684,0.0003047397,0.0021189626],"study_design_scores_gemma":[0.00006857658,0.00005903251,0.98620087,0.00001090781,0.000016474256,0.000015617168,0.0015613835,0.0006497615,0.000007106904,0.010919822,0.0004448821,0.000045565263],"about_ca_topic_score_codex":0.5986071,"about_ca_topic_score_gemma":0.9235319,"teacher_disagreement_score":0.32492474,"about_ca_system_score_codex":6.3756926e-7,"about_ca_system_score_gemma":0.00017065347,"threshold_uncertainty_score":0.98223585},"labels":[],"label_agreement":null},{"id":"W2999726538","doi":"10.1139/cjes-2019-0149","title":"Chlorine isotopes unravel conditions of formation of the Neoproterozoic rock salts from the Salt Range Formation, Pakistan","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Evaporite; Halite; Geology; Seawater; Geochemistry; Gypsum; Salt pan; Salt (chemistry); Mineralogy; Paleontology; Sedimentary rock; Chemistry; Oceanography","score_opus":0.022425301270719237,"score_gpt":0.21064561634033777,"score_spread":0.18822031506961853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2999726538","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941228,0.00046503244,0.0003641838,0.0032229864,0.00022118293,0.00013591819,0.0003215953,0.000002015959,0.0011442635],"genre_scores_gemma":[0.99918514,0.000018118513,0.00011572526,0.00052708265,0.00011436547,3.1842882e-7,0.000015928388,0.0000011305668,0.00002216676],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99894714,0.00005586744,0.00042456688,0.00007725837,0.00030632433,0.0001888378],"domain_scores_gemma":[0.99905825,0.00008504433,0.0003818853,0.000105482955,0.00014975405,0.0002195972],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033917135,0.00007774533,0.00014497778,0.00004900742,0.0003532255,0.00008641865,0.00060084916,0.00002878855,0.0007826836],"category_scores_gemma":[0.00010226367,0.00004205666,0.00008134836,0.0003933789,0.00026288978,0.0006425265,0.000007637541,0.00012563121,0.000010839733],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004545347,0.000008651308,0.968781,0.0000962213,0.000036727084,0.000010263984,0.012251861,0.0101008145,0.0028661713,0.00023278079,0.0027774354,0.0027926012],"study_design_scores_gemma":[0.00037416443,0.00024215672,0.96218127,0.00012792544,0.000028564005,0.000052785064,0.0031786908,0.0050039957,0.020707106,0.0014298016,0.006557074,0.00011648497],"about_ca_topic_score_codex":0.016598543,"about_ca_topic_score_gemma":0.1145403,"teacher_disagreement_score":0.097941756,"about_ca_system_score_codex":0.0000023641924,"about_ca_system_score_gemma":0.00055920484,"threshold_uncertainty_score":0.98995},"labels":[],"label_agreement":null},{"id":"W3000740543","doi":"10.1139/cjes-2018-0225","title":"Cannibalism of contourites by gravity flows: explanation of the facies distribution of the Ordovician Pingliang Formation along the southern margin of the Ordos Basin, China","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Yangtze University; National Natural Science Foundation of China","keywords":"Contourite; Geology; Turbidite; Facies; Ordovician; Paleontology; Structural basin; Graben; Turbidity current; Geomorphology; Sedimentary depositional environment","score_opus":0.01518620211288671,"score_gpt":0.18683412739935562,"score_spread":0.1716479252864689,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3000740543","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921278,0.00060643884,0.00009258565,0.0057855165,0.00020331408,0.00014198507,0.00075982744,0.0000010861662,0.00028146678],"genre_scores_gemma":[0.9997486,0.000016797985,0.000027567627,0.00015847008,0.000022796841,2.3626387e-7,0.0000075556595,7.427172e-7,0.000017216911],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987653,0.00016966446,0.00044417783,0.000063329506,0.00040005485,0.0001575109],"domain_scores_gemma":[0.9987249,0.000109950946,0.0007451602,0.00010743879,0.00022546866,0.000087110035],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00076622807,0.00007548088,0.00015644798,0.000038287002,0.00047028388,0.000040409628,0.0007479755,0.000036849076,0.00015417262],"category_scores_gemma":[0.00052574027,0.000030589923,0.00010799192,0.00074175943,0.00069820846,0.00034181916,0.000013126335,0.00013164426,6.643193e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010194482,0.0000058778965,0.98257303,0.000056844023,0.0000131456145,2.4702513e-7,0.005454675,0.008806997,0.00021791078,0.00025915916,0.0005727074,0.002029231],"study_design_scores_gemma":[0.00010905073,0.00011094201,0.98450494,0.000107382984,0.000022117352,0.000007885719,0.0060040816,0.0035794717,0.0028515891,0.0007519088,0.0018971724,0.00005347526],"about_ca_topic_score_codex":0.035269424,"about_ca_topic_score_gemma":0.34164536,"teacher_disagreement_score":0.30637592,"about_ca_system_score_codex":0.0000023925156,"about_ca_system_score_gemma":0.00045049467,"threshold_uncertainty_score":0.9711548},"labels":[],"label_agreement":null},{"id":"W3002972897","doi":"10.1139/cjes-2019-0119","title":"Using geographic information systems to make transparent and weighted decisions on pit development: incorporation of interactive economic, environmental, and social factors","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Environmental and Social Impact Assessments","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"World Wildlife Fund Canada; Simon Fraser University; University of Toronto","funders":"","keywords":"Geographic information system; Population; Environmental resource management; Analytic hierarchy process; Natural resource; Geography; Environmental planning; Environmental science; Operations research; Engineering; Ecology; Cartography","score_opus":0.050370642093844585,"score_gpt":0.2579942792469466,"score_spread":0.20762363715310203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3002972897","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990707,0.00001528399,0.00022826383,0.00022005504,0.00008339886,0.00011596854,0.000036456477,0.0000010976446,0.00022877763],"genre_scores_gemma":[0.99925566,0.000010888578,0.0005392343,0.00017231336,0.0000138464175,6.219801e-7,0.0000028871223,0.0000025650763,0.0000019732868],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992192,0.00003637721,0.0002970873,0.000095665564,0.00020906507,0.00014260413],"domain_scores_gemma":[0.9993434,0.000036034322,0.00023164245,0.00002308206,0.0000031097281,0.00036272127],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018417226,0.0000884496,0.00014128993,0.00012649552,0.0003270882,0.00008795304,0.00010743108,0.000032692315,0.00016292809],"category_scores_gemma":[0.000010139177,0.00007484881,0.000024306486,0.00007759993,0.000286216,0.0006587531,0.000022797674,0.00007178867,0.0000113295455],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019016017,0.000014445672,0.97572714,0.000005089458,0.000022968246,0.0000027691492,0.0152132595,0.0022779847,0.002782514,0.00011683408,0.000017343069,0.0038006525],"study_design_scores_gemma":[0.0001897736,0.00029841586,0.98991925,0.000033409564,0.000011361406,0.0000049397763,0.005865395,0.00092113717,0.0010920345,0.000052453564,0.0014824253,0.00012938245],"about_ca_topic_score_codex":0.0011682529,"about_ca_topic_score_gemma":0.0030424625,"teacher_disagreement_score":0.014192148,"about_ca_system_score_codex":0.00005870942,"about_ca_system_score_gemma":0.00008687277,"threshold_uncertainty_score":0.30522457},"labels":[],"label_agreement":null},{"id":"W3003925485","doi":"10.1139/cjes-2019-0129","title":"Geochemical constraints on Eocene–Miocene geodynamic and magmatic evolution of the Varan-Naragh area, Urumieh-Dokhtar Magmatic Arc, Iran","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Mafic; Subduction; Igneous rock; Volcanic rock; Mantle (geology); Back-arc basin; Mantle plume; Partial melting; Lithosphere; Lithophile; Volcano; Paleontology; Tectonics","score_opus":0.018474119369034193,"score_gpt":0.18301045793855653,"score_spread":0.16453633856952232,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3003925485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913083,0.00080849254,0.00004136833,0.0047723814,0.00011374515,0.00008216886,0.000056934503,0.0000035124194,0.0028131204],"genre_scores_gemma":[0.99880666,0.0000198978,0.0004070671,0.000685779,0.0000611624,1.450124e-7,0.0000029581013,0.0000013123743,0.000015042666],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99842745,0.00009814479,0.0004442405,0.00021956806,0.0004213555,0.00038926382],"domain_scores_gemma":[0.9986215,0.00020080523,0.0002823185,0.00010391556,0.000086154236,0.0007052837],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046272113,0.00014808691,0.00032333232,0.00012869808,0.00026220753,0.0000631636,0.0005118581,0.00006278201,0.0039532147],"category_scores_gemma":[0.0005456077,0.00008556399,0.00013827483,0.000661879,0.0016701217,0.00014726842,0.000011945391,0.00025722984,0.000025017836],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026041964,0.000014889554,0.9875222,0.000049415514,0.00004109821,0.000035913126,0.0003072431,0.0051990813,0.0009928466,0.0003959107,0.00012757455,0.005287825],"study_design_scores_gemma":[0.000326407,0.00046769442,0.9574716,0.00014501547,0.000075156975,0.00011554045,0.0005585796,0.027306356,0.0008166095,0.012404032,0.00012012823,0.0001928911],"about_ca_topic_score_codex":0.003688058,"about_ca_topic_score_gemma":0.030371526,"teacher_disagreement_score":0.030050572,"about_ca_system_score_codex":0.0000035211347,"about_ca_system_score_gemma":0.00042631617,"threshold_uncertainty_score":0.9969573},"labels":[],"label_agreement":null},{"id":"W3005537737","doi":"10.1139/cjes-2019-0131","title":"Tectonic domains and exhumation history of the Omineca Belt in southeastern British Columbia from <sup>40</sup>Ar/<sup>39</sup>Ar thermochronology","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University; University of Calgary","funders":"","keywords":"Geology; Pluton; Hornblende; Zircon; Thermochronology; Muscovite; Biotite; Monazite; Geochemistry; Batholith; Cretaceous; Fission track dating; Closure temperature; Tectonics; Paleontology; Quartz","score_opus":0.014124723744074605,"score_gpt":0.16257055876450513,"score_spread":0.14844583502043052,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3005537737","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99237365,0.0036778348,0.0000059058434,0.0021061532,0.000083094295,0.00007609711,0.00008307931,0.0000035951482,0.0015905962],"genre_scores_gemma":[0.99890065,0.000048587826,0.00017296539,0.0006434982,0.000094708295,3.1852156e-7,0.000006673129,0.0000018548598,0.00013076946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99847275,0.00016119111,0.00044112225,0.00026342736,0.0002892825,0.0003722397],"domain_scores_gemma":[0.9989554,0.00015010624,0.00024660918,0.00010322829,0.00007300678,0.0004716242],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041244063,0.0001064462,0.00033165928,0.00009387356,0.00019978419,0.00011842085,0.0005760155,0.000090213005,0.011309732],"category_scores_gemma":[0.00022885023,0.00008895131,0.000115950104,0.00044574132,0.0011330233,0.00022543846,0.000020195022,0.00027399778,0.00001782485],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009768728,0.000006348933,0.9856353,0.000007519661,0.00001932584,0.000042254484,0.0013417385,0.006015438,0.00008716236,0.000004505978,0.00023050814,0.0066001643],"study_design_scores_gemma":[0.00031267948,0.00022980827,0.97727156,0.000057291385,0.000029228246,0.0000503241,0.0010984599,0.017484022,0.000013491492,0.0016504055,0.001672305,0.00013041688],"about_ca_topic_score_codex":0.34568965,"about_ca_topic_score_gemma":0.8946738,"teacher_disagreement_score":0.54898417,"about_ca_system_score_codex":0.000007987537,"about_ca_system_score_gemma":0.00076511235,"threshold_uncertainty_score":0.98959404},"labels":[],"label_agreement":null},{"id":"W3005607977","doi":"10.1139/cjes-2019-0160","title":"Sedimentary deformation features as evidence for paleoseismic events in the middle Eocene in the Dongying Depression of the southern Bohai Bay Basin, eastern China","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science and Technology Major Project; National Natural Science Foundation of China; National Science Foundation","keywords":"Geology; Sedimentary rock; Cataclastic rock; Structural basin; Dike; Facies; Fault (geology); Sedimentary structures; Geomorphology; Paleontology; Geochemistry; Seismology","score_opus":0.05252642592318481,"score_gpt":0.23962906834435374,"score_spread":0.18710264242116892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3005607977","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98823524,0.0020349259,0.000029908331,0.008959073,0.00013191429,0.00020017968,0.000021920623,9.0849466e-7,0.00038595818],"genre_scores_gemma":[0.9974359,0.000029363844,0.00011560331,0.0023591213,0.000049068818,9.012697e-7,0.0000025341174,6.945974e-7,0.000006767431],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99890476,0.00018706943,0.00028428202,0.0000844575,0.00032620877,0.00021319409],"domain_scores_gemma":[0.99930155,0.00027616773,0.00021287621,0.00007281407,0.000040999083,0.00009557206],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001423886,0.000072350136,0.00010122868,0.00008703042,0.00037344356,0.00007810372,0.0008280567,0.000030895848,0.00011836079],"category_scores_gemma":[0.00035255146,0.000029854826,0.000059807517,0.0005909575,0.00014910777,0.00055201177,0.000006351925,0.00017764649,0.000005380729],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014839944,0.0000029931784,0.97990257,0.000016839844,0.0000014604097,0.000001978562,0.008795412,0.0081301285,0.0000020003888,0.000008611995,0.000036211088,0.0030869818],"study_design_scores_gemma":[0.00012823248,0.00016999221,0.9863279,0.000190187,0.000006542649,0.000038944843,0.008245138,0.0032021976,0.00003092568,0.0011729231,0.0004402252,0.000046817488],"about_ca_topic_score_codex":0.01225125,"about_ca_topic_score_gemma":0.13253753,"teacher_disagreement_score":0.12028628,"about_ca_system_score_codex":0.0000013084797,"about_ca_system_score_gemma":0.00033854874,"threshold_uncertainty_score":0.99432623},"labels":[],"label_agreement":null},{"id":"W3005610894","doi":"10.1139/cjes-2019-0074","title":"Lower Cretaceous stratigraphic characteristics and tectonic control of the eastern depression, North Yellow Sea Basin, North China","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Transtension; Transpression; Cretaceous; Paleontology; Structural basin; Lithology; Tectonics; Geomorphology; Rift; Sinistral and dextral","score_opus":0.009992791250605551,"score_gpt":0.18347966930548879,"score_spread":0.17348687805488322,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3005610894","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99728715,0.00071373675,0.000783477,0.0007549622,0.00017468932,0.000053937452,0.00002668325,0.0000051692687,0.00020016803],"genre_scores_gemma":[0.99963665,0.00007589195,0.000031888463,0.00017064261,0.00006735565,3.7127856e-7,5.788877e-7,0.0000053994804,0.000011240104],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991653,0.000040340823,0.0002879836,0.00008957463,0.000232683,0.00018411675],"domain_scores_gemma":[0.9992306,0.000019273211,0.00013089547,0.00008831394,0.00007725863,0.00045363695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013154905,0.000094211966,0.00020671362,0.00013256566,0.00015240026,0.000081098,0.00028968486,0.000029091627,0.00004340266],"category_scores_gemma":[0.00007968374,0.000060138635,0.000090678695,0.0005690791,0.00025582904,0.00017139962,0.0000063773596,0.00018269468,0.0000013034513],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000033262465,0.000002295943,0.97073364,0.000014433217,0.000037348644,0.00002208145,0.0004475739,0.028155092,0.00010124395,0.0000021196788,0.000038918814,0.00044192723],"study_design_scores_gemma":[0.00021216382,0.000100662466,0.8045178,0.000041099647,0.000046016965,0.000020367768,0.0000987076,0.19351046,0.00013257294,0.0000069107523,0.0012104512,0.000102799546],"about_ca_topic_score_codex":0.00026670928,"about_ca_topic_score_gemma":0.06892323,"teacher_disagreement_score":0.16621585,"about_ca_system_score_codex":0.0000024940339,"about_ca_system_score_gemma":0.00034160708,"threshold_uncertainty_score":0.9480665},"labels":[],"label_agreement":null},{"id":"W3006830510","doi":"10.1139/cjes-2019-0159","title":"Offshore bedrock geology of Eclipse Sound and Pond Inlet: connecting the structure and stratigraphy of Bylot and northern Baffin islands","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Laurentian University; Geological Survey of Canada","funders":"","keywords":"Geology; Fault (geology); Graben; Paleontology; Sound (geography); Seismology; Horst; Geomorphology; Tectonics","score_opus":0.023700913296002463,"score_gpt":0.1971479191853811,"score_spread":0.17344700588937864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3006830510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99401784,0.0037755647,0.0000131637125,0.0017796191,0.00006485381,0.00004477906,0.000031487725,7.038542e-7,0.00027200987],"genre_scores_gemma":[0.9994821,0.0001015934,0.00015342225,0.00018248026,0.000077273355,1.7792017e-8,0.0000012157134,6.190012e-7,0.0000012766416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993726,0.00004504118,0.0002090962,0.00010614133,0.00011269018,0.00015441731],"domain_scores_gemma":[0.9993728,0.00013791725,0.00018754233,0.000029189332,0.000065485845,0.00020707508],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025580847,0.00006846517,0.0001736665,0.000060488877,0.00029715154,0.000048056674,0.00011721776,0.000035444587,0.00015359947],"category_scores_gemma":[0.00013937021,0.000038741233,0.000020421478,0.00020640096,0.0006972488,0.00014136023,0.0000076786855,0.00010479446,2.13758e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000991666,5.243897e-7,0.9910274,0.000009257803,0.000011571956,0.0000043269933,0.0026228616,0.00044074823,0.00002811929,0.000101023885,0.000012484816,0.0057317284],"study_design_scores_gemma":[0.00015558541,0.00083745405,0.98667157,0.000011982333,0.000013031826,0.00006731769,0.006856461,0.0013322192,0.000048345035,0.0036448075,0.00030168027,0.000059556125],"about_ca_topic_score_codex":0.0038613034,"about_ca_topic_score_gemma":0.6501982,"teacher_disagreement_score":0.646337,"about_ca_system_score_codex":2.0777225e-7,"about_ca_system_score_gemma":0.000088371,"threshold_uncertainty_score":0.58371615},"labels":[],"label_agreement":null},{"id":"W3007260252","doi":"10.1139/cjes-2019-0198","title":"Extending the record of the Lomagundi–Jatuli carbon isotope excursion in the Labrador Trough, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Division of Ocean Sciences; Natural Sciences and Engineering Research Council of Canada; Alfred P. Sloan Foundation","keywords":"Geology; Authigenic; Excursion; Carbonate; Sedimentary depositional environment; Sedimentary rock; Isotopes of carbon; Geochemistry; Trough (economics); Context (archaeology); Paleontology; Total organic carbon; Chemistry; Structural basin","score_opus":0.024639399164510533,"score_gpt":0.2083855972468224,"score_spread":0.18374619808231188,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3007260252","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9667226,0.0054851426,0.0000014426275,0.015394626,0.00067640207,0.0001005676,0.000017836288,8.9975214e-7,0.011600497],"genre_scores_gemma":[0.99888533,0.00003668367,0.00006693669,0.00089888,0.000101381076,1.6862988e-7,1.6952374e-7,4.6204025e-7,0.000009995126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985848,0.0002818409,0.00030471996,0.0001221953,0.0003797443,0.000326672],"domain_scores_gemma":[0.9991016,0.0002718337,0.00024798204,0.00011765564,0.000038090424,0.00022283629],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000963379,0.00009039088,0.00015863788,0.00007411107,0.0004921265,0.00007075907,0.0011396576,0.000036841895,0.00010997729],"category_scores_gemma":[0.00021151341,0.000040457828,0.00007631691,0.0008050047,0.0006939349,0.00017306006,0.0000017011523,0.00032952474,4.8707227e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008518854,0.0000012646944,0.9794004,0.0000037395107,0.0000056543886,0.000052084815,0.0012156884,0.00023445023,0.0000137861325,0.00009651115,0.00035659762,0.018611297],"study_design_scores_gemma":[0.00009144295,0.00016569383,0.99329954,0.00003298775,0.000008551529,0.000066590124,0.0021768408,0.0006377828,0.000044342964,0.00023936518,0.0031793334,0.00005752209],"about_ca_topic_score_codex":0.7942009,"about_ca_topic_score_gemma":0.9980237,"teacher_disagreement_score":0.20382279,"about_ca_system_score_codex":0.0000019563022,"about_ca_system_score_gemma":0.0024835833,"threshold_uncertainty_score":0.440577},"labels":[],"label_agreement":null},{"id":"W3007329136","doi":"10.1139/cjes-2019-0163","title":"Discovery of a significant cave entrance in stripe karst, Horsethief Creek Group, Wells Gray Provincial Park, British Columbia, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; Royal Canadian Geographical Society; BC Hydro (Canada)","funders":"Natural Resources Canada","keywords":"Cave; Karst; Geology; Sinkhole; Hydrology (agriculture); Spring (device); Drainage; Archaeology; Geomorphology; Paleontology; Geography","score_opus":0.023073297507101742,"score_gpt":0.18942994621861914,"score_spread":0.1663566487115174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3007329136","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9925589,0.0012746089,0.000005123698,0.0006972911,0.00057117734,0.00015558497,0.003952772,0.0000017673832,0.0007827515],"genre_scores_gemma":[0.9984609,0.00015172173,0.000060234855,0.00096659584,0.00023327237,3.1787738e-7,0.000044944623,0.0000031521286,0.00007886691],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979787,0.000103038095,0.0005386701,0.00025354492,0.00054265413,0.00058338617],"domain_scores_gemma":[0.998623,0.00014340495,0.00029890172,0.00007807293,0.00008237584,0.00077423255],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00060837384,0.0001089133,0.00034321297,0.000088100875,0.0002502435,0.0006017651,0.0005496535,0.00005862647,0.0020184764],"category_scores_gemma":[0.00016815195,0.00013216278,0.00007853488,0.0007528366,0.0005041347,0.00060436846,0.0000063467237,0.00027814836,0.0000035986143],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009960134,0.0000054122806,0.99376494,0.000026254342,0.0000057378093,0.0007199053,0.00048909336,0.00035566857,0.00008404477,0.0000022457202,0.002909227,0.0016275232],"study_design_scores_gemma":[0.00029623878,0.00043031183,0.9903841,0.00012840907,0.000009827416,0.00007511388,0.0014635391,0.00048650117,0.00003752328,0.000055636112,0.0064477636,0.00018505707],"about_ca_topic_score_codex":0.9985203,"about_ca_topic_score_gemma":0.99999493,"teacher_disagreement_score":0.0059019704,"about_ca_system_score_codex":0.000009383029,"about_ca_system_score_gemma":0.004800985,"threshold_uncertainty_score":0.9988938},"labels":[],"label_agreement":null},{"id":"W3007463952","doi":"10.1139/cjes-2019-0075","title":"Origin and formation of Metabreccia in the Parkin Offset Dike, Sudbury impact structure, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Wallbridge Mining (Canada); Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Mitacs","keywords":"Dike; Geology; Breccia; Diorite; Quartz; Geochemistry; Impact structure; Impact crater; Igneous rock; Clastic rock; Petrology; Geomorphology; Sedimentary rock; Paleontology","score_opus":0.02450553944931368,"score_gpt":0.22585682083508266,"score_spread":0.20135128138576897,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3007463952","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99839884,0.00012685826,0.00006335391,0.0010563008,0.00006641018,0.000035112298,0.00008313858,2.0165892e-7,0.00016977225],"genre_scores_gemma":[0.9997042,0.0000020432544,0.000065702436,0.00016957967,0.000045212037,1.0373297e-7,0.000011330848,6.129517e-7,0.0000012120825],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99945295,0.00003563011,0.0001687835,0.00004820794,0.00016565873,0.00012877394],"domain_scores_gemma":[0.9996198,0.000032073913,0.00013170777,0.000029024242,0.000030037467,0.00015739622],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002815316,0.000043952958,0.0000917023,0.00006782809,0.00009239881,0.000058493446,0.00017697546,0.0000071624313,0.00006429712],"category_scores_gemma":[0.0000151009735,0.000026122842,0.000017322942,0.00033494734,0.00007738733,0.0005584873,0.0000022982915,0.0000753071,4.5748698e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005330752,0.0000020091907,0.9851949,0.0000044567264,0.00000825462,0.000007956786,0.0022977672,0.006338027,0.00027732566,0.00067746406,0.0021571103,0.0030293772],"study_design_scores_gemma":[0.000364157,0.00034357954,0.9577124,0.00004093003,0.000024411938,0.00003680925,0.0070595862,0.014734965,0.0010319294,0.0026801853,0.015792517,0.0001785376],"about_ca_topic_score_codex":0.560253,"about_ca_topic_score_gemma":0.92681193,"teacher_disagreement_score":0.3665589,"about_ca_system_score_codex":0.0000033214312,"about_ca_system_score_gemma":0.0016146207,"threshold_uncertainty_score":0.4426753},"labels":[],"label_agreement":null},{"id":"W3007856897","doi":"10.1139/cjes-2019-0141","title":"Early–Middle Ordovician brachiopod diversification in the middle Yangtze region of South China","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Paleontology; Baltica; Laurentia; Geology; Ordovician; China; Geography; Archaeology","score_opus":0.059486016353669034,"score_gpt":0.20773774029101266,"score_spread":0.14825172393734362,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3007856897","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9713294,0.0019320595,0.000027777476,0.002711277,0.00013514991,0.00006891481,0.000016963448,0.0000019097156,0.023776542],"genre_scores_gemma":[0.99951833,0.000014210254,0.00019576852,0.00020334162,0.00006154779,7.939867e-8,8.470259e-7,3.853558e-7,0.0000055142987],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989568,0.00014104089,0.00027682367,0.00012823775,0.00024190787,0.00025521696],"domain_scores_gemma":[0.9992663,0.00007489705,0.00025558082,0.00007946205,0.000038799728,0.00028495994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00060868746,0.000077436496,0.00015179261,0.00021293433,0.00031875927,0.00006793401,0.0006230431,0.000050105104,0.000095623815],"category_scores_gemma":[0.00012457812,0.000051683117,0.000077314704,0.0006972951,0.0005705424,0.0003718034,8.059748e-7,0.00020813143,0.0000061632754],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011670729,0.0000033492415,0.98587483,0.000004961923,0.0000047816707,0.000059095513,0.009296426,0.00019778698,0.000002820186,0.0003241244,0.000016802225,0.0042033633],"study_design_scores_gemma":[0.00013186297,0.00042512186,0.99546516,0.000030370282,0.000008053146,0.000038152684,0.0028579214,0.00028581,0.000008249652,0.00047203855,0.00021541238,0.00006186163],"about_ca_topic_score_codex":0.012619562,"about_ca_topic_score_gemma":0.31008554,"teacher_disagreement_score":0.29746598,"about_ca_system_score_codex":5.999822e-7,"about_ca_system_score_gemma":0.0004958715,"threshold_uncertainty_score":0.9939555},"labels":[],"label_agreement":null},{"id":"W3007873169","doi":"10.1139/cjes-2019-0231","title":"Dental anatomy of the apex predator <i>Sinraptor dongi</i> (Theropoda: Allosauroidea) from the Late Jurassic of China","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Canadian Museum of Nature; University of Alberta","funders":"Office of International Science and Engineering; National Museum of Natural History; Muséum National d'Histoire Naturelle; Willi Hennig Society; National Science Foundation","keywords":"Theropoda; Anatomy; Dentition; Geology; Crown (dentistry); Apex (geometry); Biology; Orthodontics; Paleontology; Medicine; Taxon","score_opus":0.013458402232995562,"score_gpt":0.20200965748635197,"score_spread":0.18855125525335642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3007873169","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9888092,0.0036091967,0.000007948219,0.005422842,0.00058618526,0.00006805248,0.00022985776,0.0000018211518,0.0012648633],"genre_scores_gemma":[0.9989348,0.0000445698,0.00015727921,0.00070606946,0.00012949895,8.048789e-8,0.0000036987879,0.000001110559,0.000022870512],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99887365,0.00019383695,0.00032609905,0.00012153492,0.00023107346,0.0002537987],"domain_scores_gemma":[0.9990042,0.00018357622,0.00036838595,0.00011080145,0.000054557284,0.00027847243],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004187182,0.00009148928,0.0002015521,0.00005173658,0.00032580542,0.000020575428,0.00095693447,0.000060690447,0.00084993977],"category_scores_gemma":[0.00016771197,0.000047172285,0.00011818607,0.00042598633,0.0016794597,0.00021578056,0.000010124252,0.00020140645,0.000016538314],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017744871,0.0000026762493,0.9975221,0.0000022539657,0.000028309589,0.000008364559,0.00038051017,0.00055566896,0.00033926943,0.00006861749,0.00038249334,0.0006919561],"study_design_scores_gemma":[0.00014244442,0.00020130211,0.9939189,0.00002113033,0.000021472923,0.000033872213,0.00036051805,0.0005358249,0.00031323457,0.0003772789,0.004016397,0.000057641326],"about_ca_topic_score_codex":0.014334011,"about_ca_topic_score_gemma":0.36283088,"teacher_disagreement_score":0.34849688,"about_ca_system_score_codex":0.0000012078397,"about_ca_system_score_gemma":0.0010283184,"threshold_uncertainty_score":0.99222964},"labels":[],"label_agreement":null},{"id":"W3007920441","doi":"10.1139/cjes-2020-0026","title":"In Memoriam / In Memoriam","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Human auditory perception and evaluation","field":"Engineering","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry","score_opus":0.05212732360454583,"score_gpt":0.2609696557557976,"score_spread":0.20884233215125178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3007920441","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9854261,0.00018151243,0.000059945465,0.0018730795,0.006254177,0.00004505117,0.0000014137431,0.0000061761134,0.0061524883],"genre_scores_gemma":[0.9977988,0.000013913309,0.00023496158,0.00037347738,0.0015282709,3.50895e-7,1.5210158e-7,0.0000034068478,0.00004666578],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9993894,0.00002579122,0.000211719,0.000057729023,0.00014949989,0.0001658258],"domain_scores_gemma":[0.9996182,0.000013243624,0.000029180475,0.000028136488,0.000024194635,0.0002870756],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004920221,0.00004697508,0.00009430815,0.00029013574,0.000036634472,0.000049609644,0.00015330376,0.000025640937,0.0052099777],"category_scores_gemma":[0.00009818883,0.00004463276,0.000021751915,0.00041051774,0.000062370564,0.00033355624,0.0000019226406,0.00013798029,0.00025950407],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009630493,0.000010687553,0.0904567,0.000048838803,0.000011380405,0.00038622576,0.022822045,0.72690356,0.0027504207,0.00018463688,0.15366973,0.0027461764],"study_design_scores_gemma":[0.0012068617,0.0003102337,0.4832638,0.00014091416,0.000007401844,0.000054411925,0.0032302442,0.096231826,0.00040202346,0.0007891308,0.41397727,0.00038588743],"about_ca_topic_score_codex":0.00007866726,"about_ca_topic_score_gemma":0.07435114,"teacher_disagreement_score":0.63067174,"about_ca_system_score_codex":0.0000164599,"about_ca_system_score_gemma":0.00036941146,"threshold_uncertainty_score":0.9956994},"labels":[],"label_agreement":null},{"id":"W3008668289","doi":"10.1139/cjes-2019-0199","title":"A discussion of “hidden subduction” in orogenic belts","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Subduction; Lithosphere; Basement; Paleontology; Paleozoic; Cretaceous; Oceanic crust; Seismology; Sedimentary rock; Tectonics","score_opus":0.03148452506038726,"score_gpt":0.21938110184585516,"score_spread":0.1878965767854679,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3008668289","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99004436,0.0025568896,0.000005428049,0.0042618476,0.0002796899,0.000046615147,0.000014371035,0.0000021354929,0.0027886438],"genre_scores_gemma":[0.9991478,0.0000706503,0.0004070543,0.00023664541,0.000100432,5.6724478e-8,8.014742e-7,0.0000010429337,0.000035539506],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990043,0.000049648857,0.00031473514,0.00012090485,0.00024820777,0.00026220054],"domain_scores_gemma":[0.999287,0.00005365711,0.00015917647,0.00004967831,0.00005776746,0.00039271428],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004474796,0.00007228969,0.00019189196,0.0002321071,0.00015350232,0.000035383262,0.0002804811,0.000028554081,0.0015436574],"category_scores_gemma":[0.00020880709,0.000043169308,0.0000676141,0.0007541993,0.00034298762,0.0002905486,0.000004187746,0.00012929442,0.000026073301],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000893015,0.0000022856857,0.9761564,0.00000687443,0.000008389295,0.000051955478,0.0014237093,0.0006208932,0.000027206568,0.000054246048,0.00015843201,0.021480672],"study_design_scores_gemma":[0.00019943765,0.00043981196,0.9918329,0.000047352685,0.0000069848975,0.000048861362,0.0015432545,0.00032152544,0.0002174398,0.0003840033,0.0048785713,0.00007987442],"about_ca_topic_score_codex":0.00978417,"about_ca_topic_score_gemma":0.54967546,"teacher_disagreement_score":0.53989124,"about_ca_system_score_codex":9.646022e-7,"about_ca_system_score_gemma":0.00090807216,"threshold_uncertainty_score":0.9993691},"labels":[],"label_agreement":null},{"id":"W3010811655","doi":"10.1139/cjes-2019-0229","title":"Emplacement of sharp-walled sulfide veins during the formation and reactivation of impact-related structures at the Broken Hammer Mine, Sudbury, Ontario","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"","keywords":"Geology; Geochemistry; Epidote; Chalcopyrite; Fluid inclusions; Chlorite; Hydrothermal circulation; Quartz; Actinolite; Breccia; Schist; Ore genesis; Vein; Metamorphic rock; Mineralogy; Seismology; Copper; Paleontology","score_opus":0.017349343973770907,"score_gpt":0.1952829639609235,"score_spread":0.1779336199871526,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3010811655","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962626,0.0004975726,0.0000033789656,0.0024884199,0.000037879374,0.0000622544,0.000020551817,8.644124e-7,0.00062646903],"genre_scores_gemma":[0.9997193,0.000016833776,0.00004217566,0.00011768099,0.000019983841,8.291823e-8,0.0000062492704,5.227353e-7,0.00007714781],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991082,0.00004869343,0.00032643016,0.00008728499,0.000256333,0.00017305942],"domain_scores_gemma":[0.9992023,0.00010715907,0.00032148996,0.000055556207,0.00008683609,0.00022662664],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00036308763,0.00007210109,0.00015576607,0.00007135209,0.00026059218,0.0000411186,0.00023227627,0.00002904569,0.003946535],"category_scores_gemma":[0.00013758735,0.000032034604,0.00007962524,0.0003304798,0.00036507295,0.00022298036,0.000010126455,0.000121377605,0.0000024766541],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039421324,0.0000022819888,0.9866664,0.0000070986293,0.000035365003,0.0000035229998,0.0020449462,0.009158774,0.0013544505,0.000020694673,0.000091273665,0.0005758187],"study_design_scores_gemma":[0.00015138775,0.00024607193,0.9943638,0.00001083108,0.000023554128,0.000029622357,0.00048499115,0.0014662937,0.0022384592,0.0005493987,0.00039045082,0.000045169265],"about_ca_topic_score_codex":0.27175808,"about_ca_topic_score_gemma":0.88823766,"teacher_disagreement_score":0.6164796,"about_ca_system_score_codex":0.0000046249374,"about_ca_system_score_gemma":0.00024691687,"threshold_uncertainty_score":0.996964},"labels":[],"label_agreement":null},{"id":"W3012010115","doi":"10.1139/cjes-2019-0080","title":"Relationship between rock physical properties and spectral mineralogy applied to exploration for an unconformity-related uranium deposit (Saskatchewan, Canada)","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"iNano Medical (Canada)","funders":"","keywords":"Geology; Chlorite; Mineralogy; Unconformity; Uranium; Porosity; Hydrothermal circulation; Geochemistry; Electrical resistivity and conductivity; Uranium ore; Physical property; Feldspar; Sedimentary rock; Quartz; Chemistry","score_opus":0.0673716506546948,"score_gpt":0.2239174815133859,"score_spread":0.1565458308586911,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3012010115","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95988685,0.000036258654,0.019642586,0.019351013,0.00010755841,0.00015659277,0.000003648167,0.000008598367,0.00080690434],"genre_scores_gemma":[0.9963295,1.1253767e-7,0.002897004,0.00051764137,0.00016285863,0.000002346163,0.0000012872364,0.0000014044837,0.00008783075],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910307,0.000025965297,0.00022630296,0.00019402307,0.00017757565,0.00027306733],"domain_scores_gemma":[0.9989189,0.00006968494,0.00011076606,0.000075831114,0.00012335677,0.0007014747],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025369914,0.00008911279,0.00015896368,0.000068081164,0.0003760138,0.00017303895,0.00043608292,0.000036208818,0.000002064652],"category_scores_gemma":[0.0001771052,0.000073136034,0.00002522149,0.00035584377,0.000070020986,0.00056186016,0.000017937264,0.00012861984,9.755203e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000096973075,0.00004315694,0.6582684,0.0002546111,0.00010398374,0.000119726814,0.09851154,0.15383717,0.024249135,0.048454538,0.0049660592,0.011094704],"study_design_scores_gemma":[0.0023591095,0.005286213,0.7022276,0.00017585626,0.00011484018,0.00035328502,0.023118723,0.14651605,0.061087105,0.036693458,0.020240296,0.0018274717],"about_ca_topic_score_codex":0.030031873,"about_ca_topic_score_gemma":0.7230852,"teacher_disagreement_score":0.69305336,"about_ca_system_score_codex":0.000010450705,"about_ca_system_score_gemma":0.002027779,"threshold_uncertainty_score":0.97642726},"labels":[],"label_agreement":null},{"id":"W3012025764","doi":"10.1139/cjes-2019-0220","title":"Petrology, age, and tectonic setting of the rapakivi-bearing Margaree pluton, Cape Breton Island, Canada: evidence for a Late Devonian posttectonic cryptic silicic-mafic magma chamber","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Cape Breton University; Nova Scotia Department of Energy; Acadia University","funders":"Natural Sciences and Engineering Research Council of Canada; Acadia University","keywords":"Mafic; Geology; Pluton; Silicic; Geochemistry; Felsic; Magma chamber; Zircon; Fractional crystallization (geology); Magma; Plagioclase; Igneous differentiation; Petrology; Partial melting; Crust; Basalt; Tectonics; Quartz; Paleontology; Volcano","score_opus":0.025808164483839588,"score_gpt":0.21017403237537416,"score_spread":0.18436586789153458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3012025764","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9860253,0.0028229447,0.000012083914,0.010532625,0.00014162995,0.00012148047,0.000045037865,0.0000029033401,0.0002960298],"genre_scores_gemma":[0.99825555,0.000029384339,0.00029241684,0.0013015466,0.00007571861,4.5097633e-7,0.0000017420888,0.000002202578,0.00004098084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983416,0.000095834504,0.00041839477,0.0002669135,0.0003282167,0.0005490305],"domain_scores_gemma":[0.9984107,0.00045591526,0.00030671578,0.00010595583,0.00013603261,0.0005846618],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00069111004,0.00015233882,0.00033997136,0.000107466534,0.00045297432,0.00008840972,0.0005148597,0.000060190843,0.00127044],"category_scores_gemma":[0.00095341436,0.00009280303,0.00013044808,0.0007063819,0.000569018,0.00018219174,0.000024127014,0.00027674114,0.0000032117775],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022727025,0.00000163144,0.9925813,0.000032333974,0.000030811745,0.000060910523,0.00033206094,0.0050564767,0.00063062616,0.0000157795,0.00009501285,0.0011403376],"study_design_scores_gemma":[0.00019882251,0.0003324008,0.98374563,0.00008920728,0.00005410653,0.00010085616,0.00020911277,0.013676854,0.00024031493,0.00045757496,0.0007489388,0.00014617137],"about_ca_topic_score_codex":0.5124869,"about_ca_topic_score_gemma":0.9926037,"teacher_disagreement_score":0.4801168,"about_ca_system_score_codex":0.0000055760315,"about_ca_system_score_gemma":0.0018336981,"threshold_uncertainty_score":0.99964255},"labels":[],"label_agreement":null},{"id":"W3012357576","doi":"10.1139/cjes-2019-0107","title":"Zircon U–Pb dating and sulfide Re–Os isotopes of the Xiarihamu Cu–Ni sulfide deposit in Qinghai Province, Northwestern China","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Chinese Academy of Geological Sciences","keywords":"Zircon; Geology; Geochemistry; Isochron; Geochronology; Petrogenesis; Sulfide; Mafic; Mineralization (soil science); Ultramafic rock; Isochron dating; Mantle (geology)","score_opus":0.015250864372490116,"score_gpt":0.18633017254282275,"score_spread":0.17107930817033262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3012357576","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99276954,0.0008105636,0.00002672995,0.004045618,0.00008745056,0.000076837714,0.000022596576,0.0000023407092,0.0021583026],"genre_scores_gemma":[0.99838287,0.000025710448,0.00076069357,0.00072821596,0.00006382739,1.2817074e-7,0.000001848449,0.0000011660436,0.000035553458],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986058,0.000095433425,0.00043726186,0.0002135679,0.0003001596,0.00034776682],"domain_scores_gemma":[0.9989688,0.00011902497,0.00027206307,0.00008333841,0.00005558188,0.0005012281],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053203694,0.00011467312,0.00026582618,0.00012788475,0.00025514993,0.00009518119,0.0005572822,0.00004516859,0.00075955986],"category_scores_gemma":[0.00034582507,0.00006675808,0.0000811457,0.0007358222,0.0005599554,0.00039255325,0.000022785543,0.00024613584,0.0000053971207],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000060794955,0.0000027539995,0.995247,0.000011759143,0.0000068093636,0.000037979185,0.00037561145,0.0018642889,0.00050481694,0.000024446239,0.00002081148,0.0018976607],"study_design_scores_gemma":[0.00013765016,0.00019605191,0.9934821,0.000071497685,0.000016284135,0.000037842954,0.00046194386,0.0025797822,0.0015419241,0.0010035007,0.00036629333,0.0001051225],"about_ca_topic_score_codex":0.13050333,"about_ca_topic_score_gemma":0.8362386,"teacher_disagreement_score":0.7057353,"about_ca_system_score_codex":0.0000015050138,"about_ca_system_score_gemma":0.00046920846,"threshold_uncertainty_score":0.8752867},"labels":[],"label_agreement":null},{"id":"W3013664542","doi":"10.1139/cjes-2019-0067","title":"Geology, geochronology, and fluid inclusion studies of the Xiaorequanzi volcanogenic massive sulphide Cu–Zn deposit in the East Tianshan Terrane, China","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Geology; Geochemistry; Fluid inclusions; Sphalerite; Overprinting; Terrane; Pyrite; Chalcopyrite; Quartz; Inclusion (mineral); Hydrothermal circulation; Molybdenite; Galena; Mineralogy; Metamorphic rock; Copper; Paleontology; Tectonics","score_opus":0.027915829321084794,"score_gpt":0.21625197006693334,"score_spread":0.18833614074584853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3013664542","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9530685,0.008450661,0.00000395053,0.03775435,0.00010358503,0.000079394755,0.000014172375,0.000001515703,0.00052384974],"genre_scores_gemma":[0.99794644,0.00015008543,0.00010475452,0.0017137928,0.00007306309,2.6831577e-7,0.0000016209516,8.1105384e-7,0.00000918686],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986496,0.00018112853,0.0003661365,0.00019163259,0.00026944058,0.0003420603],"domain_scores_gemma":[0.9991926,0.00014990917,0.00021624772,0.000094594965,0.000072859824,0.00027380002],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006855911,0.00011957069,0.00028517103,0.00012353141,0.0006128834,0.000037578164,0.0008371641,0.000058191305,0.0005355743],"category_scores_gemma":[0.00034691417,0.00005537393,0.00010452552,0.00077422184,0.0019188548,0.00014746697,0.00007296678,0.0002639807,0.000005645384],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017709017,0.000004027573,0.9931107,0.000010237323,0.000026700964,0.000054829965,0.0030901036,0.0016927462,0.00034131733,0.00007293576,0.0000916254,0.0014870291],"study_design_scores_gemma":[0.00020927715,0.000386642,0.989661,0.00003306767,0.00003504112,0.00012001366,0.0024942812,0.0021161272,0.0002762576,0.004199081,0.0003803097,0.00008893817],"about_ca_topic_score_codex":0.037861668,"about_ca_topic_score_gemma":0.55650234,"teacher_disagreement_score":0.51864064,"about_ca_system_score_codex":0.000001935628,"about_ca_system_score_gemma":0.00029372465,"threshold_uncertainty_score":0.9685453},"labels":[],"label_agreement":null},{"id":"W3014341301","doi":"10.1139/cjes-2019-0136","title":"Metamorphic and structural evolution of the Flin Flon – Athapapuskow Lake area, west-central Manitoba","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Metamorphism; Metamorphic rock; Geology; Greenschist; Metamorphic facies; Isograd; Geochemistry; Mafic; Orogeny; Petrology; Facies; Geomorphology; Paleontology; Tectonics","score_opus":0.01948584688359027,"score_gpt":0.1698012999006558,"score_spread":0.1503154530170655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3014341301","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939751,0.0018603085,0.0000111216295,0.003457857,0.00019213269,0.00003752049,0.000040045863,0.0000017571681,0.0004241406],"genre_scores_gemma":[0.99937445,0.000016205073,0.00021732382,0.00027768474,0.00010012259,3.4256995e-8,0.0000016557848,5.58291e-7,0.000011941648],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990106,0.000060570546,0.00024479706,0.0001320757,0.00026747386,0.0002844761],"domain_scores_gemma":[0.9990969,0.000047209815,0.0001724377,0.00005296848,0.0000731751,0.0005573219],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023955264,0.00008365393,0.00018022265,0.00006719868,0.00024887247,0.000059575028,0.00037792328,0.000035309775,0.003172526],"category_scores_gemma":[0.00021811841,0.000044254473,0.000104657884,0.0005242788,0.0006475007,0.00018897258,0.0000086879,0.00015543458,0.00000674722],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000046007126,6.905467e-7,0.9958175,0.0000032690516,0.000010039029,0.000008752664,0.00008781163,0.0029131565,0.00009544047,0.00006499434,0.000026122481,0.0009676514],"study_design_scores_gemma":[0.00008300393,0.00014616268,0.9881828,0.000012534594,0.000031367887,0.000048970953,0.00025269794,0.0077163693,0.00015203087,0.0026803291,0.00062891486,0.00006481724],"about_ca_topic_score_codex":0.02010127,"about_ca_topic_score_gemma":0.76927054,"teacher_disagreement_score":0.7491693,"about_ca_system_score_codex":0.000001157884,"about_ca_system_score_gemma":0.00034603954,"threshold_uncertainty_score":0.9977387},"labels":[],"label_agreement":null},{"id":"W3014519110","doi":"10.1139/cjes-2018-0276","title":"Identification of sequence stratigraphy in the Dongying Formation of the Liaoxi low uplift, Bohai Bay Basin, China","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Sequence stratigraphy; Illite; Diachronous; Paleontology; Paleoclimatology; Sequence (biology); Sedimentary rock; Diagenesis; Stratigraphy; Sedimentary depositional environment; Structural basin; Tectonics; Climate change; Clay minerals","score_opus":0.029747346241378057,"score_gpt":0.21558792152873432,"score_spread":0.18584057528735626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3014519110","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948977,0.00043005485,0.0002224472,0.003262874,0.000110062334,0.00008318339,0.000032987657,9.653317e-7,0.00095972134],"genre_scores_gemma":[0.9994692,0.000035079458,0.00018565133,0.00028410566,0.00002131875,1.6112931e-7,0.0000015823372,3.744548e-7,0.000002484682],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989933,0.000091389615,0.0004290352,0.000062838924,0.00027954945,0.00014388897],"domain_scores_gemma":[0.9992558,0.00007817373,0.00039658853,0.00006886868,0.00009397551,0.000106616244],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009740612,0.000052534255,0.00010121908,0.000119290664,0.0002399649,0.00008891373,0.0006000829,0.000024937752,0.00016168992],"category_scores_gemma":[0.00025014125,0.00002669267,0.000056361212,0.001119474,0.00035505416,0.00074334245,0.0000026780438,0.00012497239,0.0000026791895],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000058177666,0.0000054971233,0.97105,0.00006321236,0.0000035198784,0.00000327911,0.0043426333,0.018510459,0.00031195904,0.0011387852,0.000056210432,0.0045086015],"study_design_scores_gemma":[0.00005665378,0.0001355779,0.9848723,0.00005179588,0.000005032614,0.00002186847,0.0015455753,0.009702564,0.0010366386,0.0022101253,0.00031918247,0.00004269726],"about_ca_topic_score_codex":0.002735731,"about_ca_topic_score_gemma":0.07800203,"teacher_disagreement_score":0.0752663,"about_ca_system_score_codex":6.1860976e-7,"about_ca_system_score_gemma":0.00042467102,"threshold_uncertainty_score":0.93882203},"labels":[],"label_agreement":null},{"id":"W3014873076","doi":"10.1139/cjes-2019-0236","title":"Timing of Cache Creek Ocean closure: insights from new Jurassic radiolarian ages in British Columbia and Yukon and their significance for Canadian Cordillera tectonics","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Centre National de la Recherche Scientifique","keywords":"Terrane; Geology; Paleontology; Pelagic sediment; Tectonics; Structural basin; Pelagic zone; Sedimentary rock; Oceanography","score_opus":0.022951327567484324,"score_gpt":0.1787469586356629,"score_spread":0.15579563106817856,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3014873076","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99136335,0.006240728,0.000011983227,0.001790796,0.0000656597,0.000100658224,0.00018155684,0.000002011603,0.00024327445],"genre_scores_gemma":[0.99833155,0.00011513971,0.0008681155,0.00056141673,0.0000862317,1.2395323e-7,0.0000116669635,0.0000017418167,0.000024041434],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988891,0.00005583015,0.00032844002,0.00024907113,0.00013559694,0.0003419452],"domain_scores_gemma":[0.998119,0.00022925674,0.00015883286,0.00005121103,0.000071597016,0.001370112],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024501726,0.00009065844,0.0003398294,0.00010048438,0.0003045218,0.00037992172,0.00027963758,0.000076261495,0.0009316135],"category_scores_gemma":[0.00033149665,0.000090642745,0.000062416955,0.00049963925,0.00044609077,0.00022508406,0.000005465797,0.00019461333,7.1073754e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004353836,0.0000019475283,0.98849416,0.000008189753,0.000018961564,0.000051169573,0.00048168434,0.00035883448,0.00008371317,0.0000024190467,0.0003488351,0.010145728],"study_design_scores_gemma":[0.000285319,0.0003311489,0.9865135,0.000064478845,0.00002159751,0.000024777415,0.0008295963,0.006658241,0.00005883745,0.0034654788,0.0015988731,0.00014815987],"about_ca_topic_score_codex":0.9720908,"about_ca_topic_score_gemma":0.99964017,"teacher_disagreement_score":0.027549399,"about_ca_system_score_codex":0.0000030822882,"about_ca_system_score_gemma":0.001192083,"threshold_uncertainty_score":0.99998164},"labels":[],"label_agreement":null},{"id":"W3015157671","doi":"10.1139/cjes-2019-0240","title":"The age of the Tseax volcanic eruption, British Columbia, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of British Columbia; University of Lethbridge; Simon Fraser University","funders":"","keywords":"Tephra; Geology; Lava; Dense-rock equivalent; Volcano; Explosive eruption; Vulcanian eruption; Effusive eruption; Geochemistry; Radiocarbon dating; Seismology; Paleontology; Magma","score_opus":0.02024916079129088,"score_gpt":0.19999276199636049,"score_spread":0.1797436012050696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3015157671","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98664945,0.002247212,0.000001293753,0.0077844374,0.0006058238,0.000064003834,0.000042494226,9.565164e-7,0.0026043453],"genre_scores_gemma":[0.9982981,0.000054993467,0.00002135436,0.0011194919,0.0000687524,9.980793e-8,0.0000013992418,8.2499923e-7,0.00043495608],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99874127,0.0001790202,0.00025519176,0.0001034824,0.00033913978,0.0003818962],"domain_scores_gemma":[0.9989895,0.00024719143,0.00015431822,0.000086296845,0.00013298941,0.00038967954],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000774648,0.00004586614,0.00013140391,0.000023297032,0.0012019604,0.00020355899,0.00093624066,0.00003900278,0.0016914951],"category_scores_gemma":[0.0005331235,0.000035079418,0.000048537077,0.0004998206,0.0014853436,0.00011156532,0.000007971443,0.00027192954,0.000008350581],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000018087466,4.7640586e-7,0.9963781,0.0000031479433,0.000007824161,0.000100590725,0.00008252949,0.00015614103,0.0000020278153,0.000016034392,0.002803448,0.00044784625],"study_design_scores_gemma":[0.00007365583,0.00009615479,0.9695357,0.000014670083,0.0000051116194,0.00023506748,0.00035178548,0.00009684343,0.00000871072,0.00017189884,0.02936757,0.00004280444],"about_ca_topic_score_codex":0.96262735,"about_ca_topic_score_gemma":0.9999899,"teacher_disagreement_score":0.03736252,"about_ca_system_score_codex":6.7231e-7,"about_ca_system_score_gemma":0.0065316316,"threshold_uncertainty_score":0.9992211},"labels":[],"label_agreement":null},{"id":"W3015765503","doi":"10.1139/cjes-2019-0130","title":"Petrogenesis and tectonic implications of the Late Triassic Nangou granodiorite porphyry in the Eastern Kunlun Orogenic Belt, northern Tibetan Plateau","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Petrogenesis; Subduction; Magmatism; Crust; Lithosphere; Partial melting; Plateau (mathematics); Continental crust; Adakite; Magma; Mantle (geology); Oceanic crust; Tectonics; Petrology; Paleontology","score_opus":0.02413364493497955,"score_gpt":0.19488924389949708,"score_spread":0.17075559896451753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3015765503","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98512644,0.0024070265,0.0000022678414,0.0118085025,0.00004968458,0.00006830829,0.00004945345,0.0000016036195,0.00048668863],"genre_scores_gemma":[0.9991363,0.000040933275,0.000033552144,0.00072028255,0.000045627494,2.6875983e-7,0.0000020483928,9.830893e-7,0.000019994419],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989223,0.0001046508,0.00032510064,0.00013737338,0.000237942,0.00027261704],"domain_scores_gemma":[0.9991908,0.00012993801,0.00020229268,0.00010309854,0.000062217194,0.00031162996],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000552534,0.00009252773,0.0001976709,0.0000992449,0.00027712356,0.00006781791,0.00068795524,0.000035807563,0.0004137788],"category_scores_gemma":[0.00011529211,0.00004451175,0.00013594162,0.0011123243,0.0005140581,0.000122016136,0.00001021834,0.00017131284,0.000008565503],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004468159,0.0000027784445,0.99610984,0.0000029612538,0.000012293633,0.0000061365154,0.00039588337,0.0008616962,0.00013239222,0.000020945752,0.000006520079,0.002444055],"study_design_scores_gemma":[0.0001331374,0.00012764927,0.9963715,0.000011802001,0.000033692704,0.00004743639,0.0004194748,0.00072589656,0.000112637426,0.0016064101,0.00034462594,0.00006572927],"about_ca_topic_score_codex":0.01723839,"about_ca_topic_score_gemma":0.6168856,"teacher_disagreement_score":0.5996472,"about_ca_system_score_codex":0.0000012138602,"about_ca_system_score_gemma":0.00037528746,"threshold_uncertainty_score":0.9893059},"labels":[],"label_agreement":null},{"id":"W3016299685","doi":"10.1139/cjes-2020-0017","title":"The Road River Group of northern Yukon, Canada: early Paleozoic deep-water sedimentation within the Great American Carbonate Bank","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University; Yukon University","funders":"","keywords":"Geology; Ordovician; Chemostratigraphy; Paleontology; Laurentia; Devonian; Facies; Paleozoic; Carbonate; Siliciclastic; Carbonate platform; Carbonate rock; Sedimentary rock; Isotopes of carbon; Structural basin; Total organic carbon","score_opus":0.01324299271722274,"score_gpt":0.18997736037213683,"score_spread":0.1767343676549141,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3016299685","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98949045,0.002651813,0.000007713246,0.0038830303,0.00043985035,0.00008466904,0.000018304912,0.0000020202792,0.0034221641],"genre_scores_gemma":[0.99939483,0.000019713383,0.0000932442,0.0003927658,0.000087226326,2.631458e-7,0.0000011348621,8.0857626e-7,0.000009983565],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99854785,0.00017250281,0.0003559829,0.00014296155,0.00040996732,0.00037074691],"domain_scores_gemma":[0.99890697,0.000128355,0.0003208538,0.00008962285,0.0001011291,0.0004530611],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006645457,0.0001136303,0.00018022295,0.000068793,0.00081903127,0.00009605479,0.00060641987,0.000026940079,0.000063882755],"category_scores_gemma":[0.00006062177,0.000054237364,0.00007390629,0.0003808854,0.001971046,0.0002413244,0.0000014576436,0.00021021861,0.0000024008457],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025620837,7.7623554e-7,0.9781131,0.0000018454315,0.000031524392,0.00004694524,0.002417984,0.0010319989,0.000015658565,0.00004542091,0.000027398282,0.018241713],"study_design_scores_gemma":[0.00014207137,0.0003672167,0.9962356,0.000008276773,0.00001996111,0.000033745022,0.0013292675,0.0010603365,0.00008408234,0.00016040863,0.00047681268,0.00008218433],"about_ca_topic_score_codex":0.8395164,"about_ca_topic_score_gemma":0.9992642,"teacher_disagreement_score":0.15974775,"about_ca_system_score_codex":0.0000024691556,"about_ca_system_score_gemma":0.0014171258,"threshold_uncertainty_score":0.72624004},"labels":[],"label_agreement":null},{"id":"W3016662006","doi":"10.1139/cjes-2019-0176","title":"Long-term nivation rates, Cathedral Massif, northwestern British Columbia","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Denudation; Deglaciation; Massif; Landform; Ridge; Geomorphology; Glacial period; Drainage; Bedrock; Physical geography; Paleontology; Tectonics","score_opus":0.03387449965212755,"score_gpt":0.23557934419144025,"score_spread":0.2017048445393127,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3016662006","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99461526,0.0011438925,0.000019584208,0.0017719595,0.0003853346,0.00007048915,0.00003737565,0.000005002049,0.0019511248],"genre_scores_gemma":[0.9985331,0.00004295941,0.0001913572,0.00077796465,0.00015288885,1.4228645e-7,0.000013582462,0.0000016010916,0.00028636304],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99869,0.00012023846,0.0002783298,0.00018429267,0.00024735247,0.00047978392],"domain_scores_gemma":[0.99867904,0.00009721928,0.00015115835,0.000060644204,0.00012570045,0.0008862354],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00056101603,0.00006980748,0.00018552075,0.00009953743,0.00060109555,0.0005123954,0.00050727965,0.00007861473,0.006098975],"category_scores_gemma":[0.0001343292,0.000080786194,0.00006143148,0.00046476405,0.0007841989,0.00046290312,0.0000051995526,0.00027376297,0.0001558056],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004120663,0.0000018170176,0.9975128,0.0000073179135,0.0000082715405,0.0005769259,0.0001952742,0.000162447,0.0000015219543,0.000003174122,0.00025432944,0.0012720085],"study_design_scores_gemma":[0.00017324975,0.00033264267,0.99731517,0.000025439609,0.0000069396774,0.0007505165,0.00011226068,0.00025509007,0.000005812266,0.00010721425,0.000821995,0.00009366323],"about_ca_topic_score_codex":0.079424955,"about_ca_topic_score_gemma":0.9938937,"teacher_disagreement_score":0.9144687,"about_ca_system_score_codex":4.1336182e-7,"about_ca_system_score_gemma":0.0014450778,"threshold_uncertainty_score":0.99480957},"labels":[],"label_agreement":null},{"id":"W3016677756","doi":"10.1139/cjes-2019-0158","title":"Filling process and filling characteristic analysis of Paleogene Baxian sag in Bohai Bay basin, China","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science and Technology Major Project; PetroChina Company Limited","keywords":"Geology; Paleogene; Rift; Paleontology; Facies; Sedimentary depositional environment; Sedimentary rock; Structural basin; Tectonics; Provenance; Alluvial fan; Fluvial; Fault block; Fault (geology); Geomorphology; Petrology","score_opus":0.020663984192253366,"score_gpt":0.20405807070583953,"score_spread":0.18339408651358616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3016677756","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959247,0.001523807,0.000031860123,0.0016914527,0.00006953752,0.000039448256,0.000053378404,0.0000018056538,0.00066400936],"genre_scores_gemma":[0.9992741,0.00009717781,0.00024299083,0.00031008056,0.000062503095,1.08324095e-7,0.0000035674623,7.5646244e-7,0.00000874774],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989161,0.000048079517,0.00033808235,0.00017792535,0.00021491009,0.00030493902],"domain_scores_gemma":[0.99909234,0.000115213785,0.00018809126,0.000037323847,0.000066159126,0.0005008912],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003635418,0.00009733291,0.00037737194,0.00025239075,0.00021275663,0.00006350769,0.00024106067,0.00003166092,0.0011231606],"category_scores_gemma":[0.00031428863,0.000065710556,0.000080852034,0.0015419448,0.0003828892,0.00019474934,0.000005435053,0.00013835683,0.000006761215],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007693106,0.0000028097609,0.98277473,0.000012195551,0.000035233476,0.000034432964,0.000759462,0.010682077,0.000008443957,0.000005027472,0.000001905883,0.005675982],"study_design_scores_gemma":[0.000072739975,0.00025325536,0.9831832,0.000029426395,0.000053476953,0.0000044571057,0.0003805844,0.015465615,0.000030478019,0.00019343279,0.00024741527,0.00008588736],"about_ca_topic_score_codex":0.0051938314,"about_ca_topic_score_gemma":0.13401626,"teacher_disagreement_score":0.12882243,"about_ca_system_score_codex":6.340381e-7,"about_ca_system_score_gemma":0.00018650317,"threshold_uncertainty_score":0.99978995},"labels":[],"label_agreement":null},{"id":"W3018598613","doi":"10.1139/cjes-2019-0043","title":"Timing of magmatic crystallization and Sn–W–Mo greisen vein formation within the Mount Douglas Granite, New Brunswick, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"Natural Resources Canada","keywords":"Geology; Monazite; Greisen; Geochemistry; Zircon; Geochronology; Hydrothermal circulation; Cassiterite; Pegmatite; Uraninite; Fluid inclusions; Uranium; Paleontology; Tin","score_opus":0.02149046059751929,"score_gpt":0.17738711870611856,"score_spread":0.15589665810859926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3018598613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9919971,0.00092281116,0.0002542471,0.005834926,0.00009208977,0.000050650233,0.000008984754,0.000001641334,0.0008375058],"genre_scores_gemma":[0.99842185,0.000015973765,0.0006106112,0.0008449973,0.00007536582,2.359045e-8,0.0000036523363,6.669959e-7,0.000026889893],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990775,0.000048350823,0.00031891686,0.0000889413,0.0002905364,0.00017575653],"domain_scores_gemma":[0.99904525,0.000094610165,0.00025623088,0.000037388632,0.00008388477,0.0004826335],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033546277,0.00007233955,0.00014943782,0.000066990426,0.0002363883,0.000090667345,0.00025893704,0.000022452738,0.0007271544],"category_scores_gemma":[0.00026230674,0.000041423096,0.00003595585,0.00051295134,0.00022423026,0.00029351702,0.000004984834,0.00010471407,0.0000028623879],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002102018,0.000003318009,0.91403,0.000059220893,0.000036528676,0.00003905371,0.0024742268,0.07547563,0.00034767936,0.001099755,0.000977543,0.0054359874],"study_design_scores_gemma":[0.00030095875,0.00040428,0.8160485,0.0000840335,0.00007416532,0.00011076918,0.002490662,0.16725266,0.0007223408,0.007402765,0.004889113,0.0002197458],"about_ca_topic_score_codex":0.869248,"about_ca_topic_score_gemma":0.99602216,"teacher_disagreement_score":0.12677419,"about_ca_system_score_codex":0.0000024420979,"about_ca_system_score_gemma":0.002019869,"threshold_uncertainty_score":0.79618305},"labels":[],"label_agreement":null},{"id":"W3020079923","doi":"10.1139/cjes-2019-0233","title":"Draining and filling of ice-dammed lakes at the terminus of surge-type Dań Zhùr (Donjek) Glacier, Yukon, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Waterloo; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; University of Ottawa; Polar Knowledge Canada; University of Washington; Parks Canada; National Science Foundation","keywords":"Surge; Glacier; Geology; Glacier terminus; Cirque glacier; Glacier ice accumulation; Structural basin; Shelf ice; Moraine; Terminal moraine; Accumulation zone; Physical geography; Tidewater glacier cycle; Oceanography; Hydrology (agriculture); Geomorphology; Ice stream; Sea ice; Cryosphere; Geography; Ice calving","score_opus":0.04041539589662023,"score_gpt":0.20523652084645727,"score_spread":0.16482112494983703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3020079923","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9899664,0.006019853,0.000006480766,0.002807207,0.0005002846,0.000046975914,0.00007137198,0.0000011486582,0.0005802868],"genre_scores_gemma":[0.9988006,0.00014656727,0.00023673414,0.00064335746,0.00008067983,5.093583e-8,0.0000024904625,0.0000014068696,0.0000881174],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989598,0.00004097486,0.00033610867,0.00011271113,0.00029445664,0.00025599572],"domain_scores_gemma":[0.99869573,0.0004471438,0.00028743956,0.00006503205,0.00014044483,0.0003642265],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005027147,0.000080685655,0.00021131999,0.00003741698,0.00047928013,0.000040111903,0.00027813154,0.00002203465,0.0006623697],"category_scores_gemma":[0.0005107379,0.000052197738,0.000036641162,0.00053678715,0.00052102486,0.00014465548,0.000010052468,0.000098807155,8.611802e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008848437,8.4852655e-7,0.9850751,0.0000126037085,0.00001906016,0.000033819426,0.0015226275,0.0068484372,0.00003658533,0.000013239375,0.0019482767,0.0044805603],"study_design_scores_gemma":[0.00014955302,0.0002441856,0.9128633,0.000046263736,0.000022000837,0.000037942234,0.0046283198,0.0043350267,0.00009671832,0.000031829975,0.077437766,0.00010705317],"about_ca_topic_score_codex":0.62138265,"about_ca_topic_score_gemma":0.992705,"teacher_disagreement_score":0.37132233,"about_ca_system_score_codex":0.0000026162797,"about_ca_system_score_gemma":0.0020081098,"threshold_uncertainty_score":0.7252484},"labels":[],"label_agreement":null},{"id":"W3020184806","doi":"10.1139/cjes-2019-0124","title":"Petrogenesis and geodynamic setting of granitoids at Machangqing Cu–Mo (Au) deposit, western Yangtze craton, southwestern China: constraints from zircon U–Pb and molybdenite Re–Os geochronology, Lu–Hf isotopes, and geochemistry","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Regina","funders":"","keywords":"Geology; Zircon; Geochemistry; Craton; Molybdenite; Porphyritic; Geochronology; Petrogenesis; Partial melting; Crust; Mantle (geology); Petrology; Fluid inclusions; Hydrothermal circulation; Quartz; Tectonics","score_opus":0.01064241135726123,"score_gpt":0.1818019600142028,"score_spread":0.17115954865694155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3020184806","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933234,0.004796098,0.00005932112,0.0012510222,0.0000594885,0.000065274035,0.000279681,0.0000049036976,0.00016083312],"genre_scores_gemma":[0.99884737,0.000122413,0.0006035197,0.00030585122,0.000086491054,2.166593e-7,0.000018612878,0.00000264573,0.000012888366],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99850714,0.000074686315,0.00040013832,0.00036995864,0.00021729425,0.00043079664],"domain_scores_gemma":[0.99861914,0.000159286,0.0002922736,0.00007341685,0.00006151406,0.0007943804],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030038747,0.00019165724,0.00041819605,0.00012440361,0.00035269672,0.0001255148,0.00026170182,0.000105134284,0.00065997377],"category_scores_gemma":[0.000119361575,0.00014895576,0.00007337127,0.0002706247,0.0011680558,0.00024951893,0.00004473076,0.00020337802,0.000004963181],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000127923395,0.0000022652428,0.98744494,0.000033905864,0.000038009344,0.00006262848,0.000667473,0.00012758636,0.006968204,0.000001371668,0.0000031998368,0.0046376223],"study_design_scores_gemma":[0.00032029318,0.00021431221,0.9900629,0.00007862889,0.00008122649,0.0002613548,0.0012903785,0.0041902564,0.0029609108,0.0003089813,0.000036921952,0.0001938366],"about_ca_topic_score_codex":0.06144926,"about_ca_topic_score_gemma":0.4123384,"teacher_disagreement_score":0.35088915,"about_ca_system_score_codex":0.0000035468963,"about_ca_system_score_gemma":0.00019100662,"threshold_uncertainty_score":0.9448006},"labels":[],"label_agreement":null},{"id":"W3022745857","doi":"10.1139/cjes-2019-0200","title":"Geochronology, geochemistry, and Hf isotopic compositions of early Permian syenogranite and diabase from the northern Great Xing’an Range, northeastern China: petrogenesis and tectonic implications","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"People's Government of Jilin Province; National Natural Science Foundation of China; Natural Science Foundation of Jilin Province","keywords":"Zircon; Geology; Geochemistry; Petrogenesis; Carboniferous; Permian; Geochronology; Paleozoic; Partial melting; Magmatism; Mantle (geology); Tectonics; Paleontology","score_opus":0.016964104671216434,"score_gpt":0.19500648510751553,"score_spread":0.1780423804362991,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3022745857","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9892802,0.004349099,0.000013127216,0.0058805556,0.00001788652,0.000052658157,0.00022041528,0.0000029868054,0.00018305694],"genre_scores_gemma":[0.9993833,0.00010348115,0.00022276747,0.00020747857,0.00006550896,3.6902023e-7,0.000012224878,0.0000012142829,0.0000036613587],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999207,0.000056124092,0.00021204255,0.00019908075,0.0001096476,0.00021609863],"domain_scores_gemma":[0.9990221,0.00011586926,0.00012877163,0.00008540811,0.00006642814,0.0005814109],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014852697,0.00010181728,0.00019764039,0.00005668171,0.00045364356,0.00010014917,0.00024757383,0.000039713115,0.00051692384],"category_scores_gemma":[0.000056179502,0.00006378125,0.000050299834,0.00026463653,0.0010246915,0.00015225452,0.0000137332,0.00013169859,0.0000023292391],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005423469,0.0000028318618,0.9946553,0.000004258647,0.000019366105,0.000009423151,0.00040121554,0.000076930955,0.00025465348,0.000008303238,0.0000016936652,0.004560616],"study_design_scores_gemma":[0.00013698326,0.0002538417,0.9969685,0.000014321878,0.000057440862,0.00008981198,0.00028272122,0.0010752167,0.00008461893,0.00087311596,0.00008369545,0.000079717756],"about_ca_topic_score_codex":0.07821728,"about_ca_topic_score_gemma":0.5022624,"teacher_disagreement_score":0.42404512,"about_ca_system_score_codex":7.530102e-7,"about_ca_system_score_gemma":0.00014692429,"threshold_uncertainty_score":0.92792094},"labels":[],"label_agreement":null},{"id":"W3023458719","doi":"10.1139/cjes-2019-0214","title":"Research on the lithofacies and paleogeography of the lower Cambrian Xiaoerbulake Formation in the northern Tarim Basin, northwestern China","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Dolomite; Facies; Sedimentary depositional environment; Lithology; Outcrop; Sedimentary rock; Carbonate platform; Geomorphology; Shoal; Paleontology; Structural basin; Dolostone; Geochemistry; Carbonate rock","score_opus":0.035110203088338905,"score_gpt":0.2402388705387871,"score_spread":0.2051286674504482,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3023458719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98750025,0.00029348626,0.000036023972,0.0105750095,0.00007485755,0.00007907591,0.000005901048,0.0000018494899,0.001433525],"genre_scores_gemma":[0.9995846,0.00004881569,0.000009642371,0.00030407327,0.00004156908,0.0000011205448,2.874083e-7,0.0000027864432,0.000007112978],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989605,0.00016847646,0.00021787563,0.00006198902,0.0004074091,0.00018376639],"domain_scores_gemma":[0.99953705,0.00008340794,0.000059933718,0.000109697365,0.00007687226,0.00013305784],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011515345,0.0000614984,0.0000991708,0.00023925793,0.00029775058,0.00014604627,0.00046942593,0.000024075587,0.000021551168],"category_scores_gemma":[0.000083958024,0.000027567285,0.0000686923,0.0013381154,0.0003844905,0.00020336467,0.000009131595,0.00028452498,0.0000020251612],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012823859,0.000018893617,0.7869553,0.000044000255,0.000057118832,0.00004783013,0.04519139,0.16459529,0.00023788212,0.00070949184,0.0003931116,0.0017368753],"study_design_scores_gemma":[0.00021594188,0.00034630526,0.93744147,0.00013190719,0.0000180766,0.000032689422,0.018614758,0.033772573,0.00041895546,0.00026275762,0.008608242,0.0001363222],"about_ca_topic_score_codex":0.0024062872,"about_ca_topic_score_gemma":0.47310686,"teacher_disagreement_score":0.4707006,"about_ca_system_score_codex":0.000003999647,"about_ca_system_score_gemma":0.00014704974,"threshold_uncertainty_score":0.53650755},"labels":[],"label_agreement":null},{"id":"W3023618031","doi":"10.1139/e2012-070","title":"A revised biostratigraphic and well-log sequence-stratigraphic framework for the Scotian Margin, offshore eastern Canada <sup>1</sup>This article is one of a series of papers published in this CJES Special Issue on the theme of <i>Mesozoic–Cenozoic geology of the Scotian Basin</i>. <sup>2</sup>Earth Sciences Sector Contribution 20120137.","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Saint Mary's University","funders":"","keywords":"Unconformity; Geology; Paleontology; Cenomanian; Aptian; Micropaleontology; Cretaceous; Cenozoic; Sequence (biology); Biostratigraphy; Sequence stratigraphy; Structural basin; Sedimentary depositional environment; Foraminifera; Oceanography","score_opus":0.021200290592811217,"score_gpt":0.20811905429284958,"score_spread":0.18691876370003835,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3023618031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9834148,0.0025237033,0.000007404208,0.01166186,0.00031644592,0.00046332,0.00026124634,0.000001984281,0.0013491976],"genre_scores_gemma":[0.9985446,0.0002291503,0.0003706783,0.00057800225,0.00021546784,0.0000019820268,0.0000033768945,0.000002586908,0.000054187723],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99732333,0.00031350707,0.0008424058,0.00022568078,0.0006645567,0.0006305071],"domain_scores_gemma":[0.9973048,0.0009998609,0.00078565604,0.0002470832,0.0003662931,0.0002963231],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0026886608,0.00020844536,0.00047898613,0.0003220236,0.00064057333,0.00012357105,0.00093336095,0.00012577373,0.006985417],"category_scores_gemma":[0.0010346224,0.00010606046,0.00013986968,0.0017372268,0.004141242,0.0007843935,0.00001721138,0.00032429933,0.0000017023588],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006565583,0.00002442756,0.9896845,0.000077745375,0.000043326985,0.0000012210799,0.0028841884,0.0026358215,0.000052071195,0.0029947981,0.000632032,0.00090418867],"study_design_scores_gemma":[0.00051467796,0.0015954386,0.9624504,0.0006929966,0.00008792268,0.000066396395,0.01108762,0.0054826173,0.0039426433,0.004651507,0.009130614,0.00029716193],"about_ca_topic_score_codex":0.17703901,"about_ca_topic_score_gemma":0.7593339,"teacher_disagreement_score":0.5822949,"about_ca_system_score_codex":0.0000038521202,"about_ca_system_score_gemma":0.0020955165,"threshold_uncertainty_score":0.9985689},"labels":[],"label_agreement":null},{"id":"W3023916583","doi":"10.1139/cjes-2019-0087","title":"Origin and paleoenvironmental reconstruction of phosphorus-bearing sandstones of the Cambrian Xinji Formation, southwestern margin of the Ordos Basin, China","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"China Geological Survey; National Science and Technology Major Project; National Natural Science Foundation of China","keywords":"Geology; Geochemistry; Clastic rock; Sedimentary rock; Paleoclimatology; Provenance; Climate change","score_opus":0.011080861419596397,"score_gpt":0.17042667567478786,"score_spread":0.15934581425519145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3023916583","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998254,0.00035558493,0.000007718302,0.0007260276,0.00012144164,0.000043938133,0.00006364221,4.725601e-7,0.0004271762],"genre_scores_gemma":[0.9997493,0.000036282818,0.00011310536,0.000052034637,0.000025744279,4.7701853e-8,0.0000010072719,6.73875e-7,0.000021801325],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992137,0.000041054154,0.00031346493,0.00007794965,0.00022554082,0.00012830092],"domain_scores_gemma":[0.9993427,0.000018681681,0.00039516645,0.00006581798,0.000025372667,0.0001523068],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029596078,0.00006252518,0.00014216127,0.00004561006,0.00021494966,0.000024464633,0.0002753869,0.000021116428,0.00038797938],"category_scores_gemma":[0.000038072776,0.00003598605,0.000079212565,0.00032773995,0.00060655246,0.00024457343,0.000009547118,0.00008187389,7.5399345e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005789171,0.0000015850164,0.9952386,0.000014153048,0.000010374716,6.01389e-7,0.0006183785,0.0005091673,0.00069308275,0.0000045758607,0.000007578829,0.0028961324],"study_design_scores_gemma":[0.00012785169,0.000072172144,0.9838309,0.000057986526,0.000025385341,0.000060850365,0.0023706744,0.00065157685,0.012537862,0.00004938593,0.00017301473,0.00004230987],"about_ca_topic_score_codex":0.012177294,"about_ca_topic_score_gemma":0.06914543,"teacher_disagreement_score":0.056968138,"about_ca_system_score_codex":0.0000014277736,"about_ca_system_score_gemma":0.00018430506,"threshold_uncertainty_score":0.9944007},"labels":[],"label_agreement":null},{"id":"W3026695328","doi":"10.1139/cjes-2018-0247","title":"Ore geology, fluid inclusion, and stable isotope constraints on the origin of the Damoqujia gold deposit, Jiaodong Peninsula, China","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Fluid inclusions; Mesothermal; Geochemistry; Meteoric water; Quartz; Pyrite; Metamorphic rock; Inclusion (mineral); Magmatic water; Carbonate; Mineralogy; Mineralization (soil science); Isotopes of oxygen; Homogeneous; Groundwater; Chemistry","score_opus":0.017708202274410757,"score_gpt":0.192468023602298,"score_spread":0.17475982132788725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3026695328","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9732082,0.0010541907,0.0000056863414,0.020145476,0.00010929005,0.00006913666,0.000028253771,0.0000018852295,0.005377887],"genre_scores_gemma":[0.9976029,0.000039392715,0.00014165915,0.0021091637,0.000059966544,1.02801e-7,0.0000011590602,8.1022677e-7,0.000044867473],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99881977,0.00012325925,0.00028315195,0.0001664954,0.00030794638,0.00029936546],"domain_scores_gemma":[0.9989749,0.00019333305,0.00018717017,0.000093291856,0.00007606836,0.00047519567],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006310092,0.00010371876,0.00020750081,0.000063505286,0.00069241883,0.00006879585,0.0007197961,0.000044648485,0.0046874085],"category_scores_gemma":[0.00046193786,0.000045747474,0.00008723197,0.0006208764,0.0017648999,0.00012319809,0.00005102781,0.00024359195,0.00001238121],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009018745,0.0000029400562,0.9953351,0.0000040930217,0.000014079867,0.00002173875,0.00037648092,0.0013453069,0.00025867182,0.0005916716,0.00033992223,0.0017009985],"study_design_scores_gemma":[0.00011654724,0.0003221453,0.9878449,0.000030231698,0.000022157099,0.00006674509,0.00032003105,0.0036958973,0.0008847413,0.003969114,0.0026359286,0.00009160308],"about_ca_topic_score_codex":0.023947284,"about_ca_topic_score_gemma":0.11436175,"teacher_disagreement_score":0.090414464,"about_ca_system_score_codex":0.0000010228556,"about_ca_system_score_gemma":0.00038654584,"threshold_uncertainty_score":0.99622244},"labels":[],"label_agreement":null},{"id":"W3028893678","doi":"10.1139/cjes-2019-0188","title":"Between the supercontinents: Mesoproterozoic Deer Trail Group, an intermediate age unit between the Mesoproterozoic Belt–Purcell Supergroup and the Neoproterozoic Windermere Supergroup in northeastern Washington, USA","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Rodinia; Supercontinent; Supergroup; Geology; Laurentia; Craton; Zircon; Paleontology; Proterozoic; Group (periodic table); Stromatolite; Paleozoic; Tectonics","score_opus":0.030341257849298194,"score_gpt":0.21075235312419857,"score_spread":0.18041109527490037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3028893678","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97840583,0.0011621255,0.000032095777,0.019612757,0.00013095394,0.0003174933,0.00006226543,0.000008346864,0.00026811333],"genre_scores_gemma":[0.996658,0.000054463962,0.00008851683,0.002500429,0.00060829363,0.0000043900436,0.000030362085,0.0000072322164,0.000048302238],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9960357,0.00084673346,0.0009185868,0.0005193994,0.0007321995,0.00094739924],"domain_scores_gemma":[0.99761134,0.00060764916,0.00027540937,0.00029972428,0.00010340902,0.0011024801],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0028348586,0.00037674198,0.00067747454,0.00020788051,0.0011560969,0.00071144436,0.0022766176,0.00013667114,0.0014456426],"category_scores_gemma":[0.00034069625,0.00016526031,0.00024750287,0.0011753788,0.0030722115,0.0008779704,0.000065501445,0.0010619865,0.00004165176],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003085188,0.00000564987,0.98689735,0.000010411534,0.00005091366,0.00007973319,0.0032288318,0.00020182718,0.000026034371,0.000029608464,0.000009844314,0.009428949],"study_design_scores_gemma":[0.0008193308,0.00053025986,0.9911672,0.000050089086,0.00010319394,0.000044081688,0.0017628561,0.0014423305,0.000028413802,0.0019958622,0.0018054097,0.00025098605],"about_ca_topic_score_codex":0.06406666,"about_ca_topic_score_gemma":0.6212328,"teacher_disagreement_score":0.55716616,"about_ca_system_score_codex":0.000003874002,"about_ca_system_score_gemma":0.00022310246,"threshold_uncertainty_score":0.9996409},"labels":[],"label_agreement":null},{"id":"W3034268422","doi":"10.1139/cjes-2019-0177","title":"Carbonate burial dissolution related to faults and fractures in the Triassic Daye Formation of the Huandiqiao Section, Huangshi Area, Hubei, China","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Geology; Cementation (geology); Dissolution; Karst; Carbonate; Geochemistry; Hydrothermal circulation; Calcite; Fault (geology); Mineralogy; Paleontology; Cement; Materials science; Chemistry; Composite material; Metallurgy","score_opus":0.01503390631011372,"score_gpt":0.2212379451185401,"score_spread":0.2062040388084264,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3034268422","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928457,0.000273996,0.0002574853,0.0053636106,0.0002804622,0.00008698756,0.000004255273,0.000003701651,0.00088379596],"genre_scores_gemma":[0.99974525,0.000021335762,0.000017809236,0.0001377856,0.000065314955,8.757562e-7,8.134238e-7,0.0000024610893,0.000008333646],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99925417,0.00006859221,0.00027496598,0.000059060545,0.00021606628,0.00012712152],"domain_scores_gemma":[0.99963456,0.000025257721,0.0000921297,0.000054894866,0.00003584974,0.00015729952],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048279986,0.000060030605,0.00011319928,0.00019297155,0.00015666167,0.00005882742,0.00020643591,0.000037372785,0.000020332367],"category_scores_gemma":[0.00018404194,0.000033470533,0.000050858842,0.00091158977,0.00007932509,0.0002897598,0.0000052334935,0.00017016537,5.4988766e-7],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018211304,0.0000050739095,0.011745761,0.000018282626,0.000029675683,0.000010066704,0.030293567,0.95409936,0.0022533282,0.00015215884,0.0006914853,0.0006830404],"study_design_scores_gemma":[0.0011343013,0.00037132486,0.4641267,0.00018620939,0.00007371572,0.000066964465,0.006084856,0.5176697,0.002565357,0.0014732847,0.0059719854,0.00027563065],"about_ca_topic_score_codex":0.0008819586,"about_ca_topic_score_gemma":0.046260014,"teacher_disagreement_score":0.45238096,"about_ca_system_score_codex":0.000008891606,"about_ca_system_score_gemma":0.0001238579,"threshold_uncertainty_score":0.97114325},"labels":[],"label_agreement":null},{"id":"W3034932439","doi":"10.1139/cjes-2020-0020","title":"Direct evidence of sediment carbonate dissolution in response to bottom-water acidification in the Gulf of St. Lawrence, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Carbonate; Aragonite; Calcite; Geology; Bottom water; Ocean acidification; Oceanography; Carbonate minerals; Dissolution; Calcium carbonate; Sediment; Sedimentary rock; Seafloor spreading; Carbon cycle; Diagenesis; Dissolved organic carbon; Carbon dioxide; Mineralogy; Geochemistry; Seawater; Paleontology; Chemistry; Ecosystem; Ecology","score_opus":0.029104315396634335,"score_gpt":0.2345749558637613,"score_spread":0.20547064046712696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3034932439","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9888851,0.0007443616,0.000008315358,0.009792771,0.00015186613,0.00014093505,0.000036520305,8.096757e-7,0.00023928715],"genre_scores_gemma":[0.9994265,0.000025939387,0.00011798746,0.00038765644,0.000024526753,3.4133691e-7,0.0000013508295,0.0000010225086,0.0000146667435],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982745,0.0004736425,0.00041929117,0.000137592,0.0004474696,0.00024747764],"domain_scores_gemma":[0.9989053,0.0004706636,0.00017223644,0.00009706651,0.00008818778,0.00026655683],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0028979315,0.00007438668,0.0001725826,0.00029278992,0.000085621665,0.00003663284,0.00048555864,0.00002499273,0.00013243225],"category_scores_gemma":[0.00061603356,0.000042677962,0.000031441505,0.000880957,0.0002113331,0.00022654646,0.0000038874473,0.000113496804,0.0000022365314],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007571801,0.000014239375,0.905813,0.000047024783,0.000009297451,0.00010189082,0.0077793347,0.06756117,0.015036744,0.00004554055,0.0004776642,0.0023569355],"study_design_scores_gemma":[0.00011144456,0.00045753104,0.9890923,0.00013916034,0.0000043872174,0.000008552649,0.0009897212,0.0015307602,0.0055701244,0.00002075738,0.0020052907,0.000070009344],"about_ca_topic_score_codex":0.43864912,"about_ca_topic_score_gemma":0.94256073,"teacher_disagreement_score":0.5039116,"about_ca_system_score_codex":0.000007987838,"about_ca_system_score_gemma":0.0023522545,"threshold_uncertainty_score":0.5650889},"labels":[],"label_agreement":null},{"id":"W3035371951","doi":"10.1139/cjes-2019-0227","title":"Baffin Bay late Neogene palynostratigraphy at Ocean Drilling Program Site 645","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Biozone; Paleontology; Dinocyst; Pleistocene; Neogene; Early Pleistocene; Unconformity; Hiatus; Late Miocene; Biostratigraphy; Oceanography; Palynology; Sedimentary rock; Structural basin","score_opus":0.032111813370554604,"score_gpt":0.2368904243973243,"score_spread":0.2047786110267697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035371951","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9867287,0.002949643,0.0000056654203,0.00473168,0.0003207127,0.0001172171,0.000022192735,0.000011486404,0.005112698],"genre_scores_gemma":[0.9974089,0.00009627754,0.0012859819,0.0009578934,0.00013944581,1.3077886e-7,0.00000979575,0.0000019902038,0.00009952911],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982511,0.00015904468,0.0003390574,0.0002448382,0.00030668528,0.0006992942],"domain_scores_gemma":[0.99830616,0.00015404237,0.00017157935,0.0000857424,0.00010780173,0.001174702],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008124385,0.00013519784,0.00024506162,0.00028574586,0.00078148587,0.0001474309,0.0005366152,0.000099232995,0.002481993],"category_scores_gemma":[0.00016142112,0.000102819446,0.00011961185,0.0008335992,0.000983491,0.00030587454,0.0000077510285,0.0003319394,0.00022195073],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014685407,0.0000024287974,0.99464417,0.000007597144,0.000015663927,0.00032245897,0.00042828146,0.003075824,0.000011369509,0.000015990694,0.00020650675,0.0012550149],"study_design_scores_gemma":[0.00019643469,0.0008436875,0.97798383,0.000022182021,0.000013388623,0.0002676049,0.00014399124,0.0042774305,0.00014707568,0.00012484183,0.015828671,0.0001508418],"about_ca_topic_score_codex":0.0009818659,"about_ca_topic_score_gemma":0.44045794,"teacher_disagreement_score":0.43947607,"about_ca_system_score_codex":3.666866e-7,"about_ca_system_score_gemma":0.0009693155,"threshold_uncertainty_score":0.9984299},"labels":[],"label_agreement":null},{"id":"W3035442690","doi":"10.1139/cjes-2020-0065","title":"Upper Ordovician (Sandbian–Katian) carbonate outliers in the northern Ottawa–Bonnechere graben (central Canada): records of transgressions and sedimentation patterns in the Laurentian platform interior","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada; Hefei University of Technology; Hefei University; University of Ottawa","keywords":"Geology; Siliciclastic; Paleontology; Marine transgression; Facies; Chemostratigraphy; Ooid; Ordovician; Sedimentary rock; Carbonate platform; Sedimentary depositional environment; Structural basin","score_opus":0.021842522854328777,"score_gpt":0.2176120989103537,"score_spread":0.19576957605602494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035442690","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98887056,0.0013817655,0.000005104219,0.0067586475,0.00021383318,0.00011700044,0.00007560073,8.3827643e-7,0.0025766615],"genre_scores_gemma":[0.9992076,0.000030919593,0.000063569496,0.0006545864,0.00003758845,3.800504e-7,0.0000031641025,6.792758e-7,0.0000014700861],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873763,0.00016187924,0.0003523714,0.00012966135,0.0002862839,0.0003321927],"domain_scores_gemma":[0.9993591,0.00012961167,0.00016779955,0.000061448794,0.000025152047,0.00025692437],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006602204,0.00010014344,0.0001672375,0.00014910028,0.00024290953,0.000073006835,0.00049305975,0.000046595225,0.00013436237],"category_scores_gemma":[0.00005209893,0.000057500823,0.000047957186,0.00042480323,0.00031261425,0.00026169463,7.186183e-7,0.0002871324,1.9076967e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010391749,0.0000019703396,0.9773876,0.000006718501,0.0000073181673,0.00007880709,0.010866549,0.00015197985,0.000003233853,0.000016700014,0.000030389716,0.011438333],"study_design_scores_gemma":[0.00023164204,0.00020841323,0.97871035,0.000062749445,0.000010410055,0.0000378779,0.019512808,0.0008148883,0.000008294872,0.00010634387,0.00022531714,0.000070908995],"about_ca_topic_score_codex":0.7181943,"about_ca_topic_score_gemma":0.9998588,"teacher_disagreement_score":0.28166452,"about_ca_system_score_codex":0.0000033708823,"about_ca_system_score_gemma":0.0012750961,"threshold_uncertainty_score":0.2836823},"labels":[],"label_agreement":null},{"id":"W3035512785","doi":"10.1139/cjes-2018-0084","title":"Hyperpycnal flow depositional characteristics and model in an ancient continental basin: a record from the Oligocene Lower Huagang Formation in the Xihu Sag, East China Sea Shelf Basin","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Turbidity current; Sedimentary depositional environment; Ripple marks; Structural basin; Bedding; Sedimentary rock; Sedimentary structures; Lithology; Graded bedding; Lamination; Bedform; Facies; Geomorphology; Turbidite; Continental shelf; Paleontology; Geochemistry; Sediment; Sediment transport; Oceanography","score_opus":0.02396500498942229,"score_gpt":0.19697483119121587,"score_spread":0.1730098262017936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035512785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913368,0.0002984962,0.00025119097,0.0073691774,0.0001208555,0.000078583624,0.00021956667,0.0000017319886,0.0003235934],"genre_scores_gemma":[0.995337,0.000030259545,0.001351112,0.0031380937,0.000104485385,3.610746e-7,0.000036326124,9.154513e-7,0.0000014413739],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99901915,0.000082157,0.00029918784,0.0001112096,0.00024829886,0.00024002587],"domain_scores_gemma":[0.9994348,0.00008490689,0.00012001386,0.0000471369,0.00005392754,0.0002591645],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00059423095,0.00008516551,0.00012754671,0.000085966116,0.00035041018,0.0003033911,0.0003311717,0.00003350357,0.00031378487],"category_scores_gemma":[0.00012260095,0.000046995312,0.000029291758,0.0003789145,0.00021493179,0.0009361796,0.0000052045852,0.00019786466,0.0000062709264],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025744774,0.00000800683,0.9815016,0.00000411461,0.0000014604634,0.00003674139,0.0031307572,0.009279833,0.000010456498,0.00003280651,0.00007670576,0.005891808],"study_design_scores_gemma":[0.00010959383,0.00015100914,0.71931374,0.000024811665,0.0000032044256,0.00007052244,0.00079122244,0.27895322,0.000004267588,0.0002508178,0.00027449735,0.000053096883],"about_ca_topic_score_codex":0.007347579,"about_ca_topic_score_gemma":0.23458724,"teacher_disagreement_score":0.2696734,"about_ca_system_score_codex":0.0000023473237,"about_ca_system_score_gemma":0.00031132044,"threshold_uncertainty_score":0.9992626},"labels":[],"label_agreement":null},{"id":"W3037724232","doi":"10.1139/cjes-2019-0169","title":"Identifying groundwater discharge zones in the Central Mackenzie Valley using remotely sensed optical and thermal imagery","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Global Water Futures","keywords":"Thematic Mapper; Watershed; Hydrogeology; Groundwater; Geology; Remote sensing; Hydrology (agriculture); Thematic map; Environmental science; Satellite imagery; Cartography; Geography","score_opus":0.0715562108924635,"score_gpt":0.24173265027902238,"score_spread":0.17017643938655888,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3037724232","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926625,0.0012662314,0.00020552943,0.0052792835,0.00026726606,0.00005626357,0.000008537253,0.000001724017,0.0002526718],"genre_scores_gemma":[0.99539524,0.000050038456,0.003303811,0.0010425998,0.00019984522,3.8952507e-8,0.0000011556539,0.0000014046165,0.000005881401],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989814,0.00006533466,0.00023125253,0.0001235362,0.00022514208,0.00037330762],"domain_scores_gemma":[0.99941146,0.00011617738,0.00007961427,0.00004318098,0.00003263389,0.0003169546],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004434963,0.000079895835,0.00013029191,0.00004868083,0.00048213967,0.0003321313,0.00023704504,0.000021762608,0.0003312208],"category_scores_gemma":[0.00010666587,0.000048068832,0.000045114768,0.00036824832,0.00036233015,0.00041758962,0.000006503569,0.00014630552,0.0000041161766],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000083469795,0.0000028356783,0.99143505,0.00000712358,0.000008141802,0.00018389727,0.0040441947,0.001732181,0.0000958003,0.00013760576,0.00007174789,0.0022731011],"study_design_scores_gemma":[0.000110908804,0.00008272285,0.98734844,0.00002064442,0.000009463196,0.00009354219,0.0037536144,0.0075554494,0.000012171077,0.00015317021,0.0007849612,0.00007493716],"about_ca_topic_score_codex":0.018812407,"about_ca_topic_score_gemma":0.16535686,"teacher_disagreement_score":0.14654446,"about_ca_system_score_codex":0.0000014664047,"about_ca_system_score_gemma":0.0002943791,"threshold_uncertainty_score":0.9877214},"labels":[],"label_agreement":null},{"id":"W3037794323","doi":"10.1139/cjes-2019-0202","title":"An ornithurine bird coracoid from the Late Cretaceous of Alberta, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Coracoid; Geology; Cretaceous; Postcrania; Paleontology; Foramen; Taxon","score_opus":0.017030106535113602,"score_gpt":0.19348542077986808,"score_spread":0.17645531424475447,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3037794323","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9878612,0.0024939259,0.000008841676,0.0073207375,0.0005030703,0.000035104735,0.00010762095,0.0000021516025,0.001667308],"genre_scores_gemma":[0.9975228,0.000028968878,0.00017610249,0.0020616306,0.00016565077,4.2273577e-8,0.0000060800894,0.0000011641657,0.00003758689],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990378,0.00013964057,0.00025827606,0.00011314651,0.00017066392,0.00028048374],"domain_scores_gemma":[0.99871695,0.00032396926,0.00020029799,0.00008158341,0.00007557124,0.00060164084],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029860076,0.00007990744,0.0001745062,0.000046381207,0.00032093032,0.000024301546,0.0006425707,0.000044125347,0.002225539],"category_scores_gemma":[0.00019681311,0.00004896893,0.00003684142,0.00028294508,0.00069779274,0.00020324114,0.0000026829916,0.00016711789,0.000023181254],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018632778,0.0000011020056,0.9940359,0.0000010154822,0.000013085189,0.00005947506,0.00036590727,0.0039004916,0.000022001692,0.000019582476,0.00045652923,0.001106252],"study_design_scores_gemma":[0.000101119906,0.00036704456,0.97668266,0.0000075341018,0.000011227881,0.00006825263,0.00047922836,0.0024470598,0.00003142728,0.00012428775,0.019611554,0.000068615285],"about_ca_topic_score_codex":0.97176003,"about_ca_topic_score_gemma":0.9998586,"teacher_disagreement_score":0.028098574,"about_ca_system_score_codex":0.0000013369485,"about_ca_system_score_gemma":0.003946774,"threshold_uncertainty_score":0.99868655},"labels":[],"label_agreement":null},{"id":"W3041022834","doi":"10.1139/cjes-2019-0178","title":"Re–Os dating of pyrite and mineral chemistry of magnetite from the Yamansu Fe deposit, Xinjiang, northwestern China","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Magnetite; Geochemistry; Hydrothermal circulation; Pyrite; Skarn; Mineralization (soil science); Pyroxene; Diorite; Breccia; Siderite; Mineralogy; Olivine; Zircon; Fluid inclusions","score_opus":0.013902454415245208,"score_gpt":0.17707357329142054,"score_spread":0.16317111887617533,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3041022834","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99290425,0.0027847923,0.000009517107,0.0025827652,0.000036620146,0.00002575766,0.00009111289,0.0000013574582,0.001563816],"genre_scores_gemma":[0.9988158,0.00004069663,0.0006817605,0.00032273415,0.00010598293,4.3307022e-8,0.000007051775,7.7011657e-7,0.000025159869],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990546,0.000037932514,0.00033130753,0.00014408004,0.00023036358,0.00020172354],"domain_scores_gemma":[0.99905825,0.00012831457,0.0002538483,0.00006965264,0.000060442482,0.00042952332],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024908988,0.00008536778,0.00021433282,0.000031242125,0.00014344978,0.00005759696,0.0004192398,0.000034490895,0.002622018],"category_scores_gemma":[0.00015928244,0.000049389717,0.000078564284,0.00035456408,0.0005761709,0.00014281235,0.000012054019,0.00014211312,0.0000028349561],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000062877243,0.0000018324491,0.99501073,0.000011894623,0.000013255018,0.00001623667,0.00043308886,0.0006463871,0.0017014866,0.0000014313566,0.000049756785,0.0021076133],"study_design_scores_gemma":[0.00010817448,0.00016236954,0.9930587,0.00004565286,0.000030195197,0.000011861399,0.00056119525,0.003483386,0.0017986277,0.00024633596,0.00042122157,0.000072280374],"about_ca_topic_score_codex":0.09539218,"about_ca_topic_score_gemma":0.30957904,"teacher_disagreement_score":0.21418685,"about_ca_system_score_codex":3.655412e-7,"about_ca_system_score_gemma":0.00016275796,"threshold_uncertainty_score":0.9982897},"labels":[],"label_agreement":null},{"id":"W3041117205","doi":"10.1139/cjes-2020-0033","title":"Early Cretaceous Xiuyan adakitic granitoids in the Liaodong Peninsula, eastern China: petrogenesis and implications for lithospheric thinning of the North China Craton","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Adakite; Geology; Petrogenesis; Geochemistry; Craton; Underplating; Pluton; Zircon; Crust; Partial melting; Lithosphere; Subduction; Mantle (geology); Oceanic crust; Petrology; Tectonics; Paleontology","score_opus":0.019407484872377794,"score_gpt":0.1975930200126965,"score_spread":0.1781855351403187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3041117205","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893914,0.002099489,0.00004248551,0.007990429,0.000053875483,0.00010369289,0.00003923256,0.0000017842534,0.00027764955],"genre_scores_gemma":[0.9990943,0.000025442681,0.00036627843,0.00043256907,0.00006621929,6.4383966e-7,0.0000017167412,0.00000125203,0.0000115429275],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898106,0.00008754563,0.00029715375,0.00015823203,0.00019655832,0.00027943082],"domain_scores_gemma":[0.9992182,0.0001398097,0.00019487386,0.000088849425,0.00006439824,0.00029381967],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041854003,0.00009652046,0.00019465777,0.000058216247,0.0004302987,0.000121277546,0.00063786295,0.000029434843,0.00014847922],"category_scores_gemma":[0.00027530163,0.000048607297,0.000119581404,0.00093809405,0.00044456657,0.00016929953,0.000009449887,0.00016164989,0.0000015259101],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005101738,0.000002772522,0.9960613,0.000006671144,0.0000073269503,0.000003903914,0.0008793828,0.0013317203,0.000022084345,0.00003929908,0.000009112095,0.0016312754],"study_design_scores_gemma":[0.00009594471,0.0002486918,0.99445987,0.000015301752,0.000028680528,0.0000294615,0.00034383478,0.0029160765,0.000026533753,0.0015114372,0.00025688185,0.00006729825],"about_ca_topic_score_codex":0.01689306,"about_ca_topic_score_gemma":0.24899873,"teacher_disagreement_score":0.23210567,"about_ca_system_score_codex":8.8625643e-7,"about_ca_system_score_gemma":0.00024749083,"threshold_uncertainty_score":0.9896535},"labels":[],"label_agreement":null},{"id":"W3041952499","doi":"10.1139/cjes-2019-0226","title":"Upper Paleozoic stratigraphy and detrital zircon geochronology along the northwest margin of the Sverdrup Basin, Arctic Canada: insight into the paleogeographic and tectonic evolution of Crockerland","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Geological Survey of Canada","funders":"","keywords":"Geology; Permian; Paleontology; Unconformity; Paleozoic; Pennsylvanian; Sverdrup; Gondwana; Thrust fault; Carboniferous; Devonian; Sedimentary rock; Fault (geology); Structural basin","score_opus":0.010399553245730959,"score_gpt":0.16404523410992689,"score_spread":0.15364568086419592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3041952499","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9760344,0.016216915,0.000012656204,0.007336155,0.00015784016,0.00010469109,0.000018596545,7.7619126e-7,0.0001179926],"genre_scores_gemma":[0.99930257,0.0003509957,0.000048278056,0.00025442318,0.000040833056,2.8476956e-7,9.1744704e-7,7.175441e-7,9.753082e-7],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99903625,0.00011811733,0.00026973852,0.00012530906,0.00023232923,0.0002182455],"domain_scores_gemma":[0.9992246,0.00019463379,0.00022528715,0.00007126143,0.000102777725,0.00018143543],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037771853,0.00008807054,0.00016323624,0.000075512056,0.0006788703,0.000049083723,0.0002965318,0.000034744753,0.0000853927],"category_scores_gemma":[0.00016700255,0.00003921095,0.000050916387,0.0006545289,0.001452092,0.00015193579,0.000012349292,0.00017040747,2.2683761e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007087072,0.0000010877783,0.997362,0.000009961696,0.000016474065,0.0000036046597,0.00073854957,0.0003072785,0.000026061864,0.000073740965,0.000017259745,0.001436894],"study_design_scores_gemma":[0.0001150366,0.00036212677,0.99569273,0.000024501245,0.000022240236,0.000033206044,0.0021426934,0.00028558075,0.00004034601,0.00036092673,0.0008690092,0.000051632087],"about_ca_topic_score_codex":0.8003184,"about_ca_topic_score_gemma":0.9987099,"teacher_disagreement_score":0.19839156,"about_ca_system_score_codex":0.0000022687898,"about_ca_system_score_gemma":0.0008818708,"threshold_uncertainty_score":0.53502935},"labels":[],"label_agreement":null},{"id":"W3042199620","doi":"10.1139/cjes-2020-0059","title":"Regional and local controls on Archean rock-hosted cobalt mineralization at the McAra deposit, southern Superior Province, Ontario, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Archean; Geochemistry; Mafic; Greenstone belt; Siliciclastic; Sill; Metamorphism; Breccia; Felsic; Cobalt; Craton; Structural basin; Geomorphology; Sedimentary depositional environment; Paleontology","score_opus":0.015701696002960223,"score_gpt":0.1676795205508514,"score_spread":0.15197782454789116,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3042199620","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9856794,0.00065202283,0.00003422082,0.012589271,0.00006336057,0.0000709162,0.000045717607,0.0000021081569,0.00086300756],"genre_scores_gemma":[0.9941656,0.0000051633288,0.000039529885,0.0054131974,0.000078827514,1.6492969e-7,0.000011604432,0.0000010312452,0.0002848728],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99880594,0.000073724455,0.00024351102,0.000185567,0.00037592254,0.00031530653],"domain_scores_gemma":[0.99881965,0.00012715312,0.000117824406,0.000053143667,0.00007804783,0.0008041788],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021938619,0.000109351146,0.00018522875,0.00004688815,0.0004934464,0.00010156674,0.0002864117,0.000034151948,0.002630962],"category_scores_gemma":[0.00009395058,0.000059735885,0.00005689066,0.00026072437,0.00039596384,0.00009009733,0.0000072715575,0.00017317451,0.000015415613],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000040083847,0.0000017797572,0.9836339,0.000002804674,0.0000155401,0.00007242735,0.0002992728,0.013870775,0.000044612425,0.000027970373,0.00096437894,0.0010264653],"study_design_scores_gemma":[0.00033530282,0.0005697461,0.9635093,0.00002489739,0.00003588687,0.00012922344,0.00079084403,0.012892427,0.00013173404,0.00024724333,0.021156514,0.00017684058],"about_ca_topic_score_codex":0.9821436,"about_ca_topic_score_gemma":0.999955,"teacher_disagreement_score":0.020192135,"about_ca_system_score_codex":0.000009851551,"about_ca_system_score_gemma":0.002072511,"threshold_uncertainty_score":0.99828076},"labels":[],"label_agreement":null},{"id":"W3045893813","doi":"10.1139/cjes-2019-0238","title":"The role of excess oxygen for modeling high-Mn, low-Ca garnets in metapelites from the northern Central Metasedimentary Belt of the Grenville Province, Ontario, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Deutsche Forschungsgemeinschaft","keywords":"Terrane; Geology; Metamorphic rock; Geothermobarometry; Shear zone; Metamorphism; Geochemistry; Petrology; Tectonics; Seismology","score_opus":0.0103133391963037,"score_gpt":0.15670064659689867,"score_spread":0.14638730740059497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3045893813","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9901577,0.0035487793,0.0000060427765,0.00555967,0.00013746378,0.00012140583,0.00032094217,5.382691e-7,0.00014744829],"genre_scores_gemma":[0.99908537,0.000016334834,0.0001720914,0.0006304124,0.00006428723,4.367134e-7,0.000014589178,0.0000011125262,0.000015354717],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985054,0.0000953406,0.00045027878,0.00015828553,0.0004162961,0.00037440614],"domain_scores_gemma":[0.9988173,0.00037612818,0.00027729708,0.00010801399,0.00010767183,0.00031353973],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048019047,0.00010614141,0.00024941898,0.000030490452,0.00034893284,0.000049014412,0.0009984378,0.000028387498,0.0009181543],"category_scores_gemma":[0.00019375913,0.000045544377,0.00014107673,0.0003816549,0.00038496553,0.00010233214,0.000016566839,0.00018870119,7.0077897e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023034274,0.0000039481056,0.9122385,0.000003242184,0.00005067355,0.0000040401337,0.00033819547,0.08553923,0.000076266566,0.000025607405,0.000089335015,0.0016079231],"study_design_scores_gemma":[0.0003231792,0.00020317399,0.9069109,0.000052621206,0.00013081494,0.000003720542,0.0026204954,0.072330534,0.001659467,0.008294771,0.0072958823,0.00017444312],"about_ca_topic_score_codex":0.99510705,"about_ca_topic_score_gemma":0.99996114,"teacher_disagreement_score":0.013208694,"about_ca_system_score_codex":0.0000068899344,"about_ca_system_score_gemma":0.0029939841,"threshold_uncertainty_score":0.9999951},"labels":[],"label_agreement":null},{"id":"W3048109549","doi":"10.1139/cjes-2020-0075","title":"Stratigraphy and sedimentology of the Pennsylvanian Grande Anse Formation, Cumberland Basin, eastern Canada: its relationship to salt tectonics and coeval strata of the Joggins World Heritage Site","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Geology; Paleontology; Pennsylvanian; Unconformity; Sedimentology; Red beds; Sedimentary rock; Structural basin; Lithology; Salt tectonics; Anticline; Geomorphology; Geochemistry; Diapir","score_opus":0.027858918164112564,"score_gpt":0.20204851221435277,"score_spread":0.1741895940502402,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3048109549","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915781,0.0008465223,0.000014885173,0.006318393,0.00010974301,0.000107126565,0.00014746537,9.063645e-7,0.00087686727],"genre_scores_gemma":[0.99920225,0.000014845792,0.00015255823,0.0005919465,0.000015381656,1.1327765e-7,0.00000137616,6.7588644e-7,0.000020859907],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991438,0.000080800055,0.0002976669,0.0000811673,0.00022806338,0.00016851953],"domain_scores_gemma":[0.99916625,0.00012369604,0.00021841303,0.0000602738,0.000113701986,0.00031766656],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033206266,0.00006997705,0.00013475037,0.00008594794,0.0003615274,0.00006525131,0.0002703151,0.000024058798,0.00013166227],"category_scores_gemma":[0.00018163757,0.000038476424,0.000027677885,0.0006821454,0.00031080123,0.00032446795,0.000008273645,0.0001275895,5.7751095e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000061197675,9.743902e-7,0.9974014,0.000022145914,0.0000039366123,0.0000015878431,0.000781719,0.0011914803,0.000009596051,0.00022609321,0.00010298647,0.00025195465],"study_design_scores_gemma":[0.00011346695,0.00015198893,0.99524415,0.000035639678,0.000011867704,0.00004167395,0.00067163043,0.0012969683,0.0000844083,0.00025909086,0.00203885,0.00005029304],"about_ca_topic_score_codex":0.11637875,"about_ca_topic_score_gemma":0.99130225,"teacher_disagreement_score":0.8749235,"about_ca_system_score_codex":0.0000010935069,"about_ca_system_score_gemma":0.001034512,"threshold_uncertainty_score":0.8895054},"labels":[],"label_agreement":null},{"id":"W3048302731","doi":"10.1139/cjes-2020-0006","title":"Upper Cambrian and Lower Ordovician conodont biostratigraphy and revised lithostratigraphy, Boothia Peninsula, Nunavut","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Nunavut; Nunavut Research Institute","funders":"Natural Resources Canada; University of Waterloo","keywords":"Conodont; Ordovician; Paleontology; Biostratigraphy; Geology; Peninsula; Chronostratigraphy; Fauna; Lithostratigraphy; Sedimentary rock; Archaeology; Geography; Biology","score_opus":0.025530211162957537,"score_gpt":0.20027438599725278,"score_spread":0.17474417483429525,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3048302731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9778723,0.0071552526,0.000018827765,0.011625707,0.00021029756,0.00009637937,0.000028446919,0.0000047634394,0.0029880044],"genre_scores_gemma":[0.9968772,0.00039709578,0.00080813153,0.0017800204,0.00012362708,1.5000266e-7,0.0000018653527,0.000001194873,0.000010739239],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989613,0.00005745008,0.00028107018,0.00020491553,0.0001806078,0.0003146349],"domain_scores_gemma":[0.99874663,0.000061787905,0.00014166402,0.00004575493,0.000074786774,0.00092938484],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003754036,0.00012233303,0.0002148948,0.00012462691,0.0005458401,0.00030575402,0.0001678588,0.00004923782,0.00051273324],"category_scores_gemma":[0.00013011925,0.00008473072,0.00005787133,0.0003983294,0.00071256934,0.0004214177,0.000004546747,0.00014674001,0.000009989385],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011734533,0.0000013845574,0.9960128,0.0000065453205,0.000009958324,0.000042978005,0.00043260807,0.00004898943,0.000015243785,0.00019005459,0.00012540867,0.0031022613],"study_design_scores_gemma":[0.0001693526,0.0010160888,0.98521805,0.00002776718,0.000012376679,0.000043504788,0.0009534975,0.00063433865,0.000008705377,0.00033237968,0.011458406,0.00012553712],"about_ca_topic_score_codex":0.008625337,"about_ca_topic_score_gemma":0.34101453,"teacher_disagreement_score":0.33238918,"about_ca_system_score_codex":4.2586592e-7,"about_ca_system_score_gemma":0.0002662,"threshold_uncertainty_score":0.9979763},"labels":[],"label_agreement":null},{"id":"W3048306618","doi":"10.1139/cjes-2019-0211","title":"Volcanic reconstruction and geochemistry of the Powderhouse formation in the Paleoproterozoic VMS-hosting Chisel sequence, Snow Lake, Manitoba, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Mount Royal University; Laurentian University","funders":"","keywords":"Geology; Pyroclastic rock; Rhyolite; Breccia; Geochemistry; Geomorphology; Pyroclastic fall; Volcano; Volcanic rock; Explosive eruption; Petrology","score_opus":0.02538107881428444,"score_gpt":0.17284985351102677,"score_spread":0.14746877469674233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3048306618","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99416536,0.00029321798,0.000002723425,0.0043718508,0.00008144972,0.00005391943,0.000031471787,9.686134e-7,0.0009990344],"genre_scores_gemma":[0.9990866,0.000018717743,0.000103176644,0.00073197467,0.000052991425,1.5537539e-7,0.0000021123935,4.6255025e-7,0.0000037939303],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910116,0.00006706274,0.00027647888,0.000100532976,0.00025079524,0.00020398843],"domain_scores_gemma":[0.9993626,0.00009752668,0.0002193986,0.000055349174,0.000058441405,0.00020670731],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036752873,0.000069253176,0.00012311089,0.00004383257,0.00024117464,0.000059036756,0.000379553,0.000021199572,0.00046098357],"category_scores_gemma":[0.0003567427,0.00003598564,0.000041206036,0.0005593811,0.00032944392,0.00020502733,0.0000055222945,0.00019351326,9.622707e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000269655,9.034164e-7,0.9939786,0.000010915451,0.0000033962474,0.000025316804,0.00019144344,0.0008602759,0.00018243215,0.0000051759534,0.00005951961,0.004679334],"study_design_scores_gemma":[0.00011429734,0.00008108041,0.98741585,0.0000689439,0.000015609156,0.0005312047,0.0024917137,0.006458364,0.0010463936,0.0011421518,0.00054225634,0.000092115624],"about_ca_topic_score_codex":0.49234894,"about_ca_topic_score_gemma":0.99833244,"teacher_disagreement_score":0.50598353,"about_ca_system_score_codex":0.0000021935582,"about_ca_system_score_gemma":0.00058541854,"threshold_uncertainty_score":0.51103157},"labels":[],"label_agreement":null},{"id":"W3049418771","doi":"10.1139/cjes-2020-0071","title":"Albanerpetontids (Lissamphibia, Albanerpetontidae) from the Aguja Formation (lower Campanian) of West Texas, USA","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Assemblage (archaeology); Fauna; Geology; Paleontology; Taxon; Range (aeronautics); Ecology; Biology","score_opus":0.02418532900876569,"score_gpt":0.2029529597773005,"score_spread":0.1787676307685348,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3049418771","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9820214,0.003172327,0.00015513078,0.007591983,0.0009205389,0.00007898001,0.00024118494,0.0000038305857,0.0058146073],"genre_scores_gemma":[0.9973942,0.00006680514,0.0004801605,0.0016931621,0.00029377345,1.07567644e-7,0.000022427437,0.0000011516853,0.00004820731],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985542,0.00017438487,0.00045461673,0.00017171515,0.00025844804,0.0003866048],"domain_scores_gemma":[0.99859923,0.000300355,0.00035686532,0.00011162997,0.00012029036,0.0005116216],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006430878,0.000124781,0.00025094254,0.000111533016,0.00040671884,0.000056637145,0.0007473708,0.00009507826,0.0046553286],"category_scores_gemma":[0.000304682,0.00007930989,0.00010736709,0.0004457868,0.0011252203,0.000782013,0.0000062507197,0.00023240001,0.00023226891],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002621856,0.0000030304054,0.99373794,0.0000029226712,0.000018142644,0.000042375053,0.0005322986,0.0013213317,0.000056350313,0.00013389577,0.0013218572,0.0028036488],"study_design_scores_gemma":[0.00016459826,0.00040588487,0.9574882,0.00002485846,0.00002072925,0.00011116441,0.00035602256,0.0011852263,0.000072725525,0.00022481498,0.039839264,0.00010651309],"about_ca_topic_score_codex":0.043293606,"about_ca_topic_score_gemma":0.76382154,"teacher_disagreement_score":0.7205279,"about_ca_system_score_codex":0.0000019752213,"about_ca_system_score_gemma":0.0010511425,"threshold_uncertainty_score":0.99625456},"labels":[],"label_agreement":null},{"id":"W3080706473","doi":"10.1139/cjes-2020-0092","title":"Inversion of magnetic and frequency-domain electromagnetic data for investigating lithologies associated with gold mineralization in the Canadian Malartic area, Québec, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Diorite; Mafic; Geochemistry; Volcanic rock; Pluton; Petrology; Lithology; Greenstone belt; Ultramafic rock; Archean; Magnetic susceptibility; Magnetic anomaly; Gabbro; Volcano; Igneous rock; Geophysics; Seismology; Tectonics","score_opus":0.041279182580697855,"score_gpt":0.2141762546294577,"score_spread":0.17289707204875984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3080706473","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.983701,0.0010729267,0.000011640998,0.014644974,0.00003855702,0.00012745711,0.000077295816,0.0000012037673,0.0003249447],"genre_scores_gemma":[0.9949825,0.0000052625805,0.0032999488,0.0016600227,0.000026328396,3.3977716e-7,0.0000147431165,0.0000013672147,0.000009482154],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99882066,0.00017726733,0.00023797473,0.00016127001,0.00024475902,0.0003580778],"domain_scores_gemma":[0.99876595,0.00042914343,0.00014840178,0.00008480445,0.0000845739,0.00048711768],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00076886424,0.000086302716,0.00017210677,0.00012030502,0.00021333784,0.00008185838,0.00051027443,0.000032972686,0.00005545545],"category_scores_gemma":[0.0017767047,0.000053389595,0.000014733769,0.0008903,0.00036120557,0.00020071187,0.000004351305,0.00014392093,2.4923534e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008536765,0.0000032339935,0.99206907,0.000019552625,0.000008780216,0.00006290535,0.0007006798,0.0014038632,0.0001648439,0.00017419917,0.0009507457,0.0044335728],"study_design_scores_gemma":[0.00021682613,0.0015138912,0.97991014,0.00004915501,0.00002030734,0.00002104834,0.0005064692,0.014773614,0.000022374563,0.0023312867,0.0005267672,0.00010813524],"about_ca_topic_score_codex":0.9943382,"about_ca_topic_score_gemma":0.999982,"teacher_disagreement_score":0.013369751,"about_ca_system_score_codex":0.000007696543,"about_ca_system_score_gemma":0.006476722,"threshold_uncertainty_score":0.99915564},"labels":[],"label_agreement":null},{"id":"W3080822243","doi":"10.1139/cjes-2019-0183","title":"High-resolution (centimetre-scale) GPS/GIS-based 3D mapping and spatial analysis of in situ fossils in two horned-dinosaur bonebeds in the Dinosaur Park Formation (Upper Cretaceous) at Dinosaur Provincial Park, Alberta, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"3D Surveying and Cultural Heritage","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; University of Lethbridge; Royal Tyrrell Museum","funders":"","keywords":"Geology; Taphonomy; Georeference; Paleontology; Scale (ratio); Orientation (vector space); Photogrammetry; Field (mathematics); Vertebrate; Cartography; Geography; Remote sensing; Physical geography; Biology","score_opus":0.018180290232010014,"score_gpt":0.2082588245324287,"score_spread":0.19007853430041868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3080822243","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99664074,0.00059584936,0.000052981904,0.0018101893,0.00016761856,0.0001734832,0.000091363356,0.0000019843446,0.00046577226],"genre_scores_gemma":[0.9992637,0.000016696556,0.00018559188,0.00042226329,0.00006192229,8.2626786e-7,0.00003533722,0.0000020533644,0.000011578996],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99757177,0.0003884407,0.00068966206,0.0002596721,0.00056283845,0.0005275921],"domain_scores_gemma":[0.9988179,0.0002848359,0.0003502235,0.00009928282,0.00006470963,0.00038304954],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013667664,0.00017463595,0.00042878423,0.0006112386,0.00028209985,0.00015095194,0.00039932894,0.000059060374,0.00017606214],"category_scores_gemma":[0.00023632066,0.00012451744,0.00008941137,0.002186528,0.00024377368,0.00056953623,0.000008897668,0.0002782107,0.0000018376118],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003173214,0.000006332434,0.9676041,0.000015722722,0.000014130572,0.000061998275,0.0018522579,0.026191432,0.000075390184,0.0000024232488,0.00007371714,0.0040707355],"study_design_scores_gemma":[0.0004253435,0.00013146896,0.93715394,0.000063281244,0.00003451157,0.000010959604,0.0011667095,0.060361445,0.000085844295,0.000010780232,0.0004023598,0.00015337778],"about_ca_topic_score_codex":0.9568335,"about_ca_topic_score_gemma":0.9999211,"teacher_disagreement_score":0.0430876,"about_ca_system_score_codex":0.000032756667,"about_ca_system_score_gemma":0.0011887252,"threshold_uncertainty_score":0.5077673},"labels":[],"label_agreement":null},{"id":"W3080913315","doi":"10.1139/cjes-2019-0221","title":"Potential-field modelling of the prospective Chibougamau area (northeastern Abitibi subprovince, Quebec, Canada) using geological, geophysical, and petrophysical constraints","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Chicoutimi; Laurentian University","funders":"Materials and Energy Research Center; Canada First Research Excellence Fund","keywords":"Geology; Petrophysics; Pluton; Greenstone belt; Geophysics; Hydrogeology; Craton; Structural geology; Overprinting; Petrology; Geochemistry; Archean; Seismology; Tectonics; Geotechnical engineering; Porosity","score_opus":0.026038451745341813,"score_gpt":0.20069559810667784,"score_spread":0.17465714636133603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3080913315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99473625,0.00021491219,0.0021707423,0.002091813,0.00018616027,0.00010781593,0.000027040687,0.0000024711892,0.00046276534],"genre_scores_gemma":[0.9978672,0.000005726049,0.0012210922,0.00070392806,0.00017299334,1.0879362e-7,4.4579684e-7,0.0000020120042,0.00002648127],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99839157,0.00012857598,0.00032992894,0.00024402041,0.00047406994,0.00043185023],"domain_scores_gemma":[0.9985943,0.00020768735,0.0002545606,0.00008241471,0.00014458847,0.00071645423],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019880963,0.0001481363,0.00033115974,0.000057975492,0.0004182186,0.00010079924,0.0004246086,0.00004913485,0.00018315649],"category_scores_gemma":[0.00021186491,0.00008902071,0.00010884153,0.00057767355,0.0011077417,0.00021245732,0.000016048534,0.0003480476,0.0000015239027],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009593957,0.00002896723,0.71661973,0.000048619648,0.00007043912,0.00021666408,0.000480856,0.2550224,0.0008281122,0.0009885803,0.000086285225,0.025513377],"study_design_scores_gemma":[0.0002135596,0.00064653816,0.71300936,0.00005718797,0.000041294425,0.000058626698,0.00028448776,0.28216583,0.0005572464,0.0025835165,0.00017412685,0.00020823495],"about_ca_topic_score_codex":0.7860429,"about_ca_topic_score_gemma":0.92584056,"teacher_disagreement_score":0.1397976,"about_ca_system_score_codex":0.00000498898,"about_ca_system_score_gemma":0.003582066,"threshold_uncertainty_score":0.6354431},"labels":[],"label_agreement":null},{"id":"W3080999828","doi":"10.1139/cjes-2019-0187","title":"Hydrogeological and geophysical properties of the very-slow-moving Ripley Landslide, Thompson River valley, British Columbia","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Saskatchewan; Geological Survey of Canada","funders":"Engineering and Physical Sciences Research Council; Natural Environment Research Council; Sight Research UK","keywords":"Geology; Electrical resistivity tomography; Hydrogeology; Bedrock; Landslide; Seismic refraction; Geophysics; Groundwater; Geomorphology; Groundwater flow; Aquifer; Geotechnical engineering; Electrical resistivity and conductivity","score_opus":0.012991475180991797,"score_gpt":0.17293613828133883,"score_spread":0.15994466310034702,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3080999828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964379,0.00040993374,0.0000035854434,0.0013486883,0.0001434277,0.00006173463,0.0000046990867,0.0000025416048,0.0015875063],"genre_scores_gemma":[0.9990334,0.000047561287,0.00018986342,0.00041165462,0.00006343754,3.0442652e-7,8.3044235e-8,0.0000029850987,0.00025071073],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990348,0.000058753198,0.00020933688,0.00014822098,0.0003029631,0.00024591287],"domain_scores_gemma":[0.99937695,0.000020526202,0.00013132884,0.000057228288,0.000018744473,0.00039522222],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028140674,0.000060818482,0.00016349113,0.000013984053,0.00039051703,0.00018795244,0.00038429705,0.000051518186,0.0005592913],"category_scores_gemma":[0.00013179348,0.00004338686,0.000075541946,0.0002703372,0.0015072527,0.00021944851,0.000078441575,0.0001926989,0.0000075474345],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005161145,0.000007901294,0.9943065,0.000006437516,0.00001047868,0.000057201392,0.0007921024,0.00067403895,0.000988431,0.000011622414,0.001120001,0.0020201034],"study_design_scores_gemma":[0.00026321554,0.00028317337,0.9876204,0.00010934025,0.000021403033,0.00019774509,0.00024455626,0.0014289494,0.00027390633,0.0002533586,0.009187961,0.00011599158],"about_ca_topic_score_codex":0.04866721,"about_ca_topic_score_gemma":0.20744073,"teacher_disagreement_score":0.15877351,"about_ca_system_score_codex":0.0000068296054,"about_ca_system_score_gemma":0.00019709997,"threshold_uncertainty_score":0.95766777},"labels":[],"label_agreement":null},{"id":"W3081891666","doi":"10.1139/cjes-2018-0318","title":"Sources of sulphur for the Proterozoic Kiggavik uranium deposit, Nunavut, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"iNano Medical (Canada); University of Manitoba","funders":"","keywords":"Pyrite; Geology; Geochemistry; Uranium; Galena; Unconformity; Uranium ore; Mineralization (soil science); Proterozoic; Hydrothermal circulation; Mineralogy; Sedimentary rock; Sphalerite; Paleontology","score_opus":0.01920727987281912,"score_gpt":0.17949869982775138,"score_spread":0.16029141995493226,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3081891666","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98464805,0.002543471,0.000109000335,0.011781482,0.00017172305,0.00011566288,0.000067662564,0.0000017729516,0.0005611916],"genre_scores_gemma":[0.99790794,0.000014468692,0.00045468105,0.0014380937,0.0001510031,3.686448e-7,0.0000018315895,9.3516866e-7,0.00003070275],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988514,0.000037697737,0.00032366146,0.0001386382,0.0003126817,0.00033591944],"domain_scores_gemma":[0.99868995,0.00027585414,0.00021568303,0.00006326166,0.0001394658,0.00061579305],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037381888,0.00009242259,0.00021346615,0.000052835898,0.0003554436,0.00007219045,0.0006594485,0.000028492548,0.001475234],"category_scores_gemma":[0.00027001832,0.000048535116,0.00012206614,0.0004892181,0.00040730607,0.00011806571,0.000005140031,0.00012712568,0.000003927217],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016975155,0.0000018720515,0.99010545,0.000014601746,0.000030447418,0.000022354114,0.00016979135,0.006045652,0.00008937665,0.00002981298,0.00059688784,0.0028767837],"study_design_scores_gemma":[0.00025706957,0.0006878017,0.963003,0.000031538,0.00008224524,0.0000691104,0.0009986016,0.013111368,0.0036926123,0.0011974889,0.016678164,0.00019099911],"about_ca_topic_score_codex":0.82768416,"about_ca_topic_score_gemma":0.9952914,"teacher_disagreement_score":0.16760723,"about_ca_system_score_codex":0.0000012668755,"about_ca_system_score_gemma":0.0014295378,"threshold_uncertainty_score":0.9994376},"labels":[],"label_agreement":null},{"id":"W3084358718","doi":"10.1139/cjes-2020-0062","title":"Crustal structure of the metasedimentary Kisseynew domain and bounding volcanic–plutonic domains, Trans-Hudson orogen, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"University of British Columbia","keywords":"Geology; Crust; Boundary (topology); Volcano; Bouguer anomaly; Tectonics; Reflection (computer programming); Domain (mathematical analysis); Section (typography); Seismology; Geophysics; Paleontology; Gravity anomaly","score_opus":0.010030298476739283,"score_gpt":0.17242916236282543,"score_spread":0.16239886388608615,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3084358718","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9883507,0.0030516356,0.000008195786,0.007924802,0.00018587107,0.000052913223,0.00019101937,0.0000013368756,0.00023355322],"genre_scores_gemma":[0.997822,0.000018499235,0.00057865836,0.0014913022,0.00007715142,3.1190638e-8,0.000003948807,0.0000010824599,0.000007324394],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986566,0.00008365578,0.00032415037,0.00017215598,0.000417645,0.00034579335],"domain_scores_gemma":[0.9987954,0.00008673806,0.00019379793,0.00006785206,0.00005412544,0.00080210326],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025607654,0.00011793427,0.0002541855,0.000060809456,0.0004508018,0.00007931573,0.0004913777,0.000037152415,0.003865104],"category_scores_gemma":[0.00009784669,0.000065780514,0.00010064819,0.00063201325,0.0008267991,0.00016199007,0.000008328395,0.00020651269,7.559244e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015571404,0.000002246442,0.99222755,0.00001885589,0.00006667723,0.00007803793,0.0005840336,0.0026786563,0.0026308536,0.00016357447,0.00040589448,0.0011280228],"study_design_scores_gemma":[0.0005899682,0.0005700491,0.9476878,0.000069057394,0.0001918672,0.00026440088,0.004201,0.0015997312,0.0077088075,0.008988791,0.027742146,0.0003864036],"about_ca_topic_score_codex":0.71666086,"about_ca_topic_score_gemma":0.99601537,"teacher_disagreement_score":0.2793545,"about_ca_system_score_codex":0.0000034908455,"about_ca_system_score_gemma":0.0023865423,"threshold_uncertainty_score":0.9970455},"labels":[],"label_agreement":null},{"id":"W3085162590","doi":"10.1139/cjes-2020-0005","title":"Endocranial morphology of the petalichthyid placoderm <i>Ellopetalichthys scheii</i> from the Middle Devonian of Arctic Canada, with remarks on the inner ear and neck joint morphology of placoderms","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Devonian; Vertebrate; Anatomy; Geology; Paleontology; Arctic; Biology","score_opus":0.02415279324444053,"score_gpt":0.1747241398552849,"score_spread":0.15057134661084437,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3085162590","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9828485,0.0015971573,0.000008355235,0.013446605,0.00034425932,0.00013129337,0.00026051063,0.0000011489559,0.0013621335],"genre_scores_gemma":[0.99694824,0.000036234615,0.00020991589,0.0026959851,0.000083700645,3.8544422e-7,0.000004075296,0.0000024334715,0.00001901298],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99821246,0.0004062749,0.00048644363,0.00021791017,0.00030349087,0.00037341582],"domain_scores_gemma":[0.9982351,0.0006113374,0.0005710085,0.0001784755,0.00013269534,0.00027136967],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0005900114,0.0001543043,0.00038468587,0.00007159013,0.00038081437,0.000013909325,0.0007507078,0.00008475388,0.00062337593],"category_scores_gemma":[0.00036606955,0.000070209586,0.00007465801,0.000405922,0.0034106476,0.00010629122,0.00001748469,0.00037716894,0.0000023104228],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014377185,0.0000066594957,0.9950948,0.000009867272,0.00007764246,0.00007565462,0.0008561516,0.0020808014,0.00073497393,0.00025843724,0.0005421884,0.000119075725],"study_design_scores_gemma":[0.00035856623,0.0008002122,0.99460554,0.00006920457,0.000044279393,0.0005270873,0.0010414855,0.0006277863,0.00067481864,0.00024338071,0.0009137549,0.00009390325],"about_ca_topic_score_codex":0.48292032,"about_ca_topic_score_gemma":0.9665044,"teacher_disagreement_score":0.48358408,"about_ca_system_score_codex":0.0000036382376,"about_ca_system_score_gemma":0.002584279,"threshold_uncertainty_score":0.9993015},"labels":[],"label_agreement":null},{"id":"W3093405880","doi":"10.1139/cjes-2019-0128","title":"New <i>Crassigyrinus</i>-like fibula from the Tournaisian (earliest Carboniferous) of Nova Scotia","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Alberta Bone and Joint Health Institute; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Tournaisian; Carboniferous; Devonian; Viséan; Paleontology; Tetrapod (structure); Geology; Late Devonian extinction; Paleozoic; Plateau (mathematics)","score_opus":0.02535199417352218,"score_gpt":0.20521296584315363,"score_spread":0.17986097166963144,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093405880","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9821994,0.0045445445,0.00018042095,0.008016664,0.0012863289,0.00005716869,0.000100190984,0.00000419145,0.0036111432],"genre_scores_gemma":[0.99633837,0.000021039848,0.0014054702,0.0016839966,0.0005155631,1.7926238e-8,0.0000068533336,0.0000014394599,0.00002726195],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99871683,0.00015392194,0.00035311037,0.0001806783,0.0002287636,0.00036671662],"domain_scores_gemma":[0.99843025,0.00021428337,0.0002496618,0.00011605764,0.00007714533,0.00091258454],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047566678,0.00011245315,0.0002310314,0.00008677429,0.0002756101,0.00006000431,0.00089415215,0.000083476996,0.0038844198],"category_scores_gemma":[0.00016502367,0.00007158962,0.00007743323,0.0003995915,0.00086534605,0.0003882629,0.0000058166756,0.00025837464,0.000075674354],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019392903,0.0000016881067,0.99203026,0.0000011913569,0.000017682349,0.000057425514,0.0005981289,0.0028091033,0.000036504734,0.00005853172,0.0019616778,0.0024084204],"study_design_scores_gemma":[0.00016484741,0.00055026065,0.9886218,0.00001873162,0.000017545684,0.000100983016,0.00051832903,0.00075380586,0.000029771065,0.0004025076,0.008728481,0.0000929766],"about_ca_topic_score_codex":0.23347788,"about_ca_topic_score_gemma":0.9399007,"teacher_disagreement_score":0.70642287,"about_ca_system_score_codex":0.0000012646866,"about_ca_system_score_gemma":0.0024893188,"threshold_uncertainty_score":0.99702615},"labels":[],"label_agreement":null},{"id":"W3094379030","doi":"10.1139/cjes-2020-0134","title":"Cryostratigraphical studies of ground ice formation and distribution in a High Arctic polar desert landscape, Resolute Bay, Nunavut<sup>1</sup>","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université de Montréal; Université Laval; Center for Northern Studies; Queen's University","funders":"","keywords":"Permafrost; Geology; Aggradation; Arctic; Thermokarst; Sea ice; Hydrology (agriculture); Geomorphology; Physical geography; Oceanography","score_opus":0.053440533305949736,"score_gpt":0.2446611730544382,"score_spread":0.19122063974848846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094379030","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99133253,0.0050267605,0.000011603505,0.0028249547,0.000071124305,0.00006419486,0.00057803164,0.0000017712933,0.000089003435],"genre_scores_gemma":[0.9988932,0.0005687761,0.000097361444,0.00026019115,0.00009052136,1.6060963e-7,0.000086014574,0.000001112557,0.0000026313858],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989504,0.00007702292,0.00034218194,0.00012123589,0.0002366541,0.0002724891],"domain_scores_gemma":[0.99913305,0.00014199139,0.00015643041,0.00004486008,0.00012949127,0.00039418443],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006105528,0.00008911052,0.00021080518,0.000176011,0.00020769866,0.00010132633,0.00017781742,0.00004408107,0.00031231862],"category_scores_gemma":[0.00027898964,0.0000682204,0.00003489552,0.0007310557,0.00037823865,0.0007251699,0.000005274797,0.00015252215,0.0000038263456],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021103022,0.0000025071663,0.99577546,0.000042835694,0.000007751231,0.00004117572,0.0026660885,0.00079268066,0.000019495006,0.0000715666,0.00016981771,0.00038950736],"study_design_scores_gemma":[0.00027162107,0.0005060692,0.9840459,0.00010763061,0.000014134272,0.00010203675,0.004970709,0.008389294,0.00001722906,0.00046759448,0.0010135171,0.00009422969],"about_ca_topic_score_codex":0.026721356,"about_ca_topic_score_gemma":0.7006543,"teacher_disagreement_score":0.67393297,"about_ca_system_score_codex":0.0000024454769,"about_ca_system_score_gemma":0.00028421695,"threshold_uncertainty_score":0.9797598},"labels":[],"label_agreement":null},{"id":"W3094761541","doi":"10.1139/cjes-2020-0110","title":"Age and tectonic setting of Neoproterozoic granitoid rocks, Antigonish Highlands, Nova Scotia, Canada: implications for Avalonia in the northern Appalachian orogen","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; St. Francis Xavier University; Acadia University; Nova Scotia Department of Energy","funders":"Natural Sciences and Engineering Research Council of Canada; Nova Scotia Department of Energy and Mines; Nova Scotia Department of Energy; U.S. Department of Energy","keywords":"Pluton; Geology; Zircon; Geochemistry; Terrane; Felsic; Geochronology; Volcanic rock; Tectonics; Volcano; Paleontology","score_opus":0.0187232959445202,"score_gpt":0.1962660449125539,"score_spread":0.17754274896803368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094761541","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9824629,0.0009719051,0.000032465938,0.016070269,0.000048550453,0.00012009717,0.00009335864,0.0000012806252,0.00019917966],"genre_scores_gemma":[0.9987919,0.000008730453,0.00037064464,0.00074968836,0.00006613684,2.9147827e-7,0.00000891572,0.0000010201712,0.000002673417],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990071,0.0000604091,0.00030645885,0.00015522532,0.00016791969,0.00030286328],"domain_scores_gemma":[0.99918234,0.00016792369,0.0001726951,0.00006423048,0.00007603636,0.0003367975],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005425469,0.00008699412,0.00020495837,0.00008332418,0.00023577521,0.00007364659,0.00045113024,0.000028978564,0.00016140737],"category_scores_gemma":[0.00023663192,0.000052408963,0.00005932866,0.00061798276,0.00020410433,0.00009687727,0.0000052583227,0.00013840047,0.0000015850537],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004609223,0.0000018850989,0.9965295,0.000009402855,0.000008161364,0.00001329912,0.00023819513,0.0011407278,0.00007733465,0.000010563664,0.000056298515,0.0019099877],"study_design_scores_gemma":[0.00012775151,0.00016424476,0.9969394,0.000014975194,0.000017102451,0.00003582153,0.00044408446,0.0006013906,0.00005937875,0.00087275193,0.0006483635,0.00007473768],"about_ca_topic_score_codex":0.8482222,"about_ca_topic_score_gemma":0.99959016,"teacher_disagreement_score":0.15136798,"about_ca_system_score_codex":0.0000017529538,"about_ca_system_score_gemma":0.00101137,"threshold_uncertainty_score":0.21371754},"labels":[],"label_agreement":null},{"id":"W3095158619","doi":"10.1139/cjes-2020-0048","title":"Structural analysis and metamorphism of the Barlow Fault Zone, Chibougamau area, Neoarchean Abitibi Subprovince: implications for gold mineralization","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université du Québec à Chicoutimi","funders":"Materials and Energy Research Center","keywords":"Metamorphism; Geology; Greenstone belt; Geochemistry; Terrane; Archean; Mineralization (soil science); Transpression; Fault (geology); Shear zone; Seismology; Tectonics","score_opus":0.027562973063976735,"score_gpt":0.21179575231379502,"score_spread":0.1842327792498183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3095158619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9863575,0.0005468479,0.000488349,0.011928744,0.000048955335,0.000083035266,0.00017707523,0.00000180822,0.0003676565],"genre_scores_gemma":[0.9978191,0.000015650394,0.0014564097,0.00057620066,0.0000576114,2.752335e-7,0.000015857406,7.962652e-7,0.000058063393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990542,0.000047937538,0.0003170066,0.00017217903,0.00017375272,0.00023492884],"domain_scores_gemma":[0.99890864,0.0001182944,0.00024323467,0.00008061413,0.00017119141,0.000478036],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028644985,0.00008944658,0.0002481662,0.00015867675,0.0002764413,0.000077695804,0.00039421776,0.00003630345,0.00071159634],"category_scores_gemma":[0.0002952716,0.000049614537,0.0002053328,0.0014077751,0.0005819046,0.00021293934,0.0000076172746,0.00009244215,8.180862e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000043830714,0.0000010938909,0.98824257,0.0000052856685,0.000049188817,6.9971986e-7,0.0001193664,0.009266232,0.00035239386,0.00026680453,0.00006534266,0.0016266331],"study_design_scores_gemma":[0.00009426979,0.00012195265,0.97031224,0.000004857511,0.00020600334,0.000008772607,0.000099454744,0.025926732,0.0001905257,0.0025874898,0.0003741242,0.00007357818],"about_ca_topic_score_codex":0.026251603,"about_ca_topic_score_gemma":0.53921515,"teacher_disagreement_score":0.51296353,"about_ca_system_score_codex":9.93823e-7,"about_ca_system_score_gemma":0.00027984442,"threshold_uncertainty_score":0.98023266},"labels":[],"label_agreement":null},{"id":"W3096742178","doi":"10.1139/cjes-2020-0135","title":"A reinterpretation of the Snow Lake gold camp, Trans-Hudson Orogen, Canada: the use of cleavages as markers to correlate structures across deformed terranes","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"","keywords":"Geology; Terrane; Craton; Archean; Yilgarn Craton; Geochemistry; Dalradian; Metamorphism; Thrust fault; Shear zone; Metamorphic rock; Petrology; Paleontology; Tectonics","score_opus":0.025996059943429788,"score_gpt":0.20284535226383474,"score_spread":0.17684929232040494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3096742178","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99016404,0.00028340405,0.000017181626,0.00884983,0.00019885942,0.00008741552,0.00016053212,0.0000012925058,0.00023742713],"genre_scores_gemma":[0.9980313,0.000014139215,0.00016451096,0.0017032711,0.000034060817,1.4462873e-7,0.0000024189524,0.0000010958746,0.000049068152],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99865806,0.000099153556,0.0003808045,0.0001393748,0.00041641746,0.00030618167],"domain_scores_gemma":[0.9988101,0.00023942634,0.00026186163,0.00009268076,0.00013484534,0.00046107362],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003141352,0.00010382696,0.00022348274,0.000045890265,0.00022642303,0.00006766379,0.0006438314,0.0000385518,0.0014631463],"category_scores_gemma":[0.000688694,0.000048059323,0.00013482204,0.0006070592,0.0005739856,0.00016950541,0.00000868736,0.00016894458,0.000002472786],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008564322,0.0000023074208,0.91319597,0.00001635549,0.000060500206,0.000024932167,0.0028859677,0.07107214,0.00032390535,0.000025096699,0.0011886872,0.011118469],"study_design_scores_gemma":[0.00009931248,0.00029702848,0.9869679,0.000052060976,0.000040628467,0.000037501257,0.0016718501,0.002388277,0.0015202516,0.00038697952,0.006440681,0.00009749603],"about_ca_topic_score_codex":0.6540293,"about_ca_topic_score_gemma":0.99721414,"teacher_disagreement_score":0.34318483,"about_ca_system_score_codex":0.000002093651,"about_ca_system_score_gemma":0.0009871115,"threshold_uncertainty_score":0.9994497},"labels":[],"label_agreement":null},{"id":"W3107153247","doi":"10.1139/cjes-2020-0108","title":"Long-lived deformation history recorded along the Precambrian Thelon and Judge Sissons faults, northeastern Thelon Basin, Nunavut","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Laurentian University","funders":"","keywords":"Geology; Sinistral and dextral; Breccia; Transpression; Geochemistry; Unconformity; Precambrian; Seismology; Shear zone; Fault (geology); Echelon formation; Sedimentary rock; Paleontology; Tectonics","score_opus":0.028568240587094434,"score_gpt":0.18818477331101152,"score_spread":0.1596165327239171,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3107153247","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98135,0.002714119,0.000041628962,0.0123240845,0.00023245005,0.000082877734,0.00001876434,0.0000062610334,0.0032298267],"genre_scores_gemma":[0.9974373,0.00008480185,0.00022284737,0.0020003612,0.00015104981,2.4402496e-7,0.0000068588174,0.0000014639166,0.000095072355],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986609,0.00013859534,0.00034681524,0.00019424566,0.0002989552,0.00036044605],"domain_scores_gemma":[0.99862874,0.00015880504,0.00025260632,0.00008567512,0.0001095952,0.00076457777],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000699082,0.00013020306,0.00021658784,0.00010897877,0.00043043337,0.0001046096,0.00046680882,0.00005110688,0.0030803352],"category_scores_gemma":[0.00029453298,0.000071043934,0.000105539824,0.0003561805,0.0005738796,0.0004073437,0.000010044318,0.00023280068,0.00006339698],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014905684,0.000002597344,0.9829548,0.0000070804167,0.00001688231,0.00002353877,0.0011803546,0.0007614795,0.000020928454,0.000016450476,0.0001699048,0.014831088],"study_design_scores_gemma":[0.00013026698,0.00031664985,0.9818551,0.000027070071,0.00003675974,0.00007514813,0.00083539204,0.007800285,0.000065001535,0.00040511243,0.008321953,0.00013126756],"about_ca_topic_score_codex":0.035451237,"about_ca_topic_score_gemma":0.68332475,"teacher_disagreement_score":0.6478735,"about_ca_system_score_codex":0.0000040087475,"about_ca_system_score_gemma":0.0004800912,"threshold_uncertainty_score":0.997831},"labels":[],"label_agreement":null},{"id":"W3107446088","doi":"10.1139/cjes-2020-0032","title":"Petrogenesis and economic potential of the Obatogamau Formation, Chibougamau area, Abitibi greenstone belt","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto; Université du Québec à Chicoutimi","funders":"","keywords":"Geology; Greenstone belt; Geochemistry; Mafic; Lava; Petrogenesis; Basalt; Felsic; Silicic; Metamorphism; Archean; Petrology; Volcanic rock; Zircon; Basaltic andesite; Lava dome; Andesite; Volcano","score_opus":0.014241114828395017,"score_gpt":0.16759629493763586,"score_spread":0.15335518010924085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3107446088","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99211293,0.00083206437,0.000024481706,0.0055007758,0.00010768157,0.000030983916,0.00006955411,0.0000014950404,0.0013200205],"genre_scores_gemma":[0.9992781,0.000034364395,0.00018589145,0.0003979208,0.00007892545,4.1700567e-8,0.0000023890218,5.799465e-7,0.000021749054],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991768,0.000038720045,0.00028722058,0.000111365174,0.0001727998,0.00021307218],"domain_scores_gemma":[0.99915695,0.000037558155,0.00021088905,0.00005300708,0.000058606573,0.00048296017],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025208612,0.000074346906,0.00017399329,0.00007842758,0.00026892856,0.00005782479,0.0003505517,0.000029797233,0.0036240674],"category_scores_gemma":[0.00008892876,0.000042891872,0.00011139998,0.0002793265,0.00057263614,0.0002528117,0.0000097053235,0.000090398345,0.000009710042],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000046602245,0.0000011572567,0.992585,0.0000046422465,0.000011421147,0.000005435798,0.0001072869,0.005508698,0.00011165993,0.00005067894,0.00013720932,0.0014721545],"study_design_scores_gemma":[0.00010795371,0.00014227683,0.98758745,0.000010922465,0.000028708968,0.000085113716,0.00022855678,0.00931094,0.00046376185,0.0014518681,0.00051147514,0.000070942864],"about_ca_topic_score_codex":0.036007512,"about_ca_topic_score_gemma":0.4873159,"teacher_disagreement_score":0.45130837,"about_ca_system_score_codex":9.801507e-7,"about_ca_system_score_gemma":0.00032906848,"threshold_uncertainty_score":0.99728674},"labels":[],"label_agreement":null},{"id":"W3111252837","doi":"10.1139/cjes-2020-0163","title":"Dale Alan Russell (1937–2019): voyageur of a vanished world<sup>1</sup>","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Carleton University; University of Alberta; Canadian Museum of Nature","funders":"","keywords":"Adventure; Globe; Environmental ethics; History; Art history; Classics; Philosophy; Psychology","score_opus":0.022966419983245386,"score_gpt":0.2063210324685371,"score_spread":0.18335461248529172,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3111252837","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96109277,0.004540871,0.000032921304,0.0044461745,0.00047972405,0.00007521118,0.00011160882,0.0000068298323,0.029213883],"genre_scores_gemma":[0.99745196,0.00005369895,0.0009930921,0.0010056644,0.00021184691,7.9739415e-8,0.000007913853,0.0000015157617,0.00027424662],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99855834,0.00014861049,0.00041337428,0.00020492473,0.0002127282,0.00046202817],"domain_scores_gemma":[0.9985494,0.00016957447,0.00025312766,0.0000901582,0.00009206099,0.0008456911],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000659757,0.000120903416,0.00029340573,0.00030422275,0.00030369242,0.000036943104,0.0006452103,0.000073662515,0.0039105522],"category_scores_gemma":[0.00021887031,0.000093165785,0.000099677854,0.0007158512,0.0010045841,0.00036842612,0.000005557792,0.0002357529,0.00014932742],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002536918,0.0000036417957,0.9901167,0.0000065378795,0.000018346713,0.000106748994,0.0005375707,0.005253031,0.0000252688,0.00018857149,0.0025355716,0.0011826436],"study_design_scores_gemma":[0.0002505485,0.0007113873,0.9346774,0.000024690788,0.000018573512,0.00021814302,0.0004502953,0.0051378217,0.000050216306,0.0006532604,0.057661563,0.00014605674],"about_ca_topic_score_codex":0.007098537,"about_ca_topic_score_gemma":0.25588152,"teacher_disagreement_score":0.24878298,"about_ca_system_score_codex":0.0000012868659,"about_ca_system_score_gemma":0.0013193594,"threshold_uncertainty_score":0.99951327},"labels":[],"label_agreement":null},{"id":"W3112048217","doi":"10.1139/cjes-2020-0168","title":"A systematic reappraisal and quantitative study of the nonmarine teleost fishes from the late Maastrichtian of the Western Interior of North America: evidence from vertebrate microfossil localities<sup>1</sup>","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Ichthyology and Marine Biology","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; University of Alberta","funders":"University of California Museum of Paleontology; Burke Museum, University of Washington; Montana Department of Natural Resources and Conservation","keywords":"Paleontology; Geology; Taphonomy; Cretaceous; Paleogene; Cenozoic; Vertebrate; Extinction event; Taxon; Extinction (optical mineralogy); Abundance (ecology); Structural basin; Ecology; Biology; Biological dispersal; Population","score_opus":0.023985474112240085,"score_gpt":0.23204853868366868,"score_spread":0.2080630645714286,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3112048217","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99743176,0.0003403313,0.000019185107,0.0017134894,0.00013760636,0.00024636148,0.000055550074,9.329306e-7,0.000054781372],"genre_scores_gemma":[0.99945897,0.000018224566,0.000094400755,0.0003769397,0.000019058223,0.0000015536577,2.923519e-7,0.0000029526836,0.000027602919],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983663,0.000512517,0.0005323865,0.00015933799,0.00024240803,0.00018703972],"domain_scores_gemma":[0.99842995,0.0005547525,0.00063362357,0.0002003351,0.000045894376,0.00013542364],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044621277,0.00011447991,0.00037009997,0.000030820447,0.00020150589,0.000026283726,0.0010498345,0.000030637984,0.00010826489],"category_scores_gemma":[0.0008006862,0.00005349114,0.00006987373,0.0004639564,0.002479776,0.00018762704,0.00021694328,0.0001836417,0.000004428902],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028218703,0.000011285152,0.9837232,0.00003247874,0.000054118413,0.0000048946217,0.014887205,0.0006663722,0.00037707572,0.0000024363255,0.000052219795,0.0001604831],"study_design_scores_gemma":[0.00018618275,0.0007277851,0.98753035,0.00039330428,0.0000784102,0.000009812735,0.0099401735,0.0007344055,0.00025862557,0.000016011854,0.00006501172,0.000059906943],"about_ca_topic_score_codex":0.09272646,"about_ca_topic_score_gemma":0.36474887,"teacher_disagreement_score":0.2720224,"about_ca_system_score_codex":0.0000060641523,"about_ca_system_score_gemma":0.0002526916,"threshold_uncertainty_score":0.91368383},"labels":[],"label_agreement":null},{"id":"W3112098498","doi":"10.1139/cjes-2020-0161","title":"Late Devonian magmatism and clastic deposition in the upper Earn Group (central Yukon, Canada) mark the transition from passive to active margin along western Laurentia","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon University; Geological Survey of Canada","funders":"","keywords":"Geology; Diorite; Devonian; Geochemistry; Zircon; Laurentia; Clastic rock; Magmatism; Passive margin; Continental arc; Paleontology; Rift; Paleozoic; Sedimentary rock; Structural basin","score_opus":0.008349327268668867,"score_gpt":0.16671155061227313,"score_spread":0.15836222334360428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3112098498","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9635168,0.00037109636,0.00013056555,0.03555805,0.00009181318,0.00007876925,0.00008288036,0.0000012429509,0.00016882188],"genre_scores_gemma":[0.99569404,0.0000130808485,0.00017169544,0.00400199,0.0001019548,3.6160293e-7,0.00001276677,8.7853044e-7,0.0000032198816],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988439,0.00015156064,0.00021076971,0.00016016657,0.00030747763,0.00032609666],"domain_scores_gemma":[0.9991671,0.00017840137,0.00008514337,0.000044592412,0.000033303382,0.0004914792],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019868759,0.00009362131,0.000140555,0.000059259466,0.00030089298,0.0001654483,0.0003187819,0.000031296342,0.00089748437],"category_scores_gemma":[0.00006800101,0.000049123635,0.000042929307,0.0004305086,0.0001957728,0.00020196394,0.000004307325,0.00021497946,0.0000074615596],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032352695,0.000004092782,0.97775656,0.0000039629363,0.000022860955,0.00020392583,0.003122085,0.006722868,0.00007322469,0.000020434509,0.0001720789,0.0118655255],"study_design_scores_gemma":[0.00009587393,0.000121615885,0.9933439,0.000025642556,0.00002449226,0.00002467673,0.0013291477,0.003859844,0.000036311976,0.00068424776,0.0003769612,0.00007726985],"about_ca_topic_score_codex":0.72194725,"about_ca_topic_score_gemma":0.99812734,"teacher_disagreement_score":0.2761801,"about_ca_system_score_codex":0.0000033035262,"about_ca_system_score_gemma":0.00032616573,"threshold_uncertainty_score":0.9826824},"labels":[],"label_agreement":null},{"id":"W3113271861","doi":"10.1139/cjes-2020-0057","title":"Crustal thickening and uplift of the Qiangtang Terrane, Tibetan Plateau during the Late Cretaceous to early Palaeocene: geochronology and geochemistry of the Saiduopugangri granite","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Jilin University","keywords":"Geology; Geochronology; Zircon; Geochemistry; Terrane; Magmatism; Cretaceous; Provenance; Plateau (mathematics); Mantle (geology); Basalt; Petrogenesis; Petrology; Paleontology; Tectonics","score_opus":0.010383055484962421,"score_gpt":0.1713467241745507,"score_spread":0.16096366868958828,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3113271861","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9898302,0.0016086752,0.0000015834597,0.007834195,0.00007347777,0.00006148455,0.000038419606,0.0000016588602,0.0005502844],"genre_scores_gemma":[0.9993297,0.000028711462,0.00007154538,0.00046498628,0.000050432867,1.0861514e-7,4.0986876e-7,0.0000011414638,0.000052972693],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989797,0.00006754378,0.000284266,0.00014580615,0.00023865628,0.00028405213],"domain_scores_gemma":[0.99914134,0.00011682685,0.00022230567,0.00010316233,0.00007396338,0.0003424063],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032498685,0.00010249803,0.00021311312,0.000048734615,0.00042182035,0.000078098696,0.0005637113,0.00005588253,0.00043278013],"category_scores_gemma":[0.0002560415,0.000046263336,0.00009099926,0.00050454104,0.0010959227,0.00012503065,0.000042186824,0.00026412145,0.0000017428918],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001094448,0.0000011609161,0.9942841,0.000015587075,0.00001966151,0.000010211741,0.00096049294,0.0012673704,0.0026751799,0.000010602778,0.000011589204,0.00073308666],"study_design_scores_gemma":[0.000105137566,0.0001094629,0.9937191,0.00004357598,0.0000305805,0.00007052945,0.0005700006,0.0005658678,0.0038952592,0.00053699757,0.00028239065,0.00007112315],"about_ca_topic_score_codex":0.008938793,"about_ca_topic_score_gemma":0.07830405,"teacher_disagreement_score":0.06936526,"about_ca_system_score_codex":0.0000010473534,"about_ca_system_score_gemma":0.00019687702,"threshold_uncertainty_score":0.99766076},"labels":[],"label_agreement":null},{"id":"W3114057923","doi":"10.1139/cjes-2019-0196","title":"Lithogeochemical, isotopic, and U–Pb (zircon) age constraints on arc to rift magmatism, northwestern and central Avalon Terrane, Newfoundland, Canada: implications for local lithostratigraphy","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Government of Newfoundland and Labrador","funders":"","keywords":"Geology; Terrane; Zircon; Felsic; Geochemistry; Schist; Cove; Basement; Mafic; Magmatism; Continental arc; Rift; Paleontology; Metamorphic rock; Geomorphology; Volcanic rock; Archaeology; Structural basin; Tectonics","score_opus":0.02142934873207609,"score_gpt":0.2051976345337252,"score_spread":0.1837682858016491,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3114057923","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9793422,0.00038063634,0.00086159544,0.01786929,0.0000794437,0.00014851359,0.00034610173,0.0000035898254,0.00096859265],"genre_scores_gemma":[0.9938318,0.000019884723,0.0025916656,0.0034355833,0.00009320422,7.328554e-7,0.00001670751,0.0000012573614,0.000009136641],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988341,0.000029286122,0.00028784017,0.00025919723,0.00016469034,0.00042492172],"domain_scores_gemma":[0.9979443,0.00016867154,0.00009823814,0.00006238519,0.00006836034,0.0016580283],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013336973,0.00013169342,0.00023677782,0.000094247625,0.00028606332,0.00015492225,0.00023761572,0.00004465724,0.00049105234],"category_scores_gemma":[0.000112767644,0.000094880554,0.000059710746,0.00028788848,0.0006779194,0.00011978021,0.000005751709,0.00013757857,0.0000025146383],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018783434,0.000003529276,0.9778497,0.000013724594,0.000018598903,0.000036772803,0.00020952839,0.00027344612,0.00027565507,0.00021112867,0.00022295368,0.020866157],"study_design_scores_gemma":[0.00018791578,0.0005054328,0.99288136,0.000024642424,0.00002234352,0.00006467564,0.0002133166,0.00031881177,0.00013396463,0.0014927356,0.004011857,0.00014296244],"about_ca_topic_score_codex":0.41119787,"about_ca_topic_score_gemma":0.99381936,"teacher_disagreement_score":0.58262146,"about_ca_system_score_codex":0.0000023675386,"about_ca_system_score_gemma":0.0006731246,"threshold_uncertainty_score":0.592723},"labels":[],"label_agreement":null},{"id":"W3117424911","doi":"10.1139/cjes-2019-0207","title":"First occurrence of <i>Maiasaura</i> (Dinosauria, Hadrosauridae) from the Upper Cretaceous Oldman Formation of southern Alberta, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; University of Toronto; Carleton University","funders":"","keywords":"Geology; Paleontology; Skull; Cretaceous; Ridge; Cladogenesis; Biology; Phylogenetic tree","score_opus":0.01610792095205612,"score_gpt":0.18179709221081253,"score_spread":0.1656891712587564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3117424911","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98667896,0.0033841655,0.000040002258,0.007061707,0.00047225837,0.00006472275,0.00097261136,0.00000130651,0.0013242557],"genre_scores_gemma":[0.99870807,0.00003750601,0.0001483774,0.0009683132,0.00010144536,1.0524407e-7,0.00002053429,7.6648536e-7,0.00001485844],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99877805,0.000110484565,0.0004341636,0.00012997101,0.00025243714,0.00029492244],"domain_scores_gemma":[0.99856097,0.00046490703,0.00041745964,0.000092389506,0.000109247376,0.0003550125],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00033963463,0.0001006178,0.00022801622,0.000060147348,0.00033517016,0.000019604871,0.0006554079,0.0000580761,0.0013406255],"category_scores_gemma":[0.00029057596,0.000065111315,0.00007051902,0.0002976415,0.00073411566,0.00025113276,0.000005312948,0.00016598449,0.000020630685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025714095,0.0000017357075,0.9921335,0.000007123508,0.000013527603,0.000014578084,0.0016069767,0.0032565456,0.000015640288,0.000021846321,0.0023071743,0.00059562305],"study_design_scores_gemma":[0.00021157788,0.00030347155,0.96684724,0.000054115888,0.000026672753,0.00008283893,0.002412323,0.004316223,0.00016168716,0.00021568604,0.02523847,0.00012972155],"about_ca_topic_score_codex":0.8938519,"about_ca_topic_score_gemma":0.9990381,"teacher_disagreement_score":0.10518619,"about_ca_system_score_codex":0.000002419859,"about_ca_system_score_gemma":0.0023440754,"threshold_uncertainty_score":0.9995723},"labels":[],"label_agreement":null},{"id":"W3118391445","doi":"10.1139/cjes-2020-0094","title":"Geochemistry and U–Pb geochronology of the Williams Brook area, Tobique–Chaleur zone, New Brunswick: stratigraphic and geotectonic setting of gold mineralization","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Felsic; Geology; Mafic; Geochemistry; Geochronology; Zircon; Mineralization (soil science); Volcanic rock; Rhyolite; Silicic; Partial melting; Volcano; Mantle (geology)","score_opus":0.010711842198388232,"score_gpt":0.17992846788471403,"score_spread":0.1692166256863258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3118391445","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911754,0.0063163005,0.00003696654,0.0015518919,0.00006245204,0.0000278838,0.00001434834,0.0000012410678,0.00081348384],"genre_scores_gemma":[0.9988187,0.00018300713,0.000589557,0.00012808043,0.0000327654,2.9816412e-8,0.0000035949743,7.2304664e-7,0.00024352076],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99903136,0.000059033067,0.00032653115,0.00016559164,0.00018120365,0.00023628105],"domain_scores_gemma":[0.9990901,0.00010628682,0.00027435584,0.00008997966,0.00013109276,0.00030818288],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003062738,0.000091771566,0.00023240289,0.00009247499,0.00012409182,0.000041679945,0.00021538761,0.00006838457,0.0010341988],"category_scores_gemma":[0.00021807353,0.00005847525,0.00007593214,0.0005618544,0.00067904603,0.00013058294,0.0000123413865,0.00014197851,4.078054e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000024637363,0.0000029011128,0.9910536,0.000018871588,0.000017652459,0.000011562603,0.00010318086,0.0017415499,0.0042487313,0.00009955377,0.000032707412,0.00266727],"study_design_scores_gemma":[0.000147155,0.00012374618,0.9841661,0.00007790154,0.00003726233,0.00023998006,0.00034351143,0.002363993,0.009319865,0.0028536746,0.00023528688,0.00009153698],"about_ca_topic_score_codex":0.06503074,"about_ca_topic_score_gemma":0.7850357,"teacher_disagreement_score":0.72000504,"about_ca_system_score_codex":7.95944e-7,"about_ca_system_score_gemma":0.0013491587,"threshold_uncertainty_score":0.999879},"labels":[],"label_agreement":null},{"id":"W3118523056","doi":"10.1139/cjes-2020-0146","title":"Subsidence et évolution thermique des bassins de la marge atlantique camerounaise : premiers résultats à partir des puits en mer du sous-bassin de Kribi-Campo (Marge passive Ouest Africaine, Golfe de Guinée)","year":2021,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Humanities; Subsidence; Geomorphology; Art; Structural basin","score_opus":0.024788789225239923,"score_gpt":0.24783432368101727,"score_spread":0.22304553445577735,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3118523056","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96396583,0.014431174,0.0036713092,0.010022177,0.0005012734,0.00012410498,0.00019700419,0.000014024174,0.0070731016],"genre_scores_gemma":[0.9795765,0.006018118,0.012419551,0.00080957287,0.00023545978,0.0000030372453,0.000015574371,0.0000083017585,0.0009138306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99533236,0.0018089376,0.0006526311,0.0003504852,0.0004162523,0.0014393608],"domain_scores_gemma":[0.995696,0.0013653656,0.00045733975,0.0001576191,0.0006127881,0.0017108704],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":["sts"],"category_scores_codex":[0.0049521136,0.00031646749,0.00039102638,0.00029166078,0.0015833727,0.00088827393,0.0006990752,0.00029810026,0.002670616],"category_scores_gemma":[0.0044792295,0.00025430304,0.00018011034,0.0013399923,0.0035028507,0.0017929254,0.000024678451,0.0006267349,0.00005096603],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020360727,0.000044379318,0.9593747,0.00009888941,0.000040263585,0.0009319722,0.007660872,0.01887239,0.0002793558,0.001498398,0.0018359418,0.009342433],"study_design_scores_gemma":[0.00026543147,0.00039730096,0.9334193,0.00058131636,0.00007402435,0.0029918933,0.003938362,0.0074027865,0.0011815837,0.011783386,0.0375863,0.000378308],"about_ca_topic_score_codex":0.051358484,"about_ca_topic_score_gemma":0.5882716,"teacher_disagreement_score":0.53691316,"about_ca_system_score_codex":0.00008783947,"about_ca_system_score_gemma":0.01394185,"threshold_uncertainty_score":0.99999094},"labels":[],"label_agreement":null},{"id":"W3119730399","doi":"10.1139/cjes-2020-0063","title":"Nd isotope mapping of the Frontenac Terrane in southwestern Grenville Province","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"","keywords":"Geology; Terrane; Rift; Volcano; Shear zone; Mantle (geology); Seismology; Provenance; Pluton; Geochemistry; Tectonics","score_opus":0.021350940206969215,"score_gpt":0.1802428565816227,"score_spread":0.1588919163746535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3119730399","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99162567,0.0017958826,0.000007444051,0.0022373952,0.00018626089,0.00003074983,0.000016872465,6.838008e-7,0.004099072],"genre_scores_gemma":[0.99893326,0.000012987552,0.00037114238,0.00030694893,0.000038680413,5.5407792e-8,9.674209e-7,5.1853823e-7,0.00033542464],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989638,0.00007730295,0.00031060493,0.00013163703,0.00023944031,0.00027724696],"domain_scores_gemma":[0.9993547,0.000065152286,0.00016567286,0.00009085323,0.00008442202,0.00023916249],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00044110758,0.0000688339,0.00018754794,0.00012198177,0.00014062946,0.000049012175,0.0004337193,0.000032856617,0.0038710886],"category_scores_gemma":[0.00020931891,0.000037803085,0.0001064262,0.0006774779,0.00043113006,0.00011715496,0.000010154804,0.00015230659,0.000013001863],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000015544304,0.0000033159597,0.99584234,0.0000041434078,0.0000049498567,0.0000598506,0.00013361158,0.0014345193,0.00021607557,0.000014122818,0.000021448412,0.0022640924],"study_design_scores_gemma":[0.000096345604,0.000050043163,0.9941503,0.00006126561,0.0000061807214,0.000061108476,0.0006359211,0.0005905648,0.0005862365,0.0015248795,0.0021750415,0.000062146086],"about_ca_topic_score_codex":0.035672765,"about_ca_topic_score_gemma":0.8494729,"teacher_disagreement_score":0.8138001,"about_ca_system_score_codex":0.0000011750166,"about_ca_system_score_gemma":0.0008641884,"threshold_uncertainty_score":0.9970395},"labels":[],"label_agreement":null},{"id":"W3120462117","doi":"10.1139/cjes-2020-0173","title":"A redescription of <i>Lophorhothon atopus</i> (Ornithopoda: Dinosauria) from the Late Cretaceous of Alabama based on new material<sup>1</sup>","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Auburn University","keywords":"Autapomorphy; Paleontology; Holotype; Geology; Taxon; Theropoda; Cretaceous; Biology; Taxonomy (biology); Phylogenetic tree; Zoology","score_opus":0.0204320059870244,"score_gpt":0.20091405161845816,"score_spread":0.18048204563143375,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3120462117","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921473,0.0023996523,0.00003579076,0.0022346042,0.00083553785,0.000053883035,0.00032675915,0.000002646469,0.001963771],"genre_scores_gemma":[0.9980083,0.00007780005,0.0010011954,0.0005652481,0.00017959274,1.0526114e-7,0.000029767962,0.0000015526522,0.00013643899],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99855703,0.00031471637,0.00040875794,0.00016496106,0.00024640816,0.00030811198],"domain_scores_gemma":[0.9987606,0.00032103562,0.0003187906,0.00015841464,0.00013170028,0.0003094498],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007048631,0.000111611975,0.0002755458,0.00014487741,0.00026575473,0.00003886505,0.00041450278,0.00010645969,0.0027328643],"category_scores_gemma":[0.00026867798,0.000075530326,0.0001046534,0.00040891118,0.00071078603,0.0001802887,0.000004424792,0.00016548879,0.000016956994],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000101652615,0.000009108476,0.9761441,0.000005646129,0.000027022723,0.000107750515,0.00046822673,0.018325364,0.0007942133,0.000058040605,0.0010252976,0.0029336012],"study_design_scores_gemma":[0.00030838838,0.000515078,0.9843239,0.00010577641,0.00003263121,0.0001270538,0.00057631417,0.0038448533,0.0016339676,0.0011452454,0.00727656,0.00011021018],"about_ca_topic_score_codex":0.01465197,"about_ca_topic_score_gemma":0.20193511,"teacher_disagreement_score":0.18728314,"about_ca_system_score_codex":0.000002535574,"about_ca_system_score_gemma":0.002064262,"threshold_uncertainty_score":0.9981788},"labels":[],"label_agreement":null},{"id":"W3121708316","doi":"10.1139/cjes-2020-0177","title":"Mandibular force profiles and tooth morphology in growth series of <i>Albertosaurus sarcophagus</i> and <i>Gorgosaurus libratus</i> (Tyrannosauridae: Albertosaurinae) provide evidence for an ontogenetic dietary shift in tyrannosaurids<sup>1</sup>","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Calgary; Royal Tyrrell Museum","funders":"Natural Sciences and Engineering Research Council of Canada; Killam Trusts","keywords":"Ontogeny; Biology; Juvenile; Mastication; Bite force quotient; Anatomy; Morphology (biology); Mandible (arthropod mouthpart); Allometry; Predation; Zoology; Ecology; Paleontology","score_opus":0.02686360762693305,"score_gpt":0.23402887484620297,"score_spread":0.20716526721926992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3121708316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.959109,0.036970854,0.000019361572,0.002964153,0.00021386417,0.000310836,0.00013493549,0.000004181006,0.00027283392],"genre_scores_gemma":[0.995503,0.0011008576,0.0027073727,0.0004905289,0.000095404204,0.0000046499918,0.000026812744,0.0000051798875,0.00006617573],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973726,0.00039319476,0.00072515546,0.0005315366,0.0002076973,0.00076978427],"domain_scores_gemma":[0.99827075,0.00065430556,0.00026489634,0.00017063103,0.00012053911,0.00051887595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010836166,0.00025560707,0.00058010244,0.00052082416,0.00029811327,0.00007876128,0.0004416563,0.00021309395,0.0001302634],"category_scores_gemma":[0.00057576835,0.0002225975,0.00007208392,0.00061302853,0.0017457341,0.0014363313,0.000021247004,0.00029954585,0.0000016463422],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002603635,0.000022231214,0.9948186,0.000103598526,0.000017592214,0.000418726,0.0009586938,0.0014109215,0.0005210118,0.000352712,0.00006276795,0.0010527468],"study_design_scores_gemma":[0.00078967254,0.0018747633,0.9867493,0.0002352909,0.000028078857,0.0016002702,0.00058534695,0.0012838067,0.0009859122,0.005089983,0.0005069319,0.00027064723],"about_ca_topic_score_codex":0.021420194,"about_ca_topic_score_gemma":0.5864875,"teacher_disagreement_score":0.56506723,"about_ca_system_score_codex":0.0000053388085,"about_ca_system_score_gemma":0.0019879665,"threshold_uncertainty_score":0.9850963},"labels":[],"label_agreement":null},{"id":"W3122508315","doi":"10.1139/cjes-2020-0169","title":"Baby tyrannosaurid bones and teeth from the Late Cretaceous of western North America<sup>1</sup>","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Dinosaur Research Institute; Leverhulme Trust; Alberta Historical Resources Foundation; Canadian Light Source; National Science Foundation","keywords":"Paleontology; Canyon; Cretaceous; Geology; Laurasia; Tetrapod (structure); Biology; Mesozoic; Structural basin; Geomorphology","score_opus":0.015472026144885366,"score_gpt":0.2003806657613085,"score_spread":0.18490863961642315,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3122508315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9766132,0.018970983,0.000012270108,0.0028949298,0.00024610624,0.000029770748,0.00019325662,0.0000020126479,0.0010374271],"genre_scores_gemma":[0.99823797,0.00042064098,0.00037384947,0.0007083533,0.00011462498,7.921529e-8,0.000014700884,9.4570976e-7,0.00012885299],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989513,0.00018207113,0.00026613593,0.00014416437,0.00015363884,0.00030266575],"domain_scores_gemma":[0.99894977,0.00036644484,0.00017752612,0.0001014004,0.00010020354,0.00030466903],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003275859,0.000091520626,0.00021875219,0.00008754223,0.00038590957,0.000046187408,0.00033263062,0.000054106244,0.00067549833],"category_scores_gemma":[0.00015984174,0.000057805508,0.00005220465,0.0003247783,0.0014932464,0.00022339489,0.0000068634085,0.0001762358,0.000020820175],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009159127,0.0000020658065,0.99117583,0.0000017585173,0.000021030326,0.00011578817,0.00069449603,0.0029552823,0.000009426421,0.0000057473726,0.00013862266,0.0048707984],"study_design_scores_gemma":[0.00009606428,0.00017116056,0.97838974,0.000019029525,0.000017870727,0.0002923972,0.0008705644,0.00094295235,0.000014008794,0.00029922204,0.01881313,0.00007385033],"about_ca_topic_score_codex":0.015814397,"about_ca_topic_score_gemma":0.6447426,"teacher_disagreement_score":0.6289282,"about_ca_system_score_codex":7.618423e-7,"about_ca_system_score_gemma":0.0010479112,"threshold_uncertainty_score":0.9907394},"labels":[],"label_agreement":null},{"id":"W3128764755","doi":"10.1139/cjes-2020-0148","title":"Lithobiotopes of the Nemegt Gobi Basin<sup>1</sup>","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta; Tisec (Canada)","funders":"","keywords":"Geology; Facies; Paleontology; Ephemeral key; Cretaceous; Structural basin; Alluvial fan; Fluvial; Fauna; Graben; Alluvium; Trace fossil; Ecology","score_opus":0.01755906485805452,"score_gpt":0.20384327603404842,"score_spread":0.1862842111759939,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3128764755","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9755453,0.005106895,0.000009892624,0.0032328032,0.00079383946,0.00003468945,0.000051933013,0.0000016656351,0.015223006],"genre_scores_gemma":[0.99811053,0.00005941481,0.00069673295,0.000567026,0.00015600388,5.457759e-8,0.0000019921258,6.769669e-7,0.00040758966],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988909,0.00021156791,0.00027726995,0.00013015616,0.00016643837,0.00032366684],"domain_scores_gemma":[0.9991295,0.00015436049,0.00016769639,0.00011879047,0.00014976552,0.00027989334],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006927054,0.00007572108,0.0001758454,0.00011824525,0.0004467967,0.000032221134,0.00051202864,0.00007321036,0.0023572627],"category_scores_gemma":[0.00030867875,0.00004656088,0.000106463995,0.0005283627,0.0012673396,0.00021911046,0.0000062411928,0.00017476108,0.000026808784],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003886666,0.000002698974,0.99450314,0.0000030361052,0.000010855841,0.00004786777,0.00019413566,0.0025431258,0.000019432511,0.00024704915,0.000473589,0.0019511816],"study_design_scores_gemma":[0.00008991461,0.000115530056,0.9579836,0.000029553838,0.000009730722,0.0006276959,0.0005018134,0.0005529469,0.00017184115,0.0008322529,0.039023913,0.000061194056],"about_ca_topic_score_codex":0.007446122,"about_ca_topic_score_gemma":0.37356573,"teacher_disagreement_score":0.36611962,"about_ca_system_score_codex":0.000001253945,"about_ca_system_score_gemma":0.0028347436,"threshold_uncertainty_score":0.9991634},"labels":[],"label_agreement":null},{"id":"W3129417501","doi":"10.1139/cjes-2020-0089","title":"Meguma terrane orocline: U–Pb age and paleomagnetism of the Silurian Mavillette gabbro, Nova Scotia, Canada","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; University of Alberta; Technical University of Nova Scotia; Acadia University; Nova Scotia Department of Energy; Western University","funders":"","keywords":"Geology; Terrane; Paleomagnetism; Gabbro; Devonian; Sill; Geochemistry; Carboniferous; Paleozoic; Apparent polar wander; Ordovician; Paleontology; Igneous rock; Tectonics; Structural basin","score_opus":0.016379230479496715,"score_gpt":0.17306254165542573,"score_spread":0.156683311175929,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3129417501","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97582406,0.0012398621,0.0000044878593,0.020082464,0.00022597982,0.00004477935,0.000047462305,0.0000014129424,0.0025294677],"genre_scores_gemma":[0.99640626,0.000014612667,0.00045000808,0.0029556924,0.000115965944,2.460951e-8,0.0000019103118,9.5072613e-7,0.00005456632],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99870056,0.00006553294,0.00034721405,0.00017171616,0.00038475264,0.00033019908],"domain_scores_gemma":[0.99875236,0.00009702964,0.00020605014,0.00008102465,0.0000743597,0.000789205],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00028087237,0.00011106262,0.00025264395,0.00006301264,0.00020088218,0.00006037736,0.0005565937,0.000033998804,0.0055094333],"category_scores_gemma":[0.00027313223,0.000061792256,0.000085735344,0.00060969085,0.0007446723,0.00011699939,0.00001242603,0.00019094447,0.0000078007815],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005428518,0.0000016726764,0.99423194,0.000010528974,0.0000144826245,0.00017539,0.00010484106,0.0010661731,0.0002826976,0.000019356728,0.00094168965,0.0031458144],"study_design_scores_gemma":[0.0001310808,0.00019101526,0.99334735,0.000025001698,0.00002466093,0.00006664625,0.00012346846,0.00048651325,0.00040102494,0.00039304543,0.004708068,0.00010214618],"about_ca_topic_score_codex":0.8627535,"about_ca_topic_score_gemma":0.99890757,"teacher_disagreement_score":0.13615404,"about_ca_system_score_codex":0.0000010940072,"about_ca_system_score_gemma":0.0009542619,"threshold_uncertainty_score":0.99539965},"labels":[],"label_agreement":null},{"id":"W3129493663","doi":"10.1139/cjes-2021-0006","title":"The mid-Cretaceous Peninsular Ranges orogeny: a new slant on Cordilleran tectonics? II: northern United States and Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Pluton; Terrane; Orogeny; Cretaceous; Subduction; North American Plate; Back-arc basin; Paleontology; Island arc; Plate tectonics; Trough (economics); Thrust fault; Geochemistry; Tectonics","score_opus":0.011070503303250875,"score_gpt":0.17485436997577286,"score_spread":0.16378386667252198,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3129493663","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97812986,0.008856554,0.0000015121141,0.011920428,0.00020615333,0.00003291038,0.000043356038,0.000002485589,0.00080676406],"genre_scores_gemma":[0.99770075,0.0005774505,0.00009986862,0.001161953,0.00006849943,7.923343e-8,0.000015056613,0.0000013182269,0.0003750374],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99866056,0.00008788522,0.00025057406,0.00018702909,0.00037474328,0.00043921074],"domain_scores_gemma":[0.99838454,0.00031281103,0.00013210828,0.00010207976,0.00017876211,0.0008897079],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038156152,0.00012344989,0.00019799561,0.000102277525,0.0010857676,0.00019931699,0.000300523,0.000033497956,0.0017437396],"category_scores_gemma":[0.000318724,0.00006715907,0.00006697372,0.00058578764,0.00042382008,0.000074354626,0.000009898761,0.00020227785,0.0000069044027],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000309363,0.0000050544213,0.9720003,0.000004004486,0.00007911495,0.0010452931,0.00028428147,0.011404072,0.000067461915,0.00004096897,0.0010056958,0.014032818],"study_design_scores_gemma":[0.0006550783,0.0010109929,0.62751234,0.000074442374,0.000092369366,0.0010476595,0.0031900452,0.0055599883,0.0017229706,0.0053791334,0.3532841,0.0004708913],"about_ca_topic_score_codex":0.9223175,"about_ca_topic_score_gemma":0.9996616,"teacher_disagreement_score":0.35227838,"about_ca_system_score_codex":0.0000035820137,"about_ca_system_score_gemma":0.0031026362,"threshold_uncertainty_score":0.9991688},"labels":[],"label_agreement":null},{"id":"W3132904690","doi":"10.1139/cjes-2020-0154","title":"The mid-Cretaceous Peninsular Ranges orogeny: a new slant on Cordilleran tectonics? I: Mexico to Nevada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Orogeny; Cretaceous; Pluton; Subduction; Trough (economics); Back-arc basin; Geochemistry; Paleontology; Tectonics; Geomorphology","score_opus":0.019516120358406448,"score_gpt":0.2051274377110481,"score_spread":0.18561131735264166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3132904690","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9613485,0.008808618,0.000021446596,0.022258172,0.00052072504,0.00006170016,0.000023029013,0.000005091984,0.0069527477],"genre_scores_gemma":[0.99616903,0.000160672,0.0006892508,0.0021245466,0.00016409004,1.6433395e-7,0.0000032922396,0.0000015812336,0.0006873622],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982615,0.00010842923,0.00031728882,0.00024820163,0.00048753386,0.0005770257],"domain_scores_gemma":[0.99783677,0.0003221723,0.0001278913,0.00016342683,0.00017147422,0.0013782606],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006758243,0.0001410585,0.00025475246,0.00014323842,0.00079844776,0.00033706857,0.00056021346,0.00004840923,0.006656508],"category_scores_gemma":[0.00066845195,0.00007645627,0.00017761151,0.0009999162,0.0003378171,0.00011274303,0.000010659273,0.00023677576,0.00020359065],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014091907,0.00002434015,0.83447236,0.000008432594,0.00019780382,0.0030525082,0.00077232294,0.041755605,0.0013750644,0.0005643769,0.0069296304,0.110706665],"study_design_scores_gemma":[0.0006285615,0.001730995,0.45374507,0.00010604364,0.000095420095,0.0012327837,0.0015425492,0.0021615967,0.01244939,0.012388937,0.5133369,0.00058175914],"about_ca_topic_score_codex":0.018198432,"about_ca_topic_score_gemma":0.62437785,"teacher_disagreement_score":0.6061794,"about_ca_system_score_codex":0.0000026571797,"about_ca_system_score_gemma":0.0016499097,"threshold_uncertainty_score":0.99425155},"labels":[],"label_agreement":null},{"id":"W3134165338","doi":"10.1139/cjes-2020-0046","title":"Timing and provenance of Paleoproterozoic supracrustal rocks in the central Thelon tectonic zone, Canada: implications for the tectonic evolution of western Laurentia from ca. 2.1 to 1.9 Ga","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Detritus; Provenance; Zircon; Laurentia; Geochemistry; Archean; Craton; Terrane; Clastic rock; Foreland basin; Pluton; Ordovician; Paleontology; Sedimentary rock; Tectonics","score_opus":0.015778374000558336,"score_gpt":0.20390991408533596,"score_spread":0.18813154008477762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3134165338","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909456,0.003509702,0.0003126259,0.0047735265,0.000066769986,0.00012513148,0.00016914635,4.866934e-7,0.00009702082],"genre_scores_gemma":[0.9995163,0.000027283866,0.0002723285,0.00012798324,0.000032087904,0.0000011518757,0.0000051267284,6.22357e-7,0.00001711029],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999106,0.00005285877,0.00026830623,0.00013244884,0.0001699124,0.0002704639],"domain_scores_gemma":[0.99917513,0.00029797936,0.00015909188,0.0000977781,0.00011395341,0.0001560402],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035854362,0.00006549295,0.00015404545,0.00006423688,0.00020001056,0.00004012033,0.00033953047,0.000024770512,0.00027192303],"category_scores_gemma":[0.00019368241,0.000034709647,0.000052463503,0.0005236925,0.00020283044,0.000087849294,0.000006992269,0.00010286747,4.1876203e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005625988,0.000004035869,0.9918323,0.0000056243366,0.000011123264,0.0000034640045,0.00020511821,0.0046934825,0.00036804847,0.00003321381,0.000029511582,0.0028084589],"study_design_scores_gemma":[0.00008357581,0.000093599825,0.99562943,0.00003475635,0.000024488605,0.000020821539,0.0008381536,0.0009242095,0.00058592996,0.0011999788,0.0005166216,0.00004846346],"about_ca_topic_score_codex":0.78586316,"about_ca_topic_score_gemma":0.9983602,"teacher_disagreement_score":0.21249703,"about_ca_system_score_codex":0.0000046109362,"about_ca_system_score_gemma":0.0015565356,"threshold_uncertainty_score":0.29773664},"labels":[],"label_agreement":null},{"id":"W3134717738","doi":"10.1139/cjes-2020-0143","title":"Tectonic history of the Grenville-age Trenton Prong inlier, Central Appalachians, USA: evidence from SHRIMP U–Pb geochronology","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Zircon; Geology; Metamorphism; Laurentia; Geochemistry; Gneiss; Geochronology; Orogeny; Rodinia; Granulite; Terrane; Metamorphic rock; Petrology; Facies; Craton; Paleontology; Tectonics; Paleozoic","score_opus":0.027772119069698547,"score_gpt":0.19318295423470347,"score_spread":0.16541083516500493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3134717738","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9742738,0.02014685,0.00001322025,0.0018069637,0.000901643,0.00004322352,0.000030739393,0.0000018688656,0.0027816966],"genre_scores_gemma":[0.9982269,0.00019918694,0.00065986445,0.0002812112,0.00011814583,1.7140869e-7,0.000004362521,0.0000011365925,0.00050905615],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982188,0.000192282,0.00041987273,0.00026332214,0.00037920932,0.00052654033],"domain_scores_gemma":[0.9986774,0.00021082064,0.0003045615,0.00018507897,0.00011306532,0.000509087],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041402472,0.00013147107,0.00031072643,0.00013197637,0.00020143265,0.000047436915,0.00077505974,0.00007933706,0.01750806],"category_scores_gemma":[0.00049964053,0.000078131576,0.0002217971,0.00057089754,0.0013686775,0.00020542825,0.000020481073,0.00030245242,0.000028104118],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000060573198,0.000007638153,0.99237967,0.0000057653237,0.000024745741,0.00009183089,0.00026083807,0.0024757113,0.0014751456,0.000029253624,0.00022504877,0.0030182805],"study_design_scores_gemma":[0.00011474615,0.00013466176,0.98779094,0.000091126916,0.00004672484,0.00006161765,0.00017865845,0.0006876904,0.0014461469,0.0012962251,0.008033496,0.000117979325],"about_ca_topic_score_codex":0.09131166,"about_ca_topic_score_gemma":0.8324023,"teacher_disagreement_score":0.74109066,"about_ca_system_score_codex":0.000015213703,"about_ca_system_score_gemma":0.0030306603,"threshold_uncertainty_score":0.9833901},"labels":[],"label_agreement":null},{"id":"W3134829653","doi":"10.1139/cjes-2019-0134","title":"Laser ablation ICP–MS trace element composition of native gold from the Abitibi greenstone belt, Timmins, Ontario","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor; University of British Columbia, Okanagan Campus","funders":"","keywords":"Trace element; Geology; Greenstone belt; Geochemistry; Mineralogy; Rare-earth element; Analytical Chemistry (journal); Chemistry; Archean; Rare earth; Environmental chemistry","score_opus":0.019040360388961626,"score_gpt":0.21349777944613435,"score_spread":0.19445741905717273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3134829653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9796415,0.00042203953,0.0055442606,0.007562066,0.0003678632,0.00005380022,0.00001238298,0.0000030815186,0.006393002],"genre_scores_gemma":[0.99334943,0.0000048303223,0.0055402764,0.00029657607,0.000058567337,3.9148816e-7,0.000004749001,7.005534e-7,0.0007444991],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989617,0.000079631005,0.00028256475,0.00016307364,0.00030868984,0.00020436998],"domain_scores_gemma":[0.99889636,0.00013027547,0.00027715502,0.0001487573,0.0003729112,0.00017451803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006399906,0.000074442614,0.00012999143,0.000060372,0.00025019218,0.00012020182,0.0005536704,0.00003267494,0.00018811454],"category_scores_gemma":[0.000074787466,0.00005499691,0.00006145014,0.00038470677,0.00022751473,0.0003687479,0.000029394656,0.00016497241,0.0000038727603],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021069342,0.00020956752,0.8099981,0.000038594055,0.00027836012,0.0012022916,0.042209227,0.04443993,0.034043033,0.023172306,0.010603795,0.033783756],"study_design_scores_gemma":[0.00041260527,0.00021626575,0.9460837,0.0002211247,0.000022624581,0.00017377884,0.0010253525,0.0053176237,0.024852714,0.004157157,0.017309232,0.00020782526],"about_ca_topic_score_codex":0.08242525,"about_ca_topic_score_gemma":0.8118559,"teacher_disagreement_score":0.7294307,"about_ca_system_score_codex":0.000022079463,"about_ca_system_score_gemma":0.0017584839,"threshold_uncertainty_score":0.92368495},"labels":[],"label_agreement":null},{"id":"W3135777304","doi":"10.1139/cjes-2020-0132","title":"Late Neoproterozoic – early Paleozoic basin evolution in the Coal Creek inlier of Yukon, Canada: implications for the tectonic evolution of northwestern Laurentia","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon University; Geological Survey of Canada","funders":"University of Toronto; Dartmouth College; Northwestern University; National Science Foundation","keywords":"Laurentia; Rodinia; Geology; Paleozoic; Paleontology; Supercontinent; Precambrian; Baltica; Ordovician; Rift; Sedimentary depositional environment; Conodont; Craton; Structural basin; Biostratigraphy; Tectonics","score_opus":0.01520407434900185,"score_gpt":0.1968668457525749,"score_spread":0.18166277140357306,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3135777304","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9925213,0.003176285,0.00028591993,0.0034536878,0.00011973077,0.000106425374,0.00018577678,7.384852e-7,0.00015015906],"genre_scores_gemma":[0.99959254,0.000018639901,0.00018304783,0.00011620679,0.000046141715,8.266837e-7,0.000012996364,7.631958e-7,0.000028812938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99880445,0.00010610007,0.00039606245,0.00015359635,0.0002624623,0.000277329],"domain_scores_gemma":[0.9987957,0.00034244792,0.00026884646,0.00019623555,0.00025409443,0.00014270983],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008589793,0.00007219304,0.00018129298,0.00009983924,0.00026625438,0.000052500145,0.000721328,0.00003623981,0.0003950122],"category_scores_gemma":[0.0002154867,0.000041258292,0.00008596151,0.0008806493,0.00040758366,0.00015987325,0.0000091536485,0.00013960978,0.0000011602409],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004055062,0.000005463495,0.99440926,0.0000055548167,0.000014559344,0.0000036476476,0.000075034826,0.004463085,0.000045699027,0.000065378736,0.000052302355,0.0008559315],"study_design_scores_gemma":[0.00010468504,0.00010706326,0.9935696,0.000021362539,0.000040048548,0.00002532378,0.00040800936,0.0018072531,0.00003615771,0.0033590794,0.00046916853,0.000052220235],"about_ca_topic_score_codex":0.89955765,"about_ca_topic_score_gemma":0.99958843,"teacher_disagreement_score":0.100030795,"about_ca_system_score_codex":0.000005983535,"about_ca_system_score_gemma":0.002800066,"threshold_uncertainty_score":0.49671972},"labels":[],"label_agreement":null},{"id":"W3137245372","doi":"10.1139/cjes-2020-0129","title":"Geological correlation between northern Cyprus and southern Anatolia","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Nappe; Transtension; Flysch; Subduction; Paleontology; Cenozoic; Andesites; Seismology; Cretaceous; Structural basin; Tectonics; Andesite; Volcanic rock; Volcano; Rift","score_opus":0.02745108023917584,"score_gpt":0.21314802915670758,"score_spread":0.18569694891753175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3137245372","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9871807,0.005531691,0.000032163443,0.0007304133,0.00025733808,0.000025538742,0.00002986076,0.0000036734525,0.006208637],"genre_scores_gemma":[0.9990998,0.00006133649,0.000393331,0.00013748945,0.00013865923,3.8886917e-8,0.0000031760994,0.0000011259027,0.00016507102],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990609,0.00006759411,0.00022108867,0.00014538545,0.0002113417,0.0002936701],"domain_scores_gemma":[0.99913365,0.00016589672,0.00012028059,0.000058114754,0.00012788702,0.0003941772],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047555447,0.000082236686,0.00017661806,0.00013044132,0.00045315374,0.0001212365,0.00012486722,0.00004965826,0.0013219604],"category_scores_gemma":[0.00021420963,0.00005956117,0.00004830167,0.00033485141,0.00046675824,0.0001847794,0.0000052663813,0.00015519837,0.0000682005],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001140446,8.133043e-7,0.98435503,0.0000014758378,0.000011712711,0.0001481178,0.0003198189,0.0004495766,8.6261036e-7,0.000045694807,0.000017811559,0.01464793],"study_design_scores_gemma":[0.00011408352,0.0001354648,0.99369186,0.000018070103,0.000014518531,0.00023905157,0.000881776,0.00026578645,0.000014929209,0.0011422853,0.0033989153,0.00008323983],"about_ca_topic_score_codex":0.010634405,"about_ca_topic_score_gemma":0.65367275,"teacher_disagreement_score":0.64303833,"about_ca_system_score_codex":9.3785286e-7,"about_ca_system_score_gemma":0.0008457884,"threshold_uncertainty_score":0.999591},"labels":[],"label_agreement":null},{"id":"W3137656886","doi":"10.1139/cjes-2020-0140","title":"Structure from motion used to revive archived aerial photographs for geomorphological analysis: an example from Mount Meager volcano, British Columbia, Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"3D Surveying and Cultural Heritage","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geoscience BC; University of Northern British Columbia; Simon Fraser University","funders":"Agence Nationale de la Recherche","keywords":"Geology; Photogrammetry; Structure from motion; Landslide; Volcano; Aerial photography; Glacier; Mount; Landform; Digital elevation model; Remote sensing; Archaeology; Seismology; Geomorphology; Motion (physics); Artificial intelligence; Geography; Computer science","score_opus":0.04055374263935415,"score_gpt":0.21043498985406284,"score_spread":0.16988124721470868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3137656886","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99343306,0.00050629704,0.0001917849,0.00009682316,0.0008768822,0.00012747552,0.004702033,0.0000047234375,0.00006094108],"genre_scores_gemma":[0.9949708,0.000007565863,0.0034175876,0.00051452854,0.00029444485,6.338303e-7,0.00070474786,0.0000026375244,0.00008704786],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980663,0.0002401986,0.0003885767,0.00040974325,0.0004253906,0.0004698121],"domain_scores_gemma":[0.9981025,0.00020526716,0.00018511238,0.00015046546,0.00025136556,0.0011053211],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00045480658,0.00011850445,0.0003994904,0.00009549932,0.0006594046,0.0010053935,0.0004420079,0.000068928304,0.007704055],"category_scores_gemma":[0.00017500574,0.00012342192,0.00014644559,0.0007037128,0.00018834177,0.00030261977,0.000005530667,0.00016746878,0.0000021092894],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018281255,0.00000518493,0.9889702,0.000001949936,0.0001259833,0.00035385042,0.0008450975,0.0039393585,0.00074888003,0.0000010409423,0.0009387461,0.004051395],"study_design_scores_gemma":[0.0002954623,0.00017638548,0.99218184,0.00002996112,0.000101602396,0.00003323812,0.0019225015,0.0006358246,0.0001298161,0.00036127667,0.0039321063,0.0001999723],"about_ca_topic_score_codex":0.99897057,"about_ca_topic_score_gemma":0.9999964,"teacher_disagreement_score":0.007701946,"about_ca_system_score_codex":0.00001049751,"about_ca_system_score_gemma":0.00230763,"threshold_uncertainty_score":0.99320304},"labels":[],"label_agreement":null},{"id":"W3139198649","doi":"10.1139/cjes-2020-0157","title":"Seismic <i>b</i> value within the Montney play of northeastern British Columbia, Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Stantec (Canada); Geoscience BC","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Canadian Association of Petroleum Producers; BC Oil and Gas Research and Innovation Society","keywords":"Geology; Induced seismicity; Seismology; Magnitude (astronomy)","score_opus":0.01163446508151713,"score_gpt":0.17667000219846374,"score_spread":0.1650355371169466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3139198649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.983642,0.00599151,0.0000055474193,0.00082431507,0.000989103,0.00004978514,0.00011084641,0.0000017549991,0.008385141],"genre_scores_gemma":[0.9978691,0.000049902636,0.00016021798,0.0008355157,0.000098538796,1.1836751e-7,0.0000021903313,0.0000019747638,0.0009824916],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99848527,0.000106850326,0.00039965523,0.00015679024,0.0004885103,0.00036290556],"domain_scores_gemma":[0.99879885,0.00019531065,0.0002753926,0.00012618986,0.0002222959,0.00038199298],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00070361374,0.00007880952,0.00023250046,0.00003876125,0.0010638686,0.000546517,0.00045819877,0.000030426847,0.0008748772],"category_scores_gemma":[0.00021912181,0.00007277791,0.00007833013,0.00051951257,0.00054792356,0.00018847722,0.0000060898337,0.00019376235,0.0000048240618],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000011123767,0.0000019899696,0.9841225,0.0000050541103,0.000027043194,0.00029395506,0.00021758435,0.009300298,0.0000019474726,0.000008183645,0.001163387,0.004856918],"study_design_scores_gemma":[0.00014962048,0.000119483615,0.9797333,0.000086348686,0.00001861808,0.0008606114,0.0018517562,0.0010265288,0.000062448256,0.00022051464,0.015762037,0.00010877118],"about_ca_topic_score_codex":0.99685633,"about_ca_topic_score_gemma":0.99999374,"teacher_disagreement_score":0.014598649,"about_ca_system_score_codex":0.0000028731333,"about_ca_system_score_gemma":0.01045047,"threshold_uncertainty_score":0.9951593},"labels":[],"label_agreement":null},{"id":"W3142604694","doi":"10.1139/cjes-2020-0171","title":"Metatarsals of a large caenagnathid cf. <i>Anzu wyliei</i> (Theropoda: Oviraptorosauria) from the Hell Creek Formation in South Dakota, USA<sup>1</sup>","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Holotype; Theropoda; Geology; Paleontology; Archaeology; Cretaceous; Geography; Zoology; Biology; Genus","score_opus":0.023306529126636395,"score_gpt":0.2178985361526237,"score_spread":0.1945920070259873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3142604694","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.985679,0.00973207,0.00008654055,0.0009945055,0.00038372396,0.00007229563,0.0004950434,0.0000025156617,0.0025543266],"genre_scores_gemma":[0.9979536,0.00011216748,0.0007893156,0.0008368995,0.00013213417,3.0686726e-7,0.00003845806,0.0000015958144,0.00013554539],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99806046,0.00041016628,0.00052651385,0.00020835122,0.00028834573,0.0005061796],"domain_scores_gemma":[0.9986932,0.0003964011,0.00031853182,0.00016277276,0.0001396491,0.00028940584],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014541004,0.0001226343,0.0003088957,0.00018334134,0.00042505562,0.000069380185,0.00057536934,0.00011259867,0.0036523696],"category_scores_gemma":[0.00030856772,0.00008721968,0.00011138472,0.0006022979,0.000732979,0.0006346626,0.000009770667,0.000293802,0.00008759647],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016759283,0.000009181314,0.99215645,0.000004374576,0.0000249704,0.00014834706,0.0023851458,0.004063145,0.0000644475,0.00012667336,0.00037912748,0.00062137214],"study_design_scores_gemma":[0.00042183945,0.00019989695,0.97529006,0.000055203906,0.000026066773,0.00021705449,0.0038739452,0.0038451052,0.0001472667,0.001361065,0.01442873,0.000133755],"about_ca_topic_score_codex":0.033704765,"about_ca_topic_score_gemma":0.89333814,"teacher_disagreement_score":0.8596334,"about_ca_system_score_codex":0.0000038140176,"about_ca_system_score_gemma":0.0013714394,"threshold_uncertainty_score":0.9972584},"labels":[],"label_agreement":null},{"id":"W3146086115","doi":"10.1139/cjes-2020-0136","title":"Regional stagnation of the western Keewatin ice sheet and the significance of meltwater corridors and eskers, northern Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Vancouver Island University; Geological Survey of Canada","funders":"","keywords":"Meltwater; Geology; Deglaciation; Ice sheet; Geomorphology; Bedrock; Cityscape; Erosion; Moraine; Drumlin; Glacier; Ice stream; Glacial period; Physical geography; Cryosphere; Oceanography; Geography; Sea ice","score_opus":0.01841354501474504,"score_gpt":0.1857709810782439,"score_spread":0.16735743606349887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3146086115","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909961,0.0026826884,0.0000067192436,0.005770431,0.0002345665,0.000055298322,0.00004201579,3.2713697e-7,0.00021180685],"genre_scores_gemma":[0.9991293,0.00010596161,0.00013518082,0.0004473655,0.000028826202,1.3449575e-7,9.694934e-7,7.5552794e-7,0.00015152805],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992371,0.00006881032,0.00021987713,0.00008064509,0.00026610048,0.00012744639],"domain_scores_gemma":[0.99918485,0.00023606257,0.00021914612,0.000064533226,0.00018698887,0.00010844919],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041555674,0.000051881005,0.00012679056,0.000019249901,0.00031087428,0.000037980535,0.00017523863,0.0000131756815,0.00009880651],"category_scores_gemma":[0.00013170326,0.00002711392,0.000026643771,0.00027589998,0.0007822646,0.00010326128,0.0000068112186,0.000066169516,1.1716039e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005448726,8.0507755e-7,0.99490535,0.000005538815,0.000010481113,0.0000037810344,0.0007684667,0.0026759554,0.000005999942,0.00004630948,0.00020616778,0.0013656915],"study_design_scores_gemma":[0.0001769405,0.000029639621,0.99060446,0.00002670179,0.000011846059,0.000026587619,0.002713041,0.0006477011,0.000054617285,0.000099481,0.005571698,0.000037262515],"about_ca_topic_score_codex":0.76632315,"about_ca_topic_score_gemma":0.99825656,"teacher_disagreement_score":0.23193339,"about_ca_system_score_codex":0.0000020335137,"about_ca_system_score_gemma":0.001955063,"threshold_uncertainty_score":0.3468198},"labels":[],"label_agreement":null},{"id":"W3147741958","doi":"10.1139/cjes-2020-0073","title":"Magmatic activity and hydrocarbon potential revealed by Paleozoic collapse structures in the Hangjinqi area, northern Ordos Basin, China","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science and Technology Major Project; National Natural Science Foundation of China","keywords":"Geology; Permian; Paleozoic; Ordovician; Structural basin; Geochemistry; Sedimentary rock; Basement; Volcano; Carboniferous; Sedimentary depositional environment; Petrology; Paleontology; Coal measures","score_opus":0.008543338127914706,"score_gpt":0.20060689655192562,"score_spread":0.1920635584240109,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3147741958","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99565333,0.0016610681,0.00020297122,0.0013231875,0.00015478837,0.000051029954,0.000007650025,0.0000041676944,0.00094181637],"genre_scores_gemma":[0.9995678,0.0001352712,0.00008422145,0.00010333164,0.00004773303,0.0000010110416,0.0000012148603,0.000005296698,0.00005411226],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9990522,0.000114869974,0.0002148748,0.00011019356,0.00027072048,0.00023713942],"domain_scores_gemma":[0.9995021,0.000033517073,0.00007064958,0.000105204854,0.000047287474,0.000241195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003647316,0.0001025895,0.0001923534,0.00023397917,0.00018520367,0.00022215661,0.00022435073,0.00004405433,0.00007486441],"category_scores_gemma":[0.00009403835,0.00007064928,0.000059825274,0.00074325927,0.00015840652,0.00022898502,0.0000060750813,0.00019805964,0.0000011139523],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002960002,0.00007551616,0.47125652,0.00020279088,0.00037100384,0.0028666276,0.014223763,0.4714955,0.025181878,0.00012510017,0.0031741108,0.010997589],"study_design_scores_gemma":[0.0011333267,0.00022131142,0.7671434,0.00019989123,0.00013575776,0.00084858807,0.00577453,0.21719281,0.0025801233,0.0017270527,0.002426447,0.000616736],"about_ca_topic_score_codex":0.0012642394,"about_ca_topic_score_gemma":0.26073238,"teacher_disagreement_score":0.2958869,"about_ca_system_score_codex":0.000011114053,"about_ca_system_score_gemma":0.00040191083,"threshold_uncertainty_score":0.7527573},"labels":[],"label_agreement":null},{"id":"W3149221633","doi":"10.1139/cjes-2020-0165","title":"Paleolatitude and tectonic rotations of the Early Carboniferous Fountain Lake Group, Cobequid Highlands, Nova Scotia, Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; McMaster University; Western University","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta; University of Windsor","keywords":"Geology; Paleomagnetism; Clockwise; Sinistral and dextral; Apparent polar wander; Carboniferous; Terrane; Paleontology; Gondwana; Paleozoic; Fold (higher-order function); Seismology; Fault (geology); Tectonics; Structural basin","score_opus":0.01096976057806286,"score_gpt":0.17780935130204947,"score_spread":0.1668395907239866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3149221633","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939422,0.001975709,0.0000064131814,0.0017742604,0.00026431636,0.000033924425,0.000061789266,0.0000010732201,0.0019403019],"genre_scores_gemma":[0.9992808,0.000015252011,0.00029545833,0.00029551884,0.00004645086,5.142569e-8,0.000003846148,7.578354e-7,0.0000618365],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99888265,0.00007177894,0.00028229054,0.00014087431,0.00033350047,0.00028890718],"domain_scores_gemma":[0.99907064,0.00014132891,0.00016177689,0.00009157148,0.00015839466,0.0003762608],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031285465,0.000084473504,0.00018884243,0.00007457519,0.00025145896,0.000078979385,0.00031002396,0.000032450596,0.0025292505],"category_scores_gemma":[0.00021110696,0.00005024514,0.00006869792,0.00071166176,0.00047305197,0.000119164135,0.0000097157135,0.00015407338,0.000002593986],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000016554474,0.000002172493,0.99820393,0.0000037367572,0.000015642205,0.00004558196,0.00004668137,0.0010737606,0.00006433512,0.00010706813,0.00003401988,0.0004013989],"study_design_scores_gemma":[0.00010383251,0.000090747,0.9969984,0.000025704205,0.00002531795,0.00009439158,0.00017048679,0.00028038185,0.00018393683,0.0011421846,0.0008108651,0.00007373752],"about_ca_topic_score_codex":0.90943843,"about_ca_topic_score_gemma":0.9999219,"teacher_disagreement_score":0.09048348,"about_ca_system_score_codex":0.0000020075079,"about_ca_system_score_gemma":0.0021441097,"threshold_uncertainty_score":0.99838257},"labels":[],"label_agreement":null},{"id":"W3151776882","doi":"10.1139/cjes-2020-0182","title":"Cumulate gabbros in the South Andaman Island ophiolite suite (India): their bearing on the tectonic setting","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Ophiolite; Geology; Geochemistry; Mafic; Hornblende; Gabbro; Basalt; Olivine; Island arc; Ultramafic rock; Amphibole; Petrology; Subduction; Paleontology; Tectonics; Quartz; Biotite","score_opus":0.021998950651798695,"score_gpt":0.19946583906836973,"score_spread":0.17746688841657104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3151776882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9868374,0.0008899071,0.0000023434297,0.005465599,0.00010873243,0.00004833664,0.000026481937,0.0000018768442,0.0066193608],"genre_scores_gemma":[0.9979808,0.000020365404,0.00004854135,0.0017767767,0.000111555484,2.0557374e-7,0.0000034217585,9.674276e-7,0.00005741676],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985518,0.00021111671,0.00027329728,0.00018404223,0.000305742,0.00047400602],"domain_scores_gemma":[0.99892116,0.00050069235,0.00013603829,0.00013385531,0.00006601561,0.00024221727],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001697955,0.0001111357,0.0001710579,0.00014666164,0.0005970275,0.0003252026,0.0006076452,0.000039461524,0.002648644],"category_scores_gemma":[0.00037769985,0.00004807931,0.00012323647,0.0009397215,0.00036509646,0.00013670411,0.0000090446065,0.00038194205,0.00003534266],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003936936,0.0000037157279,0.99021024,0.0000024837964,0.0000114887,0.00017326092,0.0014530194,0.0067365803,0.00006557388,0.00013650986,0.000058458318,0.0011447332],"study_design_scores_gemma":[0.00010545017,0.000118902804,0.98710346,0.000050522038,0.000010411935,0.000116745694,0.0025710086,0.0023418164,0.00028766348,0.005744561,0.0014459644,0.0001034688],"about_ca_topic_score_codex":0.0050593703,"about_ca_topic_score_gemma":0.3324435,"teacher_disagreement_score":0.32738414,"about_ca_system_score_codex":0.0000015701032,"about_ca_system_score_gemma":0.0004350426,"threshold_uncertainty_score":0.99826306},"labels":[],"label_agreement":null},{"id":"W3153933235","doi":"10.1139/cjes-2020-0197","title":"<sup>40</sup>Ar/<sup>39</sup>Ar dating of Paleoproterozoic shear zones in the Ellesmere–Devon crystalline terrane, Nunavut, Canadian Arctic","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Mylonite; Terrane; Gneiss; Metamorphism; Granulite; Shear zone; Geochemistry; Protolith; Zircon; Biotite; Orogeny; Metamorphic rock; Geomorphology; Paleontology; Facies; Quartz; Tectonics","score_opus":0.02124194035484117,"score_gpt":0.20452587122955848,"score_spread":0.1832839308747173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3153933235","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9880021,0.002435531,0.000017557217,0.0055518285,0.000084442574,0.00011938324,0.000111842026,0.0000034430652,0.0036738385],"genre_scores_gemma":[0.99707884,0.00010289359,0.0013630086,0.0010842066,0.00018656274,8.316714e-7,0.000040851297,0.000003373283,0.00013944758],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9968078,0.00035130058,0.00080889236,0.00040529284,0.00066490617,0.00096178637],"domain_scores_gemma":[0.99766964,0.0003770737,0.00028500252,0.00026652115,0.000293829,0.0011079067],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018053639,0.00024782735,0.0005019222,0.0005439616,0.00057111477,0.00024282349,0.0010591439,0.00013044896,0.01442004],"category_scores_gemma":[0.00084972003,0.00015978144,0.00022610968,0.0019173376,0.00081158796,0.00039879204,0.000015766751,0.000585597,0.000050190363],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010484522,0.000017538534,0.9226128,0.000027461334,0.00003311605,0.00051988865,0.0010762485,0.071795024,0.00003312818,0.00007878521,0.00009687593,0.0036986587],"study_design_scores_gemma":[0.00040774504,0.00048054315,0.9402552,0.00027451114,0.00007444403,0.0005468929,0.0074819964,0.037541877,0.00012834699,0.005152328,0.007233561,0.00042253415],"about_ca_topic_score_codex":0.58521473,"about_ca_topic_score_gemma":0.98023033,"teacher_disagreement_score":0.3950156,"about_ca_system_score_codex":0.0000097493685,"about_ca_system_score_gemma":0.0026703891,"threshold_uncertainty_score":0.9864809},"labels":[],"label_agreement":null},{"id":"W3154203200","doi":"10.1139/cjes-2020-0164","title":"Dung analysis of the East Milford mastodons: dietary and environmental reconstructions from central Nova Scotia at ∼75 ka years BP","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University; Brock University; University of Alberta; University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada; Brock University","keywords":"Macrofossil; Ecology; Peat; Boreal; Geology; Biology; Pollen","score_opus":0.024904666739578085,"score_gpt":0.20763300977505925,"score_spread":0.18272834303548116,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3154203200","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946195,0.0031204594,0.000001973853,0.00070708315,0.00053570117,0.000030624353,0.00026632095,7.844108e-7,0.0007175784],"genre_scores_gemma":[0.99920297,0.00009844208,0.00041960497,0.00011989395,0.00003101164,3.0943028e-8,0.000020570516,8.3852353e-7,0.00010665993],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989072,0.0001588803,0.00023870026,0.00016296841,0.00019683893,0.00033537898],"domain_scores_gemma":[0.9992392,0.00013900679,0.00013569,0.00011386439,0.000024486246,0.00034773644],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031981416,0.00007131226,0.00020624089,0.0002549126,0.00035438192,0.00003740917,0.00026967586,0.00006038931,0.0071305907],"category_scores_gemma":[0.00006286556,0.000052650095,0.000119980665,0.0006221752,0.0016903633,0.00016333429,0.000015663672,0.00019282362,0.00001595525],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005714965,0.000002581502,0.99759495,0.0000012734802,0.00012373789,0.00006823974,0.00029612228,0.001266695,0.000034934208,0.000006704336,0.00003202375,0.00056703354],"study_design_scores_gemma":[0.00009269231,0.00004185865,0.9970193,0.00001428572,0.00011920597,0.0003224817,0.0011630123,0.00068386225,0.0000700185,0.00009025111,0.00032701643,0.000056004203],"about_ca_topic_score_codex":0.010373931,"about_ca_topic_score_gemma":0.86537546,"teacher_disagreement_score":0.8550015,"about_ca_system_score_codex":0.0000011806237,"about_ca_system_score_gemma":0.0005430219,"threshold_uncertainty_score":0.99621606},"labels":[],"label_agreement":null},{"id":"W3156194741","doi":"10.1139/cjes-2020-0207","title":"Quantifying the diagenetic impact in the late Ediacaran and early Palaeozoic of the Avalon Peninsula using illite “crystallinity”","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Klaus Tschira Stiftung","keywords":"Geology; Metamorphism; Greenschist; Diagenesis; Metamorphic rock; Geochemistry; Ordovician; Conodont; Imbrication; Paleontology; Illite; Orogeny; Facies; Horst; Lithology; Massif; Geomorphology; Structural basin; Tectonics; Biostratigraphy","score_opus":0.04624816023237661,"score_gpt":0.24413284402531038,"score_spread":0.19788468379293378,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3156194741","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99288714,0.0051221675,0.0000030799097,0.0014938569,0.00011660639,0.000046653367,0.00001342776,5.5149326e-7,0.000316524],"genre_scores_gemma":[0.99951315,0.00011149049,0.000093303905,0.00021691201,0.000049889328,6.671528e-8,5.714318e-7,7.3370995e-7,0.000013892529],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99867773,0.00029841694,0.00029660107,0.00011156788,0.00031755536,0.00029815358],"domain_scores_gemma":[0.9990545,0.00037259088,0.0001812023,0.00011891487,0.00008630123,0.00018648423],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013364361,0.00008618946,0.00017850347,0.0000888981,0.00039944603,0.00016769792,0.00049935834,0.000034089142,0.000541811],"category_scores_gemma":[0.00034189853,0.000033762593,0.00014434276,0.0009905674,0.00073690386,0.00013008979,0.000011693054,0.00023864981,0.0000018555431],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000020729074,0.0000022323984,0.9923939,0.000002868728,0.000008596767,0.000026693679,0.00068781147,0.0059073567,0.0003156878,0.000013472988,0.000002297853,0.0006370217],"study_design_scores_gemma":[0.00006840301,0.00006814884,0.99370384,0.000035006604,0.00002577691,0.00008505948,0.00069818314,0.0032671748,0.00013639126,0.0017203621,0.00013776876,0.000053894302],"about_ca_topic_score_codex":0.041608512,"about_ca_topic_score_gemma":0.36191872,"teacher_disagreement_score":0.3203102,"about_ca_system_score_codex":0.0000011286745,"about_ca_system_score_gemma":0.000506038,"threshold_uncertainty_score":0.9647735},"labels":[],"label_agreement":null},{"id":"W3159178851","doi":"10.1139/cjes-2020-0139","title":"Seabed disturbance and sediment mobility due to tidal current and waves on the continental shelves of Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Geological Survey of Canada","funders":"","keywords":"Continental shelf; Seabed; Geology; Oceanography; Continental margin; Sediment transport; Sediment; Current (fluid); Geomorphology; Seismology","score_opus":0.01606956398127965,"score_gpt":0.202084075785634,"score_spread":0.18601451180435435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3159178851","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99156874,0.0028651746,0.000003693058,0.0043115066,0.00022820082,0.00004455608,0.000064025066,5.2978413e-7,0.00091359497],"genre_scores_gemma":[0.9994593,0.000037449987,0.00011654113,0.00031880575,0.000024214512,1.3386934e-7,0.0000011940647,3.2721897e-7,0.000041986492],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99934214,0.000041947955,0.00016659328,0.00009020236,0.00019029736,0.00016880843],"domain_scores_gemma":[0.99930143,0.00016370299,0.00007249512,0.000045097768,0.00008863571,0.00032866167],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004155873,0.000055139917,0.000109926965,0.000038475,0.0002857475,0.00007544677,0.0001226553,0.000010849581,0.00042423364],"category_scores_gemma":[0.0002028659,0.000030496967,0.000015138186,0.00019650871,0.0002801739,0.00011191016,0.000005590117,0.00007646251,7.450565e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010250847,0.0000075427765,0.9840728,0.000026270174,0.000008513643,0.000030824576,0.00056349323,0.0010628459,0.000019750043,0.00066324085,0.0007373879,0.012797104],"study_design_scores_gemma":[0.00004865725,0.0001543351,0.98986644,0.000038877686,0.0000032011596,0.00005805549,0.0008189637,0.00028024748,0.00039108976,0.00045449156,0.007837008,0.00004861853],"about_ca_topic_score_codex":0.11604123,"about_ca_topic_score_gemma":0.93693566,"teacher_disagreement_score":0.8208944,"about_ca_system_score_codex":0.0000013302571,"about_ca_system_score_gemma":0.0012068885,"threshold_uncertainty_score":0.88984513},"labels":[],"label_agreement":null},{"id":"W3159998533","doi":"10.1139/cjes-2021-0012","title":"Geology of the Mesoproterozoic Pillar Lake Volcanics and Inspiration Sill, Armstrong, Ontario: evidence of early Midcontinent Rift magmatism in the northwestern Nipigon Embayment","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Geological Survey of Canada; Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Sill; Mafic; Geochemistry; Volcanic rock; Breccia; Zircon; Igneous rock; Rift; Basalt; Baddeleyite; Archean; Greenstone belt; Lithology; Petrology; Volcano; Geomorphology","score_opus":0.020792333325562018,"score_gpt":0.20154568699855785,"score_spread":0.18075335367299583,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3159998533","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995565,0.0022514793,0.000009362117,0.0018059138,0.000106411506,0.00007276557,0.000009659093,4.941115e-7,0.00017893822],"genre_scores_gemma":[0.99940765,0.000044727836,0.00021045687,0.0002702974,0.000020334792,2.887157e-7,0.0000015719451,5.228859e-7,0.000044155982],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987189,0.00016704993,0.00041810426,0.00014083314,0.00032899092,0.0002260762],"domain_scores_gemma":[0.9991544,0.0001407689,0.00030880075,0.00011860398,0.00013635385,0.00014110292],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00079343235,0.00008365826,0.00021304813,0.00009133566,0.0001316541,0.0000519825,0.0004110727,0.000042518965,0.00085005205],"category_scores_gemma":[0.00014835778,0.000042937074,0.00008102208,0.00044479582,0.00051573373,0.00019798528,0.000014294375,0.0001828228,0.000001575794],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000048830702,0.000005897601,0.99650043,0.000007794962,0.000007690937,0.000018387787,0.0007048717,0.0011974479,0.00011531118,0.000050879906,0.0000040913346,0.0013823315],"study_design_scores_gemma":[0.00009772741,0.0003425368,0.9966431,0.00008254844,0.000020118368,0.000048449678,0.000378411,0.00019374715,0.00034418612,0.0014298819,0.00036806756,0.000051219788],"about_ca_topic_score_codex":0.3120676,"about_ca_topic_score_gemma":0.9967043,"teacher_disagreement_score":0.6846367,"about_ca_system_score_codex":0.0000019489737,"about_ca_system_score_gemma":0.00067294895,"threshold_uncertainty_score":0.93074733},"labels":[],"label_agreement":null},{"id":"W3161379075","doi":"10.1139/cjes-2020-0217","title":"Insights into the Connaught sequence of the Timiskaming varve series from Frederick House Lake, northeastern Ontario","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Varve; Unconformity; Geology; Sequence (biology); Numbering; Paleontology; Series (stratigraphy); Structural basin; Algorithm; Sediment","score_opus":0.035322140500102385,"score_gpt":0.22111820449183126,"score_spread":0.18579606399172888,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3161379075","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909023,0.002426407,0.0000053209315,0.00267179,0.0007194491,0.00005156707,0.000018329818,0.0000022397073,0.003202565],"genre_scores_gemma":[0.99852663,0.0000423969,0.00033231743,0.00035632277,0.000057094836,1.7697009e-7,0.0000035593712,0.000001635821,0.000679882],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985829,0.0003121387,0.0002962342,0.00016567837,0.0003172447,0.00032580996],"domain_scores_gemma":[0.99878377,0.00032650333,0.00021161388,0.00020177347,0.00020858191,0.00026773778],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048497284,0.00009929236,0.00019971153,0.00009281081,0.00087598496,0.000109026805,0.0008234402,0.00007116533,0.0021639843],"category_scores_gemma":[0.0002180997,0.00005301582,0.000086405045,0.00047981652,0.002013535,0.00035150952,0.000018385688,0.00038487732,0.000035489895],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000063322163,0.0000021569654,0.9935311,0.0000027146061,0.000020487418,0.00015603012,0.00500208,0.000936778,0.000023966253,0.00009414757,0.000027506216,0.00019669901],"study_design_scores_gemma":[0.00009864668,0.000091516995,0.9847387,0.000048248654,0.000014107984,0.00030784644,0.0017137504,0.00014788436,0.00040372758,0.0022156083,0.010145597,0.00007438049],"about_ca_topic_score_codex":0.19368647,"about_ca_topic_score_gemma":0.9993367,"teacher_disagreement_score":0.80565023,"about_ca_system_score_codex":0.0000010873805,"about_ca_system_score_gemma":0.004724993,"threshold_uncertainty_score":0.9987482},"labels":[],"label_agreement":null},{"id":"W3161395520","doi":"10.1139/cjes-2020-0172","title":"Art, anatomy, and the stars: Russell and Séguin’s dinosauroid<sup>1</sup>","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Timeline; History; Genealogy; Philosophy; Epistemology","score_opus":0.013034183419568662,"score_gpt":0.20568500786392846,"score_spread":0.1926508244443598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3161395520","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96011,0.022405677,0.000010184488,0.0073356004,0.00025856702,0.000040857572,0.000030682997,0.000002351256,0.009806045],"genre_scores_gemma":[0.99753195,0.00062862114,0.00043143047,0.0009946366,0.00009818024,1.05732404e-7,0.000003474175,7.5898487e-7,0.00031082952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989424,0.000213375,0.00021227801,0.00016732277,0.00012934576,0.00033530642],"domain_scores_gemma":[0.9990061,0.00032719265,0.00009748282,0.000075614975,0.000072931194,0.00042067087],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009980287,0.00008765277,0.00018370323,0.00013242573,0.0006086865,0.00010507076,0.00021878403,0.00006147878,0.00097036554],"category_scores_gemma":[0.00022199162,0.000053286905,0.00003999782,0.00025237887,0.0024036448,0.00029010302,0.0000065611293,0.00019351498,0.000024414127],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018582336,0.0000016155376,0.9934241,0.0000030839137,0.00001756195,0.00020408492,0.0004435046,0.0005267364,0.00000297575,0.0017688392,0.00088432676,0.0027045603],"study_design_scores_gemma":[0.00040462642,0.00013988475,0.93398094,0.000015978843,0.000016732676,0.0022070534,0.0010233069,0.0031870368,0.000006345909,0.0033523932,0.055575047,0.000090669215],"about_ca_topic_score_codex":0.0033728385,"about_ca_topic_score_gemma":0.32462898,"teacher_disagreement_score":0.32125616,"about_ca_system_score_codex":8.480587e-7,"about_ca_system_score_gemma":0.0009521592,"threshold_uncertainty_score":0.9999429},"labels":[],"label_agreement":null},{"id":"W3161897031","doi":"10.1139/cjes-2020-0114","title":"The northern Appalachian terrane wreck model","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Nova Scotia Department of Energy","funders":"","keywords":"Terrane; Geology; Devonian; Ordovician; Sinistral and dextral; Fibrous joint; Paleomagnetism; Paleontology; Paleozoic; Clockwise; Fold (higher-order function); Seismology; Tectonics","score_opus":0.021128555669383695,"score_gpt":0.18902494771619197,"score_spread":0.16789639204680828,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3161897031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9693965,0.0030618834,0.00006497803,0.0068304525,0.00024099743,0.000019824849,0.000014237916,0.0000026856405,0.020368444],"genre_scores_gemma":[0.9978016,0.00005963847,0.00081984536,0.0005245801,0.000095050076,6.319465e-8,0.0000027818148,7.1862877e-7,0.0006957461],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99887705,0.000058394242,0.00025180323,0.00013750736,0.00028430115,0.0003909433],"domain_scores_gemma":[0.99890655,0.00012606116,0.00011105386,0.000098217046,0.00017165797,0.0005864514],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005984723,0.000080288526,0.00014016045,0.0000686975,0.000753175,0.00021745509,0.00047242464,0.00003300933,0.0025848758],"category_scores_gemma":[0.00025322923,0.000042100055,0.00012690939,0.00050926773,0.00054154504,0.00014911681,0.0000054435213,0.00016550007,0.00007199837],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000031931772,0.0000028802972,0.95189905,0.0000013712393,0.00001552885,0.00009223095,0.00009574121,0.034982517,0.000045105648,0.00018290557,0.00012910734,0.01255034],"study_design_scores_gemma":[0.00023206612,0.00023892104,0.8372319,0.000031639822,0.000048271497,0.0004306625,0.0010885238,0.07149503,0.00048376527,0.06082592,0.02759237,0.00030095087],"about_ca_topic_score_codex":0.009244119,"about_ca_topic_score_gemma":0.8993024,"teacher_disagreement_score":0.8900583,"about_ca_system_score_codex":8.588929e-7,"about_ca_system_score_gemma":0.0011695271,"threshold_uncertainty_score":0.9983269},"labels":[],"label_agreement":null},{"id":"W3162034988","doi":"10.1139/cjes-2021-0029","title":"A Lower Devonian age for the Corvock Granite and its significance for the structural history of South Mayo and the Laurentian margin of western Ireland","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Devonian; Diachronous; Sinistral and dextral; Batholith; Dalradian; Paleontology; Ordovician; Sill; Orogeny; Overprinting; Geochemistry; Fault (geology); Tectonics; Metamorphism","score_opus":0.02097828997315549,"score_gpt":0.19152484569433298,"score_spread":0.1705465557211775,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3162034988","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97337323,0.02264854,0.00006166655,0.0032795828,0.00026000803,0.00014592825,0.00011868767,6.1693436e-7,0.0001117179],"genre_scores_gemma":[0.9990738,0.00009255346,0.0001435577,0.0002503532,0.00005116021,6.9062315e-7,0.000002025309,8.2399634e-7,0.00038502904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99926144,0.000052134215,0.00022155546,0.00011328306,0.00015781204,0.00019379209],"domain_scores_gemma":[0.9986765,0.00075454055,0.00020560148,0.000068954876,0.00014277622,0.00015162118],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00063415937,0.000072038536,0.00018993764,0.000042304302,0.00027454717,0.00005605911,0.0002877552,0.000026119964,0.0004399133],"category_scores_gemma":[0.00022736385,0.000029178642,0.00009869389,0.00016308742,0.0012506054,0.00008087694,0.0000069592884,0.00009061087,3.2765118e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022525857,0.000005080814,0.9847754,0.00006888234,0.00016669992,0.000026103935,0.0044130855,0.002403771,0.00018875052,0.0007483951,0.00037561322,0.006602953],"study_design_scores_gemma":[0.00091673183,0.00031091453,0.9617974,0.00004864447,0.00020543116,0.00007388513,0.0021648381,0.01237938,0.00013980592,0.0051881233,0.016642531,0.00013228081],"about_ca_topic_score_codex":0.0040770182,"about_ca_topic_score_gemma":0.34269616,"teacher_disagreement_score":0.33861914,"about_ca_system_score_codex":0.0000011493269,"about_ca_system_score_gemma":0.00034916,"threshold_uncertainty_score":0.66929793},"labels":[],"label_agreement":null},{"id":"W3162184801","doi":"10.1139/cjes-2020-0070","title":"Origin and evolution of unconformities in a continental rift basin: a case study from the Lishu Depression in Songliao Basin, China","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Unconformity; Geology; Rift; Paleontology; Structural basin; Tectonics; Sedimentary rock; Fault (geology); Fault block; Sedimentary basin; Thermal subsidence; Geomorphology","score_opus":0.013682684162842977,"score_gpt":0.22489364268528,"score_spread":0.21121095852243701,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3162184801","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975554,0.0017114116,0.000047695994,0.00021318102,0.00013975428,0.000047790225,0.000007971033,0.0000018400366,0.0002749643],"genre_scores_gemma":[0.9998322,0.00003669816,0.000065669934,0.000017277254,0.000031185427,7.406911e-7,5.1200743e-7,0.0000025389356,0.000013149167],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992785,0.000075453936,0.00027829825,0.00007533633,0.00015564307,0.00013675349],"domain_scores_gemma":[0.9996463,0.000053231382,0.000059124577,0.000064945874,0.00004764165,0.00012873422],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047714697,0.00006126815,0.00016499772,0.00025272093,0.00008487172,0.00008014764,0.00010631541,0.000025806627,0.000041467312],"category_scores_gemma":[0.00010497246,0.00004223428,0.000033584292,0.0005792192,0.00011361413,0.00033009905,0.00000791417,0.00013919755,3.1794056e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021884055,0.000009812303,0.9798075,0.000003294278,0.000012405434,0.0008957452,0.005320288,0.013538978,0.00006490698,0.000013070796,0.00002651813,0.0003053094],"study_design_scores_gemma":[0.00075053115,0.000069972455,0.87371165,0.0001662192,0.000021957856,0.00040480524,0.07966139,0.044207394,0.00038061544,0.0001146487,0.0003989042,0.00011189464],"about_ca_topic_score_codex":0.080093995,"about_ca_topic_score_gemma":0.8233708,"teacher_disagreement_score":0.74327683,"about_ca_system_score_codex":0.000016289645,"about_ca_system_score_gemma":0.0004807709,"threshold_uncertainty_score":0.9260317},"labels":[],"label_agreement":null},{"id":"W3162571131","doi":"10.1139/cjes-2020-0151","title":"First mammal from the Willow Creek Formation: a new early Paleocene ptilodontid (Mammalia, Multituberculata) from near Calgary, Alberta, Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"American Museum of Natural History","keywords":"Paleogene; Paleontology; Fauna; Geology; Mammal; Cretaceous; Dominance (genetics); Willow; Ecology; Biology","score_opus":0.020088714221263133,"score_gpt":0.19233623783369835,"score_spread":0.17224752361243523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3162571131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.973427,0.009657584,0.00007832558,0.010450376,0.0017039065,0.00007477708,0.00020346919,0.0000039667566,0.004400605],"genre_scores_gemma":[0.99461406,0.00011176413,0.0021463472,0.0018875116,0.00041086742,2.2626668e-7,0.000034549736,0.0000025624206,0.00079208566],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981953,0.00013442604,0.00042831997,0.00024341508,0.00047687627,0.00052166055],"domain_scores_gemma":[0.9979524,0.0006259525,0.00022938933,0.00019371553,0.00017100414,0.000827511],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029603124,0.00016281212,0.0002757833,0.00005094944,0.0014958763,0.00042971532,0.0005872701,0.000071877774,0.004462515],"category_scores_gemma":[0.00034818563,0.000120903795,0.00010768372,0.00041274878,0.0005504915,0.00059532595,0.0000106240095,0.00027092724,0.00005902268],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000076384995,0.000001764604,0.98743576,0.0000015081603,0.000045004395,0.00025091862,0.0010354962,0.0011942287,7.707159e-7,0.000014926416,0.008307547,0.0017044365],"study_design_scores_gemma":[0.0002804252,0.000059107348,0.881667,0.00004991988,0.000031435953,0.00010599625,0.0007901153,0.0024247826,0.000009153683,0.00015716886,0.114278905,0.00014599379],"about_ca_topic_score_codex":0.99790394,"about_ca_topic_score_gemma":0.9999979,"teacher_disagreement_score":0.10597136,"about_ca_system_score_codex":0.000008020866,"about_ca_system_score_gemma":0.0063626897,"threshold_uncertainty_score":0.999804},"labels":[],"label_agreement":null},{"id":"W3162926388","doi":"10.1139/e01-027","title":"Archean rocks in the southern Rottenstone Domain: significance for the evolution of the Trans-Hudson Orogen","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Archean; Batholith; Zircon; Craton; Geochemistry; Gneiss; Crust; Terrane; Closure temperature; Geochronology; Metamorphic rock; Tectonics; Paleontology","score_opus":0.020502765077555093,"score_gpt":0.19797263640748552,"score_spread":0.17746987132993042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3162926388","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9841409,0.0014231969,0.0005004427,0.012637688,0.00010475294,0.00015166478,0.000031837637,9.565242e-7,0.0010085778],"genre_scores_gemma":[0.9993156,0.000019144623,0.00015855595,0.00035346876,0.00008633972,7.84253e-7,7.0811626e-7,6.8596677e-7,0.0000646753],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885696,0.00012393505,0.00027172948,0.00011414921,0.00031184347,0.0003213721],"domain_scores_gemma":[0.99915534,0.00035228205,0.00015992958,0.00011251659,0.00007932331,0.00014057865],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015339697,0.00007575601,0.00013830826,0.000078251294,0.00044842885,0.000046201116,0.00089392473,0.000033978853,0.0006757702],"category_scores_gemma":[0.00014876384,0.000029084187,0.00015900756,0.0008049915,0.00077819393,0.00008483462,0.0000028041268,0.00016884155,0.00000455372],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013955445,0.00000560515,0.9820113,0.000002583132,0.000009960495,0.0000044940866,0.001107893,0.013994326,0.00011065771,0.00011514769,0.000047205605,0.0025768292],"study_design_scores_gemma":[0.00018187189,0.00019174903,0.9636174,0.000024065686,0.000030734038,0.00006408375,0.009226257,0.002692911,0.00010549098,0.019054342,0.0047272793,0.00008380179],"about_ca_topic_score_codex":0.07370356,"about_ca_topic_score_gemma":0.7792224,"teacher_disagreement_score":0.7055189,"about_ca_system_score_codex":0.0000027286521,"about_ca_system_score_gemma":0.00045575085,"threshold_uncertainty_score":0.9324647},"labels":[],"label_agreement":null},{"id":"W3163083439","doi":"10.1139/cjes-2021-0031","title":"Glass fission-track ages, composition, and origin of tephra beds in the Upper Cretaceous Kanguk Formation, Banks Island, Arctic Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Tephra; Rhyolite; Geochemistry; Continental margin; Volcanic glass; Paleontology; Sedimentary rock; Caldera; Zircon; Cretaceous; Fission track dating; Volcanic rock; Volcano","score_opus":0.011297703228330997,"score_gpt":0.19337121798037257,"score_spread":0.1820735147520416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3163083439","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99025774,0.0027324113,0.0000073087117,0.005163901,0.00009353396,0.000030698666,0.000042788375,6.436803e-7,0.001670973],"genre_scores_gemma":[0.9987062,0.00006794193,0.0002620222,0.00086455606,0.000037872876,1.0585974e-7,0.000014651122,4.8215895e-7,0.000046159024],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998917,0.00010320195,0.00030914947,0.000106663065,0.00031877405,0.00024523796],"domain_scores_gemma":[0.9991477,0.00022019408,0.00013358625,0.00006830479,0.00015784324,0.00027234372],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048692807,0.00007523389,0.00017205022,0.00010860949,0.0002227362,0.00008868034,0.0002531973,0.000031878037,0.002078794],"category_scores_gemma":[0.0001591711,0.000042640262,0.000046481593,0.00060837535,0.00026734962,0.00020763736,0.000004190225,0.00016545194,0.0000033742533],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003783953,0.000004901733,0.995708,0.000012165581,0.00000824276,0.00018103416,0.0002979341,0.0017704312,0.000044776723,0.000056475306,0.00052553654,0.0013867111],"study_design_scores_gemma":[0.00013010051,0.00007943422,0.98408914,0.000051931795,0.000018646535,0.00043217937,0.0007706259,0.0013665804,0.0002246234,0.0018522412,0.010898034,0.00008645862],"about_ca_topic_score_codex":0.57317764,"about_ca_topic_score_gemma":0.99525326,"teacher_disagreement_score":0.42207563,"about_ca_system_score_codex":0.000002838919,"about_ca_system_score_gemma":0.0009820814,"threshold_uncertainty_score":0.9988334},"labels":[],"label_agreement":null},{"id":"W3163514308","doi":"10.1139/cjes-2020-0167","title":"Lower Cambrian (Series 2) small shelly fossils from along Nares Strait (Nunavut and Greenland; Laurentia)","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Laurentia; Paleontology; Promontory; Fauna; Craton; Structural basin; Series (stratigraphy); Stage (stratigraphy); Ecological succession; Paleozoic; Tectonics; Archaeology; Geography; Ecology","score_opus":0.028932610873055698,"score_gpt":0.19451562568368996,"score_spread":0.16558301481063425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3163514308","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98645407,0.007838288,0.000038840262,0.0022058836,0.0007530044,0.000034452023,0.0000716825,0.0000036069293,0.002600191],"genre_scores_gemma":[0.99744385,0.00024281941,0.0016104052,0.00026693006,0.00021600159,1.121812e-7,0.000010561753,0.0000011641868,0.00020815407],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99892485,0.000064665,0.0002546446,0.00019481727,0.00021277873,0.00034824706],"domain_scores_gemma":[0.99908453,0.00009025722,0.000122010395,0.000065674714,0.0001270142,0.00051048415],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003507264,0.00010494948,0.0001908718,0.0000791582,0.0005941135,0.0003736327,0.00020212264,0.000050943927,0.0022515247],"category_scores_gemma":[0.0001615414,0.00007524027,0.00005760772,0.00025415912,0.0004540531,0.00045675176,0.000008145908,0.00012816279,0.00002017876],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000088930665,0.0000026321984,0.98888093,0.0000027969404,0.00001792721,0.00033150273,0.00030445535,0.00038923745,0.000022744118,0.00008304491,0.00020531093,0.009750519],"study_design_scores_gemma":[0.00013332545,0.00031217406,0.98553085,0.000035150868,0.000013651003,0.00010763905,0.0017208098,0.00014684846,0.00006728809,0.0018755528,0.0099419765,0.00011473066],"about_ca_topic_score_codex":0.038076438,"about_ca_topic_score_gemma":0.957102,"teacher_disagreement_score":0.91902554,"about_ca_system_score_codex":0.0000010776521,"about_ca_system_score_gemma":0.0005768418,"threshold_uncertainty_score":0.99866056},"labels":[],"label_agreement":null},{"id":"W3168560974","doi":"10.1139/cjes-2020-0174","title":"Theropod guild structure and the tyrannosaurid niche assimilation hypothesis: implications for predatory dinosaur macroecology and ontogeny in later Late Cretaceous Asiamerica<sup>1</sup>","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Guild; Ecological niche; Cretaceous; Ecology; Predation; Biology; Taxon; Niche; Theropoda; Carnivore; Paleoecology; Paleontology; Habitat","score_opus":0.019229599193660355,"score_gpt":0.22195893465982228,"score_spread":0.20272933546616193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3168560974","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9784134,0.008709491,0.000026016507,0.011820016,0.00014265647,0.00012886277,0.00017068352,0.000002306744,0.0005865761],"genre_scores_gemma":[0.99758923,0.0002444843,0.0011270421,0.00089584664,0.00006999564,0.0000011733365,0.000007839747,0.0000014758259,0.00006293294],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989391,0.0002287325,0.000251279,0.0001963568,0.00006161359,0.0003229029],"domain_scores_gemma":[0.99898624,0.00052003184,0.0001391232,0.00009180659,0.000078314166,0.00018446852],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006184658,0.00009364585,0.00020192479,0.00013528773,0.00046411788,0.000057466666,0.00021310644,0.000103013845,0.0002842459],"category_scores_gemma":[0.00030297332,0.000060015373,0.00003913444,0.00020009995,0.0012271658,0.00019783402,0.0000060927878,0.0001647126,0.0000016841993],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003100088,0.0000019545412,0.99231064,0.000003840256,0.000019920244,0.0000127216945,0.000420107,0.0024454829,0.000029959614,0.00016586737,0.000087711574,0.004470802],"study_design_scores_gemma":[0.000433216,0.00011185689,0.9837077,0.000008976623,0.000018429191,0.0004793937,0.00022972522,0.0029182956,0.000017025155,0.007865955,0.0041357055,0.00007366568],"about_ca_topic_score_codex":0.0006350504,"about_ca_topic_score_gemma":0.28493798,"teacher_disagreement_score":0.28430292,"about_ca_system_score_codex":0.0000025553743,"about_ca_system_score_gemma":0.0006905817,"threshold_uncertainty_score":0.72811},"labels":[],"label_agreement":null},{"id":"W3170912175","doi":"10.1139/cjes-2020-0194","title":"Multi-decadal coastal evolution of a North Atlantic shelf-edge vegetated sand island — Sable Island, Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Nova Scotia Community College; Dalhousie University; Parks Canada; Greenfield Research (Canada); Université du Québec à Rimouski; Geological Survey of Canada","funders":"Natural Resources Canada; Parks Canada","keywords":"Barrier island; Geology; Oceanography; Shore; Bay","score_opus":0.009607988351532286,"score_gpt":0.18813912547574738,"score_spread":0.1785311371242151,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3170912175","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99462265,0.0028897019,0.00021946209,0.00019927976,0.0007027371,0.00005821349,0.00019762082,0.0000023053851,0.0011080108],"genre_scores_gemma":[0.998993,0.00003906017,0.00049766,0.00010179765,0.00010604293,9.529323e-8,0.00001973557,0.0000026701719,0.00023995],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99843293,0.00007578922,0.0003711471,0.00019601699,0.00042133906,0.000502752],"domain_scores_gemma":[0.9986144,0.00010488709,0.0002546714,0.00009634447,0.00029509823,0.0006346538],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037871505,0.00013527936,0.00028073107,0.00017359034,0.00036729607,0.00010520942,0.00032155516,0.000042712512,0.000846414],"category_scores_gemma":[0.00019681033,0.000106380496,0.00006715257,0.0008129742,0.0003167799,0.0003736735,0.0000069765597,0.0001771566,0.000010855124],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011032871,0.000005253411,0.9859655,0.000037466027,0.000018360199,0.00035561278,0.00012650703,0.0118973525,0.000023660597,0.0000058684177,0.00097167,0.00058172626],"study_design_scores_gemma":[0.0004448584,0.00022442038,0.97748417,0.00010074664,0.00002432458,0.00045428317,0.000294312,0.017201342,0.00017295258,0.00004358026,0.0033956065,0.00015942141],"about_ca_topic_score_codex":0.8741092,"about_ca_topic_score_gemma":0.9998877,"teacher_disagreement_score":0.12577848,"about_ca_system_score_codex":0.000007810329,"about_ca_system_score_gemma":0.012061216,"threshold_uncertainty_score":0.99353945},"labels":[],"label_agreement":null},{"id":"W3174757745","doi":"10.1139/cjes-2021-0010","title":"A revised coastal sensitivity index for Canada’s marine coasts calculated using nonparametric statistics","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"World Wildlife Fund Canada; Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Sensitivity (control systems); Nonparametric statistics; Statistics; Comparability; Index (typography); Range (aeronautics); Measure (data warehouse); Mathematics; Econometrics; Computer science; Data mining","score_opus":0.018715580525502255,"score_gpt":0.2217967903739151,"score_spread":0.20308120984841282,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3174757745","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98752093,0.00016581215,0.00809128,0.0003681022,0.0010551912,0.000119832664,0.0014172458,0.0000033655065,0.0012582166],"genre_scores_gemma":[0.98997587,0.000011727078,0.009305277,0.00026804567,0.00010123329,6.3155255e-8,0.000062435174,0.0000030533251,0.00027226904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985206,0.00008565019,0.00034787966,0.00018647309,0.0003716772,0.0004877081],"domain_scores_gemma":[0.99812675,0.00031665803,0.00022106584,0.00008920309,0.0005163071,0.0007300224],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006861372,0.0001285329,0.00026435388,0.0002505111,0.0004124179,0.00017954175,0.00015993022,0.00004174474,0.00059623003],"category_scores_gemma":[0.000730875,0.00011229131,0.00006416246,0.00086518883,0.00022998439,0.00020988965,0.000017008528,0.00016336265,0.0000014724429],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021090169,0.000005844463,0.93150157,0.000025682748,0.000025369232,0.001210758,0.000032915934,0.0361704,0.000029769793,0.00011578797,0.00041635643,0.030444458],"study_design_scores_gemma":[0.0003481696,0.00014461453,0.71291196,0.000036373953,0.000029218252,0.00093617017,0.00018006707,0.27864286,0.000040823725,0.00036505054,0.0061681,0.00019659215],"about_ca_topic_score_codex":0.93867874,"about_ca_topic_score_gemma":0.9998262,"teacher_disagreement_score":0.24247247,"about_ca_system_score_codex":0.000009221497,"about_ca_system_score_gemma":0.016541194,"threshold_uncertainty_score":0.9890341},"labels":[],"label_agreement":null},{"id":"W3174771914","doi":"10.1139/cjes-2021-0030","title":"U–Pb zircon geochronology and implications of Cambrian plutonism in the Ellsworth belt, Maine","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland; Mount Royal University","funders":"Strong","keywords":"Geology; Metamorphism; Zircon; Plutonism; Schist; Protolith; Geochronology; Geochemistry; Orogeny; Magmatism; Greenschist; Subduction; Metamorphic rock; Seismology; Tectonics","score_opus":0.01575820496672243,"score_gpt":0.2032117879305889,"score_spread":0.18745358296386647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3174771914","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9817854,0.0026112301,0.000030509025,0.009679312,0.000059245016,0.000026416441,0.000025621146,7.6757465e-7,0.0057814815],"genre_scores_gemma":[0.9983433,0.00010124776,0.00088815595,0.00057206734,0.00003754478,1.1476784e-7,0.000006044372,3.9310203e-7,0.00005113079],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991583,0.000081216225,0.0002573935,0.0001247442,0.0001256406,0.0002526687],"domain_scores_gemma":[0.9993267,0.00016803804,0.00011817601,0.00008453033,0.00008250248,0.00022004634],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00055410556,0.000059892798,0.00016463397,0.00014531318,0.00018955028,0.000050002196,0.000291321,0.000035561807,0.0016870708],"category_scores_gemma":[0.00015585075,0.000035518,0.000052693493,0.00063965615,0.00063224486,0.000108086104,0.0000056654403,0.00013463947,0.0000054489906],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000014039426,0.0000048199904,0.99387044,0.0000027535912,0.0000072305716,0.000052848256,0.00015483222,0.0004924174,0.00049650756,0.0011383793,0.000035061636,0.0037432923],"study_design_scores_gemma":[0.000083242114,0.000101553516,0.9844047,0.000009436805,0.000011764471,0.0002399949,0.0004855323,0.0001446727,0.00032486266,0.012248211,0.0018971949,0.00004885002],"about_ca_topic_score_codex":0.023123551,"about_ca_topic_score_gemma":0.7930695,"teacher_disagreement_score":0.7699459,"about_ca_system_score_codex":7.5921486e-7,"about_ca_system_score_gemma":0.0005649937,"threshold_uncertainty_score":0.9992255},"labels":[],"label_agreement":null},{"id":"W3175329553","doi":"10.1139/cjes-2020-0184","title":"Revisiting Russell’s troodontid: autecology, physiology, and speculative tool use<sup>1</sup>","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Biology; Eusociality; Ecology; Zoology; Paleontology; Extinction event; Nest (protein structural motif); Osteology; Extant taxon; Evolutionary biology; Biological dispersal","score_opus":0.023446522895553847,"score_gpt":0.2204850068848107,"score_spread":0.19703848398925686,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3175329553","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9907324,0.004157593,0.000026587943,0.0016358416,0.0003756228,0.00004393182,0.00004677568,0.000004524343,0.0029767398],"genre_scores_gemma":[0.9957148,0.00016074537,0.0030346033,0.0006135006,0.0002482283,1.2822827e-7,0.000010439139,0.0000012731607,0.00021628395],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985483,0.0002837933,0.00031833444,0.00025618958,0.00010634509,0.0004869919],"domain_scores_gemma":[0.99882674,0.00040407936,0.00017484081,0.00008804805,0.00013881619,0.00036744546],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00073728204,0.00012096293,0.0002801516,0.00019874395,0.0006310934,0.0000824821,0.00022882,0.00012169619,0.0020792894],"category_scores_gemma":[0.0005121577,0.00009625342,0.00007199857,0.00033648466,0.0013288651,0.00055227365,0.000008164839,0.00025870613,0.000036825848],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009019013,0.0000020794598,0.9946033,0.000004590461,0.00002485397,0.00025581103,0.00019877266,0.0017753004,0.00006572917,0.00052873103,0.00012200787,0.0024098053],"study_design_scores_gemma":[0.00015892395,0.00017442765,0.9841918,0.000025484027,0.000015954562,0.0015041566,0.0005447253,0.0028599992,0.000023997438,0.0013048894,0.009074809,0.00012087366],"about_ca_topic_score_codex":0.0027034096,"about_ca_topic_score_gemma":0.123751715,"teacher_disagreement_score":0.1210483,"about_ca_system_score_codex":0.000002426363,"about_ca_system_score_gemma":0.0014361013,"threshold_uncertainty_score":0.99883294},"labels":[],"label_agreement":null},{"id":"W3176729296","doi":"10.1139/cjes-2021-0039","title":"Chronology and stratigraphy of the Imlay Channel in Lapeer County, Michigan, USA","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Geological Survey; University of Toledo","keywords":"Radiocarbon dating; Geology; Deglaciation; Bedrock; Alluvium; Channel (broadcasting); Holocene; Geomorphology; Glacial period; Stratigraphy; Alluvial fan; Oceanography; Paleontology; Archaeology; Sedimentary rock; Tectonics; Geography","score_opus":0.0225452606890045,"score_gpt":0.2278976721669874,"score_spread":0.2053524114779829,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3176729296","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9879785,0.0049419412,0.0000012659244,0.002010437,0.00035186944,0.00003276187,0.0000162204,4.1250726e-7,0.0046665496],"genre_scores_gemma":[0.9994309,0.00013770821,0.00010047184,0.00022049053,0.000022000611,7.3056825e-8,7.305511e-7,4.982056e-7,0.00008711947],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99904734,0.00016576952,0.00021183606,0.000117001946,0.00014653782,0.00031151273],"domain_scores_gemma":[0.9993392,0.00019278842,0.00010267736,0.00007859605,0.000095429474,0.00019126962],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007659089,0.00005883407,0.00015836878,0.00022528724,0.00020229533,0.000029641513,0.00031094,0.00006982743,0.00084654975],"category_scores_gemma":[0.00017269932,0.000038398484,0.000039241524,0.00053190085,0.0015134255,0.00013928681,0.0000066028356,0.00023260493,0.000005669395],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000028407605,0.0000021424992,0.99896914,0.0000053901385,0.0000059099007,0.000078036814,0.0002114794,0.0003171049,0.000017797292,0.0002700145,0.000017308956,0.000102862956],"study_design_scores_gemma":[0.00013149159,0.00010081088,0.99606997,0.000026893338,0.0000036931954,0.0005483177,0.00044556585,0.000177087,0.00025489886,0.0018143863,0.00038485354,0.00004204518],"about_ca_topic_score_codex":0.0053343233,"about_ca_topic_score_gemma":0.97240824,"teacher_disagreement_score":0.9670739,"about_ca_system_score_codex":1.5170015e-7,"about_ca_system_score_gemma":0.0020634562,"threshold_uncertainty_score":0.92691267},"labels":[],"label_agreement":null},{"id":"W3179308807","doi":"10.1139/cjes-2020-0176","title":"The promise of taphonomy as a nomothetic discipline: taphonomic bias in two dinosaur-bearing faunas in North America<sup>1</sup>","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Taphonomy; Paleontology; Geology; Cretaceous; Fauna; Taxon; Paleoecology; Nomothetic; Fossil Record; Theropoda; Ecology; Biology; Nomothetic and idiographic","score_opus":0.023092536247414835,"score_gpt":0.2378182007504188,"score_spread":0.21472566450300395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3179308807","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923824,0.0034544058,0.0000044299345,0.0014095575,0.00026240724,0.000080591046,0.000021993716,0.0000015538042,0.0023826582],"genre_scores_gemma":[0.9992939,0.00016596851,0.0002905187,0.000116853225,0.0000564503,6.529026e-7,0.000005332621,0.0000014326273,0.000068855574],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983745,0.00023420215,0.0005124801,0.00021650492,0.00014287661,0.00051940803],"domain_scores_gemma":[0.9988915,0.00036311228,0.00024166837,0.00013262448,0.000064813124,0.00030629564],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00085820287,0.00011557133,0.0002706124,0.00036639645,0.00031805082,0.00005546292,0.00052654237,0.00004325,0.00039212452],"category_scores_gemma":[0.00031412777,0.00008044635,0.00007801642,0.0009770679,0.0012748394,0.0002770506,0.000011784847,0.00028596722,0.000034067212],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001832223,0.0000071191084,0.9607885,0.000002888703,0.0000072437647,0.00012514337,0.0008089998,0.034161128,0.000009484254,0.000041992804,0.000014879515,0.0040143034],"study_design_scores_gemma":[0.00031249458,0.00015808658,0.98755985,0.00003569882,0.0000046947166,0.00024514055,0.0018007946,0.006379176,0.000021919132,0.00057192944,0.0028106233,0.000099608136],"about_ca_topic_score_codex":0.03284406,"about_ca_topic_score_gemma":0.9325888,"teacher_disagreement_score":0.8997448,"about_ca_system_score_codex":0.0000067242026,"about_ca_system_score_gemma":0.0026895409,"threshold_uncertainty_score":0.97359633},"labels":[],"label_agreement":null},{"id":"W3180174157","doi":"10.1139/cjes-2021-0023","title":"Eruption of Mount Meager, British Columbia, during the early Fraser glaciation","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; Interior Health; Kelowna General Hospital; University of British Columbia","funders":"","keywords":"Geology; Pyroclastic rock; Explosive eruption; Glacial period; Volcano; Geomorphology; Ice sheet; Pyroclastic fall; Mount; Paleontology","score_opus":0.01493910571356784,"score_gpt":0.21136929652300243,"score_spread":0.19643019080943458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3180174157","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99518186,0.0019235545,0.0000044775766,0.0004278959,0.00039891023,0.000040686165,0.000020195888,0.0000014893346,0.0020009386],"genre_scores_gemma":[0.9990756,0.00008126621,0.00013354559,0.00008821981,0.00006513231,1.3399313e-7,0.0000028556437,8.2757094e-7,0.00055244693],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988654,0.00018602579,0.00025459824,0.00011375283,0.00027427598,0.00030589863],"domain_scores_gemma":[0.9991427,0.00014513114,0.00016319443,0.00008061421,0.00024309765,0.00022523037],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010430692,0.00004146208,0.00013402505,0.00008918659,0.0006510437,0.00024715785,0.0002903622,0.00006181864,0.004543862],"category_scores_gemma":[0.00027415727,0.00004119422,0.000059987982,0.0004635307,0.0006520963,0.00030944936,0.0000045006905,0.00021095703,0.000029638768],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000024179344,0.0000021703597,0.9987329,0.000005975489,0.0000094237685,0.00016728675,0.00012077362,0.00043082127,0.000016938828,0.000012312393,0.00004209756,0.00045685098],"study_design_scores_gemma":[0.0001332826,0.00008748704,0.99755627,0.000028514243,0.0000066711123,0.00042599032,0.00034439148,0.00011044947,0.00008910959,0.00040005718,0.0007714464,0.000046339726],"about_ca_topic_score_codex":0.1305306,"about_ca_topic_score_gemma":0.9876716,"teacher_disagreement_score":0.857141,"about_ca_system_score_codex":7.752942e-7,"about_ca_system_score_gemma":0.0011532403,"threshold_uncertainty_score":0.99636614},"labels":[],"label_agreement":null},{"id":"W3183001791","doi":"10.1139/cjes-2020-0145","title":"Anatomical, morphometric, and stratigraphic analyses of theropod biodiversity in the Upper Cretaceous (Campanian) Dinosaur Park Formation<sup>1</sup>","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; University of Alberta; University of Toronto; Royal British Columbia Museum","funders":"","keywords":"Geology; Paleontology; Taxon; Biostratigraphy; Autapomorphy; Theropoda; Cretaceous; Biodiversity; Taphonomy; Ecology; Biology; Phylogenetic tree","score_opus":0.03825728276626194,"score_gpt":0.24050972218998315,"score_spread":0.2022524394237212,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3183001791","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9889995,0.008605437,0.000012760132,0.0013102032,0.0000776519,0.00003751795,0.00007540546,0.0000010972768,0.0008804566],"genre_scores_gemma":[0.99896467,0.00040520303,0.00033680417,0.00026036656,0.000020969677,6.279564e-8,0.0000068890463,2.954101e-7,0.0000047688663],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99891055,0.00025937232,0.00026661306,0.00012316593,0.0001797354,0.00026053772],"domain_scores_gemma":[0.99923384,0.00025231502,0.00015088651,0.00007923799,0.00009220201,0.00019152195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000756409,0.00007761958,0.00018821137,0.0005229869,0.0003491902,0.00005522788,0.0003272908,0.00006675811,0.0005989689],"category_scores_gemma":[0.0001959943,0.00004912848,0.00006429039,0.0011909903,0.00095010217,0.0004033728,0.000003880266,0.00016702074,0.000006525198],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000061944693,0.0000052985624,0.99733436,0.0000036099518,0.000013944492,0.00009112682,0.0004631784,0.0012449234,0.000016985854,0.000049157246,0.0001258379,0.0006453697],"study_design_scores_gemma":[0.00013890854,0.00016500783,0.99301445,0.0000113698725,0.000016844902,0.00047692913,0.0031892653,0.0016674765,0.000045060082,0.00046016078,0.0007529364,0.00006155862],"about_ca_topic_score_codex":0.00791918,"about_ca_topic_score_gemma":0.29205665,"teacher_disagreement_score":0.28413746,"about_ca_system_score_codex":0.0000012973799,"about_ca_system_score_gemma":0.00062318525,"threshold_uncertainty_score":0.99868715},"labels":[],"label_agreement":null},{"id":"W3183887234","doi":"10.1139/cjes-2021-0019","title":"Boulder-strewn flats in a high-latitude macrotidal embayment, Baffin Island: geomorphology, formation, and future stability","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Memorial University of Newfoundland","funders":"Natural Resources Canada; Memorial University of Newfoundland; ArcticNet; Université Laval","keywords":"Geology; Beach morphodynamics; Oceanography; Sea level; Geomorphology; Intertidal zone; Arctic; Tidal range; Sea ice; Sediment; Sediment transport; Estuary","score_opus":0.029074129414106573,"score_gpt":0.23163283540461327,"score_spread":0.20255870599050668,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3183887234","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.991788,0.0027661023,0.000009973151,0.0033130231,0.0005744186,0.00006400018,0.0007918535,0.0000018793421,0.0006907012],"genre_scores_gemma":[0.9983544,0.0003779253,0.0003705943,0.0005267427,0.00024016447,2.0568885e-7,0.00010323311,0.000001452368,0.000025285182],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988228,0.00009767126,0.00032231686,0.0001723492,0.00019751232,0.0003873345],"domain_scores_gemma":[0.99917984,0.00007816024,0.00013485964,0.0000885174,0.000101269135,0.00041733638],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000698234,0.0001033306,0.00019569963,0.00020942213,0.0002856573,0.0002164563,0.00018994653,0.0000666282,0.010276542],"category_scores_gemma":[0.000056935376,0.000083068415,0.000037029207,0.00043488535,0.0003075156,0.00059953606,0.0000073892766,0.00019198046,0.0000151004115],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000062208,0.0000044077447,0.99483687,0.000012184317,0.000003535531,0.00025420924,0.0011138836,0.00030498375,0.00007237364,0.0000418836,0.00035575955,0.0029936756],"study_design_scores_gemma":[0.00034551232,0.00013589585,0.9818389,0.00003427035,0.000006163505,0.00058326684,0.0020777087,0.0006365742,0.00023478047,0.00041672002,0.013571355,0.000118897085],"about_ca_topic_score_codex":0.03118285,"about_ca_topic_score_gemma":0.9831122,"teacher_disagreement_score":0.95192933,"about_ca_system_score_codex":0.0000038281046,"about_ca_system_score_gemma":0.0008142092,"threshold_uncertainty_score":0.9906282},"labels":[],"label_agreement":null},{"id":"W3184906136","doi":"10.1139/cjes-2021-0003","title":"Geophysical reassessment of the role of ancient lineaments on the development of the western Laurentian margin and its sediment-hosted Zn–Pb deposits, Yukon and Northwest Territories, Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Lineament; Craton; Terrane; Paleontology; Fault (geology); Plutonism; Tectonics; Geomorphology; Geochemistry; Seismology; Pluton","score_opus":0.00920960268428472,"score_gpt":0.1770922733523499,"score_spread":0.16788267066806517,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3184906136","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996719,0.0012451852,5.031745e-7,0.0015584143,0.00016940608,0.00006015119,0.00007204631,3.7703074e-7,0.0001748933],"genre_scores_gemma":[0.9996137,0.0000125684555,0.00009422991,0.00022195496,0.000024453791,2.186807e-7,0.0000036617337,7.1941656e-7,0.000028510174],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986513,0.00009229135,0.00033568847,0.00013151005,0.00058369694,0.00020550168],"domain_scores_gemma":[0.9991177,0.00010651631,0.00027278042,0.00010013228,0.00018089842,0.00022197957],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003393048,0.00008909603,0.00018457482,0.000035876907,0.00027585775,0.00003360522,0.00034883103,0.000024644562,0.00012944634],"category_scores_gemma":[0.00008525749,0.000039867147,0.000051166244,0.00040617748,0.00030829763,0.000056475677,0.000031150117,0.00012161571,2.0082483e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000044075227,0.000011688354,0.996756,0.0000085881675,0.000027702627,0.000003358398,0.00021346794,0.00016958156,0.0006038877,0.000033348133,0.000016516855,0.0021514269],"study_design_scores_gemma":[0.000079908925,0.00006988053,0.9759803,0.000083187304,0.000024842047,0.000010862975,0.0005315824,0.00020420857,0.020893317,0.00008281892,0.0019890463,0.0000500492],"about_ca_topic_score_codex":0.41348645,"about_ca_topic_score_gemma":0.994249,"teacher_disagreement_score":0.58076257,"about_ca_system_score_codex":0.0000051241313,"about_ca_system_score_gemma":0.0019905244,"threshold_uncertainty_score":0.5904192},"labels":[],"label_agreement":null},{"id":"W3187880086","doi":"10.1139/cjes-2021-0061","title":"Neodymium isotope mapping a polygenetic TTG batholith: failed back-arc rifting in the Central Metasedimentary Belt, southwestern Grenville Province","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"Monash University; Australian Government; McMaster University","keywords":"Geology; Batholith; Magmatism; Rift; Geochemistry; Crust; Mafic; Mantle (geology); Underplating; Subduction; Continental arc; Petrology; Tectonics; Paleontology","score_opus":0.02053608848190229,"score_gpt":0.19159341854965795,"score_spread":0.17105733006775564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3187880086","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98861086,0.0033321832,0.000016583384,0.005544236,0.000205462,0.00007174545,0.00005902563,0.000001725986,0.0021581934],"genre_scores_gemma":[0.99560094,0.00003062403,0.0015696323,0.0025385218,0.00013105593,2.484815e-7,0.000013274008,0.0000013218347,0.00011435498],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99796087,0.00021409716,0.00043608446,0.00027045602,0.00042045728,0.00069805456],"domain_scores_gemma":[0.9989484,0.00015550396,0.00017691049,0.00013311466,0.00007317567,0.00051289424],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008727286,0.00014347801,0.0002555334,0.00019184459,0.00036058165,0.00025349105,0.0006248889,0.000039524053,0.0077360948],"category_scores_gemma":[0.0001329103,0.00008589925,0.00015652744,0.00095888786,0.0003872822,0.00021533633,0.000014682101,0.00027090393,0.000061542334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002962012,0.000007658832,0.9958439,0.000005838812,0.000014472122,0.00044143148,0.00074971153,0.00092788774,0.00011611504,0.000011758182,0.00006996279,0.0018083022],"study_design_scores_gemma":[0.00018439227,0.00011032656,0.98861295,0.000050140443,0.000025778474,0.00022660637,0.0029603594,0.0013986679,0.0003020422,0.0010240052,0.0049511744,0.00015356434],"about_ca_topic_score_codex":0.05042595,"about_ca_topic_score_gemma":0.6395704,"teacher_disagreement_score":0.58914447,"about_ca_system_score_codex":0.0000028375416,"about_ca_system_score_gemma":0.0010009859,"threshold_uncertainty_score":0.993171},"labels":[],"label_agreement":null},{"id":"W3190949912","doi":"10.1139/cjes-2021-0038","title":"Petrology and age of the Lepreau River Dyke, southern New Brunswick, Canada: source of the end-Triassic Fundy Group basalts","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University","funders":"","keywords":"Geology; Basalt; Outcrop; Mesozoic; Structural basin; Geochemistry; Lineament; Flood basalt; Paleontology; Tectonics","score_opus":0.0138454073470042,"score_gpt":0.16765935037797144,"score_spread":0.15381394303096724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3190949912","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99251467,0.0019360179,0.000013546269,0.003890309,0.00025242966,0.00003069875,0.000027119691,7.307888e-7,0.0013344549],"genre_scores_gemma":[0.9983366,0.000017311537,0.00015627727,0.0005453699,0.00006676198,2.0497795e-8,0.0000015523186,9.0594966e-7,0.0008751681],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986889,0.00016230026,0.00031879672,0.00015588028,0.00036910892,0.0003050127],"domain_scores_gemma":[0.9988597,0.00021234166,0.00028570028,0.0001411512,0.00009551258,0.00040560772],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042303145,0.00009299315,0.00025916618,0.00006262507,0.00026175572,0.000031438252,0.0005768727,0.000045579174,0.0025069925],"category_scores_gemma":[0.00032844496,0.00004558177,0.00013519096,0.0006563717,0.0012222775,0.00007060181,0.000024659135,0.0001941984,0.0000020213527],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000042211054,0.0000026894947,0.9955989,0.0000037986385,0.00002182601,0.00002273394,0.00023094905,0.0013077065,0.0001244234,0.000088871806,0.00011471455,0.002479161],"study_design_scores_gemma":[0.00013494954,0.00006606502,0.9925956,0.000020791838,0.000038900387,0.00007313588,0.00051586836,0.00024138381,0.0002933292,0.0019814838,0.0039764475,0.00006202523],"about_ca_topic_score_codex":0.9545703,"about_ca_topic_score_gemma":0.9994871,"teacher_disagreement_score":0.044916816,"about_ca_system_score_codex":0.0000022190545,"about_ca_system_score_gemma":0.005201086,"threshold_uncertainty_score":0.99840486},"labels":[],"label_agreement":null},{"id":"W3191379205","doi":"10.1139/cjes-2020-0007","title":"The oldest occurrence of brachylophosaurin hadrosaurids in Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature; Royal Ontario Museum; University of Toronto; Carleton University","funders":"","keywords":"Geology; Paleontology; Group (periodic table); Genus; Zoology; Biology","score_opus":0.015317731144253655,"score_gpt":0.19845981246705977,"score_spread":0.1831420813228061,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3191379205","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98449993,0.009237846,0.000002606379,0.001730747,0.0011036212,0.000022472967,0.00007832834,4.8590834e-7,0.0033239692],"genre_scores_gemma":[0.9994531,0.00014653076,0.0001288393,0.00019482449,0.000033790464,6.881154e-8,0.0000032181758,3.157042e-7,0.00003927894],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99892336,0.0001328747,0.0003127912,0.000106832405,0.00017086367,0.00035325097],"domain_scores_gemma":[0.99906594,0.0003439717,0.00015663817,0.00008107233,0.000100173995,0.00025220614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006843501,0.00006137202,0.00014398077,0.00009718715,0.00030711998,0.000023150857,0.0004206463,0.000032763073,0.0005536207],"category_scores_gemma":[0.00030058686,0.000041095307,0.000033138425,0.00049147214,0.0007184409,0.00014618946,0.000003460974,0.00017306622,0.000004966872],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004255642,0.0000011907446,0.9944642,0.0000018185559,0.0000035196304,0.0002043195,0.00003957367,0.0013398483,0.000008580081,0.00015062281,0.00027296977,0.0035090863],"study_design_scores_gemma":[0.00007926425,0.00006294597,0.9879887,0.000018711882,0.0000021827807,0.00031863526,0.00042720293,0.00028762635,0.00008071282,0.0003929418,0.010289562,0.000051486622],"about_ca_topic_score_codex":0.9197245,"about_ca_topic_score_gemma":0.9999518,"teacher_disagreement_score":0.08022722,"about_ca_system_score_codex":0.000005082313,"about_ca_system_score_gemma":0.01878867,"threshold_uncertainty_score":0.9867739},"labels":[],"label_agreement":null},{"id":"W3193489041","doi":"10.1139/cjes-2020-0185","title":"Two braincases of <i>Daspletosaurus</i> (Theropoda: Tyrannosauridae): anatomy and comparison<sup>1</sup>","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University; University of Ottawa; McGill University; Canadian Museum of Nature; University of Alberta","funders":"","keywords":"Holotype; Anatomy; Geology; Theropoda; Endocast; Paleontology; Biology; Skull; Cretaceous; Taxonomy (biology); Zoology","score_opus":0.019459755898106664,"score_gpt":0.24331475282134135,"score_spread":0.22385499692323468,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3193489041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9729089,0.018269457,0.000024234318,0.0016882959,0.0002719543,0.000035986,0.000088477784,0.000003060743,0.0067096436],"genre_scores_gemma":[0.9977042,0.00011559415,0.0015216904,0.00046324477,0.00011100006,8.676639e-8,0.000009533338,0.0000012233744,0.00007339994],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99864787,0.00019270352,0.0003960796,0.00018999625,0.00018586726,0.0003874805],"domain_scores_gemma":[0.99877024,0.00028504015,0.0002202904,0.000093890914,0.00016010866,0.00047044552],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00065390486,0.00011117219,0.00031680742,0.00023152554,0.00038188245,0.000043289907,0.00029039616,0.00006988776,0.0016693271],"category_scores_gemma":[0.00021329203,0.00008896392,0.000071309754,0.00046257945,0.0015780765,0.00031140394,0.0000064848377,0.00018928689,0.00001806378],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011040389,0.0000063490756,0.9928483,0.0000068412387,0.000026240663,0.0001981834,0.0002503776,0.002656799,0.000036596033,0.00051098975,0.00036434154,0.0030839907],"study_design_scores_gemma":[0.00038549872,0.00034638643,0.97130334,0.000043547312,0.000027950353,0.0015765683,0.001352179,0.0034296217,0.00018675847,0.0012155386,0.019987078,0.0001455589],"about_ca_topic_score_codex":0.008270051,"about_ca_topic_score_gemma":0.3617286,"teacher_disagreement_score":0.35345855,"about_ca_system_score_codex":0.0000012574429,"about_ca_system_score_gemma":0.0016632548,"threshold_uncertainty_score":0.99924326},"labels":[],"label_agreement":null},{"id":"W3194636805","doi":"10.1139/cjes-2020-0175","title":"A new species of <i>Ectenosaurus</i> (Mosasauridae: Plioplatecarpinae) from western Kansas, USA, reveals a novel suite of osteological characters for the genus<sup>1</sup>","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Osteology; Anatomy; Genus; Holotype; Dorsum; Geology; Paleontology; Biology; Zoology","score_opus":0.03472434883122487,"score_gpt":0.22131888853025833,"score_spread":0.18659453969903345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3194636805","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887851,0.0065432023,0.00040271002,0.0025471766,0.0005432171,0.00011865594,0.00046402257,0.0000020178873,0.00059388793],"genre_scores_gemma":[0.996293,0.0001638781,0.00214644,0.00047020894,0.00025629648,3.8572523e-7,0.0000214945,0.0000016648543,0.0006466402],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984058,0.00011268154,0.0005462879,0.00023471707,0.00024150521,0.00045898356],"domain_scores_gemma":[0.99792415,0.0008979312,0.0004240715,0.00015950987,0.0002085609,0.00038579004],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007638592,0.00014216657,0.00041933154,0.00016598873,0.00032390017,0.000039760038,0.0006632931,0.00013382903,0.0016439372],"category_scores_gemma":[0.0003378543,0.00009230417,0.00017722778,0.0004326997,0.0011339993,0.00027201526,0.000010590346,0.00020022558,0.000013079422],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005937482,0.0000069178095,0.99449277,0.0000082801,0.000058233196,0.000048029517,0.0004692368,0.0017506365,0.00063976005,0.0001961832,0.00035490215,0.0019156714],"study_design_scores_gemma":[0.00036624324,0.0004189644,0.98676413,0.000054801803,0.00004451073,0.0002567196,0.00070267677,0.00031107353,0.00031355378,0.0004858319,0.010171101,0.00011038364],"about_ca_topic_score_codex":0.01437092,"about_ca_topic_score_gemma":0.30195114,"teacher_disagreement_score":0.28758022,"about_ca_system_score_codex":0.0000026250004,"about_ca_system_score_gemma":0.0020067196,"threshold_uncertainty_score":0.9992687},"labels":[],"label_agreement":null},{"id":"W3194697525","doi":"10.1139/cjes-2021-0004","title":"Marine record of late-glacial readvance and last recession of Laurentide ice, inner Frobisher Bay, Baffin Island, Arctic Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Memorial University of Newfoundland","funders":"Natural Resources Canada; University of California, Irvine; Memorial University of Newfoundland; ArcticNet; University of Ottawa","keywords":"Geology; Moraine; Ice sheet; Bay; Glacial period; Paleontology; Oceanography; Radiocarbon dating","score_opus":0.012312790117218027,"score_gpt":0.2152872973405832,"score_spread":0.20297450722336516,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3194697525","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924083,0.00130031,0.000003616883,0.0009662842,0.0006059107,0.000034309807,0.000033370266,7.549918e-7,0.004647175],"genre_scores_gemma":[0.99805784,0.00020391343,0.0010198798,0.00012095944,0.000042168016,8.7108674e-8,0.0000089327295,0.0000013565007,0.0005448803],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987092,0.00017072778,0.00036455563,0.00016286681,0.00025309602,0.00033953667],"domain_scores_gemma":[0.99879545,0.0002572275,0.00024618173,0.00009332142,0.00026165615,0.00034615345],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006799254,0.00008746412,0.0002793828,0.00020260557,0.00020281626,0.0000265612,0.00025570212,0.000067563145,0.0038946762],"category_scores_gemma":[0.0003827262,0.000067936686,0.000035690577,0.00050524407,0.0006423401,0.0002265646,0.000013600681,0.0002406247,0.0000035647106],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023489009,0.000003313407,0.996573,0.000027148808,0.000012366849,0.00016537026,0.000066398956,0.00035240428,0.000018691202,0.000019106608,0.00025315312,0.002485612],"study_design_scores_gemma":[0.00022569139,0.0001535315,0.99313736,0.00008630023,0.000009978247,0.00022761142,0.00020519193,0.00014811398,0.00023753027,0.00047914716,0.0050139655,0.000075571494],"about_ca_topic_score_codex":0.4504099,"about_ca_topic_score_gemma":0.9997463,"teacher_disagreement_score":0.54933643,"about_ca_system_score_codex":9.560957e-7,"about_ca_system_score_gemma":0.0034118474,"threshold_uncertainty_score":0.9970159},"labels":[],"label_agreement":null},{"id":"W3195429318","doi":"10.1139/cjes-2021-0016","title":"Petrogenesis and mode of emplacement of a Neoarchean tonalite–trondhjemite–diorite suite: the Eau Jaune Complex, Abitibi greenstone belt","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Université du Québec à Chicoutimi","funders":"Ministère de l'Énergie et des Ressources Naturelles; Université du Québec à Chicoutimi","keywords":"Geology; Greenstone belt; Archean; Geochemistry; Diorite; Basalt; Petrology; Craton; Magmatism; Zircon; Paleontology; Tectonics","score_opus":0.029692755454375337,"score_gpt":0.23496848348432312,"score_spread":0.20527572802994778,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3195429318","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916189,0.0039227335,0.000026043634,0.002991682,0.00007332959,0.000041414358,0.00016761218,0.0000012960207,0.001157022],"genre_scores_gemma":[0.9980721,0.00009093671,0.0013747461,0.00028581623,0.000054005122,1.20356e-7,0.000013989132,0.0000010893776,0.000107220505],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99839747,0.00012487893,0.0004785342,0.00018617684,0.0004518072,0.00036114015],"domain_scores_gemma":[0.9985866,0.00025621222,0.00026937964,0.00012682883,0.00027674207,0.00048425718],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00072351744,0.00011389867,0.00034576058,0.00015972141,0.00026302325,0.000050809955,0.00036691068,0.000038959133,0.0030514188],"category_scores_gemma":[0.00018161931,0.000068836234,0.00015461598,0.00075686665,0.001302003,0.00012996286,0.000017821523,0.00013761655,0.0000026919092],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011813556,0.000010058626,0.99171656,0.000015343272,0.00004435313,0.0000503656,0.00033073933,0.0021267263,0.0013328078,0.00027370683,0.000057263485,0.0040302733],"study_design_scores_gemma":[0.0001849538,0.0002863954,0.9913483,0.000036851667,0.000059114296,0.00019874942,0.00079145055,0.0018299259,0.0014340783,0.0028983487,0.0008267649,0.00010502986],"about_ca_topic_score_codex":0.10864881,"about_ca_topic_score_gemma":0.6982009,"teacher_disagreement_score":0.58955204,"about_ca_system_score_codex":0.0000016415692,"about_ca_system_score_gemma":0.00058226415,"threshold_uncertainty_score":0.99785995},"labels":[],"label_agreement":null},{"id":"W3195856100","doi":"10.1139/cjes-2021-0035","title":"Evidence for microbially mediated silver enrichment in a middle Cambrian Burgess Shale-type deposit, Mackenzie Mountains, northwestern Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Geology; Metallogeny; Geochemistry; Oil shale; Benthic zone; Water column; Sedimentary rock; Microbial mat; Paleozoic; Lagerstätte; Paleontology; Sphalerite; Pyrite; Cyanobacteria; Oceanography","score_opus":0.03453061598703413,"score_gpt":0.22354730550888052,"score_spread":0.1890166895218464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3195856100","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99362624,0.004572297,0.0000065904383,0.00080766506,0.00049784983,0.00007945195,0.00016466613,0.0000017284815,0.00024353075],"genre_scores_gemma":[0.99830806,0.000102567115,0.00038126137,0.00068973366,0.00009656675,4.2374145e-7,0.00007300025,0.0000020744044,0.0003463107],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982951,0.000062663865,0.00045391504,0.00026203666,0.0003656537,0.00056060875],"domain_scores_gemma":[0.9985767,0.00020566065,0.0001948007,0.00011386015,0.0002498913,0.00065910874],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00060598215,0.00014125608,0.00024835323,0.00015356716,0.00031912955,0.00018330349,0.00044333402,0.000046941746,0.0012590961],"category_scores_gemma":[0.00023935208,0.00012291913,0.000083644496,0.0008010307,0.00014061127,0.0003574951,0.000008000674,0.00013769578,0.0000067695887],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017465567,0.000005624827,0.9960608,0.000023926197,0.000023458184,0.000503097,0.00015181617,0.0017267943,0.00050760654,0.0000022852623,0.00022460308,0.00075256085],"study_design_scores_gemma":[0.00040300647,0.00018606485,0.98791635,0.0003128952,0.000047904065,0.00030358575,0.0014536516,0.001395593,0.0029177328,0.000041677627,0.0047401353,0.00028137476],"about_ca_topic_score_codex":0.928983,"about_ca_topic_score_gemma":0.99974465,"teacher_disagreement_score":0.07076167,"about_ca_system_score_codex":0.000023763756,"about_ca_system_score_gemma":0.0074524838,"threshold_uncertainty_score":0.9996539},"labels":[],"label_agreement":null},{"id":"W3198350856","doi":"10.1139/cjes-2021-0043","title":"Special Issue in honour of Dale Alan Russell (1937–2019)<sup>1</sup>","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta; Carleton University; Canadian Museum of Nature","funders":"","keywords":"Honour; Geology; Geochemistry; Philosophy; Archaeology; History","score_opus":0.015940665335279314,"score_gpt":0.21157550988837573,"score_spread":0.1956348445530964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3198350856","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.937047,0.0041210665,0.0000029014125,0.0013857883,0.0011948247,0.0000356442,0.00006791417,0.0000016167791,0.056143254],"genre_scores_gemma":[0.99693817,0.00018854278,0.0006470877,0.0002361204,0.0013102132,6.0546796e-8,0.000009929606,0.0000010390602,0.00066884886],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99865335,0.00019530045,0.0003753316,0.0001759951,0.00017100631,0.0004290378],"domain_scores_gemma":[0.9991176,0.00015194835,0.00016383087,0.00008776995,0.00009939367,0.00037944256],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00088313676,0.00009369796,0.00025611577,0.00034566043,0.00022320823,0.000028554738,0.00038959208,0.00009993373,0.008120167],"category_scores_gemma":[0.00022725982,0.00007762653,0.000070128146,0.0005692376,0.00074674166,0.000302832,0.0000045736765,0.0002448148,0.00012335036],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012565477,0.0000069426737,0.9876263,0.0000038361923,0.000008553689,0.000410403,0.00047656373,0.0048300344,0.000011841738,0.00011893747,0.0027091813,0.0037848398],"study_design_scores_gemma":[0.0001898618,0.00020087096,0.8933305,0.000031766172,0.0000058149876,0.0007000272,0.0009232919,0.0006096597,0.00006384278,0.00064971397,0.10320195,0.00009266296],"about_ca_topic_score_codex":0.011529026,"about_ca_topic_score_gemma":0.6201898,"teacher_disagreement_score":0.60866076,"about_ca_system_score_codex":0.0000023703544,"about_ca_system_score_gemma":0.0023021856,"threshold_uncertainty_score":0.9950533},"labels":[],"label_agreement":null},{"id":"W3199188719","doi":"10.1139/cjes-2021-0011","title":"Landfast ice properties over the Beaufort Sea region in 2000–2019 from MODIS and Canadian Ice Service data","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada; National Aeronautics and Space Administration","keywords":"Sea ice; Geology; Bay; Arctic; Arctic ice pack; Moderate-resolution imaging spectroradiometer; Oceanography; Beaufort sea; Beaufort scale; Satellite; Physical geography; Climatology; Geography","score_opus":0.036110447261706875,"score_gpt":0.2025700359499362,"score_spread":0.16645958868822933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3199188719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98584044,0.0026155252,0.000011856406,0.008782404,0.00039569085,0.00006228437,0.0003886944,0.0000017616117,0.0019013683],"genre_scores_gemma":[0.9962907,0.00021611217,0.0002844171,0.0028129516,0.00014617913,9.205422e-8,0.000041241907,0.0000023768562,0.0002059173],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987343,0.00009030824,0.00024053773,0.00023385024,0.00026450158,0.00043652425],"domain_scores_gemma":[0.9988147,0.000114858274,0.00010659084,0.00023737113,0.00010431993,0.0006221654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006564745,0.00010780727,0.00015903659,0.00016290104,0.00058002584,0.00029130856,0.000718574,0.000053402375,0.00048981834],"category_scores_gemma":[0.00013599238,0.000069399684,0.000022881119,0.0005171269,0.00035819825,0.0008087049,0.00002043222,0.00025369582,0.00001684311],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000052798287,0.0000017963499,0.9927186,0.000005491387,0.000011511836,0.00025517828,0.0013846238,0.0011883475,0.000002444605,0.000019669576,0.0004507366,0.0039563207],"study_design_scores_gemma":[0.00015336146,0.000037683334,0.9504234,0.00009287472,0.000018361321,0.00031816564,0.0037263006,0.025762226,0.0000036486044,0.00018653201,0.019149298,0.00012810153],"about_ca_topic_score_codex":0.9351933,"about_ca_topic_score_gemma":0.9987608,"teacher_disagreement_score":0.06356756,"about_ca_system_score_codex":0.000007723449,"about_ca_system_score_gemma":0.005987621,"threshold_uncertainty_score":0.9996475},"labels":[],"label_agreement":null},{"id":"W3201247534","doi":"10.1139/cjes-2021-0041","title":"The Early Cretaceous tectonic evolution of the southern Great Xing’an Range, northeastern China: new constraints from A2-type granite and monzodiorite","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Magmatism; Subduction; Zircon; Geochemistry; Mafic; Partial melting; Underplating; Mantle (geology); Lithosphere; Paleontology; Tectonics","score_opus":0.012245305180388915,"score_gpt":0.17951702015479865,"score_spread":0.16727171497440974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3201247534","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891659,0.008716255,0.000017479986,0.0011716129,0.00024611736,0.000036996895,0.000054514945,0.0000021009143,0.00058902265],"genre_scores_gemma":[0.9993954,0.00006390561,0.00017527939,0.000064211046,0.00009788347,3.6181977e-8,0.0000018353469,0.00000109413,0.0002003602],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988503,0.00013389446,0.00025852112,0.00016671298,0.00030232882,0.00028823933],"domain_scores_gemma":[0.9989535,0.00012233654,0.00018652763,0.0001313774,0.00014423256,0.00046201848],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003927943,0.000097734584,0.00018045554,0.000058575024,0.0005579545,0.00016780064,0.0004165079,0.00004554253,0.0012970597],"category_scores_gemma":[0.00018413525,0.000048395366,0.0001010694,0.000552271,0.0010831472,0.00016005296,0.000010665749,0.00019059154,0.0000140140855],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008922045,0.0000018030705,0.9869151,0.000001080111,0.000019308,0.000022017955,0.00033212366,0.0004879827,0.00012609329,0.000025998683,0.000004458376,0.012055091],"study_design_scores_gemma":[0.00013709822,0.00014032227,0.9878691,0.000029380219,0.000040733492,0.00008290008,0.00059758784,0.0008553001,0.000091386384,0.009711583,0.00036963876,0.00007498153],"about_ca_topic_score_codex":0.13192192,"about_ca_topic_score_gemma":0.827004,"teacher_disagreement_score":0.69508207,"about_ca_system_score_codex":0.0000016988629,"about_ca_system_score_gemma":0.0009616783,"threshold_uncertainty_score":0.9996159},"labels":[],"label_agreement":null},{"id":"W3202049332","doi":"10.1139/cjes-2020-0190","title":"Description and revised diagnosis of Asia’s first recorded pachycephalosaurid, <i>Sinocephale bexelli</i> gen. nov., from the Upper Cretaceous of Inner Mongolia, China","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Royal Tyrrell Museum; Royal Ontario Museum; University of Toronto","funders":"University of California Museum of Paleontology; American Museum of Natural History","keywords":"Autapomorphy; Holotype; Paleontology; Geology; Nomen dubium; Taxon; Cretaceous; Genus; Vertebrate paleontology; Biology; Zoology; Phylogenetic tree","score_opus":0.018610375457357265,"score_gpt":0.1988171136492019,"score_spread":0.18020673819184463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3202049332","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9681534,0.02655731,0.000015180854,0.0027235355,0.0005356832,0.000063784064,0.00019981065,0.0000017342096,0.001749555],"genre_scores_gemma":[0.99627894,0.002436821,0.0008979273,0.00020494888,0.00011935476,3.7739827e-7,0.000016246757,0.0000015101382,0.000043894033],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99870735,0.00020439654,0.00041868674,0.00019266487,0.00018314018,0.00029373716],"domain_scores_gemma":[0.99877214,0.00033663143,0.00033312713,0.00013425073,0.00015407585,0.0002697584],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00060837955,0.00011175686,0.0002916771,0.00013833835,0.00035667737,0.000037626498,0.00032971252,0.000097979755,0.0014386118],"category_scores_gemma":[0.0003377483,0.00007548028,0.000090387795,0.00041966114,0.0011848147,0.00031617514,0.000007531031,0.00017685356,0.0000070545816],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018656061,0.000008396119,0.99438566,0.00000768067,0.000026204176,0.000039594895,0.0004521833,0.00024949873,0.00006478488,0.000031713178,0.0005425373,0.004173113],"study_design_scores_gemma":[0.00019887321,0.00026037026,0.987401,0.00007925873,0.000036138215,0.00022238996,0.00061433867,0.00029794665,0.00039726534,0.0005786448,0.009825185,0.000088554145],"about_ca_topic_score_codex":0.035107225,"about_ca_topic_score_gemma":0.6158448,"teacher_disagreement_score":0.5807376,"about_ca_system_score_codex":0.000002025236,"about_ca_system_score_gemma":0.0007926465,"threshold_uncertainty_score":0.9994742},"labels":[],"label_agreement":null},{"id":"W3202744759","doi":"10.1139/cjes-2021-0026","title":"Postglacial sea-level lowstand on Cumberland Peninsula, Baffin Island, Nunavut","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Memorial University of Newfoundland","funders":"Natural Resources Canada; Memorial University of Newfoundland; ArcticNet","keywords":"Geology; Sea level; Glacial period; Holocene; Oceanography; Fjord; Peninsula; Post-glacial rebound; Paleontology; Radiocarbon dating; Moraine; Deglaciation; Quaternary; Geomorphology; Archaeology; Geography","score_opus":0.036611771934350876,"score_gpt":0.250413320927542,"score_spread":0.2138015489931911,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3202744759","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96669286,0.0015264088,0.000009973373,0.0022005949,0.0009925363,0.000047245216,0.00013241,0.000002774047,0.02839518],"genre_scores_gemma":[0.9977835,0.000057018922,0.0003402427,0.0005483551,0.00019236655,1.1262714e-7,0.000015235589,0.0000018463214,0.0010613423],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998244,0.00021629926,0.00028767347,0.00023058502,0.00038769498,0.0006337661],"domain_scores_gemma":[0.9984803,0.0003208771,0.00012215505,0.00012295082,0.00022350167,0.0007301693],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010126227,0.00012601129,0.00024746085,0.00032595976,0.0006830325,0.00016811739,0.00043009093,0.00011629468,0.008207905],"category_scores_gemma":[0.0004161759,0.00009744694,0.000091373375,0.000547037,0.0007769015,0.00026220316,0.0000061544347,0.00040141455,0.00038474592],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002793771,0.000006560881,0.9961083,0.0000042568263,0.0000144584665,0.0016856482,0.00017547605,0.0006362407,0.000003362627,0.00013233916,0.000701781,0.0005036286],"study_design_scores_gemma":[0.00044745047,0.00036475185,0.98928726,0.000036460056,0.000009593331,0.0021083509,0.00029317226,0.0006367255,0.00014056347,0.00079122384,0.0057479828,0.0001364481],"about_ca_topic_score_codex":0.0033228137,"about_ca_topic_score_gemma":0.9198857,"teacher_disagreement_score":0.9165629,"about_ca_system_score_codex":7.64284e-7,"about_ca_system_score_gemma":0.0035425138,"threshold_uncertainty_score":0.9926987},"labels":[],"label_agreement":null},{"id":"W3209122749","doi":"10.1139/cjes-2021-0015","title":"The Early Devonian eurypterid <i>Leiopterella tetliei</i> from Arctic Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Subterranean biodiversity and taxonomy","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"University of Bristol","keywords":"Devonian; Appendage; Geology; Paleontology; Holotype; Arctic; Anatomy; Paleozoic; Biology; Zoology; Oceanography; Genus","score_opus":0.02737688638750187,"score_gpt":0.1648276689082908,"score_spread":0.1374507825207889,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3209122749","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98065037,0.0025434522,0.0000065850886,0.0025280102,0.0017594113,0.000033652053,0.00011948055,0.0000021328494,0.012356914],"genre_scores_gemma":[0.9977989,0.00004653967,0.0004972426,0.0012423357,0.00018606543,4.1342894e-8,0.0000045241723,0.0000011760577,0.00022316852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99869084,0.000094945484,0.00024345372,0.00016636816,0.00036089978,0.0004434648],"domain_scores_gemma":[0.9985819,0.00028614566,0.00015426574,0.00013314,0.00014409836,0.0007004387],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00036869955,0.00010299394,0.00014047556,0.000070574555,0.0011886489,0.00048160134,0.0006150248,0.00003254727,0.00333774],"category_scores_gemma":[0.00012675839,0.00007163781,0.00006868982,0.00034126156,0.0004597532,0.0002837995,0.000007459295,0.00019729912,0.000065947235],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000056160807,9.97956e-7,0.9912816,0.0000012979093,0.000018149394,0.000578378,0.0001338381,0.00016869698,0.000003248358,0.000017037468,0.0009938478,0.006797286],"study_design_scores_gemma":[0.000118649645,0.00006717269,0.7552252,0.000023622042,0.000010058234,0.00014631465,0.0007412674,0.00005846127,0.00015485617,0.0001846299,0.24316445,0.00010531285],"about_ca_topic_score_codex":0.9318968,"about_ca_topic_score_gemma":0.9992909,"teacher_disagreement_score":0.2421706,"about_ca_system_score_codex":0.000005800224,"about_ca_system_score_gemma":0.0064919204,"threshold_uncertainty_score":0.9991403},"labels":[],"label_agreement":null},{"id":"W3210410028","doi":"10.1139/cjes-2019-0234","title":"A new, “dwarfed” species of the phenacodontid “condylarth” <i>Ectocion</i> from the late Paleocene of Alberta, Canada, and its implications","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum; University of Alberta","funders":"Dirección General de Asuntos del Personal Académico, Universidad Nacional Autónoma de México; Peking University; Yale University","keywords":"Paleogene; Geology; Paleontology; Population; Sexual dimorphism; Juvenile; Ecology; Biology; Zoology; Cretaceous","score_opus":0.020000563086264047,"score_gpt":0.19728135129433833,"score_spread":0.17728078820807427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3210410028","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9657609,0.01251598,0.000008760727,0.014010305,0.00048081,0.000055001903,0.00017090542,6.8624655e-7,0.0069966572],"genre_scores_gemma":[0.9978398,0.00021428385,0.00013984136,0.0006654678,0.000062822575,9.8701136e-8,0.0000019727452,8.613772e-7,0.0010748649],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99906653,0.000108626475,0.00029584416,0.000103165105,0.00021155555,0.0002142952],"domain_scores_gemma":[0.99867827,0.00050480315,0.00027027132,0.0001215536,0.0001870765,0.00023802496],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026664935,0.00007902023,0.00018675967,0.000041820185,0.0004758521,0.00003252381,0.0003792054,0.000029593743,0.000894101],"category_scores_gemma":[0.00030882112,0.00004451037,0.00006234162,0.00040096793,0.000553853,0.00012383758,0.000009302218,0.00012138428,0.0000016462807],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001983112,0.0000010897767,0.9964985,0.0000022229087,0.000025810823,0.0000028581862,0.0006287282,0.00021323569,0.00007179154,0.0003873261,0.0015979061,0.000568496],"study_design_scores_gemma":[0.00010782384,0.000030742314,0.9861076,0.00003304111,0.000023304858,0.000032581927,0.00095871283,0.000055445435,0.00048063687,0.00042429075,0.011693234,0.00005259648],"about_ca_topic_score_codex":0.860836,"about_ca_topic_score_gemma":0.99988467,"teacher_disagreement_score":0.13904864,"about_ca_system_score_codex":0.0000016731876,"about_ca_system_score_gemma":0.0042564105,"threshold_uncertainty_score":0.97897786},"labels":[],"label_agreement":null},{"id":"W3210487123","doi":"10.1139/cjes-2021-0005","title":"Reconstruction of isostatically adjusted paleo-strandlines along the southern margin of the Laurentide Ice Sheet in the Great Lakes, Lake Agassiz, and Champlain Sea basins","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Manitoba; Geological Survey of Canada","funders":"Natural Resources Canada; U.S. Geological Survey","keywords":"Geology; Shore; Ice sheet; Paleontology; Oceanography; Isostasy; Geomorphology; Tectonics; Lithosphere","score_opus":0.024234111162556575,"score_gpt":0.22212290939317833,"score_spread":0.19788879823062175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3210487123","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99080044,0.0016514224,0.0000047582826,0.0057221428,0.00023449819,0.000086582135,0.00014603225,7.3471745e-7,0.0013534025],"genre_scores_gemma":[0.9994612,0.000095213145,0.00015728486,0.00017542524,0.000030412688,2.3044417e-7,0.0000041356,9.328766e-7,0.00007517385],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99837047,0.0006175729,0.00033705487,0.00012184274,0.00026387518,0.0002891936],"domain_scores_gemma":[0.9987321,0.00068172085,0.00018923874,0.00012945251,0.00014343644,0.00012406024],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002023021,0.00007924019,0.00018563397,0.00013078714,0.00036053814,0.00005124368,0.00044583046,0.000062575986,0.00093263114],"category_scores_gemma":[0.0004189396,0.000037853937,0.00006053615,0.00061175553,0.0018145224,0.0001267551,0.0000066389503,0.00029836805,0.0000028378647],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012019697,0.000003064084,0.99709606,0.00001377188,0.000011158992,0.000049320257,0.001023693,0.00032605106,0.000005317389,0.000071292816,0.000027383461,0.0013608681],"study_design_scores_gemma":[0.00019638032,0.00007672043,0.99207014,0.000080793936,0.0000150726555,0.0011683442,0.0049214736,0.00049659016,0.00003835349,0.0004624254,0.00042992437,0.000043763845],"about_ca_topic_score_codex":0.0041190586,"about_ca_topic_score_gemma":0.98106986,"teacher_disagreement_score":0.97695076,"about_ca_system_score_codex":2.868499e-7,"about_ca_system_score_gemma":0.0010414453,"threshold_uncertainty_score":0.9999806},"labels":[],"label_agreement":null},{"id":"W3211456013","doi":"10.1139/e10-102","title":"Basaltic to andesitic volcaniclastic rocks in the Blake River Group, Abitibi Greenstone Belt: 2. Origin, geochemistry, and geochronology <sup>1</sup>This article is a companion paper to Ross et al. 2011. Basaltic to andesitic volcaniclastic rocks in the Blake River Group, Abitibi Greenstone Belt: 1. Mode of emplacement in three areas. Canadian Journal of Earth Sciences, 48: this issue.<sup>2</sup>Ministère des Ressources naturelles et de la Faune (MRNF) Contribution BEGQ 8439-2010/2011-2. Natural Resources Canada, Earth Science Sector Contribution 20100252.","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec); Geological Survey of Canada; Institut National de la Recherche Scientifique","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Pyroclastic rock; Geology; Andesites; Geochemistry; Basalt; Andesite; Caldera; Volcanic rock; Geochronology; Group (periodic table); Volcano","score_opus":0.01097873983279496,"score_gpt":0.22336229028930835,"score_spread":0.2123835504565134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3211456013","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911835,0.0022047504,0.00016835936,0.0053042774,0.00015264851,0.0004902474,0.00027967597,0.000005499779,0.00021103663],"genre_scores_gemma":[0.9949089,0.00006285361,0.00054716715,0.004330828,0.000077860255,0.000005514748,0.000021350595,0.000007906824,0.000037614132],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99441516,0.0007760645,0.0011198043,0.00072848826,0.0013090385,0.0016514622],"domain_scores_gemma":[0.9959999,0.0010581092,0.00047033877,0.00031573555,0.0006938022,0.0014621587],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.005543557,0.00046311636,0.0007985399,0.0011009328,0.0011483121,0.0003562977,0.0014117903,0.00020600704,0.001350772],"category_scores_gemma":[0.0014804781,0.00031257045,0.00013812972,0.002001545,0.0038146358,0.0007708133,0.00005812285,0.001044474,0.000015484535],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021713033,0.00009065473,0.94819444,0.00002950776,0.000047810954,0.00039457172,0.018148048,0.030231649,0.0010615819,0.00013447742,0.0009031235,0.00054701214],"study_design_scores_gemma":[0.0010668733,0.00109179,0.96954393,0.00035271293,0.00008956363,0.0005853186,0.0023002091,0.022169162,0.00028558655,0.0009479429,0.001144307,0.0004226053],"about_ca_topic_score_codex":0.93590564,"about_ca_topic_score_gemma":0.9982149,"teacher_disagreement_score":0.06230929,"about_ca_system_score_codex":0.00011044874,"about_ca_system_score_gemma":0.0030217324,"threshold_uncertainty_score":0.99993265},"labels":[],"label_agreement":null},{"id":"W3211544365","doi":"10.1139/cjes-2021-0064","title":"Multi-criteria assessment approach of slow-moving urban landslide hazard: the case of Moulay Yacoub, Morocco","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Landslide; Bedrock; Marl; Borehole; Expansive clay; Geotechnical engineering; Soil water; Hydrology (agriculture); Geomorphology; Structural basin; Soil science","score_opus":0.018799125921867107,"score_gpt":0.25822867951244755,"score_spread":0.23942955359058044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3211544365","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920176,0.0006169974,0.0005734638,0.0003782728,0.000340388,0.0000707357,0.000021935626,0.0000018213346,0.005978779],"genre_scores_gemma":[0.9858804,0.000030846742,0.013566992,0.00009353199,0.000049476814,6.7333434e-7,9.2525755e-7,0.000005419814,0.00037177268],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986149,0.00011615382,0.00044000297,0.00017912092,0.00032766286,0.0003221768],"domain_scores_gemma":[0.99900013,0.000063182466,0.00032182658,0.00018916404,0.00007019554,0.00035550477],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012179188,0.0001092523,0.00023971216,0.00009601351,0.00033181213,0.000086530774,0.0004301564,0.000060276332,0.0008000185],"category_scores_gemma":[0.00008975504,0.000064705026,0.00012772359,0.0005258389,0.0007078815,0.0002567979,0.000056499437,0.00021930481,0.0000032060557],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016171296,0.00016588315,0.9180172,0.000060950955,0.00013756515,0.0039499383,0.005343826,0.040700343,0.021940995,0.00045715348,0.002997115,0.006212828],"study_design_scores_gemma":[0.0027634033,0.000935965,0.82672244,0.0004590136,0.00031522044,0.01694829,0.020772189,0.09025712,0.0143401595,0.00042562347,0.025182586,0.0008779981],"about_ca_topic_score_codex":0.007009922,"about_ca_topic_score_gemma":0.036821075,"teacher_disagreement_score":0.091294795,"about_ca_system_score_codex":0.0000228706,"about_ca_system_score_gemma":0.00078476296,"threshold_uncertainty_score":0.9996025},"labels":[],"label_agreement":null},{"id":"W3212329289","doi":"10.1139/cjes-2020-0198","title":"Chemostratigraphy as a tool for sequence stratigraphy in the Devonian Hare Indian Formation in the Mackenzie Mountains and Central Mackenzie Valley, Northwest Territories, Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Northwest Territories; University of Alberta","funders":"","keywords":"Sedimentary depositional environment; Geology; Chemostratigraphy; Marine transgression; Sedimentology; Sedimentary rock; Paleontology; Biogenic silica; Devonian; Deposition (geology); Sequence stratigraphy; Sediment; Geochemistry; Total organic carbon; Structural basin; Isotopes of carbon; Ecology","score_opus":0.02063851437350546,"score_gpt":0.22685659561108013,"score_spread":0.20621808123757468,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3212329289","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99052584,0.0035423248,0.0000063440334,0.0034768987,0.00026456802,0.00023067294,0.0007042822,0.000001429041,0.0012476335],"genre_scores_gemma":[0.99862754,0.000075615164,0.00038188204,0.00078210677,0.000078294506,0.0000025374534,0.00005018761,7.00684e-7,0.0000011617052],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99822813,0.00020209799,0.000415085,0.00019041201,0.0003790929,0.00058519683],"domain_scores_gemma":[0.99906784,0.00028604956,0.00017723623,0.00012556677,0.00008811979,0.00025516815],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00080745213,0.0001510883,0.00018615018,0.00023887868,0.00062740874,0.00040103603,0.00061333104,0.000073050454,0.000050093426],"category_scores_gemma":[0.00013798576,0.000097330274,0.000074059906,0.00093223364,0.0005019241,0.0007244801,8.758746e-7,0.00031677732,1.3635838e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010431901,0.0000052840232,0.9907322,0.000015898582,0.000008240922,0.0006224969,0.003107279,0.00006357221,0.00000677349,0.00063289027,0.0000949711,0.004699976],"study_design_scores_gemma":[0.0002633363,0.00019379663,0.98584265,0.00005313121,0.000008109384,0.0009370169,0.00919568,0.00016491083,0.000059421516,0.0017933345,0.0013580751,0.00013056648],"about_ca_topic_score_codex":0.8517886,"about_ca_topic_score_gemma":0.9999485,"teacher_disagreement_score":0.1481599,"about_ca_system_score_codex":0.000005015652,"about_ca_system_score_gemma":0.0047994843,"threshold_uncertainty_score":0.85140795},"labels":[],"label_agreement":null},{"id":"W3213891384","doi":"10.1139/cjes-2019-0002","title":"Geochronology, geochemistry, Sr–Nd–Hf isotope composition of the late Permian adakite in West Ujimqin, Inner Mongolia: petrogenesis and tectonic implications","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Adakite; Zircon; Petrogenesis; Partial melting; Magmatism; Pluton; Permian; Geochronology; Subduction; Crust; Olivine; Mantle (geology); Oceanic crust; Tectonics; Paleontology","score_opus":0.012191985786603347,"score_gpt":0.19863705371080387,"score_spread":0.1864450679242005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3213891384","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891674,0.003290621,0.0000029818966,0.0053913095,0.00006053142,0.000036646896,0.000054209293,0.0000016670859,0.0019946557],"genre_scores_gemma":[0.99931455,0.00012879698,0.00021617138,0.00023166515,0.000031303618,3.6184778e-7,0.0000081882945,9.015936e-7,0.00006804294],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989878,0.00007488319,0.0003171575,0.00016878068,0.00015153982,0.000299827],"domain_scores_gemma":[0.9991753,0.00008588681,0.00017780325,0.00012714948,0.0001533174,0.00028052938],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00030109042,0.00009318825,0.00020741347,0.00013238197,0.00026672898,0.000058496258,0.00034658806,0.000064887434,0.002831335],"category_scores_gemma":[0.00012246378,0.000060251958,0.000093660834,0.0008678688,0.00076714536,0.00013130052,0.000017258706,0.00018140645,0.000006989999],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002153833,0.0000067437363,0.99410146,0.0000058658566,0.000010607693,0.000016432416,0.000055539233,0.0013084317,0.0028137444,0.000060285307,0.000019849236,0.0015989023],"study_design_scores_gemma":[0.00010985036,0.000050340906,0.9904837,0.000032466287,0.000022122233,0.00018994448,0.0002348257,0.00059517584,0.0056114574,0.00222245,0.00036748778,0.00008020298],"about_ca_topic_score_codex":0.017627832,"about_ca_topic_score_gemma":0.46352914,"teacher_disagreement_score":0.4459013,"about_ca_system_score_codex":0.0000031272548,"about_ca_system_score_gemma":0.00063094706,"threshold_uncertainty_score":0.9980802},"labels":[],"label_agreement":null},{"id":"W3216042331","doi":"10.1139/cjes-2020-0209","title":"There is more Wrangellia — magnetic characterization of southern Alaska crust","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Terrane; Geology; Crust; Bay; Volcano; Island arc; Cretaceous; Volcanic arc; Seismology; Earth science; Paleontology; Oceanography; Tectonics; Subduction","score_opus":0.014149245832087879,"score_gpt":0.18247193006335402,"score_spread":0.16832268423126615,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3216042331","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933505,0.0016944066,0.000012134224,0.0022193817,0.000119776494,0.000020024117,0.00013535554,0.0000015922535,0.0024468314],"genre_scores_gemma":[0.99846536,0.00006398581,0.0002870754,0.0005166473,0.00007026176,4.493936e-8,0.000011991814,8.7139097e-7,0.0005837659],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990528,0.000045301054,0.0002704002,0.0001325265,0.0002576892,0.00024126742],"domain_scores_gemma":[0.9991536,0.000039687697,0.00016710481,0.00007615579,0.00019856427,0.0003648714],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024306832,0.00007747717,0.00018369257,0.00011213754,0.00014145808,0.00006696325,0.00026484925,0.000043351654,0.041292682],"category_scores_gemma":[0.00007927617,0.00005178582,0.00010760978,0.0006117016,0.00038619706,0.00012494312,0.00000397646,0.00009872196,0.00009650281],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000028873524,0.000004655031,0.9916864,0.0000059327485,0.000009867411,0.000060251798,0.00031636623,0.00020103139,0.0018607929,0.0000084096355,0.000031662476,0.0058117257],"study_design_scores_gemma":[0.00008777845,0.00014650033,0.9896212,0.000032832617,0.000026900425,0.000053948857,0.00083567866,0.0007442509,0.003557581,0.0011408721,0.0036561256,0.00009629895],"about_ca_topic_score_codex":0.0058970405,"about_ca_topic_score_gemma":0.09266047,"teacher_disagreement_score":0.086763434,"about_ca_system_score_codex":5.3709687e-7,"about_ca_system_score_gemma":0.00048087913,"threshold_uncertainty_score":0.9595837},"labels":[],"label_agreement":null},{"id":"W4200051464","doi":"10.1139/cjes-2021-0073","title":"Characterization of Lower and Middle Pleistocene tephra beds in the southern plains of western Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Lethbridge; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Tephra; Geology; Hornblende; Trace element; Plagioclase; Rhyolite; Geochemistry; Pleistocene; Provenance; Tephrochronology; Biotite; Paleontology; Fission track dating; Zircon; Volcano; Quartz; Volcanic rock","score_opus":0.025044479139550196,"score_gpt":0.20907970559349742,"score_spread":0.18403522645394724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200051464","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975964,0.00052661856,0.0000019870386,0.0009787626,0.0001517594,0.000034429908,0.000059823735,2.4598376e-7,0.0006500167],"genre_scores_gemma":[0.9996645,0.000026904165,0.000034055603,0.00017961125,0.000018262728,6.9584296e-8,0.000004751981,5.6308045e-7,0.00007127404],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991402,0.00014833495,0.00023097,0.000078044315,0.00019578048,0.000206653],"domain_scores_gemma":[0.9994147,0.00015248216,0.00013906106,0.000062929656,0.00009542201,0.00013541947],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007427904,0.000048245805,0.00014653166,0.00013219344,0.00012105671,0.000020261188,0.00023564084,0.00003736948,0.00030566193],"category_scores_gemma":[0.00010155072,0.000032477994,0.000019060994,0.00033605512,0.00050141016,0.000101406236,0.0000032768335,0.00013018094,0.0000017426863],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000081046355,0.0000027022234,0.9988678,0.000010040141,0.0000042807505,0.00013901181,0.0006929166,0.00007523566,0.00004443595,0.000023244005,0.0000028220638,0.00012938971],"study_design_scores_gemma":[0.00010162279,0.00013012647,0.9977106,0.00003899033,0.0000038523017,0.00026692016,0.0010324765,0.00008577869,0.00018001109,0.000073023635,0.00034218738,0.000034446584],"about_ca_topic_score_codex":0.29370034,"about_ca_topic_score_gemma":0.99845105,"teacher_disagreement_score":0.7047507,"about_ca_system_score_codex":3.8803282e-7,"about_ca_system_score_gemma":0.0027059605,"threshold_uncertainty_score":0.71100295},"labels":[],"label_agreement":null},{"id":"W4200301553","doi":"10.1139/cjes-2020-0142","title":"Regional geology and tectonic framework of the Southern Indian domain, Trans-Hudson orogen, Manitoba","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Air Canada; Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Geology; Geochemistry; Felsic; Volcanic rock; Basement; Foreland basin; Mafic; Craton; Paleontology; Volcano; Structural basin; Tectonics; Archaeology","score_opus":0.014192822468605397,"score_gpt":0.18479289029659807,"score_spread":0.17060006782799267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200301553","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.989416,0.0038979258,0.000020573752,0.005705125,0.00015021626,0.000026027285,0.000022063974,0.0000012959537,0.000760775],"genre_scores_gemma":[0.9978565,0.000059805818,0.0012623883,0.00070781243,0.00007275802,7.280563e-8,0.0000014997511,8.115132e-7,0.000038333703],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99891746,0.000108491506,0.00025883387,0.0001556859,0.00025227945,0.00030725152],"domain_scores_gemma":[0.99909306,0.00015667638,0.00015789374,0.0000950643,0.000119605225,0.00037772604],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041279828,0.00008494252,0.00019800845,0.000099888406,0.0003053737,0.00004786293,0.00037709763,0.000079789024,0.004538873],"category_scores_gemma":[0.00017249514,0.000048125254,0.0001269499,0.00064290664,0.0011196057,0.000079041936,0.0000072832318,0.00023687593,0.000010953632],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000036459126,0.000004109556,0.9967993,0.0000049361106,0.000020069498,0.00006850352,0.00046137624,0.0003355606,0.00009142707,0.00032228942,0.00002213242,0.0018666432],"study_design_scores_gemma":[0.00011263664,0.00013691568,0.91965663,0.00004825336,0.000025045767,0.0005264007,0.0034205571,0.00006594788,0.0004521852,0.07235218,0.0030977086,0.00010550616],"about_ca_topic_score_codex":0.01888755,"about_ca_topic_score_gemma":0.7308778,"teacher_disagreement_score":0.71199024,"about_ca_system_score_codex":9.599108e-7,"about_ca_system_score_gemma":0.0007255645,"threshold_uncertainty_score":0.9963711},"labels":[],"label_agreement":null},{"id":"W4205846716","doi":"10.1139/cjes-2019-0105","title":"New age constraints on magmatism and metamorphism in the Morin terrane (Grenville Province, Quebec)","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Terrane; Metamorphism; Geology; Zircon; Orogeny; Geochemistry; Laurentia; Granulite; Massif; Craton; Shear zone; Titanite; Metamorphic rock; Paleontology; Facies; Ordovician; Tectonics","score_opus":0.01867882266231591,"score_gpt":0.18925878018539988,"score_spread":0.17057995752308397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205846716","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98152494,0.0009317944,0.0000061348924,0.0059228507,0.0001438634,0.000067954825,0.000023289576,0.000001359018,0.011377826],"genre_scores_gemma":[0.9980205,0.000011254668,0.00043306046,0.0011089784,0.00004694383,2.6940597e-7,0.0000026345579,5.6480775e-7,0.00037576025],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988306,0.00014532164,0.00022587656,0.00014714533,0.0003620504,0.0002889983],"domain_scores_gemma":[0.9993184,0.00014730857,0.000107435895,0.00006804336,0.0000123592135,0.00034642158],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009663809,0.00008290034,0.0001641784,0.00023227108,0.00039469346,0.00011612147,0.00047075865,0.000018142497,0.016182575],"category_scores_gemma":[0.00008010168,0.000046899346,0.00005613906,0.0004978301,0.0005365187,0.0001047036,0.000008414306,0.0002740491,0.000013952113],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021203812,0.000019616915,0.780575,0.000006153307,0.000026167832,0.0019901134,0.0012327447,0.009915413,0.000068031324,0.002387501,0.0018999777,0.20185813],"study_design_scores_gemma":[0.00017845425,0.00036555057,0.9776579,0.000010115187,0.000012189246,0.00025741837,0.0010162824,0.00037541953,0.000014227454,0.0074109486,0.012602012,0.00009947376],"about_ca_topic_score_codex":0.19991755,"about_ca_topic_score_gemma":0.9187667,"teacher_disagreement_score":0.7188491,"about_ca_system_score_codex":0.0000019992303,"about_ca_system_score_gemma":0.000618175,"threshold_uncertainty_score":0.9847168},"labels":[],"label_agreement":null},{"id":"W4206647781","doi":"10.1139/e10-902","title":"Note of Appreciation / Note de Reconnaissance","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Legal case studies and regulations","field":"Social Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology","score_opus":0.026585253626558957,"score_gpt":0.3033841003693746,"score_spread":0.27679884674281563,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206647781","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92450875,0.00030216662,0.0003250658,0.007696517,0.0020459308,0.00006878867,0.000008175852,0.0000033686983,0.06504122],"genre_scores_gemma":[0.99629873,0.000024480021,0.0028135634,0.00008509504,0.00042115536,2.6841286e-7,8.7651046e-8,0.0000016695878,0.00035492223],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99921066,0.000051063485,0.00019307039,0.00006547016,0.00023028844,0.0002494676],"domain_scores_gemma":[0.999062,0.000096848395,0.00021621928,0.000051780993,0.00025024114,0.00032293485],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015729473,0.00004002753,0.0000981718,0.0001540256,0.00085414556,0.000067612076,0.00024186606,0.000050374645,0.00016753012],"category_scores_gemma":[0.0007562644,0.000032740147,0.00005983003,0.00041229176,0.0011574362,0.00030346002,0.0000044661624,0.00014669837,0.0000027754745],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017987695,0.00004342794,0.5436374,0.000026012718,0.000042999738,0.000070277376,0.11999391,0.0019926876,0.0074682026,0.22809139,0.0060197664,0.09259597],"study_design_scores_gemma":[0.0002787739,0.0002020846,0.33546162,0.00008473763,0.000026310774,0.0000421759,0.0061085317,0.00038641662,0.0013979293,0.010148952,0.64564216,0.00022032385],"about_ca_topic_score_codex":0.026316147,"about_ca_topic_score_gemma":0.8289981,"teacher_disagreement_score":0.802682,"about_ca_system_score_codex":0.000010915379,"about_ca_system_score_gemma":0.0036301333,"threshold_uncertainty_score":0.9801677},"labels":[],"label_agreement":null},{"id":"W4210259318","doi":"10.1139/cjes-2021-0100","title":"Constraints on the age of <i>Archaeozoon acadiense</i> and evidence for hydrothermally transported zircon in the Ashburn Formation (Green Head Group), Saint John, New Brunswick, Canada","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Nova Scotia Department of Energy; Acadia University; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Zircon; Geology; Precambrian; Geochemistry; Paleozoic; Stromatolite; Proterozoic; Archean; Paleontology; Carbonate","score_opus":0.04330937948923237,"score_gpt":0.2173376872913722,"score_spread":0.17402830780213985,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210259318","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9850085,0.0011905043,0.000084150124,0.013126841,0.00006483658,0.00017446664,0.000040835763,9.017711e-7,0.00030896376],"genre_scores_gemma":[0.9973989,0.00003457018,0.00015644879,0.0023544081,0.000031137883,5.8564933e-7,0.0000060619664,7.9942447e-7,0.000017067141],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99866533,0.00015761016,0.00033922202,0.00012733976,0.00040974253,0.0003007671],"domain_scores_gemma":[0.9988546,0.0006319816,0.0001877491,0.0000749015,0.00003795447,0.00021283356],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017058707,0.00008697305,0.00016865434,0.000114238195,0.00039935205,0.00003698879,0.0005389696,0.000020847536,0.00097357674],"category_scores_gemma":[0.00012851834,0.000046187855,0.000068522364,0.0004786557,0.0005494668,0.00016067518,0.0000046386886,0.00023572192,5.0107894e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016873128,0.000018270042,0.91995203,0.000037026613,0.000037256767,0.0002494763,0.004238544,0.021163587,0.0008795521,0.003121261,0.00040417208,0.049730103],"study_design_scores_gemma":[0.00033630137,0.0009261586,0.9793816,0.00008175597,0.000021825852,0.00014249972,0.0020508359,0.0026291187,0.00016929208,0.004360727,0.009764359,0.00013549768],"about_ca_topic_score_codex":0.9079775,"about_ca_topic_score_gemma":0.9989781,"teacher_disagreement_score":0.09100054,"about_ca_system_score_codex":0.0000066192806,"about_ca_system_score_gemma":0.001626377,"threshold_uncertainty_score":0.9999397},"labels":[],"label_agreement":null},{"id":"W4210582363","doi":"10.1139/cjes-2021-0109","title":"Accessory phase perspectives for ore-forming processes and magmatic sulphide exploration in the Labrador Trough, northern Quebec, Canada","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Nortel (Canada); Natural Resources Canada; Université du Québec à Chicoutimi; Carleton University","funders":"Natural Environment Research Council","keywords":"Geology; Geochemistry; Mafic; Ilmenite; Ultramafic rock; Apatite; Olivine; Mineral redox buffer; Chromite; Pyrrhotite; Mineralogy; Sill; Pyrite; Mantle (geology)","score_opus":0.0259215897435951,"score_gpt":0.22590474653759207,"score_spread":0.19998315679399697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210582363","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99051404,0.0023684553,0.000020139749,0.0066780644,0.00006531653,0.00010117714,0.000046495683,0.0000012086472,0.0002051022],"genre_scores_gemma":[0.9993345,0.000017811748,0.0001316252,0.00040174843,0.000050817784,0.0000026314358,0.0000070914944,7.923675e-7,0.000052974854],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999021,0.000078207726,0.0002216647,0.00013293276,0.0002872226,0.0002590026],"domain_scores_gemma":[0.9992529,0.00028886698,0.00014709834,0.000045267185,0.00009519498,0.0001706606],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006886158,0.00007461842,0.00013841214,0.00014131589,0.00065562624,0.00013381738,0.00038207968,0.000011554836,0.0009392367],"category_scores_gemma":[0.00039074972,0.000044359156,0.000030593626,0.000678965,0.00020620978,0.00044724302,0.0000053640856,0.00013166941,4.8369225e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008434001,0.0000505239,0.9219947,0.00007766626,0.00003839648,0.00020615589,0.016329344,0.021875603,0.00004272686,0.00027964683,0.000576522,0.038444415],"study_design_scores_gemma":[0.0017618277,0.0016539715,0.64078355,0.00006610422,0.00010390791,0.0002831187,0.29577124,0.0124166915,0.00023852769,0.029228607,0.017054025,0.0006383926],"about_ca_topic_score_codex":0.89591986,"about_ca_topic_score_gemma":0.9998665,"teacher_disagreement_score":0.28121108,"about_ca_system_score_codex":0.0000065496624,"about_ca_system_score_gemma":0.0021409276,"threshold_uncertainty_score":0.999974},"labels":[],"label_agreement":null},{"id":"W4210745606","doi":"10.1139/cjes-2021-0092","title":"New Mesozoic research inspired by the life and work of Dale A. Russell","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta; Canadian Museum of Nature","funders":"","keywords":"Mesozoic; Geology; Work (physics); Paleontology; Engineering","score_opus":0.0569876597037647,"score_gpt":0.2464947241385786,"score_spread":0.18950706443481388,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210745606","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96326655,0.02171593,0.000004919144,0.008562768,0.00018051955,0.000034829132,0.0000114777085,0.0000010962353,0.006221925],"genre_scores_gemma":[0.9978529,0.00018255452,0.00027124645,0.00030239075,0.00010215164,5.510882e-8,7.2112215e-7,5.496878e-7,0.0012873883],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886125,0.00013540463,0.00019162949,0.0001220452,0.00035987602,0.00032981276],"domain_scores_gemma":[0.9987009,0.00040271174,0.00007687927,0.00006680043,0.00014965358,0.00060303917],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008944402,0.000059091286,0.00015543148,0.000066271634,0.00052188855,0.000106741776,0.00032201313,0.000028676399,0.0014131147],"category_scores_gemma":[0.0005261062,0.000031173447,0.000041773987,0.0009252522,0.0009912399,0.00012366228,0.0000130020435,0.00019528187,0.000038342412],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007859694,0.000004562909,0.9608617,0.0000045879506,0.000017887334,0.000035557037,0.0004215999,0.00021674603,0.000019268935,0.00024850745,0.006903015,0.031258717],"study_design_scores_gemma":[0.0000942386,0.00026212976,0.94952697,0.000022927197,0.0000057672714,0.00002028999,0.00070409535,0.000025478672,0.00012462014,0.00381724,0.045341272,0.000054991695],"about_ca_topic_score_codex":0.021169888,"about_ca_topic_score_gemma":0.157909,"teacher_disagreement_score":0.13673912,"about_ca_system_score_codex":4.564302e-7,"about_ca_system_score_gemma":0.0010489102,"threshold_uncertainty_score":0.99949974},"labels":[],"label_agreement":null},{"id":"W4212946711","doi":"10.1139/cjes-2021-0049","title":"Biostratigraphic evidence for incremental tectonic development of early Cambrian deep-water environments in the Misty Creek embayment (Selwyn basin, Northwest Territories, Canada)","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Laurentian University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Aurora Research Institute","keywords":"Diachronous; Geology; Laurentia; Paleontology; Structural basin; Sedimentary depositional environment; Subsidence; Tectonics; Stage (stratigraphy)","score_opus":0.030280254497821655,"score_gpt":0.21831358250472538,"score_spread":0.18803332800690373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4212946711","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958345,0.002500857,0.000012721101,0.00046767519,0.00044375533,0.00021498628,0.00013712431,8.676192e-7,0.0003875025],"genre_scores_gemma":[0.9990538,0.000010283769,0.0007433137,0.00013472016,0.00003616301,0.0000040501714,0.000009165294,8.143982e-7,0.000007714717],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979253,0.00019052094,0.0005244643,0.00019808723,0.000663411,0.0004982259],"domain_scores_gemma":[0.9991935,0.00016966906,0.00022878936,0.000112472575,0.00002701459,0.00026853633],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018459178,0.00012576407,0.00020157483,0.00024233405,0.0012116955,0.00008450746,0.0007982378,0.00003124248,0.00026255418],"category_scores_gemma":[0.000040470764,0.000089304,0.00007187236,0.00034292863,0.00048937974,0.0002855441,0.0000030679266,0.00021931056,2.5333688e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026114107,0.0000089348805,0.9942003,0.000006395829,0.000018302728,0.000059666265,0.0013497105,0.0001491391,0.0000727005,0.000011559433,0.000020203412,0.0040770033],"study_design_scores_gemma":[0.00022125439,0.00058798085,0.9931029,0.0000287858,0.000011558836,0.00007850499,0.0020421015,0.00004413883,0.0003187655,0.00004318889,0.003400987,0.00011983431],"about_ca_topic_score_codex":0.8555006,"about_ca_topic_score_gemma":0.99969983,"teacher_disagreement_score":0.14419925,"about_ca_system_score_codex":0.000013615523,"about_ca_system_score_gemma":0.0041005295,"threshold_uncertainty_score":0.93195045},"labels":[],"label_agreement":null},{"id":"W4213063325","doi":"10.1139/cjes-2019-0125","title":"Magmatic and metallogenic processes associated with large igneous provinces","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Igneous rock; Geochemistry; Petrology; Earth science","score_opus":0.008170149834732266,"score_gpt":0.168134566314845,"score_spread":0.15996441648011273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213063325","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99201494,0.0024113264,0.000005061322,0.00039075786,0.00005443791,0.00006482847,0.000020094514,0.0000039224515,0.0050346428],"genre_scores_gemma":[0.99916595,0.000025079946,0.0003056887,0.000225585,0.000020553147,1.2011222e-7,0.0000036734057,9.0766815e-7,0.0002524178],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989487,0.000046132274,0.00020138524,0.00015905313,0.00027390424,0.00037085946],"domain_scores_gemma":[0.99901754,0.00017888355,0.00018287517,0.00004983108,0.00014250733,0.00042835786],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005702225,0.00009692143,0.00022597298,0.00015401795,0.00021042563,0.0001385735,0.00027063844,0.00003522574,0.004985209],"category_scores_gemma":[0.0003482044,0.000052649022,0.000041298452,0.00063375203,0.00032519558,0.0002903019,0.000004252734,0.00011256707,0.000042187563],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004337593,0.0000046929845,0.9988469,0.000012820959,0.000028670273,0.000040822393,0.00009293066,0.00046501847,0.000016058766,0.00003031948,0.000009252892,0.0004481627],"study_design_scores_gemma":[0.00027178592,0.0010309404,0.9914821,0.000092958326,0.0000678654,0.00018837725,0.00079835736,0.0015452795,0.000120704746,0.0033493484,0.00085626805,0.00019601072],"about_ca_topic_score_codex":0.003776701,"about_ca_topic_score_gemma":0.6449396,"teacher_disagreement_score":0.6411629,"about_ca_system_score_codex":9.072092e-7,"about_ca_system_score_gemma":0.0007923977,"threshold_uncertainty_score":0.99592435},"labels":[],"label_agreement":null},{"id":"W4213363176","doi":"10.1139/cjes-2021-0059","title":"Petrography, chemical composition, and age constraints of mafic intrusions from the Mesoproterozoic Soisson Intrusive Suite in the southeastern Churchill Province (Canada)","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Makivik Corporation; Geological Survey of Canada","funders":"","keywords":"Geology; Gabbro; Geochemistry; Petrography; Mafic; Layered intrusion; Olivine; Plagioclase; Anorthosite; Basalt; Intrusion; Paleontology","score_opus":0.010431938949757032,"score_gpt":0.17632990674869864,"score_spread":0.16589796779894161,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213363176","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923043,0.0007553705,0.0000038325693,0.0060653733,0.00007594939,0.00009867537,0.00024344432,9.636946e-7,0.00045205603],"genre_scores_gemma":[0.99891216,0.0000071521135,0.00012634149,0.0008912111,0.00004396382,6.512013e-7,0.000014073973,7.115684e-7,0.000003723585],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986075,0.00021282931,0.00029683576,0.00015332848,0.00045878685,0.00027073186],"domain_scores_gemma":[0.9991026,0.00035782898,0.00018692308,0.00009070182,0.00004243545,0.00021950353],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007092716,0.000089078174,0.00018365782,0.00010400989,0.00048114767,0.00007369088,0.0006796775,0.000019442119,0.0021816664],"category_scores_gemma":[0.00008614419,0.00004670795,0.00006581104,0.0005261614,0.0013104444,0.00007354372,0.000023142971,0.00032944194,9.040369e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012030442,0.00000778585,0.99565256,0.0000020509603,0.000014108643,0.0001061198,0.0007412295,0.0005713604,0.00022286647,0.00012041772,0.00005641784,0.0024930683],"study_design_scores_gemma":[0.00016083405,0.0001341203,0.9899544,0.000019532059,0.000021644755,0.00011907941,0.0041957884,0.00050192187,0.00009295216,0.0040567336,0.0006537172,0.000089237605],"about_ca_topic_score_codex":0.5097292,"about_ca_topic_score_gemma":0.9596522,"teacher_disagreement_score":0.449923,"about_ca_system_score_codex":0.0000021077958,"about_ca_system_score_gemma":0.0007409704,"threshold_uncertainty_score":0.9987305},"labels":[],"label_agreement":null},{"id":"W4213425164","doi":"10.1139/cjes-2022-0015","title":"Reply to the discussion by van Staal et al. on “The northern Appalachian terrane wreck model”","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Martec (Canada)","funders":"","keywords":"Geology; Terrane; Geochemistry; Geomorphology; Archaeology; Seismology; Tectonics; History","score_opus":0.026340557499726226,"score_gpt":0.22217545225373245,"score_spread":0.19583489475400623,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213425164","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.69311935,0.0009475508,0.000061855506,0.29219955,0.0008104345,0.00021615562,0.0002237813,0.0000073197207,0.012414023],"genre_scores_gemma":[0.96138465,0.000021287424,0.00008540196,0.03738642,0.000053800017,0.0000013990905,0.000003910081,0.0000030328126,0.0010600646],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981704,0.00022753718,0.00026362084,0.00021651441,0.0006758335,0.00044614152],"domain_scores_gemma":[0.99903244,0.0001648666,0.0001565232,0.00019823063,0.000046259443,0.00040169375],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0022499086,0.00012648122,0.00014901612,0.00016296798,0.0023607642,0.00018470305,0.0008667213,0.000012157287,0.0021019706],"category_scores_gemma":[0.0001418089,0.00005433688,0.00008927358,0.0005507838,0.00028808785,0.00015997731,0.000020346335,0.00039162327,0.00005810614],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006137586,0.000021028192,0.39736676,0.0000025426532,0.00005175053,0.000081409,0.0076092337,0.31495118,0.000018274459,0.00036880362,0.23128219,0.048185457],"study_design_scores_gemma":[0.0001573421,0.001167568,0.1016726,0.00002471938,0.0000104512355,0.0000924664,0.0044666547,0.0059573036,0.000014654182,0.00071661966,0.88552934,0.00019027741],"about_ca_topic_score_codex":0.014689194,"about_ca_topic_score_gemma":0.5112318,"teacher_disagreement_score":0.65424716,"about_ca_system_score_codex":0.0000048224715,"about_ca_system_score_gemma":0.0009442313,"threshold_uncertainty_score":0.998938},"labels":[],"label_agreement":null},{"id":"W4213443330","doi":"10.1139/cjes-2021-0117","title":"Permafrost thaw sensitivity prediction using surficial geology, topography, and remote-sensing imagery: a data-driven neural network approach","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada; Nunavut Arctic College","keywords":"Permafrost; Geology; Sensitivity (control systems); Terrain; Remote sensing; Cartography; Geography","score_opus":0.07255783072271008,"score_gpt":0.247212891215428,"score_spread":0.17465506049271792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213443330","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99182993,0.0013086336,0.00015681966,0.00040280915,0.0013385647,0.00009650572,0.0041722194,0.0000065171726,0.0006880128],"genre_scores_gemma":[0.9955287,0.000043208995,0.0028991569,0.00039612316,0.00068739476,1.8038943e-8,0.00043329629,0.0000036201284,0.000008471278],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9982133,0.000334347,0.0002782684,0.00029912274,0.00033109312,0.0005438953],"domain_scores_gemma":[0.99898666,0.00014807978,0.00020299056,0.00016429642,0.00006408399,0.00043385927],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0019420994,0.00013104967,0.00023291033,0.00030264442,0.0017896185,0.00023632293,0.0003043034,0.000041823227,0.00068764726],"category_scores_gemma":[0.000050738014,0.000117031545,0.000058013287,0.0006644838,0.0006965433,0.00059281074,0.00005131506,0.00034789645,0.0000012943226],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017912993,0.000002339594,0.93917215,0.000005173703,0.000011454165,0.00024411279,0.00041515994,0.055463463,0.00007199243,0.0000052015525,0.00041228143,0.0041787736],"study_design_scores_gemma":[0.00009940595,0.00014074947,0.43333918,0.0000101382575,0.000021240125,0.0023630983,0.0012988738,0.5614509,9.922117e-7,0.00007941831,0.0010888696,0.000107170956],"about_ca_topic_score_codex":0.08576041,"about_ca_topic_score_gemma":0.56819576,"teacher_disagreement_score":0.5059874,"about_ca_system_score_codex":0.0000032858304,"about_ca_system_score_gemma":0.000596571,"threshold_uncertainty_score":0.99950993},"labels":[],"label_agreement":null},{"id":"W4214610292","doi":"10.1139/e11-052","title":"Introduction to the E.R. Ward Neale Memorial Issue","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Contemporary Sociological Theory and Practice","field":"Social Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Memorial University of Newfoundland","keywords":"Geology; Geochemistry","score_opus":0.06399939555666613,"score_gpt":0.3251035489128531,"score_spread":0.261104153356187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4214610292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.48310837,0.0021923294,0.00014576355,0.37901062,0.021900019,0.0002445078,0.000005327645,0.0000108692575,0.11338219],"genre_scores_gemma":[0.97541034,0.00002650997,0.0002760065,0.0014749022,0.020227348,7.006376e-7,1.2575791e-7,0.0000016022544,0.0025824776],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984838,0.00061053777,0.00017113295,0.00007876485,0.00027357708,0.0003822288],"domain_scores_gemma":[0.99860495,0.0003335896,0.0001348537,0.0000746822,0.00011513207,0.0007367828],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.008633276,0.000050597966,0.00009549423,0.00008719861,0.0016117602,0.00017337714,0.0004590268,0.000045924946,0.0026052897],"category_scores_gemma":[0.002983746,0.000031467687,0.000056091256,0.00050139596,0.0006951027,0.0009752508,0.000009136333,0.00019302565,0.00020348148],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012082931,0.000051503066,0.082357146,0.000005019124,0.00005994344,0.000034084507,0.18861635,0.0005554936,0.00015845305,0.3129561,0.3635128,0.051572263],"study_design_scores_gemma":[0.000034916622,0.00009878166,0.0042957366,0.0000032476344,0.000005760747,0.000011121488,0.009596561,8.0869734e-7,0.000030887386,0.0013057434,0.9845672,0.00004919066],"about_ca_topic_score_codex":0.006704345,"about_ca_topic_score_gemma":0.04911002,"teacher_disagreement_score":0.6210544,"about_ca_system_score_codex":0.000011730596,"about_ca_system_score_gemma":0.0011285124,"threshold_uncertainty_score":0.9999101},"labels":[],"label_agreement":null},{"id":"W4220669009","doi":"10.1139/cjes-2021-0126","title":"Meighen Ice Cap: changes in geometry, mass, and climatic response since 1959","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Natural Resources Canada; National Aeronautics and Space Administration","keywords":"Geology; Ice caps; Climatology; Altitude (triangle); Atmospheric sciences; Geomorphology; Glacier; Geometry","score_opus":0.032275907690356764,"score_gpt":0.21960752786037918,"score_spread":0.18733162017002242,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220669009","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9869642,0.0057236874,0.00000674631,0.006229302,0.00043521967,0.00006186824,0.00005276732,0.000002065308,0.000524098],"genre_scores_gemma":[0.9980945,0.00012925666,0.00092841743,0.00063812843,0.000048511814,5.5448845e-7,0.0000013377199,0.0000013503051,0.0001579714],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99893713,0.00013370391,0.00021150787,0.00013087528,0.00025604147,0.00033075197],"domain_scores_gemma":[0.99914885,0.00033806148,0.00013226183,0.00006406738,0.000037990594,0.00027878972],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017959664,0.000072832205,0.00014931959,0.0002804688,0.00081353297,0.00009977797,0.00029277982,0.000015077651,0.001808545],"category_scores_gemma":[0.00025268274,0.0000612602,0.000024294972,0.0010523957,0.0002773777,0.00018847077,0.00001111324,0.00016084331,0.0000048457905],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022029943,0.000002434299,0.99060076,0.000004145775,0.00000482562,0.00008345089,0.0008625883,0.005147346,0.000014423567,0.00006720915,0.00023220589,0.0029585836],"study_design_scores_gemma":[0.00013508175,0.00039912897,0.9465032,0.000014298005,0.0000050053545,0.00007853425,0.0042918124,0.0016145533,0.0000032056043,0.00026745477,0.04660285,0.00008485981],"about_ca_topic_score_codex":0.026403762,"about_ca_topic_score_gemma":0.6831769,"teacher_disagreement_score":0.6567731,"about_ca_system_score_codex":0.0000054401576,"about_ca_system_score_gemma":0.0006634391,"threshold_uncertainty_score":0.99910396},"labels":[],"label_agreement":null},{"id":"W4220808114","doi":"10.1139/cjes-2020-0150","title":"Nearshore sediment transport as influenced by changing sea ice, north shore of Prince Edward Island, Canada","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Guelph; Geological Survey of Canada","funders":"Natural Resources Canada; Environment and Climate Change Canada; Deltares","keywords":"Sediment transport; Sediment; Oceanography; Sea ice; Geology; Seabed gouging by ice; Shore; Drift ice; Inlet; Arctic ice pack; Hydrology (agriculture); Geomorphology","score_opus":0.006088240262097216,"score_gpt":0.18275214091801284,"score_spread":0.1766639006559156,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220808114","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958358,0.00036630564,0.000043696527,0.0009805034,0.00059895485,0.00009476148,0.00054805534,0.0000024266894,0.0015294865],"genre_scores_gemma":[0.9985486,0.000022936592,0.000218154,0.0008705743,0.0000598738,4.033722e-7,0.00003726241,0.0000029845946,0.00023918322],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979621,0.000060958613,0.000398295,0.00018586068,0.00082396006,0.0005688185],"domain_scores_gemma":[0.9988285,0.00008508488,0.00028319354,0.00010357015,0.00009540925,0.0006042608],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007138988,0.00013233315,0.00023452412,0.00024888926,0.0007923845,0.000034128017,0.00063739147,0.000023213102,0.0024385187],"category_scores_gemma":[0.000042729487,0.00011241476,0.000072023955,0.0008005201,0.00034303963,0.0002675646,0.000010401274,0.00029292502,0.0000027295807],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012652162,0.0000038986827,0.9638468,0.000009454925,0.000016742135,0.00014921757,0.0012560159,0.032611437,0.0000040132563,0.000019976678,0.00030686668,0.0017629475],"study_design_scores_gemma":[0.00044227377,0.0010621697,0.90297467,0.000068527144,0.00005262205,0.00045826065,0.012870907,0.006608574,0.00007468728,0.00012464421,0.07482721,0.00043547823],"about_ca_topic_score_codex":0.74446905,"about_ca_topic_score_gemma":0.99083084,"teacher_disagreement_score":0.2463618,"about_ca_system_score_codex":0.00001580155,"about_ca_system_score_gemma":0.007541341,"threshold_uncertainty_score":0.9984734},"labels":[],"label_agreement":null},{"id":"W4220884053","doi":"10.1139/cjes-2021-0097","title":"The age and origin of the South Mountain Batholith (Nova Scotia, Canada) as constrained by zircon U–Pb geochronology, geochemistry, and O–Hf isotopes","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; University of Windsor; St. Francis Xavier University; Geological Survey of Canada; University of Alberta; Laurentian University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Zircon; Batholith; Geology; Terrane; Geochronology; Geochemistry; Nova scotia; Mantle (geology); Paleontology; Oceanography; Tectonics","score_opus":0.009981979035656056,"score_gpt":0.18498263825923783,"score_spread":0.17500065922358177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220884053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9889793,0.003152079,0.0000023377625,0.004840387,0.0001522976,0.00005604074,0.00017659155,0.0000011874041,0.0026398043],"genre_scores_gemma":[0.99895084,0.000021666814,0.00007542342,0.0006859736,0.000026863889,1.8808079e-7,0.0000038128408,8.4075094e-7,0.00023437267],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873513,0.00010906585,0.0002654883,0.00017435888,0.0003534709,0.00036248247],"domain_scores_gemma":[0.9991131,0.00020204717,0.00021575348,0.0000985565,0.000057775498,0.0003127555],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00075540936,0.000104402425,0.0001917282,0.000049671555,0.0009112056,0.00009499657,0.00051740836,0.000026363063,0.0027430058],"category_scores_gemma":[0.00022861002,0.00005593948,0.0000495581,0.00035191525,0.0021575328,0.00007939462,0.000030870062,0.0002601903,9.683198e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012871036,0.0000036660779,0.9943464,0.0000072396015,0.000034668577,0.000086782995,0.00024459473,0.00073393516,0.0010417948,0.00026988992,0.00096340274,0.0022547902],"study_design_scores_gemma":[0.00061856204,0.0007019637,0.9070604,0.000037285394,0.00009786993,0.0011366678,0.010528905,0.0015917927,0.0042842785,0.0114609245,0.06204154,0.00043979994],"about_ca_topic_score_codex":0.8106297,"about_ca_topic_score_gemma":0.98226,"teacher_disagreement_score":0.17163022,"about_ca_system_score_codex":0.000004467148,"about_ca_system_score_gemma":0.0019122311,"threshold_uncertainty_score":0.99816865},"labels":[],"label_agreement":null},{"id":"W4220901352","doi":"10.1139/cjes-2021-0040","title":"A new plastomenid trionychid (Testudines: Pan-Trionychidae) from Milk River Formation of southern Alberta (Cretaceous: Santonian)","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Ontario Museum; Royal Tyrrell Museum; Carleton University; University of Toronto","funders":"","keywords":"Paleontology; Cretaceous; Carapace; Geology; Sister group; Taxon; Clade; Reef; Phylogenetic tree; Zoology; Biology; Crustacean","score_opus":0.014599752978029693,"score_gpt":0.19819306339466827,"score_spread":0.18359331041663857,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220901352","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98935354,0.0054963813,0.0001338904,0.0009616521,0.0009241588,0.000085285064,0.00042246448,0.0000035643686,0.0026190532],"genre_scores_gemma":[0.9982096,0.00004604344,0.001055294,0.00017123326,0.00014064844,3.448368e-7,0.000024263518,0.0000016389685,0.00035096565],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99847955,0.00020674226,0.00045806888,0.00017586662,0.00030851742,0.0003712457],"domain_scores_gemma":[0.99867123,0.0003411976,0.0004304022,0.00009910678,0.0000657695,0.00039230444],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005820148,0.00012169121,0.0002694969,0.000400585,0.00073957426,0.00002621198,0.00056135346,0.000057518624,0.008084883],"category_scores_gemma":[0.0001452759,0.00009706521,0.00010738741,0.00052448513,0.0004869185,0.00037834028,0.000010274121,0.00023320023,0.00009503154],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010119488,0.0000074137156,0.98248756,0.0000026816576,0.00003423213,0.000038197322,0.003459687,0.00490495,0.00004301393,0.000032391654,0.0009936441,0.007895044],"study_design_scores_gemma":[0.00067480304,0.0010484948,0.956327,0.000024687663,0.000043705506,0.0005044605,0.004182904,0.002610984,0.000041521867,0.0019950399,0.032341648,0.00020472484],"about_ca_topic_score_codex":0.11835391,"about_ca_topic_score_gemma":0.7708196,"teacher_disagreement_score":0.6524657,"about_ca_system_score_codex":0.0000057300836,"about_ca_system_score_gemma":0.0017913015,"threshold_uncertainty_score":0.9928219},"labels":[],"label_agreement":null},{"id":"W4220933097","doi":"10.1139/cjes-2021-0108","title":"Sedimentary mercury as a proxy for redox oscillations during the Cambrian SPICE event in western Newfoundland","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Redox; Spice; Sedimentary rock; Excursion; Sedimentary depositional environment; Glauconite; Outcrop; Paleontology; Oceanography; Chemistry; Structural basin","score_opus":0.017693874332687435,"score_gpt":0.2613616873813864,"score_spread":0.24366781304869894,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220933097","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99352527,0.00018362392,0.000009844923,0.004347263,0.00036120575,0.0002263716,0.000017998453,0.0000016617394,0.0013267474],"genre_scores_gemma":[0.9979816,0.00000805294,0.00010776588,0.00063591666,0.000061773084,0.000012167213,6.4109673e-7,0.0000032106514,0.001188877],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989825,0.00006470591,0.00023886283,0.00011526087,0.00031997942,0.00027871007],"domain_scores_gemma":[0.9995042,0.000063948304,0.00014636228,0.000072216026,0.000012570328,0.00020071273],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00090813235,0.00006730153,0.00009711462,0.00012344444,0.0012283326,0.00006661143,0.0002898311,0.000010070723,0.0007942782],"category_scores_gemma":[0.00007040013,0.000048744623,0.00004892267,0.00042148292,0.00029541686,0.0002881376,0.000043024884,0.00012037891,0.000010128798],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000058674577,0.0000057529564,0.9934683,0.0000018619738,0.0000056862987,0.000013519681,0.0024405739,0.0032040856,0.00030487427,0.00003768542,0.0002447736,0.0002670422],"study_design_scores_gemma":[0.0002569243,0.00018895027,0.95335984,0.000012308373,0.000007848373,0.000152815,0.0027243537,0.0001127966,0.000041574658,0.00025662384,0.042808216,0.00007773837],"about_ca_topic_score_codex":0.0313204,"about_ca_topic_score_gemma":0.46570545,"teacher_disagreement_score":0.43438506,"about_ca_system_score_codex":0.00008265758,"about_ca_system_score_gemma":0.00039408007,"threshold_uncertainty_score":0.97513014},"labels":[],"label_agreement":null},{"id":"W4221071061","doi":"10.1139/cjes-2021-0127","title":"Subsidence drives habitat loss in a large permafrost delta, Mackenzie River outlet to the Beaufort Sea, western Arctic Canada","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; Natural Resources Canada; Geological Survey of Canada; Memorial University of Newfoundland; Dalhousie University","funders":"Office of Energy Research and Development; Natural Resources Canada; Fisheries and Oceans Canada; Environment and Climate Change Canada; Government of Canada; University of Lethbridge; ArcticNet; Aurora Research Institute","keywords":"Geology; Permafrost; Delta; Arctic; Subsidence; Sea level; River delta; Oceanography; Physical geography; Geomorphology; Geography","score_opus":0.025964872998624655,"score_gpt":0.22918742671340053,"score_spread":0.20322255371477588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221071061","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9811876,0.0013535792,0.0000029515552,0.00779223,0.0011865611,0.0001489075,0.008076099,0.0000019201548,0.00025016902],"genre_scores_gemma":[0.99467695,0.000034376073,0.000029865016,0.0048192646,0.00015797933,0.0000015197662,0.00011363166,0.000003617131,0.00016282515],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977643,0.00015132014,0.0003589101,0.00023607367,0.00070132274,0.00078807893],"domain_scores_gemma":[0.9986619,0.00018887395,0.00015550651,0.00016101118,0.00009028944,0.00074244884],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012841169,0.00014873332,0.00021661253,0.0003239425,0.0011435422,0.00018540997,0.0010392198,0.000023300805,0.005959687],"category_scores_gemma":[0.00010135657,0.00010835309,0.00006615412,0.0008946681,0.00031703434,0.00037312653,0.000032742755,0.0003674511,0.000034836776],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009864938,0.0000035273958,0.9885737,0.0000048171623,0.0000048094194,0.0006199692,0.0025910898,0.005827928,0.000002507464,0.000008380301,0.002139478,0.0002139357],"study_design_scores_gemma":[0.00016215374,0.0001891363,0.94412786,0.00003263991,0.0000069124258,0.00038921507,0.0033736387,0.00060568715,0.0000049425466,0.000057512152,0.05089494,0.00015539129],"about_ca_topic_score_codex":0.94648874,"about_ca_topic_score_gemma":0.99996156,"teacher_disagreement_score":0.053472795,"about_ca_system_score_codex":0.000027334187,"about_ca_system_score_gemma":0.0035922143,"threshold_uncertainty_score":0.994949},"labels":[],"label_agreement":null},{"id":"W4221095504","doi":"10.1139/cjes-2021-0042","title":"Structural and geochronological constraints on orogenic gold mineralization in the western Wabigoon subprovince, Canada","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia, Okanagan Campus; Laurentian University","funders":"","keywords":"Geology; Greenstone belt; Sinistral and dextral; Geochemistry; Transpression; Geochronology; Archean; Mineralization (soil science); Population; Paleontology; Tectonics","score_opus":0.01681432741788785,"score_gpt":0.1850735683108994,"score_spread":0.16825924089301156,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221095504","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947343,0.00046995596,4.5885562e-7,0.0029378235,0.00012907524,0.00004324904,0.000039130933,9.813833e-7,0.0016450171],"genre_scores_gemma":[0.99820256,0.000006271941,0.000030497487,0.0016811473,0.000034232093,2.5964147e-7,0.0000074396844,4.2321935e-7,0.000037151745],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989253,0.00012370356,0.00020402644,0.00013759214,0.00033202374,0.00027731413],"domain_scores_gemma":[0.9994849,0.00012994252,0.00009905534,0.000050354694,0.000025406396,0.0002103581],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00050945353,0.00007491421,0.00012765077,0.00011520807,0.00033664852,0.000070671784,0.00038242465,0.000018343451,0.003574963],"category_scores_gemma":[0.00008964258,0.00004128003,0.000031865246,0.00044265023,0.0004466346,0.00008635177,0.00000760293,0.00023334076,0.0000017136196],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000060451484,0.000001834859,0.9856313,0.0000012270756,0.0000035929543,0.00014256075,0.00008369206,0.007583883,0.0000081094395,0.00015721012,0.000120538825,0.006260046],"study_design_scores_gemma":[0.00011667792,0.0002904506,0.99462265,0.00000352139,0.0000050928275,0.00024604573,0.0005706379,0.0010658948,0.000007956594,0.000896666,0.002102998,0.00007143693],"about_ca_topic_score_codex":0.78439134,"about_ca_topic_score_gemma":0.99825126,"teacher_disagreement_score":0.21385992,"about_ca_system_score_codex":0.0000049121545,"about_ca_system_score_gemma":0.0009565033,"threshold_uncertainty_score":0.9973359},"labels":[],"label_agreement":null},{"id":"W4223587405","doi":"10.1139/cjes-2022-0003","title":"“Sudbury Breccia” and “Huronian Breccia”: spatial, sedimentological, and structural evidence for separate distinct breccia-forming events","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"Shell Canada","keywords":"Breccia; Geology; Clastic rock; Geochemistry; Sedimentary rock; Impact crater; Impact structure; Lithology; Basement; Petrology; Geomorphology; Paleontology","score_opus":0.03978343737201894,"score_gpt":0.25382737194112615,"score_spread":0.2140439345691072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4223587405","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99257725,0.004591496,0.000042689906,0.0019779503,0.00032686128,0.0001269328,0.000082282895,0.00000484069,0.00026970461],"genre_scores_gemma":[0.99850667,0.000057048856,0.00072916027,0.00047344787,0.000108252374,0.0000013557021,0.0000080948275,0.000001618917,0.00011434108],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982817,0.0001245452,0.0003764974,0.00031759252,0.00035948318,0.0005401673],"domain_scores_gemma":[0.99843955,0.00040166738,0.00026599367,0.000073457784,0.00008175959,0.0007375496],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010992115,0.0001584237,0.00030101038,0.000195194,0.0014708997,0.00016350673,0.0004120433,0.000041745163,0.003915133],"category_scores_gemma":[0.00036217825,0.00010994521,0.00009788387,0.0004236025,0.0004975665,0.0003942877,0.000034254605,0.00023941821,0.000003834422],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003445679,0.0000028541333,0.9786822,0.000008725726,0.000017938604,0.00003304064,0.00013888338,0.0011433959,0.000033220713,0.00002384998,0.000087522385,0.019793892],"study_design_scores_gemma":[0.00024484305,0.00095419714,0.97644955,0.000029066898,0.00004815396,0.0003430656,0.00035940687,0.008821343,0.000041986063,0.007829964,0.0046654227,0.00021302937],"about_ca_topic_score_codex":0.029927116,"about_ca_topic_score_gemma":0.2360429,"teacher_disagreement_score":0.2061158,"about_ca_system_score_codex":0.000004808427,"about_ca_system_score_gemma":0.0003973237,"threshold_uncertainty_score":0.99982905},"labels":[],"label_agreement":null},{"id":"W4224256205","doi":"10.1139/cjes-2022-0009","title":"Structural geology of the Cadillac Group along the Malartic segment of the Larder Lake Cadillac deformation zone, Quebec, and implications for gold mineralization","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval; University of Toronto; Laurentian University","funders":"","keywords":"Geology; Sinistral and dextral; Greenstone belt; Geochemistry; Shear zone; Clockwise; Arsenopyrite; Sericite; Bedding; Archean; Fold (higher-order function); Geomorphology; Quartz; Paleontology; Fault (geology); Tectonics; Chalcopyrite","score_opus":0.011994330862085434,"score_gpt":0.18993515424883053,"score_spread":0.1779408233867451,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4224256205","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98803014,0.00062988664,0.000033190998,0.010800376,0.00014955031,0.00012551062,0.00010459977,7.458997e-7,0.00012600266],"genre_scores_gemma":[0.999366,0.000007744795,0.00009458361,0.00037984832,0.00002381845,0.0000011896908,0.000008538946,5.9369836e-7,0.000117704985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991716,0.00011410563,0.00027850227,0.000081952785,0.00017600313,0.00017784597],"domain_scores_gemma":[0.99931276,0.00011475579,0.00028747943,0.000094096904,0.000097106815,0.00009381577],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005112384,0.00005668724,0.00011327976,0.00006171272,0.0006044584,0.000027234471,0.00039406912,0.000020138414,0.00066703086],"category_scores_gemma":[0.00010223355,0.000024659059,0.00008750716,0.00048131018,0.0005472205,0.00010205013,0.00001933131,0.00009116848,3.0045769e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000030867525,0.0000014813847,0.9712076,0.0000044191283,0.000010198697,1.354736e-7,0.0002292608,0.026561039,0.000089456415,0.0009975242,0.00010615172,0.0007896481],"study_design_scores_gemma":[0.00008268733,0.00006746402,0.9894542,0.0000044249996,0.000027157717,0.000043541568,0.00040911575,0.0051804655,0.00005641296,0.0029458299,0.0016913763,0.00003731533],"about_ca_topic_score_codex":0.04820825,"about_ca_topic_score_gemma":0.9147446,"teacher_disagreement_score":0.8665363,"about_ca_system_score_codex":0.0000023870496,"about_ca_system_score_gemma":0.00022074043,"threshold_uncertainty_score":0.9581298},"labels":[],"label_agreement":null},{"id":"W4224951968","doi":"10.1139/cjes-2021-0131","title":"Migrations of Devonian brine up-section and the origin of calcite-cemented sand in the Lower Cretaceous McMurray Formation, Athabasca Oil Sands","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Calcite; Devonian; Dolomite; Carbonate; Geochemistry; Cretaceous; Evaporite; Dolomitization; Diagenesis; Sedimentary rock; Paleontology; Facies; Structural basin","score_opus":0.019616363239077436,"score_gpt":0.220349664151844,"score_spread":0.2007333009127666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4224951968","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931879,0.0019210998,0.00007619536,0.0016911869,0.00025278787,0.000057837195,0.00005381811,9.2034014e-7,0.0027582524],"genre_scores_gemma":[0.9995288,0.00009710932,0.000097216085,0.00016667502,0.000023961622,8.358324e-7,0.000006242123,4.9681097e-7,0.00007865662],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99899465,0.00016617068,0.00034745582,0.000059315982,0.00028100077,0.00015141256],"domain_scores_gemma":[0.99929297,0.00021792197,0.00024631864,0.000059088565,0.00010150373,0.00008220022],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018623262,0.000054842207,0.000121631194,0.0002298357,0.00060114294,0.00006660736,0.0002882455,0.000015717198,0.0012908159],"category_scores_gemma":[0.0001482019,0.000028540542,0.000040328836,0.00081005116,0.00045849365,0.00035492456,0.000005230822,0.00013824725,8.485366e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000092970506,0.000023212158,0.9524844,0.000036314723,0.000017346667,0.00001047788,0.009344761,0.026645347,0.000019863104,0.0008579422,0.0006649248,0.0098024085],"study_design_scores_gemma":[0.0012486781,0.0013325765,0.9016071,0.0000536645,0.000032235035,0.00059129106,0.011836734,0.013615928,0.00013251445,0.0016523674,0.06774193,0.00015501668],"about_ca_topic_score_codex":0.016219893,"about_ca_topic_score_gemma":0.2955715,"teacher_disagreement_score":0.2793516,"about_ca_system_score_codex":0.0000017290326,"about_ca_system_score_gemma":0.0003906726,"threshold_uncertainty_score":0.99962217},"labels":[],"label_agreement":null},{"id":"W4225268840","doi":"10.1139/cjes-2021-0014","title":"Geochronology, geochemistry, and petrogenesis of Early Cretaceous highly differentiated I-type granites in the central Great Xing’an Range, northeastern China","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Zircon; Geochemistry; Fractional crystallization (geology); Petrogenesis; Lithophile; Partial melting; Geochronology; Cretaceous; Basalt; Crust; Igneous differentiation; Paleontology","score_opus":0.013838075458386818,"score_gpt":0.18816295096952115,"score_spread":0.17432487551113435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225268840","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958683,0.0029239617,0.0000011829823,0.0006364895,0.00011115643,0.000046192094,0.000056898265,0.0000022045988,0.00035361803],"genre_scores_gemma":[0.9997399,0.000041658524,0.000053560347,0.00009027961,0.00003970319,2.840476e-7,0.000013678511,0.0000011158826,0.00001985456],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986117,0.00018357592,0.00029254745,0.00018394004,0.00031562283,0.00041261484],"domain_scores_gemma":[0.99925697,0.00008997889,0.0001781057,0.00009941837,0.00005507045,0.0003204669],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00052402087,0.00011214509,0.00023583203,0.0002034268,0.0004011401,0.00007542272,0.000601654,0.000033565168,0.0034473536],"category_scores_gemma":[0.00007255152,0.00006945742,0.00007835717,0.0006845172,0.0005601747,0.00013294659,0.00001470193,0.0002198133,0.00000203326],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023933479,0.000010871203,0.99660224,0.000004056671,0.000012983788,0.000073902636,0.00045155847,0.0011667425,0.00014905259,0.000007897503,0.000005212488,0.0014915677],"study_design_scores_gemma":[0.0001715307,0.0006543833,0.99579054,0.0000068896647,0.000029121962,0.0001859812,0.000528951,0.0011184444,0.000119773016,0.0011208956,0.00018262693,0.00009085694],"about_ca_topic_score_codex":0.09041031,"about_ca_topic_score_gemma":0.45594808,"teacher_disagreement_score":0.3655378,"about_ca_system_score_codex":0.0000018703262,"about_ca_system_score_gemma":0.00025291933,"threshold_uncertainty_score":0.99746364},"labels":[],"label_agreement":null},{"id":"W4225888007","doi":"10.1139/cjes-2021-0105","title":"The phylogenetic affinity of the Ordovician trilobites <i>Agerina</i>, <i>Forteyaspis</i> gen. nov., and related genera, with new and revised species from Canada and the United States","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ordovician; Monophyly; Genus; Systematics; Type species; Zoology; Type (biology); Phylogenetic tree; Paleontology; Taxonomy (biology); Group (periodic table); Biology; Chemistry; Clade","score_opus":0.010756873855715075,"score_gpt":0.16702131485203384,"score_spread":0.15626444099631875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225888007","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96175003,0.033608016,8.985089e-7,0.0033022275,0.000206033,0.00011531958,0.00013605585,0.0000011429686,0.00088027935],"genre_scores_gemma":[0.9987935,0.0007038809,0.00006591243,0.00035702632,0.00002728791,3.142472e-7,0.000002154032,8.206153e-7,0.000049137685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998798,0.00025897514,0.0002757429,0.00014045477,0.00026287657,0.0002639635],"domain_scores_gemma":[0.99864066,0.00061283633,0.00029487777,0.00011849481,0.00004915738,0.00028398016],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0008027747,0.00011266124,0.00019904504,0.000085841886,0.0020074213,0.00013089702,0.0004208125,0.000022144191,0.000084712854],"category_scores_gemma":[0.0000837333,0.000050353425,0.000033089833,0.000581374,0.0023909688,0.00008875231,0.000006489516,0.0002538654,4.0212807e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005228515,0.0000011290165,0.9935202,0.0000025601566,0.000043411077,0.000018877068,0.00082755927,0.000903386,0.000021144107,0.00011275645,0.00016936046,0.0043273587],"study_design_scores_gemma":[0.00045824132,0.00020694327,0.9913376,0.000016028038,0.000030468702,0.00016283545,0.002098027,0.00039970383,0.000041805917,0.0009005426,0.004270372,0.000077439865],"about_ca_topic_score_codex":0.80626136,"about_ca_topic_score_gemma":0.9958947,"teacher_disagreement_score":0.18963334,"about_ca_system_score_codex":0.0000017141964,"about_ca_system_score_gemma":0.0018869105,"threshold_uncertainty_score":0.99929184},"labels":[],"label_agreement":null},{"id":"W4229612440","doi":"10.1139/cjes-38-10-1463","title":"Crustal structure of the Grenville Province in southeastern Labrador from refraction seismic data: evidence for a high-velocity lower crustal wedge","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Seismic refraction; Wedge (geometry); Crust; Geophysics; Geometry","score_opus":0.059339380500067256,"score_gpt":0.24264361302500384,"score_spread":0.18330423252493658,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4229612440","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99567676,0.00078794576,0.00017826575,0.001980021,0.0008078426,0.00015596514,0.0003322555,0.0000013545514,0.00007961448],"genre_scores_gemma":[0.999022,0.000043673288,0.0005358181,0.00016004771,0.00017293452,1.5918444e-7,0.000009214067,0.000001142497,0.000055014032],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99890035,0.000069737165,0.00029960563,0.00019753411,0.00025735341,0.00027538693],"domain_scores_gemma":[0.9991681,0.00016943664,0.00028149984,0.00014355419,0.0000879951,0.00014938776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045239582,0.00008897328,0.0001667901,0.00008072337,0.00033687055,0.000083547304,0.0006130051,0.00005268051,0.00040520003],"category_scores_gemma":[0.0003968743,0.000051950825,0.000041246418,0.00034185447,0.00036640957,0.00066135783,0.000019183302,0.00015775861,0.000004774528],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009755417,0.0000070215606,0.973034,0.000007864101,0.000010321397,0.000021513824,0.00037863644,0.010793231,0.00008132936,0.000030453208,0.00016640929,0.015371654],"study_design_scores_gemma":[0.00021281312,0.00025071678,0.98426074,0.000088676104,0.000011129568,0.000019402982,0.0011161184,0.009282324,0.000046942543,0.00097451324,0.0036508404,0.00008575849],"about_ca_topic_score_codex":0.15269648,"about_ca_topic_score_gemma":0.9022916,"teacher_disagreement_score":0.7495951,"about_ca_system_score_codex":0.000003698639,"about_ca_system_score_gemma":0.0008440359,"threshold_uncertainty_score":0.8529458},"labels":[],"label_agreement":null},{"id":"W4229657600","doi":"10.1139/e00-101","title":"Late Wisconsinan stratigraphy and chronology of southern St. George's Bay, Newfoundland: a re-appraisal","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Sedimentary depositional environment; Paleontology; Glacier; Fluvial; Geomorphology; Sedimentary rock; Bay; Oceanography","score_opus":0.024502871462003622,"score_gpt":0.25163023565591985,"score_spread":0.22712736419391624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4229657600","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9866577,0.0027081473,0.000011041217,0.00148768,0.00031218384,0.000049244078,0.00004344473,0.0000026368393,0.008727967],"genre_scores_gemma":[0.9991136,0.00013484438,0.00043680574,0.000093305825,0.000057691967,9.1132456e-8,0.000003081637,0.0000012765323,0.00015929369],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986866,0.00016545398,0.00030459167,0.00017128636,0.00017568219,0.0004963637],"domain_scores_gemma":[0.9988406,0.00029180045,0.00019510307,0.00009461904,0.00009554532,0.0004823492],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010287686,0.000103098195,0.0002554677,0.0004862188,0.00034537152,0.000056790574,0.00033449885,0.00010652147,0.0029868411],"category_scores_gemma":[0.00015106724,0.00007729564,0.000055767694,0.0004188339,0.002344916,0.00022780812,0.0000051093884,0.00025784344,0.000032737138],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019937686,0.0000029567204,0.99814546,0.0000055048695,0.000018154766,0.00017210172,0.00032617868,0.00020153043,0.000005936012,0.00015387159,0.000033574328,0.00091478287],"study_design_scores_gemma":[0.00025881155,0.0006058359,0.9908073,0.000022782104,0.000010581816,0.00092970557,0.00083194755,0.00038456227,0.000006025156,0.0020637175,0.003988305,0.000090457695],"about_ca_topic_score_codex":0.021208746,"about_ca_topic_score_gemma":0.93852925,"teacher_disagreement_score":0.9173205,"about_ca_system_score_codex":2.471919e-7,"about_ca_system_score_gemma":0.0012043376,"threshold_uncertainty_score":0.99792457},"labels":[],"label_agreement":null},{"id":"W4230039729","doi":"10.1139/cjes-37-9-1275","title":"Geology and U-Pb geochronology of the Island Lake greenstone belt, northwestern Superior Province, Manitoba","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geochronology; Geology; Greenstone belt; Geochemistry; Archaeology; Archean; Geography","score_opus":0.0101533617759272,"score_gpt":0.18800002248229394,"score_spread":0.17784666070636673,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4230039729","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99166924,0.00048012115,0.00021711529,0.0029372876,0.00021807091,0.000058702713,0.0000051500774,0.000003219116,0.004411109],"genre_scores_gemma":[0.9977726,0.00002000226,0.00083909597,0.00026310343,0.00005886276,4.5934107e-7,2.3763226e-7,9.1002784e-7,0.001044778],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989983,0.000062703184,0.00026683192,0.00018351528,0.00014910687,0.00033956344],"domain_scores_gemma":[0.9992688,0.00005124219,0.00016358268,0.00019830019,0.000110563386,0.00020753281],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004096437,0.0000914807,0.00018001093,0.00010729657,0.00030862688,0.00006627595,0.0009803,0.00006152564,0.00025695845],"category_scores_gemma":[0.00004962437,0.000060999584,0.00004888891,0.0002867638,0.0011799744,0.00026597947,0.000051996543,0.00015976127,0.000003934577],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004455847,0.00001115222,0.9770876,0.000018590294,0.000016768017,0.00016068426,0.00076178974,0.000754773,0.00032906674,0.0012336617,0.00019826583,0.019423168],"study_design_scores_gemma":[0.0003083996,0.00034987042,0.9446463,0.0000538446,0.000008975578,0.0024025675,0.00018619986,0.0009184955,0.00058168283,0.0016888374,0.048702564,0.00015226226],"about_ca_topic_score_codex":0.008024645,"about_ca_topic_score_gemma":0.8403765,"teacher_disagreement_score":0.83235186,"about_ca_system_score_codex":0.0000031429206,"about_ca_system_score_gemma":0.0011614958,"threshold_uncertainty_score":0.998581},"labels":[],"label_agreement":null},{"id":"W4230188309","doi":"10.1139/cjes-37-5-751","title":"Mineral aerosols: a comparison of the last glacial maximum and preindustrial Holocene","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Holocene; Glacial period; Physical geography; Geochemistry; Earth science; Geomorphology; Paleontology","score_opus":0.04213557626259849,"score_gpt":0.25943524054578077,"score_spread":0.21729966428318226,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4230188309","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915352,0.0009303352,5.9880466e-7,0.0010152182,0.00038969307,0.00006185856,0.000014463635,0.0000011174594,0.006051539],"genre_scores_gemma":[0.9994956,0.0000168794,0.00011982431,0.00008309878,0.00011202452,7.540008e-8,8.3249114e-7,7.190264e-7,0.00017089448],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988849,0.00016447759,0.00027070206,0.00011073448,0.00022212039,0.00034706458],"domain_scores_gemma":[0.99930143,0.00012569212,0.00012716807,0.000073838855,0.00005538808,0.00031645442],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007123031,0.00007255894,0.00019849066,0.00012186458,0.00043164653,0.000051346968,0.00042057768,0.00008820772,0.0028820285],"category_scores_gemma":[0.0001259749,0.00004468048,0.000050916125,0.00035233502,0.0017441644,0.0001676058,0.0000045021607,0.0002814363,0.000019934248],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023269231,0.0000031160835,0.9959936,0.0000022736538,0.000006384482,0.0000126927625,0.00025221918,0.0008254661,0.0000026061302,0.000015692534,0.00014415423,0.0027184845],"study_design_scores_gemma":[0.000270295,0.00033175322,0.9966965,0.000021399308,0.000008388036,0.00023708331,0.00018963034,0.00039645805,0.00006885022,0.00024513243,0.0014815845,0.000052967374],"about_ca_topic_score_codex":0.0027842529,"about_ca_topic_score_gemma":0.34439227,"teacher_disagreement_score":0.34160802,"about_ca_system_score_codex":2.2439475e-7,"about_ca_system_score_gemma":0.00092873466,"threshold_uncertainty_score":0.9980295},"labels":[],"label_agreement":null},{"id":"W4230618852","doi":"10.1139/cjes-2014-0068","title":"Best Paper Award 2013","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Metallurgy and Material Science","field":"Materials Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry","score_opus":0.023273328008555888,"score_gpt":0.23392910100198766,"score_spread":0.21065577299343177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4230618852","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98099023,0.00022657431,0.00039435131,0.002183205,0.003254535,0.00004057159,0.0000034907055,0.0000054970055,0.012901536],"genre_scores_gemma":[0.99550587,0.000016087994,0.0028280225,0.00063192606,0.00030838858,5.265224e-7,1.1708288e-7,0.0000033341005,0.00070570025],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.99860567,0.00010720704,0.00030045572,0.00017215704,0.00035599785,0.00045853245],"domain_scores_gemma":[0.9987462,0.000060318856,0.00019904593,0.00013093231,0.00013217857,0.00073129026],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0026425952,0.00009164516,0.00017582791,0.00017469886,0.00047556232,0.00034266314,0.0007639871,0.00004175802,0.004942502],"category_scores_gemma":[0.0003241829,0.000064368156,0.000054921642,0.00027947838,0.00080152333,0.0008758006,0.000017819666,0.00007703104,0.0006883692],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019993935,0.00003912904,0.01168453,0.000029448523,0.000010065649,0.00011822121,0.001106463,0.0027056567,0.92358375,0.04645425,0.008210802,0.00603768],"study_design_scores_gemma":[0.00032742217,0.00086758035,0.016071111,0.00013149918,0.00002040771,0.0003514829,0.00029919588,0.00022538097,0.057121262,0.007037079,0.917157,0.00039061572],"about_ca_topic_score_codex":0.0067300415,"about_ca_topic_score_gemma":0.062580295,"teacher_disagreement_score":0.90894616,"about_ca_system_score_codex":0.000004654199,"about_ca_system_score_gemma":0.0009322237,"threshold_uncertainty_score":0.99988425},"labels":[],"label_agreement":null},{"id":"W4231517608","doi":"10.1139/cjes-38-5-825","title":"Melting of heterogeneous mantle in a slab window environment: examples from the middle Tertiary Masset basalts, Queen Charlotte Islands, British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Slab; Basalt; Queen (butterfly); Window (computing); Mantle (geology); Slab window; Geochemistry; Subduction; Seismology; Petrology; Oceanic crust; Paleontology; Tectonics","score_opus":0.0187286804858305,"score_gpt":0.16593272727324399,"score_spread":0.1472040467874135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4231517608","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953715,0.0026693959,0.0000061815113,0.0008589749,0.00007986606,0.00005687498,0.00016699091,0.0000019156307,0.0007882876],"genre_scores_gemma":[0.9986712,0.00027502282,0.0003342407,0.0004956644,0.00008926029,2.6598926e-7,0.00001649149,0.0000014591678,0.000116409654],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998561,0.00011434814,0.00040936194,0.00020101987,0.00030454132,0.0004096752],"domain_scores_gemma":[0.9991082,0.00022622674,0.0002133102,0.00010318844,0.000028407467,0.00032064394],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00061039574,0.00008581552,0.00024970848,0.00007243642,0.0002584164,0.00021934764,0.00054461154,0.000049395403,0.013171351],"category_scores_gemma":[0.00010713046,0.00007024972,0.00010299866,0.00033884184,0.0004590932,0.00018473905,0.000012021654,0.00016688772,0.000021754557],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003206197,0.000005664278,0.99516106,0.0000018626572,0.000013481713,0.00018413806,0.00014323811,0.0012823183,0.00005155861,6.003412e-7,0.00008803441,0.0030648196],"study_design_scores_gemma":[0.00016316105,0.000098239434,0.992809,0.000066344335,0.000016133574,0.0001133318,0.00034788772,0.0008719344,0.00006595955,0.0028003647,0.0025456836,0.000101991056],"about_ca_topic_score_codex":0.72289807,"about_ca_topic_score_gemma":0.9750438,"teacher_disagreement_score":0.2521457,"about_ca_system_score_codex":0.000002046905,"about_ca_system_score_gemma":0.00017083772,"threshold_uncertainty_score":0.98773074},"labels":[],"label_agreement":null},{"id":"W4231899041","doi":"10.1139/cjes-37-1-81","title":"Large-scale effects of subglacial meltwater flow in the southern Slave Province, Northwest Territories, Canada","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Meltwater; Geology; Drumlin; Bedrock; Geomorphology; Erosion; Geochemistry; Glacial period; Paleontology; Ice stream; Oceanography","score_opus":0.006268264525105432,"score_gpt":0.1884439308699326,"score_spread":0.18217566634482718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4231899041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99597853,0.00067143806,8.4233153e-7,0.0007769957,0.000397485,0.000106748805,0.00009277084,0.0000010006123,0.0019741727],"genre_scores_gemma":[0.9993198,0.00001495799,0.00009401699,0.00025558262,0.00010945811,3.423223e-7,0.0000102052345,0.0000011692774,0.00019447958],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984041,0.00025876542,0.00028274205,0.00013594376,0.00035927538,0.00055921637],"domain_scores_gemma":[0.99920666,0.00026632106,0.00009063958,0.00010494265,0.000059383725,0.00027207626],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001082624,0.00009684551,0.00020475425,0.00017248762,0.00035225015,0.000047797883,0.00064397964,0.000067022826,0.0015248469],"category_scores_gemma":[0.00007192242,0.000058717193,0.000045046087,0.00039249973,0.00063014333,0.00016670003,0.0000026822484,0.00028527458,0.000020803054],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000140343855,0.0000047039443,0.9959694,0.000010480559,0.0000053292943,0.00036015577,0.0020023405,0.0005398683,4.3402528e-7,0.0000045349693,0.0000708843,0.001017837],"study_design_scores_gemma":[0.00024097778,0.00020339924,0.9898309,0.000027162101,0.000006665911,0.00018279238,0.001000333,0.0002909399,0.00005059316,0.00012548665,0.007964172,0.000076589255],"about_ca_topic_score_codex":0.86187434,"about_ca_topic_score_gemma":0.99996644,"teacher_disagreement_score":0.13809209,"about_ca_system_score_codex":0.0000010863511,"about_ca_system_score_gemma":0.004321897,"threshold_uncertainty_score":0.9993879},"labels":[],"label_agreement":null},{"id":"W4232117995","doi":"10.1139/cjes-2019-0167","title":"Understanding magnetism and electromagnetism and their implicaions: A tribute to David W. Strangway","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Computational Physics and Python Applications","field":"Computer Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Windsor; University of Toronto","funders":"","keywords":"Tribute; Electromagnetism; Geology; Magnetism; Art history; Physics; Condensed matter physics; Quantum mechanics; Art","score_opus":0.03762013464568745,"score_gpt":0.23988724706339298,"score_spread":0.20226711241770554,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4232117995","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7324848,0.0010961043,0.23922291,0.025049897,0.0002271229,0.00024310841,0.000017481421,0.000009829485,0.0016487496],"genre_scores_gemma":[0.9921314,0.000019305524,0.0073245484,0.00040820453,0.00002974527,9.4847724e-7,3.1998127e-7,0.0000021972571,0.00008332515],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99932295,0.000021390719,0.00014551982,0.00017129806,0.00012109288,0.00021771809],"domain_scores_gemma":[0.99921894,0.00011072211,0.000070570546,0.000098549,0.00005815179,0.00044305518],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034776132,0.00006996337,0.000104758044,0.00022712655,0.0002459737,0.00037820917,0.0003488027,0.00001733059,0.000016061378],"category_scores_gemma":[0.000012614502,0.000056767352,0.000024115729,0.00048961473,0.00010004769,0.00037055305,0.000028246492,0.00008299943,0.0000069560665],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000033046815,0.000012147915,0.00838701,0.000010017887,0.00001931605,0.000012629133,0.002580187,0.0010251023,0.008027136,0.9518767,0.0011098378,0.026936604],"study_design_scores_gemma":[0.0007832978,0.0023987617,0.28801194,0.00012976826,0.000010995252,0.0008823705,0.0005891156,0.026158616,0.0004844666,0.62925166,0.05073897,0.00056006527],"about_ca_topic_score_codex":0.00027783756,"about_ca_topic_score_gemma":0.0038543658,"teacher_disagreement_score":0.32262507,"about_ca_system_score_codex":0.000008281454,"about_ca_system_score_gemma":0.0005618133,"threshold_uncertainty_score":0.36470798},"labels":[],"label_agreement":null},{"id":"W4232348439","doi":"10.1139/cjes-38-10-1451","title":"Holocene paleoclimate and paleoecology determined from fossil Coleoptera at Brampton, Ontario, Canada","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Paleoecology; Holocene; Paleoclimatology; Geology; Paleontology; Taphonomy; Physical geography; Archaeology; Climate change; Oceanography; Geography","score_opus":0.018895165968469553,"score_gpt":0.21426116640926557,"score_spread":0.19536600044079602,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4232348439","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98859966,0.0030728276,0.0000015587387,0.0012884921,0.0007672458,0.00007347524,0.000035318106,0.0000031350512,0.006158308],"genre_scores_gemma":[0.99826205,0.00013832239,0.00031541006,0.00063609844,0.000070998634,3.2213717e-7,0.000007935254,0.0000016273578,0.00056723226],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998171,0.00015118012,0.00036274915,0.0002710445,0.00026181067,0.0007822331],"domain_scores_gemma":[0.99814075,0.00044236265,0.00019541988,0.00012449274,0.00010669782,0.000990301],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00064822845,0.00015386994,0.00032249154,0.00023283766,0.0008481504,0.00009429592,0.00042699263,0.00012170139,0.009966102],"category_scores_gemma":[0.00013269809,0.00012404245,0.000044972017,0.00025228635,0.0010725257,0.00024516587,0.000013147709,0.0003092377,0.00003998671],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034034994,0.0000016960047,0.9970414,0.0000022459963,0.000016990529,0.0013420774,0.00020331194,0.00013939364,0.0000013812321,0.000005307604,0.00022713131,0.0009850414],"study_design_scores_gemma":[0.00036858974,0.00026865638,0.9892707,0.000018266219,0.000013704492,0.0016432407,0.00012038871,0.00016203847,0.000017527715,0.00025624217,0.007718949,0.00014170149],"about_ca_topic_score_codex":0.9691158,"about_ca_topic_score_gemma":0.99999446,"teacher_disagreement_score":0.03087864,"about_ca_system_score_codex":0.0000040009477,"about_ca_system_score_gemma":0.0050413418,"threshold_uncertainty_score":0.9909389},"labels":[],"label_agreement":null},{"id":"W4232428029","doi":"10.1139/cjes-38-4-719","title":"Late Quaternary glacial and interglacial environments of the Nechako River - Cheslatta Lake area, central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Glacial period; Tributary; Quaternary; Interglacial; Glacial lake; Glacier; Geomorphology; Paleontology; Geography","score_opus":0.016431312922586684,"score_gpt":0.2000006823215917,"score_spread":0.18356936939900503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4232428029","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996471,0.00052603637,0.000004185034,0.00045162425,0.0005616503,0.000061021103,0.000031280328,0.0000010367578,0.0018921855],"genre_scores_gemma":[0.9988175,0.00012548965,0.00006680181,0.00014514229,0.00006771571,8.880919e-8,0.0000019245317,0.0000010943726,0.0007742581],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883294,0.00012126956,0.00023633952,0.0001364307,0.00022838695,0.00044460714],"domain_scores_gemma":[0.9993222,0.000064948086,0.00014763675,0.000072232084,0.000024326364,0.00036866215],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005157279,0.000063576495,0.00016423999,0.000075750126,0.00048472267,0.00012267655,0.00044391054,0.00007488262,0.0033586493],"category_scores_gemma":[0.00007476526,0.00005880059,0.00005932171,0.00019951878,0.0021246371,0.00020468475,0.000013945832,0.00022081318,0.000011035077],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009000636,0.0000024695835,0.9979319,0.0000021771702,0.000011045472,0.00017804294,0.00025058334,0.00015010092,0.0000034412187,0.0000032288308,0.00009130985,0.0013666914],"study_design_scores_gemma":[0.00019772073,0.0001523784,0.9940781,0.000033736742,0.000008570633,0.00085750397,0.0000832308,0.00024951206,0.000007351007,0.00079502474,0.0034731023,0.000063782354],"about_ca_topic_score_codex":0.043483313,"about_ca_topic_score_gemma":0.9870388,"teacher_disagreement_score":0.9435555,"about_ca_system_score_codex":4.9878025e-7,"about_ca_system_score_gemma":0.00042815282,"threshold_uncertainty_score":0.9975524},"labels":[],"label_agreement":null},{"id":"W4233215878","doi":"10.1139/cjes-2012-0175","title":"Richard Carr Fox, Canadian Paleontologist","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"History of Science and Natural History","field":"Arts and Humanities","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"U.S. Fish and Wildlife Service; University of Alberta","keywords":"Carr; Geology; Archaeology; Geography; Biology","score_opus":0.037914884351526026,"score_gpt":0.2088503591337254,"score_spread":0.1709354747821994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233215878","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.51255685,0.009366398,0.0000015865758,0.0053906348,0.005318409,0.00013940355,0.00002300639,0.000010157509,0.46719354],"genre_scores_gemma":[0.9877791,0.000011893221,0.00011316113,0.001299272,0.00034960549,0.0000012227778,4.5339834e-7,0.00000366544,0.010441638],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99875206,0.000032766122,0.00025875316,0.00014413205,0.00026766857,0.0005446461],"domain_scores_gemma":[0.9983343,0.000031091637,0.00015177696,0.00009373755,0.0003250274,0.0010640827],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00050376495,0.000105138686,0.00016623132,0.0007278489,0.0016660995,0.0003216834,0.0006290678,0.00004090012,0.0097968755],"category_scores_gemma":[0.0000969751,0.00007942686,0.000090160174,0.0001416358,0.0025919576,0.0010584567,0.0000037772438,0.00020288207,0.00047965063],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000066611965,0.000027138132,0.06971926,0.000034240165,0.000063983156,0.0007327939,0.11159552,0.00009850961,0.0002885065,0.098499954,0.6728023,0.046131086],"study_design_scores_gemma":[0.000060764138,0.00014116218,0.012803414,0.000021298663,0.0000057258317,0.000040370403,0.0034338466,0.00001614375,0.000007365341,0.0005422416,0.98279285,0.00013483886],"about_ca_topic_score_codex":0.7477014,"about_ca_topic_score_gemma":0.9962811,"teacher_disagreement_score":0.4752222,"about_ca_system_score_codex":0.000051496998,"about_ca_system_score_gemma":0.003750786,"threshold_uncertainty_score":0.9996336},"labels":[],"label_agreement":null},{"id":"W4233401440","doi":"10.1139/e09-908","title":"Introduction","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"","field":"","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry","score_opus":0.01925730445301998,"score_gpt":0.23870954993186147,"score_spread":0.21945224547884148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233401440","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.972853,0.00060541555,0.000037199665,0.013777909,0.001100345,0.00003541299,0.0000037518669,0.0000067915385,0.011580188],"genre_scores_gemma":[0.9969722,0.000002742438,0.0012946511,0.00029680884,0.0011413275,3.7822765e-8,1.5994694e-7,0.0000029778603,0.0002890835],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991001,0.00003642094,0.00020046833,0.00009601934,0.00026241835,0.00030460145],"domain_scores_gemma":[0.9989811,0.000010736344,0.00016347544,0.00007377801,0.00017159116,0.00059930165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011248383,0.00005630048,0.000096014905,0.00058286183,0.00027893516,0.00015735366,0.00030066047,0.000020153102,0.0007620387],"category_scores_gemma":[0.00030038165,0.000045215373,0.000045458466,0.00079529523,0.00032411105,0.0006293015,0.0000012796331,0.00012127562,0.0003677886],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000072175666,0.000095561765,0.2309574,0.000008274111,0.00006623275,0.0010672031,0.004694405,0.019317381,0.061318193,0.07398866,0.50728035,0.10113417],"study_design_scores_gemma":[0.00025535727,0.001034664,0.46530914,0.00003077595,0.000014748425,0.0013366361,0.000460422,0.00015672919,0.0034259039,0.005164629,0.5226213,0.00018969794],"about_ca_topic_score_codex":0.0007084345,"about_ca_topic_score_gemma":0.045130327,"teacher_disagreement_score":0.23435175,"about_ca_system_score_codex":0.000010652232,"about_ca_system_score_gemma":0.0017996699,"threshold_uncertainty_score":0.97229356},"labels":[],"label_agreement":null},{"id":"W4233474022","doi":"10.1139/cjes-2014-0081","title":"A low-relief hill in eastern Ontario, Canada, covered by the easily erodible Queenston Formation and derived sediments — probably the result of Quaternary tectonic uplift","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Shell (Canada)","funders":"Ministry of Environment; University of Ottawa","keywords":"Geology; Precambrian; Paleontology; Glacial period; Basement; Sedimentary rock; Clastic rock; Tectonic uplift; Ridge; Tectonics; Geochemistry; Geomorphology","score_opus":0.01484104157200577,"score_gpt":0.18606727626627073,"score_spread":0.17122623469426496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233474022","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99576014,0.00094060844,0.000029849616,0.002174089,0.00025524254,0.00013273813,0.000030101332,8.907432e-7,0.0006763633],"genre_scores_gemma":[0.9991693,0.000035227476,0.000086927095,0.0005490479,0.000024832121,4.808255e-7,0.0000033753386,0.0000011513006,0.00012966705],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998876,0.00009215913,0.00036629432,0.00010245461,0.00029955426,0.00026356365],"domain_scores_gemma":[0.9992158,0.00015630403,0.00028747646,0.00009105225,0.0000803082,0.00016909138],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010066942,0.000083687075,0.00013914645,0.000045496643,0.00043442112,0.00008170299,0.00032016452,0.000023095368,0.00012672122],"category_scores_gemma":[0.00011588215,0.000046256686,0.000025913849,0.00027692653,0.00028563154,0.0002686957,0.0000073324313,0.00013713192,0.0000014470272],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012078825,0.0000030579995,0.98986554,0.000006011318,0.000008830585,0.0000032950575,0.001402024,0.0045260377,0.000029130564,0.000015584274,0.0013653666,0.0027630632],"study_design_scores_gemma":[0.00025468765,0.00018599055,0.9804723,0.00006368539,0.0000074213613,0.000021878808,0.0010614943,0.0071207243,0.00007565164,0.000094512136,0.010574158,0.00006744791],"about_ca_topic_score_codex":0.9886958,"about_ca_topic_score_gemma":0.9998374,"teacher_disagreement_score":0.011141575,"about_ca_system_score_codex":0.000013245974,"about_ca_system_score_gemma":0.0016096912,"threshold_uncertainty_score":0.334126},"labels":[],"label_agreement":null},{"id":"W4233550507","doi":"10.1139/cjes-37-2-3-325","title":"Tectono-thermal evolution of deep crust in a Mesoproterozoic continental collision setting: the Manicouagan example","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Crust; Lithosphere; Mantle (geology); Mantle plume; Continental collision; Continental crust; Craton; Metamorphic core complex; Petrology; Geophysics; Geochemistry; Seismology; Paleontology; Tectonics; Extensional definition","score_opus":0.011090658330872959,"score_gpt":0.1836063888153291,"score_spread":0.17251573048445612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233550507","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942252,0.0010959362,0.0000088978095,0.00086385844,0.00007163512,0.0000694657,0.000010221485,0.0000017286351,0.0036530704],"genre_scores_gemma":[0.9994827,0.0000102407275,0.0002671262,0.00012328669,0.000057113855,2.0455964e-7,0.0000019117417,7.5674376e-7,0.00005669619],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99880475,0.00009536247,0.00036164885,0.00013685515,0.00027601336,0.0003253529],"domain_scores_gemma":[0.99934244,0.00011081736,0.0001577334,0.000077647346,0.00006119955,0.00025015266],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008849032,0.00008401184,0.00017932896,0.00017083775,0.00023369431,0.000058675847,0.00043493064,0.000042007137,0.012909269],"category_scores_gemma":[0.000093532144,0.0000470976,0.00009107357,0.0007070702,0.00050604943,0.0001976254,0.0000039325123,0.00016439284,0.000030842493],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016082084,0.0000071986865,0.9733155,0.0000025353975,0.00000645518,0.000024809478,0.00020253696,0.015192329,0.00027288924,0.00003589331,0.000017628196,0.010906157],"study_design_scores_gemma":[0.00016783246,0.0002143955,0.98845196,0.000024619421,0.0000105839845,0.000050624596,0.00048582864,0.007870412,0.0004236752,0.0012777008,0.00094699906,0.000075349555],"about_ca_topic_score_codex":0.1120803,"about_ca_topic_score_gemma":0.57624805,"teacher_disagreement_score":0.46416774,"about_ca_system_score_codex":0.0000031469178,"about_ca_system_score_gemma":0.0002766893,"threshold_uncertainty_score":0.98799306},"labels":[],"label_agreement":null},{"id":"W4233695770","doi":"10.1139/cjes-38-4-679","title":"New UPb and Ar/Ar isotopic age constraints on the timing of Eocene magmatism, Fort Fraser and Nechako River map areas, central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Magmatism; Geochemistry; Paleontology; Earth science; Tectonics","score_opus":0.02238064642783064,"score_gpt":0.21423142172819917,"score_spread":0.19185077530036854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233695770","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937888,0.0013856352,0.000018025268,0.0013921201,0.00021704195,0.00009492446,0.000022243645,0.0000017092988,0.0030794984],"genre_scores_gemma":[0.9984296,0.00024373505,0.0005295929,0.00032595606,0.00004949003,1.1308112e-7,0.0000020894217,0.0000011558533,0.00041827804],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99892086,0.00009353884,0.00020866178,0.00014560514,0.00019110742,0.0004402442],"domain_scores_gemma":[0.9990116,0.00022230842,0.00011226124,0.00006740347,0.000043509393,0.0005429447],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006008939,0.00006898452,0.00018019113,0.000106396874,0.0004677171,0.00019538519,0.00024663517,0.000069150636,0.0051166746],"category_scores_gemma":[0.00010602193,0.00006195554,0.000032382854,0.00018710508,0.001958736,0.00019009357,0.0000062929025,0.00021603187,0.000008720773],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003999211,0.0000015449974,0.9810894,0.0000056049735,0.000009612526,0.00041098308,0.00014327702,0.000026711557,7.642434e-7,0.000033238553,0.0009959069,0.017278926],"study_design_scores_gemma":[0.00023237572,0.00019005308,0.9949089,0.000089523746,0.000008481499,0.0008843713,0.0002766995,0.00018961223,0.000006048872,0.001550893,0.0015949352,0.00006806792],"about_ca_topic_score_codex":0.068355046,"about_ca_topic_score_gemma":0.8983442,"teacher_disagreement_score":0.8299892,"about_ca_system_score_codex":4.5587217e-7,"about_ca_system_score_gemma":0.0005578511,"threshold_uncertainty_score":0.9957928},"labels":[],"label_agreement":null},{"id":"W4234231488","doi":"10.1139/cjes-2019-0225","title":"Understanding tectonic processes and their consequences: a tribute to A.M. Celâl Şengör: Part 2","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"","keywords":"Geology; Tribute; Tectonics; Paleontology; Geochemistry; Archaeology","score_opus":0.0765119907827635,"score_gpt":0.2256693713715996,"score_spread":0.1491573805888361,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4234231488","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.978094,0.0062417537,0.00010063847,0.0035327352,0.0007339184,0.00018404878,0.00006781683,0.000009669112,0.01103545],"genre_scores_gemma":[0.9987906,0.00019105156,0.0002288507,0.00044772858,0.00008286006,2.7292518e-7,0.0000010419899,0.000002240249,0.00025534612],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99867606,0.000052303247,0.00027968947,0.00022604872,0.00023552157,0.0005303536],"domain_scores_gemma":[0.99868864,0.00031934038,0.00015142269,0.00009164584,0.000114991104,0.0006339842],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00090341107,0.0001471604,0.0002715096,0.0003631748,0.0005142376,0.0002616219,0.00032291136,0.000042065956,0.0014090602],"category_scores_gemma":[0.00028225494,0.000096784264,0.00004937612,0.0008312937,0.00062977336,0.0004110746,0.000007187634,0.00015693753,0.00007616566],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016363294,0.0000032487728,0.99222255,0.000042227344,0.000045820678,0.000062254054,0.0019636778,0.0009725566,0.000040535673,0.00036990736,0.00093799096,0.003322841],"study_design_scores_gemma":[0.0015936233,0.005871963,0.7010149,0.0013398405,0.00006859699,0.0018905775,0.033269044,0.00062025234,0.0018774922,0.017505882,0.23355362,0.001394215],"about_ca_topic_score_codex":0.0042255167,"about_ca_topic_score_gemma":0.41821593,"teacher_disagreement_score":0.4139904,"about_ca_system_score_codex":0.0000047255758,"about_ca_system_score_gemma":0.0022612398,"threshold_uncertainty_score":0.9995038},"labels":[],"label_agreement":null},{"id":"W4234239151","doi":"10.1139/cjes-2013-0067","title":"<i>Erratum:</i> U–Pb and Hf isotopic data from Franklinian Basin strata: insights into the nature of Crockerland and the timing of accretion, Canadian Arctic Islands","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Calgary","funders":"","keywords":"Geology; Structural basin; Arctic; Accretion (finance); Canada Basin; Oceanography; Paleontology","score_opus":0.02466297222580724,"score_gpt":0.20961506196902815,"score_spread":0.18495208974322092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4234239151","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9814384,0.0098345475,0.0000108081185,0.007217119,0.00026262354,0.00011170975,0.00004269578,7.1391145e-7,0.0010813687],"genre_scores_gemma":[0.9985142,0.00053021294,0.0002325892,0.0005947654,0.00009474146,2.3181036e-7,0.000013585279,8.524519e-7,0.000018874896],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991002,0.00009457587,0.00027055526,0.0001454256,0.00018934261,0.0001998951],"domain_scores_gemma":[0.99897826,0.00026294903,0.00018679837,0.00014475799,0.00014001792,0.00028720035],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005935971,0.00008301413,0.00019183374,0.00009248058,0.0006286306,0.00016921957,0.00048872293,0.00006600953,0.00040226802],"category_scores_gemma":[0.0002553694,0.00003862613,0.000022942313,0.0002538901,0.0011095864,0.0004689057,0.000016522425,0.00022316483,0.0000028110665],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011524182,0.0000017425,0.98862946,0.000010050635,0.000030524036,0.000006342602,0.0051017865,0.000121323705,0.000010937444,0.00016746989,0.0013106446,0.0045982166],"study_design_scores_gemma":[0.00023950418,0.00013263787,0.9810482,0.000045006986,0.000020920867,0.00001264772,0.0035386803,0.0023935118,0.000011014218,0.006747609,0.005746673,0.00006358638],"about_ca_topic_score_codex":0.7577629,"about_ca_topic_score_gemma":0.98606515,"teacher_disagreement_score":0.22830224,"about_ca_system_score_codex":0.0000012615994,"about_ca_system_score_gemma":0.0004981129,"threshold_uncertainty_score":0.48349816},"labels":[],"label_agreement":null},{"id":"W4234465019","doi":"10.1139/cjes-37-12-1711","title":"Records of geomagnetic secular variation since 1200 AD and the potential for chronological control of lake sediments in northern Alberta","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Secular variation; Earth's magnetic field; Geomagnetic secular variation; Variation (astronomy); Oceanography; Paleontology; Physical geography; Geophysics; Geomagnetic storm","score_opus":0.004962693820662423,"score_gpt":0.19506192741361764,"score_spread":0.19009923359295522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4234465019","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99432194,0.004124899,0.00012532681,0.00082745793,0.00009532026,0.00015460323,0.000028584689,2.5286846e-7,0.00032159532],"genre_scores_gemma":[0.99913204,0.0002555045,0.00032042264,0.00008689511,0.000044825825,0.0000027315607,0.00000232354,0.0000023164769,0.0001529321],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99925363,0.000067887704,0.00027946974,0.00011736253,0.00009980689,0.00018183555],"domain_scores_gemma":[0.99956185,0.00004475496,0.00015104775,0.00007340943,0.00008791817,0.00008104636],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004489971,0.00007237752,0.00017385774,0.00006095948,0.000091623835,0.000014514302,0.00017422455,0.000056067016,0.000078227386],"category_scores_gemma":[0.00011851908,0.000049357703,0.000059024387,0.000092858405,0.0006240258,0.000008545963,0.000007362753,0.000045024182,4.0427938e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022811927,0.00019242351,0.8600021,0.00014096446,0.0003709408,0.00006020342,0.0034452556,0.014782518,0.05216978,0.00064689084,0.00041211178,0.06549565],"study_design_scores_gemma":[0.0042385147,0.0030134318,0.98383695,0.00004481257,0.00006336085,0.000087316985,0.00017511488,0.00085340656,0.000709291,0.00046754922,0.006367514,0.00014272399],"about_ca_topic_score_codex":0.0024483707,"about_ca_topic_score_gemma":0.40457568,"teacher_disagreement_score":0.40212733,"about_ca_system_score_codex":0.0000011143676,"about_ca_system_score_gemma":0.00029556316,"threshold_uncertainty_score":0.60628927},"labels":[],"label_agreement":null},{"id":"W4235043016","doi":"10.1139/e11-059","title":"E.R. Ward Neale: a rock-solid advisor and friend","year":2012,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Australian Indigenous Culture and History","field":"Social Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Mineralogy","score_opus":0.03842310539870881,"score_gpt":0.29106771719197894,"score_spread":0.25264461179327014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4235043016","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.85799193,0.008155544,0.00005630924,0.0033355954,0.00237896,0.00014803739,0.000012508632,0.000011038038,0.12791009],"genre_scores_gemma":[0.99487513,0.00008070566,0.00038595562,0.00026018757,0.00071124284,4.3753505e-7,1.5301451e-7,0.0000032491155,0.003682915],"study_design_codex":"qualitative","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987373,0.00007739455,0.00018916263,0.00008538739,0.00029435364,0.0006164195],"domain_scores_gemma":[0.9983435,0.00003369638,0.00015655403,0.000050034025,0.00010560167,0.0013106018],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0012216048,0.00007214467,0.00013696407,0.0002058844,0.0018254613,0.0001465808,0.000279823,0.00006643955,0.0006317214],"category_scores_gemma":[0.00015242718,0.000059774462,0.000049331215,0.00030329372,0.00083490927,0.0007672067,0.0000053129365,0.00014821894,0.000036219863],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010018637,0.00003974567,0.4600304,0.000017240227,0.00004531424,0.00011261781,0.46702963,0.000054179018,0.00014977898,0.033569306,0.032733213,0.0062085525],"study_design_scores_gemma":[0.00008201562,0.00010588859,0.036421098,0.000023323377,0.00001396227,0.00006102824,0.018384315,0.0000010954029,0.00004423196,0.00024177016,0.9445049,0.000116352974],"about_ca_topic_score_codex":0.019746209,"about_ca_topic_score_gemma":0.3760735,"teacher_disagreement_score":0.9117717,"about_ca_system_score_codex":0.000022192,"about_ca_system_score_gemma":0.0026637292,"threshold_uncertainty_score":0.99947405},"labels":[],"label_agreement":null},{"id":"W4236729476","doi":"10.1139/e02-904","title":"Erratum: The High Pressure belt in the Grenville Province: architecture, timing, and exhumation","year":2002,"lang":"en","type":"erratum","venue":"Canadian Journal of Earth Sciences","topic":"Tunneling and Rock Mechanics","field":"Engineering","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Architecture; Seismology; Geography; Archaeology","score_opus":0.016006492043593567,"score_gpt":0.19849480475167627,"score_spread":0.18248831270808272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236729476","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13808927,0.45693165,0.0021209512,0.021917323,0.16296525,0.0028528513,0.00041116658,0.00014081728,0.21457073],"genre_scores_gemma":[0.982495,0.001313572,0.00033313088,0.00028934242,0.0017484137,0.0000042974566,0.0000063561083,0.000030204821,0.013779669],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99887055,0.00007384196,0.0002699191,0.0001243799,0.00033641074,0.00032489948],"domain_scores_gemma":[0.99945235,0.000059756894,0.00014016694,0.00014663454,0.000046207642,0.00015485466],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000787713,0.00016138834,0.00019147388,0.00032427008,0.00044335757,0.00024389212,0.0006380586,0.0001587382,0.000057420177],"category_scores_gemma":[0.000093228766,0.0000867334,0.000048579466,0.00029843644,0.00015546178,0.000090199785,0.000010614305,0.0010876402,0.000001966966],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000020065206,0.0000075275557,0.0001708432,0.00020830924,0.000061286984,0.00014968494,0.00846712,0.11736916,0.000013130637,0.0007316011,0.8607872,0.012032103],"study_design_scores_gemma":[0.00021959901,0.0002176818,0.004305777,0.0009199759,0.00009048918,0.0006376533,0.0009167137,0.030367928,0.000012395257,0.0023445308,0.9595681,0.00039918927],"about_ca_topic_score_codex":0.0013068046,"about_ca_topic_score_gemma":0.109632455,"teacher_disagreement_score":0.8444058,"about_ca_system_score_codex":0.000007433471,"about_ca_system_score_gemma":0.00058094854,"threshold_uncertainty_score":0.9066144},"labels":[],"label_agreement":null},{"id":"W4236731814","doi":"10.1139/cjes-2015-0075","title":"Appuyer le libre accès et offrir un plus grand choix aux auteurs","year":2015,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Health, Medicine and Society","field":"Health Professions","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Humanities; Geology; Philosophy","score_opus":0.13608875446860333,"score_gpt":0.39643653520902067,"score_spread":0.2603477807404173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236731814","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5552062,0.050634168,0.0002924817,0.34278864,0.01645808,0.0005130442,0.000077257755,0.000015819569,0.034014337],"genre_scores_gemma":[0.9108906,0.0030100017,0.004146232,0.054017194,0.0034681514,0.0000045052857,0.000004238446,0.000039532493,0.024419557],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9949907,0.0015484983,0.0009784895,0.00029077643,0.00076509966,0.0014264064],"domain_scores_gemma":[0.992538,0.0005792316,0.00059005246,0.0002356003,0.0007452551,0.0053118714],"candidate_categories":["sts","research_integrity"],"consensus_categories":[],"category_scores_codex":[0.010441759,0.00023273863,0.00057345536,0.00035935699,0.0018834753,0.00018778844,0.0009037028,0.0006099954,0.0007778919],"category_scores_gemma":[0.0021776282,0.000189931,0.00017463548,0.0011018874,0.0014832685,0.0015024131,0.00005068518,0.0026658184,0.00016929513],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042642878,0.00007384169,0.07347841,0.00042595193,0.000095115414,0.0009897631,0.21222728,0.00065870397,0.000009871943,0.014725966,0.6661677,0.0311048],"study_design_scores_gemma":[0.0019258758,0.0006679953,0.02949459,0.0012060861,0.000039390616,0.00023077131,0.0566427,0.00045169538,0.0000073699002,0.0015381324,0.9075737,0.00022167263],"about_ca_topic_score_codex":0.07093326,"about_ca_topic_score_gemma":0.3795933,"teacher_disagreement_score":0.35568443,"about_ca_system_score_codex":0.00009804869,"about_ca_system_score_gemma":0.15583277,"threshold_uncertainty_score":0.9996351},"labels":[{"model":"gemma","categories":["open_science","scholarly_communication"],"domain":null,"study_design":"not_applicable","genre":"commentary","about_ca_system":true,"about_ca_topic":false,"confidence":"low"},{"model":"gpt","categories":["scholarly_communication"],"domain":null,"study_design":"not_applicable","genre":"commentary","about_ca_system":false,"about_ca_topic":false,"confidence":"high"}],"label_agreement":"split"},{"id":"W4236766091","doi":"10.1139/cjes-38-7-1059","title":"Geochemical evolution of groundwater on Saturna Island, British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Groundwater; Geochemistry; Geomorphology; Geotechnical engineering","score_opus":0.009620460417408789,"score_gpt":0.17996144058896105,"score_spread":0.17034098017155225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236766091","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9858167,0.00064352166,0.000023911736,0.00013510256,0.00044541815,0.00004154391,0.00003501724,0.0000026838818,0.012856094],"genre_scores_gemma":[0.9985312,0.000029772511,0.00015536933,0.000106732376,0.0001898086,9.140125e-8,0.000006233927,0.0000016637294,0.0009791134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875146,0.000036257756,0.0003176423,0.0001557767,0.00034191448,0.0003969276],"domain_scores_gemma":[0.9991384,0.00004379328,0.00015588859,0.000090196976,0.000120555436,0.0004511633],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005037837,0.000075619624,0.00018178261,0.00011020529,0.00027246683,0.00038117453,0.00038756544,0.00006778808,0.005803388],"category_scores_gemma":[0.00007384343,0.00007979278,0.00008758076,0.00033777408,0.0004556903,0.00033885174,0.0000035506987,0.00018129697,0.000030682455],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007406637,0.000007150188,0.9950225,0.000005263091,0.0000069598746,0.00011099211,0.000055907094,0.00018424285,0.00019171026,0.0000044430503,0.0015851163,0.0028183337],"study_design_scores_gemma":[0.0002582101,0.00049550046,0.9808014,0.00010408532,0.0000102577405,0.0012724557,0.00023969174,0.00017319033,0.0005010124,0.0013349334,0.014665008,0.00014425062],"about_ca_topic_score_codex":0.38185313,"about_ca_topic_score_gemma":0.9482559,"teacher_disagreement_score":0.5664028,"about_ca_system_score_codex":0.000005003902,"about_ca_system_score_gemma":0.0006829777,"threshold_uncertainty_score":0.99510545},"labels":[],"label_agreement":null},{"id":"W4236835307","doi":"10.1139/cjes-38-12-1645","title":"New material of &lt;i&gt;Dracochelys&lt;/i&gt; (Eucryptodira: Sinemydidae) from the Junggar Basin, Xinjiang, People's Republic of China","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Invertebrate Taxonomy and Ecology","field":"Agricultural and Biological Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Structural basin; China; Geochemistry; Paleontology; Archaeology; Geography","score_opus":0.014990475774636431,"score_gpt":0.18823209811113306,"score_spread":0.17324162233649662,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236835307","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987039,0.00085064676,0.000007433751,0.0067766644,0.00093452475,0.00010640955,0.00006948835,0.000004902732,0.0042109294],"genre_scores_gemma":[0.9980557,0.00011835868,0.00037345607,0.0003251084,0.00070626993,6.342355e-7,0.00000692373,0.0000011569769,0.00041236755],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982104,0.00015499644,0.00059992395,0.00022363933,0.0003104974,0.0005005494],"domain_scores_gemma":[0.99844795,0.00018555032,0.0006015906,0.000096199554,0.00019322928,0.00047547222],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000943364,0.0001606478,0.0003958101,0.0000779914,0.0004179247,0.00013821754,0.0009860217,0.000120613186,0.0080970805],"category_scores_gemma":[0.00025390755,0.00006243712,0.00017587547,0.00086918956,0.0005636353,0.00043700094,0.000038978833,0.00013831488,0.000023080656],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024899933,0.00015318228,0.5403992,0.000022160782,0.00019763545,0.00016895916,0.0025891457,0.00022157477,0.30976576,0.00817692,0.074687175,0.06336928],"study_design_scores_gemma":[0.00018222457,0.00056428247,0.84235156,0.00004676196,0.000026398142,0.000084994805,0.00026549862,0.000038037626,0.0032487551,0.0007851404,0.15226007,0.00014628185],"about_ca_topic_score_codex":0.017548991,"about_ca_topic_score_gemma":0.4492374,"teacher_disagreement_score":0.4316884,"about_ca_system_score_codex":0.0000112663265,"about_ca_system_score_gemma":0.0008808594,"threshold_uncertainty_score":0.99280965},"labels":[],"label_agreement":null},{"id":"W4236922197","doi":"10.1139/cjes-37-4-601","title":"Major end moraines of Younger Dryas age on Wollaston Peninsula, Victoria Island, Canadian Arctic: implications for paleoclimate and for formation of hummocky moraine","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Moraine; Younger Dryas; Geology; Deglaciation; Glacier; Ice sheet; Arctic; Radiocarbon dating; Meltwater; Ice core; Paleoclimatology; Physical geography; Glacial period; Oceanography; Paleontology; Climate change; Geography","score_opus":0.029614544822120413,"score_gpt":0.2630895233208913,"score_spread":0.23347497849877089,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236922197","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926864,0.0005842818,0.000036004985,0.002754814,0.00020294939,0.0003245938,0.0007363588,0.0000015166161,0.0026731025],"genre_scores_gemma":[0.9984514,0.00006574394,0.0010684851,0.00013978437,0.000066474815,0.0000029796859,0.000055123164,0.0000023701148,0.00014762254],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987932,0.00005000175,0.00039567892,0.00015503472,0.00013598157,0.0004701374],"domain_scores_gemma":[0.99852985,0.00039743743,0.00021138575,0.00010361243,0.00027148952,0.00048622765],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00093622616,0.000108037515,0.0002718994,0.00053488836,0.00050993665,0.000046446145,0.00028509993,0.0000879683,0.0009800803],"category_scores_gemma":[0.00022789412,0.00008632302,0.0000756736,0.00030965227,0.000691244,0.0003269562,0.0000018701342,0.00010281461,0.000004615357],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008369214,0.000004739136,0.99658847,0.000046048626,0.000015844389,0.0000058660817,0.00041215227,0.0006014324,0.00003057749,0.0010411978,0.000106774714,0.0010631989],"study_design_scores_gemma":[0.0006817086,0.0012202379,0.98594993,0.00005774953,0.00003250862,0.00016548607,0.00023179289,0.0013060622,0.00013722455,0.0040501393,0.006040196,0.00012693513],"about_ca_topic_score_codex":0.038796578,"about_ca_topic_score_gemma":0.96605164,"teacher_disagreement_score":0.92725503,"about_ca_system_score_codex":0.0000016318168,"about_ca_system_score_gemma":0.0009812174,"threshold_uncertainty_score":0.9999332},"labels":[],"label_agreement":null},{"id":"W4236990613","doi":"10.1139/cjes-38-12-1767","title":"A new ankylosaurid (Dinosauria: Ankylosauria) from the Lower Cretaceous of China, with comments on ankylosaurian relationships","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Postcrania; Paleontology; Taxon; Sister group; Cretaceous; Geology; China; Phylogenetic tree; Geography; Biology; Archaeology; Clade","score_opus":0.028121859878815034,"score_gpt":0.21507650926173535,"score_spread":0.18695464938292033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236990613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9771218,0.0033957327,0.00010154941,0.008872951,0.0008592614,0.00012505222,0.00018624245,0.000005623181,0.009331809],"genre_scores_gemma":[0.99755424,0.00007341313,0.0011782795,0.0006561025,0.00036203003,2.190674e-7,0.00002333416,0.0000024993403,0.00014990839],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99809563,0.00037005602,0.00043626878,0.00024293084,0.00036044102,0.0004946708],"domain_scores_gemma":[0.9980838,0.00062487205,0.0003789654,0.00023277465,0.00009257586,0.0005870703],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010201811,0.00017579018,0.00029373777,0.00024044204,0.00080441695,0.00006238024,0.00076100125,0.00012597232,0.0028984454],"category_scores_gemma":[0.00026004648,0.000103767765,0.000094564006,0.0006158993,0.0009779617,0.00037806178,0.0000052936934,0.00047031956,0.000051359842],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016631337,0.000013322484,0.99287707,0.0000011182321,0.000045025587,0.00016538503,0.00038961344,0.0019558512,0.0000049182386,0.00031491168,0.0017538144,0.0023126532],"study_design_scores_gemma":[0.00044420455,0.0013099927,0.97223973,0.0000682477,0.000032887805,0.00038392012,0.0002987333,0.00025291173,0.00001092383,0.002542491,0.022282908,0.00013305996],"about_ca_topic_score_codex":0.030793265,"about_ca_topic_score_gemma":0.6394106,"teacher_disagreement_score":0.60861737,"about_ca_system_score_codex":0.000003982094,"about_ca_system_score_gemma":0.0015026404,"threshold_uncertainty_score":0.998013},"labels":[],"label_agreement":null},{"id":"W4237285205","doi":"10.1139/cjes-38-4-551","title":"Biostratigraphic and biogeographic constraints on the Carboniferous to Jurassic Cache Creek Terrane in central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Terrane; Carboniferous; Paleontology; Cretaceous; Cache; Structural basin; Tectonics","score_opus":0.01968242122907507,"score_gpt":0.20133449415544197,"score_spread":0.1816520729263669,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4237285205","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9842268,0.0028374805,0.0000019032038,0.0017151433,0.00032395023,0.00013929405,0.000059391732,0.0000036039655,0.010692399],"genre_scores_gemma":[0.99926347,0.00013424746,0.00012393988,0.00040876653,0.00005112368,4.2894754e-7,6.926144e-7,7.2878066e-7,0.000016629685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984207,0.00014439793,0.00032031638,0.00022409679,0.0002534678,0.0006369768],"domain_scores_gemma":[0.9987966,0.00018056623,0.00011561382,0.000091050184,0.00004208619,0.00077409024],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008728815,0.000102240214,0.00020694578,0.00032764435,0.0006419271,0.00074722845,0.0004034294,0.00007807774,0.00073020725],"category_scores_gemma":[0.00012098906,0.00009924384,0.000073559415,0.0010297662,0.0019910154,0.00022294465,8.6647407e-7,0.0002929666,0.0000020417913],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004808283,0.0000038538333,0.94762826,0.0000014757584,0.000009434471,0.0005014076,0.00017590236,0.000028738152,0.0000064389374,0.0000177172,0.00013422099,0.05148775],"study_design_scores_gemma":[0.00017396499,0.000523525,0.9965719,0.000092240676,0.00000729678,0.0010154191,0.00054652477,0.000049698167,0.0000022494696,0.0006114667,0.00027922698,0.0001264806],"about_ca_topic_score_codex":0.45929456,"about_ca_topic_score_gemma":0.9984816,"teacher_disagreement_score":0.539187,"about_ca_system_score_codex":0.0000010611941,"about_ca_system_score_gemma":0.000706428,"threshold_uncertainty_score":0.79952574},"labels":[],"label_agreement":null},{"id":"W4237373404","doi":"10.1139/e07-906","title":"Erratum: Geochemical and metallogenic relations in volcanic rocks of the southern Slave Province: implications for late Neoarchean tectonics","year":2007,"lang":"en","type":"erratum","venue":"Canadian Journal of Earth Sciences","topic":"Ancient and Medieval Archaeology Studies","field":"Arts and Humanities","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Tectonics; Volcano; Volcanic rock; Earth science; Seismology","score_opus":0.037685572233406676,"score_gpt":0.2514642664625719,"score_spread":0.21377869422916523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4237373404","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.76810205,0.056969997,0.00014851398,0.02562577,0.021986647,0.0021057243,0.0013654307,0.000017683446,0.123678155],"genre_scores_gemma":[0.83508205,0.00024596284,0.00019011195,0.00035074627,0.0009952472,0.000010726268,0.000014362826,0.00001900463,0.1630918],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99883497,0.000034013283,0.00042671073,0.00016588107,0.00015978294,0.00037867305],"domain_scores_gemma":[0.9988998,0.00013597033,0.00041013586,0.000110742,0.00026408408,0.00017925036],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0007858731,0.00013561212,0.00029766798,0.00036571926,0.0007194386,0.000038037037,0.0004122535,0.000116210394,0.00005534079],"category_scores_gemma":[0.0003226698,0.000087458204,0.00015115662,0.00013612359,0.0033869778,0.00009005847,0.00004196471,0.00053806795,0.0000011954405],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008348196,0.00011970058,0.22715363,0.0004226002,0.00079835724,0.000032446114,0.26516676,0.00021185522,0.00029714993,0.11739318,0.38210726,0.006213561],"study_design_scores_gemma":[0.00047759395,0.00045184954,0.031906784,0.00044703417,0.0002696781,0.00004805573,0.0113078235,0.00014080235,0.00002674322,0.035529826,0.9190374,0.0003563984],"about_ca_topic_score_codex":0.0028255864,"about_ca_topic_score_gemma":0.85446787,"teacher_disagreement_score":0.8516423,"about_ca_system_score_codex":0.000021016405,"about_ca_system_score_gemma":0.0040607294,"threshold_uncertainty_score":0.9993252},"labels":[],"label_agreement":null},{"id":"W4238474946","doi":"10.1139/e10-903","title":"Author IndexVolume 47, 2010","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Diverse Scientific and Economic Studies","field":"Economics, Econometrics and Finance","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry","score_opus":0.05518259184672476,"score_gpt":0.21385261037814154,"score_spread":0.15867001853141677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4238474946","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.71541214,0.00082881795,0.00005559056,0.0023694774,0.020270806,0.000055739012,0.00011879632,0.000004845785,0.2608838],"genre_scores_gemma":[0.9153875,0.0000097101,0.0015078225,0.00021374643,0.00024426976,4.7325187e-7,2.5234652e-7,0.000004080876,0.08263213],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990259,0.000004445656,0.0004046923,0.00018540135,0.000039496827,0.00034010466],"domain_scores_gemma":[0.9990278,0.000023757015,0.000333516,0.00012358204,0.000056101617,0.00043524543],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0016023838,0.00007410372,0.00021637333,0.0005117499,0.00037904887,0.00025612616,0.0004774919,0.00005239261,0.012318556],"category_scores_gemma":[0.0002803038,0.0000722004,0.00009225383,0.00027954372,0.0006487711,0.00046259278,0.000016908976,0.00021219361,0.0032016695],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002668677,0.000014233734,0.6200507,0.0000044849025,0.000042214164,0.000032961805,0.0014382531,0.000076269025,0.000048406197,0.18099657,0.1961799,0.0011133194],"study_design_scores_gemma":[0.00015374926,0.00005657282,0.11758566,0.000006379625,0.0000027333665,0.000036662663,0.00049888156,0.00023399646,0.000028046103,0.007714732,0.87354404,0.00013854803],"about_ca_topic_score_codex":0.0032685215,"about_ca_topic_score_gemma":0.04018841,"teacher_disagreement_score":0.6773642,"about_ca_system_score_codex":0.0000057917405,"about_ca_system_score_gemma":0.0003988164,"threshold_uncertainty_score":0.99757445},"labels":[],"label_agreement":null},{"id":"W4239478740","doi":"10.1139/e01-022","title":"Kilometre-scale folding in the Teslin zone, northern Canadian Cordillera, and its tectonic implications for the accretion of the Yukon-Tanana terrane to North America: Reply","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Terrane; Geology; Accretion (finance); Tectonics; Scale (ratio); Earth science; Seismology; Geomorphology; Geography","score_opus":0.024402562124868764,"score_gpt":0.21783915381784383,"score_spread":0.19343659169297506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239478740","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9649031,0.0012209393,0.000031977524,0.0327053,0.000077120916,0.0002120484,0.000075265154,0.000001202403,0.00077304686],"genre_scores_gemma":[0.99765307,0.000081658356,0.00013526442,0.0020185853,0.000058075868,0.000002103736,0.0000034299353,0.0000011925968,0.00004663109],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885964,0.00006673648,0.00030986517,0.00016975673,0.00019940606,0.0003945626],"domain_scores_gemma":[0.9987523,0.00038448308,0.00017230978,0.00015590407,0.00014273523,0.0003922448],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00060742034,0.00009363955,0.00017282918,0.00025628868,0.0006979512,0.000087713335,0.0007676827,0.000026532634,0.00057687046],"category_scores_gemma":[0.0004163001,0.00004229601,0.000095758114,0.0020515567,0.00032804784,0.00012011341,0.0000072917655,0.00015443139,0.0000054859242],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004566156,0.0000032112528,0.98099405,0.0000018192324,0.0000095915675,0.0000024832323,0.00036047556,0.0051923,0.000035316043,0.000013746206,0.00007649099,0.0133059425],"study_design_scores_gemma":[0.00006554305,0.0001540908,0.9891646,0.000015980926,0.0000252374,0.000039148636,0.00081285305,0.0020421327,0.000017441642,0.000317856,0.0072761723,0.00006895649],"about_ca_topic_score_codex":0.41012466,"about_ca_topic_score_gemma":0.99587053,"teacher_disagreement_score":0.5857459,"about_ca_system_score_codex":0.000005409698,"about_ca_system_score_gemma":0.0005638966,"threshold_uncertainty_score":0.63163275},"labels":[],"label_agreement":null},{"id":"W4239621148","doi":"10.1139/cjes-37-2-3-253","title":"Docking of the Central Metasedimentary Belt to Laurentia in geon 12: evidence from the 1.17-1.16 Ga Chevreuil intrusive suite and host gneisses, Quebec","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Laurentia; Suite; Geology; Geochemistry; Petrology; Geography; Ordovician","score_opus":0.025440342599154397,"score_gpt":0.20633250910958684,"score_spread":0.18089216651043244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239621148","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98565286,0.005643814,0.0000027903245,0.008015527,0.00028266595,0.00011288326,0.000038465263,0.0000010375435,0.0002499538],"genre_scores_gemma":[0.9984792,0.00029288462,0.00010367986,0.00096981553,0.00009696575,2.614789e-7,0.0000025222669,7.710564e-7,0.00005390217],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988658,0.00011570272,0.00026904888,0.00014674701,0.0002650004,0.00033770953],"domain_scores_gemma":[0.9992498,0.0002422332,0.00012511195,0.00008442304,0.000039106057,0.0002593309],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00059713225,0.000088540786,0.00015455826,0.00006217794,0.00042368224,0.00012383133,0.000438926,0.00002677618,0.0027836766],"category_scores_gemma":[0.00015925443,0.00004458415,0.00004717424,0.0004154043,0.00042188517,0.00039409843,0.000012004362,0.00013839437,0.0000065572544],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013701612,0.0000021314213,0.98353666,0.000001377469,0.000008860278,0.000008466367,0.0014363151,0.0038149047,0.000019950696,0.0000066099947,0.0005479647,0.010603079],"study_design_scores_gemma":[0.00008209529,0.00013845667,0.9925851,0.000114244576,0.000014415438,0.000009031451,0.0013579839,0.00018428366,0.00008672121,0.00017615785,0.005188632,0.00006283437],"about_ca_topic_score_codex":0.68227977,"about_ca_topic_score_gemma":0.99098766,"teacher_disagreement_score":0.3087079,"about_ca_system_score_codex":0.0000059388963,"about_ca_system_score_gemma":0.00036906105,"threshold_uncertainty_score":0.99812794},"labels":[],"label_agreement":null},{"id":"W4239867796","doi":"10.1139/cjes-38-8-1169","title":"Lithospheric structure across the craton-Cordilleran transition of northeastern British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Craton; Lithosphere; Earth science; Geochemistry; Paleontology; Tectonics","score_opus":0.008760604852264556,"score_gpt":0.18271245855922227,"score_spread":0.1739518537069577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239867796","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962731,0.0012339324,0.000026199697,0.00080275413,0.0001740931,0.000041599567,0.00010545638,0.0000020580521,0.0013407874],"genre_scores_gemma":[0.9991532,0.000040474406,0.00020198595,0.00035518437,0.000093950504,6.45279e-8,0.000004249222,8.659958e-7,0.00015002032],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886054,0.000060454746,0.00030529907,0.00013189415,0.00029024383,0.00035154782],"domain_scores_gemma":[0.9991767,0.00006449301,0.00017003491,0.000075148295,0.00014686385,0.0003667549],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00040636322,0.00006654621,0.00019582134,0.000021958673,0.000819276,0.0005531911,0.0004355045,0.00004520691,0.012761025],"category_scores_gemma":[0.000058093203,0.000050678937,0.00012480823,0.00074271765,0.00082766655,0.00021620715,0.0000023725615,0.00015907145,0.0000071081713],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000038463854,0.0000028070024,0.97446924,0.0000026143746,0.000011207247,0.000059302693,0.00022887229,0.0037290694,0.000020437983,8.892482e-7,0.000062670864,0.021409035],"study_design_scores_gemma":[0.00010383219,0.00019087117,0.991912,0.000024645233,0.000014920746,0.0003977609,0.0008631506,0.0012471951,0.000021314347,0.0019663943,0.0031768885,0.0000810026],"about_ca_topic_score_codex":0.52559686,"about_ca_topic_score_gemma":0.99612945,"teacher_disagreement_score":0.47053263,"about_ca_system_score_codex":7.1164897e-7,"about_ca_system_score_gemma":0.0002485944,"threshold_uncertainty_score":0.9881414},"labels":[],"label_agreement":null},{"id":"W4240112461","doi":"10.1139/e09-909","title":"Introduction","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"","field":"","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry","score_opus":0.01925730445301998,"score_gpt":0.23870954993186147,"score_spread":0.21945224547884148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4240112461","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.972853,0.00060541555,0.000037199665,0.013777909,0.001100345,0.00003541299,0.0000037518669,0.0000067915385,0.011580188],"genre_scores_gemma":[0.9969722,0.000002742438,0.0012946511,0.00029680884,0.0011413275,3.7822765e-8,1.5994694e-7,0.0000029778603,0.0002890835],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991001,0.00003642094,0.00020046833,0.00009601934,0.00026241835,0.00030460145],"domain_scores_gemma":[0.9989811,0.000010736344,0.00016347544,0.00007377801,0.00017159116,0.00059930165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011248383,0.00005630048,0.000096014905,0.00058286183,0.00027893516,0.00015735366,0.00030066047,0.000020153102,0.0007620387],"category_scores_gemma":[0.00030038165,0.000045215373,0.000045458466,0.00079529523,0.00032411105,0.0006293015,0.0000012796331,0.00012127562,0.0003677886],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000072175666,0.000095561765,0.2309574,0.000008274111,0.00006623275,0.0010672031,0.004694405,0.019317381,0.061318193,0.07398866,0.50728035,0.10113417],"study_design_scores_gemma":[0.00025535727,0.001034664,0.46530914,0.00003077595,0.000014748425,0.0013366361,0.000460422,0.00015672919,0.0034259039,0.005164629,0.5226213,0.00018969794],"about_ca_topic_score_codex":0.0007084345,"about_ca_topic_score_gemma":0.045130327,"teacher_disagreement_score":0.23435175,"about_ca_system_score_codex":0.000010652232,"about_ca_system_score_gemma":0.0017996699,"threshold_uncertainty_score":0.97229356},"labels":[],"label_agreement":null},{"id":"W4240528286","doi":"10.1139/cjes-38-5-813","title":"Search for a deep-mantle component in mafic lavas using a NbYZr plot","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Mafic; Geology; Geochemistry; Mantle (geology); Petrology","score_opus":0.1053724805425877,"score_gpt":0.2570725887368876,"score_spread":0.1517001081942999,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4240528286","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99551547,0.001702217,0.0005529429,0.0009718568,0.00028251458,0.00009737432,0.0000067489877,0.000001745849,0.0008691365],"genre_scores_gemma":[0.99767995,0.000114163595,0.0019277446,0.00015421637,0.00010025454,2.0692922e-7,0.0000018893797,9.409585e-7,0.000020617947],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990191,0.00004440069,0.00022298767,0.00011568368,0.00019054259,0.00040728704],"domain_scores_gemma":[0.999425,0.00009398755,0.00007084411,0.000038382168,0.00007330415,0.000298464],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008667944,0.0000653803,0.0001418722,0.00021671336,0.0004035035,0.00010327326,0.00021000575,0.000028860637,0.0005460058],"category_scores_gemma":[0.000047141315,0.000046392124,0.00004720561,0.00042531386,0.00023164865,0.00025127723,0.0000035094497,0.00009035876,0.00001934892],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017726012,0.000004573826,0.93955123,0.0000028391494,0.0000036863337,0.00006330789,0.00034816508,0.054670192,0.000025547857,0.00008682986,0.0000451654,0.0051807393],"study_design_scores_gemma":[0.0003802551,0.0006157278,0.9319902,0.000043317454,0.000004898764,0.00014780491,0.0018518856,0.046260756,0.00004278249,0.00085749046,0.017670806,0.00013407237],"about_ca_topic_score_codex":0.03175635,"about_ca_topic_score_gemma":0.56680053,"teacher_disagreement_score":0.5350442,"about_ca_system_score_codex":0.000003253727,"about_ca_system_score_gemma":0.0002957171,"threshold_uncertainty_score":0.9746913},"labels":[],"label_agreement":null},{"id":"W4240662098","doi":"10.1139/cjes-38-4-697","title":"The Cheslatta Lake suite: Miocene mafic, alkaline magmatism in central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mafic; Magmatism; Geology; Geochemistry; Suite; Paleontology; Archaeology; Tectonics","score_opus":0.018338958580312092,"score_gpt":0.22433998844982608,"score_spread":0.206001029869514,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4240662098","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9861488,0.003643608,0.000003264341,0.00254909,0.0006626006,0.000085168285,0.000029028954,0.0000028159025,0.00687562],"genre_scores_gemma":[0.99733645,0.0005660924,0.00020133235,0.00027123844,0.000098730045,2.4115522e-7,0.0000061146156,0.0000014838166,0.0015183494],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99809724,0.00019419056,0.00035520046,0.00016202414,0.00027276613,0.00091856124],"domain_scores_gemma":[0.9987849,0.00031565534,0.00012624986,0.00010047002,0.000083677194,0.0005890362],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001854927,0.00007298945,0.00018530339,0.0001464384,0.000921143,0.0005548208,0.00068181555,0.00008796608,0.0077605345],"category_scores_gemma":[0.00028805446,0.000068990965,0.00005738571,0.0006465736,0.0012984057,0.0003044277,0.0000058418964,0.00036556672,0.00008546511],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005138861,0.0000025319273,0.9934182,0.0000021189846,0.000005608318,0.0008815222,0.0000722239,0.0003601385,3.246509e-7,0.00001353047,0.0009841807,0.004254444],"study_design_scores_gemma":[0.00021380922,0.000121802696,0.96214527,0.000031145097,0.0000033718961,0.002291384,0.00018935194,0.0005212933,8.717963e-7,0.0015120696,0.032888446,0.00008117636],"about_ca_topic_score_codex":0.14657535,"about_ca_topic_score_gemma":0.9995855,"teacher_disagreement_score":0.8530102,"about_ca_system_score_codex":6.915895e-7,"about_ca_system_score_gemma":0.0012254992,"threshold_uncertainty_score":0.9931465},"labels":[],"label_agreement":null},{"id":"W4240786552","doi":"10.1139/cjes-38-3-359","title":"U-Pb ages of granitoid rocks in the northwestern Makkovik Province, Labrador: evidence for 175 million years of episodic synorogenic and postorogenic plutonism","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Plutonism; Geology; Geochemistry; Isochron; Precambrian; Clastic rock; Paleontology; Pluton; Sedimentary rock; Tectonics","score_opus":0.04518655065325993,"score_gpt":0.23517444974431762,"score_spread":0.18998789909105768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4240786552","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9888272,0.010131728,0.00003528052,0.00062638224,0.00013799743,0.0001625688,0.000021862204,0.0000010430435,0.00005590806],"genre_scores_gemma":[0.99848557,0.0010798286,0.00028106212,0.000096245145,0.000039446033,5.756925e-7,0.0000018883775,0.000001032253,0.000014330364],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989786,0.00007234657,0.00032663363,0.00012477783,0.00024174732,0.00025588062],"domain_scores_gemma":[0.9991786,0.00029375177,0.00024228392,0.000068813875,0.00007974276,0.00013683263],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009451099,0.000074824355,0.00018430522,0.00016875626,0.00019156495,0.00004668406,0.00033138625,0.000038329516,0.00005082955],"category_scores_gemma":[0.00016182735,0.00004852419,0.000064975415,0.00036337873,0.00042837873,0.00032603028,0.0000054792727,0.000083217376,0.0000019944657],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024872328,0.0000050763,0.9799043,0.000016305143,0.000007226673,0.000028592809,0.00096718525,0.0011489404,0.00005125253,0.000016653123,0.00002273171,0.01780686],"study_design_scores_gemma":[0.00016904429,0.0008280343,0.99527556,0.00008328889,0.00001394826,0.00009160969,0.0013522024,0.00026253273,0.00005070595,0.00038915832,0.0014180138,0.00006587748],"about_ca_topic_score_codex":0.040595103,"about_ca_topic_score_gemma":0.742749,"teacher_disagreement_score":0.7021539,"about_ca_system_score_codex":0.000002039136,"about_ca_system_score_gemma":0.00032288415,"threshold_uncertainty_score":0.96579367},"labels":[],"label_agreement":null},{"id":"W4241081325","doi":"10.1139/cjes-37-10-1355","title":"The last glaciation of east-central Ellesmere Island, Nunavut: ice dynamics, deglacial chronology, and sea level change","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Chronology; Glacial period; Oceanography; Ice sheet; Deglaciation; Paleontology; Sea ice; Physical geography; Geography","score_opus":0.03268461522829956,"score_gpt":0.23041770180883148,"score_spread":0.1977330865805319,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4241081325","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909983,0.0021343885,0.000005624632,0.0032357785,0.00035750246,0.00007945866,0.00010488912,0.0000016459013,0.0030824079],"genre_scores_gemma":[0.9990533,0.00042109142,0.0000776829,0.00015203988,0.00012233261,2.530667e-7,0.000008902271,0.0000011583757,0.00016326118],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987462,0.0001592702,0.0002479666,0.00013354668,0.00018435153,0.00052865053],"domain_scores_gemma":[0.99918354,0.00017616,0.00014033685,0.000074886986,0.000084148596,0.00034093982],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000869106,0.00008740177,0.0001654743,0.00016465192,0.0007641819,0.00006217325,0.0003716836,0.000095378164,0.0014643045],"category_scores_gemma":[0.0000953457,0.00005872663,0.000042997675,0.00027804982,0.0017889146,0.0002693296,0.000004348851,0.00024085329,0.000033503384],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021584152,0.000002279619,0.9879082,0.0000034537563,0.000011720726,0.000030223366,0.00042492323,0.00015356267,3.1080444e-7,0.00013299391,0.000054525706,0.011256234],"study_design_scores_gemma":[0.0002050228,0.00024935964,0.99291354,0.000016400283,0.000008274485,0.00039261134,0.00047846072,0.0033674126,0.000005411703,0.00024734144,0.0020510405,0.00006511336],"about_ca_topic_score_codex":0.0074556833,"about_ca_topic_score_gemma":0.97648126,"teacher_disagreement_score":0.9690256,"about_ca_system_score_codex":0.0000011071193,"about_ca_system_score_gemma":0.0008514654,"threshold_uncertainty_score":0.9994485},"labels":[],"label_agreement":null},{"id":"W4241764248","doi":"10.1139/e01-009","title":"Facies interpretation of Middle Carboniferous to Lower Permian Pope succession limestone of Cache Creek Group, Fort St. James, central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Université Claude Bernard Lyon 1","keywords":"Geology; Facies; Paleontology; Permian; Carboniferous; Ecological succession; Geochemistry; Structural basin","score_opus":0.017084864468604875,"score_gpt":0.21253383553175553,"score_spread":0.19544897106315065,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4241764248","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98945946,0.0042989426,0.000048695747,0.00018536102,0.0005991816,0.00010813082,0.00013078115,0.00000328363,0.005166149],"genre_scores_gemma":[0.99873567,0.0000767227,0.00092594855,0.00006710581,0.000049302264,2.3365328e-7,0.0000042607344,0.0000010789078,0.00013969066],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99838096,0.000093810464,0.00050234166,0.00018912702,0.00035519386,0.0004785606],"domain_scores_gemma":[0.99873376,0.00007670204,0.0003163714,0.000096964985,0.00015043314,0.00062577793],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006032323,0.00009528822,0.0003118433,0.00021735053,0.0003343832,0.00023642645,0.0004702289,0.00008538738,0.0006850593],"category_scores_gemma":[0.00012638445,0.000108814675,0.00012284356,0.0005506844,0.0007851046,0.0005656478,0.0000019763993,0.0001650794,0.0000011822506],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024894565,0.000010056433,0.9526296,0.000010426948,0.000015884365,0.00014612514,0.0007335101,0.00039068345,0.00004414239,0.000003485437,0.00022883307,0.045762353],"study_design_scores_gemma":[0.00017453449,0.0010842842,0.99594384,0.00020415426,0.00001817962,0.00036154673,0.0010713863,0.00036276455,0.00002604829,0.00017923363,0.00045209896,0.00012193186],"about_ca_topic_score_codex":0.5539919,"about_ca_topic_score_gemma":0.99313104,"teacher_disagreement_score":0.43913913,"about_ca_system_score_codex":0.000002853759,"about_ca_system_score_gemma":0.00089836813,"threshold_uncertainty_score":0.7500919},"labels":[],"label_agreement":null},{"id":"W4242347371","doi":"10.1139/cjes-38-11-1579","title":"Geology of the Chatham Sound region, southeast Alaska and coastal British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Sound (geography); Oceanography; Seismology; Archaeology; Paleontology","score_opus":0.021174039558762257,"score_gpt":0.2101112973742942,"score_spread":0.18893725781553194,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4242347371","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9922933,0.0014613728,0.000005525531,0.0011076164,0.00034963468,0.000057515925,0.0000149926955,0.0000014076877,0.0047086235],"genre_scores_gemma":[0.9988258,0.000093882736,0.000058179794,0.00015070537,0.00005318327,9.9829634e-8,9.128478e-7,9.758013e-7,0.00081626646],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988785,0.00016150487,0.00023605813,0.0001335409,0.00018093338,0.00040946782],"domain_scores_gemma":[0.99914753,0.000120777084,0.00016932708,0.000087464985,0.000121380755,0.00035349518],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007842806,0.00005536454,0.00017896156,0.00010242893,0.00067580777,0.0001303364,0.00042772133,0.00008049476,0.0013711182],"category_scores_gemma":[0.00018985142,0.000050165632,0.000052558324,0.0003519185,0.0032619557,0.00017202865,0.0000101880105,0.00022312887,0.0000103433085],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000034858454,0.0000022476675,0.9989095,0.0000032347857,0.000007601438,0.00016965755,0.00013258468,0.00007451716,4.068918e-7,0.000024695591,0.00018212735,0.000489995],"study_design_scores_gemma":[0.00015198764,0.00018753644,0.9862492,0.000023253204,0.0000060977095,0.008969483,0.0006843345,0.00008237729,0.0000010273872,0.0023328522,0.0012578438,0.000054022075],"about_ca_topic_score_codex":0.096986264,"about_ca_topic_score_gemma":0.9914381,"teacher_disagreement_score":0.89445186,"about_ca_system_score_codex":1.6635578e-7,"about_ca_system_score_gemma":0.0008736254,"threshold_uncertainty_score":0.99954176},"labels":[],"label_agreement":null},{"id":"W4242815848","doi":"10.1139/e2012-077","title":"Erratum: Introduction to fundamental and applied research on permafrost in Canada / Erratum : Recherche fondamentale et appliquée sur le pergélisol au Canada","year":2012,"lang":"fr","type":"erratum","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Permafrost; Oceanography","score_opus":0.19051549050012198,"score_gpt":0.31134629934561486,"score_spread":0.12083080884549288,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4242815848","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8663157,0.008068516,0.0000010587806,0.04466191,0.03126243,0.0008232438,0.0076979734,0.000003619981,0.041165553],"genre_scores_gemma":[0.97334456,0.0007309978,0.0001405775,0.0030869166,0.005543129,0.000009885825,0.0010458975,0.00003286097,0.016065167],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9931032,0.0009492788,0.0009534826,0.000852501,0.0017420023,0.0023995142],"domain_scores_gemma":[0.99502075,0.0007750806,0.00040833926,0.00033990876,0.00030880337,0.0031471269],"candidate_categories":["metaepi_narrow","sts","research_integrity","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00653981,0.00057743775,0.0008243406,0.0012407075,0.001507788,0.0006047777,0.0010865623,0.00039666847,0.0036349886],"category_scores_gemma":[0.00037023798,0.00053948665,0.00008455128,0.0020249642,0.0009922732,0.00068543345,0.00006342547,0.0034684131,0.000038180544],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009330725,0.000031610667,0.3248662,0.00011491601,0.00003073724,0.0002353414,0.0038657556,0.0015146212,0.00016644388,0.00022795332,0.6668834,0.0019696832],"study_design_scores_gemma":[0.0004333103,0.0005617265,0.37700868,0.0004019857,0.000019844387,0.00033378773,0.020370776,0.00013994909,0.00006273515,0.0000814466,0.599973,0.000612737],"about_ca_topic_score_codex":0.9998974,"about_ca_topic_score_gemma":0.9999998,"teacher_disagreement_score":0.16504043,"about_ca_system_score_codex":0.0012944893,"about_ca_system_score_gemma":0.16633491,"threshold_uncertainty_score":0.9997921},"labels":[],"label_agreement":null},{"id":"W4243048298","doi":"10.1139/cjes-2015-0123","title":"<b>Papers commemorating the 30th anniversary of the Royal Tyrrell Museum of Palaeontology</b>","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"History of Science and Natural History","field":"Arts and Humanities","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology; Archaeology; History","score_opus":0.054654811622519166,"score_gpt":0.2101288840612692,"score_spread":0.15547407243875003,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4243048298","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.82170886,0.003698543,9.0640805e-7,0.0040950663,0.0032980815,0.000076358374,0.000014017607,0.0000024649096,0.1671057],"genre_scores_gemma":[0.9975956,0.0000028042812,0.0000470606,0.00033183955,0.00013605837,1.1262094e-7,7.7824744e-8,0.0000018595839,0.0018845855],"study_design_codex":"qualitative","study_design_gemma":"not_applicable","domain_scores_codex":[0.99912584,0.00007618885,0.00024098382,0.000071261624,0.00030229246,0.00018342801],"domain_scores_gemma":[0.9990625,0.000057227924,0.00034697072,0.00010383294,0.00024109863,0.00018837773],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0009547172,0.00006204537,0.0001402535,0.00013791902,0.0006732626,0.000029282395,0.00073111785,0.000022631608,0.00027481245],"category_scores_gemma":[0.00014039614,0.000031855514,0.00009027899,0.00012009195,0.0047132103,0.00022245983,0.000012947315,0.00016970164,0.0000035854075],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000060408613,0.00007254184,0.08970638,0.00005866576,0.00008648127,0.00009424333,0.63890207,0.0046628537,0.0007868095,0.070659734,0.18639742,0.008512417],"study_design_scores_gemma":[0.0002635895,0.00046053744,0.010096368,0.000103533675,0.000029028935,0.000026270242,0.06465829,0.00025291176,0.00014139283,0.00037453897,0.9234658,0.00012775371],"about_ca_topic_score_codex":0.0067144367,"about_ca_topic_score_gemma":0.23981482,"teacher_disagreement_score":0.73706836,"about_ca_system_score_codex":0.000015408585,"about_ca_system_score_gemma":0.0016873911,"threshold_uncertainty_score":0.9998999},"labels":[],"label_agreement":null},{"id":"W4243669650","doi":"10.1139/e07-911","title":"Tribute","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"","field":"","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Tribute; Geochemistry; Archaeology","score_opus":0.05225672585809253,"score_gpt":0.2491660408666428,"score_spread":0.19690931500855025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4243669650","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98730856,0.0008695911,0.000020338714,0.0013302749,0.00052999373,0.000032055967,0.000020806468,0.000005153017,0.009883229],"genre_scores_gemma":[0.99760413,0.0000110672745,0.0011209477,0.00019488519,0.00017396727,1.3950687e-7,2.073638e-7,0.000006691139,0.00088798295],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99877536,0.000048607373,0.00025722026,0.000096481504,0.00037770704,0.00044462577],"domain_scores_gemma":[0.99838793,0.000039226878,0.00019792901,0.00008268039,0.00021585343,0.0010763545],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010008845,0.00007274996,0.00014422089,0.00059178384,0.0006330012,0.00007417689,0.00050007686,0.0000259854,0.0006672894],"category_scores_gemma":[0.00034662016,0.000057416342,0.000078091696,0.0009274665,0.0011021015,0.00054590456,0.000004628996,0.0001449925,0.00061501935],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012004931,0.000015419851,0.90396315,0.0000027372994,0.000029406729,0.002908491,0.0017164622,0.0010153932,0.0017461241,0.0016809303,0.08589864,0.001011217],"study_design_scores_gemma":[0.00043145264,0.00042558106,0.50829697,0.000042874548,0.000010769374,0.0058222366,0.00029842815,0.00009949656,0.0017289246,0.0008200217,0.48182476,0.00019847967],"about_ca_topic_score_codex":0.003697794,"about_ca_topic_score_gemma":0.16266891,"teacher_disagreement_score":0.39592612,"about_ca_system_score_codex":0.000010630545,"about_ca_system_score_gemma":0.0057549975,"threshold_uncertainty_score":0.99988145},"labels":[],"label_agreement":null},{"id":"W4243951515","doi":"10.1139/cjes-38-3-471","title":"Very high temperature, moderate pressure metamorphism in the New Russia gneiss comple×, northeastern Adirondack Highlands, metamorphic aureole to the Marcy anorthosite: Reply","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Anorthosite; Geology; Metamorphism; Gneiss; Geochemistry; Metamorphic rock; Petrology; Plagioclase; Paleontology","score_opus":0.018372102103486103,"score_gpt":0.19581444662866082,"score_spread":0.1774423445251747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4243951515","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95259315,0.00471195,0.000014407255,0.0408631,0.00028564915,0.00016226844,0.000049202237,0.000005221156,0.0013150807],"genre_scores_gemma":[0.9928367,0.000070240945,0.00040734443,0.0053731585,0.00032605973,8.487754e-7,0.000014707726,0.0000025165257,0.000968411],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99754834,0.00029843042,0.00050285336,0.00033994755,0.0006252313,0.00068521267],"domain_scores_gemma":[0.9983828,0.00020046257,0.00020480453,0.00028844352,0.00010489511,0.00081859564],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015172553,0.00022258185,0.00038631726,0.0003154172,0.0006628142,0.00046264537,0.0014114166,0.000064836895,0.004347547],"category_scores_gemma":[0.00015287765,0.00010269946,0.00017748924,0.0017160873,0.0003557578,0.00037790195,0.000016620623,0.00046446087,0.00013433112],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000055632558,0.00001397111,0.93249565,0.0000044729886,0.00006144438,0.00032304905,0.00049429864,0.061431028,0.000051146675,0.00025042446,0.0029805987,0.0018382543],"study_design_scores_gemma":[0.00023376648,0.00028957333,0.8961151,0.00003087415,0.00009632916,0.00033431558,0.00022987506,0.0021593543,0.000059284706,0.0034594792,0.0967813,0.00021075245],"about_ca_topic_score_codex":0.12072683,"about_ca_topic_score_gemma":0.7695297,"teacher_disagreement_score":0.6488028,"about_ca_system_score_codex":0.000001908085,"about_ca_system_score_gemma":0.00061616645,"threshold_uncertainty_score":0.9965626},"labels":[],"label_agreement":null},{"id":"W4244251724","doi":"10.1139/e11-053","title":"E.R. Ward Neale (1923–2008). Photograph by Penny Colton Photographie par Penny Colton.","year":2012,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Literature, Film, and Journalism Analysis","field":"Arts and Humanities","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Penny; Geology; Art; Geography; Archaeology","score_opus":0.019955308659451155,"score_gpt":0.21965453940978266,"score_spread":0.1996992307503315,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4244251724","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6362891,0.30607402,0.000028319891,0.0050387993,0.01581969,0.00041738208,0.0022917432,0.000019608877,0.034021325],"genre_scores_gemma":[0.96454555,0.00525258,0.0003505752,0.002248006,0.004125873,0.000005471789,0.00002411672,0.00004302721,0.023404822],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9947937,0.0004392468,0.0012574085,0.0004094244,0.0010194973,0.0020807083],"domain_scores_gemma":[0.9940266,0.00021725037,0.0011005917,0.00033899903,0.0007706231,0.0035459287],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","insufficient_payload"],"consensus_categories":["sts"],"category_scores_codex":[0.0034710905,0.0005441809,0.0008728907,0.0018610007,0.0036850823,0.002235885,0.0011707753,0.00026440108,0.013799901],"category_scores_gemma":[0.00015274316,0.00045949526,0.00089519215,0.001421423,0.004528526,0.0031233162,0.000032677857,0.00097445055,0.00012244874],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011620051,0.00043400723,0.23806776,0.00023554469,0.0011180226,0.00062820636,0.04996333,0.00006907648,0.0005562026,0.021658542,0.6834936,0.0036594616],"study_design_scores_gemma":[0.00058904715,0.00048857124,0.008895397,0.00039727526,0.0004507239,0.00048044327,0.0070698224,0.000052059277,0.00030264328,0.00045923883,0.98020494,0.00060981116],"about_ca_topic_score_codex":0.047746252,"about_ca_topic_score_gemma":0.27091423,"teacher_disagreement_score":0.32825643,"about_ca_system_score_codex":0.000039138595,"about_ca_system_score_gemma":0.0019934766,"threshold_uncertainty_score":0.99978566},"labels":[],"label_agreement":null},{"id":"W4244870429","doi":"10.1139/e06-123","title":"Erratum: Dynamics of rocky shores: Cretaceous, Pliocene, Pleistocene, and Recent, Baja California peninsula, Mexico","year":2006,"lang":"en","type":"erratum","venue":"Canadian Journal of Earth Sciences","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Cretaceous; Peninsula; Paleontology; Shore; Pleistocene; Rocky shore; Oceanography; Archaeology; Geography","score_opus":0.011583863862795056,"score_gpt":0.20906715413122198,"score_spread":0.19748329026842693,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4244870429","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.2442853,0.29458654,0.00045415643,0.0054972107,0.051257357,0.0013227728,0.009218138,0.00005783297,0.3933207],"genre_scores_gemma":[0.9505396,0.009694286,0.0021688107,0.00078605267,0.002432215,0.0000013274127,0.00094219594,0.000052457985,0.033383053],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99671096,0.00011356102,0.0009045984,0.0004870191,0.00083898124,0.00094485865],"domain_scores_gemma":[0.9968383,0.00014155029,0.0010720555,0.00023455411,0.0004402899,0.0012732572],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010161258,0.0004537382,0.0008648617,0.0009426687,0.000648756,0.00036368959,0.0010587868,0.00044304394,0.0011098548],"category_scores_gemma":[0.0003167004,0.000361931,0.00018439683,0.0011077218,0.0012877997,0.0004641921,0.000019170006,0.0009225639,0.000024652902],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000050717153,0.000013845385,0.42900053,0.00034588858,0.00007781483,0.00041930834,0.00018658712,0.0070461268,9.346845e-7,0.00007993498,0.5496192,0.013159118],"study_design_scores_gemma":[0.0005026009,0.0017578661,0.2936451,0.0011234671,0.00019492072,0.0010310103,0.00046202546,0.051223174,0.00001693751,0.0027533085,0.64628124,0.0010083058],"about_ca_topic_score_codex":0.044017043,"about_ca_topic_score_gemma":0.8273926,"teacher_disagreement_score":0.78337556,"about_ca_system_score_codex":0.000014522196,"about_ca_system_score_gemma":0.0070769386,"threshold_uncertainty_score":0.9998833},"labels":[],"label_agreement":null},{"id":"W4245228971","doi":"10.1139/e00-097","title":"Introduction to special issue of Canadian Journal of Earth Sciences: The Alberta Basement Transect of Lithoprobe","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Basement; Geochronology; Transect; Outcrop; Structural basin; Sedimentary basin; Socle; Sedimentary rock; Crust; Metallogeny; Earth science; Geochemistry; Paleontology; Archaeology; Inversion (geology); Geography; Quartz; Oceanography","score_opus":0.01432102248393761,"score_gpt":0.18817373465690945,"score_spread":0.17385271217297185,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4245228971","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97185475,0.0006300958,0.000009782012,0.014043967,0.00055657834,0.000085414125,0.00004095532,6.2374846e-7,0.012777817],"genre_scores_gemma":[0.9963051,0.000070221315,0.0010054734,0.00038791378,0.001647081,1.1345289e-7,0.0000016590208,0.0000013168751,0.0005811259],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99780047,0.00014347388,0.00075234525,0.00019668229,0.0006002914,0.00050674623],"domain_scores_gemma":[0.99803096,0.00015748186,0.00036185712,0.00012546784,0.0003017313,0.0010225095],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0021147418,0.00013463777,0.00037204876,0.0008727212,0.00046387754,0.000107608466,0.0009108966,0.000053063795,0.069821626],"category_scores_gemma":[0.00034597027,0.00007689044,0.00020953662,0.0025125912,0.001440424,0.00032153644,0.0000032323712,0.00021945311,0.00004139478],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009240999,0.00003756232,0.86631644,0.000027872484,0.000106464875,0.00007204297,0.0038941891,0.07092082,0.00047069316,0.00046728866,0.0071311314,0.0504631],"study_design_scores_gemma":[0.00036368822,0.0030884969,0.6202868,0.00012291413,0.00012122901,0.0003503576,0.001762183,0.0007072441,0.004544954,0.0029392177,0.36541057,0.00030233065],"about_ca_topic_score_codex":0.5525293,"about_ca_topic_score_gemma":0.98080224,"teacher_disagreement_score":0.42827293,"about_ca_system_score_codex":0.0000025483223,"about_ca_system_score_gemma":0.002343944,"threshold_uncertainty_score":0.93102866},"labels":[],"label_agreement":null},{"id":"W4245401403","doi":"10.1139/cjes-2017-0090","title":"Quaternary geology of southern Ontario and applications to hydrogeology / Géologie quaternaire du sud de l’Ontario et applications à l’hydrogéologie","year":2018,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ministry of Energy, Northern Development and Mines; University of Guelph; Natural Resources Canada; Geological Survey of Canada","funders":"","keywords":"Geology; Quaternary; Hydrogeology; Geochemistry; Archaeology; Geomorphology; Paleontology; Geography; Geotechnical engineering","score_opus":0.047212867236735324,"score_gpt":0.267137233312897,"score_spread":0.2199243660761617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4245401403","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9685948,0.004142276,0.00078824227,0.01988651,0.0005991891,0.0003617357,0.000054181935,0.00000639737,0.0055666566],"genre_scores_gemma":[0.9918315,0.00034618322,0.0027025444,0.0010734111,0.0002714216,0.000009949017,0.000009596062,0.0000048959164,0.0037505408],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997077,0.00048275254,0.00065370055,0.000438781,0.00022205822,0.001125742],"domain_scores_gemma":[0.9972808,0.00053306465,0.00038705967,0.0002674308,0.00038586804,0.0011458184],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002537794,0.00023478911,0.0005009938,0.00062818656,0.0007900064,0.00007232777,0.0010842925,0.00037677572,0.0047003096],"category_scores_gemma":[0.00018108102,0.00020911563,0.0000943168,0.0005666793,0.00727112,0.00024777415,0.00005844867,0.0006435035,0.00050724985],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039896946,0.000024508736,0.99081177,0.000016329892,0.000050367533,0.0001275171,0.0046410607,0.0007808365,0.000010927717,0.0013232309,0.00016807446,0.0020055047],"study_design_scores_gemma":[0.00028051992,0.0017941195,0.8293349,0.000038698472,0.00005059131,0.0028598034,0.00096560083,0.00019357432,0.000060084778,0.007820228,0.15638177,0.00022012173],"about_ca_topic_score_codex":0.8392142,"about_ca_topic_score_gemma":0.999573,"teacher_disagreement_score":0.16147685,"about_ca_system_score_codex":0.000013187593,"about_ca_system_score_gemma":0.010752902,"threshold_uncertainty_score":0.9962095},"labels":[],"label_agreement":null},{"id":"W4245505869","doi":"10.1139/cjes-38-5-839","title":"Lithostratigraphy and limiting optical ages of the Pleistocene fill in Fraser River valley near Clinton, south-central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Glacial period; Geology; Lithostratigraphy; Pleistocene; Glacier; Aggradation; Paleontology; Sequence (biology); Bedrock; Geomorphology; Marine isotope stage; Fluvial; Geochemistry; Sedimentary rock; Interglacial; Structural basin","score_opus":0.019251193645793568,"score_gpt":0.21565309868410915,"score_spread":0.1964019050383156,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4245505869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99558157,0.0016225517,0.000001905377,0.0004599854,0.00021442607,0.000075864926,0.000019210085,0.0000013294367,0.0020231442],"genre_scores_gemma":[0.9989177,0.00011305624,0.0007190206,0.0001448107,0.00003736909,1.317463e-7,0.0000010449328,0.0000010443027,0.00006581425],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99863034,0.00016286982,0.0003246708,0.00015291126,0.00021810945,0.0005111103],"domain_scores_gemma":[0.99907714,0.00022334902,0.00013573385,0.00007340038,0.0000804274,0.00040993767],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009837106,0.00006334233,0.00019197214,0.000104235376,0.00049086043,0.00020726927,0.0003715843,0.000088921726,0.00091872487],"category_scores_gemma":[0.0003291747,0.000058648202,0.00006519307,0.00047947295,0.0027354634,0.00020791151,0.000007649865,0.00033367117,0.0000035153787],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007060133,0.0000032739763,0.9977442,0.0000049030136,0.0000062902795,0.00020837976,0.0003639127,0.00037952495,4.4771656e-7,0.000008992834,0.00005504871,0.0012179478],"study_design_scores_gemma":[0.00022070385,0.00020014947,0.9973424,0.00007037801,0.000006230745,0.00042687092,0.0003303766,0.0004885581,0.00000355856,0.0004213793,0.0004227661,0.00006662626],"about_ca_topic_score_codex":0.09683864,"about_ca_topic_score_gemma":0.9837946,"teacher_disagreement_score":0.886956,"about_ca_system_score_codex":3.977326e-7,"about_ca_system_score_gemma":0.00082549936,"threshold_uncertainty_score":0.9999946},"labels":[],"label_agreement":null},{"id":"W4245670646","doi":"10.1139/cjes-37-12-1691","title":"The Margaree orthogneiss: an Ordovician, peri-Gondwanan, mafic-felsic igneous complex in southwestern Newfoundland","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mafic; Felsic; Ordovician; Geology; Geochemistry; Igneous rock; Petrology","score_opus":0.04054808870430459,"score_gpt":0.22099465906665805,"score_spread":0.18044657036235345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4245670646","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9889901,0.0013611283,0.0000041587405,0.0018288603,0.00029019715,0.000084340696,0.000016574115,0.0000043017585,0.007420288],"genre_scores_gemma":[0.99858004,0.00017988417,0.00017799807,0.00048799237,0.00015523589,2.9907102e-7,0.000006415658,0.0000017505196,0.00041040033],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99849105,0.00012390359,0.0003596551,0.00018159061,0.00028739596,0.00055641617],"domain_scores_gemma":[0.9991123,0.000108304244,0.000120708806,0.000108972374,0.00007158999,0.00047808804],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00085902045,0.00012139278,0.00018270861,0.00012936904,0.0012180916,0.00042247173,0.0005435869,0.00004496662,0.005177689],"category_scores_gemma":[0.00006128142,0.00007079444,0.000055148867,0.00051617285,0.00058902986,0.00043575448,0.0000039818283,0.00017038258,0.00014349472],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001539269,0.0000037947948,0.90891165,0.0000011532508,0.0000042676993,0.00009473681,0.00052549684,0.0074549387,0.0000017387388,0.000036698275,0.000059192666,0.08289096],"study_design_scores_gemma":[0.00012521514,0.00052629114,0.9334315,0.000013845464,0.000004537125,0.00010044805,0.0013624124,0.0021302884,3.0055384e-7,0.0008300778,0.061366666,0.00010840421],"about_ca_topic_score_codex":0.08865691,"about_ca_topic_score_gemma":0.98456484,"teacher_disagreement_score":0.89590794,"about_ca_system_score_codex":0.0000036782405,"about_ca_system_score_gemma":0.0003827822,"threshold_uncertainty_score":0.9957317},"labels":[],"label_agreement":null},{"id":"W4245920193","doi":"10.1139/cjes-38-8-1141","title":"Holocene and latest Pleistocene fluctuations of Stutfield Glacier, Canadian Rockies","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Holocene; Glacier; Pleistocene; Physical geography; Paleontology; Geomorphology; Earth science; Geography","score_opus":0.029643780222716038,"score_gpt":0.2181106452357252,"score_spread":0.18846686501300916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4245920193","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9878859,0.005086478,0.000024469942,0.0022130464,0.00035823573,0.000055229462,0.00004962303,0.000002082145,0.004324973],"genre_scores_gemma":[0.9980164,0.00047098947,0.0009026005,0.00032481077,0.00007980255,1.2677805e-7,0.0000026317127,0.0000013384056,0.00020127113],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990979,0.00001980384,0.00026659248,0.00010945235,0.0001763181,0.0003299659],"domain_scores_gemma":[0.9988832,0.000112123635,0.00013429324,0.000070796516,0.00016226163,0.00063733646],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00036232732,0.00008147772,0.00016191567,0.0002058124,0.00065036694,0.000083379986,0.00022919547,0.000035915116,0.0013457296],"category_scores_gemma":[0.00020926226,0.00006530503,0.00003886376,0.00063555577,0.00044755696,0.00028240366,0.0000033799938,0.00009336884,0.000005847375],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021810122,0.0000015642515,0.99129283,0.0000022809234,0.000009688769,0.000025960846,0.00030657992,0.0018046,0.0000018555893,0.00017779152,0.0004405728,0.005934092],"study_design_scores_gemma":[0.00009819616,0.00020389631,0.97091883,0.000019375151,0.000011080169,0.00008553124,0.00093542784,0.0007326816,0.0000067276624,0.00038504443,0.02652559,0.000077639044],"about_ca_topic_score_codex":0.65870583,"about_ca_topic_score_gemma":0.9897553,"teacher_disagreement_score":0.33104944,"about_ca_system_score_codex":0.0000028361521,"about_ca_system_score_gemma":0.0015944755,"threshold_uncertainty_score":0.99956715},"labels":[],"label_agreement":null},{"id":"W4246339786","doi":"10.1139/cjes-38-2-229","title":"Late Maastrichtian age of spherule deposits in northeastern Me×ico: implication for Chic×ulub scenario","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology; Cretaceous; Geochemistry","score_opus":0.023139713303714705,"score_gpt":0.21058784173724407,"score_spread":0.18744812843352937,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4246339786","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995435,0.0009106185,0.000069788846,0.0009388117,0.00017241277,0.0001052831,0.00001921935,0.000001949737,0.0023469257],"genre_scores_gemma":[0.99894595,0.000041997104,0.00061738753,0.00009841495,0.00008314982,3.9696565e-7,0.0000042706865,0.0000010156579,0.00020740417],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895155,0.00003232688,0.00031479212,0.00014235027,0.00018445204,0.00037454744],"domain_scores_gemma":[0.99927515,0.00008233874,0.00017386588,0.000059221355,0.00008956233,0.00031985986],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036799064,0.000088423585,0.00021329067,0.00014045395,0.00021111757,0.000056056666,0.0003148336,0.000038101007,0.0002292518],"category_scores_gemma":[0.000086137836,0.00005990868,0.000075047064,0.0005457386,0.00029787156,0.00020038006,0.00000488072,0.0000982938,0.000027082611],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012787049,0.00000778851,0.9771319,0.0000051576017,0.0000059385047,0.000029267932,0.00014905851,0.0031065126,0.00003825751,0.000041813822,0.000008754039,0.01946279],"study_design_scores_gemma":[0.00018463345,0.0004345693,0.9935073,0.00002938427,0.0000068740496,0.000025862353,0.00013773273,0.0006964561,0.00005564351,0.0019317158,0.0029119994,0.00007783115],"about_ca_topic_score_codex":0.027018068,"about_ca_topic_score_gemma":0.7564423,"teacher_disagreement_score":0.72942424,"about_ca_system_score_codex":0.0000015184065,"about_ca_system_score_gemma":0.0002395747,"threshold_uncertainty_score":0.9794611},"labels":[],"label_agreement":null},{"id":"W4246392186","doi":"10.1139/cjes-2019-0005","title":"Hydrochronology of a proposed deep geological repository for low- and intermediate-level nuclear waste in southern Ontario from U–Pb dating of secondary minerals: response to Alleghanian events","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Nuclear Waste Management Organization; University of Windsor; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Nuclear Waste Management Organization","keywords":"Geology; Geochemistry; Sedimentary rock; Calcite; Dolomite; Ankerite; Evaporite; Plutonism; Thermal ionization mass spectrometry; Siderite; Mineralogy; Paleontology; Magmatism; Tectonics","score_opus":0.01416253784723249,"score_gpt":0.18868443091213588,"score_spread":0.1745218930649034,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4246392186","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99894696,0.00017230856,0.000008243703,0.00028492004,0.000113884525,0.000114233255,0.00006091187,0.000001094086,0.00029744516],"genre_scores_gemma":[0.9970198,0.0000012968917,0.0026174102,0.00012810006,0.000027087954,1.8768039e-7,0.000004556784,0.0000012615797,0.00020024901],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873185,0.00011921085,0.00048435625,0.00021466218,0.00016172434,0.0002882032],"domain_scores_gemma":[0.9989413,0.000285847,0.00027324384,0.00008315566,0.000081224985,0.000335242],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00076564937,0.00009624034,0.0003474427,0.00024444453,0.00007115546,0.000019952886,0.00035867613,0.00007370748,0.002572755],"category_scores_gemma":[0.00029503813,0.00006592624,0.000076394186,0.00020064526,0.00031605607,0.00012359538,0.000017917248,0.00015333804,0.000009238427],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033434795,0.000011513251,0.98386747,0.000013633884,0.00002249544,0.000025722446,0.0023428646,0.0017164611,0.010363481,0.000003906567,0.0000061933374,0.0012919023],"study_design_scores_gemma":[0.0005426517,0.0017485159,0.9885743,0.00012396256,0.000016283553,0.000025163363,0.0033005513,0.0031807246,0.0010446603,0.0011672431,0.00014859212,0.0001273339],"about_ca_topic_score_codex":0.18478581,"about_ca_topic_score_gemma":0.8722417,"teacher_disagreement_score":0.68745583,"about_ca_system_score_codex":0.0000041602248,"about_ca_system_score_gemma":0.000554421,"threshold_uncertainty_score":0.99833906},"labels":[],"label_agreement":null},{"id":"W4246992839","doi":"10.1139/e11-029","title":"Title page and photo montage","year":2011,"lang":"en","type":"paratext","venue":"Canadian Journal of Earth Sciences","topic":"Earthquake and Disaster Impact Studies","field":"Social Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology; Geochemistry; Computer graphics (images); Computer science","score_opus":0.061472174196054795,"score_gpt":0.303648193648709,"score_spread":0.24217601945265418,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4246992839","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0080725,0.009089718,0.0000027975884,0.00022953897,0.0017215508,0.000042785185,0.000022840297,0.0000013915492,0.9808169],"genre_scores_gemma":[0.56607866,0.002617457,0.00018309268,0.0005449322,0.0009758211,6.6899366e-7,9.723717e-7,0.000009033308,0.4295894],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.999275,0.000047886315,0.00013575122,0.00008577609,0.00018518284,0.00027037374],"domain_scores_gemma":[0.9992733,0.000034890338,0.00013457466,0.000047844675,0.00006812267,0.0004412414],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0004921773,0.00007579973,0.00015874431,0.00019385142,0.00050215225,0.00015184985,0.00023254538,0.00007559737,0.016893899],"category_scores_gemma":[0.00009040324,0.00005995761,0.00004901344,0.00015047468,0.00080385926,0.00015234698,0.000009244765,0.00013429072,0.0012010558],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000020585908,0.0000049407568,0.0033257983,0.0000150415735,0.000030848907,0.00006241898,0.01798674,8.0420244e-7,0.000004127314,0.0014842695,0.9729205,0.004162497],"study_design_scores_gemma":[0.000035050336,0.00006132822,0.0015558162,0.000056644818,0.000009087921,0.0000069870134,0.0023825478,3.1717178e-7,0.000007310223,0.0002418755,0.99555993,0.00008308159],"about_ca_topic_score_codex":0.024980579,"about_ca_topic_score_gemma":0.30062568,"teacher_disagreement_score":0.55800617,"about_ca_system_score_codex":0.000005045712,"about_ca_system_score_gemma":0.0022466262,"threshold_uncertainty_score":0.9995766},"labels":[],"label_agreement":null},{"id":"W4247177411","doi":"10.1139/cjes-37-6-901","title":"Spatial distribution of surficial sediments in part of the Kingston basin of northeastern Lake Ontario, Canada","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Winnowing; Structural basin; Slumping; Sediment; Deposition (geology); Sedimentary rock; Erosion; Channel (broadcasting); Sediment transport; Geomorphology; Oceanography; Paleontology; Archaeology","score_opus":0.012710162054337093,"score_gpt":0.17896309932176388,"score_spread":0.1662529372674268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4247177411","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970872,0.00008044527,0.000002618341,0.00023779579,0.0002584388,0.000040927585,0.00020327055,2.640647e-7,0.0020890445],"genre_scores_gemma":[0.9998173,0.0000039327874,0.000023013294,0.000043869753,0.000019587136,4.1904187e-8,0.000008523729,3.5929642e-7,0.00008336544],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990396,0.00004547904,0.00038197683,0.000057301277,0.0003031107,0.00017255158],"domain_scores_gemma":[0.99943995,0.00004562252,0.00024940225,0.000050535957,0.000093109265,0.00012135431],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041996952,0.00005211405,0.00014824788,0.000059871585,0.000102116515,0.000012633488,0.00027470983,0.000025626929,0.0047194636],"category_scores_gemma":[0.00005253019,0.00003253117,0.000037524012,0.00035590903,0.00027711072,0.00015522953,0.000001880853,0.00008647149,8.6792545e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009973118,0.000003743535,0.9874619,0.0000051108937,0.0000024653061,0.000002362268,0.00018104482,0.00750269,8.3673905e-7,0.000010440783,0.000043816428,0.004775568],"study_design_scores_gemma":[0.00009154008,0.0001330795,0.98658884,0.000052158437,0.000004457764,0.000009487522,0.00010251295,0.00018380319,0.0001451639,0.000069094174,0.012584376,0.00003550109],"about_ca_topic_score_codex":0.98919296,"about_ca_topic_score_gemma":0.9999741,"teacher_disagreement_score":0.012540559,"about_ca_system_score_codex":0.0000036030522,"about_ca_system_score_gemma":0.0035422621,"threshold_uncertainty_score":0.99619037},"labels":[],"label_agreement":null},{"id":"W4247320439","doi":"10.1139/e08-913","title":"ContentsVolume 45, 2008","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Diverse Scientific and Economic Studies","field":"Economics, Econometrics and Finance","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry","score_opus":0.09082084900289605,"score_gpt":0.19784567484004106,"score_spread":0.10702482583714501,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4247320439","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5785502,0.006244051,0.00011005893,0.000752022,0.005361039,0.00005736323,0.000121102355,0.0000046017867,0.40879956],"genre_scores_gemma":[0.94660354,0.00016398562,0.0005654256,0.00030096676,0.00012008348,3.7760503e-7,2.573607e-7,0.0000033136603,0.05224203],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990642,0.0000057919997,0.0004093107,0.00016337131,0.000038677703,0.00031865473],"domain_scores_gemma":[0.99916995,0.00001833454,0.00030252512,0.000087111155,0.000060410777,0.00036166387],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007166707,0.000068721325,0.00023979391,0.0004142656,0.00050543365,0.00008208198,0.00035666575,0.00002829807,0.005395809],"category_scores_gemma":[0.00016076153,0.00006763182,0.00009953578,0.00026032433,0.00076962373,0.00041896224,0.000012034972,0.00008109097,0.00318521],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000030188298,0.000012350263,0.77156377,0.0000028187485,0.000045990408,0.00011688038,0.0013859329,0.000266505,0.0000039805745,0.03148914,0.19492853,0.00018106164],"study_design_scores_gemma":[0.00032742298,0.0001060639,0.13224058,0.000012992645,0.000002688349,0.00018043698,0.0007192901,0.0003352451,0.0000193256,0.0016214356,0.86426884,0.0001656559],"about_ca_topic_score_codex":0.0034744076,"about_ca_topic_score_gemma":0.0044784737,"teacher_disagreement_score":0.6693403,"about_ca_system_score_codex":0.000011130153,"about_ca_system_score_gemma":0.00034922565,"threshold_uncertainty_score":0.9975909},"labels":[],"label_agreement":null},{"id":"W4247429055","doi":"10.1139/cjes-38-11-1541","title":"Petrogenesis of the Early Proterozoic Matachewan dyke swarm, Canada, and implications for magma emplacement and subsequent deformation","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Petrogenesis; Proterozoic; Magma; Deformation (meteorology); Geochemistry; Petrology; Volcano; Seismology; Basalt; Tectonics","score_opus":0.01880111961239185,"score_gpt":0.19943019406392573,"score_spread":0.18062907445153387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4247429055","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99549985,0.00058822567,0.000040128878,0.0034956057,0.000049194292,0.0001073461,0.00008932711,7.0723195e-7,0.00012963242],"genre_scores_gemma":[0.99941087,0.000025385378,0.00033598556,0.00016929614,0.00001942555,8.1503623e-7,0.000002603933,5.178719e-7,0.000035092093],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99932104,0.00002586378,0.00022442659,0.000090250345,0.00013849622,0.00019990865],"domain_scores_gemma":[0.9993507,0.000052720847,0.000160177,0.000058063626,0.000094869756,0.00028342594],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032687793,0.00005966392,0.0001105183,0.00007159872,0.00031255514,0.00005520237,0.0001897247,0.000019024208,0.0001769101],"category_scores_gemma":[0.00006158767,0.000033676624,0.000038199192,0.00025517892,0.0002639377,0.00013613133,0.000005228417,0.00004592871,3.4241918e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000035364367,0.0000012511216,0.9972581,0.0000051595503,0.000006995849,7.565849e-7,0.00005140681,0.00026375309,0.00005363115,0.000054248274,0.000021959828,0.0022791582],"study_design_scores_gemma":[0.00007669455,0.00010825997,0.99625754,0.0000099839735,0.000018555042,0.000063346924,0.00011602304,0.00031178896,0.0003348745,0.0019226853,0.0007331807,0.00004703976],"about_ca_topic_score_codex":0.6873415,"about_ca_topic_score_gemma":0.99208456,"teacher_disagreement_score":0.30474305,"about_ca_system_score_codex":0.0000025784718,"about_ca_system_score_gemma":0.00056510954,"threshold_uncertainty_score":0.3147405},"labels":[],"label_agreement":null},{"id":"W4247548524","doi":"10.1139/cjesauthor01","title":"Authors Index / Index des auteursVolume 38, 2001","year":2001,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Diverse Scientific and Economic Studies","field":"Economics, Econometrics and Finance","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Index (typography)","score_opus":0.06938540363206856,"score_gpt":0.22749700565849207,"score_spread":0.1581116020264235,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4247548524","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5211602,0.060217187,0.00093803566,0.007603363,0.038956262,0.00015690748,0.00038500663,0.000008728694,0.37057436],"genre_scores_gemma":[0.5345948,0.002946368,0.0009138018,0.00038430246,0.00057875074,9.5193866e-7,7.0351524e-7,0.000013292911,0.46056703],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99719036,0.00003960052,0.0009843669,0.0004409276,0.00010869656,0.0012360394],"domain_scores_gemma":[0.9975767,0.0000655002,0.00082633505,0.00020599407,0.00017077275,0.0011546619],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0032890686,0.00022189535,0.0005669431,0.0012634991,0.0010594748,0.0007546716,0.0008863147,0.00016532309,0.03226596],"category_scores_gemma":[0.00047995936,0.00025737635,0.0002561718,0.0012068588,0.0031479814,0.001457997,0.000049456485,0.00034376408,0.0031970793],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006041709,0.000022856622,0.84249103,0.000012033806,0.00007538728,0.00015878947,0.0013726287,0.0020139194,2.8015228e-7,0.00801546,0.14105661,0.0047749337],"study_design_scores_gemma":[0.00031318163,0.00015224764,0.19808719,0.00010886107,0.000011225514,0.0002040871,0.0024401934,0.0034403282,0.0000014869551,0.0062239836,0.78874964,0.00026760384],"about_ca_topic_score_codex":0.020882,"about_ca_topic_score_gemma":0.12339233,"teacher_disagreement_score":0.647693,"about_ca_system_score_codex":0.000096412936,"about_ca_system_score_gemma":0.001314931,"threshold_uncertainty_score":0.99998784},"labels":[],"label_agreement":null},{"id":"W4247605484","doi":"10.1139/cjes-2019-0179","title":"Ali Mehmet Celâl Şengör: A geologist who unravels the histories of continents and oceans","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Marine and environmental studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor","funders":"","keywords":"Geologist; Geology; Tectonics; Plate tectonics; Earth science; Planet; Astrobiology; Paleontology","score_opus":0.01375953175117466,"score_gpt":0.17737948934368156,"score_spread":0.1636199575925069,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4247605484","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9801053,0.0026917148,0.000004447078,0.001775541,0.000386682,0.000059212194,0.000025801966,0.0000010373503,0.014950284],"genre_scores_gemma":[0.9983751,0.00018066738,0.00011257899,0.00020799994,0.00003661411,5.2324623e-8,8.245728e-7,8.8199647e-7,0.0010852672],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99920434,0.000040431656,0.00020689284,0.000102495986,0.00021540419,0.0002304444],"domain_scores_gemma":[0.9994385,0.00009976772,0.00016991394,0.00007078238,0.000028423645,0.00019260064],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005857401,0.00007765225,0.00017885964,0.00008727305,0.00027243007,0.000051595165,0.0002731101,0.000022491775,0.0012987973],"category_scores_gemma":[0.00006160319,0.000044639284,0.00004110404,0.00016176647,0.0010706678,0.00019670717,0.000010539822,0.00008784755,0.000010143003],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000035042037,0.0000012020785,0.9967238,0.000004296496,0.00001091813,0.0000070784704,0.000514852,0.00022558407,0.0000065517193,0.00012984636,0.00040569884,0.0019667018],"study_design_scores_gemma":[0.00010897819,0.00027317108,0.9320979,0.000013386673,0.0000099813105,0.000039425773,0.0012499422,0.00015624429,0.00004529938,0.00023860119,0.06570434,0.000062693594],"about_ca_topic_score_codex":0.04012162,"about_ca_topic_score_gemma":0.27786326,"teacher_disagreement_score":0.23774163,"about_ca_system_score_codex":0.0000015636459,"about_ca_system_score_gemma":0.00017203335,"threshold_uncertainty_score":0.9996142},"labels":[],"label_agreement":null},{"id":"W4247749947","doi":"10.1139/cjes-38-4-619","title":"New UPb age constraints on latest Cretaceous magmatism and associated mineralization in the Fawnie Range, Nechako Plateau, central British Columbia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Magmatism; Geology; Cretaceous; Plateau (mathematics); Geochemistry; Central asia; Zircon; Mineralization (soil science); Basin and range topography; Range (aeronautics); Paleontology; Structural basin; Physical geography; Tectonics; Geography","score_opus":0.013555131634511046,"score_gpt":0.18380529305272378,"score_spread":0.17025016141821273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4247749947","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930594,0.0006955749,0.00001118906,0.0016337949,0.00011499767,0.0000633038,0.000029527515,0.000002968258,0.0043892204],"genre_scores_gemma":[0.9985335,0.00012361034,0.00015320092,0.00078755734,0.000054306453,8.797548e-8,0.0000126058385,8.5552085e-7,0.00033428505],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988208,0.00010270095,0.0002583907,0.00014582262,0.0002666315,0.00040568988],"domain_scores_gemma":[0.9991847,0.00014915745,0.00012646883,0.00004448576,0.000040562998,0.0004546045],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005601105,0.00007393768,0.00017882408,0.00008995366,0.00027640018,0.0006114618,0.00027224014,0.000059818707,0.007665642],"category_scores_gemma":[0.00029748163,0.00006111541,0.000050992232,0.00061244704,0.00040632903,0.00018141455,0.0000026692246,0.00017903323,0.000010307026],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001912371,0.0000042971055,0.9776466,0.0000010125364,0.00000646053,0.0007016791,0.00014631054,0.0011664161,0.0000040234736,0.000012020181,0.0011501975,0.019159092],"study_design_scores_gemma":[0.00023982958,0.0001747638,0.9923801,0.000045278975,0.000011561787,0.0003177522,0.00016890564,0.0011663246,9.104188e-7,0.0039548236,0.0014523172,0.00008746791],"about_ca_topic_score_codex":0.42594984,"about_ca_topic_score_gemma":0.9923691,"teacher_disagreement_score":0.56641924,"about_ca_system_score_codex":0.0000021511125,"about_ca_system_score_gemma":0.00024328846,"threshold_uncertainty_score":0.9932415},"labels":[],"label_agreement":null},{"id":"W4247761021","doi":"10.1139/cjes-2013-0014","title":"Announcement / Communiqué","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Diverse Scientific and Economic Studies","field":"Economics, Econometrics and Finance","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry","score_opus":0.06527005938950167,"score_gpt":0.2034230505760456,"score_spread":0.13815299118654392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4247761021","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.32255012,0.0030948166,0.00006807308,0.0019161559,0.003309917,0.0000888718,0.000061254956,0.0000033107826,0.66890746],"genre_scores_gemma":[0.9737461,0.00006546811,0.0012670977,0.00050907274,0.00007414651,0.000001337196,3.4625432e-7,0.000002747837,0.02433364],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.999233,0.0000065485233,0.00035496196,0.0001092321,0.00002972747,0.00026649993],"domain_scores_gemma":[0.9993019,0.00001900907,0.00025428514,0.000101553065,0.000059982653,0.00026325035],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00088527286,0.0000569527,0.00017563661,0.0003112724,0.0003252739,0.00025460796,0.00040737423,0.000019445677,0.015181356],"category_scores_gemma":[0.00007143204,0.000053105956,0.00006231404,0.00019626744,0.0004040065,0.000508995,0.000017551944,0.000070978786,0.0055572037],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000013802403,0.000021383972,0.47484028,0.0000065724134,0.000068784204,0.000012898724,0.0026556395,0.0003073255,0.000011347829,0.17696242,0.34357902,0.0015329375],"study_design_scores_gemma":[0.00018624577,0.00011278315,0.063730225,0.000015634834,0.00000200754,0.000015386579,0.0020156207,0.0003310775,0.000014814602,0.012320037,0.9211182,0.00013794407],"about_ca_topic_score_codex":0.00960253,"about_ca_topic_score_gemma":0.0069678095,"teacher_disagreement_score":0.651196,"about_ca_system_score_codex":0.000011239209,"about_ca_system_score_gemma":0.00018725925,"threshold_uncertainty_score":0.9969926},"labels":[],"label_agreement":null},{"id":"W4248189207","doi":"10.1139/e01-059","title":"A review of <i>Leidyosuchus canadensis</i> Lambe, 1907 (Archosauria: Crocodylia) and an assessment of cranial variation based upon new material","year":2001,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Taxon; Paleontology; Fibrous joint; Foramen; Cretaceous; Variation (astronomy); Geology; Biology; Anatomy; Geography","score_opus":0.03980319738008615,"score_gpt":0.31242074261949765,"score_spread":0.2726175452394115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4248189207","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0012069971,0.9955765,0.00004460931,0.00029971494,0.0011309849,0.00027748724,0.00046979677,0.0000023936632,0.0009915136],"genre_scores_gemma":[0.002271475,0.9942566,0.0026550668,0.0002970572,0.0003907845,6.1402017e-7,0.0001031373,0.0000032564724,0.000022016673],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99737114,0.0005873023,0.0010284272,0.0002875136,0.00030324585,0.0004223802],"domain_scores_gemma":[0.9974642,0.00021836374,0.0012531234,0.0001634437,0.00017810766,0.00072281],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018879247,0.00024056352,0.0012844391,0.0005299922,0.0002137622,0.00003685539,0.00055383245,0.00023759338,0.001814368],"category_scores_gemma":[0.00016928121,0.00017987764,0.00018609138,0.00061854976,0.0006257949,0.0003042167,0.0000051922652,0.0002776312,0.0000022710105],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007578582,0.00004763088,0.101230875,0.024222143,0.00028655143,0.00044035428,0.00014237639,0.00031408633,0.000006379117,0.00039742375,0.003833183,0.86900324],"study_design_scores_gemma":[0.0003453632,0.0014615414,0.13744006,0.02208554,0.0005567037,0.0008951665,0.000017613047,0.00025780057,7.5936276e-7,0.00029091278,0.8362773,0.00037126517],"about_ca_topic_score_codex":0.07863528,"about_ca_topic_score_gemma":0.68032414,"teacher_disagreement_score":0.86863196,"about_ca_system_score_codex":0.000007621875,"about_ca_system_score_gemma":0.013046648,"threshold_uncertainty_score":0.9990981},"labels":[],"label_agreement":null},{"id":"W4248414623","doi":"10.1139/cjes-2016-0082","title":"Early–Middle Paleozoic Ecosystem Evolution and Revolution (Part 2 of 2) / Évolution et révolution des écosystèmes du Paléozoïque précoce et moyen (Partie 2 de 2)","year":2016,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Paleozoic; Geology; Paleontology","score_opus":0.03243137653924546,"score_gpt":0.21615733106521187,"score_spread":0.1837259545259664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4248414623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9087155,0.07766744,0.002500623,0.0025053818,0.0015945544,0.00019147182,0.00031880644,0.00000958353,0.0064966492],"genre_scores_gemma":[0.99486524,0.003084397,0.001500115,0.0000446032,0.0002932082,0.0000014109798,0.0000021059404,0.0000030642511,0.00020584083],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9962666,0.0011180702,0.0008818242,0.0003625707,0.0004621664,0.0009087485],"domain_scores_gemma":[0.99712753,0.00046784023,0.0008626268,0.00016450313,0.0004106264,0.000966845],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005105913,0.0002718989,0.00046564316,0.0006433525,0.00081742986,0.00014283668,0.0004051226,0.00031804186,0.00027677548],"category_scores_gemma":[0.00077573763,0.00021001304,0.0001865094,0.0006631723,0.0025984764,0.0022228537,0.000004612141,0.00030189854,0.000011671601],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004425516,0.000020071284,0.97735023,0.00011111156,0.00005427322,0.000054176417,0.0012678768,0.00035185137,0.00024023677,0.0073684948,0.00040293008,0.012734458],"study_design_scores_gemma":[0.0004908961,0.0011628752,0.9804541,0.0019479102,0.000081063736,0.001024951,0.00046496655,0.0012609999,0.00011027366,0.010900878,0.001846321,0.0002547539],"about_ca_topic_score_codex":0.039366197,"about_ca_topic_score_gemma":0.80124086,"teacher_disagreement_score":0.7618747,"about_ca_system_score_codex":0.000043717384,"about_ca_system_score_gemma":0.004080389,"threshold_uncertainty_score":0.96703076},"labels":[],"label_agreement":null},{"id":"W4248691001","doi":"10.1139/cjes-38-6-909","title":"A paleoecological analysis of a southern permafrost peatland, Charlevoix, Quebec","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Peat; Permafrost; Geology; Physical geography; Earth science; Archaeology; Oceanography; Geography","score_opus":0.028585775314361257,"score_gpt":0.2436338067976612,"score_spread":0.21504803148329993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4248691001","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921445,0.0012240814,0.000014179898,0.0008909723,0.00016228965,0.000046123452,0.00012315734,0.000002346198,0.005392322],"genre_scores_gemma":[0.9990612,0.00005828651,0.00012884548,0.00015053911,0.00004941128,1.4460235e-7,0.00001772705,8.4064294e-7,0.00053297885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984932,0.00019385677,0.00035866015,0.00016608588,0.0002807787,0.00050742406],"domain_scores_gemma":[0.9986952,0.00028020886,0.00021265192,0.00010462237,0.00015585306,0.0005514895],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012943675,0.00009827211,0.0003673648,0.000986202,0.0003538955,0.0000585104,0.00053400866,0.000103313345,0.014984522],"category_scores_gemma":[0.0002107482,0.000066872795,0.00018209244,0.0015013935,0.0013065854,0.00016249377,0.0000047667445,0.00023263846,0.00013481961],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018479886,0.000005231728,0.99706984,0.0000022018116,0.000100172416,0.00025825785,0.00048341227,0.0016175313,0.0000033404035,0.000032423744,0.000024771027,0.00038436102],"study_design_scores_gemma":[0.00013652974,0.0002475217,0.9952346,0.00000844202,0.00009908065,0.0002454333,0.0010255818,0.001275051,0.000003930572,0.00010659426,0.00153867,0.00007857755],"about_ca_topic_score_codex":0.03914336,"about_ca_topic_score_gemma":0.9827059,"teacher_disagreement_score":0.94356257,"about_ca_system_score_codex":4.7682875e-7,"about_ca_system_score_gemma":0.0011297681,"threshold_uncertainty_score":0.9859159},"labels":[],"label_agreement":null},{"id":"W4248691235","doi":"10.1139/e2012-034","title":"Fundamental and applied research on permafrost in Canada / Recherche fondamentale et appliquée sur le pergélisol au Canada","year":2012,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Permafrost; Humanities; Philosophy; Oceanography","score_opus":0.3031011907087479,"score_gpt":0.3292318405538333,"score_spread":0.026130649845085396,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4248691235","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9557989,0.012262585,3.9702635e-7,0.010867141,0.0022751128,0.00021201032,0.0030021274,9.905114e-7,0.015580704],"genre_scores_gemma":[0.9959455,0.00053962995,0.00008548665,0.001873609,0.00049822195,0.0000016958675,0.00007998649,0.000008659277,0.00096718594],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9959137,0.0005966901,0.0004968521,0.00030758695,0.0009461352,0.0017390478],"domain_scores_gemma":[0.9963676,0.001134527,0.00017767903,0.00014607233,0.00010313891,0.002070989],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.005418545,0.00024856496,0.00036392862,0.00043522604,0.0008517561,0.00026643425,0.0005314792,0.00013214706,0.0037277131],"category_scores_gemma":[0.00016132685,0.0002275975,0.000042707812,0.00094495807,0.00089915324,0.00067373336,0.000026811842,0.0011371052,0.000020463267],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029364703,0.000022369648,0.98215467,0.00004200447,0.0000116578485,0.00014654499,0.003431912,0.00059440563,0.00008759314,0.00048222666,0.009852476,0.0031447893],"study_design_scores_gemma":[0.00050501927,0.00025692786,0.79882175,0.00022166417,0.000008222003,0.000288416,0.028778518,0.0002303006,0.00020460086,0.000056844696,0.17031752,0.00031024247],"about_ca_topic_score_codex":0.9999633,"about_ca_topic_score_gemma":0.9999998,"teacher_disagreement_score":0.18333292,"about_ca_system_score_codex":0.00052047643,"about_ca_system_score_gemma":0.090348735,"threshold_uncertainty_score":0.997183},"labels":[],"label_agreement":null},{"id":"W4249052553","doi":"10.1139/cjes-2016-0138","title":"Uniformitarianism and Plate Tectonics: A Tribute to Kevin C.A. Burke and John F. Dewey / L’uniformitarisme et la tectonique des plaques : hommage à Kevin C.A. Burke et à John F. Dewey","year":2016,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismology and Earthquake Studies","field":"Computer Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Tribute; Art history; Art","score_opus":0.028622753853614902,"score_gpt":0.26457420553265276,"score_spread":0.23595145167903786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4249052553","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.87297755,0.025519013,0.022165254,0.072450645,0.0015082476,0.00044506532,0.00017128867,0.000042359778,0.004720583],"genre_scores_gemma":[0.95409995,0.006849659,0.032050487,0.003230838,0.00018409755,0.000008565019,0.000001059512,0.00002872494,0.0035466012],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9954147,0.0008172943,0.00091765774,0.0007710806,0.0005114966,0.0015677806],"domain_scores_gemma":[0.9953178,0.0013173276,0.00048170998,0.0003958207,0.00052490714,0.0019624184],"candidate_categories":["metaepi_narrow","sts","scholarly_communication"],"consensus_categories":["sts"],"category_scores_codex":[0.0064338767,0.0005602568,0.00080359227,0.0011059453,0.0015858758,0.0012469568,0.001248305,0.00036380813,0.00012668456],"category_scores_gemma":[0.0016264629,0.00041411485,0.0001685215,0.0011262944,0.0034256456,0.0032287608,0.00032263884,0.0007785738,0.000036641635],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025931842,0.0001776267,0.33007282,0.00031420478,0.0008997055,0.007138234,0.039824467,0.00075082737,0.0010819504,0.2945525,0.0079295095,0.31699884],"study_design_scores_gemma":[0.0016625772,0.0036475474,0.559097,0.0026426753,0.00013504927,0.009956044,0.0013940036,0.00064651156,0.0010221186,0.04534466,0.3731649,0.0012869228],"about_ca_topic_score_codex":0.011585496,"about_ca_topic_score_gemma":0.25012848,"teacher_disagreement_score":0.3652354,"about_ca_system_score_codex":0.000054399374,"about_ca_system_score_gemma":0.004664425,"threshold_uncertainty_score":0.9998311},"labels":[],"label_agreement":null},{"id":"W4249137924","doi":"10.1139/cjes-38-7-1037","title":"The geochemical nature of the igneous rocks of the Sharbot Lake domain, Central Metasedimentary Belt, Ontario","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Igneous rock; Geochemistry; Petrology","score_opus":0.008315460326157268,"score_gpt":0.1896496523472585,"score_spread":0.18133419202110124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4249137924","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9767676,0.0009771986,0.00009534157,0.015119138,0.0010842193,0.00008838748,0.000008890166,0.0000022143513,0.0058570066],"genre_scores_gemma":[0.9982615,0.000007561701,0.0005274516,0.000550116,0.000074190524,4.2944222e-7,2.6279102e-7,8.69237e-7,0.00057759485],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985411,0.000078419915,0.00033334584,0.00015215833,0.00047065906,0.0004242986],"domain_scores_gemma":[0.99874187,0.0001255405,0.00037331966,0.00034810306,0.00017790556,0.00023327125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008102228,0.000100356934,0.00015125221,0.000041765536,0.00062456174,0.000087692715,0.0027901821,0.000071688024,0.00012693835],"category_scores_gemma":[0.00019836934,0.00004628184,0.0001760254,0.00053932366,0.00080730097,0.00015951955,0.00011998149,0.00048549144,4.1968863e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024135146,0.00007351558,0.9639292,0.0000226629,0.00015015478,0.00018664093,0.0051577757,0.0056039207,0.0052010682,0.008515502,0.008968317,0.0021671306],"study_design_scores_gemma":[0.00057266006,0.00026631192,0.5194118,0.00029869762,0.000058549813,0.0019693517,0.0010348262,0.000839464,0.037200138,0.02592884,0.41208,0.00033935657],"about_ca_topic_score_codex":0.014008814,"about_ca_topic_score_gemma":0.66578484,"teacher_disagreement_score":0.651776,"about_ca_system_score_codex":0.00001610954,"about_ca_system_score_gemma":0.0022207592,"threshold_uncertainty_score":0.992557},"labels":[],"label_agreement":null},{"id":"W4249358876","doi":"10.1139/cjes-37-10-1377","title":"Dimorphism and a new record of &lt;i&gt;Barroisiceras&lt;/i&gt; De Grossouvre (Ammonoidea) from the Coniacian of Bagh, central India","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Ammonoidea; Geology; Paleontology; Sexual dimorphism; Cretaceous; Phanerozoic; Mesozoic; Biology; Zoology; Cenozoic; Structural basin","score_opus":0.015329339115391409,"score_gpt":0.19818708102241514,"score_spread":0.18285774190702372,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4249358876","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9690381,0.016132522,0.00000951618,0.00091357104,0.0003160034,0.000072816096,0.00015098382,0.0000023956302,0.013364083],"genre_scores_gemma":[0.9980067,0.00035531603,0.0012637051,0.000152496,0.00014285576,9.7900326e-8,0.0000015754632,9.783764e-7,0.00007629537],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984323,0.00014735133,0.00045036167,0.00018013566,0.00027545998,0.0005144242],"domain_scores_gemma":[0.99837005,0.00030014085,0.00032818763,0.00012791362,0.000054621833,0.0008190799],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00070309493,0.0001369683,0.0003107072,0.00017011518,0.00039405687,0.00008789838,0.0005817865,0.000099306366,0.0017215005],"category_scores_gemma":[0.00010445323,0.00009548205,0.000117161995,0.00039965584,0.0015376175,0.00039108316,0.0000012417798,0.00019988838,0.0000034907],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003092826,0.000003522449,0.9106683,0.0000029139417,0.00003127843,0.000041776966,0.0017404236,0.00011758614,0.00019727577,0.00018342113,0.00036136666,0.086621165],"study_design_scores_gemma":[0.00027581595,0.00032363978,0.9908748,0.000066045264,0.000029000645,0.00008184801,0.00018863613,0.00015170021,0.000108234155,0.0022499072,0.005541995,0.00010832206],"about_ca_topic_score_codex":0.038516503,"about_ca_topic_score_gemma":0.7025683,"teacher_disagreement_score":0.6640518,"about_ca_system_score_codex":0.000001735984,"about_ca_system_score_gemma":0.0020047873,"threshold_uncertainty_score":0.99919105},"labels":[],"label_agreement":null},{"id":"W4249972402","doi":"10.1139/e00-119","title":"Very high temperature, moderate pressure metamorphism in the New Russia gneiss complex, northeastern Adirondack Highlands, metamorphic aureole to the Marcy anorthosite: Reply","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Anorthosite; Metamorphism; Gneiss; Geochemistry; Metamorphic rock; Geomorphology; Petrology; Plagioclase; Paleontology","score_opus":0.02221507392176093,"score_gpt":0.20096505457185554,"score_spread":0.17874998065009462,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4249972402","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94994956,0.003739841,0.000013466527,0.04434951,0.00025079196,0.00016283034,0.0000498851,0.0000052716114,0.0014788521],"genre_scores_gemma":[0.9920167,0.00006749433,0.00045928775,0.0061318204,0.00032377578,8.313152e-7,0.000017079223,0.0000025063919,0.000980505],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99757063,0.0002964864,0.00049968256,0.00033760502,0.00061450177,0.00068108697],"domain_scores_gemma":[0.99841064,0.00018668766,0.00020386514,0.000285749,0.000100255325,0.0008128183],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014769061,0.00022166263,0.00038454222,0.00031232924,0.0006583369,0.00046044844,0.0014013918,0.00006472503,0.005360681],"category_scores_gemma":[0.00014527098,0.00010238974,0.00017646409,0.0017062709,0.00036313315,0.00036771287,0.000016480151,0.000443311,0.00013036441],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000060318693,0.000014945282,0.92817014,0.000004765433,0.0000658407,0.0003353026,0.00050840783,0.064404,0.00008243062,0.00023319558,0.004015865,0.0021047902],"study_design_scores_gemma":[0.00021517623,0.00026359386,0.893059,0.00002489751,0.000087811095,0.0002917224,0.00020395563,0.0022106206,0.000048367252,0.002880596,0.10051984,0.00019440308],"about_ca_topic_score_codex":0.10459591,"about_ca_topic_score_gemma":0.7526835,"teacher_disagreement_score":0.6480876,"about_ca_system_score_codex":0.000001907523,"about_ca_system_score_gemma":0.00059570477,"threshold_uncertainty_score":0.99554855},"labels":[],"label_agreement":null},{"id":"W4249999663","doi":"10.1139/e10-039","title":"Preface / Préface","year":2010,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"French Urban and Social Studies","field":"Social Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Face (sociological concept); Geochemistry; Philosophy","score_opus":0.0410117396163063,"score_gpt":0.25952752176344185,"score_spread":0.21851578214713555,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4249999663","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49695277,0.06890027,0.00003876025,0.041003596,0.042974178,0.00020959723,0.000032197055,0.00001087734,0.34987774],"genre_scores_gemma":[0.89067197,0.0012007598,0.0021685387,0.00057215034,0.0028446987,7.4354887e-7,1.11561015e-7,0.000008097962,0.10253295],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99792886,0.00014754236,0.00037511002,0.00017599949,0.0005626669,0.0008098078],"domain_scores_gemma":[0.9977004,0.00021759431,0.00032214174,0.000092941395,0.00033567505,0.0013312387],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["sts"],"category_scores_codex":[0.0020054118,0.00014792471,0.000279186,0.00019851586,0.0020082965,0.00035960923,0.00081305526,0.00017672156,0.004665605],"category_scores_gemma":[0.0012037712,0.000117917465,0.00014896422,0.0011583802,0.0069877165,0.00076619745,0.000017165481,0.0005924568,0.00012027766],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015409149,0.00008361561,0.071762316,0.000047773377,0.0001519477,0.0005603365,0.09792296,0.0001822373,0.00017409971,0.6555849,0.119460054,0.05405441],"study_design_scores_gemma":[0.00012104758,0.00025997096,0.012627833,0.000073069605,0.00002417201,0.000047828,0.0050316546,0.000020711437,0.00003908304,0.0042927056,0.9772947,0.00016724583],"about_ca_topic_score_codex":0.10598269,"about_ca_topic_score_gemma":0.94817334,"teacher_disagreement_score":0.85783464,"about_ca_system_score_codex":0.000028868293,"about_ca_system_score_gemma":0.009245732,"threshold_uncertainty_score":0.99929094},"labels":[],"label_agreement":null},{"id":"W4250036575","doi":"10.1139/e10-024","title":"Preface / Préface","year":2010,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"French Urban and Social Studies","field":"Social Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Face (sociological concept); Philosophy","score_opus":0.0410117396163063,"score_gpt":0.25952752176344185,"score_spread":0.21851578214713555,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4250036575","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49695277,0.06890027,0.00003876025,0.041003596,0.042974178,0.00020959723,0.000032197055,0.00001087734,0.34987774],"genre_scores_gemma":[0.89067197,0.0012007598,0.0021685387,0.00057215034,0.0028446987,7.4354887e-7,1.11561015e-7,0.000008097962,0.10253295],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99792886,0.00014754236,0.00037511002,0.00017599949,0.0005626669,0.0008098078],"domain_scores_gemma":[0.9977004,0.00021759431,0.00032214174,0.000092941395,0.00033567505,0.0013312387],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["sts"],"category_scores_codex":[0.0020054118,0.00014792471,0.000279186,0.00019851586,0.0020082965,0.00035960923,0.00081305526,0.00017672156,0.004665605],"category_scores_gemma":[0.0012037712,0.000117917465,0.00014896422,0.0011583802,0.0069877165,0.00076619745,0.000017165481,0.0005924568,0.00012027766],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015409149,0.00008361561,0.071762316,0.000047773377,0.0001519477,0.0005603365,0.09792296,0.0001822373,0.00017409971,0.6555849,0.119460054,0.05405441],"study_design_scores_gemma":[0.00012104758,0.00025997096,0.012627833,0.000073069605,0.00002417201,0.000047828,0.0050316546,0.000020711437,0.00003908304,0.0042927056,0.9772947,0.00016724583],"about_ca_topic_score_codex":0.10598269,"about_ca_topic_score_gemma":0.94817334,"teacher_disagreement_score":0.85783464,"about_ca_system_score_codex":0.000028868293,"about_ca_system_score_gemma":0.009245732,"threshold_uncertainty_score":0.99929094},"labels":[],"label_agreement":null},{"id":"W4250059764","doi":"10.1139/e08-003e","title":"A new Jurassic pliosaur from Melville Island, Canadian Arctic Archipelago&lt;br /&gt;&lt;i&gt;This article contains taxonomic descriptions. Therefore, the link to it will not be made available until the print version has been distributed&lt;/i&gt;. &lt;br /&gt;&lt;i&gt;Cet article comporte des descriptions taxonomiques. Conséquemment le lien avec celui-ci ne deviendra disponible qu'au moment où la version imprimée sera distribuée&lt;/i&gt;.","year":2008,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Archipelago; Geology; Arctic; Paleontology; The arctic; Oceanography; Link (geometry); Combinatorics","score_opus":0.037612441048851974,"score_gpt":0.20513924283958232,"score_spread":0.16752680179073035,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4250059764","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8975526,0.01363916,0.0018962522,0.074293956,0.0019581697,0.0011876503,0.005442016,0.000034584486,0.003995613],"genre_scores_gemma":[0.9893964,0.002037792,0.0024769509,0.0018576348,0.00061813404,0.000030806146,0.00044550805,0.000025839283,0.003110912],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9923557,0.0012343609,0.0015689887,0.0011374089,0.0008096075,0.0028939454],"domain_scores_gemma":[0.9931487,0.00084058964,0.0008493236,0.00086889917,0.00045998427,0.003832535],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":["sts"],"category_scores_codex":[0.00302019,0.00082589994,0.0010233416,0.00069071027,0.0068772566,0.000701097,0.0020222212,0.0004898904,0.006027647],"category_scores_gemma":[0.00047857585,0.0006249197,0.0004897741,0.001407006,0.005766923,0.0016714628,0.00015389426,0.0010069441,0.0007555981],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015598772,0.0006523373,0.56534576,0.0001389329,0.0014824587,0.001525577,0.017835585,0.042581823,0.034374665,0.02065457,0.2979729,0.015875522],"study_design_scores_gemma":[0.0012325734,0.0007446782,0.3647126,0.00023006248,0.00020605253,0.00067331037,0.00070526777,0.0059851594,0.000337396,0.0005443384,0.62403286,0.00059572153],"about_ca_topic_score_codex":0.22877611,"about_ca_topic_score_gemma":0.9737047,"teacher_disagreement_score":0.7449286,"about_ca_system_score_codex":0.0008452404,"about_ca_system_score_gemma":0.014478466,"threshold_uncertainty_score":0.9996202},"labels":[],"label_agreement":null},{"id":"W4250575888","doi":"10.1139/cjes-38-3-441","title":"Geology and tectonic setting of Paleoproterozoic granitoid suites in the Island Harbour Bay area, Makkovik Province, Labrador","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Bay; Tectonics; Harbour; Geochemistry; Seismology; Oceanography","score_opus":0.01789195499188715,"score_gpt":0.19391982608658728,"score_spread":0.17602787109470014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4250575888","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941647,0.002536849,0.000013728323,0.0019153326,0.00011201384,0.00010203917,0.000007645233,0.0000012495151,0.0011464285],"genre_scores_gemma":[0.9993487,0.000174486,0.00015891691,0.00022683188,0.000058706137,3.5848532e-7,0.0000012547946,6.530088e-7,0.000030063848],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990305,0.00009868493,0.00025678537,0.00011811356,0.00017608685,0.00031986766],"domain_scores_gemma":[0.9993814,0.00021707891,0.00016785129,0.00005292976,0.00004905868,0.00013163206],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010661919,0.00007748106,0.00016340397,0.00016757027,0.00031345795,0.00008085636,0.0002665919,0.00003674404,0.00041587785],"category_scores_gemma":[0.00022357459,0.00004305651,0.000029882918,0.0004063526,0.00044204897,0.00022719173,0.0000050196945,0.00014422645,0.0000041972958],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000610786,0.0000023720875,0.99391335,0.0000041049384,0.0000028816153,0.000049662252,0.00044327954,0.0005258137,0.000006596709,0.000025016683,0.000034228313,0.0049865963],"study_design_scores_gemma":[0.00013725288,0.00042203657,0.9942789,0.000023296176,0.000003887267,0.00017297716,0.001549677,0.0005984442,0.00000518044,0.0007118988,0.0020385117,0.000057917157],"about_ca_topic_score_codex":0.028264008,"about_ca_topic_score_gemma":0.9228822,"teacher_disagreement_score":0.89461815,"about_ca_system_score_codex":9.2714754e-7,"about_ca_system_score_gemma":0.00025344064,"threshold_uncertainty_score":0.9782069},"labels":[],"label_agreement":null},{"id":"W4250629950","doi":"10.1139/e2012-083","title":"Canadian contributions to planetary geoscience / Contributions canadiennes aux géosciences planétaires","year":2013,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Earth science; Plan (archaeology); Geochemistry; Astrobiology; Paleontology","score_opus":0.020022887704725385,"score_gpt":0.2364441257084097,"score_spread":0.21642123800368432,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4250629950","genre_codex":"commentary","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.24992286,0.011861044,0.0049492233,0.68192,0.013746938,0.00093319797,0.0022324142,0.000036699923,0.034397643],"genre_scores_gemma":[0.98178893,0.00005749237,0.002539424,0.0036232756,0.0005479553,0.000010314974,0.00000811815,0.0000038016597,0.011420714],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9947056,0.00022536653,0.0008647893,0.0006901535,0.0006876579,0.0028264197],"domain_scores_gemma":[0.98820823,0.0003724292,0.00040908722,0.00042861575,0.0026259155,0.007955727],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","insufficient_payload"],"consensus_categories":["sts"],"category_scores_codex":[0.002499569,0.00037870515,0.00050401053,0.0012140723,0.0037685079,0.0020058735,0.0034500114,0.00024085506,0.001832001],"category_scores_gemma":[0.0041431542,0.00034588441,0.0001717025,0.0031527807,0.00272617,0.002545119,0.00009799655,0.0005929453,0.00041306033],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008996581,0.00011268704,0.18713637,0.00010201533,0.00016896258,0.003584233,0.009327548,0.037215713,0.0013374456,0.5087314,0.22436924,0.027905349],"study_design_scores_gemma":[0.00031167077,0.0007711353,0.11510889,0.00046366084,0.000038203852,0.0027515523,0.0018466667,0.012675838,0.0004521113,0.020224134,0.8445474,0.00080873363],"about_ca_topic_score_codex":0.96667016,"about_ca_topic_score_gemma":0.99481064,"teacher_disagreement_score":0.73186606,"about_ca_system_score_codex":0.0002288133,"about_ca_system_score_gemma":0.046690483,"threshold_uncertainty_score":0.99998784},"labels":[],"label_agreement":null},{"id":"W4250766701","doi":"10.1139/cjes-37-2-3-271","title":"Contrasting Si-saturation in troctolite-anorthosite intrusions along the Manicouagan corridor of the Abitibi-Grenville transect","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Silicon Effects in Agriculture","field":"Agricultural and Biological Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Anorthosite; Geology; Plagioclase; Geochemistry; Olivine; Layered intrusion; Gabbro; Magma chamber; Petrology; Fractional crystallization (geology); Intrusion; Magma; Mantle (geology); Igneous rock; Volcano; Quartz","score_opus":0.011810547285502977,"score_gpt":0.1921502184903886,"score_spread":0.18033967120488562,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4250766701","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99517137,0.0005246344,5.336625e-7,0.0027715494,0.00025871073,0.00017886027,0.000020376901,0.00000253665,0.0010714302],"genre_scores_gemma":[0.99930114,0.000021650983,0.000024405172,0.00039043868,0.00016221467,0.0000012931152,0.0000010747575,5.7151624e-7,0.00009724416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99866503,0.00020753259,0.00037704947,0.00014088488,0.00029160525,0.00031790358],"domain_scores_gemma":[0.99908394,0.0003963814,0.00020984745,0.00005210451,0.00008241295,0.00017532187],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008064932,0.000107064145,0.00017433426,0.000033868324,0.0005732396,0.00010827195,0.0006414732,0.00006212867,0.0008134893],"category_scores_gemma":[0.00019563896,0.000029150642,0.00013107104,0.0009534813,0.00043677937,0.00018090288,0.00000807869,0.0002577874,0.000003394865],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002926194,0.000038978906,0.7653309,0.000008262394,0.000019722092,0.00004031618,0.0022978492,0.0024758372,0.14562877,0.0005070904,0.00031337191,0.083309636],"study_design_scores_gemma":[0.00011140261,0.00017078171,0.99453735,0.00010847205,0.00001052228,0.00011884765,0.0007168782,0.00021081009,0.0015999977,0.000079978294,0.0022550747,0.00007991063],"about_ca_topic_score_codex":0.010256536,"about_ca_topic_score_gemma":0.6542741,"teacher_disagreement_score":0.6440176,"about_ca_system_score_codex":0.000009899005,"about_ca_system_score_gemma":0.00016625428,"threshold_uncertainty_score":0.99633425},"labels":[],"label_agreement":null},{"id":"W4251184436","doi":"10.1139/cjes-37-6-923","title":"A U-Pb and &lt;sup&gt;40&lt;/sup&gt;Ar/&lt;sup&gt;39&lt;/sup&gt;Ar time scale for the Jurassic","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Scale (ratio); Geochemistry; Mineralogy; Physics","score_opus":0.01095465791149938,"score_gpt":0.1811120194273444,"score_spread":0.170157361515845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4251184436","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9715634,0.0070431093,0.000048942453,0.010001812,0.00026198773,0.0003605865,0.00040134016,0.000028336943,0.01029047],"genre_scores_gemma":[0.9891907,0.00054981257,0.0015701985,0.0017930033,0.0006935833,0.0000047700364,0.00004032545,0.00001131319,0.006146267],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9951002,0.00023785525,0.0010189645,0.0007881297,0.0011079016,0.0017469524],"domain_scores_gemma":[0.9957371,0.00089350255,0.00039875132,0.0004220221,0.00031646265,0.002232197],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0022142623,0.0005441937,0.0008740979,0.00050173514,0.0020088248,0.00079120276,0.0017215407,0.00026583672,0.028530836],"category_scores_gemma":[0.00045172495,0.0003360835,0.0005339759,0.0017109361,0.0022533387,0.00092479057,0.000039603903,0.0005443627,0.00075449096],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006645667,0.00026558526,0.5344627,0.00016832935,0.00079239986,0.00080618804,0.004631374,0.09674685,0.003550379,0.00064127543,0.057218593,0.30005178],"study_design_scores_gemma":[0.001501517,0.0020144165,0.36045334,0.00023572742,0.00048815392,0.0008402495,0.00075711106,0.11579567,0.00042445003,0.009695739,0.5063287,0.0014649171],"about_ca_topic_score_codex":0.0057968614,"about_ca_topic_score_gemma":0.15333073,"teacher_disagreement_score":0.44911012,"about_ca_system_score_codex":0.000014263465,"about_ca_system_score_gemma":0.0010388728,"threshold_uncertainty_score":0.9999091},"labels":[],"label_agreement":null},{"id":"W4252231402","doi":"10.1139/cjes-37-6-863","title":"Paleomagnetic evidence for multiple Late Pliocene - Early Pleistocene glaciations in the Klondike area, Yukon Territory","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Glacial period; Paleontology; Pleistocene; Interglacial; Loess; Aggradation; Fluvial; Early Pleistocene; Paleomagnetism; Glacier; Geomorphology; Moraine; Outwash plain; Structural basin","score_opus":0.06042747892030949,"score_gpt":0.266712236780457,"score_spread":0.20628475786014755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4252231402","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99144214,0.0036407292,0.000006339781,0.0023321519,0.00025928963,0.00020625704,0.00002668333,0.0000025938757,0.0020838035],"genre_scores_gemma":[0.998723,0.00009109937,0.00039800795,0.0003467854,0.000087824425,0.000002154154,0.0000038471144,0.000001351319,0.0003459353],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984721,0.00020494671,0.0003153833,0.00017937373,0.00025715883,0.0005710708],"domain_scores_gemma":[0.9982566,0.0011383928,0.000104282946,0.00012522355,0.00007255322,0.0003029059],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018222718,0.00010063783,0.00017143028,0.00035238775,0.00067373307,0.00012563422,0.0007401225,0.000079703364,0.0021862679],"category_scores_gemma":[0.00040096947,0.00006799813,0.00007365961,0.00049339473,0.00075495476,0.00042386202,0.0000020532057,0.00026505356,0.00006775685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033038374,0.0000045158336,0.99441487,0.0000045982583,0.000004001581,0.00006518733,0.0005603476,0.0029066375,0.0000015987782,0.000010946687,0.00008270309,0.001911557],"study_design_scores_gemma":[0.000255478,0.0006186973,0.9942891,0.000053344178,0.000008436554,0.0001447036,0.00015472631,0.0022624554,0.000006029916,0.00059851137,0.001523783,0.0000847331],"about_ca_topic_score_codex":0.011436054,"about_ca_topic_score_gemma":0.83291763,"teacher_disagreement_score":0.8214816,"about_ca_system_score_codex":9.284358e-7,"about_ca_system_score_gemma":0.0009796456,"threshold_uncertainty_score":0.9987259},"labels":[],"label_agreement":null},{"id":"W4252439835","doi":"10.1139/cjes-2019-0012","title":"Corrigendum: Salt tectonism and distribution of brackish-water trace fossils in the Cretaceous McMurray Formation, Athabasca Oil Sands, Alberta Foreland Basin","year":2019,"lang":"en","type":"erratum","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Golder Associates (Canada)","funders":"","keywords":"Geology; Foreland basin; Oil sands; Cretaceous; Trace fossil; Structural basin; Geochemistry; Paleontology; Geomorphology; Archaeology; Asphalt","score_opus":0.021058103565470603,"score_gpt":0.1993000945953731,"score_spread":0.17824199102990249,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4252439835","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8990127,0.033584703,0.0001395026,0.009494528,0.017228406,0.0004613178,0.00065988844,0.0000056173226,0.039413348],"genre_scores_gemma":[0.99349296,0.00137978,0.000039663402,0.00019165984,0.00027359335,7.633822e-7,0.00022762606,0.000002529902,0.004391419],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99814445,0.00015329546,0.00055788265,0.00020478401,0.0004431192,0.0004964645],"domain_scores_gemma":[0.9989327,0.00016111902,0.00041061165,0.00011668617,0.00014611722,0.00023276733],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013735215,0.00019300795,0.00039749817,0.00018692538,0.00051239715,0.00026124364,0.00047532504,0.00019346956,0.00046059818],"category_scores_gemma":[0.0002259274,0.00009973082,0.000098751065,0.00033735577,0.00049739896,0.0005874359,0.000008160853,0.00046985855,0.00002115848],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008441414,0.000028761655,0.65174264,0.00028837612,0.000060659368,0.00013856438,0.0104449885,0.0018998143,0.0000062837503,0.00012522422,0.28984416,0.04533611],"study_design_scores_gemma":[0.00025568614,0.0006325535,0.5125739,0.00019093814,0.000031446558,0.00021748454,0.0013316806,0.001128338,0.000016786704,0.00044991958,0.482971,0.00020024649],"about_ca_topic_score_codex":0.048760355,"about_ca_topic_score_gemma":0.7616339,"teacher_disagreement_score":0.7128735,"about_ca_system_score_codex":0.0000053363565,"about_ca_system_score_gemma":0.00057841616,"threshold_uncertainty_score":0.957574},"labels":[],"label_agreement":null},{"id":"W4252512145","doi":"10.1139/cjes-37-2-3-399","title":"Heat flow and deep thermal structure near the southeastern edge of the Canadian Shield","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Archean; Geology; Crust; Craton; Shield; Heat flow; Tectonics; High heat; Flow (mathematics); Terrane; Petrology; Geochemistry; Seismology; Thermal; Geography; Geometry; Meteorology","score_opus":0.009198975578967242,"score_gpt":0.16455175101499664,"score_spread":0.1553527754360294,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4252512145","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9888545,0.0013658962,4.684602e-7,0.0049759224,0.0001469273,0.000042161337,0.000053031996,8.880463e-7,0.0045601935],"genre_scores_gemma":[0.9987948,0.000009358375,0.00012399258,0.0008803771,0.000083417326,4.1712134e-8,0.0000010374068,7.964153e-7,0.000106203275],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990047,0.00007928422,0.00020236913,0.00011573229,0.00024485105,0.0003530512],"domain_scores_gemma":[0.99913716,0.00007236233,0.00004661569,0.000107223204,0.000051127183,0.0005855203],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035326576,0.00008960631,0.00014518356,0.000064084525,0.0010134832,0.00021298704,0.0005866557,0.00005332097,0.018001197],"category_scores_gemma":[0.000059886992,0.00003850578,0.00008830431,0.00041954557,0.0015202293,0.00011847216,0.000004446544,0.00021998666,0.000015184885],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003687109,8.301308e-7,0.9726606,0.0000017243345,0.000011314544,0.000009213916,0.000677042,0.011596891,0.000016455673,0.000014232041,0.000019941303,0.014988095],"study_design_scores_gemma":[0.00007073298,0.000091266054,0.97996855,0.000015209652,0.000022899845,0.000085504886,0.00031578005,0.012565738,0.000081678845,0.0016652087,0.005036299,0.00008112127],"about_ca_topic_score_codex":0.58500963,"about_ca_topic_score_gemma":0.9954325,"teacher_disagreement_score":0.4104229,"about_ca_system_score_codex":9.449586e-7,"about_ca_system_score_gemma":0.00091060123,"threshold_uncertainty_score":0.9828965},"labels":[],"label_agreement":null},{"id":"W4252522527","doi":"10.1139/cjes-37-12-ai-1","title":"Authors Index / Index des auteurs&lt;BR&gt;Volume 37, 2000","year":2000,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Diverse Scientific and Economic Studies","field":"Economics, Econometrics and Finance","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Index (typography); Volume (thermodynamics); Mineralogy; Thermodynamics; Physics","score_opus":0.03806193315069463,"score_gpt":0.20598382971155008,"score_spread":0.16792189656085543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4252522527","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5464174,0.069920205,0.000115967356,0.0045583784,0.02113377,0.00015813955,0.0006698305,0.0000094740135,0.35701683],"genre_scores_gemma":[0.42281052,0.002253481,0.0006133956,0.00036098668,0.00044781074,0.0000011075837,9.784785e-7,0.000013769379,0.57349795],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9968505,0.00005097799,0.0011559866,0.00055130845,0.00013811734,0.0012531189],"domain_scores_gemma":[0.9976702,0.000057294907,0.0006829878,0.00025674843,0.00013714997,0.0011956467],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0028408475,0.00027710444,0.0006692419,0.0009146718,0.0012637206,0.00092620286,0.0010373527,0.00020066294,0.11658335],"category_scores_gemma":[0.00022222337,0.00031991076,0.00031125438,0.0011428401,0.0036069702,0.0016217639,0.000035316963,0.0003828425,0.0088219205],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017267841,0.000052165324,0.7051949,0.000030115802,0.00017601991,0.00016499692,0.0047680736,0.009196079,7.014084e-7,0.0099177025,0.22592613,0.044555854],"study_design_scores_gemma":[0.00033497435,0.00017044948,0.17822036,0.000116839845,0.000016220269,0.00010760867,0.0009557656,0.004073981,0.0000020489038,0.003888477,0.8117869,0.00032638977],"about_ca_topic_score_codex":0.012962951,"about_ca_topic_score_gemma":0.061481122,"teacher_disagreement_score":0.5858607,"about_ca_system_score_codex":0.0001383011,"about_ca_system_score_gemma":0.0019473606,"threshold_uncertainty_score":0.9999253},"labels":[],"label_agreement":null},{"id":"W4252618582","doi":"10.1139/cjes-37-4-535","title":"Granite petrogenesis in the Gander Zone, NE Newfoundland: mixing of melts from multiple sources and the role of lithospheric delamination","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Magmatism; Geochemistry; Mantle (geology); Lithosphere; Subduction; Petrogenesis; Partial melting; Devonian; Igneous differentiation; Igneous rock; Petrology; Continental margin; Crust; Rift; Paleontology; Tectonics","score_opus":0.007376976343661318,"score_gpt":0.16750666217124174,"score_spread":0.16012968582758041,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4252618582","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99169564,0.0067869346,0.000008086588,0.0005191481,0.000028048218,0.000037878584,0.000012480557,6.2940757e-7,0.0009111263],"genre_scores_gemma":[0.9994328,0.00015206577,0.00025623242,0.00010079655,0.00003096712,1.4496871e-7,0.0000022910738,5.1437576e-7,0.00002421499],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999085,0.00013473941,0.00027429947,0.0000939169,0.00024148719,0.0001705564],"domain_scores_gemma":[0.9991239,0.0004957425,0.00015727335,0.00005913313,0.000051267427,0.00011273581],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00081880303,0.00006435456,0.00018541906,0.0000763269,0.00016746212,0.000053310003,0.00032001536,0.000026985028,0.0015760437],"category_scores_gemma":[0.00011520334,0.00002972174,0.00007065883,0.00053163327,0.0006821069,0.00013789245,0.0000026185273,0.000085020045,0.0000024834599],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002076275,0.0000037365373,0.97578156,0.0000013601887,0.00000929909,0.0000035816543,0.00096845,0.0029312202,0.000033529323,0.000026045589,0.000001235516,0.020219231],"study_design_scores_gemma":[0.000267908,0.00008045507,0.9827181,0.000014881048,0.000025284508,0.000014284811,0.001639543,0.008475766,0.00014769676,0.0059933397,0.00057743356,0.000045326164],"about_ca_topic_score_codex":0.24163587,"about_ca_topic_score_gemma":0.74762434,"teacher_disagreement_score":0.5059885,"about_ca_system_score_codex":6.0426515e-7,"about_ca_system_score_gemma":0.000095381874,"threshold_uncertainty_score":0.99933666},"labels":[],"label_agreement":null},{"id":"W4252788607","doi":"10.1139/cjes-38-1-21","title":"Age and composition of the Ruisseau Isabelle Mélange along the Shickshock Sud fault zone: constraints on the timing of mélanges formation in the Gaspé Appalachians","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Fault (geology); Thermochronology; Composition (language); Seismology; Geochemistry; Tectonics","score_opus":0.043680508589696646,"score_gpt":0.2510749159086011,"score_spread":0.20739440731890446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4252788607","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98289704,0.0006736978,0.000008511187,0.009093119,0.000102457445,0.00014518967,0.000012869198,7.080867e-7,0.007066418],"genre_scores_gemma":[0.9994254,0.00008317994,0.000028851195,0.00041622703,0.000023212568,3.7295683e-7,0.0000018626556,6.833841e-7,0.000020225994],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987436,0.00043781218,0.0002311562,0.00007332803,0.00026123,0.00025288903],"domain_scores_gemma":[0.99880517,0.0007813789,0.0001793013,0.00010972689,0.00004998132,0.00007442314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020189704,0.00006585245,0.00011698759,0.0001245455,0.00061423937,0.000048859198,0.00055277435,0.000045969773,0.00028927624],"category_scores_gemma":[0.000116695635,0.000027003094,0.00004082181,0.00036007358,0.0020940856,0.0001423169,0.0000063555813,0.0002866073,0.0000043100445],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009743646,0.000003905714,0.9950358,0.000006113146,0.000005194836,0.000036709338,0.0029635865,0.0006681487,0.000018557765,0.00043750662,0.000072966046,0.00074174366],"study_design_scores_gemma":[0.00011600498,0.00014303475,0.99133474,0.00006889347,0.0000069615608,0.0006469875,0.005574521,0.0013856654,0.000105433304,0.00033428695,0.00024685616,0.000036647773],"about_ca_topic_score_codex":0.004368544,"about_ca_topic_score_gemma":0.48800555,"teacher_disagreement_score":0.483637,"about_ca_system_score_codex":6.5867874e-7,"about_ca_system_score_gemma":0.0002078573,"threshold_uncertainty_score":0.7715745},"labels":[],"label_agreement":null},{"id":"W4252850283","doi":"10.1139/cjes-37-2-3-291","title":"Crustal evolution along a seismic section across the Grenville Province (western Quebec)","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Section (typography); Seismology; Geochemistry","score_opus":0.011115827511811298,"score_gpt":0.19596887800939733,"score_spread":0.18485305049758602,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4252850283","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99404556,0.0008067716,0.000041440588,0.0024809302,0.00022723044,0.000051223138,0.000021029351,0.0000040727136,0.0023217688],"genre_scores_gemma":[0.9980153,0.000015819494,0.000058632417,0.00046741968,0.00025122977,1.5446086e-7,0.0000024168537,8.4041915e-7,0.0011881904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998755,0.000079176505,0.00026482673,0.00016370747,0.00029238,0.00044494247],"domain_scores_gemma":[0.99926007,0.00007080739,0.0001235566,0.0000830745,0.000068424175,0.0003940658],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000667342,0.000096345946,0.00014004821,0.00007626742,0.0007881365,0.00021107247,0.00042138514,0.0000664843,0.0064453124],"category_scores_gemma":[0.00006352185,0.000052786047,0.000107636864,0.0005273049,0.0007129042,0.0003443693,0.0000039085867,0.0002791116,0.00013382171],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000832013,0.000003335968,0.9523521,0.0000018236763,0.000008769268,0.000035715493,0.00019014918,0.028075889,0.000014777821,0.000009914657,0.00010783169,0.019191338],"study_design_scores_gemma":[0.000083621475,0.00015499287,0.978756,0.000014367542,0.00001172767,0.00018114653,0.00038187145,0.004744958,0.000034608827,0.001005353,0.014536027,0.00009529386],"about_ca_topic_score_codex":0.44073516,"about_ca_topic_score_gemma":0.9817728,"teacher_disagreement_score":0.5410376,"about_ca_system_score_codex":0.000004189663,"about_ca_system_score_gemma":0.000703889,"threshold_uncertainty_score":0.9944629},"labels":[],"label_agreement":null},{"id":"W4253012561","doi":"10.1139/cjes-2018-0081","title":"Vaalbara Palaeomagnetism","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Craton; Paleomagnetism; Geology; Paleontology; Assemblage (archaeology); Tectonics","score_opus":0.016625203439123687,"score_gpt":0.19204082852902823,"score_spread":0.17541562508990455,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4253012561","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9561996,0.0009131746,0.000026095735,0.0015562782,0.00039408205,0.000018887626,0.000008933143,0.0000032364917,0.040879734],"genre_scores_gemma":[0.99769586,0.000012784612,0.0011151502,0.00065784494,0.0003348592,2.889368e-8,0.0000011288431,5.33841e-7,0.0001818003],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99900645,0.000037966358,0.00022410451,0.00012816695,0.00023253652,0.00037080326],"domain_scores_gemma":[0.99891406,0.00006557011,0.00010775477,0.00006578226,0.00014608829,0.0007007329],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00050983264,0.00007499928,0.00014075919,0.00019489233,0.00035779612,0.000104247585,0.00043146493,0.000036589765,0.04101335],"category_scores_gemma":[0.00018022826,0.00004710145,0.00008394612,0.0005952378,0.0011064858,0.00021407439,0.0000034244226,0.00010670937,0.0004654686],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026296307,0.0000017804838,0.99083143,9.118763e-7,0.0000067075357,0.000045669858,0.000066114124,0.00013239091,0.000056758356,0.00019895549,0.00039435123,0.0082623055],"study_design_scores_gemma":[0.00007512033,0.00061671203,0.9567931,0.000010728815,0.000011554864,0.00010879666,0.00009030677,0.0007523378,0.00032288054,0.019431451,0.021688594,0.00009841347],"about_ca_topic_score_codex":0.02381218,"about_ca_topic_score_gemma":0.54980314,"teacher_disagreement_score":0.52599096,"about_ca_system_score_codex":4.1582499e-7,"about_ca_system_score_gemma":0.00042029063,"threshold_uncertainty_score":0.98268837},"labels":[],"label_agreement":null},{"id":"W4253245761","doi":"10.1139/cjes-2016-0049","title":"Eocene Paleontology and Geology of Western North America / Paléontologie et géologie de l’Éocène de l’ouest de l’Amérique du Nord","year":2016,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology; Archaeology; Geography","score_opus":0.043102140169918715,"score_gpt":0.2665086167047893,"score_spread":0.2234064765348706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4253245761","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92793787,0.018491212,0.00066152756,0.049190685,0.0007303728,0.00010122863,0.000106058615,0.000006075481,0.002774961],"genre_scores_gemma":[0.9874084,0.008131001,0.0022552256,0.0012727753,0.00015564772,0.0000012099767,0.0000035649211,0.000004323013,0.0007678468],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9955264,0.0014396698,0.00062438264,0.00037837922,0.0002067872,0.0018243964],"domain_scores_gemma":[0.99534124,0.0022996715,0.00050856796,0.00019747175,0.0002543447,0.0013986928],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0032677373,0.0002575425,0.0006723048,0.000544004,0.00043238528,0.0000560454,0.000963085,0.00044467178,0.0011458638],"category_scores_gemma":[0.001954749,0.00018605228,0.00011226872,0.00047114302,0.008928544,0.00044061206,0.00003545213,0.0005981823,0.000048862166],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007000354,0.000020400239,0.98795164,0.00003870579,0.00005431395,0.00158404,0.00109718,0.00040135655,0.000017226268,0.0004972842,0.00019536605,0.008072464],"study_design_scores_gemma":[0.0004848531,0.0018334041,0.972118,0.00009914099,0.000036198646,0.0074614175,0.0005070589,0.00023512269,0.000049480663,0.0019880775,0.014982426,0.00020477822],"about_ca_topic_score_codex":0.021479642,"about_ca_topic_score_gemma":0.9594896,"teacher_disagreement_score":0.93801,"about_ca_system_score_codex":0.0000063617035,"about_ca_system_score_gemma":0.00718669,"threshold_uncertainty_score":0.99976724},"labels":[],"label_agreement":null},{"id":"W4253247616","doi":"10.1139/cjes-37-1-17","title":"Late Laramide dolomite recrystallization of the Husky Rainbow \"A\" hydrocarbon Devonian reservoir, northwestern Alberta, Canada: paleomagnetic and geochemical evidence","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Dolomite; Geology; Devonian; Sedimentary rock; Petrography; Diagenesis; Geochemistry; Dolomitization; Carbonate rock; Paleomagnetism; Carbonate; Mineralogy; Paleontology; Facies; Structural basin","score_opus":0.011697448739810047,"score_gpt":0.2058741987352121,"score_spread":0.19417674999540205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4253247616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9901238,0.0073074033,0.0000016781067,0.0013306726,0.00014122904,0.00009628727,0.000014994798,6.9802417e-7,0.0009832265],"genre_scores_gemma":[0.9974228,0.000798833,0.0001277131,0.00024506115,0.000080113015,0.0000013358252,0.0000022022427,0.0000055071127,0.0013164126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987864,0.00009787113,0.0003280716,0.00021057503,0.0002488101,0.000328298],"domain_scores_gemma":[0.99918526,0.00006126205,0.00017733226,0.00018528714,0.000114284136,0.00027659003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003349251,0.00013225926,0.00017343657,0.000057991587,0.00025497656,0.000045002846,0.0004102794,0.00007257973,0.00008816293],"category_scores_gemma":[0.00021982721,0.000098056764,0.00005626744,0.00023912465,0.00055950787,0.000020274816,0.000031406995,0.00010663282,5.99159e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037702168,0.000007776695,0.9760736,0.000035051533,0.000029516465,0.000027450258,0.0005171097,0.0014151377,0.019067187,0.00001059958,0.0005580958,0.0022207468],"study_design_scores_gemma":[0.00035441865,0.00070072326,0.96786475,0.00025011253,0.000038299866,0.00019000345,0.00013868479,0.00016130423,0.006164179,0.00010330284,0.023805672,0.0002285523],"about_ca_topic_score_codex":0.4120689,"about_ca_topic_score_gemma":0.9922227,"teacher_disagreement_score":0.5801538,"about_ca_system_score_codex":0.0000046410714,"about_ca_system_score_gemma":0.0016799687,"threshold_uncertainty_score":0.59184617},"labels":[],"label_agreement":null},{"id":"W4253312404","doi":"10.1139/cjes-38-3-479","title":"Late-glacial stratigraphy and history of the Gulf of St. Lawrence: Discussion","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Stratigraphy; Glacial period; Paleontology; Geochemistry; Tectonics","score_opus":0.025418009051271357,"score_gpt":0.22812940378480584,"score_spread":0.20271139473353447,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4253312404","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.985656,0.002955094,0.0000025549443,0.0009372588,0.00051251164,0.000040084295,0.000012829161,6.647116e-7,0.009882967],"genre_scores_gemma":[0.9993687,0.00010334312,0.00010053055,0.000051546423,0.000027637534,4.3099156e-8,5.9064325e-7,4.83945e-7,0.0003471142],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990835,0.00013160873,0.00023606878,0.00008929342,0.00022551153,0.00023399966],"domain_scores_gemma":[0.9993216,0.0000934239,0.00019545152,0.00007630852,0.00008004861,0.00023319376],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000809625,0.00005750783,0.00015320627,0.0002186715,0.00017812222,0.000011422355,0.00036694072,0.000057703375,0.0013008309],"category_scores_gemma":[0.00009826062,0.00002862183,0.000055822653,0.0003077241,0.002397722,0.0001805178,0.000004710563,0.00017123434,0.000002094305],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009785982,0.0000022875474,0.9983664,0.000005235406,0.000005191545,0.000015018035,0.00036037285,0.0001820174,0.000016923137,0.00013870021,0.00014969501,0.00074834],"study_design_scores_gemma":[0.00010257092,0.00021558983,0.9937236,0.000031597043,0.000006524809,0.00011143207,0.00026492955,0.00013994277,0.000029674526,0.0014024536,0.003932097,0.00003959916],"about_ca_topic_score_codex":0.0041903616,"about_ca_topic_score_gemma":0.54292804,"teacher_disagreement_score":0.53873765,"about_ca_system_score_codex":4.2569712e-7,"about_ca_system_score_gemma":0.0015585715,"threshold_uncertainty_score":0.9996121},"labels":[],"label_agreement":null},{"id":"W4254033983","doi":"10.1139/cjes-37-2-3-459","title":"The Lithoprobe Abitibi-Grenville transect: two billion years of crust formation and recycling in the Precambrian Shield of Canada","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Precambrian; Geology; Shield; Crust; Transect; Geochemistry; Archean; Proterozoic; Earth science; Petrology; Paleontology; Tectonics","score_opus":0.014782170754738743,"score_gpt":0.20215930988523517,"score_spread":0.18737713913049642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4254033983","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9772486,0.004713586,0.0000029085556,0.0008494341,0.00010516281,0.000063696774,0.000016420405,3.6797425e-7,0.016999805],"genre_scores_gemma":[0.99959725,0.00020012903,0.00011569449,0.000056443783,0.00002155953,1.0825585e-7,2.723296e-7,2.581219e-7,0.00000827031],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99908257,0.00011990921,0.0003070965,0.00006535127,0.0002134918,0.00021159182],"domain_scores_gemma":[0.9993719,0.0002718117,0.00014642524,0.000060697184,0.0000261508,0.00012305232],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013899726,0.00005043738,0.00011314906,0.00011481833,0.00028188765,0.000042161988,0.00027681355,0.00002856337,0.000091431335],"category_scores_gemma":[0.000059197777,0.000029595387,0.00003281375,0.00033475735,0.00048689963,0.0002117138,2.33077e-7,0.00013174022,1.453203e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032203367,0.0000031814536,0.53893125,0.000010680349,0.000008709611,0.000031875043,0.0029712939,0.0015726176,0.00003023329,0.00021740777,0.00006694916,0.45612362],"study_design_scores_gemma":[0.00012511408,0.00014964172,0.9969204,0.000047922527,0.0000045080105,0.000082979706,0.0009890835,0.0005134194,0.00005215672,0.00033210678,0.00074380374,0.00003884056],"about_ca_topic_score_codex":0.67000645,"about_ca_topic_score_gemma":0.9986121,"teacher_disagreement_score":0.4579892,"about_ca_system_score_codex":8.8352186e-7,"about_ca_system_score_gemma":0.0009103429,"threshold_uncertainty_score":0.33219102},"labels":[],"label_agreement":null},{"id":"W4254318787","doi":"10.1139/cjes-38-2-293","title":"Periodically forced self-organization in the long-term evolution of planktic foraminifera","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Foraminifera; Geology; Term (time); Paleontology; Oceanography; Benthic zone","score_opus":0.01744580101922377,"score_gpt":0.22989556184629562,"score_spread":0.21244976082707184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4254318787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99606323,0.0006640403,0.000055384266,0.001073764,0.00016922486,0.00007387948,0.0000035810779,0.0000018482885,0.0018950343],"genre_scores_gemma":[0.99962753,0.000044623474,0.00014673804,0.00011940876,0.00003344779,9.616912e-8,0.000004167243,7.686708e-7,0.000023235567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989064,0.00017122742,0.00026333777,0.00009355042,0.00024374272,0.00032174136],"domain_scores_gemma":[0.9992851,0.00018793691,0.00013084082,0.00007333159,0.00014680637,0.00017599737],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012886748,0.000060372255,0.00013005805,0.0003584377,0.00031040097,0.00005843614,0.00049105,0.00006880932,0.00091693393],"category_scores_gemma":[0.0002830257,0.00003902093,0.000026912676,0.0010198933,0.00055606675,0.0002519359,0.000002575167,0.00018789373,0.000025998403],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000065263935,0.000004607325,0.99843097,0.00000485517,0.0000040775026,0.00012809537,0.0006208584,0.0005027977,0.0000022170716,0.00014115583,0.000010997414,0.00014284406],"study_design_scores_gemma":[0.00015323349,0.0002766893,0.99741143,0.00002017782,0.0000056974654,0.0009924172,0.00039597164,0.00036300498,0.000010142088,0.0002599145,0.00006711744,0.000044191023],"about_ca_topic_score_codex":0.0017544063,"about_ca_topic_score_gemma":0.44417834,"teacher_disagreement_score":0.44242394,"about_ca_system_score_codex":9.3353583e-7,"about_ca_system_score_gemma":0.0015481903,"threshold_uncertainty_score":0.99999636},"labels":[],"label_agreement":null},{"id":"W4254353681","doi":"10.1139/cjes-37-5-795","title":"Instabilities in the Labrador Sea water mass structure during the last climatic cycle","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Water mass; Oceanography; Climatology; Paleontology; Earth science","score_opus":0.013331626946172131,"score_gpt":0.17824538101254395,"score_spread":0.16491375406637182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4254353681","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99274474,0.00036844413,5.853044e-7,0.0046126717,0.00014477523,0.00006212719,0.0000141528035,0.0000013958102,0.0020511104],"genre_scores_gemma":[0.9993351,0.000040111547,0.000070176444,0.00041914114,0.00009091081,1.9448e-7,0.0000014213254,5.7638226e-7,0.000042346965],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990711,0.00010932506,0.00019156723,0.000080602025,0.00021662792,0.00033077356],"domain_scores_gemma":[0.9996846,0.00008199347,0.000040118288,0.00006408593,0.000023726567,0.00010551291],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00064863905,0.00006505068,0.00009231015,0.00005860632,0.00068364653,0.00019619415,0.00038528547,0.000022698556,0.005403939],"category_scores_gemma":[0.000038200807,0.000024272278,0.000033756984,0.0002481935,0.00041337693,0.0003070299,0.0000021896853,0.0001551103,0.000043783504],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005486335,0.0000015092678,0.94337755,0.000005693442,0.000003456322,0.000030347379,0.0060377233,0.045331,0.0000071585105,0.000019744975,0.00003181048,0.0051485165],"study_design_scores_gemma":[0.000075915945,0.00010308856,0.9853805,0.000010354362,0.0000025654754,0.000050591694,0.007307446,0.0007781902,0.000021065309,0.0019720402,0.0042473646,0.000050895338],"about_ca_topic_score_codex":0.013573133,"about_ca_topic_score_gemma":0.70353055,"teacher_disagreement_score":0.6899574,"about_ca_system_score_codex":0.0000015274912,"about_ca_system_score_gemma":0.00009521025,"threshold_uncertainty_score":0.9955053},"labels":[],"label_agreement":null},{"id":"W4254700503","doi":"10.1139/cjes-2015-0073","title":"Embracing open access and offering greater choice for authors","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"scientometrics and bibliometrics research","field":"Decision Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology","score_opus":0.8505362065905454,"score_gpt":0.6242516246210477,"score_spread":0.22628458196949774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4254700503","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9781576,0.00085407833,0.0012963074,0.0027892902,0.0017058376,0.00022466575,0.000016906148,0.0000020764992,0.014953265],"genre_scores_gemma":[0.9957399,0.000007977809,0.0025019203,0.000236772,0.00017523556,0.0000017430493,1.3784755e-7,0.000004315274,0.0013320277],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99588966,0.000110458386,0.0005347058,0.0003508053,0.0025314023,0.00058296113],"domain_scores_gemma":[0.9931124,0.0013868684,0.00034558444,0.00019882801,0.0025822632,0.0023740458],"candidate_categories":["metaresearch","bibliometrics","scholarly_communication","open_science"],"consensus_categories":["metaresearch","bibliometrics"],"category_scores_codex":[0.032699253,0.0000925399,0.0002673295,0.025468096,0.0006005279,0.02003946,0.005598424,0.00005122727,0.00012347176],"category_scores_gemma":[0.038843237,0.000058799684,0.0000633275,0.03987866,0.00043581324,0.004395897,0.00047695028,0.0001521384,0.000010973494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018354098,0.0000072247326,0.9426612,0.000003941244,0.000010252474,0.000033208347,0.00051555043,0.00044735285,0.00005621056,0.0013010512,0.010935281,0.044010337],"study_design_scores_gemma":[0.0010315191,0.00083028886,0.73025733,0.00005610213,0.000010071008,0.00017025336,0.0013987465,0.0053122872,0.000771073,0.045245536,0.21462916,0.0002876611],"about_ca_topic_score_codex":0.00500054,"about_ca_topic_score_gemma":0.025082208,"teacher_disagreement_score":0.21240392,"about_ca_system_score_codex":0.00001912154,"about_ca_system_score_gemma":0.0035437387,"threshold_uncertainty_score":0.9997818},"labels":[],"label_agreement":null},{"id":"W4255000921","doi":"10.1139/cjes-38-8-1129","title":"Geochemistry and oxygen isotopic composition of the Canton Saint-Onge wollastonite deposit, central Grenville Province, Canada","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université de Montréal; Government of Canada; Polytechnique Montréal; Université du Québec à Montréal; Université du Québec à Chicoutimi","funders":"Université de Montréal; Université du Québec à Chicoutimi","keywords":"Geology; Geochemistry; Wollastonite; Mineralogy","score_opus":0.007522022151191139,"score_gpt":0.17428370015776207,"score_spread":0.16676167800657093,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255000921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9917139,0.000508638,0.0002630563,0.0034501608,0.0003005695,0.000056974328,0.00000445546,0.0000019822744,0.0037002992],"genre_scores_gemma":[0.998771,0.000011987377,0.00067513104,0.00020402602,0.000052534928,3.4777696e-7,2.5902094e-7,8.249335e-7,0.00028389646],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989672,0.000036322162,0.0002364178,0.00015247871,0.0002554282,0.0003521535],"domain_scores_gemma":[0.99911326,0.000033842847,0.00022692251,0.00015565987,0.0001284357,0.0003418975],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024010621,0.00008804464,0.00012888003,0.000054101285,0.0003615605,0.00009382902,0.0007559004,0.000036534435,0.000023958679],"category_scores_gemma":[0.000057998164,0.00006333174,0.000038461312,0.0003376296,0.0003031267,0.00015190845,0.00004777546,0.00013463655,1.5135144e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005293557,0.000012611716,0.97976977,0.000049610502,0.000022822112,0.0002507532,0.00043123472,0.0015810971,0.012266326,0.0012274977,0.0010767955,0.0033062003],"study_design_scores_gemma":[0.0003968582,0.00013682041,0.90608704,0.00027722065,0.000017574961,0.0027290187,0.00039087405,0.008524168,0.044115525,0.00063501886,0.036393248,0.00029662915],"about_ca_topic_score_codex":0.4144616,"about_ca_topic_score_gemma":0.9045264,"teacher_disagreement_score":0.49006483,"about_ca_system_score_codex":0.000033469638,"about_ca_system_score_gemma":0.003228957,"threshold_uncertainty_score":0.58943754},"labels":[],"label_agreement":null},{"id":"W4255008851","doi":"10.1139/cjes-37-2-3-235","title":"Modelling 3D architecture of western Grenville from surface geology, xenoliths, styles of magma emplacement, and Lithoprobe reflectors","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Felsic; Mafic; Crust; Underplating; Petrology; Gneiss; Xenolith; Geochemistry; Ultramafic rock; Pluton; Magma; Mylonite; Tectonics; Metamorphic rock; Basalt; Seismology; Lithosphere; Shear zone; Volcano","score_opus":0.01999691682316052,"score_gpt":0.20571396852055954,"score_spread":0.18571705169739902,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255008851","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99402934,0.0033124527,0.0000838938,0.00044996635,0.000041490694,0.000037807487,0.000082345425,0.0000016834465,0.0019610303],"genre_scores_gemma":[0.9939264,0.0001749721,0.0056549986,0.000078016354,0.000037047175,3.939341e-8,0.00000518616,0.0000010999104,0.00012222774],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987738,0.000082071245,0.00039852838,0.0001914258,0.00023741306,0.0003167568],"domain_scores_gemma":[0.9990658,0.00014623403,0.00021898073,0.0000894873,0.00007376472,0.00040573443],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00040494715,0.000115078925,0.0003251351,0.00014337302,0.00014280008,0.000033185323,0.00032102474,0.000062697385,0.0076491367],"category_scores_gemma":[0.000035403413,0.000075723074,0.00007764256,0.00035463256,0.00087781687,0.00010905745,0.000006509988,0.00015894063,0.000007402074],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020568908,0.0000043279074,0.79382205,0.0000057440607,0.000020898287,0.00000998103,0.00020673362,0.2021066,0.00008450126,0.000008260001,0.0000049325095,0.0037054194],"study_design_scores_gemma":[0.0004740731,0.0013122148,0.94872755,0.00014090723,0.00009731292,0.00010427169,0.00067074574,0.0300693,0.0012572743,0.012646219,0.004146824,0.0003533116],"about_ca_topic_score_codex":0.13124146,"about_ca_topic_score_gemma":0.34623972,"teacher_disagreement_score":0.21499826,"about_ca_system_score_codex":7.9887053e-7,"about_ca_system_score_gemma":0.00020566052,"threshold_uncertainty_score":0.993258},"labels":[],"label_agreement":null},{"id":"W4255742917","doi":"10.1139/cjes-2016-0081","title":"Early–Middle Paleozoic Ecosystem Evolution and Revolution (Part 1 of 2) / Évolution et révolution des écosystèmes du Paléozoïque précoce et moyen (Partie 1 de 2)","year":2016,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Paleozoic; Geology; Paleontology","score_opus":0.03400773181320233,"score_gpt":0.21679304692665988,"score_spread":0.18278531511345755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255742917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9103113,0.07616213,0.0025839442,0.0025279312,0.0015836025,0.000192252,0.00032984067,0.000009601203,0.0062994314],"genre_scores_gemma":[0.9949359,0.0029715025,0.001549332,0.000044610028,0.0002871133,0.0000014513442,0.0000020935786,0.0000030711674,0.00020491109],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99626565,0.0011186072,0.00088124565,0.0003629603,0.0004623292,0.0009092238],"domain_scores_gemma":[0.9971176,0.00047755908,0.00086088927,0.00016496096,0.00041194994,0.00096705195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0051462525,0.0002720238,0.00046547852,0.00064396125,0.0008173434,0.00014239,0.00040544852,0.00031803918,0.00028448604],"category_scores_gemma":[0.000789458,0.00021011225,0.00018656152,0.0006639174,0.002598528,0.0022206595,0.000004613078,0.00030199898,0.000011853898],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004444544,0.000020008634,0.97808796,0.00010927874,0.000054077584,0.00005191655,0.0012617856,0.00034816813,0.00025187503,0.0071604494,0.00041135598,0.012198664],"study_design_scores_gemma":[0.00048480404,0.0011595413,0.98067707,0.0019778959,0.00008127561,0.0010189951,0.0004706677,0.0012699215,0.000110979825,0.01074998,0.0017440164,0.00025485692],"about_ca_topic_score_codex":0.03882196,"about_ca_topic_score_gemma":0.79987955,"teacher_disagreement_score":0.76105756,"about_ca_system_score_codex":0.0000436993,"about_ca_system_score_gemma":0.0041066622,"threshold_uncertainty_score":0.9675786},"labels":[],"label_agreement":null},{"id":"W4255785558","doi":"10.1139/e00-082","title":"A comparative <sup>40</sup>Ar/<sup>39</sup>Ar conventional and laserprobe study of muscovite from the Port Mouton pluton, southwest Nova Scotia","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University","keywords":"Pluton; Muscovite; Geology; Nova scotia; Geochemistry; Amphibole; Monazite; Zircon; Metamorphic rock; Closure temperature; Orogeny; Mineralogy; Paleontology; Tectonics; Quartz","score_opus":0.030895137857618445,"score_gpt":0.22635890863809585,"score_spread":0.1954637707804774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255785558","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99615693,0.0010307285,0.000013080723,0.0012242562,0.00009054166,0.00016228888,0.00018109691,0.0000044506164,0.0011366288],"genre_scores_gemma":[0.9990427,0.000017151333,0.00025556659,0.0003928975,0.00015154498,3.1445128e-7,0.00002664999,0.0000018169937,0.000111340036],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99773085,0.00018505384,0.0006192139,0.0003546466,0.00062264036,0.00048761428],"domain_scores_gemma":[0.998171,0.0003704343,0.00036273862,0.0001594163,0.00024060736,0.0006958482],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000939687,0.00021304862,0.00049587974,0.00022154882,0.0004675558,0.00019293198,0.0006557788,0.00006831098,0.0077992235],"category_scores_gemma":[0.00014192969,0.0001253893,0.00015209956,0.0009027079,0.001215326,0.00038161132,0.000021811342,0.0003130497,0.00007250224],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035172096,0.000041530046,0.96696526,0.000002470676,0.000075826945,0.00008120483,0.0018809561,0.030434163,0.000014394336,0.000020451113,0.00013067738,0.00031789587],"study_design_scores_gemma":[0.0005170603,0.00069017016,0.9760731,0.000045546218,0.000093133036,0.00008289721,0.008883958,0.010717129,0.000028578012,0.0013600575,0.0013272988,0.00018111264],"about_ca_topic_score_codex":0.23059274,"about_ca_topic_score_gemma":0.7247403,"teacher_disagreement_score":0.49414757,"about_ca_system_score_codex":0.0000029755834,"about_ca_system_score_gemma":0.00060014747,"threshold_uncertainty_score":0.9931078},"labels":[],"label_agreement":null},{"id":"W4256643169","doi":"10.1139/e02-907","title":"Contents / Sommaire Volume 39, 2002","year":2002,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Political and Social Issues","field":"Social Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Volume (thermodynamics); Geochemistry; Thermodynamics","score_opus":0.07097881726105446,"score_gpt":0.2816619151157587,"score_spread":0.21068309785470427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4256643169","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3513777,0.09423887,0.00001863421,0.122428685,0.010847471,0.00014845577,0.00006962995,0.000011708629,0.42085886],"genre_scores_gemma":[0.7949658,0.0006833609,0.00017912156,0.0012154364,0.0016121299,4.019941e-7,1.101922e-7,0.000006297312,0.20133732],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9970246,0.00031561838,0.0004992675,0.00019767934,0.000697914,0.0012649334],"domain_scores_gemma":[0.9966643,0.00012578799,0.00027080413,0.00009176483,0.0003432302,0.0025041138],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["sts","insufficient_payload"],"category_scores_codex":[0.001113436,0.0001675236,0.0003590727,0.00023691886,0.0017415375,0.0004253108,0.0008428491,0.00019015657,0.019934274],"category_scores_gemma":[0.0007476499,0.00015344773,0.00023277442,0.0009319208,0.0064018634,0.0010701455,0.000015331532,0.00035764725,0.0014112786],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057166676,0.00021429925,0.17586811,0.00005528275,0.00016690149,0.0015182846,0.06739764,0.000091797076,0.00003173871,0.4816073,0.18159153,0.091451414],"study_design_scores_gemma":[0.00018940201,0.00029966113,0.019210225,0.00019019698,0.000036604513,0.000047850324,0.0071837963,0.0003047315,0.000013386162,0.0056062816,0.9666829,0.00023495615],"about_ca_topic_score_codex":0.08212522,"about_ca_topic_score_gemma":0.31407464,"teacher_disagreement_score":0.7850914,"about_ca_system_score_codex":0.00004839761,"about_ca_system_score_gemma":0.0013321018,"threshold_uncertainty_score":0.99955803},"labels":[],"label_agreement":null},{"id":"W4280599482","doi":"10.1139/cjes-2022-0011","title":"Quantifying simulated fine sand fraction in muddy sediment using laser diffraction","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université du Québec à Rimouski","funders":"","keywords":"Silt; Sediment; Particle-size distribution; Geology; Grain size; Mineralogy; Particle size; Granulometry; Dispersion (optics); Volume (thermodynamics); Matrix (chemical analysis); Range (aeronautics); Sorting; Soil science; Geomorphology; Materials science; Composite material; Optics","score_opus":0.06154769799517973,"score_gpt":0.26442677717618374,"score_spread":0.202879079181004,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4280599482","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976807,0.00050669006,0.000046741185,0.00028586262,0.00049389224,0.000046165373,0.00001387672,0.0000024812005,0.00092358975],"genre_scores_gemma":[0.999365,0.000009367399,0.0004131342,0.00013800454,0.000041722313,8.828202e-8,0.00000520189,7.7053346e-7,0.000026750502],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9990871,0.00007878137,0.00025614552,0.000091107,0.0002534739,0.00023341809],"domain_scores_gemma":[0.9994597,0.000092868635,0.00017803712,0.00003620462,0.000049266946,0.00018393905],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008377232,0.000059161277,0.00010516685,0.00034318722,0.00090165075,0.00012303465,0.00015772239,0.00002156506,0.006759779],"category_scores_gemma":[0.00008457112,0.000046496843,0.000030405587,0.00072748814,0.0000830495,0.0006077892,0.000004135511,0.00021190461,0.000008100175],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006244828,0.000003544803,0.49206078,0.0000020963848,0.0000017356948,0.000021633332,0.000086688335,0.50614244,0.000014897061,0.000003544786,0.000019853413,0.0016365165],"study_design_scores_gemma":[0.00024308573,0.0003809825,0.8560182,0.000022393564,0.0000076546385,0.00017537318,0.0014123896,0.13193665,0.00009929214,0.0005445369,0.009038947,0.00012049779],"about_ca_topic_score_codex":0.043655477,"about_ca_topic_score_gemma":0.20579784,"teacher_disagreement_score":0.3742058,"about_ca_system_score_codex":0.000005926405,"about_ca_system_score_gemma":0.0005224596,"threshold_uncertainty_score":0.9941482},"labels":[],"label_agreement":null},{"id":"W4280618958","doi":"10.1139/cjes-2021-0089","title":"A Random Forest approach to predict geology from geophysics in the Pontiac subprovince, Canada","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University; Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geologic map; Igneous rock; Ultramafic rock; Felsic; Mafic; Geophysics; Geochemistry; Geomorphology","score_opus":0.011743925444438258,"score_gpt":0.1769996818446225,"score_spread":0.16525575640018425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4280618958","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9551454,0.0003836042,0.0058697225,0.01743688,0.0009750108,0.0002194428,0.000022729246,0.000005051014,0.019942164],"genre_scores_gemma":[0.99614906,8.8984785e-7,0.001835816,0.0017564873,0.00008650546,0.0000072415664,0.0000014476927,8.599519e-7,0.00016167057],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985158,0.00017166327,0.00024808466,0.00021735487,0.00043075992,0.00041632366],"domain_scores_gemma":[0.9991197,0.0001749092,0.00014308374,0.0002166409,0.00007205389,0.000273599],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012959297,0.00008614197,0.00016422429,0.00014001684,0.0005572335,0.00012416036,0.00237859,0.000018883064,0.000038373902],"category_scores_gemma":[0.00018653437,0.00006209761,0.000043683896,0.00090663496,0.00014529296,0.00018018158,0.00009787438,0.0002940339,8.436535e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000040810977,0.00007641982,0.5883649,0.000014319039,0.000038346363,0.0013345309,0.008267225,0.35325176,0.000112215,0.025190046,0.020291366,0.0030181007],"study_design_scores_gemma":[0.001441356,0.0005717053,0.61143816,0.000028582377,0.000011528615,0.0008951343,0.005616089,0.048903752,0.00006939323,0.01872791,0.31182927,0.00046713176],"about_ca_topic_score_codex":0.7307404,"about_ca_topic_score_gemma":0.96306884,"teacher_disagreement_score":0.304348,"about_ca_system_score_codex":0.000023434544,"about_ca_system_score_gemma":0.0055991695,"threshold_uncertainty_score":0.99326867},"labels":[],"label_agreement":null},{"id":"W4281475867","doi":"10.1139/cjes-2022-0010","title":"The Northern Crocodile: first report of <i>Borealosuchus</i> (Eusuchia; Crocodylia) from Saskatchewan's lower Ravenscrag Formation (earliest Paleocene) with implications for biogeography","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Saskatchewan Museum; University of Regina","funders":"","keywords":"Postcrania; Geology; Paleontology; Facies; Skull; Biogeography; Genus; Range (aeronautics); Paleogene; Clade; Taxon; Zoology; Cretaceous; Biology; Phylogenetic tree","score_opus":0.012332770145841889,"score_gpt":0.1978640142162335,"score_spread":0.18553124407039162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281475867","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9890496,0.0022793806,0.00031151858,0.004838295,0.0005603759,0.0002387435,0.0012194292,0.000005222922,0.0014974339],"genre_scores_gemma":[0.9986526,0.00004482927,0.0008948284,0.00016264277,0.00009224915,0.000005834316,0.0001097075,0.0000019212002,0.00003542627],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986944,0.00008309606,0.0004467769,0.00018375636,0.00020684057,0.00038508378],"domain_scores_gemma":[0.9983593,0.00038984648,0.0005853664,0.00017694056,0.00023838913,0.00025014646],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0009065493,0.00010983571,0.00018740227,0.00020431852,0.0024809553,0.000051557938,0.00058568973,0.00004715572,0.00019436354],"category_scores_gemma":[0.000073627234,0.00007240466,0.00011461,0.0005382941,0.0011227312,0.00032011943,0.000006598174,0.00016657695,0.0000020973039],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000065932276,0.0000074187874,0.9943726,0.0000028452646,0.000026896849,0.000026203801,0.0003037592,0.0026869802,0.000012881397,0.00007315094,0.00048401428,0.0019372962],"study_design_scores_gemma":[0.00022284528,0.00067742285,0.93749017,0.000010937342,0.000024035267,0.0006436743,0.0013456169,0.00018021018,0.00001839471,0.0016900023,0.05759598,0.00010069763],"about_ca_topic_score_codex":0.025907617,"about_ca_topic_score_gemma":0.9411541,"teacher_disagreement_score":0.9152465,"about_ca_system_score_codex":0.0000042002775,"about_ca_system_score_gemma":0.0017184728,"threshold_uncertainty_score":0.9988177},"labels":[],"label_agreement":null},{"id":"W4281481140","doi":"10.1139/cjes-2022-0001","title":"Revisiting Huronian paleoslopes","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Laurentian University","funders":"","keywords":"Geology; Sedimentary depositional environment; Fluvial; Compaction; Geomorphology; Vegetation (pathology); Section (typography); Precambrian; Paleontology; Hydrology (agriculture); Geotechnical engineering; Structural basin","score_opus":0.025224436412565943,"score_gpt":0.21061480312220343,"score_spread":0.1853903667096375,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281481140","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9567007,0.0036909739,0.000028672011,0.0021179088,0.0005043228,0.00003781508,0.000035515364,0.0000043482814,0.03687974],"genre_scores_gemma":[0.99823296,0.000019640536,0.001032376,0.00047578977,0.00010012232,1.3340814e-7,0.0000025271845,5.8613375e-7,0.00013585568],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909693,0.00007163421,0.0002201357,0.00007962332,0.00025651162,0.00027517043],"domain_scores_gemma":[0.99935,0.000076905475,0.00015061344,0.000044093933,0.00005960349,0.00031875077],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010832774,0.000053226922,0.00009641365,0.00022982812,0.0013883341,0.0001439338,0.00042260505,0.000011694379,0.018603181],"category_scores_gemma":[0.00012646588,0.00003919062,0.000044766355,0.00059291517,0.0001931096,0.0003427841,0.0000057974876,0.0001659615,0.00003746967],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000017404019,9.516774e-7,0.9558708,0.0000037088923,0.0000028066636,0.000045325363,0.00022195552,0.016025255,0.0000010867609,0.0003202504,0.00014230325,0.027363785],"study_design_scores_gemma":[0.000069052076,0.00034427104,0.79165554,0.000011703229,0.000004780192,0.00040127392,0.001630457,0.0008472373,0.000008252235,0.0017097639,0.20321956,0.00009807967],"about_ca_topic_score_codex":0.0048041055,"about_ca_topic_score_gemma":0.05452227,"teacher_disagreement_score":0.20307726,"about_ca_system_score_codex":8.600532e-7,"about_ca_system_score_gemma":0.0008420842,"threshold_uncertainty_score":0.9999117},"labels":[],"label_agreement":null},{"id":"W4281658530","doi":"10.1139/cjes-2021-0162","title":"Fluid sources and mineralizing processes in greenstone belts: a stable isotope (O, H) comparison between the weakly mineralized Moly-Desgagné–Guercheville system and Val-d’Or orogenic gold deposits, Canada","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université Laval; Université du Québec à Chicoutimi","funders":"","keywords":"Geology; Geochemistry; Terrane; Fault (geology); Vein; Tectonics","score_opus":0.027997638760293247,"score_gpt":0.22359900784205258,"score_spread":0.19560136908175935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281658530","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9851422,0.008223989,0.00009808756,0.0056109196,0.00014741402,0.00015251295,0.000014747248,0.0000073983483,0.00060276134],"genre_scores_gemma":[0.99797267,0.000027319133,0.00120759,0.00024352943,0.00004273824,0.0000070567444,9.2589255e-7,0.0000026442096,0.0004955012],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99808365,0.00020564896,0.00047991562,0.00029851636,0.00042973072,0.000502535],"domain_scores_gemma":[0.9986924,0.00030130995,0.00030257116,0.00016271668,0.00014648866,0.00039454523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014651412,0.00015788396,0.00034194638,0.00018714946,0.00095395674,0.00031095665,0.0010207903,0.000032916792,0.000017703145],"category_scores_gemma":[0.00025545334,0.000108000204,0.000028013495,0.0010848553,0.00025512557,0.00035711686,0.00016184975,0.00029675287,1.6395502e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044038068,0.000031896816,0.9552106,0.0005835431,0.00011062738,0.00092452095,0.011093129,0.013841533,0.0016540305,0.0016242465,0.004850703,0.0100311],"study_design_scores_gemma":[0.0045201085,0.0022628387,0.5789494,0.0017575505,0.0001992148,0.010847897,0.069171965,0.05062474,0.0075380965,0.00085497496,0.27088583,0.0023874068],"about_ca_topic_score_codex":0.56807697,"about_ca_topic_score_gemma":0.96845645,"teacher_disagreement_score":0.40037948,"about_ca_system_score_codex":0.00004864784,"about_ca_system_score_gemma":0.0042385594,"threshold_uncertainty_score":0.7519022},"labels":[],"label_agreement":null},{"id":"W4282932625","doi":"10.1139/cjes-2021-0116","title":"Late Pleistocene heather vole, <i>Phenacomys</i>, on the North Pacific Coast of North America: environments, local extinctions, and archaeological implications","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Pleistocene-Era Hominins and Archaeology","field":"Social Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"University of Oxford","keywords":"Holocene; Vole; Pleistocene; Range (aeronautics); Geography; Geology; Context (archaeology); Population; Cave; Interglacial; Ecology; Archaeology; Biology","score_opus":0.024108022668427403,"score_gpt":0.23656105151471968,"score_spread":0.21245302884629227,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4282932625","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98681945,0.0001947468,0.00024320329,0.0112837,0.00016884116,0.00013749918,0.00010752166,0.0000030515605,0.0010419652],"genre_scores_gemma":[0.9986781,0.000121327255,0.00020644232,0.0006552103,0.00006832542,0.0000098844475,0.000002411081,0.0000042156753,0.00025409795],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99842274,0.00034185805,0.00030364766,0.00018678934,0.0003493309,0.0003956052],"domain_scores_gemma":[0.9988764,0.0002649694,0.0002768484,0.00013047109,0.000039405524,0.0004119029],"candidate_categories":["sts"],"consensus_categories":["sts"],"category_scores_codex":[0.00076250086,0.00009700127,0.00019190829,0.0001885518,0.002314801,0.000024154904,0.00055011275,0.000022596192,0.0006270052],"category_scores_gemma":[0.0000988243,0.000069662805,0.0000688206,0.0005583296,0.0057481606,0.000101699334,0.00007057063,0.000288109,0.000003154844],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012121171,0.000028654194,0.98460937,8.9059535e-7,0.000012149303,0.000014725384,0.0037446606,0.00196761,0.000009762444,0.0036650328,0.00030938152,0.00562566],"study_design_scores_gemma":[0.00010012245,0.0004944997,0.8672374,0.0000033126544,0.000007765501,0.00002679253,0.005852594,0.000046227826,0.000004720825,0.00073270395,0.12541415,0.000079742385],"about_ca_topic_score_codex":0.0034947896,"about_ca_topic_score_gemma":0.5684807,"teacher_disagreement_score":0.5649859,"about_ca_system_score_codex":0.00003145587,"about_ca_system_score_gemma":0.0009909255,"threshold_uncertainty_score":0.99898404},"labels":[],"label_agreement":null},{"id":"W4282966137","doi":"10.1139/cjes-2022-0004","title":"Glacial erosion on a snowball Earth: testing for bias in flux balance, geographic setting, and tectonic regime","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Snowball Earth; Glacial period; Craton; Paleontology; Precambrian; Rift; Geomorphology; Tectonics","score_opus":0.0452508031710366,"score_gpt":0.25322905385963435,"score_spread":0.20797825068859774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4282966137","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994022,0.0013047846,0.0000020573784,0.0009427473,0.00039387366,0.00015230218,0.00003240256,0.0000039208257,0.0031458703],"genre_scores_gemma":[0.99874,0.00001202194,0.0007307867,0.0003338033,0.00006109481,0.0000017467299,0.0000057252414,0.0000018472152,0.00011298109],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998365,0.00024461915,0.00027555446,0.00023244717,0.00027481068,0.0006075571],"domain_scores_gemma":[0.9985735,0.00076050573,0.0001704452,0.00007652769,0.00006772729,0.0003513331],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002939313,0.00010216486,0.00019974083,0.0008417908,0.0011886522,0.000080764505,0.00037735084,0.00005479326,0.00070557394],"category_scores_gemma":[0.0006629227,0.000085867294,0.00005125551,0.00084102445,0.0006040174,0.00017195029,0.0000118798625,0.00045445445,0.000009740962],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030927695,0.0000042297065,0.99648494,0.0000059343,0.0000040884006,0.00009606724,0.00012797416,0.002024542,0.000012739031,0.00007845236,0.00006208882,0.0010680308],"study_design_scores_gemma":[0.00039110956,0.0015258439,0.9903725,0.00003709383,0.000005315206,0.000504268,0.0002095658,0.0029382668,0.000016010294,0.0008930778,0.0030046823,0.00010228083],"about_ca_topic_score_codex":0.003197476,"about_ca_topic_score_gemma":0.3584137,"teacher_disagreement_score":0.35521623,"about_ca_system_score_codex":7.719782e-7,"about_ca_system_score_gemma":0.0011565061,"threshold_uncertainty_score":0.9142272},"labels":[],"label_agreement":null},{"id":"W4285494988","doi":"10.1139/cjes-2022-0045","title":"Evolution of a stratigraphic model in a fluvial deltaic wedge: implications for groundwater resource protection in an oil and gas-bearing region in the Upper Cretaceous Dunvegan Formation, Northwest Territories, Canada","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Waterloo; McMaster University; University of Guelph","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Facies; Aquifer; Structural basin; Fluvial; Groundwater flow; Hydrogeology; Sedimentary rock; Paleontology; Sequence stratigraphy; Geochemistry; Groundwater; Geomorphology","score_opus":0.01952910212447488,"score_gpt":0.20722627801193055,"score_spread":0.18769717588745566,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285494988","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99763775,0.0002479328,0.00070664013,0.001229808,0.000043411797,0.000090568414,0.0000101143,0.0000019796391,0.000031803615],"genre_scores_gemma":[0.9998295,0.000013321952,0.000069586735,0.000021733274,0.000021198024,0.000032181575,0.000005446189,0.0000033036747,0.000003779871],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99923056,0.000073083174,0.00030718461,0.00007725608,0.0001464691,0.00016545753],"domain_scores_gemma":[0.99971,0.000016490885,0.00007326169,0.00006911907,0.000046581084,0.00008452197],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005544615,0.00005682661,0.000097676806,0.00053009664,0.00023340857,0.000056172856,0.00017177459,0.000021091608,0.0000013568001],"category_scores_gemma":[0.000024966923,0.000047578254,0.000022212234,0.00082749355,0.0000585635,0.00043438363,0.0000042002407,0.00016395825,8.619694e-9],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006982586,0.0000076409515,0.08211871,0.000017148528,0.0000026718383,0.0000040801565,0.0032904283,0.9135867,0.00023618522,0.00013628346,0.000012196116,0.0005810143],"study_design_scores_gemma":[0.00029487285,0.00011923057,0.08663742,0.0000302057,0.000006532205,0.00006638301,0.005692024,0.90574193,0.000036306377,0.00072422734,0.0005596391,0.00009122758],"about_ca_topic_score_codex":0.44352296,"about_ca_topic_score_gemma":0.9987782,"teacher_disagreement_score":0.55525523,"about_ca_system_score_codex":0.00009403183,"about_ca_system_score_gemma":0.00083462795,"threshold_uncertainty_score":0.56018263},"labels":[],"label_agreement":null},{"id":"W4286009022","doi":"10.1139/cjes-2022-0029","title":"Geochronology, geochemistry, and Hf isotopic compositions of the Early Devonian Heihaibei granite in the East Kunlun Orogen, Northwest China","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Zircon; Geochronology; Geochemistry; Partial melting; Devonian; Subduction; Crust; Isotope geochemistry; Tectonics; Petrology; Paleontology; Isotope","score_opus":0.010117117904319474,"score_gpt":0.17781433859315193,"score_spread":0.16769722068883247,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4286009022","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9914996,0.0013221932,0.0000013305091,0.005085205,0.00009736333,0.000058836402,0.0001118973,0.0000011495638,0.0018224465],"genre_scores_gemma":[0.99952185,0.000012990468,0.000069724265,0.00033205678,0.0000343434,6.2133546e-7,0.0000062131185,6.384332e-7,0.00002157121],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99888915,0.00014869602,0.000262888,0.00013694169,0.00027470628,0.00028762684],"domain_scores_gemma":[0.99941665,0.00007951165,0.00016634986,0.00011150008,0.000040545478,0.00018546401],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005790305,0.00008428588,0.00016279008,0.00011810631,0.0007716372,0.000060683247,0.0007467784,0.000026587924,0.0026500386],"category_scores_gemma":[0.00005212049,0.00004591418,0.00009065229,0.00078194647,0.00093940104,0.00009377473,0.000022741382,0.00031270488,0.0000026311964],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000031406405,0.000008077438,0.99698365,0.0000026015268,0.000008474403,0.000026879818,0.0005408465,0.0016736634,0.00006287821,0.000079622085,0.000020527334,0.0005896385],"study_design_scores_gemma":[0.00010480589,0.0001738078,0.9936591,0.000008761242,0.000015714884,0.0002451372,0.00082048035,0.0004306083,0.000053910462,0.0029361232,0.0014882858,0.000063281805],"about_ca_topic_score_codex":0.090272486,"about_ca_topic_score_gemma":0.6520316,"teacher_disagreement_score":0.5617591,"about_ca_system_score_codex":0.0000020735001,"about_ca_system_score_gemma":0.00033831023,"threshold_uncertainty_score":0.9982617},"labels":[],"label_agreement":null},{"id":"W4286009048","doi":"10.1139/cjes-2022-0019","title":"A micromorphological perspective on the Neoproterozoic Smalfjord and Mortensnes Formation diamictites—Varangerfjord, Norway","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Brock University","funders":"","keywords":"Geology; Glacial period; Diamictite; Precambrian; Paleontology; Sedimentary rock; Sedimentary depositional environment; Geochemistry; Clastic rock; Structural basin","score_opus":0.02187204243221137,"score_gpt":0.1923274755748182,"score_spread":0.17045543314260683,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4286009048","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9855336,0.0009803239,0.000009750426,0.00941885,0.00012750237,0.00007662962,0.00003878157,0.0000024870642,0.0038120896],"genre_scores_gemma":[0.9980505,0.000016928396,0.000150894,0.0016385434,0.00005699629,9.253454e-7,0.0000024125054,7.1922904e-7,0.00008206504],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99893236,0.00014670752,0.00019618565,0.00015525284,0.00028181556,0.0002876579],"domain_scores_gemma":[0.9992123,0.0002172645,0.00014609392,0.00006646973,0.00008145603,0.0002764198],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007678133,0.00009085288,0.00014894165,0.00017441732,0.0010622386,0.00011777339,0.00036687392,0.000022127686,0.011272698],"category_scores_gemma":[0.00018601553,0.000048366688,0.000080216414,0.00051729585,0.0005452521,0.0001607667,0.000013068459,0.000284266,0.000034784298],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006571329,0.000026555539,0.981718,0.000004889739,0.000045030778,0.0003389909,0.0015174638,0.006880947,0.0006416131,0.0027989892,0.0009980618,0.0049637267],"study_design_scores_gemma":[0.00019690815,0.001553399,0.9593408,0.000011219889,0.00003006018,0.0007852863,0.0055410597,0.0034148716,0.0002577066,0.022661068,0.0060184263,0.00018916563],"about_ca_topic_score_codex":0.015692411,"about_ca_topic_score_gemma":0.10216699,"teacher_disagreement_score":0.086474575,"about_ca_system_score_codex":0.000004048146,"about_ca_system_score_gemma":0.00016145948,"threshold_uncertainty_score":0.9908622},"labels":[],"label_agreement":null},{"id":"W4286009361","doi":"10.1139/cjes-2021-0114","title":"Paleomagnetism of the Grum Zn–Pb–Ag deposit, Selwyn Basin, Yukon, Canada","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Windsor","funders":"","keywords":"Geology; Apparent polar wander; Paleomagnetism; Proterozoic; Geochemistry; Craton; Polar wander; Terrane; Batholith; Ordovician; Cretaceous; Metamorphism; Paleontology; Geomorphology; Tectonics","score_opus":0.008455495217120388,"score_gpt":0.15422019292098146,"score_spread":0.14576469770386108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4286009361","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98674154,0.001775605,0.0000034498405,0.0049644434,0.0006006765,0.00004509153,0.000096908865,0.0000015158962,0.0057707913],"genre_scores_gemma":[0.998125,0.000010851506,0.00020145367,0.0013015592,0.000058261547,2.0479162e-7,0.0000026569176,8.9761437e-7,0.00029908636],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99826074,0.00015501009,0.0003583335,0.00015714961,0.0006581014,0.00041068747],"domain_scores_gemma":[0.9988954,0.00012367604,0.00026115493,0.000120628385,0.000097720476,0.0005014364],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006219964,0.00009891792,0.00021323752,0.00012093403,0.00088161015,0.00004782818,0.00097447465,0.000022552886,0.013001919],"category_scores_gemma":[0.00014795494,0.000059002083,0.00013410395,0.0010267989,0.00046505957,0.00010968361,0.000022637014,0.0002683552,0.000004003637],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000033507795,0.0000033319668,0.9875686,0.0000028693073,0.000011602561,0.000054976288,0.000055943747,0.009493907,0.000049102924,0.000045138404,0.0013829164,0.0013282323],"study_design_scores_gemma":[0.000088775145,0.00021874475,0.9757757,0.000009327867,0.000023954404,0.00017320014,0.0004132942,0.00073078036,0.00039818182,0.0015832101,0.02048244,0.00010239439],"about_ca_topic_score_codex":0.93077165,"about_ca_topic_score_gemma":0.9975258,"teacher_disagreement_score":0.06675421,"about_ca_system_score_codex":0.000004535612,"about_ca_system_score_gemma":0.0024660248,"threshold_uncertainty_score":0.9879003},"labels":[],"label_agreement":null},{"id":"W4286610494","doi":"10.1139/cjes-2022-0036","title":"Radiocarbon dates and late Quaternary vertebrates from cave deposits in the central Canadian Rocky Mountains","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Parks Canada; Northern Alberta Institute of Technology; Royal Alberta Museum","funders":"","keywords":"Cave; Radiocarbon dating; Geology; Holocene; Biota; Quaternary; Deglaciation; Paleontology; Glacial period; Pleistocene; Range (aeronautics); Archaeology; Physical geography; Ecology; Geography","score_opus":0.017910572388858213,"score_gpt":0.21240079272126772,"score_spread":0.1944902203324095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4286610494","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9902301,0.0044990345,5.473373e-7,0.0031281665,0.00041863453,0.00007796707,0.000075975586,0.0000014268381,0.0015681578],"genre_scores_gemma":[0.99887365,0.0000711387,0.00004767267,0.0008976487,0.000050828086,5.29637e-7,0.000018459585,0.0000013676819,0.000038689264],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99827933,0.00040341885,0.00021389409,0.00017388405,0.00025040162,0.0006790458],"domain_scores_gemma":[0.9989654,0.0002446611,0.00007845907,0.00008784065,0.00002413928,0.0005995155],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010349015,0.00009506639,0.00015727484,0.00043134595,0.001101638,0.00013976506,0.0006900244,0.000045143457,0.0010555657],"category_scores_gemma":[0.000062362495,0.000067795874,0.000030973984,0.00043868835,0.00048250647,0.00023950421,0.000009155775,0.000436868,0.000011914967],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008326387,0.0000018066867,0.995131,0.0000012459823,0.000009260252,0.0010865604,0.0015098522,0.0019681477,0.0000028448396,0.000038076887,0.000044159744,0.00019870719],"study_design_scores_gemma":[0.00015515246,0.00020906646,0.99047333,0.000007886028,0.0000068953714,0.00073662197,0.0022557154,0.0041229366,0.00000939984,0.0010193563,0.0009191319,0.00008451388],"about_ca_topic_score_codex":0.82960975,"about_ca_topic_score_gemma":0.9977694,"teacher_disagreement_score":0.16815968,"about_ca_system_score_codex":0.0000026722096,"about_ca_system_score_gemma":0.0018190723,"threshold_uncertainty_score":0.9998576},"labels":[],"label_agreement":null},{"id":"W4286610553","doi":"10.1139/cjes-2022-0025","title":"Trapped in a graben: deposition of Huronian gold-bearing conglomerates in a fault-influenced, valley-confined, fluvial system in the southern Cobalt Basin, Ontario, Canada","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Laurentian University","funders":"","keywords":"Geology; Graben; Fluvial; Archean; Structural basin; Geomorphology; Basement; Clastic rock; Geochemistry; Shear zone; Fault (geology); Paleontology; Sedimentary rock; Tectonics","score_opus":0.012444636807765619,"score_gpt":0.18383890570548295,"score_spread":0.17139426889771733,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4286610553","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99674636,0.00053230027,0.000002414318,0.00065167504,0.00017639105,0.00012814315,0.000047929785,0.0000012643749,0.0017135437],"genre_scores_gemma":[0.9995401,0.0000036131,0.00008426824,0.0003321752,0.000013443151,0.0000015737971,0.000004825199,9.60219e-7,0.00001903909],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998422,0.00020360705,0.00050377694,0.00012479513,0.0003895343,0.00035625458],"domain_scores_gemma":[0.9993796,0.0001429066,0.00020685476,0.00006359425,0.000054430137,0.00015266666],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014199602,0.00009224783,0.0002073426,0.0003753873,0.00028944158,0.000092492155,0.0005146093,0.000027570712,0.00070565415],"category_scores_gemma":[0.00006863387,0.000065091546,0.000034476656,0.0010352229,0.00013492769,0.00024495588,0.00000578853,0.00031522266,0.0000017340811],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022450771,0.0000057113457,0.93038374,0.0000143399575,0.000002559071,0.00014966464,0.0033405854,0.06500711,0.000006414754,0.000083366154,0.000024292856,0.00095976365],"study_design_scores_gemma":[0.00043596473,0.0004191745,0.96556175,0.00009160528,0.000004569455,0.00024446924,0.027815012,0.0040025646,0.000029345107,0.00017272845,0.0011021494,0.00012068018],"about_ca_topic_score_codex":0.9940677,"about_ca_topic_score_gemma":0.9999251,"teacher_disagreement_score":0.06100455,"about_ca_system_score_codex":0.000028448954,"about_ca_system_score_gemma":0.0042053508,"threshold_uncertainty_score":0.7726418},"labels":[],"label_agreement":null},{"id":"W4287655285","doi":"10.1139/cjes-2022-0042","title":"Microbial, tidal, and storm activity in a macrotidal to shallow marine shelf environment during the Paleoproterozoic era","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Geology; Sedimentary depositional environment; Sedimentary structures; Clastic rock; Sedimentary rock; Graded bedding; Bedding; Intertidal zone; Paleontology; Siliciclastic; Geochemistry; Geomorphology; Oceanography","score_opus":0.011473362688818822,"score_gpt":0.18014076766435325,"score_spread":0.16866740497553442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4287655285","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99657035,0.00022059235,0.0000050609606,0.0023599276,0.00012391845,0.00011861505,0.000025178231,0.0000013594854,0.00057501567],"genre_scores_gemma":[0.9992483,0.00002310249,0.00032600737,0.00027712964,0.000030400613,0.0000013346593,7.71134e-7,7.796979e-7,0.0000921606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991762,0.000071619244,0.00016233408,0.00011603984,0.00019585252,0.00027793678],"domain_scores_gemma":[0.999531,0.000049103906,0.000079658705,0.000058151498,0.000012265045,0.0002698532],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00072367577,0.00007034867,0.000101405945,0.00020006124,0.00086172007,0.00013205744,0.00032457281,0.000014135635,0.007078292],"category_scores_gemma":[0.000035881774,0.00004579684,0.000024679786,0.00032214684,0.00017863404,0.000244357,0.000028511538,0.00022751694,0.0000125606775],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012788727,0.0000040634186,0.97414416,0.000005147002,0.000002281216,0.000033861492,0.00061828876,0.017249938,0.00008250025,0.000008656338,0.0000090611575,0.0078292275],"study_design_scores_gemma":[0.000103120336,0.00028900738,0.99307245,0.000005439381,0.0000018106186,0.00017815206,0.00043198297,0.00030014143,0.000048386402,0.00013752404,0.0053645326,0.00006747536],"about_ca_topic_score_codex":0.015173796,"about_ca_topic_score_gemma":0.5636225,"teacher_disagreement_score":0.5484487,"about_ca_system_score_codex":0.0000049249675,"about_ca_system_score_gemma":0.00027753864,"threshold_uncertainty_score":0.99382937},"labels":[],"label_agreement":null},{"id":"W4288036303","doi":"10.1139/cjes-2022-0030","title":"Geology, geochemistry, and apatite/titanite U–Pb geochronology of ca. 1.88 Ga alkaline ultrabasic dykes in the Southern Province near Sudbury, Ontario","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"inVentiv Health Clinical","funders":"Wilhelm und Else Heraeus-Stiftung; Deutsche Forschungsgemeinschaft","keywords":"Geology; Ultramafic rock; Titanite; Geochemistry; Geochronology; Breccia; Metamorphism; Basalt; Igneous rock; Sedimentary rock; Clastic rock; Protolith; Metamorphic rock; Outcrop; Basement","score_opus":0.011822922871341098,"score_gpt":0.18131081457470988,"score_spread":0.16948789170336878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4288036303","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942702,0.0013385443,0.0000040252653,0.0016091366,0.00008057731,0.00006765156,0.0000943579,0.0000017297612,0.0025337422],"genre_scores_gemma":[0.99898374,0.00001290894,0.00034146878,0.0003909416,0.000038037757,6.2184796e-7,0.000020120126,0.0000010311282,0.00021112394],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851847,0.00015561053,0.00038320597,0.00021549647,0.00030702454,0.00042022325],"domain_scores_gemma":[0.99910676,0.00020926994,0.00025609267,0.00011641487,0.00006810738,0.00024335891],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001134706,0.000120699966,0.00027080433,0.00016646417,0.0004692041,0.000062020124,0.0006651373,0.000048187423,0.015805004],"category_scores_gemma":[0.0001421284,0.000077134646,0.00008268091,0.00049830525,0.0013664428,0.00011026212,0.000020112075,0.00041012478,0.000012831603],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000132261475,0.000011788591,0.993609,0.000005699405,0.000012611078,0.00011089377,0.0010245524,0.0040670657,0.00014053856,0.000030829317,0.00011359808,0.00086019054],"study_design_scores_gemma":[0.00030161024,0.0007972792,0.97240555,0.000014671463,0.000035166966,0.00057608006,0.00526253,0.0022503764,0.00012864485,0.004502668,0.013532127,0.00019332192],"about_ca_topic_score_codex":0.7177613,"about_ca_topic_score_gemma":0.9876641,"teacher_disagreement_score":0.26990283,"about_ca_system_score_codex":0.000004930932,"about_ca_system_score_gemma":0.001368027,"threshold_uncertainty_score":0.98509467},"labels":[],"label_agreement":null},{"id":"W4289667390","doi":"10.1139/cjes-2022-0035","title":"Seven hydrogeological terrains characteristic of southern Ontario","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Hydrogeology; Bedrock; Geology; Groundwater; Terrain; Hydrology (agriculture); Watershed; Structural basin; Groundwater flow; Streamflow; Geomorphology; Drainage basin; Aquifer","score_opus":0.018154190414256016,"score_gpt":0.19686776817979196,"score_spread":0.17871357776553595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4289667390","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9908117,0.000029931476,0.000009901575,0.001022973,0.00020006811,0.0000423504,0.0000102040785,0.0000015886415,0.007871278],"genre_scores_gemma":[0.99771476,0.00000119945,0.00013161798,0.00039970886,0.000015537746,0.0000013052885,5.2778597e-7,0.0000016818572,0.0017336601],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991443,0.000067166235,0.00020371897,0.000110487046,0.00022567352,0.0002486362],"domain_scores_gemma":[0.99958706,0.00002133897,0.00016592667,0.00006187974,0.0000059070817,0.00015790483],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007366528,0.000061034996,0.00013433208,0.000099652236,0.0005397561,0.0000120990135,0.00040765546,0.000015328696,0.012124861],"category_scores_gemma":[0.000030423325,0.000047264257,0.000052534764,0.00018558578,0.00086630014,0.000094950745,0.00009516761,0.00015478738,0.0000537847],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000062252043,0.000012987045,0.98933506,9.975935e-7,0.000013378483,0.00008803969,0.00573347,0.0040215384,0.000109787965,0.00005039867,0.00039471136,0.00023338562],"study_design_scores_gemma":[0.00023779721,0.0008582859,0.90604204,0.00000742179,0.000026962301,0.00014425686,0.003076516,0.0001724044,0.000054509743,0.0018087638,0.08741586,0.00015520466],"about_ca_topic_score_codex":0.06052737,"about_ca_topic_score_gemma":0.5670161,"teacher_disagreement_score":0.50648874,"about_ca_system_score_codex":0.00002688093,"about_ca_system_score_gemma":0.00017641005,"threshold_uncertainty_score":0.9887782},"labels":[],"label_agreement":null},{"id":"W4289793086","doi":"10.1139/cjes-2021-0101","title":"Mechanisms, volumetric assessment, and prognosis for rapid coastal erosion of Tuktoyaktuk Island, an important natural barrier for the harbour and community","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Northwest Territories; Dalhousie University; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Environment Research Council; Natural Resources Canada; Crown-Indigenous Relations and Northern Affairs Canada; Transport Canada","keywords":"Cliff; Geology; Barrier island; Erosion; Coastal erosion; Overwash; Oceanography; Shore; Natural (archaeology); Harbour; Storm; Landform; Shoal; Physical geography; Geomorphology; Geography; Paleontology","score_opus":0.05097727636016265,"score_gpt":0.2689708532195557,"score_spread":0.21799357685939308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4289793086","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911992,0.003089759,0.00013011649,0.00044189347,0.0004760304,0.00029625744,0.004327102,0.0000014879828,0.00003817486],"genre_scores_gemma":[0.99880195,0.00013602184,0.0007179434,0.00019617865,0.000046750873,0.000003080941,0.00007577757,0.0000024267672,0.000019881922],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989802,0.00015209512,0.0002635927,0.0001082233,0.0002259251,0.00026991573],"domain_scores_gemma":[0.99874943,0.0005360613,0.0002489281,0.00007691008,0.00009891006,0.00028977633],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0027957098,0.00008633617,0.0001684644,0.00024183099,0.002169973,0.00015586318,0.00031900973,0.000021758637,0.00066717644],"category_scores_gemma":[0.00010387319,0.000057040466,0.000055672786,0.00030288324,0.00034845923,0.00029959003,0.000013502555,0.0002412402,7.4375905e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004000461,0.000012479646,0.990725,0.000020981797,0.000017229577,0.0000037877942,0.0011899915,0.000064985616,0.00053227734,0.00015409611,0.0002932198,0.006945953],"study_design_scores_gemma":[0.00050734624,0.0029538278,0.95787513,0.000023540078,0.000051807347,0.00014985858,0.009223014,0.025174709,0.00010626855,0.001338208,0.0024670195,0.00012925234],"about_ca_topic_score_codex":0.02365717,"about_ca_topic_score_gemma":0.67962605,"teacher_disagreement_score":0.65596884,"about_ca_system_score_codex":0.0000023498217,"about_ca_system_score_gemma":0.000584316,"threshold_uncertainty_score":0.99912906},"labels":[],"label_agreement":null},{"id":"W4292395110","doi":"10.1139/cjes-2022-0007","title":"The Cambrian (Furongian) olenid trilobite <i>Peltura</i> from Avalonian Nova Scotia, Canada, with a review of some species from Baltica","year":2022,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Baltica; Trilobite; Nova scotia; Ordovician; Paleontology; Geology; Oceanography","score_opus":0.03588582144797773,"score_gpt":0.23186121831860937,"score_spread":0.19597539687063165,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292395110","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00076638005,0.98304975,8.216882e-7,0.0006802441,0.0016213192,0.0003278697,0.00253361,0.0000028994236,0.011017101],"genre_scores_gemma":[0.0018029979,0.9970934,0.00022184373,0.00036400848,0.00034044648,7.383846e-7,0.000050160565,0.0000038141973,0.00012260895],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9957933,0.0007251901,0.0012423598,0.0004359512,0.0010263261,0.0007769065],"domain_scores_gemma":[0.99525833,0.0016804518,0.0015851132,0.00040193976,0.000120723846,0.00095344643],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017154486,0.00043719332,0.0016700058,0.0002973692,0.0009786455,0.00020934842,0.0020803874,0.00012359144,0.0038617973],"category_scores_gemma":[0.00034571937,0.00024836528,0.0004581164,0.0008453193,0.00167489,0.00039674048,0.0000052855657,0.0008690739,0.000010054087],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037506554,0.00001012985,0.080354705,0.002518628,0.00065883633,0.001204406,0.00020993807,0.000012076498,1.5840591e-7,0.00012881905,0.0061030355,0.90876174],"study_design_scores_gemma":[0.00012261822,0.00028423744,0.142455,0.0130439075,0.00041687142,0.00022013411,0.00021957727,0.000003131228,4.704344e-7,0.000050528317,0.8428582,0.0003253048],"about_ca_topic_score_codex":0.94050336,"about_ca_topic_score_gemma":0.99956614,"teacher_disagreement_score":0.9084365,"about_ca_system_score_codex":0.000014286655,"about_ca_system_score_gemma":0.0234642,"threshold_uncertainty_score":0.99999684},"labels":[],"label_agreement":null},{"id":"W4292920902","doi":"10.1139/cjes-2015-0174","title":"Note of appreciation/Note de reconnaissance","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Legal case studies and regulations","field":"Social Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology","score_opus":0.06640948232598107,"score_gpt":0.32521011217394336,"score_spread":0.25880062984796226,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292920902","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6954921,0.0035700682,0.0013270844,0.022954864,0.0031055636,0.00016513836,0.000020348125,0.000008740707,0.2733561],"genre_scores_gemma":[0.9964875,0.000031570344,0.0023831832,0.0001149608,0.00034441313,2.766595e-7,9.260818e-8,0.0000017078869,0.0006363263],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99907136,0.00009005812,0.00020757709,0.00006471206,0.00030543274,0.00026088193],"domain_scores_gemma":[0.9987166,0.00007764393,0.00021413721,0.00004818254,0.00039214292,0.0005513195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020208417,0.000041435862,0.00011248487,0.00015597108,0.0005922871,0.00006645565,0.00024820672,0.000037503585,0.00006126217],"category_scores_gemma":[0.00095501245,0.0000336964,0.0000545989,0.00050467026,0.0010376311,0.0003269704,0.000005659626,0.000077201505,0.000003886994],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027542435,0.00004468112,0.506271,0.000021780032,0.00005944998,0.00011981392,0.24891298,0.01243063,0.00018165352,0.15396696,0.033871155,0.044092383],"study_design_scores_gemma":[0.00040684929,0.0003135184,0.085499205,0.00011539371,0.000026842556,0.00003921413,0.021803044,0.00038231857,0.0002582986,0.016054066,0.8748917,0.00020956546],"about_ca_topic_score_codex":0.032621127,"about_ca_topic_score_gemma":0.58941525,"teacher_disagreement_score":0.8410205,"about_ca_system_score_codex":0.0000322867,"about_ca_system_score_gemma":0.007156611,"threshold_uncertainty_score":0.9984719},"labels":[],"label_agreement":null},{"id":"W4292993703","doi":"10.1139/cjes-2020-0200","title":"Taphonomy of a monodominant <i>Gryposaurus</i> sp. bonebed from the Oldman Formation (Campanian) of Alberta, Canada","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature; Royal Ontario Museum; Carleton University; University of Toronto","funders":"National Museum of Natural History; Hokkaido University; Smithsonian Institution","keywords":"Geology; Paleontology; Overbank; Cretaceous; Taphonomy; Fluvial","score_opus":0.011057881395196048,"score_gpt":0.17254392886249478,"score_spread":0.16148604746729872,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292993703","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926051,0.0021858867,0.000017772183,0.0017622447,0.0007445434,0.000069356174,0.00027516196,6.263175e-7,0.0023393356],"genre_scores_gemma":[0.99926066,0.000018066907,0.00021581582,0.00039342063,0.000049068043,3.5547936e-7,0.000017724835,7.756844e-7,0.00004409753],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987951,0.00019037361,0.00040647204,0.00010050271,0.00023759964,0.00026993128],"domain_scores_gemma":[0.9987982,0.00038370123,0.0004562167,0.0000996377,0.0000643178,0.00019792601],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006964938,0.00007554722,0.00020214451,0.00011806467,0.0005614397,0.000011091204,0.00059506734,0.000027643675,0.0019378867],"category_scores_gemma":[0.00009426657,0.00005154735,0.000061029954,0.00033451832,0.0005314555,0.00027564188,0.000008291481,0.0001641808,0.0000028080383],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003626665,0.000003882726,0.99112815,0.0000027040142,0.000019145984,0.00002165342,0.000862791,0.004261001,0.000048634847,0.0001527251,0.0019190736,0.0015439566],"study_design_scores_gemma":[0.00018682951,0.00026499393,0.96224225,0.0000119364995,0.000014831957,0.00015786312,0.002202205,0.0014724405,0.00012270406,0.00045135524,0.032799274,0.00007329129],"about_ca_topic_score_codex":0.9731353,"about_ca_topic_score_gemma":0.99942386,"teacher_disagreement_score":0.0308802,"about_ca_system_score_codex":0.000005996753,"about_ca_system_score_gemma":0.003826569,"threshold_uncertainty_score":0.9989745},"labels":[],"label_agreement":null},{"id":"W4293079618","doi":"10.1139/cjes-2021-0129","title":"Age and significance of the Fire Bay assemblage: an Ordovician arc fragment within the Clements Markham belt, northwestern Ellesmere Island, Canada","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; St. Francis Xavier University","funders":"","keywords":"Ordovician; Geology; Paleontology; Bay; Terrane; Volcanic rock; Clastic rock; Paleozoic; Pyroclastic rock; Gondwana; Volcanic arc; Laurentia; Volcano; Sedimentary rock; Subduction; Oceanography; Structural basin","score_opus":0.011599320035581635,"score_gpt":0.18676521976523786,"score_spread":0.1751658997296562,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293079618","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99512416,0.00040607445,0.0000013529103,0.0032371075,0.00026432483,0.000086513544,0.0001697332,9.4460216e-7,0.00070981495],"genre_scores_gemma":[0.99813664,0.000008053003,0.000049584338,0.0015779585,0.000041517047,6.1387806e-7,0.0000074206446,0.0000011207356,0.00017706511],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983866,0.00021210528,0.00032960818,0.00017591576,0.00059034675,0.00030542933],"domain_scores_gemma":[0.99900925,0.00011318423,0.00030304262,0.0001427087,0.000056434783,0.0003753673],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008271176,0.00010418224,0.00017758596,0.000053747393,0.0011286654,0.00008979481,0.00083424133,0.000018193945,0.0027467012],"category_scores_gemma":[0.000049803544,0.000052736716,0.00006281642,0.00055510626,0.0004966757,0.00011779591,0.000028849357,0.00027296648,6.943509e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000061131136,0.000005344525,0.9869489,0.0000027183708,0.000016409309,0.00006560325,0.00030253964,0.010488071,0.000019717078,0.00002035845,0.00013475743,0.0019894815],"study_design_scores_gemma":[0.00010480942,0.00024521662,0.98845905,0.000010613182,0.000023995679,0.000041241216,0.002504778,0.0020490715,0.000039160874,0.00071090925,0.00571372,0.00009744378],"about_ca_topic_score_codex":0.8720306,"about_ca_topic_score_gemma":0.99966097,"teacher_disagreement_score":0.12763032,"about_ca_system_score_codex":0.0000048069787,"about_ca_system_score_gemma":0.0013155171,"threshold_uncertainty_score":0.99816495},"labels":[],"label_agreement":null},{"id":"W4293116163","doi":"10.1139/cjes-2021-0166","title":"<i>Cloeon tzeltal</i> sp. nov. (Ephemeroptera: Baetidae), a Miocene mayfly from Mexican amber","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fossil Insects in Amber","field":"Agricultural and Biological Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Mayfly; Baetidae; Genus; Paleontology; Taxon; Geology; Biology; Ecology; Nymph","score_opus":0.022527462807122048,"score_gpt":0.2063938178755416,"score_spread":0.18386635506841953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293116163","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9827664,0.0010304218,0.000001108221,0.003159977,0.001179937,0.0000850297,0.00014726371,0.000010523194,0.01161933],"genre_scores_gemma":[0.99686396,0.000018758554,0.00052396447,0.0016682107,0.00047792186,0.0000029773832,0.0000063751563,0.000001533764,0.00043627928],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977525,0.00013599488,0.0004273832,0.00030830392,0.0007841587,0.0005916593],"domain_scores_gemma":[0.9986217,0.00015474834,0.00031750966,0.0000775125,0.00011827539,0.0007102458],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008675879,0.00017092725,0.0002639152,0.00008079408,0.0012220021,0.0002313533,0.0009634961,0.000048941114,0.0118162595],"category_scores_gemma":[0.00009494528,0.00007705086,0.00016093599,0.0010001687,0.0005210907,0.00032681623,0.00006963011,0.00037021693,0.000028419534],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000110147266,0.00018262939,0.789033,0.0000075796756,0.00010050759,0.0011966035,0.0016295421,0.0010355925,0.08875869,0.0012234477,0.027485335,0.08923691],"study_design_scores_gemma":[0.00027627236,0.000900977,0.6670801,0.000044941546,0.000024049647,0.00031387832,0.0016236538,0.00009031235,0.0025289042,0.0012032182,0.3255083,0.00040540582],"about_ca_topic_score_codex":0.035108782,"about_ca_topic_score_gemma":0.19873825,"teacher_disagreement_score":0.29802296,"about_ca_system_score_codex":0.000027718697,"about_ca_system_score_gemma":0.00047481523,"threshold_uncertainty_score":0.98908705},"labels":[],"label_agreement":null},{"id":"W4293445217","doi":"10.1139/cjes-2021-0069","title":"A busy time at the beach: multiple examples of gregarious dinosaur behaviour inferred from a set of trackways from the Late Cretaceous of Alberta, Canada","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal Tyrrell Museum","funders":"","keywords":"Geology; Paleontology; Cretaceous; Siltstone; Hatchling; Assemblage (archaeology); Bedding; Trace fossil; Bed; Facies; Structural basin; Biology; Ecology","score_opus":0.022296990388067615,"score_gpt":0.1944199908414173,"score_spread":0.1721230004533497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293445217","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.988989,0.005727667,0.0000015748045,0.001400452,0.0004412912,0.000090978145,0.0028864837,9.976742e-7,0.00046157732],"genre_scores_gemma":[0.99939144,0.000020902035,0.000067613764,0.00018367707,0.000045634235,5.05484e-7,0.00009559706,0.0000015314796,0.00019309472],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983298,0.00035756486,0.00048706573,0.00014835277,0.00035664727,0.0003205389],"domain_scores_gemma":[0.99735284,0.001596126,0.0005813111,0.00017770565,0.000081121005,0.00021089193],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00069028325,0.00011248327,0.0003173927,0.00009329672,0.0006715728,0.000012106149,0.0009078783,0.000049940423,0.0036617578],"category_scores_gemma":[0.00025277957,0.00006779933,0.000096248245,0.00030422155,0.0012091227,0.000108559,0.000021818507,0.00023859668,0.0000027431875],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043203614,0.000004354989,0.9895384,0.0000012546126,0.000043572032,0.000027794042,0.0015672203,0.0068545616,0.000099885605,0.000004748202,0.0010470205,0.0007679869],"study_design_scores_gemma":[0.00022971325,0.00026765597,0.98860615,0.000013429573,0.00004137517,0.000074754134,0.0015644592,0.0014727759,0.000089947986,0.00018004036,0.0073794797,0.00008023895],"about_ca_topic_score_codex":0.9873922,"about_ca_topic_score_gemma":0.9997151,"teacher_disagreement_score":0.012322872,"about_ca_system_score_codex":0.00000781417,"about_ca_system_score_gemma":0.0030126644,"threshold_uncertainty_score":0.997249},"labels":[],"label_agreement":null},{"id":"W4293704644","doi":"10.1139/cjes-2022-0065","title":"Trans-Avalonian green–black boundary (early Middle Cambrian): transform fault-driven epeirogeny and onset of 26 m.y. of shallow-marine, black mudstone in Avalonia (Rhode Island–Belgium) and Baltica","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Onlap; Geology; Ordovician; Baltica; Paleontology; Sedimentary depositional environment; Paleozoic; Gondwana","score_opus":0.018591990373648233,"score_gpt":0.2128946628473111,"score_spread":0.19430267247366287,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293704644","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98982084,0.004029621,0.000010782977,0.0008171711,0.00015788234,0.00016620099,0.00051248993,0.0000032167081,0.0044817985],"genre_scores_gemma":[0.99912673,0.00017829123,0.00056156464,0.00005698951,0.000022479351,4.9661276e-7,0.0000037802577,0.0000022522177,0.00004742195],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979558,0.00023463691,0.00062563526,0.00026512996,0.00041682023,0.00050200126],"domain_scores_gemma":[0.9988026,0.00017954236,0.00026778626,0.00011587289,0.00006301093,0.0005711767],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013411386,0.00017915451,0.00046799643,0.00063368253,0.00043415942,0.000060237828,0.0004596733,0.00008226514,0.00050776335],"category_scores_gemma":[0.000041561838,0.00015925201,0.00011278161,0.0005979833,0.0023823162,0.000402457,0.000003914602,0.00037790558,7.996554e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010754909,0.00001604931,0.9862937,0.000045177596,0.00003388682,0.0001878384,0.0042928746,0.0003783631,0.000054424698,0.000047058387,0.000017095514,0.008525992],"study_design_scores_gemma":[0.0007085326,0.0011870702,0.99324465,0.000057581918,0.000033879893,0.0003556968,0.0013886465,0.0015998168,0.00003747557,0.00078993104,0.0004253948,0.0001713289],"about_ca_topic_score_codex":0.0725487,"about_ca_topic_score_gemma":0.9075923,"teacher_disagreement_score":0.8350436,"about_ca_system_score_codex":0.0000032677758,"about_ca_system_score_gemma":0.0014010892,"threshold_uncertainty_score":0.93362725},"labels":[],"label_agreement":null},{"id":"W4293799582","doi":"10.1139/cjes-2022-0058","title":"Linking Archaean climate change with gold metallogeny","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Archean; Geochemistry; Weathering; Placer mining; Metallogeny; Continental crust; Placer deposit; Siliciclastic; Conglomerate; Proterozoic; Diagenesis; Crust; Pyrite; Earth science; Sedimentary rock; Structural basin; Paleontology; Sphalerite; Sedimentary depositional environment","score_opus":0.02888361951176888,"score_gpt":0.2012708871032111,"score_spread":0.1723872675914422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293799582","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9897224,0.0012064773,0.000003436317,0.00087883114,0.00023861247,0.00004604829,0.00009000901,0.0000032935645,0.0078109344],"genre_scores_gemma":[0.99865645,0.000025323783,0.00058125675,0.00048087887,0.00013967526,5.3628196e-7,0.000012439719,0.0000013399024,0.00010211221],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873734,0.000059757564,0.00020066935,0.00014523385,0.00041383246,0.0004431818],"domain_scores_gemma":[0.99922085,0.00003062221,0.00018005929,0.00007397502,0.00004018216,0.00045432424],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010179825,0.00008697159,0.00014624053,0.0002469497,0.0008887819,0.00009954189,0.00047781432,0.0000128946285,0.0049070506],"category_scores_gemma":[0.000011885292,0.00006335098,0.000074669355,0.00068977254,0.00027465457,0.0002352862,0.000012088205,0.00019530185,0.000012550972],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000901719,0.0000033117815,0.98245245,0.000005628689,0.000020220074,0.00022371867,0.00044772707,0.00599628,0.00003679207,0.000059648795,0.000020207906,0.010724971],"study_design_scores_gemma":[0.00053635356,0.0023754702,0.90697736,0.00008857217,0.00014522135,0.0021441423,0.008916602,0.0042761005,0.00048778547,0.001217476,0.07225397,0.0005809448],"about_ca_topic_score_codex":0.013697483,"about_ca_topic_score_gemma":0.36747333,"teacher_disagreement_score":0.35377586,"about_ca_system_score_codex":0.0000023469715,"about_ca_system_score_gemma":0.00039355006,"threshold_uncertainty_score":0.9960026},"labels":[],"label_agreement":null},{"id":"W4293842799","doi":"10.1139/cjes-2022-0046","title":"Deformation history and tectonic significance of the Sanagak Lake shear zone, Boothia Peninsula, Nunavut","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; University of British Columbia, Okanagan Campus; University of British Columbia; Geological Survey of Canada; University of Manitoba","funders":"","keywords":"Geology; Shear zone; Metamorphism; Hornblende; Terrane; Closure temperature; Craton; Shear (geology); Geochemistry; Metamorphic rock; Seismology; Fold (higher-order function); Tectonics; Geomorphology; Biotite; Petrology; Paleontology; Quartz","score_opus":0.013139527758258426,"score_gpt":0.16861456913324177,"score_spread":0.15547504137498336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293842799","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912099,0.0032927333,0.000009053994,0.0012437783,0.00027512165,0.000049870494,0.000034657336,0.0000017516159,0.0038831073],"genre_scores_gemma":[0.9992457,0.000018076456,0.00016853069,0.00034200086,0.00002661249,2.7678587e-7,0.0000018329323,6.202444e-7,0.00019636162],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989608,0.00009956227,0.00025749402,0.00010896686,0.00034999888,0.00022318681],"domain_scores_gemma":[0.9993085,0.000074835196,0.00023880275,0.00007659607,0.000057564666,0.00024367578],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00073331234,0.00006568001,0.00014480778,0.00014422183,0.0004512166,0.00002568813,0.00042421167,0.000019404359,0.011792398],"category_scores_gemma":[0.00009689378,0.000039715287,0.000082888,0.00045419426,0.00066133984,0.00017861919,0.000013294634,0.00020177838,0.0000053730614],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006619153,0.000003912707,0.9837621,0.0000062621593,0.000009078345,0.000009264605,0.0003035864,0.013319271,0.00011001295,0.00012483595,0.00033447385,0.0020105946],"study_design_scores_gemma":[0.00009524424,0.0002317796,0.957016,0.000009483523,0.000019384373,0.00008958594,0.0004745757,0.0039403997,0.000102971804,0.0017135041,0.036220163,0.00008691436],"about_ca_topic_score_codex":0.017101966,"about_ca_topic_score_gemma":0.39634165,"teacher_disagreement_score":0.37923968,"about_ca_system_score_codex":0.000004998668,"about_ca_system_score_gemma":0.0007767032,"threshold_uncertainty_score":0.98944324},"labels":[],"label_agreement":null},{"id":"W4296131986","doi":"10.1139/cjes-2022-0026","title":"Late Quaternary changes in sediment sources in the Labrador Sea","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Facies; Quaternary; Dolomite; Geochemistry; Carbonate; Sediment; Bedrock; Provenance; Precambrian; Calcite; Geomorphology; Paleontology","score_opus":0.03074298500196852,"score_gpt":0.23875495072116507,"score_spread":0.20801196571919656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296131986","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9847577,0.0020024301,1.9579923e-7,0.010954889,0.00034204056,0.00007433514,0.0000144870055,0.0000011181,0.0018527607],"genre_scores_gemma":[0.99872965,0.000035317305,0.000037960297,0.0010307999,0.000042503238,9.809773e-7,0.0000026090638,7.4816677e-7,0.00011941979],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99839234,0.00051478174,0.00018848017,0.00012211948,0.00032407188,0.00045820553],"domain_scores_gemma":[0.99940974,0.0002452754,0.00008805174,0.00007085073,0.00001755387,0.00016856017],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.003331814,0.000065576714,0.00013048893,0.00057522085,0.0005079962,0.000055135115,0.0007588685,0.00002810527,0.00304743],"category_scores_gemma":[0.0000520192,0.000043296957,0.000028052338,0.0007242999,0.00043911915,0.00013202189,0.00001000489,0.0004409358,0.00002614907],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009360817,0.000004379666,0.9893912,0.0000022021022,0.000002512693,0.0006779717,0.0021034274,0.0073413947,8.3174655e-7,0.000034163877,0.000048982034,0.00038357393],"study_design_scores_gemma":[0.00015813099,0.00036547706,0.9900317,0.000008794061,0.00000174301,0.00042465454,0.0033901387,0.001100818,0.0000077600525,0.0006409763,0.0038131184,0.0000566509],"about_ca_topic_score_codex":0.03552942,"about_ca_topic_score_gemma":0.92242306,"teacher_disagreement_score":0.88689363,"about_ca_system_score_codex":8.821205e-7,"about_ca_system_score_gemma":0.00073784986,"threshold_uncertainty_score":0.99786395},"labels":[],"label_agreement":null},{"id":"W4296579798","doi":"10.1139/cjes-2022-0037","title":"Petrology of the Halifax County complex, North Carolina, Southern Appalachians: constraints from petrography, mineral chemistry, and geothermobarometry","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Greenschist; Metamorphism; Geochemistry; Hornblende; Petrography; Augite; Amphibole; Geothermobarometry; Pigeonite; Plagioclase; Metamorphic facies; Terrane; Facies; Biotite; Paleontology; Quartz","score_opus":0.012395308576355842,"score_gpt":0.17548182148727726,"score_spread":0.1630865129109214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296579798","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953551,0.001020733,0.0000046416403,0.0009154952,0.0001246569,0.000035141587,0.001328142,0.0000019499469,0.0012141012],"genre_scores_gemma":[0.9992556,0.000008077074,0.00024535184,0.0003716331,0.00006122707,2.4098034e-7,0.000020203976,0.0000011278262,0.000036523554],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986986,0.000114837996,0.00031253704,0.00018445458,0.00036725978,0.00032231398],"domain_scores_gemma":[0.99907726,0.00012510366,0.0002754712,0.00010421673,0.00006453689,0.000353421],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041355012,0.000109446795,0.00025933742,0.00009422578,0.0005097806,0.00003643641,0.0006186851,0.000030763673,0.0127858315],"category_scores_gemma":[0.000079144746,0.00006820151,0.00015324695,0.0006480897,0.0020899528,0.000051954677,0.000021515636,0.0002645327,0.0000027714698],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000070447413,0.0000059686863,0.99664575,0.0000030347167,0.000028713514,0.000016338121,0.00013883338,0.0020099313,0.0002158862,0.00001208322,0.00003761272,0.0008787935],"study_design_scores_gemma":[0.00016661047,0.00013014914,0.99418813,0.000004423805,0.000032266595,0.00010594609,0.00088281103,0.0012682537,0.00002225842,0.0016099131,0.0015005319,0.00008868965],"about_ca_topic_score_codex":0.088368066,"about_ca_topic_score_gemma":0.40861923,"teacher_disagreement_score":0.32025117,"about_ca_system_score_codex":0.0000016076492,"about_ca_system_score_gemma":0.00037563217,"threshold_uncertainty_score":0.9881166},"labels":[],"label_agreement":null},{"id":"W4296786065","doi":"10.1139/cjes-2021-0118","title":"Rapid coastal erosion of ice-bonded deposits on Pelly Island, southeastern Beaufort Sea, Inuvialuit Settlement Region, western Canadian Arctic","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Environment Research Council; Natural Resources Canada; Fisheries and Oceans Canada; Parks Canada; Aurora Research Institute","keywords":"Shore; Geology; Storm; Oceanography; Arctic; Physical geography; Coastal erosion; Period (music); Erosion; Permafrost; Beaufort scale; Beaufort sea; Geomorphology; Geography","score_opus":0.018642144694186135,"score_gpt":0.2001540676294376,"score_spread":0.18151192293525148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296786065","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931308,0.00023921239,0.00006952651,0.002321182,0.000977033,0.00017551472,0.0005854034,0.0000035931491,0.0024977517],"genre_scores_gemma":[0.9983058,0.000027546972,0.00016357124,0.0009991539,0.00012933945,5.1542906e-7,0.000043070304,0.00000548432,0.00032550885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99767196,0.0001616675,0.0005044712,0.00024656698,0.0007483244,0.0006670323],"domain_scores_gemma":[0.9981073,0.00012445195,0.00038503483,0.00016377661,0.00014673252,0.0010726722],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009469792,0.00017739597,0.00027149025,0.0006164992,0.0011302823,0.000105685125,0.00067143433,0.000046754285,0.0020740347],"category_scores_gemma":[0.000072095805,0.00014925729,0.000119951976,0.00050695526,0.00047170915,0.0002755058,0.000014777764,0.00037917847,0.000028116083],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003673678,0.0000113422875,0.9875521,0.000012637258,0.000015734666,0.00020747016,0.0017410312,0.00609817,0.0000054388574,0.00007130841,0.00020357208,0.004044473],"study_design_scores_gemma":[0.0007650398,0.0029820448,0.9753798,0.00023592394,0.00006709354,0.0011219768,0.0071404935,0.0024994276,0.000048242826,0.0006557907,0.008696534,0.0004076262],"about_ca_topic_score_codex":0.42736018,"about_ca_topic_score_gemma":0.98456633,"teacher_disagreement_score":0.55720615,"about_ca_system_score_codex":0.000021162468,"about_ca_system_score_gemma":0.0043833684,"threshold_uncertainty_score":0.9988382},"labels":[],"label_agreement":null},{"id":"W4296916255","doi":"10.1139/cjes-2022-0051","title":"Petrogenesis of siliciclastic sediments and sedimentary rocks explored in three-dimensional Al<sub>2</sub>O<sub>3</sub>–CaO<sup>*</sup>+Na<sub>2</sub>O–K<sub>2</sub>O–FeO+MgO (A–CN–K–FM) compositional space","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Felsic; Mineralogy; Sedimentary rock; Siliciclastic; Geochemistry; Clastic rock; Plagioclase; Feldspar; Weathering; Radiogenic nuclide; Mafic; Sedimentary depositional environment; Quartz","score_opus":0.01158675043602228,"score_gpt":0.18945648774778992,"score_spread":0.17786973731176764,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296916255","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937298,0.0020099971,0.000033868437,0.0017193237,0.00063195406,0.00037312307,0.0013692459,0.00002365934,0.00010898315],"genre_scores_gemma":[0.9975419,0.00016610863,0.00021084762,0.0012967846,0.00026480894,0.000011346618,0.0004763429,0.000025672885,0.000006184371],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99263954,0.00044979146,0.0015825405,0.0011583994,0.0024720505,0.0016976495],"domain_scores_gemma":[0.9958431,0.0005011454,0.0009639062,0.000406116,0.00032293063,0.0019627707],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0020597482,0.00076836854,0.0010617399,0.0014318408,0.0021538825,0.0002872049,0.0011191473,0.00019624342,0.0009170703],"category_scores_gemma":[0.0001266654,0.0007509323,0.0004973628,0.0023813734,0.001290203,0.001217814,0.00017307336,0.00096723466,0.00008010535],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026695136,0.00018377787,0.3596951,0.0000754222,0.00033964886,0.0006499594,0.0006882825,0.14139238,0.48959228,0.000012506097,0.0014393404,0.005664356],"study_design_scores_gemma":[0.0025522776,0.001767416,0.21909857,0.00038763057,0.00041791616,0.0014358982,0.0041638264,0.04159003,0.72577596,0.00089888973,0.00043958783,0.0014719915],"about_ca_topic_score_codex":0.0048750057,"about_ca_topic_score_gemma":0.058427736,"teacher_disagreement_score":0.2361837,"about_ca_system_score_codex":0.000108574226,"about_ca_system_score_gemma":0.0020044786,"threshold_uncertainty_score":0.99999624},"labels":[],"label_agreement":null},{"id":"W4297206772","doi":"10.1139/cjes-2022-0054","title":"Structural evolution and U-Pb geochronology of the metasedimentary Nemiscau subprovince, Canada: implications for Archean tectonics in the Superior Province","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec); Université du Québec à Montréal","funders":"","keywords":"Geology; Archean; Geochemistry; Metamorphism; Terrane; Anatexis; Mafic; Shear zone; Geochronology; Orogeny; Metamorphic facies; Felsic; Metamorphic rock; Granulite; Gneiss; Petrology; Tectonics; Facies; Partial melting; Seismology; Paleontology; Crust","score_opus":0.014574625029326037,"score_gpt":0.19402023825265258,"score_spread":0.17944561322332653,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297206772","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98739177,0.0015430491,0.0000065372037,0.010459827,0.00010035358,0.00013000895,0.00023024553,5.439415e-7,0.00013766618],"genre_scores_gemma":[0.9993315,0.000004013085,0.00021383572,0.00040991342,0.000021412867,0.0000013804529,0.000006628222,4.884929e-7,0.000010838505],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99911964,0.000110618515,0.00022560166,0.000117141935,0.00017817554,0.00024882786],"domain_scores_gemma":[0.99942625,0.00019052319,0.0001373511,0.00008423402,0.00004248212,0.0001191874],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00062887865,0.00005946567,0.00012523317,0.00008379179,0.0006502676,0.000022445096,0.0005566852,0.000014275568,0.00047533377],"category_scores_gemma":[0.000103946586,0.00003071752,0.00005303704,0.00043201845,0.000532134,0.00007875,0.000014682016,0.00016858584,8.922972e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057304183,0.0000021115811,0.9921606,0.0000033893834,0.0000068689665,0.000002542972,0.00007399299,0.0055788127,0.00010693793,0.0004831441,0.00009291635,0.001482955],"study_design_scores_gemma":[0.0000936851,0.00016641767,0.98809075,0.00000256719,0.000017129905,0.000094457435,0.0008666359,0.0017441263,0.00005868141,0.0071442425,0.0016736052,0.00004768366],"about_ca_topic_score_codex":0.7769093,"about_ca_topic_score_gemma":0.99675137,"teacher_disagreement_score":0.21984205,"about_ca_system_score_codex":0.000010403425,"about_ca_system_score_gemma":0.00306356,"threshold_uncertainty_score":0.5434624},"labels":[],"label_agreement":null},{"id":"W4297206778","doi":"10.1139/cjes-2022-0089","title":"The mid-Cretaceous Peninsular Ranges orogeny: a new slant on Cordilleran tectonics? III: the orogenic foredeep","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; McMaster University","funders":"","keywords":"Geology; Paleontology; Cretaceous; Cenomanian; Trough (economics); Aptian; Foreland basin; Fluvial; Structural basin","score_opus":0.017362367382149656,"score_gpt":0.1925472076694452,"score_spread":0.17518484028729553,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297206778","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96993124,0.013332326,0.0000060795733,0.01278797,0.00051927456,0.000112237205,0.00003102466,0.0000055420846,0.0032743216],"genre_scores_gemma":[0.9979478,0.00013974418,0.00008187647,0.0011905839,0.00014855564,8.2339966e-7,0.0000039442248,0.000001836143,0.000484811],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99796623,0.00019501368,0.00034358984,0.00021736411,0.00067311275,0.00060470897],"domain_scores_gemma":[0.99840015,0.00045325552,0.00023530501,0.00018825666,0.00007063449,0.0006523977],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014506116,0.00014518444,0.00022418635,0.00013843745,0.003100671,0.00026010314,0.0011603376,0.000029759143,0.011583007],"category_scores_gemma":[0.00021826939,0.00006643863,0.00024869546,0.0009092097,0.0007246265,0.00009872654,0.000022961163,0.00043418986,0.000050437367],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046859658,0.00004341469,0.664057,0.00000807581,0.00049793185,0.0014857394,0.002997904,0.17243038,0.00034493735,0.0018932228,0.009713836,0.14605892],"study_design_scores_gemma":[0.0012949095,0.0037834852,0.22105396,0.000029676694,0.00021270008,0.0025149463,0.007514552,0.013888071,0.0010795428,0.031774774,0.7161476,0.0007058059],"about_ca_topic_score_codex":0.027950233,"about_ca_topic_score_gemma":0.46875423,"teacher_disagreement_score":0.7064338,"about_ca_system_score_codex":0.0000045379848,"about_ca_system_score_gemma":0.0011773615,"threshold_uncertainty_score":0.99819714},"labels":[],"label_agreement":null},{"id":"W4299665098","doi":"10.1139/cjes-2017-0213","title":"Note of appreciation / Note de reconnaissance","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Legal case studies and regulations","field":"Social Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology","score_opus":0.050020314383902566,"score_gpt":0.33394197248795016,"score_spread":0.28392165810404757,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4299665098","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.787412,0.0009374093,0.0005828727,0.019881269,0.0022696157,0.00011096149,0.000014742824,0.0000038191174,0.18878733],"genre_scores_gemma":[0.9975734,0.000060177532,0.00136549,0.00006056788,0.0003543157,2.3986533e-7,5.6720037e-8,0.000001525823,0.000584254],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992288,0.000052897638,0.0001786492,0.00006638255,0.00022779057,0.0002455027],"domain_scores_gemma":[0.9989156,0.0000635196,0.00041026078,0.00009167675,0.00023281261,0.00028611787],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0015261509,0.000039450777,0.00010741704,0.00011031677,0.0026415666,0.00018095132,0.00042434325,0.00003880247,0.00007634221],"category_scores_gemma":[0.0011260968,0.00003242267,0.00006318923,0.00013347149,0.0015652082,0.0005007736,0.000008303926,0.000076958015,0.0000024779038],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015790638,0.000023866703,0.73393595,0.000022369928,0.00004095893,0.000080580634,0.073726326,0.0016780864,0.0005002826,0.100906074,0.004559326,0.08451037],"study_design_scores_gemma":[0.00024212914,0.00015276672,0.70759535,0.00014299668,0.000021671322,0.000016673957,0.0040570186,0.00026583855,0.00043153588,0.00755689,0.27936363,0.00015347484],"about_ca_topic_score_codex":0.048732452,"about_ca_topic_score_gemma":0.7376643,"teacher_disagreement_score":0.6889318,"about_ca_system_score_codex":0.000019116216,"about_ca_system_score_gemma":0.0031909158,"threshold_uncertainty_score":0.99865687},"labels":[],"label_agreement":null},{"id":"W4300081363","doi":"10.1139/cjes-2016-0178","title":"Note of appreciation / Note de reconnaissance","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Legal case studies and regulations","field":"Social Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry","score_opus":0.03409496253531401,"score_gpt":0.30140965476428955,"score_spread":0.2673146922289755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4300081363","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86384606,0.0013665425,0.003392002,0.036258575,0.0021151907,0.00013763325,0.00002585473,0.0000071788795,0.09285099],"genre_scores_gemma":[0.99758804,0.00008198952,0.0012012415,0.000077211014,0.00029067518,2.7672814e-7,3.200564e-8,0.0000015926261,0.00075893407],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99917626,0.000075715354,0.00019604788,0.000066721645,0.0002286466,0.0002565982],"domain_scores_gemma":[0.99907297,0.00014342945,0.00021796071,0.000045933208,0.00022930122,0.00029041473],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013567294,0.00003888099,0.00009805166,0.00014677327,0.0006501719,0.000039469815,0.00021200666,0.000036406385,0.00015031526],"category_scores_gemma":[0.00072496454,0.000024731162,0.00005927838,0.00034781807,0.0010834932,0.00035050133,0.0000044343874,0.000044418026,0.0000041690487],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002534953,0.000031118892,0.5145797,0.000020645082,0.000050304207,0.00006627444,0.07034773,0.0007158789,0.0038893654,0.15670633,0.008154756,0.24541254],"study_design_scores_gemma":[0.00049059116,0.00032567064,0.3098235,0.00035956575,0.000028443017,0.00003100305,0.0050592157,0.00007452354,0.0017854016,0.014922743,0.6668468,0.00025251546],"about_ca_topic_score_codex":0.013319633,"about_ca_topic_score_gemma":0.5268373,"teacher_disagreement_score":0.65869206,"about_ca_system_score_codex":0.00002802519,"about_ca_system_score_gemma":0.0031710402,"threshold_uncertainty_score":0.9932507},"labels":[],"label_agreement":null},{"id":"W4300139522","doi":"10.1139/cjes-2013-0187","title":"NOTE OF APPRECIATION / NOTE DE RECONNAISSANCE","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Legal case studies and regulations","field":"Social Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology","score_opus":0.030381256513910278,"score_gpt":0.2922986514033406,"score_spread":0.26191739488943033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4300139522","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.88944924,0.0010300837,0.00065481424,0.014949434,0.0012173416,0.00015603105,0.000006672812,0.0000046188848,0.09253178],"genre_scores_gemma":[0.9969687,0.00004427542,0.0020393876,0.00012434769,0.0002590824,6.773789e-7,8.295098e-8,0.0000016402278,0.0005618112],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991624,0.00007187183,0.00020722079,0.000063632644,0.00022870852,0.00026616955],"domain_scores_gemma":[0.99901277,0.00009144066,0.00021593529,0.00004482377,0.00031078426,0.00032423498],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010024315,0.000040861512,0.00010295954,0.00015012099,0.00075647346,0.000091024165,0.00021850556,0.000038429233,0.0003168197],"category_scores_gemma":[0.00047923223,0.000032646654,0.000058125675,0.00042194282,0.0008983869,0.0004661035,0.0000045861234,0.000075900905,0.000009281465],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001077525,0.000048290563,0.5571166,0.000039531158,0.00006558973,0.000044998826,0.15727171,0.005571553,0.0018082106,0.10829269,0.023797972,0.14593205],"study_design_scores_gemma":[0.00033204877,0.0003098563,0.62791103,0.00018151631,0.00002864635,0.000029538813,0.015264211,0.0008893483,0.00068413117,0.01761105,0.33647683,0.0002817864],"about_ca_topic_score_codex":0.07220611,"about_ca_topic_score_gemma":0.5224965,"teacher_disagreement_score":0.45029044,"about_ca_system_score_codex":0.000021391434,"about_ca_system_score_gemma":0.0026819897,"threshold_uncertainty_score":0.9339721},"labels":[],"label_agreement":null},{"id":"W4300703544","doi":"10.1139/cjes-2021-0103","title":"Deep long-period earthquakes near Mount Meager, British Columbia","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Volcano; Seismology; Induced seismicity; Seismometer; Mount; Period (music); Volcanism; Tectonics","score_opus":0.015034311945706449,"score_gpt":0.19512019181929716,"score_spread":0.1800858798735907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4300703544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97849214,0.013325917,0.000015778105,0.00042346283,0.0014227014,0.000110015484,0.00007955714,0.000011847313,0.006118594],"genre_scores_gemma":[0.9976918,0.000086803884,0.00064547546,0.00052796205,0.00015910677,9.489501e-7,0.000005466451,0.0000044197855,0.0008780326],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976554,0.0001656889,0.00044230354,0.00027695223,0.00073790696,0.00072176475],"domain_scores_gemma":[0.99867195,0.0001191475,0.00025520372,0.00014185683,0.00013123215,0.00068061316],"candidate_categories":["sts","scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013514814,0.00012289788,0.0003052037,0.00017390792,0.0035933147,0.0014399268,0.00073780335,0.000037030895,0.032310884],"category_scores_gemma":[0.00017743901,0.00015032724,0.000159318,0.0008726556,0.0009211766,0.00046952537,0.000020031173,0.00039581922,0.0000711364],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000040701366,0.0000072978264,0.95721745,0.0000044476633,0.000029906787,0.0009567479,0.0006264889,0.008161529,0.0000011523798,0.000011781567,0.0017221825,0.03125696],"study_design_scores_gemma":[0.00025097607,0.00068301003,0.93020874,0.00002059678,0.000017155684,0.0018135525,0.0016162265,0.0012587926,0.0000021592248,0.00034278512,0.063577145,0.00020883893],"about_ca_topic_score_codex":0.4550118,"about_ca_topic_score_gemma":0.9876401,"teacher_disagreement_score":0.53262824,"about_ca_system_score_codex":0.0000074689824,"about_ca_system_score_gemma":0.0021108438,"threshold_uncertainty_score":0.99959666},"labels":[],"label_agreement":null},{"id":"W4300862204","doi":"10.1139/cjes-2021-0161","title":"Taphonomy and depositional history of the Southfork Quarry (Cypress Hills Formation, late Eocene) in southwestern Saskatchewan, Canada","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saskatchewan Polytechnic; Geological Survey of Canada","funders":"","keywords":"Geology; Sedimentary depositional environment; Paleontology; Facies; Taphonomy; Fluvial; Paleogene; Archaeology; Cretaceous; Structural basin; Geography","score_opus":0.014111760537016679,"score_gpt":0.1696118445113849,"score_spread":0.1555000839743682,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4300862204","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9907518,0.0050935745,0.0000046562,0.0009253523,0.00087830785,0.00005085542,0.000115856354,8.5979997e-7,0.0021787155],"genre_scores_gemma":[0.9990073,0.000006767778,0.0000683146,0.0005728992,0.00002306563,3.5892558e-7,0.0000023623727,7.0621275e-7,0.00031821497],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990542,0.00012067912,0.00027499977,0.00008326693,0.00026057533,0.00020627335],"domain_scores_gemma":[0.9994164,0.000086701206,0.00023275126,0.00005291568,0.000051062525,0.00016015483],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048046393,0.00006298987,0.00012648774,0.00014952116,0.000409896,0.000014688404,0.0002741598,0.000016734479,0.0004642765],"category_scores_gemma":[0.000025173078,0.0000465535,0.000032716398,0.00020512077,0.00044226748,0.00018912631,0.000008848025,0.00015650244,5.2449906e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045364795,0.0000013274024,0.9902441,0.000003867578,0.000004621512,0.000011868216,0.0026881003,0.005627229,0.0000022057316,0.00001645327,0.000988988,0.0004067033],"study_design_scores_gemma":[0.000144583,0.00004978098,0.9792206,0.000015359888,0.0000052529795,0.00009835209,0.005208799,0.00048482468,0.0000040537834,0.00010648555,0.01460203,0.000059853475],"about_ca_topic_score_codex":0.8171711,"about_ca_topic_score_gemma":0.9998073,"teacher_disagreement_score":0.18263622,"about_ca_system_score_codex":0.000021405624,"about_ca_system_score_gemma":0.005056281,"threshold_uncertainty_score":0.8969626},"labels":[],"label_agreement":null},{"id":"W4301187659","doi":"10.1139/cjes-2022-0070","title":"Probabilistic assessment of induced seismicity at the Alberta No. 1 geothermal project site","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"CO2 Sequestration and Geologic Interactions","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Alberta Energy; University of Waterloo","funders":"Natural Resources Canada; Mitacs","keywords":"Geothermal gradient; Induced seismicity; Geology; Pore water pressure; Borehole; Tectonics; Fault (geology); Seismology; Geothermal energy; Petrology; Geotechnical engineering; Geophysics","score_opus":0.02932792485971737,"score_gpt":0.274978874398219,"score_spread":0.24565094953850164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4301187659","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9538589,0.000007738152,0.0000066868884,0.0018844907,0.00034046874,0.00012170778,0.000010573434,0.0000010662852,0.04376835],"genre_scores_gemma":[0.9956366,7.2943163e-7,0.00013332348,0.0006083656,0.000023644008,0.000003902111,7.72119e-7,0.0000016211497,0.0035910325],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990519,0.00013537424,0.0002187745,0.00010437172,0.00030760322,0.00018197527],"domain_scores_gemma":[0.9994481,0.000096495154,0.00022191985,0.000092343966,0.000030026287,0.00011109445],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007883743,0.000054512733,0.000080869024,0.00006780154,0.00072599755,0.000034455847,0.00032058946,0.000012564985,0.014376011],"category_scores_gemma":[0.0001299706,0.000035811732,0.000051479466,0.0003225457,0.00043279436,0.00015876781,0.000057346715,0.00017888288,0.0000306178],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002433982,0.00010221981,0.7950994,0.000007468617,0.00002842985,0.000057468085,0.0043588164,0.1771329,0.009598673,0.0017063156,0.010523676,0.0013602886],"study_design_scores_gemma":[0.0002296519,0.0012010636,0.7323655,0.000013166073,0.000019116305,0.00043816344,0.0010800831,0.013392656,0.00030285385,0.00034994775,0.25043347,0.00017430303],"about_ca_topic_score_codex":0.08938181,"about_ca_topic_score_gemma":0.4802128,"teacher_disagreement_score":0.39083102,"about_ca_system_score_codex":0.000064897424,"about_ca_system_score_gemma":0.00083078217,"threshold_uncertainty_score":0.986525},"labels":[],"label_agreement":null},{"id":"W4301266471","doi":"10.1139/cjes_instruct02_f","title":"Recommandations aux auteurs","year":2002,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Diverse Scientific and Economic Studies","field":"Economics, Econometrics and Finance","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology","score_opus":0.11545510466872502,"score_gpt":0.2271129753155311,"score_spread":0.11165787064680607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4301266471","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.042328782,0.10961357,0.00013161855,0.0338025,0.050182614,0.00009851387,0.00066389097,0.0000045772476,0.76317394],"genre_scores_gemma":[0.1597816,0.0044111614,0.0021690773,0.00075821386,0.0005401079,7.863945e-7,8.4056705e-7,0.000009010102,0.8323292],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984591,0.00002013823,0.0006769048,0.0002483379,0.000050168972,0.00054537144],"domain_scores_gemma":[0.998629,0.000061953964,0.0005537111,0.0001403613,0.00010033876,0.00051469053],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013292251,0.00011688466,0.00033470461,0.00072805374,0.00083291513,0.00049144845,0.00054830406,0.00006949006,0.0793727],"category_scores_gemma":[0.00031901977,0.0001367403,0.00017333281,0.0005716628,0.0012893546,0.0009830743,0.000022550648,0.00018077591,0.008867835],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[8.594364e-7,0.000027632848,0.075593986,0.000010672824,0.00007815884,0.000044899178,0.0024990095,0.0006754941,2.4578387e-7,0.123751715,0.78716475,0.010152583],"study_design_scores_gemma":[0.00018983177,0.000109569686,0.00829142,0.00006506177,0.000011296218,0.000058099547,0.0010862258,0.0023925048,0.0000021782548,0.0026057623,0.9850271,0.00016097198],"about_ca_topic_score_codex":0.00428298,"about_ca_topic_score_gemma":0.03317618,"teacher_disagreement_score":0.19786234,"about_ca_system_score_codex":0.00002968444,"about_ca_system_score_gemma":0.00036775466,"threshold_uncertainty_score":0.9919039},"labels":[],"label_agreement":null},{"id":"W4304756383","doi":"10.1139/cjes-2022-0044","title":"The Terreneuvian MacCodrum Brook section, Mira terrane, Cape Breton Island, Nova Scotia, Canada: age constraints from ash layers, organic-walled microfossils, and trace fossils","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University","funders":"","keywords":"Acritarch; Geology; Radiometric dating; Paleontology; Terrane; Cape; Trace fossil; Stratigraphy; Geochronology; Archaeology; Geography","score_opus":0.012238984248354684,"score_gpt":0.17798044126314544,"score_spread":0.16574145701479076,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4304756383","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9862984,0.005199923,0.0000073129104,0.005151267,0.0010118209,0.000084907355,0.00032052322,0.000004086701,0.0019217778],"genre_scores_gemma":[0.9985815,0.000039705028,0.0001119274,0.0007092169,0.00016866054,2.4959255e-7,0.0000177575,0.0000020970326,0.00036883602],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979666,0.00017661831,0.00043435494,0.00030484854,0.0005094995,0.0006080689],"domain_scores_gemma":[0.99853224,0.00026376918,0.0002597755,0.00012550286,0.00007996749,0.0007387302],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00074138225,0.00017573228,0.0002859444,0.00013941582,0.0015943021,0.00032994678,0.0006930894,0.000049018596,0.018444754],"category_scores_gemma":[0.00013036755,0.00011405575,0.00009255953,0.000588068,0.0009741702,0.00017248822,0.000020078634,0.0004497321,0.000010042377],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022975699,0.000006896834,0.9831379,0.0000032924324,0.000065961714,0.0004018763,0.0003896533,0.0006919762,0.00089184934,0.000009086786,0.0039680465,0.0104104625],"study_design_scores_gemma":[0.00041867088,0.0002701804,0.9506821,0.000018428645,0.000053466498,0.0005481917,0.0028675324,0.0004582161,0.00033378793,0.0011503354,0.042901475,0.00029758806],"about_ca_topic_score_codex":0.9396208,"about_ca_topic_score_gemma":0.99968547,"teacher_disagreement_score":0.06006472,"about_ca_system_score_codex":0.000012024905,"about_ca_system_score_gemma":0.0021932675,"threshold_uncertainty_score":0.9997055},"labels":[],"label_agreement":null},{"id":"W4306639120","doi":"10.1139/cjes-2021-0062","title":"Constraining the lithostratigraphic architecture of a buried bedrock valley using surface electrical resistivity and seismic refraction tomography","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical Methods and Applications","field":"Engineering","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Waterloo; Brock University; University of Guelph","funders":"","keywords":"Bedrock; Geology; Electrical resistivity tomography; Lithology; Geomorphology; Aquifer; Seismic refraction; Groundwater; Geophysics; Paleontology; Electrical resistivity and conductivity; Geotechnical engineering","score_opus":0.02223565414314995,"score_gpt":0.24746098243098816,"score_spread":0.2252253282878382,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4306639120","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99525183,0.0006857797,0.0033249801,0.00037278418,0.00006819786,0.00005498134,0.000010707476,0.0000040099017,0.00022670503],"genre_scores_gemma":[0.9935318,0.000008518174,0.0063958964,0.00002602613,0.000031737763,7.856575e-7,1.340384e-7,0.000002895057,0.0000021864892],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9993604,0.0000916754,0.0001596877,0.00007396481,0.00015427785,0.00016001472],"domain_scores_gemma":[0.99950635,0.00016676338,0.00008870584,0.000058603106,0.000034871475,0.00014469305],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00057408836,0.000056323835,0.00010974616,0.00014906698,0.00046758336,0.00003898581,0.00014369535,0.000015799435,0.000008894813],"category_scores_gemma":[0.000042463937,0.000043021875,0.000049859435,0.0008271788,0.00026900345,0.000059675764,0.0000061307137,0.00029258538,4.0731095e-8],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021130922,0.00003248325,0.05930111,0.000046899135,0.00012785006,0.000031193937,0.0023709354,0.7928128,0.08875477,0.0034604107,0.00010401964,0.052936357],"study_design_scores_gemma":[0.0003978746,0.000807559,0.8391027,0.00009716641,0.00010897768,0.0007528096,0.0023933372,0.13320738,0.0024125937,0.012195221,0.008113885,0.00041052434],"about_ca_topic_score_codex":0.000929515,"about_ca_topic_score_gemma":0.0013940406,"teacher_disagreement_score":0.77980155,"about_ca_system_score_codex":0.0000039337524,"about_ca_system_score_gemma":0.0002817795,"threshold_uncertainty_score":0.35963205},"labels":[],"label_agreement":null},{"id":"W4306944739","doi":"10.1139/cjes-2021-0056","title":"Structure, metamorphism, and mica <sup>40</sup>Ar/<sup>39</sup>Ar thermochronology of the southern Purcell anticlinorium and its transition into the central Kootenay arc, Omineca belt, southeastern British Columbia","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Manitoba; University of Calgary","funders":"","keywords":"Geology; Metamorphism; Thermochronology; Paleontology; Craton; Geochemistry; Greenschist; Zircon; Paleozoic; Metamorphic facies; Metamorphic rock; Basement; Tectonics; Facies; Structural basin","score_opus":0.007731770170900076,"score_gpt":0.15946954201208788,"score_spread":0.1517377718411878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4306944739","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916192,0.004089338,0.0000041097505,0.0035387054,0.00011171787,0.00013989679,0.00035717394,0.0000036849208,0.00013616668],"genre_scores_gemma":[0.99898815,0.000053568823,0.0000799992,0.00058405945,0.00011071076,5.481874e-7,0.000010656661,0.000003187749,0.00016912895],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99791855,0.00034138697,0.0004404171,0.00031498345,0.00043283444,0.00055182475],"domain_scores_gemma":[0.9988959,0.0001489726,0.0002607935,0.00013545062,0.00009966624,0.00045925763],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006063614,0.00014905365,0.0003525155,0.00009979034,0.0011813189,0.00024978997,0.00071277394,0.00007008669,0.0057674265],"category_scores_gemma":[0.00009283704,0.0001032499,0.00016103484,0.0005488314,0.0013405415,0.00016395152,0.000038662176,0.0004106963,0.0000035369665],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003883754,0.000019776138,0.95197403,0.000023642417,0.00011530148,0.000081782106,0.009311545,0.029394764,0.00082291523,0.000017583809,0.00009885405,0.008100941],"study_design_scores_gemma":[0.0005366259,0.0005215372,0.95212466,0.000034533914,0.00019432696,0.00079266686,0.008945443,0.028621932,0.00013890922,0.0062066023,0.001602846,0.00027989713],"about_ca_topic_score_codex":0.21265697,"about_ca_topic_score_gemma":0.69097507,"teacher_disagreement_score":0.4783181,"about_ca_system_score_codex":0.0000030444376,"about_ca_system_score_gemma":0.00035313336,"threshold_uncertainty_score":0.99514145},"labels":[],"label_agreement":null},{"id":"W4306950699","doi":"10.1139/cjes-2022-0069","title":"Canada’s maritime frontier: the science legacy of Canada’s extended continental shelf mapping for UNCLOS","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Hydrographic Service; Bedford Institute of Oceanography; Fisheries and Oceans Canada; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada; Global Affairs Canada","keywords":"United Nations Convention on the Law of the Sea; Continental shelf; Continental margin; Context (archaeology); Geology; Exclusive economic zone; Nautical mile; Territorial waters; Geological survey; Oceanography; Tectonics; Earth science; Paleontology; Law; Political science; Convention; International law","score_opus":0.019633342153675095,"score_gpt":0.21522324789126196,"score_spread":0.19558990573758686,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4306950699","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97516704,0.0019904706,0.000017907583,0.011596462,0.0019499763,0.0002370538,0.00027946278,0.0000016521119,0.008759971],"genre_scores_gemma":[0.9984495,0.000004973994,0.00033535247,0.00066239043,0.000057247413,0.0000011536623,0.000005046669,0.0000015681203,0.00048275624],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976295,0.00015382927,0.0003833482,0.00020477016,0.0008162004,0.00081234286],"domain_scores_gemma":[0.9984502,0.00037380445,0.000266778,0.00013851449,0.00024911662,0.0005215526],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0030475182,0.00010338963,0.0002383928,0.0003205576,0.0031003447,0.00008773296,0.0014414405,0.000023476716,0.0018087904],"category_scores_gemma":[0.00042210758,0.000074961325,0.000059158418,0.00070429826,0.0018732781,0.00030879912,0.000025239944,0.00032879875,8.0940185e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017686501,0.0000027831875,0.99159026,0.0000064919927,0.000015086598,0.0000867328,0.00016493679,0.0024303906,0.000010958237,0.0005646861,0.0047758636,0.00033411413],"study_design_scores_gemma":[0.00028852207,0.00026684563,0.93629694,0.0000120673,0.000010314059,0.0006337793,0.004535703,0.0025672312,0.0001035864,0.000474908,0.0546802,0.00012987778],"about_ca_topic_score_codex":0.99165976,"about_ca_topic_score_gemma":0.9999621,"teacher_disagreement_score":0.082451664,"about_ca_system_score_codex":0.000009599542,"about_ca_system_score_gemma":0.08246126,"threshold_uncertainty_score":0.99910367},"labels":[],"label_agreement":null},{"id":"W4307561848","doi":"10.1139/cjes-2022-0066","title":"Morphology and tectonic modification of the Sudbury impact crater: the North Range","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University; Brock University","funders":"","keywords":"Geology; Impact crater; Paleomagnetism; Norite; Metamorphic rock; Gabbro; Petrography; Impact structure; Seismology; Igneous rock; Geomorphology; Geochemistry; Paleontology; Astrobiology","score_opus":0.01719105083805457,"score_gpt":0.22067631580427263,"score_spread":0.20348526496621805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307561848","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984498,0.00021777199,0.00003082597,0.00061413774,0.00016590387,0.000045533114,0.00005832709,3.3219422e-7,0.0004173673],"genre_scores_gemma":[0.99982077,0.0000011661961,0.000032324642,0.00005088324,0.00003864404,5.3552213e-7,8.6069866e-7,9.1835904e-7,0.0000538996],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994469,0.00007723185,0.000120677345,0.00006335467,0.000141554,0.00015024742],"domain_scores_gemma":[0.99958265,0.0000409254,0.00016344614,0.00008157262,0.000028842036,0.000102583195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047329447,0.00004131623,0.00006786222,0.00006215101,0.00058579515,0.000032953172,0.00041879778,0.000004616589,0.0005297527],"category_scores_gemma":[0.0000059247996,0.000021009968,0.0000429563,0.00030323115,0.00043268304,0.00010881485,0.000015679047,0.00013447573,8.094595e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000016101267,0.0000019106274,0.99244535,3.0073687e-7,0.000004553469,0.0000010972607,0.00032693162,0.005793753,0.00016987816,0.00018745656,0.00010957132,0.00095757155],"study_design_scores_gemma":[0.000055355427,0.0001048625,0.9975845,0.0000020087216,0.000005433901,0.000033745502,0.00054244685,0.0005816447,0.000042044092,0.00016405754,0.00085665245,0.00002722657],"about_ca_topic_score_codex":0.0121565545,"about_ca_topic_score_gemma":0.008227251,"teacher_disagreement_score":0.0052121086,"about_ca_system_score_codex":0.0000028171212,"about_ca_system_score_gemma":0.000832219,"threshold_uncertainty_score":0.9944216},"labels":[],"label_agreement":null},{"id":"W4308141922","doi":"10.1139/cjes-2022-0064","title":"A comparison of trace element concentrations in chromite from komatiites, picrites, and layered intrusions: implications for the formation of massive chromite layers","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université du Québec à Chicoutimi","funders":"U.S. Geological Survey","keywords":"Chromite; Geology; Layered intrusion; Geochemistry; Olivine; Trace element; Silicate; Mineral redox buffer; Ultramafic rock; Plagioclase; Chromitite; Pyroxene; Magma; Magma chamber; Quartz; Mafic; Mantle (geology); Volcano; Paleontology","score_opus":0.03542595358289023,"score_gpt":0.25585958622219956,"score_spread":0.22043363263930932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308141922","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9895217,0.004592319,0.00033923122,0.004729229,0.000056770736,0.00015814792,0.0004908803,9.3076426e-7,0.00011079816],"genre_scores_gemma":[0.99845445,0.00006562289,0.0013334685,0.000096196054,0.000016266655,0.0000025980623,0.000026560223,5.2882956e-7,0.0000043367663],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99907464,0.0000675591,0.00044594094,0.00009166585,0.00015415391,0.00016604253],"domain_scores_gemma":[0.99882686,0.000530224,0.0003542436,0.00006313952,0.000089264686,0.0001362768],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047722293,0.000056159948,0.00018861429,0.00014400354,0.00038758284,0.000031358355,0.0002660349,0.000016978642,0.0010577292],"category_scores_gemma":[0.00015981818,0.000036926478,0.000057705023,0.00048634157,0.00028916463,0.00016756561,0.00000889574,0.000100655074,4.1780166e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010312687,0.0000131388115,0.9568354,0.0000055165647,0.000014627168,5.7617586e-7,0.00091225223,0.0371216,0.0010869513,0.00039465484,0.00012287509,0.0034821266],"study_design_scores_gemma":[0.00025387117,0.00028244918,0.93485457,0.000017627955,0.000031220727,0.0000052621845,0.0037231303,0.053248726,0.00078629056,0.005221242,0.0015168075,0.00005881534],"about_ca_topic_score_codex":0.018293016,"about_ca_topic_score_gemma":0.29494634,"teacher_disagreement_score":0.27665332,"about_ca_system_score_codex":0.000003614555,"about_ca_system_score_gemma":0.0002947207,"threshold_uncertainty_score":0.99985546},"labels":[],"label_agreement":null},{"id":"W4308452385","doi":"10.1139/cjes-2022-0053","title":"Analysis of chemical weathering trends across three compositional dimensions: applications to modern and ancient mafic-rock weathering profiles","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mafic; Weathering; Geology; Mineralogy; Precambrian; Diagenesis; Geochemistry; Trace element","score_opus":0.019000422898850122,"score_gpt":0.23445697002784738,"score_spread":0.21545654712899726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308452385","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978674,0.0007543186,0.00031754584,0.0002985418,0.000036187143,0.000043136806,0.00036626038,0.000002382441,0.00031420376],"genre_scores_gemma":[0.99886274,0.0000037154045,0.0009482099,0.00009286089,0.000026898342,0.0000022430625,0.000027828759,0.0000012028429,0.00003432625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988752,0.000022041495,0.0002799171,0.0001880663,0.00035482307,0.00027996686],"domain_scores_gemma":[0.9992564,0.000040988263,0.00014668165,0.00008799315,0.000057265694,0.00041069975],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004877158,0.000083154984,0.00020453925,0.00035545207,0.0006616892,0.000065327185,0.00030786332,0.000016320757,0.0017140302],"category_scores_gemma":[0.000010634242,0.00007195121,0.00011031582,0.0015945472,0.00014725697,0.000121015226,0.000025392816,0.00010509361,0.000001887865],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010240014,0.000012930039,0.7543318,0.000004850297,0.0001349081,0.0000087816,0.0007796877,0.22992928,0.0077374345,0.00002411024,0.000015045881,0.0070108906],"study_design_scores_gemma":[0.0002193135,0.0002953188,0.875649,0.000025847594,0.00030297443,0.0001341367,0.0035920278,0.11326672,0.003508353,0.00037083513,0.002341204,0.0002942885],"about_ca_topic_score_codex":0.003156167,"about_ca_topic_score_gemma":0.038389776,"teacher_disagreement_score":0.12131713,"about_ca_system_score_codex":0.000005292523,"about_ca_system_score_gemma":0.00017378133,"threshold_uncertainty_score":0.99919856},"labels":[],"label_agreement":null},{"id":"W4309757905","doi":"10.1139/cjes-2022-0077","title":"The Paleoproterozoic Amer supergroup, Amer Fold Belt, Nunavut: stratigraphy, structure, correlations, and uranium metallogeny","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Western University; Geological Survey of Canada; Carleton University; University of Alberta; University of New Brunswick","funders":"","keywords":"Geology; Geochemistry; Orogeny; Metallogeny; Zircon; Phyllite; Conglomerate; Unconformity; Craton; Clastic rock; Kyanite; Metamorphism; Metamorphic rock; Paleontology; Sedimentary rock; Structural basin; Tectonics; Sphalerite; Schist","score_opus":0.011505253684736861,"score_gpt":0.18325641876419715,"score_spread":0.17175116507946028,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4309757905","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9892974,0.0069349613,0.000007869179,0.0018057369,0.00034269303,0.000057672743,0.00009291804,0.000003084708,0.001457685],"genre_scores_gemma":[0.99889815,0.00007276791,0.00036369808,0.00046180896,0.000059024984,5.877649e-7,0.000009269423,0.0000011043628,0.00013359316],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985188,0.00014850339,0.00031268466,0.00019103018,0.0004265693,0.000402362],"domain_scores_gemma":[0.99897754,0.00019502475,0.00016945298,0.00009758219,0.00006919539,0.0004911995],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00066332525,0.0001178645,0.0001831449,0.00018141276,0.001937157,0.00021675047,0.00051112584,0.000028848699,0.006188832],"category_scores_gemma":[0.000091496775,0.00006720244,0.000121223165,0.00076385983,0.0008540108,0.00022041192,0.0000131522365,0.00033337457,0.0000054775937],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000066055472,0.0000026258472,0.99192894,0.0000012834499,0.000035927154,0.000025791018,0.00009022925,0.0032284455,0.000074868745,0.00053655525,0.00014255998,0.0039261812],"study_design_scores_gemma":[0.00010777842,0.00034420387,0.9735111,0.000003553248,0.000043279826,0.00017316717,0.00092830206,0.0014816981,0.00004021448,0.015967438,0.0072671543,0.00013212253],"about_ca_topic_score_codex":0.024862375,"about_ca_topic_score_gemma":0.6822405,"teacher_disagreement_score":0.65737814,"about_ca_system_score_codex":0.0000012424454,"about_ca_system_score_gemma":0.00032077805,"threshold_uncertainty_score":0.9993622},"labels":[],"label_agreement":null},{"id":"W4310035879","doi":"10.1139/cjes-2022-0031","title":"Characterization of the Wager shear zone, Nunavut, Canada: Insights from microstructures and geochronology","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Université Laval; Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"","keywords":"Geology; Geochronology; Shear zone; Archean; Proterozoic; Shear (geology); Geochemistry; Lithosphere; Seismology; Paleontology; Tectonics","score_opus":0.006594872456370946,"score_gpt":0.1535775705728956,"score_spread":0.14698269811652465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4310035879","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963908,0.001299735,0.000002748597,0.0015286432,0.00033971216,0.000028922226,0.00016097978,7.0646e-7,0.00024771836],"genre_scores_gemma":[0.9992009,0.000013259771,0.00007695442,0.00061685184,0.000043475942,9.65172e-8,0.000010991623,5.398874e-7,0.00003693523],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991812,0.00008903441,0.00020860859,0.00011528927,0.00022962921,0.00017624824],"domain_scores_gemma":[0.999445,0.000058970738,0.0001854456,0.00006349731,0.000047043453,0.00020003197],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012625477,0.00006248486,0.0001475085,0.00008099887,0.0004956889,0.00002908093,0.00035584433,0.00002087395,0.005412614],"category_scores_gemma":[0.000048464844,0.000036116857,0.000041126463,0.00036244516,0.0004425673,0.00008403189,0.000016781132,0.00015677986,8.120646e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000051770153,0.0000016847038,0.99074346,0.0000015820468,0.000014069599,0.000019817442,0.00015807735,0.001534607,0.0060562263,0.000056306784,0.00005378977,0.0013552159],"study_design_scores_gemma":[0.000058149766,0.000068018555,0.99051267,0.000003811294,0.000011727743,0.00003799093,0.00020730097,0.0003586538,0.0016027336,0.0016818384,0.0054049864,0.00005214278],"about_ca_topic_score_codex":0.84878236,"about_ca_topic_score_gemma":0.99393284,"teacher_disagreement_score":0.14515047,"about_ca_system_score_codex":0.000002598779,"about_ca_system_score_gemma":0.0011711804,"threshold_uncertainty_score":0.9954966},"labels":[],"label_agreement":null},{"id":"W4310807500","doi":"10.1139/cjes-2022-0028","title":"The morphologic and paleobiogeographic implications of a new early Silurian echinoid from Anticosti Island, Quebec, Canada","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Musée de la Civilisation","funders":"","keywords":"Paleontology; Ordovician; Devonian; Echinoderm; Paleozoic; Geology; Fossil Record; Genus; Biogeography; SPINE (molecular biology); Biology; Ecology","score_opus":0.014257220865150466,"score_gpt":0.19312095787898623,"score_spread":0.17886373701383576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4310807500","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97730565,0.016206162,0.0000065366557,0.0035085506,0.00042316562,0.00006211203,0.00028966245,0.0000014997895,0.0021966673],"genre_scores_gemma":[0.99951756,0.00007739046,0.00016975074,0.0001370334,0.00004098443,2.256689e-7,0.0000025758984,4.2507304e-7,0.00005403693],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99894255,0.00011332475,0.00027690685,0.00013798989,0.00022781342,0.00030138573],"domain_scores_gemma":[0.9989056,0.00025469344,0.00024944954,0.00011166683,0.000042088366,0.00043648327],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00048108926,0.00008355999,0.00015312897,0.00017019804,0.0014429959,0.00009523365,0.00056747213,0.000026502885,0.0003860548],"category_scores_gemma":[0.00006545833,0.00005665343,0.0000563527,0.00047585793,0.0006803162,0.00015063235,0.0000024989604,0.00021529211,3.6430384e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000069962543,0.0000013033354,0.98048055,5.7574937e-7,0.00001604455,0.000026466667,0.00018615923,0.00010135296,0.000012328601,0.00012807138,0.0006279089,0.018412242],"study_design_scores_gemma":[0.000120700235,0.00016800525,0.99220294,0.000005219738,0.0000135894625,0.000079408586,0.00043937095,0.00004669635,0.000009372931,0.003227519,0.0036169325,0.00007025716],"about_ca_topic_score_codex":0.9804085,"about_ca_topic_score_gemma":0.9999017,"teacher_disagreement_score":0.022211934,"about_ca_system_score_codex":0.0000014837781,"about_ca_system_score_gemma":0.0039970907,"threshold_uncertainty_score":0.999857},"labels":[],"label_agreement":null},{"id":"W4311449851","doi":"10.1139/cjes-2022-0041","title":"The Lower Cretaceous sequence of western Alaska—demise of the Koyukuk terrane?","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Cretaceous; Terrane; Unconformity; Volcanic rock; Paleontology; Clastic rock; Sedimentary rock; Volcanic arc; Subduction; Volcano; Tectonics","score_opus":0.023425262103343412,"score_gpt":0.20177392483975823,"score_spread":0.1783486627364148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311449851","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9919711,0.0019450975,0.000002021513,0.0033628258,0.00036760943,0.000044187313,0.00006425252,0.000001072632,0.0022418657],"genre_scores_gemma":[0.99920475,0.000030117222,0.000054431668,0.00028737646,0.00003360908,1.9621923e-7,8.9459303e-7,7.0211274e-7,0.00038790324],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998529,0.0001478002,0.00037462238,0.00011767617,0.00052686804,0.00030400697],"domain_scores_gemma":[0.9988648,0.00024435128,0.00037088557,0.0001465851,0.000112671085,0.0002606726],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010802429,0.00007787533,0.0001842197,0.00008146564,0.00073680934,0.000045195407,0.0012058688,0.000021425296,0.004038295],"category_scores_gemma":[0.00023830688,0.00003655823,0.00017169997,0.00072382664,0.0012921822,0.00010785418,0.000025302546,0.00023518871,0.000005217967],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001015165,0.0000055344713,0.9860026,0.0000027230058,0.000014124551,0.000020208787,0.00016579428,0.01121197,0.00017477678,0.000022595063,0.00011396178,0.0022555233],"study_design_scores_gemma":[0.00016308989,0.00082203076,0.95418227,0.000031787673,0.00004769233,0.00026749363,0.0011101736,0.0016063544,0.00088898576,0.005784219,0.034944918,0.00015096168],"about_ca_topic_score_codex":0.0109829595,"about_ca_topic_score_gemma":0.20744935,"teacher_disagreement_score":0.19646639,"about_ca_system_score_codex":0.000001727563,"about_ca_system_score_gemma":0.0006925663,"threshold_uncertainty_score":0.9968721},"labels":[],"label_agreement":null},{"id":"W4311806039","doi":"10.1139/cjes-2022-0101","title":"A 500 ka record of volcanism and paleoenvironment in the northern Garibaldi Volcanic Belt, British Columbia","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Mafic; Geology; Felsic; Geochemistry; Volcanism; Volcanic belt; Basalt; Massif; Volcano; Volcanic rock; Earth science; Paleontology","score_opus":0.009933372983582614,"score_gpt":0.16132833526815402,"score_spread":0.1513949622845714,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311806039","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959463,0.0017233734,0.0000012191181,0.0007729695,0.00009416256,0.000056020705,0.00005667205,8.09898e-7,0.0013485051],"genre_scores_gemma":[0.99922067,0.00006671606,0.0001112122,0.00044830336,0.000027854558,5.274881e-7,0.0000037560872,7.1072736e-7,0.00012026944],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987483,0.00014255123,0.0003020844,0.00015109102,0.0003647253,0.00029126866],"domain_scores_gemma":[0.999373,0.000106355656,0.0001719758,0.000070717,0.000024740835,0.00025317972],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010424996,0.00005716238,0.00017883752,0.00007999929,0.00045451627,0.00013956723,0.00048579933,0.000019908306,0.010081387],"category_scores_gemma":[0.00007358607,0.00004975835,0.00006944433,0.0005058037,0.00050654897,0.000097059026,0.00001337602,0.00021994735,0.0000028037848],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000019028087,0.000007082401,0.9897114,0.0000018379199,0.0000056320305,0.00009505201,0.00018461737,0.0009882335,0.0000061659675,0.0000035309129,0.00011769738,0.008876857],"study_design_scores_gemma":[0.000104493796,0.00042318378,0.98963207,0.000008739017,0.000012182283,0.00020031628,0.0012942231,0.00040543385,0.000001367611,0.003923533,0.0039241803,0.00007027083],"about_ca_topic_score_codex":0.606049,"about_ca_topic_score_gemma":0.9957172,"teacher_disagreement_score":0.38966823,"about_ca_system_score_codex":0.0000023845257,"about_ca_system_score_gemma":0.00022343628,"threshold_uncertainty_score":0.9908235},"labels":[],"label_agreement":null},{"id":"W4312039327","doi":"10.1139/cjes-2022-0048","title":"Glacial microsedimentology—a new lens to investigate glacial sediments—a review","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Brock University","funders":"","keywords":"Glacial period; Geology; Sedimentology; Glacier; Sediment; Erosion; Geomorphology; Paleontology","score_opus":0.04681595992566764,"score_gpt":0.24455386690080635,"score_spread":0.1977379069751387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312039327","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86199796,0.058707982,0.000052347637,0.056713767,0.005786023,0.00053468195,0.00020058091,0.000015373134,0.015991272],"genre_scores_gemma":[0.89925414,0.0023815606,0.009099194,0.08248077,0.001974929,0.000004087015,0.000032981297,0.000012503168,0.0047598425],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984874,0.00008396867,0.00036960468,0.00018350488,0.0004136427,0.00046188373],"domain_scores_gemma":[0.9987567,0.00005787978,0.00019311601,0.00009012386,0.000071924915,0.0008302495],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008970361,0.00010996034,0.00023450506,0.00013928837,0.0013111588,0.00007980774,0.00055047846,0.000017767446,0.011354156],"category_scores_gemma":[0.00018505825,0.00009354686,0.00008780748,0.0010730352,0.00023872677,0.00025215704,0.000020469888,0.00019306931,0.00007068555],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011541188,0.0000057889447,0.78042483,0.000015088342,0.000028933184,0.000098494995,0.0008772696,0.004043868,0.000024387742,0.00017753754,0.20320657,0.011085708],"study_design_scores_gemma":[0.00014300099,0.0004132456,0.31976056,0.00005097153,0.000020281232,0.00009107001,0.000377307,0.000050965307,0.000008800558,0.00021013948,0.6787548,0.00011886928],"about_ca_topic_score_codex":0.029080523,"about_ca_topic_score_gemma":0.28124627,"teacher_disagreement_score":0.47554824,"about_ca_system_score_codex":0.0000071546,"about_ca_system_score_gemma":0.0026634538,"threshold_uncertainty_score":0.999989},"labels":[],"label_agreement":null},{"id":"W4312039392","doi":"10.1139/cjes-2022-0062","title":"Ontogeny of <i>Euphanerops longaevus</i> from the Upper Devonian Miguasha Fossil–Fish–Lagerstätte and comparison with the skeletogenesis of the sea lamprey <i>Petromyzon marinus</i>","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Canadian Museum of Nature; Université du Québec à Rimouski","funders":"","keywords":"Ontogeny; Petromyzon; Devonian; Lamprey; Biology; Vertebrate; Paleontology; Extant taxon; Larva; Fish <Actinopterygii>; Zoology; Taphonomy; Lagerstätte; Anatomy; Evolutionary biology; Ecology; Fishery","score_opus":0.014115495027014938,"score_gpt":0.19256511087061767,"score_spread":0.17844961584360275,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312039392","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98600817,0.0060535516,0.000009878714,0.0059027434,0.00050996477,0.00011192056,0.0003594546,0.0000017267258,0.0010426056],"genre_scores_gemma":[0.9988123,0.000033539083,0.00015265391,0.0008337617,0.00008266159,7.638472e-7,0.0000055532073,0.0000018713207,0.000076875804],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982932,0.0004473558,0.00034015672,0.00018455404,0.0003756394,0.00035905177],"domain_scores_gemma":[0.998522,0.000525023,0.0004519991,0.0002076004,0.0001020213,0.0001913882],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0012199631,0.00012631119,0.00026238235,0.00008613364,0.001411509,0.00003600852,0.001075456,0.000046804285,0.0007623396],"category_scores_gemma":[0.00007652811,0.000058596044,0.000093582246,0.00051686086,0.0023210887,0.00015039228,0.000029072498,0.0003228284,0.0000016248229],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043182914,0.0000057008797,0.99452937,0.0000026569771,0.000041312844,0.000010132502,0.0007176238,0.0019851516,0.000058118134,0.000030857962,0.0013746326,0.0012012769],"study_design_scores_gemma":[0.00019500288,0.00040954485,0.98035556,0.000016036993,0.00004189915,0.00017313023,0.0019305084,0.00029087186,0.00016215109,0.00012138164,0.016221445,0.00008244167],"about_ca_topic_score_codex":0.049512643,"about_ca_topic_score_gemma":0.78496224,"teacher_disagreement_score":0.7354496,"about_ca_system_score_codex":0.0000040603395,"about_ca_system_score_gemma":0.0010937242,"threshold_uncertainty_score":0.99988854},"labels":[],"label_agreement":null},{"id":"W4312105899","doi":"10.1139/cjes-2022-0060","title":"The Ediacaran–Cambrian Chapel Island Formation of Newfoundland, Canada: evaluating the impact of outcrop quality on trace-fossil data sets at the Cambrian GSSP and less-explored sections","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University; University of Saskatchewan","funders":"","keywords":"Geology; Outcrop; Paleontology; Trace fossil; Bioturbation; Burrow; Sedimentary rock; Cove; Global Boundary Stratotype Section and Point; Sedimentary structures; Sedimentary depositional environment; Sediment; Biostratigraphy; Geomorphology; Structural basin","score_opus":0.12227110547738282,"score_gpt":0.3187675440552307,"score_spread":0.1964964385778479,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312105899","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99295884,0.002236051,0.000008067418,0.002446757,0.0003482594,0.0001367112,0.00082685804,0.0000011077827,0.0010373513],"genre_scores_gemma":[0.9996977,0.00006430998,0.00001874695,0.000064314765,0.00004980745,7.9906766e-7,0.000018065937,0.0000010827091,0.00008519315],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982221,0.00035471824,0.00046078718,0.00011551074,0.0005724195,0.0002744734],"domain_scores_gemma":[0.99815536,0.0007441576,0.0005487446,0.00022474519,0.00014412975,0.0001828449],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0038513413,0.000091955226,0.00016108285,0.000086548345,0.0030724793,0.00014527736,0.0007724768,0.000020065134,0.0002883774],"category_scores_gemma":[0.00048333744,0.00004007578,0.000054410648,0.0004894924,0.0005511751,0.00042898033,0.000029504781,0.00022140177,9.1948715e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007596187,0.000006440127,0.9187714,0.000013776143,0.00003456364,0.0000029964363,0.0021988105,0.057094403,0.00001461402,0.0001625683,0.0007694666,0.020855017],"study_design_scores_gemma":[0.00017363444,0.0005954318,0.9726086,0.000012020043,0.000016437843,0.000115951036,0.0062867133,0.017026322,0.0000068534555,0.00022283355,0.0028687927,0.00006640994],"about_ca_topic_score_codex":0.8300247,"about_ca_topic_score_gemma":0.9980783,"teacher_disagreement_score":0.16805355,"about_ca_system_score_codex":0.000014409324,"about_ca_system_score_gemma":0.002746378,"threshold_uncertainty_score":0.9982254},"labels":[],"label_agreement":null},{"id":"W4313855376","doi":"10.1139/cjes-2022-0074","title":"An experimental baseline for ice-till strain indicators","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Brock University","funders":"","keywords":"Geology; Anisotropy; Kinematics; Ice stream; Shear (geology); Traction (geology); Sea ice; Geometry; Geomorphology; Petrology; Optics; Mathematics; Physics","score_opus":0.04303795560833272,"score_gpt":0.266971412201226,"score_spread":0.22393345659289327,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313855376","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965559,0.0008370596,0.00008990879,0.00082483445,0.0007752546,0.00008749794,0.0001927552,0.000008884491,0.00062788744],"genre_scores_gemma":[0.99724114,0.000021248443,0.002003795,0.00036241824,0.0002477,4.9470316e-7,0.000018518305,0.0000018397085,0.00010286937],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99907696,0.000029339722,0.0002186532,0.00012555563,0.00020031634,0.00034920176],"domain_scores_gemma":[0.99911803,0.00013354236,0.00011195558,0.00006430535,0.00005535156,0.000516811],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000988216,0.000072217124,0.00011668588,0.00022350746,0.0006470552,0.00011721293,0.0003179482,0.000025838204,0.0014194809],"category_scores_gemma":[0.00012377731,0.00005545632,0.00005928871,0.00088900886,0.0002637684,0.00033130316,0.0000020768757,0.00005973719,0.000023847928],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008740363,0.000008379694,0.9617263,0.0000040132763,0.000015674335,0.00004001178,0.0014133687,0.010937532,0.00012824299,0.00036982755,0.0038577167,0.021490166],"study_design_scores_gemma":[0.00018451165,0.000620647,0.9109224,0.000011848766,0.000006617879,0.000014536707,0.006138223,0.0077975495,0.00010290211,0.00022399092,0.07386187,0.0001148943],"about_ca_topic_score_codex":0.004379784,"about_ca_topic_score_gemma":0.23833923,"teacher_disagreement_score":0.23395944,"about_ca_system_score_codex":0.0000015167883,"about_ca_system_score_gemma":0.00071084267,"threshold_uncertainty_score":0.99949336},"labels":[],"label_agreement":null},{"id":"W4313888564","doi":"10.1139/cjes-2022-0100","title":"Precise U–Pb zircon dates from silicic super-eruptions during late Ediacaran extension in the Avalonian Caledonia terrane of southern New Brunswick, Canada","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University","funders":"Natural Sciences and Engineering Research Council of Canada; Acadia University; U.S. Department of Energy","keywords":"Zircon; Geology; Felsic; Pluton; Silicic; Geochemistry; Rhyolite; Geochronology; Terrane; Volcanic rock; Mafic; Basalt; Volcano; Paleontology","score_opus":0.02061389714998362,"score_gpt":0.19680649142174636,"score_spread":0.17619259427176273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313888564","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99508667,0.0008045397,0.0000025431525,0.0034505804,0.00019576093,0.00005883128,0.000121563,0.0000037601676,0.00027577003],"genre_scores_gemma":[0.9992597,0.0000539766,0.00017723748,0.00016325148,0.0001246342,9.281983e-8,0.000019644394,0.0000014864501,0.0001999677],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99839425,0.00010973446,0.00040918222,0.00020378553,0.00043589564,0.00044718108],"domain_scores_gemma":[0.99889636,0.00026484553,0.00014515717,0.00013841582,0.000065440676,0.0004897592],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006128998,0.00011946744,0.00025880817,0.00025875782,0.0002841364,0.000072043986,0.0006137445,0.00004891719,0.0026953467],"category_scores_gemma":[0.00021253433,0.00007062286,0.00009537857,0.0011413664,0.0003053931,0.00016211996,0.000008675937,0.00022206576,0.000053202963],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008814845,0.0000035411344,0.98285764,0.0000040054347,0.000011656553,0.00013601963,0.0009082506,0.012744468,0.0019988394,0.0000030046967,0.00014223266,0.0011815282],"study_design_scores_gemma":[0.00016426278,0.000064739295,0.99418586,0.00005315745,0.00002176785,0.00002013534,0.001358014,0.0017415284,0.00076786,0.0010134142,0.0005043156,0.000104932],"about_ca_topic_score_codex":0.9867813,"about_ca_topic_score_gemma":0.99972415,"teacher_disagreement_score":0.012942868,"about_ca_system_score_codex":0.0000031648528,"about_ca_system_score_gemma":0.002652692,"threshold_uncertainty_score":0.99821633},"labels":[],"label_agreement":null},{"id":"W4315433434","doi":"10.1139/cjes-2022-0050","title":"Late Paleoarchean to Neoarchean sedimentation on the Singhbhum Craton, eastern India: a synthesis","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Craton; Sedimentary depositional environment; Geochemistry; Continental margin; Sedimentary rock; Archean; Banded iron formation; Facies; Paleontology; Structural basin","score_opus":0.05290747236251966,"score_gpt":0.26714688561091954,"score_spread":0.21423941324839987,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4315433434","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97401017,0.00008920561,0.0000042580073,0.020029176,0.00042760014,0.00011388129,0.000016884771,0.000007653424,0.0053011463],"genre_scores_gemma":[0.99826217,0.00001202083,0.00009890208,0.0012693709,0.00009696395,9.896545e-7,0.0000024782316,0.0000019988022,0.00025508477],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982556,0.00032007,0.00024141766,0.00017835434,0.00037005675,0.0006344658],"domain_scores_gemma":[0.9980689,0.0009980019,0.00010010668,0.00011842823,0.00008113772,0.00063338946],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0024115045,0.000101731624,0.00015401242,0.00069269096,0.0008835466,0.00014806092,0.00060333434,0.00006212077,0.0014381065],"category_scores_gemma":[0.0006035657,0.00006405297,0.00006061759,0.0011364211,0.00075544376,0.00017349473,0.000007841626,0.00030415293,0.0013881633],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012388316,0.0000017342171,0.9948866,0.0000030394406,0.000010609907,0.00013874071,0.0008178979,0.0018096201,0.000006773402,0.00012719778,0.00035214276,0.00183325],"study_design_scores_gemma":[0.000071472445,0.00037212615,0.99429226,0.00004686646,0.0000061287733,0.000069342175,0.0016352083,0.0011493798,0.00020946313,0.0009948008,0.0010651888,0.00008778367],"about_ca_topic_score_codex":0.0022825135,"about_ca_topic_score_gemma":0.31111485,"teacher_disagreement_score":0.30883235,"about_ca_system_score_codex":7.320614e-7,"about_ca_system_score_gemma":0.0009313285,"threshold_uncertainty_score":0.9994747},"labels":[],"label_agreement":null},{"id":"W4315472573","doi":"10.1139/cjes-2022-0103","title":"U-Pb zircon ages from metasedimentary and plutonic rocks in the Bras d'Or terrane of Cape Breton Island, Nova Scotia, Canada: insights into the Ediacaran–Cambrian tectonomagmatic evolution of Ganderia","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Nova Scotia Department of Energy; Acadia University","funders":"Natural Sciences and Engineering Research Council of Canada; Nova Scotia Department of Energy and Mines; Nova Scotia Department of Energy; Cape Breton University; U.S. Department of Energy","keywords":"Terrane; Zircon; Geology; Metamorphism; Geochemistry; Gondwana; Pluton; Metamorphic rock; Geochronology; Paleontology; Structural basin","score_opus":0.014218928055590017,"score_gpt":0.19250999171962688,"score_spread":0.17829106366403685,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4315472573","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932922,0.003894752,0.000009576667,0.002211956,0.00021678007,0.0000868649,0.000048454276,0.0000013234305,0.00023805982],"genre_scores_gemma":[0.9995408,0.00007092875,0.00008937711,0.00020442027,0.00006172772,2.1224523e-7,0.000015232232,9.951734e-7,0.000016326012],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99856275,0.00015887505,0.0004453953,0.0001597188,0.000396016,0.00027723104],"domain_scores_gemma":[0.9988944,0.0004926598,0.00024722685,0.00011163968,0.0000559343,0.00019817388],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007654877,0.00011222686,0.00029796697,0.0002504297,0.00018796086,0.00004519683,0.0004961426,0.00004164062,0.0013246982],"category_scores_gemma":[0.0001647837,0.000052275278,0.00006742022,0.0010685588,0.00059843936,0.00017877248,0.000010199994,0.00017388727,0.0000043692944],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028365252,0.000007145653,0.9897764,0.000020557469,0.000060476203,0.00007458882,0.0021808555,0.004482648,0.0014334266,0.000018156981,0.00028610093,0.0016313151],"study_design_scores_gemma":[0.00021891369,0.00021406698,0.99009234,0.00006169986,0.000057666362,0.000021855258,0.0030607365,0.0024342362,0.0011244281,0.002389206,0.00023406508,0.00009077359],"about_ca_topic_score_codex":0.9800051,"about_ca_topic_score_gemma":0.999683,"teacher_disagreement_score":0.019677946,"about_ca_system_score_codex":0.000006227398,"about_ca_system_score_gemma":0.0012699218,"threshold_uncertainty_score":0.99958825},"labels":[],"label_agreement":null},{"id":"W4317774201","doi":"10.1139/cjes-2022-0080","title":"Geomorphic diversity of the Newfoundland and Labrador Shelves Bioregion","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada","funders":"","keywords":"Geology; Continental shelf; Oceanography; Bedrock; Channelized; Current (fluid); Structural basin; Trough (economics); Continental margin; Submarine pipeline; Geomorphology; Paleontology; Tectonics","score_opus":0.03252787380962732,"score_gpt":0.19971372974271714,"score_spread":0.16718585593308982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4317774201","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964016,0.000464412,0.0000032421008,0.0017184379,0.0002349972,0.000026569318,0.000020171286,0.0000020171901,0.0011285262],"genre_scores_gemma":[0.9996158,0.000082563565,0.000066684166,0.000100015495,0.000024278606,1.6159277e-8,8.0680775e-7,2.7789184e-7,0.00010953985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995085,0.000028871025,0.00011798754,0.00005381858,0.0001384957,0.00015234653],"domain_scores_gemma":[0.9995491,0.000078112884,0.00010283733,0.000039731734,0.000058376892,0.00017183353],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047921692,0.000039340714,0.00007561426,0.00014770245,0.0006520101,0.000056897585,0.00027259788,0.000022137425,0.0004270314],"category_scores_gemma":[0.000101101075,0.000021030517,0.000028975148,0.0006402167,0.0005999348,0.00026027046,0.0000136090175,0.000061449595,0.000012513751],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001274026,4.5588322e-7,0.99657434,0.000005695369,0.0000021433355,0.0000041698704,0.00027099592,0.0006297608,0.0000018969556,0.00014270138,0.00011356069,0.0022529946],"study_design_scores_gemma":[0.000053881366,0.0000951572,0.99368346,0.000018755514,0.000004246567,0.00003975974,0.00039933276,0.0004288253,0.000010542536,0.0026895036,0.0025449754,0.000031554187],"about_ca_topic_score_codex":0.033100884,"about_ca_topic_score_gemma":0.5282349,"teacher_disagreement_score":0.495134,"about_ca_system_score_codex":3.98583e-7,"about_ca_system_score_gemma":0.0002789085,"threshold_uncertainty_score":0.97333777},"labels":[],"label_agreement":null},{"id":"W4318773774","doi":"10.1139/cjes-2022-0093","title":"SHRIMP U–Pb geochronology of Mesoproterozoic basement and overlying Ocoee Supergroup, NC–TN: dating diagenetic xenotime and monazite overgrowths on detrital minerals to determine the age of sedimentary deposition","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Monazite; Diagenesis; Geochemistry; Zircon; Geochronology; Metamorphism; Sedimentary rock; Proterozoic; Basement; Supergroup; Precambrian; Paleontology; Laurentia; Provenance; Paleozoic; Archaeology; Tectonics","score_opus":0.022916015508310357,"score_gpt":0.21407946684313636,"score_spread":0.191163451334826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4318773774","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977207,0.0008844234,0.000019065079,0.0009474319,0.000069233276,0.00008746118,0.000055813343,0.0000021520682,0.0002136856],"genre_scores_gemma":[0.99858016,0.000051274565,0.00090885226,0.00038169982,0.000043479355,6.013791e-7,0.000013104946,0.0000012465078,0.00001959653],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988294,0.00007822701,0.00034755075,0.00018354824,0.00025972363,0.00030153137],"domain_scores_gemma":[0.99915576,0.00029246026,0.00014439641,0.000078038676,0.000045069766,0.00028427],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006011693,0.00010498953,0.00023327213,0.0003013812,0.00021309021,0.000047779165,0.00021872156,0.00003519785,0.00058226334],"category_scores_gemma":[0.00014930396,0.0000654497,0.00005600429,0.0005487602,0.00040881662,0.00014095215,0.000021571543,0.00009535593,0.0000044109333],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020455478,0.000008213558,0.9501726,0.000023875991,0.000035326593,0.000110903464,0.00032512154,0.0033839543,0.027767329,0.00002158124,0.000047114172,0.01808355],"study_design_scores_gemma":[0.00018324719,0.0011645744,0.98616844,0.00007216167,0.000033378008,0.00005032271,0.00025702835,0.003252847,0.00793905,0.0006421258,0.00013902533,0.000097777214],"about_ca_topic_score_codex":0.026705224,"about_ca_topic_score_gemma":0.0781205,"teacher_disagreement_score":0.05141528,"about_ca_system_score_codex":0.0000018847941,"about_ca_system_score_gemma":0.00008501731,"threshold_uncertainty_score":0.979776},"labels":[],"label_agreement":null},{"id":"W4319296481","doi":"10.1139/cjes-2022-0049","title":"Cratonal tidal deposits of the Paleoproterozoic Mesnard Quartzite, Lake Superior region: interpretation challenges","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Arenite; Bedding; Trough (economics); Ripple marks; Structural basin; Graded bedding; Geochemistry; Geomorphology; Deposition (geology); Paleontology; Clastic rock; Ripple","score_opus":0.03431751729559611,"score_gpt":0.21800317229367042,"score_spread":0.18368565499807432,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319296481","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.990866,0.0016470102,0.000020712801,0.0031307244,0.0004930416,0.00006894794,0.000015902362,0.000005296629,0.0037523417],"genre_scores_gemma":[0.9994697,0.00013247086,0.00013266476,0.00011544751,0.00005782739,3.2119598e-7,0.000002265079,8.9344087e-7,0.00008841496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99901944,0.00007742286,0.0002847265,0.00009577592,0.00028082976,0.00024178371],"domain_scores_gemma":[0.99929196,0.00010594942,0.00017899834,0.0000757557,0.00013786589,0.00020950247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056237355,0.000073525116,0.0001298264,0.0002146478,0.000364325,0.00008467687,0.00043402516,0.00004240389,0.0004602234],"category_scores_gemma":[0.00016797542,0.000041980056,0.00007532628,0.00070662756,0.00041227555,0.0004167625,0.0000055017963,0.00011619145,0.000034147244],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008699021,0.0000023552066,0.97336286,0.000027313126,0.000009311009,0.00002455889,0.001478253,0.0038804256,0.000007272003,0.000276058,0.0001330649,0.020789817],"study_design_scores_gemma":[0.00006595317,0.00027487965,0.9920581,0.00007795009,0.0000061021738,0.00015632858,0.00096423324,0.0010091646,0.000092154216,0.0011966999,0.004035286,0.0000631371],"about_ca_topic_score_codex":0.0007215143,"about_ca_topic_score_gemma":0.5550808,"teacher_disagreement_score":0.55435926,"about_ca_system_score_codex":5.919218e-7,"about_ca_system_score_gemma":0.0005752012,"threshold_uncertainty_score":0.5039124},"labels":[],"label_agreement":null},{"id":"W4319457681","doi":"10.1139/cjes-2022-0059","title":"Detrital zircon geochronology and provenance of the Mesoproterozoic Husky Creek Formation: a fluvial sandstone recording the waning stages of one of Earth's largest magmatic episodes","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Laurentian University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Agouron Institute","keywords":"Geology; Zircon; Large igneous province; Provenance; Geochemistry; Flood basalt; Basalt; Geochronology; Igneous rock; Fluvial; Sedimentary rock; Mafic; Detritus; Volcanic rock; Volcano; Structural basin; Paleontology; Magmatism; Volcanism; Tectonics","score_opus":0.021576624905115395,"score_gpt":0.20276918546957376,"score_spread":0.18119256056445837,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319457681","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99644864,0.0012240818,0.000042915923,0.0016817445,0.00010205964,0.000094698364,0.000040354553,0.000002142734,0.00036339008],"genre_scores_gemma":[0.9989657,0.00007659882,0.0008341141,0.0000423876,0.000034420744,3.82866e-7,0.0000018423923,9.07525e-7,0.00004364984],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987609,0.000109816705,0.0004596739,0.00011033634,0.00028177293,0.0002775397],"domain_scores_gemma":[0.9988727,0.00029098673,0.00047779776,0.000098364006,0.00012515986,0.0001350042],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011022763,0.00007785358,0.00027897194,0.00017099237,0.00030057275,0.000040937633,0.00040114092,0.00004069116,0.0006666068],"category_scores_gemma":[0.00048410054,0.000043072985,0.00009468857,0.00087740365,0.0010891177,0.000265733,0.000020062686,0.00014969536,0.0000030394453],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011273131,0.0000069597604,0.9845722,0.0000719795,0.000030555468,0.0000073701367,0.0006216138,0.0014837056,0.0055554095,0.00014245149,0.000027641034,0.0074688722],"study_design_scores_gemma":[0.00021670452,0.00049550866,0.9712621,0.00018832876,0.00003938202,0.000054368782,0.001173227,0.0021932428,0.017647486,0.0064979685,0.00014459778,0.00008706865],"about_ca_topic_score_codex":0.016903412,"about_ca_topic_score_gemma":0.2654789,"teacher_disagreement_score":0.24857551,"about_ca_system_score_codex":8.8525826e-7,"about_ca_system_score_gemma":0.00024364468,"threshold_uncertainty_score":0.9896431},"labels":[],"label_agreement":null},{"id":"W4320895070","doi":"10.1139/cjes-2022-0137","title":"Tectonic geomorphology of the Ottawa-Bonnechere Graben, Eastern Canada: implications for regional uplift and intraplate seismicity","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada; McMaster University","keywords":"Geology; Intraplate earthquake; Graben; Seismology; Tectonics; Induced seismicity; Seismic hazard; Tectonic uplift; Bedrock; Geomorphology; Post-glacial rebound; Escarpment; Structural basin; Half-graben; Glacial period","score_opus":0.040478294260731566,"score_gpt":0.23109273323384882,"score_spread":0.19061443897311725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4320895070","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98616254,0.0014804619,0.000016083784,0.011182178,0.0003735404,0.00011241845,0.00023615001,0.0000029655093,0.0004336806],"genre_scores_gemma":[0.9990763,0.00007611259,0.00013110814,0.00053884205,0.000054715252,5.8155683e-7,0.000004239912,0.0000016908033,0.000116385985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990399,0.000041882737,0.00027101536,0.00014022364,0.00015456491,0.0003524149],"domain_scores_gemma":[0.99899226,0.00032802133,0.00021736116,0.00010079734,0.00012893564,0.00023259163],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00063131645,0.00008507818,0.00017651284,0.0001488609,0.00058244966,0.000033630073,0.0003700291,0.000038374677,0.00013835209],"category_scores_gemma":[0.00017698114,0.000055382345,0.000060051534,0.00056904496,0.00063152023,0.00010037524,0.000008221142,0.00012199143,0.0000023440998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000031646593,0.0000011074419,0.9898532,0.000008243774,0.000022201893,0.000005709808,0.0001230261,0.0008835572,0.000018710381,0.00044373085,0.003121733,0.005515583],"study_design_scores_gemma":[0.00014046526,0.00011946598,0.97595674,0.000024860516,0.000013231718,0.00012853075,0.00030299998,0.0006074375,0.00005087682,0.0018618526,0.020725057,0.000068487585],"about_ca_topic_score_codex":0.63957614,"about_ca_topic_score_gemma":0.995929,"teacher_disagreement_score":0.35635287,"about_ca_system_score_codex":0.0000027970314,"about_ca_system_score_gemma":0.0029386466,"threshold_uncertainty_score":0.5213033},"labels":[],"label_agreement":null},{"id":"W4321453118","doi":"10.1139/cjes-2022-0131","title":"Celebrating dinosaurs: their behaviour, evolution, growth, and physiology","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Biology; Publication; Scope (computer science); Zoology; Ecology; Evolutionary biology; History; Political science; Computer science","score_opus":0.01908619128665314,"score_gpt":0.20940593300733273,"score_spread":0.19031974172067959,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321453118","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99368817,0.0019877218,0.0000141907485,0.0014873354,0.00073925575,0.000034141278,0.000036079742,0.00000961275,0.0020035258],"genre_scores_gemma":[0.9993527,0.00006400024,0.00022384478,0.0001618465,0.00015586625,1.6198855e-7,0.000007261491,9.1674184e-7,0.000033381068],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989894,0.000115312105,0.0002134945,0.00015912292,0.00008882782,0.00043381247],"domain_scores_gemma":[0.9992189,0.00018591712,0.00012652726,0.000051452043,0.00006215582,0.00035505055],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00062760996,0.00008659271,0.00015523503,0.00036647482,0.0006739792,0.000034126635,0.00026565918,0.000078918645,0.00035072968],"category_scores_gemma":[0.00018717482,0.00006230391,0.00004142534,0.0005245319,0.0011204388,0.00031865598,0.000004828844,0.00015593987,0.000047296162],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000033784108,9.761686e-7,0.99779487,0.000002289603,0.0000058068013,0.000026792468,0.00015879824,0.00022006175,0.00016945084,0.0005992147,0.00018197359,0.0008363673],"study_design_scores_gemma":[0.00008282269,0.0002236254,0.99297297,0.000010366092,0.0000049407054,0.00029115795,0.0005615952,0.00090080395,0.00002949551,0.00435657,0.00048827447,0.00007735492],"about_ca_topic_score_codex":0.007741395,"about_ca_topic_score_gemma":0.26660115,"teacher_disagreement_score":0.25885972,"about_ca_system_score_codex":0.000001022227,"about_ca_system_score_gemma":0.0005940292,"threshold_uncertainty_score":0.99886614},"labels":[],"label_agreement":null},{"id":"W4321614425","doi":"10.1139/cjes-2022-0055","title":"Mesoproterozoic basins (Yukon, Canada) in the evolution of supercontinent Columbia","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Laurentian University; Simon Fraser University","funders":"","keywords":"Zircon; Supercontinent; Laurentia; Geology; Provenance; Rodinia; Geochemistry; Population; Paleontology; Stromatolite; Craton; Paleozoic; Carbonate; Tectonics","score_opus":0.014217526636109647,"score_gpt":0.17925367077317703,"score_spread":0.16503614413706738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321614425","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993377,0.00041813793,0.000002729507,0.0036651185,0.00015814441,0.000051535782,0.00003723765,0.0000014358502,0.002288691],"genre_scores_gemma":[0.99958205,0.000010511005,0.000060115093,0.00021493793,0.000043730553,2.0320087e-7,0.0000030056992,4.5812183e-7,0.00008501457],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987501,0.0000932667,0.0003013478,0.000105911124,0.0004215597,0.00032783768],"domain_scores_gemma":[0.99936676,0.00013912511,0.00010643098,0.000071604,0.00008584736,0.00023024122],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011767169,0.00005692238,0.00015858402,0.00019005126,0.0001934321,0.000062350795,0.0004911779,0.00002712671,0.0020390367],"category_scores_gemma":[0.0002619148,0.00003678514,0.00006209221,0.0015495952,0.00031452367,0.00012835264,0.0000036585218,0.00012990992,0.000010848116],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000001384884,0.0000018784164,0.99622005,0.0000027390886,0.0000036310093,0.000051745857,0.00009544211,0.0021872227,0.000020887288,0.000038715345,0.00079795514,0.0005783397],"study_design_scores_gemma":[0.000063595675,0.00010062354,0.9918188,0.00001538005,0.0000066236294,0.000023231689,0.0012265256,0.0013912895,0.000024573097,0.0028176822,0.0024611128,0.000050575956],"about_ca_topic_score_codex":0.9798744,"about_ca_topic_score_gemma":0.9999095,"teacher_disagreement_score":0.02003519,"about_ca_system_score_codex":0.0000042147985,"about_ca_system_score_gemma":0.0018035369,"threshold_uncertainty_score":0.99887323},"labels":[],"label_agreement":null},{"id":"W4322623464","doi":"10.1139/cjes-2022-0113","title":"Mapping and analysis of structural lineaments using SRTM radar data and Landsat-8 OLI image: an example from the Telouet–Tighza area, Marrakech High Atlas, Morocco","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies Worldwide","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Shuttle Radar Topography Mission; Lineament; Geology; Remote sensing; Digital elevation model; Tectonics; Geologic map; Geomorphology; Seismology","score_opus":0.07613973612952696,"score_gpt":0.24495427166548764,"score_spread":0.16881453553596068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322623464","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976528,0.00092375884,0.000018735549,0.00067859684,0.00015975969,0.00004960221,0.00043314812,0.0000036628924,0.00007988917],"genre_scores_gemma":[0.9977531,0.000062978215,0.0018158203,0.00014307325,0.00010701922,5.4447906e-8,0.00008635099,0.0000011256687,0.000030464782],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873346,0.00007967947,0.00028990244,0.00026974577,0.0002857052,0.00034152117],"domain_scores_gemma":[0.9988481,0.0003464055,0.00019462971,0.00017450681,0.000064532534,0.00037185647],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00062570226,0.00011404722,0.0003158918,0.00021836758,0.0006365218,0.00018349384,0.00056805415,0.000029371213,0.0006024101],"category_scores_gemma":[0.00010113064,0.00006357871,0.000041849016,0.0013846557,0.00072880444,0.00041302224,0.00005275045,0.00013219837,0.0000029041673],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000055321616,0.0000011946717,0.9911001,0.0000021182664,0.00010109039,0.000025331208,0.000499516,0.00084797177,0.00004235124,0.0000058561345,0.00009358153,0.0072754105],"study_design_scores_gemma":[0.00012669417,0.00007897,0.9614454,0.00001629357,0.00009051555,0.000008045791,0.0013129974,0.035210732,0.000008953236,0.0007064376,0.00090629817,0.00008864817],"about_ca_topic_score_codex":0.28945556,"about_ca_topic_score_gemma":0.4630578,"teacher_disagreement_score":0.17360221,"about_ca_system_score_codex":0.0000011457516,"about_ca_system_score_gemma":0.00014628674,"threshold_uncertainty_score":0.715276},"labels":[],"label_agreement":null},{"id":"W4322768538","doi":"10.1139/cjes-2022-0067","title":"Mount Garibaldi: hazard potential from a long-dormant volcanic system in the Pacific Northwest","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"University of British Columbia; Simon Fraser University","keywords":"Lahar; Geology; Tephra; Volcanic hazards; Pyroclastic rock; Volcano; Explosive eruption; Lava; Earth science; Population; Stratovolcano; Physical geography; Geochemistry; Geography","score_opus":0.02101421615633575,"score_gpt":0.222827419006621,"score_spread":0.20181320285028526,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322768538","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939845,0.0009896278,0.000007776935,0.0016932815,0.0009270053,0.00009765727,0.000067527086,0.0000072361313,0.00222539],"genre_scores_gemma":[0.99958086,0.000046664107,0.000035440033,0.000115302166,0.00013772634,5.2665115e-7,0.000023334258,0.0000014802051,0.000058649188],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99802834,0.0003104406,0.00034577263,0.00019481507,0.00042922606,0.0006914198],"domain_scores_gemma":[0.9989914,0.00027334483,0.00013438214,0.00014852344,0.000074407726,0.00037800142],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023419245,0.00011060818,0.00021266745,0.00056953676,0.0006316037,0.00019476042,0.0009093936,0.000088787514,0.00070011016],"category_scores_gemma":[0.00008801933,0.00006916892,0.00007960052,0.0011213322,0.0007486409,0.00027128196,0.00000701881,0.00040196598,0.00055334263],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008947506,0.0000020243713,0.99396354,0.0000055924993,0.000009395296,0.0020114167,0.0005213867,0.0030793305,0.0000011224283,0.000080229496,0.00013027649,0.0001867506],"study_design_scores_gemma":[0.00016500769,0.00015590918,0.9889637,0.00003967655,0.00000900483,0.0007356432,0.003856576,0.0048380867,0.0000027088067,0.00018972335,0.0009604287,0.00008349965],"about_ca_topic_score_codex":0.047289394,"about_ca_topic_score_gemma":0.9536732,"teacher_disagreement_score":0.9063838,"about_ca_system_score_codex":0.0000016539436,"about_ca_system_score_gemma":0.001415594,"threshold_uncertainty_score":0.95905477},"labels":[],"label_agreement":null},{"id":"W4323539234","doi":"10.1139/cjes-2023-0009","title":"U–Pb geochronology: its development and importance in Canada","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geochronology; Zircon; Geology; Thermal ionization mass spectrometry; Isotope dilution; Earth science; Earth history; Geochemistry; Mass spectrometry; Paleontology; Ionization; Ion; Chemistry","score_opus":0.020579408055400553,"score_gpt":0.1839448845719254,"score_spread":0.16336547651652483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323539234","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99513423,0.0014302486,6.4440184e-7,0.0016443502,0.00012608792,0.000021142981,0.0000075950065,0.0000019362963,0.0016337889],"genre_scores_gemma":[0.99924827,0.000042176278,0.00031010344,0.00030797257,0.000023034581,1.0542218e-7,0.0000028328932,4.439667e-7,0.00006504023],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990288,0.000023316334,0.0002499575,0.00013026239,0.00018029645,0.00038734486],"domain_scores_gemma":[0.999321,0.00008062003,0.000083394785,0.000034429122,0.000038411858,0.00044217083],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047117684,0.000066545734,0.00014970973,0.0002237005,0.00016316283,0.000033715565,0.00022483784,0.000023356333,0.002322368],"category_scores_gemma":[0.00013641008,0.000046136272,0.000018412755,0.00079884485,0.00015584235,0.00012315174,0.000005286778,0.000111666675,0.00003611729],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000010155976,4.0973407e-7,0.99328727,0.0000020937348,0.0000034589461,0.00021593961,0.000052508127,0.0014540406,0.000007912934,0.000020797966,0.00009756601,0.004856992],"study_design_scores_gemma":[0.0000616544,0.000030043468,0.9921204,0.000010569116,0.0000020563107,0.00003662222,0.0003279646,0.001218206,0.00015340203,0.0008460301,0.00512237,0.000070701906],"about_ca_topic_score_codex":0.8982841,"about_ca_topic_score_gemma":0.9998969,"teacher_disagreement_score":0.10161281,"about_ca_system_score_codex":0.000004774871,"about_ca_system_score_gemma":0.0039725555,"threshold_uncertainty_score":0.99858963},"labels":[],"label_agreement":null},{"id":"W4324141264","doi":"10.1139/cjes-2022-0097","title":"Petrogenesis and geodynamic significance of late Early Jurassic complex in Qinsai, Hainan Island, South China Sea","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Gabbro; Quartz monzonite; Geology; Zircon; Diorite; Geochemistry; Petrogenesis; Subduction; Peridotite; Petrology; Geochronology; Igneous rock; Mantle (geology); Tectonics; Pluton; Paleontology","score_opus":0.01853327058695653,"score_gpt":0.19559812375511493,"score_spread":0.1770648531681584,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4324141264","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976921,0.00041131163,0.0000052689784,0.0008607311,0.00007634868,0.000044116012,0.00012486879,0.0000037246837,0.0007815062],"genre_scores_gemma":[0.9996184,0.000038283753,0.00014955789,0.000050003226,0.00002888382,1.6703075e-7,0.0000074779596,0.0000011493919,0.00010605717],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998733,0.00007024101,0.00033164435,0.00018766471,0.000257287,0.00042019077],"domain_scores_gemma":[0.99917984,0.00009606482,0.00018179203,0.00006989067,0.000053441312,0.0004189797],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00060734496,0.000103363855,0.00027646607,0.0004639266,0.00018824197,0.00006665006,0.00032695648,0.000041189745,0.0013325304],"category_scores_gemma":[0.000112931215,0.000071310584,0.000080845166,0.0013962585,0.0006164638,0.00016525864,0.000007876632,0.00013211854,0.000023436363],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057119223,0.0000021608857,0.9925142,0.0000069493253,0.000007742494,0.00007418771,0.00024684082,0.005191809,0.00009914635,0.000019507046,0.000016708613,0.0018150382],"study_design_scores_gemma":[0.00012751514,0.00018092238,0.983201,0.000021485088,0.00001039195,0.000016382597,0.00021364687,0.013435819,0.000043431926,0.002544453,0.000110662804,0.00009427593],"about_ca_topic_score_codex":0.061035313,"about_ca_topic_score_gemma":0.59861475,"teacher_disagreement_score":0.5375795,"about_ca_system_score_codex":0.0000013582076,"about_ca_system_score_gemma":0.00028635788,"threshold_uncertainty_score":0.9995804},"labels":[],"label_agreement":null},{"id":"W4327713533","doi":"10.1139/cjes-2022-0132","title":"Late Triassic granites with mafic microenclaves in the East Kunlun Orogenic Belt, northwestern China: petrogenesis and implications for continental crust evolution and geodynamic evolution","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Mafic; Zircon; Geochemistry; Partial melting; Continental crust; Adakite; Underplating; Petrogenesis; Crust; Igneous rock; Fractional crystallization (geology); Felsic; Igneous differentiation; Petrology; Craton; Lithosphere; Oceanic crust; Basalt; Subduction; Tectonics; Paleontology","score_opus":0.012932056198994728,"score_gpt":0.19742994243132758,"score_spread":0.18449788623233285,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4327713533","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99471545,0.0019800137,0.00005007551,0.0029420462,0.000040096053,0.00012186208,0.000104924104,0.0000041041694,0.000041416522],"genre_scores_gemma":[0.9996543,0.000060131842,0.00013995431,0.00005399437,0.00004129983,0.0000017078827,0.000023787168,0.0000012310148,0.000023597207],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991025,0.000054807024,0.0002170564,0.00017874867,0.0001257819,0.00032116126],"domain_scores_gemma":[0.9994193,0.00012909077,0.00012262947,0.00005824987,0.000057559748,0.00021320574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000559646,0.00009561035,0.00015604205,0.0003017052,0.0004933075,0.00012684855,0.00021151478,0.000032056934,0.000049192382],"category_scores_gemma":[0.00005005112,0.000054180255,0.00005522098,0.00089791307,0.00049196486,0.00021211132,0.000005131416,0.0000881635,0.0000035469202],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011283208,0.0000032692358,0.9976442,0.0000047051844,0.000010307772,0.0000058192945,0.00017033648,0.0007874816,0.00016019853,0.000111399924,0.000006459573,0.0010845481],"study_design_scores_gemma":[0.0002494063,0.00022177718,0.98998445,0.000017232756,0.00003718799,0.00013102213,0.00079450436,0.003928354,0.000004438981,0.0045006415,0.000052249517,0.00007873569],"about_ca_topic_score_codex":0.02153232,"about_ca_topic_score_gemma":0.75927144,"teacher_disagreement_score":0.7377391,"about_ca_system_score_codex":0.00000307167,"about_ca_system_score_gemma":0.00020059136,"threshold_uncertainty_score":0.9849834},"labels":[],"label_agreement":null},{"id":"W4328052242","doi":"10.1139/cjes-2022-0106","title":"Alkaline picritic volcanism on northern Ellesmere Island associated with initial rifting of the Sverdrup Basin, Canadian Arctic","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Julius-Maximilians-Universität Würzburg","keywords":"Geology; Volcanic rock; Geochemistry; Basalt; Permian; Carboniferous; Rift; Paleontology; Volcano; Structural basin","score_opus":0.017968602163037927,"score_gpt":0.1994220156955168,"score_spread":0.18145341353247887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4328052242","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9901576,0.000067003304,9.769113e-7,0.004765413,0.00020557473,0.000051937695,0.00014087914,0.0000037219024,0.004606869],"genre_scores_gemma":[0.99875134,0.000005634944,0.000025796782,0.0009743404,0.00008147432,1.3512998e-7,0.000012465392,0.000001913212,0.00014690915],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99847466,0.00011163378,0.0002943984,0.00016214058,0.00042185702,0.00053529104],"domain_scores_gemma":[0.9985217,0.0002601174,0.00019801459,0.000099351106,0.00024981727,0.00067099737],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007208365,0.00011808099,0.00023009899,0.00031950074,0.00056880363,0.00007404319,0.00050332415,0.000056629633,0.002687302],"category_scores_gemma":[0.0008216444,0.00006429919,0.000111051515,0.0015255017,0.00063626404,0.000113408896,0.00000548144,0.00025429516,0.000040319006],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000053210783,0.0000032515288,0.9926392,0.0000032812036,0.000029606028,0.000097308475,0.00015201802,0.0061445166,0.000008414316,0.000038361453,0.0001334597,0.00074527494],"study_design_scores_gemma":[0.0001817684,0.00040366736,0.99395454,0.00013698172,0.000042195366,0.000029796247,0.00037897515,0.0019014492,0.0000936553,0.0017433272,0.0010086877,0.0001249859],"about_ca_topic_score_codex":0.6014404,"about_ca_topic_score_gemma":0.99838483,"teacher_disagreement_score":0.3969444,"about_ca_system_score_codex":0.000006125412,"about_ca_system_score_gemma":0.0018884705,"threshold_uncertainty_score":0.9982244},"labels":[],"label_agreement":null},{"id":"W4353045599","doi":"10.1139/cjes-2022-0002","title":"Reinterpretation of a major terrane boundary in the northern Svalbard Caledonides based on metamorphic fingerprinting of rocks in northern Spitsbergen","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Terrane; Metamorphism; Metamorphic rock; Geochemistry; Metamorphic facies; Monazite; Thrust fault; Tectonics; Geomorphology; Seismology; Facies; Zircon","score_opus":0.01837435800757367,"score_gpt":0.20918399748221964,"score_spread":0.19080963947464596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4353045599","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964812,0.00026467736,0.000016376416,0.0013983245,0.0000708927,0.00005590472,0.00001246135,0.0000018581461,0.0016983474],"genre_scores_gemma":[0.99968845,0.0000060737607,0.00012102192,0.00013991946,0.000024087609,2.7729112e-7,0.0000046799264,0.000001120621,0.000014379665],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985205,0.00018911641,0.0004925182,0.00014257376,0.0003699784,0.00028530534],"domain_scores_gemma":[0.999087,0.00033908352,0.00026421435,0.00009334292,0.00008378616,0.00013260044],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002142537,0.00008902132,0.0002464053,0.00057735667,0.00010423954,0.000037299586,0.00048311925,0.000034170153,0.00053697673],"category_scores_gemma":[0.0004923897,0.000052752133,0.00012663293,0.0014554835,0.0003262082,0.00011611774,0.0000049000414,0.00018476455,0.000016318749],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010824319,0.000005952034,0.90495414,0.00000907093,0.0000059123104,0.00005097131,0.000517414,0.09042148,0.00008381504,0.0000023459859,0.0000026932598,0.003935386],"study_design_scores_gemma":[0.0001259811,0.00022281602,0.97980034,0.00010635503,0.0000124921135,0.0000066232756,0.00064979185,0.017349089,0.0001935327,0.001418836,0.00004931223,0.00006484047],"about_ca_topic_score_codex":0.06417609,"about_ca_topic_score_gemma":0.9416633,"teacher_disagreement_score":0.87748724,"about_ca_system_score_codex":0.000002221454,"about_ca_system_score_gemma":0.00039472434,"threshold_uncertainty_score":0.94205564},"labels":[],"label_agreement":null},{"id":"W4361291256","doi":"10.1139/cjes-2022-0134","title":"Lower and Upper Ordovician conodont biostratigraphy and revised lithostratigraphy in the fault and fold zones of the Boothia Uplift, south-western Boothia Peninsula, Nunavut","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Nunavut","funders":"","keywords":"Ordovician; Conodont; Geology; Paleontology; Biostratigraphy; Fold (higher-order function); Bay; Global Boundary Stratotype Section and Point; Peninsula; Oceanography; Archaeology","score_opus":0.020092581459025472,"score_gpt":0.223405992146914,"score_spread":0.20331341068788852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4361291256","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97976905,0.014636764,0.0000018640748,0.0030992215,0.00023173654,0.0001712289,0.00005939212,0.0000035216328,0.002027213],"genre_scores_gemma":[0.99922705,0.0003014276,0.00013341769,0.00028690058,0.00003696724,5.404588e-7,5.4872095e-7,0.0000010134692,0.000012152758],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985051,0.00019589442,0.00041104856,0.00022657015,0.0002716406,0.0003897487],"domain_scores_gemma":[0.99897856,0.000267773,0.0002568904,0.00014125445,0.000052459578,0.0003030689],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013728713,0.00016159758,0.0002755792,0.00046711083,0.0005604167,0.00023476071,0.00042292132,0.000093258444,0.000027262526],"category_scores_gemma":[0.000093899274,0.00009086783,0.00009357819,0.0009097003,0.002092438,0.00036837027,0.000002962156,0.0002739606,7.844545e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001147201,0.0000026944617,0.99437964,0.000014299143,0.000014180608,0.000037201142,0.0024919745,0.000011311927,0.00001824111,0.00022236457,0.000030719373,0.0027659107],"study_design_scores_gemma":[0.00023694632,0.00032713034,0.9955901,0.00011928498,0.000020364552,0.00012755727,0.0020213444,0.00016845496,0.000012771413,0.00090688403,0.0003525911,0.00011660856],"about_ca_topic_score_codex":0.0060720327,"about_ca_topic_score_gemma":0.5450562,"teacher_disagreement_score":0.5389842,"about_ca_system_score_codex":3.3959896e-7,"about_ca_system_score_gemma":0.0004088564,"threshold_uncertainty_score":0.9179138},"labels":[],"label_agreement":null},{"id":"W4361295521","doi":"10.1139/cjes-2022-0147","title":"The tectonic evolution of Thelon tectonic zone, Canada: a new model based on petrological modeling linked with Lu–Hf garnet and U–Pb accessory mineral geochronology","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia; University of Manitoba; Geological Survey of Canada; Natural Resources Canada","funders":"British Columbia Knowledge Development Fund; Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Plutonism; Geology; Metamorphism; Craton; Geochemistry; Geochronology; Terrane; Subduction; Zircon; Isochron; Dharwar Craton; Granulite; Petrology; Tectonics; Paleontology; Magmatism; Facies","score_opus":0.02018636309813869,"score_gpt":0.19367083522392392,"score_spread":0.17348447212578522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4361295521","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99297637,0.0010200865,0.00069350906,0.004415426,0.00007734273,0.000059099875,0.000018730536,0.0000062064178,0.0007332602],"genre_scores_gemma":[0.9990246,0.000048333408,0.000535411,0.00023386817,0.000051435323,3.7343548e-7,0.000003977368,0.0000015002939,0.000100496385],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9984311,0.000081529375,0.00031682436,0.00023185516,0.00039510045,0.00054361083],"domain_scores_gemma":[0.9987816,0.00029632196,0.00018239424,0.00010550676,0.00013441777,0.00049971434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006866136,0.00013734645,0.00026151488,0.00025399064,0.0004639863,0.00006875289,0.00047051266,0.0000711965,0.00029899197],"category_scores_gemma":[0.00026589804,0.00006956481,0.00006733704,0.0008286413,0.000602366,0.00011657488,0.000010230457,0.00028020696,0.0000034903505],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046718418,0.000002502753,0.15646991,0.0000030541332,0.000013945688,0.000028230092,0.000020550731,0.8416317,0.000054464894,0.00010637,0.00007874656,0.0015438035],"study_design_scores_gemma":[0.00019725041,0.000506805,0.21023875,0.000020499512,0.000020653553,0.000026116602,0.00015239991,0.78600955,0.000023066952,0.002648879,0.00006527494,0.00009075408],"about_ca_topic_score_codex":0.642611,"about_ca_topic_score_gemma":0.9899475,"teacher_disagreement_score":0.34733647,"about_ca_system_score_codex":0.0000098914425,"about_ca_system_score_gemma":0.0042544315,"threshold_uncertainty_score":0.7547178},"labels":[],"label_agreement":null},{"id":"W4361297518","doi":"10.1139/cjes-2023-0005","title":"Equilibration depth and temperature of Neogene alkaline lavas in the Cordillera of Alaska and Canada as a constraint on the lithosphere–asthenosphere boundary","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"","keywords":"Geology; Asthenosphere; Lithosphere; Neogene; Lava; Basalt; Mantle (geology); Volcanism; Geochemistry; Volcano; Tectonics; Seismology; Geomorphology; Structural basin","score_opus":0.013585324440460511,"score_gpt":0.1930330335991727,"score_spread":0.1794477091587122,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4361297518","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98975503,0.001001973,1.8839144e-7,0.006922671,0.00004553407,0.00005424725,0.000033431297,7.952358e-7,0.0021861414],"genre_scores_gemma":[0.9990134,0.00008301451,0.000053545577,0.0007891718,0.00002271387,1.453456e-7,0.000003468383,5.863606e-7,0.00003395749],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910617,0.00009488993,0.00023605568,0.000102693935,0.0002735675,0.00018661862],"domain_scores_gemma":[0.99919856,0.0003523348,0.00012916718,0.00006272112,0.00005942641,0.00019777176],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00067721005,0.00007141025,0.0001615166,0.000053521955,0.00017391061,0.000062428655,0.000234854,0.000030693707,0.001728758],"category_scores_gemma":[0.0002825539,0.000033190478,0.000031138505,0.0005596279,0.00072975655,0.000077572935,0.000005500998,0.00014238729,0.0000013296844],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016401616,0.0000050403414,0.99169296,0.000010961155,0.000021100477,0.00007563752,0.00055704365,0.0020990344,0.00038471533,0.00029265304,0.0006076084,0.00423687],"study_design_scores_gemma":[0.00011638322,0.0004092123,0.98940676,0.000057102927,0.000013261051,0.00007034315,0.0044680783,0.0011472354,0.0005837153,0.0026728953,0.0009858451,0.00006914854],"about_ca_topic_score_codex":0.55371207,"about_ca_topic_score_gemma":0.98506165,"teacher_disagreement_score":0.43134955,"about_ca_system_score_codex":9.1417365e-7,"about_ca_system_score_gemma":0.001238054,"threshold_uncertainty_score":0.9991838},"labels":[],"label_agreement":null},{"id":"W4362661539","doi":"10.1139/cjes-2022-0104","title":"A reassessment of the Erie Interstade from field work in the Cayuga basin, central New York","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Varve; Structural basin; Glacial period; Moraine; Oceanography; Period (music); Front (military); Shelf ice; Arctic; Physical geography; Arctic ice pack; Paleontology; Antarctic sea ice; Sediment; Geography","score_opus":0.050242575537570194,"score_gpt":0.2534259932576544,"score_spread":0.20318341772008422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4362661539","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98121756,0.0006645236,0.000004089549,0.014460307,0.00073075166,0.000067050925,0.000015875321,0.0000014594933,0.002838402],"genre_scores_gemma":[0.99896586,0.000026229683,0.00010586866,0.00067980064,0.000074821255,1.3241528e-7,0.0000020584187,6.533571e-7,0.0001445599],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987052,0.0002608974,0.00023064032,0.00010420517,0.0002680874,0.0004309891],"domain_scores_gemma":[0.99884915,0.00065285823,0.0001114188,0.00012363549,0.000024518087,0.00023842952],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001098602,0.00006328156,0.00013568283,0.00018522565,0.00024410899,0.0000592442,0.00090837595,0.000057126435,0.0016127779],"category_scores_gemma":[0.00026275183,0.000033234875,0.000066882625,0.0011124656,0.0005268592,0.00010673575,0.000007718407,0.00032816888,0.000026420728],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013522552,0.0000014784557,0.9932808,0.0000013863457,0.0000062402046,0.00006248837,0.0017113435,0.00035206898,4.2228046e-7,0.000053412266,0.0033147715,0.001202033],"study_design_scores_gemma":[0.00009636041,0.00011261785,0.9914916,0.000053326603,0.000004791799,0.000036314486,0.002433921,0.000058135225,0.000017105376,0.0011276364,0.004529941,0.00003821665],"about_ca_topic_score_codex":0.042402375,"about_ca_topic_score_gemma":0.83022034,"teacher_disagreement_score":0.787818,"about_ca_system_score_codex":5.995453e-7,"about_ca_system_score_gemma":0.0017091215,"threshold_uncertainty_score":0.9992999},"labels":[],"label_agreement":null},{"id":"W4366609781","doi":"10.1139/cjes-2022-0124","title":"Eruptive history of the Fort Selkirk area, Central Yukon","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Thompson Rivers University; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Simon Fraser University","keywords":"Geology; Terrane; Mafic; Volcano; Volcanism; Lava; Tectonics; Geochemistry; Geomorphology; Paleontology","score_opus":0.0453711534324647,"score_gpt":0.22916795154581768,"score_spread":0.18379679811335298,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4366609781","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.978294,0.001290975,0.0000017141667,0.0011207984,0.0017311211,0.000055902165,0.000016478163,0.0000030659146,0.01748593],"genre_scores_gemma":[0.9980976,0.000039896815,0.000058397167,0.00015046372,0.000050415467,1.0336438e-7,0.000001662384,8.760078e-7,0.001600584],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987479,0.00012566964,0.00022263618,0.00010944336,0.00027637408,0.0005179662],"domain_scores_gemma":[0.9990947,0.00019388537,0.0001599548,0.000096731,0.00009350752,0.00036118188],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010589241,0.000067737004,0.00015259808,0.00030844877,0.0002741205,0.000015472546,0.0006066936,0.000062121704,0.0018918077],"category_scores_gemma":[0.00023042804,0.000041979794,0.00009111912,0.00058935396,0.0015890894,0.00018014986,0.0000067377973,0.0002369663,0.00006376216],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005044463,0.000001153127,0.995952,0.0000037279544,0.000008647492,0.000052003117,0.00062602136,0.0014238057,0.0000032792836,0.000100165285,0.0016144362,0.00020971683],"study_design_scores_gemma":[0.00008069619,0.00013302358,0.98888606,0.000022179027,0.0000063595285,0.00013777505,0.0004459897,0.0007383136,0.000027966511,0.00059237017,0.008880282,0.000048990303],"about_ca_topic_score_codex":0.0048825443,"about_ca_topic_score_gemma":0.47140953,"teacher_disagreement_score":0.466527,"about_ca_system_score_codex":0.0000016879577,"about_ca_system_score_gemma":0.003643095,"threshold_uncertainty_score":0.9990206},"labels":[],"label_agreement":null},{"id":"W4367172719","doi":"10.1139/cjes-2022-0119","title":"Petrogenesis and geochemical evidence from early Jurassic intrusive rocks and their implications for subduction of the Paleo-Pacific Plate in the Yanbian area, Northeast China","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Zircon; Geochemistry; Partial melting; Fractional crystallization (geology); Diorite; Felsic; Petrogenesis; Basalt; Mantle wedge; Subduction; Magmatism; Lithophile; Adakite; Underplating; Petrology; Continental crust; Mafic; Oceanic crust; Mantle (geology); Paleontology; Tectonics","score_opus":0.02645876909019501,"score_gpt":0.20729846901733012,"score_spread":0.1808396999271351,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367172719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9908921,0.0010608898,0.00001570505,0.0076618944,0.00006336238,0.00008654925,0.00015926325,0.0000017284931,0.000058501515],"genre_scores_gemma":[0.99970716,0.000115323106,0.000060121914,0.00005193815,0.00004952903,0.00000107338,0.0000054140364,7.2664045e-7,0.000008728128],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999203,0.00006270633,0.00022672158,0.00016359087,0.000111688954,0.00023224141],"domain_scores_gemma":[0.99905926,0.00044847565,0.00014872692,0.00009577923,0.000064727275,0.00018300393],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005335353,0.000082344945,0.00015475217,0.0001315682,0.00035972137,0.00008367738,0.00036382943,0.000037473477,0.00010697551],"category_scores_gemma":[0.00029635915,0.00003883583,0.00007355556,0.000787992,0.0005982786,0.00017170205,0.000009349205,0.0001199949,0.000001120982],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005703213,0.0000017025872,0.99525404,0.0000024345645,0.0000070857914,9.077714e-7,0.00068759953,0.0002930722,0.00028085033,0.000011240733,0.000020257214,0.0034350837],"study_design_scores_gemma":[0.00005619937,0.00007972547,0.98635894,0.000034814424,0.00001577576,0.00002438563,0.001052413,0.001127587,0.00023550022,0.010881209,0.00008039454,0.000053075233],"about_ca_topic_score_codex":0.023505686,"about_ca_topic_score_gemma":0.3535539,"teacher_disagreement_score":0.33004823,"about_ca_system_score_codex":0.0000010646474,"about_ca_system_score_gemma":0.00015771204,"threshold_uncertainty_score":0.9829969},"labels":[],"label_agreement":null},{"id":"W4367596833","doi":"10.1139/cjes-2023-0011","title":"Crustal eduction and slab-failure magmatism in an Orosirian (2.05–1.80 Ga) postcollisional cratonic foredeep: geochronology of Seton volcanics and Compton laccoliths, Tu Cho (Great Slave Lake), NWT, Canada","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"McGill University; California Institute of Technology; Harvard University; National Science Foundation","keywords":"Geology; Foreland basin; Zircon; Geochemistry; Laurentia; Thermochronology; Craton; Geochronology; Paleontology; Geomorphology; Ordovician; Structural basin; Tectonics","score_opus":0.010546783404677249,"score_gpt":0.19790050681248617,"score_spread":0.18735372340780893,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367596833","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960335,0.00073445437,0.0000026263058,0.0025120014,0.00021273052,0.00009334908,0.00019794314,0.0000037908858,0.00020964198],"genre_scores_gemma":[0.99919766,0.000086169755,0.00035648383,0.00018772406,0.000067234476,4.2635293e-7,0.0000435849,0.0000017983277,0.00005891266],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984103,0.0000930275,0.00040388937,0.000268148,0.00032395095,0.0005007242],"domain_scores_gemma":[0.9987933,0.00013112754,0.00019709587,0.0000860935,0.00012765186,0.0006647258],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005559278,0.00014610177,0.00033441573,0.00038001197,0.00027967777,0.00009444836,0.00026479308,0.00009356787,0.001566489],"category_scores_gemma":[0.00012958533,0.00010894672,0.000044318702,0.0008598066,0.00061802415,0.00039446857,0.000016450982,0.00022498035,0.0000033030526],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015296373,0.0000048255138,0.989736,0.000012595197,0.00001295941,0.00011950452,0.00013726928,0.0037057758,0.0001003166,0.00015724736,0.00042500588,0.0055731684],"study_design_scores_gemma":[0.00026282173,0.00037405945,0.98274463,0.000040149618,0.000017914343,0.00022828918,0.00068525877,0.010185896,0.00011525691,0.0028867794,0.0023184926,0.0001404605],"about_ca_topic_score_codex":0.5523408,"about_ca_topic_score_gemma":0.9990489,"teacher_disagreement_score":0.44670808,"about_ca_system_score_codex":0.000007593802,"about_ca_system_score_gemma":0.0016723305,"threshold_uncertainty_score":0.9993462},"labels":[],"label_agreement":null},{"id":"W4376128626","doi":"10.1139/cjes-2023-0017","title":"Onshore–offshore correlation of central Lake Erie glacial deposits","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"University of Toronto","keywords":"Geology; Moraine; Geomorphology; Shore; Glacial period; Terrace (agriculture); Glacier; Debris; Submarine pipeline; Oceanography; Archaeology","score_opus":0.027651467081775873,"score_gpt":0.24201619879091815,"score_spread":0.21436473170914228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4376128626","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911393,0.00042490487,0.000017438937,0.0007531804,0.0009881144,0.000055637487,0.000054299,0.000005033139,0.006562096],"genre_scores_gemma":[0.99945146,0.00003595326,0.00018369204,0.000055217643,0.00008933298,9.089842e-8,0.00002091914,0.0000010964368,0.00016224607],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986559,0.00012152019,0.00028483215,0.00011970961,0.0002811866,0.00053685834],"domain_scores_gemma":[0.9989906,0.0002025704,0.0001454212,0.00006630608,0.000111146226,0.00048397755],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00093511614,0.00007440743,0.00017473512,0.0004901464,0.00039683768,0.000041734438,0.00036407166,0.00008985586,0.0024808138],"category_scores_gemma":[0.0002602628,0.000058964608,0.00006660077,0.00089417107,0.0009068692,0.00025045068,0.0000044704097,0.00022000993,0.00012784913],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012351392,0.0000015446005,0.99409175,0.0000050018093,0.000008596985,0.00014030098,0.00030002397,0.0041826437,0.0000022447139,0.00014910646,0.00029915306,0.00080725807],"study_design_scores_gemma":[0.00011393079,0.00023752054,0.9939865,0.00002154163,0.000007672934,0.00021287863,0.00026120487,0.0018681365,0.000039898037,0.0005119391,0.0026769685,0.00006183166],"about_ca_topic_score_codex":0.0008248962,"about_ca_topic_score_gemma":0.9103072,"teacher_disagreement_score":0.9094823,"about_ca_system_score_codex":3.0018197e-7,"about_ca_system_score_gemma":0.00147241,"threshold_uncertainty_score":0.998431},"labels":[],"label_agreement":null},{"id":"W4376129758","doi":"10.1139/cjes-2022-0136","title":"Magnetotelluric imaging of the magmatic and geothermal systems beneath Mount Meager, southwestern Canada","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Magnetotellurics; Volcano; Geothermal gradient; Fumarole; Magma chamber; Magma; Crust; Petrology; Geochemistry; Mount; Electrical resistivity and conductivity; Geomorphology; Geophysics","score_opus":0.01344458845109661,"score_gpt":0.19520630381909174,"score_spread":0.18176171536799512,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4376129758","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99632764,0.0016974129,0.000020486172,0.00069170044,0.0006751786,0.000062978615,0.000033309374,0.0000024741387,0.00048883556],"genre_scores_gemma":[0.9993366,0.000011935246,0.0001119919,0.00013790361,0.00008082829,1.1284975e-7,4.8767185e-7,0.0000015352181,0.0003186043],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987334,0.00012644324,0.00027328875,0.00011362463,0.00037931977,0.00037394176],"domain_scores_gemma":[0.9990603,0.00023046554,0.00018193394,0.00008370599,0.00006462773,0.00037900527],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007436195,0.00008639545,0.00018156045,0.00015160991,0.00028609595,0.000104559935,0.00037487323,0.00001808081,0.00013024028],"category_scores_gemma":[0.00013092498,0.000049748345,0.000046114652,0.0008737917,0.00030716186,0.00014394087,0.0000073807587,0.00012660612,0.000007010225],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000031874583,0.000001917179,0.93164784,0.000038871698,0.000011353589,0.00008312511,0.00027176595,0.01825403,0.000056222572,0.00013934771,0.00010745849,0.049384873],"study_design_scores_gemma":[0.00006985941,0.000070022696,0.97753245,0.000043798736,0.0000108658605,0.0000817093,0.0003632102,0.019907298,0.00003401086,0.00040445646,0.0014098352,0.00007250351],"about_ca_topic_score_codex":0.85786897,"about_ca_topic_score_gemma":0.939367,"teacher_disagreement_score":0.08149804,"about_ca_system_score_codex":0.0000029023145,"about_ca_system_score_gemma":0.0014823275,"threshold_uncertainty_score":0.26295853},"labels":[],"label_agreement":null},{"id":"W4377100221","doi":"10.1139/cjes-2023-0031","title":"Discussion: The Terreneuvian MacCodrum Brook section, Mira terrane, Cape Breton Island, Nova Scotia, Canada: age constraints from ash layers, organic-walled microfossils, and trace fossils","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Terrane; Geology; Paleontology; Ordovician; Tectonics; Nova scotia; Lithostratigraphy; Peninsula; Archaeology; Oceanography; Geography; Sedimentary rock","score_opus":0.016315834416765526,"score_gpt":0.19275968877136868,"score_spread":0.17644385435460314,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4377100221","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98234665,0.0015388678,0.000008741507,0.01348028,0.0008861603,0.000087755674,0.00023507573,0.00000825528,0.001408223],"genre_scores_gemma":[0.99837244,0.000046705165,0.000089025816,0.0006184924,0.0002653062,1.5360472e-7,0.000025566951,0.0000023270459,0.0005800142],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980669,0.00012321825,0.0004235491,0.00032262004,0.00044025012,0.0006234403],"domain_scores_gemma":[0.99855745,0.00020705904,0.00020971279,0.00013581825,0.00008113268,0.00080885383],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006220674,0.00019418147,0.00031755946,0.00018674618,0.0007070905,0.00032115285,0.00058914424,0.000084698964,0.0118692815],"category_scores_gemma":[0.00016522377,0.000096481825,0.00009927644,0.0009465688,0.0010673314,0.00022558005,0.000014641381,0.0003420852,0.00004904394],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011555297,0.0000041878525,0.98081166,0.000005731703,0.00005258166,0.000440593,0.0005453575,0.00034546945,0.0009899882,0.000004270881,0.0059892028,0.010799428],"study_design_scores_gemma":[0.00026709263,0.00010717932,0.9842982,0.0000482401,0.00004303543,0.00020481941,0.0019000177,0.00044458781,0.00032887555,0.000897906,0.011243933,0.00021607023],"about_ca_topic_score_codex":0.89207995,"about_ca_topic_score_gemma":0.99956256,"teacher_disagreement_score":0.1074826,"about_ca_system_score_codex":0.0000059765584,"about_ca_system_score_gemma":0.0015274204,"threshold_uncertainty_score":0.989034},"labels":[],"label_agreement":null},{"id":"W4377100527","doi":"10.1139/cjes-2023-0003","title":"Systematics and biostratigraphy of a new trilobite fauna collected from the subsurface Earlie Formation (Wuliuan Stage, Miaolingian Series, Cambrian) in southwestern Saskatchewan","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Trilobite; Geology; Biostratigraphy; Paleontology; Diachronous; Fauna; Stage (stratigraphy); Chronostratigraphy; Structural basin; Ordovician","score_opus":0.02771924378466945,"score_gpt":0.2178635291414299,"score_spread":0.19014428535676045,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4377100527","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99412215,0.003686844,0.00001929536,0.00054266374,0.0002501867,0.00016093538,0.00022652397,0.000005785314,0.0009856317],"genre_scores_gemma":[0.99923605,0.00006213419,0.00053769624,0.00003030989,0.000038103528,1.8472319e-7,0.0000056084873,8.5414257e-7,0.000089046334],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985196,0.00017118295,0.0005499422,0.00013691821,0.0002757442,0.0003466001],"domain_scores_gemma":[0.9988093,0.00024842517,0.00038690385,0.00010750305,0.00006814388,0.00037973514],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010315641,0.00012287486,0.00028630721,0.0004350616,0.00032796338,0.0001685931,0.00035847584,0.00008179696,0.00006252062],"category_scores_gemma":[0.00011500338,0.00008417641,0.00006817677,0.0014879712,0.0005100922,0.0005868399,0.0000013233229,0.00017771492,0.0000032283986],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019362395,0.0000014893767,0.9904203,0.000022610284,0.000018170327,0.000030265077,0.0074354117,0.0002874881,0.00005056683,0.000022482916,0.000067289744,0.0016246018],"study_design_scores_gemma":[0.00028552156,0.000233697,0.9845564,0.00018176889,0.0000138989635,0.000045768804,0.013244803,0.00083660334,0.000080599966,0.00033931457,0.000087693785,0.00009395613],"about_ca_topic_score_codex":0.11140038,"about_ca_topic_score_gemma":0.9788354,"teacher_disagreement_score":0.86743504,"about_ca_system_score_codex":0.0000012505932,"about_ca_system_score_gemma":0.0016208775,"threshold_uncertainty_score":0.8945169},"labels":[],"label_agreement":null},{"id":"W4377966484","doi":"10.1139/cjes-2022-0094","title":"Petrogenesis and tectonic significance of the Early Cretaceous Xizhelimu diorite in Keyouzhongqi, Inner Mongolia, China","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Diorite; Geology; Zircon; Petrogenesis; Geochemistry; Partial melting; Petrology; Petrography; Magma; Geochronology; Crust; Mantle (geology); Volcano","score_opus":0.012296220254983775,"score_gpt":0.18768707880931235,"score_spread":0.17539085855432857,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4377966484","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963187,0.0014637244,0.0000010131616,0.0012144325,0.0001413147,0.000051306597,0.000032458443,0.0000030315973,0.000774018],"genre_scores_gemma":[0.99959284,0.00008504114,0.00006800443,0.000068288406,0.00003868616,2.3423395e-7,7.6172114e-7,0.0000010613414,0.00014505818],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987727,0.00008152299,0.00030914618,0.0001665661,0.0002926123,0.00037744764],"domain_scores_gemma":[0.99923897,0.0001198119,0.00016436206,0.00009529208,0.000059054622,0.0003225412],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006928626,0.000094006355,0.00022034935,0.00030795016,0.00020796039,0.000061838204,0.00046989706,0.000044134755,0.00081437675],"category_scores_gemma":[0.00023312705,0.00005331003,0.00009925105,0.001955571,0.00072272803,0.00016161078,0.000012453184,0.00017252263,0.000014563753],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000033380145,0.0000018676473,0.99382514,0.000004775766,0.00000668405,0.000036243116,0.0001579358,0.0038774973,0.00022478285,0.000017778648,0.000011897684,0.0018320774],"study_design_scores_gemma":[0.00008179693,0.000120334735,0.9946697,0.000024128025,0.000010919574,0.000027987377,0.00014310243,0.0013574729,0.0007042229,0.0025286977,0.0002553473,0.00007628558],"about_ca_topic_score_codex":0.04276402,"about_ca_topic_score_gemma":0.34347904,"teacher_disagreement_score":0.300715,"about_ca_system_score_codex":0.0000013023517,"about_ca_system_score_gemma":0.00033455814,"threshold_uncertainty_score":0.9636103},"labels":[],"label_agreement":null},{"id":"W4378374074","doi":"10.1139/cjes-2022-0142","title":"Paralava and clinker from the Canadian Arctic: a record of combustion metamorphism dating back to the late Miocene","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Sorbonne Université; Natural Resources Canada; Université Pierre et Marie Curie; Parks Canada","keywords":"Geology; Sedimentary rock; Geochemistry; Metamorphism; Sedimentary depositional environment; Clastic rock; Paleontology; Structural basin","score_opus":0.043004695129812504,"score_gpt":0.24162078053470482,"score_spread":0.1986160854048923,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4378374074","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98775804,0.00038910744,0.00008994242,0.010823365,0.00036004614,0.000061304745,0.000020140964,0.0000044055037,0.0004936393],"genre_scores_gemma":[0.99897456,0.00010020879,0.00035348505,0.00034733885,0.00008368956,7.0975244e-7,0.0000023211187,0.0000048514034,0.00013283093],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9992208,0.000059406444,0.0002519331,0.00006831908,0.00017365826,0.00022592206],"domain_scores_gemma":[0.9991959,0.0001096216,0.00006940406,0.000105924315,0.000085237385,0.00043396157],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009043917,0.00006521736,0.00013073641,0.00026753944,0.00032846158,0.00013577727,0.00028283027,0.00002922339,0.00016696558],"category_scores_gemma":[0.0001912862,0.000037604834,0.000048278212,0.00093932566,0.00014995216,0.00014975455,0.00000767429,0.00014180814,0.000033737102],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003856334,0.000002414128,0.17702036,0.000015267873,0.0002096144,0.000044890945,0.00582669,0.7970672,0.0005489667,0.00020264955,0.009989202,0.009068881],"study_design_scores_gemma":[0.00037742523,0.00016378683,0.53315526,0.0003008769,0.00015874411,0.000028263274,0.004435791,0.37139446,0.0006221976,0.0012619887,0.08773348,0.00036775542],"about_ca_topic_score_codex":0.3259386,"about_ca_topic_score_gemma":0.9812169,"teacher_disagreement_score":0.6552783,"about_ca_system_score_codex":0.000012666211,"about_ca_system_score_gemma":0.00046696194,"threshold_uncertainty_score":0.67855},"labels":[],"label_agreement":null},{"id":"W4378978560","doi":"10.1139/cjes-2023-0002","title":"Multiple forms of bioimmuration in a coral–crinoid–bryozoan association from the Middle Devonian Onondaga Formation of southeastern Ontario","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Marine Ecology and Invasive Species","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Crinoid; Coral; Devonian; Geology; Paleontology; Tunicate; Bryozoa; Paleozoic; Rugosa; Macrofossil; Bioerosion; Biology; Ecology; Oceanography; Taxonomy (biology)","score_opus":0.03273525779577343,"score_gpt":0.20146467961737444,"score_spread":0.168729421821601,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4378978560","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967107,0.000015840515,0.000021025018,0.00060823234,0.0001864004,0.00008258452,0.000016747643,0.0000013606084,0.0023571132],"genre_scores_gemma":[0.99941045,0.00000514608,0.00013344323,0.00006036547,0.000017166632,9.290925e-7,0.00000440404,0.0000016219351,0.00036644342],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909556,0.000051757757,0.00035041332,0.00007454914,0.00023099028,0.00019675943],"domain_scores_gemma":[0.99926347,0.00013263925,0.00042482433,0.00006718179,0.00003458102,0.0000773336],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008366966,0.000054350123,0.00012338371,0.00013665912,0.00015795781,0.00002764411,0.00026941588,0.000042686897,0.00084265694],"category_scores_gemma":[0.00025044614,0.000037671754,0.00004648557,0.00044814867,0.0002464807,0.00056128256,0.000024167775,0.000109387984,0.000034341825],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057546836,0.000005044737,0.9928413,0.0000015188673,0.0000031712925,0.0000018887047,0.005215785,0.00093251665,0.0005273263,0.000045386383,0.00011144142,0.00030884088],"study_design_scores_gemma":[0.00018141409,0.000114218856,0.99308443,0.00002672619,0.0000040236037,0.0000024652034,0.00244585,0.00096162106,0.0014727123,0.0006739647,0.0009909782,0.00004158081],"about_ca_topic_score_codex":0.16257678,"about_ca_topic_score_gemma":0.989537,"teacher_disagreement_score":0.8269602,"about_ca_system_score_codex":0.00005358818,"about_ca_system_score_gemma":0.00032837974,"threshold_uncertainty_score":0.9226503},"labels":[],"label_agreement":null},{"id":"W4379931236","doi":"10.1139/cjes-2023-0027","title":"Seismic reflection stratigraphy of Lac Simard, Quebec, Canada: mass flow sedimentation in glacial Lake Barlow-Ojibway","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Geology; Varve; Turbidity current; Unconformity; Geomorphology; Deglaciation; Glacial period; Meltwater; Mudflow; Facies; Paleontology; Geochemistry; Structural basin; Sediment; Sedimentary depositional environment; Landslide","score_opus":0.023206633822728275,"score_gpt":0.2465820887036894,"score_spread":0.2233754548809611,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379931236","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942219,0.00024866365,0.000007253436,0.0016440833,0.0007723716,0.00007569098,0.000040182033,0.0000032943192,0.0029865522],"genre_scores_gemma":[0.999505,0.00003558549,0.00011598966,0.00010129458,0.00005835508,3.0848477e-7,0.000019450246,0.0000011885246,0.0001628509],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998495,0.00020929496,0.0003430509,0.00014714367,0.00035283013,0.00045269745],"domain_scores_gemma":[0.9991833,0.00020065546,0.00015130718,0.000063199215,0.00009205632,0.00030949712],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001316516,0.00008901211,0.00020397165,0.0007672983,0.00025394108,0.000038953785,0.00027277606,0.00007810647,0.0010045475],"category_scores_gemma":[0.00012183106,0.00007435965,0.00004838094,0.0013627551,0.00044295957,0.00035575306,0.000002221331,0.00024703884,0.000018665009],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018646224,0.0000011246188,0.9674102,0.000008774035,0.0000083160385,0.00010820661,0.00013632044,0.031488683,0.000012815624,0.000015999402,0.00035682574,0.00043407432],"study_design_scores_gemma":[0.0002246955,0.00020110424,0.990421,0.000023539353,0.0000056191197,0.000035585646,0.00043166996,0.0068359063,0.00021466805,0.0003320875,0.0011991496,0.00007495161],"about_ca_topic_score_codex":0.7629031,"about_ca_topic_score_gemma":0.9999616,"teacher_disagreement_score":0.23705849,"about_ca_system_score_codex":0.0000019338745,"about_ca_system_score_gemma":0.0047178087,"threshold_uncertainty_score":0.9999087},"labels":[],"label_agreement":null},{"id":"W4381281970","doi":"10.1139/cjes-2022-0148","title":"Volcanogenic massive sulfide (VMS) deposits of the Dunnage Zone of the Newfoundland Appalachians: setting, styles, key advances, and future research","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Newfoundland and Labrador; Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Altius","keywords":"Felsic; Geology; Mafic; Volcanogenic massive sulfide ore deposit; Geochemistry; Siliciclastic; Zircon; Continental arc; Metallogeny; Volcanic rock; Pyrite; Geomorphology; Sphalerite; Facies","score_opus":0.017211971815451303,"score_gpt":0.22891066724072123,"score_spread":0.21169869542526992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4381281970","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9837591,0.0077845845,0.0000016306782,0.0060431557,0.00022572688,0.000088277135,0.00004810162,0.0000020402854,0.002047406],"genre_scores_gemma":[0.9987449,0.0005459569,0.00014268923,0.000116163435,0.00014240172,2.1495437e-7,0.0000018845002,0.0000012446612,0.00030453186],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99819523,0.00024378744,0.0003437599,0.00017964971,0.00059571076,0.00044185622],"domain_scores_gemma":[0.99871397,0.0002849147,0.00027896307,0.0001596757,0.00022104576,0.00034142795],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015135087,0.000097362674,0.00022112344,0.00022325767,0.0006167196,0.000068447145,0.00084322534,0.000056750367,0.00044034427],"category_scores_gemma":[0.00035748002,0.000045817163,0.00013129911,0.0021509032,0.0015117471,0.00018271682,0.00003551265,0.00032190687,0.0000071124177],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000064323217,0.0000026811138,0.9921173,0.000018209992,0.000016215708,0.00001213693,0.00023026926,0.0012523495,0.00022968145,0.00015240171,0.000149106,0.005813245],"study_design_scores_gemma":[0.000119667806,0.00013710897,0.98277116,0.00006746281,0.000021500422,0.000038683564,0.0013200361,0.00040609713,0.0003937457,0.0038064586,0.010847575,0.000070509435],"about_ca_topic_score_codex":0.021806732,"about_ca_topic_score_gemma":0.7859226,"teacher_disagreement_score":0.76411587,"about_ca_system_score_codex":0.000002311124,"about_ca_system_score_gemma":0.0007107272,"threshold_uncertainty_score":0.9847071},"labels":[],"label_agreement":null},{"id":"W4381487331","doi":"10.1139/cjes-2023-0056","title":"Reply to the Discussion by Landing and Geyer on “The Terreneuvian MacCodrum Brook section, Mira terrane, Cape Breton Island, Nova Scotia, Canada: age constraints from ash layers, organic-walled microfossils, and trace fossils”","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University","funders":"","keywords":"Nova scotia; Cape; Geology; Terrane; Oceanography; Nova (rocket); Paleontology; Archaeology; Geography","score_opus":0.015771386392450654,"score_gpt":0.19145370464490702,"score_spread":0.17568231825245637,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4381487331","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9512478,0.0006969128,0.000007463039,0.046795134,0.0004131461,0.00009716778,0.000214513,0.000004769846,0.00052309094],"genre_scores_gemma":[0.99675363,0.00003314028,0.0000349154,0.002535152,0.00014081295,2.1454717e-7,0.000015566258,0.000002005016,0.0004845711],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99852544,0.00010916466,0.00028669494,0.0002926437,0.00033551813,0.00045055745],"domain_scores_gemma":[0.9988564,0.00024767418,0.00013240015,0.000113376445,0.00004277284,0.0006073338],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006860458,0.00015289978,0.00021828267,0.00013609116,0.00073457026,0.00031288865,0.00037414394,0.000050155653,0.0030228952],"category_scores_gemma":[0.00020267881,0.00006721505,0.0000481657,0.0006480501,0.00050232926,0.00012235611,0.000014099032,0.00026722884,0.000024469266],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020820738,0.0000038443195,0.95005554,0.000004359307,0.00004060402,0.00015398981,0.0008503916,0.00021157527,0.0019930282,0.0000045654074,0.0386263,0.008034993],"study_design_scores_gemma":[0.00023136362,0.00018767745,0.9562672,0.00007569622,0.000032477543,0.00011101141,0.002216288,0.00048954744,0.00054609095,0.00038701892,0.03924359,0.00021203737],"about_ca_topic_score_codex":0.820465,"about_ca_topic_score_gemma":0.9976496,"teacher_disagreement_score":0.17718461,"about_ca_system_score_codex":0.000005486847,"about_ca_system_score_gemma":0.00044806857,"threshold_uncertainty_score":0.9978885},"labels":[],"label_agreement":null},{"id":"W4382023803","doi":"10.1139/cjes-2022-0083","title":"Paradoxical mid-crustal displacements and stratigraphic continuity: structural evolution of the northeastern Paleoproterozoic Amer belt, Nunavut, Canada","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Fredericton; University of New Brunswick","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Proterozoic; Orogeny; Archean; Fold (higher-order function); Paleontology; Lithology; Fold and thrust belt; Unconformity; Tectonics; Foreland basin","score_opus":0.010580838826678098,"score_gpt":0.1911989966692177,"score_spread":0.1806181578425396,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4382023803","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978098,0.0006152967,0.0000025544664,0.0009275891,0.0002472134,0.00006232584,0.00008368751,0.0000018155978,0.0002497126],"genre_scores_gemma":[0.9997723,0.00000999937,0.000030892457,0.00008130316,0.000041733358,1.469432e-7,0.0000037377913,6.6657316e-7,0.000059192054],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987072,0.00007144692,0.00029514355,0.00014598235,0.00043140742,0.00034882803],"domain_scores_gemma":[0.9991714,0.00007106117,0.00019261148,0.000075920696,0.00007503596,0.00041401762],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003272422,0.00009658277,0.00018698131,0.00012203659,0.00033249572,0.000058047946,0.0003423926,0.000033168442,0.0005742039],"category_scores_gemma":[0.00009848239,0.00005309507,0.00007702939,0.00081727374,0.00073237333,0.00014141932,0.000010111713,0.00015057287,0.0000023057034],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005243499,8.67221e-7,0.9972676,0.0000044597123,0.000013369144,0.000014146474,0.00004447596,0.0010055802,0.00004563617,0.00003204092,0.000020863907,0.0015457056],"study_design_scores_gemma":[0.00011145354,0.00010007176,0.9936269,0.000023305454,0.000018209783,0.00003109697,0.00038237323,0.0033091803,0.00006986175,0.0020971159,0.00015787141,0.00007254748],"about_ca_topic_score_codex":0.7901385,"about_ca_topic_score_gemma":0.9989039,"teacher_disagreement_score":0.2087654,"about_ca_system_score_codex":0.0000023475882,"about_ca_system_score_gemma":0.0010018807,"threshold_uncertainty_score":0.628713},"labels":[],"label_agreement":null},{"id":"W4382199095","doi":"10.1139/cjes-2022-0140","title":"Geodynamic studies of southwestern Canada: subduction zone processes and backarc mantle dynamics","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Lithosphere; Craton; Forearc; Subduction; Mantle (geology); Geophysics; Mantle convection; Mantle wedge; Asthenosphere; Geodynamics; Seismology; Tectonics","score_opus":0.023900741947655294,"score_gpt":0.20802520381651887,"score_spread":0.18412446186886358,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4382199095","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959234,0.0021400088,0.000009222864,0.0013618622,0.000204067,0.000026854448,0.00006588862,0.000003067148,0.00026563308],"genre_scores_gemma":[0.9993643,0.00022101968,0.00013256051,0.00005878685,0.00004279985,9.107189e-8,0.000008315801,8.2518204e-7,0.00017130657],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99901813,0.000028301025,0.00026611902,0.00013380003,0.00026591524,0.00028774608],"domain_scores_gemma":[0.9991474,0.00013976508,0.00014571102,0.00004771841,0.00021444997,0.00030493631],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004279655,0.00008234287,0.00021995619,0.00021733635,0.00022355007,0.000036225356,0.0002066869,0.000026025273,0.00036262895],"category_scores_gemma":[0.0002807878,0.000054588,0.00003386349,0.0009629894,0.0005925876,0.00016552085,0.000007596742,0.00008671003,0.000007569638],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000034297873,0.0000014456798,0.99310726,0.00003988285,0.00002695155,0.000047093905,0.00015270163,0.004023372,0.00001782828,0.00003420715,0.00005931734,0.002486522],"study_design_scores_gemma":[0.00009203147,0.00018970031,0.98395455,0.000054800545,0.000032490243,0.00008178435,0.0041843154,0.0076289712,0.000083875835,0.003272591,0.00030565663,0.00011920947],"about_ca_topic_score_codex":0.7316163,"about_ca_topic_score_gemma":0.9993053,"teacher_disagreement_score":0.267689,"about_ca_system_score_codex":0.0000029580406,"about_ca_system_score_gemma":0.0012238764,"threshold_uncertainty_score":0.39705327},"labels":[],"label_agreement":null},{"id":"W4382199107","doi":"10.1139/cjes-2023-0004","title":"Cheakamus basalt lavas, British Columbia: a Pleistocene record of rapid, continuous eruption within a mountainous drainage system","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Lethbridge; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Lava; Basalt; Geochemistry; Phenocryst; Plagioclase; Lava field; Volcano; Geomorphology; Paleontology; Volcanic rock; Quartz","score_opus":0.021498922590671377,"score_gpt":0.2220641448163132,"score_spread":0.20056522222564183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4382199107","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99056315,0.0011234723,0.0000065457452,0.00029768117,0.001009414,0.00016822874,0.00007874429,0.000017317494,0.0067354403],"genre_scores_gemma":[0.9987272,0.0000586621,0.00033337675,0.00007620655,0.000092993425,8.414151e-7,0.000011568611,0.000003064954,0.0006961027],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978443,0.00029095548,0.00055731897,0.00023663162,0.00038830654,0.0006824801],"domain_scores_gemma":[0.9983859,0.00026383015,0.00037920603,0.00012845664,0.00025470243,0.000587905],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0032096314,0.000097748176,0.00040143408,0.0004305204,0.0006885984,0.00025171158,0.0005569235,0.00013959789,0.001183417],"category_scores_gemma":[0.0003676833,0.00011225126,0.00010114618,0.0011657499,0.0012033615,0.00030311767,0.000008486619,0.00032682298,0.00010530426],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000151437625,0.000003830751,0.99537456,0.0000491192,0.000019793655,0.00100098,0.00022155808,0.00047069284,0.0000049876,0.00005086737,0.0004035835,0.0023848603],"study_design_scores_gemma":[0.00032630863,0.0009379447,0.99123955,0.00016739497,0.000015364696,0.0019927253,0.0020549137,0.0019421204,0.000009911091,0.00034772197,0.00084033073,0.00012571603],"about_ca_topic_score_codex":0.29013664,"about_ca_topic_score_gemma":0.9828181,"teacher_disagreement_score":0.6926815,"about_ca_system_score_codex":0.000002392237,"about_ca_system_score_gemma":0.002036743,"threshold_uncertainty_score":0.99972963},"labels":[],"label_agreement":null},{"id":"W4383217081","doi":"10.1139/cjes-2023-0037","title":"Calibrating geologic strata, dinosaurs, and other fossils at Dinosaur Provincial Park (Alberta, Canada) using a new CA-ID-TIMS U–Pb geochronology","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Toronto; Royal Tyrrell Museum","funders":"National Science Foundation","keywords":"Geochronology; Geology; Biozone; Paleontology; Stratigraphy; Chronostratigraphy; Canyon; Radiometric dating; Range (aeronautics); Palynology; Biostratigraphy; Geomorphology; Sedimentary rock; Tectonics","score_opus":0.03223791580954564,"score_gpt":0.22409102637860998,"score_spread":0.19185311056906434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383217081","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937436,0.0008719802,0.000033476164,0.0012264377,0.00044641728,0.00008868898,0.00010885401,0.000006951194,0.003473602],"genre_scores_gemma":[0.99808276,0.000016256981,0.0007660737,0.000543888,0.00019072507,2.013874e-7,0.0000096908225,0.0000020302975,0.0003883745],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99837416,0.000072351686,0.00037577524,0.00021300957,0.00029707103,0.00066762534],"domain_scores_gemma":[0.9986003,0.00025059783,0.0002459013,0.000079476966,0.000056334477,0.00076740276],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004904446,0.00015108075,0.00023857242,0.00024156664,0.0010337865,0.00021121331,0.00036555468,0.00009013125,0.003223654],"category_scores_gemma":[0.00028736884,0.00010670606,0.000037753496,0.00063038367,0.00050544605,0.00048883783,0.000015730193,0.0001730218,0.000026716349],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005964,0.0000010149049,0.9796085,0.000011657116,0.000010451014,0.00009243739,0.00032698517,0.015522142,0.000022972052,0.00013228944,0.0011952118,0.0030704085],"study_design_scores_gemma":[0.00027978705,0.00047042203,0.9334366,0.00005494755,0.000025656147,0.00066981814,0.0012848245,0.025827127,0.000114536924,0.0021723807,0.0353162,0.00034770125],"about_ca_topic_score_codex":0.96131754,"about_ca_topic_score_gemma":0.9991511,"teacher_disagreement_score":0.046171866,"about_ca_system_score_codex":0.000009743101,"about_ca_system_score_gemma":0.0070773796,"threshold_uncertainty_score":0.99855155},"labels":[],"label_agreement":null},{"id":"W4383223464","doi":"10.1139/cjes-2023-0019","title":"Origin of gases and waters from a hypersaline, carbonate spring on Anticosti Island, Québec, Canada","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"","keywords":"Geology; Calcite; Meteoric water; Geochemistry; Carbonate; Halite; Ordovician; Seawater; Aragonite; Mineralogy; Oceanography; Paleontology; Structural basin; Chemistry","score_opus":0.015460494665828358,"score_gpt":0.2021319387849093,"score_spread":0.18667144411908093,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383223464","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99635273,0.0002963327,0.0000010456936,0.0011387733,0.00033964994,0.000032425018,0.00002170664,0.0000018630792,0.0018154888],"genre_scores_gemma":[0.99940085,0.000080097765,0.00012157598,0.00017407855,0.000029245011,1.6826674e-7,5.284195e-7,0.0000038545095,0.00018957982],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910986,0.000028822666,0.00020200363,0.00013017218,0.00026709758,0.0002620564],"domain_scores_gemma":[0.99934006,0.00008818425,0.00011430264,0.00006601591,0.00001038959,0.00038106364],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031316796,0.00007744865,0.00014277003,0.00011555557,0.00014708942,0.000031271502,0.00020051628,0.000022291573,0.00036397978],"category_scores_gemma":[0.000060384562,0.000053963293,0.000024915198,0.00035476088,0.00031559257,0.00009759178,0.000016409798,0.00010204282,0.000011354497],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010713508,0.000004637168,0.96168727,0.000005439177,0.000024916519,0.00026372078,0.00067042577,0.032452773,0.0024918846,0.00003585558,0.0012404218,0.0011119448],"study_design_scores_gemma":[0.0007176089,0.00045719816,0.89770454,0.00025199866,0.00004887421,0.000053631902,0.0012812483,0.007757666,0.0039915275,0.0003624933,0.086983085,0.00039010055],"about_ca_topic_score_codex":0.98492014,"about_ca_topic_score_gemma":0.996029,"teacher_disagreement_score":0.08574266,"about_ca_system_score_codex":0.000023570492,"about_ca_system_score_gemma":0.0008291276,"threshold_uncertainty_score":0.39853233},"labels":[],"label_agreement":null},{"id":"W4383747295","doi":"10.1139/cjes-2023-0057","title":"Seismicity at the intersection of the Coast Shear Zone and Anahim Volcanic Belt near Bella Coola, British Columbia, Canada","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Induced seismicity; Seismology; Shear zone; Volcanic belt; Volcano; Lithosphere; Batholith; Shear (geology); Transtension; Tectonics; Volcanic rock; Rift; Paleontology","score_opus":0.012155357745607906,"score_gpt":0.17899145319622567,"score_spread":0.16683609545061776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383747295","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950575,0.0016232254,0.0000014593435,0.0013321872,0.0008924063,0.00008628555,0.00013746135,0.0000030933593,0.0008663754],"genre_scores_gemma":[0.99820095,0.00009371995,0.000015742044,0.00046678586,0.000061679835,1.6334148e-7,0.0000019334684,0.0000019250895,0.001157105],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987532,0.00009705479,0.00026411258,0.00014484054,0.00038039757,0.00036042408],"domain_scores_gemma":[0.9991452,0.00019675374,0.00019248627,0.000105438725,0.000104435865,0.00025567488],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0008496574,0.000072284456,0.00017332392,0.000042734697,0.0017122078,0.00025633682,0.00035591493,0.000031081607,0.0007391615],"category_scores_gemma":[0.00016096409,0.00005676095,0.00005941561,0.0007955351,0.0011924925,0.00013884988,0.000023861967,0.00018443301,0.0000051913134],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000022392019,6.603566e-7,0.97729427,0.000005486076,0.000018992949,0.000033492925,0.00031355626,0.00097067974,0.0000037745754,0.0000021955777,0.011782744,0.009571917],"study_design_scores_gemma":[0.000113142,0.00012481619,0.97957987,0.000055497378,0.000013577154,0.0002633162,0.0014480496,0.0009951118,0.000016387641,0.000060155224,0.017259495,0.000070597285],"about_ca_topic_score_codex":0.99585027,"about_ca_topic_score_gemma":0.9999902,"teacher_disagreement_score":0.00950132,"about_ca_system_score_codex":0.0000092353785,"about_ca_system_score_gemma":0.0027793525,"threshold_uncertainty_score":0.9995874},"labels":[],"label_agreement":null},{"id":"W4383747358","doi":"10.1139/cjes-2023-0044","title":"Geochronology, petrogenesis, and mineralization potential of the syenogranites in the Yama fluorite deposit, Tataleng granitic batholith, Qilian Orogen, NW China","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Zircon; Geology; Geochemistry; Petrogenesis; Porphyritic; Batholith; Partial melting; Geochronology; Fluorite; Mineral redox buffer; Crust; Petrology; Quartz; Basalt; Mantle (geology); Tectonics; Paleontology; Chemistry","score_opus":0.010700184207858055,"score_gpt":0.1863286315529299,"score_spread":0.17562844734507183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383747358","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99577475,0.002232713,0.000007436181,0.0015491315,0.00014069476,0.000054607528,0.000028160177,0.0000023947223,0.00021012066],"genre_scores_gemma":[0.9995784,0.000117048774,0.00007968032,0.00014390974,0.000055856184,2.3034441e-7,0.0000077156465,8.6382596e-7,0.00001628579],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989041,0.00014269423,0.00026965496,0.00013028468,0.0002450769,0.00030820223],"domain_scores_gemma":[0.99947566,0.000097042466,0.00012800274,0.00008448695,0.000055069846,0.00015973183],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007392242,0.0000853967,0.00015526554,0.00024234189,0.00036802446,0.000100094156,0.0004697509,0.000040602128,0.000268869],"category_scores_gemma":[0.00017510583,0.000043137614,0.00008878715,0.0012912927,0.000779222,0.0001868326,0.000009687164,0.00012856936,0.000006519319],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026595592,0.0000032337218,0.99449587,0.000008069102,0.00000796963,0.00004918339,0.0003875166,0.0028587729,0.000336001,0.00008035982,0.000018418164,0.001751966],"study_design_scores_gemma":[0.00009320185,0.000097079894,0.9929127,0.000022827113,0.000027772987,0.00018965882,0.0008464001,0.0026907115,0.00021799137,0.0027481965,0.00009451206,0.000058960275],"about_ca_topic_score_codex":0.039869666,"about_ca_topic_score_gemma":0.48320723,"teacher_disagreement_score":0.44333756,"about_ca_system_score_codex":9.0239774e-7,"about_ca_system_score_gemma":0.00015756628,"threshold_uncertainty_score":0.96652395},"labels":[],"label_agreement":null},{"id":"W4383747376","doi":"10.1139/cjes-2023-0025","title":"Coseismic Coulomb stress changes on intraplate faults in the western Quebec seismic zone following three major earthquakes in the past century","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University; Western University; McMaster University","funders":"","keywords":"Intraplate earthquake; Seismology; Geology; Seismic hazard; Fault (geology); Stress field; Seismic gap; Magnitude (astronomy); Tectonics; Stress (linguistics); Finite element method","score_opus":0.026214828880806805,"score_gpt":0.2338805404117114,"score_spread":0.2076657115309046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383747376","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98484224,0.0021547303,0.0000028416803,0.0107755605,0.0007569837,0.00021806,0.000053499592,0.000008003167,0.0011880563],"genre_scores_gemma":[0.99760264,0.00020280483,0.000012094398,0.0018908883,0.0002052336,0.0000017481448,0.0000074518643,0.0000034652253,0.00007365477],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99770755,0.00025227672,0.00036385155,0.00024403121,0.00066346955,0.0007688031],"domain_scores_gemma":[0.99872285,0.0007039097,0.0001711541,0.00018463703,0.000033831682,0.00018363967],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0024567023,0.00019192547,0.00027592893,0.00068596046,0.0005931545,0.00028805647,0.0010059216,0.00006292139,0.00006336058],"category_scores_gemma":[0.000097371914,0.00010504832,0.00010194629,0.001641902,0.0004013782,0.0002619197,0.000008438208,0.0004602018,0.0000787521],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012123771,0.000008132702,0.9597525,0.000008162241,0.00001661494,0.0008575473,0.005331923,0.0048822802,0.0000013775134,0.000036407804,0.0002215418,0.028871382],"study_design_scores_gemma":[0.00034509314,0.00035335502,0.98261577,0.00017899011,0.000011418561,0.000065070075,0.007921293,0.0009195708,0.0000056516346,0.00019262827,0.0072485344,0.00014263832],"about_ca_topic_score_codex":0.12513356,"about_ca_topic_score_gemma":0.98910207,"teacher_disagreement_score":0.86396855,"about_ca_system_score_codex":0.000004646724,"about_ca_system_score_gemma":0.0005161448,"threshold_uncertainty_score":0.88069224},"labels":[],"label_agreement":null},{"id":"W4385268484","doi":"10.1139/cjes-2022-0130","title":"Fluid evolution and ore genesis of Huaduoshan Cu–Mo prospect, Duobaoshan ore field, northeastern China: evidence from fluid inclusions, H–O–S–Pb isotopes, geochronology, and geochemistry","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Geology; Molybdenite; Fluid inclusions; Pyrite; Sphalerite; Quartz; Geochemistry; Chalcopyrite; Meteoric water; Magmatic water; Mineralization (soil science); Mineralogy; Ore genesis; Hydrothermal circulation; Copper; Metallurgy; Materials science","score_opus":0.01402675133476198,"score_gpt":0.20688285635971024,"score_spread":0.19285610502494827,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385268484","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98604393,0.010730049,0.000028285947,0.0026799513,0.000113158836,0.00007813448,0.000106275795,0.000009434472,0.00021079596],"genre_scores_gemma":[0.99844843,0.00072342926,0.00051134854,0.000106918735,0.00012819614,5.414195e-7,0.000015895112,0.0000018114467,0.00006344368],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983906,0.0000708547,0.00042142556,0.00034944588,0.0003244239,0.00044320888],"domain_scores_gemma":[0.99865514,0.00025078768,0.00022512447,0.00012949269,0.0001325854,0.00060688274],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006179162,0.00016680462,0.00034603677,0.0002561752,0.0005000596,0.00008851375,0.00044192208,0.00011835582,0.0017923908],"category_scores_gemma":[0.0005732641,0.0001177751,0.000085749794,0.0007931204,0.0007857024,0.00032960373,0.00005884678,0.00019131172,0.000019194407],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016278238,0.0000041335866,0.99049133,0.000019055233,0.000020891428,0.000048620543,0.00022227429,0.00032570664,0.0033962296,0.000010219572,0.00012828856,0.0053169513],"study_design_scores_gemma":[0.00013377749,0.00032471877,0.98468584,0.0001476797,0.000042491632,0.00008517329,0.0005071241,0.0071309903,0.0018645722,0.004762453,0.00015829201,0.0001568717],"about_ca_topic_score_codex":0.15367359,"about_ca_topic_score_gemma":0.39201507,"teacher_disagreement_score":0.23834148,"about_ca_system_score_codex":0.0000036240647,"about_ca_system_score_gemma":0.00043142532,"threshold_uncertainty_score":0.9991201},"labels":[],"label_agreement":null},{"id":"W4385293128","doi":"10.1139/cjes-2023-0029","title":"<tt>PbIso</tt>: an R package and web app for calculating and plotting Pb isotope data","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; Laurentian University; Geological Survey of Canada; Natural Resources Canada","funders":"Canada First Research Excellence Fund","keywords":"Isotope; Isochron dating; Toolbox; Computer science; Software package; Software; Computational science; Isochron; Geology; Geochemistry; Programming language; Physics; Nuclear physics","score_opus":0.07193956278624461,"score_gpt":0.277902688957588,"score_spread":0.2059631261713434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385293128","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98061365,0.0006207514,0.008088125,0.007325394,0.00045324137,0.00015342524,0.000039478935,0.00003873966,0.0026671698],"genre_scores_gemma":[0.9798683,0.000016221406,0.019420907,0.00019959953,0.00013220312,8.6354544e-7,0.0000024375133,0.0000019382614,0.00035753296],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.998847,0.00003705302,0.00023077565,0.00031255864,0.00016638759,0.00040620824],"domain_scores_gemma":[0.998826,0.00016824594,0.00015858097,0.00025153084,0.000102748956,0.0004928367],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020830012,0.000088332046,0.00014385839,0.00018611898,0.0006770758,0.0004866093,0.0009983333,0.000040489314,0.000009274746],"category_scores_gemma":[0.00071679946,0.00007377593,0.000020610974,0.0004668097,0.0002592929,0.0009898026,0.00014889232,0.00011486374,0.0000016171715],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018142111,0.00004228382,0.61040485,0.0004922846,0.0001268641,0.0012381639,0.016108375,0.0050146417,0.047563754,0.04300268,0.008187708,0.2678002],"study_design_scores_gemma":[0.00084614597,0.00062962156,0.075703695,0.00031460242,0.000024102204,0.001000595,0.0038104244,0.8055983,0.0020612536,0.011137978,0.09823962,0.0006336444],"about_ca_topic_score_codex":0.00039763618,"about_ca_topic_score_gemma":0.008228919,"teacher_disagreement_score":0.80058366,"about_ca_system_score_codex":0.0000023827376,"about_ca_system_score_gemma":0.0006565519,"threshold_uncertainty_score":0.5207588},"labels":[],"label_agreement":null},{"id":"W4385293140","doi":"10.1139/cjes-2023-0065","title":"Pleistocene to Holocene volcanism in the Canadian Cordillera","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Simon Fraser University; University of British Columbia","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Dickinson College; National Science Foundation","keywords":"Geology; Volcano; Shield volcano; Lava; Volcanism; Tephra; Earth science; Caldera; Stratovolcano; Volcanic arc; Rhyolite; Volcanic plateau; Subduction; Volcanic hazards; Geochemistry; Paleontology; Volcanic rock; Tectonics","score_opus":0.030277110376857676,"score_gpt":0.21663844676283778,"score_spread":0.1863613363859801,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385293140","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9693761,0.00023723372,9.494113e-7,0.01580661,0.00021567791,0.000066996225,0.00003099363,0.0000035734818,0.014261858],"genre_scores_gemma":[0.9963125,0.000010850877,0.0001735663,0.003278228,0.000099792196,3.421922e-7,0.000005520588,9.147558e-7,0.00011830761],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984765,0.00007569098,0.00026066537,0.00016381823,0.00037031874,0.00065297994],"domain_scores_gemma":[0.99850553,0.0001330929,0.0000651769,0.00009777936,0.00008499534,0.0011134446],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001183552,0.00009383406,0.00017323403,0.00072234974,0.0005425121,0.00019215932,0.0008189067,0.000046423243,0.004993834],"category_scores_gemma":[0.00034814925,0.000054167955,0.00007373635,0.0026681235,0.00030510462,0.0001325646,0.000004539045,0.00021031719,0.00045915114],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003621139,0.0000024353456,0.98103935,0.0000016566947,0.000006649192,0.0004674321,0.00047314496,0.009877331,0.0000067612496,0.0001775743,0.001955369,0.005988681],"study_design_scores_gemma":[0.00005863194,0.00020558055,0.98726517,0.000012240693,0.0000054632837,0.000049607752,0.00053434586,0.0009898613,0.000020509973,0.00290092,0.007866141,0.000091556714],"about_ca_topic_score_codex":0.88583744,"about_ca_topic_score_gemma":0.99887115,"teacher_disagreement_score":0.113033704,"about_ca_system_score_codex":0.000004141788,"about_ca_system_score_gemma":0.0014539466,"threshold_uncertainty_score":0.9959157},"labels":[],"label_agreement":null},{"id":"W4385446944","doi":"10.1139/cjes-2023-0036","title":"A Jiangshanian (Cambrian; Furongian) trilobite fauna from the Cow Head Group, western Newfoundland","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Trilobite; Fauna; Geology; Paleontology; Bay; Group (periodic table); Taxon; Oceanography; Ecology; Ordovician; Biology","score_opus":0.03655246330316003,"score_gpt":0.2393779456321132,"score_spread":0.20282548232895317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385446944","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9773118,0.005488173,0.00002062902,0.0030577776,0.0012847901,0.00009797155,0.00020515444,0.000014255475,0.012519453],"genre_scores_gemma":[0.998715,0.000069789414,0.0001891644,0.0004808361,0.0003763288,2.692482e-7,0.000008443965,0.0000012157553,0.0001589627],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99826777,0.00017181714,0.00034778795,0.00022542257,0.00036350198,0.0006237127],"domain_scores_gemma":[0.99845415,0.00042285406,0.00021343034,0.00015717339,0.000056237393,0.00069613516],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011435265,0.00015132644,0.00024304705,0.00030819443,0.0009668127,0.0003934276,0.000850281,0.000084490435,0.0006142845],"category_scores_gemma":[0.00012570772,0.000096151634,0.00013977925,0.0009916823,0.00086624356,0.00056953554,0.0000019017916,0.00028042562,0.00016226585],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012516944,0.0000015820235,0.9800224,0.0000014566567,0.000021596277,0.00021699243,0.00048194773,0.000060530267,0.000010125178,0.00007230697,0.00020880584,0.018889781],"study_design_scores_gemma":[0.00027355275,0.00028956926,0.9872376,0.00004919924,0.000015970147,0.00013941305,0.0005015847,0.00030606246,0.000001557955,0.0009574377,0.010097797,0.00013029418],"about_ca_topic_score_codex":0.092388615,"about_ca_topic_score_gemma":0.99047154,"teacher_disagreement_score":0.8980829,"about_ca_system_score_codex":0.0000016212263,"about_ca_system_score_gemma":0.0008634923,"threshold_uncertainty_score":0.9136552},"labels":[],"label_agreement":null},{"id":"W4386054527","doi":"10.1139/cjes-2023-0018","title":"Detrital geochronology of the Cunningham Lake formation: an overlap succession linking Cache Creek terrane to Stikinia at ∼205 Ma","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta; Pacific Institute for the Mathematical Sciences; University of British Columbia; Geological Survey of Canada; Natural Resources Canada","funders":"Commission Géologique du Canada; Natural Resources Canada","keywords":"Terrane; Geology; Zircon; Siliciclastic; Detritus; Geochemistry; Geochronology; Paleontology; Sedimentary rock; Provenance; Permian; Sedimentary depositional environment; Volcanic rock; Carboniferous; Paleozoic; Volcano; Structural basin; Tectonics","score_opus":0.028875993229896712,"score_gpt":0.22644917909394033,"score_spread":0.19757318586404363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386054527","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99576294,0.00021091686,0.000013467787,0.0022214744,0.00033322474,0.000052728312,0.000050984807,0.0000058491028,0.0013483823],"genre_scores_gemma":[0.99896973,0.000009846305,0.00036865965,0.00033222904,0.00010942179,1.8027963e-7,0.000014760698,0.0000010612954,0.00019408407],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99859387,0.00008629796,0.00036133805,0.0001624186,0.00037776536,0.00041832915],"domain_scores_gemma":[0.998897,0.00012906021,0.0002195621,0.00011852591,0.000113479095,0.0005223805],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00077591167,0.00009170452,0.00020327643,0.00027985888,0.00056821434,0.000095564,0.0006820201,0.0000646567,0.0049445014],"category_scores_gemma":[0.00023847923,0.000055349094,0.00010912747,0.0013900489,0.00042200933,0.00037152128,0.000028043934,0.00016498419,0.00006340237],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000065438626,0.0000027092449,0.9874101,0.0000054925717,0.0000058989376,0.000028336668,0.00028262826,0.0075085904,0.00033738566,0.000009552067,0.00018601172,0.0042167003],"study_design_scores_gemma":[0.00010368458,0.00035463882,0.9887215,0.000050973245,0.000013941948,0.00008936891,0.0004171391,0.0023164346,0.00066283095,0.0012202169,0.0059544574,0.00009480164],"about_ca_topic_score_codex":0.018769117,"about_ca_topic_score_gemma":0.890701,"teacher_disagreement_score":0.8719319,"about_ca_system_score_codex":0.000002816728,"about_ca_system_score_gemma":0.0002974451,"threshold_uncertainty_score":0.9959651},"labels":[],"label_agreement":null},{"id":"W4386113138","doi":"10.1139/cjes-2022-0092","title":"Initial development and sedimentary provenance of a middle Paleozoic foreland basin: Clam Bank Formation, western Newfoundland","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Carleton University","funders":"","keywords":"Geology; Provenance; Foreland basin; Paleontology; Marine transgression; Unconformity; Sedimentary rock; Fluvial; Paleozoic; Laurentia; Paleocurrent; Ordovician; Devonian; Siliciclastic; Onlap; Paleosol; Sedimentary depositional environment; Geochemistry; Clastic rock; Structural basin; Loess","score_opus":0.028503792013514412,"score_gpt":0.21420051606768412,"score_spread":0.1856967240541697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386113138","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974034,0.00041066643,0.000011574525,0.0005165091,0.00013985473,0.000048561116,0.00003387901,0.0000026724067,0.0014328735],"genre_scores_gemma":[0.9991947,0.00002435978,0.00041846157,0.00011171261,0.000058596917,2.50624e-7,0.000024479908,9.4325515e-7,0.00016651957],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999013,0.000023664648,0.0003318014,0.00010651829,0.00025154595,0.00027343552],"domain_scores_gemma":[0.9993566,0.000038961593,0.00019107664,0.000047258887,0.000059237194,0.00030681895],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005830669,0.00008076922,0.00015383628,0.00022253119,0.0003164611,0.00008127626,0.00018259457,0.000027917831,0.00037697775],"category_scores_gemma":[0.000027257367,0.000061321785,0.000037530604,0.00048074417,0.00024029578,0.0004614181,0.000005784096,0.00007166529,0.000015796038],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000073932047,0.0000023020636,0.99091035,0.000030820076,0.00001654968,0.000033567783,0.00079856196,0.00047321225,0.000015777941,0.000004457926,0.00013643419,0.007570592],"study_design_scores_gemma":[0.00026357867,0.00016430466,0.98615766,0.000107164975,0.000017349446,0.00012371036,0.001320403,0.0007604741,0.001400026,0.0002833398,0.009292631,0.000109346845],"about_ca_topic_score_codex":0.0067046504,"about_ca_topic_score_gemma":0.41646278,"teacher_disagreement_score":0.40975812,"about_ca_system_score_codex":0.0000022111828,"about_ca_system_score_gemma":0.0005491602,"threshold_uncertainty_score":0.9999098},"labels":[],"label_agreement":null},{"id":"W4386244202","doi":"10.1139/cjes-2023-0080","title":"Where ice gave way to fire: deglacial volcanic activity at the edge of the Coast Mountains in Milbanke Sound, BC","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta; Geological Survey of Canada","funders":"Division of Ocean Sciences; Natural Sciences and Engineering Research Council of Canada; University of Northern British Columbia","keywords":"Geology; Cinder cone; Subaerial; Deglaciation; Geomorphology; Pillow lava; Glacial period; Ice sheet; Lava; Tephra; Paleontology; Geochemistry; Volcano","score_opus":0.033045484244651264,"score_gpt":0.2563083629441888,"score_spread":0.22326287869953754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386244202","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9897868,0.00063516403,0.000001278319,0.0068514706,0.00070654356,0.00012818132,0.00003999642,0.0000024978913,0.0018480644],"genre_scores_gemma":[0.9989293,0.000067583496,0.000011687053,0.00024013045,0.00007102979,5.424446e-7,0.0000011275934,0.0000015095467,0.00067706103],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982917,0.0003243967,0.00024194561,0.00016920401,0.0003597251,0.00061306637],"domain_scores_gemma":[0.9987685,0.00048914476,0.00014249678,0.00016470556,0.00008583518,0.00034930976],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0020198217,0.00009861366,0.00019471,0.00024194655,0.00085278216,0.00005514891,0.0009134297,0.00008217178,0.0010197362],"category_scores_gemma":[0.00035843844,0.000055393524,0.000083550156,0.0014972966,0.0012849426,0.00018368711,0.000030784973,0.00036948445,0.00020192255],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021856116,0.0000024545611,0.9948767,0.0000056598064,0.0000068884196,0.00004873017,0.0008147479,0.002627806,0.000014771416,0.000028273751,0.00082713214,0.0007249909],"study_design_scores_gemma":[0.00012782283,0.00015080966,0.9945949,0.000029478775,0.000005217009,0.00012654807,0.00078575517,0.00069769495,0.0000730124,0.00034947248,0.0029914414,0.000067878624],"about_ca_topic_score_codex":0.02911701,"about_ca_topic_score_gemma":0.99269205,"teacher_disagreement_score":0.963575,"about_ca_system_score_codex":0.0000028799054,"about_ca_system_score_gemma":0.001284875,"threshold_uncertainty_score":0.9998935},"labels":[],"label_agreement":null},{"id":"W4386245070","doi":"10.1139/cjes-2022-0143","title":"The Empress Group in Alberta, Canada","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Alberta Energy; Geological Survey of Canada","funders":"Alberta Innovates","keywords":"Geology; Bedrock; Group (periodic table); Paleontology; Glacial period; Outcrop; Transgressive; Geomorphology; Structural basin; Sedimentary depositional environment","score_opus":0.021628195615213574,"score_gpt":0.22795949061160592,"score_spread":0.20633129499639236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386245070","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9818872,0.00079392927,2.8225975e-7,0.006445269,0.00089221314,0.000041124946,0.0000056356757,0.0000013542742,0.009932996],"genre_scores_gemma":[0.99896544,0.00006613882,0.00001620623,0.00022747122,0.000042782947,1.8771134e-7,0.0000019363931,7.0825024e-7,0.0006791503],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99871033,0.00014175572,0.00021092885,0.0001009255,0.00023945801,0.00059657474],"domain_scores_gemma":[0.9985281,0.0009145138,0.00006978394,0.00007639178,0.000042248477,0.00036890976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001547653,0.00005883879,0.00010900885,0.00024170545,0.00070800586,0.00007770201,0.00061795954,0.000039698647,0.00046906518],"category_scores_gemma":[0.00034978788,0.000036112415,0.000026445025,0.00083884853,0.0006544523,0.00014729051,0.0000044863154,0.00023904942,0.00008334097],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003524455,3.4883527e-7,0.9967683,0.0000012548901,0.000003191631,0.00023940532,0.000083604165,0.0013281252,1.5377464e-7,0.00020413703,0.0008068617,0.0005611131],"study_design_scores_gemma":[0.000076600256,0.00006053654,0.97374994,0.000009567463,0.0000011684429,0.0001239119,0.00039843025,0.0009339816,0.0000031291886,0.0007767746,0.023819385,0.000046572215],"about_ca_topic_score_codex":0.96001714,"about_ca_topic_score_gemma":0.99999064,"teacher_disagreement_score":0.039973482,"about_ca_system_score_codex":5.71761e-7,"about_ca_system_score_gemma":0.0036439258,"threshold_uncertainty_score":0.6464168},"labels":[],"label_agreement":null},{"id":"W4386522085","doi":"10.1139/cjes-2023-0022","title":"Tithonian mafic intrusions in north-central Newfoundland: link to Atlantic rifting?","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Manitoba; Memorial University of Newfoundland; Government of Newfoundland and Labrador; McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada; Memorial University of Newfoundland","keywords":"Geology; Zircon; Mafic; Geochemistry; Magmatism; Rift; Gabbro; Mantle (geology); Paleontology; Igneous rock; Structural basin; Tectonics","score_opus":0.01887463928676678,"score_gpt":0.20963779010345338,"score_spread":0.1907631508166866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386522085","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99123704,0.00013596987,0.000005794969,0.0065516164,0.00033291406,0.000047459744,0.000015371828,0.0000074205086,0.0016664355],"genre_scores_gemma":[0.99869585,0.000026351807,0.00043434516,0.00052953314,0.00018826118,1.469402e-7,0.000009363261,0.000001074998,0.000115076335],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984974,0.000051599363,0.00031848258,0.00018418717,0.00027290097,0.0006754301],"domain_scores_gemma":[0.99860847,0.00012369429,0.00008391173,0.000076283955,0.000057110865,0.0010505401],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00055531965,0.00009711081,0.00020293168,0.0006282262,0.00027767228,0.00013410441,0.0004699203,0.000041581185,0.0041850037],"category_scores_gemma":[0.0003629192,0.0000660168,0.00008283588,0.002769332,0.0002085876,0.00016021714,0.000010206988,0.0002054471,0.0005503924],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000030592057,0.0000017110374,0.9821269,0.0000018566227,0.0000038114993,0.00017770502,0.00020301662,0.01320116,0.000006440668,0.000019582738,0.00012731783,0.0041274563],"study_design_scores_gemma":[0.00008163944,0.00013841965,0.98953414,0.000021792337,0.00000634118,0.000032174325,0.00012073673,0.0024057426,0.0000035734747,0.0009932189,0.0065618544,0.00010038137],"about_ca_topic_score_codex":0.123142116,"about_ca_topic_score_gemma":0.9813474,"teacher_disagreement_score":0.85820526,"about_ca_system_score_codex":0.0000026973796,"about_ca_system_score_gemma":0.00052208477,"threshold_uncertainty_score":0.9967253},"labels":[],"label_agreement":null},{"id":"W4386950580","doi":"10.1139/cjes-2023-0097","title":"A record of the Steptoean Positive Carbon Isotope Excursion (SPICE; Cambrian, Paibian) from the Cow Head Group, western Newfoundland","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Fauna; Geology; Spice; Bay; Paleontology; Excursion; Oceanography; Ecology; Biology","score_opus":0.026904533085210448,"score_gpt":0.23114478826958504,"score_spread":0.20424025518437458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386950580","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.985281,0.0023301383,0.000003713437,0.002491764,0.0013098955,0.00012828616,0.000117041076,0.000004565373,0.0083335955],"genre_scores_gemma":[0.9993697,0.00005572521,0.000075403936,0.0002230447,0.00017495306,2.07541e-7,0.000002716339,9.602187e-7,0.000097335615],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998433,0.000290749,0.0003374864,0.00018044142,0.00035669684,0.00040165815],"domain_scores_gemma":[0.99866474,0.000446298,0.00032084758,0.0001697048,0.00007609667,0.00032230347],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010403077,0.00012227787,0.00021853001,0.00016078283,0.00066321756,0.00012684427,0.0008084156,0.00007461248,0.000111290356],"category_scores_gemma":[0.00011300258,0.00006615377,0.00013140535,0.00079144666,0.0010570383,0.00026709598,0.000003300042,0.0002667434,0.000007398696],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016362343,0.0000020889645,0.98348445,0.0000018147329,0.00001909848,0.00003692988,0.00075036404,0.00004397031,0.00003287293,0.000031575444,0.000053573374,0.015526917],"study_design_scores_gemma":[0.00019368084,0.0003421546,0.9965845,0.00012959451,0.000020743539,0.000044592554,0.00080291816,0.00028611778,0.000012703275,0.00049124594,0.0010026142,0.00008918161],"about_ca_topic_score_codex":0.2396843,"about_ca_topic_score_gemma":0.9914458,"teacher_disagreement_score":0.7517615,"about_ca_system_score_codex":0.0000020495484,"about_ca_system_score_gemma":0.0007670756,"threshold_uncertainty_score":0.7653787},"labels":[],"label_agreement":null},{"id":"W4387302579","doi":"10.1139/cjes-2023-0020","title":"Late Ediacaran–early Cambrian rifting along the northern margin of Laurentia: constraints from the Yelverton Formation of Ellesmere Island, Canada","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Laurentia; Geochemistry; Volcanic rock; Zircon; Geochronology; Dike; Rift; Isochron; Rhyolite; Ordovician; Paleontology; Volcano; Structural basin","score_opus":0.011454908677036206,"score_gpt":0.17253915285718455,"score_spread":0.16108424418014833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387302579","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952718,0.00039444916,0.0000061238297,0.0028552497,0.00022147622,0.000047708712,0.0002907924,0.0000015668146,0.0009108118],"genre_scores_gemma":[0.9996193,0.00002256018,0.000027697977,0.00018515465,0.00007789637,9.987247e-8,0.000019479612,8.249969e-7,0.00004696106],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987476,0.00009304547,0.0003809671,0.00009608644,0.00039757256,0.0002847255],"domain_scores_gemma":[0.9988625,0.00039281676,0.00032703122,0.00008795095,0.00013200917,0.00019770853],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00073642674,0.0000807147,0.00018603209,0.000078071236,0.00031667826,0.000047306938,0.0005119383,0.000033810415,0.001547705],"category_scores_gemma":[0.00018699656,0.000039513132,0.000096229334,0.00066610356,0.0006389403,0.00015206993,0.000007879765,0.00016356896,0.000010516038],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000039610077,8.7785634e-7,0.99202,0.0000026841958,0.000020715672,0.000015849533,0.00037630144,0.0029341264,0.000045261062,0.000010346296,0.0002935649,0.0042762985],"study_design_scores_gemma":[0.00010957198,0.000057743244,0.99406385,0.00004151036,0.00003120627,0.0000091493075,0.001620676,0.0024032488,0.00030000883,0.00055099366,0.0007485646,0.00006345787],"about_ca_topic_score_codex":0.93050015,"about_ca_topic_score_gemma":0.9995807,"teacher_disagreement_score":0.06908054,"about_ca_system_score_codex":0.0000017143572,"about_ca_system_score_gemma":0.00092878763,"threshold_uncertainty_score":0.99936503},"labels":[],"label_agreement":null},{"id":"W4387360350","doi":"10.1139/cjes-2023-0083","title":"New insights on faulting in southwest New Brunswick and northeast Maine based on marine magnetic mapping of the Ministers Island dyke","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University; University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada; Fonds Québécois de la Recherche sur la Nature et les Technologies","keywords":"Geology; Bay; Magnetic anomaly; Tectonics; Seismology; Fault (geology); Paleontology; Oceanography","score_opus":0.02040745108285868,"score_gpt":0.19657280664562324,"score_spread":0.17616535556276455,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387360350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99245256,0.00015928491,0.000011494094,0.0023018345,0.0001876244,0.000061244435,0.0000076291003,0.0000021613084,0.0048161843],"genre_scores_gemma":[0.99890447,0.000014315667,0.00038332943,0.00035948007,0.000043715285,3.5900133e-8,0.0000022228135,9.31705e-7,0.00029151535],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99916005,0.00004059105,0.00025008345,0.00010095032,0.0002165217,0.00023182051],"domain_scores_gemma":[0.9993022,0.00016489543,0.00013358759,0.00006349663,0.000028579561,0.00030723284],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036203396,0.00007711702,0.00012378629,0.00039478205,0.00022938865,0.00008391295,0.00024689615,0.000028781935,0.00058412284],"category_scores_gemma":[0.00014154743,0.00004442221,0.000031205236,0.00095087587,0.0001757184,0.00012681611,0.000005773487,0.0001230461,0.000014828314],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007366595,0.0000013605736,0.97082454,0.0000085771635,0.000001033367,0.000013563269,0.00051993225,0.016065769,0.0000012871793,0.00005579726,0.000050165454,0.012450584],"study_design_scores_gemma":[0.00022229967,0.00038702897,0.9894893,0.00011563575,0.0000023922546,0.000016243075,0.00060893304,0.006257294,0.000006918448,0.0005547966,0.002280127,0.000058993013],"about_ca_topic_score_codex":0.05525859,"about_ca_topic_score_gemma":0.82902324,"teacher_disagreement_score":0.77376467,"about_ca_system_score_codex":0.0000010725594,"about_ca_system_score_gemma":0.0013924403,"threshold_uncertainty_score":0.9510325},"labels":[],"label_agreement":null},{"id":"W4387380806","doi":"10.1139/cjes-2023-0077","title":"Structural geology of the Mount Meager Volcanic Complex, BC, Canada: implications for geothermal energy and geohazards","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Lethbridge; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Mitacs; Natural Resources Canada; Geological Society of America","keywords":"Geology; Volcano; Massif; Geochemistry; Volcanic arc; Structural geology; Geothermal gradient; Seismology; Lineament; Subduction; Geomorphology; Paleontology; Tectonics","score_opus":0.03394532962066612,"score_gpt":0.22607933282606785,"score_spread":0.19213400320540172,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387380806","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99331784,0.0010023803,0.00000653946,0.0041453093,0.00045799755,0.00006098873,0.00016135527,0.0000024576445,0.0008451431],"genre_scores_gemma":[0.99929345,0.000039309336,0.00007911633,0.0003659724,0.00007730508,4.439055e-7,0.0000032607986,0.0000015485901,0.00013960844],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909365,0.000039266703,0.00023960868,0.000116187475,0.00015778585,0.00035349213],"domain_scores_gemma":[0.99919665,0.00021465041,0.00017241304,0.00009078193,0.000121530946,0.00020399127],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035095698,0.00007911037,0.0001713052,0.00012850437,0.00063027465,0.000033787735,0.00034626795,0.000026794638,0.00033898707],"category_scores_gemma":[0.0001098436,0.000049189188,0.000054834385,0.00040553024,0.0006461387,0.000095310956,0.000009253657,0.00005927441,7.408734e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000029706691,4.1768453e-7,0.98740953,0.000004996959,0.000025137691,0.0000033842314,0.00012114907,0.0023871993,0.000027159604,0.0020899682,0.0014022052,0.0065258984],"study_design_scores_gemma":[0.00010833526,0.00008646302,0.9815913,0.0000073141414,0.000010085778,0.000056844026,0.00022556249,0.0017171259,0.000021279007,0.0014447701,0.014669524,0.00006138535],"about_ca_topic_score_codex":0.81298184,"about_ca_topic_score_gemma":0.99875665,"teacher_disagreement_score":0.18577479,"about_ca_system_score_codex":0.0000037563595,"about_ca_system_score_gemma":0.0025586572,"threshold_uncertainty_score":0.48476267},"labels":[],"label_agreement":null},{"id":"W4387769530","doi":"10.1139/cjes-2023-0082","title":"Whitehorse Trough records Late Triassic–Cretaceous accretionary orogenesis in the Northern Canadian Cordillera via detrital mineral thermochronometry","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Dalhousie University; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada","keywords":"Geology; Thermochronology; Zircon; Cretaceous; Paleontology; Terrane; Denudation; Fission track dating; Mesozoic; Trough (economics); Geochemistry; Structural basin; Tectonics","score_opus":0.022602154775701374,"score_gpt":0.20621766298307917,"score_spread":0.1836155082073778,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387769530","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98766613,0.0012731865,0.0000028736026,0.0053252443,0.00031388836,0.00009256423,0.00006948016,0.000006523069,0.0052501354],"genre_scores_gemma":[0.9987071,0.000050442868,0.00014778346,0.00066197733,0.00020162929,8.0415424e-7,0.000031007577,0.0000025539784,0.00019667119],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99790853,0.00019510412,0.00044629243,0.0002530755,0.00042665034,0.00077037106],"domain_scores_gemma":[0.99844295,0.00029217155,0.000160064,0.00013924272,0.00011085517,0.0008546985],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013612342,0.00016832033,0.00029400096,0.0009116236,0.0005206306,0.00018231334,0.00086868304,0.00008961224,0.007688816],"category_scores_gemma":[0.00025740048,0.00010024933,0.00019575263,0.003388551,0.0004427224,0.0002947452,0.000007174137,0.00028363484,0.00022376415],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010487772,0.0000050536883,0.97963756,0.0000022608106,0.000021079888,0.00044515202,0.00026487035,0.0059398175,0.000027764832,0.0000038664275,0.00022307345,0.0134190135],"study_design_scores_gemma":[0.00018603282,0.00025644727,0.9911468,0.000015855047,0.000023289756,0.000120399156,0.0008115323,0.003276082,0.000016602879,0.0015800202,0.002392684,0.00017427986],"about_ca_topic_score_codex":0.43167096,"about_ca_topic_score_gemma":0.9919971,"teacher_disagreement_score":0.56032616,"about_ca_system_score_codex":0.0000090649555,"about_ca_system_score_gemma":0.001383824,"threshold_uncertainty_score":0.9932183},"labels":[],"label_agreement":null},{"id":"W4387823780","doi":"10.1139/cjes-2023-0078","title":"Seismicity and seismic monitoring of Canada’s volcanic zones","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadiana.org; Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Geology; Induced seismicity; Seismology; Volcano","score_opus":0.02697585243542734,"score_gpt":0.21328443844342276,"score_spread":0.18630858600799544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387823780","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933186,0.0025228632,0.000005662018,0.0009799103,0.000748533,0.00003270232,0.000030162644,0.0000041672656,0.002357402],"genre_scores_gemma":[0.99925476,0.00019006548,0.00016445843,0.00008947187,0.00010025806,5.5810133e-8,5.011782e-7,0.0000014047328,0.00019900616],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989132,0.000035506666,0.00024998098,0.00011651669,0.00029716594,0.0003875925],"domain_scores_gemma":[0.9991473,0.00016826877,0.00014996351,0.000060654136,0.00009290411,0.00038092188],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006926354,0.00008430369,0.00019148145,0.00026983963,0.0004392071,0.000046438603,0.00022596597,0.0000254578,0.00017604406],"category_scores_gemma":[0.00016302452,0.00006545674,0.000035304183,0.0005741607,0.00036296333,0.0001874437,0.0000058470364,0.00010884413,0.0000055849064],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000017262809,4.9574965e-7,0.9903532,0.000008470132,0.000013407079,0.000061554325,0.0002554128,0.0030082804,0.0000055284445,0.000027670847,0.0004606662,0.0058035343],"study_design_scores_gemma":[0.00008169852,0.00010670383,0.99263465,0.000050975566,0.0000073479123,0.00006297017,0.0012416645,0.0013219896,0.00016002895,0.0003770269,0.0038771124,0.00007785667],"about_ca_topic_score_codex":0.8359075,"about_ca_topic_score_gemma":0.9908097,"teacher_disagreement_score":0.15490212,"about_ca_system_score_codex":0.0000020874968,"about_ca_system_score_gemma":0.0034251167,"threshold_uncertainty_score":0.607601},"labels":[],"label_agreement":null},{"id":"W4387899735","doi":"10.1139/cjes-2022-0116","title":"Evaluation of carbon dioxide sequestration via interaction with peridotite and peridotite-hosted groundwaters: an experimental case study with Bay of Islands Ophiolite rocks, western Newfoundland, Canada","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"CO2 Sequestration and Geologic Interactions","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Peridotite; Abiogenic petroleum origin; Ophiolite; Dissolution; Carbon dioxide; Seawater; Aqueous solution; Ultramafic rock; Geology; Flux (metallurgy); Groundwater; Mineralogy; Analytical Chemistry (journal); Environmental chemistry; Chemistry; Methane; Geochemistry; Mantle (geology)","score_opus":0.03390566137838817,"score_gpt":0.284817565183338,"score_spread":0.2509119038049498,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387899735","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989786,0.00001980538,0.000027864913,0.00010141237,0.00017077339,0.00020736146,0.0000054073157,0.000003669163,0.0004850665],"genre_scores_gemma":[0.99982625,0.0000018198477,0.000054715678,0.000024697005,0.000029547664,0.000004255038,0.0000041047447,0.0000044631793,0.00005015538],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99855447,0.00017264325,0.00030385063,0.00017934249,0.000611692,0.00017801952],"domain_scores_gemma":[0.9992051,0.000031675205,0.0002854457,0.000098809694,0.00015648117,0.00022248454],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00085733534,0.00010895896,0.00015351428,0.00018457336,0.0002022049,0.00007049936,0.00010895853,0.000023511839,0.00018061855],"category_scores_gemma":[0.000026171223,0.000078382254,0.000016236214,0.0003990446,0.0002746594,0.00076490117,0.000011450399,0.000096378695,6.4962245e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004576452,0.000034777604,0.97156054,0.00000325979,0.000021405222,0.0003258611,0.005149588,0.019360479,0.0031543162,0.0000022935596,0.000003972224,0.0003377463],"study_design_scores_gemma":[0.001124028,0.0056732246,0.9107552,0.000091810885,0.000113306996,0.005105048,0.057937104,0.016388064,0.002418954,0.000018239985,0.00013331235,0.00024170893],"about_ca_topic_score_codex":0.7811905,"about_ca_topic_score_gemma":0.99773365,"teacher_disagreement_score":0.21654318,"about_ca_system_score_codex":0.00011550229,"about_ca_system_score_gemma":0.0009999074,"threshold_uncertainty_score":0.31963354},"labels":[],"label_agreement":null},{"id":"W4387968718","doi":"10.1139/cjes-2022-0072","title":"Tectonic setting and provenance analysis of the Yaojia Formation in the northeastern Songliao Basin, NE China: constraints from sandstone geochemistry, Hf isotopes, and zircon U–Pb chronology","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Zircon; Provenance; Geochemistry; Chronology; Structural basin; Tectonics; Geochronology; China; Isotope geochemistry; Isotope; Paleontology; Archaeology","score_opus":0.009695144238875662,"score_gpt":0.19064813801366787,"score_spread":0.1809529937747922,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387968718","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950804,0.0008801174,0.000016423657,0.0033419745,0.00004240486,0.000057146575,0.00006998962,0.0000017595667,0.0005097631],"genre_scores_gemma":[0.99962795,0.000064730986,0.00010491976,0.0001579773,0.000023793253,2.9412485e-7,0.000010154212,5.1901526e-7,0.000009682846],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990222,0.000087076674,0.00029251399,0.00014856485,0.00018787498,0.0002617704],"domain_scores_gemma":[0.999333,0.00017376062,0.00023226159,0.00008781557,0.000041803603,0.00013134499],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00074706646,0.000081671875,0.00022515525,0.00019642456,0.00023833234,0.00006948621,0.00031370245,0.00004373162,0.0004805841],"category_scores_gemma":[0.00019285796,0.000042112515,0.000071153256,0.001289175,0.00091979204,0.00019156796,0.000012080463,0.00015954436,0.000002073077],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003299014,0.0000021480841,0.98895496,0.0000056232016,0.00003357898,0.000013098008,0.0005931289,0.0015988924,0.00043957625,0.00000961233,0.000009561127,0.00833652],"study_design_scores_gemma":[0.00011594061,0.00005347564,0.9826462,0.000029308172,0.00007600422,0.000028378941,0.001213003,0.013761626,0.0005324912,0.0013692917,0.000116137606,0.0000581452],"about_ca_topic_score_codex":0.03136991,"about_ca_topic_score_gemma":0.52221143,"teacher_disagreement_score":0.4908415,"about_ca_system_score_codex":0.0000014595689,"about_ca_system_score_gemma":0.00016148324,"threshold_uncertainty_score":0.97508025},"labels":[],"label_agreement":null},{"id":"W4388208498","doi":"10.1139/cjes-2023-0059","title":"U–Pb zircon geochronology and geochemistry of the Jurassic magmatic rocks from the region of Cananea and Nacozari, northeastern Sonora, Mexico: timing and composition of the southernmost edge of the Jurassic continental arc","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochronology; Continental arc; Zircon; Igneous rock; Geochemistry; Magmatism; Batholith; Pyroclastic rock; Volcanic rock; Continental margin; Rift; Back-arc basin; Subduction; Paleontology; Tectonics; Volcano","score_opus":0.015340493466054428,"score_gpt":0.1828943433327875,"score_spread":0.16755384986673308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388208498","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950192,0.00094578805,0.0000072067437,0.0035500852,0.00009895855,0.000074134725,0.00013128038,9.366916e-7,0.00017239462],"genre_scores_gemma":[0.9998002,0.000030606436,0.000027636259,0.00008506836,0.000024331564,1.7341975e-7,0.0000028752233,0.0000010531645,0.000028055952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989684,0.00011631932,0.00035153358,0.0001322063,0.00023659435,0.00019489817],"domain_scores_gemma":[0.9988693,0.0002726621,0.00052033324,0.00013969958,0.00007984934,0.000118176235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032543365,0.00009481408,0.00024937873,0.000046328634,0.00031332477,0.000027253443,0.00043884257,0.000051293453,0.00010860024],"category_scores_gemma":[0.00011066727,0.000040364885,0.000090016016,0.00038124344,0.0019693454,0.000069330046,0.00004387064,0.00015506444,4.296693e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000080205955,0.000003506491,0.98945004,0.00002075273,0.000025958516,0.0000019361114,0.00058276387,0.00038567104,0.007561198,0.000008964859,0.000025260602,0.0019259353],"study_design_scores_gemma":[0.00016430649,0.0000642029,0.9837136,0.00015933016,0.00007246842,0.000057212,0.0017717278,0.0028920854,0.009426843,0.0015778159,0.000043974913,0.000056427813],"about_ca_topic_score_codex":0.057185184,"about_ca_topic_score_gemma":0.30133492,"teacher_disagreement_score":0.24414973,"about_ca_system_score_codex":0.0000016263712,"about_ca_system_score_gemma":0.00023643266,"threshold_uncertainty_score":0.9490931},"labels":[],"label_agreement":null},{"id":"W4388210759","doi":"10.1139/cjes-2023-0087","title":"Petrogenesis and metallogenic implications of Eocene–Oligocene magmatism in the Yulong porphyry copper belt, eastern Tibet: a review and analysis of geochronological, geochemical, and Sr–Nd–Pb–Hf isotopic data","year":2023,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Natural Science Foundation of Tibet Autonomous Region","keywords":"Geology; Geochemistry; Magmatism; Crust; Partial melting; Adakite; Underplating; Petrogenesis; Mafic; Petrology; Mantle (geology); Oceanic crust; Subduction; Tectonics; Paleontology","score_opus":0.0961250225118896,"score_gpt":0.2983055057278982,"score_spread":0.20218048321600862,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388210759","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.11481735,0.88298744,0.0000020354364,0.00080692617,0.00001999569,0.00019842581,0.0010623105,0.000002011338,0.00010351865],"genre_scores_gemma":[0.06041117,0.93882567,0.0003250889,0.000198042,0.000022667273,0.0000020795903,0.00019368305,0.0000025464042,0.000019053938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99753094,0.00023807291,0.0010646898,0.00047578235,0.00030098128,0.00038952462],"domain_scores_gemma":[0.9976854,0.0006332868,0.0008004925,0.0003992703,0.00010122016,0.00038034082],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001741713,0.00026004284,0.0018180491,0.0007465024,0.00016971995,0.0000803314,0.0011591149,0.00014159786,0.0006872405],"category_scores_gemma":[0.00042060137,0.00014399498,0.00028271845,0.0025598218,0.0012676225,0.00018445088,0.00008581125,0.0002755807,0.0000031409993],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000039779634,0.000035961617,0.6308947,0.0057432526,0.0019880545,0.00006854408,0.000109486966,0.000032473323,0.000012360839,0.00009914263,0.00025006323,0.36076197],"study_design_scores_gemma":[0.00024181139,0.0003736867,0.9359365,0.004764792,0.018531164,0.0005332659,0.00021964619,0.000505874,0.0000050056606,0.0018040313,0.03642212,0.0006621029],"about_ca_topic_score_codex":0.009618566,"about_ca_topic_score_gemma":0.15434742,"teacher_disagreement_score":0.36009988,"about_ca_system_score_codex":0.0000021847159,"about_ca_system_score_gemma":0.00046767812,"threshold_uncertainty_score":0.9969765},"labels":[],"label_agreement":null},{"id":"W4388898791","doi":"10.1139/cjes-2023-0024","title":"A Permian rhenium–osmium radiometric age for bornite at the Rock Creek deposit, Spar Lake copper–silver district (Montana, USA)—a link to the Sonoma Orogeny and the copper–silver–vanadium Midcontinent Belt?","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Bornite; Geology; Geochemistry; Permian; Isochron; Chalcocite; Chalcopyrite; Paleontology; Structural basin; Copper","score_opus":0.020275806123929794,"score_gpt":0.2075334526475445,"score_spread":0.1872576465236147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388898791","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9484094,0.0043667806,0.000045607863,0.044963814,0.0005312852,0.00040605344,0.0002988087,0.00000884281,0.00096941134],"genre_scores_gemma":[0.99517846,0.00022628091,0.00012067615,0.0022407295,0.00038264837,0.000005627995,0.000033518998,0.0000043501177,0.0018077203],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99735326,0.00019456705,0.0005329631,0.00039638815,0.00055999495,0.00096284645],"domain_scores_gemma":[0.9970081,0.0011724117,0.00025463276,0.00026839587,0.00016402945,0.0011324497],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002088881,0.00024259837,0.0004299151,0.00040920693,0.0024737013,0.00070634956,0.0012782161,0.000082775216,0.0012568714],"category_scores_gemma":[0.0008089301,0.00011139875,0.00033107007,0.0030427817,0.0009239021,0.00021256547,0.000054657747,0.00031565354,0.00014138877],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000910092,0.0000064591377,0.96449995,0.00001057653,0.00011644422,0.00016869821,0.00062496186,0.0078720795,0.000048344882,0.00005099865,0.016272735,0.010237751],"study_design_scores_gemma":[0.0005387426,0.00034075542,0.8818927,0.000022336828,0.00013038017,0.00018378675,0.0006227359,0.0061631594,0.000058919824,0.00042270904,0.10939917,0.00022461133],"about_ca_topic_score_codex":0.07974314,"about_ca_topic_score_gemma":0.96293265,"teacher_disagreement_score":0.8831895,"about_ca_system_score_codex":0.000009793393,"about_ca_system_score_gemma":0.0003966818,"threshold_uncertainty_score":0.99965614},"labels":[],"label_agreement":null},{"id":"W4388899112","doi":"10.1139/cjes-2022-0146","title":"Discussion of “Age and significance of the fire bay assemblage: an Ordovician arc fragment within the Clements Markham belt, northwestern Ellesmere Island, Canada”","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Ordovician; Geology; Bay; Assemblage (archaeology); Paleontology; Fragment (logic); Oceanography; Archaeology; Physical geography; Geography","score_opus":0.019801397392532175,"score_gpt":0.23912946314242003,"score_spread":0.21932806574988786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388899112","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994857,0.00021092093,0.0000010879564,0.0038379643,0.0003813442,0.00012862333,0.000092928596,0.0000012255264,0.000488875],"genre_scores_gemma":[0.9993879,0.00002895724,0.000028547924,0.00023085526,0.000027636917,3.857465e-7,0.0000065554505,0.000001569608,0.0002875537],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99840504,0.0003015188,0.00034343184,0.00015218902,0.00043791663,0.0003599097],"domain_scores_gemma":[0.9989641,0.00019915243,0.0002893821,0.00016606844,0.00007816505,0.00030315205],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014425794,0.00009500403,0.00019116739,0.0001202653,0.0006767367,0.000044140586,0.0006982015,0.00004882804,0.00026132888],"category_scores_gemma":[0.000086323074,0.000042747597,0.000040101277,0.0005885468,0.0011047957,0.0001557056,0.000017925036,0.0002462647,0.000002185931],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009978329,0.0000027680899,0.99679416,0.000010742251,0.000012449798,0.0000682388,0.0007278397,0.0014994085,0.000010665239,0.000021052936,0.00010008854,0.0007425777],"study_design_scores_gemma":[0.0001275973,0.00020237529,0.9950011,0.00005347033,0.000010091535,0.000044789333,0.002481703,0.0011370917,0.00005060876,0.00017524687,0.00065595936,0.00005997674],"about_ca_topic_score_codex":0.39871934,"about_ca_topic_score_gemma":0.9995318,"teacher_disagreement_score":0.6008125,"about_ca_system_score_codex":9.926647e-7,"about_ca_system_score_gemma":0.0021923836,"threshold_uncertainty_score":0.60528463},"labels":[],"label_agreement":null},{"id":"W4388923171","doi":"10.1139/cjes-2023-0039","title":"Reply to the discussion by Hadlari on “age and significance of the fire bay assemblage: an Ordovician arc fragment within the Clements Markham belt, northwestern Ellesmere Island, Canada”","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; St. Francis Xavier University","funders":"","keywords":"Geology; Ordovician; Bay; Assemblage (archaeology); Paleontology; Fragment (logic); Archaeology; Island arc; Paleozoic; Oceanography; Tectonics; Geography; Subduction","score_opus":0.017556603221378288,"score_gpt":0.2378639879401713,"score_spread":0.22030738471879302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388923171","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.956993,0.00015167195,0.0000014186346,0.041555513,0.0004748622,0.00021298254,0.00013088946,0.0000018291129,0.00047783274],"genre_scores_gemma":[0.99548906,0.000018905019,0.000014354007,0.0037200493,0.00004301671,0.0000011090162,0.000009012577,0.0000021047497,0.0007024089],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99811065,0.00040993554,0.000298018,0.00021324476,0.00052502926,0.00044311283],"domain_scores_gemma":[0.9988237,0.00026649525,0.00019847127,0.0002502529,0.00005973412,0.00040133653],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0019438727,0.000114930954,0.000161011,0.00009527614,0.0014151239,0.00011370239,0.0009587129,0.000043297743,0.00019293433],"category_scores_gemma":[0.00013323688,0.000044953427,0.00003705711,0.00064869877,0.00070048665,0.00012568674,0.0000219966,0.00035339716,0.000008800406],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015577032,0.0000029287178,0.9930341,0.0000035416017,0.000011029578,0.00006246281,0.00090269645,0.0023383566,0.0000045774395,0.000015518497,0.0026395023,0.0009696747],"study_design_scores_gemma":[0.000104492254,0.00032670182,0.9813519,0.00004485052,0.000008106357,0.000039198298,0.002398529,0.000764977,0.000029821415,0.000083329345,0.01477433,0.00007374879],"about_ca_topic_score_codex":0.45746997,"about_ca_topic_score_gemma":0.99930733,"teacher_disagreement_score":0.5418374,"about_ca_system_score_codex":0.0000018425699,"about_ca_system_score_gemma":0.0015313338,"threshold_uncertainty_score":0.9998849},"labels":[],"label_agreement":null},{"id":"W4388994894","doi":"10.1139/cjes-2023-0058","title":"Lead isotopes in New England (USA) volcanogenic massive sulfide deposits: implications for metal sources and pre-accretionary tectonostratigraphic terranes","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Waterloo; Geological Survey of Canada; Geoscience BC; Memorial University of Newfoundland","funders":"U.S. Geological Survey; Natural Sciences and Engineering Research Council of Canada; Memorial University of Newfoundland","keywords":"Terrane; Geology; Geochemistry; Isotope; Earth science; Paleontology; Tectonics","score_opus":0.02956544041343857,"score_gpt":0.24412021041195495,"score_spread":0.2145547699985164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388994894","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9801993,0.0010767033,0.0029261147,0.015115381,0.00014486013,0.00014301726,0.000007952094,0.000010085827,0.0003766158],"genre_scores_gemma":[0.99555004,0.000043606215,0.0038155776,0.000099461475,0.00007659488,0.0000053880635,0.0000013170327,0.0000012499179,0.0004067566],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990565,0.000034888122,0.00025437673,0.00021544062,0.0001080003,0.0003307615],"domain_scores_gemma":[0.9991409,0.00019667062,0.00014487964,0.00011057033,0.00010067983,0.0003062875],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055002136,0.00009222073,0.00014497472,0.00040350144,0.00035933935,0.00020936436,0.0005881659,0.000045272976,0.0000107452215],"category_scores_gemma":[0.00028602494,0.00007714298,0.000055202192,0.00089356926,0.00023913445,0.00044998768,0.00002590983,0.00009870291,0.0000013145866],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000099380195,0.00000975063,0.95394933,0.00003860001,0.00003792358,0.0000663959,0.0031015812,0.0034446921,0.0130465645,0.0066525154,0.0005067315,0.019135999],"study_design_scores_gemma":[0.00039630514,0.0002568738,0.96716666,0.00006753776,0.00000934698,0.00035539185,0.0003235779,0.0024923722,0.0024203649,0.018739522,0.007604273,0.0001677963],"about_ca_topic_score_codex":0.0014157438,"about_ca_topic_score_gemma":0.11145705,"teacher_disagreement_score":0.110041305,"about_ca_system_score_codex":0.0000035353976,"about_ca_system_score_gemma":0.0014178357,"threshold_uncertainty_score":0.90475655},"labels":[],"label_agreement":null},{"id":"W4389235330","doi":"10.1139/cjes-2023-0115","title":"Geochronology, geochemistry, and tectonic setting of Ordovician metavolcanic rocks in the Liberty–Orrington belt, Maine: implications for the evolution of peri-Gondwanan arcs in the northern Appalachians","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Directorate for Geosciences","keywords":"Geology; Terrane; Zircon; Geochemistry; Provenance; Volcanic rock; Geochronology; Sedimentary rock; Archean; Volcanic arc; Back-arc basin; Island arc; Continental arc; Subduction; Paleontology; Tectonics; Volcano","score_opus":0.01438415360449778,"score_gpt":0.21474537690231785,"score_spread":0.20036122329782008,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389235330","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98531854,0.0017175648,0.00003956182,0.012240433,0.00003196939,0.00013513598,0.000049375136,0.0000016521459,0.00046576327],"genre_scores_gemma":[0.9996889,0.00005041427,0.00007818992,0.00012471923,0.000034173812,0.000002496356,0.000007936429,9.801392e-7,0.00001216213],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99889606,0.000102731305,0.00035437613,0.00014410578,0.00016464655,0.0003380485],"domain_scores_gemma":[0.99876267,0.00071920984,0.00021699576,0.00014024421,0.00007459128,0.00008631118],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019416012,0.00008550608,0.00018287818,0.00020434913,0.0003537554,0.00004110902,0.00073569646,0.000044991604,0.00010117458],"category_scores_gemma":[0.0003740067,0.00004012347,0.00009267296,0.0014312908,0.0005810138,0.00008043235,0.0000106245725,0.00020109299,0.0000011614285],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000033683468,0.00000494537,0.9897897,0.00000961957,0.000011062044,0.0000017440866,0.000861005,0.0052659656,0.00016716338,0.00009573147,0.000017148677,0.0037724995],"study_design_scores_gemma":[0.00009415777,0.0001199383,0.98081756,0.000018891418,0.00003061551,0.000036936603,0.005970865,0.005782656,0.000029513922,0.006758404,0.0002873435,0.000053098138],"about_ca_topic_score_codex":0.08877097,"about_ca_topic_score_gemma":0.9335669,"teacher_disagreement_score":0.844796,"about_ca_system_score_codex":0.0000042170705,"about_ca_system_score_gemma":0.0004739019,"threshold_uncertainty_score":0.917297},"labels":[],"label_agreement":null},{"id":"W4389245917","doi":"10.1139/cjes-2023-0131","title":"Time to treat the climate and nature crisis as one indivisible global health emergency","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Climate Change and Health Impacts","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology","score_opus":0.04287808101706063,"score_gpt":0.33308658356099907,"score_spread":0.29020850254393843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389245917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92922485,0.00071361737,5.273794e-7,0.06389421,0.00023563576,0.00011980357,0.000056703226,0.0000063676134,0.005748289],"genre_scores_gemma":[0.99014056,0.0010706176,0.00013107389,0.008057685,0.00013776582,0.0000013974905,0.0000015983838,0.000005543239,0.000453733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99852324,0.000050644067,0.00023957214,0.00015931271,0.00035109578,0.00067616964],"domain_scores_gemma":[0.99842095,0.000027042479,0.00012647113,0.00009892004,0.000015705735,0.0013109137],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013560886,0.00008606657,0.0001436707,0.00012406085,0.000848026,0.000092420334,0.0003372986,0.000045315646,0.0043084654],"category_scores_gemma":[0.00010749083,0.00005748264,0.00003305777,0.0013207765,0.00020760052,0.00024589698,0.000053804983,0.00015035056,0.0013066158],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023017916,0.000025547663,0.4889835,0.000042973832,0.000013091336,0.00012069571,0.008396444,0.0007507236,0.00015502276,0.00035350543,0.46699575,0.03413972],"study_design_scores_gemma":[0.00013481555,0.0007361114,0.9641167,0.000059745376,0.000009050956,0.00011100586,0.0017257138,0.00006910426,0.000030324994,0.0015876197,0.031290576,0.00012922646],"about_ca_topic_score_codex":0.00905993,"about_ca_topic_score_gemma":0.11735422,"teacher_disagreement_score":0.4751332,"about_ca_system_score_codex":0.000042807238,"about_ca_system_score_gemma":0.00037156517,"threshold_uncertainty_score":0.999471},"labels":[],"label_agreement":null},{"id":"W4389427316","doi":"10.1139/cjes-2023-0014","title":"Late history of glacial Lake Agassiz in northwestern Ontario, Canada: a case study in the Sandy Lake basin","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"University of Ottawa","keywords":"Geology; Glacial lake; Shelf ice; Varve; Moraine; Shore; Deglaciation; Structural basin; Radiocarbon dating; Glacial period; Geomorphology; Physical geography; Arctic; Oceanography; Paleontology; Sediment","score_opus":0.04194474554863202,"score_gpt":0.23794465327285402,"score_spread":0.195999907724222,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389427316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961042,0.00024585018,7.960914e-8,0.00052926084,0.00065065024,0.00013153668,0.00002372985,0.0000012690278,0.0023134246],"genre_scores_gemma":[0.9993687,0.000005574185,0.000009218716,0.00018531438,0.000028164242,5.476152e-7,0.0000039740885,0.0000010342122,0.00039746435],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99821645,0.0003829337,0.00038824647,0.00015461276,0.0003530436,0.0005047118],"domain_scores_gemma":[0.9990995,0.0003488715,0.0001411404,0.000107695094,0.000057511967,0.0002452988],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0027615516,0.000092462906,0.0002445012,0.00061282626,0.00017663634,0.000025654606,0.00050764333,0.000053268894,0.0015777203],"category_scores_gemma":[0.00008576605,0.00006392427,0.000037631984,0.0007948127,0.0005335328,0.000175754,0.000006278496,0.00042064697,0.000011587178],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000117367745,0.00000818081,0.96613276,0.0000034193913,0.0000049391188,0.02348147,0.008623017,0.001333894,7.839071e-8,0.0000019147246,0.00023717381,0.00016140095],"study_design_scores_gemma":[0.000307681,0.0002647492,0.986803,0.00001602838,0.0000051292186,0.0014899417,0.006025691,0.00013935153,2.2556243e-7,0.00003041796,0.004851636,0.00006615581],"about_ca_topic_score_codex":0.993683,"about_ca_topic_score_gemma":0.99999994,"teacher_disagreement_score":0.021991529,"about_ca_system_score_codex":0.0000065200743,"about_ca_system_score_gemma":0.01388642,"threshold_uncertainty_score":0.999335},"labels":[],"label_agreement":null},{"id":"W4389607633","doi":"10.1139/cjes-2023-0055","title":"Additional <i>Albertosaurus sarcophagus</i> (Tyrannosauridae, Albertosaurinae) material from the Danek bonebed of Edmonton, Alberta, Canada with evidence of cannibalism","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Paleontology; Canyon; Postcrania; Archaeology; Taxon; Geomorphology; Geography","score_opus":0.014419313329835154,"score_gpt":0.19517530894531365,"score_spread":0.1807559956154785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389607633","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9819432,0.0016483467,0.0000017786133,0.0038426707,0.00097052706,0.000108202556,0.009533465,0.0000030964247,0.0019487501],"genre_scores_gemma":[0.998519,0.000051447576,0.00021579488,0.0004061942,0.00021853327,0.0000011258031,0.00033299727,0.000002510597,0.00025241543],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99803144,0.000206392,0.00053064997,0.00022872428,0.00048545454,0.0005173466],"domain_scores_gemma":[0.9963749,0.002367746,0.00049365975,0.00017322705,0.00020311264,0.00038737175],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005241162,0.00016301466,0.00034752412,0.00017674714,0.00040773727,0.00002895541,0.00081845315,0.00008294076,0.015197048],"category_scores_gemma":[0.0005103958,0.00010207853,0.00007187346,0.00072431134,0.0016737514,0.00044029928,0.000009150289,0.00018283524,0.000016533877],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022596797,0.0000066333155,0.9160766,0.00001626014,0.000087559994,0.0002578241,0.00041731275,0.0025528606,0.00009944828,0.00013029414,0.07954086,0.0005883587],"study_design_scores_gemma":[0.00018750395,0.00039046418,0.97462946,0.00020460057,0.00002702173,0.00023362026,0.0002958504,0.00020670604,0.00019651739,0.00027164564,0.023221496,0.00013508886],"about_ca_topic_score_codex":0.9819239,"about_ca_topic_score_gemma":0.999745,"teacher_disagreement_score":0.05855287,"about_ca_system_score_codex":0.0000056888975,"about_ca_system_score_gemma":0.0080774715,"threshold_uncertainty_score":0.99754584},"labels":[],"label_agreement":null},{"id":"W4389775588","doi":"10.1139/cjes-2023-0121","title":"Exploring the Moho beneath the Northern Canadian Cordillera, with seismically constrained gravity inversion","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Geology; Seismology; Inversion (geology); Moho; Geophysics; Tectonics","score_opus":0.04407927044088672,"score_gpt":0.18402963717025422,"score_spread":0.1399503667293675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389775588","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9798521,0.00012256943,0.0000031771767,0.015800154,0.00019339804,0.00006797468,0.000035865876,0.0000064608553,0.0039183027],"genre_scores_gemma":[0.99856323,0.000033739285,0.00007132397,0.001119564,0.00009883253,4.7379424e-7,0.0000068758727,0.0000013666454,0.00010457146],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985514,0.00008959297,0.00021685996,0.00016937296,0.00039390806,0.00057886326],"domain_scores_gemma":[0.9984508,0.00024072579,0.00011112216,0.00012537911,0.00015185078,0.0009200877],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008725037,0.00011777053,0.00016717223,0.00023280384,0.001318051,0.00019142854,0.0007307848,0.000027942837,0.0016846075],"category_scores_gemma":[0.0001731734,0.00004949676,0.00009446541,0.0015042161,0.0011347613,0.0002515436,0.000007463482,0.0002694403,0.00012276488],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000062093427,0.0000014275779,0.97660565,0.0000016343508,0.00002721337,0.00014065785,0.00033597,0.015040008,0.000011028116,0.00006849648,0.00017999913,0.0075816866],"study_design_scores_gemma":[0.000106624684,0.00023537622,0.98192936,0.000025547126,0.000031902393,0.00008104099,0.0021017275,0.0064780903,0.000046644112,0.0017885198,0.007039602,0.000135544],"about_ca_topic_score_codex":0.6418888,"about_ca_topic_score_gemma":0.9943058,"teacher_disagreement_score":0.352417,"about_ca_system_score_codex":0.0000035992846,"about_ca_system_score_gemma":0.0014853509,"threshold_uncertainty_score":0.9999821},"labels":[],"label_agreement":null},{"id":"W4389879440","doi":"10.1139/cjes-2023-0041","title":"Analysis of the late Hirnantian and early Rhuddanian unconformities of southern Ontario: evidence for far-field glacioeustatic effects","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Unconformity; Geology; Paleontology; Ordovician; Chemostratigraphy; Outcrop; Chronostratigraphy; Biozone; Marine transgression; Sequence stratigraphy; Biostratigraphy; Sedimentary rock; Structural basin; Sedimentary depositional environment","score_opus":0.029996483739638223,"score_gpt":0.23954596725164043,"score_spread":0.2095494835120022,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389879440","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964513,0.0021120876,0.000014523631,0.00027905486,0.00024166575,0.00009373565,0.000046478523,0.0000017396704,0.0007593926],"genre_scores_gemma":[0.9996309,0.000026189458,0.00014027362,0.00004031374,0.00001232991,2.3015171e-7,3.0947015e-7,4.3994388e-7,0.00014900629],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990443,0.00006145098,0.00031947717,0.000094681396,0.00021347664,0.00026664147],"domain_scores_gemma":[0.9985039,0.00078741356,0.00032573345,0.000090825306,0.00008912722,0.00020295859],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009185325,0.00008061942,0.00027653514,0.0005232365,0.00029900565,0.000051399467,0.00037557946,0.000049072416,0.00008167671],"category_scores_gemma":[0.00032356364,0.000050461764,0.00017428018,0.00097287656,0.00067030714,0.00025378374,0.0000015390102,0.00010364019,8.098174e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013378265,8.0275265e-7,0.9813615,0.000022519966,0.00010791884,0.0000059919803,0.0039237128,0.000351324,0.000021348122,0.000042758846,0.000010252555,0.014138471],"study_design_scores_gemma":[0.00009940719,0.00042760206,0.9962792,0.00011295238,0.00018306526,0.0000064336746,0.001552313,0.00069344905,0.00012634059,0.0004130148,0.000047123664,0.00005913148],"about_ca_topic_score_codex":0.28190517,"about_ca_topic_score_gemma":0.98478985,"teacher_disagreement_score":0.7028847,"about_ca_system_score_codex":8.5596486e-7,"about_ca_system_score_gemma":0.0010558148,"threshold_uncertainty_score":0.72287667},"labels":[],"label_agreement":null},{"id":"W4389979727","doi":"10.1139/cjes-2023-0089","title":"Sulphide petrology and ore genesis of the stratabound Sheep Creek sediment-hosted Zn–Pb–Ag–Sn prospect, and U–Pb zircon constraints on the timing of magmatism in the northern Alaska Range","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Zircon; Magmatism; Geology; Geochemistry; Sediment; Petrology; Geomorphology; Paleontology; Tectonics","score_opus":0.023655578773407845,"score_gpt":0.2031706038088844,"score_spread":0.17951502503547656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389979727","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930368,0.000615837,0.0000016676447,0.0049118134,0.00006272808,0.000105319654,0.000057420453,0.0000012910575,0.0012071052],"genre_scores_gemma":[0.99948984,0.000057178328,0.00008442594,0.00031283844,0.000026050973,3.490874e-7,0.0000015119396,9.2146684e-7,0.000026900607],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99874467,0.00016735167,0.0003084824,0.00014717993,0.00034653637,0.00028575477],"domain_scores_gemma":[0.99893963,0.0005171973,0.0002151297,0.000101570244,0.00007875385,0.00014772888],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014239559,0.0000914388,0.00021210688,0.00013689641,0.00027736113,0.00007473845,0.00042097564,0.00004043578,0.0011556045],"category_scores_gemma":[0.00026192795,0.000041511463,0.00006063463,0.00072487135,0.0018531873,0.00009100986,0.000011950123,0.00017248666,0.0000049028977],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008419997,0.0000040262817,0.99461097,0.000008215392,0.000016757911,0.000027098617,0.0007112412,0.00043230172,0.0003368898,0.00009945535,0.000045372642,0.0036992668],"study_design_scores_gemma":[0.00014550102,0.00022484275,0.9933815,0.000036032536,0.000022641123,0.000055879882,0.002292795,0.00068221183,0.00023167951,0.002804372,0.00006841547,0.00005414419],"about_ca_topic_score_codex":0.020066671,"about_ca_topic_score_gemma":0.6104906,"teacher_disagreement_score":0.59042394,"about_ca_system_score_codex":0.0000013340965,"about_ca_system_score_gemma":0.00026020358,"threshold_uncertainty_score":0.99975747},"labels":[],"label_agreement":null},{"id":"W4390575497","doi":"10.1139/cjes-2023-0048","title":"LA-ICP-MS zircon U–Pb ages, geochemistry, and genesis of Paleozoic granites from Biezhentao Mountain, Western Tianshan, Xinjiang","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Diorite; Zircon; Geochemistry; Paleozoic; Devonian; Continental arc; Subduction; Orogeny; Late Devonian extinction; Island arc; Continental margin; Igneous rock; Petrology; Paleontology; Tectonics; Carboniferous","score_opus":0.015210575786122747,"score_gpt":0.2001750429677915,"score_spread":0.18496446718166876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390575497","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97070265,0.026373405,0.000037043483,0.00077847927,0.0001579361,0.000030066421,0.0001677544,0.000006141321,0.0017464978],"genre_scores_gemma":[0.9986378,0.00035932864,0.0006158349,0.00010663511,0.00014111002,1.6213826e-7,0.000018076687,0.0000018456304,0.00011919866],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987131,0.00006604886,0.00034610365,0.00025091175,0.00028817082,0.00033567753],"domain_scores_gemma":[0.9988457,0.00030396716,0.00012319654,0.00008741681,0.000073573836,0.00056612847],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005072166,0.0001401699,0.00026899288,0.00023532742,0.0001695293,0.00025073675,0.00036304255,0.00008236914,0.0044679777],"category_scores_gemma":[0.00010634475,0.000095604955,0.00012056439,0.00054726435,0.00074237876,0.00031156125,0.000009796274,0.00018534524,0.000030201554],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000047887143,0.000003784242,0.98661095,0.00003185012,0.000046089095,0.00018783848,0.00025353406,0.00018240469,0.0027436924,0.000016684937,0.000107510896,0.009810857],"study_design_scores_gemma":[0.00014213288,0.00019634486,0.9761453,0.00023035918,0.00010858847,0.00016219557,0.0008500293,0.0018593885,0.0045285444,0.005768211,0.009768673,0.00024018284],"about_ca_topic_score_codex":0.09041469,"about_ca_topic_score_gemma":0.2817941,"teacher_disagreement_score":0.19137943,"about_ca_system_score_codex":0.0000015961131,"about_ca_system_score_gemma":0.00034864017,"threshold_uncertainty_score":0.9964421},"labels":[],"label_agreement":null},{"id":"W4390604863","doi":"10.1139/cjes-2023-0050","title":"Net evolution of subglacial sediment transport in the Quebec–Labrador sector of the Laurentide Ice Sheet","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Newfoundland and Labrador; University of Waterloo; Geological Survey of Canada","funders":"Commission Géologique du Canada; Ministère de l'Énergie et des Ressources Naturelles; Government of Ontario","keywords":"Geology; Ice sheet; Ice stream; Seabed gouging by ice; Glacial period; Greenland ice sheet; Bedrock; Ice divide; Antarctic sea ice; Erosion; Ice-sheet model; Geomorphology; Arctic ice pack; Cryosphere; Physical geography; Oceanography; Sea ice; Geography","score_opus":0.016954709878739045,"score_gpt":0.2245912006066845,"score_spread":0.20763649072794546,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390604863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99167556,0.0034582943,0.0000070840515,0.0022822812,0.000776089,0.00008854919,0.000030943935,0.0000011151807,0.001680086],"genre_scores_gemma":[0.9997023,0.000017475373,0.000037770926,0.0000713024,0.0000619324,1.9441516e-7,0.0000017366887,7.6329894e-7,0.0001065337],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987218,0.00023445894,0.0003073021,0.00010701401,0.0003415692,0.00028789113],"domain_scores_gemma":[0.99941176,0.00022352516,0.00009977455,0.00008993942,0.000056264806,0.00011872568],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019671987,0.00006595187,0.0001472637,0.00028929242,0.00017024647,0.000027836099,0.000605894,0.00005779889,0.0010100333],"category_scores_gemma":[0.000065709995,0.000034634053,0.00008616476,0.0008426332,0.0010443124,0.00020131301,0.0000025251406,0.00027643173,0.0000086742175],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009125107,0.0000035376675,0.99644977,0.00001966563,0.000008781998,0.000045285295,0.0012071963,0.0013951058,0.000011039454,0.00053826836,0.00012414886,0.0001880568],"study_design_scores_gemma":[0.00008040017,0.00012899107,0.99635094,0.00007074992,0.000012093189,0.00011884006,0.0008341076,0.0005221476,0.000067521956,0.0005348257,0.0012411257,0.000038225542],"about_ca_topic_score_codex":0.084039755,"about_ca_topic_score_gemma":0.9793758,"teacher_disagreement_score":0.89533603,"about_ca_system_score_codex":0.0000012674576,"about_ca_system_score_gemma":0.0025540737,"threshold_uncertainty_score":0.9999032},"labels":[],"label_agreement":null},{"id":"W4390769787","doi":"10.1139/cjes-2023-0094","title":"The influence of fluvial and glacial watershed dynamics on Holocene sediment accumulation in Cariboo Lake, Columbia Mountains, British Columbia, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; University of Toronto","funders":"University of Toronto","keywords":"Geology; Deglaciation; Varve; Holocene; Fluvial; Glacial period; Glacier; Physical geography; Oceanography; Sediment; Last Glacial Maximum; Moraine; Hydrology (agriculture); Geomorphology; Geography","score_opus":0.012687663720054506,"score_gpt":0.22492948158669662,"score_spread":0.21224181786664212,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390769787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99746984,0.0007753527,4.096728e-7,0.0007453577,0.00042999195,0.00009060943,0.00009250047,0.0000016205946,0.00039430134],"genre_scores_gemma":[0.9995705,0.00006970143,0.000021242748,0.0001173612,0.00003391758,3.0793223e-7,0.000009429777,0.0000012133228,0.00017636403],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99876004,0.0001309551,0.0002850562,0.00015085288,0.00029213345,0.0003809483],"domain_scores_gemma":[0.999217,0.0003139817,0.000073803705,0.000058761423,0.00008273546,0.00025375522],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011281751,0.00005456316,0.00014653036,0.00010044147,0.0005314573,0.00045789542,0.00027386151,0.00006253803,0.0002338298],"category_scores_gemma":[0.0001558943,0.000057301004,0.000023042521,0.00035628767,0.00082284823,0.0002132109,0.000005993316,0.00026513083,0.0000022388451],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007466616,0.0000013325173,0.99287015,0.000009301043,0.000007913314,0.00026148045,0.00009927047,0.0052168057,5.235182e-7,0.0000149756415,0.00016790426,0.0013428546],"study_design_scores_gemma":[0.00012635301,0.00020004497,0.99332637,0.00006679872,0.000004745038,0.00020245758,0.00023181694,0.004654358,0.0000019588138,0.00030146597,0.000821768,0.00006184225],"about_ca_topic_score_codex":0.97775155,"about_ca_topic_score_gemma":0.99999523,"teacher_disagreement_score":0.022243699,"about_ca_system_score_codex":0.0000044521985,"about_ca_system_score_gemma":0.0034197879,"threshold_uncertainty_score":0.6066557},"labels":[],"label_agreement":null},{"id":"W4390816920","doi":"10.1139/cjes-2023-0085","title":"Sedimentary characteristics, lithofacies, and paleogeography of the Middle–Lower Cambrian in the Tarim Basin, NW China","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Facies; Outcrop; Palaeogeography; Structural basin; Paleontology; Sedimentary rock; Hydrocarbon exploration; Precambrian; Tarim basin; Dolomite; Sedimentary depositional environment; Geomorphology; Geochemistry; Tectonics","score_opus":0.013161491628526936,"score_gpt":0.19557749158997662,"score_spread":0.1824159999614497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390816920","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99309134,0.0030128257,0.000027112677,0.0021125432,0.00064878224,0.000043673124,0.00002105594,0.0000033576932,0.0010393261],"genre_scores_gemma":[0.99952906,0.00015267095,0.000049344686,0.00016620853,0.00006848779,5.1049824e-7,6.8171147e-7,0.0000032457347,0.000029804096],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993006,0.000049656694,0.00022630184,0.00006774431,0.00019735759,0.00015836723],"domain_scores_gemma":[0.99969834,0.000030461537,0.000037363163,0.00008407261,0.000022257751,0.00012750957],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00060745835,0.00006770078,0.00011934603,0.0003281082,0.000113019836,0.00015002566,0.00027311547,0.00002432301,0.000060000544],"category_scores_gemma":[0.000030133262,0.000036339887,0.00008184175,0.00079212146,0.00029142413,0.00017963992,0.000005796575,0.00017791524,9.295219e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057743023,0.000020569847,0.96686465,0.00015693191,0.00021542591,0.00029917026,0.017456185,0.0074850307,0.00067793817,0.0009842424,0.0016951279,0.004138962],"study_design_scores_gemma":[0.00011420109,0.00009383408,0.9478637,0.00028364017,0.00005248801,0.000083974424,0.0020588848,0.015890105,0.0001478084,0.00023553282,0.033037152,0.00013869678],"about_ca_topic_score_codex":0.0026975006,"about_ca_topic_score_gemma":0.051619496,"teacher_disagreement_score":0.048921995,"about_ca_system_score_codex":0.000004445702,"about_ca_system_score_gemma":0.00023671723,"threshold_uncertainty_score":0.96568596},"labels":[],"label_agreement":null},{"id":"W4391161001","doi":"10.1139/cjes-2023-0081","title":"Petrology and lithogeochemistry of Paleozoic alkalic magmatism in the Selwyn Basin, Yukon, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; Geological Survey of Canada; Natural Resources Canada; Arthur B. McDonald-Canadian Astroparticle Physics Research Institute; Thompson Rivers University; Queen's University","funders":"Natural Resources Canada; Society of Economic Geologists Foundation; Geological Society of London","keywords":"Geology; Magmatism; Paleozoic; Geochemistry; Structural basin; Petrology; Geomorphology; Paleontology; Tectonics","score_opus":0.008896760951642105,"score_gpt":0.18196728580421226,"score_spread":0.17307052485257016,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391161001","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9822801,0.008357924,0.0000025953725,0.005614981,0.00014186157,0.000022733651,0.000038578644,0.0000011282087,0.0035401408],"genre_scores_gemma":[0.99912864,0.000072142466,0.00014174337,0.00055755116,0.000054208005,1.1189808e-7,0.0000028826287,5.3137825e-7,0.00004221694],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898595,0.00007781712,0.00027516155,0.00013581461,0.000244668,0.00028061672],"domain_scores_gemma":[0.9992686,0.00029254044,0.000074809774,0.00006254487,0.00004524602,0.00025629037],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008227807,0.000078346035,0.00017960281,0.0001435992,0.00010653057,0.00007660224,0.00034856284,0.000037556118,0.0020628055],"category_scores_gemma":[0.00016311917,0.000043333595,0.00004840412,0.0006472131,0.00048330918,0.00010882376,0.0000038585017,0.00019667803,0.0000031864042],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021287901,0.0000018175471,0.99391794,0.000022069658,0.000011211944,0.00027355857,0.00017423066,0.00037823344,0.00005178205,0.00015579717,0.0004297756,0.0045814277],"study_design_scores_gemma":[0.0000536801,0.00010104372,0.98421365,0.000043014345,0.000017907205,0.00036120976,0.00054300437,0.0016090771,0.00010505077,0.0056731757,0.007204621,0.00007456548],"about_ca_topic_score_codex":0.77538854,"about_ca_topic_score_gemma":0.9955673,"teacher_disagreement_score":0.22017878,"about_ca_system_score_codex":0.0000013669361,"about_ca_system_score_gemma":0.0012644596,"threshold_uncertainty_score":0.99884945},"labels":[],"label_agreement":null},{"id":"W4391164964","doi":"10.1139/cjes-2023-0104","title":"Present-day kinematics of the northwest Moroccan Atlantic Margin from GNSS data: west southwest extrusion at the western end of the High Atlas","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies Worldwide","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geodynamics; GNSS applications; Sinistral and dextral; Tectonics; Subsidence; Seismology; Transpression; Structural basin; Geodesy; Paleontology; Global Positioning System","score_opus":0.02453571985898701,"score_gpt":0.2105987668604106,"score_spread":0.1860630470014236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391164964","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98638684,0.001723021,0.000004417838,0.009216995,0.0013038582,0.00013908352,0.000622197,0.0000027120154,0.00060085056],"genre_scores_gemma":[0.99873066,0.00005763434,0.00004638371,0.00017751363,0.0002754053,2.3485273e-7,0.000015774289,0.0000022048941,0.0006941869],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981071,0.00019258366,0.00045848478,0.00023373759,0.00064255646,0.00036554266],"domain_scores_gemma":[0.9981769,0.00080211245,0.00031196946,0.00040452206,0.0000765638,0.00022798245],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007287215,0.0001488806,0.00027301587,0.000060137416,0.00064436474,0.00013374694,0.0019333027,0.0000409677,0.0010630802],"category_scores_gemma":[0.00019055113,0.000056567995,0.00014139901,0.0007496465,0.0018941856,0.00021968439,0.00015831765,0.00026110324,0.000057326924],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000042579272,0.0000058559144,0.99204123,0.000017283215,0.000030783707,0.00001791399,0.00042175472,0.004808359,0.000030415356,0.000050480387,0.00067612965,0.0018955591],"study_design_scores_gemma":[0.0000731184,0.0000839862,0.9812572,0.0001784344,0.00005541042,0.000022224272,0.00026027762,0.0011074569,0.00009029014,0.0007432731,0.016047502,0.000080846854],"about_ca_topic_score_codex":0.28286657,"about_ca_topic_score_gemma":0.92335296,"teacher_disagreement_score":0.64048636,"about_ca_system_score_codex":0.00000297416,"about_ca_system_score_gemma":0.00050367735,"threshold_uncertainty_score":0.9998501},"labels":[],"label_agreement":null},{"id":"W4391303160","doi":"10.1139/cjes-2023-0095","title":"Origin of a glacially influenced shallow marine chromite placer, Port au Port Bay, western Newfoundland, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Milli Eğitim Bakanliği","keywords":"Geology; Deglaciation; Bay; Fluvial; Oceanography; Chromite; Geochemistry; Sediment; Placer mining; Conglomerate; Progradation; Geomorphology; Holocene; Facies; Sedimentary rock","score_opus":0.019791997449508054,"score_gpt":0.24844101998333845,"score_spread":0.2286490225338304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391303160","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9824243,0.001261105,0.000006155025,0.0017276666,0.0014461309,0.000084583306,0.00004701833,0.000004958963,0.012998068],"genre_scores_gemma":[0.99817866,0.00005385188,0.0001797831,0.00030051544,0.00016410099,2.572347e-7,0.000011684946,0.0000027241329,0.001108443],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979357,0.00010173172,0.0004993668,0.00024569634,0.0005151968,0.00070231105],"domain_scores_gemma":[0.99846345,0.00025821698,0.00016872,0.00013143077,0.00015140027,0.0008267601],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014777337,0.0001539353,0.0003367088,0.00051220256,0.00033455066,0.00012478602,0.0006651404,0.00009933853,0.003582736],"category_scores_gemma":[0.00015024027,0.000117479656,0.00008348769,0.0006776619,0.0009175483,0.00050261704,0.00001283601,0.00038513014,0.000050686533],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019689434,0.000002075249,0.99641114,0.000028948774,0.000035826277,0.0014458548,0.00014621741,0.0009389618,0.00000367398,0.0001057983,0.00012504992,0.0007367769],"study_design_scores_gemma":[0.00016736682,0.0002795395,0.9777314,0.00007789752,0.000017353088,0.0013376204,0.00010435598,0.0004583357,0.000010441311,0.00022936019,0.019457644,0.00012869124],"about_ca_topic_score_codex":0.8918302,"about_ca_topic_score_gemma":0.9998954,"teacher_disagreement_score":0.10806524,"about_ca_system_score_codex":0.000006036606,"about_ca_system_score_gemma":0.029009784,"threshold_uncertainty_score":0.9973281},"labels":[],"label_agreement":null},{"id":"W4391765565","doi":"10.1139/cjes-2023-0049","title":"The Texas Creek landslide, southwestern British Columbia: new ages and implications for the culture history and geomorphology of the mid-Fraser River region","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University; Geological Survey of Canada; Natural Resources Canada; Geoscience BC","funders":"Commission Géologique du Canada; Lawrence Livermore National Laboratory; Natural Resources Canada; Office of Energy Research and Development; Natural Sciences and Engineering Research Council of Canada","keywords":"Landslide; Geology; Canyon; Debris; Population; Holocene; Radiocarbon dating; Tephra; Rockfall; Archaeology; Geomorphology; Physical geography; Volcano; Paleontology; Geography; Oceanography","score_opus":0.01347385679954323,"score_gpt":0.20449340620106018,"score_spread":0.19101954940151694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391765565","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96711606,0.023197947,0.000072717856,0.0081610475,0.00059464405,0.00019022751,0.00004329648,0.0000025864983,0.0006214811],"genre_scores_gemma":[0.9903514,0.0010838032,0.00010457619,0.00031752777,0.00006899847,0.0000012226994,4.3901113e-7,0.0000036866086,0.008068355],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994787,0.000026304326,0.00013314435,0.00010918805,0.00009310301,0.00015955146],"domain_scores_gemma":[0.999535,0.00012272297,0.00008746614,0.00008225285,0.000017486158,0.00015504129],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033018953,0.000040867217,0.00007020278,0.000013428189,0.00059476146,0.0002764444,0.00028366037,0.000043847733,0.00011844626],"category_scores_gemma":[0.000042915373,0.000023266643,0.00004707426,0.00012298665,0.0016054981,0.0001203085,0.00002800359,0.00012532748,0.0000011320166],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000018577587,0.0000019654224,0.85787857,0.0000045969186,0.000020170539,0.0000148596655,0.0010970559,0.000072465176,0.00004287826,0.000042040385,0.12518264,0.015640873],"study_design_scores_gemma":[0.00008620261,0.000053807453,0.59414,0.000033252738,0.000026549422,0.0003265484,0.00018678454,0.00003023652,0.0000019429508,0.00090599543,0.40417632,0.0000323213],"about_ca_topic_score_codex":0.12684402,"about_ca_topic_score_gemma":0.8803338,"teacher_disagreement_score":0.75348973,"about_ca_system_score_codex":0.000015221945,"about_ca_system_score_gemma":0.0002651288,"threshold_uncertainty_score":0.8789704},"labels":[],"label_agreement":null},{"id":"W4391765620","doi":"10.1139/cjes-2023-0101","title":"Ordovician conodont biostratigraphy of northwestern Baffin Island, Nunavut, Canada, with new insights into the age and diachronism of the Ship Point Formation in the Foxe Basin","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Nunavut","funders":"Canadian Northern Economic Development Agency","keywords":"Conodont; Ordovician; Geology; Paleontology; Diachronous; Biostratigraphy; Peninsula; Bay; Range (aeronautics); Structural basin; Oceanography; Archaeology; Geography","score_opus":0.012851359426928867,"score_gpt":0.19380729993043194,"score_spread":0.18095594050350308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391765620","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98152745,0.011803916,0.00001925951,0.0032451137,0.0002088075,0.000119386925,0.000022524635,8.435316e-7,0.0030526968],"genre_scores_gemma":[0.99962044,0.000058796933,0.00006119915,0.00021927904,0.000033154323,2.1885978e-7,7.8920476e-7,5.301782e-7,0.0000056163976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989461,0.0001453518,0.0003154243,0.0001024025,0.00028492283,0.00020582078],"domain_scores_gemma":[0.9993011,0.00024857902,0.00017351758,0.00010819502,0.000034696197,0.00013396119],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00059674744,0.00009675019,0.00015778393,0.000192907,0.00030970105,0.00012458354,0.00047982737,0.000036501362,0.000024573683],"category_scores_gemma":[0.000024181363,0.00004052434,0.000054924385,0.0006249282,0.0009011265,0.00037481613,0.000001223014,0.00021100248,1.7385959e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000090826225,0.000002073241,0.9778455,0.00001781171,0.000015004207,0.000096555224,0.011327416,0.00021680885,0.000011518732,0.00044951125,0.00011400674,0.009894734],"study_design_scores_gemma":[0.000107337815,0.0002368806,0.9944517,0.0001326688,0.000015324858,0.00012310149,0.002886075,0.0002779014,0.00008135094,0.0009662581,0.0006632848,0.000058091024],"about_ca_topic_score_codex":0.8402286,"about_ca_topic_score_gemma":0.9999658,"teacher_disagreement_score":0.15973717,"about_ca_system_score_codex":0.0000020115513,"about_ca_system_score_gemma":0.0026203357,"threshold_uncertainty_score":0.4648363},"labels":[],"label_agreement":null},{"id":"W4391836262","doi":"10.1139/cjes-2023-0091","title":"Laurentide Ice Sheet configuration in southern Ontario, Canada during the last glaciation (MIS 4 to 2) from stratigraphic drilling and LIDAR-based surficial mapping","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"The Scarborough Hospital; University of Waterloo; McMaster University; Geological Survey of Canada; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Ice sheet; Deglaciation; Glacial period; Wisconsin glaciation; Geomorphology; Ice stream; Glacial landform; Lineation; Last Glacial Maximum; Paleontology; Oceanography; Cryosphere; Sea ice; Moraine","score_opus":0.0156719551652222,"score_gpt":0.20186462361736948,"score_spread":0.18619266845214727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391836262","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99620605,0.00089403,0.00001956293,0.001720744,0.0004353093,0.000073172414,0.000032664295,0.0000022582635,0.0006162292],"genre_scores_gemma":[0.9996237,0.0000036658462,0.000085960884,0.00014550086,0.00007018751,2.5594997e-7,0.00000691527,0.0000010218179,0.00006279732],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989693,0.00011809493,0.00022919114,0.00015388863,0.00022531199,0.00030422595],"domain_scores_gemma":[0.9993244,0.0002734854,0.000058774556,0.000048455615,0.000047987436,0.00024689935],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00079336297,0.000075524724,0.00011538903,0.0003246348,0.00044245995,0.00024379222,0.00019444655,0.00004571235,0.0009952269],"category_scores_gemma":[0.00007968328,0.00005410964,0.000022790036,0.00047706952,0.00018755681,0.00018100596,0.0000017072533,0.00027803943,0.000009460493],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000062823797,5.357681e-7,0.9897347,0.000005434887,0.0000067324,0.00011251005,0.002045033,0.007852084,0.00001891755,0.0000133948515,0.0000122813335,0.00019207135],"study_design_scores_gemma":[0.00007680679,0.000042317166,0.99401456,0.0000805737,0.000004173521,0.000024382984,0.002340622,0.0026690192,0.000034113153,0.000098561126,0.0005495984,0.000065259264],"about_ca_topic_score_codex":0.97543335,"about_ca_topic_score_gemma":0.99999285,"teacher_disagreement_score":0.024559487,"about_ca_system_score_codex":0.0000034487507,"about_ca_system_score_gemma":0.004355087,"threshold_uncertainty_score":0.999918},"labels":[],"label_agreement":null},{"id":"W4391846129","doi":"10.1139/cjes-2023-0098","title":"Lílwat oral traditions of Qwelqwelústen (Mount Meager): Indigenous records of volcanic eruption, outburst flood, and landscape change in southwest British Columbia","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Assembly of First Nations; Douglas College","funders":"","keywords":"Mount; Volcano; Geology; Flood myth; Archaeology; Vulcanian eruption; Indigenous; Physical geography; Geomorphology; Seismology; Geography","score_opus":0.033830346308989304,"score_gpt":0.2415551723672205,"score_spread":0.20772482605823117,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391846129","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99015373,0.008091661,0.0000013785766,0.00031034168,0.00052181724,0.000116764466,0.00024685264,0.000003054116,0.000554376],"genre_scores_gemma":[0.99924433,0.0004090261,0.00013192218,0.000047329813,0.000067778165,7.63662e-7,0.000013229564,0.0000020576874,0.00008354712],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986577,0.00013842095,0.000398641,0.00017824123,0.00022270193,0.00040431943],"domain_scores_gemma":[0.999201,0.00016540235,0.00012234863,0.000070557486,0.000100671205,0.00033999555],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001346426,0.000073973686,0.00028459402,0.00048119243,0.00025575026,0.00017904615,0.00028890013,0.000101218975,0.0020388984],"category_scores_gemma":[0.000077061755,0.00008006127,0.00005937683,0.00073680823,0.0009679725,0.0003979133,0.000004031032,0.00027226744,0.000011534518],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003956874,0.0000061364076,0.9958105,0.000040499595,0.000016045049,0.00026609792,0.0019768062,0.00007040229,0.0000020657321,0.000011113324,0.0000653584,0.0017309873],"study_design_scores_gemma":[0.00016595199,0.0004592807,0.99593055,0.00018075711,0.000016735701,0.0009279161,0.00094770023,0.00047747002,0.0000032142812,0.00035495427,0.00045405698,0.000081422666],"about_ca_topic_score_codex":0.3534439,"about_ca_topic_score_gemma":0.9971132,"teacher_disagreement_score":0.64366937,"about_ca_system_score_codex":0.0000013103034,"about_ca_system_score_gemma":0.0011444162,"threshold_uncertainty_score":0.99887335},"labels":[],"label_agreement":null},{"id":"W4391991099","doi":"10.1139/cjes-2023-0118","title":"An ankylosaur femur from the mid-Cretaceous of the peace region of northeastern British Columbia","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal British Columbia Museum; Ocean Networks Canada Society; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Dinosaur Research Institute","keywords":"Cenomanian; Cretaceous; Geology; Fauna; Paleontology; Femur; Archaeology; Geography; Biology","score_opus":0.016893895958757222,"score_gpt":0.20186969128910748,"score_spread":0.18497579533035025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391991099","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9766184,0.019410457,0.000011263227,0.0011414699,0.001152266,0.000055574445,0.00017189064,0.0000024490919,0.0014362454],"genre_scores_gemma":[0.99932295,0.000091976704,0.00008143264,0.00014939684,0.00014603276,8.301837e-8,0.000004164374,0.0000010447237,0.00020291583],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99892634,0.0002268099,0.00027990912,0.00014264928,0.00018827386,0.00023603375],"domain_scores_gemma":[0.99920666,0.0002188109,0.00016935781,0.00013538469,0.00007900457,0.00019080087],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006132358,0.000056513298,0.00015261715,0.000044132565,0.00056287117,0.00020481217,0.0007310147,0.00006358768,0.00060621527],"category_scores_gemma":[0.00008808695,0.00004059878,0.000091165006,0.00035898795,0.0015420979,0.00025801058,0.0000035455105,0.0001835106,0.000005916175],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000044597905,0.0000023529653,0.99173063,0.0000039914958,0.000014768316,0.000079067584,0.00029259737,0.00039514274,0.000017805218,0.000008353925,0.0007414405,0.0067093824],"study_design_scores_gemma":[0.00005419687,0.00021713183,0.98736835,0.00010264429,0.000017914284,0.0007856104,0.0005324247,0.0011663238,0.000007870462,0.0007089888,0.008987084,0.000051454434],"about_ca_topic_score_codex":0.45414606,"about_ca_topic_score_gemma":0.9941537,"teacher_disagreement_score":0.54000765,"about_ca_system_score_codex":0.0000013140361,"about_ca_system_score_gemma":0.0012269033,"threshold_uncertainty_score":0.66376317},"labels":[],"label_agreement":null},{"id":"W4392119359","doi":"10.1139/cjes-2023-0074","title":"Assessing the relative threats from Canadian volcanoes","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismology and Earthquake Studies","field":"Computer Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Volcano; Geology; Seismology","score_opus":0.04633597738785592,"score_gpt":0.28955892754721513,"score_spread":0.2432229501593592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392119359","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.72098815,0.06967636,0.026027067,0.116938375,0.012460911,0.00018151212,0.000028368115,0.000051542866,0.05364768],"genre_scores_gemma":[0.99464554,0.000043491316,0.0035863915,0.0011811825,0.00022848441,5.6483606e-7,2.1976449e-7,0.000003005788,0.0003111149],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99880844,0.00010546896,0.0002131251,0.00021144886,0.00021648635,0.00044501413],"domain_scores_gemma":[0.9987472,0.0004130238,0.000073726005,0.00015711345,0.00011058819,0.00049829035],"candidate_categories":["scholarly_communication"],"consensus_categories":[],"category_scores_codex":[0.0010151416,0.00010257147,0.00013723149,0.00041196367,0.0012046805,0.0012968992,0.0010081884,0.000050498165,0.00009512353],"category_scores_gemma":[0.00017495971,0.00006164844,0.00008236447,0.0008258647,0.00072702306,0.0018710924,0.000023126957,0.00030966214,0.000057166377],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002014216,0.000009026311,0.28012782,0.000012508594,0.00047852605,0.00485989,0.035337504,0.001233009,0.00006546308,0.44148222,0.013825985,0.22256604],"study_design_scores_gemma":[0.00011465141,0.00020734756,0.6725122,0.0003123896,0.00004106447,0.0005530622,0.0021515065,0.006911597,0.00015336148,0.16820286,0.14851795,0.00032202178],"about_ca_topic_score_codex":0.25465718,"about_ca_topic_score_gemma":0.88230014,"teacher_disagreement_score":0.6276429,"about_ca_system_score_codex":0.000018777328,"about_ca_system_score_gemma":0.0067253923,"threshold_uncertainty_score":0.9997398},"labels":[],"label_agreement":null},{"id":"W4393280455","doi":"10.1139/cjes-2023-0119","title":"Description of a tetrapod trackway from the early Carboniferous Bonaventure Formation of New Brunswick, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Rimouski; McGill University","funders":"Fonds Québécois de la Recherche sur la Nature et les Technologies; Universities Space Research Association; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Carboniferous; Tetrapod (structure); Geology; Paleontology; Permian; Viséan; Structural basin","score_opus":0.02841140963878674,"score_gpt":0.20450733923842404,"score_spread":0.1760959295996373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393280455","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97087216,0.0234181,0.0000665641,0.0018733614,0.0011185064,0.000052762625,0.00007495172,0.00000214013,0.002521456],"genre_scores_gemma":[0.99930036,0.000092420414,0.00020870588,0.00013157012,0.00012018413,2.8026584e-8,0.0000030371925,9.0565266e-7,0.00014280304],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990282,0.000060278217,0.00032915975,0.00008500187,0.00030109397,0.00019628766],"domain_scores_gemma":[0.9992964,0.00017198142,0.00016926578,0.00006146434,0.00008705645,0.00021380342],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003933681,0.00007348851,0.00015312206,0.0001295911,0.00018171303,0.00006135689,0.00026899442,0.000038539052,0.00023345395],"category_scores_gemma":[0.00008221446,0.000045477947,0.00006341586,0.00040222894,0.0003251893,0.0003593965,0.0000017031783,0.0001519456,0.0000024751946],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000063694547,0.0000010778674,0.99091166,0.000009130685,0.000024754056,0.000020771635,0.002138483,0.0006282227,0.000015965974,0.00021868157,0.0023657575,0.0036590951],"study_design_scores_gemma":[0.00007563179,0.0001426727,0.9896849,0.000098434226,0.000023815413,0.000048758357,0.0014053,0.00079371117,0.000052843807,0.00040825276,0.0072141993,0.000051492094],"about_ca_topic_score_codex":0.9768774,"about_ca_topic_score_gemma":0.999915,"teacher_disagreement_score":0.028428188,"about_ca_system_score_codex":0.000004168358,"about_ca_system_score_gemma":0.007945536,"threshold_uncertainty_score":0.9976785},"labels":[],"label_agreement":null},{"id":"W4394594037","doi":"10.1139/cjes-2024-0021","title":"Geodynamic setting of Proterozoic massif-type anorthosites in the Eastern Canadian Shield","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Massif; Proterozoic; Shield; Geochemistry; Precambrian; Archean; Baltic Shield; Gneiss; Indian Shield; Petrology; Metamorphic rock; Paleontology; Tectonics","score_opus":0.01662125635954385,"score_gpt":0.2047592385629074,"score_spread":0.18813798220336356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394594037","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9879683,0.0024843356,0.000004989698,0.0040500257,0.00022954906,0.00006548711,0.000021529935,0.000002021237,0.0051737465],"genre_scores_gemma":[0.9993009,0.00001536669,0.00021271652,0.00033421532,0.000069687,1.8251899e-7,0.000004225718,9.29826e-7,0.00006179902],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987763,0.0000867006,0.00030923932,0.00014956942,0.00026066563,0.00041750964],"domain_scores_gemma":[0.9992387,0.00014460448,0.0000812149,0.00007530406,0.000058851285,0.00040128216],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010935648,0.00009088855,0.00016474219,0.00048308496,0.00017381588,0.00019130678,0.00054138206,0.000046995545,0.001670577],"category_scores_gemma":[0.00016047059,0.00005035787,0.00008742635,0.00138959,0.00028687017,0.00023174699,0.0000035208548,0.00024752333,0.000038764698],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000015445414,0.0000013099072,0.99384266,0.000010733222,0.00000740059,0.00013340729,0.00040331786,0.001369148,0.000015609277,0.0000706791,0.000030792104,0.0041133766],"study_design_scores_gemma":[0.0000371348,0.00022017087,0.9744584,0.000107109336,0.000016461341,0.00010080108,0.00073995645,0.01896824,0.000027513746,0.00363597,0.0015923682,0.00009586],"about_ca_topic_score_codex":0.6993735,"about_ca_topic_score_gemma":0.9963016,"teacher_disagreement_score":0.2969281,"about_ca_system_score_codex":0.000002353128,"about_ca_system_score_gemma":0.0011987549,"threshold_uncertainty_score":0.999242},"labels":[],"label_agreement":null},{"id":"W4394802716","doi":"10.1139/cjes-2023-0144","title":"The Devonian clastic wedge and underlying strata of southwestern Canadian Arctic Archipelago: stratigraphic revisions","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada","keywords":"Geology; Devonian; Paleontology; Late Devonian extinction; Ordovician; Clastic rock; Progradation; Outcrop; Orogeny; Reef; Facies; Structural basin; Carboniferous; Oceanography","score_opus":0.06087776532026777,"score_gpt":0.24424659033728788,"score_spread":0.18336882501702012,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394802716","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9785134,0.014599541,0.000047684433,0.0036730017,0.00061196956,0.000084732805,0.000047863206,0.0000031205943,0.0024186878],"genre_scores_gemma":[0.99931765,0.00038238315,0.00014704821,0.00007039188,0.00005604751,1.4416163e-7,0.0000017918594,0.0000011592598,0.000023383602],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989448,0.000065516,0.00028247738,0.0001342762,0.00019680285,0.00037608694],"domain_scores_gemma":[0.99880797,0.00032281733,0.00008144245,0.0000656202,0.00007496024,0.00064716506],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007997812,0.00008654598,0.0001263927,0.000240406,0.000986589,0.0004332063,0.00027225405,0.000034009037,0.0002625374],"category_scores_gemma":[0.00018550352,0.000049295522,0.000051072668,0.0004930378,0.00079472037,0.0002720528,0.000003703287,0.0001905963,0.000013259531],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000056401464,0.0000019396032,0.9186974,0.00005174937,0.000047526137,0.00014251664,0.0020238035,0.002508918,0.000011502593,0.0060824556,0.00011851766,0.07030803],"study_design_scores_gemma":[0.000043408447,0.00032863984,0.98221594,0.00017227956,0.000016805237,0.00009055267,0.003264968,0.0024755294,0.0000012307388,0.00704312,0.004263825,0.00008367753],"about_ca_topic_score_codex":0.3047876,"about_ca_topic_score_gemma":0.9950639,"teacher_disagreement_score":0.6902763,"about_ca_system_score_codex":0.0000022810657,"about_ca_system_score_gemma":0.0016529546,"threshold_uncertainty_score":0.75881445},"labels":[],"label_agreement":null},{"id":"W4394803190","doi":"10.1139/cjes-2023-0107","title":"Geochronology, geochemistry, and Hf isotope of quartz monzonite and diorite in dachaigou, the East Kunlun orogenic belt, China, and their geological significance","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"China Geological Survey","keywords":"Quartz monzonite; Diorite; Geology; Zircon; Geochemistry; Geochronology; Crust; Petrogenesis; Devonian; Pluton; Petrology; Mantle (geology); Tectonics; Paleontology","score_opus":0.01203755676673482,"score_gpt":0.19174545029227552,"score_spread":0.1797078935255407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394803190","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96191514,0.033840608,0.000009835234,0.0032871207,0.00006664815,0.000057986017,0.000043167096,0.0000030916822,0.00077638694],"genre_scores_gemma":[0.9991189,0.00056391594,0.000114670096,0.000100666584,0.000054955177,4.1496014e-7,0.0000028571287,0.0000010123706,0.00004258517],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988642,0.000080551516,0.0003070133,0.00026494183,0.00013235652,0.00035096452],"domain_scores_gemma":[0.99919957,0.00022927031,0.000094606316,0.00007973822,0.00003874085,0.00035810302],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00082195044,0.00013629303,0.00027186883,0.00015370779,0.00021234946,0.0001315492,0.00027813483,0.0000759244,0.00070984877],"category_scores_gemma":[0.00012365473,0.00007037848,0.00005655594,0.00048089417,0.0020388488,0.00017289506,0.000020417814,0.00028834277,0.0000023419943],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009773173,0.0000047524004,0.98195887,0.000024599469,0.00002538462,0.000075894735,0.00074417214,0.00030068352,0.00052642316,0.00020721703,0.000019180277,0.016103076],"study_design_scores_gemma":[0.00012014129,0.0003260747,0.97562075,0.000063874635,0.000022429824,0.00038254596,0.0011695746,0.009789211,0.00026285305,0.01086312,0.0012471514,0.0001322588],"about_ca_topic_score_codex":0.023665976,"about_ca_topic_score_gemma":0.23125671,"teacher_disagreement_score":0.20759073,"about_ca_system_score_codex":0.0000012948898,"about_ca_system_score_gemma":0.00024044041,"threshold_uncertainty_score":0.98283553},"labels":[],"label_agreement":null},{"id":"W4394803265","doi":"10.1139/cjes-2024-0017","title":"Complementarity of Hf isotopes from detrital and igneous zircon: an example from the Central Gneiss Belt, Grenville Province, Ontario","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University; Geological Survey of Canada","funders":"Norges Forskningsråd","keywords":"Zircon; Geology; Igneous rock; Gneiss; Geochemistry; Crust; Overprinting; Geochronology; Context (archaeology); Petrology; Metamorphic rock; Paleontology","score_opus":0.03130138450146026,"score_gpt":0.19460680929107405,"score_spread":0.1633054247896138,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394803265","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99349856,0.004385969,0.00002625111,0.0007665028,0.0002577878,0.000063782674,0.00028059937,0.0000031304003,0.0007173895],"genre_scores_gemma":[0.99829733,0.000025125255,0.0012113091,0.00022350834,0.00014976106,1.10734376e-7,0.000041467578,9.898109e-7,0.00005037267],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987247,0.0000711462,0.00032156863,0.00024333913,0.00028207936,0.0003571555],"domain_scores_gemma":[0.9988949,0.00031037777,0.000103184284,0.00009738462,0.000046083922,0.0005480888],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038284852,0.000112838745,0.00022832038,0.0000900024,0.00033088445,0.00025829053,0.00046270265,0.000038786246,0.012500452],"category_scores_gemma":[0.00003172097,0.000063742926,0.000087368484,0.00028470426,0.00072998786,0.0002812491,0.000013215046,0.00020427397,0.000007834451],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008035699,0.000005967198,0.99247724,0.0000022401848,0.000035445995,0.00007842928,0.00090862426,0.00017670923,0.00014115161,0.000078997306,0.0001306522,0.0059565105],"study_design_scores_gemma":[0.00011923543,0.0003416748,0.97778326,0.000037898015,0.00005190651,0.000030866515,0.000902579,0.00096256856,0.00027187122,0.008551028,0.010833545,0.000113537986],"about_ca_topic_score_codex":0.9762365,"about_ca_topic_score_gemma":0.9988309,"teacher_disagreement_score":0.022594407,"about_ca_system_score_codex":0.0000038725416,"about_ca_system_score_gemma":0.00091584586,"threshold_uncertainty_score":0.98840225},"labels":[],"label_agreement":null},{"id":"W4394903752","doi":"10.1139/cjes-2023-0054","title":"Facies analysis for the Neoarchean Itchen and Sherpa formations of the Winter Lake greenstone belt, Slave craton, Northwest Territories, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Mount Royal University; Government of Northwest Territories; University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Craton; Facies; Geochemistry; Foreland basin; Archean; Detritus; Banded iron formation; Sedimentary depositional environment; Sedimentary rock; Geomorphology; Tectonics; Structural basin; Paleontology","score_opus":0.01861703725664142,"score_gpt":0.20807861348240803,"score_spread":0.1894615762257666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394903752","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9828958,0.0044699386,0.00042097524,0.00926071,0.0006917108,0.00013425946,0.0012668013,0.000002901775,0.00085689843],"genre_scores_gemma":[0.9993925,0.000035549216,0.00019057514,0.0002058104,0.000055632416,4.9794653e-7,0.0000147089195,7.4555504e-7,0.00010397484],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99919695,0.000026771868,0.00026872996,0.00007874853,0.00021828833,0.00021051215],"domain_scores_gemma":[0.99918056,0.00032461176,0.000103969505,0.00007601787,0.00013822287,0.00017659404],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005128235,0.00007238333,0.00012786173,0.00014641733,0.00070323836,0.00022053077,0.00036697678,0.000023648685,0.00043318886],"category_scores_gemma":[0.00010981451,0.000033681285,0.000082271625,0.00085581734,0.00057962304,0.00037763928,0.000006278052,0.00010989676,5.446177e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000019210406,7.7929917e-7,0.9870339,0.000018367204,0.00007436241,0.00000254655,0.0008985098,0.0047649923,6.9956684e-7,0.00018022304,0.00027747516,0.006746228],"study_design_scores_gemma":[0.000034294266,0.00007494328,0.9350461,0.0000232577,0.00008857152,0.00003430838,0.0014917703,0.0044394764,0.000018591074,0.00050307234,0.058190458,0.000055210574],"about_ca_topic_score_codex":0.8243767,"about_ca_topic_score_gemma":0.99989516,"teacher_disagreement_score":0.17551848,"about_ca_system_score_codex":0.0000021760816,"about_ca_system_score_gemma":0.001992381,"threshold_uncertainty_score":0.54088116},"labels":[],"label_agreement":null},{"id":"W4395448601","doi":"10.1139/cjes-2024-0029","title":"Provenance and depositional age of metasedimentary rocks in the Frontenac terrane (Grenville Province, Ontario)","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Colgate University","keywords":"Geology; Provenance; Terrane; Sedimentary depositional environment; Geochemistry; Pluton; Petrology; Paleontology; Tectonics","score_opus":0.015816699237167667,"score_gpt":0.202365734870542,"score_spread":0.18654903563337433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4395448601","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95237345,0.007091146,0.0038235735,0.01604289,0.0006726096,0.00020481227,0.000011368489,0.0000056238578,0.019774523],"genre_scores_gemma":[0.9964045,0.0000058515875,0.0029614249,0.00024585726,0.000030566218,0.0000011005556,5.583285e-7,4.987135e-7,0.0003496109],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99922717,0.000036271224,0.00020617401,0.00013941419,0.00020502809,0.00018596454],"domain_scores_gemma":[0.9996361,0.000063859894,0.000071958115,0.0000837361,0.000034831945,0.00010948763],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00075761246,0.00006156906,0.000103919934,0.00013758791,0.00012213083,0.00014969031,0.0005518607,0.00002116338,0.00003960025],"category_scores_gemma":[0.000033091423,0.0000380321,0.000036309477,0.000267322,0.00025551044,0.00031524606,0.000021469828,0.00015954576,6.612063e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005082116,0.00025549327,0.7140334,0.00068768754,0.00028643798,0.020561816,0.06503155,0.0116147585,0.019501114,0.09513509,0.013684413,0.059157368],"study_design_scores_gemma":[0.0010315431,0.001816363,0.55591697,0.0019605488,0.00006209568,0.0063792523,0.0028199013,0.016470589,0.008357661,0.050769843,0.35366666,0.0007485718],"about_ca_topic_score_codex":0.028068278,"about_ca_topic_score_gemma":0.46045664,"teacher_disagreement_score":0.43238837,"about_ca_system_score_codex":0.0000092495175,"about_ca_system_score_gemma":0.0015350699,"threshold_uncertainty_score":0.9784039},"labels":[],"label_agreement":null},{"id":"W4396571636","doi":"10.1139/cjes-2023-0102","title":"Survival of mammoths (<i>Mammuthus</i> sp.) into the Late Pleistocene in Southwestern British Columbia (Vancouver Island), Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Pleistocene-Era Hominins and Archaeology","field":"Social Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia; Royal British Columbia Museum; University of Victoria; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK","keywords":"Pleistocene; Geology; Archaeology; Quaternary; Paleontology; Geography","score_opus":0.012358611509760992,"score_gpt":0.2316096669296708,"score_spread":0.2192510554199098,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396571636","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905434,0.0015228176,0.00000919651,0.0016380718,0.0030530733,0.000099788034,0.00005699517,0.0000039430633,0.0030727081],"genre_scores_gemma":[0.99715143,0.00008451517,0.00007137342,0.00028558326,0.00022862713,0.0000012462274,4.5266643e-7,0.000006810928,0.0021699704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99803287,0.00022622461,0.0004412278,0.00016824726,0.0005844969,0.0005469473],"domain_scores_gemma":[0.99892634,0.0002551403,0.0001625164,0.00009690599,0.00015412923,0.00040496874],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001967287,0.00008434265,0.0002608113,0.00015669072,0.0005678991,0.0003985473,0.00085328356,0.00006337522,0.00042242964],"category_scores_gemma":[0.000232888,0.000085033935,0.00007845114,0.00076611654,0.0019390692,0.0002728532,0.000030681837,0.0002611355,0.0000019612726],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006156131,0.000007309666,0.96479505,0.000014690275,0.000024647776,0.0010198386,0.016718434,0.00018875604,0.00001541447,0.0004064505,0.008280193,0.008523054],"study_design_scores_gemma":[0.00040063646,0.00021408945,0.8198782,0.0003903369,0.000021252621,0.00006579153,0.01464752,0.00010683862,0.000021617117,0.0034616538,0.16049659,0.00029541602],"about_ca_topic_score_codex":0.994571,"about_ca_topic_score_gemma":0.99999976,"teacher_disagreement_score":0.1522164,"about_ca_system_score_codex":0.000070043374,"about_ca_system_score_gemma":0.017481465,"threshold_uncertainty_score":0.9880885},"labels":[],"label_agreement":null},{"id":"W4396601743","doi":"10.1139/cjes-2024-0044","title":"Conjugate shear model for emplacement of mid-crustal plutons during dextral transpression, southern Nova Scotia, Canada: tectonic and petrological consequences","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada; St. Francis Xavier University","keywords":"Sinistral and dextral; Geology; Pluton; Transpression; Nova scotia; Shear zone; Shear (geology); Tectonics; Seismology; Geochemistry; Paleontology; Oceanography","score_opus":0.02466234603481869,"score_gpt":0.2132696493949746,"score_spread":0.1886073033601559,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396601743","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99281806,0.003966538,0.00019440288,0.0021693676,0.00017521836,0.000075933924,0.00032741314,0.0000039087486,0.00026913141],"genre_scores_gemma":[0.99879295,0.00002300007,0.00092274375,0.000115969735,0.000042063162,2.3400221e-7,0.0000039501942,0.0000014092249,0.00009765442],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99862736,0.000036763176,0.00038129877,0.00022821622,0.00028615445,0.0004402058],"domain_scores_gemma":[0.99904996,0.00016661534,0.00009886527,0.000051370975,0.00008594856,0.0005472673],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047424983,0.0001258015,0.00027390232,0.00016425486,0.00024038728,0.00009483452,0.00026753583,0.00005225398,0.0020450428],"category_scores_gemma":[0.000094892916,0.00007786534,0.000109432345,0.00028108383,0.0010422835,0.00014762416,0.000004907201,0.0001644028,0.0000032546975],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013376772,0.00001464366,0.80258286,0.00017822109,0.00016391031,0.00034236486,0.0009241842,0.18752085,0.005658166,0.0003170538,0.0003042269,0.0018597607],"study_design_scores_gemma":[0.0014236462,0.0019202924,0.4296005,0.00065714953,0.00039319447,0.0009402727,0.0036036687,0.53038305,0.01070143,0.017727736,0.001617424,0.0010316476],"about_ca_topic_score_codex":0.5746463,"about_ca_topic_score_gemma":0.9902782,"teacher_disagreement_score":0.4156319,"about_ca_system_score_codex":0.0000040385466,"about_ca_system_score_gemma":0.002352051,"threshold_uncertainty_score":0.9988672},"labels":[],"label_agreement":null},{"id":"W4396665229","doi":"10.1139/cjes-2023-0100","title":"Submarine geomorphology of a glaciated active margin, British Columbia, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Submarine; Geomorphology; Margin (machine learning); Physical geography; Oceanography; Geography","score_opus":0.01355103727533107,"score_gpt":0.20834932224920158,"score_spread":0.1947982849738705,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396665229","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887553,0.00383365,0.0000022798686,0.0007660275,0.0010602381,0.000060488423,0.00017479464,0.000002870295,0.0053443476],"genre_scores_gemma":[0.9986832,0.00007094041,0.00010234746,0.00014427645,0.000052077958,1.7296657e-7,0.000015466905,0.0000015692525,0.0009299114],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986105,0.00013350967,0.0003048645,0.00017469801,0.00026288282,0.0005135764],"domain_scores_gemma":[0.9988621,0.00029674024,0.00010698361,0.00006959031,0.00017650807,0.0004881192],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008093604,0.00006735162,0.00024501304,0.00021237944,0.00030084522,0.00016661332,0.00042569663,0.00008139722,0.01685843],"category_scores_gemma":[0.00022166985,0.00007655672,0.000055622622,0.0006798197,0.0011160162,0.00022213593,0.0000061021847,0.0003253148,0.000023351862],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005654677,0.0000017356701,0.9936273,0.000014341617,0.000029062516,0.002050915,0.000053764597,0.00011952126,0.000002211611,0.0000169687,0.0013102344,0.0027682548],"study_design_scores_gemma":[0.00011140606,0.00023844856,0.9818298,0.000056170862,0.000011799102,0.0027946937,0.00020011315,0.00034067314,0.000016278307,0.00046623728,0.013853309,0.000081023005],"about_ca_topic_score_codex":0.9943005,"about_ca_topic_score_gemma":0.9999915,"teacher_disagreement_score":0.016835079,"about_ca_system_score_codex":0.0000015426123,"about_ca_system_score_gemma":0.009797477,"threshold_uncertainty_score":0.99581605},"labels":[],"label_agreement":null},{"id":"W4396688357","doi":"10.1139/cjes-2024-0030","title":"A primary evaporite weld revealed in the late Paleozoic Antigonish sub-basin of Nova Scotia","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta","keywords":"Nova scotia; Evaporite; Geology; Paleozoic; Structural basin; Nova (rocket); Geochemistry; Paleontology; Seismology; Mining engineering; Oceanography","score_opus":0.017600412908878215,"score_gpt":0.20544093996518303,"score_spread":0.18784052705630483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396688357","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98488975,0.0058777663,0.000004150515,0.003387128,0.00031635328,0.00005170922,0.000026567497,0.0000026229761,0.005443976],"genre_scores_gemma":[0.999082,0.00008027343,0.00018583429,0.0004981207,0.00008691955,5.2082097e-8,0.0000042964434,8.7403055e-7,0.00006162107],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99856716,0.00014314624,0.00040731282,0.0001524352,0.0003692262,0.0003607189],"domain_scores_gemma":[0.999136,0.00032702694,0.000116199226,0.00009095172,0.00006817316,0.0002616982],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0022160262,0.00009888185,0.00024359117,0.0003558163,0.000106594285,0.00015977278,0.00056577084,0.000047420373,0.0027199679],"category_scores_gemma":[0.0001877225,0.00005369073,0.00014376923,0.0015757439,0.000595111,0.00025750196,0.000004667295,0.0002674337,0.000063422725],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000059436493,0.000004420405,0.99505675,0.00002162008,0.000011272102,0.00020689378,0.00019890229,0.0008191283,0.00014779773,0.000048185633,0.00021279544,0.0032663206],"study_design_scores_gemma":[0.00006965283,0.00017992858,0.99370164,0.00012766138,0.00002137901,0.00009478174,0.00013887239,0.0005083903,0.00016584204,0.003021221,0.0018865063,0.00008415562],"about_ca_topic_score_codex":0.047142483,"about_ca_topic_score_gemma":0.68029827,"teacher_disagreement_score":0.63315576,"about_ca_system_score_codex":0.0000014391954,"about_ca_system_score_gemma":0.00074393285,"threshold_uncertainty_score":0.99819165},"labels":[],"label_agreement":null},{"id":"W4398159283","doi":"10.1139/cjes-2023-0120","title":"Polyphase formation of a Neoarchean auriferous fault zone network in the Michipicoten greenstone belt, southern Superior craton","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Laurentian University","funders":"Canada First Research Excellence Fund","keywords":"Geology; Greenstone belt; Polyphase system; Craton; Geochemistry; Archean; Banded iron formation; Petrology; Seismology; Tectonics","score_opus":0.020179126811274515,"score_gpt":0.23035045923898478,"score_spread":0.21017133242771027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398159283","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97358674,0.0021862478,0.0119368555,0.010161596,0.00038913844,0.00008742634,0.0000057965635,0.000007959996,0.0016382572],"genre_scores_gemma":[0.997279,0.000007129223,0.0021653043,0.00026752325,0.00013252856,8.101017e-7,5.8873127e-7,0.0000011443886,0.0001459679],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99879646,0.00009742288,0.00034339225,0.0001382746,0.00026896136,0.00035548364],"domain_scores_gemma":[0.99935824,0.0001018506,0.00011583258,0.00015202178,0.00009349737,0.00017858905],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017128342,0.000086055355,0.00013962944,0.00021146987,0.00021303585,0.000245744,0.0009687542,0.00004344947,0.00002377405],"category_scores_gemma":[0.0000924897,0.000056466743,0.00006783461,0.0009988314,0.0003019086,0.00048694265,0.00002421199,0.00022904121,0.0000050605713],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007751298,0.0001946668,0.12120364,0.00067358825,0.00014266293,0.005974237,0.28993866,0.12311632,0.017475631,0.059929807,0.0069521177,0.37432116],"study_design_scores_gemma":[0.002952119,0.0044399407,0.15037958,0.0045968527,0.00012887594,0.016024163,0.048858542,0.57529515,0.00976243,0.07459614,0.11076985,0.002196339],"about_ca_topic_score_codex":0.0052452846,"about_ca_topic_score_gemma":0.10976124,"teacher_disagreement_score":0.45217887,"about_ca_system_score_codex":0.000006792122,"about_ca_system_score_gemma":0.00094684225,"threshold_uncertainty_score":0.9064833},"labels":[],"label_agreement":null},{"id":"W4398190325","doi":"10.1139/cjes-2023-0122","title":"Geochemistry, geochronology, and radiogenic isotopes of the Balmer and Confederation assemblages of the Laird Lake Area, Red Lake greenstone belt, Canada: implications for Archean tectonic evolution","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia; Lakehead University","funders":"Mitacs","keywords":"Geology; Geochemistry; Felsic; Mafic; Porphyritic; Volcanic arc; Volcanic rock; Greenstone belt; Island arc; Archean; Batholith; Conglomerate; Proterozoic; Volcano; Paleontology; Subduction; Sedimentary rock; Tectonics","score_opus":0.01568544130826207,"score_gpt":0.20209303411078605,"score_spread":0.18640759280252397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398190325","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9832501,0.0031536515,0.000040155563,0.012656111,0.0001040273,0.00010264307,0.00022762177,0.0000015339746,0.00046418305],"genre_scores_gemma":[0.99969774,0.000039632814,0.00009777318,0.00006194609,0.000032676075,7.0046724e-7,0.0000075428693,8.156819e-7,0.00006114008],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99923694,0.000048621987,0.00024677216,0.00014262591,0.00013109786,0.00019396564],"domain_scores_gemma":[0.9993137,0.00018480165,0.00014531608,0.00008822712,0.00011754604,0.00015038806],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037800023,0.000075252756,0.00015496861,0.00006137052,0.0003544453,0.00004463967,0.0002454312,0.000044155837,0.00029758873],"category_scores_gemma":[0.0002142604,0.00003980417,0.00007566167,0.00025667576,0.000856591,0.00008570563,0.000010939263,0.000109768254,1.16084145e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000034673028,0.000002381602,0.99294996,0.000025299669,0.00003476447,0.000001172992,0.000041442076,0.00037956785,0.0028567037,0.00035699076,0.0002948332,0.0030534414],"study_design_scores_gemma":[0.00008443814,0.000065052765,0.9905196,0.000042914657,0.00004951133,0.00009501513,0.00009240114,0.0017231386,0.001490449,0.0044438085,0.0013390159,0.00005467686],"about_ca_topic_score_codex":0.29928687,"about_ca_topic_score_gemma":0.99835324,"teacher_disagreement_score":0.6990664,"about_ca_system_score_codex":0.0000033437163,"about_ca_system_score_gemma":0.0014246163,"threshold_uncertainty_score":0.70537925},"labels":[],"label_agreement":null},{"id":"W4399120301","doi":"10.1139/cjes-2024-0002","title":"Petrogenesis of a TTG intrusive suite: the La Dauversière pluton, Abitibi greenstone belt, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University; Arthur B. McDonald-Canadian Astroparticle Physics Research Institute; Université du Québec à Chicoutimi","funders":"Natural Sciences and Engineering Research Council of Canada; Université du Québec à Chicoutimi; Materials and Energy Research Center; Canada First Research Excellence Fund; Ministère de l'Énergie et des Ressources Naturelles; Laurentian University","keywords":"Pluton; Greenstone belt; Geology; Petrogenesis; Geochemistry; Archean; Suite; Petrology; Basalt; Tectonics; Seismology; Archaeology","score_opus":0.01013066292751102,"score_gpt":0.2000207445685709,"score_spread":0.1898900816410599,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399120301","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93372804,0.005176786,0.0016970858,0.031221,0.0019454334,0.00011352772,0.000044804023,0.000014946513,0.026058355],"genre_scores_gemma":[0.99833333,0.000013940678,0.00066235557,0.00029377762,0.00008904705,4.357551e-7,3.0111426e-7,0.0000012736854,0.00060555554],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987731,0.00006865583,0.00026614926,0.0001825034,0.00037657554,0.00033299197],"domain_scores_gemma":[0.9988315,0.00026433068,0.00014519699,0.00018347979,0.00025141618,0.00032406033],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000961243,0.00009670367,0.00015177108,0.00016528847,0.0003204809,0.00022184111,0.0013073,0.000037136422,0.00009917307],"category_scores_gemma":[0.00028815217,0.00006432212,0.00007596152,0.00093593844,0.000541426,0.00032672452,0.000054248867,0.00019289883,0.0000015102743],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027369653,0.000067324465,0.31991917,0.0007230699,0.0007647414,0.017228397,0.029785685,0.032364875,0.007474266,0.3342492,0.12847865,0.12891725],"study_design_scores_gemma":[0.0005745597,0.0006763698,0.25055006,0.0010649605,0.00010704283,0.0078035975,0.0072554764,0.025259938,0.009933005,0.013114922,0.682671,0.0009890678],"about_ca_topic_score_codex":0.5525195,"about_ca_topic_score_gemma":0.9566755,"teacher_disagreement_score":0.55419236,"about_ca_system_score_codex":0.000020487518,"about_ca_system_score_gemma":0.009086524,"threshold_uncertainty_score":0.996531},"labels":[],"label_agreement":null},{"id":"W4399141112","doi":"10.1139/cjes-2024-0028","title":"The Yellowknife greenstone belt and underlying Central Slave Cover Group, Slave craton, Canada: constraints and questions arising from a U–Pb dating study","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Government of Northwest Territories; Industry, Tourism and Investment; Hutchinson (Canada); University of Alberta","funders":"","keywords":"Geology; Greenstone belt; Craton; Group (periodic table); Geochemistry; Cover (algebra); Archean; Seismology; Tectonics","score_opus":0.024045124161065638,"score_gpt":0.22035594502772682,"score_spread":0.19631082086666118,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399141112","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99170756,0.0052392306,0.00006768197,0.0015463276,0.00032286515,0.000068142705,0.00008815376,0.0000041055914,0.00095595804],"genre_scores_gemma":[0.9992841,0.00005820413,0.000338104,0.0001933626,0.00008322833,1.4178022e-7,0.0000058037394,0.0000012573767,0.000035809622],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99864614,0.00009691374,0.00030248085,0.00023293057,0.00030116114,0.0004203664],"domain_scores_gemma":[0.99857396,0.0005732792,0.000094937466,0.0000624047,0.00005609761,0.0006393269],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00064572785,0.00011757054,0.00018194651,0.00009419432,0.0010257306,0.00059026113,0.0002026412,0.000032485266,0.0008135412],"category_scores_gemma":[0.00022795127,0.00006969516,0.00003876137,0.00036870025,0.0010211924,0.00026178503,0.000011271418,0.0002543998,0.0000030554456],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000030433719,0.000003303607,0.97447383,0.000003540358,0.00006551355,0.0003172691,0.0004739332,0.0006429866,0.000054876145,0.00014275008,0.0001084379,0.023710528],"study_design_scores_gemma":[0.000097301636,0.00015136423,0.98334414,0.00006203579,0.000060046375,0.00009129042,0.003582892,0.008182969,0.000008787309,0.0034907772,0.0008089697,0.000119438984],"about_ca_topic_score_codex":0.89275587,"about_ca_topic_score_gemma":0.99785835,"teacher_disagreement_score":0.10510247,"about_ca_system_score_codex":0.0000052057453,"about_ca_system_score_gemma":0.001186502,"threshold_uncertainty_score":0.89077055},"labels":[],"label_agreement":null},{"id":"W4399141117","doi":"10.1139/cjes-2023-0143","title":"The Grenville Province: revisiting the orogenic framework and integrating recent findings","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Archean; Earth science","score_opus":0.014434516839484119,"score_gpt":0.2113569117481785,"score_spread":0.19692239490869437,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399141117","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9400953,0.033239182,0.00003315184,0.023605857,0.00032854814,0.00004481454,0.000006118745,0.000003808204,0.0026432376],"genre_scores_gemma":[0.99802774,0.0006819873,0.00061542314,0.00033380248,0.0002568821,1.3199951e-7,4.9280175e-7,7.9877583e-7,0.00008276281],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99901056,0.000070207505,0.00023826331,0.00013843804,0.0002247304,0.00031778726],"domain_scores_gemma":[0.99876034,0.0007725477,0.00006739024,0.0000624086,0.0000575096,0.00027979302],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016392358,0.00007751448,0.00010438729,0.00007051512,0.0011418561,0.00071306806,0.00039151407,0.000033197604,0.0015581163],"category_scores_gemma":[0.00090111914,0.00003047749,0.00007025225,0.00062409614,0.0006970305,0.00013241866,0.0000088551515,0.00034936782,0.000024141369],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000040054197,7.2789993e-7,0.62817454,0.000012480173,0.000039062576,0.000094489274,0.00057063514,0.00041472045,0.000032128813,0.0052591483,0.00024349322,0.36515453],"study_design_scores_gemma":[0.00008411092,0.0004280039,0.48242855,0.00066025014,0.00010803939,0.00075965805,0.0062868823,0.023394374,0.0002469588,0.115604445,0.36961532,0.00038340688],"about_ca_topic_score_codex":0.00436803,"about_ca_topic_score_gemma":0.16548671,"teacher_disagreement_score":0.36937183,"about_ca_system_score_codex":0.0000014355194,"about_ca_system_score_gemma":0.0005051274,"threshold_uncertainty_score":0.9993546},"labels":[],"label_agreement":null},{"id":"W4399141519","doi":"10.1139/cjes-2023-0141","title":"Tectonic evolution of high-grade metamorphic tectonites of the Meelpaeg structure near Port aux Basques, southwestern Newfoundland during the Silurian Salinic and Early-to-Middle Devonian Acadian orogenies","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland; University of Waterloo; Geological Survey of Canada","funders":"","keywords":"Geology; Tectonite; Devonian; Metamorphic rock; Tectonics; Paleontology; Seismology; Shear zone","score_opus":0.014351952398093738,"score_gpt":0.1965318553104176,"score_spread":0.1821799029123239,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399141519","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9910612,0.006183116,0.00000806137,0.0022217683,0.00023720862,0.000102685684,0.000100925274,0.0000049779774,0.00008006717],"genre_scores_gemma":[0.99940395,0.000021975644,0.00033869105,0.000066801564,0.0000941672,2.5892447e-7,0.000001385159,0.0000027045985,0.00007007064],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99837625,0.000116504576,0.0004603308,0.00023753937,0.00041742303,0.0003919303],"domain_scores_gemma":[0.99890643,0.00017466073,0.00021532874,0.00015859163,0.00011465096,0.0004303123],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00065643154,0.00015483715,0.0003078644,0.0002844621,0.00053360924,0.00022939157,0.00064664776,0.00007891829,0.0010971734],"category_scores_gemma":[0.00016400855,0.000075124,0.00016953392,0.0013131452,0.0010692944,0.0002428409,0.000023143202,0.00031267505,0.000006586983],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000062777053,0.0000020565446,0.9943093,0.000023040444,0.000059938775,0.0000145967615,0.0005392451,0.0036862832,0.0007079332,0.00016004332,0.000003179231,0.00048812546],"study_design_scores_gemma":[0.00008621092,0.00018310879,0.99235713,0.00010387806,0.00008354564,0.0001433474,0.00033072935,0.0006530759,0.00080945226,0.004671107,0.00047295622,0.000105450454],"about_ca_topic_score_codex":0.14822865,"about_ca_topic_score_gemma":0.7814329,"teacher_disagreement_score":0.6332043,"about_ca_system_score_codex":0.000006142322,"about_ca_system_score_gemma":0.0010903386,"threshold_uncertainty_score":0.99981594},"labels":[],"label_agreement":null},{"id":"W4399213420","doi":"10.1139/cjes-2023-0086","title":"Electrically anisotropic structure of the Rocky Mountain Trench near Valemount, British Columbia inferred from magnetotellurics: implications for geothermal exploration","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Mitacs","keywords":"Geology; Magnetotellurics; Anisotropy; Geothermal gradient; Electrical resistivity and conductivity; Geophysics; Fault (geology); Lithology; Geothermal exploration; Mylonite; Trench; Seismology; Petrology; Tectonics; Geothermal energy; Shear zone","score_opus":0.016963192134503025,"score_gpt":0.22731275063958153,"score_spread":0.2103495585050785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399213420","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99357104,0.001988364,0.0020312853,0.0011170565,0.00046943946,0.00017397194,0.0005104618,0.0000061762917,0.00013222828],"genre_scores_gemma":[0.99474317,0.000023906607,0.0045752414,0.00017373808,0.00023002134,5.986168e-7,0.000011624231,0.0000028192408,0.00023886269],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9988182,0.00010283388,0.00033254383,0.00019153717,0.0002198852,0.00033498392],"domain_scores_gemma":[0.9990021,0.0003364112,0.00014263544,0.0000994007,0.00014496355,0.00027447555],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023865626,0.00008055642,0.00018074756,0.00008053964,0.0005044215,0.0008207022,0.0004703943,0.00006387064,0.0009911001],"category_scores_gemma":[0.00023483676,0.00006863729,0.00012510344,0.0010768998,0.00028402905,0.00041148957,0.000004404584,0.0001901315,0.000004508681],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010852105,0.000014474585,0.403658,0.00003020375,0.000048965776,0.000011758785,0.0004001196,0.0119467145,0.0018356057,0.00028312314,0.001714738,0.58004546],"study_design_scores_gemma":[0.0001026839,0.00043658863,0.9388465,0.000034741097,0.000029936547,0.000032120395,0.000030005705,0.013438688,0.00010096176,0.03840872,0.00843873,0.00010030591],"about_ca_topic_score_codex":0.16357921,"about_ca_topic_score_gemma":0.7740868,"teacher_disagreement_score":0.61050755,"about_ca_system_score_codex":0.000004449141,"about_ca_system_score_gemma":0.0015105234,"threshold_uncertainty_score":0.99992216},"labels":[],"label_agreement":null},{"id":"W4399305353","doi":"10.1139/cjes-2024-0013","title":"Geochronology of the Mines Gaspé porphyry deposit, Québec, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia; Government of British Columbia; Lakehead University","funders":"Lakehead University","keywords":"Geology; Geochronology; Geochemistry; Petrology","score_opus":0.011001389916183215,"score_gpt":0.18935464365067256,"score_spread":0.17835325373448935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399305353","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8543245,0.015423253,0.0017865822,0.10040584,0.0045556407,0.00008776023,0.000007791595,0.000012848887,0.023395779],"genre_scores_gemma":[0.9980962,0.000007729242,0.0006554199,0.0003730269,0.00007479474,2.6168124e-7,5.4012876e-8,7.37013e-7,0.0007917654],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991201,0.000036348665,0.00023187796,0.00013718485,0.00020715567,0.00026732657],"domain_scores_gemma":[0.9992943,0.000093272625,0.00011623511,0.00016467598,0.00012561813,0.00020592634],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003671774,0.00006972971,0.000114633825,0.00009931226,0.0002130074,0.000099529745,0.0012629696,0.000030008601,0.00007660076],"category_scores_gemma":[0.00018591827,0.00004361152,0.00006236313,0.0005476515,0.00036206061,0.00019454065,0.000043103846,0.00012302696,0.0000012521512],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007954243,0.000038869126,0.6333389,0.00041744838,0.00028331045,0.004247366,0.0058600656,0.021432841,0.0142128365,0.07201426,0.20116536,0.046980742],"study_design_scores_gemma":[0.00014661142,0.00020530829,0.13478653,0.00042038743,0.00001863424,0.0033152192,0.0004766613,0.010732226,0.022968233,0.004541253,0.82208496,0.00030395025],"about_ca_topic_score_codex":0.83961236,"about_ca_topic_score_gemma":0.9962639,"teacher_disagreement_score":0.62091964,"about_ca_system_score_codex":0.000016994538,"about_ca_system_score_gemma":0.0144420145,"threshold_uncertainty_score":0.9911452},"labels":[],"label_agreement":null},{"id":"W4399366009","doi":"10.1139/cjes-2023-0133","title":"New Late Cretaceous (Cenomanian) fossil mayfly nymphs (Oligoneuriidae, Heptageniidae, Hexagenitidae) from the Redmond Formation, Labrador, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fossil Insects in Amber","field":"Agricultural and Biological Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"National Geographic Society Education Foundation","keywords":"Cretaceous; Geology; Mayfly; Paleontology; Cenomanian; Nymph; Zoology","score_opus":0.017971868805882998,"score_gpt":0.1947855255845776,"score_spread":0.1768136567786946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399366009","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96835417,0.012034671,0.000008890903,0.011237072,0.0022559795,0.00012404255,0.00017044382,0.000019706005,0.005795054],"genre_scores_gemma":[0.9942182,0.000076887554,0.00033821614,0.0013650677,0.0012314703,0.0000010913351,0.0000058748387,0.0000024663489,0.0027607365],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979271,0.00012175324,0.00048572643,0.00027479688,0.00058766524,0.0006029299],"domain_scores_gemma":[0.9983689,0.00041139274,0.00018966944,0.00009922297,0.00011950077,0.00081127393],"candidate_categories":["scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005774857,0.00020469821,0.00021441959,0.000056492165,0.00090149295,0.0010618956,0.0010609921,0.000078605706,0.0026042494],"category_scores_gemma":[0.00015998635,0.00007658866,0.00013019353,0.0010035811,0.0003163089,0.0007408702,0.00003208464,0.0003281344,0.0000501289],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044652643,0.00001906978,0.044089727,0.000031699838,0.00020476352,0.0035945089,0.0045066434,0.0007066941,0.011332284,0.002094682,0.5286655,0.4047098],"study_design_scores_gemma":[0.00009221491,0.00018381902,0.2775516,0.00012733965,0.000030354739,0.00037755285,0.0007382758,0.00028812027,0.0009157704,0.0010035211,0.71842784,0.0002636203],"about_ca_topic_score_codex":0.87981516,"about_ca_topic_score_gemma":0.9972577,"teacher_disagreement_score":0.40444615,"about_ca_system_score_codex":0.000048864615,"about_ca_system_score_gemma":0.0027709529,"threshold_uncertainty_score":0.9999751},"labels":[],"label_agreement":null},{"id":"W4399369929","doi":"10.1139/cjes-2024-0007","title":"Tonian rift successions in Newfoundland, Canada: a window to late tectonic events in the Mesoproterozoic Laurentian margin","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Rift; Window (computing); Tectonics; Margin (machine learning); Paleontology; Thermochronology; Seismology","score_opus":0.012822188061552975,"score_gpt":0.2109268924523705,"score_spread":0.19810470439081754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399369929","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98061687,0.0016525375,0.000003628296,0.015642911,0.00035188967,0.00010139137,0.000024996178,0.0000021390701,0.0016036569],"genre_scores_gemma":[0.9987445,0.0000139148315,0.00009501935,0.0009235613,0.00006452978,7.873849e-7,0.00000398393,0.0000010910626,0.00015263683],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99841946,0.00012510979,0.000327377,0.0002076589,0.00039802803,0.0005223804],"domain_scores_gemma":[0.99919814,0.00013155465,0.00005295426,0.00008844031,0.000031068746,0.000497855],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010505567,0.00011263495,0.00018968634,0.00046159886,0.0001960576,0.00014796709,0.0007004833,0.00003933958,0.003960191],"category_scores_gemma":[0.00012938866,0.00006132774,0.00007050946,0.0019365972,0.00012599854,0.00021045306,0.0000072803755,0.00033499836,0.00003996421],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000035190776,0.0000031054465,0.99297017,0.0000044175836,0.000005873333,0.00034065873,0.0002461115,0.0041024634,0.000009285361,0.000032592314,0.00013357235,0.0021482185],"study_design_scores_gemma":[0.000079366335,0.000094423274,0.98636734,0.00011126565,0.000007678069,0.000053156018,0.00021793453,0.0012211802,0.0000074727172,0.0020373105,0.009705999,0.00009686429],"about_ca_topic_score_codex":0.96509016,"about_ca_topic_score_gemma":0.999951,"teacher_disagreement_score":0.034860853,"about_ca_system_score_codex":0.000010753168,"about_ca_system_score_gemma":0.0021847945,"threshold_uncertainty_score":0.9969503},"labels":[],"label_agreement":null},{"id":"W4399519164","doi":"10.1139/cjes-2023-0060","title":"The Ottawa River Gneiss Complex revisited: definition of the metamorphic core and detachment zone of a large Grenvillian metamorphic core complex","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Memorial University of Newfoundland","funders":"","keywords":"Metamorphic core complex; Gneiss; Metamorphic rock; Geology; Detachment fault; Geochemistry; Core (optical fiber); Protolith; Petrology; Seismology; Tectonics; Extensional definition","score_opus":0.07713693567642153,"score_gpt":0.25479065275352897,"score_spread":0.17765371707710742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399519164","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98156613,0.013556293,0.000083037085,0.0019231051,0.0002864989,0.00014202476,0.00030698843,0.0000038719677,0.0021320735],"genre_scores_gemma":[0.9983277,0.0003163832,0.0010488426,0.00021153488,0.00003466417,3.0594404e-7,0.000011350935,0.000001485004,0.00004774926],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99859476,0.00009927271,0.00048613304,0.0001316304,0.000385626,0.000302557],"domain_scores_gemma":[0.9988403,0.00031357934,0.00030829752,0.00012075524,0.0001722103,0.00024490457],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015733199,0.00011342331,0.00024133013,0.00019393425,0.0007363232,0.00014386332,0.00048749978,0.000039979746,0.0014617715],"category_scores_gemma":[0.00015051862,0.000054658547,0.00011273971,0.0008672152,0.0013695578,0.00029550836,0.000013513835,0.00017859183,0.000011802936],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001425609,0.000013115034,0.9584832,0.00018195753,0.00010670506,0.000033920634,0.0010383241,0.00097247516,0.00013392759,0.028442578,0.0012618939,0.009317608],"study_design_scores_gemma":[0.00011774866,0.0002862478,0.9513365,0.0001441054,0.00007035148,0.00019544171,0.0005058852,0.0050763334,0.000027340364,0.009464736,0.03268378,0.00009151392],"about_ca_topic_score_codex":0.0035806643,"about_ca_topic_score_gemma":0.10507164,"teacher_disagreement_score":0.101490974,"about_ca_system_score_codex":0.0000017722294,"about_ca_system_score_gemma":0.00045016885,"threshold_uncertainty_score":0.99945104},"labels":[],"label_agreement":null},{"id":"W4399557488","doi":"10.1139/cjes-2023-0132","title":"Rheological bridge zones: the initiation of strain localization","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Structural Engineering and Vibration Analysis","field":"Engineering","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Rheology; Strain (injury); Bridge (graph theory); Geotechnical engineering; Seismology; Geodesy; Composite material; Materials science","score_opus":0.024671021481221966,"score_gpt":0.23427741083205098,"score_spread":0.209606389350829,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399557488","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.48377496,0.0032744426,0.50923645,0.00070509413,0.0011758709,0.00004484266,0.000021316191,0.00003334983,0.0017336636],"genre_scores_gemma":[0.9996451,0.000026896034,0.0002268921,0.000025010762,0.000059891296,1.5677111e-7,0.000001000422,0.0000021862268,0.000012869458],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996026,0.000013063571,0.0001600101,0.000035529145,0.00010416952,0.000084612126],"domain_scores_gemma":[0.9997876,0.00004047241,0.000022249224,0.000030282938,0.000039716946,0.00007962725],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024690127,0.000038183578,0.00006251862,0.00018925733,0.00005719428,0.000069820235,0.00010451431,0.000020884634,0.00013024326],"category_scores_gemma":[0.000051738618,0.00002358431,0.000040734616,0.0004877926,0.00013232336,0.00015547955,0.0000012389726,0.00006947909,0.0000025296797],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[2.526175e-7,3.684942e-7,0.0011224151,0.00001597506,0.000018729197,0.000008880729,0.0004145766,0.9833031,0.00025987087,0.008471116,0.0002320211,0.006152686],"study_design_scores_gemma":[0.00004033327,0.00006017643,0.053188995,0.00007742284,0.00002013051,0.000067375004,0.00031892504,0.941573,0.00074498466,0.0009389995,0.0028974537,0.00007216294],"about_ca_topic_score_codex":0.00017318298,"about_ca_topic_score_gemma":0.002826547,"teacher_disagreement_score":0.51587015,"about_ca_system_score_codex":0.000004550418,"about_ca_system_score_gemma":0.00016168122,"threshold_uncertainty_score":0.15772796},"labels":[],"label_agreement":null},{"id":"W4399659904","doi":"10.1139/cjes-2024-0009","title":"Upper Triassic igneous rocks of the southern Kenai Peninsula, Alaska—prelude to Early Jurassic subduction along the Western Wrangellia composite terrane margin","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Terrane; Geology; Subduction; Igneous rock; Margin (machine learning); Peninsula; Geochemistry; Paleontology; Archaeology; Tectonics","score_opus":0.0233495661457556,"score_gpt":0.20646655406671371,"score_spread":0.18311698792095812,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399659904","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98642117,0.0030174383,0.000090998,0.00827173,0.0014778475,0.00015258155,0.000037263173,0.0000056471176,0.0005253185],"genre_scores_gemma":[0.99863756,0.000037231493,0.00006812098,0.00028471643,0.00024714094,5.633238e-7,0.0000015666818,0.0000024556498,0.00072063506],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99860144,0.00012860983,0.00034326955,0.0001775426,0.00039882047,0.00035030008],"domain_scores_gemma":[0.9992562,0.00013475433,0.00014186594,0.00011528734,0.00008168977,0.00027018646],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00077389536,0.0001210513,0.00018425216,0.0001443121,0.0006664519,0.0003141433,0.0005412368,0.000044892524,0.0004697567],"category_scores_gemma":[0.00006206561,0.00005728443,0.00013418378,0.0006507251,0.00040467523,0.00026094686,0.000012246694,0.00021229917,0.00012781916],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018838271,0.0000029579446,0.98017335,0.000007892761,0.000022100201,0.000025580852,0.0032253747,0.008824067,0.00006159986,0.000007616999,0.0005435018,0.007087123],"study_design_scores_gemma":[0.00010228709,0.00039334412,0.98729205,0.00012798359,0.000031466203,0.00011691444,0.0013644288,0.0015735573,0.000091563255,0.00024026017,0.00855853,0.000107640975],"about_ca_topic_score_codex":0.042852506,"about_ca_topic_score_gemma":0.2783266,"teacher_disagreement_score":0.2354741,"about_ca_system_score_codex":0.0000038763624,"about_ca_system_score_gemma":0.00030206627,"threshold_uncertainty_score":0.96352124},"labels":[],"label_agreement":null},{"id":"W4399878350","doi":"10.1139/cjes-2024-0031","title":"The Folster Lake Formation, Nunavut: remnant of a littoral to fluvio-deltaic source to the Paleoproterozoic-age Penrhyn basin","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Nunavut; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Structural basin; Littoral zone; Geochemistry; Paleontology; Geomorphology; Oceanography","score_opus":0.027352257844433264,"score_gpt":0.21634332718977237,"score_spread":0.1889910693453391,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399878350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9612906,0.0024044209,0.00089695834,0.0325425,0.0010897254,0.00027976115,0.000037567945,0.0000061491455,0.0014523417],"genre_scores_gemma":[0.9981587,0.00004109352,0.00032952742,0.00090143416,0.00020798169,0.0000012716931,0.0000017735472,0.0000013552688,0.00035685237],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987184,0.00008724848,0.00034261862,0.00012635475,0.00035224247,0.0003731758],"domain_scores_gemma":[0.9991547,0.00016343388,0.00009013814,0.00010305463,0.000115497496,0.00037317746],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001608059,0.000089564186,0.00013294622,0.00012586915,0.00089015556,0.00048523594,0.0005072746,0.000026729558,0.00026763635],"category_scores_gemma":[0.00024953744,0.000039969444,0.00007729725,0.0007067664,0.0002476567,0.00034411735,0.000012391393,0.00013163422,0.00011381126],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010021971,0.000011386172,0.6076667,0.00006585215,0.00006832012,0.00022877092,0.02639184,0.04663264,0.00008301378,0.0011002161,0.037359647,0.2802914],"study_design_scores_gemma":[0.000045511784,0.0006036847,0.4374776,0.0000900689,0.00000914882,0.00005357199,0.0023635202,0.0018177094,0.00003645812,0.0006750881,0.55673844,0.0000892],"about_ca_topic_score_codex":0.006845117,"about_ca_topic_score_gemma":0.8652207,"teacher_disagreement_score":0.8583756,"about_ca_system_score_codex":0.000002334941,"about_ca_system_score_gemma":0.00029883106,"threshold_uncertainty_score":0.9997684},"labels":[],"label_agreement":null},{"id":"W4400068755","doi":"10.1139/cjes-2024-0033","title":"Paleoenvironmental and chemostratigraphic implications of variations in geochemical proxies across the Upper Jurassic–Lower cretaceous boundary: a case study from the Flemish Pass Basin","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University; Memorial University of Newfoundland; Geological Survey of Canada; Natural Resources Canada","funders":"Commission Géologique du Canada","keywords":"Geology; Cretaceous; Paleontology; Structural basin; Flemish; Viséan; Carboniferous; Archaeology","score_opus":0.015910011269947205,"score_gpt":0.2435983074167436,"score_spread":0.2276882961467964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400068755","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9833122,0.011461463,0.000008468761,0.0039219647,0.00019904276,0.00017453905,0.00024173874,0.0000026242947,0.00067794474],"genre_scores_gemma":[0.99968094,0.000050146416,0.00013605786,0.000069950605,0.000054110933,0.0000016881582,0.0000015824216,7.0281294e-7,0.0000048451247],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989037,0.00013005637,0.00032193554,0.00018539242,0.00018287075,0.00027605324],"domain_scores_gemma":[0.99903643,0.0005190125,0.00010458243,0.00012859362,0.000024659195,0.00018673266],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009067459,0.00010276444,0.00015241382,0.00009053599,0.00077959086,0.00031867545,0.00033300533,0.000051537852,0.00013777893],"category_scores_gemma":[0.000072873416,0.000057164907,0.00006904709,0.00047098412,0.0016962853,0.0003141307,0.0000025181337,0.00029177737,8.6388656e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000039777588,0.000010938,0.986696,0.0000018895264,0.00002584313,0.00027173714,0.0044505894,0.000013290991,0.000032688044,0.000042989777,0.000047895694,0.008402158],"study_design_scores_gemma":[0.00010740909,0.00016969981,0.9883548,0.000026786378,0.00002696555,0.0010748538,0.008581051,0.00031166786,0.000016080445,0.00088317,0.0003783655,0.00006917737],"about_ca_topic_score_codex":0.027325112,"about_ca_topic_score_gemma":0.7996527,"teacher_disagreement_score":0.7723276,"about_ca_system_score_codex":0.0000014594515,"about_ca_system_score_gemma":0.00064291403,"threshold_uncertainty_score":0.979152},"labels":[],"label_agreement":null},{"id":"W4400346106","doi":"10.1139/cjes-2024-0023","title":"Devonian plutons in the eastern Meguma terrane, Nova Scotia, Canada: zircon U–Pb, Lu–Hf, and O isotopic compositions, age, and petrogenetic implications","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; Acadia University; St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Zircon; Geology; Pluton; Nova scotia; Geochemistry; Terrane; Devonian; Geochronology; Late Devonian extinction; Mineralogy; Seismology; Geomorphology; Tectonics; Carboniferous","score_opus":0.021569757260330537,"score_gpt":0.21281713650235576,"score_spread":0.19124737924202523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400346106","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97927827,0.006520117,0.000025356105,0.012083914,0.00011788766,0.00005566205,0.000045388486,0.0000019287443,0.0018714638],"genre_scores_gemma":[0.9987741,0.000040875268,0.0004227599,0.00066682976,0.000050872866,2.1482953e-7,0.00000510027,8.0511694e-7,0.000038437713],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990946,0.00006115913,0.00022504928,0.00016759477,0.0001739667,0.000277639],"domain_scores_gemma":[0.999359,0.00015157476,0.000045453817,0.0000675521,0.000030427962,0.00034596436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033472874,0.00008705803,0.00013656917,0.00019266816,0.00025074012,0.00026523464,0.0002748695,0.000027808132,0.00070759497],"category_scores_gemma":[0.00003564184,0.00005227129,0.00003485272,0.00053268333,0.0004652846,0.00015952406,0.0000057263605,0.00016875393,0.0000071315408],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[8.960231e-7,0.00000238107,0.99495786,0.000008531291,0.00001122754,0.00017856019,0.00021777856,0.00025690417,0.00007209311,0.00034496174,0.00013240158,0.0038164086],"study_design_scores_gemma":[0.000054519813,0.000081630336,0.9915105,0.000040435218,0.000020485366,0.0003829909,0.00052269886,0.0013388903,0.00001866141,0.003265863,0.0026817247,0.000081585],"about_ca_topic_score_codex":0.8025795,"about_ca_topic_score_gemma":0.9988446,"teacher_disagreement_score":0.19626509,"about_ca_system_score_codex":0.0000028447155,"about_ca_system_score_gemma":0.0007698195,"threshold_uncertainty_score":0.77476686},"labels":[],"label_agreement":null},{"id":"W4400420434","doi":"10.1139/cjes-2024-0041","title":"The Holocene to modern Fraser River Delta, Canada: geological history, processes, deposits, natural hazards, and coastal management","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Coastal wetland ecosystem dynamics","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Simon Fraser University","funders":"","keywords":"Geology; Holocene; Delta; Natural (archaeology); River delta; Natural hazard; Archaeology; Geochemistry; Geomorphology; Earth science; Oceanography; Physical geography; Paleontology; Geography","score_opus":0.00690107996737748,"score_gpt":0.18032834122208063,"score_spread":0.17342726125470315,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400420434","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99038535,0.0044297613,0.00024912515,0.0016794152,0.0009235018,0.00012217415,0.000018272873,0.0000057422485,0.0021866646],"genre_scores_gemma":[0.9979979,0.000061348124,0.00047091645,0.00034692022,0.00004368153,0.000001854195,7.8654006e-7,0.0000051552674,0.0010714583],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986924,0.00002867419,0.0002153663,0.00022332989,0.00042250162,0.000417721],"domain_scores_gemma":[0.999211,0.000060175727,0.000056345754,0.00008522174,0.00002569804,0.00056151755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044284968,0.00011330028,0.00011340103,0.00007738834,0.00041557907,0.00018228083,0.00043505596,0.000026379466,0.000103281694],"category_scores_gemma":[0.00005255608,0.000071024,0.000027065882,0.0002929355,0.0004428289,0.0002460474,0.00009649105,0.00015751997,0.000012684476],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006597773,0.000026157559,0.6756478,0.00019720246,0.00014718875,0.0058264043,0.00244862,0.022853145,0.000059041864,0.0014704708,0.09462273,0.19663526],"study_design_scores_gemma":[0.00022118461,0.00027910038,0.6196087,0.0001882061,0.000044692104,0.0007385088,0.0006412196,0.035628263,0.000028499278,0.0007465544,0.3414585,0.00041657937],"about_ca_topic_score_codex":0.45018002,"about_ca_topic_score_gemma":0.9977854,"teacher_disagreement_score":0.5476054,"about_ca_system_score_codex":0.00015664373,"about_ca_system_score_gemma":0.0013660662,"threshold_uncertainty_score":0.5534813},"labels":[],"label_agreement":null},{"id":"W4400602269","doi":"10.1139/cjes-2024-0001","title":"The volcanic architecture and tectono-magmatic framework of the Mount Grace carbonatites, southeastern Canadian Cordillera","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Society of Economic Geologists Foundation","keywords":"Mount; Geology; Carbonatite; Volcano; Dike; Volcanic rock; Geochemistry; Architecture; Volcanic belt; Geomorphology; Seismology; Earth science; Archaeology; Mantle (geology)","score_opus":0.007871378099015423,"score_gpt":0.18362790055193523,"score_spread":0.1757565224529198,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400602269","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97310185,0.014172492,0.000015580521,0.009892112,0.00046897974,0.00006945227,0.000054259166,0.0000027893193,0.0022225028],"genre_scores_gemma":[0.9992365,0.00005360519,0.00020753246,0.00031103875,0.00008139767,1.8668739e-7,6.551077e-7,0.0000013756137,0.000107672095],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998781,0.0000827167,0.00029000724,0.0001477158,0.00030906525,0.0003894693],"domain_scores_gemma":[0.9986677,0.00043662795,0.00010929254,0.00011967206,0.00007428813,0.0005924188],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006550208,0.000105845094,0.0001707461,0.00017655795,0.00058041926,0.0002743126,0.0005904634,0.00005296195,0.0012551394],"category_scores_gemma":[0.00042462244,0.00004608855,0.00011026256,0.00080731674,0.0009961912,0.000080865284,0.00000901859,0.0003685388,0.000011590082],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000039666425,0.000002056058,0.9753455,0.00002818729,0.00007258788,0.000048228234,0.00091744843,0.0040721195,0.000039527866,0.0015525557,0.00009401577,0.017823797],"study_design_scores_gemma":[0.00005686726,0.0001951658,0.9026296,0.0003060999,0.00007760481,0.00020403942,0.0010573204,0.012418941,0.000067269255,0.06267229,0.020123865,0.0001908985],"about_ca_topic_score_codex":0.43565807,"about_ca_topic_score_gemma":0.98700505,"teacher_disagreement_score":0.55134696,"about_ca_system_score_codex":0.0000033715069,"about_ca_system_score_gemma":0.0014459661,"threshold_uncertainty_score":0.99965787},"labels":[],"label_agreement":null},{"id":"W4401106364","doi":"10.1139/cjes-2024-0027","title":"The structural setting and evolution of the Upper Beaver gold–copper deposit, Ontario, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Agnico Eagle (Canada); Université Laval; Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada; Society of Economic Geologists Canada Foundation","keywords":"Geology; Beaver; Copper; Geochemistry; Mining engineering; Paleontology; Metallurgy","score_opus":0.006469779828404871,"score_gpt":0.18157562391663898,"score_spread":0.1751058440882341,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401106364","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9844066,0.0017822544,0.00011477219,0.009052477,0.0011646742,0.00003604339,0.0000016523874,0.0000021449312,0.0034393847],"genre_scores_gemma":[0.99847853,0.000002036451,0.0004799656,0.00010253442,0.000044617078,1.8117139e-7,3.2718535e-8,5.5816463e-7,0.0008915672],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99920976,0.000034639128,0.00017569099,0.000114596165,0.00023193183,0.00023340796],"domain_scores_gemma":[0.99945843,0.000093474606,0.000087593355,0.0001142234,0.00009388559,0.0001524179],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051032705,0.00005901306,0.00006569001,0.000041294406,0.0005310856,0.00026290995,0.0006836898,0.000021211663,0.00001412547],"category_scores_gemma":[0.000107845604,0.00003021497,0.000037131686,0.00029229384,0.00029440882,0.00024673354,0.000045032146,0.00017175204,2.1149054e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000012176201,7.46551e-7,0.9684415,0.000022219443,0.000026597994,0.00006293539,0.0022027465,0.0018852483,0.0004312917,0.017849753,0.0042407326,0.0048350343],"study_design_scores_gemma":[0.000050542472,0.000037241538,0.942654,0.00012584106,0.000008090121,0.0006700042,0.0004789074,0.009929582,0.0007226038,0.0042705103,0.040958643,0.00009401917],"about_ca_topic_score_codex":0.853819,"about_ca_topic_score_gemma":0.9951678,"teacher_disagreement_score":0.14134878,"about_ca_system_score_codex":0.000043921424,"about_ca_system_score_gemma":0.0059963586,"threshold_uncertainty_score":0.99963874},"labels":[],"label_agreement":null},{"id":"W4401220513","doi":"10.1139/cjes-2023-0146","title":"Bellerophontid molluscs in the Grimsby Formation (Llandovery, lower Silurian), Hamilton, Ontario, Canada and their paleoecological and taphonomic implications","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Paleontology; Taphonomy; Escarpment; Population","score_opus":0.014323118556026733,"score_gpt":0.18839223919978332,"score_spread":0.1740691206437566,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401220513","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9826831,0.009324888,0.00001327177,0.0016401911,0.00041073177,0.00007868215,0.00003723671,0.0000017862487,0.0058100903],"genre_scores_gemma":[0.9995055,0.0001385196,0.00007994902,0.00021574747,0.000039400707,4.4354292e-7,0.00000145441,3.525584e-7,0.000018631306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99921745,0.00007064237,0.00023024065,0.00013135954,0.00009426262,0.0002560631],"domain_scores_gemma":[0.99937916,0.000251781,0.00006518801,0.00005882372,0.000021509324,0.00022353893],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00065458217,0.000089641246,0.00012886798,0.00016986778,0.00041250137,0.00022308291,0.00022704912,0.000047856905,0.00014445366],"category_scores_gemma":[0.00002574544,0.000050679486,0.000031889256,0.00023318015,0.00039815754,0.0003640846,8.859135e-7,0.00021528373,9.4015854e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000053268354,0.0000016953041,0.9864696,0.0000040785103,0.000008049367,0.000072343064,0.0020988907,0.00008851196,0.000006965187,0.00017649606,0.00053670804,0.01053129],"study_design_scores_gemma":[0.00008339129,0.00014359919,0.99119776,0.000019979398,0.000004950772,0.00045399932,0.0005795204,0.00033369596,0.000004148305,0.0010598613,0.0060504004,0.00006867839],"about_ca_topic_score_codex":0.8891585,"about_ca_topic_score_gemma":0.99995285,"teacher_disagreement_score":0.11079438,"about_ca_system_score_codex":0.0000045942656,"about_ca_system_score_gemma":0.0019337519,"threshold_uncertainty_score":0.34303927},"labels":[],"label_agreement":null},{"id":"W4401242636","doi":"10.1139/cjes-2024-0082","title":"Serpentinization of the forearc mantle wedge in subduction zones: revisiting Roy D. Hyndman’s seminal contributions 25 years later","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Forearc; Geology; Subduction; Mantle (geology); Mantle wedge; Seismology; Wedge (geometry); Tectonics; Paleontology; Geometry","score_opus":0.010472954253560488,"score_gpt":0.21951413597681618,"score_spread":0.2090411817232557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401242636","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962261,0.00082168495,0.000031673477,0.00058569823,0.001278295,0.000071437666,0.000095972835,0.0000023882963,0.0008867773],"genre_scores_gemma":[0.99945647,0.000027176735,0.00010327093,0.00002499111,0.00021291508,1.468997e-7,0.000005258164,0.0000014160222,0.00016837675],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991726,0.00007018554,0.00026263137,0.00009770964,0.00018782154,0.00020905198],"domain_scores_gemma":[0.9995866,0.000051391497,0.00011220668,0.000060062197,0.00007819676,0.00011157232],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009533768,0.00005450343,0.000117316544,0.00019027185,0.00015632602,0.00017438078,0.00021315277,0.000030211726,0.00078516896],"category_scores_gemma":[0.000082369916,0.000036833342,0.000050998424,0.00049711706,0.00017302872,0.00036100682,0.00000504567,0.00009352588,0.000022818243],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014567431,0.000009379678,0.960228,0.00013845536,0.000043765092,0.00014846982,0.0029033513,0.013328966,0.002360671,0.0056889765,0.0015160483,0.013619308],"study_design_scores_gemma":[0.000087110064,0.000059120288,0.9836078,0.00033161655,0.000018382312,0.00006409629,0.00025438963,0.0019089163,0.0008289536,0.0014012569,0.011362504,0.000075820026],"about_ca_topic_score_codex":0.009667661,"about_ca_topic_score_gemma":0.072652385,"teacher_disagreement_score":0.06298472,"about_ca_system_score_codex":0.0000023711418,"about_ca_system_score_gemma":0.00057352625,"threshold_uncertainty_score":0.996927},"labels":[],"label_agreement":null},{"id":"W4401352746","doi":"10.1139/cjes-2024-0060","title":"Coesite-bearing garnet xenocrysts from diatexite in the Nordøyane domain, Western Gneiss Region, Norway: implications for eclogite-melt interaction at ultra-high pressure","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Eclogite; Coesite; Geology; Gneiss; Geochemistry; Bearing (navigation); Migmatite; Metamorphic rock; Seismology; Petrology; Tectonics; Subduction","score_opus":0.02536534452032761,"score_gpt":0.23133806270208382,"score_spread":0.20597271818175622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401352746","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9831409,0.0028049953,0.0001577189,0.012044567,0.00032640577,0.00013370378,0.00011795125,0.0000061722867,0.0012675964],"genre_scores_gemma":[0.9985315,0.00011007724,0.00022448946,0.00056589086,0.00024274872,0.0000018753401,0.000039004957,0.0000018338277,0.00028255244],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873394,0.00011057432,0.0003304428,0.0002527566,0.00018874886,0.00038354917],"domain_scores_gemma":[0.9986997,0.00064457575,0.00012996292,0.000120899844,0.000086163425,0.00031867356],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00064503023,0.00011864595,0.0001933722,0.00023969104,0.000434184,0.00033263653,0.00052386237,0.00006343525,0.0010028614],"category_scores_gemma":[0.00013155004,0.000070809,0.00012182764,0.0006613381,0.00031069663,0.0003653193,0.0000055549885,0.00021812218,0.00004878156],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001728037,0.000006466895,0.98952293,0.000012279165,0.00003456527,0.000050309238,0.00104737,0.0057408107,0.00013743303,0.00028256423,0.00062420126,0.0025237915],"study_design_scores_gemma":[0.000115547286,0.00014873502,0.92897093,0.00007058815,0.000050180115,0.000095930896,0.00042694167,0.0006457065,0.00007326217,0.017476324,0.05179733,0.00012853289],"about_ca_topic_score_codex":0.043605253,"about_ca_topic_score_gemma":0.64376456,"teacher_disagreement_score":0.60015935,"about_ca_system_score_codex":0.0000047137087,"about_ca_system_score_gemma":0.00023960239,"threshold_uncertainty_score":0.99991035},"labels":[],"label_agreement":null},{"id":"W4401409613","doi":"10.1139/cjes-2024-0034","title":"Crustal melting recorded by dykes along the gold-bearing Melanson Brook Fault, northern New Brunswick Appalachians","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of New Brunswick; University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; West virginia; Fault (geology); Bearing (navigation); Seismology; Archaeology","score_opus":0.014191600303254816,"score_gpt":0.19817666001000894,"score_spread":0.18398505970675413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401409613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9741811,0.01136922,0.00009479488,0.0058959792,0.00051329966,0.000060793842,0.00002114859,0.000015496189,0.0078481315],"genre_scores_gemma":[0.9970291,0.00007177837,0.0004230814,0.000408333,0.00032770855,9.3021086e-8,0.0000064465444,0.0000027213719,0.0017306869],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982456,0.000082461134,0.000405426,0.00027187538,0.00040519258,0.0005894551],"domain_scores_gemma":[0.9986189,0.00028718164,0.00013125851,0.0001028765,0.00006913978,0.00079064374],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009247375,0.00016176554,0.00022993742,0.00019242769,0.00049508165,0.00059038046,0.00070250826,0.000064538996,0.0040409574],"category_scores_gemma":[0.00022513543,0.000089343055,0.00019001412,0.00084797863,0.00044919507,0.00039039023,0.000009763912,0.00041424585,0.00014914513],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004642547,0.0000026326195,0.94689125,0.000009117736,0.00004318223,0.000106477906,0.0005053721,0.004399907,0.00010782108,0.00008677272,0.0013670733,0.04647577],"study_design_scores_gemma":[0.00034469672,0.0007744389,0.7806661,0.0003627995,0.00019652465,0.00068939617,0.0038271295,0.037307885,0.0008072322,0.0092330985,0.16497399,0.00081670325],"about_ca_topic_score_codex":0.426094,"about_ca_topic_score_gemma":0.9651013,"teacher_disagreement_score":0.5390073,"about_ca_system_score_codex":0.000003681989,"about_ca_system_score_gemma":0.0017138447,"threshold_uncertainty_score":0.9968695},"labels":[],"label_agreement":null},{"id":"W4401503666","doi":"10.1139/cjes-2024-0018","title":"Unravelling the fragmented sediment–landform assemblage in an area of thick Quaternary sediment, western Hudson Bay Lowland, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; University of the Fraser Valley; Memorial University of Newfoundland; Université du Québec à Montréal; Manitoba Hydro; University of Waterloo","funders":"","keywords":"Bay; Geology; Quaternary; Landform; Sediment; Assemblage (archaeology); Oceanography; Geomorphology; Paleontology","score_opus":0.032054228598685224,"score_gpt":0.25600306812875995,"score_spread":0.22394883953007472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401503666","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99208194,0.0030008485,0.000016125538,0.0021552118,0.0009116614,0.00009212316,0.000033174623,0.0000027406936,0.0017061809],"genre_scores_gemma":[0.99934536,0.00006905741,0.000049624217,0.0002659024,0.00007115726,3.0142527e-7,0.000009482434,0.000002089242,0.00018701919],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998258,0.00019604103,0.00039636472,0.0001938046,0.00042148837,0.00053430063],"domain_scores_gemma":[0.9989223,0.00035823166,0.000120878256,0.000119701035,0.000071853254,0.0004070545],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019130309,0.0001217443,0.00022113789,0.00037768093,0.00028774468,0.00012730547,0.0006331221,0.000078100995,0.00095242314],"category_scores_gemma":[0.00004573506,0.00007448428,0.000047533355,0.0005422136,0.0004644072,0.0003863732,0.000007234014,0.0004449476,0.000015247953],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013172364,0.0000034177185,0.9953589,0.000017545812,0.000017464892,0.0005316428,0.00064234826,0.003056564,0.000009158049,0.000025941377,0.00008308041,0.00024077254],"study_design_scores_gemma":[0.0002077876,0.0004175695,0.9783189,0.00019567912,0.000013766747,0.0003479704,0.0014171118,0.0163731,0.00021050827,0.000252686,0.0021196408,0.00012524672],"about_ca_topic_score_codex":0.5344841,"about_ca_topic_score_gemma":0.9980413,"teacher_disagreement_score":0.4635572,"about_ca_system_score_codex":0.0000027718777,"about_ca_system_score_gemma":0.0038701298,"threshold_uncertainty_score":0.99996084},"labels":[],"label_agreement":null},{"id":"W4401599657","doi":"10.1139/cjes-2024-0057","title":"Classifying intrusive and strongly metamorphosed rock units: CLASS—a cooperative lithodemic and stratigraphic system","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Image Processing and 3D Reconstruction","field":"Computer Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geoscience BC; Ministère des Ressources naturelles et des Forêts (Québec); Natural Resources Canada; Alberta Energy; Government of Northwest Territories; Government of Manitoba; Centre de Géomatique du Québec; Manitoba Hydro; Geological Survey of Canada; Government of Saskatchewan","funders":"","keywords":"Geology; Geochemistry; Class (philosophy)","score_opus":0.025211706466728566,"score_gpt":0.23538139016377568,"score_spread":0.2101696836970471,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401599657","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.87362325,0.026426593,0.094748594,0.0016363814,0.0019835962,0.00012280494,0.000011164198,0.000049161896,0.0013984557],"genre_scores_gemma":[0.99005973,0.0000589245,0.009693639,0.000042978856,0.0000835834,6.807605e-7,1.4362733e-7,0.000003197997,0.000057125304],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.998945,0.00010479353,0.00026404945,0.000241052,0.00018761185,0.00025747053],"domain_scores_gemma":[0.99906176,0.000101815676,0.00012298807,0.000070293536,0.00025696022,0.00038616286],"candidate_categories":["scholarly_communication"],"consensus_categories":[],"category_scores_codex":[0.0008113128,0.00011216175,0.00017469173,0.00061924336,0.00054153544,0.001645683,0.000298329,0.000049086906,0.0000043302475],"category_scores_gemma":[0.000091024216,0.00008361009,0.000024453706,0.0011673357,0.00036679622,0.0015384767,0.0000183857,0.0002709176,0.0000014998428],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002648347,0.00002003839,0.0852135,0.0012443906,0.00054139976,0.0024512277,0.03047392,0.0057686293,0.007830293,0.44446275,0.0014641874,0.4205032],"study_design_scores_gemma":[0.0008777041,0.0014705323,0.018630598,0.0038709927,0.00014321668,0.018119179,0.022234023,0.918739,0.0041931174,0.003093793,0.0076775667,0.00095023407],"about_ca_topic_score_codex":0.00039137984,"about_ca_topic_score_gemma":0.0053096004,"teacher_disagreement_score":0.9129704,"about_ca_system_score_codex":0.000011487456,"about_ca_system_score_gemma":0.0034114236,"threshold_uncertainty_score":0.9993907},"labels":[],"label_agreement":null},{"id":"W4401800005","doi":"10.1139/cjes-2024-0019","title":"Preservation of probable MIS 7 deglacial and nonglacial deposits near the edge of the Hudson Bay Lowland in Manitoba, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; University of the Fraser Valley; Memorial University of Newfoundland; Université du Québec à Montréal; Manitoba Hydro; University of Waterloo","funders":"","keywords":"Geology; Bay; Oceanography; Paleontology; Ecological succession; Archaeology; Geography","score_opus":0.023641644263604655,"score_gpt":0.2110863114197362,"score_spread":0.18744466715613153,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401800005","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935739,0.0026766437,0.0000017129746,0.0017567181,0.0005234516,0.00010305923,0.000012103729,5.695526e-7,0.0013518643],"genre_scores_gemma":[0.9997585,0.000017381602,0.0000588873,0.000057725243,0.00004445027,2.0643628e-7,7.6546377e-7,7.8838787e-7,0.000061313855],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990207,0.00014761089,0.00023816703,0.00009649772,0.00024558321,0.0002514584],"domain_scores_gemma":[0.9994078,0.00023496848,0.000089927686,0.000066338784,0.000074385214,0.00012653091],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009445143,0.000058178113,0.0001270153,0.0001121951,0.0003524302,0.000078346435,0.00038470514,0.000048244085,0.00010631846],"category_scores_gemma":[0.0001599056,0.000031563908,0.00002821973,0.00051786157,0.0010175306,0.00021106108,0.0000064675796,0.00021297588,0.000001264364],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009417954,0.0000012344244,0.9979831,0.00002421391,0.000006902413,0.000032049415,0.00047209262,0.0008554974,0.0000047841104,0.00006819438,0.000095022886,0.0004474951],"study_design_scores_gemma":[0.0000839371,0.00009046587,0.99606395,0.000072147974,0.0000072866787,0.00012221056,0.00028259706,0.0018300267,0.00011673558,0.00025783383,0.0010372755,0.000035558147],"about_ca_topic_score_codex":0.57558405,"about_ca_topic_score_gemma":0.9997879,"teacher_disagreement_score":0.42420387,"about_ca_system_score_codex":0.0000011897157,"about_ca_system_score_gemma":0.004859655,"threshold_uncertainty_score":0.862082},"labels":[],"label_agreement":null},{"id":"W4401837528","doi":"10.1139/cjes-2024-0025","title":"Ages and structural relationships in the Ganderian central Cape Breton Highlands, Nova Scotia, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Acadia University","funders":"Cape Breton University; Acadia University; Natural Sciences and Engineering Research Council of Canada; Boise State University","keywords":"Nova scotia; Geology; Cape; Archaeology; Oceanography; Nova (rocket); Physical geography; Geography","score_opus":0.03117271890171555,"score_gpt":0.23385846181822323,"score_spread":0.20268574291650768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401837528","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98359495,0.005990222,0.0000011502402,0.0075828084,0.0009019432,0.000050060047,0.000019000054,0.0000015282028,0.0018583561],"genre_scores_gemma":[0.9995649,0.000027422955,0.000052848598,0.00020905539,0.0000859619,4.0686395e-8,0.000005182122,8.123014e-7,0.000053771997],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988266,0.00021371362,0.00018646693,0.00012662556,0.00021479279,0.00043179182],"domain_scores_gemma":[0.99916106,0.0004234302,0.000039043854,0.000054382643,0.000027090615,0.0002949737],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010909317,0.00007302029,0.00010936914,0.00023810653,0.0003910578,0.00020133638,0.0003035079,0.000051498297,0.0008519306],"category_scores_gemma":[0.0001361792,0.000043536176,0.000020835267,0.0004491959,0.000569688,0.0002562401,0.0000024744065,0.00044135118,0.000009314585],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000026000173,2.5233956e-7,0.997613,0.000006711006,0.000004849179,0.0004563641,0.00061714527,0.0004902707,3.5253953e-7,0.00024895687,0.00031376944,0.0002457172],"study_design_scores_gemma":[0.00006573304,0.00006164282,0.99458253,0.00003080636,0.0000049513897,0.0012103118,0.00081201614,0.0012797737,0.000002527207,0.00066991214,0.0012225597,0.000057205743],"about_ca_topic_score_codex":0.78522164,"about_ca_topic_score_gemma":0.9998478,"teacher_disagreement_score":0.21462621,"about_ca_system_score_codex":0.0000010633128,"about_ca_system_score_gemma":0.0029970068,"threshold_uncertainty_score":0.9328042},"labels":[],"label_agreement":null},{"id":"W4402255239","doi":"10.1139/cjes-2024-0087","title":"Petrochemistry, mineralogy, and Nd isotopic analyses of Tithonian alkaline lamprophyric intrusions, north-central Newfoundland, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University; Government of Newfoundland and Labrador","funders":"","keywords":"Petrochemistry; Geology; Geochemistry; Intrusion; Mineralogy","score_opus":0.026087794868188026,"score_gpt":0.25887745545217505,"score_spread":0.23278966058398703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402255239","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98758626,0.009077044,0.0000060596426,0.0013655929,0.0005194414,0.00003852193,0.000048601432,0.0000020837974,0.0013564095],"genre_scores_gemma":[0.9989669,0.00015661192,0.00031270887,0.0001120849,0.00011462057,1.1239258e-7,0.000010615395,0.0000012614656,0.00032511036],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883944,0.000073243755,0.00027993252,0.0001648455,0.00021838165,0.00042414048],"domain_scores_gemma":[0.99903774,0.00018346636,0.00008457049,0.000075609016,0.00008327907,0.0005353348],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034263975,0.00009769363,0.0002135055,0.00028592529,0.00024571543,0.00007366264,0.000291448,0.00005628746,0.001279775],"category_scores_gemma":[0.00011114517,0.00007026948,0.00004427927,0.0005186122,0.0007932707,0.00014622348,0.000006359195,0.00024192297,0.000005477866],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000052690234,0.0000014165893,0.99836314,0.000029610277,0.000028474784,0.00031204446,0.0000712884,0.000330542,0.000051099625,0.000026581072,0.00025747524,0.00052307395],"study_design_scores_gemma":[0.00010315851,0.00016019215,0.9910152,0.000042159918,0.000027114533,0.00083599344,0.00011941822,0.0012804705,0.0000654692,0.00011269608,0.006152867,0.00008525879],"about_ca_topic_score_codex":0.70707047,"about_ca_topic_score_gemma":0.99904335,"teacher_disagreement_score":0.2919729,"about_ca_system_score_codex":0.0000014905415,"about_ca_system_score_gemma":0.004497871,"threshold_uncertainty_score":0.9996332},"labels":[],"label_agreement":null},{"id":"W4402432768","doi":"10.1139/cjes-2024-0083","title":"Immature <i>Daspletosaurus</i> sp. specimens from the Dinosaur Park Formation provide insight into ontogenetically invariant tyrannosaurid cranial morphology","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; University of Alberta","funders":"Dinosaur Research Institute","keywords":"Morphology (biology); Geology; Biology; Paleontology","score_opus":0.014737292594064184,"score_gpt":0.205993288076068,"score_spread":0.19125599548200384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402432768","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9450677,0.022903126,0.0003973919,0.020549012,0.003558203,0.0001830421,0.0002507137,0.000016098073,0.0070746886],"genre_scores_gemma":[0.99563146,0.00020385205,0.0013450872,0.0018497768,0.00087196083,6.499315e-7,0.00004367947,0.0000024531155,0.000051077222],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982271,0.00026971978,0.00045738957,0.00026713705,0.00026119815,0.00051744416],"domain_scores_gemma":[0.9987075,0.00050338026,0.00014631505,0.00014017997,0.00008369435,0.0004189694],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009252349,0.00016700469,0.00023884742,0.00021441848,0.00070228893,0.00021758387,0.00070862216,0.0001714732,0.0020351333],"category_scores_gemma":[0.00021223437,0.00009977157,0.00011237616,0.00046056617,0.0011704805,0.0006576451,0.000009566313,0.0004570839,0.00021259702],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029601727,0.00001878118,0.9499356,0.000032902728,0.00018405705,0.002548224,0.006074323,0.0023522945,0.0036610535,0.0046586576,0.015382556,0.014855538],"study_design_scores_gemma":[0.00015501521,0.0003439121,0.8427561,0.00006131105,0.00003638794,0.0009776886,0.00019283335,0.0018475852,0.00012013964,0.004971321,0.1483834,0.00015430343],"about_ca_topic_score_codex":0.020435061,"about_ca_topic_score_gemma":0.70385295,"teacher_disagreement_score":0.68341786,"about_ca_system_score_codex":0.000005947453,"about_ca_system_score_gemma":0.0018387472,"threshold_uncertainty_score":0.99887717},"labels":[],"label_agreement":null},{"id":"W4402433060","doi":"10.1139/cjes-2024-0032","title":"Petrochemical and geochronological constraints on the origin of the Sops Arm group, the most westerly Silurian volcano-sedimentary extensional basin on the western Newfoundland composite Laurentian margin","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Geological Survey of Canada; Natural Resources Canada; Memorial University of Newfoundland; Government of Newfoundland and Labrador","funders":"Department of Natural Resources, Government of Newfoundland and Labrador","keywords":"Geology; Group (periodic table); Structural basin; Extensional definition; Margin (machine learning); Sedimentary rock; Volcano; Geochemistry; Paleontology; Rift; Seismology; Tectonics","score_opus":0.017523583963209684,"score_gpt":0.20251957253019234,"score_spread":0.18499598856698266,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402433060","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9338612,0.00096658827,0.000003510116,0.063183546,0.00035488766,0.0001047916,0.00007468943,0.000003595584,0.0014472121],"genre_scores_gemma":[0.9951487,0.000029130199,0.00004128314,0.004507493,0.00017546312,5.551364e-7,0.000005559668,0.0000016826343,0.0000901102],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983307,0.00021566832,0.00033364852,0.00025320356,0.00047846133,0.0003883023],"domain_scores_gemma":[0.99819946,0.0011309243,0.00014154341,0.0001686631,0.0000550538,0.00030436754],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010332935,0.00017014582,0.00021563617,0.00009285219,0.00070795993,0.00030974715,0.0008235791,0.000060710492,0.005797513],"category_scores_gemma":[0.00012643464,0.000057617224,0.00016014178,0.00051512715,0.0031472754,0.00010829933,0.000024204408,0.0005403129,0.00003153866],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000049931532,0.000031218642,0.9869296,0.000010007475,0.00010315373,0.00010941495,0.00030760944,0.00043679436,0.0005382471,0.002310841,0.0019960906,0.0071770935],"study_design_scores_gemma":[0.00014801041,0.0005429194,0.9810963,0.0001914582,0.00006277689,0.00029623898,0.0004908306,0.0010625884,0.00021737555,0.005591612,0.010160388,0.0001394772],"about_ca_topic_score_codex":0.015250628,"about_ca_topic_score_gemma":0.31658044,"teacher_disagreement_score":0.30132982,"about_ca_system_score_codex":0.000004793804,"about_ca_system_score_gemma":0.0003313071,"threshold_uncertainty_score":0.9995656},"labels":[],"label_agreement":null},{"id":"W4402737723","doi":"10.1139/cjes-2024-0074","title":"An unusual strophomenide brachiopod association in the Late Ordovician William Lake Lagerstätte, Williams Member of the Stony Mountain Formation (latest Katian), Manitoba","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Research Manitoba; University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Ordovician; Geology; Lagerstätte; Paleontology","score_opus":0.015430563624089299,"score_gpt":0.22587080491535597,"score_spread":0.21044024129126668,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402737723","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9877913,0.0017224354,0.000012373682,0.0016923107,0.00057873444,0.00011233712,0.000092882874,0.0000039787783,0.007993634],"genre_scores_gemma":[0.9995618,0.000030204537,0.00010120117,0.00018354112,0.000078744284,3.2745518e-7,0.000003986386,9.370978e-7,0.000039264185],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99834764,0.00032099796,0.00039969778,0.00011966319,0.00044981894,0.0003621629],"domain_scores_gemma":[0.9991366,0.00024347201,0.0002737686,0.000113549606,0.000065897155,0.00016667848],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021829354,0.000110700625,0.00015964094,0.00031227688,0.00046500226,0.00028113168,0.00061471836,0.00008522627,0.000107864296],"category_scores_gemma":[0.00009821355,0.00006309337,0.00009200082,0.0009356172,0.00035404495,0.0012429585,0.000001033304,0.0003516009,0.000005534622],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004313719,0.0000052687387,0.98950756,0.0000082788065,0.000013581055,0.00003634432,0.0017913177,0.0023044834,0.000030073954,0.00019453857,0.000076718075,0.0060275327],"study_design_scores_gemma":[0.000093958966,0.00021019585,0.99217397,0.00007150591,0.000018123477,0.00006578794,0.0021935217,0.0025596016,0.00004329645,0.0007383103,0.0017506687,0.00008108195],"about_ca_topic_score_codex":0.01122987,"about_ca_topic_score_gemma":0.97204316,"teacher_disagreement_score":0.9608133,"about_ca_system_score_codex":0.000007236586,"about_ca_system_score_gemma":0.0007928764,"threshold_uncertainty_score":0.9953544},"labels":[],"label_agreement":null},{"id":"W4402738970","doi":"10.1139/cjes-2024-0080","title":"An investigation of subaqueous failures triggered by the 1935 CE M<sub>w</sub> 6.1 Témiscaming earthquake, Quebec, Canada, as an analogue for a paleoseismic study","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Nuclear Waste Management Organization","keywords":"Geology; Seismology; Geochemistry","score_opus":0.017954374799337883,"score_gpt":0.2221435884662137,"score_spread":0.2041892136668758,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402738970","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927435,0.0049153133,0.000015614633,0.0010406428,0.00057502167,0.00032359728,0.00025816524,0.000010035925,0.00011814276],"genre_scores_gemma":[0.9993111,0.000040576866,0.000055145752,0.0003400248,0.00016774562,0.0000018900129,0.000025708603,0.000005766707,0.000052030435],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99779814,0.00025665274,0.00054346665,0.00032371344,0.0005522759,0.0005257235],"domain_scores_gemma":[0.99828434,0.0004858366,0.00025050069,0.00019223301,0.00015555501,0.0006315415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015732502,0.0001990116,0.00032125754,0.00035175163,0.0007881654,0.00040400136,0.000621552,0.00005675994,0.00014595618],"category_scores_gemma":[0.00014638908,0.00013265047,0.00009729767,0.0007445975,0.00059937517,0.00069911324,0.000004330086,0.00023753734,0.0000035053993],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058729816,0.00002799803,0.8542484,0.000067625035,0.00026614178,0.0003308287,0.012150642,0.0046894527,0.0011281577,0.00016261854,0.0054705148,0.12139889],"study_design_scores_gemma":[0.00033489332,0.0019319255,0.97302186,0.00010459786,0.000092145805,0.00011811631,0.014127963,0.0031542596,0.0018836968,0.00063841825,0.0042909854,0.00030114912],"about_ca_topic_score_codex":0.9060948,"about_ca_topic_score_gemma":0.9997456,"teacher_disagreement_score":0.12109774,"about_ca_system_score_codex":0.000009350852,"about_ca_system_score_gemma":0.008071109,"threshold_uncertainty_score":0.9975522},"labels":[],"label_agreement":null},{"id":"W4402905516","doi":"10.1139/cjes-2023-0123","title":"Changing your perspective: the impact of different visualisation methods on seismic hazard maps","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geographic Information Systems Studies","field":"Social Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Alliance de recherche numérique du Canada; Norges Forskningsråd","keywords":"Geology; Seismology; Visualization; Perspective (graphical); Seismic hazard; Hazard; Data mining; Computer science; Artificial intelligence","score_opus":0.06644458252144313,"score_gpt":0.40958159663474897,"score_spread":0.3431370141133058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402905516","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9603825,0.0019162291,0.0011029803,0.005284671,0.0018699822,0.00020893032,0.00001715317,0.00001252645,0.029205007],"genre_scores_gemma":[0.9992895,0.00004485664,0.00011795388,0.00006113049,0.00023885265,0.0000013924366,1.676589e-7,0.0000028273028,0.00024333368],"study_design_codex":"qualitative","study_design_gemma":"qualitative","domain_scores_codex":[0.99855965,0.00028508433,0.0002942615,0.000087332795,0.00044105077,0.00033259307],"domain_scores_gemma":[0.99893236,0.00026251428,0.00021698454,0.000065899265,0.0003215366,0.00020070553],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0043934993,0.00008442518,0.00016294552,0.0009512392,0.0010382172,0.00030834283,0.0003218135,0.00003475736,0.000089150635],"category_scores_gemma":[0.0004218818,0.00004688263,0.00019696867,0.0012504137,0.00075801736,0.00041046296,0.0000095492205,0.00014589475,0.000006742552],"study_design_candidate":"qualitative","study_design_consensus":"qualitative","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010229126,0.000015164851,0.045877084,0.000035833342,0.00029215578,0.000020789867,0.680909,0.00443035,0.00009184958,0.25581577,0.0014986179,0.011003158],"study_design_scores_gemma":[0.0002821335,0.00092416,0.21798304,0.00073533005,0.00006376732,0.000071602866,0.73201126,0.0040315245,0.0002957189,0.02696911,0.016297007,0.000335339],"about_ca_topic_score_codex":0.02224728,"about_ca_topic_score_gemma":0.036700867,"teacher_disagreement_score":0.22884665,"about_ca_system_score_codex":0.00007177894,"about_ca_system_score_gemma":0.0015344541,"threshold_uncertainty_score":0.98426366},"labels":[],"label_agreement":null},{"id":"W4403115773","doi":"10.1139/cjes-2024-0053","title":"Mapping of fluid venting and attenuation of hydrate bearing sediments from offshore Oregon","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"National Science Foundation","keywords":"Geology; Submarine pipeline; Geochemistry; Bearing (navigation); Attenuation; Seismology; Oceanography; Geomorphology; Mining engineering","score_opus":0.018759282384333414,"score_gpt":0.2199140666032318,"score_spread":0.20115478421889837,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403115773","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959866,0.0018131215,0.000065555476,0.00015562889,0.00029890836,0.00003779151,0.00000572532,0.0000014439642,0.001635258],"genre_scores_gemma":[0.9989208,0.00004196026,0.000918685,0.000018011206,0.000035086618,1.4809872e-7,6.409602e-7,0.000003222208,0.00006144465],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999161,0.000031247306,0.00029574448,0.000119653465,0.00022983608,0.00016252187],"domain_scores_gemma":[0.9995498,0.000045517765,0.00016422212,0.000049212853,0.000014378184,0.00017687542],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007131503,0.00005922108,0.00012546299,0.00016699891,0.00010115063,0.000048591504,0.00014915617,0.000030634783,0.000425247],"category_scores_gemma":[0.00003413806,0.000045756424,0.00003660891,0.00042076103,0.00032574165,0.00028573198,0.00002312964,0.000096965676,0.000006621701],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000066128487,0.000011362797,0.7509787,0.00005962936,0.000080087855,0.00006908493,0.0086289095,0.014208603,0.20580804,0.00023755735,0.00012194269,0.019789463],"study_design_scores_gemma":[0.0004424587,0.0004675249,0.8842874,0.0018395974,0.00008127995,0.00007518241,0.0031162505,0.04531593,0.054826815,0.0047762683,0.004432521,0.00033876157],"about_ca_topic_score_codex":0.0046525537,"about_ca_topic_score_gemma":0.0029383008,"teacher_disagreement_score":0.15098123,"about_ca_system_score_codex":0.000009326233,"about_ca_system_score_gemma":0.00012496645,"threshold_uncertainty_score":0.70333004},"labels":[],"label_agreement":null},{"id":"W4403182274","doi":"10.1139/cjes-2024-0026","title":"Nd isotope mapping in the Go Home region of Georgian Bay: a misunderstood key to the geology of the Central Gneiss Belt, Grenville Province of Ontario","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"","keywords":"Geology; Gneiss; Bay; Geochemistry; Georgian; Key (lock); Isotope; Seismology; Earth science; Metamorphic rock; Oceanography","score_opus":0.019018980957896444,"score_gpt":0.18052828397547369,"score_spread":0.16150930301757724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403182274","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98295075,0.0015490721,0.000015454292,0.012734026,0.00021665223,0.00011744286,0.000011653498,8.004274e-7,0.0024041408],"genre_scores_gemma":[0.99918944,0.000014102346,0.000121709236,0.00034177277,0.00003962634,2.314696e-7,9.651501e-7,7.649251e-7,0.0002913905],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861497,0.00014209165,0.000404457,0.00015466344,0.00031867565,0.00036514873],"domain_scores_gemma":[0.99922967,0.00019188858,0.0001885228,0.0001433275,0.000061864666,0.00018475631],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00091454503,0.00009124682,0.00022948837,0.00019374945,0.00016544414,0.000043827677,0.00094917207,0.00004470691,0.00074095436],"category_scores_gemma":[0.000121527264,0.000038964776,0.00015166364,0.0010478786,0.000844483,0.00009995001,0.000016240432,0.00024255994,0.0000043040563],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000072358207,0.000006891072,0.9907502,0.000017055632,0.00001835915,0.000043682077,0.003130989,0.0035447443,0.000047996862,0.00034371653,0.00017591825,0.0019132469],"study_design_scores_gemma":[0.00006380231,0.0002368866,0.98599076,0.00009772178,0.000019428464,0.0001099051,0.001262754,0.000549165,0.00008293892,0.0032512532,0.008272224,0.00006312876],"about_ca_topic_score_codex":0.33967963,"about_ca_topic_score_gemma":0.98420894,"teacher_disagreement_score":0.6445293,"about_ca_system_score_codex":0.0000065559893,"about_ca_system_score_gemma":0.0016289144,"threshold_uncertainty_score":0.81129307},"labels":[],"label_agreement":null},{"id":"W4403290192","doi":"10.1139/cjes-2024-0067","title":"Relative timing and controls on advanced argillic and conventional alteration of the Neoarchean Onaman volcanogenic massive sulfide deposit, Ontario, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Laurentian University","funders":"","keywords":"Geology; Geochemistry; Argillic alteration; Sulfide; Volcanogenic massive sulfide ore deposit; Pyrite; Sphalerite; Volcanic rock","score_opus":0.014231516428444618,"score_gpt":0.20812975693363794,"score_spread":0.19389824050519333,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403290192","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98794514,0.00084280525,0.0015014205,0.0075643733,0.00042192874,0.00008179965,0.000005668139,0.0000020881557,0.0016348026],"genre_scores_gemma":[0.9983511,0.000003922221,0.0009080438,0.00020926482,0.000022392205,6.470924e-7,3.0402782e-7,7.299509e-7,0.0005036075],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9992339,0.00004539949,0.00019421788,0.00015206718,0.00020536606,0.00016904235],"domain_scores_gemma":[0.9993585,0.00015862146,0.00012531657,0.00007098677,0.000099343495,0.00018726122],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000345573,0.00006807255,0.000103353166,0.00007661464,0.0002963312,0.00013163657,0.00025672803,0.000021465423,0.00001916822],"category_scores_gemma":[0.00011963765,0.000046934143,0.000032787375,0.00018428265,0.00025773727,0.00029883804,0.000021911219,0.00016342501,1.6081528e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006868747,0.000036543483,0.41009152,0.00026155196,0.00042722304,0.0011873218,0.019545682,0.054535378,0.029159984,0.4418138,0.0017839675,0.041088354],"study_design_scores_gemma":[0.0014390786,0.0011302317,0.7917241,0.0018498652,0.00007205893,0.0015450901,0.001243414,0.08969468,0.024937969,0.047334082,0.03841091,0.0006185451],"about_ca_topic_score_codex":0.29801497,"about_ca_topic_score_gemma":0.9715915,"teacher_disagreement_score":0.67357653,"about_ca_system_score_codex":0.000033992896,"about_ca_system_score_gemma":0.0035077229,"threshold_uncertainty_score":0.7066596},"labels":[],"label_agreement":null},{"id":"W4403409326","doi":"10.1139/cjes-2024-0095","title":"Crustal stress near the Yakutat microplate collision from probabilistic earthquake focal mechanisms","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon University; University of Calgary; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Collision; Focal mechanism; Probabilistic logic; Stress (linguistics); Tectonics; Statistics; Computer science","score_opus":0.019615462363263426,"score_gpt":0.21567446831904363,"score_spread":0.1960590059557802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403409326","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98132724,0.011840005,0.0001829844,0.001566336,0.002139488,0.00014510548,0.00032452503,0.000015884285,0.0024584387],"genre_scores_gemma":[0.9981378,0.000088482564,0.001109308,0.00021957853,0.00024092603,3.9258325e-7,0.000006355881,0.0000043440937,0.00019283942],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99819,0.000113149465,0.00038040665,0.0002824295,0.00048741867,0.00054663204],"domain_scores_gemma":[0.9986612,0.00051711476,0.000114064904,0.00014347273,0.000100885896,0.0004632418],"candidate_categories":["sts","scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00091848784,0.00017588535,0.00023205121,0.00019127424,0.0013345854,0.0013774253,0.00056728104,0.0000667388,0.0021212543],"category_scores_gemma":[0.00018160249,0.00010126921,0.00014419209,0.00066877645,0.0012163202,0.00042225374,0.000011719569,0.00035023832,0.00022329098],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014309508,0.00005042976,0.5205627,0.00017268614,0.0007115928,0.0068138293,0.019405976,0.10385944,0.00025257526,0.011150809,0.0077396603,0.3291372],"study_design_scores_gemma":[0.00036815496,0.0012398467,0.86734986,0.00059495744,0.000120733384,0.0005449083,0.0030651442,0.026225256,0.0005597172,0.019499233,0.0799254,0.000506779],"about_ca_topic_score_codex":0.043199666,"about_ca_topic_score_gemma":0.59772223,"teacher_disagreement_score":0.5545226,"about_ca_system_score_codex":0.0000036039082,"about_ca_system_score_gemma":0.0021325175,"threshold_uncertainty_score":0.99996555},"labels":[],"label_agreement":null},{"id":"W4403409385","doi":"10.1139/cjes-2024-0072","title":"Bridging the gap between Quebec and Newfoundland: new insights on the protracted and diachronic history of the Anticosti foreland basin","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Foreland basin; Geology; Structural basin; Bridging (networking); Paleontology","score_opus":0.036083268312056015,"score_gpt":0.20912547496392053,"score_spread":0.1730422066518645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403409385","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97712237,0.013652998,0.000015301943,0.006703578,0.0003232066,0.00010260016,0.000010102163,0.0000020766622,0.0020677426],"genre_scores_gemma":[0.99905926,0.000106183565,0.000019554658,0.00023750289,0.00011226565,1.2725262e-7,6.675563e-7,8.3056136e-7,0.0004636075],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99934196,0.000071112496,0.00016863126,0.00008158345,0.0001773793,0.00015932697],"domain_scores_gemma":[0.99924666,0.00040013107,0.00009342281,0.00006220481,0.00003194898,0.00016562422],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005467715,0.00006561854,0.000095363204,0.000091266724,0.00037624507,0.00020456196,0.00025383668,0.000026247979,0.0002356701],"category_scores_gemma":[0.00014699128,0.000024392626,0.000031269075,0.00025552444,0.00071534095,0.00029043297,0.0000052708124,0.00019460155,0.0000035535872],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045405777,0.000001558496,0.9539922,0.000029388933,0.000017476008,0.0000083479,0.0028053508,0.00038048002,0.000007060012,0.0018899421,0.0017681945,0.039095465],"study_design_scores_gemma":[0.000042854932,0.00012400052,0.93970895,0.000104427534,0.000015993572,0.000041481206,0.0001400231,0.0012545435,0.00000704144,0.0022244307,0.056293476,0.00004276176],"about_ca_topic_score_codex":0.10119139,"about_ca_topic_score_gemma":0.6136635,"teacher_disagreement_score":0.5124721,"about_ca_system_score_codex":0.000004587859,"about_ca_system_score_gemma":0.0019092548,"threshold_uncertainty_score":0.90479386},"labels":[],"label_agreement":null},{"id":"W4403462498","doi":"10.1139/cjes-2024-0085","title":"The lithosphere-asthenosphere boundary and lithosphere replacement as informed by mantle xenoliths and their host lavas","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Lithosphere; Asthenosphere; Xenolith; Mantle (geology); Geophysics; Mantle convection; Lava; Petrology; Geochemistry; Seismology; Volcano; Tectonics","score_opus":0.0077878436462324434,"score_gpt":0.19599775140699513,"score_spread":0.18820990776076268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403462498","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.905588,0.07388797,0.000005719699,0.0051315823,0.00018726627,0.000059367372,0.000027654505,0.000007484516,0.015105009],"genre_scores_gemma":[0.99608827,0.001553099,0.00016970753,0.00045935786,0.00007033379,3.5857923e-7,0.000003068641,0.000001905734,0.0016538801],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987481,0.000049305447,0.0003016011,0.00022251473,0.00023361976,0.00044480764],"domain_scores_gemma":[0.99871963,0.00035326395,0.000093159964,0.00009531943,0.000061482475,0.00067715795],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00073580403,0.00014903824,0.00018830366,0.000040703046,0.00082490157,0.0009575872,0.00031963034,0.000055274348,0.0038723522],"category_scores_gemma":[0.00016131336,0.00007231646,0.00007096635,0.00040786748,0.0011343899,0.00034485722,0.000015203884,0.00023270397,0.000045731507],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000040881016,0.000007302048,0.8957072,0.00004317092,0.00011954516,0.000113512215,0.0013594348,0.00005492075,0.000041723026,0.0010191464,0.007617732,0.09387542],"study_design_scores_gemma":[0.00021399031,0.0011057777,0.22761749,0.00017937229,0.00004496151,0.00047391152,0.005156935,0.002315766,0.00025130954,0.02968144,0.7326227,0.0003363968],"about_ca_topic_score_codex":0.020654187,"about_ca_topic_score_gemma":0.25613636,"teacher_disagreement_score":0.7250049,"about_ca_system_score_codex":0.0000024859473,"about_ca_system_score_gemma":0.0007787421,"threshold_uncertainty_score":0.99703825},"labels":[],"label_agreement":null},{"id":"W4403624101","doi":"10.1139/cjes-2024-0020","title":"New constraints to subduction zone arc and backarc mantle temperatures: a test of the corner flow model","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Mantle (geology); Seismology; Arc (geometry); Geochemistry; Geophysics; Petrology; Tectonics; Geometry","score_opus":0.015146903691868852,"score_gpt":0.1912171273791199,"score_spread":0.17607022368725103,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403624101","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918582,0.001479076,0.0002984003,0.0045215613,0.00026183145,0.000045361092,0.00006180401,0.0000025181942,0.0014712384],"genre_scores_gemma":[0.99618864,0.00002175817,0.002901273,0.00027059257,0.00008020658,5.131406e-8,9.243507e-7,6.760707e-7,0.0005358709],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992387,0.00002106632,0.0001867179,0.0001369753,0.00020956044,0.00020693154],"domain_scores_gemma":[0.99924403,0.00009203739,0.000039757717,0.00005708398,0.000059941267,0.00050715945],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00033776305,0.00006989696,0.00012719896,0.00014093916,0.00015817782,0.00012600451,0.00023797862,0.000028341989,0.0027569707],"category_scores_gemma":[0.0001779732,0.00003622536,0.000067815214,0.000589947,0.00052181724,0.0001397725,0.0000061130763,0.00013877964,0.000018449615],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012651814,0.000008280293,0.850285,0.000032531272,0.000043907385,0.00008651269,0.000875464,0.09830793,0.0032798164,0.0005578736,0.003662775,0.04284725],"study_design_scores_gemma":[0.0002456741,0.0007182249,0.7389112,0.0003891828,0.00010320561,0.00084024144,0.0008781232,0.22292408,0.0030368855,0.025625618,0.0059568575,0.0003706931],"about_ca_topic_score_codex":0.008830684,"about_ca_topic_score_gemma":0.2302479,"teacher_disagreement_score":0.22141722,"about_ca_system_score_codex":9.368689e-7,"about_ca_system_score_gemma":0.00075612345,"threshold_uncertainty_score":0.99815464},"labels":[],"label_agreement":null},{"id":"W4403830095","doi":"10.1139/cjes-2023-0125","title":"Occurrence of <i>Centrosaurus apertus</i> (Ceratopsidae: Centrosaurinae) in Saskatchewan, Canada, and expanded dinosaur diversity in the easternmost exposure of the Late Cretaceous (Campanian) Dinosaur Park Formation","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Dinosaur Research Institute","keywords":"Cretaceous; Geology; Paleontology; Diversity (politics)","score_opus":0.014880007149322517,"score_gpt":0.19320939414611585,"score_spread":0.17832938699679332,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403830095","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99319667,0.00448257,0.000004400355,0.0010958019,0.0005723439,0.00010461335,0.00029807125,0.0000012122975,0.00024429895],"genre_scores_gemma":[0.99962825,0.000086560365,0.00001607084,0.00022370917,0.000023238956,2.0165463e-7,0.0000053365034,5.2353255e-7,0.000016120928],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99864674,0.00023830935,0.000369503,0.00012948993,0.00027837185,0.00033760973],"domain_scores_gemma":[0.99930996,0.00022407899,0.00018265127,0.00009372889,0.000046451074,0.0001431258],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007486657,0.00010323768,0.00020164043,0.00015314006,0.0002960544,0.000038872324,0.00052500016,0.0000630425,0.000086765656],"category_scores_gemma":[0.00008215334,0.00006056721,0.000047502108,0.0005207412,0.0006317039,0.00036836843,0.000017617598,0.00025115698,9.115227e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015311327,0.000003946904,0.9949954,0.000024912584,0.000005737271,0.000065672655,0.0025803642,0.0006421049,0.00003182276,0.000021469798,0.00012156275,0.0014916725],"study_design_scores_gemma":[0.00017313471,0.000121566576,0.994635,0.00011387417,0.000010047415,0.00020449604,0.0030658762,0.0007772233,0.000048582435,0.00014199755,0.0006382352,0.00006995424],"about_ca_topic_score_codex":0.46244997,"about_ca_topic_score_gemma":0.9981328,"teacher_disagreement_score":0.53568286,"about_ca_system_score_codex":0.000007835043,"about_ca_system_score_gemma":0.0017207182,"threshold_uncertainty_score":0.54112965},"labels":[],"label_agreement":null},{"id":"W4403965560","doi":"10.1139/cjes-2024-0039","title":"Environmental associations and the paleoecological significance of the genus <i>Pyxidicula</i> Ehrenberg,1838 and <i>Pyxidicula muskegii</i> sp. nov. in the Hudson and James Bay region peatlands, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Ontario Forest Research Institute; Carleton University; University of Toronto; Université du Québec à Montréal; Ministry of Natural Resources and Forestry","funders":"Natural Sciences and Engineering Research Council of Canada; Government of Ontario; Ontario Ministry of Natural Resources and Forestry; Ministry of Natural Resources","keywords":"Peat; Bay; Geology; Genus; Paleoecology; Oceanography; Ecology; Geography; Paleontology; Archaeology; Biology","score_opus":0.00840201141681087,"score_gpt":0.18653910751640337,"score_spread":0.1781370960995925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403965560","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.986223,0.002880776,0.000004584981,0.009528419,0.00018710086,0.0001667175,0.000021918075,0.0000011816699,0.0009863403],"genre_scores_gemma":[0.99830806,0.0005463458,0.000025548683,0.0010082428,0.00004457426,0.0000036072502,9.861897e-7,0.000002957028,0.00005965416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99871767,0.00023316893,0.00026261003,0.00019821976,0.0003042656,0.0002840741],"domain_scores_gemma":[0.999158,0.00042677758,0.00014678828,0.00009960953,0.000005217784,0.00016359329],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011062372,0.000110752255,0.00018375844,0.00004565268,0.00045873938,0.000121224206,0.00033698382,0.000050473915,0.00004736282],"category_scores_gemma":[0.00009656208,0.000050961764,0.000044035056,0.00026730678,0.0017597126,0.0001409039,0.000050897565,0.00024023272,4.805785e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000054602606,0.0000063911193,0.9951912,0.0000037066698,0.000009376627,0.00009195535,0.000846343,0.000117540236,0.000080306956,0.00021601214,0.0020127431,0.001418933],"study_design_scores_gemma":[0.00033204874,0.000086397806,0.97065467,0.000023252347,0.000026113737,0.0003991851,0.00087326334,0.00024197939,0.0000239031,0.00028858343,0.026971282,0.00007930813],"about_ca_topic_score_codex":0.10623428,"about_ca_topic_score_gemma":0.8927976,"teacher_disagreement_score":0.7865633,"about_ca_system_score_codex":0.000031631054,"about_ca_system_score_gemma":0.00033945387,"threshold_uncertainty_score":0.8997174},"labels":[],"label_agreement":null},{"id":"W4404066806","doi":"10.1139/cjes-2024-0024","title":"New constraints on the timing and nature of metamorphism in the eastern Meguma terrane, Nova Scotia, Canada","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia; Golder Associates (Canada); St. Francis Xavier University; Acadia University","funders":"Natural Sciences and Engineering Research Council of Canada; Acadia University","keywords":"Terrane; Nova scotia; Metamorphism; Geology; Geochemistry; Seismology; Paleontology; Mineralogy; Tectonics; Oceanography","score_opus":0.03800493588408924,"score_gpt":0.24884513918540055,"score_spread":0.2108402033013113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404066806","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97042656,0.004873552,0.0000029636751,0.015326706,0.0006004907,0.000063844716,0.0000145079985,6.8623535e-7,0.008690693],"genre_scores_gemma":[0.99894667,0.000014031261,0.00009298081,0.00081706845,0.000048240032,3.7747203e-8,7.0627965e-7,7.404173e-7,0.00007953835],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989523,0.00016659958,0.00018928187,0.00011439742,0.0002866081,0.0002907825],"domain_scores_gemma":[0.9989064,0.0007323057,0.000056272907,0.00007392531,0.000030665444,0.00020047821],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015545047,0.00007279588,0.0001302794,0.00022515027,0.00017355749,0.000092296636,0.00048016995,0.00006109406,0.0019170695],"category_scores_gemma":[0.00015962693,0.00003574924,0.000029388566,0.00041504911,0.0009667692,0.00011994115,0.0000033267775,0.0005553081,0.000012432212],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000003576555,5.7620724e-7,0.9953198,0.0000060043594,0.000012724394,0.0003159356,0.00047992467,0.00012996385,0.0000010688431,0.0008005608,0.0006702032,0.0022596607],"study_design_scores_gemma":[0.00008389517,0.00013845395,0.9939003,0.00011026995,0.000010503598,0.0010168622,0.0012263529,0.00080908596,0.000025814477,0.00076455314,0.0018540544,0.00005983722],"about_ca_topic_score_codex":0.5911528,"about_ca_topic_score_gemma":0.9984419,"teacher_disagreement_score":0.40728906,"about_ca_system_score_codex":5.54637e-7,"about_ca_system_score_gemma":0.0036244334,"threshold_uncertainty_score":0.9989953},"labels":[],"label_agreement":null},{"id":"W4404097174","doi":"10.1139/cjes-2024-0088","title":"Characteristics of the Albian Westgate Formation polygonal fault system","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Fault (geology); Paleontology; Seismology","score_opus":0.017336334014521705,"score_gpt":0.18763528823963269,"score_spread":0.170298954225111,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404097174","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9908236,0.0012374427,0.000024845236,0.0016606975,0.0011377761,0.00004192707,0.0000658925,0.000003971425,0.00500384],"genre_scores_gemma":[0.9995292,0.00001648091,0.0000569563,0.00009048713,0.00014160405,6.6537496e-8,0.0000010406189,5.371381e-7,0.00016364385],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99917924,0.00004175244,0.00024986122,0.00007511811,0.00024340326,0.00021063643],"domain_scores_gemma":[0.9994978,0.00008194715,0.00011446142,0.000045728993,0.000069704976,0.00019038912],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038291642,0.00006165866,0.00012811167,0.00008217192,0.0003015943,0.00011019955,0.00029639798,0.000024226334,0.0002739401],"category_scores_gemma":[0.000070450165,0.000030087873,0.00008513113,0.00039864247,0.00041588332,0.00024868269,0.0000052918763,0.00011438864,0.00008674749],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000077520235,0.000004788589,0.9353925,0.00013536515,0.000033195407,0.00008898931,0.00090564083,0.0015253659,0.00003397786,0.0035263356,0.0003389809,0.05800713],"study_design_scores_gemma":[0.000027042985,0.00013931222,0.98599225,0.00014163669,0.00001114332,0.00008662803,0.0002967584,0.0037891492,0.00006148003,0.00056334556,0.00884097,0.00005027499],"about_ca_topic_score_codex":0.0062548313,"about_ca_topic_score_gemma":0.06306037,"teacher_disagreement_score":0.057956852,"about_ca_system_score_codex":0.0000014258329,"about_ca_system_score_gemma":0.00032893484,"threshold_uncertainty_score":0.95403636},"labels":[],"label_agreement":null},{"id":"W4404842249","doi":"10.1139/cjes-2024-0110","title":"The first <i>Otodus megalodon</i> remains from Canada and their predicted range limit","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Range (aeronautics); Limit (mathematics); Mathematics; Engineering","score_opus":0.016000014914260393,"score_gpt":0.18452698313537558,"score_spread":0.16852696822111518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404842249","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9021816,0.07075383,0.0000073756205,0.014265163,0.0025356768,0.00007190576,0.00031214822,0.0000084949925,0.009863807],"genre_scores_gemma":[0.99813956,0.00067762437,0.0000477442,0.0007218575,0.00022934256,1.9886696e-7,0.0000021185572,0.0000013326286,0.00018023846],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990356,0.000060084043,0.00022547568,0.00014902587,0.00018980721,0.00034000477],"domain_scores_gemma":[0.9987046,0.0006822547,0.0000712465,0.000075762495,0.000062246894,0.0004038559],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005917011,0.00010164306,0.00014106143,0.000096705844,0.0011980399,0.00027477278,0.00032088585,0.000036357975,0.00024034572],"category_scores_gemma":[0.00014724916,0.000054313045,0.000041036885,0.00031649953,0.0007940497,0.00021078468,0.0000042440483,0.00019387087,0.000005939565],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000040547907,3.912634e-7,0.9875174,0.0000032473254,0.000033887667,0.00008606716,0.0004912884,0.00007517366,5.512992e-7,0.000069889094,0.008867388,0.0028506462],"study_design_scores_gemma":[0.00005246791,0.000062438405,0.736598,0.000042159507,0.000008620572,0.00007919432,0.0006166151,0.00096421124,0.0000036818508,0.00028800347,0.26122493,0.0000596636],"about_ca_topic_score_codex":0.88304794,"about_ca_topic_score_gemma":0.9999753,"teacher_disagreement_score":0.25235754,"about_ca_system_score_codex":0.000003490583,"about_ca_system_score_gemma":0.0025496834,"threshold_uncertainty_score":0.9214475},"labels":[],"label_agreement":null},{"id":"W4405299922","doi":"10.1139/cjes-2024-0093","title":"Deep-Sea Borehole Fluid Pressure and Temperature Observations at Subduction Zones and their Geodynamic Implications","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Borehole; Geophysics; Geodynamics; Seismology; Tectonics; Paleontology","score_opus":0.015111108935463545,"score_gpt":0.20962177670792206,"score_spread":0.1945106677724585,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405299922","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97162783,0.023866188,0.00051642675,0.0033821862,0.00026719022,0.00004557523,0.00002627055,0.0000205062,0.00024784863],"genre_scores_gemma":[0.99887,0.0005752021,0.00022216389,0.000038619834,0.00008602093,0.0000017070462,0.000004819771,0.000005635893,0.00019584161],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99953353,0.00001584029,0.00014584855,0.0000969104,0.00007129036,0.00013660424],"domain_scores_gemma":[0.9995823,0.000025941737,0.000020071413,0.00006282598,0.00005716153,0.00025171574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016973578,0.00007187253,0.00009069101,0.00028847106,0.0003153809,0.00025900232,0.000090617395,0.00004171316,0.000033862165],"category_scores_gemma":[0.00002295353,0.000052260188,0.000034188794,0.000491268,0.00015677592,0.00042433297,0.0000058906453,0.000108493674,0.0000017694102],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004503673,0.000014158397,0.10611528,0.0002832408,0.00061929156,0.000050109185,0.010841613,0.79653656,0.062580466,0.010130965,0.006442502,0.006381279],"study_design_scores_gemma":[0.0001015932,0.000069710855,0.19084808,0.000101305326,0.00009098178,0.00030090575,0.0012072448,0.7611978,0.00057175785,0.0014633139,0.04381597,0.00023135802],"about_ca_topic_score_codex":0.0002654707,"about_ca_topic_score_gemma":0.06311379,"teacher_disagreement_score":0.08473279,"about_ca_system_score_codex":0.000006589546,"about_ca_system_score_gemma":0.00016462762,"threshold_uncertainty_score":0.95398194},"labels":[],"label_agreement":null},{"id":"W4405299933","doi":"10.1139/cjes-2024-0076","title":"Monitoring subseafloor temperature and fluid pressure in sealed ODP/IODP boreholes to constrain in-situ hydrological state and processes in igneous oceanic crust","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Gordon and Betty Moore Foundation; National Aeronautics and Space Administration; National Science Foundation","keywords":"Geology; Borehole; Igneous rock; Crust; Oceanic crust; Geochemistry; Petrology; Seismology; Paleontology; Subduction; Tectonics","score_opus":0.01162719817396364,"score_gpt":0.22179301087026032,"score_spread":0.2101658126962967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405299933","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98688585,0.011257128,6.897357e-7,0.00077674043,0.0001333215,0.00013053093,0.0000069482744,0.000002522825,0.0008062953],"genre_scores_gemma":[0.999075,0.0004877901,0.0002007763,0.00008503719,0.000028536046,0.0000015150301,1.6064958e-7,0.000004259696,0.000116904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988047,0.00007099773,0.00027722117,0.00026960322,0.0001921381,0.00038536542],"domain_scores_gemma":[0.9993791,0.00008223079,0.000040794843,0.000046716956,0.000010403007,0.00044078214],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00086878025,0.00011574322,0.00018906977,0.00031460737,0.000095160016,0.00022174502,0.00018666606,0.00006982699,0.00010986219],"category_scores_gemma":[0.00011281506,0.00008304362,0.000014026928,0.0009447666,0.0004807627,0.00031348667,0.000029064277,0.00034133007,0.0000049318087],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026253838,0.000020060002,0.9439684,0.00009112306,0.000010547978,0.0022563355,0.007119099,0.0247027,0.017356662,0.000032834047,0.00004482385,0.0043711476],"study_design_scores_gemma":[0.0004642922,0.0005074633,0.9893255,0.0009334107,0.000011677637,0.0005116335,0.0015134991,0.0015897385,0.002264961,0.0008565349,0.0017181415,0.00030314963],"about_ca_topic_score_codex":0.0014707743,"about_ca_topic_score_gemma":0.06524126,"teacher_disagreement_score":0.06377049,"about_ca_system_score_codex":0.000018095589,"about_ca_system_score_gemma":0.00036464934,"threshold_uncertainty_score":0.95181566},"labels":[],"label_agreement":null},{"id":"W4405301455","doi":"10.1139/cjes-2024-0069","title":"Three-dimensional geometry of sedimentary basins and Moho beneath Western Canada from ambient seismic noise tomography","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Seismic tomography; Tomography; Sedimentary basin; Seismic noise; Sedimentary rock; Paleontology; Tectonics; Mantle (geology)","score_opus":0.009966994190502228,"score_gpt":0.18663014233684858,"score_spread":0.17666314814634634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405301455","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9856256,0.010874657,0.00004224387,0.0014326866,0.0008485619,0.00003744757,0.0009983873,0.0000027193278,0.00013768129],"genre_scores_gemma":[0.998303,0.000055508546,0.0004984359,0.00094078993,0.00014259698,3.859844e-8,0.000020632224,0.0000025368415,0.000036483176],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99856496,0.000030088626,0.00034944437,0.00022988756,0.00049628457,0.00032931054],"domain_scores_gemma":[0.9989129,0.00015271995,0.00012381596,0.000090877904,0.000060724728,0.0006589718],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041336165,0.00013035997,0.00024298741,0.0005561196,0.00022174361,0.00015518288,0.00027927774,0.00003607757,0.001090859],"category_scores_gemma":[0.00001566634,0.00009664629,0.00010269962,0.00080084597,0.0003571979,0.00031592807,0.000007678379,0.00015321374,0.000004023692],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000394535,0.000002565522,0.98615557,0.000009375051,0.00007686716,0.00021970065,0.00006782511,0.009026989,0.00002861963,0.000009343187,0.0009156139,0.0034836102],"study_design_scores_gemma":[0.0001048419,0.0001727531,0.95465404,0.00015710766,0.000072119714,0.00008149039,0.00029252458,0.034012202,0.00012559156,0.00057831965,0.009599066,0.00014993301],"about_ca_topic_score_codex":0.9624496,"about_ca_topic_score_gemma":0.9948772,"teacher_disagreement_score":0.032427616,"about_ca_system_score_codex":0.0000047346716,"about_ca_system_score_gemma":0.0024929564,"threshold_uncertainty_score":0.99982226},"labels":[],"label_agreement":null},{"id":"W4405312757","doi":"10.1139/cjes-2024-0112","title":"Thermal control on the updip and downdip extents of megathrust earthquake rupture: revisiting Dr. Roy Hyndman's seminal contributions 30 years later","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Paleontology","score_opus":0.01611101924327021,"score_gpt":0.22626182022631394,"score_spread":0.21015080098304373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405312757","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9783504,0.012909286,0.000010061184,0.0029305974,0.00046749768,0.00011547356,0.00016890831,0.0000067503665,0.005041037],"genre_scores_gemma":[0.9990271,0.00013019628,0.000037204514,0.0003887009,0.00027120142,3.7353732e-7,0.0000016563774,0.000002805978,0.00014075986],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99854594,0.00012846163,0.00034234926,0.00018874559,0.00036732855,0.00042715238],"domain_scores_gemma":[0.99877256,0.0005760935,0.00014593227,0.00010348604,0.000103205275,0.00029870245],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016040005,0.00013460974,0.00024546604,0.00022534517,0.000521172,0.00027263557,0.0002898454,0.000052811094,0.0023631493],"category_scores_gemma":[0.00024104389,0.00007976852,0.00011052264,0.0003674875,0.0007454853,0.00025342265,0.0000064279125,0.0003138491,0.0000668608],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047328493,0.000012614395,0.8846311,0.00006159014,0.00035215972,0.0009617779,0.002745845,0.0025066182,0.00024648817,0.0042691575,0.0024392626,0.10172608],"study_design_scores_gemma":[0.00021976235,0.0003567659,0.98307693,0.00029729476,0.00005031178,0.00012388913,0.00047374313,0.0008505258,0.00008560256,0.00032555236,0.014016242,0.00012338776],"about_ca_topic_score_codex":0.0023589893,"about_ca_topic_score_gemma":0.014942516,"teacher_disagreement_score":0.10160269,"about_ca_system_score_codex":0.0000024659344,"about_ca_system_score_gemma":0.000540612,"threshold_uncertainty_score":0.9985488},"labels":[],"label_agreement":null},{"id":"W4405313315","doi":"10.1139/cjes-2024-0102","title":"A FRAMEWORK FOR ROCK PROPERTY DATA ACQUISITION, VISUALIZATION AND ANALYSIS: AN EXAMPLE FROM THE BATHURST MINING CAMP, NORTHERN NEW BRUNSWICK","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Modeling and Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of New Brunswick; Frontier Geosciences (Canada)","funders":"","keywords":"Geology; Property (philosophy); Visualization; Mining engineering; Archaeology; Geochemistry; Data mining; Computer science; Geography","score_opus":0.08787034628672132,"score_gpt":0.2757413661294412,"score_spread":0.18787101984271992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405313315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.81843704,0.008632809,0.17023352,0.002075696,0.0003190125,0.00008980002,0.00014399808,0.000011540812,0.000056573164],"genre_scores_gemma":[0.9917283,0.000056360772,0.007086284,0.00041067565,0.00043203286,1.0918771e-7,0.00017412356,0.000001939271,0.00011014021],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988336,0.00008003792,0.00026778207,0.00031723757,0.00022597349,0.00027539043],"domain_scores_gemma":[0.99877423,0.00033266595,0.00010653221,0.00019427424,0.000096294054,0.0004959864],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011423709,0.00009362547,0.00018236946,0.00020944276,0.0005763152,0.0007580224,0.00060461485,0.000052964282,0.0007580283],"category_scores_gemma":[0.00019855717,0.000045945777,0.000067270455,0.0009892134,0.00011639077,0.00058622606,0.000008532336,0.0001029067,0.000012920473],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000072875796,0.0000027498954,0.9240607,0.0000036944712,0.00015281909,0.000012214964,0.0024157292,0.06030924,8.926373e-7,0.00020725286,0.0003880842,0.012439328],"study_design_scores_gemma":[0.0000617496,0.00018535068,0.21197717,0.00007497437,0.00033692896,0.000012621291,0.002007216,0.77417874,9.748752e-7,0.0032914241,0.0077586058,0.000114221],"about_ca_topic_score_codex":0.30521902,"about_ca_topic_score_gemma":0.9459972,"teacher_disagreement_score":0.7138695,"about_ca_system_score_codex":0.0000013682875,"about_ca_system_score_gemma":0.0016703473,"threshold_uncertainty_score":0.8299879},"labels":[],"label_agreement":null},{"id":"W4405352494","doi":"10.1139/cjes-2024-0097","title":"Geodynamic evolution of felsic magmatism in the Yellowknife greenstone belt, N.W.T., Canada: evidence for Archean magmatism in a volatile-saturated environment","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Magmatism; Greenstone belt; Archean; Felsic; Geology; Geochemistry; Petrology; Mafic; Seismology; Tectonics","score_opus":0.025766135746692027,"score_gpt":0.21524663857903484,"score_spread":0.1894805028323428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405352494","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98615307,0.009328318,0.00014846216,0.0037625863,0.00016688221,0.00014616444,0.00005966167,0.0000015161725,0.00023334665],"genre_scores_gemma":[0.9991983,0.00007666875,0.00050829095,0.000118620264,0.000040435647,9.714023e-7,0.000006543866,0.0000011797425,0.00004895766],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983806,0.00012393005,0.0004854574,0.00019855108,0.00041283286,0.00039864407],"domain_scores_gemma":[0.99893934,0.00057410746,0.0001366412,0.00009069346,0.000036810143,0.00022240798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014568705,0.0001126435,0.00022988059,0.0003333165,0.0001219598,0.00006577141,0.00048000235,0.00004567869,0.00078951224],"category_scores_gemma":[0.00024605103,0.00006827897,0.000084157866,0.00085361674,0.0004298176,0.0002817297,0.0000056679896,0.00024392779,0.000006031256],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023562701,0.000012074189,0.93049496,0.000080749436,0.000024795083,0.0002709234,0.0007054409,0.03914728,0.00033995835,0.0005815808,0.00027965583,0.028038986],"study_design_scores_gemma":[0.00008702476,0.00014732595,0.9156127,0.00021818493,0.000017020184,0.00004784168,0.0003383168,0.075820744,0.000016989785,0.0073221335,0.00028245777,0.00008924852],"about_ca_topic_score_codex":0.91774184,"about_ca_topic_score_gemma":0.998841,"teacher_disagreement_score":0.08109915,"about_ca_system_score_codex":0.000022525566,"about_ca_system_score_gemma":0.0018584689,"threshold_uncertainty_score":0.8644605},"labels":[],"label_agreement":null},{"id":"W4405486682","doi":"10.1139/cjes-2024-0058","title":"An ichthyosaur rostrum from the uppermost Albian of Saskatchewan (Canada) represents the youngest diagnosable Canadian ichthyosaur prior to their demise","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Demise; Geology; Rostrum; Paleontology; Seismology; Excursion","score_opus":0.01631755443417032,"score_gpt":0.21543351731947294,"score_spread":0.19911596288530262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405486682","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9636105,0.0078700315,0.0000061370256,0.021533338,0.0021980288,0.00017803318,0.0011214713,0.000005740906,0.003476738],"genre_scores_gemma":[0.99715847,0.000045068897,0.00013376634,0.0020975962,0.0004009765,9.477114e-7,0.000024479396,0.000003882847,0.00013481406],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976786,0.0003063962,0.00044146948,0.000340796,0.0004333461,0.0007994023],"domain_scores_gemma":[0.9972724,0.00072583044,0.00014552192,0.0003453234,0.0001699062,0.0013410163],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016299752,0.00019137799,0.0002641721,0.0002194362,0.0011611109,0.00021255389,0.0016247779,0.000118092954,0.0012989168],"category_scores_gemma":[0.00040505972,0.00010449211,0.00009191172,0.0007814047,0.0010044613,0.00044109434,0.000010502619,0.000404076,0.000036722788],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014509662,0.0000027485578,0.981305,0.0000027581707,0.000045745393,0.00017584879,0.0017967528,0.0014231789,0.000031589516,0.000045998386,0.0063869925,0.008768891],"study_design_scores_gemma":[0.00006616191,0.00023566314,0.928717,0.000065007844,0.000024606155,0.00020270383,0.005447356,0.0010040095,0.00006508852,0.00046929176,0.063561335,0.00014176514],"about_ca_topic_score_codex":0.99301475,"about_ca_topic_score_gemma":0.9999879,"teacher_disagreement_score":0.05717434,"about_ca_system_score_codex":0.00002024477,"about_ca_system_score_gemma":0.017938768,"threshold_uncertainty_score":0.99961406},"labels":[],"label_agreement":null},{"id":"W4405994514","doi":"10.1139/cjes-2024-0161","title":"Note of appreciation","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Conflict of Laws and Jurisdiction","field":"Social Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry","score_opus":0.021152089319580566,"score_gpt":0.3030239290583927,"score_spread":0.28187183973881214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405994514","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6563235,0.0008997387,0.00097652164,0.008584206,0.0022027346,0.00008880664,0.0000041451653,0.0000045154975,0.33091587],"genre_scores_gemma":[0.9983675,0.000044030974,0.00036225634,0.00012254599,0.000115459094,1.4836994e-7,7.55873e-8,7.0082046e-7,0.000987271],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99932593,0.000054408203,0.00019356624,0.00005182451,0.00021796681,0.00015629153],"domain_scores_gemma":[0.9993625,0.00006972258,0.000156735,0.0000373989,0.00020878114,0.00016486125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013341241,0.000029604795,0.00008560663,0.0003306492,0.00043109214,0.00006767234,0.00022282416,0.00003563114,0.00015947693],"category_scores_gemma":[0.00032399385,0.00002639454,0.000049063285,0.0006088948,0.0004716574,0.00024266426,0.0000032937155,0.000060186376,0.000002058884],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015536814,0.000028059158,0.4247709,0.000020777927,0.00003647581,0.000015405669,0.030885695,0.00065503136,0.0008633982,0.39221948,0.0031406032,0.14734864],"study_design_scores_gemma":[0.00015660212,0.0001058494,0.17008634,0.00010849797,0.000015404943,0.0000019823465,0.0025537927,0.000084958185,0.0006101026,0.005192841,0.82101774,0.00006587083],"about_ca_topic_score_codex":0.024289064,"about_ca_topic_score_gemma":0.42817003,"teacher_disagreement_score":0.8178772,"about_ca_system_score_codex":0.000010758555,"about_ca_system_score_gemma":0.0038055298,"threshold_uncertainty_score":0.98220825},"labels":[],"label_agreement":null},{"id":"W4406142194","doi":"10.1139/cjes-2024-0141","title":"Reply to comment on “Complementarity of Hf isotopes from detrital and igneous zircon: an example from the Central Gneiss Belt, Grenville Province, Ontario”","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Zircon; Gneiss; Geology; Geochemistry; Igneous rock; Isotope; Archean; Petrology; Metamorphic rock","score_opus":0.02645229849109812,"score_gpt":0.20378714604288853,"score_spread":0.1773348475517904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406142194","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98700947,0.0005049992,0.00003309366,0.010848089,0.00018473601,0.000111582944,0.00018124351,0.0000018488317,0.0011249316],"genre_scores_gemma":[0.98892486,0.000006892109,0.0017920904,0.009129227,0.00006134491,2.5668172e-7,0.00002518629,6.4968384e-7,0.000059481234],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99868715,0.000088244,0.00035038564,0.0002573964,0.00026556145,0.00035125265],"domain_scores_gemma":[0.9987743,0.00033100267,0.00013711855,0.00015043211,0.00005931133,0.0005478359],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041432105,0.000115015995,0.00025151763,0.00011836332,0.00041910488,0.0001373594,0.0005517811,0.000029751252,0.0052454835],"category_scores_gemma":[0.00006666966,0.00006810933,0.0000710464,0.0002775935,0.00040408756,0.00012714382,0.000019889614,0.00016568476,0.0000043728273],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029367626,0.000014857034,0.9923677,0.0000011447371,0.000029918729,0.000020870426,0.00067774294,0.00036652441,0.000058110574,0.00011041165,0.0012810152,0.0050423243],"study_design_scores_gemma":[0.00020562575,0.000612619,0.9409302,0.00004089509,0.000033026008,0.0000041282337,0.00090196094,0.00013687178,0.0005440128,0.0077271834,0.048766274,0.00009722964],"about_ca_topic_score_codex":0.981106,"about_ca_topic_score_gemma":0.9967045,"teacher_disagreement_score":0.051437538,"about_ca_system_score_codex":0.00000661812,"about_ca_system_score_gemma":0.00063742517,"threshold_uncertainty_score":0.9956639},"labels":[],"label_agreement":null},{"id":"W4406142233","doi":"10.1139/cjes-2024-0099","title":"Comment on “Complementarity of Hf isotopes from detrital and igneous zircon: an example from the Central Gneiss Belt, Grenville Province, Ontario”","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University; McMaster University","funders":"","keywords":"Gneiss; Zircon; Geology; Precambrian; Geochemistry; Igneous rock; Mantle (geology); Isotope; Crustal recycling; Metamorphic rock; Continental crust","score_opus":0.026483670028461283,"score_gpt":0.19853725120306,"score_spread":0.17205358117459874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406142233","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99270034,0.00090205664,0.00002323322,0.0046257866,0.00018715521,0.000085415355,0.0001829874,0.0000017058354,0.00129135],"genre_scores_gemma":[0.99644345,0.000015387119,0.0010010253,0.002408713,0.000059472626,1.757059e-7,0.000033369597,5.971226e-7,0.000037805687],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987555,0.00009576314,0.00033141684,0.00022255312,0.00025491457,0.00033983545],"domain_scores_gemma":[0.99888754,0.00036566216,0.00015544363,0.00012446017,0.000051704843,0.0004151798],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037736158,0.000114648625,0.00024819715,0.00010057566,0.00044292823,0.00012964675,0.00052099884,0.000037320813,0.005834132],"category_scores_gemma":[0.000043885448,0.00006655313,0.00007640729,0.00025923643,0.0005992624,0.00014216025,0.000015917425,0.00018572641,0.000003136617],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019854024,0.000015405923,0.994507,0.0000012276265,0.00003284452,0.000018624265,0.00038089885,0.00023456354,0.000047076122,0.00018268413,0.00036719843,0.0041926065],"study_design_scores_gemma":[0.00024859802,0.00044526032,0.97089845,0.000036164805,0.000039800154,0.0000041141793,0.00088785787,0.00026855327,0.00045786495,0.00936148,0.017259752,0.000092094495],"about_ca_topic_score_codex":0.9684087,"about_ca_topic_score_gemma":0.99728894,"teacher_disagreement_score":0.02888021,"about_ca_system_score_codex":0.000005477769,"about_ca_system_score_gemma":0.00066491927,"threshold_uncertainty_score":0.9950747},"labels":[],"label_agreement":null},{"id":"W4406257091","doi":"10.1139/cjes-2024-0125","title":"A review of paleomagnetic studies from Northern Alaska and Yukon: implications for terrane reconstructions","year":2025,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Fish and Wildlife Service; Directorate for Geosciences; Massachusetts Institute of Technology; Geological Society of America; National Science Foundation","keywords":"Paleomagnetism; Terrane; Geology; Paleontology; Earth science; Seismology; Geochemistry; Tectonics","score_opus":0.10908313243454099,"score_gpt":0.30500346296602265,"score_spread":0.19592033053148167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406257091","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0001880489,0.99670815,0.000012463053,0.0014112301,0.0004602138,0.00033632573,0.00046746994,0.0000018264327,0.000414278],"genre_scores_gemma":[0.00020035423,0.99835396,0.0011269985,0.0001455924,0.00010023148,0.0000047388585,0.000028522069,0.0000012044635,0.000038392733],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99876493,0.00008068509,0.00065682933,0.00019560845,0.000087079934,0.00021483994],"domain_scores_gemma":[0.9982331,0.0006412829,0.0005537802,0.00009796545,0.000262551,0.00021137026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00050708663,0.00015057146,0.000914987,0.000201189,0.0004242173,0.000041965977,0.00028257596,0.00006135601,0.00018867318],"category_scores_gemma":[0.0006490012,0.00009480991,0.0002067873,0.00048429164,0.000621634,0.000119626246,0.0000072662124,0.00011163585,0.000003317645],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[6.2239866e-7,0.000001498943,0.01385496,0.0064626704,0.00007225717,0.0000010946031,0.000050092447,0.000007891884,7.326939e-9,0.000021546513,0.0005092728,0.9790181],"study_design_scores_gemma":[0.00008162654,0.00041235925,0.016618077,0.05077431,0.0006033983,0.000079826415,0.00034416185,0.000004326427,4.203685e-8,0.0022017823,0.9286974,0.00018271247],"about_ca_topic_score_codex":0.0021804962,"about_ca_topic_score_gemma":0.32432076,"teacher_disagreement_score":0.97883534,"about_ca_system_score_codex":0.000002255495,"about_ca_system_score_gemma":0.00121005,"threshold_uncertainty_score":0.6880086},"labels":[],"label_agreement":null},{"id":"W4406525803","doi":"10.1139/cjes-2024-0040","title":"<sup>40</sup> Ar/ <sup>39</sup> Ar and Rb–Sr dating of gold-bearing quartz–breccia mineralization and deformation within the Gordon Lake Region, Northwest Territories, Canada: a tribute to Dr. Nick Culshaw and 30 years on","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia, Okanagan Campus; University of British Columbia; Vancouver Island University","funders":"","keywords":"Geology; Breccia; Mineralization (soil science); Geochemistry; Quartz; Igneous rock; Clastic rock; Mineralogy; Geomorphology; Sedimentary rock; Paleontology","score_opus":0.011292592577364244,"score_gpt":0.18866177754855223,"score_spread":0.17736918497118798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406525803","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947435,0.00060615386,0.00002353603,0.0040693926,0.00007904026,0.00009206457,0.00008249186,0.000002785576,0.00030100497],"genre_scores_gemma":[0.99899566,0.000055101136,0.00016861914,0.00055191654,0.00007111007,4.6834094e-7,0.000029475663,0.0000012670553,0.00012636185],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99868864,0.00008263376,0.00044206713,0.00020816921,0.00029358084,0.00028492662],"domain_scores_gemma":[0.9989711,0.00018399482,0.00023036855,0.000092327035,0.00012996128,0.0003922199],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00075789134,0.00012992726,0.00027130265,0.00021612005,0.0003725308,0.00018644697,0.00022877964,0.000052753076,0.000080169266],"category_scores_gemma":[0.00041846876,0.000082981416,0.000035738725,0.00070260046,0.00031677235,0.00030056972,0.000015744658,0.00016684739,9.007618e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012158979,0.0000028905974,0.967899,0.000016266838,0.000021392032,0.000014204553,0.0007122179,0.027318014,0.000012599044,0.00015327065,0.00050125405,0.0033366936],"study_design_scores_gemma":[0.00019075448,0.0002496081,0.9645709,0.00015916367,0.000045224613,0.000054082993,0.0019593574,0.024327753,0.00004925208,0.0009389356,0.007311554,0.00014340498],"about_ca_topic_score_codex":0.69114685,"about_ca_topic_score_gemma":0.9929517,"teacher_disagreement_score":0.30180487,"about_ca_system_score_codex":0.0000059441645,"about_ca_system_score_gemma":0.00062155887,"threshold_uncertainty_score":0.3383884},"labels":[],"label_agreement":null},{"id":"W4406548941","doi":"10.1139/cjes-2024-0140","title":"Lithospheric thickness and the backarc–craton lithosphere step in southwestern Canada imaged by a 3D magnetotelluric study","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Magnetotellurics; Lithosphere; Geology; Craton; Seismology; Tectonics; Electrical resistivity and conductivity","score_opus":0.00724696642280007,"score_gpt":0.20726898816636427,"score_spread":0.2000220217435642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406548941","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9895824,0.0061066533,0.00010939124,0.0017862307,0.00039464614,0.00021699964,0.000014835932,0.0000023522175,0.0017864872],"genre_scores_gemma":[0.99735916,0.000029264189,0.0008546288,0.0007105329,0.00003862955,7.5432337e-7,5.9507613e-7,0.0000015679499,0.0010048791],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980466,0.0005034511,0.00038484894,0.00023347355,0.0003486897,0.00048294215],"domain_scores_gemma":[0.9986657,0.00061382726,0.00012164231,0.00011664384,0.000082643084,0.00039953523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017597032,0.0001479963,0.00032415055,0.00009691591,0.000409862,0.00025913728,0.0005317722,0.00004041639,0.0004471157],"category_scores_gemma":[0.0003040103,0.00008560198,0.00004250016,0.0015661921,0.00055083534,0.00020792556,0.000010814546,0.0003860158,0.0000045418815],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042966145,0.00001391339,0.84183836,0.000010073482,0.000014428692,0.00009653526,0.00042724126,0.0005287587,0.0000022369113,0.000041998428,0.00021838302,0.15676512],"study_design_scores_gemma":[0.00075427943,0.0003279257,0.9897423,0.000035554778,0.000020212816,0.00002448671,0.0018017928,0.003225041,0.000006691796,0.0006553343,0.0032815489,0.0001248732],"about_ca_topic_score_codex":0.9385449,"about_ca_topic_score_gemma":0.9970871,"teacher_disagreement_score":0.15664025,"about_ca_system_score_codex":0.000004841775,"about_ca_system_score_gemma":0.0027424493,"threshold_uncertainty_score":0.4895603},"labels":[],"label_agreement":null},{"id":"W4406639216","doi":"10.1139/cjes-2024-0147","title":"Cenozoic faulting in the Upper Hyland River Valley, Southeastern Yukon: A thermochronological perspective","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Lakehead University; Yukon University; Geological Survey of Canada; University of Calgary","funders":"Natural Resources Canada; Government of Alberta; Natural Sciences and Engineering Research Council of Canada; Yukon Foundation","keywords":"Cenozoic; Geology; Paleontology; Perspective (graphical); Geomorphology; Structural basin","score_opus":0.028929302569074618,"score_gpt":0.23003972089794952,"score_spread":0.2011104183288749,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406639216","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.963563,0.0026564933,0.00005807374,0.00720744,0.00027500896,0.00008180178,0.000004434994,0.000002217821,0.0261515],"genre_scores_gemma":[0.99890727,0.000043304994,0.00020613329,0.00070175924,0.00007707151,2.7752264e-7,5.24977e-7,4.354364e-7,0.000063229025],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99903876,0.00013138218,0.00019520719,0.00013594981,0.00017929348,0.00031944067],"domain_scores_gemma":[0.99951917,0.0001589265,0.000082237835,0.000054883807,0.00007431446,0.00011046552],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00085796346,0.000078517856,0.00013292827,0.00015670636,0.00049129524,0.00013618385,0.00040199794,0.0000415593,0.0006099278],"category_scores_gemma":[0.00020699525,0.000039377457,0.000057426045,0.0004697411,0.0005413545,0.00017534944,0.000006261921,0.00019451175,0.000034573626],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000082498145,0.0000040822306,0.98874944,0.0000013092921,0.000007026537,0.000043307227,0.003425209,0.0020148933,0.0000010896584,0.0010359227,0.000051613977,0.004657864],"study_design_scores_gemma":[0.00014135624,0.00021707464,0.97069365,0.000025485344,0.0000050528247,0.000024941164,0.019921765,0.00096653425,0.0000013027112,0.006122386,0.0018245413,0.000055884877],"about_ca_topic_score_codex":0.025995469,"about_ca_topic_score_gemma":0.4047273,"teacher_disagreement_score":0.37873185,"about_ca_system_score_codex":0.0000027276294,"about_ca_system_score_gemma":0.00032811228,"threshold_uncertainty_score":0.9804905},"labels":[],"label_agreement":null},{"id":"W4406639287","doi":"10.1139/cjes-2024-0068","title":"Holocene earthquake-triggered submarine landslides and turbidites in western Baffin Bay","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University; University of New Brunswick; Government of Newfoundland and Labrador; Memorial University of Newfoundland; Fisheries and Oceans Canada; Geological Survey of Canada; Natural Resources Canada","funders":"Commission Géologique du Canada; Natural Sciences and Engineering Research Council of Canada; Crown-Indigenous Relations and Northern Affairs Canada","keywords":"Geology; Submarine landslide; Holocene; Bay; Turbidite; Seismology; Submarine; Landslide; Oceanography; Geomorphology; Sediment","score_opus":0.023334184381440918,"score_gpt":0.21590295834588988,"score_spread":0.19256877396444896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406639287","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9907051,0.0037177945,0.000011697591,0.0024517754,0.00029247656,0.0000488007,0.00000673949,0.0000026811824,0.0027629633],"genre_scores_gemma":[0.9988342,0.00031537242,0.00025138745,0.00033746794,0.00005027907,1.5654803e-7,0.0000020881366,5.7457123e-7,0.00020847066],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991482,0.000050810846,0.00024554445,0.0001340656,0.00012693286,0.00029444112],"domain_scores_gemma":[0.99947125,0.0001301183,0.000080502105,0.00004433855,0.000053031217,0.0002207701],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066475576,0.00008026292,0.00017862498,0.00030385476,0.00025098896,0.00015149965,0.00018024875,0.000040502196,0.0003312756],"category_scores_gemma":[0.00019735715,0.000054544034,0.000028264889,0.0005340407,0.00028858328,0.00028505572,0.000007100038,0.00011796172,0.000013389186],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006362567,0.000001933329,0.98169607,0.0000036593428,0.0000036873148,0.000042031756,0.00010704368,0.00092638144,0.0000011084231,0.000047941496,0.00007626483,0.01708753],"study_design_scores_gemma":[0.0001927958,0.00016969342,0.9919271,0.00003927468,0.000003837023,0.000023753155,0.00029494156,0.0003280269,0.000017437113,0.00091250305,0.0060257986,0.00006483545],"about_ca_topic_score_codex":0.01733138,"about_ca_topic_score_gemma":0.7313107,"teacher_disagreement_score":0.71397936,"about_ca_system_score_codex":0.0000012549281,"about_ca_system_score_gemma":0.0003016275,"threshold_uncertainty_score":0.9892123},"labels":[],"label_agreement":null},{"id":"W4406790695","doi":"10.1139/cjes-2024-0131","title":"Crystallization conditions and magmatic–hydrothermal evolution of syenite dykes spatially associated with gold mineralization: the example of the Dolodau syenite–carbonatite complex, Abitibi greenstone belt","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"DuPont (Canada); Université du Québec à Chicoutimi","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Greenstone belt; Geology; Geochemistry; Carbonatite; Hydrothermal circulation; Mineralization (soil science); Pegmatite; Archean; Petrology; Mantle (geology); Seismology","score_opus":0.016723645095855486,"score_gpt":0.210226794438654,"score_spread":0.1935031493427985,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406790695","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95743847,0.0003198153,0.031051418,0.0049569583,0.00018485193,0.000214292,0.000025779975,0.000006941842,0.005801476],"genre_scores_gemma":[0.9985627,0.0000035463058,0.0009078905,0.00014271155,0.000016597847,0.0000011656709,0.0000026046646,0.0000011179159,0.00036169653],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895334,0.00014088558,0.0003339633,0.00012438974,0.00027209733,0.00017531043],"domain_scores_gemma":[0.99857724,0.00018510286,0.00047765853,0.00016596225,0.0005152687,0.000078773504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006847985,0.00008436826,0.00015835797,0.00017105392,0.000355112,0.00008205373,0.00057149923,0.00003914956,0.000024830351],"category_scores_gemma":[0.00032078187,0.00005097903,0.000037841226,0.0011077396,0.0009044063,0.00025706142,0.00003681181,0.00009059792,9.392518e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011617045,0.000059219565,0.58143115,0.00014085611,0.00015991947,0.00001550932,0.0033561666,0.08361443,0.025587484,0.30414936,0.00060007954,0.0008742025],"study_design_scores_gemma":[0.00034803062,0.00014035276,0.94432527,0.00043452598,0.00003730035,0.00005802119,0.00020336699,0.045147087,0.0008593908,0.007889802,0.00045142038,0.00010540787],"about_ca_topic_score_codex":0.015677543,"about_ca_topic_score_gemma":0.18893625,"teacher_disagreement_score":0.36289412,"about_ca_system_score_codex":0.000014049087,"about_ca_system_score_gemma":0.00097116915,"threshold_uncertainty_score":0.99087715},"labels":[],"label_agreement":null},{"id":"W4406790707","doi":"10.1139/cjes-2024-0118","title":"Effect of Lithospheric Thickness and Radial Mantle Viscosity Profile on Glacial Isostatic Adjustment Crustal Motions in North America","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Post-glacial rebound; Lithosphere; Mantle (geology); Isostasy; Glacial period; Petrology; Geophysics; Seismology; Geomorphology; Tectonics","score_opus":0.008928441499157586,"score_gpt":0.2247523836782533,"score_spread":0.2158239421790957,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406790707","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99251515,0.0022153228,0.000015923315,0.0002779623,0.00054082845,0.00015044538,0.000044425844,0.0000022593474,0.0042376807],"genre_scores_gemma":[0.99941623,0.000118010415,0.00020865416,0.00013354525,0.000039484123,6.0317717e-7,0.000002125583,0.0000010177979,0.000080349775],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989547,0.00014220411,0.00026213954,0.00014845711,0.0002035682,0.00028893273],"domain_scores_gemma":[0.9993095,0.00025863864,0.00013266341,0.00006580099,0.000042244574,0.0001911713],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049988856,0.00010568804,0.00026204865,0.00028788517,0.0002717471,0.000046753757,0.00018394327,0.00002892121,0.00040177407],"category_scores_gemma":[0.00018751902,0.000075423704,0.000051282816,0.00081045524,0.00056787254,0.00016567948,0.0000061632645,0.00016092796,0.000008229429],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035251785,0.000008422922,0.92713135,0.000031614083,0.000016537573,0.000032272605,0.00051284453,0.0017687957,0.0000026747912,0.000042928863,0.00009343694,0.07032386],"study_design_scores_gemma":[0.00033220844,0.0014129111,0.9961994,0.000099183584,0.000017464423,0.000012651177,0.00029525493,0.00087174866,0.00005842126,0.00005451028,0.0005754715,0.00007076626],"about_ca_topic_score_codex":0.019504117,"about_ca_topic_score_gemma":0.44144377,"teacher_disagreement_score":0.42193967,"about_ca_system_score_codex":0.0000036047106,"about_ca_system_score_gemma":0.0007596927,"threshold_uncertainty_score":0.9870251},"labels":[],"label_agreement":null},{"id":"W4406790876","doi":"10.1139/cjes-2024-0134","title":"Factors controlling high elevations in the Canadian Cordillera: Isostatic analysis and thermal contributions","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Ottawa","funders":"","keywords":"Geology; Geomorphology","score_opus":0.022015015807408656,"score_gpt":0.23088763432480275,"score_spread":0.20887261851739408,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406790876","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98899657,0.001505968,0.0001312456,0.0070181643,0.00022171826,0.00009770592,0.00012925283,0.0000013191263,0.0018980366],"genre_scores_gemma":[0.9988113,0.000032485634,0.0001440857,0.0009379529,0.000026034848,4.2969398e-7,0.000008898997,5.4268213e-7,0.000038269973],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990494,0.000079791964,0.00026903194,0.00010207055,0.00017386419,0.00032582248],"domain_scores_gemma":[0.9989393,0.00050375273,0.00009710654,0.00006919195,0.00014068083,0.00024997597],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00076477916,0.00007853071,0.00019496311,0.0005020451,0.0014495393,0.00029320834,0.000281449,0.00003107364,0.0004906327],"category_scores_gemma":[0.00036999196,0.000047965565,0.000061798484,0.0022950103,0.00034895056,0.0001860851,0.0000020435973,0.00014894527,0.0000014744048],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[8.601563e-7,0.0000015007614,0.98839056,8.879072e-7,0.00006368873,0.0000071920726,0.00053516385,0.009037042,7.296519e-7,0.0014020058,0.000057322777,0.0005030414],"study_design_scores_gemma":[0.00013091632,0.00004121025,0.990251,0.000013067828,0.00009222158,0.0000015065527,0.0023706087,0.0042888224,0.0000014709719,0.00036597805,0.0023895623,0.00005363745],"about_ca_topic_score_codex":0.80176336,"about_ca_topic_score_gemma":0.9988536,"teacher_disagreement_score":0.19709022,"about_ca_system_score_codex":0.0000075632947,"about_ca_system_score_gemma":0.0019737107,"threshold_uncertainty_score":0.99985045},"labels":[],"label_agreement":null},{"id":"W4406943669","doi":"10.1139/cjes-2024-0155","title":"Constraining the age and depositional framework of the late Paleoproterozoic to early Mesoproterozoic Muskwa Assemblage, northern British Columbia","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; Laurentian University","funders":"","keywords":"Geology; Sedimentary depositional environment; Assemblage (archaeology); Paleontology; Geochemistry; Structural basin","score_opus":0.011991836351633114,"score_gpt":0.21240626607120883,"score_spread":0.2004144297195757,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406943669","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98985785,0.0022227203,0.000076966004,0.0011559846,0.00041833645,0.000169221,0.00004846092,0.0000020153614,0.006048466],"genre_scores_gemma":[0.9987597,0.0000099976105,0.0006776032,0.00044476113,0.000037598114,6.9296595e-7,2.6025987e-7,5.3689246e-7,0.00006886207],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99888265,0.00013911197,0.0003000506,0.0001338565,0.00024273565,0.00030158457],"domain_scores_gemma":[0.9992038,0.00021226925,0.00017145576,0.00010582224,0.00008493758,0.00022170614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007293951,0.00007599799,0.00017487553,0.000102767015,0.0010202514,0.00050514267,0.0005575868,0.00007322678,0.000101240956],"category_scores_gemma":[0.0001906612,0.00005998927,0.000084245294,0.0005634285,0.0017066898,0.00018028755,0.0000032323283,0.00028825004,8.907389e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000029269213,0.0000016616231,0.9762732,0.000004833878,0.000020634836,0.000056447927,0.00042977964,0.00009154187,0.000015765943,0.00005050929,0.000035148667,0.023017561],"study_design_scores_gemma":[0.00008330158,0.00014603528,0.9957201,0.0002574448,0.000015342974,0.0001342218,0.00029635752,0.000035434154,0.000014177486,0.0031016392,0.00012992608,0.00006600684],"about_ca_topic_score_codex":0.101617195,"about_ca_topic_score_gemma":0.97878516,"teacher_disagreement_score":0.87716794,"about_ca_system_score_codex":9.051491e-7,"about_ca_system_score_gemma":0.0008735939,"threshold_uncertainty_score":0.90436524},"labels":[],"label_agreement":null},{"id":"W4406943700","doi":"10.1139/cjes-2024-0100","title":"Zircon U–Pb ages of the Chiapas Amber-Lagerstätte in the uppermost Simojovel Formation, southwest Mexico","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Zircon; Geology; Geochronology; Geochemistry; Paleontology; Lagerstätte","score_opus":0.013345636718688443,"score_gpt":0.19578522611235816,"score_spread":0.18243958939366972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406943700","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97698855,0.0007887761,0.00006123513,0.01137898,0.00022366147,0.00006691586,0.000028816221,0.0000012978553,0.010461779],"genre_scores_gemma":[0.9980398,0.000020122854,0.0001830581,0.0016244809,0.000030809828,1.6500304e-7,0.0000023564364,3.996743e-7,0.00009885016],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883103,0.00012154671,0.00036514126,0.00010440193,0.0002946311,0.0002832635],"domain_scores_gemma":[0.9992482,0.00021414476,0.00020082355,0.00011702046,0.00008347457,0.00013635108],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009931987,0.00008482199,0.00017079282,0.00020493894,0.0003531595,0.00009717457,0.00083186745,0.00004042714,0.0009228375],"category_scores_gemma":[0.00031142417,0.00003855992,0.0001264146,0.0013147458,0.0006745419,0.00030253385,0.000008517943,0.00019667257,0.000011621374],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000033574445,0.000005264736,0.9934461,0.000005965982,0.000008508363,0.000007635039,0.0005365994,0.003961361,0.0001531735,0.00055226183,0.0002743898,0.0010453443],"study_design_scores_gemma":[0.00010746422,0.00006509312,0.98323333,0.00005068968,0.000019145025,0.00002127736,0.0015874199,0.00073456304,0.0008933803,0.010542922,0.0026824262,0.000062272135],"about_ca_topic_score_codex":0.029323036,"about_ca_topic_score_gemma":0.6414204,"teacher_disagreement_score":0.6120974,"about_ca_system_score_codex":0.0000015029275,"about_ca_system_score_gemma":0.0004087763,"threshold_uncertainty_score":0.99999046},"labels":[],"label_agreement":null},{"id":"W4407014665","doi":"10.1139/cjes-2024-0066","title":"Paleoenvironmental fluctuations across the Jurassic–Cretaceous boundary, Scotian margin, Canada","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Memorial University of Newfoundland","funders":"","keywords":"Geology; Cretaceous; Paleontology; Margin (machine learning); Boundary (topology); Mesozoic; Structural basin","score_opus":0.009744871431811767,"score_gpt":0.2160139037977495,"score_spread":0.20626903236593774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407014665","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93340683,0.014861307,0.000043174172,0.0061585167,0.0019638324,0.00009613378,0.00014544539,0.0000029231812,0.04332181],"genre_scores_gemma":[0.99879986,0.000040737457,0.00019031684,0.0006339457,0.00006972288,2.275225e-7,0.0000018496268,4.4428893e-7,0.00026288567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99863136,0.00009588774,0.00029920266,0.00015564554,0.00030408727,0.0005138197],"domain_scores_gemma":[0.999108,0.00018515739,0.00015112372,0.00012813705,0.00004168843,0.00038587098],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00070134376,0.00011635592,0.00015890191,0.0001270747,0.0020691487,0.00026352474,0.0006924446,0.00004851239,0.00049575075],"category_scores_gemma":[0.00009486701,0.00007627663,0.00007855371,0.000470087,0.001646901,0.000290126,0.0000016637146,0.00025573611,0.0000067356273],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004554084,0.000001775357,0.9664129,0.0000024405908,0.000026546619,0.0000793801,0.00026873173,0.00047113112,0.00000516986,0.00013245182,0.0018015873,0.030793343],"study_design_scores_gemma":[0.00011015991,0.00006814907,0.96091133,0.000021922842,0.000012993673,0.00011832185,0.0013043568,0.00022618075,0.000026577507,0.0004958013,0.036619987,0.00008421518],"about_ca_topic_score_codex":0.60241604,"about_ca_topic_score_gemma":0.9995011,"teacher_disagreement_score":0.39708507,"about_ca_system_score_codex":0.000004632665,"about_ca_system_score_gemma":0.0059198444,"threshold_uncertainty_score":0.9997157},"labels":[],"label_agreement":null},{"id":"W4407158175","doi":"10.1139/cjes-2024-0114","title":"Introduction to the Special Issue","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta; Geological Survey of Canada; Dalhousie University","funders":"","keywords":"Geology; Earth science","score_opus":0.00902792421907229,"score_gpt":0.19199546457701996,"score_spread":0.18296754035794768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407158175","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7150925,0.00069599773,0.00007015972,0.21094523,0.002825195,0.00006427392,0.000010542253,0.0000030033477,0.0702931],"genre_scores_gemma":[0.98917097,0.000009346817,0.0004259265,0.002330842,0.0061258893,7.339633e-8,0.0000010328826,2.537342e-7,0.0019356381],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99929154,0.000038798047,0.00017137936,0.000111222216,0.0001599066,0.00022717427],"domain_scores_gemma":[0.9994537,0.00005717449,0.00005118833,0.000067095454,0.00008567048,0.00028515418],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006149758,0.000051503343,0.00009999442,0.00020126371,0.00037914806,0.00012067303,0.00041677136,0.00002049732,0.02818019],"category_scores_gemma":[0.00033423034,0.000026519372,0.00005959769,0.0010338863,0.00025422793,0.0001085971,0.0000040972614,0.00011106661,0.0003387799],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012119492,0.0000039521033,0.74410003,0.0000025448026,0.00002246651,0.000021245029,0.00019011217,0.017761897,0.000026131045,0.0010150954,0.1674417,0.06940269],"study_design_scores_gemma":[0.000023563398,0.000075993754,0.33426028,0.0000045654115,0.000008516264,0.000011716177,0.000175458,0.00016622187,0.00010657258,0.00407461,0.66105783,0.000034691933],"about_ca_topic_score_codex":0.012678711,"about_ca_topic_score_gemma":0.58131534,"teacher_disagreement_score":0.56863666,"about_ca_system_score_codex":8.3057756e-7,"about_ca_system_score_gemma":0.00036025373,"threshold_uncertainty_score":0.99389595},"labels":[],"label_agreement":null},{"id":"W4407395835","doi":"10.1139/cjes-2024-0121","title":"Structure and serpentinization of the northern Cascadia mantle wedge corner from receiver function modelling","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Statistics Canada; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Receiver function; Mantle (geology); Seismology; Mantle wedge; Wedge (geometry); Subduction; Geophysics; Lithosphere; Geometry; Tectonics","score_opus":0.010253332717250624,"score_gpt":0.17613973119397197,"score_spread":0.16588639847672135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407395835","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967564,0.0006191151,0.0002217288,0.00015551763,0.001294528,0.00004691396,0.00011042763,9.622669e-7,0.0007944415],"genre_scores_gemma":[0.9995241,0.000017991588,0.00014662347,0.00007826561,0.00007346274,2.7863239e-8,0.000003910706,8.2411435e-7,0.00015476704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994544,0.000044595203,0.00016680775,0.00008931409,0.0001225704,0.00012232982],"domain_scores_gemma":[0.9995656,0.000038261558,0.00014521166,0.00006343667,0.00009145527,0.000096008036],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019934768,0.00005383334,0.00010458213,0.000084999665,0.00024389535,0.00008953223,0.00018102679,0.000033125907,0.00058217894],"category_scores_gemma":[0.000021838714,0.00003312528,0.000026062948,0.00024208768,0.00015206855,0.0001991833,0.0000041832313,0.000060522747,0.000002742975],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010858748,0.0000012839782,0.8922569,0.000008809293,0.000021564938,0.0000023461714,0.00042450763,0.10376567,0.0004192414,0.00023031069,0.00013705238,0.0027214705],"study_design_scores_gemma":[0.00011791668,0.00003934719,0.981328,0.00006628267,0.000035344274,0.0000038966627,0.00013956151,0.0090109855,0.0008401086,0.004662775,0.0036944812,0.00006126652],"about_ca_topic_score_codex":0.04021245,"about_ca_topic_score_gemma":0.36242956,"teacher_disagreement_score":0.3222171,"about_ca_system_score_codex":6.8509814e-7,"about_ca_system_score_gemma":0.00044555616,"threshold_uncertainty_score":0.96617883},"labels":[],"label_agreement":null},{"id":"W4407395896","doi":"10.1139/cjes-2024-0152","title":"Carbonated mantle lithosphere from the Western Canadian Cordillera","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Lithosphere; Mantle (geology); Geochemistry; Seismology; Tectonics","score_opus":0.01278130325176298,"score_gpt":0.19022752529756354,"score_spread":0.17744622204580057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407395896","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9428369,0.0037386303,0.000004751798,0.013829239,0.00043077653,0.000045164357,0.0000796646,0.000003307227,0.039031606],"genre_scores_gemma":[0.9950916,0.00003131619,0.00016667772,0.0038922748,0.000091919326,1.1819966e-7,0.000008103924,7.215435e-7,0.0007172613],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885476,0.00007049195,0.00025769282,0.00016600674,0.00021201605,0.00043902063],"domain_scores_gemma":[0.9987368,0.00021265297,0.000092701164,0.00011540451,0.00011964875,0.0007227704],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003832446,0.00010304948,0.00018967703,0.00013875875,0.00055782805,0.00021268241,0.0007490586,0.000057254296,0.012205502],"category_scores_gemma":[0.00018469672,0.000056439698,0.000097472,0.00085256353,0.0004902653,0.00013701597,0.000005760876,0.00022294743,0.00008583172],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000023644131,0.000001296223,0.9948724,8.081443e-7,0.00002618104,0.00005365437,0.000062442086,0.0006589317,0.000004581522,0.000045706536,0.001143368,0.0031282462],"study_design_scores_gemma":[0.00007793472,0.000052743773,0.9511497,0.000035291672,0.000028761086,0.000010243755,0.0002631061,0.0008931783,0.000050348684,0.0033771237,0.04397749,0.00008405058],"about_ca_topic_score_codex":0.9467158,"about_ca_topic_score_gemma":0.9979513,"teacher_disagreement_score":0.052254748,"about_ca_system_score_codex":0.0000030172237,"about_ca_system_score_gemma":0.0019351932,"threshold_uncertainty_score":0.98869747},"labels":[],"label_agreement":null},{"id":"W4407723521","doi":"10.1139/cjes-2023-0010","title":"Structural analysis of an area of ductile deformation between the Murray Fault and the Grenville Front Boundary Fault near Coniston, Ontario","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"Commission Géologique du Canada","keywords":"Mylonite; Geology; Greenschist; Shear zone; Metamorphic facies; Tectonite; Gneiss; Lineation; Metamorphism; Metamorphic rock; Petrology; Foreland basin; Seismology; Geochemistry; Geomorphology; Tectonics; Facies","score_opus":0.012561784210227796,"score_gpt":0.2002020808076698,"score_spread":0.187640296597442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407723521","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958996,0.0009796703,0.000016026635,0.001183312,0.00009523241,0.00005448895,0.00005815047,9.1087065e-7,0.0017126179],"genre_scores_gemma":[0.9994971,0.000010316868,0.00024303434,0.00014502287,0.000018288247,1.218644e-7,0.000014370739,3.5993136e-7,0.00007136627],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99884933,0.00011612738,0.00043483806,0.00011905556,0.00027513786,0.00020551762],"domain_scores_gemma":[0.99892086,0.00021313928,0.00039058554,0.00011834604,0.00015994885,0.00019711984],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009436614,0.00008772163,0.00035359626,0.00022223605,0.0006247744,0.00013491369,0.0004570867,0.000040528914,0.002199374],"category_scores_gemma":[0.00015996613,0.000039086422,0.00015856557,0.0008143661,0.0023787348,0.00021926599,0.000009139305,0.00016943825,0.0000011963698],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016431512,0.0000013692165,0.98197275,0.0000029920755,0.00016544617,0.0000014673595,0.0010104289,0.013374353,0.0000055442524,0.00005780309,0.000018772515,0.0033726469],"study_design_scores_gemma":[0.00016692969,0.0001018927,0.9783779,0.000009895193,0.000363521,0.0000066137336,0.0009269047,0.01529002,0.000071207425,0.0037475305,0.0008850052,0.000052595045],"about_ca_topic_score_codex":0.43241382,"about_ca_topic_score_gemma":0.95352817,"teacher_disagreement_score":0.52111435,"about_ca_system_score_codex":0.000003137727,"about_ca_system_score_gemma":0.000692367,"threshold_uncertainty_score":0.9987128},"labels":[],"label_agreement":null},{"id":"W4407815896","doi":"10.1139/cjes-2024-0132","title":"The MacKenzie Mountains, Northwest Territories, earthquake sequence of 1953 to 1957","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Sequence (biology); Seismology; Physical geography; Geography","score_opus":0.02181227394475137,"score_gpt":0.2415953852151057,"score_spread":0.21978311127035433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407815896","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97906846,0.0061019864,0.000022468594,0.0034452395,0.0018989879,0.00013990822,0.0002651837,0.0000060627144,0.009051689],"genre_scores_gemma":[0.99837554,0.0001893593,0.000499149,0.0004770741,0.0001327135,4.2618038e-7,0.000004847068,0.0000016367311,0.00031926425],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983274,0.00007853287,0.0004816133,0.000184152,0.00039487975,0.0005334603],"domain_scores_gemma":[0.9985304,0.00039329147,0.00020452378,0.00019023695,0.00025603644,0.0004255527],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001190133,0.00013755358,0.00024841356,0.00035097759,0.0010596231,0.00021143169,0.00085042405,0.000044080625,0.0002442306],"category_scores_gemma":[0.00043286046,0.00008791662,0.00009921898,0.0011642777,0.0010100822,0.00026078784,0.0000128385645,0.00019084677,0.000020521831],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001136996,0.0000024841775,0.9596801,0.00000733688,0.000029151397,0.00003489431,0.00031905572,0.00081294874,0.000008448333,0.0011912428,0.00054007384,0.03736291],"study_design_scores_gemma":[0.00010879032,0.00029995412,0.8518892,0.0000876758,0.0000130738945,0.000032664393,0.0008010807,0.000065582906,0.00014851459,0.0009403594,0.1455148,0.000098330995],"about_ca_topic_score_codex":0.19808339,"about_ca_topic_score_gemma":0.97042876,"teacher_disagreement_score":0.7723454,"about_ca_system_score_codex":0.000003997914,"about_ca_system_score_gemma":0.0027862233,"threshold_uncertainty_score":0.8149871},"labels":[],"label_agreement":null},{"id":"W4409351176","doi":"10.1139/cjes-2025-0003","title":"Challenges in correlating the Hell Creek–Ludlow Formation contact: a lithostratigraphic study in northwestern South Dakota, U.S.A.","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology; Geochemistry; Geomorphology","score_opus":0.0627601916718088,"score_gpt":0.2682684646100469,"score_spread":0.2055082729382381,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409351176","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98443717,0.004980163,0.0000033707215,0.0011124996,0.00029178584,0.00020535197,0.0000037111574,0.0000018532247,0.008964109],"genre_scores_gemma":[0.9996913,0.00010546687,0.000027516855,0.00010405414,0.000017901557,8.903793e-7,0.0000011382823,6.7739575e-7,0.000051042283],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984143,0.0003848498,0.00041013077,0.00016049169,0.00019877778,0.0004314628],"domain_scores_gemma":[0.9990919,0.00042815984,0.00015070457,0.00010947938,0.00006238007,0.00015736787],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027479252,0.000088032466,0.00019972064,0.0007369372,0.00038479577,0.00012872007,0.00049157604,0.00006971831,0.0001608127],"category_scores_gemma":[0.00016807737,0.00006221469,0.000039335828,0.0008448146,0.00034095568,0.00042325543,0.0000058215733,0.00047208348,0.00001795886],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009604802,0.000007820991,0.99343044,0.000007250005,0.0000055479436,0.00013109493,0.0037557613,0.0008049135,1.9322911e-7,0.00005605445,0.0000020620055,0.0017892871],"study_design_scores_gemma":[0.00033284555,0.00034770655,0.98152703,0.00008840542,0.0000049395594,0.00007864718,0.015653744,0.0014707451,0.0000011293781,0.00035089644,0.00008443611,0.000059453436],"about_ca_topic_score_codex":0.024265638,"about_ca_topic_score_gemma":0.9957413,"teacher_disagreement_score":0.97147566,"about_ca_system_score_codex":8.249773e-7,"about_ca_system_score_gemma":0.0009746733,"threshold_uncertainty_score":0.98223186},"labels":[],"label_agreement":null},{"id":"W4409359819","doi":"10.1139/cjes-2024-0166","title":"A multi-proxy modern training set for reconstructing Holocene relative sea level using salt-marsh sediment (Prince Edward Island, Canada)","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Division of Ocean Sciences","keywords":"Holocene; Geology; Salt marsh; Proxy (statistics); Marsh; Sea level; Oceanography; Sediment; Physical geography; Archaeology; Geomorphology; Wetland; Geography","score_opus":0.09338376646607685,"score_gpt":0.29211527902740203,"score_spread":0.19873151256132518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409359819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9902679,0.0013052912,0.0036807957,0.001606253,0.0011131845,0.00019774397,0.00025147307,0.0000036270756,0.001573737],"genre_scores_gemma":[0.9785367,0.000010182087,0.020812657,0.00037536598,0.0000601713,5.931724e-7,0.000007305794,0.0000021357446,0.00019486315],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998142,0.00016130842,0.00040589916,0.00026984335,0.0002575943,0.00076333433],"domain_scores_gemma":[0.99843806,0.00054358767,0.0002358116,0.00009751234,0.00021510758,0.0004699051],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017480872,0.00014377336,0.00030732172,0.0004134619,0.0011547018,0.000085379455,0.00047162586,0.00010790953,0.0002060528],"category_scores_gemma":[0.0005538033,0.00012196759,0.000073314215,0.0004744113,0.00070178224,0.00033921926,0.00000926865,0.0003862005,0.0000025028778],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018872091,0.0000014928532,0.98991495,0.000014698694,0.000038891394,0.000067155655,0.0006120979,0.0075311414,0.0000054270363,0.00005376104,0.000067021305,0.0016744952],"study_design_scores_gemma":[0.0011390899,0.00029100734,0.7405323,0.0003018396,0.000055879562,0.00087458914,0.0041179005,0.24795337,0.00017934765,0.002882541,0.001324728,0.00034743542],"about_ca_topic_score_codex":0.25090134,"about_ca_topic_score_gemma":0.99135065,"teacher_disagreement_score":0.7404493,"about_ca_system_score_codex":0.000006121256,"about_ca_system_score_gemma":0.013114726,"threshold_uncertainty_score":0.99248},"labels":[],"label_agreement":null},{"id":"W4409359827","doi":"10.1139/cjes-2024-0070","title":"Mammoth (<i>Mammuthus</i>) of probable last interglacial age from southwestern Minnesota, USA","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Pleistocene-Era Hominins and Archaeology","field":"Social Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Mammoth; Interglacial; Archaeology; Geology; Paleontology; Pleistocene; Geography; Physical geography","score_opus":0.02187875196742957,"score_gpt":0.26539229999371855,"score_spread":0.243513548026289,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409359827","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97697353,0.00033914388,0.00013170997,0.0015605462,0.0012441842,0.00008663443,0.000018428338,0.0000034216384,0.019642374],"genre_scores_gemma":[0.9965989,0.000031335163,0.0015526715,0.0003022746,0.00022654493,9.911039e-7,8.506105e-7,0.0000032935138,0.001283117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984181,0.00016492675,0.00043647256,0.00018094301,0.00030538617,0.0004941749],"domain_scores_gemma":[0.99884415,0.00015379942,0.0002884992,0.000109266715,0.00017263777,0.00043164595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010641662,0.00010583786,0.00029964827,0.00046251004,0.00058618083,0.00011043855,0.00085383333,0.00008526707,0.00021926026],"category_scores_gemma":[0.0003199659,0.00009212849,0.00011078892,0.0006606157,0.0026456523,0.00036183943,0.000037574606,0.00016960586,0.00001166973],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009202731,0.000010633521,0.98476964,0.0000041087087,0.000017175686,0.000082232844,0.0072985147,0.000028114882,0.00023498556,0.0062122936,0.00030412956,0.0010289599],"study_design_scores_gemma":[0.0006516503,0.0003471422,0.85356,0.00033042973,0.000041146843,0.00001558964,0.009513859,0.0000069065795,0.0011865894,0.0099183535,0.12417034,0.00025799466],"about_ca_topic_score_codex":0.007879808,"about_ca_topic_score_gemma":0.9914969,"teacher_disagreement_score":0.9836171,"about_ca_system_score_codex":0.000020165016,"about_ca_system_score_gemma":0.00470346,"threshold_uncertainty_score":0.9987268},"labels":[],"label_agreement":null},{"id":"W4409359895","doi":"10.1139/cjes-2024-0037","title":"The glacial lakes evolution south of Lac Saint-Jean (Québec) and its implications for defining the regional deglaciation pattern","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Deglaciation; Geology; Glacial period; SAINT; Paleontology; Physical geography; Last Glacial Maximum; Oceanography; Geomorphology; Geography; Art history","score_opus":0.028052953203207165,"score_gpt":0.2538670634493283,"score_spread":0.22581411024612114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409359895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.959005,0.006955387,0.0002653429,0.03294321,0.00021252957,0.00011271884,0.00002659753,0.0000014813871,0.00047772177],"genre_scores_gemma":[0.99958205,0.00004478497,0.00004688232,0.0001821903,0.000033932283,9.0584615e-7,0.0000023744408,5.201081e-7,0.000106381296],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99927604,0.0001045625,0.00020095,0.00008810331,0.00009348537,0.0002368479],"domain_scores_gemma":[0.9985054,0.0010053081,0.00015443627,0.000059048132,0.00017200194,0.000103821316],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0012972477,0.00004868017,0.00008748828,0.00014696132,0.001381211,0.000057184403,0.00029988337,0.000041743526,0.000032195683],"category_scores_gemma":[0.00057764654,0.000027617747,0.00004035019,0.00025548396,0.0006977414,0.00011319252,0.000004201328,0.000117890595,0.0000038086005],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008386658,7.253639e-7,0.9899023,0.0000037555906,0.000009538518,3.5947892e-7,0.00019902804,0.00035467945,0.0000019646318,0.007442456,0.0000829711,0.001993842],"study_design_scores_gemma":[0.00009981456,0.000085583,0.99134827,0.000017037664,0.000011287184,0.00002472366,0.0004576208,0.001892896,0.000008284879,0.0036813808,0.0023431766,0.000029932746],"about_ca_topic_score_codex":0.011231108,"about_ca_topic_score_gemma":0.9121265,"teacher_disagreement_score":0.9008954,"about_ca_system_score_codex":0.0000011207619,"about_ca_system_score_gemma":0.0016020421,"threshold_uncertainty_score":0.9999189},"labels":[],"label_agreement":null},{"id":"W4409360427","doi":"10.1139/cjes-2024-0170","title":"The Canadian fossil record supports anagenesis in <i>Triceratops</i> (Ornithischia, Ceratopsia)","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; Carleton University; Canadian Museum of Nature","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Museum of Nature","keywords":"Geology; Paleontology; Fossil Record; Archaeology; Geography","score_opus":0.016985345887503545,"score_gpt":0.22646181812341457,"score_spread":0.209476472235911,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409360427","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.67507225,0.02380792,0.000012778233,0.01964123,0.0039979345,0.00018448925,0.000041173444,0.0000070574547,0.27723515],"genre_scores_gemma":[0.9966837,0.00022509795,0.00024910568,0.0012989452,0.000072377356,4.889168e-7,9.748954e-7,0.000001134001,0.0014681437],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99836546,0.00016294562,0.00041452708,0.00017975063,0.00020982744,0.00066751346],"domain_scores_gemma":[0.9986919,0.00025947587,0.00014797888,0.00012311684,0.00016039729,0.0006171204],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0016187461,0.000120999954,0.00020318723,0.00081363093,0.0022060608,0.0003511315,0.00057711406,0.00007892431,0.00043875226],"category_scores_gemma":[0.00033243533,0.000082801795,0.000071947194,0.0014208002,0.00082617084,0.0002990882,0.000004019843,0.00027365956,0.00003197132],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004130326,0.000001091059,0.9784567,0.0000022377267,0.000011946065,0.0001142568,0.0001515943,0.00019784935,3.1730082e-7,0.00049613224,0.0044271457,0.016136598],"study_design_scores_gemma":[0.00010302114,0.00005399739,0.76965326,0.000024192503,0.0000075204475,0.00004211688,0.00051621086,0.00019748247,0.0000041793364,0.00078602106,0.22853428,0.000077745804],"about_ca_topic_score_codex":0.7216917,"about_ca_topic_score_gemma":0.9999539,"teacher_disagreement_score":0.32161146,"about_ca_system_score_codex":0.0000115366365,"about_ca_system_score_gemma":0.007529376,"threshold_uncertainty_score":0.99909294},"labels":[],"label_agreement":null},{"id":"W4409451554","doi":"10.1139/cjes-2024-0172","title":"Age and geochemistry of basement complexes in the south-central New Québec Orogen: Archean history, terrane correlations, and Paleoproterozoic reactivation","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Government of Newfoundland and Labrador; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Terrane; Geology; Archean; Geochemistry; Basement; Petrology; Tectonics; Paleontology; Archaeology","score_opus":0.023940813335799657,"score_gpt":0.1969762248198401,"score_spread":0.17303541148404045,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409451554","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928587,0.0030933267,0.000032513337,0.0027642006,0.000044943758,0.000046374156,0.000006354454,7.904424e-7,0.0011527739],"genre_scores_gemma":[0.9993473,0.00002325399,0.00026106322,0.00025882042,0.000022724797,1.2398286e-7,0.000004061753,2.6692697e-7,0.000082325976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993252,0.00004654831,0.00022215076,0.00010216548,0.00013588036,0.0001680411],"domain_scores_gemma":[0.9995181,0.00011743151,0.00011091634,0.000048955168,0.000024685023,0.00017989079],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039297028,0.000059233593,0.00012713326,0.00012586963,0.00010661272,0.000031929994,0.00016328203,0.000025219646,0.00077195343],"category_scores_gemma":[0.00013559402,0.00003624015,0.00003064327,0.00020935488,0.00046809492,0.00008603742,0.0000037595835,0.00011625178,5.185007e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005457118,0.000003269548,0.9958936,0.000007572663,0.0000059962113,0.000012109754,0.00077613135,0.0001087377,0.00023428455,0.000043208398,0.00012306898,0.0027865744],"study_design_scores_gemma":[0.00012382315,0.00006388059,0.99409443,0.000036069378,0.000013994333,0.000014845291,0.0007364418,0.000854648,0.00010524899,0.0019756649,0.001937762,0.00004320471],"about_ca_topic_score_codex":0.2522543,"about_ca_topic_score_gemma":0.804797,"teacher_disagreement_score":0.5525427,"about_ca_system_score_codex":0.0000035909206,"about_ca_system_score_gemma":0.00071867526,"threshold_uncertainty_score":0.8452349},"labels":[],"label_agreement":null},{"id":"W4409741032","doi":"10.1139/cjes-2024-0177","title":"Dome-and-keel and linear accretionary architectures in the eastern Wabigoon superterrane, Canada: seismic profiling, magnetotelluric modelling, and gold endowment","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"Canada First Research Excellence Fund","keywords":"Geology; Keel; Seismology; Magnetotellurics; Dome (geology); Paleontology; Engineering","score_opus":0.01884960233232143,"score_gpt":0.21700657890161687,"score_spread":0.19815697656929543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409741032","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98918307,0.0059991097,0.00029778603,0.0032137302,0.00014522091,0.00011282368,0.000012560349,0.0000013500241,0.0010343497],"genre_scores_gemma":[0.99664164,0.00012542494,0.0019103381,0.0010521098,0.000059273236,4.4591357e-7,0.0000011632565,9.5048233e-7,0.00020866645],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988946,0.00014590258,0.00022621192,0.00018193273,0.00022668287,0.00032471184],"domain_scores_gemma":[0.999276,0.0002939545,0.000058063128,0.000057087396,0.000030129435,0.00028476404],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053839217,0.000109104294,0.00017790098,0.00022918575,0.00022387013,0.000101801765,0.00023225628,0.000034384106,0.00003079029],"category_scores_gemma":[0.000067670015,0.00006438043,0.000023149461,0.0004224215,0.00032751806,0.00008761355,0.00000739023,0.00025356485,6.4568604e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038107963,0.000011539934,0.7442645,0.0000531438,0.000017598642,0.0001358142,0.0008345122,0.058413662,0.000013388944,0.00044248474,0.000090450674,0.19568482],"study_design_scores_gemma":[0.00028216073,0.00048327833,0.7411329,0.00006645145,0.00001848976,0.00020799426,0.0004876841,0.2435778,0.000035272056,0.009560048,0.003996323,0.00015158422],"about_ca_topic_score_codex":0.65322423,"about_ca_topic_score_gemma":0.88591754,"teacher_disagreement_score":0.2326933,"about_ca_system_score_codex":0.000002311164,"about_ca_system_score_gemma":0.0009556613,"threshold_uncertainty_score":0.34908497},"labels":[],"label_agreement":null},{"id":"W4409741061","doi":"10.1139/cjes-2024-0130","title":"Geophysical and structural evidence for the presence of a central uplift in the South Range of the Sudbury impact structure","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Frontier Geosciences (Canada); WSP (Canada); McMaster University","funders":"","keywords":"Geology; Seismology; Range (aeronautics); Impact structure; Geophysics; Impact crater","score_opus":0.0238555705934905,"score_gpt":0.2652529974945722,"score_spread":0.2413974269010817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409741061","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99811155,0.00036830787,0.00010066109,0.0010438435,0.00015997846,0.00013210258,0.00006377858,1.6935245e-7,0.0000196119],"genre_scores_gemma":[0.9998404,0.0000020746006,0.000041503485,0.00004701354,0.000059848193,5.042958e-7,5.681936e-7,5.684676e-7,0.000007551458],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993951,0.000047664773,0.00015746316,0.000067532514,0.00015698437,0.00017525634],"domain_scores_gemma":[0.999379,0.000283901,0.00014335704,0.000088369445,0.000050928433,0.000054438347],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037959858,0.000051391322,0.00009489832,0.000055981418,0.00020971369,0.000066241875,0.0005086261,0.0000110158635,0.000015376536],"category_scores_gemma":[0.00007183746,0.000021014199,0.000059838,0.0003636275,0.00050854264,0.00032652784,0.0000091795,0.000103044884,6.480231e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011210816,0.0000013335689,0.98991734,0.0000047387084,0.00000862586,3.0405607e-7,0.0028682733,0.0043700277,0.00022946367,0.0015108698,0.00007648356,0.0010013292],"study_design_scores_gemma":[0.000093038376,0.000060306702,0.98902935,0.000068614565,0.000012877451,0.0000021184228,0.0022075647,0.004394171,0.00017629683,0.0038880429,0.000041626008,0.00002600047],"about_ca_topic_score_codex":0.0067252195,"about_ca_topic_score_gemma":0.016278468,"teacher_disagreement_score":0.009553249,"about_ca_system_score_codex":0.0000021169253,"about_ca_system_score_gemma":0.00092318567,"threshold_uncertainty_score":0.9998891},"labels":[],"label_agreement":null},{"id":"W4409888918","doi":"10.1139/cjes-2025-0007","title":"Geophysical studies of the lithosphere and plate boundaries: special issue in honour of Roy D. Hyndman","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Lithosphere; Honour; Geophysics; Plate tectonics; Seismology; Tectonics; Archaeology","score_opus":0.01324444138968375,"score_gpt":0.2316983182419958,"score_spread":0.21845387685231205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409888918","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927213,0.0019136551,9.41142e-7,0.00066756696,0.0013787681,0.000062534404,0.000043408232,6.1604106e-7,0.0032112116],"genre_scores_gemma":[0.9991181,0.00007638222,0.00015524904,0.00006161519,0.00028821078,8.719223e-8,2.7142605e-7,7.759392e-7,0.00029929416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910057,0.00007803743,0.0003277436,0.00010338044,0.00018277187,0.00020747822],"domain_scores_gemma":[0.9993959,0.00011364381,0.00020840304,0.0000761764,0.00009580934,0.000110071356],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006416778,0.0000773267,0.0002893542,0.00011303957,0.00029491226,0.00010456721,0.0003279439,0.000029900102,0.00028482144],"category_scores_gemma":[0.00015953422,0.00004771698,0.00004686949,0.00041294176,0.0013613139,0.00019316797,0.000013192396,0.00010145861,0.0000023083742],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006148291,0.000020795036,0.9628861,0.00016718105,0.000116889445,0.00005634298,0.008676054,0.002675986,0.00043605978,0.0059753074,0.0032209167,0.015706861],"study_design_scores_gemma":[0.00020454191,0.00018772206,0.9562151,0.00026487364,0.000020351137,0.00000835106,0.0018727838,0.00007647311,0.0011372714,0.0068030898,0.03313189,0.00007756681],"about_ca_topic_score_codex":0.024732877,"about_ca_topic_score_gemma":0.32110268,"teacher_disagreement_score":0.29636982,"about_ca_system_score_codex":0.0000011508756,"about_ca_system_score_gemma":0.0012428022,"threshold_uncertainty_score":0.9817615},"labels":[],"label_agreement":null},{"id":"W4410108274","doi":"10.1139/cjes-2024-0137","title":"The sabre-toothed cat <i>Smilodon fatalis</i> (Leidy, 1868) (Felidae, Machairodontinae) in the late Pleistocene–early Holocene of South America (Dolores Formation, Uruguay): new insights about its paleodistribution, taxonomy, and status of the genus","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Pleistocene; Holocene; Paleontology; Taxonomy (biology); Geochemistry; Zoology; Biology","score_opus":0.021695859566381252,"score_gpt":0.2146930085171747,"score_spread":0.19299714895079345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410108274","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97456366,0.01976586,0.00007460945,0.002083642,0.00039642656,0.00023635542,0.0001276637,0.0000024156245,0.0027493518],"genre_scores_gemma":[0.9984394,0.0009051734,0.00009409038,0.00036689526,0.000035161025,0.0000010352071,0.0000037694094,0.0000011375947,0.00015335536],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99831504,0.0002665851,0.0005511112,0.00013406276,0.00029365017,0.00043957983],"domain_scores_gemma":[0.99858147,0.00031866186,0.0005402743,0.0001678633,0.0001956104,0.00019611407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00072778965,0.00013517146,0.0002542123,0.00019529807,0.0008625674,0.0001049759,0.00067982177,0.000053220498,0.000028716806],"category_scores_gemma":[0.00036184504,0.000068103596,0.00008031336,0.00089705165,0.0016041682,0.00028172816,0.00001555552,0.00018235447,0.0000023358],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027465034,0.0000035160722,0.98957324,0.000012618188,0.000019144229,0.0000035770504,0.0035346702,0.0005888556,0.0000045523616,0.00036246204,0.0009293632,0.0049405554],"study_design_scores_gemma":[0.0002572261,0.0001407096,0.971194,0.000069168105,0.000022504893,0.000017560818,0.00301806,0.00029372773,0.00007951122,0.0002622781,0.024570677,0.00007456311],"about_ca_topic_score_codex":0.03770683,"about_ca_topic_score_gemma":0.7093041,"teacher_disagreement_score":0.67159724,"about_ca_system_score_codex":0.00000591801,"about_ca_system_score_gemma":0.0012519495,"threshold_uncertainty_score":0.9687012},"labels":[],"label_agreement":null},{"id":"W4410194013","doi":"10.1139/cjes-2024-0144","title":"In situ mica Rb–Sr geochronology and microstructural analysis to evaluate the timing and sense of shear zone movement: Shannon and d'Abbadie Faults, Yukon, Canada","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Yukon University; Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"","keywords":"Geochronology; Geology; Mica; Shear zone; Geochemistry; Seismology; Paleontology; Tectonics","score_opus":0.010100917384173246,"score_gpt":0.209570901611698,"score_spread":0.19946998422752477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410194013","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98983055,0.0031431883,0.000009662496,0.006569956,0.00006951232,0.00005484863,0.00003204099,6.0682504e-7,0.00028962063],"genre_scores_gemma":[0.9982324,0.000087823224,0.0003685951,0.0012270197,0.000015138531,1.3662604e-7,0.0000022746476,4.7448958e-7,0.00006610084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99892706,0.00007873088,0.00031060865,0.00020360175,0.00016554142,0.000314448],"domain_scores_gemma":[0.9992638,0.00017235559,0.000087549146,0.000069905516,0.00008207496,0.00032429886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052211253,0.000100425954,0.00029404077,0.00038665673,0.00023065135,0.000054451873,0.00016651342,0.000036671143,0.00036334925],"category_scores_gemma":[0.00013897174,0.000060563456,0.000037717757,0.0010323696,0.000569203,0.00010467325,0.000019453211,0.00012752235,4.777134e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002110642,0.0000020595016,0.9855899,0.000011487229,0.00012414494,0.000062053994,0.00037888793,0.0037383859,0.0013928416,0.00006421348,0.00009296992,0.008521942],"study_design_scores_gemma":[0.00015654888,0.00012572392,0.99245167,0.000019663692,0.000117359494,0.00003096431,0.0005690352,0.0038686816,0.00060817756,0.0014092753,0.00056025916,0.00008261945],"about_ca_topic_score_codex":0.7651337,"about_ca_topic_score_gemma":0.99646467,"teacher_disagreement_score":0.23133098,"about_ca_system_score_codex":0.0000036198207,"about_ca_system_score_gemma":0.0005022037,"threshold_uncertainty_score":0.39784193},"labels":[],"label_agreement":null},{"id":"W4410207856","doi":"10.1139/cjes-2024-0096","title":"First chimaeroid fish egg capsule (Chondrichthyes, Holocephali, Chimaeriformes) from upper Eocene Carmanah Group strata, West Coast of Vancouver Island, British Columbia, Canada","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Ichthyology and Marine Biology","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Waterloo","funders":"","keywords":"Chondrichthyes; Geology; Group (periodic table); Paleontology; Fish <Actinopterygii>; West coast; Oceanography; Archaeology; Fishery; Geography","score_opus":0.004117860368034844,"score_gpt":0.17753828338136055,"score_spread":0.1734204230133257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410207856","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9878345,0.000354393,0.000021663054,0.0003715574,0.0019078854,0.00010917372,0.0004313548,0.0000036268993,0.008965842],"genre_scores_gemma":[0.9962624,0.00006912709,0.0003725449,0.001393797,0.00008651709,0.0000020256232,0.000013355556,0.0000064208252,0.0017938433],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982272,0.00007249701,0.00049927365,0.00031513185,0.00029818655,0.00058773544],"domain_scores_gemma":[0.99899477,0.00006920748,0.0002613106,0.00017866744,0.00004930485,0.00044672872],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00039126514,0.00014649186,0.00036344046,0.000090618734,0.0005878128,0.000116778014,0.0007772348,0.00011709816,0.0069515263],"category_scores_gemma":[0.000115269235,0.00017116718,0.000087076995,0.00049452763,0.0011622831,0.0003572435,0.00008439774,0.00027186712,0.000011377384],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000061695237,0.00001951158,0.88500434,0.000006298504,0.000029990606,0.00014003341,0.000075158314,0.0002881085,0.00012611478,0.0000101321375,0.11348702,0.00080713915],"study_design_scores_gemma":[0.00048567276,0.00016139288,0.92463624,0.00005429539,0.000031757023,0.00008597281,0.00040625638,0.00005044323,0.000112466834,0.00017563692,0.07362092,0.0001789075],"about_ca_topic_score_codex":0.99505806,"about_ca_topic_score_gemma":0.99999505,"teacher_disagreement_score":0.039866094,"about_ca_system_score_codex":0.000075318305,"about_ca_system_score_gemma":0.001953361,"threshold_uncertainty_score":0.99395627},"labels":[],"label_agreement":null},{"id":"W4410336222","doi":"10.1139/cjes-2025-0011","title":"The enigmatic Tintina-Rocky Mountain Trench fault: A hidden solution to the BajaBC controversy?","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Credit Risk and Financial Regulations","field":"Economics, Econometrics and Finance","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Trench; Seismology; Fault (geology); Paleoseismology; Thrust fault; Paleontology; Geomorphology","score_opus":0.019346666380833856,"score_gpt":0.22803024601028357,"score_spread":0.20868357962944972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410336222","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8622928,0.008711348,0.010731052,0.0723389,0.003782151,0.000412915,0.000095529256,0.000007658308,0.04162761],"genre_scores_gemma":[0.9963932,0.00005806399,0.00029852803,0.0002602297,0.00018515486,0.0000036182478,4.0219035e-7,0.0000024671454,0.0027983533],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990335,0.00002112094,0.00044675244,0.00012391801,0.00006236807,0.0003123469],"domain_scores_gemma":[0.999167,0.00017624474,0.0002581638,0.00014581291,0.000081536986,0.00017119179],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014584915,0.000071491544,0.00016411884,0.00032500149,0.0012476615,0.00034144914,0.00052389695,0.00003468829,0.00006566682],"category_scores_gemma":[0.0009073657,0.00004782422,0.00009315558,0.0007334451,0.00024502043,0.00017911103,0.00001620102,0.00012856968,0.00006233877],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010180422,0.000010194209,0.18481831,0.0000049115715,0.000034340825,0.0000065995737,0.0016547438,0.0012234262,0.00001059697,0.7658109,0.023632722,0.022783035],"study_design_scores_gemma":[0.0001651964,0.000086512446,0.3430087,0.000030694933,0.0000069476187,0.000009640923,0.00053155515,0.0031445154,0.000009370347,0.027057102,0.625867,0.00008274608],"about_ca_topic_score_codex":0.0066199354,"about_ca_topic_score_gemma":0.17297097,"teacher_disagreement_score":0.73875386,"about_ca_system_score_codex":0.000033970664,"about_ca_system_score_gemma":0.00071714824,"threshold_uncertainty_score":0.99999505},"labels":[],"label_agreement":null},{"id":"W4410631878","doi":"10.1139/cjes-2024-0176","title":"Coeval development of dome-and-keel and linear accretionary architectures in the eastern Wabigoon superterrane, Canada: geology and geochronology","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa; University of Toronto; Laurentian University","funders":"Canada First Research Excellence Fund","keywords":"Geology; Greenschist; Geochemistry; Geochronology; Terrane; Archean; Seismology; Paleontology; Petrology; Tectonics; Metamorphism","score_opus":0.013951315606774532,"score_gpt":0.199469371933727,"score_spread":0.18551805632695245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410631878","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99102944,0.0036499829,0.000010693268,0.004593479,0.00006396795,0.00003534542,0.0000062980766,5.3072876e-7,0.0006102569],"genre_scores_gemma":[0.9987318,0.000041455987,0.00055902335,0.0006248534,0.000016116031,1.707732e-7,0.0000019604136,2.9710412e-7,0.000024316114],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991877,0.00007906888,0.00025191443,0.000129194,0.0001279521,0.00022416399],"domain_scores_gemma":[0.999467,0.00023215279,0.000066339475,0.00003930952,0.000036986017,0.00015819698],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049074955,0.00007311284,0.00018846388,0.00019932231,0.0001850517,0.000020096806,0.00020682422,0.00003902647,0.00025376034],"category_scores_gemma":[0.000111811736,0.000041084786,0.000017002536,0.00024206321,0.00079941866,0.00003911238,0.000011781592,0.00014014744,4.1726582e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009297893,0.0000018249663,0.988183,0.0000082457445,0.000010329157,0.000025003417,0.00031040618,0.00029429156,0.000014174891,0.000049891132,0.000012576317,0.01108094],"study_design_scores_gemma":[0.00012897776,0.00009096192,0.99368775,0.000017862387,0.00000852863,0.00011951357,0.00054387306,0.0017471815,0.000030319781,0.00213111,0.0014442726,0.000049676546],"about_ca_topic_score_codex":0.5777974,"about_ca_topic_score_gemma":0.9946752,"teacher_disagreement_score":0.4168778,"about_ca_system_score_codex":0.0000012959349,"about_ca_system_score_gemma":0.0011142858,"threshold_uncertainty_score":0.42501405},"labels":[],"label_agreement":null},{"id":"W4410762089","doi":"10.1139/cjes-2024-0175","title":"Stratigraphic correlation and paleogeography of the Upper Cretaceous Suquash Outcrop Area, Vancouver Island, Canada","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Royal British Columbia Museum; Geological Survey of Canada; Natural Resources Canada; Nautilus Environmental; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Palaeogeography; Geology; Outcrop; Cretaceous; Paleontology; Tectonics; Volcanism","score_opus":0.009450054518331126,"score_gpt":0.19887977173975918,"score_spread":0.18942971722142807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410762089","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9841704,0.0036790767,0.000013753637,0.0010387328,0.0009388342,0.00007172499,0.00003224554,8.6857585e-7,0.010054415],"genre_scores_gemma":[0.99932164,0.00004851207,0.00005859057,0.00025812027,0.000012727468,1.0836978e-7,9.775597e-7,5.163217e-7,0.00029882402],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989764,0.00012524446,0.00025444577,0.000118070064,0.00022925453,0.0002965463],"domain_scores_gemma":[0.99917233,0.00024800526,0.00015077942,0.0000949335,0.00012697386,0.00020699146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058555446,0.00007940511,0.00016612749,0.0003152697,0.0005015149,0.000038807975,0.00035020005,0.00006544014,0.0005551723],"category_scores_gemma":[0.00014378784,0.00004939401,0.000057350568,0.00069213996,0.0010946705,0.00013195824,0.0000048212296,0.00024113173,8.586075e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006025126,0.0000011281072,0.99766105,0.0000069783696,0.00001662424,0.000016531947,0.000067480614,0.0010295587,6.446756e-7,0.00008142508,0.00083161617,0.00028093116],"study_design_scores_gemma":[0.00013270663,0.00007527884,0.99546844,0.000040626288,0.0000149059615,0.000053031483,0.00038732143,0.0008199296,0.000012389417,0.0008124661,0.0021311764,0.00005174719],"about_ca_topic_score_codex":0.34700325,"about_ca_topic_score_gemma":0.99974525,"teacher_disagreement_score":0.652742,"about_ca_system_score_codex":3.921748e-7,"about_ca_system_score_gemma":0.0033791552,"threshold_uncertainty_score":0.6573451},"labels":[],"label_agreement":null},{"id":"W4411439279","doi":"10.1139/cjes-2025-0020","title":"Revision of Middle Cambrian trilobites and agnostids from Cape Breton Island, Nova Scotia, reveals a Guzhangian faunal interval in the Avalonian cover sequence","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Division of Earth Sciences","keywords":"Trilobite; Paleontology; Fauna; Geology; Baltica; Ammonite; Terrane; Biostratigraphy; Group (periodic table); Sequence (biology); Cape; Laurentia; Ordovician; Archaeology; Geography; Cretaceous; Ecology","score_opus":0.030646228624668894,"score_gpt":0.24649899296491917,"score_spread":0.21585276434025027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411439279","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9764897,0.0124469735,0.000026225078,0.0011068506,0.00040260487,0.00010603204,0.00015072312,0.000001289998,0.009269553],"genre_scores_gemma":[0.99907357,0.00008176848,0.00042412,0.00032945912,0.000050593637,5.5230757e-8,0.0000027832407,4.817894e-7,0.000037182665],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99853224,0.00024084376,0.00045531354,0.00019566393,0.0002466922,0.0003292474],"domain_scores_gemma":[0.9988841,0.00047776834,0.00023112318,0.0001199923,0.00007237632,0.00021467193],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014853397,0.00012257785,0.0002951165,0.0004668678,0.00023202412,0.00014006477,0.000563806,0.000081994134,0.00035836914],"category_scores_gemma":[0.00031827547,0.000081218575,0.000083538456,0.0006967129,0.00096329855,0.00038774766,0.0000022038248,0.00024312866,0.0000048572997],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021334714,0.0000037327504,0.9865208,0.00001228653,0.000012687089,0.00008644118,0.00096389366,0.000043055134,0.000051315372,0.00011859976,0.00018947989,0.011976359],"study_design_scores_gemma":[0.00026054596,0.0003073569,0.996375,0.00051145925,0.000018923472,0.00009009964,0.00081094564,0.00026053234,0.00006078139,0.0007107761,0.0005059838,0.000087599445],"about_ca_topic_score_codex":0.114330076,"about_ca_topic_score_gemma":0.8657031,"teacher_disagreement_score":0.75137305,"about_ca_system_score_codex":0.000001887073,"about_ca_system_score_gemma":0.0007768777,"threshold_uncertainty_score":0.89156765},"labels":[],"label_agreement":null},{"id":"W4412024241","doi":"10.1139/cjes-2024-0168","title":"Geology of the 1901 deposit and implications for controls on Cu–Zn–Au VMS mineralization in the Chisel Sequence, Snow Lake arc assemblage, Snow Lake, Manitoba, Canada","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Metal Extraction and Bioleaching","field":"Engineering","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Hudbay Minerals (Canada); Geoscience BC","funders":"","keywords":"Geology; Snow; Geochemistry; Mineralization (soil science); Assemblage (archaeology); Geomorphology; Paleontology; Soil water","score_opus":0.025739837350476226,"score_gpt":0.24527724783625862,"score_spread":0.2195374104857824,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412024241","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9890791,0.00022849407,0.00084061286,0.0036407036,0.00049247826,0.00019691777,0.000040762974,0.000002264919,0.005478669],"genre_scores_gemma":[0.99912834,0.000015897425,0.00010633371,0.0006197985,0.00004145308,0.0000037930329,0.0000020317495,0.0000021540968,0.000080199556],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993786,0.000054472308,0.00022646778,0.00007221428,0.00009273082,0.00017550447],"domain_scores_gemma":[0.99948597,0.00020489084,0.00008791516,0.00008001217,0.00005777239,0.00008346051],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047522725,0.000064476124,0.00011230577,0.00016061105,0.00023298778,0.000053841588,0.00025735894,0.00003050175,0.000007228709],"category_scores_gemma":[0.00023332749,0.00003929041,0.000032879965,0.00033499746,0.00011410629,0.00009496623,0.0000036910556,0.00012648624,1.1315598e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011854454,0.000017227352,0.9022784,0.000058742793,0.00005162067,0.000009457786,0.00042540068,0.04518202,0.0074271923,0.02473313,0.0028831984,0.01692176],"study_design_scores_gemma":[0.00020016938,0.000042115924,0.9778526,0.000098041965,0.00001386738,0.00003829165,0.00029935216,0.0038388954,0.00033609447,0.00048509843,0.01673383,0.00006163033],"about_ca_topic_score_codex":0.14294288,"about_ca_topic_score_gemma":0.9991501,"teacher_disagreement_score":0.85620725,"about_ca_system_score_codex":0.000020622798,"about_ca_system_score_gemma":0.0008521121,"threshold_uncertainty_score":0.86276436},"labels":[],"label_agreement":null},{"id":"W4412128695","doi":"10.1139/cjes-2025-0021","title":"New constraints on location and timing of the Great Lakes tectonic zone, central Upper Peninsula, Michigan, USA","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Peninsula; Tectonics; Seismology; Paleontology; Archaeology; Geography","score_opus":0.022658174206944638,"score_gpt":0.20805074942133106,"score_spread":0.18539257521438643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412128695","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9906685,0.00098307,0.00016941244,0.0023373996,0.0004652631,0.00005827953,0.000004614634,0.0000010112766,0.005312451],"genre_scores_gemma":[0.9990991,0.000054896867,0.00029329097,0.0002601387,0.000036674883,4.487176e-8,4.427995e-7,3.5183746e-7,0.0002550999],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993609,0.00003431025,0.00016990102,0.00008985988,0.00013942888,0.00020556441],"domain_scores_gemma":[0.9995387,0.00008490907,0.00010382344,0.000044702105,0.00005710662,0.00017075943],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023929913,0.000058320446,0.00010247905,0.000095870266,0.0003718692,0.000064484295,0.00017837979,0.00002639626,0.0008174854],"category_scores_gemma":[0.00015477871,0.00003308468,0.00003254044,0.00035652894,0.00051674613,0.00013668633,0.0000040351047,0.000083290164,0.0000052819487],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000052763853,0.0000011436055,0.97561395,0.0000045715296,0.0000069401913,0.000002410642,0.0002572116,0.0037923376,0.00001395924,0.00043429525,0.0001690921,0.019698827],"study_design_scores_gemma":[0.000100778634,0.00013715714,0.9964455,0.00008361388,0.000008391566,0.000013277904,0.0004961868,0.0007095568,0.00013747934,0.00042819796,0.0014006183,0.00003926708],"about_ca_topic_score_codex":0.010915558,"about_ca_topic_score_gemma":0.47255364,"teacher_disagreement_score":0.4616381,"about_ca_system_score_codex":0.0000012654563,"about_ca_system_score_gemma":0.0008313784,"threshold_uncertainty_score":0.99567086},"labels":[],"label_agreement":null},{"id":"W4412402022","doi":"10.1139/cjes-2025-0018","title":"Recent revisions to the North American Stratigraphic Code and suggestions for implementation by Canadian geoscientists: replacing culturally offensive unit names and utilizing Indigenous place names","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Archaeology and Natural History","field":"Social Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Geological Survey of Canada","funders":"","keywords":"Offensive; Indigenous; Unit (ring theory); Geology; Code (set theory); Archaeology; History; Engineering; Operations research; Computer science; Mathematics education; Programming language","score_opus":0.022911645472539065,"score_gpt":0.32067042530234563,"score_spread":0.2977587798298066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412402022","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9661913,0.0075518605,0.000027444932,0.024953935,0.00033443974,0.0003594704,0.00014562802,0.000003934651,0.00043199956],"genre_scores_gemma":[0.99493426,0.002177224,0.0009714465,0.001571832,0.000035195702,0.000004488138,0.0000045168636,0.0000021765904,0.00029888802],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99885905,0.00016572901,0.00021408866,0.00018189699,0.0001619815,0.00041727323],"domain_scores_gemma":[0.99859476,0.0002461671,0.00016094094,0.00006308762,0.00031833816,0.00061671814],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0011400458,0.00008128963,0.00013551401,0.00042013184,0.004714128,0.00007640631,0.00026612557,0.000030729698,0.000022093536],"category_scores_gemma":[0.0006166229,0.00006105288,0.000028032357,0.0009588444,0.001952043,0.00020560104,0.000012187324,0.00016114222,3.3896313e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017856746,0.000004291715,0.7561639,0.000011501972,0.000047273406,0.000018787685,0.07185655,0.000056664165,0.000030514266,0.0073370896,0.021580627,0.14287496],"study_design_scores_gemma":[0.00011134178,0.00017981479,0.39089796,0.000055594075,0.000026156391,0.000015894922,0.0380625,0.000012057777,0.000007595816,0.00030743494,0.570218,0.00010562731],"about_ca_topic_score_codex":0.41782284,"about_ca_topic_score_gemma":0.99902254,"teacher_disagreement_score":0.5811997,"about_ca_system_score_codex":0.000050985065,"about_ca_system_score_gemma":0.004302152,"threshold_uncertainty_score":0.9965816},"labels":[],"label_agreement":null},{"id":"W4412608650","doi":"10.1139/cjes-2025-0036","title":"L'Ordovicien supérieur du lac Saint-Jean, Québec : l’île aux Couleuvres revisitée","year":2025,"lang":"fr","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Recyc PHP (Canada); Cégep de Chicoutimi; Université du Québec à Chicoutimi","funders":"","keywords":"Geology; Humanities; Geochemistry; Art","score_opus":0.023201761910549613,"score_gpt":0.24100782506605375,"score_spread":0.21780606315550413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412608650","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.46925214,0.35188416,0.00009743183,0.076367535,0.0055168658,0.00015599446,0.00012612402,0.000009565169,0.096590206],"genre_scores_gemma":[0.9879435,0.0015596378,0.0006614751,0.0013166937,0.00045200274,3.9973818e-7,0.0000017462365,0.0000017901611,0.0080628],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9969938,0.0003529055,0.0007792912,0.00038266074,0.00042562486,0.0010657344],"domain_scores_gemma":[0.9971347,0.0006868639,0.000388135,0.00022673843,0.00033071756,0.0012328756],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":["sts"],"category_scores_codex":[0.002305983,0.00029016426,0.00052565703,0.00085911754,0.0018193139,0.00049701193,0.0012754136,0.0002346009,0.0032090521],"category_scores_gemma":[0.000933813,0.0002476092,0.00029329836,0.001404044,0.0036247987,0.0009452055,0.0000047501458,0.0006020738,0.000080348465],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019342224,0.000016128855,0.90519047,0.00004194529,0.00007170792,0.0005498008,0.0008873846,0.00095134595,0.0000045645334,0.0057617016,0.014219091,0.0722865],"study_design_scores_gemma":[0.00021844491,0.0004090576,0.6529546,0.00033992002,0.00006024317,0.0002247222,0.0008019877,0.0011211515,0.000018811244,0.0009779787,0.34267977,0.00019333957],"about_ca_topic_score_codex":0.7250751,"about_ca_topic_score_gemma":0.99083143,"teacher_disagreement_score":0.5186913,"about_ca_system_score_codex":0.000011412979,"about_ca_system_score_gemma":0.014943402,"threshold_uncertainty_score":0.9999976},"labels":[],"label_agreement":null},{"id":"W4412620893","doi":"10.1139/cjes-2024-0113","title":"Direct dating of a laminated speleothem coating a karst wall in southeastern Gaspé Peninsula, Quebec, Canada: Carboniferous, not Silurian","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Carboniferous; Karst; Speleothem; Peninsula; Paleontology; Archaeology; Cave; Structural basin","score_opus":0.01884091616985868,"score_gpt":0.225657373805496,"score_spread":0.20681645763563733,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412620893","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9847448,0.0007823755,0.000003080033,0.0012760212,0.00030674998,0.00008950488,0.000024586861,0.0000022830793,0.012770599],"genre_scores_gemma":[0.9989632,0.000010091805,0.00018023612,0.00021109219,0.000023626893,2.1029552e-7,0.0000038261282,0.0000016402246,0.0006060996],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980959,0.00025931463,0.0005237858,0.00020613354,0.0002990277,0.00061579305],"domain_scores_gemma":[0.998688,0.0004852403,0.00025777164,0.0001168938,0.00013744608,0.0003146772],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015576994,0.0001259451,0.0003596759,0.0006135552,0.00027420107,0.00006077928,0.0005926623,0.00008136442,0.0005308552],"category_scores_gemma":[0.0005443249,0.00010480876,0.000049458497,0.0008462219,0.0006351489,0.00018108662,0.000009813448,0.0003279016,0.0000059721774],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016764514,0.000003194545,0.9975891,0.000018234692,0.000012361037,0.0002367767,0.00041353432,0.0013490556,0.00002417316,0.00007203323,0.00003166401,0.00023308325],"study_design_scores_gemma":[0.0002741061,0.00008723754,0.99392575,0.0001889941,0.000007900368,0.00007637968,0.0012127792,0.0033791326,0.00031725992,0.00007863204,0.00034760273,0.00010420551],"about_ca_topic_score_codex":0.95309997,"about_ca_topic_score_gemma":0.9999239,"teacher_disagreement_score":0.04682396,"about_ca_system_score_codex":0.00000302599,"about_ca_system_score_gemma":0.008643179,"threshold_uncertainty_score":0.9969769},"labels":[],"label_agreement":null},{"id":"W4412822154","doi":"10.1139/cjes-2024-0162","title":"New family of fossil dragonfly (Odonata, Cavilabiata) from the late Cretaceous (Campanian) Dinosaur Park Formation, Alberta, Canada","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Fossil Insects in Amber","field":"Agricultural and Biological Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Odonata; Dragonfly; Cretaceous; Geology; Paleontology","score_opus":0.01560559173778772,"score_gpt":0.2012445690109687,"score_spread":0.185638977273181,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412822154","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98204565,0.0022464672,0.000009562725,0.008298294,0.0009373191,0.00009961752,0.000109831926,0.00000300471,0.006250257],"genre_scores_gemma":[0.99629515,0.000031924887,0.00018811206,0.0014509443,0.00017519045,6.7515424e-7,0.000003785342,6.9831333e-7,0.0018534858],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998404,0.00009775383,0.00049542356,0.00015639653,0.00043505355,0.0004113554],"domain_scores_gemma":[0.9982819,0.00062883977,0.00035281334,0.00009422993,0.00022321976,0.00041900075],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047128118,0.00014246708,0.00024005321,0.00004343895,0.000602611,0.00021375912,0.001105264,0.00006547241,0.0005501204],"category_scores_gemma":[0.00040364405,0.000053240557,0.000094621115,0.0008632631,0.00035584474,0.00039376013,0.000029365605,0.00020602306,0.000005411527],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006767152,0.000032995984,0.5560365,0.000024524112,0.00017999035,0.00014488345,0.0030418893,0.0014079054,0.017760035,0.0025387832,0.26892287,0.14984198],"study_design_scores_gemma":[0.000121559584,0.000106339045,0.7562304,0.000107641536,0.000021178214,0.00001783062,0.0010131272,0.00008916152,0.0011198233,0.0008760688,0.24016753,0.00012934752],"about_ca_topic_score_codex":0.97665995,"about_ca_topic_score_gemma":0.9993329,"teacher_disagreement_score":0.20019391,"about_ca_system_score_codex":0.000029791885,"about_ca_system_score_gemma":0.003420195,"threshold_uncertainty_score":0.6067279},"labels":[],"label_agreement":null},{"id":"W4412991002","doi":"10.1139/cjes-2024-0154","title":"Middle Cambrian (Drumian) trilobites and agnostid arthropods from the Manuels River Formation, Avalonian New Brunswick: bracketing the green–black facies boundary","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology; Facies; Boundary (topology); Bracketing (phenomenology); Structural basin","score_opus":0.02240660958577578,"score_gpt":0.21969157990135837,"score_spread":0.1972849703155826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412991002","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9472034,0.030458286,0.00013112958,0.010215632,0.000600319,0.00013002523,0.000054525917,0.000005670382,0.011200988],"genre_scores_gemma":[0.9974627,0.00019890179,0.0007646242,0.0008923387,0.00019141972,1.0147675e-7,0.0000027606459,7.401747e-7,0.0004864489],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985428,0.00021922275,0.00038228367,0.0001809585,0.00024935443,0.00042539448],"domain_scores_gemma":[0.99832577,0.0008370896,0.00024657726,0.00014859307,0.00007958943,0.00036238623],"candidate_categories":["sts"],"consensus_categories":["sts"],"category_scores_codex":[0.0010563975,0.00015041552,0.0002018056,0.00019856366,0.0020894133,0.00057140307,0.0006695841,0.00007154719,0.00023310287],"category_scores_gemma":[0.00029398408,0.00008499031,0.0000997192,0.0005086747,0.0031082786,0.0008707677,0.0000037818622,0.00029396062,0.000014786332],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009978175,0.0000012860323,0.9589469,0.0000051342045,0.000023420434,0.000017151682,0.0027180149,0.000060126793,0.000003219255,0.0003802025,0.0009052824,0.03692929],"study_design_scores_gemma":[0.00021151092,0.00010009689,0.977687,0.000114910705,0.000029091687,0.000072321214,0.002842489,0.00037170146,0.00003084643,0.0049412227,0.0134942,0.00010457982],"about_ca_topic_score_codex":0.14605089,"about_ca_topic_score_gemma":0.9631681,"teacher_disagreement_score":0.8171172,"about_ca_system_score_codex":0.0000017892021,"about_ca_system_score_gemma":0.0033500222,"threshold_uncertainty_score":0.9996047},"labels":[],"label_agreement":null},{"id":"W4413186425","doi":"10.1139/cjes-2025-0019","title":"Petrogenetic insights into the largest volcanic pulse in the Archean Abitibi greenstone belt, Canada: the Stoughton-Roquemaure assemblage","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Agnico Eagle (Canada); Geological Survey of Canada; Institut National de la Recherche Scientifique","funders":"Laurentian University","keywords":"Archean; Greenstone belt; Geology; Assemblage (archaeology); Volcano; Geochemistry; Volcanic belt; Volcanic rock; Paleontology","score_opus":0.011667869208090955,"score_gpt":0.2012761834976526,"score_spread":0.18960831428956165,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413186425","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9542573,0.008168107,0.000006334267,0.032621752,0.0002409257,0.00009997817,0.000008824187,0.0000016297467,0.004595152],"genre_scores_gemma":[0.9951258,0.00009810385,0.00003798607,0.004446008,0.00010325376,6.955197e-7,0.000004430912,0.000001000916,0.00018274717],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980148,0.00033964583,0.00038240806,0.00020845133,0.0005342356,0.0005204396],"domain_scores_gemma":[0.9986278,0.00060503226,0.00014568113,0.00022134029,0.00010876678,0.00029139203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015113914,0.00014796403,0.00021750998,0.00018656858,0.0010686541,0.00019275073,0.001581498,0.000048529037,0.0008264237],"category_scores_gemma":[0.00035664375,0.000058634072,0.00011323894,0.0017150097,0.00092476903,0.00013083612,0.000016047496,0.00051113,0.000008955597],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000053112817,0.000007510384,0.9881583,0.0000051047573,0.000026206784,0.00017255607,0.00090192904,0.0043828194,0.000029390072,0.0007854388,0.0011373195,0.0043881224],"study_design_scores_gemma":[0.00008789889,0.00008561205,0.9784095,0.000028222006,0.000029670799,0.000045504723,0.0019329581,0.001428123,0.00003764115,0.008433235,0.009387347,0.000094273855],"about_ca_topic_score_codex":0.9695388,"about_ca_topic_score_gemma":0.9999462,"teacher_disagreement_score":0.040868476,"about_ca_system_score_codex":0.0000083061595,"about_ca_system_score_gemma":0.0030815317,"threshold_uncertainty_score":0.904876},"labels":[],"label_agreement":null},{"id":"W4413387162","doi":"10.1139/cjes-2025-0009","title":"Two partial actinopterygian neocrania (occipital ossifications) from Blue Beach, Nova Scotia","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Nova scotia; Geology; Paleontology; Oceanography","score_opus":0.029887850394398327,"score_gpt":0.26940689704511106,"score_spread":0.23951904665071272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413387162","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9736002,0.0013559577,0.00008466236,0.0032981983,0.0017094184,0.00007766076,0.0000499785,0.000005685593,0.0198182],"genre_scores_gemma":[0.9980263,0.000013105193,0.0011054821,0.0003946811,0.00016465722,1.392207e-7,0.00001890923,0.0000012637731,0.00027544948],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983791,0.00018734422,0.00036790504,0.0002454939,0.00023369711,0.0005864558],"domain_scores_gemma":[0.9986228,0.0003703964,0.00015643617,0.00016472432,0.00013543094,0.00055024127],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00094018714,0.00012398175,0.00023041523,0.0005364834,0.00065635826,0.00020758028,0.0007571873,0.00009739418,0.005990157],"category_scores_gemma":[0.00027580338,0.00010092639,0.0000858626,0.0006934613,0.0012674597,0.00042810422,0.0000073073243,0.00040317135,0.0003888695],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014748514,0.000004635451,0.9967522,0.000002275232,0.000025759522,0.000092163114,0.00022280987,0.0006617576,0.000013210996,0.00027911045,0.000327613,0.0016036951],"study_design_scores_gemma":[0.00029508452,0.00012317649,0.9911363,0.000035853616,0.000021726306,0.0001171821,0.00060901523,0.0007095079,0.0002014512,0.00087570533,0.005763068,0.0001118941],"about_ca_topic_score_codex":0.037716344,"about_ca_topic_score_gemma":0.84062755,"teacher_disagreement_score":0.80291116,"about_ca_system_score_codex":8.594181e-7,"about_ca_system_score_gemma":0.002651844,"threshold_uncertainty_score":0.9949185},"labels":[],"label_agreement":null},{"id":"W4414172289","doi":"10.1139/cjes-2024-0142","title":"Age, stable isotopes, and redescription of the first mammoth tooth from the Labrador Peninsula","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Pleistocene-Era Hominins and Archaeology","field":"Social Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Mammoth; Peninsula; Cave; Interglacial; Before Present; Pleistocene; Taphonomy; Range (aeronautics)","score_opus":0.023233220347580512,"score_gpt":0.25071802249070396,"score_spread":0.22748480214312344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414172289","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97090274,0.0013877957,0.000018333627,0.016994232,0.00066615787,0.00009680865,0.000020544634,0.0000016137366,0.009911752],"genre_scores_gemma":[0.99736935,0.00011966065,0.0003326635,0.0008377226,0.00009468903,6.5454645e-7,1.7036454e-7,0.0000015105065,0.0012435613],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990911,0.00013940566,0.00020837756,0.0001033202,0.00021052231,0.00024729857],"domain_scores_gemma":[0.99931276,0.00018703545,0.00016859175,0.00010083235,0.00008388397,0.00014687295],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0010952319,0.000056486577,0.00013136784,0.00009298064,0.0013055613,0.00011884006,0.00063880126,0.00004017321,0.00012223417],"category_scores_gemma":[0.0003787339,0.000032321896,0.000047063786,0.00049396744,0.0024916038,0.00020308497,0.00003312732,0.00012690187,6.740401e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057830816,0.0000051705138,0.9557177,0.0000029166786,0.000012406591,0.000011361143,0.008902644,0.0000316182,0.000080343685,0.030478384,0.003090012,0.0016617052],"study_design_scores_gemma":[0.0001285595,0.000042988537,0.79814476,0.000078521116,0.000011441489,0.0000033974518,0.0042328597,0.000023212095,0.00011850653,0.0053983917,0.19177285,0.00004449998],"about_ca_topic_score_codex":0.059642315,"about_ca_topic_score_gemma":0.95462286,"teacher_disagreement_score":0.89498055,"about_ca_system_score_codex":0.000012342822,"about_ca_system_score_gemma":0.0022420865,"threshold_uncertainty_score":0.9999946},"labels":[],"label_agreement":null},{"id":"W4414223913","doi":"10.1139/cjes-2023-0001","title":"<i>Edmontosaurus</i> from the Rocky Mountain foothills, Alberta, and its chronostratigraphic position in the Late Cretaceous Brazeau Formation and correlative units in western Canada","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Evolutionary Biology","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Mount Royal University; University of Alberta; University of Saskatchewan","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Cretaceous; Canyon; Genus; Zircon; Vertebrate; Radiometric dating","score_opus":0.01011410153657705,"score_gpt":0.19111334282039164,"score_spread":0.1809992412838146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414223913","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97798,0.011796539,0.0000044448575,0.008847363,0.00017612598,0.00009584583,0.00005176446,5.4818395e-7,0.001047333],"genre_scores_gemma":[0.9979302,0.00017718587,0.000008009033,0.0018179565,0.000018030049,3.645892e-7,0.000011667685,3.624687e-7,0.000036179084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99913055,0.0002606984,0.00020951025,0.00009180705,0.00009408369,0.00021334545],"domain_scores_gemma":[0.99914235,0.0005949623,0.000096272415,0.00004101798,0.000035579822,0.00008981049],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055161153,0.00007351963,0.00010917595,0.00013959761,0.00036993105,0.000056396635,0.00021395324,0.00005425481,0.00002758492],"category_scores_gemma":[0.000106758285,0.00004371591,0.000009520587,0.00044952522,0.0002800716,0.00038181985,0.0000027501812,0.00021411412,7.4519437e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000111609315,9.1387057e-7,0.9966012,0.0000016920831,0.0000045931824,0.0000254083,0.001471146,0.000885005,0.0000044931744,0.00012448165,0.00009246442,0.00077744183],"study_design_scores_gemma":[0.00015313036,0.00009068937,0.9920885,0.00005171459,0.000006630272,0.000080425154,0.0017179409,0.0034118951,0.0000062000736,0.0010047713,0.0013372599,0.00005084486],"about_ca_topic_score_codex":0.8657927,"about_ca_topic_score_gemma":0.9999152,"teacher_disagreement_score":0.13412254,"about_ca_system_score_codex":0.0000046297077,"about_ca_system_score_gemma":0.0013858892,"threshold_uncertainty_score":0.28452477},"labels":[],"label_agreement":null},{"id":"W4414430925","doi":"10.1139/cjes-2025-0039","title":"An Early Devonian fossil assemblage in the Clam Bank Formation (western Newfoundland): implications for Lochkovian paleogeography, paleoceanography, and biogeography in the Canadian Appalachian orogen","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Marine transgression; Devonian; Paleozoic; Biogeography; Assemblage (archaeology); Macrofossil; Faunal assemblage; Taxon; Littoral zone","score_opus":0.01785917244073568,"score_gpt":0.23696957136724928,"score_spread":0.2191103989265136,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414430925","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9845523,0.0015555146,0.00005629997,0.011277542,0.00006948449,0.0002870801,0.00009186382,0.0000029023663,0.0021070065],"genre_scores_gemma":[0.99834055,0.000047163547,0.00023596865,0.0013004132,0.000041660813,0.000004746582,0.000024883508,0.0000011097187,0.00000352331],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983351,0.0002156641,0.00041589353,0.0002322903,0.00020771679,0.0005933359],"domain_scores_gemma":[0.99890256,0.0002356141,0.00013405696,0.000188097,0.00010240386,0.00043725982],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018160398,0.00015165597,0.00020651647,0.0013713447,0.000984418,0.0006899741,0.000990547,0.00009042271,0.000057388526],"category_scores_gemma":[0.00007106057,0.00008510057,0.00014809391,0.0028288297,0.0006065705,0.00050735346,0.000003580315,0.00024842034,0.0000016372975],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000431664,0.0000082431225,0.9944264,0.000005818031,0.000009289506,0.000008004559,0.00053756847,0.00013481123,0.0000039723373,0.0005703645,0.000019545534,0.004271659],"study_design_scores_gemma":[0.00018405134,0.0002299744,0.9811599,0.000026211355,0.000023962371,0.000028100798,0.0010744818,0.00034157003,0.0000024157337,0.014436637,0.002378771,0.00011389689],"about_ca_topic_score_codex":0.49635783,"about_ca_topic_score_gemma":0.99942,"teacher_disagreement_score":0.5030621,"about_ca_system_score_codex":0.0000032754813,"about_ca_system_score_gemma":0.0005717621,"threshold_uncertainty_score":0.75714463},"labels":[],"label_agreement":null},{"id":"W4414563354","doi":"10.1139/cjes-2025-0005","title":"Insights into a synorogenic origin for REE-bearing carbonatites in the Central Metasedimentary Belt Boundary Zone of the Grenville Province","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University; Ministère des Ressources naturelles et des Forêts (Québec); Geological Survey of Canada; Université du Québec à Montréal; Polytechnique Montréal","funders":"Natural Resources Canada","keywords":"Carbonatite; Zircon; Pegmatite; Overprinting; Igneous rock; Mafic; Geochronology; Orogeny; Shear zone; Isochron","score_opus":0.015051714766212896,"score_gpt":0.2251401558304291,"score_spread":0.2100884410642162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414563354","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9698326,0.023900444,0.000016577955,0.0014856481,0.0005648784,0.00019785667,0.000020386913,0.000001013091,0.003980593],"genre_scores_gemma":[0.99906045,0.00002790906,0.00061672326,0.0002380432,0.00003761397,7.659753e-7,9.667348e-7,3.79966e-7,0.000017161448],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886256,0.00014307429,0.00032219285,0.0001333647,0.0002285131,0.00031027207],"domain_scores_gemma":[0.99925554,0.0002805629,0.00017486616,0.000114988965,0.00004550554,0.00012850988],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00077014643,0.00009061288,0.00017492504,0.0002902164,0.00059387216,0.000076798584,0.0007741373,0.00004353983,0.000026265392],"category_scores_gemma":[0.00010269345,0.000049440725,0.00011853287,0.00065140746,0.00096748833,0.00023077312,0.000002003096,0.00018186786,2.1988713e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015444328,0.000006750349,0.9897183,0.000016573804,0.000032361426,0.000020656427,0.0009234647,0.00028057932,0.00010013131,0.0011391441,0.000106135645,0.00764044],"study_design_scores_gemma":[0.00019456517,0.00015617623,0.99210745,0.000077353565,0.000025944752,0.000019994608,0.0007095361,0.000380741,0.00035093687,0.0030893744,0.002827849,0.000060080594],"about_ca_topic_score_codex":0.04845534,"about_ca_topic_score_gemma":0.9187927,"teacher_disagreement_score":0.87033737,"about_ca_system_score_codex":0.0000032660168,"about_ca_system_score_gemma":0.002864969,"threshold_uncertainty_score":0.9578811},"labels":[],"label_agreement":null},{"id":"W4414563522","doi":"10.1139/cjes-2025-0053","title":"Cretaceous to Miocene exhumation of the Purcell Mountains, southeastern British Columbia","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Evolution and Paleontology Studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Alberta Energy; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Cretaceous; Fission track dating; Zircon; Geochronology; Hornblende; Cenozoic; Outcrop; Craton","score_opus":0.014368444928861586,"score_gpt":0.2094219908193625,"score_spread":0.19505354589050092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414563522","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9697207,0.003188753,0.00003249142,0.0013994236,0.0008112213,0.00008768954,0.00004206043,0.0000021089877,0.024715507],"genre_scores_gemma":[0.99729884,0.000023895092,0.00022566218,0.00062490505,0.00003709536,1.3310898e-7,5.8052103e-7,5.934736e-7,0.0017883021],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991326,0.00007978194,0.0002672108,0.00010076522,0.0001901685,0.00022952922],"domain_scores_gemma":[0.99936676,0.00007054197,0.00014821405,0.00007769059,0.0001414997,0.00019526915],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00052417774,0.000048619633,0.00014539872,0.000119586475,0.0005645882,0.0001734461,0.0004067165,0.0000339433,0.0009892064],"category_scores_gemma":[0.00019574768,0.000045033543,0.000062880266,0.00051775895,0.0004892921,0.000120619894,0.000005634531,0.00009116208,0.000012965181],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000017655195,0.0000015527312,0.99313587,0.0000053035956,0.000008954216,0.0000054440725,0.00024685313,0.00077533495,0.0000035433868,0.00001214385,0.0013329877,0.004470277],"study_design_scores_gemma":[0.00009034757,0.00008481634,0.9873193,0.00009228349,0.000010509055,0.000045691835,0.0008794279,0.0002047448,0.000007786082,0.00022728805,0.01099053,0.000047295765],"about_ca_topic_score_codex":0.15974379,"about_ca_topic_score_gemma":0.9954042,"teacher_disagreement_score":0.8356604,"about_ca_system_score_codex":0.0000015446215,"about_ca_system_score_gemma":0.00079053617,"threshold_uncertainty_score":0.999924},"labels":[],"label_agreement":null},{"id":"W4414593475","doi":"10.1139/cjes-2025-0013","title":"Cretaceous strike–slip displacement along the Porcupine fault system and potential links to the opening of the Canada Basin","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon University","funders":"National Science Foundation Graduate Research Fellowship Program","keywords":"Fault (geology); Terrane; Cretaceous; Fault scarp; Devonian; Arctic; Tectonics; Sinistral and dextral; Structural basin; Deformation (meteorology)","score_opus":0.012959141635880902,"score_gpt":0.19340782585927963,"score_spread":0.18044868422339871,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414593475","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96413434,0.0019645367,0.000093730705,0.031218816,0.001103719,0.00017417231,0.000027747737,9.824139e-7,0.0012819392],"genre_scores_gemma":[0.99869025,0.000024342657,0.000051459137,0.0010017712,0.00007042194,3.5804246e-7,5.692169e-7,5.120805e-7,0.00016032056],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989658,0.000109233144,0.0002599654,0.00010221537,0.00031864378,0.0002441419],"domain_scores_gemma":[0.99938923,0.00011100608,0.0001476503,0.00009331972,0.000092730144,0.00016603412],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009970482,0.000072116665,0.00012992104,0.000045409182,0.0012179969,0.00014560735,0.00051436474,0.000026541777,0.000097638054],"category_scores_gemma":[0.00015643673,0.000028619597,0.00003697605,0.00043816853,0.0002652752,0.00008696483,0.000022005757,0.00015524,0.0000010309137],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018913042,0.0000017356816,0.84410775,0.000016458367,0.0000341433,0.000029661478,0.0006064417,0.138944,0.0000073761144,0.00034179538,0.00469603,0.011195665],"study_design_scores_gemma":[0.00009372141,0.00013343639,0.95206136,0.000088710054,0.000022791393,0.000042328866,0.006735757,0.00464177,0.00002598864,0.000032794345,0.036066417,0.000054931737],"about_ca_topic_score_codex":0.7555679,"about_ca_topic_score_gemma":0.99543726,"teacher_disagreement_score":0.23986936,"about_ca_system_score_codex":0.000005816064,"about_ca_system_score_gemma":0.001284682,"threshold_uncertainty_score":0.9367971},"labels":[],"label_agreement":null},{"id":"W4414763113","doi":"10.1139/cjes-2024-0129","title":"Structural, geochronological, and metamorphic discontinuities across the Monashee décollement, southern British Columbia, Canada","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Allochthon; Precambrian; Shear zone; Imbrication; Metamorphic rock; Thrust fault; Shear (geology); Classification of discontinuities; Main Central Thrust; Basement","score_opus":0.018497530467021912,"score_gpt":0.2282068261684241,"score_spread":0.2097092957014022,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414763113","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9873487,0.006713717,9.009622e-7,0.0030056017,0.000466909,0.000092857794,0.0001403912,0.0000021198127,0.0022288444],"genre_scores_gemma":[0.9965279,0.00008177665,0.000055535642,0.0006314411,0.000041472216,4.6730395e-7,0.0000026123816,7.7721046e-7,0.0026580251],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986536,0.00014465091,0.0002612048,0.00017080852,0.00020178097,0.00056798954],"domain_scores_gemma":[0.9991278,0.0003009354,0.00011597734,0.00009083716,0.00009517235,0.00026924352],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00097070145,0.00007683003,0.00020721897,0.000059156904,0.0019353468,0.00069298135,0.0005765396,0.000059001522,0.002779389],"category_scores_gemma":[0.00021246857,0.000062045634,0.000040876046,0.0003228669,0.0023164933,0.0001682965,0.00001612993,0.00028640966,0.000004541866],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000022511354,5.3349646e-7,0.99711066,0.000004547808,0.000023572458,0.00011489259,0.00014821273,0.000106455365,3.6669198e-7,0.00002273553,0.000897755,0.0015679983],"study_design_scores_gemma":[0.0001469216,0.00007630057,0.9872462,0.000023436762,0.000010869044,0.00034539914,0.0042311065,0.00014488432,0.0000016610461,0.001293966,0.006406587,0.00007265244],"about_ca_topic_score_codex":0.98142517,"about_ca_topic_score_gemma":0.99999124,"teacher_disagreement_score":0.018566096,"about_ca_system_score_codex":0.0000010723003,"about_ca_system_score_gemma":0.0033959872,"threshold_uncertainty_score":0.999364},"labels":[],"label_agreement":null},{"id":"W4415486671","doi":"10.1139/cjes-2025-0027","title":"Extending the western Hudson Bay Lowland Quaternary stratigraphy, in Manitoba Canada, to at least Marine Isotope Stage 10","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Isotope Analysis in Ecology","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Manitoba Hydro; University of the Fraser Valley; University of Toronto; University of Waterloo","funders":"Commission Géologique du Canada","keywords":"Interglacial; Glacial period; Marine isotope stage; Quaternary; Stage (stratigraphy); Bay; Radiocarbon dating; Stratigraphy; Boreal; Ice sheet","score_opus":0.0130446299740771,"score_gpt":0.22513072920162117,"score_spread":0.21208609922754407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415486671","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9793182,0.000086632775,0.000027260949,0.0030686934,0.00037147518,0.00012190826,0.000006716679,0.0000013527055,0.016997784],"genre_scores_gemma":[0.9901602,0.000011480716,0.00019991604,0.0013760264,0.000033376866,0.0000023876444,4.4875932e-7,0.0000034095174,0.008212703],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99849147,0.000106886604,0.00036441922,0.00022077437,0.00033258568,0.00048386943],"domain_scores_gemma":[0.9992609,0.00008347169,0.00013850251,0.00017523557,0.000019614987,0.00032227725],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009005657,0.00011812767,0.00019068489,0.0002996416,0.00040882715,0.0001145175,0.00088789506,0.000033021795,0.0031398041],"category_scores_gemma":[0.00007878845,0.00008398424,0.000050991937,0.0009023418,0.00038127543,0.00023246827,0.000117307995,0.0001717246,0.000043359873],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000061989986,0.0000038869302,0.9913083,0.0000018059169,0.000008055355,0.00018303076,0.00011145443,0.0041821892,0.00008769618,0.000042588632,0.002084479,0.001980348],"study_design_scores_gemma":[0.00011794848,0.00008963792,0.9580544,0.000025269937,0.000007840152,0.00003082848,0.0004849483,0.00029604317,0.00014285085,0.000073041825,0.04058297,0.0000942243],"about_ca_topic_score_codex":0.87783474,"about_ca_topic_score_gemma":0.9999373,"teacher_disagreement_score":0.122102566,"about_ca_system_score_codex":0.00015996798,"about_ca_system_score_gemma":0.00090005447,"threshold_uncertainty_score":0.99777144},"labels":[],"label_agreement":null},{"id":"W4415529211","doi":"10.1139/cjes-2025-0016","title":"Silurian mafic magmatism related to post-collisional extension, Appalachian orogen, western Newfoundland","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Government of Newfoundland and Labrador","funders":"","keywords":"Silicic; Zircon; Magmatism; Mafic; Petrogenesis; Fractional crystallization (geology); Gabbro; Igneous differentiation; Anatexis; Lithosphere","score_opus":0.009458294232488378,"score_gpt":0.2107143807533818,"score_spread":0.20125608652089344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415529211","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97945327,0.0011274548,0.000043264805,0.012916407,0.0005463431,0.00008320484,0.00003602476,0.000006659197,0.0057873474],"genre_scores_gemma":[0.99474734,0.00001324173,0.0013458247,0.0026052427,0.000051507865,2.037089e-7,0.000010363614,0.0000012503784,0.0012250207],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983033,0.0000836782,0.00047966014,0.00027659544,0.00036399794,0.0004927519],"domain_scores_gemma":[0.998295,0.00015336878,0.00014041946,0.00013184648,0.00025953332,0.001019822],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00076778536,0.00014663691,0.00028536323,0.00058549765,0.0005249406,0.00022966528,0.0005977498,0.000079439895,0.0067839306],"category_scores_gemma":[0.0003758889,0.00009715925,0.00013852144,0.0014030683,0.0003574619,0.00025325254,0.000013298682,0.00021827567,0.00029942184],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011247885,0.0000056172566,0.98899424,0.0000036442736,0.000022092914,0.0000984237,0.000087554174,0.005094355,0.0000908044,0.00031201524,0.00026794508,0.005012037],"study_design_scores_gemma":[0.00015524669,0.00023219312,0.9790349,0.000064955864,0.000025635136,0.00010994399,0.00017455622,0.00084939145,0.000028928189,0.009752094,0.009436949,0.00013521056],"about_ca_topic_score_codex":0.038583633,"about_ca_topic_score_gemma":0.8007171,"teacher_disagreement_score":0.7621335,"about_ca_system_score_codex":0.0000032144953,"about_ca_system_score_gemma":0.0009773435,"threshold_uncertainty_score":0.994124},"labels":[],"label_agreement":null},{"id":"W4415598806","doi":"10.1139/cjes-2024-0174","title":"Research on the enrichment and mineralization of Nb–Ta elements in alkaline rhyolite of the Early Cretaceous Toudaoqiao deposit, the Great Xing'an Range","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Geochronology of Asian Mineral Deposits","field":"Economics, Econometrics and Finance","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Mineralization (soil science); Rhyolite; Zircon; Partial melting; Mantle (geology); Magmatism; Asthenosphere; Igneous differentiation; Cretaceous","score_opus":0.04294984724954679,"score_gpt":0.26865509016999206,"score_spread":0.22570524292044528,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415598806","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9861769,0.002485143,0.000009900306,0.0054066763,0.0001317547,0.00011739432,0.000014331597,4.250405e-7,0.005657459],"genre_scores_gemma":[0.99899626,0.0000775337,0.000063578904,0.00018260251,0.000025697009,0.0000016574035,4.2920584e-7,0.0000016966768,0.00065053254],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99902004,0.00008810608,0.00043551705,0.00013309786,0.00008623852,0.00023700975],"domain_scores_gemma":[0.99929345,0.000098198165,0.00026360137,0.00017670583,0.00009349766,0.00007457414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019934068,0.00006451125,0.00016153757,0.0002819586,0.0002943179,0.00006405011,0.0005056985,0.000043199805,0.00005609789],"category_scores_gemma":[0.00019964066,0.000038092352,0.00004376324,0.0006676903,0.0005632144,0.00011040289,0.000029944895,0.00018252619,0.0000015884638],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023104318,0.000025503345,0.9712692,0.00002184651,0.00003197344,0.000008156313,0.0011068892,0.0006105849,0.00075689115,0.02512223,0.00042715625,0.00059649907],"study_design_scores_gemma":[0.0003333208,0.00026989143,0.98748416,0.00013787401,0.0000063243338,0.000015629688,0.0004826899,0.00052013807,0.0020514706,0.006307687,0.0023313991,0.000059391925],"about_ca_topic_score_codex":0.008975808,"about_ca_topic_score_gemma":0.05731364,"teacher_disagreement_score":0.048337832,"about_ca_system_score_codex":0.000013734836,"about_ca_system_score_gemma":0.00018869097,"threshold_uncertainty_score":0.9976235},"labels":[],"label_agreement":null},{"id":"W4416075358","doi":"10.1139/cjes-2024-0164","title":"Assessing recent shoreline change in northeastern Haida Gwaii, BC","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; Queen's University","funders":"","keywords":"Shore; Coastal erosion; Storm; Overwash; Erosion; Climate change; Barrier island; Foredune; Aggradation","score_opus":0.03598736170149952,"score_gpt":0.25598947058912536,"score_spread":0.22000210888762584,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416075358","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97452056,0.0013823884,0.00007400791,0.0034646897,0.0013078388,0.00007901343,0.000014114349,0.0000033918816,0.01915398],"genre_scores_gemma":[0.99837637,0.00012178776,0.00051363,0.0006274828,0.0001119232,1.6902796e-7,0.000005268647,0.0000010651249,0.00024231797],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989451,0.000047034966,0.00030353715,0.0001397158,0.00019605884,0.00036855365],"domain_scores_gemma":[0.9993475,0.000060957984,0.00010496175,0.00007052354,0.00009108324,0.00032494287],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007716425,0.00009049704,0.00016140174,0.0005840579,0.00019886708,0.00027524878,0.0003436356,0.000036005276,0.0009688621],"category_scores_gemma":[0.000095580304,0.00006984871,0.00004342292,0.0009154417,0.00021184848,0.0007152665,0.000009771122,0.00018290564,0.000012319648],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000030390163,0.0000025661043,0.7531371,0.000003873086,0.0000021741112,0.00006010969,0.00010145922,0.0008463783,0.0000010659993,0.00006184555,0.00001892247,0.24576145],"study_design_scores_gemma":[0.0001376579,0.00009508806,0.962167,0.000112590256,0.0000048600623,0.000036201487,0.00040871787,0.012817767,0.000003247752,0.00061168126,0.023517571,0.00008756516],"about_ca_topic_score_codex":0.1257599,"about_ca_topic_score_gemma":0.9708127,"teacher_disagreement_score":0.8450528,"about_ca_system_score_codex":0.000003545298,"about_ca_system_score_gemma":0.0014238739,"threshold_uncertainty_score":0.9999444},"labels":[],"label_agreement":null},{"id":"W4416887731","doi":"10.1139/cjes-2025-0054","title":"Cambrian linguliformean brachiopods of the Pika and Sullivan Formations (Miaolingian), southern Rocky Mountains, Alberta, Canada","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Trilobite; Grainstone; Biozone; Fauna; Ordovician; Laurentia; Ammonite; Refugium (fishkeeping)","score_opus":0.007649608156355806,"score_gpt":0.1961564723127967,"score_spread":0.18850686415644088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416887731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.956,0.0029221051,0.000018103776,0.0013844514,0.00055896095,0.000065883425,0.000084431835,0.0000011732093,0.03896491],"genre_scores_gemma":[0.99927217,0.000014173129,0.0001892291,0.00025113288,0.000035838875,8.023298e-8,8.750195e-7,4.2303205e-7,0.00023605605],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898076,0.00006658571,0.0003409031,0.00010189597,0.00020188824,0.0003079595],"domain_scores_gemma":[0.9991095,0.00017624458,0.00022979222,0.0001001533,0.00008642784,0.00029790087],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000469517,0.00009448816,0.00016899333,0.0002124316,0.00082315877,0.00007661828,0.00046320303,0.000050935832,0.000071893264],"category_scores_gemma":[0.00020319865,0.00006211094,0.00006455125,0.00044282185,0.0006006946,0.00022241716,0.0000018176027,0.00018602065,5.028737e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000034962547,0.0000012070349,0.9926616,0.000007827239,0.000015974312,0.000004724973,0.00066232984,0.000326393,0.000003455208,0.00039491677,0.000058527927,0.0058595324],"study_design_scores_gemma":[0.00011542229,0.0000564361,0.9943323,0.0000638864,0.00001714937,0.000057230194,0.002074414,0.0006430836,0.000035637717,0.00046249665,0.002071275,0.00007065241],"about_ca_topic_score_codex":0.9154031,"about_ca_topic_score_gemma":0.9999072,"teacher_disagreement_score":0.084504075,"about_ca_system_score_codex":0.000002497614,"about_ca_system_score_gemma":0.005561211,"threshold_uncertainty_score":0.986535},"labels":[],"label_agreement":null},{"id":"W4416887792","doi":"10.1139/cjes-2025-0051","title":"Holocene tephrochronology in the Northern Cordilleran Volcanic Province, northwestern British Columbia","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; University of Alberta","keywords":"Tephra; Tephrochronology; Volcano; Holocene; Basalt; Volcanic hazards; Volcanic glass; Rhyolite; Chronology","score_opus":0.008426466331752003,"score_gpt":0.182108806906908,"score_spread":0.173682340575156,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416887792","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98909044,0.0015017849,0.000009123665,0.0014885258,0.00020645159,0.00007696943,0.000019705709,0.000002892421,0.00760412],"genre_scores_gemma":[0.9980472,0.000034059678,0.00008379092,0.0013766594,0.000054205593,3.43656e-7,0.0000043760197,6.7612757e-7,0.0003986938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99870044,0.00010815623,0.00034561552,0.0001935951,0.00021259605,0.0004395992],"domain_scores_gemma":[0.9993113,0.00014266658,0.00012739829,0.00010018813,0.00009804389,0.00022039065],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006957121,0.00007765851,0.00022114391,0.00016290293,0.00039592793,0.00031010783,0.00081398146,0.000057990994,0.0033301995],"category_scores_gemma":[0.00012299501,0.000062821804,0.00009408546,0.0010393194,0.00081680395,0.00017300904,0.000007208889,0.00025094106,0.000027898237],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000002154468,0.0000063449042,0.98688644,0.0000029390822,0.000008714006,0.00018004335,0.00004784571,0.00073420594,0.0000012211322,0.000007541952,0.00021669533,0.011905878],"study_design_scores_gemma":[0.00015116445,0.0001770102,0.99181145,0.00003157981,0.000013511693,0.00013687789,0.00037573534,0.00033561912,0.0000021253813,0.0028105902,0.004073541,0.000080774706],"about_ca_topic_score_codex":0.7111168,"about_ca_topic_score_gemma":0.9996771,"teacher_disagreement_score":0.28856033,"about_ca_system_score_codex":0.0000026798268,"about_ca_system_score_gemma":0.0013525627,"threshold_uncertainty_score":0.9975809},"labels":[],"label_agreement":null},{"id":"W4417062586","doi":"10.1139/cjes-2025-0012","title":"Receiver function insights into crust and lithospheric fabric in Northern Canada","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Manitoba","funders":"","keywords":"Receiver function; Lithosphere; Bouguer anomaly; Crust; Upper crust; Density contrast; Inversion (geology); Tectonics","score_opus":0.0061971136088881515,"score_gpt":0.17478840042950633,"score_spread":0.1685912868206182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417062586","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99156505,0.0027859877,0.000015770589,0.00040862325,0.0012375015,0.000047025358,0.0000050194617,0.0000013517702,0.003933687],"genre_scores_gemma":[0.9992498,0.00005257271,0.00012328081,0.00029890612,0.000062878076,1.2749858e-7,0.0000012761739,8.7868267e-7,0.00021023511],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992171,0.000052815412,0.00021833013,0.00012844539,0.00016062384,0.00022268317],"domain_scores_gemma":[0.9994726,0.00005457683,0.00009482581,0.00005627173,0.00007127214,0.00025042225],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029663419,0.000076845805,0.00015157992,0.00017142398,0.00025059047,0.00013390489,0.00018961087,0.000030661795,0.0002571354],"category_scores_gemma":[0.000052595904,0.000058290938,0.000016873812,0.000561663,0.00015962153,0.00028027457,0.0000038084547,0.00008680048,0.0000046924333],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009441812,0.0000017657587,0.98357207,0.00001148687,0.000009405989,0.00005563317,0.00035609058,0.002806717,0.00004675366,0.0001811352,0.00038940477,0.012560116],"study_design_scores_gemma":[0.00011130383,0.00008155508,0.9528518,0.000046094323,0.000007224925,0.000005422722,0.00031213116,0.00025940867,0.000039810882,0.0015638226,0.044646844,0.00007458616],"about_ca_topic_score_codex":0.9494336,"about_ca_topic_score_gemma":0.999757,"teacher_disagreement_score":0.050323386,"about_ca_system_score_codex":0.00000450969,"about_ca_system_score_gemma":0.0033871008,"threshold_uncertainty_score":0.60085714},"labels":[],"label_agreement":null},{"id":"W4417209351","doi":"10.1139/cjes-2025-0044","title":"New Middle Cambrian (Drumian) U-Pb age of Cape Breton Island volcanism and Cambrian–lowest Ordovician stratigraphic reevaluation confirm the Bourinot belt (southern “Bras d’Or terrane”) is Avalonian","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ordovician; Proterozoic; Terrane; Volcano; Trilobite; Lithostratigraphy; Precambrian; Sequence (biology); Chemostratigraphy","score_opus":0.029478750832469206,"score_gpt":0.23810219396333338,"score_spread":0.20862344313086417,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417209351","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96484315,0.007235025,0.00009044173,0.003445277,0.00067978963,0.0002329871,0.00017615645,0.000005622228,0.023291571],"genre_scores_gemma":[0.99796635,0.00007448753,0.00046407967,0.0004770117,0.00012244072,3.681128e-7,0.0000046757773,0.0000016203163,0.0008889952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99792814,0.00021710992,0.0006005827,0.00029550956,0.00042546316,0.0005331951],"domain_scores_gemma":[0.99846196,0.0001910493,0.00039891212,0.00021597723,0.00013939757,0.0005927002],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001324601,0.00022023107,0.00037502366,0.00056457485,0.0009488165,0.00028755466,0.0006595004,0.00014917227,0.00069404376],"category_scores_gemma":[0.00013677643,0.00014447572,0.00013129911,0.00079148024,0.0014023612,0.00037294437,0.0000026622956,0.0003390187,0.000004557278],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000050905794,0.000005635848,0.96665156,0.000025552852,0.000064315594,0.00011757525,0.003610211,0.000034619115,0.00016667155,0.0004167815,0.0002798084,0.02857635],"study_design_scores_gemma":[0.00048527148,0.00052828057,0.9929515,0.00015977447,0.00007567047,0.00017184972,0.0023841115,0.00028510898,0.00009426252,0.0010968961,0.0015983355,0.00016894237],"about_ca_topic_score_codex":0.17989057,"about_ca_topic_score_gemma":0.9879675,"teacher_disagreement_score":0.8080769,"about_ca_system_score_codex":0.0000026096711,"about_ca_system_score_gemma":0.0040992713,"threshold_uncertainty_score":0.8255706},"labels":[],"label_agreement":null},{"id":"W630960179","doi":"10.1139/e08-055","title":"Geochemistry of the Lower Cretaceous Chaswood Formation, Nova Scotia, Canada: provenance and diagenesisGeological Survey of Canada Contribution 20080004.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Bedford Institute of Oceanography; Geological Survey of Canada","funders":"","keywords":"Geology; Geochemistry; Zircon; Basement; Unconformity; Provenance; Clastic rock; Mafic; Heavy mineral; Diagenesis; Cretaceous; Sedimentary rock; Paleontology; Archaeology","score_opus":0.014149313809790075,"score_gpt":0.1724930559767948,"score_spread":0.15834374216700473,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W630960179","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99666435,0.0017622925,0.0000054708603,0.0005058426,0.00019247699,0.000046517427,0.00028894722,4.4876325e-7,0.00053363864],"genre_scores_gemma":[0.9997452,0.000024770825,0.000027561515,0.00009408584,0.000021256492,5.4536397e-8,0.000011192604,5.987118e-7,0.00007530431],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99877125,0.000057883983,0.00037958956,0.000105248895,0.00039988424,0.0002861703],"domain_scores_gemma":[0.998818,0.00009057554,0.00039078007,0.00008778358,0.0003247085,0.0002882018],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058019854,0.00008634261,0.00020948218,0.000034370914,0.0003134666,0.000013605242,0.00031696717,0.00003468747,0.00062914734],"category_scores_gemma":[0.00040859933,0.00005627086,0.000038929527,0.00043088238,0.00054924446,0.00014454217,0.0000066887715,0.00009573633,2.7165876e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007652979,0.0000037516309,0.99724597,0.000010459572,0.000012485451,0.000025984124,0.00002850629,0.0014937484,0.00011519768,0.0000017812887,0.00091410306,0.00014036067],"study_design_scores_gemma":[0.000112108224,0.00006915315,0.98868644,0.000027505792,0.0000107279575,0.00019465365,0.00010502644,0.0004895814,0.009858328,0.000017953169,0.00035713552,0.00007136423],"about_ca_topic_score_codex":0.9960526,"about_ca_topic_score_gemma":0.99995875,"teacher_disagreement_score":0.009743131,"about_ca_system_score_codex":0.000008747055,"about_ca_system_score_gemma":0.007562385,"threshold_uncertainty_score":0.9980638},"labels":[],"label_agreement":null},{"id":"W7106794162","doi":"10.1139/cjes-2025-0088","title":"New U–Pb geochronological constraints on the tectono-magmatic evolution of the Chibougamau–Chapais region, northeastern Abitibi greenstone belt, Québec","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Toronto; Université du Québec à Chicoutimi","funders":"","keywords":"Felsic; Mafic; Magmatism; Diorite; Greenstone belt; Craton; Archean; Volcano; Intrusion","score_opus":0.01345738195892652,"score_gpt":0.1860240287690737,"score_spread":0.1725666468101472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7106794162","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9621717,0.0010961028,0.00026711117,0.024596704,0.00025361005,0.00009920895,0.000012423574,0.000003842697,0.011499333],"genre_scores_gemma":[0.99856263,0.00000984576,0.00016472737,0.0008468931,0.00006580762,1.925668e-7,8.062604e-7,7.042437e-7,0.00034841002],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986131,0.00012521567,0.00040699096,0.00018091754,0.000323222,0.00035051684],"domain_scores_gemma":[0.9987746,0.00033954388,0.0002748819,0.00017725307,0.00012771736,0.00030601924],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005792863,0.00012656463,0.00024411561,0.00018430936,0.0005343345,0.000060775626,0.0008116171,0.000063794985,0.003946002],"category_scores_gemma":[0.0005754248,0.000056622626,0.00019796749,0.00092277705,0.0020298895,0.0001028177,0.000014354565,0.00028108378,0.000029551802],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010423343,0.0000076963925,0.9711358,0.00000593926,0.000032672342,0.000013451345,0.00008518012,0.0016414191,0.000059918497,0.0019124638,0.0004966478,0.024598416],"study_design_scores_gemma":[0.00011419203,0.00020125035,0.98542416,0.00010863221,0.000033403318,0.00006258931,0.00030538184,0.0007016158,0.000097686134,0.012062226,0.000810682,0.00007820709],"about_ca_topic_score_codex":0.4308284,"about_ca_topic_score_gemma":0.9633181,"teacher_disagreement_score":0.5324897,"about_ca_system_score_codex":0.000007651006,"about_ca_system_score_gemma":0.0024602537,"threshold_uncertainty_score":0.9969645},"labels":[],"label_agreement":null},{"id":"W7116794789","doi":"10.1139/cjes-2025-0091","title":"Mechanical and anisotropic properties of the Duvernay Formation","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Hydraulic Fracturing and Reservoir Analysis","field":"Engineering","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Waterloo","funders":"","keywords":"Anisotropy; Transverse isotropy; Core (optical fiber); Isotropy; Oil shale; Hydraulic fracturing; Directional drilling; Drilling; Core sample","score_opus":0.011184352497398308,"score_gpt":0.19055787289886855,"score_spread":0.17937352040147025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7116794789","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99608237,0.0013135786,0.000601073,0.00073254143,0.00020864318,0.000018277022,5.7304163e-7,0.000001998233,0.0010409533],"genre_scores_gemma":[0.9997266,0.000044441655,0.00008626221,0.000031917574,0.000013866477,1.2594684e-7,1.2923254e-8,8.6080155e-7,0.00009591142],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9996655,0.000013645412,0.00012666482,0.000025397283,0.00008532869,0.00008344044],"domain_scores_gemma":[0.9998192,0.000008094414,0.000032482374,0.000042308067,0.00003289279,0.00006498576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016608564,0.000029558767,0.00006887057,0.000116089905,0.00011014935,0.000034102304,0.00015174269,0.000017369783,0.000008420909],"category_scores_gemma":[0.000053161497,0.000016148057,0.00003284657,0.00020454232,0.00011724727,0.00012315331,0.00000544263,0.00006479792,3.248868e-7],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010581354,0.000016287462,0.0625724,0.00059232506,0.00031350012,0.000026503718,0.0044821696,0.8685515,0.03974465,0.0036719819,0.0029902635,0.017027855],"study_design_scores_gemma":[0.0007958075,0.00025149097,0.22721846,0.001903535,0.00019264939,0.0001740507,0.0031989347,0.26898336,0.44972706,0.0028437078,0.04433014,0.00038080665],"about_ca_topic_score_codex":0.0006309146,"about_ca_topic_score_gemma":0.018320922,"teacher_disagreement_score":0.5995681,"about_ca_system_score_codex":0.000004294618,"about_ca_system_score_gemma":0.00018244106,"threshold_uncertainty_score":0.9995922},"labels":[],"label_agreement":null},{"id":"W787789143","doi":"10.1139/e07-072","title":"Quaternary stratigraphy of the Prophet River, northeastern British ColumbiaThis article is one of a selection of papers published in this Special Issue on the theme <i>Geology of northeastern British Columbia and northwestern Alberta: diamonds, shallow gas, gravel, and glaciers</i>.","year":2008,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"British Geological Survey; University of Victoria","keywords":"Geology; Glacial period; Quaternary; Radiocarbon dating; Deglaciation; Fluvial; Moraine; Silt; Wisconsin glaciation; Glacial lake; Floodplain; Paleontology; Macrofossil; Geomorphology; Archaeology; Holocene; Oceanography; Structural basin; Ice stream","score_opus":0.012367846802528509,"score_gpt":0.18431988703143162,"score_spread":0.17195204022890312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W787789143","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99528694,0.0007550035,2.0285444e-7,0.0005176505,0.00017213302,0.00022100036,0.000061914274,8.866734e-7,0.0029842937],"genre_scores_gemma":[0.9991958,0.00024442837,0.000045788427,0.00010787185,0.00006413198,7.513968e-7,0.0000017383925,0.0000023753573,0.00033712454],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99813104,0.00030010004,0.000573035,0.00022899365,0.0003960615,0.00037078193],"domain_scores_gemma":[0.9987068,0.00027235635,0.00047216602,0.00013013986,0.0002047308,0.00021376563],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007904153,0.000095951575,0.00040141275,0.00013491615,0.00056210643,0.0001459837,0.00044469,0.00010650848,0.0029643485],"category_scores_gemma":[0.0001330253,0.00008926169,0.00008642682,0.00064096734,0.0039000213,0.0002725758,0.000014691406,0.00028735283,0.0000011118793],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003702525,0.000029160545,0.9967015,0.000030902705,0.000034167173,0.000037472306,0.0017485401,0.000040900253,0.000024675073,0.0000040937466,0.00009142235,0.001220183],"study_design_scores_gemma":[0.0004153655,0.00080653996,0.9964545,0.00013871063,0.000015734746,0.0006879045,0.00054252945,0.0002627654,0.00010447366,0.0003517393,0.0001397993,0.00007995574],"about_ca_topic_score_codex":0.7145018,"about_ca_topic_score_gemma":0.99836737,"teacher_disagreement_score":0.28386554,"about_ca_system_score_codex":8.458444e-7,"about_ca_system_score_gemma":0.00064708694,"threshold_uncertainty_score":0.99881077},"labels":[],"label_agreement":null},{"id":"W853253482","doi":"10.1139/cjes-2015-0237","title":"Hydrothermal alteration and lithogeochemistry of the Boundary volcanogenic massive sulphide deposit, central Newfoundland, Canada","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Memorial University of Newfoundland","keywords":"Sericite; Chlorite; Felsic; Geology; Geochemistry; Hydrothermal circulation; Pyrite; Rhyolite; Mineralogy; Mafic; Quartz; Volcanic rock; Volcano","score_opus":0.006635962087201843,"score_gpt":0.16423178201193414,"score_spread":0.1575958199247323,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W853253482","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946991,0.0011586547,0.0000151201775,0.0030345172,0.00018148516,0.00003057896,0.000059454913,8.10417e-7,0.0008202351],"genre_scores_gemma":[0.99943274,0.000024188563,0.00010252261,0.00023779573,0.000083734216,7.324882e-8,0.0000012511221,6.7071255e-7,0.00011700153],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99901867,0.00004742129,0.00024209317,0.00012075769,0.00026185217,0.00030919505],"domain_scores_gemma":[0.9991444,0.00009779883,0.00017817545,0.00007157878,0.00007596265,0.00043208056],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019763368,0.000080027385,0.00013903875,0.00004348845,0.00027925996,0.00005768715,0.00030298863,0.000031019274,0.0015127482],"category_scores_gemma":[0.00013995258,0.00003718615,0.00006519664,0.00022548629,0.00061218685,0.00015495463,0.0000064060755,0.00007869893,0.0000013208294],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000055467285,0.0000011359434,0.9956407,0.0000031086536,0.000012578367,0.000020997417,0.000027619693,0.00026860446,0.0016749973,0.00002102073,0.00005401221,0.0022696878],"study_design_scores_gemma":[0.0001264803,0.00006240435,0.9910923,0.00003763488,0.000018472798,0.000118503456,0.0000511557,0.00033145418,0.0053491495,0.0012931342,0.0014440881,0.000075192256],"about_ca_topic_score_codex":0.81021535,"about_ca_topic_score_gemma":0.99698573,"teacher_disagreement_score":0.18677042,"about_ca_system_score_codex":0.000005128127,"about_ca_system_score_gemma":0.002055183,"threshold_uncertainty_score":0.9994},"labels":[],"label_agreement":null}]}